{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":2700,"total_is_capped":false,"direct_labels_cover":1,"predictions_cover":2700,"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":"ce1286224ff2","filters":{"topic":"Geological formations and processes"}},"results":[{"id":"W2050440902","doi":"10.1016/j.earscirev.2008.10.003","title":"Towards the standardization of sequence stratigraphy","year":2008,"lang":"en","type":"article","venue":"Earth-Science Reviews","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":1451,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto; Dalhousie University; Queen's University; University of Saskatchewan; University of Alberta","funders":"","keywords":"Sequence stratigraphy; Sequence (biology); Paleontology; Geology; Sedimentary depositional environment; Stratigraphic unit; Stratigraphy; Facies; Structural basin; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.08958100715150681,"gpt":0.277733464963282,"spread":0.1881524578117752,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001153877,0.00007919234,0.0001604191,0.00005850714,0.0004617225,0.00003371365,0.0004019612,0.00002151344,0.001223773],"category_scores_gemma":[0.0002557987,0.00003924741,0.00006160441,0.001260977,0.0008528565,0.0004881839,0.000009732249,0.00007634842,0.0001125909],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001119321,"about_ca_system_score_gemma":0.0001903187,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001435773,"about_ca_topic_score_gemma":0.0001783072,"domain_scores_codex":[0.9989045,0.00006838806,0.0002983317,0.0001486017,0.0003879407,0.000192185],"domain_scores_gemma":[0.9994128,0.00004217453,0.000146346,0.0002124987,0.0001189295,0.0000672911],"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":[0.00002017586,0.00004966299,0.1044504,0.0002531047,0.00001051886,0.000008114921,0.00264484,0.004858171,0.01222464,0.01164622,0.0009953203,0.8628388],"study_design_scores_gemma":[0.000154316,0.000429572,0.5176699,0.0001098885,0.00001715468,0.0001286558,0.0002058183,0.002371855,0.01771073,0.005158569,0.4557061,0.0003375011],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.4370055,0.07028928,0.2294906,0.002248488,0.001052097,0.002404983,0.0002537964,0.0001529184,0.2571024],"genre_scores_gemma":[0.9764801,0.01130583,0.01196271,0.0001560112,0.00002291836,0.000001800374,0.000008442127,6.141196e-7,0.00006160164],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8625013,"threshold_uncertainty_score":0.9996892,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2094581504","doi":"10.1016/j.earscirev.2006.10.002","title":"Morphologic and facies trends through the fluvial–marine transition in tide-dominated depositional systems: A schematic framework for environmental and sequence-stratigraphic interpretation","year":2007,"lang":"en","type":"article","venue":"Earth-Science Reviews","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":957,"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":"Geology; Fluvial; Sedimentary depositional environment; Facies; Sediment transport; Estuary; Sedimentary rock; Sediment; Transition zone; Progradation; Delta; Barrier island; Dominance (genetics); Oceanography; Geomorphology; Paleontology; Structural basin; Geochemistry; Shore","retraction":null,"screen_n_in":null,"score":{"opus":0.03173022157433312,"gpt":0.2743300068193711,"spread":0.242599785245038,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001385232,0.0001171171,0.0001907527,0.0001010857,0.0003409259,0.0001115226,0.0001201873,0.00005392416,0.000182526],"category_scores_gemma":[0.0001206004,0.0000683105,0.00003420437,0.0004291192,0.0004767474,0.0005915202,0.000009611966,0.0001217879,0.00001152365],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004197595,"about_ca_system_score_gemma":0.00001476935,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00008480284,"about_ca_topic_score_gemma":0.0002909502,"domain_scores_codex":[0.9989396,0.00007378469,0.0003684595,0.0002218818,0.0001698843,0.000226331],"domain_scores_gemma":[0.9994453,0.0002791342,0.000118256,0.0000888004,0.00001404839,0.00005446214],"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":[0.000175583,0.0001091727,0.03936081,0.0009720659,0.00001993568,0.00001675444,0.01021464,0.002007045,0.01458129,0.01341535,0.00002737232,0.9191],"study_design_scores_gemma":[0.0008969813,0.001278732,0.8404095,0.0009246093,0.00009115295,0.0007038737,0.004530365,0.09714241,0.002575945,0.04552109,0.005099435,0.0008259515],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8872718,0.01258277,0.09709418,0.0005223889,0.0001111935,0.0008764731,0.00006815986,0.00002181799,0.001451251],"genre_scores_gemma":[0.9740626,0.002319819,0.02332675,0.0001703602,0.00001543495,0.00001700645,0.00006463099,0.000001082001,0.00002228225],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.918274,"threshold_uncertainty_score":0.2785621,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2113298788","doi":"10.2110/jsr.2006.060","title":"Width and Thickness of Fluvial Channel Bodies and Valley Fills in the Geological Record: A Literature Compilation and Classification","year":2006,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":733,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Fluvial; Channel (broadcasting); Geomorphology; Paleontology; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.05917683243658815,"gpt":0.3006360911779547,"spread":0.2414592587413665,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001609512,0.00005221092,0.000115349,0.0001456451,0.0001420361,0.00006648161,0.00008647979,0.000054959,0.00008370757],"category_scores_gemma":[0.00005490142,0.00002765206,0.00001231775,0.0001491024,0.0002085611,0.000302735,0.00001499577,0.000299093,8.694818e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002088238,"about_ca_system_score_gemma":0.00001645172,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0003365466,"about_ca_topic_score_gemma":0.000334028,"domain_scores_codex":[0.9990298,0.000238541,0.0002456447,0.00007681195,0.0002893025,0.0001198988],"domain_scores_gemma":[0.9991926,0.000508917,0.00009190068,0.00003890173,0.0001329928,0.00003471434],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002458103,0.00004979972,0.9852562,0.00008144842,0.000008552576,0.00001325383,0.001955923,0.0001848034,0.0001438686,0.0001697165,0.0008559516,0.01103465],"study_design_scores_gemma":[0.000275057,0.0004829914,0.9787812,0.0000535803,0.000004567671,0.0001124926,0.001052761,0.003121929,0.000017785,0.01538722,0.0006763092,0.00003412161],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9912063,0.004551344,0.00001681564,0.003458614,0.00003162297,0.0001016395,0.00002590443,0.000001270469,0.0006064793],"genre_scores_gemma":[0.9976491,0.001564533,0.0005722783,0.00007731875,0.0000749897,5.473273e-7,0.00003781364,5.957886e-7,0.00002279368],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0152175,"threshold_uncertainty_score":0.1299427,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2165248235","doi":"10.1139/t01-089","title":"Submarine landslides: advances and challenges","year":2002,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":732,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Submarine; Submarine landslide; Mass movement; Submarine pipeline; Landslide; Geology; Debris; Hazard; Natural hazard; Geotechnical engineering; Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.03016852435739726,"gpt":0.1983593863854703,"spread":0.168190862028073,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001763,0.00007508013,0.00009853138,0.00009912953,0.0002679321,0.00007960435,0.0001408234,0.00007433495,0.007446334],"category_scores_gemma":[0.00009780315,0.0000530316,0.00002472541,0.0000981109,0.00007514021,0.0002624342,0.000004774322,0.0002416028,0.0001567454],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004487587,"about_ca_system_score_gemma":0.00002657315,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003990591,"about_ca_topic_score_gemma":0.06202261,"domain_scores_codex":[0.9993543,0.00002230983,0.0001423355,0.00009820324,0.00009975983,0.0002830947],"domain_scores_gemma":[0.9992445,0.00006200962,0.00003587046,0.00006430482,0.00003371206,0.0005596314],"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":[0.000003066036,0.000004527079,0.0258682,0.00002307269,0.000005953425,0.00007975812,0.00005501731,0.0008930409,1.633859e-7,0.0002678145,0.0009953844,0.971804],"study_design_scores_gemma":[0.0001304468,0.0001408847,0.1275592,0.00001477325,0.000005902154,0.001028869,0.0001086487,0.006030946,0.000001021565,0.005824315,0.8590229,0.0001320144],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"review","genre_gemma":"empirical","genre_scores_codex":[0.2020196,0.5832669,0.0004674976,0.07648194,0.0008167429,0.0003098567,0.0001276014,0.0001827823,0.1363272],"genre_scores_gemma":[0.9424879,0.05654016,0.0002926235,0.0004471001,0.0001038067,3.079531e-7,0.000003993411,0.000001269158,0.0001228469],"genre_candidate":"empirical","genre_consensus":null,"teacher_disagreement_score":0.971672,"threshold_uncertainty_score":0.993461,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W597470951","doi":"10.1017/cbo9780511975622","title":"Ichnology: Organism-Substrate Interactions in Space and Time","year":2011,"lang":"en","type":"book","venue":"","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":638,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Ichnology; Trace fossil; Ichnofacies; Sedimentology; Paleontology; Geology; Sequence stratigraphy; Facies; Multicellular organism; Ecology; Biology","retraction":null,"screen_n_in":null,"score":{"opus":0.01845308936171609,"gpt":0.1999618981042062,"spread":0.1815088087424901,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00007147506,0.0001267382,0.0001612242,0.0001267053,0.0000580077,0.00003229788,0.0001139964,0.0001428296,0.05555766],"category_scores_gemma":[0.00001242099,0.00009103125,0.0000169771,0.00007430351,0.00009049745,0.0001639357,0.00001308574,0.0002710328,0.004531644],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002395617,"about_ca_system_score_gemma":0.00006681612,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005213518,"about_ca_topic_score_gemma":0.005207554,"domain_scores_codex":[0.9994679,0.00001337721,0.0001541196,0.0001652733,0.00005119707,0.0001481409],"domain_scores_gemma":[0.9997007,0.00007499014,0.00005866693,0.00009115216,0.00002292353,0.00005154231],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0002138788,0.0001909788,0.3455356,0.000810405,0.000320123,0.0003300273,0.00328321,0.0003407922,0.00002949994,0.2824331,0.1367754,0.2297369],"study_design_scores_gemma":[0.0002134678,0.0002087235,0.0969781,0.00006759903,0.00004379859,0.0001343359,0.0001343664,0.0008670898,0.0000393176,0.3154387,0.5853178,0.0005566477],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.004351808,0.0005126674,0.00001122579,0.0002572235,0.00008323581,0.00008404456,0.00003255301,0.00005098253,0.9946163],"genre_scores_gemma":[0.1186014,0.000259946,0.000588966,0.0001330049,0.00002931478,6.406627e-7,0.0002257931,0.000002531987,0.8801584],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.4485424,"threshold_uncertainty_score":0.9962434,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2140747300","doi":"10.1306/051204740933","title":"A Simple Universal Equation for Grain Settling Velocity","year":2004,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":598,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Settling; Geology; Simple (philosophy); Thermodynamics; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.1064699774409404,"gpt":0.3413713870947868,"spread":0.2349014096538464,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00172628,0.00004773944,0.00009218264,0.0001694001,0.0002743758,0.00004589089,0.000176495,0.00003585466,0.0007903665],"category_scores_gemma":[0.000134984,0.00003439599,0.00005069813,0.0002740861,0.00006515279,0.0004445215,0.00000945449,0.0002222436,0.00002946638],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002210741,"about_ca_system_score_gemma":0.0001733937,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007376565,"about_ca_topic_score_gemma":0.0001309341,"domain_scores_codex":[0.9989933,0.00005957108,0.0002144298,0.00006702287,0.0004383219,0.0002273594],"domain_scores_gemma":[0.9991788,0.0002858058,0.00008044032,0.00004546067,0.000302647,0.0001068581],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","study_design_scores_codex":[0.003332387,0.0005688081,0.3278525,0.0004788647,0.0003962493,0.0002153197,0.006167121,0.3682462,0.001031837,0.004672278,0.02715918,0.2598793],"study_design_scores_gemma":[0.007943735,0.01016552,0.2783924,0.000202847,0.00007668103,0.0002578117,0.01437047,0.04661166,0.004734287,0.5294577,0.1072339,0.0005529759],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9914461,0.0003290211,0.004297546,0.003033892,0.0001412538,0.0001546312,0.00004336377,0.000005723703,0.0005484454],"genre_scores_gemma":[0.9937812,0.00006449583,0.005745209,0.0001472928,0.0001702615,3.619994e-7,0.00005908145,0.000001242538,0.00003086179],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5247855,"threshold_uncertainty_score":0.8653959,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4256425339","doi":"10.1017/cbo9780511975622","title":"Ichnology","year":2011,"lang":"en","type":"book","venue":"Cambridge University Press eBooks","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":549,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Ichnology; Trace fossil; Ichnofacies; Paleontology; Sedimentology; Geology; Sequence stratigraphy; Facies; Ecology; Biology; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.02408993887767123,"gpt":0.1696356399150012,"spread":0.14554570103733,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005757256,0.0001956878,0.0002287628,0.0001207239,0.0001784644,0.00002225818,0.0005168458,0.0003869243,0.0002993821],"category_scores_gemma":[0.000006839882,0.0001829507,0.00008866758,0.00001441825,0.0002438155,0.00009323321,0.0000567847,0.0003383059,0.0003563165],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009319465,"about_ca_system_score_gemma":0.000135481,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007192687,"about_ca_topic_score_gemma":0.00006030139,"domain_scores_codex":[0.9992182,0.00003402685,0.0001166401,0.0002638676,0.0001139517,0.0002533197],"domain_scores_gemma":[0.9993837,0.00005341014,0.000119278,0.0002531651,0.00007521603,0.0001152234],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0001236056,0.00001262769,0.000679194,0.0002430709,0.0001472117,0.0003625819,0.00008740606,0.00002240079,5.154819e-7,0.7253538,0.2366444,0.03632312],"study_design_scores_gemma":[0.000123934,0.00007666128,0.0009559096,0.00001795675,0.00007578111,0.00001951439,0.00001832014,0.00005472574,0.00001508733,0.00009047551,0.998316,0.0002355879],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.0002861866,0.0003891001,0.00007980059,0.000008746862,0.0002112093,0.0001364042,0.0003221691,0.0001296658,0.9984367],"genre_scores_gemma":[0.003874294,0.0001116975,0.0001298316,0.00007047662,0.00006140224,6.899403e-8,0.0003115876,0.000003526857,0.9954371],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.7616716,"threshold_uncertainty_score":0.7460514,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1561808238","doi":"10.3133/pp1661f","title":"Turbidite event history—Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone","year":2012,"lang":"en","type":"article","venue":"USGS professional paper","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":495,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Holocene; Abyssal plain; Paleontology; Canyon; Sedimentary rock; Submarine canyon; Continental margin; Oceanography; Geomorphology; Structural basin; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.03599025665324938,"gpt":0.3065729548615507,"spread":0.2705826982083013,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004331565,0.00006755078,0.0000889029,0.00002276331,0.0001973852,0.000003724749,0.00009143239,0.00006502313,0.0008683959],"category_scores_gemma":[0.00009609455,0.00003707857,0.00004547542,0.00008298256,0.00009416685,0.0002156681,0.00001586951,0.00008647041,0.000008362328],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000055571,"about_ca_system_score_gemma":0.00004116766,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001539567,"about_ca_topic_score_gemma":0.000040996,"domain_scores_codex":[0.9994192,0.00009230983,0.0001607078,0.00009479827,0.00007530538,0.0001577124],"domain_scores_gemma":[0.9994351,0.0002332306,0.00009513229,0.0001080369,0.00006256696,0.00006597878],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002999956,0.0000602364,0.9306473,0.00007344883,0.00001214014,1.788799e-8,0.0005570003,0.00008739244,0.0008623051,0.002226877,0.004789456,0.06065381],"study_design_scores_gemma":[0.00008154152,0.00001849889,0.9193442,0.00001045031,0.00001215066,0.000007287663,0.00006652986,0.0001512513,0.0002057964,0.001951436,0.07809492,0.00005594682],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9892811,0.004467727,0.001164628,0.002758466,0.0009686012,0.0002763576,0.00008159533,0.00001278231,0.000988749],"genre_scores_gemma":[0.9925721,0.000064793,0.005448639,0.0005689226,0.0001015692,0.00001084856,0.00004620342,0.000001554913,0.001185365],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07330547,"threshold_uncertainty_score":0.9508327,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2097237010","doi":"10.1144/gsl.sp.2000.172.01.01","title":"The falling stage systems tract: recognition and importance in sequence stratigraphic analysis","year":2000,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":445,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"","keywords":"Geology; Falling (accident); Sequence (biology); Stage (stratigraphy); Paleontology; Medicine","retraction":null,"screen_n_in":null,"score":{"opus":0.04472861255724696,"gpt":0.2412041366407967,"spread":0.1964755240835498,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006233746,0.0001194108,0.0001780026,0.00005064855,0.0006794709,0.0003458361,0.0002327808,0.0001379294,0.00719172],"category_scores_gemma":[0.00009484369,0.00007501212,0.000117851,0.001684516,0.0002976815,0.0004489696,0.000007516535,0.0002571275,0.00008999599],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006357825,"about_ca_system_score_gemma":0.00003276746,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001233026,"about_ca_topic_score_gemma":0.00681656,"domain_scores_codex":[0.9986947,0.00008748457,0.0003988286,0.0002888935,0.0002081172,0.0003219405],"domain_scores_gemma":[0.9991519,0.000374953,0.0001091422,0.0001662986,0.0000876592,0.0001099958],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000009577196,0.00004064443,0.9406593,0.000008586213,0.0000403236,0.000001620423,0.0001969317,0.006868828,0.000001364531,0.00185244,0.0002597242,0.05006061],"study_design_scores_gemma":[0.000102113,0.00003948061,0.9544701,0.000002528265,0.00002884181,0.000004257844,0.0004920568,0.01379811,4.301183e-7,0.005996852,0.02493923,0.0001259852],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9818258,0.001167526,0.0001197371,0.00237096,0.00004078443,0.000257037,0.0001716136,0.00005987807,0.01398663],"genre_scores_gemma":[0.9940416,0.004075362,0.0003626724,0.0001976426,0.0001595267,0.00002069405,0.0004964703,0.00000113293,0.0006448626],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04993463,"threshold_uncertainty_score":0.9937158,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2022928215","doi":"10.1130/0016-7606(2001)113<0443:oicftl>2.0.co;2","title":"Opening Iapetus: Constraints from the Laurentian margin in Newfoundland","year":2001,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":439,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Memorial University of Newfoundland; Western University","funders":"","keywords":"Citation; Library science; Icon; Geologist; Margin (machine learning); History; Art history; Archaeology; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.01561450991004078,"gpt":0.2110154713847474,"spread":0.1954009614747066,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002712082,0.000123738,0.0002313796,0.00001007407,0.0001675768,0.00003936184,0.0003485326,0.00009956733,0.07279602],"category_scores_gemma":[0.0001043729,0.00007041215,0.0001156268,0.0002955029,0.0007736153,0.00004627352,0.00003965904,0.0002381947,0.0004206267],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003582832,"about_ca_system_score_gemma":0.00001928968,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02205611,"about_ca_topic_score_gemma":0.001216195,"domain_scores_codex":[0.9988936,0.0001045501,0.0002851185,0.0002147371,0.0001866171,0.0003153699],"domain_scores_gemma":[0.999019,0.0006322449,0.0001187503,0.0001277964,0.00003311236,0.00006907341],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002944997,0.00002724598,0.9516342,0.000003947568,0.00001442769,0.000004520783,0.0003179592,0.001315405,0.000003523546,0.00002145318,0.007946199,0.03868167],"study_design_scores_gemma":[0.000256377,0.00009431289,0.7056862,0.00001268116,0.000006154505,0.000007531931,0.001469723,0.001342105,0.000001301213,0.001225543,0.2897932,0.000104937],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9400411,0.001734055,0.001650883,0.03401133,0.00009667686,0.0002405649,0.00008274469,0.00005061637,0.02209202],"genre_scores_gemma":[0.9858788,0.0007954624,0.009253363,0.003670702,0.00005225128,0.000002192945,0.0001662699,0.000001346486,0.000179606],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.281847,"threshold_uncertainty_score":0.9844561,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2138666479","doi":"10.2110/jsr.2009.026","title":"Hyperpycnal Rivers and Prodeltaic Shelves in the Cretaceous Seaway of North America","year":2009,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":430,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Simon Fraser University","funders":"University of Houston","keywords":"Geology; Cretaceous; Oceanography; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.04154351910877294,"gpt":0.2942055029127188,"spread":0.2526619838039458,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000974653,0.00005244356,0.0001260527,0.000180634,0.0001074954,0.0000301082,0.0002558584,0.00001871121,0.0003694071],"category_scores_gemma":[0.00004802998,0.00002786057,0.00002894171,0.0004412263,0.0001747939,0.0002819585,0.0000086278,0.0003396643,0.00000787184],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003389712,"about_ca_system_score_gemma":0.00006354391,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002579767,"about_ca_topic_score_gemma":0.0002167819,"domain_scores_codex":[0.9987784,0.0001702111,0.0002431989,0.00006543046,0.000552483,0.000190263],"domain_scores_gemma":[0.9994063,0.0002607107,0.00008180022,0.00006264139,0.0001208056,0.00006769522],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002011323,0.00008274388,0.816452,0.00002584388,0.00001564747,0.00006632349,0.001501908,0.001984517,0.00003112313,0.000005836993,0.001329235,0.1783037],"study_design_scores_gemma":[0.0002564076,0.001819374,0.9877831,0.00002042664,0.000006665191,0.0001023417,0.001615398,0.0009586221,0.00004289313,0.001169454,0.006182197,0.00004306109],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9934968,0.001953864,0.000005160041,0.003265565,0.00002234867,0.00009119052,0.00001016146,0.000001216412,0.001153672],"genre_scores_gemma":[0.9981224,0.0009530418,0.0005365461,0.0003149561,0.00004377256,1.507851e-7,0.000007917093,5.188667e-7,0.00002070831],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1782607,"threshold_uncertainty_score":0.4044749,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W384515273","doi":"10.2110/pec.06.84","title":"Facies Models Revisited","year":2006,"lang":"en","type":"book","venue":"SEPM (Society for Sedimentary Geology) eBooks","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":413,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Facies; Computer science; Geomorphology","retraction":null,"screen_n_in":null,"score":{"opus":0.01956207065554768,"gpt":0.2110800448303055,"spread":0.1915179741747578,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003629863,0.0006031524,0.000711013,0.00009852007,0.000606894,0.00007752301,0.0005606235,0.0008140426,0.00234624],"category_scores_gemma":[0.000008864062,0.0005003473,0.0009437553,0.00006986022,0.0004842752,0.0002329236,0.00006332098,0.0005428703,0.0002428272],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003032674,"about_ca_system_score_gemma":0.0002225348,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007419643,"about_ca_topic_score_gemma":0.0003699877,"domain_scores_codex":[0.9974564,0.00003398331,0.0006739412,0.0006867804,0.0003646608,0.0007841942],"domain_scores_gemma":[0.9986042,0.0003112183,0.000353792,0.0003944808,0.0001678464,0.0001684426],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0000795911,0.00002551457,0.002209514,0.0006884352,0.0006010863,0.000009513672,0.0004763542,0.004357203,0.000001762594,0.003991587,0.9745151,0.01304432],"study_design_scores_gemma":[0.0005479883,0.0003987108,0.0003949015,0.00005991587,0.0002521182,0.00002448951,0.00008731285,0.007644632,0.00001352529,0.1533775,0.8365302,0.0006686826],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.001330956,0.005136336,0.001340735,0.0005035387,0.0007106453,0.001583205,0.003390304,0.0003310135,0.9856732],"genre_scores_gemma":[0.003978628,0.0001728478,0.009091894,0.005230109,0.0006716459,0.00003594656,0.02194981,0.00002758905,0.9588415],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.1493859,"threshold_uncertainty_score":0.9997448,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2098479229","doi":"10.2110/jsr.2009.046","title":"Processes That Initiate Turbidity Currents and Their Influence on Turbidites: A Marine Geology Perspective","year":2009,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":405,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Turbidite; Geology; Turbidity current; Perspective (graphical); Marine geology; Oceanography; Geomorphology; Sediment; Sedimentary depositional environment; Geometry","retraction":null,"screen_n_in":null,"score":{"opus":0.08470394817834467,"gpt":0.3409239514753001,"spread":0.2562200032969555,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008970576,0.0001189088,0.0001988059,0.0002779873,0.0002316216,0.00007679678,0.0002761972,0.00005726058,0.001359468],"category_scores_gemma":[0.0003268349,0.00006343842,0.00003346807,0.0004014272,0.0002021031,0.0006490812,0.0000309129,0.0005925694,0.00003995382],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001457179,"about_ca_system_score_gemma":0.0001399182,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007060308,"about_ca_topic_score_gemma":0.0001298187,"domain_scores_codex":[0.9986697,0.0001602698,0.0002342721,0.0001539483,0.0004596643,0.0003221324],"domain_scores_gemma":[0.9984726,0.0005552842,0.0001242268,0.00008514285,0.0005869699,0.0001758105],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001179921,0.0003823263,0.896041,0.0001453634,0.0001026229,0.0001515947,0.003783419,0.001328348,0.00006059198,0.0002074479,0.00240794,0.09420937],"study_design_scores_gemma":[0.0005844494,0.004220547,0.9267161,0.000100284,0.000008512173,0.0002742402,0.003032221,0.0002473457,0.0008319929,0.05976461,0.004073218,0.0001465161],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9912766,0.001669006,0.000006923362,0.00390808,0.00008820632,0.0001170291,0.00002105657,0.000007626953,0.002905448],"genre_scores_gemma":[0.9969692,0.002030547,0.0001407118,0.0006694878,0.0001326863,4.598504e-7,0.00001570543,0.000001348928,0.00003989048],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.09406285,"threshold_uncertainty_score":0.9995534,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1487180362","doi":"10.1007/978-90-481-3071-9_1","title":"Submarine Mass Movements and Their Consequences","year":2009,"lang":"en","type":"book-chapter","venue":"","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":355,"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; Natural Resources Canada","funders":"","keywords":"China; Submarine; Submarine landslide; Submarine pipeline; Geography; Geology; Oceanography; Archaeology","retraction":null,"screen_n_in":null,"score":{"opus":0.02180005563743038,"gpt":0.1942513715112924,"spread":0.172451315873862,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008104951,0.0001698496,0.0001759815,0.00004966176,0.00009812875,0.00006110676,0.0001135644,0.0001245439,0.02541104],"category_scores_gemma":[0.00000650627,0.00009698991,0.00003116748,0.00001573892,0.0001446033,0.0001027095,0.00000722891,0.0001148282,0.0003016501],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":8.649292e-7,"about_ca_system_score_gemma":0.00002143646,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002512735,"about_ca_topic_score_gemma":0.0006744646,"domain_scores_codex":[0.9994326,0.00000500854,0.0001633058,0.0001677501,0.00009528622,0.0001360064],"domain_scores_gemma":[0.9996811,0.0000574945,0.00006663306,0.0000859153,0.00003162803,0.00007723468],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","study_design_scores_codex":[0.00002338303,0.000005227921,0.01415262,0.00007202754,0.0000634574,0.00001989695,0.00008446981,0.00006120293,0.00000368133,0.0613472,0.001372321,0.9227945],"study_design_scores_gemma":[0.00008547962,0.0001949047,0.01028115,0.00002612609,0.000007691161,0.00001720579,0.00003697721,0.0001997553,0.00002166479,0.5806237,0.4082453,0.0002600459],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.0007458712,0.001473093,0.00003484875,0.000346464,0.00005773041,0.00009407608,0.00008449337,0.00003830232,0.9971251],"genre_scores_gemma":[0.1613374,0.002448883,0.0006228349,0.0013519,0.00005645015,3.268945e-7,0.0003371501,0.000002212131,0.8338428],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.9225345,"threshold_uncertainty_score":0.9754798,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2002011430","doi":"10.1144/gsl.sp.2005.252.01.01","title":"The Neuquén Basin: an overview","year":2005,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":350,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Structural basin; Paleontology; Earth science","retraction":null,"screen_n_in":null,"score":{"opus":0.04585770775316127,"gpt":0.2651951989945269,"spread":0.2193374912413656,"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":[0.0005406916,0.0001432765,0.0001459252,0.00001734334,0.00159941,0.0003661872,0.0006398287,0.0001503608,0.02080458],"category_scores_gemma":[0.0002096536,0.00008065161,0.0001755039,0.0005996728,0.0003669776,0.0007167496,0.00003819813,0.0002647077,0.00151878],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000874635,"about_ca_system_score_gemma":0.00006057666,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002315345,"about_ca_topic_score_gemma":0.002263468,"domain_scores_codex":[0.9985715,0.0000998465,0.0003191734,0.0002817191,0.0002843267,0.0004434869],"domain_scores_gemma":[0.9988168,0.0003601718,0.00009943495,0.0003373586,0.0001681759,0.0002180462],"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":[0.0000194966,0.0001713127,0.1565171,0.000008526653,0.00003131423,3.977586e-7,0.0003145892,0.001880797,0.000001774093,0.2034958,0.1424049,0.4951541],"study_design_scores_gemma":[0.00007081139,0.00004976531,0.377521,7.409873e-7,0.000005095655,0.000004734581,0.00009035478,0.001916292,0.000001839413,0.008769713,0.6114828,0.00008688054],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.4040066,0.00894785,0.001298169,0.2828141,0.0009222248,0.001049549,0.0002323433,0.0008934417,0.2998357],"genre_scores_gemma":[0.9622555,0.006949435,0.007055726,0.01073548,0.005064897,0.00003350807,0.0007173053,0.00000550187,0.007182599],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.558249,"threshold_uncertainty_score":0.9997004,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W321577279","doi":"10.1007/0-306-47669-x_5","title":"Sediment Core Collection and Extrusion","year":2005,"lang":"en","type":"book-chapter","venue":"Kluwer Academic Publishers eBooks","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":346,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba; Queen's University","funders":"","keywords":"Sediment core; Geology; Extrusion; Sediment; Archaeology; Geomorphology; Geography; Metallurgy; Materials science","retraction":null,"screen_n_in":null,"score":{"opus":0.03099437761227734,"gpt":0.223160084977734,"spread":0.1921657073654567,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003260526,0.0003166381,0.0002936505,0.0002298711,0.0002987869,0.0002137467,0.0002749473,0.0008719715,0.008701744],"category_scores_gemma":[0.0000364275,0.0002514216,0.00007081876,0.00003657999,0.0001848933,0.0005855002,0.00004715894,0.001058382,0.0002206799],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001763358,"about_ca_system_score_gemma":0.0001046222,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001249986,"about_ca_topic_score_gemma":0.0001663093,"domain_scores_codex":[0.9984576,0.00001411901,0.0004076174,0.0004088029,0.0003927046,0.0003191495],"domain_scores_gemma":[0.999198,0.00009957372,0.0002240714,0.0001622855,0.00008361536,0.0002324205],"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":[0.0001222454,0.000006507902,0.007823629,0.0001584224,0.0001123528,0.00001538771,0.0008097942,0.0001103843,0.000008691161,0.0130603,0.2877483,0.690024],"study_design_scores_gemma":[0.000222058,0.000101424,0.002351674,0.00007537583,0.00004634404,0.00005612438,0.00004015632,0.000504162,0.000006042393,0.03717976,0.9590572,0.0003597474],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.002436429,0.002543335,0.0000185424,0.0005353105,0.0005109828,0.0003275997,0.00005537185,0.0001176171,0.9934548],"genre_scores_gemma":[0.04857466,0.0004611011,0.0003696857,0.001384951,0.0005366135,0.000004673108,0.0003777497,0.0000140658,0.9482765],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.6896642,"threshold_uncertainty_score":0.9999938,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W584173116","doi":"10.1007/978-3-319-00666-6","title":"Fluvial Depositional Systems","year":2013,"lang":"en","type":"book","venue":"Springer geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":343,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Fluvial; Sedimentary depositional environment; Geology; Interpretation (philosophy); Paleontology; Philosophy; Linguistics; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.01221809623477351,"gpt":0.1856080245694774,"spread":0.1733899283347038,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001088661,0.0002039569,0.0002893567,0.0001089407,0.0001563598,0.00006338127,0.0002706855,0.0004180782,0.02385484],"category_scores_gemma":[0.00002215097,0.000157812,0.00007313081,0.00004362052,0.0001585871,0.0001190232,0.00002666755,0.0003248048,0.02075317],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006201103,"about_ca_system_score_gemma":0.000156664,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007960624,"about_ca_topic_score_gemma":0.0004276836,"domain_scores_codex":[0.9989008,0.00004193912,0.0002857793,0.0002644779,0.0001821199,0.0003248867],"domain_scores_gemma":[0.9993473,0.0001454859,0.0001341843,0.0001736364,0.0000922631,0.0001071527],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0001082066,0.00007250088,0.260633,0.001354219,0.0005312962,0.0002530738,0.0002574775,0.01834586,0.000005248569,0.153886,0.5191944,0.04535874],"study_design_scores_gemma":[0.0001420818,0.0001728585,0.08307908,0.00003884924,0.00003144707,0.0001847708,0.000009540037,0.001760314,0.000001125218,0.02538457,0.8887976,0.000397798],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.005261668,0.004261848,0.0001537258,0.0001976623,0.001722716,0.0002508977,0.00007729307,0.0000931373,0.9879811],"genre_scores_gemma":[0.127578,0.0002046386,0.0004770143,0.0003929838,0.001113782,0.00001012929,0.002080316,0.0000071506,0.868136],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.3696032,"threshold_uncertainty_score":0.9800093,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2173216887","doi":"10.2110/palo.2004.p04-32","title":"Colonization of Brackish-Water Systems through Time: Evidence from the Trace-Fossil Record","year":2005,"lang":"en","type":"article","venue":"Palaios","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":331,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada; Simon Fraser University; University of Alberta; University of Saskatchewan","funders":"","keywords":"Brackish water; Colonization; Trace fossil; Geology; Fossil Record; TRACE (psycholinguistics); Paleontology; Earth science; Geochemistry; Archaeology; Geography; Oceanography; Salinity","retraction":null,"screen_n_in":null,"score":{"opus":0.0287330048710887,"gpt":0.225890642889476,"spread":0.1971576380183873,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002088842,0.00007043315,0.0001080929,0.00001010689,0.0001435547,0.00006105042,0.0001993895,0.00005251144,0.004287593],"category_scores_gemma":[0.0001020194,0.00003476031,0.00002659883,0.0001219446,0.00005627672,0.0004512261,0.000007762394,0.00006620183,0.001341886],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001885804,"about_ca_system_score_gemma":0.00001605809,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002291372,"about_ca_topic_score_gemma":0.000795749,"domain_scores_codex":[0.9992914,0.00007643158,0.0002196201,0.000112208,0.0001612252,0.0001391437],"domain_scores_gemma":[0.9993212,0.0003721925,0.00007433006,0.0001346881,0.00007085979,0.00002676436],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00007296982,0.00003648386,0.869247,0.00007190702,0.00003483841,0.000001894542,0.004562945,0.03376552,0.0004095526,0.00006827866,0.008636969,0.08309169],"study_design_scores_gemma":[0.0002740381,0.0002387447,0.6788492,0.0002067863,0.00005182273,0.00001100187,0.0004300255,0.08439132,0.003593789,0.001458836,0.2302034,0.0002910338],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.987583,0.006201502,0.0005752812,0.002027082,0.0001793748,0.0001900954,0.00006208652,0.00003219101,0.003149423],"genre_scores_gemma":[0.998439,0.0002800509,0.0005957992,0.000094027,0.0001409885,0.000002112371,0.0000435881,0.000001246033,0.0004032268],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2215664,"threshold_uncertainty_score":0.9994357,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2937564221","doi":"10.1016/s0037-0738(01)00061-6","title":"Sedimentary Basins: Evolution, Facies, and Sediment Budget","year":2001,"lang":"en","type":"article","venue":"Sedimentary Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":306,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Facies; Geochemistry; Sedimentary rock; Sediment; Sedimentary budget; Sedimentary basin; Geomorphology; Structural basin; Sediment transport","retraction":null,"screen_n_in":null,"score":{"opus":0.009216774577482658,"gpt":0.2012922515055121,"spread":0.1920754769280295,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002475064,0.0002161386,0.0002227508,0.0001305073,0.0003624909,0.00003095651,0.0001907665,0.0001164576,0.01827394],"category_scores_gemma":[0.00001628893,0.0001747285,0.00004290914,0.0002626956,0.0002922119,0.0004014986,0.0000482279,0.0001750711,0.0005815764],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001338893,"about_ca_system_score_gemma":0.00004724643,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006979265,"about_ca_topic_score_gemma":0.001673604,"domain_scores_codex":[0.9985136,0.00009009174,0.0003159562,0.0003647155,0.0002151957,0.0005004675],"domain_scores_gemma":[0.9993681,0.0001208301,0.00007817858,0.000184332,0.00004596877,0.0002025417],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000682612,0.00004171309,0.9803424,0.00001671739,0.00004733405,0.00003400232,0.0001709798,0.0005580357,0.00001424673,0.0004118874,0.007598695,0.01069568],"study_design_scores_gemma":[0.0007128685,0.000569259,0.7149501,0.000008563755,0.00003805355,0.0003856015,0.0007911497,0.001956952,0.00006426544,0.01103214,0.2691776,0.0003133375],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9722359,0.005257519,0.0003594248,0.007477525,0.0007413623,0.0002865741,0.000127159,0.0001231015,0.0133915],"genre_scores_gemma":[0.9905685,0.000589437,0.001317233,0.006023195,0.0001606054,0.000004991887,0.0006506883,0.000003530891,0.000681841],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2653923,"threshold_uncertainty_score":0.9996334,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1974360698","doi":"10.1038/ngeo1376","title":"Palaeozoic landscapes shaped by plant evolution","year":2012,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":306,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Fluvial; Pennsylvanian; Paleozoic; Devonian; Geology; Paleontology; Floodplain; Vegetation (pathology); Ecology; Riparian zone; Earth science; Habitat; Biology","retraction":null,"screen_n_in":null,"score":{"opus":0.006504148199062175,"gpt":0.2021108435464335,"spread":0.1956066953473713,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003115692,0.00008677222,0.00007654665,0.00004666294,0.0002579537,0.00004650597,0.000235604,0.0001403609,0.001589224],"category_scores_gemma":[0.0001131058,0.00005599496,0.00002322521,0.0003816583,0.00005976007,0.0005889493,0.00001082246,0.0002364594,0.0004051386],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003010811,"about_ca_system_score_gemma":0.00002232464,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002117519,"about_ca_topic_score_gemma":0.0002088841,"domain_scores_codex":[0.9990785,0.00002453443,0.0001047804,0.0001439648,0.000265264,0.0003830264],"domain_scores_gemma":[0.9996125,0.00008116187,0.00004561304,0.00008927975,0.00002967483,0.0001417976],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000006437454,0.00001637263,0.9932615,0.000008052363,0.000001348184,4.433483e-7,0.00007708132,0.00002735587,0.00006994169,0.000721143,0.002981962,0.002828347],"study_design_scores_gemma":[0.00007001452,0.00004491181,0.9259508,0.000005427824,0.000003928601,0.00002322248,0.00007247433,0.005905642,0.00003372805,0.0007605535,0.0670002,0.0001291358],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9791331,0.009102982,0.001389535,0.0005076033,0.0007884917,0.00009442274,0.0002349784,0.00008013502,0.008668751],"genre_scores_gemma":[0.9984692,0.00005812329,0.0005103188,0.0004313787,0.0001037391,8.713766e-7,0.0001507556,7.720125e-7,0.0002748329],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06731075,"threshold_uncertainty_score":0.9993235,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W105210259","doi":"10.1007/978-1-4020-3609-5_29","title":"Biogenic sedimentary structures","year":2007,"lang":"en","type":"book-chapter","venue":"","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":293,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Sedimentary rock; Geochemistry","retraction":null,"screen_n_in":null,"score":{"opus":0.03185750941181054,"gpt":0.2223201240496021,"spread":0.1904626146377915,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00007936237,0.0001679181,0.0001433731,0.00009896913,0.00009581626,0.00002960029,0.0001598825,0.0002072037,0.2417416],"category_scores_gemma":[0.000003250833,0.000108723,0.00007343662,0.00002298636,0.00006939391,0.00007695624,0.000009335632,0.0001658317,0.002598673],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001540739,"about_ca_system_score_gemma":0.00002368136,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0004766942,"about_ca_topic_score_gemma":0.001080032,"domain_scores_codex":[0.9992868,0.000002787523,0.0001880287,0.0001645303,0.0001882381,0.0001696068],"domain_scores_gemma":[0.9996442,0.00005671693,0.00006299611,0.0001179651,0.00002862202,0.00008951385],"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":[0.00006749932,0.000007106464,0.01454818,0.0001120381,0.0002188054,0.00008090074,0.00007402695,0.0003761678,8.569233e-7,0.4054107,0.04918221,0.5299215],"study_design_scores_gemma":[0.00004899742,0.00007510793,0.006615366,0.000007338479,0.00002115555,0.00002323184,0.000009114654,0.00003086272,0.00001345835,0.1482132,0.844729,0.000213135],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.0002769071,0.002246942,0.00004608246,0.00009114496,0.0002512269,0.0000836772,0.000138781,0.00005824169,0.996807],"genre_scores_gemma":[0.04794444,0.0007237329,0.0032525,0.003221967,0.0003855147,1.875014e-7,0.002115184,0.000006546947,0.9423499],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.7955468,"threshold_uncertainty_score":0.9981779,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2160469173","doi":"10.1306/12131010111","title":"Seismic geomorphology and sedimentology of a tidally influenced river deposit, Lower Cretaceous Athabasca oil sands, Alberta, Canada","year":2011,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":255,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Nexen (Canada); University of Calgary","funders":"","keywords":"Geology; Sedimentology; Oil sands; Cretaceous; Geomorphology; Geochemistry; Paleontology; Archaeology; Asphalt; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.00729923814558842,"gpt":0.1684834737024933,"spread":0.1611842355569048,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008913507,0.000119186,0.0001938702,0.00003594235,0.00009285643,0.00000796926,0.0001609214,0.00008847037,0.01347813],"category_scores_gemma":[0.00005305026,0.00009199876,0.00002387284,0.00008041625,0.0001963222,0.00004021795,0.00002295081,0.00009836306,0.0001361421],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002729099,"about_ca_system_score_gemma":0.00008826802,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9115384,"about_ca_topic_score_gemma":0.7427611,"domain_scores_codex":[0.999172,0.00005038335,0.0002262873,0.000184539,0.0001093218,0.0002574786],"domain_scores_gemma":[0.999463,0.000161633,0.00009683715,0.0001207235,0.00005409697,0.0001037396],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001818047,0.00003538176,0.9829364,0.00006770123,0.00004845615,0.00008874914,0.0008765077,0.0002980116,0.00001724722,0.00006008081,0.007050929,0.008338762],"study_design_scores_gemma":[0.0004723754,0.0004381787,0.8721994,0.00001821275,0.00003582879,0.0002931081,0.0001096972,0.0005710303,0.0004191085,0.0003041683,0.1249034,0.0002355416],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.980453,0.0007642899,0.00002315994,0.0005743289,0.0001289108,0.00004610671,0.0000394485,0.00000942667,0.01796136],"genre_scores_gemma":[0.9970413,0.0001076911,0.0006817295,0.001141239,0.00001168161,0.000001585879,0.00004422692,0.000002029066,0.0009684855],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1687774,"threshold_uncertainty_score":0.9874237,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2154930938","doi":"10.2110/jsr.2005.029","title":"Discontinuity-Bounded Alluvial Sequences of the Southern Gangetic Plains, India: Aggradation and Degradation in Response to Monsoonal Strength","year":2005,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":253,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Aggradation; Geology; Discontinuity (linguistics); Alluvium; Monsoon; Geomorphology; Climatology; Fluvial; Structural basin; Mathematics","retraction":null,"screen_n_in":null,"score":{"opus":0.0326750587042836,"gpt":0.2947070500101455,"spread":0.2620319913058619,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002411948,0.0000603182,0.0001137936,0.000246163,0.0001443435,0.00005423936,0.000229577,0.0000369973,0.0004808294],"category_scores_gemma":[0.0002218089,0.00003542459,0.00002773685,0.0003717803,0.0001412172,0.000389951,0.00002610147,0.0002780819,0.00001291711],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001736725,"about_ca_system_score_gemma":0.0001394808,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007408933,"about_ca_topic_score_gemma":0.003074158,"domain_scores_codex":[0.9983715,0.0004212555,0.0003373843,0.00008258258,0.0006091667,0.0001780461],"domain_scores_gemma":[0.9991186,0.0004731001,0.0001334998,0.00006625971,0.0001225584,0.00008593496],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001944421,0.000120966,0.9042198,0.00003305087,0.00002760009,0.00001308743,0.005314015,0.002885874,0.002745497,0.00004476848,0.0004856024,0.08216529],"study_design_scores_gemma":[0.0006404078,0.0008031849,0.9866103,0.0001098404,0.000009635255,0.00004143034,0.004396755,0.001000781,0.002261849,0.001806339,0.002234322,0.00008516582],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9933663,0.0004870318,0.00000859542,0.005817679,0.00004791158,0.0001307767,0.00004544537,0.000001503688,0.00009475429],"genre_scores_gemma":[0.9986068,0.00007757268,0.001046027,0.00009690262,0.00007919405,6.343662e-7,0.00001065367,0.000001189091,0.00008100423],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08239046,"threshold_uncertainty_score":0.5264745,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2414676298","doi":"10.1038/ncomms11896","title":"First wide-angle view of channelized turbidity currents links migrating cyclic steps to flow characteristics","year":2016,"lang":"en","type":"article","venue":"Nature Communications","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":243,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bedform; Channelized; Turbidity current; Geology; Hydraulic jump; Flow (mathematics); Geomorphology; Channel (broadcasting); Surge; Mechanics; Physics; Sedimentary depositional environment; Sediment; Sediment transport; Telecommunications; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.03265251327730473,"gpt":0.2740317764666546,"spread":0.2413792631893499,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023971,0.0001093831,0.0001892885,0.00006868334,0.0003194142,0.00002797735,0.0008551236,0.0002240345,0.0005986131],"category_scores_gemma":[0.0008767142,0.00006795473,0.00005636657,0.0003569276,0.00008366759,0.0001783202,0.00008791525,0.000411868,0.0002324646],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004354482,"about_ca_system_score_gemma":0.00002853603,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001024706,"about_ca_topic_score_gemma":0.003361253,"domain_scores_codex":[0.999135,0.00008872724,0.0003163008,0.0001307017,0.0001541595,0.0001751649],"domain_scores_gemma":[0.9980685,0.000762546,0.0001448612,0.0007229602,0.0001979519,0.00010319],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004063855,0.0002052329,0.6996723,0.0001566495,0.00005095301,7.886038e-7,0.001086353,0.0001860779,0.0001161905,0.0008717789,0.006408877,0.2912042],"study_design_scores_gemma":[0.0002236445,0.00009050626,0.6986176,0.0002396169,0.00002194407,0.000003045598,0.0000508071,0.002610281,0.0001587842,0.0008209282,0.2969635,0.0001993629],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9312107,0.01702192,0.002554522,0.03834501,0.00108019,0.0009471131,0.002230718,0.0001984776,0.00641135],"genre_scores_gemma":[0.98958,0.001807262,0.007747613,0.0004774964,0.00003730626,0.000007412108,0.0002738044,0.00000248051,0.00006667098],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2910048,"threshold_uncertainty_score":0.6554394,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2164625060","doi":"10.1046/j.1365-3091.2001.00357.x","title":"Bedforms and associated sedimentary structures formed under supercritical water flows over aggrading sand beds","year":2001,"lang":"en","type":"article","venue":"Sedimentology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":242,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Brock University","funders":"Core Research for Evolutional Science and Technology","keywords":"Bedform; Geology; Sedimentary structures; Flume; Sedimentary rock; Geomorphology; Aggradation; Sediment transport; Fluvial; Sedimentary depositional environment; Sediment; Paleontology; Flow (mathematics); Structural basin; Geometry","retraction":null,"screen_n_in":null,"score":{"opus":0.01476780854856425,"gpt":0.2358283911744247,"spread":0.2210605826258605,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002039112,0.0001554073,0.0002072486,0.00008551773,0.0002638739,0.00005624749,0.0001088253,0.0001640537,0.01149159],"category_scores_gemma":[0.00002626917,0.00009295874,0.00003706537,0.0001070371,0.0001430273,0.0003266642,0.00002404729,0.0001571757,0.00007050059],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007290657,"about_ca_system_score_gemma":0.00001366023,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000860972,"about_ca_topic_score_gemma":0.00107279,"domain_scores_codex":[0.9988148,0.000059657,0.0002255787,0.0002182096,0.0001659769,0.0005158436],"domain_scores_gemma":[0.9996213,0.0001054836,0.00001072553,0.00008583555,0.00002821985,0.0001484711],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001630114,0.00007160765,0.9823655,0.00004525949,0.0001874153,0.00005375646,0.002883384,0.0002408447,0.0008298009,0.001530523,0.003487902,0.008140971],"study_design_scores_gemma":[0.002268442,0.0008293656,0.8224028,0.00002157619,0.0001287785,0.0004524883,0.002342321,0.007052314,0.002445718,0.1431514,0.01821615,0.000688573],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9933202,0.0004806636,0.00007246681,0.001562034,0.0003827436,0.0001130046,0.00002986392,0.00004913652,0.0039899],"genre_scores_gemma":[0.9973229,0.00009873644,0.0001857827,0.001743361,0.00006477508,0.000001795225,0.0004818218,0.000002946937,0.00009783841],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1599627,"threshold_uncertainty_score":0.989412,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2142396396","doi":"10.1111/j.1365-3091.2007.00926.x","title":"Dimensions and architecture of late Pleistocene submarine lobes off the northern margin of East Corsica","year":2008,"lang":"en","type":"article","venue":"Sedimentology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":237,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Dalhousie University; Institut Français de Recherche pour l'Exploitation de la Mer","keywords":"Geology; Sedimentary depositional environment; Lobe; Paleontology; Facies; Structural basin; Submarine; Geomorphology; Pleistocene; Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.01339158973120124,"gpt":0.1928999345769826,"spread":0.1795083448457813,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008355147,0.00007034835,0.0001564702,0.00002959583,0.0001131805,0.000002061321,0.0001089999,0.00004418532,0.0006472102],"category_scores_gemma":[0.0000297448,0.00003916065,0.00002532763,0.0001269135,0.0003989048,0.00002993348,0.00002057998,0.00007955648,0.00001344402],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":6.158049e-7,"about_ca_system_score_gemma":0.00001961085,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001253807,"about_ca_topic_score_gemma":0.004212524,"domain_scores_codex":[0.9994666,0.00004535462,0.0001694052,0.00009362202,0.00008867666,0.0001363178],"domain_scores_gemma":[0.9995891,0.0001327462,0.00008890795,0.0001047238,0.0000440139,0.00004050479],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000834137,0.00002809385,0.9666384,0.00002649364,0.0000258867,0.000005127135,0.001033202,0.001684673,0.00005604192,0.0001397705,0.00008985492,0.030189],"study_design_scores_gemma":[0.0002227469,0.0003226193,0.992346,0.000006116126,0.00001626766,0.00009044957,0.0001320438,0.0006427942,0.0001998627,0.001629768,0.004328291,0.00006302568],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9949908,0.001495762,0.0000327657,0.0008592294,0.00005852618,0.00008882092,0.00004075281,0.000008163684,0.002425203],"genre_scores_gemma":[0.9992412,0.0001814204,0.0003011886,0.0001032233,0.00001173286,6.519651e-7,0.00003477528,0.000001009802,0.000124768],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03012597,"threshold_uncertainty_score":0.7086498,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2162494062","doi":"10.1111/j.1365-3091.2009.01050.x","title":"Counter point bar deposits: lithofacies and reservoir significance in the meandering modern Peace River and ancient McMurray Formation, Alberta, Canada","year":2009,"lang":"en","type":"article","venue":"Sedimentology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":230,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Nexen (Canada); University of Calgary","funders":"University at Buffalo; Parks Canada","keywords":"Point bar; Geology; Fluvial; Silt; Paleontology; Geomorphology; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.01094863036175043,"gpt":0.1990751791533297,"spread":0.1881265487915793,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000201118,0.0000829677,0.0001039433,0.00002958342,0.0001620116,0.00004256644,0.0001056256,0.00003643214,0.0000805133],"category_scores_gemma":[0.00003279315,0.00005151484,0.00000732743,0.00008817184,0.00007402344,0.0002638271,0.000007753041,0.00008483346,0.000003451157],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006433193,"about_ca_system_score_gemma":0.00003898876,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1447467,"about_ca_topic_score_gemma":0.7509526,"domain_scores_codex":[0.9993161,0.00006171726,0.0001548277,0.0001320826,0.0001232954,0.000211988],"domain_scores_gemma":[0.999668,0.0001369521,0.0000407905,0.00007958765,0.00002698869,0.00004770794],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001388981,0.00004883096,0.9277658,0.0001341475,0.00002216111,0.00004537488,0.03083828,0.008449427,0.00008747745,0.001383561,0.006074403,0.02501166],"study_design_scores_gemma":[0.0002732325,0.000152537,0.9659576,0.00001276904,0.000007335423,0.00009948271,0.001565922,0.01625549,0.00006870332,0.002736333,0.01274122,0.0001294065],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9893141,0.002246346,0.0002971424,0.005308059,0.00004831483,0.0001354382,0.00000971782,0.000006024246,0.00263486],"genre_scores_gemma":[0.9972063,0.0001445439,0.0001694512,0.002391955,0.000009817149,0.000001841358,0.00002043452,5.938384e-7,0.00005506404],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6062059,"threshold_uncertainty_score":0.8609486,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2082942560","doi":"10.1306/8626cacd-173b-11d7-8645000102c1865d","title":"Sandy Fans-From Amazon to Hueneme and Beyond","year":2001,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":230,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Amazon rainforest; Geology","retraction":null,"screen_n_in":null,"score":{"opus":0.01072333107424131,"gpt":0.1964717701752515,"spread":0.1857484391010102,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008967829,0.00007598713,0.00008770765,0.00003067305,0.0001270704,0.00005843461,0.00009998731,0.00004215348,0.02722365],"category_scores_gemma":[0.00004306776,0.00005619211,0.00001508727,0.000112874,0.00003080026,0.00004250224,0.00001227092,0.00005711773,0.002673425],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":6.838551e-7,"about_ca_system_score_gemma":0.000005965483,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002202629,"about_ca_topic_score_gemma":0.0009720689,"domain_scores_codex":[0.9994488,0.00001889444,0.0001104535,0.0001507306,0.00009838562,0.0001727112],"domain_scores_gemma":[0.9996583,0.00009274052,0.00002094046,0.00008746797,0.00002010437,0.0001203979],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.00007632346,0.00002302697,0.7433172,0.00001126523,0.00001341561,0.00002853792,0.0005876911,0.0005094421,0.00004365432,0.000237992,0.03883774,0.2163137],"study_design_scores_gemma":[0.00009307549,0.00008799128,0.3992123,0.000003919544,0.00000371935,0.000007721666,0.0001127669,0.00008090769,0.00002860245,0.00144762,0.5988368,0.00008453875],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9298092,0.0007415865,0.0001348641,0.007601615,0.00008352472,0.00007619885,0.00004081076,0.00003526279,0.06147696],"genre_scores_gemma":[0.9940075,0.0002018815,0.001753903,0.002905133,0.00006827207,0.000001122291,0.00007462461,0.000001263421,0.0009863452],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.559999,"threshold_uncertainty_score":0.9981031,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1945302183","doi":"10.2110/jsr.2015.63","title":"Deep-Water Sediment Bypass","year":2015,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":225,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"U.S. Geological Survey; Strong; International Association of Sedimentologists; Society for Sedimentary Geology","keywords":"Geology; Sediment; Deep water; Hydrology (agriculture); Oceanography; Geochemistry; Geomorphology; Geotechnical engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.1223679375037015,"gpt":0.3363671365674912,"spread":0.2139991990637898,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002856174,0.00007225412,0.0001373675,0.0002180343,0.0001428113,0.000073732,0.0003107424,0.00004473109,0.006212804],"category_scores_gemma":[0.00005820028,0.00003872319,0.00004751335,0.0002263394,0.0001056505,0.0005108313,0.00002996435,0.0003864134,0.0007534236],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001666111,"about_ca_system_score_gemma":0.0001078092,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0004421757,"about_ca_topic_score_gemma":0.00006700281,"domain_scores_codex":[0.997979,0.0001725736,0.0003251549,0.00008460788,0.001071037,0.000367571],"domain_scores_gemma":[0.9988716,0.0001279692,0.00005860492,0.00009025642,0.0004879417,0.0003636511],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.00144717,0.0004221523,0.7112299,0.0001025146,0.0003070232,0.0007000016,0.005565546,0.02508006,0.0004820451,0.0001639059,0.1592112,0.09528844],"study_design_scores_gemma":[0.004588614,0.0104218,0.1033531,0.0001119183,0.00007069919,0.001441888,0.01580291,0.01448234,0.01398044,0.04266018,0.7924704,0.0006157064],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9772364,0.002009817,0.0001160964,0.005520625,0.0005495902,0.0001105127,0.000005609347,0.000008032594,0.01444335],"genre_scores_gemma":[0.99756,0.00009520169,0.001365329,0.0003478345,0.0003161037,3.656523e-7,0.00002326323,0.000001699483,0.0002902416],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6332592,"threshold_uncertainty_score":0.9946957,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2144585407","doi":"10.1007/s100400000069","title":"A tectono-geomorphic model of the hydrogeology of deeply weathered crystalline rock: Evidence from Uganda","year":2000,"lang":"en","type":"article","venue":"Hydrogeology Journal","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":211,"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":"International Development Research Centre","keywords":"Geology; Aquifer; Hydrogeology; Bedrock; Weathering; Geochemistry; Geomorphology; Meteoric water; Groundwater; Terrain; Mantle (geology); Earth science; Geotechnical engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.02371218956130257,"gpt":0.2083564282586488,"spread":0.1846442386973462,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004222629,0.0001637043,0.0003702508,0.00007588256,0.0002426265,0.00001372077,0.000651952,0.000181127,0.02309724],"category_scores_gemma":[0.0001607724,0.00009843847,0.0001588485,0.0002741439,0.0003414073,0.0002436522,0.00002842392,0.0003955615,0.00009430288],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003442602,"about_ca_system_score_gemma":0.00017438,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008154855,"about_ca_topic_score_gemma":0.001495438,"domain_scores_codex":[0.9983837,0.0002032375,0.0006388914,0.0001863678,0.000253534,0.0003342427],"domain_scores_gemma":[0.9987864,0.0003372779,0.0003720272,0.000261077,0.0001316683,0.0001115626],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.000166832,0.00003896466,0.5006544,0.00001474057,0.0000588651,0.000007608842,0.0003301123,0.49298,0.0005804274,0.00003236028,0.00009124878,0.005044393],"study_design_scores_gemma":[0.001250621,0.000772366,0.1798702,0.0002168417,0.0001670138,0.001221069,0.0001329524,0.7297377,0.005947706,0.07900913,0.00129906,0.0003753557],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9929875,0.003212649,0.00114112,0.00110342,0.00009658426,0.00009941503,0.00006676261,0.00001318368,0.001279412],"genre_scores_gemma":[0.9977617,0.00074581,0.0009508443,0.0002169115,0.00005904151,9.418973e-7,0.00001466227,0.000003086939,0.0002470447],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3207842,"threshold_uncertainty_score":0.9777958,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2171856802","doi":"10.2110/jsr.2015.03","title":"Key Future Directions For Research On Turbidity Currents and Their Deposits","year":2015,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":207,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Bedford Institute of Oceanography; University of New Brunswick; Memorial University of Newfoundland; Carleton University; Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Turbidity current; Key (lock); Turbidity; Earth science; Geomorphology; Oceanography; Sedimentary depositional environment; Structural basin; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.2648897023952091,"gpt":0.4139151390724569,"spread":0.1490254366772478,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004259925,0.00007456067,0.0001337968,0.0003466033,0.0004927584,0.0001077128,0.0002441059,0.00006192554,0.0002506144],"category_scores_gemma":[0.0002125233,0.00004348874,0.00004146286,0.0004715594,0.0001424278,0.0003634246,0.00002747085,0.000679266,0.00003760194],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001791108,"about_ca_system_score_gemma":0.0001515325,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002821945,"about_ca_topic_score_gemma":0.0002895217,"domain_scores_codex":[0.9982352,0.0003221799,0.0002232244,0.0001215064,0.0007454047,0.000352504],"domain_scores_gemma":[0.9978575,0.0007828409,0.00005481917,0.00008749888,0.0008721994,0.0003451679],"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":[0.002589363,0.0005678219,0.2818629,0.0002091346,0.0001895428,0.00004334425,0.005893426,0.0008538837,0.0001009913,0.0003760553,0.2433428,0.4639707],"study_design_scores_gemma":[0.00170815,0.00810351,0.1613253,0.0001381847,0.00001386542,0.0002359424,0.01391406,0.002045964,0.001570499,0.02255537,0.7881792,0.0002100297],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9862056,0.005977924,0.00001750915,0.00476346,0.0005923882,0.0002199381,0.0000591412,0.000005745284,0.002158266],"genre_scores_gemma":[0.9973786,0.001090231,0.0004678716,0.00008655641,0.0008186621,0.000002127824,0.00003011678,0.000002223649,0.0001235992],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5448363,"threshold_uncertainty_score":0.3789949,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2611608464","doi":"10.1126/sciadv.1601693","title":"Miocene flooding events of western Amazonia","year":2017,"lang":"en","type":"article","venue":"Science Advances","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":204,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Directorate for Geosciences; Departamento Administrativo de Ciencia, Tecnología e Innovación (COLCIENCIAS); Smithsonian Institution; Division of Earth Sciences; National Science Foundation","keywords":"Amazon rainforest; Flooding (psychology); Geology; Paleontology; Geography; Earth science; Ecology; Biology","retraction":null,"screen_n_in":null,"score":{"opus":0.02388479074871872,"gpt":0.2821104803504518,"spread":0.2582256896017331,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003475979,0.00005893133,0.00009351118,0.00005188313,0.0008267078,0.00008548427,0.0007640077,0.00001567417,0.0003199578],"category_scores_gemma":[0.000219117,0.00003964139,0.00001935246,0.0001496787,0.0005873533,0.002022678,0.00002951207,0.00003956424,0.0001027651],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001171205,"about_ca_system_score_gemma":0.00004773716,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001827413,"about_ca_topic_score_gemma":0.0003175726,"domain_scores_codex":[0.9992141,0.00000686827,0.0001303706,0.0001579621,0.0002758765,0.00021482],"domain_scores_gemma":[0.9994396,0.00003336803,0.0001594939,0.0002257919,0.00007170142,0.00007005325],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000003424055,0.000004379172,0.9182451,0.00001188136,6.998312e-7,4.873319e-7,0.0000479998,0.0006001155,0.0001389948,0.00004343183,0.000001779583,0.08090168],"study_design_scores_gemma":[0.00007017675,0.00006368787,0.9883398,0.00002251922,0.000002111063,0.000003174795,0.00007799625,0.0002878286,0.005181469,0.004251591,0.001630652,0.00006899015],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9876322,0.0006549282,0.00008515381,0.0001976097,0.0003018919,0.00004428952,0.00001256025,0.0000120546,0.01105937],"genre_scores_gemma":[0.9981328,0.00009166783,0.001555358,0.00003303531,0.00002448877,3.520089e-7,0.00000189264,4.761106e-7,0.0001598988],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0808327,"threshold_uncertainty_score":0.6358452,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2146075665","doi":"10.1111/bre.12043","title":"Passive‐margin salt basins: hyperextension, evaporite deposition, and salt tectonics","year":2014,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":201,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Salt tectonics; Evaporite; Geochemistry; Salt dome; Tectonics; Geomorphology; Petrology; Paleontology; Structural basin; Diapir","retraction":null,"screen_n_in":null,"score":{"opus":0.03986664291525057,"gpt":0.2924155826015183,"spread":0.2525489396862678,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001345039,0.0001138503,0.0001566849,0.0001741828,0.000676671,0.0001851144,0.0002094941,0.0001076371,0.00157809],"category_scores_gemma":[0.0008118741,0.00008216703,0.00002856367,0.00053011,0.0002494474,0.000262213,0.00003837963,0.0003359674,0.0005507125],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004895515,"about_ca_system_score_gemma":0.00007422423,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001162766,"about_ca_topic_score_gemma":0.001113216,"domain_scores_codex":[0.9981403,0.000345844,0.0002129129,0.0002942666,0.0005311418,0.0004755106],"domain_scores_gemma":[0.9984003,0.0007266896,0.00003762463,0.0002258432,0.0003908717,0.0002186451],"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":[0.0001402377,0.00008820584,0.3075664,0.0002350404,0.00002269022,0.00003144822,0.0002812902,0.0003996945,0.0003205017,0.005044659,0.0130538,0.672816],"study_design_scores_gemma":[0.0003093222,0.0003918833,0.8559067,0.00005045174,0.000006437478,0.000073805,0.0001186686,0.01613855,0.0004445096,0.01457166,0.111793,0.0001950815],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9724864,0.001576906,0.0006964215,0.005159365,0.0001373208,0.0002858453,0.00005826296,0.00007402024,0.01952551],"genre_scores_gemma":[0.9961371,0.0005530206,0.002306132,0.0004288174,0.0001070682,0.000004068044,0.00008880713,0.00000375131,0.0003712706],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.672621,"threshold_uncertainty_score":0.9993346,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2115135275","doi":"10.1016/j.crte.2004.03.017","title":"Un nouveau point de départ pour l'histoire de l'Atlantique central","year":2004,"lang":"fr","type":"article","venue":"Comptes Rendus Géoscience","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":200,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Humanities; Magnetic anomaly; Crust; Paleontology; Philosophy","retraction":null,"screen_n_in":null,"score":{"opus":0.01908143090414324,"gpt":0.2191950182184465,"spread":0.2001135873143033,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005561565,0.0002684027,0.0002549451,0.00009403091,0.0009836971,0.0002383439,0.000788458,0.0002034583,0.008583595],"category_scores_gemma":[0.0002461007,0.0002317401,0.0001082536,0.0006792057,0.0009281547,0.0006019036,0.00006294504,0.0004201287,0.001349232],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001064759,"about_ca_system_score_gemma":0.0007720366,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004465677,"about_ca_topic_score_gemma":0.0007948257,"domain_scores_codex":[0.9974205,0.0001327577,0.0003652406,0.0004397838,0.0003222517,0.001319466],"domain_scores_gemma":[0.9987398,0.000176847,0.000143082,0.0002657591,0.00008159899,0.0005929449],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006644381,0.0005925465,0.6585743,0.0003172282,0.00003382426,0.0004593662,0.005506099,0.1440496,0.001053598,0.02119316,0.03210231,0.1360515],"study_design_scores_gemma":[0.0008244194,0.0006067719,0.7390043,0.0003638393,0.00005382737,0.001437329,0.001215717,0.03785592,0.003307029,0.06327403,0.1511239,0.0009329717],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8828873,0.02867327,0.01980642,0.04209853,0.002874614,0.0002582249,0.0001796568,0.0001634548,0.02305855],"genre_scores_gemma":[0.9724787,0.002100223,0.01999793,0.001414497,0.0002029223,0.000003015321,0.00004221389,0.000004994751,0.003755438],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1351186,"threshold_uncertainty_score":0.9994283,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1973417608","doi":"10.1306/8626d06d-173b-11d7-8645000102c1865d","title":"Lowstand Alluvial Bypass Systems: Incised vs. Unincised","year":2001,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":199,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Petro-Canada","funders":"","keywords":"Geology; Alluvium; Geomorphology; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.01260170916312024,"gpt":0.1928993240729201,"spread":0.1802976149097999,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002936534,0.0001318137,0.0001714021,0.00005457769,0.0002289622,0.0001081222,0.000233374,0.00009020228,0.02263423],"category_scores_gemma":[0.00008752392,0.0000969627,0.00004157902,0.0002117674,0.00007454235,0.00008180554,0.00001337215,0.0001207686,0.004698661],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003848459,"about_ca_system_score_gemma":0.00003070129,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001485739,"about_ca_topic_score_gemma":0.0002764497,"domain_scores_codex":[0.9989322,0.00007163209,0.0002500284,0.0001923379,0.0002385012,0.0003153249],"domain_scores_gemma":[0.9994075,0.0001513676,0.00007379121,0.0001605884,0.00006915095,0.0001375848],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.001274153,0.0002022449,0.6951092,0.0002476173,0.0001137365,0.0004116867,0.001026119,0.03355987,0.00003951838,0.002318619,0.2112337,0.05446352],"study_design_scores_gemma":[0.000461134,0.0001675724,0.06310508,0.00001646138,0.000009867746,0.00005242285,0.0002012599,0.003312141,0.00001160881,0.000318419,0.9321519,0.0001921231],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8469028,0.001622167,0.0006751512,0.004032491,0.0005527854,0.0003041573,0.00006731606,0.0001723173,0.1456707],"genre_scores_gemma":[0.9954406,0.0001960567,0.0002809853,0.0006556168,0.0001329279,0.000002872563,0.0001097281,0.00000273874,0.003178463],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7209182,"threshold_uncertainty_score":0.9960763,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2143999902","doi":"10.1306/07050504121","title":"Classification and characterizations of biogenically enhanced permeability","year":2005,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":199,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Permeability (electromagnetism); Chemistry","retraction":null,"screen_n_in":null,"score":{"opus":0.01563034553466947,"gpt":0.2129006733919235,"spread":0.197270327857254,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000122902,0.00004441777,0.00006955755,0.00002145146,0.00006949472,0.00001365406,0.00006255369,0.00003687097,0.007279352],"category_scores_gemma":[0.00008924658,0.0000336825,0.00001654296,0.00008112802,0.00008143848,0.00005419227,0.000005045883,0.00003636052,0.0002444926],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":7.797432e-7,"about_ca_system_score_gemma":0.00001052894,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0000595612,"about_ca_topic_score_gemma":0.00008048719,"domain_scores_codex":[0.9995685,0.00002447012,0.0001634549,0.00009946823,0.00006476539,0.00007938358],"domain_scores_gemma":[0.9996995,0.00007441385,0.00005597093,0.0000803169,0.00005007939,0.00003974959],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000588583,0.0001111095,0.6290346,0.00007759115,0.00001574224,2.37486e-7,0.0006119503,0.0003740904,0.00841596,0.00190307,0.0006884099,0.3587084],"study_design_scores_gemma":[0.00006480848,0.00004162075,0.955434,0.000003378051,0.000003792138,0.000001534569,0.00003812416,0.0009444688,0.0006927856,0.0002133134,0.04251463,0.00004755437],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9874632,0.0001262855,0.0003840296,0.004381977,0.00002029105,0.00006893125,0.00003380522,0.00001796785,0.007503562],"genre_scores_gemma":[0.9973157,0.0001281641,0.002123797,0.0001904779,0.00002550838,0.000001144016,0.00008118522,6.302081e-7,0.0001334101],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3586609,"threshold_uncertainty_score":0.9936281,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2136073011","doi":"10.2112/05-0607.1","title":"Wetland Loss in World Deltas","year":2008,"lang":"en","type":"article","venue":"Journal of Coastal Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":198,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Wetland; Delta; Indus; Nile delta; River delta; Niger delta; Hydrology (agriculture); Physical geography; Geology; Geography; Environmental science; Water resource management; Ecology; Geomorphology; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.1004069924060419,"gpt":0.3354213135194543,"spread":0.2350143211134124,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001214781,0.00004211972,0.000110119,0.0003859512,0.0001315509,0.00002864586,0.000203652,0.00002661155,0.002330298],"category_scores_gemma":[0.0002743592,0.00002680086,0.00003214708,0.0006988226,0.0001452858,0.0002971916,0.00001528138,0.0004346047,0.0001549771],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002902511,"about_ca_system_score_gemma":0.0001556945,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000517012,"about_ca_topic_score_gemma":0.009185184,"domain_scores_codex":[0.9987725,0.0001081942,0.0002498004,0.0000514423,0.0005710353,0.0002470493],"domain_scores_gemma":[0.9991627,0.0003630562,0.00005361859,0.00004926406,0.0002492672,0.0001221431],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001369304,0.00002669861,0.9809501,0.00001153798,0.000003756953,0.000483094,0.0001553884,0.001010897,0.000009378743,0.00005958047,0.002260424,0.01489222],"study_design_scores_gemma":[0.0002950719,0.0003124764,0.9678681,0.0000287449,6.135318e-7,0.0005091231,0.0001299385,0.0003410389,0.00009232068,0.003461055,0.02691569,0.00004584147],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9760226,0.0005809112,0.0000310329,0.0007322902,0.0000681469,0.00003468071,0.000007356594,0.000001964773,0.02252104],"genre_scores_gemma":[0.9982448,0.0004850008,0.0002816186,0.00003153147,0.00008112108,1.183217e-7,0.000003525776,7.828959e-7,0.0008714939],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02465527,"threshold_uncertainty_score":0.9985817,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2235801309","doi":"10.1016/j.earscirev.2015.10.013","title":"Estimation of source area, river paleo-discharge, paleoslope, and sediment budgets of linked deep-time depositional systems and implications for hydrocarbon potential","year":2015,"lang":"en","type":"article","venue":"Earth-Science Reviews","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":195,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"McMaster University","funders":"ExxonMobil Research and Engineering Company; Ecopetrol; BHP Billiton; Shell; Chevron; BP","keywords":"Sedimentary depositional environment; Provenance; Geology; Sedimentary rock; Siliciclastic; Fluvial; Context (archaeology); Paleontology; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.02717798880770632,"gpt":0.248598738832113,"spread":0.2214207500244067,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008727757,0.0000961561,0.0002448923,0.00008203259,0.0001645789,0.00004264897,0.0001278484,0.00003993284,0.00003195237],"category_scores_gemma":[0.0001743468,0.00006767494,0.00003400309,0.0002793003,0.0003488941,0.0003383312,0.00001829197,0.00003977776,0.0000113755],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001778653,"about_ca_system_score_gemma":0.00005931382,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00006756707,"about_ca_topic_score_gemma":0.00002084069,"domain_scores_codex":[0.9990084,0.00004451766,0.0003877677,0.0001983488,0.0001958603,0.000165074],"domain_scores_gemma":[0.9992542,0.00007786906,0.00024793,0.0001217659,0.0001477563,0.0001505325],"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":[0.0001104626,0.0002179437,0.1400404,0.001983983,0.00005167907,0.000001071573,0.002696846,0.07149202,0.01741432,0.002114655,0.0004011549,0.7634755],"study_design_scores_gemma":[0.0007200863,0.0007819825,0.533721,0.0003053411,0.0001078394,0.0001235734,0.0001313278,0.4529214,0.00118472,0.002871162,0.006755255,0.0003763784],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8165416,0.03803675,0.1416447,0.0003798684,0.0001541026,0.001595819,0.0001377862,0.00002665959,0.001482708],"genre_scores_gemma":[0.9787396,0.0009748362,0.0201102,0.00002662273,0.00002032703,0.00001365353,0.0000696814,0.000001287053,0.00004376272],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7630991,"threshold_uncertainty_score":0.2759704,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1980139141","doi":"10.1130/g25481a.1","title":"Tide- and wave-generated fluid mud deposits in the Tilje Formation (Jurassic), offshore Norway","year":2009,"lang":"en","type":"article","venue":"Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":188,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Queen's University","funders":"","keywords":"Citation; Geology; Icon; Submarine pipeline; Paleontology; Queen (butterfly); Download; Oceanography; Archaeology; Library science; World Wide Web; History; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.01720269741729351,"gpt":0.2069179218244285,"spread":0.189715224407135,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001958247,0.00007827192,0.00009843236,0.00005743224,0.0001416305,0.00003457402,0.0001051656,0.00007995171,0.0005366611],"category_scores_gemma":[0.00003203538,0.00004562869,0.00001375691,0.0002091496,0.00005206755,0.0002211123,0.000005333853,0.00009978915,0.0001496102],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001155793,"about_ca_system_score_gemma":0.00001149489,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002147827,"about_ca_topic_score_gemma":0.004574192,"domain_scores_codex":[0.999362,0.0000830416,0.0001691865,0.0001056782,0.00007494394,0.0002051297],"domain_scores_gemma":[0.9997387,0.00008214276,0.00003847871,0.00008357289,0.00002332544,0.00003381107],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001135307,0.00006771295,0.5817187,0.00004265738,0.00001164112,0.0000678656,0.003770996,0.004267321,0.0002230084,0.004104716,0.004567969,0.4010438],"study_design_scores_gemma":[0.0001443097,0.0002019854,0.9800739,0.000002872729,0.000004093513,0.0001162866,0.000119456,0.009675508,0.0001213436,0.005824844,0.003641736,0.00007367099],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9842858,0.000743931,0.0001884383,0.004097857,0.00006357304,0.000105411,0.000006150573,0.0000153115,0.01049349],"genre_scores_gemma":[0.9977081,0.0001278832,0.0002443613,0.001647998,0.00003472632,0.000001180243,0.0001669367,5.189486e-7,0.00006831809],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4009702,"threshold_uncertainty_score":0.5876062,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1540714975","doi":"10.2110/pec.07.52.0027","title":"The Ichnofacies Paradigm","year":2007,"lang":"en","type":"book-chapter","venue":"SEPM (Society for Sedimentary Geology) eBooks","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":187,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta; Simon Fraser University","funders":"","keywords":"Geology; Ichnology; Diagenesis; Paleontology; Petrophysics; Sedimentary rock; Interpretation (philosophy); Geologic record; Sequence (biology); Ichnofacies; Trace fossil; Facies","retraction":null,"screen_n_in":null,"score":{"opus":0.02820919559323079,"gpt":0.2333030119331205,"spread":0.2050938163398897,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006525553,0.0004855373,0.000416195,0.00005432764,0.00135165,0.00008441313,0.0006151934,0.0006277956,0.002577096],"category_scores_gemma":[0.00001393118,0.0003173629,0.000755643,0.00003082897,0.000974103,0.000122229,0.00005818436,0.0005641263,0.0004056545],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001526237,"about_ca_system_score_gemma":0.000109764,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0003166758,"about_ca_topic_score_gemma":0.0013808,"domain_scores_codex":[0.997848,0.00001285524,0.000562884,0.0004768287,0.000340618,0.0007587923],"domain_scores_gemma":[0.9983139,0.0007223291,0.0003016373,0.0004013991,0.0000918236,0.0001688996],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0005889907,0.00003937414,0.01059901,0.0005867029,0.003293439,0.00004136381,0.002127482,0.0005015436,0.000003473631,0.3911906,0.2134196,0.3776085],"study_design_scores_gemma":[0.0002821796,0.0003266007,0.0005251467,0.00001955973,0.0001236963,0.00002803236,0.0001557347,0.0002554216,0.00001522451,0.156753,0.8411444,0.0003710494],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.001132912,0.009617392,0.0003652393,0.002242251,0.00170444,0.001383641,0.0007452755,0.0002328145,0.982576],"genre_scores_gemma":[0.01060229,0.001631725,0.004600044,0.009180225,0.000924371,0.00003012904,0.002739903,0.00003875499,0.9702526],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.6277248,"threshold_uncertainty_score":0.9999484,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2067621802","doi":"10.1016/s0025-3227(02)00548-0","title":"Variability in form and growth of sediment waves on turbidite channel levees","year":2002,"lang":"en","type":"article","venue":"Marine Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":187,"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":"U.S. Geological Survey","keywords":"Geology; Turbidite; Turbidity current; Overbank; Levee; Sediment; Geomorphology; Bedform; Channel (broadcasting); Bathymetry; Sedimentary depositional environment; Sediment transport; Oceanography; Geotechnical engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.01742934181716316,"gpt":0.1938541332656962,"spread":0.176424791448533,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002532814,0.00006740617,0.0001325922,0.00006499442,0.00003332552,0.000004441367,0.00007050445,0.00005536584,0.005231307],"category_scores_gemma":[0.0001078215,0.00004763579,0.00001376174,0.0001079497,0.00009465708,0.00006842984,0.00002736774,0.00007444034,0.00004072454],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001286762,"about_ca_system_score_gemma":0.000003322085,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001963056,"about_ca_topic_score_gemma":0.001172696,"domain_scores_codex":[0.9994576,0.00004705074,0.0001579128,0.0001248404,0.00005802116,0.0001545518],"domain_scores_gemma":[0.999628,0.0002041937,0.00003899325,0.00007242818,0.000021695,0.00003469439],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001666541,0.00003383609,0.9817311,0.00003495363,0.000003439156,0.000002092689,0.000174352,0.0001672971,6.962988e-7,0.0009981432,0.00005890273,0.01677848],"study_design_scores_gemma":[0.0001674927,0.0002631788,0.9496669,0.000002601485,0.000002069229,0.000007958714,0.00001810282,0.008866136,0.00004317994,0.04047838,0.0004281795,0.00005578854],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9634591,0.000067842,0.00001851553,0.0009775053,0.00007131298,0.0000721937,0.000008140128,0.000009520771,0.03531589],"genre_scores_gemma":[0.9992346,0.0001088731,0.0002016466,0.0001943248,0.00001731587,0.000001281142,0.00002368939,5.953034e-7,0.000217648],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03948024,"threshold_uncertainty_score":0.9956781,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2090301004","doi":"10.1016/j.sedgeo.2011.04.020","title":"Subsurface and outcrop characterization of large tidally influenced point bars of the Cretaceous McMurray Formation (Alberta, Canada)","year":2011,"lang":"en","type":"article","venue":"Sedimentary Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":186,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Alberta","funders":"","keywords":"Outcrop; Geology; Facies; Cretaceous; Paleontology; Point bar; Oil sands; Marine transgression; Geomorphology; Structural basin; Archaeology","retraction":null,"screen_n_in":null,"score":{"opus":0.007771796164601,"gpt":0.1761726929585587,"spread":0.1684008967939577,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001299506,0.00007917261,0.0001351394,0.00002960408,0.00008979235,0.000002904587,0.0001365055,0.00005149416,0.002115663],"category_scores_gemma":[0.00002465801,0.00005173141,0.0000197719,0.0001149974,0.0001011477,0.0002319583,0.00002277516,0.00006354375,0.000005652112],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002936329,"about_ca_system_score_gemma":0.0000734586,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.2536106,"about_ca_topic_score_gemma":0.4318618,"domain_scores_codex":[0.9992939,0.00006229548,0.0002689331,0.00009238087,0.0001228973,0.0001596175],"domain_scores_gemma":[0.9995513,0.00005319257,0.0001834982,0.0001100741,0.00006191021,0.00004001552],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004924854,0.0000150988,0.9962265,0.00005172201,0.00001639925,7.560948e-7,0.001586582,0.0001453793,0.0008194512,0.0001250782,0.00003916895,0.0009245684],"study_design_scores_gemma":[0.0001828057,0.0001210071,0.9889609,0.000007692638,0.00001411747,0.00001339002,0.0002644822,0.0009957119,0.007871079,0.0003252666,0.001178523,0.00006505153],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9970027,0.00008850828,0.00007103097,0.0004588007,0.0001572693,0.0001451505,0.00008014765,0.000004502245,0.00199195],"genre_scores_gemma":[0.9989127,0.00003509539,0.0001620358,0.0006757927,0.000005743716,7.926859e-7,0.0001417253,0.000001106561,0.00006500801],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1782513,"threshold_uncertainty_score":0.9987965,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2886767111","doi":"10.1146/annurev-fluid-122316-045049","title":"Sediment Resuspension and Transport by Internal Solitary Waves","year":2018,"lang":"en","type":"article","venue":"Annual Review of Fluid Mechanics","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":186,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Waterloo; Queen's University","funders":"","keywords":"Turbulence; Internal wave; Geology; Sediment transport; Sediment; Reynolds stress; Boundary layer; Oceanography; Scale (ratio); Environmental science; Geophysics; Meteorology; Mechanics; Geomorphology; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01000482982237186,"gpt":0.2368794722879938,"spread":0.2268746424656219,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003950995,0.00008509017,0.0001838696,0.00001996167,0.00006335095,0.000004150535,0.0001117917,0.00003705409,0.001600231],"category_scores_gemma":[0.00005183003,0.00005642656,0.00003702288,0.00009502461,0.00004653007,0.0001689949,0.00001058165,0.00005473977,0.00006030418],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000108603,"about_ca_system_score_gemma":0.00001981321,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002053357,"about_ca_topic_score_gemma":0.0000651119,"domain_scores_codex":[0.9992692,0.00003028205,0.0002726052,0.0001280223,0.0001671786,0.0001326962],"domain_scores_gemma":[0.9996059,0.00003693177,0.00006288186,0.00009699153,0.000119975,0.00007734999],"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":[0.000296497,0.0001800733,0.008777237,0.01360176,0.0001376392,0.00002514315,0.002111784,0.00001170184,0.001508891,0.009813942,0.1366601,0.8268752],"study_design_scores_gemma":[0.0006753971,0.00469758,0.01310335,0.008338571,0.0002114107,0.0001441115,0.001035372,0.008065853,0.009994477,0.01533803,0.9376437,0.0007521312],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"review","genre_gemma":"empirical","genre_scores_codex":[0.4273008,0.5454802,0.003568262,0.0035748,0.0008689679,0.0008262245,0.001167201,0.00007814292,0.01713545],"genre_scores_gemma":[0.8785453,0.1186331,0.0007283613,0.00180031,0.00004377444,6.342767e-7,0.000137114,0.00000155856,0.0001098533],"genre_candidate":"empirical","genre_consensus":null,"teacher_disagreement_score":0.8261231,"threshold_uncertainty_score":0.9993125,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2192490761","doi":"10.1016/b978-0-444-53813-0.00004-6","title":"The Ichnofacies Paradigm","year":2012,"lang":"en","type":"book-chapter","venue":"Developments in sedimentology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":181,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta; Simon Fraser University","funders":"","keywords":"Ichnofacies; Geology; Facies; Paleontology; Sedimentary depositional environment","retraction":null,"screen_n_in":null,"score":{"opus":0.02500414306539584,"gpt":0.222366346388906,"spread":0.1973622033235102,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002983033,0.0002108189,0.0002256351,0.0001019645,0.0002433652,0.00003107454,0.0003106394,0.0002704252,0.00533665],"category_scores_gemma":[0.00002166276,0.0001304453,0.00003327886,0.00004829083,0.0002040316,0.000130956,0.00003265982,0.0002779906,0.002360838],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001005569,"about_ca_system_score_gemma":0.00007723699,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00005853682,"about_ca_topic_score_gemma":0.001149502,"domain_scores_codex":[0.9988073,0.000020285,0.0003673638,0.0001894632,0.0001953123,0.0004202577],"domain_scores_gemma":[0.9993936,0.000221947,0.0001381132,0.0001532779,0.00002118032,0.0000719285],"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":[0.00004116212,0.00001291188,0.1604189,0.0000388813,0.0001117213,0.00002669727,0.0005645624,0.00003914964,1.23781e-7,0.354846,0.003364699,0.4805352],"study_design_scores_gemma":[0.00009141112,0.00002001386,0.05900294,0.00001378023,0.000007024991,0.000019063,0.00001828386,0.000006844326,0.000001758394,0.04177595,0.89887,0.0001729021],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.0007576642,0.01029199,0.00001582704,0.0006261874,0.0009752577,0.0002078673,0.00002834369,0.00003430503,0.9870626],"genre_scores_gemma":[0.2659539,0.01167967,0.002441154,0.001686055,0.0002405866,0.00002052796,0.001087132,0.00001976805,0.7168712],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.8955053,"threshold_uncertainty_score":0.9984159,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2276570023","doi":"10.1017/cbo9780511975622.004","title":"Paleobiology of trace fossils","year":2011,"lang":"en","type":"book-chapter","venue":"Cambridge University Press eBooks","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":178,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Trace fossil; Ichnology; TRACE (psycholinguistics); Geology; Paleontology; Sedimentology; Paleobiology; Connection (principal bundle); Engineering; Philosophy","retraction":null,"screen_n_in":null,"score":{"opus":0.03175281156110635,"gpt":0.1771620700708204,"spread":0.1454092585097141,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006810697,0.000176763,0.0002846591,0.00009063604,0.00009616353,0.000007855871,0.0003535285,0.0002960234,0.0003960089],"category_scores_gemma":[0.000007052332,0.0001580599,0.0001149315,0.000006713614,0.0002951515,0.00006767192,0.00003102477,0.0002057137,0.00005565281],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002840495,"about_ca_system_score_gemma":0.00004878739,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000622525,"about_ca_topic_score_gemma":0.00004390528,"domain_scores_codex":[0.9993407,0.00002259378,0.000161746,0.0002117253,0.00009093525,0.0001723753],"domain_scores_gemma":[0.9993317,0.00007541332,0.0002005196,0.0002057809,0.00009448081,0.00009209135],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0001724897,0.000009018049,0.0009985205,0.0002212029,0.0001246629,0.0000857674,0.0001079948,0.00001836059,0.000004643769,0.9575781,0.006910158,0.03376904],"study_design_scores_gemma":[0.0001713149,0.0001625458,0.003625756,0.00004524759,0.00008302931,0.00001584306,0.00002055087,0.0000233246,0.00009887542,0.0001960915,0.995315,0.0002424023],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.001392264,0.000680196,0.0001024563,0.000004831798,0.0001217437,0.000134935,0.0005568232,0.00003620779,0.9969705],"genre_scores_gemma":[0.0788052,0.0002586141,0.0001144397,0.000018033,0.0000301681,4.133439e-8,0.00009855552,0.000002755099,0.9206722],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.9884049,"threshold_uncertainty_score":0.6445494,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2071859844","doi":"10.1306/02220605065","title":"Reconstructing the architecture and sequence stratigraphy of the preserved fluvial record as a tool for reservoir development: A reality check","year":2006,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":174,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Fluvial; Sequence stratigraphy; Sequence (biology); Stratigraphy; Architecture; Paleontology; Archaeology; Facies; Geography; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.02692697173353587,"gpt":0.2239462708305966,"spread":0.1970192990970608,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004890943,0.00008706496,0.0001014528,0.00001817808,0.0003958182,0.00004930863,0.000248569,0.00005155938,0.0005159222],"category_scores_gemma":[0.0002462437,0.00004357688,0.00004467692,0.0001496697,0.0001792642,0.00004095459,0.00002140942,0.0001232576,0.000005926192],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000106415,"about_ca_system_score_gemma":0.00005993933,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003548359,"about_ca_topic_score_gemma":0.004565503,"domain_scores_codex":[0.9992073,0.00009041066,0.0002585597,0.0001465442,0.0001254452,0.0001717409],"domain_scores_gemma":[0.9992661,0.0003756533,0.0001302665,0.0001494127,0.00005594738,0.00002257422],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003565355,0.0000292708,0.9231135,0.0003381329,0.00004261991,0.000001413266,0.001020304,0.001565543,0.0002731239,0.001964021,0.004495413,0.06680018],"study_design_scores_gemma":[0.0003860777,0.0001810077,0.7238073,0.00007893152,0.00001792282,0.00003983281,0.0003915033,0.0007699819,0.001525702,0.06406557,0.2085104,0.0002257404],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9899315,0.0002039066,0.00008026609,0.004023443,0.00005586569,0.0003316267,0.00005325664,0.00001433385,0.005305848],"genre_scores_gemma":[0.9928181,0.00001174666,0.006684131,0.000134166,0.00004331477,0.00000879565,0.00002581269,0.000001313062,0.000272646],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.204015,"threshold_uncertainty_score":0.5648986,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1981091938","doi":"10.1016/j.sedgeo.2012.07.018","title":"Tidal dunes versus tidal bars: The sedimentological and architectural characteristics of compound dunes in a tidal seaway, the lower Baronia Sandstone (Lower Eocene), Ager Basin, Spain","year":2012,"lang":"en","type":"article","venue":"Sedimentary Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":167,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta; Queen's University","funders":"","keywords":"Geology; Paleocurrent; Ichnofacies; Paleontology; Ripple marks; Geomorphology; Accretion (finance); Structural basin; Sedimentary depositional environment","retraction":null,"screen_n_in":null,"score":{"opus":0.01549268994324316,"gpt":0.2266061768021588,"spread":0.2111134868589156,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007491651,0.0002651086,0.0003721902,0.00008292474,0.0002782079,0.0000356158,0.0003328834,0.0001509004,0.004175972],"category_scores_gemma":[0.00007937856,0.0001398188,0.0000773835,0.0002268355,0.0009569539,0.0002269461,0.0001051004,0.0003862387,0.0000815358],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005096688,"about_ca_system_score_gemma":0.00004089714,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002740476,"about_ca_topic_score_gemma":0.001992614,"domain_scores_codex":[0.998025,0.0003524182,0.0004443343,0.0002615154,0.0002602212,0.0006564844],"domain_scores_gemma":[0.9983799,0.001060901,0.000150579,0.0002336196,0.00004009999,0.0001349213],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0008579187,0.0001423143,0.9912204,0.00002699472,0.00006443923,0.00002465329,0.000864707,0.0002073919,0.00002633396,0.0002529928,0.0002698694,0.006041979],"study_design_scores_gemma":[0.0008919506,0.0007587501,0.987387,0.00001142615,0.00004646712,0.0001585111,0.00052983,0.0008151374,0.00005878056,0.0005046573,0.008631708,0.00020577],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9909788,0.001359217,0.00001572386,0.00494952,0.001198312,0.0002917898,0.00008248819,0.00002450633,0.001099584],"genre_scores_gemma":[0.997726,0.00008535611,0.0002769428,0.001364834,0.0002479782,0.000007050616,0.0002001171,0.00000444656,0.00008724406],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.008361839,"threshold_uncertainty_score":0.9967343,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2297661888","doi":"10.1016/j.sedgeo.2016.01.005","title":"Downstream-migrating fluvial point bars in the rock record","year":2016,"lang":"en","type":"article","venue":"Sedimentary Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":165,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary; Laurentian University","funders":"","keywords":"Meander (mathematics); Point bar; Geology; Fluvial; Alluvial fan; Geomorphology; Aggradation; Alluvium; Floodplain; Sinuosity; Sedimentary rock; Paleontology; Geometry; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.01081416287358387,"gpt":0.2043039107096191,"spread":0.1934897478360353,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003202387,0.00009933984,0.0001125587,0.00005958228,0.0001344152,0.00001341651,0.0002469896,0.00006007494,0.01303029],"category_scores_gemma":[0.00004822939,0.00004545701,0.00003383834,0.0001563952,0.00006674278,0.0002173597,0.00001610054,0.0001053775,0.0008805421],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000031697,"about_ca_system_score_gemma":0.0000213822,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004901321,"about_ca_topic_score_gemma":0.008601532,"domain_scores_codex":[0.9990543,0.0001423679,0.0002217705,0.0001713836,0.0001090913,0.0003010608],"domain_scores_gemma":[0.9993712,0.0003867529,0.00005120709,0.0001322224,0.0000150618,0.00004359553],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000374461,0.00001709498,0.9104961,0.000004485941,0.000007019018,0.00001658834,0.0003748742,0.0002430219,0.00002316395,0.0001559105,0.002697014,0.08592735],"study_design_scores_gemma":[0.0008118412,0.0007219707,0.9286756,0.00002101598,0.00001218618,0.0001254905,0.001640393,0.001043979,0.0001981,0.02111861,0.04538253,0.0002483217],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9772489,0.0002091609,0.0001364284,0.01136874,0.0003346653,0.0001366026,0.00002269545,0.00002568446,0.01051709],"genre_scores_gemma":[0.996106,0.00006826759,0.0005035367,0.002996283,0.0001044868,0.000003428959,0.00005962635,0.000001035914,0.000157311],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08567902,"threshold_uncertainty_score":0.9998974,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2119253142","doi":"10.1111/sed.12068","title":"Mud dispersal across a Cretaceous prodelta: Storm‐generated, wave‐enhanced sediment gravity flows inferred from mudstone microtexture and microfacies","year":2013,"lang":"en","type":"article","venue":"Sedimentology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":160,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"","keywords":"Geology; Silt; Settling; Siltstone; Geomorphology; Sediment; Deposition (geology); Petrology; Mineralogy; Facies; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.0133309931635852,"gpt":0.2258108631823217,"spread":0.2124798700187365,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001417585,0.00027569,0.0003541769,0.00004967871,0.0003707734,0.0001542276,0.0001860375,0.0002392765,0.003728943],"category_scores_gemma":[0.00004012765,0.0002022674,0.00005122868,0.0001844583,0.0002571524,0.0003805985,0.00005956308,0.000247568,0.0004585337],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009168663,"about_ca_system_score_gemma":0.00004147476,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01069587,"about_ca_topic_score_gemma":0.009348298,"domain_scores_codex":[0.9983503,0.00009920021,0.0003315613,0.0004565512,0.0001721813,0.0005901587],"domain_scores_gemma":[0.9992566,0.00009493985,0.0001167119,0.0002150044,0.0001152531,0.000201513],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0007049069,0.0005166402,0.4566484,0.0002942918,0.0007441359,0.000111109,0.03229993,0.003183729,0.2014328,0.0001486444,0.01063275,0.2932826],"study_design_scores_gemma":[0.003594076,0.001232023,0.8632371,0.00005554456,0.000133803,0.00020735,0.004755592,0.03525061,0.046972,0.006506082,0.03639855,0.001657261],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.992488,0.004031565,0.0005551011,0.001267261,0.000476496,0.0004958283,0.0003105444,0.00008125913,0.0002939179],"genre_scores_gemma":[0.9957425,0.0001732266,0.002342358,0.0006873602,0.00009749756,0.0000215764,0.0006512405,0.000004826929,0.0002794421],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4065886,"threshold_uncertainty_score":0.9971818,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1674302729","doi":"10.1111/j.1365-3091.2007.00948.x","title":"Deep‐water foreland basin deposits of the Cerro Toro Formation, Magallanes basin, Chile: architectural elements of a sinuous basin axial channel belt","year":2008,"lang":"en","type":"article","venue":"Sedimentology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":159,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"Hess Corporation","keywords":"Geology; Conglomerate; Foreland basin; Turbidity current; Facies; Turbidite; Geomorphology; Structural basin; Sedimentary rock; Paleontology; Cretaceous; Outcrop; Geochemistry; Sedimentary depositional environment","retraction":null,"screen_n_in":null,"score":{"opus":0.01168373468269079,"gpt":0.196498416295979,"spread":0.1848146816132882,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001634809,0.0001525105,0.00028214,0.00008485714,0.0002499896,0.000009482388,0.0002871403,0.0001019996,0.0009912922],"category_scores_gemma":[0.00004206369,0.00008344777,0.00008335411,0.0001605538,0.0002269256,0.0001641241,0.00003720745,0.0001104016,0.00003096115],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004260623,"about_ca_system_score_gemma":0.00003115876,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001131684,"about_ca_topic_score_gemma":0.003493589,"domain_scores_codex":[0.9986401,0.0001247575,0.0004742374,0.0001568855,0.000249416,0.0003545842],"domain_scores_gemma":[0.9993976,0.00008419493,0.0001887186,0.0001701702,0.00009470887,0.00006454387],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002564278,0.00009477122,0.9829206,0.0001606186,0.00007963208,0.00001070193,0.004335944,0.002662082,0.0001846171,0.00007952061,0.0008087874,0.008406232],"study_design_scores_gemma":[0.0008570199,0.000513607,0.978999,0.00002198876,0.00004050863,0.0005692265,0.00018442,0.002711267,0.01231775,0.001591668,0.002007322,0.0001862834],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9954093,0.0002559175,0.00030128,0.0009105888,0.0003226925,0.0002642579,0.0000556946,0.00001731006,0.002462978],"genre_scores_gemma":[0.9987229,0.00003026679,0.0004733962,0.0003842602,0.00005028647,0.0000033578,0.0002299405,0.000002773973,0.0001027901],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01213314,"threshold_uncertainty_score":0.9999219,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}