{"meta":{"query_hash":"011dbca685ad","filters":{"venue":"Russian Geology and Geophysics"},"cohort_total":39,"direct_labels_cover":0,"predictions_cover":39,"exported":39,"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/011dbca685ad","api":"https://metacan.xera.ac/api/v1/cohort?venue=Russian+Geology+and+Geophysics"},"results":[{"id":"W1975484586","doi":"10.1016/j.rgg.2012.12.001","title":"The Kotuikan ring structure as possible evidence for a large impact event in the northern Siberian craton","year":2013,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Tectonics; Impact structure; Mantle (geology); Plate tectonics; Earth science; Paleontology; Astrobiology; Impact crater","score_opus":0.007574265319366906,"score_gpt":0.26095925088053634,"score_spread":0.25338498556116945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975484586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883825,0.000067614026,0.000049499195,0.000016889777,0.0000026456817,0.0000028702666,0.000048901195,0.000002194563,0.00097126234],"genre_scores_gemma":[0.9997305,0.000036365465,0.000048749273,0.00000459679,0.0000028200072,0.0000014185067,0.000057543923,6.427991e-7,0.00011722245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991965,0.00001131303,0.000009915179,0.000017867214,0.000017434522,0.000023900722],"domain_scores_gemma":[0.999635,0.00005637029,0.00012135571,0.00004356266,0.00006424693,0.000079511614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026134527,0.00016691598,0.00018492575,0.001364232,0.0007152829,0.0004764691,0.00021121187,0.00030009175,0.0027093466],"category_scores_gemma":[0.0005481001,0.00014999809,0.00012991409,0.0010697009,0.00067148835,0.000261029,0.000812672,0.00019387271,0.0002358858],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019226006,0.00002606435,0.9734231,0.000039171537,0.000044897417,0.002222824,0.0010555497,0.00040063198,0.0137431435,0.00042332427,0.00012335215,0.008305734],"study_design_scores_gemma":[0.000002969446,0.000018977587,0.9987226,0.0000049429755,0.000010454315,0.00023783636,0.00033639764,0.00022268969,0.00023659211,0.000036546364,0.0001676923,0.000002154818],"about_ca_topic_score_codex":0.01705876,"about_ca_topic_score_gemma":0.025398461,"teacher_disagreement_score":0.01705876,"about_ca_system_score_codex":0.00041945072,"about_ca_system_score_gemma":0.00038037286,"threshold_uncertainty_score":0.033918917},"labels":[],"label_agreement":null},{"id":"W1976694523","doi":"10.1016/j.rgg.2012.07.003","title":"Physicochemical prerequisites for the formation of primary orebody zoning at copper-nickel sulfide deposits (<i>by the example of the systems</i>Fe–Ni–S<i>and</i>Cu–Fe–S)","year":2012,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Metal Extraction and Bioleaching","field":"Engineering","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":"","keywords":"Crystallization; Fractional crystallization (geology); Sulfide; Geology; Fractionation; Nickel; Phase diagram; Zoning; Phase (matter); Thermodynamics; Copper; Mineralogy; Partition coefficient; Geochemistry; Materials science; Metallurgy; Chemistry; Basalt; Law; Physics","score_opus":0.011280658289295167,"score_gpt":0.2058814828980446,"score_spread":0.19460082460874942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976694523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971324,0.00005309211,0.0017265761,0.0000090037565,0.0000012989846,0.000010730521,0.00020238051,0.000043097152,0.00082132197],"genre_scores_gemma":[0.9990308,0.000028602977,0.00060331676,0.0000015356989,4.6054313e-7,0.000007916535,0.00012404546,0.000007999515,0.0001953725],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999374,0.0000044364897,0.0000044411718,0.00002416087,0.000014131739,0.000015417148],"domain_scores_gemma":[0.99989176,0.00003760824,0.000025257792,0.000009925196,0.000020738724,0.000014648484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008749123,0.00010395448,0.00018060586,0.000308351,0.00027890576,0.0004507562,0.00017595149,0.00018342376,0.0016097274],"category_scores_gemma":[0.0003979429,0.00017121006,0.00017068503,0.00017745183,0.00032247033,0.00015617583,0.00015304885,0.000166188,0.0001565247],"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":[0.00017484283,0.000021433216,0.01196214,0.00009147425,0.000010213554,0.0002035075,0.00015525104,0.005940301,0.9771274,0.0017793849,0.0000904176,0.0024436058],"study_design_scores_gemma":[0.000022088008,0.0001575233,0.089484446,0.00000843116,0.000018546405,0.00020129849,0.00021676875,0.04704739,0.8597653,0.0014266266,0.0016318229,0.000019748684],"about_ca_topic_score_codex":0.005605941,"about_ca_topic_score_gemma":0.0043082014,"teacher_disagreement_score":0.005605941,"about_ca_system_score_codex":0.00051500346,"about_ca_system_score_gemma":0.00042294772,"threshold_uncertainty_score":0.011146605},"labels":[],"label_agreement":null},{"id":"W1980422934","doi":"10.1016/j.rgg.2007.02.007","title":"Isotopic composition (H, O, Cl, Sr) of ground brines of the Siberian Platform","year":2007,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geochemistry; Geology; Artesian aquifer; Brine; Structural basin; Context (archaeology); Groundwater; Stable isotope ratio; Isotope analysis; Aquifer; Mineralogy; Geomorphology; Chemistry; Oceanography; Paleontology; Geotechnical engineering","score_opus":0.011934875268347349,"score_gpt":0.19715252173548362,"score_spread":0.18521764646713626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980422934","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991505,0.00007656245,0.000067743225,0.0000040519144,0.000001121107,8.6455145e-7,0.0000994495,0.0000031164589,0.0005966202],"genre_scores_gemma":[0.9991817,0.00008881609,0.00007614547,0.00000417522,0.0000011335358,0.000001589054,0.00020968536,0.000002519867,0.00043412962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999436,0.000005554041,0.0000044851677,0.000015755362,0.000015921543,0.000014578834],"domain_scores_gemma":[0.9999399,0.000007342496,0.0000187872,0.000005623902,0.000020887022,0.000007457369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000088266046,0.0001986566,0.00021957872,0.001263614,0.0004262853,0.0004104643,0.0001188309,0.000101348596,0.0013558258],"category_scores_gemma":[0.00012690005,0.00016606491,0.00012418415,0.0007090853,0.0003333709,0.00017708927,0.00039078246,0.00008675937,0.00019457292],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004070038,0.000028214452,0.6943771,0.0001293398,0.00013672632,0.0008757533,0.0017580718,0.0008540665,0.28383937,0.00038231656,0.00010671903,0.017105358],"study_design_scores_gemma":[0.0000064298633,0.000042512565,0.99401677,0.0000098593255,0.00001807675,0.00012500478,0.00042615063,0.00023889056,0.004410123,0.0000725482,0.00062977016,0.0000039390716],"about_ca_topic_score_codex":0.021000788,"about_ca_topic_score_gemma":0.025945915,"teacher_disagreement_score":0.021000788,"about_ca_system_score_codex":0.0003052977,"about_ca_system_score_gemma":0.00027101013,"threshold_uncertainty_score":0.041757107},"labels":[],"label_agreement":null},{"id":"W1987620754","doi":"10.1016/j.rgg.2013.07.007","title":"Plate reconstructions in the Arctic region based on joint analysis of gravity, magnetic, and seismic anomalies","year":2013,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Magnetic anomaly; Clockwise; Subduction; Seismic tomography; Seismology; Arctic; Plate tectonics; Structural basin; Tectonics; Lineation; Paleontology; Mantle (geology); Geophysics; Fold (higher-order function); Oceanography","score_opus":0.014255445855511006,"score_gpt":0.18241008196142033,"score_spread":0.16815463610590933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987620754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98508483,0.00081338536,0.00640561,0.000059280046,0.000031172207,0.000008961906,0.0035785495,0.00034424107,0.0036740147],"genre_scores_gemma":[0.9874008,0.0003316498,0.005953692,0.000005831447,0.000013826493,0.000005982696,0.0054601487,0.000035981728,0.00079210027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.000015826932,0.0000055025607,0.00002569739,0.000017835371,0.0000138550895],"domain_scores_gemma":[0.9998324,0.000013713287,0.000042259242,0.00001941223,0.00006977371,0.000022371547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003115652,0.0004393916,0.00017922695,0.0029234542,0.00045826484,0.0006620646,0.00023891682,0.00026006094,0.0013794814],"category_scores_gemma":[0.00054136827,0.00021904259,0.00055941276,0.0017662006,0.00018642582,0.00015326017,0.00038093605,0.00021818276,0.00070939964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007137048,0.00010601347,0.6054712,0.00015642813,0.0010779406,0.0012612707,0.00062086445,0.22237846,0.04116646,0.0041388143,0.0031069403,0.11980185],"study_design_scores_gemma":[0.00002824342,0.000071687005,0.7699048,0.000075350996,0.0002367478,0.0003523726,0.0005763284,0.21642154,0.0035563244,0.0009216156,0.0078034373,0.000051593066],"about_ca_topic_score_codex":0.06209767,"about_ca_topic_score_gemma":0.0808627,"teacher_disagreement_score":0.06209767,"about_ca_system_score_codex":0.0004606768,"about_ca_system_score_gemma":0.000635181,"threshold_uncertainty_score":0.12347245},"labels":[],"label_agreement":null},{"id":"W1999188701","doi":"10.1016/j.rgg.2008.06.007","title":"Neoproterozoic rift and within-plate magmatism in the Yenisei Ridge: implications for the breakup of Rodinia","year":2008,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":60,"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":"Rodinia; Geology; Magmatism; Rift; Geochemistry; Supercontinent; Ultramafic rock; Mantle plume; Basalt; Igneous rock; Large igneous province; Petrology; Earth science; Paleontology; Craton; Lithosphere; Tectonics","score_opus":0.0150394787838835,"score_gpt":0.20794912938042343,"score_spread":0.19290965059653992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999188701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971788,0.00066194014,0.000057869118,0.00011768924,0.0000045821243,0.000007751572,0.00014093325,0.000011480776,0.0018190244],"genre_scores_gemma":[0.99915254,0.00017279155,0.000068622874,0.000015452779,0.000004917498,0.0000050905787,0.00012986381,0.000004549183,0.00044630744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989665,0.000007483984,0.00000906287,0.000033378084,0.0000086982545,0.00004471651],"domain_scores_gemma":[0.999859,0.000012689551,0.000049140366,0.000016989616,0.00003413346,0.00002813966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028836413,0.00032995702,0.0003031034,0.00095812784,0.0008271439,0.0009339756,0.00035958816,0.00050417037,0.0022341327],"category_scores_gemma":[0.00032581176,0.0002569709,0.00023416796,0.0009044631,0.00086971757,0.00062507583,0.00063404086,0.00030931438,0.00033862222],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048125998,0.00003978425,0.9123841,0.00015251341,0.00007192073,0.0016117371,0.002504441,0.00072220847,0.0576749,0.0015274915,0.00019170997,0.022637922],"study_design_scores_gemma":[0.00000922141,0.000024716168,0.99678016,0.00001767807,0.000010615621,0.00013119979,0.000679463,0.00015091214,0.0009543588,0.00007014279,0.0011668435,0.0000045532684],"about_ca_topic_score_codex":0.038126707,"about_ca_topic_score_gemma":0.04223828,"teacher_disagreement_score":0.038126707,"about_ca_system_score_codex":0.0017522608,"about_ca_system_score_gemma":0.00073933194,"threshold_uncertainty_score":0.0758096},"labels":[],"label_agreement":null},{"id":"W2022149390","doi":"10.1016/j.rgg.2011.07.007","title":"Comprehensive zonal subdivisions of Siberian Jurassic and their significance for Circum-Arctic correlations","year":2011,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic; Boreal; Geology; Paleontology; Subdivision; The arctic; Physical geography; Oceanography; Geography; Archaeology","score_opus":0.03637848192092604,"score_gpt":0.2049889747376668,"score_spread":0.16861049281674076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022149390","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882316,0.0006421692,0.0018274003,0.000039341605,0.000009964491,0.0000075221233,0.00074594445,0.000040707746,0.00845527],"genre_scores_gemma":[0.99813145,0.00018633396,0.00070716743,0.000004036368,0.000004010231,0.000004915608,0.0005068054,0.0000057225466,0.00044956172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998565,0.00003007374,0.00001938232,0.00004035183,0.000027815202,0.000025901065],"domain_scores_gemma":[0.99952304,0.00007714732,0.00010060498,0.00007963656,0.000163468,0.000056199733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045476892,0.00012135439,0.0001235368,0.002007691,0.00042359758,0.000606898,0.00010550097,0.000056454795,0.0021529468],"category_scores_gemma":[0.0010603801,0.000098521065,0.00016193211,0.0018695873,0.00031267962,0.00029146258,0.00051464967,0.00012949629,0.00016252288],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008300363,0.000007907495,0.94794583,0.000037960755,0.00011841109,0.000055921166,0.0007534107,0.0020297624,0.0036029282,0.0050699124,0.0004296839,0.039865196],"study_design_scores_gemma":[8.258514e-7,0.0000043208092,0.9974934,0.000006152698,0.000015719363,0.000016455475,0.00013572894,0.0005059077,0.00012450486,0.0005957378,0.0010991121,0.0000023053067],"about_ca_topic_score_codex":0.015766481,"about_ca_topic_score_gemma":0.03638515,"teacher_disagreement_score":0.015766481,"about_ca_system_score_codex":0.00036874448,"about_ca_system_score_gemma":0.00055083213,"threshold_uncertainty_score":0.03134942},"labels":[],"label_agreement":null},{"id":"W2022438019","doi":"10.1016/j.rgg.2006.11.002","title":"Detailed biostratigraphy of Triassic deposits in the Lena lower reaches (<i>northern Yakutia</i>)","year":2007,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Biostratigraphy; Geology; Paleontology; Fauna; Stratigraphy; Ecology","score_opus":0.013188591011300524,"score_gpt":0.2001154183845536,"score_spread":0.18692682737325308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022438019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983461,0.00016851642,0.000030922565,0.000008965187,8.7190114e-7,0.000003755653,0.0002105371,0.000007631146,0.0012227371],"genre_scores_gemma":[0.99870694,0.00011062205,0.000063472275,0.000003984177,9.699332e-7,0.00000406916,0.0004141797,0.0000038136936,0.00069197034],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999089,0.0000055689484,0.000008850843,0.00001958166,0.000020441592,0.000036697198],"domain_scores_gemma":[0.99992514,0.0000044278804,0.000020599835,0.000004331038,0.000027891703,0.000017577193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010930671,0.00018005529,0.00026800894,0.0020545695,0.0006873089,0.0007370682,0.00020105152,0.0001218558,0.0015225201],"category_scores_gemma":[0.00012773433,0.00021957955,0.00013655255,0.0017110491,0.0003876008,0.0002639035,0.00041975453,0.0001339567,0.00023289636],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001155643,0.000026802207,0.9690437,0.00007990474,0.00006485494,0.00042674097,0.0015624161,0.000657249,0.013615589,0.00023064097,0.00020327244,0.013973363],"study_design_scores_gemma":[0.0000015559344,0.000005548287,0.99903524,0.0000064277333,0.0000066105995,0.00006941046,0.00019850589,0.00008177614,0.00018252095,0.000009138388,0.00040186328,0.0000014955627],"about_ca_topic_score_codex":0.18315504,"about_ca_topic_score_gemma":0.33345112,"teacher_disagreement_score":0.18315504,"about_ca_system_score_codex":0.0013059089,"about_ca_system_score_gemma":0.0011474814,"threshold_uncertainty_score":0.36417794},"labels":[],"label_agreement":null},{"id":"W2026759829","doi":"10.1016/j.rgg.2013.07.019","title":"Conditions of the accumulation of organic matter and metals in the bottom sediments of the Chukchi Sea","year":2013,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":45,"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; Total organic carbon; Rift; Organic matter; Geochemistry; Cenozoic; Anoxic waters; Oceanography; Continental shelf; Structural basin; Paleontology; Environmental chemistry","score_opus":0.019073029778828715,"score_gpt":0.2257447724895057,"score_spread":0.20667174271067698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026759829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995783,0.00006023351,0.000015667198,0.0000044060944,0.0000010796509,0.0000013049593,0.00013032605,0.0000023040152,0.00020638312],"genre_scores_gemma":[0.9994561,0.00006309612,0.0000441915,0.0000054862135,0.000001289607,0.0000025214965,0.00024412117,0.0000014920038,0.0001816675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991286,0.0000059443405,0.000008390094,0.000018810679,0.00001960917,0.00003442557],"domain_scores_gemma":[0.9998073,0.000013764724,0.00005185635,0.000005413526,0.00007308511,0.000048617392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009021043,0.00035990987,0.00024220721,0.0017584522,0.00087570504,0.00070354756,0.00014813156,0.00020327186,0.0004996031],"category_scores_gemma":[0.0001480138,0.00026352258,0.00012566039,0.0012704349,0.00044718475,0.0002094493,0.0003617588,0.0001621973,0.00011464658],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002974661,0.000029516017,0.87984973,0.0001335818,0.00010406606,0.00063982006,0.000909082,0.00049159996,0.11332153,0.000064533684,0.0001196828,0.004039403],"study_design_scores_gemma":[0.0000021889769,0.000013403765,0.9981912,0.0000040605555,0.000012029285,0.000034118148,0.00033109635,0.000109390356,0.0011757358,0.000005905786,0.00011775931,0.0000031615195],"about_ca_topic_score_codex":0.1238556,"about_ca_topic_score_gemma":0.15173349,"teacher_disagreement_score":0.1238556,"about_ca_system_score_codex":0.00079969753,"about_ca_system_score_gemma":0.00080668525,"threshold_uncertainty_score":0.24626935},"labels":[],"label_agreement":null},{"id":"W2027003688","doi":"10.1016/j.rgg.2009.08.001","title":"Early Proterozoic diamond-bearing kimberlites of Karelia and their formation peculiarities","year":2009,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Kimberlite; Geology; Geochemistry; Diatreme; Phenocryst; Proterozoic; Breccia; Craton; Phlogopite; Archean; Olivine; Mantle (geology); Xenolith; Volcanic rock; Paleontology; Volcano; Tectonics","score_opus":0.005905039767181587,"score_gpt":0.16956854523705667,"score_spread":0.16366350546987507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027003688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99829453,0.0002589512,0.00003721545,0.000008502317,0.0000010801127,0.000004488365,0.00014016528,0.000003916906,0.0012510549],"genre_scores_gemma":[0.9994041,0.0000958079,0.000042470245,0.0000041845296,0.0000016343995,0.0000021822011,0.00012611607,0.0000017183266,0.00032185187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985373,0.0000069391076,0.000012737704,0.000037721107,0.00002307191,0.00006567726],"domain_scores_gemma":[0.9998511,0.000015037873,0.000050310817,0.000008639468,0.00003767754,0.00003726235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012068795,0.00022764291,0.00023440074,0.0032370123,0.000740155,0.0008706702,0.0002829711,0.0002329812,0.0026789198],"category_scores_gemma":[0.0003264171,0.0002785077,0.00014030741,0.00156757,0.0007141247,0.00037109666,0.0007313176,0.0001522698,0.0004442908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037734892,0.000055925324,0.9294389,0.00017193535,0.00009207961,0.0015217231,0.0023855986,0.00036191742,0.047079727,0.00054824963,0.00013246875,0.017834086],"study_design_scores_gemma":[0.0000034973127,0.000013736361,0.99828017,0.0000064847254,0.0000057106904,0.00039866264,0.00039634397,0.00005174451,0.00027722676,0.00002719688,0.00053541636,0.0000038066837],"about_ca_topic_score_codex":0.015421865,"about_ca_topic_score_gemma":0.036823116,"teacher_disagreement_score":0.015421865,"about_ca_system_score_codex":0.00066195603,"about_ca_system_score_gemma":0.0004134233,"threshold_uncertainty_score":0.030664206},"labels":[],"label_agreement":null},{"id":"W2031838306","doi":"10.1016/j.rgg.2012.08.007","title":"The behavior of noble-metal admixtures during fractional crystallization of As- and Co-containing Cu–Fe–Ni sulfide melts","year":2012,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"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":"Sulfide; Fractional crystallization (geology); Crystallization; Partition coefficient; Metal; Noble metal; Phase (matter); Mineralogy; Solid solution; Analytical Chemistry (journal); Mineral; Geology; Materials science; Chemistry; Mantle (geology); Geochemistry; Metallurgy","score_opus":0.007219826045283237,"score_gpt":0.21620327598749112,"score_spread":0.20898344994220788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031838306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984219,0.00016419485,0.00065430434,0.000008115908,0.0000026605462,0.000006623852,0.00013958925,0.000045932058,0.0005568175],"genre_scores_gemma":[0.9984061,0.00009085276,0.00073375704,0.0000041125622,0.0000020245725,0.000010834447,0.0001898208,0.000032561464,0.00052982906],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999793,0.000021093141,0.000019376137,0.000057200672,0.00006664897,0.0000426468],"domain_scores_gemma":[0.9998274,0.0000454075,0.000031906275,0.000019403802,0.00005504761,0.000020816826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021493773,0.00021219732,0.0003491434,0.00047366013,0.00033007376,0.00041947715,0.00023890041,0.00014166035,0.00078425405],"category_scores_gemma":[0.00055687653,0.00018974871,0.00019686022,0.00039216795,0.0003290363,0.00021294785,0.00025278688,0.00026179067,0.00016253899],"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":[0.00026485976,0.000011256587,0.002100383,0.000038698894,0.000013983194,0.000053073185,0.000103957944,0.00034457626,0.9948719,0.000094047515,0.000023787463,0.0020794682],"study_design_scores_gemma":[0.0000040934406,0.00007841985,0.0063201725,0.0000027049646,0.000008504656,0.000034282002,0.00005747927,0.0017606916,0.99121314,0.000015385323,0.0005008074,0.0000043597065],"about_ca_topic_score_codex":0.0036117875,"about_ca_topic_score_gemma":0.004527563,"teacher_disagreement_score":0.0036117875,"about_ca_system_score_codex":0.0004088713,"about_ca_system_score_gemma":0.00031588742,"threshold_uncertainty_score":0.007181525},"labels":[],"label_agreement":null},{"id":"W2039386996","doi":"10.1016/j.rgg.2007.05.004","title":"Debatable questions of Boreal Triassic stratigraphy: boundary between middle and upper series","year":2007,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Biostratigraphy; Paleontology; Boreal; Stratigraphy; Ladinian; Stage (stratigraphy); Series (stratigraphy); Boundary (topology); Structural basin; Tectonics","score_opus":0.01281088056706102,"score_gpt":0.22047267967392492,"score_spread":0.2076617991068639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039386996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43966833,0.28672612,0.0097221015,0.040488865,0.0036878174,0.00004096658,0.00068957603,0.00031824232,0.21865793],"genre_scores_gemma":[0.98321956,0.010566386,0.0011029586,0.001424186,0.001410912,0.00001536552,0.00014472843,0.000032158543,0.0020837486],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99935645,0.00023206032,0.000071536924,0.00013714023,0.00012132293,0.00008158826],"domain_scores_gemma":[0.9971566,0.0009015055,0.000520734,0.00026496162,0.00074064574,0.00041540104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031694903,0.00016330175,0.00029615752,0.0018382655,0.0010283029,0.0023721838,0.0008271391,0.00046897988,0.002537029],"category_scores_gemma":[0.00688547,0.000083972336,0.00010112646,0.0015360767,0.0044767195,0.0034783133,0.00086230907,0.0008263915,0.00034890432],"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":[0.0008831381,0.000068826,0.10449918,0.0013453488,0.00012441569,0.0005461014,0.01735179,0.0010497731,0.0061141253,0.5482586,0.020829525,0.29892915],"study_design_scores_gemma":[0.0000415697,0.0002670551,0.34710404,0.0026151843,0.000106310996,0.00096241024,0.032724123,0.0010762033,0.0019676504,0.28290176,0.33016267,0.00007104148],"about_ca_topic_score_codex":0.00468224,"about_ca_topic_score_gemma":0.006138255,"teacher_disagreement_score":0.00468224,"about_ca_system_score_codex":0.0011664451,"about_ca_system_score_gemma":0.0007339277,"threshold_uncertainty_score":0.016762078},"labels":[],"label_agreement":null},{"id":"W2044201246","doi":"10.1016/j.rgg.2012.08.001","title":"Structure of the upper mantle in the Circum-Arctic region from regional seismic tomography","year":2012,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":73,"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; Lithosphere; Seismic tomography; Subduction; Seismology; Mantle (geology); Mantle plume; Arctic; Rift; Precambrian; Crust; Geophysics; Paleontology; Tectonics; Oceanography","score_opus":0.007646569028716254,"score_gpt":0.18534779877216198,"score_spread":0.17770122974344574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044201246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8919959,0.0004667754,0.1019422,0.00017291804,0.00001746342,0.000026458325,0.0012004277,0.00042062288,0.0037573716],"genre_scores_gemma":[0.9869422,0.00028646953,0.011480123,0.000011556575,0.000008202987,0.0000143252255,0.00050535786,0.000027953489,0.00072382926],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99996877,0.0000065845848,0.0000018321492,0.000008899627,0.000008188164,0.000005708862],"domain_scores_gemma":[0.9999572,0.000007752751,0.0000114695,0.000005459343,0.000012198745,0.0000059983167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012315255,0.00045844642,0.0002222207,0.00048835773,0.0001934233,0.0009098813,0.0004310425,0.0003360121,0.00073785416],"category_scores_gemma":[0.00030066565,0.0002967301,0.00051761226,0.00053762936,0.00023471875,0.00029691207,0.00034193322,0.00024451333,0.00015971002],"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":[0.00005482792,0.000016576845,0.0147421565,0.000014654301,0.00005908275,0.000098175275,0.000037798756,0.9715217,0.0056011905,0.0009635837,0.00016678068,0.00672341],"study_design_scores_gemma":[0.000004340826,0.000007451231,0.0040493165,0.0000032862627,0.00001554683,0.000022670305,0.000011371972,0.99496645,0.00031239926,0.00039126477,0.00021089565,0.0000050025533],"about_ca_topic_score_codex":0.07390286,"about_ca_topic_score_gemma":0.035941266,"teacher_disagreement_score":0.07390286,"about_ca_system_score_codex":0.00053688476,"about_ca_system_score_gemma":0.00069106254,"threshold_uncertainty_score":0.14694536},"labels":[],"label_agreement":null},{"id":"W2060039518","doi":"10.1016/j.rgg.2009.03.006","title":"Tectonics and petroleum potential of the East Arctic province","year":2009,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Cretaceous; Rift; Paleontology; Oceanic basin; Arctic; Basement; Structural basin; Cenozoic; Paleozoic; Tectonics; Craton; Continental margin; Continental shelf; Plate tectonics; Earth science; Geomorphology; Oceanography","score_opus":0.005126702425440864,"score_gpt":0.16398046586506398,"score_spread":0.15885376343962312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060039518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99242604,0.00083589565,0.000078545316,0.00004351328,0.0000028086715,0.0000018153872,0.00043506827,0.0000020753996,0.0061743096],"genre_scores_gemma":[0.9982992,0.0005731839,0.000105746316,0.0000036800936,0.0000027659557,9.774592e-7,0.00033318106,8.7214374e-7,0.00068049744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992883,0.000010541995,0.0000047910225,0.000013279352,0.000020744892,0.000021861257],"domain_scores_gemma":[0.99983215,0.000017329563,0.00004045388,0.000007385454,0.00007413797,0.000028557779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018221018,0.00010252114,0.00007723547,0.0012724579,0.0004353238,0.0006126448,0.00007431787,0.000041438965,0.00083030737],"category_scores_gemma":[0.00019985353,0.00005325486,0.00008657615,0.001230026,0.00019087757,0.00015840662,0.00024558738,0.000105932435,0.00014384175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016319107,0.000020025072,0.9495017,0.000069805836,0.00006893319,0.00048742024,0.0010738856,0.002057595,0.004129303,0.0035261104,0.0004118321,0.038490217],"study_design_scores_gemma":[0.000004108188,0.000028950108,0.9897289,0.00003978332,0.000032245982,0.00021143773,0.0013618345,0.0010580308,0.00081427774,0.0003561695,0.006359228,0.0000049647015],"about_ca_topic_score_codex":0.16291736,"about_ca_topic_score_gemma":0.21455048,"teacher_disagreement_score":0.16291736,"about_ca_system_score_codex":0.00088891125,"about_ca_system_score_gemma":0.0011457409,"threshold_uncertainty_score":0.3239382},"labels":[],"label_agreement":null},{"id":"W2061937450","doi":"10.1016/j.rgg.2006.12.004","title":"Neoproterozoic evolution of Rodinia: constraints from new paleomagnetic data on the western margin of the Siberian craton","year":2007,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Laurentia; Rodinia; Craton; Supercontinent; Geology; Gondwana; Paleomagnetism; Paleontology; Apparent polar wander; Baltica; Precambrian; Paleozoic; Ordovician; Structural basin; Tectonics","score_opus":0.01416698428497549,"score_gpt":0.19805076250206569,"score_spread":0.1838837782170902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061937450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955077,0.0008906574,0.00019204617,0.000032133827,0.0000046956393,0.0000036078986,0.00037742185,0.0000114038285,0.0029802248],"genre_scores_gemma":[0.9985209,0.00037205665,0.00018035254,0.000007914041,0.0000063920957,0.0000023004786,0.00069061207,0.0000034370646,0.0002160904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987316,0.000014110524,0.00002339492,0.000032522104,0.000035814628,0.000021118907],"domain_scores_gemma":[0.99958736,0.00006086433,0.00010688504,0.000051650994,0.00013642659,0.000056824003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054928544,0.0003372353,0.00036290183,0.0036678747,0.0008190723,0.0013920075,0.00024467355,0.00018540368,0.0024008867],"category_scores_gemma":[0.00072411675,0.00016946456,0.00023387477,0.0036011934,0.0005805007,0.00046644924,0.00072573393,0.00024379983,0.00038809257],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024134474,0.00002400193,0.9544147,0.00011899559,0.000111063426,0.0005227252,0.0011452215,0.0016837785,0.014363489,0.0005257772,0.00010802306,0.026740817],"study_design_scores_gemma":[0.000002610965,0.000011644936,0.99768865,0.000015852358,0.000015757147,0.00008709101,0.0002069361,0.00040137657,0.0005028049,0.00007635352,0.000987406,0.0000035599926],"about_ca_topic_score_codex":0.03348743,"about_ca_topic_score_gemma":0.04662839,"teacher_disagreement_score":0.03348743,"about_ca_system_score_codex":0.0011241683,"about_ca_system_score_gemma":0.0006021351,"threshold_uncertainty_score":0.066585064},"labels":[],"label_agreement":null},{"id":"W2062552293","doi":"10.1016/j.rgg.2010.08.005","title":"Phanerozoic mafic magmatism in the southern Siberian craton: geodynamic implications","year":2010,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Wilfrid Laurier University; University of Ottawa","funders":"","keywords":"Geology; Craton; Magmatism; Mafic; Geochemistry; Mantle plume; Subduction; Dike; Crust; Flood basalt; Paleozoic; Continental crust; Earth science; Paleontology; Lithosphere; Tectonics; Volcanism","score_opus":0.004808931700074575,"score_gpt":0.186980834790992,"score_spread":0.18217190309091744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062552293","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934949,0.001345597,0.00009341407,0.00023990708,0.000010882343,0.0000048288725,0.00021606582,0.000014635806,0.0045796633],"genre_scores_gemma":[0.998982,0.00050245016,0.000043202588,0.00001742462,0.00000809709,0.0000014302672,0.00012513965,0.000002701022,0.00031744275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999503,0.0000053636572,0.000004878834,0.000013048494,0.0000086276705,0.000017830382],"domain_scores_gemma":[0.9998691,0.000010293983,0.000026352369,0.000008850996,0.000043229484,0.000042163247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026275264,0.0003164161,0.00021484001,0.0016845281,0.0011039265,0.0010755054,0.0003127884,0.00035763436,0.0037582943],"category_scores_gemma":[0.00039530452,0.00017064466,0.00019807274,0.0015137943,0.0006549915,0.00049701775,0.0006782351,0.00023222406,0.00032334524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013277879,0.00003447978,0.9459565,0.00015069214,0.00011250878,0.0010064872,0.001506425,0.0035284,0.015564652,0.0012855409,0.00039819375,0.03032332],"study_design_scores_gemma":[0.000002787633,0.000007617162,0.99798787,0.000012747468,0.000007722194,0.0000714988,0.00032244207,0.00062434457,0.00018796313,0.00013296233,0.00063906633,0.0000029564235],"about_ca_topic_score_codex":0.1280553,"about_ca_topic_score_gemma":0.12192869,"teacher_disagreement_score":0.1280553,"about_ca_system_score_codex":0.0019827196,"about_ca_system_score_gemma":0.0009853143,"threshold_uncertainty_score":0.2546199},"labels":[],"label_agreement":null},{"id":"W2067111765","doi":"10.1016/j.rgg.2007.10.009","title":"Melt inclusions in eclogite garnet: experimental study of natural processes","year":2008,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Eclogite; Geology; Inclusion (mineral); Crystallization; Geochemistry; Melt inclusions; Mineral; Recrystallization (geology); Mineralogy; Petrography; Terrane; Mantle (geology); Petrology; Materials science; Chemical engineering; Tectonics; Metallurgy; Subduction","score_opus":0.010885962836587004,"score_gpt":0.21069251091354996,"score_spread":0.19980654807696296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067111765","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900717,0.000067069835,0.00031999336,0.000006178807,0.0000016955104,0.000008710647,0.0001186418,0.000014473556,0.0004560672],"genre_scores_gemma":[0.9991565,0.000071828574,0.0003186232,0.0000038746184,0.000002936199,0.000012292335,0.00017608,0.000007945259,0.00025005257],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99987197,0.000011983475,0.0000059630947,0.000036237,0.00003907586,0.000034795048],"domain_scores_gemma":[0.99986446,0.000035494522,0.000025226267,0.00001963762,0.00004045168,0.000014699133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014054135,0.00022159063,0.00021850734,0.0002909448,0.0004858268,0.00022687111,0.00030229852,0.00024174488,0.0011647436],"category_scores_gemma":[0.00018563046,0.00014692415,0.00013381422,0.00027626983,0.0004374864,0.00028199187,0.00033320094,0.00025144077,0.00012575509],"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":[0.00026617898,0.00008584053,0.00537086,0.000055170636,0.000010213935,0.00012234421,0.000149887,0.00032930152,0.9923664,0.00012991086,0.000032892407,0.0010809827],"study_design_scores_gemma":[0.00003053845,0.00050817826,0.03528603,0.000005976159,0.000022258231,0.00016748307,0.00012301082,0.0032001275,0.95956385,0.00009032061,0.000992346,0.000009847995],"about_ca_topic_score_codex":0.0023186589,"about_ca_topic_score_gemma":0.002456732,"teacher_disagreement_score":0.0023186589,"about_ca_system_score_codex":0.00037292164,"about_ca_system_score_gemma":0.00011809295,"threshold_uncertainty_score":0.0046103597},"labels":[],"label_agreement":null},{"id":"W2068741591","doi":"10.1016/j.rgg.2015.03.007","title":"The room for the Vendian in the International Chronostratigraphic Chart","year":2015,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Paleontology; Series (stratigraphy); Proterozoic; Range (aeronautics); Precambrian; Tectonics","score_opus":0.021114988737752485,"score_gpt":0.23112761332282422,"score_spread":0.21001262458507175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068741591","genre_codex":"other","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":[0.1584416,0.028613998,0.04055507,0.014554298,0.009532274,0.0001750591,0.0049297046,0.0011107158,0.74208736],"genre_scores_gemma":[0.91462886,0.0098755555,0.04161036,0.000837646,0.0012211092,0.00017080393,0.006059035,0.0005781646,0.0250185],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9994079,0.00017353203,0.00009156617,0.00013002935,0.0000963814,0.00010058284],"domain_scores_gemma":[0.9984347,0.00022077317,0.00021535378,0.00029463455,0.000662869,0.00017173725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014401685,0.0004381191,0.00019377624,0.0032122992,0.0012270778,0.0037689053,0.0005233777,0.00025081154,0.0057097883],"category_scores_gemma":[0.003229565,0.000105211235,0.000160097,0.0062312144,0.0015418328,0.0023252734,0.0009199485,0.0011980793,0.000736144],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015854178,0.000016793942,0.03980906,0.00027953825,0.000029860934,0.00031205628,0.0046487073,0.0014109869,0.0013653255,0.6120392,0.061477333,0.27845263],"study_design_scores_gemma":[0.0000070078195,0.000026053081,0.039303977,0.0002324583,0.000016400943,0.00023069132,0.0017797718,0.0006477498,0.000526652,0.015257881,0.9419489,0.00002240352],"about_ca_topic_score_codex":0.017642463,"about_ca_topic_score_gemma":0.017545663,"teacher_disagreement_score":0.017642463,"about_ca_system_score_codex":0.0027603302,"about_ca_system_score_gemma":0.0016296741,"threshold_uncertainty_score":0.03507954},"labels":[],"label_agreement":null},{"id":"W2074678879","doi":"10.1016/j.rgg.2013.10.008","title":"Ultramafic–mafic igneous complexes of the Precambrian East Siberian metallogenic province (<i>southern framing of the Siberian craton</i>): age, composition, origin, and ore potential","year":2013,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Precambrian; Geochemistry; Mafic; Mantle plume; Ultramafic rock; Massif; Craton; Riphean; Flood basalt; Peridotite; Large igneous province; Gabbro; Magmatism; Igneous rock; Basalt; Paleontology; Tectonics; Lithosphere; Volcanism","score_opus":0.0047836312309982405,"score_gpt":0.16364794651145737,"score_spread":0.15886431528045913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074678879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988834,0.00014891438,0.00007630052,0.00000731273,9.643367e-7,0.0000016468249,0.00012038873,0.0000035965572,0.00075743115],"genre_scores_gemma":[0.99907887,0.00006269258,0.000073694704,0.0000032680111,0.0000012506218,0.0000014691541,0.00037794944,0.0000017641167,0.00039896107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994063,0.000006523428,0.0000068271315,0.000016609916,0.000012745678,0.000016654947],"domain_scores_gemma":[0.9998965,0.00000852377,0.000028531116,0.00001002598,0.000028138329,0.000028264169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015696725,0.00017484199,0.00012977344,0.0009821604,0.00050044915,0.00048025537,0.00015557476,0.00009418549,0.0017654055],"category_scores_gemma":[0.00016807787,0.00010865699,0.0001223672,0.0007164942,0.00022607863,0.00020164282,0.00036299558,0.00010548046,0.00029741327],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011330536,0.0000121205885,0.9511579,0.000041389227,0.000060993105,0.00033052242,0.0007510075,0.0002859307,0.034119092,0.0001529079,0.000100126366,0.01287467],"study_design_scores_gemma":[8.585015e-7,0.0000060763914,0.9986708,0.0000023475018,0.000004670515,0.00007114459,0.00009002821,0.00014418593,0.00065881596,0.000013593704,0.00033667398,8.9010234e-7],"about_ca_topic_score_codex":0.054588582,"about_ca_topic_score_gemma":0.081481904,"teacher_disagreement_score":0.054588582,"about_ca_system_score_codex":0.0005641341,"about_ca_system_score_gemma":0.0003890944,"threshold_uncertainty_score":0.10854167},"labels":[],"label_agreement":null},{"id":"W2079151737","doi":"10.1016/j.rgg.2009.11.019","title":"Manganoan ilmenite as kimberlite/diamond indicator mineral","year":2009,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada)","funders":"","keywords":"Ilmenite; Kimberlite; Geology; Geochemistry; Augite; Mineralogy; Mineral; Pyrope; Mantle (geology); Plagioclase; Metallurgy; Materials science","score_opus":0.004401418628419165,"score_gpt":0.18630444023129225,"score_spread":0.18190302160287308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079151737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99685776,0.00034774674,0.00032462282,0.000009456198,0.0000022318488,0.0000072031426,0.0001993676,0.000030284835,0.0022213697],"genre_scores_gemma":[0.99803025,0.00007583422,0.00084253214,0.00000446722,9.4247144e-7,0.0000030879087,0.00014042918,0.0000034246596,0.00089892076],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994636,0.00000474709,0.0000025862678,0.000020587546,0.000013869954,0.000011854757],"domain_scores_gemma":[0.9999472,0.000006081686,0.0000149511125,0.0000035556668,0.000017097698,0.000011173512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006484184,0.0001393428,0.00007288366,0.00085665454,0.00018501976,0.00021366475,0.00013607786,0.00011999348,0.0014890685],"category_scores_gemma":[0.000103567225,0.000070353824,0.000050328832,0.0002796449,0.00010035124,0.000090623515,0.00012496756,0.000057999332,0.00021177871],"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":[0.00014444526,0.000016844215,0.23685627,0.00009933581,0.00001967456,0.00034381208,0.00026361615,0.00007186889,0.74889076,0.00018510436,0.00011204973,0.012996287],"study_design_scores_gemma":[0.0000050527365,0.00008600295,0.8665303,0.000024100935,0.000023487515,0.0007398474,0.00040231232,0.0009891824,0.12483311,0.00007062949,0.0062896474,0.000006270189],"about_ca_topic_score_codex":0.005751694,"about_ca_topic_score_gemma":0.019595081,"teacher_disagreement_score":0.005751694,"about_ca_system_score_codex":0.00023548357,"about_ca_system_score_gemma":0.00009946751,"threshold_uncertainty_score":0.011436462},"labels":[],"label_agreement":null},{"id":"W2396034471","doi":"10.1016/j.rgg.2016.04.004","title":"The Mesoproterozoic mantle plume beneath the northern part of the Siberian craton","year":2016,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; Frontier Geosciences (Canada)","funders":"","keywords":"Craton; Geology; Geochemistry; Mantle plume; Mantle (geology); Supercontinent; Mafic; Rodinia; Lithosphere; Paleontology; Tectonics","score_opus":0.004990776751722798,"score_gpt":0.16070202060461064,"score_spread":0.15571124385288784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2396034471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974113,0.00028659072,0.00009193358,0.000033402077,0.000002700656,0.0000027054302,0.00017169019,0.000013003651,0.0019867618],"genre_scores_gemma":[0.9990539,0.00011302013,0.00010319709,0.000007933064,0.0000021035248,0.000001295472,0.0001682523,0.000002566001,0.0005476898],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999715,0.0000017083158,0.0000020909874,0.000007461368,0.0000087815515,0.00000829693],"domain_scores_gemma":[0.9999598,0.0000035100193,0.000007816835,0.0000032723592,0.000015368374,0.00001013357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008349349,0.00019374743,0.00021715339,0.0009146921,0.0005595149,0.0004556541,0.00014320086,0.00017929771,0.001978706],"category_scores_gemma":[0.00009470271,0.00015985263,0.00012504183,0.00064631447,0.00019657024,0.00017864617,0.0003511037,0.00013321103,0.0002242953],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023743825,0.000032058262,0.69010043,0.00019292883,0.000089467925,0.0016548315,0.0016522785,0.001653236,0.27053362,0.0008591431,0.0002424012,0.032752234],"study_design_scores_gemma":[0.000004961005,0.000016843795,0.99454594,0.000016318156,0.000013078711,0.00023077353,0.00034040897,0.0007774184,0.0027971026,0.00006219845,0.0011913022,0.0000036907516],"about_ca_topic_score_codex":0.047954958,"about_ca_topic_score_gemma":0.055316646,"teacher_disagreement_score":0.047954958,"about_ca_system_score_codex":0.0006978761,"about_ca_system_score_gemma":0.0005125705,"threshold_uncertainty_score":0.09535164},"labels":[],"label_agreement":null},{"id":"W2398112667","doi":"10.1016/j.rgg.2016.04.003","title":"Tectonic activity of the early Earth (4.56–3.4(2.7?) Ga)","year":2016,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Hadean; Archean; Geology; Early Earth; Mantle (geology); Crust; Geochemistry; Earth's internal heat budget; Mantle convection; Basalt; Zircon; Plate tectonics; Meteorite; Crustal recycling; Earth science; Continental crust; Tectonics; Lithosphere; Astrobiology; Paleontology","score_opus":0.006075007186055914,"score_gpt":0.17053241605542935,"score_spread":0.16445740886937343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2398112667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.936481,0.005076682,0.0027376008,0.0005968127,0.00013428189,0.000056166424,0.0037713065,0.0003079106,0.050838303],"genre_scores_gemma":[0.98799556,0.00094177725,0.0014247153,0.00008976192,0.00005136104,0.000009595098,0.0024727709,0.000048656464,0.006965747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999106,0.000011398503,0.000005460796,0.000030122328,0.000012609006,0.00002974137],"domain_scores_gemma":[0.99993885,0.0000038395997,0.000018711884,0.0000088175075,0.000018810091,0.000010942319],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018025938,0.00044923363,0.00024561572,0.0018283537,0.0006768426,0.00068234064,0.00028217284,0.0004534618,0.006131853],"category_scores_gemma":[0.00016544694,0.00017038161,0.00031803167,0.0016401082,0.0004914414,0.00038298513,0.0006058424,0.00034506235,0.0013638404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016703901,0.00021671195,0.47729868,0.001482119,0.00084187574,0.0055548064,0.0033202528,0.021323275,0.22759062,0.032335322,0.00830642,0.22005953],"study_design_scores_gemma":[0.00004130689,0.0001434672,0.9281687,0.00008314298,0.00012639943,0.0011018622,0.00047066231,0.0023527453,0.0054553235,0.0012735843,0.060751744,0.000031026928],"about_ca_topic_score_codex":0.029054893,"about_ca_topic_score_gemma":0.025812745,"teacher_disagreement_score":0.029054893,"about_ca_system_score_codex":0.0014668899,"about_ca_system_score_gemma":0.00029802523,"threshold_uncertainty_score":0.057771504},"labels":[],"label_agreement":null},{"id":"W2400529896","doi":"10.1016/j.rgg.2015.09.020","title":"Relationship between platinum-bearing ultramafic–mafic intrusions and large igneous provinces (<i>exemplified by the Siberian Craton</i>)","year":2016,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; Carleton University","funders":"","keywords":"Massif; Geology; Mafic; Ultramafic rock; Geochemistry; Proterozoic; Craton; Igneous rock; Geochronology; Paleontology","score_opus":0.010046136061599957,"score_gpt":0.19714311136049648,"score_spread":0.18709697529889652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2400529896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99848807,0.00024916566,0.000048735514,0.00001127133,0.0000016039119,0.000001107799,0.00017261688,0.0000036543722,0.0010238243],"genre_scores_gemma":[0.9994691,0.000086625274,0.00004530707,0.00000370509,0.000001490031,8.040644e-7,0.00023006853,0.000001154949,0.00016167595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999273,0.000006830166,0.000011755987,0.000024135225,0.000012770681,0.000017153752],"domain_scores_gemma":[0.99979705,0.000024165312,0.00007981344,0.000020027464,0.0000431266,0.000035785648],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015944269,0.00014449446,0.00014764954,0.0013864633,0.00032847587,0.00047874404,0.00014305074,0.00010606698,0.002314199],"category_scores_gemma":[0.00032270065,0.00008703415,0.00014048225,0.0013778001,0.00025571906,0.00022941417,0.00038613868,0.00011814678,0.00019159657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053206768,0.0000055762257,0.9893539,0.000018466566,0.000041770993,0.00011320734,0.00021612973,0.00009157551,0.0031891519,0.000097456155,0.00006346638,0.0067560812],"study_design_scores_gemma":[4.047934e-7,0.0000034365428,0.99942386,0.000002852376,0.0000041173716,0.00004686671,0.00007789519,0.00006017403,0.00015919725,0.0000153457,0.00020511007,6.8751507e-7],"about_ca_topic_score_codex":0.034632962,"about_ca_topic_score_gemma":0.057245575,"teacher_disagreement_score":0.034632962,"about_ca_system_score_codex":0.00050728227,"about_ca_system_score_gemma":0.00039844488,"threshold_uncertainty_score":0.068862736},"labels":[],"label_agreement":null},{"id":"W2406466134","doi":"10.1016/j.rgg.2016.01.015","title":"The 1501 Ma Kuonamka Large Igneous Province of northern Siberia: U–Pb geochronology, geochemistry, and links with coeval magmatism on other crustal blocks","year":2016,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Carleton University","funders":"","keywords":"Geology; Sill; Craton; Dike; Geochronology; Geochemistry; Magmatism; Igneous rock; Large igneous province; Crust; Basalt; Zircon; Mantle (geology); Paleontology; Tectonics","score_opus":0.0032076447145038354,"score_gpt":0.16937665269883634,"score_spread":0.1661690079843325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2406466134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973122,0.0003193161,0.000076074146,0.000032498225,0.0000040508176,0.0000037874076,0.0002560282,0.0000110814235,0.001985112],"genre_scores_gemma":[0.99917245,0.00008495115,0.00006725465,0.0000088992165,0.0000029935586,0.000002720804,0.00036579865,0.0000028320637,0.00029211637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999244,0.000005808346,0.000008016014,0.000025366573,0.0000149483485,0.000021487574],"domain_scores_gemma":[0.9998772,0.000007892328,0.000027464146,0.000013624189,0.000042581385,0.000031271375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002584656,0.00028960727,0.00031164038,0.0016045482,0.0007335495,0.0005623185,0.00022019995,0.00019847901,0.0020539723],"category_scores_gemma":[0.00022240725,0.00015984286,0.00021131964,0.0013132097,0.00043952628,0.0003371077,0.0009693948,0.00017731129,0.00037902073],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017232771,0.00003486459,0.958756,0.000076492935,0.00011943783,0.00056745333,0.0010252211,0.00062285893,0.01728105,0.00023308,0.00029159716,0.02081961],"study_design_scores_gemma":[0.000002347164,0.0000069172493,0.9990109,0.0000057309107,0.000007121828,0.00004402236,0.00015910371,0.00020995183,0.00018193103,0.00001729323,0.00035301378,0.0000016285267],"about_ca_topic_score_codex":0.0678332,"about_ca_topic_score_gemma":0.06652164,"teacher_disagreement_score":0.0678332,"about_ca_system_score_codex":0.0010459682,"about_ca_system_score_gemma":0.0005781061,"threshold_uncertainty_score":0.13487673},"labels":[],"label_agreement":null},{"id":"W2478530891","doi":"10.1016/j.rgg.2016.06.006","title":"Characteristics of gas accumulation in a less efficient tight-gas reservoir, He 8 interval, Sulige gas field, Ordos Basin, China","year":2016,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Natural gas field; Tight gas; Geology; Wet gas; Sichuan basin; Petroleum engineering; Saturation (graph theory); Petrology; Natural gas; Geochemistry; Chemistry; Hydraulic fracturing","score_opus":0.012120577791753491,"score_gpt":0.23479032930643579,"score_spread":0.2226697515146823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2478530891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967957,0.000015991925,0.000030686508,0.0000031067227,3.9098828e-7,0.0000015122371,0.00009379214,0.0000043187692,0.00017067572],"genre_scores_gemma":[0.99960023,0.000013385231,0.000047569945,0.0000019230254,9.171681e-7,0.000002031015,0.00014076065,0.0000013831151,0.00019181459],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991083,0.0000048479055,0.000008299133,0.00003109275,0.000022358607,0.000022513259],"domain_scores_gemma":[0.9998497,0.000018249013,0.000045282413,0.000008198002,0.000048697366,0.000029807363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012964195,0.00020445016,0.000242307,0.0018838223,0.0005135931,0.00048878737,0.00031253864,0.00023943104,0.0006344528],"category_scores_gemma":[0.00018204017,0.00016967668,0.0001613103,0.0015757798,0.0004735466,0.00035518222,0.00032031842,0.00010839487,0.000072127805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022275004,0.000040837775,0.96295047,0.00004509634,0.00003316487,0.00081641605,0.00086057134,0.0011655455,0.027672857,0.00013051188,0.000101069076,0.005960657],"study_design_scores_gemma":[0.0000039942965,0.000028027333,0.9967134,0.0000023737236,0.000007855286,0.00007909971,0.00047147536,0.0012978557,0.0011861824,0.000025877527,0.00017717655,0.000006669594],"about_ca_topic_score_codex":0.051855348,"about_ca_topic_score_gemma":0.076697834,"teacher_disagreement_score":0.051855348,"about_ca_system_score_codex":0.0006649795,"about_ca_system_score_gemma":0.0005165312,"threshold_uncertainty_score":0.103107035},"labels":[],"label_agreement":null},{"id":"W2560128787","doi":"10.1016/j.rgg.2016.04.007","title":"Basaltic magmatism and strike-slip tectonics in the Arctic margin of Eurasia: evidence for the early stage of geodynamic evolution of the Amerasia Basin","year":2016,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Magmatism; Geodynamics; Tectonics; Continental margin; Structural basin; Paleontology; Plate tectonics; Arctic; Canada Basin; Earth science; Oceanography","score_opus":0.018915581267662906,"score_gpt":0.22245743914009286,"score_spread":0.20354185787242995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560128787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992235,0.0001304679,0.00004362611,0.000012470515,0.000001017134,8.145745e-7,0.000057035322,0.0000012477814,0.000529819],"genre_scores_gemma":[0.9994863,0.00012137644,0.00009824771,0.000004713363,0.0000015884231,0.0000010756688,0.000125597,0.000001179968,0.00015992014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999397,0.000008674425,0.0000075632834,0.000021838614,0.000011760427,0.000010485969],"domain_scores_gemma":[0.9997472,0.000033715747,0.0000799023,0.000016397491,0.000080700505,0.000042090738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022521462,0.000108837536,0.000099390425,0.0007719458,0.0002576954,0.00044999784,0.00015560012,0.00009090974,0.0008153547],"category_scores_gemma":[0.00036267203,0.00010175512,0.0001224112,0.00071605906,0.00033460697,0.00030674774,0.00033239694,0.00009660712,0.00007047523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000928232,0.000012725421,0.977505,0.00002526561,0.00003754977,0.00019523759,0.0012828667,0.00020840255,0.011484462,0.0001985627,0.000052863143,0.008904265],"study_design_scores_gemma":[0.0000014862167,0.000006762459,0.99905866,0.0000047824,0.000006689637,0.00005447926,0.00038349192,0.00012168754,0.00016051685,0.000036556954,0.00016378613,0.0000012041536],"about_ca_topic_score_codex":0.03918963,"about_ca_topic_score_gemma":0.048090525,"teacher_disagreement_score":0.03918963,"about_ca_system_score_codex":0.00030035252,"about_ca_system_score_gemma":0.0005456663,"threshold_uncertainty_score":0.07792306},"labels":[],"label_agreement":null},{"id":"W2785561692","doi":"10.1016/j.rgg.2018.01.004","title":"Reconstruction of brackish-water systems using an ichnological framework","year":2018,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","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":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Estuary; Ichnology; Brackish water; Bay; Trace fossil; Geology; Sedimentary rock; Oceanography; Structural basin; Cretaceous; Paleontology; Salinity","score_opus":0.01995193134533465,"score_gpt":0.2295938057497547,"score_spread":0.20964187440442003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2785561692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89904445,0.00095046195,0.06324434,0.0005806485,0.000041902767,0.000071676215,0.0015875947,0.00037943808,0.034099497],"genre_scores_gemma":[0.99163985,0.0003130059,0.0065645254,0.000011625189,0.000008494745,0.000012371127,0.00032794202,0.000038102986,0.001083992],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999349,0.000019823752,0.000004577543,0.000016688067,0.000013302856,0.000010648376],"domain_scores_gemma":[0.9999479,0.000006800908,0.000010141106,0.000008204111,0.000016656959,0.000010232952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010293433,0.00023459746,0.00017083157,0.0012859729,0.0005694814,0.0011275794,0.00040032435,0.00030645364,0.0026360145],"category_scores_gemma":[0.0005097091,0.00020341997,0.00031428033,0.0012884623,0.0006307416,0.0004929251,0.0009725041,0.0002874701,0.00036736834],"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":[0.00025418054,0.000084893625,0.22205871,0.00022335103,0.00024216484,0.0017942808,0.0016588275,0.5634851,0.024928816,0.08901956,0.0021433707,0.09410682],"study_design_scores_gemma":[0.000039077382,0.00007790002,0.23343995,0.00009683965,0.000069821996,0.00032004376,0.0022762532,0.71581006,0.0015578087,0.029616492,0.016626125,0.00006962359],"about_ca_topic_score_codex":0.039413914,"about_ca_topic_score_gemma":0.047189806,"teacher_disagreement_score":0.039413914,"about_ca_system_score_codex":0.00083939836,"about_ca_system_score_gemma":0.0008319471,"threshold_uncertainty_score":0.07836902},"labels":[],"label_agreement":null},{"id":"W2788325195","doi":"10.1016/j.rgg.2018.01.001","title":"Comparisons among the Oortsog, Dulaan, and Nomgon mafic–ultramafic intrusions in central Mongolia and Ni–Cu deposits in NW China: implications for economic Ni–Cu–PGE ore exploration in central Mongolia","year":2018,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Ultramafic rock; Mafic; Olivine; Layered intrusion; Mantle (geology); Basalt; Sulfide; Petrology; Chemistry","score_opus":0.010818031520440946,"score_gpt":0.21097061893572386,"score_spread":0.2001525874152829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788325195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997578,0.0000708937,0.000012879934,0.00000455856,2.7832624e-7,0.0000011845532,0.000033560704,0.0000011074584,0.00011774936],"genre_scores_gemma":[0.9997042,0.000039424798,0.000052092077,0.0000039558518,6.216046e-7,0.0000017991771,0.00009692088,9.170133e-7,0.00010016412],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998754,0.0000109463945,0.000016184806,0.000037759608,0.000022331604,0.00003734715],"domain_scores_gemma":[0.9997707,0.00002605504,0.00008370038,0.000014913217,0.000052843716,0.0000518456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025497918,0.0001834542,0.00025500497,0.0012296577,0.00046275352,0.0005409899,0.00028411136,0.0002749177,0.00047865554],"category_scores_gemma":[0.00021921954,0.00020385724,0.00018671401,0.0011140507,0.00036421418,0.00031489276,0.0004185215,0.000114618386,0.000054138458],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000080712234,0.000014323855,0.977428,0.00005476299,0.000080055266,0.00015901815,0.0026006766,0.00012602692,0.0130665945,0.00007695793,0.000040524443,0.006272223],"study_design_scores_gemma":[0.0000014718618,0.00000739476,0.99894994,0.0000037016152,0.000009262961,0.000036562913,0.000551768,0.00008425223,0.000199945,0.0000050549024,0.0001493111,0.0000013725279],"about_ca_topic_score_codex":0.050727163,"about_ca_topic_score_gemma":0.1058302,"teacher_disagreement_score":0.050727163,"about_ca_system_score_codex":0.0008042943,"about_ca_system_score_gemma":0.000495446,"threshold_uncertainty_score":0.100863814},"labels":[],"label_agreement":null},{"id":"W2802283442","doi":"10.1016/j.rgg.2018.04.004","title":"Geochemical characteristics and analysis of crude-oil source in the deep-water area of the Baiyun Sag, South China Sea","year":2018,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","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":"","keywords":"Source rock; Maturity (psychological); Geology; Geochemistry; Sedimentary depositional environment; Organic matter; Crude oil; Facies; Petroleum engineering; Paleontology; Chemistry","score_opus":0.004768181374221061,"score_gpt":0.18545222214184284,"score_spread":0.1806840407676218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802283442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997266,0.000047996866,0.000037605685,0.0000025788283,5.955014e-7,9.91881e-7,0.000058788486,0.0000011094418,0.00012373734],"genre_scores_gemma":[0.9996207,0.000041402796,0.00007448624,0.0000032908968,0.0000010117509,0.0000014709578,0.00013470979,0.0000012032601,0.000121681005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999323,0.0000050551175,0.000008251926,0.000019851415,0.0000204877,0.000014024407],"domain_scores_gemma":[0.99989724,0.000010880783,0.000033876426,0.0000045604907,0.00002865928,0.000024874931],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116519666,0.00026292203,0.00020447317,0.0010790958,0.0003754207,0.00027202957,0.00012536703,0.00017948775,0.00040014638],"category_scores_gemma":[0.000121363075,0.00013319222,0.00015997583,0.0012871454,0.00028683795,0.00029446487,0.00036314738,0.00011058355,0.00006295863],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084681364,0.000018128132,0.94264346,0.00005147752,0.00004512473,0.00032704166,0.00049100217,0.0002337708,0.05059897,0.000052326486,0.000030697356,0.0054233507],"study_design_scores_gemma":[0.0000016152027,0.000013830412,0.9982735,0.000002121274,0.000007321442,0.00004356768,0.0002196169,0.00023023158,0.0010762855,0.000011492975,0.00011860081,0.0000018368726],"about_ca_topic_score_codex":0.02531856,"about_ca_topic_score_gemma":0.040872894,"teacher_disagreement_score":0.02531856,"about_ca_system_score_codex":0.00040589966,"about_ca_system_score_gemma":0.00038971272,"threshold_uncertainty_score":0.05034238},"labels":[],"label_agreement":null},{"id":"W3138059994","doi":"10.15372/rgg2020161","title":"Chlorine in the Earth’s Mantle as an Indicator of the Global Recycling of Oceanic Crust","year":2020,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Greenstone belt; Geochemistry; Archean; Olivine; Lithosphere; Primitive mantle; Mantle plume; Oceanic crust; Transition zone; Seafloor spreading; Crust; Subduction; Early Earth; Partial melting; Geophysics; Tectonics; Paleontology","score_opus":0.011007660888233219,"score_gpt":0.2039333707071058,"score_spread":0.19292570981887258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138059994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905473,0.00032582603,0.00009047526,0.0000103168595,8.790002e-7,0.0000011655428,0.00017034242,0.000004595721,0.0003417123],"genre_scores_gemma":[0.99954706,0.00004899291,0.0000903502,0.000004796443,9.221957e-7,0.0000011560342,0.00012419364,0.0000020686828,0.0001804377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992275,0.0000068503314,0.0000040892246,0.000028892095,0.000016514552,0.000020912994],"domain_scores_gemma":[0.9998572,0.000014438523,0.000043180684,0.000010675315,0.000053687283,0.000020937085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014842945,0.00021557377,0.00016243271,0.0019483652,0.00032048277,0.00049400935,0.0002518926,0.00033969292,0.0006579831],"category_scores_gemma":[0.0002208867,0.00012986033,0.00014676635,0.00091341144,0.00034332814,0.0003056501,0.00040397764,0.00020565788,0.00010167015],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036449812,0.000014403846,0.70123047,0.000064154025,0.000093404466,0.00021019654,0.00043902194,0.00031862632,0.29214075,0.0001411322,0.000048902908,0.004934473],"study_design_scores_gemma":[0.000004909153,0.00004204938,0.98267865,0.000007218541,0.000024919898,0.00011138668,0.00021038973,0.00035867153,0.015970409,0.000039397077,0.0005475763,0.0000043784594],"about_ca_topic_score_codex":0.024863372,"about_ca_topic_score_gemma":0.024198571,"teacher_disagreement_score":0.024863372,"about_ca_system_score_codex":0.00063140347,"about_ca_system_score_gemma":0.00020940436,"threshold_uncertainty_score":0.049437284},"labels":[],"label_agreement":null},{"id":"W3139185554","doi":"10.15372/rgg2020127","title":"The Anyue Giant Gas Field in the Sichuan Basin as the Largest Gas Field in Marine Carbonate Deposits from Domestic China","year":2020,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Petro-Canada","funders":"","keywords":"Sichuan basin; Natural gas field; Geology; Natural gas; Carbonate; Lithology; Drilling; Geochemistry; Wet gas; Petroleum engineering; Chemistry","score_opus":0.004346608198860135,"score_gpt":0.19756256810404307,"score_spread":0.19321595990518295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3139185554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986571,0.00016623446,0.00008254409,0.000025541694,0.0000026945663,0.0000075217513,0.00010037029,0.000006836417,0.00095113326],"genre_scores_gemma":[0.999183,0.00007706344,0.000113629394,0.000008953811,0.000003103294,0.0000047237204,0.00019772502,0.0000011859106,0.00041052178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998747,0.000008369531,0.000009422501,0.000026692105,0.00004035676,0.000040386407],"domain_scores_gemma":[0.9998957,0.000012419341,0.000021326961,0.000009290034,0.00003183216,0.000029392695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022393033,0.00027011143,0.0002478673,0.00234274,0.001061354,0.0005161104,0.00035299596,0.00019671067,0.0007607],"category_scores_gemma":[0.00020914836,0.00015849485,0.00019498634,0.003064295,0.0005162536,0.0002524001,0.00059140864,0.00011997678,0.00004917315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112167414,0.00004763261,0.9529918,0.0001818531,0.00009127202,0.0032848546,0.002810166,0.0011734855,0.0089504365,0.0012358348,0.0005461676,0.028574396],"study_design_scores_gemma":[0.000008506744,0.000025978703,0.9936487,0.000018919387,0.000023740367,0.00041757393,0.00160873,0.0009649071,0.0007341424,0.000114104376,0.0024259612,0.000008754615],"about_ca_topic_score_codex":0.07658942,"about_ca_topic_score_gemma":0.13864544,"teacher_disagreement_score":0.07658942,"about_ca_system_score_codex":0.0008810078,"about_ca_system_score_gemma":0.0015522047,"threshold_uncertainty_score":0.15228719},"labels":[],"label_agreement":null},{"id":"W3139231599","doi":"10.15372/rgg2020122","title":"Discovery of Intracratonic Rift in the Upper Yangtze and Its Control Effect on the Formation of the Anyue Giant Gas Field","year":2020,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Petro-Canada","funders":"","keywords":"Geology; Rift; Facies; Paleontology; Stage (stratigraphy); Structural basin; Source rock; Craton; Fault block; Geochemistry; Tectonics","score_opus":0.004625590170649517,"score_gpt":0.184429784545686,"score_spread":0.1798041943750365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3139231599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99908197,0.0001901688,0.00010041521,0.00002368207,0.0000022644415,0.0000039321267,0.000058089154,0.000007186333,0.0005322367],"genre_scores_gemma":[0.99956435,0.00006323778,0.0000683929,0.0000069517223,0.000003629565,0.0000034026802,0.00009913183,0.0000014194549,0.00018945742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989223,0.000011217108,0.000006833575,0.000039505463,0.000021609463,0.000028604141],"domain_scores_gemma":[0.99985194,0.00001840608,0.000043447715,0.000009247561,0.00003697938,0.000039922903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020581951,0.00030787865,0.00025305888,0.0015712844,0.00048133187,0.0003836493,0.00024168908,0.00019239455,0.0009362958],"category_scores_gemma":[0.00021196417,0.0001391979,0.00017191986,0.001378805,0.0005245756,0.0002526924,0.0004246686,0.00019194507,0.0000676061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013192392,0.000028211794,0.9374688,0.0001222102,0.000095430165,0.0015641571,0.0013669452,0.0004681272,0.039285064,0.0005638994,0.00018961368,0.018715497],"study_design_scores_gemma":[0.000006490458,0.000022529524,0.9978734,0.000004498751,0.000017499937,0.00014909133,0.00041586717,0.00028742928,0.0005523857,0.00006736962,0.0005983606,0.000005097666],"about_ca_topic_score_codex":0.010648184,"about_ca_topic_score_gemma":0.017890573,"teacher_disagreement_score":0.010648184,"about_ca_system_score_codex":0.0003885749,"about_ca_system_score_gemma":0.0005135973,"threshold_uncertainty_score":0.021172404},"labels":[],"label_agreement":null},{"id":"W3153086097","doi":"10.2113/rgg20194091","title":"Ultramagnesian Olivine in the Monchepluton (Fo96) and Pados-Tundra (Fo93) Layered Intrusions (Kola Peninsula)","year":2021,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Olivine; Chromite; Geology; Geochemistry; Plagioclase; Layered intrusion; Augite; Kimberlite; Mineralogy; Mantle (geology); Mafic","score_opus":0.006451202361640338,"score_gpt":0.18391220246433487,"score_spread":0.17746100010269453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3153086097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994696,0.000060267696,0.000016818181,0.0000023722719,5.9784884e-7,6.745697e-7,0.00010441576,0.000002897391,0.0003422657],"genre_scores_gemma":[0.999681,0.000023062272,0.00002687586,0.0000017090513,4.9914604e-7,7.8915286e-7,0.00012193137,0.0000015492795,0.00014260715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.0000040210894,0.0000048514985,0.000024250088,0.000012172797,0.0000134372685],"domain_scores_gemma":[0.999926,0.000006824831,0.000028571954,0.000005820682,0.000014032922,0.00001869475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000076352895,0.00019261609,0.00011406506,0.00097639824,0.0003150378,0.00038324448,0.000159329,0.0001676278,0.0008620753],"category_scores_gemma":[0.000114334245,0.00013890951,0.000105241335,0.00044393563,0.0002457879,0.0001678727,0.00031053738,0.00011915531,0.00019429225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054138736,0.000030936753,0.7762339,0.00006889857,0.0001175296,0.0005138591,0.00074111245,0.00031259077,0.21268742,0.00009074209,0.00007170545,0.008589848],"study_design_scores_gemma":[0.000001815362,0.000011376459,0.99831945,0.0000019390832,0.0000047127696,0.000080949045,0.0000663422,0.00006254894,0.0012817989,0.0000039862225,0.0001641943,9.620402e-7],"about_ca_topic_score_codex":0.013232245,"about_ca_topic_score_gemma":0.020683166,"teacher_disagreement_score":0.013232245,"about_ca_system_score_codex":0.00043651555,"about_ca_system_score_gemma":0.00013893971,"threshold_uncertainty_score":0.026310444},"labels":[],"label_agreement":null},{"id":"W4220753308","doi":"10.2113/rgg20204282","title":"Stages of Paleoarchean to Paleoproterozoic Basic–ultrabasic Magmatism in the Sarmatian Craton","year":2022,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magmatism; Ultramafic rock; Geology; Geochemistry; Craton; Basalt; Igneous rock; Mantle (geology); Petrology; Tectonics; Paleontology","score_opus":0.008538019828027734,"score_gpt":0.1972061967940194,"score_spread":0.18866817696599167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220753308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99821836,0.0002745934,0.000039797433,0.000014155732,0.0000015499043,0.000004667437,0.000104584535,0.0000047135513,0.00133767],"genre_scores_gemma":[0.9992987,0.00011960778,0.000057155925,0.000003894067,0.0000018211538,0.0000018299404,0.0001265297,0.0000013968412,0.00038906728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999403,0.0000049818423,0.000006528486,0.000017778957,0.000010792794,0.000019506393],"domain_scores_gemma":[0.9999006,0.0000080539685,0.000034363056,0.000006175739,0.000029210752,0.000021700262],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016298098,0.00021778372,0.0001155806,0.0015927341,0.00033901533,0.0005297647,0.00018347886,0.00020237049,0.0018937286],"category_scores_gemma":[0.00022586987,0.0001791955,0.00015956267,0.00071294827,0.00038134845,0.00024796327,0.0004474052,0.00016522985,0.0003001095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005254598,0.00003870418,0.8992371,0.00018161483,0.0000905279,0.0008778974,0.002837633,0.0007229359,0.074750036,0.00085592887,0.00017124282,0.019710986],"study_design_scores_gemma":[0.000002072817,0.00001926774,0.99870515,0.0000060345114,0.0000039225433,0.0000675697,0.00012559653,0.00007023297,0.0004919967,0.000015690055,0.0004909206,0.0000016186495],"about_ca_topic_score_codex":0.019851875,"about_ca_topic_score_gemma":0.032830574,"teacher_disagreement_score":0.019851875,"about_ca_system_score_codex":0.0007153204,"about_ca_system_score_gemma":0.00039713396,"threshold_uncertainty_score":0.03947264},"labels":[],"label_agreement":null},{"id":"W4280646234","doi":"10.2113/rgg20214435","title":"Late Mesozoic–Cenozoic Tectonics and Geodynamics of the East Arctic Region","year":2022,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Paleontology; Cretaceous; Lithosphere; Plate tectonics; Continental margin; Ridge push; Passive margin; Foreland basin; Tectonics; Rift","score_opus":0.009049241112476883,"score_gpt":0.1661954935778642,"score_spread":0.15714625246538733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280646234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992299,0.0011519927,0.0005663373,0.00023270649,0.000011931496,0.0000023057517,0.00020074658,0.000011377027,0.0055235233],"genre_scores_gemma":[0.9985448,0.00048623775,0.00019692545,0.000008097985,0.0000044736976,0.000001152337,0.00006924537,0.0000020615478,0.00068698666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996793,0.0000062769523,0.000002041006,0.000007426322,0.000007974548,0.000008405075],"domain_scores_gemma":[0.9999083,0.000009014633,0.000026205038,0.0000050086123,0.000035439964,0.000015967342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019676544,0.00009596506,0.000052420866,0.0005718697,0.00034658815,0.00053969154,0.00014347026,0.000087958106,0.0007297223],"category_scores_gemma":[0.0001693082,0.000059205096,0.00010430321,0.00044379663,0.00017166401,0.00021382964,0.00018040606,0.0001257853,0.00007985785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013285459,0.00003333843,0.88177764,0.0000940181,0.00012183171,0.0005339984,0.00291794,0.029584449,0.009276458,0.019662675,0.00094808685,0.05491673],"study_design_scores_gemma":[0.000005931174,0.000026571162,0.9662519,0.00005857137,0.000026281667,0.00015810954,0.0016635954,0.017659605,0.0007834757,0.002113246,0.0112418495,0.00001081069],"about_ca_topic_score_codex":0.12682763,"about_ca_topic_score_gemma":0.16424969,"teacher_disagreement_score":0.12682763,"about_ca_system_score_codex":0.0010783739,"about_ca_system_score_gemma":0.0008038105,"threshold_uncertainty_score":0.2521788},"labels":[],"label_agreement":null},{"id":"W4312121586","doi":"10.2113/rgg20224455","title":"Kuvaevite, Ir5Ni10S16, a New Mineral Species, Its Associations and Genetic Features, from the Sisim River Placer Zone, Eastern Sayans","year":2022,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Mineralogy and Gemology Studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Pleochroism; Geology; Placer mining; Pentlandite; Mineralogy; Geochemistry; Mineral; Analytical Chemistry (journal); Chemistry; Environmental chemistry; Pyrite","score_opus":0.010985948894037909,"score_gpt":0.1894549459535433,"score_spread":0.17846899705950542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312121586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971118,0.00019760648,0.0002945693,0.000009144579,0.000008096658,0.000021978543,0.00049886544,0.000009642606,0.0018483432],"genre_scores_gemma":[0.993396,0.00014362148,0.0012099984,0.000019926283,0.000005294198,0.000027309501,0.0023964446,0.000009909673,0.0027915037],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9997539,0.000008361349,0.000032218242,0.00013159374,0.000045105167,0.000028937618],"domain_scores_gemma":[0.99990726,0.000012038237,0.00002605385,0.000013228544,0.000023684077,0.000017671353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017263458,0.00030866425,0.0002807988,0.0011934863,0.00093612896,0.00052512443,0.00051732967,0.00033345164,0.0011053418],"category_scores_gemma":[0.00013572435,0.0002528756,0.00031472137,0.0010042418,0.00041207683,0.000272328,0.0006555654,0.00026370957,0.0005323455],"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":[0.0007400099,0.00027252483,0.34857973,0.00029860975,0.00020777823,0.0033749852,0.0052300342,0.00049011776,0.5907382,0.00065816054,0.00036572717,0.049044237],"study_design_scores_gemma":[0.000028337736,0.00028786148,0.96373636,0.00006750683,0.00007486019,0.0043566483,0.0031350283,0.00042825224,0.008910158,0.00014160102,0.018799782,0.00003359773],"about_ca_topic_score_codex":0.008408985,"about_ca_topic_score_gemma":0.022704015,"teacher_disagreement_score":0.008408985,"about_ca_system_score_codex":0.00048065447,"about_ca_system_score_gemma":0.00025744323,"threshold_uncertainty_score":0.016720116},"labels":[],"label_agreement":null},{"id":"W4322494517","doi":"10.2113/rgg20224493","title":"A Detailed Model of Magnetic Field Sources of the Earth’s Core Obtained by Solving the Inverse Problem of Magnetometry","year":2023,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","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":"Magnetization; Magnetic dipole; Magnetometer; Dipole; Magnetic field; Earth's magnetic field; Inverse problem; Inverse; Dipole model of the Earth's magnetic field; Geophysics; Physics; Magnetic anomaly; Computational physics; Field (mathematics); Geology; Geometry; Mathematical analysis; Interplanetary magnetic field; Mathematics; Solar wind; Quantum mechanics","score_opus":0.00810733542478357,"score_gpt":0.20581520006279277,"score_spread":0.1977078646380092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322494517","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":[0.20322247,0.00051675434,0.7547829,0.0004805299,0.000058936963,0.00008138499,0.0005400065,0.0006745599,0.03964243],"genre_scores_gemma":[0.94837755,0.00023166888,0.042091973,0.000050068138,0.000016415059,0.000078057084,0.00022987413,0.00005695788,0.008867463],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994564,0.000013423636,0.0000024449519,0.00001427439,0.000016354263,0.000007882278],"domain_scores_gemma":[0.99994075,0.000018716682,0.000009253103,0.000006986035,0.000018109942,0.000006124718],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013259474,0.00041675227,0.00041216525,0.0003464998,0.00032535766,0.00065352494,0.0008076836,0.00089668337,0.0019338506],"category_scores_gemma":[0.00030637215,0.00030636808,0.000520152,0.0003388494,0.0004806288,0.0005955751,0.000442938,0.00034194966,0.000303701],"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":[0.000029643386,0.000013089228,0.00077909156,0.00004685314,0.000017287537,0.00019787275,0.00005682497,0.9776273,0.006218661,0.010775118,0.00028114888,0.00395721],"study_design_scores_gemma":[0.00000795342,0.000012392556,0.00033640148,0.0000049026194,0.0000063751386,0.00003812777,0.000013456969,0.9966807,0.0005167686,0.0017890352,0.0005887586,0.0000050766776],"about_ca_topic_score_codex":0.009649898,"about_ca_topic_score_gemma":0.0044337544,"teacher_disagreement_score":0.009649898,"about_ca_system_score_codex":0.0005699951,"about_ca_system_score_gemma":0.00079210236,"threshold_uncertainty_score":0.01918745},"labels":[],"label_agreement":null},{"id":"W4383101463","doi":"10.2113/rgg20234538","title":"Mineral–Geochemical and Geotectonic Features of the Lotmvara-II Ultrabasic Sill, Serpentinite Belt (Kola Peninsula)","year":2023,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Sill; Ultramafic rock; Olivine; Geochemistry; Chromite; Amphibole; Mafic; Igneous rock; Mantle (geology); Porphyritic; Ilmenite; Mineralogy; Quartz; Paleontology","score_opus":0.005629521708848005,"score_gpt":0.18122421127344882,"score_spread":0.1755946895646008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383101463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99854654,0.00013641367,0.000035407025,0.000005369374,8.888177e-7,0.0000021269962,0.0002502665,0.000004097211,0.001018935],"genre_scores_gemma":[0.99936897,0.00005449571,0.000042682408,0.00000509006,0.0000011430435,0.0000017654775,0.0003162236,0.0000015395053,0.00020797907],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999577,0.0000029781015,0.000004399578,0.0000146904695,0.0000080206555,0.000012306826],"domain_scores_gemma":[0.9999466,0.0000037929206,0.000023152614,0.0000028783147,0.000010102761,0.000013525422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058644026,0.00020789856,0.00009723642,0.0014560928,0.00024818038,0.00039184952,0.00013157631,0.00010527055,0.0012932689],"category_scores_gemma":[0.000062972074,0.00012635862,0.00009226492,0.0005985835,0.0002561583,0.00015660889,0.00025831285,0.00007730318,0.00040008995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017925534,0.00002759021,0.9511578,0.00005989364,0.000050358885,0.0006101326,0.000620944,0.00028363138,0.03734616,0.00009663213,0.00013304393,0.009434659],"study_design_scores_gemma":[0.0000013344417,0.000011956254,0.9991603,0.0000029097785,0.000003007859,0.00011419932,0.00014958871,0.000060028127,0.0003029433,0.000005353862,0.00018739827,0.0000010518597],"about_ca_topic_score_codex":0.0095301615,"about_ca_topic_score_gemma":0.015008564,"teacher_disagreement_score":0.0095301615,"about_ca_system_score_codex":0.00035579814,"about_ca_system_score_gemma":0.00016822746,"threshold_uncertainty_score":0.01894939},"labels":[],"label_agreement":null},{"id":"W4402233551","doi":"10.2113/rgg20244752","title":"Features of Dispersal of Late Anisian Ammonoids of the Boreal Realm","year":2024,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Boreal; Paleontology; Geology; Archipelago; Fauna; Biostratigraphy; Biological dispersal; Physical geography; Oceanography; Geography; Ecology; Population; Biology","score_opus":0.004913752167900068,"score_gpt":0.20166875435130377,"score_spread":0.1967550021834037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402233551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995542,0.000044444285,0.000028555858,0.000004496202,6.1204906e-7,8.171764e-7,0.000037939622,0.0000013464971,0.00032761926],"genre_scores_gemma":[0.9997936,0.000022206754,0.00003992308,0.0000015700977,9.456253e-7,8.779917e-7,0.00006720449,6.4671104e-7,0.00007302294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999263,0.000009833535,0.000006603989,0.000026682286,0.000012450602,0.00001815516],"domain_scores_gemma":[0.99974936,0.000024963403,0.00010667881,0.000012396474,0.0000498772,0.000056709556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001547464,0.00009951125,0.00009650059,0.0009057115,0.00039493613,0.00034828304,0.0001536853,0.000076911565,0.0009026002],"category_scores_gemma":[0.00037417747,0.000070615766,0.000086329565,0.00054780056,0.00025953757,0.00021010975,0.00030774396,0.00008996216,0.00008867919],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008047017,0.000010701273,0.98886514,0.000010826941,0.000019918312,0.00012434376,0.00075618236,0.000068811474,0.0042256466,0.00010253758,0.000074734686,0.0056607365],"study_design_scores_gemma":[6.699121e-7,0.0000068438835,0.9994437,0.0000012045143,0.0000017150452,0.00007232695,0.0002479057,0.0000502685,0.00004098365,0.000009257266,0.00012414242,8.8126336e-7],"about_ca_topic_score_codex":0.02133592,"about_ca_topic_score_gemma":0.05617249,"teacher_disagreement_score":0.02133592,"about_ca_system_score_codex":0.00025277626,"about_ca_system_score_gemma":0.00020793026,"threshold_uncertainty_score":0.042423487},"labels":[],"label_agreement":null},{"id":"W4409023530","doi":"10.2113/rgg20254837","title":"GEOGRAPHIC DIFFERENTIATION OF BOREAL AMMONOIDS IN THE LADINIAN AGE (<i>Middle Triassic</i>)","year":2025,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ladinian; Geology; Paleontology; Boreal; Structural basin","score_opus":0.010152967215233897,"score_gpt":0.21052175729031536,"score_spread":0.20036879007508146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409023530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999355,0.00014449224,0.000025095076,0.0000068796517,9.682725e-7,0.0000014035928,0.000097063574,0.0000017704468,0.0003674048],"genre_scores_gemma":[0.9994149,0.00010892282,0.00011408212,0.000005206854,0.000001526647,0.00000263529,0.0002097257,0.0000011292486,0.00014173126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988854,0.000013615641,0.000009628013,0.000045127934,0.000015365784,0.000027618875],"domain_scores_gemma":[0.99967766,0.000021738235,0.00014593128,0.0000133821195,0.000064192405,0.000077064615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018137174,0.00011611394,0.00009975732,0.0010987876,0.00039446034,0.0003483923,0.00015750548,0.00013584176,0.0005696703],"category_scores_gemma":[0.00031980764,0.00008966805,0.00011408844,0.000786681,0.00029729534,0.00024692735,0.00036233247,0.00010958495,0.00010628749],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053638054,0.0000068799977,0.9911684,0.000010084358,0.000015912305,0.000041535724,0.0009818309,0.000022253791,0.002490301,0.000048077356,0.00005752312,0.0051034377],"study_design_scores_gemma":[4.4016124e-7,0.000007724919,0.9994899,0.0000013219625,0.0000017051628,0.000040267238,0.00028195328,0.000010989192,0.000027795248,0.0000032643645,0.00013376921,8.705499e-7],"about_ca_topic_score_codex":0.06784998,"about_ca_topic_score_gemma":0.19633347,"teacher_disagreement_score":0.06784998,"about_ca_system_score_codex":0.00038896888,"about_ca_system_score_gemma":0.00023115949,"threshold_uncertainty_score":0.1349101},"labels":[],"label_agreement":null}]}