{"meta":{"query_hash":"2d68d1404727","filters":{"venue":"SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS eBooks"},"cohort_total":3,"direct_labels_cover":0,"predictions_cover":3,"exported":3,"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/2d68d1404727","api":"https://metacan.xera.ac/api/v1/cohort?venue=SOCIETY+OF+ECONOMIC+PALEONTOLOGISTS+AND+MINERALOGISTS+eBooks"},"results":[{"id":"W2484306789","doi":"10.5724/gcs.03.23.0647","title":"Seismic and Sequence Stratigraphy of a Braided Fluvial Sheet, Lower Cretaceous Missisauga Formation, Offshore Nova Scotia, Canada: Implications for Deep-Water Exploration","year":2003,"lang":"en","type":"book-chapter","venue":"SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS eBooks","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nova scotia; Geology; Cretaceous; Fluvial; Paleontology; Sequence (biology); Submarine pipeline; Sequence stratigraphy; Stratigraphy; Oceanography; Tectonics; Structural basin; Facies","score_opus":0.04631399269857681,"score_gpt":0.23360241504500626,"score_spread":0.18728842234642945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2484306789","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":[0.4558014,0.01647983,0.014063325,0.0074399495,0.0014960861,0.0057636434,0.010347085,0.00015025065,0.48845845],"genre_scores_gemma":[0.99149036,0.00062882184,0.002617074,0.00041278487,0.000053156196,0.000009475883,0.0008527001,0.000008201739,0.0039274413],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99846274,0.000020109006,0.0007602214,0.00038053456,0.00008384839,0.00029254364],"domain_scores_gemma":[0.9988566,0.00015556176,0.0004921473,0.0002226789,0.00015265138,0.00012034901],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00022169,0.0003313942,0.00057189807,0.000060138616,0.00017703518,0.00004511787,0.00017282815,0.00031623643,0.00014998611],"category_scores_gemma":[0.000016595535,0.00025680964,0.00018253548,0.00001320321,0.0006658516,0.00023201387,0.0000145881095,0.00014622259,0.0000014272508],"study_design_candidate":"theoretical_or_conceptual","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":[0.0018589846,0.0003035216,0.24031025,0.020934695,0.0052546198,0.000027310794,0.021554047,0.025753682,0.0035894902,0.25850445,0.115735866,0.3061731],"study_design_scores_gemma":[0.007759797,0.004386263,0.11292418,0.00094293396,0.0016513747,0.00071857864,0.0030951104,0.059341975,0.0012613594,0.59799194,0.2031671,0.0067593907],"about_ca_topic_score_codex":0.039470904,"about_ca_topic_score_gemma":0.8301802,"teacher_disagreement_score":0.7907093,"about_ca_system_score_codex":0.000018433244,"about_ca_system_score_gemma":0.00022930649,"threshold_uncertainty_score":0.99998844},"labels":[],"label_agreement":null},{"id":"W2490516367","doi":"10.5724/gcs.05.25.0203","title":"A Review of Tectonic Events on the Passive Margin of Eastern North America","year":2005,"lang":"en","type":"review","venue":"SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS eBooks","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":44,"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; Diachronous; Paleontology; Tectonics; Cretaceous; Margin (machine learning); Passive margin; Seafloor spreading; Breakup; Seismology","score_opus":0.052052964266158616,"score_gpt":0.27993214911779024,"score_spread":0.2278791848516316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2490516367","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000733501,0.9866746,0.000006106037,0.00014118734,0.0000729346,0.0006237211,0.00055241043,0.000009006461,0.011186545],"genre_scores_gemma":[0.00542582,0.9934934,0.00023791808,0.00030563964,0.0000436027,0.00001693154,0.00017277531,0.00000419933,0.00029970563],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981346,0.00014402326,0.0010413369,0.0003152754,0.00010570639,0.00025905788],"domain_scores_gemma":[0.99743706,0.00054397143,0.0015417914,0.0003528422,0.000058004975,0.00006631517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030584369,0.00034403006,0.0016182152,0.000045278495,0.00007491942,0.000008313551,0.00047663142,0.00018541988,0.00042962644],"category_scores_gemma":[0.00005979165,0.00018929895,0.00066139485,0.00006957789,0.0007329177,0.000043231812,0.00003592888,0.00024228155,0.000022715907],"study_design_candidate":"not_applicable","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":[0.0000064274973,0.000016572889,0.0016140154,0.027577052,0.00016940013,3.8447357e-7,0.000081482765,0.000013607834,2.3221876e-8,0.00010310802,0.0009382864,0.9694796],"study_design_scores_gemma":[0.00018718773,0.0003755419,0.0032608071,0.016873863,0.00035451658,0.000017395996,0.0000801599,0.00012224828,3.0044825e-7,0.00018847654,0.97818667,0.00035286174],"about_ca_topic_score_codex":0.0008868566,"about_ca_topic_score_gemma":0.0025852825,"teacher_disagreement_score":0.9772484,"about_ca_system_score_codex":0.000009778752,"about_ca_system_score_gemma":0.00017652543,"threshold_uncertainty_score":0.77193874},"labels":[],"label_agreement":null},{"id":"W2496191451","doi":"10.5724/gcs.04.24.0502","title":"A Comparison of Salt Tectonic Subprovinces Beneath the Scotian Slope and Laurentian Fan","year":2004,"lang":"en","type":"book-chapter","venue":"SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS eBooks","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":51,"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; Tectonics; Salt tectonics; Paleontology; Geomorphology","score_opus":0.03612801621689252,"score_gpt":0.2708577670640818,"score_spread":0.2347297508471893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2496191451","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":[0.39451617,0.028901363,0.000015228641,0.0009580562,0.00048038905,0.0009520263,0.0004435504,0.000048236456,0.573685],"genre_scores_gemma":[0.98292696,0.0017966618,0.000350099,0.00008253712,0.00006560951,0.0000025139552,0.00012998558,0.00000888014,0.0146367615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980378,0.000068721754,0.00071579515,0.0005929114,0.00013295158,0.00045179168],"domain_scores_gemma":[0.9983778,0.00038712224,0.0006563953,0.0003949222,0.000049801714,0.00013397147],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00052190846,0.00041735466,0.0010628591,0.0000799928,0.00025689497,0.000035792964,0.0004505034,0.00066567824,0.00050096074],"category_scores_gemma":[0.000015616617,0.00029530318,0.0002802487,0.000012777639,0.0047145532,0.000052738356,0.00007069204,0.0005944543,0.000013161835],"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":[0.000067187335,0.000011321896,0.97347814,0.00036220413,0.00032302414,0.0000061203373,0.0012887033,0.000047611135,0.000009535515,0.019234316,0.00039815973,0.004773677],"study_design_scores_gemma":[0.0035748621,0.0024046483,0.87362826,0.0007165565,0.00075695704,0.00037491752,0.0015497296,0.0015900399,0.00017847113,0.09510775,0.018105563,0.0020122512],"about_ca_topic_score_codex":0.0035001659,"about_ca_topic_score_gemma":0.26544833,"teacher_disagreement_score":0.5884108,"about_ca_system_score_codex":0.000007464114,"about_ca_system_score_gemma":0.00027579468,"threshold_uncertainty_score":0.99994993},"labels":[],"label_agreement":null}]}