{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":110,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":110,"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"},"query_hash":"7af568683d47","filters":{"venue":"Gondwana Research"}},"results":[{"id":"W2026638428","doi":"10.1016/j.gr.2012.12.026","title":"The supercontinent cycle: A retrospective essay","year":2013,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":735,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Supercontinent; Geology; Continental drift; Rodinia; Paleontology; Plate tectonics; Tectonics; Earth science; Orogeny; Phanerozoic; Breakup; Astrobiology; Craton; Cenozoic","retraction":null,"screen_n_in":null,"score":{"opus":0.02447912993237691,"gpt":0.2659008105247413,"spread":0.2414216805923644,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001105057,0.00008847148,0.0001288088,0.00005685924,0.0006847902,0.0002572259,0.0004983416,0.00005512581,0.04555677],"category_scores_gemma":[0.0006272361,0.00004322668,0.00008480773,0.000677283,0.0004282721,0.0001421498,0.00005942106,0.0004530278,0.007186276],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001087696,"about_ca_system_score_gemma":0.00004016597,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.03120487,"about_ca_topic_score_gemma":0.009514679,"domain_scores_codex":[0.9979568,0.0002393747,0.0001598487,0.0002963737,0.0006731935,0.0006743707],"domain_scores_gemma":[0.9985712,0.000569881,0.00001710485,0.0002927297,0.0003427596,0.0002063697],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001958562,0.00002900246,0.8899097,0.000004380521,0.00004487917,0.00001041304,0.0001153031,0.00003322704,0.0004416942,0.001174954,0.01851953,0.0896973],"study_design_scores_gemma":[0.00008224187,0.00007744518,0.8681467,0.000002491429,0.000003297089,0.00000220132,0.0003133283,0.005653537,0.0001804025,0.1159371,0.009521622,0.00007968429],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8984852,0.0007901005,0.000005424602,0.0111817,0.00005137941,0.0001919894,0.000009479556,0.00002794668,0.0892568],"genre_scores_gemma":[0.9949572,0.0001284167,0.00007115288,0.0001124892,0.0001072326,0.000010753,0.00001882469,0.000001528469,0.004592422],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1147621,"threshold_uncertainty_score":0.9935867,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2062168342","doi":"10.1016/j.gr.2009.08.001","title":"Evolution of the Rheic Ocean","year":2009,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":648,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Gondwana; Geology; Paleontology; Laurentia; Paleozoic; Pangaea; Terrane; Devonian; Baltica; Fibrous joint; Ordovician; Orogeny; Carboniferous; Passive margin; Rift; Subduction; Permian; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.03835834361532416,"gpt":0.2757826268680039,"spread":0.2374242832526797,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005799957,0.00004539873,0.00008740201,0.00006125029,0.0001595823,0.00001306697,0.0003672212,0.00003984357,0.004314016],"category_scores_gemma":[0.0002209694,0.00002319735,0.00007910572,0.0009041759,0.000194495,0.0000396437,0.00001942139,0.0002189293,0.0001975047],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005155113,"about_ca_system_score_gemma":0.00003680582,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003163025,"about_ca_topic_score_gemma":0.0009458272,"domain_scores_codex":[0.9988289,0.0001478365,0.0001166512,0.0001419341,0.0004879898,0.0002766816],"domain_scores_gemma":[0.9994871,0.0001115863,0.00002204904,0.0002008841,0.0001056556,0.00007270009],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003112397,0.0000415559,0.959649,0.000006750771,0.000009620882,0.000002511543,0.0000423565,0.000642258,0.001394203,0.002109463,0.003673838,0.03239728],"study_design_scores_gemma":[0.00005133902,0.00008417049,0.9037752,0.000004440664,0.000003411425,0.000001205544,0.00005867143,0.002166343,0.0009213679,0.09187949,0.001020308,0.00003411022],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.968806,0.0006346002,0.000007564917,0.002990199,0.00002405709,0.00006167185,0.000008892218,0.000008795909,0.02745824],"genre_scores_gemma":[0.999086,0.00001545561,0.00005005189,0.00006523087,0.00003864261,7.876887e-8,0.000006412858,3.582724e-7,0.0007378338],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08977003,"threshold_uncertainty_score":0.9965962,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2094090764","doi":"10.1016/j.gr.2011.08.005","title":"Destruction of the eastern North China Craton in a backarc setting: Evidence from crustal deformation kinematics","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":395,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"National Natural Science Foundation of China","keywords":"Geology; Cretaceous; Craton; Paleontology; Paleogene; Rift; Pacific Plate; Lithosphere; Seismology; Subduction; Structural basin; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.09397878559567177,"gpt":0.274333352503562,"spread":0.1803545669078902,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006287433,0.00007500784,0.0001314013,0.00009761068,0.0001051771,0.00002206933,0.0003827422,0.00005424035,0.003501307],"category_scores_gemma":[0.0004613336,0.00004271777,0.00006152537,0.0008254096,0.0001892794,0.0002103381,0.00006563446,0.0003115065,0.0001440858],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007083523,"about_ca_system_score_gemma":0.0000420126,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0634096,"about_ca_topic_score_gemma":0.05639837,"domain_scores_codex":[0.9984632,0.0002702731,0.0002766331,0.0001744648,0.0005379962,0.0002774742],"domain_scores_gemma":[0.9993609,0.0001702714,0.00006658382,0.0002243594,0.00010425,0.00007362195],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003890247,0.00001477831,0.9873946,0.00002318505,0.000006219015,0.000002064389,0.000811583,0.0004230497,0.0001891016,0.0000096864,0.00001783795,0.01106905],"study_design_scores_gemma":[0.00007132407,0.00005206574,0.9516606,0.00005189879,0.000006164697,0.000001241201,0.0002967877,0.03739674,0.001449382,0.008956358,0.000005698284,0.0000517015],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9975849,0.0001422325,0.0000457991,0.0002589424,0.00003261626,0.0001307558,0.00001892719,0.000006840188,0.001778947],"genre_scores_gemma":[0.9990476,0.0000308517,0.0007983238,0.00001381126,0.00002520588,0.00000155211,0.00002660349,0.000001093766,0.00005496171],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03697369,"threshold_uncertainty_score":0.9974096,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1988258618","doi":"10.1016/j.gr.2013.01.004","title":"Recognition of ocean plate stratigraphy in accretionary orogens through Earth history: A record of 3.8billion years of sea floor spreading, subduction, and accretion","year":2013,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":347,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Windsor","funders":"Ministry of Education of the People's Republic of China; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; United Nations Educational, Scientific and Cultural Organization","keywords":"Geology; Oceanic crust; Subduction; Paleontology; Accretion (finance); Basalt; Accretionary wedge; Earth science; Sedimentary rock; Archean; Geochemistry; Continental crust; Oceanic basin; Diachronous; Convergent boundary; Plate tectonics; Crust; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.06040351211620746,"gpt":0.2576042181217313,"spread":0.1972007060055238,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000586677,0.00008182733,0.0002445779,0.0003097258,0.000032905,0.000007374725,0.0001276108,0.0001006537,0.007686408],"category_scores_gemma":[0.0001814285,0.00006996355,0.00007417538,0.000738724,0.0004001127,0.0002538538,0.00002144736,0.0002068732,0.00004065711],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007201127,"about_ca_system_score_gemma":0.00004779466,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.03342149,"about_ca_topic_score_gemma":0.00401355,"domain_scores_codex":[0.9985349,0.0002109817,0.0003580145,0.0002518278,0.0004069182,0.0002373564],"domain_scores_gemma":[0.9991881,0.0001743975,0.0001197174,0.0001395502,0.0002997269,0.00007847677],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000226142,0.0001182997,0.904086,0.0001750765,0.00005610786,0.000006649193,0.0008273005,0.00008080454,0.01214837,0.00009391732,0.000800783,0.08138056],"study_design_scores_gemma":[0.0002987607,0.000459098,0.9525959,0.00006580233,0.00001662274,0.000005639522,0.0007727806,0.001738737,0.006318666,0.03729827,0.0003133497,0.0001163038],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9970866,0.0007108641,0.000008304756,0.0001387996,0.00003247663,0.000197788,0.00005368895,0.0000070383,0.001764371],"genre_scores_gemma":[0.9977086,0.0007996095,0.001218762,0.000008715798,0.00002013831,0.000002122984,0.0001882855,0.000002038954,0.00005170107],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08126426,"threshold_uncertainty_score":0.9932207,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2609095816","doi":"10.1016/j.gr.2017.04.020","title":"Exceptionally preserved fossil assemblages through geologic time and space","year":2017,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":188,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; W. M. Keck Foundation; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Sedimentary depositional environment; Paleontology; Taphonomy; Lagerstätte; Authigenic; Bioturbation; Paleozoic; Proterozoic; Ordovician; Earth science; Diagenesis; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.1140798388776752,"gpt":0.3536477960144201,"spread":0.2395679571367449,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001414289,0.000129117,0.0001926602,0.00009119523,0.001950566,0.0004029718,0.0006900655,0.0001717041,0.00132835],"category_scores_gemma":[0.0005665877,0.0001021005,0.00005608599,0.00009446113,0.001266223,0.0006891637,0.00001829085,0.0004342294,0.0002650012],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002462543,"about_ca_system_score_gemma":0.0001025226,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004924472,"about_ca_topic_score_gemma":0.01139942,"domain_scores_codex":[0.9980248,0.000324233,0.0001441563,0.0004045228,0.0005030723,0.000599247],"domain_scores_gemma":[0.9986258,0.0004595557,0.00007171951,0.0005499514,0.0001294697,0.000163481],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001161701,0.00002733097,0.8969344,0.00002450947,0.00005144635,0.0001104558,0.0002210404,0.00001189094,0.0007748912,0.0009858997,0.006820841,0.0939211],"study_design_scores_gemma":[0.0002616784,0.0001901344,0.9822698,0.0000135197,0.000004643335,0.00001579409,0.00005652585,0.0008950462,0.0001078984,0.0142211,0.00184017,0.000123692],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.6306735,0.006023317,0.0000112518,0.00312325,0.00006227912,0.0001511068,0.00002984993,0.00002685616,0.3598986],"genre_scores_gemma":[0.9959219,0.0003867443,0.0006801813,0.00001806403,0.000117874,0.000003158863,0.00001024382,9.258888e-7,0.00286095],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3652484,"threshold_uncertainty_score":0.9995846,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1965434603","doi":"10.1016/j.gr.2011.06.010","title":"Kinematics and dynamics of the Namche Barwa Syntaxis, eastern Himalaya: Constraints from deformation, fabrics and geochronology","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":162,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Polytechnique Montréal","funders":"Chinese Academy of Geological Sciences; China Geological Survey; China University of Geosciences; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Terrane; Seismology; Crust; Fibrous joint; Metamorphism; Shear zone; Zircon; Subduction; Shear (geology); Geochronology; Petrology; Geochemistry; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.05300123620486179,"gpt":0.2444482559927927,"spread":0.1914470197879309,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004634582,0.00008850537,0.0001830132,0.00006711691,0.0001531758,0.00002378032,0.000264888,0.00009611953,0.004086154],"category_scores_gemma":[0.000284325,0.00005121411,0.00003650312,0.0002818155,0.00120649,0.00007473127,0.0001214939,0.000265837,0.00005116946],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004641487,"about_ca_system_score_gemma":0.00003311463,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01174334,"about_ca_topic_score_gemma":0.01002585,"domain_scores_codex":[0.9988318,0.0001710531,0.0002292838,0.0001915182,0.0002908915,0.0002854617],"domain_scores_gemma":[0.9991785,0.0003165228,0.00006434666,0.0001934975,0.0001328919,0.0001142769],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001517061,0.00001658939,0.9605975,0.00003238417,0.00003412677,0.000002488594,0.0003391324,0.000009799108,0.00006639551,0.0006651106,0.00004105193,0.0381803],"study_design_scores_gemma":[0.0001547636,0.00007757162,0.9205043,0.00001726729,0.00002207142,0.00001153669,0.0009915689,0.03216908,0.000327013,0.04558061,0.00006148886,0.00008275374],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9930953,0.0005165671,0.0001211318,0.0007128212,0.00002724814,0.0001060097,0.0001341627,0.000007243556,0.005279531],"genre_scores_gemma":[0.9987847,0.0001442325,0.0008900789,0.00004717926,0.00001397444,9.605184e-7,0.00005213624,0.000001307487,0.00006548981],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0449155,"threshold_uncertainty_score":0.9968243,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1984979818","doi":"10.1016/j.gr.2014.11.002","title":"Remarkable insights into the paleoecology of the Avalonian Ediacaran macrobiota","year":2014,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":154,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Department of Environment and Conservation, Government of Newfoundland and Labrador; Natural Environment Research Council; Sight Research UK; Cambridge Philosophical Society; National Geographic Society","keywords":"Paleoecology; Taphonomy; Ecology; Macrofossil; Paleontology; Geology; Biodiversity; Benthic zone; Acritarch; Biology","retraction":null,"screen_n_in":null,"score":{"opus":0.02488428610234523,"gpt":0.27877115858781,"spread":0.2538868724854648,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002121003,0.0001036738,0.0001829551,0.0001188818,0.0009116284,0.00003749322,0.00103964,0.000150216,0.0003378565],"category_scores_gemma":[0.0003415461,0.00005195038,0.0001046107,0.0006056888,0.001465207,0.00007959618,0.00001194781,0.0006085213,0.00007178951],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003369797,"about_ca_system_score_gemma":0.0001444899,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002725809,"about_ca_topic_score_gemma":0.154505,"domain_scores_codex":[0.9972045,0.001365239,0.0002242627,0.000261005,0.0004511577,0.0004937745],"domain_scores_gemma":[0.9980133,0.00111077,0.0000647846,0.0005971254,0.0001180764,0.00009590889],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006459204,0.00002308816,0.7781869,0.00003102358,0.0000424713,0.000004424368,0.002014657,0.00003033753,0.000577719,0.002823911,0.004548339,0.2116526],"study_design_scores_gemma":[0.0001648029,0.0001470924,0.9738489,0.00001118767,0.00000615788,0.0000053443,0.0002112663,0.0003863307,0.0005426616,0.007530321,0.01707947,0.00006651253],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.7281989,0.004310245,0.00000921345,0.003312227,0.0003721694,0.0002526151,0.000004412412,0.00001137524,0.2635288],"genre_scores_gemma":[0.9991981,0.0001228731,0.00009264204,0.0000858835,0.0001131169,0.000003106116,0.000002853923,8.833257e-7,0.0003805662],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2709991,"threshold_uncertainty_score":0.8609231,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1982501717","doi":"10.1016/j.gr.2011.09.014","title":"Revision of the Cretaceous–Paleogene stratigraphic framework, facies architecture and provenance of the Xigaze forearc basin along the Yarlung Zangbo suture zone","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada; Dalhousie University","funders":"","keywords":"Geology; Forearc; Paleontology; Flysch; Cretaceous; Aptian; Paleogene; Facies; Carbonate platform; Paleocurrent; Provenance; Sedimentary rock; Structural basin; Subduction; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.04934288276717389,"gpt":0.2543683138426476,"spread":0.2050254310754737,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008479373,0.0001389863,0.0002355663,0.00003520195,0.0005538147,0.00002888771,0.0007596375,0.0001056254,0.000428342],"category_scores_gemma":[0.0004886528,0.00004973988,0.000140758,0.0007965186,0.001802996,0.00004957923,0.0001935935,0.0007630409,0.000009016066],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001523952,"about_ca_system_score_gemma":0.00004285855,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002321576,"about_ca_topic_score_gemma":0.006242002,"domain_scores_codex":[0.997897,0.0004934419,0.0002248706,0.0002681308,0.0007008628,0.0004156678],"domain_scores_gemma":[0.9984968,0.0007072858,0.0001006771,0.0004825864,0.0001488371,0.00006378314],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002098944,0.00006897136,0.7369831,0.0002239953,0.00008605018,0.000005633817,0.003776199,0.0001142035,0.0002324404,0.002283645,0.0004769231,0.2555389],"study_design_scores_gemma":[0.00008722403,0.0002345519,0.9727471,0.0001327865,0.00001361363,0.000004867973,0.0006409921,0.0001191643,0.00150358,0.01971108,0.004729147,0.00007583333],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9803512,0.01186292,0.0000348585,0.003561648,0.00006292648,0.0005797783,0.00007360813,0.000007323755,0.003465751],"genre_scores_gemma":[0.9984439,0.0006812002,0.0002450727,0.00008264714,0.00004808054,0.000002855292,0.000001992724,0.000002501047,0.00049177],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2554631,"threshold_uncertainty_score":0.6643212,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2008845716","doi":"10.1016/j.gr.2011.02.010","title":"Zircon U–Pb chronology and Hf isotope of the Xingxingxia granodiorite from the Central Tianshan zone (NW China): Implications for the tectonic evolution of the southern Altaids","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":144,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Regina","funders":"National Key Research and Development Program of China; State Key Laboratory of Geological Processes and Mineral Resources; National Natural Science Foundation of China","keywords":"Geology; Zircon; Subduction; Paleozoic; Geochemistry; Precambrian; Tectonics; Craton; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.04474226731964102,"gpt":0.252166321660057,"spread":0.207424054340416,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008108909,0.00009799937,0.0001649185,0.00003298873,0.000665827,0.00002020405,0.0009692764,0.00008423069,0.001039851],"category_scores_gemma":[0.0002939054,0.00003656326,0.0001594756,0.000601119,0.001173037,0.00004491215,0.0001335571,0.0003328493,0.00001401624],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009465782,"about_ca_system_score_gemma":0.00008744825,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.07652273,"about_ca_topic_score_gemma":0.03356353,"domain_scores_codex":[0.9985491,0.0003040653,0.0002236798,0.0002470202,0.0002579148,0.0004181916],"domain_scores_gemma":[0.9984379,0.0007205227,0.0001003098,0.0005527896,0.0001309133,0.00005751923],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008503866,0.00003961738,0.9685407,0.00001575445,0.0001106051,1.028628e-7,0.001316316,0.00006863208,0.01223794,0.001311386,0.0002726736,0.01600122],"study_design_scores_gemma":[0.0001666631,0.00008239893,0.9644496,0.00001096627,0.00005389556,0.00000161876,0.0006603643,0.001184006,0.002691737,0.02993494,0.0007122803,0.00005154012],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9855281,0.003209271,0.0007947692,0.008863663,0.00007598454,0.0005235715,0.0004058438,0.000007731194,0.000591086],"genre_scores_gemma":[0.9993954,0.00009405729,0.000113168,0.0000522094,0.00006630392,0.00001173214,0.0000161172,0.000002533494,0.0002484941],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04295919,"threshold_uncertainty_score":0.9998733,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2082333936","doi":"10.1016/j.gr.2014.08.001","title":"Crustal structure of the Indus–Tsangpo suture zone and its ophiolites in southern Tibet","year":2014,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":134,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Polytechnique Montréal","funders":"Chinese Academy of Geological Sciences; China Geological Survey; Institute of Geology, Chinese Academy of Geological Sciences; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Ophiolite; Geology; Flysch; Fibrous joint; Terrane; Forearc; Shear zone; Massif; Nappe; Paleontology; Continental margin; Continental collision; Subduction; Thrust fault; Cretaceous; Plate tectonics; Eurasian Plate; Oceanic crust; Foreland basin; Paleogene; Fault (geology); Structural basin; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.02733668637912154,"gpt":0.2533789354113277,"spread":0.2260422490322061,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004846024,0.00008305239,0.0001674185,0.00009181959,0.0001078359,0.00002596353,0.0003306876,0.0001171021,0.004346984],"category_scores_gemma":[0.0003819156,0.00004321363,0.00004350572,0.0006847756,0.0002248255,0.00004216992,0.00007988562,0.0004884755,0.00004757267],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002276935,"about_ca_system_score_gemma":0.00002465848,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005527987,"about_ca_topic_score_gemma":0.02175229,"domain_scores_codex":[0.998592,0.0002787329,0.0001494241,0.0002216762,0.0004149716,0.0003432459],"domain_scores_gemma":[0.9993461,0.000265493,0.00003107129,0.0001691832,0.00008629372,0.0001018104],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004073047,0.00001643174,0.9780539,0.00003680638,0.00001497122,0.000002890755,0.0004480717,0.0003278528,0.007214391,0.0004513041,0.0001385892,0.01325411],"study_design_scores_gemma":[0.0002283798,0.00008571908,0.9712119,0.00001770327,0.000006153325,0.00000332639,0.0005961675,0.00467125,0.001729722,0.02012289,0.001226529,0.0001003279],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9953574,0.0008771499,0.000001188349,0.001570632,0.0000191277,0.00009241235,0.0001076222,0.000005015268,0.00196944],"genre_scores_gemma":[0.9992087,0.0000187201,0.00004518307,0.00008658684,0.00006058006,3.854985e-7,0.00002495329,0.000001410667,0.0005534722],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01967159,"threshold_uncertainty_score":0.9965632,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2094067546","doi":"10.1016/j.gr.2011.05.012","title":"Juvenile contribution of the Neoproterozoic Rio Negro Magmatic Arc (Ribeira Belt, Brazil): Implications for Western Gondwana amalgamation","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université du Québec à Montréal","funders":"Fundação Carlos Chagas Filho de Amparo à Pesquisa do Estado do Rio de Janeiro; Universidade do Estado do Rio de Janeiro; Petrobras; Financiadora de Estudos e Projetos; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Gondwana; Geology; Mafic; Felsic; Back-arc basin; Magmatism; Geochemistry; Subduction; Shear zone; Continental arc; Magma; Paleontology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.07860536329626523,"gpt":0.3081627351570748,"spread":0.2295573718608096,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001083021,0.0001361174,0.000271476,0.0001340917,0.0004502465,0.00004696155,0.0006709329,0.0001130688,0.002444859],"category_scores_gemma":[0.0005451668,0.00008481339,0.00020249,0.0008712369,0.0003804785,0.0001537949,0.00007542413,0.0002860418,0.0001750088],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001531657,"about_ca_system_score_gemma":0.00008177623,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006227907,"about_ca_topic_score_gemma":0.01057512,"domain_scores_codex":[0.9979874,0.0002603129,0.0004349897,0.0003345326,0.0004213152,0.0005614432],"domain_scores_gemma":[0.9982924,0.0004276773,0.0001506547,0.0004853779,0.0004869828,0.0001568766],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009333251,0.0001183582,0.9724344,0.00007485424,0.00005921131,6.861559e-7,0.0002481638,0.00005115275,0.003062513,0.001758298,0.001214518,0.02088451],"study_design_scores_gemma":[0.0002938387,0.0001724991,0.9360723,0.00002124549,0.00003503973,0.000003352517,0.00005790386,0.001107395,0.004166185,0.05682949,0.001134585,0.0001060985],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9907185,0.0003370955,0.001065991,0.003398393,0.00005979074,0.0009161269,0.0002265114,0.00002928438,0.003248337],"genre_scores_gemma":[0.9982052,0.00002202414,0.0005581119,0.0001389866,0.00005611419,0.00005010427,0.0002699732,0.000003741875,0.0006956856],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05507119,"threshold_uncertainty_score":0.998467,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2061185233","doi":"10.1016/j.gr.2011.10.012","title":"Discovery of a dismembered metamorphic sole in the Saga ophiolitic mélange, South Tibet: Assessing an Early Cretaceous disruption of the Neo-Tethyan supra-subduction zone and consequences on basin closing","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia; Memorial University of Newfoundland; Saint Mary's University; Université Laval","funders":"China University of Geosciences, Beijing; National Science Foundation","keywords":"Geology; Ophiolite; Hornblende; Subduction; Geochemistry; Metamorphic rock; Cretaceous; Fibrous joint; Paleontology; Plateau (mathematics); Tectonics; Biotite; Quartz","retraction":null,"screen_n_in":null,"score":{"opus":0.1467388160361876,"gpt":0.3084593355964375,"spread":0.1617205195602499,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00159562,0.0001154544,0.000245087,0.0001465004,0.0002143175,0.00009715746,0.0003551919,0.00007710313,0.0002762029],"category_scores_gemma":[0.000271767,0.00005800427,0.00008288669,0.0007154401,0.001041057,0.0003246508,0.00003973992,0.0003855566,0.00000708389],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006220264,"about_ca_system_score_gemma":0.0000558896,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02341398,"about_ca_topic_score_gemma":0.006490505,"domain_scores_codex":[0.9973908,0.001065532,0.0002844534,0.0002987896,0.0005985619,0.0003618707],"domain_scores_gemma":[0.9989958,0.0004459126,0.000108056,0.0002976152,0.00008583997,0.00006671865],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002029853,0.0001481699,0.9733711,0.00006939512,0.00004001631,0.00002057905,0.003722583,0.0001069114,0.01376363,0.0006466041,0.000008448945,0.007899559],"study_design_scores_gemma":[0.0001605541,0.0003189592,0.9743575,0.0000575551,0.00003481991,0.000009217088,0.003781292,0.0009159068,0.007032925,0.01323141,0.000009878097,0.0000899214],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9969199,0.0003894888,0.00001879524,0.0006142244,0.00003365326,0.0001830736,0.00004413979,0.000005739833,0.001790989],"genre_scores_gemma":[0.9996579,0.00003352577,0.0001134452,0.00003895725,0.00003454949,0.000002778999,0.00002499378,0.000002467689,0.00009138366],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01692348,"threshold_uncertainty_score":0.9830892,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2320891775","doi":"10.1016/j.gr.2016.02.008","title":"Characterisation of Triassic rifting in Peru and implications for the early disassembly of western Pangaea","year":2016,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Tectonic Studies in Latin America","field":"Earth and Planetary Sciences","cited_by":115,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Université de Genève; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Rift; Pangaea; Paleontology; Subduction; Zircon; Seafloor spreading; Transtension; Passive margin; Tectonics; Structural basin; Permian","retraction":null,"screen_n_in":null,"score":{"opus":0.12628248233871,"gpt":0.3585703403740641,"spread":0.2322878580353541,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009071137,0.00004378066,0.00012285,0.00005885593,0.0001173155,0.000008364757,0.0001612225,0.00002817867,0.0001343576],"category_scores_gemma":[0.0005780654,0.00002048043,0.00002596655,0.0002354092,0.0003219204,0.00005120075,0.0000322583,0.00006251938,0.000005089468],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003023737,"about_ca_system_score_gemma":0.00002229074,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001504236,"about_ca_topic_score_gemma":0.0004832933,"domain_scores_codex":[0.9992362,0.0001051487,0.0001866051,0.0001314429,0.0001371299,0.0002034454],"domain_scores_gemma":[0.9966362,0.003047046,0.00006601265,0.0001385411,0.00008518557,0.00002700455],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003034334,0.000006862904,0.6252779,0.000009362328,0.000006115595,5.909841e-8,0.0001857545,9.745394e-7,0.001108196,0.0001383998,0.00002009834,0.3732159],"study_design_scores_gemma":[0.0002482921,0.0001844553,0.9978706,0.00001847885,0.000002811048,4.455979e-7,0.0001992545,0.00005880467,0.0001226591,0.0008225476,0.0004421917,0.0000294373],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9941361,0.0004360518,0.0002144905,0.003294634,0.00002452055,0.000275448,0.00009822993,0.000004128368,0.001516401],"genre_scores_gemma":[0.9994664,0.0002581107,0.000126677,0.00001321016,0.00002497036,0.00001390263,0.000004331197,0.000001264418,0.00009116538],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3731865,"threshold_uncertainty_score":0.2273965,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2131004195","doi":"10.1016/j.gr.2006.02.004","title":"Field and geochemical characteristics of the Mesoarchean (∼3075Ma) Ivisaartoq greenstone belt, southern West Greenland: Evidence for seafloor hydrothermal alteration in supra-subduction oceanic crust","year":2006,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Saskatchewan; University of Windsor","funders":"University of Saskatchewan","keywords":"Geology; Geochemistry; Pillow lava; Metasomatism; Greenstone belt; Ultramafic rock; Metamorphism; Epidote; Archean; Petrology; Quartz; Volcanic rock; Paleontology; Mantle (geology); Chlorite","retraction":null,"screen_n_in":null,"score":{"opus":0.05713069905662258,"gpt":0.2986701447701246,"spread":0.241539445713502,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001109448,0.0001268405,0.0002363764,0.0001064717,0.0002001017,0.00004667641,0.0002785288,0.0001201849,0.001083255],"category_scores_gemma":[0.0005217222,0.00008360555,0.00009004345,0.0004446424,0.0003332408,0.0001176854,0.0000570895,0.0003706293,0.00002680815],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001040371,"about_ca_system_score_gemma":0.00005122706,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0316696,"about_ca_topic_score_gemma":0.02473246,"domain_scores_codex":[0.9981538,0.0002320871,0.000343599,0.0003539108,0.0004712422,0.0004453693],"domain_scores_gemma":[0.9985896,0.0008688964,0.00007609632,0.0002292618,0.0001465485,0.00008962132],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003413994,0.00006047612,0.9694598,0.00008771828,0.00001348118,0.000003988774,0.0001420473,0.00006900031,0.01003518,0.0001178421,0.0003034145,0.01936565],"study_design_scores_gemma":[0.0003662761,0.0002576237,0.9678966,0.00006627482,0.0000213593,0.000008812071,0.0001551497,0.01931922,0.005817279,0.005800754,0.0001443343,0.0001463132],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9956368,0.0004372727,0.00008686248,0.00308786,0.00003642277,0.0003218293,0.0001004499,0.00001019576,0.0002823423],"genre_scores_gemma":[0.999021,0.00004207456,0.0001534961,0.00007558823,0.0001988313,0.000007531743,0.000120719,0.00000356021,0.0003772345],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01925022,"threshold_uncertainty_score":0.9998299,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2085102081","doi":"10.1016/j.gr.2010.03.009","title":"U–Pb and Hf isotopic study of zircons from migmatised amphibolites in the Cathaysia Block: Implications for the early Paleozoic peak tectonothermal event in Southeastern China","year":2010,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Waterloo","funders":"","keywords":"Zircon; Geology; Paleozoic; Geochemistry; Tectonics; Protolith; Craton; Geochronology; Block (permutation group theory); Basalt; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.03591501789007503,"gpt":0.2991447322616008,"spread":0.2632297143715258,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009817982,0.00009264926,0.0001750704,0.0001162366,0.0001903655,0.0000559916,0.0005376065,0.00005512171,0.0005131724],"category_scores_gemma":[0.000205271,0.00004653204,0.0000522862,0.0005376281,0.0002322102,0.00004137823,0.00004326801,0.000420345,0.00001404793],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001499816,"about_ca_system_score_gemma":0.00003005367,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0677807,"about_ca_topic_score_gemma":0.2727692,"domain_scores_codex":[0.9986453,0.0002489387,0.000255818,0.0002622517,0.0002565869,0.0003310867],"domain_scores_gemma":[0.9980986,0.001383051,0.00004448561,0.0003583903,0.00005429297,0.00006115493],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002689101,0.0001508253,0.9870737,0.000005703677,0.00001756274,9.920433e-7,0.002943082,0.00005797267,0.002330141,0.00005271534,0.000006711038,0.007333731],"study_design_scores_gemma":[0.0004171702,0.0001630874,0.987545,0.000004996891,0.000013414,9.919131e-7,0.002147379,0.001659663,0.00006421754,0.007846463,0.00007916352,0.00005843027],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9954201,0.0003624837,0.000008210642,0.003075909,0.00001481424,0.0007427783,0.0001187925,0.000004748832,0.0002521414],"genre_scores_gemma":[0.9997464,0.00001431383,0.00005061056,0.00002782542,0.0000427402,0.00005370208,0.00002320897,0.000001871071,0.00003931907],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2049885,"threshold_uncertainty_score":0.938427,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2045400016","doi":"10.1016/j.gr.2012.03.010","title":"The missing Rheic Ocean magmatic arcs: Provenance analysis of Late Paleozoic sedimentary clastic rocks of SW Iberia","year":2012,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Provenance; Terrane; Carboniferous; Devonian; Paleozoic; Paleontology; Basement; Fibrous joint; Gondwana; Ordovician; Late Devonian extinction; Sedimentary rock; Clastic rock; Geochemistry; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.03851934402023529,"gpt":0.2898302675979484,"spread":0.2513109235777132,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001822181,0.0001284324,0.0003907045,0.0002646047,0.0002811654,0.00003277301,0.0004800016,0.00006547185,0.003869149],"category_scores_gemma":[0.0003927884,0.00007267834,0.0002236197,0.00221365,0.000497616,0.0001205336,0.00006730278,0.0003053153,0.00007881299],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007653235,"about_ca_system_score_gemma":0.00004593696,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004491415,"about_ca_topic_score_gemma":0.001506107,"domain_scores_codex":[0.9974176,0.0003633245,0.0004575419,0.0002377824,0.0007963947,0.0007273693],"domain_scores_gemma":[0.9977587,0.001335287,0.000144403,0.0003678097,0.0001628302,0.0002309366],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00007584039,0.00007599339,0.9770325,0.00008265197,0.0005749275,0.000002606221,0.0002406631,0.002134491,0.0009602529,0.00004463191,0.0003803272,0.01839514],"study_design_scores_gemma":[0.0001599558,0.0001415969,0.9468392,0.00003745786,0.0004261362,0.000001269788,0.0003722924,0.04161657,0.002278817,0.007090298,0.0008916315,0.0001447631],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9912298,0.004781852,0.00005351844,0.0008900692,0.00004709577,0.0001448919,0.00005163454,0.00001025587,0.002790911],"genre_scores_gemma":[0.9989712,0.00016378,0.0002051066,0.00004511257,0.00005195173,0.000001358587,0.00008145773,0.000002404013,0.0004776925],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03948208,"threshold_uncertainty_score":0.9970415,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2059959942","doi":"10.1016/j.gr.2009.08.009","title":"Comparative evolution of the Iapetus and Rheic Oceans: A North America perspective","year":2009,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Saint Mary's University; St. Mary's University; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Consejo Nacional de Ciencia y Tecnología; St. Francis Xavier University; National Science Foundation","keywords":"Laurentia; Gondwana; Geology; Baltica; Paleontology; Terrane; Ordovician; Passive margin; Obduction; Metamorphism; Paleozoic; Orogeny; Subduction; Oceanic crust; Rift; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.0428722285752376,"gpt":0.2975680942797018,"spread":0.2546958657044642,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002089232,0.00007011469,0.0001678724,0.00007452675,0.0002162283,0.00001900216,0.0002304654,0.00002953705,0.0009827013],"category_scores_gemma":[0.0001564325,0.00003816541,0.00006121704,0.001047136,0.0005415463,0.00005748029,0.00002692065,0.0002658251,0.00007182237],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001272713,"about_ca_system_score_gemma":0.00004812378,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.008444612,"about_ca_topic_score_gemma":0.006099574,"domain_scores_codex":[0.9987684,0.0002101841,0.0001158815,0.0002190796,0.0004098241,0.0002766701],"domain_scores_gemma":[0.9992974,0.0001963401,0.00003570789,0.0001499944,0.0002268543,0.00009367046],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000164603,0.0001187695,0.9700522,0.000009636673,0.00006881599,0.000006315423,0.002203297,0.0009281046,0.0005653491,0.001616356,0.001687931,0.02257863],"study_design_scores_gemma":[0.00008742997,0.0002348949,0.9619521,0.000004941087,0.000008955971,0.00000199809,0.002327575,0.003152079,0.00009845854,0.03143199,0.0006441179,0.00005549162],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9797224,0.002351061,0.000013297,0.002413604,0.00001330204,0.0001161311,0.00003143463,0.000008113152,0.01533059],"genre_scores_gemma":[0.9995355,0.00008304151,0.0000752559,0.00006542433,0.00003003949,4.774085e-7,0.000008947379,4.245776e-7,0.0002009114],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02981564,"threshold_uncertainty_score":0.9999306,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2794438358","doi":"10.1016/j.gr.2018.02.006","title":"A giant circumferential dyke swarm associated with the High Arctic Large Igneous Province (HALIP)","year":2018,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Graben; Igneous rock; Magmatism; Arctic; Plume; Swarm behaviour; Mantle plume; Mafic; Lithosphere; Tectonics; Geophysics; Seismology; Paleontology; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.05129977394640978,"gpt":0.272679124425991,"spread":0.2213793504795812,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001410978,0.0001193657,0.0001492562,0.00005585682,0.001339971,0.0001604532,0.0003781985,0.00007481017,0.003466523],"category_scores_gemma":[0.0003561162,0.00006114803,0.00003487895,0.0005547272,0.0005337983,0.0001084364,0.00006859237,0.0003770054,0.001159128],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002237585,"about_ca_system_score_gemma":0.0001108149,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01354825,"about_ca_topic_score_gemma":0.1587,"domain_scores_codex":[0.9974867,0.0003905546,0.0001383939,0.0003323735,0.0008346669,0.0008173363],"domain_scores_gemma":[0.9989088,0.0003146612,0.00004945905,0.0002400641,0.0003645613,0.0001224625],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001953186,0.000947694,0.7251416,0.0001531877,0.0008786356,0.000749314,0.006672009,0.0009112436,0.0002869561,0.008196523,0.1071811,0.1469286],"study_design_scores_gemma":[0.001094933,0.003683872,0.933818,0.0000580107,0.00003281718,0.000016408,0.003065849,0.008888306,0.0001196081,0.003587926,0.04526437,0.0003699124],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9867409,0.0003121318,0.0002375399,0.006605944,0.0001676049,0.0004848832,0.0000735655,0.00005329395,0.005324114],"genre_scores_gemma":[0.9979347,0.00004305119,0.00003251749,0.0001859652,0.0002866521,0.000008027453,0.0001277473,0.000003984163,0.001377354],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2086764,"threshold_uncertainty_score":0.9999601,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3172183348","doi":"10.1016/j.gr.2021.05.025","title":"Provenance and Paleozoic tectonic evolution of Ganderia and its relationships with Avalonia and Megumia in the Appalachian-Caledonide orogen","year":2021,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta; Nova Scotia Department of Energy; Acadia University; University of Waterloo; Geological Survey of Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Laurentia; Baltica; Ordovician; Geology; Orogeny; Paleontology; Paleozoic; Devonian; Gondwana; Terrane; Accretion (finance); Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.04578459327531258,"gpt":0.2580544060452327,"spread":0.2122698127699201,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001074383,0.00007360286,0.0001450478,0.00007410818,0.0001984258,0.00004102202,0.00009409186,0.0000586613,0.0001751321],"category_scores_gemma":[0.0003481579,0.00004117368,0.0000147677,0.0007144286,0.0002361449,0.00007995382,0.00003198166,0.0003506674,0.000007908196],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000399466,"about_ca_system_score_gemma":0.00006992773,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001348253,"about_ca_topic_score_gemma":0.02864117,"domain_scores_codex":[0.9986331,0.0004020044,0.0001405633,0.0002712428,0.0003011148,0.0002519722],"domain_scores_gemma":[0.9992191,0.0004552074,0.00002856659,0.0001228795,0.00009615391,0.00007812674],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004285648,0.00001568494,0.9962105,0.00004936145,0.00001204561,0.00001703012,0.0001769574,0.0000316288,0.0009130132,0.0006420103,0.00001419633,0.00187476],"study_design_scores_gemma":[0.0002322585,0.0001017557,0.9840497,0.00002594237,0.00001209406,0.00003557979,0.0007186374,0.003108712,0.0004058258,0.01115168,0.00009577086,0.00006200192],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9860191,0.01080641,0.000007867159,0.001828943,0.000003728445,0.000148116,0.00001202537,0.000004178054,0.001169617],"genre_scores_gemma":[0.9991579,0.0005237145,0.0001538878,0.00001664998,0.0000116642,0.000004042554,0.00001438926,0.000001181369,0.000116547],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02729292,"threshold_uncertainty_score":0.9890836,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2285539797","doi":"10.1016/j.gr.2016.01.006","title":"Tectono-magmatic evolution of Late Jurassic to Early Cretaceous granitoids in the west central Lhasa subterrane, Tibet","year":2016,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Lakehead University","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Geology; Magmatism; Zircon; Subduction; Cretaceous; Geochemistry; Continental arc; Back-arc basin; Mesozoic; Fibrous joint; Paleontology; Structural basin; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.03552887501509349,"gpt":0.2667818291175338,"spread":0.2312529541024403,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001199268,0.0001110649,0.0002102982,0.0002309052,0.0001301033,0.00004296492,0.0006015185,0.00007363126,0.004611348],"category_scores_gemma":[0.0003912768,0.00005220139,0.00008638586,0.001264469,0.000274991,0.0001043686,0.00003799608,0.0002646194,0.0009713374],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002060163,"about_ca_system_score_gemma":0.00005502979,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01413391,"about_ca_topic_score_gemma":0.02491429,"domain_scores_codex":[0.9975511,0.0004358878,0.0002797949,0.000286123,0.0007259265,0.0007211502],"domain_scores_gemma":[0.998734,0.0006491081,0.00003694783,0.0002962406,0.0001102465,0.0001734546],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001206697,0.00005721366,0.9500961,0.00002441025,0.00001617527,0.00002802187,0.0003657103,0.0001123034,0.007306739,0.0001218815,0.0005217901,0.04122897],"study_design_scores_gemma":[0.0002165263,0.0002749252,0.9871832,0.00003658925,0.000007568078,0.000003100893,0.0001468799,0.0003985171,0.0004594724,0.01041444,0.0007650748,0.0000937075],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9909484,0.0003591943,0.00006846197,0.003996536,0.0000404935,0.0002277516,0.0000475078,0.0000129559,0.004298719],"genre_scores_gemma":[0.9993356,0.0000344588,0.00007074638,0.00005213708,0.00005655403,0.000005031751,0.00001197726,0.000002046972,0.0004313918],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04113526,"threshold_uncertainty_score":0.9998065,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2061062987","doi":"10.1016/j.gr.2012.04.012","title":"Late Paleozoic peperites in West Junggar, China, and how they constrain regional tectonic and palaeoenvironmental setting","year":2012,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Saint Mary's University","funders":"Chinese Academy of Geological Sciences; China Scholarship Council; Chinese Academy of Sciences","keywords":"Geology; Paleozoic; Ophiolite; Devonian; Lava; Basalt; Geochemistry; Paleontology; Crust; Late Devonian extinction; Sedimentary rock; Oceanic crust; Structural basin; Tectonics; Carboniferous; Subduction","retraction":null,"screen_n_in":null,"score":{"opus":0.02966287501949184,"gpt":0.2514980903116902,"spread":0.2218352152921984,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00114113,0.0001160572,0.000161878,0.0001184226,0.0002151372,0.00007135113,0.0001237234,0.00007700605,0.002362544],"category_scores_gemma":[0.00008084565,0.00008172042,0.00003305118,0.0002097422,0.0005596513,0.0001607032,0.00006901828,0.0004173656,0.00007364419],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005540673,"about_ca_system_score_gemma":0.00001317413,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00178766,"about_ca_topic_score_gemma":0.004125577,"domain_scores_codex":[0.9983799,0.000237234,0.0001097472,0.0002837525,0.0003423001,0.000647023],"domain_scores_gemma":[0.9992484,0.0003529016,0.00002396079,0.0001039192,0.00001102854,0.0002597535],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001392068,0.00001964504,0.9730746,0.00001326257,0.000009510211,0.0000107074,0.0002437043,0.00001082325,0.0008099924,0.00003722518,0.0000530278,0.02570355],"study_design_scores_gemma":[0.0001980415,0.00005877465,0.9951219,0.00001202741,0.000004954592,0.00002664415,0.0005824762,0.001459445,0.00008881445,0.001691234,0.000641017,0.0001146559],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9890034,0.004291578,7.566886e-7,0.004832174,0.0000127409,0.0001034522,0.00002635566,0.00001005226,0.001719508],"genre_scores_gemma":[0.9986553,0.000642853,0.0001697135,0.00006596505,0.00005787053,0.000002395882,0.00004537678,0.000002061062,0.0003584154],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02558889,"threshold_uncertainty_score":0.9985494,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1988810157","doi":"10.1016/s1342-937x(05)71155-2","title":"Geology, Geochemistry and Tectonic Significance of Mafic-ultramafic Rocks of Mesoproterozoic Phulad Ophiolite Suite of South Delhi Fold Belt, NW Indian Shield","year":2005,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Laurentian University; University of Windsor","funders":"University Grants Commission","keywords":"Geology; Geochemistry; Ophiolite; Ultramafic rock; Mafic; Hornblende; Petrology; Schist; Gabbro; Volcanic rock; Basalt; Tectonics; Metamorphic rock; Biotite; Paleontology; Volcano","retraction":null,"screen_n_in":null,"score":{"opus":0.02784182962093756,"gpt":0.2649126467748413,"spread":0.2370708171539038,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001049088,0.0001884689,0.0005295214,0.0002448575,0.0001100825,0.00001696017,0.0005715034,0.0002367313,0.004590289],"category_scores_gemma":[0.000382458,0.0001453825,0.0001525723,0.0008682972,0.001021224,0.0000863224,0.0001026482,0.0005414569,0.00002964756],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007153332,"about_ca_system_score_gemma":0.0001028163,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0113786,"about_ca_topic_score_gemma":0.003202506,"domain_scores_codex":[0.9974348,0.0001758916,0.0005691558,0.0004902247,0.0006518535,0.0006780587],"domain_scores_gemma":[0.9983763,0.0005007942,0.0001970492,0.0004204818,0.0002514604,0.0002539909],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002674105,0.0001375155,0.9232745,0.0004705386,0.0001498597,0.0000185447,0.0006672407,0.0007789826,0.05000982,0.00005274647,0.0001769559,0.02399594],"study_design_scores_gemma":[0.001086063,0.0008792517,0.6226669,0.000126248,0.00007926059,0.00002555303,0.001511047,0.003942415,0.3596594,0.00898392,0.0005468414,0.0004931238],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.993417,0.003006695,0.0000166223,0.0005979393,0.00001111091,0.0002445216,0.0001992267,0.00001263555,0.002494286],"genre_scores_gemma":[0.9988944,0.0001769698,0.000382564,0.00003824007,0.0000575972,0.000005991368,0.0001008308,0.000003906625,0.0003395179],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3096496,"threshold_uncertainty_score":0.9963197,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1127533065","doi":"10.1016/j.gr.2015.05.015","title":"Geochemistry, petrogenesis and tectonic setting of Neoproterozoic mafic–ultramafic rocks from the western Jiangnan orogen, South China","year":2015,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Windsor","funders":"China Geological Survey; National Natural Science Foundation of China","keywords":"Geology; Geochemistry; Mafic; Petrogenesis; Ultramafic rock; Zircon; Craton; Rodinia; Terrane; Petrology; Geochronology; Basalt; Tectonics; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.04744710725384557,"gpt":0.2676982935913178,"spread":0.2202511863374722,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001142721,0.0001684593,0.0002826404,0.00006516506,0.0002549478,0.0001023395,0.0005863139,0.0001139714,0.001907453],"category_scores_gemma":[0.0004604888,0.00009977299,0.0001008273,0.0006349972,0.0003505763,0.00006568407,0.0001329681,0.0004326047,0.0001619128],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008182998,"about_ca_system_score_gemma":0.0000901797,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.04015462,"about_ca_topic_score_gemma":0.006265004,"domain_scores_codex":[0.9976199,0.0002627099,0.000282031,0.0004607892,0.0007829998,0.000591614],"domain_scores_gemma":[0.9986416,0.0003731934,0.0000832068,0.0004041773,0.000167559,0.0003302306],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005207723,0.00001769474,0.9838542,0.00001811415,0.00005099459,0.00001047817,0.000627457,0.000125094,0.001165312,0.000001072694,0.0003452041,0.01373234],"study_design_scores_gemma":[0.0004526548,0.0001776336,0.9799299,0.00003452569,0.00004788355,0.0000164555,0.001947925,0.003176862,0.00894602,0.004069156,0.0009699295,0.0002311165],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9930413,0.003250853,0.00002127795,0.002010345,0.00002534011,0.0001583331,0.0001701537,0.00002392972,0.001298416],"genre_scores_gemma":[0.9991739,0.00004328302,0.0001540584,0.00007021626,0.0001251556,0.000004658191,0.0001467057,0.000004197407,0.000277781],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03388961,"threshold_uncertainty_score":0.999005,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2559889514","doi":"10.1016/j.gr.2016.12.003","title":"Lower Permian conodonts from Palaeo-Tethys Ocean Plate Stratigraphy in the Chiang Mai-Chiang Rai Suture Zone, northern Thailand","year":2016,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"Australian Research Council","keywords":"Terrane; Geology; Fibrous joint; Permian; Paleontology; Nappe; Shear zone; Structural basin; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.03649786468575394,"gpt":0.2761750812800784,"spread":0.2396772165943244,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001655573,0.0002689755,0.0003110181,0.0003366885,0.0005707522,0.0001764152,0.001017205,0.0002824802,0.001302289],"category_scores_gemma":[0.0000965124,0.0001460758,0.0001680933,0.000649738,0.0007366195,0.0003792935,0.000007047649,0.000878398,0.0001942022],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007206786,"about_ca_system_score_gemma":0.0001975588,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01403686,"about_ca_topic_score_gemma":0.538412,"domain_scores_codex":[0.9962734,0.0009236776,0.0003458426,0.0006081765,0.0008111895,0.001037712],"domain_scores_gemma":[0.9978332,0.001163821,0.00007645888,0.0006003608,0.00008117369,0.0002450066],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002041315,0.00003931232,0.8793204,0.000007807524,0.00005104024,0.0002656623,0.001187245,0.000005440367,0.0001040514,0.0001669732,0.001611466,0.1170364],"study_design_scores_gemma":[0.0009256373,0.0002130224,0.9924842,0.00006247488,0.00000837658,0.00001433036,0.001111965,0.00009182054,0.00003922126,0.002646708,0.002173108,0.0002291697],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9169965,0.004539112,0.0000271822,0.00338325,0.0002429022,0.0003990906,0.0005316759,0.00003439839,0.07384591],"genre_scores_gemma":[0.9990205,0.0002310834,0.00008200466,0.0001167936,0.0002336194,0.000004097181,0.00005144326,0.000003384253,0.0002570736],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5243752,"threshold_uncertainty_score":0.9996107,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2075666553","doi":"10.1016/j.gr.2011.12.001","title":"Origin of Archean tonalite–trondhjemite–granodiorite (TTG) suites and granites in the Fiskenæsset region, southern West Greenland: Implications for continental growth","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Windsor","funders":"","keywords":"Eclogite; Geology; Geochemistry; Archean; Partial melting; Basalt; Continental crust; Crust; Petrology; Subduction; Paleontology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.1323738077199813,"gpt":0.3071516397401789,"spread":0.1747778320201976,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001258489,0.0001180192,0.0002186122,0.0001764137,0.0001969723,0.00003697628,0.0004575861,0.00006941897,0.0005840014],"category_scores_gemma":[0.0004102203,0.00006997013,0.00009563542,0.0006653249,0.0005214653,0.00007470045,0.00003289885,0.0002557479,0.00003177631],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002973883,"about_ca_system_score_gemma":0.00002773622,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02878037,"about_ca_topic_score_gemma":0.01745676,"domain_scores_codex":[0.9984635,0.0002192506,0.0002776464,0.0003098017,0.0002754116,0.0004544551],"domain_scores_gemma":[0.9979436,0.001447226,0.00005600853,0.0002287733,0.0002060117,0.0001183334],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008083683,0.00005113681,0.9912233,0.00002930837,0.00001724017,0.000003084547,0.001078963,7.240776e-7,0.0002145857,0.001493256,0.000322788,0.005484797],"study_design_scores_gemma":[0.0003165927,0.0001643094,0.9166277,0.00001107886,0.00001557873,0.00001023018,0.001064803,0.0001187716,0.00011935,0.08069108,0.0007657526,0.00009473791],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9933095,0.0008456642,0.00003479412,0.003081971,0.000009912891,0.0003264608,0.000415709,0.00001035455,0.001965649],"genre_scores_gemma":[0.999016,0.0001074322,0.0002967457,0.00009851071,0.00004522072,0.00001790258,0.0002567118,0.000002792866,0.0001587262],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07919783,"threshold_uncertainty_score":0.9776871,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1968974268","doi":"10.1016/j.gr.2008.08.001","title":"A Kaapvaal craton debate: Nucleus of an early small supercontinent or affected by an enhanced accretion event?","year":2008,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Pretoria; National Research Foundation","keywords":"Craton; Geology; Supercontinent; Obduction; Geochemistry; Terrane; Snowball Earth; Paleontology; Earth science; Subduction; Oceanic crust; Tectonics; Glacial period","retraction":null,"screen_n_in":null,"score":{"opus":0.05054179079020282,"gpt":0.2875017530719866,"spread":0.2369599622817838,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006886404,0.0001569125,0.0002986304,0.0001542921,0.000283795,0.00004578314,0.0004998348,0.0001472686,0.01165862],"category_scores_gemma":[0.0002710628,0.0001043181,0.00009584879,0.0009222458,0.0003409705,0.0002753148,0.00004159987,0.0003652041,0.0002354935],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008187551,"about_ca_system_score_gemma":0.0000772779,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.02598001,"about_ca_topic_score_gemma":0.01826462,"domain_scores_codex":[0.9973286,0.0005264978,0.0003065472,0.0004864437,0.0007010835,0.0006508224],"domain_scores_gemma":[0.9987251,0.0001843718,0.00004885532,0.000331439,0.0002895787,0.0004206587],"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":[0.002377758,0.001348749,0.2808088,0.00008811782,0.0001429707,0.0002719021,0.001301658,0.0003991283,0.5940366,0.00003453354,0.001704826,0.1174849],"study_design_scores_gemma":[0.0007859344,0.003053324,0.8629135,0.0000193044,0.00002155941,0.0000182263,0.0003073512,0.009290715,0.1215995,0.0009097313,0.000768886,0.0003119349],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9980706,0.0001581742,0.00008291146,0.0002066421,0.00002893644,0.0002107046,0.0001105097,0.00004525422,0.001086298],"genre_scores_gemma":[0.997674,0.0001143476,0.0004637589,0.00004130652,0.00006030182,0.000005063481,0.0005357364,0.000004469712,0.001100961],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5821047,"threshold_uncertainty_score":0.9996495,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3124183020","doi":"10.1016/j.gr.2020.12.026","title":"Nanoparticles in fossil and mineral fuel sectors and their impact on environment and human health: A review and perspective","year":2021,"lang":"en","type":"review","venue":"Gondwana Research","topic":"Radioactivity and Radon Measurements","field":"Health Professions","cited_by":64,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba","funders":"","keywords":"Coal; Fossil fuel; Environmental science; Coal mining; Hazardous waste; Human health; Waste management; Mining engineering; Geology; Medicine; Environmental health; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.3748560844717131,"gpt":0.5635187784128814,"spread":0.1886626939411684,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00471453,0.000418673,0.001914358,0.0003053744,0.0008654603,0.00004863096,0.0001191361,0.0002736999,0.0001026297],"category_scores_gemma":[0.000275451,0.0002452045,0.0000971804,0.0003593324,0.0003240092,0.00009727934,0.0003132461,0.002066541,0.000006911225],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001019115,"about_ca_system_score_gemma":0.0006099882,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002196606,"about_ca_topic_score_gemma":0.001317306,"domain_scores_codex":[0.9920171,0.005261858,0.0005957073,0.0008207656,0.0004414873,0.0008630457],"domain_scores_gemma":[0.9977662,0.00113797,0.0001987873,0.0003547207,0.00007000274,0.0004723343],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.00004410875,0.0003537739,0.00383755,0.1304995,0.0004014708,0.00005555362,0.006374551,6.693336e-8,0.00007223118,0.000415913,0.004542789,0.8534025],"study_design_scores_gemma":[0.001576269,0.001382094,0.03729368,0.127102,0.0002187004,0.00007620041,0.005228958,0.000004118231,0.000001569159,0.0002840683,0.8260877,0.0007447219],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"review","genre_gemma":"review","genre_scores_codex":[0.03073156,0.9647753,1.362094e-7,0.001352672,0.00002728618,0.002769313,0.0001111471,0.00001008443,0.0002224739],"genre_scores_gemma":[0.005885886,0.9932554,0.00001314711,0.0001333921,0.00008227323,0.0003080338,0.00001970241,0.00003198082,0.0002701522],"genre_candidate":"review","genre_consensus":"review","teacher_disagreement_score":0.8526577,"threshold_uncertainty_score":0.9999148,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3161127917","doi":"10.1016/j.gr.2021.04.011","title":"Correlation and difference between conventional and unconventional reservoirs and their unified genetic classification","year":2021,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":63,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Unconventional oil; Fossil fuel; Petroleum engineering; Petroleum; Source rock; Buoyancy; Earth science; Petrology; Paleontology; Structural basin; Oil shale; Ecology","retraction":null,"screen_n_in":null,"score":{"opus":0.07867261268472453,"gpt":0.3042439209367194,"spread":0.2255713082519949,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004465002,0.0001069676,0.0001548944,0.0002155118,0.0002188089,0.0001333665,0.00007100527,0.0001032576,0.00008480801],"category_scores_gemma":[0.00009927474,0.00009833675,0.00002929597,0.0004296,0.0002026499,0.0001122958,0.00008817133,0.0002941054,0.00001051576],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00004155007,"about_ca_system_score_gemma":0.00005769522,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00002620468,"about_ca_topic_score_gemma":0.0001099913,"domain_scores_codex":[0.9987629,0.0002087149,0.0002176158,0.0002759419,0.0003219023,0.0002129391],"domain_scores_gemma":[0.9991929,0.0002478143,0.00002083544,0.0001737136,0.0002061078,0.0001586436],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001130055,0.000217689,0.7147689,0.001314135,0.001290718,0.00006742006,0.004224268,0.01075445,0.09748042,0.04152662,0.003553453,0.1246889],"study_design_scores_gemma":[0.0004929891,0.00002887631,0.5952439,0.00003908543,0.00001869745,0.0000101534,0.001045417,0.3943219,0.0007107396,0.006252757,0.001683847,0.0001516062],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9839264,0.002362018,0.01144316,0.001066801,0.0000434043,0.0001239689,0.0000242141,0.00004929413,0.0009607247],"genre_scores_gemma":[0.9971842,0.001282163,0.000225864,0.000009401259,0.00006238469,0.00002175718,0.0001590706,0.00001471137,0.001040433],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3835675,"threshold_uncertainty_score":0.4010056,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2482626957","doi":"10.1016/j.gr.2016.06.007","title":"The Paleoproterozoic Wernecke Supergroup of Yukon, Canada: Relationships to orogeny in northwestern Laurentia and basins in North America, East Australia, and China","year":2016,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs","keywords":"Laurentia; Geology; Craton; Orogeny; Zircon; Supercontinent; Rodinia; Supergroup; Terrane; Archean; Geochemistry; Paleontology; Proterozoic; Foreland basin; Geochronology; Structural basin; Paleozoic; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.04882550167791184,"gpt":0.2525931071196566,"spread":0.2037676054417448,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005782967,0.0000946774,0.0001733642,0.000127459,0.0001519257,0.00003000533,0.0002220901,0.00004297001,0.0005579692],"category_scores_gemma":[0.0002614506,0.00004975289,0.00002012256,0.0008433411,0.0002866109,0.00007353443,0.00005864303,0.0002656127,0.00002537298],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001192286,"about_ca_system_score_gemma":0.00007647237,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8379681,"about_ca_topic_score_gemma":0.9994184,"domain_scores_codex":[0.9983642,0.0002687885,0.000253434,0.0002867271,0.000385416,0.0004415096],"domain_scores_gemma":[0.9991193,0.0004078012,0.00002886636,0.0001777007,0.00005663239,0.0002096468],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003469316,0.00001095317,0.9797026,0.00000813413,0.000007060801,0.00001337475,0.0001541558,0.00002440059,0.0000478956,0.00001709345,0.00006872974,0.0199109],"study_design_scores_gemma":[0.0001637666,0.00007416948,0.9970468,0.00001727065,0.000002880043,0.000002059483,0.0002635994,0.0001601034,0.00002210544,0.0004355492,0.001736392,0.00007529052],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9957565,0.0003615819,0.000003173073,0.003424731,0.00001353985,0.0001360942,0.0001602543,0.000002804552,0.0001412985],"genre_scores_gemma":[0.9993879,0.0001093568,0.00004573945,0.00002159031,0.00001378529,0.000005143379,0.00002426768,0.000001505831,0.0003907717],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1614503,"threshold_uncertainty_score":0.6109372,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2011888263","doi":"10.1016/j.gr.2010.11.019","title":"A comparison of the evolution of arc complexes in Paleozoic interior and peripheral orogens: Speculations on geodynamic correlations","year":2010,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada; St. Francis Xavier University","funders":"Natural Resources Canada; Consejo Nacional de Investigaciones Científicas y Técnicas; Killam Trusts; St. Francis Xavier University","keywords":"Geology; Gondwana; Ordovician; Paleozoic; Paleontology; Subduction; Terrane; Baltica; Laurentia; Obduction; Continental margin; Oceanic crust; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.04667226557358047,"gpt":0.3228391075592415,"spread":0.276166841985661,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003455336,0.00005674794,0.0001594867,0.0001289355,0.000122343,0.00001173591,0.0001856686,0.00005273128,0.002637519],"category_scores_gemma":[0.0002616907,0.00003511093,0.00005394669,0.0005814924,0.0005143507,0.0000352137,0.00003691476,0.0003944743,0.0000142902],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007439396,"about_ca_system_score_gemma":0.00003673341,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.009456586,"about_ca_topic_score_gemma":0.1002408,"domain_scores_codex":[0.9989973,0.0001396891,0.0002301979,0.0001495923,0.0003005472,0.0001826361],"domain_scores_gemma":[0.9993317,0.0003036903,0.00005195009,0.0001683166,0.00009432977,0.00005000007],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002333761,0.00003719257,0.9878695,0.00000905657,0.000006806038,2.88809e-7,0.0001530744,0.001528676,0.007058854,0.00147676,0.00001633708,0.001820117],"study_design_scores_gemma":[0.0001011555,0.00007588613,0.9009041,0.0000137805,0.000004852361,9.802859e-7,0.0004214059,0.09038341,0.0002483912,0.007767657,0.00004275224,0.00003564454],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9966149,0.0001476304,0.00002482081,0.0005468922,0.00003550772,0.0001234702,0.00004097928,0.000003537251,0.002462229],"genre_scores_gemma":[0.9997051,0.000004970977,0.0001629794,0.000006155498,0.00001313147,0.000001375909,0.00002159951,8.732169e-7,0.00008380345],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.09078423,"threshold_uncertainty_score":0.9982742,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1976851313","doi":"10.1016/j.gr.2008.11.005","title":"Influence of supercontinents on deep mantle flow","year":2008,"lang":"en","type":"article","venue":"Gondwana Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Australian Research Council","keywords":"Geology; Supercontinent; Mantle (geology); Mantle convection; Subduction; Hotspot (geology); Geophysics; Mantle wedge; Volcanism; Rift; Mantle plume; Laurasia; Asthenosphere; Geodynamics; Plate tectonics; Earth science; Paleontology; Gondwana; Lithosphere; Tectonics; Craton","retraction":null,"screen_n_in":null,"score":{"opus":0.04766276220774446,"gpt":0.28730719830687,"spread":0.2396444360991255,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005417678,0.00008150988,0.0001657255,0.0001258387,0.0002033387,0.00002162761,0.0003377398,0.0000509315,0.001654462],"category_scores_gemma":[0.0001053455,0.00006426246,0.00003548525,0.0002774526,0.0001972024,0.0001347553,0.0000291308,0.0001496816,0.001448139],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002494644,"about_ca_system_score_gemma":0.00006019135,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004926718,"about_ca_topic_score_gemma":0.0004532186,"domain_scores_codex":[0.9984167,0.0001503382,0.0001709507,0.0002137241,0.0006528929,0.0003953562],"domain_scores_gemma":[0.9992551,0.0001662325,0.00002409031,0.0002871803,0.000153849,0.0001135444],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001252446,0.0005821687,0.6633206,0.0004999376,0.0002290407,0.001170597,0.004605631,0.1353374,0.09946177,0.002655459,0.03195662,0.0589284],"study_design_scores_gemma":[0.0003125376,0.0003036457,0.973249,0.00002966661,0.000003167429,0.000006934337,0.00003878119,0.001619185,0.01143824,0.0007940702,0.01207069,0.0001341069],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.991333,0.0001074081,0.000003867425,0.00009784936,0.00008598628,0.0001388801,0.00008264845,0.00001337955,0.008136972],"genre_scores_gemma":[0.998747,0.0001282266,0.0001865827,0.00003280073,0.00009038122,0.000001665892,0.00003499176,0.000003463825,0.0007749217],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3099284,"threshold_uncertainty_score":0.9993293,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2801120065","doi":"10.1016/j.gr.2018.03.020","title":"Mesozoic and Cenozoic multiple deformations in the Helanshan Tectonic Belt, Northern China","year":2018,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"National Key Research and Development Program of China; Northwest University; National Natural Science Foundation of China; Northwestern University","keywords":"Geology; Unconformity; Massif; Horst; Paleontology; Cretaceous; Graben; Tectonic phase; Mesozoic; Tectonics; Cenozoic; Phanerozoic; Paleozoic; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.04016320235525352,"gpt":0.2819233158706966,"spread":0.241760113515443,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00121597,0.0000875622,0.0001179546,0.0001540055,0.0004709562,0.00008120506,0.0003932112,0.00005711684,0.003256759],"category_scores_gemma":[0.0003054367,0.00004673065,0.00004077298,0.001018188,0.0004357792,0.00009727542,0.00004538033,0.0003827315,0.0008575568],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000574921,"about_ca_system_score_gemma":0.00003205731,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.02362711,"about_ca_topic_score_gemma":0.3049197,"domain_scores_codex":[0.9984087,0.0002755244,0.0001625106,0.0002278624,0.000431391,0.0004939575],"domain_scores_gemma":[0.9991997,0.0003776881,0.00002061639,0.0002214444,0.00007357592,0.0001069769],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002087142,0.00002599888,0.9738476,0.000008075166,0.000009006631,0.000007420825,0.0007570518,0.00005412674,0.00007320909,0.00003351173,0.0001648899,0.0249982],"study_design_scores_gemma":[0.0001785243,0.0001653609,0.97635,0.00000626139,0.000004745183,0.00001082696,0.000642577,0.01052393,0.00008947267,0.009749849,0.002194254,0.00008416121],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9843654,0.0005679182,0.00001273255,0.002803121,0.00001651565,0.0001548678,0.00003309093,0.00001432539,0.01203202],"genre_scores_gemma":[0.9994392,0.00006194942,0.00006666144,0.0001210766,0.0000846747,0.000004607209,0.00008325426,0.000001421954,0.0001370894],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2812926,"threshold_uncertainty_score":0.9999204,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2538146354","doi":"10.1016/j.gr.2016.09.013","title":"Paleogeographic forcing of the strontium isotopic cycle in the Neoproterozoic","year":2016,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université du Québec à Montréal; McGill University","funders":"Agence Nationale de la Recherche","keywords":"Supercontinent; Geology; Rodinia; Snowball Earth; Gondwana; Continental drift; Paleontology; Glacial period; Phanerozoic; Igneous rock; Earth science; Large igneous province; Continental crust; Continental arc; Sill; Tectonics; Rift; Craton; Cenozoic; Geochemistry; Magmatism","retraction":null,"screen_n_in":null,"score":{"opus":0.03626847208283509,"gpt":0.2660860261113193,"spread":0.2298175540284842,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001233844,0.00006518375,0.0001148095,0.00009407389,0.000151124,0.0000220052,0.000738273,0.00004575377,0.00299905],"category_scores_gemma":[0.0002181793,0.00002232637,0.0001042647,0.0009532493,0.0003600146,0.00005814717,0.00005108161,0.000237824,0.00007791346],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002386929,"about_ca_system_score_gemma":0.00002206498,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.008057032,"about_ca_topic_score_gemma":0.02045809,"domain_scores_codex":[0.9983014,0.0003798069,0.0001720791,0.0001887173,0.0005477103,0.0004102929],"domain_scores_gemma":[0.9990585,0.0004724656,0.00003187931,0.0003331216,0.00005753188,0.0000465197],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001136967,0.00001420925,0.9740614,0.000007307597,0.000006275338,0.000002405614,0.00006039504,0.0000454559,0.000561295,0.000149674,0.00008007033,0.02500012],"study_design_scores_gemma":[0.0001374894,0.00005919506,0.9742868,0.00001923384,0.000003375887,0.00000127444,0.0001801763,0.0003098422,0.0004850515,0.02368448,0.0007916693,0.00004142334],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.987712,0.0003630129,0.00001596373,0.006518859,0.00002738142,0.0001832611,0.00001249504,0.00000459745,0.005162463],"genre_scores_gemma":[0.99955,0.00004208506,0.00002615322,0.00008114592,0.00003822859,0.000004855403,0.000002323656,8.2834e-7,0.000254329],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02495869,"threshold_uncertainty_score":0.9985484,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2076961975","doi":"10.1016/j.gr.2014.01.015","title":"U–Pb geochronology and Hf-isotopes on detrital zircons of Lower Paleozoic strata from Hainan Island: New clues for the early crustal evolution of southeastern South China","year":2014,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Polytechnique Montréal","funders":"Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Supercontinent; Rodinia; Gondwana; Zircon; Geochronology; Paleozoic; Orogeny; Paleontology; Large igneous province; Geochemistry; Population; Ordovician; Clastic rock; Sedimentary rock; Craton; Magmatism; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.02932955624694453,"gpt":0.2560572781357638,"spread":0.2267277218888193,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006546716,0.0001201646,0.0002904202,0.0001252745,0.0001823801,0.00003488019,0.0003564669,0.0001128904,0.001291907],"category_scores_gemma":[0.0004894696,0.00006962039,0.0001118542,0.0002594943,0.0006503406,0.00006144605,0.00005717633,0.0002608887,0.00004049806],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002521053,"about_ca_system_score_gemma":0.00006229302,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.03936163,"about_ca_topic_score_gemma":0.03155496,"domain_scores_codex":[0.9984342,0.0002002767,0.0002576793,0.000329451,0.0003728429,0.0004054854],"domain_scores_gemma":[0.9982474,0.001152867,0.00008358437,0.0002804606,0.0001027238,0.0001329102],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001217135,0.0001119147,0.9283772,0.00006348065,0.0001895333,0.000004088616,0.001375179,0.0004752625,0.002570139,0.001273777,0.000321891,0.06402041],"study_design_scores_gemma":[0.0006757907,0.001707827,0.9473861,0.00002621836,0.00004245137,0.000001303332,0.001067815,0.007485189,0.0008816806,0.04023095,0.0003692122,0.0001254901],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9946014,0.00124582,0.001808194,0.0007681674,0.00004525849,0.0002235239,0.0004638687,0.000008488058,0.0008353086],"genre_scores_gemma":[0.9992497,0.00002550661,0.000258997,0.00001346739,0.0001285321,0.000002338752,0.00005837413,0.000002479802,0.0002605911],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06389492,"threshold_uncertainty_score":0.999621,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1965210690","doi":"10.1016/j.gr.2014.08.018","title":"Geochemistry and petrogenesis of Early Carboniferous volcanic rocks in East Junggar, North Xinjiang: Implications for post-collisional magmatism and geodynamic process","year":2014,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Saint Mary's University","funders":"National Science and Technology Major Project; National Natural Science Foundation of China","keywords":"Geology; Geochemistry; Mafic; Felsic; Volcanic rock; Petrogenesis; Magmatism; Andesite; Carboniferous; Basalt; Petrology; Volcano; Paleontology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.02218413524825652,"gpt":0.2720166370450274,"spread":0.2498325017967709,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000465657,0.0001168559,0.000238673,0.0001531898,0.0001656235,0.0000397774,0.0002369163,0.00008823229,0.0002109862],"category_scores_gemma":[0.0003288025,0.00009178917,0.00004869581,0.0005046384,0.0002404007,0.00007127039,0.00005057719,0.0001912364,0.000006621542],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006004687,"about_ca_system_score_gemma":0.00008327483,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.007254156,"about_ca_topic_score_gemma":0.03281011,"domain_scores_codex":[0.998593,0.00006962999,0.0002475907,0.0003877147,0.0002811422,0.0004209719],"domain_scores_gemma":[0.9988958,0.0003858574,0.00005214035,0.0001780322,0.0002867225,0.0002014471],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006149836,0.00003161395,0.9803824,0.0001289623,0.00001622627,0.000001011147,0.0000822674,0.0001372136,0.001188698,0.00003891142,0.0000193871,0.01791182],"study_design_scores_gemma":[0.0002644761,0.0001717084,0.9798644,0.00001569811,0.0000135166,0.000007771899,0.0001064478,0.01211393,0.0001412699,0.007146983,0.00004484823,0.000108931],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9968578,0.0009159904,0.00004040473,0.001102519,0.000007282505,0.0002109411,0.0002772428,0.000008729745,0.0005790591],"genre_scores_gemma":[0.9993793,0.00006379423,0.0001727707,0.0000252222,0.00002754979,0.00001792786,0.0001710159,0.000003078937,0.0001393801],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02555596,"threshold_uncertainty_score":0.9993566,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1028072543","doi":"10.1016/j.gr.2015.05.014","title":"Rifting, subduction and collisional records from pluton petrogenesis and geochronology in the Hindu Kush, NW Pakistan","year":2015,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of Peshawar; National Science Foundation","keywords":"Geology; Geochronology; Pluton; Terrane; Gondwana; Subduction; Anatexis; Tectonics; Geochemistry; Rift; Paleontology; Petrogenesis; Earth science; Partial melting; Mantle (geology)","retraction":null,"screen_n_in":null,"score":{"opus":0.0896012696715825,"gpt":0.3235706739444954,"spread":0.2339694042729129,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001831242,0.00009304945,0.000163893,0.0001308041,0.0001954062,0.00009484421,0.0002396606,0.000104047,0.001754452],"category_scores_gemma":[0.0003640241,0.00005593732,0.00002652287,0.0005182375,0.0003782802,0.00009015523,0.00006253374,0.000354609,0.00008336658],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001044269,"about_ca_system_score_gemma":0.00005967047,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.07698026,"about_ca_topic_score_gemma":0.05577223,"domain_scores_codex":[0.9981139,0.0004676844,0.0001774003,0.0003588072,0.000505436,0.0003768103],"domain_scores_gemma":[0.9989173,0.0006255739,0.00002932212,0.000158923,0.00009634162,0.0001724839],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009997312,0.0000250932,0.9710364,0.000004208726,0.00001301877,0.00003108184,0.0003795189,0.00003516587,0.00007188041,0.0001425238,0.001216097,0.02694506],"study_design_scores_gemma":[0.0003341031,0.000217144,0.9525785,0.000005789807,0.000009726539,0.00001700425,0.002276172,0.003711481,0.00009607566,0.03120705,0.009444403,0.0001025607],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9899715,0.00287941,0.000004542765,0.004622112,0.00004548805,0.00009480714,0.00005434227,0.000009596873,0.002318193],"genre_scores_gemma":[0.9989796,0.0002485949,0.0002798451,0.00010192,0.0001132004,0.000003263764,0.0001192307,0.000001438275,0.0001529216],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03106453,"threshold_uncertainty_score":0.9991581,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2078736667","doi":"10.1016/j.gr.2014.08.007","title":"Role of crustal contribution in the early stage of the Damara Orogen, Namibia: New constraints from combined U–Pb and Lu–Hf isotopes from the Goas Magmatic Complex","year":2014,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Rio Tinto; Universiteit Stellenbosch","keywords":"Geology; Geochronology; Zircon; Craton; Geochemistry; Subduction; Diorite; Magma; Tectonics; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.03192923434763661,"gpt":0.2576266414898989,"spread":0.2256974071422623,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001354444,0.0001084771,0.0002793234,0.00003207921,0.0001887455,0.00006622196,0.0007181635,0.00007764272,0.00448925],"category_scores_gemma":[0.0008701916,0.00004801696,0.00008478495,0.0004786428,0.001030183,0.00006068836,0.0001059053,0.0003774339,0.00003553841],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004062476,"about_ca_system_score_gemma":0.00005776979,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1305769,"about_ca_topic_score_gemma":0.04707627,"domain_scores_codex":[0.9974881,0.0009793249,0.0003182841,0.0002338526,0.000648972,0.0003314071],"domain_scores_gemma":[0.9965222,0.002812345,0.00009791264,0.0003583822,0.0001220036,0.00008715704],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001060972,0.00004318467,0.9782449,0.000008334419,0.00005086874,0.000001609615,0.0006022039,0.00004994105,0.006277553,0.001075016,0.0005186461,0.01302165],"study_design_scores_gemma":[0.0005346608,0.0001288771,0.9540446,0.00002268676,0.00001906077,4.97073e-7,0.001653585,0.004825393,0.0009410455,0.0370834,0.0006843895,0.00006176042],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9937427,0.0005819525,0.00002687845,0.003502433,0.00001462245,0.0003185339,0.0006255041,0.000004713801,0.00118266],"genre_scores_gemma":[0.9994021,0.0000346551,0.00008659731,0.0001885975,0.00003730744,0.000001774507,0.0001693773,0.00000148933,0.00007811888],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08350063,"threshold_uncertainty_score":0.9964208,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2921153176","doi":"10.1016/j.gr.2019.01.019","title":"Timing and mechanism of Bangong-Nujiang ophiolite emplacement in the Gerze area of central Tibet","year":2019,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Université Laval","funders":"Fundamental Research Funds for the Central Universities; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Ophiolite; Terrane; Geology; Geochemistry; Subduction; Foreland basin; Ultramafic rock; Obduction; Peridotite; Lithosphere; Oceanic crust; Paleontology; Mantle (geology); Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.06704472527705056,"gpt":0.2860825376738281,"spread":0.2190378123967775,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001161334,0.00006586401,0.0001782913,0.0001159853,0.00004331248,0.00001613016,0.0002691527,0.00004660962,0.004712726],"category_scores_gemma":[0.00008016617,0.00003763343,0.00004639776,0.0004553577,0.00012238,0.00004668529,0.00004609915,0.0002013472,0.00004584032],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003010482,"about_ca_system_score_gemma":0.00002182094,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005943076,"about_ca_topic_score_gemma":0.001906813,"domain_scores_codex":[0.9985812,0.0001887894,0.0001938298,0.0001874909,0.0004713671,0.0003773106],"domain_scores_gemma":[0.9992676,0.0003927799,0.00003593134,0.0001768197,0.00005682334,0.00007001351],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001070446,0.00006493035,0.9833044,0.0001086839,0.00003449942,0.0000134596,0.0009297189,0.0003884595,0.005296115,0.002656031,0.0004189585,0.006677668],"study_design_scores_gemma":[0.0004032926,0.0003656037,0.958002,0.00004516319,0.00001208461,0.000004667077,0.001658278,0.01177302,0.004340029,0.02223007,0.001047688,0.0001180772],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9904296,0.0003942636,0.000005572786,0.0008029814,0.00002025885,0.0001619321,0.00002863926,0.000002471776,0.008154253],"genre_scores_gemma":[0.9994491,0.00007845926,0.00008154944,0.00005870422,0.00001279709,0.000001081524,0.0000280878,8.962982e-7,0.0002892981],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02530241,"threshold_uncertainty_score":0.9961971,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2998895523","doi":"10.1016/j.gr.2019.12.009","title":"High-resolution LA-ICP-MS mapping of deep-sea polymetallic micronodules and its implications on element mobility","year":2020,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Lakehead University","funders":"Fundamental Research Funds for the Central Universities; National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Geology; Rhodochrosite; Birnessite; Uraninite; Siderite; Mineralogy; Rare-earth element; Trace element; Geochemistry; Authigenic; Calcite; Manganese; Chemistry; Materials science; Uranium; Diagenesis; Rare earth","retraction":null,"screen_n_in":null,"score":{"opus":0.05852188830935499,"gpt":0.2880761938422075,"spread":0.2295543055328525,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006810926,0.0000934088,0.0001541663,0.00008610095,0.0002534406,0.00004110304,0.000225645,0.00004937869,0.002066403],"category_scores_gemma":[0.0000987137,0.00008192084,0.00005283949,0.0005348087,0.0001327289,0.00008187127,0.00005433953,0.0002010219,0.0001084444],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001075635,"about_ca_system_score_gemma":0.00003679081,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002612948,"about_ca_topic_score_gemma":0.0006836144,"domain_scores_codex":[0.99858,0.0001744973,0.0002311665,0.0003386616,0.0003493288,0.0003263582],"domain_scores_gemma":[0.9993225,0.0001680172,0.00004907775,0.0001802427,0.00008399819,0.0001961942],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004516179,0.0004872508,0.5212573,0.0008962717,0.0004983973,0.0000149756,0.001876407,0.005244873,0.2327102,0.003157916,0.002490257,0.2309146],"study_design_scores_gemma":[0.0004695856,0.0003340013,0.9142105,0.00002482179,0.00003088858,0.000003393074,0.001202152,0.02156118,0.05579556,0.001132344,0.005010724,0.0002248775],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9923553,0.001044667,0.00009343218,0.004159969,0.000009781917,0.0001792673,0.0002308435,0.00001460948,0.001912153],"genre_scores_gemma":[0.9991165,0.0001511743,0.0002669374,0.00007360906,0.00004704796,0.000005189398,0.0002643948,0.000002165482,0.00007292048],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3929532,"threshold_uncertainty_score":0.9988458,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2781235931","doi":"10.1016/j.gr.2017.12.003","title":"Amber inclusions from New Zealand","year":2017,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Fossil Insects in Amber","field":"Agricultural and Biological Sciences","cited_by":43,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Royal British Columbia Museum","funders":"Royal Society Te Apārangi","keywords":"Ecology; Biodiversity; Biota; Biology; Ecosystem; Endemism","retraction":null,"screen_n_in":null,"score":{"opus":0.1642364288526373,"gpt":0.3884797060772829,"spread":0.2242432772246456,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000598167,0.00009829268,0.0001281461,0.00001559586,0.001772113,0.0004508353,0.001080937,0.0001242872,0.006554729],"category_scores_gemma":[0.0006165688,0.00003487154,0.00005999783,0.0001548464,0.000296742,0.0001936867,0.001011059,0.0004125735,0.001333159],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00004688149,"about_ca_system_score_gemma":0.00004265914,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1053427,"about_ca_topic_score_gemma":0.03839618,"domain_scores_codex":[0.9982367,0.0001345216,0.0001271397,0.0003472766,0.0006437202,0.0005106782],"domain_scores_gemma":[0.9987984,0.0004362788,0.0000490176,0.000315456,0.0001201016,0.0002807293],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"not_applicable","study_design_gemma":"observational","study_design_scores_codex":[0.00006321399,0.00008760253,0.0518603,0.000001488098,0.00002184751,0.00005321792,0.0002859607,5.093917e-7,0.1487678,0.00050252,0.5347225,0.263633],"study_design_scores_gemma":[0.0001379078,0.00007349036,0.6296561,0.00001621894,0.0000021553,0.000001809779,0.00006348619,0.00001978397,0.001970188,0.01178439,0.3561684,0.0001060659],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9420865,0.0001272115,3.623242e-7,0.01034752,0.0001828294,0.0001414214,0.00004966027,0.00004085755,0.04702366],"genre_scores_gemma":[0.9335432,0.00004918008,0.0001520608,0.000108881,0.0009687568,0.000007934572,0.00002663703,0.000001234948,0.06514212],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5777959,"threshold_uncertainty_score":0.9995275,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2112002313","doi":"10.1016/j.gr.2014.08.009","title":"Peri-Gondwanan terrane interactions recorded in the Cambrian–Ordovician detrital zircon geochronology of North Wales","year":2014,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK; Division of Orthopaedic Surgery, University of Alberta; University of Alberta","keywords":"Geology; Ordovician; Terrane; Paleontology; Provenance; Precambrian; Detritus; Zircon; Supergroup; Sedimentary rock; Geochronology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.05317121172022166,"gpt":0.2942191832182584,"spread":0.2410479714980368,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001219508,0.0001288333,0.0002839789,0.0003592632,0.000224083,0.00004304593,0.0006844758,0.00007200452,0.005177627],"category_scores_gemma":[0.0007081265,0.00007987699,0.0001175458,0.001285949,0.0004786515,0.0001129985,0.00005329091,0.0006500007,0.0003731888],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009945901,"about_ca_system_score_gemma":0.00004948337,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.04902553,"about_ca_topic_score_gemma":0.5794181,"domain_scores_codex":[0.997521,0.0007205127,0.000351091,0.0003526599,0.0004578972,0.0005968327],"domain_scores_gemma":[0.9982055,0.00110164,0.00006285518,0.0003726555,0.0001413075,0.0001160044],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005710244,0.00007750779,0.8950035,0.00001867542,0.00002102285,0.00001479588,0.0002224878,0.00008910201,0.0006728836,0.0001489677,0.0002918617,0.1033821],"study_design_scores_gemma":[0.0002146576,0.0002860586,0.9861276,0.00001064873,0.00001035565,0.0000132055,0.0006293822,0.002336075,0.0002224903,0.003048408,0.006989775,0.0001113695],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9826118,0.0002058599,0.00005141626,0.0031966,0.00007555183,0.0001544555,0.00003738347,0.00001366135,0.01365321],"genre_scores_gemma":[0.9988706,0.00005345414,0.0003140908,0.0001567699,0.0001062817,0.000006202461,0.0001521649,0.000002406948,0.0003380213],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5303925,"threshold_uncertainty_score":0.9957318,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2020511410","doi":"10.1016/j.gr.2012.03.004","title":"U–Pb geochronological constraints on the Triassic–Jurassic Ayú Complex, southern Mexico: Derivation from the western margin of Pangea-A","year":2012,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Geology; Zircon; Geochemistry; Protolith; Anatexis; Metamorphism; Igneous rock; Continental arc; Island arc; Diorite; Geochronology; Paleozoic; Subduction; Petrology; Partial melting; Paleontology; Volcanic rock; Crust","retraction":null,"screen_n_in":null,"score":{"opus":0.1863149293674407,"gpt":0.3139901249606218,"spread":0.1276751955931812,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001964454,0.0001503192,0.0002678715,0.00005486413,0.0003722711,0.00006610958,0.0007079064,0.0001193263,0.04039202],"category_scores_gemma":[0.0007113295,0.00006412856,0.0001393455,0.000515834,0.001278746,0.00007025256,0.00008614389,0.0005579427,0.001899104],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000920606,"about_ca_system_score_gemma":0.00003759831,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006898517,"about_ca_topic_score_gemma":0.003571134,"domain_scores_codex":[0.9971253,0.0008176974,0.0003072525,0.0002760046,0.0008108107,0.0006629263],"domain_scores_gemma":[0.9957749,0.003451891,0.00009677194,0.0004051015,0.0001098222,0.0001615627],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001790665,0.0001412223,0.8893632,0.000006904096,0.0001129399,0.000004568779,0.0005728241,0.0000595735,0.003709133,0.0005710895,0.006964517,0.09831499],"study_design_scores_gemma":[0.0002540894,0.000127501,0.9843758,0.00001348725,0.00002104339,0.000001696052,0.001253705,0.0005587694,0.001276116,0.006333941,0.005670576,0.0001132126],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9761388,0.000484787,0.00005967374,0.01604993,0.0000511692,0.0002454027,0.0002880376,0.00002096639,0.006661247],"genre_scores_gemma":[0.998512,0.00003494791,0.0001019038,0.0006894042,0.0002115722,0.000006467029,0.0002132059,0.000002683073,0.0002278209],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.09820178,"threshold_uncertainty_score":0.9997146,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3091854134","doi":"10.1016/j.gr.2020.08.019","title":"Silurian-Devonian granites and associated intermediate-mafic rocks along the eastern Kunlun Orogen, western China: Evidence for a prolonged post-collisional lithospheric extension","year":2020,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Saskatchewan","funders":"China Geological Survey; National Natural Science Foundation of China","keywords":"Geology; Mafic; Geochemistry; Petrogenesis; Zircon; Porphyritic; Quartz monzonite; Partial melting; Devonian; Asthenosphere; Petrology; Subduction; Crust; Mantle (geology); Pluton; Quartz; Tectonics; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.08540833622606116,"gpt":0.3091383356754776,"spread":0.2237299994494165,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00136429,0.0002065895,0.0003235505,0.00005931784,0.0006021573,0.0002342016,0.0006029907,0.0001351567,0.001315433],"category_scores_gemma":[0.003727771,0.0001184619,0.0001449702,0.0008576397,0.0003491847,0.0002156058,0.0001716254,0.0005502028,0.0002197869],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009614885,"about_ca_system_score_gemma":0.00009344153,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005808554,"about_ca_topic_score_gemma":0.01223499,"domain_scores_codex":[0.9970816,0.0004426517,0.0003321171,0.0006484986,0.0007891917,0.000705924],"domain_scores_gemma":[0.9971793,0.001713193,0.00008947365,0.0002226076,0.0003955156,0.0003998576],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0005523094,0.00004090645,0.9837558,0.00005422984,0.00006905418,0.00003755669,0.0008160945,0.0002528284,0.0005660517,0.000003504239,0.0004431742,0.01340852],"study_design_scores_gemma":[0.0004035665,0.0008492228,0.9388402,0.00007701802,0.00003817602,0.000006954981,0.0003510653,0.05734881,0.0001152564,0.001063915,0.0007222282,0.0001836009],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9773945,0.003898516,0.00005539717,0.01778433,0.00004705479,0.0006071354,0.0001047548,0.00004411895,0.0000641994],"genre_scores_gemma":[0.998285,0.0001768911,0.0001205966,0.0007714779,0.0001590226,0.00002294574,0.0001429256,0.000006632467,0.0003145344],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05709598,"threshold_uncertainty_score":0.9995975,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2032687833","doi":"10.1016/j.gr.2011.09.016","title":"Geology of the Fuding inlier in southeastern China: Implication for late Paleozoic Cathaysian paleogeography","year":2011,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"Nanjing University","keywords":"Geology; Provenance; Paleozoic; Terrane; Paleontology; Arenite; Permian; Precambrian; Zircon; Geochemistry; Basement; Siliciclastic; Paleocurrent; Craton; Ordovician; Conglomerate; Sedimentary rock; Clastic rock; Structural basin; Facies; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.06755550641946317,"gpt":0.2795403768170003,"spread":0.2119848703975372,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008475825,0.00008378577,0.0001683687,0.0001936653,0.0001369154,0.000009671471,0.0004710054,0.00008497606,0.001701279],"category_scores_gemma":[0.0001379021,0.00004903487,0.0001319175,0.0008956653,0.00032444,0.00004542135,0.00005364644,0.0002486758,0.00005390177],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001694303,"about_ca_system_score_gemma":0.00002387733,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01077905,"about_ca_topic_score_gemma":0.01421529,"domain_scores_codex":[0.9986262,0.0001719414,0.0002331368,0.0002691668,0.0002403631,0.0004591637],"domain_scores_gemma":[0.9993289,0.0001621111,0.00005898712,0.0002749255,0.00009381562,0.00008133672],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003851941,0.00003207303,0.9909927,0.00001768183,0.00001373612,8.270942e-7,0.000350491,0.00003707146,0.0003689482,0.0002108378,0.00001106194,0.007926013],"study_design_scores_gemma":[0.0001484005,0.0000841935,0.9518828,0.000007471523,0.000006600302,9.376995e-7,0.0001583683,0.001167097,0.0006556513,0.04569205,0.0001359135,0.00006051831],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9923131,0.0003062336,0.0000247124,0.0006071814,0.00002754957,0.0002640659,0.00003149775,0.000007478596,0.006418194],"genre_scores_gemma":[0.99955,0.00002909193,0.0001959429,0.0000255824,0.0000257797,0.00001250751,0.00002620553,0.000001754139,0.0001331554],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04548121,"threshold_uncertainty_score":0.9992113,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1992819492","doi":"10.1016/j.gr.2009.08.007","title":"The high-pressure Iberian–Czech belt in the Variscan orogen: Extrusion into the upper (Gondwanan) plate?","year":2009,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Saint Mary's University; St. Mary's University; Dalhousie University; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Consejo Nacional de Ciencia y Tecnología","keywords":"Geology; Massif; Subduction; Metamorphism; Ophiolite; Nappe; Gondwana; Paleontology; Obduction; Passive margin; Blueschist; Geochemistry; Fibrous joint; Petrology; Eclogite; Tectonics; Oceanic crust; Rift","retraction":null,"screen_n_in":null,"score":{"opus":0.02471974025735018,"gpt":0.2775801371151272,"spread":0.2528603968577771,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004249402,0.000201555,0.0002294234,0.0001156313,0.001749044,0.000353997,0.002025341,0.0001591789,0.005896744],"category_scores_gemma":[0.0004537841,0.00007602597,0.000141218,0.001590958,0.0005539132,0.00013217,0.0001183604,0.00118177,0.0006812399],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009713595,"about_ca_system_score_gemma":0.00008004299,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.02654212,"about_ca_topic_score_gemma":0.03478832,"domain_scores_codex":[0.9956983,0.001106524,0.0003493888,0.0004823329,0.001387371,0.0009760597],"domain_scores_gemma":[0.9972263,0.001612036,0.00005493226,0.0007986632,0.0001462016,0.00016188],"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":[0.000637785,0.0002702479,0.1863651,0.0000267291,0.0001809203,0.0002083383,0.005216981,0.002623344,0.001870626,0.01069152,0.03576962,0.7561387],"study_design_scores_gemma":[0.0002835827,0.0003064043,0.6896628,0.00001242413,0.00003121415,0.00001382971,0.002156258,0.003352547,0.0004473827,0.1749986,0.1285155,0.000219428],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9100671,0.006137244,0.000007286826,0.07041893,0.00009208803,0.0004000212,0.0000182303,0.00002658792,0.01283253],"genre_scores_gemma":[0.9961986,0.0006091344,0.0001051579,0.00106428,0.0001940321,0.000009422176,0.00006778979,0.000003010795,0.001748563],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7559193,"threshold_uncertainty_score":0.9995505,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2036630392","doi":"10.1016/j.gr.2013.08.025","title":"Palaeoproterozoic orogenic gold style mineralization at the Southwestern Archaean Tanzanian cratonic margin, Lupa Goldfield, SW Tanzania: Implications from U–Pb titanite geochronology","year":2013,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Mylonite; Geology; Geochemistry; Shear zone; Archean; Hornblende; Geochronology; Greenschist; Greenstone belt; Metamorphic rock; Quartz; Biotite; Seismology; Paleontology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.03429234600400339,"gpt":0.2590792806654169,"spread":0.2247869346614135,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005446778,0.0002521679,0.0003052166,0.00016617,0.0005857957,0.0002005086,0.0009383628,0.0002209154,0.08098787],"category_scores_gemma":[0.0001947934,0.0001594881,0.0001694518,0.0009976216,0.0005958611,0.0001971218,0.0002660477,0.0006654477,0.010534],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003821501,"about_ca_system_score_gemma":0.00008450332,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.07600757,"about_ca_topic_score_gemma":0.2141456,"domain_scores_codex":[0.9967518,0.0004877693,0.0004272097,0.000732013,0.0005917372,0.001009436],"domain_scores_gemma":[0.997766,0.0006350198,0.0001012884,0.0008453291,0.0003184735,0.0003339142],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006402244,0.0001010789,0.9104548,0.00002778315,0.0002210892,0.00002158746,0.0005856699,0.0002425665,0.0309522,0.0005487347,0.01306492,0.04371557],"study_design_scores_gemma":[0.0003881035,0.0001911289,0.9566333,0.00001203973,0.00004326936,0.00001627865,0.0004840606,0.003285214,0.0009204353,0.02697296,0.01074981,0.0003033813],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.979794,0.001460657,0.0001410945,0.01118569,0.00006815333,0.0006514327,0.0002907893,0.00006411481,0.006344066],"genre_scores_gemma":[0.9925954,0.000177599,0.0002678228,0.0006128785,0.0001921042,0.00007532859,0.001073937,0.000009423309,0.004995516],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1381381,"threshold_uncertainty_score":0.9902364,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2087233605","doi":"10.1016/j.gr.2014.11.007","title":"Multiple subduction cycles in the Alpine orogeny, as recorded in single zircon crystals (Rhodope zone, Greece)","year":2014,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Zircon; Geology; Geochemistry; Metamorphism; Protolith; Orogeny; Metamorphic rock; Gneiss; Subduction; Geochronology; Alpine orogeny; Petrology; Paleontology; Tectonics; Mesozoic","retraction":null,"screen_n_in":null,"score":{"opus":0.07214562735291068,"gpt":0.2949074988036245,"spread":0.2227618714507138,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003384774,0.0001280308,0.0002319636,0.0002781527,0.0001719384,0.00008789231,0.0005107796,0.0001065723,0.00532299],"category_scores_gemma":[0.001391577,0.00007925712,0.00007436836,0.001443024,0.0002277356,0.0001428302,0.00004718317,0.0005062657,0.0007682616],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001327219,"about_ca_system_score_gemma":0.00002903978,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.08231683,"about_ca_topic_score_gemma":0.1762099,"domain_scores_codex":[0.9969243,0.001080281,0.0003097226,0.0004161613,0.0006259278,0.0006436369],"domain_scores_gemma":[0.9983274,0.00110609,0.00004141633,0.000310194,0.00009531988,0.000119523],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002243405,0.0002486645,0.7863891,0.00003139055,0.00001506432,0.0000566881,0.0004271707,0.001980406,0.01509877,0.0001633404,0.001314831,0.1940502],"study_design_scores_gemma":[0.001002413,0.0007335276,0.8919052,0.00004020212,0.00001012731,0.00002779346,0.001777277,0.02757697,0.006509629,0.03773109,0.03232132,0.0003644465],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9856879,0.000461111,0.00004887436,0.003678533,0.00004629825,0.000218522,0.00001000089,0.00001853131,0.009830266],"genre_scores_gemma":[0.9986786,0.0001221962,0.0003801813,0.0001844007,0.0001117911,0.000006868073,0.0001116846,0.000002768885,0.0004014967],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1936858,"threshold_uncertainty_score":0.9955863,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2038388972","doi":"10.1016/s1342-937x(05)70885-6","title":"The Hypothetical Mesoproterozoic Supercontinent Columbia: Implications of the Siberian-West Laurentian Connection","year":2002,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Queen's University","funders":"","keywords":"Supercontinent; Laurentia; Geology; Craton; Rodinia; Proterozoic; Rift; Paleontology; Facies; Paleozoic; Tectonics; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.05460669095689438,"gpt":0.2587566734589394,"spread":0.204149982502045,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007112192,0.00007045353,0.0001244265,0.0000334749,0.0008285399,0.0001171326,0.0005815789,0.00006604465,0.02615456],"category_scores_gemma":[0.0004541151,0.00003848191,0.000130945,0.0007649601,0.0007093334,0.00004738993,0.00006140949,0.000342288,0.0004342554],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005863883,"about_ca_system_score_gemma":0.00001650307,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01326081,"about_ca_topic_score_gemma":0.1344284,"domain_scores_codex":[0.9983171,0.0003255095,0.0002305779,0.0002341567,0.0004724997,0.0004201857],"domain_scores_gemma":[0.9986728,0.0005639908,0.00003689183,0.0004215354,0.0001872416,0.0001175263],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002433808,0.00015599,0.8853242,0.00001815781,0.00007987337,0.000002222064,0.000148068,0.00008067954,0.002632594,0.001574244,0.02779026,0.08216935],"study_design_scores_gemma":[0.0001451991,0.00009701007,0.949122,0.000007039769,0.00001775056,0.000007815318,0.0002145998,0.002107466,0.0006236828,0.02121139,0.02636453,0.00008153486],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9540669,0.0008225421,0.000008853363,0.03027416,0.00007811088,0.0002933657,0.0000543299,0.00001604742,0.01438573],"genre_scores_gemma":[0.9969879,0.0001231884,0.00003347039,0.00008373639,0.00006027146,0.00001056842,0.00001662465,0.000001817051,0.002682429],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1211676,"threshold_uncertainty_score":0.99331,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3111001588","doi":"10.1016/j.gr.2020.10.018","title":"Early Paleozoic tectonic transition from oceanic to continental subduction in the North Qaidam tectonic belt: Constraints from geochronology and geochemistry of syncollisional magmatic rocks","year":2020,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Waterloo","funders":"Fundamental Research Funds for the Central Universities; Natural Science Foundation of Anhui Province; China Scholarship Council; National Natural Science Foundation of China","keywords":"Geology; Subduction; Geochemistry; Mantle wedge; Partial melting; Zircon; Geochronology; Mafic; Oceanic crust; Continental crust; Adakite; Petrology; Mantle (geology); Continental arc; Tectonics; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.02438032434858287,"gpt":0.244080197287967,"spread":0.2196998729393841,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003931481,0.000149184,0.0003163918,0.00009790708,0.0001373893,0.00004569762,0.000385618,0.0001249092,0.007564695],"category_scores_gemma":[0.0002780985,0.0001041341,0.00008280809,0.0008040455,0.0004559246,0.00008364876,0.0000474924,0.0005779256,0.0001251275],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001048035,"about_ca_system_score_gemma":0.00007131701,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01617069,"about_ca_topic_score_gemma":0.01349223,"domain_scores_codex":[0.9978823,0.0002875712,0.0003517771,0.0004880643,0.0005623586,0.0004279285],"domain_scores_gemma":[0.9987775,0.0006877622,0.00005551706,0.0001874406,0.00009052136,0.0002012443],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0005186028,0.0001434316,0.9492247,0.00007543032,0.0001223371,0.0001011948,0.002458216,0.0006698509,0.01880113,0.00001346298,0.0002760378,0.02759563],"study_design_scores_gemma":[0.0005278618,0.0003121209,0.9879774,0.00002889469,0.00002865827,0.000005623811,0.001114257,0.005254822,0.001659359,0.002894381,0.00005929967,0.0001372694],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9939018,0.0009037317,0.00006543494,0.003936472,0.00001979853,0.0002627803,0.0005131171,0.00001418534,0.0003827107],"genre_scores_gemma":[0.9988012,0.00007185206,0.0001477677,0.0001913379,0.00008963324,0.000005754033,0.0006842071,0.000002500565,0.000005778087],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03875277,"threshold_uncertainty_score":0.9933425,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1998998540","doi":"10.1016/j.gr.2012.02.007","title":"Sampling oxygenated Archean hydrosphere: Implications from fractionations of Th/U and Ce/Ce* in hydrothermally altered volcanic sequences","year":2012,"lang":"en","type":"article","venue":"Gondwana Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Geochemistry; Terrane; Archean; Mafic; Felsic; Igneous rock; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.1052892130528405,"gpt":0.3318998387876512,"spread":0.2266106257348107,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008182079,0.00009694944,0.0001806247,0.0001808252,0.0001893769,0.0000340197,0.0002601983,0.00008361044,0.009560389],"category_scores_gemma":[0.0002641717,0.00007479732,0.00004898188,0.0009935793,0.0002780414,0.0002042845,0.00004325593,0.000352345,0.0001105322],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001231017,"about_ca_system_score_gemma":0.00007249988,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.05091671,"about_ca_topic_score_gemma":0.01966699,"domain_scores_codex":[0.998397,0.0002091515,0.0002802979,0.0002674434,0.0003604332,0.0004857076],"domain_scores_gemma":[0.998648,0.0007706359,0.00005747376,0.0001969562,0.0001121047,0.0002147888],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002118762,0.00007110342,0.9749507,0.000009955592,0.00003457216,7.992838e-7,0.000290152,0.0007996961,0.01292051,0.0005394145,0.00009033758,0.01027162],"study_design_scores_gemma":[0.0001304226,0.00003492979,0.9429125,0.00001054744,0.000008052792,0.000002215512,0.0002941929,0.005706442,0.0008925529,0.04920634,0.0007065867,0.00009517316],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9908004,0.001322832,0.00008260788,0.001870631,0.00002480911,0.0001458908,0.0001525255,0.00001601931,0.005584307],"genre_scores_gemma":[0.9980282,0.0001583371,0.001283223,0.00005831822,0.00007778778,0.000007377081,0.000271404,0.000002556025,0.0001128536],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04866692,"threshold_uncertainty_score":0.9982215,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}