{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":10,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":10,"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":"87e109afbbc5","filters":{"venue":"Ofioliti"}},"results":[{"id":"W2794524394","doi":"10.4454/ofioliti.v43i1.505","title":"First occurrences of Ni-phosphides in chromitites from the ophiolite complexes of Alapaevsk, Russia and Gerakini-Ormylia, Greece","year":2018,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"SGS (Canada)","funders":"","keywords":"Ophiolite; Chromite; Phosphide; Peridotite; Olivine; Electron microprobe; Geology; Chromitite; Geochemistry; Mineralogy; Nickel; Mantle (geology); Materials science; Metallurgy","authors":[{"name":"Alkiviadis Sideridis","is_ca":false},{"name":"Federica Zaccarini","is_ca":false},{"name":"Tassos Grammatikopoulos","is_ca":true},{"name":"Pavlos Tsitsanis","is_ca":false},{"name":"Basilios Tsikouras","is_ca":false},{"name":"E. V. Pushkarev","is_ca":false},{"name":"Giorgio Garuti","is_ca":false},{"name":"Konstantin Hatzipanagiotou","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01594366380655007,"gpt":0.2071966362982454,"spread":0.1912529724916954,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001773824,0.0001201827,0.0003085744,0.00003601039,0.00008004071,0.00001765582,0.0002800263,0.00005631861,0.005138999],"category_scores_gemma":[0.0001365185,0.00006131473,0.00006380961,0.0002522868,0.0008524974,0.00008565665,0.0000385842,0.00008719249,0.00003457176],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001177232,"about_ca_system_score_gemma":0.00001582052,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.05096476,"about_ca_topic_score_gemma":0.02884174,"domain_scores_codex":[0.9990027,0.00005407749,0.0003248157,0.0002248992,0.0001675936,0.0002259438],"domain_scores_gemma":[0.9989275,0.0006545175,0.000128136,0.0001702189,0.00005147651,0.00006818178],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002904348,0.00001802996,0.9957619,0.00001701753,0.00002195326,0.00000150425,0.0002403048,0.00001487354,0.0001773158,0.0004829659,0.0002805643,0.002954479],"study_design_scores_gemma":[0.0001422362,0.0001080389,0.9457564,0.00005770362,0.00001873506,0.000001323762,0.0001427061,0.001079586,0.001883981,0.04964239,0.001073845,0.00009302281],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9935938,0.002022291,0.000002249526,0.000701824,0.00005248286,0.00006229656,0.0004440662,0.000007586426,0.003113477],"genre_scores_gemma":[0.9990113,0.0002388642,0.0003655737,0.0001731852,0.00009943674,7.875299e-7,0.0000807527,0.000001023458,0.00002910235],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05000552,"threshold_uncertainty_score":0.9957705,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1548043353","doi":"10.4454/ofioliti.v26i2a.143","title":"NEOGENE TUSCAN SHELF-WESTERN TUSCANY EXTENSION EVIDENCES OF THE EARLY POST-COMPRESSIONAL DEPOSITS (TYRRHENIAN SEA- NORTHERN APENNINES, ITALY)","year":2001,"lang":"en","type":"article","venue":"Ofioliti","topic":"Maritime and Coastal Archaeology","field":"Arts and Humanities","cited_by":8,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Guelph","funders":"","keywords":"Geology; Neogene; Rift; Paleontology; Structural basin; Half-graben; Sedimentary rock; Graben; Sedimentary basin; Evaporite; Tectonics; Unconformity","authors":[{"name":"Vincenzo Pascucci","is_ca":false},{"name":"Gianfranco Fontanesi","is_ca":false},{"name":"Saverio Merlini","is_ca":false},{"name":"Ivan Martini","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02032661575802112,"gpt":0.2159651644839101,"spread":0.195638548725889,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001030213,0.0002144937,0.0002804064,0.00007502131,0.0003613999,0.00005773979,0.0004624248,0.00006413198,0.001398113],"category_scores_gemma":[0.00002876776,0.000141126,0.000178653,0.00005975227,0.0005146927,0.0002300995,0.0003515613,0.0001581289,0.00009453993],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001738462,"about_ca_system_score_gemma":0.00008150665,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01097116,"about_ca_topic_score_gemma":0.05619766,"domain_scores_codex":[0.9984729,0.0001222407,0.0003586174,0.0003077009,0.0003458039,0.0003927399],"domain_scores_gemma":[0.9989406,0.0001088569,0.0001555552,0.0003859045,0.0002977572,0.0001113196],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003668423,0.0003166962,0.8953785,0.0001026175,0.0001494168,0.0001102971,0.0157224,0.00002316063,0.005767671,0.0242552,0.000666689,0.05714049],"study_design_scores_gemma":[0.0006983912,0.0005535882,0.9074249,0.0004483447,0.0001002052,0.0001757946,0.001379656,0.000102068,0.002333186,0.004377575,0.08184106,0.0005652313],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9737692,0.0007916322,0.000004152527,0.001554361,0.0003853372,0.0002002212,0.0000533126,0.0000443182,0.02319747],"genre_scores_gemma":[0.9831076,0.00004305055,0.00002738413,0.0006777683,0.0005024888,0.00001627477,0.0000233985,0.00002445037,0.01557758],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08117437,"threshold_uncertainty_score":0.9995148,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1934787481","doi":"10.4454/ofioliti.v30i2.322","title":"TRACE ELEMENT GEOCHEMISTRY OF MANTLE OLIVINE AND ITS APPLICATION TO GEOTHERMOMETRY","year":2005,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","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; Geochemistry; Olivine; Mantle (geology); Trace element; Petrology","authors":[{"name":"Jan C.M. De Hoog","is_ca":false},{"name":"Louise Gall","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.007022510522021243,"gpt":0.2002823275227943,"spread":0.1932598170007731,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009005826,0.00006559222,0.000115214,0.00002645735,0.00002624125,0.000005155109,0.00009026332,0.00003423699,0.007222211],"category_scores_gemma":[0.00002605861,0.00004941215,0.00003021873,0.000135271,0.00002066729,0.00003056521,0.00001224851,0.00004101489,0.0001834138],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001684508,"about_ca_system_score_gemma":0.000004054204,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0003483178,"about_ca_topic_score_gemma":0.000236566,"domain_scores_codex":[0.9994282,0.000009060231,0.000137135,0.0001634333,0.0001078889,0.0001543441],"domain_scores_gemma":[0.9996947,0.00003876926,0.00003585451,0.00008819057,0.0000267257,0.0001157427],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008094687,0.0001870029,0.5204911,0.0001727518,0.00008109995,0.000003379249,0.0001717581,0.003630126,0.1397541,0.0008568264,0.0009124958,0.3336584],"study_design_scores_gemma":[0.0002207823,0.00009844443,0.8047865,0.00001393898,0.00003334853,0.000007144898,0.00007147952,0.02359552,0.1499874,0.003006298,0.01795299,0.0002261157],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9889759,0.0007501687,0.00008467743,0.001124021,0.000005355868,0.0000630972,0.00005097175,0.00001122745,0.008934542],"genre_scores_gemma":[0.9986589,0.00003736576,0.0004592918,0.0002341327,0.00006921082,0.000001669081,0.00003854791,8.6879e-7,0.0005000216],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3334323,"threshold_uncertainty_score":0.9936853,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1504099847","doi":"10.4454/ofioliti.v26i2b.163","title":"GEOCHEMISTRY OF OPHIOLITIC BASALTS FROM THE METCHOSIN IGNEOUS COMPLEX ON SOUTHERN VANCOUVER ISLAND, AND THEIR INFERRED PALEOTECTONIC SETTING","year":2001,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":1,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Université Laval","funders":"","keywords":"Igneous rock; Ophiolite; Geology; Basalt; Geochemistry; Volcanic rock; Ultramafic rock; Large igneous province; Continental margin; Rift; Mantle (geology); Trace element; Plate tectonics; Volcano; Tectonics; Paleontology; Magmatism","authors":[{"name":"Marc Constantin","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01581891021475563,"gpt":0.2086856147288401,"spread":0.1928667045140845,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002612058,0.0002152252,0.0002525091,0.00001969132,0.0001598725,0.00005675832,0.0006561551,0.0001020447,0.0001737855],"category_scores_gemma":[0.0002147998,0.0001444838,0.00008148932,0.0001371786,0.000125294,0.00006146463,0.0002478302,0.0002158419,0.00001480505],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000192028,"about_ca_system_score_gemma":0.0000483548,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002430088,"about_ca_topic_score_gemma":0.0001233009,"domain_scores_codex":[0.9986718,0.00009219431,0.0002738144,0.0004148044,0.000163403,0.0003840358],"domain_scores_gemma":[0.9983003,0.0006656075,0.0001559232,0.0007073173,0.00008490279,0.00008592728],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","study_design_scores_codex":[0.0007206495,0.001763234,0.1214721,0.001290753,0.001676637,0.000904246,0.06584563,0.007164315,0.4426881,0.02378962,0.09023529,0.2424494],"study_design_scores_gemma":[0.00691943,0.0006993325,0.07591733,0.001705186,0.0001349606,0.000602,0.01155412,0.2616637,0.1542595,0.3371868,0.1459884,0.003369319],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.940142,0.0003217183,0.00462319,0.002193015,0.0001663665,0.0001786291,0.0001183573,0.0001116778,0.05214504],"genre_scores_gemma":[0.9980101,0.00001494281,0.0004659947,0.0005812408,0.0001347575,0.000008356014,0.00001777319,0.000004979209,0.0007618695],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3133971,"threshold_uncertainty_score":0.5891877,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3163806503","doi":"10.4454/ofioliti.v46i2.542","title":"CORUNDUM-BEARING VEINS IN CHLORITITE FROM THE ETIROL-LEVAZ AUSTROALPINE CONTINENTAL SLICE (VALTOURNENCHE, AOSTA, ITALY)","year":2021,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geochemistry; Metamorphism; Metamorphic facies; Greenschist; Igneous rock; Eclogite; Ultramafic rock; Omphacite; Recrystallization (geology); Petrology; Facies; Geomorphology; Paleontology","authors":[{"name":"Roberto Compagnoni","is_ca":false},{"name":"Roberto Cossio","is_ca":false},{"name":"Daniele Regis","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01661342913690948,"gpt":0.2011453092695246,"spread":0.1845318801326152,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001838702,0.0001595506,0.0002671634,0.00002850943,0.000123522,0.00008266004,0.000340823,0.00009186675,0.01791625],"category_scores_gemma":[0.0002939321,0.0001061339,0.0001404437,0.0003818787,0.0001144649,0.0001157047,0.00008518482,0.0003366671,0.0004439861],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006448966,"about_ca_system_score_gemma":0.00003323931,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.02833918,"about_ca_topic_score_gemma":0.0239936,"domain_scores_codex":[0.9985412,0.00009497506,0.0002836183,0.000378062,0.0002576448,0.0004444468],"domain_scores_gemma":[0.9990906,0.0003669676,0.00005858143,0.0002820752,0.00005158903,0.0001502208],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002911405,0.00007488189,0.9919331,0.000006360802,0.00004221666,0.0001594685,0.00009917852,0.0001943204,0.001484145,0.000204682,0.0008058948,0.004966645],"study_design_scores_gemma":[0.0003903902,0.00004164913,0.9789768,0.00002717176,0.00003100297,0.00001191981,0.00045906,0.001554184,0.002198012,0.006026808,0.01010225,0.0001807657],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9776081,0.001463685,0.00000911437,0.004564932,0.0001434189,0.00006086113,0.0002259285,0.00002725404,0.01589671],"genre_scores_gemma":[0.99628,0.0001343414,0.0002061426,0.001311059,0.0002955429,0.000001610543,0.0007606618,0.000002596872,0.001008062],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01867189,"threshold_uncertainty_score":0.993816,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1585295534","doi":"10.4454/ofioliti.v30i2.277","title":"EXPERIMENTAL HYDROUS PARTIAL MELTING OF HARZBURGITE AT SHALLOW PRESSURES: IMPLICATIONS ON HYDROUS LATE-STAGE MAGMATIC PROCESSES WITHIN THE MANTLE/CRUST TRANSITION OF THE OCEANIC LITHOSPHERE","year":2005,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Ophiolite; Geology; Partial melting; Geochemistry; Mantle (geology); Lithosphere; Oceanic crust; Solidus; Mid-ocean ridge; Peridotite; Crust; Mineral redox buffer; Petrology; Subduction; Tectonics","authors":[{"name":"Jürgen Koepke","is_ca":false},{"name":"Sandrin T. Feig","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01423065569089699,"gpt":0.2123524745218198,"spread":0.1981218188309228,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001628109,0.0001401394,0.0002122525,0.00001513293,0.0002117082,0.000017288,0.0003282887,0.00006073382,0.003101603],"category_scores_gemma":[0.00006385842,0.00007213846,0.000131951,0.0002290524,0.000201515,0.00009038212,0.00002544397,0.0001173127,0.00004683254],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006282269,"about_ca_system_score_gemma":0.00002686684,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00081401,"about_ca_topic_score_gemma":0.001213666,"domain_scores_codex":[0.9988376,0.0000869285,0.0003648932,0.0002281477,0.0002598243,0.0002226176],"domain_scores_gemma":[0.9992189,0.0001883541,0.0002147756,0.0002685911,0.00004532511,0.00006398869],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0007940746,0.001433505,0.3269237,0.001166588,0.0005966271,0.00001427708,0.01435219,0.5836535,0.0596328,0.003385631,0.0006250789,0.007422062],"study_design_scores_gemma":[0.001059872,0.0005614774,0.2978552,0.0003232507,0.0003914301,0.00002477969,0.002034999,0.1275105,0.5621181,0.005278646,0.002189904,0.0006518172],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9916757,0.0009761017,0.00001069781,0.001095054,0.0000246963,0.0002094642,0.0001530039,0.00002081123,0.00583442],"genre_scores_gemma":[0.9989085,0.00001652421,0.00009134184,0.0003124801,0.00005485739,0.000006114445,0.0000544715,0.000003235135,0.0005524762],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5024853,"threshold_uncertainty_score":0.9978097,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1608112513","doi":"10.4454/ofioliti.v30i2.294","title":"A RE-OS ISOTOPE STUDY OF KIMBERLITE DERIVED PERIDOTITE XENOLITHS FROM FINLAND: CONSTRAINTS FOR THE ORIGIN OF LAYERED CONTINENTAL MANTLE","year":2005,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Craton; Kimberlite; Geochemistry; Xenolith; Peridotite; Mantle (geology); Archean; Metasomatism; Lithosphere; Paleontology; Tectonics","authors":[{"name":"P. Peltonen","is_ca":false},{"name":"Gerhard Brügmann","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02218521916109934,"gpt":0.2329388831066254,"spread":0.210753663945526,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001559553,0.0001184642,0.0003158335,0.00002595528,0.00007167079,0.00001343891,0.0002376681,0.00004664306,0.01364259],"category_scores_gemma":[0.00006860042,0.00006813844,0.0001318042,0.0001022397,0.0002004634,0.00004805017,0.00001950281,0.00008003622,0.00004739971],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002025218,"about_ca_system_score_gemma":0.00001880967,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.007238347,"about_ca_topic_score_gemma":0.005609915,"domain_scores_codex":[0.998998,0.00005903609,0.000330047,0.0002176345,0.0001700268,0.000225284],"domain_scores_gemma":[0.9990214,0.0005063851,0.0001323421,0.0001954509,0.00007011842,0.00007426836],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001861165,0.000230056,0.9811498,0.00001613955,0.0002038339,0.000003325815,0.000766049,0.0006023676,0.001805177,0.00008337276,0.000248984,0.0147048],"study_design_scores_gemma":[0.001592901,0.0003570577,0.9769086,0.00001718524,0.0001266079,0.000001674056,0.00311759,0.009602891,0.003102599,0.001606832,0.003402987,0.0001630558],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9940795,0.0002646311,0.00006671016,0.0004531681,0.00004537302,0.0003221906,0.0006749797,0.000009043079,0.004084459],"genre_scores_gemma":[0.9985438,0.00001884147,0.0008389997,0.0001436449,0.00009510136,0.000005228488,0.00009977767,0.000001851595,0.0002527311],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01454175,"threshold_uncertainty_score":0.9993725,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1575318919","doi":"10.4454/ofioliti.v30i2.296","title":"THE COMPOSITE MANTLE EVOLUTION OF THE ERRO-TOBBIO PERIDOTITE (VOLTRI MASSIF, LIGURIA ALPS, ITALY)","year":2005,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University","funders":"","keywords":"Peridotite; Geology; Geochemistry; Mylonite; Massif; Mantle (geology); Shear zone; Tectonite; Lithosphere; Spinel; Olivine; Protolith; Petrology; Metamorphic rock; Seismology; Tectonics; Paleontology","authors":[{"name":"Giovanni B. Piccardo","is_ca":false},{"name":"Eugenio Poggi","is_ca":false},{"name":"Franco Marco Elter","is_ca":false},{"name":"Reinoud L.M. Vissers","is_ca":false},{"name":"G. Ranalli","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006048505862397111,"gpt":0.1722515834324458,"spread":0.1662030775700487,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001895063,0.0001067828,0.0001474423,0.00002036354,0.00028198,0.0000322034,0.0003887336,0.00005714177,0.002443025],"category_scores_gemma":[0.00005796188,0.00004907379,0.0001783598,0.0002390211,0.0002432599,0.00007346194,0.0000358184,0.0001282826,0.0003357111],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000874437,"about_ca_system_score_gemma":0.00002235723,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001876323,"about_ca_topic_score_gemma":0.00303912,"domain_scores_codex":[0.9989902,0.00007830519,0.0002262221,0.0001768359,0.0002409564,0.0002874979],"domain_scores_gemma":[0.9993689,0.0001443063,0.00009303148,0.0002597994,0.00005556898,0.00007838671],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006360674,0.00006068968,0.9662874,0.0000168781,0.00008430487,0.000002404541,0.00008604288,0.00201545,0.004826022,0.003988122,0.004379943,0.01818911],"study_design_scores_gemma":[0.0001330978,0.00003689171,0.9228718,0.00001159061,0.00004218909,0.000006328991,0.00008325862,0.005988922,0.002914345,0.01103067,0.05676305,0.0001178874],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9571955,0.001980988,0.0000192258,0.005913003,0.00013674,0.0000840955,0.00005959034,0.00002002877,0.03459087],"genre_scores_gemma":[0.9967591,0.00005686959,0.0001501239,0.0002450338,0.0001599613,7.999886e-7,0.00002697794,0.000001384886,0.002599742],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0523831,"threshold_uncertainty_score":0.9984689,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2112888976","doi":"10.4454/ofioliti.v30i2.302","title":"SOFTENING OF THE SUBCONTINENTAL LITHOSPHERIC MANTLE BY ASTHENOSPHERE MELTS AND THE CONTINENTAL EXTENSION/ OCEANIC SPREADING TRANSITION","year":2005,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Asthenosphere; Geochemistry; Peridotite; Mantle (geology); Lithosphere; Basalt; Partial melting; Oceanic crust; Transition zone; Petrology; Subduction; Paleontology; Tectonics","authors":[{"name":"G. Ranalli","is_ca":true},{"name":"Giovanni B. Piccardo","is_ca":false},{"name":"Pedro Corona-Chávez","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.003835103205607457,"gpt":0.1602886661018728,"spread":0.1564535628962653,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001753176,0.000104608,0.0001907487,0.000005365374,0.0001498034,0.00002209376,0.0001506598,0.00004236104,0.002568166],"category_scores_gemma":[0.00003660728,0.00004899273,0.0001255137,0.0001231036,0.0002686519,0.00008184023,0.0000186208,0.0001101442,0.00002609195],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000182063,"about_ca_system_score_gemma":0.000004195093,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001393511,"about_ca_topic_score_gemma":0.0003390893,"domain_scores_codex":[0.9991808,0.00007653436,0.0001999892,0.0001792997,0.0001613353,0.0002020615],"domain_scores_gemma":[0.9995829,0.0001413361,0.00007814913,0.0001150341,0.00002459276,0.00005799704],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0007365491,0.0001864795,0.8582673,0.00008050382,0.0002410011,0.00001027512,0.002159029,0.00112767,0.0195161,0.003049572,0.003857984,0.1107675],"study_design_scores_gemma":[0.001954348,0.00008667151,0.934699,0.00006875283,0.0001704252,0.00006439465,0.001133322,0.0385136,0.01261647,0.007102113,0.003294463,0.0002964337],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9913027,0.002261997,0.00003843183,0.002305872,0.00003726355,0.00009195616,0.00003668585,0.0000139851,0.003911156],"genre_scores_gemma":[0.9987091,0.0000628621,0.0002110943,0.000535501,0.00005998618,6.26061e-7,0.0000311028,0.000001841139,0.0003879222],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1104711,"threshold_uncertainty_score":0.9983436,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1503138264","doi":"10.4454/ofioliti.v30i2.313","title":"THE ROLE OF DUNITES FOR EXTRACTION OF MELTS FROM THE MANTLE TO THE OCEANIC CRUST","year":2005,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Peridotite; Geology; Mantle (geology); Geochemistry; Olivine; Crust; Overprinting; Oceanic crust; Petrology; Metamorphic rock; Subduction; Tectonics; Seismology","authors":[{"name":"Guenter Suhr","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009965041470786041,"gpt":0.2049472008625454,"spread":0.1949821593917593,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001977387,0.00005062119,0.00008507431,0.000007567307,0.0001371657,0.00001300973,0.0002618735,0.0000250315,0.001547628],"category_scores_gemma":[0.0001615873,0.0000188258,0.00008300078,0.000104268,0.00006902792,0.00003116967,0.00001209235,0.00005227812,0.00008540601],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001074323,"about_ca_system_score_gemma":0.000007942956,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00431403,"about_ca_topic_score_gemma":0.005303884,"domain_scores_codex":[0.9994844,0.00003812174,0.0001434558,0.00008902864,0.0001120143,0.0001329893],"domain_scores_gemma":[0.9986617,0.001028717,0.00006151389,0.0001589488,0.00005612453,0.00003299806],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0005232884,0.0001533133,0.4304352,0.00001714458,0.0003224353,7.542183e-7,0.001196078,0.006945295,0.0116044,0.0225079,0.02394927,0.5023449],"study_design_scores_gemma":[0.0001073616,0.00009200362,0.5654248,0.000008364791,0.00006315917,0.000001063016,0.001522219,0.008343688,0.02079821,0.08792153,0.3156368,0.00008076916],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9776502,0.00241391,0.00003165752,0.01044631,0.00004288859,0.0001308779,0.0002115401,0.000006140124,0.009066456],"genre_scores_gemma":[0.9988338,0.00005644785,0.000202771,0.0004305836,0.0001519684,0.000001532607,0.00003441036,7.317315e-7,0.0002877527],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5022641,"threshold_uncertainty_score":0.9993651,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}