{"meta":{"query_hash":"e1e3faccad0c","filters":{"venue":"Lithosphere"},"cohort_total":99,"direct_labels_cover":0,"predictions_cover":99,"exported":99,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/e1e3faccad0c","api":"https://metacan.xera.ac/api/v1/cohort?venue=Lithosphere"},"results":[{"id":"W1971953156","doi":"10.1130/l154.1","title":"Rapid synconvergent exhumation of Miocene-aged lower orogenic crust in the eastern Himalaya","year":2011,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":176,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Royal Government of Bhutan; Natural Environment Research Council; Killam Trusts; Dalhousie University; Sight Research UK","keywords":"Geology; Granulite; Zircon; Eclogite; Geochemistry; Metamorphism; Protolith; Crust; Mafic; Continental crust; Subduction; Continental collision; Petrology; Tectonics; Facies; Seismology; Paleontology; Structural basin","score_opus":0.02903569337919184,"score_gpt":0.1886564079169326,"score_spread":0.15962071453774077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971953156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991647,0.000112327194,0.000082392995,0.00001066359,5.9726705e-7,0.0000013290271,0.000048758815,0.000005233929,0.00057393446],"genre_scores_gemma":[0.99960834,0.00009753113,0.00006516409,0.0000057803163,0.0000018042829,6.399438e-7,0.00005991706,0.0000015724468,0.00015920083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999342,0.000007059054,0.000006675123,0.000020267906,0.000015440624,0.000016243806],"domain_scores_gemma":[0.9999051,0.000012989057,0.0000379423,0.0000128624715,0.00001509979,0.000015961794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013300122,0.00013842425,0.000102798775,0.00089760707,0.00034530342,0.0005453632,0.00015861368,0.00012873394,0.0008939404],"category_scores_gemma":[0.00028231303,0.0001524751,0.00010608094,0.0006823936,0.00037045265,0.00023333622,0.0003829846,0.00013382672,0.0001605847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012087711,0.000011998213,0.9329888,0.000054414824,0.00006051021,0.00086373714,0.0021077984,0.0007233334,0.046664998,0.00025356156,0.000055554723,0.016094515],"study_design_scores_gemma":[0.0000010491872,0.0000072032844,0.9988405,0.0000015574362,0.0000056145263,0.00009614836,0.0001284224,0.00012745765,0.000625202,0.000014584349,0.00015088914,0.0000013347158],"about_ca_topic_score_codex":0.013501185,"about_ca_topic_score_gemma":0.018810913,"teacher_disagreement_score":0.013501185,"about_ca_system_score_codex":0.0004097803,"about_ca_system_score_gemma":0.00016256596,"threshold_uncertainty_score":0.026845217},"labels":[],"label_agreement":null},{"id":"W1976529238","doi":"10.1130/l335.1","title":"U-Pb geochronology of 1.1 Ga diabase in the southwestern United States: Testing models for the origin of a post-Grenville large igneous province","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; Frontier Geosciences (Canada)","funders":"","keywords":"Geochronology; Geology; Igneous rock; Geochemistry; Seismology","score_opus":0.018069339038584785,"score_gpt":0.2076656262932273,"score_spread":0.1895962872546425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976529238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988398,0.000050440234,0.00007420749,0.000024691299,0.0000010815955,0.0000030361186,0.00031523526,0.00000835697,0.000683158],"genre_scores_gemma":[0.99910694,0.000047405432,0.00026038673,0.000011090826,0.0000011245005,0.0000030916408,0.00042033847,0.0000027174676,0.00014696187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000061857,0.0000028660043,0.000017753395,0.000007989027,0.000008430799],"domain_scores_gemma":[0.99981576,0.00003213719,0.000050525887,0.00001927058,0.000053727625,0.00002858794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021145125,0.00012545577,0.000103633014,0.0007008283,0.00043574208,0.00035911062,0.00029869398,0.00016156382,0.0006314119],"category_scores_gemma":[0.00042290078,0.00013091229,0.00012155278,0.00053683895,0.00020823423,0.00020611253,0.00027481338,0.00019617852,0.00007924989],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006459583,0.000016695112,0.99027175,0.000008236062,0.00001778591,0.00008424427,0.00031296216,0.0005989849,0.0041610477,0.000108021995,0.00016579784,0.004189898],"study_design_scores_gemma":[0.0000034946045,0.0000075270605,0.9982475,0.000003850985,0.0000076214833,0.000022553537,0.00011818967,0.0008412738,0.00041257992,0.000016372454,0.0003178741,0.0000013019537],"about_ca_topic_score_codex":0.20397414,"about_ca_topic_score_gemma":0.44157848,"teacher_disagreement_score":0.20397414,"about_ca_system_score_codex":0.0011914616,"about_ca_system_score_gemma":0.00039235415,"threshold_uncertainty_score":0.40557373},"labels":[],"label_agreement":null},{"id":"W2002823043","doi":"10.1130/l414.1","title":"Effects of Paleogene faults on the reconstruction of the metamorphic history of the northwestern Thor-Odin culmination of the Monashee complex, southeastern British Columbia","year":2015,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; University of New Brunswick","funders":"","keywords":"Culmination; Geology; Paleogene; Context (archaeology); Metamorphism; Fault (geology); Metamorphic rock; Paleontology; Monazite; Seismology; Cretaceous","score_opus":0.017719611215683773,"score_gpt":0.16683562002673785,"score_spread":0.14911600881105408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002823043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99833494,0.00008407639,0.00009197371,0.000033005457,0.0000010986826,0.0000030959266,0.0002338696,0.000008041679,0.0012099838],"genre_scores_gemma":[0.9993777,0.00004419065,0.00012537657,0.0000044711187,4.247427e-7,0.0000010590982,0.0001421124,0.0000022985932,0.00030218996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998118,0.000029800607,0.000011192229,0.000047260557,0.000043438722,0.000056511017],"domain_scores_gemma":[0.99966276,0.000052780095,0.000050521336,0.00002425164,0.00015203805,0.000057631732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023358128,0.00016480454,0.00013287483,0.001054808,0.0011438564,0.0012108687,0.00029279277,0.00017305388,0.0018522674],"category_scores_gemma":[0.0012728259,0.00013715937,0.00017954099,0.0013864738,0.0004855183,0.00015451963,0.0004253458,0.00018687626,0.00014302251],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013509895,0.000013062726,0.971016,0.000023356932,0.000050168186,0.00013828294,0.00062413886,0.00436703,0.003677771,0.00045324283,0.00024414035,0.019257762],"study_design_scores_gemma":[0.0000025237164,0.0000044350763,0.9957653,0.0000104777755,0.000012207998,0.00002577509,0.00048340127,0.0028318216,0.00030189176,0.000028749231,0.0005296741,0.0000038057187],"about_ca_topic_score_codex":0.93919396,"about_ca_topic_score_gemma":0.9826429,"teacher_disagreement_score":0.060806036,"about_ca_system_score_codex":0.0068508987,"about_ca_system_score_gemma":0.0047198185,"threshold_uncertainty_score":0.12232822},"labels":[],"label_agreement":null},{"id":"W2010119110","doi":"10.1130/l364.1","title":"New ties between the Alexander terrane and Wrangellia and implications for North America Cordilleran evolution","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; Memorial University of Newfoundland; Yukon University","funders":"","keywords":"Terrane; Pennsylvanian; Paleozoic; Geology; Basement; Zircon; Paleontology; Tectonics; Earth science; Geochemistry; Archaeology; Geography; Structural basin","score_opus":0.01271435256919948,"score_gpt":0.19869594044556296,"score_spread":0.18598158787636349,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010119110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98223245,0.0019994597,0.00010275089,0.0011284738,0.00002033274,0.000007603284,0.000076432516,0.00001753427,0.01441502],"genre_scores_gemma":[0.99791735,0.0004349343,0.00016797532,0.000104634884,0.000020621916,0.0000036964457,0.00007794284,0.0000056759236,0.0012672733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997633,0.00003208945,0.000011379036,0.00009149545,0.000029240244,0.00007253558],"domain_scores_gemma":[0.99965286,0.00003361458,0.00012279497,0.000025313146,0.00007136773,0.00009410071],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035371247,0.00020136942,0.00023357038,0.0011663474,0.0017901269,0.0016729095,0.0004829006,0.00043851437,0.0038311274],"category_scores_gemma":[0.0009492776,0.00012359147,0.00013495814,0.0013457445,0.0015581932,0.00081059354,0.0011145184,0.00047349173,0.0002391543],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021141114,0.00005360186,0.86704576,0.00015988632,0.00009558454,0.0022692983,0.018368818,0.00032815334,0.009036745,0.008271083,0.0010620453,0.09309763],"study_design_scores_gemma":[0.000005939604,0.00001619454,0.9874535,0.000044569086,0.000015340918,0.00031252272,0.003442571,0.00016003603,0.00018380552,0.0008223141,0.0075338017,0.000009524248],"about_ca_topic_score_codex":0.14701985,"about_ca_topic_score_gemma":0.38399124,"teacher_disagreement_score":0.85298014,"about_ca_system_score_codex":0.0033294428,"about_ca_system_score_gemma":0.0012946066,"threshold_uncertainty_score":0.29232824},"labels":[],"label_agreement":null},{"id":"W2045533599","doi":"10.1130/l199.1","title":"New constraints on Eocene extension within the Canadian Cordillera and identification of Phanerozoic protoliths for footwall gneisses of the Okanagan Valley shear zone","year":2012,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Geology; Gneiss; Shear zone; Transpression; Shear (geology); Transtension; Metamorphic rock; Metamorphism; Protolith; Terrane; Tectonite; Geochemistry; Metamorphic core complex; Paleontology; Geomorphology; Fault (geology); Extensional definition; Sinistral and dextral; Tectonics","score_opus":0.016682195479726294,"score_gpt":0.21407871461971584,"score_spread":0.19739651913998954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045533599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9781974,0.0019563274,0.00047316853,0.000152572,0.000010800032,0.000018081235,0.001114991,0.000033739594,0.01804304],"genre_scores_gemma":[0.99593854,0.00068484346,0.0006853116,0.000039964645,0.000005052686,0.0000056855274,0.00090030726,0.000013477621,0.0017268672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997713,0.000006438257,0.000011319338,0.00006571733,0.000071774055,0.00007351455],"domain_scores_gemma":[0.99957377,0.000020925103,0.000064167856,0.000025487192,0.00024795995,0.00006762395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020008384,0.00042112044,0.0002214284,0.0023504382,0.002029762,0.00131117,0.0003910394,0.00021529422,0.0031645424],"category_scores_gemma":[0.0005861994,0.00021295779,0.00016543746,0.0025562285,0.00082617457,0.00038932523,0.0008505191,0.00032006658,0.00029107076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022980088,0.000023611861,0.85869277,0.0001844793,0.00010617726,0.0005779533,0.0047628204,0.0010143096,0.042717475,0.0035081594,0.0012424769,0.08694],"study_design_scores_gemma":[0.0000025156958,0.0000045597394,0.9925922,0.000021976351,0.000014199571,0.00006654447,0.00074089103,0.00028952307,0.0004902823,0.00008141994,0.005688695,0.00000730098],"about_ca_topic_score_codex":0.93228966,"about_ca_topic_score_gemma":0.9904785,"teacher_disagreement_score":0.06771034,"about_ca_system_score_codex":0.0094533665,"about_ca_system_score_gemma":0.007163704,"threshold_uncertainty_score":0.13621813},"labels":[],"label_agreement":null},{"id":"W2062717515","doi":"10.1130/l286.1","title":"Temporal variations in Holocene slip rate along the central Garlock fault, Pilot Knob Valley, California","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"McGill University; Purdue University; National Science Foundation","keywords":"Holocene; Geology; Slip (aerodynamics); Alluvium; Alluvial fan; Quaternary; Fault (geology); Pleistocene; Geodetic datum; Seismology; Paleontology; Geodesy","score_opus":0.014761437935689865,"score_gpt":0.20968991363849296,"score_spread":0.19492847570280308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062717515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991652,0.000050010898,0.000023807192,0.000011356925,0.0000017369201,0.000001526727,0.00030818448,0.0000049041464,0.00043333712],"genre_scores_gemma":[0.99934393,0.000049260754,0.000040218914,0.0000035304238,0.0000022470933,0.0000022866807,0.00033939484,0.0000013751174,0.00021766081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999131,0.000006779063,0.0000064145675,0.000035640824,0.000016624816,0.000021526217],"domain_scores_gemma":[0.9995234,0.00007969973,0.00015485496,0.000029580218,0.00013424296,0.00007808994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017849992,0.00011622294,0.00012088722,0.00088488206,0.00046957366,0.00045062817,0.00021828075,0.00017388054,0.0010768181],"category_scores_gemma":[0.0005914543,0.00014301678,0.000064529835,0.0006191959,0.0002729222,0.00020601154,0.00022150064,0.00014790402,0.000108337925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009501816,0.00002240982,0.99301845,0.00001463423,0.000030264413,0.00005442443,0.0005555229,0.00027948595,0.0012037687,0.000035787714,0.0004027758,0.004287467],"study_design_scores_gemma":[0.0000013412483,0.000005616093,0.9996301,0.0000020278976,0.0000032165917,0.000009662222,0.00010331493,0.000074532276,0.000037861966,0.0000031056775,0.0001281774,9.488371e-7],"about_ca_topic_score_codex":0.12500384,"about_ca_topic_score_gemma":0.35492492,"teacher_disagreement_score":0.12500384,"about_ca_system_score_codex":0.00066962134,"about_ca_system_score_gemma":0.00027980734,"threshold_uncertainty_score":0.2485525},"labels":[],"label_agreement":null},{"id":"W2067336156","doi":"10.1130/l98.1","title":"Testing modes of exhumation in collisional orogens: Synconvergent channel flow in the southeastern Canadian Cordillera","year":2010,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Massachusetts Institute of Technology","keywords":"Geology; Foreland basin; Crust; Tectonics; Seismology; Flow (mathematics); Channel (broadcasting); Shear (geology); Geomorphology; Shear zone; Petrology; Geophysics; Mechanics; Physics","score_opus":0.017322655946091156,"score_gpt":0.1917111117254447,"score_spread":0.17438845577935352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067336156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99545646,0.00090960006,0.00035728162,0.000059958307,0.0000032636422,0.00001328236,0.00011160346,0.000015546048,0.003073061],"genre_scores_gemma":[0.99893373,0.0004676327,0.00025415662,0.000010638222,0.000001913103,0.0000029984199,0.00006619362,0.0000036495135,0.00025910712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976844,0.000013226367,0.000009618743,0.00007046158,0.00007270577,0.00006554114],"domain_scores_gemma":[0.999777,0.000040154657,0.00005549026,0.000018304261,0.00008118839,0.000027803233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004014596,0.00031610913,0.0002352919,0.00212042,0.001443661,0.0011247353,0.00080263335,0.00033739497,0.0011122889],"category_scores_gemma":[0.0010482506,0.00015936348,0.00028778653,0.0016074306,0.0013539902,0.00054325914,0.00075150793,0.0002522187,0.00005564185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004001958,0.000048651505,0.896793,0.0003261556,0.00022286702,0.0012086637,0.004769561,0.012235434,0.0105369855,0.0057049603,0.00022346208,0.06753002],"study_design_scores_gemma":[0.000019837267,0.000053966294,0.9773573,0.000057155936,0.000108825756,0.00022641792,0.003056004,0.0132694105,0.0020085266,0.00080745626,0.0029998252,0.00003523798],"about_ca_topic_score_codex":0.7976622,"about_ca_topic_score_gemma":0.84140825,"teacher_disagreement_score":0.2023378,"about_ca_system_score_codex":0.0075290115,"about_ca_system_score_gemma":0.0043240166,"threshold_uncertainty_score":0.40705878},"labels":[],"label_agreement":null},{"id":"W2075670662","doi":"10.1130/l65.1","title":"State of stress in central and eastern North American seismic zones","year":2010,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Clockwise; Seismology; Induced seismicity; Azimuth; Borehole; Focal mechanism; Stress field; Intraplate earthquake; Stress (linguistics); Magnitude (astronomy); Geodesy; Rotation (mathematics); Tectonics; Geometry; Paleontology","score_opus":0.006495146780503489,"score_gpt":0.1957644384445398,"score_spread":0.1892692916640363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075670662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985598,0.000053941552,0.000660596,0.000020827662,4.8038464e-7,0.000004158622,0.00015665637,0.000009886155,0.00053375866],"genre_scores_gemma":[0.998845,0.00004572866,0.00058855687,0.000008026398,0.0000016528143,0.000008008163,0.00032664082,0.0000019609506,0.00017445748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997856,0.00004511486,0.000013692417,0.00007485255,0.000040633724,0.000040146388],"domain_scores_gemma":[0.9994004,0.00013883424,0.00019277378,0.000030510342,0.00016460642,0.00007282394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005928896,0.00016833495,0.000207475,0.0012715462,0.00044195633,0.0005626158,0.00025282134,0.0002048295,0.0005943465],"category_scores_gemma":[0.0012559395,0.0002478387,0.00021304209,0.0011336397,0.0003404946,0.00022483956,0.00061946514,0.00018180322,0.0000603435],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001605581,0.000041495136,0.9707143,0.000019101555,0.00010721283,0.00008211502,0.0008451951,0.0082519865,0.0032001506,0.00045313482,0.0002643286,0.015860407],"study_design_scores_gemma":[0.000008281378,0.000012481299,0.98648864,0.000008151751,0.000022922492,0.000027998312,0.00032199456,0.012217852,0.0001796283,0.00030592372,0.00039651548,0.000009533453],"about_ca_topic_score_codex":0.12178893,"about_ca_topic_score_gemma":0.21238965,"teacher_disagreement_score":0.12178893,"about_ca_system_score_codex":0.0008344981,"about_ca_system_score_gemma":0.0007927502,"threshold_uncertainty_score":0.24216008},"labels":[],"label_agreement":null},{"id":"W2085980973","doi":"10.1130/l164.1","title":"Miocene bivergent crustal extension in the Aegean: Evidence from the western Cyclades (Greece)","year":2011,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":156,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Accelerated Innovation Research Initiative Turning Top Science and Ideas into High-Impact Values; Austrian Science Fund","keywords":"CYCLADES; Geology; Crust; Blueschist; Detachment fault; Seismology; Shear zone; Shear (geology); Late Miocene; Fault (geology); Normal fault; Paleontology; Geochemistry; Tectonics; Subduction; Structural basin; Eclogite","score_opus":0.07141097716849992,"score_gpt":0.23727679951961622,"score_spread":0.1658658223511163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085980973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99689734,0.0004268186,0.000038651928,0.000033655495,0.0000028447585,0.0000040196296,0.000088603316,0.0000032517328,0.0025048014],"genre_scores_gemma":[0.99874926,0.00052136136,0.00010061466,0.000029724963,0.000006213708,0.000003134847,0.00016996407,0.0000025766294,0.00041709884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989426,0.000015462276,0.000016519294,0.000037380523,0.00001710573,0.000019193936],"domain_scores_gemma":[0.999846,0.000012698963,0.000067212626,0.000016225253,0.000034760516,0.000022983715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021720948,0.00031608655,0.00018531637,0.0015467765,0.00037749571,0.0005723763,0.00022856204,0.00030201508,0.0015979161],"category_scores_gemma":[0.00031358356,0.00013729047,0.00017393296,0.0011701589,0.0008208053,0.00045293698,0.000595116,0.00016005243,0.0003035942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016504136,0.000027893953,0.9545162,0.00015796913,0.00012675588,0.0015777982,0.004270311,0.00027949724,0.012625798,0.00030095404,0.00023869055,0.025713045],"study_design_scores_gemma":[0.0000040174036,0.000026352267,0.9966978,0.000021018617,0.000014565948,0.00043465698,0.0012123102,0.000052409643,0.00019747508,0.00003954714,0.0012959851,0.0000038966355],"about_ca_topic_score_codex":0.019714018,"about_ca_topic_score_gemma":0.033393588,"teacher_disagreement_score":0.019714018,"about_ca_system_score_codex":0.00043189593,"about_ca_system_score_gemma":0.00034118525,"threshold_uncertainty_score":0.039198577},"labels":[],"label_agreement":null},{"id":"W2104656423","doi":"10.1130/l425.1","title":"Mid-Miocene initiation of orogen-parallel extension, NW Nepal Himalaya","year":2015,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; Northwestern University; Geological Society of America","keywords":"Geology; Lineation; Monazite; Shear zone; Metamorphism; Thermochronology; Muscovite; Shear (geology); Geochronology; Closure temperature; Shearing (physics); Geochemistry; Deformation mechanism; Quartz; Tectonics; Petrology; Seismology; Paleontology; Zircon","score_opus":0.027849849995491054,"score_gpt":0.21812437911789503,"score_spread":0.19027452912240397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104656423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9836483,0.00026227912,0.00018054568,0.0000980618,0.0000036831457,0.000015947884,0.00018194939,0.000025637954,0.01558364],"genre_scores_gemma":[0.99706763,0.00031972496,0.00015195923,0.0000492052,0.0000049419764,0.0000113193,0.00017246389,0.0000057620787,0.0022170118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991155,0.000009695462,0.0000048377156,0.000027887894,0.000013225864,0.000032781627],"domain_scores_gemma":[0.9999076,0.000012451058,0.00002242991,0.0000088905235,0.000028447314,0.000020163647],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120812656,0.00016214333,0.00009703172,0.00077119365,0.00083242403,0.0009876742,0.0002653092,0.0002146234,0.0022790844],"category_scores_gemma":[0.00045745916,0.00023092798,0.0000920842,0.00054263993,0.00048012854,0.00039909894,0.000645849,0.00022909415,0.00049033616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031393272,0.00010486987,0.7896557,0.00048894295,0.000110034714,0.0073892986,0.025809726,0.0011734809,0.0826016,0.005139975,0.0019299627,0.08528246],"study_design_scores_gemma":[0.0000057151,0.00003654486,0.98500407,0.000048427835,0.000016708638,0.0009855832,0.0024685315,0.00041522985,0.0016622884,0.00023913929,0.009106335,0.000011360286],"about_ca_topic_score_codex":0.026542172,"about_ca_topic_score_gemma":0.06053629,"teacher_disagreement_score":0.026542172,"about_ca_system_score_codex":0.0007198365,"about_ca_system_score_gemma":0.0007960052,"threshold_uncertainty_score":0.052775383},"labels":[],"label_agreement":null},{"id":"W2107179794","doi":"10.1130/l225.1","title":"Age, construction, and exhumation of the midcrust of the Jurassic Bonanza arc, Vancouver Island, Canada","year":2012,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Alberta; University of Victoria","funders":"","keywords":"Geology; Plutonism; Pluton; Subduction; Crust; Batholith; Zircon; Geochemistry; Island arc; Seismology; Back-arc basin; Forearc; Diorite; Tectonics","score_opus":0.005357811120158264,"score_gpt":0.15633706159395908,"score_spread":0.1509792504738008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107179794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98843575,0.0010897618,0.00016740209,0.00006349911,0.000005510732,0.0000178067,0.0037919853,0.000025879284,0.0064024515],"genre_scores_gemma":[0.99301696,0.0004948694,0.00042567268,0.000013297609,0.0000015479957,0.000010852583,0.0022010312,0.000014589144,0.0038211492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998275,0.0000067610963,0.0000063996354,0.000043495944,0.00005145433,0.00006426371],"domain_scores_gemma":[0.9994173,0.00002038483,0.00006146862,0.000016911388,0.00037617865,0.00010780193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016678585,0.00027095719,0.00017286355,0.0030772972,0.0018366737,0.001055198,0.0005556682,0.00020337441,0.0023850673],"category_scores_gemma":[0.000555625,0.00026885147,0.00013288067,0.002207688,0.00042809316,0.00019727471,0.0005447112,0.00027337793,0.00044109166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001312444,0.000018514029,0.9383176,0.00007017955,0.00004783643,0.00020269626,0.002545177,0.00076773367,0.0071576512,0.00040235787,0.0012022989,0.049136676],"study_design_scores_gemma":[8.4866195e-7,0.0000040123577,0.9955409,0.0000141196615,0.00000463266,0.000044164088,0.00040357563,0.00014266079,0.00027137483,0.000014788617,0.0035551677,0.000003724954],"about_ca_topic_score_codex":0.97904164,"about_ca_topic_score_gemma":0.9955101,"teacher_disagreement_score":0.020958364,"about_ca_system_score_codex":0.01094657,"about_ca_system_score_gemma":0.006364828,"threshold_uncertainty_score":0.07942331},"labels":[],"label_agreement":null},{"id":"W2111447315","doi":"10.1130/l310.1","title":"Two flysch belts having distinctly different provenance suggest no stratigraphic link between the Wrangellia composite terrane and the paleo-Alaskan margin","year":2013,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Flysch; Geology; Provenance; Clastic rock; Paleocurrent; Conglomerate; Geochemistry; Paleontology; Sedimentary rock; Tectonics","score_opus":0.011276631541862779,"score_gpt":0.19300217188535493,"score_spread":0.18172554034349214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111447315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964091,0.00010671918,0.0001191837,0.00001263228,0.0000020202128,0.000008336204,0.00030015173,0.000015638792,0.0030261623],"genre_scores_gemma":[0.9976052,0.000057658264,0.00034629187,0.000010553619,0.0000017543996,0.0000058862256,0.0006555497,0.000003788784,0.001313245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999269,0.0000029451176,0.0000056472722,0.000028891607,0.0000135434075,0.000022056913],"domain_scores_gemma":[0.9997712,0.000019602017,0.00008173351,0.00002574583,0.00005050234,0.000051215713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007541386,0.00019260233,0.00013778609,0.0014934302,0.00051423116,0.00051400915,0.00016281774,0.00013383782,0.0031373014],"category_scores_gemma":[0.00018912519,0.000109135806,0.00013186834,0.0006223263,0.00031527726,0.00023617026,0.0003640722,0.0001551993,0.00039470993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011184394,0.0000202132,0.9511629,0.000036463374,0.00004434713,0.00021915675,0.00087972404,0.00006751072,0.032546163,0.00031948515,0.00013408504,0.014458037],"study_design_scores_gemma":[0.0000012962142,0.00000869733,0.998643,0.0000033011343,0.0000046634595,0.00011796067,0.00024981107,0.000026216769,0.0005355662,0.000023282124,0.0003848017,0.0000015243276],"about_ca_topic_score_codex":0.020955933,"about_ca_topic_score_gemma":0.121883236,"teacher_disagreement_score":0.020955933,"about_ca_system_score_codex":0.0003558358,"about_ca_system_score_gemma":0.00024822511,"threshold_uncertainty_score":0.04166788},"labels":[],"label_agreement":null},{"id":"W2114406239","doi":"10.1130/l299.1","title":"Mantle roots of major Precambrian shear zones inferred from structure of the Great Slave Lake shear zone, northwest Canada","year":2013,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Craton; Shear zone; Subduction; Lithosphere; Mantle (geology); Crust; Seismology; Obduction; Precambrian; Petrology; Archean; Geochemistry; Tectonics; Oceanic crust","score_opus":0.004063369776379861,"score_gpt":0.15541461837258197,"score_spread":0.1513512485962021,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114406239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958586,0.00017585901,0.000077501994,0.00003683991,0.0000012861789,0.000005470096,0.0011260806,0.000011720797,0.0027066844],"genre_scores_gemma":[0.9973688,0.00018430516,0.00021002271,0.000009237774,8.2206003e-7,0.0000026856449,0.0010807167,0.000004829589,0.0011385127],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.000001219748,0.0000021676906,0.000013401047,0.000018483128,0.000026693999],"domain_scores_gemma":[0.9998622,0.0000067683054,0.000016357377,0.0000049900927,0.00007247595,0.000037180052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000056527086,0.00021152949,0.00011520923,0.0014366707,0.0010397597,0.0006646041,0.00025028051,0.00011991146,0.0020311852],"category_scores_gemma":[0.00032051085,0.00015561304,0.000108192464,0.0016034341,0.0003680719,0.0001257136,0.00045947146,0.0001378522,0.00017244194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001224843,0.0000107073265,0.950383,0.000054307988,0.000053802683,0.00025305408,0.002340726,0.00085138157,0.020515308,0.0010074439,0.0013343116,0.023073385],"study_design_scores_gemma":[0.0000039709153,0.0000024890503,0.99716586,0.00000988331,0.00000994912,0.00002506378,0.0007009102,0.00041088372,0.00044373385,0.000038295337,0.0011852379,0.0000037204313],"about_ca_topic_score_codex":0.9767983,"about_ca_topic_score_gemma":0.9943821,"teacher_disagreement_score":0.023201704,"about_ca_system_score_codex":0.0061382256,"about_ca_system_score_gemma":0.0068206885,"threshold_uncertainty_score":0.046676636},"labels":[],"label_agreement":null},{"id":"W2118993002","doi":"10.1130/l346.1","title":"Pre- to post-Cordilleran transposition history of Joss Mountain: Insights into the exhumation of the Shuswap complex, southeastern Canadian Cordillera","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Devonian; Culmination; Lithosphere; Subduction; Metamorphic rock; Crust; Paleontology; Shear zone; Proterozoic; Metamorphism; Continental crust; Continental collision; Seismology; Tectonics","score_opus":0.008725191126194909,"score_gpt":0.1734559933508536,"score_spread":0.1647308022246587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118993002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99763787,0.00022973726,0.000117551004,0.000047893525,0.0000023041105,0.000005472046,0.0003285892,0.000017111017,0.0016136427],"genre_scores_gemma":[0.9989796,0.000115204195,0.0001846199,0.000011855421,0.0000012467702,0.0000024345345,0.00026377648,0.000005119803,0.0004361979],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987507,0.0000039913602,0.000004117471,0.000032540564,0.000037473754,0.000046767113],"domain_scores_gemma":[0.9998522,0.000009034542,0.000023925812,0.000010045884,0.00007200468,0.000032785276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015510226,0.0003671425,0.00021821042,0.0013189511,0.001608373,0.00095385924,0.00038629313,0.00031959062,0.0020715934],"category_scores_gemma":[0.00041539277,0.00017829868,0.0002520007,0.0017401279,0.0006887971,0.00029907696,0.0006509161,0.00022029085,0.00014522848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015483887,0.0000328621,0.9297021,0.00007762418,0.00012777491,0.0007673853,0.002864507,0.0027657202,0.029091004,0.0010383881,0.0005628566,0.032814916],"study_design_scores_gemma":[0.0000024889375,0.000006402727,0.9963147,0.000008181571,0.000013890019,0.00006693604,0.0006215011,0.001089551,0.00051217916,0.000041121264,0.0013165344,0.000006538936],"about_ca_topic_score_codex":0.9251535,"about_ca_topic_score_gemma":0.97127444,"teacher_disagreement_score":0.074846506,"about_ca_system_score_codex":0.0058707935,"about_ca_system_score_gemma":0.00539093,"threshold_uncertainty_score":0.1505745},"labels":[],"label_agreement":null},{"id":"W2122778387","doi":"10.1130/l381.1","title":"Metamorphism and geochronology of the exhumed Himalayan midcrust, Likhu Khola region, east-central Nepal: Recognition of a tectonometamorphic discontinuity","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Tekes; University of Saskatchewan; National Science Foundation","keywords":"Geology; Metamorphism; Metamorphic rock; Foreland basin; Monazite; Discontinuity (linguistics); Metamorphic core complex; Geochronology; Geochemistry; Paleontology; Zircon; Tectonics; Extensional definition","score_opus":0.01308800255958923,"score_gpt":0.16801477194496528,"score_spread":0.15492676938537606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122778387","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99814904,0.000066833454,0.000057041736,0.000012116879,6.939883e-7,0.000007130982,0.0001381131,0.0000061587803,0.0015628921],"genre_scores_gemma":[0.9994685,0.000043972177,0.000111023925,0.0000065262143,0.0000010124539,0.000005887931,0.00014009104,0.0000017007285,0.00022119512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999262,0.00000823733,0.000007581633,0.000024670346,0.000014292978,0.000018994986],"domain_scores_gemma":[0.99987817,0.00001995831,0.000031921954,0.000012231329,0.000039177263,0.000018501863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008887907,0.0001426511,0.00011365671,0.0011748564,0.0005506258,0.0006270589,0.0003282793,0.00021077952,0.0009988273],"category_scores_gemma":[0.0003326756,0.00018101947,0.000099768265,0.0011581993,0.00046806742,0.000261031,0.00042110033,0.00014539946,0.0002133165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015919317,0.00005142728,0.92951286,0.00012408751,0.000055230852,0.0024068865,0.009634349,0.0006007675,0.03476812,0.00042277822,0.00022047068,0.022043921],"study_design_scores_gemma":[0.0000027761482,0.000013101277,0.997317,0.000008248645,0.000007973372,0.0004043552,0.001046559,0.0002078208,0.00052294525,0.0000169895,0.00044894326,0.0000032202224],"about_ca_topic_score_codex":0.046680428,"about_ca_topic_score_gemma":0.09379489,"teacher_disagreement_score":0.046680428,"about_ca_system_score_codex":0.00063089427,"about_ca_system_score_gemma":0.00042778108,"threshold_uncertainty_score":0.092817426},"labels":[],"label_agreement":null},{"id":"W2125764459","doi":"10.1130/l292.1","title":"Transpressive uplift and exhumation of continental lower crust revealed by synkinematic monazite reactions","year":2013,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Continental crust; Crust; Orogeny; Monazite; Shear zone; Transpression; Geochemistry; Craton; Seismology; Lithosphere; Paleontology; Petrology; Tectonics; Zircon","score_opus":0.004274041142713226,"score_gpt":0.1688911712460425,"score_spread":0.16461713010332926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125764459","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995011,0.000018802215,0.000044232576,0.0000042336483,2.6803096e-7,9.757842e-7,0.00005863386,0.000003306256,0.00036848057],"genre_scores_gemma":[0.99973315,0.000025375024,0.000052592466,0.0000030116164,3.3018506e-7,6.537558e-7,0.00005528526,0.000001502835,0.0001281047],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999484,0.0000044551766,0.0000040148116,0.000014063985,0.000012407789,0.000016668058],"domain_scores_gemma":[0.99989605,0.00000976014,0.000034157518,0.000014985577,0.000027218934,0.000017748407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011607231,0.00016716922,0.0001233734,0.0007704565,0.0003821509,0.00045980662,0.00015781501,0.00012920595,0.0007835776],"category_scores_gemma":[0.0002801343,0.00019933835,0.00009597493,0.0007050554,0.00048115983,0.00014679896,0.00035544168,0.00014449554,0.00009155474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000117201416,0.000011439275,0.86169565,0.000023493323,0.00005529591,0.00020360039,0.0010048266,0.0008451791,0.12783709,0.00026435434,0.00006987553,0.007871961],"study_design_scores_gemma":[0.000001055316,0.000005326731,0.9980782,9.584902e-7,0.0000040770133,0.000033048273,0.00013322633,0.00018213215,0.0014501745,0.000014598675,0.00009527625,0.0000017489322],"about_ca_topic_score_codex":0.13019526,"about_ca_topic_score_gemma":0.3567031,"teacher_disagreement_score":0.13019526,"about_ca_system_score_codex":0.0009299226,"about_ca_system_score_gemma":0.0005677306,"threshold_uncertainty_score":0.2588749},"labels":[],"label_agreement":null},{"id":"W2126210028","doi":"10.1130/l325.1","title":"Tectonic control of topography, rainfall patterns, and erosion during rapid post–12 Ma uplift of the Bolivian Andes","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Institute for Advanced Research","funders":"","keywords":"Geology; Foreland basin; Tectonics; Fluvial; Erosion; Landform; Geomorphology; Paleontology; Channel (broadcasting); Physical geography; Structural basin; Geography","score_opus":0.004765530097171675,"score_gpt":0.18811319229748186,"score_spread":0.18334766220031018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126210028","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967084,0.00031391464,0.00007445802,0.00007573233,0.0000019119475,0.0000067650935,0.00020862641,0.000012298451,0.0025978135],"genre_scores_gemma":[0.9993773,0.0001196237,0.000091367016,0.000011114763,0.0000024711428,0.0000043791133,0.00018277613,0.0000050961544,0.00020583042],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971706,0.00004138701,0.0000132692485,0.0000769839,0.00003278128,0.00011849297],"domain_scores_gemma":[0.9996438,0.000033895496,0.00016007076,0.000046773424,0.000056627643,0.000058898764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005778345,0.0001990491,0.00030236196,0.0015339346,0.00072360557,0.001805254,0.00048903225,0.00020726855,0.0014232979],"category_scores_gemma":[0.0011269808,0.00027926176,0.00023991047,0.0015579774,0.0012015977,0.00044240127,0.0011996638,0.00044299415,0.0001533486],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002587754,0.000045099972,0.9515306,0.00008963265,0.00022585971,0.00026545025,0.0034717352,0.0042064325,0.009129506,0.0018378814,0.00039156378,0.02854748],"study_design_scores_gemma":[0.0000042201664,0.000008243771,0.9983783,0.000018952094,0.000010290189,0.000025235611,0.00048208545,0.00028400516,0.000080083955,0.00012390464,0.00057942374,0.00000529541],"about_ca_topic_score_codex":0.12906268,"about_ca_topic_score_gemma":0.16267724,"teacher_disagreement_score":0.12906268,"about_ca_system_score_codex":0.0044002132,"about_ca_system_score_gemma":0.0009514232,"threshold_uncertainty_score":0.2566229},"labels":[],"label_agreement":null},{"id":"W2131889110","doi":"10.1130/l437.1","title":"Lateral extrusion, underplating, and out-of-sequence thrusting within the Himalayan metamorphic core, Kanchenjunga, Nepal","year":2015,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Metamorphism; Geology; Metamorphic rock; Metamorphic core complex; Monazite; Paleontology; Underplating; Geochemistry; Sequence (biology); Zircon; Tectonics; Subduction","score_opus":0.07374924574213865,"score_gpt":0.25116270502010396,"score_spread":0.1774134592779653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131889110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990221,0.00004522017,0.000120433586,0.000010108458,5.4654714e-7,0.0000029128962,0.00012467463,0.000012711814,0.00066114526],"genre_scores_gemma":[0.9994842,0.00003922581,0.000109735935,0.0000039159077,5.2044317e-7,0.0000029672362,0.00015800436,0.0000027510107,0.00019873871],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999522,0.000004097051,0.0000039052074,0.000020539304,0.000006500191,0.000012697115],"domain_scores_gemma":[0.9999336,0.000011922337,0.000017131888,0.0000098674645,0.000017771143,0.000009699986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000078595054,0.00018065271,0.00013775758,0.00092906656,0.00045850995,0.00076996186,0.00031838298,0.00025712728,0.0007124025],"category_scores_gemma":[0.00023188422,0.0002784947,0.0001962294,0.0010183224,0.000430451,0.00026821086,0.00043431448,0.00015615097,0.00012828692],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011326462,0.000036834426,0.9302716,0.000113829985,0.00014761859,0.0013706413,0.0033622868,0.018989371,0.022989826,0.0006038965,0.0002584627,0.021742303],"study_design_scores_gemma":[0.000006080558,0.000018292554,0.9900686,0.000011879014,0.000045359728,0.000274164,0.0007574677,0.007675152,0.000558343,0.00009057979,0.00048571776,0.00000834533],"about_ca_topic_score_codex":0.12576121,"about_ca_topic_score_gemma":0.21732794,"teacher_disagreement_score":0.12576121,"about_ca_system_score_codex":0.00081319414,"about_ca_system_score_gemma":0.00071200513,"threshold_uncertainty_score":0.2500584},"labels":[],"label_agreement":null},{"id":"W2142340508","doi":"10.1130/l396.1","title":"Late Miocene upper-crustal deformation within the interior of the southern Puna Plateau, central Andes","year":2015,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of California, Los Angeles; University of Toronto; Geological Society of America","keywords":"Geology; Plateau (mathematics); Geochronology; Structural basin; Lithosphere; Zircon; Seismology; Volcano; Paleontology; Deformation (meteorology); Geomorphology; Tectonics","score_opus":0.011707392327231758,"score_gpt":0.1831787480282897,"score_spread":0.17147135570105795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142340508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979607,0.00013223324,0.00006522273,0.000019303385,0.0000022642762,0.0000053194135,0.00009411448,0.000017547076,0.0017033587],"genre_scores_gemma":[0.9992461,0.00011407274,0.00012397567,0.000007991958,0.000002532683,0.0000073909514,0.00014700646,0.0000036973458,0.00034719275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988174,0.000013146372,0.000008057257,0.000046708323,0.000018062408,0.00003212568],"domain_scores_gemma":[0.9997503,0.000033306842,0.00007419302,0.000022748543,0.00005835112,0.000060955754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032927762,0.00028670207,0.00024322937,0.0011132758,0.00084394973,0.0010201392,0.00033182578,0.00020579282,0.0010247803],"category_scores_gemma":[0.000545548,0.00026777294,0.00018880628,0.001121973,0.0007883526,0.00041862545,0.00065821863,0.00021642455,0.00012138529],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017459482,0.00006198899,0.9525485,0.00010423534,0.00009807042,0.0008519153,0.0030692723,0.0010342323,0.018124321,0.0003207544,0.00021182785,0.0234002],"study_design_scores_gemma":[0.000003068141,0.000013405884,0.99899,0.000004541157,0.0000057499233,0.00009000203,0.00023747295,0.00012663122,0.00007771657,0.000018554822,0.00043032653,0.0000025100974],"about_ca_topic_score_codex":0.033596184,"about_ca_topic_score_gemma":0.06639268,"teacher_disagreement_score":0.033596184,"about_ca_system_score_codex":0.0006104297,"about_ca_system_score_gemma":0.00052353286,"threshold_uncertainty_score":0.06680125},"labels":[],"label_agreement":null},{"id":"W2164032007","doi":"10.1130/l360.1","title":"Multisystem dating of modern river detritus from Tajikistan and China: Implications for crustal evolution and exhumation of the Pamir","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Arizona; National Geographic Society; National Science Foundation","keywords":"Geology; Terrane; Cenozoic; Mesozoic; Tectonics; Paleontology; Detritus; Plateau (mathematics); Geochemistry; Structural basin","score_opus":0.008079340276209724,"score_gpt":0.1911458717421795,"score_spread":0.1830665314659698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164032007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986596,0.00027100954,0.00026837736,0.000012211216,0.0000024750148,0.0000021926874,0.00013201905,0.000008028622,0.0006440225],"genre_scores_gemma":[0.9980558,0.000189062,0.000939257,0.000020578784,0.000004905514,0.0000059249546,0.00035972448,0.0000062962395,0.00041839268],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998485,0.000015602669,0.000019265715,0.00006430038,0.000027017704,0.000025228246],"domain_scores_gemma":[0.9997404,0.00003513041,0.00007561952,0.000031575986,0.00008338839,0.000033788678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004150789,0.00035334934,0.00025185922,0.001813293,0.0007249107,0.00064534723,0.00041279435,0.00022594073,0.00044749264],"category_scores_gemma":[0.0004495796,0.00025653958,0.00020743404,0.001910125,0.00030114848,0.00029708905,0.0006038567,0.00025067385,0.000102074075],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012220764,0.000020155272,0.86615247,0.00006388093,0.000112269554,0.00030979895,0.0009797155,0.00023620386,0.11011766,0.00010423249,0.00007059526,0.021710817],"study_design_scores_gemma":[0.0000023473904,0.000020444537,0.9963252,0.00000400426,0.000030676198,0.00013254765,0.00015717426,0.00025002428,0.0024606648,0.000012564633,0.00060175173,0.0000026146554],"about_ca_topic_score_codex":0.013242037,"about_ca_topic_score_gemma":0.039194964,"teacher_disagreement_score":0.013242037,"about_ca_system_score_codex":0.0003920384,"about_ca_system_score_gemma":0.00038916158,"threshold_uncertainty_score":0.026329935},"labels":[],"label_agreement":null},{"id":"W2168176243","doi":"10.1130/l134.1","title":"U-Pb-Hf characterization of the central Coast Mountains batholith: Implications for petrogenesis and crustal architecture","year":2011,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":131,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Terrane; Batholith; Geology; Pluton; Zircon; Geochemistry; Mafic; Metamorphism; Fibrous joint; Shear zone; Crust; Paleontology; Tectonics","score_opus":0.015610122297335079,"score_gpt":0.18333438248544381,"score_spread":0.16772426018810874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168176243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99803656,0.0002871042,0.0001606275,0.000006896894,5.750429e-7,0.0000024140402,0.00016287004,0.00000862565,0.0013342726],"genre_scores_gemma":[0.9986565,0.00018012004,0.00037450166,0.0000055424503,0.0000011290355,0.0000032701892,0.000221278,0.000004944327,0.0005527312],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999521,0.000002682492,0.0000040162054,0.000017320108,0.000010077768,0.0000137298475],"domain_scores_gemma":[0.99987495,0.000014141398,0.00002756808,0.00001434077,0.00005057955,0.000018478508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010799342,0.00020953559,0.00020551204,0.0019112962,0.00068312534,0.000660253,0.00024802002,0.00012346637,0.0011911676],"category_scores_gemma":[0.00026942804,0.0001563667,0.000102385726,0.0018063361,0.00047272554,0.00019009496,0.00042150138,0.00010678314,0.0001963477],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010745189,0.000012288611,0.89857805,0.00008663026,0.00005524675,0.00030586106,0.0018669943,0.00053951814,0.065360114,0.0001391726,0.00010605611,0.032842655],"study_design_scores_gemma":[6.727464e-7,0.000007064561,0.9984426,0.000004684778,0.0000060352386,0.000101678714,0.00030657323,0.000108045315,0.0006732994,0.000017035396,0.00033070034,0.0000016913859],"about_ca_topic_score_codex":0.28346145,"about_ca_topic_score_gemma":0.54393,"teacher_disagreement_score":0.28346145,"about_ca_system_score_codex":0.00070234074,"about_ca_system_score_gemma":0.0006928543,"threshold_uncertainty_score":0.5636231},"labels":[],"label_agreement":null},{"id":"W2181767236","doi":"10.1130/l461.1","title":"Orocline formation at the core of Pangea: A structural study of the Cantabrian orocline, NW Iberian Massif","year":2015,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Massif; Anticline; Sinistral and dextral; Paleontology; SLATES; Fold (higher-order function); Foreland basin; Paleozoic; Shear zone; Seismology; Tectonics; Geochemistry","score_opus":0.03847621522637881,"score_gpt":0.23253360020382843,"score_spread":0.19405738497744962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181767236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997355,0.00062881084,0.000027105005,0.0000329465,0.0000024355777,0.000010846888,0.00018561371,0.000005036869,0.0017522628],"genre_scores_gemma":[0.9986738,0.00037932623,0.00014285925,0.000022728078,0.0000074163995,0.00001121661,0.0004401411,0.0000049547784,0.0003175846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980587,0.000013620541,0.000011373369,0.00007588181,0.000026377254,0.00006699683],"domain_scores_gemma":[0.9998716,0.0000061536607,0.00005065705,0.0000081041235,0.000042057778,0.00002135429],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002759755,0.0005238905,0.00035969206,0.0027679668,0.001465089,0.0015560047,0.0006626179,0.0005810886,0.0015547911],"category_scores_gemma":[0.0003302903,0.00028973626,0.00028713563,0.0022851143,0.0010726169,0.0005868456,0.0011753774,0.00033776555,0.0003204232],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058097194,0.00019779342,0.91149956,0.00023044743,0.00023431699,0.0011608164,0.008401619,0.00066978444,0.036260676,0.0004755513,0.00056146184,0.039727017],"study_design_scores_gemma":[0.0000033412934,0.000009933006,0.99903,0.000006325254,0.0000074361874,0.000034285953,0.00035468387,0.00005713348,0.000070217626,0.000009089215,0.00041577185,0.0000018277464],"about_ca_topic_score_codex":0.2343953,"about_ca_topic_score_gemma":0.2878651,"teacher_disagreement_score":0.2343953,"about_ca_system_score_codex":0.0025103122,"about_ca_system_score_gemma":0.00067613955,"threshold_uncertainty_score":0.46606195},"labels":[],"label_agreement":null},{"id":"W2272325154","doi":"10.1130/l426.1","title":"Paradigm lost: Buoyancy thwarted by the strength of the Western Gneiss Region (ultra)high-pressure terrane, Norway","year":2015,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Terrane; Geology; Subduction; Metamorphism; Orogeny; Gneiss; Metamorphic rock; Alpine orogeny; Continental collision; Tectonics; Geochemistry; Paleontology; Earth science; Mesozoic","score_opus":0.014242174122226385,"score_gpt":0.19142630216477088,"score_spread":0.1771841280425445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2272325154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98873144,0.00026682587,0.0024642434,0.00042941156,0.000037744292,0.0000051016596,0.00019825711,0.000019940402,0.007847221],"genre_scores_gemma":[0.998735,0.00010618648,0.0004263018,0.000020300611,0.0000039806164,0.0000018886022,0.000049580765,0.0000065975046,0.0006502127],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999583,0.00000909721,0.0000025096087,0.0000129792215,0.000008284439,0.00000896717],"domain_scores_gemma":[0.9999262,0.000016593463,0.000028256303,0.000006154595,0.000008902075,0.000013872651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012232648,0.00014084777,0.000110472465,0.00012695475,0.00026296265,0.0010332562,0.00042927905,0.0003182255,0.0011379985],"category_scores_gemma":[0.0005865009,0.000107489184,0.00020630856,0.0001398965,0.0008095754,0.0004985271,0.00044420292,0.00024132042,0.0000760625],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003894206,0.000058609035,0.17900182,0.00013155228,0.000107391556,0.0010916828,0.0009575412,0.72701794,0.018912245,0.055202194,0.0019161794,0.015213437],"study_design_scores_gemma":[0.00006502753,0.00013616488,0.16234757,0.00005196922,0.000043372078,0.00027652824,0.0017494133,0.809687,0.0019385341,0.015679887,0.007957955,0.000066535344],"about_ca_topic_score_codex":0.11369512,"about_ca_topic_score_gemma":0.08849719,"teacher_disagreement_score":0.11369512,"about_ca_system_score_codex":0.0013284164,"about_ca_system_score_gemma":0.000742975,"threshold_uncertainty_score":0.22606665},"labels":[],"label_agreement":null},{"id":"W2308936313","doi":"10.1130/l471.1","title":"A synthesis of Jurassic and Early Cretaceous crustal evolution along the southern margin of the Arctic Alaska–Chukotka microplate and implications for defining tectonic boundaries active during opening of Arctic Ocean basins","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Paleontology; Arctic; Cretaceous; Mesozoic; Tectonics; Structural basin; Plate tectonics; Paleozoic; Proterozoic; Zircon; Oceanography","score_opus":0.009396611145979965,"score_gpt":0.19016238609546096,"score_spread":0.18076577494948098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2308936313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78286827,0.15453468,0.006530413,0.00081896083,0.00030751358,0.000110447596,0.029900217,0.00016097516,0.024768602],"genre_scores_gemma":[0.89755124,0.07557659,0.0071855946,0.00013271169,0.0000808837,0.00010834879,0.015350969,0.00003925697,0.0039744186],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997824,0.000016659129,0.00005849602,0.00009301663,0.000026506626,0.000022962598],"domain_scores_gemma":[0.99938166,0.00015688178,0.00014259,0.000039625545,0.00023168825,0.000047523594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047407008,0.00053645327,0.0005557379,0.006539426,0.0006102825,0.001530963,0.00021512348,0.00028342524,0.0049590063],"category_scores_gemma":[0.00088219566,0.00027894272,0.0005021215,0.008987306,0.000324902,0.0009698097,0.0005282905,0.00025989563,0.000339334],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072685274,0.00009544495,0.40858725,0.01786864,0.00203403,0.0016109586,0.014510379,0.013992745,0.035928067,0.0061492277,0.0064740386,0.49202228],"study_design_scores_gemma":[0.000011191677,0.00007918695,0.93252665,0.0026888284,0.0010796024,0.00022182074,0.0048772204,0.0010937627,0.0013623331,0.0011737183,0.05484381,0.00004200341],"about_ca_topic_score_codex":0.059125535,"about_ca_topic_score_gemma":0.11788007,"teacher_disagreement_score":0.059125535,"about_ca_system_score_codex":0.0017897852,"about_ca_system_score_gemma":0.0026713451,"threshold_uncertainty_score":0.11756277},"labels":[],"label_agreement":null},{"id":"W2317622691","doi":"10.1130/l123.1","title":"Coseismic, dilational-fault and extension-fracture related pit chain formation in Iceland: Analog for pit chains on Mars","year":2011,"lang":"en","type":"article","venue":"Lithosphere","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University","keywords":"Geology; Fault scarp; Basalt; Lava; Echelon formation; Impact crater; Fluvial; Fault (geology); Mars Exploration Program; Geomorphology; Graben; Rift; Volcano; Sedimentary rock; Petrology; Geochemistry; Seismology; Structural basin","score_opus":0.017417959728370253,"score_gpt":0.21789837301176454,"score_spread":0.20048041328339428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317622691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975177,0.0001210631,0.00010046089,0.00002574219,0.0000040411483,0.000012596046,0.00026648608,0.00000736736,0.0019445418],"genre_scores_gemma":[0.9992974,0.0000927097,0.00013384999,0.000008265512,0.000005602665,0.0000039773468,0.00023584449,0.000001980632,0.00022036648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.00000908593,0.00000483672,0.00002353782,0.000010337128,0.000031811276],"domain_scores_gemma":[0.9998734,0.000010800916,0.00004738216,0.000014304661,0.000028437931,0.000025556225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101432706,0.00017714771,0.000111565714,0.0008650133,0.00041451544,0.00041631708,0.00026972,0.00019616002,0.0014959866],"category_scores_gemma":[0.00025778217,0.00012092307,0.00012976205,0.0006887593,0.00061319483,0.00019433096,0.00031362812,0.00015348745,0.00014231334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019672909,0.000091469985,0.9693145,0.000046424142,0.000043187258,0.0011492948,0.0008431461,0.0012210069,0.007711266,0.0005338438,0.000600104,0.018248936],"study_design_scores_gemma":[0.0000037036978,0.000023364268,0.9983631,0.000006390019,0.000004037967,0.0002229401,0.00024103781,0.00046737763,0.0001580995,0.00005201094,0.0004566625,0.000001345353],"about_ca_topic_score_codex":0.049665473,"about_ca_topic_score_gemma":0.048996802,"teacher_disagreement_score":0.049665473,"about_ca_system_score_codex":0.00090405165,"about_ca_system_score_gemma":0.00032496522,"threshold_uncertainty_score":0.0987528},"labels":[],"label_agreement":null},{"id":"W2319959760","doi":"10.1130/l149.1","title":"Petrochronologic record of metamorphism and melting in the upper Greater Himalayan sequence, Manaslu–Himal Chuli Himalaya, west-central Nepal","year":2011,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; University of Saskatchewan","funders":"National Science Foundation","keywords":"Monazite; Geology; Metamorphism; Foreland basin; Geochemistry; Metamorphic rock; Paleontology; Sequence (biology); Partial melting; Zircon; Tectonics; Crust","score_opus":0.032970245007104014,"score_gpt":0.19819635729549373,"score_spread":0.1652261122883897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319959760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977266,0.00010814735,0.000086328895,0.000014635246,5.213217e-7,0.0000048279553,0.00021413363,0.000010291595,0.0018345985],"genre_scores_gemma":[0.9993782,0.00009210363,0.0001092364,0.0000044497924,0.000002130807,0.000003421484,0.00015794649,0.0000018914269,0.00025051433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993765,0.000009685734,0.0000067120363,0.000018778039,0.00001323802,0.000013970272],"domain_scores_gemma":[0.9998627,0.00002345629,0.000039384147,0.000017158925,0.000035542696,0.000021898388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009142736,0.00013556395,0.00009745885,0.0017829956,0.0006602042,0.0003955484,0.00022261706,0.0001366668,0.0011047344],"category_scores_gemma":[0.0002843742,0.00015968048,0.00007421808,0.0016906108,0.00043525695,0.00022178,0.00036665582,0.0001187446,0.00018280305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007273973,0.00004289459,0.93725806,0.00010664226,0.000076696175,0.0014388991,0.0073593096,0.00080243294,0.023255251,0.0004932264,0.00027657757,0.0288173],"study_design_scores_gemma":[0.0000012777558,0.000013636454,0.99761176,0.000006671882,0.000012285041,0.00035235705,0.00052498584,0.00023795773,0.0005267688,0.000030076902,0.0006796032,0.0000026266423],"about_ca_topic_score_codex":0.04579987,"about_ca_topic_score_gemma":0.11096099,"teacher_disagreement_score":0.04579987,"about_ca_system_score_codex":0.0005443774,"about_ca_system_score_gemma":0.00051015336,"threshold_uncertainty_score":0.0910666},"labels":[],"label_agreement":null},{"id":"W2323909420","doi":"10.1130/l103.1","title":"Nature of the Moho transition in NW Canada from combined near-vertical and wide-angle seismic-reflection studies","year":2010,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Crust; Seismogram; Seismology; Mantle (geology); Décollement; Lithosphere; Transition zone; Tectonics; Subduction; Reflection (computer programming); Geophysics","score_opus":0.005462231441955363,"score_gpt":0.1898973542016639,"score_spread":0.18443512275970853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323909420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971482,0.00007859526,0.0006089096,0.000026341206,0.0000012472459,0.0000068879626,0.00039519783,0.00002616672,0.001708508],"genre_scores_gemma":[0.99890494,0.0000705309,0.0004367281,0.0000042900597,5.050427e-7,0.0000010413974,0.0003324688,0.0000052077817,0.0002442296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991786,0.0000041798744,0.0000033874746,0.000019958703,0.000030844385,0.000023836239],"domain_scores_gemma":[0.99991846,0.000009326305,0.000010425679,0.0000059760337,0.000036905603,0.000018872812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112382535,0.00020984707,0.00011171741,0.0004811929,0.00046500535,0.0006989031,0.0004340093,0.00023494872,0.0008906378],"category_scores_gemma":[0.00040371585,0.00016835857,0.00023256971,0.00073080976,0.0003514264,0.00021327824,0.00034767477,0.0001713198,0.00008102858],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040127547,0.000074646625,0.6851248,0.00015086096,0.00020229537,0.0008067346,0.0010146234,0.20696771,0.05046672,0.0036305191,0.0008655136,0.05029428],"study_design_scores_gemma":[0.000034905937,0.000050717757,0.7958005,0.000032538584,0.00012086829,0.0001755895,0.0014873692,0.19156192,0.0072979825,0.00078864215,0.0025881638,0.000060864444],"about_ca_topic_score_codex":0.9188823,"about_ca_topic_score_gemma":0.9495334,"teacher_disagreement_score":0.08111769,"about_ca_system_score_codex":0.0036665155,"about_ca_system_score_gemma":0.004547249,"threshold_uncertainty_score":0.16319078},"labels":[],"label_agreement":null},{"id":"W2327966818","doi":"10.1130/l167.1","title":"The spreading-rate dependence of anomalous skewness of Pacific plate magnetic anomaly 32: Revisited","year":2011,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Institut de Physique du Globe de Paris; National Science Foundation","keywords":"Skewness; Magnetic anomaly; Geology; Paleomagnetism; Anomaly (physics); Kurtosis; Geodesy; Asymmetry; Residual; Geophysics; Seismology; Physics; Statistics; Mathematics; Condensed matter physics","score_opus":0.01007390583748636,"score_gpt":0.2061120256234684,"score_spread":0.19603811978598204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2327966818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973441,0.00006582202,0.0020809162,0.0000144135265,0.0000020209015,0.000004795955,0.000076931734,0.000024285755,0.00038680978],"genre_scores_gemma":[0.99939334,0.000021434767,0.00041453194,0.0000046043688,0.0000015727624,0.0000023127836,0.00011424503,0.000008526731,0.000039467985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995529,0.00012346279,0.000048628903,0.00011089191,0.000114248665,0.000049881903],"domain_scores_gemma":[0.99352527,0.0027987582,0.0019547006,0.0009535362,0.0005589272,0.00020883462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015160239,0.00041599252,0.00025751686,0.0008184537,0.00012931786,0.0004970308,0.0004712377,0.0003016755,0.0007544326],"category_scores_gemma":[0.007529863,0.0002352392,0.0005603135,0.00045543438,0.00058610697,0.00051882793,0.00053404423,0.0005981697,0.000170129],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005485841,0.000056674176,0.71587634,0.0000835546,0.0003165714,0.00053753523,0.0003240581,0.013218983,0.25684583,0.00084635353,0.00007726793,0.011268374],"study_design_scores_gemma":[0.000026686905,0.00043406096,0.8695829,0.000015110792,0.00010909435,0.0011095593,0.0001531316,0.06870752,0.057962887,0.0015349926,0.00030384466,0.00006017257],"about_ca_topic_score_codex":0.0026759503,"about_ca_topic_score_gemma":0.0015602412,"teacher_disagreement_score":0.0026759503,"about_ca_system_score_codex":0.0002493528,"about_ca_system_score_gemma":0.0002342497,"threshold_uncertainty_score":0.0080176},"labels":[],"label_agreement":null},{"id":"W2345828295","doi":"10.1130/l531.1","title":"Record of orogenic cyclicity in the Alberta foreland basin, Canadian Cordillera","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"Shell Canada","keywords":"Zircon; Geology; Foreland basin; Paleontology; Structural basin; Cretaceous; Sedimentary rock; Provenance; Mesozoic; Fluvial; Sedimentary basin; Group (periodic table); Passive margin; Geochemistry; Rift","score_opus":0.00835301995471322,"score_gpt":0.17755249031538775,"score_spread":0.16919947036067454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2345828295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956741,0.00054293504,0.00008255387,0.000054100714,0.0000027776236,0.000008258098,0.0010449021,0.000017375636,0.0025730822],"genre_scores_gemma":[0.9975569,0.00035540192,0.00024586168,0.00002161872,0.00000252831,0.000004673116,0.000977073,0.000004424329,0.0008314293],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982244,0.000007536355,0.0000075781204,0.00004971268,0.000063817606,0.00004894672],"domain_scores_gemma":[0.9994149,0.000025395972,0.00011558087,0.000026141302,0.00032930324,0.00008866542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020527489,0.00023716764,0.00016976052,0.0028321014,0.0013990932,0.00087070593,0.0005375576,0.00018200424,0.001139414],"category_scores_gemma":[0.0006790891,0.00015639221,0.00011156592,0.0031382083,0.0006908686,0.00017537379,0.00045605694,0.0001674267,0.00010959644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000827089,0.000014098949,0.9729436,0.00003271121,0.00005938523,0.00011855267,0.0011086345,0.00032827258,0.0047673713,0.00026267016,0.0004995471,0.019782405],"study_design_scores_gemma":[0.0000010311454,0.0000027214753,0.9990005,0.00000380376,0.0000063680277,0.000018222163,0.00015119163,0.0001079942,0.000112784,0.000012912849,0.00057990104,0.000002577425],"about_ca_topic_score_codex":0.9735702,"about_ca_topic_score_gemma":0.99239385,"teacher_disagreement_score":0.026429772,"about_ca_system_score_codex":0.0102600185,"about_ca_system_score_gemma":0.0060075466,"threshold_uncertainty_score":0.07444197},"labels":[],"label_agreement":null},{"id":"W2398605979","doi":"10.1130/l508.1","title":"Upper-crustal cooling of the Wrangellia composite terrane in the northern St. Elias Mountains, western Canada","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Terrane; Thermochronology; Geology; Fission track dating; Subduction; Zircon; Paleontology; Cretaceous; North American Plate; Forearc; Seismology; Tectonics; Geomorphology","score_opus":0.006980236738239949,"score_gpt":0.17512675534022323,"score_spread":0.1681465186019833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2398605979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998667,0.00014442457,0.000016856793,0.000023175597,0.0000011207568,0.000002860913,0.000343322,0.0000045264987,0.0007968318],"genre_scores_gemma":[0.9981516,0.000117591015,0.00007739303,0.000012845977,0.0000012174412,0.0000036000831,0.00048737053,0.0000031798022,0.0011452569],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998772,0.0000066949647,0.000005257133,0.00003379269,0.000030458776,0.00004648991],"domain_scores_gemma":[0.9997216,0.000014661755,0.000045699573,0.00001116525,0.00014261757,0.00006428841],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015454674,0.0001700852,0.00014403212,0.0009019322,0.0010426805,0.00065298204,0.00036938075,0.00013530708,0.00094809185],"category_scores_gemma":[0.00034335352,0.00011520857,0.00012475136,0.00092252553,0.00026567598,0.00021520576,0.00046036008,0.00018497478,0.00012922639],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007149721,0.000021615802,0.9793336,0.000028993965,0.00005236992,0.00041504498,0.002128744,0.00033511777,0.0043491283,0.0000709285,0.0005034548,0.012689564],"study_design_scores_gemma":[9.771002e-7,0.0000028946492,0.99856853,0.0000038073003,0.000003673361,0.000028814,0.0006217163,0.000062188345,0.00009431193,0.0000029630312,0.0006083286,0.0000017866697],"about_ca_topic_score_codex":0.94290745,"about_ca_topic_score_gemma":0.9879871,"teacher_disagreement_score":0.057092547,"about_ca_system_score_codex":0.005343664,"about_ca_system_score_gemma":0.003624741,"threshold_uncertainty_score":0.114857495},"labels":[],"label_agreement":null},{"id":"W2471443014","doi":"10.1130/l524.1","title":"Corrugated architecture of the Okanagan Valley shear zone and the Shuswap metamorphic complex, Canadian Cordillera","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University; National Science Foundation","keywords":"Geology; Metamorphic rock; Shear zone; Architecture; Shear (geology); Seismology; Paleontology; Geomorphology; Archaeology; Geography; Tectonics","score_opus":0.009090009297603823,"score_gpt":0.16499265629153526,"score_spread":0.15590264699393144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2471443014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99501556,0.0002494393,0.0000708127,0.00003992685,0.0000020943905,0.000014503139,0.00032497855,0.000012574472,0.004270064],"genre_scores_gemma":[0.9987853,0.00009711405,0.00015137618,0.000008661187,6.800938e-7,0.0000050925332,0.00025223842,0.00000336025,0.00069622876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996289,0.000013525471,0.000017301998,0.00010817906,0.00009104831,0.0001410337],"domain_scores_gemma":[0.99957186,0.000021889222,0.000077645935,0.000021991917,0.00022119183,0.00008544989],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014941566,0.00033531754,0.00026461374,0.00363636,0.0022831322,0.0015082986,0.0005976696,0.0002486631,0.002790847],"category_scores_gemma":[0.00080571807,0.00030093922,0.00018843076,0.004086416,0.0017211926,0.0002568673,0.0010803754,0.00026062664,0.0002129789],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010698992,0.000015304266,0.9592602,0.00007277969,0.00008021739,0.00033319267,0.002456194,0.0006995964,0.007150073,0.0011110962,0.00045813603,0.028256198],"study_design_scores_gemma":[0.0000015474892,0.000004494875,0.99845624,0.0000075496287,0.000007834665,0.000040239524,0.0007124655,0.00016549481,0.00008663393,0.000033021435,0.00048081242,0.0000036096471],"about_ca_topic_score_codex":0.96995294,"about_ca_topic_score_gemma":0.99359107,"teacher_disagreement_score":0.030047059,"about_ca_system_score_codex":0.01192526,"about_ca_system_score_gemma":0.0105716605,"threshold_uncertainty_score":0.08652425},"labels":[],"label_agreement":null},{"id":"W2491848358","doi":"10.1130/l525.1","title":"Detrital zircon ages indicate an Early Cretaceous episode of blueschist-facies metamorphism in southern Alaska: Implications for the Mesozoic paleogeography of the northern Cordillera","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Blueschist; Schist; Zircon; Terrane; Metamorphism; Facies; Sedimentary depositional environment; Cretaceous; Geochemistry; Paleontology; Subduction; Metamorphic rock; Eclogite; Structural basin; Tectonics","score_opus":0.0121753276353693,"score_gpt":0.1994761092603344,"score_spread":0.1873007816249651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2491848358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994072,0.000088347115,0.00002712446,0.000005704741,6.5803937e-7,0.0000010386985,0.00006932137,0.0000035980174,0.00039695],"genre_scores_gemma":[0.99922454,0.00007964384,0.00008150688,0.0000040745936,8.357307e-7,0.0000010591431,0.00012609208,8.3801405e-7,0.0004813093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995184,0.0000021975734,0.0000051114507,0.000020625921,0.000010773739,0.000009517009],"domain_scores_gemma":[0.9999194,0.000006675145,0.000031910335,0.000005517827,0.000020757143,0.000015750866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116675335,0.00013311325,0.000102582555,0.00069559435,0.00041429102,0.00043675033,0.00011747096,0.00013113293,0.0011865327],"category_scores_gemma":[0.00020121683,0.00011787288,0.00006989909,0.00040867532,0.00019625561,0.00017619894,0.00034808554,0.00008813307,0.00013900053],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005653397,0.000008009677,0.9730243,0.00002103933,0.000013243282,0.0002667008,0.0009548928,0.00009786152,0.017571755,0.000038926515,0.000035477453,0.007911174],"study_design_scores_gemma":[6.526301e-7,0.00000596565,0.9992859,0.0000021244014,0.00000376527,0.000063934516,0.00015219889,0.000044696917,0.0002972493,0.000004545982,0.00013845936,6.4643507e-7],"about_ca_topic_score_codex":0.05976504,"about_ca_topic_score_gemma":0.17360713,"teacher_disagreement_score":0.05976504,"about_ca_system_score_codex":0.00069360115,"about_ca_system_score_gemma":0.00025792056,"threshold_uncertainty_score":0.11883432},"labels":[],"label_agreement":null},{"id":"W2514231633","doi":"10.1130/l557.1","title":"Detrital zircon record of mid-Paleozoic convergent margin activity in the northern U.S. Rocky Mountains: Implications for the Antler orogeny and early evolution of the North American Cordillera","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Idaho State University; National Science Foundation","keywords":"Geology; Allochthon; Laurentia; Orogeny; Zircon; Devonian; Paleozoic; Paleontology; Provenance; Ordovician; Terrane; Passive margin; Paleocurrent; Baltica; Carboniferous; Nappe; Rift; Clastic rock; Sedimentary rock; Structural basin; Tectonics","score_opus":0.010559383889263118,"score_gpt":0.20154081487520867,"score_spread":0.19098143098594556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2514231633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990901,0.00007042922,0.000027278167,0.000011743869,8.863609e-7,0.0000013895694,0.00033493785,0.000003606748,0.00045968348],"genre_scores_gemma":[0.9988696,0.00007441793,0.00013393119,0.00000936057,0.0000027155372,0.0000027051542,0.0005200627,0.0000018709395,0.00038535547],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999645,0.0000023666432,0.000003527721,0.000010991024,0.000009903197,0.000008730943],"domain_scores_gemma":[0.99991226,0.0000072489356,0.000027755355,0.0000064874957,0.000029670877,0.000016513888],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010197164,0.000108263564,0.000094920775,0.000721691,0.00035294585,0.0002616377,0.00013029993,0.00008808812,0.0007752358],"category_scores_gemma":[0.00016046027,0.00008149337,0.00005237075,0.00050011487,0.000104539795,0.00010309957,0.0002837605,0.000095100346,0.000105008374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006029719,0.000018635623,0.9786325,0.000016049155,0.000017323577,0.000110798115,0.0006427145,0.000075688644,0.008810728,0.000092370596,0.00022463134,0.011298266],"study_design_scores_gemma":[0.0000010357413,0.0000055564337,0.9992741,0.0000022142788,0.00000582472,0.000026206304,0.000083736784,0.00006060145,0.00023214212,0.0000050898093,0.0003030749,4.807879e-7],"about_ca_topic_score_codex":0.088899665,"about_ca_topic_score_gemma":0.3264399,"teacher_disagreement_score":0.088899665,"about_ca_system_score_codex":0.00042471717,"about_ca_system_score_gemma":0.000318745,"threshold_uncertainty_score":0.17676443},"labels":[],"label_agreement":null},{"id":"W2515950217","doi":"10.1130/l537.1","title":"Provenance approaches in polydeformed metasedimentary successions: Determining nearest neighboring cratons during the deposition of the Paleoproterozoic Murmac Bay Group","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Craton; Geochronology; Provenance; Zircon; Geology; Geochemistry; Bay; Ecological succession; Paleontology; Sedimentary depositional environment; Tectonics; Structural basin","score_opus":0.014066263297013394,"score_gpt":0.1868992102588938,"score_spread":0.17283294696188042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515950217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942814,0.00069021963,0.0019452281,0.00003028762,0.000013232363,0.000021818269,0.00045092136,0.000035397054,0.0025314076],"genre_scores_gemma":[0.9957646,0.0002695902,0.0027592517,0.000017920589,0.00000668045,0.000011035501,0.0005038186,0.000021043123,0.0006460786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996661,0.000030831707,0.000042922824,0.00012052753,0.00008511365,0.00005456351],"domain_scores_gemma":[0.999005,0.00009632564,0.00025542738,0.000115699084,0.00044943966,0.00007808742],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006287873,0.00019524846,0.00022653263,0.0026118662,0.0009164727,0.0010357911,0.0004292539,0.00023518312,0.0014104613],"category_scores_gemma":[0.002126618,0.00018889108,0.0001989546,0.0017370858,0.00045237795,0.00035067086,0.0011013326,0.0002049983,0.00026738312],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027371533,0.00002333362,0.9127758,0.00012668682,0.00009417395,0.0008814106,0.004198642,0.0009438628,0.03204775,0.0007560096,0.00021704391,0.047661494],"study_design_scores_gemma":[0.000010281005,0.000033770903,0.9892426,0.000054508753,0.00006151039,0.00032796297,0.0010398467,0.0012112588,0.0035237072,0.00018284674,0.0043017827,0.000010000441],"about_ca_topic_score_codex":0.11750158,"about_ca_topic_score_gemma":0.32647783,"teacher_disagreement_score":0.11750158,"about_ca_system_score_codex":0.0010203939,"about_ca_system_score_gemma":0.000992434,"threshold_uncertainty_score":0.2336353},"labels":[],"label_agreement":null},{"id":"W2534777955","doi":"10.1130/l580.1","title":"The end of Midcontinent Rift magmatism and the paleogeography of Laurentia","year":2017,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Laurentia; Geology; Paleomagnetism; Rift; Paleontology; Zircon; Magmatism; Volcanic rock; Basalt; Apparent polar wander; Geochemistry; Earth science; Volcano; Tectonics","score_opus":0.0041608271035264086,"score_gpt":0.1777745046295144,"score_spread":0.173613677525988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2534777955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99390656,0.00070287485,0.00006106776,0.00013341426,0.00000352859,0.0000024745038,0.0002009723,0.000011899557,0.0049770996],"genre_scores_gemma":[0.9987192,0.00025510968,0.00015092998,0.000024353776,0.000005906037,0.0000025261675,0.0001948134,0.0000051720267,0.000641911],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985564,0.000016486345,0.000008249169,0.000054780976,0.000023990855,0.00004094236],"domain_scores_gemma":[0.999747,0.000022755237,0.000109933666,0.000016602185,0.000054691085,0.000049019865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002298025,0.00012903726,0.00014019133,0.0009011449,0.00068230287,0.00094130746,0.00028219732,0.0001314316,0.0010592095],"category_scores_gemma":[0.0005405961,0.000085133375,0.00010229965,0.00047358,0.0003843833,0.00031286658,0.0004583072,0.00016921606,0.0001956344],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015002195,0.000020321377,0.93573076,0.00008517389,0.00007943108,0.00071924814,0.004474139,0.00050541956,0.016884796,0.00097025465,0.00054450915,0.03983594],"study_design_scores_gemma":[0.0000016597029,0.0000067249193,0.9968905,0.000018989185,0.000006512138,0.000086991626,0.0002695804,0.0001074899,0.00024814147,0.000043812688,0.002316117,0.0000035448447],"about_ca_topic_score_codex":0.1705332,"about_ca_topic_score_gemma":0.46423584,"teacher_disagreement_score":0.1705332,"about_ca_system_score_codex":0.0019715175,"about_ca_system_score_gemma":0.0009350694,"threshold_uncertainty_score":0.3390811},"labels":[],"label_agreement":null},{"id":"W2547696873","doi":"10.1130/l559.1","title":"Oroclinal buckling of the Armorican ribbon continent: An alternative tectonic model for Pangean amalgamation and Variscan orogenesis","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Gondwana; Geology; Supercontinent; Paleozoic; Paleontology; Subduction; Laurasia; Paleomagnetism; Terrane; Ophiolite; Tectonics; Craton","score_opus":0.016850791823152075,"score_gpt":0.20998602519023782,"score_spread":0.19313523336708574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2547696873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92906964,0.0011762782,0.011950115,0.002387582,0.000115878225,0.00006130966,0.00026177993,0.00030801946,0.054669343],"genre_scores_gemma":[0.9936255,0.0002607541,0.0018460696,0.00012628414,0.000030225901,0.000024596837,0.0001165064,0.000029206876,0.0039408533],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980694,0.00004160547,0.000009729244,0.000067158486,0.000016759563,0.000057726083],"domain_scores_gemma":[0.99986565,0.000011369005,0.00003987558,0.00002211867,0.000022368898,0.000038500046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034007238,0.00050052645,0.00043734148,0.0009735145,0.00090439373,0.0022553222,0.001248773,0.00094327715,0.0065079033],"category_scores_gemma":[0.0005089687,0.00031915127,0.0007111843,0.00083099667,0.00276443,0.0013755347,0.0010847037,0.0005200826,0.00086258847],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012587295,0.00024587786,0.14513518,0.00045291384,0.00026295317,0.0036048952,0.007977878,0.12129551,0.030450301,0.6115105,0.0048724804,0.07293284],"study_design_scores_gemma":[0.0004950151,0.0006512731,0.2599308,0.00033042862,0.00028049934,0.0023615651,0.008272289,0.41163066,0.0027170132,0.26601493,0.047062792,0.00025288278],"about_ca_topic_score_codex":0.03164988,"about_ca_topic_score_gemma":0.031360947,"teacher_disagreement_score":0.03164988,"about_ca_system_score_codex":0.0025896365,"about_ca_system_score_gemma":0.0012759677,"threshold_uncertainty_score":0.06293136},"labels":[],"label_agreement":null},{"id":"W2547829642","doi":"10.1130/l576.1","title":"Interference folding and orocline implications: A structural study of the Ponga Unit, Cantabrian orocline, northern Spain","year":2016,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Victoria","funders":"","keywords":"Geology; Unit (ring theory); Folding (DSP implementation); Interference (communication); Seismology; Paleontology; Engineering; Telecommunications; Structural engineering","score_opus":0.016043034185046382,"score_gpt":0.21995791004540866,"score_spread":0.20391487586036228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2547829642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979373,0.00031218104,0.00008036955,0.000021383708,0.0000019958084,0.000016264485,0.00014933468,0.0000070353562,0.0014741193],"genre_scores_gemma":[0.9986634,0.00017433614,0.0002660723,0.000012537163,0.0000030454673,0.000015036062,0.0003941034,0.000005031947,0.00046638396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972254,0.00002770104,0.000013264437,0.00012625844,0.0000402482,0.000069980815],"domain_scores_gemma":[0.99979895,0.000024687022,0.00007620618,0.000022987542,0.000055304245,0.000021935075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026476037,0.00046666941,0.0003832881,0.0013917615,0.00061099016,0.0012237314,0.0009580143,0.00047066598,0.0016324128],"category_scores_gemma":[0.0006767826,0.0002146893,0.00029271375,0.0016285101,0.001012521,0.00038557698,0.0010133268,0.00020838836,0.00023386854],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007015059,0.00013969037,0.933762,0.00023440967,0.00017482441,0.0010877058,0.003686451,0.0018737024,0.010397487,0.00035946156,0.00035850707,0.047224205],"study_design_scores_gemma":[0.000015793636,0.000032216038,0.9982868,0.000014122627,0.000013704655,0.000057022193,0.00061988423,0.00024888318,0.00008542708,0.000032924236,0.0005902135,0.000002923332],"about_ca_topic_score_codex":0.17659467,"about_ca_topic_score_gemma":0.24520665,"teacher_disagreement_score":0.17659467,"about_ca_system_score_codex":0.0021890148,"about_ca_system_score_gemma":0.0009715168,"threshold_uncertainty_score":0.35113358},"labels":[],"label_agreement":null},{"id":"W2597602745","doi":"10.1130/l631.1","title":"Diffusion-zoned pyroxenes in an isotopically heterogeneous mantle lithosphere beneath the Dunedin Volcanic Group, New Zealand, and their implications for intraplate alkaline magma sources","year":2017,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Research and Innovation Foundation; Canada Excellence Research Chairs, Government of Canada; University of Stirling; Canada Research Chairs","keywords":"Geology; Xenolith; Geochemistry; Mantle (geology); Metasomatism; Trace element; Radiogenic nuclide; Peridotite; Lithosphere; Paleontology; Tectonics","score_opus":0.015016371848174326,"score_gpt":0.22439863422294237,"score_spread":0.20938226237476804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2597602745","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99929917,0.00014130028,0.000033960125,0.00001647783,8.6308097e-7,0.0000021556343,0.00003964654,0.0000013443151,0.000465104],"genre_scores_gemma":[0.99941826,0.00015334357,0.00006936836,0.000006289089,0.0000015904096,0.000002278839,0.00005789646,0.0000018340347,0.00028926015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999176,0.0000039472293,0.0000056751323,0.00002958418,0.00001959941,0.000023548984],"domain_scores_gemma":[0.9998884,0.000015216776,0.000039979073,0.0000057766333,0.000025347232,0.000025304338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016375566,0.00024690802,0.0002272465,0.0013618785,0.00061114633,0.0009981437,0.00037538097,0.00024477014,0.0011682343],"category_scores_gemma":[0.00036866503,0.00026906427,0.0001449258,0.0007438248,0.00097606296,0.00052618387,0.00055645395,0.00020652013,0.00013243363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034060213,0.000042852243,0.70788467,0.000107120955,0.00007878525,0.0012290354,0.0046647545,0.00035774923,0.27082455,0.0003020941,0.000057405232,0.014110453],"study_design_scores_gemma":[0.0000058539013,0.00001590468,0.99766207,0.000003943978,0.000010923821,0.00016889651,0.00078449096,0.00014344686,0.0008793875,0.000044781293,0.00027587498,0.000004482832],"about_ca_topic_score_codex":0.11272398,"about_ca_topic_score_gemma":0.18605265,"teacher_disagreement_score":0.11272398,"about_ca_system_score_codex":0.0014483478,"about_ca_system_score_gemma":0.00045687277,"threshold_uncertainty_score":0.2241357},"labels":[],"label_agreement":null},{"id":"W2601287886","doi":"10.1130/l609.1","title":"Geology and in situ stress of the MH-2 borehole, Idaho, USA: Insights into western Snake River Plain structure from geothermal exploration drilling","year":2017,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"U.S. Air Force; University of Alberta; Natural Sciences and Engineering Research Council of Canada; Utah State University; U.S. Department of Energy","keywords":"Geology; Borehole; Basalt; Drilling; Geothermal gradient; Lithology; Geochemistry; Sedimentary rock; Petrology; Paleontology","score_opus":0.014393439724470736,"score_gpt":0.21654029397565008,"score_spread":0.20214685425117934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2601287886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99815637,0.000020607215,0.000106217405,0.000019450363,0.0000014879731,0.000007362571,0.0004512051,0.000009953657,0.0012272198],"genre_scores_gemma":[0.9988102,0.000034996916,0.00036069108,0.000015379102,0.0000025906515,0.000012003317,0.0003918645,0.0000032347218,0.000369146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992836,0.000006867678,0.000005759915,0.000019407762,0.00002566473,0.000013990929],"domain_scores_gemma":[0.99983716,0.000016086275,0.000047905127,0.000011085307,0.00005529623,0.000032365733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014047034,0.00017423654,0.00012962577,0.0009914794,0.0003552723,0.00037827584,0.0003683127,0.00021438471,0.00064394885],"category_scores_gemma":[0.00028425007,0.00015056913,0.00008537451,0.0008300142,0.00029909177,0.00025073122,0.0005444021,0.00016027738,0.00015976393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000087412234,0.000082044964,0.9741856,0.000024704332,0.000016138487,0.00027442112,0.0012438959,0.00037603313,0.014976036,0.000105744206,0.00042061074,0.008207338],"study_design_scores_gemma":[0.0000019716256,0.0000073186625,0.9987704,0.0000029822006,0.0000026674693,0.000036697806,0.00034108767,0.00034331813,0.00033080453,0.0000103623215,0.00015078206,0.0000016112948],"about_ca_topic_score_codex":0.06508027,"about_ca_topic_score_gemma":0.24588884,"teacher_disagreement_score":0.06508027,"about_ca_system_score_codex":0.0005968812,"about_ca_system_score_gemma":0.0004513838,"threshold_uncertainty_score":0.12940294},"labels":[],"label_agreement":null},{"id":"W2606981039","doi":"10.1130/l643.1","title":"A Pangean rim of fire: Reviewing the Triassic of western Laurentia","year":2017,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"","keywords":"Laurentia; Geology; Terrane; Subduction; Foreland basin; Paleontology; Context (archaeology); Zircon; Plate tectonics; Earth science; Tectonics","score_opus":0.052625748666945284,"score_gpt":0.2508153674637973,"score_spread":0.198189618796852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2606981039","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.45531806,0.49201456,0.0009141698,0.005409208,0.0006715792,0.000028535584,0.0003291887,0.000057663143,0.045257024],"genre_scores_gemma":[0.77216136,0.21881069,0.0011119975,0.0012504181,0.0006530594,0.000018838158,0.00037367828,0.00003669212,0.005583269],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99983346,0.000020278354,0.00002982923,0.00003105348,0.00003277444,0.00005259579],"domain_scores_gemma":[0.9995043,0.0000809769,0.00020894506,0.000018473034,0.0001241142,0.00006312324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055960135,0.00028089838,0.00018846849,0.0036112214,0.00088359043,0.0013799039,0.00048653616,0.00024292181,0.000935237],"category_scores_gemma":[0.0011872121,0.0001152323,0.00014769897,0.0031678847,0.0011933264,0.0014289254,0.000854848,0.00040222442,0.00022909351],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031765955,0.000036342666,0.20291506,0.0058899075,0.00017444347,0.010438742,0.0528083,0.0011847515,0.0115033975,0.01271639,0.014343579,0.6876715],"study_design_scores_gemma":[0.0000051346096,0.00006487082,0.60280186,0.0028551836,0.000109487526,0.0030166213,0.014941049,0.0002582083,0.0014170193,0.0010348446,0.37346584,0.000029909228],"about_ca_topic_score_codex":0.10410903,"about_ca_topic_score_gemma":0.31688488,"teacher_disagreement_score":0.10410903,"about_ca_system_score_codex":0.002905098,"about_ca_system_score_gemma":0.0029918842,"threshold_uncertainty_score":0.2070061},"labels":[],"label_agreement":null},{"id":"W2618146114","doi":"10.1130/l650.1","title":"Age and volcanic stratigraphy of the Eocene Siletzia oceanic plateau in Washington and on Vancouver Island","year":2017,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Terrane; Geology; Zircon; Basement; Sedimentary depositional environment; Basalt; Paleontology; Stratigraphy; Plateau (mathematics); Geochemistry; Sedimentary rock; Volcanic rock; Volcano; Structural basin; Tectonics; Archaeology","score_opus":0.008119232414397519,"score_gpt":0.1889409372217477,"score_spread":0.1808217048073502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618146114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978338,0.00016819191,0.000024948718,0.000014461452,0.0000012013979,0.0000039576453,0.00024953636,0.0000042551515,0.00169961],"genre_scores_gemma":[0.997514,0.00021549915,0.00012083162,0.000010045664,0.0000011237029,0.000004895748,0.0006242395,0.0000026002315,0.0015067966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999348,0.0000038133676,0.000004022107,0.000015541256,0.000022624776,0.000019110093],"domain_scores_gemma":[0.99984205,0.000012725766,0.000029742849,0.0000059080103,0.00006622071,0.000043189913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011846536,0.00013166832,0.00009448568,0.0013492004,0.00063105515,0.00070393283,0.00018966859,0.00013603127,0.0007715626],"category_scores_gemma":[0.00022595214,0.00014037058,0.00007355485,0.0012941363,0.000361844,0.0001504599,0.0003646422,0.0001363406,0.00012389968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031031785,0.0000094680045,0.98279136,0.000018305522,0.000031434785,0.00020421413,0.0012693362,0.00011371194,0.0027572694,0.00008409442,0.0002534694,0.012436394],"study_design_scores_gemma":[9.385895e-7,0.0000035632706,0.9984321,0.000007499059,0.000003966134,0.00003505628,0.00065860763,0.00006506258,0.0000919602,0.0000062772056,0.0006939442,0.0000010927743],"about_ca_topic_score_codex":0.63014084,"about_ca_topic_score_gemma":0.927169,"teacher_disagreement_score":0.36985916,"about_ca_system_score_codex":0.0017958841,"about_ca_system_score_gemma":0.0012004913,"threshold_uncertainty_score":0.74407464},"labels":[],"label_agreement":null},{"id":"W2791509529","doi":"10.1130/l683.1","title":"Late Paleozoic to Triassic arc magmatism north of the Sverdrup Basin in the Canadian Arctic: Evidence from detrital zircon U-Pb geochronology","year":2018,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"","keywords":"Geology; Paleozoic; Paleontology; Sverdrup; Mesozoic; Permian; Zircon; Geochronology; Magmatism; Arctic; Structural basin; Detritus; Early Triassic; Tectonics; Oceanography","score_opus":0.02721686545349423,"score_gpt":0.21430550410037139,"score_spread":0.18708863864687716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791509529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987186,0.0026511317,0.0001874647,0.0003792021,0.00001719009,0.000009967856,0.0008512213,0.000016244485,0.008701581],"genre_scores_gemma":[0.9973116,0.0012455068,0.00022440813,0.000052358315,0.000005367932,0.000002750623,0.00036360705,0.0000066792636,0.00078775414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996271,0.000016324655,0.000016051408,0.00009486724,0.0001250466,0.00012053043],"domain_scores_gemma":[0.99877375,0.000061285216,0.00013438582,0.00004002922,0.00086754304,0.00012297573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006562099,0.0002359092,0.00027969744,0.002803933,0.003538295,0.0015717519,0.0007493904,0.00036281036,0.0017543255],"category_scores_gemma":[0.0012665946,0.00030016413,0.0001828477,0.003086992,0.0016003981,0.0004574426,0.00097252685,0.0003235142,0.00018845375],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020754313,0.0000358477,0.9294997,0.00017495528,0.00012304593,0.00029100277,0.0074267723,0.0005347046,0.007708497,0.0022470488,0.0015454665,0.050205376],"study_design_scores_gemma":[0.0000032228759,0.000005029322,0.9947937,0.000040682244,0.000018561446,0.00005649393,0.0012605399,0.00013118406,0.00025467147,0.00007212472,0.0033569818,0.0000067106917],"about_ca_topic_score_codex":0.9858766,"about_ca_topic_score_gemma":0.9956292,"teacher_disagreement_score":0.01412338,"about_ca_system_score_codex":0.010049977,"about_ca_system_score_gemma":0.017470594,"threshold_uncertainty_score":0.07291806},"labels":[],"label_agreement":null},{"id":"W2888823675","doi":"10.1130/l704.1","title":"Deformation and extensional exhumation of 1.9 Ga high-pressure granulites along the Wholdaia Lake shear zone, south Rae craton, Northwest Territories, Canada","year":2018,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Geology; Granulite; Shear zone; Extensional definition; Craton; Shear (geology); Deformation (meteorology); Seismology; Geochemistry; Sinistral and dextral; High pressure; Geomorphology; Petrology; Tectonics; Structural basin; Oceanography","score_opus":0.004585447076452351,"score_gpt":0.15963515272520787,"score_spread":0.15504970564875553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888823675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969524,0.000064173895,0.00004465003,0.000026740436,0.0000018255672,0.000005899959,0.00086953194,0.000014616862,0.0020201583],"genre_scores_gemma":[0.9982497,0.000058686688,0.00006446707,0.000010241403,0.0000012481903,0.0000031572454,0.00041226635,0.000007648514,0.0011926354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999094,0.0000028903903,0.000004346743,0.000021272572,0.000030022833,0.00003204606],"domain_scores_gemma":[0.9997577,0.000019046962,0.000035096295,0.000012897015,0.00012347536,0.000051781182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013091903,0.00021642559,0.00021160352,0.0013603113,0.0014051234,0.00082125637,0.0005323323,0.0003764426,0.0022812877],"category_scores_gemma":[0.00041025112,0.00027347592,0.00019377365,0.0014189787,0.00079263316,0.00023498162,0.00056475814,0.00023824826,0.0003071955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005203582,0.00008736473,0.9431889,0.00009187671,0.00013081073,0.00054127735,0.0030938475,0.0068833977,0.0270111,0.00037406865,0.0012881889,0.016788833],"study_design_scores_gemma":[0.000004141587,0.000004297629,0.9986864,0.0000043004784,0.0000058279493,0.000020738371,0.0002460377,0.000402966,0.00026481066,0.000007040758,0.0003500001,0.0000033758738],"about_ca_topic_score_codex":0.9230536,"about_ca_topic_score_gemma":0.9578416,"teacher_disagreement_score":0.07694638,"about_ca_system_score_codex":0.005155144,"about_ca_system_score_gemma":0.0030647584,"threshold_uncertainty_score":0.15479898},"labels":[],"label_agreement":null},{"id":"W2895983101","doi":"10.1130/l713.1","title":"Earliest sedimentological evidence for marine ingressions in the eastern North American rift system, Central Atlantic Margin","year":2018,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Ingression; Geology; Rift; Paleontology; Margin (machine learning); Oceanography; Current (fluid); Structural basin; Fishery","score_opus":0.03653089062709338,"score_gpt":0.2653304977471033,"score_spread":0.22879960712000993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895983101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971474,0.0002700387,0.000049357466,0.00007511488,0.0000032106784,0.0000013645162,0.00007948396,0.0000025012896,0.0023716034],"genre_scores_gemma":[0.99940753,0.00018096913,0.000066964836,0.000012720394,0.0000039923634,8.657162e-7,0.000068752415,7.716077e-7,0.00025749442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999944,0.000009150408,0.000007147949,0.00001616042,0.000011852739,0.000011803332],"domain_scores_gemma":[0.9992079,0.00011477318,0.00025823695,0.00004983103,0.00029627775,0.00007300522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003310507,0.000080635626,0.00007576685,0.0007978517,0.0005364405,0.00048511257,0.0001589551,0.00017285417,0.0014459513],"category_scores_gemma":[0.00088195526,0.000114205235,0.000058827693,0.0005478076,0.000718271,0.00029959035,0.00032888545,0.00017737504,0.00012035938],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010547346,0.000014397271,0.9772879,0.000035492565,0.000023383745,0.00019584985,0.00072690815,0.00015094162,0.006195887,0.0004939128,0.00017468954,0.014595273],"study_design_scores_gemma":[0.0000015717308,0.0000062820322,0.9989617,0.000009479292,0.0000053670797,0.000026908538,0.00025970832,0.000047378566,0.00020855141,0.000041889944,0.0004297326,0.0000012624913],"about_ca_topic_score_codex":0.0373498,"about_ca_topic_score_gemma":0.15664676,"teacher_disagreement_score":0.0373498,"about_ca_system_score_codex":0.0005321978,"about_ca_system_score_gemma":0.0004293425,"threshold_uncertainty_score":0.074264765},"labels":[],"label_agreement":null},{"id":"W2896457435","doi":"10.1130/l731.1","title":"Eocene Basalt of Summit Creek: Slab breakoff magmatism in the central Washington Cascades, USA","year":2018,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Magmatism; Basalt; Geochemistry; Terrane; Subduction; Accretion (finance); Mantle (geology); Tectonics; Paleontology","score_opus":0.01068586161940186,"score_gpt":0.20643607536856795,"score_spread":0.1957502137491661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896457435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98911744,0.00045549756,0.000053629974,0.00018709329,0.000006720803,0.000019793762,0.00069324183,0.000019513516,0.009447066],"genre_scores_gemma":[0.9946437,0.00053397135,0.0001585061,0.00005620395,0.00000662515,0.000011574472,0.00070856995,0.000005932435,0.00387493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999578,0.000001548633,0.0000018381811,0.000014382748,0.000012414724,0.000012055954],"domain_scores_gemma":[0.99991965,0.0000037845225,0.000020225809,0.0000024482042,0.000029803905,0.000024086432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006949049,0.00016487464,0.00009493897,0.0011753523,0.0012797145,0.0007196434,0.0002328395,0.00023341563,0.0031102572],"category_scores_gemma":[0.00015099111,0.00011090182,0.00006989203,0.00091765873,0.00031855516,0.00034735573,0.0003954762,0.00030413797,0.00028603862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095601885,0.000091246395,0.92104965,0.000102987025,0.000052449996,0.0016225706,0.0059241517,0.00036754805,0.025609383,0.0006545033,0.0026720252,0.041757904],"study_design_scores_gemma":[0.0000015549126,0.000008193849,0.99411327,0.000024286328,0.0000058468568,0.00006707301,0.001259408,0.00010722889,0.00039611684,0.000038629576,0.00397587,0.0000025576003],"about_ca_topic_score_codex":0.477375,"about_ca_topic_score_gemma":0.7942849,"teacher_disagreement_score":0.477375,"about_ca_system_score_codex":0.0023789452,"about_ca_system_score_gemma":0.0014437739,"threshold_uncertainty_score":0.94919276},"labels":[],"label_agreement":null},{"id":"W2897433433","doi":"10.1130/l724.1","title":"Structural evolution of a crustal-scale shear zone through a decreasing temperature regime: The Yukon River shear zone, Yukon-Tanana terrane, Northern Cordillera","year":2018,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia; Simon Fraser University; University of Ottawa; Okanagan University College; Geological Survey of Canada","funders":"","keywords":"Geology; Shear zone; Terrane; Metamorphism; Shear (geology); Zircon; Shearing (physics); Permian; Petrology; Paleontology; Seismology; Geomorphology; Tectonics; Structural basin","score_opus":0.008541801812509426,"score_gpt":0.1990491356624444,"score_spread":0.19050733384993496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897433433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989029,0.00012701518,0.000058105667,0.000013562712,0.0000014693844,0.0000033123702,0.00019682273,0.000011116493,0.0006857087],"genre_scores_gemma":[0.9990853,0.00007100124,0.00014789168,0.000008863377,7.415505e-7,0.000004247134,0.00029671358,0.000005275607,0.00037998066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989355,0.000004315514,0.000006391385,0.00004661769,0.000019917376,0.000029217097],"domain_scores_gemma":[0.9998254,0.000007901484,0.000037429494,0.000010332678,0.000086948785,0.000031945638],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000108175234,0.00024339453,0.0002208747,0.0012612855,0.00094383815,0.0007980992,0.00034557888,0.00028768147,0.0011747775],"category_scores_gemma":[0.00025911996,0.00019703373,0.00019100921,0.0016215012,0.00068684603,0.0002624164,0.00061253615,0.00020514982,0.00017343528],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001154867,0.000019685953,0.9417422,0.00007101161,0.000107003274,0.00033465849,0.002381929,0.0006684797,0.040738273,0.0003337258,0.00025792868,0.013229583],"study_design_scores_gemma":[0.0000016838084,0.000006500782,0.99873465,0.0000035610954,0.000008267715,0.000044214845,0.0004620806,0.00016454574,0.00025321354,0.000013506221,0.00030425523,0.0000034990317],"about_ca_topic_score_codex":0.4182531,"about_ca_topic_score_gemma":0.6505211,"teacher_disagreement_score":0.58174694,"about_ca_system_score_codex":0.0023693216,"about_ca_system_score_gemma":0.001839615,"threshold_uncertainty_score":0.83163714},"labels":[],"label_agreement":null},{"id":"W2897791207","doi":"10.1130/l1001.1","title":"Time scale for the development of thickened crust in the Cretaceous North Cascades magmatic arc, Washington, and relationship to Cretaceous flare-up magmatism","year":2018,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Batholith; Geology; Zircon; Crust; Cretaceous; Continental crust; Geochemistry; Magmatism; Geochronology; Pluton; Paleontology; Tectonics","score_opus":0.016904022430981516,"score_gpt":0.22337212206564316,"score_spread":0.20646809963466164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897791207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988846,0.00014228851,0.000031002775,0.000015399477,8.529338e-7,0.0000023708496,0.00015575823,0.0000029547457,0.00076484866],"genre_scores_gemma":[0.99934834,0.00009325091,0.000039452018,0.0000033835472,9.567627e-7,0.000001817486,0.00014921048,8.005603e-7,0.00036277153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999759,0.0000013649641,0.0000015347742,0.000010569703,0.0000041608714,0.000006402588],"domain_scores_gemma":[0.99986386,0.000015433372,0.00005725128,0.0000077707555,0.000026403803,0.000029225816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008065093,0.00010157539,0.00005004493,0.0007367595,0.00032400034,0.00042415093,0.00012534241,0.00013152312,0.0015827533],"category_scores_gemma":[0.00027465884,0.00010570247,0.00007711345,0.00032599506,0.00025195818,0.0002459072,0.00030620833,0.0001733609,0.00010839238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000109740264,0.000017861177,0.969118,0.000019673336,0.000032141565,0.0001619397,0.00051065366,0.00023867401,0.021946253,0.00014993765,0.00013770604,0.007557401],"study_design_scores_gemma":[3.9159272e-7,0.0000034695727,0.99940014,0.000001596974,0.0000023336524,0.00002033142,0.00008750412,0.000038842794,0.0003028941,0.000006174933,0.00013577924,5.405975e-7],"about_ca_topic_score_codex":0.063098244,"about_ca_topic_score_gemma":0.14414954,"teacher_disagreement_score":0.063098244,"about_ca_system_score_codex":0.0006277816,"about_ca_system_score_gemma":0.00031152868,"threshold_uncertainty_score":0.12546194},"labels":[],"label_agreement":null},{"id":"W2908390347","doi":"10.1130/l1011.1","title":"Uplift and exhumation of the Russell Fiord and Boundary blocks along the northern Fairweather transform fault, Alaska","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of Cincinnati; American Chemical Society Petroleum Research Fund; National Science Foundation","keywords":"Geology; Seismology; Strike-slip tectonics; Tectonics; Fault (geology); North American Plate; Transform fault; Plate tectonics; Paleontology","score_opus":0.004247275172217801,"score_gpt":0.16754935623046874,"score_spread":0.16330208105825095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908390347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993426,0.000029834982,0.000025961528,0.0000041884996,8.386888e-7,0.0000010095969,0.000042279644,0.0000031462848,0.0005501106],"genre_scores_gemma":[0.99951184,0.000023825127,0.00004442134,0.0000027001179,6.359738e-7,0.0000012315523,0.000068469715,9.6795e-7,0.00034600278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999194,0.0000060286857,0.0000064251267,0.000030492147,0.00001726525,0.00002030564],"domain_scores_gemma":[0.99983037,0.000019700707,0.00005323647,0.000014671155,0.000038090755,0.000043821496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015129376,0.00009823889,0.0001301205,0.000733533,0.0005586439,0.00036259578,0.00016535088,0.00016731993,0.0009443751],"category_scores_gemma":[0.0003796275,0.00014961183,0.00009364904,0.00041527284,0.00060122105,0.00023378336,0.0004123417,0.000115009454,0.00012877127],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018638662,0.00003860608,0.9512375,0.000032736163,0.00003769444,0.0005462913,0.0032540879,0.00091856346,0.030831404,0.0002033417,0.00015788525,0.012555441],"study_design_scores_gemma":[0.0000016291567,0.000011326247,0.99904865,0.000003389333,0.000004134189,0.000033214183,0.00024132043,0.00014478307,0.00031427294,0.000013122021,0.00018250197,0.0000017054278],"about_ca_topic_score_codex":0.10807425,"about_ca_topic_score_gemma":0.25213438,"teacher_disagreement_score":0.10807425,"about_ca_system_score_codex":0.0006392977,"about_ca_system_score_gemma":0.00039108898,"threshold_uncertainty_score":0.21489036},"labels":[],"label_agreement":null},{"id":"W2911950088","doi":"10.1130/l1005.1","title":"Late Mesozoic reactivation of Precambrian basement structures and their resulting effects on the sequence stratigraphic architecture of the Viking Formation of east-central Alberta, Canada","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Precambrian; Geology; Mesozoic; Paleontology; Sequence (biology); Basement; Architecture; Archaeology; Geography; Structural basin","score_opus":0.00612448653088077,"score_gpt":0.15875818416923232,"score_spread":0.15263369763835155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911950088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955686,0.000474348,0.000046883884,0.00008873214,0.000005031675,0.0000053281587,0.00047613255,0.0000096461645,0.0033253615],"genre_scores_gemma":[0.9980116,0.00023721482,0.00006574176,0.000012622634,0.0000014691784,0.000001782381,0.00021872603,0.000003860502,0.0014470672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997899,0.000009704781,0.000005732902,0.000037066697,0.000064558415,0.00009302974],"domain_scores_gemma":[0.9996437,0.000014695748,0.000055694916,0.000012084265,0.0001496595,0.0001241881],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015828914,0.00031562732,0.0001646156,0.0011585827,0.0014637602,0.0012649941,0.0005163099,0.00021490802,0.00235654],"category_scores_gemma":[0.00056661665,0.00019272082,0.00015350207,0.0013437977,0.0011130865,0.000201119,0.00057963823,0.00028607622,0.00019556185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047481942,0.000043402564,0.9238743,0.00008199993,0.000116753436,0.0008102761,0.0048946054,0.002976178,0.030901834,0.0024762403,0.0013925314,0.031957068],"study_design_scores_gemma":[0.0000020542439,0.0000058893224,0.99785304,0.0000057625275,0.0000051536867,0.000025764823,0.0007201732,0.00015680712,0.00021682908,0.000022842569,0.0009822702,0.0000035298126],"about_ca_topic_score_codex":0.9762706,"about_ca_topic_score_gemma":0.9938169,"teacher_disagreement_score":0.023729384,"about_ca_system_score_codex":0.01804367,"about_ca_system_score_gemma":0.013446277,"threshold_uncertainty_score":0.1309166},"labels":[],"label_agreement":null},{"id":"W2935714062","doi":"10.1130/l1049.1","title":"A structural model for the South Tibetan detachment system in northwestern Bhutan from integration of temperature, fabric, strain, and kinematic data","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Geology; Sill; Shear zone; Metamorphic rock; Intrusion; Deformation (meteorology); Shear (geology); Kinematics; Seismology; Tectonics; Displacement (psychology); Geomorphology; Geochemistry; Petrology","score_opus":0.022646948591122845,"score_gpt":0.21717728391587263,"score_spread":0.19453033532474978,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2935714062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97606486,0.00018842492,0.014097296,0.00027441062,0.000014364204,0.0000427237,0.00091811485,0.0001598085,0.008240091],"genre_scores_gemma":[0.99611616,0.00006570113,0.0022463552,0.000018099096,0.000005279785,0.000022517665,0.00046745647,0.000021523892,0.0010369228],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998956,0.000016885147,0.0000062008908,0.000041564184,0.000016344058,0.000023386343],"domain_scores_gemma":[0.99991024,0.000014436536,0.00001743795,0.000011683127,0.000021457268,0.000024729503],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014890647,0.00035775217,0.00029496048,0.000978689,0.0008527584,0.0013145863,0.0011582298,0.0007736628,0.004833248],"category_scores_gemma":[0.00040441827,0.0005123104,0.000538464,0.0008957087,0.0008567595,0.00051323563,0.0008726706,0.00036731194,0.000588588],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007578641,0.00006561482,0.080973536,0.0000761069,0.00008712512,0.000369558,0.00055848475,0.88691485,0.0080114,0.011672686,0.00066959905,0.010525298],"study_design_scores_gemma":[0.000039850227,0.000036097324,0.028484112,0.000019739338,0.00002912265,0.00008935197,0.0001969422,0.96581763,0.00020102678,0.0038327451,0.0012311072,0.000022310995],"about_ca_topic_score_codex":0.12866528,"about_ca_topic_score_gemma":0.106192075,"teacher_disagreement_score":0.12866528,"about_ca_system_score_codex":0.002533177,"about_ca_system_score_gemma":0.0015655138,"threshold_uncertainty_score":0.25583273},"labels":[],"label_agreement":null},{"id":"W2946564934","doi":"10.1130/l1017.1","title":"Mesozoic evolution of the eastern Pamir","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Houston; National Science Foundation","keywords":"Terrane; Geology; Nappe; Thrust fault; Gneiss; Metamorphic facies; Greenschist; Crust; Metamorphism; Schist; Geochemistry; Continental crust; Zircon; Paleontology; Facies; Metamorphic rock; Tectonics","score_opus":0.004359310365745113,"score_gpt":0.15893866836160006,"score_spread":0.15457935799585495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946564934","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99445313,0.000116947,0.00006265909,0.00004192591,0.000003849835,0.0000038403523,0.000098928824,0.000010872933,0.0052079605],"genre_scores_gemma":[0.99935764,0.000033830904,0.00011469846,0.000013409756,0.0000027485278,0.0000021890198,0.00009130355,0.0000022588858,0.0003819102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991965,0.0000087766,0.000003015751,0.000024716765,0.000013720005,0.000030184257],"domain_scores_gemma":[0.9999374,0.0000049546693,0.000018915965,0.00000484206,0.000021465261,0.000012418946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017245427,0.00014378731,0.0001127076,0.0008032898,0.00063574145,0.0005207748,0.00028461724,0.0001288967,0.0016103191],"category_scores_gemma":[0.00019575008,0.000147408,0.00011433086,0.0006832262,0.00038109696,0.00013979328,0.00050736545,0.00017168789,0.00023848236],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014957183,0.000032463257,0.9429782,0.00005799554,0.00009315983,0.0007879902,0.0035243707,0.0008517541,0.019830609,0.0014368657,0.0006409065,0.029616183],"study_design_scores_gemma":[0.0000015268806,0.000010155201,0.99827516,0.0000048548513,0.0000044956723,0.000080715196,0.0003649468,0.00017856101,0.00009501509,0.00002530134,0.00095779024,0.00000152059],"about_ca_topic_score_codex":0.05875349,"about_ca_topic_score_gemma":0.16354021,"teacher_disagreement_score":0.05875349,"about_ca_system_score_codex":0.00088051276,"about_ca_system_score_gemma":0.0004792296,"threshold_uncertainty_score":0.11682302},"labels":[],"label_agreement":null},{"id":"W2952167181","doi":"10.1130/l1068.1","title":"Detrital zircon U-Pb data reveal a Mississippian sediment dispersal network originating in the Appalachian orogen, traversing North America along its southern shelf, and reaching as far as the southwest United States","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Detritus; Foreland basin; Zircon; Ordovician; Provenance; Paleocurrent; Pennsylvanian; Devonian; Paleontology; Craton; Paleozoic; Pangaea; Oceanography; Laurentia; Sedimentary rock; Clastic rock; Structural basin; Permian; Tectonics","score_opus":0.01231630316972024,"score_gpt":0.20881006881303388,"score_spread":0.19649376564331364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2952167181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865663,0.00009148975,0.000105823325,0.000011433039,6.468979e-7,0.0000017431199,0.00047737744,0.000006470877,0.00064829254],"genre_scores_gemma":[0.99806195,0.00010079091,0.00030033267,0.000008503377,0.0000012554784,0.0000034691427,0.00093985855,0.0000021992996,0.0005815572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000027387196,0.0000038001097,0.000019365973,0.000006384003,0.000010910452],"domain_scores_gemma":[0.999864,0.000009622948,0.000041197716,0.000011509408,0.000053767064,0.0000198221],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007886345,0.00015657245,0.00010722659,0.0014556665,0.0007430356,0.0005459543,0.00012092709,0.00011450783,0.0008611525],"category_scores_gemma":[0.00014767687,0.00014361124,0.00009589479,0.0014244933,0.00020171647,0.00012147018,0.0003912251,0.00012395474,0.00019564261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041417126,0.000006890956,0.981783,0.000012997116,0.0000314732,0.0001525728,0.00076085614,0.00016721898,0.0069133495,0.00009400096,0.00018219244,0.009854055],"study_design_scores_gemma":[0.0000014614104,0.0000070757296,0.9976549,0.0000041209087,0.000013192442,0.000085579646,0.00030253705,0.00020875006,0.0005076126,0.000021810045,0.0011913469,0.0000016090808],"about_ca_topic_score_codex":0.14013901,"about_ca_topic_score_gemma":0.41741738,"teacher_disagreement_score":0.859861,"about_ca_system_score_codex":0.00051642756,"about_ca_system_score_gemma":0.00036311362,"threshold_uncertainty_score":0.27864665},"labels":[],"label_agreement":null},{"id":"W2965685267","doi":"10.2113/2020/8825465","title":"Formation of Anorthositic Rocks within the Blair River Inlier of Northern Cape Breton Island, Nova Scotia (Canada)","year":2020,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of Nova Scotia; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Science and Technology, Taiwan","keywords":"Geology; Geochemistry; Terrane; Mafic; Nova scotia; Basalt; Magma; Zircon; Gabbro; Petrology; Paleontology; Tectonics; Oceanography","score_opus":0.008028996407223632,"score_gpt":0.16489153874643722,"score_spread":0.1568625423392136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965685267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99364567,0.00036766272,0.00004519274,0.00006402878,0.0000048349416,0.000029167606,0.0008121802,0.0000102938275,0.0050208936],"genre_scores_gemma":[0.9953402,0.00022887069,0.00016857705,0.000032110747,0.0000020907707,0.000009740514,0.00052177685,0.0000059028293,0.00369068],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980575,0.000008557717,0.0000098613,0.000052110096,0.000050090566,0.0000736651],"domain_scores_gemma":[0.9995603,0.000024464363,0.000090194364,0.000013528297,0.00018995363,0.00012152881],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013180535,0.00023247926,0.00016459143,0.0015161269,0.0016977886,0.0011170316,0.0004363009,0.00021856379,0.0022781682],"category_scores_gemma":[0.00034651466,0.00029652793,0.00011993251,0.0010733963,0.0006201521,0.00015715699,0.0004653286,0.00020973706,0.00027234358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013691332,0.000037205315,0.9551906,0.00017038343,0.00007257134,0.0015572755,0.0033492197,0.00039754668,0.022603082,0.00032002028,0.0016051069,0.014560138],"study_design_scores_gemma":[0.000003008953,0.0000049888217,0.9974497,0.000019428975,0.0000044526564,0.00007590686,0.0007334209,0.00006287363,0.00019633876,0.0000047613203,0.001442063,0.0000029974337],"about_ca_topic_score_codex":0.97206,"about_ca_topic_score_gemma":0.99441963,"teacher_disagreement_score":0.027939975,"about_ca_system_score_codex":0.009077759,"about_ca_system_score_gemma":0.0062398426,"threshold_uncertainty_score":0.06586403},"labels":[],"label_agreement":null},{"id":"W2973544877","doi":"10.1130/l1032.1","title":"Fabrics, geothermometry, and geochronology of the Songshugou ophiolite: Insights into the tectonic evolution of the Shangdan suture, Qinling orogen, China","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Ophiolite; Geochemistry; Metamorphism; Amphibole; Ultramafic rock; Subduction; Schist; Fibrous joint; Geochronology; Metamorphic rock; Glaucophane; Blueschist; Zircon; Mafic; Metamorphic facies; Eclogite; Facies; Tectonics; Seismology; Paleontology; Quartz","score_opus":0.0030296720523202434,"score_gpt":0.16311109924327857,"score_spread":0.16008142719095833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2973544877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934524,0.00009068196,0.00010007823,0.000007931412,0.0000013036165,0.000003821747,0.00011024533,0.0000052750224,0.00033549577],"genre_scores_gemma":[0.9995276,0.00004579767,0.00009457236,0.000003172846,0.0000017538252,0.0000023109685,0.00011608861,0.000003074427,0.00020564749],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987435,0.000007993278,0.000007992577,0.000045250636,0.000035324003,0.00002916812],"domain_scores_gemma":[0.9998932,0.000008581128,0.000035151803,0.000006072971,0.00003301998,0.000024002053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022925498,0.00038425068,0.0002207147,0.0029215114,0.0005042045,0.00044609376,0.00025848285,0.00021760647,0.0008010974],"category_scores_gemma":[0.0001857969,0.00021064171,0.00021975131,0.0016184403,0.00051531114,0.00023279001,0.00031902743,0.00010862851,0.00009147158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001524172,0.000032120988,0.8758263,0.00010427786,0.000088208355,0.0004378625,0.0013148265,0.0012727813,0.10926255,0.00023949934,0.00010065826,0.011168562],"study_design_scores_gemma":[0.0000035592827,0.000014306723,0.99835384,0.0000019204736,0.000011642814,0.000049900333,0.00017078262,0.0005430321,0.0006201695,0.000014078592,0.00021355342,0.0000032887267],"about_ca_topic_score_codex":0.08206063,"about_ca_topic_score_gemma":0.1195889,"teacher_disagreement_score":0.08206063,"about_ca_system_score_codex":0.0009489146,"about_ca_system_score_gemma":0.0005818296,"threshold_uncertainty_score":0.16316599},"labels":[],"label_agreement":null},{"id":"W2982735066","doi":"10.1130/l1099.1","title":"Ages and geochemistry of Early Jurassic granitoids in the Lesser Xing’an–Zhangguangcai Ranges, NE China: Petrogenesis and tectonic implications","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Petrogenesis; Magmatism; Geochemistry; Subduction; Mesozoic; Continental arc; Tethys Ocean; Paleozoic; Metallogeny; Tectonics; Paleontology; Mantle (geology); Structural basin","score_opus":0.00759576153469489,"score_gpt":0.19756002867908984,"score_spread":0.18996426714439496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982735066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992454,0.00011764176,0.000032029606,0.000011156165,0.0000011406918,0.0000021837907,0.00014348651,0.000004783326,0.00044216833],"genre_scores_gemma":[0.9993006,0.00008874309,0.00006860772,0.0000046882446,0.0000015584835,0.0000033558301,0.00021069238,0.0000024500832,0.00031922918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999168,0.0000059314525,0.000008132594,0.00003159945,0.000020782007,0.000016863942],"domain_scores_gemma":[0.9998568,0.000008243186,0.000050677034,0.000010654016,0.00004023123,0.00003329394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016583341,0.00031058327,0.00019834317,0.00197504,0.00085762196,0.0005445352,0.00027762252,0.00021980013,0.00082418096],"category_scores_gemma":[0.00018577742,0.00024962754,0.00021497402,0.001966187,0.0005523707,0.00025388927,0.0004691764,0.00014951442,0.00009466226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086036554,0.00000998219,0.9777965,0.000039220933,0.000059004244,0.00017592094,0.001060631,0.00036572877,0.01539935,0.000117710675,0.000059528644,0.0048303576],"study_design_scores_gemma":[0.0000016315652,0.0000040584273,0.9992706,0.0000019777895,0.0000065077206,0.000028006969,0.00017195924,0.00007579997,0.00017745317,0.000010953868,0.00024918694,0.0000018188999],"about_ca_topic_score_codex":0.09964146,"about_ca_topic_score_gemma":0.22454597,"teacher_disagreement_score":0.09964146,"about_ca_system_score_codex":0.0010252817,"about_ca_system_score_gemma":0.0006255965,"threshold_uncertainty_score":0.19812292},"labels":[],"label_agreement":null},{"id":"W2997501586","doi":"10.1130/l1104.1","title":"Evolution of the Yangtze River network, southeastern Tibet: Insights from thermochronology and sedimentology","year":2019,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fundamental Research Funds for the Central Universities; Chengdu University; Chengdu University of Technology; National Natural Science Foundation of China; McGill University","keywords":"Geology; Thermochronology; Fluvial; Tributary; Cenozoic; Zircon; Plateau (mathematics); Sedimentology; Sinistral and dextral; Geomorphology; Geochemistry; Pluton; Paleontology; Fault (geology); Structural basin; Tectonics","score_opus":0.004067161061368693,"score_gpt":0.1545944253952401,"score_spread":0.1505272643338714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997501586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992224,0.000071988776,0.00009052333,0.000024829898,0.0000010852568,0.0000020350412,0.0001560039,0.0000066611155,0.00042445582],"genre_scores_gemma":[0.999582,0.000033499553,0.000091681126,0.0000060793027,0.0000013831956,0.000002483392,0.00015849661,0.0000019547638,0.00012240511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999021,0.000022894521,0.000008243136,0.000031118678,0.000018502466,0.000017187118],"domain_scores_gemma":[0.99978286,0.000035348403,0.0000613217,0.000014272706,0.000066281296,0.0000399021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042929832,0.00020692714,0.0001551749,0.0019055597,0.0005580138,0.00080491044,0.00025615463,0.0002106371,0.0011403718],"category_scores_gemma":[0.0004822081,0.00015426714,0.00015551988,0.0026216428,0.00044693312,0.0003145735,0.00031919082,0.00013379254,0.00008705697],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032707863,0.000013666901,0.98334724,0.000027409566,0.000066852255,0.00028220142,0.00080310245,0.0012516272,0.00532343,0.00027973013,0.00012358931,0.008448444],"study_design_scores_gemma":[0.000002414285,0.000010463879,0.9981797,0.000004171554,0.000009522928,0.000046300458,0.00029035396,0.0010382162,0.00010894122,0.000059992202,0.00024651445,0.0000034693633],"about_ca_topic_score_codex":0.04561945,"about_ca_topic_score_gemma":0.07997345,"teacher_disagreement_score":0.04561945,"about_ca_system_score_codex":0.00097640615,"about_ca_system_score_gemma":0.00059377495,"threshold_uncertainty_score":0.09070784},"labels":[],"label_agreement":null},{"id":"W3004112572","doi":"10.1130/l1115.1","title":"Provenance of Pennsylvanian–Permian sedimentary rocks associated with the Ancestral Rocky Mountains orogeny in southwestern Laurentia: Implications for continental-scale Laurentian sediment transport systems","year":2020,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"University of Houston; National Science Foundation","keywords":"Laurentia; Geology; Pennsylvanian; Paleontology; Basement; Sedimentary rock; Sedimentary basin; Provenance; Structural basin; Paleozoic; Archaeology","score_opus":0.012451567506904215,"score_gpt":0.19798964805250613,"score_spread":0.18553808054560192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004112572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983327,0.0001263388,0.000063613224,0.00002059105,0.0000017542965,0.000003152011,0.00015382524,0.0000045382903,0.0012935435],"genre_scores_gemma":[0.9995567,0.000054111966,0.000078261495,0.00000840226,0.0000027251338,0.0000021212397,0.0001367371,0.000002175598,0.00015871193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998319,0.000023162855,0.000011827654,0.000053378288,0.000027501457,0.00005216849],"domain_scores_gemma":[0.9996911,0.00002744037,0.00013503508,0.00002244559,0.00008026264,0.00004383257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000327673,0.00016080351,0.0001778616,0.0011566393,0.0006717863,0.0008543937,0.00028657718,0.00010358786,0.0009224755],"category_scores_gemma":[0.00051791087,0.00008407249,0.00010544305,0.0008042357,0.0005481866,0.00021150045,0.0005127711,0.00014172129,0.00015800685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010989709,0.000013737471,0.977793,0.000023088225,0.000043849494,0.00032954797,0.001149931,0.00023897135,0.009909343,0.00019890838,0.00012114775,0.010068705],"study_design_scores_gemma":[0.0000017400389,0.000005534116,0.9990252,0.00000716519,0.0000049686473,0.00005199106,0.00026274982,0.00009473402,0.00021062305,0.0000125080205,0.00032123775,0.0000015418728],"about_ca_topic_score_codex":0.08875824,"about_ca_topic_score_gemma":0.22991028,"teacher_disagreement_score":0.08875824,"about_ca_system_score_codex":0.0010490877,"about_ca_system_score_gemma":0.0005404204,"threshold_uncertainty_score":0.17648321},"labels":[],"label_agreement":null},{"id":"W3006500046","doi":"10.1130/l1138.1","title":"Along-strike variations in sediment provenance within the Nanaimo basin reveal mechanisms of forearc basin sediment influx events","year":2020,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary; Washington State University","keywords":"Geology; Provenance; Structural basin; Zircon; Forearc; Paleontology; Geomorphology; Subduction; Tectonics","score_opus":0.011703206092603034,"score_gpt":0.19638476734438756,"score_spread":0.18468156125178453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006500046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99917126,0.000054759766,0.00007857361,0.000008199537,0.000001202772,0.0000018720436,0.000088426474,0.0000044584617,0.00059120706],"genre_scores_gemma":[0.99944323,0.000045604138,0.00010852484,0.000004534244,0.0000014772273,0.0000028567435,0.00015097775,0.000002508187,0.0002403654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.0000038737094,0.000004058289,0.00001782627,0.000008308871,0.000011582476],"domain_scores_gemma":[0.999905,0.000010517011,0.000031914955,0.000010772043,0.000028399612,0.00001339419],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015858782,0.00015643219,0.00015492091,0.00078516256,0.0003701104,0.0004425731,0.0001522338,0.00015167856,0.0014410788],"category_scores_gemma":[0.00030944977,0.00014749407,0.000116509116,0.0007211469,0.00019951271,0.00024526072,0.000505261,0.00011640317,0.00015878543],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006864105,0.000012529216,0.96547633,0.00001975074,0.0000438084,0.0001577541,0.00075408944,0.00019523289,0.024192587,0.00013173283,0.00007295083,0.008874561],"study_design_scores_gemma":[7.785034e-7,0.0000048280117,0.99912375,0.0000020405398,0.00000642644,0.000019505174,0.00015419573,0.0002131439,0.0002952791,0.00002004238,0.00015880697,0.0000011520411],"about_ca_topic_score_codex":0.012365217,"about_ca_topic_score_gemma":0.046774957,"teacher_disagreement_score":0.9876348,"about_ca_system_score_codex":0.0002481151,"about_ca_system_score_gemma":0.00018230802,"threshold_uncertainty_score":0.024586499},"labels":[],"label_agreement":null},{"id":"W3084599869","doi":"10.2113/2020/8854686","title":"U-Th-Pb Geochronology and Lu-Hf Isotope Geochemistry of Detrital Zircons in Metasedimentary Rocks of the Southern Coast Mountains Batholith","year":2020,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"University of Arizona; National Science Foundation","keywords":"Terrane; Batholith; Geology; Geochronology; Protolith; Geochemistry; Tectonics; Metamorphism; Mesozoic; Paleontology","score_opus":0.00809026636446578,"score_gpt":0.17664829740208374,"score_spread":0.16855803103761796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084599869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994468,0.00006147772,0.00004888826,0.0000020687062,4.296603e-7,0.0000015551717,0.000118549324,0.0000036364625,0.00031657048],"genre_scores_gemma":[0.9991278,0.00004676346,0.00013047196,0.0000022867703,5.8861457e-7,0.0000021051214,0.00019392178,0.000003032745,0.0004929406],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999511,0.0000024408837,0.0000056589574,0.000017442886,0.00001054584,0.000012903289],"domain_scores_gemma":[0.9999329,0.000006426696,0.00001806304,0.0000072265693,0.000023397079,0.0000119380975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010173979,0.00019078133,0.00015913117,0.0012081629,0.00044462108,0.00037950973,0.00020576654,0.00013112366,0.0007993516],"category_scores_gemma":[0.00016145171,0.00022435818,0.00015003227,0.0006462264,0.00021866988,0.00017540841,0.00027365825,0.00010152628,0.00021627828],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011640451,0.000013749677,0.8803056,0.0000430452,0.00004431932,0.00034694147,0.001381769,0.00019863773,0.10698487,0.00006111565,0.00004166096,0.010461905],"study_design_scores_gemma":[0.0000010737995,0.000015540585,0.9966139,0.000002692605,0.000006897277,0.00007735653,0.00019168213,0.00007863139,0.0028370786,0.0000038272187,0.0001701103,0.0000012293831],"about_ca_topic_score_codex":0.052539226,"about_ca_topic_score_gemma":0.15081462,"teacher_disagreement_score":0.9474608,"about_ca_system_score_codex":0.00052131765,"about_ca_system_score_gemma":0.0002445567,"threshold_uncertainty_score":0.104466856},"labels":[],"label_agreement":null},{"id":"W3085716197","doi":"10.2113/2020/8837633","title":"Evolution of Subduction Dynamics beneath West Avalonia in Middle to Late Ordovician Times","year":2020,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Volcanic rock; Ordovician; Felsic; Volcanic arc; Subduction; Volcano; Pyroclastic rock; Island arc; Geochemistry; Paleontology; Andesite; Tectonics","score_opus":0.010100475654711439,"score_gpt":0.1771821745189198,"score_spread":0.16708169886420834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3085716197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99840707,0.00017025246,0.000017959766,0.000017347047,0.0000015836603,0.0000022055049,0.00011173269,0.000004692324,0.0012672363],"genre_scores_gemma":[0.9993855,0.0000708117,0.000017903061,0.000002589043,0.0000013357053,9.097085e-7,0.00012803524,0.0000015679128,0.00039133898],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998982,0.0000076209058,0.000006879139,0.000021431568,0.000021171625,0.000044617926],"domain_scores_gemma":[0.9996947,0.000027671702,0.00007752088,0.000015390462,0.00009290173,0.00009187414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025390572,0.00022875694,0.00013360486,0.0024743408,0.0005679879,0.0016180597,0.00034506628,0.00019675476,0.0019450124],"category_scores_gemma":[0.0005441215,0.000121397454,0.00014477994,0.0017575636,0.000579264,0.00027424985,0.0005709134,0.00018892981,0.00020955974],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001443457,0.000019233872,0.9779308,0.000034789075,0.000037822865,0.00040432537,0.0029806432,0.0005845324,0.0053132214,0.0006154795,0.00017869759,0.011756126],"study_design_scores_gemma":[0.0000014948122,0.000006784137,0.9984366,0.00000566017,0.0000024003677,0.00003360774,0.00069373136,0.00014310372,0.00008292594,0.000027932909,0.000563974,0.0000018297694],"about_ca_topic_score_codex":0.3633395,"about_ca_topic_score_gemma":0.49559572,"teacher_disagreement_score":0.3633395,"about_ca_system_score_codex":0.0023479527,"about_ca_system_score_gemma":0.0009726033,"threshold_uncertainty_score":0.7224493},"labels":[],"label_agreement":null},{"id":"W3087516629","doi":"10.2113/2020/2298288","title":"Late Cretaceous to Paleocene Tectonometamorphic Evolution of the Blanchard River Assemblage, Southwest Yukon: New Insight into the Terminal Accretion of Insular Terranes in the Northern Cordillera","year":2020,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; Simon Fraser University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; University of California, Santa Barbara","keywords":"Terrane; Geology; Cretaceous; Metamorphism; Paleontology; Accretion (finance); Metamorphic facies; North American Plate; Tectonics; Facies; Geomorphology; Plate tectonics; Structural basin","score_opus":0.012905755190414198,"score_gpt":0.18989785195259662,"score_spread":0.17699209676218242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087516629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984681,0.00016595353,0.000031217183,0.000021419824,0.0000010788827,0.0000022882332,0.00016861854,0.0000047921517,0.0011364425],"genre_scores_gemma":[0.9988992,0.000098690754,0.00010508061,0.00000928763,8.7330653e-7,0.000002187686,0.00028051014,0.000003385499,0.000600752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994504,0.000003804449,0.0000033659487,0.000021213807,0.000009210636,0.000017464086],"domain_scores_gemma":[0.99988055,0.000009558697,0.000025891688,0.000008723069,0.00005240335,0.000022806293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009076378,0.00016134798,0.00014424969,0.0010323942,0.0007559417,0.0005918953,0.0002302811,0.0002008528,0.002025961],"category_scores_gemma":[0.00017226035,0.00012163417,0.00010916671,0.0009269552,0.00028633518,0.00024069496,0.00033422856,0.00014426977,0.00021226106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004410739,0.000013184753,0.97610384,0.000030564417,0.000030423866,0.0002702186,0.0030877113,0.00016167082,0.008476776,0.000109698565,0.00022657482,0.011445149],"study_design_scores_gemma":[5.6784796e-7,0.0000030781705,0.99876046,0.000005465596,0.0000025838215,0.000038893228,0.00065197947,0.00007147041,0.00008359522,0.000008264798,0.0003725109,0.0000010942363],"about_ca_topic_score_codex":0.3123854,"about_ca_topic_score_gemma":0.7078945,"teacher_disagreement_score":0.68761456,"about_ca_system_score_codex":0.0012991948,"about_ca_system_score_gemma":0.00076882244,"threshold_uncertainty_score":0.6211343},"labels":[],"label_agreement":null},{"id":"W3098921757","doi":"10.2113/2020/8856566","title":"Magma Loading in the Southern Coast Plutonic Complex, British Columbia and Washington","year":2020,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pluton; Geology; Geochemistry; Plagioclase; Hornblende; Zircon; Magmatism; Subduction; Biotite; Tectonics; Seismology; Quartz; Paleontology","score_opus":0.015468553908464949,"score_gpt":0.1797565148915312,"score_spread":0.16428796098306625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3098921757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99721366,0.00013631202,0.000015590043,0.00006880605,0.0000018161186,0.000011939221,0.0006194553,0.000004794711,0.0019277683],"genre_scores_gemma":[0.99640936,0.00019429665,0.0000685327,0.000037722602,0.00000158616,0.000012270444,0.00075053377,0.0000034218706,0.002522312],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983287,0.000010162883,0.000010528796,0.000026710799,0.00005712129,0.0000626526],"domain_scores_gemma":[0.99937916,0.000035868732,0.00010563521,0.000016301441,0.00031056028,0.0001523483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001293915,0.00020036583,0.00016838602,0.002268509,0.0018591275,0.0010002184,0.00042899005,0.00030317306,0.0022769265],"category_scores_gemma":[0.0007293031,0.00023431762,0.00009824994,0.0036920377,0.00046523477,0.00024195171,0.0007112619,0.00030575093,0.0002474503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042902226,0.000023838094,0.9878319,0.000022985007,0.00002411019,0.00036415894,0.0016524036,0.00007042271,0.0010646782,0.00006140821,0.0006709937,0.008170284],"study_design_scores_gemma":[0.0000015947091,0.000004830945,0.99676055,0.000009249008,0.0000044848503,0.000054518354,0.001993536,0.00004990429,0.000081059385,0.0000062393606,0.0010320395,0.0000020195132],"about_ca_topic_score_codex":0.9723829,"about_ca_topic_score_gemma":0.99337476,"teacher_disagreement_score":0.027617097,"about_ca_system_score_codex":0.008795523,"about_ca_system_score_gemma":0.005523908,"threshold_uncertainty_score":0.06381631},"labels":[],"label_agreement":null},{"id":"W3134709846","doi":"10.2113/2021/7866944","title":"U-Pb and Hf Analyses of Detrital Zircons from Paleozoic and Cretaceous Strata on Vancouver Island, British Columbia: Constraints on the Paleozoic Tectonic Evolution of Southern Wrangellia","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Terrane; Geology; Paleozoic; Devonian; Zircon; Permian; Crust; Island arc; Paleontology; Subduction; Geochemistry; Tectonics; Structural basin","score_opus":0.012871338904331845,"score_gpt":0.19783371689677845,"score_spread":0.1849623779924466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134709846","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968663,0.00023442414,0.000047161604,0.0000233006,0.0000012209887,0.0000058206347,0.0009810573,0.000010780455,0.001830069],"genre_scores_gemma":[0.9961318,0.00020656413,0.00022425105,0.000015221637,0.000001355319,0.000008048212,0.0014009759,0.000007982931,0.0020038218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987566,0.0000054128946,0.00000761368,0.000031249685,0.0000398737,0.00004007025],"domain_scores_gemma":[0.99973637,0.000014606677,0.000033288088,0.000010311432,0.00015508928,0.000050408053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014744766,0.00022526702,0.00018040571,0.0023828752,0.0015458945,0.0010022036,0.00037759508,0.0002026439,0.0015431291],"category_scores_gemma":[0.00029923808,0.0002092383,0.00012731031,0.0018427934,0.00023771844,0.00012750445,0.00050753885,0.00016395362,0.00029334403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007093031,0.000016303566,0.9595409,0.000042223757,0.00004473314,0.00028292066,0.0015833427,0.00018558002,0.020698782,0.00007025212,0.00051759486,0.016946523],"study_design_scores_gemma":[9.15274e-7,0.0000023245832,0.9986609,0.000004774464,0.000004287527,0.00002697715,0.0003586164,0.000051699622,0.00023976578,0.0000026909274,0.000645661,0.0000013616827],"about_ca_topic_score_codex":0.8937301,"about_ca_topic_score_gemma":0.97777927,"teacher_disagreement_score":0.106269896,"about_ca_system_score_codex":0.0029008384,"about_ca_system_score_gemma":0.0019676932,"threshold_uncertainty_score":0.21379143},"labels":[],"label_agreement":null},{"id":"W3165606589","doi":"10.2113/2021/7866155","title":"Pre-Mississippian Stratigraphic Architecture of the Porcupine Shear Zone, Yukon and Alaska, and Significance in the Evolution of Northern Laurentia","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University","funders":"Dartmouth College; Geological Society of America; National Science Foundation","keywords":"Geology; Laurentia; Siliciclastic; Zircon; Geochronology; Paleontology; Felsic; Geochemistry; Terrane; Dolostone; Devonian; Anatexis; Mafic; Sedimentary rock; Carbonate rock; Crust; Sedimentary depositional environment; Paleozoic; Partial melting; Tectonics","score_opus":0.004221428874135238,"score_gpt":0.17261546390700763,"score_spread":0.1683940350328724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3165606589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990159,0.00008955853,0.000017501305,0.00000906223,5.512807e-7,0.000001104708,0.000043049327,0.0000023156038,0.0008209001],"genre_scores_gemma":[0.9994281,0.00007029158,0.000051444276,0.0000037574368,5.2585943e-7,0.0000013025602,0.00007987916,0.0000010566224,0.0003637234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993134,0.0000046401196,0.0000051052807,0.00002760618,0.000011785591,0.000019453553],"domain_scores_gemma":[0.99987173,0.0000068369422,0.000046745285,0.0000064251876,0.000037301947,0.00003099597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012101466,0.00012765458,0.000092853545,0.00085197145,0.00069621304,0.00063611544,0.0001654829,0.00009677696,0.00092881965],"category_scores_gemma":[0.00019741303,0.00009574375,0.000070386304,0.0006137763,0.00036942444,0.00020108065,0.00042484573,0.00009991831,0.00011883227],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038164377,0.000008993783,0.98152727,0.000018074466,0.000024745896,0.00018174,0.0018370833,0.00011046335,0.008780347,0.00014692455,0.00006888842,0.0072571705],"study_design_scores_gemma":[3.468492e-7,0.000003564467,0.9987778,0.000004637433,0.0000022059937,0.000033983575,0.0006842762,0.000041777716,0.00013160387,0.00000734313,0.00031153735,9.018239e-7],"about_ca_topic_score_codex":0.18903327,"about_ca_topic_score_gemma":0.5514759,"teacher_disagreement_score":0.81096673,"about_ca_system_score_codex":0.0009051813,"about_ca_system_score_gemma":0.0007779025,"threshold_uncertainty_score":0.37586594},"labels":[],"label_agreement":null},{"id":"W3166560357","doi":"10.2113/2021/5559457","title":"Filling Provenance in Fracture Cavity Formation within Aksu Area, Tarim Basin, NW China: Indicators from Major and Trace Element, Carbon-Oxygen, and Strontium Isotope Compositions","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Geology; Ordovician; Diagenesis; Geochemistry; Trace element; Provenance; Fracture (geology); Isotopes of oxygen; Isotopes of strontium; Rare-earth element; δ18O; Sedimentary rock; Strontium; Carbonate; Mineralogy; Paleontology; Stable isotope ratio; Chemistry","score_opus":0.005340900413754682,"score_gpt":0.18930851311646693,"score_spread":0.18396761270271225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3166560357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998759,0.000019036483,0.00002412432,0.0000018735176,2.679502e-7,0.0000010426005,0.000020423611,0.0000016693551,0.00005563703],"genre_scores_gemma":[0.99983287,0.000010307196,0.000046218633,0.0000011050759,4.079982e-7,0.0000013137526,0.00003557036,4.7399217e-7,0.00007172915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987507,0.000007652132,0.000013168343,0.00004503094,0.000024664547,0.000034442135],"domain_scores_gemma":[0.9998417,0.000018177774,0.00006184402,0.000013210179,0.000044185326,0.000020819367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016060492,0.0002027413,0.00020010865,0.001305733,0.0005773354,0.00033932994,0.0003379562,0.00019474443,0.00045183362],"category_scores_gemma":[0.00024186476,0.0001781734,0.00017469768,0.0010663474,0.000517502,0.00023223158,0.00040309978,0.00008521736,0.000037519585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074942705,0.000014556486,0.9752343,0.000036948804,0.00002372623,0.0004330511,0.0012026322,0.00024481144,0.013573524,0.0001231472,0.00003654771,0.009001775],"study_design_scores_gemma":[0.0000013868405,0.000017552897,0.99842596,0.0000034807595,0.000008483049,0.00012116005,0.00046562322,0.00033677657,0.00051796535,0.000017399716,0.000081546816,0.0000027362619],"about_ca_topic_score_codex":0.037120547,"about_ca_topic_score_gemma":0.098990425,"teacher_disagreement_score":0.037120547,"about_ca_system_score_codex":0.00051785953,"about_ca_system_score_gemma":0.000542262,"threshold_uncertainty_score":0.07380897},"labels":[],"label_agreement":null},{"id":"W3175972537","doi":"10.2113/2021/7866186","title":"Synsedimentary to Diagenetic Cu±Co Mineralization in Mesoproterozoic Pyritic Shale Driven by Magmatic-Hydrothermal Activity on the Edge of the Great Falls Tectonic Zone–Black Butte, Helena Embayment, Belt-Purcell Basin, USA: Evidence from Sulfide Re-Os Isotope Geochemistry","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Geochemistry; Isochron; Butte; Pyrite; Chalcopyrite; Metallogeny; Sphalerite; Paleontology; Copper","score_opus":0.01324597233122461,"score_gpt":0.21263202004098752,"score_spread":0.19938604770976293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175972537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994117,0.0000413765,0.000024246567,0.00000487403,3.860471e-7,0.0000012893173,0.000067407804,0.0000032076312,0.00044556812],"genre_scores_gemma":[0.99965334,0.000023015713,0.00003880157,0.0000032834928,5.033359e-7,0.0000010748691,0.00007905102,0.000001209149,0.00019971233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999542,0.000004148458,0.0000024433973,0.000018950428,0.000009152902,0.000011122356],"domain_scores_gemma":[0.99992776,0.000006983299,0.0000180491,0.0000065556555,0.000024369065,0.000016393415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009461227,0.00012248814,0.00008762039,0.0006021716,0.00046228772,0.0004915159,0.00017022621,0.00017624011,0.0010828411],"category_scores_gemma":[0.00013985501,0.00012418545,0.000055561417,0.00035918097,0.00033592308,0.00016780676,0.00022159125,0.00010528389,0.00012539298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015000314,0.00003513066,0.90705675,0.000019203257,0.00003025231,0.00027538015,0.0006114676,0.00016297166,0.08503277,0.0001229988,0.00008611393,0.0064170016],"study_design_scores_gemma":[0.0000013123724,0.000012871184,0.997759,0.0000013360722,0.000003332695,0.000040547755,0.00013276043,0.00012373156,0.0016982818,0.000011629653,0.00021439436,7.7396743e-7],"about_ca_topic_score_codex":0.03726885,"about_ca_topic_score_gemma":0.10180811,"teacher_disagreement_score":0.03726885,"about_ca_system_score_codex":0.0005281415,"about_ca_system_score_gemma":0.0002879611,"threshold_uncertainty_score":0.07410383},"labels":[],"label_agreement":null},{"id":"W3195083122","doi":"10.2113/2021/2993537","title":"Quantitative Characterization of Tidal Couplets in Oil Sands Reservoir, the Upper McMurray Formation, Northeastern Alberta, Canada","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Petrophysics; Oil sands; Tidal flat; Fluvial; Asphalt; Geotechnical engineering; Geomorphology; Cartography; Porosity","score_opus":0.008239138796621989,"score_gpt":0.2035470782078421,"score_spread":0.1953079394112201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195083122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99729663,0.000057132114,0.0009784702,0.00000787301,0.0000013358224,0.00003110871,0.00043894435,0.000037136786,0.0011513748],"genre_scores_gemma":[0.99768,0.000042107786,0.0010512464,0.0000034231248,8.751402e-7,0.000010589536,0.00038918757,0.000004468771,0.0008183037],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997863,0.000006197588,0.000010795239,0.000042685006,0.00012369681,0.000030288298],"domain_scores_gemma":[0.99971586,0.000020601632,0.000044881574,0.000010180977,0.00017180336,0.00003656771],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016735631,0.0003218324,0.00018690334,0.003503382,0.00080491614,0.00074896915,0.00040439586,0.00017585035,0.0005274704],"category_scores_gemma":[0.00038053698,0.00014192495,0.00016315327,0.002196743,0.00044097228,0.00018660097,0.0003697297,0.00011257516,0.00011182293],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008953053,0.000052056814,0.9255094,0.00005685791,0.00004620863,0.0003823007,0.00095837214,0.006605318,0.030899614,0.0002658289,0.00031554833,0.034819115],"study_design_scores_gemma":[0.0000026476184,0.000020764566,0.97762567,0.000008446901,0.000016322623,0.000058537684,0.0012283894,0.016176792,0.0041888356,0.000029832929,0.0006313647,0.000012562701],"about_ca_topic_score_codex":0.677085,"about_ca_topic_score_gemma":0.8712114,"teacher_disagreement_score":0.32291502,"about_ca_system_score_codex":0.0026636932,"about_ca_system_score_gemma":0.0016438757,"threshold_uncertainty_score":0.6496334},"labels":[],"label_agreement":null},{"id":"W3205284708","doi":"10.2113/2021/3358149","title":"U-Pb Geochronology and Hf Isotope Geochemistry of the Turtleback Complex and East Sound Group, San Juan Islands, Northwestern North American Cordillera","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Zircon; Terrane; Geology; Igneous rock; Geochronology; Geochemistry; Metamorphism; Magmatism; Pluton; Paleozoic; Sedimentary rock; Paleontology; Tectonics","score_opus":0.010495047099117442,"score_gpt":0.1880894026764687,"score_spread":0.17759435557735126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3205284708","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994023,0.00004488354,0.000016161697,0.000006157217,5.184443e-7,0.0000013207755,0.00006188916,0.0000036171014,0.0004631784],"genre_scores_gemma":[0.9989976,0.00004377277,0.00009827781,0.0000054993457,9.928408e-7,0.0000021704734,0.00019037901,0.0000020904597,0.0006591416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994814,0.000003510728,0.0000031133895,0.000017644677,0.000014435225,0.000013197242],"domain_scores_gemma":[0.9998678,0.0000075956414,0.000030284184,0.000007885792,0.000060997347,0.000025380525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010925168,0.00016479276,0.000101383586,0.0011956055,0.00051941676,0.00039633975,0.00019270611,0.0001262105,0.0014520357],"category_scores_gemma":[0.00022853371,0.00010538927,0.00005923458,0.0006164091,0.0002739125,0.00015425876,0.0003163229,0.000097896336,0.00014775968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004602454,0.000013123024,0.9826261,0.000012422734,0.00001930301,0.00010181721,0.0008264756,0.00007288452,0.006827391,0.000042436808,0.00010684975,0.009305107],"study_design_scores_gemma":[0.0000011748921,0.000007204956,0.99908185,0.0000022714014,0.0000038106382,0.000026248908,0.00032124587,0.0000718957,0.00023020366,0.0000039465745,0.00024950842,6.464356e-7],"about_ca_topic_score_codex":0.23113911,"about_ca_topic_score_gemma":0.47898436,"teacher_disagreement_score":0.7688609,"about_ca_system_score_codex":0.000830798,"about_ca_system_score_gemma":0.0003759425,"threshold_uncertainty_score":0.4595875},"labels":[],"label_agreement":null},{"id":"W3209540857","doi":"10.2113/2021/8356327","title":"Provenance of the Incipient Passive Margin of NW Laurentia (Neoproterozoic): Detrital Zircon from Continental Slope and Basin Floor Deposits of the Windermere Supergroup, Southern Canadian Cordillera","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Ottawa; BP (Canada); Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; University of Ottawa; University of Calgary","keywords":"Laurentia; Rodinia; Geology; Paleontology; Continental margin; Provenance; Passive margin; Zircon; Supercontinent; Rift; Baltica; Sedimentary depositional environment; Structural basin; Craton; Paleozoic; Ordovician; Tectonics","score_opus":0.0038981401764011992,"score_gpt":0.1497789098187439,"score_spread":0.1458807696423427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3209540857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952342,0.000290392,0.000093495095,0.000025633735,0.0000031700185,0.0000079254505,0.0010837385,0.000012873925,0.003248504],"genre_scores_gemma":[0.99760926,0.00012789328,0.00018433588,0.000017257098,0.0000021341755,0.0000042604183,0.0006852672,0.000007312413,0.0013623221],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998412,0.0000042914357,0.000007575705,0.000048192538,0.000044661912,0.00005399188],"domain_scores_gemma":[0.99968493,0.000010632271,0.000050365437,0.00001264942,0.00018565118,0.000055695305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022443221,0.00029434022,0.0002350661,0.002062671,0.0016797212,0.0009632954,0.000372267,0.00017920353,0.0014850759],"category_scores_gemma":[0.0003834983,0.00015062356,0.00012967434,0.0015944025,0.00041564848,0.00020087906,0.00045233287,0.000145101,0.0002914784],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018852409,0.000016002128,0.91368073,0.00006745229,0.000075660864,0.00033830194,0.0028756913,0.00024328826,0.05670224,0.00039880685,0.0006333037,0.024780104],"study_design_scores_gemma":[0.0000014040877,0.000005528423,0.99741805,0.000008734977,0.0000075944663,0.00004006022,0.0002716618,0.00007326259,0.0007375419,0.000008425867,0.0014254362,0.0000022862232],"about_ca_topic_score_codex":0.89869463,"about_ca_topic_score_gemma":0.9710886,"teacher_disagreement_score":0.101305366,"about_ca_system_score_codex":0.0055264756,"about_ca_system_score_gemma":0.0026683728,"threshold_uncertainty_score":0.2038039},"labels":[],"label_agreement":null},{"id":"W4200375904","doi":"10.2113/2021/2964057","title":"Interpretation of Magnetic Anomalies over 2D Fault and Sheet-Type Mineralized Structures Using Very Fast Simulated Annealing Global Optimization: An Understanding of Uncertainty and Geological Implications","year":2021,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Banaras Hindu University","keywords":"Fault (geology); Geology; Dislocation; Seismology; Magnetic anomaly; Type (biology); Fault plane; Geometry; Geophysics; Condensed matter physics; Physics; Mathematics; Paleontology","score_opus":0.028227565867840077,"score_gpt":0.28021483043786816,"score_spread":0.25198726457002807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200375904","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.31893396,0.00011312784,0.67791426,0.00027598935,0.00001983282,0.00005032442,0.00007834493,0.00065241667,0.001961803],"genre_scores_gemma":[0.8841151,0.00004515703,0.11472754,0.00005002424,0.000010259947,0.00007105648,0.000120111836,0.000088239736,0.0007724791],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998305,0.00007989097,0.0000073607753,0.000035546025,0.000024720573,0.000021931311],"domain_scores_gemma":[0.9995821,0.0002588471,0.00003439722,0.00003807102,0.00006801673,0.000018547504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007527858,0.0006589605,0.0005833488,0.000530162,0.00040636057,0.00058916723,0.00057698286,0.0008707992,0.0008517669],"category_scores_gemma":[0.0013233136,0.00029890562,0.0006555579,0.00030749437,0.0005466664,0.00034476607,0.00039517155,0.0004866871,0.000090472065],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002254476,0.000011768493,0.0007033976,0.000010022999,0.00001640096,0.000022228196,0.000022388738,0.99303645,0.0008882905,0.0006697477,0.000084710766,0.0045120497],"study_design_scores_gemma":[0.0000018569898,0.0000045402912,0.00009407455,7.0649133e-7,0.0000013297165,0.0000017758751,0.000004111199,0.99943703,0.0001249905,0.000302996,0.000025695876,8.8802943e-7],"about_ca_topic_score_codex":0.008052217,"about_ca_topic_score_gemma":0.007770795,"teacher_disagreement_score":0.008052217,"about_ca_system_score_codex":0.0005780656,"about_ca_system_score_gemma":0.00089614996,"threshold_uncertainty_score":0.016010702},"labels":[],"label_agreement":null},{"id":"W4212969042","doi":"10.2113/2022/2103213","title":"Strain Partitioning along Terrane Bounding and Intraterrane Shear Zones: Constraints from a Long-Lived Transpressional System in West Gondwana (Ribeira Belt, Brazil)","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Carleton University","funders":"Australian Research Council; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Fundação de Amparo à Pesquisa do Estado de São Paulo","keywords":"Geology; Shear zone; Terrane; Strain partitioning; Gondwana; Shear (geology); Simple shear; Lithosphere; Sinistral and dextral; Overprinting; Supercontinent; Shearing (physics); Transpression; Seismology; Petrology; Crenulation; Tectonics; Craton; Geotechnical engineering","score_opus":0.012850778511345333,"score_gpt":0.20733067586310433,"score_spread":0.194479897351759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212969042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99944204,0.00006776888,0.00011113379,0.000012495984,4.4791165e-7,0.0000023525924,0.00009566007,0.0000033443841,0.00026464838],"genre_scores_gemma":[0.99964225,0.000043956134,0.00012879483,0.0000047992376,9.929227e-7,0.000002258956,0.00013722367,0.0000025347554,0.000037303522],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998042,0.000024442064,0.000016301705,0.000080410704,0.000027389273,0.00004720592],"domain_scores_gemma":[0.99974793,0.00004145157,0.00007333238,0.000032649037,0.000069973845,0.000034761684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002732307,0.00032499307,0.00037745148,0.002224481,0.00065795175,0.0010318687,0.0005270613,0.00043854193,0.00083320966],"category_scores_gemma":[0.00064885325,0.00035159494,0.0003607353,0.0019535562,0.0007044224,0.00042524017,0.001032745,0.00019754237,0.00023308562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061461506,0.000037981066,0.95760727,0.000038771122,0.00013408139,0.0002661588,0.0019105576,0.0007763289,0.027214168,0.00023303909,0.00005482073,0.0116655035],"study_design_scores_gemma":[0.0000017590424,0.000011162599,0.99771106,0.0000065869517,0.000017557568,0.0000705118,0.00068099314,0.0010932595,0.00021470917,0.000055563178,0.00013183494,0.000005010639],"about_ca_topic_score_codex":0.0515612,"about_ca_topic_score_gemma":0.13154615,"teacher_disagreement_score":0.0515612,"about_ca_system_score_codex":0.00054947106,"about_ca_system_score_gemma":0.0004448591,"threshold_uncertainty_score":0.102522194},"labels":[],"label_agreement":null},{"id":"W4213131605","doi":"10.2113/2022/3936881","title":"Geothermal Accumulation Constrained by the Tectonic Transformation in the Gonghe Basin, Northeastern Tibetan Plateau","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Ministry of Natural Resources","keywords":"Geology; Transtension; Structural basin; Geothermal gradient; Tectonics; Plateau (mathematics); Fault (geology); Geomorphology; Geochemistry; Seismology; Paleontology; Rift","score_opus":0.013754155235180306,"score_gpt":0.20765397915992495,"score_spread":0.19389982392474464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213131605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993216,0.000056524852,0.00004203516,0.000020826561,8.1745145e-7,0.000002277367,0.00007639283,0.0000044354233,0.00047507117],"genre_scores_gemma":[0.9996742,0.000032363456,0.000032462212,0.000005470627,0.0000014804476,0.000003161579,0.00014756058,0.0000010759347,0.00010222725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991393,0.000014659081,0.0000071922486,0.000024943762,0.000013544368,0.000025679834],"domain_scores_gemma":[0.99989784,0.000014282095,0.000025376035,0.000008439594,0.000026769814,0.000027222903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024714,0.00021175086,0.00019473383,0.0012798145,0.0005180639,0.0007812306,0.00025978786,0.00021582263,0.0009305333],"category_scores_gemma":[0.0003244569,0.00014773615,0.0001774845,0.0019286787,0.00048665004,0.00025099958,0.00047816755,0.00014698596,0.00006338151],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011981939,0.000036885773,0.9719267,0.000053872365,0.000103082646,0.0006838543,0.0014545665,0.0027042138,0.011002746,0.00045854045,0.00017395371,0.011281805],"study_design_scores_gemma":[0.0000072315506,0.000010895672,0.9979576,0.0000052987343,0.000009554665,0.000051566876,0.0003945105,0.0011469333,0.000080011356,0.000091640875,0.00024165718,0.0000031465509],"about_ca_topic_score_codex":0.042159326,"about_ca_topic_score_gemma":0.06535702,"teacher_disagreement_score":0.042159326,"about_ca_system_score_codex":0.0008116076,"about_ca_system_score_gemma":0.00074224325,"threshold_uncertainty_score":0.08382785},"labels":[],"label_agreement":null},{"id":"W4224116821","doi":"10.2113/2022/7780662","title":"Experimental Study on Influences of Self-Preservation Effects and Memory Effects on the Hydrate Decomposition Process","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Hydrate; Methane; Cabin pressurization; Decomposition; Clathrate hydrate; Materials science; Metastability; Phase (matter); Chemical process of decomposition; Phase transition; Thermodynamics; Chemistry; Chemical engineering; Composite material; Organic chemistry; Physics","score_opus":0.007112452927839635,"score_gpt":0.25097017603764027,"score_spread":0.24385772310980064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224116821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99681574,0.00009708962,0.0025565426,0.000012405634,0.000006039995,0.000009272227,0.00007098169,0.000042623535,0.00038932965],"genre_scores_gemma":[0.9976047,0.00009088189,0.001879641,0.000006799838,0.0000028416043,0.000011651766,0.000047760346,0.000009449008,0.00034623162],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998561,0.000010502676,0.000008035597,0.000039112,0.000059393482,0.000026887823],"domain_scores_gemma":[0.9997391,0.000086116,0.0000585359,0.00004588676,0.00005547477,0.0000149130865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019834204,0.00024745008,0.00017890068,0.00016009746,0.00016037736,0.00013341174,0.0002931296,0.0002625618,0.0013358422],"category_scores_gemma":[0.00036050685,0.00014264199,0.00024668072,0.00016521646,0.00024669248,0.0003862725,0.00020549381,0.00035367924,0.00010888612],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058959842,0.00002746179,0.0003842141,0.000047776928,0.0000029910198,0.000038454105,0.000029948547,0.00036555622,0.99793386,0.00008704422,0.000017197937,0.0010064779],"study_design_scores_gemma":[0.0000051155425,0.00021954559,0.0016005675,0.000001539506,0.0000061552473,0.00002664531,0.000029256837,0.003300993,0.99460214,0.000024176803,0.00017813712,0.0000056399535],"about_ca_topic_score_codex":0.00052873965,"about_ca_topic_score_gemma":0.0005671178,"teacher_disagreement_score":0.0013358422,"about_ca_system_score_codex":0.00016372801,"about_ca_system_score_gemma":0.0001058129,"threshold_uncertainty_score":0.0044687986},"labels":[],"label_agreement":null},{"id":"W4229011793","doi":"10.2113/2022/3086647","title":"Influence of High-Temperature Treatment on Strength and Failure Behaviors of a Quartz-Rich Sandstone under True Triaxial Condition","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China; State Key Laboratory of Safety and Health for Metal Mines","keywords":"Quartz; Brittleness; Geology; Shear modulus; Shear (geology); Overburden pressure; Ductility (Earth science); Failure mode and effects analysis; Shear stress; Modulus; Geotechnical engineering; Tension (geology); Mineralogy; Composite material; Materials science; Petrology; Ultimate tensile strength","score_opus":0.005368068767065782,"score_gpt":0.2140379469476118,"score_spread":0.20866987818054603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229011793","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99871624,0.00009760899,0.00092135987,0.000007586264,0.0000039572033,0.0000036583074,0.0000532224,0.000013323568,0.00018305612],"genre_scores_gemma":[0.9992939,0.000054503675,0.00033302582,0.0000041154267,0.0000011192498,0.000004590613,0.000042264764,0.0000049886266,0.00026156628],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99986553,0.0000149304,0.000010619051,0.000028145963,0.000050749342,0.000030000994],"domain_scores_gemma":[0.99983156,0.00003699281,0.000039967115,0.000027982283,0.000044526325,0.00001893804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017233855,0.00022605275,0.00019142857,0.00018409852,0.00020615419,0.00018510147,0.00013097796,0.00018711679,0.0013496946],"category_scores_gemma":[0.00024287529,0.00016942578,0.00023629323,0.00015070415,0.00029364848,0.00021008031,0.00016694971,0.00020956915,0.00013600649],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019254802,0.000013446729,0.002404289,0.000047652975,0.000011668201,0.00004855422,0.000046342026,0.00082481455,0.9949881,0.000018222338,0.00001809229,0.0013864799],"study_design_scores_gemma":[0.0000089478835,0.00045212195,0.04173241,0.00000431349,0.000025350439,0.00005714575,0.00010112199,0.0058653234,0.95125973,0.000024375557,0.00045862168,0.0000104082255],"about_ca_topic_score_codex":0.0017852877,"about_ca_topic_score_gemma":0.003496286,"teacher_disagreement_score":0.0017852877,"about_ca_system_score_codex":0.00014696339,"about_ca_system_score_gemma":0.00011855101,"threshold_uncertainty_score":0.004515171},"labels":[],"label_agreement":null},{"id":"W4282944364","doi":"10.2113/2022/9441099","title":"Eocene Volcanic Complex from Central British Columbia: The Role of Fractional Crystallization during the Magmatic Evolution","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University","funders":"Ministry of Science and Technology","keywords":"Geology; Geochemistry; Fractional crystallization (geology); Volcanic rock; Volcano; Mafic; Structural basin; Crust; Geomorphology","score_opus":0.004364747970274076,"score_gpt":0.153884313370872,"score_spread":0.1495195654005979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4282944364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99245477,0.0009657825,0.00004366477,0.00015516393,0.0000033365836,0.000012666979,0.000646657,0.000011912584,0.005706094],"genre_scores_gemma":[0.99825305,0.00040628682,0.00006449085,0.000031374384,0.0000018660492,0.0000045097518,0.00036424404,0.000005605106,0.00086848397],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997887,0.000014025323,0.000013521791,0.000046588666,0.00006025217,0.00007696102],"domain_scores_gemma":[0.9992855,0.00007408451,0.00012066126,0.000025939455,0.00034761796,0.00014615073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024696806,0.00022849972,0.00023078204,0.0021985916,0.0020388328,0.0017785457,0.0006213262,0.00031207385,0.002238265],"category_scores_gemma":[0.0011467962,0.0001809187,0.00012186417,0.0024770624,0.0006946721,0.00026409127,0.00060725067,0.00032380858,0.00019621519],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012045964,0.0000220604,0.9641747,0.000084770596,0.000073536205,0.00050225924,0.002685758,0.0003991751,0.007427701,0.00029607775,0.0007137342,0.023499753],"study_design_scores_gemma":[0.000001978616,0.0000028545592,0.99729425,0.00002420932,0.000010388028,0.000062919666,0.0008819675,0.00020131162,0.00021817583,0.000022656415,0.0012754946,0.0000037414275],"about_ca_topic_score_codex":0.96843797,"about_ca_topic_score_gemma":0.98836845,"teacher_disagreement_score":0.03156203,"about_ca_system_score_codex":0.010395062,"about_ca_system_score_gemma":0.006060617,"threshold_uncertainty_score":0.07542181},"labels":[],"label_agreement":null},{"id":"W4283159644","doi":"10.2113/2022/4584611","title":"Age and Chemostratigraphy of the Finlayson Lake District, Yukon: Implications for Volcanogenic Massive Sulfide (VMS) Mineralization and Tectonics along the Western Laurentian Continental Margin","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; University of British Columbia; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Felsic; Magmatism; Geochemistry; Continental arc; Zircon; Continental crust; Mafic; Continental margin; Terrane; Geochronology; Rift; Back-arc basin; Crust; Subduction; Earth science; Paleontology; Tectonics","score_opus":0.008919482259012996,"score_gpt":0.1938577660068296,"score_spread":0.18493828374781662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283159644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99901557,0.0000720545,0.000025866302,0.000016582084,5.701524e-7,0.0000023944754,0.0002139772,0.000004612229,0.0006483091],"genre_scores_gemma":[0.9993393,0.000037532944,0.000052889514,0.0000049476507,3.5769193e-7,0.0000014505131,0.00019448256,0.000001729691,0.00036741863],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993384,0.000004392178,0.00000553981,0.000019935414,0.000014972401,0.000021384456],"domain_scores_gemma":[0.99989355,0.0000057739535,0.000030693896,0.000005190577,0.000045161443,0.000019572022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009857313,0.00014949105,0.00013673223,0.00086631486,0.000564068,0.00050175935,0.00021825268,0.00015228605,0.0011704614],"category_scores_gemma":[0.00015142653,0.000115918236,0.00010114768,0.0011775469,0.00027535393,0.00024778958,0.00036404096,0.00006941419,0.0001470419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003126814,0.0000052021956,0.985538,0.000021203863,0.000022863785,0.000101616875,0.00077180995,0.00013643655,0.007912346,0.00006981541,0.00012097491,0.005268522],"study_design_scores_gemma":[8.201329e-7,0.000004144521,0.99894136,0.0000029201537,0.0000033138313,0.000022909744,0.00043276354,0.00009616852,0.00021452563,0.000006428742,0.0002733696,0.0000012402264],"about_ca_topic_score_codex":0.46789247,"about_ca_topic_score_gemma":0.7613991,"teacher_disagreement_score":0.53210753,"about_ca_system_score_codex":0.0019059839,"about_ca_system_score_gemma":0.0012504936,"threshold_uncertainty_score":0.9303381},"labels":[],"label_agreement":null},{"id":"W4283170398","doi":"10.2113/2022/9585729","title":"Detrital Zircon U-Pb Geochronology of Upper Devonian and Lower Carboniferous Strata of Western Laurentia (North America): A Record of Transition from Passive to Convergent Margin","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"Natural Resources Canada; University of Calgary","keywords":"Laurentia; Geology; Orogeny; Paleontology; Provenance; Facies; Paleocurrent; Supercontinent; Paleozoic; Devonian; Foreland basin; Carboniferous; Zircon; Late Devonian extinction; Gondwana; Passive margin; Ordovician; Terrane; Rift; Craton; Tectonics; Structural basin","score_opus":0.005371632944047231,"score_gpt":0.17444249970877648,"score_spread":0.16907086676472924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283170398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973477,0.00022080641,0.000056667985,0.000014162039,0.0000014006077,0.0000026640153,0.0006131169,0.000011346975,0.0017320388],"genre_scores_gemma":[0.9986123,0.00009124293,0.00012673868,0.000008345901,0.0000012831704,0.0000020760626,0.0005311305,0.0000033531924,0.0006235097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999422,0.0000026051223,0.0000031077525,0.00001933288,0.000014085481,0.000018717996],"domain_scores_gemma":[0.999863,0.000008016547,0.0000351545,0.000006717734,0.000057288595,0.000029764356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011420479,0.00017407016,0.000111449706,0.001284102,0.0005393418,0.0006010821,0.00025542203,0.00009527436,0.00089613546],"category_scores_gemma":[0.0001864802,0.00007824171,0.00006768326,0.0008967637,0.00022617221,0.00012546487,0.00033922255,0.00009361484,0.000145405],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007840041,0.000013152751,0.9763299,0.000021207765,0.000022026692,0.00016034795,0.0007336873,0.00024011079,0.0094348965,0.00014070186,0.0002732039,0.012552449],"study_design_scores_gemma":[9.3308705e-7,0.000003775332,0.9987079,0.000004546083,0.0000040685045,0.000032602977,0.00018618641,0.000097155425,0.00027079115,0.000009697654,0.00068120856,0.0000010865108],"about_ca_topic_score_codex":0.4978861,"about_ca_topic_score_gemma":0.79485065,"teacher_disagreement_score":0.4978861,"about_ca_system_score_codex":0.001441669,"about_ca_system_score_gemma":0.00069618557,"threshold_uncertainty_score":0.98997617},"labels":[],"label_agreement":null},{"id":"W4288068417","doi":"10.2113/2022/5261253","title":"Phase Behavior in Nanopores and Its Indication for Cyclic Gas Injection in a Volatile Oil Reservoir from Duvernay Shale","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science and Technology Major Project; China National Petroleum Corporation","keywords":"Petroleum engineering; Oil shale; Caprock; Shale oil; Fossil fuel; Geology; Oil shale gas; Wellhead; Bubble point; Tight oil; Natural gas; Geochemistry; Chemistry; Bubble; Paleontology; Organic chemistry","score_opus":0.013500463591149134,"score_gpt":0.2537770433394001,"score_spread":0.24027657974825095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4288068417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985952,0.00018989496,0.0005722536,0.000023461656,0.000004951715,0.000005662542,0.00022518198,0.000054038617,0.0003292318],"genre_scores_gemma":[0.99857306,0.00009809121,0.00069893186,0.000015535685,0.0000019727538,0.00001028678,0.00018969725,0.0000088139495,0.0004035971],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999044,0.0000062475774,0.0000058179535,0.000024692263,0.00003689389,0.00002189404],"domain_scores_gemma":[0.9998011,0.000043167718,0.000043517157,0.0000082851675,0.00008262982,0.000021355962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012100081,0.00014761336,0.00015018485,0.00038886527,0.00029254664,0.00020560749,0.00016790055,0.00022022851,0.0009132918],"category_scores_gemma":[0.00019435468,0.00011728359,0.00019825638,0.0002203625,0.0002564821,0.00027209806,0.00016462707,0.00029088015,0.00014512894],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007623007,0.000020316378,0.003523189,0.000043820604,0.000005122017,0.0001461109,0.00010425279,0.0002146348,0.99436426,0.000038990915,0.000053595282,0.001409537],"study_design_scores_gemma":[0.0000043640684,0.00021660709,0.039544057,0.000010681773,0.00001601589,0.00011195357,0.00029191538,0.0057828194,0.9532155,0.00003222618,0.00075667177,0.000017234304],"about_ca_topic_score_codex":0.0044911937,"about_ca_topic_score_gemma":0.006644011,"teacher_disagreement_score":0.0044911937,"about_ca_system_score_codex":0.00026193698,"about_ca_system_score_gemma":0.00013503886,"threshold_uncertainty_score":0.008930087},"labels":[],"label_agreement":null},{"id":"W4293184316","doi":"10.2113/2022/7708357","title":"150 Myr of Episodic Metamorphism Recorded in the Yukon-Tanana Terrane, Northern Canadian Cordillera: Evidence from Monazite and Xenotime Petrochronology","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; University of Waterloo; Institut National de la Recherche Scientifique; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Metamorphic rock; Kyanite; Andalusite; Terrane; Metamorphism; Monazite; Sillimanite; Geochemistry; Zircon; Paleontology; Biotite; Quartz; Tectonics","score_opus":0.014252001854264222,"score_gpt":0.18332403345892406,"score_spread":0.16907203160465983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293184316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971765,0.0002967438,0.00009069796,0.00003980628,0.0000029965986,0.000009068329,0.0005132529,0.000017875249,0.0018530389],"genre_scores_gemma":[0.99896383,0.00011800633,0.00011836452,0.0000149899215,0.00000184605,0.0000041811863,0.00033438427,0.000004917179,0.0004393835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998387,0.000006360899,0.0000067421065,0.00004930743,0.000051126495,0.000047720398],"domain_scores_gemma":[0.9995616,0.00001983675,0.000070621965,0.000020887546,0.0002570245,0.00006994267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022135329,0.00024561127,0.00025420752,0.0018660057,0.0021648295,0.0007630451,0.0005025831,0.00035083774,0.0016262463],"category_scores_gemma":[0.0005288856,0.00017089461,0.00016150145,0.0016111978,0.0008565717,0.00024821283,0.00069344684,0.0002796649,0.00016372584],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001317626,0.000017066908,0.9586027,0.00009259064,0.0000934876,0.0006017733,0.0037340482,0.0004119255,0.019458046,0.00030872176,0.00081039337,0.015737386],"study_design_scores_gemma":[0.0000015708645,0.0000050738263,0.9977743,0.000010084554,0.0000100871985,0.00007609917,0.00053356495,0.00018580405,0.00024512294,0.000010878897,0.001142976,0.0000044449353],"about_ca_topic_score_codex":0.93421394,"about_ca_topic_score_gemma":0.98227215,"teacher_disagreement_score":0.06578606,"about_ca_system_score_codex":0.0072846073,"about_ca_system_score_gemma":0.004291243,"threshold_uncertainty_score":0.13234693},"labels":[],"label_agreement":null},{"id":"W4293190603","doi":"10.2113/2022/1192067","title":"Shear Response of Rough Rock Discontinuities Subjected to Impact Loading: Experimental Study and Theoretical Modelling","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Institute of Rock and Soil Mechanics, Chinese Academy of Sciences; State Key Laboratory of Geomechanics and Geotechnical Engineering; China Scholarship Council; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Classification of discontinuities; Discontinuity (linguistics); Cohesion (chemistry); Shear (geology); Weibull distribution; Geotechnical engineering; Materials science; Shear rate; Direct shear test; Geology; Composite material; Mathematics; Rheology","score_opus":0.011917614860356324,"score_gpt":0.2473953771520296,"score_spread":0.23547776229167328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293190603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99479806,0.00011565648,0.00439118,0.000010665963,0.0000043306395,0.000023441467,0.00014116375,0.00006011423,0.00045523062],"genre_scores_gemma":[0.9984848,0.0000900578,0.0011433717,0.0000028661334,0.0000013057701,0.000008938582,0.00006342137,0.0000037831014,0.00020139343],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997693,0.000014596574,0.000014709387,0.000039863677,0.00012025901,0.00004136021],"domain_scores_gemma":[0.9997249,0.00006917221,0.000066059496,0.000054394226,0.0000636249,0.000021785232],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003320698,0.00042432686,0.00034055905,0.0006328877,0.00020612843,0.00025005153,0.00041267063,0.0005743401,0.0019538985],"category_scores_gemma":[0.00046554464,0.00023731127,0.00028913302,0.00049446226,0.0004360905,0.00025016887,0.00027938906,0.00029095393,0.00025888463],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034460492,0.000106722175,0.0071996986,0.0001567249,0.000012204193,0.00034537402,0.00019374769,0.016033178,0.9682847,0.00015492781,0.000068033056,0.0070999716],"study_design_scores_gemma":[0.000034856446,0.001644205,0.085377365,0.0000330631,0.00005623864,0.00020721216,0.00040527614,0.16268098,0.7484701,0.00022217797,0.0008126223,0.00005589808],"about_ca_topic_score_codex":0.0012148017,"about_ca_topic_score_gemma":0.0013393831,"teacher_disagreement_score":0.0019538985,"about_ca_system_score_codex":0.0001959486,"about_ca_system_score_gemma":0.00014421847,"threshold_uncertainty_score":0.006536424},"labels":[],"label_agreement":null},{"id":"W4293215998","doi":"10.2113/2022/4087265","title":"Improved Unet in Lithology Identification of Coal Measure Strata","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Fundamental Research Funds for the Central Universities; State Key Laboratory of Coal Resources and Safe Mining","keywords":"Lithology; Geology; Identification (biology); Convolutional neural network; Feature (linguistics); Logging; Well logging; Set (abstract data type); Data set; Mining engineering; Pattern recognition (psychology); Computer science; Data mining; Artificial intelligence; Petrology; Geophysics","score_opus":0.01218556123547732,"score_gpt":0.22240952017895832,"score_spread":0.210223958943481,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293215998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.54238564,0.00081300596,0.44827113,0.00036654292,0.0001237201,0.000118906384,0.00053439155,0.0028493274,0.0045373165],"genre_scores_gemma":[0.904741,0.0001567988,0.090582244,0.000116886025,0.00003056488,0.000041518077,0.0007613499,0.000087657456,0.003482026],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99972373,0.000030790758,0.000019259436,0.00010165986,0.000071646464,0.000052917632],"domain_scores_gemma":[0.9996061,0.00009032823,0.000044312295,0.0000513172,0.0001821766,0.000025750369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006983931,0.0005064993,0.00055603246,0.0012396324,0.00032831248,0.00078096415,0.00093624357,0.0007689378,0.0012145622],"category_scores_gemma":[0.0011922971,0.00025019297,0.0006856962,0.00068969536,0.00029940647,0.001033588,0.0006713431,0.00055274204,0.00040596776],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037100312,0.0002467568,0.021888731,0.00011903714,0.00010694779,0.0002569001,0.00009274221,0.36257347,0.020877592,0.0012964486,0.0028071462,0.5893632],"study_design_scores_gemma":[0.0000058827122,0.0000245189,0.0026116094,0.0000050456324,0.0000096506055,0.000043883378,0.000014443447,0.9932326,0.0034579798,0.00026902498,0.00031977042,0.0000056651616],"about_ca_topic_score_codex":0.013098026,"about_ca_topic_score_gemma":0.016457869,"teacher_disagreement_score":0.013098026,"about_ca_system_score_codex":0.00068511744,"about_ca_system_score_gemma":0.0009229928,"threshold_uncertainty_score":0.026043594},"labels":[],"label_agreement":null},{"id":"W4293364455","doi":"10.2113/2022/3011662","title":"Early Paleozoic Continental Arc Mafic Magmatism in the North Qaidam Tectonic Belt: Implications for Subduction of the Proto-Tethyan Oceanic Lithosphere","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Fundamental Research Funds for the Central Universities; Natural Science Foundation of Anhui Province; National Natural Science Foundation of China","keywords":"Geology; Geochemistry; Mafic; Subduction; Zircon; Mantle wedge; Mantle (geology); Peridotite; Geochronology; Eclogite; Continental collision; Petrology; Tectonics; Paleontology","score_opus":0.01008426711862363,"score_gpt":0.19917199849860526,"score_spread":0.18908773137998164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293364455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99811506,0.00046052624,0.000079267396,0.000061958875,0.0000018546981,0.00000362033,0.000090100126,0.000003386915,0.0011842268],"genre_scores_gemma":[0.999286,0.0001967051,0.00012342051,0.000010970659,0.0000031062698,0.0000022174754,0.00007550079,0.0000015017245,0.00030059606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999547,0.000005630618,0.0000037065295,0.000013866473,0.0000076269203,0.000014476278],"domain_scores_gemma":[0.9999244,0.00000896702,0.000030198393,0.0000044200506,0.000019160043,0.000012830902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002271001,0.00018494674,0.0001685939,0.0010720075,0.00044110676,0.00054842664,0.00020921636,0.00021350774,0.0020183711],"category_scores_gemma":[0.00021331343,0.00015084777,0.00014373343,0.00085315463,0.0004568615,0.00037570644,0.00029878225,0.0001613103,0.00019877542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095586714,0.000024011655,0.950234,0.000078353965,0.000026451893,0.00031197938,0.00158645,0.00062343356,0.026872128,0.00074167247,0.00009118356,0.019314766],"study_design_scores_gemma":[0.0000015174008,0.000010360884,0.99899095,0.0000067437695,0.0000035205578,0.00004154068,0.0002526997,0.00020602731,0.00022454603,0.000045894423,0.0002151214,0.0000010790916],"about_ca_topic_score_codex":0.034674667,"about_ca_topic_score_gemma":0.047468003,"teacher_disagreement_score":0.034674667,"about_ca_system_score_codex":0.0013035615,"about_ca_system_score_gemma":0.0005202732,"threshold_uncertainty_score":0.068945706},"labels":[],"label_agreement":null},{"id":"W4306291336","doi":"10.2113/2022/1232390","title":"Quantifying Centimeter- to Microscale Heterogeneities in Sedimentary, Compositional, and Geomechanical Properties of Siltstone Deposits in the Lower Triassic Montney Formation, Northeastern British Columbia, Canada","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Siltstone; Geology; Sedimentary rock; Sedimentary structures; Geochemistry; Facies; Sedimentary depositional environment; Mineralogy; Geomorphology; Structural basin","score_opus":0.014694172767557225,"score_gpt":0.19390631636766478,"score_spread":0.17921214360010757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306291336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987197,0.00009509584,0.00010970859,0.000009347569,5.8194985e-7,0.000009301603,0.00037685386,0.00000897121,0.00067046704],"genre_scores_gemma":[0.9986731,0.00008063548,0.00021264545,0.000010263272,8.8787465e-7,0.000007522324,0.00036416194,0.0000042021243,0.0006466924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976975,0.000007355528,0.00001218604,0.000056180375,0.00009011516,0.00006451624],"domain_scores_gemma":[0.9995995,0.000023481245,0.00007663968,0.000013742216,0.0002134458,0.00007318304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016661783,0.00032925155,0.0002395763,0.0029039145,0.0015453905,0.0009879486,0.00041757702,0.0002274236,0.0010846143],"category_scores_gemma":[0.0004335542,0.00023848645,0.00017545038,0.0023944462,0.0006441548,0.0002263176,0.00053784484,0.00017977088,0.00018509121],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006449055,0.000017158514,0.963125,0.00003457986,0.00006518743,0.00019292177,0.0012999247,0.00042454328,0.023878751,0.000057973757,0.00020182041,0.010637619],"study_design_scores_gemma":[4.2682345e-7,0.0000018696117,0.99924266,0.0000019447118,0.000003128939,0.0000122725905,0.00023903215,0.00012912611,0.0002309037,0.0000033733183,0.00013399808,0.000001276853],"about_ca_topic_score_codex":0.9253748,"about_ca_topic_score_gemma":0.9809248,"teacher_disagreement_score":0.074625194,"about_ca_system_score_codex":0.004499674,"about_ca_system_score_gemma":0.002627146,"threshold_uncertainty_score":0.15012932},"labels":[],"label_agreement":null},{"id":"W4311923524","doi":"10.2113/2022/9601288","title":"Complex Late Triassic-Middle Jurassic Subduction-Related Magmatic History from Detritus of Nominal Middle Jurassic Brooks Range Ophiolite, Northern Alaska","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Vetenskapsrådet","keywords":"Terrane; Geology; Ophiolite; Igneous rock; Geochemistry; Continental crust; Paleontology; Subduction; Oceanic crust; Clastic rock; Zircon; Sedimentary rock; Crust; Tectonics","score_opus":0.03163369093775196,"score_gpt":0.18373085921935164,"score_spread":0.1520971682815997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311923524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991424,0.00010048834,0.00003543589,0.00000518164,0.0000014511764,0.0000010994999,0.000082565224,0.0000019810298,0.00062935444],"genre_scores_gemma":[0.999124,0.0000925303,0.00005716741,0.0000034208879,0.0000010566445,0.0000014243284,0.00015321322,0.0000012117702,0.0005659723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999529,0.0000026753664,0.0000057673897,0.000017295808,0.000010362833,0.000011042905],"domain_scores_gemma":[0.99992466,0.00000681465,0.000017886672,0.0000056505673,0.000021353266,0.000023700824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009812008,0.00012729697,0.00008876989,0.0006482935,0.0006486273,0.0004955104,0.000098225115,0.000098512806,0.0012174404],"category_scores_gemma":[0.00014975741,0.000077034216,0.00007415427,0.0004574805,0.00021247793,0.00021394955,0.00031078735,0.00011130749,0.00014226789],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004926637,0.000009507101,0.96683425,0.0000242127,0.00001630767,0.0002285422,0.0014122572,0.00009091829,0.024603717,0.000078711295,0.00004109405,0.0066111675],"study_design_scores_gemma":[4.0554542e-7,0.00000736722,0.998281,0.0000031456682,0.000004693235,0.00008606769,0.00059283694,0.000031721196,0.00063811056,0.000017945686,0.00033565745,9.635273e-7],"about_ca_topic_score_codex":0.037991483,"about_ca_topic_score_gemma":0.14989029,"teacher_disagreement_score":0.037991483,"about_ca_system_score_codex":0.00046189793,"about_ca_system_score_gemma":0.00035333418,"threshold_uncertainty_score":0.07554072},"labels":[],"label_agreement":null},{"id":"W4315701619","doi":"10.2113/2022/9823275","title":"Resolving Quaternary Tectonic Activity with High-Resolution Data in Space and Time","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Institute of Geology, China Earthquake Administration; National Natural Science Foundation of China","keywords":"Geology; Tectonics; Active fault; Seismology; Fault (geology); Paleoseismology; Quaternary; Geologic record; Paleontology","score_opus":0.015770073779200817,"score_gpt":0.21067429460194362,"score_spread":0.1949042208227428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315701619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5111033,0.09535609,0.18853109,0.0382271,0.041860726,0.00028052562,0.06320335,0.008241344,0.05319654],"genre_scores_gemma":[0.6933131,0.037420746,0.1460078,0.0041802237,0.03345458,0.00015109146,0.06541835,0.0023110213,0.0177431],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9994573,0.000074192074,0.000060739923,0.00013416562,0.00020597296,0.00006757565],"domain_scores_gemma":[0.9974783,0.0005035403,0.00039105842,0.00037519127,0.00092855335,0.00032330744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020183348,0.00041855322,0.0007321719,0.003148223,0.00066431466,0.0034506053,0.00085724326,0.0012757793,0.004390512],"category_scores_gemma":[0.004019967,0.0004424706,0.0004938415,0.0038069582,0.00048354844,0.0021352647,0.0019024343,0.0014237834,0.0018571969],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003481808,0.00025868902,0.15863676,0.0013262149,0.00062999135,0.0013309916,0.001250265,0.02196149,0.053566888,0.007264075,0.2607642,0.49266222],"study_design_scores_gemma":[0.00007725272,0.00016093542,0.27989125,0.0005735558,0.0003983771,0.00081252115,0.0011684237,0.1068041,0.0117877675,0.01477952,0.5833195,0.00022675801],"about_ca_topic_score_codex":0.0043255542,"about_ca_topic_score_gemma":0.010453315,"teacher_disagreement_score":0.004390512,"about_ca_system_score_codex":0.00048044603,"about_ca_system_score_gemma":0.00070138054,"threshold_uncertainty_score":0.014687717},"labels":[],"label_agreement":null},{"id":"W4316037421","doi":"10.2113/2023/8926187","title":"Failure Mechanisms and Constitutive Model of Composite Rock under Dynamic Loading","year":2023,"lang":"en","type":"article","venue":"Lithosphere","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Fundamental Research Funds for the Central Universities","keywords":"Composite number; Dissipation; Split-Hopkinson pressure bar; Elastic modulus; Materials science; Joint (building); Rock mechanics; Constitutive equation; Stress (linguistics); Composite material; Geotechnical engineering; Structural engineering; Geology; Strain rate; Finite element method; Engineering","score_opus":0.010786791534657806,"score_gpt":0.21156871833323868,"score_spread":0.20078192679858087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4316037421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7899954,0.00047478886,0.19721636,0.00018296015,0.000032085176,0.000073330666,0.0003764887,0.00039258922,0.01125595],"genre_scores_gemma":[0.9946926,0.000114141934,0.002943727,0.000009646541,0.0000043267546,0.000037103353,0.00008522997,0.000012872514,0.002100525],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997615,0.000025706473,0.0000135659975,0.000057631325,0.00010960352,0.000031864398],"domain_scores_gemma":[0.99980587,0.000038634193,0.000056813777,0.000031735945,0.000051749714,0.000015164961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030487534,0.0004657584,0.00033656915,0.0011565837,0.0003207013,0.0004449072,0.0010364639,0.0008039384,0.0013797093],"category_scores_gemma":[0.00042186232,0.00029572414,0.0005117801,0.00044866017,0.00080649665,0.0005938157,0.00028462402,0.00028782935,0.00031507024],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000737377,0.00008210305,0.007437889,0.00009975987,0.000025484816,0.00062007713,0.00014507752,0.90676624,0.068033904,0.0076729795,0.00028561722,0.0087571535],"study_design_scores_gemma":[0.0000035636124,0.000020324642,0.0019288983,0.000004155947,0.0000050698245,0.00009108812,0.000022560687,0.9946577,0.0024228103,0.00060335477,0.00023253843,0.000007936118],"about_ca_topic_score_codex":0.0065736347,"about_ca_topic_score_gemma":0.0028932241,"teacher_disagreement_score":0.0065736347,"about_ca_system_score_codex":0.00042722665,"about_ca_system_score_gemma":0.000614815,"threshold_uncertainty_score":0.013070762},"labels":[],"label_agreement":null},{"id":"W4390103467","doi":"10.2113/2023/lithosphere_2023_254","title":"Melting of Subducted Continental Crust in the Cimmerian Collisional Orogenic Belt, NE Iran","year":2023,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Chinese Academy of Sciences; Geological Survey and Mineral Exploration of Iran; National Natural Science Foundation of China","keywords":"Terrane; Geology; Zircon; Continental crust; Geochemistry; Subduction; Crust; Metamorphism; Fibrous joint; Oceanic crust; Partial melting; Petrology; Paleontology; Tectonics","score_opus":0.019511161870719145,"score_gpt":0.21820033795493646,"score_spread":0.19868917608421732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390103467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989687,0.00017961724,0.00004202681,0.000009802331,0.000001212229,0.0000026432076,0.00008238713,0.0000039638326,0.00070965674],"genre_scores_gemma":[0.9994856,0.00012494676,0.0000760985,0.0000053860394,0.0000019220329,0.0000017028609,0.00015873999,0.0000018562744,0.00014371824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999093,0.000005261244,0.000006848267,0.00002348606,0.00002379447,0.00003135459],"domain_scores_gemma":[0.99993193,0.000004145222,0.00003368887,0.0000063975453,0.000017123579,0.0000066746943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018281944,0.00021076707,0.00014948449,0.0017081936,0.00047468705,0.0004153423,0.00024624015,0.00015068288,0.000784879],"category_scores_gemma":[0.00019550014,0.00013528811,0.00016305824,0.0012505364,0.00027872075,0.00018902242,0.00032683933,0.00011452454,0.00014149539],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018668093,0.00002641323,0.94508827,0.000058459547,0.00007212431,0.0006489384,0.0014164896,0.00052811584,0.030849423,0.00019099754,0.00014323989,0.020790908],"study_design_scores_gemma":[0.00000270133,0.000014425137,0.9980313,0.0000046177674,0.000008981441,0.00011463202,0.00031316144,0.00010204192,0.0007000359,0.000018219282,0.00068846747,0.0000013517467],"about_ca_topic_score_codex":0.03168356,"about_ca_topic_score_gemma":0.03670967,"teacher_disagreement_score":0.03168356,"about_ca_system_score_codex":0.0009186732,"about_ca_system_score_gemma":0.00036007547,"threshold_uncertainty_score":0.062998295},"labels":[],"label_agreement":null},{"id":"W4396506027","doi":"10.2113/2024/lithosphere_2023_285","title":"Compilation of Apatite Fission-Track Data from the Northeast Atlantic Realm: A Jigsaw Puzzle with Missing Pieces","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto","funders":"","keywords":"Jigsaw; Fission track dating; Apatite; Geology; Track (disk drive); Realm; Paleontology; Archaeology; Geochemistry; Geography; Computer science; Mathematics education","score_opus":0.018948382518088287,"score_gpt":0.2537891322918127,"score_spread":0.23484074977372443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396506027","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49049166,0.035193946,0.028816495,0.0054077297,0.0018067699,0.0003500279,0.40195835,0.0022406636,0.033734415],"genre_scores_gemma":[0.37843394,0.02517454,0.10059748,0.0016673745,0.0011746346,0.0005360815,0.48140895,0.002013383,0.008993568],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99773955,0.00014792872,0.00047382087,0.00033554676,0.0011885235,0.00011450817],"domain_scores_gemma":[0.975276,0.0037362245,0.0024576217,0.0029709039,0.014334779,0.0012244734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0036851522,0.00049545587,0.0006021615,0.013130748,0.0009222171,0.002298501,0.0009875891,0.0005262423,0.0020069687],"category_scores_gemma":[0.011029195,0.00034507402,0.0005217708,0.012669869,0.00067274383,0.00096404506,0.002023136,0.00086847163,0.0011218452],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003746107,0.00012613097,0.3804344,0.005056307,0.00066026655,0.0021414256,0.0044040424,0.0019164389,0.027402502,0.0025631804,0.061526924,0.51339376],"study_design_scores_gemma":[0.00001965052,0.000053373904,0.5867767,0.002294447,0.00018999036,0.00043768375,0.0016508893,0.0007931387,0.0033367793,0.00088239077,0.40347755,0.00008751103],"about_ca_topic_score_codex":0.12108226,"about_ca_topic_score_gemma":0.2615733,"teacher_disagreement_score":0.12108226,"about_ca_system_score_codex":0.0014922325,"about_ca_system_score_gemma":0.004781365,"threshold_uncertainty_score":0.24075496},"labels":[],"label_agreement":null},{"id":"W4399534895","doi":"10.2113/2023/lithosphere_2023_285","title":"Compilation of Apatite Fission-Track Data from the Northeast Atlantic Realm: A Jigsaw Puzzle with Missing Pieces","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto","funders":"","keywords":"Fission track dating; Geology; Thermochronology; Paleontology; Tectonics; Physical geography; Earth science; Geography","score_opus":0.044698509798556656,"score_gpt":0.23686951321790525,"score_spread":0.1921710034193486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399534895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49049166,0.035193946,0.028816495,0.0054077297,0.0018067699,0.0003500279,0.40195835,0.0022406636,0.033734415],"genre_scores_gemma":[0.37843394,0.02517454,0.10059748,0.0016673745,0.0011746346,0.0005360815,0.48140895,0.002013383,0.008993568],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99773955,0.00014792872,0.00047382087,0.00033554676,0.0011885235,0.00011450817],"domain_scores_gemma":[0.975276,0.0037362245,0.0024576217,0.0029709039,0.014334779,0.0012244734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0036851522,0.00049545587,0.0006021615,0.013130748,0.0009222171,0.002298501,0.0009875891,0.0005262423,0.0020069687],"category_scores_gemma":[0.011029195,0.00034507402,0.0005217708,0.012669869,0.00067274383,0.00096404506,0.002023136,0.00086847163,0.0011218452],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003746107,0.00012613097,0.3804344,0.005056307,0.00066026655,0.0021414256,0.0044040424,0.0019164389,0.027402502,0.0025631804,0.061526924,0.51339376],"study_design_scores_gemma":[0.00001965052,0.000053373904,0.5867767,0.002294447,0.00018999036,0.00043768375,0.0016508893,0.0007931387,0.0033367793,0.00088239077,0.40347755,0.00008751103],"about_ca_topic_score_codex":0.12108226,"about_ca_topic_score_gemma":0.2615733,"teacher_disagreement_score":0.12108226,"about_ca_system_score_codex":0.0014922325,"about_ca_system_score_gemma":0.004781365,"threshold_uncertainty_score":0.24075496},"labels":[],"label_agreement":null},{"id":"W4402411029","doi":"10.2113/2024/lithosphere_2024_114","title":"The Miocene Acceleration of Strike-Slip Deformation in the Northern Tian Shan, Central Asia","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Central asia; Seismology; Tian; Strike-slip tectonics; Slip (aerodynamics); Deformation (meteorology); Paleontology; Tectonics; Physical geography; Geography; Ancient history; Oceanography","score_opus":0.009837345283311223,"score_gpt":0.19664790640595975,"score_spread":0.18681056112264852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402411029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990202,0.00006256581,0.00010542852,0.000021620948,0.0000017146979,0.0000014428563,0.00013779891,0.000009140542,0.00064015284],"genre_scores_gemma":[0.9995049,0.0000473386,0.000053986485,0.0000034384543,0.0000010482844,0.0000015225735,0.00014891781,0.0000018072595,0.00023699454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999664,0.0000029990047,0.000003071925,0.000011854813,0.0000073516658,0.00000831322],"domain_scores_gemma":[0.999931,0.000006070149,0.000016715876,0.00000797201,0.000025401017,0.000012868877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011951774,0.00018737727,0.00011121551,0.0006443067,0.000315393,0.00038279645,0.00019355689,0.00014801323,0.000894972],"category_scores_gemma":[0.00016298192,0.00012019881,0.00017483899,0.00086711266,0.00022632278,0.0001826386,0.00020993613,0.00011158092,0.00012617644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010949953,0.000025937727,0.94650525,0.00008243133,0.00008902215,0.0005362265,0.0016386864,0.0074315206,0.020459432,0.00030372044,0.00037923042,0.022439057],"study_design_scores_gemma":[0.0000032912776,0.00001678293,0.9931519,0.0000074483605,0.000022115408,0.000082495666,0.00036748947,0.0047243345,0.0008564267,0.00005151371,0.00071041693,0.000005765651],"about_ca_topic_score_codex":0.073712274,"about_ca_topic_score_gemma":0.12121991,"teacher_disagreement_score":0.073712274,"about_ca_system_score_codex":0.00083189394,"about_ca_system_score_gemma":0.000651361,"threshold_uncertainty_score":0.14656645},"labels":[],"label_agreement":null},{"id":"W4402518877","doi":"10.2113/2023/lithosphere_2024_114","title":"The Miocene Acceleration of Strike-Slip Deformation in the Northern Tian Shan, Central Asia","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; China Scholarship Council","keywords":"Geology; Central asia; Seismology; Tian; Slip (aerodynamics); Deformation (meteorology); Late Miocene; Paleontology; Physical geography; Geography; Ancient history; Oceanography; History","score_opus":0.009837345283311223,"score_gpt":0.19664790640595975,"score_spread":0.18681056112264852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402518877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990202,0.00006256581,0.00010542852,0.000021620948,0.0000017146979,0.0000014428563,0.00013779891,0.000009140542,0.00064015284],"genre_scores_gemma":[0.9995049,0.0000473386,0.000053986485,0.0000034384543,0.0000010482844,0.0000015225735,0.00014891781,0.0000018072595,0.00023699454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999664,0.0000029990047,0.000003071925,0.000011854813,0.0000073516658,0.00000831322],"domain_scores_gemma":[0.999931,0.000006070149,0.000016715876,0.00000797201,0.000025401017,0.000012868877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011951774,0.00018737727,0.00011121551,0.0006443067,0.000315393,0.00038279645,0.00019355689,0.00014801323,0.000894972],"category_scores_gemma":[0.00016298192,0.00012019881,0.00017483899,0.00086711266,0.00022632278,0.0001826386,0.00020993613,0.00011158092,0.00012617644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010949953,0.000025937727,0.94650525,0.00008243133,0.00008902215,0.0005362265,0.0016386864,0.0074315206,0.020459432,0.00030372044,0.00037923042,0.022439057],"study_design_scores_gemma":[0.0000032912776,0.00001678293,0.9931519,0.0000074483605,0.000022115408,0.000082495666,0.00036748947,0.0047243345,0.0008564267,0.00005151371,0.00071041693,0.000005765651],"about_ca_topic_score_codex":0.073712274,"about_ca_topic_score_gemma":0.12121991,"teacher_disagreement_score":0.073712274,"about_ca_system_score_codex":0.00083189394,"about_ca_system_score_gemma":0.000651361,"threshold_uncertainty_score":0.14656645},"labels":[],"label_agreement":null},{"id":"W4403251406","doi":"10.2113/2024/lithosphere_2023_299","title":"The Benkar Fault Zone: An Orogen-Scale Cross Fault in the Eastern Nepal Himalaya","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Teck (Canada)","funders":"","keywords":"Geology; Fault (geology); Seismology; Scale (ratio); Normal fault; Geography; Cartography","score_opus":0.014115605177614883,"score_gpt":0.2573157925065447,"score_spread":0.2432001873289298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403251406","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935055,0.00027445742,0.00020059216,0.00006943501,0.000002798116,0.000012884696,0.00013863522,0.000010042959,0.00578573],"genre_scores_gemma":[0.99931467,0.00007048935,0.00016391592,0.000012383641,0.0000016120451,0.0000039932493,0.00007812272,0.0000010834335,0.00035370502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999068,0.000012552688,0.0000063678144,0.000025674337,0.000017785891,0.00003092725],"domain_scores_gemma":[0.9999167,0.000021032512,0.000023270703,0.0000070363208,0.000021291176,0.000010704773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008563747,0.0001327896,0.00011063165,0.0013425894,0.0006006583,0.0006625986,0.00016658255,0.00024187118,0.0014809502],"category_scores_gemma":[0.00028673786,0.000100562946,0.0000691246,0.0014363677,0.00043248612,0.0002869698,0.00048545699,0.0001264677,0.0001484088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010120697,0.000046045414,0.90492463,0.0001858767,0.000063688814,0.0032602923,0.0084693665,0.0010362348,0.016584568,0.0017811545,0.00046464388,0.06308223],"study_design_scores_gemma":[0.00000468837,0.000022433636,0.99238104,0.000039805684,0.000015818889,0.001108772,0.0025842404,0.000600379,0.00067656586,0.00023820558,0.0023203231,0.0000076265414],"about_ca_topic_score_codex":0.019060062,"about_ca_topic_score_gemma":0.03254195,"teacher_disagreement_score":0.019060062,"about_ca_system_score_codex":0.00043836495,"about_ca_system_score_gemma":0.0003208221,"threshold_uncertainty_score":0.037898242},"labels":[],"label_agreement":null},{"id":"W4404379954","doi":"10.2113/2023/lithosphere_2024_220","title":"Low-Temperature Thermochronology: Advances, Applications, and Innovations in Tectonics, Earth Surface Processes and Ore Deposits","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Chinese Academy of Geological Sciences; National Natural Science Foundation of China","keywords":"Thermochronology; Geology; Tectonics; Earth surface; Earth science; Earth (classical element); Geochemistry; Astrobiology; Seismology","score_opus":0.004236549200888021,"score_gpt":0.1969586111683165,"score_spread":0.19272206196742847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404379954","genre_codex":"methods","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.30920684,0.18128811,0.46996856,0.004327918,0.0015347775,0.0001215604,0.0029791235,0.0023962667,0.028176846],"genre_scores_gemma":[0.7837348,0.05367399,0.15154858,0.00065477204,0.0009236267,0.00009173776,0.0012644012,0.0008143355,0.0072937277],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99949276,0.0001344854,0.000035204474,0.00018148716,0.00012915314,0.000026899823],"domain_scores_gemma":[0.9985079,0.00038233737,0.00029619387,0.0002724646,0.00047969,0.000061403385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024760033,0.0006077445,0.00061581895,0.002046581,0.00040662056,0.0022809391,0.001014382,0.00064754236,0.0015714773],"category_scores_gemma":[0.003253065,0.00031652622,0.0004048111,0.004401964,0.001514175,0.0018381717,0.0011615293,0.0010407794,0.0006098859],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055211375,0.00012441915,0.15390083,0.0016423907,0.00024315756,0.00014498236,0.0009627941,0.014263732,0.06791049,0.039028008,0.0030465808,0.7181805],"study_design_scores_gemma":[0.000115401795,0.00070226844,0.36983404,0.0011195756,0.00076383824,0.0020554366,0.0013286023,0.12649603,0.14047147,0.105457686,0.25129527,0.000360375],"about_ca_topic_score_codex":0.0033751125,"about_ca_topic_score_gemma":0.0055144704,"teacher_disagreement_score":0.0033751125,"about_ca_system_score_codex":0.00095165294,"about_ca_system_score_gemma":0.0012972573,"threshold_uncertainty_score":0.013094544},"labels":[],"label_agreement":null},{"id":"W4404413347","doi":"10.2113/2024/lithosphere_2024_145","title":"A New Geological Map of the Marginal Basins of Eastern Papua New Guinea: Implications for Crustal Accretion and Mineral Endowment at Arc–Continent Collisions","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; Mount Royal University; University of Ottawa","funders":"","keywords":"New guinea; Geology; Accretion (finance); Endowment; Seismology; Arc (geometry); Structural basin; Geochemistry; Paleontology; Geometry; History; Law; Political science","score_opus":0.015821911442803625,"score_gpt":0.22287259224486686,"score_spread":0.20705068080206324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404413347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95281434,0.0035611468,0.0017177231,0.00058715144,0.000076767305,0.00015825621,0.0113913445,0.00019416139,0.029499065],"genre_scores_gemma":[0.9840678,0.0015877844,0.00756918,0.000048013077,0.000025615374,0.0001078787,0.0028745402,0.000022668137,0.0036965148],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999558,0.000006581184,0.0000051697803,0.00001023311,0.0000101361,0.000012168726],"domain_scores_gemma":[0.9997876,0.000036292666,0.00005576108,0.000021474943,0.00007132115,0.000027530388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013878572,0.00021143834,0.00012250835,0.0039616884,0.0002935267,0.0004891423,0.00022640525,0.00013072816,0.004832638],"category_scores_gemma":[0.00052649993,0.0001177035,0.00012990591,0.003477905,0.00024773594,0.00040190894,0.0006700104,0.00019081717,0.00028940523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026295788,0.00011928272,0.6026237,0.0016667057,0.00017915512,0.0032647487,0.008853218,0.004470936,0.027133055,0.0045538917,0.008740275,0.33813208],"study_design_scores_gemma":[0.0000071582,0.000029547788,0.9682576,0.00018100231,0.000027826836,0.0006594361,0.0015260411,0.000714284,0.00054349995,0.00035577864,0.027687915,0.000009928287],"about_ca_topic_score_codex":0.046288185,"about_ca_topic_score_gemma":0.06639316,"teacher_disagreement_score":0.046288185,"about_ca_system_score_codex":0.00042548325,"about_ca_system_score_gemma":0.0006044279,"threshold_uncertainty_score":0.09203756},"labels":[],"label_agreement":null},{"id":"W4407033326","doi":"10.2113/2025/lithosphere_2024_227","title":"<b>Titanomagnetite Rims on Hornblende Phenocrysts in Intermediate Subvolcanic Intrusions, Torud–Ahmad Abad Magmatic Belt, Iran: Examination of</b> <b>Devolatilization and Oxidation Processes</b>","year":2025,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Phenocryst; Geology; Geochemistry; Hornblende; Andesite; Pyroxene; Felsic; Diorite; Mafic; Volcanic rock; Dacite; Igneous rock; Petrology; Olivine; Biotite; Quartz; Zircon; Volcano","score_opus":0.006610806114811124,"score_gpt":0.1991291409582275,"score_spread":0.19251833484341638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407033326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992447,0.00015336127,0.00003344781,0.000009001437,0.0000017095847,0.0000028634333,0.00011098032,0.000005484357,0.00043858273],"genre_scores_gemma":[0.99933225,0.00006672622,0.00008415733,0.0000071702902,0.0000022104284,0.0000023388097,0.00014905291,0.0000027909546,0.00035323866],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99995184,0.0000030860656,0.0000032025835,0.000014001763,0.000015369586,0.000012460815],"domain_scores_gemma":[0.99991405,0.0000063174502,0.000030651874,0.0000029860537,0.000028116421,0.000017835993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008469571,0.00015936393,0.000121193414,0.0013686143,0.000306741,0.00030422874,0.00020658018,0.00023144996,0.00077131635],"category_scores_gemma":[0.0000971343,0.00016029619,0.00012076198,0.00048729684,0.00024708346,0.00014681017,0.0001717624,0.00012384664,0.00018353204],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023308878,0.00005024824,0.79548836,0.00006938808,0.00005133492,0.00080133247,0.0011424859,0.000082979685,0.19411044,0.00006164198,0.00016826294,0.007740502],"study_design_scores_gemma":[9.976279e-7,0.000011781491,0.99810886,0.0000016374498,0.0000030878869,0.00011681309,0.00021344238,0.000034783217,0.0012981269,0.0000052701844,0.00020457996,6.918307e-7],"about_ca_topic_score_codex":0.018309265,"about_ca_topic_score_gemma":0.039623123,"teacher_disagreement_score":0.018309265,"about_ca_system_score_codex":0.00029203168,"about_ca_system_score_gemma":0.00013065562,"threshold_uncertainty_score":0.036405385},"labels":[],"label_agreement":null},{"id":"W4407044651","doi":"10.2113/2025/lithosphere_2024_224","title":"Dating Subhorizontal Ductile Fabric in the Feidong Complex via Zircon and Titanite U–Pb Geochronology: Insights into Middle Triassic Transpressional Deformation along the Southern Tan-Lu Fault Zone","year":2025,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Geology; Zircon; Geochronology; Foreland basin; Geochemistry; Metamorphic rock; Fault (geology); Thrust fault; Seismology; Continental collision; Petrology; Tectonics; Subduction","score_opus":0.01346044588242943,"score_gpt":0.20409245172824247,"score_spread":0.19063200584581305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407044651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999464,0.00005129039,0.00016006213,0.0000031093366,5.315183e-7,0.0000018053182,0.000052190437,0.000004577639,0.00026260564],"genre_scores_gemma":[0.99945396,0.0000381673,0.00021594277,0.0000025047384,8.2359486e-7,0.0000025990719,0.00008539802,0.0000028379454,0.00019783374],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999218,0.0000058948044,0.0000067368824,0.000029012148,0.000018926516,0.000017500328],"domain_scores_gemma":[0.9999219,0.000006442372,0.000023429286,0.00000798147,0.000026366257,0.000013800978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025140267,0.00026159704,0.00016995227,0.0016665902,0.00048498058,0.0005197372,0.00020510836,0.00021389387,0.0006007316],"category_scores_gemma":[0.00020633826,0.0001847097,0.00012518176,0.00091500283,0.00032593883,0.00028159397,0.00034733606,0.000084936975,0.000112462185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007131198,0.000012229816,0.9180792,0.00002189723,0.00003488911,0.0001513844,0.0009233443,0.0005446002,0.06701507,0.00013721827,0.00004469617,0.012964102],"study_design_scores_gemma":[0.0000018413953,0.000012836532,0.9972198,0.0000018882258,0.0000071377817,0.000059179452,0.00015383468,0.0004488843,0.00177902,0.00001672431,0.00029680645,0.0000019244194],"about_ca_topic_score_codex":0.02282067,"about_ca_topic_score_gemma":0.048555963,"teacher_disagreement_score":0.02282067,"about_ca_system_score_codex":0.00051896146,"about_ca_system_score_gemma":0.00028588268,"threshold_uncertainty_score":0.045375705},"labels":[],"label_agreement":null},{"id":"W4407836374","doi":"10.2113/2023/lithosphere_2023_293","title":"Uplift History of the Eastern Pamir Inferred from Inversion of Thermochronometric Data and River Profile","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Inversion (geology); Seismology; Tectonics","score_opus":0.039163074186685194,"score_gpt":0.2029651826452186,"score_spread":0.1638021084585334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407836374","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985669,0.000029062747,0.00026273725,0.0000073894503,0.0000013681826,0.000002256905,0.00009365202,0.000019574576,0.0010170079],"genre_scores_gemma":[0.9995635,0.000013080206,0.00021054751,0.0000024248848,9.3583714e-7,0.0000014073977,0.00008523341,0.000002859418,0.00012000275],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992204,0.000011025411,0.000005595768,0.00002798551,0.000014513265,0.00001876756],"domain_scores_gemma":[0.99989605,0.000016577194,0.0000306904,0.0000149302705,0.00003249064,0.000009240644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020368045,0.00016535104,0.0001427846,0.0008303741,0.00021151135,0.0003312524,0.00022051719,0.00014839761,0.0008749157],"category_scores_gemma":[0.00035492986,0.00014745581,0.00012451259,0.0007601087,0.00018793876,0.00016234367,0.00033598088,0.00015099125,0.00022384194],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021585186,0.000029274479,0.9001488,0.000050575014,0.000071165254,0.00057219085,0.00072784664,0.00254215,0.06154134,0.00044409325,0.00020088507,0.03345584],"study_design_scores_gemma":[0.0000023883006,0.000027841774,0.9937509,0.000004549164,0.000013286742,0.0001195833,0.0001236916,0.0032214369,0.0021725588,0.000033790868,0.00052593654,0.0000039883116],"about_ca_topic_score_codex":0.0077339574,"about_ca_topic_score_gemma":0.014988311,"teacher_disagreement_score":0.0077339574,"about_ca_system_score_codex":0.00020867765,"about_ca_system_score_gemma":0.00017641715,"threshold_uncertainty_score":0.015377879},"labels":[],"label_agreement":null},{"id":"W4409163981","doi":"10.2113/2025/lithosphere_2024_193","title":"Hydrothermal Vesuvianite: A U-Pb Dating Mineral","year":2025,"lang":"en","type":"article","venue":"Lithosphere","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Natural Science Foundation of China","keywords":"Hydrothermal circulation; Geology; Mineral; Geochemistry; Mineralogy; Seismology; Materials science; Metallurgy","score_opus":0.006063208963333846,"score_gpt":0.19564216244003707,"score_spread":0.18957895347670323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409163981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938512,0.001010614,0.0016146348,0.000048786067,0.000008059329,0.000012836199,0.00045946043,0.000070139606,0.0029243822],"genre_scores_gemma":[0.9957438,0.00019165073,0.0028339343,0.000010531536,0.0000056642307,0.0000052514724,0.0002488062,0.000011774486,0.000948502],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992156,0.0000068720083,0.0000046710916,0.000033727672,0.00002271324,0.000010432663],"domain_scores_gemma":[0.9999521,0.000006422457,0.000014304326,0.0000055243313,0.000014317114,0.0000073478523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010179918,0.00023014085,0.00015516291,0.00093542103,0.00037264603,0.00046190142,0.00022473863,0.00019285463,0.001009371],"category_scores_gemma":[0.00017275877,0.00010322745,0.00007790282,0.0007291162,0.00030392146,0.00025472624,0.00040386865,0.0001239921,0.00013981327],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014253706,0.000017682314,0.12645008,0.00018350585,0.00004099746,0.00078514573,0.0003615032,0.0004563122,0.82779425,0.0007146189,0.00028606597,0.04276739],"study_design_scores_gemma":[0.000021538537,0.00016002488,0.7030867,0.000041602107,0.000049982267,0.0023662192,0.0004131548,0.0038675277,0.24830115,0.00049989583,0.04117011,0.000022186436],"about_ca_topic_score_codex":0.0050357548,"about_ca_topic_score_gemma":0.0050007068,"teacher_disagreement_score":0.0050357548,"about_ca_system_score_codex":0.00024137936,"about_ca_system_score_gemma":0.00021310119,"threshold_uncertainty_score":0.010012865},"labels":[],"label_agreement":null},{"id":"W4414849541","doi":"10.2113/2025/lithosphere_2025_107","title":"Pore-Scale Assessment of Gas Expansion Induced by Formation Uplift in Tight Sandstones","year":2025,"lang":"en","type":"article","venue":"Lithosphere","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Petro-Canada","funders":"PetroChina Company Limited; National Natural Science Foundation of China","keywords":"Tight gas; Natural gas; Natural gas field; Saturation (graph theory); Homogeneous; RADIUS","score_opus":0.006030146544024859,"score_gpt":0.24787072415310207,"score_spread":0.2418405776090772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414849541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99805427,0.0000704089,0.0013180937,0.0000051989023,0.0000025741635,0.0000057872912,0.00013755923,0.000057069945,0.00034895175],"genre_scores_gemma":[0.99895227,0.000029448338,0.00075556565,0.0000046247537,0.0000010870805,0.000004350823,0.00007497862,0.0000053269237,0.00017247822],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985707,0.000009376385,0.000008113439,0.00004472698,0.0000476897,0.000033007364],"domain_scores_gemma":[0.9998165,0.000038850638,0.00003938879,0.000014507153,0.000060698047,0.00003013682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024628238,0.00019525777,0.00018746806,0.0009020998,0.00028176396,0.00036996737,0.00022664259,0.00026481313,0.0008527085],"category_scores_gemma":[0.0003288055,0.00016224355,0.00015221913,0.00041760187,0.00039345946,0.00045487168,0.00041677608,0.00025750557,0.00010181112],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026821776,0.000040790022,0.060422663,0.00012032471,0.000028441282,0.00028178527,0.0003525384,0.0016994814,0.9261708,0.00023063897,0.000085345295,0.010298979],"study_design_scores_gemma":[0.000014120124,0.0002432394,0.6553185,0.000018377692,0.00005922002,0.00037535976,0.00077147735,0.026141329,0.31517035,0.00024414368,0.0015940982,0.000049709382],"about_ca_topic_score_codex":0.004807733,"about_ca_topic_score_gemma":0.007384809,"teacher_disagreement_score":0.004807733,"about_ca_system_score_codex":0.00024439284,"about_ca_system_score_gemma":0.0001925891,"threshold_uncertainty_score":0.009559512},"labels":[],"label_agreement":null}]}