{"meta":{"query_hash":"afcff8162c20","filters":{"venue":"Basin Research"},"cohort_total":81,"direct_labels_cover":0,"predictions_cover":81,"exported":81,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/afcff8162c20","api":"https://metacan.xera.ac/api/v1/cohort?venue=Basin+Research"},"results":[{"id":"W1544039212","doi":"10.1111/j.1365-2117.2009.00443.x","title":"Importance of predecessor basin history on sedimentary fill of a retroarc foreland basin: provenance analysis of the Cretaceous Magallanes basin, Chile (50–52°S)","year":2009,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Foreland basin; Provenance; Geology; Detritus; Paleontology; Diachronous; Sedimentary depositional environment; Zircon; Sedimentary rock; Paleocurrent; Structural basin; Isopach map; Lithic fragment; Cretaceous; Clastic rock","score_opus":0.03194670409207083,"score_gpt":0.26023685676582053,"score_spread":0.2282901526737497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1544039212","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97940207,0.0017927749,0.000004486956,0.0031576494,0.000052578867,0.0003618153,0.00046365507,0.00001343381,0.014751511],"genre_scores_gemma":[0.99720794,0.00020208217,0.00033057277,0.00049475423,0.000041438427,0.00000386376,0.00015899578,0.0000042008396,0.0015561268],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9962007,0.00050337974,0.0007030092,0.0005631881,0.001463315,0.0005664263],"domain_scores_gemma":[0.9976435,0.0007112443,0.00037073094,0.0007674162,0.00034225188,0.00016489382],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014948066,0.00022329004,0.0007998185,0.00039386438,0.00012257174,0.000013542,0.00083795504,0.0001376577,0.00886594],"category_scores_gemma":[0.0005845224,0.00013652125,0.00048181068,0.0018801915,0.00068371964,0.000095052914,0.000061591985,0.00044085432,0.000015215458],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053867075,0.0002839085,0.9831388,0.000085487125,0.00029607886,0.000012995196,0.00013522137,0.0011948238,0.0011741922,0.00005888711,0.009820844,0.0032601138],"study_design_scores_gemma":[0.0003023015,0.00069684687,0.97893476,0.000072603034,0.00023042102,0.000002796389,0.00006962493,0.004108348,0.0061382097,0.0015837704,0.007701809,0.00015848003],"about_ca_topic_score_codex":0.006285276,"about_ca_topic_score_gemma":0.002588997,"teacher_disagreement_score":0.01780587,"about_ca_system_score_codex":0.000036873902,"about_ca_system_score_gemma":0.00014248461,"threshold_uncertainty_score":0.9920401},"labels":[],"label_agreement":null},{"id":"W1580955337","doi":"10.1111/j.1365-2117.2011.00501.x","title":"Rapid extensive erosion of the North Alpine foreland basin at 5-4 Ma","year":2011,"lang":"en","type":"article","venue":"Basin Research","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Social Fund; AGE-WELL; Alexander von Humboldt-Stiftung","keywords":"Foreland basin; Molasse; Geology; Neogene; Thermochronology; Denudation; Paleontology; Tectonics; Fission track dating; Structural basin; Erosion; Magnetostratigraphy; Geomorphology; Late Miocene; Plateau (mathematics); Sedimentary rock","score_opus":0.10476734896925531,"score_gpt":0.29211176550714324,"score_spread":0.18734441653788791,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1580955337","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9591281,0.0007993714,0.000004273609,0.0009060545,0.00016657739,0.00037603982,0.000050765964,0.000012111826,0.0385567],"genre_scores_gemma":[0.99667263,0.00034109215,0.00020940564,0.00010309333,0.000038405375,0.000004519709,0.000037633698,0.0000044226827,0.0025888174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99697894,0.0010652957,0.00024081225,0.00033479423,0.00065733487,0.00072281866],"domain_scores_gemma":[0.99820673,0.00070790574,0.00006149103,0.000543319,0.00032504997,0.0001554961],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0015685023,0.00012150349,0.0002283767,0.00018960674,0.00057381066,0.000010745646,0.00066792965,0.00017178655,0.00906762],"category_scores_gemma":[0.00040740872,0.000074340394,0.000092932125,0.0006219155,0.0014835218,0.00008246727,0.00013070165,0.0005985188,0.0009965779],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036631964,0.000043722903,0.99292547,0.000024900206,0.000015876705,0.00003651361,0.0003603145,0.00000387635,0.000023703848,0.00018806763,0.0041052047,0.0019060166],"study_design_scores_gemma":[0.0003516037,0.00028969016,0.99428934,0.000031734256,0.000006412258,0.00007566994,0.00012359612,0.000239487,0.0013925584,0.0010302748,0.002088172,0.00008146626],"about_ca_topic_score_codex":0.0013422584,"about_ca_topic_score_gemma":0.010652604,"teacher_disagreement_score":0.0375445,"about_ca_system_score_codex":0.0000037653872,"about_ca_system_score_gemma":0.00014467626,"threshold_uncertainty_score":0.99978125},"labels":[],"label_agreement":null},{"id":"W1830135526","doi":"10.1111/j.1365-2117.2010.00497.x","title":"Timing and mechanisms controlling evaporite diapirism on Ellef Ringnes Island, Canadian Arctic Archipelago","year":2010,"lang":"en","type":"article","venue":"Basin Research","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Toronto","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Diapir; Evaporite; Geology; Archipelago; Paleontology; Salt tectonics; Sedimentary rock; Salt dome; Structural basin; Tectonics; Rift; Graben; Geochemistry; Geomorphology; Oceanography","score_opus":0.0331811264638438,"score_gpt":0.29009755106441926,"score_spread":0.25691642460057545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1830135526","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97817564,0.00021480964,0.004012107,0.0024541696,0.00047001004,0.000441653,0.000028993343,0.00015992085,0.014042672],"genre_scores_gemma":[0.9985714,0.00011520417,0.00042516264,0.00007691016,0.00017799195,0.00003642873,0.000015857291,0.00004200373,0.0005390659],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99829113,0.00011602878,0.00019880093,0.00026875967,0.00049561745,0.0006296485],"domain_scores_gemma":[0.998761,0.00029816,0.00001349983,0.00033059722,0.00012262832,0.00047414558],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011944782,0.00015415056,0.00021008168,0.0007816317,0.00033482022,0.00017731251,0.00020817001,0.0001401506,0.0002959363],"category_scores_gemma":[0.0003159407,0.00014053544,0.0000604413,0.00039737948,0.00008565525,0.00009625805,0.00003616181,0.000997934,0.00016528193],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004090124,0.000410044,0.012078936,0.0014208087,0.0015637538,0.0013534252,0.018336723,0.15251426,0.52154136,0.1172908,0.009751976,0.16332889],"study_design_scores_gemma":[0.0013331599,0.00014122558,0.0025955827,0.00012334337,0.000037725364,0.000019748548,0.00089900516,0.9472367,0.010470023,0.014400128,0.022143908,0.00059943745],"about_ca_topic_score_codex":0.021222407,"about_ca_topic_score_gemma":0.28026426,"teacher_disagreement_score":0.79472244,"about_ca_system_score_codex":0.00007363971,"about_ca_system_score_gemma":0.00009327902,"threshold_uncertainty_score":0.98529536},"labels":[],"label_agreement":null},{"id":"W1918429016","doi":"10.1111/bre.12147","title":"Regional stratigraphy and subsidence of Orphan Basin near the time of breakup and implications for rifting processes","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Geology; Rift; Thermal subsidence; Subsidence; Continental crust; Paleontology; Tectonic subsidence; Crust; Lithosphere; Continental margin; Passive margin; Structural basin; Seismology; Tectonics","score_opus":0.10575741917450958,"score_gpt":0.3228942014262803,"score_spread":0.2171367822517707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1918429016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922258,0.0012998689,0.000020782452,0.005357545,0.0000023088337,0.00014806553,0.00007060264,0.0000039177075,0.00087105954],"genre_scores_gemma":[0.9986668,0.00007156932,0.0011082835,0.00003719484,0.00001594577,0.0000037668838,0.000022313507,8.0180905e-7,0.000073326206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922013,0.000089754234,0.00014060497,0.0001579667,0.00022399308,0.00016755586],"domain_scores_gemma":[0.99814177,0.0011933363,0.00004527258,0.00010469495,0.0004158446,0.00009906775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009656841,0.00004848489,0.00011817046,0.00004591488,0.00016949819,0.00004110112,0.00015707305,0.000032807977,0.00013468805],"category_scores_gemma":[0.0007205164,0.000027665237,0.000024422716,0.00045918938,0.0007926603,0.00006546061,0.00002075906,0.000078115656,0.000003341485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006245852,0.00002416561,0.99091786,0.00007763182,0.000016146789,2.6748287e-7,0.00021832195,0.00002677998,0.0007698369,0.00059163885,0.00096184126,0.0063330433],"study_design_scores_gemma":[0.00013002807,0.0001882444,0.9279258,0.000019048162,0.000011131033,0.0000061751107,0.00025155404,0.00163692,0.0010257817,0.06793376,0.0008231177,0.000048389695],"about_ca_topic_score_codex":0.003461163,"about_ca_topic_score_gemma":0.001252265,"teacher_disagreement_score":0.067342125,"about_ca_system_score_codex":5.9362327e-7,"about_ca_system_score_gemma":0.000119581586,"threshold_uncertainty_score":0.5232266},"labels":[],"label_agreement":null},{"id":"W1920371487","doi":"10.1111/bre.12152","title":"Salt tectonics in an intracontinental transform setting: Cumberland and Sackville basins, southern New Brunswick, Canada","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of New Brunswick","funders":"Agence Nationale de Sécurité Sanitaire de l’Alimentation, de l’Environnement et du Travail; New Brunswick Innovation Foundation; Petroleum Research Newfoundland and Labrador","keywords":"Geology; Unconformity; Paleontology; Red beds; Pennsylvanian; Diapir; Anticline; Evaporite; Geomorphology; Structural basin","score_opus":0.04669535743084163,"score_gpt":0.28991773409113186,"score_spread":0.24322237666029023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1920371487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9871727,0.0008063686,0.000015781408,0.0027272739,0.00005764611,0.0001851092,0.0000665453,0.000015580923,0.008952989],"genre_scores_gemma":[0.99826473,0.000061050014,0.0006773507,0.00011901093,0.000065518274,6.196266e-7,0.00009561291,0.0000031803077,0.00071295083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99853206,0.0001415631,0.00019087191,0.00020645285,0.0004768688,0.00045217713],"domain_scores_gemma":[0.99918157,0.0001735707,0.000020605743,0.000115802206,0.000098294884,0.00041014608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010835566,0.00009610469,0.00012970428,0.0000989736,0.0001520509,0.00012435162,0.00019808931,0.00007223893,0.0007458346],"category_scores_gemma":[0.00016969592,0.0000725085,0.000011604521,0.00037060305,0.00009054232,0.00025248743,0.00001461222,0.00032387828,0.000050933028],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007695735,0.000018290702,0.8972712,0.000023656172,0.0000029466607,0.00002333199,0.00096782297,0.00019929092,0.0000030849862,0.000054522054,0.002349992,0.099008895],"study_design_scores_gemma":[0.001195627,0.0004475873,0.86683756,0.00003724867,0.0000040112977,0.00005453427,0.007625249,0.011472798,0.00012772025,0.0022237205,0.109682426,0.00029151273],"about_ca_topic_score_codex":0.92829245,"about_ca_topic_score_gemma":0.99708116,"teacher_disagreement_score":0.10733243,"about_ca_system_score_codex":0.000016758418,"about_ca_system_score_gemma":0.0026017367,"threshold_uncertainty_score":0.8166366},"labels":[],"label_agreement":null},{"id":"W1968295696","doi":"10.1111/bre.12077","title":"Historical developments in<scp>W</scp>heeler diagrams and future directions","year":2014,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sequence (biology); Diagram; Sequence diagram; Chart; Dimension (graph theory); Geology; Stratigraphic unit; Computer science; Paleontology; Programming language; Mathematics; Pure mathematics; Unified Modeling Language; Statistics","score_opus":0.04964001869464606,"score_gpt":0.2845416739892975,"score_spread":0.23490165529465146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968295696","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92786473,0.0020662877,0.000023654615,0.0014568698,0.00023483197,0.00012146345,0.000003842972,0.000027791531,0.06820053],"genre_scores_gemma":[0.99547744,0.0011602748,0.0008394171,0.00007200474,0.0001717319,0.000005659431,0.000017485987,0.0000016924545,0.0022542696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99887806,0.00017496865,0.00013352864,0.00017400486,0.00030236316,0.00033704867],"domain_scores_gemma":[0.998907,0.0007799079,0.000015431055,0.000086072985,0.000079702666,0.00013187714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009542794,0.00006510286,0.000100306796,0.00017134717,0.00029582845,0.00007206623,0.00013090445,0.000080862716,0.0002795136],"category_scores_gemma":[0.00063250976,0.000046819725,0.000013958916,0.0005946064,0.00006620756,0.00014515087,0.000021514063,0.000271291,0.00020472493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000025877148,0.000018777933,0.7802896,0.000016298929,0.000001936882,0.000002085803,0.00028691554,0.000006632865,0.0000011412598,0.00033323152,0.003982756,0.21505807],"study_design_scores_gemma":[0.0000506568,0.000034244917,0.50936896,0.0000029257997,3.841751e-7,0.000002797732,0.00012370141,0.000119323566,0.000004206323,0.000768721,0.48950735,0.000016709953],"about_ca_topic_score_codex":0.0013079157,"about_ca_topic_score_gemma":0.0020378092,"teacher_disagreement_score":0.4855246,"about_ca_system_score_codex":0.000014388216,"about_ca_system_score_gemma":0.00004192304,"threshold_uncertainty_score":0.3060478},"labels":[],"label_agreement":null},{"id":"W1970726042","doi":"10.1111/bre.12078","title":"Rifting and pre‐rift lithosphere variability in the <scp>O</scp>rphan <scp>B</scp>asin, <scp>N</scp>ewfoundland margin, Eastern <scp>C</scp>anada","year":2014,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; University of Saskatchewan","funders":"","keywords":"Geology; Rift; Lithosphere; Subsidence; Thermal subsidence; Tectonics; Paleontology; Seismology; Passive margin; Continental margin; Structural basin","score_opus":0.026905859872440794,"score_gpt":0.26268953111621524,"score_spread":0.23578367124377445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970726042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91517127,0.0020483602,0.00018613071,0.0008111596,0.00020538834,0.0009797883,0.00016850825,0.00012314142,0.08030625],"genre_scores_gemma":[0.9840178,0.0003908346,0.00080134877,0.0008314431,0.00065405807,0.000054624525,0.0002854248,0.000034009892,0.012930469],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9863815,0.0044484395,0.0011895116,0.0021232213,0.002771969,0.0030853865],"domain_scores_gemma":[0.9550113,0.041538864,0.00033842918,0.001431974,0.00056391413,0.0011154886],"candidate_categories":["metaresearch","metaepi_narrow","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0123648625,0.00085437665,0.0011682251,0.00037599102,0.0012655469,0.0010885342,0.0022095395,0.00072086934,0.0006017225],"category_scores_gemma":[0.04191576,0.00058372563,0.0003678638,0.0028609817,0.00133081,0.00057217793,0.000559923,0.002524639,0.0008133724],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010145565,0.0003010223,0.9727865,0.0002585908,0.00010132344,0.00011229406,0.002234064,0.0003374866,0.00024365763,0.00029439776,0.013719177,0.009601351],"study_design_scores_gemma":[0.0010153449,0.00050337287,0.7621438,0.00012662109,0.00008380602,0.00006441478,0.0052258144,0.018046828,0.00055168447,0.020549593,0.19158204,0.00010668197],"about_ca_topic_score_codex":0.030543337,"about_ca_topic_score_gemma":0.025831347,"teacher_disagreement_score":0.2106427,"about_ca_system_score_codex":0.00005264212,"about_ca_system_score_gemma":0.00028014323,"threshold_uncertainty_score":0.9999646},"labels":[],"label_agreement":null},{"id":"W1980383452","doi":"10.1111/j.1365-2117.2009.00415.x","title":"Basin evolution, diagenesis and uranium mineralization in the Paleoproterozic Thelon Basin, Nunavut, Canada","year":2009,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Cameco (Canada); Queen's University","funders":"","keywords":"Diagenesis; Geology; Geochemistry; Fluid inclusions; Illite; Uranium ore; Quartz; Uranium; Paleontology; Clay minerals","score_opus":0.0261426786254805,"score_gpt":0.2501355753589375,"score_spread":0.223992896733457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980383452","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97786385,0.00089226186,0.000043906457,0.0170127,0.000027699483,0.00023657441,0.000027508204,0.0000100422885,0.003885482],"genre_scores_gemma":[0.998172,0.000117851116,0.00009669439,0.0011472283,0.00008100154,0.000004418709,0.00006987834,0.0000013972167,0.00030952733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976279,0.0006558276,0.00020866288,0.0003173605,0.0007071017,0.00048310377],"domain_scores_gemma":[0.99906003,0.00045571267,0.00002834184,0.00021520915,0.00011949814,0.00012120036],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013348681,0.000117168194,0.00016822618,0.00011813064,0.00027617117,0.00008943762,0.000313884,0.000068837944,0.0017171381],"category_scores_gemma":[0.0003866991,0.00006874721,0.000036767447,0.001095012,0.0001268231,0.000094048046,0.000015267236,0.0002528659,0.000027540684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003260375,0.000030059675,0.98563087,0.000009628426,0.0000044990284,0.000031280713,0.00007345798,0.00012322323,0.00012583545,0.00020199879,0.0037787445,0.00995778],"study_design_scores_gemma":[0.00013453116,0.000084649604,0.9864888,0.000010985401,0.0000057788707,0.0000075836233,0.00021052425,0.003189234,0.00012295645,0.0068361238,0.0028099217,0.00009887646],"about_ca_topic_score_codex":0.8069664,"about_ca_topic_score_gemma":0.9000007,"teacher_disagreement_score":0.0930343,"about_ca_system_score_codex":0.000017943046,"about_ca_system_score_gemma":0.00012983696,"threshold_uncertainty_score":0.99919546},"labels":[],"label_agreement":null},{"id":"W1988326650","doi":"10.1111/bre.12029","title":"Magnetic anomalies associated with salt tectonism, deep structure and regional tectonics in the Maritimes Basin, Atlantic Canada","year":2013,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Lineation; Evaporite; Carboniferous; Salt tectonics; Geochemistry; Orogeny; Paleontology; Unconformity; Permian; Sedimentary rock; Geomorphology; Diapir; Tectonics; Structural basin","score_opus":0.02058359222539793,"score_gpt":0.2291832354767851,"score_spread":0.20859964325138716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988326650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99182326,0.00095459115,0.0000016229097,0.003913832,0.000015052874,0.0002865597,0.00003146536,0.000009392563,0.0029642559],"genre_scores_gemma":[0.99899364,0.00009829323,0.00017826816,0.0004441507,0.000015867889,0.000006204093,0.000101427024,0.0000022505913,0.00015988344],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839425,0.00030039935,0.00013275533,0.00017481128,0.0005738316,0.0004239787],"domain_scores_gemma":[0.99865896,0.0009527635,0.00002603321,0.00013015166,0.00015674069,0.00007532968],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00048347245,0.00009822667,0.000119133605,0.000088344146,0.00034911375,0.00021589789,0.0002640124,0.00006761967,0.0033780055],"category_scores_gemma":[0.00023735143,0.000052550855,0.000009686071,0.0005837135,0.0002605144,0.00014840692,0.000018248711,0.0003616848,0.000015868263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016679853,0.000010780132,0.9891024,0.000028092754,0.0000060516686,0.000024039671,0.00016216456,0.00011164544,0.0000036162303,0.00013597548,0.0025809235,0.007817618],"study_design_scores_gemma":[0.00015501416,0.00018049292,0.99133545,0.000021540998,0.0000023966427,0.000045289555,0.00062431325,0.0020478473,0.0000059465697,0.002116807,0.0033767861,0.00008810416],"about_ca_topic_score_codex":0.65324366,"about_ca_topic_score_gemma":0.8981924,"teacher_disagreement_score":0.24494873,"about_ca_system_score_codex":0.000010516461,"about_ca_system_score_gemma":0.00029384706,"threshold_uncertainty_score":0.997533},"labels":[],"label_agreement":null},{"id":"W1989929516","doi":"10.1111/bre.12047","title":"Exhumation of the Huangling anticline in the Three Gorges region: Cenozoic sedimentary record from the western Jianghan Basin, China","year":2013,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China University of Geosciences; National Natural Science Foundation of China","keywords":"Anticline; Geology; Sedimentary rock; Craton; Paleontology; Basement; Provenance; Geomorphology; Geochemistry; Cenozoic; Structural basin; Tectonics","score_opus":0.0657196628901782,"score_gpt":0.2770129124572045,"score_spread":0.2112932495670263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989929516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9420523,0.00042835425,0.000009888941,0.055461835,0.00006270137,0.00032858312,0.000018492483,0.0000073697597,0.0016304418],"genre_scores_gemma":[0.9985712,0.00009435813,0.00009768786,0.0008580616,0.00017110704,0.000006151074,0.00006119497,0.0000019755191,0.00013822726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977489,0.000716237,0.00026974973,0.00023627418,0.00064842176,0.00038037993],"domain_scores_gemma":[0.9980908,0.0012603999,0.00006972623,0.00043662108,0.000087312466,0.00005513301],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014437268,0.000098663666,0.00015992188,0.00004731679,0.00028674988,0.000085493004,0.000859432,0.000060433045,0.005085536],"category_scores_gemma":[0.00030919258,0.000038834292,0.00009275011,0.00075376173,0.00031461354,0.00012720937,0.000080951926,0.00044447073,0.0001833969],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017924749,0.0000323323,0.97639024,0.0000062809204,0.000011249665,0.0000032022647,0.00027804228,0.000045672663,0.00008346597,0.000013503815,0.002585981,0.020532118],"study_design_scores_gemma":[0.00012317968,0.000053922566,0.9838644,0.000036417146,0.000009348519,0.0000019846248,0.00041735065,0.0030285025,0.00023472804,0.010679734,0.0014933995,0.000057005116],"about_ca_topic_score_codex":0.24061133,"about_ca_topic_score_gemma":0.045555133,"teacher_disagreement_score":0.1950562,"about_ca_system_score_codex":0.0000053961976,"about_ca_system_score_gemma":0.000024702324,"threshold_uncertainty_score":0.995824},"labels":[],"label_agreement":null},{"id":"W1997668118","doi":"10.1111/j.1365-2117.2007.00319.x","title":"Syntectonic subaqueous mass flows of the Neoproterozoic Otavi Group, Namibia: where is the evidence of global glaciation?","year":2007,"lang":"en","type":"article","venue":"Basin Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"De Beers (Canada); The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Diamictite; Facies; Glacial period; Snowball Earth; Paleontology; Geochemistry; Breccia; Craton; Clastic rock; Sedimentology; Geomorphology; Sedimentary rock; Structural basin; Tectonics","score_opus":0.04596357362602526,"score_gpt":0.32825839510724136,"score_spread":0.2822948214812161,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997668118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9669742,0.015253709,0.0001402755,0.0021093136,0.00016927315,0.00048592643,0.00005027651,0.000010436831,0.01480662],"genre_scores_gemma":[0.9993932,0.00017322232,0.0003042246,0.000034352273,0.00004505461,0.0000022991362,7.224557e-7,7.823417e-7,0.000046104662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997331,0.0006374976,0.00033711566,0.0002528061,0.0009418652,0.0004996931],"domain_scores_gemma":[0.9978271,0.0012585405,0.00012160267,0.0005180109,0.00019712336,0.00007762439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0040032975,0.00010886511,0.00018258132,0.000055514076,0.0003827103,0.000034222965,0.0009136136,0.00014342341,0.0002879542],"category_scores_gemma":[0.00039209903,0.000061326,0.00013798641,0.0009719616,0.00069927954,0.00015177912,0.000009042592,0.0004376736,0.00001607881],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017672691,0.000018583509,0.93494225,0.00005877514,0.000026721555,0.000010097492,0.00017033234,0.00001227281,0.0006182526,0.00029575123,0.00023677248,0.06343348],"study_design_scores_gemma":[0.00012234054,0.00020433747,0.9958914,0.00014015652,0.000009197884,0.000016542232,0.00023120221,0.0005333222,0.0009033167,0.0017802897,0.0001051028,0.000062775645],"about_ca_topic_score_codex":0.009120049,"about_ca_topic_score_gemma":0.08951938,"teacher_disagreement_score":0.080399334,"about_ca_system_score_codex":0.000012753825,"about_ca_system_score_gemma":0.00019456496,"threshold_uncertainty_score":0.9974783},"labels":[],"label_agreement":null},{"id":"W2007728421","doi":"10.1111/j.1365-2117.2005.00274.x","title":"Dynamic modelling of passive margin salt tectonics: effects of water loading, sediment properties and sedimentation patterns","year":2005,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Salt tectonics; Sedimentary rock; Pore water pressure; Petrology; Geomorphology; Continental margin; Diapir; Growth fault; Geotechnical engineering; Tectonics; Structural basin; Geochemistry; Seismology","score_opus":0.048138193380781916,"score_gpt":0.2742931349748198,"score_spread":0.22615494159403787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007728421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973938,0.0007848172,0.00082582585,0.00041423034,0.000024291281,0.00025256033,0.000014200383,0.000007295401,0.00028302058],"genre_scores_gemma":[0.9984794,0.00032979593,0.0010057102,0.000019816413,0.000010828629,0.000004883371,0.000031196058,0.0000017856242,0.00011656569],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99904126,0.00010087836,0.00017814874,0.0001237442,0.0003264237,0.0002295391],"domain_scores_gemma":[0.9995714,0.00014627464,0.00003333651,0.00007799674,0.00012176327,0.00004922891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041993964,0.00006314437,0.00011148895,0.00012525596,0.00010100226,0.000024548788,0.00009351622,0.000041844105,0.00044073927],"category_scores_gemma":[0.000024715366,0.00003723044,0.000017850722,0.00010095337,0.00010582521,0.00017489247,0.00002200284,0.00011089166,0.000028628278],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005456736,0.00037008323,0.40055007,0.0066254805,0.00015167255,0.000015128808,0.013263102,0.24684636,0.029134665,0.0002508192,0.00023797821,0.302009],"study_design_scores_gemma":[0.0006235421,0.00079990015,0.08300795,0.00030502147,0.000015828413,0.000006053101,0.0008355287,0.5242255,0.38839006,0.00093676284,0.00068165374,0.00017224392],"about_ca_topic_score_codex":0.0011940368,"about_ca_topic_score_gemma":0.00019268985,"teacher_disagreement_score":0.3592554,"about_ca_system_score_codex":0.00000598637,"about_ca_system_score_gemma":0.0000244171,"threshold_uncertainty_score":0.4825786},"labels":[],"label_agreement":null},{"id":"W2013292490","doi":"10.1111/bre.12053","title":"Deep‐water continental margins: geological and economic frontiers","year":2014,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Geological Society of London","keywords":"Geology; Continental margin; Tectonics; Magmatism; Paleontology; Rift; Drilling; Earth science","score_opus":0.03174339153715655,"score_gpt":0.2528566931759327,"score_spread":0.22111330163877613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013292490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9750623,0.00031552828,0.000053872187,0.0032016775,0.00011638764,0.00010742977,0.000006010963,0.000019948358,0.02111683],"genre_scores_gemma":[0.9974485,0.00008916317,0.00041306016,0.00018417188,0.00016402696,0.0000025043626,0.000020884097,0.0000013342953,0.0016763777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986661,0.00023175868,0.0001084583,0.0002865127,0.00018658322,0.00052055926],"domain_scores_gemma":[0.9994669,0.00025571705,0.000009449981,0.00009516854,0.000025276537,0.00014749376],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00069079257,0.000088541114,0.00017684672,0.00004381556,0.00029468312,0.00006307868,0.00015965864,0.00006129088,0.0029204662],"category_scores_gemma":[0.00008788833,0.000048059494,0.000034866036,0.00004608884,0.0005347481,0.000064862084,0.00008034863,0.000205415,0.0034639682],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006573328,0.000016540562,0.94555753,0.0000069207213,0.0000125156475,0.000007678611,0.000051938026,0.0000930013,0.000010290103,0.0006236185,0.0029555208,0.050598685],"study_design_scores_gemma":[0.00020173326,0.00023042648,0.9164096,0.0000018613972,0.000001941297,0.0000030217518,0.00010111528,0.009263062,0.000042720105,0.009862453,0.06379702,0.0000850334],"about_ca_topic_score_codex":0.002831081,"about_ca_topic_score_gemma":0.00093585264,"teacher_disagreement_score":0.0608415,"about_ca_system_score_codex":0.0000034372788,"about_ca_system_score_gemma":0.000004921793,"threshold_uncertainty_score":0.997991},"labels":[],"label_agreement":null},{"id":"W2016925797","doi":"10.1111/bre.12120","title":"Collapse‐induced fluidization structures in the <scp>L</scp>ower <scp>C</scp>retaceous <scp>A</scp>thabasca <scp>O</scp>il <scp>S</scp>ands <scp>D</scp>eposit, <scp>W</scp>estern <scp>C</scp>anada","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Chevron (Canada)","funders":"","keywords":"Geology; Aquifer; Devonian; Trough (economics); Fluidization; Petrology; Cretaceous; Geomorphology; Geochemistry; Geotechnical engineering; Groundwater; Paleontology","score_opus":0.05966106355791461,"score_gpt":0.293393466702117,"score_spread":0.2337324031442024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016925797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8653653,0.017729409,0.0005446185,0.0006497596,0.0038190135,0.006713993,0.002853171,0.0013514681,0.100973256],"genre_scores_gemma":[0.92421764,0.0056592845,0.0019452109,0.0028973455,0.0034177755,0.0008606525,0.0052312445,0.0006641605,0.055106666],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.95455,0.007545026,0.006129411,0.0067155315,0.012974006,0.012085978],"domain_scores_gemma":[0.9109541,0.069770396,0.0030038243,0.0056628566,0.0051645897,0.0054442286],"candidate_categories":["metaresearch","metaepi_narrow","sts","scholarly_communication","open_science","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","research_integrity"],"category_scores_codex":[0.014800957,0.0052689444,0.0050529917,0.0050996337,0.006206692,0.0073102736,0.010871596,0.0048020217,0.00028078567],"category_scores_gemma":[0.097503304,0.0044237827,0.001877301,0.014823281,0.0034206873,0.0056090825,0.002424206,0.008853255,0.0048245196],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050909348,0.0022250465,0.20241967,0.00194942,0.001378821,0.0023317602,0.041140184,0.010262226,0.0034790235,0.002261009,0.7277244,0.0047775856],"study_design_scores_gemma":[0.0071694227,0.0042361333,0.13459164,0.00079155696,0.0006997558,0.0016161816,0.08402897,0.010125194,0.020677477,0.009755606,0.72581816,0.00048990303],"about_ca_topic_score_codex":0.010628387,"about_ca_topic_score_gemma":0.013364242,"teacher_disagreement_score":0.082702346,"about_ca_system_score_codex":0.00090138137,"about_ca_system_score_gemma":0.00529132,"threshold_uncertainty_score":0.9992914},"labels":[],"label_agreement":null},{"id":"W2032212014","doi":"10.1111/bre.12126","title":"The Hesperides basin: a continental‐scale upper Palaeozoic to Triassic basin in southern Gondwana","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Petrobras; Dalhousie University","keywords":"Geology; Gondwana; Paleontology; Paleozoic; Structural basin; Sedimentary rock; Foreland basin; Sedimentary basin; Permian","score_opus":0.07161468179155699,"score_gpt":0.30331537373758055,"score_spread":0.23170069194602355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032212014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9639037,0.0006674682,0.000008430391,0.022483883,0.00009149719,0.00032229722,0.00006487293,0.000028399232,0.012429452],"genre_scores_gemma":[0.9921036,0.000038196627,0.00025165442,0.00059495337,0.00015898552,0.000014166318,0.00004074952,0.00000513963,0.0067925802],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9963552,0.0008164596,0.0003656035,0.00049206434,0.0010049732,0.00096574315],"domain_scores_gemma":[0.99769235,0.0010990719,0.00003687743,0.00039737762,0.00021134994,0.00056294736],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0038161657,0.00017799,0.00032867404,0.00020626571,0.0003137616,0.00022713064,0.00069253193,0.00010593682,0.004764998],"category_scores_gemma":[0.0014051069,0.00009976241,0.00014115479,0.0014783378,0.00038867435,0.00009036613,0.00010831834,0.00048820555,0.00447535],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003841578,0.000067866706,0.9556537,0.000005746883,0.000015635174,0.000034176177,0.0006292129,0.00007844732,0.00015115607,0.000033461856,0.009912372,0.03303403],"study_design_scores_gemma":[0.0009927865,0.000377701,0.8214559,0.000036374386,0.000011848774,0.000010165393,0.008112056,0.002804566,0.00067904143,0.010068636,0.15512523,0.00032573214],"about_ca_topic_score_codex":0.0365815,"about_ca_topic_score_gemma":0.045177165,"teacher_disagreement_score":0.14521286,"about_ca_system_score_codex":0.000022485061,"about_ca_system_score_gemma":0.00012303077,"threshold_uncertainty_score":0.9962998},"labels":[],"label_agreement":null},{"id":"W2038410447","doi":"10.1111/bre.12037","title":"Exposed evaporite diapirs and minibasins above a canopy in central Sverdrup Basin, Axel Heiberg Island, Arctic Canada","year":2013,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Diapir; Evaporite; Paleontology; Anticline; Anhydrite; Carboniferous; Paleogene; Unconformity; Geochemistry; Structural basin; Gypsum","score_opus":0.04356109522764386,"score_gpt":0.2512313562203975,"score_spread":0.20767026099275362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038410447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875833,0.00080120994,0.0000033852414,0.0070724804,0.00019810491,0.0004703201,0.00007101961,0.000010386095,0.0037898093],"genre_scores_gemma":[0.9978261,0.0005705965,0.00012592573,0.00043605888,0.00010781573,0.000015501746,0.000077235585,0.0000040500468,0.0008367398],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974213,0.00030805415,0.00025305356,0.00038614846,0.00065709633,0.0009743],"domain_scores_gemma":[0.9988121,0.00051474484,0.000034252036,0.0001763016,0.00014944685,0.000313205],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005734615,0.00015116722,0.00022643938,0.000102046055,0.0003121324,0.00013457394,0.0001909314,0.00008081816,0.0031110337],"category_scores_gemma":[0.0003323227,0.00011479218,0.000026989039,0.00047338073,0.00018255922,0.0002252947,0.000046252684,0.00034634265,0.00013852619],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000069231224,0.000026644033,0.9674398,0.000029615567,0.000010759046,0.000058538517,0.00044505927,0.00008960074,0.000028931454,0.000027723034,0.015214761,0.016559351],"study_design_scores_gemma":[0.00042635883,0.00019161892,0.9715687,0.000023943265,0.0000023636424,0.0000052196892,0.0014819877,0.00224621,0.000031098665,0.00057596504,0.023295807,0.00015072162],"about_ca_topic_score_codex":0.95677406,"about_ca_topic_score_gemma":0.9846131,"teacher_disagreement_score":0.027839055,"about_ca_system_score_codex":0.000060233648,"about_ca_system_score_gemma":0.00030673118,"threshold_uncertainty_score":0.99780023},"labels":[],"label_agreement":null},{"id":"W2038791401","doi":"10.1111/bre.12119","title":"Complex interplay of faulting, glacioeustatic variations and halokinesis during deposition of upper Viséan units over thick salt in the western Cumberland Basin of Atlantic Canada","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Structural basin; Devonian; Paleontology; Orogeny; Canada Basin; Fault (geology); Sedimentary depositional environment; Clastic rock","score_opus":0.0594043541480969,"score_gpt":0.31476925320764426,"score_spread":0.25536489905954735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038791401","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983695,0.000061239174,0.00005664217,0.00042824427,0.000016173519,0.00017872582,0.00007091133,0.0000020779464,0.000816462],"genre_scores_gemma":[0.99965745,0.000018537894,0.00017516688,0.0000365809,0.000008033378,0.0000018094522,0.00006813234,0.0000013617977,0.000032897635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986715,0.00034627056,0.00026913243,0.000090419555,0.00045440104,0.00016830314],"domain_scores_gemma":[0.99880075,0.0006816538,0.00007975148,0.000108898814,0.00027771824,0.00005121336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009267151,0.00005721105,0.00014163932,0.00012677617,0.000077585224,0.000022984055,0.00016262817,0.000034075158,0.00011831633],"category_scores_gemma":[0.00040342635,0.000036889494,0.000010336363,0.000547556,0.00011402462,0.0001180563,0.000023307657,0.00012649452,0.0000015447948],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051708324,0.000019011057,0.9974562,0.00019552546,0.0000058956352,0.0000026462535,0.0014071506,0.0002774429,0.000052171592,0.00007476667,0.00015083083,0.00030664384],"study_design_scores_gemma":[0.00026852582,0.0000993186,0.99301636,0.00007888624,0.0000050826425,0.000012515628,0.0010717063,0.004976802,0.00014304259,0.00015874367,0.00012833533,0.00004065089],"about_ca_topic_score_codex":0.7218743,"about_ca_topic_score_gemma":0.6668353,"teacher_disagreement_score":0.05503899,"about_ca_system_score_codex":0.000006619431,"about_ca_system_score_gemma":0.0002256723,"threshold_uncertainty_score":0.33924407},"labels":[],"label_agreement":null},{"id":"W2039945588","doi":"10.1111/j.1365-2117.2009.00457.x","title":"Role of the bedrock topography in the Quaternary filling of a giant estuarine basin: the Lower St. Lawrence Estuary, Eastern Canada","year":2010,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies; Louisiana-Pacific (Canada); Université du Québec à Rimouski; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bedrock; Quaternary; Sedimentary rock; Geomorphology; Paleontology; Structural basin; Bathymetry; Geochemistry; Oceanography","score_opus":0.02747459264958465,"score_gpt":0.262069277943408,"score_spread":0.23459468529382335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039945588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99117976,0.00025202232,0.000003217714,0.0034239322,0.00010001263,0.00022243697,0.000045014658,0.0000026104099,0.0047709905],"genre_scores_gemma":[0.99959385,0.000036901834,0.00007279842,0.00014379254,0.000030369345,0.000004070299,0.000008346731,0.0000014091532,0.00010848263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99836314,0.00027322286,0.00022588976,0.00012897939,0.000719089,0.0002896652],"domain_scores_gemma":[0.9985867,0.0008149693,0.00006158257,0.00035965198,0.00013657972,0.0000404919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014139658,0.00007574034,0.00010956152,0.000060781655,0.00024483496,0.000041118437,0.001005753,0.000043248645,0.00073189125],"category_scores_gemma":[0.00020632443,0.00003130826,0.00004437595,0.00075997075,0.00032439892,0.000085428444,0.00006325055,0.0005130349,0.0000072741227],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032985532,0.00004635208,0.98683715,0.000027146925,0.000005667137,0.0000041882604,0.00050920225,0.00034775844,0.000094566116,0.00024857014,0.00047557426,0.011370813],"study_design_scores_gemma":[0.00007421935,0.00011397192,0.98244256,0.000026353,0.0000024411322,0.000007655694,0.0014168348,0.004999557,0.00028031704,0.0017335808,0.008853586,0.000048931448],"about_ca_topic_score_codex":0.723367,"about_ca_topic_score_gemma":0.85306185,"teacher_disagreement_score":0.12969491,"about_ca_system_score_codex":0.0000018041596,"about_ca_system_score_gemma":0.00024829124,"threshold_uncertainty_score":0.8013696},"labels":[],"label_agreement":null},{"id":"W2040200892","doi":"10.1111/j.1365-2117.2012.00553.x","title":"A three‐dimensional stratigraphic model for the Messinian crisis in the Pannonian Basin, eastern Hungary","year":2012,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Formations and Processes Exploration","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Unconformity; Structural basin; Facies; Tectonics; Inversion (geology); Paleontology; Neogene; Sedimentary basin analysis; Back-stripping; Late Miocene; Sedimentary basin; Geomorphology","score_opus":0.18456962963278886,"score_gpt":0.3493629999930702,"score_spread":0.16479337036028133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040200892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9339002,0.003118105,0.015583956,0.041198622,0.00021585103,0.0016683893,0.00017141968,0.00003490904,0.0041085924],"genre_scores_gemma":[0.99758756,0.000039072103,0.0013304412,0.0007286633,0.00011290783,0.000046505724,0.00007767505,0.0000024714398,0.000074689415],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9982655,0.0002488612,0.00020113718,0.00015483558,0.0006088142,0.0005208248],"domain_scores_gemma":[0.9985219,0.0009774271,0.000033652184,0.00024405673,0.00013998995,0.000082967235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0039173304,0.00009341384,0.0000939858,0.00012525296,0.00070394576,0.00016782379,0.0004123864,0.00007487433,0.00036848572],"category_scores_gemma":[0.000117781856,0.000045272107,0.00005234806,0.00059246103,0.0001387974,0.0005041281,0.000017676604,0.00033696662,0.00012005898],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031941856,0.00025571484,0.8348144,0.00009725558,0.000032132626,0.0000041105905,0.007489603,0.023934986,0.000010096081,0.006211417,0.020112095,0.10671875],"study_design_scores_gemma":[0.00013566237,0.00008300178,0.4270433,0.000008261582,0.000004793701,0.000004801338,0.0013986999,0.5584345,0.0000040471923,0.009268065,0.0035451713,0.000069715454],"about_ca_topic_score_codex":0.0016796249,"about_ca_topic_score_gemma":0.009318757,"teacher_disagreement_score":0.5344995,"about_ca_system_score_codex":0.0000031261595,"about_ca_system_score_gemma":0.00009948765,"threshold_uncertainty_score":0.5414253},"labels":[],"label_agreement":null},{"id":"W2047926936","doi":"10.1046/j.1365-2117.2001.00146.x","title":"Drainage patterns and tectonic forcing: a model study for the Swiss Alps","year":2001,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Dalhousie University; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Tectonics; Forcing (mathematics); Geomorphology; Tectonic uplift; Massif; Drainage; Paleontology; Climatology","score_opus":0.14409560307987748,"score_gpt":0.35996081708536304,"score_spread":0.21586521400548556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047926936","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98886216,0.00040924893,0.0030339744,0.0023981605,0.000022690725,0.0007552871,0.00003164005,0.000018113366,0.0044687414],"genre_scores_gemma":[0.998625,0.00012021824,0.00016363384,0.00008407482,0.000032619486,0.000024880384,0.000010699094,0.0000018363138,0.0009370354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990412,0.000077912206,0.00010492598,0.00016188671,0.00027278883,0.00034131395],"domain_scores_gemma":[0.99886864,0.0007984864,0.0000147510245,0.0001543075,0.00009691979,0.00006688655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014204062,0.000062140905,0.00007667148,0.00006833903,0.00066756253,0.0001456064,0.00023321695,0.000031520336,0.00041049474],"category_scores_gemma":[0.00017942967,0.000033714245,0.00002080926,0.0002464468,0.00007932043,0.00012636057,0.000030604613,0.0001603554,0.0000280223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111875575,0.00007468543,0.89434004,0.000048323058,0.000017485789,0.0000085484235,0.0011773106,0.004699468,0.000003398391,0.0005459997,0.0005955046,0.09837738],"study_design_scores_gemma":[0.00030858762,0.00047367153,0.70135784,0.0000066647376,0.000006102517,0.000010562373,0.0027875702,0.28062594,0.000008668663,0.010223314,0.004116634,0.000074415766],"about_ca_topic_score_codex":0.002080588,"about_ca_topic_score_gemma":0.004927384,"teacher_disagreement_score":0.27592647,"about_ca_system_score_codex":0.0000020790744,"about_ca_system_score_gemma":0.00003862242,"threshold_uncertainty_score":0.5134419},"labels":[],"label_agreement":null},{"id":"W2064362397","doi":"10.1046/j.1365-2117.2002.00163.x","title":"Cooling of the Sverdrup Basin during Tertiary basin inversion: implications for hydrocarbon exploration","year":2002,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Geology; Fission track dating; Anticline; Paleogene; Paleontology; Orogeny; Outcrop; Cretaceous; Thrust fault; Structural basin; Fault (geology); Zircon","score_opus":0.14072495957356404,"score_gpt":0.29835644074017653,"score_spread":0.1576314811666125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064362397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9744664,0.00039998718,0.00027221497,0.021203838,0.00014447398,0.0006866659,0.00004715791,0.000026495381,0.002752755],"genre_scores_gemma":[0.9987495,0.00028432813,0.0002899588,0.00014814075,0.00012344126,0.000025274216,0.000031865402,0.000003596417,0.00034387223],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985804,0.00022349182,0.00023490968,0.00025142884,0.00034709205,0.00036268082],"domain_scores_gemma":[0.9990343,0.0003983154,0.000063964384,0.00026243785,0.000167404,0.00007357749],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000673187,0.00008956886,0.00013200221,0.00008446676,0.00084716774,0.000046184803,0.0002798761,0.00007175594,0.00044164117],"category_scores_gemma":[0.0003528697,0.000060190658,0.000079786,0.0005379019,0.00016636655,0.0002558247,0.00005700573,0.00017490753,0.00006429518],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023274169,0.00013651224,0.9338475,0.00015369128,0.00004049893,0.0000020405457,0.0013839796,0.00287736,0.0026711314,0.0006685679,0.017036002,0.040949985],"study_design_scores_gemma":[0.00035791151,0.00015016769,0.9599012,0.0000398038,0.000009262801,0.000002302328,0.00057817844,0.026298134,0.002284624,0.0021520208,0.008112822,0.00011358293],"about_ca_topic_score_codex":0.0013659237,"about_ca_topic_score_gemma":0.0006443621,"teacher_disagreement_score":0.0408364,"about_ca_system_score_codex":0.000015331843,"about_ca_system_score_gemma":0.000019342686,"threshold_uncertainty_score":0.6515815},"labels":[],"label_agreement":null},{"id":"W2082927476","doi":"10.1111/bre.12131","title":"Quantifying the influence of sill intrusion on the thermal evolution of organic‐rich sedimentary rocks in nonvolcanic passive margins: an example from <scp>ODP</scp> 210‐1276, offshore Newfoundland, Canada","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Engineering and Physical Sciences Research Council; Shell","keywords":"Sill; Geology; Magmatism; Sedimentary rock; Submarine pipeline; Sedimentary basin; Maturity (psychological); Geochemistry; Structural basin; Igneous rock; Petrology; Paleontology; Tectonics; Oceanography; Law","score_opus":0.06710515247278126,"score_gpt":0.26458100313842847,"score_spread":0.1974758506656472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082927476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976288,0.00032026457,0.000004563226,0.0011520167,0.00004288234,0.00023314104,0.00006385225,0.0000054458287,0.00054900727],"genre_scores_gemma":[0.9995104,0.00002977072,0.000027129527,0.00020428716,0.00006363806,0.0000038948983,0.00011157217,0.0000032026096,0.000046107336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99699616,0.0007469417,0.0003353895,0.00033464294,0.0011419005,0.00044496713],"domain_scores_gemma":[0.9967751,0.0022480001,0.000115561554,0.00040471912,0.0002958024,0.00016079866],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013703953,0.00013716955,0.0002471739,0.00009862251,0.00019045762,0.000029806852,0.0007140253,0.00008639406,0.000983038],"category_scores_gemma":[0.0006913981,0.000069747475,0.000041539213,0.001051804,0.0002536386,0.00012441083,0.00011419026,0.00050227286,0.000025231771],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007704484,0.000054066677,0.98774624,0.0000072944977,0.000024229868,0.000011105489,0.0007157357,0.006577798,0.0031437546,0.000033107597,0.00066501636,0.0009446066],"study_design_scores_gemma":[0.00025438616,0.00020987763,0.9835172,0.000032974403,0.000011696546,0.0000010123789,0.005928983,0.0058140084,0.0019908545,0.00171392,0.00047321361,0.000051848856],"about_ca_topic_score_codex":0.98086226,"about_ca_topic_score_gemma":0.97395766,"teacher_disagreement_score":0.0069045704,"about_ca_system_score_codex":0.00007585107,"about_ca_system_score_gemma":0.00050502684,"threshold_uncertainty_score":0.9999302},"labels":[],"label_agreement":null},{"id":"W2088892005","doi":"10.1111/bre.12075","title":"Deep vs. shallow controlling factors of the crustal thermal field – insights from 3D modelling of the<scp>B</scp>eaufort‐<scp>M</scp>ackenzie<scp>B</scp>asin (<scp>A</scp>rctic<scp>C</scp>anada)","year":2014,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Geology; Crust; Thermal conductivity; Lithosphere; Sedimentary rock; Continental crust; Structural basin; Petrology; Thermal; Geochemistry; Geophysics; Geomorphology; Paleontology; Tectonics; Thermodynamics","score_opus":0.05656446862733528,"score_gpt":0.2475723213863489,"score_spread":0.19100785275901364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088892005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9635172,0.0036569568,0.0033489421,0.00039936908,0.0011784015,0.001718216,0.00028173224,0.00013039267,0.025768783],"genre_scores_gemma":[0.99362415,0.0011831147,0.00075315114,0.00061542174,0.00078461395,0.00004982707,0.00020975851,0.00007245311,0.0027074798],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9874432,0.0022206425,0.0017416622,0.0016842135,0.00411406,0.0027961992],"domain_scores_gemma":[0.96203524,0.033643354,0.0009426354,0.0015797637,0.0010213334,0.00077767204],"candidate_categories":["metaresearch","metaepi_narrow","sts","research_integrity"],"consensus_categories":[],"category_scores_codex":[0.0029211335,0.0010810845,0.0016338436,0.00044757378,0.0023978583,0.00054397254,0.0027971629,0.0010217212,0.00012236525],"category_scores_gemma":[0.019539729,0.00069741625,0.0008365062,0.0018974199,0.0013167291,0.0008608202,0.0007281858,0.0024908185,0.00020750456],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000100543715,0.00096726464,0.64627635,0.00051464466,0.0011334671,0.00009775955,0.026503084,0.2849906,0.005261973,0.0022466644,0.025097266,0.0068103806],"study_design_scores_gemma":[0.0036783589,0.0020754868,0.356136,0.0005212364,0.00033664482,0.000017311795,0.039742973,0.4442162,0.029830549,0.011035124,0.11214876,0.00026138537],"about_ca_topic_score_codex":0.018544516,"about_ca_topic_score_gemma":0.012351568,"teacher_disagreement_score":0.29014036,"about_ca_system_score_codex":0.00008808618,"about_ca_system_score_gemma":0.00045578557,"threshold_uncertainty_score":0.99981046},"labels":[],"label_agreement":null},{"id":"W2100918471","doi":"10.1111/bre.12117","title":"Sequence hierarchy in a Mesoproterozoic interior sag basin: from basin fill to reservoir scale, the Tombador Formation, Chapada Diamantina Basin, Brazil","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Unconformity; Geology; Paleontology; Sedimentary depositional environment; Fluvial; Alluvium; Facies; Alluvial fan; Sequence stratigraphy; Sequence (biology); Structural basin; Sedimentary rock","score_opus":0.10959792285260703,"score_gpt":0.3376592210563597,"score_spread":0.22806129820375268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100918471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96761054,0.00045526703,0.0002350752,0.022974543,0.00020302461,0.0010611764,0.00038753764,0.000063587075,0.0070092375],"genre_scores_gemma":[0.99412286,0.000096907555,0.0025247892,0.0017522036,0.00016460198,0.00007035127,0.00025648565,0.000010148726,0.0010016627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9952027,0.0011558325,0.00063718733,0.0005604094,0.001378772,0.0010650618],"domain_scores_gemma":[0.9970329,0.0010414757,0.00009952299,0.000689342,0.0006147037,0.00052209763],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.004598679,0.00027098492,0.00037537198,0.0005103395,0.00057542586,0.0005379146,0.001395894,0.00017089296,0.0028653399],"category_scores_gemma":[0.0019497402,0.00017579056,0.00008135577,0.002309973,0.00042398914,0.0012266745,0.00025026864,0.0007914248,0.0019597532],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014868435,0.00020680971,0.7222339,0.000268241,0.000038673737,0.00018052742,0.020535387,0.0010115566,0.00023563055,0.00034399275,0.08750328,0.1659552],"study_design_scores_gemma":[0.000792353,0.00067561754,0.81782305,0.00027021606,0.000006782124,0.000037556503,0.0047597187,0.007514231,0.0014676641,0.0077613876,0.15845966,0.00043173577],"about_ca_topic_score_codex":0.030726539,"about_ca_topic_score_gemma":0.024130251,"teacher_disagreement_score":0.16552345,"about_ca_system_score_codex":0.000056495257,"about_ca_system_score_gemma":0.0003471415,"threshold_uncertainty_score":0.9988173},"labels":[],"label_agreement":null},{"id":"W2109716983","doi":"10.1111/j.1365-2117.2011.00531.x","title":"Compressional salt tectonics and synkinematic strata of the western <scp>K</scp>uqa foreland basin, southern <scp>T</scp>ian <scp>S</scp>han, <scp>C</scp>hina","year":2012,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"PetroChina Company Limited","keywords":"Diapir; Geology; Foreland basin; Salt tectonics; Structural basin; Sedimentary depositional environment; Geochemistry; Tectonics; Canada Basin; Anticline; Paleontology; Geomorphology","score_opus":0.05249547323962228,"score_gpt":0.29254056563635006,"score_spread":0.24004509239672778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109716983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9517736,0.015245879,0.000060562008,0.0003202395,0.0006200378,0.0014219087,0.0010148784,0.00013386563,0.029409025],"genre_scores_gemma":[0.9803686,0.0011103915,0.000488231,0.00028019844,0.00059642555,0.00004195266,0.0001793527,0.00007679304,0.01685806],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99008095,0.0014649815,0.0011709023,0.0011713564,0.0031643098,0.0029475205],"domain_scores_gemma":[0.9788838,0.017677732,0.0005325024,0.001491062,0.00047986527,0.00093500834],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004513742,0.0008686539,0.0012135452,0.00057447405,0.0016636271,0.0005039394,0.001849618,0.0005738799,0.00016860702],"category_scores_gemma":[0.0080857575,0.0006027326,0.0003838093,0.0014483343,0.0016052622,0.00068526703,0.00070903735,0.0019873485,0.0009059731],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011353012,0.00032649,0.9413643,0.00064346107,0.00034788292,0.000055042743,0.009258893,0.000109103625,0.00030471903,0.00022934031,0.04276418,0.004585254],"study_design_scores_gemma":[0.0016482556,0.00057650916,0.87719566,0.00068552454,0.00014386818,0.000182703,0.018329019,0.001660545,0.0018265453,0.0013479957,0.09628317,0.000120210825],"about_ca_topic_score_codex":0.0026395926,"about_ca_topic_score_gemma":0.0041819494,"teacher_disagreement_score":0.06416862,"about_ca_system_score_codex":0.00004145051,"about_ca_system_score_gemma":0.00056087284,"threshold_uncertainty_score":0.9998719},"labels":[],"label_agreement":null},{"id":"W2119205759","doi":"10.1111/j.1365-2117.2004.00229.x","title":"Salt tectonics driven by differential sediment loading: stability analysis and finite‐element experiments","year":2004,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Overburden; Diapir; Salt tectonics; Sedimentary rock; Sedimentary basin; Evaporite; Geotechnical engineering; Tectonics; Deformation (meteorology); Petrology; Structural basin; Geomorphology; Seismology; Geochemistry","score_opus":0.06585529109196885,"score_gpt":0.3263706316192474,"score_spread":0.26051534052727854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119205759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995545,0.00042564416,0.0016815088,0.0005879413,0.00003536667,0.00021704193,0.00013687802,0.000020596282,0.0013499702],"genre_scores_gemma":[0.99872416,0.00015853567,0.00073678565,0.000041016996,0.000017013714,0.000006817338,0.00025201045,0.0000015307364,0.000062135885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983778,0.00014128536,0.00020444495,0.00028221754,0.0005883488,0.0004058767],"domain_scores_gemma":[0.99928963,0.00021722796,0.00003102795,0.00018024835,0.000098467855,0.00018339],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005826379,0.00009864426,0.00015916322,0.00016300094,0.00037548796,0.00014181495,0.00018940581,0.0000588357,0.007284381],"category_scores_gemma":[0.000101545724,0.000072131385,0.00004581372,0.0007189891,0.0001682298,0.00013208756,0.000051941424,0.00019479476,0.000091925875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008949756,0.00025424513,0.98429525,0.0000562241,0.00018344761,0.0000057424218,0.0008503154,0.0023553097,0.00073647825,0.00016204546,0.00042538202,0.010586087],"study_design_scores_gemma":[0.0011516417,0.0008931387,0.9421913,0.00001970449,0.000080459846,0.000001984451,0.0011436159,0.014241981,0.030046556,0.002738556,0.007137687,0.0003533818],"about_ca_topic_score_codex":0.002982643,"about_ca_topic_score_gemma":0.0008393041,"teacher_disagreement_score":0.04210393,"about_ca_system_score_codex":0.000018964027,"about_ca_system_score_gemma":0.000059739185,"threshold_uncertainty_score":0.9936231},"labels":[],"label_agreement":null},{"id":"W2121369179","doi":"10.1111/j.1365-2117.2004.00228.x","title":"Multiscale structure in sedimentary basins","year":2004,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Scale (ratio); Geology; Scale space; A priori and a posteriori; Geologic map; Context (archaeology); Outcrop; Computer science; Artificial intelligence; Paleontology; Cartography; Image processing; Geography; Image (mathematics)","score_opus":0.06357895217191296,"score_gpt":0.32180281908887926,"score_spread":0.2582238669169663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121369179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99318165,0.00029742223,0.000075763426,0.0035168254,0.000058695587,0.000091888425,0.00008207027,0.000019353098,0.0026763356],"genre_scores_gemma":[0.99714726,0.00004379047,0.0021441386,0.00023060205,0.00008257656,6.6184737e-7,0.000086855085,0.0000018331307,0.0002622982],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984836,0.00016710078,0.00014064439,0.00027776018,0.00047984344,0.00045107753],"domain_scores_gemma":[0.9995368,0.000111774796,0.000011568698,0.00016810799,0.000046002355,0.00012570564],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00062944763,0.00007514614,0.00012169535,0.00021877368,0.00015536098,0.000043019496,0.00023106819,0.000078366356,0.0039078463],"category_scores_gemma":[0.00009817639,0.00005506129,0.00003975753,0.0006383907,0.00010755822,0.00008262289,0.000020472984,0.0004090195,0.00044953343],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031390955,0.000048671503,0.84364927,0.000009099985,0.0000081022,0.0001012524,0.00018016886,0.1190016,0.00010839091,0.000055109238,0.00046223027,0.036344696],"study_design_scores_gemma":[0.00048644023,0.00010798641,0.9716724,0.000022893655,0.0000027730293,0.000006234712,0.0002613034,0.014601929,0.00029298745,0.008070992,0.004360134,0.0001139163],"about_ca_topic_score_codex":0.030313132,"about_ca_topic_score_gemma":0.040040717,"teacher_disagreement_score":0.12802312,"about_ca_system_score_codex":0.000012643129,"about_ca_system_score_gemma":0.00005859532,"threshold_uncertainty_score":0.9970027},"labels":[],"label_agreement":null},{"id":"W2122208601","doi":"10.1111/j.1365-2117.2004.00234.x","title":"The Marinoan glaciation (Neoproterozoic) in northeast Svalbard","year":2004,"lang":"en","type":"article","venue":"Basin Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":182,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Diamictite; Dolostone; Geology; Snowball Earth; Grainstone; Paleontology; Siliciclastic; Glacial period; Unconformity; Sedimentary rock; Carbonate rock; Clastic rock; Facies","score_opus":0.049487738295577156,"score_gpt":0.3097050969580171,"score_spread":0.26021735866243995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122208601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.83533835,0.0012298282,0.000017164826,0.002977117,0.000108869244,0.00026684298,0.000007739601,0.000015616997,0.16003847],"genre_scores_gemma":[0.99953,0.00010245682,0.0001657202,0.00002150486,0.000059432514,0.000005988059,0.000005001952,5.226073e-7,0.000109355446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838656,0.0003112728,0.00016079529,0.00019881569,0.0004447999,0.000497767],"domain_scores_gemma":[0.9993184,0.00031148279,0.00002329214,0.00020663014,0.000055389668,0.00008478816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001897307,0.00007045004,0.00008502697,0.00013829491,0.00056348304,0.00009741574,0.000315697,0.00007902227,0.000077340206],"category_scores_gemma":[0.00014848186,0.000047282378,0.00003707608,0.00045538033,0.00030130165,0.00013453086,0.0000024342896,0.0004185752,0.00011638137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006565148,0.000011717846,0.71885866,0.0000032723178,0.0000036271647,0.000022710206,0.000138135,0.000045770288,0.000006952714,0.00074148073,0.000043218293,0.28005877],"study_design_scores_gemma":[0.00027826618,0.00009834412,0.9889189,0.000011606892,7.1473124e-7,0.000008407785,0.0001651806,0.0001107079,0.00004967667,0.0092419805,0.0010589765,0.000057238216],"about_ca_topic_score_codex":0.011497961,"about_ca_topic_score_gemma":0.18807231,"teacher_disagreement_score":0.28000155,"about_ca_system_score_codex":0.000008476902,"about_ca_system_score_gemma":0.00015073063,"threshold_uncertainty_score":0.9950846},"labels":[],"label_agreement":null},{"id":"W2130950370","doi":"10.1046/j.1365-2117.2002.00182.x","title":"Mid‐Palaeocene palaeogeography of the eastern North Sea basin: integrating geological evidence and 3D geodynamic modelling","year":2002,"lang":"en","type":"article","venue":"Basin Research","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Subaerial; Palaeogeography; Geology; Structural basin; Paleontology; Cretaceous; Lithosphere; Submarine; Geomorphology; Tectonics; Oceanography; Volcanism","score_opus":0.11699473959248918,"score_gpt":0.29462566712619476,"score_spread":0.17763092753370557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130950370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898011,0.00395992,0.00012319392,0.0019066717,0.00010005443,0.0003628837,0.000025115824,0.000021859767,0.0036991888],"genre_scores_gemma":[0.99722844,0.0013118793,0.0008205612,0.00008461162,0.000047812846,0.0000062084882,0.000013843534,0.000004907396,0.0004817482],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9957272,0.0015848951,0.00036284872,0.00054258876,0.00083471683,0.0009477831],"domain_scores_gemma":[0.9963752,0.002574073,0.000084276275,0.00048169255,0.00028462027,0.00020014193],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023642704,0.00019299935,0.00032792962,0.0002964819,0.0007041766,0.00006460908,0.0007828904,0.00023013345,0.0016115208],"category_scores_gemma":[0.0006612334,0.00012334663,0.00010648596,0.0010719644,0.0019136728,0.00020089319,0.00017651843,0.0012284183,0.00022311827],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058107507,0.000038088525,0.99446553,0.00007418682,0.000021677746,0.000035110214,0.00022179823,0.0018996266,0.0000030979456,0.000044823813,0.00007228718,0.003065693],"study_design_scores_gemma":[0.00013694077,0.00013788306,0.64483917,0.00008865176,0.0000067765395,0.00004403104,0.00009189701,0.35412446,0.000016049215,0.00032446868,0.00009834864,0.00009136004],"about_ca_topic_score_codex":0.0030311632,"about_ca_topic_score_gemma":0.0056012142,"teacher_disagreement_score":0.35222483,"about_ca_system_score_codex":0.0000026368336,"about_ca_system_score_gemma":0.000062589235,"threshold_uncertainty_score":0.99930114},"labels":[],"label_agreement":null},{"id":"W2138500572","doi":"10.1111/bre.12123","title":"Continental margin syn‐rift salt tectonics at intermediate width margins","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Killam Trusts; Dalhousie University; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Geology; Rift; Evaporite; Graben; Salt tectonics; Clastic rock; Sedimentary rock; Passive margin; Half-graben; Lithosphere; Petrology; Progradation; Diapir; Salt pan; Geomorphology; Paleontology; Geochemistry; Tectonics; Sedimentary depositional environment","score_opus":0.09646655519021707,"score_gpt":0.32334962319133426,"score_spread":0.22688306800111718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138500572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92203516,0.0025968144,0.0000060177667,0.001225959,0.0004973615,0.00032077593,0.00011696295,0.0000775819,0.07312334],"genre_scores_gemma":[0.9930441,0.00038073488,0.00026403114,0.000155219,0.00023049754,0.000006264062,0.000090899746,0.000010478124,0.0058177784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99684423,0.00036630323,0.0002656931,0.00044353612,0.001113032,0.00096722733],"domain_scores_gemma":[0.99834234,0.00058753183,0.000049384285,0.00038368968,0.00022113825,0.0004158955],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0021324179,0.00018894863,0.0002810429,0.00024606497,0.00037533208,0.00011525752,0.0004618469,0.00010566366,0.004362535],"category_scores_gemma":[0.0005865769,0.00015025689,0.000084436404,0.00054155797,0.00048175934,0.00016420173,0.00018439283,0.00051037164,0.004811037],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028396267,0.000050605857,0.8756638,0.000031825657,0.000056222714,0.00022509124,0.00063304475,0.000023305316,0.00004492934,0.00015196663,0.06069016,0.06214508],"study_design_scores_gemma":[0.0008861492,0.00038840692,0.83908886,0.000039064067,0.0000071506433,0.00004133807,0.00058395584,0.0011653652,0.00039170214,0.0005335585,0.1566559,0.00021857201],"about_ca_topic_score_codex":0.00407768,"about_ca_topic_score_gemma":0.012644073,"teacher_disagreement_score":0.095965736,"about_ca_system_score_codex":0.000043600507,"about_ca_system_score_gemma":0.0002371492,"threshold_uncertainty_score":0.99654764},"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,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Salt tectonics; Evaporite; Geochemistry; Salt dome; Tectonics; Geomorphology; Petrology; Paleontology; Structural basin; Diapir","score_opus":0.03986664291525057,"score_gpt":0.29241558260151834,"score_spread":0.2525489396862678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146075665","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9724864,0.0015769063,0.0006964215,0.005159365,0.00013732079,0.0002858453,0.00005826296,0.000074020245,0.019525507],"genre_scores_gemma":[0.9961371,0.00055302057,0.002306132,0.00042881744,0.00010706818,0.0000040680443,0.00008880713,0.0000037513096,0.00037127058],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99814034,0.000345844,0.00021291293,0.00029426662,0.00053114176,0.00047551058],"domain_scores_gemma":[0.99840033,0.00072668964,0.00003762463,0.00022584318,0.0003908717,0.00021864506],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013450392,0.000113850314,0.00015668488,0.0001741828,0.000676671,0.0001851144,0.00020949406,0.00010763712,0.0015780897],"category_scores_gemma":[0.0008118741,0.000082167026,0.000028563667,0.00053011003,0.00024944736,0.000262213,0.000038379625,0.00033596737,0.00055071246],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014023768,0.00008820584,0.30756643,0.00023504042,0.000022690218,0.000031448224,0.00028129024,0.00039969455,0.0003205017,0.005044659,0.013053802,0.672816],"study_design_scores_gemma":[0.00030932223,0.00039188328,0.85590667,0.00005045174,0.0000064374776,0.000073805,0.00011866858,0.016138546,0.00044450958,0.0145716565,0.111792974,0.00019508149],"about_ca_topic_score_codex":0.001162766,"about_ca_topic_score_gemma":0.0011132156,"teacher_disagreement_score":0.67262095,"about_ca_system_score_codex":0.000004895515,"about_ca_system_score_gemma":0.000074224234,"threshold_uncertainty_score":0.9993346},"labels":[],"label_agreement":null},{"id":"W2155171122","doi":"10.1111/j.1365-2117.2010.00483.x","title":"Diverse products of near‐surface sediment mobilization in an ancient eolianite: outcrop features of the early Jurassic Navajo Sandstone","year":2010,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Sedimentary depositional environment; Outcrop; Sedimentology; Sedimentary rock; Sediment; Sedimentary structures; Geomorphology; Context (archaeology); Paleontology; Geochemistry","score_opus":0.04873196452004646,"score_gpt":0.31232210046750125,"score_spread":0.2635901359474548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155171122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978096,0.00015783116,0.0000019610188,0.0004920262,0.00014071117,0.0003255673,0.00004205318,0.00000634044,0.00102391],"genre_scores_gemma":[0.99918497,0.00001632677,0.00047755646,0.000021876871,0.000017654727,0.0000014457498,0.000022707307,0.000001574168,0.00025589595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863064,0.0001895509,0.00018906844,0.00017128598,0.00057347014,0.00024597463],"domain_scores_gemma":[0.9991141,0.00011989482,0.000062023624,0.00027291945,0.00036879216,0.000062301595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011720408,0.00006572441,0.00010850576,0.000060004295,0.00018609963,0.00004691716,0.00033421136,0.00006688317,0.0006121777],"category_scores_gemma":[0.00031540668,0.000038769565,0.000021023787,0.0009506473,0.0003737056,0.00021466361,0.000042081632,0.0003212212,0.000023548608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057659545,0.000102148195,0.98027635,0.00007029458,0.0000025175464,0.0000010226396,0.0011553775,0.0025606647,0.0054856413,0.00013982659,0.0003263858,0.0098221265],"study_design_scores_gemma":[0.00014264107,0.00017450454,0.9872787,0.000017051496,0.0000019532597,0.0000013922588,0.0004733529,0.0013585852,0.009439609,0.00018443869,0.0008800548,0.000047699745],"about_ca_topic_score_codex":0.0048236083,"about_ca_topic_score_gemma":0.0058313506,"teacher_disagreement_score":0.009774427,"about_ca_system_score_codex":0.0000034345173,"about_ca_system_score_gemma":0.00015441855,"threshold_uncertainty_score":0.7291885},"labels":[],"label_agreement":null},{"id":"W2273165393","doi":"10.1111/bre.12186","title":"Numerical modelling study of mechanisms of mid‐basin salt canopy evolution and their potential applications to the Northwestern Gulf of Mexico","year":2016,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Canada Research Chairs; Government of Canada; International Business Machines Corporation","keywords":"Diapir; Salt tectonics; Geology; Anticline; Structural basin; Tectonics; Seafloor spreading; Paleontology; Geomorphology; Geochemistry; Earth science","score_opus":0.05546091281408478,"score_gpt":0.29466390149693145,"score_spread":0.23920298868284667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2273165393","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.75180185,0.000099785204,0.24691667,0.0004857,0.000015913007,0.00041756927,0.00009417041,0.0000044073154,0.00016395426],"genre_scores_gemma":[0.99910855,0.00003128905,0.0007753431,0.000008764491,0.000015089337,0.000012451483,0.0000067821775,0.0000016860085,0.000040057213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885225,0.00019678344,0.00024727717,0.00014988655,0.0003680922,0.000185688],"domain_scores_gemma":[0.99904954,0.00032999815,0.00006474611,0.00020373856,0.0002840175,0.00006798042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008323226,0.00006191441,0.00014208314,0.00011629622,0.00015294019,0.000012171045,0.0002604299,0.0000366443,0.00015405664],"category_scores_gemma":[0.000032025666,0.00002952992,0.00002377405,0.0004516643,0.00011683726,0.000083262225,0.000036131765,0.00007479095,0.000013470909],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007445875,0.001043684,0.6633236,0.00027196927,0.000118040596,0.0000019991157,0.0055030906,0.17881764,0.00569511,0.003925291,0.00015371444,0.14040127],"study_design_scores_gemma":[0.0014006532,0.004725582,0.8216818,0.00014198644,0.00003840648,0.00001678596,0.011941121,0.075579576,0.025787897,0.05658287,0.001741101,0.00036219755],"about_ca_topic_score_codex":0.009900594,"about_ca_topic_score_gemma":0.0019776898,"teacher_disagreement_score":0.2473067,"about_ca_system_score_codex":0.0000034973943,"about_ca_system_score_gemma":0.000061831335,"threshold_uncertainty_score":0.99669254},"labels":[],"label_agreement":null},{"id":"W2288915326","doi":"10.1111/bre.12192","title":"Comment on Non‐unique stratal geometries: implications for sequence stratigraphic interpretations, by: P.M. Burgess and G.D. Prince,<i>Basin Research</i>(2015) 27, 351–365","year":2016,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Sequence stratigraphy; Aggradation; Paleontology; Stratigraphy; Progradation; Sequence (biology); Sedimentology; Context (archaeology); Unconformity; Structural basin; Facies; Tectonics","score_opus":0.12957001815579403,"score_gpt":0.3997173805888732,"score_spread":0.27014736243307913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2288915326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8041971,0.0012311417,0.0069256923,0.17121099,0.0001450804,0.0027838263,0.004481235,0.00010269048,0.008922289],"genre_scores_gemma":[0.99590707,0.0011467453,0.0011445254,0.00052674435,0.000042658856,0.00011841548,0.00025789344,0.000006326538,0.00084961805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99728763,0.00042447858,0.00036253565,0.0004936228,0.00063821976,0.0007935092],"domain_scores_gemma":[0.99386305,0.004621715,0.00006549713,0.00041922595,0.00070519705,0.000325306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0041019726,0.00016639427,0.00020410588,0.00056417397,0.0010022045,0.00031512362,0.00056473305,0.00013761446,0.0006705564],"category_scores_gemma":[0.001206496,0.00010767987,0.000049206945,0.0012499965,0.00084869296,0.00051369413,0.000059688497,0.0004300092,0.00011872001],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005114059,0.00035435104,0.52356213,0.0003890645,0.00007640435,0.000007019017,0.00062105944,0.000038858114,0.0020773862,0.031407297,0.24351195,0.19744308],"study_design_scores_gemma":[0.001020805,0.0029154015,0.5334937,0.00037966974,0.000010817573,0.000020523215,0.0010953681,0.0006360253,0.003987742,0.06902303,0.3868897,0.0005272216],"about_ca_topic_score_codex":0.001166715,"about_ca_topic_score_gemma":0.000762048,"teacher_disagreement_score":0.19691586,"about_ca_system_score_codex":0.000023470175,"about_ca_system_score_gemma":0.00028172173,"threshold_uncertainty_score":0.7708248},"labels":[],"label_agreement":null},{"id":"W2507357822","doi":"10.1111/bre.12217","title":"Oligocene‐Miocene Great Lakes in the India‐Asia Collision Zone","year":2016,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Fibrous joint; Paleontology; Structural basin; Collision zone; Neogene; Subduction; Facies; Late Miocene; Tectonics","score_opus":0.07126863303156059,"score_gpt":0.31867765558419126,"score_spread":0.24740902255263067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2507357822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9610747,0.00048142366,0.0000463308,0.006067398,0.000048282847,0.00020730226,0.000045465255,0.000015058881,0.032014],"genre_scores_gemma":[0.99794865,0.00050441135,0.00016129678,0.00014121002,0.0000609497,0.000005690601,0.000020761508,0.0000014566949,0.0011555598],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99829984,0.00036878508,0.00017315686,0.00017311156,0.00056062307,0.00042447052],"domain_scores_gemma":[0.9985056,0.0011017701,0.0000224973,0.00019924899,0.000097239375,0.00007367275],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0022083514,0.00007338335,0.000095458294,0.00016698455,0.00027708264,0.00009403966,0.00043634136,0.00007295448,0.0033455365],"category_scores_gemma":[0.000409722,0.000030854666,0.000024067002,0.00083998305,0.00018921825,0.0002244961,0.000022508204,0.00017778513,0.0011840104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006561995,0.00003543853,0.81878537,0.00002007732,0.0000030351748,0.000033883964,0.0002752745,0.000041063584,0.000028894567,0.0009867799,0.0053813164,0.17434324],"study_design_scores_gemma":[0.00021309644,0.00015413489,0.93960625,0.000033153734,9.584156e-7,0.00001374614,0.00030277076,0.00011340182,0.0002967306,0.00287927,0.05632115,0.0000653323],"about_ca_topic_score_codex":0.0011430994,"about_ca_topic_score_gemma":0.0020789993,"teacher_disagreement_score":0.17427792,"about_ca_system_score_codex":0.0000052289074,"about_ca_system_score_gemma":0.00006999415,"threshold_uncertainty_score":0.9995937},"labels":[],"label_agreement":null},{"id":"W2562243282","doi":"10.1111/bre.12232","title":"Geological controls on the present temperature field of the western Sverdrup Basin, Canadian Arctic Archipelago","year":2016,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Department of Science and Technology, Ministry of Science and Technology, India","keywords":"Geology; Structural basin; Paleontology; Archipelago; Sverdrup; Arctic; Anticline; Diapir; Orogeny; Unconformity; Oceanography; Geomorphology; Geochemistry","score_opus":0.06202367340018737,"score_gpt":0.2830428678969877,"score_spread":0.2210191944968003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2562243282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8145783,0.00013946007,0.0000024774286,0.1788401,0.00011995222,0.00039271003,0.000039458027,0.0000061542555,0.005881419],"genre_scores_gemma":[0.99643695,0.00010260656,0.0000065916524,0.0018425194,0.00014480593,0.000009182748,0.000003662054,0.0000016795414,0.0014519781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782205,0.0007144683,0.00015363652,0.00022081545,0.0005626651,0.0005263931],"domain_scores_gemma":[0.99657476,0.0027705345,0.000031403582,0.0003277349,0.0001471969,0.00014839566],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011418998,0.000093320516,0.00013676877,0.00004744049,0.000523851,0.000050489947,0.00051206764,0.00009782413,0.0021038845],"category_scores_gemma":[0.0015337031,0.000031323867,0.000068912974,0.00023897101,0.00036991222,0.000047665475,0.000055751676,0.00037234172,0.00028673335],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001881332,0.000025292986,0.9566163,0.000008804451,0.000021477194,0.000012362118,0.00018367873,0.00006317476,0.0001269248,0.0012834473,0.022179151,0.019291265],"study_design_scores_gemma":[0.00016769007,0.00043572462,0.9532923,0.000041929132,0.000002638584,0.0000025880622,0.00017749591,0.000051212824,0.0003223704,0.0029747798,0.04247309,0.000058164962],"about_ca_topic_score_codex":0.15282659,"about_ca_topic_score_gemma":0.34013668,"teacher_disagreement_score":0.1873101,"about_ca_system_score_codex":0.000014001137,"about_ca_system_score_gemma":0.00010854145,"threshold_uncertainty_score":0.9988083},"labels":[],"label_agreement":null},{"id":"W2585814178","doi":"10.1111/bre.12233","title":"Application of multi‐kinetic apatite fission track and (U‐Th)/He thermochronology to source rock thermal history: a case study from the Mackenzie Plain, NWT, Canada","year":2017,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"Natural Resources Canada; University of Texas at Austin","keywords":"Fission track dating; Thermochronology; Geology; Apatite; Oil shale; Mineralogy; Source rock; Geochemistry; Population; Cretaceous; Fission; Uranium; Kinetic energy; Paleontology; Zircon; Structural basin; Neutron; Nuclear physics","score_opus":0.05612299579725157,"score_gpt":0.2871745988686021,"score_spread":0.2310516030713505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2585814178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960369,0.00053028675,0.000063426545,0.002602281,0.000026844149,0.0003879347,0.00006393891,0.000006778267,0.00028163538],"genre_scores_gemma":[0.99935365,0.000011075352,0.00009227858,0.00014743653,0.000055960936,0.00001036383,0.000028756735,0.0000025212926,0.00029797803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848384,0.00032790823,0.00017524528,0.00034161325,0.00037546345,0.00029594603],"domain_scores_gemma":[0.998504,0.0006269348,0.00007709946,0.0005196135,0.00010868343,0.0001636655],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005315681,0.00010240408,0.0001842427,0.00003713928,0.00048394827,0.000036034024,0.0005199395,0.000058143374,0.0022254807],"category_scores_gemma":[0.00037139698,0.00005865967,0.000029325844,0.0000971966,0.0001819444,0.000039313392,0.00011100803,0.0002543394,0.000033415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009602331,0.00007879864,0.9150152,0.0000073067363,0.000036044174,0.000124167,0.0007480787,0.0005078255,0.0010840923,0.0000018081964,0.0016891679,0.080611445],"study_design_scores_gemma":[0.0002884352,0.00016544649,0.96531445,0.00000576901,0.000020262281,0.000013408086,0.0011907048,0.025634957,0.00018320372,0.000072917086,0.0070230453,0.00008741716],"about_ca_topic_score_codex":0.9753008,"about_ca_topic_score_gemma":0.9533361,"teacher_disagreement_score":0.08052403,"about_ca_system_score_codex":0.000019865802,"about_ca_system_score_gemma":0.00010091034,"threshold_uncertainty_score":0.9986866},"labels":[],"label_agreement":null},{"id":"W2605216192","doi":"10.1111/bre.12243","title":"Tectonic uplift of the Xichang Basin (<scp>SE</scp>Tibetan Plateau) revealed by structural geology and thermochronology data","year":2017,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Natural Science Foundation of China","keywords":"Geology; Thermochronology; Structural basin; Tectonics; Plateau (mathematics); Tectonic uplift; Geomorphology; Cenozoic; Fission track dating; Basin and range topography; Paleontology; Geochemistry","score_opus":0.08630089182402725,"score_gpt":0.3279973329938719,"score_spread":0.24169644116984465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2605216192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98801905,0.0019351422,0.0000030245305,0.0042914245,0.00008079256,0.00019252456,0.00024348509,0.000012259193,0.005222269],"genre_scores_gemma":[0.99809813,0.00019845486,0.0001327275,0.00014283722,0.00006614525,0.0000016480732,0.00014461408,0.0000032603791,0.0012121947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99757886,0.00048411658,0.00025532363,0.000567731,0.00043086737,0.0006831149],"domain_scores_gemma":[0.9972201,0.0009932666,0.00014473034,0.0013808844,0.00010642987,0.00015457932],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013200693,0.00015175302,0.00035020843,0.00007547833,0.00081392005,0.00008964903,0.0021883654,0.00019016939,0.0038455005],"category_scores_gemma":[0.0018235927,0.000085374646,0.00006245791,0.00022006538,0.0017706505,0.00015472122,0.0007543826,0.00056691584,0.00008386975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024503615,0.000013809741,0.9774235,0.00002461956,0.000057031677,0.000010586576,0.00006129281,0.0000068919526,0.002529439,0.00010246777,0.0035839877,0.016161906],"study_design_scores_gemma":[0.00027213115,0.000107766624,0.98097855,0.000011706004,0.000019073941,0.00002100945,0.000107728934,0.003625028,0.0016104286,0.009112268,0.0040743025,0.000059996248],"about_ca_topic_score_codex":0.018886799,"about_ca_topic_score_gemma":0.0076680956,"teacher_disagreement_score":0.016101908,"about_ca_system_score_codex":0.000004526801,"about_ca_system_score_gemma":0.000066333545,"threshold_uncertainty_score":0.9970651},"labels":[],"label_agreement":null},{"id":"W2738438420","doi":"10.1111/bre.12257","title":"The role of pre‐existing structures during rifting, continental breakup and transform system development, offshore West Greenland","year":2017,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Shell","keywords":"Geology; Rift; Terrane; Submarine pipeline; Paleontology; Seismology; Continental margin; Continental shelf; Isochron dating; Sinistral and dextral; Continental crust; Inversion (geology); Fault (geology); Structural basin; Stage (stratigraphy); Tectonics; Oceanography; Isochron; Geochemistry","score_opus":0.051517177459503474,"score_gpt":0.2914600113380701,"score_spread":0.23994283387856663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2738438420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9829005,0.00081865693,0.0000032428366,0.0002456939,0.000046005916,0.00019026644,0.000014182862,0.00001027994,0.015771195],"genre_scores_gemma":[0.9995148,0.00009937781,0.00012386938,0.0000013670342,0.0000634888,0.0000027326057,0.000010420146,0.0000017542638,0.0001821436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895734,0.00007442555,0.0001729171,0.00015934154,0.0003263263,0.000309661],"domain_scores_gemma":[0.99947095,0.00017624914,0.00007154012,0.00013693322,0.00008102879,0.00006330358],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00084621256,0.0000719402,0.000116135,0.00002495643,0.0027300236,0.00019740313,0.0002496916,0.00004137314,0.000045520406],"category_scores_gemma":[0.00015310297,0.000041134845,0.000018135606,0.000042678803,0.00029725538,0.00010854303,0.000053495816,0.00014692445,0.000008370371],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009328999,0.0000028546494,0.89082336,0.00005515083,0.000013509007,0.0000036269298,0.0005671936,0.000007435279,0.00006978882,0.00024113772,0.0000134373895,0.10810922],"study_design_scores_gemma":[0.00018113008,0.000046063622,0.9917878,0.000038364687,0.000002139994,0.000009014457,0.0026488202,0.00060979027,0.0009256762,0.0002654862,0.0034322625,0.000053482192],"about_ca_topic_score_codex":0.0057599978,"about_ca_topic_score_gemma":0.012819819,"teacher_disagreement_score":0.10805573,"about_ca_system_score_codex":0.0000045977877,"about_ca_system_score_gemma":0.000021336542,"threshold_uncertainty_score":0.9985683},"labels":[],"label_agreement":null},{"id":"W2744015449","doi":"10.1111/bre.12259","title":"Sediment routing evolution in the North Alpine Foreland Basin, Austria: interplay of transverse and longitudinal sediment dispersal","year":2017,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foreland basin; Molasse; Zircon; Provenance; Paleontology; Precambrian; Sedimentology; Massif; Detritus; Paleocurrent; Structural basin; Clastic rock","score_opus":0.050569492211720884,"score_gpt":0.3114528615037376,"score_spread":0.2608833692920167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2744015449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942315,0.0001530852,0.00006246507,0.0034526756,0.000033895343,0.00017456984,0.000039226976,0.000003646196,0.001848904],"genre_scores_gemma":[0.99968946,0.000042789132,0.00008351208,0.000022832228,0.00005778596,0.0000024497992,0.000031141095,0.0000011092887,0.0000688937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984074,0.00020609888,0.00021222649,0.0002602606,0.0005458503,0.00036812652],"domain_scores_gemma":[0.9992189,0.0003130371,0.000058942445,0.00025047123,0.00006740418,0.00009128593],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015581547,0.000093637726,0.00018272664,0.00008574189,0.00035349585,0.00007827369,0.00037616084,0.000056070658,0.0009837253],"category_scores_gemma":[0.00026002838,0.00005288558,0.000060234386,0.00019375824,0.000405656,0.0001177177,0.0000539252,0.0003275619,0.000025099887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011854107,0.000048383306,0.99649596,0.000014436872,0.0000186672,0.000021105052,0.00017564966,0.000097115604,0.000046711346,0.00014692938,0.00014241456,0.0026741042],"study_design_scores_gemma":[0.000422115,0.00020808626,0.99053866,0.000027762093,0.000016893817,0.000005351443,0.0004346674,0.0071662725,0.00011295482,0.00079654396,0.00020533604,0.00006537962],"about_ca_topic_score_codex":0.026942033,"about_ca_topic_score_gemma":0.028203897,"teacher_disagreement_score":0.007069157,"about_ca_system_score_codex":0.000010224252,"about_ca_system_score_gemma":0.00002847369,"threshold_uncertainty_score":0.9999295},"labels":[],"label_agreement":null},{"id":"W2794086882","doi":"10.1111/bre.12283","title":"Detrital zircon and apatite constraints on depositional ages, sedimentation rates and provenance: Pliocene Productive Series, South Caspian Basin, Azerbaijan","year":2018,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Zircon; Geology; Sedimentary depositional environment; Provenance; Neogene; Geochemistry; Geochronology; Archean; Detritus; Paleontology; Proterozoic; Sedimentary rock; Structural basin; Tectonics","score_opus":0.03599120320993523,"score_gpt":0.28622647529304984,"score_spread":0.25023527208311463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794086882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934863,0.00028000283,0.000017385213,0.00257486,0.000039059105,0.0002795527,0.00016296442,0.000016340216,0.0031435248],"genre_scores_gemma":[0.99753934,0.000055556484,0.0015037459,0.00016787107,0.00018852577,0.0000056705535,0.00020653133,0.0000024566039,0.00033032085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843264,0.00018029947,0.0001372775,0.00045512134,0.00043199369,0.00036267974],"domain_scores_gemma":[0.9992512,0.00019256944,0.00003838578,0.00010525515,0.0002307438,0.00018187528],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005458158,0.000119869306,0.00014934315,0.00012480734,0.00038598664,0.00011410647,0.00008481501,0.00007016348,0.0015180741],"category_scores_gemma":[0.00027889505,0.00008736224,0.000022840399,0.0004198302,0.001234596,0.00018558893,0.0000301679,0.00021952088,0.00009397054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006345217,0.00010694983,0.89179856,0.000071807255,0.00007143715,0.00006339631,0.0006628444,0.0000092455675,0.012233659,0.000594267,0.0012841356,0.09246916],"study_design_scores_gemma":[0.0004116191,0.0010694902,0.9507224,0.00004141401,0.000012924353,0.000040562358,0.00045384184,0.00033413418,0.04144326,0.0047570164,0.00054514664,0.00016819045],"about_ca_topic_score_codex":0.0014574442,"about_ca_topic_score_gemma":0.0007733804,"teacher_disagreement_score":0.092300974,"about_ca_system_score_codex":0.000007762552,"about_ca_system_score_gemma":0.00004692393,"threshold_uncertainty_score":0.99939466},"labels":[],"label_agreement":null},{"id":"W2911646502","doi":"10.1111/bre.12341","title":"Monoclinal flexure of an orogenic plateau margin during subduction, south Turkey","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"National University of Science and Technology; Natural Sciences and Engineering Research Council of Canada; Nederlandse Organisatie voor Wetenschappelijk Onderzoek","keywords":"Geology; Forearc; Outcrop; Plateau (mathematics); Subduction; Monocline; Paleontology; Seismology; Continental margin; Syncline; Tectonics; Geomorphology; Sedimentary rock","score_opus":0.040692745564718635,"score_gpt":0.28348721079325356,"score_spread":0.24279446522853493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911646502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995973,0.0001765357,0.0000014071895,0.0003696207,0.00004747471,0.00012518674,0.00003663814,0.00002080537,0.0032493274],"genre_scores_gemma":[0.9977271,0.000018046116,0.00031153235,0.000017337235,0.000087990826,0.0000010186309,0.00008234685,0.000002299656,0.0017523088],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981815,0.00021962351,0.00021257563,0.00035191656,0.00058357534,0.00045076548],"domain_scores_gemma":[0.99920523,0.00011940087,0.00003999596,0.00028259296,0.00016223457,0.00019053997],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007744497,0.00009524831,0.00020110485,0.00015534497,0.00012889582,0.000034017605,0.00032679064,0.000093831804,0.029439418],"category_scores_gemma":[0.000090706926,0.000067587265,0.00008954083,0.0006241777,0.00015078639,0.00013141273,0.000038749782,0.00034464576,0.0014037059],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022979474,0.00004445459,0.9900489,0.000045836245,0.000026078369,0.000014796188,0.00014590168,0.0018991231,0.005788821,0.000043117518,0.00007110605,0.001642094],"study_design_scores_gemma":[0.00029570964,0.00021669807,0.9763468,0.000011378045,0.000008480425,0.000010475998,0.00054567715,0.0053658406,0.012922455,0.0036719467,0.0004797862,0.0001247488],"about_ca_topic_score_codex":0.005189471,"about_ca_topic_score_gemma":0.000869658,"teacher_disagreement_score":0.028035711,"about_ca_system_score_codex":0.0000045102292,"about_ca_system_score_gemma":0.000044349945,"threshold_uncertainty_score":0.9993738},"labels":[],"label_agreement":null},{"id":"W2911921614","doi":"10.1111/bre.12342","title":"Forward stratigraphic modelling of sediment pathways and depocentres in salt‐influenced passive‐margin basins: Lower Cretaceous, central Scotian Basin","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Offshore Energy Research Association","keywords":"Geology; Structural basin; Provenance; Salt tectonics; Cretaceous; Tectonics; Basin modelling; Sedimentary basin; Sedimentary rock; Paleontology; Passive margin; Sedimentary basin analysis; Rift; Geomorphology; Diapir","score_opus":0.04165806781241898,"score_gpt":0.260843255932774,"score_spread":0.21918518812035503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911921614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943854,0.0013765221,0.0001382029,0.0004585965,0.00009874224,0.0004943136,0.00010919572,0.000016832704,0.0029221831],"genre_scores_gemma":[0.9978225,0.00074285694,0.0012071232,0.00006809744,0.00002153739,0.0000033100293,0.000039029277,0.0000040236573,0.0000915225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975714,0.00025932508,0.00038722763,0.00035190358,0.0006934763,0.00073667243],"domain_scores_gemma":[0.9989245,0.00041117045,0.00007203558,0.00022056756,0.00016105452,0.00021065709],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00086696877,0.00015633622,0.00026973928,0.0003300483,0.00014494704,0.00010842646,0.00026372282,0.00012541843,0.0021048374],"category_scores_gemma":[0.00010228255,0.00012034537,0.000053655007,0.000696848,0.00021605068,0.00037793367,0.00003273845,0.00037050014,0.000079377416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016261269,0.000077546574,0.9599537,0.00021448075,0.000013179846,0.000018947158,0.00046011587,0.029200692,0.00010353473,0.00041278428,0.00013030821,0.009252094],"study_design_scores_gemma":[0.00072659797,0.0005914746,0.87059146,0.00023457778,0.000006313661,0.000008554417,0.0009071228,0.120192036,0.0011017341,0.0030541376,0.0023356408,0.0002503632],"about_ca_topic_score_codex":0.0034291197,"about_ca_topic_score_gemma":0.002716177,"teacher_disagreement_score":0.09099135,"about_ca_system_score_codex":0.000009415885,"about_ca_system_score_gemma":0.00018777004,"threshold_uncertainty_score":0.9988074},"labels":[],"label_agreement":null},{"id":"W2929117452","doi":"10.1111/bre.12364","title":"Anticosti foreland basin offshore of western Newfoundland: Concealed record of northern Appalachian orogen development","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Department of Natural Resources, Government of Newfoundland and Labrador","keywords":"Foreland basin; Geology; Devonian; Paleontology; Ordovician; Tectonic subsidence; Diachronous; Structural basin; Stratigraphy; Tectonics; Subsidence; Seismology","score_opus":0.042454490831342645,"score_gpt":0.2784594121438215,"score_spread":0.23600492131247888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2929117452","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99203,0.00018968777,0.0000144005135,0.00033109027,0.000042412015,0.00024742814,0.000037417634,0.00000985505,0.0070976694],"genre_scores_gemma":[0.9980271,0.000034643348,0.0007076264,0.000036538313,0.000029439649,0.0000014758377,0.00013154095,0.0000031986576,0.0010284679],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979147,0.00020730913,0.00041164533,0.00031790193,0.000703968,0.00044447967],"domain_scores_gemma":[0.9987247,0.00047488557,0.00010019977,0.00026813857,0.00026498782,0.00016711728],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093728385,0.00012578865,0.00040519852,0.00014599755,0.00007528677,0.00002158138,0.00039478386,0.00009814163,0.006777831],"category_scores_gemma":[0.00013033027,0.00008512556,0.00009450303,0.00051471876,0.0002182501,0.000061707906,0.0000593438,0.00023788144,0.00055666245],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014556156,0.000050530423,0.9766942,0.00007244454,0.000048755082,0.0000055064593,0.00011666176,0.00005187611,0.00031922405,0.000011867941,0.00003875393,0.022444593],"study_design_scores_gemma":[0.0003350157,0.00023214375,0.9921525,0.000045164194,0.00001047605,0.0000026643215,0.000117990625,0.0006025533,0.0013059103,0.00064798695,0.0044336095,0.00011395042],"about_ca_topic_score_codex":0.015314896,"about_ca_topic_score_gemma":0.07100069,"teacher_disagreement_score":0.055685792,"about_ca_system_score_codex":0.000008199075,"about_ca_system_score_gemma":0.00014661749,"threshold_uncertainty_score":0.99413013},"labels":[],"label_agreement":null},{"id":"W2939178618","doi":"10.1111/bre.12365","title":"Age, stratigraphy, sedimentology and tectonic setting of the Sigri Pyroclastic Formation and its fossil forests, Early Miocene, Lesbos, Greece","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pyroclastic rock; Geology; Pyroclastic fall; Geochemistry; Sedimentary rock; Sedimentology; Fluvial; Conglomerate; Paleontology; Geomorphology; Volcano; Explosive eruption; Structural basin","score_opus":0.03046252964583021,"score_gpt":0.2636214345588963,"score_spread":0.2331589049130661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2939178618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99523723,0.0015623419,0.0000045197876,0.00085136096,0.00002184956,0.00020722937,0.000018625859,0.000007340297,0.0020895018],"genre_scores_gemma":[0.9996454,0.00007663874,0.000068258145,0.000023942517,0.000014607067,0.0000016176134,0.000009923081,0.0000011319408,0.00015848083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874675,0.0001984054,0.00017558807,0.00021079117,0.00034543916,0.00032303738],"domain_scores_gemma":[0.9991455,0.0005094142,0.000052114043,0.00012469324,0.00008049849,0.00008774295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005594859,0.00008163982,0.00015723036,0.00009301529,0.00015528064,0.00004405216,0.00016833839,0.00007501656,0.0005254983],"category_scores_gemma":[0.00016500747,0.000047399662,0.000042373864,0.00046443153,0.00018155381,0.00012778585,0.000054695756,0.00024183371,0.000027933247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027227417,0.000010084955,0.987914,0.00007515551,0.000013655914,0.0000020433367,0.0000962609,0.00006588378,0.0017526697,0.0002769741,0.000057198144,0.009708821],"study_design_scores_gemma":[0.00017510058,0.0001698482,0.9807698,0.00002332622,0.000009308534,0.0000069891753,0.00011265142,0.010218916,0.0013987817,0.00693545,0.000119629745,0.000060201255],"about_ca_topic_score_codex":0.0022472907,"about_ca_topic_score_gemma":0.009196216,"teacher_disagreement_score":0.010153032,"about_ca_system_score_codex":0.0000020101286,"about_ca_system_score_gemma":0.0000243283,"threshold_uncertainty_score":0.5753838},"labels":[],"label_agreement":null},{"id":"W2946987982","doi":"10.1111/bre.12378","title":"Initiation and early evolution of a forearc basin: Georgia Basin, Canada","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sedimentary depositional environment; Geology; Marine transgression; Forearc; Paleontology; Unconformity; Structural basin; Progradation; Facies; Outcrop; Lithology; Sequence stratigraphy; Sedimentary basin analysis; Tectonics; Subduction","score_opus":0.03388086447697976,"score_gpt":0.26430523633885944,"score_spread":0.2304243718618797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946987982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97824615,0.0005278819,0.000030290561,0.0007599644,0.000066386056,0.00021432582,0.00006799749,0.000008262374,0.020078762],"genre_scores_gemma":[0.9990831,0.000043822263,0.00022004545,0.000033867298,0.00002439038,0.0000015791871,0.000027403741,0.0000017400458,0.0005640599],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998645,0.00016436663,0.00017852019,0.00016118157,0.0005500173,0.0003009206],"domain_scores_gemma":[0.99902904,0.00041031282,0.000042890733,0.0001353931,0.00028431127,0.000098050186],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00091941986,0.00006586843,0.00012688528,0.0001368291,0.00015775485,0.000048539318,0.00014037236,0.00006121699,0.0025659169],"category_scores_gemma":[0.00023467402,0.000051233586,0.000017290424,0.0004541835,0.00010954367,0.00027791472,0.00002225603,0.00017626575,0.00009289826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041598734,0.000007635994,0.98922205,0.000074259835,0.000004364025,0.0000019020619,0.000088214816,0.00006055092,0.000018633613,0.00091055525,0.00087874586,0.008691472],"study_design_scores_gemma":[0.00015988239,0.00020212219,0.9814151,0.000021730293,0.0000020612242,0.0000054629886,0.00025788293,0.0013251435,0.00013835062,0.0025193521,0.013888754,0.000064156244],"about_ca_topic_score_codex":0.7400639,"about_ca_topic_score_gemma":0.31560698,"teacher_disagreement_score":0.42445695,"about_ca_system_score_codex":0.000021321468,"about_ca_system_score_gemma":0.00065869774,"threshold_uncertainty_score":0.99834585},"labels":[],"label_agreement":null},{"id":"W2966040055","doi":"10.1111/bre.12393","title":"The stratigraphic record of minibasin subsidence, Precaspian Basin, Kazakhstan","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Condor Petroleum (Canada)","funders":"Condor Petroleum","keywords":"Geology; Diapir; Subsidence; Sedimentary rock; Paleontology; Permian; Structural basin; Sedimentary basin; Tectonic subsidence; Hydrocarbon exploration; Oceanography","score_opus":0.061753281450261654,"score_gpt":0.3105447678445639,"score_spread":0.24879148639430226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966040055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92524546,0.00071726216,0.0000062748068,0.0015952424,0.000156893,0.0003427468,0.00004523636,0.000016495196,0.07187439],"genre_scores_gemma":[0.99630344,0.00049662066,0.00041961408,0.000044114677,0.000035201625,0.000003301525,0.000023536777,0.0000023025368,0.0026718522],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99790686,0.00037897285,0.0003042602,0.00021983252,0.0007032809,0.00048681718],"domain_scores_gemma":[0.99791104,0.0012245135,0.00007094916,0.00036716595,0.00031202578,0.00011433464],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0023925041,0.0000957514,0.00015958841,0.00015877781,0.0003999709,0.00014265816,0.0005637724,0.00008378163,0.0060148085],"category_scores_gemma":[0.00036217322,0.000055820026,0.000060941882,0.0010368964,0.0003606112,0.0002525919,0.000023319015,0.0003282477,0.00069361774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012336085,0.000021194748,0.9011418,0.00006462227,0.000010528301,0.0000030262177,0.000112677706,0.000040525632,0.00003200812,0.0020366418,0.0023786975,0.094034895],"study_design_scores_gemma":[0.00012813762,0.0005759268,0.92078704,0.000036704987,0.0000024451808,0.000005499138,0.0007722095,0.00076399016,0.00036502004,0.007323304,0.06914744,0.000092263384],"about_ca_topic_score_codex":0.0038698835,"about_ca_topic_score_gemma":0.008086148,"teacher_disagreement_score":0.09394263,"about_ca_system_score_codex":0.000002779143,"about_ca_system_score_gemma":0.00017271476,"threshold_uncertainty_score":0.99489385},"labels":[],"label_agreement":null},{"id":"W2967896635","doi":"10.1111/bre.12398","title":"Impact of the East African Rift System on the routing of the deep‐water drainage network offshore Tanzania, western Indian Ocean","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Koninklijk Nederlands Instituut voor Onderzoek der Zee; European Social Fund; Shell; Natural Environment Research Council; Sight Research UK; United States Science Support Program","keywords":"Geology; Submarine canyon; East African Rift; Graben; Continental margin; Canyon; Submarine pipeline; Tectonics; Ridge; Oceanography; Rift; Paleontology; Continental shelf; Geomorphology","score_opus":0.03375008549402132,"score_gpt":0.26911577395296155,"score_spread":0.23536568845894024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967896635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97274446,0.00005278797,0.0000018644469,0.0011753163,0.000089887435,0.00044296612,0.000044480905,0.0000073984443,0.025440808],"genre_scores_gemma":[0.99946195,0.0000021162173,0.0000066629245,0.00004243004,0.000056823807,0.0000011087842,0.00000733511,0.0000030776644,0.00041851852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978649,0.00066016597,0.0002313428,0.00014457322,0.0006324612,0.00046652684],"domain_scores_gemma":[0.9987247,0.00052515516,0.00009244121,0.00046873247,0.00013296964,0.00005601625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00214709,0.00009732208,0.00015379564,0.00004629405,0.00044564687,0.0000748186,0.00088928995,0.00006346576,0.0008479729],"category_scores_gemma":[0.00012639642,0.00003184619,0.00011592493,0.00063312583,0.00025092045,0.000078133875,0.00010374578,0.0003726706,0.00014534226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037924492,0.000012450515,0.9921804,0.000060935552,0.000016945924,8.987914e-7,0.0015951055,0.0042805583,0.000010100217,0.00059060164,0.00020723035,0.0010068266],"study_design_scores_gemma":[0.000081093654,0.00019891236,0.9938516,0.00012282464,0.000003781314,0.000006362444,0.0025039802,0.0022047441,0.00011719439,0.00033523265,0.0005214608,0.000052815285],"about_ca_topic_score_codex":0.0020907917,"about_ca_topic_score_gemma":0.0009274706,"teacher_disagreement_score":0.026717437,"about_ca_system_score_codex":0.000009971256,"about_ca_system_score_gemma":0.000084688334,"threshold_uncertainty_score":0.92847085},"labels":[],"label_agreement":null},{"id":"W2970356769","doi":"10.1111/bre.12380","title":"Obstructed minibasins on a salt‐detached slope: An example from above the Sigsbee canopy, northern Gulf of Mexico","year":2019,"lang":"en","type":"article","venue":"Basin Research","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Salt tectonics; Oceanography; Paleontology; Structural basin; Diapir","score_opus":0.07938434485671968,"score_gpt":0.3012457322877725,"score_spread":0.22186138743105283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970356769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98954797,0.00019352858,0.000010459677,0.0006504945,0.00010590717,0.0003074963,0.0005323873,0.00001808473,0.008633661],"genre_scores_gemma":[0.99691784,0.000038543487,0.00017834002,0.00023018375,0.000140973,0.0000017141076,0.00038674974,0.000009904075,0.002095721],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9969323,0.00060063857,0.0003079142,0.0004973766,0.0011144199,0.00054734363],"domain_scores_gemma":[0.99735767,0.0012862921,0.00009412013,0.00087114976,0.00020118739,0.00018956065],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011367013,0.00016090361,0.00031069928,0.00019025862,0.0002219774,0.000116258394,0.0007975266,0.000098409895,0.0142565025],"category_scores_gemma":[0.000113655544,0.0001012758,0.000109302884,0.0008393443,0.00022192311,0.00013639574,0.000040200855,0.00039428126,0.0011072732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005010094,0.00015212057,0.9024276,0.000023439166,0.00021850395,0.00002974954,0.0022307818,0.0029175708,0.0029616838,0.00016891341,0.0017643212,0.08660427],"study_design_scores_gemma":[0.0005854816,0.00042472305,0.9610803,0.000031487783,0.000023641187,0.0000018007927,0.0029888295,0.01365107,0.001457156,0.0009369472,0.018621672,0.00019687675],"about_ca_topic_score_codex":0.28917912,"about_ca_topic_score_gemma":0.051596656,"teacher_disagreement_score":0.23758246,"about_ca_system_score_codex":0.000014984771,"about_ca_system_score_gemma":0.00022970878,"threshold_uncertainty_score":0.9996705},"labels":[],"label_agreement":null},{"id":"W3002217656","doi":"10.1111/bre.12278","title":"Basin Research outstanding reviewers 2018–19","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Globe; Library science; Publishing; Certificate; History; Sociology; Political science; Medicine; Law; Ophthalmology; Computer science","score_opus":0.26926423289922075,"score_gpt":0.41701055977619306,"score_spread":0.1477463268769723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002217656","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3068576,0.004596895,0.00052133005,0.07161688,0.0004904493,0.00273157,0.00003871752,0.0002016393,0.61294496],"genre_scores_gemma":[0.97024953,0.003786906,0.0020326898,0.0014823147,0.0004752347,0.000103446,0.000018340987,0.00009186605,0.021759667],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99257946,0.0021638696,0.00039278358,0.000820916,0.0026996739,0.0013433141],"domain_scores_gemma":[0.9976156,0.0007654159,0.000047529316,0.0006027881,0.00008274395,0.00088592217],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.010939575,0.00018388705,0.00030733817,0.00017252793,0.00077697716,0.00016973032,0.00092152925,0.0001703517,0.016627915],"category_scores_gemma":[0.0020384307,0.00014633032,0.00010614059,0.0027349866,0.0008315738,0.00021872426,0.0010801817,0.0017410188,0.015467625],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024067819,0.00017781439,0.0266426,0.00024564244,0.000046586076,0.00023342711,0.0035474736,0.00037072095,0.02090516,0.002507084,0.9268037,0.01827913],"study_design_scores_gemma":[0.0004950327,0.00035155745,0.0038919433,0.00010711817,0.000007197762,0.0000074293453,0.0011075117,0.0019682762,0.0018143634,0.0017430179,0.9882283,0.00027825884],"about_ca_topic_score_codex":0.001126307,"about_ca_topic_score_gemma":0.000015880192,"teacher_disagreement_score":0.66339195,"about_ca_system_score_codex":0.0005273689,"about_ca_system_score_gemma":0.00009406267,"threshold_uncertainty_score":0.98529893},"labels":[],"label_agreement":null},{"id":"W3003682078","doi":"10.1111/bre.12435","title":"Ordovician tectonic shift in the western North China Craton constrained by stratigraphic and geochronological analyses","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Natural Science Foundation of China","keywords":"Ordovician; Geology; Terrane; Craton; Paleontology; Carbonate platform; Foreland basin; Passive margin; Zircon; Onlap; Provenance; Diachronous; Tectonic subsidence; Tectonics; Rift; Structural basin; Unconformity; Facies","score_opus":0.08730979000307593,"score_gpt":0.32135037335954225,"score_spread":0.23404058335646633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003682078","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9748229,0.00089783716,0.000014046341,0.021927757,0.000004366327,0.00016099107,0.00006260365,0.000019099067,0.0020904406],"genre_scores_gemma":[0.99873567,0.00013447902,0.000042987715,0.00093255535,0.00003608223,0.0000033454673,0.00010262362,0.0000011935438,0.000011058303],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979488,0.00047460067,0.00021422074,0.00039971576,0.00047880196,0.00048384516],"domain_scores_gemma":[0.9991084,0.0004929943,0.00002771969,0.00014780826,0.000027382313,0.00019572114],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059594365,0.00012929911,0.00022993532,0.000088779394,0.00020737557,0.00013230278,0.0004270571,0.00008407398,0.002486222],"category_scores_gemma":[0.00026442495,0.000068691574,0.000060627517,0.0013569188,0.0005087497,0.00007512057,0.00003697287,0.00063751324,0.00008192483],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003545154,0.00003389612,0.9933562,0.000010976992,0.0000144026235,0.000053247222,0.00018784098,0.00004969387,0.00017509506,0.000034000852,0.00019481138,0.0058543845],"study_design_scores_gemma":[0.00017913798,0.0003255595,0.9944355,0.0000040723144,0.000008931417,0.000003705216,0.00025296706,0.0017968095,0.000048137845,0.0022116934,0.0006346882,0.00009880436],"about_ca_topic_score_codex":0.009494363,"about_ca_topic_score_gemma":0.06336107,"teacher_disagreement_score":0.05386671,"about_ca_system_score_codex":0.0000018238027,"about_ca_system_score_gemma":0.00003991288,"threshold_uncertainty_score":0.99842566},"labels":[],"label_agreement":null},{"id":"W3007302607","doi":"10.1111/bre.12442","title":"Predicting sediment discharges and erosion rates in deep time—examples from the late Cretaceous North American continent","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Erosion; Sediment; Cenomanian; Cretaceous; Paleontology; Tectonics; Structural basin; Sedimentary budget; Sedimentary depositional environment; Sediment transport","score_opus":0.050460869777612286,"score_gpt":0.28226088356136114,"score_spread":0.23180001378374887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007302607","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872804,0.0010629874,0.000019254363,0.011071048,0.000013306922,0.00018476137,0.00008727218,0.000018029883,0.0002629033],"genre_scores_gemma":[0.9986806,0.0005214387,0.00024096553,0.00032628333,0.0000540519,0.000003486298,0.00013035629,0.0000017537393,0.000041100815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988547,0.00024298581,0.00015187921,0.00017054653,0.00030324503,0.00027662606],"domain_scores_gemma":[0.99871963,0.0010037507,0.000035030567,0.00007786204,0.00004826381,0.000115457355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047273195,0.00007336282,0.00011863955,0.000030272931,0.00027581723,0.00013244235,0.00018144074,0.000018870825,0.0008394839],"category_scores_gemma":[0.00031798484,0.000040969953,0.000014176006,0.00041585884,0.00017257404,0.000113309776,0.000052407824,0.00023677279,0.0001392326],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043210857,0.0000066460307,0.9807849,0.000007812655,0.0000038320673,0.0000030304527,0.00085334113,0.0004106314,0.000040242438,0.0000027811443,0.00017662131,0.017666936],"study_design_scores_gemma":[0.00010733439,0.00014645832,0.9459947,0.000011260311,0.0000021611393,5.664064e-7,0.0007821992,0.049562704,0.000081716986,0.00009699585,0.0031602615,0.000053668464],"about_ca_topic_score_codex":0.009952269,"about_ca_topic_score_gemma":0.009308915,"teacher_disagreement_score":0.049152073,"about_ca_system_score_codex":0.000002019131,"about_ca_system_score_gemma":0.000023515353,"threshold_uncertainty_score":0.99664056},"labels":[],"label_agreement":null},{"id":"W3014632940","doi":"10.1111/bre.12623","title":"Effects of contemporaneous orogenesis on sedimentation in the Late Cretaceous Western Interior Basin, northern Utah and southwestern Wyoming","year":2021,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"American Association of Petroleum Geologists; University of Houston; National Science Foundation","keywords":"Geology; Unconformity; Paleontology; Conglomerate; Cretaceous; Sedimentary depositional environment; Outcrop; Biostratigraphy; Sedimentary rock; Geochronology; Isopach map; Structural basin; Facies","score_opus":0.03323743745063917,"score_gpt":0.2813790757293768,"score_spread":0.24814163827873764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014632940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99719054,0.00082914927,0.0000052826554,0.0013511142,0.00002456378,0.0001748219,0.000016176453,0.000006691359,0.00040163548],"genre_scores_gemma":[0.99929196,0.00008194561,0.000033089826,0.00029226005,0.000024249559,0.000004038423,0.000034433888,0.000002397445,0.00023563941],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981463,0.0006667782,0.00020985426,0.0002462438,0.000457365,0.00027343724],"domain_scores_gemma":[0.998105,0.0015233922,0.000042995765,0.0001498037,0.000107304004,0.00007151043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007456866,0.00009871871,0.00021334106,0.000092403985,0.00009219059,0.000067472465,0.00017908296,0.000058663227,0.0003365858],"category_scores_gemma":[0.00026913633,0.00006055119,0.000056807374,0.00040118778,0.00014917375,0.000044552817,0.000035538756,0.00020910733,0.00007288619],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001272406,0.000047483238,0.97413504,0.00008040166,0.00002228284,0.00035367828,0.0009859644,0.00006769609,0.0035544408,0.0000021233425,0.0000074175505,0.020616254],"study_design_scores_gemma":[0.0004288885,0.0002661729,0.9817541,0.00007902563,0.000018869523,0.000026539637,0.0011349767,0.00055787456,0.0149691515,0.0004055599,0.00026161413,0.00009720497],"about_ca_topic_score_codex":0.0060095596,"about_ca_topic_score_gemma":0.019376112,"teacher_disagreement_score":0.020519048,"about_ca_system_score_codex":0.000004603564,"about_ca_system_score_gemma":0.000032693944,"threshold_uncertainty_score":0.9985177},"labels":[],"label_agreement":null},{"id":"W3024795497","doi":"10.1111/bre.12468","title":"Interplay of eustatic, tectonic and autogenic controls on a Late Devonian carbonate platform, northern Canning Basin, Australia","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds De La Recherche Scientifique - FNRS","keywords":"Geology; Facies; Paleontology; Tectonics; Sedimentary depositional environment; Tectonic uplift; Structural basin; Geomorphology","score_opus":0.0823606683208225,"score_gpt":0.34390038848473875,"score_spread":0.26153972016391624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024795497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9798493,0.00007747293,0.0010620666,0.010679926,0.00004507225,0.00031314528,0.000011643052,0.00006437067,0.007897016],"genre_scores_gemma":[0.99731916,0.0000062199574,0.001073952,0.00020669136,0.000032695243,0.000018575416,0.000002450295,0.0000047339654,0.0013355475],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9979727,0.00016768408,0.0002881753,0.0004798232,0.00051185105,0.00057975645],"domain_scores_gemma":[0.9986501,0.00038975858,0.00008187171,0.00036781465,0.00027583842,0.0002346146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00101337,0.0001543629,0.00027078,0.00011211587,0.00015086097,0.00011168415,0.0007355465,0.00009487472,0.00007742022],"category_scores_gemma":[0.0006963933,0.00013566097,0.00005697274,0.0005359492,0.00018415794,0.00013124125,0.00042209245,0.00054638064,0.000037320107],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002343841,0.0008122035,0.38364866,0.003285477,0.0011562415,0.0030015006,0.05745009,0.014751813,0.376026,0.06130741,0.012225622,0.08399114],"study_design_scores_gemma":[0.0067464574,0.003872262,0.21497175,0.0010620633,0.000045484787,0.00014994013,0.0015705382,0.5434,0.13688457,0.012735195,0.07688783,0.0016739228],"about_ca_topic_score_codex":0.00059034996,"about_ca_topic_score_gemma":0.00012977014,"teacher_disagreement_score":0.5286482,"about_ca_system_score_codex":0.00005389611,"about_ca_system_score_gemma":0.00020034862,"threshold_uncertainty_score":0.5532094},"labels":[],"label_agreement":null},{"id":"W3039313537","doi":"10.1111/bre.12489","title":"Burial dolomitization driven by modified seawater and basal aquifer‐sourced brines: Insights from the Middle and Upper Devonian of the Western Canadian Sedimentary Basin","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"MacEwan University","funders":"Natural Environment Research Council; American Association of Petroleum Geologists","keywords":"Dolomitization; Geology; Geochemistry; Dolomite; Devonian; Authigenic; Stylolite; Sedimentary rock; Dolostone; Evaporite; Clastic rock; Diagenesis; Carbonate rock; Facies; Paleontology; Structural basin","score_opus":0.05319119730530494,"score_gpt":0.25031930539823133,"score_spread":0.19712810809292639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3039313537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792479,0.0013120136,0.0000074215795,0.016078634,0.00007713703,0.0002957588,0.00029456374,0.0000067177366,0.0026797997],"genre_scores_gemma":[0.9983743,0.00004770343,0.000044321423,0.0013170675,0.000121452395,0.0000020129178,0.000055996974,0.0000016491637,0.00003551241],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99833477,0.0005980592,0.00016447708,0.0002741637,0.0003254071,0.0003031144],"domain_scores_gemma":[0.9991259,0.0003979285,0.000032738062,0.00014534523,0.000045232886,0.00025283007],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025945102,0.00010815667,0.00014985859,0.00005388444,0.00046539944,0.00008617587,0.0002742825,0.00010857034,0.00010653726],"category_scores_gemma":[0.000063160114,0.00006342704,0.00003248148,0.0002047132,0.00054033723,0.00012834666,0.000011110294,0.00028387064,0.0000044533213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011549326,0.000005660433,0.9905372,0.000009714152,0.00003122106,0.000006547799,0.0028404815,0.000008681641,0.0003235932,0.000009835219,0.0030500805,0.0030614478],"study_design_scores_gemma":[0.0004508991,0.00008517402,0.99377847,0.00002111989,0.000009597132,0.0000022877382,0.00042977175,0.0020530827,0.0006975594,0.00015967521,0.002232206,0.000080152575],"about_ca_topic_score_codex":0.46475914,"about_ca_topic_score_gemma":0.36316714,"teacher_disagreement_score":0.10159199,"about_ca_system_score_codex":0.0000039855267,"about_ca_system_score_gemma":0.00014900106,"threshold_uncertainty_score":0.6484534},"labels":[],"label_agreement":null},{"id":"W3044614124","doi":"10.1111/bre.12495","title":"Sequence stratigraphy of a Middle to Upper Ordovician foreland succession (Ottawa Embayment, central Canada): Evidence for tectonic control on sequence architecture along southern Laurentia","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foreland basin; Paleontology; Onlap; Ordovician; Laurentia; Facies; Craton; Sequence stratigraphy; Tectonic subsidence; Carbonate platform; Passive margin; Diachronous; Subsidence; Structural basin; Tectonics; Rift","score_opus":0.11973081120965241,"score_gpt":0.3300245374293994,"score_spread":0.210293726219747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3044614124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98123497,0.0025942002,0.0012671188,0.008428895,0.0001380032,0.0015084541,0.0018197023,0.000032650638,0.0029760331],"genre_scores_gemma":[0.99852335,0.000019282228,0.00085893396,0.00043288976,0.00009160641,0.0000204608,0.000028234375,0.000003081221,0.000022159164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967042,0.00044169684,0.00038478494,0.000588842,0.000917862,0.00096258445],"domain_scores_gemma":[0.9977034,0.0011782709,0.000105011,0.00029239678,0.00017366462,0.00054730894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079977646,0.00022326257,0.000336285,0.00019023009,0.0004210975,0.00007141867,0.00070102146,0.00013467013,0.00020064016],"category_scores_gemma":[0.0005718552,0.000174381,0.0001351572,0.00070613716,0.0003047866,0.00013697425,0.000004744462,0.00053205393,0.000006296708],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012534757,0.00002845479,0.94716173,0.00018717635,0.00006710358,0.000054145374,0.0009225216,0.0009019931,0.003793357,0.00021542581,0.00076464255,0.044649977],"study_design_scores_gemma":[0.0006773682,0.0012557949,0.9916378,0.00034462655,0.00002005338,0.00000684383,0.0005697432,0.002999094,0.0011811553,0.0005073535,0.0005595713,0.00024058313],"about_ca_topic_score_codex":0.26940718,"about_ca_topic_score_gemma":0.911389,"teacher_disagreement_score":0.64198184,"about_ca_system_score_codex":0.000015351936,"about_ca_system_score_gemma":0.0011119946,"threshold_uncertainty_score":0.7354579},"labels":[],"label_agreement":null},{"id":"W3046259337","doi":"10.1111/bre.12497","title":"Characterization of Late Cretaceous to Miocene source rocks in the Eastern Mediterranean Sea: An integrated numerical approach of stratigraphic forward modelling and petroleum system modelling","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Source rock; Cretaceous; Facies; Paleontology; Upwelling; Structural basin; Total organic carbon; Neogene; Organic matter; Geochemistry; Oceanography","score_opus":0.07359246591134755,"score_gpt":0.27202519302846906,"score_spread":0.1984327271171215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046259337","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.51904035,0.00004816074,0.48048353,0.00015555542,0.0000064052338,0.00015849454,0.000008766971,0.000026289286,0.00007243812],"genre_scores_gemma":[0.9988108,0.000062950836,0.0009216899,0.000015587,0.000047534788,0.00002948772,0.0000728591,0.00002769884,0.000011378732],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9980234,0.00039213191,0.00043111978,0.00024979704,0.0006353572,0.00026817748],"domain_scores_gemma":[0.99936026,0.00006228507,0.00004382654,0.00022209682,0.00014252323,0.00016897847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083964586,0.0001395262,0.00033635803,0.0003660987,0.000056975958,0.000060298313,0.00028613265,0.000093881376,0.0000028539914],"category_scores_gemma":[0.000020530277,0.000106285224,0.000056393797,0.0011919013,0.00004328633,0.00015130716,0.00003422441,0.00038218938,0.0000015705715],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006564508,0.000035171644,0.00063274376,0.0003370771,0.000034992485,0.000003418747,0.006167716,0.98734176,0.004951902,0.000015102197,0.0000023115335,0.00041213658],"study_design_scores_gemma":[0.00019424525,0.00010528356,0.000045653152,0.000075737626,0.000013755432,0.0000015896497,0.003235549,0.9948938,0.0012826148,0.0000050515127,0.00005396981,0.00009274738],"about_ca_topic_score_codex":0.00024502975,"about_ca_topic_score_gemma":0.000018949957,"teacher_disagreement_score":0.47977048,"about_ca_system_score_codex":0.000023815166,"about_ca_system_score_gemma":0.000028349443,"threshold_uncertainty_score":0.43341857},"labels":[],"label_agreement":null},{"id":"W3084241576","doi":"10.1111/bre.12509","title":"Landscape responses to intraplate deformation in the Kalahari constrained by sediment provenance and chronology in the Okavango Basin","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ASTER","funders":"Hebrew University of Jerusalem; Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"Geology; Provenance; Craton; Structural basin; Rift; Paleontology; Geochemistry; Diachronous; Archean; Geomorphology; Tectonics","score_opus":0.053911356985407985,"score_gpt":0.3014183406815982,"score_spread":0.24750698369619017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084241576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94579417,0.0004565224,0.000033448814,0.048787348,0.000013262018,0.00039174102,0.000044857305,0.00000911307,0.0044695362],"genre_scores_gemma":[0.99747276,0.00010547618,0.00010936815,0.0022105994,0.000018124489,0.000015733514,0.00004396954,7.4031266e-7,0.000023196515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889165,0.0004361103,0.00012723425,0.000113125985,0.00021514963,0.00021670312],"domain_scores_gemma":[0.99920857,0.000637216,0.000015601849,0.000076577235,0.000025254429,0.00003680397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017630425,0.00004900769,0.00006891418,0.000072631075,0.00010811372,0.00007329228,0.00022544537,0.00003829908,0.00023719532],"category_scores_gemma":[0.00039605793,0.000024544306,0.0000074146888,0.0005009643,0.000088790104,0.00011872525,0.000014349153,0.00022784118,0.000066880726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008887645,0.00011206201,0.60383105,0.00019989448,0.000010561052,0.000066799366,0.027028795,0.00052568497,0.00018714048,0.0029179696,0.09796412,0.26626715],"study_design_scores_gemma":[0.0004293941,0.00066843,0.83808523,0.000020170415,0.0000014192291,0.000027227747,0.004795426,0.004519732,0.00011692519,0.0017219314,0.14950748,0.000106654625],"about_ca_topic_score_codex":0.00047886636,"about_ca_topic_score_gemma":0.00061837,"teacher_disagreement_score":0.2661605,"about_ca_system_score_codex":0.0000023372036,"about_ca_system_score_gemma":0.000045651082,"threshold_uncertainty_score":0.25971225},"labels":[],"label_agreement":null},{"id":"W3094702616","doi":"10.1111/bre.12525","title":"Cambrian syn‐rift tectonic pulses at unconformity‐bounded carbonates in the Avalon Zone of Newfoundland, Canada","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Rift; Unconformity; Paleontology; Facies; Carbonate; Siliciclastic; Escarpment; Geochemistry; Carbonate rock; Rift zone; Conglomerate; Clastic rock; Sedimentary rock; Tectonics","score_opus":0.048946445326626196,"score_gpt":0.25939016950061916,"score_spread":0.21044372417399296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094702616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95880985,0.0005931966,5.7971954e-7,0.016008126,0.0000580873,0.00027558708,0.000047221707,0.000008532239,0.024198806],"genre_scores_gemma":[0.9980564,0.000063113155,0.000017429922,0.00073411496,0.000077297234,0.0000040788477,0.000036640173,0.0000020509267,0.001008864],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976955,0.00033197913,0.00023178846,0.00026601698,0.0008868213,0.0005878868],"domain_scores_gemma":[0.998253,0.0012975599,0.000037632315,0.0001751271,0.000084935666,0.00015172962],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006555542,0.0001192741,0.00025078905,0.00004090327,0.00028788732,0.00003990672,0.00051178556,0.00004505642,0.0011398741],"category_scores_gemma":[0.00045187573,0.00006797817,0.000049280417,0.00087666,0.00029997312,0.00005020287,0.00008872904,0.00040144732,0.00012486645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015581967,0.000023545392,0.98722714,0.000045128945,0.000017146464,0.000092601695,0.0002472193,0.0001386832,0.000037952108,0.00023590114,0.0017991395,0.009979716],"study_design_scores_gemma":[0.00024986133,0.00023938713,0.95324373,0.000010616788,0.0000034398213,0.0000032996177,0.00041610165,0.00075199764,0.000052269064,0.00039569841,0.044540018,0.0000935536],"about_ca_topic_score_codex":0.96212816,"about_ca_topic_score_gemma":0.9954028,"teacher_disagreement_score":0.042740878,"about_ca_system_score_codex":0.000023745406,"about_ca_system_score_gemma":0.00027571435,"threshold_uncertainty_score":0.9997732},"labels":[],"label_agreement":null},{"id":"W3113443506","doi":"10.1111/bre.12536","title":"Leaky salt: Pipe trails record the history of cross‐evaporite fluid escape in the northern Levant Basin, Eastern Mediterranean","year":2020,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Evaporite; Geology; Anticline; Sedimentary rock; Structural basin; Salt dome; Paleontology; Salt tectonics; Halite; Petrology; Diapir","score_opus":0.1576133731041894,"score_gpt":0.3236505311837055,"score_spread":0.1660371580795161,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113443506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9639898,0.0024622716,0.000037945272,0.0136809,0.00029783568,0.00040120006,0.00005615336,0.000017334489,0.019056587],"genre_scores_gemma":[0.99752057,0.00020248356,0.000065418695,0.0010184781,0.00020328314,0.0000060723587,0.000047490783,0.0000039871416,0.00093224377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973688,0.00069871836,0.00037279772,0.0002519702,0.000872257,0.0004354414],"domain_scores_gemma":[0.99841785,0.00089152553,0.00006881167,0.00029517684,0.00020955583,0.00011707293],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0027937368,0.000120410965,0.00018202799,0.00009070458,0.00020633482,0.0000951151,0.000937537,0.000077886216,0.0033460322],"category_scores_gemma":[0.00069971074,0.000062217936,0.0000695562,0.00056955894,0.0005694869,0.00020171677,0.000039020088,0.00052310096,0.0004506932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040525605,0.00006798272,0.7207328,0.00019318261,0.0000144770975,0.000038349233,0.014652263,0.00040656934,0.000113125876,0.000052480704,0.013822117,0.24950138],"study_design_scores_gemma":[0.0003361029,0.000580155,0.5465206,0.000030549716,0.000004586174,0.000012028754,0.0020492105,0.009118733,0.000042844145,0.00056771404,0.44059917,0.00013830095],"about_ca_topic_score_codex":0.0043131285,"about_ca_topic_score_gemma":0.009431667,"teacher_disagreement_score":0.42677706,"about_ca_system_score_codex":0.000012865456,"about_ca_system_score_gemma":0.0002599576,"threshold_uncertainty_score":0.99756503},"labels":[],"label_agreement":null},{"id":"W3185457400","doi":"10.1111/bre.12584","title":"Indian plate structural inheritance in the Himalayan foreland basin, Nepal","year":2021,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Foreland basin; Geology; Basement; Paleontology; Neogene; Structural basin; Isopach map; Subsidence; Onlap; Geomorphology; Seismology; Sedimentary depositional environment; Facies","score_opus":0.05070624697182616,"score_gpt":0.2964622601926566,"score_spread":0.24575601322083043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3185457400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9830064,0.00058880204,0.0000012988771,0.0060793892,0.00004016338,0.00009088001,0.000036823374,0.000008889673,0.010147362],"genre_scores_gemma":[0.9985069,0.00006020438,0.0003545466,0.00050798676,0.00008912184,0.0000024018798,0.00011536433,0.0000015300302,0.00036195756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978386,0.00049658865,0.00017747885,0.00031276981,0.0006082018,0.00056632113],"domain_scores_gemma":[0.99896145,0.0005676102,0.000019594681,0.00023643249,0.00009933713,0.000115604984],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009754539,0.00009590725,0.00016078216,0.00008120483,0.00023110006,0.00013014232,0.00040772083,0.00008334998,0.009706419],"category_scores_gemma":[0.00038420784,0.00005459352,0.00006877691,0.0011739203,0.00019958147,0.00009526449,0.000041671392,0.000593087,0.00027862255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032366996,0.000012719858,0.9861209,0.000009164843,0.0000074477084,0.00040717627,0.0002488019,0.000072977215,0.000064062566,0.00012405303,0.0006315846,0.012268765],"study_design_scores_gemma":[0.00017500484,0.000052716063,0.9728479,0.0000094454235,0.0000027232802,0.000039627066,0.00073662354,0.0011810794,0.00024115409,0.021374088,0.0032529375,0.00008670622],"about_ca_topic_score_codex":0.00585325,"about_ca_topic_score_gemma":0.03829542,"teacher_disagreement_score":0.03244217,"about_ca_system_score_codex":0.000005202444,"about_ca_system_score_gemma":0.00006639917,"threshold_uncertainty_score":0.99119884},"labels":[],"label_agreement":null},{"id":"W3198520477","doi":"10.1111/bre.12611","title":"Mass transport deposits in reflection seismic data offshore Oregon, USA","year":2021,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Submarine landslide; Submarine pipeline; Landslide; Continental margin; Seismology; Subduction; Margin (machine learning); Sediment; Thrust fault; Passive margin; Geomorphology; Submarine; Tectonics; Oceanography; Rift","score_opus":0.16779481410731142,"score_gpt":0.36553209228900935,"score_spread":0.19773727818169792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3198520477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95876586,0.002377919,0.000081497434,0.0014736826,0.0001684348,0.00015184806,0.00008346161,0.000022834096,0.03687448],"genre_scores_gemma":[0.99625736,0.0008763435,0.0005582317,0.00010402744,0.00010202742,0.0000020343416,0.00030984607,0.000004346628,0.0017857538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978408,0.00029437116,0.00020806408,0.0005060666,0.00062225276,0.0005284073],"domain_scores_gemma":[0.99891317,0.00027578772,0.000018404366,0.0005707869,0.00012839506,0.00009345009],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001291118,0.00009877047,0.00017039682,0.00017137283,0.00024312238,0.00005347407,0.0003950046,0.00008218265,0.0016678297],"category_scores_gemma":[0.00016525503,0.000087011606,0.000029040435,0.0011182865,0.00011020418,0.00022641236,0.000041127096,0.00045428963,0.00039588512],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041874115,0.000024343532,0.9188658,0.000026529291,0.000016301905,0.00043268228,0.00017384735,0.00014060595,0.000119333396,0.000034749915,0.0018611501,0.078262806],"study_design_scores_gemma":[0.00023545728,0.000060027294,0.97146827,0.000036960086,0.0000047289323,0.00003312958,0.00038704192,0.0027099529,0.00092421146,0.0003826646,0.023653165,0.000104413004],"about_ca_topic_score_codex":0.0068089887,"about_ca_topic_score_gemma":0.15918015,"teacher_disagreement_score":0.15237115,"about_ca_system_score_codex":0.000013795649,"about_ca_system_score_gemma":0.0002877443,"threshold_uncertainty_score":0.99980474},"labels":[],"label_agreement":null},{"id":"W3205472953","doi":"10.1111/bre.12619","title":"The Appalachian area as a tectonostratigraphic analogue for the Barents Sea shelf","year":2021,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Oljedirektoratet","keywords":"Geology; Foreland basin; Paleontology; Structural basin; Sedimentary basin; Sedimentary rock; Sedimentary basin analysis; Basement; Paleozoic; Subduction; Orogeny; Passive margin; Canada Basin; Earth science; Rift; Tectonics; Archaeology; Geography","score_opus":0.11953901813863015,"score_gpt":0.32438235903862794,"score_spread":0.20484334089999778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3205472953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8504107,0.012288356,0.000593819,0.09542857,0.00075138494,0.0017622432,0.0002342052,0.00006533934,0.0384654],"genre_scores_gemma":[0.99758184,0.0011927144,0.00006923961,0.0002168482,0.00011622341,0.000030287538,0.00010758501,0.0000017284542,0.0006835608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984669,0.00026834363,0.00012819532,0.00022518793,0.00044860996,0.00046275728],"domain_scores_gemma":[0.9974344,0.0020077166,0.000018880264,0.00023646739,0.00022005457,0.00008253002],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.001412066,0.000075001946,0.000084572894,0.000027162185,0.0021075874,0.0002521188,0.00030425715,0.000047638514,0.00064872025],"category_scores_gemma":[0.00086119206,0.000034491826,0.000071628456,0.0005354785,0.00025468858,0.000056510493,0.00003487383,0.00025018814,0.00017292594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002496013,0.000048695136,0.7383125,0.00002793002,0.00012665146,0.000038331713,0.00039089436,0.0009850832,0.000043406326,0.00415528,0.040510535,0.21511114],"study_design_scores_gemma":[0.00016775526,0.00022986483,0.8126516,0.000007776276,0.000006312698,0.000006162011,0.002580639,0.008480227,0.00008522307,0.0075459685,0.16816437,0.00007413329],"about_ca_topic_score_codex":0.0036339057,"about_ca_topic_score_gemma":0.04108328,"teacher_disagreement_score":0.215037,"about_ca_system_score_codex":0.0000042468623,"about_ca_system_score_gemma":0.00011615705,"threshold_uncertainty_score":0.9991915},"labels":[],"label_agreement":null},{"id":"W4224042917","doi":"10.1111/bre.12668","title":"Reconstructing subsurface sandbody connectivity from temporal evolution of surface networks","year":2022,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Bathymetry; Overbank; Subsurface flow; Channel (broadcasting); Aquifer; Channelized; Geomorphology; Groundwater; Fluvial; Geotechnical engineering","score_opus":0.061607030226872354,"score_gpt":0.29514271928689667,"score_spread":0.2335356890600243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224042917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99278873,0.0014205624,0.00054979423,0.0002148154,0.00017418954,0.0001527708,0.00018525326,0.000023676183,0.004490223],"genre_scores_gemma":[0.99861,0.000027191503,0.0010904066,0.0000099486515,0.000034819263,0.0000015458244,0.000121510726,0.0000018218152,0.000102728845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980727,0.0006998556,0.00020507071,0.00020685958,0.00049686164,0.0003186464],"domain_scores_gemma":[0.99844396,0.0011182813,0.00007328142,0.0001588164,0.00013407771,0.00007158129],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0022681123,0.000066990004,0.00014395775,0.00007052644,0.0007186489,0.000036726608,0.00025446562,0.000045824094,0.010339274],"category_scores_gemma":[0.00023409537,0.000058361635,0.000035675857,0.0007597775,0.00016388542,0.00017406348,0.00006705675,0.00045801816,0.000034811725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006571056,0.000017144917,0.92747325,0.000007859329,0.000006321938,0.000002319035,0.000077677716,0.066771366,0.000036205485,0.00011158961,0.00034641448,0.0050841523],"study_design_scores_gemma":[0.00022607653,0.00024111083,0.8138228,0.000010465139,0.0000034497107,0.000009814811,0.0027215416,0.1745205,0.00017857771,0.005362797,0.002785072,0.00011778359],"about_ca_topic_score_codex":0.03310809,"about_ca_topic_score_gemma":0.0015060895,"teacher_disagreement_score":0.11365041,"about_ca_system_score_codex":0.000017997476,"about_ca_system_score_gemma":0.00013379427,"threshold_uncertainty_score":0.9905654},"labels":[],"label_agreement":null},{"id":"W4285796126","doi":"10.1111/bre.12697","title":"Seismic characterization and depositional significance of the Nahr Menashe deposits: Implications for the terminal phases of the Messinian salinity crisis in the north‐east Levant Basin, offshore Lebanon","year":2022,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Evaporite; Geology; Sedimentary depositional environment; Facies; Halite; Sabkha; Paleontology; Structural basin; Tectonics; Deposition (geology); Period (music); Salt tectonics; Geochemistry; Diapir","score_opus":0.062379299331344784,"score_gpt":0.3099119493175918,"score_spread":0.24753264998624702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285796126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98015517,0.0002064951,0.00028667398,0.017275194,0.000045839985,0.0007639046,0.0011169921,0.0000030613428,0.00014666567],"genre_scores_gemma":[0.9991851,0.00005474568,0.000054698583,0.0003951124,0.000027616428,0.00009160623,0.00013807222,0.0000020278762,0.000051038263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838245,0.0005788108,0.0002547974,0.00015107733,0.00044259307,0.00019024905],"domain_scores_gemma":[0.9984485,0.00097172597,0.00011755978,0.00027222195,0.00016607952,0.000023926857],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0012180097,0.00007145305,0.00009689024,0.000053506305,0.0013360013,0.00005850599,0.00064964785,0.000025427476,0.0001313678],"category_scores_gemma":[0.00017719343,0.000031338936,0.000051940748,0.00075567706,0.0003205154,0.00009699536,0.000073119474,0.00024247362,5.334928e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011964085,0.000114237766,0.9803167,0.000060859056,0.000012308147,3.6869866e-7,0.0011419302,0.0014815956,0.00051775534,0.00022784762,0.00073108764,0.0152756795],"study_design_scores_gemma":[0.00012412829,0.00011002966,0.9911992,0.00001170861,0.000011699205,0.000026870097,0.0014482435,0.0029115516,0.00036579432,0.00048286762,0.0032656726,0.000042237174],"about_ca_topic_score_codex":0.00087368564,"about_ca_topic_score_gemma":0.0021761507,"teacher_disagreement_score":0.019029908,"about_ca_system_score_codex":0.0000068314844,"about_ca_system_score_gemma":0.00018298454,"threshold_uncertainty_score":0.9999641},"labels":[],"label_agreement":null},{"id":"W4296102049","doi":"10.1111/bre.12714","title":"Ordovician tectonic transition from passive margin into peripheral foreland in the southern Ordos: A diagnostic insight into the closure of Erlangping Ocean between the North Qinling Arc and North China Block","year":2022,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Science Basic Research Program of Shaanxi Province; National Natural Science Foundation of China","keywords":"Geology; Foreland basin; Paleontology; Ordovician; Passive margin; Carbonate platform; Continental margin; Accretionary wedge; Tectonics; Rift; Structural basin; Subduction; Facies","score_opus":0.01934402220824027,"score_gpt":0.23499826183470746,"score_spread":0.21565423962646718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296102049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98818785,0.0010136989,0.000008708986,0.010082687,0.000014010063,0.00035923958,0.0001623246,0.000007729777,0.0001637572],"genre_scores_gemma":[0.9992793,0.0000810958,0.000033222917,0.00019482822,0.00010200322,0.000014665841,0.00027876865,0.0000036813185,0.000012418764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99721247,0.0011391643,0.00026356254,0.000304835,0.0007151876,0.0003647724],"domain_scores_gemma":[0.9971343,0.0024334593,0.00006309471,0.00025351957,0.000049980412,0.0000655932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010378958,0.00013297176,0.00021689222,0.00008124076,0.00097191415,0.0000761964,0.00061519584,0.000044454853,0.0005586691],"category_scores_gemma":[0.00028707954,0.000060458613,0.00008668537,0.0011212314,0.0003847432,0.000050630086,0.00009463867,0.0009330026,0.000007593313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052355987,0.000026054897,0.9577594,0.000012775198,0.000036344987,0.000021131475,0.030822355,0.003174328,0.0000057796915,0.000004644371,0.000018886249,0.008065973],"study_design_scores_gemma":[0.00022894744,0.0001912923,0.9803284,0.00001481953,0.000032459382,0.0000027318995,0.00993514,0.0041572396,0.000004848087,0.0045525953,0.00046074466,0.000090779],"about_ca_topic_score_codex":0.118587114,"about_ca_topic_score_gemma":0.3306613,"teacher_disagreement_score":0.21207418,"about_ca_system_score_codex":0.000013303145,"about_ca_system_score_gemma":0.00005512937,"threshold_uncertainty_score":0.8872823},"labels":[],"label_agreement":null},{"id":"W4297312356","doi":"10.1111/bre.12716","title":"Architecture, structural and tectonic significance of the Seagap fault (offshore Tanzania) in the framework of the East African Rift","year":2022,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; Università degli Studi di Napoli Federico II; National Science Foundation","keywords":"Geology; Seismology; Rift; Fault (geology); Seafloor spreading; Tectonics; Paleontology; Strike-slip tectonics; Neogene; Detachment fault; Trough (economics); Fracture zone; Structural basin; Extensional definition","score_opus":0.040038904698186856,"score_gpt":0.28710718077102954,"score_spread":0.24706827607284268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297312356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893651,0.0020019144,0.0000022381537,0.003835433,0.0001108895,0.00056187756,0.00014980804,0.0000050751833,0.0039676847],"genre_scores_gemma":[0.99963087,0.0000338929,0.00006040644,0.00011403966,0.000038175996,0.0000130189,0.0000018972175,0.0000037211933,0.00010399986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99663085,0.0013381974,0.00021547315,0.00024488117,0.0011664407,0.0004041771],"domain_scores_gemma":[0.99805206,0.0012525516,0.00008376101,0.0005189065,0.00005932908,0.00003339813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017581512,0.00010643074,0.00018081191,0.00008747836,0.00073005166,0.000030289979,0.0010573626,0.00004024392,0.00045925748],"category_scores_gemma":[0.00046331424,0.00004931994,0.00007758504,0.0014694126,0.00094380754,0.000027548256,0.00022488362,0.0011564331,0.0000017816036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000108184766,0.000023044135,0.9586754,0.000049021128,0.000028583014,0.0000060189686,0.0065678796,0.0015479194,0.000094404975,0.0014537403,0.00027443314,0.0311714],"study_design_scores_gemma":[0.00013563345,0.00014136595,0.98588526,0.00003030415,0.000005288818,0.000014636356,0.0052255318,0.00030547514,0.0001682857,0.005604274,0.0024205784,0.00006334405],"about_ca_topic_score_codex":0.0036277708,"about_ca_topic_score_gemma":0.0061201346,"teacher_disagreement_score":0.031108057,"about_ca_system_score_codex":0.000008057807,"about_ca_system_score_gemma":0.00017091203,"threshold_uncertainty_score":0.5615041},"labels":[],"label_agreement":null},{"id":"W4307169220","doi":"10.1111/bre.12728","title":"Stratigraphic record of continental breakup, offshore NW Australia—Discussion","year":2022,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Geology; Unconformity; Paleontology; Continental margin; Continental shelf; Continental crust; Rift; Breakup; Submarine pipeline; Tectonics; Oceanography","score_opus":0.10351012676448587,"score_gpt":0.3257675982762244,"score_spread":0.22225747151173855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307169220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98831207,0.000120479635,8.569243e-7,0.003211773,0.00009605597,0.00018356094,0.00013924428,0.0000142835825,0.007921695],"genre_scores_gemma":[0.9936382,0.000023367755,0.00007767549,0.000029696092,0.000056190107,0.0000062641197,0.000057557954,0.0000013376892,0.006109712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979806,0.00039731734,0.00018657111,0.00024800404,0.0007866303,0.00040088827],"domain_scores_gemma":[0.99942356,0.00022563654,0.00003716386,0.00014078188,0.00006878508,0.00010404589],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072475447,0.00008345132,0.00018868412,0.00009041288,0.00048935314,0.000019502637,0.00030047653,0.000030736013,0.01730531],"category_scores_gemma":[0.0000675982,0.000047281737,0.0000836905,0.00063885166,0.0003129283,0.00005192324,0.00010409761,0.0004215719,0.00025120098],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000198951,0.000116118856,0.932551,0.000019737727,0.000015603748,0.000025700667,0.00009733871,0.000086176275,0.0001112328,0.0003860868,0.0065039634,0.059888087],"study_design_scores_gemma":[0.00016852787,0.0009536361,0.9653985,0.0000060537254,0.0000028080224,0.000003325107,0.00080315646,0.00018969491,0.00008791819,0.004512957,0.027796077,0.00007737733],"about_ca_topic_score_codex":0.009834996,"about_ca_topic_score_gemma":0.0027943747,"teacher_disagreement_score":0.05981071,"about_ca_system_score_codex":0.0000033254357,"about_ca_system_score_gemma":0.000024543733,"threshold_uncertainty_score":0.9967586},"labels":[],"label_agreement":null},{"id":"W4311731768","doi":"10.1111/bre.12741","title":"Multi‐proxy evidence for rapidly shifting sediment sources to the Taiwan Western Foreland Basin at the Miocene–Pliocene transition","year":2022,"lang":"en","type":"article","venue":"Basin Research","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Science and Technology, Taiwan","keywords":"Foreland basin; Geology; Illite; Late Miocene; Paleontology; Neogene; Authigenic; Sediment; Glacial period; Pleistocene; Geochemistry; Structural basin; Clay minerals","score_opus":0.12755549368156724,"score_gpt":0.36242534094230106,"score_spread":0.23486984726073382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311731768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9186251,0.0027997554,0.00022427253,0.075921655,0.00021641575,0.0018137438,0.00015553621,0.000026549747,0.00021695904],"genre_scores_gemma":[0.9951169,0.0000745095,0.0003519694,0.0014681293,0.00015599257,0.00025878244,0.00011773992,0.000009533861,0.0024464726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9947142,0.0022578074,0.00029217682,0.0005751096,0.0010579797,0.0011027079],"domain_scores_gemma":[0.9943072,0.004790394,0.000055717424,0.00049858965,0.00016018013,0.0001878842],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.009963737,0.00016891447,0.00021586167,0.00021257815,0.004519374,0.0001258442,0.0010405816,0.00009261547,0.0022650806],"category_scores_gemma":[0.0006815223,0.00010178004,0.00011457197,0.0007373194,0.00047875603,0.00012504857,0.00021662969,0.00082568504,0.00036053188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000880254,0.00003837707,0.9853391,0.000043056854,0.000031893607,0.000021561209,0.0030851106,0.003996327,0.00004722769,0.0000114641525,0.004137981,0.0023676422],"study_design_scores_gemma":[0.00094436033,0.0010266132,0.9292895,0.000049910937,0.000023384997,0.000126934,0.0038741839,0.02026625,0.0005356126,0.00017980703,0.043458838,0.00022456012],"about_ca_topic_score_codex":0.0013234973,"about_ca_topic_score_gemma":0.009893477,"teacher_disagreement_score":0.07649176,"about_ca_system_score_codex":0.000019719546,"about_ca_system_score_gemma":0.0002078073,"threshold_uncertainty_score":0.998647},"labels":[],"label_agreement":null},{"id":"W4319836266","doi":"10.1111/bre.12755","title":"Heat flow and thermal regime in the Guaymas Basin, Gulf of California: Estimates of conductive and advective heat transport","year":2023,"lang":"en","type":"article","venue":"Basin Research","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Centro de Investigación Científica y de Educación Superior de Ensenada, Baja California","keywords":"Sill; Geology; Advection; Structural basin; Geomorphology; Canada Basin; Thermal conduction; Petrology; Oceanography","score_opus":0.04462035568798867,"score_gpt":0.3099917299204694,"score_spread":0.26537137423248075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319836266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967231,0.00046866856,0.00019450682,0.0010501548,0.000018130566,0.00025237934,0.00005843948,0.000031087642,0.0012035153],"genre_scores_gemma":[0.99929285,0.0004379123,0.00012906561,0.000009817479,0.000015423328,0.00003575445,0.000021524653,0.000017398626,0.000040274812],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987294,0.00019028404,0.0002320815,0.00017472933,0.00041471253,0.0002588084],"domain_scores_gemma":[0.9991961,0.00041874786,0.0000070672745,0.00020596231,0.000115818664,0.00005626725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012375164,0.00010477794,0.0002701981,0.0003724127,0.00006339434,0.000013574679,0.00013340681,0.00007631205,0.000040688315],"category_scores_gemma":[0.0001140389,0.00007352995,0.000046342502,0.0010510007,0.00029746877,0.000096942465,0.000031259984,0.00027044694,0.0000062434137],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006642732,0.0004597384,0.16829425,0.0021448769,0.0010780732,0.0003525795,0.07068738,0.464004,0.27954665,0.00080480194,0.004863606,0.0070997444],"study_design_scores_gemma":[0.0013133762,0.00023384375,0.1542665,0.00021362581,0.000060570917,0.000013825368,0.013658551,0.7644812,0.06380318,0.0009757787,0.00069182506,0.00028771718],"about_ca_topic_score_codex":0.000607249,"about_ca_topic_score_gemma":0.00021623666,"teacher_disagreement_score":0.30047718,"about_ca_system_score_codex":0.000024173049,"about_ca_system_score_gemma":0.00003581821,"threshold_uncertainty_score":0.29984644},"labels":[],"label_agreement":null},{"id":"W4381848348","doi":"10.1111/bre.12789","title":"Basin scale evolution of zebra textures in fault‐controlled, hydrothermal dolomite bodies: Insights from the Western Canadian Sedimentary Basin","year":2023,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Memorial University of Newfoundland","funders":"Natural Environment Research Council; International Association of Sedimentologists; University of Manchester; Sight Research UK; American Association of Petroleum Geologists Foundation; Society for Sedimentary Geology; Science and Technology Facilities Council; British Sedimentological Research Group","keywords":"Dolomitization; Dolomite; Geology; Geochemistry; Dolostone; Siliciclastic; Sedimentary rock; Breccia; Petrography; Diagenesis; Recrystallization (geology); Carbonate rock; Petrology; Geomorphology; Structural basin; Sedimentary depositional environment","score_opus":0.026982500772166247,"score_gpt":0.2627376392685234,"score_spread":0.23575513849635715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381848348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.977166,0.0012527247,0.0000032160585,0.016127862,0.00007339116,0.00040626468,0.00030781332,0.000025324462,0.00463743],"genre_scores_gemma":[0.99738824,0.000086217806,0.000041454306,0.0012263312,0.00015230366,0.000013029291,0.0002636502,0.0000044565754,0.00082430977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967787,0.0008988303,0.00038795787,0.000430798,0.000765575,0.00073810806],"domain_scores_gemma":[0.99754107,0.0016961747,0.000054330594,0.00033078538,0.00010002171,0.0002775982],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012711694,0.00016803949,0.0004137606,0.00042471237,0.00030211327,0.00006604456,0.00059556606,0.00015343948,0.0038005768],"category_scores_gemma":[0.00031343556,0.00009852425,0.0001515634,0.001248628,0.00040745232,0.00013685474,0.00006459439,0.0005008398,0.00080659776],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027843664,0.00003252366,0.9885988,0.000008786938,0.000045972894,0.000043966655,0.00042165932,0.0006914297,0.00030789134,0.000032807904,0.006297321,0.0032404074],"study_design_scores_gemma":[0.0009531382,0.00008008692,0.97291845,0.000039665323,0.000014754025,0.0000011648037,0.0007268746,0.007945155,0.00059170404,0.0069583366,0.009640152,0.00013051233],"about_ca_topic_score_codex":0.935397,"about_ca_topic_score_gemma":0.8546688,"teacher_disagreement_score":0.08072824,"about_ca_system_score_codex":0.00004180635,"about_ca_system_score_gemma":0.00020110543,"threshold_uncertainty_score":0.9999714},"labels":[],"label_agreement":null},{"id":"W4385225958","doi":"10.1111/bre.12804","title":"Controls on sedimentation in a deep‐water foredeep: Central Pindos foreland basin, western Greece","year":2023,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Hellenic Foundation for Research and Innovation; General Secretariat for Research and Technology","keywords":"Geology; Facies; Foreland basin; Sedimentary depositional environment; Paleontology; Sedimentary rock; Progradation; Paleogene; Structural basin; Isopach map; Geomorphology","score_opus":0.07213525932378438,"score_gpt":0.329928650814726,"score_spread":0.2577933914909416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385225958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99107134,0.000049357106,0.000040981056,0.0029240632,0.00010153813,0.00041432903,0.000041590833,0.00004371811,0.005313091],"genre_scores_gemma":[0.9983353,0.00006167648,0.000060037535,0.0002724904,0.00006369696,0.000016064509,0.0003956301,0.0000032331025,0.00079188385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980416,0.00022087486,0.00021324544,0.00022545688,0.0005426554,0.0007561333],"domain_scores_gemma":[0.9991915,0.00045810797,0.000019701,0.00012889362,0.000075622054,0.00012617193],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011564392,0.000096165095,0.00013686065,0.00032319006,0.00023203687,0.00013306981,0.00020235813,0.00008163905,0.0020162861],"category_scores_gemma":[0.00013390339,0.0000613294,0.00003378786,0.0005882266,0.00008737721,0.00025293286,0.000022404256,0.00026234845,0.0024619014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022690183,0.000029617142,0.96547204,0.000037381644,0.00000691801,0.000042561143,0.0005669567,0.0025593597,0.000029453118,0.00009663347,0.001139096,0.029793076],"study_design_scores_gemma":[0.00076364016,0.00033549248,0.9728612,0.000025367346,0.0000018432065,0.0000044015023,0.00034944326,0.01326268,0.00044544044,0.002962993,0.00889125,0.000096271],"about_ca_topic_score_codex":0.001879984,"about_ca_topic_score_gemma":0.006674894,"teacher_disagreement_score":0.029696805,"about_ca_system_score_codex":0.000010708034,"about_ca_system_score_gemma":0.00003666064,"threshold_uncertainty_score":0.998896},"labels":[],"label_agreement":null},{"id":"W4387575155","doi":"10.1111/bre.12824","title":"Late <scp>Permian‐Early</scp> Triassic intracontinental tectonic inversion in the Junggar Basin, <scp>NW</scp> China: New insights from detrital zircon geochronology and seismic reflection data","year":2023,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University; Geological Survey of Canada; Natural Resources Canada; Saint Mary's University","funders":"National Natural Science Foundation of China","keywords":"Geology; Permian; Paleontology; Provenance; Terrane; Transtension; Rift; Inversion (geology); Tectonics; Zircon; Structural basin; Seismology","score_opus":0.06173294480409336,"score_gpt":0.2937699253505958,"score_spread":0.23203698054650246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387575155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99286544,0.0013574963,0.000020513253,0.0026922303,0.0001777478,0.0003693871,0.00012567877,0.00008121617,0.0023103028],"genre_scores_gemma":[0.99615246,0.0006865514,0.000121096535,0.00020242871,0.00031398912,0.0000048512497,0.0012965398,0.000007466202,0.0012146239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9958442,0.0011056504,0.00039330652,0.00095594325,0.00078894064,0.0009119676],"domain_scores_gemma":[0.9957496,0.0031938413,0.00008569896,0.0006287126,0.00006265268,0.00027947375],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017091546,0.00025654107,0.00041521713,0.0005934054,0.00047187836,0.00024290287,0.001083089,0.00031951332,0.0003893787],"category_scores_gemma":[0.002382936,0.00016551594,0.00008962975,0.002761626,0.0004159807,0.00045823737,0.00039256006,0.0012042692,0.0010463494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015123912,0.00020465258,0.82210505,0.00006470078,0.00018163539,0.00065413426,0.002579773,0.00046804134,0.020680051,0.000042241532,0.052766077,0.100102395],"study_design_scores_gemma":[0.0011982524,0.00045310037,0.94327456,0.00003041464,0.0000393368,0.00001699038,0.00083472155,0.028498977,0.0030407717,0.009073514,0.01346385,0.00007553426],"about_ca_topic_score_codex":0.05369292,"about_ca_topic_score_gemma":0.020068722,"teacher_disagreement_score":0.12116948,"about_ca_system_score_codex":0.000024762952,"about_ca_system_score_gemma":0.0001215358,"threshold_uncertainty_score":0.9997315},"labels":[],"label_agreement":null},{"id":"W4389194937","doi":"10.1111/bre.12830","title":"Stratigraphy, palaeogeography and evolution of the lower Nanaimo Group (Cretaceous), Georgia Basin, Canada","year":2023,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Clastic rock; Conglomerate; Sedimentary depositional environment; Paleontology; Cretaceous; Structural basin; Canyon; Forearc; Geochemistry; Geomorphology; Tectonics","score_opus":0.02482543683176385,"score_gpt":0.2504478844204864,"score_spread":0.22562244758872252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389194937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9881882,0.0013153062,0.0000066635207,0.0013296016,0.00013757824,0.00019092021,0.0001497973,0.00001901946,0.008662923],"genre_scores_gemma":[0.9994028,0.00021110647,0.0000513916,0.000037649486,0.000021919093,0.0000025517472,0.000021418242,0.0000016116811,0.00024953863],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984286,0.00021946202,0.00016709634,0.00017220993,0.0006430859,0.00036953908],"domain_scores_gemma":[0.99913585,0.00038671543,0.00003536382,0.00019440851,0.00015094188,0.00009674179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091359374,0.00007737469,0.00010486559,0.00016828257,0.0004396932,0.000050379578,0.00027069173,0.000055523236,0.0006169159],"category_scores_gemma":[0.0001665527,0.00004702408,0.000043164455,0.0019358804,0.000317654,0.000118401775,0.000036734968,0.00021696503,0.000019641597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018865521,0.000011015304,0.9852381,0.000051556664,0.000010120561,0.0000048583474,0.000036597172,0.00011431497,0.000016532118,0.0009054134,0.007342488,0.0062501854],"study_design_scores_gemma":[0.00007545782,0.000112690715,0.97277945,0.000018528166,0.0000031053207,0.0000034555496,0.00036948157,0.0008970918,0.00003592152,0.004360031,0.021283578,0.00006118273],"about_ca_topic_score_codex":0.5749605,"about_ca_topic_score_gemma":0.7938216,"teacher_disagreement_score":0.21886106,"about_ca_system_score_codex":0.0000059686645,"about_ca_system_score_gemma":0.00034398047,"threshold_uncertainty_score":0.6754796},"labels":[],"label_agreement":null},{"id":"W4390698167","doi":"10.1111/bre.12840","title":"An exploratory study of “large‐ <i>n</i> ” detrital zircon geochronology of the Book Cliffs, <scp>UT</scp> via rapid (3 s/analysis) <scp>U–Pb</scp> dating","year":2024,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Zircon; Geochronology; Provenance; Geology; Unconformity; Sedimentary depositional environment; Transect; Grain size; Paleontology; Mineralogy; Geochemistry; Sedimentary rock; Geomorphology","score_opus":0.03975114578980075,"score_gpt":0.3041846698917394,"score_spread":0.26443352410193866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390698167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98986304,0.005267778,0.00025106795,0.00015942186,0.00013101182,0.0004139481,0.00016951333,0.000053832548,0.0036903622],"genre_scores_gemma":[0.99858344,0.00016278539,0.0001857648,0.000117467105,0.00013892226,0.00001261997,0.00015737426,0.000008150385,0.00063346134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9942804,0.0017957683,0.0007510235,0.0008423172,0.0013699122,0.0009605636],"domain_scores_gemma":[0.9947935,0.003546998,0.00015874051,0.0008605081,0.00035645082,0.0002838556],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00369046,0.00026088223,0.00068122393,0.00067035615,0.00036336062,0.00010746839,0.0012261455,0.00021305306,0.0025486678],"category_scores_gemma":[0.001340755,0.00016668793,0.00037895486,0.004148886,0.00059297116,0.0003519025,0.00026013452,0.00092302775,0.000222987],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022357748,0.001275693,0.94135875,0.00020591741,0.0013414653,0.00011531056,0.0030349123,0.0019317656,0.032594167,0.000101022815,0.007580553,0.010438091],"study_design_scores_gemma":[0.0015285119,0.004607058,0.74485207,0.00012165099,0.0015294154,0.00002199717,0.04146148,0.0532311,0.11174778,0.0062817377,0.034337964,0.00027925035],"about_ca_topic_score_codex":0.0025730531,"about_ca_topic_score_gemma":0.0070745596,"teacher_disagreement_score":0.1965067,"about_ca_system_score_codex":0.000014062673,"about_ca_system_score_gemma":0.00016337981,"threshold_uncertainty_score":0.99836314},"labels":[],"label_agreement":null},{"id":"W4391032602","doi":"10.1111/bre.12841","title":"Rift segmentation caused by reactivation of multiple basement structure systems: Evidence from the Hailar‐Tamtsag Rift, northeast Asia","year":2024,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Minnow Environmental (Canada)","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Rift; Geology; Basement; Seismology; Segmentation; Fault (geology); Half-graben; Paleontology; Tectonics; Geography; Artificial intelligence","score_opus":0.07026883296117574,"score_gpt":0.31666076146664957,"score_spread":0.2463919285054738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391032602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9826091,0.013329837,0.00016520056,0.0014165483,0.0003315758,0.00064318016,0.0009716623,0.000040214265,0.0004927155],"genre_scores_gemma":[0.9986398,0.00048091973,0.0000937038,0.000025488418,0.00015269165,0.0000105659265,0.000304231,0.0000060645825,0.00028649883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974683,0.0005433837,0.0002745356,0.0003573039,0.0010355647,0.00032089185],"domain_scores_gemma":[0.996513,0.0029007797,0.000056769088,0.00030266287,0.00016276,0.00006400926],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012304534,0.0001271769,0.00016076183,0.000098262804,0.00032764598,0.00019219884,0.00025638175,0.00006869265,0.00088510686],"category_scores_gemma":[0.00033742926,0.00008011821,0.00004706438,0.000551199,0.00015752703,0.0003011807,0.000029586447,0.000355916,0.000095605756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009123473,0.000022003893,0.9210682,0.00015838213,0.00014810257,0.000016458975,0.0020268825,0.00032630708,0.00837135,0.000048502217,0.02507533,0.042647254],"study_design_scores_gemma":[0.00021790965,0.00014975715,0.9685427,0.00048164534,0.000022977343,0.0000020812683,0.0031765723,0.010956254,0.0061980593,0.00009389665,0.0100360485,0.00012210777],"about_ca_topic_score_codex":0.070995316,"about_ca_topic_score_gemma":0.018989312,"teacher_disagreement_score":0.052006003,"about_ca_system_score_codex":0.000020924357,"about_ca_system_score_gemma":0.00015056503,"threshold_uncertainty_score":0.99891156},"labels":[],"label_agreement":null},{"id":"W4393953392","doi":"10.1111/bre.12862","title":"Sequence stratigraphy and palaeogeography of the Upper Jurassic and Lower Cretaceous in the Eastern Barents Sea","year":2024,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Palaeogeography; Cretaceous; Paleontology; Geology; Stratigraphy; Sequence (biology); Sequence stratigraphy; Biology; Structural basin; Tectonics; Sedimentary depositional environment","score_opus":0.08078647610410039,"score_gpt":0.3089289935949132,"score_spread":0.22814251749081282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393953392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879335,0.0063988897,0.0000029120145,0.003212271,0.00006840652,0.00019072104,0.000027937147,0.000004984486,0.00216037],"genre_scores_gemma":[0.9988592,0.0009953945,0.000018294098,0.00006704219,0.00002073569,0.000003354824,0.0000045625607,9.301467e-7,0.000030454921],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988704,0.0002698264,0.00009940074,0.00017523291,0.0003753504,0.00020983737],"domain_scores_gemma":[0.9994875,0.00032714754,0.000009748854,0.00011022833,0.00003145918,0.000033872762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081997225,0.00005945473,0.000071180926,0.000071218004,0.000172713,0.00012226882,0.00015809195,0.000035154488,0.00009990341],"category_scores_gemma":[0.00004784762,0.000026573553,0.000030222498,0.000589491,0.00039861895,0.00008782167,0.000031615666,0.00022434811,0.000010466072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011888481,0.0000070923466,0.978419,0.00002745978,0.00000601298,0.000010126221,0.00036266382,0.000008259367,0.000012998027,0.00012930541,0.00020428495,0.02080093],"study_design_scores_gemma":[0.00004875589,0.00012409932,0.99015415,0.000040800136,0.0000026436,0.0000043715954,0.0007965017,0.003319823,0.000006044567,0.0027300431,0.0027367375,0.00003605096],"about_ca_topic_score_codex":0.002074227,"about_ca_topic_score_gemma":0.0038769047,"teacher_disagreement_score":0.020764878,"about_ca_system_score_codex":9.1432906e-7,"about_ca_system_score_gemma":0.000016669372,"threshold_uncertainty_score":0.31356245},"labels":[],"label_agreement":null},{"id":"W4399706869","doi":"10.1111/bre.12878","title":"Re‐routing of submarine channels by Plio‐Quaternary extensional tectonics along the Tanzania margin and implications for an offshore branch of the East African Rift System","year":2024,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Extensional tectonics; Graben; Paleontology; Rift; Neogene; Tectonics; Seafloor spreading; Passive margin; Extensional fault; Seismology; Horst and graben; Half-graben; Cretaceous; Basement; Structural basin","score_opus":0.06580525415021769,"score_gpt":0.3085787062657979,"score_spread":0.2427734521155802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399706869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903141,0.0019150496,0.00021171273,0.004682806,0.0000808938,0.0005103426,0.00057569175,0.000018637971,0.0016907353],"genre_scores_gemma":[0.99953043,0.000045535795,0.00011959052,0.0000187271,0.000042466192,0.000014475957,0.000061821505,0.0000033382073,0.00016361388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888724,0.00016237775,0.00023413902,0.00018407548,0.00028767297,0.00024449106],"domain_scores_gemma":[0.9987201,0.0007408444,0.00004787426,0.00022602241,0.0002066618,0.000058491045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015918441,0.00007206603,0.0001198042,0.0000700298,0.00039016554,0.00008200348,0.0003462606,0.00004906576,0.00009663432],"category_scores_gemma":[0.0001415987,0.00003640381,0.000039397517,0.00056554395,0.00025489205,0.00011732391,0.000058402777,0.00017914343,0.0000038876733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023132394,0.0000989774,0.87126607,0.0017494119,0.00008097543,0.0000023879536,0.002562475,0.0010305778,0.0015013904,0.01859189,0.0061780186,0.09670653],"study_design_scores_gemma":[0.0001425338,0.0002955202,0.9103718,0.00022009363,0.00001540482,0.000036400943,0.002820132,0.07778089,0.00059864484,0.003072458,0.0045432653,0.00010285096],"about_ca_topic_score_codex":0.0017801829,"about_ca_topic_score_gemma":0.0009020669,"teacher_disagreement_score":0.096603684,"about_ca_system_score_codex":0.000003983256,"about_ca_system_score_gemma":0.00009044285,"threshold_uncertainty_score":0.30008775},"labels":[],"label_agreement":null},{"id":"W4409857930","doi":"10.1111/bre.70027","title":"Characterisation and Architecture of Subsurface Strata in the Whatcom Sub‐Basin, Georgia Basin, Canada and <scp>USA</scp>","year":2025,"lang":"en","type":"article","venue":"Basin Research","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Structural basin; Geology; Architecture; Geochemistry; Geomorphology; Archaeology; Geography","score_opus":0.019308961127521805,"score_gpt":0.26760104830634,"score_spread":0.2482920871788182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409857930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949891,0.00076777325,0.0002990015,0.002035732,0.000048592625,0.00025637547,0.000028889763,0.000015945103,0.0015586193],"genre_scores_gemma":[0.9987778,0.0005872978,0.000054159464,0.00007880371,0.000022828537,0.000020511126,0.000025930327,0.000013546708,0.00041909848],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99826825,0.00038090252,0.00027438,0.000224795,0.0005164757,0.0003351927],"domain_scores_gemma":[0.99881834,0.000642407,0.000025794168,0.00033210294,0.00010544868,0.00007592333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011975936,0.00013633879,0.0002373915,0.00032954867,0.00011293164,0.00012413709,0.00024105469,0.00008189803,0.000015666372],"category_scores_gemma":[0.0002760703,0.00010606935,0.000028384198,0.0009917765,0.00012429238,0.0001212969,0.00006818026,0.00050943537,0.0000016629132],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012871051,0.000355557,0.72615266,0.0031359305,0.00073751167,0.00023315236,0.020058157,0.033871964,0.11297773,0.0029095393,0.04081285,0.058626268],"study_design_scores_gemma":[0.00069003756,0.000043215816,0.9184085,0.0001720407,0.000030103081,0.000007804641,0.0037873015,0.022436732,0.020299578,0.0005055771,0.033481903,0.00013716493],"about_ca_topic_score_codex":0.11335086,"about_ca_topic_score_gemma":0.4979714,"teacher_disagreement_score":0.38462055,"about_ca_system_score_codex":0.00009059262,"about_ca_system_score_gemma":0.00030035936,"threshold_uncertainty_score":0.8925534},"labels":[],"label_agreement":null},{"id":"W7114790075","doi":"10.1111/bre.70079","title":"The Spatial and Temporal Evolution of Mixed Carbonate‐Clastic Mud‐Dominated Basin Fill Successions: The Middle to Late Devonian Shelf Margin, Western Canada","year":2025,"lang":"en","type":"article","venue":"Basin Research","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Imperial Oil (Canada)","funders":"Imperial Oil Limited","keywords":"Sedimentary depositional environment; Marine transgression; Facies; Carbonate; Outcrop; Devonian; Carbonate platform; Clastic rock; Structural basin; Sequence stratigraphy","score_opus":0.027334800297030424,"score_gpt":0.27278185442313646,"score_spread":0.24544705412610604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7114790075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9764331,0.0042809146,0.00003595372,0.006537136,0.000372381,0.00042527282,0.00012556947,0.000009830887,0.011779861],"genre_scores_gemma":[0.9990356,0.00004810132,0.00005853586,0.00004302661,0.000029285407,0.000008432241,0.000008664763,0.0000010582802,0.000767271],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976299,0.00085514947,0.00026463525,0.00026611975,0.0004887485,0.000495449],"domain_scores_gemma":[0.99780315,0.0015692769,0.00005059303,0.0002741967,0.00016735114,0.00013544467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015783489,0.000121481615,0.0001796318,0.00015846716,0.00092088996,0.00007749704,0.00046440342,0.0000928562,0.000052312218],"category_scores_gemma":[0.00045270275,0.00007018896,0.000034377048,0.00064495107,0.0005258054,0.00007056239,0.000015860502,0.00036314043,0.0000030602582],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026446977,0.000011074714,0.95360506,0.000029986712,0.000030515946,0.000018550454,0.00012009023,0.00003026061,0.000039024802,0.00011664769,0.0021312097,0.04360314],"study_design_scores_gemma":[0.00024907265,0.000092533235,0.99194455,0.00008200696,0.00000838371,0.0000034110492,0.00040196325,0.002632328,0.00012971378,0.0004686579,0.0039100805,0.000077309945],"about_ca_topic_score_codex":0.8244552,"about_ca_topic_score_gemma":0.98603296,"teacher_disagreement_score":0.16157778,"about_ca_system_score_codex":0.000021593147,"about_ca_system_score_gemma":0.0010151446,"threshold_uncertainty_score":0.7082834},"labels":[],"label_agreement":null},{"id":"W7114925935","doi":"10.1111/bre.70080","title":"Depositional Characteristics of a Tectonically Controlled Washover Fan Succession in a Semi‐Enclosed Seaway: A Case Study in the Xihu Depression, East China Sea Shelf Basin","year":2025,"lang":"en","type":"article","venue":"Basin Research","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"China Scholarship Council; Simon Fraser University; China National Offshore Oil Corporation; National Natural Science Foundation of China","keywords":"Sedimentary depositional environment; Paleocurrent; Provenance; Structural basin; Barrier island; Turbidite; Sedimentary rock; Facies; Evaporite; Marine transgression","score_opus":0.031550518554196,"score_gpt":0.3266718013760475,"score_spread":0.2951212828218515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7114925935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99335074,0.00020000438,0.000051977055,0.0010799536,0.000042688072,0.0011690645,0.00008453212,0.000011149131,0.0040099053],"genre_scores_gemma":[0.9995237,0.00003031375,0.00010226459,0.00011204341,0.000021854756,0.000047265443,0.00006461545,0.0000023196487,0.00009559552],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99682796,0.0011384088,0.000572931,0.00029868478,0.00074259256,0.00041943998],"domain_scores_gemma":[0.99784404,0.0015023629,0.00008005709,0.00027221176,0.00022503933,0.0000762841],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0035528217,0.00014004669,0.0003698953,0.00042400853,0.00034446962,0.00012930536,0.00045470832,0.00011276151,0.00078116567],"category_scores_gemma":[0.0010536903,0.00008036733,0.000059657687,0.001525223,0.00016281079,0.00019692192,0.00007254349,0.00062321365,0.000016620008],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00080260995,0.0005157117,0.9892592,0.00007019709,0.00001274207,0.0006377908,0.0008655452,0.00013205758,0.000029653203,0.00004906779,0.00010379619,0.0075216554],"study_design_scores_gemma":[0.002418689,0.00024657176,0.98609334,0.00013694123,0.000008879531,0.00010101705,0.0024339573,0.0078552505,0.00002777681,0.00049902446,0.00009072163,0.00008780859],"about_ca_topic_score_codex":0.014188021,"about_ca_topic_score_gemma":0.015423167,"teacher_disagreement_score":0.0077231936,"about_ca_system_score_codex":0.000014473508,"about_ca_system_score_gemma":0.0003436539,"threshold_uncertainty_score":0.99237657},"labels":[],"label_agreement":null}]}