{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":598,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":598,"direct_label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline (scores rank; they never assert a category)","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"query_hash":"bf26f243c413","filters":{"venue":"Geophysical Journal International"}},"results":[{"id":"W2022712506","doi":"10.1093/gji/ggs030","title":"Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":618,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Post-glacial rebound; Geology; Deglaciation; Geodesy; Viscoelasticity; Viscosity; Altimeter; Ice sheet; Sea level; Glacial period; Geomorphology; Oceanography; Physics; Thermodynamics","retraction":null,"screen_n_in":null,"score":{"opus":0.01414752231894246,"gpt":0.24875584634419,"spread":0.2346083240252476,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002486018,0.00006830013,0.0001175087,0.00005101575,0.00005744176,0.00001759494,0.0001842883,0.00001252631,0.00003910829],"category_scores_gemma":[0.00005465441,0.00005201425,0.00002459068,0.0001531625,0.00002911495,0.0001383596,0.00002434123,0.00009988357,0.000006170009],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001830768,"about_ca_system_score_gemma":0.000132764,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1016735,"about_ca_topic_score_gemma":0.09441894,"domain_scores_codex":[0.9989516,0.0001123965,0.0002247396,0.00008957119,0.0004703003,0.0001513809],"domain_scores_gemma":[0.9993846,0.0001456332,0.0001032946,0.00007542347,0.000115937,0.0001750469],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0008217129,0.0003872466,0.8742684,0.00001949682,0.00006317359,0.000001848052,0.00168208,0.09227169,0.02026504,0.0006018399,0.0002118292,0.009405632],"study_design_scores_gemma":[0.0002035743,0.0001122362,0.9899765,0.00003799379,0.000007688888,0.000005792162,0.0001098872,0.008221443,0.0007470237,0.00037501,0.0001477787,0.00005502416],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9977472,0.00001902517,0.000882785,0.0007643893,0.0003226028,0.0001343583,0.00007979558,0.000001238966,0.00004863499],"genre_scores_gemma":[0.9989345,0.000001250571,0.0007537098,0.0001947348,0.0000888475,7.673949e-7,0.000008976764,0.000001881829,0.00001532326],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1157081,"threshold_uncertainty_score":0.9221056,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2109254022","doi":"10.1093/gji/ggu140","title":"The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based on GPS positioning, exposure age dating of ice thicknesses, and relative sea level histories","year":2014,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":562,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Jet Propulsion Laboratory; National Oceanic and Atmospheric Administration; Compute Canada; National Aeronautics and Space Administration; California Institute of Technology; University of Toronto","keywords":"Geology; Deglaciation; Radiocarbon dating; Holocene; Post-glacial rebound; Ice shelf; Last Glacial Maximum; Bay; Glacier; Ice sheet; Sea ice; Peninsula; Oceanography; Physical geography; Climatology; Cryosphere; Geomorphology; Paleontology; Geography; Archaeology","retraction":null,"screen_n_in":null,"score":{"opus":0.02654462529804052,"gpt":0.2623762503393056,"spread":0.235831625041265,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006323534,0.0001037427,0.0001877417,0.0000807036,0.0004494627,0.00004703146,0.0002780975,0.00007691619,0.0001109541],"category_scores_gemma":[0.0003964053,0.00007308166,0.0000693239,0.00007211067,0.0005528794,0.0001849801,0.00002682963,0.0005184518,0.000008995644],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005858607,"about_ca_system_score_gemma":0.00009069047,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001889734,"about_ca_topic_score_gemma":0.0003177359,"domain_scores_codex":[0.9985898,0.0002892805,0.0003010046,0.0001507258,0.0004793788,0.00018981],"domain_scores_gemma":[0.9974819,0.00181953,0.0002485143,0.0001027881,0.0002681675,0.00007904076],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0007902418,0.00007778469,0.9693643,0.00002025948,0.0001140742,0.00002202389,0.0005861149,0.01034045,0.0002930815,0.01710627,0.0001190364,0.001166381],"study_design_scores_gemma":[0.0006855192,0.0005417388,0.6749297,0.00007419423,0.00002983497,0.00008681956,0.0001111506,0.305456,0.0001622656,0.01742366,0.0003819339,0.000117212],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9835059,0.00007523493,0.002576236,0.003385239,0.0004153587,0.00007206846,0.0001029667,0.000006067133,0.009860925],"genre_scores_gemma":[0.9983077,0.00002294779,0.00111171,0.0001373084,0.0001770582,6.516635e-7,0.00008434978,0.000002568228,0.0001556997],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2951156,"threshold_uncertainty_score":0.345695,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2170860899","doi":"10.1111/j.1365-246x.2007.03698.x","title":"Non-parametric seismic data recovery with curvelet frames","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":555,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Curvelet; Seismic inversion; Compressed sensing; Algorithm; Inversion (geology); Computer science; Geophysical imaging; Parametric statistics; Synthetic seismogram; Sampling (signal processing); Data compression; Synthetic data; Geology; Seismology; Artificial intelligence; Mathematics; Computer vision; Wavelet transform","retraction":null,"screen_n_in":null,"score":{"opus":0.02656171050425738,"gpt":0.2412824083118224,"spread":0.214720697807565,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001921284,0.0001279859,0.0001493721,0.0002008454,0.0002146924,0.0001154702,0.0008962845,0.00004327412,0.00108253],"category_scores_gemma":[0.00006802802,0.00009154159,0.00006068188,0.0002461883,0.0001302275,0.0008656594,0.00004768196,0.0004423016,0.0005004946],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001215534,"about_ca_system_score_gemma":0.0001100254,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001221671,"about_ca_topic_score_gemma":0.000005104454,"domain_scores_codex":[0.9987138,0.00003337342,0.0002049217,0.0002513982,0.000570279,0.0002262382],"domain_scores_gemma":[0.9992267,0.0001283342,0.0001356485,0.0002536889,0.0001212043,0.0001343813],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0003289885,0.0001936874,0.1881677,0.00000695353,0.0002680183,0.0006577231,0.0001360015,0.003617724,0.00003369794,0.00004016096,0.5102309,0.2963185],"study_design_scores_gemma":[0.0007890518,0.0005359213,0.2733612,0.00007890756,0.00002805889,0.003551684,0.00008834553,0.539765,0.0004036301,0.00431062,0.1766392,0.0004483133],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9689922,0.0001020139,0.01530163,0.002939398,0.001145228,0.00007356366,0.0001658574,0.00008146148,0.01119866],"genre_scores_gemma":[0.9890825,0.0002638558,0.005687059,0.002804569,0.00076886,3.241911e-7,0.0002433151,0.000005048214,0.001144458],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5361473,"threshold_uncertainty_score":0.9998306,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1981304827","doi":"10.1111/j.1365-246x.2005.02553.x","title":"On post-glacial sea level - II. Numerical formulation and comparative results on spherically symmetric models","year":2005,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":480,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Shore; Sea level; Geology; Post-glacial rebound; Marine transgression; Mathematics; Geodesy; Applied mathematics; Oceanography; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.0740241268431118,"gpt":0.2741825049805768,"spread":0.200158378137465,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001973741,0.0001782097,0.0002003454,0.0001215329,0.0003209031,0.0001545693,0.0002227786,0.00005443402,0.0002339845],"category_scores_gemma":[0.00007521413,0.000139675,0.0001070963,0.0001807014,0.00003603314,0.000473417,0.00002270429,0.0003986105,0.0003109894],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003272567,"about_ca_system_score_gemma":0.00004393217,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002951321,"about_ca_topic_score_gemma":0.00008931968,"domain_scores_codex":[0.9981382,0.00006532323,0.0003244119,0.0002633315,0.0009528278,0.0002558414],"domain_scores_gemma":[0.9990771,0.0001936135,0.0001730818,0.00008804887,0.0002510667,0.0002170435],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.006305996,0.002023996,0.007711905,0.000007826592,0.000494165,0.00006112632,0.001518906,0.2318006,0.0003736892,0.1003096,0.008442259,0.64095],"study_design_scores_gemma":[0.001694278,0.001502255,0.6077299,0.00003424213,0.00001818963,0.00003187626,0.00003248207,0.3542685,0.0001017885,0.031721,0.002581601,0.0002838712],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9676136,0.00001979129,0.001144459,0.002650759,0.00052528,0.0001144224,0.0003859526,0.00001771521,0.02752796],"genre_scores_gemma":[0.9964691,0.000006752285,0.001012411,0.0009663379,0.0009862742,6.85997e-7,0.0001732867,0.000003488067,0.0003816456],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6406661,"threshold_uncertainty_score":0.5695783,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2137972163","doi":"10.1111/j.1365-246x.2004.02276.x","title":"The Source-Scanning Algorithm: mapping the distribution of seismic sources in time and space","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":447,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Seismogram; Waveform; Algorithm; Amplitude; Brightness; A priori and a posteriori; Geology; Episodic tremor and slip; Computer science; Subduction; Seismology; Optics; Telecommunications; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01054358402378899,"gpt":0.2061085287879775,"spread":0.1955649447641885,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003061148,0.00006737814,0.0000870274,0.0000273149,0.0002883736,0.0001023606,0.0002158894,0.00001612429,0.00004032086],"category_scores_gemma":[0.00005452243,0.00003623599,0.00005025169,0.0001030973,0.0001622193,0.0001025347,0.00002765059,0.0002271137,0.00002773231],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009037126,"about_ca_system_score_gemma":0.00002628781,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008928549,"about_ca_topic_score_gemma":0.0001181404,"domain_scores_codex":[0.9992589,0.00003850571,0.0001724964,0.00008115872,0.0002966778,0.0001522468],"domain_scores_gemma":[0.9995272,0.0002422468,0.0001029889,0.00004689999,0.00004670507,0.00003393046],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.00008089244,0.00006809683,0.2160922,0.000005302076,0.0002625305,0.0000367526,0.002919616,0.05461136,0.0001112037,0.001022132,0.0004240388,0.7243659],"study_design_scores_gemma":[0.0003369382,0.00004431147,0.9553062,0.0000498358,0.000006376667,0.00008963724,0.0004616957,0.02981206,0.00006306802,0.008415183,0.005349365,0.00006533947],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9920337,0.0006232002,0.001844255,0.004894685,0.000166851,0.00003923539,0.00001936985,0.000005417055,0.0003732528],"genre_scores_gemma":[0.9991676,0.0001739055,0.0001114176,0.00007154518,0.0002677049,3.507679e-7,0.00001063754,0.000001366703,0.0001954971],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.739214,"threshold_uncertainty_score":0.2217966,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2020219450","doi":"10.1046/j.1365-246x.2003.01766.x","title":"Fast inversion of large-scale magnetic data using wavelet transforms and a logarithmic barrier method","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Image and Signal Denoising Methods","field":"Computer Science","cited_by":425,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Conjugate gradient method; Wavelet; Wavelet transform; Algorithm; Mathematics; Logarithm; Coefficient matrix; Matrix (chemical analysis); Solver; Stationary wavelet transform; Wavelet packet decomposition; Computer science; Mathematical optimization; Mathematical analysis; Artificial intelligence; Eigenvalues and eigenvectors; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.02818622910144782,"gpt":0.3187276320347983,"spread":0.2905414029333505,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009546106,0.0001210071,0.0001943164,0.0001395354,0.0001249736,0.0001678882,0.000883968,0.0000517192,0.00007502652],"category_scores_gemma":[0.00009549021,0.00009966071,0.0000780082,0.0001704274,0.0000570365,0.0009113153,0.0002384309,0.0002927674,0.000005608254],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003200006,"about_ca_system_score_gemma":0.00009241545,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00001584927,"about_ca_topic_score_gemma":0.000001871757,"domain_scores_codex":[0.9984925,0.0002413684,0.0002982796,0.0002829274,0.0004633699,0.0002215275],"domain_scores_gemma":[0.9991572,0.0001301158,0.0001184965,0.0002877579,0.0001752156,0.0001311463],"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":[0.0001992668,0.0008486598,0.000636838,0.00006468715,0.0003082912,0.0003359922,0.004597967,0.0006148599,0.3370153,0.05570566,0.001143071,0.5985293],"study_design_scores_gemma":[0.002019906,0.0001829288,0.001068598,0.00007552919,0.00004206599,0.00105818,0.0001360758,0.9320898,0.01670616,0.04143481,0.004929617,0.0002562984],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"methods","genre_gemma":"methods","genre_scores_codex":[0.05121738,0.00007992516,0.9471185,0.0003344506,0.0004495001,0.00004789955,0.00002492015,0.00001005476,0.0007174281],"genre_scores_gemma":[0.1899157,0.00003217602,0.809163,0.0003683218,0.0001837215,6.193487e-7,0.000006453066,0.000009998805,0.0003199471],"genre_candidate":"methods","genre_consensus":"methods","teacher_disagreement_score":0.931475,"threshold_uncertainty_score":0.4064046,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2064499777","doi":"10.1111/j.1365-246x.2007.03371.x","title":"Fault locking, block rotation and crustal deformation in the Pacific Northwest","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":408,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Subduction; Clockwise; Pacific Plate; Seafloor spreading; Sinistral and dextral; North American Plate; Geodesy; Crust; Basin and Range Province; Shear (geology); Slip (aerodynamics); Shear zone; Fault (geology); Tectonics; Rotation (mathematics); Paleontology; Geometry","retraction":null,"screen_n_in":null,"score":{"opus":0.01048575702719284,"gpt":0.2322396766132462,"spread":0.2217539195860533,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004357374,0.00007447939,0.00007054098,0.00008860807,0.0001695679,0.0001262719,0.0001360042,0.00002721146,0.0001208028],"category_scores_gemma":[0.00004305269,0.00004733586,0.0000397068,0.0001181708,0.00005282037,0.000294016,0.000008006357,0.0002471248,0.00005821701],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007314852,"about_ca_system_score_gemma":0.00001490219,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005434718,"about_ca_topic_score_gemma":0.003618006,"domain_scores_codex":[0.9991332,0.00003289255,0.0002142732,0.0000873114,0.0003632471,0.0001691006],"domain_scores_gemma":[0.999579,0.0001801435,0.0000879203,0.0000420946,0.00006720384,0.00004367948],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006227026,0.00003848082,0.8052082,0.000003136047,0.00003351682,0.00009361134,0.00209332,0.0007098708,0.00001676649,0.0006576896,0.0002181095,0.190865],"study_design_scores_gemma":[0.0002471698,0.0000607802,0.9916245,0.00001114092,0.000004530788,0.0003030781,0.001483135,0.002656982,0.00001174126,0.001590448,0.001943655,0.00006286529],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9894072,0.0001077705,0.0001942713,0.0007284866,0.0003079459,0.00005437922,0.000009944893,0.000006987079,0.00918301],"genre_scores_gemma":[0.9991453,0.00006929095,0.000100143,0.0001906376,0.0004188483,3.657312e-7,0.0000284575,0.00000126407,0.00004564306],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1908021,"threshold_uncertainty_score":0.2018932,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1995637978","doi":"10.1046/j.1365-246x.2003.01942.x","title":"On post-glacial sea level: I. General theory","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":396,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Toronto","funders":"","keywords":"Sea level; Shore; Geology; Post-glacial rebound; Geodesy; Glacial period; Geodetic datum; Climatology; Oceanography; Geomorphology","retraction":null,"screen_n_in":null,"score":{"opus":0.0266955317727427,"gpt":0.2431934141195075,"spread":0.2164978823467648,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003919097,0.000148465,0.000131065,0.0000846232,0.0002122424,0.000173647,0.0003052301,0.00004537102,0.005254588],"category_scores_gemma":[0.0001571079,0.0001163525,0.0001681339,0.00009038113,0.00005102615,0.000216813,0.000008077354,0.0003615577,0.001530637],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001433268,"about_ca_system_score_gemma":0.0000801869,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000141134,"about_ca_topic_score_gemma":0.00006891449,"domain_scores_codex":[0.9983629,0.0001631753,0.0002061863,0.000189755,0.0007926969,0.0002853088],"domain_scores_gemma":[0.9992821,0.0001056251,0.0000999511,0.0001011631,0.0002178166,0.0001933513],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","study_design_scores_codex":[0.001015446,0.0009994662,0.1446351,0.000009571209,0.0007518262,0.0003726982,0.000427607,0.004985617,0.002065938,0.496777,0.01490776,0.333052],"study_design_scores_gemma":[0.000697528,0.0002919575,0.688597,0.00001528958,0.00001606161,0.00009474951,0.00003289413,0.0007725235,0.0004091429,0.3007133,0.008120069,0.0002394303],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9484116,0.00002722941,0.0006116849,0.0005543477,0.002816144,0.00005836514,0.0001916769,0.00001555546,0.04731341],"genre_scores_gemma":[0.99529,0.000005093327,0.000369181,0.001321307,0.001034742,4.449338e-7,0.00007954752,0.000004915985,0.001894716],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.543962,"threshold_uncertainty_score":0.9992468,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2016755848","doi":"10.1111/j.1365-246x.2009.04429.x","title":"Seismic tomography of the southern California crust based on spectral-element and adjoint methods","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":373,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Seismogram; Multitaper; Seismology; Seismic tomography; Tomography; Inversion (geology); Sedimentary basin; Algorithm; Geophysics; Mantle (geology); Mathematics; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01068642268481783,"gpt":0.2527177138205391,"spread":0.2420312911357212,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002884275,0.00008836987,0.0001033135,0.00009435301,0.0001013706,0.00004972832,0.0002398744,0.00002450608,0.0006287158],"category_scores_gemma":[0.00002945466,0.00005330171,0.000132154,0.00009735446,0.00007858725,0.0000547324,0.00000829042,0.000239872,0.00002778022],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007395505,"about_ca_system_score_gemma":0.00002614218,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001979763,"about_ca_topic_score_gemma":0.000001970749,"domain_scores_codex":[0.9991311,0.0001000936,0.0001907941,0.0001135639,0.0003363114,0.0001281688],"domain_scores_gemma":[0.9995853,0.0000742213,0.0001248119,0.00009058505,0.00005597829,0.0000690555],"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":[0.0002951458,0.0003023681,0.08109239,0.000009615352,0.0001066143,0.0000156418,0.000302985,0.008530525,0.001916594,0.0005982573,0.01911358,0.8877163],"study_design_scores_gemma":[0.0005734974,0.0004788319,0.2765773,0.0001133706,0.00002914773,0.00005886111,0.0001627625,0.656675,0.00972392,0.02873531,0.02666961,0.0002023667],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9296655,0.0001053163,0.02788898,0.0319672,0.0009408345,0.0001714329,0.0003172896,0.00005820451,0.008885215],"genre_scores_gemma":[0.9890038,0.00001073163,0.005936712,0.004763563,0.0001898169,1.742149e-7,0.000008180638,0.000001726288,0.00008534455],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8875139,"threshold_uncertainty_score":0.6883997,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2098065241","doi":"10.1111/j.1365-246x.2011.05044.x","title":"Forward and adjoint simulations of seismic wave propagation on fully unstructured hexahedral meshes","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":354,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Canada Research Chairs; University of Toronto","funders":"","keywords":"Polygon mesh; Hexahedron; Finite element method; Domain decomposition methods; Mesh generation; Computational science; Computer science; Wave propagation; Algorithm; Physics; Structural engineering; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.02321338823346787,"gpt":0.2203991270000919,"spread":0.197185738766624,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009919071,0.00009224234,0.0001144271,0.0001244421,0.00009023578,0.00003613999,0.0001249892,0.0000304506,0.000846859],"category_scores_gemma":[0.00004537187,0.00006965208,0.00006605075,0.00006343061,0.00009957592,0.0002708438,0.00001216495,0.0001841325,0.00001957523],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008254056,"about_ca_system_score_gemma":0.0000301627,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0003393262,"about_ca_topic_score_gemma":0.000006350457,"domain_scores_codex":[0.999198,0.00003997342,0.000223836,0.0001251299,0.0002946377,0.0001184053],"domain_scores_gemma":[0.9995202,0.0000565823,0.000150153,0.00006608473,0.0001276336,0.00007931281],"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":[0.001189721,0.0003795157,0.1012154,0.00004456672,0.0004433368,0.000096651,0.004078128,0.006860034,0.00284097,0.01205494,0.008363102,0.8624336],"study_design_scores_gemma":[0.0007097273,0.0006108888,0.4056915,0.00009815754,0.00003527895,0.0002398338,0.000231076,0.4793008,0.01656488,0.09224847,0.004008399,0.000260986],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9879075,0.0000183339,0.003777215,0.0007849441,0.0004957262,0.00007618939,0.00005900196,0.00003005224,0.006850985],"genre_scores_gemma":[0.9962611,0.0000147137,0.002813165,0.0005437832,0.0001959389,2.632594e-7,0.00003338263,0.000002792919,0.0001348352],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8621727,"threshold_uncertainty_score":0.9272512,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2108434249","doi":"10.1111/j.1365-246x.2012.05557.x","title":"A new glacial isostatic adjustment model for Antarctica: calibrated and tested using observations of relative sea-level change and present-day uplift rates","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":348,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Ottawa","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Deglaciation; Post-glacial rebound; Geology; Geodesy; Lithosphere; Last Glacial Maximum; Ice sheet; Sea level; Tectonic uplift; Glacial period; Glacier; Climatology; Geomorphology; Seismology; Oceanography; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.2121645101076659,"gpt":0.3114751841054659,"spread":0.0993106739978,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002117979,0.00012042,0.0001640453,0.00006383051,0.0001345549,0.00005981999,0.0000946751,0.0000378051,0.00005183493],"category_scores_gemma":[0.0000623005,0.00009965366,0.00005316668,0.00009691215,0.00005390464,0.0008966324,0.00002302372,0.0001294974,0.000002568111],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001060926,"about_ca_system_score_gemma":0.00007007149,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001082632,"about_ca_topic_score_gemma":0.00009210283,"domain_scores_codex":[0.9990361,0.00005459358,0.0002356672,0.0001268807,0.0003222624,0.0002245147],"domain_scores_gemma":[0.9991995,0.0001765404,0.000168159,0.00004890286,0.0001871973,0.0002197465],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002279507,0.0002958415,0.9545683,0.0000510859,0.0005195009,0.000002641906,0.003516189,0.002000215,0.003655193,0.003409852,0.0008858716,0.03086738],"study_design_scores_gemma":[0.0004464078,0.00006077683,0.6334848,0.00003254368,0.0000442681,0.000008430889,0.00004242675,0.3578863,0.0000701774,0.007791903,0.00005490679,0.00007713951],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9734852,0.0002965395,0.0237366,0.001243185,0.0004145554,0.0002745543,0.0005066642,0.000006025534,0.00003664851],"genre_scores_gemma":[0.9897504,0.00002771778,0.009122565,0.0001492495,0.0006906656,0.000002237861,0.0001037726,0.00000480539,0.0001486105],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.355886,"threshold_uncertainty_score":0.4063759,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2132509829","doi":"10.1046/j.1365-246x.2000.00090.x","title":"Modelling teleseismic waves in dipping anisotropic structures","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":343,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Anisotropy; Classification of discontinuities; Geology; Seismic anisotropy; Amplitude; Seismogram; Slowness; Geophysics; Mantle (geology); Discontinuity (linguistics); Planar; Lithosphere; Seismic wave; Seismology; Optics; Tectonics; Physics; Mathematical analysis","retraction":null,"screen_n_in":null,"score":{"opus":0.0121890768258558,"gpt":0.2210809186679565,"spread":0.2088918418421007,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001030879,0.0001293461,0.0001757826,0.00008477359,0.0001138166,0.0002272438,0.0003369233,0.00004617475,0.00811761],"category_scores_gemma":[0.000007289171,0.0001036705,0.00008105196,0.00009005697,0.00004046288,0.0003774205,0.00001118268,0.0002433307,0.0003649012],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008770764,"about_ca_system_score_gemma":0.00003202416,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00122263,"about_ca_topic_score_gemma":0.00004649629,"domain_scores_codex":[0.9988415,0.00005496265,0.000288723,0.0001824008,0.0003579277,0.0002744381],"domain_scores_gemma":[0.9996459,0.00005398624,0.00007281671,0.00008216557,0.00004325247,0.0001018461],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0001357815,0.00006020386,0.006907573,0.000007552547,0.00007467096,0.0001413376,0.0003069171,0.885845,0.0009737739,0.002693607,0.0003437028,0.1025099],"study_design_scores_gemma":[0.001138487,0.0001482328,0.3118081,0.00009343335,0.00002278171,0.0001790327,0.00007393862,0.4711376,0.0005610125,0.1839213,0.03038818,0.0005278161],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9931998,0.00006379847,0.0006404378,0.0003246745,0.0007845858,0.00004713232,0.00004208977,0.00001568297,0.004881771],"genre_scores_gemma":[0.9969059,0.0001248043,0.0008743741,0.0001683662,0.001350879,4.579227e-7,0.00003794564,0.00000438145,0.0005329259],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4147074,"threshold_uncertainty_score":0.9927891,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2065081008","doi":"10.1111/j.1365-246x.2004.02203.x","title":"Bounded influence magnetotelluric response function estimation","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":332,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Queen's University","funders":"","keywords":"Magnetotellurics; Estimator; Leverage (statistics); Bounded function; Outlier; Weighting; Mathematics; Statistics; Mathematical analysis; Engineering; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.0088689365087217,"gpt":0.242982625067583,"spread":0.2341136885588613,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003878781,0.0001531868,0.0001513364,0.0001375309,0.0002387215,0.0002386437,0.0003161067,0.0000675544,0.001097865],"category_scores_gemma":[0.0003936245,0.0001213798,0.0001395143,0.000361706,0.0000831157,0.0006479833,0.00001605732,0.000445802,0.001763578],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003448847,"about_ca_system_score_gemma":0.000106152,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002412318,"about_ca_topic_score_gemma":0.00001779732,"domain_scores_codex":[0.9983768,0.0001555645,0.0003034265,0.0002266739,0.0006290191,0.0003085028],"domain_scores_gemma":[0.9990615,0.0002819945,0.0001386376,0.0001064902,0.0001804919,0.0002308635],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0024386,0.0002578323,0.001638213,0.00000643114,0.00009625104,0.0001294239,0.0002017343,0.1647125,0.003103161,0.004567632,0.0001828018,0.8226655],"study_design_scores_gemma":[0.0005767836,0.0005879251,0.7254512,0.00001668409,0.00001739485,0.0001528516,0.00001365057,0.0108156,0.0002837006,0.2592712,0.002649119,0.0001638543],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9630867,0.00003239089,0.03204526,0.002739339,0.0009016895,0.00006760023,0.00001069877,0.00004717184,0.001069159],"genre_scores_gemma":[0.9902707,0.00001045998,0.007709144,0.0007203897,0.0006475084,0.00000109104,0.00002409192,0.000003953304,0.0006127111],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8225016,"threshold_uncertainty_score":0.9998153,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2141008939","doi":"10.1111/j.1365-246x.2006.03131.x","title":"Models of large-scale viscous flow in the Earth's mantle with constraints from mineral physics and surface observations","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":332,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Geoid; Mantle (geology); Geology; Geophysics; Lithosphere; Mantle convection; Transition zone; Viscosity; Heat flux; Physics; Mechanics; Thermodynamics; Heat transfer; Tectonics; Seismology","retraction":null,"screen_n_in":null,"score":{"opus":0.01377240660821753,"gpt":0.2103030808763249,"spread":0.1965306742681074,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001526395,0.0001062723,0.0001655279,0.00002037041,0.00008708456,0.0001172554,0.0002168386,0.0000303023,0.0002149701],"category_scores_gemma":[0.000004259027,0.00006776596,0.00004412531,0.00008473141,0.0001225606,0.0003313424,0.00001426524,0.0001477302,0.00001167139],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002086111,"about_ca_system_score_gemma":0.00003363533,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001993779,"about_ca_topic_score_gemma":0.001445296,"domain_scores_codex":[0.9990188,0.0000653528,0.0002273192,0.0001382264,0.0003772113,0.0001731281],"domain_scores_gemma":[0.9995255,0.0001318085,0.0001207411,0.00008634605,0.00009591763,0.00003972117],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","study_design_scores_codex":[0.0004291184,0.0009807221,0.2263723,0.00002668001,0.000294057,0.0001977343,0.002952186,0.7084137,0.02217816,0.02648362,0.00235739,0.009314336],"study_design_scores_gemma":[0.0009923001,0.00008763196,0.7824927,0.00005244466,0.0000298265,0.0000330567,0.000199296,0.1524691,0.0005625397,0.06240228,0.0005001262,0.00017867],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9932736,0.000031565,0.003811674,0.0004492448,0.0002055634,0.00006972952,0.0007133277,0.000004953392,0.001440407],"genre_scores_gemma":[0.9951102,0.00001013001,0.003963151,0.00009885109,0.0005320587,5.753431e-7,0.0001895746,0.000003238299,0.00009222065],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5561204,"threshold_uncertainty_score":0.3014011,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2041314276","doi":"10.1111/j.1365-246x.2004.02190.x","title":"A comparison of automatic techniques for estimating the regularization parameter in non-linear inverse problems","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":312,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Underdetermined system; Regularization (linguistics); Inverse problem; Mathematics; Applied mathematics; Inverse; Inversion (geology); Mathematical optimization; Tikhonov regularization; Linear model; Computer science; Algorithm; Mathematical analysis; Statistics; Artificial intelligence; Geology; Geometry","retraction":null,"screen_n_in":null,"score":{"opus":0.03102947738420715,"gpt":0.319854513456422,"spread":0.2888250360722149,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003691922,0.0001028354,0.0002164446,0.00008851873,0.00009362299,0.00005053449,0.0003042148,0.00004966532,0.00005833998],"category_scores_gemma":[0.0003629871,0.00006480442,0.0001200811,0.0002607346,0.00007717185,0.0001925638,0.00001445415,0.0002816943,0.00001556649],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001493518,"about_ca_system_score_gemma":0.00004265076,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002003736,"about_ca_topic_score_gemma":0.00006554212,"domain_scores_codex":[0.9988437,0.00006478789,0.0004352134,0.0001340532,0.0003277137,0.0001944762],"domain_scores_gemma":[0.9990633,0.0004252314,0.0002430498,0.00007899846,0.0001293455,0.00006013785],"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":[0.0001001642,0.000486847,0.01463397,0.00006751618,0.00007939854,0.000005217305,0.0008880613,0.2345072,0.001429648,0.001286799,0.0001535971,0.7463616],"study_design_scores_gemma":[0.0003520516,0.0003006114,0.06627145,0.00009316079,0.0000121758,0.00001056924,0.00002784496,0.8014635,0.001687576,0.1296068,0.00009104041,0.00008317922],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.7225282,0.00001423156,0.2742192,0.002119293,0.0004085417,0.0003589093,0.00001388121,0.00002194819,0.0003157803],"genre_scores_gemma":[0.809604,0.000001482835,0.1898706,0.0001238862,0.0003280147,0.000006304344,0.000019888,0.000002934036,0.00004283639],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7462784,"threshold_uncertainty_score":0.2642647,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2124032182","doi":"10.1046/j.1365-246x.2002.01702.x","title":"Greenland glacial history and local geodynamic consequences","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":305,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Ice sheet; Post-glacial rebound; Ice-sheet model; Glacial period; Greenland ice sheet; Geodetic datum; Last Glacial Maximum; Inversion (geology); Geophysics; Climatology; Geodesy; Ice stream; Sea ice; Paleontology; Geomorphology; Cryosphere; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.0224722750817882,"gpt":0.2321841120361891,"spread":0.2097118369544009,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001583798,0.00008975317,0.0001245843,0.00008919743,0.0001443319,0.00003527986,0.0002220383,0.00007427701,0.01391695],"category_scores_gemma":[0.00004077464,0.0000714471,0.00005177025,0.00003780754,0.0008022059,0.000200503,0.00001592104,0.0004181865,0.0008319005],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006656453,"about_ca_system_score_gemma":0.00003060053,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001201667,"about_ca_topic_score_gemma":0.0004615379,"domain_scores_codex":[0.9990828,0.00009866049,0.0001605738,0.0001541639,0.0002655985,0.0002382051],"domain_scores_gemma":[0.9994956,0.0001732401,0.00006241667,0.00005061483,0.00006508283,0.0001530242],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004425977,0.00002240229,0.9853939,0.000002336131,0.00004386052,0.0002579762,0.00008876836,0.00006842909,0.0000109564,0.000932302,0.001731667,0.01140314],"study_design_scores_gemma":[0.0004821422,0.0001496342,0.9380179,0.00001003431,0.00001109738,0.002788534,0.00005455967,0.03504091,0.000003979106,0.008835823,0.01446698,0.0001383765],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9579232,0.001114824,0.0002027146,0.003416725,0.001017253,0.00003614334,0.00001773235,0.00001448878,0.03625686],"genre_scores_gemma":[0.9972843,0.0002340784,0.0001165786,0.0003773807,0.0003202786,3.809609e-7,0.00001693757,0.000001479243,0.001648589],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04737598,"threshold_uncertainty_score":0.9999461,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2117580125","doi":"10.1111/j.1365-246x.2009.04463.x","title":"The angular velocities of the plates and the velocity of Earth's centre from space geodesy","year":2010,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":287,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Geodesy; Satellite geodesy; Figure of the Earth; Geology; Earth (classical element); Space (punctuation); Angular velocity; Geophysics; Seismology; Physics; Astronomy; Classical mechanics; Geodetic datum; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.006323428202666121,"gpt":0.1881012627493221,"spread":0.1817778345466559,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003370458,0.00008104484,0.0001214417,0.00001336904,0.0003036862,0.00009605683,0.0004607118,0.00002970454,0.000155489],"category_scores_gemma":[0.0001245372,0.00003551459,0.0001213324,0.00006159031,0.000530657,0.00009597975,0.00004229616,0.0003602986,0.000008117243],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001203475,"about_ca_system_score_gemma":0.00003564703,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002011281,"about_ca_topic_score_gemma":0.0009289326,"domain_scores_codex":[0.9989614,0.00008430106,0.0001950946,0.0000841576,0.0005471107,0.0001279701],"domain_scores_gemma":[0.9990112,0.000419974,0.0002140658,0.0001307451,0.0001781756,0.00004583477],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001094634,0.0002238899,0.7586932,0.00001951042,0.001327326,0.0000112791,0.005775632,0.001167173,0.01306734,0.06668167,0.001724456,0.1502139],"study_design_scores_gemma":[0.0004814605,0.00001430661,0.919793,0.00001833834,0.00002022658,0.000006000746,0.000238241,0.003581824,0.001883695,0.07185491,0.002058172,0.00004988638],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.994486,0.000159082,0.00001819887,0.003522717,0.0009619029,0.00005893869,0.00008759653,0.000001968888,0.000703549],"genre_scores_gemma":[0.9992242,0.00002931988,0.0001273394,0.00007392767,0.0003317385,2.047394e-7,0.00000643648,0.00000173628,0.0002051279],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1610997,"threshold_uncertainty_score":0.3040469,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2104933591","doi":"10.1111/j.1365-246x.2006.03156.x","title":"Full waveform tomography for lithospheric imaging: results from a blind test in a realistic crustal model","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":278,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Queen's University","funders":"","keywords":"Tomography; Waveform; Geology; Seismology; Seismic tomography; Geodesy; Earth structure; Lithosphere; Acoustics; Physics; Optics; Computer science; Tectonics; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.01242773610722414,"gpt":0.2326910787084108,"spread":0.2202633426011867,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002151317,0.0001377748,0.0001493829,0.0001462697,0.0001032908,0.0001786183,0.0003198781,0.00004206607,0.0001622444],"category_scores_gemma":[0.000131752,0.0001144581,0.0001498058,0.0001635774,0.00007602848,0.000359412,0.00001539597,0.0002671107,0.00003519215],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002467858,"about_ca_system_score_gemma":0.00006090617,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.009705369,"about_ca_topic_score_gemma":0.0001898589,"domain_scores_codex":[0.998714,0.00001863046,0.0004044343,0.0002445086,0.0003500509,0.0002683569],"domain_scores_gemma":[0.9992083,0.0003001083,0.0001641655,0.00009964662,0.0001381035,0.00008965458],"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":[0.009752597,0.001874724,0.1617444,0.0000312452,0.0001998724,0.0005342568,0.001152655,0.07242046,0.002712105,0.002833686,0.2825024,0.4642417],"study_design_scores_gemma":[0.001337127,0.00009873995,0.04357169,0.00004369662,0.00001026663,0.00003786457,0.00005078416,0.873906,0.0001215819,0.07587397,0.004788972,0.0001592724],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9122416,0.0001848383,0.04426152,0.009475255,0.001226792,0.0003533942,0.002568059,0.0001676047,0.02952091],"genre_scores_gemma":[0.9841534,0.00001590374,0.01313864,0.0007286452,0.0008369668,0.000002336116,0.0005669496,0.000005652855,0.0005514777],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8014856,"threshold_uncertainty_score":0.9968891,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2138575022","doi":"10.1111/j.1365-246x.2009.04467.x","title":"Regression analysis of MCS intensity and ground motion parameters in Italy and its application in ShakeMap","year":2010,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Performance and Analysis","field":"Engineering","cited_by":277,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Mercalli intensity scale; Scale (ratio); Intensity (physics); Regression analysis; Regression; Robustness (evolution); Ground motion; Geology; Peak ground acceleration; Data set; Linear regression; Statistics; Seismology; Geodesy; Mathematics; Geography; Cartography","retraction":null,"screen_n_in":null,"score":{"opus":0.007968873869151627,"gpt":0.2379078565136039,"spread":0.2299389826444523,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001508359,0.00007727764,0.0001955864,0.0004702779,0.00001797952,0.0000266277,0.00008219175,0.00005135482,0.000007846567],"category_scores_gemma":[0.00002601714,0.0000676653,0.0000573043,0.0003494481,0.00002687098,0.0002812545,0.00002559423,0.0003031745,0.000001807832],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000324523,"about_ca_system_score_gemma":0.000003881188,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00007115705,"about_ca_topic_score_gemma":0.0001266942,"domain_scores_codex":[0.9993868,0.000009217066,0.0002483426,0.0001071669,0.0001578396,0.00009063326],"domain_scores_gemma":[0.9997342,0.00003388704,0.00006609598,0.00005650491,0.00006515787,0.00004416144],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.000173626,0.0003909012,0.4518088,0.00006931352,0.001509196,0.0000311484,0.001785273,0.07922869,0.3011736,0.002203655,0.00005440294,0.1615714],"study_design_scores_gemma":[0.0001574771,0.000006822658,0.4535405,0.00001678569,0.00004658575,0.000007297578,0.00004792124,0.5444053,0.001130643,0.0005760796,0.00001426265,0.00005030229],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9986001,0.00003438714,0.001009392,0.0001481765,0.0001066063,0.00002912436,0.00000478224,0.00000718647,0.00006020028],"genre_scores_gemma":[0.9995961,0.0001355593,0.0001483206,0.00002971584,0.00005742595,0.000002940569,0.00001544289,0.000004409178,0.00001011465],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4651767,"threshold_uncertainty_score":0.2759311,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2138154318","doi":"10.1111/j.1365-246x.2005.02609.x","title":"The rotational stability of an ice-age earth","year":2005,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":270,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research; Adolph C. and Mary Sprague Miller Institute for Basic Research in Science, University of California Berkeley; National Aeronautics and Space Administration; David and Lucile Packard Foundation; National Science Foundation","keywords":"Lithosphere; Geology; Earth's rotation; Hydrostatic equilibrium; Post-glacial rebound; Geophysics; Rotation (mathematics); Observable; Crust; Geodesy; Physics; Glacial period; Seismology; Geometry; Mathematics; Tectonics; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.02554271721239051,"gpt":0.2495930907392321,"spread":0.2240503735268416,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004483689,0.00008577971,0.00009737181,0.00002970304,0.0002464304,0.00014535,0.0004135844,0.00002358613,0.000962105],"category_scores_gemma":[0.00005746873,0.00005645507,0.0001060486,0.00007627268,0.0001111321,0.000415097,0.00001264853,0.0002231962,0.0001553274],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006905131,"about_ca_system_score_gemma":0.00006217688,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001979627,"about_ca_topic_score_gemma":0.0007773287,"domain_scores_codex":[0.9985316,0.00008663404,0.0002781678,0.0001236368,0.0007994665,0.000180451],"domain_scores_gemma":[0.9992123,0.0001330269,0.0001518129,0.0001180057,0.0002576343,0.0001272141],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0003785472,0.0006088605,0.1096475,0.000005964426,0.0002518786,0.00002375953,0.0005414679,0.004038716,0.003704069,0.008156252,0.0005772693,0.8720658],"study_design_scores_gemma":[0.0003228374,0.0001251239,0.9596328,0.000006587268,0.000008056763,0.00001922184,0.00006830606,0.009863106,0.001000994,0.01714013,0.01172327,0.00008955293],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9934409,0.00004197006,0.0001108144,0.001152069,0.0005467127,0.00005275111,0.00006105519,0.000006596838,0.004587125],"genre_scores_gemma":[0.9977245,0.00001021443,0.000908132,0.0001273651,0.0009888244,4.733074e-7,0.00004992537,0.000002046775,0.0001884909],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8719762,"threshold_uncertainty_score":0.9999511,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2109717268","doi":"10.1046/j.1365-246x.2002.01809.x","title":"Simulated annealing inversion of multimode Rayleigh wave dispersion curves for geological structure","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":268,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"","keywords":"Inversion (geology); Superposition principle; Simulated annealing; Rayleigh wave; Geology; Surface wave; Optics; Mathematical analysis; Mathematics; Algorithm; Physics; Seismology","retraction":null,"screen_n_in":null,"score":{"opus":0.02633852332692557,"gpt":0.229275624883658,"spread":0.2029371015567324,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008707277,0.0001079573,0.0001963566,0.00008001558,0.0001232373,0.00003529097,0.0002108315,0.0000612289,0.005405298],"category_scores_gemma":[0.00009176767,0.00007521498,0.0002211485,0.0001079191,0.0000631437,0.0001984146,0.00001563499,0.0001875747,0.00002133904],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007697294,"about_ca_system_score_gemma":0.000007155742,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002008825,"about_ca_topic_score_gemma":0.00001387627,"domain_scores_codex":[0.9989851,0.00003942525,0.0002740711,0.0001616405,0.0003601203,0.0001797158],"domain_scores_gemma":[0.9992936,0.0001900838,0.0001740826,0.00006662267,0.0001655076,0.0001101614],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0008891665,0.0005521791,0.1787239,0.0001758899,0.001359785,0.0001589091,0.0006799098,0.626229,0.008811076,0.0008049637,0.03358041,0.1480348],"study_design_scores_gemma":[0.0004729105,0.0001209624,0.03022984,0.00006938968,0.00003921927,0.00002005943,0.00004389493,0.9643034,0.0001943817,0.003216486,0.00118537,0.0001041149],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9961136,0.0003423426,0.0009482059,0.001574213,0.0003951767,0.00006622395,0.0002629951,0.000009781696,0.0002874896],"genre_scores_gemma":[0.997243,0.0003153059,0.001011673,0.0005288829,0.0004648239,8.109974e-8,0.0002173148,0.000002572366,0.0002163105],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3380744,"threshold_uncertainty_score":0.9955039,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2095646703","doi":"10.1046/j.1365-246x.2003.01850.x","title":"Partial melt or aqueous fluid in the mid-crust of Southern Tibet? Constraints from INDEPTH magnetotelluric data","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":265,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Magnetotellurics; Geology; Tectonics; Crust; Electrical resistivity and conductivity; Mineralogy; Geophysics; Partial melting; Petrology; Aqueous solution; Seismology","retraction":null,"screen_n_in":null,"score":{"opus":0.04349539231043829,"gpt":0.2784874183807405,"spread":0.2349920260703023,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006166751,0.00017302,0.000269896,0.0000807786,0.00009219182,0.000112877,0.001180987,0.00007812171,0.007855601],"category_scores_gemma":[0.0005427176,0.00009886894,0.000107352,0.0003477574,0.0002195262,0.0002146668,0.0000390812,0.0005754303,0.0004938153],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000731871,"about_ca_system_score_gemma":0.0001342722,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001204171,"about_ca_topic_score_gemma":0.000288874,"domain_scores_codex":[0.99761,0.0005161208,0.0004746556,0.0003026445,0.0007547381,0.0003418891],"domain_scores_gemma":[0.9982946,0.000995633,0.0001875122,0.0002944421,0.00008477041,0.0001430469],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0004549718,0.0005216091,0.01246313,0.000006505997,0.0001480177,0.0004335753,0.000544611,0.0006167977,0.0006963484,0.0006311224,0.0006596719,0.9828237],"study_design_scores_gemma":[0.005936224,0.002118623,0.7134127,0.0001761785,0.0002524564,0.001304456,0.002433275,0.05825488,0.003329844,0.1569682,0.05440417,0.001408946],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9910352,0.0002209589,0.001691142,0.001097975,0.0008100231,0.0001333785,0.0007493863,0.00001166553,0.004250244],"genre_scores_gemma":[0.9965631,0.00003358372,0.001830722,0.0004246769,0.0007244372,7.791875e-7,0.0001392165,0.000004295897,0.0002792081],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9814147,"threshold_uncertainty_score":0.9930514,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1883408522","doi":"10.1111/j.1365-246x.2012.05669.x","title":"Multidimensional time-series analysis of ground deformation from multiple InSAR data sets applied to Virunga Volcanic Province","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":226,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Interferometric synthetic aperture radar; Geodesy; Geology; Remote sensing; Synthetic aperture radar; Time series; Series (stratigraphy); Lava; Volcano; Seismology; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.01270914702929741,"gpt":0.2421398529699879,"spread":0.2294307059406905,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001836809,0.0001590104,0.0002594084,0.0002210652,0.00007269001,0.00004056408,0.0004898927,0.00006679961,0.0002313064],"category_scores_gemma":[0.000058201,0.0001403349,0.00009160486,0.0003289554,0.00003731002,0.0005902452,0.0001709276,0.0001981916,0.0001221043],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001227196,"about_ca_system_score_gemma":0.00002835148,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00009216179,"about_ca_topic_score_gemma":0.00003121411,"domain_scores_codex":[0.9987748,0.00001951112,0.0004067729,0.0001624558,0.0004360004,0.0002004084],"domain_scores_gemma":[0.9990757,0.0001625731,0.000123658,0.0003581084,0.0001372286,0.0001427952],"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":[0.0004752171,0.001869215,0.0105671,0.00004540302,0.00965045,0.000008860933,0.002557729,0.006826977,0.2838694,0.02000223,0.01631096,0.6478164],"study_design_scores_gemma":[0.0006517645,0.00005970236,0.1911966,0.00006199362,0.0007402972,0.00003123282,0.0001538956,0.5527645,0.02881538,0.001343673,0.2235209,0.0006599862],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.6095089,0.00006904639,0.3878203,0.0002368947,0.0002993972,0.0002160495,0.0007042773,0.0001302408,0.0010149],"genre_scores_gemma":[0.8444863,0.00001573965,0.1543755,0.00007330576,0.0003256175,0.00001117812,0.0006582129,0.00001895146,0.00003515632],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6471564,"threshold_uncertainty_score":0.5722691,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2101194783","doi":"10.1111/j.1365-246x.2009.04133.x","title":"Joint seismic, geodynamic and mineral physical constraints on three-dimensional mantle heterogeneity: Implications for the relative importance of thermal versus compositional heterogeneity","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":224,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Mantle (geology); Geology; Geophysics; Mantle convection; Core–mantle boundary; Scaling; Geodynamics; Thermal; Shear (geology); Tectonics; Seismology; Physics; Petrology; Lithosphere; Geometry; Thermodynamics","retraction":null,"screen_n_in":null,"score":{"opus":0.02705559996976724,"gpt":0.2730007752795438,"spread":0.2459451753097766,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001795402,0.0001872634,0.00025666,0.00004787648,0.0002975937,0.00008609359,0.0002683944,0.00004984134,0.000134702],"category_scores_gemma":[0.00003059443,0.0001276374,0.0002167116,0.00005567096,0.0002633628,0.0002196148,0.0000251952,0.0002100641,0.00001929962],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001358893,"about_ca_system_score_gemma":0.00005224799,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00004535835,"about_ca_topic_score_gemma":0.00005861361,"domain_scores_codex":[0.9987565,0.00005277237,0.0003332097,0.0002576378,0.0003543468,0.0002455205],"domain_scores_gemma":[0.9987978,0.0004686824,0.0002722612,0.0001517299,0.0001909134,0.0001185691],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.008789912,0.002816709,0.05791845,0.0000556974,0.004305635,0.00007752418,0.0005581898,0.1293723,0.4035224,0.2061503,0.003456004,0.1829768],"study_design_scores_gemma":[0.001203902,0.0006810665,0.9317645,0.00002524663,0.00007085252,0.00005957468,0.000005375442,0.03964193,0.001485579,0.02473571,0.0001477102,0.0001785398],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9925882,0.00004964006,0.001573996,0.003504605,0.0006083685,0.0002155934,0.001101762,0.00001133219,0.0003465691],"genre_scores_gemma":[0.9979115,0.000007111954,0.0006110013,0.0004002714,0.0008419573,0.000004190519,0.0002040264,0.000005063653,0.00001489414],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8738461,"threshold_uncertainty_score":0.5204901,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2123740616","doi":"10.1093/gji/ggt221","title":"Numerical simulation of acoustic emission in brittle rocks by two-dimensional finite-discrete element analysis","year":2013,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":219,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Acoustic emission; Dissipation; Finite element method; Brittleness; Geology; Solver; Fracture mechanics; Mechanics; Elastic energy; Discrete element method; Deformation (meteorology); Structural engineering; Physics; Acoustics; Computer science; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.007252395310035561,"gpt":0.2495856455393701,"spread":0.2423332502293346,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009766254,0.0001221398,0.0002111224,0.0002074735,0.00003933842,0.00004605423,0.0001620388,0.00004716872,0.0004786254],"category_scores_gemma":[0.00004244634,0.0001127664,0.0001569706,0.0002263856,0.000006552557,0.000203201,0.00004004463,0.0002668085,0.00002429897],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001001171,"about_ca_system_score_gemma":0.00001519533,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00009508967,"about_ca_topic_score_gemma":0.000002954632,"domain_scores_codex":[0.9987498,0.00002283782,0.0004520011,0.0001326415,0.0004552637,0.0001874918],"domain_scores_gemma":[0.9994305,0.0001211024,0.00009136542,0.00007862172,0.0001685368,0.0001098682],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00001038996,0.00006067243,0.000221805,0.000003790586,0.0001678275,0.000002629652,0.00003693438,0.9618153,0.03547624,0.00001189686,0.0004488325,0.001743684],"study_design_scores_gemma":[0.0003904428,0.00002719793,0.0004862266,0.00003069198,0.00004365008,0.000002540387,0.0000129545,0.9944564,0.003036218,0.001320208,0.00007880029,0.000114726],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.5487587,0.00003980595,0.4506472,0.00009139456,0.0002221787,0.00005477575,0.00001249915,0.00001668095,0.0001567601],"genre_scores_gemma":[0.9990946,0.000009399306,0.0005109842,0.00004433338,0.0001749754,0.000006246515,0.00005221278,0.00001458685,0.00009263997],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4503359,"threshold_uncertainty_score":0.5240613,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2119723105","doi":"10.1111/j.1365-246x.2006.02885.x","title":"The<i>S</i>receiver functions: synthetics and data example","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":215,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Receiver function; Classification of discontinuities; Seismogram; Lithosphere; Geology; Seismology; Mantle (geology); Waveform; Geophysics; Mathematical analysis; Computer science; Telecommunications; Mathematics; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.0190133644909618,"gpt":0.2320459716611154,"spread":0.2130326071701536,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002899651,0.0000924444,0.00009449138,0.00002546984,0.0004122662,0.000492359,0.0005161772,0.00002775538,0.0005767806],"category_scores_gemma":[0.00003425855,0.00005915164,0.00003370091,0.00004849026,0.0001096227,0.0003576204,0.00006888725,0.0001474777,0.0002736248],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002889531,"about_ca_system_score_gemma":0.00002644898,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002016756,"about_ca_topic_score_gemma":0.000409782,"domain_scores_codex":[0.9990417,0.00005377222,0.0002039844,0.0001830903,0.0003285792,0.0001888252],"domain_scores_gemma":[0.9992848,0.0002453754,0.0001012313,0.0002112958,0.00008284033,0.00007442395],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0005639509,0.0004535128,0.07142258,0.0000254045,0.0008052614,0.0002107897,0.0002163818,0.004554267,0.007314687,0.05476196,0.3625444,0.4971268],"study_design_scores_gemma":[0.000266434,0.00004891162,0.2676646,0.00001285966,0.0000320191,0.0001246465,0.00003739071,0.004882124,0.0001096639,0.03384552,0.6928173,0.0001585816],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9697031,0.000671356,0.001583908,0.003773844,0.006373161,0.0001341988,0.0008939671,0.00004547958,0.01682096],"genre_scores_gemma":[0.9946783,0.0001547822,0.0002837994,0.0001037727,0.002521753,5.087236e-7,0.0002369484,0.000003631391,0.002016539],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4969682,"threshold_uncertainty_score":0.6315343,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2142446883","doi":"10.1111/j.1365-246x.2011.05090.x","title":"On the robustness of predictions of sea level fingerprints","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":209,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Geophysics; Ice sheet; Solid earth; Polar; Sensitivity (control systems); Robustness (evolution); Statistical physics; Geodesy; Physics; Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.08569027010484442,"gpt":0.2378429866662568,"spread":0.1521527165614123,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002091088,0.00006719554,0.00009802726,0.00005086198,0.00007656473,0.00001407852,0.0003487032,0.00002209706,0.001919615],"category_scores_gemma":[0.00006419452,0.00004235138,0.0001083024,0.00008713878,0.00008211911,0.00009697434,0.00001310627,0.0001830102,0.00005200825],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003602958,"about_ca_system_score_gemma":0.00003569483,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005734375,"about_ca_topic_score_gemma":0.00006146241,"domain_scores_codex":[0.9990449,0.00004319744,0.00021205,0.00007923695,0.0005157691,0.000104849],"domain_scores_gemma":[0.9993472,0.0001035933,0.0001771528,0.00009802781,0.0002202069,0.00005385702],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001169901,0.002938115,0.7284638,0.00005067884,0.001817735,0.00004658752,0.002401667,0.04170674,0.001971683,0.05960988,0.01199556,0.1478276],"study_design_scores_gemma":[0.0001667167,0.0001363675,0.9703205,0.00003795855,0.00001349705,0.00001167128,0.00004389793,0.008672833,0.001032044,0.01943828,0.00007380969,0.00005241152],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9868929,0.000007162107,0.001393023,0.0002330019,0.0008969156,0.00004584089,0.0001872999,0.000003379569,0.01034049],"genre_scores_gemma":[0.9993074,0.00000466693,0.0002945986,0.00004697832,0.0001911056,3.863868e-7,0.00001112682,0.000001664409,0.0001420517],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2418567,"threshold_uncertainty_score":0.9989927,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2082355668","doi":"10.1111/j.1365-246x.2005.02536.x","title":"Glacial isostatic adjustment on 3-D Earth models: a finite-volume formulation","year":2005,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":199,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Adolph C. and Mary Sprague Miller Institute for Basic Research in Science, University of California Berkeley; National Science Foundation","keywords":"Geology; Classification of discontinuities; Discretization; Geodesy; Finite volume method; Regular grid; Grid; Interpolation (computer graphics); Geometry; Geophysics; Mathematics; Mechanics; Mathematical analysis; Physics; Classical mechanics","retraction":null,"screen_n_in":null,"score":{"opus":0.02667308461915942,"gpt":0.2652878061868597,"spread":0.2386147215677003,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002066522,0.0001188983,0.0001362829,0.0001428555,0.0002112103,0.00006684122,0.000270626,0.00007715834,0.005688792],"category_scores_gemma":[0.00006352208,0.00009569879,0.0001053601,0.0000848338,0.0000668442,0.0004606854,0.00001486759,0.0004677617,0.003657683],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005636524,"about_ca_system_score_gemma":0.0000569578,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00002367853,"about_ca_topic_score_gemma":0.0002261784,"domain_scores_codex":[0.9986691,0.0001002161,0.000249933,0.000175475,0.0004897199,0.0003155452],"domain_scores_gemma":[0.9993134,0.0002459986,0.00009374877,0.00008393647,0.0001098893,0.0001530734],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0005753519,0.0002147321,0.6753181,0.000004772267,0.0001284745,0.00006499676,0.0003367864,0.2553862,0.000008691401,0.01070686,0.001296451,0.05595859],"study_design_scores_gemma":[0.0005039161,0.0002277868,0.4828323,0.00001361229,0.000007748336,0.0001076396,0.00002336735,0.4976472,0.00001385292,0.01474581,0.003776457,0.0001004017],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9468052,0.00009652523,0.002850093,0.005666029,0.001028343,0.0001168407,0.00004021452,0.00002841733,0.04336833],"genre_scores_gemma":[0.9947653,0.00005029975,0.001076106,0.0009108964,0.00129931,0.000001414533,0.0001020405,0.000002874262,0.00179172],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2422609,"threshold_uncertainty_score":0.9971181,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2129020528","doi":"10.1111/j.1365-246x.2004.02387.x","title":"Elastic velocity models for gas-hydrate-bearing sediments-a comparison","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":197,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Clathrate hydrate; Porosity; Geology; Sediment; Mineralogy; Biot number; Hydrate; Saturation (graph theory); Seafloor spreading; Context (archaeology); Amplitude; Soil science; Geophysics; Thermodynamics; Geomorphology; Geotechnical engineering; Chemistry; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.02143407640520479,"gpt":0.2670592079146627,"spread":0.2456251315094579,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001958534,0.0001468027,0.0001724198,0.00003864304,0.0002172029,0.0001052412,0.0003514395,0.00006304483,0.0006776822],"category_scores_gemma":[0.00002532814,0.0001205234,0.0001440925,0.00009821804,0.00008283,0.0003937717,0.0001370771,0.000370457,0.0004448671],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000347805,"about_ca_system_score_gemma":0.00002203005,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00008048204,"about_ca_topic_score_gemma":0.00000519714,"domain_scores_codex":[0.9986036,0.00002361964,0.000331823,0.000228872,0.0005077243,0.0003043996],"domain_scores_gemma":[0.9994623,0.00006007588,0.0001640092,0.00008978251,0.00003750319,0.000186298],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0001199986,0.0004607557,0.0005867348,0.000004090874,0.0001402233,0.00001410068,0.0004870534,0.9749013,0.009240449,0.007258564,0.0009495794,0.005837137],"study_design_scores_gemma":[0.003245095,0.0003628395,0.004605044,0.00007645351,0.00006969457,0.0000989519,0.0001107569,0.5129367,0.004930789,0.4664689,0.006623704,0.000471109],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8545088,0.00002662613,0.1305039,0.00133698,0.00132756,0.0001760889,0.00001234437,0.00003160306,0.01207613],"genre_scores_gemma":[0.9927682,0.00001563891,0.005840505,0.0002578954,0.0004749824,0.00001134694,0.00001494614,0.00001647681,0.0006000127],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4619646,"threshold_uncertainty_score":0.7420145,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1845580858","doi":"10.1111/j.1365-246x.2010.04905.x","title":"PADM2M: a penalized maximum likelihood model of the 0-2 Ma palaeomagnetic axial dipole moment","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":186,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Dipole; Geology; Moment (physics); Magnetic dipole; Amplitude; Data set; Standard deviation; Geodesy; Seismology; Physics; Mathematics; Statistics; Optics; Classical mechanics","retraction":null,"screen_n_in":null,"score":{"opus":0.01577823142868728,"gpt":0.2255897025260624,"spread":0.2098114710973751,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001245979,0.0001886846,0.00018171,0.00004254888,0.0001281432,0.00002772573,0.0006176023,0.00008257177,0.0003254451],"category_scores_gemma":[0.00004882079,0.0001338228,0.0002962677,0.00006598802,0.0001856439,0.00001013494,0.0003483611,0.0001945051,0.00003249792],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001276482,"about_ca_system_score_gemma":0.00008585165,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0000402945,"about_ca_topic_score_gemma":0.00001677304,"domain_scores_codex":[0.9986224,0.00006701458,0.0003613732,0.0002340359,0.0004249227,0.0002902345],"domain_scores_gemma":[0.999188,0.00001243344,0.0002150804,0.0002570017,0.0002177028,0.0001097779],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.001339145,0.001877782,0.02072106,0.00004295261,0.000973895,0.00003872432,0.00167907,0.0004337053,0.9226216,0.004395733,0.02014622,0.02573012],"study_design_scores_gemma":[0.01107618,0.005201675,0.588652,0.0003132866,0.0005482679,0.0007478042,0.000632583,0.008789062,0.1912325,0.1630684,0.02786979,0.001868496],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9819032,0.0003833458,0.002850487,0.0007462969,0.0008859031,0.0001524312,0.00006305717,0.000007379078,0.01300788],"genre_scores_gemma":[0.994789,0.0002197387,0.001638445,0.0002521561,0.0005487318,0.00001744651,0.00001467532,0.000016946,0.002502885],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7313891,"threshold_uncertainty_score":0.5457137,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2139403704","doi":"10.1111/j.1365-246x.2004.02338.x","title":"Using commercial finite element packages for the study of earth deformations, sea levels and the state of stress","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":185,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"","keywords":"Finite element method; Viscoelasticity; Stress (linguistics); Deformation (meteorology); Earth (classical element); Earth model; Physics; Mechanics; Geology; Geophysics; Meteorology","retraction":null,"screen_n_in":null,"score":{"opus":0.05875554078108961,"gpt":0.288059169230841,"spread":0.2293036284497514,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004103434,0.00007143871,0.0001284622,0.00003407086,0.0002191664,0.00006469157,0.0002241105,0.000009198137,0.00002675523],"category_scores_gemma":[0.00003895044,0.00003750431,0.00007137105,0.00006304726,0.0001018102,0.0001504956,0.00002116446,0.0001191876,0.000001697073],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003237709,"about_ca_system_score_gemma":0.00003961702,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001525915,"about_ca_topic_score_gemma":0.000919027,"domain_scores_codex":[0.9990233,0.00006172842,0.0002798415,0.00006465351,0.0004610441,0.0001094228],"domain_scores_gemma":[0.9991791,0.0002616447,0.0002375058,0.00007269518,0.0002145053,0.00003453181],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","study_design_scores_codex":[0.00106733,0.001148523,0.2991429,0.00004467123,0.001369368,0.000004836911,0.009376904,0.5533138,0.0002446198,0.002337592,0.00004132598,0.1319082],"study_design_scores_gemma":[0.003001472,0.0002728023,0.9518363,0.00003200883,0.00006171846,0.000005211545,0.0008351225,0.02470544,0.0003536381,0.01877112,0.00005899835,0.00006618685],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9940152,0.00005237912,0.004568089,0.0004761978,0.0002470451,0.000251975,0.0003525247,0.000001366039,0.00003528213],"genre_scores_gemma":[0.9995211,0.0000124994,0.0002401941,0.00005984866,0.000139849,0.0000012937,0.00001249055,0.000001632474,0.00001111207],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6526934,"threshold_uncertainty_score":0.2306737,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2172160159","doi":"10.1111/j.1365-246x.2004.02317.x","title":"Hypocentre determination offshore of eastern Taiwan using the Maximum Intersection method","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":178,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Residual; Geodesy; Seismology; Intersection (aeronautics); Subduction; Weighting; Magnitude (astronomy); Mathematics; Tectonics; Physics; Algorithm; Geography; Cartography","retraction":null,"screen_n_in":null,"score":{"opus":0.0248036735810925,"gpt":0.2758376413610244,"spread":0.2510339677799319,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000201682,0.00009740939,0.0001231143,0.00007866051,0.0001645897,0.00006670519,0.0002407022,0.00003244772,0.0004127691],"category_scores_gemma":[0.00004765717,0.00006298337,0.0001335255,0.0001160994,0.00007817232,0.0002430811,0.00002146679,0.0002265858,0.00003755636],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002157322,"about_ca_system_score_gemma":0.00005042351,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000411122,"about_ca_topic_score_gemma":0.0003438515,"domain_scores_codex":[0.9990177,0.0000611857,0.0002492959,0.0001194557,0.0003973217,0.000155112],"domain_scores_gemma":[0.9994525,0.00007496202,0.0001906642,0.0000738886,0.0001575583,0.00005043584],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0002780406,0.0002065233,0.1537296,0.00001881416,0.0004729441,0.00009074653,0.003739054,0.03366429,0.001527143,0.002400511,0.0000865836,0.8037858],"study_design_scores_gemma":[0.00188663,0.0005007422,0.7844822,0.0002094495,0.0001346675,0.001330526,0.004206113,0.1176265,0.003554171,0.08335382,0.002324232,0.000390998],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.962489,0.00008688759,0.03156495,0.00112633,0.001231868,0.00006598928,0.00001893821,0.00001125463,0.00340479],"genre_scores_gemma":[0.9952267,0.00001420293,0.004025717,0.000108245,0.0005543375,2.532131e-7,0.000008564482,0.000002775714,0.00005921055],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8033948,"threshold_uncertainty_score":0.4519533,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2136525356","doi":"10.1046/j.1365-246x.2000.00231.x","title":"A precisely dated Proterozoic palaeomagnetic pole from the North China craton, and its relevance to palaeocontinental reconstruction","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":174,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Royal Ontario Museum; College of Family Physicians of Canada","funders":"","keywords":"Paleomagnetism; Craton; Geology; Laurentia; Zircon; Proterozoic; Paleontology; Remanence; Apparent polar wander; Precambrian; Position (finance); Paleozoic; Magnetization; Tectonics; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.005900489680706948,"gpt":0.1859096909647011,"spread":0.1800092012839942,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008197166,0.0001390462,0.0001553236,0.00002966712,0.0002036311,0.0001613678,0.0003348594,0.00003729959,0.01832316],"category_scores_gemma":[0.00009508927,0.00008234338,0.00009006127,0.0001892948,0.00007001206,0.0002253443,0.00002524909,0.0003109286,0.0006429578],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005082658,"about_ca_system_score_gemma":0.00001383558,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001096685,"about_ca_topic_score_gemma":0.001298443,"domain_scores_codex":[0.9988255,0.00007504617,0.0002721467,0.000267252,0.0003375614,0.0002225246],"domain_scores_gemma":[0.9994261,0.0001236332,0.00008241516,0.00008598308,0.00007805745,0.0002038326],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003175578,0.00008335714,0.545986,0.000002139087,0.0001303527,0.00003241158,0.0001997368,0.001125721,0.00156922,0.00002778657,0.0006550542,0.4498706],"study_design_scores_gemma":[0.000245438,0.0001140359,0.9774488,0.00002174809,0.00002234751,0.0001023559,0.00001480072,0.01122183,0.0001556125,0.008101268,0.002429121,0.0001226005],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9922761,0.0001465319,0.00002186415,0.006015275,0.000194888,0.000126455,0.0001416556,0.00001753618,0.001059728],"genre_scores_gemma":[0.9976085,0.0001166514,0.0003261362,0.0006056481,0.0006866884,0.000003105639,0.00009800895,0.000002241488,0.0005529717],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.449748,"threshold_uncertainty_score":0.9825742,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2168016945","doi":"10.1111/j.1365-246x.2010.04562.x","title":"Constraining models of postglacial rebound using space geodesy: a detailed assessment of model ICE-5G (VM2) and its relatives","year":2010,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":164,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Deglaciation; Ice sheet; Post-glacial rebound; Mantle (geology); Lithosphere; Last Glacial Maximum; North American Plate; Geodesy; Antarctic ice sheet; Holocene; Oceanography; Cryosphere; Geophysics; Plate tectonics; Sea ice; Tectonics; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.05728523936810088,"gpt":0.3023942730384431,"spread":0.2451090336703422,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003685286,0.0001330501,0.0002438783,0.0001034182,0.0001276629,0.00006890904,0.0002117964,0.00006228485,0.0001340649],"category_scores_gemma":[0.00005191011,0.0001152383,0.0001069477,0.00008481572,0.0001495864,0.0005132704,0.00002384996,0.0004514436,0.000002549937],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007114903,"about_ca_system_score_gemma":0.0002018807,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001608734,"about_ca_topic_score_gemma":0.00007001065,"domain_scores_codex":[0.9985635,0.00004988927,0.0003570535,0.0001714428,0.000666383,0.0001917782],"domain_scores_gemma":[0.9989436,0.00009612807,0.0003650859,0.00007629737,0.000385569,0.000133296],"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":[0.000350655,0.000497869,0.2386649,0.00006308233,0.0007889469,0.00003490228,0.001939575,0.1920403,0.4584821,0.09544446,0.00002786995,0.01166536],"study_design_scores_gemma":[0.0004807143,0.00007828134,0.117532,0.000044114,0.00003221942,0.00003547026,0.00007248988,0.8331783,0.0008013213,0.04762761,0.000006535506,0.000110879],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9925619,0.00003067628,0.002780822,0.0001603175,0.0003855182,0.00007220001,0.0001103001,0.000004231219,0.003894082],"genre_scores_gemma":[0.992529,0.0000110146,0.007173364,0.00002322492,0.0001876519,2.546646e-7,0.00001464475,0.000004113925,0.0000567741],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6411381,"threshold_uncertainty_score":0.4699283,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2002980452","doi":"10.1093/gji/ggt465","title":"3-D inversion of airborne electromagnetic data parallelized and accelerated by local mesh and adaptive soundings","year":2013,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":160,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Polygon mesh; Depth sounding; Inversion (geology); Algorithm; Computer science; Geology; Transmitter; Inverse problem; Geophysics; Computational science; Mathematics; Telecommunications; Seismology","retraction":null,"screen_n_in":null,"score":{"opus":0.02480768869694137,"gpt":0.2507477494372514,"spread":0.22594006074031,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001670523,0.0001395016,0.0002319327,0.00006339032,0.0001017418,0.000122366,0.0003743882,0.00005876716,0.001100746],"category_scores_gemma":[0.00008915274,0.00010285,0.00003906168,0.0001638043,0.0002059218,0.0005645242,0.00008086598,0.0003239061,0.00006329831],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000555983,"about_ca_system_score_gemma":0.00002718587,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001135896,"about_ca_topic_score_gemma":0.000016156,"domain_scores_codex":[0.9987311,0.0001149096,0.0002622841,0.0002712672,0.0003695936,0.0002507812],"domain_scores_gemma":[0.9990813,0.0002961552,0.000137005,0.0001065227,0.0001410417,0.0002380435],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0003858626,0.0001822461,0.004643621,0.00001342326,0.0002039649,0.0000135924,0.0001005356,0.00003815724,0.01081738,0.001028514,0.01434271,0.96823],"study_design_scores_gemma":[0.001770053,0.001747024,0.5297349,0.00004231419,0.00006640764,0.000125852,0.0001219957,0.3749844,0.001272206,0.08690008,0.002846619,0.0003881178],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9943318,0.0003220924,0.002454256,0.001987342,0.0001430988,0.0001045285,0.00005545307,0.00001200567,0.0005894364],"genre_scores_gemma":[0.9955784,0.0001985697,0.003407068,0.000259359,0.0001646813,7.663657e-7,0.00009018648,0.000003212401,0.0002977675],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9678419,"threshold_uncertainty_score":0.9998124,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2118230965","doi":"10.1046/j.1365-246x.2000.00089.x","title":"Characterization of the magnetotelluric tensor in terms of its invariants","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":160,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Victoria","funders":"Australian National University; Natural Sciences and Engineering Research Council of Canada; University of Cambridge; University of Victoria","keywords":"Magnetotellurics; Invariant (physics); Geology; Geometry; Tensor (intrinsic definition); Rotation (mathematics); Geophysics; Gaussian; Electrical impedance; Mathematical analysis; Physics; Mathematics; Electrical resistivity and conductivity","retraction":null,"screen_n_in":null,"score":{"opus":0.01083640904775488,"gpt":0.220970654032831,"spread":0.2101342449850762,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001469483,0.00008238854,0.0001670702,0.00006741228,0.00003642437,0.00001984208,0.0003878193,0.00004065371,0.004775948],"category_scores_gemma":[0.00007360099,0.00005032657,0.0001122079,0.0003655026,0.00005666541,0.0001910001,0.00001213828,0.0002374318,0.00009987125],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004406068,"about_ca_system_score_gemma":0.00002135199,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00008130139,"about_ca_topic_score_gemma":0.00001613227,"domain_scores_codex":[0.9988695,0.0001271151,0.0003522275,0.0001099768,0.0003851951,0.0001559472],"domain_scores_gemma":[0.9995351,0.0001051361,0.0001603606,0.00007921224,0.0000622332,0.00005798876],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.000200746,0.0002602242,0.06469528,0.00001418557,0.00003479091,0.00001209208,0.0001167219,0.001057361,0.04399645,0.0005879987,0.00002238499,0.8890018],"study_design_scores_gemma":[0.0002379827,0.0000981181,0.9792858,0.00003352694,0.000005952542,0.00002124026,0.00000198805,0.007565768,0.005059096,0.006938175,0.000692589,0.00005972119],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9943614,0.00001043632,0.00006049785,0.0007462848,0.0002946299,0.00006739196,0.00003944219,0.000002943608,0.004416998],"genre_scores_gemma":[0.9977149,0.00005441242,0.0001652818,0.0001389139,0.0002512753,3.832838e-7,0.00001110529,0.000001917708,0.001661772],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9145906,"threshold_uncertainty_score":0.9961338,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2102964909","doi":"10.1046/j.1365-246x.2003.01919.x","title":"Assessment of crustal velocity models using seismic refraction and reflection tomography","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Tomography; Seismic tomography; Inversion (geology); Seismology; Data set; Geodesy; Algorithm; Geophysics; Computer science; Mantle (geology); Optics; Tectonics; Artificial intelligence; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.02721597301602707,"gpt":0.2892064489532421,"spread":0.261990475937215,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002398251,0.00007135286,0.00009580145,0.0001471783,0.0001861205,0.00004637759,0.00007599853,0.00003562598,0.0001835441],"category_scores_gemma":[0.00001745835,0.0000618159,0.00006549728,0.0001096976,0.0000606464,0.0005049556,0.000008468234,0.0002260654,0.000001369118],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001817788,"about_ca_system_score_gemma":0.00004959117,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007387155,"about_ca_topic_score_gemma":0.000002739387,"domain_scores_codex":[0.9992284,0.00007054456,0.0001833956,0.0001144549,0.0002968928,0.0001062874],"domain_scores_gemma":[0.9995835,0.00003773574,0.0001466442,0.00004656575,0.0001230396,0.00006252676],"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":[0.0003204306,0.0006887963,0.3862401,0.00007006866,0.0007234475,0.00007812677,0.001009364,0.1705785,0.01577481,0.01907459,0.005439118,0.4000027],"study_design_scores_gemma":[0.0002051649,0.00009241454,0.05022184,0.00002730924,0.00001479073,0.0002207067,0.000103265,0.9124122,0.001136713,0.03356763,0.001905297,0.00009263602],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9105272,0.00003915749,0.08121107,0.0001658648,0.0005535594,0.00003416429,0.000009800308,0.00001839241,0.007440778],"genre_scores_gemma":[0.9894226,0.00006345248,0.01008911,0.0002496904,0.0001127263,1.575555e-7,0.000006941328,0.000002037581,0.00005330075],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7418337,"threshold_uncertainty_score":0.2520779,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2117822793","doi":"10.1046/j.1365-246x.2002.01586.x","title":"On the postglacial isostatic adjustment of the British Isles and the shallow viscoelastic structure of the Earth","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Geology; Ice sheet; Holocene; Sea level; Last Glacial Maximum; Glacial period; Deglaciation; Physical geography; Oceanography; Isostasy; Series (stratigraphy); Paleontology; Climatology; Geomorphology; Geography; Tectonics; Lithosphere","retraction":null,"screen_n_in":null,"score":{"opus":0.008479873214676107,"gpt":0.2022554018672511,"spread":0.193775528652575,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001695366,0.00007223301,0.0001207334,0.00001666278,0.0004392306,0.00006525323,0.0005727311,0.0000404474,0.002194785],"category_scores_gemma":[0.0002379991,0.00002828371,0.0001137207,0.00008846675,0.0009129316,0.00005151912,0.0000486606,0.0004920656,0.0000205842],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001055127,"about_ca_system_score_gemma":0.000023452,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001494639,"about_ca_topic_score_gemma":0.001579665,"domain_scores_codex":[0.9987974,0.0003379698,0.0001893061,0.00008900692,0.0004405827,0.000145806],"domain_scores_gemma":[0.9986378,0.0009923778,0.0001465148,0.0001139691,0.00007862643,0.00003068958],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000189035,0.00005858388,0.9829842,0.00000861769,0.0001841004,0.000007929785,0.0005951722,0.001121669,0.000071658,0.01136847,0.0008600426,0.002550524],"study_design_scores_gemma":[0.000458781,0.00006975212,0.9663483,0.00004668141,0.00002007572,0.0002916781,0.00008160411,0.009016193,0.00004789935,0.02350392,0.00008032445,0.000034785],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9881043,0.0002496569,0.000005198014,0.009076249,0.0005881425,0.0001141391,0.00005226021,0.000001346184,0.001808731],"genre_scores_gemma":[0.9987044,0.00007332422,0.000008601804,0.0006288927,0.0001512546,4.347027e-7,0.000002167372,0.000001382744,0.0004294839],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01663589,"threshold_uncertainty_score":0.9987174,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2114370777","doi":"10.1046/j.1365-246x.2003.01822.x","title":"Three-dimensional tomographic inversion of combined reflection and refraction seismic traveltime data","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":147,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Inversion (geology); Geology; Covariance; Tomography; Seismic inversion; Synthetic data; Inverse transform sampling; Inverse problem; Algorithm; Geometry; Mathematical analysis; Seismology; Optics; Surface wave; Mathematics; Physics; Tectonics; Statistics","retraction":null,"screen_n_in":null,"score":{"opus":0.02566478809900145,"gpt":0.2550015808391915,"spread":0.2293367927401901,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003685437,0.00009662881,0.0001248563,0.000181153,0.0001417244,0.00004994312,0.0002394101,0.0000525271,0.0005604114],"category_scores_gemma":[0.00007458403,0.00008117365,0.00005087242,0.0001479936,0.0001026356,0.000561045,0.00002411471,0.0002772677,0.00002794347],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009039394,"about_ca_system_score_gemma":0.00004375123,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0009703955,"about_ca_topic_score_gemma":0.00002177966,"domain_scores_codex":[0.9989708,0.000065693,0.0002370895,0.0002024988,0.0003944541,0.0001294648],"domain_scores_gemma":[0.9993757,0.00009029586,0.0001739571,0.0001467789,0.0001221887,0.0000910801],"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":[0.001427366,0.0006791443,0.2473854,0.00005052174,0.0006168775,0.00009388419,0.0002506736,0.001828807,0.01219697,0.00310103,0.142693,0.5896763],"study_design_scores_gemma":[0.001271358,0.0005457879,0.127478,0.0001057826,0.00005676418,0.0005747211,0.00007775395,0.778887,0.004273857,0.06144499,0.02498146,0.0003025015],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.989177,0.0001121955,0.005272552,0.001846362,0.001148056,0.00007247203,0.0000563422,0.00003947903,0.002275577],"genre_scores_gemma":[0.9962465,0.00006614368,0.00278384,0.0005442856,0.0001305491,1.664701e-7,0.0001272087,0.000003075658,0.00009825452],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7770582,"threshold_uncertainty_score":0.6136112,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2002777061","doi":"10.1111/j.1365-246x.2007.03360.x","title":"Non-linear primary-multiple separation with directional curvelet frames","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Multiple; Curvelet; Residual; Separation (statistics); Algorithm; Distortion (music); SIGNAL (programming language); Source separation; Mathematics; Computer science; Domain (mathematical analysis); Time domain; Statistics; Artificial intelligence; Wavelet; Mathematical analysis; Wavelet transform; Arithmetic","retraction":null,"screen_n_in":null,"score":{"opus":0.00969803977702956,"gpt":0.2521325992156367,"spread":0.2424345594386072,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003498032,0.0001176219,0.0001168583,0.0001311049,0.0001929658,0.00009930085,0.0002230557,0.00004790239,0.0008617135],"category_scores_gemma":[0.00003386634,0.00008656688,0.00007700096,0.0001299792,0.00008383994,0.0004702757,0.00001065325,0.0003567697,0.0002450451],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002560023,"about_ca_system_score_gemma":0.0000608187,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005487525,"about_ca_topic_score_gemma":0.00003568895,"domain_scores_codex":[0.9987823,0.00002018284,0.0002234329,0.0001677003,0.0005835184,0.0002228518],"domain_scores_gemma":[0.9993231,0.0001464518,0.0001285009,0.00007085234,0.0002006498,0.0001305016],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00101644,0.0002657269,0.6921979,0.00001019173,0.0002254968,0.000177728,0.0003029127,0.002829111,0.001632838,0.0002762512,0.05840612,0.2426593],"study_design_scores_gemma":[0.0007881289,0.00031696,0.8047432,0.00005056236,0.00001535798,0.0004865728,0.00009048059,0.06834453,0.004853498,0.002081099,0.1179373,0.0002922672],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8744493,0.00003635715,0.09186894,0.001853353,0.001405948,0.00009805191,0.00004000722,0.000106688,0.03014137],"genre_scores_gemma":[0.9847257,0.00001924791,0.01078503,0.001904722,0.001389303,4.614996e-7,0.0001487917,0.000004622178,0.001022164],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.242367,"threshold_uncertainty_score":0.9435158,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2282264169","doi":"10.1093/gji/ggv419","title":"Comparison of the STA/LTA and power spectral density methods for microseismic event detection","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":133,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Geophone; Microseism; Event (particle physics); Computer science; Spectral density; Term (time); Filter (signal processing); Data mining; Pattern recognition (psychology); Algorithm; Geology; Artificial intelligence; Seismology; Computer vision; Physics; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.03839265672517489,"gpt":0.3796254407431983,"spread":0.3412327840180234,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003912915,0.00007002323,0.0001374716,0.00003632784,0.0001342875,0.00004908804,0.0003508299,0.00002703313,0.000002402267],"category_scores_gemma":[0.0001402219,0.00004816367,0.00008876382,0.00006518195,0.00009266564,0.0001562137,0.0001782299,0.0001865907,0.000002587981],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003619174,"about_ca_system_score_gemma":0.00003972092,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00001806087,"about_ca_topic_score_gemma":0.000005239975,"domain_scores_codex":[0.999289,0.0001079605,0.0001935578,0.0001240232,0.0001649438,0.0001204723],"domain_scores_gemma":[0.9992974,0.0001491796,0.0001522241,0.00009873319,0.0002465095,0.00005592402],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.001309769,0.001998711,0.07273682,0.00002941525,0.001592434,0.0000164323,0.0139748,0.002307327,0.125497,0.126254,0.01181013,0.6424731],"study_design_scores_gemma":[0.00175151,0.001118954,0.587672,0.00003156728,0.00004269119,0.0004233812,0.0003852217,0.09038351,0.09593471,0.2114512,0.01055477,0.0002504631],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"methods","genre_gemma":"empirical","genre_scores_codex":[0.4727203,0.0000667206,0.5241452,0.001678255,0.001280918,0.00004258756,0.00000120979,0.000005622866,0.00005917199],"genre_scores_gemma":[0.9749334,0.000002980818,0.02460037,0.0002109954,0.0001654103,0.00000201628,2.735422e-7,0.000002434814,0.00008211236],"genre_candidate":"empirical","genre_consensus":null,"teacher_disagreement_score":0.6422226,"threshold_uncertainty_score":0.1964057,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2136633733","doi":"10.1111/j.1365-246x.2004.02270.x","title":"Contemporary kinematics of the southern Aegean and the Mediterranean Ridge","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Canadian Nautical Research Society","funders":"","keywords":"Geology; Kinematics; Geodesy; Seismology; Ridge; Deformation (meteorology); Seamount; Strain rate; Accretionary wedge; Shear zone; Geometry; Tectonics; Subduction; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.02060609875480814,"gpt":0.2220293668690154,"spread":0.2014232681142073,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002355927,0.0000727858,0.0001261958,0.00002103136,0.0001651795,0.00004598613,0.00029161,0.00001912577,0.0001968271],"category_scores_gemma":[0.00008745929,0.0000318448,0.0001076127,0.00005981891,0.000371214,0.00007991766,0.00002939213,0.000212611,0.00003392467],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002500489,"about_ca_system_score_gemma":0.00004197573,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000514166,"about_ca_topic_score_gemma":0.0001196007,"domain_scores_codex":[0.9992031,0.00005475173,0.0002131805,0.0000687604,0.0003670015,0.00009322506],"domain_scores_gemma":[0.9994585,0.0002017158,0.0001533007,0.00008096558,0.00006578394,0.00003971488],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.002472749,0.0007121791,0.6098551,0.000142418,0.004041176,0.0002465444,0.05867094,0.01534974,0.0006963606,0.07122262,0.01702706,0.2195631],"study_design_scores_gemma":[0.004500742,0.000139833,0.8911899,0.00015454,0.00005213121,0.0003179717,0.001924474,0.002756145,0.0002299074,0.09635469,0.002199327,0.0001803735],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.980175,0.0004340296,0.00007966791,0.008979468,0.0007425248,0.00007643684,0.00006066594,0.000005905828,0.009446261],"genre_scores_gemma":[0.9988695,0.00004002224,0.00008407767,0.0003985039,0.0004716999,2.948978e-7,0.000004255067,0.000001679156,0.0001299082],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2813348,"threshold_uncertainty_score":0.2155118,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2106678640","doi":"10.1046/j.1365-246x.2003.01861.x","title":"Evolution of orogenic wedges and continental plateaux: insights from crustal thermal-mechanical models overlying subducting mantle lithosphere","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":131,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Subduction; Lithosphere; Mantle (geology); Crust; Mantle wedge; Petrology; Oceanic crust; Wedge (geometry); Geophysics; Seismology; Continental crust; Décollement; Tectonics; Geometry","retraction":null,"screen_n_in":null,"score":{"opus":0.01209346760994966,"gpt":0.1970273901300062,"spread":0.1849339225200566,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0000960028,0.0001369429,0.0002285406,0.0000408433,0.0001267544,0.00006617797,0.0001870234,0.0000749586,0.003347979],"category_scores_gemma":[0.00008175571,0.00009819761,0.0001613171,0.0001048094,0.00009499403,0.0003561094,0.00002902808,0.0002962185,0.00003932224],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001243313,"about_ca_system_score_gemma":0.00002970656,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00136124,"about_ca_topic_score_gemma":0.0002228527,"domain_scores_codex":[0.9987889,0.00008046321,0.0003369083,0.0002294962,0.0003687131,0.0001955522],"domain_scores_gemma":[0.9993423,0.0001501453,0.0001737486,0.00006777408,0.0001130173,0.0001530742],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","study_design_scores_codex":[0.0008385409,0.0008287371,0.7251906,0.00003109783,0.001505085,0.0002558857,0.001013292,0.02483436,0.1355137,0.07636393,0.0002062533,0.03341855],"study_design_scores_gemma":[0.001080784,0.000194052,0.3555546,0.00006339567,0.0001063213,0.0001446739,0.001016084,0.1429535,0.007888949,0.4903549,0.0002735299,0.0003693397],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9952562,0.0007861824,0.0007635567,0.0001384205,0.0003174817,0.00003624867,0.00003764656,0.00001155096,0.002652695],"genre_scores_gemma":[0.9984287,0.00004556227,0.001097528,0.00004496509,0.0002649247,3.976201e-7,0.00003419943,0.000002722165,0.00008099106],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4139909,"threshold_uncertainty_score":0.9975631,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2106066058","doi":"10.1111/j.1365-246x.2007.03365.x","title":"Inversion of time domain three-dimensional electromagnetic data","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Inverse problem; Inversion (geology); Time domain; Tikhonov regularization; Discretization; Algorithm; Electromagnetic field; Mathematical analysis; Computer science; Mathematics; Geology; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01768341552178101,"gpt":0.2570587184525148,"spread":0.2393753029307338,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007857918,0.0001426294,0.0002229271,0.0001321073,0.0001120294,0.00004258794,0.0008901061,0.0000666797,0.00341708],"category_scores_gemma":[0.0001502161,0.0001078004,0.0001205787,0.0003098801,0.0001155807,0.0003218692,0.00008602158,0.0004112513,0.0007014668],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009978266,"about_ca_system_score_gemma":0.00006167281,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002617754,"about_ca_topic_score_gemma":0.00009445909,"domain_scores_codex":[0.9980415,0.00007894262,0.0004039468,0.0002692559,0.0008334156,0.0003729893],"domain_scores_gemma":[0.9986424,0.0005261415,0.0001928215,0.0002272534,0.0001671332,0.0002442257],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.001053565,0.0005311514,0.0150433,0.00001217196,0.0002629518,0.0002113031,0.00004616545,0.000581724,0.03314235,0.001432639,0.009208848,0.9384738],"study_design_scores_gemma":[0.00092057,0.0009910504,0.7553165,0.00003709754,0.00004112321,0.00021332,0.000009144102,0.0768236,0.001801852,0.1567517,0.006768709,0.0003254017],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9888511,0.00009839597,0.003962828,0.001349944,0.0006138839,0.00007006701,0.00007107724,0.00001955407,0.004963149],"genre_scores_gemma":[0.9774197,0.000008616766,0.02005231,0.000359528,0.001316652,1.229413e-7,0.000214464,0.000005266417,0.0006233509],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9381484,"threshold_uncertainty_score":0.9974939,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2100814877","doi":"10.1111/j.1365-246x.2006.03096.x","title":"Efficient waveform tomography for lithospheric imaging: implications for realistic, two-dimensional acquisition geometries and low-frequency data","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Queen's University","funders":"","keywords":"Waveform; Tomography; Geology; Sampling (signal processing); Seismic tomography; Viscoelasticity; Acoustics; Algorithm; Geodesy; Seismology; Computer science; Physics; Optics; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.01485573251624665,"gpt":0.2616221710121165,"spread":0.2467664384958698,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003911229,0.0001309546,0.0001347016,0.0001502736,0.0003612197,0.0002101782,0.0003967586,0.00002879654,0.0001134175],"category_scores_gemma":[0.00009146039,0.0001081173,0.00009815631,0.0001643059,0.0001363518,0.0002780544,0.00003897404,0.000114737,0.00000719643],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002114613,"about_ca_system_score_gemma":0.00006650028,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001363939,"about_ca_topic_score_gemma":0.00001356096,"domain_scores_codex":[0.9988563,0.00001566154,0.0002974088,0.000294284,0.0002892249,0.0002470865],"domain_scores_gemma":[0.998838,0.0002947554,0.0001636957,0.0001831954,0.00042201,0.00009831404],"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":[0.0006912061,0.0008063162,0.2565632,0.0001040286,0.0003168283,0.00001542247,0.0001176079,0.01405017,0.006111728,0.03461988,0.2269748,0.4596288],"study_design_scores_gemma":[0.0009473036,0.000125041,0.3522257,0.00005123123,0.00005121291,0.0001853318,0.00002933946,0.4918991,0.0003113767,0.1476862,0.006221655,0.0002665351],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8064049,0.0009407108,0.1573436,0.02110207,0.002030346,0.0008293214,0.006747773,0.0002173146,0.004383969],"genre_scores_gemma":[0.9742302,0.00001092473,0.0219312,0.0008756021,0.0009747385,0.000007395947,0.001853115,0.000006609119,0.0001102335],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4778489,"threshold_uncertainty_score":0.4408894,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3000382179","doi":"10.1093/gji/ggz574","title":"The upper mantle beneath the South Atlantic Ocean, South America and Africa from waveform tomography with massive data sets","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"European Regional Development Fund; Geological Survey of Ireland; Science Foundation Ireland; Centre of Excellence for Environmental Decisions, Australian Research Council","keywords":"Craton; Geology; Lithosphere; Crust; Mantle (geology); Seismology; Seismogram; Geophysics; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.0230018667355595,"gpt":0.2103759652765725,"spread":0.187374098541013,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007747435,0.0001423057,0.000142783,0.00002302916,0.0005533866,0.0003152376,0.0007009386,0.00002213068,0.0003169471],"category_scores_gemma":[0.00005159998,0.00006247393,0.00006620187,0.0001401829,0.000253069,0.0002030676,0.0001157723,0.0003517188,0.0001043192],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002464544,"about_ca_system_score_gemma":0.00003553816,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002663177,"about_ca_topic_score_gemma":0.0001029294,"domain_scores_codex":[0.9987917,0.0000472315,0.0001741578,0.0002478057,0.000493072,0.0002460485],"domain_scores_gemma":[0.9991474,0.0003151934,0.0001444381,0.0001887426,0.00006843916,0.0001358563],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0006103903,0.00004459569,0.8876124,0.0000059455,0.001615238,0.0001913892,0.01176373,0.000372092,0.00001085696,0.0003527629,0.01149453,0.08592609],"study_design_scores_gemma":[0.0004485688,0.0002294325,0.9482626,0.0000240369,0.00008277709,0.00003903202,0.003566725,0.0199803,0.000005323843,0.00167862,0.02550673,0.0001758212],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9788212,0.0008617628,0.0002351695,0.01624941,0.0003042867,0.000110407,0.00069636,0.00002370938,0.002697652],"genre_scores_gemma":[0.99795,0.0002009686,0.0002542718,0.0007430066,0.0006774143,4.058884e-7,0.0001103202,0.000004294398,0.00005935554],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08575026,"threshold_uncertainty_score":0.4256259,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2116910913","doi":"10.1111/j.1365-246x.2004.02175.x","title":"Shear wave anisotropy beneath the Cascadia subduction zone and western North American craton","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Craton; Seismology; Shear (geology); Shear zone; Shear wave splitting; Anisotropy; Geophysics; Petrology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.009701036025300916,"gpt":0.212035285330212,"spread":0.2023342493049111,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001184234,0.0001424936,0.0001738724,0.00004751499,0.0002780585,0.0003146917,0.000217124,0.00002352715,0.0001904316],"category_scores_gemma":[0.00001341104,0.00009198487,0.00007089196,0.00011497,0.0001752284,0.0003382852,0.00002723338,0.0002285354,0.0001381519],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001267532,"about_ca_system_score_gemma":0.00004553757,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003660661,"about_ca_topic_score_gemma":0.001832803,"domain_scores_codex":[0.9988844,0.00005400554,0.0002189031,0.0001947748,0.0004039682,0.0002439315],"domain_scores_gemma":[0.9994279,0.00005008995,0.0001589651,0.0001087056,0.0000982816,0.0001560811],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001082599,0.0006971156,0.5899821,0.00003607821,0.00123277,0.0008069263,0.004116165,0.02874468,0.009564755,0.01144423,0.002338897,0.3499537],"study_design_scores_gemma":[0.0003796986,0.0002392316,0.9897178,0.00001150118,0.00002788633,0.0002800039,0.00006244093,0.0004854483,0.0005515525,0.002984032,0.005107167,0.0001532665],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9954021,0.0000354707,0.0008408547,0.002335694,0.001003581,0.00006996908,0.00009044418,0.00001657649,0.0002053385],"genre_scores_gemma":[0.9967896,0.0001386719,0.0004463029,0.0003512222,0.002054109,9.721391e-7,0.00005446605,0.000005410614,0.000159289],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3997357,"threshold_uncertainty_score":0.5533848,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2163583063","doi":"10.1093/gji/ggu131","title":"Tracking basement cross-strike discontinuities in the Indian crust beneath the Himalayan orogen using gravity data – relationship to upper crustal faults","year":2014,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Geology; Basement; Foreland basin; Precambrian; Seismology; Collision zone; Crust; Bouguer anomaly; Tectonics; Continental collision; Lineament; Graben; Fault (geology); Paleontology; Craton; Gravity anomaly; Lithosphere","retraction":null,"screen_n_in":null,"score":{"opus":0.05146971206530718,"gpt":0.2959515705741,"spread":0.2444818585087929,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009945991,0.0001504464,0.0001652925,0.00008120771,0.0004305718,0.0004564151,0.001361217,0.00004959339,0.001355641],"category_scores_gemma":[0.0005143773,0.00007628912,0.0001298446,0.0002682571,0.0001401003,0.0004500725,0.000123522,0.0005445975,0.00009495952],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001578379,"about_ca_system_score_gemma":0.00003168359,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003034441,"about_ca_topic_score_gemma":0.003906002,"domain_scores_codex":[0.9980935,0.0002294209,0.0003794152,0.0002862245,0.0006856322,0.0003258156],"domain_scores_gemma":[0.9987684,0.0005849013,0.0001349369,0.0002803367,0.00009826753,0.0001331544],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003736317,0.00005799301,0.9849877,0.000001603388,0.0000337853,0.00001751369,0.0004631597,0.005930161,0.00004477667,0.000714672,0.0001154204,0.007595788],"study_design_scores_gemma":[0.000186061,0.00004334955,0.9619258,0.00001785985,0.00002385411,0.00005066861,0.0005075626,0.01908203,0.00002388884,0.0165909,0.001426972,0.0001210546],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9926728,0.00002575558,0.0003973896,0.005621409,0.0002177473,0.00009173941,0.0002207433,0.000007272063,0.0007451512],"genre_scores_gemma":[0.9973437,0.000003599761,0.0003806308,0.001065103,0.0008427721,0.000001272172,0.0002730121,0.000002480668,0.0000874398],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02306196,"threshold_uncertainty_score":0.9995573,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1853937621","doi":"10.1046/j.1365-246x.1998.00388.x","title":"The complex-image method for calculating the magnetic and electric fields produced at the surface of the Earth by the auroral electrojet","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Electrojet; Computation; Electric field; Magnetic field; Computational physics; Electric current; Geophysics; Surface (topology); Simple (philosophy); Physics; Electric potential; Electromagnetic induction; Mathematical analysis; Mathematics; Algorithm; Earth's magnetic field; Geometry; Quantum mechanics; Voltage; Electromagnetic coil","retraction":null,"screen_n_in":null,"score":{"opus":0.02051469864066298,"gpt":0.267455233955477,"spread":0.246940535314814,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0009676444,0.0001648872,0.0001735025,0.00001359163,0.001402349,0.0002341611,0.0009163416,0.00004361083,0.0003320311],"category_scores_gemma":[0.0004872408,0.00005568924,0.0002262113,0.0003563332,0.0002207014,0.00008885749,0.00007460274,0.0006503934,0.00002077312],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008586346,"about_ca_system_score_gemma":0.00002383787,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002905803,"about_ca_topic_score_gemma":0.0001752505,"domain_scores_codex":[0.9977645,0.0006915675,0.0003301465,0.0002128207,0.0005874411,0.0004135615],"domain_scores_gemma":[0.9956198,0.003674091,0.0002347323,0.0002402058,0.0001623714,0.00006884699],"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":[0.0003377716,0.0001635693,0.003450107,0.00001446306,0.0003579821,0.000002952112,0.0007395187,0.002314654,0.04668678,0.003070562,0.04617222,0.8966894],"study_design_scores_gemma":[0.0007933598,0.0009168299,0.2873979,0.00001643614,0.0001419947,0.0002432137,0.0001244925,0.6013553,0.01086941,0.03409801,0.06373546,0.0003075851],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9037958,0.001671198,0.003548191,0.08806914,0.0005881776,0.0006607965,0.00005665697,0.00001458023,0.001595407],"genre_scores_gemma":[0.9934546,0.00008135223,0.001232805,0.00126843,0.0005684508,0.00000554364,0.000005361944,0.000006177552,0.003377243],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8963819,"threshold_uncertainty_score":0.9998977,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2069509807","doi":"10.1046/j.1365-246x.2001.01550.x","title":"Glacial isostatic adjustment on a rotating earth","year":2001,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Geoid; Post-glacial rebound; Geology; Geodesy; Spherical harmonics; Geodetic datum; Earth's rotation; Geophysics; Observable; Mantle (geology); Polar motion; Glacial period; Physics; Geomorphology; Measured depth","retraction":null,"screen_n_in":null,"score":{"opus":0.02411416042894655,"gpt":0.2492000391994654,"spread":0.2250858787705188,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001692189,0.0001332715,0.0001274183,0.00008003605,0.0001918819,0.0001551001,0.0002653819,0.00002720925,0.002650181],"category_scores_gemma":[0.00004660808,0.0001070782,0.0001234529,0.0001164291,0.00003180183,0.0002274374,0.00001159595,0.0002999812,0.001586332],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009058299,"about_ca_system_score_gemma":0.00003908639,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001737919,"about_ca_topic_score_gemma":0.00008290225,"domain_scores_codex":[0.9984251,0.00005630441,0.0002323906,0.0001790267,0.0008303046,0.0002768508],"domain_scores_gemma":[0.9994248,0.0000736886,0.0001247913,0.00008377955,0.0001177197,0.0001752092],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0003468462,0.0003652243,0.2100223,0.000004661343,0.0001934992,0.0002182073,0.0002958665,0.003843981,0.0002556227,0.00175679,0.001668482,0.7810285],"study_design_scores_gemma":[0.0005924167,0.0003109805,0.9687195,0.00004148369,0.00001117388,0.00008624254,0.00004901787,0.01262194,0.00004230923,0.01062418,0.006748074,0.0001526672],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9749917,0.00003234659,0.0003280262,0.001043752,0.001899629,0.00007690885,0.00002932721,0.00001738279,0.0215809],"genre_scores_gemma":[0.9957881,0.00002343165,0.0005042371,0.0008740302,0.001884471,8.597256e-7,0.00004437453,0.000003928137,0.0008765502],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7808758,"threshold_uncertainty_score":0.999191,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}