{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":1137,"total_is_capped":false,"direct_labels_cover":1,"predictions_cover":1137,"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":"cafb3b95b00d","filters":{"topic":"Seismic Waves and Analysis"}},"results":[{"id":"W2162770137","doi":"10.1190/1.1543223","title":"The <i>S</i> -transform with windows of arbitrary and varying shape","year":2003,"lang":"en","type":"article","venue":"Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":503,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"S transform; Constant Q transform; Harmonic wavelet transform; Short-time Fourier transform; Fourier transform; Algorithm; Window function; Computer science; Invertible matrix; Fractional Fourier transform; Filter (signal processing); Wavelet transform; Continuous wavelet transform; Window (computing); Gaussian; Discrete wavelet transform; Mathematics; Wavelet; Mathematical analysis; Fourier analysis; Artificial intelligence; Computer vision; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.005481863354910049,"gpt":0.1665355805424476,"spread":0.1610537171875376,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008367,0.00006569308,0.00009451929,0.00001071742,0.0001468403,0.00002492279,0.00006621861,0.00001552856,0.00006257044],"category_scores_gemma":[0.000003077553,0.0000362459,0.00003186835,0.0001520256,0.00008567762,0.0000849449,0.000001676409,0.00006139515,0.000008244747],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":4.22964e-7,"about_ca_system_score_gemma":0.00002254768,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0003661189,"about_ca_topic_score_gemma":0.00008003755,"domain_scores_codex":[0.9995437,0.00001607093,0.00008711209,0.00009694558,0.000116241,0.0001399773],"domain_scores_gemma":[0.9997219,0.00008992562,0.00003648783,0.00009900531,0.00001383233,0.00003888083],"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":[0.0002275037,0.00009004204,0.4011402,0.0001534035,0.0005934621,0.00003905129,0.001364191,0.005033711,0.0006571464,0.02107948,0.0004302258,0.5691916],"study_design_scores_gemma":[0.002784647,0.001179827,0.601622,0.0001561157,0.0006084889,0.00009119846,0.003281897,0.06493317,0.006351243,0.2096646,0.1078842,0.001442581],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9673973,0.0007230301,0.00007521701,0.0001628658,0.00003750942,0.00006577469,0.00002284315,0.000008218763,0.03150729],"genre_scores_gemma":[0.9990818,0.000234545,0.0002856064,0.0002375675,0.00002496871,2.39933e-7,0.0000100299,0.000001814209,0.0001234127],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.567749,"threshold_uncertainty_score":0.1478065,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3045022196","doi":"10.1126/science.abd2438","title":"Global quieting of high-frequency seismic noise due to COVID-19 pandemic lockdown measures","year":2020,"lang":"en","type":"article","venue":"Science","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":378,"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; McGill University; University of British Columbia","funders":"University of California, Santa Barbara; Agencia Nacional de Investigación y Desarrollo; K. H. Renlunds stiftelse; Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México; Fonds National de la Recherche Luxembourg; Consejo Nacional de Ciencia y Tecnología; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Sight Research UK; Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; National Science Foundation; Earthquake Commission; Royal Society; Natural Environment Research Council; Boğaziçi Üniversitesi","keywords":"Coronavirus disease 2019 (COVID-19); Pandemic; 2019-20 coronavirus outbreak; Noise (video); Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2); Acoustics; Seismology; Computer science; Geology; Virology; Medicine; Physics; Artificial intelligence; Internal medicine","retraction":null,"screen_n_in":null,"score":{"opus":0.03699201989764146,"gpt":0.26292251505063,"spread":0.2259304951529886,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007774711,0.0001291252,0.0002377253,0.00006333931,0.0002721412,0.00007554354,0.0008165109,0.00003741759,0.0004976559],"category_scores_gemma":[0.0007713066,0.000104247,0.00007147344,0.002300749,0.000474443,0.0002386453,0.00004793594,0.00007549349,0.0001632561],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003041582,"about_ca_system_score_gemma":0.0004478133,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01989012,"about_ca_topic_score_gemma":0.001734304,"domain_scores_codex":[0.9980369,0.00005407615,0.0002755031,0.0005066524,0.0007128236,0.0004140802],"domain_scores_gemma":[0.9987624,0.00007118936,0.0001064709,0.0002281389,0.00007387798,0.0007578657],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002351514,0.000009108307,0.854897,0.00003123185,0.00001042713,0.00003767744,0.0004702208,0.1149922,0.001550337,0.0001306034,0.0003519857,0.02749565],"study_design_scores_gemma":[0.0003873007,0.000267776,0.8848277,0.00003098497,0.00005301536,0.00006916047,0.001065263,0.1042816,0.0003522487,0.003874666,0.00428577,0.000504463],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9859537,0.0004496861,0.007811203,0.004203788,0.0001702262,0.0001142128,0.0001820624,0.00006009293,0.001055028],"genre_scores_gemma":[0.9906744,0.0000323707,0.001741559,0.007424469,0.00009949636,4.156661e-7,0.000009997098,0.000001639313,0.00001565536],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0299307,"threshold_uncertainty_score":0.9866365,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2008095626","doi":"10.1029/2007jb005248","title":"Broadband ambient noise surface wave tomography across the United States","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":311,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Rayleigh wave; Geology; Seismology; Ambient noise level; Surface wave; Seismic noise; Dispersion (optics); Rayleigh scattering; Azimuth; Crust; Phase velocity; Love wave; Group velocity; Noise (video); Geodesy; Geophysics; Wave propagation; Optics; Physics; Longitudinal wave; Geomorphology; Mechanical wave","retraction":null,"screen_n_in":null,"score":{"opus":0.03981498808270457,"gpt":0.2969762105447445,"spread":0.25716122246204,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00119059,0.0001586506,0.0003209532,0.00003173516,0.0007986166,0.0001710721,0.0005616298,0.00005706108,0.0007575834],"category_scores_gemma":[0.000218212,0.00008523029,0.0003466365,0.001722156,0.0007913085,0.0002430785,0.00004907845,0.0008194408,0.0001143234],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001153246,"about_ca_system_score_gemma":0.0001220093,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01977363,"about_ca_topic_score_gemma":0.0005406039,"domain_scores_codex":[0.9966373,0.0004387358,0.0004185906,0.0002020505,0.001574576,0.0007287209],"domain_scores_gemma":[0.9972612,0.001272285,0.000182179,0.0002747027,0.0006292505,0.0003803409],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.002021876,0.0008848106,0.710786,0.00007469446,0.001421183,0.002429278,0.006727116,0.1407717,0.001354617,0.0001696976,0.100433,0.03292605],"study_design_scores_gemma":[0.0006555279,0.0010697,0.895429,0.00005221227,0.00003264068,0.0001111671,0.004381117,0.05156863,0.0004820489,0.003313026,0.04269115,0.0002138353],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9966627,0.001064347,0.00005370313,0.00163078,0.0001105999,0.00009049509,0.00005010743,0.000008450429,0.0003288215],"genre_scores_gemma":[0.9961607,0.00194331,0.0003123725,0.0002619946,0.0003570273,2.368712e-7,0.00002347231,0.000006176849,0.0009347062],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1846429,"threshold_uncertainty_score":0.9867538,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2168379187","doi":"10.1098/rspa.2007.0277","title":"The origin of deep ocean microseisms in the North Atlantic Ocean","year":2008,"lang":"en","type":"article","venue":"Proceedings of the Royal Society A Mathematical Physical and Engineering Sciences","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":294,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Microseism; Geology; Seismology; Amplitude; Wind wave; Waves and shallow water; Hindcast; Geophysics; Climatology; Oceanography; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.009145311517432251,"gpt":0.1877689017422587,"spread":0.1786235902248264,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004066505,0.0001087394,0.0001957842,0.00001257387,0.0003275114,0.0000494704,0.0005624046,0.00002355463,0.00000468295],"category_scores_gemma":[0.00007964612,0.00004427585,0.0001724262,0.000506787,0.0007278332,0.00008270807,0.00003524922,0.0001432213,0.000001438802],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002254294,"about_ca_system_score_gemma":0.00001067417,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001396588,"about_ca_topic_score_gemma":0.000003904198,"domain_scores_codex":[0.9990367,0.000005801047,0.000200488,0.0001474312,0.0003710059,0.0002385557],"domain_scores_gemma":[0.9994457,0.0003441501,0.00008148015,0.00006257457,0.00002616455,0.00003992483],"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":[0.00002142884,0.000321149,0.8813237,0.0008444872,0.0001647871,0.000001574784,0.02175504,0.06264026,0.0003886822,0.02982527,0.00158854,0.001125087],"study_design_scores_gemma":[0.00008498608,0.00006260524,0.1788975,0.0000468456,0.00002945799,0.000006499988,0.001335027,0.8101018,0.0000777243,0.009166465,0.00008427115,0.0001067819],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9988757,0.0001096355,0.0000406601,0.0005234922,0.00002136959,0.00007937763,0.000003147914,0.000008442499,0.0003381437],"genre_scores_gemma":[0.9994182,0.0000390145,0.0004120965,0.00004905647,0.0000499377,3.432783e-7,4.186373e-7,0.00000189355,0.00002903017],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7474616,"threshold_uncertainty_score":0.2681732,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2064903949","doi":"10.1016/s0267-7261(02)00008-8","title":"Comparing shear-wave velocity profiles inverted from multichannel surface wave with borehole measurements","year":2002,"lang":"en","type":"article","venue":"Soil Dynamics and Earthquake Engineering","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":284,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Borehole; Geology; Surface wave; Wave velocity; Seismology; Shear (geology); Mineralogy; Geodesy; Geotechnical engineering; Optics","retraction":null,"screen_n_in":null,"score":{"opus":0.03261646460313791,"gpt":0.1717019330316376,"spread":0.1390854684284996,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001380021,0.0002369659,0.0002967941,0.00006848116,0.0001596898,0.0001192645,0.00008284192,0.00007549776,0.0002385096],"category_scores_gemma":[0.00002467072,0.0002023827,0.00005511288,0.0002318289,0.00004441239,0.0001722758,0.00001820499,0.0002047227,0.00002497493],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001147399,"about_ca_system_score_gemma":0.00001028484,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005407612,"about_ca_topic_score_gemma":0.003330957,"domain_scores_codex":[0.9987398,0.00002296493,0.0002129487,0.0003449472,0.0002915431,0.0003878238],"domain_scores_gemma":[0.9994271,0.00005815056,0.00005682516,0.0001834147,0.00004106974,0.0002334556],"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":[0.00001494114,0.00002209482,0.2429065,0.00003438858,0.0001813719,0.000029514,0.0003680675,0.7429347,0.00004139757,0.00002022936,0.00003426994,0.01341252],"study_design_scores_gemma":[0.0002797374,0.0000283177,0.3271686,0.0000414345,0.00002932212,0.000004433441,0.0001228882,0.6720509,0.0000243281,0.00001476641,0.00003593909,0.0001992964],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9953765,0.0005289646,0.003024942,0.0001101284,0.0001272936,0.00009964587,0.0001260887,0.00007826832,0.0005281569],"genre_scores_gemma":[0.9958131,0.0001007427,0.003570263,0.00006367304,0.0000672348,6.77633e-7,0.0002441744,0.00001253984,0.0001276462],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08426215,"threshold_uncertainty_score":0.8252928,"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":"W2085505927","doi":"10.1016/j.soildyn.2010.08.010","title":"Full scale experimental study on vibration scattering using open and in-filled (GeoFoam) wave barriers","year":2010,"lang":"en","type":"article","venue":"Soil Dynamics and Earthquake Engineering","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":254,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"","keywords":"Trench; Vibration; Structural engineering; Ground vibrations; Scale model; Rayleigh scattering; Finite element method; Rayleigh wave; Acoustics; Engineering; Vibration isolation; Surface wave; Materials science; Physics; Optics; Aerospace engineering; Composite material; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.009761487963762019,"gpt":0.2130096469578656,"spread":0.2032481589941036,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002282277,0.0001509619,0.0001892008,0.0001349642,0.0001479725,0.0002394885,0.00009080968,0.00005253178,0.0001064321],"category_scores_gemma":[0.00001615237,0.0001429783,0.00002475015,0.0001472087,0.00002816542,0.0002395562,0.00004410239,0.0001847348,0.000002409066],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005668537,"about_ca_system_score_gemma":0.00001524665,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001521823,"about_ca_topic_score_gemma":0.005309911,"domain_scores_codex":[0.999177,0.00001634538,0.0001760719,0.0002813739,0.0001135204,0.000235677],"domain_scores_gemma":[0.9996201,0.00003249372,0.00003343797,0.0001292274,0.0000079164,0.0001768695],"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":[0.0001413585,0.00009852952,0.5581112,0.00003262287,0.00008114386,0.00006144122,0.002029455,0.4111057,0.01358711,0.0001387239,0.000002084671,0.01461069],"study_design_scores_gemma":[0.0002989519,0.0001041217,0.3264902,0.000013094,0.000007035878,0.000008963613,0.001339042,0.671536,0.00005384507,0.00001031915,0.000006631276,0.0001317813],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9991186,0.00004393987,0.0001710962,0.00005390477,0.0002122161,0.0001693062,0.0000198615,0.00001668466,0.0001943839],"genre_scores_gemma":[0.999191,0.000008894215,0.0006458876,0.00005026882,0.00005056582,0.000001444222,0.00002530004,0.000007745719,0.00001892229],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2604303,"threshold_uncertainty_score":0.5830487,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2327371768","doi":"10.1190/1.3628095","title":"Field trials of distributed acoustic sensing for geophysical monitoring","year":2011,"lang":"en","type":"article","venue":"","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":211,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Distributed acoustic sensing; Geology; Field (mathematics); Geophysics; Field trial; Remote sensing; Acoustics; Computer science; Telecommunications; Physics; Fiber optic sensor","retraction":null,"screen_n_in":null,"score":{"opus":0.08469364980301597,"gpt":0.2718182509403453,"spread":0.1871246011373293,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002820505,0.00005481513,0.0002372874,0.00002659828,0.00004093268,0.000009066347,0.00005883939,0.00003140953,0.0006364391],"category_scores_gemma":[0.0002490598,0.0000377192,0.0001417424,0.00008603126,0.00001441777,0.00004539419,0.000003265896,0.00002893427,0.000009094438],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":6.574125e-7,"about_ca_system_score_gemma":0.000009807431,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003576516,"about_ca_topic_score_gemma":0.00005931104,"domain_scores_codex":[0.9994349,0.00002842487,0.000240795,0.00009809572,0.00007332458,0.0001244424],"domain_scores_gemma":[0.9991661,0.0005985178,0.00008035589,0.00008174053,0.00002955468,0.00004374481],"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":[0.001144987,0.0001577883,0.4221972,0.0002229258,0.0009314258,0.00002711007,0.0009485999,0.004746218,0.009742756,0.0005997753,0.004763063,0.5545181],"study_design_scores_gemma":[0.001481915,0.00123008,0.4550254,0.000110659,0.0009161869,0.000006332493,0.002959669,0.4235318,0.09558024,0.01696009,0.001514102,0.0006835428],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8994167,0.00005554386,0.09773372,0.00007400625,0.0003116661,0.0001116046,0.00019919,0.00002291007,0.002074681],"genre_scores_gemma":[0.9946336,0.000008726614,0.004997824,0.00003260446,0.0001751705,1.015333e-7,0.00004359636,0.000001061809,0.0001073488],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5538346,"threshold_uncertainty_score":0.6968562,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4220997854","doi":"10.1007/s10950-021-10062-9","title":"A review of the microtremor horizontal-to-vertical spectral ratio (MHVSR) method","year":2022,"lang":"en","type":"review","venue":"Journal of Seismology","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":208,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"BC Hydro (Canada); Western University","funders":"Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Strong","keywords":"Microtremor; Geology; Standardization; Seismology; Bedrock; Hydrogeology; Inversion (geology); Geophysics; Geotechnical engineering; Computer science; Tectonics; Geomorphology","retraction":null,"screen_n_in":null,"score":{"opus":0.04366727100721039,"gpt":0.3233202714697396,"spread":0.2796530004625292,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00145203,0.0002615469,0.002187314,0.0002263036,0.00009067587,0.00001544163,0.0009334821,0.0001315917,0.008117289],"category_scores_gemma":[0.000284894,0.0001424177,0.001542992,0.0007182601,0.00007336117,0.0000584164,0.00006272551,0.0008035525,0.00005710142],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003051818,"about_ca_system_score_gemma":0.00052956,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002419959,"about_ca_topic_score_gemma":0.00002078271,"domain_scores_codex":[0.9966263,0.001089789,0.00140091,0.00022388,0.0003734548,0.0002856351],"domain_scores_gemma":[0.9979686,0.0005684829,0.0009196073,0.0003234048,0.0000645466,0.0001554262],"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":[0.00001192011,0.00002583687,0.00003108249,0.006629117,0.0003791943,0.00006955049,0.00001863401,0.00004191815,0.000001145188,0.00003129441,0.009058142,0.9837022],"study_design_scores_gemma":[0.00007695148,0.0002898167,0.0000603276,0.007322286,0.001735066,0.002427648,0.0000194642,0.00003825733,0.000001444072,0.00007060705,0.9878126,0.00014549],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"review","genre_gemma":"review","genre_scores_codex":[0.00003336369,0.9961587,0.0002902741,0.001964378,0.0007811461,0.0002646163,0.0001085727,0.000002564759,0.0003964046],"genre_scores_gemma":[0.000003619794,0.9931514,0.002536405,0.003508511,0.0004873843,9.442472e-7,0.00003153097,0.000008332087,0.0002718705],"genre_candidate":"review","genre_consensus":"review","teacher_disagreement_score":0.9835567,"threshold_uncertainty_score":0.9927894,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2046816840","doi":"10.2118/140561-pa","title":"First Downhole Application of Distributed Acoustic Sensing for Hydraulic-Fracturing Monitoring and Diagnostics","year":2012,"lang":"en","type":"article","venue":"SPE Drilling & Completion","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":162,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Shell (Canada)","funders":"","keywords":"Hydraulic fracturing; Tight gas; Distributed acoustic sensing; Well stimulation; Completion (oil and gas wells); Directional drilling; Petroleum engineering; Drilling; Geology; Engineering; Fiber optic sensor; Optical fiber; Telecommunications; Mechanical engineering; Reservoir engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.01794578032835719,"gpt":0.2321114397524533,"spread":0.2141656594240961,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001827098,0.00008709343,0.0001479428,0.00004959143,0.0001862779,0.00002762746,0.00004601485,0.00003980709,0.00001133971],"category_scores_gemma":[0.0001061762,0.00008123057,0.00003772393,0.000112079,0.00003005597,0.0001097616,0.000007276155,0.00005148457,0.000006274237],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007262494,"about_ca_system_score_gemma":0.000003840516,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0009666259,"about_ca_topic_score_gemma":0.00005742165,"domain_scores_codex":[0.9993483,0.00001310719,0.0001845747,0.0001345947,0.0001147928,0.0002045942],"domain_scores_gemma":[0.9992236,0.0004430882,0.000116832,0.0001026676,0.00004262584,0.00007122444],"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":[0.0000231439,0.0000212175,0.6964725,0.0001322055,0.0000392435,4.715832e-7,0.0002509223,0.2784281,0.001990213,0.00004407118,0.00004871558,0.02254924],"study_design_scores_gemma":[0.0001262643,0.00002527744,0.4817247,0.00004597795,0.0000734061,0.000003115388,0.0001369614,0.5122787,0.001009544,0.0003725218,0.004090507,0.0001130538],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.6825133,0.0004507687,0.3164811,0.0001116176,0.0001693564,0.0001161643,0.0001063257,0.00002031151,0.00003100089],"genre_scores_gemma":[0.9940497,0.0002170679,0.004805733,0.0000188015,0.00047031,6.1483e-7,0.0004313691,0.000003807461,0.000002598732],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3116754,"threshold_uncertainty_score":0.3312486,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2063820785","doi":"10.4133/jeeg5.3.1","title":"Comparing Shear-Wave Velocity Profiles from MASW with Borehole Measurements in Unconsolidated Sediments, Fraser River Delta, B.C., Canada","year":2000,"lang":"en","type":"article","venue":"Journal of Environmental and Engineering Geophysics","topic":"Seismic Waves and Analysis","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":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Borehole; Geology; Surface wave; Wave velocity; Test site; Seismology; Shear (geology); Geophysics; Mineralogy; Geotechnical engineering; Optics; Petrology","retraction":null,"screen_n_in":null,"score":{"opus":0.008889537808434813,"gpt":0.1432366134708642,"spread":0.1343470756624294,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007013987,0.0001260372,0.0002077746,0.00003150279,0.00004247544,0.00001778465,0.00006238479,0.00002446648,0.0004458681],"category_scores_gemma":[0.000001337477,0.00009875081,0.00002927272,0.00006791911,0.00003066808,0.0001641152,0.000006519287,0.0001542463,0.000004939782],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003146433,"about_ca_system_score_gemma":0.00002825381,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.1464694,"about_ca_topic_score_gemma":0.01313314,"domain_scores_codex":[0.9992039,0.00001596417,0.0002037023,0.000113168,0.0002902563,0.0001729974],"domain_scores_gemma":[0.999736,0.00002309706,0.00006583393,0.00006113123,0.000004128207,0.0001098398],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00007081973,0.00004762036,0.8705277,0.000009412153,0.0001722095,0.0000852924,0.0001209403,0.1193721,0.0007506111,3.669824e-7,0.00008862992,0.008754216],"study_design_scores_gemma":[0.0005013674,0.00004669156,0.9794477,0.00004219594,0.00003833811,0.000006102422,0.0001060299,0.01889875,0.0001584352,0.00001700246,0.0006074312,0.0001299354],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9994091,0.0002860642,0.00002275948,0.00002306707,0.00004862539,0.00003443942,0.00009899108,0.000002727309,0.00007419668],"genre_scores_gemma":[0.9987999,0.0001008678,0.0008647105,0.00006931832,0.0000691169,1.605766e-7,0.00006303234,0.000004260021,0.00002860143],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1333362,"threshold_uncertainty_score":0.8592144,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2044872654","doi":"10.1126/science.1229379","title":"Stress State in the Largest Displacement Area of the 2011 Tohoku-Oki Earthquake","year":2013,"lang":"en","type":"article","venue":"Science","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":146,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Victoria; McGill University","funders":"Japan Society for the Promotion of Science; Natural Environment Research Council; United States Science Support Program","keywords":"Geology; Seismology; Crust; Borehole; Magnitude (astronomy); Interplate earthquake; Stress (linguistics); Intraplate earthquake; Tectonics; Geophysics; Geotechnical engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.00992081597347021,"gpt":0.1954872574287501,"spread":0.1855664414552799,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006543995,0.00006458912,0.00007894493,0.00005243738,0.0001751627,0.00008738789,0.0007710761,0.00001123611,0.001667362],"category_scores_gemma":[0.00003084688,0.00002892634,0.00003933382,0.0005818136,0.0003898195,0.0002343356,0.00002775319,0.0000783223,0.0001226853],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002410048,"about_ca_system_score_gemma":0.00005746178,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01146142,"about_ca_topic_score_gemma":0.005562406,"domain_scores_codex":[0.9988815,0.00005346237,0.0001475769,0.0001772513,0.0004771751,0.0002630331],"domain_scores_gemma":[0.9994781,0.00007291578,0.00006527419,0.0003024648,0.00003421615,0.00004701303],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000001793191,0.00002002679,0.9839005,0.000003979947,0.000002728347,0.000001048442,0.0005172088,0.004560168,0.0001256274,0.00005197946,0.000453777,0.01036119],"study_design_scores_gemma":[0.00005246055,0.00002075579,0.9863055,0.00001014791,0.000003313656,8.587324e-7,0.0006572767,0.01103078,0.000189952,0.0008584902,0.0008217302,0.00004869539],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9958584,0.0001290315,0.00001933931,0.001054651,0.0001280704,0.0001315264,0.00006421246,0.000003068127,0.002611738],"genre_scores_gemma":[0.9989486,0.00002920853,0.00003421766,0.0004068295,0.00001216135,0.000001048197,0.000004010415,6.47501e-7,0.0005633164],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01031249,"threshold_uncertainty_score":0.9992452,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1982675089","doi":"10.1139/t09-026","title":"Measuring shear and compression wave velocities of soil using bender–extender elements","year":2009,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":137,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"Defence Science and Technology Agency - Singapore; Petroleum Technology Research Centre","keywords":"Acoustics; Shear (geology); Sine wave; Materials science; Oscilloscope; Geotechnical engineering; Geology; Composite material; Engineering; Voltage; Physics; Electrical engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.04658887536743618,"gpt":0.2214226870901398,"spread":0.1748338117227036,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002933003,0.00009871188,0.0001891221,0.0002005275,0.0002788739,0.00006799824,0.0001174554,0.00007927365,0.0005067074],"category_scores_gemma":[0.00002995663,0.00008153786,0.00007198835,0.0001314536,0.00007064157,0.0001316466,0.000005774195,0.0002645908,0.000002345295],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001944024,"about_ca_system_score_gemma":0.0001749385,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.03310318,"about_ca_topic_score_gemma":0.005917674,"domain_scores_codex":[0.9989616,0.00004332584,0.00029149,0.0001313958,0.0002392533,0.0003329437],"domain_scores_gemma":[0.9992373,0.0000240745,0.00009883443,0.00009237618,0.00004757768,0.0004998237],"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":[0.00006191285,0.00003760462,0.03731073,0.00003823058,0.0002442988,0.0005629765,0.0003335683,0.2845136,0.001311846,0.000215176,0.001672604,0.6736975],"study_design_scores_gemma":[0.0004533083,0.0001722001,0.3784553,0.0001815586,0.0001060493,0.0006032012,0.0007956554,0.6112804,0.00014998,0.00523272,0.002254258,0.0003153886],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9950206,0.001527772,0.00168185,0.0007838213,0.0001097396,0.00005318975,0.00005283152,0.00001040872,0.0007597396],"genre_scores_gemma":[0.9978706,0.0001904445,0.001253564,0.0005459878,0.0001032335,2.51447e-8,0.000007954309,0.000002289988,0.00002592908],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6733821,"threshold_uncertainty_score":0.9733354,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1836947475","doi":"10.1029/2003gc000520","title":"Strong directivity of ocean‐generated seismic noise","year":2004,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Microseism; Geology; Swell; Seismology; Seismic noise; Noise (video); Slowness; Ambient noise level; Azimuth; Geodesy; Geophysics; Acoustics; Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.007649651997355588,"gpt":0.1887984503431812,"spread":0.1811487983458256,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001816244,0.0002421476,0.0004172878,0.00004317239,0.0001310798,0.00004515479,0.0002780783,0.000110229,0.0002255561],"category_scores_gemma":[0.00002169287,0.0002222005,0.0002041211,0.0004706978,0.0000837173,0.0001425451,0.00001990353,0.0001642803,0.0001018736],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001553623,"about_ca_system_score_gemma":0.0001276089,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0156964,"about_ca_topic_score_gemma":0.0001183439,"domain_scores_codex":[0.9984279,0.0000368015,0.0003700436,0.0004026646,0.0003602661,0.0004023421],"domain_scores_gemma":[0.9989952,0.00005093421,0.0002475716,0.000430641,0.0001199193,0.0001556841],"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":[0.00009297879,0.0003457955,0.1537527,0.0008390339,0.0006522091,0.00008081018,0.0004899704,0.7725061,0.06203866,0.0001566863,0.0007324405,0.008312631],"study_design_scores_gemma":[0.005558017,0.0005050591,0.1984643,0.0009194753,0.0008364457,0.0001338087,0.004012192,0.3979734,0.3664315,0.01498426,0.006373771,0.003807747],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9935061,0.0003690032,0.0003889987,0.00006761627,0.0002204031,0.0001016915,0.0005271612,0.00006115955,0.00475792],"genre_scores_gemma":[0.9985285,0.00002669536,0.00007929674,0.00003954206,0.0003551386,6.939604e-7,0.0005499927,0.000006996398,0.0004131699],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3745327,"threshold_uncertainty_score":0.9908582,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2130315788","doi":"10.1190/1.1468604","title":"Atmospheric sources for audio-magnetotelluric (AMT) sounding","year":2002,"lang":"en","type":"article","venue":"Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":111,"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":"Depth sounding; Amplitude; Magnetotellurics; Geology; Daytime; Lightning detection; Ionosphere; Attenuation; Geophysics; SIGNAL (programming language); Environmental science; Remote sensing; Acoustics; Meteorology; Physics; Atmospheric sciences; Computer science; Thunderstorm; Optics","retraction":null,"screen_n_in":null,"score":{"opus":0.01558270712591559,"gpt":0.1795251416307105,"spread":0.1639424345047949,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00007475451,0.0001304114,0.0001761132,0.00001161691,0.0002508058,0.00008314376,0.0001722534,0.00004184352,0.002519845],"category_scores_gemma":[0.00001575875,0.0001104374,0.0001583453,0.000339137,0.00004454731,0.0001414025,0.000007342318,0.00006729256,0.0008999545],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003227655,"about_ca_system_score_gemma":0.000006825327,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0006005015,"about_ca_topic_score_gemma":0.0000531347,"domain_scores_codex":[0.999099,0.00001726406,0.0001473725,0.0002341794,0.0001608004,0.0003413459],"domain_scores_gemma":[0.9995144,0.0001313102,0.00007242581,0.0001702613,0.00002412126,0.00008745329],"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":[0.00003211086,0.0001157004,0.1030331,0.0001339254,0.0002833719,0.00002358752,0.001361394,0.04767574,0.0002078729,0.0009529399,0.01358053,0.8325997],"study_design_scores_gemma":[0.0005309163,0.0002876139,0.05695624,0.00002026647,0.0001748968,0.000007644197,0.0005979446,0.7711708,0.0000573646,0.01636368,0.1532062,0.0006264089],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9878783,0.00151093,0.00364398,0.0002659726,0.000310536,0.0001247813,0.00006028551,0.0000679773,0.006137299],"genre_scores_gemma":[0.9874453,0.0001633282,0.002889955,0.0004539804,0.000626341,0.0000015025,0.00006925951,0.000006382218,0.00834395],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8319733,"threshold_uncertainty_score":0.999878,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2082539625","doi":"10.1029/2002jb002258","title":"Application of the S transform to prestack noise attenuation filtering","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Western University","funders":"","keywords":"Attenuation; Acoustics; Algorithm; Filter (signal processing); Residual; Noise (video); Computer science; Wavelet transform; Fourier transform; SIGNAL (programming language); Geology; Wavelet; Mathematics; Physics; Optics; Mathematical analysis; Artificial intelligence","retraction":null,"screen_n_in":null,"score":{"opus":0.02673731183594984,"gpt":0.2922631650392468,"spread":0.2655258532032969,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007268801,0.00006368163,0.0001587634,0.00001856898,0.0001146852,0.00003621577,0.0003211286,0.00002881713,0.0002742958],"category_scores_gemma":[0.0003180858,0.00003725194,0.0001487759,0.0006098401,0.00007890215,0.0001483751,0.000009364644,0.0002363581,0.00004130264],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009501521,"about_ca_system_score_gemma":0.00009331787,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001492294,"about_ca_topic_score_gemma":0.0002575711,"domain_scores_codex":[0.9984208,0.0001738723,0.0002853137,0.0001013098,0.0007965891,0.0002221122],"domain_scores_gemma":[0.9990178,0.0002873382,0.0001132261,0.0001704944,0.0002695255,0.0001415634],"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":[0.0006272803,0.000423104,0.2716876,0.0001612639,0.0003096889,0.00001735251,0.001242044,0.09096529,0.0408801,0.003126203,0.005314232,0.5852458],"study_design_scores_gemma":[0.0003682477,0.0006297588,0.9309377,0.00008221684,0.00003694213,0.000008346017,0.000680062,0.02010793,0.009003346,0.01425282,0.02376724,0.0001253878],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9934033,0.0001215485,0.002960233,0.001016427,0.00005711424,0.0001521388,0.000009744181,0.000001982213,0.002277487],"genre_scores_gemma":[0.998482,0.00003809493,0.001017429,0.0000510581,0.0001151518,6.947415e-7,0.000001242236,0.000002567529,0.000291697],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6592501,"threshold_uncertainty_score":0.3003347,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2148414895","doi":"10.1190/geo2011-0077.1","title":"Solid angles and the impact of receiver-array geometry on microseismic moment-tensor inversion","year":2011,"lang":"en","type":"article","venue":"Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium","keywords":"Inversion (geology); Microseism; Mathematics; Mathematical analysis; Inverse problem; Geometry; Geodesy; Geology; Seismology","retraction":null,"screen_n_in":null,"score":{"opus":0.01611488015309924,"gpt":0.2286445403943259,"spread":0.2125296602412266,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001264317,0.0001136333,0.0002050091,0.00006497045,0.0001072374,0.00001786451,0.000145229,0.00003707436,0.0004072548],"category_scores_gemma":[0.000009722358,0.00006307318,0.0001538607,0.0002427006,0.0001940285,0.00008720661,0.0000106232,0.00008604487,0.00009367116],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003356368,"about_ca_system_score_gemma":0.00001696089,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01114238,"about_ca_topic_score_gemma":0.00002137875,"domain_scores_codex":[0.9993482,0.00004852708,0.0001322303,0.0001594815,0.0001292413,0.0001823022],"domain_scores_gemma":[0.9995331,0.00008257156,0.0001052462,0.000189346,0.00002852369,0.00006121984],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.002418022,0.0004242152,0.8092025,0.0001134829,0.001537481,0.0000280676,0.009210607,0.005667679,0.01041545,0.00112453,0.007782859,0.1520751],"study_design_scores_gemma":[0.001050029,0.000491139,0.9765614,0.00002983871,0.0001042856,0.000003364564,0.0007828432,0.007618735,0.00275165,0.01004255,0.0003362056,0.000227994],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9972908,0.0001805089,0.00002768341,0.00006969909,0.00006400234,0.00007113328,0.0001120095,0.000008632609,0.002175554],"genre_scores_gemma":[0.9990759,0.0002933088,0.00009781143,0.0002187272,0.0000568266,2.107113e-7,0.00004031682,0.000002734701,0.0002141519],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1673589,"threshold_uncertainty_score":0.9954425,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2160748827","doi":"10.1111/j.1365-246x.2011.05302.x","title":"Trans-dimensional inversion of microtremor array dispersion data with hierarchical autoregressive error models","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Microtremor; Autoregressive model; Geology; Inverse theory; Inversion (geology); Seismology; Dispersion (optics); Geodesy; Mathematics; Statistics; Physics; Optics","retraction":null,"screen_n_in":null,"score":{"opus":0.04290334620229783,"gpt":0.2376790054226062,"spread":0.1947756592203084,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001454041,0.0001431079,0.0002115971,0.0001238018,0.0001209861,0.000034573,0.0007333459,0.0000500259,0.002223323],"category_scores_gemma":[0.00001338685,0.00009179941,0.000127775,0.0001102771,0.0001867621,0.000622365,0.0000353943,0.0003048741,0.00002668631],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007824419,"about_ca_system_score_gemma":0.0000813034,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0006586024,"about_ca_topic_score_gemma":0.00006775699,"domain_scores_codex":[0.9985164,0.00006193072,0.0002816122,0.0002789051,0.0006564133,0.0002047084],"domain_scores_gemma":[0.999189,0.00007147922,0.0001923612,0.0002136843,0.00013932,0.000194209],"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":[0.02248558,0.00610383,0.348578,0.0001974896,0.009581107,0.003178784,0.01243361,0.1707875,0.05671734,0.007614989,0.03782335,0.3244984],"study_design_scores_gemma":[0.001457648,0.00051132,0.1274946,0.0002114029,0.0001908197,0.000291015,0.0003329044,0.8470673,0.0008857885,0.0195271,0.001631155,0.0003989689],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9868994,0.00008668318,0.007598964,0.001339826,0.0004076945,0.00006574927,0.0005152556,0.00001314695,0.003073234],"genre_scores_gemma":[0.9910368,0.00003156816,0.00778764,0.0002304148,0.0003160613,1.428978e-7,0.0003847888,0.00000462067,0.0002079766],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6762798,"threshold_uncertainty_score":0.9986888,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2734956986","doi":"10.1139/cgj-2016-0302","title":"Tool for analysis of multichannel analysis of surface waves (MASW) field data and evaluation of shear wave velocity profiles of soils","year":2017,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"Háskóli Íslands; Landsvirkjun","keywords":"Surface wave; Geology; Software; Geotechnical engineering; Dispersion (optics); Wave velocity; Inversion (geology); Soil water; Shear (geology); Acoustics; Seismology; Soil science; Engineering; Optics; Computer science; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.07840653653722526,"gpt":0.3045442493736626,"spread":0.2261377128364374,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002440034,0.0001073737,0.0007173964,0.0006608991,0.0001762314,0.00003488446,0.0005512209,0.0001307616,0.0005310248],"category_scores_gemma":[0.001235201,0.0000889041,0.0003221478,0.0006214434,0.000210252,0.000151079,0.0000344449,0.00013165,1.724308e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001062138,"about_ca_system_score_gemma":0.0003585287,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1266335,"about_ca_topic_score_gemma":0.07992195,"domain_scores_codex":[0.9983341,0.000102155,0.0006588012,0.0002328032,0.0004502895,0.0002218145],"domain_scores_gemma":[0.9975201,0.0003477973,0.0007683113,0.000690279,0.0004555533,0.0002179222],"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":[0.0001123369,0.00005186333,0.2548287,0.0001005005,0.01212587,0.000005979798,0.0002826801,0.6442643,0.0005055037,0.00004012131,0.0003232656,0.0873588],"study_design_scores_gemma":[0.0001601971,0.00006047543,0.3439628,0.00001963255,0.007316517,0.000001069146,0.0001256415,0.6478477,0.0002821928,0.0001328511,0.00002817822,0.00006267213],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9939944,0.0003826017,0.001726558,0.000412479,0.00003774917,0.000142135,0.003254636,0.000001528767,0.00004787229],"genre_scores_gemma":[0.9975616,0.0001542657,0.001968736,0.00003120233,0.00002444428,2.700129e-7,0.0002451549,0.000002333587,0.00001199745],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08913413,"threshold_uncertainty_score":0.9368671,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2089897414","doi":"10.1016/j.jastp.2012.01.018","title":"Infrasound production by bolides: A global statistical study","year":2012,"lang":"en","type":"article","venue":"Journal of Atmospheric and Solar-Terrestrial Physics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Natural Resources Canada; Western University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Infrasound; Amplitude; Range (aeronautics); Scaling; Exponent; Ranging; Yield (engineering); Waveform; Function (biology); Energy (signal processing); Physics; Environmental science; Wind speed; Meteorology; Computational physics; Statistics; Mathematics; Geodesy; Geology; Acoustics; Optics; Materials science; Geometry","retraction":null,"screen_n_in":null,"score":{"opus":0.01211579082539462,"gpt":0.2425864026047018,"spread":0.2304706117793072,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004053745,0.0001393149,0.0003149281,0.000002604913,0.0001290467,0.0001020467,0.000107662,0.00004364242,0.000144114],"category_scores_gemma":[0.00009046599,0.0001013276,0.00008265887,0.0002048298,0.00007194559,0.000543286,0.00001063339,0.0001721388,0.00001325819],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001130989,"about_ca_system_score_gemma":0.00005613752,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0006590943,"about_ca_topic_score_gemma":0.00001947049,"domain_scores_codex":[0.9987575,0.0001256429,0.0003817386,0.0001241889,0.0003505317,0.0002603745],"domain_scores_gemma":[0.9992707,0.00008601104,0.0002831467,0.00009290768,0.00003472404,0.0002324639],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002371918,0.0003221327,0.9208256,0.000006503441,0.0002156775,0.00001092325,0.0003391095,0.0009438685,0.00001337332,0.00002662649,0.006127789,0.07093122],"study_design_scores_gemma":[0.002637637,0.002248068,0.958859,0.00003841947,0.0008497119,0.0001499946,0.005376247,0.009649231,0.00001395629,0.007578551,0.01204905,0.0005501112],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9906812,0.0007968995,0.007106093,0.00006673566,0.001037028,0.00009891388,0.00003378751,0.00000664767,0.0001726692],"genre_scores_gemma":[0.9953634,0.0001733421,0.002095673,0.00007103749,0.002240413,1.685131e-7,0.00001434347,0.00000319194,0.00003839194],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0703811,"threshold_uncertainty_score":0.4132018,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2151860765","doi":"10.1190/1.2937172","title":"Application of seismic interferometry to extract P- and S-wave propagation and observation of shear-wave splitting from noise data at Cold Lake, Alberta, Canada","year":2008,"lang":"en","type":"article","venue":"Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Shear wave splitting; Seismology; Surface wave; Borehole; Interferometry; Rayleigh wave; Shear (geology); Polarization (electrochemistry); Waveform; Geodesy; Optics; Physics; Geotechnical engineering; Radar; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.03041725311186589,"gpt":0.1984779228352729,"spread":0.168060669723407,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000819376,0.00008790449,0.0001820259,0.00003434838,0.00007503312,0.000008782305,0.00008292493,0.00002735419,0.00002849838],"category_scores_gemma":[0.00003273882,0.00008201021,0.00001477322,0.0002372701,0.00004106018,0.0001784132,0.00004367286,0.00004840656,0.000002696292],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006737918,"about_ca_system_score_gemma":0.00006021265,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.7304046,"about_ca_topic_score_gemma":0.474749,"domain_scores_codex":[0.9992003,0.00002163146,0.0002339891,0.0002567871,0.0001801885,0.0001070566],"domain_scores_gemma":[0.9992776,0.0001665316,0.00016684,0.0002752529,0.00004798017,0.00006580334],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006289763,0.00003153415,0.9271521,0.0000938597,0.00008321751,0.000004646356,0.000598439,0.002695345,0.005926818,0.00003084866,0.0004166642,0.06290361],"study_design_scores_gemma":[0.00009889528,0.00002838956,0.7787374,0.00001808056,0.00003239394,0.00000214318,0.00006921168,0.2188492,0.001035496,0.0001169381,0.0009280261,0.00008380849],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9971266,0.00008324502,0.001670764,0.0001457276,0.00003305217,0.0001396586,0.0007113222,0.000003431629,0.00008618346],"genre_scores_gemma":[0.9967871,0.0000437122,0.001320062,0.0001608575,0.00005369642,6.668529e-7,0.001499743,0.000003112248,0.0001310391],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2556555,"threshold_uncertainty_score":0.5348355,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1976566745","doi":"10.1130/g21488.1","title":"Conduit implosion during Vulcanian eruptions","year":2005,"lang":"en","type":"article","venue":"Geology","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"McGill University","funders":"","keywords":"Library science; Humanities; Technical university; History; Art; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.00843711920690486,"gpt":0.202768878735877,"spread":0.1943317595289722,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00005627591,0.00005705344,0.00009241483,0.00006304876,0.0001357435,0.00001044295,0.00009141029,0.00004745077,0.01297678],"category_scores_gemma":[0.000006652879,0.00004746485,0.00004237943,0.00009998855,0.00004629786,0.00007215962,0.00000826204,0.00006807796,0.001813724],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002210982,"about_ca_system_score_gemma":0.00001085336,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003182731,"about_ca_topic_score_gemma":0.004920344,"domain_scores_codex":[0.9994536,0.00002504068,0.0001058522,0.0001434885,0.00005597071,0.0002160463],"domain_scores_gemma":[0.9997574,0.00002547198,0.00002759943,0.0001111773,0.00001138375,0.00006693444],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002060206,0.0000230348,0.9231693,0.000007818589,0.0000571025,0.00003314739,0.0002536203,0.0160161,0.0009294084,0.0006213151,0.001606746,0.05726181],"study_design_scores_gemma":[0.0002021789,0.00003506934,0.9324498,0.000002033977,0.00001750027,0.00004967172,0.00009814627,0.008574982,0.0001232001,0.0006803165,0.05765746,0.0001096815],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9882492,0.00019781,0.00003303239,0.002549382,0.00009320297,0.00002588484,0.00001359167,0.00003140089,0.008806484],"genre_scores_gemma":[0.9962212,0.00006519195,0.000338622,0.0007285497,0.0002216501,2.529414e-7,0.00005694855,0.000001249188,0.00236628],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05715213,"threshold_uncertainty_score":0.9989635,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1969052312","doi":"10.1785/0119990098","title":"Integrated Use of Seismograph and Strong-Motion Data to Determine Soil Amplification: Response of the Fraser River Delta to the Duvall and Georgia Strait Earthquakes","year":2000,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismometer; Seismology; Delta; River delta; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.03807166264619596,"gpt":0.2242986636695276,"spread":0.1862270010233316,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000522584,0.0001312027,0.0002899974,0.00001863349,0.0001369023,0.00001804309,0.0006209672,0.00007143553,0.001108885],"category_scores_gemma":[0.0001950261,0.00006226084,0.0001726363,0.0004004934,0.0009581924,0.0000302627,0.0001264908,0.0001276481,0.000004230005],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002314898,"about_ca_system_score_gemma":0.0000274114,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01853287,"about_ca_topic_score_gemma":0.00002690848,"domain_scores_codex":[0.9985763,0.0003554503,0.0003524676,0.0002806824,0.0002708271,0.0001643121],"domain_scores_gemma":[0.9984893,0.0005374906,0.0002279277,0.0006008393,0.0000738026,0.00007068759],"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":[0.00232505,0.000375407,0.1872472,0.0001029033,0.0006557435,0.000001740476,0.003508586,0.07369467,0.001435125,0.00002995458,0.07705096,0.6535726],"study_design_scores_gemma":[0.0001524252,0.0002361188,0.777917,0.00003338411,0.00007746544,0.000002517641,0.0006933692,0.007040122,0.000134211,0.0000525497,0.2135763,0.00008460326],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.969393,0.0001364796,0.0005622716,0.02882839,0.00001938774,0.0002145457,0.00081978,0.000004631621,0.00002147213],"genre_scores_gemma":[0.9891332,0.0001847399,0.005275068,0.004888645,0.00001430766,8.581207e-7,0.0000420637,0.000002997076,0.0004580916],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.653488,"threshold_uncertainty_score":0.9998043,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2146795711","doi":"10.1190/1.1581031","title":"Repeatability of multimode Rayleigh-wave dispersion studies","year":2003,"lang":"en","type":"article","venue":"Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":92,"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":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Rayleigh wave; Dispersion (optics); Rayleigh scattering; Surface wave; Phase velocity; Optics; Geology; Repeatability; Materials science; Physics; Mathematics; Statistics","retraction":null,"screen_n_in":null,"score":{"opus":0.04010530782189491,"gpt":0.2410872347272822,"spread":0.2009819269053872,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001639347,0.00008936152,0.0002159607,0.00002319731,0.00007902998,0.000007353045,0.00006340435,0.00002518584,0.0002420575],"category_scores_gemma":[0.00007950957,0.00006629379,0.0001098248,0.0001961706,0.0000958945,0.00009255482,0.00000706639,0.00005587052,0.00005569585],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002541743,"about_ca_system_score_gemma":0.00001730524,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001002966,"about_ca_topic_score_gemma":0.0001033637,"domain_scores_codex":[0.9992635,0.00006120877,0.0001687141,0.0001906232,0.0001609655,0.0001550434],"domain_scores_gemma":[0.9994655,0.0001157033,0.00007301547,0.0002429356,0.00005704101,0.00004580348],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006842438,0.0002154424,0.9062933,0.0002161144,0.0005584987,0.00002229622,0.002157409,0.01150148,0.0007290797,0.003052913,0.0006150205,0.07456997],"study_design_scores_gemma":[0.0009235413,0.0003012145,0.8853995,0.00006845428,0.0003708395,0.000006029498,0.006978258,0.03835075,0.004580472,0.05468536,0.007632241,0.0007033353],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9961032,0.0009711074,0.0001010248,0.00004223969,0.0001412266,0.00005113902,0.0000572748,0.00001225855,0.002520477],"genre_scores_gemma":[0.9983657,0.0002259118,0.001045126,0.00006525277,0.00003881522,2.032697e-7,0.00003763212,0.000001634814,0.0002197194],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07386664,"threshold_uncertainty_score":0.2703382,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1981535646","doi":"10.1190/1.2987375","title":"Robust processing of magnetotelluric data in the AMT dead band using the continuous wavelet transform","year":2008,"lang":"en","type":"article","venue":"Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Magnetotellurics; Wavelet; Jackknife resampling; Attenuation; Energy (signal processing); Algorithm; Geology; Coherence (philosophical gambling strategy); Amplitude; Geodesy; Computer science; Remote sensing; Mathematics; Optics; Physics; Statistics; Artificial intelligence","retraction":null,"screen_n_in":null,"score":{"opus":0.06522849476983458,"gpt":0.2269154215794977,"spread":0.1616869268096631,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002680476,0.00009723201,0.0001722785,0.00003001001,0.0002066122,0.00003405885,0.0005563864,0.00002927738,0.00006775142],"category_scores_gemma":[0.000008952013,0.00005168695,0.00004742536,0.0004940332,0.0001410602,0.0002543584,0.00001026803,0.000131067,0.000008072572],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001567153,"about_ca_system_score_gemma":0.00005939871,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005226752,"about_ca_topic_score_gemma":0.0006967167,"domain_scores_codex":[0.9991184,0.00005165609,0.0001951236,0.0001759194,0.0002468472,0.0002120364],"domain_scores_gemma":[0.999413,0.00009599606,0.00007974116,0.0003669939,0.00002256589,0.00002167589],"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":[0.000108127,0.0002653143,0.134471,0.0002349671,0.0001404521,0.0002839022,0.01386948,0.07463077,0.000411203,0.0001218692,0.0007213559,0.7747416],"study_design_scores_gemma":[0.0005062241,0.0001060187,0.2709852,0.00005578906,0.0001729712,0.000124415,0.003946611,0.7181505,0.000136284,0.00210623,0.003371348,0.0003384776],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9959931,0.0006876237,0.001472982,0.0002757177,0.00003716515,0.0001083123,0.0001080959,0.000005789027,0.001311234],"genre_scores_gemma":[0.9988379,0.0001365457,0.0004323362,0.000255812,0.0001178521,1.958813e-7,0.000134885,0.00000266636,0.00008180534],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7744031,"threshold_uncertainty_score":0.790132,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2076262430","doi":"10.1103/physreve.65.066605","title":"Diffusing acoustic wave spectroscopy","year":2002,"lang":"en","type":"article","venue":"Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; University of Oxford","keywords":"Autocorrelation; Physics; Computational physics; Diffusion; Scattering; Spectroscopy; Mesoscopic physics; Speed of sound; Particle velocity; Acoustic wave; Range (aeronautics); Optics; Acoustics; Materials science; Condensed matter physics; Quantum mechanics","retraction":null,"screen_n_in":null,"score":{"opus":0.0173338745639854,"gpt":0.2745255430520147,"spread":0.2571916684880293,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001296074,0.0004325082,0.0008418913,0.00005164676,0.0004155241,0.0001054646,0.0002244402,0.00009574733,0.001952526],"category_scores_gemma":[0.0001020513,0.000329682,0.0002589916,0.0002924973,0.0004340953,0.0002635017,0.0001420706,0.0006301457,0.000580747],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002048171,"about_ca_system_score_gemma":0.00001618819,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00004917004,"about_ca_topic_score_gemma":0.00001499178,"domain_scores_codex":[0.99753,0.0001397663,0.0006141489,0.0006925033,0.0004138166,0.0006096988],"domain_scores_gemma":[0.9986156,0.0004336867,0.0001458662,0.0003660133,0.00005892869,0.0003799279],"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":[0.0002692384,0.003118132,0.008099767,0.006208753,0.0022229,0.001531313,0.004847887,0.003568429,0.003031169,0.0912124,0.14484,0.73105],"study_design_scores_gemma":[0.0006244475,0.0005425281,0.006248115,0.0008175217,0.0007220419,0.00006362343,0.000147895,0.791243,0.00009381414,0.1960605,0.002654115,0.000782389],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.6225041,0.07257385,0.06572755,0.0215719,0.005127038,0.002704464,0.003241007,0.0008381748,0.2057119],"genre_scores_gemma":[0.976835,0.01755668,0.001733651,0.0008570842,0.001050624,0.000004058377,0.000485095,0.00002708267,0.001450736],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7876746,"threshold_uncertainty_score":0.9999155,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3159347950","doi":"10.1029/2021jb022358","title":"Distributed Acoustic Sensing in Volcano‐Glacial Environments—Mount Meager, British Columbia","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Calgary","funders":"Natural Resources Canada; Government of Canada","keywords":"Induced seismicity; Geology; Seismology; Volcano; Seismometer; Mount; Geothermal gradient; Volcanology; Seismic noise; Geophysics; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.02115783574065141,"gpt":0.2738891551421014,"spread":0.25273131940145,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001053005,0.0001022329,0.0004587593,0.0001048835,0.0002492055,0.0005803,0.0002318593,0.00008195172,0.001783457],"category_scores_gemma":[0.0007470218,0.0001216293,0.0002229062,0.0008379713,0.0002148624,0.000272814,0.0000488472,0.0009019669,0.0001185212],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003818519,"about_ca_system_score_gemma":0.0003344474,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.03484105,"about_ca_topic_score_gemma":0.06825476,"domain_scores_codex":[0.9966949,0.0004629401,0.0005195198,0.0002692792,0.001375196,0.0006781626],"domain_scores_gemma":[0.9986113,0.0004834527,0.0001428867,0.0001811481,0.0002091176,0.0003721408],"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":[0.0006250321,0.001879747,0.3899891,0.0002024402,0.001027157,0.04664238,0.0007178109,0.07409217,0.03562789,0.00002926623,0.02263818,0.4265288],"study_design_scores_gemma":[0.0007121908,0.0002893134,0.9464428,0.000140814,0.00003466879,0.0001894135,0.0005515809,0.0399143,0.0001787296,0.001776727,0.009586413,0.0001830522],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9983104,0.0003096582,0.0003782371,0.0003067728,0.0001605992,0.00006178678,0.0001379091,0.00000377314,0.0003308243],"genre_scores_gemma":[0.9972174,0.0005127874,0.0002503186,0.0001127797,0.0006081957,1.157117e-7,0.00007283483,0.000005777859,0.001219849],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5564536,"threshold_uncertainty_score":0.9991291,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2149104678","doi":"10.1190/1.1993267","title":"Underwater MASW to evaluate stiffness of water-bottom sediments","year":2005,"lang":"en","type":"article","venue":"The Leading Edge","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Nova Scotia Community College; Geological Survey of Canada","funders":"","keywords":"Underwater; Geology; Seismology; Oceanography; Geotechnical engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.02766920078167625,"gpt":0.2587951810634826,"spread":0.2311259802818063,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004021672,0.0000910133,0.0001464843,0.00006223308,0.0001023867,0.00003306167,0.0002608317,0.00002706186,0.001685429],"category_scores_gemma":[0.000006813607,0.00004567286,0.00005903337,0.0001296918,0.00004029468,0.00008017738,0.0000180049,0.00007642762,0.003073191],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005169445,"about_ca_system_score_gemma":0.000009240862,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000488987,"about_ca_topic_score_gemma":0.0001394389,"domain_scores_codex":[0.9991595,0.00005744988,0.0001624818,0.0001494206,0.0002082111,0.000263],"domain_scores_gemma":[0.9996239,0.0000513614,0.00003009798,0.0002023771,0.0000224016,0.0000698638],"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":[0.0002551526,0.0001319867,0.08595434,0.00009696389,0.0005995648,0.00001863059,0.01301904,0.2064255,0.04020219,0.0002241465,0.02856673,0.6245058],"study_design_scores_gemma":[0.001899742,0.0003363398,0.3526721,0.0001926752,0.000616058,0.00002876886,0.001601053,0.2321732,0.08303398,0.005714294,0.3204618,0.001269982],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.991158,0.00006500333,0.0001632241,0.003893712,0.000180259,0.00007752566,0.00001321102,0.00001881883,0.004430213],"genre_scores_gemma":[0.9913295,0.000007929742,0.0002535708,0.0009898687,0.0001688198,4.421777e-7,0.00002902679,0.000003413794,0.007217439],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6232358,"threshold_uncertainty_score":0.9992272,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2110793813","doi":"10.1139/t00-047","title":"Phase and amplitude responses associated with the measurement of shear-wave velocity in sand by bender elements","year":2000,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"Engineering and Physical Sciences Research Council","keywords":"Shear (geology); Attenuation; Dispersion (optics); Amplitude; Geotechnical engineering; Wave velocity; Geology; Phase velocity; Shear waves; Wave propagation; Shear velocity; Mechanics; Optics; Physics; Turbulence","retraction":null,"screen_n_in":null,"score":{"opus":0.02659811589332755,"gpt":0.2260446996224481,"spread":0.1994465837291206,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001080808,0.00009211408,0.0001659371,0.00009394159,0.0001813823,0.00005979806,0.0001269331,0.00006165566,0.001997569],"category_scores_gemma":[0.00007102318,0.00005763198,0.00003881919,0.0002397907,0.0001196336,0.00006545383,0.00000268424,0.000289908,0.000002519802],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003971754,"about_ca_system_score_gemma":0.0002571729,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.04515311,"about_ca_topic_score_gemma":0.08219191,"domain_scores_codex":[0.9988394,0.0001187627,0.0002450722,0.0001316128,0.0003525978,0.0003125555],"domain_scores_gemma":[0.999377,0.00007376011,0.00007504202,0.00009413265,0.00004806666,0.0003320124],"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":[0.00165597,0.0005116126,0.1484384,0.00002072213,0.001200295,0.0009084608,0.0008916373,0.01824447,0.0005432162,0.00002669025,0.04375918,0.7837993],"study_design_scores_gemma":[0.00405844,0.0009993787,0.9066643,0.0001658089,0.0001900831,0.0001547741,0.0004874897,0.03541113,0.00008194733,0.0008095764,0.05053247,0.0004445672],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9964022,0.0006559452,0.00005184344,0.002234177,0.00001190066,0.00007945781,0.0002275617,0.000003562939,0.0003333649],"genre_scores_gemma":[0.9989866,0.0001414694,0.00004683126,0.0007062135,0.0000182367,3.332423e-7,0.00001929521,0.000002395798,0.00007860598],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7833548,"threshold_uncertainty_score":0.9989147,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2109827084","doi":"10.1016/j.epsl.2011.06.026","title":"Investigation of Cascadia segmentation with ambient noise tomography","year":2011,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Transport Canada","keywords":"Geology; Subduction; Seismology; Terrane; Crust; Slab; Episodic tremor and slip; Shear zone; Lithosphere; Mantle (geology); Seismic tomography; Geophysics; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.01373538187236467,"gpt":0.1649915292919954,"spread":0.1512561474196308,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002478843,0.0001019665,0.0001150975,0.0002468227,0.0001516178,0.00003449607,0.000136732,0.00001929635,0.0003763091],"category_scores_gemma":[0.000003913496,0.00007333038,0.00002052934,0.0006005103,0.0006189042,0.0004461312,0.000004615,0.00006362677,0.0000171039],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":8.271489e-7,"about_ca_system_score_gemma":0.00002734956,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006417474,"about_ca_topic_score_gemma":0.0007477074,"domain_scores_codex":[0.9990227,0.00002925759,0.0001482735,0.0002556147,0.000312025,0.0002321618],"domain_scores_gemma":[0.9995632,0.00002883141,0.00008973333,0.0001230225,0.00001809323,0.0001771128],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002637557,0.000001921573,0.9899902,0.000008664427,0.00001169203,0.00001100893,0.0006058541,0.0004931967,0.005919498,0.000007271378,0.00004915941,0.002875208],"study_design_scores_gemma":[0.000131761,0.000174694,0.9922892,0.00001292562,0.00002344193,0.00001844935,0.0001992056,0.002887257,0.004035703,0.00004449987,0.0000679323,0.0001149043],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9986591,0.0001120912,0.00009885748,0.000216349,0.00007330782,0.00008892411,0.00005160306,0.00001314359,0.0006865766],"genre_scores_gemma":[0.9940248,0.00003097628,0.004331225,0.00145077,0.00002260818,2.517627e-7,0.0001263256,0.000001269919,0.00001179111],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.005669767,"threshold_uncertainty_score":0.9701344,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2794101160","doi":"10.1016/j.jvolgeores.2018.03.003","title":"A generic model for the shallow velocity structure of volcanoes","year":2018,"lang":"en","type":"article","venue":"Journal of Volcanology and Geothermal Research","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Université de Strasbourg; Agence Nationale de la Recherche","keywords":"Volcano; Geology; Seismology; Geophysics; Borehole; Basalt; Scaling; Volcanology; Petrology; Geotechnical engineering; Geometry","retraction":null,"screen_n_in":null,"score":{"opus":0.06631889696757155,"gpt":0.3226831176021877,"spread":0.2563642206346161,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008795509,0.0000680663,0.0001935543,0.0001492202,0.0002581948,0.00002063891,0.0003186642,0.00008812949,0.0006517461],"category_scores_gemma":[0.0001749086,0.00003645218,0.00008073964,0.0002240488,0.0007028104,0.00007858054,0.00001908456,0.0002580792,0.000002443844],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003363085,"about_ca_system_score_gemma":0.000158406,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005578321,"about_ca_topic_score_gemma":0.001943873,"domain_scores_codex":[0.9990104,0.0001041427,0.0002348028,0.0001047761,0.0002719341,0.0002739068],"domain_scores_gemma":[0.9988348,0.0004560832,0.0001373525,0.0001149803,0.000383307,0.00007348741],"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":[0.002926053,0.00009920706,0.3389184,0.0001448311,0.00138221,0.00002457079,0.003389572,0.04712892,0.01757717,0.001685172,0.007049419,0.5796744],"study_design_scores_gemma":[0.0004511739,0.0008519771,0.237252,0.00001541556,0.00005339019,0.00007007439,0.0004969662,0.7456735,0.0004379133,0.01081899,0.003801357,0.00007726956],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9943376,0.002231466,0.001649002,0.001387793,0.00009632984,0.00007007231,0.00006783869,0.000001430464,0.0001584585],"genre_scores_gemma":[0.9978028,0.0005020629,0.0007949726,0.0001911745,0.0003246997,1.788956e-7,0.000001573739,0.000002532185,0.0003800345],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6985446,"threshold_uncertainty_score":0.7136162,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2474675250","doi":"10.1016/j.jcp.2016.08.012","title":"A fast marching algorithm for the factored eikonal equation","year":2016,"lang":"en","type":"article","venue":"Journal of Computational Physics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Seventh Framework Programme; European Commission","keywords":"Eikonal equation; Fast marching method; Eikonal approximation; Mathematics; Algorithm; Applied mathematics; Mathematical analysis","retraction":null,"screen_n_in":null,"score":{"opus":0.02683986764294976,"gpt":0.2416663771045522,"spread":0.2148265094616024,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002450359,0.00005804719,0.0001012781,0.00003167017,0.0001207779,0.00004236148,0.0001297667,0.00001332266,0.00008297536],"category_scores_gemma":[0.0000224528,0.00002767704,0.0001494387,0.00008520272,0.00003561034,0.0002137454,0.000003687398,0.00005284238,0.00001099476],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005653966,"about_ca_system_score_gemma":0.00007139361,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00002162547,"about_ca_topic_score_gemma":0.000002476896,"domain_scores_codex":[0.9992802,0.00002812467,0.000213874,0.00005774334,0.0003213754,0.00009869142],"domain_scores_gemma":[0.9983325,0.001179711,0.0002384872,0.00003627861,0.0001708609,0.00004217042],"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":[0.00001266702,0.000008026158,0.001117436,0.00000132897,0.00007110298,7.001482e-7,0.00003912366,0.212219,0.00001070823,0.0003942848,0.0002564012,0.7858692],"study_design_scores_gemma":[0.0003728438,0.00007442393,0.06157171,0.00001727139,0.00003820144,0.00001640023,0.0000560833,0.7766558,0.00001300486,0.1604244,0.0007042681,0.00005553546],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"methods","genre_gemma":"empirical","genre_scores_codex":[0.03380266,0.00007210048,0.9644033,0.001325345,0.0001943939,0.00004181069,0.0001092189,0.000002748587,0.00004843846],"genre_scores_gemma":[0.9701339,0.00001339189,0.02858576,0.0002027709,0.0009750041,1.790735e-7,0.00002831445,0.000002293486,0.00005837764],"genre_candidate":"empirical","genre_consensus":null,"teacher_disagreement_score":0.9363313,"threshold_uncertainty_score":0.1128637,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2104740196","doi":"10.1029/2009jb006307","title":"Composition and variation of noise recorded at the Yellowknife Seismic Array, 1991–2007","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Seismology; Microseism; Seismogram; Seismic noise; Seismometer; Rayleigh wave; Noise (video); Seismic array; Ambient noise level; Surface wave; Seismic wave; Geophysics; Oceanography","retraction":null,"screen_n_in":null,"score":{"opus":0.02088276562735475,"gpt":0.2791448895651213,"spread":0.2582621239377666,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009911398,0.00009156913,0.0002470878,0.00002631146,0.0002256311,0.00006352045,0.0002280944,0.00004768423,0.0006350038],"category_scores_gemma":[0.0001358479,0.00005419048,0.0001371913,0.0003711614,0.0001970035,0.0002024835,0.00001394958,0.0003449856,0.00004692198],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001451199,"about_ca_system_score_gemma":0.00005597486,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003214064,"about_ca_topic_score_gemma":0.0001232242,"domain_scores_codex":[0.9981683,0.0002950779,0.0003524384,0.0001326171,0.0007872654,0.0002642759],"domain_scores_gemma":[0.9985164,0.0006867481,0.0002276969,0.0001456895,0.00026179,0.0001616138],"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":[0.005682833,0.001305351,0.08192392,0.0001682501,0.001016668,0.0002582198,0.002616551,0.04068371,0.1558035,0.001006697,0.04702031,0.662514],"study_design_scores_gemma":[0.0005089078,0.001259338,0.9544684,0.00007123339,0.00005788294,0.00003069498,0.0003423882,0.02518988,0.0006386049,0.01286006,0.004460124,0.0001125423],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9946129,0.0006630811,0.0002554964,0.002721419,0.00007501898,0.00007827509,0.00001419519,0.000003152506,0.001576408],"genre_scores_gemma":[0.9977392,0.0004699917,0.0006431888,0.0002028132,0.0003673124,1.147563e-7,0.00001071869,0.000002309843,0.0005643368],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8725444,"threshold_uncertainty_score":0.6952846,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3000496716","doi":"10.1029/2019jb018582","title":"Shear Velocity Model of Alaska Via Joint Inversion of Rayleigh Wave Ellipticity, Phase Velocities, and Receiver Functions Across the Alaska Transportable Array","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Terrane; Seismology; Asthenosphere; Crust; Volcano; North American Plate; Basin and range topography; Mantle (geology); Geophysics; Geomorphology; Tectonics; Lithosphere; Plate tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.07711832854481288,"gpt":0.3001547491015689,"spread":0.223036420556756,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001083599,0.0001479488,0.000555481,0.00009924737,0.0003071142,0.00005048387,0.0002616902,0.00007775096,0.000315664],"category_scores_gemma":[0.0001678386,0.00009534075,0.0002670909,0.0006600268,0.0006498928,0.0003307035,0.00003197923,0.0007606786,0.00001607542],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007015181,"about_ca_system_score_gemma":0.0002313052,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008552526,"about_ca_topic_score_gemma":0.00007194586,"domain_scores_codex":[0.9973462,0.0002176485,0.0005962008,0.0002147874,0.001172049,0.0004531094],"domain_scores_gemma":[0.9983289,0.0003554788,0.0002829859,0.0001745932,0.000454937,0.0004030547],"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":[0.01056087,0.003041855,0.04855234,0.001698865,0.003390138,0.00030385,0.04535159,0.518876,0.2347685,0.0003168725,0.01416227,0.1189769],"study_design_scores_gemma":[0.002145906,0.002846572,0.06550212,0.000136051,0.0001692668,0.00001367639,0.003937261,0.9024495,0.01841457,0.003022854,0.001103748,0.0002584354],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9945754,0.0001720241,0.002841374,0.0017107,0.0000498658,0.0001169087,0.0002974104,0.000004116786,0.0002321325],"genre_scores_gemma":[0.9983401,0.0005535567,0.0004789292,0.0001487055,0.0002240355,2.867441e-7,0.00002330433,0.000005685344,0.0002254464],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3835735,"threshold_uncertainty_score":0.3887883,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2769998628","doi":"10.1190/tle36120981.1","title":"Validation of DAS data integrity against standard geophones — DAS field test at Aquistore site","year":2017,"lang":"en","type":"article","venue":"The Leading Edge","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Petroleum Technology Research Centre","keywords":"Geophone; Vertical seismic profile; Borehole; Accelerometer; Noise (video); Computer science; Geology; Data acquisition; Repeatability; Acoustics; Seismology; Remote sensing; Geotechnical engineering; Artificial intelligence","retraction":null,"screen_n_in":null,"score":{"opus":0.0532676495405943,"gpt":0.308093005341183,"spread":0.2548253558005887,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005608451,0.00009243347,0.0001787346,0.00003216528,0.0005322062,0.0001069403,0.0008949963,0.0000509799,0.0004674521],"category_scores_gemma":[0.0005603434,0.00005929349,0.00005089553,0.0000620365,0.0001219281,0.0002447627,0.0001167623,0.0001517183,0.000280016],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006812787,"about_ca_system_score_gemma":0.00002600191,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003257137,"about_ca_topic_score_gemma":0.002092889,"domain_scores_codex":[0.9992365,0.00003974925,0.0001636017,0.000211257,0.0001886872,0.0001601882],"domain_scores_gemma":[0.9982787,0.0003621212,0.0001915788,0.001087884,0.00003401689,0.00004571867],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005921478,0.00001489228,0.9159572,0.00003844256,0.00005839415,0.000009568079,0.0007384692,0.000269865,0.001368996,0.00002722665,0.04542745,0.03603027],"study_design_scores_gemma":[0.0008769197,0.0003722001,0.683267,0.0003066548,0.0003552352,0.0000161117,0.0006982344,0.05775711,0.0206563,0.001964068,0.2329555,0.0007746976],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9852304,0.0002185508,0.00009726132,0.001812263,0.0003995969,0.00006028745,0.000740898,0.00001772835,0.01142303],"genre_scores_gemma":[0.9961895,0.0001231558,0.0001270101,0.0002501249,0.0002454003,1.46353e-7,0.0005860711,0.000002795422,0.002475808],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2326902,"threshold_uncertainty_score":0.5118273,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1973966093","doi":"10.1785/0120010152","title":"Global Comparisons of Earthquake Source Spectra","year":2002,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magnitude (astronomy); Seismology; Geology; Moment magnitude scale; Spectral line; Richter magnitude scale; Source model; Seismic moment; Tectonics; Scale (ratio); Geodesy; Physics; Fault (geology); Geometry; Computational physics; Astrophysics; Scaling; Mathematics","retraction":null,"screen_n_in":null,"score":{"opus":0.01730638664358775,"gpt":0.2034456377515046,"spread":0.1861392511079169,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001384723,0.0001192221,0.0004117439,0.000007593427,0.00008781147,0.000005737161,0.0004421722,0.00008017682,0.01068571],"category_scores_gemma":[0.00004564999,0.00007239287,0.0006513808,0.000334294,0.0008685234,0.00000787797,0.00004480005,0.0001124155,0.00005518384],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003243365,"about_ca_system_score_gemma":0.000007682661,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01450346,"about_ca_topic_score_gemma":0.000002435347,"domain_scores_codex":[0.998819,0.0001048426,0.0003509448,0.0001846557,0.0003154763,0.0002250727],"domain_scores_gemma":[0.9991308,0.0001747655,0.0003448568,0.0002478737,0.00003765541,0.00006404474],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0000412371,0.0003393201,0.2565452,0.00005859888,0.0003223619,0.000001380315,0.0002985789,0.03824502,0.00002566942,0.0000846855,0.6431895,0.06084839],"study_design_scores_gemma":[0.0001857118,0.0002314545,0.3177376,0.00001675026,0.00006003292,0.000005431765,0.0007023329,0.01701803,0.00004583996,0.0002774757,0.6636063,0.0001129716],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.879608,0.002768669,0.007736882,0.08135518,0.0001925935,0.0002860572,0.0004376086,0.0000564248,0.02755859],"genre_scores_gemma":[0.9830112,0.0002635332,0.01038107,0.005231357,0.00003454884,1.791826e-7,0.000007008772,0.000001778314,0.001069288],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1034032,"threshold_uncertainty_score":0.9920591,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1988719636","doi":"10.1016/s0267-7261(02)00117-3","title":"Surface and downhole shear wave seismic methods for thick soil site investigations","year":2002,"lang":"en","type":"article","venue":"Soil Dynamics and Earthquake Engineering","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Bedrock; Geology; Overburden; Geophone; Borehole; Penetrometer; Shear (geology); Seismology; Surface wave; Shear wave splitting; Seismic refraction; Seismic wave; Passive seismic; Geotechnical engineering; Geomorphology; Soil science; Soil water; Petrology; Optics","retraction":null,"screen_n_in":null,"score":{"opus":0.01709427103247902,"gpt":0.2198443499452987,"spread":0.2027500789128197,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003116189,0.0001764417,0.0002222326,0.00008312755,0.0002170388,0.0001255679,0.00005748547,0.00009087184,0.0001126768],"category_scores_gemma":[0.00007192942,0.0001652908,0.00006031127,0.000200438,0.00005876597,0.0001563228,0.00001501695,0.0001574427,0.00001347919],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004395424,"about_ca_system_score_gemma":0.00001040328,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001048228,"about_ca_topic_score_gemma":0.0005719748,"domain_scores_codex":[0.9990836,0.0000282344,0.0001982293,0.0002850495,0.00008900154,0.0003158939],"domain_scores_gemma":[0.9993218,0.0002297782,0.00004180963,0.000143886,0.00002664497,0.0002361332],"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":[0.000002520502,0.000005497431,0.007933018,0.0000664678,0.00005219433,0.000002727344,0.0002940253,0.9063091,0.00009065191,0.0004704364,0.00007759971,0.08469573],"study_design_scores_gemma":[0.0001816592,0.00004395252,0.03166622,0.00002014244,0.0000404443,0.00001456644,0.0000811629,0.9650618,0.00001448039,0.000552549,0.002107765,0.0002152155],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9372241,0.001548171,0.05958909,0.0008475016,0.0001436498,0.0001046176,0.0001762079,0.00005842005,0.0003082003],"genre_scores_gemma":[0.9552001,0.000652597,0.04303178,0.0002327694,0.0000697117,0.000001209448,0.0001440303,0.0000108659,0.0006569425],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08448052,"threshold_uncertainty_score":0.6740363,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2980825071","doi":"10.1016/j.jappgeo.2019.103866","title":"Bedrock depth evaluation using microtremor measurement: empirical guidelines at weathered granite formation in Singapore","year":2019,"lang":"en","type":"article","venue":"Journal of Applied Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":73,"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":"Nazarbayev University; Land Transport Authority - Singapore","keywords":"Microtremor; Bedrock; Borehole; Geology; Seismology; Surface wave; Overburden; Geomorphology; Geotechnical engineering; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.1088548652286063,"gpt":0.2999019508160151,"spread":0.1910470855874088,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008912609,0.0001211718,0.0002622594,0.0001399634,0.00007061545,0.00004207962,0.0001299487,0.00005826963,0.0001714198],"category_scores_gemma":[0.00002111076,0.00009466226,0.0001243261,0.000324884,0.00001354162,0.000253363,0.000009169277,0.0001442174,0.00007573743],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00006541401,"about_ca_system_score_gemma":0.00007915904,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001880568,"about_ca_topic_score_gemma":0.0003166976,"domain_scores_codex":[0.9982655,0.00004699333,0.0005727986,0.0001222917,0.0008142678,0.0001781573],"domain_scores_gemma":[0.998957,0.00003105419,0.0004860429,0.0001124145,0.000353034,0.00006045548],"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":[0.0006781854,0.0001376199,0.08798973,0.0001009772,0.0002120011,0.00001922581,0.00181184,0.5982225,0.06950436,0.00001973131,0.0009602954,0.2403435],"study_design_scores_gemma":[0.002597841,0.0001738701,0.1722823,0.0002121791,0.0003373509,0.00006771899,0.001424928,0.8100261,0.002917968,0.007414838,0.002146082,0.0003988042],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9976576,0.0002949325,0.0003259521,0.0001155036,0.0001360927,0.0001577205,0.000006720479,0.000003711845,0.001301746],"genre_scores_gemma":[0.9978901,0.00003668269,0.00152646,0.0002711353,0.0002299107,1.793708e-7,0.00002704525,0.000004390208,0.00001415168],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2399447,"threshold_uncertainty_score":0.3860215,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2069575561","doi":"10.1016/j.biocon.2012.08.005","title":"Narwhals and seismic exploration: Is seismic noise increasing the risk of ice entrapments?","year":2012,"lang":"en","type":"article","venue":"Biological Conservation","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Pinngortitaleriffik","keywords":"Geology; Seismology","retraction":null,"screen_n_in":null,"score":{"opus":0.04996707287603953,"gpt":0.2354143609740085,"spread":0.185447288097969,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000719376,0.00008770214,0.0001301106,0.00002846193,0.0001745861,0.00002848599,0.00008444306,0.00006691994,0.0004246529],"category_scores_gemma":[0.0001838664,0.00004829888,0.00004812725,0.0001749017,0.0001129194,0.0002660153,0.00001172836,0.000072886,0.00003014929],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002399992,"about_ca_system_score_gemma":0.00001092651,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003377558,"about_ca_topic_score_gemma":0.00002485161,"domain_scores_codex":[0.9991036,0.0002783719,0.0002136852,0.0001314233,0.0001097762,0.0001631124],"domain_scores_gemma":[0.9991204,0.0005144138,0.0001624979,0.000106392,0.00003548356,0.00006084215],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000287523,0.0000114101,0.9923406,0.000003809661,0.00002747049,1.90966e-7,0.0002150333,0.0002491086,0.0002178367,0.00005248856,0.0002464702,0.006606792],"study_design_scores_gemma":[0.0001150164,0.00005155566,0.9384719,0.00000791658,0.00004350408,0.000003419498,0.0005574045,0.05170656,0.0001887686,0.001279405,0.007491557,0.00008301994],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9950266,0.001039163,0.001006232,0.002398001,0.00007299793,0.0001028343,0.00006854011,0.00001435555,0.0002712248],"genre_scores_gemma":[0.9951615,0.001022398,0.0003025474,0.003277792,0.00009328946,0.00000111006,0.0001022526,0.000001157008,0.0000379273],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05386876,"threshold_uncertainty_score":0.5105879,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1969375253","doi":"10.1139/t07-013","title":"In situ shear wave velocity from multichannel analysis of surface waves (MASW) tests at eight Norwegian research sites","year":2007,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":true,"about_ca":false},"ca_institutions":"","funders":"","keywords":"Geology; Silt; Geotechnical engineering; Shear modulus; Shear (geology); Stiffness; Surface wave; Mineralogy; Geomorphology; Materials science; Optics; Composite material","retraction":null,"screen_n_in":null,"score":{"opus":0.04094490118772477,"gpt":0.2773497597630497,"spread":0.2364048585753249,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002742661,0.0001941122,0.0005533125,0.001499325,0.0003894595,0.00008626121,0.0004885034,0.0002847814,0.004497206],"category_scores_gemma":[0.0004153962,0.0001671461,0.0003076998,0.002991256,0.0002983749,0.0001942873,0.00003653137,0.0009654477,0.000096253],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001751533,"about_ca_system_score_gemma":0.0003289296,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.3902881,"about_ca_topic_score_gemma":0.7863258,"domain_scores_codex":[0.9968932,0.0002298821,0.0006908263,0.0004075383,0.0007229109,0.00105567],"domain_scores_gemma":[0.9970366,0.0009302,0.0001513472,0.0003568555,0.0002112784,0.001313729],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002389543,0.0001322526,0.7385638,0.000020382,0.001767923,0.004476401,0.001210985,0.223522,0.006853644,0.00005148162,0.005797385,0.01736484],"study_design_scores_gemma":[0.0002438568,0.00007023929,0.8799217,0.00002801952,0.0002069285,0.00002650061,0.0004257179,0.1151606,0.0003880032,0.0006315782,0.002671203,0.0002256721],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9961674,0.0007267427,0.000200594,0.001578939,0.0001004058,0.00009196913,0.000428243,0.000008140974,0.0006975442],"genre_scores_gemma":[0.9976338,0.0001734131,0.001163547,0.000397035,0.0001755667,1.22941e-7,0.0001873469,0.000006977901,0.0002622049],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3960378,"threshold_uncertainty_score":0.9964128,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1570817337","doi":"10.1109/pes.2004.1373161","title":"Performance of \"WAMS East\" in providing dynamic information for the North East blackout of August 14, 2003","year":2004,"lang":"en","type":"article","venue":"IEEE Power Engineering Society General Meeting, 2004.","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"University of Alberta","keywords":"Blackout; Electric power system; Phasor; Task (project management); Interconnection; Computer science; Work (physics); Event (particle physics); Global Positioning System; Units of measurement; Engineering; Telecommunications; Systems engineering; Power (physics)","retraction":null,"screen_n_in":null,"score":{"opus":0.005638326056985844,"gpt":0.1809929765261192,"spread":0.1753546504691334,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003709179,0.000156721,0.0002148923,0.00006355766,0.00007298657,0.00002425595,0.0002121139,0.00006973835,0.0000263038],"category_scores_gemma":[0.00005149041,0.0001214238,0.0001618628,0.0005351295,0.00004688877,0.0002834785,0.000007777619,0.000130898,0.00000510845],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002444371,"about_ca_system_score_gemma":0.00007472682,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008039889,"about_ca_topic_score_gemma":0.0001973513,"domain_scores_codex":[0.9989056,0.000008975587,0.0004128093,0.0001326075,0.000231192,0.0003087965],"domain_scores_gemma":[0.9994676,0.00003460782,0.0001827634,0.000156964,0.0001094267,0.00004871313],"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":[0.000009734797,0.000008991799,0.02421441,0.0001096725,0.00004443101,1.344637e-7,0.001110371,0.9731865,0.000341797,0.000007120667,0.0002132746,0.0007535909],"study_design_scores_gemma":[0.0004627893,0.00008484236,0.0418193,0.0001010878,0.0000309791,0.000001868085,0.0003877262,0.9555004,0.0005747634,0.000004308312,0.0008554487,0.0001765384],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9923401,0.0004012285,0.006332121,0.00007561901,0.0003799059,0.0002348244,0.00008894738,0.00002378722,0.0001234823],"genre_scores_gemma":[0.993882,0.0001031126,0.005722834,0.00007272782,0.00005722021,0.00000415911,0.0000617406,0.000006787776,0.00008944283],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01768612,"threshold_uncertainty_score":0.4951518,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1525966310","doi":"10.1029/2012jb009651","title":"Tidal calibration of plate boundary observatory borehole strainmeters","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Borehole; Coupling (piping); Geology; Geodesy; Observatory; Boundary (topology); GNSS applications; Geodetic datum; Seismology; Geophysics; Physics; Geotechnical engineering; Mathematics; Mathematical analysis; Satellite; Astrophysics; Materials science","retraction":null,"screen_n_in":null,"score":{"opus":0.06010335255071511,"gpt":0.3177843045791912,"spread":0.2576809520284761,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001600319,0.0001028768,0.000331784,0.0002039859,0.0001477682,0.00007034227,0.0002737438,0.00006127393,0.0006387767],"category_scores_gemma":[0.0001982629,0.00007491389,0.0002293438,0.000463878,0.0002737222,0.0007962247,0.00002205854,0.0005341316,0.00005179641],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006389538,"about_ca_system_score_gemma":0.0002158854,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007241073,"about_ca_topic_score_gemma":0.00003879104,"domain_scores_codex":[0.9974456,0.0002902267,0.0004366227,0.0001080398,0.001190443,0.0005290717],"domain_scores_gemma":[0.9985887,0.0003958971,0.0002171843,0.0001566834,0.0002257605,0.000415812],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001612114,0.00136478,0.767,0.0003376462,0.001327038,0.0002728074,0.003577235,0.01275555,0.03560102,0.001869796,0.01574824,0.1585338],"study_design_scores_gemma":[0.000435976,0.000889525,0.9612495,0.00006149844,0.00003877587,0.00001923804,0.0006978739,0.02474618,0.002557899,0.002622582,0.006524879,0.0001560485],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9979737,0.00043482,0.0001481424,0.000303681,0.0001769093,0.00005338858,0.00005263455,0.000004012107,0.0008526481],"genre_scores_gemma":[0.9981206,0.0001161283,0.0006374417,0.00009094824,0.0007112779,1.29161e-7,0.00001913444,0.000004363593,0.0002999794],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1942495,"threshold_uncertainty_score":0.6994157,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2035627120","doi":"10.1144/sp307.4","title":"The feasibility of generating low-frequency volcano seismicity by flow through a deformable channel","year":2008,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":68,"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":"Induced seismicity; Geology; Volcano; Seismology; Low frequency; Channel (broadcasting); Flow (mathematics); Mechanics; Physics; Computer science; Telecommunications","retraction":null,"screen_n_in":null,"score":{"opus":0.03492329687670907,"gpt":0.2364391690937303,"spread":0.2015158722170212,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004608209,0.0001677948,0.0002683011,0.00001384277,0.001620653,0.00007422607,0.0005093414,0.000154264,0.001879889],"category_scores_gemma":[0.0002247319,0.0001052571,0.0003753786,0.0007388834,0.0006796852,0.0003653103,0.00004585231,0.0002585598,0.00006400857],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002247319,"about_ca_system_score_gemma":0.0001178856,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004162467,"about_ca_topic_score_gemma":0.0004896024,"domain_scores_codex":[0.9981862,0.000104714,0.0004840403,0.000374229,0.0003702934,0.0004805468],"domain_scores_gemma":[0.9988077,0.0002397449,0.0002180159,0.0003893035,0.0002130371,0.000132221],"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":[0.00004098388,0.0004511848,0.5589422,0.00002926887,0.0002648535,0.000002471038,0.001677498,0.03564541,0.0002907937,0.004125082,0.3909842,0.007546016],"study_design_scores_gemma":[0.0009694068,0.0002849544,0.4132072,0.000009919174,0.00008216655,0.00003222309,0.001368149,0.4384747,0.0001928667,0.03255725,0.1121028,0.0007183889],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9601045,0.001123792,0.009714935,0.01094048,0.0002645995,0.0004009584,0.0006132245,0.0001025846,0.01673495],"genre_scores_gemma":[0.9851583,0.001831931,0.006546205,0.002502135,0.001115206,0.0000103933,0.0007724179,0.000004696516,0.00205872],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4028293,"threshold_uncertainty_score":0.9996791,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2334442844","doi":"10.1093/gji/ggw085","title":"Evaluation of the southern California seismic velocity models through simulation of recorded events","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Faculty of Veterinary Medicine, University of Calgary; Southern California Earthquake Center; U.S. Geological Survey; University of Southern California","keywords":"Geology; Seismology; Magnitude (astronomy); Strong ground motion; Seismic wave; Geodesy; Ground motion; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.04130771518530076,"gpt":0.2714446192405749,"spread":0.2301369040552741,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005677908,0.00007049766,0.000120928,0.00003621693,0.0000642319,0.00001048248,0.0002664104,0.0000329043,0.001250313],"category_scores_gemma":[0.0001254255,0.00003574752,0.0001801534,0.0001088513,0.00005317156,0.0002119015,0.00001532553,0.00008029147,0.0000618943],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000201117,"about_ca_system_score_gemma":0.000084295,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005869597,"about_ca_topic_score_gemma":0.00004321688,"domain_scores_codex":[0.9982373,0.0001709794,0.0003152422,0.0001013419,0.00107693,0.00009826739],"domain_scores_gemma":[0.9988684,0.0001320722,0.0003448166,0.00009787336,0.0005241297,0.00003272196],"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":[0.00004863648,0.00005067867,0.01668295,0.000002226374,0.0001827737,2.956007e-7,0.0001544254,0.8832551,0.0003522652,0.00006437805,0.00006907347,0.09913722],"study_design_scores_gemma":[0.0003718703,0.00002000514,0.04414086,0.00004296018,0.00007720904,0.000002571659,0.00005718445,0.8192035,0.000147169,0.1357297,0.0001590467,0.00004786638],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9800318,0.00002382312,0.01754551,0.0008625177,0.0003397314,0.00005519585,0.0004127316,0.000002964501,0.000725686],"genre_scores_gemma":[0.9993848,0.00001732237,0.0001448217,0.0000805226,0.0002269258,2.321807e-7,0.00001365618,0.000002125416,0.0001296578],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1356654,"threshold_uncertainty_score":0.9996627,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1907149755","doi":"10.1139/t10-081","title":"Development of a Vs<sub>30</sub>(NEHRP) map for the city of Ottawa, Ontario, Canada","year":2011,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":true,"about_ca":true},"ca_institutions":"Carleton University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bedrock; Geology; Borehole; Seismology; Shear (geology); Ambient noise level; Soil water; Seismic refraction; Wave velocity; Geophone; Geotechnical engineering; Seismic wave; Geomorphology; Soil science; Petrology","retraction":null,"screen_n_in":null,"score":{"opus":0.02150194379087255,"gpt":0.1804893731086683,"spread":0.1589874293177957,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005245186,0.0001143818,0.0002390584,0.00009999498,0.0002781055,0.00001694648,0.0004549938,0.00007995662,0.003154971],"category_scores_gemma":[0.00004943235,0.00007844575,0.0001294136,0.0001422119,0.00009294815,0.00004860221,0.000008569409,0.0002775045,0.000004755214],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00009233886,"about_ca_system_score_gemma":0.005348283,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9950247,"about_ca_topic_score_gemma":0.9997695,"domain_scores_codex":[0.998705,0.00002338547,0.0004840315,0.0001332444,0.0002643728,0.0003899201],"domain_scores_gemma":[0.9989123,0.00009776047,0.0002068102,0.0001739693,0.0001070575,0.0005021086],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003535528,0.0001393748,0.4750423,0.0001774597,0.002397697,0.0004638557,0.003664299,0.01291982,0.0006010138,0.001226419,0.1205036,0.3825107],"study_design_scores_gemma":[0.0003394498,0.0001212399,0.7476135,0.0000554893,0.0001490881,0.00006998338,0.0003986265,0.003280348,0.00187045,0.0008606415,0.244967,0.000274203],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9933116,0.0005474744,0.002764304,0.00128298,0.0004718877,0.0002437415,0.0002815019,0.000006322544,0.001090188],"genre_scores_gemma":[0.997533,0.00001298291,0.001739633,0.0005492396,0.00006022323,8.489098e-7,0.00001516795,0.000003283299,0.00008557575],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3822365,"threshold_uncertainty_score":0.9977563,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2326258331","doi":"10.1061/41095(365)130","title":"Optimum MASW Survey—Revisit after a Decade of Use","year":2010,"lang":"en","type":"article","venue":"GeoFlorida 2010","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geoscience BC","funders":"","keywords":"Offset (computer science); Wavelength; Geology; Physics; Optics; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.01598797208431409,"gpt":0.2106079968261397,"spread":0.1946200247418257,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046685,0.0001384984,0.00023504,0.0001064639,0.00005951412,0.00007086968,0.0002497656,0.0001137588,0.009424117],"category_scores_gemma":[0.0001179232,0.0001079754,0.0001236441,0.0002897553,0.00009085677,0.000250088,0.00002055302,0.0002628331,0.0005460035],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":8.995995e-7,"about_ca_system_score_gemma":0.00003227995,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01264599,"about_ca_topic_score_gemma":0.00655817,"domain_scores_codex":[0.9988936,0.00004951056,0.0002505821,0.0002543323,0.0002322411,0.0003197398],"domain_scores_gemma":[0.9990876,0.0001973798,0.00009111836,0.0003932026,0.00007664932,0.0001540006],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004198619,0.00001024093,0.9928902,0.000007613512,0.00003034158,0.00001101904,0.00003081774,0.0001555955,0.0001798258,0.00001348192,0.001643764,0.004985054],"study_design_scores_gemma":[0.0001207336,0.00002857687,0.9774606,0.000005685634,0.00002837808,0.000004853898,0.00001351952,0.00305679,0.0001237945,0.00009894382,0.01891132,0.0001467644],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9974925,0.0001437257,0.00009671105,0.0001506894,0.001044077,0.00006588271,0.0004382213,0.00001846492,0.0005497505],"genre_scores_gemma":[0.9959294,0.00006766531,0.001356904,0.0002282702,0.0002536354,6.700133e-7,0.0001835394,0.000004797974,0.001975177],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01726756,"threshold_uncertainty_score":0.9939289,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2602772114","doi":"10.1002/2016jb013356","title":"Automated detection and cataloging of global explosive volcanism using the International Monitoring System infrasound network","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Natural Resources Canada; National Science Foundation","keywords":"Infrasound; Explosive material; Explosive eruption; Warning system; SIGNAL (programming language); Computer science; Volcano; Hazard; Seismology; Geology; Volcanic hazards; Volcanism; Remote sensing; Real-time computing; Telecommunications; Magma; Acoustics; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.05486887721328785,"gpt":0.3466716415219118,"spread":0.2918027643086239,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001023808,0.00007869198,0.0002210016,0.00005154356,0.0006917378,0.0003334053,0.0004571212,0.00004030871,0.00001080985],"category_scores_gemma":[0.0003087923,0.00005020689,0.0000968347,0.0001591037,0.0002330916,0.0003923706,0.00007434417,0.0003082994,0.000005186203],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002346652,"about_ca_system_score_gemma":0.00009902061,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004020593,"about_ca_topic_score_gemma":0.0001836947,"domain_scores_codex":[0.9984173,0.0001349293,0.0002801816,0.0001132709,0.0007787795,0.000275582],"domain_scores_gemma":[0.998701,0.0002623095,0.000371669,0.0001794068,0.0003605111,0.0001250887],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004312657,0.00006762912,0.8607951,0.0001094886,0.0009206983,0.0002379411,0.0005261818,0.08483209,0.01020703,0.0004276392,0.0001786521,0.04126627],"study_design_scores_gemma":[0.0001710838,0.0001311073,0.629869,0.0001555924,0.00002740665,0.00005399924,0.000898832,0.3673696,0.0004709824,0.0007334474,0.00006838544,0.00005049119],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9985918,0.0001563426,0.0002702744,0.0001311653,0.0005310478,0.0000524095,0.00001459096,0.000007717728,0.0002446169],"genre_scores_gemma":[0.9983782,0.00008539835,0.0002895447,0.000006083869,0.001223471,1.538592e-7,0.000001216623,0.000002158471,0.00001381347],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2825375,"threshold_uncertainty_score":0.6077961,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1945607800","doi":"10.1002/2013jb010535","title":"Ambient seismic noise tomography of Canada and adjacent regions: Part I. Crustal structures","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Alberta; University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Royal Society Te Apārangi; Royal Society; Marsden Fund; National Science Foundation","keywords":"Geology; Crust; Mantle (geology); Seismology; Transition zone; Craton; Continental crust; Seismic tomography; Shield; Receiver function; Shear velocity; Velocity gradient; Seismometer; Geophysics; Petrology; Lithosphere; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.01958870606416186,"gpt":0.2573237911233822,"spread":0.2377350850592204,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004634102,0.0001281631,0.0003829419,0.0002345588,0.000172045,0.00008845938,0.0002665729,0.00004495259,0.0007276339],"category_scores_gemma":[0.0001778561,0.00008700769,0.000162832,0.0005102665,0.0002820349,0.0002401315,0.00003416099,0.0004878552,0.00001042552],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008188228,"about_ca_system_score_gemma":0.0004775672,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.4527464,"about_ca_topic_score_gemma":0.06159693,"domain_scores_codex":[0.9974059,0.0001988913,0.000438092,0.0001768245,0.001264691,0.0005155952],"domain_scores_gemma":[0.9982643,0.0003276458,0.0002102414,0.0001843449,0.000490842,0.0005226969],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001320195,0.0009104373,0.4873636,0.0007068858,0.002636748,0.001058619,0.002026476,0.04681681,0.007976951,0.002275338,0.250926,0.195982],"study_design_scores_gemma":[0.0003784176,0.0006589725,0.9613267,0.00008448914,0.00003052267,0.00003415879,0.0009244485,0.01815786,0.0006798919,0.009722074,0.007844906,0.0001576073],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9975444,0.0005558372,0.00001988963,0.001211136,0.0001237005,0.000110121,0.00004760131,0.000002505037,0.0003847734],"genre_scores_gemma":[0.998542,0.0004954077,0.000144359,0.0001782775,0.0002896299,3.103108e-7,0.000007109314,0.000003700046,0.00033917],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4739631,"threshold_uncertainty_score":0.9555265,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2164656247","doi":"10.1007/978-1-4020-9508-5_12","title":"Meteor Generated Infrasound: Theory and Observation","year":2009,"lang":"en","type":"book-chapter","venue":"","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"","keywords":"Meteoroid; Meteor (satellite); Infrasound; Atmosphere (unit); Thermosphere; Hypervelocity; Range (aeronautics); Geology; Atmospherics; Meteorology; Environmental science; Physics; Astronomy; Geophysics; Aerospace engineering; Acoustics; Engineering; Ionosphere","retraction":null,"screen_n_in":null,"score":{"opus":0.01860966892259705,"gpt":0.1955860032445477,"spread":0.1769763343219507,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002601451,0.0001824744,0.0002288577,0.00009579329,0.00008573498,0.00007993693,0.00008824759,0.0001672781,0.01423832],"category_scores_gemma":[0.00001501571,0.0001335627,0.00007320957,0.00003310736,0.00004683695,0.00009186338,0.000004903489,0.00012362,0.0002277321],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002177576,"about_ca_system_score_gemma":0.00002295766,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00036566,"about_ca_topic_score_gemma":0.0003587855,"domain_scores_codex":[0.9992559,0.00002464725,0.0001874175,0.0002527552,0.0001533801,0.0001258817],"domain_scores_gemma":[0.9995293,0.000123298,0.00008793928,0.0001476676,0.00003316116,0.0000786309],"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":[0.00005470887,0.000004840335,0.002950224,0.00002107716,0.0003441936,0.0000285358,0.00005402632,0.0006425946,0.00002183422,0.2823687,0.007921932,0.7055874],"study_design_scores_gemma":[0.0001450659,0.000104992,0.02109947,0.00002794462,0.0002319655,0.000008916066,0.00002803137,0.005419448,0.000007187693,0.4022998,0.5701477,0.0004795452],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"other","genre_gemma":"other","genre_scores_codex":[0.005309332,0.002542723,0.0002387716,0.0002082326,0.00009945458,0.00008954978,0.00009800273,0.00005330961,0.9913606],"genre_scores_gemma":[0.005958135,0.001475721,0.001072358,0.002810534,0.000208658,8.738341e-8,0.001078021,0.000005414404,0.9873911],"genre_candidate":"other","genre_consensus":"other","teacher_disagreement_score":0.7051078,"threshold_uncertainty_score":0.9866628,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1980416220","doi":"10.1016/j.jappgeo.2005.08.003","title":"Evaluation of MASW techniques to image steeply dipping cavities in laterally inhomogeneous terrain","year":2006,"lang":"en","type":"article","venue":"Journal of Applied Geophysics","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Geophone; Bedrock; Overburden; Seismology; Terrain; Borehole; Rayleigh wave; Geodesy; Surface wave; Geomorphology; Geotechnical engineering; Optics","retraction":null,"screen_n_in":null,"score":{"opus":0.009091279021833308,"gpt":0.2219943462820393,"spread":0.212903067260206,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009579608,0.00009842942,0.0002557129,0.0001969683,0.00003120206,0.00003626887,0.0001473983,0.0000395734,0.0001058918],"category_scores_gemma":[0.00001028678,0.00008102089,0.00008462701,0.0002846178,0.00002915354,0.0001263268,0.000009168809,0.0001168123,0.00001004951],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001704334,"about_ca_system_score_gemma":0.00007942183,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001435515,"about_ca_topic_score_gemma":0.0004675215,"domain_scores_codex":[0.9986495,0.00004703489,0.0004503609,0.0000991944,0.0006009293,0.0001529202],"domain_scores_gemma":[0.9993438,0.00004175713,0.0002933242,0.00009597445,0.0001847269,0.00004048837],"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":[0.0003353836,0.000250404,0.01678431,0.00009779801,0.0002203685,0.00008216404,0.002752135,0.2166151,0.1184419,0.0005989618,0.00102826,0.6427932],"study_design_scores_gemma":[0.002205186,0.001055157,0.6679662,0.0004049253,0.0008228438,0.00006181911,0.004254615,0.04588303,0.06121959,0.2117616,0.003280692,0.001084392],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9912339,0.00006687857,0.0002236377,0.0001188348,0.00004435409,0.0001159338,0.00002020882,0.00000464552,0.00817155],"genre_scores_gemma":[0.9959601,0.00001256982,0.003607131,0.0001481592,0.0002199401,6.709687e-7,0.00001321093,0.000003553701,0.0000346729],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6511819,"threshold_uncertainty_score":0.3303936,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}