{"meta":{"query_hash":"670bdb744788","filters":{"venue":"Sedimentary basins of the world"},"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/670bdb744788","api":"https://metacan.xera.ac/api/v1/cohort?venue=Sedimentary+basins+of+the+world"},"results":[{"id":"W1521097560","doi":"10.1016/s1874-5997(08)00006-3","title":"Chapter 6 The Maritimes Basin of Atlantic Canada: Basin Creation and Destruction in the Collisional Zone of Pangea","year":2008,"lang":"en","type":"book-chapter","venue":"Sedimentary basins of the world","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"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":"Geology; Thermal subsidence; Structural basin; Paleontology; Terrane; Rift; Canada Basin; Pull apart basin; Thermochronology; Oceanic crust; Geomorphology; Subduction; Tectonics; Sedimentary basin","score_opus":0.008894857235429559,"score_gpt":0.1696579337999209,"score_spread":0.16076307656449132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1521097560","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":[0.91353726,0.0019970923,0.0000013203033,0.0098727485,0.00020440029,0.00048486318,0.0010008492,0.0000047009944,0.072896786],"genre_scores_gemma":[0.9915275,0.0004099646,0.00013102617,0.00062724,0.000058288,8.5135747e-7,0.0002102975,0.0000034216307,0.007031414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986254,0.00007808286,0.00042576148,0.00020136287,0.00052698684,0.0001423852],"domain_scores_gemma":[0.9988812,0.00045538862,0.00031254106,0.0002642761,0.000051246367,0.000035301036],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024254392,0.00018523305,0.00036594114,0.00009069024,0.00010826809,0.0000056739004,0.00035715947,0.00006545372,0.0032973501],"category_scores_gemma":[0.000017935474,0.00008791732,0.00014138999,0.00014114213,0.0005307335,0.00004437959,0.000045377663,0.00023064937,0.0000018355869],"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":[0.00039505895,0.00007988768,0.9719248,0.0001318249,0.00036817693,0.00001949802,0.00024292992,0.0007997282,0.000091733185,0.004043726,0.009767242,0.01213539],"study_design_scores_gemma":[0.0002830734,0.000092764174,0.953088,0.00021052055,0.0002628195,0.00003423041,0.00008493162,0.0003414601,0.0005194649,0.006810592,0.03808803,0.00018412924],"about_ca_topic_score_codex":0.5512482,"about_ca_topic_score_gemma":0.86203647,"teacher_disagreement_score":0.31078827,"about_ca_system_score_codex":0.000010691363,"about_ca_system_score_gemma":0.000075006996,"threshold_uncertainty_score":0.9976138},"labels":[],"label_agreement":null},{"id":"W1558361082","doi":"10.1016/s1874-5997(08)00016-6","title":"Chapter 16 Geology of the Late Cretaceous to Cenozoic Beaufort-Mackenzie Basin, Canada","year":2008,"lang":"en","type":"book-chapter","venue":"Sedimentary basins of the world","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":8,"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":"Geology; Paleontology; Cretaceous; Structural basin; Passive margin; Unconformity; Canada Basin; Rift; Continental margin; Thermal subsidence; Tectonics; Subsidence; Geomorphology","score_opus":0.014762041507469648,"score_gpt":0.17992403757643302,"score_spread":0.16516199606896337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1558361082","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16865934,0.0072801346,0.0000035666585,0.049626306,0.0069273603,0.002135148,0.0037869348,0.00004586837,0.76153535],"genre_scores_gemma":[0.70788205,0.00095716317,0.0001208967,0.012800158,0.00030213155,0.0000028001261,0.00030954264,0.000022464592,0.2776028],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99825996,0.000043544645,0.00049681077,0.00030392432,0.00053976785,0.00035599765],"domain_scores_gemma":[0.99874526,0.00012764435,0.0003825626,0.0005580994,0.00007597854,0.000110453584],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001227247,0.00033092836,0.0005027903,0.00005932656,0.0003279637,0.000006129024,0.00073254487,0.000101613325,0.0060900473],"category_scores_gemma":[0.000016421418,0.00018482193,0.00024109358,0.00010873824,0.00036046575,0.000048549613,0.0001944085,0.0003214912,0.00004538188],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008522641,0.00009147256,0.30349082,0.00020245902,0.0014935087,0.00008655022,0.00088258117,0.0201392,0.000027126856,0.0035686714,0.62948376,0.039681587],"study_design_scores_gemma":[0.00018964795,0.00015463127,0.06496449,0.000097151045,0.00009883505,0.0000109877,0.00003775853,0.00003390404,0.00020236414,0.0014240029,0.93251497,0.00027127008],"about_ca_topic_score_codex":0.4065535,"about_ca_topic_score_gemma":0.962003,"teacher_disagreement_score":0.5554495,"about_ca_system_score_codex":0.000043958138,"about_ca_system_score_gemma":0.00013564568,"threshold_uncertainty_score":0.9948185},"labels":[],"label_agreement":null},{"id":"W1607305776","doi":"10.1016/s1874-5997(08)00003-8","title":"Chapter 3 Appalachian Foreland Basin of Canada","year":2008,"lang":"en","type":"book-chapter","venue":"Sedimentary basins of the world","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":44,"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":"Laurentia; Ordovician; Geology; Paleontology; Foreland basin; Diachronous; Orogeny; Rodinia; Trilobite; Passive margin; Rift; Continental margin; Paleozoic; Devonian; Baltica; Tectonics","score_opus":0.007872751757132295,"score_gpt":0.15368183489264153,"score_spread":0.14580908313550925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607305776","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.043158732,0.001475972,5.4575355e-7,0.0034763552,0.00045264236,0.00023555387,0.0017774799,0.000011424144,0.9494113],"genre_scores_gemma":[0.6946268,0.00015902241,0.00020799563,0.001790276,0.0001404117,4.0554153e-7,0.0003155464,0.000008916111,0.3027506],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984131,0.00001534091,0.00045615307,0.00029201328,0.0005615911,0.00026180837],"domain_scores_gemma":[0.9989421,0.00012334636,0.00033888884,0.00041478162,0.000046716763,0.00013416338],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000919739,0.0002858324,0.0005248696,0.000096659365,0.00011680064,0.000003401535,0.0005389232,0.00008520725,0.031872254],"category_scores_gemma":[0.0000087551725,0.00017293304,0.00034052695,0.00008551673,0.0003293677,0.000033070584,0.00006571166,0.00030805566,0.000022622047],"study_design_candidate":"not_applicable","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":[0.00043521516,0.00009891119,0.7992508,0.00026231655,0.0017203924,0.000108146436,0.00013032468,0.002113346,0.000051916755,0.007201939,0.17306967,0.0155570125],"study_design_scores_gemma":[0.0005154423,0.00016162408,0.15390202,0.00030059062,0.00046986953,0.000024900006,0.000018712017,0.0002865406,0.002029129,0.028258268,0.81332433,0.00070856937],"about_ca_topic_score_codex":0.38965106,"about_ca_topic_score_gemma":0.9383511,"teacher_disagreement_score":0.6514681,"about_ca_system_score_codex":0.000011936212,"about_ca_system_score_gemma":0.00012111142,"threshold_uncertainty_score":0.96901274},"labels":[],"label_agreement":null}]}