{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":4,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":4,"direct_label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline (scores rank; they never assert a category)","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12","author_layer_release":"2026-06-26"},"query_hash":"09267ab85194","filters":{"venue":"Journal of Geological Research"}},"results":[{"id":"W1975903104","doi":"10.1155/2012/327037","title":"A Fast Interpretation Method for Inverse Modeling of Residual Gravity Anomalies Caused by Simple Geometry","year":2012,"lang":"en","type":"article","venue":"Journal of Geological Research","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Faculty of Science, Cairo University; Cairo University","keywords":"Residual; Gravity anomaly; Anomaly (physics); Geometry; Inversion (geology); Cylinder; Amplitude; Inverse; Nonlinear system; Interpretation (philosophy); Geology; Mathematical analysis; Free-air gravity anomaly; Mathematics; Inverse problem; Simple (philosophy); Geodesy; Physics; Bouguer anomaly; Optics; Seismology; Algorithm; Computer science","authors":[{"name":"Khalid S. Essa","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.1108920994972042,"gpt":0.4014524883868048,"spread":0.2905603888896006,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006681012,0.0001026331,0.0003770663,0.0002389397,0.0001300361,0.00002749812,0.0003048635,0.0001321764,0.0003928953],"category_scores_gemma":[0.00466116,0.00006439334,0.0001524566,0.0006017266,0.0001443842,0.0002668029,0.00003841226,0.000577386,0.00001317238],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001040292,"about_ca_system_score_gemma":0.00006196798,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0004899483,"about_ca_topic_score_gemma":0.00005209802,"domain_scores_codex":[0.9970223,0.001047838,0.0004861013,0.0001433915,0.0007136927,0.0005866967],"domain_scores_gemma":[0.9950986,0.003771706,0.0001788806,0.0001003899,0.0005382987,0.0003121597],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.004277268,0.0008326011,0.2481997,0.0002378574,0.0002329982,0.00001836646,0.001132975,0.03984362,0.01032937,0.001083613,0.005881866,0.6879297],"study_design_scores_gemma":[0.001203669,0.006083109,0.2368197,0.0000430938,0.00006751203,0.00003047492,0.0009926019,0.6228281,0.005387105,0.1243027,0.00194111,0.0003008368],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9032867,0.0005526928,0.09517661,0.0004291793,0.00008078655,0.0001452075,0.00004297635,0.000004848883,0.000280985],"genre_scores_gemma":[0.9635282,0.00004013974,0.03603797,0.0000689263,0.0002118728,0.000001333073,0.00001526423,0.000002396758,0.00009392279],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6876289,"threshold_uncertainty_score":0.558018,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2000557059","doi":"10.1155/2012/879393","title":"Gas Hydrate Formation and Dissipation Histories in the Northern Margin of Canada: Beaufort-Mackenzie and the Sverdrup Basins","year":2012,"lang":"en","type":"article","venue":"Journal of Geological Research","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Permafrost; Interglacial; Glacial period; Arctic; Oceanography; Post-glacial rebound; Physical geography; Holocene; Arctic ice pack; Continental margin; Climatology; Geomorphology; Paleontology; Tectonics","authors":[{"name":"Jacek Majorowicz","is_ca":true},{"name":"Jan Šаfanda","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0352729273233818,"gpt":0.2790718438119848,"spread":0.243798916488603,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004615808,0.00005191642,0.0001237854,0.00003295256,0.0001490734,0.00001486108,0.0001577379,0.00004260144,0.0001473048],"category_scores_gemma":[0.0004250913,0.00002129773,0.00001928479,0.0001865917,0.0004646415,0.0001970441,0.00009611525,0.0003804342,0.000001009104],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000137797,"about_ca_system_score_gemma":0.00003556242,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01753141,"about_ca_topic_score_gemma":0.06669634,"domain_scores_codex":[0.9983745,0.0005033354,0.0002655781,0.00005226302,0.0005743121,0.0002300402],"domain_scores_gemma":[0.999094,0.0005776171,0.0001405997,0.00007580051,0.00003362829,0.00007834491],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001284579,0.0002323462,0.9510866,0.00005108555,0.00003608579,0.00003284432,0.0185999,0.001225021,0.001418826,0.004293145,0.00266528,0.01907431],"study_design_scores_gemma":[0.001217782,0.0003960698,0.9676256,0.00002898853,0.00001961942,0.0001033747,0.003024029,0.002959549,0.0002616554,0.009641746,0.01462659,0.00009496557],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.991594,0.0009862605,0.00002476059,0.004632829,0.00003823281,0.0001313688,0.000001501391,5.298929e-7,0.002590475],"genre_scores_gemma":[0.9993329,0.0004192322,0.00004486891,0.0000545485,0.00002988563,0.000002995988,7.835595e-7,0.000001885116,0.0001129226],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04916492,"threshold_uncertainty_score":0.9890109,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2064067666","doi":"10.1155/2013/815841","title":"Estimating Pore Space Hydrate Saturation Using Dissociation Gas Evolution Measurements: In Relevance to Laboratory Testing of Natural or Artificially Synthesised Hydrate-Bearing Soil Specimens","year":2013,"lang":"en","type":"article","venue":"Journal of Geological Research","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Hydrate; Saturation (graph theory); Clathrate hydrate; Characterisation of pore space in soil; Dissociation (chemistry); Natural gas; Mineralogy; Computer science; Soil science; Thermodynamics; Materials science; Environmental science; Chemistry; Geology; Geotechnical engineering; Mathematics; Porosity; Physics; Physical chemistry","authors":[{"name":"Anuruddhika G. Jayasinghe","is_ca":true},{"name":"J LH Grozic","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.1073707308605324,"gpt":0.3374551288934731,"spread":0.2300843980329407,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.004739525,0.0001474046,0.0003233019,0.0002242632,0.0002132385,0.00007614148,0.0002740035,0.0001414451,0.0003704797],"category_scores_gemma":[0.009558575,0.0001008074,0.00005112115,0.001474107,0.0001592153,0.0005637287,0.0001744385,0.0008159781,0.00005327565],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0009978765,"about_ca_system_score_gemma":0.0001319549,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0004759179,"about_ca_topic_score_gemma":0.0001461868,"domain_scores_codex":[0.996388,0.0007185229,0.0008198927,0.0002656448,0.001282152,0.0005257887],"domain_scores_gemma":[0.9977894,0.0008703275,0.0005580359,0.0001490186,0.0004574232,0.0001758109],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0001733622,0.0001069483,0.03565523,0.00001773295,0.00001441769,0.00002081649,0.0003138703,0.2120228,0.7487876,0.00001862029,0.00004056566,0.002827989],"study_design_scores_gemma":[0.0009176558,0.001154037,0.3739488,0.001017145,0.000035131,0.0000351738,0.0009707657,0.5471537,0.06687285,0.007423777,0.00003533491,0.0004356819],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9974764,0.0001047917,0.0006602159,0.0006329581,0.0001465867,0.0003553791,9.10231e-7,0.000008803254,0.000613984],"genre_scores_gemma":[0.9756932,0.000009881138,0.02403801,0.00002247777,0.0001153682,0.000005743109,7.977754e-7,0.0000120292,0.0001025283],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6819148,"threshold_uncertainty_score":0.9987843,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2154283496","doi":"10.1155/2012/369513","title":"The Dabie Extensional Tectonic System: Structural Framework","year":2012,"lang":"en","type":"article","venue":"Journal of Geological Research","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Chinese Academy of Sciences; Institute of Geology and Geophysics, Chinese Academy of Sciences; University of Science and Technology of China; University of British Columbia; National Natural Science Foundation of China","keywords":"Geology; Mylonite; Extensional definition; Shearing (physics); Extensional tectonics; Shear zone; Shear (geology); Metamorphic rock; Seismology; Tectonics; Metamorphic core complex; Petrology; Extensional fault; Geochemistry; Geotechnical engineering","authors":[{"name":"Quanlin Hou","is_ca":false},{"name":"Hongyuan Zhang","is_ca":false},{"name":"Qing Liu","is_ca":false},{"name":"Jun Li","is_ca":false},{"name":"Yudong Wu","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.06839202406231146,"gpt":0.3316959319801288,"spread":0.2633039079178173,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004600082,0.0001172095,0.0002809612,0.00008971101,0.0007364347,0.0000849403,0.0007126501,0.0001630911,0.007658241],"category_scores_gemma":[0.003942579,0.00004608997,0.0002222063,0.0005738102,0.0006344203,0.0001538663,0.00008943049,0.001442711,0.0004420291],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001564883,"about_ca_system_score_gemma":0.00005535157,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001863054,"about_ca_topic_score_gemma":0.00005780219,"domain_scores_codex":[0.9965333,0.0006283717,0.0004696752,0.0001430914,0.001330908,0.0008946037],"domain_scores_gemma":[0.994266,0.0043812,0.0001576557,0.0001869017,0.0005156529,0.000492588],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002714791,0.0000310874,0.9727142,0.00001131786,0.00006370575,0.00007207519,0.00003497685,0.0003510287,0.0001241325,0.008207594,0.00092591,0.0171925],"study_design_scores_gemma":[0.0001065823,0.0003462364,0.92501,0.00002396673,0.00001733394,0.000327349,0.0003640956,0.001292354,0.00006311541,0.06769761,0.004664527,0.00008685257],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9853661,0.00717804,0.00006022194,0.002965162,0.0003325186,0.00006544818,0.00000341415,0.00001088211,0.004018207],"genre_scores_gemma":[0.9976686,0.00018998,0.001058132,0.0001009864,0.0008159769,5.611889e-7,0.000002672226,0.000001363663,0.0001617435],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05949002,"threshold_uncertainty_score":0.9932489,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}