{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":8,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":8,"direct_label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline (scores rank; they never assert a category)","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12","author_layer_release":"2026-06-26"},"query_hash":"4b98142f8ec3","filters":{"venue":"Lithology and Mineral Resources"}},"results":[{"id":"W2022207791","doi":"10.1134/s0024490215010046","title":"Geochemistry of C, O, and Sr isotopes in the Neoproterozoic carbonates from the southwestern Patom paleobasin, southern Middle Siberia","year":2015,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Marl; δ13C; Isotopes of carbon; Sedimentology; Paleontology; Chemostratigraphy; Geochemistry; Excursion; Precambrian; Total organic carbon; Stable isotope ratio; Structural basin","authors":[{"name":"B. G. Pokrovsky","is_ca":false},{"name":"M. I. Bujakaite","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02419800426599987,"gpt":0.2155361310869821,"spread":0.1913381268209822,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001614391,0.0002715769,0.0002384837,0.001619802,0.0008748202,0.0006354925,0.0002300318,0.0001936512,0.0009499337],"category_scores_gemma":[0.0002035471,0.0002107126,0.0001597941,0.001152838,0.0003723034,0.0002302636,0.0004922018,0.0001430454,0.0001919487],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007147548,"about_ca_system_score_gemma":0.0004879848,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.07387748,"about_ca_topic_score_gemma":0.1067373,"domain_scores_codex":[0.999936,0.000005259298,0.000008618271,0.00002161758,0.00001417902,0.00001436018],"domain_scores_gemma":[0.9998915,0.0000095155,0.00002758905,0.000007883716,0.00003620285,0.00002729552],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001605028,0.00001903841,0.9635404,0.00004293286,0.00007685192,0.0003087828,0.001257334,0.0001784443,0.02590002,0.0000622513,0.00006558835,0.008387845],"study_design_scores_gemma":[0.00000193446,0.000005799604,0.9993825,0.000002756923,0.000005946357,0.00004079307,0.0001704549,0.00007867767,0.0001952019,0.000005296376,0.000109474,0.000001033271],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9994388,0.0001127437,0.00001302796,0.000007032039,0.000001202275,0.000001041618,0.0001019676,0.000001952874,0.0003222347],"genre_scores_gemma":[0.999455,0.00008728489,0.00003590623,0.000008032625,0.000001438652,0.000002748649,0.0002119218,0.000001694476,0.0001960022],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07387748,"threshold_uncertainty_score":0.1468949,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2059572788","doi":"10.1134/s0024490210060040","title":"Nature of the structural and crystal-chemical heterogeneity of the Mg-rich glauconite (Riphean, Anabar Uplift)","year":2010,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Clay minerals and soil interactions","field":"Materials Science","cited_by":36,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"Russian Academy of Sciences","keywords":"Glauconite; Electron microprobe; Geology; Chlorite; Octahedron; Structural formula; Riphean; Mineralogy; Crystallography; Mineral; Brucite; Platy; Mica; Chemistry; Crystal structure; Geochemistry; Materials science; Quartz; Sedimentary rock; Magnesium","authors":[{"name":"V. A. Drits","is_ca":false},{"name":"Т. А. Ivanovskaya","is_ca":false},{"name":"B. A. Sakharov","is_ca":false},{"name":"B. B. Zvyagina","is_ca":false},{"name":"Arkadiusz Derkowski","is_ca":true},{"name":"N. V. Gor’kova","is_ca":false},{"name":"E. V. Pokrovskaya","is_ca":false},{"name":"А. Т. Savichev","is_ca":false},{"name":"Т. S. Zaitseva","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005923570035614872,"gpt":0.2528015355256668,"spread":0.2468779654900519,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005461339,0.000161817,0.0001159313,0.0006276994,0.0002234008,0.0002291759,0.0001533004,0.0001282989,0.0006356115],"category_scores_gemma":[0.00009690422,0.0001178771,0.00007560474,0.0002548654,0.0002575228,0.0001248216,0.000164292,0.0001133817,0.0001305358],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001613711,"about_ca_system_score_gemma":0.0001265179,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004698589,"about_ca_topic_score_gemma":0.008689977,"domain_scores_codex":[0.9999349,0.000004699814,0.000004643523,0.00003012226,0.00001710333,0.000008577101],"domain_scores_gemma":[0.999943,0.000006483168,0.00001805606,0.00000506677,0.0000150783,0.00001238916],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.00008226267,0.0000169089,0.0482568,0.00006505589,0.00002784194,0.0002226383,0.0001323336,0.0001221749,0.9486237,0.00003771698,0.00002338644,0.002389274],"study_design_scores_gemma":[0.000004944681,0.00006232944,0.9757144,0.000003301104,0.00001488501,0.0003667615,0.0001125352,0.0002630346,0.02299549,0.00001975554,0.0004385309,0.000003995341],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9990819,0.0001518218,0.0001249341,0.000004823046,9.786753e-7,0.00000374995,0.0001942507,0.000006825316,0.0004307683],"genre_scores_gemma":[0.9990628,0.00006216308,0.0001559088,0.000006164365,0.000001984216,0.000003918477,0.0003675011,0.00000278922,0.0003367349],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.004698589,"threshold_uncertainty_score":0.009342432,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2799648086","doi":"10.1134/s0024490218030045","title":"Reef Formations in the West Canada Basin and Their Oil and Gas Potential","year":2018,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Reef; Geology; Devonian; Structural basin; Sedimentology; Paleontology; Extinction event; Mineral resource classification; Canada Basin; Oceanography; Geochemistry; Biological dispersal; Population","authors":[{"name":"V. G. Kuznetsov","is_ca":false},{"name":"Л. М. Журавлева","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.007606523189309066,"gpt":0.19123116213716,"spread":0.1836246389478509,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001444278,0.000217673,0.000178196,0.00275671,0.001982149,0.001482809,0.0004369317,0.0001755782,0.002696798],"category_scores_gemma":[0.0005891507,0.0002136448,0.0001521991,0.00422478,0.0009428764,0.0003979412,0.0008224424,0.0002337874,0.0001964473],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.01562796,"about_ca_system_score_gemma":0.01252127,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9919071,"about_ca_topic_score_gemma":0.9981453,"domain_scores_codex":[0.9997632,0.000008767439,0.000008083392,0.00003094198,0.0000619092,0.0001271163],"domain_scores_gemma":[0.9996947,0.00001295426,0.00005461473,0.000008811623,0.0001279328,0.0001009773],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001136824,0.00002095662,0.947999,0.00006917423,0.00005836643,0.000481872,0.003987085,0.0005313432,0.001741934,0.003187693,0.001754041,0.04005491],"study_design_scores_gemma":[0.000001935759,0.000004707469,0.9919277,0.00002241811,0.000008330238,0.000109741,0.002648778,0.0002153195,0.0001316725,0.0001122766,0.004810394,0.000006726786],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9912412,0.001022828,0.00007933914,0.0001638026,0.000003434271,0.000008805301,0.001415095,0.00001173802,0.00605377],"genre_scores_gemma":[0.9961325,0.0006291623,0.0001534821,0.00001821388,0.00000110941,0.000003789669,0.0005761657,0.000004618116,0.002481089],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01562796,"threshold_uncertainty_score":0.1133893,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4383535224","doi":"10.1134/s002449022370013x","title":"The Application of Various Mineral Prospectivity Modeling in the Exploration of Orogenic Gold Deposit in Saqez-Sardasht Region, Northwest Iran","year":2023,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":4,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of New Brunswick","funders":"","keywords":"Prospectivity mapping; Geology; Mineral exploration; Geochemistry; Mineral resource classification; Tectonics; Mining engineering; Mineralogy; Geomorphology; Seismology; Structural basin","authors":[{"name":"Farzaneh Mami Khalifani","is_ca":true},{"name":"Ali Imamalipour","is_ca":false},{"name":"Samaneh Barak","is_ca":false},{"name":"Maysam Abedi","is_ca":false},{"name":"Golnaz Jozanikohan","is_ca":false},{"name":"Abbas Bahroudi","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03080748015400505,"gpt":0.2440457525222132,"spread":0.2132382723682082,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003738747,0.0003707644,0.0002260504,0.001139718,0.0002480427,0.0004973633,0.0003853627,0.0002908857,0.0002766317],"category_scores_gemma":[0.0004943763,0.0001795732,0.0004824164,0.0006074682,0.0001532859,0.0002708002,0.0002485441,0.0001525408,0.00005508429],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0006654096,"about_ca_system_score_gemma":0.0006196352,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.04297683,"about_ca_topic_score_gemma":0.03843042,"domain_scores_codex":[0.9998965,0.00002325089,0.000007017014,0.00002633084,0.00002727304,0.00001961096],"domain_scores_gemma":[0.999915,0.00002908694,0.00001849335,0.000006090162,0.00002499058,0.000006249181],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0002398589,0.000148235,0.2999052,0.000135334,0.0001728728,0.0006470938,0.0005337099,0.6106002,0.01838726,0.0007154296,0.0002789194,0.06823599],"study_design_scores_gemma":[0.00001603633,0.00007166094,0.1172505,0.00001228796,0.00004695235,0.0001000916,0.0005425405,0.8774216,0.003804362,0.0004114543,0.000303986,0.00001849084],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9957637,0.00004490621,0.003631689,0.00003250559,0.000001600457,0.00001190489,0.00005430905,0.00002640912,0.0004330251],"genre_scores_gemma":[0.997054,0.00003239208,0.00276672,0.000002200053,8.618064e-7,0.000004550204,0.00003539164,0.000001555561,0.000102475],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04297683,"threshold_uncertainty_score":0.08545333,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4366135923","doi":"10.1134/s0024490222700055","title":"C and O Isotope Composition of the Neoproterozoic Pre-, Syn-, and Postglacial Carbonates: Evidence from the Longdor Uplift and Western Slope of the Aldan Shield, Southern Siberian Platform","year":2023,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Carbonate; Dolomite; Glacial period; Geochemistry; Calcite; Paleontology; Facies; Carbonate minerals; Isotopes of carbon; Loess; δ18O; Stable isotope ratio; Isotope; Structural basin; Chemistry","authors":[{"name":"A. V. Shatsillo","is_ca":false},{"name":"S. V. Rud’ko","is_ca":false},{"name":"И. В. Латышева","is_ca":false},{"name":"B. G. Pokrovsky","is_ca":false},{"name":"D. V. Rud’ko","is_ca":false},{"name":"I. V. Fedyukin","is_ca":false},{"name":"А. Б. Кузнецов","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01703567890186279,"gpt":0.2234835931782427,"spread":0.2064479142763799,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001256835,0.0002028962,0.0001644416,0.001013787,0.0005487768,0.0003825622,0.0001750564,0.0001492966,0.001009611],"category_scores_gemma":[0.0001460209,0.000143528,0.0001150745,0.0008557604,0.0003235487,0.0001871304,0.0003281748,0.0001244375,0.0001805088],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0003854186,"about_ca_system_score_gemma":0.0002783662,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.03540812,"about_ca_topic_score_gemma":0.05724123,"domain_scores_codex":[0.9999448,0.000005342401,0.000004740993,0.00001555384,0.00001531941,0.00001409346],"domain_scores_gemma":[0.9999144,0.000007251288,0.00001920227,0.000007419511,0.00002662163,0.00002508466],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002188405,0.00002895741,0.9389382,0.00003525271,0.00005924937,0.0002790886,0.0008849977,0.0001019377,0.05172139,0.00005815173,0.00006141578,0.007612463],"study_design_scores_gemma":[0.000001597696,0.000008835899,0.9992581,0.000001875874,0.000004305781,0.00003556361,0.0001382498,0.00005174055,0.0003679496,0.000007008208,0.0001240089,7.797851e-7],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9992961,0.0001171374,0.0000191106,0.000005473765,0.000001476158,0.000001007369,0.0001134462,0.000001438104,0.0004448319],"genre_scores_gemma":[0.9993704,0.00009579644,0.00003751475,0.000006509935,0.000001704039,0.000002140016,0.0002772245,0.000001395044,0.0002074368],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03540812,"threshold_uncertainty_score":0.07040405,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2788827493","doi":"10.1134/s0024490218010054","title":"Carbon, oxygen, and sulfur isotope compositions and model of the Silurian rock formation in northwestern Belarus","year":2018,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Carbonate; Gypsum; Geochemistry; Lithification; Abiogenic petroleum origin; Carbonate rock; Tufa; Clastic rock; Evaporite; Paleontology; Anhydrite; Calcite; Red beds; Supralittoral zone; Sedimentary rock; Methane; Intertidal zone; Oceanography","authors":[{"name":"А. А. Махнач","is_ca":false},{"name":"С. А. Кручек","is_ca":false},{"name":"B. G. Pokrovsky","is_ca":false},{"name":"Galina STRELTSOVA","is_ca":false},{"name":"О. V. Murashko","is_ca":false},{"name":"О. Л. Петров","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01485404491020275,"gpt":0.2253074203883613,"spread":0.2104533754781585,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008793471,0.0001397208,0.0001383902,0.0009013171,0.0004454791,0.0004181498,0.0003331692,0.0001127443,0.0009215284],"category_scores_gemma":[0.000135492,0.0001367412,0.0002258305,0.0004268043,0.0003549131,0.0002010038,0.0002336608,0.00008131576,0.0001339322],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001703237,"about_ca_system_score_gemma":0.0005472988,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.134236,"about_ca_topic_score_gemma":0.1515724,"domain_scores_codex":[0.9999354,0.000006185887,0.000003556849,0.00002014408,0.00001076358,0.00002397255],"domain_scores_gemma":[0.9999647,0.000003801644,0.00001229752,0.000003214742,0.000008705652,0.000007233819],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001487596,0.00005279367,0.9075507,0.00008709719,0.00008683294,0.0007595987,0.001221054,0.04884563,0.01811177,0.001773667,0.0004835137,0.02087871],"study_design_scores_gemma":[0.00001129544,0.00004756207,0.9827696,0.00001066892,0.00002047672,0.0001160578,0.0005962742,0.01455726,0.0004674692,0.0001870931,0.00120909,0.000007134736],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9987294,0.00008553173,0.0002635699,0.00001936982,0.000001382874,0.000002711218,0.0001561947,0.00002403041,0.0007177288],"genre_scores_gemma":[0.9996331,0.00002243344,0.00009362978,0.000002122531,7.974063e-7,0.000001258494,0.00009585801,0.000002809948,0.0001480123],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.134236,"threshold_uncertainty_score":0.2669093,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3084789262","doi":"10.1134/s0024490220040045","title":"Facies Structure and Quantitative Parameters of Pleistocene Sedimentation on the Deep-Sea Floor of the Southern Pacific Ocean and in the Scotia Sea","year":2020,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Terrigenous sediment; Geology; Oceanography; Pleistocene; Sedimentology; Facies; Sedimentation; Peninsula; Holocene; Nova scotia; Sediment; Structural basin; Paleontology; Archaeology","authors":[{"name":"M. A. Levitan","is_ca":false},{"name":"T. N. Gelvi","is_ca":false},{"name":"L. G. Domaratskaya","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02383890129465356,"gpt":0.2391810839593668,"spread":0.2153421826647132,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001335225,0.0001848686,0.00008512932,0.001458937,0.0002059224,0.0003399061,0.000110112,0.0001068568,0.0008888739],"category_scores_gemma":[0.0004319361,0.000166888,0.0001614122,0.0009369543,0.0003604354,0.0001206877,0.0002635618,0.0000930513,0.0001226947],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007058393,"about_ca_system_score_gemma":0.0004337016,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.2044763,"about_ca_topic_score_gemma":0.319133,"domain_scores_codex":[0.9999511,0.000005759222,0.000005026719,0.00001524844,0.000007954635,0.00001489858],"domain_scores_gemma":[0.999699,0.00004165251,0.0001027553,0.00002190186,0.00007019245,0.00006456448],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000606634,0.000004277088,0.9954736,0.00001055167,0.00003240226,0.00008096924,0.0001651103,0.0003425649,0.002011565,0.00005546147,0.00005916891,0.001703725],"study_design_scores_gemma":[6.6665e-7,0.000001789787,0.9998227,0.000001040648,0.000001552546,0.00001317295,0.00003131951,0.00007525193,0.00002172394,0.00000420021,0.00002605928,5.013595e-7],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.999178,0.00006324113,0.00002116826,0.000004561611,6.843503e-7,0.000001489099,0.0003596198,0.000002495084,0.0003686816],"genre_scores_gemma":[0.999504,0.00002925226,0.00002284933,0.000001385292,5.628034e-7,0.000001093957,0.0003041822,8.846586e-7,0.0001357503],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2044763,"threshold_uncertainty_score":0.4065721,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2012222568","doi":"10.1134/s0024490210040024","title":"Behavior of kimberlite indicator minerals during the formation of mechanical dispersion halos in glacial settings","year":2010,"lang":"en","type":"article","venue":"Lithology and Mineral Resources","topic":"Geotechnical and Geomechanical Engineering","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Kimberlite; Glacial period; Glacier; Dispersion (optics); Clay minerals; Halo; Geochemistry; Sedimentology; Craton; Mineralogy; Earth science; Geomorphology; Paleontology; Tectonics","authors":[{"name":"N. P. Pokhilenko","is_ca":false},{"name":"В. П. Афанасьев","is_ca":false},{"name":"Mikhail Vavilov","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.003462572957653632,"gpt":0.1933577123828165,"spread":0.1898951394251629,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001322952,0.0001480105,0.0001589416,0.001257504,0.0004847391,0.0004634495,0.0002068672,0.000150708,0.000566052],"category_scores_gemma":[0.0003972428,0.0001697691,0.0001069242,0.0004260202,0.0005315689,0.0001600178,0.0003115144,0.0001600579,0.0000989622],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000461942,"about_ca_system_score_gemma":0.0002807822,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01816248,"about_ca_topic_score_gemma":0.03474649,"domain_scores_codex":[0.9999024,0.000005621862,0.000004741452,0.00002420811,0.00003541087,0.00002768183],"domain_scores_gemma":[0.9997208,0.00002806676,0.00007563001,0.00001223022,0.00008283186,0.00008040844],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0007302041,0.0000568916,0.4003366,0.00007543311,0.00003712075,0.0006644102,0.001992854,0.0002984733,0.5888132,0.0001524901,0.00008508506,0.006757147],"study_design_scores_gemma":[0.000005076117,0.000119475,0.9644725,0.000004778892,0.00001156146,0.0001682556,0.0006512023,0.0003678734,0.03372206,0.00002068205,0.0004494288,0.00000702538],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9994518,0.00004549758,0.00007075625,0.000002797975,6.616015e-7,0.000002585662,0.00005296215,0.000004254101,0.0003685754],"genre_scores_gemma":[0.9993987,0.00003334639,0.0001415532,0.000002767611,7.161155e-7,0.00000274601,0.00007856512,0.00000361586,0.0003378976],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01816248,"threshold_uncertainty_score":0.03611356,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}