{"meta":{"query_hash":"54ecf11f5c2e","filters":{"venue":"Geochemistry International"},"cohort_total":17,"direct_labels_cover":0,"predictions_cover":17,"exported":17,"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/54ecf11f5c2e","api":"https://metacan.xera.ac/api/v1/cohort?venue=Geochemistry+International"},"results":[{"id":"W2009814466","doi":"10.1134/s0016702913110050","title":"Unusual acid melts in the area of the unique Rosia Montana gold deposit, Apuseni Mountains, Romania: Evidence from inclusions in quartz","year":2013,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Science North","funders":"","keywords":"Melt inclusions; Orthoclase; Phenocryst; Quartz; Geology; Fluid inclusions; Mineralogy; Electron microprobe; Plagioclase; Geochemistry; Sanidine; Analytical Chemistry (journal); Chemistry; Mantle (geology)","score_opus":0.011132863516434097,"score_gpt":0.20345020603146313,"score_spread":0.19231734251502902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009814466","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892378,0.00034176788,0.000011112836,0.005399167,0.000061882354,0.00011330607,0.00010103737,0.000008672045,0.0047252676],"genre_scores_gemma":[0.99903244,0.00004454997,0.00012701853,0.00044386028,0.000056602974,0.000009957388,0.0001847019,0.0000013423157,0.000099506564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864244,0.000086030115,0.0003484697,0.00027094583,0.0004458404,0.00020627474],"domain_scores_gemma":[0.9991162,0.00038027525,0.00011297466,0.00026176003,0.0000754924,0.000053309646],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019334652,0.00013746585,0.00016299877,0.000036419184,0.000057234953,0.000046156056,0.0010216195,0.00010321652,0.003688056],"category_scores_gemma":[0.00031363883,0.00007720779,0.00010482388,0.0003134408,0.00011578841,0.00015685616,0.00011246208,0.00030797708,0.00003948344],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019030367,0.000059239464,0.9648428,0.0000050496988,0.000021102584,0.000011981986,0.00031056802,0.0006215617,0.032877713,0.000025170411,0.00053474127,0.00067103904],"study_design_scores_gemma":[0.00015094638,0.000014107595,0.9527675,0.0000755223,0.000011908631,0.0000101891055,0.00037622888,0.013546005,0.024913715,0.007928105,0.00009850528,0.00010724846],"about_ca_topic_score_codex":0.06521311,"about_ca_topic_score_gemma":0.05346141,"teacher_disagreement_score":0.012924443,"about_ca_system_score_codex":0.000021586959,"about_ca_system_score_gemma":0.000034093944,"threshold_uncertainty_score":0.9972227},"labels":[],"label_agreement":null},{"id":"W2011322324","doi":"10.1134/s0016702907040027","title":"Archean metaterrigenous rocks: Major geochemical constraints","year":2007,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geochemistry and Elemental 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":"Archean; Geology; Geochemistry; Petrology; Earth science","score_opus":0.008352417100523325,"score_gpt":0.22340605257436907,"score_spread":0.21505363547384576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011322324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7770121,0.00009096511,0.0010288571,0.00048174255,0.00027892424,0.00005320913,0.0003008658,0.000065291075,0.22068805],"genre_scores_gemma":[0.99418885,0.000008064863,0.0009739826,0.0002681739,0.00043377382,0.0000010912561,0.0022514802,0.0000035731916,0.0018710437],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9982411,0.000010583788,0.00037977388,0.00038740295,0.00049540756,0.00048572125],"domain_scores_gemma":[0.99924767,0.00008113574,0.00011019843,0.00020506764,0.000102187056,0.00025371878],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040837118,0.00020124024,0.0001686977,0.00005579262,0.00013928188,0.00006656568,0.0004992346,0.00011294577,0.047257006],"category_scores_gemma":[0.00008048975,0.00019131231,0.00015731566,0.00013309636,0.00020993882,0.00011477027,0.000035172794,0.00023385821,0.00043663877],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003502027,0.00029818478,0.6377025,0.00009178566,0.001016831,0.0005505498,0.00043055686,0.00035675365,0.18764834,0.000062499654,0.007150803,0.16434099],"study_design_scores_gemma":[0.0011463731,0.000045699708,0.08543803,0.000039319628,0.00011988569,0.00069610635,0.0013648677,0.0021548464,0.87930566,0.0036718657,0.025192754,0.0008245747],"about_ca_topic_score_codex":0.00059881294,"about_ca_topic_score_gemma":0.0003768549,"teacher_disagreement_score":0.69165736,"about_ca_system_score_codex":0.000022754473,"about_ca_system_score_gemma":0.00004629803,"threshold_uncertainty_score":0.95361394},"labels":[],"label_agreement":null},{"id":"W2027472088","doi":"10.1134/s0016702908090048","title":"The accumulation of Cu, Zn, Cd, and Pb in the aquatic biomass of sulphide tailing ponds","year":2008,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Mine drainage and remediation techniques","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Tailings; Environmental science; Biomass (ecology); Aquatic ecosystem; Environmental chemistry; Ecosystem; Trophic level; Aquatic plant; Chemistry; Ecology; Macrophyte; Biology","score_opus":0.02253237774316262,"score_gpt":0.2827743197989133,"score_spread":0.2602419420557507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027472088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99283874,0.00003810152,0.00030182864,0.0006882616,0.000023413477,0.000056037385,0.0000046653113,0.0000050027083,0.006043941],"genre_scores_gemma":[0.999389,0.000059210757,0.000250402,0.00002845437,0.000024794086,0.0000069876573,0.000018427461,0.0000019504866,0.00022077558],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99939805,0.000016149741,0.00019017886,0.00008257055,0.00025227058,0.000060782426],"domain_scores_gemma":[0.99963075,0.00012605019,0.00011373771,0.000105989864,0.00001312428,0.000010348746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025282582,0.000045405865,0.000048012553,0.000016562351,0.000046095007,0.0000060394004,0.00020988227,0.000031130738,0.00013299336],"category_scores_gemma":[0.00015961587,0.000029093286,0.000022554437,0.00008537819,0.00016439157,0.000060470786,0.000057831123,0.000050279672,0.0000023045473],"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":[0.000013487247,0.000047258392,0.05850702,0.0000112637435,0.0000087562885,0.0000033804638,0.0011413388,0.000048235197,0.9376759,0.00013266639,0.0009934697,0.0014172039],"study_design_scores_gemma":[0.00029878164,0.0000200859,0.077036105,0.000024607025,0.000005532828,0.000033569107,0.0005454898,0.008546032,0.90840137,0.0034329507,0.0015654077,0.00009008872],"about_ca_topic_score_codex":0.00016475155,"about_ca_topic_score_gemma":0.000037423568,"teacher_disagreement_score":0.029274568,"about_ca_system_score_codex":0.000022966145,"about_ca_system_score_gemma":0.000007283843,"threshold_uncertainty_score":0.1456184},"labels":[],"label_agreement":null},{"id":"W2029359424","doi":"10.1134/s001670291010006x","title":"Mineralogy and major-trace element geochemistry of the Haymana manganese mineralizations, Ankara, Turkey","year":2010,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Manganese; Trace element; TRACE (psycholinguistics); Metallurgy; Materials science","score_opus":0.005727276749746972,"score_gpt":0.21917093689506273,"score_spread":0.21344366014531577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029359424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92728907,0.00013022753,0.0018976192,0.017207628,0.000853886,0.00013538559,0.00005754409,0.00007450251,0.052354164],"genre_scores_gemma":[0.9851632,0.000010318921,0.0037836258,0.00019030488,0.00021982919,0.000020691597,0.000065426546,0.0000036744075,0.0105429385],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985873,0.000018880946,0.00034751845,0.00043618213,0.00035810724,0.00025199034],"domain_scores_gemma":[0.9986041,0.00006991142,0.00023167141,0.00068954326,0.00031585532,0.000088912726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021586208,0.00019454784,0.0001547171,0.000030989573,0.00012124151,0.00007455065,0.001364606,0.00016029902,0.00056199904],"category_scores_gemma":[0.00026900438,0.00016374994,0.0000904771,0.00016459884,0.00019201702,0.0001419369,0.0005992632,0.00032148306,0.000004654152],"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":[0.000006829756,0.00010114096,0.015383701,0.00008559995,0.000072270996,0.000011756495,0.00017534233,0.00009879146,0.9630856,0.0072018835,0.013231007,0.00054608367],"study_design_scores_gemma":[0.0009603611,0.000013607693,0.018264068,0.0000652055,0.000034632376,0.0005843933,0.000108004606,0.027424121,0.8307731,0.009266984,0.111995555,0.0005099716],"about_ca_topic_score_codex":0.00008662462,"about_ca_topic_score_gemma":0.000024082232,"teacher_disagreement_score":0.13231249,"about_ca_system_score_codex":0.000019629882,"about_ca_system_score_gemma":0.0000731375,"threshold_uncertainty_score":0.66775286},"labels":[],"label_agreement":null},{"id":"W2043047487","doi":"10.1134/s0016702914090080","title":"Radioactive elements in collisional and within-plate Sodic-Potassic Granitoids: Accumulation levels and metallogenic significance","year":2014,"lang":"en","type":"article","venue":"Geochemistry International","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":"Precambrian; Geology; Craton; Geochemistry; Baltic Shield; Continental crust; Uranium; Massif; Magmatism; Crust; Paleontology; Tectonics","score_opus":0.0202503023159345,"score_gpt":0.2404333608546528,"score_spread":0.2201830585387183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043047487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968515,0.00010680547,0.00019290627,0.0005038801,0.0000780423,0.000057456746,0.000116904856,0.000011966103,0.0020805185],"genre_scores_gemma":[0.9978073,0.000018065799,0.0014863746,0.00015402249,0.00008172726,0.000002958375,0.00030240623,0.0000014508076,0.00014568644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989544,0.00003512012,0.00025373627,0.0003279575,0.00026290645,0.00016588658],"domain_scores_gemma":[0.9995012,0.00017138124,0.00010510353,0.000071671755,0.00005425378,0.00009636353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026059983,0.00012624639,0.00015448267,0.00004734034,0.0000687801,0.000050242732,0.00014110167,0.000068009074,0.002698972],"category_scores_gemma":[0.00015168077,0.00010424674,0.000035931516,0.000106007414,0.00011414644,0.0001336191,0.000028187631,0.00014055784,0.000017277054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074177275,0.0000311603,0.97255844,0.000013608263,0.0000814946,0.000007184611,0.00006737499,0.0013476062,0.01857835,0.00015857055,0.00004062359,0.0070414115],"study_design_scores_gemma":[0.00066745933,0.000032581644,0.8484633,0.000017043805,0.00002508291,0.000021694212,0.00006370249,0.104441054,0.009123491,0.036511157,0.00042481563,0.00020859414],"about_ca_topic_score_codex":0.00038523084,"about_ca_topic_score_gemma":0.0004311351,"teacher_disagreement_score":0.12409511,"about_ca_system_score_codex":0.000008212176,"about_ca_system_score_gemma":0.000015978605,"threshold_uncertainty_score":0.9982127},"labels":[],"label_agreement":null},{"id":"W2050140946","doi":"10.1134/s0016702910040051","title":"Mantle source of the Archean Panozero pluton, Karelia: evidence from isotope-geochemical study of rocks and minerals","year":2010,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Russian Academy of Sciences; Earth Sciences Division","keywords":"Pluton; Geochemistry; Geology; Archean; Mantle (geology); Mafic; Xenolith; Quartz monzonite; Tectonics; Paleontology","score_opus":0.012544183266942593,"score_gpt":0.21735570557087464,"score_spread":0.20481152230393204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050140946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997297,0.00012176976,0.000012437836,0.00071046967,0.0001174691,0.00007744231,0.00011581365,0.0000094971665,0.001538107],"genre_scores_gemma":[0.99915904,0.000015974978,0.00019843385,0.00005474743,0.00012210138,0.00000198345,0.000073856354,0.0000015760537,0.00037229175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99877757,0.000026534446,0.00033205922,0.00029779543,0.0004153426,0.00015072888],"domain_scores_gemma":[0.9990277,0.0003174948,0.00017445683,0.0002627534,0.00013422381,0.00008331769],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013715781,0.00012764285,0.00020640263,0.000020263777,0.000049606773,0.00001773857,0.0005763659,0.00009268035,0.006888837],"category_scores_gemma":[0.0004944895,0.00008222614,0.000092828166,0.000109741246,0.0002107208,0.00006978155,0.00012520091,0.00028800732,0.000008706314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003349391,0.00008675456,0.7356932,0.000008198009,0.000051988452,0.0000012850148,0.00015626919,0.00013029511,0.26285043,0.0000015243277,0.00021291288,0.00077359204],"study_design_scores_gemma":[0.00043785875,0.00006217678,0.6280508,0.000051272073,0.00007255155,0.000012650785,0.00047266227,0.0050154706,0.3616262,0.003439853,0.0005773881,0.00018111513],"about_ca_topic_score_codex":0.008413324,"about_ca_topic_score_gemma":0.0019446661,"teacher_disagreement_score":0.10764245,"about_ca_system_score_codex":0.0000019821537,"about_ca_system_score_gemma":0.000020649473,"threshold_uncertainty_score":0.99818975},"labels":[],"label_agreement":null},{"id":"W2071654491","doi":"10.1134/s0016702913110086","title":"Supergene transformed naphthides: Peculiarities of trace-element composition","year":2013,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Trace element; Geology; Geochemistry; Supergene (geology); Petroleum; Environmental chemistry; Organic matter; Structural basin; Mineralogy; Chemistry; Paleontology; Weathering","score_opus":0.00653662721839008,"score_gpt":0.20731156411539434,"score_spread":0.20077493689700426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071654491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95625156,0.00013609929,0.0057115895,0.00079359225,0.00020704235,0.00008614296,0.000055369623,0.000100863566,0.036657758],"genre_scores_gemma":[0.998769,0.00012400167,0.0003338456,0.000020129748,0.00008279692,0.000046825022,0.00026191722,0.000008649635,0.0003528337],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992991,0.000005192212,0.00025946874,0.000088744804,0.0002411036,0.00010636278],"domain_scores_gemma":[0.9997105,0.000011905114,0.000022995642,0.000092767325,0.00011303372,0.00004878234],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00003793735,0.00009171961,0.00011014242,0.00005486414,0.000021675187,0.000025078261,0.00014503587,0.00005374985,0.004478855],"category_scores_gemma":[0.0000058551677,0.00009187467,0.00009293281,0.000069146656,0.000030661584,0.0001456475,0.000008685036,0.00007361064,0.000039855164],"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":[0.000006673067,0.000075849646,0.0004679058,0.00011333141,0.00033694916,0.0000019687564,0.0005421622,0.025753634,0.96535784,0.0001850817,0.0060209036,0.0011377059],"study_design_scores_gemma":[0.00034408958,0.000008378801,0.00042423874,0.000029774184,0.000018338025,0.0000061141272,0.00059731683,0.1683788,0.82677835,0.000284808,0.0029809729,0.00014883664],"about_ca_topic_score_codex":0.000031058204,"about_ca_topic_score_gemma":0.0000057355824,"teacher_disagreement_score":0.14262517,"about_ca_system_score_codex":0.000047409325,"about_ca_system_score_gemma":0.000010464722,"threshold_uncertainty_score":0.9964312},"labels":[],"label_agreement":null},{"id":"W2079246956","doi":"10.1134/s0016702906030037","title":"Kaidun meteorite: Crystals of oxides in cavities","year":2006,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lockheed Martin (Canada)","funders":"","keywords":"Meteorite; Geology; Breccia; Mineral; Crystallization; Acicular; Composition (language); Chondrite; Parent body; Clastic rock; Mineralogy; Geochemistry; Crystallography; Materials science; Astrobiology; Chemistry; Sedimentary rock; Microstructure; Physics; Metallurgy","score_opus":0.003361954125630755,"score_gpt":0.20128700729421095,"score_spread":0.1979250531685802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079246956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90716976,0.000019811801,0.00036122216,0.0000737591,0.00007898991,0.000019039118,0.00022058024,0.0000048451434,0.09205199],"genre_scores_gemma":[0.99660766,3.129967e-7,0.000610743,0.0000065921504,0.0001823922,0.0000029234056,0.000335668,0.000001855751,0.0022518535],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994796,0.0000052390114,0.00016155408,0.00010598429,0.00014667843,0.000100958525],"domain_scores_gemma":[0.99978,0.00003397612,0.00006442645,0.00007094042,0.00003482194,0.000015849795],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000621239,0.000060893468,0.000074629905,0.000027276677,0.0000137288025,0.0000138985615,0.00016717704,0.00001609587,0.0018398934],"category_scores_gemma":[0.0000036496265,0.00006183212,0.0000349469,0.00004951604,0.000044685687,0.000083318926,0.000022972845,0.000056693993,0.0000075114135],"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":[0.000009969444,0.00007371844,0.7529071,0.000008034791,0.000018104309,0.0000032308392,0.000058910693,0.0010428991,0.23853885,0.004134354,0.0021422782,0.0010625288],"study_design_scores_gemma":[0.0007942321,0.000019081948,0.43045104,0.00006999146,0.0000105669615,0.000006957352,0.0009801539,0.0028733565,0.5419934,0.011174092,0.011285369,0.0003417904],"about_ca_topic_score_codex":0.0011348858,"about_ca_topic_score_gemma":0.000012256261,"teacher_disagreement_score":0.3224561,"about_ca_system_score_codex":0.000009345759,"about_ca_system_score_gemma":0.000024806222,"threshold_uncertainty_score":0.99907255},"labels":[],"label_agreement":null},{"id":"W2092232265","doi":"10.1134/s0016702913030051","title":"Late pleistocene sedimentation history of the Shirshov Ridge, Bering Sea","year":2013,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Pleistocene; Lithology; Glacial period; Ridge; Sedimentary rock; Oceanography; Deposition (geology); Terrigenous sediment; Sedimentation; Geochemistry; Sea level; Sediment; Geomorphology; Paleontology","score_opus":0.014360174252286901,"score_gpt":0.22228033607284972,"score_spread":0.20792016182056283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092232265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93181896,0.00014261341,0.0000054074635,0.001191314,0.00066349405,0.00006442143,0.000035791425,0.0000104844685,0.066067524],"genre_scores_gemma":[0.99290746,0.000008803511,0.000099982026,0.00015336896,0.000066385546,0.0000034806487,0.00021116844,0.0000011664546,0.006548189],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993684,0.000026303536,0.00014030497,0.00012507297,0.00020042906,0.0001394828],"domain_scores_gemma":[0.9996065,0.00007482779,0.00007607953,0.00012029744,0.00008399944,0.000038300725],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010369159,0.000062098705,0.00006677721,0.000022802924,0.000042581425,0.000007252038,0.00030932663,0.00006734642,0.019598246],"category_scores_gemma":[0.000051794006,0.000048402282,0.000043547792,0.00003807011,0.00017255261,0.00009205566,0.000024651565,0.00014569853,0.00025468826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010961323,0.000008607232,0.9931195,0.000011728319,0.000023332435,0.0000013791583,0.00007073081,0.00025980055,0.001112863,0.00001499701,0.004924699,0.00044144117],"study_design_scores_gemma":[0.00016308193,0.0000087926455,0.9847771,0.000009390396,0.000004520414,0.00002324884,0.000029647244,0.0063007833,0.0057891062,0.00042103915,0.0024151667,0.000058130936],"about_ca_topic_score_codex":0.0006306904,"about_ca_topic_score_gemma":0.00025702425,"teacher_disagreement_score":0.061088506,"about_ca_system_score_codex":0.000009306635,"about_ca_system_score_gemma":0.0000747093,"threshold_uncertainty_score":0.98129797},"labels":[],"label_agreement":null},{"id":"W2122685953","doi":"10.1134/s0016702908060062","title":"Metamorphic rocks of the Murmansk domain (Kola Peninsula) as compared with the oldest rock associations of the northeastern Baltic shield, Canada, and Greenland","year":2008,"lang":"en","type":"article","venue":"Geochemistry International","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":"Geology; Archean; Baltic Shield; Gneiss; Geochemistry; Metamorphic rock; Precambrian; Greenstone belt; Volcanic rock; Basement; Shield; Petrology; Volcano; Archaeology","score_opus":0.009426125762233947,"score_gpt":0.1743801270855957,"score_spread":0.16495400132336174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122685953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925723,0.00008215774,0.000010512891,0.0032310653,0.000044424585,0.00006396448,0.00029202344,0.0000031287473,0.0037004072],"genre_scores_gemma":[0.9986403,0.0000052945825,0.000017316379,0.0002224829,0.000040764473,0.0000015209146,0.000078126664,0.0000011870617,0.0009930253],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989772,0.000042877113,0.00019556344,0.0001464612,0.0005079327,0.00013000108],"domain_scores_gemma":[0.99927264,0.00017475846,0.00020273251,0.0001817613,0.00011960312,0.000048515256],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008655914,0.00010111555,0.00014794705,0.000009173244,0.00019292375,0.00001079247,0.00049362093,0.000038840775,0.0013597307],"category_scores_gemma":[0.000071374925,0.00004486367,0.000078273595,0.00015445732,0.00016686162,0.000029747856,0.000053786334,0.00015965258,0.0000028676168],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015409087,0.000014619599,0.99703705,0.0000052654636,0.00008763751,0.0000022758054,0.000086633256,0.002049287,0.0004645799,0.0000075958123,0.0001918175,0.000037813898],"study_design_scores_gemma":[0.00021000416,0.000010324171,0.99245167,0.000012011036,0.000047854213,0.000050658426,0.00014137884,0.0028745742,0.0032165616,0.00054126716,0.00037219826,0.00007149802],"about_ca_topic_score_codex":0.3066742,"about_ca_topic_score_gemma":0.5961219,"teacher_disagreement_score":0.2894477,"about_ca_system_score_codex":0.0000070885258,"about_ca_system_score_gemma":0.000115782,"threshold_uncertainty_score":0.99955314},"labels":[],"label_agreement":null},{"id":"W2147111500","doi":"10.1134/s0016702906020017","title":"Endogenic cycles and the problem of crustal growth","year":2006,"lang":"en","type":"article","venue":"Geochemistry International","topic":"High-pressure geophysics and materials","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":"Russian Foundation for Basic Research","keywords":"Geology; Earth science; Geochemistry; Astrobiology; Petrology; Paleontology; Biology","score_opus":0.0035377670518376265,"score_gpt":0.17363855899860697,"score_spread":0.17010079194676936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147111500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93721205,0.0001407209,0.000022091488,0.0004267644,0.00009743869,0.000051204603,0.00025610093,0.000009308457,0.06178435],"genre_scores_gemma":[0.9988059,0.000017914941,0.0003026334,0.000020667376,0.00022931873,0.0000013285618,0.00017108493,0.0000010663655,0.00045008902],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995312,0.000011429979,0.00013157995,0.00009526364,0.00014943027,0.00008106722],"domain_scores_gemma":[0.99975336,0.000057984438,0.000070236696,0.00005424774,0.00004785426,0.000016297527],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010331939,0.00005560895,0.00007703758,0.000009506185,0.0000374568,0.000034331435,0.00014583199,0.000023901854,0.0012003828],"category_scores_gemma":[0.000008679395,0.000036864767,0.000030893338,0.000022605016,0.00012520874,0.00004867798,0.000016642958,0.000032546133,0.000011252208],"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":[0.0011598367,0.0002231827,0.46826044,0.00043847712,0.00063239667,0.000046420126,0.0007142294,0.0023299658,0.3740906,0.10953598,0.022696305,0.019872176],"study_design_scores_gemma":[0.003297745,0.000035324745,0.36627764,0.000052323336,0.00007134428,0.00010372965,0.00012465923,0.002510285,0.45096117,0.15801392,0.018149989,0.00040189383],"about_ca_topic_score_codex":0.0024156482,"about_ca_topic_score_gemma":0.00006852192,"teacher_disagreement_score":0.10198282,"about_ca_system_score_codex":8.6377224e-7,"about_ca_system_score_gemma":0.000013686471,"threshold_uncertainty_score":0.99971265},"labels":[],"label_agreement":null},{"id":"W2588241041","doi":"10.1134/s0016702917010049","title":"Geochemical controls on the formation of unconformity-type Au–U deposits (Northern Transbaikalia)","year":2017,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Irkutsk State University","keywords":"Unconformity; Geology; Geochemistry; Petrology; Sedimentary rock","score_opus":0.015916437339408195,"score_gpt":0.2282555400479342,"score_spread":0.212339102708526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588241041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92507505,0.000016827084,0.000030173123,0.0022072413,0.00016677371,0.00006025332,0.00016088053,0.000010743976,0.07227208],"genre_scores_gemma":[0.9985047,0.000008231783,0.000028506984,0.000120247525,0.00017855072,0.0000019007487,0.000593246,0.0000017775509,0.0005628256],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989708,0.000011868625,0.00026316274,0.00016729653,0.00039603264,0.00019080655],"domain_scores_gemma":[0.99910206,0.000081540034,0.00026019747,0.0003446705,0.00014366122,0.00006787607],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019834649,0.0001273618,0.00013346128,0.000016402833,0.0003317376,0.000091355854,0.0007372959,0.00007423667,0.002680286],"category_scores_gemma":[0.00018476493,0.00009136608,0.00012089128,0.000035283607,0.00014440008,0.00019352528,0.00002169368,0.00014604504,0.00008746541],"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":[0.0005146344,0.0001304804,0.8845546,0.00008368685,0.00036071677,0.000016177928,0.00035316034,0.001105802,0.090239026,0.00017561177,0.0017077507,0.020758333],"study_design_scores_gemma":[0.00070725515,0.00006206319,0.12077539,0.00006784776,0.000061825885,0.00003727048,0.0003279358,0.010974108,0.86235666,0.0014644061,0.0029163086,0.00024893892],"about_ca_topic_score_codex":0.00073636405,"about_ca_topic_score_gemma":0.0019147565,"teacher_disagreement_score":0.7721176,"about_ca_system_score_codex":0.000016311773,"about_ca_system_score_gemma":0.00004771091,"threshold_uncertainty_score":0.9982314},"labels":[],"label_agreement":null},{"id":"W2886953068","doi":"10.1134/s0016702918080049","title":"In situ LA-ICPMS Isotopic and Geochronological Studies on Carbonatites and Phoscorites from the Guli Massif, Maymecha-Kotuy, Polar Siberia","year":2018,"lang":"en","type":"article","venue":"Geochemistry International","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":"Activation Laboratories","funders":"","keywords":"Carbonatite; Massif; Geochemistry; Geology; Mantle (geology)","score_opus":0.014204479552026847,"score_gpt":0.23628332744861813,"score_spread":0.22207884789659127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886953068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98343736,0.0011284073,0.0000019127012,0.00749424,0.00016453261,0.0000431951,0.00013126954,0.000016949496,0.0075821294],"genre_scores_gemma":[0.9978554,0.00022108364,0.00030059577,0.00088276516,0.00037811644,0.0000027957801,0.00014523105,0.0000013649968,0.00021264996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901885,0.00003795542,0.00019732483,0.00035999558,0.00020308317,0.00018281993],"domain_scores_gemma":[0.99907815,0.0006223438,0.00006312234,0.00011784819,0.000058409176,0.000060121976],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000151359,0.00015205183,0.00016967881,0.000025434825,0.00010654668,0.00006519592,0.000236356,0.00010060422,0.004319468],"category_scores_gemma":[0.00037887547,0.00009215415,0.000037907004,0.000085386746,0.0004627807,0.00007169455,0.00008517207,0.00019698702,0.0000546721],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007723645,0.000046467718,0.96725273,0.000009539575,0.00015540396,0.000039908817,0.00038769183,0.0000118334765,0.027185695,0.00040761923,0.0010135642,0.0034123042],"study_design_scores_gemma":[0.00045003468,0.0000847246,0.87770426,0.000042015563,0.000027628936,0.000020989737,0.00060655683,0.0023741182,0.029375477,0.084950745,0.0041160644,0.0002473721],"about_ca_topic_score_codex":0.001956491,"about_ca_topic_score_gemma":0.0028821777,"teacher_disagreement_score":0.08954846,"about_ca_system_score_codex":0.0000069575244,"about_ca_system_score_gemma":0.00001116623,"threshold_uncertainty_score":0.99659073},"labels":[],"label_agreement":null},{"id":"W2970745978","doi":"10.1134/s0016702919090106","title":"Texture and Genesis of Polycrystalline Varieties of Diamond Based on Phase-Contrast and Diffraction Contrast Tomography","year":2019,"lang":"en","type":"article","venue":"Geochemistry International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada)","funders":"","keywords":"Texture (cosmology); Diamond; Materials science; Phase contrast microscopy; Contrast (vision); Diffraction; Mineralogy; Crystallography; Phase (matter); Analytical Chemistry (journal); Chemistry; Metallurgy; Optics; Chromatography; Physics","score_opus":0.0038022091984537833,"score_gpt":0.19734079141957026,"score_spread":0.19353858222111647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970745978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99614125,0.00014283057,0.00010592639,0.000090023816,0.00017160985,0.0000679025,0.0011329489,0.000006177482,0.0021413052],"genre_scores_gemma":[0.9993198,0.00002795041,0.00008631664,0.000035529305,0.00008301392,8.358327e-7,0.0003480129,0.000002009613,0.00009656297],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994105,0.000011280842,0.0001610382,0.00014962691,0.00018441502,0.00008314544],"domain_scores_gemma":[0.9995885,0.00009844963,0.00012739091,0.00008344108,0.00006224444,0.000039984152],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000077460165,0.00008838477,0.0001512887,0.00003855044,0.00002027278,0.000023986982,0.00007592664,0.000056060297,0.0015347737],"category_scores_gemma":[0.000016282771,0.00007593559,0.000032464235,0.000034647164,0.0000698527,0.00006792143,0.0000071583645,0.000043120024,0.0000018028329],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000593311,0.00014440528,0.22835112,0.00017789897,0.00012583719,0.0000024830122,0.0000936267,0.00050614995,0.7631995,0.00016363549,0.00024505786,0.006396973],"study_design_scores_gemma":[0.0027115082,0.00029436534,0.734939,0.00009174781,0.000056431083,0.000007800108,0.000151275,0.019644406,0.23917516,0.00079029216,0.0018815307,0.00025649343],"about_ca_topic_score_codex":0.00041865258,"about_ca_topic_score_gemma":0.000015047701,"teacher_disagreement_score":0.52402437,"about_ca_system_score_codex":0.0000010273179,"about_ca_system_score_gemma":0.000014853829,"threshold_uncertainty_score":0.99937797},"labels":[],"label_agreement":null},{"id":"W4366823064","doi":"10.1134/s0016702923060071","title":"Granophyre Norites and Diorites of the Jarva-Varaka Massif (Monchegorsk Ore Area, Kola Region, Russia): Geology, Petrography, Geochemistry, Geochronology and Origin","year":2023,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geochemistry; Massif; Felsic; Mafic; Diorite; Gneiss; Porphyritic; Anorthosite; Hornfels; Greenschist; Petrology; Plagioclase; Metamorphism; Biotite; Quartz; Zircon; Metamorphic rock","score_opus":0.011836885064424473,"score_gpt":0.20506210484469783,"score_spread":0.19322521978027335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366823064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9837974,0.00076208176,0.000010415126,0.0052190907,0.00019025661,0.00007572831,0.0002161798,0.00006875428,0.00966014],"genre_scores_gemma":[0.99724686,0.00043540882,0.00018545809,0.00011451111,0.00016025687,0.00000658215,0.0006548208,0.0000039516385,0.001192159],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826366,0.000045659268,0.00037497163,0.00056617026,0.00033740312,0.00041216254],"domain_scores_gemma":[0.9989144,0.0002723138,0.00020130121,0.00030535724,0.00014894737,0.00015763867],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018622112,0.00027132942,0.0003280096,0.00008919949,0.00018619122,0.000051063824,0.000548202,0.00023553056,0.003043868],"category_scores_gemma":[0.0002673464,0.00018979669,0.00017946429,0.0004954395,0.0010441889,0.000090336376,0.00019231434,0.00032331978,0.00002308783],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029289798,0.000027928992,0.98764116,0.000050245766,0.00013653755,0.000029994313,0.000036166995,0.00005895783,0.006032361,0.00013963107,0.0017055294,0.004112181],"study_design_scores_gemma":[0.000494715,0.00004578808,0.95138985,0.000036931535,0.00007318795,0.00020995132,0.0002658297,0.005942929,0.01058341,0.025062403,0.005580371,0.0003146526],"about_ca_topic_score_codex":0.0015096238,"about_ca_topic_score_gemma":0.00039235564,"teacher_disagreement_score":0.036251344,"about_ca_system_score_codex":0.0000069286616,"about_ca_system_score_gemma":0.000039041977,"threshold_uncertainty_score":0.99786747},"labels":[],"label_agreement":null},{"id":"W4389477469","doi":"10.1134/s0016702923020118","title":"Geochemistry of the Massive Dolomites in Eastern Black Sea Region: REE Implications for Dolomite Petrogenesis","year":2023,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Dolomitization; Geology; Dolomite; Dolostone; Diagenesis; Geochemistry; Cretaceous; Carbonate; Fluid inclusions; Sedimentary rock; Calcite; Paleontology; Carbonate rock; Hydrothermal circulation; Facies","score_opus":0.026371859032734046,"score_gpt":0.24103629708400415,"score_spread":0.2146644380512701,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389477469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9797612,0.00006474033,0.00004722225,0.010943842,0.00009558325,0.000112316004,0.0006412194,0.000032717428,0.008301172],"genre_scores_gemma":[0.9967536,0.00003660119,0.00014413019,0.00014396591,0.000163394,0.000017228944,0.0009720128,0.000002774552,0.0017662947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988024,0.000020411248,0.0003420367,0.0003472922,0.00021372986,0.00027413265],"domain_scores_gemma":[0.99897504,0.00030985827,0.00017819497,0.00029340107,0.00016955043,0.000073927244],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014931304,0.000143585,0.00018439296,0.00005220079,0.00007144399,0.000023754847,0.00066928676,0.00011489018,0.0017187268],"category_scores_gemma":[0.000387985,0.00010437695,0.00023616172,0.00046331366,0.00020200835,0.000053930664,0.00007775586,0.00012840402,0.000059279733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004057148,0.000025253777,0.9809345,0.000035337172,0.000053590054,0.0000028225297,0.000027191418,0.0013218835,0.013055847,0.000046354493,0.0034097263,0.0010469327],"study_design_scores_gemma":[0.00044688798,0.000014315711,0.89389217,0.00003825218,0.00003287423,0.00001494444,0.00017854274,0.020326177,0.058795724,0.02443988,0.0016200554,0.00020015835],"about_ca_topic_score_codex":0.00026689397,"about_ca_topic_score_gemma":0.00027181956,"teacher_disagreement_score":0.0870423,"about_ca_system_score_codex":0.000011874826,"about_ca_system_score_gemma":0.000042012998,"threshold_uncertainty_score":0.99919385},"labels":[],"label_agreement":null},{"id":"W4409946653","doi":"10.1134/s0016702925600105","title":"Diverse Lavas of the Tigilsky Dol and Mount Oxi Massif (Sredinny Range, Kamchatka): a Perspective from the New Sr–Nd Isotope Data","year":2025,"lang":"en","type":"article","venue":"Geochemistry International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Massif; Geology; Geochemistry; Mount; Volcano; Range (aeronautics); Perspective (graphical); Earth science; Materials science","score_opus":0.016189460134681713,"score_gpt":0.23214050729397254,"score_spread":0.2159510471592908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409946653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.934181,0.0015696089,0.000064251464,0.024182452,0.00030555835,0.0001092323,0.002236966,0.000016330088,0.037334625],"genre_scores_gemma":[0.99575806,0.000094883515,0.00015153184,0.0006433426,0.00020985132,9.090535e-7,0.000465854,8.9768383e-7,0.0026746998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990233,0.00002595433,0.00017501385,0.00034344418,0.0002943981,0.00013787214],"domain_scores_gemma":[0.99911815,0.00023823786,0.00009035004,0.00039197574,0.00010258433,0.00005868882],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011762352,0.00011690125,0.00013578993,0.000015103161,0.00011296451,0.0000558787,0.0010752106,0.00006767024,0.010275496],"category_scores_gemma":[0.00036553456,0.000063444095,0.00007589485,0.0001701829,0.00023552266,0.00008685631,0.00029332476,0.00018261837,0.000019878751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013654961,0.000057953308,0.9358825,0.000012072613,0.0005133714,0.000006820062,0.00042974143,0.00010305071,0.004581956,0.0009991445,0.050510917,0.006765941],"study_design_scores_gemma":[0.000966696,0.000018186036,0.84914494,0.00007956813,0.00022924934,0.000008467852,0.0036083027,0.011439803,0.010898314,0.07258206,0.050764326,0.0002600847],"about_ca_topic_score_codex":0.014412722,"about_ca_topic_score_gemma":0.0028637894,"teacher_disagreement_score":0.086737536,"about_ca_system_score_codex":0.000011015275,"about_ca_system_score_gemma":0.00006446491,"threshold_uncertainty_score":0.99215037},"labels":[],"label_agreement":null}]}