{"meta":{"query_hash":"75b8bddccdc0","filters":{"topic":"High-pressure geophysics and materials"},"cohort_total":1445,"direct_labels_cover":0,"predictions_cover":1445,"exported":1445,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/75b8bddccdc0","api":"https://metacan.xera.ac/api/v1/cohort?topic=High-pressure+geophysics+and+materials"},"results":[{"id":"W1038392753","doi":"10.1007/978-3-642-34023-9_2","title":"Thermal Properties of Rocks and Density of Fluids","year":2014,"lang":"en","type":"book-chapter","venue":"Lecture notes in earth system sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":127,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"","keywords":"Geothermal gradient; Thermal conductivity; Thermal; Anisotropy; Earth (classical element); Geology; Mineralogy; Petrology; Geophysics; Petroleum engineering; Geochemistry; Materials science; Thermodynamics; Physics; Composite material; Optics","score_opus":0.014352318323304357,"score_gpt":0.18331644286574936,"score_spread":0.168964124542445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1038392753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9342879,0.004735105,0.0007323876,0.00004725698,0.00094256696,0.00051569985,0.00012088914,0.000033535678,0.058584653],"genre_scores_gemma":[0.9989535,0.00003683239,0.0002373341,0.000017805532,0.00014599308,5.277608e-7,0.0000061600335,0.0000047942685,0.0005970114],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99846184,0.00007567285,0.00044294732,0.00035841894,0.0004375834,0.00022353533],"domain_scores_gemma":[0.999193,0.00015089923,0.00032177466,0.00020924349,0.000071867194,0.000053183463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067658076,0.00023310365,0.00065355044,0.0001452908,0.0001012758,0.000046174217,0.0003026493,0.00020650284,0.00014551083],"category_scores_gemma":[0.000037123416,0.00015058565,0.000064592816,0.0000681364,0.0005616575,0.00007192086,0.000035226676,0.00011599934,0.000014452289],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000826759,0.00008025633,0.2623674,0.023104291,0.0006275587,0.0001048369,0.012632934,0.18230754,0.17802155,0.060607444,0.00007792758,0.2792415],"study_design_scores_gemma":[0.0037076436,0.0076330933,0.20134768,0.034029856,0.0010098942,0.000290383,0.00063258363,0.06168635,0.63484275,0.029880762,0.016983818,0.007955205],"about_ca_topic_score_codex":0.0021654237,"about_ca_topic_score_gemma":0.0018701857,"teacher_disagreement_score":0.45682117,"about_ca_system_score_codex":0.0000014836149,"about_ca_system_score_gemma":0.00008560609,"threshold_uncertainty_score":0.6140705},"labels":[],"label_agreement":null},{"id":"W1150645350","doi":"10.1038/srep13039","title":"Hydrogen segregation and its roles in structural stability and metallization: silane under pressure","year":2015,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); University of Saskatchewan","funders":"National Key Research and Development Program of China; RIKEN; Program for New Century Excellent Talents in University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Jilin University; Ministry of Education, Culture, Sports, Science and Technology; University of Saskatchewan","keywords":"Enthalpy; Delocalized electron; Disilane; Metastability; Silane; Crystallography; Hydrogen; Chemistry; Silicon; Atom (system on chip); Electronic structure; Decomposition; Crystal structure; Phase (matter); Materials science; Computational chemistry; Thermodynamics","score_opus":0.02090584701058758,"score_gpt":0.22216291300224428,"score_spread":0.2012570659916567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1150645350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966494,0.001533963,0.000004528454,0.000070529524,0.0010943086,0.00019716703,0.000021041198,0.000018450799,0.0004106146],"genre_scores_gemma":[0.9994416,0.000005326704,0.00006628953,0.000008896926,0.00003364065,0.0000010194203,0.00015098727,0.0000019281233,0.00029028967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99885154,0.00007368207,0.00023437593,0.00040469738,0.00028092504,0.00015479603],"domain_scores_gemma":[0.9994782,0.000019260668,0.000110270186,0.00018990258,0.00007770133,0.00012464111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009824755,0.00008941595,0.00014237457,0.0000499177,0.00011107787,0.00024634003,0.00004774716,0.000044394485,0.00025767757],"category_scores_gemma":[0.00005881029,0.000069406655,0.00001131545,0.00015617331,0.000093925104,0.00038152907,0.00002202026,0.00003623474,0.0000055247574],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008131721,0.000041711897,0.9205349,0.00024364785,0.000085701744,0.00020175286,0.0049726786,0.028836144,0.03730218,0.0017595368,0.00074946583,0.0051909285],"study_design_scores_gemma":[0.00068379444,0.00011211028,0.68346816,0.00004903993,0.00011926801,0.00028704034,0.00056782214,0.04246115,0.057773124,0.20025054,0.0135230385,0.0007049052],"about_ca_topic_score_codex":0.0003992808,"about_ca_topic_score_gemma":0.0014416092,"teacher_disagreement_score":0.23706676,"about_ca_system_score_codex":0.0000019397294,"about_ca_system_score_gemma":0.000057738212,"threshold_uncertainty_score":0.28303212},"labels":[],"label_agreement":null},{"id":"W122467843","doi":"10.1007/978-3-642-02940-0_11","title":"The Calculation of High-Pressure Ternary Phase Diagrams","year":2009,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Tekna Plasma Systems (Canada)","funders":"","keywords":"Phase diagram; Ternary operation; Thermodynamics; Phase (matter); Phase equilibrium; High pressure; Ternary plot; Binary number; Ternary numeral system; CALPHAD; Materials science; Statistical physics; Computer science; Chemistry; Physics; Mathematics; Arithmetic","score_opus":0.010539425418355949,"score_gpt":0.21550280838364838,"score_spread":0.20496338296529243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W122467843","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0064297053,0.0033497869,0.00014078454,0.0004204242,0.0018823752,0.00068680936,0.0011489803,0.00009447905,0.98584664],"genre_scores_gemma":[0.4467948,0.0005556094,0.00013969705,0.00008869208,0.0006525857,7.2311093e-7,0.0007638867,0.000010257494,0.55099374],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988273,0.0000257826,0.00035623534,0.00024625577,0.00034515967,0.00019929228],"domain_scores_gemma":[0.9990816,0.00012397603,0.00026486345,0.00039159434,0.00006226262,0.00007567365],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018338453,0.00023302682,0.00034645328,0.000037646427,0.00014032488,0.0000731734,0.00031850656,0.00019473143,0.0034108693],"category_scores_gemma":[0.0000076165197,0.00013790285,0.00011673532,0.00001847794,0.00009702719,0.00008555877,0.000016427975,0.00012338953,0.00023713888],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003071417,0.000055217584,0.00023704916,0.0001248943,0.00050520705,0.000051507774,0.00011224637,0.0020952763,0.0003177056,0.20660375,0.025545217,0.76404476],"study_design_scores_gemma":[0.00048067913,0.00032308119,0.0044094254,0.00006444324,0.00020734235,0.0000038059075,0.0000023770021,0.0007160923,0.00030682355,0.07142066,0.92169815,0.00036708498],"about_ca_topic_score_codex":0.0017320396,"about_ca_topic_score_gemma":0.0006561691,"teacher_disagreement_score":0.896153,"about_ca_system_score_codex":0.0000010451201,"about_ca_system_score_gemma":0.000032313088,"threshold_uncertainty_score":0.9975001},"labels":[],"label_agreement":null},{"id":"W1233791839","doi":"10.1016/j.epsl.2015.08.023","title":"Diamonds in ophiolites: Contamination or a new diamond growth environment?","year":2015,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"New South Wales Government; Chinese Academy of Geological Sciences; Chinese Academy of Sciences; National Cancer Research Institute; University of New South Wales; University of Alberta; Macquarie University; Australian National Fabrication Facility","keywords":"Ophiolite; Geology; Diamond; Geochemistry; Massif; Fractionation; Trace element; Mineralogy; Materials science; Paleontology; Chemistry; Metallurgy; Tectonics","score_opus":0.015155348570862636,"score_gpt":0.1875818879920476,"score_spread":0.17242653942118497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1233791839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99680114,0.0002603813,0.000047361376,0.0011494223,0.00037983072,0.00018229772,0.00007578724,0.000021439002,0.0010823513],"genre_scores_gemma":[0.9971558,0.000085904285,0.00086475175,0.0012757252,0.00018721251,8.1165973e-7,0.00017132053,0.0000026611885,0.00025581496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99845964,0.00006286602,0.00020580261,0.00039571745,0.00041981708,0.0004561513],"domain_scores_gemma":[0.9992316,0.00010174136,0.00006518943,0.00015697275,0.000009610569,0.0004349325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058053556,0.00016376583,0.00019614988,0.00018198589,0.000114425246,0.00017122309,0.00026031307,0.00004385181,0.0005522274],"category_scores_gemma":[0.000057582507,0.00012350178,0.000016047234,0.00029280304,0.00028330844,0.0008044952,0.000020993983,0.0001023357,0.0002495966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022902695,0.000022578848,0.96936524,0.000026475329,0.000011054583,0.00023651078,0.0018369654,0.005542932,0.0037475443,0.00011555472,0.003832952,0.015033142],"study_design_scores_gemma":[0.0006205509,0.00019596278,0.9868279,0.000015300351,0.000007647296,0.0000229553,0.000074995165,0.0026794337,0.00031903558,0.0002865436,0.008702656,0.00024702976],"about_ca_topic_score_codex":0.0062219114,"about_ca_topic_score_gemma":0.0012847959,"teacher_disagreement_score":0.017462626,"about_ca_system_score_codex":0.000003644283,"about_ca_system_score_gemma":0.00010406223,"threshold_uncertainty_score":0.94057107},"labels":[],"label_agreement":null},{"id":"W12603904","doi":"10.1016/b978-044452748-6.00008-0","title":"Theory and Observations – Teleseismic Body-Wave Scattering and Receiver-Side Structure","year":2007,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Seismogram; Scattering; Receiver function; Inverse scattering problem; Inverse problem; Deconvolution; Geology; Algorithm; Seismology; Computer science; Mathematics; Mathematical analysis; Lithosphere; Physics; Optics","score_opus":0.02195466228991701,"score_gpt":0.21179281697229985,"score_spread":0.18983815468238283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W12603904","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.080243334,0.0022455787,0.0000069482107,0.000052125943,0.0006786844,0.00043239782,0.000942829,0.000054627668,0.91534346],"genre_scores_gemma":[0.1425525,0.00054203725,0.0009100317,0.0008686081,0.00085522723,0.0000019229788,0.00037784048,0.0000410884,0.8538507],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99875116,0.000044031625,0.00029522608,0.0004268131,0.00019944765,0.00028334328],"domain_scores_gemma":[0.99918115,0.00017329326,0.0001711079,0.00027787068,0.000044084994,0.00015250136],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00034132012,0.00034096857,0.0004124237,0.00010019139,0.00021814299,0.0001377703,0.00012782266,0.00026031223,0.00072988344],"category_scores_gemma":[0.0000129139235,0.0002892707,0.000052986168,0.000011151491,0.00021806046,0.00008735862,0.000051415074,0.0002583561,0.000033414995],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000335932,9.3901724e-7,0.00028044684,0.00012877521,0.000087527646,0.00004314844,0.00022124496,0.0000044301423,0.0007184975,0.0072992723,0.00004331779,0.9911388],"study_design_scores_gemma":[0.00022181861,0.00005413695,0.03142479,0.00029400832,0.00017019443,0.0000643607,0.000016244045,0.000025466528,0.00016391254,0.15289971,0.81403595,0.0006294095],"about_ca_topic_score_codex":0.000027149297,"about_ca_topic_score_gemma":0.0002618816,"teacher_disagreement_score":0.9905094,"about_ca_system_score_codex":0.0000037579516,"about_ca_system_score_gemma":0.000040461386,"threshold_uncertainty_score":0.99995595},"labels":[],"label_agreement":null},{"id":"W1412375272","doi":"10.1038/srep12823","title":"The electrical conductivity of Al2O3 under shock-compression","year":2015,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China; Western Canada Research Grid; Compute Canada; University of Saskatchewan; National Science Foundation","keywords":"Sapphire; Materials science; Compression (physics); Shock (circulatory); Opacity; Electrical resistivity and conductivity; Conductivity; Shock front; Thermal conductivity; Thermodynamics; Thermodynamic equilibrium; Metal; Scattering; Shock wave; Composite material; Metallurgy; Chemistry; Optics; Physics; Laser; Physical chemistry","score_opus":0.028255301860699883,"score_gpt":0.24108224872858702,"score_spread":0.21282694686788714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1412375272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98657364,0.00032743745,0.00007394509,0.00014787709,0.0083806,0.00013337003,0.000006074212,0.000021339927,0.0043357117],"genre_scores_gemma":[0.9984016,0.0000026022367,0.000120498546,0.000010401788,0.00008939337,8.289893e-7,0.000032175474,0.0000019253164,0.0013406213],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985314,0.00009775412,0.00028834667,0.00031150793,0.0005295934,0.00024142093],"domain_scores_gemma":[0.9989646,0.00007052869,0.00020925657,0.00048340895,0.00013746374,0.0001347094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017716535,0.00008037523,0.0001465909,0.000035037352,0.00028677698,0.00019160846,0.00016276061,0.000040155977,0.00018839152],"category_scores_gemma":[0.000084352774,0.00004585114,0.00004547186,0.00024042785,0.00025522546,0.00016005654,0.00002508839,0.00006019324,0.000049317452],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030020537,0.00033648312,0.15802668,0.0000641844,0.00016727758,0.00043466125,0.0020813541,0.0111307455,0.4019652,0.006713046,0.3758078,0.04297238],"study_design_scores_gemma":[0.00030405418,0.00017527105,0.06969943,0.000028757493,0.000037054186,0.00016647666,0.00027511222,0.0016547877,0.09932925,0.32658693,0.5013367,0.0004061789],"about_ca_topic_score_codex":0.00054099836,"about_ca_topic_score_gemma":0.00018257395,"teacher_disagreement_score":0.3198739,"about_ca_system_score_codex":0.0000027875765,"about_ca_system_score_gemma":0.00016179406,"threshold_uncertainty_score":0.22056855},"labels":[],"label_agreement":null},{"id":"W1438525221","doi":"10.1016/j.jrmge.2015.07.004","title":"Effects of porosity on seismic velocities, elastic moduli and Poisson's ratios of solid materials and rocks","year":2015,"lang":"en","type":"article","venue":"Journal of Rock Mechanics and Geotechnical Engineering","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Porosity; Poisson's ratio; Poisson distribution; Mineralogy; Moduli; Isotropy; Materials science; Auxetics; Shear (geology); Composite material; Geology; Physics; Mathematics; Optics","score_opus":0.005792419503817097,"score_gpt":0.18280415530345748,"score_spread":0.17701173579964039,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1438525221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9569899,0.00062433555,0.041900635,0.0000423279,0.00029341868,0.00009106073,0.00004868449,0.0000073773977,0.000002258106],"genre_scores_gemma":[0.99924046,0.00028217645,0.00037374927,0.00001624403,0.00007511866,3.3616655e-7,0.0000022141078,0.000004693454,0.000005009323],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99922365,0.000024333118,0.00033250314,0.000098446326,0.00018866865,0.00013238609],"domain_scores_gemma":[0.99937993,0.00012758035,0.00021506564,0.00006319683,0.00006790353,0.00014631645],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003538902,0.00011835715,0.00040707635,0.00007333898,0.00002782686,0.000020909552,0.00007607437,0.00009191638,0.0000065176423],"category_scores_gemma":[0.00013650529,0.00009330111,0.000026063315,0.000049024602,0.0000068279014,0.00010292856,0.000033390876,0.0001051325,3.6018577e-7],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025844434,0.000045894023,0.00003969219,0.00077044626,0.000102473205,0.00003329507,0.00022562518,0.76691335,0.22882774,0.0012166138,0.00007923228,0.0014871618],"study_design_scores_gemma":[0.002759124,0.004308867,0.005626144,0.0010208978,0.00030343456,0.00027874834,0.00009095869,0.6092111,0.3637526,0.011265069,0.0008000224,0.00058308063],"about_ca_topic_score_codex":0.0000706046,"about_ca_topic_score_gemma":0.0000018758432,"teacher_disagreement_score":0.15770231,"about_ca_system_score_codex":0.000002692181,"about_ca_system_score_gemma":0.00002483125,"threshold_uncertainty_score":0.3804709},"labels":[],"label_agreement":null},{"id":"W1490207451","doi":"10.1063/1.4929368","title":"Pressure-induced changes in the electron density distribution in <i>α</i>-Ge near the <i>α-β</i> transition","year":2015,"lang":"en","type":"article","venue":"Applied Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Argonne National Laboratory; Chinese Academy of Sciences; Sandia National Laboratories; China Scholarship Council; U.S. Department of Energy","keywords":"Valence (chemistry); Atomic orbital; Chemistry; Atomic physics; Electronic structure; Electron density; Valence electron; Synchrotron; Diamond anvil cell; Condensed matter physics; Crystallography; Electron; Molecular physics; Diffraction; Physics; Computational chemistry; Optics","score_opus":0.013527302852103146,"score_gpt":0.19676999560447356,"score_spread":0.1832426927523704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1490207451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949695,0.000027564376,0.00017420435,0.0038017444,0.00015849112,0.00043138224,0.00007087654,0.000019361329,0.00034687374],"genre_scores_gemma":[0.99625456,0.000005018617,0.0000130654025,0.0030017805,0.0003158179,0.000016568696,0.00038719425,0.0000043657146,0.0000016271923],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99885356,0.00016141334,0.00013783317,0.00022239551,0.0002921011,0.00033266665],"domain_scores_gemma":[0.99955285,0.000085352665,0.000064696476,0.00024421694,0.0000137616835,0.00003914836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056508783,0.00014706494,0.00016702486,0.0000120581835,0.000141763,0.00014433257,0.0002773464,0.000048017664,0.000008349746],"category_scores_gemma":[0.0000036232373,0.00009344408,0.000029659717,0.00027835902,0.00007661117,0.00010619284,0.000009196299,0.00020536804,0.000046785695],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011042433,0.0004449886,0.010538062,0.00015387574,0.00015757467,0.00007174585,0.04353678,0.14697763,0.7380354,0.01578106,0.025094463,0.0181042],"study_design_scores_gemma":[0.008210087,0.000752438,0.5753792,0.0001267149,0.00052900525,0.000028797574,0.0028080563,0.016390434,0.260587,0.02710245,0.104927495,0.0031583211],"about_ca_topic_score_codex":0.0033168867,"about_ca_topic_score_gemma":0.0022407467,"teacher_disagreement_score":0.56484115,"about_ca_system_score_codex":0.000006835051,"about_ca_system_score_gemma":0.000033231438,"threshold_uncertainty_score":0.50141627},"labels":[],"label_agreement":null},{"id":"W1491977556","doi":"","title":"Obtaining Unique, Comprehensive Deep Seismic Sounding Data Sets for CTBT Monitoring and Broad Seismological Studies","year":2007,"lang":"en","type":"article","venue":"Defense Technical Information Center (DTIC)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Depth sounding; Geology; Coda","score_opus":0.09012821163966218,"score_gpt":0.3315097952613531,"score_spread":0.24138158362169093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1491977556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9467892,0.0005110962,0.049226645,0.00025873637,0.0010178111,0.0007190871,0.0004282405,0.00027138548,0.00077776896],"genre_scores_gemma":[0.9872666,0.00015121147,0.011092162,0.000569382,0.00013050511,0.0000044590065,0.0007719339,0.0000044900225,0.000009262661],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99855745,0.00004369347,0.0005324818,0.00022613279,0.0002183154,0.00042190423],"domain_scores_gemma":[0.9986679,0.00056776276,0.00018467726,0.00030572023,0.00014324488,0.00013068099],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075671816,0.00018896704,0.00029856223,0.00010006873,0.00027718095,0.00016515575,0.00028728842,0.00012717403,0.000022188313],"category_scores_gemma":[0.0001905797,0.0001525656,0.0000413784,0.00014099272,0.00012170709,0.00095383,0.00016576657,0.00015135681,0.000043122458],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002905109,0.00028164746,0.24910556,0.0021515947,0.0011408011,0.00014565335,0.011004585,0.011205745,0.0017482043,0.007506069,0.015946262,0.69685876],"study_design_scores_gemma":[0.00456176,0.0009178276,0.45714292,0.00059167994,0.00031417605,0.0003363637,0.0061970176,0.026542658,0.0016462179,0.009738807,0.48999268,0.002017888],"about_ca_topic_score_codex":0.000072698596,"about_ca_topic_score_gemma":0.000012948282,"teacher_disagreement_score":0.6948409,"about_ca_system_score_codex":0.000010991373,"about_ca_system_score_gemma":0.000013457629,"threshold_uncertainty_score":0.62214446},"labels":[],"label_agreement":null},{"id":"W1502075163","doi":"10.1002/jgrb.50114","title":"Low shear velocities in the sub‐lithospheric mantle beneath the Indian shield?","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Education, India; Ministry of Earth Sciences","keywords":"Geology; Indian Shield; Lithosphere; Craton; Discontinuity (linguistics); Shield; Seismology; Classification of discontinuities; Mantle (geology); Mantle plume; Archean; Precambrian; Shear zone; Transition zone; Plume; Crust; Shear (geology); Baltic Shield; Geophysics; Petrology; Geochemistry; Tectonics","score_opus":0.024072411896120326,"score_gpt":0.27876451179820955,"score_spread":0.25469209990208924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1502075163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954351,0.00017457393,0.000006929765,0.0023713198,0.0002431117,0.00030154455,0.00001847032,0.0000048490183,0.0014440629],"genre_scores_gemma":[0.99816495,0.000219312,0.00008428391,0.00025771046,0.0009648503,0.0000049159207,0.000005507449,0.000006032201,0.00029241192],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9967369,0.0007161891,0.0004032967,0.00016671784,0.0012855023,0.000691414],"domain_scores_gemma":[0.99807864,0.0010454169,0.00013817058,0.00031703332,0.0002384741,0.00018223962],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001993633,0.00014877823,0.00032615187,0.000090483714,0.0003339094,0.000500325,0.0009209658,0.00007153752,0.0011539877],"category_scores_gemma":[0.00021298553,0.000071706774,0.00013515925,0.0005429563,0.00033163972,0.00045503242,0.000048997055,0.00087382534,0.0008506127],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022671225,0.0034592543,0.11445973,0.0011619881,0.0012343618,0.003781412,0.12098727,0.016958011,0.049180638,0.0163533,0.11142689,0.55873],"study_design_scores_gemma":[0.0003923285,0.00088078337,0.9693406,0.00009260177,0.000011313067,0.00003855086,0.0031996553,0.0009812078,0.0025111614,0.017361084,0.0050075683,0.00018313777],"about_ca_topic_score_codex":0.0057883062,"about_ca_topic_score_gemma":0.0005861816,"teacher_disagreement_score":0.85488087,"about_ca_system_score_codex":0.00000510459,"about_ca_system_score_gemma":0.00015834763,"threshold_uncertainty_score":0.99992734},"labels":[],"label_agreement":null},{"id":"W1504250525","doi":"10.1109/plasma.2000.854855","title":"Shock waves generated by intense femtosecond lasers","year":2002,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Laser; Shock wave; Femtosecond; Plasma; Atomic physics; Shock (circulatory); Electromagnetic radiation; Physics; Wavelength; Relaxation (psychology); Thermal conduction; Electron; Pulse (music); Optics; Materials science; Mechanics; Thermodynamics","score_opus":0.012977880365029717,"score_gpt":0.17656312813981465,"score_spread":0.16358524777478492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1504250525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9656646,0.00029715803,0.000012421732,0.0003015742,0.00046546495,0.00007297661,0.00027626188,0.00006166107,0.032847874],"genre_scores_gemma":[0.9791355,0.000067723835,0.00013778274,0.00070089725,0.00011011848,5.240758e-7,0.0001990242,0.0000030228139,0.019645402],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993052,0.000036096222,0.00013626883,0.0001843443,0.000107662134,0.0002304121],"domain_scores_gemma":[0.99966764,0.000032237283,0.000030546304,0.00013526871,0.000026275238,0.000108057],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00007459459,0.00010545701,0.00013294243,0.000023462193,0.00008396134,0.00009498912,0.00012384818,0.000045392982,0.06596657],"category_scores_gemma":[0.000008144007,0.00007707629,0.000029384675,0.00008348179,0.000034556942,0.00013665087,0.000007267913,0.000043671953,0.0023923605],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023812054,0.00003316608,0.009300729,0.000018486422,0.00006538011,0.000029107772,0.00035307324,0.0003838042,0.031168027,0.00017524177,0.94587916,0.01256999],"study_design_scores_gemma":[0.0013767398,0.0005055296,0.033579282,0.000020371428,0.00006614585,0.000027418038,0.00037489898,0.04227181,0.1238873,0.0011102036,0.7954332,0.0013470992],"about_ca_topic_score_codex":0.001900118,"about_ca_topic_score_gemma":0.0006486496,"teacher_disagreement_score":0.15044598,"about_ca_system_score_codex":8.1580794e-7,"about_ca_system_score_gemma":0.0000043905284,"threshold_uncertainty_score":0.9983844},"labels":[],"label_agreement":null},{"id":"W1505059248","doi":"10.1002/2015gl064522","title":"Stability and properties of liquid CO<sub>2</sub> at high pressure and high temperature: Implications for electrical conductivities in Earth's lower mantle","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Western Canada Research Grid","keywords":"Mantle (geology); Oxygen; Materials science; Delocalized electron; Chemical physics; Ionic bonding; Thermodynamics; Metal; Chemistry; Ion; Geology; Geophysics; Physics; Metallurgy","score_opus":0.04542808469584391,"score_gpt":0.2680440962217054,"score_spread":0.22261601152586147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1505059248","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99580187,0.00038845587,0.0000026388727,0.002660911,0.000085949025,0.00065137376,0.00037032686,0.000015515707,0.000022951544],"genre_scores_gemma":[0.99948686,0.00004770387,0.00006183682,0.0000932909,0.00016342006,0.000042798158,0.00006016824,0.000007588229,0.000036332796],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9981737,0.00028762443,0.00022037864,0.0004199801,0.00038145386,0.00051686226],"domain_scores_gemma":[0.9989294,0.00039283466,0.000047059875,0.00025137284,0.00017178491,0.00020758872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065924635,0.00015134613,0.0003334884,0.00008847654,0.00016625333,0.00009074594,0.00016162824,0.000085318876,0.000018981369],"category_scores_gemma":[0.00020631624,0.000116439995,0.00003447911,0.00020907153,0.0005167887,0.00026006257,0.00006956135,0.00022166061,0.000011674621],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00083217135,0.000064990774,0.0019178549,0.00011412393,0.000028557783,0.0000021147162,0.00022783774,0.000031646305,0.9944236,0.00084039185,0.0011400613,0.0003765982],"study_design_scores_gemma":[0.0008806613,0.0010100362,0.14908612,0.000035691373,0.000024014245,0.000002981786,0.00006048865,0.00015493321,0.84470046,0.0022136916,0.0015758056,0.0002551077],"about_ca_topic_score_codex":0.0020039321,"about_ca_topic_score_gemma":0.00036453205,"teacher_disagreement_score":0.14972319,"about_ca_system_score_codex":0.0000075775183,"about_ca_system_score_gemma":0.00009185855,"threshold_uncertainty_score":0.47482854},"labels":[],"label_agreement":null},{"id":"W1517234230","doi":"10.1029/174gm15","title":"Mantle dynamics and the D″ layer: Impacts of the post perovskite phase","year":2007,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mantle (geology); Geology; Post-perovskite; Transition zone; Geophysics; Earth science","score_opus":0.00990957649122916,"score_gpt":0.21768211503331975,"score_spread":0.20777253854209057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1517234230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6996939,0.0018943732,0.00003211672,0.0008295657,0.0016225905,0.001353002,0.0041506104,0.00006481164,0.290359],"genre_scores_gemma":[0.9860117,0.00031465612,0.00004017309,0.0003052583,0.00039526672,0.000001406098,0.00021848606,0.000017941005,0.012695117],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99854314,0.000050791812,0.00035736154,0.000314106,0.0003934052,0.00034120213],"domain_scores_gemma":[0.99867153,0.0002690004,0.00031542787,0.0005317194,0.000083529114,0.0001287972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027749522,0.00033878896,0.00055083376,0.000078186866,0.00021695219,0.00008186843,0.00044604606,0.00019389334,0.0003523657],"category_scores_gemma":[0.000014587922,0.00017412372,0.00036981353,0.00008849006,0.00083120976,0.00008417521,0.000079964666,0.0003290311,0.00007898923],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0030158672,0.00027531758,0.0040588775,0.00061880954,0.0015044875,0.000088246634,0.0015907129,0.000096391115,0.0008620953,0.820819,0.0025413388,0.16452886],"study_design_scores_gemma":[0.015741106,0.002925396,0.3585834,0.0012405862,0.0033263646,0.000119104574,0.0002884311,0.009139911,0.0013606705,0.47415712,0.12886396,0.00425396],"about_ca_topic_score_codex":0.0027029756,"about_ca_topic_score_gemma":0.0013644985,"teacher_disagreement_score":0.3545245,"about_ca_system_score_codex":0.0000023548464,"about_ca_system_score_gemma":0.000036788322,"threshold_uncertainty_score":0.7100559},"labels":[],"label_agreement":null},{"id":"W1518740426","doi":"10.1038/ngeo.2007.44","title":"Core–mantle boundary heat flow","year":2007,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":496,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Earth's internal heat budget; Mantle (geology); Core–mantle boundary; Geology; Geophysics; Radiogenic nuclide; Planetary differentiation; Mantle convection; Geodynamics; Hotspot (geology); Mantle wedge; Subduction; Tectonics; Paleontology","score_opus":0.012319869695722728,"score_gpt":0.24363661317340635,"score_spread":0.2313167434776836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1518740426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9809752,0.00092545873,0.0007293117,0.00019837251,0.003899706,0.0001374646,0.00014338666,0.00007799575,0.012913067],"genre_scores_gemma":[0.9939605,0.000019883366,0.0032251435,0.0010002002,0.00044819782,3.4031692e-7,0.000057137073,0.000003166269,0.0012854387],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842316,0.000018162747,0.0001758279,0.000366099,0.00047676594,0.000539959],"domain_scores_gemma":[0.99934894,0.0001036574,0.000038889357,0.00026669793,0.00005790513,0.00018392301],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00084705127,0.00014077184,0.00015666077,0.000075165364,0.00035219433,0.00013456981,0.00045015616,0.00017496232,0.0012793366],"category_scores_gemma":[0.0000685378,0.00010706447,0.0000470642,0.00040644692,0.00020192606,0.0002794985,0.000026526808,0.00028702835,0.0005341816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005316838,0.0002617666,0.63440615,0.00020037682,0.00006898346,0.00088872766,0.0016934823,0.0030055505,0.09385196,0.01042274,0.04616357,0.20850502],"study_design_scores_gemma":[0.0001976835,0.00011074218,0.74214506,0.000018478484,0.000010050081,0.00003224044,0.000036535457,0.0026619164,0.0019566054,0.0026736911,0.24983682,0.00032018352],"about_ca_topic_score_codex":0.0009187609,"about_ca_topic_score_gemma":0.001242436,"teacher_disagreement_score":0.20818484,"about_ca_system_score_codex":0.0000037181092,"about_ca_system_score_gemma":0.00007540868,"threshold_uncertainty_score":0.9996336},"labels":[],"label_agreement":null},{"id":"W1520790674","doi":"10.1029/2007tc002132","title":"Stacked uppermost mantle layers within the Slave craton of NW Canada as defined by anisotropic seismic discontinuities","year":2008,"lang":"en","type":"article","venue":"Tectonics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Kimberlite; Classification of discontinuities; Mantle (geology); Anisotropy; Seismology; Craton; Seismic array; Geophysics; Discontinuity (linguistics); Seismogram; Petrology; Tectonics","score_opus":0.006831149485949141,"score_gpt":0.17514740795799025,"score_spread":0.1683162584720411,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1520790674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99566,0.00040494822,0.000011195934,0.00029229632,0.00041909114,0.00014058851,0.000611656,0.000021652595,0.0024385909],"genre_scores_gemma":[0.9983009,0.00007912346,0.00006440526,0.00025075185,0.00003769529,0.0000014305615,0.000109075525,0.000005796264,0.0011508344],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9990364,0.00005888008,0.00022568913,0.00016329426,0.0002697583,0.00024602085],"domain_scores_gemma":[0.9994377,0.00008904349,0.00013282833,0.00024652452,0.00003409304,0.000059827395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009908214,0.0001376702,0.00022039916,0.000015718077,0.00020951022,0.000028517648,0.00022003875,0.000043002594,0.000842617],"category_scores_gemma":[0.000023199067,0.00009041911,0.00003594434,0.000101051904,0.00012856106,0.00007441108,0.00001846401,0.00008873277,0.000037990234],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013810146,0.0005024407,0.2361378,0.00092836475,0.0017875365,0.0012043472,0.031529017,0.06080269,0.16134425,0.02017564,0.47078365,0.013423254],"study_design_scores_gemma":[0.0039767935,0.0017404788,0.36251482,0.00018982805,0.00036860627,0.00029567425,0.006133448,0.019629328,0.3484245,0.008239193,0.24577253,0.0027148055],"about_ca_topic_score_codex":0.65907586,"about_ca_topic_score_gemma":0.47642425,"teacher_disagreement_score":0.22501111,"about_ca_system_score_codex":0.0000074531426,"about_ca_system_score_gemma":0.00041113127,"threshold_uncertainty_score":0.9226065},"labels":[],"label_agreement":null},{"id":"W1527018161","doi":"10.1063/1.1773924","title":"Reconciliation of <i>ab initio</i> theory and experimental elastic properties of Al2O3","year":2004,"lang":"en","type":"article","venue":"Applied Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Ab initio; Ab initio quantum chemistry methods; Thermodynamics; Materials science; Sign (mathematics); Experimental data; Computational chemistry; Condensed matter physics; Theoretical physics; Statistical physics; Physics; Chemistry; Quantum mechanics; Molecule; Mathematics; Mathematical analysis","score_opus":0.011516417797135444,"score_gpt":0.18276013962125248,"score_spread":0.17124372182411704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1527018161","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99842346,0.0000846463,0.00031746173,0.000038875005,0.000097943106,0.00013526094,0.00003996165,0.0000106355155,0.00085174135],"genre_scores_gemma":[0.9993517,0.00000570201,0.00025751864,0.00026526581,0.00008116729,0.0000033378706,0.000029692052,0.0000036907654,0.0000019630768],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994568,0.00002385408,0.00015894172,0.00012612352,0.00012571107,0.000108548564],"domain_scores_gemma":[0.9997224,0.000033087916,0.00010615578,0.00009802525,0.000013268272,0.000027061398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010934026,0.00008923244,0.00016217667,0.000015679609,0.00003832276,0.000012340859,0.00007094148,0.000021994001,0.000036216177],"category_scores_gemma":[0.0000022582828,0.0000741835,0.000023437708,0.000054391312,0.00013793667,0.000093200084,0.0000101879605,0.0000337411,0.000014092168],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000087052664,0.000022606608,0.00015494767,0.00004722202,0.000022587732,3.4290363e-7,0.0011072041,0.0034412798,0.98443526,0.010177469,0.000020135065,0.00048388954],"study_design_scores_gemma":[0.00045740337,0.000051114057,0.0017262778,0.000028537728,0.000017218767,5.206458e-7,0.00021860914,0.0000084236935,0.99221045,0.005111808,0.00005278898,0.000116862204],"about_ca_topic_score_codex":0.0001824455,"about_ca_topic_score_gemma":0.0000049139767,"teacher_disagreement_score":0.007775173,"about_ca_system_score_codex":0.0000019485785,"about_ca_system_score_gemma":0.00001658884,"threshold_uncertainty_score":0.30251154},"labels":[],"label_agreement":null},{"id":"W1532997732","doi":"10.1029/2010gl043965","title":"Geodynamic models of Archean continental collision and the formation of mantle lithosphere keels","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Imbrication; Geology; Underplating; Lithosphere; Mantle (geology); Crust; Craton; Transition zone; Continental crust; Archean; Collision zone; Petrology; Crustal recycling; Geophysics; Mantle convection; Geochemistry; Seismology; Tectonics","score_opus":0.01813682859017436,"score_gpt":0.2579912510572722,"score_spread":0.23985442246709787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1532997732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971431,0.000032236185,0.00017150833,0.00117623,0.000112388865,0.00031595543,0.00011029103,0.0000065090744,0.00093177235],"genre_scores_gemma":[0.9994641,0.000030077515,0.0002392381,0.000046436562,0.00009995974,0.00000354198,0.000041379248,0.0000033239971,0.000071957395],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985607,0.00020301112,0.0002282749,0.00015902388,0.00055497553,0.0002939758],"domain_scores_gemma":[0.9989437,0.00056310085,0.00008514723,0.00022946359,0.000100107114,0.0000784664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009042965,0.00008612613,0.0002303684,0.0000420096,0.00012810084,0.00004775837,0.00025896248,0.0000428868,0.000108324246],"category_scores_gemma":[0.00007103942,0.000053166,0.000060114467,0.00015820228,0.00074890204,0.00025516734,0.00005957967,0.00026539146,0.000034889632],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016209253,0.00015217098,0.0019170245,0.0004403705,0.00007627573,0.000011122456,0.0025580148,0.0034013458,0.93410015,0.038912997,0.0027060937,0.01410351],"study_design_scores_gemma":[0.005693982,0.00068138813,0.19976215,0.00020475149,0.00007271347,0.000013093689,0.00084563973,0.59194076,0.09479344,0.10323087,0.0021693713,0.0005918436],"about_ca_topic_score_codex":0.0063074054,"about_ca_topic_score_gemma":0.00031509672,"teacher_disagreement_score":0.8393067,"about_ca_system_score_codex":0.000001440434,"about_ca_system_score_gemma":0.000023058972,"threshold_uncertainty_score":0.9534952},"labels":[],"label_agreement":null},{"id":"W1534014660","doi":"10.1002/jgrb.50220","title":"Influence of viscosity pressure dependence on deep lithospheric tectonics during continental collision","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Subduction; Mantle (geology); Continental collision; Collision zone; Mantle convection; Geophysics; Tectonics; Petrology; Seismology","score_opus":0.01304457261042342,"score_gpt":0.27589102561061735,"score_spread":0.26284645300019394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1534014660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987913,0.00018871886,0.000014855893,0.00009799265,0.00013468567,0.00030025124,0.000033455366,0.000008738386,0.00043005313],"genre_scores_gemma":[0.9989852,0.00016324215,0.0002986541,0.00001965073,0.00029578706,0.0000017516264,0.0000032604712,0.0000069413713,0.00022553606],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9966855,0.0003395309,0.0005495867,0.0002450105,0.0016005592,0.0005798059],"domain_scores_gemma":[0.99761975,0.0005093446,0.00035386212,0.00029178848,0.0008726482,0.00035263487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008283115,0.00017594092,0.0005138924,0.000115160095,0.00022967083,0.00015801656,0.00060536904,0.000095645424,0.0005698863],"category_scores_gemma":[0.0004354012,0.00012626246,0.00014821373,0.00042830838,0.00023757084,0.0006846933,0.000084091465,0.0006480857,0.00032352444],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028322388,0.001314965,0.08279183,0.0007778274,0.00051559805,0.0003396614,0.0012876301,0.3564899,0.54108816,0.0006504361,0.00083750696,0.011074256],"study_design_scores_gemma":[0.0005428628,0.0013536685,0.9354834,0.00019454968,0.00001957873,0.000016873495,0.000056222812,0.0043486655,0.056336895,0.0011476628,0.00034968834,0.00014995254],"about_ca_topic_score_codex":0.0027761327,"about_ca_topic_score_gemma":0.000092782546,"teacher_disagreement_score":0.85269153,"about_ca_system_score_codex":0.0000058009673,"about_ca_system_score_gemma":0.00014865813,"threshold_uncertainty_score":0.6239855},"labels":[],"label_agreement":null},{"id":"W1535820277","doi":"","title":"Implications for Core Formation of the Earth from High Pressure-Temperature Au Partitioning Experiments","year":2005,"lang":"en","type":"article","venue":"NASA STI Repository (National Aeronautics and Space Administration)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Aeronautics and Space Administration; University of Alberta; National Science Foundation","keywords":"Mantle (geology); Chondrite; Silicate; Trace element; Geology; Mineralogy; Mafic; Geochemistry; Meteorite; Planetary differentiation; Chemistry; Mantle wedge; Astrobiology; Tectonics; Lithosphere","score_opus":0.020583987200454037,"score_gpt":0.2507094400896207,"score_spread":0.23012545288916667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1535820277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99473506,0.0001551426,0.00038014102,0.0017635295,0.0003529805,0.00035667492,0.0010685116,0.000016083035,0.001171856],"genre_scores_gemma":[0.99606824,0.000008029377,0.0022634787,0.0000934922,0.00038376314,0.000018015318,0.0006188465,0.0000037021875,0.00054242095],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99912626,0.000032471584,0.0002810169,0.0001806948,0.000252405,0.00012716504],"domain_scores_gemma":[0.9992443,0.00012850799,0.00021159861,0.00013894083,0.00021473266,0.00006196094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011102369,0.0001093687,0.00012476358,0.00002046592,0.00048455596,0.00010481517,0.00011467058,0.00007649096,0.000061991086],"category_scores_gemma":[0.000033480497,0.00008489601,0.00004453559,0.00006367663,0.00007340448,0.00030352463,0.000012232217,0.00005641187,0.0000031891855],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060484663,0.0006055141,0.20819844,0.00029468304,0.0004921155,0.0000014557638,0.0030984147,0.04992239,0.36541682,0.36119246,0.0058929846,0.0042798626],"study_design_scores_gemma":[0.00036801706,0.00010336399,0.93550116,0.000025474921,0.000057945883,0.000006334474,0.000041776304,0.003415651,0.045330808,0.0038671056,0.011144541,0.00013780818],"about_ca_topic_score_codex":0.00018797332,"about_ca_topic_score_gemma":0.0005743337,"teacher_disagreement_score":0.72730273,"about_ca_system_score_codex":0.000007691085,"about_ca_system_score_gemma":0.0001910801,"threshold_uncertainty_score":0.37268618},"labels":[],"label_agreement":null},{"id":"W1536700970","doi":"10.1029/2007gc001627","title":"Influence of convergent plate boundaries on upper mantle flow and implications for seismic anisotropy","year":2007,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Geology; Mantle convection; Mantle (geology); Plate tectonics; Downwelling; Geophysics; Buoyancy; Convection; Subduction; Mechanics; Convergent boundary; Hotspot (geology); Oceanic crust; Physics; Seismology; Upwelling","score_opus":0.007486420967144747,"score_gpt":0.21695386056551022,"score_spread":0.20946743959836547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1536700970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958458,0.00015075535,0.0007276625,0.00008887107,0.00030698464,0.00034160464,0.001910466,0.000033553075,0.00059429306],"genre_scores_gemma":[0.9986345,0.000023512337,0.00034720218,0.000060958286,0.00025705466,0.000008877937,0.0004095501,0.000007754201,0.0002505992],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987161,0.000014792272,0.0003693568,0.00034138776,0.00016948038,0.00038886422],"domain_scores_gemma":[0.99900365,0.00014570117,0.00021673809,0.00035025284,0.000151558,0.00013209374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026562196,0.00020490756,0.000315578,0.000029300152,0.00028343004,0.000096355645,0.00019398112,0.00010170694,0.00005100324],"category_scores_gemma":[0.000024274192,0.00018843081,0.00007259399,0.000107179454,0.0001651256,0.0001131182,0.000022201582,0.00007255208,0.000041424784],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011147193,0.00034468,0.12762156,0.0044593643,0.000624119,0.000017692291,0.0018856226,0.058144763,0.770859,0.014249417,0.005196792,0.015482251],"study_design_scores_gemma":[0.0019371962,0.00057055533,0.5798825,0.00032553903,0.00019079218,0.000039269074,0.00032106225,0.011652858,0.30165383,0.03284938,0.06926189,0.0013151468],"about_ca_topic_score_codex":0.0012687189,"about_ca_topic_score_gemma":0.00005944651,"teacher_disagreement_score":0.46920517,"about_ca_system_score_codex":0.00000549496,"about_ca_system_score_gemma":0.000078602534,"threshold_uncertainty_score":0.7683986},"labels":[],"label_agreement":null},{"id":"W1542303810","doi":"10.1088/0953-8984/19/42/420301","title":"Proceedings of the 3rd Asian Conference on High Pressure Research, Lijiang City, Yunnan Province of China, October 16–20, 2006","year":2007,"lang":"en","type":"article","venue":"Journal of Physics Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"China; Presentation (obstetrics); High pressure; Library science; Political science; Geography; Engineering; Medicine; Archaeology; Engineering physics","score_opus":0.02260045690270094,"score_gpt":0.2541481249988131,"score_spread":0.23154766809611219,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1542303810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97805357,0.000044126857,0.000041814117,0.0010293862,0.00045381347,0.00026970424,0.0001571603,0.000004927386,0.019945519],"genre_scores_gemma":[0.9969697,0.00000567214,0.00014676226,0.0001705525,0.00046164676,3.9571893e-7,0.000004417778,0.00000946368,0.0022313767],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978057,0.00007473138,0.00058752135,0.0001876125,0.00096288294,0.00038150902],"domain_scores_gemma":[0.9980661,0.00010780439,0.00082744105,0.00021334714,0.0006675903,0.000117685224],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011861247,0.00017845,0.0004309704,0.000102941725,0.000116022115,0.00008580104,0.000629542,0.000096314674,0.0009729857],"category_scores_gemma":[0.00003294505,0.00011405984,0.00014544981,0.0002500972,0.00027518466,0.00033026826,0.00005769906,0.00045668025,0.000036098194],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019269702,0.00089565397,0.26549196,0.001659597,0.0007708163,0.00005944136,0.003756568,0.0007580739,0.5319036,0.025342168,0.15799476,0.009440333],"study_design_scores_gemma":[0.0010414439,0.0007591155,0.6281385,0.00064620154,0.00014055632,0.00002695016,0.00025442214,0.0000378015,0.3198435,0.043132905,0.005654957,0.0003236897],"about_ca_topic_score_codex":0.000508323,"about_ca_topic_score_gemma":0.00015830917,"teacher_disagreement_score":0.3626465,"about_ca_system_score_codex":0.0000070964857,"about_ca_system_score_gemma":0.00014783938,"threshold_uncertainty_score":0.9999403},"labels":[],"label_agreement":null},{"id":"W1542565838","doi":"10.1093/gji/ggv227","title":"A normal mode treatment of semi-diurnal body tides on an aspherical, rotating and anelastic Earth","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Science Council; Harvard University","keywords":"Geophysics; Normal mode; Earth's rotation; Geology; Mantle (geology); Geodesy; Oscillation (cell signaling); Physics","score_opus":0.02160023705004744,"score_gpt":0.26378013823847773,"score_spread":0.2421799011884303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1542565838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99716586,0.000035366254,0.0003031524,0.00011730917,0.0006989621,0.00005761318,0.00008916626,0.0000112899925,0.0015212845],"genre_scores_gemma":[0.9973319,0.000022379812,0.0012139345,0.000054601827,0.0011602096,9.4476076e-7,0.000046258374,0.0000047668527,0.00016495933],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987852,0.000086733744,0.0002872828,0.00017421435,0.00046042263,0.00020612047],"domain_scores_gemma":[0.9991808,0.000109055836,0.00018049724,0.000084871965,0.00013752352,0.00030725586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012853017,0.00014421223,0.00022633804,0.000050318147,0.000094404386,0.00016147351,0.00014221988,0.000036474583,0.00036425237],"category_scores_gemma":[0.0000366427,0.000103782426,0.00006540145,0.00005539665,0.00006899138,0.0003628734,0.000012963786,0.00010497834,0.00005426679],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005254488,0.004666219,0.23383771,0.00007138809,0.0018038591,0.0015895783,0.0077757747,0.31930083,0.06239226,0.008913156,0.0020549782,0.35233977],"study_design_scores_gemma":[0.0043459637,0.01380042,0.6279691,0.00017270718,0.00017502054,0.0010694702,0.0004899745,0.3033394,0.0095905075,0.028459933,0.00969615,0.0008913427],"about_ca_topic_score_codex":0.0007462763,"about_ca_topic_score_gemma":0.00005634721,"teacher_disagreement_score":0.3941314,"about_ca_system_score_codex":0.000007145289,"about_ca_system_score_gemma":0.00006972362,"threshold_uncertainty_score":0.42321244},"labels":[],"label_agreement":null},{"id":"W1547289598","doi":"10.1139/e09-076","title":"How the crust meets the mantle: Lithoprobe perspectives on the Mohorovičić discontinuity and crust–mantle transitionThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada; University of British Columbia; Memorial University of Newfoundland","funders":"","keywords":"Crust; Geology; Mantle (geology); Discontinuity (linguistics); Lithosphere; Tectonics; Oceanic crust; Geophysics; Seismology; Transect; Continental crust; Subduction","score_opus":0.009757262496140943,"score_gpt":0.18099052039585128,"score_spread":0.17123325789971033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1547289598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93524694,0.00085491076,0.0000020993762,0.060794085,0.00021768094,0.00039337703,0.00012608996,0.0000013430838,0.0023634504],"genre_scores_gemma":[0.9992243,0.00014133462,0.0000674429,0.00022878083,0.00022558888,0.0000027848378,4.7604928e-7,0.0000024846236,0.00010681879],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9985318,0.00029304053,0.0003262187,0.00017829797,0.00042199806,0.00024862957],"domain_scores_gemma":[0.9984366,0.0006456275,0.00041165247,0.00022312572,0.00018875429,0.000094212846],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026701214,0.00012881863,0.0002747394,0.00008062793,0.00049835484,0.00036327183,0.00053700316,0.000044501463,0.0013053188],"category_scores_gemma":[0.00055524224,0.00004733608,0.00006699905,0.0004180107,0.0030968678,0.00043281747,0.000012577878,0.00025653667,7.5933485e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0034100926,0.00047942818,0.17844902,0.0005360833,0.00076824677,0.000041339976,0.49316615,0.0010033385,0.044192176,0.25162184,0.011056493,0.015275804],"study_design_scores_gemma":[0.0020494268,0.0018358115,0.7517113,0.00064241653,0.00026394526,0.00009998571,0.14414416,0.00069193833,0.053672444,0.022853162,0.02152559,0.0005098411],"about_ca_topic_score_codex":0.018003175,"about_ca_topic_score_gemma":0.20843652,"teacher_disagreement_score":0.5732623,"about_ca_system_score_codex":0.0000021969527,"about_ca_system_score_gemma":0.00043164266,"threshold_uncertainty_score":0.99961615},"labels":[],"label_agreement":null},{"id":"W1552909705","doi":"10.1029/2005gc000924","title":"Mantle convection with reversing mobile plates: A benchmark study","year":2005,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Reversing; Geology; Convection; Mantle convection; Aperiodic graph; Geophysics; Mantle (geology); Oscillation (cell signaling); Plate tectonics; Nusselt number; Mechanics; Lithosphere; Seismology; Physics; Materials science; Mathematics","score_opus":0.004926612047766773,"score_gpt":0.1880271232128843,"score_spread":0.18310051116511755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1552909705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913062,0.00016230495,0.000032325122,0.000023002756,0.0004040309,0.0006406039,0.00018751797,0.0001154528,0.007128562],"genre_scores_gemma":[0.99751306,0.000007636328,0.00011822552,0.00002514852,0.0011248124,0.000024710627,0.00031988445,0.000011902195,0.00085462304],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980998,0.000065495326,0.00034981818,0.00054403424,0.0004412986,0.00049953704],"domain_scores_gemma":[0.9989334,0.00007190535,0.00022173263,0.00049494026,0.00011406527,0.0001639913],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023359334,0.00031370958,0.0004041449,0.000036052923,0.00035100087,0.00017783814,0.00027126414,0.000098838,0.0011100981],"category_scores_gemma":[0.000006367857,0.00026394232,0.00007202085,0.00025395176,0.000056784127,0.00032263686,0.000026202986,0.00017056552,0.0005584121],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021894986,0.0040722457,0.5336085,0.0035083464,0.0027558065,0.0007083814,0.018112225,0.13960223,0.20992497,0.00014352973,0.014627542,0.070746765],"study_design_scores_gemma":[0.019087203,0.008382689,0.20725393,0.0020071778,0.0019974448,0.0008365046,0.046712838,0.056518607,0.30629653,0.0016457082,0.33828866,0.010972719],"about_ca_topic_score_codex":0.004187555,"about_ca_topic_score_gemma":0.0005764662,"teacher_disagreement_score":0.32635453,"about_ca_system_score_codex":0.00001467739,"about_ca_system_score_gemma":0.000058070327,"threshold_uncertainty_score":0.9999813},"labels":[],"label_agreement":null},{"id":"W1556293097","doi":"10.1002/jgrb.50060","title":"Modification of continental lithosphere by tectonic processes: A tomographic image of central North America","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Manitoba Hydro","keywords":"Geology; Terrane; Rift; Lithosphere; Proterozoic; Gondwana; Seismology; Orogeny; Laurentia; Precambrian; Tectonics; Paleontology","score_opus":0.015545024852970882,"score_gpt":0.27522410765621813,"score_spread":0.25967908280324725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1556293097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99839896,0.00031540327,0.00009547892,0.0001939096,0.00008851807,0.00029019406,0.00020586686,0.0000061556634,0.00040548877],"genre_scores_gemma":[0.99867463,0.00047419936,0.00048630865,0.000010138342,0.00019629706,0.0000026199248,0.00004438185,0.0000067186324,0.00010473097],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973028,0.00022596854,0.0006438497,0.00019051798,0.0010880413,0.00054887537],"domain_scores_gemma":[0.9973964,0.0003143667,0.0005218777,0.00021938962,0.0012461463,0.00030181123],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003731047,0.00014829589,0.00053868874,0.00012644076,0.00009014756,0.000092399605,0.0004738102,0.000055533572,0.00098274],"category_scores_gemma":[0.00027120727,0.000107652086,0.00016395276,0.00080119143,0.0004605049,0.000558225,0.000032721844,0.00035484467,0.00008630259],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00194265,0.0033409148,0.17005688,0.0026219722,0.0009613039,0.000071809336,0.0036861028,0.0019753168,0.704905,0.00020810947,0.016089413,0.09414056],"study_design_scores_gemma":[0.0010862502,0.0030373107,0.93665713,0.0002277743,0.000053194763,0.00001051687,0.00060545566,0.00286607,0.050283663,0.0018926525,0.00297937,0.0003006012],"about_ca_topic_score_codex":0.004897475,"about_ca_topic_score_gemma":0.00014008045,"teacher_disagreement_score":0.76660025,"about_ca_system_score_codex":0.0000035362877,"about_ca_system_score_gemma":0.00028618277,"threshold_uncertainty_score":0.9999305},"labels":[],"label_agreement":null},{"id":"W1557166423","doi":"10.1029/2007gc001839","title":"Formation and exhumation of ultra‐high‐pressure rocks during continental collision: Role of detachment in the subduction channel","year":2008,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Subduction; Continental collision; Eclogitization; Slab; Geophysics; Buoyancy; Collision zone; Petrology; Seismology; Tectonics; Oceanic crust; Mechanics","score_opus":0.005754819609301302,"score_gpt":0.17353122122370282,"score_spread":0.16777640161440152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1557166423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99811816,0.0005639652,0.000017908182,0.000017928769,0.00014338593,0.00028643472,0.0002534359,0.00001112688,0.0005876532],"genre_scores_gemma":[0.9993041,0.00010549337,0.000010904319,0.000003129278,0.00018172753,0.000008061682,0.00035261404,0.0000031621037,0.000030812047],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99880576,0.000065005195,0.00042173185,0.0001862443,0.00033527598,0.0001859734],"domain_scores_gemma":[0.99926484,0.000050438786,0.0003425651,0.00021914084,0.00008725342,0.000035770543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021850133,0.00014313828,0.0002848046,0.000029263869,0.00013303419,0.000021677404,0.00015601625,0.000078683166,0.00004779195],"category_scores_gemma":[0.0000106693,0.00011348868,0.00004783171,0.00015162134,0.000058931124,0.00026148924,0.000012909346,0.00007730264,0.000005034151],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024459563,0.0002072286,0.026046222,0.0023423305,0.0000957762,0.000010944458,0.0084639555,0.020706767,0.9407566,0.00010408286,0.00012002254,0.00090143096],"study_design_scores_gemma":[0.0010032364,0.00010077707,0.22494927,0.00019647834,0.000057808473,0.00009391935,0.002644159,0.0044173105,0.7653475,0.00070929306,0.00020322116,0.00027704568],"about_ca_topic_score_codex":0.0032864348,"about_ca_topic_score_gemma":0.000059724232,"teacher_disagreement_score":0.19890304,"about_ca_system_score_codex":0.0000031928698,"about_ca_system_score_gemma":0.000017029439,"threshold_uncertainty_score":0.49681282},"labels":[],"label_agreement":null},{"id":"W1558050095","doi":"10.1029/164gm06","title":"Archean thermal regime and stabilization of the cratons","year":2006,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Centre National de la Recherche Scientifique","keywords":"Archean; Craton; Geology; Thermal; Geophysics; Earth science; Geochemistry; Physics; Paleontology; Tectonics; Thermodynamics","score_opus":0.008685128219921418,"score_gpt":0.17462872361280002,"score_spread":0.1659435953928786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1558050095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.55129564,0.00072372425,0.000032715718,0.00026210488,0.0007461815,0.0007780497,0.0012995683,0.000069298076,0.44479272],"genre_scores_gemma":[0.9768085,0.000058995203,0.00006491385,0.00005288133,0.0003645395,0.0000016385516,0.00020109722,0.000015413138,0.022432033],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9989076,0.000041817922,0.00026445062,0.0002938506,0.00028068427,0.00021159589],"domain_scores_gemma":[0.99920374,0.00008708082,0.00021864798,0.00037132704,0.000050240087,0.00006893856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008609317,0.00024134354,0.00035549313,0.000053499938,0.00012297687,0.000042131483,0.0002325866,0.0001567402,0.00036934376],"category_scores_gemma":[0.000004683819,0.00015920648,0.00018465387,0.00005741857,0.00038251426,0.00007063596,0.00004269315,0.00017574607,0.000046500772],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000774045,0.0005563911,0.08521924,0.0021684095,0.0018082248,0.000057722118,0.0022786385,0.0066711814,0.020470187,0.67301327,0.03599039,0.17099231],"study_design_scores_gemma":[0.0005477095,0.00036543654,0.6548757,0.0002764732,0.0004096933,0.0000035021005,0.0000150384385,0.0005408921,0.0012553663,0.24960855,0.091068976,0.0010326643],"about_ca_topic_score_codex":0.0010963642,"about_ca_topic_score_gemma":0.00019071177,"teacher_disagreement_score":0.56965643,"about_ca_system_score_codex":0.000001095856,"about_ca_system_score_gemma":0.00003329638,"threshold_uncertainty_score":0.6492252},"labels":[],"label_agreement":null},{"id":"W1559584481","doi":"10.1002/2014jb011802","title":"Sharp mantle transition from cratons to Cordillera in southwestern Canada","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Helmholtz-Alberta Initiative","keywords":"Geology; Craton; Mantle (geology); Lithosphere; Transition zone; Foreland basin; Subduction; Terrane; Seismology; Crust; Paleontology; Geophysics; Tectonics","score_opus":0.048504575349437896,"score_gpt":0.3013517490641233,"score_spread":0.2528471737146854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1559584481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966778,0.00005622285,0.000024513705,0.0012786092,0.0003986719,0.00014095647,0.00029542483,0.0000037010245,0.0011241124],"genre_scores_gemma":[0.99860555,0.000012218303,0.00016652956,0.0001992866,0.0008296244,9.021925e-7,0.00004398022,0.0000054580255,0.00013644839],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9972592,0.00030429687,0.0003914168,0.00019432166,0.0013329091,0.00051785196],"domain_scores_gemma":[0.9983803,0.00027869965,0.00008762702,0.00017715298,0.00038231217,0.00069390476],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00077469106,0.00012530811,0.00039553698,0.000150262,0.0000791097,0.0001356522,0.00035490305,0.000051543324,0.0009883104],"category_scores_gemma":[0.00016534636,0.00009767011,0.000062526786,0.0003696484,0.00005323196,0.0002653922,0.000027806956,0.00042506718,0.0002633478],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.017728224,0.0037735356,0.18908057,0.0004843969,0.0015994722,0.017075669,0.041094705,0.18533559,0.15755865,0.0010107458,0.2547589,0.13049954],"study_design_scores_gemma":[0.0020346248,0.0018961697,0.9536995,0.00027702653,0.000029138098,0.000018082956,0.0012487852,0.0053930017,0.0060933344,0.005782056,0.02305757,0.00047068807],"about_ca_topic_score_codex":0.6489834,"about_ca_topic_score_gemma":0.5587982,"teacher_disagreement_score":0.76461893,"about_ca_system_score_codex":0.000018784061,"about_ca_system_score_gemma":0.0010224234,"threshold_uncertainty_score":0.9999249},"labels":[],"label_agreement":null},{"id":"W1564429322","doi":"","title":"Structure of the uppermost mantle beneath North America : Regional surface wave tomography and thermo-chemical interpretation","year":2002,"lang":"en","type":"dissertation","venue":"Data Archiving and Networked Services (DANS)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismogram; Seismic tomography; Earth structure; Rayleigh wave; Tomography; Seismology; Inversion (geology); Phase velocity; Surface wave; Geophysics; Geodesy; Mantle (geology); Physics; Tectonics; Optics","score_opus":0.00846380788608917,"score_gpt":0.19130796817885148,"score_spread":0.18284416029276232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1564429322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929463,0.0011581202,0.000007861906,0.00002437643,0.00033762195,0.00018189193,0.004853585,0.00001691875,0.0004733213],"genre_scores_gemma":[0.971107,0.00082925666,0.00023854886,0.000059383914,0.00015672136,5.372726e-7,0.027514314,0.000011579189,0.00008263887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986163,0.00012500597,0.0002796964,0.00048464493,0.00025414815,0.000240201],"domain_scores_gemma":[0.9988964,0.0001552993,0.00029996486,0.0005393578,0.000027284768,0.00008165428],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006234315,0.00027247085,0.00033933966,0.000037814418,0.00020017677,0.00010031376,0.0006565797,0.000101601974,0.000102992795],"category_scores_gemma":[0.0000033411916,0.00018194594,0.000049893453,0.00017102079,0.0001112369,0.0001660312,0.00010263844,0.00021484519,0.000001699274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022195699,0.00017262944,0.4443914,0.0066890847,0.001784316,0.00004357221,0.087991714,0.012262266,0.05660964,0.00010697476,0.0029408007,0.38478804],"study_design_scores_gemma":[0.00023013717,0.000066760906,0.8552632,0.0007250717,0.00028137938,0.000016645927,0.0011454067,0.13907315,0.00033876448,0.0005994735,0.001756272,0.0005037667],"about_ca_topic_score_codex":0.0026195664,"about_ca_topic_score_gemma":0.0116028935,"teacher_disagreement_score":0.41087177,"about_ca_system_score_codex":0.0000011181663,"about_ca_system_score_gemma":0.000017498078,"threshold_uncertainty_score":0.741954},"labels":[],"label_agreement":null},{"id":"W1568562874","doi":"10.1029/gm046p0065","title":"Seismic Wave Scattering and the Earth's Structure in the Lower Mantle","year":2011,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geophysics; Mantle (geology); Earth (classical element); Scattering; Core–mantle boundary; Structure of the Earth; Seismology; Physics; Astronomy; Optics","score_opus":0.011444055923410223,"score_gpt":0.1730004333864021,"score_spread":0.1615563774629919,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1568562874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7507759,0.001697878,0.000021232701,0.00095876167,0.0018741228,0.001399945,0.0009615093,0.00007214717,0.2422385],"genre_scores_gemma":[0.9914256,0.0002741149,0.00003562644,0.0005436383,0.0005331247,0.0000038496346,0.00009340214,0.00001452411,0.0070761642],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9986476,0.000078779616,0.00026091514,0.0003916515,0.00027610638,0.00034495065],"domain_scores_gemma":[0.9991323,0.00017323824,0.00013561118,0.00047057527,0.000021103788,0.00006720272],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019902995,0.00035162995,0.0004526972,0.00007935619,0.00017750631,0.0001572897,0.0003911426,0.00018373602,0.0009834279],"category_scores_gemma":[0.000003723411,0.0001814602,0.00017889454,0.000064698,0.00052133464,0.000099393714,0.00005619714,0.00044972537,0.00017816704],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038333777,0.00032538548,0.0063461163,0.0010595513,0.0021136312,0.0010227608,0.017193457,0.0011583243,0.00079364475,0.61501735,0.009959645,0.34117678],"study_design_scores_gemma":[0.0012433585,0.00023835464,0.18661389,0.00019078446,0.00025801468,0.000040975057,0.000050544033,0.00071377587,0.000045377103,0.6838161,0.12581107,0.0009777717],"about_ca_topic_score_codex":0.001923326,"about_ca_topic_score_gemma":0.00042983296,"teacher_disagreement_score":0.340199,"about_ca_system_score_codex":7.841163e-7,"about_ca_system_score_gemma":0.000014945232,"threshold_uncertainty_score":0.9999298},"labels":[],"label_agreement":null},{"id":"W1570439565","doi":"","title":"Structure and Emplacement of High-level Magmatic Systems","year":2009,"lang":"en","type":"article","venue":"Geoscience Canada","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Geology; Geochemistry","score_opus":0.007326141873892201,"score_gpt":0.17228814625079752,"score_spread":0.16496200437690534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1570439565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977921,0.00017711581,0.00008016093,0.00016544874,0.00074861967,0.000111403766,0.00068629987,0.0000052867385,0.0002335495],"genre_scores_gemma":[0.99925184,0.0000072379053,0.00030812382,0.00015523167,0.00003983735,2.0350956e-7,0.000023647592,7.6721483e-7,0.00021311764],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991213,0.000023510212,0.00015845857,0.0001658494,0.00031546075,0.000215399],"domain_scores_gemma":[0.99962103,0.000026671309,0.00007859561,0.00013774727,0.000030344527,0.00010558672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011565841,0.00008287021,0.00015845166,0.000024345312,0.00009588069,0.00004901314,0.00016619955,0.000020837304,0.00022423296],"category_scores_gemma":[0.000014395624,0.00006248949,0.000007259296,0.00011863519,0.00004987442,0.000095392905,0.000006969812,0.00003006502,0.0000017066749],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031053743,0.00016411005,0.30102134,0.002339715,0.0002194337,0.0004368528,0.0031831323,0.13236465,0.107837625,0.06780737,0.079853475,0.30446178],"study_design_scores_gemma":[0.00018042621,0.00012795698,0.99081147,0.000032436925,0.000012830381,0.000014328849,0.000105257095,0.002101956,0.0013145651,0.0015630149,0.0035431257,0.00019266225],"about_ca_topic_score_codex":0.86215883,"about_ca_topic_score_gemma":0.6104867,"teacher_disagreement_score":0.6897901,"about_ca_system_score_codex":0.000004822535,"about_ca_system_score_gemma":0.00024136245,"threshold_uncertainty_score":0.39662093},"labels":[],"label_agreement":null},{"id":"W1574263627","doi":"10.1029/gm046p0041","title":"The Excitation of Core Modes by Earthquakes","year":2011,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Excitation; Core (optical fiber); Geophysics; Physics; Optics; Quantum mechanics","score_opus":0.02064258821819732,"score_gpt":0.19627288080121358,"score_spread":0.17563029258301627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1574263627","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16495074,0.0036761274,0.00007283815,0.00010052068,0.0012776721,0.0008316376,0.0026563455,0.00012381046,0.8263103],"genre_scores_gemma":[0.94341,0.00094277255,0.000094635776,0.000041962194,0.00031690794,0.0000044261737,0.000539413,0.000019752333,0.054630168],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9986745,0.000026292617,0.00035840675,0.00031184882,0.00033995873,0.00028900497],"domain_scores_gemma":[0.99888074,0.00021622727,0.0003148645,0.00039188433,0.00009151167,0.0001047577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012574933,0.0002964971,0.00041728732,0.00005722204,0.00019754053,0.0000574346,0.0003701352,0.00018633199,0.0004889228],"category_scores_gemma":[0.000007607756,0.00019786021,0.00025828445,0.000051992844,0.0003814799,0.00010234067,0.000021918388,0.00018463963,0.00035587282],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050356355,0.000103841085,0.0011430285,0.00025400857,0.0008601351,0.000014178969,0.00068448763,0.000091660455,0.0032963017,0.7659881,0.03212554,0.19493513],"study_design_scores_gemma":[0.00021108365,0.00041043197,0.022506274,0.00009221606,0.00015590782,9.2647525e-7,0.000019938972,0.00010248933,0.00037397395,0.82041276,0.15516615,0.0005478498],"about_ca_topic_score_codex":0.0011556299,"about_ca_topic_score_gemma":0.00017057407,"teacher_disagreement_score":0.7784592,"about_ca_system_score_codex":8.6913366e-7,"about_ca_system_score_gemma":0.000025070247,"threshold_uncertainty_score":0.8068505},"labels":[],"label_agreement":null},{"id":"W1575742052","doi":"10.1029/gm010p0349","title":"Review of Geophysical Evidence on Crust and Upper-Mantle Structure On the Eastern Seaboard Of Canada","year":2011,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Crust; Continental crust; Mantle (geology); Oceanic crust; Continental margin; Structural basin; Geophysics; Continental shelf; Oceanic basin; Seismology; Paleontology; Subduction; Tectonics; Oceanography","score_opus":0.021581660540427126,"score_gpt":0.19860985223658997,"score_spread":0.17702819169616285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1575742052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.69930327,0.037143633,0.0000058916726,0.0021094976,0.0029230097,0.0036135728,0.009914806,0.00008565685,0.24490064],"genre_scores_gemma":[0.9804643,0.009607266,0.00003588603,0.0016084916,0.00054299325,0.0000039394417,0.00013277997,0.00003271605,0.0075716325],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979337,0.00008577702,0.00048534843,0.0005002982,0.0006520203,0.0003428704],"domain_scores_gemma":[0.99803984,0.00047299918,0.00047271588,0.00071599876,0.00012655983,0.00017188764],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014257821,0.0004641784,0.0009553704,0.00006516569,0.00010726999,0.000023035975,0.000523786,0.0001580452,0.0012640662],"category_scores_gemma":[0.000039006132,0.00028946085,0.0002565848,0.00008960947,0.00034266824,0.00007536017,0.000060823128,0.00039148287,0.000049763086],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0032908127,0.00057456695,0.009596466,0.051074088,0.0038573376,0.00022807883,0.0014186251,0.00014707228,0.0021879335,0.5797596,0.15676118,0.19110426],"study_design_scores_gemma":[0.0012218835,0.0072013102,0.24944001,0.11287798,0.0024514352,0.000018690973,0.00006105297,0.00028621178,0.0061929924,0.20410573,0.41114235,0.0050003347],"about_ca_topic_score_codex":0.12365375,"about_ca_topic_score_gemma":0.016451206,"teacher_disagreement_score":0.37565383,"about_ca_system_score_codex":0.0000038943826,"about_ca_system_score_gemma":0.00017355174,"threshold_uncertainty_score":0.9999558},"labels":[],"label_agreement":null},{"id":"W1586005529","doi":"10.1002/2015gc005845","title":"Lithospheric architecture beneath <scp>H</scp>udson <scp>B</scp>ay","year":2015,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"National Science Foundation","keywords":"Craton; Lithosphere; Geology; Archean; Precambrian; Seismology; Asthenosphere; Classification of discontinuities; Proterozoic; Shear (geology); Geophysics; Petrology; Paleontology; Tectonics","score_opus":0.011396898534465046,"score_gpt":0.19626094458758164,"score_spread":0.1848640460531166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1586005529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9413177,0.0019243353,0.00022818129,0.00004430428,0.0021690263,0.0005216308,0.0011728974,0.00033401928,0.0522879],"genre_scores_gemma":[0.9813841,0.00004932935,0.00052004337,0.00013172686,0.0035419182,0.000030420953,0.0016244729,0.000048672704,0.012669327],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9952631,0.00019123039,0.0007586604,0.0011438188,0.0011564785,0.0014867099],"domain_scores_gemma":[0.9962337,0.0006719745,0.0005578012,0.0012344079,0.0003569448,0.00094516494],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00068698276,0.00082884275,0.0009934127,0.000056255478,0.0003482224,0.0005085236,0.0010714541,0.00044864797,0.00013406202],"category_scores_gemma":[0.00044006528,0.00074494776,0.00030810368,0.0006572116,0.0001623986,0.00034063795,0.00014173487,0.0005309878,0.0017185608],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001833833,0.0018063432,0.14104828,0.008349366,0.0029266013,0.0015422571,0.03175897,0.105703846,0.21090782,0.0018185851,0.45291126,0.041043293],"study_design_scores_gemma":[0.002823551,0.00068443024,0.020414844,0.00049584545,0.0004106763,0.00025180785,0.0055555394,0.006123346,0.07373152,0.018272312,0.870255,0.0009811036],"about_ca_topic_score_codex":0.0048486837,"about_ca_topic_score_gemma":0.00017960796,"teacher_disagreement_score":0.41734377,"about_ca_system_score_codex":0.000026797257,"about_ca_system_score_gemma":0.0003387329,"threshold_uncertainty_score":0.99950016},"labels":[],"label_agreement":null},{"id":"W1594118858","doi":"10.1029/2011gc003818","title":"Upper mantle <i>P</i> velocity structure beneath the Midwestern United States derived from triplicated waveforms","year":2012,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"California Institute of Technology; National Science Foundation","keywords":"Geology; Lithosphere; Seismology; Asthenosphere; Discontinuity (linguistics); Low-velocity zone; Craton; Mantle (geology); Subduction; Tectonics; Seismic velocity; Shear velocity; Geophysics; Geodesy; Meteorology","score_opus":0.00807956193560096,"score_gpt":0.19011890068473866,"score_spread":0.1820393387491377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1594118858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913909,0.00044959952,0.000058050933,0.0001710061,0.00131193,0.00038400522,0.0054722056,0.0001238602,0.0006384761],"genre_scores_gemma":[0.98587847,0.00004700683,0.00008510408,0.00026415795,0.0020057666,0.000010641514,0.0111844465,0.000019792651,0.00050462],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9975151,0.00011865165,0.0004737598,0.00047239536,0.0004974451,0.0009226578],"domain_scores_gemma":[0.99818945,0.00019676518,0.00032875067,0.00084308133,0.00013962176,0.00030231164],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002506787,0.00046597433,0.00048324006,0.00003264276,0.0004419895,0.00023550239,0.00068819104,0.00023133331,0.0011239275],"category_scores_gemma":[0.000015189154,0.00027463786,0.00014927486,0.00037664312,0.00013034382,0.00033414442,0.00008489633,0.00030598577,0.00042761414],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007091015,0.00060720975,0.3266269,0.0013434283,0.002168299,0.000057279474,0.012557001,0.011466807,0.60906535,0.00029700156,0.013740942,0.021360707],"study_design_scores_gemma":[0.0023797837,0.00013503114,0.41802776,0.00024482264,0.0005343752,0.000060464066,0.0026874007,0.017266972,0.4083421,0.009876189,0.13767585,0.002769258],"about_ca_topic_score_codex":0.017357523,"about_ca_topic_score_gemma":0.00025478235,"teacher_disagreement_score":0.20072322,"about_ca_system_score_codex":0.000012961701,"about_ca_system_score_gemma":0.000050798084,"threshold_uncertainty_score":0.99997056},"labels":[],"label_agreement":null},{"id":"W1595312842","doi":"10.1002/pssb.201350149","title":"Thermodynamic modelling of liquids: CALPHAD approaches and contributions from statistical physics","year":2013,"lang":"en","type":"article","venue":"physica status solidi (b)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"CALPHAD; Formalism (music); Statistical physics; Thermodynamics; Scale (ratio); Monte Carlo method; Chemistry; Physics; Phase diagram; Mathematics","score_opus":0.02945810155024804,"score_gpt":0.2157831394512742,"score_spread":0.18632503790102617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1595312842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94473785,0.00022903601,0.048098836,0.000068530775,0.00011577648,0.00028328097,0.005292339,0.000034198434,0.001140155],"genre_scores_gemma":[0.9967094,0.00007827814,0.0022529382,0.000023742135,0.00020109703,0.0000080703685,0.00070164306,0.000007635303,0.000017165663],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988297,0.00007799347,0.00023003323,0.0002772001,0.00019157183,0.0003934783],"domain_scores_gemma":[0.9991881,0.0002599143,0.000107475855,0.00020846236,0.00007235826,0.00016363988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060253125,0.00017159957,0.00034734586,0.000016636905,0.00011635249,0.00007488294,0.0001145415,0.000049946975,0.00032043448],"category_scores_gemma":[0.000011782845,0.00014061798,0.00004583255,0.000078839104,0.00017713301,0.00024522428,0.000025038744,0.00009677991,0.00011051977],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073846505,0.0019671556,0.027131306,0.0007944017,0.0021573654,0.000026894882,0.013771903,0.2805598,0.1544359,0.358062,0.004404208,0.1559506],"study_design_scores_gemma":[0.00045964657,0.0001285707,0.032276046,0.000025202133,0.00009639324,4.1732656e-7,0.00014845694,0.8156397,0.0035839677,0.14702052,0.00028591225,0.00033520782],"about_ca_topic_score_codex":0.017538069,"about_ca_topic_score_gemma":0.00007205467,"teacher_disagreement_score":0.53507984,"about_ca_system_score_codex":0.000003482544,"about_ca_system_score_gemma":0.000048099268,"threshold_uncertainty_score":0.98900425},"labels":[],"label_agreement":null},{"id":"W1597815664","doi":"","title":"Combined U-Pb columbite and laser 40Ar/39Ar mica ages from rare-element pegmatites, Superior Province of Northwestern Ontario","year":2000,"lang":"en","type":"book-chapter","venue":"Open Research Online (The Open University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Columbite; Pegmatite; Mica; Geochemistry; Geology; Materials science; Metallurgy; Paleontology; Ceramic","score_opus":0.04437416857069309,"score_gpt":0.2574163527982827,"score_spread":0.21304218422758958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1597815664","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5399291,0.00012978571,6.436741e-7,0.00068519154,0.0001468221,0.00445914,0.010595748,0.000015845812,0.44403777],"genre_scores_gemma":[0.042599652,0.0012134211,0.00081078894,0.00009794939,0.00011949144,0.000002133221,0.005843012,0.000028985103,0.94928455],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99748373,0.00028953387,0.0003714944,0.0007234605,0.00067306514,0.00045873437],"domain_scores_gemma":[0.9981751,0.00033284258,0.00022848349,0.00078931364,0.00022095554,0.00025332207],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005873593,0.00032575746,0.0007430564,0.00019212873,0.0005618674,0.000884705,0.0034413503,0.00018877818,0.023653558],"category_scores_gemma":[0.000008378869,0.00027606418,0.000082747516,0.00012557258,0.00046247107,0.0006628513,0.0015624273,0.0005525123,0.00020474978],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.05494407,0.0057854312,0.23013891,0.0031111308,0.016205454,0.019757925,0.027084501,0.0021014975,0.007994692,0.08237077,0.16699806,0.38350755],"study_design_scores_gemma":[0.0014860431,0.0006265819,0.027076561,0.0003640248,0.00011956426,0.0000020068885,0.00018927247,0.000028004024,0.000108364366,0.0019275269,0.9676325,0.00043956467],"about_ca_topic_score_codex":0.64653665,"about_ca_topic_score_gemma":0.8842299,"teacher_disagreement_score":0.80063444,"about_ca_system_score_codex":0.000042876996,"about_ca_system_score_gemma":0.0010268892,"threshold_uncertainty_score":0.9999691},"labels":[],"label_agreement":null},{"id":"W1597830786","doi":"10.1002/9781118670101.ch12","title":"On the Radial Profile of Mantle Viscosity","year":2013,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Viscosity; Geophysics; Physics; Thermodynamics","score_opus":0.008838554758537133,"score_gpt":0.17908987812137137,"score_spread":0.17025132336283424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1597830786","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92012495,0.000006877399,0.000012293,0.00031164195,0.00019298511,0.00015484376,0.00003554268,0.000009153344,0.07915169],"genre_scores_gemma":[0.99823606,0.0000021150775,0.00009247246,0.0001633477,0.000060269696,0.0000012744619,0.000011912715,7.639675e-7,0.0014318015],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9996532,0.000029208857,0.00006910668,0.00006593884,0.00009049983,0.00009205188],"domain_scores_gemma":[0.9997389,0.00008166076,0.000026357551,0.00011381707,0.000013646262,0.00002562034],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008460007,0.000041011812,0.000066526336,0.000008463257,0.000047396894,0.000026180802,0.00011127712,0.000016050244,0.04857917],"category_scores_gemma":[0.000008767691,0.000019849786,0.000019498395,0.00003243977,0.000029620725,0.00005509206,0.000005584796,0.000022901291,0.0026496842],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016833108,0.00023381559,0.05160002,0.00011970317,0.00015994837,0.000006757476,0.0009454971,0.0012882919,0.064875714,0.16840942,0.66412324,0.048069257],"study_design_scores_gemma":[0.00026913208,0.0003326769,0.8812375,0.000015070836,0.000014400933,0.0000011855975,0.00007761353,0.0035024947,0.07632301,0.027074426,0.010928777,0.0002236991],"about_ca_topic_score_codex":0.005330209,"about_ca_topic_score_gemma":0.00012460434,"teacher_disagreement_score":0.82963747,"about_ca_system_score_codex":2.1741307e-7,"about_ca_system_score_gemma":0.000007743431,"threshold_uncertainty_score":0.99812686},"labels":[],"label_agreement":null},{"id":"W1599440120","doi":"10.1002/jgrb.50110","title":"Seismic velocities, anisotropy, and shear‐wave splitting of antigorite serpentinites and tectonic implications for subduction zones","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Geology; Subduction; Seismic anisotropy; Forearc; Mantle (geology); Anisotropy; Shear wave splitting; Shear (geology); Mantle wedge; Tectonics; Peridotite; Mineralogy; Seismology; Geochemistry; Petrology","score_opus":0.041683451132613354,"score_gpt":0.3059987396211144,"score_spread":0.26431528848850105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1599440120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979938,0.00033949513,0.0003420237,0.000754291,0.000112078495,0.00030092342,0.000081337595,0.000005732927,0.000070268004],"genre_scores_gemma":[0.9964738,0.00046398188,0.002432543,0.000015421454,0.0004488388,0.0000031905145,0.000013126992,0.000005984656,0.00014314019],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985842,0.00013863227,0.0003888932,0.00017953693,0.00032722473,0.00038149508],"domain_scores_gemma":[0.99802345,0.0008085614,0.00021433082,0.00013273014,0.00062383164,0.00019709038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081182376,0.000111219066,0.00035355685,0.00015292878,0.00026272744,0.00017368473,0.00012705284,0.00005546594,0.00010154083],"category_scores_gemma":[0.00027059385,0.00008633793,0.0000730062,0.00020412209,0.00026991527,0.0004684125,0.000040089973,0.00022336477,0.000013277421],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010078477,0.0006273362,0.123976946,0.002010209,0.0007957218,0.00002014806,0.0031908308,0.0018870207,0.5552071,0.013136767,0.0031879437,0.29495218],"study_design_scores_gemma":[0.00050059427,0.0010134707,0.9421384,0.00008878921,0.000028948287,0.000033465614,0.00029398553,0.0127439415,0.0044209035,0.03761517,0.0009859775,0.00013637419],"about_ca_topic_score_codex":0.0016483288,"about_ca_topic_score_gemma":0.000028357945,"teacher_disagreement_score":0.8181614,"about_ca_system_score_codex":0.0000026749406,"about_ca_system_score_gemma":0.00010884922,"threshold_uncertainty_score":0.35207587},"labels":[],"label_agreement":null},{"id":"W1601447128","doi":"10.1029/2010gl043219","title":"Deepest mantle viscosity: Constraints from Earth rotation anomalies","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Post-glacial rebound; Geophysics; Earth's rotation; Polar; Inner core; Viscosity; Geodesy; Glacial period; Physics; Paleontology; Thermodynamics","score_opus":0.02250874900743095,"score_gpt":0.27123000836453703,"score_spread":0.2487212593571061,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1601447128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99419314,0.000011234998,0.00007977322,0.0016075668,0.0006403471,0.00024177776,0.00028724762,0.000050089016,0.0028888418],"genre_scores_gemma":[0.99731827,0.000005867055,0.0008013045,0.00038220338,0.0010332706,0.0000059429526,0.00029999248,0.0000074114755,0.00014571515],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.997731,0.00021828314,0.00018657898,0.00042506435,0.0007738871,0.0006651914],"domain_scores_gemma":[0.99870884,0.00054911844,0.000047417107,0.00034952286,0.00009251159,0.0002525695],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004301748,0.00015777981,0.00022048234,0.00009312451,0.00033835933,0.0003216386,0.0003868392,0.00007794932,0.0036171626],"category_scores_gemma":[0.00012772897,0.0001334758,0.0000706263,0.00023225174,0.0006516774,0.00031207473,0.000051485105,0.0005368035,0.003946795],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007389346,0.000077644,0.023002187,0.000022508904,0.000059498776,0.00011030258,0.0003475607,0.000095360185,0.94662106,0.0027170957,0.003350282,0.023522612],"study_design_scores_gemma":[0.00048495547,0.00013916139,0.9497859,0.0000228887,0.000016574533,0.000002939021,0.00009600232,0.0010621626,0.026934138,0.008849959,0.012240397,0.00036496195],"about_ca_topic_score_codex":0.009906868,"about_ca_topic_score_gemma":0.0017650785,"teacher_disagreement_score":0.9267837,"about_ca_system_score_codex":0.0000022968948,"about_ca_system_score_gemma":0.00005906981,"threshold_uncertainty_score":0.99729365},"labels":[],"label_agreement":null},{"id":"W1602001262","doi":"10.4401/ag-4589","title":"On amplitudes of P near the shadow zone","year":2010,"lang":"en","type":"article","venue":"Annals of Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Amplitude; Geology; Seismology; Geodesy; Mantle (geology); Variation (astronomy); Physics; Geophysics; Optics; Astrophysics","score_opus":0.023315094485349335,"score_gpt":0.25216113763841214,"score_spread":0.2288460431530628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1602001262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953805,0.000042753232,0.000021417498,0.00035588356,0.00040348773,0.00009979821,0.00020058405,0.000010696151,0.0034848363],"genre_scores_gemma":[0.99923766,0.000026208583,0.00014593637,0.00028531277,0.00016910773,7.2995675e-7,0.00003095439,0.0000035610037,0.00010054952],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99918693,0.000034591227,0.00020166667,0.00013589243,0.0002483642,0.00019255636],"domain_scores_gemma":[0.99909574,0.00021281,0.00016163017,0.00037085073,0.00010944192,0.00004950589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002440527,0.00010601326,0.0002169291,0.000016945265,0.00011553394,0.000048836755,0.00031904082,0.000046395893,0.000572365],"category_scores_gemma":[0.00003298621,0.0000668835,0.000091358845,0.00012426639,0.00026040574,0.000091451795,0.000017478704,0.000114624556,0.00016549371],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009170337,0.0010868965,0.037486367,0.0005622473,0.0007089994,0.000018872504,0.003995787,0.0071674343,0.23165831,0.47169828,0.029536963,0.2151628],"study_design_scores_gemma":[0.00032692365,0.0007822847,0.73609227,0.00005370669,0.000046327594,0.0000016109258,0.000056463712,0.00052250497,0.08589962,0.14785092,0.027990717,0.00037666876],"about_ca_topic_score_codex":0.0036876372,"about_ca_topic_score_gemma":0.00033241158,"teacher_disagreement_score":0.6986059,"about_ca_system_score_codex":1.0856977e-7,"about_ca_system_score_gemma":0.00004068935,"threshold_uncertainty_score":0.62669957},"labels":[],"label_agreement":null},{"id":"W1604785025","doi":"10.1029/2012gc004162","title":"The effective elastic thickness of the continental lithosphere: Comparison between rheological and inverse approaches","year":2012,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Adolph C. and Mary Sprague Miller Institute for Basic Research in Science, University of California Berkeley; Alexander von Humboldt-Stiftung","keywords":"Lithosphere; Geology; Craton; Inverse; Continental crust; Upper crust; Distribution (mathematics); Geophysics; Crust; Geometry; Seismology; Mathematics; Mathematical analysis","score_opus":0.017337293935321473,"score_gpt":0.20603909673645662,"score_spread":0.18870180280113516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1604785025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958765,0.00086730724,0.000042083095,0.00006654469,0.00066834176,0.00041514222,0.0002123833,0.000023927138,0.0018277667],"genre_scores_gemma":[0.99897724,0.000009131302,0.000027892002,0.0000104112605,0.0006896034,0.0000129515,0.00007304228,0.0000054985026,0.00019420167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983767,0.00023046636,0.00035863073,0.00024776885,0.00032344842,0.00046293833],"domain_scores_gemma":[0.9983633,0.0007374764,0.00032967512,0.00037860213,0.00005500161,0.0001359452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005975446,0.00023412137,0.00042615543,0.000005823434,0.0003905385,0.00007944399,0.0003845198,0.00018673722,0.000043233027],"category_scores_gemma":[0.00007692016,0.00012815141,0.000105702165,0.00014849847,0.0004027845,0.00012276927,0.0001086961,0.00029532384,0.000036583795],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053047406,0.00006132176,0.9880337,0.00034833813,0.00016327725,6.3770875e-7,0.00072184735,0.00017334752,0.0044628875,0.0006833027,0.00038410796,0.004914188],"study_design_scores_gemma":[0.00045168778,0.00006976667,0.97364676,0.0000946594,0.00016550372,0.00001221125,0.0009783459,0.0017891995,0.0183258,0.0011865635,0.002933783,0.00034573584],"about_ca_topic_score_codex":0.0011177029,"about_ca_topic_score_gemma":0.00007390593,"teacher_disagreement_score":0.014386954,"about_ca_system_score_codex":0.000004551655,"about_ca_system_score_gemma":0.00002755081,"threshold_uncertainty_score":0.5225863},"labels":[],"label_agreement":null},{"id":"W1607153631","doi":"10.1002/grl.50257","title":"Broadband array observations of the 300 km seismic discontinuity","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Center for High Performance Computing","keywords":"Geology; Seismic array; Discontinuity (linguistics); Classification of discontinuities; Mantle (geology); Seismology; Subduction; Eclogite; Basalt; Seismic wave; Stishovite; Geophysics; Transition zone; Crust; Petrology; Tectonics; Quartz; Paleontology","score_opus":0.03768964053772479,"score_gpt":0.2654500818033348,"score_spread":0.22776044126561001,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607153631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892519,0.000019243382,0.00003950854,0.008772458,0.00028464128,0.00042633226,0.00013162429,0.00001625857,0.001058027],"genre_scores_gemma":[0.9982143,0.0000057416637,0.0001172011,0.0005321429,0.0003304611,0.000012734042,0.000037183054,0.0000049504247,0.0007452944],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978672,0.00033296482,0.0002217554,0.00026754633,0.0007559549,0.0005545505],"domain_scores_gemma":[0.9987735,0.00041560896,0.00006870655,0.0004712278,0.00013571106,0.00013522658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037316303,0.000121498844,0.00020995954,0.00004583453,0.00029362072,0.00014824654,0.00063454494,0.00004291849,0.00088778103],"category_scores_gemma":[0.00013895673,0.000074380325,0.00011250498,0.00042553357,0.00046071253,0.00031460158,0.00006412508,0.0002967222,0.00076307025],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026111391,0.000085255204,0.03560896,0.00006408453,0.000057772286,0.000002673887,0.00051813666,0.00091808283,0.9145123,0.0007624272,0.042942613,0.004501586],"study_design_scores_gemma":[0.0001522453,0.00004424847,0.97801787,0.00002494849,0.000007554744,3.8362205e-7,0.000044768913,0.0006349606,0.009285782,0.0042147916,0.0074572014,0.0001152629],"about_ca_topic_score_codex":0.023967689,"about_ca_topic_score_gemma":0.00032010497,"teacher_disagreement_score":0.9424089,"about_ca_system_score_codex":0.0000048639686,"about_ca_system_score_gemma":0.000057798272,"threshold_uncertainty_score":0.9825318},"labels":[],"label_agreement":null},{"id":"W1608015442","doi":"10.1038/35074000","title":"Deep-mantle high-viscosity flow and thermochemical structure inferred from seismic and geodynamic data","year":2001,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":354,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Western University","funders":"","keywords":"Geology; Mantle (geology); Geophysics; Mantle convection; Seismic tomography; Convection; Mantle wedge; Geodynamics; Rheology; Viscosity; Upwelling; Thermal; Core–mantle boundary; Seismology; Lithosphere; Mechanics; Tectonics; Thermodynamics; Physics","score_opus":0.006128263066582614,"score_gpt":0.20579383599561216,"score_spread":0.19966557292902953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1608015442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949109,0.0021052342,0.00007023497,0.0003270758,0.00041276618,0.00009621472,0.0018727252,0.000028935216,0.00017590073],"genre_scores_gemma":[0.99480546,0.00022201061,0.00090099935,0.00037883414,0.00032513906,1.8098191e-7,0.0033264968,0.0000045551105,0.000036334717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991271,0.00003820684,0.000102530525,0.00038109536,0.00015462837,0.00019647126],"domain_scores_gemma":[0.9994058,0.00006822643,0.000042072952,0.00036950412,0.000017184206,0.000097181546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000067252004,0.00014670448,0.00019542583,0.000020923664,0.00011018462,0.0001105801,0.0002855119,0.00051519397,0.0008488308],"category_scores_gemma":[0.000023111366,0.00010966776,0.000011837947,0.0000656224,0.00006529398,0.00022672211,0.00009078899,0.00054178835,0.000015483363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011538144,0.00013977152,0.51170963,0.0002690716,0.00079582207,0.00053563615,0.0017175224,0.0054361564,0.1548826,0.0005847871,0.025391065,0.29738414],"study_design_scores_gemma":[0.00064450403,0.000036956142,0.8663249,0.00002472424,0.00008289616,0.00003393861,0.00002696698,0.10723436,0.00067988853,0.013249273,0.011293373,0.000368215],"about_ca_topic_score_codex":0.0020051405,"about_ca_topic_score_gemma":0.0018613457,"teacher_disagreement_score":0.3546153,"about_ca_system_score_codex":0.0000013479004,"about_ca_system_score_gemma":0.000015742646,"threshold_uncertainty_score":0.9294102},"labels":[],"label_agreement":null},{"id":"W1611586638","doi":"10.1029/2008tc002292","title":"Deep subduction and rapid exhumation: Role of crustal strength and strain weakening in continental subduction and ultrahigh‐pressure rock exhumation","year":2008,"lang":"en","type":"article","venue":"Tectonics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Subduction; Geology; Crust; Buoyancy; Plume; Eclogitization; Continental crust; Petrology; Seismology; Geophysics; Tectonics; Oceanic crust; Mechanics","score_opus":0.007052366371471119,"score_gpt":0.1814140847555928,"score_spread":0.1743617183841217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1611586638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99683106,0.0022911334,0.000073365445,0.00003463964,0.00012939629,0.00016175027,0.000071915645,0.00002490496,0.00038181114],"genre_scores_gemma":[0.9982796,0.001185456,0.000317141,0.0000042476518,0.00007532051,0.0000014839718,0.000121765996,0.0000040508476,0.000010965022],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992004,0.000057607376,0.00023919385,0.00020920936,0.00014426722,0.00014929204],"domain_scores_gemma":[0.9996648,0.000043405045,0.00012451256,0.00008363383,0.00003216368,0.000051494306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017064053,0.00011811737,0.00019703664,0.00008123588,0.00013697651,0.00003981445,0.000040365085,0.000077898636,0.00034520653],"category_scores_gemma":[0.00002035618,0.000112661146,0.00001524952,0.0000899233,0.00007143272,0.0003681399,0.000011010428,0.00008362789,0.0000018943523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090234826,0.00031224452,0.3401495,0.0010536305,0.0002615203,0.000033999513,0.028563242,0.023139253,0.27825785,0.0043080947,0.00015167092,0.32286665],"study_design_scores_gemma":[0.0010715517,0.00023728872,0.94762015,0.00004897822,0.00004679558,0.00009104264,0.0011227134,0.03834514,0.009743101,0.0005609722,0.0008384658,0.0002737887],"about_ca_topic_score_codex":0.0009137811,"about_ca_topic_score_gemma":0.000519815,"teacher_disagreement_score":0.6074707,"about_ca_system_score_codex":0.0000017632894,"about_ca_system_score_gemma":0.00001519491,"threshold_uncertainty_score":0.4594188},"labels":[],"label_agreement":null},{"id":"W1632335309","doi":"10.21236/ada485986","title":"Waveform Modeling of the Crust and Upper Mantle Using S, Sp, SsPmP, and Shear-Coupled PL Waves","year":2008,"lang":"en","type":"report","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Crust; Seismology; Shear (geology); Mantle (geology); Geophysics; Waveform; Shear zone; Petrology; Computer science; Telecommunications","score_opus":0.03713534009174734,"score_gpt":0.23724976523832805,"score_spread":0.2001144251465807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1632335309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96759856,0.0022103395,0.00006003847,0.000036399986,0.0009376374,0.00028982075,0.00024989597,0.000017571414,0.02859975],"genre_scores_gemma":[0.99093485,0.0052583716,0.0007868514,0.000033012722,0.0003514062,5.2776164e-7,0.000072043695,0.000011634336,0.0025513256],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985407,0.000028467708,0.0003796972,0.00031303221,0.0004711518,0.00026697083],"domain_scores_gemma":[0.99932736,0.000040324645,0.00017975506,0.00026721062,0.00010266473,0.00008265646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032361195,0.00023669213,0.00048890425,0.0000589484,0.0002237704,0.000073445495,0.00014870857,0.00019623873,0.0006708098],"category_scores_gemma":[0.000025392384,0.00013607909,0.00007704513,0.00007055878,0.00013170695,0.00012891353,0.000066945315,0.00014205795,0.0000055683045],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00108525,0.00058277015,0.5207509,0.020080678,0.0048415633,0.0005669569,0.011904403,0.2820757,0.02668586,0.002133407,0.027398206,0.101894334],"study_design_scores_gemma":[0.0006744795,0.0001387668,0.0863729,0.0007338606,0.0004638712,0.00058437994,0.00035284244,0.88455796,0.00097062334,0.0014470327,0.022416357,0.001286925],"about_ca_topic_score_codex":0.034059763,"about_ca_topic_score_gemma":0.00077384606,"teacher_disagreement_score":0.60248226,"about_ca_system_score_codex":0.0000041105955,"about_ca_system_score_gemma":0.00025322303,"threshold_uncertainty_score":0.97237253},"labels":[],"label_agreement":null},{"id":"W1632383993","doi":"10.1029/157gm05","title":"Surface wave tomography applied to the North American upper mantle","year":2005,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Tomography; Geology; Seismic tomography; Mantle (geology); Surface wave; Seismology; Geophysics; High resolution; Physics; Remote sensing; Optics","score_opus":0.010098297316428865,"score_gpt":0.18614146070469242,"score_spread":0.17604316338826356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1632383993","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.45977545,0.0004629361,0.0000660015,0.0013585769,0.0015289766,0.0020881551,0.0032978624,0.00034852355,0.5310735],"genre_scores_gemma":[0.9514281,0.00028928544,0.0010965915,0.0017991259,0.0028044702,0.000015776126,0.0009105655,0.00006878452,0.041587275],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99729764,0.000037966907,0.00043265644,0.0008306305,0.0006458122,0.0007552822],"domain_scores_gemma":[0.99821967,0.00014551391,0.0002646551,0.00091045734,0.000069693924,0.00038999817],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00013117596,0.0006633651,0.0008236529,0.00016904576,0.00032155716,0.00019635295,0.00069096714,0.0001408077,0.001229032],"category_scores_gemma":[0.0000030901515,0.00045859037,0.00050514686,0.00036851963,0.0003735175,0.00008568576,0.0000924016,0.00046228478,0.0042178934],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013047023,0.00040104208,0.021894941,0.0002766546,0.0031443997,0.00018634497,0.0022793678,0.014469683,0.0004979625,0.08354898,0.12612295,0.745873],"study_design_scores_gemma":[0.00018620044,0.00030830497,0.20945258,0.000031066815,0.00021626089,0.0000028937495,0.000022378883,0.000092575596,0.000056260982,0.004726379,0.7837995,0.0011055749],"about_ca_topic_score_codex":0.001640122,"about_ca_topic_score_gemma":0.003194386,"teacher_disagreement_score":0.7447674,"about_ca_system_score_codex":0.000003945528,"about_ca_system_score_gemma":0.000035800156,"threshold_uncertainty_score":0.99978656},"labels":[],"label_agreement":null},{"id":"W1633959171","doi":"10.1029/2011gl047705","title":"Sharp thermal transition in the forearc mantle wedge as a consequence of nonlinear mantle wedge flow","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Forearc; Mantle wedge; Wedge (geometry); Geology; Transition zone; Mantle (geology); Geophysics; Thermal; Nonlinear system; Seismology; Petrology; Subduction; Physics; Tectonics; Thermodynamics; Optics","score_opus":0.05410277053972061,"score_gpt":0.28188915725148095,"score_spread":0.22778638671176032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1633959171","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99196684,0.000035388228,0.000030500818,0.0017993015,0.00011888786,0.00042931255,0.00021309791,0.000014330852,0.0053923214],"genre_scores_gemma":[0.99861914,0.000018469707,0.0003868644,0.00053915347,0.00024477192,0.000014097232,0.000093760435,0.0000070846713,0.00007668641],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99754953,0.00049587927,0.00025035057,0.00031622365,0.0007442154,0.0006438111],"domain_scores_gemma":[0.999035,0.0003797743,0.00004791624,0.0003514987,0.00007492585,0.00011086506],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000983566,0.00014876241,0.00024136547,0.000111136906,0.00015020632,0.00006217315,0.0006267396,0.000063967,0.001607066],"category_scores_gemma":[0.00005923493,0.000100583275,0.00009701644,0.00038190486,0.0005207999,0.00023022987,0.000032910695,0.00036872135,0.001276328],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033625192,0.0014335952,0.0047068177,0.00071649253,0.00024493382,0.0034864077,0.03156978,0.001220561,0.9023864,0.0064011677,0.012731542,0.03173973],"study_design_scores_gemma":[0.0035769576,0.0022727132,0.8301272,0.00041259947,0.00009384267,0.00009610409,0.0021023916,0.028710194,0.0965474,0.024093535,0.010586817,0.0013802727],"about_ca_topic_score_codex":0.015318348,"about_ca_topic_score_gemma":0.00041142985,"teacher_disagreement_score":0.8254204,"about_ca_system_score_codex":0.000005081232,"about_ca_system_score_gemma":0.00007656813,"threshold_uncertainty_score":0.9995013},"labels":[],"label_agreement":null},{"id":"W1634405285","doi":"10.1029/gm046p0023","title":"Variational Calculation of Core Modes in Realistic Earth Models","year":2011,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Eigenfunction; Compressibility; Inner core; Core (optical fiber); Physics; Stratification (seeds); Classical mechanics; Geophysics; Mechanics; Geology; Eigenvalues and eigenvectors; Quantum mechanics; Optics","score_opus":0.03890541344427483,"score_gpt":0.21183974771000053,"score_spread":0.1729343342657257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1634405285","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.103417404,0.00045358657,0.0021736587,0.00003472823,0.00082947174,0.0010379683,0.0035032746,0.00010760398,0.8884423],"genre_scores_gemma":[0.988918,0.00010204238,0.0007792066,0.000026411575,0.00025658534,0.000003453703,0.0012873748,0.000015651085,0.008611247],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9984999,0.000026919286,0.00046478177,0.00038297483,0.00036958093,0.0002558567],"domain_scores_gemma":[0.99912214,0.00010116592,0.00028120674,0.0003056818,0.00008910434,0.00010068873],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00012437088,0.00029049077,0.00055304397,0.00021023044,0.000049754977,0.000022949487,0.0002187593,0.0002526701,0.000766964],"category_scores_gemma":[0.0000061293977,0.00026289132,0.00019644725,0.000086145956,0.00013571446,0.00017457156,0.000023802279,0.00019406185,0.00011442924],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018500778,0.000060569622,0.0010669801,0.00012308445,0.00012526437,0.00001630354,0.0002916398,0.030287042,0.00012419427,0.9604802,0.00019285854,0.00704686],"study_design_scores_gemma":[0.00026931858,0.00013107665,0.04740669,0.00012186409,0.00008649975,9.4407244e-7,0.0000024314606,0.032636452,0.000023002796,0.9178493,0.0010824527,0.00038994275],"about_ca_topic_score_codex":0.006611039,"about_ca_topic_score_gemma":0.0007631775,"teacher_disagreement_score":0.8855006,"about_ca_system_score_codex":0.0000021516328,"about_ca_system_score_gemma":0.000055243727,"threshold_uncertainty_score":0.99998236},"labels":[],"label_agreement":null},{"id":"W1641332181","doi":"10.1103/physrevb.74.245209","title":"Pressure-induced phase transformations in the<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mi mathvariant=\"normal\">Ba</mml:mi><mml:mn>8</mml:mn></mml:msub><mml:msub><mml:mi mathvariant=\"normal\">Si</mml:mi><mml:mn>46</mml:mn></mml:msub></mml:mrow></mml:math>clathrate","year":2006,"lang":"lv","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Synchrotron Radiation Laboratory; RIKEN; Zhejiang University; Ministry of Education of the People's Republic of China; National Natural Science Foundation of China","keywords":"Isostructural; Rietveld refinement; Materials science; Phase transition; Diffraction; Powder diffraction; Crystallography; Condensed matter physics; Physics; Phase (matter); Crystal structure; Chemistry; Optics","score_opus":0.017990369902074983,"score_gpt":0.25062829407673043,"score_spread":0.23263792417465545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1641332181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5501528,0.0079085,0.00079817243,0.0020753508,0.0038757129,0.00020776245,0.0029458946,0.00031647112,0.43171936],"genre_scores_gemma":[0.97824204,0.007988236,0.0010425843,0.0024312865,0.0035984127,0.0012460033,0.004629716,0.0005266093,0.00029511718],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9870879,0.00115541,0.0029890153,0.002160497,0.0032428743,0.0033643104],"domain_scores_gemma":[0.99099666,0.0019310624,0.0025359967,0.0029544819,0.00022644566,0.001355334],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.0033858533,0.0013528746,0.00078509736,0.00047635415,0.0023100495,0.0022540172,0.003284526,0.0017900071,0.31551865],"category_scores_gemma":[0.0009664608,0.0021541626,0.0024021012,0.0019870382,0.0013956804,0.0029746916,0.0010356455,0.0021617936,0.0057281274],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014147536,0.001199217,0.000014845172,0.0056217406,0.0017466957,0.0017720829,0.002940773,0.002710646,0.006095522,0.64047235,0.33031753,0.005693853],"study_design_scores_gemma":[0.003206952,0.0023286755,0.00029408853,0.003991957,0.004091694,0.0011926399,0.0008141257,0.042177096,0.90077317,0.0011515769,0.03698796,0.0029900924],"about_ca_topic_score_codex":0.0049138973,"about_ca_topic_score_gemma":0.003191878,"teacher_disagreement_score":0.89467764,"about_ca_system_score_codex":0.000011346066,"about_ca_system_score_gemma":0.0016584434,"threshold_uncertainty_score":0.9999222},"labels":[],"label_agreement":null},{"id":"W1656703508","doi":"10.1029/2004gl019438","title":"Shear‐wave splitting observations in the lower Great Lakes region: Evidence for regional anisotropic domains and keel‐modified asthenospheric flow","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; Western University","funders":"","keywords":"Shear wave splitting; Geology; Lithosphere; Seismic anisotropy; Seismology; Rift; Geophysics; Keel; Asthenosphere; Anisotropy; Mantle (geology); Tectonics; Crust; Shear (geology); Seismometer; Geodesy; Petrology; Physics","score_opus":0.13849138688641938,"score_gpt":0.3107166644583459,"score_spread":0.17222527757192652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1656703508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9734237,0.00014115967,0.00093044585,0.024622662,0.00013890184,0.00061622076,0.000026344804,0.000020510977,0.00008003606],"genre_scores_gemma":[0.9951682,0.000070411574,0.0024254331,0.0014968875,0.0006764202,0.000041949654,0.000041681924,0.0000078902785,0.0000711272],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9976677,0.00029192254,0.00023063393,0.0004489588,0.0006759874,0.0006848095],"domain_scores_gemma":[0.9977997,0.0015872559,0.00005167062,0.0003431936,0.00009259241,0.00012557878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00076852815,0.00016560213,0.00022444542,0.000056369874,0.00050199166,0.00026337386,0.00036555118,0.000060719874,0.000032497715],"category_scores_gemma":[0.00024324331,0.00011573514,0.00008252163,0.00045761763,0.000361676,0.0003812907,0.000040063325,0.00029870836,0.00004196563],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009751602,0.002958624,0.07686802,0.0026195738,0.00084912515,0.004283429,0.03731406,0.1842544,0.16886026,0.2841024,0.10615264,0.12198587],"study_design_scores_gemma":[0.0015495021,0.0008399939,0.9371657,0.0003277699,0.000027165333,0.000024089546,0.000354252,0.006303754,0.00009844905,0.046400543,0.0064719524,0.00043686765],"about_ca_topic_score_codex":0.0030931872,"about_ca_topic_score_gemma":0.0005661701,"teacher_disagreement_score":0.8602976,"about_ca_system_score_codex":0.00001678827,"about_ca_system_score_gemma":0.000089023044,"threshold_uncertainty_score":0.47195423},"labels":[],"label_agreement":null},{"id":"W1668804495","doi":"","title":"The convective mantle and the not so passive margins","year":2010,"lang":"en","type":"article","venue":"EGUGA","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"National laboratory; Meteorology; Library science; Geography; Engineering physics; Engineering","score_opus":0.0034327834540909172,"score_gpt":0.17710490696751413,"score_spread":0.1736721235134232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1668804495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848398,0.000103867016,0.0000046462083,0.003470113,0.0016083824,0.00017787238,0.00008514745,0.000013720152,0.009696456],"genre_scores_gemma":[0.99822646,0.00004626465,0.000027838669,0.00033004224,0.00030153012,0.000002120729,0.0000071692234,0.000001718393,0.0010568427],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99952507,0.000055071716,0.00007115787,0.00010485722,0.00009687082,0.00014698763],"domain_scores_gemma":[0.99939865,0.00034686763,0.00004150185,0.00015409064,0.00002052767,0.00003837874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002490495,0.00006333758,0.00008559323,0.000006458789,0.00044628858,0.00017805616,0.00014971335,0.000029076276,0.00057877175],"category_scores_gemma":[0.000037251295,0.00002776833,0.000022699547,0.000031915104,0.00034644463,0.00005407633,0.000017080265,0.000102345395,0.00024020497],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001997273,0.00007956159,0.15627775,0.00008074699,0.0006544799,0.00014294349,0.018674856,0.0001477162,0.039273012,0.5231073,0.07790497,0.18165939],"study_design_scores_gemma":[0.0006932559,0.000039618673,0.6357339,0.000003421003,0.000025249425,0.000011235738,0.00025226772,0.00027844807,0.0040117023,0.01192949,0.34688264,0.0001388034],"about_ca_topic_score_codex":0.0014424452,"about_ca_topic_score_gemma":0.002766362,"teacher_disagreement_score":0.51117784,"about_ca_system_score_codex":2.94532e-7,"about_ca_system_score_gemma":0.000018887924,"threshold_uncertainty_score":0.6337145},"labels":[],"label_agreement":null},{"id":"W1679049788","doi":"10.1029/2006gc001376","title":"Role of mantle flow at the North Fiji Basin: Insights from anomalous topography","year":2006,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Lithosphere; Upwelling; Structural basin; Subduction; Basin and range topography; Mantle convection; Geophysics; Transition zone; Ocean surface topography; Basin and Range Province; Mantle wedge; Seismology; Tectonics; Geomorphology; Geodesy; Oceanography","score_opus":0.0029681043446100016,"score_gpt":0.1502642458837974,"score_spread":0.14729614153918738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1679049788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833539,0.0015969094,0.000008479923,0.00002971135,0.00046622177,0.0002374768,0.0027157883,0.000052671217,0.011538821],"genre_scores_gemma":[0.99521303,0.000018673903,0.000059951173,0.000029256169,0.0011942132,0.000007778402,0.002746247,0.000011148675,0.0007196787],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980703,0.00007911205,0.00048112415,0.00047072407,0.00047392084,0.0004248314],"domain_scores_gemma":[0.99853426,0.00016048971,0.0003319496,0.0007599144,0.000113545575,0.00009982033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008778608,0.00031763423,0.00046633132,0.0000293953,0.00029370148,0.000092841095,0.0005034073,0.00012801026,0.0008091846],"category_scores_gemma":[0.0000064935507,0.00023226635,0.00021512277,0.00030263973,0.00014557342,0.00012589333,0.00006842555,0.00012603065,0.00032239375],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031852478,0.00042010483,0.56880975,0.0007189602,0.0006200655,0.000087080036,0.0012058326,0.0132557545,0.39301342,0.0004381695,0.013585783,0.007526585],"study_design_scores_gemma":[0.00088518823,0.00011508892,0.7614527,0.00012017593,0.00020692793,0.000015669862,0.0003402754,0.0053260475,0.15455179,0.0149035705,0.06100116,0.0010813987],"about_ca_topic_score_codex":0.0419218,"about_ca_topic_score_gemma":0.0051571825,"teacher_disagreement_score":0.23846163,"about_ca_system_score_codex":0.0000063886496,"about_ca_system_score_gemma":0.000049571154,"threshold_uncertainty_score":0.9644581},"labels":[],"label_agreement":null},{"id":"W1708825675","doi":"10.1088/1367-2630/10/12/123016","title":"Anomalous compressive behavior in CeO<sub>2</sub>nanocubes under high pressure","year":2008,"lang":"en","type":"article","venue":"New Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Ministry of Education of the People's Republic of China; National University of Singapore","keywords":"Nanocrystalline material; Bulk modulus; Nanocrystal; Compressibility; Shear modulus; Hardening (computing); Physics; Diffraction; Condensed matter physics; Modulus; Nanoparticle; Composite material; Thermodynamics; Nanotechnology; Materials science; Optics","score_opus":0.015580974717458623,"score_gpt":0.2100515524274768,"score_spread":0.1944705777100182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1708825675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977169,0.00067101495,0.00019715245,0.0000642935,0.0008933061,0.00012405959,0.00008657454,0.0000112819935,0.00023543132],"genre_scores_gemma":[0.9980217,0.00018019474,0.00035083856,0.000086368644,0.001209535,5.38331e-7,0.000018799217,0.000009037062,0.00012296754],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985948,0.00009160667,0.0004219898,0.00016955996,0.0004154348,0.0003066117],"domain_scores_gemma":[0.9990625,0.000093248935,0.00036613373,0.00017466983,0.00011572367,0.00018777385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000107872715,0.00019152445,0.00043030622,0.0000671959,0.000109853514,0.000052851632,0.00031723492,0.00007129842,0.0002172476],"category_scores_gemma":[0.00000976995,0.00015599275,0.0001195838,0.00017488308,0.00008101244,0.00045185804,0.000020082118,0.00023787201,0.00006650012],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008930936,0.0010821978,0.37371513,0.00017448534,0.00054436876,0.0024144996,0.0027965852,0.10735351,0.39744636,0.002190168,0.019357197,0.09203239],"study_design_scores_gemma":[0.0016629542,0.00054902927,0.8614622,0.00008263545,0.00016096422,0.00019546946,0.0000534022,0.00013581343,0.124781184,0.007171114,0.003346349,0.00039889984],"about_ca_topic_score_codex":0.00081175443,"about_ca_topic_score_gemma":0.00016685648,"teacher_disagreement_score":0.48774704,"about_ca_system_score_codex":0.000004637435,"about_ca_system_score_gemma":0.00019000516,"threshold_uncertainty_score":0.63611996},"labels":[],"label_agreement":null},{"id":"W171334953","doi":"","title":"Fe-bearing Mineral Abundance in Primitive Chondrites by Mössbauer Spectroscopy","year":2008,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science Supplement","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Chondrite; DEPT; Mössbauer spectroscopy; Mineral; Archaeology; Mineralogy; Chemistry; Geology; Geochemistry; Meteorite; Astrobiology; Physics; Materials science; Geography; Metallurgy; Crystallography; Stereochemistry","score_opus":0.010134629136284282,"score_gpt":0.21306594543025298,"score_spread":0.2029313162939687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W171334953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954231,0.0009044286,0.00005098101,0.00034505487,0.0006058201,0.0002538548,0.0010201432,0.000020014095,0.0013766367],"genre_scores_gemma":[0.9926822,0.0006374806,0.0054799924,0.00026553427,0.00013220163,0.0000026673463,0.00060224155,0.0000039527977,0.00019373828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978076,0.00005252675,0.00031880804,0.00052335305,0.0005197606,0.0007779037],"domain_scores_gemma":[0.9993743,0.000109266955,0.00006253964,0.00019520549,0.00003657908,0.00022213413],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00059044955,0.00021507542,0.00028248315,0.0001483447,0.0004530723,0.0001405259,0.00031771848,0.0000427574,0.001024086],"category_scores_gemma":[0.000024254963,0.00018761931,0.000026238911,0.00032268866,0.0004645788,0.00044268565,0.000043540014,0.0001425949,0.000049922826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000102814716,0.00010644633,0.85479623,0.00007577679,0.000029040079,0.00023949119,0.0014637567,0.0008201723,0.12950492,0.0012235561,0.009366797,0.0022709959],"study_design_scores_gemma":[0.000898007,0.00055372773,0.9251206,0.000041510677,0.000020257408,0.00007329071,0.00021205614,0.0044792853,0.023557477,0.0008008612,0.04359827,0.0006446555],"about_ca_topic_score_codex":0.0064495406,"about_ca_topic_score_gemma":0.0014897727,"teacher_disagreement_score":0.10594744,"about_ca_system_score_codex":0.000009445831,"about_ca_system_score_gemma":0.00009654023,"threshold_uncertainty_score":0.99988914},"labels":[],"label_agreement":null},{"id":"W1727379991","doi":"10.1139/cjes-2013-0111","title":"How feasible was subduction in the Archean?","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Asthenosphere; Geology; Subduction; Mantle (geology); Archean; Lithosphere; Mantle convection; Partial melting; Crust; Oceanic crust; Eclogitization; Geophysics; Petrology; Mantle wedge; Hotspot (geology); Crustal recycling; Geochemistry; Continental crust; Seismology; Tectonics","score_opus":0.0269510506331437,"score_gpt":0.20288968541686606,"score_spread":0.17593863478372235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1727379991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99053806,0.00035145204,0.0000067398764,0.005487719,0.000748525,0.00008934061,0.000007997772,0.0000013776926,0.0027688162],"genre_scores_gemma":[0.9990253,0.000014891254,0.0002827464,0.00022163911,0.00025605844,3.08069e-7,0.0000014524859,8.3772613e-7,0.00019680607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990817,0.00010047814,0.00014844022,0.00009119891,0.00023935895,0.00033885436],"domain_scores_gemma":[0.99945074,0.00006314126,0.00010142153,0.00007756863,0.000061894134,0.0002452354],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001024461,0.000063141306,0.000108361484,0.00018111328,0.00024425582,0.0006641393,0.000433352,0.000024426201,0.0010982748],"category_scores_gemma":[0.00007494421,0.000035916197,0.000035462486,0.00034570022,0.0002455056,0.00072114926,0.0000018394427,0.00010265197,0.00006688616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000085132515,0.000015643252,0.9600146,0.000021661152,0.000017848522,0.00013412932,0.004576244,0.0043790983,0.0011393995,0.0022778823,0.008176008,0.019239008],"study_design_scores_gemma":[0.00009845983,0.00018866209,0.96881616,0.00001991604,0.00000440745,0.00008830002,0.0017464845,0.00023155335,0.00020208443,0.005959284,0.022556705,0.00008799465],"about_ca_topic_score_codex":0.05710592,"about_ca_topic_score_gemma":0.36818936,"teacher_disagreement_score":0.31108344,"about_ca_system_score_codex":7.897445e-7,"about_ca_system_score_gemma":0.0005299184,"threshold_uncertainty_score":0.99981487},"labels":[],"label_agreement":null},{"id":"W1732620039","doi":"10.1029/2010gl045136","title":"Thermal response of the mantle following the formation of a “super‐plate”","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Hotspot (geology); Geology; Supercontinent; Mantle (geology); Subduction; Mantle convection; Plate tectonics; Mantle wedge; Geophysics; Continental margin; Mantle plume; Earth science; Paleontology; Tectonics; Lithosphere; Craton","score_opus":0.021685788742083573,"score_gpt":0.2701038513500971,"score_spread":0.24841806260801355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1732620039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99574775,0.000011950143,0.000009182166,0.00315599,0.00037494145,0.00024463938,0.000045213834,0.0000068786467,0.00040348407],"genre_scores_gemma":[0.99953955,0.0000014186048,0.000048156948,0.00016392382,0.00015791018,0.0000034999737,0.000006912454,0.000003628833,0.00007498496],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9980202,0.00053323625,0.00020068137,0.00013507908,0.00076459785,0.0003462439],"domain_scores_gemma":[0.99843895,0.00094444177,0.00006740339,0.00043088428,0.00006476438,0.000053562948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001626995,0.00008289849,0.00015166827,0.00004551206,0.00024659737,0.00004736743,0.0006148303,0.00004244398,0.00021626535],"category_scores_gemma":[0.00026589274,0.000041631913,0.00013995876,0.00029974445,0.00034836296,0.00019400193,0.00007257334,0.0003501733,0.00011977795],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021924435,0.000017281423,0.0010385715,0.000017847035,0.00001575235,0.0000029341732,0.0005696236,0.00019081209,0.9957398,0.000247117,0.00090724137,0.0010337719],"study_design_scores_gemma":[0.00042907635,0.00017091223,0.6583878,0.000045050532,0.000023371658,0.0000018492817,0.00019858048,0.0025699262,0.33230168,0.0011952529,0.0045224335,0.00015410232],"about_ca_topic_score_codex":0.002019738,"about_ca_topic_score_gemma":0.00014333965,"teacher_disagreement_score":0.66343814,"about_ca_system_score_codex":0.0000018423128,"about_ca_system_score_gemma":0.00005110094,"threshold_uncertainty_score":0.30532533},"labels":[],"label_agreement":null},{"id":"W1759698","doi":"","title":"A Study of Long-Range Seismic Profile Data in Western China","year":2007,"lang":"en","type":"article","venue":"Defense Technical Information Center (DTIC)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Plateau (mathematics); Geology; China; Attenuation; Mantle (geology); Amplitude; Shield; Seismology; Geography; Physics; Paleontology; Mathematics","score_opus":0.027227408685699204,"score_gpt":0.264761024772987,"score_spread":0.23753361608728782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1759698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939176,0.000011825698,0.0011322497,0.00004287182,0.00020895564,0.0006001603,0.00045382217,0.000060323076,0.0035722037],"genre_scores_gemma":[0.99863833,0.000006403482,0.00021856892,0.00014105214,0.00003850575,0.0000023808234,0.00093263236,0.0000027928245,0.000019335219],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985577,0.000044362445,0.00065441604,0.00015395891,0.0003199286,0.00026965374],"domain_scores_gemma":[0.99910027,0.000057853926,0.00018796962,0.00053925783,0.00003805025,0.000076588745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082884164,0.00012545775,0.00023090171,0.00014780759,0.000041935007,0.00005841472,0.00045658136,0.00007501017,0.000244436],"category_scores_gemma":[0.0000460986,0.00010199669,0.000025589845,0.00022868873,0.000039051785,0.0009784171,0.00010689094,0.00012869661,0.00026864657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024883734,0.0004444984,0.9839612,0.00012291328,0.00002607428,0.000039559127,0.0019270094,0.00044025193,0.000035629808,0.000045940047,0.0009106703,0.011797373],"study_design_scores_gemma":[0.0008610845,0.0001922527,0.99497026,0.000031739928,0.000013073256,0.000015215949,0.0001555582,0.00095468824,0.00005760169,0.000035510602,0.0025792115,0.00013380672],"about_ca_topic_score_codex":0.0013312299,"about_ca_topic_score_gemma":0.0028982162,"teacher_disagreement_score":0.011663566,"about_ca_system_score_codex":0.0000047420895,"about_ca_system_score_gemma":0.00001841252,"threshold_uncertainty_score":0.41593042},"labels":[],"label_agreement":null},{"id":"W181202405","doi":"","title":"In situ High-Pressure Studies of Energetic Materials by Vibrational Spectroscopy and X-ray diffraction","year":2013,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ontario Ministry of Research and Innovation","keywords":"Diffraction; Spectroscopy; In situ; Materials science; X-ray crystallography; Analytical Chemistry (journal); Chemistry; Physics; Optics","score_opus":0.032154298003164515,"score_gpt":0.26401275665934165,"score_spread":0.23185845865617713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W181202405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998407,0.00035533475,0.00004067794,0.00022223577,0.0004639412,0.00025422106,0.00018437312,0.000026197564,0.000046009292],"genre_scores_gemma":[0.9986442,0.0002942721,0.00013930064,0.00009144934,0.00009624968,8.837715e-7,0.00009765334,0.000007722086,0.00062827335],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985623,0.00024538022,0.00027774659,0.00036527816,0.00025536626,0.0002939232],"domain_scores_gemma":[0.9992745,0.00011993314,0.000200827,0.00020508117,0.00008847997,0.00011119183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021599222,0.00021695234,0.00040189576,0.00019307774,0.00011305859,0.0001672456,0.00025705373,0.00012005481,0.0005074607],"category_scores_gemma":[0.000022502652,0.00020545309,0.000032080305,0.00017899895,0.00013242284,0.001951773,0.00007032174,0.00012975831,0.00011408498],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060749044,0.000035125897,0.44085044,0.00009115747,0.00006896103,0.000014971022,0.0001636945,0.00011150741,0.55847377,0.000062106265,0.000010724361,0.00005678333],"study_design_scores_gemma":[0.0004444976,0.00010753622,0.859159,0.000054421682,0.000048069734,0.0000024374037,0.0001140883,4.938819e-7,0.1389533,0.00063189905,0.00028950337,0.00019474606],"about_ca_topic_score_codex":0.0003488792,"about_ca_topic_score_gemma":0.0018220788,"teacher_disagreement_score":0.4195205,"about_ca_system_score_codex":0.000009957416,"about_ca_system_score_gemma":0.000026688442,"threshold_uncertainty_score":0.8378134},"labels":[],"label_agreement":null},{"id":"W1814741581","doi":"10.1139/cjp-2013-0349","title":"Structural phase transition of refractory metal carbides at high pressure","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Carbide; Structural stability; Phase (matter); Transition metal; Thermodynamics; Metal; Phase transition; High pressure; Refractory metals; Physics; Refractory (planetary science); Stability (learning theory); Structural change; Crystallography; Materials science; Chemistry; Metallurgy; Structural engineering","score_opus":0.010502881552461494,"score_gpt":0.19511922465115764,"score_spread":0.18461634309869615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1814741581","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979419,0.0004589952,0.000020969075,0.00008297084,0.0006589102,0.0000782297,0.00051177887,0.0000023203668,0.00024391073],"genre_scores_gemma":[0.9992077,0.0000077752175,0.00012615786,0.000046676196,0.00047863176,2.0779657e-7,0.000054292064,0.0000041553267,0.00007441409],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9992373,0.000054961438,0.00025892828,0.00008010614,0.0001669393,0.00020173738],"domain_scores_gemma":[0.99914414,0.000030288465,0.00023455448,0.00010553612,0.00016386522,0.00032162503],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008694322,0.00010191796,0.00025317247,0.00005021171,0.00008893028,0.000040045397,0.00016290051,0.00004559238,0.0029434965],"category_scores_gemma":[0.000009424109,0.000080768456,0.00008985874,0.00007358037,0.00008444247,0.0004215272,0.0000020897814,0.00009399346,0.000029294426],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006391203,0.00021020103,0.03276874,0.0010903069,0.0032385867,0.0005678438,0.019644916,0.10528628,0.530189,0.006897844,0.039624967,0.25984222],"study_design_scores_gemma":[0.008815722,0.004689349,0.59681886,0.00043813713,0.0021269713,0.00029684877,0.0010226285,0.008176997,0.24569309,0.07263878,0.05701797,0.0022646207],"about_ca_topic_score_codex":0.064005084,"about_ca_topic_score_gemma":0.011813278,"teacher_disagreement_score":0.56405014,"about_ca_system_score_codex":0.000006324512,"about_ca_system_score_gemma":0.00023659956,"threshold_uncertainty_score":0.99796796},"labels":[],"label_agreement":null},{"id":"W1819619727","doi":"10.1139/cjp-2015-0020","title":"Pressure-induced vibrational and superconducting properties of lanthanum hydrides from first principles calculations","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"China Academy of Engineering Physics","keywords":"Superconductivity; Lanthanum; Octahedron; Phonon; Condensed matter physics; Hydrogen; Physics; Infrared; Raman spectroscopy; Crystallography; Chemistry; Crystal structure; Quantum mechanics","score_opus":0.07698047896457505,"score_gpt":0.20870789897176573,"score_spread":0.13172742000719068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1819619727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983115,0.0006032352,0.00005108091,0.00017496521,0.00037041405,0.00005140246,0.00023696691,0.0000023119721,0.00019811705],"genre_scores_gemma":[0.99894315,0.000004476227,0.0005022389,0.000018202181,0.00048405686,2.0062281e-7,0.000025996635,0.0000031161962,0.00001859117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99938565,0.000036873505,0.00022604351,0.000075605334,0.00014686346,0.00012895241],"domain_scores_gemma":[0.99929196,0.000037381255,0.00014588852,0.00007420131,0.00016364895,0.00028690696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014752505,0.00007562394,0.0001771787,0.000039353756,0.000102388796,0.000066121145,0.00011089987,0.000033130113,0.00008672351],"category_scores_gemma":[0.00007259598,0.000059444792,0.00003113607,0.000058399924,0.00006548858,0.00037967338,0.000004924947,0.00006605181,0.000004889561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000117734424,0.000067260975,0.6646528,0.0002599491,0.0008212016,0.00008560006,0.025352526,0.17844239,0.11539302,0.007892457,0.0017128738,0.005202166],"study_design_scores_gemma":[0.0024284439,0.0007710805,0.5760629,0.00093296764,0.00064017304,0.000104398794,0.0046250434,0.036592294,0.31871802,0.023196686,0.03465785,0.0012701356],"about_ca_topic_score_codex":0.06416314,"about_ca_topic_score_gemma":0.06843508,"teacher_disagreement_score":0.20332499,"about_ca_system_score_codex":0.0000035225303,"about_ca_system_score_gemma":0.0005499845,"threshold_uncertainty_score":0.9485636},"labels":[],"label_agreement":null},{"id":"W1824696493","doi":"","title":"Exotic Nuclei in the Crust of Magnetars","year":2013,"lang":"en","type":"article","venue":"Dépôt institutionnel de l'Université libre de Bruxelles (Université Libre de Bruxelles)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magnetar; Crust; Physics; Astrophysics; Atomic mass; Nuclear physics; Atomic physics; Geology; Geophysics; Neutron star","score_opus":0.009734215463993329,"score_gpt":0.1645445432847559,"score_spread":0.15481032782076257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1824696493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9744486,0.0008990933,0.00086549914,0.0014885071,0.00032198572,0.0006364459,0.00024541424,0.00013167191,0.020962758],"genre_scores_gemma":[0.99546057,0.00065788324,0.0016470038,0.00059904094,0.00018172924,0.0000025814131,0.00018027122,0.000020259302,0.0012506515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971477,0.00040332906,0.0004174851,0.0005626817,0.00048439114,0.0009844447],"domain_scores_gemma":[0.9983032,0.00027677167,0.0002850255,0.00064820243,0.00012395265,0.00036289467],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004582078,0.0004471566,0.0005423901,0.00043045013,0.0006519928,0.00022186672,0.0017320935,0.00035837028,0.004911896],"category_scores_gemma":[0.00004006336,0.0004159408,0.00027459773,0.0010455218,0.00046020382,0.0015643302,0.00018430532,0.0004364242,0.00063407805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004525243,0.0019209784,0.3222126,0.001580062,0.0012203372,0.007514958,0.088266715,0.18879092,0.024792474,0.10981306,0.16166112,0.08770154],"study_design_scores_gemma":[0.00544383,0.00038448937,0.8698081,0.0002685128,0.00030982043,0.0004767119,0.023170482,0.02046369,0.00082321046,0.004050391,0.07363269,0.0011681154],"about_ca_topic_score_codex":0.018439813,"about_ca_topic_score_gemma":0.0025930717,"teacher_disagreement_score":0.54759544,"about_ca_system_score_codex":0.00008311492,"about_ca_system_score_gemma":0.00045604247,"threshold_uncertainty_score":0.99982923},"labels":[],"label_agreement":null},{"id":"W1839055989","doi":"10.1063/1.4934502","title":"Mechanisms for pressure-induced crystal-crystal transition, amorphization, and devitrification of SnI4","year":2015,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Argonne National Laboratory; Basic Energy Sciences; Western Canada Research Grid; Office of Science; University of Chicago; U.S. Department of Energy","keywords":"Ambient pressure; Polyamorphism; Amorphous solid; Materials science; Crystallography; Recrystallization (geology); Crystal structure; Phase transition; Devitrification; Chemical physics; Crystal (programming language); Crystallization; Chemistry; Condensed matter physics; Thermodynamics; Physics","score_opus":0.02419839389770946,"score_gpt":0.22142803557853996,"score_spread":0.19722964168083051,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1839055989","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94523114,0.00017335796,0.05376179,0.0003183317,0.00015636747,0.00017731263,0.000103311715,0.0000058414184,0.00007256151],"genre_scores_gemma":[0.99867564,0.000013132772,0.0009827571,0.000043145003,0.0002453348,4.3501728e-7,0.000029620542,0.000003890002,0.0000060630796],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99926734,0.00005375839,0.0002856544,0.00006289444,0.00023113529,0.00009920485],"domain_scores_gemma":[0.9990941,0.00011200031,0.00030250227,0.00009366164,0.00031506835,0.00008265469],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047304184,0.00007873626,0.00019798048,0.000014695399,0.000035492998,0.000019916226,0.00014412924,0.000041767456,0.000015737156],"category_scores_gemma":[0.00004677925,0.00005163192,0.000046278572,0.000080587175,0.00004765119,0.00019086055,0.0000051404822,0.00006142613,0.0000010372329],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000273847,0.000035684647,0.000021370044,0.000056000397,0.00005779522,2.4288119e-7,0.0008966074,0.0030169454,0.9930041,0.0012464096,0.0005890861,0.0008018994],"study_design_scores_gemma":[0.0010805291,0.00032543376,0.0005201182,0.000042650816,0.00032195664,0.000020624293,0.00017783369,0.0048060277,0.818666,0.17312318,0.0007603281,0.00015531387],"about_ca_topic_score_codex":0.000037554222,"about_ca_topic_score_gemma":0.0000013459386,"teacher_disagreement_score":0.1743381,"about_ca_system_score_codex":0.0000017183941,"about_ca_system_score_gemma":0.000054488963,"threshold_uncertainty_score":0.21054885},"labels":[],"label_agreement":null},{"id":"W1841242412","doi":"10.1039/c5cp01510c","title":"Structural morphologies of high-pressure polymorphs of strontium hydrides","year":2015,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Monatomic ion; Electronegativity; Chemical physics; Valence electron; Molecule; Chemistry; Crystallography; Strontium; Hydrogen; Crystal structure; Valence (chemistry); Electron; Materials science; Organic chemistry","score_opus":0.017248964619091346,"score_gpt":0.21870732553551475,"score_spread":0.2014583609164234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1841242412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708265,0.00012634562,0.000033640772,0.000037830192,0.0001352447,0.00008706185,0.00074766093,0.000047979443,0.0017015779],"genre_scores_gemma":[0.99843967,0.0000025629627,0.0003490344,0.000011431427,0.0007782007,0.0000017334032,0.00032749862,0.000010582351,0.00007928124],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99839205,0.000028696744,0.0003546209,0.00035996732,0.00050144346,0.00036322704],"domain_scores_gemma":[0.9987612,0.00012411467,0.00029167856,0.00044447844,0.00016669036,0.00021186529],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007379524,0.0002822882,0.00067400147,0.0000089605655,0.000028048542,0.000021865864,0.0005231558,0.00010803985,0.00021869074],"category_scores_gemma":[0.00007699582,0.00023296438,0.00017261894,0.00017704676,0.0004108069,0.00019213534,0.00009113058,0.00018326071,0.00002137889],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001182601,0.0001184772,0.0015325057,0.00024821443,0.00010924922,0.0000029888156,0.00013871831,0.007254346,0.9885116,0.0003887561,0.000637485,0.0009394041],"study_design_scores_gemma":[0.0004440756,0.00005304258,0.0014177071,0.000021195687,0.00009472783,0.0000018596795,0.000050698054,0.003160617,0.9737021,0.020710198,0.000087449946,0.00025633376],"about_ca_topic_score_codex":0.0012269615,"about_ca_topic_score_gemma":0.0000014240997,"teacher_disagreement_score":0.020321442,"about_ca_system_score_codex":0.000004654249,"about_ca_system_score_gemma":0.00007209489,"threshold_uncertainty_score":0.9500012},"labels":[],"label_agreement":null},{"id":"W1852646792","doi":"10.1029/2011tc002886","title":"A three‐dimensional Moho depth model for the Tien Shan from EGM2008 gravity data","year":2011,"lang":"en","type":"article","venue":"Tectonics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Lithosphere; Terrane; Seismology; Subduction; Gravity anomaly; Crust; Inversion (geology); Structural basin; Mantle (geology); Discontinuity (linguistics); Isostasy; Tectonics; Geodesy; Geophysics; Geomorphology; Paleontology","score_opus":0.10652550292735984,"score_gpt":0.24856233544639458,"score_spread":0.14203683251903476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1852646792","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9573599,0.0011526922,0.026204955,0.0002024596,0.0012604182,0.0008339744,0.011014783,0.00013356088,0.0018372304],"genre_scores_gemma":[0.9880091,0.000018515266,0.010671662,0.00018081433,0.00014504569,0.000003952753,0.00088638754,0.0000062882955,0.00007823683],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990956,0.00001641947,0.00014822837,0.0003019061,0.00018381735,0.0002539997],"domain_scores_gemma":[0.9989512,0.00014937273,0.00006669526,0.000730345,0.000033614644,0.00006875019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028311784,0.00012180807,0.00015401977,0.000014286074,0.00021574603,0.0000421054,0.0007485043,0.000059805734,0.0007246005],"category_scores_gemma":[0.000025272735,0.000075960095,0.000041074996,0.000053771917,0.000062927116,0.000155363,0.00009198201,0.00007639424,0.00013073625],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0046003344,0.0012515286,0.1507925,0.00030742717,0.0028000847,0.000108841115,0.012007977,0.17588378,0.010440685,0.025553899,0.21528277,0.4009702],"study_design_scores_gemma":[0.00023342765,0.000045912606,0.05418902,0.0000058404094,0.000068547924,0.0000012328218,0.0000075132284,0.91089755,0.00026320392,0.030867716,0.003260009,0.00016000749],"about_ca_topic_score_codex":0.013433333,"about_ca_topic_score_gemma":0.023308396,"teacher_disagreement_score":0.7350138,"about_ca_system_score_codex":0.0000014298969,"about_ca_system_score_gemma":0.000074140364,"threshold_uncertainty_score":0.9945137},"labels":[],"label_agreement":null},{"id":"W1853033159","doi":"10.1063/1.4927566","title":"Effects of stacking disorder on thermal conductivity of cubic ice","year":2015,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Vetenskapsrådet; Carl Tryggers Stiftelse för Vetenskaplig Forskning","keywords":"Stacking; Cubic crystal system; Materials science; Thermal conductivity; Ice crystals; Hexagonal crystal system; Annealing (glass); Crystal structure; Crystallography; Mineralogy; Chemistry; Composite material; Optics; Physics","score_opus":0.0166446268038781,"score_gpt":0.22269066947321123,"score_spread":0.20604604266933313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1853033159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989321,0.00017589051,0.000073259245,0.000045847173,0.00021964619,0.000052669748,0.000012392046,0.0000021498022,0.0004860389],"genre_scores_gemma":[0.9996191,0.00001019675,0.000050168903,0.000025961092,0.00028433258,6.082476e-8,0.0000018154772,0.0000028147526,0.0000055519363],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992178,0.000105098145,0.00021162396,0.000045647554,0.00031162446,0.000108170134],"domain_scores_gemma":[0.9989802,0.00038841038,0.00035322792,0.00010569389,0.00011224142,0.000060202903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003573573,0.00007847896,0.00025842784,0.000010422411,0.000015252889,0.000006634168,0.00022326496,0.000028479699,0.000022562725],"category_scores_gemma":[0.000059753875,0.000044085864,0.000064974076,0.00007633255,0.00010317491,0.00012384767,0.000014521283,0.00012615726,0.0000059386243],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004628852,0.00013594546,0.0010785693,0.000091615766,0.00007463508,0.0000020444381,0.00073678646,0.0041640946,0.98884076,0.00020030641,0.00023710192,0.003975253],"study_design_scores_gemma":[0.00050686265,0.00030226362,0.0030521613,0.000058201927,0.00007931573,0.0000023288073,0.000037241974,0.00014917899,0.98792726,0.007688678,0.00012673531,0.00006975911],"about_ca_topic_score_codex":0.00013966052,"about_ca_topic_score_gemma":0.0000011297785,"teacher_disagreement_score":0.007488372,"about_ca_system_score_codex":0.0000019048713,"about_ca_system_score_gemma":0.000041686948,"threshold_uncertainty_score":0.17977694},"labels":[],"label_agreement":null},{"id":"W1854257507","doi":"10.1063/1.4930095","title":"Mechanical and thermal properties of γ-Mg2SiO4 under high temperature and high pressure conditions such as in mantle: A first principles study","year":2015,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Wilfrid Laurier University","funders":"National Natural Science Foundation of China","keywords":"Thermal conductivity; Thermodynamics; Thermal expansion; Thermal; Grüneisen parameter; Materials science; High pressure; Mantle (geology); Phonon; Work (physics); Mineralogy; Geology; Condensed matter physics; Geophysics; Physics","score_opus":0.024337995307466113,"score_gpt":0.21873634043179366,"score_spread":0.19439834512432755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1854257507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989464,0.0003567857,0.0000012439245,0.00037233962,0.00009252938,0.00015215568,0.000038193237,0.0000035965684,0.00003671547],"genre_scores_gemma":[0.9996712,0.000036972215,0.000030106958,0.000040321804,0.0001911421,6.331802e-7,0.0000044534104,0.0000040259333,0.000021115033],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99912727,0.000108047905,0.00027085815,0.000089984125,0.00027611907,0.00012774738],"domain_scores_gemma":[0.99943256,0.00010004209,0.00016581266,0.00011394493,0.00009644059,0.00009122225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035997314,0.00011134844,0.00029013876,0.000016895656,0.00004583959,0.00003697241,0.00017654694,0.000054815067,0.000033434808],"category_scores_gemma":[0.000034812696,0.00006044778,0.0000227561,0.00007519844,0.000130672,0.00016865741,0.000044010867,0.00019468892,0.0000019333322],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020253444,0.00095585856,0.01178239,0.00027565248,0.0005572232,0.00003693072,0.00714382,0.021123322,0.9503225,0.004748645,0.00062494574,0.00040334766],"study_design_scores_gemma":[0.0063687856,0.0022432925,0.17766576,0.0005310978,0.00089958764,0.00016491013,0.0035862948,0.0017147028,0.7350027,0.07067661,0.00042328853,0.0007229744],"about_ca_topic_score_codex":0.00048450567,"about_ca_topic_score_gemma":0.000044251585,"teacher_disagreement_score":0.21531983,"about_ca_system_score_codex":0.0000020751806,"about_ca_system_score_gemma":0.000053060467,"threshold_uncertainty_score":0.2464989},"labels":[],"label_agreement":null},{"id":"W1862686990","doi":"10.1139/p11-062","title":"High temperature elastic anharmonicity in lanthanum mono-chalcogenides","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Anharmonicity; Lanthanum; Physics; Thermodynamics; Atmospheric temperature range; Range (aeronautics); Condensed matter physics; Materials science; Composite material; Nuclear physics","score_opus":0.0182405484838012,"score_gpt":0.1771531159347035,"score_spread":0.15891256745090232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1862686990","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979728,0.00022476712,0.000014363373,0.000039361083,0.0009210625,0.000050024344,0.00016972118,0.0000031497282,0.00060474925],"genre_scores_gemma":[0.9990917,0.000020585212,0.00029842267,0.00008088428,0.00045329318,1.8032269e-7,0.000013836211,0.0000045350807,0.000036594916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991845,0.000065184555,0.00023976096,0.00010082767,0.000112224654,0.00029752805],"domain_scores_gemma":[0.9992875,0.000035600984,0.00013663985,0.00010579843,0.00007581063,0.00035868332],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002015643,0.00011512602,0.00023597907,0.00008551153,0.000085274136,0.000049879327,0.00023803407,0.00006092679,0.0008297503],"category_scores_gemma":[0.00002441649,0.00009495538,0.00006187872,0.00015609428,0.000054057895,0.00023273347,0.0000031562165,0.0002193738,0.00007103361],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041627375,0.00020928933,0.86331755,0.00024303472,0.00054842624,0.005588471,0.014305185,0.016314002,0.04041266,0.01574876,0.012643831,0.03025252],"study_design_scores_gemma":[0.000766481,0.00038229278,0.9299908,0.00014590498,0.00007685468,0.00008335001,0.00031236192,0.0001158898,0.035188675,0.030634247,0.0018109339,0.0004921818],"about_ca_topic_score_codex":0.067911245,"about_ca_topic_score_gemma":0.096204504,"teacher_disagreement_score":0.06667328,"about_ca_system_score_codex":0.000008461766,"about_ca_system_score_gemma":0.000406106,"threshold_uncertainty_score":0.9382956},"labels":[],"label_agreement":null},{"id":"W1866187292","doi":"10.2138/am-2002-0104","title":"<sup>29</sup> Si MAS NMR study of diopside–Ca-Tschermak clinopyroxenes: Detecting both tetrahedral and octahedral Al substitution","year":2002,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts; University of Alberta","keywords":"Diopside; Octahedron; Crystallography; Chemistry; Tetrahedron; Silicate; Chemical shift; NMR spectra database; Pyroxene; Spectral line; Mineralogy; Olivine; Physical chemistry; Crystal structure; Physics","score_opus":0.019762092922074963,"score_gpt":0.23390432238422937,"score_spread":0.21414222946215442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1866187292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967766,0.00021283506,0.000029733026,0.00011055208,0.00015517577,0.0002967466,0.00010956016,0.000056077242,0.0022527291],"genre_scores_gemma":[0.9986399,0.00007241242,0.0006046263,0.00017159381,0.00024903766,0.0000047200983,0.00005109034,0.000009865003,0.00019676505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980453,0.00020280073,0.0004920139,0.00047681967,0.00031884012,0.0004641764],"domain_scores_gemma":[0.99901724,0.0001606503,0.00028904338,0.00031684333,0.00005054568,0.00016565484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023835876,0.0002781356,0.0005346542,0.00009853724,0.00022468453,0.000101512574,0.00023109699,0.00005210826,0.00070075254],"category_scores_gemma":[0.00008026899,0.00023237184,0.000071020375,0.00034723306,0.00058475655,0.00026665066,0.000035583256,0.00015759491,0.00006721706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013266857,0.00032535123,0.9473724,0.000049874634,0.00013180028,0.00013720666,0.0022833126,0.014536938,0.006711281,0.000089231544,0.0009001565,0.02732982],"study_design_scores_gemma":[0.0017954323,0.0029867848,0.93006366,0.000039300456,0.00017584862,0.00007674534,0.0035741255,0.053853977,0.00038894697,0.00011289024,0.006028457,0.00090385205],"about_ca_topic_score_codex":0.03292135,"about_ca_topic_score_gemma":0.002690569,"teacher_disagreement_score":0.03931704,"about_ca_system_score_codex":0.0000055796304,"about_ca_system_score_gemma":0.000017457689,"threshold_uncertainty_score":0.9735185},"labels":[],"label_agreement":null},{"id":"W1867125714","doi":"10.1103/physrevb.66.014110","title":"Equation of state and the Hugoniot of laser shock-compressed deuterium: Demonstration of a basis-function-free method for quantum calculations","year":2002,"lang":"en","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Equation of state; Shock (circulatory); Compressibility; Path integral Monte Carlo; Physics; Deuterium; Electron; Quantum; Shock wave; Path integral formulation; Thermodynamics; Quantum mechanics","score_opus":0.0244815516455097,"score_gpt":0.27320783466046195,"score_spread":0.24872628301495225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1867125714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8959437,0.002520473,0.09339586,0.0037877967,0.00027859982,0.001946754,0.0010137267,0.000015476237,0.001097628],"genre_scores_gemma":[0.99793255,0.0002637145,0.0012263726,0.00039992135,0.00004567026,0.00001697534,0.000049059512,0.000004585571,0.00006114093],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988871,0.00021875055,0.00042400116,0.0001580794,0.00019337113,0.000118695614],"domain_scores_gemma":[0.99845624,0.0007700243,0.00032921997,0.0002663039,0.00014310618,0.000035131725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038330478,0.00011121591,0.0004489769,0.000027300024,0.000050238385,0.000014842849,0.0001255154,0.000023121222,0.0007282541],"category_scores_gemma":[0.00006543331,0.00007338657,0.00012634581,0.00010501762,0.0001220437,0.000119437515,0.000014808043,0.00004302767,0.000020421303],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0034562645,0.001495636,0.020376423,0.028923687,0.0023451296,0.0000041736103,0.0048788483,0.021706982,0.63244486,0.14467505,0.061441775,0.0782512],"study_design_scores_gemma":[0.0070784204,0.0007821214,0.11429928,0.0013671061,0.002162823,0.000007081997,0.00006195936,0.46802992,0.14699876,0.25226578,0.006128811,0.00081795227],"about_ca_topic_score_codex":0.00026123188,"about_ca_topic_score_gemma":0.000040212588,"teacher_disagreement_score":0.48544607,"about_ca_system_score_codex":9.88475e-7,"about_ca_system_score_gemma":0.000011739176,"threshold_uncertainty_score":0.7973872},"labels":[],"label_agreement":null},{"id":"W1867260020","doi":"10.1002/2015gl065142","title":"Variations in grain size and viscosity based on vacancy diffusion in minerals, seismic tomography, and geodynamically inferred mantle rheology","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle (geology); Geology; Grain size; Rheology; Viscosity; Seismic tomography; Arrhenius equation; Diffusion creep; Mineralogy; Geophysics; Thermodynamics; Materials science; Grain boundary; Physics; Microstructure; Activation energy; Chemistry; Composite material","score_opus":0.020162965224324418,"score_gpt":0.26829727936257997,"score_spread":0.24813431413825554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1867260020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934638,0.000029884959,0.0000859603,0.0055741314,0.00011092057,0.00030820214,0.00006833177,0.000014420131,0.00034435515],"genre_scores_gemma":[0.9987911,0.000017301156,0.00022281749,0.000722138,0.00008530445,0.000011115967,0.00006725914,0.000005130987,0.00007782927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978453,0.0005419869,0.00020793243,0.00041307954,0.00044042882,0.0005512727],"domain_scores_gemma":[0.99871576,0.0007690275,0.000033130313,0.00020098513,0.000042135973,0.00023895864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079217023,0.00014763555,0.00026619143,0.00026770387,0.00009291668,0.000090961854,0.00017007459,0.000080808924,0.00005332717],"category_scores_gemma":[0.00029090984,0.00012553466,0.00002865741,0.0004721727,0.00023250194,0.0001458604,0.00006786489,0.00033733045,0.00003309716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023193085,0.0012501891,0.7934607,0.0002643173,0.00006336305,0.00080132636,0.0017758321,0.013175077,0.15811151,0.007227393,0.0054981466,0.016052807],"study_design_scores_gemma":[0.0010185544,0.00024793882,0.8949584,0.000034123088,0.000003307063,0.0000010792603,0.000016041588,0.099460274,0.000033075565,0.003645974,0.00043397915,0.00014730461],"about_ca_topic_score_codex":0.02056909,"about_ca_topic_score_gemma":0.002911109,"teacher_disagreement_score":0.15807843,"about_ca_system_score_codex":0.000010430559,"about_ca_system_score_gemma":0.000063732536,"threshold_uncertainty_score":0.98595303},"labels":[],"label_agreement":null},{"id":"W1882002156","doi":"10.1139/e09-040","title":"Teleseismic studies of the Canadian landmass: Lithoprobe and its legacyThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.ESS Contribution 20090305.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; University of British Columbia; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Subduction; Craton; Seismology; Plate tectonics; Earth science; Tectonics; Paleontology","score_opus":0.012318321302582227,"score_gpt":0.20117687588025251,"score_spread":0.18885855457767028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1882002156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898946,0.0016135387,2.6716486e-7,0.006664582,0.00036162103,0.00029071755,0.00020090875,7.141805e-7,0.00097300584],"genre_scores_gemma":[0.99952275,0.00013983021,0.000043177875,0.00011167791,0.0001244981,0.0000011101731,7.928307e-7,0.0000015704633,0.000054583354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986769,0.00016356003,0.0004521349,0.00012795851,0.0003289474,0.00025052103],"domain_scores_gemma":[0.99845105,0.00031504207,0.00052775594,0.00012677575,0.0004349582,0.00014443217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002196795,0.00009991932,0.00035604078,0.00015089223,0.00027929185,0.00010694106,0.00034881217,0.000053052165,0.0005333313],"category_scores_gemma":[0.0012694488,0.00004832964,0.000044307104,0.0005220001,0.001581633,0.00041500528,0.0000107423975,0.00016293286,4.9291054e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081699603,0.000089974594,0.9036831,0.0006337788,0.0004019958,0.000016461117,0.039699696,0.00086085114,0.016965829,0.030406862,0.002343907,0.0040805526],"study_design_scores_gemma":[0.0023113906,0.0010545821,0.87874067,0.0008754854,0.00017968593,0.00006061474,0.009212716,0.0004802065,0.08081295,0.012579177,0.013362109,0.0003304333],"about_ca_topic_score_codex":0.28393692,"about_ca_topic_score_gemma":0.92356044,"teacher_disagreement_score":0.6396235,"about_ca_system_score_codex":0.000004218098,"about_ca_system_score_gemma":0.0014007137,"threshold_uncertainty_score":0.7208314},"labels":[],"label_agreement":null},{"id":"W1885207547","doi":"10.1111/j.1365-246x.2011.05027.x","title":"Adjoint centroid-moment tensor inversions","year":2011,"lang":"fr","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Seismogram; Hessian matrix; Centroid; Tensor (intrinsic definition); Mathematics; Conjugate gradient method; Applied mathematics; Mathematical analysis; Inverse problem; Moment (physics); Geology; Geometry; Algorithm; Physics; Seismology; Classical mechanics","score_opus":0.04289680669250186,"score_gpt":0.22186385651178211,"score_spread":0.17896704981928024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1885207547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.80826163,0.002187694,0.002291976,0.020763986,0.07134584,0.00046381284,0.0018740058,0.00008381413,0.09272722],"genre_scores_gemma":[0.9520062,0.0012680219,0.0031566012,0.001286996,0.008759538,0.0000031170935,0.00014217243,0.000020681857,0.033356667],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974775,0.00018633543,0.00056107144,0.0003435103,0.00077606476,0.00065553567],"domain_scores_gemma":[0.99849874,0.00008574213,0.00032678532,0.00020199278,0.00029698425,0.00058976054],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032241433,0.00029648622,0.00034300436,0.00012824188,0.00032171892,0.0002882663,0.0007046354,0.0001327696,0.048340775],"category_scores_gemma":[0.000043639826,0.00025416943,0.00032690185,0.00014404401,0.0002307082,0.0006870554,0.000110087414,0.00051539874,0.006767359],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017861385,0.0044457987,0.03989337,0.0001688406,0.0036547524,0.0034500693,0.008440196,0.0017951006,0.009254986,0.19094536,0.52260065,0.21356474],"study_design_scores_gemma":[0.0012213677,0.000579437,0.17482351,0.00022408337,0.00018925221,0.00042849162,0.00029761682,0.0023718292,0.0017187456,0.030934623,0.78660536,0.00060567626],"about_ca_topic_score_codex":0.0022755507,"about_ca_topic_score_gemma":0.00007223977,"teacher_disagreement_score":0.2640047,"about_ca_system_score_codex":0.000044316497,"about_ca_system_score_gemma":0.00015072215,"threshold_uncertainty_score":0.99999106},"labels":[],"label_agreement":null},{"id":"W1887050604","doi":"10.1029/2010gl043654","title":"Waveform inversion for S‐wave structure in the lowermost mantle beneath the Arctic: Implications for mineralogy and chemical composition","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Geology; Core–mantle boundary; Mantle (geology); Geophysics; Arctic; Transition zone; Shear velocity; Mineralogy; Meteorology; Oceanography; Physics","score_opus":0.028031918948686108,"score_gpt":0.2831888192608133,"score_spread":0.2551569003121272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1887050604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9706432,0.0000084000085,0.000075556054,0.027825242,0.0001376589,0.0008033425,0.0004492181,0.0000058368378,0.000051542313],"genre_scores_gemma":[0.9972924,0.0000045549355,0.0005812607,0.0010664067,0.0005301968,0.000040594146,0.00046789265,0.0000042546967,0.000012451374],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989441,0.000078595374,0.00012276351,0.00024173662,0.00020653111,0.00040625577],"domain_scores_gemma":[0.99845123,0.0011314111,0.000029869543,0.000244752,0.00007460594,0.00006815432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004228142,0.00009610457,0.0001230535,0.00004028994,0.0003517505,0.00012666835,0.00028516367,0.00006133434,0.000032556996],"category_scores_gemma":[0.0000650393,0.000052371517,0.000048171336,0.0001403204,0.0002862986,0.00009950615,0.00003197317,0.0002961075,0.000007936294],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014966518,0.000032265343,0.0007852267,0.00004851871,0.000015688714,0.0000014655473,0.00042197754,0.000016573817,0.97978973,0.008312436,0.0048241387,0.005602312],"study_design_scores_gemma":[0.0021929138,0.00054186664,0.804786,0.00003963949,0.00007629833,0.00003330065,0.00028905546,0.013634829,0.023481954,0.12450551,0.029862544,0.0005560338],"about_ca_topic_score_codex":0.0011929352,"about_ca_topic_score_gemma":0.0006231708,"teacher_disagreement_score":0.95630777,"about_ca_system_score_codex":0.000004320875,"about_ca_system_score_gemma":0.000021357828,"threshold_uncertainty_score":0.27054158},"labels":[],"label_agreement":null},{"id":"W1897970409","doi":"10.1002/jrs.3049","title":"Raman investigation of hydrostatic and nonhydrostatic compressions of OH‐ and F‐apophyllites up to 8 GPa","year":2011,"lang":"en","type":"article","venue":"Journal of Raman Spectroscopy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Raman spectroscopy; Hydrostatic equilibrium; Hydrostatic pressure; Compression (physics); Wavenumber; Diamond anvil cell; Silicate; Ion; Materials science; Molecule; Analytical Chemistry (journal); Chemistry; Diffraction; Mineralogy; Crystallography; Thermodynamics; Optics; Composite material; Physics; Organic chemistry","score_opus":0.017783861559482785,"score_gpt":0.22192318402944136,"score_spread":0.20413932246995858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1897970409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998725,0.00029266864,0.00014788943,0.00008779211,0.0002393166,0.00013053547,0.00006801358,0.0000036218917,0.00030513963],"genre_scores_gemma":[0.9903345,0.00010670762,0.009411539,0.000054195487,0.00005377291,2.914066e-7,0.000005957295,0.0000041984217,0.000028830515],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989243,0.000079330144,0.000491823,0.00011561673,0.00023125851,0.00015768576],"domain_scores_gemma":[0.9989998,0.00012245208,0.00047772366,0.00011758644,0.00008559273,0.00019687318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033091658,0.0001150676,0.00038264284,0.00014443614,0.000057933234,0.000033425582,0.00013237486,0.000036053094,0.0002410855],"category_scores_gemma":[0.000044949356,0.00008646785,0.00003851583,0.00012963402,0.0001565435,0.0002092088,0.000018841245,0.00008591924,0.000003776176],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045428154,0.000050152143,0.1959464,0.00035040593,0.00011009484,0.000018901017,0.014148183,0.00018638247,0.7862693,0.0008795575,0.0006138584,0.0009724954],"study_design_scores_gemma":[0.0008073173,0.0017548959,0.6193458,0.00029831374,0.000109596665,0.000033797107,0.00046148358,0.00039445804,0.35923162,0.017277779,0.00010797949,0.00017699023],"about_ca_topic_score_codex":0.0005358436,"about_ca_topic_score_gemma":0.000059191978,"teacher_disagreement_score":0.4270377,"about_ca_system_score_codex":0.0000019409852,"about_ca_system_score_gemma":0.000041042287,"threshold_uncertainty_score":0.35260564},"labels":[],"label_agreement":null},{"id":"W1899041869","doi":"10.1002/mame.201400122","title":"Characterization of Viscoelasticity and Self‐Healing Ability of VHB 4910","year":2014,"lang":"en","type":"article","venue":"Macromolecular Materials and Engineering","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Viscoelasticity; Materials science; Hydrogen bond; Fourier transform infrared spectroscopy; Composite material; Self-healing; Raman spectroscopy; Covalent bond; Ultimate tensile strength; Shear modulus; Molecule; Chemical engineering; Optics","score_opus":0.0026026257957439776,"score_gpt":0.15688760271809482,"score_spread":0.15428497692235085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1899041869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99662894,0.000032441523,0.0028836066,0.000008121183,0.00021213797,0.00008279999,0.000106102234,0.000019950698,0.000025874393],"genre_scores_gemma":[0.9989405,0.000039079303,0.0009107557,0.00000624323,0.000052007505,7.2728545e-7,0.000045299766,0.0000044942612,8.6271893e-7],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99938875,0.000038121318,0.00023123636,0.00013668336,0.00008048095,0.0001247467],"domain_scores_gemma":[0.9997256,0.000028353748,0.000080051286,0.000095358424,0.000023571456,0.00004707201],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002933522,0.00009685217,0.000251857,0.00003139963,0.000026859523,0.000034620123,0.000047416554,0.0000436096,0.00008205644],"category_scores_gemma":[0.000026229334,0.00008663563,0.000013676173,0.000041088835,0.000024670757,0.00006605653,0.000018523975,0.000019910542,0.0000011592645],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008826926,0.000006887301,0.00079429685,0.00039740276,0.000012049199,6.2370844e-7,0.00008344344,0.00038018607,0.9977277,0.00026338146,1.7421902e-7,0.00032505346],"study_design_scores_gemma":[0.00014666148,0.000071495626,0.25771484,0.00005125008,0.000024475032,0.0000035630583,0.0000023699736,0.0041965484,0.7374125,0.000107929336,0.00015647427,0.000111914334],"about_ca_topic_score_codex":0.00028789893,"about_ca_topic_score_gemma":0.0000035078624,"teacher_disagreement_score":0.26031518,"about_ca_system_score_codex":6.7904296e-7,"about_ca_system_score_gemma":0.0000044129456,"threshold_uncertainty_score":0.35328984},"labels":[],"label_agreement":null},{"id":"W1900738386","doi":"10.1139/v11-130","title":"Theoretical study on chemical bond parameters and properties of LnAl<sub>3</sub>(BO<sub>3</sub>)<sub>4</sub>","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Chemistry; Chemical bond; Ionic bonding; Crystallography; Computational chemistry; Bond length; Physical chemistry; Thermodynamics; Crystal structure; Ion; Organic chemistry","score_opus":0.015138869611292393,"score_gpt":0.17384509644136653,"score_spread":0.15870622683007413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1900738386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978613,0.00037214204,0.000002473199,0.000106343585,0.00029856226,0.00018117494,0.00014400051,0.000009513107,0.0010244597],"genre_scores_gemma":[0.99951094,0.000053142376,0.000037538848,0.00010142201,0.00025884245,0.0000023196133,0.000014768807,0.000017922968,0.000003089679],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9979032,0.00008380213,0.0006623421,0.00034599335,0.0004091671,0.0005954671],"domain_scores_gemma":[0.99800694,0.000087479086,0.00035691328,0.0003151254,0.00017007394,0.0010634864],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00051871076,0.00033695946,0.0006045293,0.00009653678,0.00014111778,0.00011794506,0.00043953804,0.0002056959,0.00014306439],"category_scores_gemma":[0.00017493874,0.00027098996,0.00014936735,0.0001463561,0.00066649937,0.000188546,0.000022788841,0.0004232429,0.000023487562],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021466667,0.000070104914,0.004803584,0.000110967805,0.00013967286,0.00021596265,0.000950588,0.00001699415,0.9901951,0.000047388625,0.00044057454,0.002794408],"study_design_scores_gemma":[0.000558326,0.00029561837,0.00950474,0.00017754792,0.00011225689,0.00012812261,0.00040298238,0.000019173398,0.98742765,0.0010017939,0.000051605246,0.00032020314],"about_ca_topic_score_codex":0.00060664787,"about_ca_topic_score_gemma":0.0007339791,"teacher_disagreement_score":0.0047011566,"about_ca_system_score_codex":0.00002226267,"about_ca_system_score_gemma":0.0005688755,"threshold_uncertainty_score":0.99997425},"labels":[],"label_agreement":null},{"id":"W1924944938","doi":"10.1002/2014tc003669","title":"Lithospheric discontinuity structure in Alaska, thickness variations determined by<i>Sp</i>receiver functions","year":2015,"lang":"en","type":"article","venue":"Tectonics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Geology; Seismology; Induced seismicity; Discontinuity (linguistics); Tectonics; Volcano; Context (archaeology); Geomorphology; Paleontology","score_opus":0.010476297194192212,"score_gpt":0.2070730457679338,"score_spread":0.1965967485737416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1924944938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99451333,0.0002595165,0.0006315916,0.0001752431,0.0011087947,0.00020422156,0.00075025304,0.000073236064,0.0022838141],"genre_scores_gemma":[0.9977866,0.000011906464,0.0008319757,0.0000912565,0.00010820625,0.0000030341,0.00027297364,0.000005879987,0.00088819733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895394,0.0000922172,0.00021198735,0.00025066448,0.00020452148,0.00028665675],"domain_scores_gemma":[0.99940443,0.000069128575,0.000083719235,0.00025301866,0.00005672393,0.00013296443],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002221034,0.00014901203,0.00020895632,0.000031200416,0.00009971475,0.00010206242,0.0002060352,0.00010167022,0.0013608021],"category_scores_gemma":[0.00006209889,0.00012261493,0.00003540373,0.00029994888,0.00004524353,0.00025729294,0.000021576549,0.00014924338,0.00015961299],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042265927,0.00039142455,0.81314886,0.00014254071,0.00022853437,0.000084061016,0.009239122,0.03541318,0.01433404,0.001248757,0.048098113,0.07724872],"study_design_scores_gemma":[0.0018398713,0.00026037538,0.87378097,0.000037315116,0.000106247244,0.000022343847,0.00030904554,0.011470206,0.0011092311,0.009547885,0.10064309,0.00087342795],"about_ca_topic_score_codex":0.0035052877,"about_ca_topic_score_gemma":0.007985519,"teacher_disagreement_score":0.07637529,"about_ca_system_score_codex":0.0000093890485,"about_ca_system_score_gemma":0.00011461219,"threshold_uncertainty_score":0.9995521},"labels":[],"label_agreement":null},{"id":"W1930176674","doi":"10.1002/2015jb012209","title":"Magnitude and symmetry of seismic anisotropy in mica‐ and amphibole‐bearing metamorphic rocks and implications for tectonic interpretation of seismic data from the southeast Tibetan Plateau","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"Centre of Excellence for Core to Crust Fluid Systems, Australian Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Schist; Geology; Amphibole; Metamorphic rock; Mica; Gneiss; Muscovite; Crenulation; Geochemistry; Petrology; Seismology; Quartz; Tectonics; Shear zone","score_opus":0.07223117621662183,"score_gpt":0.3364663469106367,"score_spread":0.26423517069401486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930176674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968566,0.00084990537,0.0006349668,0.0005480844,0.000049176935,0.00023387413,0.0007933372,0.0000024298288,0.00003167029],"genre_scores_gemma":[0.99887925,0.00024401656,0.0006482669,0.000019971496,0.00013106552,0.0000012467974,0.00006003144,0.00000559981,0.000010524805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851495,0.00024104922,0.00042413268,0.00021812525,0.00034684967,0.00025490558],"domain_scores_gemma":[0.99811167,0.00094064797,0.000240062,0.00027349676,0.00026016732,0.00017393852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012463225,0.00010977368,0.00040818698,0.00013391176,0.00008833357,0.00008602095,0.00036214272,0.000042134834,0.00000838113],"category_scores_gemma":[0.00037223866,0.000073851115,0.00003785495,0.00020782635,0.00026837483,0.00032972865,0.00014186132,0.00027391972,0.0000022170818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0076215216,0.000918327,0.48605672,0.0011116469,0.0016679312,0.000039581115,0.01111879,0.013033215,0.28669745,0.002369364,0.0013845067,0.18798093],"study_design_scores_gemma":[0.0012537075,0.0006769983,0.8483823,0.00018716784,0.000093666866,0.000018737153,0.0006796011,0.12044029,0.0016025669,0.02624394,0.00028888893,0.00013212657],"about_ca_topic_score_codex":0.004630876,"about_ca_topic_score_gemma":0.00063816993,"teacher_disagreement_score":0.36232558,"about_ca_system_score_codex":0.000003333669,"about_ca_system_score_gemma":0.00015220701,"threshold_uncertainty_score":0.700053},"labels":[],"label_agreement":null},{"id":"W1930767292","doi":"10.1139/cjes-2013-0115","title":"Plume–plate interaction","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Plume; Geology; Plate tectonics; Mantle plume; Panache; Hotspot (geology); Geophysics; Meteorology; Paleontology; Geography; Lithosphere; Tectonics","score_opus":0.015486874880743242,"score_gpt":0.2080923402778804,"score_spread":0.19260546539713716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930767292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98023087,0.00013109847,0.00010478667,0.000386113,0.002415798,0.000029337574,0.00002211294,0.0000033799452,0.016676534],"genre_scores_gemma":[0.99874586,0.0000078880885,0.00052117556,0.00019213904,0.00037313186,3.988363e-8,0.0000019552353,0.0000011135783,0.00015670455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999196,0.00006189488,0.00020589009,0.00009597515,0.00018025361,0.00025999523],"domain_scores_gemma":[0.9992389,0.00006600398,0.00016322204,0.00006381284,0.00006741683,0.00040061702],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008324875,0.000066545355,0.00013193098,0.00017794505,0.0002674469,0.00023992741,0.0002804082,0.000027257847,0.0027047738],"category_scores_gemma":[0.000087951485,0.000048493108,0.000044197917,0.00018072309,0.00017166874,0.00048041748,0.000002101993,0.00008123159,0.00013841817],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052482952,0.000016033382,0.8267945,0.00004302849,0.00007894182,0.00017489861,0.0023786742,0.05449405,0.0023101743,0.006877519,0.0063789207,0.10040079],"study_design_scores_gemma":[0.00023193556,0.00063242484,0.6255617,0.000073342846,0.000019704725,0.0001636988,0.00023539412,0.003666687,0.0011284754,0.004688795,0.36336648,0.0002313434],"about_ca_topic_score_codex":0.018373815,"about_ca_topic_score_gemma":0.18874167,"teacher_disagreement_score":0.35698757,"about_ca_system_score_codex":5.656228e-7,"about_ca_system_score_gemma":0.000374007,"threshold_uncertainty_score":0.9982069},"labels":[],"label_agreement":null},{"id":"W1930906939","doi":"10.1103/physrevb.92.085137","title":"Dynamical and anharmonic effects on the electron-phonon coupling and the zero-point renormalization of the electronic structure","year":2015,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada","keywords":"Anharmonicity; Renormalization; Physics; Zero-point energy; Coupling (piping); Condensed matter physics; Zero (linguistics); Phonon; Quantum mechanics; Electron; Electronic structure; Point (geometry); Quantum electrodynamics; Materials science","score_opus":0.005995070638745082,"score_gpt":0.21936402814955855,"score_spread":0.21336895751081347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930906939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9836064,0.014096526,0.000027976921,0.0015228563,0.00008293821,0.0005219445,0.000012301577,0.000006950765,0.00012209656],"genre_scores_gemma":[0.9955847,0.0037365395,0.0000028136274,0.00055807905,0.0000930225,0.0000038032285,0.000011564329,0.0000032696933,0.0000061787205],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99915004,0.00019458492,0.00013085967,0.00014345054,0.0001955813,0.0001854606],"domain_scores_gemma":[0.9992603,0.0003574495,0.000105612635,0.0002050271,0.00002816102,0.00004342984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042943453,0.0001114907,0.00025284907,0.000005314937,0.000102809594,0.00003299848,0.00016706201,0.000018762106,0.0000129736645],"category_scores_gemma":[0.00013017813,0.000042436244,0.000047467245,0.00012001366,0.000121171615,0.000052506304,0.000027086306,0.00014871098,0.0000058273663],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012816055,0.0002198975,0.008285142,0.0067062564,0.00068852736,0.000004751545,0.0027747944,0.006839722,0.039606128,0.85505474,0.0073495866,0.07118888],"study_design_scores_gemma":[0.0036545158,0.0017842848,0.09996548,0.0031117518,0.0013176574,0.00003317956,0.000038839295,0.1563584,0.049861453,0.66760665,0.015259709,0.0010080823],"about_ca_topic_score_codex":0.00013199299,"about_ca_topic_score_gemma":0.000040115887,"teacher_disagreement_score":0.18744807,"about_ca_system_score_codex":0.0000037347752,"about_ca_system_score_gemma":0.000037116442,"threshold_uncertainty_score":0.17304999},"labels":[],"label_agreement":null},{"id":"W193616070","doi":"","title":"A new density model of the upper mantle of North America","year":2010,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismic tomography; Mantle (geology); Gravity anomaly; Crust; Geothermal gradient; Transition zone; Geophysics; Seismology; Residual; Paleontology; Oil field","score_opus":0.031973575581142846,"score_gpt":0.29281525872718805,"score_spread":0.2608416831460452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W193616070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9844943,0.00001587825,0.0016353786,0.002860604,0.00040182317,0.000748567,0.009209952,0.000019077706,0.00061440887],"genre_scores_gemma":[0.99068594,0.000025127934,0.005858327,0.00009554767,0.0001292907,0.000007042642,0.0016277739,0.0000048609286,0.0015660787],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99761486,0.000113578244,0.00033278787,0.00040255825,0.0010018985,0.0005343419],"domain_scores_gemma":[0.9976998,0.0002501193,0.00022801662,0.0008748344,0.0006865997,0.00026065306],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012789454,0.000114204864,0.00018791156,0.00016816736,0.00035971246,0.000111328874,0.0012733563,0.000041800806,0.0010702201],"category_scores_gemma":[0.00066274253,0.00007709909,0.000082258135,0.0008871356,0.00048647536,0.0005925655,0.00017732251,0.00020131827,0.00006050221],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030352362,0.0005579902,0.46942577,0.0005018811,0.00007623555,0.0000013832713,0.0023137503,0.0016810372,0.060092617,0.022179184,0.3313152,0.11155143],"study_design_scores_gemma":[0.0006070967,0.00009986164,0.6123004,0.000032326556,0.000033138625,0.0000028055988,0.0001114287,0.1216023,0.02283824,0.00412084,0.23789412,0.00035743887],"about_ca_topic_score_codex":0.010137582,"about_ca_topic_score_gemma":0.011819168,"teacher_disagreement_score":0.14287464,"about_ca_system_score_codex":0.0000038529606,"about_ca_system_score_gemma":0.0005765449,"threshold_uncertainty_score":0.99984294},"labels":[],"label_agreement":null},{"id":"W1936698890","doi":"10.1002/jgrb.50352","title":"A new calibration of seismic velocities, anisotropy, fabrics, and elastic moduli of amphibole‐rich rocks","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Amphibole; Geology; Peridotite; Mafic; Gneiss; Gabbro; Plagioclase; Petrology; Geochemistry; Mineralogy; Igneous rock; Basalt; Quartz; Metamorphic rock","score_opus":0.020930141843029097,"score_gpt":0.26859670691990023,"score_spread":0.24766656507687113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1936698890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949588,0.00022983448,0.0038972327,0.00025132793,0.00016987632,0.0001830465,0.000053735315,0.000004823731,0.00025132467],"genre_scores_gemma":[0.99773896,0.00019474195,0.0011160552,0.000020811545,0.00047226803,5.822987e-7,0.0000112865255,0.0000063236457,0.00043898093],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9976412,0.00023646864,0.0005682615,0.00016571647,0.0009903592,0.00039801284],"domain_scores_gemma":[0.9981316,0.00044492178,0.00033237058,0.00016998537,0.0005798648,0.00034125778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004959483,0.0001370906,0.00051896996,0.00019664943,0.00009579762,0.000102410835,0.00028143337,0.000067281566,0.00063399074],"category_scores_gemma":[0.00022815535,0.000102750295,0.00009167515,0.00034828985,0.00020631605,0.000537452,0.000054111275,0.00031166727,0.00004167596],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002637417,0.0012736253,0.06525523,0.0021479041,0.001450246,0.00018643541,0.0074428828,0.06722381,0.5624733,0.0060300026,0.041289296,0.24258985],"study_design_scores_gemma":[0.0022386925,0.0052952836,0.74123174,0.0004243614,0.000106402294,0.000049681094,0.0006723631,0.1209904,0.05464102,0.07147552,0.002350684,0.00052383565],"about_ca_topic_score_codex":0.010676478,"about_ca_topic_score_gemma":0.000110259505,"teacher_disagreement_score":0.6759765,"about_ca_system_score_codex":0.0000039789247,"about_ca_system_score_gemma":0.00035453378,"threshold_uncertainty_score":0.99591154},"labels":[],"label_agreement":null},{"id":"W1938698763","doi":"10.1029/2008gc002042","title":"Scaling relationships for chemical lid convection with applications to cratonal lithosphere","year":2008,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Lithosphere; Mantle convection; Craton; Convection; Geophysics; Mantle (geology); Convective heat transfer; Petrology; Scaling; Boundary layer; Combined forced and natural convection; Natural convection; Mechanics; Tectonics; Geometry; Seismology; Physics","score_opus":0.02043901106899202,"score_gpt":0.20951856262083413,"score_spread":0.1890795515518421,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1938698763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98556674,0.00010155026,0.009493909,0.00010662559,0.00021552802,0.00090710615,0.00066388486,0.0001344017,0.0028102724],"genre_scores_gemma":[0.9942743,0.0000049811383,0.0026253737,0.000045081702,0.0011948812,0.00016788216,0.000966128,0.000013757515,0.00070760184],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99843156,0.000031747244,0.0003268963,0.00049422745,0.00030470162,0.0004108598],"domain_scores_gemma":[0.9987622,0.00021312869,0.00015590887,0.0003817411,0.00023948199,0.00024757578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019039735,0.00024170557,0.00031041075,0.000021013982,0.00053638284,0.000079772486,0.00023471989,0.0001381214,0.00014877746],"category_scores_gemma":[0.000033129185,0.00021776283,0.00008632674,0.00030040924,0.0000706715,0.00014405003,0.000017203241,0.00016087588,0.00027389513],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023501825,0.0011458434,0.1933371,0.0054029753,0.0013512652,0.00010363539,0.0064712195,0.058638874,0.674288,0.008151311,0.026474632,0.022285014],"study_design_scores_gemma":[0.0059386273,0.00091106805,0.08230814,0.0008854699,0.0006338262,0.0008017643,0.002460217,0.024164638,0.55156964,0.016063523,0.3082402,0.006022916],"about_ca_topic_score_codex":0.0006155983,"about_ca_topic_score_gemma":0.000050982235,"teacher_disagreement_score":0.28176555,"about_ca_system_score_codex":0.000011076985,"about_ca_system_score_gemma":0.00012426681,"threshold_uncertainty_score":0.8880111},"labels":[],"label_agreement":null},{"id":"W1941054767","doi":"10.1103/physrevb.93.014306","title":"Light atom quantum oscillations in UC and US","year":2016,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Nuclear Laboratories","funders":"Basic Energy Sciences; Sociedad Española de Nefrología; Office of Experimental Program to Stimulate Competitive Research; U.S. Department of Energy","keywords":"Anharmonicity; Physics; Atomic physics; Scattering; Atom (system on chip); Hydrogen atom; Harmonic oscillator; Inelastic scattering; Inelastic neutron scattering; Quantum; Condensed matter physics; Optics; Quantum mechanics","score_opus":0.014358702089221997,"score_gpt":0.3068284477311522,"score_spread":0.2924697456419302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1941054767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.933614,0.052250564,0.0002688459,0.008357051,0.0003203805,0.0012693852,0.00020333356,0.00008584484,0.0036305836],"genre_scores_gemma":[0.8731639,0.1241973,0.000050111717,0.0018597727,0.00057948165,0.000031169096,0.000036260986,0.000015295664,0.00006670564],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9971649,0.00035739888,0.00062006473,0.000712301,0.00053306157,0.0006122636],"domain_scores_gemma":[0.9981212,0.0005731875,0.0002497082,0.0005999595,0.000090063004,0.000365858],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047506092,0.00042324915,0.0013402557,0.000049919,0.00012266323,0.000054653214,0.0003873653,0.000043642965,0.00044590476],"category_scores_gemma":[0.0003167413,0.0002481844,0.0003059844,0.0005572564,0.00012389098,0.0004307208,0.00007834207,0.00019366978,0.0021660144],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000081689745,0.0009991181,0.047376897,0.01289663,0.0001950293,0.000087947694,0.00023012758,0.00001836525,0.046837892,0.581634,0.026014987,0.28362736],"study_design_scores_gemma":[0.0007579414,0.0003761544,0.1498616,0.017007241,0.00043905078,0.000012352872,0.000003492567,0.0020358737,0.001658869,0.19541647,0.6311195,0.0013114917],"about_ca_topic_score_codex":0.00025106376,"about_ca_topic_score_gemma":0.00010565242,"teacher_disagreement_score":0.6051045,"about_ca_system_score_codex":0.000010978211,"about_ca_system_score_gemma":0.00006300329,"threshold_uncertainty_score":0.999997},"labels":[],"label_agreement":null},{"id":"W1943639071","doi":"10.1002/2015gc006061","title":"Torsion of a cylinder of partially molten rock with a spherical inclusion: Theory and simulation","year":2015,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Environment Research Council; Sight Research UK; Leverhulme Trust","keywords":"Torsion (gastropod); Inclusion (mineral); Mechanics; Porosity; Geology; Viscosity; Deformation (meteorology); Mantle (geology); Materials science; Mineralogy; Geotechnical engineering; Composite material; Physics; Geophysics","score_opus":0.010720633411801087,"score_gpt":0.2144990813171059,"score_spread":0.2037784479053048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1943639071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963573,0.00026312147,0.0010890175,0.000013939782,0.00012557172,0.00017628729,0.00012526948,0.000020478641,0.0018289943],"genre_scores_gemma":[0.9993187,0.000004370323,0.00020860844,0.000010673242,0.0002189896,0.0000020006944,0.00011462509,0.000005968579,0.00011605072],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99864954,0.00010394831,0.00034126663,0.00025511338,0.0004416928,0.00020846646],"domain_scores_gemma":[0.9988925,0.00014362895,0.00030334652,0.00027739612,0.00022952314,0.00015359887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045456077,0.00017244768,0.00038561938,0.000015873313,0.00008402687,0.000020833657,0.00016023935,0.000099840254,0.00009895364],"category_scores_gemma":[0.000042791864,0.00013066939,0.000043571654,0.00015276071,0.00006516242,0.00012705424,0.000103428116,0.00006822106,0.000010862813],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033194823,0.00036860874,0.05423464,0.0021273703,0.00037293078,0.000040803647,0.006070466,0.8031094,0.12428618,0.00086547656,0.0002580537,0.0049465625],"study_design_scores_gemma":[0.008480746,0.0032865906,0.06522575,0.0014960057,0.0007699376,0.000082174076,0.004176619,0.5203225,0.3304893,0.056874115,0.0060476763,0.0027486149],"about_ca_topic_score_codex":0.0012683778,"about_ca_topic_score_gemma":0.000041845426,"teacher_disagreement_score":0.28278697,"about_ca_system_score_codex":0.0000035869134,"about_ca_system_score_gemma":0.000107634994,"threshold_uncertainty_score":0.5328543},"labels":[],"label_agreement":null},{"id":"W1949554075","doi":"10.1002/2015gl065018","title":"Mantle‐driven uplift of Hangai Dome: New seismic constraints from adjoint tomography","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Upwelling; Mantle (geology); Seismic tomography; Lithosphere; Seismology; Geophysics; Mantle wedge; Partial melting; Crust; Petrology; Tectonics","score_opus":0.04950039734614027,"score_gpt":0.28427260187511155,"score_spread":0.2347722045289713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1949554075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934057,0.00011249813,0.00026387174,0.0023394744,0.00047756018,0.00031739718,0.00051943125,0.00004207683,0.0025219952],"genre_scores_gemma":[0.99746674,0.000014765172,0.0008170749,0.00047439628,0.00080933684,0.0000035467413,0.00022933759,0.0000097787315,0.00017504355],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9969077,0.00032004385,0.0003176794,0.00047263436,0.0012093462,0.0007725717],"domain_scores_gemma":[0.99818504,0.00044056505,0.0000923207,0.00046099236,0.00015479645,0.00066626805],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000517268,0.0002037831,0.00042016988,0.0001897638,0.00010759947,0.00012272412,0.00058674865,0.00008353888,0.0012928024],"category_scores_gemma":[0.00013229832,0.00016878442,0.00015114342,0.0004992112,0.0007182327,0.0002282,0.00009512944,0.00034880795,0.0017661278],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013236135,0.0004674008,0.041376244,0.00019301743,0.0007578184,0.00055243046,0.0036003313,0.006194031,0.39243227,0.00322095,0.4803903,0.069491595],"study_design_scores_gemma":[0.007408491,0.0022106671,0.71845627,0.00051775225,0.00018958075,0.000013513898,0.00124668,0.010418119,0.05298469,0.10042107,0.103901386,0.0022318033],"about_ca_topic_score_codex":0.03073088,"about_ca_topic_score_gemma":0.00026609655,"teacher_disagreement_score":0.67708004,"about_ca_system_score_codex":0.000007976134,"about_ca_system_score_gemma":0.00021198326,"threshold_uncertainty_score":0.99962014},"labels":[],"label_agreement":null},{"id":"W1950837150","doi":"10.1002/2015gc005937","title":"Variations of the lithospheric strength and elastic thickness in <scp>N</scp>orth <scp>A</scp>merica","year":2015,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; U.S. Geological Survey; Alexander von Humboldt-Stiftung","keywords":"Lithosphere; Craton; Geology; Crust; Mantle (geology); Proterozoic; Lithospheric flexure; Rift; Geophysics; Petrology; Seismic tomography; Seismology; Tectonics","score_opus":0.00933151974174019,"score_gpt":0.19302456366270926,"score_spread":0.18369304392096908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1950837150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841577,0.00094570196,0.000079815414,0.000024365634,0.0010359561,0.00035211706,0.0005491401,0.000048498187,0.012806701],"genre_scores_gemma":[0.9975719,0.000040542727,0.00017761704,0.000036132624,0.00046275932,0.000017318887,0.00018863336,0.0000143370025,0.0014908003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99760383,0.00016934374,0.0005728696,0.0005112074,0.0005787729,0.00056395924],"domain_scores_gemma":[0.99755806,0.000810325,0.0004856741,0.0006536723,0.00022910425,0.00026316202],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00041893517,0.0003558206,0.00056487275,0.00003437387,0.00016122607,0.00013868537,0.00055162585,0.00019409646,0.000023556477],"category_scores_gemma":[0.00058993296,0.00027893475,0.000103244405,0.0006737556,0.00016408929,0.0002107563,0.0001154171,0.00027105774,0.00006157068],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006535001,0.0020137294,0.8211292,0.0067206305,0.0008520878,0.00010750481,0.023572953,0.03884926,0.061392047,0.0059845094,0.025492778,0.013819928],"study_design_scores_gemma":[0.0045608203,0.0006147305,0.76753443,0.0015075782,0.00071666104,0.00017281767,0.019091057,0.029792987,0.02811328,0.031496257,0.1153379,0.0010614683],"about_ca_topic_score_codex":0.0063325823,"about_ca_topic_score_gemma":0.00035056987,"teacher_disagreement_score":0.08984513,"about_ca_system_score_codex":0.000011118319,"about_ca_system_score_gemma":0.0004220948,"threshold_uncertainty_score":0.99996626},"labels":[],"label_agreement":null},{"id":"W1952808813","doi":"10.1002/2013jb010661","title":"Antigorite‐induced seismic anisotropy and implications for deformation in subduction zones and the Tibetan Plateau","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"China Geological Survey; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Shear wave splitting; Slab; Lithosphere; Seismic anisotropy; Trench; Seismology; Anisotropy; Mantle (geology); Shear (geology); Petrology; Crust; Mantle wedge; Geophysics; Tectonics","score_opus":0.03164634874895272,"score_gpt":0.3132510682928685,"score_spread":0.28160471954391575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1952808813","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963754,0.000080818856,0.00073112076,0.0023156065,0.0001280907,0.00025623298,0.000020193333,0.0000039073834,0.00008864781],"genre_scores_gemma":[0.9988139,0.00024424843,0.0003785712,0.000038180282,0.0004748139,0.000002529234,0.000010069897,0.000003315217,0.00003436532],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987425,0.00028874844,0.0002990566,0.0001239722,0.00026547108,0.00028020795],"domain_scores_gemma":[0.99855703,0.0008538304,0.00013785562,0.00011499362,0.00021858823,0.00011771151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019308111,0.000083637584,0.0002647751,0.00012418516,0.00026714453,0.00016382073,0.00013598084,0.0000474913,0.000010567391],"category_scores_gemma":[0.00030907203,0.00005079706,0.000047086713,0.00018683317,0.00017876769,0.00039103176,0.000020113215,0.00023272526,0.000010317189],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0073089083,0.00058621546,0.061635833,0.0007987715,0.00041549894,0.000015131137,0.0077856104,0.008037465,0.12798154,0.18220232,0.0016723034,0.6015604],"study_design_scores_gemma":[0.002109354,0.00091131934,0.82929945,0.000048140686,0.000022921411,0.000029978552,0.00017151689,0.045223806,0.0013770272,0.118541755,0.0021340912,0.0001306505],"about_ca_topic_score_codex":0.0008580616,"about_ca_topic_score_gemma":0.00017937332,"teacher_disagreement_score":0.7676636,"about_ca_system_score_codex":0.0000029954815,"about_ca_system_score_gemma":0.000050444924,"threshold_uncertainty_score":0.2071444},"labels":[],"label_agreement":null},{"id":"W1953499253","doi":"10.1029/2011jb008692","title":"Geodynamic models of mature continental collision: Evolution of an orogen from lithospheric subduction to continental retreat/delamination","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lithosphere; Subduction; Collision zone; Crust; Mantle (geology); Continental collision; Eclogitization; Crustal recycling; Continental crust; Geophysics; Convergent boundary; Delamination (geology); Seismology; Oceanic crust; Petrology; Tectonics","score_opus":0.019030902965546426,"score_gpt":0.2788301857286024,"score_spread":0.25979928276305597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1953499253","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99721456,0.00085548277,0.0005350173,0.00008936639,0.00051528885,0.00026374197,0.00024513813,0.000007937923,0.0002734732],"genre_scores_gemma":[0.99517506,0.00005502385,0.0037069973,0.0000056454237,0.00084752275,0.0000015399536,0.000069787886,0.000010079413,0.00012832045],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9969634,0.00041836454,0.0006436017,0.00020513067,0.0013118717,0.00045763756],"domain_scores_gemma":[0.99783164,0.0002957429,0.00044728778,0.0002495304,0.0008125091,0.00036325975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010578904,0.00017027852,0.00051976944,0.00004103439,0.000112237845,0.000054850134,0.00038149077,0.00013023218,0.00049244834],"category_scores_gemma":[0.00018236389,0.00013083318,0.00015895377,0.00053753855,0.0001633236,0.0011744777,0.000050318504,0.0002963722,0.000034436718],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.012301753,0.004140166,0.22057992,0.00041852065,0.00094717374,0.00008647431,0.0055711665,0.034574736,0.64440495,0.00923698,0.004485726,0.06325246],"study_design_scores_gemma":[0.0009982738,0.0022321374,0.942281,0.00019219836,0.000082945655,0.000017292023,0.0014430892,0.018020157,0.024615902,0.009468697,0.0004101393,0.00023816574],"about_ca_topic_score_codex":0.014261814,"about_ca_topic_score_gemma":0.00048630446,"teacher_disagreement_score":0.7217011,"about_ca_system_score_codex":0.000041356117,"about_ca_system_score_gemma":0.00013264272,"threshold_uncertainty_score":0.9923023},"labels":[],"label_agreement":null},{"id":"W1955979307","doi":"10.1029/2007gc001834","title":"Integrated geophysical‐petrological modeling of the lithosphere and sublithospheric upper mantle: Methodology and applications","year":2008,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":289,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; European Social Fund; Macquarie University","keywords":"Geology; Lithosphere; Geophysics; Mantle (geology); Observable; Seismology; Tectonics; Physics","score_opus":0.024704310212993096,"score_gpt":0.21133865874961077,"score_spread":0.18663434853661767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1955979307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99504846,0.0010557099,0.0014826728,0.00006641835,0.00016932999,0.00033325065,0.00024415905,0.000046080597,0.0015539251],"genre_scores_gemma":[0.9978067,0.00015367797,0.0012034649,0.000040941883,0.00029732348,0.000022689135,0.00009096942,0.000008851995,0.00037536034],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982883,0.00017660102,0.00041073005,0.0004928755,0.00025519644,0.00037634769],"domain_scores_gemma":[0.998799,0.00022197625,0.00021710101,0.00048082907,0.00014390735,0.00013717543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027382528,0.0002747193,0.0005306357,0.000012984637,0.00032432762,0.00004245183,0.0003294668,0.00018151525,0.00014014683],"category_scores_gemma":[0.000041626623,0.00018731997,0.00009991431,0.0003056675,0.00034554224,0.000111990696,0.000096528696,0.00023331412,0.000017944822],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066022197,0.0007910444,0.6801948,0.004268492,0.0011605894,0.00007707853,0.0034556885,0.020293085,0.22642437,0.013227873,0.0012838001,0.048162967],"study_design_scores_gemma":[0.0030894103,0.0005649761,0.539847,0.00042786868,0.00066214707,0.0008334875,0.0025772161,0.34180853,0.027805245,0.058737468,0.020572232,0.003074382],"about_ca_topic_score_codex":0.0043582674,"about_ca_topic_score_gemma":0.00004648239,"teacher_disagreement_score":0.32151544,"about_ca_system_score_codex":0.0000038291982,"about_ca_system_score_gemma":0.00007277117,"threshold_uncertainty_score":0.76386863},"labels":[],"label_agreement":null},{"id":"W1958905693","doi":"10.1002/2013jb010484","title":"The impact of Rayleigh number on assessing the significance of supercontinent insulation","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Government of Ontario; Compute Canada","keywords":"Mantle (geology); Subduction; Geology; Hotspot (geology); Supercontinent; Mantle convection; Geophysics; Continental margin; Earth science; Paleontology; Tectonics; Craton","score_opus":0.03483319028969537,"score_gpt":0.36566625384661283,"score_spread":0.33083306355691744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1958905693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974712,0.000031379554,0.000048612423,0.00029904852,0.00017032392,0.00014342701,0.000018167655,0.0000021635906,0.0018156908],"genre_scores_gemma":[0.99915963,0.000063727755,0.000053708725,0.000009069934,0.00059891527,6.0254115e-7,0.0000029069201,0.000004232335,0.000107209155],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9971281,0.00082046614,0.000484886,0.000112388814,0.0011017832,0.00035231948],"domain_scores_gemma":[0.9961888,0.002458233,0.00035113384,0.00027167308,0.00060774066,0.00012239357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030906075,0.000107299944,0.0003436865,0.000054892866,0.00026029,0.00014537232,0.00044750402,0.000042840784,0.00016426262],"category_scores_gemma":[0.00068506517,0.000047671456,0.00021863,0.00029175833,0.00032687996,0.00025173684,0.000026041693,0.00039155423,0.000046965597],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003102309,0.001289187,0.2550581,0.00027081158,0.0010279932,0.00003005478,0.0027481704,0.075757645,0.50542086,0.013280532,0.006111368,0.13590296],"study_design_scores_gemma":[0.0002771865,0.00089366006,0.9774167,0.000069334004,0.000011013879,0.000002708185,0.00006881156,0.0052393293,0.008496613,0.0063152765,0.0011468617,0.00006251751],"about_ca_topic_score_codex":0.0022718755,"about_ca_topic_score_gemma":0.00003299785,"teacher_disagreement_score":0.7223586,"about_ca_system_score_codex":0.0000048613074,"about_ca_system_score_gemma":0.00019182473,"threshold_uncertainty_score":0.34344113},"labels":[],"label_agreement":null},{"id":"W1959726294","doi":"10.1029/2010gl044366","title":"Formation of cratonic mantle keels by arc accretion: Evidence from S receiver functions","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Lithosphere; Craton; Classification of discontinuities; Mantle (geology); Asthenosphere; Plate tectonics; Geophysics; Tectonics; Accretion (finance); Seismology","score_opus":0.03426834005363012,"score_gpt":0.28260075100410753,"score_spread":0.24833241095047742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1959726294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99545896,0.00006459975,0.00038291918,0.0024137206,0.00049370545,0.00021688164,0.0003939738,0.000025823194,0.0005494368],"genre_scores_gemma":[0.99854743,0.000050844228,0.00020970393,0.00013912634,0.000468336,0.000007859629,0.00029943482,0.000004941174,0.0002723461],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99800175,0.00021825075,0.00023402448,0.00030286037,0.00079732726,0.00044580098],"domain_scores_gemma":[0.9984687,0.000756722,0.000076585915,0.00038318054,0.00015013185,0.00016471003],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00052870763,0.000119186894,0.00019594499,0.000078316734,0.00023522967,0.00011947041,0.000390071,0.00007397968,0.003112388],"category_scores_gemma":[0.00019932553,0.00009900654,0.00007487433,0.00031926093,0.00029110658,0.00071026356,0.000046047448,0.000444388,0.0018035887],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007634747,0.000028317165,0.0012847709,0.000022718721,0.000015424526,0.000003736663,0.00015258594,0.000055004955,0.9545082,0.00006632585,0.039520983,0.004265575],"study_design_scores_gemma":[0.0009799495,0.0006457509,0.5056513,0.0002872708,0.000073335264,0.000004152804,0.00021939557,0.0076671545,0.3855625,0.007430137,0.09065245,0.0008265935],"about_ca_topic_score_codex":0.008002496,"about_ca_topic_score_gemma":0.0004379578,"teacher_disagreement_score":0.5689457,"about_ca_system_score_codex":0.0000053104154,"about_ca_system_score_gemma":0.00005191971,"threshold_uncertainty_score":0.9989736},"labels":[],"label_agreement":null},{"id":"W1961184383","doi":"10.1002/2015gl063733","title":"Inverting interpolated receiver functions with surface wave dispersion and gravity: Application to the western U.S. and adjacent Canada and Mexico","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Laboratory Directed Research and Development; Northwestern University; National Science Foundation","keywords":"Receiver function; Geology; Interpolation (computer graphics); Geodesy; Smoothing; Azimuth; Dispersion (optics); Surface wave; Rayleigh wave; Seismology; Geophysics; Mathematical analysis; Geometry; Physics; Mathematics; Optics; Classical mechanics","score_opus":0.02568855382191007,"score_gpt":0.24262774911567467,"score_spread":0.2169391952937646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1961184383","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875905,0.000044369997,0.000121464414,0.011764027,0.00006749279,0.00029908255,0.00006047733,0.000010135098,0.000042455424],"genre_scores_gemma":[0.9989196,0.000013294228,0.00006205332,0.00079755153,0.00008304497,0.000004035333,0.0000314314,0.000004313251,0.00008468393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986844,0.00016701053,0.00009411816,0.0002986306,0.00043736186,0.00031844949],"domain_scores_gemma":[0.99923855,0.00017308332,0.000025988997,0.00016404733,0.000076350065,0.0003220083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003887461,0.000102933525,0.00013030924,0.000027879072,0.0002570537,0.00014745147,0.00009058328,0.000023086694,0.0000069892812],"category_scores_gemma":[0.00003842084,0.00006297175,0.0000075007874,0.00019291509,0.0001607936,0.00012727974,0.000080249694,0.00017709885,0.000021431622],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002716955,0.00012500388,0.6227295,0.00022787487,0.00032609442,0.00011035986,0.011274567,0.0055045504,0.09513874,0.00036166498,0.06311824,0.19836648],"study_design_scores_gemma":[0.0006810037,0.0005798792,0.93682396,0.00008011438,0.000033958622,0.000014865215,0.00073170656,0.014490839,0.00078466506,0.00027595498,0.045129556,0.00037348518],"about_ca_topic_score_codex":0.57881063,"about_ca_topic_score_gemma":0.34558305,"teacher_disagreement_score":0.3140945,"about_ca_system_score_codex":0.000013616617,"about_ca_system_score_gemma":0.000069583635,"threshold_uncertainty_score":0.66635835},"labels":[],"label_agreement":null},{"id":"W1963743614","doi":"10.1029/2011jb008294","title":"Grain-size distribution in the mantle wedge of subduction zones","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Mantle wedge; Geology; Mantle (geology); Subduction; Grain size; Hotspot (geology); Dislocation creep; Transition zone; Olivine; Slab; Creep; Geophysics; Mineralogy; Materials science; Seismology; Composite material; Geomorphology; Tectonics","score_opus":0.046814698223816315,"score_gpt":0.2881822686364277,"score_spread":0.2413675704126114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963743614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99682564,0.0002195959,0.000048417744,0.00020854294,0.0002891398,0.00012679436,0.000037374146,0.0000028439972,0.0022416376],"genre_scores_gemma":[0.9989672,0.00013885027,0.00030347207,0.0000129326945,0.00038709212,0.0000010151496,0.000007926298,0.0000028283487,0.00017869692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99790233,0.00049482525,0.00037913,0.00011493241,0.00078378274,0.0003250037],"domain_scores_gemma":[0.9986795,0.000582338,0.00018771454,0.00017357335,0.00028804716,0.00008878667],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016911427,0.00009059289,0.00024760386,0.000011673596,0.00010092156,0.000045357276,0.00045445748,0.000051267536,0.0010005987],"category_scores_gemma":[0.0003819704,0.000052647556,0.00010800871,0.00040514593,0.00023222594,0.0002701803,0.000022203758,0.00033127377,0.00009201631],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013408758,0.0065984195,0.42591277,0.0011060556,0.0008362165,0.0014756038,0.021781199,0.00074314204,0.058067266,0.077974156,0.17525002,0.21684639],"study_design_scores_gemma":[0.00033916233,0.00077096955,0.95697606,0.000050231796,0.000013341441,0.0000139464955,0.00068989577,0.00008584008,0.0030870927,0.033913963,0.0039837286,0.000075786564],"about_ca_topic_score_codex":0.00663518,"about_ca_topic_score_gemma":0.0006444318,"teacher_disagreement_score":0.53106326,"about_ca_system_score_codex":0.0000061314477,"about_ca_system_score_gemma":0.000089231646,"threshold_uncertainty_score":0.99997973},"labels":[],"label_agreement":null},{"id":"W1963798614","doi":"10.1021/jp5036713","title":"A Density Functional Tight Binding Model with an Extended Basis Set and Three-Body Repulsion for Hydrogen under Extreme Thermodynamic Conditions","year":2014,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry A","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University","funders":"Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"Tight binding; Basis set; Density functional theory; Chemistry; Range (aeronautics); Statistical physics; Thermodynamics; Computational chemistry; Electronic structure; Physics; Materials science","score_opus":0.021125105342188606,"score_gpt":0.22464282583261583,"score_spread":0.2035177204904272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963798614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911662,0.000009335149,0.008332464,0.00012528608,0.000016098964,0.00006597197,0.00010453025,0.0000074099516,0.00017273621],"genre_scores_gemma":[0.9993797,0.000002323853,0.00012690172,0.000035954246,0.0003282372,7.809574e-7,0.000066567154,0.0000046753357,0.00005483855],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993736,0.000040353334,0.00013809213,0.00011308991,0.000196189,0.0001386421],"domain_scores_gemma":[0.99936616,0.00015482618,0.00017028398,0.00013329941,0.00007350973,0.000101934114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027955003,0.00010794184,0.00018088077,0.000011251425,0.00021127902,0.00003514365,0.00012286707,0.000033510256,0.00008382001],"category_scores_gemma":[0.000011545599,0.000060477454,0.000055667075,0.00004363994,0.00008847386,0.00016502917,0.000010133424,0.0001012405,0.000002498939],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047686804,0.00006401788,0.00014740892,0.00003380799,0.00008433826,0.0000015029946,0.000105727566,0.054395575,0.9441373,0.00019905578,0.00007472851,0.00027966342],"study_design_scores_gemma":[0.0006984228,0.00031406689,0.016544417,0.00004045122,0.00023752374,0.00008298483,0.00005828538,0.8897395,0.052588187,0.03949445,0.000024743174,0.00017697968],"about_ca_topic_score_codex":0.000025220603,"about_ca_topic_score_gemma":0.0000210772,"teacher_disagreement_score":0.8915491,"about_ca_system_score_codex":0.0000039015536,"about_ca_system_score_gemma":0.000035175377,"threshold_uncertainty_score":0.2466199},"labels":[],"label_agreement":null},{"id":"W1964076309","doi":"10.1063/1.4704698","title":"Temperature dependent elastic constants for crystals with arbitrary symmetry: Combined first principles and continuum elasticity theory","year":2012,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Wilfrid Laurier University","funders":"National Natural Science Foundation of China","keywords":"Elasticity (physics); Gibbs free energy; Anisotropy; Thermal expansion; Hexagonal crystal system; Elastic energy; Diamond; Thermal; Energy minimization","score_opus":0.009893732386524046,"score_gpt":0.19419757982921962,"score_spread":0.18430384744269557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964076309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954139,0.00020124315,0.0016297495,0.000017599608,0.00039313108,0.0003050957,0.00023680177,0.000011142721,0.0017913355],"genre_scores_gemma":[0.99791336,0.000028241035,0.0012433585,0.000089730485,0.00066328456,0.0000022405793,0.000022175675,0.000009346246,0.000028289118],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9989386,0.00003451191,0.0003137093,0.00012908,0.00026395163,0.0003201274],"domain_scores_gemma":[0.9986602,0.00054041366,0.00039373562,0.00010860952,0.00009648609,0.00020053456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048067723,0.0001907923,0.0004201106,0.00003395787,0.00016893477,0.00010205566,0.00014207815,0.00007020377,0.00005644158],"category_scores_gemma":[0.000022894275,0.00012551418,0.00005199399,0.00008375391,0.00011003742,0.00024645604,0.000015638132,0.00017294934,0.000005250198],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.033954963,0.0025604442,0.21434999,0.0029631532,0.0048182067,0.00012586765,0.007207328,0.033855878,0.21050172,0.47622293,0.0053637233,0.008075815],"study_design_scores_gemma":[0.020768248,0.005484787,0.55578554,0.0010594897,0.0029124052,0.00035994285,0.0024032954,0.002779949,0.1759022,0.21047175,0.018818857,0.0032535456],"about_ca_topic_score_codex":0.0000057600078,"about_ca_topic_score_gemma":0.000022223916,"teacher_disagreement_score":0.34143555,"about_ca_system_score_codex":0.000003937405,"about_ca_system_score_gemma":0.000066114255,"threshold_uncertainty_score":0.51183194},"labels":[],"label_agreement":null},{"id":"W1964659894","doi":"10.1063/1.3686557","title":"Shock-induced formation of a disordered solid from a dense particle suspension","year":2012,"lang":"en","type":"article","venue":"AIP conference proceedings","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada; McGill University","funders":"","keywords":"Suspension (topology); Volume fraction; Materials science; Shock (circulatory); Shock wave; Ethylene glycol; Compressibility; Particle (ecology); Mechanics; Composite material; Chemical physics; Chemical engineering; Physics; Geology","score_opus":0.028927274397667974,"score_gpt":0.23520019824937702,"score_spread":0.20627292385170903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964659894","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784267,0.000059486574,0.00021488388,0.00012501597,0.00019771104,0.00016057231,0.000037981914,0.000035188546,0.0013264894],"genre_scores_gemma":[0.99948704,0.000022446004,0.0002425132,0.0000468238,0.00011686027,0.0000030247988,0.00004596577,0.0000034360007,0.000031913853],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99909085,0.000013091022,0.00024397609,0.00014106838,0.0002015994,0.00030942503],"domain_scores_gemma":[0.9994638,0.000038169615,0.00015414205,0.00007982026,0.00014227247,0.00012182748],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019227882,0.00011536151,0.0002018008,0.000035145782,0.000079878264,0.0000730055,0.00013957742,0.00006208666,0.0008610687],"category_scores_gemma":[0.000053217904,0.000094216084,0.00003312887,0.00013272084,0.000031638945,0.0008651275,0.000022503204,0.00005650885,0.0001878935],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010444741,0.000058597572,0.24276137,0.000049959282,0.00001773837,5.1749953e-7,0.0073393285,0.0000022067868,0.7422052,0.0014905947,0.00026454288,0.0057055056],"study_design_scores_gemma":[0.0007750588,0.0003007543,0.53032815,0.00011354313,0.000085968284,0.000005618065,0.0022475906,0.02710191,0.42991838,0.0076529104,0.001020758,0.00044938028],"about_ca_topic_score_codex":0.001445047,"about_ca_topic_score_gemma":0.00016322646,"teacher_disagreement_score":0.3122868,"about_ca_system_score_codex":0.0000023014718,"about_ca_system_score_gemma":0.000023855366,"threshold_uncertainty_score":0.9428098},"labels":[],"label_agreement":null},{"id":"W1965784154","doi":"10.1093/gji/ggt242","title":"Detection of a tall ridge at the core–mantle boundary from scattered PKP energy","year":2013,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Mantle (geology); Slowness; Core–mantle boundary; Geophysics; Crust; Seismic wave; Seismology; Earth structure; Mantle convection; Tectonics; Plate tectonics; Structure of the Earth; Scattering; Lithosphere; Physics; Optics","score_opus":0.010032903149769646,"score_gpt":0.2021969302495054,"score_spread":0.19216402709973576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965784154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99514276,0.000097432305,0.00036800723,0.0006364265,0.0019533485,0.000054465392,0.00031418927,0.000010215543,0.0014231768],"genre_scores_gemma":[0.99709547,0.000033021963,0.00006291901,0.00030488643,0.001455241,0.0000023183136,0.00016173854,0.000004440832,0.0008799409],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988805,0.00006124959,0.00028691458,0.00015377032,0.000432245,0.00018534345],"domain_scores_gemma":[0.99924964,0.0001460792,0.0002268108,0.00013521558,0.00014730806,0.00009497856],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00009915611,0.00011632874,0.0001614939,0.00004089323,0.00019965567,0.00018791296,0.0003842718,0.000044041815,0.008210892],"category_scores_gemma":[0.000018367777,0.000074179334,0.00012588134,0.00006253102,0.0001220855,0.0002982576,0.000051739607,0.00013029292,0.00081175583],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039058214,0.00022654187,0.01530694,0.0000116647,0.0007195933,0.000038656137,0.00047686306,0.0014496498,0.81072277,0.000910287,0.025992222,0.14375421],"study_design_scores_gemma":[0.0006580144,0.00019275003,0.8464401,0.000037768536,0.000050432296,0.00006944527,0.000051654737,0.0076433946,0.04743936,0.042743564,0.054404244,0.00026929638],"about_ca_topic_score_codex":0.01165324,"about_ca_topic_score_gemma":0.0007976322,"teacher_disagreement_score":0.8311331,"about_ca_system_score_codex":0.000010345565,"about_ca_system_score_gemma":0.000029862213,"threshold_uncertainty_score":0.9999662},"labels":[],"label_agreement":null},{"id":"W1965818384","doi":"10.1029/2006gl028009","title":"Thermochemical structure and dynamics of the African superplume","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":214,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Buoyancy; Mantle (geology); Plume; Convection; Geology; Geophysics; Core–mantle boundary; Mechanics; Physics; Meteorology","score_opus":0.013356883081099127,"score_gpt":0.25344316541233064,"score_spread":0.24008628233123153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965818384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996315,0.000024775369,0.000018499295,0.0023412216,0.00014070487,0.00015583454,0.00008993343,0.000009353478,0.00090466376],"genre_scores_gemma":[0.9994209,0.000003853823,0.00008786302,0.00016232174,0.00023797175,4.5002832e-7,0.000024865629,0.0000043170858,0.000057462723],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99834293,0.00013260452,0.00015710156,0.00022769412,0.00064165634,0.0004980249],"domain_scores_gemma":[0.99907005,0.00041906902,0.00003577747,0.0002794926,0.000060756138,0.00013488087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047988805,0.00010243154,0.0001668996,0.000046003515,0.0001692735,0.000048392885,0.00038721572,0.000055792174,0.00023858265],"category_scores_gemma":[0.00009401415,0.00006229432,0.00005316074,0.00031605441,0.00066617393,0.00007433238,0.00008139293,0.00031244502,0.000019345582],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022097414,0.000047073445,0.043481138,0.0000875745,0.00006256262,0.000023441693,0.0007311951,0.000062749015,0.92739993,0.0063188337,0.0017115758,0.019852957],"study_design_scores_gemma":[0.0002341031,0.00008964076,0.9577755,0.00002137495,0.000011985707,0.000004008064,0.0001534406,0.00090780854,0.031183839,0.0081017595,0.0013429126,0.00017367392],"about_ca_topic_score_codex":0.0027753506,"about_ca_topic_score_gemma":0.0005642788,"teacher_disagreement_score":0.9142943,"about_ca_system_score_codex":0.0000063738867,"about_ca_system_score_gemma":0.000027854547,"threshold_uncertainty_score":0.41955182},"labels":[],"label_agreement":null},{"id":"W1966614619","doi":"10.1180/minmag.2011.075.5.2657","title":"Transmission X-ray diffraction as a new tool for diamond fluid inclusion studies","year":2011,"lang":"en","type":"article","venue":"Mineralogical Magazine","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Basic Energy Sciences; Natural Sciences and Engineering Research Council of Canada; European Synchrotron Radiation Facility; Deutsche Forschungsgemeinschaft; U.S. Department of Energy","keywords":"Halite; Diamond; Kimberlite; Geology; Mineralogy; Inclusion (mineral); Mineral; Mica; Fluid inclusions; Crystal (programming language); Phlogopite; Geochemistry; Quartz; Materials science; Paleontology; Metallurgy; Mantle (geology); Gypsum","score_opus":0.043228451880697766,"score_gpt":0.2587224055616183,"score_spread":0.21549395368092053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966614619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99085516,0.0009952083,0.0015139425,0.0008337559,0.00065191183,0.0004908249,0.00006085754,0.00008823758,0.004510133],"genre_scores_gemma":[0.9880362,0.000278567,0.0069171353,0.00054602284,0.0005196739,0.000008280026,0.00016167526,0.0000060330794,0.0035263742],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99891716,0.000052728352,0.00026059686,0.00029979355,0.00018926684,0.0002804539],"domain_scores_gemma":[0.99943566,0.00012511757,0.00006552093,0.0001388472,0.000054034066,0.0001808142],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021076994,0.00018095932,0.0002933333,0.00003954129,0.0002606654,0.000029278477,0.00015075259,0.00009148459,0.003521135],"category_scores_gemma":[0.0001262892,0.00011282436,0.00008968989,0.00009851029,0.000045614805,0.00020112477,0.000048467362,0.000062955456,0.00040643732],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018356757,0.0002967077,0.0034939733,0.00018382417,0.00012997266,0.000071969385,0.0033242295,0.00034272668,0.7030567,0.0013998449,0.07879707,0.20706733],"study_design_scores_gemma":[0.0016490401,0.0018360768,0.44451344,0.000062524756,0.00011666055,0.000009879426,0.000032140826,0.0011363268,0.0023575241,0.05056736,0.49714127,0.0005777645],"about_ca_topic_score_codex":0.00041380987,"about_ca_topic_score_gemma":0.00008296443,"teacher_disagreement_score":0.70069915,"about_ca_system_score_codex":0.000003284583,"about_ca_system_score_gemma":0.000025658343,"threshold_uncertainty_score":0.9973898},"labels":[],"label_agreement":null},{"id":"W1966691426","doi":"10.1029/2002jb002345","title":"Crustal fabric in the Tibetan Plateau based on waveform inversions for seismic anisotropy parameters","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":175,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Crust; Lithosphere; Seismology; Seismic anisotropy; Anisotropy; Plateau (mathematics); Geophysics; Shear wave splitting; Magnetotellurics; Mantle (geology); Continental crust; Receiver function; Deformation (meteorology); Tectonics","score_opus":0.03944199815686796,"score_gpt":0.2970100677575396,"score_spread":0.25756806960067163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966691426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960508,0.000044108376,0.0004876882,0.0019822863,0.00022731927,0.00038383662,0.00006519967,0.000006333817,0.00075243955],"genre_scores_gemma":[0.99705046,0.00002640993,0.0021706242,0.0003471882,0.00031533057,0.0000039504603,0.0000149381995,0.0000072286443,0.000063863],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.997464,0.0002615091,0.00037004674,0.00019990985,0.0010861345,0.00061837386],"domain_scores_gemma":[0.9979142,0.0013088922,0.0001468281,0.0002355598,0.00018799216,0.00020654168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013175096,0.00015854146,0.00031613326,0.000050020106,0.00027822642,0.00018131583,0.00064286834,0.00007636925,0.00016630352],"category_scores_gemma":[0.00031828845,0.000091494876,0.0002051263,0.00046364602,0.00019603313,0.00026009747,0.000019427142,0.00054043287,0.00011333255],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01134259,0.0028799463,0.012078516,0.00039423187,0.00039551719,0.0014256575,0.0034329174,0.85027397,0.0077418303,0.013243345,0.0245523,0.07223917],"study_design_scores_gemma":[0.014963841,0.027367042,0.43690798,0.0008728959,0.00015925764,0.00007120194,0.0049119764,0.14106628,0.0091339545,0.32518694,0.038066275,0.0012923339],"about_ca_topic_score_codex":0.0043355636,"about_ca_topic_score_gemma":0.00047214323,"teacher_disagreement_score":0.7092077,"about_ca_system_score_codex":0.00003436924,"about_ca_system_score_gemma":0.00035427028,"threshold_uncertainty_score":0.6554104},"labels":[],"label_agreement":null},{"id":"W1967551476","doi":"10.1144/gsl.sp.2004.239.01.12","title":"Lithospheric structure of the Canadian Shield inferred from inversion of surface-wave dispersion with thermodynamic <i>a priori</i> constraints","year":2004,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Lithosphere; A priori and a posteriori; Inversion (geology); Shield; Geology; Dispersion (optics); Surface wave; Geophysics; Seismology; Physics; Petrology; Optics; Philosophy","score_opus":0.010403176948026602,"score_gpt":0.18325703045166886,"score_spread":0.17285385350364224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967551476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926618,0.000041571606,0.000088984016,0.0022451545,0.00022126413,0.00030255032,0.0012965384,0.00001618854,0.0031259728],"genre_scores_gemma":[0.99766946,0.000027671655,0.0014919832,0.0002270625,0.00016884539,6.0514526e-7,0.0003663188,0.0000029088467,0.00004515211],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989416,0.000053802018,0.00023145165,0.0002352958,0.00029162454,0.0002462529],"domain_scores_gemma":[0.9991806,0.00007540236,0.00019028221,0.00028655483,0.00012342351,0.00014370025],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000084405656,0.00013214393,0.00022370627,0.000011167879,0.00028968925,0.000046746463,0.00032410864,0.00018783059,0.0045460695],"category_scores_gemma":[0.000037135716,0.000077593446,0.00011970922,0.00041165957,0.00065582927,0.00013675382,0.000035941855,0.0001688036,0.000009884048],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014703712,0.00022931205,0.8929034,0.000056322802,0.00033966298,0.0000035928463,0.004575489,0.024923364,0.03009258,0.036343068,0.0034479469,0.0069382144],"study_design_scores_gemma":[0.0005068815,0.00008680548,0.9835324,0.000019934992,0.000040303185,0.0000015021299,0.00021270105,0.00040762068,0.0012900368,0.010514365,0.0032246516,0.00016275783],"about_ca_topic_score_codex":0.18590398,"about_ca_topic_score_gemma":0.31369153,"teacher_disagreement_score":0.12778755,"about_ca_system_score_codex":0.000023473827,"about_ca_system_score_gemma":0.00039496645,"threshold_uncertainty_score":0.99636394},"labels":[],"label_agreement":null},{"id":"W1967830312","doi":"10.1103/physrevlett.87.165504","title":"Temperature Measurements of Shock Compressed Liquid Deuterium up to 230 GPa","year":2001,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Deuterium; Compressibility; Materials science; Shock (circulatory); Compression (physics); Degenerate energy levels; Thermodynamics; Analytical Chemistry (journal); Condensed matter physics; Atomic physics; Physics; Chemistry; Composite material","score_opus":0.02930022626827754,"score_gpt":0.2671224932220912,"score_spread":0.23782226695381364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967830312","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992563,0.0017154736,0.000026773347,0.004028006,0.0005393428,0.00045854814,0.00009168714,0.000029961106,0.000547218],"genre_scores_gemma":[0.987968,0.0006820993,0.00011225191,0.0107371975,0.00037737816,0.0000072815906,0.00008287646,0.0000070117026,0.000025876994],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985704,0.00013209127,0.0002820608,0.0002867938,0.00041972677,0.0003089155],"domain_scores_gemma":[0.9992844,0.000052832274,0.00010195444,0.0003281,0.0000630029,0.00016974901],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019400236,0.00019712918,0.00053010794,0.000027746577,0.000058251808,0.00003421683,0.00033757908,0.0000143989655,0.0005304405],"category_scores_gemma":[0.000029903198,0.00014809347,0.0001404055,0.00024400877,0.000038924405,0.00013263192,0.000026674532,0.00008993887,0.00035374766],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020541514,0.00009147693,0.0029136182,0.0013373514,0.00012027501,0.000019059247,0.00022733751,0.0022336484,0.94239956,0.000028934488,0.04815516,0.0022681544],"study_design_scores_gemma":[0.0022553136,0.001851802,0.12765221,0.00843813,0.0008821206,0.000029382836,0.000028725455,0.00074959086,0.19290915,0.00024184244,0.66202563,0.0029361008],"about_ca_topic_score_codex":0.00021714083,"about_ca_topic_score_gemma":0.000020042236,"teacher_disagreement_score":0.74949044,"about_ca_system_score_codex":0.0000031217,"about_ca_system_score_gemma":0.000014584427,"threshold_uncertainty_score":0.60390764},"labels":[],"label_agreement":null},{"id":"W1968804842","doi":"10.1127/0935-1221/2006/0018-0161","title":"Shock-induced crystal-plastic deformation and post-shock annealing of quartz: microstructural evidence from crystalline target rocks of the Charlevoix impact structure, Canada","year":2006,"lang":"en","type":"article","venue":"European Journal of Mineralogy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Quartz; Shock (circulatory); Materials science; Annealing (glass); Deformation (meteorology); Shock metamorphism; Geology; Mineralogy; Composite material; Impact crater","score_opus":0.00705248927037941,"score_gpt":0.18805263865860633,"score_spread":0.18100014938822692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968804842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99731,0.0006509435,0.00008536127,0.00009039991,0.0006048635,0.00006889095,0.0011485872,0.0000021241513,0.000038860453],"genre_scores_gemma":[0.99913186,0.000011672042,0.0003425241,0.000033917193,0.00036870336,2.448399e-8,0.000090653404,0.000006400332,0.000014273044],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99838537,0.00033892438,0.00069431076,0.00011282628,0.00027087706,0.00019766524],"domain_scores_gemma":[0.9985763,0.00018094893,0.0008034267,0.00013712823,0.0002208805,0.00008132425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027829778,0.00015745696,0.000339558,0.000068916306,0.000075401396,0.000034367928,0.00028092376,0.000027378846,0.00030717754],"category_scores_gemma":[0.00010414242,0.00009423985,0.000074293224,0.00010396795,0.000053750777,0.00024243293,0.000024629499,0.00013781371,6.485327e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020766623,0.0000055396786,0.05514456,0.000043247455,0.00005546063,0.00003044663,0.00034366094,0.03947311,0.90365326,0.000003152853,0.0006718775,0.00036800967],"study_design_scores_gemma":[0.0004850618,0.0003765473,0.98322445,0.00012189843,0.00005506011,0.00012753351,0.000064000276,0.0012408894,0.013810749,0.00015548033,0.0002019583,0.00013636278],"about_ca_topic_score_codex":0.2618414,"about_ca_topic_score_gemma":0.102797024,"teacher_disagreement_score":0.9280799,"about_ca_system_score_codex":0.000008450325,"about_ca_system_score_gemma":0.000183964,"threshold_uncertainty_score":0.9135746},"labels":[],"label_agreement":null},{"id":"W1969643340","doi":"10.1088/0953-8984/26/2/025401","title":"Equation of state of zircon- and scheelite-type dysprosium orthovanadates: a combined experimental and theoretical study","year":2013,"lang":"en","type":"article","venue":"Journal of Physics Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; Brockhouse Institute for Materials Research","funders":"","keywords":"Scheelite; Dysprosium; Chemistry; Ab initio; Zircon; Density functional theory; Crystallography; Thermodynamics; Ab initio quantum chemistry methods; Computational chemistry; Inorganic chemistry; Molecule; Physics","score_opus":0.009891422354050949,"score_gpt":0.21718170280173724,"score_spread":0.2072902804476863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969643340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99927217,0.00009292143,0.00010640904,0.00007162176,0.0001488634,0.00019304613,0.000022094671,0.0000018077824,0.000091054884],"genre_scores_gemma":[0.9995593,0.000005904538,0.000291383,0.00007073259,0.00004210145,4.951589e-7,0.00000521478,0.00000405901,0.000020809623],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991001,0.00008776928,0.00037785136,0.00009449266,0.00022831223,0.00011145721],"domain_scores_gemma":[0.9992176,0.00009561793,0.00033093966,0.000094454685,0.00019045209,0.00007093575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022613534,0.000098870274,0.00030637762,0.000037466518,0.000029227416,0.00004767138,0.00007772769,0.000021384516,0.00073862384],"category_scores_gemma":[0.000009679157,0.00007251628,0.000028215869,0.000057137804,0.00016360715,0.00026223715,0.000019747386,0.00006936527,0.000012482597],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035819656,0.00029030652,0.11171438,0.00010965162,0.00019700894,0.000007622512,0.0025820653,0.00010758672,0.8814916,0.0014094067,0.0003865492,0.0013456302],"study_design_scores_gemma":[0.003996402,0.0040729004,0.506707,0.00011912546,0.00018943587,0.000019148774,0.001615631,0.001606008,0.43658867,0.044675265,0.00003465284,0.0003757695],"about_ca_topic_score_codex":0.00022196039,"about_ca_topic_score_gemma":0.0000051231045,"teacher_disagreement_score":0.44490293,"about_ca_system_score_codex":0.0000012807642,"about_ca_system_score_gemma":0.000029653724,"threshold_uncertainty_score":0.80874133},"labels":[],"label_agreement":null},{"id":"W1970013775","doi":"10.1021/jp204373t","title":"Polymerization of Carbon Dioxide: A Chemistry View of Molecular-to-Nonmolecular Phase Transitions","year":2011,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Division of Materials Research; U.S. Department of Energy; National Science Foundation","keywords":"Polymerization; Phase transition; Chemistry; Chemical physics; Phase (matter); Phase boundary; Phase diagram; Covalent bond; Carbon fibers; Depolymerization; Diamond; Thermodynamics; Kinetics; Polymer; Materials science; Polymer chemistry; Organic chemistry; Physics","score_opus":0.009264210987464029,"score_gpt":0.2165055664369787,"score_spread":0.2072413554495147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970013775","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99714136,0.00016455274,0.00035299675,0.000044567874,0.000023852801,0.000050123468,0.00009468624,0.0000033346314,0.0021245189],"genre_scores_gemma":[0.9997689,0.000011296345,0.000063090854,0.000014881672,0.000108935456,2.7524487e-7,0.00001313433,0.0000043198957,0.00001514088],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99920315,0.00003461951,0.00031382614,0.0000735477,0.00025336698,0.00012151626],"domain_scores_gemma":[0.9992994,0.000031925778,0.00029109415,0.00017908453,0.00009826572,0.00010023233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013379211,0.00010510601,0.00028496177,0.000010431942,0.000022701488,0.0000056629747,0.00027076047,0.000034490065,0.00029514614],"category_scores_gemma":[0.00002210908,0.000072794355,0.00012477644,0.00015243223,0.00008840198,0.000053743974,0.000009869941,0.00009338026,0.0000020074535],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011541997,0.00013757717,0.000019876312,0.00010804122,0.000053449032,0.0000063954153,0.0005481405,0.00037697874,0.99780583,0.0000069973753,0.0000032059975,0.00081806513],"study_design_scores_gemma":[0.00029729115,0.00012515175,0.00022011086,0.00006483079,0.00012814779,0.000013876905,0.000058186317,0.00021079398,0.99841124,0.0003594516,0.00003517818,0.0000757519],"about_ca_topic_score_codex":0.00008122655,"about_ca_topic_score_gemma":3.9860961e-7,"teacher_disagreement_score":0.0026275588,"about_ca_system_score_codex":0.0000016868909,"about_ca_system_score_gemma":0.00004901798,"threshold_uncertainty_score":0.3231643},"labels":[],"label_agreement":null},{"id":"W1970078057","doi":"10.1063/1.4886971","title":"Pressure induced spin transition revealed by iron M2,3-edge spectroscopy","year":2014,"lang":"en","type":"article","venue":"Applied Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of Saskatchewan","funders":"","keywords":"Multiplet; Raman spectroscopy; Spin transition; Spectroscopy; Condensed matter physics; Spin (aerodynamics); Spin states; Enhanced Data Rates for GSM Evolution; Raman scattering; Materials science; High pressure; Chemistry; Chemical physics; Spectral line; Physics; Engineering physics; Optics; Thermodynamics","score_opus":0.0061438831605175005,"score_gpt":0.19131099114321068,"score_spread":0.18516710798269317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970078057","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901726,0.000022936263,0.0037060708,0.00071035407,0.000389188,0.00034956168,0.00016484296,0.000096011456,0.0043884045],"genre_scores_gemma":[0.995572,0.000004841204,0.00047542414,0.0024414854,0.00089365424,0.000009054726,0.000554638,0.000014661793,0.000034268327],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99857473,0.00007625056,0.00022182576,0.00042024112,0.0002854913,0.00042147396],"domain_scores_gemma":[0.99936,0.000056645637,0.000119640055,0.00033407815,0.0000136694025,0.000115913936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018787365,0.00025241342,0.00031064122,0.000024645014,0.00016225231,0.00010516034,0.00025583143,0.00008388047,0.00029854986],"category_scores_gemma":[0.0000024610217,0.00023599228,0.00006787427,0.00014058729,0.000058562553,0.0001592582,0.000010129246,0.00016927587,0.00043959246],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000381341,0.000026336536,0.00021179217,0.000054120657,0.000030725143,7.2800594e-7,0.00024636564,0.0021077676,0.9809474,0.000992428,0.012908872,0.0024353424],"study_design_scores_gemma":[0.004117738,0.00052529835,0.050980628,0.00009791099,0.00054441637,0.000003313855,0.00008231819,0.004983877,0.8429576,0.0074423268,0.08538893,0.0028756289],"about_ca_topic_score_codex":0.0004660778,"about_ca_topic_score_gemma":0.000018295448,"teacher_disagreement_score":0.13798977,"about_ca_system_score_codex":0.0000032474518,"about_ca_system_score_gemma":0.000011538216,"threshold_uncertainty_score":0.9623486},"labels":[],"label_agreement":null},{"id":"W1970306532","doi":"10.1038/nature13080","title":"Hydrous mantle transition zone indicated by ringwoodite included within diamond","year":2014,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":788,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Ringwoodite; Transition zone; Kimberlite; Olivine; Mantle (geology); Geology; Geochemistry; Magmatism; Lithosphere; Tectonics; Paleontology","score_opus":0.0028643325306399793,"score_gpt":0.18309078532522122,"score_spread":0.18022645279458124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970306532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952845,0.00034052532,0.00013043982,0.00039836738,0.0006545044,0.00011524603,0.00033139266,0.00007146508,0.0026735475],"genre_scores_gemma":[0.99765617,0.000012589645,0.00016568795,0.0007758557,0.00024938982,0.0000010148583,0.00086557626,0.0000050945937,0.00026863167],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.999136,0.00007334502,0.00014256379,0.000216728,0.0002301493,0.00020123305],"domain_scores_gemma":[0.9996254,0.000038088256,0.000077095494,0.00015127819,0.000020702684,0.00008743496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023872637,0.00012136727,0.00016552559,0.000040474584,0.00012621592,0.000056960063,0.00017043966,0.00050214736,0.0005520854],"category_scores_gemma":[0.00001611745,0.00009657971,0.00003136372,0.00013132673,0.00003466006,0.00013614351,0.0000075774947,0.00053036964,0.00026948913],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009869302,0.0005576517,0.02715439,0.00062756153,0.0005231732,0.00015301208,0.011351573,0.013458561,0.6598801,0.0028379995,0.22664472,0.05582434],"study_design_scores_gemma":[0.0037013176,0.0010613304,0.18410265,0.00019046685,0.0002721898,0.00004977486,0.00015331116,0.026520267,0.3087443,0.01328429,0.45966965,0.0022504418],"about_ca_topic_score_codex":0.0006501124,"about_ca_topic_score_gemma":0.00031906908,"teacher_disagreement_score":0.3511358,"about_ca_system_score_codex":0.0000017922054,"about_ca_system_score_gemma":0.00001092419,"threshold_uncertainty_score":0.6044948},"labels":[],"label_agreement":null},{"id":"W1970770733","doi":"10.1103/physrevb.72.214108","title":"Layered single-bonded nonmolecular phase of nitrogen from first-principles simulation","year":2005,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Defence Research and Development Canada; Western University","funders":"Defence Research and Development Canada","keywords":"Metastability; Enthalpy; Phase diagram; Phase (matter); Nitrogen; Materials science; Crystallography; Solid nitrogen; Thermodynamics; Physics; Chemistry","score_opus":0.04422886232028474,"score_gpt":0.2991298797942337,"score_spread":0.254901017473949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970770733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899748,0.0077033266,0.0002704987,0.00023101455,0.00007357768,0.00028718062,0.00030099816,0.00002661666,0.001132004],"genre_scores_gemma":[0.9979117,0.00059179874,0.0006340026,0.00023463597,0.00035590338,0.0000022438307,0.00025489996,0.000004677513,0.000010154147],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99904674,0.000069289876,0.00027822968,0.00020574176,0.00023405337,0.00016595278],"domain_scores_gemma":[0.99928904,0.00017459199,0.00015473067,0.00024913313,0.000046555186,0.00008595068],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010033567,0.00013047311,0.00039209254,0.000013761031,0.000045781577,0.0000195762,0.0001679409,0.00002215497,0.0010327105],"category_scores_gemma":[0.00007442263,0.00010264177,0.00013062055,0.00010999873,0.000033131466,0.00013271271,0.000016188207,0.0000454593,0.00042431377],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045782412,0.0033168136,0.0057004634,0.0036810068,0.000626353,0.000038759168,0.0010186036,0.40119275,0.23715477,0.0039038956,0.0016385216,0.34127024],"study_design_scores_gemma":[0.002515413,0.00069408276,0.007515299,0.0020009375,0.00068600813,0.0000013400687,0.000009633853,0.43535006,0.122424126,0.016454307,0.41131163,0.0010371536],"about_ca_topic_score_codex":0.00035786745,"about_ca_topic_score_gemma":0.00009345397,"teacher_disagreement_score":0.4096731,"about_ca_system_score_codex":0.0000024507217,"about_ca_system_score_gemma":0.00001474066,"threshold_uncertainty_score":0.9998805},"labels":[],"label_agreement":null},{"id":"W1970992798","doi":"10.1038/srep00372","title":"Large amplitude fluxional behaviour of elemental calcium under high pressure","year":2012,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of Saskatchewan","funders":"","keywords":"Tetragonal crystal system; Octahedron; Isotropy; Anisotropy; Reflection (computer programming); Amplitude; Cubic crystal system; Diffraction; Crystallography; Distortion (music); Molecular dynamics; Molecular physics; Jahn–Teller effect; Materials science; Condensed matter physics; Chemistry; Physics; Crystal structure; Computational chemistry; Optics; Ion; Quantum mechanics","score_opus":0.016323836998017857,"score_gpt":0.2435471452750876,"score_spread":0.22722330827706977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970992798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98573524,0.00040201837,0.00014162085,0.00003295243,0.012128042,0.00019775628,0.0003034764,0.0000290301,0.0010298515],"genre_scores_gemma":[0.9963595,0.0000010853323,0.00024849703,0.00002484603,0.00027131662,0.0000022300155,0.000755578,0.000004484509,0.002332432],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99802357,0.00005420911,0.00042490585,0.0003648159,0.0006259632,0.0005065371],"domain_scores_gemma":[0.9989926,0.000023326738,0.00026071677,0.0004522572,0.00008202687,0.00018906768],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013108632,0.00013180838,0.00020980778,0.000069127665,0.00023588502,0.00012470566,0.00014904939,0.000062570005,0.008169804],"category_scores_gemma":[0.0000156795,0.00010578828,0.00007728382,0.000169853,0.00013046792,0.00034673195,0.00004304544,0.000062819156,0.00011976449],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020736254,0.00030741954,0.9255272,0.00006488826,0.00008496754,0.000043750977,0.00055067235,0.00049147406,0.043363106,0.0026757156,0.02657491,0.00029517015],"study_design_scores_gemma":[0.00016928389,0.000034597513,0.8816579,0.000015248015,0.00008741271,0.000053000473,0.0001322117,0.000032593314,0.035056304,0.00439886,0.07811989,0.0002427233],"about_ca_topic_score_codex":0.000968238,"about_ca_topic_score_gemma":0.00014148734,"teacher_disagreement_score":0.051544975,"about_ca_system_score_codex":0.0000025379895,"about_ca_system_score_gemma":0.00006525485,"threshold_uncertainty_score":0.9927369},"labels":[],"label_agreement":null},{"id":"W1972020394","doi":"10.1002/2014gl059269","title":"Crustal structure beneath SE Tibet from joint analysis of receiver functions and Rayleigh wave dispersion","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Natural Science Foundation of China","keywords":"Geology; Crust; Seismology; Receiver function; Rayleigh wave; Block (permutation group theory); Dispersion (optics); Joint (building); Seismic array; Flow (mathematics); Anisotropy; Lithosphere; Geophysics; Surface wave; Tectonics; Geometry; Optics","score_opus":0.03013242095378375,"score_gpt":0.2545158118885318,"score_spread":0.22438339093474804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972020394","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99711317,0.000030913616,0.00013636543,0.0007831323,0.00016394381,0.0001318377,0.0012593672,0.000015445923,0.0003658459],"genre_scores_gemma":[0.99834234,0.000018156617,0.00022650594,0.0001383033,0.0003506368,0.0000012538759,0.0007773241,0.0000052028795,0.00014028842],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978855,0.00033334192,0.00021122105,0.00043445177,0.0006970461,0.0004383995],"domain_scores_gemma":[0.9988054,0.00045877227,0.00006617201,0.00035049915,0.000097744516,0.00022142456],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031657435,0.00015122588,0.00040386023,0.00023631084,0.00023238287,0.000103143335,0.00016332945,0.00007248403,0.0018774077],"category_scores_gemma":[0.00009598625,0.00011408904,0.00012800055,0.0006312081,0.00030080305,0.00017511487,0.00006864226,0.00026154023,0.000078726545],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048594785,0.00012870143,0.03509219,0.00008824302,0.0017512898,0.000034093264,0.0017010455,0.0074786423,0.9106478,0.0008771544,0.011108172,0.030606722],"study_design_scores_gemma":[0.00035260187,0.00020582374,0.9686422,0.000020105294,0.00030151798,3.941761e-7,0.00010992553,0.020893086,0.0039096586,0.001544404,0.003793472,0.0002268065],"about_ca_topic_score_codex":0.017182311,"about_ca_topic_score_gemma":0.00092966115,"teacher_disagreement_score":0.93355,"about_ca_system_score_codex":0.0000059354034,"about_ca_system_score_gemma":0.000020460762,"threshold_uncertainty_score":0.999035},"labels":[],"label_agreement":null},{"id":"W1972376274","doi":"10.1139/e10-002","title":"Models of large, hot orogens containing a collage of reworked and accreted terranesThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Orogeny; Terrane; Crust; Diachronous; Tectonics; Paleontology; Earth science","score_opus":0.012954205343682697,"score_gpt":0.1948832386383253,"score_spread":0.1819290332946426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972376274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997003,0.00037449057,0.0000023486618,0.0009345986,0.00012118899,0.00019758241,0.00013610875,6.969689e-7,0.0012299771],"genre_scores_gemma":[0.9994935,0.000053429023,0.00032728395,0.000048814687,0.000053882133,5.7989826e-7,8.3629806e-7,0.0000016866851,0.000020021764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987413,0.00012261646,0.00051718147,0.00011663009,0.00030555783,0.00019669336],"domain_scores_gemma":[0.99855214,0.00030084624,0.00066171447,0.000120616394,0.00025730536,0.00010739749],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019747938,0.00008593878,0.00039779235,0.00015208939,0.00010197357,0.000049814666,0.00027389266,0.00004971864,0.0009923683],"category_scores_gemma":[0.00041246938,0.00004841449,0.00004224464,0.00049730507,0.001253391,0.00034789363,0.0000099441695,0.000105206105,1.2489548e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0053709554,0.00021086741,0.7280664,0.0010577462,0.00044999612,0.00003187434,0.114004485,0.0029588868,0.116939224,0.02704749,0.0007576755,0.003104432],"study_design_scores_gemma":[0.007274815,0.0052958676,0.7023924,0.0020925612,0.00035856644,0.00011837373,0.035353135,0.006819015,0.21309339,0.023142265,0.0033895036,0.00067012705],"about_ca_topic_score_codex":0.02315932,"about_ca_topic_score_gemma":0.14510821,"teacher_disagreement_score":0.12194888,"about_ca_system_score_codex":9.919135e-7,"about_ca_system_score_gemma":0.0006749351,"threshold_uncertainty_score":0.99992085},"labels":[],"label_agreement":null},{"id":"W1973614220","doi":"10.1063/1.1394759","title":"Interferometric investigation of femtosecond laser-heated expanded states","year":2001,"lang":"en","type":"article","venue":"Physics of Plasmas","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"Femtosecond; Physics; Laser; Interferometry; Optics; Phase (matter); Plasma; Atomic physics; Reflectivity; Nuclear physics","score_opus":0.020491404388831964,"score_gpt":0.21351668660631587,"score_spread":0.1930252822174839,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973614220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99779886,0.000043682172,0.000099663965,0.000026724198,0.00023053726,0.00010249117,0.00023236207,0.000019065948,0.0014466158],"genre_scores_gemma":[0.99910593,0.000056364122,0.00032895492,0.000018418341,0.00007406583,8.617053e-7,0.0003150328,0.0000041596995,0.00009623743],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991493,0.00004701186,0.0002855881,0.00015490825,0.00019386638,0.00016927348],"domain_scores_gemma":[0.999316,0.00015484763,0.00020509498,0.0001647565,0.00008879503,0.00007054228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001366856,0.00011434153,0.00026752768,0.000092211914,0.000034701778,0.000019839772,0.00016393821,0.00003977268,0.0005458736],"category_scores_gemma":[0.000020830785,0.00009937393,0.000049444723,0.00047068766,0.00008737252,0.00022824926,0.000014253449,0.000052720516,0.000065474036],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000497433,0.00020722116,0.6964323,0.00048794545,0.00033994918,0.000013054252,0.0028365182,0.02297295,0.24678607,0.0016224618,0.0018218721,0.025982244],"study_design_scores_gemma":[0.0007338431,0.00041077554,0.1749645,0.000061887724,0.000051641062,0.0000022636655,0.00012430335,0.0030663433,0.7893824,0.030445648,0.0004975393,0.0002588629],"about_ca_topic_score_codex":0.0012617504,"about_ca_topic_score_gemma":0.00015267207,"teacher_disagreement_score":0.54259634,"about_ca_system_score_codex":0.0000016359537,"about_ca_system_score_gemma":0.000029229666,"threshold_uncertainty_score":0.5976933},"labels":[],"label_agreement":null},{"id":"W1973737268","doi":"10.1111/j.1365-246x.2008.03963.x","title":"Extraction of absolute<i>P</i>velocity from receiver functions","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Slowness; Geology; Crust; Receiver function; Mantle (geology); Geodesy; Craton; Range (aeronautics); Seismic velocity; Seismology; Lithosphere; Geophysics; Tectonics; Materials science","score_opus":0.018282106736506137,"score_gpt":0.2287532187295395,"score_spread":0.21047111199303337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973737268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98956215,0.000034807603,0.001082482,0.00027086094,0.0030307882,0.000038074188,0.0003596465,0.000016240188,0.0056049316],"genre_scores_gemma":[0.9961385,0.00009244013,0.0006971935,0.00008095854,0.0018296336,4.731192e-7,0.0001496983,0.0000032362295,0.0010078709],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99891406,0.000052370167,0.00029266538,0.00014924009,0.00043841652,0.00015324198],"domain_scores_gemma":[0.9992683,0.00012756893,0.00021377948,0.00009592212,0.00018769565,0.0001067246],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000098962104,0.00010074448,0.000168432,0.000058434893,0.00018247234,0.000042870015,0.00023206911,0.000050648978,0.00656237],"category_scores_gemma":[0.000033961915,0.0000837427,0.00012728905,0.00008227007,0.000084585976,0.00042079494,0.000014445196,0.00019544901,0.00064180925],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033917278,0.0027309475,0.18902798,0.000051485877,0.003803045,0.0011883292,0.004178471,0.033136256,0.27222404,0.004450339,0.21556456,0.27025282],"study_design_scores_gemma":[0.0003223141,0.00006732996,0.9694103,0.00001412892,0.000022077811,0.00008794945,0.000026034517,0.0014341802,0.0013829693,0.005101188,0.02201019,0.00012136615],"about_ca_topic_score_codex":0.0023312878,"about_ca_topic_score_gemma":0.00006867006,"teacher_disagreement_score":0.7803823,"about_ca_system_score_codex":0.000006969997,"about_ca_system_score_gemma":0.000055146123,"threshold_uncertainty_score":0.9943458},"labels":[],"label_agreement":null},{"id":"W1973830274","doi":"10.1063/1.3668603","title":"<i>Ab initio</i> based polarizable force field generation and application to liquid silica and magnesia","year":2011,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Regroupement Québécois sur les Matériaux de Pointe","funders":"","keywords":"Polarizability; Molecular dynamics; Interatomic potential; Force field (fiction); Field (mathematics); Ab initio; Electrostatics; Pairwise comparison; Parametrization (atmospheric modeling)","score_opus":0.013534514051777859,"score_gpt":0.19616591261981414,"score_spread":0.18263139856803629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973830274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99347484,0.00008136901,0.005315235,0.00035185373,0.000051746265,0.0000784188,0.000013395124,0.00000439561,0.00062877097],"genre_scores_gemma":[0.9979542,0.000017464394,0.0008973745,0.0007931565,0.0003195207,4.2840617e-7,0.000008544443,0.0000022984702,0.00000704172],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99958354,0.000027244012,0.0001392886,0.000060431008,0.00010256257,0.00008690343],"domain_scores_gemma":[0.9996339,0.00007062638,0.00009097794,0.000082250415,0.0000469894,0.00007523903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016716454,0.000061617444,0.000105257284,0.000009585292,0.00004871435,0.000022265865,0.000096392876,0.00003069501,0.00004142783],"category_scores_gemma":[0.000013173278,0.000040580624,0.0000170681,0.000051885607,0.000029378316,0.00012238714,0.000010590741,0.00006760014,0.0000057656557],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022660081,0.000017401082,0.00026972886,0.000015031726,0.000008274693,5.7925917e-7,0.00023271675,0.00010210467,0.99409866,0.00022331816,0.00047460332,0.0043310057],"study_design_scores_gemma":[0.00021369358,0.00037690808,0.00095163286,0.000010877972,0.00005371378,0.000009577614,0.000012620486,0.0023318564,0.98996943,0.005239002,0.000731946,0.00009874627],"about_ca_topic_score_codex":0.00014348845,"about_ca_topic_score_gemma":0.0000046821347,"teacher_disagreement_score":0.005015684,"about_ca_system_score_codex":9.558195e-7,"about_ca_system_score_gemma":0.000014905946,"threshold_uncertainty_score":0.16548298},"labels":[],"label_agreement":null},{"id":"W1973923819","doi":"10.1081/sl-100002009","title":"INFRARED SPECTRA OF BROMOFORM AT HIGH PRESSURES","year":2001,"lang":"en","type":"article","venue":"Spectroscopy Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Wavenumber; Chemistry; Bromoform; Infrared; Spectral line; Degenerate energy levels; Analytical Chemistry (journal); Classification of discontinuities; Infrared spectroscopy; Diamond anvil cell; High pressure; Mineralogy; Thermodynamics; Optics; Organic chemistry","score_opus":0.005919524342160943,"score_gpt":0.19688292704178587,"score_spread":0.19096340269962492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973923819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9843827,0.00011564593,0.00019880147,0.0008730264,0.0006344033,0.00016998542,0.00014199529,0.00005955954,0.013423898],"genre_scores_gemma":[0.9954148,0.00004243906,0.0027500826,0.00062497304,0.00032863775,0.0000016078626,0.00012315757,0.0000078992,0.0007064306],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987215,0.00004034403,0.00025156589,0.00026352174,0.00030419716,0.00041890438],"domain_scores_gemma":[0.9993846,0.000054360116,0.00013244495,0.0003163127,0.000018218394,0.000094109295],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012090625,0.00017435284,0.0002795133,0.00007565286,0.00010698027,0.000047588765,0.0002802245,0.00005196235,0.007299115],"category_scores_gemma":[0.00000920148,0.00014795309,0.00007763016,0.00015914455,0.00011276291,0.0001542663,0.000018572313,0.00007782693,0.00028434533],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004203129,0.000054300224,0.11293539,0.0000852925,0.00010784072,0.00010507118,0.00021602407,0.00497123,0.8509191,0.0007831032,0.029101038,0.00030125096],"study_design_scores_gemma":[0.00079980795,0.00031194306,0.4595894,0.000037177135,0.00006778871,0.000015486858,0.00001225916,0.00036126433,0.5013419,0.0031889167,0.033814207,0.00045985187],"about_ca_topic_score_codex":0.0017676939,"about_ca_topic_score_gemma":0.00042199675,"teacher_disagreement_score":0.34957725,"about_ca_system_score_codex":0.0000074037916,"about_ca_system_score_gemma":0.000022438882,"threshold_uncertainty_score":0.99360836},"labels":[],"label_agreement":null},{"id":"W1974465048","doi":"10.1007/s003390201688","title":"The low-frequency density of states for amorphous and crystalline ices","year":2002,"lang":"en","type":"article","venue":"Applied Physics A","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Amorphous solid; Materials science; Density of states; Annealing (glass); Amorphous ice; Neutron scattering; Scattering; Low frequency; Crystallography; Analytical Chemistry (journal); Chemistry; Condensed matter physics; Physics; Optics","score_opus":0.009514400260144317,"score_gpt":0.17844840916636284,"score_spread":0.1689340089062185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974465048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972531,0.00024301333,0.00041685716,0.000059747726,0.000086067266,0.0002627017,0.00021985701,0.0000160442,0.0014425907],"genre_scores_gemma":[0.9989873,0.00018504291,0.0005201061,0.000049458013,0.00014222141,0.000005039778,0.00005288738,0.000003853051,0.000054066786],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99942154,0.000010865252,0.00014176597,0.00014271808,0.00010685632,0.00017623523],"domain_scores_gemma":[0.99947006,0.00020156584,0.000098823075,0.00015258024,0.00003511977,0.00004186177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011216176,0.000092798335,0.00015252855,0.0000065743898,0.00017207766,0.00004789183,0.00012318586,0.000023905039,0.00006311688],"category_scores_gemma":[0.0000041274457,0.00006183547,0.00002861744,0.000057942812,0.00010363445,0.000049218746,0.0000115304065,0.000032835545,0.000017878185],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055845885,0.00046585666,0.022931393,0.0011296786,0.00068264164,0.0000113616425,0.0052371337,0.0101954155,0.3718604,0.25538284,0.010775583,0.32076925],"study_design_scores_gemma":[0.0021969194,0.0004953468,0.05708012,0.000050721526,0.00021849823,0.0000037472948,0.00036571326,0.027712824,0.10073868,0.7839662,0.02612743,0.0010437889],"about_ca_topic_score_codex":0.00046646327,"about_ca_topic_score_gemma":0.00017648122,"teacher_disagreement_score":0.5285834,"about_ca_system_score_codex":6.226119e-7,"about_ca_system_score_gemma":0.000005927918,"threshold_uncertainty_score":0.25215772},"labels":[],"label_agreement":null},{"id":"W1974908130","doi":"10.4028/www.scientific.net/kem.368-372.21","title":"Electrical Behavior of PSZT Ferroelectric Ceramic under Shock Wave Compression","year":2008,"lang":"en","type":"article","venue":"Key engineering materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Association of Emergency Physicians","funders":"","keywords":"Materials science; Ferroelectricity; Ceramic; Shock wave; Lead zirconate titanate; Composite material; Ferroelectric ceramics; Shock (circulatory); Polarization (electrochemistry); Dielectric; Mechanics; Optoelectronics; Physics; Chemistry","score_opus":0.015331770003352766,"score_gpt":0.19189395293400757,"score_spread":0.17656218293065482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974908130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99789333,0.00016289494,0.00039033813,0.000019533432,0.0009285168,0.00022060769,0.00012577325,0.00009944255,0.00015953546],"genre_scores_gemma":[0.99884886,0.000082301456,0.0005682506,0.00002468167,0.00021568792,0.000005971313,0.00012777428,0.000013494486,0.00011299821],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99869865,0.00005277946,0.00037801758,0.0002352165,0.00025177485,0.00038355138],"domain_scores_gemma":[0.99948984,0.00006777448,0.00009652419,0.00021965537,0.00004016549,0.00008600978],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014452191,0.00020409592,0.00041409206,0.00012017414,0.000080272264,0.000037592505,0.00017657335,0.000111187765,0.0015587443],"category_scores_gemma":[0.000021038233,0.00017378891,0.00005439552,0.0001924769,0.000029191558,0.00011919558,0.000019057712,0.0000734251,0.00009755473],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041835337,0.00003886185,0.0013390544,0.000050509967,0.000025081663,0.0000341083,0.00006249843,0.008534447,0.9889045,0.00019032319,0.0004763179,0.0003024903],"study_design_scores_gemma":[0.0004054673,0.00018620415,0.41234586,0.000039468865,0.000053236487,0.00008622562,0.0000021739468,0.0029034398,0.5824115,0.000095503216,0.0010911024,0.0003797966],"about_ca_topic_score_codex":0.00055757875,"about_ca_topic_score_gemma":0.0000048529705,"teacher_disagreement_score":0.41100678,"about_ca_system_score_codex":0.0000064899086,"about_ca_system_score_gemma":0.000034119334,"threshold_uncertainty_score":0.99935395},"labels":[],"label_agreement":null},{"id":"W1975794819","doi":"10.1016/s0012-821x(03)00037-2","title":"The unique dynamics of the Pacific Hemisphere mantle and its signature on seismic anisotropy","year":2003,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Institut de Physique du Globe de Paris; Canadian Institute for Advanced Research","keywords":"Geology; Mantle (geology); Upwelling; Mantle convection; Seismic anisotropy; Hotspot (geology); Mid-ocean ridge; Mantle wedge; Southern Hemisphere; Core–mantle boundary; Geophysics; Seismology; Oceanography; Climatology; Tectonics; Subduction","score_opus":0.003767453504979307,"score_gpt":0.1609933252382852,"score_spread":0.15722587173330588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975794819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99462676,0.00051102095,0.000010532544,0.0021245044,0.0004765907,0.0001728236,0.00016869238,0.000009593671,0.0018994595],"genre_scores_gemma":[0.9986273,0.00016819457,0.000083247985,0.0008103798,0.000034028402,3.512622e-7,0.000024201008,0.0000021312849,0.0002501589],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989134,0.000102101825,0.0001312892,0.00025357286,0.00028683234,0.00031279653],"domain_scores_gemma":[0.99943936,0.00015702356,0.00007725421,0.00021058042,0.00001546319,0.0001003251],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040737772,0.00013192791,0.00012320402,0.00002522823,0.00058570266,0.00012033053,0.0002863822,0.000044174292,0.000115622],"category_scores_gemma":[0.000028217555,0.000070833135,0.000022198168,0.00020445828,0.0004410984,0.00015222066,0.000014172164,0.00015657998,0.000016051337],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061299006,0.00008947985,0.64026785,0.00043061262,0.00018758498,0.00016689232,0.0024512107,0.09184868,0.16547918,0.039055582,0.012652608,0.04675735],"study_design_scores_gemma":[0.0006500375,0.00040102805,0.85879284,0.00010347103,0.00004589853,0.00013754712,0.00049672095,0.04794323,0.017486513,0.002702272,0.070530266,0.00071016705],"about_ca_topic_score_codex":0.0002388777,"about_ca_topic_score_gemma":0.0003567339,"teacher_disagreement_score":0.21852502,"about_ca_system_score_codex":0.0000012810265,"about_ca_system_score_gemma":0.00004504762,"threshold_uncertainty_score":0.45048106},"labels":[],"label_agreement":null},{"id":"W1975953746","doi":"10.1002/cjg2.3370","title":"Crustal Velocity Structure of the Deep Continental Subduction Zone — A Wide Angle Reflection/Refraction Seismic Study on the Eastern Dabie Orogen","year":2003,"lang":"en","type":"article","venue":"Chinese Journal of Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Geology; Crust; Subduction; Seismology; Continental crust; Metamorphic rock; Fibrous joint; Metamorphic core complex; Dome (geology); Discontinuity (linguistics); Continental collision; Petrology; Geophysics; Geomorphology; Tectonics; Extensional definition","score_opus":0.009906737811296928,"score_gpt":0.22346120489339039,"score_spread":0.21355446708209347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975953746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99728364,0.00006206083,0.00016251366,0.00014921626,0.0018845183,0.00023771638,0.000042484513,0.000005958081,0.00017188904],"genre_scores_gemma":[0.9993078,0.000008412135,0.000032111617,0.000084672305,0.0004843795,3.9406146e-7,0.0000065604854,0.0000066409048,0.00006904354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998572,0.00029866336,0.00037888176,0.00013547998,0.0004530668,0.00016190179],"domain_scores_gemma":[0.99876416,0.00012575628,0.000631167,0.00023923971,0.00018534262,0.000054312597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030306843,0.00017979692,0.00029177035,0.000042049942,0.00026184742,0.000063514686,0.0002475046,0.00005018472,0.00013431271],"category_scores_gemma":[0.00010519669,0.00008559486,0.00014620344,0.00032173438,0.00006864186,0.00027717935,0.000015023889,0.00028387783,0.000012250891],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094073097,0.00090696936,0.88812757,0.00006404183,0.0006958743,0.000026711365,0.005370424,0.031599145,0.065681025,0.00024324474,0.00052179385,0.0058224765],"study_design_scores_gemma":[0.0009319828,0.0007252629,0.98088557,0.00003332077,0.0001495265,0.000063051135,0.0012324818,0.0009679222,0.0073723565,0.0066712527,0.0007738808,0.00019338746],"about_ca_topic_score_codex":0.0005663721,"about_ca_topic_score_gemma":0.00038891443,"teacher_disagreement_score":0.092758015,"about_ca_system_score_codex":0.000010594474,"about_ca_system_score_gemma":0.00006790275,"threshold_uncertainty_score":0.3490457},"labels":[],"label_agreement":null},{"id":"W1976482679","doi":"10.1029/2009jb006470","title":"Low heat flux and large variations of lithospheric thickness in the Canadian Shield","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Lithosphere; Heat flux; Geology; Shield; Craton; Radiogenic nuclide; Geophysics; Crust; Mantle (geology); Flux (metallurgy); High heat; Latitude; Heat transfer; Petrology; Seismology; Tectonics; Geodesy; Mechanics","score_opus":0.01810635633446694,"score_gpt":0.2795181924853129,"score_spread":0.26141183615084596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976482679","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958925,0.00013973918,0.00001947364,0.0011579182,0.00032958042,0.00013891589,0.00004598289,0.0000019691006,0.0022739237],"genre_scores_gemma":[0.9988213,0.000036675843,0.00052242394,0.000077922836,0.00038069783,0.0000011594202,0.000005241088,0.0000036710255,0.00015089291],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980339,0.0003347001,0.00031829244,0.00012780078,0.00073184416,0.00045348197],"domain_scores_gemma":[0.9982517,0.0009222964,0.00008208955,0.00020585083,0.00027951668,0.00025858186],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002235672,0.000096422875,0.00025571662,0.000026703128,0.00025709713,0.00017485369,0.00048163164,0.00009547008,0.0012238359],"category_scores_gemma":[0.000485764,0.00005846305,0.00006239408,0.00046360894,0.00020402818,0.00024470736,0.000024585064,0.00080786407,0.000034238685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012011685,0.0019694257,0.6910544,0.00075259164,0.00038724393,0.0010407537,0.018673565,0.0014462522,0.06178099,0.112310074,0.021884646,0.087498896],"study_design_scores_gemma":[0.00040693555,0.000429139,0.9712152,0.00005043676,0.00001363357,0.000020831189,0.00044743915,0.0010908225,0.0005532971,0.016323257,0.009340966,0.000108075896],"about_ca_topic_score_codex":0.27378264,"about_ca_topic_score_gemma":0.56959236,"teacher_disagreement_score":0.2958097,"about_ca_system_score_codex":0.000005246672,"about_ca_system_score_gemma":0.0005166302,"threshold_uncertainty_score":0.99968916},"labels":[],"label_agreement":null},{"id":"W1976851313","doi":"10.1016/j.gr.2008.11.005","title":"Influence of supercontinents on deep mantle flow","year":2008,"lang":"en","type":"article","venue":"Gondwana Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Australian Research Council","keywords":"Geology; Supercontinent; Mantle (geology); Mantle convection; Subduction; Hotspot (geology); Geophysics; Mantle wedge; Volcanism; Rift; Mantle plume; Laurasia; Asthenosphere; Geodynamics; Plate tectonics; Earth science; Paleontology; Gondwana; Lithosphere; Tectonics; Craton","score_opus":0.04766276220774446,"score_gpt":0.28730719830686996,"score_spread":0.2396444360991255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976851313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991333,0.00010740813,0.0000038674248,0.000097849355,0.000085986285,0.00013888007,0.00008264845,0.000013379551,0.008136972],"genre_scores_gemma":[0.998747,0.00012822663,0.00018658274,0.00003280073,0.00009038122,0.0000016658917,0.000034991765,0.0000034638247,0.0007749217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984167,0.00015033824,0.00017095073,0.0002137241,0.0006528929,0.0003953562],"domain_scores_gemma":[0.9992551,0.00016623246,0.000024090308,0.00028718027,0.000153849,0.000113544374],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005417678,0.000081509876,0.00016572552,0.00012583875,0.00020333873,0.000021627615,0.0003377398,0.000050931496,0.0016544621],"category_scores_gemma":[0.00010534547,0.00006426246,0.00003548525,0.0002774526,0.00019720237,0.00013475528,0.000029130795,0.00014968163,0.0014481387],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001252446,0.0005821687,0.6633206,0.0004999376,0.00022904074,0.0011705967,0.004605631,0.13533735,0.09946177,0.0026554586,0.031956624,0.0589284],"study_design_scores_gemma":[0.00031253757,0.00030364568,0.97324896,0.000029666611,0.0000031674294,0.0000069343373,0.000038781192,0.0016191851,0.011438239,0.00079407025,0.01207069,0.00013410689],"about_ca_topic_score_codex":0.0049267183,"about_ca_topic_score_gemma":0.0004532186,"teacher_disagreement_score":0.3099284,"about_ca_system_score_codex":0.000002494644,"about_ca_system_score_gemma":0.000060191345,"threshold_uncertainty_score":0.9993293},"labels":[],"label_agreement":null},{"id":"W1978533014","doi":"10.1093/petrology/41.1.3","title":"Liquidus Phase Relations in the System CaO–MgO–Al2O3–SiO2 at 2·0 GPa: Applications to Basalt Fractionation, Eclogites, and Igneous Sapphirine","year":2000,"lang":"en","type":"article","venue":"Journal of Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Liquidus; Anorthite; Geology; Enstatite; Diopside; Geochemistry; Plagioclase; Mineralogy; Fractional crystallization (geology); Igneous rock; Eclogite; Silicic; Basalt; Quartz; Phase (matter); Meteorite; Chemistry; Chondrite","score_opus":0.007770841681233116,"score_gpt":0.23795587341847949,"score_spread":0.23018503173724636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978533014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924986,0.00036342166,0.00038642486,0.0031938613,0.00020089858,0.00018639084,0.0000998859,0.000008901211,0.0030616445],"genre_scores_gemma":[0.9981888,0.00008780729,0.000481832,0.00039201457,0.00041877804,0.000005534486,0.000032458956,0.0000026729376,0.00039011086],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.99900496,0.0001622632,0.00038349183,0.000121207246,0.00016854896,0.00015951453],"domain_scores_gemma":[0.9992454,0.00029580097,0.00017450169,0.00012440633,0.00007468724,0.00008519444],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053104555,0.000084239815,0.0001987575,0.00012660596,0.00021944886,0.000036334415,0.00016900722,0.00006373171,0.0016046627],"category_scores_gemma":[0.000035390854,0.000056642806,0.000035238638,0.00017587174,0.000040204613,0.000117474134,0.00000769445,0.00013617217,0.0001727016],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0065950886,0.002072891,0.24286044,0.00035607873,0.0008033115,0.0016693927,0.009449352,0.38063696,0.028806137,0.01995056,0.12062693,0.18617286],"study_design_scores_gemma":[0.0020120305,0.0013727363,0.32068458,0.000029382705,0.00011226322,0.0014462176,0.00026995194,0.0038239693,0.00006241431,0.0014781683,0.66847175,0.00023653086],"about_ca_topic_score_codex":0.00033032784,"about_ca_topic_score_gemma":0.00076446007,"teacher_disagreement_score":0.5478448,"about_ca_system_score_codex":0.0000123109085,"about_ca_system_score_gemma":0.000041779163,"threshold_uncertainty_score":0.999308},"labels":[],"label_agreement":null},{"id":"W1979263279","doi":"10.1038/ngeo1950","title":"Ephemeral isopycnicity of cratonic mantle keels","year":2013,"lang":"et","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Craton; Lithosphere; Keel; Mantle (geology); Radiogenic nuclide; Geophysics; Mantle plume; Subduction; Mantle convection; Buoyancy; Geochemistry; Earth science; Paleontology; Tectonics; Oceanography","score_opus":0.0049137054043654075,"score_gpt":0.20885408348243434,"score_spread":0.20394037807806892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979263279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987159,0.002422206,0.000061388055,0.0008131192,0.003271876,0.0004385078,0.00056119356,0.000032413474,0.0052403025],"genre_scores_gemma":[0.9929042,0.0001996717,0.00093699375,0.00061299914,0.00032095565,0.0000037193165,0.000045489305,0.0000071043737,0.0049688825],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99717593,0.00012659274,0.0004722276,0.0006517561,0.0007832309,0.000790281],"domain_scores_gemma":[0.99847,0.00014513238,0.00031239173,0.00057357963,0.00023444393,0.00026446185],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005562798,0.00030419623,0.00047960898,0.00010197017,0.00027550026,0.00021789696,0.0010579491,0.0004370813,0.010661748],"category_scores_gemma":[0.0001240678,0.00023760961,0.00013333253,0.0006377015,0.00050235994,0.00074590935,0.00011944586,0.0005416895,0.0016967545],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002840775,0.0014956996,0.3530451,0.0019244454,0.00036126137,0.0001314327,0.0036137486,0.0017214745,0.38625386,0.022750711,0.16794643,0.060471725],"study_design_scores_gemma":[0.0007026863,0.00074345164,0.88154435,0.00023553809,0.00009713657,0.000019319961,0.00017661674,0.0065661496,0.024684062,0.00881561,0.07528462,0.0011304358],"about_ca_topic_score_codex":0.00817907,"about_ca_topic_score_gemma":0.000324421,"teacher_disagreement_score":0.52849925,"about_ca_system_score_codex":0.0000067017777,"about_ca_system_score_gemma":0.00022284836,"threshold_uncertainty_score":0.99908054},"labels":[],"label_agreement":null},{"id":"W1979383347","doi":"10.1103/physrevb.75.245102","title":"Giant dipole resonance of Ba in<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mi mathvariant=\"normal\">Ba</mml:mi><mml:mn>8</mml:mn></mml:msub><mml:msub><mml:mi mathvariant=\"normal\">Si</mml:mi><mml:mn>46</mml:mn></mml:msub></mml:mrow></mml:math>: An approach for studying high-pressure induced phase transitions of nanostructured materials","year":2007,"lang":"lv","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of Saskatchewan","funders":"European Synchrotron Radiation Facility; Agence Nationale de la Recherche; Deutsche Forschungsgemeinschaft","keywords":"Physics; Resonance (particle physics); Dipole; Spectral line; Scattering; Momentum transfer; Lattice (music); Ambient pressure; Atomic physics; Materials science; Optics; Thermodynamics; Quantum mechanics","score_opus":0.021312810325479336,"score_gpt":0.2567712464141609,"score_spread":0.23545843608868156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979383347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9009408,0.006010154,0.0012433261,0.00056324346,0.0033915832,0.00022702295,0.0052178176,0.00018542696,0.082220644],"genre_scores_gemma":[0.98342717,0.003611039,0.003614972,0.00096591254,0.0022663993,0.00083514757,0.0047174785,0.00046559324,0.00009630707],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9890597,0.0008586588,0.002891479,0.0020220329,0.0024824387,0.0026856803],"domain_scores_gemma":[0.99195343,0.0013340766,0.002789831,0.0024863337,0.00024314939,0.0011931943],"candidate_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0033678422,0.0011001865,0.00087974593,0.00044314846,0.0014493711,0.0010046744,0.0024952968,0.0016329364,0.17371461],"category_scores_gemma":[0.0009816244,0.0018179434,0.0016708383,0.0015007555,0.0013266942,0.0019602042,0.0009480268,0.0012892346,0.00060891826],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0051170327,0.002050487,0.00002217333,0.014556822,0.003002501,0.0014252132,0.0048308386,0.002280715,0.098202206,0.74188364,0.117428765,0.009199607],"study_design_scores_gemma":[0.0027328758,0.0023234377,0.0004096253,0.0033216255,0.002777643,0.00043799166,0.00079232076,0.012039902,0.9686915,0.00050100964,0.004153771,0.0018182662],"about_ca_topic_score_codex":0.0033256824,"about_ca_topic_score_gemma":0.0013985065,"teacher_disagreement_score":0.8704893,"about_ca_system_score_codex":0.0000088324705,"about_ca_system_score_gemma":0.0012241711,"threshold_uncertainty_score":0.99985063},"labels":[],"label_agreement":null},{"id":"W1979964005","doi":"10.1007/s00269-009-0314-2","title":"Theoretical modeling of the Al paramagnetic center and its precursors in stishovite","year":2009,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Western Canada Research Grid","keywords":"Stishovite; Chemistry; Electron paramagnetic resonance; Paramagnetism; Hyperfine structure; Diamagnetism; Octahedron; Oxygen; Crystallography; Atomic physics; Nuclear magnetic resonance; Condensed matter physics; Crystal structure; Thermodynamics; Physics","score_opus":0.007778022848184599,"score_gpt":0.20158937027637983,"score_spread":0.19381134742819522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979964005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970199,0.00035872334,0.0000030192384,0.00021292339,0.000020604026,0.000053416003,0.00007087622,0.000001972887,0.002258559],"genre_scores_gemma":[0.99976736,0.000081419144,0.00003353958,0.000041425592,0.000034802582,2.872516e-7,0.000010605792,0.0000012569591,0.00002932409],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995266,0.000015320118,0.0001422567,0.00011337578,0.00009455361,0.000107847576],"domain_scores_gemma":[0.9997904,0.000023519084,0.00004981294,0.00008331381,0.00001912719,0.00003387642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000070284514,0.000074306496,0.00015748807,0.000003896232,0.000018666748,0.0000121767525,0.00008162812,0.000027328007,0.00008054463],"category_scores_gemma":[0.000008911755,0.00005129132,0.000023012713,0.000041083826,0.00007075463,0.000039348728,0.000012233825,0.00004456873,2.837544e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000121825586,0.00015412954,0.007994486,0.00030158728,0.000025387408,0.000002283088,0.00061895774,0.0120373815,0.96260345,0.008933565,0.00013220747,0.0070747565],"study_design_scores_gemma":[0.0016610203,0.0001954325,0.038955722,0.00040140635,0.00007259518,0.00000977973,0.00009031431,0.38367364,0.44472754,0.12949061,0.00019853999,0.0005233891],"about_ca_topic_score_codex":0.00005258111,"about_ca_topic_score_gemma":0.0000036030826,"teacher_disagreement_score":0.5178759,"about_ca_system_score_codex":3.4464665e-7,"about_ca_system_score_gemma":0.0000076206484,"threshold_uncertainty_score":0.20915994},"labels":[],"label_agreement":null},{"id":"W1980124979","doi":"10.1103/physrevlett.105.215501","title":"Pressure-Induced Intermolecular Interactions in Crystalline Silane-Hydrogen","year":2010,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Silane; Chemical physics; Intermolecular force; Materials science; Lattice (music); Molecular dynamics; Raman spectroscopy; Hydrogen bond; Hydrogen; Molecular physics; Computational chemistry; Chemistry; Molecule; Physics; Organic chemistry; Optics","score_opus":0.013570198788470983,"score_gpt":0.2698376917337725,"score_spread":0.2562674929453015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980124979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958389,0.0006105545,0.00002162219,0.0021378843,0.00032416912,0.00031493025,0.00004471551,0.000033857188,0.0006734109],"genre_scores_gemma":[0.99560475,0.00020760125,0.00007985388,0.0036210192,0.00036577787,0.000009650559,0.0000858524,0.0000068032205,0.000018668312],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.998878,0.00009730646,0.00025821585,0.0002906585,0.0001967681,0.00027907483],"domain_scores_gemma":[0.99936956,0.00009084769,0.00009286821,0.00031398603,0.000020114916,0.000112630914],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017526667,0.00017364729,0.00036668737,0.00004050527,0.000044665445,0.00004390899,0.00028782923,0.000011052525,0.0010568327],"category_scores_gemma":[0.00005252412,0.00013840786,0.00012292052,0.00016488934,0.00003967194,0.00018469033,0.000024230445,0.0003056393,0.000443067],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017532446,0.00010991989,0.0024752866,0.0005431276,0.000065548404,0.000060641574,0.00012545644,0.0013045423,0.988047,0.00019955235,0.0019379562,0.0051134424],"study_design_scores_gemma":[0.0015352354,0.00028964036,0.12859035,0.0030694185,0.0007449969,0.00007692573,0.000020888065,0.053295646,0.029183138,0.0023432167,0.77835727,0.0024932832],"about_ca_topic_score_codex":0.0008499794,"about_ca_topic_score_gemma":0.0005267933,"teacher_disagreement_score":0.95886385,"about_ca_system_score_codex":0.0000016323436,"about_ca_system_score_gemma":0.000015052763,"threshold_uncertainty_score":0.99985635},"labels":[],"label_agreement":null},{"id":"W1980231965","doi":"10.1127/0935-1221/2003/0015-0931","title":"Spectroscopic 2D-tomography: Residual pressure and strain around mineral inclusions in diamonds","year":2004,"lang":"en","type":"article","venue":"European Journal of Mineralogy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Mineral; Strain (injury); Tomography; Materials science; Residual; Fluid inclusions; Geology; Diamond anvil cell; High pressure; Mineralogy; Crystallography; Metallurgy; Chemistry; Quartz; Optics","score_opus":0.009370205367005802,"score_gpt":0.2087671271820842,"score_spread":0.1993969218150784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980231965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99381864,0.0014259493,0.000029470611,0.0007062474,0.00044132245,0.00006554616,0.000074643285,0.0000072547045,0.0034309488],"genre_scores_gemma":[0.9974145,0.00013053486,0.0013591411,0.00014812719,0.0007336799,9.77963e-8,0.000022762508,0.0000073352694,0.00018376441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857956,0.00034837492,0.00044184228,0.00016485674,0.00018759837,0.00027774737],"domain_scores_gemma":[0.9994446,0.000050211806,0.00019684878,0.0001194973,0.000038789793,0.00015004956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006839262,0.00014808385,0.00029308262,0.00020753537,0.00007935957,0.00006605478,0.00023140387,0.00003075587,0.00025364026],"category_scores_gemma":[0.000036739704,0.00011467411,0.000054129836,0.00014928622,0.000105528154,0.000198282,0.00003461921,0.00021836488,0.00002050161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010386708,0.0005684322,0.48730275,0.0002344733,0.00063264964,0.011339502,0.009141542,0.056078013,0.40226814,0.0041197496,0.007139265,0.020136815],"study_design_scores_gemma":[0.0016804421,0.00075820915,0.9872126,0.00006524732,0.000056956495,0.00017557816,0.00007313537,0.000026347427,0.00018944003,0.002369653,0.0072119273,0.00018043922],"about_ca_topic_score_codex":0.00050751015,"about_ca_topic_score_gemma":0.0011213229,"teacher_disagreement_score":0.49990988,"about_ca_system_score_codex":0.0000022060876,"about_ca_system_score_gemma":0.000049834976,"threshold_uncertainty_score":0.46762744},"labels":[],"label_agreement":null},{"id":"W1980645347","doi":"10.1029/2000jb900023","title":"Evidence for local variations in the depth to the 410 km discontinuity beneath Albuquerque, New Mexico","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Advanced Research Projects Agency; National Science Foundation","keywords":"Geology; Discontinuity (linguistics); Transition zone; Seismology; Rift; Tectonics; Geomorphology; Geophysics","score_opus":0.07516622116508138,"score_gpt":0.3494456398958886,"score_spread":0.27427941873080725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980645347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97268504,0.0009733011,0.0053584855,0.017688151,0.0003143949,0.0009986705,0.000083300045,0.00000888056,0.0018897806],"genre_scores_gemma":[0.9954395,0.00017618471,0.0015559732,0.0003671629,0.0013202884,0.000008468148,0.0000054117095,0.0000058783867,0.0011210929],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9970259,0.0006241991,0.0004323093,0.0002191581,0.0011104416,0.0005880125],"domain_scores_gemma":[0.99588215,0.0031779958,0.0001045039,0.00033917782,0.0002291466,0.00026703416],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026988995,0.00014326512,0.00029557775,0.000018166813,0.00034688314,0.00036503666,0.0011757283,0.000056239514,0.0015358988],"category_scores_gemma":[0.0007988064,0.00007032087,0.00016298571,0.00057213573,0.00014341151,0.00043957712,0.000034426153,0.0004647628,0.0002355274],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024570955,0.0003831522,0.014311051,0.000049714985,0.00015619378,0.00008624164,0.00421998,0.04181455,0.00058100314,0.0068633785,0.105253115,0.8238245],"study_design_scores_gemma":[0.00067856105,0.0017341791,0.8519198,0.00022494054,0.000045401026,0.000015469865,0.00051774626,0.0074744863,0.00030549633,0.04316119,0.093704484,0.00021828928],"about_ca_topic_score_codex":0.017021574,"about_ca_topic_score_gemma":0.020692682,"teacher_disagreement_score":0.8376087,"about_ca_system_score_codex":0.000014665968,"about_ca_system_score_gemma":0.00039903793,"threshold_uncertainty_score":0.99937683},"labels":[],"label_agreement":null},{"id":"W1981273289","doi":"10.1029/2001gl014392","title":"Towards evaluating the viscosity of the Earth's outer core: An experimental high pressure study of liquid Fe‐S (8.5 wt.% S)","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Viscosity; Outer core; Inner core; Thermodynamics; Materials science; Isothermal process; Synchrotron; Volume (thermodynamics); Core (optical fiber); Temperature dependence of liquid viscosity; Analytical Chemistry (journal); Chemistry; Relative viscosity; Composite material; Physics; Optics; Chromatography","score_opus":0.0956084923520528,"score_gpt":0.3482173937585056,"score_spread":0.25260890140645276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981273289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975163,0.00007745936,0.0000022936335,0.0009564693,0.00031433726,0.0008044699,0.00009369352,0.000014090731,0.00022090337],"genre_scores_gemma":[0.9992096,0.0000028245354,0.00005159414,0.00017982212,0.00036926402,0.0000148846,0.000009524459,0.000008109256,0.00015440692],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9958533,0.0011236393,0.00033160677,0.00038804548,0.0017767084,0.00052668515],"domain_scores_gemma":[0.9984534,0.0003447683,0.00013638164,0.0007923718,0.00015204238,0.000121041085],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011030126,0.0001767432,0.00032455008,0.000048534665,0.00041292197,0.00009026099,0.0010438708,0.000049210557,0.0010703105],"category_scores_gemma":[0.00011144267,0.000096689684,0.00010793343,0.00036199176,0.0005275646,0.00022585409,0.00021214821,0.00036953908,0.00008537804],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074270944,0.0014670072,0.003990221,0.00007680724,0.00022486722,0.00001627685,0.009286031,0.0038052588,0.97365284,0.00039425583,0.0026595958,0.003684143],"study_design_scores_gemma":[0.0023768607,0.013520496,0.7567443,0.00009831277,0.00017101207,0.0000041901385,0.00231356,0.018086089,0.20396297,0.0005096331,0.0015965089,0.0006160488],"about_ca_topic_score_codex":0.014994645,"about_ca_topic_score_gemma":0.0002735068,"teacher_disagreement_score":0.76968986,"about_ca_system_score_codex":0.000003992865,"about_ca_system_score_gemma":0.000040796207,"threshold_uncertainty_score":0.9998428},"labels":[],"label_agreement":null},{"id":"W1981422200","doi":"10.1073/pnas.1006508107","title":"Silane plus molecular hydrogen as a possible pathway to metallic hydrogen","year":2010,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Intermolecular force; Intramolecular force; Molecule; Silane; Chemistry; Hydrogen; Hydrogen bond; Metallic hydrogen; Molecular dynamics; Chemical physics; Molecular vibration; Ab initio; Metal; Computational chemistry; Crystallography; Stereochemistry; Organic chemistry","score_opus":0.017728047672965343,"score_gpt":0.25106843547712093,"score_spread":0.23334038780415559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981422200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983736,0.00006385366,1.6590428e-7,0.0011767667,0.000051244773,0.00020760096,0.00007154788,0.000012875721,0.014679964],"genre_scores_gemma":[0.9982856,0.0000047939106,0.00089573907,0.00042520167,0.00009726311,0.0000031828938,8.6332625e-7,0.000002404705,0.0002849719],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99813557,0.000007215696,0.0002678387,0.0002706433,0.0010973053,0.00022145784],"domain_scores_gemma":[0.99945086,0.0000578652,0.0002376907,0.000014929999,0.00013998298,0.00009868663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010976477,0.00011251283,0.0001915146,0.00012043072,0.00018279195,0.00005383851,0.0010416071,0.0000792197,0.0003063472],"category_scores_gemma":[0.00023759392,0.0000721133,0.00007916106,0.00060950714,0.00033151795,0.0003259535,0.00007420373,0.00012703684,0.000057139576],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011426469,0.000011180964,0.0018993195,0.000019256693,0.000016801241,3.8048157e-8,0.00013448663,0.0006285913,0.9749761,0.021924997,0.00007874503,0.00029902585],"study_design_scores_gemma":[0.00009260599,0.00006543687,0.01595913,0.000017330342,0.000013072191,0.000010182456,0.000029652909,0.00054294814,0.91377676,0.06778267,0.0016009157,0.00010929662],"about_ca_topic_score_codex":0.00022469995,"about_ca_topic_score_gemma":0.0000027078631,"teacher_disagreement_score":0.061199374,"about_ca_system_score_codex":0.0000025991164,"about_ca_system_score_gemma":0.000067407615,"threshold_uncertainty_score":0.3354287},"labels":[],"label_agreement":null},{"id":"W1982385705","doi":"10.1103/physrevlett.105.235503","title":"High-Pressure Phases of Calcium: Density-Functional Theory and Diffusion Quantum Monte Carlo Approach","year":2010,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Density functional theory; Phase diagram; Quantum Monte Carlo; Monte Carlo method; Diffusion; Diffusion Monte Carlo; Stability (learning theory); Thermodynamics; Materials science; Statistical physics; Quantum; Phase (matter); Physics; Condensed matter physics; Molecular physics; Monte Carlo molecular modeling; Quantum mechanics; Markov chain Monte Carlo; Computer science; Mathematics","score_opus":0.01272526826713251,"score_gpt":0.2331594023156471,"score_spread":0.22043413404851459,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982385705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996,0.0024267125,0.00024087695,0.0004542837,0.00040678759,0.00023934337,0.00011654746,0.000022479686,0.0000929868],"genre_scores_gemma":[0.99735427,0.00056732167,0.00016925712,0.0014093216,0.00040523964,0.0000042642837,0.00006347882,0.0000054697953,0.000021364149],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99883944,0.00016606881,0.00021255876,0.00029170146,0.0002833921,0.00020681748],"domain_scores_gemma":[0.9992112,0.00025550002,0.00012739723,0.00025492598,0.0000390541,0.00011192651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034529605,0.0001774144,0.0004681167,0.000024898083,0.000094769755,0.000028011857,0.00015566351,0.000021099875,0.00027422732],"category_scores_gemma":[0.000064670035,0.00012337405,0.000105308216,0.00009502686,0.00017890715,0.00013980424,0.00003164817,0.00017977576,0.00002462653],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034334417,0.0005049296,0.011174432,0.004166906,0.00033208504,0.000019768526,0.00039572397,0.0018579611,0.9251182,0.029315334,0.013627519,0.013143775],"study_design_scores_gemma":[0.0032181502,0.00065586326,0.848896,0.0020445427,0.0030787347,0.00008109093,0.00007367025,0.03334773,0.019559838,0.018990114,0.067169,0.002885245],"about_ca_topic_score_codex":0.0007536828,"about_ca_topic_score_gemma":0.000018202587,"teacher_disagreement_score":0.9055584,"about_ca_system_score_codex":6.3224036e-7,"about_ca_system_score_gemma":0.000012818942,"threshold_uncertainty_score":0.50310475},"labels":[],"label_agreement":null},{"id":"W1983749814","doi":"10.1111/j.1365-246x.2007.03509.x","title":"Time-dependence in mantle convection models featuring dynamically evolving plates","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Plate tectonics; Mantle convection; Convection; Geology; Mantle (geology); Mechanics; Bending of plates; Hot plate; Geometry; Geophysics; Physics; Materials science; Lithosphere; Mathematics; Seismology","score_opus":0.0075526941919928136,"score_gpt":0.21741321646744247,"score_spread":0.20986052227544966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983749814","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98739785,0.0000456132,0.003096883,0.00021299941,0.001388486,0.000067152156,0.000028811874,0.000027903778,0.0077343024],"genre_scores_gemma":[0.9976416,0.000021647735,0.0007494928,0.0000689568,0.0008620392,3.7868608e-7,0.000039432376,0.000005303902,0.00061113713],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9986326,0.000039140872,0.00032888434,0.00020281193,0.00046735807,0.0003292163],"domain_scores_gemma":[0.9993583,0.00015764628,0.0001317444,0.000077553996,0.00014537301,0.00012936271],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050035556,0.00013045373,0.00017008284,0.000139282,0.00011245679,0.00019897567,0.0003172215,0.00006763346,0.0014711223],"category_scores_gemma":[0.000043821576,0.00011238038,0.00006927803,0.00013009839,0.000048535498,0.00076045457,0.000028683538,0.00030964284,0.00046233519],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026687002,0.0011937713,0.15067138,0.00010354142,0.00088356814,0.0033365374,0.0032858716,0.44654724,0.20395894,0.01396017,0.0037633067,0.16962697],"study_design_scores_gemma":[0.0007010729,0.00011025969,0.6517444,0.000107794534,0.000014977401,0.00022707481,0.00008319237,0.30936822,0.0022444325,0.034469202,0.00058077916,0.0003485326],"about_ca_topic_score_codex":0.0006205826,"about_ca_topic_score_gemma":0.00033977322,"teacher_disagreement_score":0.50107306,"about_ca_system_score_codex":0.000023831097,"about_ca_system_score_gemma":0.000036519443,"threshold_uncertainty_score":0.9994417},"labels":[],"label_agreement":null},{"id":"W1983765469","doi":"10.1139/e01-084","title":"Integrated teleseismic studies of the southern Alberta upper mantle","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Lithosphere; Seismometer; Subduction; Seismology; Mantle (geology); Receiver function; Magnetotellurics; Tectonics; Crust; Seismic array; Geophysics; Petrology; Electrical resistivity and conductivity","score_opus":0.028906027961729,"score_gpt":0.20761807597400125,"score_spread":0.17871204801227225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983765469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919244,0.001935203,0.0000015198162,0.000940095,0.0010009683,0.00004943372,0.000064505155,0.0000011630739,0.004082717],"genre_scores_gemma":[0.9977766,0.000046740086,0.00014102441,0.00015342637,0.00009644148,7.448308e-8,4.6115935e-7,0.0000014647443,0.0017837153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909055,0.00007520663,0.00026151445,0.00009394498,0.00022312434,0.00025564668],"domain_scores_gemma":[0.99927825,0.00010305724,0.00020981742,0.00010312514,0.000120017554,0.0001857472],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042279653,0.00008295016,0.00019225568,0.00011234511,0.00028575805,0.000073930474,0.00050581846,0.000027348484,0.002962986],"category_scores_gemma":[0.00015310681,0.000043197204,0.00007509246,0.00033836588,0.0006083577,0.00016959151,0.000005968847,0.00008516093,0.00009786094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016588272,0.000020859274,0.9505741,0.00004975698,0.00019328156,0.000054382246,0.016143486,0.0086691165,0.001195905,0.0007495219,0.008842656,0.013490344],"study_design_scores_gemma":[0.000867592,0.0011527041,0.727137,0.0007663369,0.00017551727,0.00033264284,0.021212284,0.00674612,0.0054673576,0.0073852967,0.22794034,0.0008168015],"about_ca_topic_score_codex":0.073977955,"about_ca_topic_score_gemma":0.41331145,"teacher_disagreement_score":0.33933347,"about_ca_system_score_codex":8.392041e-7,"about_ca_system_score_gemma":0.0002734047,"threshold_uncertainty_score":0.99794847},"labels":[],"label_agreement":null},{"id":"W1984129730","doi":"10.1103/physrevlett.94.025502","title":"Ordering of Hydrogen Bonds in High-Pressure Low-Temperature<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:msub><mml:mi mathvariant=\"normal\">H</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:mi mathvariant=\"normal\">O</mml:mi></mml:math>","year":2005,"lang":"lv","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Hydrogen bond; Physics; Inelastic neutron scattering; Crystallography; Materials science; Scattering; Chemistry; Inelastic scattering; Molecule; Quantum mechanics","score_opus":0.01026786841120486,"score_gpt":0.22316320916563942,"score_spread":0.21289534075443456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984129730","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97826093,0.006553373,0.00008194533,0.0024817851,0.0014187325,0.000119188124,0.0009992892,0.00011857422,0.009966206],"genre_scores_gemma":[0.9838969,0.0059973714,0.00096320326,0.0044907006,0.0026157685,0.0002486062,0.0014676927,0.00023399261,0.00008574645],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99281335,0.0004832429,0.0017180897,0.0013859969,0.0017168998,0.0018824049],"domain_scores_gemma":[0.9953515,0.00072219956,0.0014217356,0.0016848348,0.0000927227,0.0007270275],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0015308056,0.0008619041,0.0007355466,0.00023000367,0.0007660674,0.0007562607,0.001753044,0.0006711237,0.020478042],"category_scores_gemma":[0.00037283896,0.001219436,0.0010899485,0.0009643897,0.000700449,0.0014426657,0.00078392617,0.001207736,0.0024635175],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009662049,0.00078132225,0.000056624092,0.0115384245,0.0019602086,0.0016914991,0.0021534956,0.020207992,0.05383515,0.77907836,0.12423129,0.0034994076],"study_design_scores_gemma":[0.0026061886,0.0014438063,0.0006813511,0.008973641,0.0033443696,0.0006136341,0.00027372994,0.13012308,0.79644805,0.00047491607,0.051770624,0.0032466017],"about_ca_topic_score_codex":0.0020839693,"about_ca_topic_score_gemma":0.00065062096,"teacher_disagreement_score":0.7786035,"about_ca_system_score_codex":0.000007851242,"about_ca_system_score_gemma":0.0005040575,"threshold_uncertainty_score":0.9990255},"labels":[],"label_agreement":null},{"id":"W1984248827","doi":"10.1029/2005jb003850","title":"Detection of an ultralow velocity zone at the core‐mantle boundary using diffracted <i>PKKP</i><sub><i>ab</i></sub> waves","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Slowness; Geology; Mantle (geology); Core–mantle boundary; Diffraction; Seismology; Azimuth; Geodesy; Geophysics; S-wave; P wave; Seismic wave; Epicenter; Seismic velocity; Physics; Optics","score_opus":0.02589569798582467,"score_gpt":0.2747572788215298,"score_spread":0.24886158083570512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984248827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982734,0.000493536,0.00029695546,0.00006987864,0.0003671543,0.00019543296,0.00009010732,0.0000123607515,0.00020118624],"genre_scores_gemma":[0.99786353,0.00010456446,0.0006690644,0.000022207283,0.0011635289,8.9789773e-7,0.000024480596,0.000013129414,0.00013859503],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99652743,0.00052448653,0.0006139058,0.00025625605,0.0014524538,0.00062546285],"domain_scores_gemma":[0.9976426,0.0007643217,0.00044911163,0.0003294266,0.00058145967,0.00023308769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012762509,0.00020606673,0.0004663932,0.000031658037,0.00065051444,0.00019961855,0.0005105298,0.00011256471,0.00028534688],"category_scores_gemma":[0.0001804015,0.00013119074,0.00020509676,0.00050432427,0.00063645595,0.0005710565,0.00005010478,0.0005629342,0.000060052997],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069247023,0.00017117322,0.002516791,0.00004304891,0.00006556529,0.000053195217,0.000066684144,0.0025607941,0.97718644,0.000039168586,0.00038385775,0.016220795],"study_design_scores_gemma":[0.00066465704,0.0011604532,0.3829014,0.0000782325,0.000060039416,0.00004575879,0.00013233135,0.008862384,0.5965497,0.0074824607,0.0018342537,0.00022833746],"about_ca_topic_score_codex":0.011113322,"about_ca_topic_score_gemma":0.004392955,"teacher_disagreement_score":0.38063675,"about_ca_system_score_codex":0.000031107364,"about_ca_system_score_gemma":0.00023947602,"threshold_uncertainty_score":0.9954718},"labels":[],"label_agreement":null},{"id":"W1984478074","doi":"10.1038/nature01130","title":"The strength of Mg0.9Fe0.1SiO3 perovskite at high pressure and temperature","year":2002,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Brookhaven National Laboratory; RIKEN; Canadian Institutes of Health Research","keywords":"Silicate perovskite; Ringwoodite; Perovskite (structure); Mantle (geology); Diamond anvil cell; Geology; Post-perovskite; Mineralogy; Olivine; Rheology; Materials science; Thermodynamics; High pressure; Geophysics; Composite material; Chemistry; Crystallography","score_opus":0.003685120012474655,"score_gpt":0.1750248865100931,"score_spread":0.17133976649761845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984478074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9712509,0.023962107,4.784336e-8,0.0009413069,0.0007217423,0.00013977783,0.0005005556,0.000023231125,0.0024603168],"genre_scores_gemma":[0.9935423,0.00071639585,0.000051233532,0.00016532248,0.00026473534,8.3039686e-7,0.00004755874,0.0000042795377,0.0052073225],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990959,0.00006110725,0.00014306192,0.0002167168,0.00026145333,0.00022175143],"domain_scores_gemma":[0.99941444,0.00011648981,0.00008187394,0.00025795153,0.0000531026,0.00007610895],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012762829,0.00013925823,0.00018046534,0.000020645874,0.0002857914,0.00008076348,0.00022650948,0.0005108226,0.0016220413],"category_scores_gemma":[0.000036716225,0.00007902832,0.00003943528,0.00010327015,0.000092576636,0.000103509985,0.00003123661,0.00055372494,0.000042614094],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009957228,0.00023263812,0.12598555,0.0009476142,0.0011000162,0.00010632168,0.0035789816,0.000960647,0.09716952,0.013642686,0.6542785,0.10100181],"study_design_scores_gemma":[0.00048760278,0.00018936758,0.4593246,0.00004686877,0.00009811136,0.000013139796,0.000052251307,0.00042710901,0.0055268034,0.00074229477,0.53281283,0.00027904933],"about_ca_topic_score_codex":0.00022047707,"about_ca_topic_score_gemma":0.00046440738,"teacher_disagreement_score":0.33333904,"about_ca_system_score_codex":8.3516494e-7,"about_ca_system_score_gemma":0.0000068548275,"threshold_uncertainty_score":0.9992906},"labels":[],"label_agreement":null},{"id":"W1985506593","doi":"10.1111/j.1468-4004.2011.52621.x","title":"The Hudson Bay Lithospheric Experiment","year":2011,"lang":"en","type":"article","venue":"Astronomy & Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Precambrian; Geology; Bay; Lithosphere; Tectonics; Earth science; Plate tectonics; Seismometer; Volcano; Paleontology; Hadean; Arctic; Crust; Seismology; Oceanography","score_opus":0.012894881332691408,"score_gpt":0.18350590410202985,"score_spread":0.17061102276933846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985506593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96841145,0.00039592158,0.0010042818,0.00005247707,0.0012696638,0.0002655095,0.000036628626,0.00006765879,0.028496403],"genre_scores_gemma":[0.9941356,0.000019364687,0.004576883,0.000046740755,0.00040552104,0.000010535412,0.000033527187,0.0000068813424,0.00076491974],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9989012,0.000055910456,0.00020013742,0.00024423312,0.00017177894,0.00042675677],"domain_scores_gemma":[0.9993186,0.00005462326,0.000103496444,0.00037901275,0.000034143057,0.00011010147],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014319483,0.00017613858,0.00016528525,0.000008085953,0.00031797032,0.00010133801,0.000363515,0.0000355226,0.0014033857],"category_scores_gemma":[0.0000032603418,0.000118810334,0.000082703235,0.00010037967,0.0000998784,0.0001958629,0.00003189477,0.00008523519,0.001248395],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027339146,0.00026615307,0.1250055,0.000028863367,0.00036216702,0.000018329501,0.004892729,0.00037792887,0.0020005822,0.024295432,0.0044661895,0.83801275],"study_design_scores_gemma":[0.000370835,0.0003781548,0.6771944,0.000014113525,0.00005195545,0.0000016479413,0.0007471071,0.00017993385,0.009045969,0.006194977,0.30532122,0.00049968995],"about_ca_topic_score_codex":0.0022312168,"about_ca_topic_score_gemma":0.00013207532,"teacher_disagreement_score":0.837513,"about_ca_system_score_codex":0.000003056302,"about_ca_system_score_gemma":0.00004684333,"threshold_uncertainty_score":0.99952924},"labels":[],"label_agreement":null},{"id":"W1985610935","doi":"10.1103/physrevb.67.153202","title":"Isotherms for the liquid-gas phase transition in silicon from NPT Monte Carlo simulations","year":2003,"lang":"en","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Spinodal; Monte Carlo method; Physics; Silicon; Atom (system on chip); Phase transition; Isothermal process; Thermodynamics; Phase (matter); Condensed matter physics; Statistical physics; Quantum mechanics","score_opus":0.018228757866460638,"score_gpt":0.29230952116340164,"score_spread":0.274080763296941,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985610935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923091,0.0023528147,0.000543817,0.002550814,0.00020998831,0.00088913867,0.0007181034,0.0000181706,0.00040807738],"genre_scores_gemma":[0.99421304,0.00025834882,0.00004066482,0.005096711,0.00018500748,0.00002670122,0.00010595813,0.000008982905,0.000064595464],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99892646,0.00015489238,0.00026435335,0.0002600991,0.00015085707,0.00024331857],"domain_scores_gemma":[0.99899036,0.00056017225,0.000080406564,0.0002685932,0.000036843612,0.00006365088],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017130368,0.0001634638,0.00034060393,0.000019501731,0.00009359371,0.000048279962,0.00014014488,0.000033239518,0.003199174],"category_scores_gemma":[0.000036203783,0.00010899466,0.00013650222,0.00010534099,0.00004735122,0.00014385047,0.0000037733332,0.000089199,0.00038227325],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0035125236,0.003977908,0.0057778372,0.0055363374,0.0014879139,0.00012723272,0.015017037,0.12140998,0.6538786,0.009110602,0.1084864,0.0716776],"study_design_scores_gemma":[0.01672264,0.002078014,0.031959314,0.002921688,0.0023596224,0.000014847968,0.00030830054,0.21726607,0.065049134,0.11552393,0.54197717,0.0038192528],"about_ca_topic_score_codex":0.00081385666,"about_ca_topic_score_gemma":0.00037246925,"teacher_disagreement_score":0.5888295,"about_ca_system_score_codex":0.000003165758,"about_ca_system_score_gemma":0.00002180739,"threshold_uncertainty_score":0.997712},"labels":[],"label_agreement":null},{"id":"W1985646195","doi":"10.1103/physrevlett.102.015701","title":"First-Order Liquid-Liquid Phase Transition in Compressed Nitrogen","year":2009,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Liquid nitrogen; Phase transition; Materials science; Molecular dynamics; Dissociation (chemistry); Liquid liquid; Liquid phase; Chemical physics; Nitrogen; First order; Phase (matter); Critical point (mathematics); Thermodynamics; Physical chemistry; Chemistry; Computational chemistry; Organic chemistry; Chromatography; Physics","score_opus":0.013811486027449969,"score_gpt":0.2636080868760991,"score_spread":0.24979660084864913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985646195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98430383,0.0026630454,0.00024493292,0.011903907,0.00010733254,0.0004093609,0.00007057815,0.00004057519,0.00025644767],"genre_scores_gemma":[0.97962415,0.0014548398,0.00010398832,0.018356018,0.00027468076,0.0000056676154,0.00017504478,0.000004145142,0.000001451924],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988087,0.000116770294,0.00026352145,0.00027216465,0.0002254941,0.00031336705],"domain_scores_gemma":[0.9995276,0.00006929088,0.00007043631,0.00020632324,0.000021828737,0.00010452385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015783333,0.00018087673,0.00043279788,0.00003276872,0.00006342916,0.00003060588,0.00019499085,0.000013982871,0.00047332217],"category_scores_gemma":[0.000015194576,0.00014685173,0.00011448642,0.0002472038,0.000037957136,0.00020889542,0.0000046012856,0.00011004291,0.0003018776],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0046373024,0.0043703425,0.00052333577,0.0073658237,0.00032471982,0.0006693044,0.004235305,0.09170159,0.8020538,0.0017344797,0.04331288,0.039071076],"study_design_scores_gemma":[0.025016053,0.0194352,0.040606927,0.021122856,0.0021698037,0.000077200384,0.00008936398,0.12863825,0.060923614,0.01054101,0.68130195,0.010077775],"about_ca_topic_score_codex":0.00026351347,"about_ca_topic_score_gemma":0.000040240906,"teacher_disagreement_score":0.74113023,"about_ca_system_score_codex":0.0000035571968,"about_ca_system_score_gemma":0.000012612248,"threshold_uncertainty_score":0.598844},"labels":[],"label_agreement":null},{"id":"W1986427123","doi":"10.1063/1.3013788","title":"Containment of fluid samples in the hydrothermal diamond-anvil cell without the use of metal gaskets: Performance and advantages for <i>in situ</i> analysis","year":2008,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Gasket; Materials science; Diamond; Diamond anvil cell; Inconel; Analytical Chemistry (journal); Composite material; Metal; Distilled water; Optics; Metallurgy; Chemistry; Alloy","score_opus":0.02822628530934037,"score_gpt":0.23419607825632005,"score_spread":0.20596979294697967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986427123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99579793,0.0030291926,0.0000038092785,0.000033424556,0.00009643083,0.00063233764,0.0002956482,0.0000011977254,0.000110042194],"genre_scores_gemma":[0.9897976,0.009717516,0.00029375433,0.000059418577,0.0000073425012,0.000008533713,0.000072367766,0.0000018425213,0.0000416159],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864644,0.00014783627,0.0004999038,0.00019310604,0.0003409003,0.00017184198],"domain_scores_gemma":[0.99925095,0.00012094776,0.0002871918,0.0002782238,0.000039433624,0.000023237231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011930804,0.00010409061,0.00044352433,0.00009100949,0.00009678961,0.00002149098,0.0002687211,0.000018803086,0.000064810476],"category_scores_gemma":[0.000024215642,0.00005549897,0.00010011302,0.00043392926,0.00030493137,0.00021359127,0.00002120061,0.000035585508,0.0000015482564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095955416,0.0001926791,0.9399396,0.0041450304,0.00017281808,0.0000016772092,0.0014499966,0.00041350047,0.02999015,0.00007464605,0.0001910932,0.023332842],"study_design_scores_gemma":[0.0011478552,0.0003181875,0.8854359,0.0016062458,0.000689878,0.0000052568435,0.00025301924,0.0025284137,0.09304745,0.00005468462,0.014621361,0.00029175606],"about_ca_topic_score_codex":0.000427001,"about_ca_topic_score_gemma":0.00027675505,"teacher_disagreement_score":0.063057296,"about_ca_system_score_codex":0.0000021775725,"about_ca_system_score_gemma":0.000026963826,"threshold_uncertainty_score":0.22631824},"labels":[],"label_agreement":null},{"id":"W1987024574","doi":"10.1103/physrevlett.91.035002","title":"Nonequilibrium and Non-Steady-State Evolution of a Shock State","year":2003,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Shock wave; Shock (circulatory); Non-equilibrium thermodynamics; Discontinuity (linguistics); Compressibility; Physics; Equation of state; Steady state (chemistry); Mechanics; Thermodynamics; Chemistry","score_opus":0.008566586236974783,"score_gpt":0.22435916202410355,"score_spread":0.21579257578712877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987024574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99461895,0.0037426578,0.0001728101,0.000356265,0.00014062424,0.00025608647,0.000075416116,0.000012647741,0.0006245131],"genre_scores_gemma":[0.9975907,0.0014864854,0.00012740272,0.00070189557,0.000048213675,0.0000025697564,0.000014959952,0.0000043551727,0.000023416118],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990224,0.00011460597,0.00022384417,0.00021490002,0.00018945677,0.00023477044],"domain_scores_gemma":[0.99951094,0.000073304975,0.00011685121,0.00017963098,0.000024663788,0.00009460344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021466395,0.0001358443,0.00037835317,0.000021230224,0.00003634258,0.000021007681,0.00009794583,0.000006122245,0.000098350494],"category_scores_gemma":[0.000025523515,0.000104117746,0.00007256034,0.00013842066,0.00007898242,0.00016392075,0.000010666313,0.00006235465,0.00012361306],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002580148,0.00058371376,0.09313533,0.023990022,0.0006284442,0.00011240613,0.0027257903,0.020092878,0.7880274,0.0032253142,0.029357402,0.03786326],"study_design_scores_gemma":[0.0033476083,0.0014209116,0.7639576,0.007169107,0.0010261516,0.000046661706,0.00006490455,0.024807738,0.023039136,0.017424801,0.15401556,0.0036798269],"about_ca_topic_score_codex":0.00034302133,"about_ca_topic_score_gemma":0.000019866333,"teacher_disagreement_score":0.7649883,"about_ca_system_score_codex":0.0000028561888,"about_ca_system_score_gemma":0.000021387696,"threshold_uncertainty_score":0.42457983},"labels":[],"label_agreement":null},{"id":"W1987240447","doi":"10.1029/2007jb005355","title":"Mantle convection models with temperature‐ and depth‐dependent thermal expansivity","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Heat flux; Mantle (geology); Nusselt number; Thermodynamics; Convection; Mantle convection; Thermal; Materials science; Mechanics; Geology; Physics; Heat transfer; Geophysics; Reynolds number; Turbulence","score_opus":0.034578419135425434,"score_gpt":0.2664102568944208,"score_spread":0.2318318377589954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987240447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973379,0.00041102065,0.00005920129,0.00018489547,0.00014544385,0.00013216492,0.000014197251,0.000009622243,0.0017055706],"genre_scores_gemma":[0.9980535,0.00028017265,0.00060238293,0.000029929686,0.0005424936,0.0000011042107,0.0000033265203,0.000007190238,0.00047989638],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99781835,0.00028275396,0.00024775276,0.00020431564,0.0010339901,0.00041284968],"domain_scores_gemma":[0.998725,0.00029590618,0.00012448475,0.00015863782,0.00041350143,0.00028248935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005724423,0.00014437642,0.00032037048,0.000022175129,0.00034439703,0.00012244208,0.00022346147,0.0000718041,0.0003041203],"category_scores_gemma":[0.000052913576,0.000088928486,0.000062402,0.00019350268,0.00031177892,0.00061066693,0.00003062391,0.00048013387,0.000045293084],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01841401,0.0024709401,0.30010113,0.00068562984,0.0019961526,0.008350727,0.008736877,0.06966121,0.46222177,0.007818714,0.017231734,0.10231109],"study_design_scores_gemma":[0.0014012341,0.002651968,0.97039616,0.00009300821,0.000034039615,0.00037433015,0.00040939427,0.0030672385,0.01444592,0.005997168,0.0008224171,0.00030711474],"about_ca_topic_score_codex":0.0031106882,"about_ca_topic_score_gemma":0.00055288314,"teacher_disagreement_score":0.670295,"about_ca_system_score_codex":0.000007249174,"about_ca_system_score_gemma":0.00018496452,"threshold_uncertainty_score":0.4702451},"labels":[],"label_agreement":null},{"id":"W1987827353","doi":"10.1029/2002jb002201","title":"Effective elastic thickness <i>T</i><sub><i>e</i></sub> of the lithosphere in western Canada","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Lithosphere; Geology; Crust; Craton; Heat flow; Radiogenic nuclide; Geophysics; Bouguer anomaly; Seismology; Gravity anomaly; Tectonics; Mantle (geology); Thermal; Physics; Meteorology","score_opus":0.011143007113667886,"score_gpt":0.24525299506927078,"score_spread":0.2341099879556029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987827353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973835,0.00052858936,0.000020914944,0.00016677036,0.0006204461,0.0002813167,0.00003028469,0.000002716267,0.0009654763],"genre_scores_gemma":[0.9994844,0.00006807386,0.000083402425,0.000049824386,0.00020845508,0.0000024888338,0.0000010771895,0.000008456952,0.0000937758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99594694,0.0012623004,0.0005332014,0.00020913758,0.0014625968,0.0005858176],"domain_scores_gemma":[0.99693453,0.0017858016,0.00029953997,0.00028773773,0.00046835197,0.00022405533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015030167,0.00017875282,0.0004980479,0.000015454125,0.0001500306,0.00007137745,0.0006228098,0.00008067695,0.00017079379],"category_scores_gemma":[0.0009611177,0.00010884821,0.00014077705,0.0006855329,0.00025755068,0.00021977311,0.000049807066,0.00073994504,0.000023304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014684594,0.0007438578,0.80899835,0.00065810914,0.00042497375,0.00060533953,0.001067356,0.01690597,0.11854716,0.0022821531,0.007429723,0.04086853],"study_design_scores_gemma":[0.000760445,0.0005283354,0.9225642,0.0003051493,0.000026048538,0.00002647738,0.00022927331,0.00011499737,0.064994276,0.0061417595,0.004123474,0.0001855817],"about_ca_topic_score_codex":0.21336313,"about_ca_topic_score_gemma":0.45997486,"teacher_disagreement_score":0.24661173,"about_ca_system_score_codex":0.000034342454,"about_ca_system_score_gemma":0.0012795121,"threshold_uncertainty_score":0.7918752},"labels":[],"label_agreement":null},{"id":"W1988192838","doi":"10.1103/physrevlett.100.045504","title":"Pressure-Induced Hydrogen-Dominant Metallic State in Aluminum Hydride","year":2008,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":168,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Hydride; Materials science; Metal; Superconductivity; Hydrogen; Metallic hydrogen; Aluminium; Phase (matter); Hydrogen storage; Molecule; Covalent bond; High pressure; Condensed matter physics; Atomic physics; Crystallography; Thermodynamics; Metallurgy; Chemistry; Alloy; Physics","score_opus":0.020545423256360634,"score_gpt":0.2450101833806424,"score_spread":0.22446476012428176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988192838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99384737,0.0040544574,0.000007732006,0.0011185145,0.00019087552,0.00045949625,0.00004878066,0.000027079026,0.00024568383],"genre_scores_gemma":[0.9921724,0.0037431302,0.00004596392,0.0037094338,0.00020141136,0.000014630315,0.000046479596,0.000009444682,0.000057099307],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981665,0.00020773936,0.00036727852,0.00040528693,0.00037093833,0.00048226462],"domain_scores_gemma":[0.9992316,0.000107963875,0.00013685247,0.0003505164,0.000018092842,0.00015498263],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002771091,0.00025142147,0.00067900587,0.00004359782,0.00008395297,0.000021654856,0.00032813134,0.000012849747,0.00031175234],"category_scores_gemma":[0.000038059505,0.00019099297,0.0001769769,0.00026202557,0.00007811728,0.0002452661,0.000026596948,0.00015948089,0.0009107737],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017747271,0.0006803654,0.02121801,0.004112606,0.0006132411,0.0015307709,0.0020298315,0.0098296795,0.92285883,0.00031254315,0.018045703,0.01859094],"study_design_scores_gemma":[0.003818515,0.0007589423,0.3468544,0.0040832874,0.0011967381,0.00019241581,0.000014334036,0.02257239,0.13057685,0.004528142,0.48065296,0.0047510345],"about_ca_topic_score_codex":0.0023946615,"about_ca_topic_score_gemma":0.000119608965,"teacher_disagreement_score":0.792282,"about_ca_system_score_codex":0.0000038102623,"about_ca_system_score_gemma":0.000030898867,"threshold_uncertainty_score":0.99986714},"labels":[],"label_agreement":null},{"id":"W1988422428","doi":"10.1039/c1cp21791g","title":"Metallization of solid hydrogen: the challenge and possible solutions","year":2011,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Hydrogen; Impurity; Hydrogen molecule; Materials science; Chemistry; Nanotechnology; Chemical physics; Organic chemistry","score_opus":0.03087363022301336,"score_gpt":0.21897437785019544,"score_spread":0.18810074762718207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988422428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98943543,0.00013470328,0.00013219315,0.00006831375,0.000033687476,0.000096211494,0.00017195792,0.000033917106,0.009893603],"genre_scores_gemma":[0.99935174,0.000029604938,0.00008356698,0.000019646406,0.0003872533,0.0000032506582,0.00008303203,0.0000060396537,0.000035874542],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99912554,0.000019069317,0.00017507568,0.00023923662,0.0001921339,0.0002489397],"domain_scores_gemma":[0.9994099,0.000068965186,0.00010912732,0.00026098793,0.000052527103,0.00009849775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007133323,0.000155122,0.00024690162,0.000003774707,0.00009149686,0.000013310435,0.00023047958,0.000054232725,0.00022403158],"category_scores_gemma":[0.000018249346,0.00010857626,0.000090554386,0.00011932114,0.00026594513,0.00012338455,0.00005097588,0.000118056196,0.000025274812],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028151957,0.00023313692,0.00012855287,0.00013011845,0.00008018506,0.0000011093435,0.0007596121,0.0001286528,0.99449277,0.0021278213,0.00008669251,0.0018032135],"study_design_scores_gemma":[0.00012873115,0.000022708991,0.00039920022,0.000011032334,0.000068603484,0.0000013305234,0.00002502801,0.0026390357,0.94035494,0.056092698,0.00010484584,0.00015182956],"about_ca_topic_score_codex":0.00012168791,"about_ca_topic_score_gemma":0.0000016578686,"teacher_disagreement_score":0.054137796,"about_ca_system_score_codex":0.0000020091966,"about_ca_system_score_gemma":0.000021820102,"threshold_uncertainty_score":0.44276115},"labels":[],"label_agreement":null},{"id":"W1988443063","doi":"10.1029/2002gl015925","title":"Shear stress at the base of shield lithosphere","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mantle (geology); Geology; Asthenosphere; Lithosphere; Geophysics; Mantle convection; Anisotropy; Plate tectonics; Stress field; Shield; Shear stress; Seismology; Seismic anisotropy; Tectonics; Mechanics; Petrology; Finite element method; Physics","score_opus":0.039415240848969295,"score_gpt":0.2670615508102298,"score_spread":0.2276463099612605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988443063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9874154,0.00023389416,0.0000074233362,0.006716941,0.0001959872,0.00023161549,0.0002236941,0.000019627932,0.0049554687],"genre_scores_gemma":[0.997052,0.00005112916,0.00006698663,0.00040662216,0.00042824948,0.0000051519946,0.000033303913,0.0000063505545,0.001950199],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99753463,0.0003601021,0.00020341837,0.00031370003,0.0009512912,0.00063684146],"domain_scores_gemma":[0.998372,0.0008284502,0.00005042905,0.0005082023,0.0000681554,0.0001727391],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00049349345,0.00013239482,0.00021554228,0.000037548172,0.00031832987,0.00008770317,0.0005297749,0.000050910323,0.011188763],"category_scores_gemma":[0.000116394425,0.00008274328,0.000102614846,0.00034954137,0.0004985946,0.00013628241,0.0000980371,0.0003071249,0.002435844],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066820753,0.0007456986,0.05014827,0.0006530038,0.00038738167,0.00042841848,0.0048921425,0.006824293,0.234994,0.004215952,0.61232543,0.08371722],"study_design_scores_gemma":[0.0023450162,0.0017945503,0.650268,0.0003628732,0.00011284939,0.000014276786,0.0010061824,0.020058127,0.11570868,0.004662516,0.20201015,0.0016567521],"about_ca_topic_score_codex":0.0060932944,"about_ca_topic_score_gemma":0.00038360507,"teacher_disagreement_score":0.60011977,"about_ca_system_score_codex":0.0000058226797,"about_ca_system_score_gemma":0.000013851001,"threshold_uncertainty_score":0.9983409},"labels":[],"label_agreement":null},{"id":"W1988893500","doi":"10.1063/1.3483438","title":"Precision spectroscopy of Kaonic helium-3 and helium-4 3d→2p X-rays","year":2010,"lang":"en","type":"article","venue":"AIP conference proceedings","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Helium; Physics; Atomic physics; Nuclear physics; Isospin; Resonance (particle physics)","score_opus":0.009902818782205365,"score_gpt":0.21845844226905656,"score_spread":0.2085556234868512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988893500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988981,0.00009251684,0.00012334788,0.00017971311,0.000497379,0.00020321143,0.00005788972,0.00004286757,0.009822081],"genre_scores_gemma":[0.99656826,0.00018057274,0.002747057,0.000059380865,0.00019605056,0.000002729531,0.000016815758,0.000005658084,0.00022344974],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99877495,0.000008259675,0.00027605172,0.0003541182,0.00026666385,0.00031996568],"domain_scores_gemma":[0.99930334,0.000059150047,0.00016472542,0.00012838707,0.00020005884,0.00014436587],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003420431,0.00017979158,0.00029311347,0.000071407114,0.00011102947,0.00018237662,0.00028422568,0.000115341405,0.0021043872],"category_scores_gemma":[0.00008298008,0.00014495023,0.000034445664,0.0001337504,0.00015498475,0.00037544157,0.000042928295,0.00019198928,0.00011948584],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005761896,0.000022729408,0.0732811,0.000095565214,0.000016789856,0.0000012194346,0.00070932944,7.258569e-7,0.918904,0.0021166056,0.00047752063,0.0043168087],"study_design_scores_gemma":[0.0011341701,0.0012354979,0.5938666,0.0002635218,0.000117850635,0.000039126317,0.00043315534,0.0077427477,0.34584737,0.0318491,0.016503023,0.0009678278],"about_ca_topic_score_codex":0.00072709104,"about_ca_topic_score_gemma":0.00022190392,"teacher_disagreement_score":0.57305664,"about_ca_system_score_codex":0.0000012288216,"about_ca_system_score_gemma":0.00006965368,"threshold_uncertainty_score":0.99880785},"labels":[],"label_agreement":null},{"id":"W1989423582","doi":"10.1016/j.ssc.2011.10.003","title":"Prediction of a bcc–hcp phase transition for Sn: A first-principles study","year":2011,"lang":"en","type":"article","venue":"Solid State Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Superconductivity; Metadynamics; Density functional theory; Condensed matter physics; Ab initio; Ab initio quantum chemistry methods; Phase transition; Phase (matter); Materials science; Superconducting transition temperature; Phonon; Coupling (piping); Chemistry; Crystallography; Thermodynamics; Computational chemistry; Molecular dynamics; Physics; Metallurgy; Molecule","score_opus":0.15533634714848937,"score_gpt":0.3012011922485877,"score_spread":0.14586484510009834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989423582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869102,0.00016192147,0.0033746192,0.00017284692,0.0001969278,0.0011542947,0.0046077245,0.00006419793,0.0033572174],"genre_scores_gemma":[0.9967118,0.00018058399,0.002379803,0.000015346972,0.000021749429,0.000041512063,0.00059418404,0.000004237463,0.00005076572],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9992278,0.00010167679,0.00031005006,0.00012496849,0.00009485167,0.0001406421],"domain_scores_gemma":[0.99890405,0.00010814622,0.000121974364,0.00070809695,0.00010505107,0.00005265342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029903234,0.00008495424,0.00016280102,0.000053074065,0.0002779265,0.000020147581,0.00040744618,0.000025889563,0.00025749864],"category_scores_gemma":[0.000019112946,0.00007748715,0.000051216113,0.00010525721,0.0000829087,0.00016301972,0.00002407893,0.00004965988,0.000019755164],"study_design_candidate":"qualitative","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0052969255,0.028105661,0.118804954,0.001437885,0.003087503,0.000016962791,0.6877117,0.0542894,0.013839791,0.01679327,0.0053428053,0.06527312],"study_design_scores_gemma":[0.012267497,0.0091043655,0.55864066,0.00022277773,0.0009487454,0.000009580976,0.011964525,0.29603845,0.008061057,0.035713274,0.06591162,0.0011174446],"about_ca_topic_score_codex":0.0018282536,"about_ca_topic_score_gemma":0.0043786475,"teacher_disagreement_score":0.6757472,"about_ca_system_score_codex":0.0000021210258,"about_ca_system_score_gemma":0.000031052507,"threshold_uncertainty_score":0.31598344},"labels":[],"label_agreement":null},{"id":"W1989544004","doi":"10.1139/e09-074","title":"Initiation, development, and benefits of Lithoprobe — shaping the direction of Earth science research in Canada and beyondThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.Lithoprobe Contribution 1480.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geography; Engineering","score_opus":0.024747062645303332,"score_gpt":0.2201690240189951,"score_spread":0.19542196137369178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989544004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99687266,0.0006639637,0.0000011825836,0.0014700389,0.00015404749,0.00027755537,0.000060220875,5.1358643e-7,0.0004997877],"genre_scores_gemma":[0.9995586,0.00010702469,0.00023854732,0.000033538985,0.00004983094,0.0000015786839,8.5033423e-7,0.0000013779407,0.000008608759],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982258,0.00018719885,0.0005675562,0.00016265776,0.00059675233,0.00026002416],"domain_scores_gemma":[0.9981451,0.00047443804,0.0005247044,0.00011195934,0.0006388075,0.00010497434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005867134,0.00008259051,0.00028189653,0.00027903894,0.0002839094,0.00008887767,0.00029300535,0.00003538153,0.00018082687],"category_scores_gemma":[0.0011767105,0.000045835222,0.000016366204,0.0012252299,0.0022330545,0.00052496715,0.000021226464,0.00017740065,7.817042e-8],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037392369,0.000039704442,0.9458896,0.0002561676,0.000037964834,0.0000024116803,0.017728902,0.0005121438,0.01995091,0.008740957,0.000045744953,0.006421594],"study_design_scores_gemma":[0.00050933636,0.00022887797,0.90737206,0.00032101446,0.0000123637865,0.000011345345,0.0025097057,0.00022967768,0.08630106,0.002010636,0.0004185526,0.00007534801],"about_ca_topic_score_codex":0.59989464,"about_ca_topic_score_gemma":0.9666732,"teacher_disagreement_score":0.36677858,"about_ca_system_score_codex":0.000006637829,"about_ca_system_score_gemma":0.0034469983,"threshold_uncertainty_score":0.82277817},"labels":[],"label_agreement":null},{"id":"W1989842007","doi":"10.1029/1999gc000035","title":"Constraining mantle density structure using geological evidence of surface uplift rates: The case of the African Superplume","year":2000,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":314,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Seismology; Geophysics","score_opus":0.019918806031540552,"score_gpt":0.2318536837015472,"score_spread":0.21193487767000663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989842007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976677,0.00042073306,0.000008631087,0.000056384324,0.0002685847,0.00027894642,0.00063683704,0.00001811544,0.00064407726],"genre_scores_gemma":[0.99950457,0.000014363545,0.00009000741,0.00002325401,0.00021174361,7.743523e-7,0.00002709865,0.0000059833187,0.00012219051],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99819374,0.0002107515,0.0005028985,0.00036519574,0.00031910214,0.00040834013],"domain_scores_gemma":[0.99831337,0.0003709891,0.00035038966,0.0007177586,0.00015982537,0.00008764577],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004138742,0.0002603131,0.00049586355,0.000009148055,0.0003269284,0.000059625407,0.00058278505,0.00014192722,0.0014272933],"category_scores_gemma":[0.000053816802,0.00015440144,0.00016053962,0.00030702227,0.0004979204,0.00013021847,0.00006254546,0.00022203758,0.000015667614],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023698654,0.00008549578,0.076203994,0.0016209253,0.0003077069,0.0003065316,0.0025251675,0.07947706,0.83617693,0.00024595318,0.00018393584,0.0026293315],"study_design_scores_gemma":[0.0014243576,0.00035267478,0.07246685,0.002009019,0.0009862066,0.003985167,0.0073409714,0.07658713,0.82522887,0.0067996057,0.0007907885,0.0020283672],"about_ca_topic_score_codex":0.014646754,"about_ca_topic_score_gemma":0.0004488789,"teacher_disagreement_score":0.014197875,"about_ca_system_score_codex":0.0000056262525,"about_ca_system_score_gemma":0.00014291679,"threshold_uncertainty_score":0.99948555},"labels":[],"label_agreement":null},{"id":"W1990277017","doi":"10.1002/2014gl060630","title":"Seismic evidence for rotating mantle flow around subducting slab edge associated with oceanic microplate capture","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Subduction; Slab; Seismology; Mantle (geology); Slab window; Buoyancy; Mantle wedge; Geophysics; Oceanic crust; Transition zone; Plate tectonics; Shear wave splitting; Clockwise; Tectonics; Geometry; Mechanics; Physics","score_opus":0.04839631582163823,"score_gpt":0.29123385269863616,"score_spread":0.24283753687699794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990277017","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959386,0.0000632671,0.0010787233,0.0017434941,0.00030383843,0.0005564951,0.00010965839,0.00006247413,0.00014343562],"genre_scores_gemma":[0.99670136,0.00000585049,0.0013166665,0.0004929682,0.00094154733,0.000015883612,0.00016304429,0.000020576916,0.0003421324],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99667424,0.0004850399,0.00026054666,0.0006260097,0.0007913849,0.0011627643],"domain_scores_gemma":[0.9963006,0.0027807632,0.00012331823,0.00035198487,0.00021993117,0.00022340663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016789992,0.00024528918,0.00036862944,0.000095403535,0.0006342107,0.0003728972,0.00048473393,0.00008728207,0.00009308108],"category_scores_gemma":[0.0010304417,0.00018934943,0.00009863259,0.00041873622,0.000243736,0.00041505622,0.00005310314,0.00046745158,0.00030830994],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023963358,0.00035649902,0.043111257,0.0013228708,0.00089558464,0.00021061582,0.004546352,0.07228766,0.7692889,0.0008566918,0.04940112,0.055326123],"study_design_scores_gemma":[0.0022783435,0.001392053,0.22958167,0.0010944612,0.00013191691,0.000014546284,0.0003140234,0.7468055,0.0071719554,0.0031634294,0.0066733835,0.0013787478],"about_ca_topic_score_codex":0.0023916825,"about_ca_topic_score_gemma":0.0002632781,"teacher_disagreement_score":0.7621169,"about_ca_system_score_codex":0.000018169545,"about_ca_system_score_gemma":0.0000848493,"threshold_uncertainty_score":0.7721446},"labels":[],"label_agreement":null},{"id":"W1991095788","doi":"10.1103/physrevb.72.132201","title":"Intermediate range chemical ordering in amorphous and liquid water, Si, and Ge","year":2005,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Neutron diffraction; Materials science; Radial distribution function; Amorphous solid; Germanium; Structure factor; Diffraction; Silicon; Amorphous ice; Coordination number; Amorphous silicon; Range (aeronautics); Hydrogen; Crystallography; Pair distribution function; Liquid water; Molecule; Shell (structure); Molecular dynamics; Physics; Thermodynamics; Crystalline silicon; Optics; Chemistry; Ion; Computational chemistry","score_opus":0.009490821971505308,"score_gpt":0.23361852990356777,"score_spread":0.22412770793206246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991095788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98913723,0.009851283,0.0000016244089,0.0004297096,0.00005344013,0.00015119155,0.000015018689,0.000015520214,0.00034498246],"genre_scores_gemma":[0.9879936,0.011183371,0.0000505644,0.0004606482,0.00027256837,0.0000037771892,0.000021319098,0.0000035110618,0.000010640327],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99928856,0.000038406582,0.00016075707,0.0002009433,0.00009223586,0.0002190767],"domain_scores_gemma":[0.99972177,0.000051336883,0.000026581245,0.00009537433,0.000008092459,0.00009685635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014922007,0.000113606686,0.0003198346,0.000013527121,0.000023555387,0.00002839263,0.00008053006,0.000019042323,0.00018456267],"category_scores_gemma":[0.000022061184,0.00007326786,0.000028703045,0.000045595327,0.000056457262,0.00013320628,0.000036795493,0.00007911932,0.00014509259],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040938557,0.0003692169,0.012886153,0.0071557947,0.00008571741,0.000111782305,0.0025231056,0.0000740472,0.22500198,0.0008699362,0.0011292326,0.7493836],"study_design_scores_gemma":[0.006219378,0.0017790901,0.24097544,0.009299907,0.00059175375,0.0001254865,0.000055264554,0.017269744,0.13392144,0.010024519,0.5755314,0.0042065713],"about_ca_topic_score_codex":0.00022272614,"about_ca_topic_score_gemma":0.0000933555,"teacher_disagreement_score":0.7451771,"about_ca_system_score_codex":0.0000014528706,"about_ca_system_score_gemma":0.0000044935705,"threshold_uncertainty_score":0.29877767},"labels":[],"label_agreement":null},{"id":"W1991300959","doi":"10.1007/s00410-012-0786-9","title":"Platelet development in cuboid diamonds: insights from micro-FTIR mapping","year":2012,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Cuboid; Diamond; Context (archaeology); Chemistry; Octahedron; Crystallography; Analytical Chemistry (journal); Mineralogy; Metallurgy; Materials science; Geology; Geometry; Environmental chemistry; Mathematics; Crystal structure","score_opus":0.009261732234046114,"score_gpt":0.21654039030348665,"score_spread":0.20727865806944054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991300959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953063,0.0020202976,0.00023954822,0.0006311344,0.0007020221,0.00013911824,0.0003675843,0.000019876405,0.00057408214],"genre_scores_gemma":[0.99718934,0.00003711565,0.0009210879,0.00066089624,0.00032696314,0.000010793779,0.00072235015,0.0000026120238,0.00012883701],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99886614,0.00013501714,0.00025938358,0.0002208871,0.000053627577,0.00046492484],"domain_scores_gemma":[0.9994282,0.00018938108,0.00004746065,0.00011800327,0.000036952737,0.00017999213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018432402,0.0001396751,0.0002919989,0.00014725552,0.00016160675,0.000021134436,0.00010760884,0.00015038285,0.00054116815],"category_scores_gemma":[0.0000496901,0.00012096146,0.00002079535,0.00013254352,0.000062446954,0.00012896639,0.000030192252,0.00011688641,0.00038051367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028290335,0.00017044101,0.8380277,0.000021117607,0.00021721766,0.00007546893,0.005004825,0.00033530424,0.135725,0.0068805055,0.0043927683,0.008866706],"study_design_scores_gemma":[0.0005436672,0.000041836327,0.783145,0.000006472298,0.000009536825,0.000009484968,0.000022823067,0.000037314967,0.0018076729,0.0008124616,0.21339925,0.00016444881],"about_ca_topic_score_codex":0.0017029187,"about_ca_topic_score_gemma":0.0036374473,"teacher_disagreement_score":0.20900647,"about_ca_system_score_codex":0.000007114838,"about_ca_system_score_gemma":0.000039390652,"threshold_uncertainty_score":0.5925412},"labels":[],"label_agreement":null},{"id":"W1991607695","doi":"10.1103/physrevlett.111.175502","title":"Stable All-Nitrogen Metallic Salt at Terapascal Pressures","year":2013,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"Engineering and Physical Sciences Research Council","keywords":"Materials science; Nitrogen; Metal; Salt (chemistry); Metallurgy; Physics; Chemistry; Physical chemistry","score_opus":0.015264299164398977,"score_gpt":0.23874132712049187,"score_spread":0.2234770279560929,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991607695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9838917,0.009443056,0.000010440913,0.0044430513,0.00023722318,0.0006760827,0.0000820814,0.0000686641,0.0011476855],"genre_scores_gemma":[0.9787119,0.002394677,0.00020138721,0.017761204,0.00050373323,0.000038681697,0.00020599633,0.000012177107,0.00017021236],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.998353,0.00016751992,0.00026527772,0.0003589804,0.0003715468,0.00048366695],"domain_scores_gemma":[0.99915534,0.00013456115,0.00011225253,0.00035450136,0.000031702897,0.00021164224],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015686279,0.00023910492,0.00052528246,0.000021458583,0.00012080968,0.00010800776,0.00034789686,0.000014345794,0.00600545],"category_scores_gemma":[0.000020872965,0.00016782206,0.00019842542,0.000118186545,0.00008549871,0.00035709748,0.000046798054,0.000103295446,0.0059538335],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057072506,0.00031084957,0.016017726,0.0043314057,0.001144892,0.000056072142,0.0004454334,0.0013494217,0.3795934,0.0009755668,0.57396585,0.021752317],"study_design_scores_gemma":[0.0004474061,0.00014628297,0.039129198,0.00053140474,0.00060632516,0.000011580538,0.0000036494034,0.002067151,0.007477397,0.0048512975,0.9436696,0.0010587065],"about_ca_topic_score_codex":0.0014900935,"about_ca_topic_score_gemma":0.000037074333,"teacher_disagreement_score":0.37211603,"about_ca_system_score_codex":0.0000045501947,"about_ca_system_score_gemma":0.000010774859,"threshold_uncertainty_score":0.9949032},"labels":[],"label_agreement":null},{"id":"W1992120116","doi":"10.1046/j.1365-246x.2003.01807.x","title":"Lithospheric structure beneath the Archaean Slave Province and Proterozoic Wopmay orogen, northwestern Canada, from a lithoprobe refraction/wide-angle reflection survey","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Terrane; Craton; Proterozoic; Crust; Archean; Lithosphere; Continental crust; Seismic refraction; Mantle (geology); Seismology; Paleontology; Tectonics","score_opus":0.010275137118750792,"score_gpt":0.21083416712068148,"score_spread":0.20055903000193068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992120116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99591076,0.00013435772,0.00048373282,0.0005097023,0.0017046009,0.00021437794,0.0007079849,0.000014187365,0.00032030244],"genre_scores_gemma":[0.99735004,0.00003567973,0.00064241723,0.00034966707,0.0007680051,0.000003233465,0.00022762579,0.000009245795,0.0006140673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99808025,0.000352625,0.00033912633,0.00032547797,0.0006031113,0.00029940222],"domain_scores_gemma":[0.9988726,0.00026964475,0.00028437914,0.00018084655,0.0002124225,0.00018011595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031370186,0.0002135815,0.00021889592,0.000028214481,0.00038859728,0.0003795405,0.00031052873,0.000064876636,0.00085663813],"category_scores_gemma":[0.00011039875,0.00014030239,0.00005751793,0.00012823223,0.00007481808,0.0003618132,0.000028511266,0.0003965538,0.000021252412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056621985,0.00015685328,0.94413364,0.000027097194,0.00074030453,0.0002217715,0.0010919009,0.0028143718,0.0046531814,0.0007418125,0.0033675537,0.0414853],"study_design_scores_gemma":[0.00032740485,0.00011604589,0.97064406,0.000026295596,0.000029723778,0.0001125999,0.00006182193,0.0005244165,0.0011842584,0.0063927765,0.020352917,0.00022767499],"about_ca_topic_score_codex":0.5176149,"about_ca_topic_score_gemma":0.76440686,"teacher_disagreement_score":0.24679196,"about_ca_system_score_codex":0.0000378173,"about_ca_system_score_gemma":0.00039393367,"threshold_uncertainty_score":0.9379587},"labels":[],"label_agreement":null},{"id":"W1992334091","doi":"10.5539/apr.v6n4p26","title":"Pressure Dependency Grüneisen Parameter r for bcc Mo","year":2014,"lang":"en","type":"article","venue":"Applied Physics Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Beijing University of Civil Engineering and Architecture","keywords":"Thermodynamics; Materials science; Yield (engineering); Work (physics); Dependency (UML); Molybdenum; Melting point; Melting temperature; Equation of state; Physics; Metallurgy; Computer science","score_opus":0.053883455831540326,"score_gpt":0.30734780963867897,"score_spread":0.25346435380713866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992334091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8246837,0.00031224437,0.016435025,0.00043963926,0.0011134346,0.004511662,0.0011320594,0.000284201,0.15108801],"genre_scores_gemma":[0.9962852,0.000015368276,0.0013415203,0.00007661088,0.001032336,0.00006417394,0.00018557002,0.000014927304,0.0009842946],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9977574,0.00014109144,0.00020449689,0.00048390075,0.00066710415,0.0007460298],"domain_scores_gemma":[0.99820787,0.00096947403,0.00005645043,0.00042472658,0.00016122854,0.00018026243],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011538691,0.00017474116,0.00027948458,0.00005552085,0.0003660587,0.00021535758,0.0005363355,0.00010701821,0.00044027343],"category_scores_gemma":[0.00006560402,0.00014404522,0.00007767172,0.00024450032,0.00013119556,0.00013380828,0.000058180987,0.00024499642,0.00092774647],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081743475,0.00032464386,0.0058837617,0.0008516126,0.00043337996,0.00000412261,0.0011234878,0.016864687,0.0647271,0.34571397,0.031335723,0.5319201],"study_design_scores_gemma":[0.0011531918,0.00034547344,0.010827938,0.000022228298,0.00006405446,0.0000010965807,0.00006375967,0.038050435,0.028217722,0.68001395,0.2406061,0.0006340155],"about_ca_topic_score_codex":0.00071758503,"about_ca_topic_score_gemma":0.00006898804,"teacher_disagreement_score":0.53128606,"about_ca_system_score_codex":0.000002431701,"about_ca_system_score_gemma":0.000050616178,"threshold_uncertainty_score":0.99985015},"labels":[],"label_agreement":null},{"id":"W1992572869","doi":"10.1002/2013gc005211","title":"A comparison of mantle convection models featuring plates","year":2014,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Mantle convection; Mantle (geology); Rheology; Convection; Viscosity; Geology; Mechanics; Geophysics; Physics; Thermodynamics; Lithosphere","score_opus":0.01566263061219619,"score_gpt":0.2281425962161714,"score_spread":0.2124799656039752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992572869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98329985,0.00018917734,0.0006127434,0.000016975557,0.00066209515,0.00015533456,0.00015272421,0.00007362906,0.0148374485],"genre_scores_gemma":[0.99863696,0.0000068628183,0.00012234457,0.0000081816015,0.0005363072,0.0000037583577,0.00032741923,0.000008101071,0.0003500517],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99849486,0.000058749498,0.0004225852,0.00033999173,0.00032686975,0.00035696654],"domain_scores_gemma":[0.9989187,0.00011587639,0.00032318739,0.00038954467,0.00014200453,0.00011069931],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002472184,0.00022379919,0.0005165235,0.000030725485,0.0001362393,0.0000692351,0.00026503814,0.00012775033,0.00019923357],"category_scores_gemma":[0.000019884743,0.00020842167,0.00009284327,0.00017337732,0.00005942953,0.0001899823,0.000027492619,0.00012782466,0.00013216576],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031993768,0.00045522483,0.13392146,0.004824358,0.00051222777,0.000011269998,0.002849344,0.19084808,0.6414029,0.0046898355,0.0037399335,0.016425414],"study_design_scores_gemma":[0.0010928687,0.00025187977,0.024391986,0.00034921605,0.00013647415,0.0000185977,0.0005835437,0.36868408,0.5791521,0.020461485,0.0038548636,0.0010229058],"about_ca_topic_score_codex":0.0028837686,"about_ca_topic_score_gemma":0.00007562317,"teacher_disagreement_score":0.177836,"about_ca_system_score_codex":0.0000040352884,"about_ca_system_score_gemma":0.00003166775,"threshold_uncertainty_score":0.8499189},"labels":[],"label_agreement":null},{"id":"W1992635609","doi":"10.2138/am.2005.1960","title":"Synchrotron micro-X-ray fluorescence analysis of natural diamonds: First steps in identification of mineral inclusions in situ","year":2005,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Kimberlite; XANES; Synchrotron; Microprobe; Diamond; Beamline; Mineralogy; Mineral; Analytical Chemistry (journal); Spectroscopy; X-ray fluorescence; Materials science; Diamond type; Geology; Mantle (geology); Chemistry; Geochemistry; Fluorescence; Metallurgy; Material properties of diamond; Optics; Physics; Environmental chemistry","score_opus":0.006087970424528178,"score_gpt":0.22680855805547226,"score_spread":0.22072058763094407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992635609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988107,0.0001935105,0.00001726823,0.00031395408,0.000088387074,0.00014190307,0.00021950078,0.000008057773,0.00020672297],"genre_scores_gemma":[0.9980432,0.00007698376,0.0013579378,0.00003643304,0.00004829638,0.0000033603553,0.0003600495,0.0000032789155,0.000070491114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851775,0.00010982168,0.00062944106,0.00028081797,0.00020984538,0.000252338],"domain_scores_gemma":[0.99910545,0.00014015773,0.00037566095,0.00028064317,0.000048638118,0.000049454058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002584532,0.00014028144,0.00051168056,0.0004318631,0.0000392276,0.000019445617,0.00029946503,0.00003514379,0.00010982443],"category_scores_gemma":[0.00006983078,0.00012133508,0.00009544492,0.0014958967,0.00035322577,0.0001702693,0.000034762048,0.000086931665,0.000012090594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043434226,0.00010234092,0.5212362,0.000020982021,0.00006543607,0.0000055504725,0.0006795224,0.030570688,0.44193265,0.000030496056,0.00014179303,0.0051709176],"study_design_scores_gemma":[0.00019129158,0.00005368397,0.9852587,0.000018037772,0.00007291221,4.2352858e-7,0.00011140752,0.009214859,0.004740876,0.000012102728,0.00018730563,0.00013837751],"about_ca_topic_score_codex":0.05113204,"about_ca_topic_score_gemma":0.1305907,"teacher_disagreement_score":0.46402252,"about_ca_system_score_codex":0.000011831043,"about_ca_system_score_gemma":0.00002761255,"threshold_uncertainty_score":0.95518655},"labels":[],"label_agreement":null},{"id":"W1992978784","doi":"10.1016/j.epsl.2006.08.003","title":"Three-dimensional finite-element modeling of the glacial isostatic adjustment in Fennoscandia","year":2006,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Post-glacial rebound; Geology; Mantle (geology); Ice sheet; Geophysics; Crust; Glacial period; Shear (geology); Seismic tomography; Geodesy; Geomorphology; Petrology","score_opus":0.008118329942388716,"score_gpt":0.1779108735213528,"score_spread":0.16979254357896406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992978784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99791545,0.00021561838,0.00010436965,0.0005578357,0.0005220717,0.00020086642,0.00014683402,0.0000071250947,0.00032981165],"genre_scores_gemma":[0.9986164,0.0000063630505,0.00056782534,0.00060418085,0.00011055561,7.0882936e-7,0.00008289589,0.0000015746923,0.000009515665],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9986371,0.000038159913,0.00025929435,0.00026516247,0.000444154,0.00035615978],"domain_scores_gemma":[0.9996089,0.000080829486,0.00007641847,0.0001547017,0.000012562663,0.000066633525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038263304,0.0001248741,0.00016016456,0.000096084696,0.00018149694,0.000045952776,0.00023116526,0.00002436887,0.00031031607],"category_scores_gemma":[0.000009959952,0.000083969506,0.000026935712,0.00026941445,0.00025017394,0.00019808798,0.000024655066,0.00008602618,0.000019669525],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003436329,0.000012026466,0.31590724,0.000016466049,0.0000037680377,0.000008000734,0.00006962594,0.6802173,0.0023325582,0.00006517991,0.00020132534,0.0011321565],"study_design_scores_gemma":[0.00021045988,0.00003705327,0.7371319,0.000023580893,0.000006209629,0.00000317696,0.0000066246985,0.26181436,0.00015468567,0.0003697672,0.00014276704,0.00009942172],"about_ca_topic_score_codex":0.01851439,"about_ca_topic_score_gemma":0.0141404895,"teacher_disagreement_score":0.42122465,"about_ca_system_score_codex":0.0000020815398,"about_ca_system_score_gemma":0.00006148054,"threshold_uncertainty_score":0.98802143},"labels":[],"label_agreement":null},{"id":"W1993281405","doi":"10.1103/physreve.67.026412","title":"Theoretical model of x-ray scattering as a dense matter probe","year":2003,"lang":"en","type":"article","venue":"Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":219,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Laboratory Directed Research and Development; Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"Physics; Scattering; Degenerate energy levels; Plasma; Structure factor; Compton scattering; Electron; Random phase approximation; Omega; Warm dense matter; Atomic physics; Dynamic structure factor; Compton wavelength; Coupling (piping); Thomson scattering; Computational physics; Condensed matter physics; Quantum mechanics; Inelastic scattering; Inelastic neutron scattering","score_opus":0.009636408302472836,"score_gpt":0.2703092201472366,"score_spread":0.26067281184476376,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993281405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79373515,0.006087171,0.04146584,0.0032873792,0.002239039,0.002646123,0.0019893835,0.00021888393,0.14833105],"genre_scores_gemma":[0.9951418,0.0010170265,0.0028047536,0.0002966372,0.00019138353,0.000011018327,0.00016147288,0.000023245782,0.0003526745],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9975221,0.000246268,0.0007210848,0.00060445705,0.00038853803,0.0005175538],"domain_scores_gemma":[0.99869263,0.00033209697,0.00017097549,0.0004036021,0.000098779674,0.00030188757],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002831458,0.00041042993,0.0009120466,0.000036809222,0.00020110326,0.00006414011,0.00026274586,0.00010968829,0.002027195],"category_scores_gemma":[0.000109774206,0.00030923734,0.00018777205,0.00013831985,0.00079308427,0.00022915573,0.00015319238,0.0003905484,0.0005119234],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012631924,0.00044118604,0.0009433262,0.0022699398,0.00022707034,0.00004410472,0.0010061458,0.0016940674,0.0036259883,0.9771232,0.0029840267,0.009514639],"study_design_scores_gemma":[0.0004391081,0.0004042668,0.0019445377,0.0007267401,0.0003216589,0.000026550373,0.00004288991,0.059286993,0.0013916778,0.93447995,0.00038348036,0.00055212696],"about_ca_topic_score_codex":0.000024501525,"about_ca_topic_score_gemma":0.000002967783,"teacher_disagreement_score":0.20140666,"about_ca_system_score_codex":0.000008349347,"about_ca_system_score_gemma":0.00006395146,"threshold_uncertainty_score":0.999936},"labels":[],"label_agreement":null},{"id":"W1993495470","doi":"10.1063/1.3615936","title":"First-principles study of liquid gallium at ambient and high pressure","year":2011,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"RIKEN","keywords":"Gallium; Ambient pressure; Chemical physics; Molecular dynamics; Line (geometry); Materials science; k-nearest neighbors algorithm; Condensed matter physics; Crystallography; Thermodynamics; Physics; Chemistry; Computational chemistry; Geometry; Metallurgy; Computer science","score_opus":0.02550275485534807,"score_gpt":0.2042898785845401,"score_spread":0.17878712372919203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993495470","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992606,0.00017044894,0.000011532017,0.000035825775,0.00017308035,0.00009579114,0.00002303417,0.0000038034655,0.00022585734],"genre_scores_gemma":[0.9995507,0.00005200302,0.000100197714,0.00002033074,0.00023763547,2.0403003e-7,0.0000018372612,0.0000035250218,0.00003358045],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991442,0.00006178821,0.0003039417,0.000078474855,0.00027641395,0.00013516516],"domain_scores_gemma":[0.9992309,0.000106390704,0.00032924776,0.00016841164,0.00008586837,0.00007913195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002700609,0.000102285536,0.00026236364,0.000011056941,0.00005583668,0.000009943992,0.00028838692,0.000031896016,0.00021925733],"category_scores_gemma":[0.000015484706,0.00005906207,0.00004341597,0.00005544764,0.00009437145,0.00010309556,0.000058679394,0.000106217194,0.0000071377794],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013912029,0.0037681246,0.08395141,0.00078606716,0.002397248,0.00007352439,0.053813778,0.036390956,0.79754156,0.0020576562,0.003988911,0.0013187029],"study_design_scores_gemma":[0.0017098081,0.0032046768,0.13223438,0.000099587895,0.0008241039,0.00003713963,0.00044317875,0.0009858753,0.850317,0.007626721,0.002159648,0.00035788707],"about_ca_topic_score_codex":0.0005433874,"about_ca_topic_score_gemma":0.000034989105,"teacher_disagreement_score":0.0533706,"about_ca_system_score_codex":0.0000015292318,"about_ca_system_score_gemma":0.00001302214,"threshold_uncertainty_score":0.24084812},"labels":[],"label_agreement":null},{"id":"W1994023511","doi":"10.1029/2009jb007199","title":"Layered convection and the impacts of the perovskite‐postperovskite phase transition on mantle dynamics under isochemical conditions","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mantle (geology); Mantle convection; Geology; Transition zone; Geophysics; Core–mantle boundary; Convection; Physics; Mechanics; Lithosphere; Tectonics; Seismology","score_opus":0.01437133996648712,"score_gpt":0.29947296581061794,"score_spread":0.28510162584413085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994023511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99615735,0.00005620452,0.000050325652,0.002554852,0.00034935496,0.00021322927,0.00013607826,0.0000042509346,0.00047838467],"genre_scores_gemma":[0.9993009,0.000065305205,0.00005930044,0.00010116418,0.0003806641,0.0000012646448,0.00001357265,0.0000054016123,0.00007245233],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9981663,0.00036492443,0.00032287964,0.00013409747,0.00073123147,0.00028056322],"domain_scores_gemma":[0.99806994,0.0010474564,0.00019327429,0.00021315893,0.00031776517,0.00015841702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008989183,0.00011642171,0.00027400113,0.000017314176,0.00031185301,0.00011048961,0.0003032225,0.0000853342,0.0005600113],"category_scores_gemma":[0.00027258205,0.000057891473,0.00015896968,0.00022741953,0.0008683811,0.0001949462,0.000024099407,0.00075290666,0.000019424817],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01132435,0.0017392026,0.0055060266,0.00025489856,0.00071075984,0.000047680882,0.0029551336,0.002367873,0.87492365,0.07694504,0.0051619653,0.018063448],"study_design_scores_gemma":[0.017737122,0.0055446047,0.6273491,0.0004655066,0.0003197968,0.00021894187,0.0031084046,0.055998262,0.10029131,0.18631613,0.002000337,0.00065047306],"about_ca_topic_score_codex":0.0018481876,"about_ca_topic_score_gemma":0.0010500264,"teacher_disagreement_score":0.77463233,"about_ca_system_score_codex":0.000007949811,"about_ca_system_score_gemma":0.00012278295,"threshold_uncertainty_score":0.6131731},"labels":[],"label_agreement":null},{"id":"W1994290480","doi":"10.1029/2002jb002026","title":"Symmetric and asymmetric lithospheric extension: Relative effects of frictional‐plastic and viscous strain softening","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":322,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Lithosphere; Geology; Rheology; Softening; Shear (geology); Mantle (geology); Simple shear; Rift; Crust; Mechanics; Tectonics; Petrology; Seismology; Geophysics; Materials science; Physics; Composite material","score_opus":0.017486760400286377,"score_gpt":0.27013521476684266,"score_spread":0.25264845436655625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994290480","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99099785,0.0068498114,0.00053203135,0.000046895577,0.00034032523,0.0001697075,0.000016177608,0.000006436413,0.0010407759],"genre_scores_gemma":[0.99506354,0.0006826484,0.00387618,0.000012234475,0.00020038143,0.000001028538,0.0000016751956,0.000008277961,0.00015404768],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9972657,0.0005659214,0.00044815463,0.00026097332,0.0010222212,0.00043701608],"domain_scores_gemma":[0.99282366,0.0059168465,0.00028660704,0.00013817196,0.0004926912,0.00034203377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012122706,0.00017672179,0.0005080048,0.00008854976,0.00022577438,0.00010920071,0.00016603898,0.00009008348,0.00014417386],"category_scores_gemma":[0.004044949,0.00012681574,0.00009136188,0.0012777499,0.00025438113,0.00041414044,0.000037885402,0.0004810411,0.00001792869],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028562753,0.0020646781,0.22682846,0.0033992794,0.0024873938,0.0024405776,0.0028367827,0.003422764,0.06971485,0.12460476,0.004055891,0.5552883],"study_design_scores_gemma":[0.0010415493,0.0030145035,0.9573206,0.00025388855,0.000089754205,0.00008650042,0.00023882107,0.001371411,0.0016455698,0.03357992,0.001129459,0.00022808008],"about_ca_topic_score_codex":0.00056813145,"about_ca_topic_score_gemma":0.000017959963,"teacher_disagreement_score":0.7304921,"about_ca_system_score_codex":0.000009153362,"about_ca_system_score_gemma":0.00015863068,"threshold_uncertainty_score":0.51713955},"labels":[],"label_agreement":null},{"id":"W1994538123","doi":"10.1029/2007jb005009","title":"Imaging mantle discontinuities using least squares Radon transform","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Classification of discontinuities; Seismology; Discontinuity (linguistics); Lithosphere; Mantle (geology); Subduction; Radon transform; Radon; Passive seismic; Bedrock; Geophysics; Tectonics; Geomorphology","score_opus":0.0316318417854828,"score_gpt":0.31053137622616944,"score_spread":0.27889953444068666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994538123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99313086,0.00088508235,0.0009177347,0.00027193766,0.00047951506,0.00014637111,0.000030988387,0.000012849473,0.004124629],"genre_scores_gemma":[0.99654627,0.000073099895,0.0014408109,0.000023546416,0.0014706249,2.4644442e-7,0.000004630933,0.000010882188,0.00042991567],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9969265,0.00018000686,0.00055910205,0.00020285789,0.0012825306,0.0008490058],"domain_scores_gemma":[0.9982962,0.00059764774,0.00019276957,0.00018256085,0.00038484656,0.00034599993],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002158941,0.00018097473,0.00040909625,0.000053502754,0.00032174535,0.00028623277,0.0004834171,0.000055413617,0.0011349572],"category_scores_gemma":[0.00013878221,0.00012870444,0.00020596482,0.00033694287,0.00033066142,0.00072078395,0.000032054686,0.0005025082,0.00009349198],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0048843115,0.00082523335,0.13054463,0.00053495105,0.0005803525,0.002766354,0.0045811157,0.0034049493,0.15047818,0.0060284585,0.008583668,0.6867878],"study_design_scores_gemma":[0.0025327061,0.0018986098,0.8402794,0.00069450994,0.00013693691,0.00025157942,0.0076760785,0.0070460606,0.043325305,0.054518256,0.04065212,0.0009884587],"about_ca_topic_score_codex":0.006558478,"about_ca_topic_score_gemma":0.0009893418,"teacher_disagreement_score":0.70973474,"about_ca_system_score_codex":0.00001867313,"about_ca_system_score_gemma":0.0001726336,"threshold_uncertainty_score":0.99977815},"labels":[],"label_agreement":null},{"id":"W1995087097","doi":"10.1016/j.tecto.2013.08.011","title":"3-D crust and mantle structure in southern Ontario, Canada via receiver function imaging","year":2013,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Lithosphere; Crust; Seismology; Classification of discontinuities; Graben; Discontinuity (linguistics); Receiver function; Mantle (geology); Subduction; Geophysics; Tectonics","score_opus":0.0027912142924200562,"score_gpt":0.1397360831180032,"score_spread":0.13694486882558315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995087097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977871,0.000049993152,0.000021661832,0.000057915608,0.00038613315,0.00013693466,0.00007673356,0.000016395557,0.0014671091],"genre_scores_gemma":[0.99913585,0.0000017940225,0.000086895874,0.00016783879,0.0001099694,0.0000012726454,0.00006453213,0.0000044672506,0.0004273928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933827,0.000021529591,0.000117298725,0.00018839768,0.00012199208,0.00021252983],"domain_scores_gemma":[0.99972045,0.0000211826,0.00004839841,0.00012459946,0.00002477557,0.000060594997],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000032180422,0.000118146454,0.00013842575,0.000021982927,0.00007488681,0.00006934949,0.00007960212,0.000028794606,0.0058066733],"category_scores_gemma":[0.0000019994493,0.00009948448,0.000012685155,0.00007475831,0.000027008045,0.00018441373,0.000011962682,0.000104712846,0.00009190033],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009756748,0.000033036817,0.6564706,0.00010036178,0.000081126316,0.000042432162,0.0040024742,0.0040283767,0.043956846,0.00017430216,0.0064608133,0.2845521],"study_design_scores_gemma":[0.0002459339,0.00002401315,0.9861874,0.000009411519,0.000014573632,0.0000024535282,0.00020135389,0.001579947,0.00057250547,0.0078746155,0.0030522943,0.00023551288],"about_ca_topic_score_codex":0.9956324,"about_ca_topic_score_gemma":0.9912014,"teacher_disagreement_score":0.3297168,"about_ca_system_score_codex":0.00001389494,"about_ca_system_score_gemma":0.0001081677,"threshold_uncertainty_score":0.99510217},"labels":[],"label_agreement":null},{"id":"W1995620670","doi":"10.1088/0953-8984/22/9/095503","title":"First-principles studies of liquid lithium under pressure","year":2010,"lang":"en","type":"article","venue":"Journal of Physics Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"RIKEN","keywords":"Lithium (medication); Materials science; Molecular dynamics; Range (aeronautics); Similarity (geometry); Thermodynamics; Phase (matter); Compression (physics); Chemical physics; Electronic structure; Chemistry; Computational chemistry; Physics; Computer science; Organic chemistry","score_opus":0.027151909492662232,"score_gpt":0.24986767872131904,"score_spread":0.22271576922865682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995620670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99602646,0.00038106518,0.00010454019,0.0007303768,0.0015636535,0.00008026327,0.000073373,0.0000070115743,0.0010332415],"genre_scores_gemma":[0.9972613,0.00004209111,0.00079519185,0.00035977233,0.00085547677,3.939723e-7,0.0000042866372,0.000007554546,0.0006739236],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987728,0.00005362016,0.00049184106,0.0001288178,0.00034530775,0.00020759211],"domain_scores_gemma":[0.99846476,0.00025000784,0.0005878457,0.00023352337,0.00037356743,0.000090263],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035000208,0.0001585357,0.0004518728,0.00004908609,0.00007948831,0.00004616694,0.00029598555,0.000073899624,0.0018429448],"category_scores_gemma":[0.000039605915,0.00011387315,0.00014769904,0.00008004756,0.00016123932,0.000287833,0.00003092886,0.00026142984,0.00013214716],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017443295,0.00055464316,0.102915324,0.0020929694,0.004356016,0.00011597707,0.0058907354,0.08792565,0.7095624,0.014815893,0.06886237,0.0011636681],"study_design_scores_gemma":[0.0034542184,0.0020056672,0.3513987,0.00058911886,0.001350849,0.00019333672,0.0010487403,0.0010890225,0.4243079,0.0679527,0.1452131,0.0013966364],"about_ca_topic_score_codex":0.00007242895,"about_ca_topic_score_gemma":0.00008374602,"teacher_disagreement_score":0.2852545,"about_ca_system_score_codex":0.0000012778504,"about_ca_system_score_gemma":0.00006228132,"threshold_uncertainty_score":0.9990695},"labels":[],"label_agreement":null},{"id":"W1996412456","doi":"10.1038/417536a","title":"An inverted continental Moho and serpentinization of the forearc mantle","year":2002,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":626,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; University of British Columbia","funders":"Oregon State University","keywords":"Forearc; Geology; Mantle wedge; Mantle (geology); Lithosphere; Subduction; Seismology; Geophysics; Upwelling; Underplating; Petrology; Tectonics","score_opus":0.005716669338353602,"score_gpt":0.18931607415428106,"score_spread":0.18359940481592746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996412456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970564,0.00022937263,0.0000019987658,0.000171305,0.00024300494,0.0000725912,0.00009099448,0.0000076022043,0.0021266963],"genre_scores_gemma":[0.9994765,0.000019715977,0.000044306682,0.00016478787,0.000050513536,1.3218249e-7,0.000042756317,0.0000012428046,0.00020006242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996819,0.00002530733,0.00005733696,0.00007473534,0.00009564053,0.00006508182],"domain_scores_gemma":[0.9998208,0.000010101386,0.000034408647,0.00009092938,0.000020609494,0.000023131995],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00004793431,0.000039537637,0.00005916788,0.000010349064,0.000049452727,0.00002051215,0.00008823061,0.00013302096,0.0011191868],"category_scores_gemma":[0.000009216506,0.00002398551,0.000012293463,0.00006630144,0.000028163287,0.00008921338,0.0000066001458,0.00012140132,0.000011080778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003674224,0.00006571538,0.93703675,0.0000747351,0.000039222694,0.000003435545,0.00093721645,0.00018499634,0.025937859,0.0016418849,0.013373601,0.020667847],"study_design_scores_gemma":[0.0002005849,0.000034964927,0.97721446,0.0000098433975,0.000011901746,0.000002663269,0.000028755721,0.010394329,0.005836245,0.00055076624,0.00565414,0.0000613752],"about_ca_topic_score_codex":0.0002487354,"about_ca_topic_score_gemma":0.00027809624,"teacher_disagreement_score":0.040177684,"about_ca_system_score_codex":2.2828578e-7,"about_ca_system_score_gemma":0.000002216535,"threshold_uncertainty_score":0.99979395},"labels":[],"label_agreement":null},{"id":"W1996493171","doi":"10.1029/2007gl031932","title":"Empirical transfer functions: Application to determination of outermost core velocity structure using <i>SmKS</i> phases","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Waveform; Seismogram; Deconvolution; Transfer function; Core (optical fiber); Geology; Gaussian; Stack (abstract data type); Computational physics; Physics; Optics; Computer science; Seismology","score_opus":0.06250673636538946,"score_gpt":0.3485920917965348,"score_spread":0.2860853554311453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996493171","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9512719,0.000010855096,0.04721279,0.00045742397,0.0001911778,0.00042522472,0.00031101497,0.000023845438,0.000095803654],"genre_scores_gemma":[0.99750614,0.0000014760984,0.001324845,0.00046679235,0.0004940612,0.000003476961,0.00016924429,0.0000070437604,0.000026926786],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99785495,0.00010720326,0.00029580446,0.00037829904,0.0008138491,0.00054990855],"domain_scores_gemma":[0.9988509,0.00040937078,0.000038925486,0.00027897194,0.00019350594,0.00022832635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005809008,0.00014695044,0.00023622581,0.00017239699,0.00024058018,0.000060316925,0.00027674017,0.00008028309,0.0001894629],"category_scores_gemma":[0.000086712214,0.00012551605,0.00007280295,0.0006390363,0.00019570882,0.00019751689,0.00002705139,0.00023484914,0.00007984367],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002677468,0.00006481658,0.004838932,0.000050580697,0.000016307436,0.000011818243,0.00036074952,0.00056672184,0.9498183,0.000056954403,0.0007292079,0.043217856],"study_design_scores_gemma":[0.0015043713,0.0010013779,0.68311703,0.00012463024,0.00009693107,0.000014583053,0.00030175995,0.017019188,0.27294168,0.0030728874,0.01981887,0.0009867111],"about_ca_topic_score_codex":0.0019375214,"about_ca_topic_score_gemma":0.00043089726,"teacher_disagreement_score":0.6782781,"about_ca_system_score_codex":0.000016808784,"about_ca_system_score_gemma":0.00005146334,"threshold_uncertainty_score":0.51183957},"labels":[],"label_agreement":null},{"id":"W1997308216","doi":"10.1103/physrevlett.89.195507","title":"Structural Stability and Phase Transitions in<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:msub><mml:mi mathvariant=\"normal\">K</mml:mi><mml:mn>8</mml:mn></mml:msub><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">S</mml:mi><mml:mi mathvariant=\"normal\">i</mml:mi></mml:mrow><mml:mn>46</mml:mn></mml:msub></mml:math>Clathrate under High Pressure","year":2002,"lang":"lv","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences; University of Ottawa","funders":"","keywords":"Isostructural; Crystallography; Physics; Phase transition; Ab initio; Phonon; Phase (matter); Materials science; Crystal structure; Condensed matter physics; Chemistry; Quantum mechanics","score_opus":0.018562033630468374,"score_gpt":0.23684460614228545,"score_spread":0.21828257251181707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997308216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8262101,0.006555408,0.0008373197,0.004497559,0.0044588535,0.00018348683,0.003853314,0.00034652717,0.15305747],"genre_scores_gemma":[0.9785697,0.0062529617,0.0015622579,0.0051481244,0.0030576363,0.00089494523,0.0037354052,0.000631008,0.00014796664],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.98620975,0.0012548693,0.0029261555,0.0027630886,0.0031220547,0.003724097],"domain_scores_gemma":[0.990518,0.0018113175,0.0025118478,0.0030660897,0.00020447533,0.001888279],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"category_scores_codex":[0.0026823129,0.0015159807,0.00085017795,0.0005283951,0.002477962,0.0023608392,0.0027817546,0.0017395207,0.5367804],"category_scores_gemma":[0.0008511118,0.0026329793,0.0022704073,0.0017736895,0.0023912387,0.003236391,0.001403644,0.00245772,0.0028238955],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027398618,0.0012175684,0.000048546455,0.009730973,0.0038933614,0.003966183,0.004959141,0.0069658286,0.012547468,0.43302974,0.5163542,0.0045470987],"study_design_scores_gemma":[0.0044289734,0.0024992265,0.0006132985,0.0041176416,0.0052514146,0.0019343169,0.0010791683,0.041615732,0.9211051,0.00089932885,0.01235149,0.0041043344],"about_ca_topic_score_codex":0.0037175776,"about_ca_topic_score_gemma":0.0021964586,"teacher_disagreement_score":0.9085576,"about_ca_system_score_codex":0.000015511097,"about_ca_system_score_gemma":0.0011117366,"threshold_uncertainty_score":0.99984366},"labels":[],"label_agreement":null},{"id":"W1997897225","doi":"10.1039/c2cp40160f","title":"Structural phase transitions induced by pressure in ammonium borohydride","year":2012,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Steacie Institute for Molecular Sciences","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Orthorhombic crystal system; Rietveld refinement; Raman spectroscopy; Powder diffraction; Crystallography; Borohydride; Diffraction; Ab initio; Phase (matter); Chemistry; Synchrotron radiation; Phase transition; Ab initio quantum chemistry methods; X-ray crystallography; Materials science; Crystal structure; Thermodynamics; Molecule; Organic chemistry; Physics","score_opus":0.013006464605161564,"score_gpt":0.24126253751204135,"score_spread":0.2282560729068798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997897225","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960441,0.00010849581,0.000021092534,0.00010444714,0.000118877964,0.00014523606,0.0008393659,0.00007130338,0.0025470525],"genre_scores_gemma":[0.9970331,0.00000239346,0.00005425266,0.0000653704,0.0016572322,0.000008638996,0.001115178,0.000014276249,0.00004951984],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9982853,0.00003411163,0.00026740436,0.00037142026,0.0003313947,0.0007103734],"domain_scores_gemma":[0.999137,0.00008492731,0.00009176401,0.00030105395,0.00003253345,0.00035272603],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00006701236,0.00032090006,0.0004188204,0.000008517962,0.00007713635,0.00005522264,0.00030582512,0.00013247748,0.00040302638],"category_scores_gemma":[0.000017822027,0.00029234073,0.00013897473,0.00024212446,0.00011182525,0.00044945843,0.000026641985,0.00037072293,0.00008003566],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007527367,0.00034110167,0.00034316356,0.00008434695,0.00003376429,0.0000013706274,0.00029491313,0.00015155027,0.99646014,0.00007072962,0.0005182217,0.0016254529],"study_design_scores_gemma":[0.0008587237,0.000021939757,0.000570666,0.000016132653,0.000063792366,0.0000017764316,0.000019921534,0.0044722767,0.9900929,0.0022703859,0.001184249,0.0004272819],"about_ca_topic_score_codex":0.00027317202,"about_ca_topic_score_gemma":0.000001861089,"teacher_disagreement_score":0.0063672573,"about_ca_system_score_codex":0.000008779004,"about_ca_system_score_gemma":0.000027619608,"threshold_uncertainty_score":0.99995285},"labels":[],"label_agreement":null},{"id":"W1997901857","doi":"10.1016/j.polar.2014.09.001","title":"Regional seismic wave propagation (Lg &amp; Sn phases) in the Amerasia Basin and High Arctic","year":2014,"lang":"en","type":"article","venue":"Polar Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geology; Continental crust; Crust; Structural basin; Seismology; Ridge; Continental shelf; Seismic refraction; Arctic; Oceanic crust; Continental margin; Tectonics; Geophysics; Paleontology; Subduction; Oceanography","score_opus":0.017107903844676416,"score_gpt":0.22025735021597073,"score_spread":0.2031494463712943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997901857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708116,0.00006224453,0.00045251276,0.0014908599,0.00022134854,0.00014115342,0.00002254712,0.000010279062,0.00051790994],"genre_scores_gemma":[0.99837756,0.000015485703,0.00058370916,0.00082399946,0.00011526993,0.0000014521119,0.000029797126,0.0000013946869,0.00005131358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888587,0.00011898265,0.0001223635,0.00025935937,0.00036161643,0.00025182514],"domain_scores_gemma":[0.99952865,0.00011238005,0.000059319755,0.00019438332,0.00003891731,0.00006635636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001231897,0.000083125364,0.00009839544,0.0000700536,0.0002590738,0.00020500593,0.0002651949,0.00002184742,0.00014659707],"category_scores_gemma":[0.00011213941,0.00005299734,0.000013479536,0.00033130735,0.00034595167,0.0003645537,0.000014847874,0.00007374175,0.00007316605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017660529,0.0002662864,0.7547896,0.00024248913,0.000024727535,0.000035965095,0.009887451,0.0036275976,0.050648842,0.049109492,0.0016915223,0.12949942],"study_design_scores_gemma":[0.00020369743,0.00007729981,0.9608161,0.000026420925,0.0000077547165,0.000028876799,0.000036702153,0.008903454,0.0003976275,0.008914403,0.020439275,0.00014837409],"about_ca_topic_score_codex":0.01088579,"about_ca_topic_score_gemma":0.0012561759,"teacher_disagreement_score":0.20602651,"about_ca_system_score_codex":0.0000035675453,"about_ca_system_score_gemma":0.00005634108,"threshold_uncertainty_score":0.99570084},"labels":[],"label_agreement":null},{"id":"W1998263865","doi":"10.1007/s00269-009-0347-6","title":"Isothermal compression behavior of (Mg,Fe)O using neon as a pressure medium","year":2009,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Chemistry; Neon; Spin crossover; Compression (physics); Isothermal process; Volume (thermodynamics); Crystallite; Analytical Chemistry (journal); Diffraction; Diamond anvil cell; Crystallography; Synchrotron; X-ray crystallography; Thermodynamics; High pressure; Argon; Optics; Chromatography","score_opus":0.013194040323664207,"score_gpt":0.23521396170970182,"score_spread":0.22201992138603763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998263865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968508,0.00048863346,0.000011929944,0.00003876631,0.00005373778,0.00008117125,0.0001792862,0.000008510643,0.002287152],"genre_scores_gemma":[0.9990063,0.000030635703,0.00020714787,0.000022085836,0.00021806211,5.1966424e-7,0.00005911914,0.0000032638327,0.00045292222],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992464,0.000015877014,0.000220141,0.00016893876,0.00019282966,0.00015579154],"domain_scores_gemma":[0.99950355,0.00002286625,0.00018868306,0.00015939676,0.00005191376,0.00007356563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006715582,0.00013131546,0.00029234853,0.000007677031,0.00004484402,0.000017673028,0.00013057684,0.00006375107,0.00040480235],"category_scores_gemma":[0.000004984886,0.00010925178,0.000053563803,0.000051055984,0.0000711196,0.0000902217,0.000013529368,0.000052854914,0.0000016600885],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032832475,0.00005839183,0.0014031575,0.000110949964,0.00001593096,0.0000018970487,0.00010413082,0.0004722254,0.9948323,0.000023692406,0.000157772,0.0027867677],"study_design_scores_gemma":[0.0003588701,0.00007959909,0.012272817,0.00009341653,0.00010924537,0.0000051126185,0.000025835483,0.0019020038,0.9830033,0.0011592866,0.000818055,0.00017247],"about_ca_topic_score_codex":0.0006539844,"about_ca_topic_score_gemma":0.0000021942953,"teacher_disagreement_score":0.011828963,"about_ca_system_score_codex":5.209961e-7,"about_ca_system_score_gemma":0.00002456981,"threshold_uncertainty_score":0.4455158},"labels":[],"label_agreement":null},{"id":"W1998561539","doi":"10.1029/2005jb003921","title":"Upper mantle velocity‐temperature conversion and composition determined from seismic refraction and heat flow","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique","keywords":"Geology; Mantle (geology); Lithosphere; Core–mantle boundary; Geophysics; Solidus; Mantle wedge; Seismic refraction; Petrology; Seismology; Tectonics; Materials science","score_opus":0.010963374117811035,"score_gpt":0.249413758935008,"score_spread":0.23845038481719696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998561539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983404,0.00050433644,0.00003207211,0.0005501597,0.00021580051,0.00010715243,0.000065392735,0.0000073343394,0.00017733293],"genre_scores_gemma":[0.997507,0.00022151877,0.0011403252,0.00004665289,0.0008287832,4.4296905e-7,0.000049433656,0.000005105435,0.00020079032],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985039,0.00024044765,0.0002458455,0.00019203917,0.00054504187,0.00027267844],"domain_scores_gemma":[0.99905354,0.00039488554,0.000082015125,0.00010153755,0.00020120843,0.00016684266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003541206,0.00012237093,0.00026787596,0.00002175681,0.00026226323,0.00023400036,0.0001150499,0.00009402401,0.00032663287],"category_scores_gemma":[0.00002950633,0.000081590304,0.000053110813,0.00012041266,0.00015485709,0.0004384211,0.00003084945,0.00034708282,0.000044112294],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0046317866,0.00047906503,0.06515423,0.0002990566,0.00028188515,0.00063989224,0.0005837861,0.005532701,0.80895305,0.00019008738,0.029677205,0.08357728],"study_design_scores_gemma":[0.0012711314,0.00090066495,0.92778075,0.00015982833,0.000048700465,0.00004949921,0.00013318019,0.033753425,0.018012006,0.009835327,0.0078192605,0.00023625666],"about_ca_topic_score_codex":0.009548821,"about_ca_topic_score_gemma":0.00019105595,"teacher_disagreement_score":0.8626265,"about_ca_system_score_codex":0.0000095335845,"about_ca_system_score_gemma":0.000052187475,"threshold_uncertainty_score":0.9970467},"labels":[],"label_agreement":null},{"id":"W1998601546","doi":"10.1029/2005jb004024","title":"The thermal structure of subduction zone back arcs","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":413,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria; Dalhousie University","funders":"","keywords":"Subduction; Geology; Mantle (geology); Lithosphere; Geophysics; Volcanic arc; Back-arc basin; Mantle wedge; Hotspot (geology); Slab; Mantle convection; Seismology; Plate tectonics; Thermal; Convection; Tectonics; Mechanics","score_opus":0.016323309362238622,"score_gpt":0.26453292796386996,"score_spread":0.24820961860163132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998601546","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99691725,0.0006777265,0.00002567318,0.00033178696,0.0004084721,0.00010896719,0.00003221267,0.0000035481328,0.0014943415],"genre_scores_gemma":[0.9968688,0.000088214714,0.00048410182,0.0000072539274,0.0016240063,1.8391201e-7,0.0000066938123,0.000005464208,0.0009153152],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99748856,0.00038526516,0.00045017156,0.00013026847,0.0011118874,0.00043384798],"domain_scores_gemma":[0.99812204,0.00073326874,0.0002780953,0.00021856079,0.0005296178,0.000118428514],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007540099,0.0001175411,0.00028041613,0.000015036979,0.00026500315,0.00013932603,0.00049282005,0.00007108923,0.0012800364],"category_scores_gemma":[0.00012254299,0.00006401069,0.0001367001,0.0003059985,0.00038457228,0.00024609457,0.000031764135,0.00044208858,0.000094911244],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0034903053,0.00051783177,0.06893512,0.00022928894,0.0004431394,0.0001273162,0.00043433913,0.017926252,0.73965186,0.011572485,0.045248527,0.11142357],"study_design_scores_gemma":[0.0006586262,0.001315544,0.88551337,0.000064193424,0.000030313262,0.000022550592,0.00020099367,0.00066810707,0.043209467,0.036373664,0.031757567,0.00018563733],"about_ca_topic_score_codex":0.00630266,"about_ca_topic_score_gemma":0.0011372481,"teacher_disagreement_score":0.8165782,"about_ca_system_score_codex":0.000006482867,"about_ca_system_score_gemma":0.00014280493,"threshold_uncertainty_score":0.99963295},"labels":[],"label_agreement":null},{"id":"W1998768110","doi":"10.1103/physrevc.81.045804","title":"Unified description of neutron superfluidity in the neutron-star crust with analogy to anisotropic multiband BCS superconductors","year":2010,"lang":"en","type":"article","venue":"Physical Review C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Superfluidity; Neutron star; Physics; Pairing; Neutron; Nuclear physics; s-process; Anisotropy; Condensed matter physics; Superconductivity; Quantum mechanics; Nuclear reaction","score_opus":0.024106060841460008,"score_gpt":0.2542703956360426,"score_spread":0.2301643347945826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998768110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819356,0.0004723616,0.0000022473596,0.00041901704,0.00019267741,0.00044548002,0.000057505935,0.000009137947,0.00020798827],"genre_scores_gemma":[0.99872816,0.00061090477,0.000111699665,0.000287223,0.00018338385,0.0000064896035,0.000059195943,0.000004024428,0.000008894171],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989466,0.00017142415,0.00019734821,0.00023226601,0.00021162041,0.00024075442],"domain_scores_gemma":[0.9993899,0.000104557184,0.000051936404,0.0003208047,0.000049698516,0.0000831201],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025509478,0.00014763513,0.00039067754,0.000029660861,0.00005416872,0.000029964767,0.00028659232,0.000028970768,0.00022844062],"category_scores_gemma":[0.00003699318,0.00008243212,0.000058626294,0.00026282572,0.000082356724,0.00019292171,0.000013071011,0.00017722455,0.00007277903],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013649312,0.00047733184,0.06434085,0.0012357711,0.000044694803,0.000019097768,0.0014960694,0.0003093058,0.9164458,0.007946243,0.0012154189,0.0063329227],"study_design_scores_gemma":[0.00024030656,0.00034634458,0.9851575,0.00015375363,0.000066318025,0.0000027585072,0.00005124623,0.00015823224,0.001741601,0.00028071486,0.011625096,0.00017612676],"about_ca_topic_score_codex":0.004201384,"about_ca_topic_score_gemma":0.00422975,"teacher_disagreement_score":0.92081666,"about_ca_system_score_codex":0.0000019152642,"about_ca_system_score_gemma":0.000035259465,"threshold_uncertainty_score":0.6351263},"labels":[],"label_agreement":null},{"id":"W1998778353","doi":"10.1103/physrevlett.104.035002","title":"Picosecond Short-Range Disordering in Isochorically Heated Aluminum at Solid Density","year":2010,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Agence Nationale de la Recherche","keywords":"Materials science; Warm dense matter; XANES; Picosecond; Spectroscopy; K-edge; Aluminium; Molecular physics; Ultrashort pulse; Lattice (music); Atomic physics; Absorption spectroscopy; Laser; Analytical Chemistry (journal); Optics; Chemistry; Physics","score_opus":0.011324322638296797,"score_gpt":0.2472410270158513,"score_spread":0.2359167043775545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998778353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960757,0.00077673537,0.000010431455,0.0018834103,0.0004144309,0.000311133,0.000033069384,0.000034389213,0.00046068928],"genre_scores_gemma":[0.9947796,0.0007645283,0.0000686377,0.003968552,0.00031504274,0.0000071045383,0.000072520124,0.0000071781037,0.000016827595],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986631,0.00008385526,0.0002765833,0.0003498045,0.00023020615,0.00039640404],"domain_scores_gemma":[0.9993732,0.000108788314,0.00005695822,0.00029629006,0.000019433757,0.00014535789],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022379316,0.00019858402,0.00050231104,0.000027236652,0.00008820461,0.000041932813,0.00024919838,0.000021688931,0.0008254375],"category_scores_gemma":[0.000041765066,0.0001586299,0.00012237152,0.00018181105,0.00007260363,0.00016259057,0.000040960163,0.0002483694,0.00055317336],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007881224,0.00029679827,0.18121505,0.0017382838,0.00009310567,0.00015659894,0.00042996983,0.0005897107,0.77091396,0.00019881706,0.012114882,0.032174017],"study_design_scores_gemma":[0.00044244938,0.00010917363,0.93666065,0.00051110215,0.00011171881,0.000013528358,0.000004087919,0.0027731773,0.0049524256,0.00048703543,0.05300052,0.000934161],"about_ca_topic_score_codex":0.00056051346,"about_ca_topic_score_gemma":0.0019551357,"teacher_disagreement_score":0.7659615,"about_ca_system_score_codex":0.000005224782,"about_ca_system_score_gemma":0.000011687238,"threshold_uncertainty_score":0.9037962},"labels":[],"label_agreement":null},{"id":"W1999653356","doi":"10.1046/j.1365-246x.2000.00159.x","title":"Gravitational stability of spherical self-gravitating relaxation models","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Alexander von Humboldt-Stiftung","keywords":"Instability; Physics; Classical mechanics; Stratification (seeds); Mechanics; Convection; Convective instability; Elastic instability; Gravitation; Viscoelasticity; Geophysics; Thermodynamics","score_opus":0.014584141113308274,"score_gpt":0.23081028130711473,"score_spread":0.21622614019380645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999653356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903905,0.00002433998,0.0010044286,0.00026889698,0.0005877112,0.00007550676,0.00015132954,0.000024995126,0.0074722916],"genre_scores_gemma":[0.9902287,0.000026260204,0.008702382,0.00007585238,0.0006701673,0.0000010426693,0.0001240712,0.000004535827,0.0001669939],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998345,0.000116184965,0.00046734526,0.00019292263,0.00067044655,0.00020807251],"domain_scores_gemma":[0.99910897,0.00018938989,0.0002236721,0.00010314748,0.0002471668,0.00012764367],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031371866,0.00012803107,0.00020605982,0.000040089995,0.00012853375,0.000103417995,0.00029504488,0.000052766063,0.008446135],"category_scores_gemma":[0.00003795065,0.000107000684,0.00013849426,0.00012353397,0.00006753346,0.00057380146,0.000011140936,0.00019253444,0.0002156253],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00299885,0.0028542406,0.09356029,0.00017297514,0.0016974652,0.00016572533,0.008779325,0.24395385,0.047726464,0.05557937,0.005357187,0.53715426],"study_design_scores_gemma":[0.0012728784,0.00042737587,0.6028766,0.00006854583,0.000079615405,0.0000972421,0.00017923967,0.08402131,0.002852359,0.30275834,0.004858221,0.00050829095],"about_ca_topic_score_codex":0.00033801404,"about_ca_topic_score_gemma":0.000020865218,"teacher_disagreement_score":0.53664595,"about_ca_system_score_codex":0.000011459146,"about_ca_system_score_gemma":0.00007031929,"threshold_uncertainty_score":0.99246025},"labels":[],"label_agreement":null},{"id":"W2000139835","doi":"10.1093/gji/ggv086","title":"Deriving crustal properties from the P Coda without deconvolution: the southwestern Superior Province, North America","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Basement; Mafic; Crust; Deconvolution; Receiver function; Felsic; Archean; Sedimentary rock; Lithosphere; Seismology; Petrology; Paleontology; Tectonics; Physics","score_opus":0.024858946590449984,"score_gpt":0.21314373382444265,"score_spread":0.18828478723399267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000139835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99393433,0.00016064789,0.00051076635,0.0020598797,0.002032996,0.00014673278,0.00025430802,0.000026508043,0.00087381795],"genre_scores_gemma":[0.9950593,0.00001972317,0.00016829287,0.0007164556,0.003505763,0.0000035076243,0.000089483845,0.0000069241164,0.00043052746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983673,0.00015882039,0.00030639546,0.00020487348,0.0006748058,0.00028782274],"domain_scores_gemma":[0.999105,0.0001256783,0.00019155342,0.00018775443,0.00021751273,0.0001725386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001982466,0.00017447893,0.00019101976,0.000023198221,0.00039264612,0.0006862633,0.00079426775,0.00003412372,0.00055636454],"category_scores_gemma":[0.00006997893,0.00008489352,0.00010952308,0.000086566506,0.00024789415,0.00047525833,0.00007792521,0.00029826444,0.0006569803],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00079862407,0.00021621138,0.9034818,0.000010611477,0.0007949782,0.00013357811,0.0077446275,0.0119005805,0.0021890495,0.00039647342,0.010267036,0.062066436],"study_design_scores_gemma":[0.00067456986,0.00018392518,0.89286405,0.000050950057,0.000070917245,0.000095809744,0.0012860469,0.008960482,0.00016720867,0.0019298759,0.09338316,0.00033299014],"about_ca_topic_score_codex":0.005394204,"about_ca_topic_score_gemma":0.0029520136,"teacher_disagreement_score":0.08311612,"about_ca_system_score_codex":0.0000139474,"about_ca_system_score_gemma":0.0002324643,"threshold_uncertainty_score":0.8444372},"labels":[],"label_agreement":null},{"id":"W2001100815","doi":"10.1140/epjb/e2013-40178-0","title":"Phase diagram of aluminum from EAM potentials","year":2013,"lang":"en","type":"article","venue":"The European Physical Journal B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Regroupement Québécois sur les Matériaux de Pointe","funders":"","keywords":"Binodal; Spinodal; Phase diagram; Monte Carlo method; Statistical physics; Aluminium; Atom (system on chip); Spinodal decomposition; Diagram; Materials science; Thermodynamics; Physics; Phase (matter); Mathematics; Computer science; Statistics; Metallurgy; Quantum mechanics","score_opus":0.011361450251412483,"score_gpt":0.21924506441491542,"score_spread":0.20788361416350293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001100815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9797584,0.00008184914,0.000089278496,0.00022841689,0.00045954788,0.0000983287,0.000098377604,0.000014811921,0.01917099],"genre_scores_gemma":[0.99689615,0.000026684778,0.000073886404,0.00008683704,0.0027400656,2.1797969e-7,0.00002324769,0.0000068034833,0.00014608864],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998655,0.00051429763,0.00024485824,0.0001161069,0.00025631196,0.00021340737],"domain_scores_gemma":[0.99926084,0.00013529917,0.00019468079,0.0002127471,0.000058959384,0.00013749057],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00035037112,0.00011534395,0.00021482866,0.000017495115,0.00014248202,0.00015657813,0.00045154957,0.0000115903795,0.0011762378],"category_scores_gemma":[0.000025464185,0.00006224299,0.00012102459,0.0000695873,0.00010474638,0.00020352614,0.000030419142,0.00015467154,0.0022577588],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074820586,0.0005591569,0.0004566084,0.000011180257,0.0002260377,0.000071373826,0.0013682648,0.0006800225,0.28195444,0.00017552456,0.02737071,0.68705183],"study_design_scores_gemma":[0.007676095,0.0032547165,0.5847529,0.00025316933,0.00072383246,0.00011279934,0.0006059158,0.00550194,0.08396038,0.27551517,0.03604061,0.0016024772],"about_ca_topic_score_codex":0.00073703413,"about_ca_topic_score_gemma":0.0000045959982,"teacher_disagreement_score":0.68544936,"about_ca_system_score_codex":7.857884e-7,"about_ca_system_score_gemma":0.0000118049,"threshold_uncertainty_score":0.99973685},"labels":[],"label_agreement":null},{"id":"W2001327875","doi":"10.1063/1.1351838","title":"Tailoring sphere density for high pressure physical property measurements on liquids","year":2001,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Alexander von Humboldt-Stiftung","keywords":"Materials science; Spherical shell; SPHERES; Composite number; Grind; Shell (structure); Liquid metal; Composite material; Physical property; Sapphire; Metal; Core (optical fiber); Optics; Metallurgy; Physics","score_opus":0.041005130622792846,"score_gpt":0.2532575835319384,"score_spread":0.21225245290914554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001327875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99335235,0.00067062164,0.000006965719,0.00011972435,0.0018903494,0.0010413786,0.00018823445,0.000026039626,0.0027043044],"genre_scores_gemma":[0.99657476,0.00062861,0.00034417945,0.00012534323,0.00019251501,0.0000121298,0.00015719031,0.00000634383,0.001958917],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980025,0.000086948894,0.00036520418,0.00046567674,0.0007156004,0.00036401858],"domain_scores_gemma":[0.9990147,0.000024992794,0.00021714602,0.00041958416,0.0002075285,0.00011608437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00088850793,0.00019438971,0.0004495203,0.000041236006,0.00028197165,0.00010235737,0.00038041087,0.000041531843,0.0007525332],"category_scores_gemma":[0.00007624569,0.000120782526,0.00012591442,0.00026580002,0.00011495392,0.00025663222,0.00003125491,0.00006661803,0.0002107393],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048196275,0.000798541,0.046155356,0.018159417,0.00045574727,0.00000834265,0.00023368483,0.00014927542,0.029078227,0.0009487539,0.0147977965,0.8887329],"study_design_scores_gemma":[0.0029945297,0.0018744649,0.08234678,0.02108673,0.0009646321,0.000015708385,0.000040903058,0.0021823726,0.16590916,0.0031953973,0.7177525,0.001636826],"about_ca_topic_score_codex":0.00023553974,"about_ca_topic_score_gemma":0.000036873935,"teacher_disagreement_score":0.88709605,"about_ca_system_score_codex":0.0000059079766,"about_ca_system_score_gemma":0.00006657132,"threshold_uncertainty_score":0.82397103},"labels":[],"label_agreement":null},{"id":"W2001529371","doi":"10.1103/physrevlett.102.255503","title":"Single-Crystal Structural Characterization of the Metallic Phase of Oxygen","year":2009,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Monoclinic crystal system; Materials science; Single crystal; Phase (matter); Metal; Raman spectroscopy; Crystal structure; Crystallography; Diffraction; Oxygen; Solid oxygen; Chemistry; Optics; Physics","score_opus":0.018343147627555206,"score_gpt":0.25200225739657933,"score_spread":0.23365910976902413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001529371","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784464,0.00037668674,0.00001237419,0.0012634654,0.00011947795,0.00020337025,0.00010856191,0.000006304217,0.000065095424],"genre_scores_gemma":[0.9978966,0.00013770498,0.000025215359,0.0017342934,0.00011917635,4.592328e-7,0.00008094543,0.0000017080521,0.0000038590906],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9992746,0.000080960795,0.00021689419,0.00011137044,0.00019982547,0.00011633971],"domain_scores_gemma":[0.9995338,0.00002502681,0.00020687444,0.00017929739,0.00002278534,0.00003227153],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007471409,0.0000918486,0.0003014472,0.000010470878,0.000029145216,0.000009918257,0.00019106352,0.000005867597,0.00016082883],"category_scores_gemma":[0.000016082518,0.0000536767,0.00012845689,0.00014087145,0.000053094198,0.00011643535,0.0000076070446,0.000039149727,0.000009188219],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007452084,0.000025903912,0.000090474496,0.00018119754,0.000012837329,3.233139e-7,0.0000404259,0.000021469301,0.9926634,0.00010610936,0.000043093987,0.0068073138],"study_design_scores_gemma":[0.001437077,0.00090303464,0.6442613,0.002295619,0.00079093943,0.0000084303,0.000006491655,0.0031969475,0.32527554,0.0027102116,0.018280093,0.000834336],"about_ca_topic_score_codex":0.000032010725,"about_ca_topic_score_gemma":0.0000015518582,"teacher_disagreement_score":0.66738784,"about_ca_system_score_codex":0.0000010906863,"about_ca_system_score_gemma":0.000007753701,"threshold_uncertainty_score":0.21888722},"labels":[],"label_agreement":null},{"id":"W2002813230","doi":"10.1029/2007jb005538","title":"Time dependence in 3‐D mantle convection models featuring evolving plates: Effect of lower mantle viscosity","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Mantle convection; Mantle (geology); Plate tectonics; Convection; Geology; Geophysics; Viscosity; Mantle wedge; Earth's internal heat budget; Core–mantle boundary; Mechanics; Thermodynamics; Physics; Lithosphere; Tectonics; Seismology","score_opus":0.022792157099672094,"score_gpt":0.27141717786334174,"score_spread":0.24862502076366966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002813230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978291,0.00044152065,0.000046984864,0.000033094744,0.00021884525,0.00017753146,0.000014187182,0.000007769228,0.0012309735],"genre_scores_gemma":[0.9988843,0.00017353162,0.00028415225,0.0000045084585,0.00026550033,9.54614e-7,0.0000033980357,0.0000073968968,0.00037626497],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973288,0.0004601133,0.00043493076,0.00021671194,0.0010692124,0.0004902165],"domain_scores_gemma":[0.998084,0.000992653,0.0002114776,0.00018998056,0.0003350537,0.00018679685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013666067,0.00015933349,0.00052239245,0.000050877854,0.00017407133,0.000055444212,0.0004037174,0.00009276352,0.0008031339],"category_scores_gemma":[0.00028925258,0.000115201845,0.00013510823,0.0004217792,0.00023796686,0.0007465835,0.0000578137,0.0005336031,0.0001700485],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.020377751,0.0020544801,0.31349367,0.0016963213,0.00095740374,0.007450778,0.003805483,0.21722272,0.39348942,0.00043273545,0.01167439,0.027344843],"study_design_scores_gemma":[0.0025199368,0.006592613,0.80215335,0.0008266274,0.00005145274,0.00021995846,0.00013029507,0.103148215,0.077429235,0.006118047,0.0002989381,0.0005113332],"about_ca_topic_score_codex":0.004375595,"about_ca_topic_score_gemma":0.00026155423,"teacher_disagreement_score":0.48865968,"about_ca_system_score_codex":0.000019959287,"about_ca_system_score_gemma":0.0001463816,"threshold_uncertainty_score":0.8793753},"labels":[],"label_agreement":null},{"id":"W2002901351","doi":"10.1038/nature07788","title":"Electronic acceleration of atomic motions and disordering in bismuth","year":2009,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":303,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Bismuth; Excitation; Femtosecond; Excited state; Electron; Materials science; Atomic physics; Phase transition; Valence electron; Condensed matter physics; Crystal structure; Diffraction; Electron diffraction; Laser; Molecular physics; Chemistry; Crystallography; Optics; Physics","score_opus":0.003912320660552376,"score_gpt":0.20652379153096365,"score_spread":0.20261147087041126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002901351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981988,0.0008363538,0.000011791128,0.00022606253,0.00006191184,0.000053814747,0.00001471596,0.0000069726075,0.0005895606],"genre_scores_gemma":[0.9996749,0.000118580196,0.00005561699,0.00006826622,0.00003070777,1.440462e-7,0.000030871786,6.4504803e-7,0.000020248823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99969953,0.000012247884,0.00006543056,0.00007474988,0.000051106963,0.00009694228],"domain_scores_gemma":[0.999902,0.000008146281,0.000021972106,0.00004608881,0.000007754835,0.000014037356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006039425,0.00003846966,0.00006817554,0.00003416733,0.00002388822,0.000015431122,0.000041120376,0.00013181922,0.00007985012],"category_scores_gemma":[0.000006381221,0.00003179946,0.00000867738,0.00008199078,0.0000069653606,0.000089811125,0.000001939867,0.00020069254,0.0000030961883],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020272774,0.00023243013,0.45996597,0.00017474731,0.000062624196,0.000014680783,0.0026314831,0.011288257,0.19484085,0.06967592,0.0013063625,0.25960392],"study_design_scores_gemma":[0.00014628269,0.00005099176,0.98710287,0.000008321296,0.0000033517063,8.6428696e-7,0.000010748403,0.00096373283,0.0015968442,0.00933057,0.00073385565,0.000051570667],"about_ca_topic_score_codex":0.00015548896,"about_ca_topic_score_gemma":0.00072804873,"teacher_disagreement_score":0.52713686,"about_ca_system_score_codex":9.617936e-7,"about_ca_system_score_gemma":0.000012951416,"threshold_uncertainty_score":0.12967443},"labels":[],"label_agreement":null},{"id":"W2002915288","doi":"10.1086/313359","title":"Equation of State and Material Property Measurements of Hydrogen Isotopes at the High‐Pressure, High‐Temperature Insulator‐Metal Transition","year":2000,"lang":"en","type":"article","venue":"The Astrophysical Journal Supplement Series","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Deuterium; Compressibility; Equation of state; Shock wave; Hydrogen; Laser; Shock (circulatory); Atomic physics; Metallic hydrogen; Supercritical fluid; Physics; Shock front; Materials science; Thermodynamics; Optics","score_opus":0.011033410472364835,"score_gpt":0.19124412426198475,"score_spread":0.18021071378961992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002915288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99725854,0.0000757118,0.000020116899,0.00096665486,0.00019026338,0.0002958379,0.0011770035,0.0000053250637,0.000010567422],"genre_scores_gemma":[0.9987064,0.00012207706,0.00046124568,0.00003735819,0.00026709517,0.0000032247399,0.00016771814,0.0000060885577,0.00022877564],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998371,0.0002982085,0.00040372915,0.00014685049,0.0005499384,0.00023027412],"domain_scores_gemma":[0.9994473,0.000028263945,0.00020673769,0.00017138374,0.000082569095,0.00006373389],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035973385,0.00016962767,0.0002922361,0.000020541824,0.0003396439,0.000092056835,0.0002231179,0.0000316525,0.0052882396],"category_scores_gemma":[0.000004261912,0.00007550692,0.0000693004,0.00008433345,0.00021731004,0.0003541121,0.000024033146,0.00010581605,0.000017270544],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025755407,0.000111040106,0.0010856796,0.000077697856,0.00045446257,0.0000037102309,0.0012015788,0.017098052,0.9671185,0.00030367836,0.00046261257,0.009507473],"study_design_scores_gemma":[0.0011572632,0.0012588898,0.077170454,0.000058566275,0.00032839226,0.00002815564,0.00011403682,0.00012152674,0.91014475,0.0070724324,0.0023007211,0.00024479217],"about_ca_topic_score_codex":0.0013852344,"about_ca_topic_score_gemma":0.000113075075,"teacher_disagreement_score":0.07608478,"about_ca_system_score_codex":0.000003859549,"about_ca_system_score_gemma":0.000028156963,"threshold_uncertainty_score":0.9956211},"labels":[],"label_agreement":null},{"id":"W2002916784","doi":"10.1103/physrevlett.106.145502","title":"Controlling the Bonding and Band Gaps of Solid Carbon Monoxide with Pressure","year":2011,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"Engineering and Physical Sciences Research Council","keywords":"Carbon monoxide; Materials science; Chemistry; Organic chemistry","score_opus":0.014569482994758604,"score_gpt":0.22130594895334937,"score_spread":0.20673646595859077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002916784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888497,0.009180682,0.000017990142,0.00071365084,0.000059901413,0.00029779866,0.000033497476,0.000011150906,0.00083559944],"genre_scores_gemma":[0.99763364,0.0010133605,0.000077356475,0.0011489952,0.00010515827,0.000003673034,0.0000041073226,0.000003624021,0.000010105464],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99930686,0.00008030116,0.00014648022,0.00015449719,0.00014330307,0.00016858499],"domain_scores_gemma":[0.9995398,0.00010980423,0.00011747257,0.000164643,0.000016683613,0.000051631167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018292942,0.00011277385,0.00035318738,0.000010015277,0.00005027396,0.000013319641,0.00013002857,0.0000065047666,0.000046479632],"category_scores_gemma":[0.000012961036,0.00005830473,0.00004551525,0.00006691502,0.000099464,0.00007480477,0.000008453772,0.000067120745,0.000005173348],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014203166,0.00047488126,0.21862116,0.022078466,0.0031691652,0.00014923743,0.012953164,0.00512375,0.69742364,0.008504662,0.0073018284,0.022779733],"study_design_scores_gemma":[0.0048517664,0.0020614427,0.66601014,0.014597762,0.007552084,0.000070503476,0.00022729057,0.020869836,0.15150872,0.006668415,0.1220845,0.0034975205],"about_ca_topic_score_codex":0.0007152507,"about_ca_topic_score_gemma":0.00001687796,"teacher_disagreement_score":0.5459149,"about_ca_system_score_codex":4.0978472e-7,"about_ca_system_score_gemma":0.0000066969865,"threshold_uncertainty_score":0.23775978},"labels":[],"label_agreement":null},{"id":"W2002935388","doi":"10.1016/j.tecto.2005.02.013","title":"Upper mantle structure of Arctic Canada from Rayleigh wave dispersion","year":2005,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Mantle (geology); Rayleigh wave; Phase velocity; Geodesy; Seismology; Geophysics; Wave propagation; Physics; Optics","score_opus":0.004931228423618756,"score_gpt":0.16196028327839174,"score_spread":0.15702905485477298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002935388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973783,0.000120242286,0.000014820108,0.000103114566,0.00043068727,0.000089480105,0.0011188549,0.000016119036,0.0007284085],"genre_scores_gemma":[0.9983083,0.000012346904,0.000690562,0.00013149071,0.00046343112,2.1632101e-7,0.00029015663,0.0000053893555,0.00009810864],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991491,0.000026591402,0.00017249853,0.00019652312,0.00024200979,0.00021331932],"domain_scores_gemma":[0.99948716,0.000062213054,0.00009251473,0.00024452087,0.00003783293,0.000075762546],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000023490607,0.00013683162,0.00022008784,0.000016731741,0.00006942782,0.000021553233,0.00015807858,0.000045608514,0.0037722404],"category_scores_gemma":[0.000006356914,0.00010858292,0.000043528682,0.000090160334,0.00003793308,0.00011845163,0.000016588892,0.00008184553,0.00005361014],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003538233,0.00016192142,0.092973344,0.00030615818,0.0004820282,0.000055756955,0.0018424261,0.023268016,0.7178214,0.0026446355,0.0107779605,0.1493125],"study_design_scores_gemma":[0.0008065947,0.00013368302,0.5753048,0.0000759682,0.00013345905,0.0000033301558,0.00012572022,0.0047882344,0.3744624,0.010359333,0.033063382,0.00074308354],"about_ca_topic_score_codex":0.6989281,"about_ca_topic_score_gemma":0.4171107,"teacher_disagreement_score":0.48233148,"about_ca_system_score_codex":0.000009528543,"about_ca_system_score_gemma":0.000112531015,"threshold_uncertainty_score":0.99713844},"labels":[],"label_agreement":null},{"id":"W2003143784","doi":"10.1038/35019050","title":"Evidence for a late chondritic veneer in the Earth's mantle from high-pressure partitioning of palladium and platinum","year":2000,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Palladium; Silicate; Platinum; Platinum group; Mantle (geology); Geology; Solubility; Iridium; Osmium; Rhodium; Mineralogy; Geochemistry; Chemistry; Ruthenium; Physical chemistry","score_opus":0.015067780430598162,"score_gpt":0.23533471077920465,"score_spread":0.22026693034860648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003143784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939778,0.0043258606,0.0000036490253,0.0005005784,0.00021475287,0.00019074166,0.0004886278,0.00000795649,0.0002900406],"genre_scores_gemma":[0.9986562,0.00016058321,0.00039367212,0.00029913586,0.00016866234,0.000003834379,0.0000921408,0.0000025601764,0.00022321439],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993579,0.00005619598,0.00012800925,0.00015928138,0.00014425245,0.0001544046],"domain_scores_gemma":[0.9994388,0.00034024633,0.00003785139,0.00013579799,0.00002046127,0.000026838114],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018631,0.0000789659,0.00014186818,0.000018183056,0.00006474863,0.000051720508,0.00014354127,0.00021733722,0.0014747313],"category_scores_gemma":[0.00004146473,0.000053658896,0.000024126686,0.000075822725,0.00003304316,0.0001375027,0.0000047804933,0.00024982815,0.000017482766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003981163,0.00036098532,0.63197434,0.002114915,0.0007275791,0.00024275862,0.023653693,0.088617004,0.07789418,0.007834005,0.031305596,0.13129376],"study_design_scores_gemma":[0.00046968955,0.00008292861,0.968744,0.0002165896,0.000053437496,0.000001773124,0.000039695457,0.001666553,0.0019158728,0.006553894,0.020113435,0.0001421605],"about_ca_topic_score_codex":0.0013647514,"about_ca_topic_score_gemma":0.0011658664,"teacher_disagreement_score":0.3367696,"about_ca_system_score_codex":3.9505383e-7,"about_ca_system_score_gemma":0.000013603585,"threshold_uncertainty_score":0.99943805},"labels":[],"label_agreement":null},{"id":"W2003347652","doi":"10.1103/physrevb.69.132101","title":"Electron-phonon coupling in high-pressure Nb","year":2004,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Pseudopotential; Brillouin zone; Condensed matter physics; Fermi surface; Coupling (piping); Phonon; Physics; Fermi level; Plane wave; Topology (electrical circuits); Electron; Materials science; Superconductivity; Quantum mechanics","score_opus":0.00895869051214711,"score_gpt":0.2497637588691399,"score_spread":0.24080506835699278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003347652","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97596014,0.021407584,0.00003060738,0.0005796576,0.00025646653,0.00035792924,0.000046423047,0.000043515472,0.0013177055],"genre_scores_gemma":[0.9935206,0.0055235173,0.000099168275,0.00041872854,0.00033273365,0.0000058061173,0.00006774191,0.0000052901496,0.000026412186],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9989159,0.000032587075,0.00021718215,0.0002722376,0.00021682258,0.00034526092],"domain_scores_gemma":[0.9995252,0.00006147339,0.00007310988,0.00022458169,0.000022639511,0.00009303329],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002050292,0.00015668652,0.00043387336,0.00002158996,0.000051400086,0.000033790406,0.00022193408,0.00002680654,0.00036188425],"category_scores_gemma":[0.00003853897,0.000120006,0.000079537065,0.00022800788,0.000029842085,0.00015567956,0.00001520394,0.00014235725,0.0008682906],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047869675,0.0023892422,0.033008646,0.019203877,0.0006621967,0.00041742585,0.0010440515,0.6042166,0.064204454,0.19176953,0.0074911914,0.07511411],"study_design_scores_gemma":[0.004824918,0.0012920275,0.37261915,0.00973093,0.00087480573,0.000018745504,0.000018873447,0.012405268,0.03486102,0.32677078,0.23327577,0.0033076918],"about_ca_topic_score_codex":0.0022533506,"about_ca_topic_score_gemma":0.00024099606,"teacher_disagreement_score":0.5918113,"about_ca_system_score_codex":0.000004051187,"about_ca_system_score_gemma":0.00004808481,"threshold_uncertainty_score":0.99990964},"labels":[],"label_agreement":null},{"id":"W2005888050","doi":"10.1007/s00410-003-0442-5","title":"Diamond formation and source carbonation: mineral associations in diamonds from Namibia","year":2003,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canada Research Chairs; Deutsche Forschungsgemeinschaft","keywords":"Geology; Phlogopite; Peridotite; Geochemistry; Coesite; Mineral; Olivine; Metamorphic rock; Kimberlite; Mantle (geology); Pseudomorph; Pyroxene; Eclogite; Diamond; Mineralogy; Quartz; Materials science; Paleontology; Tectonics","score_opus":0.006040092586197932,"score_gpt":0.21459924664291577,"score_spread":0.20855915405671785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005888050","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942273,0.0006396783,0.00086223055,0.0015387028,0.00028363604,0.00014171249,0.001093435,0.000016958891,0.0011963485],"genre_scores_gemma":[0.9981232,0.000042715386,0.00021318097,0.00040690802,0.00010803965,0.000009434225,0.0008566491,0.0000022767742,0.00023757764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900925,0.00022503099,0.00022617476,0.00020997353,0.00006192253,0.0002676295],"domain_scores_gemma":[0.99939775,0.00028374116,0.00006118138,0.000093538925,0.000058934238,0.00010482298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027204995,0.00011038343,0.00023342921,0.000119934535,0.00016800824,0.000040445066,0.000052090076,0.0001386592,0.00023079179],"category_scores_gemma":[0.00021382252,0.000105110295,0.00001998205,0.00014247175,0.000063634034,0.00015658468,0.000010722909,0.00009674641,0.000027244349],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007201438,0.000053439384,0.9612741,0.000008181285,0.0000690497,0.00001542751,0.0011724802,0.0019268142,0.0076802652,0.022443315,0.002459896,0.002825029],"study_design_scores_gemma":[0.00084853196,0.00010325375,0.9635962,0.0000033288488,0.00003384517,0.000010222534,0.00003063931,0.001892108,0.00008846327,0.00628156,0.026956003,0.00015579509],"about_ca_topic_score_codex":0.003179637,"about_ca_topic_score_gemma":0.016520962,"teacher_disagreement_score":0.024496106,"about_ca_system_score_codex":0.000007933311,"about_ca_system_score_gemma":0.000026090562,"threshold_uncertainty_score":0.92190844},"labels":[],"label_agreement":null},{"id":"W2006098558","doi":"10.1088/1742-6596/500/0/001002","title":"18th APS-SCCM and 24th AIRAPT","year":2014,"lang":"en","type":"article","venue":"Journal of Physics Conference Series","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Library science; Multidisciplinary approach; Metropolitan area; Chinese academy of sciences; Engineering physics; Engineering; Computer science; History; Sociology; Social science; Archaeology; China","score_opus":0.012788449498267601,"score_gpt":0.19610164397141625,"score_spread":0.18331319447314864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006098558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98782295,0.00015307298,0.0040906733,0.00050682935,0.0009204957,0.00006584401,0.000048889167,0.000015493044,0.006375774],"genre_scores_gemma":[0.9980959,0.0001377416,0.00088267785,0.00008381812,0.00062240334,1.4526717e-7,0.000007278891,0.0000031850263,0.0001668427],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9991953,0.00006834445,0.00024332164,0.00010496415,0.00021539067,0.00017270405],"domain_scores_gemma":[0.9992899,0.000061763065,0.0002596827,0.000114716444,0.00016020099,0.00011375715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025917208,0.000121469035,0.00028958716,0.000028578843,0.00009764617,0.00016836725,0.00017975579,0.00003662655,0.00029093583],"category_scores_gemma":[0.000028828304,0.000088904846,0.00004980638,0.00006490459,0.0001196079,0.0006091696,0.000015640308,0.00011157818,0.00003095806],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004003836,0.00009524686,0.040934287,0.00023103987,0.00023902113,0.00003608971,0.0030535187,0.0009454649,0.028507762,0.17065573,0.0024545614,0.7524469],"study_design_scores_gemma":[0.0016706791,0.0028225256,0.32570657,0.0002887588,0.00021633478,0.0001762527,0.0008910872,0.0011733901,0.11176978,0.45047808,0.10377739,0.0010291628],"about_ca_topic_score_codex":0.000117575124,"about_ca_topic_score_gemma":0.000073566196,"teacher_disagreement_score":0.75141776,"about_ca_system_score_codex":9.901465e-7,"about_ca_system_score_gemma":0.00006551248,"threshold_uncertainty_score":0.36254343},"labels":[],"label_agreement":null},{"id":"W2006623615","doi":"10.1111/j.1365-246x.2004.02447.x","title":"Normal-mode theory of a rotating earth model using a Lagrangian perturbation of a spherical model of reference","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Spherical coordinate system; Spherical harmonics; Classical mechanics; Physics; Superposition principle; Equations of motion; Perturbation (astronomy); Bipolar coordinates; Cylindrical coordinate system; Hydrostatic equilibrium; Coordinate system; Isotropy; Generalized coordinates; Mathematical analysis; Mechanics; Mathematics; Geometry; Optics; Quantum mechanics","score_opus":0.029783079723644808,"score_gpt":0.2546097070014421,"score_spread":0.2248266272777973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006623615","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9263335,0.000016836211,0.07187373,0.000040921463,0.00012241029,0.000052702675,0.00021128258,0.000004663012,0.0013439385],"genre_scores_gemma":[0.9704479,0.000010997681,0.02928693,0.00002690794,0.00012761455,3.4668653e-7,0.000024507874,0.00000406172,0.0000707137],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99872965,0.000051426527,0.00046382585,0.00012574339,0.00047292406,0.0001564199],"domain_scores_gemma":[0.99904406,0.00007283493,0.00043366256,0.000092268165,0.0002823738,0.000074783835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022319223,0.00010799314,0.00026044546,0.000064236694,0.00005213432,0.000024580273,0.00026702098,0.000049396065,0.00017075846],"category_scores_gemma":[0.00004976662,0.00008721556,0.00012241521,0.00009068162,0.00009451299,0.00031857495,0.000024590645,0.00014114339,0.000005135114],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018182122,0.00008676084,0.0004377453,0.000020758622,0.000058818077,0.0000017720938,0.00054125243,0.8852704,0.096094735,0.014667672,0.0000020764087,0.0026361537],"study_design_scores_gemma":[0.00048000336,0.00012066055,0.0044187787,0.0001049249,0.000034762146,0.000011739124,0.00005565696,0.8334139,0.013178103,0.14807026,0.0000037513807,0.00010748866],"about_ca_topic_score_codex":0.0005378574,"about_ca_topic_score_gemma":0.000034335648,"teacher_disagreement_score":0.13340259,"about_ca_system_score_codex":0.000005348672,"about_ca_system_score_gemma":0.00015968432,"threshold_uncertainty_score":0.35565472},"labels":[],"label_agreement":null},{"id":"W2006960032","doi":"10.1029/2010jb000866","title":"The North American upper mantle: Density, composition, and evolution","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":175,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Gravity anomaly; Crust; Geophysics; Sedimentary rock; Transition zone; Core–mantle boundary; Oceanic crust; Seismic tomography; Seismology; Subduction; Tectonics; Paleontology; Oil field","score_opus":0.012393364563094767,"score_gpt":0.27032545474418795,"score_spread":0.2579320901810932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006960032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981845,0.00012667953,0.000031319203,0.0008399089,0.00034458408,0.00009322386,0.000013749261,0.000006123012,0.00035990172],"genre_scores_gemma":[0.9982913,0.00013673712,0.00054906926,0.00002791621,0.00086056686,5.439082e-7,0.0000036610359,0.0000041361736,0.0001260848],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998181,0.00024142662,0.0002564657,0.00013973561,0.00078298606,0.00039837847],"domain_scores_gemma":[0.9981328,0.00077888824,0.00016306709,0.0001823001,0.00048541444,0.00025747917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082726334,0.00010072687,0.0002159515,0.000015112673,0.0006005043,0.000282336,0.00034799866,0.000029635752,0.00011576204],"category_scores_gemma":[0.00017997598,0.000058021353,0.000068789115,0.00029575196,0.00073648844,0.0002295822,0.000052104577,0.0006179193,0.00010174354],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064295117,0.00013679061,0.8919425,0.000027109889,0.00013263272,0.00008266748,0.00016827817,0.00008616062,0.026796373,0.005212471,0.0075280624,0.06724401],"study_design_scores_gemma":[0.0001459145,0.0003552597,0.9885874,0.000008451007,0.000011606239,0.000028440181,0.000074663745,0.00039858304,0.00046120168,0.0056482023,0.0042052157,0.00007507604],"about_ca_topic_score_codex":0.004324162,"about_ca_topic_score_gemma":0.006776395,"teacher_disagreement_score":0.09664489,"about_ca_system_score_codex":0.000004874831,"about_ca_system_score_gemma":0.000112202266,"threshold_uncertainty_score":0.6536868},"labels":[],"label_agreement":null},{"id":"W2007031612","doi":"10.1038/nmat1525","title":"Anharmonic motions of Kr in the clathrate hydrate","year":2005,"lang":"en","type":"article","venue":"Nature Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"Basic Energy Sciences; Office of Science","keywords":"Anharmonicity; Clathrate hydrate; Inelastic neutron scattering; Phonon; Thermal conductivity; Scattering; Neutron scattering; Chemical physics; Molecular dynamics; Materials science; Inelastic scattering; Hydrate; Thermal; Condensed matter physics; Phonon scattering; Chemistry; Physics; Thermodynamics; Computational chemistry; Optics","score_opus":0.007082163427689779,"score_gpt":0.22115691893364883,"score_spread":0.21407475550595906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007031612","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946471,0.00040394432,0.0000022396684,0.0007688152,0.00070375693,0.00019387623,0.00039765777,0.000016295502,0.0028663306],"genre_scores_gemma":[0.9986984,0.00006908185,0.0001876055,0.00043149447,0.0003950039,0.000002559381,0.00011247472,0.0000033521983,0.00010003453],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989609,0.00018449068,0.00028788982,0.00016019768,0.00018792391,0.00021859632],"domain_scores_gemma":[0.9995535,0.000055722732,0.000109431356,0.00022890305,0.00002876023,0.000023665032],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00065001147,0.000114377784,0.00022384242,0.000054203454,0.000060291546,0.00007965869,0.00030645833,0.00015435225,0.0026931656],"category_scores_gemma":[0.000025818048,0.00007010106,0.000033519445,0.00015930261,0.00004188641,0.00015677199,0.000011468467,0.00012552747,0.00025136094],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013970691,0.00015267996,0.004693439,0.00014556141,0.000058314086,0.000031272873,0.0017179045,0.0027438595,0.9690799,0.00776245,0.008217468,0.005257403],"study_design_scores_gemma":[0.0006970819,0.00013212272,0.57040143,0.00006366843,0.00004820705,0.00001456752,0.00008484325,0.00012946848,0.37621665,0.0060930206,0.045754693,0.00036426735],"about_ca_topic_score_codex":0.00046923096,"about_ca_topic_score_gemma":0.0005222033,"teacher_disagreement_score":0.59286326,"about_ca_system_score_codex":0.0000017763965,"about_ca_system_score_gemma":0.000023372517,"threshold_uncertainty_score":0.99821854},"labels":[],"label_agreement":null},{"id":"W2007318010","doi":"10.1038/nature03182","title":"Neon isotopes constrain convection and volatile origin in the Earth's mantle","year":2005,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":165,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council","keywords":"Mantle (geology); Neon; Isotopes of neon; Geology; Isotopic signature; Mantle plume; Mantle convection; Earth's internal heat budget; Hotspot (geology); Astrobiology; Geochemistry; Subduction; Geophysics; Isotope; Physics; Argon; Paleontology","score_opus":0.0059347791482406405,"score_gpt":0.21449410389381862,"score_spread":0.20855932474557798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007318010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98742366,0.0007202637,0.0000036023184,0.0013906823,0.00025038095,0.00012798302,0.000053802232,0.000013121241,0.010016489],"genre_scores_gemma":[0.9983952,0.000040104547,0.00016368867,0.00070802274,0.00024829037,7.634904e-7,0.000031564443,0.0000011812833,0.0004111689],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99955463,0.000049384056,0.00007249761,0.00010901307,0.00009942508,0.00011506368],"domain_scores_gemma":[0.99981457,0.000057892852,0.000023317421,0.000072453775,0.000009769346,0.00002200924],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019317977,0.000061016395,0.00007819209,0.00002342045,0.00006130929,0.000064297616,0.00007656911,0.00019409493,0.001266344],"category_scores_gemma":[0.000009766022,0.000037989976,0.00001214682,0.00007304794,0.000034297274,0.00011579074,0.0000034502914,0.00033872886,0.0000831266],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030374536,0.00013414634,0.404186,0.00016476102,0.00008144686,0.0001149385,0.0074568875,0.0017271778,0.016468186,0.022110505,0.07597671,0.47127548],"study_design_scores_gemma":[0.00028323795,0.000048332036,0.4105879,0.000012765136,0.000007810732,0.00001742012,0.00014416203,0.0017614624,0.0009615345,0.0011063896,0.5849493,0.00011969731],"about_ca_topic_score_codex":0.0005880795,"about_ca_topic_score_gemma":0.0033361707,"teacher_disagreement_score":0.5089726,"about_ca_system_score_codex":6.00185e-7,"about_ca_system_score_gemma":0.000012731438,"threshold_uncertainty_score":0.9996466},"labels":[],"label_agreement":null},{"id":"W2007469772","doi":"10.1007/s10751-011-0552-9","title":"Kaonic 3He and 4He X-ray measurements in SIDDHARTA","year":2012,"lang":"en","type":"article","venue":"Hyperfine Interactions","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Autoritatea Natională pentru Cercetare Stiintifică; Austrian Science Fund; Bundesministerium für Wissenschaft und Forschung; Bundesministerium für Bildung, Wissenschaft und Kultur; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Physics; Helium; Nuclear physics; Atomic physics","score_opus":0.04353494433852637,"score_gpt":0.25371296902523904,"score_spread":0.21017802468671268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007469772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859789,0.00040122587,0.0000137145635,0.00034076272,0.0012476989,0.00009628493,0.00003651006,0.000020046242,0.011864867],"genre_scores_gemma":[0.9986549,0.000026458805,0.00017525695,0.00014091174,0.00027421676,0.0000031457873,0.00003578522,0.0000030489582,0.0006862867],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993343,0.000052015854,0.00014943018,0.00011975789,0.00010872268,0.00023582553],"domain_scores_gemma":[0.9996726,0.000059489812,0.00003794344,0.00011772139,0.000021441134,0.000090839014],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019031826,0.000087095614,0.000117198266,0.000065840744,0.000081316146,0.000048988495,0.00006725202,0.000025445404,0.004163419],"category_scores_gemma":[0.000035699893,0.00007179612,0.000021024025,0.000098559176,0.000021014594,0.0004052512,0.000011459931,0.00009079763,0.0006413911],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039395658,0.00015479192,0.96020347,0.000025512276,0.000051210285,0.0000026871858,0.0007494034,0.00046676074,0.024719026,0.00020000312,0.0050098207,0.008377891],"study_design_scores_gemma":[0.00023937352,0.000032653596,0.8328836,0.000026028552,0.000021355661,0.000013250549,0.000096654876,0.00025707233,0.00083479634,0.00012830377,0.16532369,0.00014319464],"about_ca_topic_score_codex":0.001725605,"about_ca_topic_score_gemma":0.0029251436,"teacher_disagreement_score":0.16031387,"about_ca_system_score_codex":0.000003349694,"about_ca_system_score_gemma":0.000012409048,"threshold_uncertainty_score":0.9967469},"labels":[],"label_agreement":null},{"id":"W2007679236","doi":"10.1029/2001jb000252","title":"Lithospheric deformation during the early stages of continental collision: Numerical experiments and comparison with South Island, New Zealand","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Lithosphere; Geology; Mantle (geology); Subduction; Collision zone; Geophysics; Lithospheric flexure; Plate tectonics; Convergent boundary; Continental collision; Obduction; Mantle convection; Crust; Seismology; Petrology; Oceanic crust; Tectonics","score_opus":0.024692170720567026,"score_gpt":0.2731670057277871,"score_spread":0.2484748350072201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007679236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866253,0.0006921505,0.00004245915,0.00015455959,0.000077566365,0.00015944912,0.000020966236,0.0000045945912,0.00018571598],"genre_scores_gemma":[0.9982144,0.00008494456,0.00050920265,0.000007141993,0.0002834448,7.9159906e-7,0.000002158245,0.000005515458,0.0008923653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99795043,0.00021010934,0.00040321265,0.00013509848,0.00096837425,0.00033274895],"domain_scores_gemma":[0.9988624,0.00027525602,0.00029767852,0.00014384754,0.00019298088,0.00022784925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033766,0.00013071651,0.00036763903,0.000013063502,0.0002053368,0.00017605376,0.0002650069,0.000043348264,0.00067934557],"category_scores_gemma":[0.000059636746,0.000068702684,0.00006210895,0.00026647488,0.00019565696,0.00035146068,0.000039252434,0.00029113668,0.000032191507],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019593681,0.00025832615,0.97143716,0.0000798897,0.0002253881,0.000055316777,0.009385364,0.0015198216,0.0035497735,0.00006232364,0.004281716,0.0071855807],"study_design_scores_gemma":[0.0015177974,0.0020105892,0.98764914,0.00010271508,0.000025400594,0.000022210286,0.0012239371,0.001834872,0.0037941183,0.00020680956,0.0014754011,0.00013701868],"about_ca_topic_score_codex":0.0028668984,"about_ca_topic_score_gemma":0.00011729145,"teacher_disagreement_score":0.016212,"about_ca_system_score_codex":0.0000063840844,"about_ca_system_score_gemma":0.000043458233,"threshold_uncertainty_score":0.74383575},"labels":[],"label_agreement":null},{"id":"W2008008578","doi":"10.1016/j.pepi.2004.08.035","title":"Crustal structure of the India–Asia collision zone, southern Tibet, from INDEPTH MT investigations","year":2005,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"National Science Foundation","keywords":"Magnetotellurics; Geology; Longitude; Crust; Seismology; Fibrous joint; Mantle (geology); Collision zone; Transect; Geodesy; Lithosphere; Tectonics; Geophysics; Latitude; Electrical resistivity and conductivity; Oceanography","score_opus":0.006185345744653659,"score_gpt":0.1751851867517724,"score_spread":0.16899984100711873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008008578","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929451,0.00015868648,0.000012493821,0.00015974499,0.00041821916,0.00018912046,0.005778125,0.0000087962835,0.00032975202],"genre_scores_gemma":[0.99883866,0.00001513576,0.00035244963,0.00013386489,0.00026332116,2.505582e-7,0.00029251503,0.0000047509684,0.000099064346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990335,0.00010673648,0.0002647322,0.00017413552,0.00025055406,0.00017033723],"domain_scores_gemma":[0.9992354,0.00009184229,0.000253676,0.00031792224,0.000028640965,0.00007251455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061483326,0.00016064102,0.0002449696,0.000021094293,0.00014337174,0.000034401834,0.00039073342,0.000071718365,0.00043544348],"category_scores_gemma":[0.000013814887,0.00009239539,0.00007892824,0.00013091671,0.00022456273,0.00013958133,0.000057968038,0.00016271732,0.000022260638],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028363478,0.000074436175,0.81042874,0.00015418565,0.00038937453,0.0000024428184,0.009761904,0.036560543,0.11014809,0.00043461475,0.0012837492,0.030478317],"study_design_scores_gemma":[0.00038774728,0.000089066605,0.9376531,0.00013369738,0.00010335728,0.0000042762167,0.00031269545,0.0025085073,0.050980575,0.004298016,0.003289932,0.0002389786],"about_ca_topic_score_codex":0.0056237974,"about_ca_topic_score_gemma":0.0052913604,"teacher_disagreement_score":0.12722445,"about_ca_system_score_codex":9.616847e-7,"about_ca_system_score_gemma":0.000052722276,"threshold_uncertainty_score":0.8501537},"labels":[],"label_agreement":null},{"id":"W2008193319","doi":"10.1029/2009jb006914","title":"North American lithospheric discontinuity structure imaged by <i>Ps</i> and <i>Sp</i> receiver functions","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":320,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Asthenosphere; Low-velocity zone; Classification of discontinuities; Discontinuity (linguistics); Mantle (geology); Seismology; Phanerozoic; Crust; Geophysics; Structural basin; Tectonics; Paleontology; Cenozoic","score_opus":0.00908960442543535,"score_gpt":0.2538796834060443,"score_spread":0.24479007898060892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008193319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977016,0.0002036865,0.00003488245,0.00047362735,0.00049660145,0.00015092563,0.00033674506,0.000014645015,0.0005873274],"genre_scores_gemma":[0.99631757,0.00014726809,0.001749822,0.00006849139,0.0009253593,0.0000010365412,0.000028983939,0.000011366017,0.00075011567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99741364,0.0003101971,0.00039977932,0.00031110522,0.00094377977,0.0006215166],"domain_scores_gemma":[0.99786913,0.00057381333,0.00028898474,0.0002889944,0.00043876487,0.0005403109],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056951493,0.0002156836,0.00048302085,0.0000165773,0.00037690977,0.00034153732,0.0004636165,0.000064656975,0.0012078349],"category_scores_gemma":[0.00032588234,0.00014874524,0.0001196012,0.00060192286,0.0008142712,0.00054309424,0.000065661705,0.0012724595,0.000071569186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00093397486,0.00030531074,0.54384345,0.00007284604,0.00026523232,0.00011792928,0.00039555054,0.00008783402,0.12724721,0.00012176592,0.09358989,0.233019],"study_design_scores_gemma":[0.00045293482,0.00083908264,0.932443,0.000015574835,0.000037955535,0.000024529934,0.00017830852,0.00013324738,0.0018861732,0.0015451346,0.062207274,0.00023673769],"about_ca_topic_score_codex":0.006665617,"about_ca_topic_score_gemma":0.013140173,"teacher_disagreement_score":0.38859957,"about_ca_system_score_codex":0.000005770413,"about_ca_system_score_gemma":0.00016563943,"threshold_uncertainty_score":0.9999491},"labels":[],"label_agreement":null},{"id":"W2008359302","doi":"10.1063/1.3280730","title":"A density-functional approximation for relativistic kinetic energy","year":2009,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Kinetic energy; Physics; Relativistic quantum chemistry; Quantum electrodynamics; Scalar (mathematics); Dirac (video compression format); Atom (system on chip); Atomic orbital; Dirac equation; Quantum mechanics; Electron; Mathematics","score_opus":0.013304358625105562,"score_gpt":0.1988683290475863,"score_spread":0.18556397042248074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008359302","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8647879,0.000115699855,0.13269545,0.0006754805,0.00041571874,0.00009821088,0.000019058709,0.000011242125,0.0011812585],"genre_scores_gemma":[0.9981052,0.0000067312976,0.00071292475,0.00019712721,0.00090690935,1.4656705e-7,0.000021077714,0.0000017768206,0.000048067694],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9994365,0.000032024724,0.00018962163,0.000049090882,0.00018536953,0.00010738446],"domain_scores_gemma":[0.9993805,0.00021604341,0.00018570347,0.00007292862,0.000099826924,0.000044971086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001927705,0.00006890209,0.00014045977,0.000010337068,0.000049398088,0.000021513144,0.000117237,0.000027487524,0.000038155267],"category_scores_gemma":[0.000039546725,0.00004156591,0.0000659244,0.00006250233,0.000032873868,0.00010274575,0.0000032128667,0.00007296246,0.0000067956753],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011269759,0.00020307564,0.00021542523,0.000049656166,0.00014352292,0.000004379277,0.000423661,0.013711602,0.85091525,0.052639145,0.011818922,0.06874838],"study_design_scores_gemma":[0.00054966414,0.0002414522,0.005306753,0.000027707034,0.00014828265,0.00003317674,0.0000085431475,0.0073790476,0.15716639,0.82756555,0.001431595,0.00014184738],"about_ca_topic_score_codex":0.0000115321845,"about_ca_topic_score_gemma":5.112083e-7,"teacher_disagreement_score":0.77492636,"about_ca_system_score_codex":0.0000027321016,"about_ca_system_score_gemma":0.000023315934,"threshold_uncertainty_score":0.16950086},"labels":[],"label_agreement":null},{"id":"W2009286275","doi":"10.1111/j.1365-246x.2008.03982.x","title":"Rayleigh wave phase-velocity heterogeneity and multilayered azimuthal anisotropy of the Superior Craton, Ontario","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Innovation Trust","keywords":"Anisotropy; Isotropy; Geology; Phase velocity; Azimuth; Rayleigh wave; Craton; Smoothing; Inversion (geology); Computational physics; Surface wave; Geodesy; Geophysics; Seismology; Physics; Optics; Mathematics; Tectonics; Statistics","score_opus":0.02566703347110572,"score_gpt":0.23738384793122097,"score_spread":0.21171681446011525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009286275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977742,0.000034358443,0.000092152666,0.00018249071,0.001187023,0.00008863801,0.00022002516,0.000008130177,0.00041302008],"genre_scores_gemma":[0.9984256,0.00004153778,0.00055905426,0.000107198895,0.0005451542,6.7036365e-7,0.000017998787,0.0000040457835,0.00029874733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99863964,0.000086770626,0.00033533925,0.0001952076,0.00049174734,0.00025126542],"domain_scores_gemma":[0.99927664,0.00006618626,0.00019446686,0.0001374834,0.0001643513,0.00016088312],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012320442,0.00015329254,0.00024583694,0.000034933946,0.0003076534,0.00007795597,0.0003181872,0.000056616416,0.0013144846],"category_scores_gemma":[0.000031588475,0.00010016166,0.00015655489,0.000063665895,0.0002187166,0.00026285884,0.00005653791,0.0002407998,0.000030753108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017509813,0.0013368723,0.8307077,0.00004549088,0.0011480591,0.00047418452,0.0050519295,0.0016778497,0.12233331,0.0017609269,0.0029240542,0.030788599],"study_design_scores_gemma":[0.0011972032,0.00015858821,0.9754641,0.0000159744,0.000022400318,0.00033754628,0.000017834667,0.0018683162,0.013979108,0.001088514,0.005701667,0.00014874346],"about_ca_topic_score_codex":0.009717393,"about_ca_topic_score_gemma":0.0053245905,"teacher_disagreement_score":0.14475636,"about_ca_system_score_codex":0.000016175289,"about_ca_system_score_gemma":0.00015219091,"threshold_uncertainty_score":0.99959844},"labels":[],"label_agreement":null},{"id":"W2010026423","doi":"10.1016/j.lithos.2015.04.003","title":"Evolution of diamond resorption in a silicic aqueous fluid at 1–3 GPa: Application to kimberlite emplacement and mantle metasomatism","year":2015,"lang":"en","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Kimberlite; Metasomatism; Geology; Diamond; Dissolution; Mineralogy; Mantle (geology); Geochemistry; Materials science; Chemical engineering; Metallurgy","score_opus":0.010133783315304625,"score_gpt":0.21774081721472296,"score_spread":0.20760703389941834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010026423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99735594,0.00070960796,0.0004921869,0.000085655476,0.00011205292,0.0003704153,0.00010361261,0.000013592158,0.0007569344],"genre_scores_gemma":[0.99891233,0.00001866772,0.00069261,0.000026379963,0.000044674834,0.0000123986365,0.00008241457,0.0000024889457,0.0002080395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99925035,0.00007126725,0.00019705991,0.00018116858,0.00016268987,0.00013746094],"domain_scores_gemma":[0.9996292,0.000027994261,0.00006365444,0.00015780206,0.000027358381,0.000093971285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031211518,0.000077359065,0.00014977489,0.00006562992,0.000029178598,0.00001705078,0.000064081156,0.000040072187,0.00007968719],"category_scores_gemma":[0.00001827644,0.000067250054,0.000013708354,0.0001298955,0.000019447694,0.000097429416,0.00002243628,0.00002307671,0.00010395637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007595437,0.00015397598,0.8464703,0.00027605268,0.00005090707,0.000012294257,0.0077570723,0.0063534533,0.06949425,0.002554777,0.0026590407,0.06345835],"study_design_scores_gemma":[0.00045918583,0.00020377796,0.9777666,0.000023344179,0.000019519688,0.0000045774304,0.00010298566,0.0045927805,0.0036171349,0.0024993808,0.010570928,0.00013982473],"about_ca_topic_score_codex":0.013074284,"about_ca_topic_score_gemma":0.004004259,"teacher_disagreement_score":0.13129628,"about_ca_system_score_codex":0.000013995422,"about_ca_system_score_gemma":0.000016169633,"threshold_uncertainty_score":0.9934977},"labels":[],"label_agreement":null},{"id":"W2010073944","doi":"10.1016/j.pepi.2004.08.019","title":"Time dependent subduction dynamics driven by the instability of stagnant slabs in the transition zone","year":2004,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Slab; Subduction; Slab window; Transition zone; Instability; Convergent boundary; Geophysics; Mantle (geology); Volcanic arc; Trench; Seismology; Mechanics; Tectonics; Oceanic crust; Physics","score_opus":0.005028891237647043,"score_gpt":0.17249260070033304,"score_spread":0.167463709462686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010073944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99746114,0.0001214343,0.00009871298,0.0005491378,0.0002050871,0.0002687886,0.0011492037,0.000004997943,0.00014150531],"genre_scores_gemma":[0.9994567,0.00005650611,0.000033636177,0.000070840055,0.00005027692,9.483171e-7,0.0003135057,0.0000023537577,0.000015211982],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99907476,0.00016445946,0.00024561296,0.00014297564,0.00022039309,0.00015179564],"domain_scores_gemma":[0.9994849,0.000087068984,0.00013466596,0.00024807165,0.000019954778,0.000025341387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030357265,0.00011805056,0.00019300725,0.000014981667,0.00008996076,0.000022983473,0.0002858896,0.00003729523,0.00007651614],"category_scores_gemma":[0.0000062096606,0.00006025918,0.000055205586,0.00010526255,0.0002144945,0.00013374479,0.000014421479,0.00012920992,0.000008988474],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031180703,0.0009751583,0.15860164,0.001340183,0.000724246,0.000030118992,0.05799813,0.5170038,0.15059426,0.0027686814,0.0006529783,0.10619274],"study_design_scores_gemma":[0.0028343145,0.0015456349,0.88431853,0.00041637497,0.0003314633,0.00008277496,0.0034943665,0.03561414,0.047229897,0.022292668,0.00094489235,0.0008949612],"about_ca_topic_score_codex":0.008567598,"about_ca_topic_score_gemma":0.0058935042,"teacher_disagreement_score":0.7257169,"about_ca_system_score_codex":0.0000023807902,"about_ca_system_score_gemma":0.000026115356,"threshold_uncertainty_score":0.9980344},"labels":[],"label_agreement":null},{"id":"W2010472073","doi":"10.1063/1.2357644","title":"Stability of rocksalt phase of zinc oxide under strong compression: Synchrotron x-ray diffraction experiments and first-principles calculation studies","year":2006,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Diffraction; Materials science; X-ray crystallography; Synchrotron; Phase (matter); Zinc; Synchrotron radiation; Analytical Chemistry (journal); Crystallography; Thermodynamics; Condensed matter physics; Chemistry; Optics; Metallurgy; Physics","score_opus":0.04423637080959692,"score_gpt":0.2884320584672576,"score_spread":0.2441956876576607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010472073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981488,0.00035337324,0.0009534308,0.000009099747,0.00014606744,0.000131494,0.00004386227,0.000004112875,0.00020973475],"genre_scores_gemma":[0.9989566,0.00005211698,0.0007653707,0.0000044557296,0.00019445727,7.7917974e-7,0.000019038669,0.0000036372226,0.0000035319704],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99889976,0.000035615845,0.00051300414,0.0001142455,0.00031846084,0.00011891665],"domain_scores_gemma":[0.99882036,0.00012824527,0.0007611226,0.00011513036,0.00013083825,0.000044277287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001991593,0.00011953747,0.0003908772,0.000027996992,0.00008469478,0.00001645701,0.00008169532,0.000038545513,0.00003402481],"category_scores_gemma":[0.000005303382,0.00009062813,0.000057426,0.00006683841,0.00009251652,0.00019970663,0.000019300458,0.000075508484,9.1156267e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061683205,0.00041893535,0.010273606,0.00024602734,0.00018059998,0.000001575845,0.0005968366,0.61791503,0.36709443,0.0012109804,0.00009045207,0.0013547263],"study_design_scores_gemma":[0.0036341944,0.00055671146,0.45623603,0.00022486485,0.0002635312,0.000003001327,0.0014546148,0.022370186,0.5056882,0.008668955,0.00055181974,0.00034787357],"about_ca_topic_score_codex":0.00027435366,"about_ca_topic_score_gemma":0.00004326709,"teacher_disagreement_score":0.5955448,"about_ca_system_score_codex":0.000008800987,"about_ca_system_score_gemma":0.000027377753,"threshold_uncertainty_score":0.3695708},"labels":[],"label_agreement":null},{"id":"W2010669345","doi":"10.1080/10543400600809359","title":"An Overview of the High‐Pressure Vibrational Spectra of Clays and Related Minerals","year":2006,"lang":"en","type":"article","venue":"Applied Spectroscopy Reviews","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Martian; Clay minerals; Mineralogy; Astrobiology; Chemistry; Martian surface; Mineral; High pressure; Mars Exploration Program; Environmental chemistry; Geology; Geochemistry; Thermodynamics; Physics; Organic chemistry","score_opus":0.015808724435075205,"score_gpt":0.24625375147318282,"score_spread":0.23044502703810762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010669345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9245497,0.04704965,0.00010465495,0.00025950806,0.00047524134,0.0014315376,0.0004238356,0.00003086751,0.02567499],"genre_scores_gemma":[0.9926968,0.0034339766,0.0033733724,0.000069648166,0.00016478675,0.0000049556065,0.00012449625,0.000005636284,0.00012631892],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987391,0.00011211872,0.00053789787,0.00023634106,0.00020041103,0.00017412736],"domain_scores_gemma":[0.9991667,0.000040626306,0.00036358376,0.0003675137,0.00001999408,0.000041534477],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037451126,0.00015609805,0.00049861224,0.000025908757,0.000076433134,0.00002644214,0.00023956531,0.0000634924,0.0018821281],"category_scores_gemma":[0.000006002072,0.0000964646,0.00007478465,0.00019859856,0.000121739125,0.000094349474,0.000014344893,0.000078105484,0.000028600998],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026300973,0.000049330618,0.0033686692,0.00030139522,0.00002860581,5.028485e-7,0.00005928692,0.000387752,0.88495284,0.10770457,0.0023605379,0.0007602017],"study_design_scores_gemma":[0.00079167524,0.00027343578,0.40229487,0.0002334815,0.000357439,0.000009568542,0.000016158425,0.0003205625,0.44443437,0.08625379,0.064484596,0.0005300408],"about_ca_topic_score_codex":0.0009891378,"about_ca_topic_score_gemma":0.00026062713,"teacher_disagreement_score":0.44051847,"about_ca_system_score_codex":0.0000011893886,"about_ca_system_score_gemma":0.000025715526,"threshold_uncertainty_score":0.9990303},"labels":[],"label_agreement":null},{"id":"W2010829207","doi":"10.1016/j.crte.2003.07.001","title":"A new natural, super-hard, transparent polymorph of carbon from the Popigai impact crater, Russia","year":2003,"lang":"en","type":"article","venue":"Comptes Rendus Géoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Centre National de la Recherche Scientifique","keywords":"Synchrotron; Crystallography; X-ray crystallography; Impact crater; Physics; Carbon fibers; Diffraction; Materials science; Mineralogy; Geology; Chemistry; Optics; Astrobiology; Composite material","score_opus":0.024266349550141012,"score_gpt":0.23386602746708612,"score_spread":0.20959967791694512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010829207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910713,0.005279555,0.00007245786,0.00022596848,0.0014814514,0.00015630988,0.000303786,0.000028237979,0.0013809424],"genre_scores_gemma":[0.9988544,0.00012530679,0.0004980626,0.000114919436,0.00012243314,8.592098e-7,0.00004697447,0.0000042346883,0.00023282702],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983758,0.00013572641,0.00028735484,0.00036920543,0.00041880843,0.00041314235],"domain_scores_gemma":[0.99906445,0.0001747379,0.00011523585,0.00043192768,0.00003113173,0.00018250047],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000236476,0.00020840883,0.00030142476,0.000038288606,0.00017545775,0.00013497105,0.00068766647,0.00005317974,0.0033525613],"category_scores_gemma":[0.00003873727,0.000120016746,0.00010362403,0.00034186486,0.0002003428,0.00017443809,0.000016507965,0.0001320175,0.00007486642],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017117127,0.00013331343,0.69634855,0.000037162295,0.00014395478,0.00004071216,0.003283701,0.003919223,0.26454455,0.0010619491,0.0123692695,0.017946467],"study_design_scores_gemma":[0.0004633661,0.00019340416,0.9561433,0.00006169292,0.000046583285,0.000010505775,0.00007953957,0.0014944905,0.032754786,0.0012519435,0.0071354215,0.00036496425],"about_ca_topic_score_codex":0.03264886,"about_ca_topic_score_gemma":0.00053868355,"teacher_disagreement_score":0.25979477,"about_ca_system_score_codex":0.0000051516536,"about_ca_system_score_gemma":0.0001756464,"threshold_uncertainty_score":0.99755853},"labels":[],"label_agreement":null},{"id":"W2011665680","doi":"10.1029/2008gl036331","title":"Crustal structure beneath the Florida‐to‐Edmonton broadband seismometer array","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Seismometer; Seismology; Rift; Orogeny; Crust; Proterozoic; Paleozoic; Metamorphism; Lithosphere; Tectonics; Petrology; Geophysics; Geochemistry","score_opus":0.021472977991427354,"score_gpt":0.2733097236939273,"score_spread":0.2518367457025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011665680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97947484,0.000048364636,0.00012348984,0.017668052,0.00044975372,0.00046595352,0.00021649891,0.00004528818,0.0015077681],"genre_scores_gemma":[0.9930156,0.000008147675,0.00026517897,0.004321337,0.001864337,0.000004304408,0.000083603554,0.000008241829,0.00042927937],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99656934,0.00031382055,0.00022646814,0.0005393984,0.0012427829,0.0011081831],"domain_scores_gemma":[0.9985448,0.00034549675,0.00004146985,0.00058139197,0.000107463056,0.00037939145],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050907256,0.00024520644,0.00029335674,0.00012573063,0.000558223,0.00044756825,0.00079220074,0.00007926405,0.0008851341],"category_scores_gemma":[0.00010970481,0.00015105442,0.00011757816,0.0006131837,0.00020501306,0.00026383917,0.00004283819,0.0005566422,0.0008821187],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045417922,0.00006964389,0.0012972811,0.000031170362,0.00009541481,0.00011431044,0.0015367802,0.0037409966,0.8622816,0.0011384211,0.076715276,0.052524928],"study_design_scores_gemma":[0.000677197,0.0010613452,0.81015646,0.000048734848,0.000035146044,0.000009506486,0.00013020047,0.0005995173,0.034028053,0.010943734,0.14155625,0.0007538356],"about_ca_topic_score_codex":0.0032975043,"about_ca_topic_score_gemma":0.00022474617,"teacher_disagreement_score":0.82825357,"about_ca_system_score_codex":0.000011567075,"about_ca_system_score_gemma":0.000051993582,"threshold_uncertainty_score":0.9998958},"labels":[],"label_agreement":null},{"id":"W2011922582","doi":"10.1029/2007jb005127","title":"The teleseismic signature of fossil subduction: Northwestern Canada","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Seismology; Terrane; Mantle (geology); Layering; Fibrous joint; Seismometer; Precambrian; Underplating; Geophysics; Tectonics; Paleontology","score_opus":0.02195976402395505,"score_gpt":0.2545378857312254,"score_spread":0.23257812170727032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011922582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961838,0.0017403325,0.000009076091,0.0005952624,0.00066777744,0.00009893114,0.000035260946,0.0000034862749,0.00066606695],"genre_scores_gemma":[0.997435,0.00033917598,0.00012262494,0.000022665958,0.001050799,5.723467e-7,0.0000029020284,0.000005027015,0.0010212848],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99709755,0.00029382546,0.0004483421,0.00014099957,0.0015535327,0.00046576106],"domain_scores_gemma":[0.9974947,0.0010139182,0.0002684984,0.0002457787,0.00074127904,0.00023582508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066534925,0.00012504113,0.00032071336,0.000012463449,0.0005141999,0.00006153172,0.0006417777,0.000057769637,0.00029036077],"category_scores_gemma":[0.0002008325,0.00007076779,0.0001222375,0.00035465605,0.00040745406,0.00020899887,0.000034672157,0.0005442477,0.000023172406],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0050897207,0.00076323556,0.2654384,0.00040611404,0.0014465809,0.0032589303,0.002513782,0.014287971,0.027361056,0.0020060295,0.48092127,0.19650692],"study_design_scores_gemma":[0.00057824235,0.0010161713,0.84185815,0.00006949699,0.0000230389,0.00013183703,0.0005191533,0.0004439091,0.005823821,0.004225009,0.145101,0.00021020352],"about_ca_topic_score_codex":0.53686494,"about_ca_topic_score_gemma":0.34866744,"teacher_disagreement_score":0.5764197,"about_ca_system_score_codex":0.000015372003,"about_ca_system_score_gemma":0.001335087,"threshold_uncertainty_score":0.66321766},"labels":[],"label_agreement":null},{"id":"W2012003540","doi":"10.1016/s0040-1951(01)00136-6","title":"Seismic anisotropy of mantle xenoliths and constraints on upper mantle structure beneath the southern Canadian Cordillera","year":2001,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Northwestern University","keywords":"Geology; Asthenosphere; Seismic anisotropy; Xenolith; Lithosphere; Mantle (geology); Anisotropy; Core–mantle boundary; Geophysics; Seismology; Tectonics","score_opus":0.007160290793880191,"score_gpt":0.1854627989896308,"score_spread":0.1783025081957506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012003540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921889,0.000057888134,0.000015716212,0.00015904644,0.00019900408,0.00017823854,0.0014176008,0.000017715243,0.005765925],"genre_scores_gemma":[0.9992141,0.000032112595,0.00009346653,0.0002642526,0.0001595976,7.1419504e-7,0.00007080486,0.000007666489,0.00015730143],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991543,0.000039081107,0.00014378407,0.0002048641,0.00015710188,0.00030082455],"domain_scores_gemma":[0.9994621,0.00005030385,0.000075333606,0.00025848125,0.000034324174,0.00011940493],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00005539241,0.00015928733,0.00020740672,0.000038468235,0.00018369305,0.00005287761,0.00019385341,0.000062063154,0.002605896],"category_scores_gemma":[0.000005111646,0.00010530183,0.00003813196,0.00010732614,0.00020617775,0.000054630993,0.000011896131,0.00010674806,0.00013275926],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008854551,0.00031305366,0.3393871,0.00044832137,0.0013562498,0.0003344157,0.015238693,0.03710018,0.0767229,0.034146287,0.0051238444,0.48894352],"study_design_scores_gemma":[0.0023144998,0.0012205198,0.87173164,0.00019391687,0.0003122115,0.00011105029,0.002442752,0.016543616,0.027383981,0.048673816,0.027293783,0.001778208],"about_ca_topic_score_codex":0.07038707,"about_ca_topic_score_gemma":0.014990226,"teacher_disagreement_score":0.5323446,"about_ca_system_score_codex":0.0000044499698,"about_ca_system_score_gemma":0.00008071514,"threshold_uncertainty_score":0.99830586},"labels":[],"label_agreement":null},{"id":"W2012124270","doi":"10.1063/1.3504858","title":"Shock wave propagation in dense particle suspensions","year":2010,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Suspension (topology); Materials science; Particle (ecology); Shock wave; Dilatant; Shock (circulatory); Stress (linguistics); Range (aeronautics); Mechanics; Composite material; Physics; Geology","score_opus":0.013738888204367493,"score_gpt":0.20870928119651405,"score_spread":0.19497039299214655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012124270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99696195,0.0000065099,0.000063237014,0.000046771987,0.00043304663,0.000086135195,0.0000057814545,0.0000050565936,0.0023915167],"genre_scores_gemma":[0.9986363,0.000006388693,0.0007765655,0.000054020402,0.0005005644,3.885171e-7,0.0000062272607,0.0000030809106,0.000016459551],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9992954,0.000016129132,0.00025609147,0.00007951397,0.00019665914,0.00015618315],"domain_scores_gemma":[0.99951625,0.00005765759,0.00018038967,0.00010465653,0.00006025759,0.000080819096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026149862,0.00007476612,0.00016622672,0.000021640984,0.000049140286,0.000045911773,0.00009401113,0.000038960185,0.00024972344],"category_scores_gemma":[0.000011312715,0.000056441593,0.000038433536,0.0001257647,0.00003206958,0.00014897215,0.0000076099104,0.00020299702,0.000071716095],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040651154,0.00023315857,0.023899043,0.000028373079,0.000048566784,0.000090520196,0.0014562352,0.04355669,0.8812936,0.021224828,0.0007341449,0.027028352],"study_design_scores_gemma":[0.0021375762,0.00032350342,0.48765042,0.000045686516,0.000097941396,0.000059184335,0.0002862415,0.028988233,0.36020315,0.11243995,0.0072163465,0.000551762],"about_ca_topic_score_codex":0.000044401717,"about_ca_topic_score_gemma":0.0002881914,"teacher_disagreement_score":0.52109045,"about_ca_system_score_codex":0.0000017239089,"about_ca_system_score_gemma":0.000053961994,"threshold_uncertainty_score":0.27342963},"labels":[],"label_agreement":null},{"id":"W2012915084","doi":"10.1167/13.9.1146","title":"Mach Bands: Contrast normalization?","year":2013,"lang":"en","type":"article","venue":"Journal of Vision","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Normalization (sociology); Contrast (vision); Physics; Optics; Sociology","score_opus":0.00550765521025245,"score_gpt":0.21582846298051897,"score_spread":0.21032080777026652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012915084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955333,0.00022409332,0.0003973331,0.0002981289,0.0007705306,0.000059373695,0.000010008628,0.0000047220287,0.0027025032],"genre_scores_gemma":[0.99897015,0.00006463472,0.00040704996,0.000108928274,0.00031106282,7.413689e-8,0.000007866539,0.0000014411731,0.00012879242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99939805,0.00003623443,0.00023070899,0.000045597488,0.00019016965,0.000099221405],"domain_scores_gemma":[0.9995356,0.000037986872,0.00016880984,0.0000541367,0.00012403193,0.000079437195],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020158516,0.000050384755,0.0001229898,0.00004237449,0.000052726908,0.00010061499,0.00010590247,0.000027779193,0.006093544],"category_scores_gemma":[0.000017733142,0.00003208202,0.000038137692,0.00005507812,0.0000133848425,0.00041310882,0.0000042783163,0.00004730941,0.00034128802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036617764,0.00029418722,0.38592002,0.00014107981,0.00022506878,0.0001316958,0.0011772409,0.013961887,0.14092413,0.00091701315,0.20550436,0.25043717],"study_design_scores_gemma":[0.00038930788,0.00030306875,0.9779152,0.00003674076,0.000015001979,0.000031126667,0.000028093631,0.0018086482,0.0008313107,0.0013620933,0.017201304,0.00007806066],"about_ca_topic_score_codex":0.00025863328,"about_ca_topic_score_gemma":0.000018852043,"teacher_disagreement_score":0.59199524,"about_ca_system_score_codex":9.745894e-7,"about_ca_system_score_gemma":0.00001761226,"threshold_uncertainty_score":0.994815},"labels":[],"label_agreement":null},{"id":"W2013937395","doi":"10.2138/rmg.2007.67.4","title":"Long-Range Order in Amphiboles","year":2007,"lang":"en","type":"article","venue":"Reviews in Mineralogy and Geochemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"","keywords":"Crystal (programming language); Humanities; Art; Art history","score_opus":0.012011925559518738,"score_gpt":0.24483816332573555,"score_spread":0.2328262377662168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013937395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97053266,0.023865117,0.000011697801,0.00008201279,0.00011066128,0.00011366659,0.000014626023,0.000005915076,0.0052636303],"genre_scores_gemma":[0.99340653,0.0054922644,0.00031365594,0.00017677237,0.00014832187,0.0000020442642,0.000099147284,0.000001987609,0.00035928775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991493,0.000042021664,0.00029688101,0.00020441483,0.000054968412,0.00025240873],"domain_scores_gemma":[0.9996824,0.00006575219,0.000054150656,0.00012982497,0.000011882794,0.000055982488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007296622,0.00011433767,0.00028436887,0.000036263333,0.000024664894,0.000012947053,0.00009205717,0.00010128537,0.00080593425],"category_scores_gemma":[0.00005016883,0.00009184525,0.000022941984,0.00016289,0.000055638135,0.00005478112,0.000010940939,0.00010504304,0.000053326672],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040738865,0.00003111648,0.95964444,0.00033205003,0.0000054105444,0.00010363095,0.000108544795,0.000021104635,0.0052997293,0.000041650223,0.0005430024,0.033828557],"study_design_scores_gemma":[0.0003375506,0.000015304893,0.9530292,0.00015355674,0.0000089619425,0.000022089323,0.000014631809,0.000040849758,0.00068763475,0.00058366166,0.044905975,0.00020056946],"about_ca_topic_score_codex":0.0007194839,"about_ca_topic_score_gemma":0.00757887,"teacher_disagreement_score":0.044362973,"about_ca_system_score_codex":0.0000016556872,"about_ca_system_score_gemma":0.000011423812,"threshold_uncertainty_score":0.8824415},"labels":[],"label_agreement":null},{"id":"W2014019829","doi":"10.1029/2000jb000021","title":"Investigating the heterogeneity of the D″ region beneath the northern Pacific using a seismic array","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Deutsche Forschungsgemeinschaft","keywords":"Slowness; Geology; Discontinuity (linguistics); Mantle (geology); Downwelling; Seismology; Seismic array; Classification of discontinuities; Upwelling; Transition zone; Hotspot (geology); Geodesy; Geophysics; Oceanography","score_opus":0.06967101905515533,"score_gpt":0.28364874586209954,"score_spread":0.2139777268069442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014019829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99653643,0.0006168071,0.000047961603,0.0018581597,0.0002660204,0.00020516239,0.000012220896,0.0000040830087,0.00045313322],"genre_scores_gemma":[0.99886733,0.00007951814,0.00013561036,0.00007125171,0.00067966816,8.3807953e-7,5.418734e-7,0.000007484445,0.00015776436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99672174,0.0009879211,0.00044776176,0.00016310989,0.0012300933,0.0004493848],"domain_scores_gemma":[0.9976689,0.0009085109,0.00043572925,0.0004623955,0.00038449274,0.00013995368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011037732,0.00014710134,0.00028551178,0.000010641166,0.0010393105,0.00014556388,0.00104976,0.00005622688,0.00013561343],"category_scores_gemma":[0.00041461142,0.000059570302,0.00024314616,0.000515778,0.0007438002,0.00020190381,0.00009453218,0.0006178206,0.00002270205],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041612884,0.00067441975,0.6389231,0.00032620586,0.0010993157,0.0001485207,0.015293226,0.08746094,0.14820178,0.0009669024,0.009453153,0.09703627],"study_design_scores_gemma":[0.0010464358,0.0013381733,0.8573298,0.00061672344,0.00019503638,0.00024726015,0.0032296586,0.06453856,0.022279678,0.032199178,0.016457627,0.00052190694],"about_ca_topic_score_codex":0.0041775466,"about_ca_topic_score_gemma":0.0008838309,"teacher_disagreement_score":0.21840663,"about_ca_system_score_codex":0.000011977336,"about_ca_system_score_gemma":0.000122289,"threshold_uncertainty_score":0.79936415},"labels":[],"label_agreement":null},{"id":"W2014697496","doi":"10.1007/s004100100297","title":"Kankan diamonds (Guinea) III: δ13C and nitrogen characteristics of deep diamonds","year":2002,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Asthenosphere; Geology; Kimberlite; Craton; Mantle (geology); Geochemistry; Lithosphere; Eclogite; Population; Subduction; Tectonics; Paleontology","score_opus":0.006602355760129913,"score_gpt":0.20634305620287394,"score_spread":0.19974070044274403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014697496","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994004,0.0012736393,0.00037843964,0.0012336618,0.00034603314,0.00013448033,0.0013499672,0.000020185118,0.0012595669],"genre_scores_gemma":[0.998527,0.00020817673,0.00013127952,0.00033444658,0.00024235446,0.000006403824,0.00029833452,0.0000032896978,0.00024871095],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891996,0.00011237445,0.00029458283,0.00025214124,0.00006732854,0.00035359358],"domain_scores_gemma":[0.99924845,0.00019971878,0.00009324098,0.0001712162,0.00010004669,0.00018732286],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018643256,0.0001521542,0.00042114733,0.00010967899,0.00017299924,0.000024224431,0.00011137467,0.00015248585,0.0013968082],"category_scores_gemma":[0.000099828176,0.00013350176,0.0000383794,0.000119020515,0.00022231789,0.00007448431,0.000031701653,0.00009783379,0.00005856355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030027318,0.00013568641,0.93887764,0.00005708613,0.00030804655,0.00006481775,0.0008719632,0.00009529269,0.018209357,0.01530397,0.0042984555,0.02147741],"study_design_scores_gemma":[0.001468213,0.0008554327,0.9563225,0.000007699088,0.00019790792,0.00009760742,0.000020701193,0.0034590315,0.00042112597,0.0035925226,0.033197228,0.00036003123],"about_ca_topic_score_codex":0.00046597206,"about_ca_topic_score_gemma":0.0006708584,"teacher_disagreement_score":0.028898774,"about_ca_system_score_codex":0.0000019919053,"about_ca_system_score_gemma":0.000009453039,"threshold_uncertainty_score":0.99951607},"labels":[],"label_agreement":null},{"id":"W2014933081","doi":"10.1029/2005gl025145","title":"Crustal velocity structure across the southern Korean Peninsula from seismic refraction survey","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Crust; Peninsula; Seismology; Transect; Seismic refraction; Discontinuity (linguistics); Basin and Range Province; Mantle (geology); Cretaceous; Geophysics; Paleontology; Tectonics","score_opus":0.02485958721636855,"score_gpt":0.28145761248997825,"score_spread":0.2565980252736097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014933081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914921,0.00003240646,0.000068402434,0.0017224989,0.00039256454,0.0002621014,0.005780733,0.000044077922,0.00020510454],"genre_scores_gemma":[0.9960294,0.0000034974325,0.000051108844,0.00034777803,0.0016158343,0.000003227623,0.0016125644,0.000011851149,0.00032476525],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99631083,0.0009509007,0.00024271142,0.00050554995,0.0010848411,0.0009051611],"domain_scores_gemma":[0.9981659,0.0009846363,0.00008591767,0.00048798727,0.00013745151,0.00013810174],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009525977,0.0002115512,0.00025348688,0.000037905735,0.00081326114,0.00047327165,0.00060526305,0.00010306864,0.0007405997],"category_scores_gemma":[0.00012474153,0.00013813286,0.00009198418,0.00038808145,0.00045840445,0.00023025509,0.000087022265,0.0006621749,0.001236683],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002653553,0.00040292475,0.23665667,0.00011065905,0.00047828958,0.00036196917,0.006261425,0.035155654,0.50977236,0.00044025868,0.15679342,0.050912846],"study_design_scores_gemma":[0.00029219984,0.000051937557,0.9815408,0.00000862209,0.0000085428155,0.0000012459446,0.00017133236,0.0041276533,0.0017927754,0.004392501,0.0073857433,0.00022662207],"about_ca_topic_score_codex":0.39106542,"about_ca_topic_score_gemma":0.023989698,"teacher_disagreement_score":0.74488413,"about_ca_system_score_codex":0.000014653203,"about_ca_system_score_gemma":0.000061416824,"threshold_uncertainty_score":0.999541},"labels":[],"label_agreement":null},{"id":"W2015492492","doi":"10.1002/2014jb011638","title":"Multiparameter adjoint tomography of the crust and upper mantle beneath East Asia: 1. Model construction and comparisons","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":167,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Subduction; Crust; Seismology; Transition zone; Tectonics; Seismic tomography; Geophysics","score_opus":0.06514569360163264,"score_gpt":0.3020480019943682,"score_spread":0.23690230839273557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015492492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982162,0.00021843964,0.00013084024,0.00036738836,0.0001822452,0.00014269548,0.00007744046,0.0000033194199,0.00066142797],"genre_scores_gemma":[0.9968962,0.00007087718,0.00273663,0.000017583283,0.0001926845,5.4199637e-7,0.000002386275,0.0000039943443,0.00007907913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982083,0.00023365357,0.00032793614,0.0001547851,0.00076568464,0.0003096311],"domain_scores_gemma":[0.99876416,0.00016419575,0.00018321362,0.00017140467,0.0003974972,0.00031954012],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080924924,0.00011441754,0.0003664105,0.00012527456,0.00015027849,0.00010750204,0.00019825099,0.00006045492,0.000042464246],"category_scores_gemma":[0.00013897703,0.000068582696,0.0000995949,0.0002181971,0.00058942067,0.0002524283,0.000074472715,0.0003788007,0.0000108210525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004714583,0.0015032283,0.73179805,0.0007050011,0.0013372871,0.00013360835,0.010587936,0.05332765,0.060917784,0.013475681,0.01886987,0.102629304],"study_design_scores_gemma":[0.0018651956,0.001500815,0.858101,0.0002106382,0.000095987125,0.00013421755,0.0015827605,0.10913299,0.007754558,0.016345935,0.0029769074,0.0002989804],"about_ca_topic_score_codex":0.00060351606,"about_ca_topic_score_gemma":0.00010385143,"teacher_disagreement_score":0.12630294,"about_ca_system_score_codex":0.0000023352363,"about_ca_system_score_gemma":0.00014052317,"threshold_uncertainty_score":0.27967212},"labels":[],"label_agreement":null},{"id":"W2015856353","doi":"10.1063/1.3675478","title":"Time-resolved one-dimensional detection of x-ray scattering in pulsed magnetic fields","year":2012,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brockhouse Institute for Materials Research; Canadian Institute for Advanced Research; McMaster University","funders":"U.S. Department of Energy","keywords":"Detector; Optics; Diffraction; Physics; Reciprocal lattice; STRIPS; Synchronizing; Magnetic field; Scattering; Materials science; Computer science","score_opus":0.014114801314772467,"score_gpt":0.21920805905007387,"score_spread":0.2050932577353014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015856353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99511045,0.0029465328,0.000002566275,0.00002605342,0.000988173,0.0002510146,0.000043609914,0.0000054931616,0.00062608375],"genre_scores_gemma":[0.9991123,0.00035652562,0.0002246327,0.00004374908,0.000036021735,0.0000019340082,0.00005393305,0.000002210469,0.00016870102],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987483,0.00008240253,0.0004173566,0.00016605412,0.00034499317,0.0002409096],"domain_scores_gemma":[0.9994879,0.000023863202,0.00016774713,0.00020782741,0.000046647354,0.000066031374],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00096008874,0.00009009093,0.00027861155,0.00009721061,0.000057219568,0.00001878219,0.00016176638,0.0000385323,0.0026204393],"category_scores_gemma":[0.000028972541,0.00007609935,0.000056158886,0.00029000032,0.00011335617,0.00022318211,0.000025650723,0.00004912713,0.00021464491],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004552499,0.00024193544,0.027700745,0.0059787626,0.000036330788,0.0000010441432,0.0002083337,0.00013655142,0.44065845,0.000014949745,0.00026383292,0.5247136],"study_design_scores_gemma":[0.001521562,0.00047398385,0.68925047,0.015158937,0.00020443651,0.000009496328,0.000033000968,0.005590567,0.27116194,0.00031315742,0.015458718,0.0008237662],"about_ca_topic_score_codex":0.00023308977,"about_ca_topic_score_gemma":0.000035467983,"teacher_disagreement_score":0.6615497,"about_ca_system_score_codex":0.0000035097319,"about_ca_system_score_gemma":0.000024191359,"threshold_uncertainty_score":0.9982913},"labels":[],"label_agreement":null},{"id":"W2016492658","doi":"10.1029/2001gl014109","title":"Effects of nonlinear rheology on degree 2 harmonic deformation in a spherical self‐gravitating earth","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Rheology; Mantle (geology); Geology; Nonlinear system; Geophysics; Post-glacial rebound; Spherical harmonics; Physics; Glacial period; Thermodynamics","score_opus":0.03232915629991261,"score_gpt":0.26804558854252797,"score_spread":0.23571643224261535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016492658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981744,0.000047022026,0.000037199607,0.0006391345,0.00013710093,0.0003243995,0.000016666032,0.000025955089,0.0005980999],"genre_scores_gemma":[0.99798876,0.000026704894,0.0014201823,0.00025468686,0.00020154406,0.000008648871,0.000023704564,0.000006219371,0.000069538226],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99759895,0.0005065437,0.00027735095,0.00029177216,0.00065932475,0.00066604884],"domain_scores_gemma":[0.99832743,0.0012122634,0.000067617795,0.00020122099,0.000056480614,0.00013498693],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045393725,0.00014190115,0.00029495035,0.0001419639,0.00010753166,0.0000456123,0.00027748136,0.000070014314,0.00028181952],"category_scores_gemma":[0.000237117,0.00011566608,0.00007131897,0.0005036095,0.00017160951,0.00017534502,0.000037265534,0.00040194474,0.0011056572],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013037963,0.0023688138,0.023540009,0.0018775403,0.00026736638,0.0008826619,0.007876668,0.0062662563,0.7701737,0.0037701512,0.0067863455,0.17488664],"study_design_scores_gemma":[0.0022204972,0.0020834475,0.865294,0.00021842158,0.000024289902,0.0000053494737,0.00008323555,0.08385355,0.042094607,0.0012227237,0.0023519052,0.00054802356],"about_ca_topic_score_codex":0.0018543614,"about_ca_topic_score_gemma":0.00011507369,"teacher_disagreement_score":0.84175396,"about_ca_system_score_codex":0.0000084656385,"about_ca_system_score_gemma":0.000019828352,"threshold_uncertainty_score":0.9996721},"labels":[],"label_agreement":null},{"id":"W2016517503","doi":"10.1111/j.1365-246x.1976.tb01244.x","title":"Mantle Plume Separation and the Expanding Earth","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal of the Royal Astronomical Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Plume; Geology; Mantle plume; Mantle (geology); Geodesy; Geophysics; Hotspot (geology); Solid earth; Great circle; RADIUS; Panache; Geometry; Seismology; Meteorology; Physics; Tectonics; Lithosphere; Mathematics","score_opus":0.004968009347092078,"score_gpt":0.2061564098797373,"score_spread":0.20118840053264522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016517503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979386,0.00006489192,0.0006678764,0.0005054236,0.00046453648,0.00008526188,0.000010163473,0.000004268864,0.0002590072],"genre_scores_gemma":[0.9981025,0.0000025283234,0.0005719299,0.00009242171,0.0010323853,1.7413771e-7,0.0000019234517,0.000002644748,0.00019347844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908626,0.00008333329,0.0002836027,0.00009849813,0.00021202707,0.00023625785],"domain_scores_gemma":[0.9993148,0.00023765981,0.00021432506,0.000104418905,0.000030380726,0.00009841225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007695732,0.000100677964,0.00022330308,0.000006172841,0.00023558798,0.00009209675,0.0002477295,0.000043659507,0.0001086504],"category_scores_gemma":[0.000015979724,0.000047835485,0.0002806719,0.000051138308,0.0002462725,0.000101104495,0.000044159337,0.00022339028,0.000028669463],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008315422,0.0007197586,0.44431424,0.00017630098,0.002907308,0.000017995248,0.011776224,0.30439016,0.019297382,0.018376188,0.025253955,0.16445506],"study_design_scores_gemma":[0.0012459692,0.00009962794,0.98094016,0.000018368703,0.00008052266,0.0000023394673,0.00018224618,0.01142475,0.0010994803,0.0017267625,0.0030608636,0.00011893092],"about_ca_topic_score_codex":0.00019906796,"about_ca_topic_score_gemma":0.00001992575,"teacher_disagreement_score":0.5366259,"about_ca_system_score_codex":0.000004671275,"about_ca_system_score_gemma":0.000024943967,"threshold_uncertainty_score":0.19506745},"labels":[],"label_agreement":null},{"id":"W2016973289","doi":"10.1029/2006gl027668","title":"Recycling the lid: Effects of subduction and stirring on boundary layer dynamics in bottom‐heated planetary mantle convection","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research; National Science Foundation","keywords":"Geology; Mantle (geology); Subduction; Mantle convection; Geophysics; Mantle wedge; Mantle plume; Transition zone; Lithosphere; Plate tectonics; Plume; Downwelling; Boundary layer; Convection; Upwelling; Venus; Tectonics; Mechanics; Astrobiology; Thermodynamics; Seismology; Oceanography","score_opus":0.014331118567103516,"score_gpt":0.2530985269157111,"score_spread":0.2387674083486076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016973289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975841,0.00007891579,0.000016946038,0.0012885479,0.00033140174,0.00030629907,0.000028278493,0.000018246557,0.00034726466],"genre_scores_gemma":[0.9993182,0.000036798563,0.000037191196,0.000089039895,0.00033721802,0.000004733908,0.00012271528,0.0000057544453,0.000048365102],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9983155,0.00034508752,0.0001963053,0.00027494773,0.000461545,0.00040658267],"domain_scores_gemma":[0.9988658,0.0008195675,0.00004995875,0.00017954709,0.000030983418,0.000054153414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005494851,0.00011819827,0.00019322435,0.00013385383,0.00020937642,0.00009240155,0.00014038966,0.000057475496,0.000029129405],"category_scores_gemma":[0.000054994678,0.00008573389,0.000032500167,0.0002885009,0.00023346291,0.00013920089,0.000024391069,0.0004022445,0.000052760883],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00224416,0.00052514154,0.27935815,0.0013821974,0.00017617976,0.0004452797,0.00086783833,0.019813761,0.64419013,0.0059632515,0.0069576045,0.038076308],"study_design_scores_gemma":[0.0004806076,0.00028283725,0.9701037,0.000121262565,0.000012169208,0.0000037361594,0.00006080221,0.013479035,0.011657666,0.003122778,0.0005093999,0.00016603018],"about_ca_topic_score_codex":0.034759782,"about_ca_topic_score_gemma":0.0020732717,"teacher_disagreement_score":0.69074553,"about_ca_system_score_codex":0.000017887696,"about_ca_system_score_gemma":0.000021803035,"threshold_uncertainty_score":0.9716678},"labels":[],"label_agreement":null},{"id":"W2017119638","doi":"10.1038/nature06123","title":"Electronic and structural transitions in dense liquid sodium","year":2007,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":154,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Melting point; Alkali metal; Sodium; Ambient pressure; Chemical physics; Chemistry; Condensed matter physics; Lithium (medication); Electronic structure; Ab initio; Materials science; Thermodynamics; Computational chemistry; Physics; Composite material","score_opus":0.003047219520273503,"score_gpt":0.20885419388330562,"score_spread":0.2058069743630321,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017119638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972442,0.0011214155,0.000008752325,0.00037188997,0.00022332411,0.00006465889,0.000044515225,0.000014007115,0.00090727827],"genre_scores_gemma":[0.99938184,0.000021999089,0.00007299428,0.00029091016,0.0001304434,1.5486647e-7,0.00005244609,0.0000015294477,0.00004766549],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99947035,0.000016030102,0.00007726278,0.00011515491,0.000082054445,0.00023916688],"domain_scores_gemma":[0.9998472,0.000022874876,0.000014981644,0.00005804458,0.000011786959,0.00004513443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015384474,0.00006272676,0.00007998256,0.000039972165,0.000053176613,0.000022595415,0.000055431854,0.00025936877,0.00030416515],"category_scores_gemma":[0.0000059384815,0.000049846676,0.000014520962,0.000088868146,0.000021749582,0.00008001539,0.0000025050904,0.0004571987,0.000013688482],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.010117443,0.00022052544,0.35564888,0.0007185265,0.00044849966,0.0016256565,0.021349965,0.0040417397,0.36528355,0.11291859,0.01002533,0.11760131],"study_design_scores_gemma":[0.0006246613,0.00026703137,0.9669104,0.000016351216,0.000019854684,0.00004475434,0.00012713888,0.00033921553,0.0070600547,0.0076679,0.016630605,0.00029201055],"about_ca_topic_score_codex":0.00023430106,"about_ca_topic_score_gemma":0.006742806,"teacher_disagreement_score":0.61126155,"about_ca_system_score_codex":0.0000017358044,"about_ca_system_score_gemma":0.000019876048,"threshold_uncertainty_score":0.37626442},"labels":[],"label_agreement":null},{"id":"W2017208652","doi":"10.1029/2005gc001053","title":"Differences between Archean and Proterozoic lithospheres: Assessment of the possible major role of thermal conductivity","year":2006,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archean; Geology; Mantle convection; Craton; Mantle (geology); Lithosphere; Proterozoic; Geophysics; Geochemistry; Petrology; Earth's internal heat budget; Mantle plume; Seismology; Tectonics","score_opus":0.008036319166365307,"score_gpt":0.20436166595127012,"score_spread":0.19632534678490482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017208652","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99445176,0.00024800675,0.000010749953,0.000024957326,0.00013236386,0.00036517187,0.00076057465,0.000017369837,0.0039890483],"genre_scores_gemma":[0.99922436,0.000002860876,0.00010568639,0.0000024265262,0.00035121822,0.000007945175,0.00008417418,0.0000058571063,0.00021545905],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844176,0.00012499752,0.00042417232,0.0003083199,0.00039418996,0.00030654707],"domain_scores_gemma":[0.9988452,0.000126762,0.00044628402,0.0004239023,0.00009293132,0.00006490069],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027101714,0.00021860837,0.00048456146,0.000013433256,0.00013924342,0.000056384706,0.00036006043,0.00010055153,0.00011627416],"category_scores_gemma":[0.000008625257,0.00014850512,0.00010066395,0.00014959495,0.00023306256,0.00011717741,0.0000683814,0.00013703313,0.00000323336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008935596,0.00004674172,0.72454435,0.00045282562,0.000057284375,6.8614366e-7,0.000096834796,0.000070079295,0.27366608,0.0002114859,0.00001278407,0.00083191827],"study_design_scores_gemma":[0.00022361634,0.000051622857,0.8537488,0.00009892186,0.00005030987,0.000001841135,0.00014730313,0.00036990942,0.13997209,0.0051226635,0.00004855593,0.00016433315],"about_ca_topic_score_codex":0.01915974,"about_ca_topic_score_gemma":0.00024677947,"teacher_disagreement_score":0.133694,"about_ca_system_score_codex":0.0000035751948,"about_ca_system_score_gemma":0.00010588148,"threshold_uncertainty_score":0.98737174},"labels":[],"label_agreement":null},{"id":"W2017695905","doi":"10.2113/gscanmin.43.4.1411","title":"RIETVELD REFINEMENT OF CLINOPYROXENES WITH INTERMEDIATE Ca-CONTENT ALONG THE JOIN DIOPSIDE ENSTATITE","year":2005,"lang":"en","type":"article","venue":"The Canadian Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Diopside; Enstatite; Geology; Join (topology); Rietveld refinement; Geochemistry; Mineralogy; Crystallography; Chemistry; Mathematics; Crystal structure; Meteorite; Combinatorics; Physics; Astrobiology; Chondrite","score_opus":0.025480752903742975,"score_gpt":0.20455638060681006,"score_spread":0.1790756277030671,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017695905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856679,0.00031308964,0.000008629997,0.007443993,0.00027992704,0.00023701685,0.00051394926,0.0000097432385,0.0055257482],"genre_scores_gemma":[0.99602807,0.00003696069,0.00019558061,0.001684141,0.00029023914,0.000004485421,0.000118618096,0.000004751548,0.0016371841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895096,0.000085163585,0.00026417163,0.00016203223,0.00018794189,0.0003497059],"domain_scores_gemma":[0.999223,0.000088182795,0.00012219747,0.0003368478,0.00006171567,0.00016805492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003810917,0.00014263252,0.00018894975,0.000043670185,0.0002474026,0.00008114607,0.00036382722,0.00003456861,0.00090202154],"category_scores_gemma":[0.000028468685,0.0000670211,0.000043135416,0.000103227554,0.00033505823,0.000074082156,0.0000114175555,0.0000970176,0.00011144103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082178455,0.00012594934,0.50184447,0.00026806234,0.001078487,0.00044117813,0.01202976,0.06068778,0.014825788,0.016741509,0.28112793,0.11000726],"study_design_scores_gemma":[0.0005793513,0.00026379697,0.8045425,0.000064096654,0.0000916457,0.000023044291,0.00033009233,0.0010140423,0.0017290437,0.00027186816,0.1907444,0.00034614347],"about_ca_topic_score_codex":0.8432787,"about_ca_topic_score_gemma":0.9928529,"teacher_disagreement_score":0.302698,"about_ca_system_score_codex":0.000013101807,"about_ca_system_score_gemma":0.000197512,"threshold_uncertainty_score":0.98765033},"labels":[],"label_agreement":null},{"id":"W2017923954","doi":"10.1111/j.1755-6724.2012.00608.x","title":"Elastic and Seismic Properties of Dabie‐Sulu Ultrahigh Pressure Metamorphic Rocks","year":2012,"lang":"en","type":"article","venue":"Acta Geologica Sinica - English Edition","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"Chinese Academy of Geological Sciences; Ministry of Land and Resources of the People's Republic of China; Guangzhou Institute of Geochemistry, Chinese Academy of Sciences; Chinese Academy of Sciences","keywords":"Felsic; Mafic; Eclogite; Metamorphic rock; Geology; Gneiss; Protolith; Anorthite; Geochemistry; Bulk modulus; Plagioclase; Mineralogy; Quartz; Subduction; Materials science; Composite material","score_opus":0.016559486733205002,"score_gpt":0.19081522259153452,"score_spread":0.1742557358583295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017923954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934632,0.0014258103,0.000033279946,0.00016444674,0.0021987928,0.00025807603,0.00028157435,0.000089360656,0.0020854347],"genre_scores_gemma":[0.9976397,0.00022118054,0.000088857814,0.00009235233,0.0015996819,0.000007640385,0.00019262191,0.000005667987,0.0001522918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851954,0.00018753085,0.0003520618,0.00028164257,0.00025420703,0.00040499025],"domain_scores_gemma":[0.9990036,0.00023941461,0.00022384229,0.00024776897,0.00013602576,0.00014937272],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046210244,0.00020293031,0.00037130777,0.000055404616,0.00014993193,0.000052596308,0.00020963345,0.00019001313,0.0013483892],"category_scores_gemma":[0.00047719336,0.00014143442,0.000060422368,0.0001155011,0.00023412437,0.0006962887,0.000038879778,0.00016131184,0.000028817856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022765717,0.0024795905,0.6091669,0.0032331028,0.0025018712,0.000037811515,0.021659216,0.019753445,0.23331024,0.0029595727,0.0873532,0.01526843],"study_design_scores_gemma":[0.0010728225,0.0008961375,0.8010055,0.00016323823,0.0007450612,0.000027094731,0.00052228925,0.0016209199,0.021257127,0.0018852674,0.16991356,0.00089099957],"about_ca_topic_score_codex":0.00037952283,"about_ca_topic_score_gemma":0.000023182887,"teacher_disagreement_score":0.2120531,"about_ca_system_score_codex":0.0000014407194,"about_ca_system_score_gemma":0.000025062507,"threshold_uncertainty_score":0.9995645},"labels":[],"label_agreement":null},{"id":"W2018352513","doi":"10.1029/2012jb009639","title":"P‐wave tomography of eastern North America: Evidence for mantle evolution from Archean to Phanerozoic, and modification during subsequent hot spot tectonism","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies; Leverhulme Trust; Université du Québec à Montréal","keywords":"Geology; Craton; Archean; Terrane; Proterozoic; Lithosphere; Magmatism; Mantle (geology); Earth science; Phanerozoic; Paleontology; Seismology; Geochemistry; Tectonics; Structural basin; Cenozoic","score_opus":0.09011731236591311,"score_gpt":0.3227740299132828,"score_spread":0.2326567175473697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018352513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99690413,0.0011593787,0.001127361,0.00015206641,0.00017879806,0.0003271969,0.00011107277,0.0000060604943,0.000033947992],"genre_scores_gemma":[0.99631846,0.0001413181,0.0026615674,0.000010259769,0.00078750815,0.000005517912,0.000013928858,0.000007344593,0.000054089047],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.997824,0.00022131627,0.0004061199,0.00020775011,0.0008137382,0.00052706036],"domain_scores_gemma":[0.998028,0.00071937946,0.00024705505,0.00021240929,0.00037999885,0.00041318647],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065754354,0.00013931887,0.0003513017,0.000051230236,0.00017333929,0.00007816784,0.0002654722,0.00004653339,0.00012253458],"category_scores_gemma":[0.00028981603,0.00010671867,0.0001222372,0.0003328284,0.00018418237,0.00051711354,0.00004812576,0.00020784345,0.000033260403],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.006554415,0.0006535506,0.4166847,0.0005368734,0.00044044977,0.000029468038,0.0035395098,0.0020039463,0.49462906,0.0004260809,0.0005450425,0.07395692],"study_design_scores_gemma":[0.0003487881,0.0007650812,0.9802753,0.0001547762,0.000035477264,0.0000034194745,0.0002312875,0.0010657655,0.014968946,0.0016664597,0.00035290825,0.00013179705],"about_ca_topic_score_codex":0.0067530684,"about_ca_topic_score_gemma":0.0003490722,"teacher_disagreement_score":0.5635906,"about_ca_system_score_codex":0.000017250804,"about_ca_system_score_gemma":0.000078741505,"threshold_uncertainty_score":0.99986106},"labels":[],"label_agreement":null},{"id":"W2018553921","doi":"10.1029/2001gl013712","title":"The influence of continental surface area on the assembly time for supercontinents","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Supercontinent; Geology; Mantle (geology); Geophysics; Geodesy; Paleontology; Tectonics; Craton","score_opus":0.03452787916867365,"score_gpt":0.26484538228545107,"score_spread":0.23031750311677743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018553921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98668176,0.000031061525,0.0000026800965,0.011790373,0.000108868335,0.0005256272,0.00016075558,0.000014185371,0.0006846618],"genre_scores_gemma":[0.99837935,0.000023523606,0.000020217303,0.00043223423,0.00017743681,0.000010379454,0.000019909046,0.000006066727,0.0009308672],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99780655,0.00029432913,0.00021588911,0.00026041348,0.0007841023,0.00063871243],"domain_scores_gemma":[0.9958805,0.0034319437,0.00005702397,0.00038599072,0.00014405571,0.00010049531],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00092217,0.00013466057,0.00019858021,0.000026308036,0.0005238533,0.00016309635,0.0006800528,0.00003713538,0.00029629646],"category_scores_gemma":[0.00040985,0.0000698843,0.000107097185,0.00017785729,0.00043154057,0.00013745787,0.00004458249,0.00022445904,0.0009851996],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038099225,0.00016730708,0.003085466,0.000045976376,0.00013690618,0.00001675775,0.0004858224,0.0047100647,0.8497834,0.0021747092,0.13605559,0.002956996],"study_design_scores_gemma":[0.0023656162,0.0020926485,0.7393722,0.00025094487,0.00006441933,0.00000398398,0.0002745325,0.05140613,0.053730085,0.0044713253,0.14493972,0.0010283873],"about_ca_topic_score_codex":0.0012854123,"about_ca_topic_score_gemma":0.000049875824,"teacher_disagreement_score":0.79605335,"about_ca_system_score_codex":0.0000040701752,"about_ca_system_score_gemma":0.000013640555,"threshold_uncertainty_score":0.99979264},"labels":[],"label_agreement":null},{"id":"W2018560750","doi":"10.1029/2001jb000889","title":"Style of density stratification in the mantle and true polar wander induced by ice loading","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mantle (geology); Buoyancy; Geology; Adiabatic process; Stratification (seeds); Geophysics; Physics; Thermodynamics","score_opus":0.0425720052261674,"score_gpt":0.28583346358454326,"score_spread":0.24326145835837587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018560750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997942,0.00053407956,0.000010849412,0.0004183461,0.000048621863,0.0001086235,0.000013115156,0.0000017618431,0.00092262926],"genre_scores_gemma":[0.99948835,0.00013869967,0.00011161745,0.000028533028,0.00014992422,4.287541e-7,0.0000028813763,0.0000026182322,0.000076961194],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9982286,0.00041057845,0.00029747374,0.000121489305,0.00068666413,0.00025521024],"domain_scores_gemma":[0.9988565,0.0005945258,0.00014707251,0.0001440507,0.00016192325,0.00009593684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011320439,0.0000807675,0.00022034571,0.000017450597,0.000119601114,0.000108232176,0.00028522816,0.000051222043,0.00046394486],"category_scores_gemma":[0.00018219715,0.000049776652,0.00004386955,0.00026153086,0.00012012357,0.00027088885,0.000016821374,0.00034487597,0.00003003711],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009031595,0.001333655,0.09313185,0.0003303077,0.00026174798,0.00017015438,0.0081459675,0.00019666161,0.7541249,0.0043218266,0.03837518,0.09870463],"study_design_scores_gemma":[0.0009509854,0.001420614,0.95732987,0.00010539154,0.000029716886,0.000020940348,0.00190709,0.0030860782,0.02106069,0.011031996,0.0028459972,0.00021065513],"about_ca_topic_score_codex":0.004176007,"about_ca_topic_score_gemma":0.00047844273,"teacher_disagreement_score":0.86419797,"about_ca_system_score_codex":0.0000043721234,"about_ca_system_score_gemma":0.00003101279,"threshold_uncertainty_score":0.63129014},"labels":[],"label_agreement":null},{"id":"W2018758912","doi":"10.1029/2004jb003114","title":"Effect of plastic‐viscous layering and strain softening on mode selection during lithospheric extension","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Dissipation; Strain rate; Materials science; Softening; Viscosity; Mechanics; Shearing (physics); Shear rate; Simple shear; Deformation (meteorology); Shear (geology); Composite material; Thermodynamics; Physics","score_opus":0.014254560275623414,"score_gpt":0.2927199691219359,"score_spread":0.27846540884631243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018758912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991858,0.00022774293,0.00008081079,0.00004522831,0.0001361293,0.00012039473,0.000014390645,0.00001063455,0.00017887514],"genre_scores_gemma":[0.99808145,0.00009680226,0.0009733764,0.0000055544774,0.00074152526,8.1732856e-7,0.0000017455999,0.000008993701,0.000089751346],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99776477,0.00036519562,0.00037233802,0.00021073512,0.0008565129,0.0004304779],"domain_scores_gemma":[0.99790514,0.0013585668,0.0001992899,0.00011316979,0.00020549903,0.00021833081],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010080483,0.00015978591,0.00040878216,0.000029291776,0.00020459914,0.0000980092,0.00018335712,0.000067787085,0.00022279957],"category_scores_gemma":[0.0005021721,0.000111065754,0.00011131549,0.00025329928,0.000119202465,0.0003292957,0.000034324235,0.0004442878,0.000030132844],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0066039474,0.00025202247,0.040323213,0.0005933071,0.00026044366,0.00012445955,0.00052355166,0.118982434,0.5799845,0.00021620968,0.00030902657,0.2518269],"study_design_scores_gemma":[0.001644792,0.008732337,0.8545623,0.0005514162,0.00006269557,0.000049353173,0.000085590356,0.042405616,0.09047305,0.0008159411,0.0003305379,0.00028639077],"about_ca_topic_score_codex":0.0011510091,"about_ca_topic_score_gemma":0.0001259258,"teacher_disagreement_score":0.8142391,"about_ca_system_score_codex":0.000013612375,"about_ca_system_score_gemma":0.0000640236,"threshold_uncertainty_score":0.452913},"labels":[],"label_agreement":null},{"id":"W2018800485","doi":"10.1038/nature11571","title":"Mechanisms for oscillatory true polar wander","year":2012,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Division of Materials Research","keywords":"Geology; Lithosphere; Geophysics; Paleomagnetism; Hydrostatic equilibrium; Mantle (geology); Physics; Geodesy; Paleontology; Tectonics","score_opus":0.007669634064538862,"score_gpt":0.21693335969170685,"score_spread":0.209263725627168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018800485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96169186,0.007212756,0.0013572422,0.0009019848,0.012549549,0.00073179096,0.0016933033,0.00016107668,0.013700418],"genre_scores_gemma":[0.9962826,0.000008601148,0.0016731252,0.00086544757,0.00059244345,0.0000014050227,0.0001177293,0.000003884391,0.00045479368],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993731,0.000020552545,0.00007503003,0.000113634494,0.00013820306,0.00027947864],"domain_scores_gemma":[0.9996741,0.00004505733,0.000032546068,0.000121350036,0.0000260328,0.000100918434],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022812877,0.000086521715,0.00011334977,0.000022851304,0.00010525889,0.00003059955,0.00011204596,0.00043979878,0.0010909131],"category_scores_gemma":[0.000020778227,0.00006309713,0.000047578596,0.00004834289,0.000011999284,0.00016428376,0.0000059520903,0.00024448262,0.00016394988],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006547095,0.00026855659,0.11317118,0.0006349735,0.00051381055,0.000016193939,0.0029062359,0.0004114059,0.13847145,0.31902283,0.3757461,0.048182525],"study_design_scores_gemma":[0.0004681531,0.00009283994,0.16184482,0.000010471645,0.00004590691,0.00000614965,0.000058454305,0.00012738115,0.011453284,0.022015417,0.8035356,0.00034152693],"about_ca_topic_score_codex":0.000078901096,"about_ca_topic_score_gemma":0.00004827181,"teacher_disagreement_score":0.4277895,"about_ca_system_score_codex":0.000001265942,"about_ca_system_score_gemma":0.000015902491,"threshold_uncertainty_score":0.9998222},"labels":[],"label_agreement":null},{"id":"W2018978033","doi":"10.1029/2002jb002286","title":"Lithospheric structure across oblique continental collision in New Zealand from wide‐angle <i>P</i> wave modeling","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Seismology; Lithosphere; Crust; Mantle (geology); Low-velocity zone; Continental collision; Collision zone; Geophysics; Tectonics","score_opus":0.02701311379457307,"score_gpt":0.2880261159715224,"score_spread":0.26101300217694934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018978033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976139,0.00089248235,0.00018152164,0.00022764894,0.00044361214,0.00019451272,0.00014568983,0.00000869517,0.00029193284],"genre_scores_gemma":[0.99501884,0.00018059376,0.0033708885,0.00006532735,0.000622537,5.157135e-7,0.000022242433,0.000012828908,0.00070620765],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99662817,0.0005214652,0.00062094064,0.00031974146,0.0011245203,0.0007851524],"domain_scores_gemma":[0.99796635,0.0007916895,0.00020698037,0.00024387996,0.00032229046,0.0004688126],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00091902,0.00022597835,0.00056826643,0.00001847212,0.0001787614,0.00032218423,0.0004015323,0.00015466513,0.0012904663],"category_scores_gemma":[0.00061521097,0.0001645316,0.00015019185,0.0005492975,0.000112273345,0.00052760215,0.000048086997,0.00077317597,0.000059771803],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0064316536,0.0010800528,0.6744793,0.00015479124,0.00061472674,0.002431331,0.007545228,0.16208337,0.06403203,0.0016239601,0.04098958,0.038533952],"study_design_scores_gemma":[0.008445277,0.0031367098,0.6439873,0.00081003533,0.00007244461,0.00008219244,0.0027614415,0.0510359,0.023502715,0.21072645,0.054109704,0.0013298558],"about_ca_topic_score_codex":0.030586202,"about_ca_topic_score_gemma":0.009267077,"teacher_disagreement_score":0.2091025,"about_ca_system_score_codex":0.000024094701,"about_ca_system_score_gemma":0.0005061013,"threshold_uncertainty_score":0.99962246},"labels":[],"label_agreement":null},{"id":"W2019568187","doi":"10.1016/j.physb.2006.05.277","title":"Methodology and recent developments for using neutron diffraction to characterize the mechanical properties of rocks","year":2006,"lang":"en","type":"article","venue":"Physica B Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Beamline; Neutron diffraction; Materials science; Anisotropy; Crystal twinning; Neutron; Diffraction; Differential stress; Deformation (meteorology); Mineralogy; Composite material; Geology; Optics; Microstructure; Physics; Nuclear physics","score_opus":0.07137208843904047,"score_gpt":0.256147639968013,"score_spread":0.18477555152897251,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019568187","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99740565,0.000023093193,0.00074635394,0.0011307766,0.00025351337,0.00032350994,0.000044014905,0.000008420443,0.000064664564],"genre_scores_gemma":[0.9974282,0.0000035618657,0.0017337141,0.0005576657,0.00015054009,0.0000090873455,0.000026409605,0.000004857085,0.00008599642],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99929774,0.00009457678,0.00017391577,0.00016959573,0.00008973804,0.00017446105],"domain_scores_gemma":[0.99961513,0.000095506555,0.00009263098,0.00010423369,0.00006367311,0.000028846323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016875913,0.000094713556,0.00019652209,0.000021529457,0.00009590509,0.0000354838,0.00008264462,0.00003170631,0.00013464331],"category_scores_gemma":[0.000009170845,0.000061829676,0.000023314955,0.000054165084,0.000039528786,0.00008188907,0.000019811732,0.00003657654,0.000027342978],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014531895,0.000016794871,0.0005830012,0.000038403727,0.000021541608,2.3283238e-7,0.000116891104,0.000094346135,0.9972516,0.00012954268,0.0004110924,0.0011912682],"study_design_scores_gemma":[0.0005233118,0.00012310059,0.36639804,0.00004264606,0.00008929044,0.0000063016864,0.000075186035,0.00070064265,0.6145886,0.0022887879,0.014871839,0.00029222568],"about_ca_topic_score_codex":0.0012600672,"about_ca_topic_score_gemma":0.000109354136,"teacher_disagreement_score":0.38266292,"about_ca_system_score_codex":0.0000024280844,"about_ca_system_score_gemma":0.000019375473,"threshold_uncertainty_score":0.2521341},"labels":[],"label_agreement":null},{"id":"W2019825905","doi":"10.1016/j.jeurceramsoc.2004.02.018","title":"Mechanical and microstructural characterization of calcium aluminosilicate (CAS) and SiO2/CAS composites deformed at high temperature and high pressure","year":2004,"lang":"en","type":"article","venue":"Journal of the European Ceramic Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Alexander von Humboldt-Stiftung","keywords":"Materials science; Aluminosilicate; Calcium aluminosilicate; Composite material; Characterization (materials science); High pressure; Microstructure; Mineralogy; Nanotechnology; Engineering physics","score_opus":0.006435261648605551,"score_gpt":0.18847061932478723,"score_spread":0.18203535767618167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019825905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984223,0.00026129122,0.0000057804714,0.00060436915,0.0003772534,0.000110512214,0.00019820483,0.0000054950656,0.000014787032],"genre_scores_gemma":[0.99885255,0.00034019895,0.00031262578,0.00017452966,0.00022479614,6.81927e-8,0.00002810423,0.000006927475,0.00006019972],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99911666,0.00013977067,0.00029199553,0.00013984254,0.00017089346,0.00014081055],"domain_scores_gemma":[0.9993665,0.000039651415,0.00033473427,0.00010879353,0.000065405344,0.00008490514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028954435,0.00013379166,0.00025044364,0.000012771146,0.00020103858,0.0000884265,0.00015701953,0.00005814297,0.000022274528],"category_scores_gemma":[0.000011524534,0.00007874148,0.000072331335,0.00005494374,0.00014553104,0.00016103766,0.00008287821,0.00015975696,0.0000011452416],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005550376,0.000008621534,0.0065992866,0.00006057172,0.0000814701,0.0000039939673,0.00064994587,0.00010376769,0.9918341,0.000034553224,0.00009923418,0.0004689561],"study_design_scores_gemma":[0.0007379035,0.0001045262,0.9070647,0.000057016874,0.00010563559,0.000193971,0.000028389739,0.000068776935,0.09097413,0.00025709957,0.00030569843,0.00010215419],"about_ca_topic_score_codex":0.0001512677,"about_ca_topic_score_gemma":0.00001475265,"teacher_disagreement_score":0.90085995,"about_ca_system_score_codex":0.000005323107,"about_ca_system_score_gemma":0.000018376424,"threshold_uncertainty_score":0.32109845},"labels":[],"label_agreement":null},{"id":"W2020041704","doi":"10.1103/physrevlett.107.146102","title":"Pressure Solution at the Molecular Scale","year":2011,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Nautical Research Society","funders":"","keywords":"Scale (ratio); Materials science; Statistical physics; Physics; Quantum mechanics","score_opus":0.015809374074469203,"score_gpt":0.22309276252192234,"score_spread":0.20728338844745314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020041704","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9708526,0.018031895,0.00014676098,0.0046503553,0.00038011975,0.0005250262,0.0000764165,0.00005063742,0.0052861953],"genre_scores_gemma":[0.9909373,0.0006939581,0.00007844003,0.00801178,0.0001659445,0.000006791436,0.000036945174,0.000004128479,0.0000646955],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99913937,0.00012406752,0.00012462096,0.00019457372,0.00020452183,0.00021286536],"domain_scores_gemma":[0.99953103,0.000034498982,0.00006854477,0.0002859365,0.000014446475,0.000065572],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016019926,0.00011586581,0.00020178473,0.0000067361743,0.00011172134,0.000017776503,0.0002352252,0.000007693101,0.001306509],"category_scores_gemma":[0.000010123437,0.0000670793,0.00011447216,0.00008618748,0.00008883881,0.00009251081,0.000028782995,0.00006828936,0.0013242613],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022387295,0.0004823325,0.021218263,0.006184329,0.00082209264,0.00014086388,0.0027762938,0.0029768308,0.580872,0.006141175,0.30895513,0.06920684],"study_design_scores_gemma":[0.00053229247,0.00024016114,0.21805608,0.0012230988,0.0013674073,0.00002246449,0.000010972078,0.0048951013,0.027233608,0.0036762732,0.7414128,0.0013297247],"about_ca_topic_score_codex":0.0005091143,"about_ca_topic_score_gemma":0.000040697,"teacher_disagreement_score":0.55363834,"about_ca_system_score_codex":0.0000014060499,"about_ca_system_score_gemma":0.0000058412184,"threshold_uncertainty_score":0.99960643},"labels":[],"label_agreement":null},{"id":"W2020368491","doi":"10.1016/j.tecto.2006.04.010","title":"Petrofabrics and seismic properties of garnet peridotite from the UHP Sulu terrane (China): Implications for olivine deformation mechanism in a cold and dry subducting continental slab","year":2006,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Peridotite; Geology; Olivine; Enstatite; Metamorphic rock; Geochemistry; Seismic anisotropy; Mantle wedge; Metamorphism; Lineation; Pyroxene; Mantle (geology); Subduction; Petrology; Seismology; Meteorite; Tectonics; Chondrite","score_opus":0.009990455973007803,"score_gpt":0.18120775906780293,"score_spread":0.17121730309479513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020368491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979442,0.0002889468,0.00040371376,0.00032492567,0.000093136514,0.00037930315,0.0004916949,0.000018886056,0.000055205343],"genre_scores_gemma":[0.99923706,0.00003476012,0.0003253881,0.000044410674,0.00014386539,0.000010886427,0.00016727531,0.000005406966,0.000030955984],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99935764,0.00003230272,0.00022022812,0.00015637602,0.00007358302,0.0001598471],"domain_scores_gemma":[0.9996166,0.000072897325,0.00013070699,0.0001241733,0.00003291395,0.000022669325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014251562,0.00011299143,0.00018883999,0.00002648214,0.00013366208,0.00006616724,0.00009192309,0.000034449953,0.0000085217525],"category_scores_gemma":[0.00001234444,0.000079895784,0.000024082114,0.00008778396,0.00007105919,0.00023361597,0.000020789535,0.000055182496,0.000001717986],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111568515,0.000070598006,0.056877017,0.00021166545,0.000040363884,5.9646624e-7,0.0020131478,0.0015634676,0.9238571,0.0089725545,0.000114584735,0.0061673457],"study_design_scores_gemma":[0.0013560519,0.0002279433,0.79650086,0.00012466066,0.0000945011,0.000004813007,0.0004891699,0.03766963,0.13552128,0.026898365,0.00070536317,0.00040734283],"about_ca_topic_score_codex":0.018531194,"about_ca_topic_score_gemma":0.001333907,"teacher_disagreement_score":0.7883358,"about_ca_system_score_codex":0.0000033243214,"about_ca_system_score_gemma":0.000020080304,"threshold_uncertainty_score":0.9880045},"labels":[],"label_agreement":null},{"id":"W2020620266","doi":"10.1063/1.2837809","title":"On the pressure-induced loss of crystallinity in orthophosphates of zinc and calcium","year":2008,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Institute for Nanotechnology; Western University","funders":"","keywords":"Zinc; Crystallinity; Metal; Calcium; Raman spectroscopy; Phosphate; Zinc phosphate; Chemistry; Inorganic chemistry; Crystallography; Organic chemistry","score_opus":0.025027113233298877,"score_gpt":0.226350046229563,"score_spread":0.20132293299626414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020620266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991997,0.00022092107,0.000011426201,0.00013782056,0.0000717695,0.0000617615,0.000032910317,0.0000013040462,0.00026238913],"genre_scores_gemma":[0.9997156,0.00009810212,0.000025452897,0.000042386484,0.00010751143,1.0009916e-7,0.0000016591138,0.000002325772,0.0000068262434],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99918014,0.000089229645,0.00031338353,0.00005249793,0.00025427135,0.000110477675],"domain_scores_gemma":[0.998871,0.00056764303,0.00032249946,0.00012145305,0.00007654107,0.000040857405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039729598,0.00008178551,0.0002634853,0.000011107424,0.00003203087,0.0000050011377,0.00023463301,0.00003626971,0.00005832235],"category_scores_gemma":[0.000060824284,0.000040350613,0.00005409638,0.00009529048,0.00018664575,0.000072768846,0.0000177498,0.000167005,0.0000017993951],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012096651,0.00028374195,0.016314825,0.0001392278,0.00018691998,0.000018668308,0.0025214525,0.0039205533,0.9716256,0.0017823689,0.00065127306,0.001345702],"study_design_scores_gemma":[0.0005105175,0.00024611395,0.029358273,0.000085421365,0.000071714574,0.0000187958,0.00004408532,0.00033233754,0.9419188,0.027181497,0.00012614923,0.00010630634],"about_ca_topic_score_codex":0.0002785971,"about_ca_topic_score_gemma":0.000004165857,"teacher_disagreement_score":0.029706815,"about_ca_system_score_codex":9.5049427e-7,"about_ca_system_score_gemma":0.000039184924,"threshold_uncertainty_score":0.16454501},"labels":[],"label_agreement":null},{"id":"W2020712329","doi":"10.1016/j.tecto.2011.04.015","title":"Mantle convection models featuring plate tectonic behavior: An overview of methods and progress","year":2011,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; The Scarborough Hospital","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Plate tectonics; Mantle convection; Mantle (geology); Geology; Convection; Geophysics; Hotspot (geology); Ocean surface topography; Tectonics; Mechanics; Subduction; Seismology; Geodesy; Physics","score_opus":0.11595014873004203,"score_gpt":0.3286305688821093,"score_spread":0.21268042015206726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020712329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99662757,0.0011704589,0.0004354689,0.0000026909752,0.0002710189,0.0002473404,0.000063953725,0.000068232155,0.0011132373],"genre_scores_gemma":[0.9850178,0.00021785637,0.014626282,0.000008921476,0.00006190346,0.0000067630763,0.000029973113,0.000008603347,0.000021925776],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99911505,0.000099644916,0.00020011305,0.00025776398,0.00010772085,0.00021968514],"domain_scores_gemma":[0.9994448,0.000025283094,0.00013505461,0.0002556978,0.000055186636,0.00008402161],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024153978,0.00015427888,0.00027628653,0.000044623263,0.00008779815,0.000033075594,0.00015043102,0.000068846995,0.00022824307],"category_scores_gemma":[0.0000027187089,0.00013170388,0.000040496176,0.00014881715,0.000106773776,0.00041686557,0.000025921086,0.00008860631,0.000012996504],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039886977,0.0006069095,0.04028158,0.0010018114,0.0002895667,0.00003637179,0.006152627,0.0010503741,0.10702613,0.019846536,0.000036384154,0.8232728],"study_design_scores_gemma":[0.00083687226,0.0010193379,0.6448203,0.00012486886,0.00034221902,0.000027032616,0.00014503789,0.013742499,0.29226375,0.045518696,0.00032393623,0.00083545933],"about_ca_topic_score_codex":0.0018186149,"about_ca_topic_score_gemma":0.000071973234,"teacher_disagreement_score":0.8224374,"about_ca_system_score_codex":0.0000021696176,"about_ca_system_score_gemma":0.000024929244,"threshold_uncertainty_score":0.5370729},"labels":[],"label_agreement":null},{"id":"W2020740664","doi":"10.1139/e10-009","title":"Mantle heterogeneities and their significance: results from Lithoprobe seismic reflection and refraction – wide-angle reflection studiesThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.Lithoprobe Contribution 1486.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Geology; Lithosphere; Craton; Mantle (geology); Subduction; Archean; Seismology; Tectonics; Geophysics; Paleontology","score_opus":0.013375847078095526,"score_gpt":0.20810172393337018,"score_spread":0.19472587685527465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020740664","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950344,0.000776744,0.000010595473,0.0027021896,0.0004082217,0.00030521266,0.00021359428,0.000002595364,0.0005464645],"genre_scores_gemma":[0.99921656,0.0002995788,0.00015806351,0.00006829264,0.00020164014,0.0000024973485,0.000004815687,0.000002456441,0.000046119192],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99858296,0.00022780348,0.0005204606,0.00021473631,0.00025071527,0.00020335107],"domain_scores_gemma":[0.998378,0.00046420106,0.0006633362,0.00012684343,0.00027271375,0.000094947805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022426713,0.00012552463,0.00034571072,0.00015515334,0.00030485343,0.0001410638,0.00014126055,0.000071362076,0.00020536732],"category_scores_gemma":[0.0007879058,0.00006986446,0.000036173627,0.00041789107,0.0011136981,0.0005612724,0.000010305796,0.00018146314,4.5858948e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013348309,0.00026167635,0.61063194,0.00068199093,0.0007071192,0.000021377658,0.082190216,0.0019308976,0.2569667,0.0035707275,0.0022862768,0.027402794],"study_design_scores_gemma":[0.0049305325,0.0043933485,0.58258784,0.0008265034,0.00022697775,0.00010447123,0.014397615,0.001632968,0.34793127,0.027243916,0.015194002,0.0005305732],"about_ca_topic_score_codex":0.050164487,"about_ca_topic_score_gemma":0.18026793,"teacher_disagreement_score":0.13010344,"about_ca_system_score_codex":0.0000054552597,"about_ca_system_score_gemma":0.00029786793,"threshold_uncertainty_score":0.95616055},"labels":[],"label_agreement":null},{"id":"W2021350091","doi":"10.1063/1.2126125","title":"Compton scattering of elemental silicon at high pressure","year":2005,"lang":"en","type":"article","venue":"Applied Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); Steacie Institute for Molecular Sciences; University of Saskatchewan","funders":"","keywords":"Compton scattering; Monochromator; Silicon; Scattering; Synchrotron radiation; Optics; Materials science; Metastability; Physics; Optoelectronics","score_opus":0.0069962151306101235,"score_gpt":0.18534268445245064,"score_spread":0.1783464693218405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021350091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99703264,0.000029113364,0.00006945973,0.0003326135,0.00019314844,0.00019282389,0.00019864248,0.000035259192,0.0019163049],"genre_scores_gemma":[0.997816,0.000004227634,0.000488924,0.0008051321,0.00056486693,0.0000034699083,0.00026823796,0.000007911497,0.000041199874],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989893,0.000019213947,0.00022066297,0.00024943703,0.00023949759,0.00028189487],"domain_scores_gemma":[0.99951303,0.00004032281,0.00013457726,0.0002389584,0.0000104898345,0.00006260028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000078816505,0.00016414608,0.00024254712,0.000020834515,0.00009943691,0.00002951319,0.000179761,0.00003376173,0.00089517294],"category_scores_gemma":[5.1687203e-7,0.00015331923,0.000053440308,0.00007653814,0.00009404938,0.00011722981,0.00003997469,0.00006570666,0.00032044115],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046130644,0.000027933771,0.0052870847,0.00004993288,0.00007147307,0.0000011161217,0.00018883302,0.03847386,0.94701153,0.0010339282,0.0024897358,0.005318439],"study_design_scores_gemma":[0.0011602683,0.00006181521,0.08367138,0.000027059194,0.0001313521,0.0000025200181,0.000036511254,0.0010311414,0.8826629,0.0003545591,0.03022555,0.0006349369],"about_ca_topic_score_codex":0.00053043215,"about_ca_topic_score_gemma":0.00005506639,"teacher_disagreement_score":0.0783843,"about_ca_system_score_codex":0.000004197508,"about_ca_system_score_gemma":0.000006503877,"threshold_uncertainty_score":0.9801516},"labels":[],"label_agreement":null},{"id":"W2022932591","doi":"10.1016/j.precamres.2011.10.016","title":"Imaging Archaean-age whole mineral systems","year":2011,"lang":"en","type":"article","venue":"Precambrian Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Environment Research Council","keywords":"Geology; Mantle (geology); Peridotite; Geochemistry; Craton; Kimberlite; Lithosphere; Petrology; Archean; Geophysics; Seismology; Tectonics","score_opus":0.09303907220708757,"score_gpt":0.2934805800181565,"score_spread":0.20044150781106895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022932591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8276535,0.00074723084,0.000056753124,0.0001441072,0.0011216643,0.00049670157,0.00018167558,0.00009084788,0.16950749],"genre_scores_gemma":[0.99250495,0.00002013431,0.00033262078,0.000022101725,0.0005089145,0.000008999539,0.00007845276,0.000008883446,0.0065149283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976317,0.00044166934,0.00022531285,0.00036278134,0.0005843701,0.00075415085],"domain_scores_gemma":[0.9990711,0.00013054567,0.000040538205,0.0003866462,0.00012349829,0.00024762697],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0016846568,0.00013058494,0.00020220716,0.00017341803,0.000247259,0.00024217424,0.0005016424,0.000048339076,0.0016143849],"category_scores_gemma":[0.00006550682,0.000107387576,0.000046989826,0.00025147985,0.00020301536,0.00024983942,0.00007197677,0.00023130751,0.002410503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009489807,0.00038447732,0.64642686,0.0010111867,0.00030620335,0.0026960757,0.015254914,0.0005537439,0.08018644,0.018031726,0.09286466,0.14133471],"study_design_scores_gemma":[0.00060360413,0.00023503261,0.86691236,0.00011644835,0.000016743994,0.000037046488,0.0006739992,0.005951572,0.002061395,0.003728698,0.11913251,0.0005305944],"about_ca_topic_score_codex":0.023843022,"about_ca_topic_score_gemma":0.0010415086,"teacher_disagreement_score":0.22048548,"about_ca_system_score_codex":0.0000044613384,"about_ca_system_score_gemma":0.00006235968,"threshold_uncertainty_score":0.9992983},"labels":[],"label_agreement":null},{"id":"W2023593919","doi":"10.1029/2007jb005190","title":"Weakening of the subduction interface and its effects on surface heat flow, slab dehydration, and mantle wedge serpentinization","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":260,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Mantle wedge; Geology; Forearc; Slab; Subduction; Mantle (geology); Geophysics; Slab window; Wedge (geometry); Decoupling (probability); Petrology; Transition zone; Tectonics; Seismology; Oceanic crust; Geometry","score_opus":0.021304000915928784,"score_gpt":0.26878113902735107,"score_spread":0.24747713811142227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023593919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983369,0.00068059465,0.000050693892,0.0002902192,0.00029736414,0.00016751848,0.000008260706,0.00000387881,0.00016458098],"genre_scores_gemma":[0.99887586,0.00033223568,0.00022868658,0.000011737238,0.00024942777,3.206662e-7,0.0000019205609,0.0000046440155,0.00029518927],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99843705,0.00035215562,0.000250114,0.00014283968,0.00060656824,0.00021126207],"domain_scores_gemma":[0.9988766,0.0004788372,0.000114978924,0.00010839985,0.00031088525,0.00011030465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005253414,0.00009786434,0.00022255686,0.000013358227,0.0002874268,0.000058437898,0.00015847565,0.000046897632,0.00010420661],"category_scores_gemma":[0.00028578955,0.00006127746,0.000044436594,0.00023754402,0.0001365531,0.00029873117,0.000042247528,0.0002457228,0.00002078266],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003410222,0.0005445316,0.18242694,0.001183989,0.00046831372,0.00012544081,0.0052372594,0.06252841,0.695889,0.0015713075,0.009600649,0.03701394],"study_design_scores_gemma":[0.00082713424,0.001250579,0.75772226,0.00025237026,0.000029158575,0.00005323663,0.00011599246,0.018250572,0.21830538,0.0018174122,0.0012219682,0.00015395142],"about_ca_topic_score_codex":0.00042437075,"about_ca_topic_score_gemma":0.00007681853,"teacher_disagreement_score":0.5752953,"about_ca_system_score_codex":0.0000050985,"about_ca_system_score_gemma":0.00006708353,"threshold_uncertainty_score":0.24988225},"labels":[],"label_agreement":null},{"id":"W2024295140","doi":"10.1029/2007gl029515","title":"Density structure and buoyancy of the oceanic lithosphere revisited","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"European Social Fund","keywords":"Geology; Mantle (geology); Lithosphere; Geophysics; Subduction; Buoyancy; Thermal; Adiabatic process; Oceanic crust; Layering; Density contrast; Crust; Compressibility; Tectonics; Seismology; Thermodynamics; Physics","score_opus":0.015404382521860837,"score_gpt":0.26230391350980337,"score_spread":0.24689953098794254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024295140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982309,0.00012290811,0.000022522043,0.00074128836,0.00015370792,0.00021192884,0.00007531101,0.000011990987,0.00042946043],"genre_scores_gemma":[0.99913836,0.00001433439,0.00015457318,0.0002762753,0.00029917603,2.2564508e-7,0.0000144614505,0.000004140376,0.00009844842],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99819475,0.00019895645,0.00018409124,0.00026717864,0.00065919786,0.00049583346],"domain_scores_gemma":[0.9989661,0.00038500185,0.000059014517,0.00034569055,0.00010414408,0.00014003925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066816935,0.0001124621,0.00020374829,0.000034719826,0.00022945047,0.000060262904,0.00033432402,0.000057214507,0.00029429965],"category_scores_gemma":[0.00014784606,0.00006978061,0.000059134505,0.00041571827,0.000360888,0.000101419864,0.0000867856,0.00032519325,0.00004079344],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003679417,0.00006430071,0.24377601,0.00036323981,0.00011718005,0.000073764095,0.00071178126,0.00006095323,0.7160914,0.0055195503,0.011395637,0.021458263],"study_design_scores_gemma":[0.00014028631,0.000051963365,0.9795893,0.000033854383,0.000008980409,0.0000022889355,0.000023667213,0.00005508625,0.015962759,0.002587153,0.001452694,0.00009198202],"about_ca_topic_score_codex":0.0019414354,"about_ca_topic_score_gemma":0.00018214401,"teacher_disagreement_score":0.73581326,"about_ca_system_score_codex":0.0000037186344,"about_ca_system_score_gemma":0.000028702454,"threshold_uncertainty_score":0.32223746},"labels":[],"label_agreement":null},{"id":"W2024405321","doi":"10.1063/1.2772427","title":"High-pressure phase transition observed in barium hydride","year":2007,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Steacie Institute for Molecular Sciences; University of Ottawa","funders":"","keywords":"Bulk modulus; Materials science; Phase transition; Raman spectroscopy; Hydride; Barium; Ionic bonding; Phase (matter); Isothermal process; Diffraction; Crystallography; X-ray crystallography; Metal; Thermodynamics; Chemistry; Ion; Metallurgy","score_opus":0.014677319181883228,"score_gpt":0.22246815306723255,"score_spread":0.20779083388534933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024405321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994868,0.00007668695,0.0027278482,0.00006402089,0.00062887004,0.00012045133,0.00006495236,0.000010528819,0.0014386802],"genre_scores_gemma":[0.997472,0.000020354162,0.001196315,0.00015746198,0.0010892911,2.8458632e-7,0.000044927798,0.000006147037,0.0000132390915],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99872315,0.000025971955,0.00049912976,0.0001323455,0.0003371606,0.00028224217],"domain_scores_gemma":[0.9992888,0.00009007753,0.0002987417,0.00013207506,0.000064802654,0.00012550698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066532043,0.00014587904,0.00035247905,0.000065367785,0.000054162563,0.000049763254,0.00021090009,0.00007546137,0.00024317676],"category_scores_gemma":[0.0000047924195,0.00012139039,0.00008474773,0.00021530701,0.00003545247,0.0002494159,0.0000056930626,0.00022320056,0.000034764103],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003780767,0.0008250816,0.0010931212,0.00018406897,0.0002832805,0.00030531627,0.002716505,0.6648777,0.27127078,0.0064580142,0.001814042,0.046391323],"study_design_scores_gemma":[0.026025523,0.0022236267,0.18609796,0.00032076795,0.00090284116,0.00007069758,0.0011185056,0.027585566,0.54771256,0.15155095,0.054123748,0.0022672527],"about_ca_topic_score_codex":0.00024325676,"about_ca_topic_score_gemma":0.00015341968,"teacher_disagreement_score":0.63729215,"about_ca_system_score_codex":0.000004068444,"about_ca_system_score_gemma":0.00004428562,"threshold_uncertainty_score":0.49501565},"labels":[],"label_agreement":null},{"id":"W2024683579","doi":"10.1016/j.ssnmr.2005.09.010","title":"Stress, strain, and NMR","year":2005,"lang":"en","type":"article","venue":"Solid State Nuclear Magnetic Resonance","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Observable; Stress (linguistics); Electric field gradient; Cauchy stress tensor; Tensor (intrinsic definition); Materials science; Density functional theory; Nuclear magnetic resonance; Electromagnetic shielding; Computational chemistry; Condensed matter physics; Molecular physics; Chemistry; Physics; Quadrupole; Classical mechanics; Composite material; Atomic physics; Mathematics; Quantum mechanics; Geometry","score_opus":0.006096845414132943,"score_gpt":0.19605730664746202,"score_spread":0.18996046123332908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024683579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97963345,0.0058935015,0.0000033606073,0.00062916084,0.0001683191,0.00018036392,0.0013958134,0.00007372129,0.012022315],"genre_scores_gemma":[0.9943089,0.0017885405,0.001355768,0.0004302163,0.00022567491,8.504683e-7,0.000035417816,0.000011008385,0.001843647],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99890274,0.000046749778,0.00019931715,0.00029056353,0.000196592,0.00036405047],"domain_scores_gemma":[0.9995452,0.000032789027,0.00005109442,0.0002058244,0.000028100501,0.00013700094],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001233612,0.00014786379,0.00018445431,0.0000274668,0.00013889562,0.0001413188,0.00017472624,0.00004326772,0.004512216],"category_scores_gemma":[0.000013264987,0.00012865492,0.000026792148,0.000075089105,0.00013042672,0.00017341012,0.000023835619,0.00008802108,0.0007230515],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006818903,0.000026248083,0.004705785,0.000038720595,0.0000070903184,0.0000281168,0.0008514037,0.0007451835,0.0010937466,0.00059212727,0.004200524,0.9876429],"study_design_scores_gemma":[0.00029809444,0.0001707834,0.45278227,0.000021694925,0.000007488066,0.0000064752817,0.000047449426,0.0035446107,0.00008917408,0.0012706424,0.5415563,0.00020505337],"about_ca_topic_score_codex":0.00032549378,"about_ca_topic_score_gemma":0.00053858705,"teacher_disagreement_score":0.9874378,"about_ca_system_score_codex":0.0000017379305,"about_ca_system_score_gemma":0.000017693657,"threshold_uncertainty_score":0.9963978},"labels":[],"label_agreement":null},{"id":"W2024883634","doi":"10.1029/2001gl013567","title":"Evolution of subducting mantle lithosphere at a continental plate boundary","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Lithosphere; Mantle (geology); Convergent boundary; Collision zone; Plate tectonics; Geophysics; Crustal recycling; Mantle convection; Mantle wedge; Continental crust; Seismology; Oceanic crust; Tectonics","score_opus":0.023973757964524157,"score_gpt":0.2710516885031785,"score_spread":0.24707793053865434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024883634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995224,0.00017962909,0.000040861694,0.00086170057,0.00031825402,0.00020832717,0.000081466635,0.00003137569,0.0030544142],"genre_scores_gemma":[0.9980149,0.000024267105,0.0001721479,0.00006351745,0.0005223233,0.0000031992902,0.00007184852,0.000006949649,0.0011208144],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9976985,0.00022058659,0.00024691742,0.0003456876,0.0007881814,0.000700164],"domain_scores_gemma":[0.9991152,0.00027465308,0.000077302546,0.00027027735,0.00009459953,0.000167951],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000554781,0.00013804912,0.00025543696,0.00007064737,0.00034497742,0.000083102415,0.00029872602,0.000055217115,0.0012936742],"category_scores_gemma":[0.0000818288,0.00011752892,0.00009576649,0.00037408303,0.00036487437,0.00024327383,0.00008684416,0.00024213165,0.0010238313],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010935039,0.00018221392,0.16466092,0.00018156246,0.000116755466,0.000305567,0.00061724475,0.00079421274,0.8007215,0.0013279545,0.022418546,0.00758001],"study_design_scores_gemma":[0.0011777633,0.0004889114,0.92521316,0.00012744503,0.000029325698,0.000038102655,0.0003552855,0.0032114417,0.015841225,0.0034964185,0.04948109,0.0005398613],"about_ca_topic_score_codex":0.011516854,"about_ca_topic_score_gemma":0.00053672754,"teacher_disagreement_score":0.7848803,"about_ca_system_score_codex":0.000025610292,"about_ca_system_score_gemma":0.000053242005,"threshold_uncertainty_score":0.999754},"labels":[],"label_agreement":null},{"id":"W2025843858","doi":"10.1016/j.jmr.2011.09.001","title":"High pressure magnetic resonance imaging with metallic vessels","year":2011,"lang":"en","type":"article","venue":"Journal of Magnetic Resonance","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Pressure vessel; Magnetic resonance imaging; Materials science; Nuclear magnetic resonance; Ultimate tensile strength; Nuclear magnetic resonance spectroscopy; Metal; Magnetic field; Resonance (particle physics); Porosity; High pressure; Composite material; Mechanics; Metallurgy; Radiology; Physics; Atomic physics","score_opus":0.010099932220970241,"score_gpt":0.18637050884919723,"score_spread":0.17627057662822698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025843858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7861453,0.2061437,0.000057829937,0.00025141842,0.0010858298,0.0002916455,0.00011120526,0.000032420834,0.0058805915],"genre_scores_gemma":[0.9864478,0.0013943192,0.009469402,0.0001853287,0.0004158469,0.0000021900248,0.0000037658033,0.000015994367,0.002065315],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9978475,0.00015435021,0.00060405006,0.0003002081,0.00062228565,0.0004715823],"domain_scores_gemma":[0.9986717,0.00009641712,0.00042377986,0.00036946568,0.0002316481,0.0002070074],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053362164,0.00026847151,0.0005127592,0.000105316394,0.00011856526,0.000108098386,0.0006362461,0.000062585874,0.0048072548],"category_scores_gemma":[0.000044783068,0.00018587556,0.000097178905,0.00025735627,0.0001980794,0.00045799694,0.00002522486,0.0002469864,0.00010275386],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028600697,0.000359254,0.19612162,0.00026382614,0.0000946092,0.0022163528,0.0024297344,0.0004766938,0.0042186836,0.00326628,0.010396018,0.77729684],"study_design_scores_gemma":[0.00093474647,0.0011323337,0.7563188,0.0001648089,0.00014410725,0.00024584448,0.000040320563,0.00015931008,0.0010347809,0.0023035423,0.23722856,0.00029286163],"about_ca_topic_score_codex":0.00080219476,"about_ca_topic_score_gemma":0.00008260214,"teacher_disagreement_score":0.777004,"about_ca_system_score_codex":0.0000030747262,"about_ca_system_score_gemma":0.000109284134,"threshold_uncertainty_score":0.9961025},"labels":[],"label_agreement":null},{"id":"W2026434180","doi":"10.1107/s0108767302087214","title":"Structure of HDA under pressure by<i>in-situ</i>neutron diffraction to 2.5 GPa","year":2002,"lang":"en","type":"article","venue":"Acta Crystallographica Section A Foundations of Crystallography","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; University of Guelph","funders":"","keywords":"Crystallography; Materials science; Mathematics; Chemistry","score_opus":0.008743564927371562,"score_gpt":0.21060146863600415,"score_spread":0.2018579037086326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026434180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941177,0.00023440043,0.00050360314,0.0005294745,0.0008142527,0.0006473391,0.0006277275,0.000077385674,0.0024481418],"genre_scores_gemma":[0.9985763,0.00020348582,0.00052424084,0.000109081724,0.00009463015,0.000008723256,0.0003850586,0.00001644223,0.000082046674],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99759537,0.00018340207,0.000748951,0.00052629015,0.0005141023,0.00043186537],"domain_scores_gemma":[0.99849516,0.00016112777,0.0004441357,0.0005104913,0.00021073536,0.00017832052],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019733867,0.00031492705,0.0005091654,0.001175448,0.0001923977,0.00009205547,0.00038259686,0.0002454787,0.0022565806],"category_scores_gemma":[0.000035733843,0.00031155848,0.00025736573,0.002217922,0.00024129273,0.00063288875,0.000031011194,0.00025272343,0.0000013166975],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010121163,0.0002443266,0.029145742,0.00010666024,0.00020044963,9.535837e-7,0.00028162944,0.0038340134,0.9631299,0.000271339,0.0022158888,0.00046792897],"study_design_scores_gemma":[0.0013094904,0.0008144458,0.81988084,0.00009563085,0.00024465175,0.000014673757,0.00035380313,0.00038097095,0.0019253045,0.0048184195,0.16941527,0.0007464733],"about_ca_topic_score_codex":0.0018326377,"about_ca_topic_score_gemma":0.0048441095,"teacher_disagreement_score":0.9612045,"about_ca_system_score_codex":0.000005690588,"about_ca_system_score_gemma":0.000022603943,"threshold_uncertainty_score":0.99993366},"labels":[],"label_agreement":null},{"id":"W2026812879","doi":"10.1103/physreve.81.036107","title":"Crystallization of classical multicomponent plasmas","year":2010,"lang":"en","type":"article","venue":"Physical Review E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Crystallization; Plasma; Materials science; Physics; Thermodynamics; Nuclear physics","score_opus":0.01408545914909262,"score_gpt":0.25684486047487715,"score_spread":0.24275940132578452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026812879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99505997,0.00058743794,0.00008664616,0.00030988306,0.00037031667,0.00022182337,0.00006123466,0.000022743543,0.003279952],"genre_scores_gemma":[0.9986007,0.0005978313,0.0003603812,0.00010786061,0.00023136157,0.0000017447353,0.00006905317,0.000002569684,0.000028461242],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99931395,0.0000421737,0.00018112108,0.00013991064,0.00019375693,0.00012910567],"domain_scores_gemma":[0.99951833,0.00009934027,0.00008889183,0.00017416605,0.000037979615,0.00008130637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011576118,0.00008670261,0.00027589584,0.000010917867,0.00003024838,0.000012148696,0.00013621114,0.000019883402,0.00085032365],"category_scores_gemma":[0.000066314446,0.000060351365,0.0000786964,0.00008263351,0.000057046203,0.00007713745,0.000011471747,0.00008954547,0.0002658119],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005105521,0.0005507891,0.0063928966,0.0033105116,0.0000730932,0.000008366592,0.00017204415,0.00033837123,0.84605235,0.05085604,0.0031385322,0.08905598],"study_design_scores_gemma":[0.0010151471,0.0004539794,0.26920378,0.0016027334,0.0004026385,0.000009718227,0.000008629006,0.034240656,0.063908525,0.025006926,0.6030947,0.0010525676],"about_ca_topic_score_codex":0.0001056897,"about_ca_topic_score_gemma":0.000067559806,"teacher_disagreement_score":0.7821438,"about_ca_system_score_codex":4.7065163e-7,"about_ca_system_score_gemma":0.000015853178,"threshold_uncertainty_score":0.93104476},"labels":[],"label_agreement":null},{"id":"W2027274494","doi":"10.1038/nature13391","title":"Possible control of subduction zone slow-earthquake periodicity by silica enrichment","year":2014,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":208,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Paleontology; Tectonics","score_opus":0.002863164169108051,"score_gpt":0.18866198878411738,"score_spread":0.18579882461500932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027274494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950475,0.0008499766,0.00024110387,0.0005398556,0.0007958117,0.00014969615,0.00028396366,0.00002972551,0.0020623647],"genre_scores_gemma":[0.998556,0.000024698755,0.00012206996,0.00042036283,0.0002664417,0.0000010739684,0.00012753911,0.0000027951912,0.000478987],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990896,0.000083568615,0.00016443469,0.00020005884,0.00026527382,0.00019707784],"domain_scores_gemma":[0.9995216,0.000055513065,0.00009712416,0.0001852054,0.000061388964,0.00007914345],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027454252,0.00011020029,0.00022355854,0.000029969475,0.00009668675,0.000040520685,0.00014275538,0.0004827639,0.0009275187],"category_scores_gemma":[0.00003306241,0.000084938874,0.000051743795,0.000099744255,0.00004000551,0.00010158279,0.0000060841303,0.00044991347,0.000089175854],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009369206,0.0003971115,0.21375717,0.00039245578,0.0002958965,0.000010252589,0.0010918461,0.0033474548,0.54192966,0.0042321407,0.1274918,0.10611727],"study_design_scores_gemma":[0.0015466989,0.0005416587,0.5949786,0.000029419181,0.00007588712,0.0000063408274,0.000048060876,0.0020050155,0.03381713,0.000994399,0.36556306,0.0003937891],"about_ca_topic_score_codex":0.00075571256,"about_ca_topic_score_gemma":0.00014638793,"teacher_disagreement_score":0.50811255,"about_ca_system_score_codex":0.0000016739484,"about_ca_system_score_gemma":0.000019161487,"threshold_uncertainty_score":0.99998575},"labels":[],"label_agreement":null},{"id":"W2027537911","doi":"10.1029/1999jb900387","title":"Mantle variation within the Canadian Shield: Travel times from the portable broadband Archean‐Proterozoic Transect 1989","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Mantle (geology); Proterozoic; Archean; Transition zone; Craton; Crust; Seismology; Geophysics; Tectonics; Paleontology","score_opus":0.024214023866403034,"score_gpt":0.25752968909503515,"score_spread":0.23331566522863212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027537911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886883,0.0004689758,0.000026684062,0.00391574,0.00025922022,0.0003135987,0.00015218546,0.0000060676316,0.006169212],"genre_scores_gemma":[0.9960972,0.00008966308,0.00026907393,0.0002652743,0.0012050685,0.000002672393,0.000021318085,0.000008696048,0.002041048],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99697053,0.0006605196,0.00043100055,0.00021374632,0.0011309712,0.0005932475],"domain_scores_gemma":[0.9980076,0.0010059259,0.00013924524,0.00031488933,0.00018172813,0.000350608],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018528983,0.00016418574,0.00029924724,0.00001650045,0.00081753626,0.00048325848,0.00082593714,0.000093645336,0.011711591],"category_scores_gemma":[0.00013772579,0.00008259854,0.00014300336,0.00034249632,0.00028909548,0.00030655615,0.00001111123,0.0007793033,0.00041779084],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009865172,0.0014108092,0.06820168,0.00027764807,0.004061363,0.0018885258,0.05424344,0.04734292,0.038505245,0.016017731,0.22177221,0.53641325],"study_design_scores_gemma":[0.000709108,0.0007366872,0.9146275,0.000099475925,0.00007452685,0.000022062803,0.00048171615,0.0037070704,0.0016227124,0.053654846,0.024007935,0.00025635614],"about_ca_topic_score_codex":0.6999647,"about_ca_topic_score_gemma":0.41249526,"teacher_disagreement_score":0.84642583,"about_ca_system_score_codex":0.000017888324,"about_ca_system_score_gemma":0.000750854,"threshold_uncertainty_score":0.98919183},"labels":[],"label_agreement":null},{"id":"W2028201395","doi":"10.1029/2010jb007631","title":"GyPSuM: A joint tomographic model of mantle density and seismic wave speeds","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":541,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Geophysics; Seismic wave; Seismic tomography; Core–mantle boundary; Tectonics; Seismology; Amplitude; Geodynamics; Physics","score_opus":0.04075578214290497,"score_gpt":0.272984101326426,"score_spread":0.232228319183521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028201395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981824,0.00012899509,0.00011792705,0.00027485058,0.00023594746,0.000116398485,0.00003018225,0.0000058797436,0.00090739486],"genre_scores_gemma":[0.99660873,0.00014467178,0.002556894,0.000026279762,0.00039368682,3.6938516e-7,0.0000027878739,0.00000645708,0.00026010082],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978409,0.0001562213,0.00042633235,0.00019305357,0.00094512675,0.0004383764],"domain_scores_gemma":[0.9983765,0.00030576505,0.00021789226,0.0002405878,0.0005139125,0.00034533988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012405721,0.00014324246,0.00045217964,0.000046469537,0.00014750347,0.000101021615,0.00027421812,0.00009757355,0.00040739204],"category_scores_gemma":[0.0002140028,0.00010103589,0.00015439306,0.00027449927,0.00044537257,0.00027564508,0.000071980634,0.0007141036,0.000029147943],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013000339,0.00059025735,0.044605248,0.0003890679,0.00041815598,0.0003073503,0.0010262093,0.003940456,0.8906499,0.0056916047,0.005528791,0.045552928],"study_design_scores_gemma":[0.0013039928,0.0019059718,0.6250484,0.00015218464,0.00009449985,0.00010040203,0.00026552795,0.14185175,0.063786976,0.16369788,0.0013566914,0.00043570664],"about_ca_topic_score_codex":0.0023640296,"about_ca_topic_score_gemma":0.00048908824,"teacher_disagreement_score":0.82686293,"about_ca_system_score_codex":0.0000026467903,"about_ca_system_score_gemma":0.00017933559,"threshold_uncertainty_score":0.44606572},"labels":[],"label_agreement":null},{"id":"W2028415353","doi":"10.1007/s00269-003-0303-9","title":"Compression mechanisms of coesite","year":2003,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Eidgenössische Technische Hochschule Zürich; National Science Foundation","keywords":"Coesite; Tetrahedron; Chemistry; Anisotropy; Rotation (mathematics); Compression (physics); Crystallography; Deformation (meteorology); Diffraction; Crystal structure; Mineralogy; Thermodynamics; Geometry; Geology; Physics; Composite material; Optics; Materials science; Tectonics","score_opus":0.00942494930246012,"score_gpt":0.19547564305493204,"score_spread":0.1860506937524719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028415353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876297,0.00017495992,0.00025794064,0.000010971429,0.00005448195,0.00003865832,0.000120750075,0.0000049300243,0.011707622],"genre_scores_gemma":[0.998909,0.000029380946,0.0006066742,0.000009949931,0.000037092173,3.3562148e-7,0.000039641334,0.0000019917552,0.0003659564],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99951345,0.000014941595,0.00014971681,0.0001108008,0.00011297852,0.00009808583],"domain_scores_gemma":[0.9996597,0.00003089949,0.00011536811,0.0001128031,0.00003514173,0.000046092075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007933826,0.000079842706,0.00020025233,0.000004151507,0.000027289896,0.000008208014,0.00006557774,0.000032197953,0.0004685495],"category_scores_gemma":[0.0000067869505,0.00006470948,0.000033138007,0.00004056151,0.000046811834,0.00004127272,0.000007019615,0.000026358146,0.0000025912518],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007417202,0.000020787387,0.0008189798,0.00012953002,0.000012875287,4.9058815e-7,0.00003143883,0.00015342854,0.99639213,0.0016956181,0.00020300015,0.0005342976],"study_design_scores_gemma":[0.00017849635,0.000020638321,0.0010308593,0.000029068553,0.000014775362,0.000001080348,0.000016714384,0.00016996577,0.9747989,0.022754783,0.00090323144,0.000081455415],"about_ca_topic_score_codex":0.00014102882,"about_ca_topic_score_gemma":0.0000018278369,"teacher_disagreement_score":0.021593206,"about_ca_system_score_codex":2.750096e-7,"about_ca_system_score_gemma":0.000010914764,"threshold_uncertainty_score":0.51302886},"labels":[],"label_agreement":null},{"id":"W2028635687","doi":"10.1029/2003gl017754","title":"The influence of phase boundary deflection on velocity anomalies of stagnant slabs in the transition zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Slab; Transition zone; Slab window; Discontinuity (linguistics); Geophysics; Deflection (physics); Mantle wedge; Mantle (geology); Seismic tomography; Seismology; Mantle convection; Mechanics; Physics; Tectonics; Oceanic crust; Optics","score_opus":0.02662603596190203,"score_gpt":0.299776902851212,"score_spread":0.27315086688930995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028635687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99797976,0.000043812637,0.000032426793,0.0012340631,0.00007382784,0.00026692875,0.000059128255,0.0000045490497,0.00030552442],"genre_scores_gemma":[0.9996577,0.000042651434,0.00002811381,0.00018147862,0.000054541313,0.000007038892,0.000013524027,0.0000024467338,0.000012493206],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9976656,0.0008244962,0.00022933957,0.00017636898,0.0007409175,0.00036326595],"domain_scores_gemma":[0.99863434,0.0009337715,0.00006269456,0.00024784837,0.00007975274,0.00004156622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015168614,0.00008932637,0.00015921914,0.000069839196,0.0002789286,0.00006442735,0.00027573548,0.00003176233,0.000033564105],"category_scores_gemma":[0.00014030316,0.00005051146,0.000052439227,0.0004265468,0.0005214268,0.00013917219,0.000007535399,0.00024766332,0.00002865904],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018244035,0.0006148489,0.0018959927,0.00024804517,0.00008413707,0.000055593766,0.006087378,0.012104813,0.9406972,0.012059817,0.0017258327,0.022601955],"study_design_scores_gemma":[0.0029435246,0.0039131576,0.82336235,0.00022491906,0.00003670568,0.0000063691236,0.0014730019,0.0016062852,0.12634124,0.019364018,0.020237178,0.0004912687],"about_ca_topic_score_codex":0.004735443,"about_ca_topic_score_gemma":0.00053448696,"teacher_disagreement_score":0.8214663,"about_ca_system_score_codex":0.000005782742,"about_ca_system_score_gemma":0.00007124306,"threshold_uncertainty_score":0.7158605},"labels":[],"label_agreement":null},{"id":"W2028757731","doi":"10.1007/s00269-014-0704-y","title":"Equation of state of a synthetic ulvöspinel, (Fe1.94Ti0.03)Ti1.00O4.00, at ambient temperature","year":2014,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Spinel; Bulk modulus; Chemistry; Synchrotron; Equation of state; Magnetite; Diffraction; Isothermal process; X-ray crystallography; Yield (engineering); Analytical Chemistry (journal); Thermodynamics; Crystallography; Mineralogy; Materials science; Metallurgy; Optics; Physics","score_opus":0.008763291339571657,"score_gpt":0.19214895798634674,"score_spread":0.18338566664677508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028757731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978831,0.00019390113,0.000017587949,0.000055028286,0.000066475994,0.00007605821,0.0003337372,0.0000063881853,0.0013677673],"genre_scores_gemma":[0.99904424,0.00008326548,0.00010449598,0.000012847055,0.00010773231,0.0000012260207,0.00014278007,0.0000046847426,0.00049874745],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990772,0.000027397786,0.00031730576,0.0001976331,0.0002251819,0.00015527144],"domain_scores_gemma":[0.99925405,0.00006570144,0.00029539835,0.00021922936,0.00009919959,0.00006640701],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016893365,0.00014127775,0.00036528,0.000011262134,0.00003748152,0.0000136604085,0.00012396292,0.000047647685,0.00022542555],"category_scores_gemma":[0.000024019653,0.00011630939,0.000064536674,0.00007897056,0.000111292546,0.000062165935,0.000025739675,0.000045177123,0.0000045463967],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033886063,0.00003957153,0.0010929034,0.00048462878,0.000029110563,3.0082504e-7,0.00015465445,0.0012296219,0.9952809,0.000052881802,0.0003112237,0.0012902999],"study_design_scores_gemma":[0.00027817884,0.00007608041,0.0040443093,0.00009949422,0.000032166663,0.0000010707424,0.000012984841,0.0011878678,0.99078834,0.0027075377,0.00063558883,0.00013637896],"about_ca_topic_score_codex":0.00031982997,"about_ca_topic_score_gemma":0.000009832369,"teacher_disagreement_score":0.0044925753,"about_ca_system_score_codex":0.0000015341601,"about_ca_system_score_gemma":0.000018751683,"threshold_uncertainty_score":0.47429594},"labels":[],"label_agreement":null},{"id":"W2028767031","doi":"10.1002/2013gl059116","title":"Seismic anisotropy of the Archean crust in the Minnesota River Valley, Superior Province","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Rhodes University; University of Minnesota; National Science Foundation","keywords":"Geology; Crust; Layering; Seismic anisotropy; Anisotropy; Gneiss; Mantle (geology); Archean; Lithosphere; Geophysics; Shear (geology); Seismology; Shear wave splitting; Shear zone; Petrology; Geochemistry; Metamorphic rock; Tectonics","score_opus":0.02319170673660253,"score_gpt":0.25793319657962865,"score_spread":0.23474148984302612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028767031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889757,0.00001646717,0.00003302515,0.009643514,0.00015909463,0.0004219953,0.000045677993,0.000009108865,0.00069541985],"genre_scores_gemma":[0.99847645,0.000009547792,0.000090876834,0.0009153702,0.0003598745,0.000007387638,0.000013496088,0.000005770272,0.00012121763],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9966869,0.001134727,0.00022376263,0.0003174362,0.0009909675,0.0006462115],"domain_scores_gemma":[0.9984208,0.00080307416,0.00005245699,0.00058279687,0.000057425827,0.00008347884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001265857,0.00014054347,0.0002280629,0.00006297992,0.00024212911,0.00009629961,0.0011481697,0.000046730227,0.00013109349],"category_scores_gemma":[0.000190604,0.00007485829,0.000103692495,0.00040381105,0.0008067698,0.00015483219,0.00010238186,0.00042642275,0.0002588577],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001195547,0.0011309856,0.17833512,0.0008905413,0.00021291246,0.00015312515,0.015342967,0.015061988,0.6351646,0.029542806,0.07207076,0.05089866],"study_design_scores_gemma":[0.00046043703,0.00024271665,0.96040154,0.0000494761,0.000011199987,0.0000026157104,0.00014914459,0.0067401174,0.0026891523,0.0046824506,0.024370622,0.00020056067],"about_ca_topic_score_codex":0.013454719,"about_ca_topic_score_gemma":0.000559985,"teacher_disagreement_score":0.7820664,"about_ca_system_score_codex":0.000006503366,"about_ca_system_score_gemma":0.0000876138,"threshold_uncertainty_score":0.99311477},"labels":[],"label_agreement":null},{"id":"W2029518893","doi":"10.1103/physrevb.67.174110","title":"Brillouin and Raman spectroscopy of the ferroelastic rutile-to-<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">CaCl</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math>transition in<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">SnO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math>at high pressure","year":2003,"lang":"lv","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Waterloo; Deutsche Forschungsgemeinschaft","keywords":"Raman spectroscopy; Brillouin zone; Rutile; Brillouin Spectroscopy; Phase transition; Spectroscopy; Brillouin scattering; Materials science; Raman scattering; Phase (matter); Order (exchange); Physics; Analytical Chemistry (journal); Nuclear magnetic resonance; Condensed matter physics; Optics; Chemistry; Laser","score_opus":0.012675110543165691,"score_gpt":0.23494907899646894,"score_spread":0.22227396845330324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029518893","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49055147,0.0036657336,0.00082992367,0.0017969566,0.005118938,0.00013774558,0.0018940403,0.00034681382,0.49565837],"genre_scores_gemma":[0.971185,0.005521687,0.0026038408,0.0060243425,0.004576426,0.0024735301,0.004903,0.0017429442,0.0009691748],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9768655,0.0018568783,0.0048202747,0.0044722366,0.0059365537,0.006048565],"domain_scores_gemma":[0.9819105,0.0039344407,0.0052055516,0.0055328184,0.00044722424,0.002969464],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"category_scores_codex":[0.0047967834,0.00248801,0.0011572692,0.0011384281,0.0032862416,0.0036859096,0.005160871,0.0045154965,0.83453125],"category_scores_gemma":[0.0030014045,0.0045622285,0.0043698447,0.0030101712,0.0041484646,0.003831789,0.0037412276,0.0039907824,0.0077453917],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0037662892,0.00088135333,0.000047493548,0.00656553,0.003580077,0.0033008417,0.0030747303,0.0031503327,0.0130503625,0.44920817,0.51214147,0.0012333506],"study_design_scores_gemma":[0.003956161,0.0031971938,0.00073475426,0.0053339237,0.005501016,0.0033879462,0.0015306125,0.0473701,0.9121466,0.00018903315,0.012502985,0.0041496293],"about_ca_topic_score_codex":0.0048780804,"about_ca_topic_score_gemma":0.0045423633,"teacher_disagreement_score":0.8990963,"about_ca_system_score_codex":0.000029836603,"about_ca_system_score_gemma":0.0032738617,"threshold_uncertainty_score":0.9987856},"labels":[],"label_agreement":null},{"id":"W2029630573","doi":"10.1007/s00024-006-0111-5","title":"Elasticity, Yielding and Episodicity in Simple Models of Mantle Convection","year":2006,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"State Government of Victoria; Australian Government; Ontario Ministry of Natural Resources and Forestry","keywords":"Plasticity; Elasticity (physics); Mantle convection; Creep; Constitutive equation; Geology; Finite element method; Linear elasticity; Convection; Mantle (geology); Mechanics; Statistical physics; Computer science; Subduction; Applied mathematics; Econometrics; Mathematics; Physics; Geophysics; Thermodynamics; Seismology","score_opus":0.007973143194061217,"score_gpt":0.1792393645120994,"score_spread":0.17126622131803818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029630573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938045,0.00008316953,0.0005316687,0.000019020905,0.000052742776,0.000118016425,0.0000574293,0.0000121883795,0.005321243],"genre_scores_gemma":[0.99965024,0.00003438442,0.000106471096,0.0000254808,0.00011278936,0.0000017001103,0.00004681769,0.0000027720107,0.0000193696],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9994005,0.000011972038,0.00015784209,0.00017178075,0.00009646329,0.0001614593],"domain_scores_gemma":[0.9997597,0.000061737286,0.00006414553,0.00006924797,0.000012645163,0.00003254654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008761556,0.00009678216,0.000200431,0.000031520245,0.00006159174,0.00003117295,0.00004492529,0.000049847666,0.00003464736],"category_scores_gemma":[0.0000015708337,0.00008595102,0.000014755898,0.00009253544,0.000056505538,0.000102163605,0.000017566123,0.00005916283,0.0000055589117],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049526314,0.00041573946,0.2174925,0.0011545868,0.00010928213,0.000020534137,0.0019572203,0.13861345,0.13712247,0.4272669,0.0009691499,0.0743829],"study_design_scores_gemma":[0.0006477843,0.00008345924,0.42898557,0.000024067354,0.000039930277,0.000002441862,0.00008475354,0.012933441,0.013860249,0.5425816,0.00044607715,0.00031061683],"about_ca_topic_score_codex":0.004283566,"about_ca_topic_score_gemma":0.0007667025,"teacher_disagreement_score":0.21149306,"about_ca_system_score_codex":8.736011e-7,"about_ca_system_score_gemma":0.000009260298,"threshold_uncertainty_score":0.64754987},"labels":[],"label_agreement":null},{"id":"W2030599528","doi":"10.1063/1.4794360","title":"Temperature and pressure dependent geometry optimization and elastic constant calculations for arbitrary symmetry crystals: Applications to MgSiO3 perovskites","year":2013,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hatch (Canada); Wilfrid Laurier University","funders":"National Natural Science Foundation of China","keywords":"Orthorhombic crystal system; Lattice constant; Lattice energy; Symmetry (geometry); Lattice (music); Work (physics); Crystal (programming language); Energy minimization; Thermodynamics; Materials science; Gibbs free energy; Crystal structure; Condensed matter physics; Chemistry; Physics; Geometry; Computational chemistry; Diffraction; Crystallography; Mathematics; Quantum mechanics","score_opus":0.007235700385172962,"score_gpt":0.2089997140774703,"score_spread":0.20176401369229735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030599528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93218684,0.0013331303,0.06222546,0.00020351274,0.00021238833,0.001750208,0.0006853425,0.000025876207,0.0013772476],"genre_scores_gemma":[0.9783071,0.00009886119,0.020970117,0.00013847325,0.00037557594,0.000018864008,0.000053940563,0.000007651952,0.000029360739],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991736,0.000015481744,0.00029094415,0.00016789329,0.00018620779,0.00016589904],"domain_scores_gemma":[0.99915105,0.00020194566,0.0001994692,0.00010756132,0.00016182761,0.0001781568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013068793,0.00013665936,0.0002535851,0.000071394854,0.00018390577,0.00020309722,0.00010147212,0.00006973653,0.00008754],"category_scores_gemma":[0.000013502479,0.00010740679,0.000037113114,0.00016178384,0.00004676363,0.0002359866,0.000017458266,0.000111989044,0.000005956388],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001558079,0.00016445863,0.0023377126,0.0003969098,0.00035659506,0.0000017580827,0.0004814776,0.8846716,0.08417247,0.015331349,0.0020211288,0.0099087],"study_design_scores_gemma":[0.013302614,0.004136385,0.18565476,0.0009403685,0.004983308,0.000362871,0.0063295127,0.35118794,0.0621231,0.2989937,0.06591851,0.006066911],"about_ca_topic_score_codex":0.000026342559,"about_ca_topic_score_gemma":0.0000042043093,"teacher_disagreement_score":0.5334837,"about_ca_system_score_codex":0.0000024492515,"about_ca_system_score_gemma":0.000044956632,"threshold_uncertainty_score":0.4379922},"labels":[],"label_agreement":null},{"id":"W2031147584","doi":"10.1103/physrevb.73.212301","title":"Dynamics of elemental lithium at megabar pressures","year":2006,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences; University of Saskatchewan","funders":"","keywords":"Orthorhombic crystal system; Lithium (medication); Physics; Condensed matter physics; Raman spectroscopy; Materials science; Atomic physics; Crystal structure; Crystallography; Chemistry; Quantum mechanics","score_opus":0.006868706092278793,"score_gpt":0.23605755600253808,"score_spread":0.22918884991025928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031147584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9490677,0.017198931,0.00002288931,0.00051389815,0.00027870308,0.00046386302,0.0008664076,0.000040346138,0.03154727],"genre_scores_gemma":[0.99753964,0.0012012582,0.00009202499,0.00010752398,0.00026208127,0.0000025320094,0.00038369902,0.000003689498,0.0004075783],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99909174,0.00006152596,0.00023541326,0.0001739543,0.00024672336,0.00019063438],"domain_scores_gemma":[0.99953866,0.00006710991,0.00012298775,0.00019024765,0.000030165338,0.000050855022],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012662848,0.00011819253,0.000351921,0.000010480842,0.00005009389,0.000013227304,0.00017001646,0.000016170918,0.001097998],"category_scores_gemma":[0.000013132175,0.00008583029,0.00011415714,0.00009225132,0.000056837023,0.00008661207,0.000027630795,0.000042903815,0.00026262243],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003747804,0.0025795314,0.23498614,0.030765412,0.0007375904,0.00009284252,0.0003912944,0.003951075,0.10461989,0.30506897,0.19697401,0.11945846],"study_design_scores_gemma":[0.0009781272,0.00064512476,0.52218264,0.0021793623,0.0008522725,0.0000123058035,0.000014677679,0.01347341,0.031126948,0.07703472,0.35008937,0.0014110234],"about_ca_topic_score_codex":0.001592845,"about_ca_topic_score_gemma":0.00058535615,"teacher_disagreement_score":0.2871965,"about_ca_system_score_codex":0.0000031424356,"about_ca_system_score_gemma":0.000012155079,"threshold_uncertainty_score":0.9998151},"labels":[],"label_agreement":null},{"id":"W2031494751","doi":"10.1063/1.4915524","title":"Thermal transport properties of halide solid solutions: Experiments vs equilibrium molecular dynamics","year":2015,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Thermal conductivity; Thermal diffusivity; Thermodynamics; Phonon; Solid solution; Halide; Thermal; Work (physics); Chemistry; Materials science; Physics; Condensed matter physics","score_opus":0.03278819152727269,"score_gpt":0.23098295383466438,"score_spread":0.1981947623073917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031494751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99807304,0.0005435182,0.00036197665,0.00016267707,0.0002272486,0.000068283625,0.000028488414,0.0000060372386,0.0005287372],"genre_scores_gemma":[0.99948835,0.000009177368,0.0001615696,0.00005749428,0.00024976226,2.6779563e-7,0.000011108776,0.0000054870716,0.000016773707],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99891824,0.00006909566,0.0003546818,0.00006342855,0.00039485257,0.00019968947],"domain_scores_gemma":[0.99929357,0.000024444058,0.0002627949,0.00015516732,0.0001581071,0.00010592153],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003639394,0.0001118013,0.00027356594,0.000012519795,0.000024580846,0.000014287764,0.00035462552,0.000040895015,0.000027037095],"category_scores_gemma":[0.000016983286,0.0000658598,0.00009844231,0.00007309001,0.00015399286,0.00020305834,0.000018709039,0.00011937637,0.000009332428],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031654796,0.00006083002,0.00019589922,0.000022843793,0.00007295074,0.000004688592,0.00088704465,0.012854965,0.98502386,0.00012298785,0.00009466005,0.00034272007],"study_design_scores_gemma":[0.0003407836,0.00012527537,0.00014396552,0.000048956557,0.00008395079,0.000009181818,0.00012632537,0.0029577103,0.9925514,0.0034591206,0.000050983246,0.000102383645],"about_ca_topic_score_codex":0.00015416068,"about_ca_topic_score_gemma":0.0000015386602,"teacher_disagreement_score":0.009897255,"about_ca_system_score_codex":0.000007946497,"about_ca_system_score_gemma":0.00013383284,"threshold_uncertainty_score":0.2685685},"labels":[],"label_agreement":null},{"id":"W2031897474","doi":"10.1016/j.lithos.2004.04.008","title":"Inclusions in diamonds from the K14 and K10 kimberlites, Buffalo Hills, Alberta, Canada: diamond growth in a plume?","year":2004,"lang":"en","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Kimberlite; Asthenosphere; Geology; Mantle (geology); Geochemistry; Eclogite; Craton; Diamond; Coesite; Lithosphere; Mantle plume; Subduction; Paleontology; Chemistry; Tectonics","score_opus":0.004312821830476043,"score_gpt":0.1686619384795089,"score_spread":0.16434911664903284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031897474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943727,0.0010560275,0.0000021395367,0.0020204275,0.00028322206,0.00020007689,0.00052558107,0.000007993651,0.0015318197],"genre_scores_gemma":[0.9987306,0.00013243906,0.00012247212,0.0005648206,0.00013045745,0.0000049996834,0.0001948762,0.0000046469095,0.000114684975],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988964,0.000087769105,0.000236808,0.0002690798,0.00019162323,0.00031827297],"domain_scores_gemma":[0.9992604,0.00036843045,0.00005142056,0.0001922454,0.000014037844,0.00011345302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017452467,0.00014803561,0.00022107054,0.000035713092,0.0001264607,0.00006834618,0.00022946637,0.000067770765,0.00031536134],"category_scores_gemma":[0.00008122771,0.00010148589,0.00002019375,0.00020917626,0.000056805206,0.0001409023,0.000057262187,0.0001442431,0.000020375715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019185836,0.000026786198,0.9943182,0.0000101479845,0.00001078991,0.00005824607,0.0027546047,0.0001719233,0.000051944764,0.00069946644,0.0007554187,0.0011233281],"study_design_scores_gemma":[0.00043711683,0.000021092343,0.98000944,0.000041254953,0.000008137548,0.0000018385798,0.00011506714,0.00008983715,0.00012371545,0.007050022,0.011949499,0.000153],"about_ca_topic_score_codex":0.9983066,"about_ca_topic_score_gemma":0.9981017,"teacher_disagreement_score":0.014308739,"about_ca_system_score_codex":0.000015169462,"about_ca_system_score_gemma":0.00024416862,"threshold_uncertainty_score":0.41384748},"labels":[],"label_agreement":null},{"id":"W2033791808","doi":"10.1130/0091-7613(2002)030<0419:mszrtc>2.0.co;2","title":"Mantle shear zones revisited: The connection between the cratons and mantle dynamics","year":2002,"lang":"en","type":"article","venue":"Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geological survey; Geology; Columbia university; Craton; Mantle (geology); Earth science; Geophysics; Paleontology; Media studies; Sociology; Tectonics","score_opus":0.012869522888200159,"score_gpt":0.19558564173017193,"score_spread":0.18271611884197178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033791808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9830587,0.0008497957,0.00015462894,0.0052602156,0.00044025562,0.00016679846,0.000110418594,0.000028486029,0.009930705],"genre_scores_gemma":[0.99823093,0.0002301199,0.000043508175,0.00028632005,0.0002633271,0.0000013182621,0.00005474515,0.0000022438358,0.0008874809],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99936914,0.000120403914,0.00011157458,0.00014223765,0.000065904984,0.00019071567],"domain_scores_gemma":[0.99951464,0.000211147,0.000046557645,0.00018018653,0.000015930118,0.00003151637],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021065884,0.000076529555,0.00012703602,0.000018174322,0.00029443862,0.000044497778,0.0001391332,0.000058368387,0.0035473472],"category_scores_gemma":[0.000018029832,0.000040618248,0.000021303189,0.000073092815,0.0001573996,0.000052124808,0.000022906912,0.00008267156,0.00045562247],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030716375,0.000024745284,0.8741898,0.000061450126,0.00016772392,0.00002631814,0.0009158681,0.00060796173,0.00009004127,0.021417307,0.024256285,0.07821177],"study_design_scores_gemma":[0.00015579,0.00010959731,0.9038557,0.00000438259,0.000053794978,0.00003997656,0.00012904726,0.008866816,0.00003713579,0.008412747,0.07819873,0.00013629018],"about_ca_topic_score_codex":0.0014571231,"about_ca_topic_score_gemma":0.000828761,"teacher_disagreement_score":0.078075476,"about_ca_system_score_codex":9.1870714e-7,"about_ca_system_score_gemma":0.0000032922092,"threshold_uncertainty_score":0.99736357},"labels":[],"label_agreement":null},{"id":"W2033955470","doi":"10.1029/2007jb005123","title":"Near‐surface diagnostics of dripping or delaminating lithosphere","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":208,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Mantle (geology); Lithospheric flexure; Delamination (geology); Crust; Thermal subsidence; Geophysics; Asthenosphere; Petrology; Tectonics; Seismology","score_opus":0.04921053624879411,"score_gpt":0.30782857982396966,"score_spread":0.25861804357517554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033955470","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99690586,0.0010474982,0.00009000856,0.000121687975,0.00031107772,0.00013360818,0.00003041874,0.000010329102,0.0013494953],"genre_scores_gemma":[0.9879452,0.0009794147,0.009847162,0.000016800974,0.0005314212,4.548427e-7,0.000003881072,0.000010853709,0.0006648018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966221,0.0003858838,0.0006963307,0.00020774554,0.0014795033,0.00060842483],"domain_scores_gemma":[0.99472904,0.0033720864,0.00040580015,0.00025264948,0.0009211718,0.0003192374],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011228501,0.0001785187,0.00057183026,0.000011696986,0.00039224364,0.00010463479,0.00060481083,0.00009680286,0.0017072519],"category_scores_gemma":[0.002222268,0.00011954619,0.00017050412,0.00058171566,0.00051510823,0.00040048282,0.00007169722,0.0005610204,0.000120128156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0055189137,0.0022183093,0.6430086,0.0014092732,0.0013020936,0.0067503485,0.010322396,0.06148896,0.030895114,0.0025115947,0.059155688,0.17541872],"study_design_scores_gemma":[0.0017477864,0.004616964,0.9413871,0.0007934901,0.00007963366,0.00022728226,0.0014474918,0.011017538,0.01241221,0.006093286,0.01958037,0.0005968241],"about_ca_topic_score_codex":0.0022725882,"about_ca_topic_score_gemma":0.00028443523,"teacher_disagreement_score":0.29837853,"about_ca_system_score_codex":0.000010970379,"about_ca_system_score_gemma":0.0005421171,"threshold_uncertainty_score":0.99920535},"labels":[],"label_agreement":null},{"id":"W2033978320","doi":"10.1103/physrevb.76.233104","title":"Charge transfer in silicon clathrates studied by Compton scattering","year":2007,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Engineering and Physical Sciences Research Council","keywords":"Physics; Atomic physics; Compton scattering; Momentum transfer; Valence (chemistry); Charge (physics); Silicon; Scattering; Electron; Nuclear physics; Optics; Quantum mechanics","score_opus":0.015072284294664008,"score_gpt":0.2697846019317677,"score_spread":0.25471231763710367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033978320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845204,0.012141803,0.000021503995,0.00028066503,0.00013983522,0.00028528273,0.00005449321,0.000023595041,0.0025324698],"genre_scores_gemma":[0.99523544,0.0038744765,0.000008667792,0.0006183476,0.00015561027,0.000002637614,0.00007056924,0.000003895329,0.000030343474],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990238,0.000048062608,0.00023949366,0.00021905501,0.00016254488,0.00030704567],"domain_scores_gemma":[0.9996385,0.000103907354,0.000027488191,0.00013074419,0.000014362374,0.00008500326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037127602,0.00013737105,0.0003987196,0.000016689737,0.000044277123,0.000020600304,0.00011528892,0.000019026846,0.0005550074],"category_scores_gemma":[0.000011455638,0.00010297897,0.000067719295,0.000156484,0.000035878613,0.00010889095,0.00000803329,0.00009049901,0.0005369858],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021020617,0.0011735681,0.071997866,0.0074293925,0.00019929672,0.00011217509,0.0015736261,0.00008571622,0.6378601,0.00584945,0.0138430605,0.25966555],"study_design_scores_gemma":[0.0022262067,0.0007274824,0.5428984,0.005122304,0.00027614075,0.000008594285,0.00005143039,0.0018246147,0.12370161,0.004360466,0.31651273,0.0022900074],"about_ca_topic_score_codex":0.00040709673,"about_ca_topic_score_gemma":0.00016878927,"teacher_disagreement_score":0.5141585,"about_ca_system_score_codex":0.0000024389176,"about_ca_system_score_gemma":0.000006604122,"threshold_uncertainty_score":0.6902045},"labels":[],"label_agreement":null},{"id":"W2034395230","doi":"10.1021/ja110618g","title":"Synthesis of the Missing Oxide of Xenon, XeO<sub>2</sub>, and Its Implications for Earth’s Missing Xenon","year":2011,"lang":"en","type":"article","venue":"Journal of the American Chemical Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Xenon; Chemistry; Raman spectroscopy; Xenon difluoride; Noble gas; Valence (chemistry); Oxide; Oxygen; Atomic physics; Atmosphere (unit); Spectral line; Analytical Chemistry (journal); Inorganic chemistry; Physics; Organic chemistry; Thermodynamics","score_opus":0.018672830303110514,"score_gpt":0.22198141989579517,"score_spread":0.20330858959268466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034395230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983236,0.00018359939,0.0000828984,0.0010619017,0.00007466437,0.00009162858,0.00008051119,0.0000027573046,0.000098402066],"genre_scores_gemma":[0.99668103,0.00009074203,0.002969974,0.00016527539,0.00008302179,5.649353e-7,6.435017e-7,0.000004619736,0.000004107161],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991774,0.000055835324,0.00035449612,0.00009675257,0.00015593051,0.00015957748],"domain_scores_gemma":[0.9984548,0.00030672498,0.0008803309,0.00016350026,0.000118975026,0.000075675496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003226866,0.00009250454,0.0003122383,0.000009327208,0.00012577942,0.000016452832,0.00034068723,0.000036442587,0.000013519494],"category_scores_gemma":[0.00016096384,0.000051508378,0.00029883042,0.00014662146,0.00028127345,0.00007783746,0.000035073343,0.00010117658,3.8618367e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030951694,0.000022178385,0.0042867884,0.00003641208,0.000064705426,5.4701953e-8,0.0002628155,0.0000128576285,0.98739403,0.000019234212,0.00032612777,0.007543843],"study_design_scores_gemma":[0.000085016545,0.00003174787,0.110324785,0.00006602546,0.000106981286,0.000009412929,0.0000975248,0.00009301592,0.8876298,0.0013082227,0.000185975,0.00006149456],"about_ca_topic_score_codex":0.00013928213,"about_ca_topic_score_gemma":0.000003336472,"teacher_disagreement_score":0.106038,"about_ca_system_score_codex":0.000004019329,"about_ca_system_score_gemma":0.000068894195,"threshold_uncertainty_score":0.21004505},"labels":[],"label_agreement":null},{"id":"W2034650858","doi":"10.1046/j.1365-246x.2000.00039.x","title":"Observations of PKP(DF) and PKP(BC) across the United Kingdom: implications for studies of attenuation in the Earth's core","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Mantle (geology); Attenuation; Geology; Amplitude; Inner core; Seismology; Scattering; Geophysics; Physics; Optics","score_opus":0.13801255933271064,"score_gpt":0.3528370262427865,"score_spread":0.21482446691007587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034650858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945161,0.000046084253,0.000068786074,0.0045327935,0.00021201152,0.00016426439,0.00035651776,0.0000030128447,0.00010044469],"genre_scores_gemma":[0.998942,0.0001094799,0.0002243582,0.00021867974,0.000287666,0.0000066861553,0.00010871736,0.0000021769565,0.00010019128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917376,0.000065207474,0.00032588877,0.00009656413,0.00020858838,0.00012996988],"domain_scores_gemma":[0.99882734,0.00058153266,0.00018730998,0.000106014595,0.00027343273,0.000024364179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042494235,0.000076538476,0.00014682708,0.000039409875,0.00020747886,0.00006041445,0.00030440468,0.00002590427,0.000101544065],"category_scores_gemma":[0.000091047084,0.00004347578,0.000059073598,0.00019229166,0.00016602316,0.00016812248,0.000013477065,0.00010159308,0.000005483916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009536222,0.0008189155,0.59866,0.00015986587,0.0013620959,0.000008376449,0.021075238,0.034169775,0.032682154,0.1698745,0.008128195,0.13210727],"study_design_scores_gemma":[0.00030282733,0.000076442266,0.9718426,0.000027662301,0.00002175715,0.000009605408,0.00027539273,0.001293789,0.000114578106,0.021277657,0.004705185,0.00005249674],"about_ca_topic_score_codex":0.0010220838,"about_ca_topic_score_gemma":0.000379942,"teacher_disagreement_score":0.37318262,"about_ca_system_score_codex":0.000002472102,"about_ca_system_score_gemma":0.000023745506,"threshold_uncertainty_score":0.17728907},"labels":[],"label_agreement":null},{"id":"W2035612946","doi":"10.2138/am.2007.2433","title":"Vibrational dynamics in H+-substituted forsterite: A first-principles molecular dynamics study","year":2007,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Forsterite; Molecular dynamics; Atom (system on chip); Chemistry; Spectral line; Proton; Ion; Infrared spectroscopy; Molecular vibration; Infrared; Density functional theory; Atmospheric temperature range; Vibrational spectrum; Dynamics (music); Molecular physics; Atomic physics; Physical chemistry; Computational chemistry; Molecule; Physics; Mineralogy; Thermodynamics","score_opus":0.011661749199345551,"score_gpt":0.23437124009659746,"score_spread":0.22270949089725192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035612946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903443,0.000023149112,0.0037856684,0.00028996842,0.0002714516,0.00031878226,0.00024871083,0.000044512326,0.004673455],"genre_scores_gemma":[0.9959815,0.000005793117,0.0028799055,0.00013859938,0.000068098496,0.000004352689,0.0008231666,0.000007713462,0.00009084395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998514,0.00006213251,0.00039400707,0.00034754758,0.000267669,0.00041466497],"domain_scores_gemma":[0.99929994,0.00011939278,0.00015676243,0.0002681023,0.000041935047,0.00011385945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032457488,0.00019902588,0.00030916653,0.00013187365,0.00010484908,0.00008863733,0.00028118247,0.000040261177,0.00016268164],"category_scores_gemma":[0.000053122734,0.00018056907,0.000050419116,0.00047473176,0.0002532849,0.0001490186,0.000031870517,0.00010643188,0.00005556201],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001339008,0.00020630652,0.96231365,0.000014261838,0.000041270407,0.00046010443,0.0002923621,0.025231859,0.00036105255,0.0065452773,0.000033106153,0.0043668505],"study_design_scores_gemma":[0.00042936392,0.00028046826,0.9020947,0.000008863356,0.000017371309,0.0000119508095,0.00085842237,0.095198885,0.000045272693,0.00033502013,0.0003994138,0.00032022162],"about_ca_topic_score_codex":0.042291112,"about_ca_topic_score_gemma":0.41615558,"teacher_disagreement_score":0.37386447,"about_ca_system_score_codex":0.00004518054,"about_ca_system_score_gemma":0.000054720258,"threshold_uncertainty_score":0.96408635},"labels":[],"label_agreement":null},{"id":"W2036264045","doi":"10.1029/2004gl021080","title":"Anisotropy of the flexural response of the lithosphere in the Canadian Shield","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Lithosphere; Shield; Geology; Anisotropy; Flexural strength; Geophysics; Seismology; Petrology; Tectonics; Physics; Materials science; Optics; Composite material","score_opus":0.02634217695026945,"score_gpt":0.2710980626453812,"score_spread":0.24475588569511178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036264045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97414005,0.00002873084,0.0000010897836,0.024689263,0.00017957496,0.00032010558,0.000086806125,0.0000027845826,0.0005515939],"genre_scores_gemma":[0.9988668,0.0000035333237,0.000036903224,0.0008867678,0.00011230346,0.0000037718519,0.000003467603,0.000003264271,0.00008316951],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973046,0.0009459738,0.00019190535,0.00017468855,0.0008754544,0.00050736003],"domain_scores_gemma":[0.9986919,0.00055718893,0.000054893793,0.00055331603,0.0000558943,0.0000867719],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010733365,0.000095194955,0.0001562622,0.000041767747,0.00030007694,0.000064561784,0.0011652173,0.000051069936,0.00013783539],"category_scores_gemma":[0.00029115216,0.000043521402,0.00010486493,0.00069631357,0.00061402045,0.00008151364,0.000057369678,0.0003956499,0.000053566502],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0040737833,0.000581735,0.21848598,0.0003897409,0.00023656063,0.00025908602,0.029683758,0.028588954,0.61444604,0.06598699,0.02804566,0.009221711],"study_design_scores_gemma":[0.0002371096,0.00010422585,0.98446435,0.000046156383,0.0000050786634,0.0000012677781,0.00020181414,0.000037660593,0.0070179654,0.0056092637,0.002203168,0.00007196001],"about_ca_topic_score_codex":0.57459456,"about_ca_topic_score_gemma":0.2989993,"teacher_disagreement_score":0.76597834,"about_ca_system_score_codex":0.000018175417,"about_ca_system_score_gemma":0.00042605549,"threshold_uncertainty_score":0.71379215},"labels":[],"label_agreement":null},{"id":"W2036820661","doi":"10.1111/j.1365-246x.2006.02980.x","title":"Analytical approach for the toroidal relaxation of viscoelastic earth","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Asthenosphere; Viscoelasticity; Lithosphere; Toroid; Geology; Geophysics; Mantle (geology); Propagator; Mechanics; Inner core; Physics; Seismology; Thermodynamics","score_opus":0.010945365286820457,"score_gpt":0.22549910748031382,"score_spread":0.21455374219349335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036820661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85480547,0.00014116862,0.12714608,0.0010772666,0.0027323489,0.00033638888,0.00038131833,0.000024664809,0.013355303],"genre_scores_gemma":[0.99496406,0.0000074612863,0.0018340726,0.000041868156,0.0023303048,0.0000018656433,0.00011523597,0.0000034109048,0.0007017357],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99897265,0.00003672594,0.00029851735,0.00012668871,0.00039375175,0.00017166273],"domain_scores_gemma":[0.99921244,0.00029362,0.00019078447,0.00008573808,0.00016749576,0.00004990402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024227079,0.00009268945,0.00014706013,0.000040973602,0.00013988593,0.00011914562,0.00029422066,0.000037321952,0.00045671433],"category_scores_gemma":[0.00005244345,0.00005691434,0.00014478796,0.00007169579,0.00008232968,0.00018260286,0.000013163089,0.000117111544,0.000032437998],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020254508,0.0013325029,0.05900517,0.000119721946,0.001386385,0.000031012052,0.00039042707,0.5112016,0.01604511,0.29904264,0.03046242,0.078957535],"study_design_scores_gemma":[0.00087029784,0.0002622077,0.62665707,0.000017718166,0.000118031036,0.000049463502,0.000048665475,0.33397463,0.0011265385,0.021162163,0.015499466,0.0002137283],"about_ca_topic_score_codex":0.00044227633,"about_ca_topic_score_gemma":0.000029164827,"teacher_disagreement_score":0.5676519,"about_ca_system_score_codex":0.000003600184,"about_ca_system_score_gemma":0.00003631996,"threshold_uncertainty_score":0.50007015},"labels":[],"label_agreement":null},{"id":"W2037040278","doi":"10.1130/g21963.1","title":"Surface erosion control on the evolution of the deep lithosphere","year":2006,"lang":"en","type":"article","venue":"Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Citation; Icon; Crust; Materiality (auditing); Earth science; Library science; Tectonics; Paleontology; Computer science","score_opus":0.00432583835713527,"score_gpt":0.16790210902245606,"score_spread":0.1635762706653208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037040278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930249,0.0002499824,0.00016516128,0.0010911995,0.0005463421,0.00013161515,0.000028688974,0.000009205894,0.0047528967],"genre_scores_gemma":[0.9992244,0.000003192758,0.000027414077,0.00013282165,0.00009425353,5.320233e-7,0.0000069478274,0.0000011668304,0.0005092518],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993996,0.0001556261,0.0001104911,0.00009653361,0.00009293827,0.00014478972],"domain_scores_gemma":[0.99954706,0.0001573844,0.00007567661,0.0001836089,0.000024531031,0.000011717999],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018528005,0.000057897283,0.00010031908,0.0000044236817,0.000111961774,0.00000780617,0.00017078107,0.00005138186,0.0011461945],"category_scores_gemma":[0.000016669199,0.000027480146,0.000035141686,0.000061492625,0.000101602884,0.000021614998,0.000009264701,0.00005057115,0.00015417156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011608068,0.000034701723,0.851532,0.000012440925,0.000019204645,0.0000016771841,0.00008592535,0.09135581,0.010821648,0.041551735,0.0038060378,0.0006627421],"study_design_scores_gemma":[0.00017850692,0.00007140205,0.9821921,0.0000043961195,0.000010782338,0.0000014536764,0.000023768138,0.0017375869,0.0009204262,0.0116164135,0.0031962616,0.00004689663],"about_ca_topic_score_codex":0.016570909,"about_ca_topic_score_gemma":0.0043813093,"teacher_disagreement_score":0.1306601,"about_ca_system_score_codex":0.0000018574437,"about_ca_system_score_gemma":0.000017565704,"threshold_uncertainty_score":0.9997669},"labels":[],"label_agreement":null},{"id":"W2037633582","doi":"10.1016/j.actamat.2013.12.002","title":"Stability of the two-phase (α/ω) microstructure of shocked zirconium","year":2014,"lang":"en","type":"article","venue":"Acta Materialia","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Kinectrics (Canada); Queen's University","funders":"","keywords":"Materials science; Microstructure; Phase (matter); Isothermal process; Zirconium; Metastability; Thermodynamics; Thermal expansion; Volume fraction; Dislocation; Composite material; Crystallography; Metallurgy; Chemistry","score_opus":0.010045906162766315,"score_gpt":0.22354816494745275,"score_spread":0.21350225878468643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037633582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99465936,0.000008820002,0.000006182233,0.00008741024,0.0036244958,0.0001559175,0.0008549679,0.000011194696,0.0005916523],"genre_scores_gemma":[0.9995232,0.0000016859572,0.0001490627,0.00004122474,0.00016344468,5.700609e-7,0.000060647762,0.0000035326898,0.00005659272],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990353,0.00016815706,0.00030223926,0.00016324678,0.00015706416,0.00017401703],"domain_scores_gemma":[0.9992258,0.000028927081,0.00021181062,0.00043885445,0.00005244154,0.000042158503],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032276032,0.00011320589,0.0002697283,0.000014479646,0.000056368022,0.00003699081,0.00034926544,0.00005511438,0.003626567],"category_scores_gemma":[0.00004105821,0.000069637405,0.00005983391,0.0000723508,0.0001495771,0.000092603455,0.000035658824,0.000036147296,0.00001615334],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009265975,0.000017600712,0.0069675962,0.00007750598,0.000012437226,1.6026448e-7,0.0001497782,0.000004688287,0.99170923,0.00028453465,0.00046406183,0.00021973928],"study_design_scores_gemma":[0.0006378572,0.000081066326,0.114024065,0.00001487382,0.000025984365,0.0000013707562,0.000016425054,0.000041850417,0.8751391,0.0014174932,0.008502005,0.00009791994],"about_ca_topic_score_codex":0.0023200547,"about_ca_topic_score_gemma":0.00022541886,"teacher_disagreement_score":0.11657015,"about_ca_system_score_codex":0.0000011833508,"about_ca_system_score_gemma":0.000028289682,"threshold_uncertainty_score":0.99728423},"labels":[],"label_agreement":null},{"id":"W2037684951","doi":"10.1039/c4ce01749h","title":"Density functional theory study of the magnetic shielding mechanism for<sup>11</sup>B in pentaborate minerals: ulexite and probertite","year":2014,"lang":"en","type":"article","venue":"CrystEngComm","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Winnipeg; University of Manitoba","funders":"","keywords":"Electromagnetic shielding; Boron; Density functional theory; Atomic orbital; Mechanism (biology); Crystallography; Chemistry; Materials science; Atomic physics; Computational chemistry; Physics; Nuclear physics; Electron; Composite material; Quantum mechanics","score_opus":0.013566094612626122,"score_gpt":0.19517880472755317,"score_spread":0.18161271011492705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037684951","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985137,0.00006351909,0.0001757739,0.000099345,0.00027001207,0.0005221412,0.000033191718,0.000011146554,0.00031118887],"genre_scores_gemma":[0.99941915,0.000003857662,0.00010827128,0.000110262146,0.00011475043,0.0000088100605,0.000011922004,0.0000043125506,0.00021866748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989417,0.000299286,0.00022499757,0.0002040881,0.00015040499,0.00017952874],"domain_scores_gemma":[0.99935365,0.00024385683,0.000086840024,0.0002149232,0.000057176534,0.0000435776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007451416,0.00011586613,0.00021493921,0.000042792763,0.00013922184,0.000053020754,0.00015490902,0.000044718312,0.00012908595],"category_scores_gemma":[0.00007760111,0.00007675481,0.000032060187,0.00010531322,0.000044038017,0.000100003475,0.000037075824,0.00006381203,0.0000044840795],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00087997393,0.00070349785,0.78802794,0.0008171585,0.00020537789,0.000010371947,0.013164636,0.026648605,0.04389312,0.113100454,0.001202716,0.0113461595],"study_design_scores_gemma":[0.0025395178,0.0008266057,0.88018394,0.00011584121,0.00013848496,0.00000899325,0.0018967006,0.03228548,0.0012363773,0.0787645,0.0015974117,0.0004061331],"about_ca_topic_score_codex":0.00079073233,"about_ca_topic_score_gemma":0.0024564622,"teacher_disagreement_score":0.09215602,"about_ca_system_score_codex":0.0000016820635,"about_ca_system_score_gemma":0.000013888761,"threshold_uncertainty_score":0.31299704},"labels":[],"label_agreement":null},{"id":"W2037704177","doi":"10.1139/e05-032","title":"Lithospheric structure of the Trans-Hudson Orogen from seismic refraction - wide-angle reflection studies","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of British Columbia; PotashCorp (Canada)","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; National Science Foundation","keywords":"Geology; Lithosphere; Craton; Seismology; Fibrous joint; Gneiss; Mantle (geology); Archean; Fold (higher-order function); Crust; Clockwise; Tectonics; Seismic anisotropy; Metamorphic rock; Crustal recycling; Collision zone; Petrology; Geophysics; Geochemistry","score_opus":0.020524818843044773,"score_gpt":0.23426551346496496,"score_spread":0.2137406946219202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037704177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945139,0.0023717757,0.00002924465,0.0010828564,0.0014827797,0.000062950734,0.000101485144,0.000002696314,0.0003522833],"genre_scores_gemma":[0.9983046,0.00008955387,0.00097225135,0.00019865885,0.00034153377,6.7873714e-8,0.0000022261174,0.0000018239126,0.00008925291],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989984,0.000097077,0.00029076205,0.00012422603,0.00027256433,0.00021693978],"domain_scores_gemma":[0.99923015,0.00007891288,0.00030552596,0.00010025058,0.00011936836,0.00016579521],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032535236,0.000090901274,0.00019589353,0.00006803657,0.00036083424,0.00008083308,0.00031492457,0.000045789104,0.0009421994],"category_scores_gemma":[0.00007359641,0.00005461897,0.000069966016,0.00036706362,0.00027003651,0.0004689009,0.000003035144,0.00011161521,0.0000073170772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000087657296,0.000023085631,0.6644153,0.000055331875,0.00033803363,0.000024661615,0.012100018,0.22511168,0.03662351,0.00017836198,0.003916442,0.057125892],"study_design_scores_gemma":[0.000317466,0.0004402152,0.85302114,0.00015179861,0.00010845542,0.000053046973,0.0016727602,0.0010488135,0.036325507,0.004918657,0.10169465,0.00024747924],"about_ca_topic_score_codex":0.030742612,"about_ca_topic_score_gemma":0.4138014,"teacher_disagreement_score":0.3830588,"about_ca_system_score_codex":0.0000034710083,"about_ca_system_score_gemma":0.00056381646,"threshold_uncertainty_score":0.9999711},"labels":[],"label_agreement":null},{"id":"W2038365841","doi":"10.1063/1.2969909","title":"Equation of state for diamond in wide ranges of pressure and temperature","year":2008,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Debye model; Anharmonicity; Phonon; Diamond; Thermodynamics; Melting curve analysis; Atmospheric temperature range; Melting temperature; Equation of state; Condensed matter physics; Materials science; Ambient pressure; Volume (thermodynamics); Range (aeronautics); Debye; Diamond anvil cell; Chemistry; Physics; High pressure","score_opus":0.013674379154146644,"score_gpt":0.20208277039590622,"score_spread":0.18840839124175957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038365841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990316,0.0003302151,0.000099805715,0.000013617527,0.00008467563,0.0001316043,0.00012617993,0.00000118399,0.00018112874],"genre_scores_gemma":[0.9988462,0.00018086206,0.00082315144,0.000014572042,0.00010478519,5.276785e-7,0.000011614257,0.000002559155,0.00001572928],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994142,0.000014515461,0.00027271564,0.00006126641,0.00015240317,0.00008486505],"domain_scores_gemma":[0.99935514,0.0001368325,0.00034215493,0.000057113415,0.00007747091,0.00003126414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018117717,0.00006692788,0.00027138638,0.000031722582,0.000024126624,0.0000074659847,0.00007272989,0.000032637214,0.000011414516],"category_scores_gemma":[0.000009271455,0.00005077198,0.00003523817,0.00007343491,0.00004740398,0.00010859272,0.0000045183174,0.000060622166,3.6110234e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026657414,0.00025443255,0.046186615,0.0010561451,0.00036353176,0.000011622891,0.00936643,0.32357532,0.5983045,0.0016057338,0.0019577644,0.014652188],"study_design_scores_gemma":[0.0037767938,0.00075189804,0.42920426,0.00016416384,0.0002069028,0.0000079583615,0.00021571029,0.0037503652,0.5044536,0.053848915,0.0032735558,0.00034586657],"about_ca_topic_score_codex":0.000051123152,"about_ca_topic_score_gemma":0.000016778258,"teacher_disagreement_score":0.38301763,"about_ca_system_score_codex":5.652376e-7,"about_ca_system_score_gemma":0.00003834271,"threshold_uncertainty_score":0.20704213},"labels":[],"label_agreement":null},{"id":"W2038700915","doi":"10.1103/physrevb.72.174103","title":"Electronic and crystal structures of osmium under high pressure","year":2005,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences; University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Fermi surface; Condensed matter physics; Anomaly (physics); Electronic structure; Electronic band structure; Phonon; Materials science; Physics; Fermi level; Lattice (music); Electron; Superconductivity; Quantum mechanics","score_opus":0.006040423022616625,"score_gpt":0.23344842314829015,"score_spread":0.22740800012567353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038700915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94617754,0.05147007,0.000025357669,0.00064541836,0.00008590045,0.0002555089,0.00012372211,0.00002164694,0.0011948412],"genre_scores_gemma":[0.9941912,0.005000338,0.00007692509,0.00031352864,0.00031099346,0.0000012195634,0.000030452044,0.0000030171323,0.000072317525],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99925643,0.000054080905,0.00014803388,0.00016859075,0.00016312387,0.00020973064],"domain_scores_gemma":[0.9996308,0.000056336026,0.00007703911,0.00014802004,0.000023687751,0.00006410985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009005985,0.00010967086,0.00031900557,0.000009909605,0.000035178542,0.000016585162,0.000115698,0.000018509752,0.0007693739],"category_scores_gemma":[0.000013059713,0.00007499895,0.000052556094,0.000067600406,0.000053433672,0.000111538815,0.000014589906,0.0000725233,0.000039319853],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023452856,0.00048566677,0.008085067,0.0142235,0.0010200578,0.0000067181068,0.00057997653,0.008029591,0.10168594,0.53401476,0.017501637,0.31413254],"study_design_scores_gemma":[0.00082833605,0.0006264205,0.31322727,0.00080183503,0.0008881049,0.000013678578,0.000012276355,0.0018365008,0.0158308,0.19086026,0.4741555,0.0009190349],"about_ca_topic_score_codex":0.00030759966,"about_ca_topic_score_gemma":0.00007894703,"teacher_disagreement_score":0.45665386,"about_ca_system_score_codex":8.7584056e-7,"about_ca_system_score_gemma":0.00002412045,"threshold_uncertainty_score":0.8424105},"labels":[],"label_agreement":null},{"id":"W2038860882","doi":"10.1016/j.jsg.2007.11.002","title":"The analogue shear zone: From rheology to associated geometry","year":2007,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Rheology; Geology; Shear (geology); Finite strain theory; Shear zone; Strain hardening exponent; Geotechnical engineering; Mechanics; Finite element method; Materials science; Petrology; Composite material; Physics","score_opus":0.006974036008845784,"score_gpt":0.2236713222184617,"score_spread":0.21669728620961592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038860882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99468994,0.00047618605,0.00025714925,0.0009796051,0.0031906643,0.000057968216,0.000048931983,0.0000075612775,0.0002919956],"genre_scores_gemma":[0.99794453,0.000028847142,0.0006585488,0.00043408445,0.0006928356,6.7047246e-8,0.000027980535,0.0000027959495,0.00021029281],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985992,0.00013518734,0.00049697474,0.00012693401,0.00021767712,0.0004240674],"domain_scores_gemma":[0.9985419,0.0006335844,0.00036120092,0.00013209597,0.0001584647,0.00017277889],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00084553024,0.000120230645,0.00033172168,0.000107046646,0.0002018076,0.000041414536,0.00039963046,0.00013240479,0.0014452694],"category_scores_gemma":[0.0002349697,0.000069461836,0.00008394234,0.00020721417,0.00013064202,0.00009954804,0.00002893247,0.00023369936,0.00008967747],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010791167,0.00001459121,0.922124,0.000005955361,0.00059340784,0.00045869767,0.00063836994,0.004128215,0.00684746,0.0022105644,0.005591902,0.056307666],"study_design_scores_gemma":[0.00027374717,0.00030477194,0.98701966,0.0000040313344,0.000025472626,0.00008372259,0.000073379524,0.00007600745,0.00035513224,0.005137517,0.0065541365,0.00009242162],"about_ca_topic_score_codex":0.00295379,"about_ca_topic_score_gemma":0.004065971,"teacher_disagreement_score":0.06489561,"about_ca_system_score_codex":0.000006349003,"about_ca_system_score_gemma":0.00004169007,"threshold_uncertainty_score":0.99946755},"labels":[],"label_agreement":null},{"id":"W2039451408","doi":"10.1103/physreva.83.012509","title":"Construction of integrable model Kohn-Sham potentials by analysis of the structure of functional derivatives","year":2011,"lang":"en","type":"article","venue":"Physical Review A","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Kohn–Sham equations; Physics; Functional derivative; Integrable system; Density functional theory; Derivative (finance); Hybrid functional; Orbital-free density functional theory; Order (exchange); Quantum mechanics; Applied mathematics; Mathematical physics; Mathematics","score_opus":0.020471941293249668,"score_gpt":0.2268228474604809,"score_spread":0.20635090616723123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039451408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957169,0.0017039871,0.00088252034,0.000022473667,0.00008245389,0.0001430991,0.0007623119,0.0000035854966,0.0006826582],"genre_scores_gemma":[0.9990193,0.00044743964,0.000409102,0.000032474214,0.00001673755,4.9203777e-7,0.000058701182,0.0000015074428,0.000014226046],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992303,0.00008240206,0.00027730805,0.0001202094,0.00020731414,0.00008241705],"domain_scores_gemma":[0.9993143,0.000044209326,0.0003280431,0.00018499968,0.00010165788,0.000026752365],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000084853215,0.00008449334,0.00048258292,0.00002771457,0.000026070791,0.00000288936,0.00015057545,0.000019272382,0.0010003715],"category_scores_gemma":[0.00003780509,0.0000478722,0.00021222218,0.00040812825,0.0001549757,0.00008177508,0.000015211764,0.000044788525,0.0000016955084],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017914247,0.0004127776,0.036397804,0.0036648354,0.0035468875,3.1164495e-7,0.0012670154,0.013264584,0.8684365,0.046103377,0.0018778545,0.024848897],"study_design_scores_gemma":[0.00042990036,0.00026068016,0.3226898,0.00121571,0.0065418244,0.0000017446982,0.00012416468,0.038222656,0.518078,0.11140786,0.0005209419,0.0005066628],"about_ca_topic_score_codex":0.000549235,"about_ca_topic_score_gemma":0.000031573793,"teacher_disagreement_score":0.35035846,"about_ca_system_score_codex":7.7846977e-7,"about_ca_system_score_gemma":0.00002824237,"threshold_uncertainty_score":0.99991286},"labels":[],"label_agreement":null},{"id":"W2039915378","doi":"10.1007/s00410-014-1012-8","title":"Iron speciation in minerals and glasses probed by $$\\hbox{M}_{2/3}$$ M 2 / 3 -edge X-ray Raman scattering spectroscopy","year":2014,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Raman spectroscopy; Oxidation state; Ferric; Ferrous; Crystallography; Octahedron; Chemistry; Raman scattering; Analytical Chemistry (journal); X-ray Raman scattering; Spectroscopy; Scattering; K-edge; Spectral line; Inorganic chemistry; Crystal structure; Physics; Metal; Optics","score_opus":0.003868607797558825,"score_gpt":0.21922133412407677,"score_spread":0.21535272632651795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039915378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929182,0.00042601718,0.00094210077,0.003803158,0.00035584264,0.00023147646,0.00035175882,0.000026005195,0.0009454337],"genre_scores_gemma":[0.9977851,0.00007435187,0.00038934563,0.000632841,0.0003166581,0.000011443067,0.00041194833,0.000004012464,0.00037431525],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986776,0.00022028602,0.00026086945,0.00035805037,0.00006310462,0.00042007508],"domain_scores_gemma":[0.9993997,0.00020572064,0.000070174,0.00014438883,0.000044737535,0.00013525445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004098499,0.00016438935,0.00034770527,0.00013380521,0.00015426846,0.000068158086,0.000096564254,0.00013461172,0.0003301926],"category_scores_gemma":[0.00012747428,0.0001482251,0.000020793823,0.00012038214,0.00011608655,0.00013788832,0.00002505695,0.000110668385,0.0000604058],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031560374,0.00008691843,0.3017077,0.000057598783,0.000049056667,0.000013520854,0.00032231622,0.0009284104,0.66979414,0.006411121,0.017595494,0.002718088],"study_design_scores_gemma":[0.0019592033,0.00083270157,0.8819832,0.000019052786,0.000053746386,0.000026664873,0.000015686057,0.0030888147,0.002351054,0.0035009466,0.105746485,0.0004224277],"about_ca_topic_score_codex":0.0012259105,"about_ca_topic_score_gemma":0.0034820333,"teacher_disagreement_score":0.6674431,"about_ca_system_score_codex":0.0000066668244,"about_ca_system_score_gemma":0.00001687524,"threshold_uncertainty_score":0.6044444},"labels":[],"label_agreement":null},{"id":"W2039919643","doi":"10.1016/j.epsl.2010.04.050","title":"Electrical conductivity of basaltic and carbonatite melt-bearing peridotites at high pressures: Implications for melt distribution and melt fraction in the upper mantle","year":2010,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":133,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Carbonatite; Geology; Peridotite; Olivine; Silicate; Mantle (geology); Partial melting; Mineralogy; Basalt; Carbonate; Electrical resistivity and conductivity; Geochemistry; Materials science; Metallurgy; Chemistry","score_opus":0.008027304633465597,"score_gpt":0.20727001755413943,"score_spread":0.19924271292067383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039919643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973298,0.00016778558,0.000042619966,0.0015101669,0.00016433946,0.00028798732,0.00045566828,0.000008226377,0.000033407257],"genre_scores_gemma":[0.9989622,0.000061942315,0.0004106994,0.00022983162,0.00007406526,0.0000037422135,0.00024845952,0.0000016977649,0.000007344101],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999089,0.00005102855,0.00014375817,0.00029088338,0.00016892505,0.0002564171],"domain_scores_gemma":[0.9993246,0.00036043886,0.00007177085,0.00014221526,0.000020390651,0.00008059402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056825887,0.000105133906,0.00015504395,0.00006438399,0.00032881548,0.00010255609,0.00013304247,0.00004471165,0.000040607953],"category_scores_gemma":[0.000065416876,0.00007490907,0.000014517362,0.00015463162,0.00037857253,0.0003698741,0.000017228263,0.00012710842,0.0000017432648],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006639025,0.00001564621,0.7716604,0.00005492249,0.000012205891,0.000002071805,0.00033486538,0.00021776985,0.21909651,0.00072428357,0.00023802649,0.0075769285],"study_design_scores_gemma":[0.00017992199,0.00006171958,0.99180615,0.000005507434,0.00001813721,0.000020974605,0.00001600756,0.0023749187,0.0024652719,0.00025252157,0.002700271,0.0000985725],"about_ca_topic_score_codex":0.0035255789,"about_ca_topic_score_gemma":0.0019026462,"teacher_disagreement_score":0.22014579,"about_ca_system_score_codex":0.0000014178785,"about_ca_system_score_gemma":0.000022256643,"threshold_uncertainty_score":0.5329644},"labels":[],"label_agreement":null},{"id":"W2040190639","doi":"10.1103/physrevc.69.052801","title":"Proton-shell effects in neutron-star matter","year":2004,"lang":"en","type":"article","venue":"Physical Review C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Physics; Neutron; Neutron star; Shell (structure); Proton; Nuclear physics; Magic number (chemistry); Nuclear drip line; Equation of state; Nuclear matter; r-process; Atomic physics; MAGIC (telescope); Nuclear reaction; Thermodynamics; Nucleon; Materials science; Astrophysics; Nucleosynthesis","score_opus":0.007187231928634184,"score_gpt":0.24074338832180622,"score_spread":0.23355615639317204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040190639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99000597,0.0043697204,0.0000042768274,0.00075332215,0.00018952644,0.0012053384,0.0000214005,0.000024289531,0.003426156],"genre_scores_gemma":[0.99702597,0.0011653217,0.00011827735,0.0013601846,0.00021986415,0.000033156528,0.000034070363,0.000004918968,0.00003822598],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999127,0.00006895047,0.00014681638,0.00022745793,0.00016088417,0.0002689245],"domain_scores_gemma":[0.9995929,0.00005926438,0.000049912294,0.0002017399,0.00001220875,0.00008395876],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000119764554,0.00013901597,0.0003559277,0.000017060878,0.00003021453,0.000027246084,0.00016729912,0.000018268473,0.0004655574],"category_scores_gemma":[0.000014160391,0.0000980379,0.00007966357,0.00014679687,0.000029621611,0.00013662738,0.000014186839,0.000095343865,0.0055067614],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005390981,0.006450073,0.348633,0.17357069,0.0005023734,0.0013521566,0.0031457269,0.012653282,0.120021425,0.07647713,0.026974684,0.22968036],"study_design_scores_gemma":[0.00090762496,0.00027560137,0.88555413,0.003757897,0.00007942725,0.0000045481816,0.0000025094068,0.00016853453,0.00460125,0.027682025,0.07634791,0.0006185421],"about_ca_topic_score_codex":0.00074567256,"about_ca_topic_score_gemma":0.00005141326,"teacher_disagreement_score":0.53692114,"about_ca_system_score_codex":0.0000034090851,"about_ca_system_score_gemma":0.000023621345,"threshold_uncertainty_score":0.99526757},"labels":[],"label_agreement":null},{"id":"W2040629898","doi":"10.1029/2001jb000594","title":"Modeling <i>S</i> wave amplitude patterns for events in the Kurile slab using three‐dimensional Gaussian beams","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Slab; Geology; Amplitude; Subduction; Residual; Seismology; Seismometer; Slab window; Geophysics; Seismogram; Geodesy; Physics; Tectonics; Optics; Oceanic crust","score_opus":0.08633695797169516,"score_gpt":0.311055591709627,"score_spread":0.22471863373793183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040629898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972235,0.0003959047,0.0010959535,0.0004720933,0.00027084208,0.00032813652,0.00006650697,0.000004485656,0.00014257806],"genre_scores_gemma":[0.99691564,0.00003878025,0.001865061,0.00009883621,0.0009995361,0.000003312432,0.000009880979,0.000009530895,0.000059400278],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99694604,0.0003191659,0.00050592225,0.00023399708,0.0013039942,0.00069088046],"domain_scores_gemma":[0.99839264,0.0007586415,0.00013995028,0.0002378169,0.0002824898,0.00018848175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015580573,0.00016998399,0.00036331904,0.000030871382,0.00030662466,0.00013112079,0.00054068223,0.00007579821,0.0006881861],"category_scores_gemma":[0.00016729129,0.00010329299,0.0001909574,0.00028025778,0.000079335,0.00035596066,0.00004497545,0.00048660772,0.000046011915],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0032996007,0.0032101867,0.11082234,0.0007114563,0.0008478387,0.0009901108,0.0046187867,0.76640683,0.022394495,0.003074808,0.008984849,0.07463869],"study_design_scores_gemma":[0.0014509606,0.0011023078,0.077084765,0.0002865783,0.00004478331,0.000053000622,0.00033437408,0.88246024,0.00034064605,0.035209842,0.001306365,0.00032611264],"about_ca_topic_score_codex":0.0057140007,"about_ca_topic_score_gemma":0.0012864207,"teacher_disagreement_score":0.116053425,"about_ca_system_score_codex":0.000015693024,"about_ca_system_score_gemma":0.00008065882,"threshold_uncertainty_score":0.8637898},"labels":[],"label_agreement":null},{"id":"W2040776738","doi":"10.1139/e00-068","title":"Seismic imaging of the upper mantle beneath the Rocky Mountain foreland, southwestern Alberta","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary; Geological Survey of Canada; Western University","funders":"","keywords":"Geology; Seismology; Foreland basin; Crust; Mantle (geology); Tectonics; Geochemistry","score_opus":0.0074339561446724305,"score_gpt":0.1837045797332695,"score_spread":0.17627062358859708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040776738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99293363,0.00044097923,0.0000054316424,0.001501741,0.0005187813,0.000070083835,0.000065635126,0.0000010454035,0.0044626733],"genre_scores_gemma":[0.99842936,0.000017861244,0.000041489486,0.0003635888,0.00015259538,1.313968e-7,0.0000014460676,0.0000019827162,0.0009915305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897647,0.000074816344,0.0002548443,0.0001081201,0.0002637311,0.00032204652],"domain_scores_gemma":[0.9993503,0.0000903569,0.00016588312,0.00014679262,0.000051561918,0.00019508287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000558598,0.000090673784,0.00014486801,0.00006889386,0.0004951765,0.0001791429,0.00072124053,0.000022328366,0.0029419295],"category_scores_gemma":[0.000026302303,0.00004382044,0.000086600834,0.00022794314,0.0003834772,0.0002622929,0.000005951248,0.00009783228,0.000057891313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057608627,0.0000020345733,0.97843164,0.000003901241,0.000011092808,0.000006520732,0.0010607564,0.01665285,0.000035261466,0.00010104736,0.00026346353,0.0034256927],"study_design_scores_gemma":[0.0001443776,0.00007171689,0.95914805,0.000055861587,0.000025654046,0.00011096415,0.00041686668,0.0032537975,0.00027519523,0.0014137004,0.034976445,0.000107354186],"about_ca_topic_score_codex":0.1288067,"about_ca_topic_score_gemma":0.40722236,"teacher_disagreement_score":0.27841565,"about_ca_system_score_codex":0.0000010275992,"about_ca_system_score_gemma":0.00058706285,"threshold_uncertainty_score":0.9979695},"labels":[],"label_agreement":null},{"id":"W2040879223","doi":"10.1103/physrevb.78.140101","title":"High-pressure phases of calcium and their finite-temperature phase boundaries","year":2008,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Phase diagram; Orthorhombic crystal system; Materials science; Alkali metal; Phase (matter); Thermodynamics; Condensed matter physics; Phase transition; Alkaline earth metal; Density functional theory; Crystallography; Metal; Physics; Chemistry; Computational chemistry; Crystal structure; Metallurgy","score_opus":0.021185868761213637,"score_gpt":0.27073087408459445,"score_spread":0.2495450053233808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040879223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94238985,0.055250153,0.000017792654,0.00029595045,0.0002563368,0.00027182425,0.0010793387,0.000030233956,0.0004085356],"genre_scores_gemma":[0.99072576,0.008278645,0.00006163473,0.00034463985,0.00031901855,0.0000034269804,0.0001656156,0.0000047145254,0.000096573574],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990588,0.00008759847,0.00023090617,0.0002385434,0.00017562494,0.00020854482],"domain_scores_gemma":[0.9992569,0.00020836182,0.00011482084,0.00024177747,0.000063810396,0.00011429911],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001052823,0.00019451251,0.00062497164,0.000017471544,0.00020583843,0.000047224807,0.00016506626,0.000033029417,0.00061721116],"category_scores_gemma":[0.00009360782,0.00012155673,0.00009988634,0.00014280771,0.00033885633,0.00017990584,0.000022210466,0.000102777456,0.000037476457],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014984338,0.00521411,0.009967841,0.033475026,0.0024122049,0.00036297835,0.009598186,0.001269425,0.49141192,0.04685412,0.16110043,0.23683532],"study_design_scores_gemma":[0.0024895854,0.0013473979,0.012386833,0.0020163828,0.00056736975,0.000042471715,0.000038097125,0.0010783504,0.09883734,0.012912025,0.8671297,0.0011544414],"about_ca_topic_score_codex":0.0005204034,"about_ca_topic_score_gemma":0.000017693528,"teacher_disagreement_score":0.7060293,"about_ca_system_score_codex":5.280236e-7,"about_ca_system_score_gemma":0.000057020658,"threshold_uncertainty_score":0.67580295},"labels":[],"label_agreement":null},{"id":"W2041581428","doi":"10.1080/00268970412331292687","title":"Simulation study of solvent shifts of vibrational overtone spectra","year":2004,"lang":"en","type":"article","venue":"Molecular Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Chemistry; Intermolecular force; Anharmonicity; Overtone; Intramolecular force; Solvent; Spectral line; Thermodynamics; Computational chemistry; Molecule; Physics; Quantum mechanics; Organic chemistry","score_opus":0.011262776060451106,"score_gpt":0.22682759965975835,"score_spread":0.21556482359930723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041581428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97366893,0.000023979015,0.025533821,0.000012724906,0.00009854406,0.00017759674,0.00004596872,0.000007946786,0.0004305082],"genre_scores_gemma":[0.99900043,9.690255e-7,0.0008506791,0.000017387174,0.000060796196,5.8654143e-7,0.000063963125,0.000003086244,0.0000020954121],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99928355,0.00002969565,0.00018449374,0.0001233673,0.0002834036,0.00009550583],"domain_scores_gemma":[0.9996352,0.000026294243,0.000110735105,0.00015212609,0.00004730394,0.000028298524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061312596,0.00007764716,0.00015698194,0.000017740365,0.000028784285,0.000011384533,0.00008862475,0.000021218904,0.000091835136],"category_scores_gemma":[0.000007205899,0.00007108325,0.000044799326,0.000111901565,0.000023780753,0.00008756969,0.000009257287,0.000029627254,0.00001398523],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020463365,0.00027081426,0.0014923498,0.0000158483,0.00003723835,0.000004369857,0.00037853088,0.9154097,0.0793653,0.002605844,0.0000016387218,0.00039793403],"study_design_scores_gemma":[0.0023334443,0.0015118299,0.30088592,0.000045364784,0.00013016807,4.4769973e-7,0.00016496352,0.022649286,0.58772045,0.08410916,0.000051082294,0.00039789293],"about_ca_topic_score_codex":0.0008560804,"about_ca_topic_score_gemma":0.0000672803,"teacher_disagreement_score":0.8927604,"about_ca_system_score_codex":0.0000017342342,"about_ca_system_score_gemma":0.00003307453,"threshold_uncertainty_score":0.28986907},"labels":[],"label_agreement":null},{"id":"W2041853596","doi":"10.1063/1.3139060","title":"Structural transformations in carbon under extreme pressure: Beyond diamond","year":2009,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Diamond; Metastability; Carbon fibers; Ab initio quantum chemistry methods; Allotropy; Ab initio; Metadynamics; Materials science; Crystal structure; Phase (matter); Crystallography; Chemistry; Computational chemistry; Molecular dynamics; Phase diagram; Composite number; Organic chemistry; Molecule; Composite material","score_opus":0.015135432988180883,"score_gpt":0.20922412113250405,"score_spread":0.19408868814432317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041853596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968337,0.0003583932,0.00003758736,0.00054122513,0.00016137556,0.000061156396,0.000019538824,0.000004637578,0.001982375],"genre_scores_gemma":[0.99935794,0.000029413584,0.00008050035,0.0001458764,0.00036348542,6.287839e-8,0.000007831691,0.0000019129245,0.000012996498],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9992162,0.000050313254,0.0002767133,0.00005077913,0.00024018776,0.00016580801],"domain_scores_gemma":[0.9995823,0.000081187005,0.0001354897,0.00010019064,0.000040138726,0.000060677397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018635592,0.000093376926,0.0001869745,0.000017581802,0.000028906132,0.00002824467,0.00024059744,0.00003830844,0.00007493442],"category_scores_gemma":[0.0000072653197,0.000055848577,0.000055822708,0.000118243624,0.00004590814,0.00022193966,0.0000037265527,0.00018999107,0.0000035436533],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009003184,0.00020920597,0.0050064935,0.00009085921,0.0002535987,0.0000215613,0.007443529,0.114427045,0.8134228,0.004250764,0.0018804083,0.052093413],"study_design_scores_gemma":[0.0019481105,0.00035171187,0.107424445,0.00008816186,0.0003607669,0.0000664264,0.00017536173,0.016681202,0.24373288,0.62762153,0.0009807023,0.0005686743],"about_ca_topic_score_codex":0.00008906569,"about_ca_topic_score_gemma":0.00001084126,"teacher_disagreement_score":0.62337077,"about_ca_system_score_codex":0.0000026550167,"about_ca_system_score_gemma":0.000027875962,"threshold_uncertainty_score":0.2277439},"labels":[],"label_agreement":null},{"id":"W2042333155","doi":"10.1103/physrevb.65.184201","title":"Dynamical properties of liquid Al near melting:  An orbital-free molecular dynamics study","year":2002,"lang":"en","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Queen's University","keywords":"Pseudopotential; Molecular dynamics; Ab initio; Perturbation theory (quantum mechanics); Kinetic energy; Fragment molecular orbital; Molecular orbital; Neutron scattering; Scattering; Physics; Molecular physics; Materials science; Atomic physics; Classical mechanics; Molecule; Quantum mechanics","score_opus":0.017896152714096995,"score_gpt":0.25176925797404526,"score_spread":0.23387310525994826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042333155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953927,0.0013313383,0.000023690958,0.0012223236,0.00014733708,0.00062974717,0.00010558706,0.00004210573,0.0011052019],"genre_scores_gemma":[0.9976464,0.00006746111,0.00012999498,0.0018918619,0.000080402635,0.000011368513,0.000052855743,0.000017348499,0.000102341786],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9979224,0.0002895957,0.00047695238,0.00043855794,0.00049399986,0.0003784962],"domain_scores_gemma":[0.99874705,0.000055380657,0.00018280058,0.00074470334,0.000099728866,0.00017034315],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024706882,0.0002802792,0.0007020393,0.000029193496,0.00009350371,0.000084967854,0.00054880086,0.000040626222,0.0028132214],"category_scores_gemma":[0.00005909874,0.00020867868,0.00013971493,0.00014203493,0.00017039757,0.00024191284,0.00007810987,0.00016772255,0.001177202],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015369102,0.012252097,0.03249876,0.011850655,0.002042848,0.0013223487,0.009481287,0.0019470257,0.8667895,0.0054096747,0.037635867,0.01723303],"study_design_scores_gemma":[0.01364526,0.028042896,0.14074586,0.007704645,0.0056665833,0.00033687532,0.0013357548,0.6274049,0.11355865,0.025355268,0.024017554,0.012185707],"about_ca_topic_score_codex":0.00046569118,"about_ca_topic_score_gemma":0.000071673334,"teacher_disagreement_score":0.75323087,"about_ca_system_score_codex":0.000006557057,"about_ca_system_score_gemma":0.00002478011,"threshold_uncertainty_score":0.99960047},"labels":[],"label_agreement":null},{"id":"W2042344123","doi":"10.1007/s00410-011-0635-2","title":"Toward a quantitative model of metamorphic nucleation and growth","year":2011,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Nucleation; Metamorphic rock; Crystallization; Surface energy; Thermodynamics; Gibbs free energy; Mineralogy; Isobaric process; Geology; Crystal (programming language); Materials science; Geochemistry","score_opus":0.038645135087588926,"score_gpt":0.2412706810122067,"score_spread":0.20262554592461776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042344123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896972,0.00034730855,0.007329494,0.00060604344,0.00010910754,0.00010623557,0.0006956052,0.000011393946,0.0010976022],"genre_scores_gemma":[0.9972956,0.00006377834,0.002297966,0.00019266644,0.000023081635,0.000003203601,0.000065704706,0.0000015474745,0.000056439934],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9994066,0.000084834195,0.00015321944,0.00015845132,0.000036020854,0.00016089361],"domain_scores_gemma":[0.999603,0.00008751715,0.00005361568,0.00006797215,0.00011074235,0.00007719318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018366774,0.00007890841,0.00022416598,0.000082335275,0.00007639184,0.0000064562523,0.00005652496,0.00007459714,0.00024018144],"category_scores_gemma":[0.00007976206,0.000065855296,0.000019786892,0.000066402536,0.00014600552,0.000081648235,0.000014484481,0.00004710646,0.000019724972],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00080137356,0.00007185588,0.07984131,0.000051514828,0.00023733337,0.00001169953,0.003478222,0.00082823343,0.038123433,0.8748839,0.00074425613,0.0009268578],"study_design_scores_gemma":[0.0015158828,0.0017643125,0.81211805,0.000011009699,0.0002982406,0.000043821477,0.00008980126,0.03042676,0.002341008,0.1503273,0.0007027626,0.00036105013],"about_ca_topic_score_codex":0.0015929819,"about_ca_topic_score_gemma":0.0004863366,"teacher_disagreement_score":0.73227674,"about_ca_system_score_codex":8.6315396e-7,"about_ca_system_score_gemma":0.000020495747,"threshold_uncertainty_score":0.26855013},"labels":[],"label_agreement":null},{"id":"W2042516064","doi":"10.1107/s0909049508030859","title":"Selected techniques in diamond anvil cell crystallography: centring samples using X-ray transmission and rocking powder samples to improve X-ray diffraction image quality","year":2008,"lang":"en","type":"article","venue":"Journal of Synchrotron Radiation","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Centring; Diffraction; Optics; X-ray; Beam (structure); Rotation (mathematics); Collimated light; Sample (material); X-ray crystallography; Calibration; Materials science; Detector; Synchrotron; Diamond anvil cell; Physics; Geometry; Mathematics; Laser","score_opus":0.014840673849341122,"score_gpt":0.2406332059873249,"score_spread":0.22579253213798378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042516064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879861,0.0005284142,0.0109273335,0.00007157353,0.00014144531,0.00026551113,0.00003840207,0.000018518467,0.000022693222],"genre_scores_gemma":[0.9853465,0.0005366556,0.013800507,0.000028798875,0.00025157107,9.965777e-7,0.000023529681,0.0000074643503,0.0000039997553],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984364,0.00020567083,0.000581301,0.00020189742,0.0003078828,0.00026686635],"domain_scores_gemma":[0.9990489,0.00013737958,0.00045957198,0.00008652821,0.000120908626,0.00014670077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055702386,0.00016183726,0.00033140567,0.00032543082,0.00019146856,0.00009062782,0.000097052056,0.00009211968,0.00007502344],"category_scores_gemma":[0.0000580599,0.00013817633,0.00006600706,0.00030426824,0.000030827912,0.0007650811,0.000007449797,0.00016912754,9.912447e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001383246,0.00004443462,0.09626069,0.00006375502,0.000016381113,0.000011037571,0.00071413355,0.004393994,0.88544726,0.0000016955893,0.000027911208,0.012880385],"study_design_scores_gemma":[0.00048286695,0.00020419597,0.951855,0.000080182785,0.000028664168,0.000014214404,0.000097300675,0.0011600292,0.044633202,0.00008827225,0.001160469,0.0001955882],"about_ca_topic_score_codex":0.0025987134,"about_ca_topic_score_gemma":0.00010877934,"teacher_disagreement_score":0.85559434,"about_ca_system_score_codex":0.000028137945,"about_ca_system_score_gemma":0.00007878254,"threshold_uncertainty_score":0.5634667},"labels":[],"label_agreement":null},{"id":"W2043003387","doi":"10.1134/s1075701513010066","title":"Oxygen potential of diamond formation in the lower mantle","year":2013,"lang":"en","type":"article","venue":"Geology of Ore Deposits","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada)","funders":"Russian Academy of Sciences","keywords":"Mineral redox buffer; Mantle (geology); Silicate perovskite; Silicate; Diamond; Fugacity; Geology; Wüstite; Oxygen; Post-perovskite; Disproportionation; Geochemistry; Mineralogy; Materials science; Chemistry; Metallurgy; Physical chemistry","score_opus":0.005802460024757472,"score_gpt":0.18010864659995138,"score_spread":0.1743061865751939,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043003387","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975809,0.000103337035,0.000061478204,0.00022974002,0.00021579329,0.0001439445,0.000012619091,0.0000031623777,0.0016490284],"genre_scores_gemma":[0.99965835,0.000012424621,0.00015001629,0.00006209373,0.000033295193,0.0000015853219,0.00004280307,8.590308e-7,0.00003856132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994849,0.000064924796,0.00017204724,0.00006659883,0.00008932847,0.00012219243],"domain_scores_gemma":[0.9997319,0.00003277729,0.00008404382,0.00010568671,0.000030794796,0.0000147782175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011020548,0.000049375823,0.00011731646,0.000032988493,0.000026219866,0.0000080700665,0.00015845841,0.00005018732,0.00057233614],"category_scores_gemma":[0.000006596796,0.000031498606,0.000024494195,0.00005955627,0.00005785821,0.00013028996,0.000010353084,0.000033672182,0.000109919885],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041654363,0.0005767111,0.6802658,0.00057734054,0.00021012066,0.00018544859,0.008510328,0.012750764,0.22503638,0.0027904275,0.0157639,0.05291622],"study_design_scores_gemma":[0.00014309734,0.00011394631,0.9918287,0.0000055550445,0.000008843252,0.00001540818,0.000057209338,0.00051989174,0.0056607863,0.0014686474,0.00013546857,0.000042494477],"about_ca_topic_score_codex":0.003353762,"about_ca_topic_score_gemma":0.0011820539,"teacher_disagreement_score":0.31156284,"about_ca_system_score_codex":3.1464322e-7,"about_ca_system_score_gemma":0.000005424901,"threshold_uncertainty_score":0.6266679},"labels":[],"label_agreement":null},{"id":"W2043314288","doi":"10.1103/physrevb.62.9305","title":"Structure and phase transitions of the 6,6-cyclopropane isomer of<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">C</mml:mi></mml:mrow><mml:mrow><mml:mn>61</mml:mn></mml:mrow></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math>","year":2000,"lang":"lv","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Materials Research; University of Pennsylvania; University of Waterloo; State University of New York; U.S. Department of Energy; National Science Foundation","keywords":"Crystallography; Orthorhombic crystal system; Cyclopropane; Physics; Lattice (music); Differential scanning calorimetry; Materials science; Octahedron; Phase transition; Crystal structure; Condensed matter physics; Chemistry; Thermodynamics","score_opus":0.012915518746095353,"score_gpt":0.2392445979459041,"score_spread":0.22632907919980877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043314288","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.29201007,0.004298819,0.0005224765,0.0022057984,0.004263289,0.0001097316,0.0026796574,0.00028267255,0.6936275],"genre_scores_gemma":[0.97104126,0.006347501,0.001985729,0.0061325794,0.0046917163,0.0017855206,0.005281319,0.001525485,0.0012089116],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9790794,0.0017285242,0.004497279,0.003850078,0.0054825908,0.0053621293],"domain_scores_gemma":[0.983557,0.0032416342,0.0047244066,0.005230946,0.00045754548,0.0027884706],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"category_scores_codex":[0.0037517135,0.0021326113,0.0010062642,0.0010558191,0.0031363708,0.003112541,0.005151977,0.004065268,0.97639906],"category_scores_gemma":[0.0020171832,0.004084031,0.004500502,0.0029555932,0.0050955727,0.0036864183,0.0028022202,0.0036503717,0.0057056937],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003808444,0.0009227494,0.000035719382,0.006390635,0.004280007,0.0030284415,0.0037543823,0.0020119748,0.014627641,0.0995372,0.85716975,0.004433046],"study_design_scores_gemma":[0.004253034,0.0029761347,0.00052594504,0.0041151987,0.0055696797,0.0032623196,0.0015689868,0.0077537335,0.95134336,0.00019061945,0.01452571,0.0039152615],"about_ca_topic_score_codex":0.004825768,"about_ca_topic_score_gemma":0.0037066815,"teacher_disagreement_score":0.9706934,"about_ca_system_score_codex":0.00001780521,"about_ca_system_score_gemma":0.0032959438,"threshold_uncertainty_score":0.9991415},"labels":[],"label_agreement":null},{"id":"W2043400417","doi":"10.1021/jp906261s","title":"Pressure-Induced Transformations in Diborane: A Raman Spectroscopic Study","year":2009,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Diborane; Raman spectroscopy; Chemistry; Molecule; Phase (matter); Crystallography; Boranes; Boron; Organic chemistry; Physics","score_opus":0.008860364268945695,"score_gpt":0.240199896879451,"score_spread":0.23133953261050533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043400417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99775505,0.000057844867,0.000010302192,0.0002786169,0.00004623307,0.000111652895,0.000009033447,0.000005809004,0.0017254379],"genre_scores_gemma":[0.99951816,0.00000662277,0.000007918367,0.000025907491,0.00039309537,2.0998381e-7,0.0000027443302,0.0000015352551,0.000043839555],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99920094,0.00006984731,0.0002507862,0.000062996274,0.00025361124,0.00016184711],"domain_scores_gemma":[0.999568,0.00007237054,0.00012779419,0.00013326912,0.000033442902,0.000065117485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002844266,0.000097492535,0.00022684157,0.000014986407,0.00006222059,0.000038554987,0.0002978207,0.000023170789,0.00021185039],"category_scores_gemma":[0.000014484689,0.00005797061,0.00005786799,0.0001298503,0.00001978821,0.00016214944,0.0000034321417,0.00021002465,0.000015522864],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003342095,0.0009646544,0.002589879,0.00005824231,0.00010126184,0.000036465462,0.007955043,0.0073513184,0.9773452,0.000042839412,0.00020088033,0.003019981],"study_design_scores_gemma":[0.0029922652,0.0020551286,0.6410573,0.00010661535,0.00040690476,0.000040440013,0.0010137617,0.003997559,0.33913094,0.008024606,0.000744683,0.00042976116],"about_ca_topic_score_codex":0.0001093921,"about_ca_topic_score_gemma":0.00001923018,"teacher_disagreement_score":0.63846743,"about_ca_system_score_codex":0.000002479433,"about_ca_system_score_gemma":0.00003422179,"threshold_uncertainty_score":0.23639728},"labels":[],"label_agreement":null},{"id":"W2043500097","doi":"10.1029/2002jb001951","title":"Linearized inverse scattering of teleseismic waves for anisotropic crust and mantle structure: 2. Numerical examples and application to data from Canadian stations","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Anisotropy; Geology; Crust; Mantle (geology); Isotropy; Coda; Seismology; Azimuth; Geophysics; Scattering; Shear waves; Normal moveout; Shear (geology); Seismic anisotropy; Physics; Petrology; Optics","score_opus":0.04097726588591492,"score_gpt":0.30236853207524256,"score_spread":0.2613912661893276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043500097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957565,0.0001940722,0.002385422,0.0002734579,0.00006702716,0.00024002125,0.001038627,0.0000023727248,0.000042499687],"genre_scores_gemma":[0.9814192,0.00007081194,0.018198753,0.00004197931,0.00016616385,0.0000013605835,0.000075022785,0.0000053740573,0.000021356243],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99883336,0.00011113365,0.00026169137,0.00021092755,0.0003024989,0.00028041823],"domain_scores_gemma":[0.9985642,0.00055303995,0.00010105805,0.00022179805,0.00018981948,0.0003701033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003269188,0.00009151586,0.0002576495,0.000030755353,0.00016863267,0.00011110103,0.00026918473,0.000042752912,0.00030601813],"category_scores_gemma":[0.0003639674,0.00007171221,0.000023046643,0.00016711207,0.0001372913,0.00022711499,0.00003969841,0.00013687839,0.000007685068],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022361076,0.00038328607,0.14541157,0.0007420518,0.00098883,0.000078902434,0.0032886004,0.0077979066,0.5365193,0.006958234,0.023983153,0.27161208],"study_design_scores_gemma":[0.0016863645,0.0011937782,0.8457487,0.00010302588,0.0000974465,0.000013169233,0.0009826438,0.04915767,0.007948956,0.044165682,0.0485189,0.00038361037],"about_ca_topic_score_codex":0.14861423,"about_ca_topic_score_gemma":0.05135949,"teacher_disagreement_score":0.7003372,"about_ca_system_score_codex":0.000007159564,"about_ca_system_score_gemma":0.00023875054,"threshold_uncertainty_score":0.9659507},"labels":[],"label_agreement":null},{"id":"W2043772661","doi":"10.1029/2001jb001646","title":"Equation of state of liquid Fe‐10 wt % S: Implications for the metallic cores of planetary bodies","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Ontario","keywords":"Materials science; Equation of state; Mantle (geology); Extrapolation; Thermodynamics; Inner core; Core–mantle boundary; Outer core; Analytical Chemistry (journal); Isothermal process; Metal; Intermetallic; Mineralogy; Chemistry; Physics; Composite material; Metallurgy; Geophysics","score_opus":0.06818059425981572,"score_gpt":0.32303528347400917,"score_spread":0.25485468921419346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043772661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99658316,0.0016793968,0.00034603523,0.00026991905,0.00011432523,0.00030851422,0.00031731112,0.0000025754716,0.00037873627],"genre_scores_gemma":[0.99762946,0.00046597523,0.0015143139,0.000008286286,0.00011434753,0.0000033539138,0.00001774066,0.0000053247277,0.00024118039],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99794227,0.00030787662,0.0006642548,0.00012471463,0.0006609377,0.00029996785],"domain_scores_gemma":[0.9952124,0.0029209075,0.00056698587,0.00025311016,0.00094133965,0.00010525677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014689948,0.00011212217,0.00044992944,0.000028733259,0.00012623721,0.000028629895,0.00044110377,0.00003951452,0.00043902438],"category_scores_gemma":[0.00081903994,0.00006719668,0.00019053437,0.00022991624,0.0003809985,0.00019176023,0.000021749709,0.00016342636,0.0000105073],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.015075601,0.002105704,0.036113895,0.0023581039,0.0043445523,0.00001811264,0.0035037945,0.046821054,0.7078674,0.060874727,0.021300942,0.09961612],"study_design_scores_gemma":[0.0016561523,0.009774203,0.59707636,0.00025494478,0.00031955057,0.00001127197,0.0006150158,0.002323819,0.20244937,0.16705547,0.018122643,0.00034119075],"about_ca_topic_score_codex":0.0017876492,"about_ca_topic_score_gemma":0.0003475361,"teacher_disagreement_score":0.5609625,"about_ca_system_score_codex":0.0000038638223,"about_ca_system_score_gemma":0.00024725808,"threshold_uncertainty_score":0.4807009},"labels":[],"label_agreement":null},{"id":"W2043967560","doi":"10.1016/j.commatsci.2012.05.040","title":"A modified Morse potential accounting for non-zero temperature in molecular statics for Nickel crystals","year":2012,"lang":"en","type":"article","venue":"Computational Materials Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Statics; Nickel; Interatomic potential; Molecular dynamics; Morse potential; Thermodynamics; Morse code; Zero (linguistics); Materials science; Thermal; Crystal (programming language); Thermal expansion; Stress (linguistics); Chemistry; Statistical physics; Computational chemistry; Physics; Metallurgy; Classical mechanics; Atomic physics","score_opus":0.011454349815313365,"score_gpt":0.24199898270471076,"score_spread":0.2305446328893974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043967560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95982707,0.000029687375,0.03685208,0.00007775063,0.001510472,0.00069995574,0.00093218655,0.000018944074,0.000051880783],"genre_scores_gemma":[0.9645167,0.0000013365463,0.03468673,0.00017176059,0.00024349715,0.000027437942,0.00032304515,0.0000069663456,0.000022533726],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99837273,0.000034708155,0.00036215378,0.00030343197,0.0003662533,0.0005607031],"domain_scores_gemma":[0.9992383,0.00015863864,0.00015588888,0.00012358787,0.00020589505,0.000117686766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012604815,0.00015687374,0.0002462167,0.000128154,0.00027944188,0.0003834604,0.0003256433,0.000057899408,0.00007769044],"category_scores_gemma":[0.00011827503,0.00013809287,0.000041125382,0.0002348303,0.00014595248,0.0006891695,0.00003195912,0.000033095504,0.00002032396],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008468133,0.00003881467,0.00043639453,0.00010679136,0.000007150016,0.0000016955544,0.0002452938,0.26020783,0.7344761,0.004052423,0.00015361303,0.00018925568],"study_design_scores_gemma":[0.0041597793,0.00042669848,0.19882086,0.0002058991,0.00009651246,0.00003383387,0.00026319583,0.28820443,0.38120648,0.124221444,0.00066955213,0.0016913185],"about_ca_topic_score_codex":0.00011445752,"about_ca_topic_score_gemma":0.000006190548,"teacher_disagreement_score":0.3532696,"about_ca_system_score_codex":0.00000899243,"about_ca_system_score_gemma":0.0001780608,"threshold_uncertainty_score":0.56312644},"labels":[],"label_agreement":null},{"id":"W2044201246","doi":"10.1016/j.rgg.2012.08.001","title":"Structure of the upper mantle in the Circum-Arctic region from regional seismic tomography","year":2012,"lang":"en","type":"article","venue":"Russian Geology and Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Seismic tomography; Subduction; Seismology; Mantle (geology); Mantle plume; Arctic; Rift; Precambrian; Crust; Geophysics; Paleontology; Tectonics; Oceanography","score_opus":0.007646569028716254,"score_gpt":0.18534779877216198,"score_spread":0.17770122974344574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044201246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970094,0.0006207459,0.000010744854,0.0011842278,0.00046305681,0.00012867317,0.00006707988,0.0000055758883,0.0005105113],"genre_scores_gemma":[0.9987267,0.000041725474,0.000034039116,0.0007813093,0.00031715442,9.26911e-7,0.000059808288,0.0000026491157,0.000035661764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99911517,0.00018714642,0.00014905851,0.00015466652,0.00012716926,0.00026680675],"domain_scores_gemma":[0.9994459,0.00013031322,0.0001015177,0.00027256607,0.000010093124,0.00003959618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009585419,0.00012048358,0.00017549009,0.000030562325,0.00013211703,0.000014766215,0.00024868216,0.00010449766,0.00017524484],"category_scores_gemma":[0.0000053040894,0.00006568593,0.00006198927,0.00017774307,0.0002458201,0.0001285038,0.000023239543,0.00016136722,0.000017154372],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003076795,0.000028216265,0.98377347,0.000023029183,0.000032376345,0.00000259455,0.0017372452,0.00008197347,0.0002800509,0.012455654,0.00024820518,0.0013064371],"study_design_scores_gemma":[0.00013992783,0.000022234137,0.92899066,0.000012716147,0.000025744328,0.0000128627935,0.00011650407,0.00005843059,0.00010677459,0.068673216,0.0017576375,0.000083298575],"about_ca_topic_score_codex":0.004284031,"about_ca_topic_score_gemma":0.00043505046,"teacher_disagreement_score":0.056217566,"about_ca_system_score_codex":9.267454e-7,"about_ca_system_score_gemma":0.000017428538,"threshold_uncertainty_score":0.6476202},"labels":[],"label_agreement":null},{"id":"W2044512437","doi":"10.1016/j.jnucmat.2010.11.019","title":"Thermo-oxidation of DIII-D codeposits on open surfaces and in simulated tile gaps","year":2010,"lang":"en","type":"article","venue":"Journal of Nuclear Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"DIII-D; Tile; Nuclear engineering; Radiochemistry; Materials science; Environmental science; Chemistry; Physics; Nuclear physics; Composite material; Tokamak; Engineering; Plasma","score_opus":0.00984851232777752,"score_gpt":0.2286520154113303,"score_spread":0.21880350308355276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044512437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984554,0.0000176934,6.808665e-8,0.00009901049,0.00068475946,0.00011913629,0.00006395196,0.0000033068322,0.0005566425],"genre_scores_gemma":[0.9996168,0.00004732331,0.00016141226,0.000055291675,0.00008841234,5.3435755e-8,0.0000075744374,0.00000515724,0.00001798759],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991882,0.00008014856,0.00039133447,0.00008634442,0.00014715802,0.00010681736],"domain_scores_gemma":[0.99938565,0.000060029244,0.00035837767,0.00009576925,0.000054892145,0.000045281242],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006475231,0.000081617734,0.0003065768,0.00006105003,0.000037750193,0.00016746389,0.00023663855,0.00006428586,0.002448719],"category_scores_gemma":[0.000042459393,0.00005817631,0.00001810311,0.000051240408,0.000035010577,0.00029081447,0.000025963636,0.000068676476,0.000032105345],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038176976,0.000028647455,0.0021025394,0.00002054452,0.0000141138935,0.000009065824,0.00015251043,0.0004060932,0.99623907,0.000060417184,0.00014575846,0.00043947558],"study_design_scores_gemma":[0.0006281515,0.0003102779,0.8227148,0.00008529254,0.000016853312,0.000014932797,0.000029808698,0.00007852717,0.1737305,0.00047182958,0.0018184929,0.00010052741],"about_ca_topic_score_codex":0.000889594,"about_ca_topic_score_gemma":0.00016629163,"teacher_disagreement_score":0.8225086,"about_ca_system_score_codex":0.0000010900096,"about_ca_system_score_gemma":0.0000180673,"threshold_uncertainty_score":0.99846315},"labels":[],"label_agreement":null},{"id":"W2045064400","doi":"10.1139/e09-059","title":"Thermal regime of the lithosphere in the Canadian ShieldThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Lithosphere; Mantle (geology); Geothermal gradient; Geology; Crust; Heat flow; Geophysics; Earth's internal heat budget; Shield; Basin and Range Province; Heat generation; Seismic refraction; Petrology; Thermal; Tectonics; Seismology; Mantle wedge; Thermodynamics","score_opus":0.00875305441685488,"score_gpt":0.17718491727916563,"score_spread":0.16843186286231077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045064400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97953707,0.00033235594,1.1730847e-7,0.011248052,0.00029657612,0.00024236024,0.00007065891,4.5382058e-7,0.008272362],"genre_scores_gemma":[0.99946994,0.000021728703,0.00007326574,0.00022675787,0.00013443023,9.300249e-7,3.7427537e-7,0.0000016311083,0.000070917886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985629,0.00023258121,0.00043846882,0.00011481767,0.00039550636,0.0002557605],"domain_scores_gemma":[0.9987362,0.0003236175,0.000460902,0.00021222417,0.00015644607,0.00011061561],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026624575,0.00009190008,0.00026249807,0.00010436148,0.00020173534,0.00010578263,0.0007560265,0.000056283294,0.0023486293],"category_scores_gemma":[0.00051327277,0.000039167993,0.00005818279,0.0007194431,0.001699786,0.00028353735,0.000009154011,0.00023005501,7.8592916e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043818814,0.00007347265,0.905803,0.00017763514,0.0000930722,0.00001518661,0.060473047,0.001196103,0.0046812603,0.022004563,0.0017103789,0.0033340843],"study_design_scores_gemma":[0.0006499572,0.0004128286,0.9681002,0.00026894233,0.000040515904,0.000017418957,0.0069679637,0.00013001534,0.011770516,0.0047507705,0.006759452,0.0001314355],"about_ca_topic_score_codex":0.6187836,"about_ca_topic_score_gemma":0.9760853,"teacher_disagreement_score":0.35730174,"about_ca_system_score_codex":0.0000026818427,"about_ca_system_score_gemma":0.0017852847,"threshold_uncertainty_score":0.99856335},"labels":[],"label_agreement":null},{"id":"W2046306977","doi":"10.1007/s00024-010-0100-6","title":"On the Causes of Frequency-Dependent Apparent Seismological Q","year":2010,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Attenuation; Attenuation coefficient; Residual; Physics; Crust; Absorption (acoustics); Order (exchange); Frequency band; Geology; Computational physics; Seismology; Geodesy; Optics; Mathematics; Geophysics; Telecommunications; Algorithm; Computer science","score_opus":0.010463147614898633,"score_gpt":0.19470011188776754,"score_spread":0.1842369642728689,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046306977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914382,0.00002381675,0.000021833273,0.00024269885,0.00029037273,0.00017774919,0.00011731035,0.000019002986,0.0076690246],"genre_scores_gemma":[0.99922854,0.000015056009,0.00007805242,0.00036345632,0.00021106722,0.000005559624,0.000033866512,0.0000031266095,0.000061283856],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99924624,0.000019963692,0.00014425794,0.00019969889,0.00019932717,0.00019049397],"domain_scores_gemma":[0.9994411,0.00017063062,0.00008016764,0.00022632901,0.00002061615,0.00006116988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014073963,0.00013213303,0.00018588331,0.000013594294,0.00012698726,0.000044298416,0.00018417946,0.00006862702,0.00054226234],"category_scores_gemma":[0.000009693711,0.00007425557,0.000034178014,0.00006682277,0.00012778425,0.000032492353,0.000021811356,0.00017984639,0.00011964219],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009376269,0.00016276473,0.0054057203,0.00006453137,0.00008847673,0.000009249396,0.0005767555,0.00037801257,0.102397375,0.8676382,0.0010261696,0.022159021],"study_design_scores_gemma":[0.00048171807,0.00030830398,0.20177643,0.000016709677,0.00008675453,0.0000065958257,0.00014686183,0.000099140765,0.05168561,0.7387099,0.0061593936,0.00052256905],"about_ca_topic_score_codex":0.00039494428,"about_ca_topic_score_gemma":0.00011545762,"teacher_disagreement_score":0.19637072,"about_ca_system_score_codex":4.0552968e-7,"about_ca_system_score_gemma":0.000017163075,"threshold_uncertainty_score":0.5937392},"labels":[],"label_agreement":null},{"id":"W2048246159","doi":"10.1139/e05-002","title":"Geophysical transect across a Paleoproterozoic continentcontinent collision zone: The Trans-Hudson Orogen","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Geological Survey of Canada","funders":"","keywords":"Geology; Lithosphere; Bouguer anomaly; Craton; Mantle (geology); Collision zone; Geophysics; Seismology; Archean; Gravity anomaly; Crust; Magnetotellurics; Tectonics; Geochemistry; Paleontology; Electrical resistivity and conductivity","score_opus":0.01403909613216625,"score_gpt":0.22253763056999462,"score_spread":0.20849853443782837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048246159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99393815,0.0008395295,0.00014947087,0.0034049626,0.0007789496,0.00019278213,0.00014318604,0.0000058844666,0.0005470817],"genre_scores_gemma":[0.9982902,0.000043522923,0.00040963563,0.00034431988,0.00071895606,7.7496145e-7,0.0000044338026,0.0000033297626,0.00018482223],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981505,0.00012789159,0.00042859875,0.00020524574,0.00045350916,0.00063425436],"domain_scores_gemma":[0.99886644,0.00011063436,0.00021208418,0.00014341829,0.0001430091,0.0005244047],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012576025,0.00016274762,0.0002896996,0.00008565269,0.0007639426,0.00043389565,0.00070335163,0.000057014313,0.0010253732],"category_scores_gemma":[0.00004376419,0.000095920084,0.00014404867,0.00043634092,0.0005157243,0.00048330228,0.0000038008689,0.00017945333,0.000077459335],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003609559,0.00017242429,0.68451977,0.000121799094,0.00039469518,0.0005571171,0.03627098,0.066545375,0.017224755,0.0018363588,0.005826407,0.18616936],"study_design_scores_gemma":[0.00080720324,0.00061696634,0.75819343,0.000095188094,0.000050121547,0.00016224253,0.0006811273,0.0015180457,0.005287683,0.00022883821,0.23201732,0.00034183727],"about_ca_topic_score_codex":0.021362582,"about_ca_topic_score_gemma":0.42430478,"teacher_disagreement_score":0.4029422,"about_ca_system_score_codex":0.0000016081704,"about_ca_system_score_gemma":0.00065852865,"threshold_uncertainty_score":0.9998878},"labels":[],"label_agreement":null},{"id":"W2049366686","doi":"10.1038/416310a","title":"Development of anisotropic structure in the Earth's lower mantle by solid-state convection","year":2002,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; National Science Foundation","keywords":"Mantle (geology); Anisotropy; Geology; Isotropy; Subduction; Mantle convection; Core–mantle boundary; Seismic anisotropy; Slab; Geophysics; Homogeneous; Hotspot (geology); Petrology; Seismology; Physics; Tectonics; Optics; Thermodynamics","score_opus":0.005895451752923291,"score_gpt":0.20041900394477782,"score_spread":0.19452355219185452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049366686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974189,0.00042439392,0.0000049894425,0.00012196689,0.0004470509,0.000099442805,0.00042008696,0.000008070706,0.0010551361],"genre_scores_gemma":[0.9987942,0.000022799577,0.00035202884,0.0002454997,0.000050537317,5.4741724e-7,0.00013253432,0.0000017947574,0.00040004175],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99940896,0.00003612691,0.00012558603,0.00011474576,0.00017688061,0.00013769534],"domain_scores_gemma":[0.99978447,0.000026313694,0.000050589966,0.00009991741,0.000018416826,0.000020304164],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000068574715,0.000075735836,0.00010248144,0.000023549688,0.000058592705,0.000027201855,0.00013962825,0.0001901727,0.0061025424],"category_scores_gemma":[0.000007258266,0.000046973822,0.000016672053,0.00010960947,0.000020202751,0.00006636732,0.0000052232417,0.00031648797,0.000062056686],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033382588,0.00045724283,0.061859608,0.00047802157,0.00028819544,0.00016237078,0.026582614,0.0025156676,0.22612952,0.0009564618,0.4926144,0.1876221],"study_design_scores_gemma":[0.00040634503,0.000078210614,0.2550429,0.000025670415,0.000009354588,0.000007028079,0.0001045596,0.0004591516,0.024004381,0.00062955735,0.7190105,0.00022236536],"about_ca_topic_score_codex":0.00006698314,"about_ca_topic_score_gemma":0.0009190773,"teacher_disagreement_score":0.22639608,"about_ca_system_score_codex":0.0000011171861,"about_ca_system_score_gemma":0.000010075791,"threshold_uncertainty_score":0.994806},"labels":[],"label_agreement":null},{"id":"W2049950941","doi":"10.1063/1.3098140","title":"An electron-preceding perspective on the deformation of materials","year":2009,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Eigenvalues and eigenvectors; Tensor (intrinsic definition); Density functional theory; Cauchy stress tensor; Electron; Derivative (finance); Matrix (chemical analysis); Electron density; Electronic structure; Density matrix; Quantum mechanics; Physics; Chemistry; Condensed matter physics; Computational chemistry; Mathematics; Geometry; Quantum","score_opus":0.010023198483632877,"score_gpt":0.23540396278726108,"score_spread":0.22538076430362822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049950941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998027,0.000026885626,0.000045844743,0.00052296073,0.00011079545,0.00005438757,0.000011366607,0.0000035765518,0.0011971615],"genre_scores_gemma":[0.99922997,0.000018288642,0.000039599552,0.000155739,0.000547915,5.874453e-8,0.000004425149,0.0000016360625,0.0000023904136],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993315,0.000065541346,0.00021596893,0.00004076844,0.000228297,0.00011797804],"domain_scores_gemma":[0.99934554,0.00010118312,0.00029428717,0.00011854245,0.00010716308,0.000033293778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047422523,0.00007260809,0.00015808965,0.000009076374,0.000080497215,0.00005208643,0.00029050995,0.000024281517,0.00006515105],"category_scores_gemma":[0.000022189848,0.000033683875,0.000043326832,0.00007126061,0.00004159966,0.00020050666,0.0000035682913,0.00010650255,0.000009775667],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020404003,0.00003139361,0.0000129165155,0.0000032304818,0.00001947386,2.5032125e-7,0.00075834827,0.0009541818,0.99225336,0.0048882174,0.0002513249,0.0006232561],"study_design_scores_gemma":[0.000089388595,0.00027924989,0.00085331564,0.000016951999,0.000028516391,0.000004727038,0.00014703759,0.000103496415,0.92448914,0.07392024,0.000023812428,0.0000441184],"about_ca_topic_score_codex":0.000064277876,"about_ca_topic_score_gemma":8.347517e-7,"teacher_disagreement_score":0.06903203,"about_ca_system_score_codex":0.0000059208305,"about_ca_system_score_gemma":0.000021375652,"threshold_uncertainty_score":0.13735884},"labels":[],"label_agreement":null},{"id":"W2050164221","doi":"10.1088/0953-8984/14/44/396","title":"First-principles studies of pressure-induced phase transitions in SiO<sub>2</sub>","year":2002,"lang":"en","type":"article","venue":"Journal of Physics Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Assertion; Softening; Structural stability; Work (physics); Phase transition; Space (punctuation); Phase (matter); Stability (learning theory); Materials science; Condensed matter physics; Crystallography; Physics; Thermodynamics; Chemistry; Engineering; Structural engineering; Computer science; Quantum mechanics; Composite material","score_opus":0.04929392370684062,"score_gpt":0.25839335630981053,"score_spread":0.20909943260296993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050164221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99774384,0.00050670316,0.00006536514,0.0006704007,0.0004237867,0.00011731054,0.00011711424,0.0000055695045,0.00034992953],"genre_scores_gemma":[0.9992524,0.0000977442,0.00013042185,0.00019582883,0.0002732736,9.849351e-7,0.0000052324785,0.000006963473,0.00003714929],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99863327,0.00009277354,0.00059891865,0.00013812496,0.00031025033,0.000226644],"domain_scores_gemma":[0.99900985,0.00013847907,0.0004211251,0.00016665498,0.00018414794,0.00007976576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024083567,0.00016206285,0.00050431,0.00009650699,0.00007037742,0.00003448407,0.0001891278,0.00005495003,0.00078117015],"category_scores_gemma":[0.000020490828,0.000130694,0.00014446862,0.00015406345,0.00007826715,0.0003356656,0.000011934434,0.00016872317,0.00011189963],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028950945,0.0008710427,0.0066958475,0.0006303203,0.0008596555,0.0001679711,0.007851945,0.039746203,0.92981523,0.00042155426,0.008563086,0.0040876535],"study_design_scores_gemma":[0.012655002,0.0021468196,0.095362544,0.0012730368,0.0011112404,0.00013443545,0.0014288075,0.016074099,0.8434044,0.01925198,0.0057471753,0.0014104383],"about_ca_topic_score_codex":0.000030585656,"about_ca_topic_score_gemma":0.00009383938,"teacher_disagreement_score":0.08866669,"about_ca_system_score_codex":0.0000036955007,"about_ca_system_score_gemma":0.000023196935,"threshold_uncertainty_score":0.85532653},"labels":[],"label_agreement":null},{"id":"W2050515251","doi":"10.1139/e05-028","title":"Constraints on the composition of the crust and uppermost mantle in northwestern Canada: <i>Vp</i>/<i>Vs</i> variations along Lithoprobe's SNorCLE transect","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Terrane; Craton; Crust; Foreland basin; Mantle (geology); Mafic; Continental crust; Crustal recycling; Seismic refraction; Seismology; Geochemistry; Tectonics","score_opus":0.01069680597234208,"score_gpt":0.18039242210153628,"score_spread":0.1696956161291942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050515251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99438703,0.00012635424,0.00000766528,0.0036790024,0.0003320984,0.00010075337,0.00020918708,7.828273e-7,0.0011571313],"genre_scores_gemma":[0.99916756,0.000011394792,0.00008418938,0.0006427612,0.00007456596,2.1926235e-7,0.000002082897,0.0000012138988,0.000016025411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909186,0.00010144214,0.0002589763,0.0000956464,0.00023562624,0.00021646106],"domain_scores_gemma":[0.99941885,0.00013829391,0.00015290703,0.00008187034,0.000048722093,0.00015935673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055719056,0.000073458155,0.00013402976,0.00006899229,0.000340885,0.000092872135,0.00028569222,0.000023195607,0.00039612528],"category_scores_gemma":[0.000019577017,0.00004189666,0.000030412368,0.00023018915,0.00041303883,0.0001729137,0.0000031167194,0.000104652,0.0000022012014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026954194,0.000019206776,0.9598451,0.000019587522,0.000029938044,0.000046751655,0.0027740202,0.023460593,0.0015072477,0.0021672742,0.00040195428,0.0097013265],"study_design_scores_gemma":[0.00013565578,0.000077987395,0.9965588,0.000067120774,0.000009353458,0.00004742206,0.00018149763,0.00041305117,0.00081450585,0.000113766655,0.001516979,0.00006389916],"about_ca_topic_score_codex":0.6796844,"about_ca_topic_score_gemma":0.9956383,"teacher_disagreement_score":0.3159539,"about_ca_system_score_codex":0.0000029465784,"about_ca_system_score_gemma":0.0014723603,"threshold_uncertainty_score":0.4337294},"labels":[],"label_agreement":null},{"id":"W2050822222","doi":"10.1007/s00269-011-0465-9","title":"The pressure-induced ringwoodite to Mg-perovskite and periclase post-spinel phase transition: a Bader’s topological analysis of the ab initio electron densities","year":2011,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute of Steel Construction","keywords":"Ringwoodite; Periclase; Spinel; Chemistry; Density functional theory; Ab initio; Topology (electrical circuits); Perovskite (structure); Phase transition; Ab initio quantum chemistry methods; Atoms in molecules; Stishovite; Condensed matter physics; Olivine; Computational chemistry; Thermodynamics; Molecule; Crystallography; Physics; Materials science; Mineralogy; High pressure; Metallurgy","score_opus":0.021053939178289995,"score_gpt":0.2299245969545195,"score_spread":0.2088706577762295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050822222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980994,0.0003194145,0.000012584538,0.00022039037,0.000034533306,0.00009427919,0.00034496887,0.0000061945457,0.0008682256],"genre_scores_gemma":[0.99954057,0.000061466126,0.000040856085,0.000095758405,0.00009291139,0.0000031632933,0.000039140767,0.0000026515888,0.00012347163],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99924755,0.000036779264,0.00021281705,0.00018393388,0.0001469058,0.00017199958],"domain_scores_gemma":[0.9994767,0.00006128061,0.0001161579,0.0001920915,0.00008238226,0.000071401104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011637326,0.00013011738,0.00028433354,0.000012145041,0.00014725165,0.00003368072,0.00014317605,0.000045001125,0.0001229744],"category_scores_gemma":[0.000014451826,0.000077571276,0.0000912097,0.00015709751,0.00016136626,0.000061412036,0.000021441789,0.000063839805,5.366662e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015584998,0.00007596775,0.0005704421,0.000087466404,0.00038516909,0.0000017244017,0.0018784232,0.0001281721,0.9954128,0.00024767243,0.00007551717,0.0009807709],"study_design_scores_gemma":[0.00081846304,0.00037739685,0.046844374,0.000042563348,0.0013120918,0.0000075207336,0.00061224564,0.002423934,0.94460016,0.0018317901,0.0007731173,0.0003563464],"about_ca_topic_score_codex":0.00081099756,"about_ca_topic_score_gemma":0.00006431229,"teacher_disagreement_score":0.05081267,"about_ca_system_score_codex":8.39039e-7,"about_ca_system_score_gemma":0.00001938323,"threshold_uncertainty_score":0.31632647},"labels":[],"label_agreement":null},{"id":"W2050910020","doi":"10.1103/physrevb.87.064408","title":"Magnetic ordering in nanocrystalline gadolinium: A neutron diffraction study","year":2013,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies; Fonds National de la Recherche Luxembourg","keywords":"Gadolinium; Nanocrystalline material; Neutron diffraction; Materials science; Crystallite; Magnetization; Condensed matter physics; Magnetic moment; Nuclear magnetic resonance; Order (exchange); Diffraction; Crystallography; Physics; Magnetic field; Optics; Chemistry; Nanotechnology","score_opus":0.012925326751455569,"score_gpt":0.25573773962333757,"score_spread":0.242812412871882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050910020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99462676,0.0033214216,0.0000025682414,0.00020841263,0.00015076177,0.00078768155,0.0000059425056,0.000024270825,0.00087217666],"genre_scores_gemma":[0.9973667,0.0020651855,0.000033745495,0.00020573538,0.00021217868,0.000025577483,0.000019593028,0.0000042189627,0.00006706787],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99901545,0.0001169971,0.00023511572,0.00022709623,0.00017482339,0.00023049621],"domain_scores_gemma":[0.9995868,0.00006694531,0.0000546886,0.00018901435,0.000026553762,0.00007595463],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014440742,0.00012991365,0.0003425109,0.000021844535,0.000036862748,0.000047757527,0.00013382509,0.000013540757,0.0018037179],"category_scores_gemma":[0.00002832455,0.00009502318,0.00005061238,0.00018249615,0.000016268381,0.00021179472,0.000016731841,0.00009728352,0.0014268119],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001370693,0.0053113867,0.18563794,0.0071752323,0.00013236146,0.00010298408,0.0017466233,0.0045148777,0.10615813,0.00078305247,0.0043761996,0.68392414],"study_design_scores_gemma":[0.0003044368,0.00038747938,0.9880646,0.00033200407,0.00004254613,0.0000012259471,0.000028767688,0.003222185,0.000036972626,0.0011438787,0.0062173484,0.00021859378],"about_ca_topic_score_codex":0.004682187,"about_ca_topic_score_gemma":0.00053806196,"teacher_disagreement_score":0.80242664,"about_ca_system_score_codex":0.0000023149885,"about_ca_system_score_gemma":0.000011545209,"threshold_uncertainty_score":0.99935067},"labels":[],"label_agreement":null},{"id":"W2052251912","doi":"10.1016/s0031-9201(01)00194-7","title":"S-wave velocity structure of the Canadian upper mantle","year":2001,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Craton; Mantle (geology); Seismology; Rift; Crust; Keel; Shield; Geophysics; Transition zone; Paleontology; Tectonics; Oceanography","score_opus":0.009494658521361212,"score_gpt":0.17379351000891,"score_spread":0.16429885148754877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052251912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958617,0.00010926949,0.0000014165761,0.00022650849,0.00066154473,0.00013436965,0.0012640589,0.0000040338264,0.0017370854],"genre_scores_gemma":[0.99939007,0.000027214839,0.00006593623,0.00017145333,0.00012267125,1.0632496e-7,0.00007093692,0.0000028548718,0.00014876969],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99926007,0.00006564363,0.00016597069,0.0001301818,0.0001700995,0.0002080619],"domain_scores_gemma":[0.9994552,0.000038551687,0.00011886094,0.0002740732,0.000026624966,0.00008665299],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006223343,0.00012272329,0.00019254454,0.000019162982,0.00016950659,0.000026323214,0.000280805,0.000052267987,0.00078770955],"category_scores_gemma":[0.00000902297,0.00006841779,0.00006933678,0.000106593274,0.00016876515,0.000079323596,0.000029176306,0.00011934873,0.00001066663],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014267841,0.00001911107,0.96295375,0.00014730213,0.00019015705,0.000009057398,0.0013697821,0.0033831445,0.010126214,0.00070738513,0.0010745075,0.019876938],"study_design_scores_gemma":[0.000116579984,0.000040586037,0.9817662,0.00004246841,0.000033625573,0.00001672642,0.000028645287,0.0007117843,0.007897741,0.0034696788,0.005759791,0.00011613362],"about_ca_topic_score_codex":0.1986753,"about_ca_topic_score_gemma":0.32569894,"teacher_disagreement_score":0.12702365,"about_ca_system_score_codex":0.0000011940053,"about_ca_system_score_gemma":0.00007340487,"threshold_uncertainty_score":0.8624867},"labels":[],"label_agreement":null},{"id":"W2052341392","doi":"10.1016/j.tecto.2006.01.016","title":"Effects of trench-zone scattering on receiver functions over a subduction zone: A 3-D finite-difference modelling study","year":2006,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Trench; Scattering; Receiver function; Amplitude; Crust; Mantle (geology); Underplating; Coda; Waveform; Geophysics; Tectonics; Lithosphere; Optics; Physics","score_opus":0.010205363172445298,"score_gpt":0.19309085021998917,"score_spread":0.18288548704754387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052341392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901646,0.000039790884,0.008143606,0.000009189226,0.00059519685,0.00036432073,0.000065318985,0.00007320263,0.0005447796],"genre_scores_gemma":[0.99885523,0.0000075764706,0.00019426957,0.000015244448,0.00036322916,0.000009426687,0.00006337269,0.0000090283975,0.00048264614],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9987894,0.00007875576,0.0002601345,0.00033337742,0.00027828594,0.00026002526],"domain_scores_gemma":[0.9992766,0.00021236528,0.00015045195,0.0002664731,0.000046209654,0.000047934234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097760625,0.00020611928,0.00030242826,0.00009110957,0.00015703392,0.000053733627,0.00014302148,0.000053150023,0.00015850257],"category_scores_gemma":[0.0000064697133,0.00018073928,0.00007356115,0.00029242388,0.00005254262,0.00014664435,0.000015544487,0.00012000285,0.00012710108],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031966972,0.0012198159,0.015569473,0.00025938608,0.00014676612,0.00002494657,0.00092688436,0.82535833,0.13534427,0.00037949067,0.00025850316,0.02019248],"study_design_scores_gemma":[0.0027841688,0.0026231857,0.82489085,0.00024193639,0.00040943618,0.0000026677205,0.00015363863,0.093930125,0.06816038,0.004871579,0.00075234304,0.0011796991],"about_ca_topic_score_codex":0.010505392,"about_ca_topic_score_gemma":0.00035200137,"teacher_disagreement_score":0.80932134,"about_ca_system_score_codex":0.000006684925,"about_ca_system_score_gemma":0.000022337486,"threshold_uncertainty_score":0.99608374},"labels":[],"label_agreement":null},{"id":"W2053042052","doi":"10.1103/physrevlett.100.205005","title":"Temperature Relaxation in Hot Dense Hydrogen","year":2008,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Physics; Relaxation (psychology); Hydrogen; Range (aeronautics); Condensed matter physics; Atmospheric temperature range; Atomic physics; Electron; Landau quantization; Quantum; Quantum mechanics; Materials science; Thermodynamics","score_opus":0.013041422042538723,"score_gpt":0.2279770155715307,"score_spread":0.21493559352899197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053042052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949921,0.0029845177,0.0000010629301,0.001426823,0.00010640317,0.00020280722,0.00001915735,0.000021029944,0.00024614873],"genre_scores_gemma":[0.9900634,0.0034223085,0.000038343853,0.006127438,0.00024187115,0.000004161929,0.000079862075,0.0000035824582,0.000019008618],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991398,0.00010194465,0.00016577197,0.00020160705,0.00019127205,0.00019960522],"domain_scores_gemma":[0.9996345,0.000056772584,0.00006433807,0.00016742907,0.000011912696,0.00006505301],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011798097,0.00011653093,0.00027173426,0.000022114084,0.00006183035,0.000013449858,0.00012766053,0.0000114755285,0.00021097159],"category_scores_gemma":[0.00002968745,0.00008766652,0.000074531876,0.00019286758,0.000041346942,0.00014675401,0.0000072670196,0.00010797874,0.00064251496],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031837155,0.0006036778,0.13601086,0.0045964792,0.00022340962,0.0015203145,0.002941156,0.023892147,0.6520235,0.0008516229,0.1562733,0.020745153],"study_design_scores_gemma":[0.00082031125,0.00016251752,0.9079691,0.0017543336,0.00011949687,0.00006881182,0.000008139906,0.0024114884,0.00630439,0.000623094,0.07863933,0.0011189725],"about_ca_topic_score_codex":0.0002915438,"about_ca_topic_score_gemma":0.000037542177,"teacher_disagreement_score":0.7719583,"about_ca_system_score_codex":0.0000029335351,"about_ca_system_score_gemma":0.000014437654,"threshold_uncertainty_score":0.8258444},"labels":[],"label_agreement":null},{"id":"W2053774522","doi":"10.1103/physrevlett.98.117004","title":"Novel Superconductivity in Metallic<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:msub><mml:mi>SnH</mml:mi><mml:mn>4</mml:mn></mml:msub></mml:math>under High Pressure","year":2007,"lang":"lv","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":228,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Superconductivity; Coupling (piping); Physics; Condensed matter physics; Fermi surface; Metal; Phonon; Crystallography; Materials science; Chemistry","score_opus":0.021697347751032197,"score_gpt":0.2490417547879118,"score_spread":0.2273444070368796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053774522","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98651904,0.0050775553,0.00037569198,0.0026197908,0.001897641,0.00013859555,0.0007678681,0.00009082426,0.002512989],"genre_scores_gemma":[0.9868814,0.0035484591,0.0008616482,0.005388478,0.0020015696,0.00012953671,0.000986417,0.00013550447,0.00006700365],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.994229,0.00034669545,0.0011471222,0.001285565,0.0014212376,0.0015703497],"domain_scores_gemma":[0.9962507,0.0010067475,0.0007787701,0.001286319,0.00007250393,0.0006049823],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0017127004,0.00070838275,0.0006743168,0.00013686888,0.00056413043,0.0005281176,0.0011719227,0.00040646052,0.0051247035],"category_scores_gemma":[0.00034915633,0.0008860126,0.0009781374,0.00067647686,0.0007019996,0.0012275159,0.00045796973,0.0009816281,0.0024854033],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032851522,0.0005711574,0.000037551665,0.004489789,0.0009847548,0.0004681867,0.0007529473,0.0018312644,0.04349123,0.9293449,0.015454532,0.0022452057],"study_design_scores_gemma":[0.005693664,0.0030454255,0.009681494,0.014988396,0.010596487,0.00083903124,0.00084463344,0.20148471,0.53467405,0.0030935635,0.20680808,0.008250494],"about_ca_topic_score_codex":0.0041025337,"about_ca_topic_score_gemma":0.0010798889,"teacher_disagreement_score":0.9262513,"about_ca_system_score_codex":0.000007465337,"about_ca_system_score_gemma":0.00028812114,"threshold_uncertainty_score":0.9993591},"labels":[],"label_agreement":null},{"id":"W2054207406","doi":"10.1029/2004jb003454","title":"Three‐dimensional numerical simulations of mantle flow beneath mid‐ocean ridges","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Lithosphere; Geology; Mantle (geology); Mantle convection; Geophysics; Ridge; Mid-ocean ridge; Ridge push; Streamlines, streaklines, and pathlines; Convection; Hotspot (geology); Geometry; Mechanics; Seismology; Tectonics; Physics","score_opus":0.02991270680784733,"score_gpt":0.29635713492845384,"score_spread":0.2664444281206065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054207406","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976573,0.00044428426,0.00024356206,0.0006923395,0.00022596515,0.00012081202,0.00014773197,0.000008553342,0.0004594589],"genre_scores_gemma":[0.99172485,0.000027543181,0.00669827,0.000031697073,0.0013103458,2.4173485e-7,0.00001961631,0.00000845239,0.00017898816],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99710685,0.0001930259,0.0005607078,0.00020421803,0.0014341201,0.0005010947],"domain_scores_gemma":[0.9975715,0.0010126643,0.00023414726,0.00023481844,0.00061713165,0.0003297386],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006882718,0.00015965862,0.0004545021,0.00003743246,0.00020859911,0.000079715246,0.00045948286,0.00007882341,0.0033392776],"category_scores_gemma":[0.00027176182,0.00011302803,0.00019853766,0.0003682497,0.00023144127,0.00037723183,0.000057565307,0.00041481556,0.00021411755],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022877452,0.001827435,0.07110868,0.00017613568,0.0007207031,0.0002203054,0.00065467495,0.70162505,0.024184868,0.0017188482,0.04449095,0.15098462],"study_design_scores_gemma":[0.0018979054,0.002763538,0.6507674,0.00021932196,0.00008457695,0.000040482104,0.0001152359,0.27213982,0.016588362,0.026615363,0.028244307,0.000523722],"about_ca_topic_score_codex":0.0016746209,"about_ca_topic_score_gemma":0.0004903649,"teacher_disagreement_score":0.5796587,"about_ca_system_score_codex":0.0000112244825,"about_ca_system_score_gemma":0.00022919697,"threshold_uncertainty_score":0.9975718},"labels":[],"label_agreement":null},{"id":"W2056262142","doi":"10.1029/2007gl029463","title":"On the relative importance of mineral phase transitions and viscosity stratification in controlling the sinking rates of detached slab remnants","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Toronto","funders":"","keywords":"Mantle (geology); Slab; Stratification (seeds); Geology; Viscosity; Transition zone; Phase boundary; Convection; Geophysics; Mantle convection; Mechanics; Mineralogy; Thermodynamics; Phase (matter); Physics; Subduction; Seismology; Tectonics","score_opus":0.04722508059434411,"score_gpt":0.3297997697540928,"score_spread":0.2825746891597487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056262142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99575126,0.000042861317,0.000346113,0.003244466,0.000030436566,0.0003309859,0.00005652102,0.0000030741683,0.00019425945],"genre_scores_gemma":[0.99972135,0.00000734616,0.00006319481,0.000118210126,0.00005526648,0.0000027437738,0.000022060116,0.0000022269444,0.000007618856],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985673,0.00032241593,0.0002605921,0.00017235654,0.00040242253,0.00027495646],"domain_scores_gemma":[0.99755555,0.002061238,0.000092408336,0.00017788017,0.00007047932,0.00004241445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018038654,0.000078302706,0.00017265246,0.00005854249,0.00017013012,0.000033309167,0.00016668635,0.00002917369,0.000032123327],"category_scores_gemma":[0.00019007962,0.00004395488,0.000038970724,0.00030168373,0.00038301825,0.00013014642,0.000008627874,0.0002420019,0.0000045560523],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006038884,0.00012095371,0.005448002,0.000028418513,0.000038539816,0.00001312304,0.0016433401,0.00051080657,0.9728268,0.016955556,0.000076203316,0.0017343672],"study_design_scores_gemma":[0.0017823206,0.00058380706,0.8704742,0.00015169628,0.000030847685,0.0000011950583,0.00062347646,0.013120241,0.07777982,0.035208184,0.00004120808,0.0002029696],"about_ca_topic_score_codex":0.0011229395,"about_ca_topic_score_gemma":0.0009328425,"teacher_disagreement_score":0.89504695,"about_ca_system_score_codex":0.000003687762,"about_ca_system_score_gemma":0.000025041843,"threshold_uncertainty_score":0.1792428},"labels":[],"label_agreement":null},{"id":"W2056431363","doi":"10.1029/2012jb009203","title":"Effect of depleted continental lithosphere counterflow and inherited crustal weakness on rifting of the continental lithosphere: General results","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; Dalhousie University","funders":"","keywords":"Geology; Rift; Lithosphere; Seafloor spreading; Mantle (geology); Crust; Continental crust; Passive margin; Continental margin; Underplating; Isostasy; Petrology; Geophysics; Paleontology; Tectonics","score_opus":0.01664627050085438,"score_gpt":0.2858377807031319,"score_spread":0.26919151020227755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056431363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99638253,0.0009501289,0.000004760108,0.00012879744,0.0006176927,0.00035628013,0.0002127253,0.00000837121,0.0013387162],"genre_scores_gemma":[0.9985183,0.000054920725,0.00028372917,0.000019402725,0.0008239945,0.000001807005,0.000011805428,0.000015375852,0.00027064895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.995597,0.0011564849,0.00087818026,0.00024309261,0.0014199802,0.0007052619],"domain_scores_gemma":[0.9964243,0.0017868632,0.00068843935,0.0003203057,0.00045083562,0.00032921208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026137638,0.0002757364,0.00077968865,0.000019670806,0.00021362174,0.00009820099,0.0005515296,0.00013409478,0.00026139116],"category_scores_gemma":[0.0009693158,0.00016089462,0.00026236742,0.00043987855,0.0005705285,0.00039361595,0.0001291726,0.0006306864,0.000015573709],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.024125842,0.0012203153,0.76124775,0.001042481,0.00089400436,0.000084517465,0.002229786,0.0005742629,0.1268544,0.0008851138,0.00627938,0.07456213],"study_design_scores_gemma":[0.004151266,0.0051994054,0.9100773,0.0006888456,0.00010982277,0.00004218069,0.0004520172,0.0014986246,0.07407929,0.0002177464,0.0031686274,0.00031491474],"about_ca_topic_score_codex":0.004521157,"about_ca_topic_score_gemma":0.00019475725,"teacher_disagreement_score":0.1488295,"about_ca_system_score_codex":0.000014238909,"about_ca_system_score_gemma":0.000117264484,"threshold_uncertainty_score":0.68346673},"labels":[],"label_agreement":null},{"id":"W2058234714","doi":"10.1111/j.1365-246x.2005.02623.x","title":"Lowermost mantle anisotropy beneath the north Pacific from differential<i>S-ScS</i>splitting","year":2005,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Anisotropy; Seismic anisotropy; Mantle (geology); Geophysics; Subduction; Isotropy; Seismology; Hotspot (geology); Shear wave splitting; Tectonics; Physics","score_opus":0.007967075203716551,"score_gpt":0.20301199113759408,"score_spread":0.19504491593387752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058234714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916145,0.00005691985,0.00075402175,0.0019607479,0.0022713856,0.00007616586,0.0004997616,0.000027995986,0.0027385026],"genre_scores_gemma":[0.9909891,0.00007145662,0.0006095692,0.00036385123,0.0070061353,0.0000011574822,0.0002939319,0.0000076809,0.0006571309],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9983758,0.00008052221,0.0003570961,0.00024821766,0.0006036062,0.00033480892],"domain_scores_gemma":[0.99918336,0.00016442011,0.00020981056,0.00018721413,0.00009675979,0.00015844412],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000117346106,0.00019077104,0.0002058682,0.000040643547,0.00038620472,0.000517007,0.0006652036,0.0000469805,0.005963621],"category_scores_gemma":[0.000020332034,0.00012074158,0.00016760631,0.00008403567,0.000078978,0.00037499465,0.000052048028,0.00031657962,0.0011652226],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012501373,0.0013157721,0.38880286,0.00002788806,0.0024786992,0.00042478903,0.0041172067,0.016191918,0.047106087,0.014544078,0.050438922,0.47330165],"study_design_scores_gemma":[0.00069018477,0.000100034325,0.8671129,0.000033044667,0.0000723347,0.00004587506,0.000112880916,0.009323404,0.0017344153,0.00783477,0.1125727,0.00036746988],"about_ca_topic_score_codex":0.00059659587,"about_ca_topic_score_gemma":0.00028777414,"teacher_disagreement_score":0.47831002,"about_ca_system_score_codex":0.000010792444,"about_ca_system_score_gemma":0.000036514077,"threshold_uncertainty_score":0.9996125},"labels":[],"label_agreement":null},{"id":"W2058249593","doi":"10.1016/j.epsl.2007.11.025","title":"Modelling tectonic styles and ultra-high pressure (UHP) rock exhumation during the transition from oceanic subduction to continental collision","year":2007,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":280,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Natural Environment Research Council; Killam Trusts; Sight Research UK","keywords":"Geology; Subduction; Continental collision; Lithosphere; Eclogitization; Collision zone; Continental crust; Obduction; Continental margin; Mantle (geology); Convergent boundary; Underplating; Craton; Passive margin; Geophysics; Oceanic crust; Tectonics; Seismology; Rift","score_opus":0.005205389239741596,"score_gpt":0.16736001195897912,"score_spread":0.16215462271923753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058249593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99585783,0.00028587293,0.002307402,0.00056389754,0.0003503976,0.00030067016,0.00023971965,0.000032932247,0.00006128623],"genre_scores_gemma":[0.99861354,0.00006715641,0.00045400238,0.00038626365,0.0002532277,5.2467124e-7,0.00020706088,0.000003088451,0.000015157414],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9986249,0.000047427548,0.00020375788,0.0003994706,0.00036144102,0.0003629919],"domain_scores_gemma":[0.9994982,0.000105075764,0.0000692889,0.0001449196,0.000019267258,0.00016325935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005447365,0.00015318728,0.00015003631,0.00010760781,0.00067121803,0.0002415862,0.0001613939,0.00004478752,0.00018024915],"category_scores_gemma":[0.000008203927,0.00011282336,0.000019098743,0.0002175831,0.00012347702,0.0006189779,0.00000893658,0.00011379031,0.000029297604],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000336162,0.00001116439,0.017494205,0.00004842647,0.000027861923,0.00002099877,0.002069097,0.7239109,0.25358713,0.00003884128,0.00009315043,0.0023620704],"study_design_scores_gemma":[0.00036779838,0.00009923167,0.9305715,0.000042964206,0.000037601756,0.0000335492,0.00026697468,0.052421253,0.015242227,0.00006177783,0.00059224904,0.0002628597],"about_ca_topic_score_codex":0.0042262077,"about_ca_topic_score_gemma":0.0004918836,"teacher_disagreement_score":0.9130773,"about_ca_system_score_codex":0.0000020604245,"about_ca_system_score_gemma":0.000013590744,"threshold_uncertainty_score":0.63887906},"labels":[],"label_agreement":null},{"id":"W2058870065","doi":"10.1016/s0012-821x(02)00750-1","title":"Mode coupling in a viscoelastic self-gravitating spherical earth induced by axisymmetric loads and lateral viscosity variations","year":2002,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Viscoelasticity; Spherical harmonics; Rotational symmetry; Physics; Mantle (geology); Mechanics; Viscosity; Nonlinear system; Rheology; Mode coupling; Classical mechanics; Harmonics; Coupling (piping); Geophysics; Materials science; Optics; Thermodynamics; Composite material","score_opus":0.00933467108112386,"score_gpt":0.19481832953976616,"score_spread":0.1854836584586423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058870065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984304,0.0002318465,0.0001510346,0.00038665975,0.000252471,0.0001744391,0.000119345845,0.000039086077,0.00021477145],"genre_scores_gemma":[0.99620724,0.000049364673,0.0029715176,0.0006049227,0.00006587107,9.689451e-7,0.000078115525,0.0000035437654,0.000018475972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998286,0.000057053778,0.00025661886,0.0004839209,0.0003587351,0.00055767084],"domain_scores_gemma":[0.99929947,0.00020979035,0.00008117628,0.0001371131,0.000013417233,0.00025904994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038284878,0.00019656694,0.000243623,0.00019022742,0.00039006802,0.00032214716,0.00018970521,0.000058164223,0.00024602542],"category_scores_gemma":[0.000038122955,0.00017336733,0.000018868905,0.00067300355,0.00017173516,0.0006357564,0.000026280377,0.00020536153,0.00006504316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000064486536,0.00010640867,0.85402435,0.000100090976,0.000046210327,0.00013358882,0.0024540669,0.050009742,0.08608825,0.00011310603,0.00040636878,0.006453301],"study_design_scores_gemma":[0.00032237542,0.00012349617,0.6330077,0.000018055462,0.000012960953,0.000016587986,0.000017256052,0.36578134,0.00015911194,0.00004954356,0.0002431505,0.00024838865],"about_ca_topic_score_codex":0.003758275,"about_ca_topic_score_gemma":0.00046980506,"teacher_disagreement_score":0.3157716,"about_ca_system_score_codex":0.0000024868298,"about_ca_system_score_gemma":0.000020131945,"threshold_uncertainty_score":0.7069714},"labels":[],"label_agreement":null},{"id":"W2058873732","doi":"10.1139/e04-047","title":"Phanerozoic vertical motions of Hudson Bay","year":2004,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Devonian; Thermal subsidence; Paleozoic; Paleontology; Sedimentary basin; Lithosphere; Structural basin; Ordovician; Rift; Sedimentary rock; Cretaceous; Subsidence; Basin and range topography; Tectonic subsidence; Tectonics","score_opus":0.01810539976870911,"score_gpt":0.2121238993553354,"score_spread":0.1940184995866263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058873732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948693,0.00036029893,0.00009575305,0.00048722443,0.0008680962,0.00003701331,0.00004295078,0.0000021115495,0.0032372805],"genre_scores_gemma":[0.9987946,0.000015075749,0.0009234699,0.00007620624,0.0001525845,5.1719024e-8,0.0000018496524,0.0000011553651,0.000035006713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99906075,0.000034489964,0.00026788283,0.000095980984,0.00025290487,0.00028801887],"domain_scores_gemma":[0.99924856,0.000033282824,0.0000940458,0.00007399519,0.00009095845,0.00045916517],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004830411,0.00006940049,0.00016948789,0.00018183471,0.00020618546,0.00008295501,0.0003188847,0.00003331042,0.0015309654],"category_scores_gemma":[0.00008371492,0.000050957184,0.00006173887,0.00030285766,0.0004058859,0.00031119463,0.000002637241,0.00007198629,0.000053998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044341723,0.00009413733,0.73683316,0.00008989941,0.00014364943,0.0005270626,0.003788152,0.19597039,0.015832122,0.03526632,0.0008711505,0.010539605],"study_design_scores_gemma":[0.00042024264,0.000785094,0.9760332,0.00010508585,0.000032550444,0.00011521448,0.00024314331,0.00016930439,0.0075436807,0.008590573,0.0057837986,0.00017808753],"about_ca_topic_score_codex":0.01905255,"about_ca_topic_score_gemma":0.18119,"teacher_disagreement_score":0.23920004,"about_ca_system_score_codex":0.0000010131796,"about_ca_system_score_gemma":0.0012216651,"threshold_uncertainty_score":0.9993818},"labels":[],"label_agreement":null},{"id":"W2059274653","doi":"10.1007/s00269-005-0030-5","title":"Ab initio elasticity of FeS2 pyrite from 0 to 135 GPa","year":2005,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Chemistry; Ab initio; Pyrite; Ab initio quantum chemistry methods; Elasticity (physics); Polynomial; Equation of state; Thermodynamics; Moduli; Computation; Computational chemistry; Molecular physics; Mineralogy; Quantum mechanics; Physics; Molecule; Mathematical analysis; Organic chemistry","score_opus":0.010428324621621063,"score_gpt":0.20277400435141787,"score_spread":0.19234567972979683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059274653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99299777,0.00013738593,0.000039347986,0.00011625107,0.000047808728,0.00004768303,0.0011570303,0.0000073649053,0.005449345],"genre_scores_gemma":[0.9984274,0.000034483146,0.00059713627,0.00006360947,0.0004858162,8.270327e-7,0.00015411332,0.0000030660915,0.0002335522],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993271,0.000009079368,0.00021304515,0.00016728086,0.00014432373,0.00013915732],"domain_scores_gemma":[0.9995388,0.00006503045,0.00010753581,0.00014286941,0.000052300707,0.000093513605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005492668,0.00010989963,0.0002600142,0.000006673413,0.000029805997,0.00001740271,0.00011746094,0.000039596944,0.00073880696],"category_scores_gemma":[0.000012746883,0.00009770436,0.00004191206,0.000057344874,0.000055781362,0.00007243883,0.000020092648,0.000040295912,0.000015527488],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003250334,0.000049230723,0.0028485325,0.000088663364,0.000036844238,8.934911e-7,0.00017146982,0.0010721239,0.9877662,0.00005921712,0.0014898634,0.0063844533],"study_design_scores_gemma":[0.00031498857,0.000039390634,0.020225022,0.000056499328,0.00003892203,5.822623e-7,0.000025731308,0.00057383743,0.9698629,0.0026451026,0.00602226,0.00019478341],"about_ca_topic_score_codex":0.0010940516,"about_ca_topic_score_gemma":0.00003910359,"teacher_disagreement_score":0.017903324,"about_ca_system_score_codex":8.678559e-7,"about_ca_system_score_gemma":0.000015640879,"threshold_uncertainty_score":0.80894184},"labels":[],"label_agreement":null},{"id":"W2059995124","doi":"10.1103/physrevb.77.052103","title":"Metastable high-pressure single-bonded phases of nitrogen predicted via genetic algorithm","year":2008,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Metastability; Crystal structure; Materials science; Crystal structure prediction; Enthalpy; Atom (system on chip); Nitrogen; Crystallography; Physics; Atomic physics; Condensed matter physics; Thermodynamics; Chemistry; Quantum mechanics","score_opus":0.016913243568612804,"score_gpt":0.22999854888909632,"score_spread":0.21308530532048353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059995124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9241301,0.06924755,0.0017488021,0.00015220592,0.0005058406,0.0010303688,0.0017420131,0.00013054982,0.0013125888],"genre_scores_gemma":[0.9905851,0.0047860225,0.0036786206,0.00017903194,0.0003841326,0.000008361267,0.00027865623,0.000009697354,0.00009037016],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983771,0.00015208474,0.00038941734,0.00031844154,0.00042853178,0.0003344431],"domain_scores_gemma":[0.9989686,0.00012273202,0.00026638768,0.00037128443,0.0001094008,0.00016161654],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000114390685,0.00022503051,0.00076650747,0.000029227856,0.00010945749,0.000015127511,0.00030579214,0.000032710097,0.001817625],"category_scores_gemma":[0.000061014467,0.00016805697,0.00017464095,0.00029278334,0.0001301143,0.00016188524,0.000029313049,0.000087196684,0.00012856215],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030616068,0.0044564856,0.011331452,0.010965758,0.0030615404,0.00039433458,0.0013914844,0.0036843866,0.2142063,0.0010233774,0.03250922,0.7166695],"study_design_scores_gemma":[0.0059023825,0.0048301257,0.1007454,0.004523833,0.008120743,0.00029583357,0.00004178017,0.034298833,0.35738707,0.07431566,0.4051063,0.004432036],"about_ca_topic_score_codex":0.0011812531,"about_ca_topic_score_gemma":0.000010650192,"teacher_disagreement_score":0.7122375,"about_ca_system_score_codex":0.00000160868,"about_ca_system_score_gemma":0.000045425495,"threshold_uncertainty_score":0.99909484},"labels":[],"label_agreement":null},{"id":"W2061016685","doi":"10.1139/e05-037","title":"Tectonic significance of potential-field anomalies in western Canada: results from the Lithoprobe SNORCLE transect","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Precambrian; Crust; Seismology; Tectonics; Mantle (geology); Gravity anomaly; Subduction; Terrane; Geophysics; Paleontology","score_opus":0.012003999488134196,"score_gpt":0.18852000359939314,"score_spread":0.17651600411125895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061016685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99377,0.0010506815,0.000014951474,0.003262784,0.00050724973,0.00008017366,0.00034305238,0.0000013270612,0.0009697781],"genre_scores_gemma":[0.9990572,0.000035627236,0.00030147005,0.00032358203,0.0002245759,1.729543e-7,0.000003522239,0.0000015211032,0.000052377163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986795,0.000105635525,0.00044005105,0.00014856542,0.0003035099,0.00032271657],"domain_scores_gemma":[0.9991045,0.00025559476,0.0002366269,0.00012286668,0.000062389605,0.00021802059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085711846,0.00009152959,0.00020989124,0.000087685396,0.00016976304,0.000101004814,0.0005533402,0.00003504094,0.00047351554],"category_scores_gemma":[0.00009579933,0.000059839465,0.000045409404,0.00029026065,0.00021036001,0.00026251198,0.000003244713,0.000121601945,0.000004649061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020310322,0.0000206466,0.83850473,0.000022641916,0.00006514472,0.00030497074,0.0042155976,0.12113753,0.0035381408,0.00015186053,0.0018537458,0.029981906],"study_design_scores_gemma":[0.00030590573,0.00019435487,0.98056877,0.00007608596,0.000012691883,0.000017016933,0.00033970553,0.00040949322,0.00398268,0.0001816686,0.013788563,0.00012309203],"about_ca_topic_score_codex":0.9608619,"about_ca_topic_score_gemma":0.9992725,"teacher_disagreement_score":0.14206403,"about_ca_system_score_codex":0.000002794094,"about_ca_system_score_gemma":0.003054283,"threshold_uncertainty_score":0.5418167},"labels":[],"label_agreement":null},{"id":"W2061749031","doi":"10.1029/1999gl008474","title":"Diffusion creep of fine‐grained garnetite: Implications for the flow strength of subducting slabs","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Creep; Diffusion creep; Geology; Diffusion; Grain boundary diffusion coefficient; Grain boundary; Grain Boundary Sliding; Grain size; Lithosphere; Materials science; Mineralogy; Thermodynamics; Composite material; Microstructure; Seismology; Tectonics","score_opus":0.0337006040846132,"score_gpt":0.2932031854400066,"score_spread":0.2595025813553934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061749031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930655,0.0000638352,0.0001541354,0.0051399046,0.000080264515,0.0004455906,0.00045250804,0.0000132816085,0.00058502],"genre_scores_gemma":[0.9982713,0.000043004886,0.0007714494,0.00008012688,0.00039415524,0.000016474009,0.0001272638,0.0000057417756,0.00029051767],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99846953,0.00015071665,0.00026621346,0.00024903376,0.00041150925,0.0004529951],"domain_scores_gemma":[0.99753094,0.0017619537,0.00007048702,0.0004040273,0.00014193548,0.0000906781],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000554581,0.00010857751,0.00022528642,0.00005976795,0.00027311774,0.000042666645,0.00045847878,0.000038782237,0.00081735465],"category_scores_gemma":[0.00019995851,0.00007166512,0.000116846466,0.00035316203,0.0003188292,0.00008969048,0.000030134375,0.00015531342,0.00005514587],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005878721,0.00018271964,0.0049496205,0.00024971578,0.00014319971,0.0000020709144,0.00088953244,0.0047211023,0.63083434,0.0035584967,0.020224934,0.33365637],"study_design_scores_gemma":[0.0016500785,0.0009422541,0.87742144,0.00012121089,0.00009110533,0.000002090382,0.00017933943,0.036547706,0.028084224,0.011276294,0.043181203,0.00050305255],"about_ca_topic_score_codex":0.0037716834,"about_ca_topic_score_gemma":0.0002321821,"teacher_disagreement_score":0.8724718,"about_ca_system_score_codex":0.000002814353,"about_ca_system_score_gemma":0.000040959712,"threshold_uncertainty_score":0.894946},"labels":[],"label_agreement":null},{"id":"W2061813458","doi":"10.1103/physrevlett.96.137402","title":"Valence Band X-Ray Emission Spectra of Compressed Germanium","year":2006,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Germanium; Valence (chemistry); Materials science; Density functional theory; Spectral line; Diamond; Semimetal; Condensed matter physics; Valence band; Density of states; Metal; Band gap; Atomic physics; Physics; Silicon; Optoelectronics","score_opus":0.009015939680443567,"score_gpt":0.22910717717723963,"score_spread":0.22009123749679607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061813458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897676,0.0050582937,0.0001334952,0.0013633557,0.00023351767,0.00028358932,0.00010443075,0.000032466694,0.0030232598],"genre_scores_gemma":[0.9973184,0.0009213584,0.00010349484,0.0011631957,0.00037646986,0.000001535756,0.00008264464,0.0000037638383,0.000029146038],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990151,0.00008001263,0.00023468742,0.00020349532,0.0002585693,0.00020813034],"domain_scores_gemma":[0.9994781,0.00009646421,0.00012955502,0.00021434508,0.000020705858,0.000060813665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012257816,0.00013238705,0.0003718052,0.000015375703,0.000045850506,0.000019560384,0.00020483517,0.00000839596,0.00047672688],"category_scores_gemma":[0.0000057286115,0.00009593731,0.000111359186,0.00011504321,0.00006727121,0.000109995766,0.000008786832,0.00006761357,0.00016059156],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024204932,0.00012846042,0.0048241545,0.0026821396,0.0000293143,0.000020334735,0.000049797123,0.0032984826,0.94164556,0.00046775021,0.0450981,0.0017316906],"study_design_scores_gemma":[0.0010247645,0.00027758646,0.5808957,0.0050060702,0.0004915993,0.000008662134,0.0000054566044,0.0050354223,0.19410013,0.0024762484,0.20923235,0.0014460123],"about_ca_topic_score_codex":0.00054750504,"about_ca_topic_score_gemma":0.0000058810483,"teacher_disagreement_score":0.7475454,"about_ca_system_score_codex":0.000001394452,"about_ca_system_score_gemma":0.0000093800045,"threshold_uncertainty_score":0.5219825},"labels":[],"label_agreement":null},{"id":"W2062808943","doi":"10.1103/physrevb.73.094202","title":"Vibrational features of water’s amorph at high pressures","year":2006,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Umeå Universitet","keywords":"Debye model; Plateau (mathematics); Debye; Thermodynamics; Thermal conductivity; Materials science; Physics; Condensed matter physics; Mathematics","score_opus":0.007213857579904474,"score_gpt":0.22170250832790078,"score_spread":0.2144886507479963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062808943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97197735,0.01443734,0.000021168395,0.000844744,0.00034173246,0.0003884431,0.00045331745,0.000041851974,0.011494044],"genre_scores_gemma":[0.99754757,0.0006834033,0.00015208006,0.00018339093,0.0005002531,0.0000035348762,0.00053994724,0.0000034070868,0.00038644572],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990781,0.0000683515,0.0002019227,0.00018043266,0.00028247602,0.00018870292],"domain_scores_gemma":[0.9995868,0.000072245195,0.00007801216,0.00017483623,0.00004072003,0.000047377962],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000104785795,0.00012049849,0.0003405263,0.000011951769,0.00006477016,0.000019579697,0.00016110051,0.000019430792,0.0019840547],"category_scores_gemma":[0.00001184863,0.00007093171,0.00009929648,0.000058541358,0.000058738988,0.000107964705,0.000024275761,0.000043804008,0.00038952555],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024500856,0.0007709546,0.016536845,0.009318743,0.00030220742,0.00004337685,0.00024440326,0.00685294,0.56484556,0.12736005,0.24575044,0.027729465],"study_design_scores_gemma":[0.0003396496,0.00016778357,0.5728824,0.0005702721,0.00022916165,0.000006083779,0.000001238852,0.00018422687,0.2437878,0.0523507,0.12899403,0.00048665798],"about_ca_topic_score_codex":0.0020886797,"about_ca_topic_score_gemma":0.00018514752,"teacher_disagreement_score":0.5563456,"about_ca_system_score_codex":0.0000012860884,"about_ca_system_score_gemma":0.000010868263,"threshold_uncertainty_score":0.99892825},"labels":[],"label_agreement":null},{"id":"W2063442400","doi":"10.1002/asna.200310210","title":"Mapping the shape of the accretion disk of Hercules X‐1","year":2004,"lang":"en","type":"article","venue":"Astronomische Nachrichten","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Physics; Astrophysics; Accretion disc; Accretion (finance); Modulation (music); Orbit (dynamics); Phase (matter); Intermediate polar; Turn (biochemistry); Binary number; Orbital inclination; Astronomy; Stars; Nuclear magnetic resonance","score_opus":0.014093336830217164,"score_gpt":0.18889374403554307,"score_spread":0.17480040720532591,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063442400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652284,0.00021067078,0.00014599867,0.0003343083,0.00020080357,0.00014852475,0.00007376202,0.0000064447713,0.0023566182],"genre_scores_gemma":[0.9993174,0.000009349838,0.000455888,0.00002565471,0.00011115521,0.0000013301592,0.000017726277,0.0000025177046,0.000058986578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993276,0.000058636993,0.00021175545,0.00011294019,0.00013954972,0.00014949242],"domain_scores_gemma":[0.9994721,0.000055957913,0.00017908518,0.000238637,0.000027511653,0.000026700292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024174637,0.00008515816,0.00015111406,0.000018227809,0.00009054074,0.000017763814,0.00035622212,0.000034012817,0.00050514546],"category_scores_gemma":[0.000018596827,0.00004378821,0.00008586238,0.00012533859,0.00010835262,0.00008519856,0.000032115207,0.00006589544,0.000043944165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017460533,0.00015198198,0.72334903,0.00017310893,0.00044246097,0.0000013872267,0.0037231564,0.11398259,0.08440261,0.0061385427,0.000925851,0.06653465],"study_design_scores_gemma":[0.0002765946,0.00004093617,0.98662937,0.00003083598,0.000028141721,9.12375e-7,0.00028506975,0.00036484067,0.008217311,0.00075050665,0.0032985145,0.00007694622],"about_ca_topic_score_codex":0.0017735899,"about_ca_topic_score_gemma":0.000112646725,"teacher_disagreement_score":0.26328033,"about_ca_system_score_codex":0.0000020469122,"about_ca_system_score_gemma":0.000051786774,"threshold_uncertainty_score":0.55309886},"labels":[],"label_agreement":null},{"id":"W2063466232","doi":"10.1130/0091-7613(2000)28<655:mtbotc>2.0.co;2","title":"Modeling the behavior of the continental mantle lithosphere during plate convergence","year":2000,"lang":"en","type":"article","venue":"Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Nova scotia; Geology; Citation; Icon; Mantle (geology); Library science; Paleontology; Oceanography; Computer science; Tectonics","score_opus":0.00742373080063679,"score_gpt":0.188652481647993,"score_spread":0.1812287508473562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063466232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99769616,0.00015756869,0.000005196965,0.00012922488,0.0004624361,0.00013967793,0.000037614132,0.000009700083,0.0013624299],"genre_scores_gemma":[0.99842906,0.00004355593,0.00003114765,0.000048051905,0.00006528129,0.000002924461,0.000007390718,0.0000016800756,0.0013709086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994404,0.0000520532,0.00014103869,0.00011182967,0.00007927092,0.00017542466],"domain_scores_gemma":[0.9997317,0.000020206864,0.000036015674,0.00017693866,0.000013902421,0.00002122679],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008690281,0.00006445703,0.0001086584,0.0000045584634,0.00013482553,0.000009139772,0.00024413,0.00003996347,0.011618598],"category_scores_gemma":[0.0000036121526,0.00003463792,0.00003971886,0.00004549834,0.00009925464,0.00004137006,0.000018540404,0.00005963428,0.00018966748],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018802221,0.00004885381,0.849359,0.00004669211,0.0000614633,0.00003128171,0.0010985916,0.12876332,0.010403,0.00060228666,0.00020342106,0.009194086],"study_design_scores_gemma":[0.00035719186,0.00004586798,0.9678507,0.000013213195,0.000045784163,0.00004306868,0.00010143007,0.02301312,0.005286279,0.00071152806,0.0023807872,0.00015106736],"about_ca_topic_score_codex":0.0049223406,"about_ca_topic_score_gemma":0.0009226719,"teacher_disagreement_score":0.11849169,"about_ca_system_score_codex":4.970263e-7,"about_ca_system_score_gemma":0.000011815829,"threshold_uncertainty_score":0.98928493},"labels":[],"label_agreement":null},{"id":"W2063670250","doi":"10.1016/j.pepi.2006.03.025","title":"Mantle fabric at multiple scales across an Archean–Proterozoic boundary, Grenville Front, Canada","year":2006,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Manitoba","funders":"","keywords":"Geology; Magnetotellurics; Lithosphere; Archean; Proterozoic; Seismology; Mantle (geology); Tectonics; Shear wave splitting; Geophysics; Paleontology; Electrical resistivity and conductivity","score_opus":0.006953844909235862,"score_gpt":0.18248622578814094,"score_spread":0.17553238087890508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063670250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953398,0.0004255019,0.00001525687,0.00008368568,0.0006340143,0.00020570857,0.0027594138,0.000014019378,0.0005225862],"genre_scores_gemma":[0.99841386,0.000016954065,0.0001526705,0.000099444405,0.00029020777,0.0000011763958,0.0006571915,0.000007104422,0.0003613724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986926,0.000098127326,0.00026664877,0.00028153165,0.00026474928,0.00039634123],"domain_scores_gemma":[0.9992945,0.0000820742,0.00015464032,0.00033134784,0.000022383243,0.0001150474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011699991,0.00021584898,0.00029853778,0.000013673974,0.00034677688,0.00007179767,0.0003403331,0.00004721723,0.00025485072],"category_scores_gemma":[0.000006207666,0.00015369405,0.00006176212,0.000056952857,0.00020811585,0.00014238997,0.00006674513,0.00010998061,0.00003477367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027908347,0.000047699246,0.9702891,0.00015432692,0.000075673386,0.000019312512,0.00034575493,0.0056572193,0.009759367,0.000024291428,0.0025006123,0.0108475415],"study_design_scores_gemma":[0.00031761033,0.00010167212,0.97675115,0.000033595028,0.000020015332,0.000014658039,0.000048672522,0.0024282984,0.007008081,0.0007967727,0.012224377,0.000255084],"about_ca_topic_score_codex":0.75005215,"about_ca_topic_score_gemma":0.9469729,"teacher_disagreement_score":0.19692075,"about_ca_system_score_codex":0.0000040300197,"about_ca_system_score_gemma":0.000063337786,"threshold_uncertainty_score":0.6267462},"labels":[],"label_agreement":null},{"id":"W2063731469","doi":"10.1063/1.3686547","title":"Chemical bonding evolution towards phase transtions for nitrogen-rich high energy density solids under high pressure","year":2012,"lang":"en","type":"article","venue":"AIP conference proceedings","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Chemical physics; Nitrogen; Chemical bond; Phase transition; Phase (matter); Diatomic molecule; Chemistry; Molecule; Materials science; Thermodynamics; Organic chemistry","score_opus":0.021095492536064672,"score_gpt":0.23911257849405498,"score_spread":0.2180170859579903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063731469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94796747,0.00020371075,0.049055215,0.00054475036,0.00070559344,0.00028598943,0.00037655447,0.00012544551,0.00073529035],"genre_scores_gemma":[0.9971507,0.00001557047,0.0014012303,0.0001306803,0.00075800327,0.000026935224,0.00026570124,0.000010386515,0.00024075311],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99843055,0.000014480226,0.00027080995,0.00035363596,0.00028050333,0.00065001805],"domain_scores_gemma":[0.99918836,0.00004647279,0.0001232949,0.00010401411,0.00028084777,0.00025698342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026874646,0.00024612644,0.00032194046,0.000071835784,0.00028497426,0.0001625874,0.00025376474,0.0001867384,0.0005930604],"category_scores_gemma":[0.000041449584,0.00021894387,0.00007844444,0.00017588865,0.00009791644,0.0007181679,0.000022660473,0.00011410818,0.00003191811],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036805525,0.00032580385,0.034539755,0.00024594142,0.0002442279,0.0000010939841,0.0013083597,0.000020772011,0.2655149,0.6882018,0.0038475173,0.00538178],"study_design_scores_gemma":[0.0062178946,0.00095107965,0.08642732,0.00021493192,0.0016778782,0.000072258474,0.0010108833,0.015528591,0.37495998,0.4769441,0.03326325,0.0027318355],"about_ca_topic_score_codex":0.0021194522,"about_ca_topic_score_gemma":0.000050978764,"teacher_disagreement_score":0.21125768,"about_ca_system_score_codex":0.000011649059,"about_ca_system_score_gemma":0.00009948299,"threshold_uncertainty_score":0.89282715},"labels":[],"label_agreement":null},{"id":"W2064027263","doi":"10.1088/0256-307x/23/8/101","title":"First-Principles Study of Orthorhombic Perovskites MgSiO <sub>3</sub> up to 120 GPa and Its Geophysical Implications","year":2006,"lang":"en","type":"article","venue":"Chinese Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"Japan Society for the Promotion of Science","keywords":"Orthorhombic crystal system; Bulk modulus; Materials science; Perovskite (structure); Condensed matter physics; Thermodynamics; Lattice constant; Effective mass (spring–mass system); Plane wave; Lattice (music); Crystal structure; Diffraction; Physics; Chemistry; Crystallography; Classical mechanics","score_opus":0.01221911254607895,"score_gpt":0.2138115407494611,"score_spread":0.20159242820338213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064027263","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980049,0.000038025155,0.00009819944,0.00066267647,0.00025847796,0.0005098724,0.00025951146,0.000048017264,0.0001203065],"genre_scores_gemma":[0.9989653,0.000007809254,0.000056317636,0.00021281283,0.0005666927,0.000017317181,0.00014135196,0.000013421411,0.000018931389],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998574,0.00005889206,0.0003286751,0.00044509,0.00026444197,0.00032886222],"domain_scores_gemma":[0.9991282,0.00016717362,0.00013862186,0.00036232057,0.00007230805,0.00013137971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000100361,0.000274853,0.00039984816,0.00006205722,0.00024757884,0.00009411444,0.00027420293,0.000037474158,0.00002513111],"category_scores_gemma":[0.000020810297,0.00022189823,0.00007696815,0.00036732433,0.000058561203,0.00025245224,0.00007296875,0.000098632656,0.0000926883],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072678435,0.0004494609,0.39862144,0.00012920516,0.00010763451,0.000008782683,0.0020935687,0.07798284,0.5167709,0.0012959285,0.0012510567,0.001216492],"study_design_scores_gemma":[0.00039385972,0.00014322475,0.98751915,0.000015049213,0.000048213024,0.00000146925,0.000039055838,0.0017111531,0.008440974,0.0012552475,0.0001380913,0.0002945429],"about_ca_topic_score_codex":0.0014880745,"about_ca_topic_score_gemma":0.0009560506,"teacher_disagreement_score":0.5888977,"about_ca_system_score_codex":0.0000036592219,"about_ca_system_score_gemma":0.000017808621,"threshold_uncertainty_score":0.9048747},"labels":[],"label_agreement":null},{"id":"W2064306087","doi":"10.1063/1.4876220","title":"Carbon tetrachloride under extreme conditions","year":2014,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); University of Saskatchewan","funders":"National Research Council Canada; Western Economic Diversification Canada; Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy","keywords":"Carbon tetrachloride; Raman spectroscopy; Synchrotron; Tetrachloride; CCL4; Phase (matter); Irradiation; Diffraction; Infrared spectroscopy; Analytical Chemistry (journal); Decomposition; Chemistry; X-ray crystallography; Materials science; Physics; Environmental chemistry; Organic chemistry; Optics; Nuclear physics","score_opus":0.0186848482043854,"score_gpt":0.21184247503104794,"score_spread":0.19315762682666254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064306087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99505,0.000049420963,0.00032147244,0.00032785325,0.00037279184,0.000029583889,0.000013835317,0.0000070270994,0.003828004],"genre_scores_gemma":[0.998414,0.000011097183,0.0000689968,0.00019351521,0.0012701383,7.6528195e-8,0.00000806047,0.0000031023656,0.000031024214],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99931335,0.000059022743,0.00020370116,0.000050700033,0.00023077126,0.00014246455],"domain_scores_gemma":[0.9992955,0.00026085755,0.00017396272,0.00012864651,0.00006460662,0.00007642763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029232784,0.00008018239,0.00016579172,0.000010322281,0.00004627731,0.00002459225,0.00023940207,0.000030559444,0.00016213136],"category_scores_gemma":[0.000027152355,0.000046970512,0.000063091364,0.0000721746,0.00008339336,0.00009447595,0.0000088675615,0.00015382165,0.000032046864],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001644709,0.00010036018,0.0018869002,0.000032990425,0.00015274512,0.000004794891,0.00039963843,0.0105920015,0.9721854,0.005229918,0.0038136088,0.005437177],"study_design_scores_gemma":[0.000936644,0.0002471892,0.01684038,0.00007019587,0.0003376741,0.00007097161,0.00009816792,0.004604292,0.502613,0.46803135,0.005740631,0.00040947355],"about_ca_topic_score_codex":0.00009978095,"about_ca_topic_score_gemma":0.000004066303,"teacher_disagreement_score":0.46957237,"about_ca_system_score_codex":0.0000025759236,"about_ca_system_score_gemma":0.000022137452,"threshold_uncertainty_score":0.19154018},"labels":[],"label_agreement":null},{"id":"W2064772207","doi":"10.1029/2009jb006856","title":"A low‐velocity zone atop the transition zone in northwestern Canada","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Transition zone; Receiver function; Lithosphere; Seismology; Discontinuity (linguistics); Poisson distribution; Shear velocity; Geodesy; Mineralogy; Geophysics; Tectonics; Meteorology; Geography","score_opus":0.01478828535559344,"score_gpt":0.25506231773986077,"score_spread":0.24027403238426734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064772207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974801,0.00007274428,0.00006945258,0.0013466461,0.0005295655,0.00015542946,0.00004950179,0.0000041229464,0.00029241684],"genre_scores_gemma":[0.99854547,0.000036876205,0.0002195138,0.00010477225,0.00089615857,0.0000014131166,0.000008622482,0.0000054936386,0.00018165584],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99728185,0.0003259281,0.00041727867,0.00017491885,0.0012602353,0.00053977297],"domain_scores_gemma":[0.99832267,0.000704689,0.00014213075,0.00023529088,0.00033545343,0.00025977663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012644168,0.00013696712,0.0003159904,0.000017731567,0.00021928185,0.00014330793,0.0005675156,0.00007189717,0.0008789245],"category_scores_gemma":[0.00011741646,0.00008303577,0.000093099676,0.00041081852,0.00021920398,0.00026996533,0.00002683579,0.0010746791,0.00005443928],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0058041923,0.0024758035,0.24116655,0.00068854203,0.0008237463,0.0055570845,0.010213127,0.017985435,0.13240975,0.0035837214,0.03476604,0.54452604],"study_design_scores_gemma":[0.0007677215,0.0004374007,0.9772094,0.000071690316,0.000015458165,0.000034762197,0.0004800697,0.0020744419,0.0030885495,0.0024883407,0.013129597,0.00020255308],"about_ca_topic_score_codex":0.82294375,"about_ca_topic_score_gemma":0.9675729,"teacher_disagreement_score":0.73604286,"about_ca_system_score_codex":0.000015055824,"about_ca_system_score_gemma":0.0008560524,"threshold_uncertainty_score":0.96236074},"labels":[],"label_agreement":null},{"id":"W2065131799","doi":"10.1029/2008jb005726","title":"Rocky Mountain evolution: Tying Continental Dynamics of the Rocky Mountains and Deep Probe seismic experiments with receiver functions","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tying; Geology; Seismology; Geophysics; Receiver function; Lithosphere; Tectonics","score_opus":0.014669932529936024,"score_gpt":0.2623075794854516,"score_spread":0.24763764695551554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065131799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969203,0.00047975927,0.0009169528,0.00057758635,0.00014823569,0.0002375101,0.000034111832,0.0000066458597,0.0006789151],"genre_scores_gemma":[0.9987332,0.00004517603,0.00037720604,0.000037833222,0.0002747282,0.0000012494637,0.000007247875,0.0000056341937,0.0005176996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99787545,0.00024169225,0.00034938357,0.0001892464,0.0009423506,0.00040187006],"domain_scores_gemma":[0.9987783,0.0001842935,0.00024715174,0.00019867507,0.00040927026,0.00018234257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043323566,0.0001522588,0.000316059,0.000023976858,0.00036896433,0.00011371404,0.000349581,0.000061756866,0.00019212597],"category_scores_gemma":[0.000085510204,0.00008905575,0.00009232922,0.00036854425,0.00025143605,0.00038249386,0.00004475888,0.00039306027,0.000014628451],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0070378934,0.0026505718,0.6970362,0.00041082082,0.0014562722,0.00029373122,0.004505196,0.047781963,0.083249666,0.010697971,0.007313025,0.1375667],"study_design_scores_gemma":[0.0013326025,0.0025906954,0.95618254,0.00021566392,0.00006645957,0.000057887777,0.0022249655,0.024247432,0.0018617966,0.009526112,0.0014473835,0.00024646023],"about_ca_topic_score_codex":0.0023117997,"about_ca_topic_score_gemma":0.0006326828,"teacher_disagreement_score":0.25914636,"about_ca_system_score_codex":0.00004066124,"about_ca_system_score_gemma":0.00018088287,"threshold_uncertainty_score":0.36315882},"labels":[],"label_agreement":null},{"id":"W2065146837","doi":"10.1016/j.tecto.2004.08.006","title":"Crustal and mantle strengths in continental lithosphere: is the jelly sandwich model obsolete?","year":2004,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":195,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Crust; Mafic; Continental crust; Crustal recycling; Mantle (geology); Petrology; Felsic; Underplating; Geophysics; Geochemistry; Seismology; Tectonics","score_opus":0.006826135086596188,"score_gpt":0.20150654544610044,"score_spread":0.19468041035950426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065146837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99516886,0.00022852486,0.00012046322,0.00031779343,0.00014833354,0.00018154422,0.00018842342,0.000030814706,0.0036152555],"genre_scores_gemma":[0.9988377,0.0000690177,0.00049671246,0.0002568308,0.00011788629,0.0000024013423,0.000029261817,0.000006372368,0.00018381198],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99911803,0.000021955553,0.00017561494,0.00024083108,0.00016453183,0.00027906318],"domain_scores_gemma":[0.99959946,0.000057366215,0.000058287984,0.0002046724,0.00001851529,0.00006170439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009818393,0.00015840768,0.00019190111,0.000015348453,0.00011828662,0.000098431905,0.00018286715,0.000053634063,0.0002763824],"category_scores_gemma":[0.000008083712,0.00011044695,0.000041250576,0.00012776017,0.00009588344,0.0001615027,0.000030107316,0.00012719216,0.00009797567],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010852958,0.0011098486,0.08240858,0.0005777367,0.00054488436,0.00029890114,0.027656399,0.3232939,0.06575022,0.05678303,0.0058690505,0.43462217],"study_design_scores_gemma":[0.0092604235,0.00086072204,0.49007165,0.0002474881,0.00023715233,0.00003374827,0.0016236757,0.14080276,0.07218922,0.26843464,0.013426121,0.002812382],"about_ca_topic_score_codex":0.0036697385,"about_ca_topic_score_gemma":0.0007902452,"teacher_disagreement_score":0.43180978,"about_ca_system_score_codex":0.0000040210584,"about_ca_system_score_gemma":0.00005107439,"threshold_uncertainty_score":0.5547572},"labels":[],"label_agreement":null},{"id":"W2065252419","doi":"10.1016/j.lithos.2004.03.049","title":"Mapping the mantle lithosphere for diamond potential using teleseismic methods☆","year":2004,"lang":"en","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Craton; Geology; Lithosphere; Mantle (geology); Magnetotellurics; Seismology; Classification of discontinuities; Kimberlite; Geophysics; Crust; Xenolith; Discontinuity (linguistics); Petrology; Tectonics; Electrical resistivity and conductivity","score_opus":0.031604821516595,"score_gpt":0.26738952712945896,"score_spread":0.23578470561286397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065252419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8947745,0.0006008528,0.1019539,0.00033813412,0.0010506127,0.00042238663,0.000162992,0.000040924748,0.00065569725],"genre_scores_gemma":[0.8831211,0.00001806303,0.115523405,0.0003098651,0.0006417953,0.000005611108,0.000039895334,0.00000852239,0.0003317497],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99906874,0.000086823005,0.00018349814,0.000220311,0.00012285278,0.00031780297],"domain_scores_gemma":[0.9995121,0.00009291396,0.00007965337,0.00021991842,0.000030858828,0.00006457237],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004610189,0.00012626639,0.0001733272,0.000020572474,0.00030911548,0.00013349803,0.00023653888,0.00006015781,0.00042825154],"category_scores_gemma":[0.000025726293,0.00008189187,0.000087441615,0.000120532226,0.00005197048,0.0001336052,0.000019316945,0.000069209804,0.00008046373],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008167928,0.00032418958,0.036371708,0.0012453625,0.0009654301,0.00020200922,0.019568782,0.17903787,0.09361936,0.012774936,0.005170387,0.6499032],"study_design_scores_gemma":[0.0028889943,0.00036896547,0.34314868,0.00024051336,0.00027526074,0.00011624043,0.002372586,0.04178437,0.03717572,0.15757504,0.41249147,0.0015621575],"about_ca_topic_score_codex":0.0061220387,"about_ca_topic_score_gemma":0.00014641798,"teacher_disagreement_score":0.648341,"about_ca_system_score_codex":0.0000033953227,"about_ca_system_score_gemma":0.000046342055,"threshold_uncertainty_score":0.92547315},"labels":[],"label_agreement":null},{"id":"W2065467771","doi":"10.1063/1.4874158","title":"The metallization and superconductivity of dense hydrogen sulfide","year":2014,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":751,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Superconductivity; Hydrogen sulfide; Sulfide; Materials science; Hydrogen; Condensed matter physics; Engineering physics; Metallurgy; Physics; Quantum mechanics; Sulfur","score_opus":0.010694627385802102,"score_gpt":0.19947679563717888,"score_spread":0.18878216825137678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065467771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990277,0.0003233907,0.00022543398,0.00015406025,0.000086619286,0.00002948631,0.000005292564,0.0000017257587,0.00014624505],"genre_scores_gemma":[0.99954927,0.00012821854,0.000060204195,0.000024654171,0.00022674128,4.391007e-8,0.0000015200126,0.000001778197,0.0000075891858],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99941915,0.00010822,0.00018001323,0.000037619793,0.00016982529,0.000085153544],"domain_scores_gemma":[0.9992363,0.00038596627,0.00016973469,0.0001007595,0.000068109366,0.0000391524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006260406,0.00005519448,0.00014759357,0.00000487882,0.000057854813,0.000018920451,0.00016405425,0.000019743418,0.000015802108],"category_scores_gemma":[0.0000717444,0.000025975167,0.000041108084,0.00005015019,0.00013320158,0.00012552118,0.00001266525,0.00007270611,0.0000030642839],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009467221,0.000018154637,0.0009104189,0.000020011481,0.00006748439,3.3658958e-7,0.0002799466,0.0007387329,0.98618263,0.0014140373,0.00015441774,0.0101191355],"study_design_scores_gemma":[0.00023830646,0.00007832062,0.0028292916,0.000021874697,0.00013394111,0.000017317343,0.00003506546,0.0012043917,0.9069302,0.087120295,0.0013087007,0.000082284474],"about_ca_topic_score_codex":0.00007668762,"about_ca_topic_score_gemma":0.000004607497,"teacher_disagreement_score":0.08570626,"about_ca_system_score_codex":8.0378834e-7,"about_ca_system_score_gemma":0.000013758496,"threshold_uncertainty_score":0.10592366},"labels":[],"label_agreement":null},{"id":"W2066725172","doi":"10.1029/2007gl031517","title":"D″ beneath the Arctic from inversion of shear waveforms","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Inversion (geology); Seismometer; Arctic; The arctic; Geodesy; Seismology; Waveform; Physics; Oceanography","score_opus":0.028395404682785168,"score_gpt":0.27171156878979474,"score_spread":0.24331616410700957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066725172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962083,0.000047165548,0.000055545483,0.002311734,0.0002692874,0.00019916901,0.00007956272,0.000014924809,0.0008142885],"genre_scores_gemma":[0.99857527,0.000018854975,0.00017320286,0.00044063106,0.00060127606,0.0000010946441,0.00007853482,0.0000048847623,0.00010625717],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9977214,0.00016151818,0.00022055137,0.00026877585,0.0009917534,0.0006360352],"domain_scores_gemma":[0.99830306,0.000991903,0.00005432426,0.0003878175,0.000092828974,0.00017008308],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001149623,0.00011626313,0.00019630804,0.000062702595,0.00024907597,0.00006480149,0.0004991581,0.000051350686,0.00065274024],"category_scores_gemma":[0.00011464462,0.00006744022,0.0000904761,0.00036213556,0.00040885966,0.00016153132,0.00007125969,0.00032466513,0.0007181801],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001535491,0.00033290035,0.06142127,0.00023155227,0.00035562183,0.00023523961,0.0047891266,0.0013572362,0.7996811,0.005504434,0.025102837,0.099453166],"study_design_scores_gemma":[0.00045489965,0.0002942904,0.9459788,0.00005914823,0.000021830709,9.540022e-7,0.0003221209,0.0015020709,0.028731294,0.012867472,0.009524895,0.00024220652],"about_ca_topic_score_codex":0.04120604,"about_ca_topic_score_gemma":0.0005281861,"teacher_disagreement_score":0.88455755,"about_ca_system_score_codex":0.000008193585,"about_ca_system_score_gemma":0.000033355627,"threshold_uncertainty_score":0.96517867},"labels":[],"label_agreement":null},{"id":"W2067555601","doi":"10.1063/1.3549593","title":"Structural and optical properties of liquid CO2 for pressures up to 1 TPa","year":2011,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"U.S. Department of Energy","keywords":"Shock (circulatory); Materials science; Phase transition; Shock wave; Thermodynamics; Carbon dioxide; Phase (matter); Range (aeronautics); Liquid phase; Equation of state; Reflectivity; Conductivity; Physical chemistry; Composite material; Optics; Chemistry; Organic chemistry; Physics","score_opus":0.034948298641269075,"score_gpt":0.21769929910849872,"score_spread":0.18275100046722964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067555601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99919736,0.00019703634,0.0000645752,0.00007450891,0.00018583552,0.0001001746,0.00002735562,0.0000026584055,0.00015050692],"genre_scores_gemma":[0.99907213,0.000009966878,0.0005500387,0.000042373053,0.00030717682,2.9090484e-7,0.0000011087313,0.0000028973159,0.000014006348],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994248,0.00002377765,0.00021642349,0.00005415702,0.00015384413,0.00012695884],"domain_scores_gemma":[0.9995187,0.00007431674,0.00013047337,0.00008468006,0.00011081572,0.00008103599],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018048477,0.000077559955,0.0002111419,0.000008817518,0.000031394145,0.000012877657,0.00019338971,0.000027726419,0.00003901327],"category_scores_gemma":[0.00004011598,0.000040426046,0.000046535486,0.000033497374,0.00011616455,0.00010611177,0.000020637299,0.0000668101,0.0000019117838],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002605186,0.00001760074,0.00023235228,0.00010713983,0.00009139724,7.023546e-7,0.0028555254,0.00020358701,0.9906992,0.00080787466,0.0005169506,0.0018625172],"study_design_scores_gemma":[0.00021920171,0.0004023205,0.0017204783,0.000037781483,0.00008483942,0.000008803499,0.000055393,0.00012214332,0.98977035,0.0073282546,0.0001736182,0.00007680826],"about_ca_topic_score_codex":0.000064139786,"about_ca_topic_score_gemma":0.0000017413423,"teacher_disagreement_score":0.0065203803,"about_ca_system_score_codex":7.300563e-7,"about_ca_system_score_gemma":0.00002134936,"threshold_uncertainty_score":0.16485263},"labels":[],"label_agreement":null},{"id":"W2067747516","doi":"10.1130/g24982a.1","title":"Mantle lithosphere delamination driving plateau uplift and synconvergent extension in eastern Anatolia","year":2008,"lang":"en","type":"article","venue":"Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":232,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"National Science Foundation","keywords":"Lithosphere; Geology; Mantle (geology); Delamination (geology); Citation; Tectonics; Paleontology; Library science; Computer science","score_opus":0.010885306192701411,"score_gpt":0.200878789293969,"score_spread":0.18999348310126757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067747516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99805963,0.00033968585,0.000068383684,0.0001319066,0.00045010826,0.00008107752,0.000004697754,0.000016626584,0.00084787875],"genre_scores_gemma":[0.998959,0.00020268766,0.00021866384,0.00006263156,0.00005112901,9.403084e-7,0.000033340213,0.0000022858749,0.00046930512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993171,0.000051958774,0.00014582193,0.00020360087,0.00007264252,0.00020889207],"domain_scores_gemma":[0.9997441,0.00003980803,0.000046400706,0.00009892614,0.000018462759,0.000052298674],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000117193405,0.00008256549,0.00015228549,0.00003949749,0.000077525896,0.000009252222,0.00006453197,0.00007550687,0.000934829],"category_scores_gemma":[0.000013812872,0.00007223298,0.000013502885,0.000060642622,0.000059434115,0.000098493634,0.000021127256,0.000054883934,0.00021417042],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016250167,0.000009803549,0.9934587,0.000011793712,0.000005521392,0.00012711501,0.00030610204,0.0004215621,0.000240777,0.00019277968,0.00015658437,0.0050530285],"study_design_scores_gemma":[0.00019814845,0.000050736635,0.9881808,0.000009724349,0.000003701343,0.000062686486,0.000034948724,0.0085807415,0.00014236207,0.0008395923,0.0018039057,0.00009266213],"about_ca_topic_score_codex":0.0035169474,"about_ca_topic_score_gemma":0.0034978685,"teacher_disagreement_score":0.008159179,"about_ca_system_score_codex":0.0000014958408,"about_ca_system_score_gemma":0.000014577077,"threshold_uncertainty_score":0.9999784},"labels":[],"label_agreement":null},{"id":"W2067781441","doi":"10.1103/physrevb.81.140104","title":"Consecutive Peierls distortions and high-pressure phase transitions in<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mrow><mml:mtext>YH</mml:mtext></mml:mrow><mml:mn>3</mml:mn></mml:msub></mml:mrow></mml:math>","year":2010,"lang":"lv","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Phase (matter); Crystal structure; Materials science; Crystallography; Thermodynamics; Phase transition; Physics; Transformation (genetics); Series (stratigraphy); Enthalpy; Algorithm; Computer science; Chemistry; Quantum mechanics; Geology","score_opus":0.015620165789186437,"score_gpt":0.25560603369550094,"score_spread":0.23998586790631452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067781441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.832541,0.0073090973,0.00028546678,0.0016832027,0.0027826468,0.00011706632,0.0031286792,0.00013696014,0.1520159],"genre_scores_gemma":[0.9858322,0.0063021616,0.00061759213,0.0014006161,0.002103197,0.0005443054,0.0027328583,0.00022005344,0.00024697895],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9933427,0.00049107935,0.0014451547,0.0014991617,0.0015209537,0.0017009327],"domain_scores_gemma":[0.99467945,0.0012721616,0.0012105086,0.0016225893,0.00014345319,0.0010718637],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012590721,0.000770333,0.00055224734,0.00020781897,0.0012415892,0.0008901793,0.0012908602,0.00097574794,0.21818832],"category_scores_gemma":[0.00086886145,0.001186745,0.001218239,0.0008525204,0.0016484343,0.001276624,0.00052994787,0.0014669104,0.0024666924],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066517765,0.0007142401,0.000016886697,0.0033101824,0.0010430332,0.00076308474,0.0020243411,0.00038259698,0.0070431787,0.87571037,0.10356705,0.0047598546],"study_design_scores_gemma":[0.0042768093,0.0035000918,0.0016138686,0.006483779,0.007186839,0.000976846,0.0011584362,0.13496624,0.75331515,0.0008616144,0.08182172,0.0038385757],"about_ca_topic_score_codex":0.002592698,"about_ca_topic_score_gemma":0.0030968082,"teacher_disagreement_score":0.8748488,"about_ca_system_score_codex":0.0000046040586,"about_ca_system_score_gemma":0.000896181,"threshold_uncertainty_score":0.99905825},"labels":[],"label_agreement":null},{"id":"W2068001720","doi":"10.1107/s0108767302092115","title":"First-principles studies of phase transitions at high pressure in SiO<sub>2</sub>","year":2002,"lang":"en","type":"article","venue":"Acta Crystallographica Section A Foundations of Crystallography","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"High pressure; Phase transition; Phase (matter); Materials science; Condensed matter physics; Thermodynamics; Physics; Quantum mechanics","score_opus":0.026135828225739823,"score_gpt":0.24088653703413745,"score_spread":0.21475070880839764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068001720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995508,0.00093164045,0.00020039568,0.0005480989,0.0005311695,0.0006118309,0.0008989787,0.00009391216,0.00067595515],"genre_scores_gemma":[0.99685216,0.0021292295,0.0004897068,0.000034627268,0.00008643522,0.000035384284,0.0003337413,0.00001611392,0.000022605076],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973045,0.00021069335,0.0010165136,0.00053027103,0.0004950045,0.0004430152],"domain_scores_gemma":[0.99810725,0.00034720314,0.0005408638,0.0005314848,0.0003321945,0.00014099995],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040444007,0.00035095547,0.0006889506,0.0013496046,0.00044032108,0.000053731186,0.00034552233,0.0002084282,0.0011258153],"category_scores_gemma":[0.00009477893,0.00033898224,0.00039145333,0.0021545852,0.00076710747,0.000604097,0.000045202283,0.00019891249,0.0000020537934],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040398157,0.0016933595,0.027952397,0.00085279124,0.0014867309,0.000015572223,0.0026693956,0.031258196,0.93017244,0.0014926417,0.0011654319,0.0008370744],"study_design_scores_gemma":[0.014784791,0.005001726,0.66229045,0.0010386239,0.002247792,0.00009997761,0.0028189544,0.01882271,0.010265107,0.021614771,0.25775245,0.003262623],"about_ca_topic_score_codex":0.00056512316,"about_ca_topic_score_gemma":0.0102927685,"teacher_disagreement_score":0.91990733,"about_ca_system_score_codex":0.000008158921,"about_ca_system_score_gemma":0.000025503019,"threshold_uncertainty_score":0.99990624},"labels":[],"label_agreement":null},{"id":"W2068038420","doi":"10.1144/gsl.sp.2006.253.01.04","title":"Surface topography and internal strain variation in wide hot orogens from three-dimensional analogue and two-dimensional numerical vice models","year":2006,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Variation (astronomy); Surface (topology); Strain (injury); Geology; Versa; Geodesy; Geometry; Mathematics; Physics; Computer science; Biology; Anatomy","score_opus":0.013709515188389124,"score_gpt":0.2095683593601631,"score_spread":0.195858844171774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068038420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932461,0.00024466438,0.0018772808,0.002413057,0.00017503764,0.00022622223,0.0008684904,0.000051228108,0.0008979611],"genre_scores_gemma":[0.9895559,0.000019200725,0.00810599,0.0004926741,0.0006427021,0.0000047938793,0.0011218763,0.0000042674474,0.00005257954],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983373,0.0001083239,0.0003728512,0.00052509876,0.00031057574,0.00034581465],"domain_scores_gemma":[0.9991227,0.00035251045,0.00012309113,0.00015387185,0.000094496965,0.00015336972],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032514645,0.00019342292,0.00028658105,0.000042110314,0.00025621254,0.00016715379,0.00016339164,0.00016454722,0.0017043276],"category_scores_gemma":[0.00003107643,0.0001610878,0.00009719894,0.00036139713,0.00022785328,0.0003735523,0.00007058782,0.00020570275,0.000023954488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014487187,0.00036779937,0.7722754,0.000010729131,0.00013706025,0.000011224539,0.00033056128,0.1769276,0.0035862483,0.035690457,0.008443968,0.0020740735],"study_design_scores_gemma":[0.0004757277,0.000039869203,0.8765225,0.0000046191785,0.000019350893,0.0000037334673,0.000011708721,0.051181834,0.000012148361,0.07049908,0.0010459793,0.00018348258],"about_ca_topic_score_codex":0.02096535,"about_ca_topic_score_gemma":0.00954611,"teacher_disagreement_score":0.12574576,"about_ca_system_score_codex":0.000008772792,"about_ca_system_score_gemma":0.000048138638,"threshold_uncertainty_score":0.9992083},"labels":[],"label_agreement":null},{"id":"W2068081664","doi":"10.1103/physrevb.64.224101","title":"Non-Arrhenius stretched exponential dielectric relaxation in antiferromagnetic<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">TiBO</mml:mi></mml:mrow><mml:mrow><mml:mn>3</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math>single crystals","year":2001,"lang":"lv","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Arrhenius equation; Dielectric; Relaxation (psychology); Cole–Cole equation; Parameterized complexity; Exponential function; Materials science; Spectral line; Thermodynamics; Antiferromagnetism; Condensed matter physics; Physics; Nuclear magnetic resonance; Mathematics; Mathematical analysis; Quantum mechanics; Algorithm; Kinetics","score_opus":0.014965198475797366,"score_gpt":0.23892949287912263,"score_spread":0.22396429440332527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068081664","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.65447414,0.0021577964,0.0002605495,0.0010074949,0.0020053883,0.00006545943,0.00039002884,0.000104221035,0.33953494],"genre_scores_gemma":[0.9866248,0.0036488117,0.00068422785,0.0026868558,0.0025080272,0.0005259195,0.0023985694,0.00040370983,0.00051911536],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99082786,0.00065748283,0.0020177115,0.0017851721,0.0022574663,0.0024543274],"domain_scores_gemma":[0.9935005,0.0013146001,0.002073084,0.0019669277,0.00016322012,0.0009817107],"candidate_categories":["metaepi_narrow","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0017283662,0.000906229,0.0005326944,0.0004035908,0.0009552428,0.0014991905,0.0017387812,0.0013615914,0.7197184],"category_scores_gemma":[0.0008943519,0.0015912695,0.0014959608,0.0012955908,0.0010162838,0.0016256556,0.0009168566,0.0013240416,0.006406729],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027481206,0.0010401951,0.00011045028,0.0060377396,0.0018962235,0.0038081433,0.002993694,0.0013550749,0.054735254,0.21722342,0.7032767,0.0047749695],"study_design_scores_gemma":[0.0018402125,0.0018081251,0.0012856981,0.0024857244,0.0017869791,0.00081739,0.00039784322,0.042189475,0.9393358,0.00014766993,0.006072965,0.0018320845],"about_ca_topic_score_codex":0.0026564638,"about_ca_topic_score_gemma":0.0013808624,"teacher_disagreement_score":0.8846006,"about_ca_system_score_codex":0.000008727569,"about_ca_system_score_gemma":0.00091674435,"threshold_uncertainty_score":0.99993485},"labels":[],"label_agreement":null},{"id":"W2068100876","doi":"10.1016/j.epsl.2009.01.020","title":"Subduction adjacent to deep continental roots: Enhanced negative pressure in the mantle wedge, mountain building and continental motion","year":2009,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"National Science Foundation","keywords":"Geology; Subduction; Mantle wedge; Lithosphere; Mantle (geology); Wedge (geometry); Plate tectonics; Convergent boundary; Mantle convection; Continental collision; Hotspot (geology); Geophysics; Seismology; Tectonics; Oceanic crust; Geometry","score_opus":0.004963004980585257,"score_gpt":0.19607510074360981,"score_spread":0.19111209576302457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068100876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958513,0.00025574098,0.00020677676,0.0026310093,0.0003105202,0.00040777092,0.000071764625,0.000017466942,0.00024767366],"genre_scores_gemma":[0.9967416,0.00003126453,0.0005416739,0.002427449,0.00015888205,0.0000013475977,0.00007570085,0.0000016452759,0.000020425696],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985995,0.00009535911,0.00018395741,0.00039823627,0.00032355633,0.00039935517],"domain_scores_gemma":[0.99958676,0.00007188002,0.00006479373,0.00012765327,0.0000144064,0.00013448906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054824573,0.00016124653,0.00017109854,0.00012295418,0.00029482052,0.00024692962,0.00021289001,0.000034586617,0.00012543736],"category_scores_gemma":[0.000027905682,0.00011737509,0.00001706279,0.0002776196,0.00018916896,0.00056084566,0.000013313954,0.00012412938,0.00002813041],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067034,0.0000952354,0.2861669,0.000070015834,0.00003749049,0.000115770286,0.007938824,0.030308817,0.5966586,0.00035212078,0.0017507237,0.07583517],"study_design_scores_gemma":[0.000353657,0.00014927328,0.9897306,0.000021232921,0.000012162115,0.000030209041,0.00027474723,0.003424336,0.0042041996,0.000100135,0.001521593,0.00017786257],"about_ca_topic_score_codex":0.0017706433,"about_ca_topic_score_gemma":0.000983961,"teacher_disagreement_score":0.7035637,"about_ca_system_score_codex":0.000002068654,"about_ca_system_score_gemma":0.000010913332,"threshold_uncertainty_score":0.47864172},"labels":[],"label_agreement":null},{"id":"W2068465863","doi":"10.1029/2007gl031396","title":"Effect of lower mantle viscosity on the time‐dependence of plate velocities in three‐dimensional mantle convection models","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Mantle convection; Mantle (geology); Geology; Geophysics; Convection; Viscosity; Earth's internal heat budget; Plate tectonics; Mechanics; Thermodynamics; Physics; Lithosphere; Seismology","score_opus":0.022327623940491547,"score_gpt":0.2707042091419947,"score_spread":0.24837658520150319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068465863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99807334,0.000016181997,0.00006451337,0.00042190216,0.00016043919,0.00031845804,0.000057001977,0.000008378568,0.00087976345],"genre_scores_gemma":[0.9996789,0.0000034223276,0.000024945624,0.00009110782,0.0000995614,0.0000027413926,0.000016652759,0.0000045360803,0.00007810443],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99778384,0.00034652016,0.00023707983,0.0002468782,0.0009274214,0.000458285],"domain_scores_gemma":[0.99736845,0.0021776848,0.00007040072,0.00024548877,0.00006791387,0.00007008506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025133665,0.00012594728,0.0002693616,0.00012046442,0.0001152275,0.000024707722,0.00029379094,0.000056227283,0.00035869094],"category_scores_gemma":[0.00008166302,0.00007984926,0.00007504561,0.00027901668,0.00037190432,0.00015031207,0.000051107698,0.00030345013,0.00027249375],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008680623,0.00036450813,0.0049280096,0.0004076532,0.00016547562,0.00024977914,0.00062482315,0.046217866,0.9197435,0.006415528,0.00361679,0.00858549],"study_design_scores_gemma":[0.0017876371,0.0047682514,0.36574996,0.00048097273,0.000038664195,0.00000644094,0.000060642742,0.10517616,0.50083435,0.020276742,0.00021061825,0.0006095668],"about_ca_topic_score_codex":0.00612659,"about_ca_topic_score_gemma":0.00029983622,"teacher_disagreement_score":0.41890907,"about_ca_system_score_codex":0.000008535073,"about_ca_system_score_gemma":0.000029169114,"threshold_uncertainty_score":0.9261613},"labels":[],"label_agreement":null},{"id":"W2068626653","doi":"10.1016/j.lithos.2008.05.008","title":"Thermal evolution of cratonic roots","year":2008,"lang":"my","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Archean; Geology; Crust; Craton; Mantle (geology); Terrane; Proterozoic; Continental crust; Lithosphere; Geochemistry; Petrology; Earth's internal heat budget; Radiogenic nuclide; Earth science; Mantle convection; Tectonics; Paleontology","score_opus":0.011762416534742012,"score_gpt":0.19509271262254374,"score_spread":0.18333029608780171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068626653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884532,0.0027390302,0.00004947414,0.00007430007,0.0010112628,0.00017664675,0.0002766639,0.000022549864,0.007196846],"genre_scores_gemma":[0.99704707,0.00015280575,0.00021675536,0.0000272318,0.0004456584,0.0000012292877,0.000038246242,0.00000557747,0.0020654218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986946,0.00014001575,0.00031259615,0.00024349864,0.0002754016,0.0003338783],"domain_scores_gemma":[0.99932045,0.000058986152,0.00016319162,0.00029143578,0.00005859817,0.00010735661],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002065191,0.00015865604,0.00029991596,0.000047919995,0.00017174431,0.000022865705,0.00022977099,0.000117710515,0.0033572302],"category_scores_gemma":[0.000017523478,0.00013365556,0.000091310496,0.00017106153,0.00014351742,0.00019261922,0.000023939296,0.00009030514,0.0008805255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027177064,0.00022226939,0.9585249,0.0003260763,0.0001842649,0.00011243718,0.0029659565,0.0019116903,0.0203669,0.0027376534,0.0037993614,0.008576755],"study_design_scores_gemma":[0.00028609103,0.0002062018,0.97940344,0.000048138634,0.00004021977,0.000008772945,0.00003538764,0.0012780452,0.0036540367,0.000311787,0.014535336,0.00019254092],"about_ca_topic_score_codex":0.008948279,"about_ca_topic_score_gemma":0.00019279872,"teacher_disagreement_score":0.020878578,"about_ca_system_score_codex":0.000004008377,"about_ca_system_score_gemma":0.00016819804,"threshold_uncertainty_score":0.9998974},"labels":[],"label_agreement":null},{"id":"W2069249891","doi":"10.1021/jp068287v","title":"High-pressure Induced Conformational and Phase Transformations of 1,2-Dichloroethane Probed by Raman Spectroscopy","year":2007,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Raman spectroscopy; Phase (matter); Lattice (music); Diamond anvil cell; Spectroscopy; Chemistry; Crystallography; Phase transition; High pressure; Materials science; Condensed matter physics; Thermodynamics; Optics; Organic chemistry","score_opus":0.006813448366188212,"score_gpt":0.23831671971144927,"score_spread":0.23150327134526105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069249891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830633,0.00010675131,0.00039036444,0.00017423852,0.00005224233,0.00007699083,0.00019276988,0.0000049064224,0.0006954128],"genre_scores_gemma":[0.99950004,0.000018116125,0.00009440958,0.000023320352,0.00029056906,1.5398588e-7,0.000046014542,0.0000023358334,0.000025049803],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991073,0.00002622443,0.0003531998,0.000050830527,0.00030487074,0.00015756891],"domain_scores_gemma":[0.99923617,0.00015718307,0.0003175644,0.00009107472,0.00009197723,0.00010601542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047231666,0.00010225253,0.00023791924,0.000015313208,0.000074111624,0.000023403585,0.0001971085,0.000041145762,0.00026752034],"category_scores_gemma":[0.000019400299,0.00006370902,0.00005217037,0.00008049252,0.000098353514,0.00023182215,0.0000067606175,0.00017414553,0.0000036780539],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027234587,0.0000837316,0.000024283056,0.00007235961,0.00006023322,0.0000010424305,0.0006548148,0.00022316226,0.99750054,0.000064764245,0.00033039352,0.00071234244],"study_design_scores_gemma":[0.0010601531,0.00022606345,0.00097577577,0.00002331497,0.000102082435,0.000020487461,0.0001204438,0.00058585766,0.9950719,0.0011465814,0.00058509375,0.00008224737],"about_ca_topic_score_codex":0.000074100375,"about_ca_topic_score_gemma":0.0000034843915,"teacher_disagreement_score":0.0024286283,"about_ca_system_score_codex":0.0000017669327,"about_ca_system_score_gemma":0.00003729566,"threshold_uncertainty_score":0.29291603},"labels":[],"label_agreement":null},{"id":"W2072008803","doi":"10.1016/j.jog.2004.05.002","title":"Time evolution of negative buoyancy of an oceanic slab subducting with varying velocity","year":2004,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Slab; Buoyancy; Eclogitization; Lithosphere; Mantle (geology); Geophysics; Slab window; Oceanic crust; Seismology; Mechanics; Tectonics; Physics","score_opus":0.004835572563951889,"score_gpt":0.1892266465600781,"score_spread":0.1843910739961262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072008803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982804,0.00008549664,0.0009430678,0.000023943425,0.00018200616,0.000057363308,0.000056430727,0.000004150845,0.00036713303],"genre_scores_gemma":[0.9933555,0.000015997048,0.0064766384,0.000004813314,0.000120407785,3.7777742e-8,0.00000979699,0.0000036770841,0.0000131156485],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990454,0.000052153508,0.0003901603,0.00008625838,0.0002795338,0.00014654495],"domain_scores_gemma":[0.9987858,0.000053107695,0.0007375479,0.00010109894,0.000255556,0.00006686852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039686807,0.000092195056,0.00029083525,0.000078669415,0.00006028081,0.0000151631975,0.00016512364,0.00004557526,0.00010239451],"category_scores_gemma":[0.00003822485,0.00006863334,0.000052514573,0.0001568544,0.0000801206,0.00041269063,0.0000082030765,0.00011336252,0.0000052734545],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017906855,0.00043204785,0.026294127,0.0004098901,0.0005539482,0.00014437464,0.004484105,0.8195418,0.13465631,0.0018562693,0.00001925394,0.009817207],"study_design_scores_gemma":[0.005864873,0.0067919553,0.79814583,0.0010864037,0.0005662025,0.0006740064,0.0015315475,0.10359507,0.031117553,0.04967637,0.000052823496,0.0008973655],"about_ca_topic_score_codex":0.0009259193,"about_ca_topic_score_gemma":0.00014524833,"teacher_disagreement_score":0.7718517,"about_ca_system_score_codex":0.0000140117245,"about_ca_system_score_gemma":0.0001910029,"threshold_uncertainty_score":0.27987862},"labels":[],"label_agreement":null},{"id":"W2072924052","doi":"10.1007/s00410-010-0528-9","title":"Growth of diamond in hydrous silicate melts","year":2010,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Diamond; Mantle (geology); Silicate; Geology; Lithosphere; Crystallization; Geochemistry; Dissolution; Mineralogy; Chemical engineering; Materials science; Composite material; Tectonics","score_opus":0.003843839926191324,"score_gpt":0.21893342144374495,"score_spread":0.2150895815175536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072924052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99590105,0.00012546602,0.000056844696,0.001701147,0.00041867924,0.000107936474,0.00057036144,0.000010226995,0.001108269],"genre_scores_gemma":[0.9993055,0.000018155217,0.00011251068,0.00022490737,0.00010917251,0.0000045860343,0.0001219187,0.0000015513164,0.00010170739],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99924463,0.00007657556,0.00019825516,0.00018305298,0.0000413577,0.0002561008],"domain_scores_gemma":[0.9994912,0.00017584822,0.00004614212,0.00012819181,0.000062780324,0.00009580671],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025151236,0.00008580127,0.00025184092,0.00011312207,0.000058839574,0.000008167443,0.0001126446,0.00012495928,0.00045031228],"category_scores_gemma":[0.00013708453,0.000073404924,0.000023158895,0.00012729385,0.00013823382,0.000051059502,0.000016603562,0.00013131363,0.00006197357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026153793,0.00008642272,0.6955173,0.000022208724,0.00005252269,0.000039369912,0.000276593,0.00023026124,0.25232387,0.04760015,0.0014884714,0.002101321],"study_design_scores_gemma":[0.00064137427,0.00024176473,0.97901005,0.0000024337526,0.00002175829,0.00002614668,0.0000033943368,0.00029605057,0.002320161,0.009851417,0.007460128,0.00012535401],"about_ca_topic_score_codex":0.00353547,"about_ca_topic_score_gemma":0.014793896,"teacher_disagreement_score":0.28349274,"about_ca_system_score_codex":8.489864e-7,"about_ca_system_score_gemma":0.000025392488,"threshold_uncertainty_score":0.8255341},"labels":[],"label_agreement":null},{"id":"W2073044435","doi":"10.1103/physrevlett.107.015702","title":"Direct Measurement of Microstructural Avalanches during the Martensitic Transition of Cobalt Using Coherent X-Ray Scattering","year":2011,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Scattering; Materials science; Condensed matter physics; Diffusionless transformation; Phase (matter); Martensite; Microscale chemistry; Phase transition; Amplitude; Cobalt; Physics; Optics; Microstructure; Metallurgy","score_opus":0.03188186118854304,"score_gpt":0.2233705123846724,"score_spread":0.19148865119612934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073044435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978396,0.0014658169,0.000028902465,0.00016214504,0.00014254448,0.0002537856,0.000047167545,0.000008082941,0.000051901367],"genre_scores_gemma":[0.9992061,0.00020539235,0.000120376,0.00036920133,0.000085705804,0.0000016509222,0.0000073768274,0.0000037820596,4.0525055e-7],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99902207,0.00012466007,0.00026023228,0.00014522181,0.00027391085,0.00017393436],"domain_scores_gemma":[0.99954724,0.000028572911,0.00016001008,0.00017778335,0.000048710997,0.00003766152],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022764331,0.00012237621,0.00037285752,0.00001451948,0.00005600586,0.000008952025,0.0001378379,0.000006486426,0.00012768782],"category_scores_gemma":[0.00000866894,0.00007656878,0.00012651974,0.00008098482,0.00010937612,0.00007992904,0.000009239643,0.0000475555,0.000009774103],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021692615,0.000017025752,0.0011023813,0.001605026,0.00005495713,0.0000021644757,0.00050155324,0.0006095374,0.99562025,0.0000034068944,0.000031956126,0.00043002542],"study_design_scores_gemma":[0.00037659213,0.00009872036,0.70749986,0.0035037317,0.0005272842,0.000010483946,0.000035048557,0.0014662184,0.2858423,0.00007687609,0.00017108997,0.00039182196],"about_ca_topic_score_codex":0.0008420703,"about_ca_topic_score_gemma":0.000018473842,"teacher_disagreement_score":0.709778,"about_ca_system_score_codex":0.0000045895704,"about_ca_system_score_gemma":0.0000099679,"threshold_uncertainty_score":0.31223843},"labels":[],"label_agreement":null},{"id":"W2074019545","doi":"10.1016/j.jvolgeores.2005.04.010","title":"Heat flow, heat transfer and lithosphere rheology in geothermal areas: Features and examples","year":2005,"lang":"en","type":"article","venue":"Journal of Volcanology and Geothermal Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geothermal gradient; Geology; Lithosphere; Heat transfer; Geothermal energy; Convective heat transfer; Geophysics; Petrology; Convection; Crust; Borehole; Mechanics; Geotechnical engineering; Seismology; Tectonics","score_opus":0.022049299935532337,"score_gpt":0.2746393258981594,"score_spread":0.2525900259626271,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074019545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98355025,0.012878106,0.000012259943,0.0025429262,0.00010266482,0.000110172936,0.000024688412,0.000004906924,0.00077401113],"genre_scores_gemma":[0.9954439,0.0035391268,0.00016647084,0.00020398412,0.00030718878,0.0000011446436,0.0000033002902,0.000006190577,0.00032871283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982879,0.00043521042,0.0003112071,0.00022826558,0.00023282353,0.0005045855],"domain_scores_gemma":[0.99919677,0.00040930219,0.000015108789,0.00010317192,0.000083842984,0.00019178119],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012894983,0.00014644522,0.00037888717,0.000186287,0.00016621857,0.00007120695,0.00016166085,0.00020707274,0.0014260885],"category_scores_gemma":[0.00006026143,0.00010605616,0.000031478467,0.00011165225,0.0005555412,0.00025191298,0.000030401881,0.0005098465,0.000009408481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033116671,0.0001807262,0.7803585,0.0002087838,0.0002529656,0.0005644225,0.004409596,0.002998231,0.01916859,0.0017803535,0.0014100686,0.18535613],"study_design_scores_gemma":[0.001236213,0.00061954785,0.9850575,0.000058827,0.00001539917,0.0007040121,0.00022939559,0.001324273,0.00076251075,0.00077987474,0.0090616625,0.00015080122],"about_ca_topic_score_codex":0.0028261386,"about_ca_topic_score_gemma":0.00554501,"teacher_disagreement_score":0.20469902,"about_ca_system_score_codex":0.000004545928,"about_ca_system_score_gemma":0.00007661739,"threshold_uncertainty_score":0.99948674},"labels":[],"label_agreement":null},{"id":"W2075280618","doi":"10.1029/2004jb003382","title":"High‐velocity lid of East Antarctica: Evidence of a depleted continental lithosphere","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; U.S. Geological Survey","keywords":"Lithosphere; Geology; Mantle (geology); Low-velocity zone; Geophysics; Seismology; Tectonics","score_opus":0.04012262263014144,"score_gpt":0.30570446414022145,"score_spread":0.26558184151008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075280618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971067,0.0014178662,0.000058926224,0.00056543504,0.00020688462,0.00017991624,0.000070956696,0.0000075161934,0.00038581245],"genre_scores_gemma":[0.9930271,0.00028798252,0.0057068104,0.000022831244,0.00080783456,8.434814e-7,0.0000046071787,0.000008475298,0.00013355367],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99620974,0.00045590868,0.0008939932,0.00023634917,0.0016538645,0.0005501727],"domain_scores_gemma":[0.9964695,0.001177433,0.00057528424,0.00030504065,0.001138074,0.00033469463],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014804631,0.00019015178,0.00075275335,0.000028924149,0.00011744077,0.000070523674,0.00073054817,0.000097760785,0.002211738],"category_scores_gemma":[0.00080561364,0.00013740947,0.00025589537,0.000522739,0.0005178927,0.0006208871,0.00008721264,0.0005034799,0.000085207656],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01747824,0.0036164527,0.2863734,0.0022285548,0.0019126544,0.00044509795,0.0031824813,0.0054783653,0.36556348,0.006938981,0.02377637,0.2830059],"study_design_scores_gemma":[0.0017812526,0.0046807695,0.9102679,0.0012663875,0.00011444432,0.000041666004,0.0007242908,0.002226784,0.069489256,0.0046082116,0.0044101826,0.00038889115],"about_ca_topic_score_codex":0.009868748,"about_ca_topic_score_gemma":0.00086205924,"teacher_disagreement_score":0.62389445,"about_ca_system_score_codex":0.0000150007045,"about_ca_system_score_gemma":0.00040760808,"threshold_uncertainty_score":0.9987004},"labels":[],"label_agreement":null},{"id":"W2075502267","doi":"10.1007/s004100000181","title":"Experimental investigation of large-ion-lithophile-element-, high-field-strength-element- and rare-earth-element-partitioning between calcic amphibole and basaltic melt: the effects of pressure and oxygen fugacity","year":2000,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":119,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Amphibole; Mineral redox buffer; Analytical Chemistry (journal); Partition coefficient; Ionic radius; Trace element; Lile; Alkali metal; Electron microprobe; Mineralogy; Geology; Chemistry; Basalt; Partial melting; Mantle (geology); Ion; Geochemistry; Quartz","score_opus":0.005395588409158378,"score_gpt":0.23322699926520138,"score_spread":0.227831410856043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075502267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940419,0.002912621,0.00011723872,0.0012479738,0.0001224794,0.00039414022,0.0011197579,0.000011209483,0.000032683543],"genre_scores_gemma":[0.99882805,0.00017429708,0.00012215425,0.0002753236,0.00012646978,0.000019469444,0.00038537552,0.0000033695758,0.00006546747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986747,0.00030585137,0.00033290236,0.00028212706,0.00010142283,0.00030299253],"domain_scores_gemma":[0.9990706,0.00047652228,0.00011312674,0.00014168907,0.000057485067,0.00014061623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035302574,0.00015798231,0.0003636784,0.00007088139,0.0003087815,0.000029554696,0.0000767949,0.00011450646,0.0005151382],"category_scores_gemma":[0.00006820165,0.00012603564,0.000023927785,0.00009412195,0.00023964257,0.0001229597,0.000043400283,0.0000959694,0.0000029415228],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006109588,0.00013702124,0.82191324,0.00047439887,0.0008503935,0.000013260997,0.002755611,0.00027585635,0.15038295,0.01398195,0.0016230601,0.006981267],"study_design_scores_gemma":[0.002389894,0.0013282371,0.94773716,0.000044571705,0.00034966014,0.000011748175,0.00007498359,0.00058271975,0.03925225,0.0015995792,0.0064150332,0.00021416238],"about_ca_topic_score_codex":0.0012749188,"about_ca_topic_score_gemma":0.00051495194,"teacher_disagreement_score":0.12582389,"about_ca_system_score_codex":0.000001674075,"about_ca_system_score_gemma":0.000023142515,"threshold_uncertainty_score":0.5640402},"labels":[],"label_agreement":null},{"id":"W2075707259","doi":"10.1103/physrevb.75.134104","title":"Electron-phonon coupling in the high-pressure hcp phase of xenon: A first-principles study","year":2007,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Condensed matter physics; Pseudopotential; Physics; Superconductivity; Phonon; Anisotropy; Coulomb; Fermi surface; Lattice (music); Electron; Quantum mechanics","score_opus":0.027989368087841967,"score_gpt":0.3141242999765324,"score_spread":0.28613493188869044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075707259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98845214,0.009692622,0.000022156599,0.00015896774,0.000120630546,0.00078491576,0.000043636635,0.000014399743,0.00071053684],"genre_scores_gemma":[0.99805075,0.0014301382,0.000028929931,0.0001582584,0.000272522,0.0000075977955,0.000033434055,0.0000045298807,0.000013858074],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985414,0.000090747504,0.00039361432,0.0002547777,0.0003842651,0.0003351509],"domain_scores_gemma":[0.9989652,0.00039993165,0.00016518404,0.00036791968,0.000040152423,0.000061628016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001308391,0.00016709632,0.00051007967,0.000028416922,0.00008104227,0.000027385046,0.00043495875,0.000021872153,0.00020365714],"category_scores_gemma":[0.00007831648,0.00010168303,0.000090993744,0.00033731895,0.000043830732,0.00010308925,0.000023510815,0.00015097886,0.00008099503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005050502,0.052708484,0.3180205,0.04466969,0.0031921053,0.0014371687,0.029736785,0.25405958,0.03314896,0.08466006,0.012640626,0.16067556],"study_design_scores_gemma":[0.0061564352,0.0059505072,0.7240654,0.0034662113,0.0016882478,0.000012439067,0.00053687056,0.03556286,0.010727575,0.009515783,0.20046972,0.0018479185],"about_ca_topic_score_codex":0.0016224358,"about_ca_topic_score_gemma":0.0010507386,"teacher_disagreement_score":0.40604493,"about_ca_system_score_codex":0.0000020672942,"about_ca_system_score_gemma":0.000025920901,"threshold_uncertainty_score":0.41465136},"labels":[],"label_agreement":null},{"id":"W2076373492","doi":"10.1103/physrevlett.85.5130","title":"Phonon Anomaly in High-Pressure Zn","year":2000,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Phonon; Anomaly (physics); Condensed matter physics; Materials science; Physics","score_opus":0.008109875462964412,"score_gpt":0.2244212293145564,"score_spread":0.216311353851592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076373492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890854,0.005045886,0.0000024523247,0.003201908,0.00017045619,0.00027340715,0.00007092914,0.00003503191,0.0021145653],"genre_scores_gemma":[0.9863798,0.0031969363,0.000074358584,0.00978971,0.00037667714,0.0000062312674,0.00007791761,0.000005839194,0.00009252592],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987566,0.00013264899,0.00023383035,0.0003109736,0.00022528574,0.0003406917],"domain_scores_gemma":[0.99948496,0.00007449644,0.000054409935,0.00027874028,0.000009247278,0.00009816358],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016504909,0.00017813394,0.00044405845,0.000024122155,0.000046347846,0.000041215364,0.00027105783,0.0000130107655,0.006675557],"category_scores_gemma":[0.000010779617,0.00013813691,0.00009846663,0.00022121175,0.000048857506,0.00020255658,0.000009310168,0.00012312483,0.00256951],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004224931,0.0010130649,0.076506786,0.0092007965,0.0004842011,0.00059186213,0.0009606759,0.063640036,0.044864185,0.001627948,0.18447854,0.61620945],"study_design_scores_gemma":[0.00064010115,0.00011595069,0.4493654,0.001166628,0.00017863286,0.0000052912565,0.0000022683776,0.0024501716,0.00047649632,0.000912757,0.54391557,0.00077073945],"about_ca_topic_score_codex":0.001807983,"about_ca_topic_score_gemma":0.00007649883,"teacher_disagreement_score":0.6154387,"about_ca_system_score_codex":0.0000020197056,"about_ca_system_score_gemma":0.00001177433,"threshold_uncertainty_score":0.9982071},"labels":[],"label_agreement":null},{"id":"W2076573064","doi":"10.1016/j.gca.2010.07.005","title":"Majoritic garnet: A new approach to pressure estimation of shock events in meteorites and the encapsulation of sub-lithospheric inclusions in diamond","year":2010,"lang":"en","type":"article","venue":"Geochimica et Cosmochimica Acta","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Japan Society for the Promotion of Science; National Science Foundation","keywords":"Chondrite; Meteorite; Pyroxene; Coesite; Geology; Mineralogy; Diamond; Olivine; Chemistry; Analytical Chemistry (journal); Geochemistry; Eclogite; Astrobiology","score_opus":0.007390557844487826,"score_gpt":0.21962309286336926,"score_spread":0.21223253501888142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076573064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736017,0.000073164905,0.00010221455,0.00064958073,0.00015673426,0.00067920744,0.00011199334,0.000010498528,0.0008564638],"genre_scores_gemma":[0.9947285,0.000038377082,0.0049466,0.000075585805,0.000034012202,0.000009234222,0.00011895455,0.0000062381805,0.000042509728],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99849564,0.00023072108,0.00046990218,0.0002992074,0.00026232252,0.00024218568],"domain_scores_gemma":[0.9989817,0.00038628318,0.00018027781,0.0003169983,0.000037004833,0.00009769468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007881674,0.00016827554,0.00040775503,0.00012047713,0.000056606055,0.000024223898,0.00030438649,0.0001062268,0.00010696362],"category_scores_gemma":[0.00031321082,0.00012505132,0.00004766144,0.0003917276,0.000098018005,0.00019952931,0.00008776191,0.0002172911,0.0000049020587],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029781256,0.0012979333,0.20447508,0.0011709011,0.0002856045,0.000004289706,0.0276261,0.08645329,0.63483816,0.018453358,0.0017359613,0.020681193],"study_design_scores_gemma":[0.001571549,0.00006853008,0.92193943,0.00008149474,0.000069498485,0.0000048287757,0.00006452799,0.04414567,0.005420908,0.026199978,0.0001995508,0.00023400258],"about_ca_topic_score_codex":0.0049137953,"about_ca_topic_score_gemma":0.0026949763,"teacher_disagreement_score":0.7174644,"about_ca_system_score_codex":0.0000021121555,"about_ca_system_score_gemma":0.00007907844,"threshold_uncertainty_score":0.7428222},"labels":[],"label_agreement":null},{"id":"W2076736646","doi":"10.1038/nature05174","title":"Observation of an O8 molecular lattice in the ɛ phase of solid oxygen","year":2006,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":171,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Engineering and Physical Sciences Research Council","keywords":"Solid oxygen; Oxygen; Crystallography; Molecule; Crystal structure; Raman spectroscopy; Monoclinic crystal system; Chemistry; Phase (matter); Materials science; Chemical physics; Physics; Optics","score_opus":0.010520150041051822,"score_gpt":0.2533452974649686,"score_spread":0.24282514742391675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076736646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983629,0.00031353498,0.00000751753,0.0001390098,0.00008893852,0.00007859743,0.00017104675,0.0000033551726,0.0008351098],"genre_scores_gemma":[0.9991676,0.0000031393329,0.0003735885,0.00017978862,0.000059830978,3.0389572e-7,0.00019389408,0.0000010675079,0.000020771355],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9995375,0.000055704328,0.00011474568,0.000070483875,0.00014905573,0.00007247159],"domain_scores_gemma":[0.9997477,0.000029320725,0.00006299246,0.0001196156,0.000030759165,0.000009625662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019622379,0.000042783748,0.00008769889,0.00002026475,0.000014303187,0.000007801673,0.00014438303,0.00014803301,0.00007800117],"category_scores_gemma":[0.00001195266,0.000027860871,0.000017867946,0.0001216448,0.000015904252,0.00008492503,0.0000026043194,0.00014018378,0.0000030529493],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039048606,0.00078563194,0.042551816,0.00032271587,0.000055665754,0.000092179835,0.0020015722,0.02024343,0.8951162,0.01622317,0.003782385,0.018434742],"study_design_scores_gemma":[0.0008120448,0.00022299986,0.8725964,0.000022914166,0.000030718915,0.0000020899822,0.00009030905,0.0024397045,0.10293507,0.012179721,0.008536534,0.00013151739],"about_ca_topic_score_codex":0.0017133728,"about_ca_topic_score_gemma":0.00063576165,"teacher_disagreement_score":0.83004457,"about_ca_system_score_codex":3.4279918e-7,"about_ca_system_score_gemma":0.000011697732,"threshold_uncertainty_score":0.25901186},"labels":[],"label_agreement":null},{"id":"W2077137667","doi":"10.1103/physrevb.65.104104","title":"Symmetry-general least-squares extraction of elastic data for strained materials from<i>ab initio</i>calculations of stress","year":2002,"lang":"en","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1329,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Ab initio; Hydrostatic pressure; Ab initio quantum chemistry methods; Elastic modulus; Materials science; Symmetry (geometry); Elastic energy; Triclinic crystal system; Physics; Thermodynamics; Quantum mechanics; Mathematics; Geometry","score_opus":0.04612410442990759,"score_gpt":0.30718964319126413,"score_spread":0.2610655387613565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077137667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97297233,0.0013398611,0.0009141431,0.0007005079,0.00046233105,0.00069795485,0.022319356,0.000023221673,0.0005702982],"genre_scores_gemma":[0.9951663,0.0004016705,0.0005952165,0.00035137282,0.00039433877,0.0000110135425,0.0029877208,0.000010755947,0.00008158996],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9984806,0.00013669611,0.0005438882,0.00034144465,0.00026756566,0.0002297865],"domain_scores_gemma":[0.9984445,0.00045318238,0.00035924534,0.0005718678,0.00009266394,0.000078535166],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016499996,0.00018864262,0.0006211531,0.000040530307,0.00005534974,0.00003901852,0.00034227895,0.000045454097,0.009477282],"category_scores_gemma":[0.00007462967,0.00015523632,0.000105260944,0.00011392496,0.00008696577,0.00029950755,0.00003616563,0.000059629514,0.00028220762],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021070559,0.000773625,0.00305746,0.007427148,0.0005263243,0.0000109346265,0.00022944353,0.00039222074,0.9124287,0.004777959,0.061988167,0.008177326],"study_design_scores_gemma":[0.0063444125,0.0013668523,0.31112406,0.0077786455,0.0046073883,0.000023644216,0.00012264407,0.030835463,0.5124713,0.08554886,0.036481626,0.003295066],"about_ca_topic_score_codex":0.0005805776,"about_ca_topic_score_gemma":0.000047413338,"teacher_disagreement_score":0.39995736,"about_ca_system_score_codex":0.0000019145168,"about_ca_system_score_gemma":0.0000138946525,"threshold_uncertainty_score":0.9914282},"labels":[],"label_agreement":null},{"id":"W2077437571","doi":"10.1007/s002699900054","title":"Elasticity of the pyrope (Mg 3 Al 2 Si 3 O 12 )-majorite (MgSiO 3 ) garnets solid solution","year":2000,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"National Science Foundation","keywords":"Pyrope; Crystallite; Chemistry; Brillouin Spectroscopy; Mineralogy; Elasticity (physics); Shear modulus; Elastic modulus; Solid solution; Analytical Chemistry (journal); Anisotropy; Bulk modulus; Crystallography; Composite material; Materials science; Brillouin scattering; Optics; Physics","score_opus":0.008265012332750347,"score_gpt":0.1975772438535339,"score_spread":0.18931223152078355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077437571","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875852,0.00014975903,0.000008230091,0.00010781365,0.00008454485,0.00006155869,0.00023582256,0.0000072076637,0.011759863],"genre_scores_gemma":[0.998061,0.00009571855,0.00004780281,0.00004884159,0.00021878413,6.7095436e-7,0.00004990348,0.0000033201727,0.001473933],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99920994,0.000021453212,0.00022364232,0.00017039488,0.00019481813,0.00017974232],"domain_scores_gemma":[0.99953824,0.00003898445,0.00013362593,0.00019096979,0.00003982894,0.000058362013],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008893906,0.00012428504,0.00023814515,0.0000037549542,0.00007791241,0.00001898904,0.00016378268,0.000045953973,0.0011997137],"category_scores_gemma":[0.000009099708,0.0000874638,0.000070478956,0.000058486814,0.00014625634,0.00007256743,0.00001988383,0.00006167,0.000009849115],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037482172,0.000049636958,0.0024210215,0.00011707575,0.000032125197,6.398948e-7,0.00009539751,0.0012361682,0.98815936,0.000030362835,0.0019753415,0.005845401],"study_design_scores_gemma":[0.0006162497,0.0000714889,0.05152814,0.00011393492,0.000089628425,0.0000044685626,0.000017243186,0.005205565,0.92159134,0.0034701878,0.01696252,0.00032924727],"about_ca_topic_score_codex":0.00072767935,"about_ca_topic_score_gemma":0.000026516633,"teacher_disagreement_score":0.066568024,"about_ca_system_score_codex":0.0000010602025,"about_ca_system_score_gemma":0.000022944321,"threshold_uncertainty_score":0.9997133},"labels":[],"label_agreement":null},{"id":"W2077999302","doi":"10.1007/s10751-008-9838-y","title":"High-temperature cation ordering in olivine: an in situ Mössbauer study of synthetic (Mg0.55Fe0.45)2 SiO4","year":2008,"lang":"en","type":"article","venue":"Hyperfine Interactions","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Mössbauer spectroscopy; Olivine; Octahedron; In situ; Chemistry; Spectral line; Metal; Crystallography; Analytical Chemistry (journal); Solid solution; Mineralogy; Materials science; Crystal structure; Physics","score_opus":0.015218142202238707,"score_gpt":0.23540324050232136,"score_spread":0.22018509830008265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077999302","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846005,0.000032946762,0.0000019706188,0.00013120956,0.00065584923,0.00024148381,0.00003328329,0.000022227545,0.0004209741],"genre_scores_gemma":[0.99941933,0.000031364852,0.00011756591,0.000028116574,0.00013188917,0.000009145511,0.00008608462,0.000006283276,0.00017022507],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989283,0.00012713636,0.00034837684,0.00025181932,0.00015657033,0.00018781419],"domain_scores_gemma":[0.9994548,0.00009284413,0.000085353604,0.00025214985,0.000058945236,0.000055923705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001346703,0.00013353088,0.0002567516,0.00022074545,0.00009270569,0.000029220048,0.00014429902,0.000049995568,0.0009095238],"category_scores_gemma":[0.000048030684,0.00011822758,0.000025438589,0.00034972627,0.000026289783,0.00040167378,0.000015147026,0.00018633435,0.000071378556],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002569641,0.002625398,0.39079934,0.000077537195,0.000063999156,0.00015312181,0.0112351775,0.0662008,0.5258346,0.000092565555,0.00045605295,0.0022043972],"study_design_scores_gemma":[0.00064816553,0.00031369063,0.9855372,0.00007258513,0.000018937297,0.00004057563,0.0013159254,0.00057583506,0.010329213,0.00006021772,0.00087080075,0.0002168802],"about_ca_topic_score_codex":0.018469777,"about_ca_topic_score_gemma":0.06179689,"teacher_disagreement_score":0.5947378,"about_ca_system_score_codex":0.000007398398,"about_ca_system_score_gemma":0.000036155223,"threshold_uncertainty_score":0.99586475},"labels":[],"label_agreement":null},{"id":"W2078298593","doi":"10.1029/2008jb006167","title":"Poisson's ratios of crystalline rocks as a function of hydrostatic confining pressure","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Poisson's ratio; Overburden pressure; Poisson distribution; Hydrostatic pressure; Geology; Mineralogy; Hydrostatic equilibrium; Materials science; Thermodynamics; Physics; Mathematics; Geotechnical engineering; Statistics","score_opus":0.02085502792996626,"score_gpt":0.2878396508076306,"score_spread":0.26698462287766433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078298593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953004,0.00077541167,0.00034981323,0.0003068511,0.00013989804,0.00017903204,0.000043619526,0.000006413335,0.0028985695],"genre_scores_gemma":[0.99837536,0.00008636884,0.0005384313,0.000036084137,0.00037249393,4.3901247e-7,0.00001060679,0.0000050689464,0.00057515333],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99715775,0.0003240704,0.00066941517,0.00016954396,0.0012976638,0.00038155203],"domain_scores_gemma":[0.9975957,0.000631536,0.0005198155,0.00020848839,0.00082550023,0.00021891444],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010139736,0.00014517906,0.00055193214,0.000039270773,0.00010588629,0.000064281,0.00036490537,0.0000810081,0.0016126431],"category_scores_gemma":[0.00051196275,0.0001063257,0.00016566637,0.00035834595,0.00016516555,0.00034873138,0.00002149335,0.0003681289,0.000034973298],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.012231308,0.001910926,0.01377002,0.0010050316,0.001418753,0.0002874328,0.0027148991,0.0687267,0.7037553,0.010945748,0.014867141,0.16836673],"study_design_scores_gemma":[0.004223854,0.03016086,0.71083057,0.0010285467,0.00043857007,0.000046362,0.0013412978,0.01378612,0.054419894,0.15719925,0.02583122,0.0006934229],"about_ca_topic_score_codex":0.0017876897,"about_ca_topic_score_gemma":0.00008267235,"teacher_disagreement_score":0.6970606,"about_ca_system_score_codex":0.0000037625323,"about_ca_system_score_gemma":0.00026685235,"threshold_uncertainty_score":0.9993},"labels":[],"label_agreement":null},{"id":"W2080149369","doi":"10.1103/physrevlett.92.196403","title":"Temperature Dependence of the Energy Gap of Semiconductors in the Low-Temperature Limit","year":2004,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Semiconductor; Condensed matter physics; Extant taxon; Limit (mathematics); Band gap; Range (aeronautics); Exponent; Atmospheric temperature range; Materials science; Physics; Thermodynamics; Quantum mechanics","score_opus":0.011185427382339493,"score_gpt":0.2237137987499375,"score_spread":0.212528371367598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080149369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99262035,0.0033653989,3.2396255e-7,0.0035059513,0.00017984146,0.0001818199,0.000050817413,0.0000042880692,0.00009122449],"genre_scores_gemma":[0.9917495,0.0014668928,0.0000117842965,0.006596019,0.00014697418,0.0000033865913,0.000017972427,0.0000031787745,0.0000042687693],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988801,0.00018773224,0.00024391475,0.00017847696,0.00032875992,0.00018103454],"domain_scores_gemma":[0.999335,0.00011082407,0.00014180374,0.00035472488,0.000026375781,0.000031277148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020316395,0.00013992515,0.00034252158,0.00001516732,0.000047456604,0.00001900558,0.0005463909,0.000020854228,0.000047433532],"category_scores_gemma":[0.000038898343,0.0000665336,0.00014968452,0.0003405726,0.000109371016,0.00012971241,0.000019601815,0.00017245907,0.0000092713135],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010300089,0.000076233206,0.0011741681,0.00083803077,0.000024985655,0.000007923966,0.0004993044,0.0035913263,0.99040157,0.0017932991,0.0012749328,0.0003079188],"study_design_scores_gemma":[0.0014887739,0.00034970234,0.21722448,0.013610658,0.00045129535,0.00004059427,0.00019757511,0.00007829646,0.74530596,0.0075985426,0.012307405,0.0013467368],"about_ca_topic_score_codex":0.001123484,"about_ca_topic_score_gemma":0.00024731687,"teacher_disagreement_score":0.24509564,"about_ca_system_score_codex":0.0000028781124,"about_ca_system_score_gemma":0.000043947053,"threshold_uncertainty_score":0.2713161},"labels":[],"label_agreement":null},{"id":"W2080302484","doi":"10.1063/1.3137582","title":"<i>Ab initio</i> molecular dynamics study of the static, dynamic, and electronic properties of liquid mercury at room temperature","year":2009,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Pseudopotential; Ab initio; Omega; Dynamic structure factor; Inelastic neutron scattering; Molecular dynamics; Dispersion relation; Long wavelength limit; Relaxation (psychology); Dispersion (optics); Condensed matter physics; Physics; Neutron; Structure factor; Materials science; Molecular physics; Neutron scattering; Quantum mechanics","score_opus":0.0047802397042860595,"score_gpt":0.18874955237234645,"score_spread":0.18396931266806038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080302484","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99876654,0.0006232341,0.0000076244733,0.00030329975,0.00006056353,0.00014978292,0.000033246914,0.000002732551,0.000052952833],"genre_scores_gemma":[0.9997022,0.000099375146,0.000018082106,0.000112025926,0.00005024158,1.6581758e-7,0.000004557308,0.0000040092164,0.000009348662],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989524,0.00012508493,0.00033884007,0.00007385852,0.0003427144,0.00016709884],"domain_scores_gemma":[0.99924445,0.000055173477,0.00035598368,0.00018627306,0.000116748204,0.00004139916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024311364,0.00012128454,0.00030085217,0.000011623525,0.00005525004,0.000015192669,0.00032526313,0.000039531515,0.000010428308],"category_scores_gemma":[0.000018711948,0.000060060156,0.00006579672,0.0001136132,0.00010044537,0.0001014477,0.000030430383,0.00022070664,6.6796554e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000443747,0.00014114624,0.00012624447,0.000032725267,0.00008193046,0.000001504196,0.0010185832,0.0012418194,0.9963544,0.000111379406,0.000037688136,0.00040885614],"study_design_scores_gemma":[0.00075157755,0.0015315178,0.0017760566,0.00010444537,0.00030207742,0.000027896329,0.00038941044,0.0011957134,0.9848772,0.008845715,0.000030623727,0.00016771696],"about_ca_topic_score_codex":0.00004608807,"about_ca_topic_score_gemma":0.000020882686,"teacher_disagreement_score":0.011477127,"about_ca_system_score_codex":0.000010325387,"about_ca_system_score_gemma":0.00007582425,"threshold_uncertainty_score":0.24491821},"labels":[],"label_agreement":null},{"id":"W2080396547","doi":"10.1144/sp360.11","title":"The microstructural and rheological evolution of shear zones","year":2011,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Imperial Oil (Canada)","funders":"","keywords":"Rheology; Shear (geology); Geology; Materials science; Composite material; Petrology","score_opus":0.018699095917751433,"score_gpt":0.20398045199438367,"score_spread":0.18528135607663224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080396547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9871508,0.00044568218,0.00036827303,0.0013403815,0.00036920657,0.00021261789,0.0000916916,0.000049332968,0.009972015],"genre_scores_gemma":[0.9962268,0.00021861283,0.002510255,0.00007278961,0.0005107822,0.0000044011526,0.000044383396,0.0000015299297,0.00041044992],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99905556,0.00007613929,0.0002457302,0.00021575319,0.00014529997,0.00026149562],"domain_scores_gemma":[0.99935526,0.00016024895,0.000112274145,0.00017921872,0.000104152794,0.00008885101],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029046595,0.00010116264,0.00015949128,0.000011929078,0.00048639654,0.00006087641,0.0002631622,0.00012366363,0.0029649676],"category_scores_gemma":[0.00009440788,0.00005733911,0.00009945109,0.00019300573,0.0007766554,0.00014635485,0.00005493583,0.00010797474,0.000052678464],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000097998534,0.00008322528,0.44854826,0.0000147165965,0.00007874142,7.478452e-7,0.00094089523,0.0000274609,0.0010190879,0.524035,0.012319283,0.0128346365],"study_design_scores_gemma":[0.00010934011,0.000078186786,0.93548113,0.0000010935908,0.000011671546,0.000004400867,0.00013800994,0.000117665644,0.00007844099,0.041157916,0.02274112,0.000081008795],"about_ca_topic_score_codex":0.00094309164,"about_ca_topic_score_gemma":0.0002312502,"teacher_disagreement_score":0.4869329,"about_ca_system_score_codex":0.0000037621617,"about_ca_system_score_gemma":0.00002906835,"threshold_uncertainty_score":0.99794644},"labels":[],"label_agreement":null},{"id":"W2081450125","doi":"10.1063/1.2829408","title":"Conformational and phase transformations of chlorocyclohexane at high pressures by Raman spectroscopy","year":2008,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Raman spectroscopy; Conformational isomerism; Diamond anvil cell; Phase transition; Phase (matter); Chemistry; Ambient pressure; Hysteresis; Compression (physics); Crystallography; High pressure; Thermodynamics; Molecule; Condensed matter physics; Organic chemistry; Optics","score_opus":0.008805716987327478,"score_gpt":0.21347505019857754,"score_spread":0.20466933321125005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081450125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983293,0.00028176937,0.0003415012,0.0001749243,0.00007765598,0.0000614057,0.00024030272,0.0000037345303,0.00048942195],"genre_scores_gemma":[0.99925864,0.00025780284,0.00017340951,0.000051277093,0.00017873518,1.4312579e-7,0.00005800448,0.0000020718437,0.000019890404],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992304,0.000028312528,0.00031391456,0.00003890518,0.0002738318,0.000114667426],"domain_scores_gemma":[0.99940723,0.0001262434,0.00025623612,0.00007422547,0.00006622593,0.00006986296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014107345,0.00008328956,0.00020900836,0.000011808396,0.000088809364,0.000010771059,0.00015923652,0.00002893365,0.0002263033],"category_scores_gemma":[0.000007891574,0.000051662864,0.000045561388,0.000051021412,0.00017239494,0.0002681318,0.000008465257,0.000095265,0.0000057935495],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005175205,0.00010702322,0.00028159967,0.000052700558,0.000099213445,0.0000017429091,0.0014261401,0.0006837562,0.9846815,0.0002714014,0.011056457,0.00082094106],"study_design_scores_gemma":[0.0011597043,0.0001674065,0.0012027452,0.000015959555,0.000078588084,0.00006993191,0.00001979966,0.00046995038,0.98974204,0.004656805,0.0023222042,0.00009487537],"about_ca_topic_score_codex":0.00006235295,"about_ca_topic_score_gemma":0.0000011691232,"teacher_disagreement_score":0.008734253,"about_ca_system_score_codex":0.0000022956256,"about_ca_system_score_gemma":0.000025151976,"threshold_uncertainty_score":0.24778624},"labels":[],"label_agreement":null},{"id":"W2081533071","doi":"10.1029/2010jb007796","title":"Constraints on the deep thermal structure of the Dharwar craton, India, from heat flow, shear wave velocities, and mantle xenoliths","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université du Québec à Montréal","funders":"Université du Québec à Montréal","keywords":"Geology; Mantle (geology); Dharwar Craton; Geophysics; Earth's internal heat budget; Lithosphere; Craton; Heat flux; Downwelling; Mantle wedge; Transition zone; Mantle convection; Petrology; Seismology; Heat transfer; Tectonics; Mechanics; Physics; Upwelling","score_opus":0.029306173770903523,"score_gpt":0.24029905383420552,"score_spread":0.210992880063302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081533071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963227,0.00030351203,0.000006867837,0.00022785283,0.00027851615,0.00018375722,0.0002625944,0.0000035252406,0.0024106668],"genre_scores_gemma":[0.9988524,0.00006177712,0.00047906107,0.00010659424,0.0004373364,5.2262277e-7,0.000004052874,0.0000073542888,0.000050937204],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9975856,0.0005312457,0.00035008212,0.00017983651,0.0009422212,0.0004110301],"domain_scores_gemma":[0.99828535,0.0008429259,0.00015290055,0.00030119167,0.00023773703,0.00017989465],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004970596,0.0001618421,0.00033562898,0.00001323798,0.0002844581,0.0000919724,0.00055565225,0.0000918548,0.007910144],"category_scores_gemma":[0.0001933389,0.00007622601,0.00011763266,0.0001831979,0.0009550903,0.00016168297,0.00008197792,0.00062415947,0.000033816486],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009851365,0.001575461,0.17330827,0.00055541494,0.0042006555,0.0010692971,0.050984506,0.0024757055,0.23030353,0.029458178,0.02017282,0.4760448],"study_design_scores_gemma":[0.00043473032,0.000651479,0.9397255,0.000098300276,0.00003419968,0.000011428424,0.0010746802,0.0008968394,0.028996402,0.027479304,0.00045872817,0.00013841015],"about_ca_topic_score_codex":0.004789073,"about_ca_topic_score_gemma":0.0002649637,"teacher_disagreement_score":0.7664172,"about_ca_system_score_codex":0.00000670226,"about_ca_system_score_gemma":0.00017960562,"threshold_uncertainty_score":0.99299675},"labels":[],"label_agreement":null},{"id":"W2082187021","doi":"10.1073/pnas.1118168109","title":"Superconductive sodalite-like clathrate calcium hydride at high pressures","year":2012,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":915,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Sodalite; Hydride; Superconductivity; Crystallography; Hydrogen; Chemistry; Stoichiometry; Clathrate hydrate; Crystal structure; Hydrogen storage; Condensed matter physics; Physical chemistry; Physics; Hydrate; Zeolite","score_opus":0.046495676971454326,"score_gpt":0.2751301119224178,"score_spread":0.2286344349509635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082187021","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99045944,0.0004072147,1.6651508e-7,0.0008016582,0.00018351893,0.00014985702,0.00016401884,0.000011935607,0.007822187],"genre_scores_gemma":[0.9984956,0.000020724707,0.00047184835,0.00021329636,0.00030120823,0.0000022186262,0.0000014233251,0.0000021911835,0.00049151893],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9981836,0.000015886286,0.00028671726,0.00021617202,0.0010019377,0.00029570085],"domain_scores_gemma":[0.9993321,0.00013374291,0.00029178546,0.000011198685,0.00015415608,0.000077049226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012864374,0.000119055025,0.00019694687,0.00008130373,0.00030041195,0.000034406898,0.00066352,0.00008419446,0.00036481812],"category_scores_gemma":[0.00012723073,0.00007258048,0.000068333524,0.00035675697,0.0007055705,0.0010269716,0.00009043382,0.000098912,0.000022922803],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006742937,0.00007118085,0.22994304,0.0001411602,0.00007650027,1.4517587e-8,0.0016878855,0.0007870152,0.7060413,0.056145854,0.004645665,0.0003929885],"study_design_scores_gemma":[0.00013138134,0.00003913812,0.58464587,0.00003146034,0.000028273895,0.00000552223,0.00013002874,0.00025672297,0.3799459,0.03208365,0.0025575564,0.00014449537],"about_ca_topic_score_codex":0.0003620175,"about_ca_topic_score_gemma":0.0000012227325,"teacher_disagreement_score":0.35470283,"about_ca_system_score_codex":0.0000059758554,"about_ca_system_score_gemma":0.000020287578,"threshold_uncertainty_score":0.39945024},"labels":[],"label_agreement":null},{"id":"W2082720414","doi":"10.1016/j.actamat.2004.11.021","title":"Representation of misorientations in Rodrigues–Frank space: application to the Bain, Kurdjumov–Sachs, Nishiyama–Wassermann and Pitsch orientation relationships in the Gibeon meteorite","year":2004,"lang":"en","type":"article","venue":"Acta Materialia","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Misorientation; Orientation (vector space); Transformation (genetics); Meteorite; Representation (politics); Materials science; Crystallography; Mathematics; Physics; Geometry; Chemistry; Astrobiology","score_opus":0.016434243186015524,"score_gpt":0.24934839402883052,"score_spread":0.232914150842815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082720414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99512744,0.000038535698,0.0003071725,0.0025077623,0.000803945,0.0007997027,0.00010382963,0.000014510097,0.00029712202],"genre_scores_gemma":[0.9985177,0.000040365725,0.00065889914,0.00010049387,0.00012371037,0.000045094344,0.00045877305,0.0000052105925,0.00004977464],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998563,0.00033743752,0.00038926184,0.00026907175,0.00025403,0.000187214],"domain_scores_gemma":[0.9993177,0.0001112618,0.00015990672,0.00031550587,0.000054864053,0.000040784973],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00087772886,0.000121690944,0.0001743701,0.00010873733,0.00016463126,0.00015403454,0.00022324071,0.00006547806,0.000053068157],"category_scores_gemma":[0.00010700147,0.00008434488,0.000022789609,0.0006324907,0.000047538506,0.00041311464,0.000017180471,0.00009097944,0.00004721851],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008393153,0.00035694556,0.5216796,0.00030632576,0.00008247447,0.000018571407,0.06690254,0.022852568,0.31952643,0.058540028,0.004922446,0.0039727855],"study_design_scores_gemma":[0.00055567716,0.00006011074,0.98494637,0.000026894333,0.000025383622,0.0000032165722,0.0015719527,0.00013995908,0.0043123257,0.0060104774,0.0022214097,0.00012622307],"about_ca_topic_score_codex":0.009731857,"about_ca_topic_score_gemma":0.006335446,"teacher_disagreement_score":0.46326682,"about_ca_system_score_codex":0.000008030824,"about_ca_system_score_gemma":0.000028345168,"threshold_uncertainty_score":0.9968624},"labels":[],"label_agreement":null},{"id":"W2083320121","doi":"10.1081/sl-120014940","title":"RAMAN AND INFRARED SPECTRA OF IODOFORM AT HIGH PRESSURES","year":2002,"lang":"en","type":"article","venue":"Spectroscopy Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Raman spectroscopy; Chemistry; Infrared; Intramolecular force; Infrared spectroscopy; Intermolecular force; Dissociation (chemistry); Iodoform; Analytical Chemistry (journal); Spectral line; Photochemistry; Molecule; Physical chemistry; Optics; Stereochemistry; Organic chemistry","score_opus":0.006948713338207523,"score_gpt":0.17923974677922963,"score_spread":0.17229103344102212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083320121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99245065,0.00032494395,0.0000445394,0.0010417154,0.00033726788,0.00014987327,0.00013020811,0.000039063656,0.0054817363],"genre_scores_gemma":[0.9966292,0.00006161271,0.0022423111,0.000522292,0.00018217083,0.0000011250365,0.000038636343,0.0000058878736,0.00031677607],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989968,0.00003428238,0.00019630679,0.0002392421,0.0002157548,0.00031761196],"domain_scores_gemma":[0.99952334,0.00005252568,0.00010115665,0.00022485972,0.000010984842,0.00008713897],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000088022054,0.00015111512,0.00024486208,0.00006206473,0.00010569691,0.00005520477,0.00016175551,0.000044388296,0.0058799568],"category_scores_gemma":[0.00000785829,0.00012713872,0.000042973912,0.0000882316,0.00014010274,0.00013027048,0.000018177927,0.00006776906,0.00013058023],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018123024,0.00006011908,0.09766129,0.00019723554,0.00013317073,0.000053977903,0.0007281527,0.001547486,0.8439713,0.0008874469,0.053838443,0.00074016524],"study_design_scores_gemma":[0.0011463194,0.00044107565,0.5499869,0.000047126818,0.000095268675,0.00001171549,0.000019759207,0.0019168735,0.42373893,0.0017497042,0.020264143,0.00058222306],"about_ca_topic_score_codex":0.00085906853,"about_ca_topic_score_gemma":0.00017568785,"teacher_disagreement_score":0.45232558,"about_ca_system_score_codex":0.0000038968155,"about_ca_system_score_gemma":0.0000048387756,"threshold_uncertainty_score":0.9950288},"labels":[],"label_agreement":null},{"id":"W2083705334","doi":"10.1029/2011jb008536","title":"Shear wave structure in the Grenville Province beneath the lower Great Lakes region from Rayleigh wave tomography","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Seismology; Rayleigh wave; Shear (geology); Seismic tomography; Low-velocity zone; Phase velocity; Induced seismicity; Geophysics; Mantle (geology); Surface wave; Tectonics; Petrology","score_opus":0.04169893560721682,"score_gpt":0.24894733710205721,"score_spread":0.2072484014948404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083705334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959501,0.0006640935,0.000012156122,0.0005968393,0.00036731278,0.00031844,0.00007908665,0.000006140702,0.002005809],"genre_scores_gemma":[0.9979725,0.000173257,0.000518122,0.00012098891,0.0010300591,0.0000020388845,0.000009940129,0.000009166025,0.00016392069],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99648035,0.00085290684,0.00043946673,0.0002864238,0.0013157884,0.0006250976],"domain_scores_gemma":[0.9979338,0.00093010865,0.00022024027,0.0004839828,0.00024994725,0.00018189715],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009417101,0.0002213548,0.00038342137,0.00003236714,0.00033474044,0.00022745128,0.0008917767,0.00011281585,0.0016575108],"category_scores_gemma":[0.00016189582,0.000101691985,0.00021850735,0.0005103517,0.00045744775,0.00032731864,0.00006538579,0.0008930908,0.000044840694],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.020830251,0.004271574,0.36618656,0.00042921913,0.0025557966,0.018922359,0.04503676,0.001743078,0.02168064,0.022395883,0.109371476,0.3865764],"study_design_scores_gemma":[0.00062140764,0.0017661597,0.9219855,0.00012332702,0.000047327827,0.00005106083,0.0009573579,0.0005730931,0.0013143454,0.061397936,0.010917775,0.00024473088],"about_ca_topic_score_codex":0.014002158,"about_ca_topic_score_gemma":0.005153909,"teacher_disagreement_score":0.5557989,"about_ca_system_score_codex":0.000009036343,"about_ca_system_score_gemma":0.00016460923,"threshold_uncertainty_score":0.9992551},"labels":[],"label_agreement":null},{"id":"W2083771754","doi":"10.1103/physrevlett.97.155503","title":"Systematic Method to New Phases of Polymeric Nitrogen under High Pressure","year":2006,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada; University of Ottawa","funders":"","keywords":"Metastability; Nitrogen; Nitrogen atom; Materials science; Atom (system on chip); Chemical physics; High pressure; Simple (philosophy); Thermodynamics; Computer science; Chemistry; Physics; Group (periodic table); Organic chemistry","score_opus":0.01136088840414144,"score_gpt":0.2639486641630699,"score_spread":0.25258777575892843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083771754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8463406,0.10053731,0.03292454,0.012648768,0.0009576761,0.0044410443,0.0006622109,0.0002058212,0.0012820087],"genre_scores_gemma":[0.98828125,0.00019268511,0.0039110295,0.006746633,0.00063860154,0.000012294835,0.000076737,0.000010586167,0.0001301932],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99855405,0.00023437681,0.00037959652,0.00025091242,0.00032318378,0.00025787498],"domain_scores_gemma":[0.9991187,0.0002475066,0.00019108588,0.00029288768,0.000023707464,0.00012612963],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020325539,0.0001850274,0.00077959674,0.000033004326,0.000037858925,0.00003064628,0.00026512283,0.000010236407,0.00044963742],"category_scores_gemma":[0.000023023882,0.00012996164,0.00016279887,0.00026834157,0.00002556695,0.00010287995,0.000016826732,0.00004996004,0.00022940313],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014440839,0.00066549797,0.002262887,0.18274601,0.0016618231,0.00004862055,0.00041319852,0.08922153,0.52017176,0.011601571,0.17800759,0.01305509],"study_design_scores_gemma":[0.0076964586,0.00350761,0.09135401,0.19498433,0.029586283,0.00014719155,0.00014485203,0.011949836,0.3324203,0.12507117,0.19053827,0.012599691],"about_ca_topic_score_codex":0.0067410427,"about_ca_topic_score_gemma":0.00002146878,"teacher_disagreement_score":0.18775149,"about_ca_system_score_codex":0.0000017146298,"about_ca_system_score_gemma":0.000023002995,"threshold_uncertainty_score":0.99987316},"labels":[],"label_agreement":null},{"id":"W2083942738","doi":"10.4028/www.scientific.net/ssp.170.282","title":"Interpretation of the Magnetic Order, Neutron Diffraction and &lt;sup&gt;111&lt;/sup&gt;Cd PAC Studies of NdScGe","year":2011,"lang":"en","type":"article","venue":"Diffusion and defect data, solid state data. Part B, Solid state phenomena/Solid state phenomena","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Manitoba","funders":"Canada Research Chairs","keywords":"Neutron diffraction; Tetragonal crystal system; Quadrupole; Condensed matter physics; Materials science; Magnetic moment; Ferromagnetism; Curie temperature; Electric field gradient; Magnetic structure; Crystallography; Diffraction; Nuclear magnetic resonance; Physics; Magnetic field; Crystal structure; Atomic physics; Chemistry; Magnetization; Optics","score_opus":0.03540017818430608,"score_gpt":0.2669057944244249,"score_spread":0.23150561624011884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083942738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94458205,0.0046574106,0.0004244449,0.00010028703,0.0012596102,0.0015683866,0.04615233,0.00011522535,0.001140283],"genre_scores_gemma":[0.9683994,0.021721184,0.00041319526,0.00020356747,0.0002366855,0.000032688233,0.008546004,0.00007358869,0.00037369877],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99297035,0.0008738033,0.0020229642,0.0018433388,0.0009183739,0.0013711877],"domain_scores_gemma":[0.99431425,0.00055746816,0.0013482393,0.0028444417,0.00039681213,0.000538788],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.001773085,0.0010380212,0.0017591361,0.00036394806,0.00072896807,0.00029452395,0.0017178635,0.00013262253,0.0004829595],"category_scores_gemma":[0.00022008234,0.00077827025,0.00015036859,0.0006889209,0.0010061535,0.0018007847,0.0018836719,0.00043575375,0.000080259735],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.023990432,0.0069881203,0.05675342,0.012618372,0.011059953,0.0002462478,0.26652974,0.033101004,0.105943896,0.0011717217,0.038668796,0.4429283],"study_design_scores_gemma":[0.023092369,0.01208884,0.3503045,0.0025148839,0.00463021,0.0001657514,0.017057914,0.3570643,0.0060998737,0.039762326,0.17720325,0.010015739],"about_ca_topic_score_codex":0.0014533675,"about_ca_topic_score_gemma":0.0025500355,"teacher_disagreement_score":0.43291256,"about_ca_system_score_codex":0.000031458072,"about_ca_system_score_gemma":0.00018431684,"threshold_uncertainty_score":0.99946684},"labels":[],"label_agreement":null},{"id":"W2084460525","doi":"10.1021/jp503409p","title":"Robust Diffusive Proton Motions in Phase IV of Solid Hydrogen","year":2014,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Ergodicity; Proton; Molecular dynamics; Supercell; Ergodic theory; Hydrogen; Phase (matter); Statistical physics; Range (aeronautics); Chemical physics; Materials science; Computational chemistry; Molecular physics; Physics; Chemistry; Quantum mechanics; Mathematics","score_opus":0.012823142931407057,"score_gpt":0.2356207147631088,"score_spread":0.22279757183170176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084460525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99873596,0.000019818634,0.00005065951,0.000094109564,0.000031985244,0.000078647645,0.00004677004,0.000002500366,0.0009395578],"genre_scores_gemma":[0.9994493,0.000007352388,0.00001981578,0.0000119002125,0.00046149755,4.9045224e-7,0.0000065042013,0.0000022632184,0.00004085454],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993115,0.000063737796,0.00024384091,0.00005846277,0.00019299796,0.00012947092],"domain_scores_gemma":[0.9993976,0.0000999386,0.0002574812,0.00012555919,0.000054252556,0.000065162785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028470263,0.00007985076,0.00024158951,0.00001169591,0.000036210055,0.000008560489,0.0002510945,0.000027116384,0.00020975793],"category_scores_gemma":[0.00004697389,0.000047646205,0.00007348679,0.00008047405,0.000075180054,0.00007654012,0.00001212094,0.00013448467,0.000010268114],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007806264,0.0002153538,0.0002443336,0.00006550619,0.000024122162,0.0000027289702,0.0003387902,0.019928087,0.9782509,0.0000128855,0.00006615714,0.0007730566],"study_design_scores_gemma":[0.0009867692,0.0002678348,0.0025399379,0.00006649389,0.00006065946,0.0000144197775,0.00006192665,0.015286413,0.977098,0.0030576868,0.00045400724,0.00010588823],"about_ca_topic_score_codex":0.000072832176,"about_ca_topic_score_gemma":0.0000051623615,"teacher_disagreement_score":0.004641673,"about_ca_system_score_codex":0.000002141376,"about_ca_system_score_gemma":0.000027747988,"threshold_uncertainty_score":0.22967023},"labels":[],"label_agreement":null},{"id":"W2085139057","doi":"10.1063/1.3369625","title":"A note on the metallization of compressed liquid hydrogen","year":2010,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Schematic; Phase diagram; Realization (probability); Molecular dynamics; Quadratic equation; Hydrogen; Construct (python library); Phase (matter); Covalent bond","score_opus":0.012127104961769875,"score_gpt":0.2150929473497651,"score_spread":0.20296584238799523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085139057","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983155,0.000022514352,0.00015357579,0.00042612996,0.00020429889,0.000053891745,0.000018958435,0.0000029737862,0.0008021506],"genre_scores_gemma":[0.99929684,0.000011785626,0.00007133878,0.00014183154,0.0004630424,9.749559e-8,0.0000051024294,0.0000026955213,0.0000072830944],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993203,0.00006183195,0.00021434724,0.000041552164,0.00026793435,0.00009399912],"domain_scores_gemma":[0.999078,0.00034970752,0.00028459422,0.00016383034,0.000084395244,0.00003947269],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003697712,0.00007140929,0.00016325094,0.00000781448,0.000040907606,0.00001390814,0.00036643233,0.000032099222,0.00021179524],"category_scores_gemma":[0.000047214027,0.000032556112,0.000074396776,0.000078264275,0.00010266379,0.000072962765,0.0000122477,0.00020019828,0.000020308582],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016611248,0.000026341055,0.000018959017,0.0000060280377,0.000030345813,4.2930267e-7,0.00017044565,0.0015688991,0.9964813,0.00087027805,0.00024310565,0.00041777032],"study_design_scores_gemma":[0.0001241275,0.0001019291,0.00017947714,0.000012487834,0.000059639875,0.0000037486147,0.0000060879656,0.0007679368,0.98689365,0.0107177785,0.0010854495,0.0000476749],"about_ca_topic_score_codex":0.000042131895,"about_ca_topic_score_gemma":0.0000031826924,"teacher_disagreement_score":0.0098475,"about_ca_system_score_codex":6.783545e-7,"about_ca_system_score_gemma":0.00002462712,"threshold_uncertainty_score":0.23190093},"labels":[],"label_agreement":null},{"id":"W2085275314","doi":"10.1029/2003jb002427","title":"Lithospheric structure and composition of the Archean western Superior Province from seismic refraction/wide‐angle reflection and gravity modeling","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Queen's University","funders":"","keywords":"Geology; Crust; Lithosphere; Granulite; Anisotropy; Mantle (geology); Archean; Seismology; Geophysics; Petrology; Tectonics; Geochemistry; Geomorphology; Facies","score_opus":0.023491789667122856,"score_gpt":0.2823281550475438,"score_spread":0.258836365380421,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085275314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981882,0.0004142897,0.00044319546,0.0005532846,0.00016052776,0.00015836544,0.00005395839,0.000005155252,0.000023030076],"genre_scores_gemma":[0.9980641,0.00012222666,0.0014525426,0.00003147233,0.00028822114,4.2189666e-7,0.0000060216535,0.000005573873,0.000029438648],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9983774,0.00026973523,0.0003086454,0.00018674607,0.00061646046,0.00024103049],"domain_scores_gemma":[0.99904203,0.00023753794,0.00017969037,0.00015546699,0.00024237916,0.00014288856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036814765,0.0001170745,0.0002749691,0.000011398466,0.00026891212,0.00013706596,0.00019546786,0.00007042558,0.000042488697],"category_scores_gemma":[0.000088177185,0.00007393558,0.00006126905,0.00018191061,0.00022024989,0.00040713043,0.000052298048,0.00045369196,0.0000029549522],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003710376,0.0005387142,0.2659075,0.00051827135,0.00046701808,0.000099121404,0.003644749,0.1598264,0.4999746,0.00048533813,0.00021521823,0.06461269],"study_design_scores_gemma":[0.001132982,0.0011524316,0.87209153,0.00034278916,0.0000701953,0.000045759378,0.00033188294,0.0147284055,0.02027986,0.08924801,0.00035350732,0.00022266379],"about_ca_topic_score_codex":0.017595856,"about_ca_topic_score_gemma":0.0016234725,"teacher_disagreement_score":0.606184,"about_ca_system_score_codex":0.00001721944,"about_ca_system_score_gemma":0.00018453327,"threshold_uncertainty_score":0.9889461},"labels":[],"label_agreement":null},{"id":"W2085820764","doi":"10.1029/2011jb008733","title":"Experimental investigation of the stability of Fe‐rich carbonates in the lower mantle","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; Agence Nationale de la Recherche","keywords":"Mantle (geology); Transmission electron microscopy; Diamond anvil cell; Diamond; Geology; Mineralogy; Analytical Chemistry (journal); Materials science; Chemistry; Geochemistry; High pressure; Thermodynamics; Metallurgy; Nanotechnology","score_opus":0.057747721425269856,"score_gpt":0.2872829741340818,"score_spread":0.22953525270881198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085820764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977577,0.00025695845,9.2513307e-7,0.00011008705,0.00017142849,0.00015711864,0.000011774559,0.0000011820994,0.0015328742],"genre_scores_gemma":[0.9996799,0.000013549758,0.00016220578,0.000015102152,0.000104795516,0.0000010396591,9.4672447e-7,0.000002584771,0.000019879562],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99769247,0.00065431796,0.00040196595,0.000104232546,0.0009156567,0.00023133364],"domain_scores_gemma":[0.99871916,0.00050234364,0.00023040749,0.00023910975,0.00024246164,0.0000665226],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015328501,0.00008228943,0.00023548283,0.00001306002,0.00005797421,0.000022285076,0.0006309744,0.000041216426,0.0010249201],"category_scores_gemma":[0.00019972303,0.000040012215,0.00010283154,0.0003626213,0.00046911804,0.00017589526,0.00004777233,0.00028065243,0.0000072219723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013524406,0.0011888349,0.624499,0.0001650762,0.00012361331,0.00003989036,0.014654911,0.00013099227,0.35192853,0.0024987452,0.0013870153,0.0020309319],"study_design_scores_gemma":[0.00019633994,0.0006934283,0.77585053,0.000044318087,0.0000073393335,0.0000018347538,0.0012238488,0.0000984639,0.21306702,0.008708568,0.00006362902,0.000044689645],"about_ca_topic_score_codex":0.008659356,"about_ca_topic_score_gemma":0.0004431355,"teacher_disagreement_score":0.15135148,"about_ca_system_score_codex":0.0000061352293,"about_ca_system_score_gemma":0.00014499987,"threshold_uncertainty_score":0.9998883},"labels":[],"label_agreement":null},{"id":"W2086043381","doi":"10.1063/1.3533957","title":"Highly repulsive interaction in novel inclusion D2–N2 compound at high pressure: Raman and x-ray evidence","year":2011,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Department of Energy; University of Saskatchewan; National Science Foundation","keywords":"Inclusion (mineral); Raman spectroscopy; Homogeneous; High pressure; Crystallography; X-ray; Hexagonal crystal system; Chemistry; Materials science; Chemical physics; Thermodynamics; Mineralogy; Optics; Physics","score_opus":0.028968311003689372,"score_gpt":0.23421848849198587,"score_spread":0.2052501774882965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086043381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986686,0.00038212695,0.00007399885,0.00019116183,0.00036463886,0.000085682004,0.0000148692025,0.0000051899747,0.00021369472],"genre_scores_gemma":[0.9990376,0.00012072208,0.00034659202,0.00009855051,0.00035531673,2.2890212e-7,0.0000055991395,0.0000040485693,0.0000312915],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990227,0.00008881249,0.0003329026,0.00011200922,0.00028412565,0.0001594556],"domain_scores_gemma":[0.9989952,0.0003296254,0.00036212342,0.0001499785,0.0000837986,0.0000792796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004765598,0.00012002188,0.00024979867,0.000022905822,0.00010599675,0.000026924587,0.0002925026,0.000051863433,0.00012467254],"category_scores_gemma":[0.000052197658,0.00007489558,0.00004254196,0.000093126575,0.000105859064,0.00044099684,0.0001609981,0.00022332842,0.00001187151],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015092375,0.00013899719,0.003589952,0.0000711829,0.00008005139,0.000017184038,0.0052532656,0.0011373799,0.9847868,0.00021424217,0.00054873805,0.002652963],"study_design_scores_gemma":[0.0023284347,0.00079332537,0.16503483,0.0009697638,0.00049832184,0.00020094044,0.00019743045,0.0033835971,0.7680653,0.053798895,0.0040254593,0.00070369476],"about_ca_topic_score_codex":0.0009894073,"about_ca_topic_score_gemma":0.000029804714,"teacher_disagreement_score":0.2167215,"about_ca_system_score_codex":0.000010609651,"about_ca_system_score_gemma":0.000028141534,"threshold_uncertainty_score":0.3054153},"labels":[],"label_agreement":null},{"id":"W2086769994","doi":"10.1029/2006gl028337","title":"Anomalous uplift of the Apennines and subsidence of the Adriatic: The result of active mantle flow?","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Science Foundation","keywords":"Geology; Mantle (geology); Crust; Ocean surface topography; Residual; Transition zone; Geophysics; Seismic tomography; Seismology; Geodesy","score_opus":0.021821857532218082,"score_gpt":0.2712608261371332,"score_spread":0.24943896860491513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086769994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99619174,0.000055647906,0.000011045706,0.0025960843,0.00018274006,0.00033084577,0.00010753656,0.0000031388752,0.0005212077],"genre_scores_gemma":[0.99955124,0.000016794826,0.000055227287,0.00012420712,0.00014023273,0.0000016196788,0.0000030722083,0.0000034917637,0.00010414755],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99801546,0.0003210259,0.00026957475,0.00019283101,0.0008354699,0.0003656248],"domain_scores_gemma":[0.9977253,0.0014338164,0.00015529573,0.00048572654,0.00014372023,0.000056136683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001099874,0.000099320016,0.00021574476,0.000036498008,0.00020075402,0.000024280842,0.0007232013,0.000038458395,0.00006774912],"category_scores_gemma":[0.0003334095,0.00004431183,0.000089582936,0.000442195,0.0010607698,0.00009146743,0.00015465001,0.00023171393,0.000012423725],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009951714,0.00015504248,0.06154146,0.00031683827,0.00019116057,0.000012376887,0.0048573185,0.00079035707,0.9032697,0.003045807,0.0040540593,0.02077072],"study_design_scores_gemma":[0.00016617365,0.00007784104,0.92842317,0.000051894443,0.000015072005,0.0000010323076,0.00020597807,0.00034211855,0.06893895,0.0012833038,0.00043520486,0.00005925276],"about_ca_topic_score_codex":0.0067559974,"about_ca_topic_score_gemma":0.0006163706,"teacher_disagreement_score":0.8668817,"about_ca_system_score_codex":0.0000026279247,"about_ca_system_score_gemma":0.00005551743,"threshold_uncertainty_score":0.9998581},"labels":[],"label_agreement":null},{"id":"W2087864878","doi":"10.1029/2004jb003435","title":"Shear wave properties and Poisson's ratios of ultrahigh‐pressure metamorphic rocks from the Dabie‐Sulu orogenic belt, China: Implications for crustal composition","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Geology; Eclogite; Metamorphism; Crust; Metamorphic rock; Metamorphic facies; Craton; Subduction; Geochemistry; Petrology; Seismic anisotropy; Shear (geology); Shear zone; Continental crust; Mantle (geology); Tectonics; Seismology; Geomorphology; Facies","score_opus":0.0453886717733781,"score_gpt":0.27808402679735506,"score_spread":0.23269535502397695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087864878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912093,0.0029759274,0.00028380955,0.004307396,0.00009459423,0.0004648872,0.0005672073,0.000008150832,0.000088704015],"genre_scores_gemma":[0.9972151,0.00024510123,0.0012421893,0.000051038085,0.0010497312,0.000007802198,0.000047524183,0.000009419254,0.00013213122],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99796516,0.0003348409,0.0004805661,0.00022376691,0.0006107707,0.00038490767],"domain_scores_gemma":[0.9978973,0.0008579156,0.0002669345,0.0002601632,0.00052526896,0.00019241835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074717985,0.00016356977,0.00041885392,0.000017655144,0.00044456456,0.00017865791,0.00040081458,0.00008022016,0.0002776593],"category_scores_gemma":[0.00021199613,0.000094896925,0.000169851,0.00019403217,0.00032229966,0.0004623545,0.00004808536,0.0003493404,0.00001013152],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0045306394,0.0011640328,0.025917772,0.0003988195,0.0025369867,0.000019087709,0.0048477757,0.017335176,0.8243078,0.0055876407,0.018807922,0.094546326],"study_design_scores_gemma":[0.0014288443,0.0015503366,0.9266962,0.00016661498,0.00034081071,0.00002941979,0.00043506542,0.007054818,0.034991946,0.0154793365,0.011520074,0.00030655126],"about_ca_topic_score_codex":0.0045299116,"about_ca_topic_score_gemma":0.00062647543,"teacher_disagreement_score":0.9007784,"about_ca_system_score_codex":0.0000068942295,"about_ca_system_score_gemma":0.00016706926,"threshold_uncertainty_score":0.68479013},"labels":[],"label_agreement":null},{"id":"W2088281183","doi":"10.1063/1.4907866","title":"Strength and texture of Pt compressed to 63 GPa","year":2015,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Basic Energy Sciences; U.S. Department of Energy; Brookhaven National Laboratory; Office of Science; National Science Foundation","keywords":"Materials science; Texture (cosmology); Crystallite; Compressive strength; Cubic crystal system; Diamond; Yield (engineering); Grain size; Composite material; Compression (physics); Diffraction; Particle size; Close-packing of equal spheres; Crystallography; Metallurgy; Optics; Chemistry","score_opus":0.015977412125378072,"score_gpt":0.2149353176677201,"score_spread":0.19895790554234202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088281183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933631,0.000076053206,0.00017979906,0.000040954663,0.00027040057,0.00008119006,0.000090926,0.0000042069505,0.005893382],"genre_scores_gemma":[0.9981203,0.000011860546,0.001287057,0.000086321765,0.00046047533,1.624698e-7,0.000009102512,0.0000031167508,0.000021620775],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99928147,0.000016194585,0.00023774747,0.000079988175,0.0002638767,0.00012072553],"domain_scores_gemma":[0.99933153,0.000050262304,0.00023653239,0.000100455734,0.00009453741,0.0001866909],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017563654,0.00009232506,0.00028344177,0.000027258842,0.00002620831,0.000035259003,0.00015416744,0.000033770848,0.000052098032],"category_scores_gemma":[0.0000064894734,0.0000672955,0.00003363175,0.0000979743,0.00003313018,0.000092278606,0.000015836275,0.00008741473,0.000014182772],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003689719,0.00077809015,0.016891478,0.0005101819,0.0008154448,0.00007578815,0.013739852,0.4659311,0.19933695,0.02192218,0.07658675,0.1997225],"study_design_scores_gemma":[0.010798976,0.00425243,0.22466935,0.00043018337,0.0007478863,0.000070835755,0.0031009994,0.014792921,0.27976018,0.20493783,0.2542859,0.0021525088],"about_ca_topic_score_codex":0.00006392875,"about_ca_topic_score_gemma":0.000011949968,"teacher_disagreement_score":0.45113817,"about_ca_system_score_codex":0.0000013392948,"about_ca_system_score_gemma":0.000052490737,"threshold_uncertainty_score":0.2744231},"labels":[],"label_agreement":null},{"id":"W2088322578","doi":"10.1103/physreva.61.062901","title":"Vicinage effect on the charge state of fast clusters in solids","year":2000,"lang":"en","type":"article","venue":"Physical Review A","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Physics; Ion; Formalism (music); Electron; Atomic physics; Cluster (spacecraft); Traverse; Bound state; Charge exchange; Charge (physics); Quantum mechanics","score_opus":0.008340154497131227,"score_gpt":0.24214958857843108,"score_spread":0.23380943408129984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088322578","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987448,0.0011177184,4.6827546e-7,0.00040021676,0.000051286333,0.00036946405,0.000043644868,0.000007793603,0.010561426],"genre_scores_gemma":[0.9968761,0.0020270767,0.0000020118646,0.00087035657,0.000066114604,0.000005299127,0.000012320093,0.0000025936336,0.00013809855],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991571,0.00019778841,0.00015915894,0.000139222,0.00016576634,0.00018098531],"domain_scores_gemma":[0.99947995,0.00022326119,0.00004900724,0.00019151777,0.0000072781077,0.000048961097],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031165156,0.00010901411,0.00034758463,0.00001146202,0.00002881964,0.0000123147365,0.00016941821,0.00000794984,0.0018036185],"category_scores_gemma":[0.000025944084,0.00005479169,0.000081405226,0.00014740565,0.000037753936,0.00005006076,0.0000063335488,0.00007582012,0.0010052155],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021998916,0.00022942304,0.0019033949,0.0031473115,0.000061297505,0.00002353775,0.0006596278,0.0008209661,0.0046679885,0.0014645462,0.002660301,0.9841416],"study_design_scores_gemma":[0.004069157,0.009018838,0.4884241,0.023532992,0.0006420401,0.0000107977685,0.000026395186,0.019387472,0.04965375,0.024314089,0.3778931,0.0030272848],"about_ca_topic_score_codex":0.00026756572,"about_ca_topic_score_gemma":0.000030151476,"teacher_disagreement_score":0.9811143,"about_ca_system_score_codex":0.0000011589784,"about_ca_system_score_gemma":0.000009222206,"threshold_uncertainty_score":0.9997726},"labels":[],"label_agreement":null},{"id":"W2088610216","doi":"10.1126/science.1153282","title":"Superconductivity in Hydrogen Dominant Materials: Silane","year":2008,"lang":"en","type":"article","venue":"Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":395,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Metallic hydrogen; Superconductivity; Silane; Hydrogen; Metal; Materials science; Alloy; Hydrogen storage; Phase (matter); Room-temperature superconductor; Chemical physics; Condensed matter physics; Chemistry; Metallurgy; High-temperature superconductivity; Composite material; Physics","score_opus":0.019903854823237154,"score_gpt":0.21742086270815647,"score_spread":0.19751700788491933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088610216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784994,0.00008302597,0.000002581674,0.000058634025,0.0006400806,0.0001045964,0.00005385572,0.000016553817,0.0011907088],"genre_scores_gemma":[0.999544,0.000043964923,0.00015844345,0.000035148914,0.000077658646,0.0000011210478,0.000008466788,0.0000015587524,0.00012962375],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998809,0.000046959092,0.00015497734,0.0003108415,0.00030004134,0.0003781763],"domain_scores_gemma":[0.9996039,0.000031028907,0.000033973338,0.00021026713,0.000024628489,0.00009619491],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073370663,0.000091388094,0.00016389054,0.00008992665,0.0002267683,0.000051133142,0.000367736,0.00002868724,0.0013550593],"category_scores_gemma":[0.000050779512,0.00006963442,0.00001534143,0.00039592615,0.00047838478,0.00057780213,0.00002762254,0.000042459356,0.00050148286],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016684078,0.000019619232,0.043243103,0.000008486618,0.0000012461056,0.00007014434,0.00043471914,0.00019143382,0.9550995,0.000093406146,0.000043880715,0.0007777818],"study_design_scores_gemma":[0.0001615967,0.00003890261,0.5704605,0.000010625042,0.0000018138902,0.000041220563,0.000031878488,0.00012107762,0.42681733,0.00073242985,0.0014258623,0.00015676695],"about_ca_topic_score_codex":0.0043160804,"about_ca_topic_score_gemma":0.0004936681,"teacher_disagreement_score":0.52828217,"about_ca_system_score_codex":0.0000041759527,"about_ca_system_score_gemma":0.0001322274,"threshold_uncertainty_score":0.99955785},"labels":[],"label_agreement":null},{"id":"W2088728133","doi":"10.1139/p08-134","title":"First-principle calculations of the structure and elastic properties of GaAs under pressure","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Pseudopotential; Wurtzite crystal structure; Condensed matter physics; Physics; Bulk modulus; Anisotropy; Debye model; Density functional theory; Plane wave; Lattice (music); Quantum mechanics; Diffraction","score_opus":0.012751497413827093,"score_gpt":0.1861877226375588,"score_spread":0.17343622522373173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088728133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985008,0.0005900148,0.000049105405,0.00031426715,0.00022096378,0.000060088747,0.00018074318,8.011083e-7,0.0000831639],"genre_scores_gemma":[0.9997206,0.0000074429217,0.00006788856,0.00003966729,0.00012341133,2.2301839e-8,0.0000018965975,0.0000015927388,0.000037493075],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9995231,0.00002672256,0.00017629474,0.000048531652,0.00011633909,0.000109013636],"domain_scores_gemma":[0.9994823,0.000017175986,0.00018101133,0.000098990815,0.000104507926,0.000116051815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000050534174,0.00006244782,0.00015111924,0.000024647845,0.0000930787,0.000021091839,0.00014409293,0.000030279913,0.000094806346],"category_scores_gemma":[0.000016955644,0.00003816653,0.000041961408,0.00008578676,0.00009241012,0.00010286173,0.0000030010438,0.00007041092,5.1497136e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005519678,0.000031266147,0.10153763,0.00032217623,0.00029794459,0.000009790437,0.0036701637,0.83912313,0.028968848,0.021300662,0.0011283422,0.003554839],"study_design_scores_gemma":[0.0002925652,0.00016453322,0.9546259,0.00019830048,0.00016934997,0.000018595914,0.00008095627,0.002026189,0.018146751,0.019986577,0.004148926,0.00014132138],"about_ca_topic_score_codex":0.004010892,"about_ca_topic_score_gemma":0.014314233,"teacher_disagreement_score":0.8530883,"about_ca_system_score_codex":0.0000019389431,"about_ca_system_score_gemma":0.0002686412,"threshold_uncertainty_score":0.7987678},"labels":[],"label_agreement":null},{"id":"W2089096512","doi":"10.1144/gsl.sp.2006.268.01.05","title":"Crustal flow modes in large hot orogens","year":2006,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":322,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Geophysics; Flow (mathematics); Earth science; Geometry","score_opus":0.012575613287656849,"score_gpt":0.212745588927745,"score_spread":0.20016997564008815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089096512","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93798715,0.0001698796,0.0009574368,0.002981927,0.00034065312,0.00036150607,0.00082865945,0.00015723062,0.056215573],"genre_scores_gemma":[0.99252653,0.00005490984,0.002491596,0.00035622795,0.0021119756,0.000013081498,0.0010984674,0.0000037854923,0.0013434318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984641,0.000067719855,0.00031796363,0.0003625072,0.00024921662,0.0005384745],"domain_scores_gemma":[0.9994135,0.00009746724,0.00007886406,0.00022424514,0.000079103585,0.00010680822],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031266513,0.00015468583,0.00023525915,0.00003688153,0.00029300756,0.0001639719,0.00029776205,0.00018165605,0.013839113],"category_scores_gemma":[0.000045904024,0.00012491852,0.00016735296,0.00047601518,0.00013754667,0.00027110256,0.00004448902,0.00016579324,0.0005189117],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007053348,0.0008445464,0.6063978,0.000025546384,0.000060302536,0.000013203469,0.00045058035,0.021598881,0.0009799014,0.16265297,0.2007868,0.0061189444],"study_design_scores_gemma":[0.00037136415,0.000031320633,0.79175633,0.0000019765353,0.00000928389,0.0000019269753,0.000083737614,0.0055492213,0.000062217885,0.012317098,0.18961331,0.0002022208],"about_ca_topic_score_codex":0.0022643704,"about_ca_topic_score_gemma":0.0058346963,"teacher_disagreement_score":0.18535854,"about_ca_system_score_codex":0.000009731078,"about_ca_system_score_gemma":0.0000536822,"threshold_uncertainty_score":0.9870624},"labels":[],"label_agreement":null},{"id":"W2089429075","doi":"10.1016/j.jog.2008.03.008","title":"Postglacial isostatic adjustment in a self-gravitating spherical earth with power-law rheology","year":2008,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Post-glacial rebound; Geology; Mantle (geology); Rheology; Power law; Geophysics; Viscoelasticity; Ice sheet; Geomorphology; Physics; Thermodynamics","score_opus":0.005133426436437344,"score_gpt":0.19003332375624352,"score_spread":0.18489989731980616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089429075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973142,0.00014232489,0.00027670868,0.000094488976,0.0004442911,0.00009067468,0.000022817494,0.000008237371,0.001606248],"genre_scores_gemma":[0.9871855,0.00005636563,0.012368732,0.00018965143,0.0001284059,2.6798608e-7,0.00001105192,0.000005115529,0.00005493028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987619,0.00010748847,0.0004248523,0.00012054995,0.00029294993,0.00029226326],"domain_scores_gemma":[0.9992866,0.00011565039,0.00030129385,0.00009080399,0.00008772758,0.00011790798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024995577,0.00013297102,0.000342459,0.00006200426,0.0000875451,0.000023778875,0.00015894357,0.00006000499,0.00029122047],"category_scores_gemma":[0.000017269145,0.000095368785,0.00005553556,0.00013575902,0.00009034282,0.00019211245,0.000011003573,0.00020019535,0.000035201225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033099577,0.0011369453,0.8622033,0.00021441441,0.00067350274,0.008173145,0.0119479615,0.083239906,0.004882895,0.017618936,0.00034515408,0.0062538753],"study_design_scores_gemma":[0.0018847126,0.0029418287,0.9779714,0.00007980806,0.000059885904,0.0016233177,0.000368619,0.011411041,0.000066323904,0.0022094697,0.0010436457,0.00033997034],"about_ca_topic_score_codex":0.00059107895,"about_ca_topic_score_gemma":0.0012100678,"teacher_disagreement_score":0.11576807,"about_ca_system_score_codex":0.0000078689745,"about_ca_system_score_gemma":0.00014026463,"threshold_uncertainty_score":0.3889026},"labels":[],"label_agreement":null},{"id":"W2089547272","doi":"10.1016/j.lithos.2004.04.028","title":"Features of coated diamonds from the Snap Lake/King Lake kimberlite dyke, Slave craton, Canada, as revealed by optical topography","year":2004,"lang":"en","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Kimberlite; Nitrogen; Annealing (glass); Spectroscopy; Vacancy defect; Materials science; Dissolution; Mineralogy; Analytical Chemistry (journal); Geology; Geochemistry; Crystallography; Chemistry; Metallurgy; Environmental chemistry","score_opus":0.003974183884618593,"score_gpt":0.1817129055536487,"score_spread":0.1777387216690301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089547272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9860118,0.0010090985,0.0000133806,0.0009305912,0.00052526646,0.00021723518,0.0029691963,0.000028160664,0.008295245],"genre_scores_gemma":[0.99759305,0.00004339894,0.00025553253,0.0006756312,0.00019223335,0.0000028795623,0.00089805876,0.000006228589,0.0003329991],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986756,0.00008940712,0.00027357182,0.0002708905,0.0003618185,0.00032870274],"domain_scores_gemma":[0.99915767,0.00021100222,0.000114796145,0.00031671848,0.000058674006,0.0001411591],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017585717,0.00018028953,0.00029033693,0.00002222415,0.0001520222,0.00008991408,0.0003195665,0.000094916155,0.0013560931],"category_scores_gemma":[0.000047308313,0.00011959727,0.00007274435,0.00022332848,0.00010817253,0.0000946669,0.000021392068,0.00014705838,0.000023281043],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045522302,0.00017667189,0.8871219,0.00015708117,0.0007737503,0.00028007335,0.004118089,0.0007019609,0.008137255,0.004252904,0.083736554,0.010088527],"study_design_scores_gemma":[0.00045924453,0.00008469713,0.8874652,0.000060447648,0.00007176523,0.000004085982,0.000086764914,0.000008934251,0.0074566253,0.0025195514,0.10154051,0.00024216274],"about_ca_topic_score_codex":0.78068054,"about_ca_topic_score_gemma":0.9391954,"teacher_disagreement_score":0.15851483,"about_ca_system_score_codex":0.0000027292501,"about_ca_system_score_gemma":0.00016849276,"threshold_uncertainty_score":0.9995568},"labels":[],"label_agreement":null},{"id":"W2089574489","doi":"10.1002/2013je004466","title":"Time‐dependent rotational stability of dynamic planets with elastic lithospheres","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Planets","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Ottawa","funders":"Harvard University","keywords":"Planet; Bulge; Mars Exploration Program; Physics; Mantle (geology); Mechanics; Inertia; Geology; Geophysics; Classical mechanics; Astrobiology; Astrophysics; Galaxy","score_opus":0.019035322420653963,"score_gpt":0.26759271676112584,"score_spread":0.24855739434047186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089574489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99778014,0.0001118018,0.000029231165,0.00017386979,0.00012572813,0.00029505038,0.00024573953,0.0000076015435,0.0012308626],"genre_scores_gemma":[0.99889886,0.000025437914,0.0005528427,0.000013181607,0.00019937486,0.0000020776795,0.000099521,0.000006480116,0.0002022015],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9966377,0.00039094122,0.00052698946,0.00022391336,0.0017192145,0.00050121656],"domain_scores_gemma":[0.99698085,0.0015098675,0.00030726567,0.00022266721,0.0006444044,0.00033496215],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00095828495,0.00016931236,0.00045786603,0.00010946243,0.000113632545,0.00011106482,0.0004502461,0.00007649345,0.008031774],"category_scores_gemma":[0.00019717618,0.00010882511,0.00006885728,0.00021438883,0.00033193568,0.00039202633,0.00003107045,0.00045742522,0.00090188184],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.019285277,0.0059068287,0.3019063,0.0027953382,0.003597363,0.002413204,0.005038658,0.045566633,0.39703372,0.0018310539,0.044935446,0.16969019],"study_design_scores_gemma":[0.0008720138,0.0028271698,0.9818058,0.00014023187,0.000034664947,0.00007057505,0.00015980781,0.0067850896,0.001875513,0.004647826,0.00054930896,0.00023198905],"about_ca_topic_score_codex":0.0033671062,"about_ca_topic_score_gemma":0.00032425343,"teacher_disagreement_score":0.6798995,"about_ca_system_score_codex":0.000011815382,"about_ca_system_score_gemma":0.00029609565,"threshold_uncertainty_score":0.999876},"labels":[],"label_agreement":null},{"id":"W2090044000","doi":"10.1007/pl00007667","title":"Experimental study of the K2ZrSi3O9 (wadeite)–K2TiSi3O9 and K2(Zr,Ti)Si3O9–phlogopite systems at 2–3 GPa","year":2000,"lang":"en","type":"article","venue":"Contributions to Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Phlogopite; Forsterite; Solid solution; Mica; Solubility; Geology; Mineralogy; Materials science; Analytical Chemistry (journal); Crystallography; Mantle (geology); Chemistry; Geochemistry; Metallurgy; Physical chemistry","score_opus":0.005881071942817648,"score_gpt":0.2244729234519695,"score_spread":0.21859185150915186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090044000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949081,0.0016682555,0.000007971213,0.0006913941,0.00060454535,0.00046805726,0.00086299627,0.000017349757,0.0007713493],"genre_scores_gemma":[0.9977442,0.00004234202,0.000009366757,0.000261429,0.00017634427,0.000017204447,0.00007870206,0.0000036774072,0.0016667264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985597,0.0003443918,0.00030479702,0.00032938053,0.000110014706,0.00035169534],"domain_scores_gemma":[0.99929494,0.00017053375,0.00007944153,0.00027011728,0.000053283788,0.00013168601],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023777525,0.0001718974,0.00039361417,0.00006162823,0.00041754526,0.000033664583,0.00018874332,0.00013070427,0.0012691811],"category_scores_gemma":[0.000026227644,0.00012070146,0.000038351147,0.00012880829,0.00020938451,0.00007497226,0.00006232207,0.000103718245,0.000060832306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019644424,0.0012008228,0.8729638,0.00008352762,0.00082048227,0.000108175904,0.006335732,0.0070102345,0.08313523,0.007977733,0.014122095,0.0042777564],"study_design_scores_gemma":[0.002757158,0.0022016705,0.9318008,0.000014849675,0.00016493184,0.00019224484,0.00028975116,0.0005674124,0.0009803324,0.00023795287,0.060453583,0.00033932307],"about_ca_topic_score_codex":0.0028978817,"about_ca_topic_score_gemma":0.0017333289,"teacher_disagreement_score":0.0821549,"about_ca_system_score_codex":0.0000059803333,"about_ca_system_score_gemma":0.000021116646,"threshold_uncertainty_score":0.9996438},"labels":[],"label_agreement":null},{"id":"W2090255613","doi":"10.1016/j.scriptamat.2004.09.031","title":"The possible role of partial dislocations in facilitating transformations of the Nishiyama–Wassermann type","year":2004,"lang":"en","type":"article","venue":"Scripta Materialia","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Partial dislocations; Interpretation (philosophy); Phenomenon; Slip (aerodynamics); Materials science; Type (biology); Analogy; Dislocation; Crystallography; Theoretical physics; Physics; Epistemology; Chemistry; Biology; Philosophy; Thermodynamics; Composite material; Linguistics; Paleontology","score_opus":0.009857876892761491,"score_gpt":0.2104553502912202,"score_spread":0.2005974733984587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090255613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918057,0.000102248574,0.0000123931395,0.0002725833,0.0061820424,0.00019461891,0.00029484456,0.000008639502,0.0011269493],"genre_scores_gemma":[0.99939185,0.000016736862,0.00010666917,0.000012889124,0.00004088837,0.0000030401677,0.000039978215,0.0000021092926,0.00038586304],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99921954,0.00007486483,0.00031898348,0.000081972175,0.0001453551,0.00015927544],"domain_scores_gemma":[0.9996193,0.000008443599,0.00009908411,0.00020267372,0.000047226455,0.000023279628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025767324,0.00006952802,0.00011882425,0.000020303038,0.00016065309,0.00006293331,0.00025399827,0.000031870262,0.00014208685],"category_scores_gemma":[0.00003266298,0.000040597588,0.000034583903,0.00018553925,0.000097803604,0.00018719099,0.0000119718425,0.000035720605,0.000030895517],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004630818,0.00025593396,0.07759557,0.000505921,0.00014517817,0.0000021851354,0.029161127,0.0068304753,0.79852235,0.07369175,0.0057649477,0.0070614587],"study_design_scores_gemma":[0.0009160553,0.00017289544,0.71708566,0.00016249853,0.000054754662,0.000002810703,0.0028822287,0.00058088254,0.19322623,0.05529843,0.029328648,0.00028888162],"about_ca_topic_score_codex":0.0051628393,"about_ca_topic_score_gemma":0.0019651195,"teacher_disagreement_score":0.6394901,"about_ca_system_score_codex":0.000002594359,"about_ca_system_score_gemma":0.00007114871,"threshold_uncertainty_score":0.7804703},"labels":[],"label_agreement":null},{"id":"W2090510953","doi":"10.1103/physrevlett.104.065702","title":"Structure and Phase Boundaries of Compressed Liquid Hydrogen","year":2010,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts; Dalhousie University; Western Canada Research Grid","keywords":"Molecular dynamics; Dissociation (chemistry); Phase transition; Chemical physics; Hydrogen; Compressed hydrogen; Materials science; Hydrogen molecule; Thermodynamics; Liquid hydrogen; Drop (telecommunication); Condensed matter physics; Physics; Hydrogen storage; Physical chemistry; Chemistry; Computational chemistry; Quantum mechanics","score_opus":0.008636000098331138,"score_gpt":0.25243926060449745,"score_spread":0.24380326050616632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090510953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99650306,0.0017383788,0.0000065499703,0.0010525857,0.00019589951,0.00016721265,0.0002432893,0.000013290746,0.00007975752],"genre_scores_gemma":[0.99751693,0.00030487275,0.00010428413,0.0017895489,0.00020714446,9.741632e-7,0.000071305,0.0000030880867,0.0000018569294],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993343,0.0000424255,0.00015612177,0.00016279516,0.00015346415,0.00015094169],"domain_scores_gemma":[0.99956125,0.00006266324,0.00009189983,0.00018376796,0.000018728113,0.000081682745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000076158336,0.000115291776,0.00034077768,0.0000122674155,0.000078945486,0.000045564993,0.00014250718,0.000010419146,0.00050110574],"category_scores_gemma":[0.000022754612,0.00008228881,0.00005499856,0.00006584894,0.00025890334,0.000111056055,0.000015182546,0.0001074072,0.000022038641],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044345885,0.000035579775,0.00047311248,0.0008779871,0.00003825797,0.0000044405074,0.00012780385,0.000039649654,0.99250185,0.00050579134,0.0014850391,0.0038661526],"study_design_scores_gemma":[0.0026081922,0.0011392913,0.025177373,0.0013245262,0.00077133987,0.00003186844,0.000011222119,0.0043783532,0.37035683,0.0047843284,0.58788323,0.0015334538],"about_ca_topic_score_codex":0.00021041758,"about_ca_topic_score_gemma":0.0000375565,"teacher_disagreement_score":0.622145,"about_ca_system_score_codex":3.0365246e-7,"about_ca_system_score_gemma":0.000015770756,"threshold_uncertainty_score":0.5486756},"labels":[],"label_agreement":null},{"id":"W2091484291","doi":"10.1103/physrevlett.103.055503","title":"Structural Prediction and Phase Transformation Mechanisms in Calcium at High Pressure","year":2009,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Metadynamics; Anharmonicity; Enthalpy; Thermodynamics; Materials science; Phase (matter); Transformation (genetics); Range (aeronautics); Superconductivity; Phase transition; Molecular dynamics; Condensed matter physics; Physics; Chemistry; Computational chemistry; Quantum mechanics","score_opus":0.012415776284752527,"score_gpt":0.2516268038170663,"score_spread":0.2392110275323138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091484291","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99469954,0.0014905853,0.00014714424,0.0028723695,0.00014813748,0.00036498377,0.00016922748,0.00002605777,0.000081967904],"genre_scores_gemma":[0.996467,0.00057865796,0.000061439,0.0025562972,0.00012289692,0.0000026397934,0.00020431318,0.0000019694,0.0000048064576],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99920624,0.000070331625,0.00018567243,0.00017933427,0.00017630294,0.00018213919],"domain_scores_gemma":[0.999744,0.000024040453,0.0000549223,0.00009890136,0.000008920308,0.000069227026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011122864,0.000121355784,0.0002556723,0.000021518714,0.00006161454,0.000027329977,0.00007433859,0.0000124344015,0.00016756219],"category_scores_gemma":[0.000005747591,0.00009095619,0.000041289422,0.00008807617,0.000021325824,0.00028844428,0.0000040830137,0.00006982091,0.000030016892],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061593455,0.00033005996,0.0022413023,0.005476182,0.00017760959,0.00006625912,0.0031333338,0.018888056,0.67891717,0.01374844,0.0076966872,0.26870897],"study_design_scores_gemma":[0.006914052,0.0019308778,0.74949443,0.0026438097,0.0009356955,0.000049007336,0.000023994866,0.15601255,0.01983092,0.028685883,0.03160742,0.0018713416],"about_ca_topic_score_codex":0.0001744851,"about_ca_topic_score_gemma":0.000018862153,"teacher_disagreement_score":0.7472531,"about_ca_system_score_codex":0.00000304836,"about_ca_system_score_gemma":0.0000041434073,"threshold_uncertainty_score":0.3709086},"labels":[],"label_agreement":null},{"id":"W2092260788","doi":"10.1016/j.tecto.2008.07.003","title":"The three-dimensional thermo-mechanical signature of ridge subduction and slab window migration","year":2008,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Subduction; Slab window; Forearc; Slab; Geodynamics; Lithosphere; Seismology; Metamorphism; Window (computing); Mantle (geology); Asthenosphere; Plate tectonics; Mid-ocean ridge; Magmatism; Geophysics; Trench; Volcanic arc; Petrology; Mantle wedge; Tectonics; Oceanic crust","score_opus":0.010146633227909893,"score_gpt":0.18382183506816388,"score_spread":0.17367520184025398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092260788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987266,0.0002809007,0.00006372507,0.00019058243,0.00035061126,0.00013391244,0.0000700648,0.000025072482,0.00015853638],"genre_scores_gemma":[0.9993903,0.00007485291,0.0001626229,0.000031279116,0.00023739008,0.0000012982725,0.000056459277,0.0000037594239,0.000042049516],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993024,0.00004250881,0.00015107734,0.00015833754,0.00019776677,0.00014793087],"domain_scores_gemma":[0.99953103,0.0001159863,0.00009530677,0.00016253995,0.00005498848,0.000040173752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012291715,0.00010444014,0.00014220393,0.000014464102,0.0002792382,0.00002103776,0.000103722115,0.00006267357,0.0000642141],"category_scores_gemma":[0.000011856941,0.0000664724,0.00004020964,0.000103651466,0.0001256954,0.00011916767,0.000013698871,0.0000973601,0.000026952675],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005377865,0.00012687067,0.013570687,0.000066372304,0.0001758999,0.000020397296,0.0007479956,0.0035567658,0.9146924,0.010252038,0.0030834894,0.053169325],"study_design_scores_gemma":[0.0008490723,0.0005998844,0.73337865,0.000035763256,0.000082082646,0.000041510466,0.000042747655,0.01198372,0.20659712,0.041284375,0.004582376,0.00052271894],"about_ca_topic_score_codex":0.0010428078,"about_ca_topic_score_gemma":0.0004056252,"teacher_disagreement_score":0.7198079,"about_ca_system_score_codex":0.00000145422,"about_ca_system_score_gemma":0.000038363964,"threshold_uncertainty_score":0.27106658},"labels":[],"label_agreement":null},{"id":"W2092424049","doi":"10.1073/pnas.1120243109","title":"Stability of dense liquid carbon dioxide","year":2012,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Western Canada Research Grid","keywords":"Phase diagram; Triple point; Melting point; Phase transition; Thermodynamics; Ab initio; Mantle (geology); Materials science; Chemistry; Phase (matter); Physics; Organic chemistry","score_opus":0.035616554578066645,"score_gpt":0.25825565201739326,"score_spread":0.2226390974393266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092424049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99084514,0.0002135468,7.960378e-8,0.00027666602,0.000055324585,0.00009215558,0.00004499266,0.000004611168,0.008467494],"genre_scores_gemma":[0.99954635,0.00001566927,0.00028076692,0.000037723974,0.00010060457,6.707204e-7,1.5944975e-7,8.638772e-7,0.000017204862],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986349,0.000010299165,0.00027935553,0.00011882445,0.00079416984,0.0001624728],"domain_scores_gemma":[0.9993411,0.00011153507,0.00034851674,0.000008092276,0.00014774641,0.00004306849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018254769,0.000064833715,0.00015685007,0.00005283377,0.00007419547,0.0000072262874,0.00046889586,0.00004748606,0.000094648865],"category_scores_gemma":[0.000276295,0.00003958706,0.000050938834,0.0003268896,0.00056014606,0.0003589631,0.00004014542,0.000057843416,0.0000015305975],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048951377,0.000037605023,0.26637855,0.00010527629,0.0000128577385,1.2736262e-9,0.00041546384,0.00006521313,0.7251385,0.0076012863,0.000047564063,0.00014872482],"study_design_scores_gemma":[0.000042783144,0.000042408,0.4057491,0.000023283277,0.000008023886,9.2072355e-7,0.00007078815,0.00009103459,0.5893517,0.004501041,0.000076521115,0.000042334497],"about_ca_topic_score_codex":0.00019804065,"about_ca_topic_score_gemma":6.9828786e-7,"teacher_disagreement_score":0.13937058,"about_ca_system_score_codex":0.000002503734,"about_ca_system_score_gemma":0.000021799846,"threshold_uncertainty_score":0.20638816},"labels":[],"label_agreement":null},{"id":"W2092678271","doi":"10.1016/j.gca.2009.02.011","title":"The effect of CO2 on the speciation of RbBr in solution at temperatures to 579°C and pressures to 0.26GPa","year":2009,"lang":"en","type":"article","venue":"Geochimica et Cosmochimica Acta","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Basic Energy Sciences; Natural Sciences and Engineering Research Council of Canada; Simon Fraser University; Australian Synchrotron; U.S. Department of Energy","keywords":"Extended X-ray absorption fine structure; Chemistry; Corundum; Coordination number; Pairing; Genetic algorithm; Salt (chemistry); Ion; Inorganic chemistry; Analytical Chemistry (journal); Mineralogy; Absorption spectroscopy; Physical chemistry; Chromatography","score_opus":0.0058634593454207256,"score_gpt":0.21712183206534538,"score_spread":0.21125837271992465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092678271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887573,0.00007442034,0.0000014790525,0.008843932,0.00019037766,0.000693914,0.00017026137,0.000012850924,0.0012554605],"genre_scores_gemma":[0.9990159,0.00006529278,0.000055136687,0.000645564,0.00007784885,0.0000056363424,0.00003845161,0.0000040694686,0.000092059716],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984823,0.0003530934,0.00030822793,0.00026293166,0.00030927293,0.0002842067],"domain_scores_gemma":[0.9985299,0.0008578149,0.00014504591,0.00034771208,0.000037448837,0.000082073144],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008323693,0.00017828836,0.00030227023,0.00008229294,0.00018283841,0.000067582245,0.00032547957,0.00006198882,0.000070792354],"category_scores_gemma":[0.00027999518,0.000097967684,0.000052685013,0.0002063111,0.00006362414,0.000072107905,0.000046382585,0.00012285524,0.000019467412],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003983103,0.000101455465,0.014489852,0.00008856846,0.00009398927,0.0000039812494,0.0021667203,0.0025953809,0.9197048,0.003382157,0.04710669,0.0062832907],"study_design_scores_gemma":[0.00042496578,0.0015022916,0.7884377,0.000108375105,0.000034058987,0.000002988873,0.000020282529,0.00021674695,0.1996579,0.001608317,0.0077788704,0.00020749192],"about_ca_topic_score_codex":0.0004790607,"about_ca_topic_score_gemma":0.0012995533,"teacher_disagreement_score":0.77394783,"about_ca_system_score_codex":0.000005617716,"about_ca_system_score_gemma":0.000019747466,"threshold_uncertainty_score":0.39950064},"labels":[],"label_agreement":null},{"id":"W2092773977","doi":"10.1063/1.4870526","title":"High-pressure single-crystal elasticity study of CO2 across phase I-III transition","year":2014,"lang":"en","type":"article","venue":"Applied Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"U.S. Department of Energy","keywords":"Brillouin Spectroscopy; Elasticity (physics); Phase transition; Materials science; Single crystal; Anisotropy; Bulk modulus; Raman spectroscopy; Elastic modulus; Brillouin scattering; Diffraction; Shear modulus; Analytical Chemistry (journal); Condensed matter physics; Thermodynamics; Crystallography; Chemistry; Optics; Composite material; Physics","score_opus":0.010805254302345057,"score_gpt":0.2137910198923616,"score_spread":0.20298576559001655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092773977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99113595,0.0000046181026,0.007258811,0.000057717618,0.00037962702,0.00042420832,0.00041210707,0.00005723129,0.00026974897],"genre_scores_gemma":[0.9986379,6.345745e-7,0.00015665135,0.00033228897,0.00056342746,0.0000066479743,0.00028610727,0.0000111230465,0.00000520964],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9984459,0.00008683498,0.00033406526,0.00037405672,0.00038234415,0.00037677778],"domain_scores_gemma":[0.9992183,0.00012547686,0.0001982107,0.00032825288,0.0000355574,0.00009424074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021912795,0.00023616446,0.00044330925,0.000022186194,0.00018286589,0.00007440851,0.00025569194,0.00005630135,0.00015138222],"category_scores_gemma":[0.0000036207405,0.00021605568,0.00006407929,0.00016503193,0.000117662676,0.00015385021,0.00001988023,0.000123883,0.00004917419],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000502492,0.0009757154,0.0002805997,0.00008971134,0.00021084616,0.000004432996,0.004931753,0.13015322,0.855473,0.0007453206,0.0007365894,0.005896314],"study_design_scores_gemma":[0.08679256,0.009860677,0.08326905,0.00023521026,0.0032609587,0.0000123741265,0.0068020774,0.025881786,0.752725,0.008096851,0.016175266,0.0068881987],"about_ca_topic_score_codex":0.0014789937,"about_ca_topic_score_gemma":0.00012690332,"teacher_disagreement_score":0.10427144,"about_ca_system_score_codex":0.0000021804171,"about_ca_system_score_gemma":0.000008055964,"threshold_uncertainty_score":0.8810495},"labels":[],"label_agreement":null},{"id":"W2093306856","doi":"10.1029/2007gl029535","title":"New constraints on the upper mantle structure of the Slave craton from Rayleigh wave inversion","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Craton; Lithosphere; Geology; Mantle (geology); Geophysics; Anisotropy; Seismogram; Seismology; Amplitude; Tectonics; Physics","score_opus":0.026277385617072477,"score_gpt":0.2556632531616265,"score_spread":0.22938586754455403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093306856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912715,0.000014199376,0.000039151946,0.0057798894,0.0004594958,0.00030113524,0.00026645532,0.000010245449,0.001857926],"genre_scores_gemma":[0.99762404,0.0000042171423,0.00011320974,0.0014369419,0.000619322,3.7706047e-7,0.00004096355,0.0000055552496,0.00015539321],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9976006,0.00029638768,0.00019293636,0.00029891267,0.0010563888,0.00055477885],"domain_scores_gemma":[0.998021,0.0012062474,0.000070669674,0.00047660535,0.00006290247,0.00016256329],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004380426,0.00014786878,0.00018956652,0.000052965115,0.00029435955,0.00008011531,0.00054581923,0.00007651073,0.0046524396],"category_scores_gemma":[0.0001286742,0.00007444632,0.00010884972,0.00030874708,0.00053822034,0.00008585122,0.000083629646,0.00047674103,0.00033891224],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003288415,0.00003548594,0.0040103975,0.00002010254,0.00009263661,0.000037314094,0.0008430569,0.00011817916,0.89554554,0.0040891385,0.06581505,0.029064288],"study_design_scores_gemma":[0.0004973622,0.00017029005,0.63686347,0.00008605618,0.000021662621,0.0000012274348,0.0002504714,0.00025657914,0.33926395,0.014047637,0.0083036935,0.00023763067],"about_ca_topic_score_codex":0.0077959793,"about_ca_topic_score_gemma":0.00039302057,"teacher_disagreement_score":0.63285303,"about_ca_system_score_codex":0.00000821637,"about_ca_system_score_gemma":0.000076123804,"threshold_uncertainty_score":0.9988112},"labels":[],"label_agreement":null},{"id":"W2093381495","doi":"10.1103/physrevlett.89.224301","title":"Nature of Mechanical Instabilities and Their Effect on Kinetic Friction","year":2002,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Kinetic energy; Materials science; Mechanics; Classical mechanics; Thermodynamics; Physics","score_opus":0.008781779574567739,"score_gpt":0.21456007982518271,"score_spread":0.20577830025061497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093381495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932934,0.0046521854,0.0000041249864,0.0011647887,0.00015493053,0.00020398558,0.00003402588,0.00001501903,0.00047751475],"genre_scores_gemma":[0.99601007,0.0015771398,0.000012584165,0.0022383556,0.00014121538,0.0000028164475,0.0000110693645,0.0000026733833,0.000004091461],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993202,0.00013184795,0.00012530427,0.00016858778,0.00012744205,0.00012663439],"domain_scores_gemma":[0.9994658,0.00027583016,0.000054803113,0.00014575261,0.000009638302,0.0000481445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001198259,0.00011861566,0.00032197594,0.00001515026,0.000033543576,0.000012909971,0.00008374633,0.000015687157,0.0002855478],"category_scores_gemma":[0.000042759235,0.00007065487,0.0000759088,0.00008148881,0.000046626225,0.000060358092,0.000008422539,0.00012450025,0.00006393709],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027895367,0.0007069326,0.0064396188,0.02287346,0.00046899694,0.000030965602,0.0019084978,0.0018099814,0.5517757,0.012684146,0.03712728,0.36389545],"study_design_scores_gemma":[0.004650186,0.014487314,0.27755195,0.01783618,0.0014676563,0.000056004523,0.00009087422,0.075244695,0.19165078,0.013984088,0.39823788,0.0047423868],"about_ca_topic_score_codex":0.000055382865,"about_ca_topic_score_gemma":0.0000038456096,"teacher_disagreement_score":0.36111063,"about_ca_system_score_codex":0.0000011747719,"about_ca_system_score_gemma":0.0000011934594,"threshold_uncertainty_score":0.31265482},"labels":[],"label_agreement":null},{"id":"W2093476123","doi":"10.1103/physrevb.87.024101","title":"Bonding, structures, and band gap closure of hydrogen at high pressures","year":2013,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Engineering and Physical Sciences Research Council; U.S. Department of Energy","keywords":"Ab initio; Anharmonicity; Raman spectroscopy; Band gap; Molecular dynamics; Molecular physics; Ab initio quantum chemistry methods; Valence (chemistry); Hydrogen; Spectral line; Chemistry; Graphene; Electronic structure; Materials science; Chemical physics; Condensed matter physics; Molecule; Computational chemistry; Nanotechnology; Physics","score_opus":0.011799737512688837,"score_gpt":0.23639426814409348,"score_spread":0.22459453063140464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093476123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9712545,0.02617262,5.174059e-7,0.00021890494,0.000090295165,0.00035100026,0.00012564835,0.000014953481,0.0017715383],"genre_scores_gemma":[0.9964528,0.0028089595,0.00006496543,0.00018325116,0.00018409357,0.00000473405,0.00006548977,0.000004366642,0.00023131522],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990838,0.00007609077,0.00020132147,0.00022035989,0.00021830155,0.00020009192],"domain_scores_gemma":[0.9994159,0.00009239422,0.00012577944,0.00021237622,0.00003598528,0.00011761465],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009690483,0.00014527474,0.00044179658,0.000013087777,0.000063643274,0.000027911692,0.00015293453,0.000027623599,0.0021759784],"category_scores_gemma":[0.0000310659,0.000096364995,0.000070482754,0.000074675736,0.00008192897,0.00013688437,0.000029377352,0.00005635563,0.00018147696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016680882,0.000379278,0.31387258,0.027686404,0.0010975011,0.000037618564,0.0010563205,0.000395129,0.23726009,0.10949109,0.191614,0.11694319],"study_design_scores_gemma":[0.00055019825,0.00032222574,0.6402013,0.00093071634,0.0004405444,0.0000116302,0.0000052450046,0.00019218895,0.03657197,0.15898393,0.16110678,0.00068329903],"about_ca_topic_score_codex":0.0016868676,"about_ca_topic_score_gemma":0.000050237104,"teacher_disagreement_score":0.3263287,"about_ca_system_score_codex":0.000001006012,"about_ca_system_score_gemma":0.00001004772,"threshold_uncertainty_score":0.99873614},"labels":[],"label_agreement":null},{"id":"W2093488255","doi":"10.1144/sp282.6","title":"Roles of lithospheric strain softening and heterogeneity in determining the geometry of rifts and continental margins","year":2007,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Lithosphere; Rift; Strain (injury); Continental margin; Geometry; Seismology; Mathematics; Tectonics","score_opus":0.013795743416175642,"score_gpt":0.23032090032066338,"score_spread":0.21652515690448773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093488255","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99824345,0.00024215566,0.00016076826,0.00031502565,0.00007067165,0.00014619519,0.00013101309,0.000009742833,0.00068096555],"genre_scores_gemma":[0.9982647,0.00009317879,0.001326175,0.000075562624,0.00016291582,0.0000013841251,0.000049301958,0.0000015848727,0.000025235402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913853,0.00004377274,0.00029322176,0.00017744978,0.00013730883,0.00020968882],"domain_scores_gemma":[0.9993467,0.00029123557,0.0001433129,0.000101933176,0.000053545227,0.00006330692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000655625,0.00008632213,0.00020217155,0.000020885878,0.00011484697,0.000037751823,0.00013884746,0.00008652859,0.00025728],"category_scores_gemma":[0.000099338235,0.000058690952,0.000056317982,0.0002562326,0.00034808088,0.00011593217,0.000050501476,0.00009318049,0.000001284735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000127829735,0.00003506503,0.9827157,0.000011334059,0.000013246071,3.0069523e-7,0.00035531702,0.000030655927,0.0007617272,0.0011404945,0.00007983585,0.014843517],"study_design_scores_gemma":[0.00023653613,0.00005002323,0.9962147,0.000004435128,0.000008408888,0.0000013722088,0.00026966716,0.00016619332,0.00021602848,0.00059174385,0.002175877,0.00006504582],"about_ca_topic_score_codex":0.00033826358,"about_ca_topic_score_gemma":0.0013753929,"teacher_disagreement_score":0.014778472,"about_ca_system_score_codex":0.0000019588392,"about_ca_system_score_gemma":0.000014286763,"threshold_uncertainty_score":0.28170356},"labels":[],"label_agreement":null},{"id":"W2093584929","doi":"10.1107/s0021889805017358","title":"Quantum software interfaced with crystal-structure databases: tools, results and perspectives","year":2005,"lang":"en","type":"article","venue":"Journal of Applied Crystallography","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"ASCII; Computer science; File format; Database; Software; Diamond; Computational science; Operating system; Materials science","score_opus":0.013821076914315972,"score_gpt":0.2046896934621049,"score_spread":0.19086861654778892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093584929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99544406,0.0007957265,0.00093441794,0.0002596457,0.0001303416,0.00017083406,0.0008526021,0.000028103825,0.0013842558],"genre_scores_gemma":[0.986237,0.00015656784,0.013111181,0.000081502796,0.0003344245,4.3125138e-7,0.00006138713,0.000007971974,0.000009552508],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99868023,0.000033842996,0.0004193135,0.00025820726,0.00033967508,0.00026869803],"domain_scores_gemma":[0.9989666,0.00011682567,0.000422776,0.0002029514,0.00011612531,0.00017476972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026778577,0.00021684333,0.00036824864,0.0002013925,0.00013116203,0.00017466204,0.00022817736,0.000058740414,0.0002505997],"category_scores_gemma":[0.000023812052,0.0001427123,0.0000737433,0.00022819311,0.0001700425,0.00048722248,0.000022303351,0.00022589431,0.0000024767219],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.055394094,0.001192272,0.047752164,0.0011189855,0.0057681864,0.0007240266,0.047958896,0.07719823,0.566479,0.021113824,0.035721358,0.13957895],"study_design_scores_gemma":[0.01724228,0.005294662,0.4220455,0.0006898372,0.0010838875,0.0011868161,0.023957802,0.000630759,0.011725426,0.01561783,0.4972274,0.0032978016],"about_ca_topic_score_codex":0.0000562375,"about_ca_topic_score_gemma":0.000259237,"teacher_disagreement_score":0.5547536,"about_ca_system_score_codex":0.0000035394855,"about_ca_system_score_gemma":0.00005116342,"threshold_uncertainty_score":0.5819639},"labels":[],"label_agreement":null},{"id":"W2093892371","doi":"10.1016/j.lithos.2008.09.016","title":"A comparison of cratonic roots through consistent analysis of seismic surface waves","year":2008,"lang":"en","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; Agence Nationale de la Recherche","keywords":"Lithosphere; Yilgarn Craton; Craton; Geology; Proterozoic; Mantle (geology); Geophysics; Seismology; Tectonics","score_opus":0.03683670256979684,"score_gpt":0.276400810759729,"score_spread":0.23956410818993215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093892371","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968646,0.00070743787,0.00013640197,0.00003448956,0.00014089012,0.0000901384,0.0002787369,0.000012740111,0.0017345274],"genre_scores_gemma":[0.99858254,0.000057925412,0.0010312239,0.000027272717,0.000017435428,2.6892965e-7,0.00008618731,0.0000019813788,0.00019516866],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990441,0.00007692178,0.0003510479,0.00016308918,0.00020716176,0.00015766322],"domain_scores_gemma":[0.9993622,0.000100610494,0.00020121613,0.00023679827,0.0000568544,0.00004237226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010924708,0.00009544527,0.0005334857,0.00004463749,0.000059141563,0.000008230773,0.00013894124,0.000037823393,0.0007505441],"category_scores_gemma":[0.000010939782,0.00007597602,0.0001305078,0.00038073034,0.000113924805,0.00008045874,0.0000118655735,0.000039970106,0.000030001178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026399362,0.000053247448,0.97027946,0.000038157174,0.00040455864,0.000003962096,0.0016763329,0.02585169,0.0010937904,0.00010318636,0.00024941986,0.00021981461],"study_design_scores_gemma":[0.0001430483,0.00008814778,0.96077853,0.000013619165,0.0003542377,0.0000013642555,0.00011794794,0.02510104,0.01105712,0.00014026712,0.0020954062,0.00010928923],"about_ca_topic_score_codex":0.010384466,"about_ca_topic_score_gemma":0.00070859323,"teacher_disagreement_score":0.00996333,"about_ca_system_score_codex":9.476591e-7,"about_ca_system_score_gemma":0.00004115053,"threshold_uncertainty_score":0.99620545},"labels":[],"label_agreement":null},{"id":"W2094433872","doi":"10.1103/physreve.86.036407","title":"Electron-ion and ion-ion potentials for modeling warm dense matter: Applications to laser-heated or shock-compressed Al and Si","year":2012,"lang":"en","type":"article","venue":"Physical Review E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Warm dense matter; Ion; Quasistatic process; Electron; Atomic physics; Yukawa potential; Shock wave; Physics; Condensed matter physics; Materials science; Thermodynamics; Quantum mechanics","score_opus":0.02252704594283983,"score_gpt":0.28872263050205893,"score_spread":0.2661955845592191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094433872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831611,0.008760876,0.0047560656,0.0012511533,0.00013428456,0.0016059075,0.00019522493,0.00003943943,0.00009596712],"genre_scores_gemma":[0.99486715,0.002836641,0.00038164406,0.0011879815,0.00043596057,0.00007982001,0.00016719654,0.000007913233,0.0000356724],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990163,0.000060715876,0.00021001673,0.00025741206,0.00012992296,0.0003256763],"domain_scores_gemma":[0.99939686,0.00012167871,0.00005893244,0.00016616349,0.000044471923,0.00021188433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002123796,0.00015401865,0.00035600067,0.000021554373,0.00014469797,0.00005624205,0.000094633855,0.000025595371,0.00010271148],"category_scores_gemma":[0.000021208694,0.00010887482,0.000050535375,0.00010156003,0.000019213476,0.00018120166,0.000023385697,0.00005199867,0.0001486587],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013541393,0.0012134726,0.0056036836,0.012404404,0.0004676188,0.000005203063,0.0010990521,0.008396785,0.7125499,0.0036764739,0.031992085,0.22123718],"study_design_scores_gemma":[0.0031786307,0.0016341548,0.020962086,0.0034128465,0.0021511621,0.000065076725,0.000061882485,0.17652689,0.12713581,0.01957579,0.64175504,0.0035406132],"about_ca_topic_score_codex":0.00015620387,"about_ca_topic_score_gemma":0.000021115937,"teacher_disagreement_score":0.60976297,"about_ca_system_score_codex":0.0000023068317,"about_ca_system_score_gemma":0.0000129181035,"threshold_uncertainty_score":0.4439786},"labels":[],"label_agreement":null},{"id":"W2094468904","doi":"10.1139/e03-038","title":"Structure of the crust and upper mantle of the Great Slave Lake shear zone, northwestern Canada, from teleseismic analysis and gravity modelling","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Shear zone; Seismology; Lithosphere; Crust; Shear wave splitting; Shear (geology); Mantle (geology); Receiver function; Gravity anomaly; Geophysics; Petrology; Tectonics; Paleontology","score_opus":0.008146625900337245,"score_gpt":0.16826840997737313,"score_spread":0.1601217840770359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094468904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99809426,0.00048194797,0.000040993247,0.00011263689,0.00030931205,0.000050257197,0.00080914807,3.4128993e-7,0.00010112571],"genre_scores_gemma":[0.99960214,0.000020009948,0.0002359286,0.00006621375,0.000027490156,2.4431644e-8,0.0000019065121,0.000001187478,0.000045099274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99908847,0.00009378152,0.00023187418,0.00012127967,0.00027507884,0.00018950288],"domain_scores_gemma":[0.99931014,0.000060789163,0.00023571345,0.00012710999,0.00007182795,0.00019444125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023060889,0.00008503187,0.00023128504,0.000086859865,0.00027938996,0.000070103175,0.00027625918,0.000031987773,0.00029712467],"category_scores_gemma":[0.000018488363,0.000044757442,0.000057031386,0.0003893868,0.00035623388,0.0001239686,0.0000071825652,0.00008785961,1.3997936e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000020228122,7.1732615e-7,0.9593716,0.0000050273843,0.000043985045,0.000003126258,0.00029203805,0.03989463,0.00013824011,0.000040809024,0.0000122910415,0.00019547896],"study_design_scores_gemma":[0.000074596195,0.00002569175,0.99446917,0.000025240939,0.00011403254,0.000012936657,0.00020102615,0.0019269281,0.0013621994,0.0006378916,0.0010834101,0.000066901826],"about_ca_topic_score_codex":0.8949585,"about_ca_topic_score_gemma":0.99816996,"teacher_disagreement_score":0.103211455,"about_ca_system_score_codex":0.0000010287284,"about_ca_system_score_gemma":0.0009730951,"threshold_uncertainty_score":0.32533067},"labels":[],"label_agreement":null},{"id":"W2094862865","doi":"10.1063/1.2919571","title":"The relation between shock-state particle velocity and free surface velocity: A molecular dynamics study on single crystal Cu and silica glass","year":2008,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Shock (circulatory); Materials science; Particle velocity; Isotropy; Anisotropy; Stress (linguistics); Crystal (programming language); Free surface; Relaxation (psychology); Particle (ecology); Molecular dynamics; Shock wave; Composite material; Mechanics; Chemistry; Optics; Physics","score_opus":0.01436683828710193,"score_gpt":0.2060720399094291,"score_spread":0.19170520162232718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094862865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988935,0.00005549845,0.00034624012,0.00010169215,0.00007856065,0.00017663749,0.00005466989,0.000008536834,0.000284688],"genre_scores_gemma":[0.99958813,0.00003428105,0.00021041594,0.000027186097,0.000116522344,3.7286247e-7,0.0000066406856,0.0000059712493,0.000010463097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989769,0.00006419638,0.00028227604,0.00014264426,0.00034410943,0.00018988788],"domain_scores_gemma":[0.99919784,0.00022512987,0.0002488956,0.0001637392,0.00005814381,0.00010626436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033967211,0.00012910251,0.00023843725,0.000011075165,0.00032997833,0.00009696083,0.00015001123,0.000035122954,0.0000029678274],"category_scores_gemma":[0.000015547534,0.000091046066,0.000033339227,0.000109247536,0.00010999091,0.00012966382,0.000033005083,0.00017088653,0.0000038847857],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031293218,0.0014609015,0.4511303,0.00012459914,0.0016059714,0.00031454573,0.025898378,0.29214323,0.12325766,0.0055001704,0.0007069344,0.09472797],"study_design_scores_gemma":[0.0016598505,0.0011087847,0.93851036,0.00001476166,0.00014801424,0.000013988845,0.0005329512,0.024987334,0.006785358,0.025584675,0.00033578463,0.00031814075],"about_ca_topic_score_codex":0.0000834295,"about_ca_topic_score_gemma":0.000058279737,"teacher_disagreement_score":0.48738006,"about_ca_system_score_codex":0.000009979552,"about_ca_system_score_gemma":0.000044185937,"threshold_uncertainty_score":0.3712751},"labels":[],"label_agreement":null},{"id":"W2094928143","doi":"10.3367/ufne.0179.200901d.0091","title":"Direct observations of the viscosity of Earth's outer core and extrapolation of measurements of the viscosity of liquid iron","year":2009,"lang":"en","type":"article","venue":"Physics-Uspekhi","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Extrapolation; Viscosity; Arrhenius equation; Outer core; Thermodynamics; Chemistry; Volume (thermodynamics); Temperature dependence of liquid viscosity; Core (optical fiber); Atmospheric pressure; Inner core; Activation energy; Materials science; Relative viscosity; Physics; Physical chemistry; Composite material","score_opus":0.051165918583064296,"score_gpt":0.2324689803649944,"score_spread":0.1813030617819301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094928143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981076,0.00007880791,0.000044125565,0.000059919137,0.00015848652,0.0002387476,0.00030020913,0.0000036586018,0.0010084533],"genre_scores_gemma":[0.99971414,0.000012313867,0.00016391846,0.000020373127,0.00004110279,3.9332832e-7,0.000018270115,0.0000023098096,0.00002716167],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989588,0.00009740172,0.0003458759,0.00012926068,0.00035937608,0.000109277054],"domain_scores_gemma":[0.9989431,0.000056036315,0.00049594697,0.0003304985,0.00014978653,0.00002462129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024513353,0.00010392363,0.00030678112,0.000017731567,0.000066017776,0.0000058284495,0.00023476376,0.00003790524,0.000033600823],"category_scores_gemma":[0.000023344639,0.00006546338,0.000103282066,0.00019185587,0.00017513309,0.00015245541,0.00002925879,0.000047162775,6.095789e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111874535,0.00014307567,0.21427813,0.00013236704,0.000049350318,4.97464e-8,0.0007974482,0.0015347586,0.78139025,0.0006872519,0.00004212551,0.0008333007],"study_design_scores_gemma":[0.00013078918,0.00010820947,0.6332049,0.00005770139,0.000048816044,7.681647e-8,0.0000071716627,0.00014497146,0.3654724,0.00076121994,0.00002093011,0.000042831292],"about_ca_topic_score_codex":0.0013572541,"about_ca_topic_score_gemma":0.00026472905,"teacher_disagreement_score":0.41892675,"about_ca_system_score_codex":0.0000012660788,"about_ca_system_score_gemma":0.000040108876,"threshold_uncertainty_score":0.26695192},"labels":[],"label_agreement":null},{"id":"W2095082201","doi":"10.1139/p09-006","title":"High-pressure phase transition and thermodynamic properties of MgSe: Ab initio study","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Heat capacity; Ab initio; Thermodynamics; Debye model; Phase transition; Physics; Debye; Caesium; Phase (matter); Debye function; Ab initio quantum chemistry methods; High pressure; Condensed matter physics; Debye length; Ion; Molecule; Quantum mechanics","score_opus":0.013759937875660436,"score_gpt":0.2008207895339652,"score_spread":0.18706085165830477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095082201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99860924,0.0005503878,0.00006660412,0.00013342036,0.00020832302,0.00012179029,0.00021299401,0.000002805295,0.00009441567],"genre_scores_gemma":[0.9996004,0.000017243614,0.000043383046,0.00007232177,0.00024041382,1.5776564e-7,0.000013078208,0.0000029543985,0.000010038654],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9993166,0.000065480235,0.00023813,0.00008265577,0.0001399234,0.00015725581],"domain_scores_gemma":[0.9994376,0.0000108986715,0.0001549843,0.000090955815,0.000104794584,0.00020080198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015455767,0.00009833945,0.00024597842,0.000059198363,0.0000889536,0.000053346623,0.00012712067,0.000031055515,0.00009908377],"category_scores_gemma":[0.000006878464,0.00007582643,0.000039618502,0.000085511274,0.0000627321,0.00025831448,0.0000010834799,0.00008993185,0.000003390164],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00174632,0.0019263846,0.014691418,0.000717034,0.0019429249,0.0012263001,0.06599076,0.044727646,0.3745619,0.00767364,0.0024832468,0.4823124],"study_design_scores_gemma":[0.019365747,0.021347953,0.7974591,0.0012370072,0.002589553,0.00027517008,0.0075501753,0.011351399,0.0551231,0.07759362,0.003645649,0.0024615314],"about_ca_topic_score_codex":0.008236525,"about_ca_topic_score_gemma":0.0052007465,"teacher_disagreement_score":0.78276765,"about_ca_system_score_codex":0.00000255234,"about_ca_system_score_gemma":0.00021188795,"threshold_uncertainty_score":0.9983677},"labels":[],"label_agreement":null},{"id":"W2095263981","doi":"10.1111/j.1745-3933.2009.00688.x","title":"Constraining white dwarf kicks in globular clusters – IV. Retarding core collapse","year":2009,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Globular cluster; Physics; Astrophysics; White dwarf; Astronomy; Core (optical fiber); Stars; Optics","score_opus":0.009267406507130163,"score_gpt":0.19135413241721944,"score_spread":0.1820867259100893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095263981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99520767,0.000058226822,0.000023262804,0.0033846719,0.00044511136,0.00023084616,0.000105335545,0.000021433949,0.00052344485],"genre_scores_gemma":[0.9963567,2.512689e-7,0.002489399,0.00092122715,0.00017229511,8.989366e-7,0.000027638973,0.0000049304563,0.000026630887],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99850965,0.00008475125,0.00039536774,0.0003085401,0.00023939746,0.00046232357],"domain_scores_gemma":[0.99932,0.00008701454,0.00022193122,0.0002527567,0.000015705127,0.00010262659],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003813883,0.0002062954,0.0003777345,0.000018594648,0.0001433621,0.00008009362,0.00050457293,0.000092100745,0.00014511391],"category_scores_gemma":[0.000019404786,0.00015806485,0.00028523357,0.000116427145,0.00023009657,0.00013039247,0.00004605784,0.00021023377,0.000015043602],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053582844,0.000016848371,0.13810994,0.000014430156,0.000042614447,0.0000011816652,0.0005238722,0.8585153,0.00072566804,0.0000075459843,0.0013547214,0.00063429703],"study_design_scores_gemma":[0.0007540138,0.00007578082,0.7310869,0.000098074095,0.00006377027,8.046241e-8,0.00038268993,0.26633134,0.00030782344,0.000023918208,0.0005934276,0.00028218076],"about_ca_topic_score_codex":0.00097640767,"about_ca_topic_score_gemma":0.00013456099,"teacher_disagreement_score":0.592977,"about_ca_system_score_codex":0.000020073461,"about_ca_system_score_gemma":0.00003160736,"threshold_uncertainty_score":0.6445698},"labels":[],"label_agreement":null},{"id":"W2095317490","doi":"10.1046/j.1365-246x.2000.00027.x","title":"Surface loading of a viscoelastic planet--III. Aspherical models","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research; David and Lucile Packard Foundation","keywords":"Eigenfunction; Normal mode; Viscoelasticity; Perturbation (astronomy); Linearization; Eigenvalues and eigenvectors; Physics; Mathematical analysis; Lithosphere; Mode coupling; Perturbation theory (quantum mechanics); Series expansion; Classical mechanics; Nonlinear system; Mathematics; Geology; Quantum mechanics","score_opus":0.012523705950257062,"score_gpt":0.21992086295124338,"score_spread":0.20739715700098632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095317490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98035234,0.000056116998,0.00086070073,0.00016094638,0.0008814062,0.00005528806,0.00017539553,0.000019268693,0.017438564],"genre_scores_gemma":[0.99723667,0.0000566378,0.0008208901,0.00008936353,0.00082255946,2.4393012e-7,0.00008771026,0.0000049853707,0.0008809601],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986155,0.00005835499,0.00036535985,0.00017438908,0.0005272792,0.00025909572],"domain_scores_gemma":[0.99939996,0.0001302064,0.00013789664,0.0000973555,0.00007334529,0.00016120961],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014609373,0.0001396939,0.0002500445,0.000029268156,0.000094706666,0.00012018648,0.0003811094,0.000052488067,0.01818354],"category_scores_gemma":[0.000008872318,0.000110942354,0.00009271438,0.00008481086,0.0000745912,0.00039516363,0.000014401055,0.00019961997,0.0006309983],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012467892,0.0004312698,0.004073263,0.00003279711,0.0005999365,0.00024698238,0.0007068298,0.88315415,0.013101061,0.0066247005,0.008265047,0.08151718],"study_design_scores_gemma":[0.004070968,0.0012222759,0.13616295,0.0002851789,0.00021478509,0.0007435371,0.00017652639,0.6847009,0.004209835,0.10945786,0.057303324,0.0014518602],"about_ca_topic_score_codex":0.00095554366,"about_ca_topic_score_gemma":0.000021946324,"teacher_disagreement_score":0.19845325,"about_ca_system_score_codex":0.0000057497764,"about_ca_system_score_gemma":0.000046051286,"threshold_uncertainty_score":0.982714},"labels":[],"label_agreement":null},{"id":"W2096034816","doi":"10.1029/2003jb002619","title":"Continuous GPS measurements of postglacial adjustment in Fennoscandia: 2. Modeling results","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":268,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Geology; Geodesy; Global Positioning System; Deglaciation; Glacial period; Mantle (geology); Geophysics; Geomorphology; Computer science","score_opus":0.05618779735429352,"score_gpt":0.30508349167453214,"score_spread":0.24889569432023861,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096034816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962984,0.00058668817,0.000057353187,0.0002470133,0.00039441546,0.00021766059,0.00004936043,0.0000050911995,0.002144026],"genre_scores_gemma":[0.99808246,0.00011351957,0.0011324034,0.00001794544,0.0005849606,0.0000010088404,0.000008939837,0.000006789437,0.000051969713],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9963336,0.00031443758,0.0008640735,0.00022598144,0.001674809,0.00058707123],"domain_scores_gemma":[0.9983221,0.00024029307,0.00029341463,0.0002074831,0.0006827014,0.00025398546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019625893,0.00016175337,0.0005496793,0.000058929785,0.00009455934,0.000067348774,0.0004710188,0.0000885158,0.00013523588],"category_scores_gemma":[0.0005263603,0.00012061438,0.00014972422,0.00043620766,0.0001390425,0.00032133888,0.000044693625,0.0004537658,0.0000568313],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.02659878,0.0042822417,0.09696046,0.00054212054,0.001007185,0.0012410899,0.0055930996,0.65430987,0.10450577,0.0024881219,0.0025638707,0.099907376],"study_design_scores_gemma":[0.028987497,0.016191272,0.7741949,0.00254554,0.0001923237,0.00007514826,0.0022876603,0.017542616,0.04447772,0.10998526,0.0020658385,0.0014542099],"about_ca_topic_score_codex":0.015663663,"about_ca_topic_score_gemma":0.0017935702,"teacher_disagreement_score":0.6772345,"about_ca_system_score_codex":0.000036059082,"about_ca_system_score_gemma":0.00043379152,"threshold_uncertainty_score":0.9908911},"labels":[],"label_agreement":null},{"id":"W2096615428","doi":"10.1002/2015jb012270","title":"Limitations on silicon in the outer core: Ultrasonic measurements at high temperatures and high d<i>K</i>/d<i>P</i> values of Fe‐Ni‐Si liquids at high pressures","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Hawai'i; National Science Foundation","keywords":"Materials science; Bulk modulus; Silicon; Isothermal process; Elastic modulus; Ultrasonic sensor; Analytical Chemistry (journal); Elasticity (physics); High pressure; Thermodynamics; Composite material; Metallurgy; Chemistry; Organic chemistry","score_opus":0.12297395898668054,"score_gpt":0.3227110052730766,"score_spread":0.19973704628639607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096615428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708605,0.00045478521,0.0000010225522,0.0010165214,0.00047786435,0.0003438874,0.00015189078,0.0000077309805,0.0004602766],"genre_scores_gemma":[0.99804693,0.00029776557,0.00011876954,0.00020327793,0.00066690025,0.0000043249556,0.00004097555,0.0000113704455,0.00060965255],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9950638,0.0009890392,0.000623963,0.00032424537,0.0023664536,0.00063249463],"domain_scores_gemma":[0.99675864,0.0015278757,0.00029670307,0.0003817199,0.0006798645,0.0003551753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027280299,0.00025238644,0.0006226815,0.00021788313,0.00028810074,0.00018693962,0.00061328907,0.00011569733,0.000110217836],"category_scores_gemma":[0.0007703064,0.00015386645,0.000118915654,0.00039245797,0.00040816766,0.0003535758,0.00009286802,0.00060839404,0.00009231778],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.022196222,0.0043530236,0.19223201,0.0008875881,0.0019368395,0.0011831053,0.020723196,0.029684093,0.57888687,0.010435996,0.12678048,0.01070055],"study_design_scores_gemma":[0.0023902194,0.0051507647,0.9392969,0.0002508637,0.00008651777,0.000040385738,0.00025564944,0.0002469655,0.037356734,0.011016212,0.0035712523,0.0003375309],"about_ca_topic_score_codex":0.0028295089,"about_ca_topic_score_gemma":0.0013405754,"teacher_disagreement_score":0.7470649,"about_ca_system_score_codex":0.000021631831,"about_ca_system_score_gemma":0.00021313001,"threshold_uncertainty_score":0.6274492},"labels":[],"label_agreement":null},{"id":"W2097037407","doi":"10.1046/j.1365-246x.2003.01857.x","title":"The equilibrium form of a rotating earth with an elastic shell","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; University of Toronto","funders":"","keywords":"Flattening; Hydrostatic equilibrium; Figure of the Earth; Inviscid flow; Mantle (geology); Perturbation (astronomy); Physics; Mechanics; Earth's rotation; Classical mechanics; Geology; Geophysics; Geodesy","score_opus":0.009348047503807888,"score_gpt":0.2195081398950922,"score_spread":0.21016009239128433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097037407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99324733,0.000027422973,0.00047534154,0.000115841234,0.0007489794,0.000059451166,0.00003348739,0.000008412246,0.005283755],"genre_scores_gemma":[0.9977047,0.000008671176,0.0014165306,0.000043072378,0.00044755137,7.0023754e-7,0.000014197043,0.000004114048,0.0003604715],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9988786,0.00008151329,0.0002469849,0.00012120739,0.00044386392,0.00022785999],"domain_scores_gemma":[0.99922705,0.00019927956,0.00019075713,0.00010628029,0.00016077509,0.00011583914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002840805,0.0001018396,0.00013246648,0.000029631809,0.000167295,0.00020481768,0.00030413782,0.000022904076,0.00060510606],"category_scores_gemma":[0.00005813116,0.000056999426,0.00005962824,0.00007644738,0.00008887294,0.00037392435,0.000010135641,0.00014990235,0.000067446716],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0055983397,0.0018009197,0.19759256,0.00016981897,0.003080618,0.00060055987,0.006973281,0.063617826,0.099877626,0.30797464,0.0022760388,0.3104378],"study_design_scores_gemma":[0.0041059637,0.005397049,0.6386071,0.00028667325,0.00020743987,0.001023801,0.0010376015,0.06185838,0.026215557,0.20110793,0.058851182,0.0013013459],"about_ca_topic_score_codex":0.000120973906,"about_ca_topic_score_gemma":0.00011534596,"teacher_disagreement_score":0.44101453,"about_ca_system_score_codex":0.000001902032,"about_ca_system_score_gemma":0.000070007314,"threshold_uncertainty_score":0.6625487},"labels":[],"label_agreement":null},{"id":"W2097135359","doi":"10.1111/j.1365-246x.2012.05549.x","title":"Time-dependent convection models of mantle thermal structure constrained by seismic tomography and geodynamics: implications for mantle plume dynamics and CMB heat flux","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Mantle convection; Geophysics; Mantle (geology); Geodynamics; Seismic tomography; Geology; Convection; Mechanics; Physics; Lithosphere; Tectonics; Seismology","score_opus":0.005634812453795363,"score_gpt":0.20815554879923298,"score_spread":0.20252073634543763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097135359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98714805,0.00013731373,0.0075993207,0.00047386056,0.0004714999,0.00016001031,0.0035975552,0.000011630585,0.0004007772],"genre_scores_gemma":[0.99824977,0.000037370693,0.00051711686,0.000067990586,0.00036417952,0.0000015432901,0.00055602985,0.0000064111377,0.00019960054],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991758,0.000034848043,0.00024261359,0.00015135923,0.0001709784,0.0002244346],"domain_scores_gemma":[0.9994516,0.000092787304,0.00012563776,0.00007442236,0.00011452548,0.00014104902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013225457,0.00013207339,0.0001922003,0.00006654866,0.00013858311,0.00008913663,0.00013679772,0.00006720592,0.00028638676],"category_scores_gemma":[0.00000699452,0.00010999832,0.00006620575,0.000044145403,0.00013653791,0.00041996947,0.00002292774,0.00011585753,0.0000060470866],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013694158,0.00093248003,0.11480005,0.00030842185,0.0026523108,0.000008498762,0.0021921508,0.07269306,0.604628,0.053406607,0.0050223526,0.14198661],"study_design_scores_gemma":[0.0015246919,0.0002470985,0.18308485,0.00004275161,0.00015713782,0.00025765266,0.00015657354,0.76458895,0.002399696,0.04634652,0.00074973365,0.00044437216],"about_ca_topic_score_codex":0.00018400529,"about_ca_topic_score_gemma":0.000023789626,"teacher_disagreement_score":0.69189584,"about_ca_system_score_codex":0.000007962336,"about_ca_system_score_gemma":0.000020153824,"threshold_uncertainty_score":0.44856012},"labels":[],"label_agreement":null},{"id":"W2098297614","doi":"10.1111/j.1365-246x.2004.02464.x","title":"Seismic singularities at upper-mantle phase transitions: a site percolation model","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Classification of discontinuities; Singularity; Geology; Gravitational singularity; Phase transition; Exponent; Transition zone; Mantle (geology); Discontinuity (linguistics); Seismic wave; Geophysics; Statistical physics; Physics; Geometry; Mathematics; Mathematical analysis; Condensed matter physics","score_opus":0.012548283808612577,"score_gpt":0.24421640288178004,"score_spread":0.23166811907316745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098297614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9805413,0.000039877974,0.014565376,0.0018926732,0.0008765956,0.000085682535,0.0005054468,0.00003318584,0.0014598828],"genre_scores_gemma":[0.99582535,0.000033490025,0.0015540163,0.00038258903,0.0011243694,0.0000015714962,0.00037815576,0.0000065418217,0.0006938875],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987597,0.00003570457,0.00028624057,0.00019570104,0.00047012657,0.00025254767],"domain_scores_gemma":[0.9994816,0.0000338011,0.00010865171,0.00009516421,0.00013376295,0.00014699719],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013130423,0.00015012336,0.0001719271,0.00009145467,0.00034681466,0.00024808958,0.00021286565,0.00005845705,0.0014229126],"category_scores_gemma":[0.000015873922,0.00013039506,0.00015475824,0.00007252677,0.00006805641,0.00061260647,0.000017374763,0.00018312005,0.00063205644],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044927647,0.00058330945,0.0016854116,0.000023198594,0.0002190491,0.00010112117,0.0026165203,0.93444675,0.043684836,0.007050423,0.001321591,0.00781849],"study_design_scores_gemma":[0.005204474,0.0004867629,0.03530627,0.00015368103,0.000128547,0.0005557352,0.00016562102,0.7765255,0.0048154467,0.1668823,0.00902236,0.00075327593],"about_ca_topic_score_codex":0.00034169375,"about_ca_topic_score_gemma":0.00011329797,"teacher_disagreement_score":0.15983188,"about_ca_system_score_codex":0.00003564484,"about_ca_system_score_gemma":0.00008386629,"threshold_uncertainty_score":0.9994899},"labels":[],"label_agreement":null},{"id":"W2099585999","doi":"10.1111/j.1365-246x.2012.05413.x","title":"Tomography of core-mantle boundary and lowermost mantle coupled by geodynamics","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geodynamics; Seismic tomography; Geology; Mantle (geology); Core–mantle boundary; Geophysics; Mantle convection; Tomography; Seismic anisotropy; Lithosphere; Seismology; Tectonics; Physics","score_opus":0.007437444273956139,"score_gpt":0.22039677304471997,"score_spread":0.21295932877076382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099585999","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99507904,0.00040922206,0.00031620375,0.00020620764,0.0017703808,0.00005589113,0.00042403772,0.000010222118,0.0017287695],"genre_scores_gemma":[0.99817044,0.00014651004,0.00028023333,0.000114294555,0.0008866967,4.9525846e-7,0.00016777604,0.0000049017453,0.00022865429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891204,0.00002834666,0.00027066207,0.00012246959,0.00039224574,0.00027426172],"domain_scores_gemma":[0.9993505,0.00008845589,0.00018246048,0.00008603224,0.000099357014,0.00019320389],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021264373,0.00012730695,0.00020264869,0.00006485641,0.00012124845,0.000109514775,0.00022986873,0.00005009924,0.0013576125],"category_scores_gemma":[0.00001720393,0.0001026526,0.00008934632,0.000078544275,0.0001406848,0.0003983146,0.00003178928,0.00015514252,0.000080984995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010226358,0.001461485,0.7609063,0.00014267955,0.0015235819,0.00008882858,0.0015385319,0.0005555785,0.12480167,0.0141727505,0.04132814,0.052457828],"study_design_scores_gemma":[0.0009704308,0.0002773286,0.92991656,0.00006123664,0.000083873776,0.00017689694,0.000100756915,0.008258839,0.0014155156,0.010835851,0.047465954,0.00043678237],"about_ca_topic_score_codex":0.0004060238,"about_ca_topic_score_gemma":0.000024000336,"teacher_disagreement_score":0.16901025,"about_ca_system_score_codex":0.0000038877974,"about_ca_system_score_gemma":0.000024007131,"threshold_uncertainty_score":0.9995553},"labels":[],"label_agreement":null},{"id":"W2100271147","doi":"10.1029/2008gl035342","title":"Plumes anchored by a high viscosity lower mantle in a 3D mantle convection model featuring dynamically evolving plates","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle (geology); Geology; Mantle convection; Plate tectonics; Lithosphere; Intraplate earthquake; Geophysics; Mantle plume; Convection; Hotspot (geology); Plume; Mechanics; Seismology; Physics; Tectonics; Meteorology","score_opus":0.01834063965403833,"score_gpt":0.24661709777241883,"score_spread":0.2282764581183805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100271147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99768305,0.000069452675,0.00029814863,0.00083923317,0.000230461,0.00031672383,0.00014565114,0.00005595714,0.0003613391],"genre_scores_gemma":[0.9983222,0.000050025374,0.0005684355,0.00018794027,0.0002333302,0.000012248902,0.00016110057,0.000013175988,0.00045154267],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9971343,0.00022392019,0.0002658501,0.00057926454,0.0008387804,0.0009578438],"domain_scores_gemma":[0.9990372,0.00029308538,0.00005552204,0.00030480814,0.0000938378,0.0002155426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042513252,0.0002204423,0.00034979687,0.00016353022,0.0003933214,0.0001503395,0.0003819569,0.00010429362,0.00030519578],"category_scores_gemma":[0.00009753451,0.0001950342,0.00007296007,0.0004514497,0.00030177322,0.00047775524,0.00008599637,0.00054351083,0.00041906512],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011530673,0.00060237484,0.036257084,0.0002112357,0.00014564663,0.000794191,0.0013118156,0.03834259,0.8692587,0.00025446742,0.048958685,0.0027101524],"study_design_scores_gemma":[0.0013553082,0.00034022747,0.57140887,0.0001277075,0.00001576921,0.000012872659,0.000045349763,0.41645527,0.0072182766,0.0016744719,0.000608563,0.0007373315],"about_ca_topic_score_codex":0.014436195,"about_ca_topic_score_gemma":0.0006051162,"teacher_disagreement_score":0.8620404,"about_ca_system_score_codex":0.00003393657,"about_ca_system_score_gemma":0.00007168145,"threshold_uncertainty_score":0.99212676},"labels":[],"label_agreement":null},{"id":"W2100486566","doi":"10.1016/j.epsl.2010.03.017","title":"Joint seismic–geodynamic-mineral physical modelling of African geodynamics: A reconciliation of deep-mantle convection with surface geophysical constraints","year":2010,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":224,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Canada Research Chairs; Canadian Institute for Advanced Research; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Geodynamics; Mantle (geology); Mantle convection; Asthenosphere; Geophysics; Cape verde; Hotspot (geology); Core–mantle boundary; Seismic anisotropy; Upwelling; Craton; Seismic tomography; Plate tectonics; Ocean surface topography; Lithosphere; Seismology; Tectonics; Climatology","score_opus":0.007711911515575614,"score_gpt":0.17013001154217025,"score_spread":0.16241810002659463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100486566","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99656636,0.000009948566,0.0020430223,0.00017473657,0.00032047994,0.00018511272,0.00026074142,0.000018196173,0.0004213892],"genre_scores_gemma":[0.9969522,0.000005931436,0.0026615406,0.000090961636,0.00010604109,4.0719777e-7,0.00016682841,0.0000036673168,0.000012418462],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985445,0.000045537883,0.0002610574,0.00037517396,0.0004149119,0.00035881615],"domain_scores_gemma":[0.99924994,0.00010355513,0.00021421237,0.00021036297,0.000064751264,0.0001571819],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036866494,0.00017884324,0.00033551405,0.00009343603,0.00014491996,0.00005244453,0.00018461254,0.00004735329,0.00013096152],"category_scores_gemma":[0.000012831916,0.0001405786,0.000041039257,0.00026260404,0.0011963084,0.00041157773,0.0000138548285,0.00020235272,0.000014486651],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016988374,0.000045178997,0.042461585,0.000081348495,0.00003675076,0.000013326277,0.0010564274,0.578061,0.37278476,0.00019776697,0.000013076106,0.0050788955],"study_design_scores_gemma":[0.00027522672,0.00021289659,0.18530492,0.000017734938,0.000024591141,0.00002317198,0.00007438261,0.81052387,0.0031815944,0.0001274976,0.00004446364,0.00018963027],"about_ca_topic_score_codex":0.0046356386,"about_ca_topic_score_gemma":0.001068828,"teacher_disagreement_score":0.3696032,"about_ca_system_score_codex":0.0000016594386,"about_ca_system_score_gemma":0.00007023382,"threshold_uncertainty_score":0.700773},"labels":[],"label_agreement":null},{"id":"W2100488177","doi":"10.1029/2006jb004850","title":"On the origin and significance of subadiabatic temperature gradients in the mantle","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Advection; Internal heating; Mantle (geology); Geology; Convection; Mechanics; Mantle convection; Energy balance; Geothermal gradient; Geophysics; Temperature gradient; Internal energy; Thermodynamics; Physics; Meteorology; Subduction","score_opus":0.028404235653963637,"score_gpt":0.29591157892059433,"score_spread":0.26750734326663067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100488177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976227,0.0002678576,0.0000027152334,0.00059477147,0.00011440152,0.00018005162,0.000009396521,0.0000012605386,0.001206846],"genre_scores_gemma":[0.9994242,0.00007380401,0.00006364134,0.000093122086,0.00022957778,7.150827e-7,0.0000011301381,0.0000028049967,0.00011101378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980032,0.00038545486,0.00029350753,0.00011232274,0.00086409564,0.00034143304],"domain_scores_gemma":[0.9965061,0.0029579657,0.00012639086,0.00017214776,0.00014342397,0.00009395616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030641002,0.00009017685,0.00021350392,0.0000210226,0.000108546046,0.000082366736,0.00045656494,0.000041377752,0.00040251628],"category_scores_gemma":[0.00038860863,0.000040314775,0.00005668749,0.00039393455,0.00025837292,0.00011123859,0.000015237204,0.00048763465,0.000025041869],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008923417,0.002959026,0.38332534,0.000899545,0.0007103773,0.0022862377,0.014445647,0.0029774976,0.16134715,0.23266412,0.09423295,0.09522868],"study_design_scores_gemma":[0.00037275106,0.0011565628,0.950814,0.0001160084,0.000010637973,0.000009529985,0.0008581403,0.00013970076,0.003392977,0.04033479,0.0027019065,0.000092983966],"about_ca_topic_score_codex":0.0016329393,"about_ca_topic_score_gemma":0.00066512235,"teacher_disagreement_score":0.5674887,"about_ca_system_score_codex":0.0000046307273,"about_ca_system_score_gemma":0.00007094776,"threshold_uncertainty_score":0.44072708},"labels":[],"label_agreement":null},{"id":"W2100600821","doi":"10.1016/j.epsl.2014.01.009","title":"Variation of thermal conductivity and heat flux at the Earth's core mantle boundary","year":2014,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Engineering and Physical Sciences Research Council; Office of Science; Natural Environment Research Council; European Commission; Sight Research UK","keywords":"Geophysics; Mantle (geology); Mantle convection; Thermal conductivity; Geology; Convection; Earth's internal heat budget; Post-perovskite; Core–mantle boundary; Thermal conduction; Heat flux; Anisotropy; Lithosphere; Plate tectonics; Petrology; Heat transfer; Tectonics; Thermodynamics; Physics","score_opus":0.009814760987111726,"score_gpt":0.18299469338748545,"score_spread":0.17317993240037372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100600821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99714065,0.00019487215,0.000025500487,0.00092204247,0.00041760982,0.00013643956,0.00013711861,0.000012849422,0.0010129205],"genre_scores_gemma":[0.99845725,0.000018036879,0.00020470042,0.00096007984,0.00013120599,3.6323203e-7,0.000104904124,0.0000018625573,0.0001215787],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988888,0.00008803936,0.00014531585,0.0002890292,0.00030096906,0.0002878352],"domain_scores_gemma":[0.99942476,0.00018432464,0.000062196654,0.00019964621,0.000015307562,0.000113766706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007794999,0.0001229558,0.00016778179,0.000049749895,0.00051456504,0.00011580969,0.00017324973,0.000033145665,0.00074775703],"category_scores_gemma":[0.000022463268,0.000079709,0.000018591552,0.00012809517,0.0008881538,0.00037110777,0.00003187959,0.00008390791,0.00005816725],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014587592,0.000013485227,0.34061548,0.00007300679,0.000031176565,0.000012050332,0.0012614483,0.006275473,0.63422203,0.00023321898,0.0007425521,0.016374182],"study_design_scores_gemma":[0.00016443818,0.00009376948,0.9845717,0.000007839149,0.000012744097,0.000023327744,0.000013371022,0.004677626,0.0021818364,0.000089540925,0.008045379,0.00011845288],"about_ca_topic_score_codex":0.0025193947,"about_ca_topic_score_gemma":0.0007183853,"teacher_disagreement_score":0.6439562,"about_ca_system_score_codex":6.971524e-7,"about_ca_system_score_gemma":0.000026915563,"threshold_uncertainty_score":0.81874156},"labels":[],"label_agreement":null},{"id":"W2101194783","doi":"10.1111/j.1365-246x.2009.04133.x","title":"Joint seismic, geodynamic and mineral physical constraints on three-dimensional mantle heterogeneity: Implications for the relative importance of thermal versus compositional heterogeneity","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":224,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Mantle (geology); Geology; Geophysics; Mantle convection; Core–mantle boundary; Scaling; Geodynamics; Thermal; Shear (geology); Tectonics; Seismology; Physics; Petrology; Lithosphere; Geometry; Thermodynamics","score_opus":0.027055599969767242,"score_gpt":0.2730007752795438,"score_spread":0.24594517530977655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101194783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99258816,0.000049640064,0.001573996,0.0035046055,0.0006083685,0.0002155934,0.001101762,0.000011332189,0.00034656914],"genre_scores_gemma":[0.9979115,0.0000071119543,0.0006110013,0.00040027135,0.0008419573,0.0000041905187,0.00020402638,0.000005063653,0.000014894137],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987565,0.00005277237,0.0003332097,0.00025763785,0.00035434676,0.00024552047],"domain_scores_gemma":[0.99879783,0.00046868244,0.00027226115,0.00015172988,0.00019091339,0.00011856911],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017954022,0.00018726343,0.00025665996,0.000047876478,0.00029759368,0.00008609359,0.00026839442,0.000049841336,0.00013470203],"category_scores_gemma":[0.00003059443,0.00012763737,0.0002167116,0.000055670964,0.00026336283,0.00021961475,0.0000251952,0.00021006408,0.000019299621],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008789912,0.0028167092,0.057918448,0.0000556974,0.004305635,0.00007752418,0.00055818976,0.12937234,0.4035224,0.20615034,0.0034560037,0.18297681],"study_design_scores_gemma":[0.0012039021,0.00068106654,0.9317645,0.000025246627,0.00007085252,0.000059574682,0.0000053754416,0.03964193,0.001485579,0.02473571,0.00014771016,0.00017853976],"about_ca_topic_score_codex":0.000045358345,"about_ca_topic_score_gemma":0.000058613612,"teacher_disagreement_score":0.87384605,"about_ca_system_score_codex":0.000013588933,"about_ca_system_score_gemma":0.00005224799,"threshold_uncertainty_score":0.5204901},"labels":[],"label_agreement":null},{"id":"W2101428021","doi":"10.1029/2011jb008431","title":"Small‐scale convection at a continental back‐arc to craton transition: Application to the southern Canadian Cordillera","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Netherlands Research Centre for Integrated Solid Earth Sciences; IFP Energies Nouvelles; University of Toronto; Natural Sciences and Engineering Research Council of Canada; Vrije Universiteit Amsterdam","keywords":"Craton; Lithosphere; Geology; Mantle (geology); Mantle convection; Transition zone; Geophysics; Mantle wedge; Petrology; Seismology; Tectonics","score_opus":0.031227978444540557,"score_gpt":0.24830413715664157,"score_spread":0.217076158712101,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101428021","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99103874,0.000048675178,0.00035716133,0.0025212849,0.00027484118,0.0004914322,0.00012360599,0.000007636449,0.005136595],"genre_scores_gemma":[0.99731547,0.000011111898,0.00061205623,0.00038493678,0.0008137927,0.00000731994,0.000013976368,0.000008927877,0.0008324347],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9979842,0.00026807486,0.00033210692,0.00022708521,0.00065136445,0.0005371975],"domain_scores_gemma":[0.99827766,0.00015042591,0.00009580267,0.00024033063,0.00045415107,0.00078161067],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00074889394,0.00014018524,0.000261578,0.000036595382,0.00041031008,0.00012123764,0.00047837268,0.0000657902,0.0048500677],"category_scores_gemma":[0.00005748106,0.000091760456,0.0001149586,0.000421087,0.000104457,0.00013038289,0.000031177693,0.0002860916,0.0036589166],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.018112168,0.0018703744,0.08648359,0.00040415104,0.0014313537,0.0006008416,0.08197557,0.0069742906,0.20946488,0.0018241713,0.18983662,0.401022],"study_design_scores_gemma":[0.0012965791,0.0043088407,0.8113011,0.00016963492,0.00008479694,0.00007016794,0.0038167161,0.0021302039,0.016501758,0.0031410132,0.15652965,0.0006495239],"about_ca_topic_score_codex":0.28579888,"about_ca_topic_score_gemma":0.4021436,"teacher_disagreement_score":0.7248175,"about_ca_system_score_codex":0.00003690858,"about_ca_system_score_gemma":0.0002049633,"threshold_uncertainty_score":0.99711686},"labels":[],"label_agreement":null},{"id":"W2101802987","doi":"10.1111/j.1365-246x.2008.03909.x","title":"Topography of Earth's inner core boundary from high-quality waveform doublets","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Inner core; Waveform; Mantle (geology); Geophysics; Core–mantle boundary; Geodesy; Seismology; Scale (ratio); Boundary (topology); Earth's rotation; Core (optical fiber); Physics; Cartography; Optics; Geography","score_opus":0.027112263479744048,"score_gpt":0.25124175700550233,"score_spread":0.22412949352575828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101802987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99245065,0.000060451337,0.00017370592,0.0003347374,0.0025667488,0.00006080147,0.00068047387,0.00001932668,0.0036531046],"genre_scores_gemma":[0.99609715,0.00007891462,0.0010428381,0.00022388704,0.0018901189,6.7798493e-7,0.00032457637,0.000005189137,0.00033666738],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819833,0.000061416606,0.000511833,0.00021693793,0.00075528986,0.000256196],"domain_scores_gemma":[0.9989562,0.0001394936,0.00031825644,0.00016860774,0.00024469369,0.00017272304],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019609118,0.00016614895,0.00032713916,0.00009940811,0.00021863938,0.000093818235,0.00044946466,0.00007368021,0.004580116],"category_scores_gemma":[0.000028702972,0.00012723384,0.00021257761,0.00013740786,0.00021453878,0.00042678378,0.000038999373,0.00025742353,0.0002613903],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003436672,0.0017049923,0.7037803,0.000082508166,0.0031238934,0.0012366271,0.0030672376,0.0035111506,0.13208908,0.04078304,0.016999569,0.09018493],"study_design_scores_gemma":[0.0006655812,0.00011348897,0.95208925,0.000023064413,0.000018049786,0.000048200272,0.000020571786,0.00014142362,0.0040661334,0.03066556,0.011960813,0.00018786098],"about_ca_topic_score_codex":0.004493716,"about_ca_topic_score_gemma":0.00015783733,"teacher_disagreement_score":0.24830894,"about_ca_system_score_codex":0.0000037880282,"about_ca_system_score_gemma":0.000086828695,"threshold_uncertainty_score":0.99632984},"labels":[],"label_agreement":null},{"id":"W2103568123","doi":"10.1017/s0885715614000487","title":"An empirical assessment of two-dimensional (2D) Debye–Scherrer-type image-plate X-ray diffraction data collapsed into a 1D diffractogram","year":2014,"lang":"en","type":"article","venue":"Powder Diffraction","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Sudbury","funders":"National Institute of Standards and Technology","keywords":"Materials science; Diffraction; Powder diffraction; Rietveld refinement; Intensity (physics); Crystallography; X-ray crystallography; Standard deviation; Analytical Chemistry (journal); Optics; Physics; Mathematics; Statistics","score_opus":0.027649550913481674,"score_gpt":0.3270289178972564,"score_spread":0.29937936698377476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103568123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99367267,0.000041596322,0.0026355518,0.00032393818,0.0020163464,0.00033558192,0.00012834123,0.000115176554,0.0007307944],"genre_scores_gemma":[0.9877378,0.000025924941,0.008694813,0.00024391075,0.0005738213,0.000004481087,0.0026189731,0.000019967703,0.00008035454],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9970659,0.00049315486,0.00056916976,0.000743919,0.0006943604,0.00043347143],"domain_scores_gemma":[0.99765104,0.00039105126,0.0004570567,0.0010175146,0.00021395256,0.00026938962],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009206437,0.00032305752,0.00049083005,0.00014477407,0.00030508556,0.00021588606,0.00048513198,0.00017764464,0.001850316],"category_scores_gemma":[0.00012402612,0.00027237047,0.000076576325,0.00031680998,0.00010884078,0.0014941703,0.000070712274,0.00030938844,0.00021416968],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006985032,0.001595233,0.28335357,0.00020953112,0.00034450414,0.000019924193,0.00046472586,0.018787328,0.62923187,0.00013930781,0.0055137468,0.05964177],"study_design_scores_gemma":[0.00084897346,0.0003570623,0.8182275,0.000025654901,0.00012417896,0.0000078933535,0.0000482402,0.16784558,0.0008239385,0.00091078173,0.010432851,0.00034728885],"about_ca_topic_score_codex":0.007630159,"about_ca_topic_score_gemma":0.0012606326,"teacher_disagreement_score":0.6284079,"about_ca_system_score_codex":0.000019843928,"about_ca_system_score_gemma":0.00013326532,"threshold_uncertainty_score":0.9999728},"labels":[],"label_agreement":null},{"id":"W2104426674","doi":"10.1111/j.1365-246x.2011.05011.x","title":"On the visibility of the inner-core shear wave phase PKJKP at long periods","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Seismogram; Inner core; Geology; Classification of discontinuities; Seismology; Amplitude; Attenuation; Shear (geology); Mantle (geology); Geophysics; Phase (matter); Seismic wave; Earth model; Geodesy; Physics; Optics; Mathematics; Mathematical analysis; Petrology","score_opus":0.045001307535784046,"score_gpt":0.25583051073413704,"score_spread":0.210829203198353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104426674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99201596,0.000012663098,0.000052835505,0.00054654485,0.0020213595,0.00010026323,0.00015813328,0.00000659577,0.005085626],"genre_scores_gemma":[0.998385,0.0000069420466,0.00006474035,0.00032853862,0.00068937795,9.5066724e-7,0.000014821591,0.0000037394964,0.00050589675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986668,0.00011607915,0.00030779574,0.0001667711,0.000544948,0.00019756058],"domain_scores_gemma":[0.9990866,0.00017293352,0.00022707823,0.00024506205,0.0001815386,0.000086754204],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00036149108,0.0001276847,0.00016145469,0.000028419958,0.00026151625,0.00006386964,0.00057327905,0.00004173436,0.0092155095],"category_scores_gemma":[0.00012827181,0.000061994964,0.00019059032,0.00009041008,0.00019137189,0.00014425672,0.000071866096,0.00025034708,0.00020949531],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.011503399,0.0075432877,0.39904726,0.00016760896,0.0034020427,0.0006449494,0.020738086,0.0039003557,0.0700943,0.2282483,0.072781496,0.18192892],"study_design_scores_gemma":[0.00064289576,0.0003417698,0.9443547,0.000048121536,0.000032702643,0.000049518683,0.00005161985,0.002092462,0.0095511405,0.040582996,0.0020893775,0.00016267798],"about_ca_topic_score_codex":0.00044287462,"about_ca_topic_score_gemma":0.000080291196,"teacher_disagreement_score":0.54530746,"about_ca_system_score_codex":0.000010726217,"about_ca_system_score_gemma":0.00004308857,"threshold_uncertainty_score":0.9916902},"labels":[],"label_agreement":null},{"id":"W2104975642","doi":"10.1016/s0040-1951(03)00177-x","title":"Microstructures, petrofabrics and seismic properties of ultra high-pressure eclogites from Sulu region, China: implications for rheology of subducted continental crust and origin of mantle reflections","year":2003,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Eclogite; Geology; Subduction; Mantle (geology); Coesite; Continental crust; Crust; Omphacite; Metamorphic rock; Geochemistry; Peridotite; Oceanic crust; Lithosphere; Shear zone; Petrology; Seismology; Tectonics","score_opus":0.017466759550607208,"score_gpt":0.2223430425483737,"score_spread":0.2048762829977665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104975642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99640226,0.0009766023,0.0004289195,0.00008367252,0.00016378863,0.0002849628,0.0015349269,0.000016504951,0.00010834731],"genre_scores_gemma":[0.9985101,0.00016655207,0.0010747844,0.000012798243,0.000046490204,0.0000046245946,0.00011867955,0.000006814542,0.000059138983],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991951,0.000054879947,0.00029516546,0.00022547627,0.00007261338,0.00015676768],"domain_scores_gemma":[0.99926496,0.00009826178,0.00026134844,0.00020976245,0.00012582715,0.00003981631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006762314,0.00013796898,0.0003772415,0.000049288246,0.00009862096,0.000015032405,0.00010787359,0.00007686947,0.000023123786],"category_scores_gemma":[0.00005396068,0.000112202135,0.0000406127,0.00013329447,0.0003127635,0.000089952686,0.000011278444,0.000059980226,3.919236e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089518435,0.000035553512,0.02451735,0.00016289925,0.00010264099,2.1224487e-7,0.00024969733,0.00031166102,0.9642643,0.009878288,0.000088495435,0.00029940766],"study_design_scores_gemma":[0.00073030515,0.00024273017,0.39206758,0.000036545625,0.00018421598,0.00000935562,0.000081412065,0.00019543219,0.5889825,0.016489416,0.0007838884,0.00019657599],"about_ca_topic_score_codex":0.006426045,"about_ca_topic_score_gemma":0.00023937844,"teacher_disagreement_score":0.37528175,"about_ca_system_score_codex":0.0000014345353,"about_ca_system_score_gemma":0.000053191427,"threshold_uncertainty_score":0.9714301},"labels":[],"label_agreement":null},{"id":"W2105476294","doi":"10.1016/j.lithos.2010.04.010","title":"The lithospheric root beneath Hudson Bay, Canada from Rayleigh wave dispersion: No clear seismological distinction between Archean and Proterozoic mantle","year":2010,"lang":"en","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Archean; Mantle (geology); Craton; Terrane; Proterozoic; Bay; Rayleigh wave; Geophysics; Seismology; Geothermal gradient; Surface wave; Tectonics; Geochemistry; Physics","score_opus":0.008070843901151191,"score_gpt":0.177973570079508,"score_spread":0.1699027261783568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105476294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966854,0.00008638133,0.000055643188,0.0005996334,0.0009507895,0.0002717021,0.00033027938,0.00002835824,0.0009918167],"genre_scores_gemma":[0.99755013,0.000014714899,0.00067599135,0.000077242046,0.00085732783,0.000004778407,0.00019255796,0.000005595104,0.000621676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998837,0.000103096594,0.00020304491,0.00031059553,0.00023325707,0.0003130101],"domain_scores_gemma":[0.9992379,0.00022497776,0.000082695144,0.0002529352,0.00002950413,0.00017199658],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002353327,0.00015627591,0.0001939201,0.0000063920097,0.00043624235,0.00015775587,0.00017819575,0.00009181985,0.0010209932],"category_scores_gemma":[0.000045776924,0.00009361372,0.000031361873,0.000059841135,0.00010301697,0.00008805579,0.000041076128,0.00023004515,0.0000612911],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013212906,0.000016322922,0.95270973,0.000023495773,0.000044666096,0.000034305664,0.00022251568,0.0000065922995,0.0004507467,0.00020290264,0.001142749,0.045013864],"study_design_scores_gemma":[0.00013277332,0.000109991655,0.87111944,0.000008046898,0.000020139556,0.0000032626388,0.00003659096,0.00045678447,0.00026582924,0.0009149167,0.12680103,0.00013118026],"about_ca_topic_score_codex":0.6636587,"about_ca_topic_score_gemma":0.44449615,"teacher_disagreement_score":0.2191625,"about_ca_system_score_codex":0.000003966867,"about_ca_system_score_gemma":0.00006109757,"threshold_uncertainty_score":0.99989223},"labels":[],"label_agreement":null},{"id":"W2105825831","doi":"10.1029/1999jb900377","title":"On scaling relations in time‐dependent mantle convection and the heat transfer constraint on layering","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Convection; Mechanics; Scaling; Mantle convection; Rayleigh number; Heat flux; Heat transfer; Convective heat transfer; Internal heating; Thermodynamics; Natural convection; Physics; Geology; Geometry; Mathematics","score_opus":0.017520762100011387,"score_gpt":0.26460805763544853,"score_spread":0.24708729553543715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105825831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936406,0.00009653739,0.000017003611,0.00087425177,0.00008378937,0.00016920625,0.0000125898305,0.0000048085676,0.0051012305],"genre_scores_gemma":[0.999008,0.00013485721,0.000034009827,0.00007266592,0.00020905689,0.000001254299,0.0000019397569,0.0000040436666,0.0005341434],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9981336,0.0004410577,0.00028776968,0.00014387984,0.00071036187,0.0002833391],"domain_scores_gemma":[0.99833536,0.0013241371,0.000019491323,0.00010769321,0.00006712197,0.0001462101],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013855267,0.00009699928,0.00024015566,0.000023068469,0.00020641144,0.0001499771,0.00017892192,0.00004996162,0.004290244],"category_scores_gemma":[0.00014421574,0.000057005094,0.000065151704,0.00016466677,0.00025329276,0.00014312759,0.000007808215,0.00050814124,0.0003661327],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.03489224,0.0017861295,0.01842978,0.00019952086,0.0007128715,0.0009861238,0.0060445135,0.43815815,0.029332522,0.04243867,0.0052278936,0.42179158],"study_design_scores_gemma":[0.018828934,0.0077594453,0.7257047,0.0016691105,0.00013060666,0.00018562151,0.0012321896,0.0825678,0.013031335,0.13843232,0.009378338,0.0010795825],"about_ca_topic_score_codex":0.0020258457,"about_ca_topic_score_gemma":0.00016825131,"teacher_disagreement_score":0.7072749,"about_ca_system_score_codex":0.000010597704,"about_ca_system_score_gemma":0.0000656951,"threshold_uncertainty_score":0.99661994},"labels":[],"label_agreement":null},{"id":"W2105834100","doi":"10.1063/1.1699489","title":"Static high-pressure structural studies on Dy to 119 GPa","year":2004,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Livermore National Laboratory; Ryerson University; U.S. Department of Energy","keywords":"Monoclinic crystal system; Dysprosium; Diamond anvil cell; Crystallography; Materials science; Diffraction; Phase (matter); Chemistry; Crystal structure; Inorganic chemistry; Physics","score_opus":0.015262446986390435,"score_gpt":0.24397378702803796,"score_spread":0.22871134004164753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105834100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99737984,0.00006172268,0.00008942417,0.00024144202,0.0012610347,0.0001525225,0.00012466703,0.000012011727,0.0006773564],"genre_scores_gemma":[0.9963481,0.000017155406,0.0019783678,0.0005530967,0.0010544664,7.446974e-7,0.000012661043,0.0000073443416,0.00002807383],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99872744,0.000021882319,0.00038289005,0.00015965379,0.00045627338,0.00025188472],"domain_scores_gemma":[0.9991374,0.00008714188,0.00032749074,0.00017499342,0.000118064694,0.00015490905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018827626,0.0001889094,0.00043082458,0.000049676317,0.00012397494,0.00007515035,0.00027501243,0.000038015423,0.00010542138],"category_scores_gemma":[0.000015026696,0.00013199337,0.000072813484,0.0001637663,0.000046298028,0.00014385297,0.000019779436,0.00017300532,0.00013536304],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002930106,0.000030768653,0.00012113929,0.000058036967,0.00023023182,0.000024073848,0.0017245419,0.97922707,0.0039539197,0.009901026,0.001324375,0.0031118016],"study_design_scores_gemma":[0.0050774347,0.003116961,0.056177124,0.0003241127,0.0007163922,0.000030698353,0.0019643167,0.0008767721,0.12902604,0.7887378,0.012538492,0.0014138558],"about_ca_topic_score_codex":0.00009825124,"about_ca_topic_score_gemma":0.000026117634,"teacher_disagreement_score":0.9783503,"about_ca_system_score_codex":0.000007852264,"about_ca_system_score_gemma":0.00006985009,"threshold_uncertainty_score":0.5382533},"labels":[],"label_agreement":null},{"id":"W2107055027","doi":"10.1007/s00269-009-0305-3","title":"Structural change in lead fluorapatite at high pressure","year":2009,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Chemistry; Fluorapatite; Apatite; Crystallography; Crystal structure; Synchrotron; Diamond anvil cell; Powder diffraction; High pressure; Analytical Chemistry (journal); Mineralogy; Thermodynamics; Optics","score_opus":0.013976869700688144,"score_gpt":0.21440133426555957,"score_spread":0.20042446456487142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107055027","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975294,0.0007135187,4.4927592e-7,0.00014076519,0.000059109523,0.00007565319,0.00022156494,0.00000879015,0.001250754],"genre_scores_gemma":[0.9988121,0.0000624688,0.00007636003,0.000058500413,0.0003189353,0.0000010214904,0.00016028507,0.0000022311858,0.0005081454],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999341,0.00001144713,0.00015927035,0.00018304997,0.00012698618,0.00017823007],"domain_scores_gemma":[0.9996868,0.000017795155,0.00008756381,0.00013294682,0.000022881522,0.00005205194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000049524664,0.00012464517,0.00023631191,0.000007971286,0.00003788365,0.000020021444,0.000102125,0.000050336344,0.00034845737],"category_scores_gemma":[0.0000036563201,0.000104934246,0.000030452346,0.00006462918,0.00004208262,0.000114851515,0.000012706505,0.000048088816,0.0000047782796],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007705493,0.00003481853,0.044450942,0.0002651439,0.000031699245,0.000007657884,0.0005319485,0.0005700337,0.9283789,0.00023849704,0.0005856349,0.024827678],"study_design_scores_gemma":[0.0009882714,0.00012183367,0.5997332,0.000097853386,0.000052893432,0.0000050828935,0.000016187094,0.003954765,0.38214055,0.009856651,0.0025230509,0.0005097165],"about_ca_topic_score_codex":0.0015957924,"about_ca_topic_score_gemma":0.000083566396,"teacher_disagreement_score":0.5552822,"about_ca_system_score_codex":0.0000010666914,"about_ca_system_score_gemma":0.000006246242,"threshold_uncertainty_score":0.42790946},"labels":[],"label_agreement":null},{"id":"W2107450543","doi":"10.1111/j.1365-246x.2006.03287.x","title":"Seismic anisotropy of the Slave craton, NW Canada, from joint interpretation of<i>SKS</i>and Rayleigh waves","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Anisotropy; Rayleigh wave; Craton; Seismology; Polarization (electrochemistry); Seismic anisotropy; Love wave; Azimuth; Lithosphere; Geophysics; Seismogram; Mantle (geology); Surface wave; Wave propagation; Longitudinal wave; Tectonics; Physics; Mechanical wave; Optics","score_opus":0.005764571347535668,"score_gpt":0.19442197772152922,"score_spread":0.18865740637399356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107450543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949073,0.00006564349,0.0017782924,0.000441158,0.0017123206,0.00005672736,0.0003088294,0.0000032427647,0.0007264625],"genre_scores_gemma":[0.99881524,0.00002066456,0.0003432145,0.0001847535,0.0005054353,1.7262902e-7,0.0000323132,0.0000032684686,0.000094949835],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987427,0.000058513357,0.00041987188,0.00012858331,0.00049298257,0.00015734637],"domain_scores_gemma":[0.9991255,0.00016453453,0.0003486617,0.00010242099,0.00017156257,0.000087318935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020690757,0.00010809676,0.00020743023,0.000039061626,0.00008032106,0.000046763813,0.00027500867,0.000036759175,0.00045362173],"category_scores_gemma":[0.00004694977,0.000071535775,0.000088917324,0.000068147994,0.0000978051,0.00015561441,0.000036190464,0.00015286254,0.0000068116515],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024109273,0.00053605746,0.28978214,0.0001454505,0.0025208213,0.00018209046,0.006134393,0.028172594,0.4648835,0.016086658,0.013339978,0.17580537],"study_design_scores_gemma":[0.0003306436,0.0000657909,0.9358958,0.00006595551,0.000035836412,0.000019800762,0.000097805336,0.007457722,0.04193415,0.012519793,0.0014634059,0.00011329318],"about_ca_topic_score_codex":0.15879896,"about_ca_topic_score_gemma":0.04135898,"teacher_disagreement_score":0.6461137,"about_ca_system_score_codex":0.000011106315,"about_ca_system_score_gemma":0.00014060458,"threshold_uncertainty_score":0.9761337},"labels":[],"label_agreement":null},{"id":"W2107933621","doi":"10.1139/cjp-2014-0616","title":"A first-principles study of bulk aluminum at high pressure","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Compressibility; Thermodynamics; Gibbs free energy; Physics; Phase transition; Ab initio; Volume (thermodynamics); Phase (matter); Zero temperature; Aluminium; Atmospheric temperature range; Range (aeronautics); Transition temperature; Energy density; Condensed matter physics; Materials science; Theoretical physics; Quantum mechanics","score_opus":0.014510643872195311,"score_gpt":0.1871577507483056,"score_spread":0.1726471068761103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107933621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976234,0.00013231297,0.000034918845,0.000079546604,0.00084484887,0.00010633365,0.00014892338,0.000003002077,0.0010267476],"genre_scores_gemma":[0.9988561,0.000004727314,0.0001044452,0.00003658536,0.0006494644,2.8138317e-7,0.000009651353,0.000005480213,0.00033321322],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9989901,0.00008001647,0.00032729402,0.00011651861,0.00023564207,0.00025041864],"domain_scores_gemma":[0.9988423,0.000082928054,0.00033423357,0.00021504305,0.00014908296,0.00037639643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027831225,0.0001208091,0.00032878463,0.00005845,0.00016114801,0.000044506556,0.00034246864,0.00004205108,0.000717383],"category_scores_gemma":[0.00004246173,0.00009937909,0.000067390276,0.000108290995,0.00006538254,0.00014353922,0.000010251009,0.00009439884,0.000039219358],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013070578,0.00019398391,0.37800452,0.00023856972,0.0006606532,0.00014082335,0.007761306,0.5926786,0.0004526213,0.0041543026,0.0095703835,0.006013536],"study_design_scores_gemma":[0.002197242,0.0026132276,0.78373426,0.00015907045,0.0004935191,0.000038676957,0.0005206498,0.0063478206,0.0026393307,0.008999763,0.19163506,0.00062136515],"about_ca_topic_score_codex":0.050099846,"about_ca_topic_score_gemma":0.15907788,"teacher_disagreement_score":0.5863308,"about_ca_system_score_codex":0.000005628529,"about_ca_system_score_gemma":0.00019602467,"threshold_uncertainty_score":0.95622563},"labels":[],"label_agreement":null},{"id":"W2107987930","doi":"10.1111/j.1365-246x.2009.04229.x","title":"Seismic structure of the southern Apennines as revealed by waveform modelling of regional surface waves","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Lamont-Doherty Earth Observatory, Columbia University; National Science Foundation","keywords":"Geology; Seismology; Subduction; Crust; Seismogram; Mantle (geology); Tectonics; Rayleigh wave; Shear (geology); Geophysics; Surface wave; Petrology","score_opus":0.011148716548951615,"score_gpt":0.20984144650111242,"score_spread":0.1986927299521608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107987930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968667,0.0000739131,0.0003942461,0.0011781391,0.0005170117,0.000063372776,0.00038793022,0.000005635943,0.0005130487],"genre_scores_gemma":[0.99812675,0.000031198768,0.00034559195,0.0002037966,0.00044470758,4.8354938e-8,0.00005221333,0.0000034434659,0.0007922669],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99868023,0.000055110184,0.00036998946,0.00013707286,0.0005849613,0.0001726319],"domain_scores_gemma":[0.9991736,0.00006412038,0.00037535123,0.0001264131,0.00018874205,0.0000717825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010848427,0.00013130515,0.00022623029,0.000028294879,0.000097376076,0.000049371927,0.0005109363,0.000056229706,0.0006598296],"category_scores_gemma":[0.000014709916,0.00007998832,0.0001567647,0.000090869355,0.00008459236,0.0001788658,0.000018270546,0.00019065238,0.00002575779],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006411915,0.00026159882,0.012936225,0.000041200816,0.00043408383,0.000011199348,0.0018684837,0.7105709,0.2536023,0.0034186647,0.006650619,0.009563555],"study_design_scores_gemma":[0.0025016055,0.0008530573,0.19295684,0.00049244217,0.00019884748,0.00035592288,0.000589284,0.290048,0.0688287,0.4322709,0.009905381,0.0009990141],"about_ca_topic_score_codex":0.0006584415,"about_ca_topic_score_gemma":0.000012405489,"teacher_disagreement_score":0.42885226,"about_ca_system_score_codex":0.00000462693,"about_ca_system_score_gemma":0.000056012097,"threshold_uncertainty_score":0.7224671},"labels":[],"label_agreement":null},{"id":"W2109160930","doi":"10.5194/se-5-447-2014","title":"Lithosphere and upper-mantle structure of the southern Baltic Sea estimated from modelling relative sea-level data with glacial isostatic adjustment","year":2014,"lang":"en","type":"article","venue":"Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Post-glacial rebound; Deglaciation; Lithosphere; Mantle (geology); Glacial period; Ice sheet; Baltic Shield; Isostasy; Last Glacial Maximum; Crust; Geophysics; Oceanography; Geomorphology; Seismology; Tectonics","score_opus":0.023706876759279134,"score_gpt":0.22113443389002285,"score_spread":0.19742755713074372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109160930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98924446,0.00022755611,0.002347997,0.000058164045,0.00019461244,0.00020938426,0.007466207,0.000016858408,0.00023476146],"genre_scores_gemma":[0.99261963,0.000014889922,0.006506109,0.000049177215,0.00011141426,3.2229408e-7,0.00058601587,0.0000074198097,0.0001050284],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99896634,0.00011265319,0.00017618193,0.00029366853,0.00023704753,0.00021409003],"domain_scores_gemma":[0.9992024,0.00010387526,0.00013239194,0.00044740055,0.000038020604,0.00007597076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010243494,0.00015538382,0.00025014463,0.000011574805,0.00014089957,0.000050298353,0.00027752318,0.000056942758,0.00063454936],"category_scores_gemma":[0.000019250256,0.00009036572,0.000019704683,0.00008312992,0.00010877489,0.000174645,0.000055622444,0.00010524646,0.000035922545],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060319767,0.000075937336,0.48994794,0.00032982166,0.0006067092,0.000009609928,0.013162756,0.47009605,0.0025480199,0.000775557,0.00040427278,0.021440128],"study_design_scores_gemma":[0.0006803977,0.00015529754,0.3110947,0.00019002343,0.00016455448,0.0000032916855,0.00031854602,0.679178,0.0013461797,0.006283459,0.00030709014,0.00027844706],"about_ca_topic_score_codex":0.00825691,"about_ca_topic_score_gemma":0.0044884775,"teacher_disagreement_score":0.20908196,"about_ca_system_score_codex":9.836742e-7,"about_ca_system_score_gemma":0.000053558822,"threshold_uncertainty_score":0.99834716},"labels":[],"label_agreement":null},{"id":"W2110246618","doi":"10.1029/2012gl054328","title":"Seismic anisotropy of subducting oceanic uppermost mantle from fossil spreading","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Subduction; Mantle (geology); Seismic anisotropy; Anisotropy; Slab; Seismology; Geophysics; Receiver function; Shear wave splitting; Mantle wedge; Lithosphere; Tectonics","score_opus":0.037958787889965845,"score_gpt":0.285744309520322,"score_spread":0.24778552163035614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110246618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971417,0.00020549171,0.00012537585,0.000517298,0.00055854896,0.00017776067,0.00019498022,0.00003290437,0.0010458936],"genre_scores_gemma":[0.99766135,0.00001920232,0.0004888755,0.00012371683,0.0014933792,0.0000022788047,0.00009408381,0.000010461866,0.000106649284],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9972098,0.00031347823,0.00027024286,0.0003320752,0.0008141974,0.0010602007],"domain_scores_gemma":[0.9985152,0.00065850606,0.000086500004,0.0003753321,0.00007188445,0.00029257528],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067857193,0.00017293486,0.0003225361,0.000098995246,0.00026141325,0.00009563581,0.00043973405,0.00006524663,0.0009104452],"category_scores_gemma":[0.00013118469,0.0001459267,0.000105016734,0.0003395315,0.0002549274,0.000453018,0.000085511856,0.00033021707,0.0013410999],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017380998,0.00014851126,0.09593312,0.00009983283,0.00012680845,0.000024411162,0.0012883699,0.00035139357,0.8827546,0.0011996238,0.010826997,0.0070725116],"study_design_scores_gemma":[0.00057111843,0.0001918811,0.90388256,0.000097779506,0.00004247167,0.000003838867,0.00039462213,0.003902024,0.0776293,0.0030528305,0.009734311,0.0004972854],"about_ca_topic_score_codex":0.011133213,"about_ca_topic_score_gemma":0.000028734808,"teacher_disagreement_score":0.8079494,"about_ca_system_score_codex":0.0000104731225,"about_ca_system_score_gemma":0.000040010316,"threshold_uncertainty_score":0.9994365},"labels":[],"label_agreement":null},{"id":"W2111169774","doi":"10.1029/1999jb900378","title":"Crustal structure of NW British Columbia and SE Alaska from seismic wide‐angle studies: Coast Plutonic Complex to Stikinia","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Crust; Seismology; Tectonics; Continental crust; Fibrous joint; Mantle (geology); Seismic refraction; Accretionary wedge; Subduction; Paleontology","score_opus":0.03120696549639647,"score_gpt":0.2946911557177235,"score_spread":0.263484190221327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111169774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971279,0.0010390771,0.0000051466563,0.00020059093,0.0001833563,0.00023109798,0.0010093963,0.000009065482,0.00019439313],"genre_scores_gemma":[0.99686587,0.00046046913,0.0010729741,0.00012459666,0.00054607017,7.3510483e-7,0.000026558091,0.000011458866,0.00089126494],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9970608,0.00033893346,0.00058309035,0.00031481078,0.0011280526,0.0005743382],"domain_scores_gemma":[0.99760383,0.0009821188,0.00019074797,0.00023182073,0.0005303384,0.0004611147],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040795043,0.00016473864,0.0007322896,0.000016333295,0.00027226875,0.00042167495,0.00047359508,0.00008792404,0.009275532],"category_scores_gemma":[0.00029313136,0.00016653605,0.000119444136,0.000360576,0.00042219952,0.00031451668,0.00008743838,0.00043611566,0.00006588637],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033897497,0.0008439541,0.14811543,0.0005947348,0.0024787416,0.0014855843,0.0066683968,0.013527076,0.060214452,0.000035685327,0.3299748,0.4326714],"study_design_scores_gemma":[0.0010167009,0.0017089235,0.96134615,0.00029028428,0.00005723451,0.0000319091,0.0008958875,0.00061284157,0.00044039654,0.009964679,0.02337795,0.000257062],"about_ca_topic_score_codex":0.13271727,"about_ca_topic_score_gemma":0.0849535,"teacher_disagreement_score":0.8132307,"about_ca_system_score_codex":0.000014605661,"about_ca_system_score_gemma":0.00021738665,"threshold_uncertainty_score":0.99163014},"labels":[],"label_agreement":null},{"id":"W2111443216","doi":"10.1016/s0010-8545(99)00150-2","title":"Pressure-tuning spectroscopy of inorganic compounds: a summary of the past 15 years","year":2000,"lang":"en","type":"article","venue":"Coordination Chemistry Reviews","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Chemistry; Intramolecular force; Diamond anvil cell; Raman spectroscopy; Spectroscopy; Metal; Chemical physics; Infrared spectroscopy; Nanotechnology; High pressure; Computational chemistry; Stereochemistry; Organic chemistry; Optics; Engineering physics","score_opus":0.01227152420585085,"score_gpt":0.22403016809084805,"score_spread":0.2117586438849972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111443216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96979374,0.008590677,0.000011733781,0.00013892223,0.0001908241,0.0003240429,0.00014261251,0.000015908692,0.020791527],"genre_scores_gemma":[0.996245,0.0008501822,0.00014134252,0.000028197415,0.00013035152,0.0000017815149,0.00006674041,0.0000032462744,0.0025331185],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99917257,0.000071689814,0.0003461268,0.00013972806,0.00015572424,0.00011417935],"domain_scores_gemma":[0.9993707,0.00003524719,0.00024733285,0.0002744937,0.0000385337,0.00003367529],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026485237,0.000094503914,0.00028507097,0.000008764376,0.000044838212,0.000017790642,0.00029508176,0.00004444533,0.0057828454],"category_scores_gemma":[0.00003048491,0.000068060945,0.000081933,0.0001903176,0.00007131661,0.000074813586,0.000014644163,0.0000659806,0.00003602237],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032246622,0.00006328822,0.032593086,0.0013464928,0.00005394794,9.3058026e-7,0.00022162066,0.00023182541,0.9181572,0.00002032408,0.02767016,0.019608859],"study_design_scores_gemma":[0.0003619725,0.000033803575,0.07099701,0.00041219767,0.00012158021,0.000005234134,0.00001857615,0.0003372929,0.18821287,0.00028384876,0.7389814,0.00023417293],"about_ca_topic_score_codex":0.00010738533,"about_ca_topic_score_gemma":0.000008952586,"teacher_disagreement_score":0.72994435,"about_ca_system_score_codex":0.000001981335,"about_ca_system_score_gemma":0.00002718504,"threshold_uncertainty_score":0.995126},"labels":[],"label_agreement":null},{"id":"W2111936551","doi":"10.5539/jmsr.v4n2p1","title":"Modulation of Anisotropy on Phonon Transportation in MgS: Theoretical Studies","year":2014,"lang":"en","type":"article","venue":"Journal of Materials Science Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Education Department of Henan Province; National Natural Science Foundation of China","keywords":"Slowness; Anisotropy; Phonon; Condensed matter physics; Group velocity; Transverse plane; Lattice (music); Materials science; Physics; Optics; Quantum mechanics; Acoustics","score_opus":0.0509966256409234,"score_gpt":0.35766523969178327,"score_spread":0.3066686140508599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111936551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998848,0.000034485558,0.000047459485,0.00018113814,0.000523151,0.00009257024,0.000018465025,0.000002087653,0.00025263245],"genre_scores_gemma":[0.9992056,0.00011857415,0.00048602594,0.000009848612,0.00017030197,4.3579468e-7,0.0000025594893,0.0000019316842,0.0000047242684],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99763256,0.00037903825,0.000489675,0.00014184296,0.0010755517,0.00028133794],"domain_scores_gemma":[0.9988222,0.00032227323,0.00019945209,0.00012035504,0.00045745404,0.000078274046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009451196,0.00006794791,0.00028182537,0.00036892612,0.0001038882,0.00008087132,0.00033690647,0.000034780358,0.00037742584],"category_scores_gemma":[0.00050294626,0.000044955712,0.000025962756,0.0004176227,0.00071258924,0.00035613,0.00000802546,0.00009353176,0.000022307211],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041597843,0.000050469902,0.0028562474,0.00006753146,0.000007312598,0.0000074243667,0.0007477092,0.0049453103,0.96754056,0.020582994,0.000037615497,0.0027408476],"study_design_scores_gemma":[0.00044127385,0.0011819634,0.389205,0.00018086226,0.000005531497,0.0000035082633,0.0002898716,0.00067381386,0.5592783,0.04858241,0.000071879214,0.000085550855],"about_ca_topic_score_codex":0.0001610442,"about_ca_topic_score_gemma":0.000036115678,"teacher_disagreement_score":0.40826222,"about_ca_system_score_codex":0.000011510994,"about_ca_system_score_gemma":0.0001221034,"threshold_uncertainty_score":0.41325483},"labels":[],"label_agreement":null},{"id":"W2112665602","doi":"10.1002/2014jb011321","title":"Crustal anisotropy in a subduction zone forearc: Northern Cascadia","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Anisotropy; Terrane; Subduction; Seismology; Schist; Seismometer; Tectonics; Paleontology; Metamorphic rock","score_opus":0.024728495141485674,"score_gpt":0.2976169257470217,"score_spread":0.272888430605536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112665602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977696,0.000059170143,0.00018360981,0.00032517253,0.0003568738,0.0001404134,0.000031020136,0.000008422065,0.0011257327],"genre_scores_gemma":[0.9975995,0.000070040434,0.00038108905,0.000028826225,0.0015881502,9.1240605e-7,0.000015154463,0.000008259725,0.00030811265],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9969346,0.00053655636,0.00047069977,0.00022385195,0.0011353834,0.00069891516],"domain_scores_gemma":[0.9984249,0.000399843,0.00017551603,0.00022370493,0.00042205688,0.00035396207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019811126,0.0001506397,0.00045247553,0.00028870182,0.00016464561,0.00016260713,0.0003645413,0.00008708357,0.0003864219],"category_scores_gemma":[0.0003602844,0.00011272604,0.00014294645,0.0004762289,0.00019312481,0.0004526367,0.000035867084,0.00064541603,0.0003380725],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0072729746,0.0025030721,0.3443561,0.0005895746,0.0006230274,0.0020140833,0.005876766,0.034258634,0.124807216,0.014036689,0.008987145,0.45467472],"study_design_scores_gemma":[0.0014770828,0.0027082686,0.9430598,0.00011131519,0.000019568046,0.0000754263,0.0001832087,0.010698532,0.00347631,0.016144464,0.02173617,0.0003098515],"about_ca_topic_score_codex":0.007087179,"about_ca_topic_score_gemma":0.005917146,"teacher_disagreement_score":0.59870374,"about_ca_system_score_codex":0.000011038992,"about_ca_system_score_gemma":0.0001962129,"threshold_uncertainty_score":0.9995247},"labels":[],"label_agreement":null},{"id":"W2113158526","doi":"10.1002/2013gc005056","title":"Continental scale body wave tomography of India: Evidence for attrition and preservation of lithospheric roots","year":2014,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"Department of Science and Technology, Ministry of Science and Technology, India","keywords":"Geology; Lithosphere; Seismology; Indian Shield; Rift; Mantle (geology); Volcano; Volcanism; Seismic tomography; Geophysics; Paleontology; Proterozoic; Tectonics","score_opus":0.016362000436036157,"score_gpt":0.21892413721869472,"score_spread":0.20256213678265855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113158526","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975395,0.00050382526,0.00030755776,0.00002188655,0.00030766823,0.0003993667,0.0005148367,0.00001947122,0.00038588134],"genre_scores_gemma":[0.99879557,0.000029661102,0.0003421958,0.0000067963524,0.00031429442,0.000014486124,0.00038171656,0.0000057821576,0.00010949525],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987161,0.000054560674,0.00042698364,0.00030191606,0.00026150918,0.00023888629],"domain_scores_gemma":[0.99871784,0.00028944822,0.00041696377,0.00027891234,0.00021548202,0.00008134654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038278216,0.00016939295,0.00041175535,0.000024413592,0.00007585816,0.00003817357,0.00015285412,0.00010711674,0.000044463613],"category_scores_gemma":[0.00006874682,0.00016062502,0.00010544148,0.00018573347,0.00009437234,0.0002707224,0.000024862675,0.000053870113,0.0000028395443],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028694692,0.00012363124,0.31283185,0.005442052,0.00012564825,8.352735e-7,0.0003424571,0.00017518675,0.6758845,0.00028995686,0.00044908587,0.004047863],"study_design_scores_gemma":[0.0010166474,0.0004138501,0.71230006,0.000741753,0.0001331104,0.000006029702,0.0001301773,0.009224902,0.2707905,0.003896262,0.00094383355,0.00040289995],"about_ca_topic_score_codex":0.0019623851,"about_ca_topic_score_gemma":0.00004591728,"teacher_disagreement_score":0.405094,"about_ca_system_score_codex":0.000001974941,"about_ca_system_score_gemma":0.000026068401,"threshold_uncertainty_score":0.6550098},"labels":[],"label_agreement":null},{"id":"W2113567600","doi":"10.1016/j.epsl.2005.01.038","title":"Continental insulation, mantle cooling, and the surface area of oceans and continents","year":2005,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":143,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mantle (geology); Lithosphere; Geology; Mantle convection; Subduction; Geophysics; Mantle wedge; Hotspot (geology); Earth's internal heat budget; Plate tectonics; Internal heating; Mechanics; Seismology; Tectonics","score_opus":0.005798919662908191,"score_gpt":0.17418523987080967,"score_spread":0.16838632020790148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113567600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99654937,0.00080244424,0.000013705711,0.0019185276,0.0001415826,0.00015398032,0.00013648396,0.000009868644,0.00027405718],"genre_scores_gemma":[0.9984235,0.00019259403,0.00036738405,0.0008362811,0.00006754085,1.2792229e-7,0.000053984168,0.0000014203758,0.000057138455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910516,0.000044328783,0.00017666664,0.0002263196,0.00022014475,0.00022737349],"domain_scores_gemma":[0.99955434,0.00013257696,0.00008486665,0.00010567288,0.00001692604,0.00010561797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005080446,0.00010930835,0.00018071705,0.000040458515,0.00025832368,0.00011021334,0.00012630178,0.000023251347,0.00013330921],"category_scores_gemma":[0.000019483909,0.00007092253,0.000013095626,0.00010304336,0.00097395084,0.00032610618,0.0000200242,0.000063250714,0.000009825892],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024735858,0.00000863647,0.97689295,0.00002793019,0.000022471559,0.0000072073053,0.0010893862,0.0038505543,0.011960433,0.00016660852,0.00057367265,0.0051528173],"study_design_scores_gemma":[0.0007835853,0.000033904456,0.9771647,0.000013003397,0.000015278803,0.000026495609,0.000045279307,0.016201777,0.00041500694,0.000033390865,0.0051547643,0.000112813555],"about_ca_topic_score_codex":0.0017931886,"about_ca_topic_score_gemma":0.000335243,"teacher_disagreement_score":0.012351222,"about_ca_system_score_codex":3.5679778e-7,"about_ca_system_score_gemma":0.000013135786,"threshold_uncertainty_score":0.35885626},"labels":[],"label_agreement":null},{"id":"W2115074785","doi":"10.1209/0295-5075/78/37003","title":"Superconductivity in high-pressure SiH <sub>4</sub>","year":2007,"lang":"en","type":"article","venue":"Europhysics Letters (EPL)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Superconductivity; Monoclinic crystal system; Condensed matter physics; Phase (matter); Materials science; High pressure; Symmetry (geometry); Metal; Coupling (piping); Ambient pressure; Electron; Physics; Thermodynamics; Quantum mechanics; Molecule","score_opus":0.0074794792878525645,"score_gpt":0.18465516286649603,"score_spread":0.17717568357864347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115074785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960483,0.000088006636,0.00047337462,0.0005745422,0.0015345234,0.000237462,0.00015135226,0.00009298113,0.0007995027],"genre_scores_gemma":[0.9973305,0.000021815058,0.00024626523,0.0013326927,0.00089519046,0.0000014858146,0.00011513119,0.000021521357,0.000035382207],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99769896,0.00017585426,0.00036935508,0.0005763948,0.00042945694,0.0007499708],"domain_scores_gemma":[0.9989874,0.00019369957,0.000111584246,0.00049353426,0.000041504878,0.00017229181],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00051818276,0.00032444714,0.0004041591,0.00012953236,0.00015218976,0.00012379655,0.0004081711,0.0000907951,0.0001850248],"category_scores_gemma":[0.00003088772,0.00030610772,0.00010117476,0.00043826792,0.00014054345,0.0005588853,0.000049933493,0.0003306682,0.00079344766],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007590649,0.000071130824,0.012659832,0.000057434543,0.00004356888,0.00025693115,0.0003074142,0.0026995647,0.96992797,0.00062693976,0.0015088768,0.011764418],"study_design_scores_gemma":[0.0010152728,0.00013816412,0.6858424,0.00006004695,0.00007928564,0.000008964709,0.000044798213,0.00029635892,0.2950318,0.0023528095,0.014134082,0.0009960065],"about_ca_topic_score_codex":0.0018031363,"about_ca_topic_score_gemma":0.00038666706,"teacher_disagreement_score":0.6748962,"about_ca_system_score_codex":0.0000065335803,"about_ca_system_score_gemma":0.000028540237,"threshold_uncertainty_score":0.99998456},"labels":[],"label_agreement":null},{"id":"W2115614316","doi":"10.1016/j.pepi.2010.02.001","title":"On the interaction of the geotherm with a post-perovskite phase transition in the deep mantle","year":2010,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Classification of discontinuities; Latent heat; Geothermal gradient; Phase transition; Geology; Mantle (geology); Phase boundary; Geophysics; Petrology; Perovskite (structure); Thermodynamics; Phase (matter); Materials science; Condensed matter physics; Chemistry; Physics; Crystallography","score_opus":0.0059694962394431905,"score_gpt":0.1926185132639107,"score_spread":0.1866490170244675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115614316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973744,0.000021071604,0.000010106606,0.0010158814,0.00036858616,0.00027900565,0.00029391906,0.0000037091552,0.00063327997],"genre_scores_gemma":[0.9993249,0.000009831741,0.000014385582,0.00049674365,0.00008486761,0.0000015386744,0.000049203256,0.0000032129003,0.000015306425],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99924374,0.00014973342,0.00016285418,0.00012020142,0.00019025491,0.0001332272],"domain_scores_gemma":[0.9992789,0.00022907264,0.0001383694,0.00031118153,0.000021947122,0.000020534615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000213755,0.00012068728,0.0001440451,0.000016937083,0.00011528207,0.000034945006,0.0003510444,0.00003140957,0.00028316988],"category_scores_gemma":[0.000011115102,0.000045737812,0.000058940568,0.00010084098,0.0001770795,0.000108059736,0.000010891397,0.00023957939,0.000009677839],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.014254028,0.0019978802,0.11506853,0.0010088477,0.0011545875,0.00004786262,0.09889097,0.072136715,0.47722512,0.01437185,0.0013873703,0.20245624],"study_design_scores_gemma":[0.0024432156,0.002225237,0.90553063,0.0005473928,0.000262056,0.00010778657,0.0029026393,0.020528931,0.051426303,0.010059021,0.0033549163,0.00061187806],"about_ca_topic_score_codex":0.0027860275,"about_ca_topic_score_gemma":0.0056019006,"teacher_disagreement_score":0.7904621,"about_ca_system_score_codex":4.0822366e-7,"about_ca_system_score_gemma":0.000015504143,"threshold_uncertainty_score":0.42116588},"labels":[],"label_agreement":null},{"id":"W2116267660","doi":"10.1002/jgrb.50294","title":"Sea level variations during snowball Earth formation and evolution: 2. The influence of Earth's rotation","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Compute Canada","keywords":"Mantle (geology); Earth's rotation; Lithosphere; Snowball Earth; Geology; Convection; Geophysics; Mantle convection; Sea level; Geodesy; Mechanics; Physics; Oceanography; Tectonics; Paleontology; Glacial period","score_opus":0.029629635731009366,"score_gpt":0.28163811794983656,"score_spread":0.2520084822188272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116267660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835426,0.00007308844,0.00028732364,0.0005436384,0.00009687063,0.0002926203,0.000061968734,0.0000062519707,0.0002839751],"genre_scores_gemma":[0.9987784,0.0000971988,0.000531324,0.000020315789,0.00036251717,0.0000030784147,0.000010300821,0.0000040945683,0.00019279036],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99762505,0.00037389074,0.00049596373,0.00013678272,0.0009883189,0.000379979],"domain_scores_gemma":[0.9978143,0.000464798,0.00030817042,0.00019471308,0.0010239828,0.00019405154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010354372,0.00011683394,0.000269711,0.00016033217,0.00038993516,0.00021168737,0.00027934476,0.00005910441,0.00025486175],"category_scores_gemma":[0.00035048017,0.0000762762,0.00007918051,0.00039789232,0.00021875672,0.0014218629,0.00004738654,0.00037475248,0.00018648805],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013107316,0.0008341677,0.13571203,0.0013026635,0.000767702,0.000078336896,0.009505592,0.1531527,0.62309265,0.02931085,0.0016254501,0.043307114],"study_design_scores_gemma":[0.0003347255,0.00031098156,0.9807056,0.00006637118,0.0000135754335,0.000019172538,0.00012415285,0.0066055567,0.0036934204,0.0078067635,0.00023665714,0.00008303123],"about_ca_topic_score_codex":0.0030958762,"about_ca_topic_score_gemma":0.00038062307,"teacher_disagreement_score":0.84499353,"about_ca_system_score_codex":0.0000036835468,"about_ca_system_score_gemma":0.0001599065,"threshold_uncertainty_score":0.46800593},"labels":[],"label_agreement":null},{"id":"W2116718662","doi":"10.1029/2011gc003519","title":"Crustal structure across the central Alaska Range: Anatomy of a Mesozoic collisional zone","year":2011,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Geology; Fibrous joint; Felsic; Crust; Continental crust; Continental margin; Underplating; Shear zone; Subduction; Petrology; Geomorphology; Paleontology; Seismology; Geochemistry; Mafic; Tectonics","score_opus":0.008909681753992748,"score_gpt":0.2148218979392491,"score_spread":0.20591221618525635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116718662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897009,0.0003181308,0.000035533787,0.000027203749,0.00083672104,0.0003369083,0.00565612,0.00004327929,0.0030452097],"genre_scores_gemma":[0.9982288,0.000013552518,0.00009343003,0.000028107852,0.0007156448,0.0000056004187,0.0004490664,0.000011322616,0.00045450896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976262,0.00008941105,0.00050240825,0.00043624363,0.0005942509,0.0007515292],"domain_scores_gemma":[0.9985044,0.00010510457,0.00037605606,0.0006337229,0.0001878462,0.00019286553],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025555125,0.00033596324,0.0004937806,0.000017788405,0.0002891067,0.000085164174,0.0006971854,0.00018166967,0.0017983688],"category_scores_gemma":[0.000021412412,0.00023605442,0.00018746233,0.00029956165,0.00024321703,0.00018094886,0.000076016935,0.00021505111,0.000072048024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026766018,0.0011839265,0.55848294,0.005699031,0.0030770847,0.0004306892,0.03745128,0.005818072,0.33978623,0.0043025822,0.016715907,0.024375645],"study_design_scores_gemma":[0.0028816084,0.0003070815,0.7390285,0.0003089154,0.00029879183,0.00015697407,0.0037497755,0.0028609117,0.21957168,0.007777937,0.021242576,0.0018152405],"about_ca_topic_score_codex":0.005360384,"about_ca_topic_score_gemma":0.00055125024,"teacher_disagreement_score":0.18054555,"about_ca_system_score_codex":0.000006661058,"about_ca_system_score_gemma":0.0001321558,"threshold_uncertainty_score":0.9991141},"labels":[],"label_agreement":null},{"id":"W2116831667","doi":"10.1111/j.1365-246x.2008.03826.x","title":"Impact of regional mantle flow on subducting plate geometry and interplate stress: insights from physical modelling","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Slab; Lithosphere; Mantle (geology); Seismology; Intraplate earthquake; Slab window; Overpressure; Mantle wedge; Geophysics; Drag; Oceanic crust; Mechanics; Tectonics","score_opus":0.024359720132326543,"score_gpt":0.2481307697873114,"score_spread":0.22377104965498487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116831667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975555,0.00006667426,0.00081455667,0.00006718382,0.0006306767,0.000050249633,0.00037746536,0.000014364854,0.00042332485],"genre_scores_gemma":[0.9969852,0.00011161063,0.00077840296,0.000035987516,0.0018662637,4.511111e-7,0.00015596816,0.00000800163,0.000058141595],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99854213,0.00006167998,0.00033159702,0.0002735192,0.0005561822,0.00023488629],"domain_scores_gemma":[0.9990597,0.0002511322,0.0002526802,0.00012175634,0.00013438439,0.00018035987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006307069,0.00020792932,0.000333828,0.00014155495,0.00018578114,0.00009057829,0.00028924766,0.000059286987,0.0003993196],"category_scores_gemma":[0.000019788034,0.00015217827,0.00020901431,0.00010089462,0.00012912891,0.00042107588,0.0000371483,0.0003287749,0.00008892812],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024031198,0.0011343571,0.078846,0.000033098353,0.002078897,0.00066051923,0.0051799263,0.8655619,0.02111046,0.00207298,0.0014901438,0.019428588],"study_design_scores_gemma":[0.0012530914,0.00072956365,0.45767763,0.00022992931,0.000055514385,0.00020105495,0.00009547904,0.5087766,0.0027402192,0.027501155,0.00025700853,0.00048271782],"about_ca_topic_score_codex":0.0013821784,"about_ca_topic_score_gemma":0.000014493348,"teacher_disagreement_score":0.37883165,"about_ca_system_score_codex":0.000012415617,"about_ca_system_score_gemma":0.000051466646,"threshold_uncertainty_score":0.62056494},"labels":[],"label_agreement":null},{"id":"W2116910913","doi":"10.1111/j.1365-246x.2004.02175.x","title":"Shear wave anisotropy beneath the Cascadia subduction zone and western North American craton","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Craton; Seismology; Shear (geology); Shear zone; Shear wave splitting; Anisotropy; Geophysics; Petrology; Tectonics","score_opus":0.009701036025300916,"score_gpt":0.21203528533021201,"score_spread":0.2023342493049111,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116910913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954021,0.000035470704,0.0008408547,0.002335694,0.0010035806,0.00006996908,0.00009044418,0.000016576492,0.00020533854],"genre_scores_gemma":[0.9967896,0.00013867191,0.0004463029,0.0003512222,0.002054109,9.721391e-7,0.000054466054,0.0000054106144,0.00015928899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888444,0.00005400554,0.00021890311,0.00019477478,0.0004039682,0.00024393153],"domain_scores_gemma":[0.99942786,0.000050089948,0.00015896511,0.00010870564,0.0000982816,0.00015608106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011842339,0.00014249363,0.00017387242,0.000047514986,0.0002780585,0.00031469174,0.00021712403,0.00002352715,0.00019043163],"category_scores_gemma":[0.000013411036,0.00009198487,0.00007089196,0.00011496996,0.00017522844,0.00033828523,0.00002723338,0.00022853537,0.00013815188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010825994,0.0006971156,0.5899821,0.000036078207,0.0012327699,0.00080692634,0.0041161655,0.028744683,0.0095647555,0.011444233,0.0023388967,0.34995368],"study_design_scores_gemma":[0.00037969855,0.00023923158,0.9897178,0.000011501177,0.000027886334,0.00028000394,0.00006244093,0.00048544825,0.00055155245,0.002984032,0.0051071667,0.0001532665],"about_ca_topic_score_codex":0.0036606607,"about_ca_topic_score_gemma":0.0018328029,"teacher_disagreement_score":0.3997357,"about_ca_system_score_codex":0.00001267532,"about_ca_system_score_gemma":0.000045537567,"threshold_uncertainty_score":0.55338484},"labels":[],"label_agreement":null},{"id":"W2117274454","doi":"10.1046/j.1365-246x.2000.00091.x","title":"Westward drift of the lithosphere: not a result of rotational drag","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Asthenosphere; Lithosphere; Geology; Geophysics; Drag; Angular velocity; Toroid; Geodesy; Mechanics; Seismology; Physics; Classical mechanics; Tectonics","score_opus":0.007800545018761287,"score_gpt":0.21420972324820475,"score_spread":0.20640917822944346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117274454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98833793,0.00002430956,0.00004066882,0.0011394463,0.0009698599,0.00006717168,0.00032013402,0.000005962352,0.009094487],"genre_scores_gemma":[0.996779,0.000028844019,0.0005322904,0.00015446063,0.00070090033,5.9713193e-7,0.000026712522,0.0000032317002,0.0017739391],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99852777,0.0000838852,0.00042066112,0.00012609089,0.0006885807,0.00015303954],"domain_scores_gemma":[0.9992036,0.00013339207,0.00025707003,0.00013308089,0.00020058776,0.00007221852],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019985702,0.00010114772,0.00018705732,0.000025629864,0.00009104037,0.000052902455,0.0005219749,0.000041975753,0.00993288],"category_scores_gemma":[0.000048986396,0.00006508116,0.00017830374,0.00011787137,0.00012900979,0.00019904031,0.00001877085,0.00016761334,0.0001461526],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0040678554,0.0015255586,0.1688482,0.00013285973,0.0018331569,0.00009513985,0.0033508455,0.08578255,0.064771645,0.04872173,0.030097203,0.5907732],"study_design_scores_gemma":[0.00056432944,0.00011439825,0.9574308,0.00007149516,0.000028614788,0.000036547444,0.000020582816,0.0013954733,0.0073344926,0.012246605,0.02062947,0.00012722016],"about_ca_topic_score_codex":0.00059574144,"about_ca_topic_score_gemma":0.000042592583,"teacher_disagreement_score":0.78858256,"about_ca_system_score_codex":0.0000035231553,"about_ca_system_score_gemma":0.00008506197,"threshold_uncertainty_score":0.99097216},"labels":[],"label_agreement":null},{"id":"W2117368666","doi":"10.1093/gji/ggt099","title":"Glacial isostatic adjustment model with composite 3-D Earth rheology for Fennoscandia","year":2013,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"European Social Fund; Natural Sciences and Engineering Research Council of Canada; Nederlandse Organisatie voor Wetenschappelijk Onderzoek","keywords":"Geology; Mantle (geology); Post-glacial rebound; Rheology; Geophysics; Olivine; Creep; Glacial period; Mineralogy; Geomorphology; Thermodynamics","score_opus":0.009246787444377593,"score_gpt":0.2173834187572201,"score_spread":0.2081366313128425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117368666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9726859,0.000029794459,0.020902814,0.0015297023,0.001413524,0.00032369356,0.00024153765,0.000023463072,0.0028496229],"genre_scores_gemma":[0.9890451,0.000019682187,0.0072584664,0.0005581676,0.0013234993,0.000011904374,0.00017273996,0.0000069962716,0.001603433],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99886435,0.000037680948,0.0002513372,0.00019359427,0.00033621056,0.00031682185],"domain_scores_gemma":[0.99926525,0.00010198981,0.00015070992,0.00008657884,0.0002179072,0.00017756395],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008657618,0.00015507132,0.00021618229,0.00006178077,0.00016478538,0.00020782302,0.0002822507,0.000042690157,0.0020014956],"category_scores_gemma":[0.000008694286,0.000108054504,0.00009089313,0.000049246955,0.000075596836,0.0003840384,0.00001782619,0.00013850146,0.00043636307],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005626982,0.0018563246,0.06980063,0.00020334116,0.0036156615,0.00018904332,0.002742982,0.4184106,0.06494664,0.101309225,0.08299165,0.24830692],"study_design_scores_gemma":[0.0026605076,0.0009906336,0.49488688,0.00006199894,0.000092697876,0.0001501415,0.000059198628,0.44141254,0.00100175,0.053367354,0.004788963,0.00052733696],"about_ca_topic_score_codex":0.00037695112,"about_ca_topic_score_gemma":0.000089782145,"teacher_disagreement_score":0.42508626,"about_ca_system_score_codex":0.000006217313,"about_ca_system_score_gemma":0.000068530135,"threshold_uncertainty_score":0.9989108},"labels":[],"label_agreement":null},{"id":"W2117646422","doi":"10.1139/p11-021","title":"The renormalization group and the effective action","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Algoma University","funders":"","keywords":"Physics; Renormalization group; Renormalization; Mathematical physics; Effective action; Scalar (mathematics); Anomaly (physics); Action (physics); Functional renormalization group; Function (biology); TRACE (psycholinguistics); Asymptotic safety in quantum gravity; Scalar field theory; Group (periodic table); Tensor (intrinsic definition); Quantum mechanics; Pure mathematics; Quantum gravity","score_opus":0.012837115268313595,"score_gpt":0.17974965279799765,"score_spread":0.16691253752968405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117646422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98995167,0.0010238054,0.0012654603,0.00024357431,0.0020675703,0.00023502424,0.00003188976,0.0000037554807,0.005177224],"genre_scores_gemma":[0.99949825,0.00006691527,0.000027650352,0.000055816672,0.00032307298,3.0956818e-7,0.0000024964359,0.0000014546669,0.000024028604],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9996068,0.00009611953,0.00009454046,0.000035415913,0.00006272359,0.00010440946],"domain_scores_gemma":[0.99959296,0.000085765365,0.00011624138,0.000057995938,0.000046025314,0.00010101323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034183357,0.000043654738,0.00007268529,0.000012594919,0.00029343442,0.00007152164,0.00010092534,0.000016109361,0.00005284015],"category_scores_gemma":[0.000020315654,0.000021557045,0.000026937427,0.000056418183,0.00013019492,0.00016325954,0.0000016556112,0.000063036015,0.0000069444914],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006387098,0.000015448262,0.06496386,0.000048548318,0.00037129954,0.000053293625,0.015617968,0.000931065,0.00047494273,0.17337918,0.005312504,0.73819315],"study_design_scores_gemma":[0.0013706196,0.00037686693,0.79084146,0.00004579842,0.0001633649,0.00006676661,0.00069885695,0.0009596475,0.0020158566,0.15717955,0.04605457,0.00022664542],"about_ca_topic_score_codex":0.022345606,"about_ca_topic_score_gemma":0.0489135,"teacher_disagreement_score":0.73796654,"about_ca_system_score_codex":0.0000025771137,"about_ca_system_score_gemma":0.00006505721,"threshold_uncertainty_score":0.98416466},"labels":[],"label_agreement":null},{"id":"W2118406240","doi":"10.1029/2010gc003172","title":"Subducting slabs: Jellyfishes in the Earth's mantle","year":2010,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Transition zone; Slab; Mantle (geology); Subduction; Lithosphere; Geophysics; Mantle wedge; Seismic tomography; Seismology; Petrology; Tectonics","score_opus":0.006791508033869773,"score_gpt":0.1891174610997816,"score_spread":0.18232595306591182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118406240","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97421014,0.00009100556,0.0000052366645,0.00016738485,0.0013436035,0.00024467852,0.00015813176,0.000054785738,0.02372503],"genre_scores_gemma":[0.9973016,0.000008352584,0.00009218543,0.000081009326,0.0016809145,0.000009989953,0.00023912427,0.000008602554,0.0005782466],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9980915,0.00008595147,0.00038012568,0.0004315647,0.00042871086,0.0005820991],"domain_scores_gemma":[0.99876744,0.00021335957,0.00017473423,0.0006799839,0.0000683181,0.00009614115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073385326,0.00026565444,0.00031298862,0.00003126644,0.00023622834,0.00027696838,0.0006912417,0.00014942126,0.00087541447],"category_scores_gemma":[0.000054363547,0.00019634845,0.0000989009,0.00029944335,0.00009309785,0.000216476,0.000032646545,0.00045085853,0.00060840085],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000796273,0.00018828384,0.11366934,0.00089554704,0.00011648366,0.00026110464,0.0034463615,0.0007674309,0.860835,0.0021364295,0.004316903,0.0132874735],"study_design_scores_gemma":[0.0027807676,0.0002805954,0.3793358,0.00039054584,0.00019671816,0.0005051808,0.006601462,0.008184365,0.31452063,0.029035527,0.25430626,0.0038621724],"about_ca_topic_score_codex":0.006458795,"about_ca_topic_score_gemma":0.0022542358,"teacher_disagreement_score":0.5463144,"about_ca_system_score_codex":0.00000169392,"about_ca_system_score_gemma":0.00006250295,"threshold_uncertainty_score":0.97638094},"labels":[],"label_agreement":null},{"id":"W2118987944","doi":"10.1111/j.1365-246x.2005.02788.x","title":"Large time step numerical modelling of the flow of Maxwell materials","year":2005,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Viscoelasticity; Maxwell's equations; Mechanics; Geology; Classical mechanics; Physics","score_opus":0.010197728303153554,"score_gpt":0.20508023591356594,"score_spread":0.1948825076104124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118987944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98692787,0.000035008998,0.008033179,0.0006600572,0.001343962,0.00008505611,0.0007082796,0.000008546981,0.0021980302],"genre_scores_gemma":[0.99581975,0.000013446071,0.0022731593,0.0000915638,0.0012146104,3.2941355e-7,0.000052366715,0.0000042465,0.000530521],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986534,0.00009272647,0.00042881008,0.000118548356,0.00050888606,0.00019763282],"domain_scores_gemma":[0.9992854,0.0000716147,0.0003018381,0.00012816676,0.00014375334,0.00006923005],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002746529,0.00010762509,0.00024410007,0.000037810038,0.00007576995,0.000053886743,0.0004841922,0.000043099237,0.0050460277],"category_scores_gemma":[0.000017498554,0.00006881903,0.0001427678,0.000075430435,0.00005317509,0.0002076279,0.000043935957,0.00012093613,0.00020426926],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008914333,0.0010754007,0.004685919,0.000080118545,0.0008519394,0.000026163409,0.0012359844,0.8083658,0.13440353,0.01052934,0.010522473,0.027331868],"study_design_scores_gemma":[0.0018505484,0.00029285785,0.04732504,0.00020929734,0.00013765546,0.000107978216,0.00006412143,0.7457222,0.13274853,0.014572942,0.05641504,0.0005538511],"about_ca_topic_score_codex":0.00012283502,"about_ca_topic_score_gemma":0.0000053807944,"teacher_disagreement_score":0.062643684,"about_ca_system_score_codex":0.0000046636533,"about_ca_system_score_gemma":0.000040313385,"threshold_uncertainty_score":0.9958635},"labels":[],"label_agreement":null},{"id":"W2119243980","doi":"10.1002/2015jb012064","title":"The impacts of mantle phase transitions and the iron spin crossover in ferropericlase on convective mixing—is the evidence for compositional convection definitive? New results from a Yin‐Yang overset grid‐based control volume model","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle convection; Mantle (geology); Subduction; Convection; Geophysics; Spin transition; Spin crossover; Geodynamics; Condensed matter physics; Petrology; Tectonics; Mechanics; Physics; Seismology","score_opus":0.09986677130596558,"score_gpt":0.3730705947074852,"score_spread":0.2732038234015196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119243980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877106,0.00024344663,0.0009303557,0.007933208,0.00015872368,0.00060566195,0.0023184256,0.0000030890362,0.00009647403],"genre_scores_gemma":[0.9990372,0.000068836685,0.00008414537,0.00030486728,0.0004098116,0.000005414987,0.000032222935,0.000005029828,0.000052457784],"study_design_codex":"randomized_trial","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99750805,0.00066734117,0.0004426305,0.00019403642,0.0008369214,0.0003510262],"domain_scores_gemma":[0.99423987,0.004581134,0.0002650427,0.00018729584,0.0005004534,0.00022620292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023345675,0.00013476973,0.0003477948,0.000068171204,0.0003895667,0.00021181592,0.00025376197,0.00005226367,0.000029102786],"category_scores_gemma":[0.0010644926,0.000066308734,0.00014708392,0.00019014289,0.0006283483,0.00031046584,0.000013538068,0.00041080805,0.00001646749],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.5605148,0.002317799,0.0018015313,0.0001980716,0.0011039446,0.00020834328,0.02874224,0.27434042,0.06572481,0.009471608,0.04674961,0.00882679],"study_design_scores_gemma":[0.038990263,0.0054556346,0.07033173,0.0005659376,0.00015241532,0.000015134189,0.0010609395,0.84740967,0.009175391,0.02545504,0.0011085012,0.00027932055],"about_ca_topic_score_codex":0.0053767134,"about_ca_topic_score_gemma":0.000640337,"teacher_disagreement_score":0.5730693,"about_ca_system_score_codex":0.000016319029,"about_ca_system_score_gemma":0.0005890661,"threshold_uncertainty_score":0.8128018},"labels":[],"label_agreement":null},{"id":"W2119723105","doi":"10.1111/j.1365-246x.2006.02885.x","title":"The<i>S</i>receiver functions: synthetics and data example","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":215,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Receiver function; Classification of discontinuities; Seismogram; Lithosphere; Geology; Seismology; Mantle (geology); Waveform; Geophysics; Mathematical analysis; Computer science; Telecommunications; Mathematics; Tectonics","score_opus":0.019013364490961797,"score_gpt":0.2320459716611154,"score_spread":0.2130326071701536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119723105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96970314,0.000671356,0.0015839081,0.0037738443,0.0063731615,0.00013419878,0.0008939671,0.000045479577,0.01682096],"genre_scores_gemma":[0.99467826,0.00015478225,0.00028379943,0.00010377266,0.0025217528,5.087236e-7,0.00023694838,0.0000036313909,0.0020165388],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99904174,0.000053772223,0.00020398437,0.00018309029,0.0003285792,0.00018882523],"domain_scores_gemma":[0.9992848,0.00024537538,0.000101231344,0.00021129576,0.00008284033,0.00007442395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002899651,0.0000924444,0.000094491385,0.00002546984,0.0004122662,0.00049235905,0.0005161772,0.000027755385,0.0005767806],"category_scores_gemma":[0.000034258548,0.000059151644,0.000033700908,0.000048490256,0.000109622655,0.00035762045,0.00006888725,0.00014747768,0.00027362484],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056395086,0.00045351282,0.07142258,0.000025404504,0.00080526137,0.0002107897,0.00021638183,0.004554267,0.007314687,0.05476196,0.36254442,0.4971268],"study_design_scores_gemma":[0.00026643404,0.00004891162,0.26766458,0.000012859663,0.000032019103,0.00012464651,0.00003739071,0.004882124,0.000109663866,0.03384552,0.6928173,0.00015858159],"about_ca_topic_score_codex":0.0020167565,"about_ca_topic_score_gemma":0.000409782,"teacher_disagreement_score":0.4969682,"about_ca_system_score_codex":0.0000028895308,"about_ca_system_score_gemma":0.000026448979,"threshold_uncertainty_score":0.6315343},"labels":[],"label_agreement":null},{"id":"W2120089680","doi":"10.1016/j.tecto.2006.06.002","title":"Probing the history of the Mathematician paleoplate using surface waves","year":2006,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Surface (topology); Surface wave; Geophysics; Seismology; Geometry; Computer science; Mathematics; Telecommunications","score_opus":0.016133281034771588,"score_gpt":0.1868398317347869,"score_spread":0.17070655070001534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120089680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926788,0.00023312669,0.00006959787,0.000048199832,0.0008507473,0.00019889158,0.000025535746,0.000024234003,0.005870834],"genre_scores_gemma":[0.99859345,0.0000026756668,0.00040976022,0.000036975776,0.00016491825,4.420112e-7,0.0000055944593,0.000005424284,0.00078073697],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99922234,0.000065676155,0.00020455974,0.000125289,0.00019070388,0.00019144085],"domain_scores_gemma":[0.9993534,0.0000841252,0.000195028,0.00032006402,0.000030502617,0.000016852817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017284078,0.000115159484,0.00017047134,0.000009434006,0.00012641997,0.000024352881,0.00029197044,0.000032103017,0.00014273307],"category_scores_gemma":[0.00000566187,0.00006147558,0.00007487777,0.000114096234,0.00014603815,0.00008891138,0.000023418592,0.000076407065,0.000031571133],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056150242,0.00019115051,0.023576392,0.00058700255,0.00017278708,0.000009095078,0.0065307617,0.23274732,0.71034354,0.015398821,0.0052003353,0.0051866206],"study_design_scores_gemma":[0.0014589495,0.000259859,0.41012743,0.000686737,0.00070362986,0.000031145537,0.0006976485,0.12980258,0.20904167,0.20187224,0.043132987,0.00218513],"about_ca_topic_score_codex":0.0046567884,"about_ca_topic_score_gemma":0.0002786294,"teacher_disagreement_score":0.5013019,"about_ca_system_score_codex":0.000009692592,"about_ca_system_score_gemma":0.00008301594,"threshold_uncertainty_score":0.7039702},"labels":[],"label_agreement":null},{"id":"W2121738677","doi":"10.2138/am.2006.1772","title":"Phase transitions and volumetric properties of cryolite, Na<sub>3</sub>AlF<sub>6</sub>: Differential thermal analysis to 100 MPa","year":2006,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Cryolite; Differential thermal analysis; Thermodynamics; Eutectic system; Bar (unit); Melting point; Liquidus; Chemistry; Analytical Chemistry (journal); Phase transition; Materials science; Phase (matter); Metallurgy; Crystallography; Aluminium; Microstructure; Diffraction; Chromatography","score_opus":0.009824487578560961,"score_gpt":0.2082528786617011,"score_spread":0.19842839108314014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121738677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973458,0.00019944437,0.00062068703,0.00018576963,0.000118731754,0.00022760603,0.0008841424,0.000042332005,0.00037545714],"genre_scores_gemma":[0.99899703,0.00004128661,0.00016495687,0.00010402489,0.00022183885,0.000009278446,0.0004131088,0.00000962188,0.00003882649],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9983128,0.00013918808,0.00042069764,0.00041287983,0.00029420623,0.0004202487],"domain_scores_gemma":[0.9992315,0.000047737463,0.00018317327,0.00027612783,0.000086777,0.00017468784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000107079075,0.0002599062,0.00061488687,0.00040753,0.00016959991,0.00011377309,0.00019342685,0.000047131325,0.00009763722],"category_scores_gemma":[0.000021761074,0.00020499028,0.0001688974,0.0014731028,0.0005349547,0.0001524212,0.000020155345,0.00008149003,0.00004027517],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012412414,0.00020563327,0.008416362,0.000022954931,0.00020261428,0.000011951483,0.0001560186,0.00215406,0.968109,0.000026904403,0.0002763744,0.020294016],"study_design_scores_gemma":[0.0010998045,0.001136947,0.6346369,0.000022137623,0.0010067355,0.0000090838475,0.00013051715,0.004797723,0.35603198,0.000058054604,0.00037549023,0.0006946427],"about_ca_topic_score_codex":0.021981457,"about_ca_topic_score_gemma":0.0046899007,"teacher_disagreement_score":0.6262205,"about_ca_system_score_codex":0.000004665415,"about_ca_system_score_gemma":0.00003418974,"threshold_uncertainty_score":0.9845312},"labels":[],"label_agreement":null},{"id":"W2121887611","doi":"10.1111/j.1365-246x.2006.03259.x","title":"New insights into the lithosphere beneath the Superior Province from Rayleigh wave dispersion and receiver function analysis","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Manitoba; Western University","funders":"","keywords":"Geology; Lithosphere; Mantle (geology); Crust; Receiver function; Seismology; Seismometer; Rayleigh wave; Craton; Rift; Baltic Shield; Geophysics; Shear velocity; Shear (geology); Low-velocity zone; Surface wave; Tectonics; Petrology; Turbulence","score_opus":0.0065094538849051736,"score_gpt":0.19888715226415835,"score_spread":0.19237769837925317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121887611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99171597,0.00039610613,0.0043303375,0.0014224972,0.0011856518,0.00009069504,0.000025146928,0.000011919031,0.0008216602],"genre_scores_gemma":[0.99574196,0.00016183734,0.00053371384,0.00031617173,0.0022803443,4.068096e-7,0.00008393049,0.0000038432386,0.00087779714],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987248,0.00008204362,0.00026037276,0.00022807872,0.00051030336,0.00019441219],"domain_scores_gemma":[0.99919266,0.0002552602,0.00014294143,0.0001544305,0.000100942125,0.00015377316],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026955185,0.00014558414,0.00017430833,0.00004803439,0.0004408993,0.00039095504,0.00031986358,0.0000549267,0.0020129622],"category_scores_gemma":[0.000024701807,0.00007204429,0.00014355719,0.00020297582,0.00008766041,0.00037473583,0.00004482276,0.0002524748,0.00008718323],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018248165,0.00015724161,0.12253927,0.00000930032,0.0038936595,0.00017632073,0.008856962,0.0029633266,0.012056949,0.007571465,0.0057779877,0.8341727],"study_design_scores_gemma":[0.00027243985,0.000096382675,0.9422803,0.000013108414,0.00028423395,0.0000085487645,0.0002447944,0.002999575,0.0005780605,0.012162487,0.04092065,0.00013941298],"about_ca_topic_score_codex":0.008000353,"about_ca_topic_score_gemma":0.0035000236,"teacher_disagreement_score":0.8340333,"about_ca_system_score_codex":0.000011379012,"about_ca_system_score_gemma":0.00005388865,"threshold_uncertainty_score":0.99889934},"labels":[],"label_agreement":null},{"id":"W2121958340","doi":"10.1016/j.jorganchem.2005.07.064","title":"Pressure-tuning vibrational spectra of the heterobimetallic complexes, Ph3MCo(CO)4 (M = Sn, Pb)","year":2005,"lang":"en","type":"article","venue":"Journal of Organometallic Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Chemistry; Spectral line; Medicinal chemistry","score_opus":0.010112072647542616,"score_gpt":0.20700545447347035,"score_spread":0.19689338182592775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121958340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99378705,0.0010901609,0.000183153,0.00043037592,0.00026013274,0.00007622721,0.00013185666,0.000009177552,0.0040318775],"genre_scores_gemma":[0.9964644,0.000063667445,0.0017425941,0.00007398825,0.0008700707,2.1303889e-7,0.000027231434,0.0000071623217,0.0007507134],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998469,0.000050899394,0.000616823,0.00014652978,0.00049753586,0.00021919268],"domain_scores_gemma":[0.9987799,0.00007602179,0.00066786545,0.00024741207,0.00010934828,0.00011944787],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034957123,0.00016806563,0.00038170954,0.000028193523,0.00011067804,0.00007393436,0.00058570545,0.00007511283,0.014055669],"category_scores_gemma":[0.000046995807,0.000112122936,0.00021537804,0.00018205473,0.0001281262,0.0002788121,0.000028083094,0.0002158832,0.000033538476],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029320578,0.000060808656,0.0026994713,0.00007394884,0.00019975271,0.000003883697,0.00008822036,0.003340861,0.99237186,0.000038185102,0.0005769592,0.00051671505],"study_design_scores_gemma":[0.0005323476,0.00005180113,0.044504568,0.000053294705,0.00016065771,0.00016849308,0.000032281394,0.00039876648,0.9031394,0.00037154346,0.050377052,0.00020979736],"about_ca_topic_score_codex":0.000029034896,"about_ca_topic_score_gemma":0.000010640378,"teacher_disagreement_score":0.089232475,"about_ca_system_score_codex":0.000006467602,"about_ca_system_score_gemma":0.00013293161,"threshold_uncertainty_score":0.9868456},"labels":[],"label_agreement":null},{"id":"W2122118585","doi":"10.1029/2002jb002259","title":"Shear velocity structure and azimuthal anisotropy beneath eastern North America from Rayleigh wave inversion","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":155,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Shear wave splitting; Asthenosphere; Seismology; Rayleigh wave; Geophysics; Crust; Mantle (geology); Shear velocity; Shear (geology); Anisotropy; Surface wave; Tectonics; Petrology; Physics","score_opus":0.024590184529305677,"score_gpt":0.2549399305617055,"score_spread":0.23034974603239983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122118585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982773,0.00042334152,0.00008537845,0.00011875622,0.00030037173,0.00012598446,0.00021106143,0.000008317268,0.0004494782],"genre_scores_gemma":[0.99453485,0.00021990883,0.0043490413,0.000061436105,0.0006228935,3.2387732e-7,0.000029317593,0.00000907847,0.00017314327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970745,0.000538539,0.0003672446,0.00030771576,0.001146965,0.00056505424],"domain_scores_gemma":[0.9982211,0.0005051226,0.00020793898,0.00022942587,0.00033190777,0.00050447724],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031346624,0.00021158018,0.00047186785,0.00002564417,0.00030431175,0.00023182419,0.00030839676,0.00009791356,0.0027446698],"category_scores_gemma":[0.0002516605,0.00014971559,0.00011446568,0.00031839864,0.00031485892,0.00040948828,0.00005767103,0.0006020346,0.00012323403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00429736,0.0007547165,0.66997844,0.00028997974,0.0012197103,0.0016940391,0.0042819935,0.003462414,0.032319058,0.001800477,0.014661736,0.2652401],"study_design_scores_gemma":[0.0015511109,0.0021915939,0.9262574,0.000088726185,0.0000663228,0.000022206557,0.0006289804,0.0042989557,0.006500256,0.024240268,0.03370302,0.00045121272],"about_ca_topic_score_codex":0.006402434,"about_ca_topic_score_gemma":0.00047310148,"teacher_disagreement_score":0.2647889,"about_ca_system_score_codex":0.000013357125,"about_ca_system_score_gemma":0.00019435139,"threshold_uncertainty_score":0.998167},"labels":[],"label_agreement":null},{"id":"W2122253728","doi":"10.1785/0120130233","title":"Crustal and Upper-Mantle Anisotropy Related to Fossilized Transpression Fabric along the Denali Fault, Northern Canadian Cordillera","year":2014,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Agence Nationale de la Recherche","keywords":"Transpression; Geology; Seismology; Mantle (geology); Fault (geology); Paleontology; Sinistral and dextral","score_opus":0.006158500750160494,"score_gpt":0.19133115733457437,"score_spread":0.18517265658441387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122253728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97327316,0.00022394759,0.00020855511,0.02408096,0.00015063697,0.00030539787,0.000112210415,0.00001719441,0.0016279186],"genre_scores_gemma":[0.9933849,0.0000744978,0.0016311512,0.004461562,0.0000325035,0.0000020644857,0.000013119724,0.0000045049983,0.00039568893],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987362,0.00023358632,0.0002703541,0.0002275749,0.00023758542,0.00029467605],"domain_scores_gemma":[0.99917567,0.0002356788,0.0001539281,0.00023744868,0.000046275218,0.00015101941],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026873915,0.0001445358,0.0003177161,0.0000107561345,0.000320471,0.000024456394,0.00039921858,0.00010970118,0.0020503174],"category_scores_gemma":[0.0000639015,0.00007258404,0.00019150469,0.00013859528,0.00043258735,0.000013109974,0.000042413158,0.0001425764,0.000036462377],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011395217,0.00048795276,0.28877312,0.00049230736,0.0011762193,0.00001987913,0.015222306,0.040941108,0.018591814,0.00088435365,0.35611486,0.27615654],"study_design_scores_gemma":[0.0004413939,0.0004026642,0.3141994,0.000054338347,0.000062375126,0.000007555566,0.00044875307,0.0017848593,0.00063345913,0.00061187847,0.68113023,0.0002231176],"about_ca_topic_score_codex":0.3714567,"about_ca_topic_score_gemma":0.0010054916,"teacher_disagreement_score":0.3704512,"about_ca_system_score_codex":0.000004153925,"about_ca_system_score_gemma":0.000035492474,"threshold_uncertainty_score":0.99886197},"labels":[],"label_agreement":null},{"id":"W2122484400","doi":"10.1111/j.1365-246x.2004.02139.x","title":"A study of the uppermost inner core from<i>PKKP</i>and<i>P</i>′<i>P</i>′ differential traveltimes","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Inner core; Geology; Differential rotation; Outer core; Isotropy; Anisotropy; Mantle (geology); Core (optical fiber); Geodesy; Differential (mechanical device); Polar; Perpendicular; Structure of the Earth; Geophysics; Geometry; Physics; Mathematics; Optics; Astronomy","score_opus":0.014149707217727025,"score_gpt":0.22559648075529978,"score_spread":0.21144677353757277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122484400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99661094,0.000025859754,0.00006931729,0.00048708165,0.001952335,0.00014117679,0.0002157147,0.000009776101,0.0004877719],"genre_scores_gemma":[0.9985903,0.000015559961,0.00009784865,0.00014750798,0.0009927117,0.0000012206225,0.000028498187,0.0000052435457,0.00012109102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859476,0.00006252067,0.0003523555,0.000205391,0.0005891256,0.00019583672],"domain_scores_gemma":[0.9993295,0.00008087024,0.0002184034,0.00015652626,0.000105942534,0.000108733584],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000088722045,0.00016061464,0.0002441608,0.00004278413,0.00018642911,0.00013537295,0.0005114736,0.00004596634,0.00082375505],"category_scores_gemma":[0.00002803616,0.000097218726,0.00011292869,0.0000956789,0.00010866487,0.00019271248,0.00007265811,0.0002487652,0.000049889237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022883196,0.0073371865,0.65897477,0.00005794123,0.00410081,0.0005237754,0.027761616,0.017866105,0.18180612,0.016735632,0.003804919,0.07874282],"study_design_scores_gemma":[0.0017604886,0.0002605751,0.97504526,0.000040879353,0.00007107962,0.000038414026,0.0002816236,0.0001956695,0.0021278055,0.0194963,0.00051789696,0.00016398422],"about_ca_topic_score_codex":0.002772476,"about_ca_topic_score_gemma":0.0004020454,"teacher_disagreement_score":0.31607053,"about_ca_system_score_codex":0.000005871132,"about_ca_system_score_gemma":0.00005265508,"threshold_uncertainty_score":0.90195405},"labels":[],"label_agreement":null},{"id":"W2122990195","doi":"10.1086/499776","title":"A Neutron Star with a Massive Progenitor in Westerlund 1","year":2005,"lang":"en","type":"article","venue":"The Astrophysical Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":259,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Herzberg Institute of Astrophysics","funders":"","keywords":"Pulsar; Physics; Astrophysics; Neutron star; Magnetar; Binary pulsar; Astronomy; X-ray pulsar; Luminosity; RADIUS; Pulsar planet; Millisecond pulsar; Galaxy","score_opus":0.006666263875062734,"score_gpt":0.1946818980923481,"score_spread":0.18801563421728537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122990195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982978,0.000038789916,0.00005432,0.0012160528,0.000120476994,0.00012074857,0.000020777687,0.000009385728,0.00012161621],"genre_scores_gemma":[0.99604356,0.0000065907093,0.002269585,0.00009580898,0.0014932659,0.0000015189926,0.0000046181735,0.000004451107,0.00008061231],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990062,0.00011321493,0.00016691869,0.00012398661,0.00026490912,0.00032477046],"domain_scores_gemma":[0.9995721,0.000047354326,0.00009641527,0.00013894,0.000030567022,0.00011460255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013122709,0.00012027703,0.00016733617,0.00002950252,0.00013839724,0.00016440697,0.00026611547,0.000021946393,0.00033912866],"category_scores_gemma":[0.0000036533609,0.00006113369,0.00004554985,0.00010866547,0.000078878045,0.00024171817,0.00001176077,0.00025877854,0.00024109404],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0071669114,0.0013271121,0.08437004,0.00008003755,0.00073441595,0.0013462163,0.0075207097,0.21364892,0.38309002,0.0040327567,0.0038696616,0.2928132],"study_design_scores_gemma":[0.001024111,0.0008576271,0.98787105,0.000046537953,0.000043961387,0.00010677369,0.00016095162,0.002142921,0.00093059824,0.00067055324,0.0059199673,0.00022491885],"about_ca_topic_score_codex":0.00015051468,"about_ca_topic_score_gemma":0.00023635193,"teacher_disagreement_score":0.90350103,"about_ca_system_score_codex":0.000005692585,"about_ca_system_score_gemma":0.000058239748,"threshold_uncertainty_score":0.3713221},"labels":[],"label_agreement":null},{"id":"W2124161683","doi":"10.1046/j.1365-246x.2001.00497.x","title":"A reflector at 200 km depth beneath the northwest Pacific","year":2001,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismogram; Classification of discontinuities; Seismology; Reflector (photography); Mantle (geology); Subduction; Pacific Plate; Geodesy; Jump; Seafloor spreading; Geophysics; Tectonics; Optics","score_opus":0.015214840885146977,"score_gpt":0.23795219173395618,"score_spread":0.2227373508488092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124161683","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97334707,0.00008965863,0.00007640554,0.0022078461,0.002493748,0.00008293444,0.00020534571,0.0000258793,0.021471124],"genre_scores_gemma":[0.9923366,0.00015420199,0.00011676375,0.00033862152,0.0032194906,0.0000016095389,0.00017420415,0.000006163333,0.0036523608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849623,0.00008191556,0.0002823259,0.0002096699,0.00058879185,0.0003410705],"domain_scores_gemma":[0.9992259,0.00013011991,0.00016079034,0.00017122838,0.0001344876,0.00017747177],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00020608578,0.0001639497,0.00017104021,0.000051115,0.00042340154,0.00031111468,0.0005615336,0.000047890182,0.0061366153],"category_scores_gemma":[0.000026788832,0.00009971198,0.0001513981,0.00013245924,0.00008488143,0.00027754722,0.000042761858,0.00023989454,0.0016936618],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001473691,0.0005291226,0.7945714,0.000016650785,0.0010308094,0.0012722368,0.0013669804,0.006774439,0.0119360015,0.005962635,0.06622412,0.10884188],"study_design_scores_gemma":[0.00037355028,0.0001207125,0.7101325,0.000016040067,0.000028346254,0.00043771212,0.000048788585,0.0010860979,0.0002341755,0.0043652086,0.28295153,0.00020537157],"about_ca_topic_score_codex":0.0010009996,"about_ca_topic_score_gemma":0.001909395,"teacher_disagreement_score":0.21672742,"about_ca_system_score_codex":0.000016857979,"about_ca_system_score_gemma":0.000046483743,"threshold_uncertainty_score":0.99908364},"labels":[],"label_agreement":null},{"id":"W2124785446","doi":"10.1029/2008jb006091","title":"Spatial variations of P wave attenuation in the mantle beneath North America","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Seismometer; Subduction; Tectonics; Attenuation; Mantle (geology); Amplitude; Geodesy; Geophysics","score_opus":0.03178687503724948,"score_gpt":0.28722519453506584,"score_spread":0.25543831949781637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124785446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99689364,0.0001054422,0.00034406656,0.0009938005,0.00010371709,0.00014379564,0.000038056503,0.0000024303633,0.0013750514],"genre_scores_gemma":[0.998585,0.000077794924,0.0006978555,0.00007977253,0.00049226696,5.92605e-7,0.000017220444,0.0000021234607,0.0000473828],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99781007,0.00039977694,0.00039209623,0.00011374814,0.0009868172,0.0002974891],"domain_scores_gemma":[0.99860525,0.0006100253,0.00021807489,0.0001767569,0.0003034486,0.0000864456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007763185,0.00008740254,0.00025424862,0.000029080105,0.00011276359,0.000074746895,0.00036774942,0.000035520185,0.00049286016],"category_scores_gemma":[0.0002552423,0.000052605905,0.000091798334,0.00048742184,0.00010392384,0.00022012915,0.000012976588,0.00031256184,0.000058266338],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001628948,0.0017756991,0.09832505,0.00008749193,0.00020640132,0.00039340914,0.006460634,0.01432762,0.012051197,0.005091433,0.011891422,0.8477607],"study_design_scores_gemma":[0.0002734579,0.0011128855,0.9814987,0.000025127176,0.000012974146,0.0000041581216,0.00017222368,0.0034442013,0.00023421383,0.011016833,0.0021409278,0.00006428147],"about_ca_topic_score_codex":0.006192935,"about_ca_topic_score_gemma":0.0016322698,"teacher_disagreement_score":0.88317364,"about_ca_system_score_codex":0.000006214291,"about_ca_system_score_gemma":0.00013686944,"threshold_uncertainty_score":0.9361907},"labels":[],"label_agreement":null},{"id":"W2125405138","doi":"10.1073/pnas.0812624106","title":"High-pressure polymeric phases of carbon dioxide","year":2009,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"","keywords":"Crystallography; Amorphous solid; Stishovite; Cristobalite; Chemistry; Phase (matter); Carbon dioxide; Materials science; Thermodynamics; High pressure; Organic chemistry; Physics","score_opus":0.018715727011414607,"score_gpt":0.2490050314272957,"score_spread":0.23028930441588108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125405138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909195,0.0004343529,1.4539015e-7,0.0009447658,0.000049207934,0.0000964821,0.00008434455,0.000008177148,0.007463075],"genre_scores_gemma":[0.9992103,0.000032458476,0.00041574548,0.000118223856,0.000107664004,4.1889513e-7,4.499966e-7,9.454436e-7,0.00011377194],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99845463,0.000007278354,0.00030479618,0.00017801668,0.00090465025,0.00015064719],"domain_scores_gemma":[0.99930674,0.00007643234,0.00044551844,0.000009710759,0.00012731669,0.0000343108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005792699,0.00008947988,0.00021337782,0.00009949033,0.00009371772,0.000015006253,0.0007052804,0.000053949472,0.0000937725],"category_scores_gemma":[0.00013599322,0.000055747332,0.0000589341,0.0005266392,0.00044024267,0.00028450208,0.000022887443,0.000065445405,8.1765387e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038808757,0.000048424572,0.016351277,0.000059459726,0.00002675394,1.0550159e-8,0.00013729848,0.0011760637,0.96107125,0.019041793,0.00027803652,0.0017708465],"study_design_scores_gemma":[0.00012413324,0.00011294121,0.34164184,0.000050615337,0.000024808003,0.000001913742,0.000039266783,0.00032954913,0.62280583,0.034620937,0.000169901,0.00007827015],"about_ca_topic_score_codex":0.00031793021,"about_ca_topic_score_gemma":3.5571708e-7,"teacher_disagreement_score":0.3382654,"about_ca_system_score_codex":0.0000012047612,"about_ca_system_score_gemma":0.000024644189,"threshold_uncertainty_score":0.22733103},"labels":[],"label_agreement":null},{"id":"W2125742341","doi":"10.2113/gscanmin.43.2.513","title":"MICROSTRUCTURES OF COMMON POLYGONAL SERPENTINES FROM AXIAL HRTEM IMAGING, ELECTRON DIFFRACTION, AND LATTICE-SIMULATION DATA","year":2005,"lang":"en","type":"article","venue":"The Canadian Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"High-resolution transmission electron microscopy; Electron diffraction; Lattice (music); Microstructure; Diffraction; Materials science; Crystallography; Transmission electron microscopy; Composite material; Optics; Nanotechnology; Physics; Chemistry","score_opus":0.01694895472815197,"score_gpt":0.24573395678502577,"score_spread":0.2287850020568738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125742341","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99483126,0.00057927653,0.0000050307085,0.0016588536,0.00020880772,0.0000878645,0.0021080845,0.000008466721,0.0005123506],"genre_scores_gemma":[0.9971251,0.000013108141,0.00013397422,0.00034733088,0.0005137789,2.429626e-7,0.0017337616,0.0000033528422,0.00012933952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999318,0.00005426354,0.00015864897,0.00017758616,0.00008775048,0.00020373851],"domain_scores_gemma":[0.9993976,0.00008363143,0.0000849248,0.000305311,0.0000265531,0.000102028374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013311481,0.0000970095,0.00012997133,0.00003663742,0.0002029655,0.000105806925,0.0002851849,0.000033969518,0.00049109705],"category_scores_gemma":[0.000019516876,0.00006916372,0.000014317007,0.000051861796,0.00013046044,0.00019528969,0.00001748306,0.000068664616,0.000018330195],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003010368,0.00004456537,0.80537343,0.00005417803,0.00022994561,0.000020650663,0.0012210723,0.03538949,0.046492927,0.0015656604,0.043002922,0.066304095],"study_design_scores_gemma":[0.00017845148,0.000012390518,0.9197616,0.000005534892,0.00003767608,0.0000045562083,0.000011547772,0.02101819,0.00036528506,0.0010021348,0.05748464,0.0001179678],"about_ca_topic_score_codex":0.79954314,"about_ca_topic_score_gemma":0.94812953,"teacher_disagreement_score":0.1485864,"about_ca_system_score_codex":0.000005818459,"about_ca_system_score_gemma":0.000078370154,"threshold_uncertainty_score":0.5377168},"labels":[],"label_agreement":null},{"id":"W2127153226","doi":"10.1016/j.tecto.2009.06.010","title":"Deep-mantle contributions to the surface dynamics of the North American continent","year":2009,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Lawrence Livermore National Laboratory; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canadian Institute for Advanced Research; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Mantle (geology); Mantle convection; Lithosphere; Post-glacial rebound; Ocean surface topography; Hotspot (geology); Geophysics; Plate tectonics; Upwelling; Buoyancy; North American Plate; Convection; Isostasy; Seismology; Tectonics; Geodesy; Geomorphology; Glacial period; Oceanography; Meteorology; Mechanics","score_opus":0.0040773848013541105,"score_gpt":0.20476698812844218,"score_spread":0.20068960332708807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127153226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932245,0.000025832114,0.0011383102,0.0035939037,0.00029338532,0.00028340283,0.0006820595,0.000026268812,0.0007323426],"genre_scores_gemma":[0.9991829,0.000009789431,0.00011485869,0.00041865458,0.0001262459,8.016324e-7,0.000063577994,0.0000026661278,0.000080550504],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9991874,0.00006153239,0.00017391045,0.00014409902,0.00019483083,0.00023819793],"domain_scores_gemma":[0.99924994,0.000076515156,0.0001332275,0.00038517264,0.00009531214,0.00005984369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010418105,0.00011333479,0.00020146529,0.000009819876,0.0001902501,0.000037380276,0.0004085391,0.000015530717,0.00004523693],"category_scores_gemma":[0.000028349281,0.00006243903,0.00007456739,0.00042267307,0.00010275783,0.000047128815,0.000022564238,0.000086207416,0.00009273332],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026438467,0.00041270017,0.1948856,0.000043219334,0.00028397338,0.000008426625,0.002250112,0.6093471,0.01391726,0.033191863,0.007452996,0.13794234],"study_design_scores_gemma":[0.00015459563,0.00020533876,0.9766569,0.0000086752725,0.0000478583,9.1212564e-7,0.00005958499,0.012217607,0.0030424932,0.0018352768,0.0055851685,0.00018555693],"about_ca_topic_score_codex":0.0026340787,"about_ca_topic_score_gemma":0.006931371,"teacher_disagreement_score":0.7817713,"about_ca_system_score_codex":0.000006147818,"about_ca_system_score_gemma":0.00003905642,"threshold_uncertainty_score":0.39819568},"labels":[],"label_agreement":null},{"id":"W2127196892","doi":"10.1046/j.1365-246x.2002.01620.x","title":"Effects of mantle flow law stress exponent on postglacial induced surface motion and gravity in Laurentia","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Mantle (geology); Geophysics; Lithosphere; Laurentia; Rheology; Power law; Viscoelasticity; Physics; Seismology; Thermodynamics; Tectonics","score_opus":0.009086099087753974,"score_gpt":0.20454900895173914,"score_spread":0.19546290986398515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127196892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978125,0.00003917255,0.00003506098,0.0002196053,0.0010660165,0.000080331134,0.000084818064,0.0000059407557,0.0006565301],"genre_scores_gemma":[0.99935836,0.000029420253,0.000094962284,0.000057751,0.0003798616,3.9969856e-7,0.00002969632,0.0000030079007,0.00004654954],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990234,0.000090589994,0.0002156229,0.00015011843,0.0003596416,0.00016065143],"domain_scores_gemma":[0.9995853,0.00010543895,0.000114507915,0.000057881756,0.00005371543,0.00008321337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000104347426,0.000108087115,0.00017558009,0.00005126135,0.00006253597,0.00007935036,0.00015233111,0.00004878738,0.0004623872],"category_scores_gemma":[0.000018566592,0.000089077046,0.000053817657,0.000057280864,0.000041763607,0.00020657043,0.000018475168,0.00017591295,0.00006568118],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022889248,0.0061596837,0.21999106,0.00054053735,0.0010006786,0.00121366,0.004952851,0.040169142,0.48126543,0.03997334,0.0024792498,0.19996545],"study_design_scores_gemma":[0.0016252432,0.00045443687,0.91941077,0.00016223738,0.000030824925,0.000022195067,0.000024941253,0.022998141,0.046680376,0.007948665,0.0003657759,0.00027637873],"about_ca_topic_score_codex":0.0009576613,"about_ca_topic_score_gemma":0.00019943567,"teacher_disagreement_score":0.69941974,"about_ca_system_score_codex":0.0000056625363,"about_ca_system_score_gemma":0.000004582823,"threshold_uncertainty_score":0.50628155},"labels":[],"label_agreement":null},{"id":"W2127685082","doi":"10.1002/grl.50879","title":"Lithospheric fabric variations in central North America: Influence of rifting and Archean tectonic styles","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Manitoba Hydro","keywords":"Geology; Lithosphere; Terrane; Archean; Tectonics; Rift; Mantle (geology); Seismology; Shear wave splitting; Shear zone; Paleontology; Geophysics","score_opus":0.015363985784493824,"score_gpt":0.2477553071575118,"score_spread":0.23239132137301796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127685082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984642,0.000044690372,0.000046298792,0.00080913433,0.000030747648,0.00031444393,0.000041243795,0.000015882573,0.00023335608],"genre_scores_gemma":[0.9990499,0.000046938538,0.0006019513,0.00013363411,0.00009758033,0.000012270399,0.000030932777,0.0000049593978,0.000021834227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979361,0.0002784988,0.00025414317,0.00031153497,0.00048304652,0.0007366231],"domain_scores_gemma":[0.9988831,0.0005674805,0.00006617116,0.00021262004,0.00008355298,0.00018703956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023911867,0.00012429766,0.0002459579,0.00009858239,0.00013402019,0.000107775,0.00026440728,0.00003309236,0.00021360673],"category_scores_gemma":[0.00019551758,0.00010410884,0.000037475285,0.0007269508,0.0003678425,0.0003318508,0.00006479561,0.00030247506,0.00018243399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061452214,0.00016741124,0.80478007,0.0002140743,0.0000650629,0.00003055793,0.002448528,0.018206345,0.112519875,0.0005982622,0.00051976857,0.06038857],"study_design_scores_gemma":[0.00014572329,0.00008700572,0.9950807,0.000023112469,0.00000356591,4.3976374e-7,0.00008076725,0.0034531914,0.00014700631,0.0005984824,0.0002679794,0.00011200715],"about_ca_topic_score_codex":0.056736413,"about_ca_topic_score_gemma":0.0007737512,"teacher_disagreement_score":0.19030063,"about_ca_system_score_codex":0.000007667748,"about_ca_system_score_gemma":0.00006040556,"threshold_uncertainty_score":0.94954485},"labels":[],"label_agreement":null},{"id":"W2127984748","doi":"10.1002/cjg2.847","title":"A Study on Crustal Anisotropy Using P to S Converted Phases of Receiver Functions: Application to Ailaoshan‐Red River Fault Zone","year":2006,"lang":"en","type":"article","venue":"Chinese Journal of Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Victoria University of Wellington; University of Manitoba","keywords":"Geology; Anisotropy; Receiver function; Transverse plane; Seismology; Crust; Waveform; Mantle (geology); Polarization (electrochemistry); Broadband; Lithosphere; Tectonics; Geophysics; Physics; Optics","score_opus":0.012168345276679779,"score_gpt":0.25158523090165896,"score_spread":0.23941688562497918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127984748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99205315,0.00002359468,0.00663143,0.00008011992,0.0005093674,0.0003907595,0.00014838867,0.00001077197,0.00015243299],"genre_scores_gemma":[0.99818045,0.0000027669926,0.00086206174,0.00008146263,0.00071150984,0.0000014621565,0.000032706423,0.000007686356,0.000119880824],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986575,0.000068392015,0.0004798697,0.00018912906,0.00041658408,0.0001884801],"domain_scores_gemma":[0.9988899,0.000078539924,0.0003749664,0.00021042058,0.00032084875,0.00012527454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017294088,0.00019111588,0.00042289164,0.00015536985,0.000114761475,0.000045226712,0.00021238379,0.00003999193,0.00012076228],"category_scores_gemma":[0.000029721037,0.00013804842,0.000103999235,0.0005073183,0.000033717715,0.00024539966,0.000019184272,0.00009673894,0.000081559345],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003471255,0.0034534335,0.16250405,0.00008531948,0.0005350703,0.00012446154,0.003558996,0.2872224,0.5137226,0.00016710533,0.005302009,0.019853286],"study_design_scores_gemma":[0.002384225,0.0033847445,0.98139143,0.00009194532,0.00023449355,0.000023923381,0.00044403493,0.0021565666,0.0050220266,0.0023158262,0.0020958355,0.00045496845],"about_ca_topic_score_codex":0.0018127249,"about_ca_topic_score_gemma":0.00014968112,"teacher_disagreement_score":0.81888735,"about_ca_system_score_codex":0.000010218779,"about_ca_system_score_gemma":0.000053714346,"threshold_uncertainty_score":0.56294507},"labels":[],"label_agreement":null},{"id":"W2128155858","doi":"10.1144/gsl.sp.2002.199.01.02","title":"Seismic heterogeneity and anisotropy in the Western Superior Province, Canada: insights into the evolution of an Archaean craton","year":2002,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Queen's University","funders":"","keywords":"Archean; Craton; Geology; Anisotropy; Seismology; Paleontology; Earth science; Tectonics; Physics","score_opus":0.01333255597973714,"score_gpt":0.2032183269606457,"score_spread":0.18988577098090856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128155858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940384,0.00029743297,0.0000725859,0.004553237,0.00009774524,0.00032880812,0.00006816588,0.000014433429,0.00052920525],"genre_scores_gemma":[0.99866927,0.000115842544,0.00012916961,0.0005074909,0.00040841266,0.000010198118,0.000081651495,0.0000018008628,0.00007618052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988389,0.00020969036,0.000235799,0.00024207949,0.00025404012,0.00021947024],"domain_scores_gemma":[0.9994066,0.000116220166,0.000084384475,0.00026303213,0.000057596462,0.000072189236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002449265,0.00010899966,0.00015795277,0.000016587726,0.00036580858,0.00008660235,0.00039386097,0.00007706717,0.00021797814],"category_scores_gemma":[0.000032605127,0.000059290454,0.000048560036,0.00027018323,0.0003302917,0.0002225496,0.000039332284,0.0001379661,0.000006370894],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004497109,0.00039695232,0.94112295,0.000046014666,0.000064180735,0.0000060211228,0.008891664,0.0028010875,0.00076563656,0.020387491,0.012187923,0.013285113],"study_design_scores_gemma":[0.0001543384,0.00008467977,0.93568736,0.0000017792278,0.000008899047,0.0000030115173,0.00029170682,0.0043992,0.0000413683,0.0019431313,0.057296466,0.00008805069],"about_ca_topic_score_codex":0.36242485,"about_ca_topic_score_gemma":0.83931935,"teacher_disagreement_score":0.4768945,"about_ca_system_score_codex":0.000020433967,"about_ca_system_score_gemma":0.00011114015,"threshold_uncertainty_score":0.64182085},"labels":[],"label_agreement":null},{"id":"W2128895710","doi":"10.1038/ngeo658","title":"Core formation and metal–silicate fractionation of osmium and iridium from gold","year":2009,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Osmium; Mantle (geology); Silicate; Iridium; Geology; Meteorite; Partition coefficient; Platinum group; Geochemistry; Mineralogy; Astrobiology; Chemistry; Platinum; Ruthenium; Physics","score_opus":0.013845398193786274,"score_gpt":0.2322709527281058,"score_spread":0.21842555453431953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128895710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99731195,0.00074716465,0.00016050972,0.0005865941,0.0003014414,0.000091092836,0.00015542292,0.000015106506,0.0006307356],"genre_scores_gemma":[0.9984619,0.00008945832,0.0008974548,0.0003171726,0.000057545123,3.1053602e-7,0.000076976736,7.4133396e-7,0.00009842191],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993419,0.000017508472,0.00012600714,0.00018455519,0.00021387206,0.00011613214],"domain_scores_gemma":[0.99963707,0.00005817293,0.00010389234,0.000095624106,0.000051674986,0.000053538595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018889029,0.00007301915,0.00011250145,0.000047918493,0.000080134385,0.00004655779,0.000098885685,0.00008961116,0.000060230963],"category_scores_gemma":[0.00004673838,0.000056311343,0.000013190236,0.00014492792,0.00007205157,0.000529693,0.000008391125,0.00009963465,0.000007914169],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019155715,0.000092381255,0.07434788,0.00008669299,0.00002774235,0.00000824017,0.0013689979,0.00030397504,0.73499566,0.008420475,0.0027788498,0.17737757],"study_design_scores_gemma":[0.00012888886,0.00007698913,0.974978,0.0000107044025,0.000012955251,0.000004360976,0.000025317107,0.0030102069,0.0070112203,0.008708066,0.0059405975,0.00009263775],"about_ca_topic_score_codex":0.0006319436,"about_ca_topic_score_gemma":0.00011714981,"teacher_disagreement_score":0.9006302,"about_ca_system_score_codex":0.000001208275,"about_ca_system_score_gemma":0.000013225331,"threshold_uncertainty_score":0.22963098},"labels":[],"label_agreement":null},{"id":"W2129458104","doi":"10.1029/2009gc002375","title":"Shear wave anisotropy beneath Nicaragua and Costa Rica: Implications for flow in the mantle wedge","year":2009,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Nuclear Safety Commission","keywords":"Geology; Shear wave splitting; Mantle wedge; Seismic anisotropy; Mantle (geology); Olivine; Subduction; Seismology; Anisotropy; Geometry; Geophysics; Mineralogy; Physics; Tectonics; Optics","score_opus":0.01574359602382391,"score_gpt":0.22248186005973927,"score_spread":0.20673826403591536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129458104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99219203,0.00057197176,0.0002378034,0.0010400136,0.00021598992,0.0007507598,0.001689038,0.00004389816,0.0032584995],"genre_scores_gemma":[0.99787277,0.000052017604,0.0004087278,0.0002128589,0.0005322535,0.000027278635,0.00075615617,0.00000584225,0.00013209903],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985871,0.00005262057,0.00031333795,0.0004188359,0.00017445681,0.00045369525],"domain_scores_gemma":[0.9990012,0.00018425356,0.00012533697,0.00051450933,0.00007327703,0.000101400874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029297188,0.00022785833,0.00031920592,0.000023806417,0.00026242368,0.00017360218,0.00032075387,0.0001079862,0.000056208974],"category_scores_gemma":[0.000022375225,0.0001745871,0.00008372884,0.00019689772,0.00005403297,0.00012801038,0.000017299306,0.00012236467,0.000043673925],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010198335,0.001915794,0.100514896,0.0035212778,0.00065788254,0.00014453649,0.009275321,0.008564313,0.5424641,0.040141672,0.07891506,0.21286531],"study_design_scores_gemma":[0.0022992447,0.00048873294,0.8659433,0.00018066834,0.00018283093,0.00010710892,0.0007353852,0.01624062,0.01036626,0.07295192,0.029161723,0.0013422245],"about_ca_topic_score_codex":0.0007947061,"about_ca_topic_score_gemma":0.00007979659,"teacher_disagreement_score":0.76542836,"about_ca_system_score_codex":0.000006140867,"about_ca_system_score_gemma":0.000047674595,"threshold_uncertainty_score":0.71194553},"labels":[],"label_agreement":null},{"id":"W2129616465","doi":"10.1144/sp389.7","title":"The Hudson Bay Lithospheric Experiment (HuBLE): insights into Precambrian plate tectonics and the development of mantle keels","year":2013,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; Geological Survey of Canada; Natural Resources Canada; University of Calgary","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Precambrian; Geology; Bay; Lithosphere; Mantle (geology); Plate tectonics; Tectonics; Paleontology; Oceanography","score_opus":0.010301229835693702,"score_gpt":0.20806530769612955,"score_spread":0.19776407786043584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129616465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97924256,0.0014231409,0.0005271685,0.00517613,0.00037443236,0.0009252408,0.000009387693,0.00005146169,0.01227047],"genre_scores_gemma":[0.9912865,0.00052797946,0.006252664,0.00019086979,0.00042756912,0.000095834555,0.000059285274,0.00000393785,0.0011553518],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9986547,0.000118681695,0.00040626823,0.0002629594,0.00026517047,0.0002922074],"domain_scores_gemma":[0.99894977,0.00034961206,0.00017826383,0.00028527912,0.00012795247,0.00010911899],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004526212,0.00014651635,0.00022345089,0.000009094324,0.0009944821,0.00027539145,0.00042052922,0.000107400156,0.0022037833],"category_scores_gemma":[0.00006414675,0.00007109125,0.000095574665,0.00024527698,0.000553886,0.00020192873,0.000107834414,0.00012763143,0.00014203473],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042083592,0.0007147449,0.04938464,0.00014742035,0.0011017829,0.0000012717771,0.0683454,0.0010305714,0.006662447,0.3990138,0.07787564,0.39530146],"study_design_scores_gemma":[0.0007361098,0.000069075286,0.5124093,0.000007297273,0.000021973961,0.0000011888593,0.0010593784,0.0013085554,0.0012458558,0.020010186,0.46289477,0.00023628333],"about_ca_topic_score_codex":0.0007882459,"about_ca_topic_score_gemma":0.0009459389,"teacher_disagreement_score":0.4630247,"about_ca_system_score_codex":0.000007886331,"about_ca_system_score_gemma":0.00008010702,"threshold_uncertainty_score":0.9987083},"labels":[],"label_agreement":null},{"id":"W2129633729","doi":"10.1046/j.1365-246x.2002.01712.x","title":"LITH5.0: a revised crustal model for Canada based on Lithoprobe results","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Geology; Mantle (geology); Interpolation (computer graphics); Spline (mechanical); Geodesy; Seismology; Geophysics; Computer science; Engineering","score_opus":0.02106262925495937,"score_gpt":0.21777063403222188,"score_spread":0.19670800477726252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129633729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.80826885,0.00021286015,0.033661835,0.04112625,0.014950572,0.0016946367,0.017623058,0.00019046868,0.082271464],"genre_scores_gemma":[0.99217045,0.000011852944,0.0016845809,0.0013396152,0.0016093834,0.000003486922,0.00017394935,0.000006995842,0.0029996636],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9984015,0.00004450307,0.00036507292,0.00024971802,0.0006246577,0.0003145334],"domain_scores_gemma":[0.99904543,0.00021683337,0.00018452438,0.00014661855,0.00019666084,0.00020992679],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020508512,0.0001650019,0.00020364058,0.000057232563,0.00019305109,0.00020199675,0.00036904737,0.00004645313,0.0010789535],"category_scores_gemma":[0.00013657041,0.00012957658,0.00013393974,0.00007046371,0.00003026431,0.0001778681,0.000010911644,0.00019165053,0.00008758694],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022443624,0.0004842515,0.0009360851,0.000056651144,0.000257646,0.0002043792,0.00030177907,0.6335795,0.0007794342,0.003158087,0.29841223,0.05958561],"study_design_scores_gemma":[0.0010706333,0.00015258348,0.005063263,0.000043778546,0.00001588647,0.0000099501785,0.000005616733,0.960611,0.00011622313,0.002108644,0.030616451,0.00018596981],"about_ca_topic_score_codex":0.020874018,"about_ca_topic_score_gemma":0.014673756,"teacher_disagreement_score":0.32703152,"about_ca_system_score_codex":0.000024281126,"about_ca_system_score_gemma":0.00015874622,"threshold_uncertainty_score":0.9998342},"labels":[],"label_agreement":null},{"id":"W2131064045","doi":"10.1017/s0885715613001255","title":"Crystal structure of a birefringent andradite–grossular from Crowsnest Pass, Alberta, Canada","year":2013,"lang":"en","type":"article","venue":"Powder Diffraction","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Andradite; Grossular; Pleochroism; Crystallography; Rietveld refinement; Electron microprobe; Analytical Chemistry (journal); Crystal structure; Phase (matter); Powder diffraction; Chemistry; Homogeneous; Materials science; Birefringence; Mineralogy; Physics; Metallurgy; Skarn; Optics; Thermodynamics","score_opus":0.004881914877149126,"score_gpt":0.1691446523867039,"score_spread":0.16426273750955478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131064045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99758625,0.0000956947,0.000012351034,0.000185979,0.0011164483,0.00014821076,0.00042967743,0.000011103981,0.00041426913],"genre_scores_gemma":[0.99895054,0.000011592268,0.00007116282,0.00008821434,0.00028828337,0.0000012338409,0.00038279893,0.0000049079795,0.000201245],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99912214,0.00003781252,0.00019936216,0.00019971158,0.00023959856,0.00020137886],"domain_scores_gemma":[0.99945164,0.00008357924,0.00013641053,0.00018053995,0.00004821415,0.000099590296],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000022557457,0.0001273281,0.00018366294,0.000025388776,0.00008834709,0.00007389011,0.00010728738,0.00006105044,0.008312237],"category_scores_gemma":[0.000015501888,0.00010251752,0.0000309968,0.000068037814,0.000024349107,0.0002906485,0.000008678568,0.00007242196,0.00006278518],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008435681,0.00007191945,0.4058301,0.000109992376,0.0002456075,0.000014304682,0.00063698797,0.0023270927,0.56375426,0.00008314983,0.016434811,0.010407443],"study_design_scores_gemma":[0.0001752622,0.000025638132,0.97086304,0.000010446537,0.000026430063,0.0000023682508,0.00004997928,0.00063860125,0.007885636,0.0007443692,0.019430008,0.00014822533],"about_ca_topic_score_codex":0.98953766,"about_ca_topic_score_gemma":0.911158,"teacher_disagreement_score":0.56503296,"about_ca_system_score_codex":0.000007849736,"about_ca_system_score_gemma":0.000086232634,"threshold_uncertainty_score":0.9925943},"labels":[],"label_agreement":null},{"id":"W2131628398","doi":"10.1103/physreve.73.036401","title":"Static and dynamic conductivity of warm dense matter within a density-functional approach: Application to aluminum and gold","year":2006,"lang":"en","type":"article","venue":"Physical Review E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute for Microstructural Sciences","funders":"","keywords":"Warm dense matter; Conductivity; Density functional theory; Electrical resistivity and conductivity; Ion; Fermi's golden rule; Atomic physics; Electron; Scattering; Ionization; Perturbation theory (quantum mechanics); Range (aeronautics); Physics; Condensed matter physics; Materials science; Quantum mechanics; Fermi Gamma-ray Space Telescope","score_opus":0.01047376079811858,"score_gpt":0.2293348196484258,"score_spread":0.21886105885030724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131628398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972104,0.00079167256,0.0009842311,0.0002679559,0.000035494675,0.00035218016,0.000062239254,0.000008125316,0.00028771214],"genre_scores_gemma":[0.99872345,0.00013088166,0.00060230406,0.00034794293,0.000055176042,0.000008867984,0.00008105972,0.0000028149977,0.000047520833],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993384,0.00005656269,0.00015287561,0.00021416169,0.00013395933,0.000104053055],"domain_scores_gemma":[0.9996443,0.00006529174,0.0000805158,0.00011943092,0.00002986011,0.000060625734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013114234,0.00009543323,0.00028265652,0.000015006377,0.0000311014,0.000017910224,0.000042600197,0.000013671253,0.000031779295],"category_scores_gemma":[0.000011198071,0.000072076116,0.000025091249,0.00008412328,0.00006362419,0.00008337875,0.000015559908,0.000042008895,0.000068920184],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005860152,0.0021361539,0.18352075,0.03646471,0.00046174476,0.000020299161,0.0020632872,0.0064625,0.52750283,0.04895027,0.02980199,0.16202943],"study_design_scores_gemma":[0.0004424221,0.00019373934,0.9347647,0.00042940193,0.00031426788,0.000028457973,0.000025155687,0.020690504,0.002923829,0.036225654,0.003403041,0.00055884774],"about_ca_topic_score_codex":0.00078494934,"about_ca_topic_score_gemma":0.0000960417,"teacher_disagreement_score":0.75124395,"about_ca_system_score_codex":0.0000015393582,"about_ca_system_score_gemma":0.00001000474,"threshold_uncertainty_score":0.29391786},"labels":[],"label_agreement":null},{"id":"W2132233970","doi":"10.1111/j.1365-246x.2008.03888.x","title":"Geometrical attenuation, frequency dependence of<i>Q</i>, and the absorption band problem","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Attenuation; Parametrization (atmospheric modeling); Amplitude; Inversion (geology); Absorption (acoustics); Computational physics; Spectral shape analysis; Physics; Frequency band; Optics; Tectonics; Power law; Scattering; Geometry; Geology; Mathematics; Spectral line; Bandwidth (computing); Quantum mechanics; Telecommunications; Statistics; Seismology; Computer science","score_opus":0.01406351638720785,"score_gpt":0.21947170323205356,"score_spread":0.2054081868448457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132233970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939071,0.00017319326,0.0011192907,0.0011195898,0.00051168486,0.00009973431,0.00004551314,0.000008641154,0.0030152502],"genre_scores_gemma":[0.9980595,0.00027437136,0.000712252,0.00011072614,0.00064955425,0.0000012150982,0.000022213024,0.0000024383432,0.00016770975],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987811,0.00008951012,0.0003181076,0.00013595512,0.00052741583,0.00014792166],"domain_scores_gemma":[0.99917907,0.00023376572,0.0002108411,0.00008133827,0.00021277228,0.00008220406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035282862,0.00009400729,0.00017713658,0.0000759097,0.00020197718,0.0000768847,0.00026602452,0.00003839964,0.00057414867],"category_scores_gemma":[0.00008931374,0.000057034096,0.00007885531,0.00014885733,0.00025570195,0.00031235424,0.000017027189,0.00017125114,0.00007710012],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022275783,0.00067916285,0.7059513,0.00010292496,0.0013514825,0.000365429,0.004112518,0.00968031,0.02993555,0.11970481,0.009178424,0.11671056],"study_design_scores_gemma":[0.00149693,0.00011881038,0.9174193,0.000027371494,0.000036193716,0.0005109415,0.00002526319,0.0023148493,0.0007625351,0.075739115,0.0013834966,0.00016516591],"about_ca_topic_score_codex":0.000697485,"about_ca_topic_score_gemma":0.000023273746,"teacher_disagreement_score":0.21146807,"about_ca_system_score_codex":0.0000038627077,"about_ca_system_score_gemma":0.000043576485,"threshold_uncertainty_score":0.6286526},"labels":[],"label_agreement":null},{"id":"W2132509829","doi":"10.1046/j.1365-246x.2000.00090.x","title":"Modelling teleseismic waves in dipping anisotropic structures","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":343,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Anisotropy; Classification of discontinuities; Geology; Seismic anisotropy; Amplitude; Seismogram; Slowness; Geophysics; Mantle (geology); Discontinuity (linguistics); Planar; Lithosphere; Seismic wave; Seismology; Optics; Tectonics; Physics; Mathematical analysis","score_opus":0.012189076825855802,"score_gpt":0.22108091866795646,"score_spread":0.20889184184210066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132509829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931998,0.00006379847,0.00064043776,0.00032467447,0.0007845858,0.00004713232,0.00004208977,0.000015682974,0.004881771],"genre_scores_gemma":[0.99690586,0.00012480428,0.00087437406,0.00016836617,0.0013508785,4.5792274e-7,0.00003794564,0.0000043814503,0.00053292594],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988415,0.00005496265,0.00028872298,0.00018240082,0.00035792773,0.00027443815],"domain_scores_gemma":[0.99964595,0.00005398624,0.00007281671,0.00008216557,0.000043252472,0.000101846075],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010308788,0.00012934614,0.0001757826,0.00008477359,0.000113816604,0.0002272438,0.00033692335,0.000046174755,0.00811761],"category_scores_gemma":[0.0000072891708,0.00010367051,0.000081051956,0.00009005697,0.000040462877,0.00037742054,0.000011182677,0.00024333072,0.00036490118],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013578148,0.000060203856,0.0069075734,0.0000075525472,0.000074670956,0.0001413376,0.00030691706,0.885845,0.00097377395,0.0026936072,0.00034370276,0.102509886],"study_design_scores_gemma":[0.001138487,0.00014823276,0.3118081,0.00009343335,0.000022781713,0.00017903268,0.000073938616,0.47113764,0.00056101254,0.18392134,0.03038818,0.00052781607],"about_ca_topic_score_codex":0.0012226305,"about_ca_topic_score_gemma":0.00004649629,"teacher_disagreement_score":0.41470736,"about_ca_system_score_codex":0.000008770764,"about_ca_system_score_gemma":0.000032024163,"threshold_uncertainty_score":0.9927891},"labels":[],"label_agreement":null},{"id":"W2132562668","doi":"10.1073/pnas.1305116110","title":"Electronic structure of carbon dioxide under pressure and insights into the molecular-to-nonmolecular transition","year":2013,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Western University","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China; U.S. Department of Energy","keywords":"Raman spectroscopy; Chemical physics; Phase transition; Carbon dioxide; Amorphous solid; Chemistry; Phase (matter); Molecular dynamics; Materials science; Raman scattering; Carbon fibers; Crystallography; Thermodynamics; Computational chemistry; Optics; Organic chemistry; Physics","score_opus":0.0065647234340604375,"score_gpt":0.21052461283507798,"score_spread":0.20395988940101753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132562668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965417,0.00066044834,0.0000022017516,0.002033149,0.000014329869,0.00023004718,0.000013527163,0.000003436775,0.0005011857],"genre_scores_gemma":[0.99951494,0.000023332139,0.00014648125,0.00027434854,0.000024131472,0.0000014295551,4.6687725e-7,0.0000015040775,0.000013353275],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988683,0.000011468698,0.00018685874,0.00016891939,0.000634762,0.00012972915],"domain_scores_gemma":[0.9996013,0.0000450811,0.00017382963,0.000011141792,0.00013752158,0.000031093285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024218937,0.00008025089,0.00012669657,0.00006497377,0.00010650485,0.00003347508,0.00043446946,0.00005571514,0.00003252144],"category_scores_gemma":[0.000045505436,0.00004252478,0.000032392993,0.0003483188,0.0003661761,0.0002537747,0.000028914164,0.000087390225,5.701758e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006819085,0.000005114634,0.00063109247,0.000045497964,0.000025481917,2.5107958e-9,0.001056348,0.0030810307,0.97658706,0.018311072,0.000019952493,0.0002305502],"study_design_scores_gemma":[0.000083873005,0.00007294783,0.118477486,0.00003647525,0.00003287969,0.0000018361819,0.00022691984,0.0017803119,0.60404396,0.2750187,0.00014542468,0.00007918165],"about_ca_topic_score_codex":0.00032049324,"about_ca_topic_score_gemma":0.0000027078459,"teacher_disagreement_score":0.37254307,"about_ca_system_score_codex":0.0000017367971,"about_ca_system_score_gemma":0.00002389829,"threshold_uncertainty_score":0.17341103},"labels":[],"label_agreement":null},{"id":"W2132633001","doi":"10.1139/v09-124","title":"A comparative study on the LDA + <i>U</i> and hybrid functional methods on the description of the electronic structure of YTiO <sub>3</sub> under high pressure","year":2009,"lang":"en","type":"article","venue":"Canadian Journal of Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Chemistry; Hybrid functional; Density functional theory; Electronic structure; Local-density approximation; Mixing (physics); Hubbard model; Band gap; High pressure; Statistical physics; Matching (statistics); Computational chemistry; Chemical physics; Thermodynamics; Molecular physics; Quantum mechanics; Physics; Statistics; Mathematics","score_opus":0.016664197487622885,"score_gpt":0.2124560835627188,"score_spread":0.19579188607509593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132633001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99808985,0.00025800735,0.000021193038,0.00093251746,0.00015485687,0.000116465235,0.0001371796,9.556246e-7,0.00028897892],"genre_scores_gemma":[0.9995828,0.0000055560795,0.0000077524755,0.00024516686,0.0001256451,2.2528616e-7,0.000004880131,0.000001816951,0.000026159056],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991754,0.00017745087,0.00020332004,0.00008950265,0.00020080262,0.00015348193],"domain_scores_gemma":[0.99923575,0.00015655345,0.0002662509,0.00015938561,0.00009376433,0.00008828445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003355428,0.000101978636,0.00019083021,0.000017483675,0.00015412929,0.000040674568,0.00022307817,0.000034591212,0.0002715292],"category_scores_gemma":[0.00003335687,0.0000490267,0.000051854193,0.00008364969,0.000108951754,0.000049530936,0.000003349452,0.00025411713,4.7081596e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018864112,0.000046295878,0.0031467066,0.000026930504,0.0003739783,0.0000050728513,0.001023799,0.011987297,0.9757892,0.000884606,0.005656653,0.0008708028],"study_design_scores_gemma":[0.0002578317,0.00027177544,0.2698998,0.00004441216,0.0000990136,0.000030014702,0.00055802416,0.000048458554,0.71931136,0.008785551,0.00060939667,0.000084396845],"about_ca_topic_score_codex":0.00053997536,"about_ca_topic_score_gemma":0.0012945951,"teacher_disagreement_score":0.26675308,"about_ca_system_score_codex":0.000008583706,"about_ca_system_score_gemma":0.00036127257,"threshold_uncertainty_score":0.29730543},"labels":[],"label_agreement":null},{"id":"W2133222974","doi":"10.1002/2014jb011067","title":"Bayesian inference for ultralow velocity zones in the Earth's lowermost mantle: Complex ULVZ beneath the east of the Philippines","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Australian Government","keywords":"Geology; Bayesian inference; Bayesian probability; Mantle (geology); Parallel tempering; Inversion (geology); Nonlinear system; Geophysics; Algorithm; Geodesy; Seismology; Computer science; Markov chain Monte Carlo; Physics; Artificial intelligence; Tectonics","score_opus":0.05248532653138223,"score_gpt":0.3222693776096103,"score_spread":0.26978405107822806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133222974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99377894,0.00005737512,0.00073447736,0.0036068338,0.0003369164,0.0005137591,0.00015298423,0.0000043713744,0.0008143394],"genre_scores_gemma":[0.99841815,0.00005555011,0.00030216845,0.00016282174,0.0009172821,0.0000036051752,0.00000995931,0.0000060720963,0.00012441039],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99653727,0.0009154776,0.0005280959,0.0001955833,0.0012369569,0.0005866125],"domain_scores_gemma":[0.9965077,0.0021458813,0.0002914869,0.00044730757,0.00047853327,0.00012909579],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031141997,0.00017543002,0.00045140184,0.00008544571,0.0004909593,0.0001917025,0.0013459759,0.00006553546,0.00021742232],"category_scores_gemma":[0.0009099304,0.00007707987,0.00022961841,0.0005259377,0.00056997506,0.00022075608,0.000049970262,0.0005726207,0.000029101046],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.007920924,0.004081854,0.16998532,0.0023951642,0.0014968985,0.00017713624,0.030995365,0.0492441,0.23877065,0.106144205,0.02014728,0.3686411],"study_design_scores_gemma":[0.0006639868,0.000917311,0.942566,0.00013319499,0.00002709307,0.000012878984,0.00032680403,0.014009824,0.00229564,0.029319772,0.009566427,0.00016110211],"about_ca_topic_score_codex":0.0010113432,"about_ca_topic_score_gemma":0.0011734057,"teacher_disagreement_score":0.7725806,"about_ca_system_score_codex":0.0000027847996,"about_ca_system_score_gemma":0.00019428952,"threshold_uncertainty_score":0.3776112},"labels":[],"label_agreement":null},{"id":"W2133351858","doi":"10.1016/j.jsg.2006.12.006","title":"Importance of differentiating ductile slickenside striations from stretching lineations and variation of shear direction across a high-strain zone","year":2007,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; Western University; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lineation; Geology; Striation; Shear zone; Shear (geology); Simple shear; Perpendicular; Seismology; Geometry; Petrology; Tectonics","score_opus":0.00858220416703783,"score_gpt":0.2378474200250564,"score_spread":0.22926521585801857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133351858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975148,0.000112689195,0.0012117444,0.000096248885,0.0007299141,0.000058186968,0.00025903524,0.000004302031,0.00001306895],"genre_scores_gemma":[0.99375457,0.00001886342,0.0057963403,0.00000921029,0.00034876014,7.7269696e-8,0.00006201355,0.000002215457,0.0000079371775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989122,0.0000642289,0.00062405417,0.000100385165,0.00015093072,0.00014820865],"domain_scores_gemma":[0.9985554,0.0002563588,0.00090219756,0.00007492749,0.00015974227,0.000051360985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035285254,0.00008343502,0.00029911558,0.000067786146,0.00009469584,0.000016407625,0.000073317926,0.00006640952,0.00021442144],"category_scores_gemma":[0.000115252325,0.00006622766,0.000044933156,0.00010199751,0.00006626422,0.00022042693,0.000011678415,0.00011370258,3.9986418e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018584922,0.000017553024,0.80371916,0.000038363705,0.00021091865,0.000009313579,0.004177269,0.008188162,0.1666191,0.0006111579,0.000010220628,0.016212929],"study_design_scores_gemma":[0.00035311776,0.00011456052,0.99165934,0.000015172162,0.000041787865,0.000022160293,0.0002665291,0.00096776447,0.0026282878,0.0038669582,0.0000075631992,0.000056729303],"about_ca_topic_score_codex":0.004917437,"about_ca_topic_score_gemma":0.0027476647,"teacher_disagreement_score":0.18794021,"about_ca_system_score_codex":0.0000036248712,"about_ca_system_score_gemma":0.000026253574,"threshold_uncertainty_score":0.7433727},"labels":[],"label_agreement":null},{"id":"W2133569200","doi":"10.1073/pnas.0510489103","title":"Carbon under extreme conditions: Phase boundaries and electronic properties from first-principles theory","year":2006,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":220,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Uranus; Diamond; Phase diagram; Phase boundary; Carbon fibers; Materials science; Melting point; Chemical physics; Triple point; Phase (matter); Condensed matter physics; Thermodynamics; Chemistry; Physics; Planet; Astrophysics; Quantum mechanics","score_opus":0.03958058187513419,"score_gpt":0.24523381216492093,"score_spread":0.20565323028978674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133569200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930133,0.0011376298,5.5046354e-7,0.00090415875,0.00002931552,0.00011966225,0.00011591381,0.000010767292,0.004668677],"genre_scores_gemma":[0.9995241,0.000040917297,0.00009998574,0.00007917909,0.000106588544,0.0000025514623,0.0000020503612,0.0000014499631,0.00014318105],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99890006,0.000010072506,0.00022076504,0.0001861165,0.0005213725,0.00016162383],"domain_scores_gemma":[0.99955446,0.000107829765,0.00022055607,0.000007476631,0.00008957424,0.000020137626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063769723,0.00008542376,0.00013118614,0.000060296763,0.00040889278,0.00011549929,0.00032686215,0.00004599707,0.0001066021],"category_scores_gemma":[0.00008306574,0.00005161907,0.000029063634,0.000186862,0.0014258422,0.00034921613,0.000032357875,0.000068819805,0.0000012645712],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010611615,0.00007930103,0.02629813,0.00009275282,0.000054275002,1.6122518e-8,0.00046130517,0.00241002,0.24461482,0.72530913,0.00034922277,0.00022492472],"study_design_scores_gemma":[0.00023521758,0.00005795764,0.18440196,0.00005622479,0.000023469987,0.000002038291,0.00017500209,0.0029236062,0.094024256,0.7168352,0.0011629045,0.000102165424],"about_ca_topic_score_codex":0.0008281471,"about_ca_topic_score_gemma":0.00002149335,"teacher_disagreement_score":0.15810382,"about_ca_system_score_codex":0.0000043406603,"about_ca_system_score_gemma":0.00005259096,"threshold_uncertainty_score":0.5253575},"labels":[],"label_agreement":null},{"id":"W2133569395","doi":"10.1016/j.tecto.2009.05.030","title":"Body-wave tomography of western Canada","year":2009,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Subduction; Seismology; Transition zone; Mantle (geology); Batholith; Hotspot (geology); Slab window; Transform fault; Magmatism; Lithosphere; Seismic tomography; Plate tectonics; Seismogram; Volcanism; Convergent boundary; Geophysics; Tectonics; Oceanic crust","score_opus":0.007327553563681519,"score_gpt":0.17479568126461792,"score_spread":0.1674681277009364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133569395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928474,0.0000807883,0.000040152532,0.00009369059,0.0003217458,0.00009515663,0.00018455581,0.000029614665,0.006306926],"genre_scores_gemma":[0.99931324,0.000008056799,0.00013967241,0.00022881372,0.00016476371,3.0160845e-7,0.000053868534,0.0000025546829,0.000088760535],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991944,0.000023811312,0.00017956049,0.00015739839,0.00022072477,0.0002241453],"domain_scores_gemma":[0.99952835,0.00003350534,0.000095112235,0.00022550035,0.000041224055,0.00007629731],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057968744,0.000120984034,0.00022155938,0.000027660622,0.000051969735,0.000022120013,0.00015063939,0.00003121099,0.00023693923],"category_scores_gemma":[0.000003830189,0.000103512524,0.000050226252,0.00018545976,0.000030647057,0.000091505986,0.0000059554854,0.000056599656,0.000021280295],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005729439,0.0006314812,0.30651572,0.0004993361,0.0006902503,0.00040303118,0.0017148169,0.0118630715,0.2328005,0.013814884,0.027104456,0.4033895],"study_design_scores_gemma":[0.00027842418,0.0002801057,0.93869287,0.000024568499,0.000037150465,0.000002839866,0.000018883393,0.00027806297,0.044608586,0.007285363,0.008160674,0.0003324811],"about_ca_topic_score_codex":0.33649474,"about_ca_topic_score_gemma":0.13618124,"teacher_disagreement_score":0.6321772,"about_ca_system_score_codex":0.0000022779768,"about_ca_system_score_gemma":0.000119737284,"threshold_uncertainty_score":0.8795812},"labels":[],"label_agreement":null},{"id":"W2133675958","doi":"10.5194/se-2-315-2011","title":"Influence of the Ringwoodite-Perovskite transition on mantle convection in spherical geometry as a function of Clapeyron slope and Rayleigh number","year":2011,"lang":"en","type":"article","venue":"Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Environment Research Council; Cardiff University","keywords":"Mantle convection; Ringwoodite; Geology; Rayleigh number; Convection; Transition zone; Mantle (geology); Geophysics; Phase transition; Natural convection; Thermodynamics; Tectonics; Physics; Subduction; Seismology","score_opus":0.00825796178718896,"score_gpt":0.19246666213976904,"score_spread":0.18420870035258008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133675958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963728,0.000018729308,0.000019547122,0.000014234624,0.00017966451,0.00012283516,0.000024992774,0.0000076149627,0.0032395727],"genre_scores_gemma":[0.99976176,0.000026048132,0.00005495533,0.00006481843,0.000033740187,9.0337664e-7,0.000007480028,0.000002482148,0.000047791902],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99935097,0.00006990846,0.00018026622,0.00013628973,0.00014178458,0.000120807046],"domain_scores_gemma":[0.9997085,0.000029266977,0.00008678612,0.00011688612,0.000026805163,0.00003178765],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014235095,0.00007730876,0.00015379781,0.00002977865,0.00003929179,0.000008513221,0.00006101885,0.00005675921,0.00091349485],"category_scores_gemma":[0.0000121697985,0.000055212175,0.00002939842,0.00016744203,0.00007960616,0.00013458834,0.000006376395,0.000074102034,0.000059923077],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025187489,0.00037378166,0.81536245,0.0004597262,0.00012374176,0.00001434661,0.0076432936,0.036392704,0.11331268,0.0021278746,0.00008961406,0.021581056],"study_design_scores_gemma":[0.000248612,0.00023238666,0.97693443,0.00004329425,0.0000134264765,0.0000028055078,0.000049390987,0.00016827346,0.02124421,0.00085619424,0.00014112213,0.00006584672],"about_ca_topic_score_codex":0.0028277435,"about_ca_topic_score_gemma":0.0004197925,"teacher_disagreement_score":0.16157201,"about_ca_system_score_codex":9.897125e-7,"about_ca_system_score_gemma":0.000015479303,"threshold_uncertainty_score":0.9999998},"labels":[],"label_agreement":null},{"id":"W2133956049","doi":"10.1139/e98-088","title":"Teleseismic studies of the lithosphere below the Abitibi-Grenville Lithoprobe transect","year":2000,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université du Québec à Montréal; Polytechnique Montréal; Geological Survey of Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Polytechnique Montréal; New Mexico State University","keywords":"Geology; Lithosphere; Receiver function; Seismology; Crust; Archean; Anisotropy; Magnetotellurics; Mantle (geology); Seismic anisotropy; Geophysics; Transect; Tectonics; Petrology; Paleontology; Electrical resistivity and conductivity","score_opus":0.019262946180558255,"score_gpt":0.21343484969406734,"score_spread":0.19417190351350908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133956049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987356,0.005472031,0.0000015723167,0.0017355862,0.0007435166,0.000102317565,0.00008298209,0.0000017820784,0.004504231],"genre_scores_gemma":[0.9985311,0.00026576422,0.00016546181,0.00028054137,0.00017943064,2.262358e-7,4.8343475e-7,0.0000019191089,0.0005750801],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987229,0.00014697542,0.00033430624,0.00012465156,0.00033479242,0.00033635864],"domain_scores_gemma":[0.9991919,0.00016538972,0.00018243451,0.00015950363,0.000100268226,0.00020050751],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010453622,0.00010832634,0.00023439249,0.000047993974,0.0006811195,0.00013649589,0.0007734066,0.00003341485,0.0033115875],"category_scores_gemma":[0.00007313088,0.00004983615,0.00012134017,0.0004306435,0.0010755905,0.00022507593,0.00000403372,0.00012921261,0.000026596052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009448899,0.000042830958,0.6210497,0.0001664251,0.00043813736,0.00016374992,0.023349622,0.07428963,0.001549981,0.0017590823,0.0071965875,0.2698998],"study_design_scores_gemma":[0.00023316074,0.00041499687,0.908341,0.00019711851,0.000056686706,0.00012727873,0.0016248316,0.00020304827,0.0011966809,0.0032839926,0.08412769,0.00019353814],"about_ca_topic_score_codex":0.025089772,"about_ca_topic_score_gemma":0.27145776,"teacher_disagreement_score":0.2872913,"about_ca_system_score_codex":0.0000010325854,"about_ca_system_score_gemma":0.0007938227,"threshold_uncertainty_score":0.99759954},"labels":[],"label_agreement":null},{"id":"W2134654661","doi":"10.1029/2003jb002405","title":"Structure of the crust in the vicinity of the Banggong‐Nujiang suture in central Tibet from INDEPTH magnetotelluric data","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada","funders":"","keywords":"Geology; Crust; Terrane; Magnetotellurics; Subduction; Lithosphere; Seismology; Mantle (geology); Underplating; Batholith; Fibrous joint; Tectonics; Geophysics; Petrology; Electrical resistivity and conductivity","score_opus":0.033656859149668907,"score_gpt":0.2872264206256238,"score_spread":0.2535695614759549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134654661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968502,0.00055243936,0.0000015823548,0.0012966802,0.0002937812,0.00023104268,0.000462891,0.0000012557961,0.00031011604],"genre_scores_gemma":[0.9988473,0.00007306466,0.00015527554,0.00008676816,0.00074586197,2.2303229e-7,0.000014231325,0.00000472801,0.00007251429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99634475,0.0010787797,0.00053949386,0.0001933737,0.0013847743,0.000458847],"domain_scores_gemma":[0.99779296,0.0009043975,0.00031922123,0.00074625824,0.00014932748,0.000087855784],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010236935,0.00014019106,0.00036791994,0.000020378568,0.000111865,0.00007395092,0.0026117556,0.000100632926,0.00093176094],"category_scores_gemma":[0.00042036566,0.0000604264,0.00011610574,0.000808388,0.00034640642,0.00031897423,0.00022764676,0.0010442488,0.000007644017],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012477172,0.0007684902,0.863675,0.00017648164,0.00019817818,0.000075389864,0.005394105,0.0153899975,0.03823875,0.0007102805,0.013367824,0.060757767],"study_design_scores_gemma":[0.00038713586,0.00012741191,0.9888742,0.000100717734,0.000017154292,0.000003301585,0.00041359567,0.0009572077,0.002873943,0.0037258577,0.0024520839,0.000067365065],"about_ca_topic_score_codex":0.021101177,"about_ca_topic_score_gemma":0.026545452,"teacher_disagreement_score":0.12519921,"about_ca_system_score_codex":0.000011946465,"about_ca_system_score_gemma":0.00031250497,"threshold_uncertainty_score":0.9999815},"labels":[],"label_agreement":null},{"id":"W2134681638","doi":"10.1103/physreve.64.035401","title":"Results on the energy-relaxation rates of dense two-temperature aluminum, carbon, and silicon plasmas close to liquid-metal conditions","year":2001,"lang":"en","type":"article","venue":"Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Relaxation (psychology); Silicon; Ion; Plasma; Atomic physics; Electron; Coupling (piping); Coupling constant; Materials science; Condensed matter physics; Aluminium; Carbon fibers; Physics; Quantum mechanics","score_opus":0.011312661889289609,"score_gpt":0.28679028427765463,"score_spread":0.27547762238836504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134681638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894672,0.0012774823,0.000047331483,0.0023162172,0.0005189905,0.0004971884,0.0012122643,0.000036984027,0.0046263295],"genre_scores_gemma":[0.99539614,0.0027022671,0.000075598226,0.00034609338,0.00047013076,0.000015968482,0.0006266982,0.00001570993,0.00035136976],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99769884,0.0002998327,0.00068744103,0.000590716,0.00034820882,0.00037498053],"domain_scores_gemma":[0.99804944,0.0009646712,0.00021363654,0.0003744115,0.00013130285,0.0002665246],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00027338354,0.00037987382,0.0007214283,0.000048596045,0.00031424203,0.00007077125,0.00021495872,0.00010474584,0.00010978202],"category_scores_gemma":[0.0002281505,0.0002517729,0.00011901135,0.00024449243,0.00040901374,0.00016140002,0.00014422687,0.00034836988,0.00004967813],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004910018,0.0020119317,0.00132159,0.002181508,0.0015021118,0.00037545364,0.007049369,0.0030074408,0.07508403,0.81821,0.03331671,0.05102986],"study_design_scores_gemma":[0.00653589,0.01445542,0.07407042,0.007913126,0.0026189338,0.00023768005,0.0009199926,0.0650093,0.06344626,0.74518096,0.015385519,0.0042264997],"about_ca_topic_score_codex":0.00019386219,"about_ca_topic_score_gemma":0.00009429673,"teacher_disagreement_score":0.07302902,"about_ca_system_score_codex":0.000009395967,"about_ca_system_score_gemma":0.000041000738,"threshold_uncertainty_score":0.99999344},"labels":[],"label_agreement":null},{"id":"W2134702148","doi":"10.1073/pnas.0805601105","title":"Inelastic x-ray scattering of dense solid oxygen: Evidence for intermolecular bonding","year":2008,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Intermolecular force; Crystallography; Solid oxygen; Delocalized electron; Chemical physics; Synchrotron; Molecule; Chemistry; Molecular solid; Chemical bond; Phase (matter); Oxygen; Materials science; Physics","score_opus":0.07077641488510383,"score_gpt":0.3006463085427192,"score_spread":0.22986989365761534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134702148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99858373,0.00022867929,0.000013048459,0.0005172145,0.00005678249,0.00016193606,0.000033626002,0.0000053931753,0.00039961323],"genre_scores_gemma":[0.9977629,0.000032854794,0.0019817466,0.00008224866,0.000080325066,0.000002461287,2.2776541e-7,0.0000016811449,0.000055529392],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986601,0.000006171711,0.00034276998,0.00018766806,0.0006488223,0.00015445903],"domain_scores_gemma":[0.9991025,0.00023961831,0.00041897607,0.000009069744,0.00019769555,0.000032176915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009061855,0.000081731196,0.00018960827,0.00011297076,0.00019190699,0.000017191787,0.0006456082,0.00004212468,0.000031895896],"category_scores_gemma":[0.00059661956,0.000054856177,0.00007835794,0.00033712952,0.000654522,0.00042469948,0.000050757724,0.000053084535,0.0000017828313],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037489714,0.000011669738,0.013416202,0.00018418078,0.000016573384,1.8474013e-8,0.0003193279,0.0014346546,0.9818171,0.0023466724,0.00025911126,0.00015696848],"study_design_scores_gemma":[0.00018315199,0.00015264665,0.34883702,0.00053878303,0.00002729165,0.000015203882,0.00008827535,0.005442741,0.6285276,0.015915718,0.00013042314,0.00014112938],"about_ca_topic_score_codex":0.000040648014,"about_ca_topic_score_gemma":2.6867153e-7,"teacher_disagreement_score":0.3532895,"about_ca_system_score_codex":0.0000030522037,"about_ca_system_score_gemma":0.00003546288,"threshold_uncertainty_score":0.24116135},"labels":[],"label_agreement":null},{"id":"W2134897811","doi":"10.1016/j.tecto.2012.12.034","title":"New heat flow measurements in Oman and the thermal state of the Arabian Shield and Platform","year":2013,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Agence Nationale de la Recherche","keywords":"Geology; Lithosphere; Geophysics; Mantle (geology); Precambrian; Plume; Heat flux; Rift; Crust; Shield; Geothermal gradient; Petrology; Mantle plume; Seismology; Heat transfer; Geochemistry; Tectonics; Mechanics","score_opus":0.01314337870226427,"score_gpt":0.17995468835689077,"score_spread":0.1668113096546265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134897811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976615,0.0001306456,0.000009024226,0.00024981945,0.00013771433,0.0003135402,0.000015115053,0.0000076175565,0.0014750819],"genre_scores_gemma":[0.99962217,0.00001983095,0.00011324743,0.00011076402,0.0000557667,0.0000021311473,0.0000030300698,0.0000029999244,0.00007007985],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99936074,0.000043821805,0.00014873648,0.00012226497,0.00015898679,0.00016545976],"domain_scores_gemma":[0.99964535,0.00006703222,0.000047189962,0.0001800011,0.0000142783065,0.00004613369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017202512,0.00010067963,0.00016896654,0.000013739057,0.00007809828,0.000064324806,0.00015918064,0.000023023878,0.00013418478],"category_scores_gemma":[0.000007994355,0.00005074134,0.0000258089,0.000089165136,0.00011746718,0.00016665083,0.0000306402,0.00007805218,0.000016905244],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043754003,0.000070915004,0.28561705,0.00018461353,0.00021333333,0.0000024180606,0.013534767,0.009402314,0.0669851,0.0011930347,0.0006856347,0.6216733],"study_design_scores_gemma":[0.0010569732,0.000056435525,0.9703109,0.000031754957,0.000019040226,9.144289e-7,0.00004832313,0.0033323327,0.008354519,0.016546588,0.000106929634,0.0001352473],"about_ca_topic_score_codex":0.015613068,"about_ca_topic_score_gemma":0.0015628693,"teacher_disagreement_score":0.6846939,"about_ca_system_score_codex":0.0000012551574,"about_ca_system_score_gemma":0.000025015099,"threshold_uncertainty_score":0.99094206},"labels":[],"label_agreement":null},{"id":"W2136361263","doi":"10.1051/0004-6361/201322913","title":"The cooling rate of neutron stars after thermonuclear shell flashes","year":2013,"lang":"en","type":"article","venue":"Astronomy and Astrophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Physics; Astrophysics; Neutron star; Thermonuclear fusion; Power law; Stars; Accretion (finance); Opacity; Nuclear physics; Plasma; Statistics; Quantum mechanics","score_opus":0.003979226729290934,"score_gpt":0.15725117848109804,"score_spread":0.1532719517518071,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136361263","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99873215,0.0001333691,0.00034741708,0.00007139984,0.00015680735,0.00015227274,0.000051245435,0.000011597571,0.0003437202],"genre_scores_gemma":[0.99749327,0.000025016525,0.0021577317,0.00002713265,0.00016337929,0.000003873889,0.000017130606,0.0000053101658,0.00010714779],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9992757,0.000058258356,0.00017311725,0.00015684852,0.0000724253,0.00026367742],"domain_scores_gemma":[0.9995447,0.00008336933,0.000094331335,0.00017173614,0.000035523615,0.00007036425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009084357,0.000128667,0.0001603157,0.000011668124,0.00016158455,0.00013193765,0.00014301273,0.00002497181,0.00036502583],"category_scores_gemma":[0.0000021751355,0.00008399878,0.00004699823,0.00004639468,0.00013235307,0.00024250583,0.0000265196,0.000075943026,0.00016970148],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038256153,0.000055943903,0.027078772,0.000052652093,0.00019763337,0.0000033100237,0.0005867659,0.0051598325,0.04181371,0.0013086039,0.0008232138,0.922537],"study_design_scores_gemma":[0.00032024068,0.00026227802,0.93590254,0.000024516394,0.000040872983,5.8004343e-7,0.0003198889,0.00086506916,0.0036389057,0.0010927288,0.057300497,0.00023191309],"about_ca_topic_score_codex":0.0008342127,"about_ca_topic_score_gemma":0.000028286931,"teacher_disagreement_score":0.9223051,"about_ca_system_score_codex":8.762157e-7,"about_ca_system_score_gemma":0.000016584709,"threshold_uncertainty_score":0.3996777},"labels":[],"label_agreement":null},{"id":"W2138890585","doi":"10.1103/physrevlett.114.157004","title":"High-Pressure Hydrogen Sulfide from First Principles: A Strongly Anharmonic Phonon-Mediated Superconductor","year":2015,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":488,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Engineering and Physical Sciences Research Council; Cambridge Commonwealth Trust; Ministerio de Economía y Competitividad; Partnership for Advanced Computing in Europe AISBL; National Natural Science Foundation of China; Eusko Jaurlaritza; Agence Nationale de la Recherche; Graphene Flagship","keywords":"Anharmonicity; Superconductivity; Condensed matter physics; Phonon; Physics; Zero-point energy; Harmonic; Materials science; Quantum mechanics","score_opus":0.029540819703707862,"score_gpt":0.23753788536959283,"score_spread":0.20799706566588497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138890585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9819065,0.012649075,0.0000075269068,0.0030188716,0.00056813285,0.000497792,0.0011198935,0.00009983598,0.00013237598],"genre_scores_gemma":[0.9926193,0.001573952,0.00019087997,0.0033571108,0.0010675268,0.000017420663,0.0011301724,0.000017903216,0.000025765385],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99770665,0.0002062589,0.0004195968,0.0005743626,0.0005448965,0.0005482161],"domain_scores_gemma":[0.9984661,0.00027120527,0.00016720798,0.00057590933,0.00006118033,0.00045839412],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00028778482,0.00036023892,0.0007881789,0.000032140102,0.00010034929,0.00009367554,0.00059108273,0.00003171642,0.0012754637],"category_scores_gemma":[0.00014675864,0.00027667618,0.00018767707,0.00023358206,0.00011206081,0.00041205526,0.00006102745,0.0002082025,0.0030537217],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009701999,0.0020939119,0.084671244,0.009658812,0.006037499,0.001045168,0.0071823155,0.19392076,0.25327966,0.0018614237,0.42928374,0.009995267],"study_design_scores_gemma":[0.0026744788,0.00042382508,0.04364395,0.0020055827,0.0016764407,0.000008945478,0.00006678941,0.017150162,0.005616328,0.000977579,0.9234203,0.002335578],"about_ca_topic_score_codex":0.006362717,"about_ca_topic_score_gemma":0.00023155528,"teacher_disagreement_score":0.4941366,"about_ca_system_score_codex":0.000010258257,"about_ca_system_score_gemma":0.0000820489,"threshold_uncertainty_score":0.9999685},"labels":[],"label_agreement":null},{"id":"W2140053748","doi":"10.1016/j.epsl.2007.04.053","title":"Predicted elastic properties of the hydrous D phase at mantle pressures: Implications for the anisotropy of subducted slabs near 670-km discontinuity and in the lower mantle","year":2007,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"European Science Foundation; European Commission","keywords":"Bulk modulus; Geology; Anisotropy; Compressibility; Mantle (geology); Subduction; Seismic anisotropy; Thermodynamics; Mineralogy; Geophysics; Physics; Seismology; Optics","score_opus":0.011673153634955639,"score_gpt":0.20944936798505873,"score_spread":0.1977762143501031,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140053748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965509,0.00043759952,0.000061546256,0.0013907234,0.00021457921,0.0006003949,0.000690936,0.000006415356,0.00004687784],"genre_scores_gemma":[0.99941033,0.000037546455,0.00011582078,0.00030864115,0.000051994,0.0000025879128,0.00004118294,0.000002079349,0.000029812229],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99892074,0.00006200327,0.00024082561,0.00022928903,0.00024018985,0.00030692434],"domain_scores_gemma":[0.9992016,0.00030561432,0.00012743771,0.0002876201,0.000024238268,0.000053489002],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007269392,0.00011457766,0.00015684156,0.000039297563,0.00044984583,0.0000766705,0.00043481347,0.000029264587,0.000038426442],"category_scores_gemma":[0.00004892107,0.00005343696,0.000028531587,0.00023859176,0.0011183532,0.00018500304,0.000034403303,0.000080512174,0.0000016253933],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011785203,0.000115595896,0.5513811,0.00021936074,0.000069925285,0.000009442687,0.0053429664,0.004022738,0.4298218,0.00013637962,0.001340891,0.006361253],"study_design_scores_gemma":[0.00038609278,0.00014383506,0.99016845,0.000025473448,0.00003659385,0.000014368638,0.00008231072,0.003004702,0.0038215898,0.00005451855,0.0021753146,0.00008675273],"about_ca_topic_score_codex":0.0023604706,"about_ca_topic_score_gemma":0.0042376546,"teacher_disagreement_score":0.4387873,"about_ca_system_score_codex":0.0000010315247,"about_ca_system_score_gemma":0.00003509488,"threshold_uncertainty_score":0.4120619},"labels":[],"label_agreement":null},{"id":"W2140368641","doi":"10.1002/2014jb011352","title":"Plagioclase preferred orientation and induced seismic anisotropy in mafic igneous rocks","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Mafic; Plagioclase; Geology; Gabbro; Pyroxene; Geochemistry; Anorthosite; Layered intrusion; Igneous rock; Amphibole; Ultramafic rock; Petrology; Olivine; Quartz","score_opus":0.03118887681411533,"score_gpt":0.306215153947378,"score_spread":0.2750262771332627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140368641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986857,0.00004552917,0.00013481556,0.00019456874,0.0002512057,0.00015729904,0.00002471968,0.000007194568,0.0004989414],"genre_scores_gemma":[0.9989338,0.00007861124,0.00018722206,0.000053340988,0.00059695035,9.819514e-7,0.00001649361,0.000006325211,0.00012627165],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99749315,0.00052065763,0.00041596475,0.00023467852,0.00083290593,0.0005026223],"domain_scores_gemma":[0.99862915,0.00048365557,0.00016591517,0.00017163409,0.00023808108,0.00031153433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013203351,0.00013938075,0.00038494455,0.00024981392,0.0001490362,0.00017684276,0.00024211816,0.00008841529,0.0001408672],"category_scores_gemma":[0.0003426394,0.00010739996,0.000062529965,0.00032711952,0.000104678846,0.00037286626,0.00003764015,0.0005320679,0.0000980801],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009292572,0.0020121285,0.10447311,0.0008715915,0.00051217957,0.0018187084,0.0092149135,0.048580825,0.38078722,0.0051413034,0.0067505604,0.43054488],"study_design_scores_gemma":[0.0032111616,0.005448019,0.8747994,0.0002375528,0.000035252204,0.00010336228,0.00030774093,0.058250614,0.013487007,0.036740676,0.0068956516,0.00048359093],"about_ca_topic_score_codex":0.002024878,"about_ca_topic_score_gemma":0.00036190925,"teacher_disagreement_score":0.77032626,"about_ca_system_score_codex":0.0000067552483,"about_ca_system_score_gemma":0.00013589357,"threshold_uncertainty_score":0.43796432},"labels":[],"label_agreement":null},{"id":"W2140928176","doi":"10.1093/mnras/stt113","title":"Light-curve analysis and orbital period change of the extreme mass-ratio overcontact binary AW CrB","year":2013,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Los Alamos National Laboratory; Science and Technology Facilities Council; Queen's University; University of Leicester; National Science Foundation; University of Cambridge; Keele University; Queen's University Belfast; University of Michigan; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Physics; Light curve; Contact binary; Astrophysics; Mass ratio; Orbital period; Binary number; Asymmetry; Coalescence (physics); Astronomy; Stars; Binary star; Low Mass","score_opus":0.011508381209488633,"score_gpt":0.18142616210692764,"score_spread":0.169917780897439,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140928176","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981066,0.00017786487,0.0000044396456,0.0007145413,0.0002370057,0.00027296183,0.00023078888,0.000007434903,0.00024835014],"genre_scores_gemma":[0.9991912,4.2788545e-7,0.00047919224,0.000031220898,0.00014189247,0.0000044330504,0.00001732666,0.0000038773474,0.00013038483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99895525,0.00010320441,0.00029343806,0.00021799857,0.00019890649,0.00023120567],"domain_scores_gemma":[0.999241,0.000079385485,0.00026619015,0.00030267055,0.000037628688,0.00007313165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018356944,0.00015229706,0.00034592536,0.000012840137,0.00016169151,0.00007814294,0.00041034867,0.000078529265,0.0007884786],"category_scores_gemma":[0.000012687445,0.00008330432,0.00039866686,0.0001318054,0.00014686951,0.0002056299,0.000101304635,0.000103170336,0.000013655611],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028769984,0.000048596743,0.90960544,0.000039208717,0.00053098483,1.1775205e-7,0.0010446092,0.08606913,0.0017573818,0.0000210832,0.00038749102,0.00046717972],"study_design_scores_gemma":[0.00013296284,0.000053977066,0.88271356,0.000010000731,0.00022800121,5.7002816e-9,0.00017030409,0.1156734,0.0007722196,0.000022335753,0.00013221081,0.00009101634],"about_ca_topic_score_codex":0.013360969,"about_ca_topic_score_gemma":0.0007411545,"teacher_disagreement_score":0.029604267,"about_ca_system_score_codex":0.0000058956266,"about_ca_system_score_gemma":0.000021007578,"threshold_uncertainty_score":0.9932091},"labels":[],"label_agreement":null},{"id":"W2140945940","doi":"10.1016/j.epsl.2009.12.005","title":"On the Vp/Vs–Mg# correlation in mantle peridotites: Implications for the identification of thermal and compositional anomalies in the upper mantle","year":2009,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada; European Social Fund; Macquarie University","keywords":"Mantle (geology); Geology; Lithosphere; Transition zone; Spinel; Geophysics; Mineralogy; Petrology; Seismology; Tectonics","score_opus":0.009475594619802812,"score_gpt":0.20229576269455318,"score_spread":0.19282016807475036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140945940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9832863,0.00012854129,0.00007117762,0.015794186,0.000087562476,0.000323985,0.00015961735,0.0000031023071,0.00014548095],"genre_scores_gemma":[0.9976152,0.000027690538,0.0000708964,0.0021271629,0.000039158756,0.0000031146706,0.000106403466,7.542632e-7,0.000009578867],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933106,0.000057401783,0.00016218047,0.00015466647,0.0001445352,0.00015016976],"domain_scores_gemma":[0.9992422,0.0005256259,0.000066235276,0.0001365495,0.000010202761,0.000019219375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007145062,0.00006815554,0.00007249432,0.000058724687,0.00030701392,0.00010973026,0.00021033104,0.000017243881,0.000049484443],"category_scores_gemma":[0.00001845174,0.000034845834,0.000013650389,0.00015773889,0.0002612337,0.00018843771,0.0000044429994,0.00006433131,0.000006792269],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026353283,0.000059165886,0.8001542,0.000029950777,0.00001365197,0.0000033404995,0.0039567063,0.05801744,0.1069492,0.016806785,0.0012458358,0.012500181],"study_design_scores_gemma":[0.000097504795,0.00005802755,0.98690265,0.000008499118,0.00000491378,0.0000053979948,0.000081608116,0.011616496,0.00016264922,0.0007139651,0.00029929055,0.000048963473],"about_ca_topic_score_codex":0.0003082407,"about_ca_topic_score_gemma":0.00020773266,"teacher_disagreement_score":0.18674847,"about_ca_system_score_codex":8.186475e-7,"about_ca_system_score_gemma":0.000013420729,"threshold_uncertainty_score":0.2361334},"labels":[],"label_agreement":null},{"id":"W2141008939","doi":"10.1111/j.1365-246x.2006.03131.x","title":"Models of large-scale viscous flow in the Earth's mantle with constraints from mineral physics and surface observations","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":332,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geoid; Mantle (geology); Geology; Geophysics; Lithosphere; Mantle convection; Transition zone; Viscosity; Heat flux; Physics; Mechanics; Thermodynamics; Heat transfer; Tectonics; Seismology","score_opus":0.013772406608217533,"score_gpt":0.21030308087632493,"score_spread":0.19653067426810739,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141008939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99327356,0.000031565003,0.003811674,0.0004492448,0.00020556337,0.00006972952,0.00071332767,0.0000049533924,0.0014404075],"genre_scores_gemma":[0.9951102,0.0000101300075,0.003963151,0.000098851095,0.0005320587,5.753431e-7,0.00018957455,0.0000032382986,0.000092220645],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990188,0.000065352804,0.00022731921,0.00013822639,0.00037721128,0.00017312812],"domain_scores_gemma":[0.9995255,0.00013180853,0.00012074112,0.00008634605,0.000095917625,0.000039721173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015263949,0.00010627229,0.00016552793,0.000020370413,0.00008708456,0.00011725543,0.00021683861,0.000030302299,0.0002149701],"category_scores_gemma":[0.0000042590273,0.00006776596,0.000044125314,0.00008473141,0.00012256062,0.00033134242,0.000014265236,0.00014773021,0.000011671393],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042911843,0.0009807221,0.22637229,0.00002668001,0.000294057,0.0001977343,0.0029521862,0.7084137,0.022178164,0.026483616,0.0023573905,0.009314336],"study_design_scores_gemma":[0.0009923001,0.00008763196,0.7824927,0.00005244466,0.0000298265,0.000033056698,0.000199296,0.15246914,0.00056253973,0.062402282,0.00050012616,0.00017867002],"about_ca_topic_score_codex":0.001993779,"about_ca_topic_score_gemma":0.0014452965,"teacher_disagreement_score":0.5561204,"about_ca_system_score_codex":0.000002086111,"about_ca_system_score_gemma":0.000033635333,"threshold_uncertainty_score":0.3014011},"labels":[],"label_agreement":null},{"id":"W2141312907","doi":"10.1093/gji/ggu375","title":"Lg attenuation in northeast China using NECESSArray data","year":2014,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Apache (Canada)","funders":"","keywords":"Geology; Structural basin; Attenuation; Volcano; Seismology; Volcanism; Sedimentary rock; Sedimentary basin; Geomorphology; Tectonics; Paleontology","score_opus":0.027482569787229977,"score_gpt":0.265119126785914,"score_spread":0.237636556998684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141312907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908811,0.000014934077,0.003495218,0.00076720444,0.0019069348,0.000052811905,0.00014835672,0.0000118850785,0.0027215641],"genre_scores_gemma":[0.9962571,0.000010693257,0.0008741728,0.00012801576,0.0023161648,2.3071249e-7,0.00033044835,0.0000043810733,0.0000787438],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986853,0.00011275776,0.0003000919,0.00023334922,0.00044177574,0.00022672066],"domain_scores_gemma":[0.99938244,0.00006673408,0.00016252813,0.00021658398,0.00006748412,0.00010421944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004791693,0.000116944146,0.00017043833,0.0000906204,0.00011694893,0.00023095413,0.0007019183,0.000040922714,0.0010659203],"category_scores_gemma":[0.000074439,0.00009549341,0.0000438818,0.000110584275,0.000038640217,0.00073190866,0.00005705864,0.00020693346,0.00022997161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039383472,0.0004736036,0.6443317,0.000037610465,0.00027587172,0.00012339385,0.0007465952,0.07908574,0.013283584,0.0052864077,0.0029435167,0.25301817],"study_design_scores_gemma":[0.00041717163,0.000041739193,0.80533314,0.00003793516,0.000013327705,0.000046879857,0.000015555572,0.17930867,0.00007217188,0.0080723595,0.0064779357,0.00016312665],"about_ca_topic_score_codex":0.0017948502,"about_ca_topic_score_gemma":0.00041156402,"teacher_disagreement_score":0.25285503,"about_ca_system_score_codex":0.000007780077,"about_ca_system_score_gemma":0.000042314856,"threshold_uncertainty_score":0.99984723},"labels":[],"label_agreement":null},{"id":"W2141592070","doi":"10.1139/e00-116","title":"On the possibility of anisotropic heat flow in the inner core","year":2001,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Alexander von Humboldt-Stiftung","keywords":"Anisotropy; Thermal conductivity; Materials science; Condensed matter physics; Inner core; Electrical resistivity and conductivity; Conductivity; Atmospheric temperature range; Thermodynamics; Composite material; Chemistry; Physics; Optics","score_opus":0.028413774839814342,"score_gpt":0.22124807501887558,"score_spread":0.19283430017906125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141592070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99433345,0.00016535555,0.0000025116099,0.0013746774,0.00037758125,0.000068959846,0.00008785496,7.089538e-7,0.0035889123],"genre_scores_gemma":[0.9992927,0.000013655113,0.00007893489,0.0004815749,0.00009366688,1.4613246e-7,0.0000019472955,6.764606e-7,0.00003670937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999051,0.00012200023,0.00022909825,0.00009087666,0.00026967234,0.00023737043],"domain_scores_gemma":[0.9993038,0.00029312668,0.00009142509,0.00013026239,0.000052880467,0.00012846077],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012527178,0.00006466672,0.00012970946,0.000098101875,0.00023555577,0.00010308493,0.0005579861,0.000023593928,0.0042247586],"category_scores_gemma":[0.00016120568,0.000029083489,0.000043885582,0.00041549103,0.00039442175,0.00014758222,0.0000025528448,0.00010729842,0.000021209227],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003787892,0.00002157345,0.9683859,0.000009388091,0.0000139206495,0.00016783908,0.002798634,0.016815545,0.00017757008,0.0038297477,0.004003025,0.0037390012],"study_design_scores_gemma":[0.000089882866,0.00034504375,0.98384994,0.000036522324,0.0000043960654,0.00004008755,0.00047851785,0.0007615922,0.00005753962,0.006669378,0.0076102833,0.00005683115],"about_ca_topic_score_codex":0.027788946,"about_ca_topic_score_gemma":0.3746604,"teacher_disagreement_score":0.34687147,"about_ca_system_score_codex":8.405881e-7,"about_ca_system_score_gemma":0.0005082826,"threshold_uncertainty_score":0.9966855},"labels":[],"label_agreement":null},{"id":"W2142358311","doi":"10.1111/j.1365-246x.2011.05245.x","title":"The rotational stability of a convecting earth: assessing inferences of rapid TPW in the late cretaceous","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mantle convection; Lithosphere; Mantle (geology); Geology; Geophysics; Amplitude; Convection; Forcing (mathematics); Physics; Mechanics; Atmospheric sciences; Paleontology; Tectonics; Quantum mechanics","score_opus":0.043344781929186386,"score_gpt":0.257849454891379,"score_spread":0.2145046729621926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142358311","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938535,0.000065787855,0.00010829199,0.00021367516,0.00061067595,0.000072786424,0.000037329515,0.000003150816,0.005034772],"genre_scores_gemma":[0.9994245,0.000033639302,0.00026908124,0.00003474971,0.0002058329,0.0000010092506,0.000010084994,0.0000016776936,0.000019404268],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998562,0.00025710542,0.00043766768,0.00009135291,0.0004919257,0.00015997973],"domain_scores_gemma":[0.99856025,0.00073244516,0.000360035,0.00009895865,0.00021241297,0.00003589686],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000998556,0.00008507537,0.00015976741,0.000041275616,0.0001456779,0.000119519624,0.00047043167,0.000028698896,0.0009386982],"category_scores_gemma":[0.00016106312,0.00004592382,0.000090176756,0.00011395434,0.00018258004,0.00030582095,0.000021045451,0.0002040478,0.000013164423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009362016,0.0008056594,0.717155,0.00008171833,0.0006300583,0.00007004673,0.022105215,0.0020651943,0.027465694,0.021678783,0.00018111491,0.20682532],"study_design_scores_gemma":[0.00022746672,0.000119703654,0.9719117,0.000035170793,0.000012898287,0.000016117381,0.0008152303,0.0018457618,0.0042075957,0.020386146,0.0003487209,0.000073431576],"about_ca_topic_score_codex":0.0007847662,"about_ca_topic_score_gemma":0.00023520926,"teacher_disagreement_score":0.25475675,"about_ca_system_score_codex":0.000002414689,"about_ca_system_score_gemma":0.000089761335,"threshold_uncertainty_score":0.9999746},"labels":[],"label_agreement":null},{"id":"W2142761168","doi":"10.1039/c5ra06998j","title":"Prediction of novel crystal structures and superconductivity of compressed HBr","year":2015,"lang":"en","type":"article","venue":"RSC Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saskatoon Medical Imaging; University of Saskatchewan","funders":"","keywords":"Superconductivity; Materials science; Crystal (programming language); Crystal structure; Crystallography; Chemistry; Condensed matter physics; Physics; Computer science","score_opus":0.03633245396488554,"score_gpt":0.2349075157302461,"score_spread":0.19857506176536055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142761168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99672616,0.0011530991,0.00030326162,0.000011222368,0.00036378112,0.000073500705,0.00077408185,0.000010480552,0.0005843975],"genre_scores_gemma":[0.99836195,0.000058220165,0.0014542559,0.0000036297722,0.00006797191,3.1177228e-7,0.00003964208,0.0000014257415,0.000012583086],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994894,0.00002431506,0.0001377195,0.000113455964,0.00014856293,0.00008649369],"domain_scores_gemma":[0.9996847,0.00004550879,0.00007843552,0.00008546481,0.000052989446,0.000052927975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000103148275,0.000065614106,0.0001727624,0.00002378537,0.000024806823,0.000009347172,0.00006697873,0.000028146638,0.00007627458],"category_scores_gemma":[0.00002403489,0.000049968483,0.000015301785,0.000048537015,0.00011557936,0.00034923648,0.000010133543,0.000027006401,7.128594e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034413513,0.0001312745,0.27284527,0.0005484715,0.000086486354,0.0000023065961,0.0017272293,0.025979204,0.68090403,0.0029531475,0.0003451026,0.014133357],"study_design_scores_gemma":[0.0017856306,0.00057545956,0.8485895,0.00006781243,0.00006125625,0.00001212561,0.000742153,0.0038520794,0.11719909,0.01367367,0.013167232,0.00027398905],"about_ca_topic_score_codex":0.00086932845,"about_ca_topic_score_gemma":0.00016409608,"teacher_disagreement_score":0.5757442,"about_ca_system_score_codex":5.5913586e-7,"about_ca_system_score_gemma":0.000020001753,"threshold_uncertainty_score":0.20376556},"labels":[],"label_agreement":null},{"id":"W2143944118","doi":"10.1063/1.1703523","title":"An ice phase of lowest thermal conductivity","year":2004,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Vetenskapsrådet","keywords":"Thermal conductivity; Materials science; Phase (matter); Ice crystals; Conductivity; Thermal; Amorphous ice; Hexagonal crystal system; Amorphous solid; Mineralogy; Analytical Chemistry (journal); Thermodynamics; Crystallography; Composite material; Chemistry; Optics; Physics; Physical chemistry; Chromatography","score_opus":0.020561987620124227,"score_gpt":0.2584261557225517,"score_spread":0.23786416810242744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143944118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990313,0.00005664323,0.00023390939,0.000099674355,0.00017604008,0.00003646532,0.000039793296,0.00000384898,0.00032231852],"genre_scores_gemma":[0.9991369,0.000008709575,0.00018182445,0.00005419236,0.00060716504,3.9026627e-8,0.0000064108885,0.0000027017645,0.0000020566176],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993242,0.00005435936,0.00021789125,0.000051967385,0.00022822809,0.00012332246],"domain_scores_gemma":[0.999346,0.00007996614,0.00026308728,0.00014805718,0.000084517495,0.000078333454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030385898,0.00007971588,0.00020621024,0.0000080314785,0.0000317506,0.000014994124,0.0003012762,0.000029585213,0.00011791792],"category_scores_gemma":[0.000013496963,0.000046100093,0.00006351927,0.00007311032,0.00013254672,0.00027924206,0.000007626095,0.00013429786,0.000012160996],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001885637,0.00018432866,0.00012376327,0.000010415032,0.00002819323,0.0000031384498,0.00032226506,0.0044681607,0.9917837,0.00018205585,0.000032053005,0.0026733903],"study_design_scores_gemma":[0.00086328597,0.00031023432,0.0011357826,0.00001877521,0.000066682784,0.0000144771775,0.000034117722,0.000085185195,0.98128176,0.016008647,0.00009883463,0.000082207946],"about_ca_topic_score_codex":0.00016808577,"about_ca_topic_score_gemma":0.0000028051638,"teacher_disagreement_score":0.01582659,"about_ca_system_score_codex":0.0000021483654,"about_ca_system_score_gemma":0.000056279583,"threshold_uncertainty_score":0.18799073},"labels":[],"label_agreement":null},{"id":"W2144870609","doi":"10.1111/j.1365-246x.2006.03002.x","title":"Investigating the lowermost mantle using migrations of long-period<i>S</i>-<i>ScS</i>data","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Scattering; Core–mantle boundary; Slab; Discontinuity (linguistics); Mantle wedge; Transition zone; Seismology; Geophysics; Geometry; Subduction; Physics; Tectonics; Optics; Mathematical analysis","score_opus":0.026854824581526437,"score_gpt":0.2551915321909933,"score_spread":0.22833670760946684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144870609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939371,0.00011587494,0.0011554781,0.0010792125,0.0013712357,0.000078216406,0.0005428672,0.000012291024,0.0017077404],"genre_scores_gemma":[0.99594337,0.000010241662,0.0013068594,0.0001465968,0.0020237416,3.642342e-7,0.00033308112,0.000005049358,0.0002306955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861544,0.00007862349,0.00040484016,0.00018283451,0.0005074558,0.00021080131],"domain_scores_gemma":[0.99909055,0.0001208772,0.00029487282,0.00026092638,0.00016124282,0.00007155631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002937385,0.0001245068,0.00016740937,0.000046708352,0.0002862799,0.00025199464,0.0008439317,0.000037488455,0.0007863136],"category_scores_gemma":[0.000054352226,0.00008326814,0.000082545776,0.00013890435,0.00016509308,0.0004684525,0.00007845573,0.00019075852,0.00007676976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021947731,0.0010208361,0.4296027,0.0001208774,0.0012224092,0.00041264258,0.0015141093,0.14908995,0.2930135,0.017971398,0.06924767,0.03656439],"study_design_scores_gemma":[0.000777015,0.00011349717,0.8618409,0.00015853529,0.0001517503,0.00048444342,0.00015946342,0.086651206,0.007527791,0.026717616,0.014925454,0.00049232313],"about_ca_topic_score_codex":0.0030269825,"about_ca_topic_score_gemma":0.0005056281,"teacher_disagreement_score":0.4322382,"about_ca_system_score_codex":0.0000052368755,"about_ca_system_score_gemma":0.000089646375,"threshold_uncertainty_score":0.8609583},"labels":[],"label_agreement":null},{"id":"W2144871560","doi":"10.1111/j.1365-246x.2006.03225.x","title":"Lateral variations in mantle rheology: implications for convection related surface observables and inferred viscosity models","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Mantle convection; Geoid; Geophysics; Rheology; Observable; Viscosity; Context (archaeology); Seismic tomography; Ocean surface topography; Buoyancy; Convection; Mechanics; Physics; Geodesy; Thermodynamics; Seismology; Tectonics; Lithosphere","score_opus":0.022879990169827353,"score_gpt":0.261856824598175,"score_spread":0.23897683442834763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144871560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9801174,0.00003218688,0.016100008,0.0015657855,0.0009085947,0.00015388722,0.0001784269,0.000019253548,0.0009244826],"genre_scores_gemma":[0.99767715,0.00003953986,0.0014158679,0.00009843569,0.00024699554,0.0000015006517,0.00017735739,0.0000039383945,0.00033919496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909407,0.000041652977,0.0003325681,0.00017697903,0.00012345328,0.00023129836],"domain_scores_gemma":[0.9993351,0.0002228789,0.00013668292,0.000071520575,0.00013691306,0.00009689415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004246281,0.00010152657,0.00015609793,0.000076525226,0.00017852684,0.0001205009,0.00015347174,0.00007542982,0.00014828568],"category_scores_gemma":[0.000032401542,0.00009076401,0.000053461827,0.00010270334,0.000049938564,0.00050489866,0.000019257843,0.00015116116,0.000019726333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000643756,0.000400171,0.5031904,0.00003056997,0.0003811576,0.000026395535,0.0011146319,0.05066729,0.019135838,0.41035542,0.0011021583,0.012952225],"study_design_scores_gemma":[0.00050648005,0.000053346837,0.81148714,0.000011441329,0.000013799427,0.00003586437,0.000012678366,0.04872051,0.00014125851,0.13843648,0.00047830888,0.00010270805],"about_ca_topic_score_codex":0.00078518013,"about_ca_topic_score_gemma":0.0005133,"teacher_disagreement_score":0.30829674,"about_ca_system_score_codex":0.000012888556,"about_ca_system_score_gemma":0.000035089113,"threshold_uncertainty_score":0.3701249},"labels":[],"label_agreement":null},{"id":"W2145553586","doi":"10.1016/s0264-3707(01)00012-6","title":"On the advection of sharp material interfaces in geodynamic problems: entrainment of the D″ layer","year":2001,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Advection; Entrainment (biomusicology); Layer (electronics); Geophysics; Thermodynamics; Materials science; Physics","score_opus":0.008638237623155522,"score_gpt":0.19324675628173285,"score_spread":0.18460851865857733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145553586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975886,0.000044755743,0.000035366487,0.00035980679,0.0010394558,0.00014921886,0.00007908823,0.0000017478251,0.0007019935],"genre_scores_gemma":[0.9996552,0.00012680123,0.00003107377,0.000040090097,0.000082960105,4.3683949e-7,0.0000046074056,0.0000030381143,0.000055815806],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9988427,0.0001240918,0.0005033647,0.00007617235,0.00030303688,0.00015060959],"domain_scores_gemma":[0.9991047,0.0000982301,0.00056239165,0.00014521695,0.00006347348,0.000026019527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006192567,0.0000955658,0.00022153402,0.00006278451,0.00004122886,0.000025592559,0.00032762898,0.000048253067,0.00072983],"category_scores_gemma":[0.00003167494,0.00004825367,0.000079259764,0.00012687412,0.00006668837,0.0001050256,0.00002066435,0.0001318527,0.0000054291954],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026030543,0.00085571414,0.16899145,0.00043072936,0.00048726882,0.000049620263,0.004673287,0.49551633,0.30404747,0.006874567,0.0008144159,0.014656093],"study_design_scores_gemma":[0.0014528997,0.0015534103,0.91844606,0.0008388425,0.00012598318,0.00012495904,0.000767115,0.038876507,0.0138984695,0.021393234,0.0021780361,0.00034449156],"about_ca_topic_score_codex":0.0006217861,"about_ca_topic_score_gemma":0.0012082862,"teacher_disagreement_score":0.7494546,"about_ca_system_score_codex":0.000010008851,"about_ca_system_score_gemma":0.00004200185,"threshold_uncertainty_score":0.7991127},"labels":[],"label_agreement":null},{"id":"W2145568254","doi":"10.1029/2009gl039387","title":"Detection of a ULVZ at the base of the mantle beneath the northwest Pacific","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Subduction; Mantle (geology); Seismology; Slab; Slowness; Pacific Plate; Seismic tomography; Pacific ocean; Geophysics; Tectonics; Oceanography","score_opus":0.019877142993391966,"score_gpt":0.24824349785047187,"score_spread":0.2283663548570799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145568254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99167967,0.00006158229,0.000007521525,0.006992448,0.00017275773,0.00030730502,0.00012602995,0.0000068718255,0.0006458449],"genre_scores_gemma":[0.9991985,0.00001679687,0.0000058813393,0.00031791165,0.00022144357,0.0000033623794,0.000014573108,0.0000029695252,0.00021856652],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9979882,0.00042437355,0.0001889674,0.00020020692,0.0008135317,0.00038469658],"domain_scores_gemma":[0.99866104,0.0005414563,0.000086040534,0.00057051197,0.00008145583,0.000059477214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071363,0.00010193526,0.00015722123,0.000032636915,0.00045805553,0.000047494792,0.00058788265,0.00003262803,0.00021389646],"category_scores_gemma":[0.00008213938,0.000043738633,0.00012457075,0.00042790573,0.0005126231,0.00007579246,0.00006148535,0.00024456182,0.00013525796],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002483253,0.00008853531,0.005082857,0.00003841613,0.000048754013,0.0000075774415,0.0007873899,0.0011374346,0.96689713,0.0004828086,0.0049715387,0.020209238],"study_design_scores_gemma":[0.00021021764,0.00026677255,0.8789204,0.000025373578,0.00002225977,0.0000024534802,0.00014753529,0.00060136634,0.11002605,0.0016130409,0.008054331,0.000110248664],"about_ca_topic_score_codex":0.00684697,"about_ca_topic_score_gemma":0.0016941279,"teacher_disagreement_score":0.8738375,"about_ca_system_score_codex":0.0000058346077,"about_ca_system_score_gemma":0.000033635253,"threshold_uncertainty_score":0.9997665},"labels":[],"label_agreement":null},{"id":"W2145592785","doi":"10.1046/j.1365-246x.2002.01759.x","title":"The lowermost mantle beneath northern Asia-I. Multi-azimuth studies of a D″ heterogeneity","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Slowness; Geology; Seismometer; Seismology; Azimuth; Great circle; Discontinuity (linguistics); Geodesy; Geometry","score_opus":0.04459834567272255,"score_gpt":0.27476988121614027,"score_spread":0.2301715355434177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145592785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99499285,0.0007335471,0.00009877619,0.0008089752,0.0019294545,0.0000745737,0.00014951495,0.000011928067,0.0012003857],"genre_scores_gemma":[0.9977387,0.00044730413,0.00019546416,0.00006367903,0.0008075039,8.5020395e-7,0.000013670834,0.0000046380997,0.0007281646],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99868405,0.00007774185,0.00035357336,0.00016077954,0.00047840815,0.00024544357],"domain_scores_gemma":[0.99904853,0.00019060209,0.00024119127,0.00014910626,0.0002715602,0.0000989799],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002276479,0.00013909736,0.00021451367,0.0000341492,0.00029100745,0.00013510697,0.00047473612,0.000034396362,0.00053856545],"category_scores_gemma":[0.00008007469,0.00008395062,0.00015626842,0.00007578121,0.00016719042,0.00018981512,0.000043150445,0.0001631408,0.00036456183],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011267645,0.002655252,0.38182932,0.00015506393,0.008767939,0.00081185956,0.007830139,0.018502843,0.029438546,0.0095061185,0.023160508,0.5162156],"study_design_scores_gemma":[0.0027069864,0.0008129774,0.8847548,0.0001767009,0.00019191756,0.00030939432,0.00096634805,0.03023792,0.010991461,0.011489293,0.05647354,0.000888669],"about_ca_topic_score_codex":0.00016369316,"about_ca_topic_score_gemma":0.00062844955,"teacher_disagreement_score":0.515327,"about_ca_system_score_codex":0.000007816556,"about_ca_system_score_gemma":0.000015796511,"threshold_uncertainty_score":0.5896914},"labels":[],"label_agreement":null},{"id":"W2145651782","doi":"10.1111/j.1365-246x.2004.02257.x","title":"Stresses induced in continental lithospheres by axisymmetric spherical convection","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Saskatchewan","funders":"","keywords":"Geology; Mantle (geology); Mantle convection; Mechanics; Geophysics; Convection; Continental margin; Plate tectonics; Subduction; Geometry; Physics; Seismology; Tectonics","score_opus":0.008576975976596587,"score_gpt":0.2254087858776004,"score_spread":0.2168318099010038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145651782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945083,0.00009324087,0.00035523018,0.0007059502,0.0019010641,0.000074555755,0.000084240346,0.00002167561,0.0022557175],"genre_scores_gemma":[0.9982728,0.000051568404,0.00034486147,0.00016465224,0.0009172845,0.0000013036615,0.00008554567,0.000005246951,0.00015678014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864054,0.000057175388,0.00033969883,0.00021344883,0.00046922176,0.00027989934],"domain_scores_gemma":[0.99945915,0.00007881348,0.00015005139,0.00007346899,0.00008868114,0.00014981595],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013694295,0.00015172476,0.0002125809,0.00007571721,0.000091924994,0.00024043383,0.00029824406,0.00007056876,0.0018711756],"category_scores_gemma":[0.00006409521,0.0001254637,0.000089593144,0.00025374137,0.00004674751,0.00043380438,0.000021592527,0.00029528458,0.00030793514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019498168,0.0036748757,0.49098352,0.000069642905,0.0009400642,0.0012537363,0.0013766737,0.019219322,0.18409617,0.011617123,0.018125791,0.26669326],"study_design_scores_gemma":[0.0031991848,0.0005516877,0.94330806,0.000092801645,0.00002492407,0.00015505288,0.00021234991,0.0007374165,0.020070666,0.019599697,0.01152382,0.00052431686],"about_ca_topic_score_codex":0.0045538163,"about_ca_topic_score_gemma":0.0003188599,"teacher_disagreement_score":0.45232457,"about_ca_system_score_codex":0.000025405181,"about_ca_system_score_gemma":0.000059758328,"threshold_uncertainty_score":0.99904126},"labels":[],"label_agreement":null},{"id":"W2145819791","doi":"10.1002/2013gc005168","title":"Lithospheric architecture of the Slave craton, northwest Canada, as determined from an interdisciplinary 3‐D model","year":2014,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Craton; Geology; Lithosphere; Kimberlite; Overprinting; Metasomatism; Mantle (geology); Xenolith; Magnetotellurics; Classification of discontinuities; Geochemistry; Seismology; Geophysics; Petrology; Tectonics; Electrical resistivity and conductivity","score_opus":0.0037335790868658195,"score_gpt":0.19482597988853034,"score_spread":0.19109240080166454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145819791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933859,0.00006665111,0.0002026721,0.000111349065,0.00070923107,0.0002143826,0.00186774,0.00003451665,0.0034075552],"genre_scores_gemma":[0.9979556,0.000001666828,0.0001409455,0.000111837646,0.0006654745,0.0000067230485,0.00070482306,0.000013966729,0.00039891902],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99794227,0.0001200483,0.00046820016,0.00051356776,0.00051372265,0.0004421648],"domain_scores_gemma":[0.99812305,0.00012151407,0.0003767147,0.001037761,0.00012620508,0.0002147409],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00016066672,0.00034604585,0.00049111934,0.0000107042715,0.0002735502,0.00007794735,0.00085027784,0.0001319393,0.00028400618],"category_scores_gemma":[0.000024024459,0.00025153824,0.00013455526,0.00018094742,0.0001025041,0.000121414254,0.00014663344,0.00020616438,0.0000235535],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006141002,0.00046146326,0.09883093,0.001959328,0.0007382263,0.00008057062,0.0067830067,0.5056923,0.3291476,0.0003805519,0.0037327614,0.051579177],"study_design_scores_gemma":[0.0017975,0.00044793825,0.25304797,0.0006826967,0.00042199082,0.000056011875,0.0010418848,0.49103567,0.18993247,0.053978607,0.004891959,0.0026653237],"about_ca_topic_score_codex":0.6904217,"about_ca_topic_score_gemma":0.5556471,"teacher_disagreement_score":0.15421703,"about_ca_system_score_codex":0.000011436253,"about_ca_system_score_gemma":0.00041787935,"threshold_uncertainty_score":0.9999937},"labels":[],"label_agreement":null},{"id":"W2146152489","doi":"10.1029/2008jb006217","title":"Shear wave velocity structure of the lower crust in southern Africa: Evidence for compositional heterogeneity within Archaean and Proterozoic terrains","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Prairie Oat Growers Association","keywords":"Geology; Crust; Felsic; Mafic; Proterozoic; Archean; Shear zone; Shear (geology); Geochemistry; Craton; Seismology; Tectonics; Petrology","score_opus":0.06558919030580417,"score_gpt":0.3116959110280747,"score_spread":0.24610672072227052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146152489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983755,0.00023232236,0.000044622084,0.00063919456,0.000118452976,0.00039773562,0.0001584452,0.0000025436639,0.00003122446],"genre_scores_gemma":[0.99774814,0.00001183296,0.0018652293,0.00003993497,0.0002900953,0.0000010440533,0.000002534233,0.0000039079614,0.000037292295],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978593,0.000361701,0.00041092496,0.00019256394,0.000818676,0.0003568235],"domain_scores_gemma":[0.99860525,0.00054075057,0.00022748522,0.0001784728,0.00029644082,0.00015159849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081373286,0.00013088441,0.00033192383,0.000020528762,0.00017237371,0.00007713512,0.0003657774,0.000068704176,0.00010401319],"category_scores_gemma":[0.00034491008,0.0000771662,0.00012122466,0.00022464537,0.00036398155,0.00021751068,0.00004646089,0.00041614936,0.0000026334396],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01448566,0.0018951464,0.090166055,0.00089788536,0.00050967035,0.0002106685,0.017655883,0.01229595,0.79787755,0.0032292479,0.0021609159,0.058615357],"study_design_scores_gemma":[0.0007856812,0.0025749018,0.9399986,0.0004621201,0.000021024494,0.00001991448,0.00028181745,0.0032831174,0.010519264,0.041769437,0.00011840606,0.00016569879],"about_ca_topic_score_codex":0.0010044774,"about_ca_topic_score_gemma":0.0006935414,"teacher_disagreement_score":0.8498326,"about_ca_system_score_codex":0.00001180327,"about_ca_system_score_gemma":0.00017533926,"threshold_uncertainty_score":0.31467465},"labels":[],"label_agreement":null},{"id":"W2146360206","doi":"10.1002/ggge.20179","title":"Buoyancy and localizing properties of continental mantle lithosphere: Insights from thermomechanical models of the eastern Gulf of Aden","year":2013,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Centre National de la Recherche Scientifique; Agence Nationale de la Recherche","keywords":"Geology; Mantle (geology); Lithosphere; Asthenosphere; Seafloor spreading; Mantle wedge; Mid-ocean ridge; Transition zone; Mantle convection; Geophysics; Subduction; Rift; Oceanic crust; Low-velocity zone; Petrology; Seismology; Tectonics","score_opus":0.010769268575345462,"score_gpt":0.16309415436054134,"score_spread":0.15232488578519587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146360206","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968189,0.0015707755,0.00004708417,0.000019599716,0.00026158785,0.00029356833,0.0002952352,0.000011228343,0.00068204023],"genre_scores_gemma":[0.9995973,0.000019094103,0.00003940391,0.000006537443,0.00014587516,0.0000041275666,0.000039606468,0.0000073758542,0.00014068437],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986166,0.00006806776,0.000509032,0.0002611752,0.0003402545,0.00020487813],"domain_scores_gemma":[0.99886006,0.00006476328,0.00042839377,0.0004235773,0.00015429694,0.000068915564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000073927404,0.00019526915,0.00049250625,0.000009924882,0.000064981126,0.000041467778,0.00036320667,0.00010986807,0.00013817473],"category_scores_gemma":[0.000013430175,0.0001260223,0.00010125788,0.0001001248,0.0001916255,0.00017763299,0.00009517835,0.00008721494,0.000014402669],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047436195,0.000072285584,0.011997998,0.0009356025,0.00014633051,0.0000010547125,0.0011124879,0.0008324956,0.9835817,0.0001973755,0.000051042935,0.0010241801],"study_design_scores_gemma":[0.0007040426,0.00008788898,0.013205461,0.0010438085,0.00010564408,0.0000040744517,0.0011140915,0.039208815,0.93024,0.013822992,0.000085738364,0.00037746047],"about_ca_topic_score_codex":0.03675976,"about_ca_topic_score_gemma":0.00011545117,"teacher_disagreement_score":0.053341728,"about_ca_system_score_codex":0.0000018996935,"about_ca_system_score_gemma":0.0000474103,"threshold_uncertainty_score":0.96965456},"labels":[],"label_agreement":null},{"id":"W2147111500","doi":"10.1134/s0016702906020017","title":"Endogenic cycles and the problem of crustal growth","year":2006,"lang":"en","type":"article","venue":"Geochemistry International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Russian Foundation for Basic Research","keywords":"Geology; Earth science; Geochemistry; Astrobiology; Petrology; Paleontology; Biology","score_opus":0.0035377670518376265,"score_gpt":0.17363855899860697,"score_spread":0.17010079194676936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147111500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93721205,0.0001407209,0.000022091488,0.0004267644,0.00009743869,0.000051204603,0.00025610093,0.000009308457,0.06178435],"genre_scores_gemma":[0.9988059,0.000017914941,0.0003026334,0.000020667376,0.00022931873,0.0000013285618,0.00017108493,0.0000010663655,0.00045008902],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995312,0.000011429979,0.00013157995,0.00009526364,0.00014943027,0.00008106722],"domain_scores_gemma":[0.99975336,0.000057984438,0.000070236696,0.00005424774,0.00004785426,0.000016297527],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010331939,0.00005560895,0.00007703758,0.000009506185,0.0000374568,0.000034331435,0.00014583199,0.000023901854,0.0012003828],"category_scores_gemma":[0.000008679395,0.000036864767,0.000030893338,0.000022605016,0.00012520874,0.00004867798,0.000016642958,0.000032546133,0.000011252208],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011598367,0.0002231827,0.46826044,0.00043847712,0.00063239667,0.000046420126,0.0007142294,0.0023299658,0.3740906,0.10953598,0.022696305,0.019872176],"study_design_scores_gemma":[0.003297745,0.000035324745,0.36627764,0.000052323336,0.00007134428,0.00010372965,0.00012465923,0.002510285,0.45096117,0.15801392,0.018149989,0.00040189383],"about_ca_topic_score_codex":0.0024156482,"about_ca_topic_score_gemma":0.00006852192,"teacher_disagreement_score":0.10198282,"about_ca_system_score_codex":8.6377224e-7,"about_ca_system_score_gemma":0.000013686471,"threshold_uncertainty_score":0.99971265},"labels":[],"label_agreement":null},{"id":"W2147253037","doi":"10.1190/1.2213951","title":"Improved Green's functions for passive-source structural studies","year":2006,"lang":"en","type":"article","venue":"Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Receiver function; Seismogram; Geology; Deconvolution; Function (biology); Lithosphere; Seismology; Component (thermodynamics); Computer science; Algorithm; Physics","score_opus":0.01131346913743534,"score_gpt":0.21771456078875817,"score_spread":0.20640109165132284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147253037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949256,0.0002929251,0.0010022257,0.00024823216,0.0016931135,0.00037340226,0.0007080466,0.000106608226,0.0006498281],"genre_scores_gemma":[0.9921639,0.0000059049894,0.0005755305,0.000098942335,0.0017377542,0.000010674557,0.00042309097,0.000007849807,0.0049763434],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99905014,0.000023378041,0.00019371592,0.00025994418,0.00012922441,0.00034361053],"domain_scores_gemma":[0.9994002,0.00012170978,0.00010884232,0.00019831466,0.00012019048,0.00005074674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000586421,0.00017350233,0.00024361929,0.000026352034,0.00034627103,0.00006849359,0.00014047994,0.000047553294,0.00011534957],"category_scores_gemma":[0.000012386096,0.00013716148,0.000102212565,0.0001171161,0.000079040125,0.00018129413,0.000017629713,0.00005663453,0.000113079666],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011073421,0.00028866605,0.039686106,0.0015766319,0.0023314848,0.000037035672,0.0028666437,0.04749718,0.107858375,0.028367067,0.1099257,0.65845776],"study_design_scores_gemma":[0.0035764354,0.001284999,0.4071541,0.000065713415,0.0008193693,0.000013049577,0.0011907314,0.029198537,0.008273022,0.24558717,0.30041027,0.0024265987],"about_ca_topic_score_codex":0.005482661,"about_ca_topic_score_gemma":0.0011478115,"teacher_disagreement_score":0.6560312,"about_ca_system_score_codex":0.000002907459,"about_ca_system_score_gemma":0.00002547679,"threshold_uncertainty_score":0.82881796},"labels":[],"label_agreement":null},{"id":"W2148321586","doi":"10.1785/gssrl.82.1.69","title":"New Regional Moment Tensors in South Africa","year":2011,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Moment (physics); Geology; Seismology; Physics; Classical mechanics","score_opus":0.15716022143937083,"score_gpt":0.288205094133104,"score_spread":0.1310448726937332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148321586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894172,0.00010527856,0.0002911591,0.004127181,0.0001263845,0.00024416,0.00002101293,0.00003362355,0.0056340233],"genre_scores_gemma":[0.99608207,0.000013660996,0.0016089845,0.0011548381,0.00017221808,0.0000041272465,0.000018189134,0.0000032333196,0.00094266084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977853,0.00034417686,0.00019160596,0.00035430322,0.0005870834,0.00073754153],"domain_scores_gemma":[0.9992789,0.00019107266,0.00003062533,0.00020365643,0.00003127207,0.0002644449],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009682831,0.00011610321,0.0001805297,0.00015026006,0.00010301014,0.000050285977,0.0003987684,0.000081736136,0.005473813],"category_scores_gemma":[0.000081591614,0.000079546306,0.000048578888,0.00032078032,0.00018600501,0.00009287041,0.000048636288,0.00030954575,0.0011179261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0032636302,0.000655085,0.44217798,0.00015123152,0.00025334873,0.006475283,0.04961611,0.006879986,0.019834287,0.025470456,0.37654924,0.06867337],"study_design_scores_gemma":[0.0006297421,0.0005214167,0.80823815,0.000028524537,0.000005287527,0.0000067889537,0.0003398326,0.00027889299,0.00039448278,0.018069962,0.17112887,0.00035801562],"about_ca_topic_score_codex":0.0055846213,"about_ca_topic_score_gemma":0.00004326652,"teacher_disagreement_score":0.3660602,"about_ca_system_score_codex":0.000008267559,"about_ca_system_score_gemma":0.000055146036,"threshold_uncertainty_score":0.99965984},"labels":[],"label_agreement":null},{"id":"W2148933774","doi":"10.1002/jgrb.50102","title":"Subcontinental sinking slab remnants in a spherical geometry mantle model","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Slab; Geology; Mantle (geology); Transition zone; Slab window; Subduction; Lithosphere; Mantle wedge; Geophysics; Mantle convection; Seismology; Tectonics; Oceanic crust","score_opus":0.03614595234854423,"score_gpt":0.3067936215938322,"score_spread":0.270647669245288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148933774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99695146,0.000102945545,0.000103382285,0.0004485862,0.00024257008,0.00020333669,0.000020091358,0.000008744268,0.0019188795],"genre_scores_gemma":[0.99710524,0.00009321264,0.0013975349,0.000073050665,0.00064232346,0.000001572034,0.0000075355997,0.000009340795,0.0006701969],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9966365,0.00028930765,0.000595608,0.00025556982,0.0013441317,0.000878848],"domain_scores_gemma":[0.99845314,0.0003725699,0.00018411434,0.00022518424,0.00037022473,0.00039478234],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012868779,0.0001755052,0.0005413628,0.00026120793,0.00014576325,0.00026768725,0.0005254994,0.00010078776,0.0015485752],"category_scores_gemma":[0.00028173998,0.00012926878,0.00015750715,0.00063115207,0.00017850245,0.00073962373,0.000078522455,0.00078618695,0.0010255348],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026930117,0.0030371535,0.24586691,0.00056174555,0.0005509059,0.0026266207,0.003673422,0.0632307,0.44678116,0.0024999762,0.029611621,0.19886675],"study_design_scores_gemma":[0.0014836189,0.0010873631,0.82876706,0.00022751764,0.000016815184,0.000051885305,0.00026967505,0.1341148,0.006384102,0.02517176,0.0020009018,0.0004244732],"about_ca_topic_score_codex":0.0037433684,"about_ca_topic_score_gemma":0.0002761809,"teacher_disagreement_score":0.58290017,"about_ca_system_score_codex":0.000010622111,"about_ca_system_score_gemma":0.00020488822,"threshold_uncertainty_score":0.9997523},"labels":[],"label_agreement":null},{"id":"W2149073923","doi":"10.2113/gscanmin.41.2.441","title":"LAMELLAR MINERALS OF THE CUPROBISMUTITE SERIES AND RELATED PADERAITE: A NEW OCCURRENCE AND IMPLICATIONS","year":2003,"lang":"en","type":"article","venue":"The Canadian Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Series (stratigraphy); Geology; Geochemistry; Mineralogy; Paleontology","score_opus":0.012777160543899923,"score_gpt":0.19362026487134096,"score_spread":0.18084310432744102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149073923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9715878,0.0016859475,0.000002222789,0.011696068,0.00029776007,0.00031354223,0.00089353346,0.000010633036,0.013512505],"genre_scores_gemma":[0.996956,0.00009045602,0.00008822109,0.00030930198,0.000023768593,0.0000010925081,0.000032742053,0.0000018669584,0.0024965818],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99940264,0.000080686135,0.00013681517,0.00013311084,0.00005821124,0.00018855112],"domain_scores_gemma":[0.99948376,0.00004777227,0.000062605315,0.00022519332,0.000024975358,0.00015569663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015994428,0.00008929477,0.000114879025,0.000024609697,0.0002743643,0.000074423704,0.00014858606,0.000044852244,0.00027863114],"category_scores_gemma":[0.00006644265,0.000050632207,0.0000194028,0.00014021862,0.00031295154,0.00007075954,0.000007747911,0.00006440759,0.000008954214],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050080234,0.00002745002,0.34549576,0.00018347366,0.00022514164,0.000023524448,0.0059023523,0.0026072687,0.03944234,0.35328594,0.24182248,0.010934165],"study_design_scores_gemma":[0.0003747117,0.00008816946,0.6680143,0.000038174858,0.0000791747,0.00014999592,0.00013946234,0.000094333685,0.0009449911,0.033104032,0.29662418,0.00034848953],"about_ca_topic_score_codex":0.27283973,"about_ca_topic_score_gemma":0.59880334,"teacher_disagreement_score":0.32596362,"about_ca_system_score_codex":0.0000023954549,"about_ca_system_score_gemma":0.00019812488,"threshold_uncertainty_score":0.7320025},"labels":[],"label_agreement":null},{"id":"W2149076338","doi":"10.1146/annurev.earth.031208.100045","title":"Frictional Melting Processes in Planetary Materials: From Hypervelocity Impact to Earthquakes","year":2010,"lang":"en","type":"article","venue":"Annual Review of Earth and Planetary Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":198,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Hypervelocity; Meteorite; Impact crater; Slip (aerodynamics); Geology; Materials science; Composite material; Mineralogy; Astrobiology","score_opus":0.012468612340211375,"score_gpt":0.2503233543406679,"score_spread":0.2378547420004565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149076338","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9803073,0.014079006,0.0000011310228,0.000267253,0.0004030189,0.00029477954,0.0038944788,0.000017513252,0.00073550973],"genre_scores_gemma":[0.990175,0.0065656025,0.0015402063,0.0005902982,0.00023214628,0.0000017715934,0.0008776765,0.0000027102974,0.000014557438],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981792,0.00012596336,0.00048595387,0.0004222904,0.00040860995,0.0003779931],"domain_scores_gemma":[0.99894327,0.00045519634,0.00016874254,0.00015498922,0.00006806863,0.00020975457],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010645643,0.00022223701,0.00051111454,0.00011714716,0.00016769295,0.00008286688,0.00033501734,0.00007068954,0.004634208],"category_scores_gemma":[0.00024729964,0.00015474124,0.000041490915,0.0004188392,0.00015218343,0.0005262793,0.000024047866,0.00014005725,0.00012831291],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022807097,0.000084340034,0.9325483,0.003910976,0.000084930434,0.00005900827,0.0014601303,0.0009698512,0.0075447964,0.00010576277,0.0018004901,0.051203337],"study_design_scores_gemma":[0.00012237822,0.00029325657,0.9873152,0.0009103185,0.000019967329,0.000020282123,0.00007554686,0.00006627247,0.00088552764,0.00024714644,0.0097907325,0.00025341735],"about_ca_topic_score_codex":0.025428012,"about_ca_topic_score_gemma":0.014413403,"teacher_disagreement_score":0.05476685,"about_ca_system_score_codex":3.962521e-7,"about_ca_system_score_gemma":0.00015304436,"threshold_uncertainty_score":0.99627566},"labels":[],"label_agreement":null},{"id":"W2149659360","doi":"10.1139/p10-004","title":"Pressure derivative of the melting temperature for some alkali halides","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Halide; Alkali metal; Physics; Thermodynamics; Derivative (finance); Melting temperature; Melting point; Work (physics); Constant (computer programming); Inorganic chemistry; Chemistry; Materials science; Quantum mechanics; Composite material","score_opus":0.009308055411129175,"score_gpt":0.19699846073464147,"score_spread":0.1876904053235123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149659360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967392,0.00022707337,0.000016460215,0.00039480935,0.0017569934,0.00012468825,0.0005568356,0.0000016910041,0.00018222998],"genre_scores_gemma":[0.9984082,0.000002492914,0.00034197053,0.00013101107,0.0010074567,3.4266702e-7,0.000008084004,0.000004300812,0.0000961371],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99937993,0.000034368088,0.00020019502,0.00007112263,0.00012212404,0.00019226443],"domain_scores_gemma":[0.999141,0.00008684454,0.00027589485,0.0001337186,0.00018717095,0.00017539773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021415339,0.000087148954,0.00019069672,0.000026101015,0.0001764622,0.000063262254,0.0003219453,0.000049511975,0.0001303752],"category_scores_gemma":[0.00009259958,0.000055777837,0.000107256375,0.000090387926,0.00010263395,0.00022798179,0.000004081455,0.00018552713,0.0000019300035],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001322618,0.00006164123,0.10609996,0.00060006045,0.001124567,0.000050331866,0.0092573045,0.018774698,0.70621663,0.0829259,0.034677457,0.040079184],"study_design_scores_gemma":[0.0013046762,0.0004157625,0.21337831,0.0003180954,0.00044476776,0.00006400535,0.00063295726,0.0008375968,0.51061493,0.12415977,0.14713612,0.0006929824],"about_ca_topic_score_codex":0.0051981285,"about_ca_topic_score_gemma":0.019042265,"teacher_disagreement_score":0.19560169,"about_ca_system_score_codex":0.0000014300086,"about_ca_system_score_gemma":0.0004340624,"threshold_uncertainty_score":0.9988577},"labels":[],"label_agreement":null},{"id":"W2149967502","doi":"10.1154/1.3076082","title":"<i>Ab initio</i> structure determination of SrBi <sub>2</sub> OB <sub>4</sub> O <sub>9</sub> by powder X-ray/neutron diffraction and NMR spectroscopy","year":2009,"lang":"en","type":"article","venue":"Powder Diffraction","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Triclinic crystal system; Crystallography; Neutron diffraction; Crystal structure; Ab initio; Materials science; Boron; Powder diffraction; Single crystal; Chemistry; Analytical Chemistry (journal)","score_opus":0.006069828444442862,"score_gpt":0.20692162048230858,"score_spread":0.2008517920378657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149967502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957974,0.00037261992,0.0004110811,0.00041203972,0.0013629314,0.0006477449,0.0005153156,0.00015517809,0.00032566744],"genre_scores_gemma":[0.99603903,0.0013392528,0.00015199161,0.00047908272,0.000754843,0.0000102149315,0.0011759932,0.000036598063,0.000013017387],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9965085,0.00028253932,0.00078974385,0.00090558786,0.0007229786,0.0007906885],"domain_scores_gemma":[0.99801606,0.00021659928,0.0007914116,0.00048611785,0.00019533744,0.00029446877],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00033118087,0.0006279352,0.00068784395,0.0002935954,0.00045876135,0.00032551307,0.00023870218,0.0004555834,0.00012191567],"category_scores_gemma":[0.00006713001,0.0006051753,0.00016583188,0.00040855218,0.00014519754,0.0018041116,0.000032190794,0.000526737,0.000119631615],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024223197,0.00014128565,0.0018946587,0.000093099385,0.000043906268,0.000008539958,0.00019286973,0.00017585265,0.9442215,0.000030459067,0.0012323529,0.051723246],"study_design_scores_gemma":[0.0007521315,0.00038936653,0.2892359,0.000060449624,0.00015137631,0.000030313737,0.00006712288,0.0006716857,0.7056823,0.0016953556,0.00077029556,0.0004937379],"about_ca_topic_score_codex":0.00034069087,"about_ca_topic_score_gemma":0.00045112972,"teacher_disagreement_score":0.28734124,"about_ca_system_score_codex":0.000052750776,"about_ca_system_score_gemma":0.000079153324,"threshold_uncertainty_score":0.99964},"labels":[],"label_agreement":null},{"id":"W2151834862","doi":"10.1029/2000jb000018","title":"Thermal evolution of Earth: Models with time‐dependent layering of mantle convection which satisfy the Urey ratio constraint","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Toronto","funders":"","keywords":"Mantle convection; Mantle (geology); Geology; Convection; Geophysics; Earth's internal heat budget; Layering; Rayleigh number; Internal heating; Thermal; Natural convection; Mechanics; Thermodynamics; Lithosphere; Physics","score_opus":0.027389382411171663,"score_gpt":0.24664431809387766,"score_spread":0.219254935682706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151834862","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995498,0.00037122998,0.00080043793,0.000187635,0.00010309045,0.00019435683,0.00003358847,0.000004982499,0.0028066523],"genre_scores_gemma":[0.9989278,0.00006641027,0.00046918404,0.0000050123826,0.00024353359,0.0000010343061,0.00000204173,0.0000056270997,0.00027937695],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99759597,0.0003871156,0.00042908243,0.00013883937,0.0011366403,0.00031236032],"domain_scores_gemma":[0.99815804,0.00047626335,0.0003266239,0.00019724558,0.0007250073,0.000116818555],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009872678,0.0001180495,0.00033538553,0.00002341531,0.0001497709,0.000063414845,0.00030420502,0.000057896723,0.0017753618],"category_scores_gemma":[0.00010346159,0.00006730868,0.00007443529,0.0003130918,0.00030303482,0.0003578245,0.000027844988,0.00034382453,0.000057778525],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022266011,0.00067698664,0.015015604,0.0003001994,0.00086055737,0.00008218389,0.0023584766,0.45519882,0.47897506,0.013241606,0.0013514583,0.029712455],"study_design_scores_gemma":[0.0032654707,0.009366853,0.42465627,0.0006725392,0.00020270918,0.000104401384,0.001771903,0.45849136,0.08250837,0.017736163,0.0006194915,0.0006044726],"about_ca_topic_score_codex":0.0031477066,"about_ca_topic_score_gemma":0.0005891268,"teacher_disagreement_score":0.40964067,"about_ca_system_score_codex":0.000008080031,"about_ca_system_score_gemma":0.00014397572,"threshold_uncertainty_score":0.99913716},"labels":[],"label_agreement":null},{"id":"W2152928412","doi":"10.1017/s0263034605050718","title":"Idealized slab plasma approach for the study of warm dense matter","year":2005,"lang":"en","type":"article","venue":"Laser and Particle Beams","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; University of British Columbia","funders":"","keywords":"Isochoric process; Slab; Warm dense matter; Plasma; Shock wave; Shock (circulatory); Field (mathematics)","score_opus":0.01694090369704145,"score_gpt":0.22665698336211335,"score_spread":0.2097160796650719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152928412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99869317,0.000081024424,0.00012920196,0.00016085066,0.000091195354,0.00039761505,0.000057186586,0.000010047333,0.0003797262],"genre_scores_gemma":[0.9989961,0.0000075008275,0.00039392698,0.00014559524,0.000119169046,0.000012019681,0.000012841077,0.000002992388,0.00030985026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99938893,0.00004242744,0.00015782678,0.00013756957,0.00010122595,0.00017204054],"domain_scores_gemma":[0.9995939,0.00014294403,0.000041672465,0.00015078069,0.000018861276,0.00005182817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021937306,0.000075503325,0.00013530266,0.000007717892,0.00011651867,0.000046005207,0.00009597694,0.000021192254,0.00034695072],"category_scores_gemma":[0.000005911498,0.00004452222,0.000026076352,0.000050807535,0.000031634976,0.00007664935,0.000010900629,0.000026313493,0.000045636785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017430709,0.0011274916,0.8639191,0.0001897152,0.00041440924,0.000005269829,0.013215336,0.05435636,0.0054049823,0.00044631035,0.007599179,0.051578782],"study_design_scores_gemma":[0.007759321,0.0012435954,0.7200385,0.000013562382,0.00043831876,0.000010252464,0.0029636156,0.17798625,0.05160384,0.0007315024,0.036623813,0.0005874639],"about_ca_topic_score_codex":0.0008276191,"about_ca_topic_score_gemma":0.00035925966,"teacher_disagreement_score":0.14388064,"about_ca_system_score_codex":4.445551e-7,"about_ca_system_score_gemma":0.0000053504814,"threshold_uncertainty_score":0.37988672},"labels":[],"label_agreement":null},{"id":"W2152993362","doi":"10.1021/jp3100415","title":"Pressure-Induced Polymorphic Transitions in Crystalline Diborane Deduced by Comparison of Simulated and Experimental Vibrational Spectra","year":2013,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Ontario Ministry of Economic Development and Innovation","keywords":"Diborane; Raman spectroscopy; Chemistry; Spectral line; Infrared spectroscopy; Boranes; Crystallography; Physical chemistry; Boron; Organic chemistry; Physics","score_opus":0.01009432942179204,"score_gpt":0.240511577447466,"score_spread":0.23041724802567398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152993362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999089,0.00031829122,0.000020708476,0.00027387985,0.000018629806,0.00007605076,0.0000601251,0.0000031484633,0.00014018656],"genre_scores_gemma":[0.9997525,0.0000027106166,0.000034251876,0.000011350194,0.00015710772,2.6724138e-7,0.000026060492,0.000002774335,0.000012959975],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99926513,0.00005135172,0.00028726188,0.00007015318,0.00020896526,0.00011714523],"domain_scores_gemma":[0.9995293,0.00010048419,0.00017450532,0.00007560831,0.000045491965,0.000074632364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000092585724,0.00009576364,0.0002572326,0.00001184855,0.00004302273,0.000024597943,0.00013788634,0.00003433615,0.0006540573],"category_scores_gemma":[0.000007767493,0.000063444255,0.000043004846,0.00007469414,0.00006938569,0.00015455738,0.000006231508,0.00013551474,0.0000029811224],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000073165946,0.0001610393,0.00019007787,0.000018992792,0.000030808584,7.4429215e-7,0.00060061924,0.010643901,0.98814774,0.0000054844213,0.00008089068,0.000046563917],"study_design_scores_gemma":[0.0005026362,0.00014830839,0.004768683,0.000023990111,0.000039358107,0.000006573874,0.00021311521,0.027502097,0.9663931,0.00030212846,0.00001811307,0.0000818613],"about_ca_topic_score_codex":0.00026705643,"about_ca_topic_score_gemma":0.000005499424,"teacher_disagreement_score":0.021754578,"about_ca_system_score_codex":0.0000018863557,"about_ca_system_score_gemma":0.000026469594,"threshold_uncertainty_score":0.7161469},"labels":[],"label_agreement":null},{"id":"W2154165902","doi":"10.1111/j.1365-246x.2008.03891.x","title":"Dynamical modelling of lithospheric extension and small-scale convection: implications for magmatism during the formation of volcanic rifted margins","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Crust; Igneous rock; Lithosphere; Magmatism; Rift; Mantle convection; Continental crust; Mantle (geology); Geophysics; Oceanic crust; Underplating; Petrology; Continental margin; Crustal recycling; Seismology; Geochemistry; Subduction; Tectonics","score_opus":0.021564428318077013,"score_gpt":0.21294700856417936,"score_spread":0.19138258024610236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154165902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95057416,0.000058221318,0.048207354,0.0004075696,0.0003718274,0.00012987778,0.0001467129,0.000006749518,0.00009752242],"genre_scores_gemma":[0.997172,0.00015444022,0.0022520553,0.000020758567,0.00024749376,0.0000030435872,0.00004521458,0.0000034952188,0.000101490565],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9992259,0.00003607311,0.00033896722,0.00011060039,0.00016619214,0.00012225787],"domain_scores_gemma":[0.9992314,0.0001240339,0.00025635574,0.00009134256,0.00024178057,0.00005507642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013354578,0.00008226044,0.00016159406,0.000035047866,0.00023767243,0.000029280436,0.00015965321,0.00003641805,0.00007180232],"category_scores_gemma":[0.000015873302,0.00005820721,0.000083564155,0.00007838594,0.000095085874,0.0002252318,0.000018041781,0.000094535506,0.000003666328],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028213158,0.0011829167,0.11638445,0.00084372837,0.0010819529,0.000026010794,0.007849182,0.40184596,0.38673642,0.026657617,0.0014732226,0.05309722],"study_design_scores_gemma":[0.00040652262,0.00008058575,0.795056,0.000032320007,0.000024768151,0.00017106993,0.000036526308,0.19581077,0.0013505195,0.0067710327,0.00017949335,0.00008043352],"about_ca_topic_score_codex":0.0002755442,"about_ca_topic_score_gemma":0.00007072094,"teacher_disagreement_score":0.67867154,"about_ca_system_score_codex":0.0000061156875,"about_ca_system_score_gemma":0.000025019966,"threshold_uncertainty_score":0.23736212},"labels":[],"label_agreement":null},{"id":"W2154395699","doi":"10.1111/1755-6724.12253","title":"Surface Expressions of Rayleigh‐Taylor Instability in Continental Interiors","year":2014,"lang":"en","type":"article","venue":"Acta Geologica Sinica - English Edition","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Crust; Lithosphere; Gravity anomaly; Deflection (physics); Petrology; Continental crust; Seismology; Instability; Geophysics; Isostasy; Tectonics; Paleontology; Mechanics","score_opus":0.012475746347607165,"score_gpt":0.21811582938745389,"score_spread":0.2056400830398467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154395699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916265,0.000019855303,0.00002482022,0.00016937341,0.0019074263,0.00020171193,0.0002080538,0.000058431324,0.0057838364],"genre_scores_gemma":[0.9987498,0.000023406426,0.00036319697,0.000060101585,0.0004398154,0.00000309209,0.00033809384,0.00000334648,0.000019163164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983985,0.00032240766,0.00047053173,0.00033287163,0.00019738739,0.00027833373],"domain_scores_gemma":[0.99870205,0.00058263465,0.00021980252,0.00030045473,0.000106475694,0.00008858843],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072796224,0.00015498357,0.00036885563,0.000045941335,0.000074246214,0.000032522767,0.00028108415,0.00015653575,0.0029825666],"category_scores_gemma":[0.0009498099,0.00012038254,0.000073605515,0.00014907485,0.0002075664,0.00034214527,0.000052291358,0.00015856,0.000029462019],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082441425,0.00084684626,0.86271113,0.00019647385,0.00006520839,0.000011719209,0.0031091613,0.0024644623,0.11400491,0.0010858111,0.009588166,0.0050916784],"study_design_scores_gemma":[0.00074039923,0.00036460027,0.969864,0.00005418471,0.00001647968,6.7909866e-7,0.00031254403,0.00054728147,0.0068843784,0.0016288264,0.0193443,0.00024230842],"about_ca_topic_score_codex":0.0007608141,"about_ca_topic_score_gemma":0.00046894033,"teacher_disagreement_score":0.10715287,"about_ca_system_score_codex":0.0000039438673,"about_ca_system_score_gemma":0.000018554229,"threshold_uncertainty_score":0.99792886},"labels":[],"label_agreement":null},{"id":"W2154523330","doi":"10.1306/2dc40968-0e47-11d7-8643000102c1865d","title":"Powder X-Ray Diffraction Analysis of Homogeneous and Heterogeneous Sedimentary Dolostones","year":2001,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Homogeneous; Geology; Sedimentary rock; Diffraction; Mineralogy; Geochemistry; X-ray; X-ray crystallography; Powder diffraction; Geomorphology; Crystallography; Optics; Physics; Chemistry; Thermodynamics","score_opus":0.038514049130031716,"score_gpt":0.30989028463772955,"score_spread":0.27137623550769785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154523330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99670875,0.002003528,0.000009183961,0.00049174274,0.00038423637,0.00012110349,0.00009705103,0.000004436089,0.00017996841],"genre_scores_gemma":[0.99756426,0.0015664593,0.00023990349,0.00012739975,0.00031889713,4.9068e-7,0.000058541904,0.000005081442,0.00011898929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99769837,0.00030611525,0.00051996944,0.00019368523,0.00093407976,0.0003477836],"domain_scores_gemma":[0.99877346,0.00032846988,0.0002545401,0.00018237774,0.00024484636,0.00021629766],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013538415,0.00013107642,0.0004468046,0.0007316316,0.00016695396,0.000060378752,0.0002411197,0.000065159285,0.003297709],"category_scores_gemma":[0.000019622561,0.000099615165,0.00014740546,0.0007039025,0.00016333237,0.00030729908,0.00003941232,0.00023733634,0.000017585106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025417919,0.0005241344,0.81890017,0.000108297514,0.006600374,0.0013803961,0.0012551767,0.03783097,0.09985399,0.000011076514,0.0039276984,0.02706594],"study_design_scores_gemma":[0.001261616,0.0025211389,0.9626997,0.00006723448,0.0014190563,0.0004968087,0.00087653805,0.0035130165,0.009815536,0.0005615839,0.016436,0.00033178733],"about_ca_topic_score_codex":0.004935092,"about_ca_topic_score_gemma":0.00031305858,"teacher_disagreement_score":0.14379953,"about_ca_system_score_codex":0.000013011946,"about_ca_system_score_gemma":0.000056203095,"threshold_uncertainty_score":0.99761343},"labels":[],"label_agreement":null},{"id":"W2154746660","doi":"10.1029/2004gl020939","title":"Lithospheric anisotropy structure inferred from collocated teleseismic and magnetotelluric observations: Great Slave Lake shear zone, northern Canada","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Manitoba; Western University","funders":"","keywords":"Geology; Lithosphere; Shear wave splitting; Anisotropy; Seismology; Magnetotellurics; Geophysics; Shear (geology); Seismic anisotropy; Mantle (geology); Shear zone; Tectonics; Petrology; Electrical resistivity and conductivity","score_opus":0.018176033042577228,"score_gpt":0.22455137456006172,"score_spread":0.2063753415174845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154746660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99470663,0.00017162012,0.00013858391,0.002984902,0.00026102967,0.00040865768,0.0012392176,0.00004445839,0.000044889282],"genre_scores_gemma":[0.99662393,0.000041512496,0.0010283687,0.0008609152,0.00044025408,0.0000073094766,0.00080333947,0.000015928834,0.0001784108],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9971442,0.00021257755,0.00027588865,0.00057614886,0.00096352055,0.0008276481],"domain_scores_gemma":[0.9987006,0.00032133693,0.00006645666,0.00039853057,0.00015943471,0.0003536148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014439701,0.00027014248,0.00035834056,0.000057805108,0.00042559643,0.00026121925,0.00039460274,0.000096828684,0.00063001335],"category_scores_gemma":[0.000091873066,0.0002271168,0.000046957695,0.0006871339,0.00027888754,0.00026603273,0.00007175371,0.0004220326,0.00012798117],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015041642,0.00036825208,0.3968363,0.00045855145,0.0009592008,0.0025188406,0.003317396,0.07980535,0.43063566,0.0016007527,0.020885779,0.061109748],"study_design_scores_gemma":[0.00084527803,0.00019224586,0.9779744,0.00003802128,0.00002511432,0.0000040588966,0.000081427184,0.0013151774,0.0011184976,0.003897728,0.014114087,0.00039397183],"about_ca_topic_score_codex":0.90243924,"about_ca_topic_score_gemma":0.86575794,"teacher_disagreement_score":0.5811381,"about_ca_system_score_codex":0.00004345173,"about_ca_system_score_gemma":0.0005504582,"threshold_uncertainty_score":0.92615545},"labels":[],"label_agreement":null},{"id":"W2155394217","doi":"10.1111/j.1365-246x.2006.02973.x","title":"Automated<i>SKS</i>splitting and upper-mantle anisotropy beneath Canadian seismic stations","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shear wave splitting; Seismogram; Anisotropy; Geology; Eigenvalues and eigenvectors; Transverse plane; Seismic anisotropy; Seismology; Physics; Optics","score_opus":0.005042493934564183,"score_gpt":0.20825351434925052,"score_spread":0.20321102041468633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155394217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892089,0.000061867504,0.00035461236,0.0016925747,0.0011402261,0.000071213784,0.00053933816,0.000062992454,0.0068682996],"genre_scores_gemma":[0.99575275,0.000026763131,0.0015854713,0.00040458573,0.0013698349,8.822793e-7,0.00026197487,0.000006219885,0.0005915082],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880284,0.00004558436,0.00026921558,0.00019197914,0.00031548424,0.0003748878],"domain_scores_gemma":[0.9992972,0.00007084611,0.000114372655,0.00007858927,0.000109320885,0.0003296898],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015612322,0.00013846268,0.00015263988,0.00012248682,0.0003689498,0.00042248963,0.00021678004,0.00004916452,0.0010172857],"category_scores_gemma":[0.000025104415,0.00011926042,0.00006343223,0.00008852846,0.000057308,0.00036469876,0.000016350128,0.00016401272,0.0002561545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002816857,0.00058346195,0.4766644,0.00009801991,0.0010441956,0.0013212042,0.0016211215,0.11983639,0.030303994,0.11478095,0.1680716,0.08539298],"study_design_scores_gemma":[0.00059840234,0.00010800206,0.7959321,0.000042582396,0.000043796972,0.000212473,0.000086216955,0.100939006,0.0007084901,0.03336255,0.06757724,0.00038909796],"about_ca_topic_score_codex":0.123102784,"about_ca_topic_score_gemma":0.013578789,"teacher_disagreement_score":0.31926775,"about_ca_system_score_codex":0.000019274037,"about_ca_system_score_gemma":0.0001778166,"threshold_uncertainty_score":0.99989593},"labels":[],"label_agreement":null},{"id":"W2156399339","doi":"10.1111/j.1365-246x.2006.03103.x","title":"Effects of mode coupling and location of rotational axis on glacial induced rotational deformation in a laterally heterogeneous viscoelastic earth","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Rotation around a fixed axis; Spherical harmonics; Viscoelasticity; Mechanics; Amplitude; Physics; Coupling (piping); Harmonics; Mantle (geology); Classical mechanics; Geophysics; Materials science; Optics","score_opus":0.005570970232800811,"score_gpt":0.21813127474767044,"score_spread":0.21256030451486962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156399339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99815243,0.00002247278,0.0010479614,0.00006424015,0.00039772567,0.00012492425,0.00004443679,0.000005128639,0.00014066613],"genre_scores_gemma":[0.99909985,0.000006517915,0.00041171053,0.000025283169,0.00031377916,0.000002475798,0.00012335724,0.0000037035581,0.0000133446465],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99875814,0.000043256106,0.00044595348,0.00013163876,0.000483962,0.00013706893],"domain_scores_gemma":[0.9991151,0.0002121766,0.0002878031,0.000042396507,0.000295657,0.00004687423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013114543,0.00011345007,0.00018886478,0.00016279871,0.000055629185,0.000055007764,0.00011729753,0.0000490724,0.00006341652],"category_scores_gemma":[0.00005979037,0.000098757395,0.000042737942,0.00014904507,0.000042989563,0.00030725735,0.000011067723,0.00011869629,0.000015050699],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007101549,0.00035416317,0.021598514,0.00013342746,0.0000959787,0.000023687102,0.00035739614,0.87996095,0.08189761,0.009202788,0.000016695514,0.0056486083],"study_design_scores_gemma":[0.00090925896,0.000259547,0.8317251,0.00015500477,0.000014834642,0.000020024405,0.000006733222,0.14045905,0.016302872,0.01001872,0.000011177465,0.000117671894],"about_ca_topic_score_codex":0.0007963117,"about_ca_topic_score_gemma":0.00018912167,"teacher_disagreement_score":0.8101266,"about_ca_system_score_codex":0.000009260416,"about_ca_system_score_gemma":0.00007349265,"threshold_uncertainty_score":0.40272096},"labels":[],"label_agreement":null},{"id":"W2156855697","doi":"10.1139/e10-022","title":"Upper mantle thermochemical structure from seismic–geodynamic flow models: constraints from the Lithoprobe initiativeThis article is one of a series of papers published in this Special Issue on the theme <i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Geophysics; Mantle convection; Transition zone; Geodynamics; Geoid; Mantle plume; Craton; Seismic tomography; Lithosphere; Tectonics; Seismology","score_opus":0.009903632176611782,"score_gpt":0.1810299918179349,"score_spread":0.1711263596413231,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156855697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99204445,0.0003641916,0.000009026896,0.004189859,0.0003168969,0.0002099857,0.0009840039,0.0000012388873,0.0018803363],"genre_scores_gemma":[0.9986883,0.000038531434,0.00074970955,0.00025902517,0.00024423123,7.252219e-7,0.000006384113,0.0000024760889,0.000010654207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986259,0.00018543882,0.00043256895,0.00017124075,0.00036157997,0.00022331641],"domain_scores_gemma":[0.99847317,0.0006237009,0.00043461306,0.00018114195,0.00017854302,0.00010882444],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00097207027,0.00012180401,0.00031991935,0.00006717,0.00016501537,0.00012325842,0.0005314239,0.00007487723,0.006599397],"category_scores_gemma":[0.00036199612,0.00005731948,0.000058676535,0.00031541425,0.002541243,0.00038642652,0.000014427132,0.0002745363,0.0000011354138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003438249,0.00028507138,0.54090065,0.00033913882,0.0011903888,0.00005641687,0.1878112,0.014109503,0.18694752,0.035243142,0.0041960767,0.02548266],"study_design_scores_gemma":[0.0041435673,0.0010092108,0.51635975,0.0011672758,0.0003293174,0.000062945095,0.023499208,0.027953645,0.11669381,0.30451542,0.0034799997,0.00078584964],"about_ca_topic_score_codex":0.05239807,"about_ca_topic_score_gemma":0.13254872,"teacher_disagreement_score":0.26927227,"about_ca_system_score_codex":0.000002008618,"about_ca_system_score_gemma":0.00075982,"threshold_uncertainty_score":0.9943087},"labels":[],"label_agreement":null},{"id":"W2156887873","doi":"10.1093/gji/ggs053","title":"Comparison of spherical-shell and plane-layer mantle convection thermal structure in viscously stratified models with mixed-mode heating: implications for the incorporation of temperature-dependent parameters","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mantle convection; Mantle (geology); Spherical shell; Convection; Rayleigh number; Spherical geometry; Mechanics; Internal heating; Thermal; Geophysics; Thermodynamics; Natural convection; Materials science; Geometry; Physics; Geology; Shell (structure); Mathematics; Composite material","score_opus":0.028136040930153462,"score_gpt":0.28399901620654844,"score_spread":0.25586297527639495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156887873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955702,0.000064413274,0.0032379455,0.00023335453,0.00033939225,0.00019904472,0.000268805,0.0000038312924,0.00008301825],"genre_scores_gemma":[0.9978828,0.000011058926,0.0017376145,0.000026112903,0.00022779511,0.0000036101055,0.00009392483,0.000004106357,0.000012977928],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9991446,0.000054494267,0.00032282018,0.00010922486,0.0002239626,0.00014489016],"domain_scores_gemma":[0.9992402,0.00021069168,0.0002952452,0.000082575716,0.00011376375,0.00005751663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014599522,0.00010315402,0.00020113548,0.00003608375,0.00008771981,0.00006299627,0.00014632482,0.000049391874,0.00004521914],"category_scores_gemma":[0.000012408361,0.00006314534,0.000037988186,0.000062859144,0.000071648334,0.00033050086,0.000010483614,0.00014481418,8.65681e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094271556,0.0003129021,0.21545911,0.000054035176,0.0002708076,8.967818e-7,0.0015763027,0.3928196,0.37311888,0.007964533,0.00016438164,0.0073158345],"study_design_scores_gemma":[0.00091878633,0.00039785888,0.8946273,0.000050572373,0.000074534626,0.000032480257,0.00045770913,0.048465133,0.041969527,0.012770164,0.00004133777,0.00019462768],"about_ca_topic_score_codex":0.0006647323,"about_ca_topic_score_gemma":0.00055048935,"teacher_disagreement_score":0.67916816,"about_ca_system_score_codex":0.000006068047,"about_ca_system_score_gemma":0.000039384697,"threshold_uncertainty_score":0.25749922},"labels":[],"label_agreement":null},{"id":"W2157131428","doi":"10.1103/physrevb.68.165102","title":"Self-consistent modification to the electron density of states due to electron-phonon coupling in metals","year":2003,"lang":"en","type":"article","venue":"Physical review. B, Condensed matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Condensed matter physics; Electron; Polaron; Phonon; Coupling (piping); Coupling strength; Physics; Crossover; Quantum mechanics; Materials science","score_opus":0.012603480832471918,"score_gpt":0.2669141826967049,"score_spread":0.254310701864233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157131428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99554974,0.0010521275,0.00027706375,0.0017185226,0.000098132405,0.00082364737,0.00002782484,0.000016407801,0.00043652224],"genre_scores_gemma":[0.9961424,0.0002937929,0.00022828666,0.0031705666,0.000051224117,0.000023607456,0.000034463934,0.0000073239635,0.00004834676],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99853045,0.00017535263,0.000356899,0.00031651842,0.00025382938,0.00036695905],"domain_scores_gemma":[0.9991416,0.00018903697,0.00012440393,0.0003505449,0.00008694974,0.00010747675],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00060306245,0.00017732763,0.0005016062,0.0000438962,0.00006000782,0.000037161168,0.00020351217,0.000024201838,0.0002817085],"category_scores_gemma":[0.00005775358,0.00012259868,0.00009594445,0.0002886886,0.00002048384,0.000080586266,0.0000151934255,0.000109604945,0.0010661097],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007305836,0.0017109246,0.033238765,0.007029366,0.0009991152,0.00008325484,0.0045203343,0.061158825,0.8136989,0.023225266,0.049209174,0.004395485],"study_design_scores_gemma":[0.00084352074,0.0007006923,0.15246235,0.0007984328,0.00057523313,0.00002655282,0.00005867999,0.005969128,0.73754686,0.02232778,0.07732379,0.0013670115],"about_ca_topic_score_codex":0.00037272985,"about_ca_topic_score_gemma":0.00022725071,"teacher_disagreement_score":0.11922359,"about_ca_system_score_codex":0.000010109101,"about_ca_system_score_gemma":0.00004679845,"threshold_uncertainty_score":0.9997117},"labels":[],"label_agreement":null},{"id":"W2158031954","doi":"10.1016/j.epsl.2012.09.056","title":"Crustal eclogitization and lithosphere delamination in orogens","year":2012,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":232,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Crust; Eclogitization; Mantle (geology); Magmatism; Delamination (geology); Geophysics; Continental crust; Petrology; Subduction; Seismology; Tectonics; Oceanic crust","score_opus":0.006164782762931524,"score_gpt":0.1795271888044888,"score_spread":0.17336240604155728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158031954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99787456,0.00047275593,0.000036638226,0.0003719529,0.0002492569,0.00010502486,0.000038983504,0.000016319895,0.00083448447],"genre_scores_gemma":[0.99835384,0.00007369613,0.0007051766,0.0006158611,0.00011533615,4.2245938e-7,0.00011063168,0.0000014904138,0.00002355371],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990502,0.000043063024,0.00012558214,0.00020647784,0.00019997353,0.00037467573],"domain_scores_gemma":[0.9996536,0.000057140252,0.000040813204,0.0000793791,0.000008839934,0.00016022171],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047746065,0.00009930273,0.0001068973,0.00008132948,0.00016714391,0.00010921263,0.00008456094,0.00003402611,0.00029052334],"category_scores_gemma":[0.00002181727,0.00008355017,0.0000081443495,0.00021219264,0.00022181106,0.0008675832,0.000011664338,0.00006533439,0.000042997934],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011349841,0.000004908772,0.98753965,0.000011827457,0.0000020639857,0.0000072985686,0.00037694254,0.0006171047,0.0032302723,0.00008767823,0.00008034802,0.008030564],"study_design_scores_gemma":[0.00012872792,0.000024812229,0.99550927,0.000007854914,0.000004602383,0.000021187212,0.00005522433,0.0022476711,0.00030689655,0.00003910748,0.001532718,0.00012193216],"about_ca_topic_score_codex":0.0011507691,"about_ca_topic_score_gemma":0.0004618418,"teacher_disagreement_score":0.007969624,"about_ca_system_score_codex":0.0000012107098,"about_ca_system_score_gemma":0.000015974962,"threshold_uncertainty_score":0.34070772},"labels":[],"label_agreement":null},{"id":"W2158297208","doi":"10.1073/pnas.0710473105","title":"Pressure-induced metallization of silane","year":2007,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Brookhaven National Laboratory; Basic Energy Sciences; Office of Science; Division of Materials Research; U.S. Department of Energy; National Nuclear Security Administration; National Science Foundation","keywords":"Silane; Raman spectroscopy; Infrared; Hydride; Hydrogen; Metal; Infrared spectroscopy; Opacity; Chemistry; Spectral line; Hydrogen bond; Phase (matter); Materials science; Germane; Analytical Chemistry (journal); Molecule; Silicon; Organic chemistry; Optics","score_opus":0.035447999304617006,"score_gpt":0.2755196337669825,"score_spread":0.2400716344623655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158297208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870451,0.00010709984,0.0000024442286,0.0002207455,0.000049566355,0.0001185196,0.00003881079,0.0000058721375,0.012411812],"genre_scores_gemma":[0.99907196,0.000011424367,0.0006861589,0.000047686328,0.00007417603,2.967994e-7,5.4119437e-7,0.0000010067738,0.000106728374],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9984998,0.0000054070642,0.00031916174,0.00014082053,0.0009082439,0.00012657573],"domain_scores_gemma":[0.99919146,0.00010716895,0.0004571776,0.000006709471,0.0002091771,0.000028317501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018183545,0.000064650645,0.00015003026,0.00009856996,0.00009216075,0.0000137051675,0.000522947,0.00005649479,0.000115480936],"category_scores_gemma":[0.00019955638,0.000040337967,0.000046751742,0.0004954322,0.0002814745,0.00032418102,0.000026515147,0.00004607594,0.0000018203011],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029670005,0.00002679523,0.024971524,0.00011472411,0.000031230586,4.7541007e-9,0.00022080267,0.0008489406,0.9399696,0.032619867,0.00021726952,0.00094956224],"study_design_scores_gemma":[0.0000778433,0.00004739731,0.36258593,0.000030003164,0.000020411298,0.0000012756058,0.00005037343,0.00050167006,0.61707914,0.019074023,0.00047831878,0.000053595806],"about_ca_topic_score_codex":0.00010550261,"about_ca_topic_score_gemma":0.000001344207,"teacher_disagreement_score":0.33761442,"about_ca_system_score_codex":0.0000011592924,"about_ca_system_score_gemma":0.00001865421,"threshold_uncertainty_score":0.16449346},"labels":[],"label_agreement":null},{"id":"W2159007048","doi":"10.1785/0120020036","title":"Imaging Crustal Structure along Refraction Profiles Using Multicomponent Recordings of First-Arrival Coda","year":2002,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Air Force Office of Scientific Research; Defense Threat Reduction Agency; University of Saskatchewan; University of Wyoming","keywords":"Coda; Geology; Seismology; Crust; Refraction; Seismic refraction; Waveform; Mantle (geology); Scattering; Receiver function; Geophysics; Optics; Lithosphere; Physics; Tectonics","score_opus":0.015613149662565424,"score_gpt":0.20316664930017014,"score_spread":0.18755349963760473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159007048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951997,0.000175347,0.00022071887,0.0036016149,0.0002718803,0.00018478108,0.0001676518,0.00001534253,0.00016299146],"genre_scores_gemma":[0.98360246,0.000069782414,0.015636165,0.0005418737,0.00007143444,4.464285e-7,0.000011865294,0.0000039510064,0.000062026185],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.998851,0.000103942926,0.00035995254,0.00020059512,0.00027410986,0.00021039636],"domain_scores_gemma":[0.9990124,0.00016624008,0.00052523176,0.00018452597,0.000067369154,0.000044222583],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001407971,0.00013562413,0.00035386876,0.000011541662,0.00013487303,0.0000122547945,0.00027517215,0.00007489997,0.0037794688],"category_scores_gemma":[0.000052036783,0.00008601882,0.00024662106,0.00010946311,0.00045211505,0.000029671426,0.000065398635,0.00013065973,0.000006487748],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007740934,0.0010532705,0.42064202,0.0016627826,0.0009290521,0.000017354412,0.006886704,0.09562722,0.2102072,0.00009011434,0.14856979,0.11354042],"study_design_scores_gemma":[0.0011983957,0.0005370834,0.3204786,0.0002955973,0.00023385047,0.00004389143,0.0018289158,0.09235819,0.030343818,0.00094074773,0.5510227,0.0007181928],"about_ca_topic_score_codex":0.023761716,"about_ca_topic_score_gemma":0.0000015678509,"teacher_disagreement_score":0.40245295,"about_ca_system_score_codex":0.000005533497,"about_ca_system_score_gemma":0.0000071375785,"threshold_uncertainty_score":0.9971312},"labels":[],"label_agreement":null},{"id":"W2159236823","doi":"10.1111/j.1365-246x.2008.03726.x","title":"Use of receiver functions in wide-angle controlled-source crustal data sets","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nexen (Canada); University of Saskatchewan","funders":"","keywords":"Geology; Geodesy; Seismology; Receiver function; Geophysics; Remote sensing; Tectonics; Lithosphere","score_opus":0.05523727802556011,"score_gpt":0.2517692811605846,"score_spread":0.1965320031350245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159236823","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952765,0.00003894356,0.00058729795,0.00044961582,0.0013919737,0.00010179893,0.0006333654,0.000011923312,0.0015085626],"genre_scores_gemma":[0.9968308,0.00005956189,0.00041732632,0.00014671386,0.00052742544,7.698737e-7,0.00033712434,0.0000045249863,0.0016757406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99856085,0.00010390053,0.00042674376,0.00021194296,0.00048247434,0.00021406941],"domain_scores_gemma":[0.9989218,0.00036452015,0.00022111408,0.00022796546,0.00015201818,0.00011254533],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021695194,0.00012301437,0.0003052011,0.00011751264,0.000117271135,0.000086555694,0.00050343847,0.000049009155,0.0022155936],"category_scores_gemma":[0.00021020068,0.00009713511,0.00009947425,0.00012447877,0.000105761574,0.00087106775,0.00006588977,0.00022189782,0.00022603896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00545361,0.0017777459,0.69634604,0.00003595892,0.0015357916,0.0011008027,0.0014138974,0.075949706,0.007507747,0.0012221619,0.15539697,0.05225957],"study_design_scores_gemma":[0.0026706161,0.00016753054,0.89931655,0.000052252435,0.000046567824,0.0002166319,0.000056213095,0.021751722,0.00017182744,0.0014042546,0.07387712,0.000268726],"about_ca_topic_score_codex":0.0018545322,"about_ca_topic_score_gemma":0.00026553258,"teacher_disagreement_score":0.2029705,"about_ca_system_score_codex":0.000006937464,"about_ca_system_score_gemma":0.00008288968,"threshold_uncertainty_score":0.9986965},"labels":[],"label_agreement":null},{"id":"W2159817637","doi":"10.1002/qua.23197","title":"Outstanding questions in electron–ion energy relaxation, lattice stability, and dielectric function of warm dense matter","year":2011,"lang":"en","type":"article","venue":"International Journal of Quantum Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Warm dense matter; Dielectric; Ion; Superheating; Femtosecond; Electron; Relaxation (psychology); Condensed matter physics; Non-equilibrium thermodynamics; Lattice (music); Quantum; Chemistry; Atomic physics; Laser; Materials science; Physics; Thermodynamics; Quantum mechanics","score_opus":0.015879804712703786,"score_gpt":0.22044109547287336,"score_spread":0.20456129076016957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159817637","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971267,0.00026101028,0.00097433245,0.00010053781,0.00033658615,0.000017327658,0.00001714518,0.0000033047186,0.001163067],"genre_scores_gemma":[0.99957204,0.00012822011,0.00008213841,0.000027925958,0.00013930135,3.1883044e-7,0.000013912152,0.000002526873,0.000033591696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991846,0.000036456386,0.0003636973,0.00009174616,0.00022368343,0.0000998115],"domain_scores_gemma":[0.99930584,0.00007019452,0.00032372767,0.000055561613,0.00020049371,0.000044181957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028225654,0.000070838534,0.0001298943,0.00007102367,0.000021509444,0.000022457458,0.00012944516,0.00004862344,0.00088490633],"category_scores_gemma":[0.00005430401,0.000060916336,0.00003623279,0.0000730759,0.000033194046,0.00020446163,0.000009975522,0.00009384823,0.0000033451631],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014083269,0.00026153316,0.53868634,0.00011256429,0.0002677016,0.00006440025,0.001081971,0.00030521685,0.4521874,0.0033434855,0.00029516776,0.001985911],"study_design_scores_gemma":[0.0008038179,0.0002180794,0.5493102,0.00015367103,0.00007079346,0.00015233204,0.0001399112,0.0014834732,0.41758853,0.029237734,0.00063211296,0.00020936769],"about_ca_topic_score_codex":0.00057245593,"about_ca_topic_score_gemma":0.00005497675,"teacher_disagreement_score":0.034598876,"about_ca_system_score_codex":0.000013456581,"about_ca_system_score_gemma":0.000048050144,"threshold_uncertainty_score":0.96891034},"labels":[],"label_agreement":null},{"id":"W2160368807","doi":"10.1111/j.1365-246x.2009.04242.x","title":"Mantle reflectivity structure beneath oceanic hotspots","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Transition zone; Mantle (geology); Core–mantle boundary; Ringwoodite; Geophysics; Mantle convection; Hotspot (geology); Classification of discontinuities; Mantle plume; Mantle wedge; Seismology; Lithosphere; Tectonics","score_opus":0.00827407087636254,"score_gpt":0.2364559654151492,"score_spread":0.22818189453878668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160368807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9871296,0.000043627504,0.00023556256,0.0009801838,0.0020216804,0.000059000962,0.00019447194,0.000031623553,0.009304228],"genre_scores_gemma":[0.99581665,0.000025861485,0.00056676817,0.0005154729,0.0024912574,1.140873e-7,0.00006312017,0.0000034710151,0.00051727233],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987271,0.00005612711,0.00022564468,0.00021276897,0.0004926653,0.00028570532],"domain_scores_gemma":[0.99941003,0.00004699814,0.00013849647,0.00012348144,0.000114896546,0.00016609725],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012384173,0.00015615179,0.00019324351,0.000071678674,0.00018694095,0.00026733158,0.00040702574,0.00006275283,0.003607875],"category_scores_gemma":[0.000026681753,0.000119855,0.00011643556,0.0001070287,0.000032035096,0.00041347908,0.000014457458,0.00028508835,0.00027728957],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015664768,0.0009668157,0.04672821,0.0000323004,0.00096476614,0.0012149599,0.0010194884,0.012286416,0.22036153,0.046960182,0.04340733,0.6244915],"study_design_scores_gemma":[0.00034983712,0.0002112467,0.9096086,0.000017287948,0.0000196519,0.000153822,0.000009394486,0.0013314504,0.0019513048,0.07848843,0.007650772,0.00020818347],"about_ca_topic_score_codex":0.00009192731,"about_ca_topic_score_gemma":0.00002909203,"teacher_disagreement_score":0.8628804,"about_ca_system_score_codex":0.000010331655,"about_ca_system_score_gemma":0.000044645683,"threshold_uncertainty_score":0.99730295},"labels":[],"label_agreement":null},{"id":"W2162128595","doi":"10.1046/j.1365-246x.2002.01697.x","title":"Receiver function analysis of the North American crust and upper mantle","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Crust; Felsic; Archean; Phanerozoic; Precambrian; Mafic; Mantle (geology); Receiver function; Craton; Continental crust; Transition zone; Plate tectonics; Granulite; Geochemistry; Tectonics; Geophysics; Paleontology; Lithosphere; Structural basin; Cenozoic","score_opus":0.009339989227569286,"score_gpt":0.19661512680324644,"score_spread":0.18727513757567715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162128595","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99672306,0.000026252132,0.00006208075,0.00050826307,0.0006360061,0.000029149469,0.00011369463,0.000004560809,0.0018969502],"genre_scores_gemma":[0.9987446,0.00007202448,0.00006840476,0.00018423566,0.00035922244,2.65938e-7,0.000018803436,0.000001796814,0.0005506327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992161,0.000051442163,0.00018026735,0.00011471299,0.00032002697,0.00011747044],"domain_scores_gemma":[0.9995235,0.000054920994,0.00018143415,0.000090094385,0.000085905005,0.000064147],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006683126,0.000075212825,0.00016524468,0.00008714989,0.00010854872,0.000074153075,0.00019715636,0.000014270628,0.0028755113],"category_scores_gemma":[0.000016533213,0.000046824483,0.00012992618,0.00033387123,0.00011464427,0.00015397811,0.00002070829,0.00011196525,0.00006433736],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000064834545,0.00007931178,0.9295833,0.0000035356336,0.0012226126,0.000005647224,0.00021431272,0.0036353888,0.00051343476,0.00046007714,0.0023586117,0.06185892],"study_design_scores_gemma":[0.0000893217,0.000047812304,0.9854014,0.0000034695536,0.00020304939,0.0000053798003,0.000018033003,0.008274941,0.000038478644,0.0002763576,0.005582343,0.000059436512],"about_ca_topic_score_codex":0.0006141851,"about_ca_topic_score_gemma":0.00043447388,"teacher_disagreement_score":0.06179948,"about_ca_system_score_codex":0.0000030390574,"about_ca_system_score_gemma":0.0000058382834,"threshold_uncertainty_score":0.99803597},"labels":[],"label_agreement":null},{"id":"W2162559162","doi":"10.1109/hpcs.2008.26","title":"Exploring the High Pressure Phase Diagrams of Light Elements Using Large Scale Ab-initio Molecular Dynamics Simulations","year":2008,"lang":"en","type":"article","venue":"Proceedings/Proceedings (International Symposium on High Performance Computing Systems and Applications)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Molecular dynamics; Phase diagram; Ab initio; Scale (ratio); Statistical physics; Dynamics (music); Ab initio quantum chemistry methods; Phase (matter); Chemical physics; Physics; Computational chemistry; Chemistry; Molecule; Quantum mechanics","score_opus":0.02082941296843017,"score_gpt":0.2358465655758445,"score_spread":0.21501715260741433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162559162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99625224,0.000085804895,0.00068070757,0.0002152456,0.00052079855,0.0007965972,0.00030798002,0.00008507246,0.0010555349],"genre_scores_gemma":[0.9982251,0.00015311182,0.00051477604,0.000050253177,0.0007721018,0.000051563133,0.00014926105,0.000019921037,0.000063891486],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9977918,0.00000853535,0.0006870724,0.0004990166,0.00063146546,0.00038206056],"domain_scores_gemma":[0.9986024,0.00005614558,0.00056395534,0.00012505583,0.00054103916,0.00011142414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039731892,0.00028777492,0.00033724378,0.00013031198,0.0009099701,0.0002517627,0.00047825486,0.00007308515,0.000022271815],"category_scores_gemma":[0.000012782678,0.00023323743,0.00005888572,0.00035676136,0.00009448347,0.0006472844,0.00008262827,0.00018067443,0.000012470295],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045513676,0.0013891514,0.5515052,0.0026553697,0.0009809725,0.000005773949,0.007038446,0.15984997,0.12903523,0.1386172,0.00044698128,0.008020554],"study_design_scores_gemma":[0.0016917242,0.00027934855,0.03862712,0.00045683119,0.00015413745,0.00007017598,0.0005404495,0.93446106,0.013938578,0.00022098115,0.008924523,0.00063506654],"about_ca_topic_score_codex":0.0003139063,"about_ca_topic_score_gemma":0.000004362968,"teacher_disagreement_score":0.7746111,"about_ca_system_score_codex":0.00003096798,"about_ca_system_score_gemma":0.000028077095,"threshold_uncertainty_score":0.95111465},"labels":[],"label_agreement":null},{"id":"W2162720913","doi":"10.1139/v07-096","title":"Examining the structural changes in Fe<sub>2</sub>(CO)<sub>9</sub> under high external pressures by Raman spectroscopy","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Raman spectroscopy; Chemistry; Diamond anvil cell; Metal; Phase (matter); High pressure; Crystallography; Spectroscopy; Analytical Chemistry (journal); Structural change; Thermodynamics","score_opus":0.009367163419423587,"score_gpt":0.20055772914840972,"score_spread":0.19119056572898613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162720913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969391,0.0012772889,0.000028775268,0.0002989411,0.0005914242,0.000075608186,0.00017388549,0.00000639432,0.0006085575],"genre_scores_gemma":[0.9985346,0.00006507218,0.00004410056,0.00022893405,0.0010431912,4.6056016e-7,0.00003924981,0.000010890639,0.000033494714],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9983766,0.000053165077,0.00038912136,0.00020976808,0.00031982452,0.0006515023],"domain_scores_gemma":[0.99874276,0.000121805395,0.0003090918,0.00019900071,0.000063679865,0.0005636404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000623281,0.00022419001,0.00030555404,0.00007792518,0.00020077599,0.00022112687,0.0004965058,0.00013811052,0.00048773113],"category_scores_gemma":[0.00003928137,0.00017104467,0.000058782905,0.00013523322,0.00014530722,0.00017183051,0.000009053577,0.00039333495,0.000011821052],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038917817,0.0000031359825,0.011753206,0.000029884108,0.000036265068,0.00019845348,0.00022422422,0.00035036783,0.9822352,0.0000046927366,0.0021917424,0.0029338917],"study_design_scores_gemma":[0.0002929518,0.00004552316,0.14306132,0.000069584334,0.000020751135,0.00011322434,0.0001840625,0.000015624923,0.85487384,0.00050421036,0.0006326898,0.00018619785],"about_ca_topic_score_codex":0.0044515547,"about_ca_topic_score_gemma":0.040326327,"teacher_disagreement_score":0.13130811,"about_ca_system_score_codex":0.000031545627,"about_ca_system_score_gemma":0.00034837454,"threshold_uncertainty_score":0.9771852},"labels":[],"label_agreement":null},{"id":"W2164207654","doi":"10.1029/2006jb004861","title":"Lithospheric variations across the Superior Province, Ontario, Canada: Evidence from tomography and shear wave splitting","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Western University; Université du Québec à Montréal; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Shear wave splitting; Seismology; Crust; Shear (geology); Rift; Seismic tomography; Tectonics; Shear zone; Shear velocity; Geophysics; Geodesy; Mantle (geology); Petrology; Physics","score_opus":0.028756546527365548,"score_gpt":0.2800530623343392,"score_spread":0.25129651580697365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164207654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970583,0.00125536,0.0001761458,0.00055847404,0.0003692373,0.0002158646,0.000055785662,0.000006602847,0.00030424283],"genre_scores_gemma":[0.9958015,0.000083352264,0.0027984784,0.00007280058,0.0008451102,0.0000010437665,0.000004395019,0.0000069522084,0.00038634398],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9968403,0.00027834173,0.0005252864,0.00026575764,0.0013349142,0.0007553758],"domain_scores_gemma":[0.9957246,0.0029657267,0.00021244002,0.00027010654,0.00044814654,0.0003789395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025741465,0.00017041806,0.00034829005,0.00001035773,0.0006684613,0.00038019285,0.00047212173,0.00006888421,0.00090734725],"category_scores_gemma":[0.00054772245,0.000104173174,0.0001045842,0.00043391032,0.00030683333,0.000487264,0.00009118791,0.00070303545,0.000013829568],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016536167,0.0002192058,0.84329635,0.000111795925,0.0005729365,0.0010674986,0.0074987994,0.0005709201,0.007394399,0.00074894284,0.007694213,0.12917134],"study_design_scores_gemma":[0.00019819844,0.00033238085,0.9874366,0.00011341945,0.000023319424,0.0000124515645,0.0007079674,0.00036858584,0.00052862265,0.0018422187,0.008306059,0.00013021052],"about_ca_topic_score_codex":0.97986037,"about_ca_topic_score_gemma":0.97395617,"teacher_disagreement_score":0.14414023,"about_ca_system_score_codex":0.00004873849,"about_ca_system_score_gemma":0.001477033,"threshold_uncertainty_score":0.9934816},"labels":[],"label_agreement":null},{"id":"W2164256893","doi":"10.1088/0953-8984/21/37/375101","title":"Estimating the quantum effects from molecular vibrations of water under high pressures and temperatures","year":2009,"lang":"en","type":"article","venue":"Journal of Physics Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Research Council Canada","keywords":"Quantum; Equation of state; Ab initio; Molecular dynamics; Electron; Vibration; Density functional theory; Ion; Simple (philosophy); Physics; Thermodynamics; Materials science; Quantum mechanics","score_opus":0.005119929024448666,"score_gpt":0.20106838384294878,"score_spread":0.19594845481850012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164256893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99609226,0.00022181218,0.0019730031,0.0011421238,0.00037318614,0.00008766042,0.000034483302,0.0000041944804,0.00007125811],"genre_scores_gemma":[0.99737114,0.000002908507,0.0012430354,0.0010256902,0.0003195519,2.5324005e-7,0.00001613424,0.000003956385,0.000017321501],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991535,0.000108992775,0.00026993413,0.00009923757,0.00022605853,0.00014228113],"domain_scores_gemma":[0.99936414,0.00015964692,0.00020185798,0.00014149034,0.00008439779,0.000048492202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014255116,0.00011789903,0.0002551988,0.00002470796,0.00009037237,0.00012245761,0.00015312777,0.000036937665,0.00023384343],"category_scores_gemma":[0.000008716778,0.00006226464,0.00006378495,0.00003810045,0.00006017097,0.00021336526,0.000010752577,0.00012781036,0.00001634458],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058787366,0.00003776705,0.0019516225,0.000045663288,0.00017248956,0.000023897113,0.0006234379,0.019890444,0.9732555,0.0015188291,0.001842772,0.00057877164],"study_design_scores_gemma":[0.0007096309,0.0002692691,0.19184496,0.00012366884,0.00024175552,0.000018689017,0.000038604507,0.0019929274,0.5607759,0.2436905,0.000081024446,0.00021312408],"about_ca_topic_score_codex":0.00017334262,"about_ca_topic_score_gemma":0.000004457625,"teacher_disagreement_score":0.41247967,"about_ca_system_score_codex":9.089961e-7,"about_ca_system_score_gemma":0.000018251658,"threshold_uncertainty_score":0.25604215},"labels":[],"label_agreement":null},{"id":"W2164320268","doi":"10.1086/321487","title":"Phase‐dependent Spectral Variability in 4U 1907+09","year":2001,"lang":"en","type":"article","venue":"The Astrophysical Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; McGill University","funders":"","keywords":"Physics; Astrophysics; Pulsar; Flux (metallurgy); Neutron star; Orbit (dynamics); Sky; Light curve; Spectral line; X-ray binary; Astronomy; Absorption (acoustics); Flare; X-ray pulsar; Optics","score_opus":0.010757701536439922,"score_gpt":0.23008921726224138,"score_spread":0.21933151572580145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164320268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99506605,0.000019021685,0.0018920994,0.00064408686,0.0005389754,0.000103357685,0.000032209267,0.000014065317,0.0016901359],"genre_scores_gemma":[0.997828,0.000032814296,0.000485444,0.00008055578,0.0014599841,6.502648e-7,0.000008926004,0.000003633564,0.000099979385],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998393,0.00036860126,0.00028359765,0.00017857253,0.0003488814,0.00042736926],"domain_scores_gemma":[0.9993516,0.0001458836,0.00010106816,0.0002198645,0.000028234921,0.00015334498],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006958475,0.00014019749,0.00023269259,0.000031668696,0.000183156,0.00016843098,0.00039909614,0.000034837944,0.0019031756],"category_scores_gemma":[0.000031536638,0.000083492145,0.00009529871,0.00015368187,0.00008815055,0.00020309868,0.00002056202,0.00038213923,0.0003776876],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0034207986,0.0037538297,0.10363,0.000033797165,0.0003278339,0.0017172399,0.0016031701,0.030285764,0.18230504,0.010779723,0.0024402267,0.6597026],"study_design_scores_gemma":[0.004175296,0.0015219449,0.90087134,0.000042823936,0.00008767662,0.00043148888,0.00017500049,0.006650123,0.0027167283,0.0777234,0.005043311,0.00056086096],"about_ca_topic_score_codex":0.0007028539,"about_ca_topic_score_gemma":0.00014235487,"teacher_disagreement_score":0.79724133,"about_ca_system_score_codex":0.000008202241,"about_ca_system_score_gemma":0.00005089398,"threshold_uncertainty_score":0.9990092},"labels":[],"label_agreement":null},{"id":"W2164692278","doi":"10.1785/0120080341","title":"Lg Attenuation near the North Korean Border with China, Part II: Model Development from the 2006 Nuclear Explosion in North Korea","year":2009,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; Chinese Academy of Sciences","keywords":"China; Attenuation; Seismology; Geology; Nuclear explosion; Geography; Physics; Nuclear physics; Archaeology; Optics","score_opus":0.010862570910940535,"score_gpt":0.18883553656508315,"score_spread":0.1779729656541426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164692278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96979004,0.00007163528,0.00012445035,0.029340135,0.000042038017,0.00026292654,0.00009410895,0.000014691404,0.00025999907],"genre_scores_gemma":[0.9846727,0.00008993184,0.005982556,0.008971565,0.00005085093,0.0000025160693,0.00008571533,0.000004135737,0.00014002516],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9987439,0.00013908243,0.000294163,0.00022651808,0.00035932838,0.00023700751],"domain_scores_gemma":[0.9992565,0.00011026407,0.00026265052,0.00029297138,0.000039147228,0.00003849662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020913192,0.00015748589,0.00026632933,0.0000041248936,0.0004966039,0.00003304363,0.0005218883,0.000058931575,0.00053935696],"category_scores_gemma":[0.000021336076,0.00006499213,0.000116863834,0.00017674,0.00045435925,0.000024032697,0.000069032976,0.00016902515,0.000022097984],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070494885,0.0007477085,0.18931997,0.00003187997,0.00023044208,0.0000038021399,0.022575881,0.46188915,0.00015818443,0.00008953338,0.24183758,0.08241095],"study_design_scores_gemma":[0.00020082861,0.00019841416,0.7859668,0.00002086957,0.000021064641,5.568622e-7,0.00019164805,0.0058464603,0.000041103674,0.00022006172,0.20717452,0.00011767635],"about_ca_topic_score_codex":0.013158569,"about_ca_topic_score_gemma":0.00012228424,"teacher_disagreement_score":0.59664685,"about_ca_system_score_codex":0.0000045046627,"about_ca_system_score_gemma":0.00004859589,"threshold_uncertainty_score":0.9934129},"labels":[],"label_agreement":null},{"id":"W2164799651","doi":"10.4401/ag-6603","title":"Tomography of core-mantle boundary and lowermost mantle coupled by geodynamics: joint models of shear and compressional velocity","year":2015,"lang":"en","type":"article","venue":"Annals of Geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Seismic tomography; Geodynamics; Core–mantle boundary; Geophysics; Scaling; Cosmic microwave background; Seismology; Shear velocity; Geodesy; Physics; Tectonics; Geometry; Mechanics; Anisotropy","score_opus":0.047723348395955656,"score_gpt":0.24754260283995316,"score_spread":0.1998192544439975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164799651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99596095,0.0014063757,0.00016981286,0.000063064486,0.00013890305,0.00013800342,0.0015959021,0.00000852373,0.00051846233],"genre_scores_gemma":[0.998837,0.0003611247,0.00045300083,0.00006342857,0.000038124075,7.1810837e-7,0.00021002699,0.0000055848263,0.000031007265],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988425,0.000038531103,0.00035672716,0.00021204706,0.00034083278,0.0002093882],"domain_scores_gemma":[0.99906904,0.000073857984,0.00027494214,0.0001983333,0.00023559238,0.0001482316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002775758,0.00015496655,0.00047647205,0.00005093898,0.000058711175,0.000021835565,0.00013577545,0.000069384136,0.000047081045],"category_scores_gemma":[0.000011426912,0.0001328359,0.00006651095,0.00012568691,0.00039530676,0.0002306791,0.00005759688,0.00006862208,0.000003050086],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0076169856,0.004891778,0.19022144,0.009315969,0.0038324052,0.00011120402,0.018314768,0.060290888,0.49049118,0.039814394,0.08283003,0.09226896],"study_design_scores_gemma":[0.0032657457,0.0026801622,0.3885764,0.000640638,0.0002371116,0.000016091386,0.0006195561,0.291822,0.04490992,0.26279667,0.0030568796,0.0013788379],"about_ca_topic_score_codex":0.0038188228,"about_ca_topic_score_gemma":0.000042663865,"teacher_disagreement_score":0.44558126,"about_ca_system_score_codex":5.950976e-7,"about_ca_system_score_gemma":0.000063783446,"threshold_uncertainty_score":0.5772943},"labels":[],"label_agreement":null},{"id":"W2165380249","doi":"10.1002/cphc.200500117","title":"Phase Stability and Broken‐Symmetry Transition of Elemental Lithium up to 140 GPa","year":2005,"lang":"en","type":"article","venue":"ChemPhysChem","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Steacie Institute for Molecular Sciences","funders":"","keywords":"Lithium (medication); Annealing (glass); Phase transition; Materials science; Condensed matter physics; Transition metal; Phase (matter); Symmetry (geometry); Phonon; High pressure; Structural stability; Chemical physics; Symmetry breaking; Electronic structure; Crystallography; Chemistry; Engineering physics; Physics; Metallurgy; Quantum mechanics; Catalysis","score_opus":0.01420996718786901,"score_gpt":0.23798365608313893,"score_spread":0.2237736888952699,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165380249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971619,0.000097573204,0.00007176668,0.00031828423,0.00013056789,0.00016416454,0.00043047016,0.000021693944,0.0016035789],"genre_scores_gemma":[0.99854255,0.0000119504,0.0008106881,0.00019877781,0.00022097828,0.0000017203113,0.00014872642,0.000003326293,0.00006129104],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991905,0.000023851935,0.00020935234,0.00022332268,0.00016073344,0.00019225541],"domain_scores_gemma":[0.9995941,0.000032465487,0.000050081937,0.00015747214,0.000033562254,0.00013230537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019739947,0.00011333775,0.00019165428,0.000028367935,0.000051012757,0.000027604145,0.00009168104,0.00004567404,0.001397836],"category_scores_gemma":[0.000009291298,0.000101733225,0.000040369654,0.00010208597,0.00005104637,0.0001746816,0.000010416249,0.00004708012,0.000050800547],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036098386,0.0003269134,0.0035144698,0.00022852384,0.000051733823,0.0000021487817,0.003322585,0.000043590255,0.94084084,0.00016615845,0.0024343275,0.04870771],"study_design_scores_gemma":[0.00094601116,0.00020055463,0.005427045,0.000012443466,0.000019747717,0.0000014843531,0.00019478475,0.00030620868,0.98010546,0.00013617819,0.01249929,0.0001508073],"about_ca_topic_score_codex":0.00028999464,"about_ca_topic_score_gemma":0.00007417324,"teacher_disagreement_score":0.0485569,"about_ca_system_score_codex":0.0000032025107,"about_ca_system_score_gemma":0.000019731668,"threshold_uncertainty_score":0.999515},"labels":[],"label_agreement":null},{"id":"W2166438801","doi":"10.1093/gji/ggt266","title":"Multiresolution imaging of mantle reflectivity structure using SS and P'P' precursors","year":2013,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Transition zone; Geology; Mantle (geology); Subduction; Receiver function; Seismology; Hotspot (geology); Mantle wedge; Discontinuity (linguistics); Mineralogy; Lithosphere; Geophysics; Tectonics","score_opus":0.009945781973770499,"score_gpt":0.23799195481954907,"score_spread":0.22804617284577858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166438801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977391,0.000051525367,0.000334168,0.0001668161,0.0010948248,0.00006565167,0.00008073811,0.000007220247,0.000459987],"genre_scores_gemma":[0.9980253,0.000010145295,0.0013139471,0.000036160374,0.00052435667,2.3681967e-7,0.000016506314,0.0000028942316,0.00007043076],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999218,0.000053218628,0.00018666941,0.00012786713,0.00025765965,0.00015661524],"domain_scores_gemma":[0.99951524,0.000050348197,0.00015750878,0.000059063837,0.0001352727,0.00008255235],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000085845364,0.00009089252,0.00013635222,0.000056904348,0.00010061268,0.00012685936,0.00014113472,0.00002855926,0.0010923096],"category_scores_gemma":[0.000025142368,0.00007119345,0.000045695193,0.000051507417,0.00006934481,0.0004974967,0.000024261279,0.00012875501,0.000022029246],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001898869,0.00015909405,0.2738976,0.000060720493,0.00031385708,0.00003309001,0.00080502953,0.008468557,0.60169715,0.0017391909,0.0017273468,0.11090853],"study_design_scores_gemma":[0.00035492715,0.000049488335,0.89277345,0.000044280987,0.000023692377,0.00010807862,0.000047552046,0.07816605,0.007442215,0.020340238,0.00048820916,0.00016181538],"about_ca_topic_score_codex":0.0019786693,"about_ca_topic_score_gemma":0.000043647866,"teacher_disagreement_score":0.61887586,"about_ca_system_score_codex":0.0000059074105,"about_ca_system_score_gemma":0.000021842674,"threshold_uncertainty_score":0.9998208},"labels":[],"label_agreement":null},{"id":"W2168810179","doi":"10.1103/physrevlett.108.045503","title":"Persistence and Eventual Demise of Oxygen Molecules at Terapascal Pressures","year":2012,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"Engineering and Physical Sciences Research Council","keywords":"Solid oxygen; Materials science; Oxygen; Superconductivity; Electronic band structure; Electronic structure; Chemical physics; Density functional theory; Condensed matter physics; Molecule; Metal; Computational chemistry; Chemistry; Physics; Quantum mechanics; Metallurgy","score_opus":0.017380020175758373,"score_gpt":0.23771326682394014,"score_spread":0.22033324664818177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168810179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97461087,0.023973525,0.000013819428,0.00069388107,0.000107356675,0.00017137954,0.00006291566,0.000011298432,0.0003549831],"genre_scores_gemma":[0.99572414,0.0022468246,0.00016274516,0.0016116061,0.00020452299,0.0000029827345,0.000027226875,0.0000034391176,0.00001650777],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99911153,0.00009969865,0.00016425083,0.00016056345,0.00020980355,0.00025413293],"domain_scores_gemma":[0.99950016,0.000102416714,0.00009023047,0.00015381808,0.000015277952,0.00013810619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015964743,0.00012566574,0.0003170612,0.000012589202,0.000053020394,0.000012447072,0.00013776623,0.00000945872,0.00019596601],"category_scores_gemma":[0.000027520824,0.000091313006,0.00009380786,0.000059985192,0.000104407845,0.00016797266,0.00003310032,0.00004798427,0.000076797616],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026951137,0.0006081962,0.2621619,0.014958996,0.00077051943,0.000027894492,0.004871344,0.0014586621,0.6026773,0.0013723057,0.046244185,0.0645792],"study_design_scores_gemma":[0.00042915117,0.00015853145,0.8938689,0.0012709599,0.00056173076,0.000019142835,0.00002242075,0.0014323888,0.0061850995,0.00018950335,0.09513775,0.00072440784],"about_ca_topic_score_codex":0.00009757374,"about_ca_topic_score_gemma":0.000005072325,"teacher_disagreement_score":0.631707,"about_ca_system_score_codex":0.0000015674469,"about_ca_system_score_gemma":0.000004841933,"threshold_uncertainty_score":0.37236366},"labels":[],"label_agreement":null},{"id":"W2171247886","doi":"10.1093/jxb/erl190","title":"Further quantification of the role of internal unstirred layers during the measurement of transport coefficients in giant internodes of Chara by a new stop-flow technique","year":2006,"lang":"en","type":"article","venue":"Journal of Experimental Botany","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Waterloo; Deutscher Akademischer Austauschdienst","keywords":"Plant stem; Chara; Flow (mathematics); Botany; Environmental science; Chemistry; Biology; Mechanics; Physics","score_opus":0.00831160957441205,"score_gpt":0.2082496738479385,"score_spread":0.19993806427352645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171247886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973822,0.0017229827,0.00028046395,0.000028318198,0.00016619446,0.00018216786,0.00007417545,0.0000013780398,0.00016208198],"genre_scores_gemma":[0.9997619,0.000015750004,0.00016732351,0.000003360013,0.000026080988,7.9048067e-7,0.0000014022434,0.0000034919783,0.00001990463],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99863225,0.00006034377,0.0006678644,0.00007878939,0.00045986302,0.000100861],"domain_scores_gemma":[0.99905807,0.000014997294,0.0006964896,0.00012915056,0.0000749811,0.000026342615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042323006,0.00009041881,0.00025731837,0.00005172608,0.00001900078,0.0000061537435,0.00030995204,0.000033139437,0.00013290306],"category_scores_gemma":[0.0000054193742,0.000053253803,0.00011299823,0.00010243296,0.00009548464,0.00008080581,0.00001056114,0.000070239126,3.7988684e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030478177,0.00015685847,0.01939322,0.0000129610835,0.000030527463,9.05764e-7,0.00095897354,0.0008179363,0.9780032,0.000017472421,0.000022028915,0.00028111023],"study_design_scores_gemma":[0.00038876917,0.00013176218,0.07851715,0.00021363074,0.000013856783,0.0000048020684,0.00063716655,0.00024050666,0.91964453,0.00004438471,0.00011792911,0.00004550734],"about_ca_topic_score_codex":0.002904172,"about_ca_topic_score_gemma":0.0001848077,"teacher_disagreement_score":0.05912393,"about_ca_system_score_codex":0.000011911182,"about_ca_system_score_gemma":0.000046473506,"threshold_uncertainty_score":0.43902588},"labels":[],"label_agreement":null},{"id":"W2181016351","doi":"10.1002/2015jb012228","title":"Variability and origin of seismic anisotropy across eastern Canada: Evidence from shear wave splitting measurements","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Leverhulme Trust","keywords":"Lithosphere; Geology; Seismic anisotropy; Shear wave splitting; Anisotropy; Geophysics; Mantle (geology); Seismology; Tectonics; Shear (geology); Petrology; Physics","score_opus":0.15346457239793038,"score_gpt":0.3517145771071379,"score_spread":0.1982500047092075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181016351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986008,0.00020355005,0.00013858418,0.00021381388,0.00038285,0.0001428539,0.00015047759,0.00000392493,0.00016317928],"genre_scores_gemma":[0.998288,0.000047473844,0.00089268154,0.000029596813,0.0006523423,4.3519248e-7,0.000006039392,0.0000055442497,0.00007788512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99572784,0.0007549611,0.0005856405,0.00027320802,0.0020666495,0.00059169444],"domain_scores_gemma":[0.9968339,0.0009393156,0.00030050552,0.00027395738,0.0010437494,0.0006085751],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0042892653,0.0001579669,0.0005547534,0.00004908788,0.00014774816,0.00013277166,0.00035623673,0.000055016157,0.000121744655],"category_scores_gemma":[0.0014571561,0.00011837822,0.00007313039,0.0002383275,0.00023330253,0.00046982453,0.00009556313,0.00043958568,0.000026085168],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033191997,0.00042365046,0.89255506,0.0004247885,0.00062585576,0.00047232467,0.0050700004,0.00969211,0.04442833,0.00012865468,0.0020356018,0.040824436],"study_design_scores_gemma":[0.0010143343,0.001006175,0.9634338,0.0004006357,0.00003967453,0.000015941936,0.0005010856,0.018794635,0.00763286,0.005370274,0.0015385738,0.000251978],"about_ca_topic_score_codex":0.57880515,"about_ca_topic_score_gemma":0.04274665,"teacher_disagreement_score":0.5360585,"about_ca_system_score_codex":0.00002576597,"about_ca_system_score_gemma":0.001361485,"threshold_uncertainty_score":0.9747207},"labels":[],"label_agreement":null},{"id":"W2184769552","doi":"10.1063/1.4936849","title":"High pressure–low temperature phase diagram of barium: Simplicity versus complexity","year":2015,"lang":"en","type":"article","venue":"Applied Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Ottawa","funders":"","keywords":"Barium; Phase diagram; Phase (matter); Diagram; Materials science; Atmospheric temperature range; Thermodynamics; High pressure; Yield (engineering); Chemistry; Physics; Metallurgy; Mathematics","score_opus":0.02801643365671541,"score_gpt":0.23729950910582856,"score_spread":0.20928307544911315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184769552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961654,0.000027092528,0.00027561866,0.0002901512,0.0009476518,0.00033373604,0.0008346244,0.00006640096,0.0010593036],"genre_scores_gemma":[0.9973203,0.000002961901,0.00059048994,0.0005221324,0.0007578836,0.0000062437425,0.0007790997,0.000010478681,0.000010409798],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985206,0.000060835697,0.0002676135,0.00035732193,0.0004170191,0.00037661605],"domain_scores_gemma":[0.9990223,0.00010181686,0.00017626426,0.0004273587,0.00006393153,0.00020831058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018352173,0.00025676104,0.00043360904,0.000026275955,0.00010292529,0.00007785156,0.00036032096,0.00008446473,0.00014947854],"category_scores_gemma":[0.0000093603,0.0002245621,0.0000791378,0.00020869526,0.00020831941,0.0001590588,0.000037547667,0.00017495416,0.00011080194],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024231777,0.0006119714,0.001154827,0.00026897172,0.00061470165,0.000018886047,0.001119977,0.10250344,0.7880905,0.037322573,0.057947442,0.007923474],"study_design_scores_gemma":[0.0386816,0.0017895084,0.051465802,0.00010593448,0.0013010643,0.0000054193947,0.00034850408,0.005726645,0.8204328,0.03022527,0.04542617,0.00449131],"about_ca_topic_score_codex":0.0016286524,"about_ca_topic_score_gemma":0.000065463864,"teacher_disagreement_score":0.0967768,"about_ca_system_score_codex":0.000003919959,"about_ca_system_score_gemma":0.00004562855,"threshold_uncertainty_score":0.9157377},"labels":[],"label_agreement":null},{"id":"W2185320370","doi":"10.1007/978-3-030-10475-7_64-1","title":"Energy Budget of the Earth","year":2011,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Earth's internal heat budget; Mantle (geology); Radiogenic nuclide; Energy budget; Heat flow; Geology; Lithosphere; Mantle convection; Geophysics; Crust; Planetary differentiation; Earth science; Thermal; Thermodynamics; Physics; Tectonics; Seismology","score_opus":0.014760925631804676,"score_gpt":0.20151191719286368,"score_spread":0.186750991561059,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2185320370","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.047345027,0.002459553,0.000022395558,0.00014782278,0.004781372,0.0006516446,0.0010686459,0.000056785873,0.9434668],"genre_scores_gemma":[0.3468553,0.039052937,0.007954477,0.0002877831,0.0018369071,0.000017588756,0.00014038014,0.00009187628,0.60376275],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9917016,0.00025329855,0.002247537,0.0015683298,0.0029648305,0.0012644071],"domain_scores_gemma":[0.9943386,0.0005571075,0.0029170215,0.0012743891,0.00050862634,0.0004042794],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021450634,0.0010396771,0.0018538723,0.00067050074,0.0008785855,0.00012662436,0.0039999653,0.0005440528,0.009869229],"category_scores_gemma":[0.00021372772,0.0007145938,0.00069433905,0.0011997102,0.009452623,0.0014615674,0.0004556808,0.00047432203,0.0001294788],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086981716,0.00068969454,0.1876416,0.002418356,0.0009329677,0.00010950842,0.009230181,0.0064460617,0.002656683,0.7144849,0.0070766495,0.06744359],"study_design_scores_gemma":[0.00060971704,0.003312163,0.084383465,0.0009832698,0.00033101227,0.00004885937,0.00031023976,0.00014926353,0.005402344,0.062819324,0.8396834,0.001966906],"about_ca_topic_score_codex":0.0043929247,"about_ca_topic_score_gemma":0.012445445,"teacher_disagreement_score":0.8326068,"about_ca_system_score_codex":0.0000016072636,"about_ca_system_score_gemma":0.0019839874,"threshold_uncertainty_score":0.9995305},"labels":[],"label_agreement":null},{"id":"W2187117077","doi":"","title":"A brief comparison of the frequency spectra from the Hussar 2011 and Priddis 2012 test shoots and the theoretical predictions of the Sharpe Hollow Cavity Model","year":2012,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Spectral line; Explosive material; Computational physics; Physics; Low frequency; Environmental science; Statistics; Materials science; Chemistry; Mathematics; Quantum mechanics","score_opus":0.01299818889661648,"score_gpt":0.21192797979137923,"score_spread":0.19892979089476276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2187117077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98480415,0.001301124,0.0002431955,0.002554682,0.0003529224,0.00047992455,0.0014865763,0.000011649898,0.008765751],"genre_scores_gemma":[0.9992804,0.00006904576,0.0001893112,0.00013863594,0.00013490369,0.0000027013068,0.000011452352,0.000003297335,0.00017024441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99891967,0.00020667975,0.000251347,0.00014693441,0.000258421,0.00021697978],"domain_scores_gemma":[0.99863434,0.00069082796,0.00013312403,0.00044339077,0.00003161395,0.00006668298],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053490367,0.00012655594,0.00023832847,0.0000074618647,0.00031487798,0.00004624622,0.00039366557,0.00006057277,0.0011368751],"category_scores_gemma":[0.000079235724,0.000043801276,0.00007142649,0.00007428969,0.0011916292,0.00016581651,0.00008108541,0.00015025756,0.0000070971178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006309498,0.00012646124,0.87762827,0.000018000701,0.00008650186,8.607505e-8,0.0033882812,0.00048117083,0.0017861938,0.10995421,0.0061092176,0.00035849822],"study_design_scores_gemma":[0.00034850213,0.000028109669,0.9476339,0.000017043565,0.0001554676,0.0000021169135,0.00016494002,0.021883415,0.0013448361,0.02804542,0.0002894938,0.000086746644],"about_ca_topic_score_codex":0.006867366,"about_ca_topic_score_gemma":0.001597551,"teacher_disagreement_score":0.08190879,"about_ca_system_score_codex":0.0000011176717,"about_ca_system_score_gemma":0.000034923236,"threshold_uncertainty_score":0.99977624},"labels":[],"label_agreement":null},{"id":"W2190598423","doi":"10.1039/c5ja00261c","title":"Bulk sensitive determination of the Fe<sup>3+</sup>/Fe<sub>Tot</sub>-ratio in minerals by Fe L<sub>2/3</sub>-edge X-ray Raman scattering","year":2015,"lang":"en","type":"article","venue":"Journal of Analytical Atomic Spectrometry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Bundesministerium für Bildung und Forschung; European Synchrotron Radiation Facility","keywords":"Analytical Chemistry (journal); X-ray; Materials science; Scattering; Raman scattering; Chemistry; Raman spectroscopy; Physics; Optics","score_opus":0.011349517131570598,"score_gpt":0.22303756677947462,"score_spread":0.21168804964790403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2190598423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99740666,0.00014665097,0.00053280947,0.00081366947,0.00046231152,0.00017621061,0.0000888321,0.000010743193,0.00036211754],"genre_scores_gemma":[0.9988256,0.000067965935,0.0002934191,0.0001823982,0.0005471864,5.7159724e-7,0.000021220036,0.000013663846,0.00004796953],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9970885,0.0002905737,0.0010211878,0.00030931816,0.0007975749,0.00049287715],"domain_scores_gemma":[0.9981743,0.00032569972,0.00063883845,0.00028446698,0.00025573166,0.0003209409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013662078,0.00029309888,0.00077538285,0.0004415771,0.0000891535,0.00015273571,0.00042738966,0.00016507479,0.00007193585],"category_scores_gemma":[0.00031824622,0.00021073874,0.0002615988,0.00083422434,0.00023617763,0.00045811222,0.000056911926,0.00042708375,0.000072068244],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027037982,0.000164301,0.013942893,0.00006677526,0.00017973015,0.0001275892,0.00050348253,0.0031607207,0.9753288,0.0001520182,0.002969723,0.0031335668],"study_design_scores_gemma":[0.0021919373,0.0006398977,0.100660674,0.00029350782,0.0003234449,0.00023406706,0.00061134953,0.07299941,0.8184004,0.0025606705,0.0004309087,0.00065374677],"about_ca_topic_score_codex":0.00023981874,"about_ca_topic_score_gemma":0.0001274004,"teacher_disagreement_score":0.15692843,"about_ca_system_score_codex":0.00008059701,"about_ca_system_score_gemma":0.00019796305,"threshold_uncertainty_score":0.8593676},"labels":[],"label_agreement":null},{"id":"W2193331770","doi":"10.1093/gji/ggv364","title":"Extraction of weak<i>PcP</i>phases using the slant-stacklet transform – II: constraints on lateral variations of structure near the core–mantle boundary","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mantle (geology); Core–mantle boundary; Geology; Amplitude; Cosmic microwave background; Coda; Geophysics; Inner core; Waveform; Geodesy; Seismology; Physics; Anisotropy; Optics","score_opus":0.03085429144108503,"score_gpt":0.2793314175421674,"score_spread":0.24847712610108236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2193331770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938741,0.000028663571,0.00068525615,0.00088645756,0.0018447805,0.00011373941,0.0010210772,0.0000061583364,0.0015397744],"genre_scores_gemma":[0.99866635,0.000009044611,0.000313128,0.00011053999,0.00072884845,3.7316738e-7,0.00008172845,0.0000038078344,0.00008620294],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99874043,0.00007653039,0.0003443971,0.00011112858,0.00056621846,0.00016128986],"domain_scores_gemma":[0.99911726,0.00016922317,0.00029475192,0.00011761079,0.00022497588,0.0000761839],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025816445,0.00011865323,0.00017776506,0.000039862363,0.00037335372,0.0001683904,0.0003417427,0.00004632211,0.00129252],"category_scores_gemma":[0.000038489772,0.000064702086,0.000108690234,0.00008973892,0.00036152685,0.0002620931,0.000016176036,0.00023607843,0.0000105466825],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00577699,0.002181031,0.019746512,0.00013158565,0.004044747,0.00018550438,0.02449695,0.23885149,0.42012593,0.09085071,0.025497641,0.1681109],"study_design_scores_gemma":[0.0072563086,0.0035415085,0.35813653,0.00055237004,0.0006995459,0.0018676574,0.0020853444,0.16714247,0.048488103,0.28437895,0.1244316,0.0014196098],"about_ca_topic_score_codex":0.00064916286,"about_ca_topic_score_gemma":0.00007569418,"teacher_disagreement_score":0.37163782,"about_ca_system_score_codex":0.000009153036,"about_ca_system_score_gemma":0.00020231347,"threshold_uncertainty_score":0.99962044},"labels":[],"label_agreement":null},{"id":"W2217704384","doi":"10.1002/2015gc006088","title":"<i>SKS</i> splitting beneath <scp>T</scp>ransportable <scp>A</scp>rray stations in eastern <scp>N</scp>orth <scp>A</scp>merica and the signature of past lithospheric deformation","year":2015,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Lithosphere; Lineation; Seismology; Asthenosphere; Anisotropy; Mantle (geology); Seismic anisotropy; Shear wave splitting; Geophysics; Tectonics","score_opus":0.00892809820687172,"score_gpt":0.1928181034638615,"score_spread":0.18389000525698979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2217704384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97130454,0.003789905,0.0003833266,0.000032729713,0.0010620416,0.0011930458,0.0019741845,0.00016632176,0.020093907],"genre_scores_gemma":[0.9901129,0.00021792302,0.00045319236,0.00018466557,0.0012137421,0.000097466305,0.002819712,0.00006370498,0.0048367213],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99380314,0.00036666018,0.0016788677,0.0011547281,0.0014095469,0.0015870595],"domain_scores_gemma":[0.9931127,0.002633862,0.00172499,0.0011724496,0.00069704547,0.00065899466],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0015848501,0.0010036101,0.0015166774,0.00012453817,0.0005250402,0.00056850613,0.0010475751,0.0005565993,0.000015848505],"category_scores_gemma":[0.0010019238,0.0008293354,0.00031970683,0.0013239795,0.0003906397,0.0010344016,0.00017514506,0.0007982741,0.00015734912],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014718778,0.0022383207,0.5647175,0.014208088,0.0024088551,0.000332203,0.11678422,0.12565316,0.0709332,0.002463905,0.09063667,0.009476692],"study_design_scores_gemma":[0.017544735,0.0013539791,0.14536478,0.00379742,0.002047558,0.00033168306,0.17228812,0.065912746,0.06873589,0.018424748,0.5027686,0.0014297863],"about_ca_topic_score_codex":0.0083444305,"about_ca_topic_score_gemma":0.0004178549,"teacher_disagreement_score":0.41935274,"about_ca_system_score_codex":0.00003909728,"about_ca_system_score_gemma":0.0005251413,"threshold_uncertainty_score":0.99941576},"labels":[],"label_agreement":null},{"id":"W2230633998","doi":"10.1007/978-81-322-1170-9_20","title":"Diamonds from the Behradih Kimberlite Pipe, Bastar Craton, India: A Reconnaissance Study","year":2013,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada)","funders":"","keywords":"Kimberlite; Craton; Diamond; Population; Geochemistry; Diatreme; Geology; Xenolith; Chemistry; Paleontology; Mantle (geology); Tectonics","score_opus":0.015825056390518604,"score_gpt":0.1920641072505383,"score_spread":0.1762390508600197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2230633998","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05486428,0.001796585,0.000010489618,0.00031136384,0.0022896004,0.0014531086,0.002358244,0.00012076757,0.93679553],"genre_scores_gemma":[0.48563623,0.00029505865,0.00015596871,0.0009777546,0.0017191054,0.000015247573,0.000919004,0.000036557314,0.5102451],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99781233,0.000094228904,0.0005231295,0.0006956825,0.00046490584,0.00040973682],"domain_scores_gemma":[0.9981636,0.00037662114,0.0003010518,0.0008780829,0.000089357076,0.00019132876],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033411855,0.0005173927,0.0006502837,0.000052808366,0.00027368782,0.00037789886,0.0007659984,0.00026397684,0.09875526],"category_scores_gemma":[0.000016593965,0.00031598267,0.0001451109,0.000043870397,0.00015555623,0.00023893565,0.00006444727,0.00037800265,0.008255255],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028567933,0.00031568177,0.12278294,0.00013668492,0.0030248868,0.0005097102,0.007217018,0.00010947512,0.00015643475,0.031987578,0.7221186,0.1113553],"study_design_scores_gemma":[0.0004494011,0.00032844726,0.198341,0.000091447255,0.00024118129,0.000002783427,0.00012577472,0.000038899012,0.00003865029,0.028591055,0.77088183,0.0008695294],"about_ca_topic_score_codex":0.019144392,"about_ca_topic_score_gemma":0.0110908495,"teacher_disagreement_score":0.43077195,"about_ca_system_score_codex":0.0000034834704,"about_ca_system_score_gemma":0.00007501599,"threshold_uncertainty_score":0.99992925},"labels":[],"label_agreement":null},{"id":"W2235522816","doi":"10.1139/p11-040","title":"Analysis of a new two-parameter equation of state for MgO","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Natural Science Foundation of Anhui Province; Anhui University; Ministry of Education of the People's Republic of China","keywords":"Physics; Equation of state; Isothermal process; Basis (linear algebra); Thermodynamics; Lattice (music); Bulk modulus; Derivative (finance); Statistical physics; Geometry","score_opus":0.052498730716501,"score_gpt":0.22811708560954566,"score_spread":0.17561835489304467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2235522816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909963,0.00007182584,0.007907228,0.000013365289,0.0002307973,0.00006314701,0.0004104774,8.107675e-7,0.0003060261],"genre_scores_gemma":[0.99792165,0.0000040993446,0.0018651057,0.0000234343,0.000104404106,1.0382164e-7,0.000025696481,0.0000023074094,0.0000532031],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993738,0.000024709225,0.00029925525,0.000058363537,0.00010329191,0.0001405976],"domain_scores_gemma":[0.9990521,0.00006186195,0.00039371548,0.00009671248,0.0001727327,0.00022288527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019206593,0.00006174001,0.0002874072,0.00014526963,0.000025180345,0.000013371004,0.0001451281,0.000018544559,0.00037885024],"category_scores_gemma":[0.000029563773,0.00005189406,0.00015351223,0.0002580642,0.000037687256,0.00014580513,0.0000013871378,0.000033096552,0.000003039949],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005945277,0.00011513405,0.42146507,0.00027652865,0.0076890183,0.000044520977,0.02837428,0.13605201,0.013947787,0.010462186,0.0049240193,0.3760549],"study_design_scores_gemma":[0.0024304178,0.0022936382,0.6532625,0.00015254387,0.0053622997,0.0000057089846,0.00038750313,0.034159843,0.09217927,0.20495804,0.0040815272,0.0007266859],"about_ca_topic_score_codex":0.060294457,"about_ca_topic_score_gemma":0.052525785,"teacher_disagreement_score":0.37532824,"about_ca_system_score_codex":0.0000030207514,"about_ca_system_score_gemma":0.00043752606,"threshold_uncertainty_score":0.96476316},"labels":[],"label_agreement":null},{"id":"W2256697032","doi":"10.1103/physrevb.75.134108","title":"Structural phase transition in<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:mi mathvariant=\"normal\">Ca</mml:mi><mml:msub><mml:mi mathvariant=\"normal\">H</mml:mi><mml:mn>2</mml:mn></mml:msub></mml:mrow></mml:math>at high pressures","year":2007,"lang":"lv","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); University of Ottawa; Steacie Institute for Molecular Sciences; University of Guelph; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Crystallography; Physics; Phase transition; Order (exchange); Hexagonal crystal system; Phase (matter); Materials science; Condensed matter physics; Chemistry; Quantum mechanics","score_opus":0.014892569201744229,"score_gpt":0.24826014659790663,"score_spread":0.2333675773961624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2256697032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88673025,0.0056898906,0.00034193706,0.0007298857,0.0027787746,0.00009871432,0.0015566177,0.0001429865,0.10193092],"genre_scores_gemma":[0.98518187,0.005622928,0.0008547363,0.0015907559,0.0028412817,0.00027083827,0.0032391874,0.0002537408,0.00014466867],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9921644,0.00050416775,0.0017502661,0.0014525846,0.0019907735,0.0021378272],"domain_scores_gemma":[0.9947629,0.0010963186,0.0014545257,0.0015772241,0.000114798575,0.0009942476],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0019512859,0.0008264929,0.0005459715,0.00023589913,0.001182093,0.0009632928,0.0015606588,0.0010241364,0.20945969],"category_scores_gemma":[0.0005151645,0.0012799898,0.0013141168,0.0009038551,0.00090409274,0.0016854042,0.00065996806,0.0011234843,0.0032458627],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002048519,0.0005598419,0.00001684679,0.006377445,0.001217986,0.0021480913,0.002091937,0.0021772077,0.0065089525,0.86160827,0.107523575,0.007721355],"study_design_scores_gemma":[0.00280974,0.002228536,0.0008556509,0.0042554475,0.002934672,0.00097227475,0.0004058983,0.068991445,0.89558053,0.001041814,0.01756786,0.0023561523],"about_ca_topic_score_codex":0.0033888458,"about_ca_topic_score_gemma":0.0017662002,"teacher_disagreement_score":0.8890716,"about_ca_system_score_codex":0.000007671434,"about_ca_system_score_gemma":0.00063833874,"threshold_uncertainty_score":0.99896497},"labels":[],"label_agreement":null},{"id":"W2272100246","doi":"10.1038/srep10458","title":"Structures of the metallic and superconducting high pressure phases of solid CS2","year":2015,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Western Canada Research Grid; Compute Canada","keywords":"Superconductivity; Metastability; Crystal structure; Materials science; Crystallography; Magnetism; Metal; Crystal structure prediction; Phase (matter); Chemical physics; Condensed matter physics; Chemistry; Physics","score_opus":0.025182665673912263,"score_gpt":0.23590688050008887,"score_spread":0.21072421482617662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2272100246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99379444,0.00069100485,0.0000021349533,0.000031854455,0.004904203,0.00013757178,0.00007514364,0.000008672134,0.00035499674],"genre_scores_gemma":[0.9990295,0.000002396785,0.00021614396,0.00000558586,0.00006248979,4.2498604e-7,0.000024194449,0.0000020836467,0.0006571661],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99878263,0.00006105635,0.00033310454,0.00027748744,0.0003958611,0.00014982886],"domain_scores_gemma":[0.9990485,0.00003195203,0.0002834535,0.0004236987,0.00013666671,0.00007578235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008452274,0.0000858278,0.00021722134,0.000040874114,0.000116759045,0.00006954656,0.00014753724,0.00003515269,0.00036967115],"category_scores_gemma":[0.00015303574,0.000050179573,0.00004282734,0.00017140887,0.00034407686,0.00019496193,0.000038862683,0.00003976828,0.0000012337763],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004810384,0.0000853703,0.1554612,0.00037181278,0.00028852955,0.00006999211,0.0045600194,0.006871118,0.81208515,0.0013846656,0.013586324,0.0051876805],"study_design_scores_gemma":[0.0002545682,0.00008840265,0.060607232,0.000053000706,0.00019756534,0.0001398444,0.0004825652,0.00015359267,0.81893504,0.09050007,0.028343061,0.0002450352],"about_ca_topic_score_codex":0.0018731466,"about_ca_topic_score_gemma":0.00018172922,"teacher_disagreement_score":0.094853975,"about_ca_system_score_codex":5.3263756e-7,"about_ca_system_score_gemma":0.00009256933,"threshold_uncertainty_score":0.40476397},"labels":[],"label_agreement":null},{"id":"W2272254305","doi":"10.2138/am-2004-0418","title":"Isothermal equation of state and compressional behavior of tetragonal edingtonite","year":2004,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tetragonal crystal system; Equation of state; Isothermal process; Tetrahedron; Crystallography; Diffraction; Chemistry; Single crystal; Deformation (meteorology); High pressure; Thermodynamics; Materials science; Mineralogy; Crystal structure; Physics; Composite material; Optics","score_opus":0.014298502294193596,"score_gpt":0.23103145810201225,"score_spread":0.21673295580781865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2272254305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984892,0.000050769515,0.00017438395,0.000054477074,0.00009191598,0.000069499016,0.00038838314,0.0000054420616,0.0006759026],"genre_scores_gemma":[0.99777055,0.00002156706,0.0019931395,0.000031974865,0.000043511947,9.946608e-7,0.00007759619,0.000002241191,0.000058398306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993982,0.000023964009,0.00019068886,0.0001158158,0.0001519075,0.00011946657],"domain_scores_gemma":[0.9996154,0.000047785485,0.00017815859,0.000075300195,0.000035313948,0.000048082293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006721006,0.000075362215,0.00018779715,0.000038622355,0.000031115847,0.000010211684,0.00007734185,0.0000135739665,0.0002814375],"category_scores_gemma":[0.000009098381,0.000059378417,0.000025303058,0.00008770418,0.0004376097,0.000071293754,0.000009672075,0.000032800664,0.000007683192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017742309,0.00016422794,0.4873212,0.000056126853,0.000045247853,0.000016830081,0.0006013229,0.012382763,0.43066254,0.001195555,0.00010688286,0.067269884],"study_design_scores_gemma":[0.00034569087,0.00031782917,0.9888129,0.000018533852,0.000020456928,0.0000050966114,0.000043595846,0.00020008479,0.009367449,0.00051907107,0.00023786098,0.00011142193],"about_ca_topic_score_codex":0.015616099,"about_ca_topic_score_gemma":0.0003511578,"teacher_disagreement_score":0.5014917,"about_ca_system_score_codex":0.0000011199155,"about_ca_system_score_gemma":0.000027622216,"threshold_uncertainty_score":0.990939},"labels":[],"label_agreement":null},{"id":"W2274719868","doi":"10.2138/am-2002-1007","title":"Evolution of local electronic structure in alabandite and niningerite solid solutions [(Mn,Fe)S, (Mg,Mn)S, (Mg,Fe)S] using sulfur <i>K</i> - and <i>L</i> -edge XANES spectroscopy","year":2002,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Ryerson University","keywords":"XANES; Antibonding molecular orbital; Crystallography; Spectral line; Electron; X-ray absorption spectroscopy; Transition metal; Solid solution; Synchrotron radiation; Absorption edge; Chemistry; Materials science; Electronic structure; Analytical Chemistry (journal); Absorption spectroscopy; Condensed matter physics; Physics; Band gap; Atomic orbital; Computational chemistry; Metallurgy; Optics","score_opus":0.010530581823435546,"score_gpt":0.21730321331275493,"score_spread":0.20677263148931938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2274719868","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945446,0.0034685635,0.000537095,0.00021217397,0.00016753314,0.00015503282,0.00066674425,0.00002839547,0.0002198417],"genre_scores_gemma":[0.99801284,0.0006646907,0.0007753883,0.0001509063,0.00018030424,0.0000014923293,0.00014476334,0.000010397247,0.000059205657],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9982732,0.00012538859,0.000351015,0.00041616385,0.00018471156,0.0006494993],"domain_scores_gemma":[0.9993033,0.00007938453,0.00023585491,0.00021017795,0.000045562032,0.00012574092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014186448,0.0002545328,0.00049150997,0.00012447334,0.00017524514,0.00006983183,0.00014411393,0.00007209798,0.00015161284],"category_scores_gemma":[0.000023241277,0.00023147409,0.000042181888,0.00040570323,0.0009615539,0.00023069815,0.000036656093,0.0001827551,0.0000064614346],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017462356,0.000119889686,0.10552225,0.00014441767,0.00011169581,0.000057882447,0.0009443419,0.006024449,0.8729679,0.0012983625,0.003978708,0.008655484],"study_design_scores_gemma":[0.0045234337,0.0037452888,0.7752573,0.0003422293,0.00050185184,0.0007059621,0.0022769617,0.14871374,0.03230233,0.006411451,0.021878827,0.0033406317],"about_ca_topic_score_codex":0.020054843,"about_ca_topic_score_gemma":0.009214136,"teacher_disagreement_score":0.8406656,"about_ca_system_score_codex":0.000021416214,"about_ca_system_score_gemma":0.000050192175,"threshold_uncertainty_score":0.9864707},"labels":[],"label_agreement":null},{"id":"W227523156","doi":"10.1017/s0074180900002400","title":"R CrB: Photometric Evidence Regarding the Nature of its Pulsation, and a Putative Connection between Pulsation and Deep Declines","year":2000,"lang":"en","type":"article","venue":"Symposium - International Astronomical Union","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Photometry (optics); Cepheid variable; Period (music); Astrophysics; Physics; Photoelectric effect; Astronomy; Optics; Stars","score_opus":0.011316007242310501,"score_gpt":0.24307306305741105,"score_spread":0.23175705581510056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W227523156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99724567,0.00029014,0.00030958743,0.0012012769,0.00028486125,0.00018792544,0.00010348921,0.0000110589,0.0003659719],"genre_scores_gemma":[0.998812,0.00022258665,0.00030229887,0.000031388634,0.00032695124,0.0000031085863,0.00019127098,0.000003206104,0.0001071783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910736,0.00012147619,0.00025222974,0.0002212705,0.00018437198,0.00011330169],"domain_scores_gemma":[0.99921703,0.0004153821,0.00013888773,0.000069097965,0.00010818343,0.000051431267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039417698,0.00010288378,0.0001414779,0.00010748561,0.00010874782,0.00009812512,0.00013491172,0.000076668606,0.00029919465],"category_scores_gemma":[0.0000954247,0.000075699594,0.00002953556,0.0001411497,0.00007239226,0.00045717222,0.000018371105,0.00011384405,0.000013861586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003811137,0.00003783208,0.8655568,0.00005984021,0.00022738273,8.794343e-7,0.00065923715,0.015161477,0.014622393,0.001652768,0.00006758632,0.101572715],"study_design_scores_gemma":[0.00028357617,0.00010232829,0.9810968,0.000049798426,0.000036648238,0.000003444553,0.000058363104,0.012026039,0.004320204,0.0006489034,0.0012675105,0.00010640305],"about_ca_topic_score_codex":0.00032394726,"about_ca_topic_score_gemma":0.000036981684,"teacher_disagreement_score":0.115540005,"about_ca_system_score_codex":0.000009838869,"about_ca_system_score_gemma":0.000015934105,"threshold_uncertainty_score":0.32759714},"labels":[],"label_agreement":null},{"id":"W227809023","doi":"","title":"Post-Shock Crystal-Plastic Processes in Quartz from Crystalline Target Rocks of the Charlevoix Impact Structure","year":2004,"lang":"en","type":"article","venue":"LPI","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Cathodoluminescence; Hypervelocity; Electron backscatter diffraction; Quartz; Transmission electron microscopy; Scanning electron microscope; Optical microscope; Mineralogy; Geology; Microscopy; Materials science; Microstructure; Shock (circulatory); Composite material; Optics; Optoelectronics; Luminescence; Nanotechnology","score_opus":0.0047588868696381145,"score_gpt":0.1969060889706261,"score_spread":0.19214720210098798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W227809023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994285,0.00034007817,0.000074370466,0.00012498029,0.0003313847,0.00017127895,0.0045147385,0.000015433357,0.00014274058],"genre_scores_gemma":[0.99921393,0.0000124307735,0.00015363909,0.00006116219,0.00017870044,7.951453e-7,0.0003307076,0.000005293834,0.00004336268],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990216,0.000039488736,0.00024500384,0.00020601344,0.00023379951,0.00025408427],"domain_scores_gemma":[0.9994244,0.00010171212,0.00012722173,0.00021443164,0.00006542411,0.000066828514],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00005997591,0.0001591972,0.0002453726,0.000042422624,0.000065215805,0.000047046382,0.0002969653,0.00007846715,0.0026137491],"category_scores_gemma":[0.000091161455,0.00009438646,0.00005357003,0.00022968627,0.000050232757,0.00016706224,0.000019343057,0.000107384694,0.000024921788],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046006782,0.00016737681,0.33854795,0.00041481789,0.00014592428,0.00003932196,0.005011239,0.47287348,0.18129365,0.00008002132,0.0003857246,0.0005804307],"study_design_scores_gemma":[0.000999401,0.00030885523,0.9557453,0.00014968893,0.000036792,0.0000058824667,0.00015600375,0.00039319764,0.021907661,0.018237833,0.0017151242,0.00034430958],"about_ca_topic_score_codex":0.021254664,"about_ca_topic_score_gemma":0.015272021,"teacher_disagreement_score":0.6171973,"about_ca_system_score_codex":0.0000046627924,"about_ca_system_score_gemma":0.00018132375,"threshold_uncertainty_score":0.998298},"labels":[],"label_agreement":null},{"id":"W2280208863","doi":"10.1002/2015jb012453","title":"Rayleigh wave azimuthally anisotropic phase velocity maps beneath western Canada","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Craton; Lithosphere; Laurentia; Foreland basin; Asthenosphere; Seismic anisotropy; Geophysics; Anisotropy; Paleontology; Crust; Seismology; Mantle (geology); Tectonics; Physics","score_opus":0.04092351643871263,"score_gpt":0.3051730938125086,"score_spread":0.264249577373796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2280208863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99640536,0.00007995784,0.00009800956,0.0012653838,0.0006235792,0.00015686484,0.00038969165,0.000009993827,0.0009711787],"genre_scores_gemma":[0.99666476,0.00016522706,0.00021100177,0.00010270392,0.0015959565,8.641158e-7,0.000014532802,0.000009951345,0.0012349825],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99592274,0.000456265,0.00055897253,0.00029341935,0.0018576661,0.0009109246],"domain_scores_gemma":[0.9973556,0.0007114569,0.00025937607,0.00032725633,0.00065604993,0.0006903024],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001055158,0.00021941194,0.0005761681,0.00013055887,0.00027596948,0.0001633031,0.00055364013,0.00008309027,0.001237527],"category_scores_gemma":[0.00028852865,0.00012956187,0.00015107368,0.00027839837,0.0002164331,0.00046488893,0.000069415764,0.0004375328,0.00025612104],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00797836,0.0027270594,0.058922656,0.0005696225,0.0019388316,0.012036409,0.0018954623,0.0008489407,0.24507241,0.0060493406,0.077351354,0.58460957],"study_design_scores_gemma":[0.007775009,0.006409054,0.7702421,0.00047149695,0.0000943135,0.00018889853,0.00018091308,0.00055703754,0.03297068,0.018399546,0.16173126,0.0009796899],"about_ca_topic_score_codex":0.11347697,"about_ca_topic_score_gemma":0.10243549,"teacher_disagreement_score":0.71131945,"about_ca_system_score_codex":0.00002694904,"about_ca_system_score_gemma":0.0013797119,"threshold_uncertainty_score":0.99967545},"labels":[],"label_agreement":null},{"id":"W2287876505","doi":"10.1139/cjes-2015-0228","title":"Earth evolution and dynamics—a tribute to Kevin Burke","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Plate tectonics; Mantle convection; Mantle plume; Hotspot (geology); Lithosphere; Subduction; Kimberlite; Geophysics; Tectonophysics; Tectonics; Paleontology","score_opus":0.00969521518978276,"score_gpt":0.19201112239451693,"score_spread":0.18231590720473417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2287876505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931967,0.00038040642,0.00055323367,0.0034810891,0.00090369105,0.00007118765,0.00019687651,0.0000037544107,0.0012130651],"genre_scores_gemma":[0.9982435,0.000022268903,0.000679363,0.00012656605,0.00019751627,1.262407e-7,0.000001359545,0.0000015351799,0.0007277433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998964,0.000056924826,0.00023177048,0.00015283324,0.00021993698,0.00037449677],"domain_scores_gemma":[0.99886245,0.00008159387,0.0001172994,0.00008002405,0.00009519818,0.0007634665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000828029,0.00008878683,0.00016719465,0.00024458722,0.00028880587,0.00018495828,0.0002679261,0.0000353211,0.0008544452],"category_scores_gemma":[0.00013917898,0.000053506286,0.000035536646,0.0002749368,0.00024879377,0.00043914065,0.0000058679043,0.000046839774,0.00009756027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038106067,0.0000061351852,0.9385183,0.000014608592,0.00003225003,0.00011485699,0.00038340682,0.0010698974,0.0029837252,0.0042759497,0.002233497,0.05032927],"study_design_scores_gemma":[0.00017985987,0.0004959932,0.9500504,0.00008967806,0.000011704031,0.00008103265,0.000098529825,0.00028193888,0.00036317224,0.0028757893,0.045304332,0.00016756625],"about_ca_topic_score_codex":0.015228979,"about_ca_topic_score_gemma":0.41995525,"teacher_disagreement_score":0.4047263,"about_ca_system_score_codex":0.0000022642723,"about_ca_system_score_gemma":0.0006698614,"threshold_uncertainty_score":0.9913287},"labels":[],"label_agreement":null},{"id":"W2290015869","doi":"10.5194/se-7-355-2016","title":"Strain localization in ultramylonitic marbles by simultaneous activation of dislocation motion and grain boundary sliding (Syros, Greece)","year":2016,"lang":"en","type":"article","venue":"Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada; Universität Wien; Austrian Science Fund","keywords":"Misorientation; Dislocation creep; Dislocation; Grain boundary; Slip (aerodynamics); Grain Boundary Sliding; Materials science; Crystallography; Deformation (meteorology); Grain boundary strengthening; Climb; Grain size; Peierls stress; Creep; Mineralogy; Geology; Geometry; Microstructure; Composite material; Physics; Chemistry; Thermodynamics","score_opus":0.006656606935939686,"score_gpt":0.20566819368021907,"score_spread":0.19901158674427938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2290015869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9844632,0.000077637946,0.0144903,0.00014974912,0.00014974468,0.00019041135,0.00030450782,0.000021724425,0.00015268258],"genre_scores_gemma":[0.99934876,0.000085526844,0.00011015333,0.000031926793,0.0000469007,0.0000011177302,0.00027445427,0.0000042395895,0.0000969505],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99917835,0.00009147024,0.00022178027,0.00018079662,0.0001533796,0.00017421106],"domain_scores_gemma":[0.99959236,0.00012947251,0.00010314508,0.000090165624,0.000038522532,0.000046352558],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021845645,0.00009752135,0.00014651235,0.00006485189,0.000077081044,0.000046561436,0.000054842152,0.000060619484,0.00017520665],"category_scores_gemma":[0.00008969838,0.000074296375,0.000015315074,0.000120943456,0.00006217865,0.00030615882,0.0000049522637,0.00003232811,0.000012981521],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016960657,0.00009765994,0.070245266,0.0002634548,0.000034832912,0.000007745774,0.0015543983,0.010386369,0.51950717,0.0011791185,0.0001801592,0.39637426],"study_design_scores_gemma":[0.003704881,0.0009221316,0.50528955,0.00096099917,0.000077390534,0.000018690658,0.0006847088,0.16136098,0.2845271,0.034166202,0.0069187516,0.0013686013],"about_ca_topic_score_codex":0.00089960167,"about_ca_topic_score_gemma":0.0005733171,"teacher_disagreement_score":0.4350443,"about_ca_system_score_codex":0.0000035900775,"about_ca_system_score_gemma":0.000021271147,"threshold_uncertainty_score":0.30297184},"labels":[],"label_agreement":null},{"id":"W2291760404","doi":"10.1093/gji/ggv368","title":"Ultra-low velocity zones beneath the Philippine and Tasman Seas revealed by a trans-dimensional Bayesian waveform inversion","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Mantle (geology); Geophysics; Inverse problem; Bayesian probability; Parallel tempering; Markov chain Monte Carlo; Geodesy; Statistical physics; Seismology; Mathematics; Mathematical analysis; Physics; Statistics","score_opus":0.010600460236991235,"score_gpt":0.20867095697818736,"score_spread":0.19807049674119612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2291760404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99069613,0.00013761174,0.00034604163,0.005718889,0.001229457,0.00011942895,0.0003644762,0.000020794947,0.0013671708],"genre_scores_gemma":[0.9969759,0.000055253713,0.0002941736,0.00063569855,0.0011731395,0.000001223992,0.00021721849,0.000005717079,0.00064168527],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9984087,0.000103387756,0.0002797672,0.00022575771,0.0007102587,0.00027215015],"domain_scores_gemma":[0.99913055,0.00010206073,0.00014005546,0.000111171474,0.00017755301,0.000338611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040173408,0.00018063415,0.0002121413,0.000045924196,0.00028364404,0.0002122368,0.00034779223,0.00006260063,0.0008632938],"category_scores_gemma":[0.00004066792,0.00011275867,0.00009429651,0.00009326978,0.00013744194,0.0003972227,0.000023892606,0.00026184256,0.00008066476],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.006093078,0.0023779713,0.09091351,0.00023401373,0.003266593,0.0008602308,0.010743721,0.014072588,0.07574029,0.011406207,0.32640123,0.45789057],"study_design_scores_gemma":[0.010031518,0.0018247315,0.58448386,0.0004203137,0.00039076802,0.0013961499,0.00088988704,0.11671673,0.007830312,0.106888376,0.1668682,0.0022591667],"about_ca_topic_score_codex":0.0006157727,"about_ca_topic_score_gemma":0.000077462944,"teacher_disagreement_score":0.49357036,"about_ca_system_score_codex":0.000013602325,"about_ca_system_score_gemma":0.000075418764,"threshold_uncertainty_score":0.94524616},"labels":[],"label_agreement":null},{"id":"W2295888934","doi":"10.1007/s00269-015-0795-0","title":"High-pressure X-ray diffraction and Raman spectroscopy of CaFe2O4-type β-CaCr2O4","year":2016,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Natural Science Foundation of China","keywords":"Chemistry; Raman spectroscopy; Compressibility; Bulk modulus; Diamond anvil cell; Orthorhombic crystal system; Diffraction; Isothermal process; Anisotropy; Phase transition; X-ray crystallography; Thermal expansion; Analytical Chemistry (journal); Synchrotron; Crystallography; Thermodynamics; Crystal structure; Optics","score_opus":0.007060405362715774,"score_gpt":0.20028958996202076,"score_spread":0.193229184599305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2295888934","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99827,0.0003954303,0.00002437682,0.00011553184,0.00011367349,0.000054568412,0.00023150323,0.00000866289,0.00078626396],"genre_scores_gemma":[0.9983442,0.00031817818,0.00025202392,0.000009950831,0.00026318303,5.401753e-7,0.00003541934,0.0000041083863,0.00077243923],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99932534,0.000015501122,0.00019059409,0.00019672359,0.00012184741,0.0001500258],"domain_scores_gemma":[0.9994728,0.00006881142,0.00016838542,0.000163879,0.000056345827,0.000069793234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008094636,0.00012764923,0.0002850424,0.000008107753,0.000039680475,0.000016846941,0.00008433046,0.000055542245,0.00041602596],"category_scores_gemma":[0.000014069788,0.00008647109,0.000029766257,0.00004994048,0.000120586585,0.00011211844,0.000018311015,0.00003670551,0.0000036059876],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047595364,0.000022120146,0.0042807264,0.00015897962,0.00004088747,5.137434e-7,0.000040742616,0.000037564158,0.993022,0.000095904594,0.00038956906,0.0018633702],"study_design_scores_gemma":[0.00054666016,0.00009429839,0.05031471,0.00007796274,0.00007527306,0.0000016528879,0.00001728111,0.000079040015,0.94054157,0.0048245746,0.0032377092,0.00018928334],"about_ca_topic_score_codex":0.0006982244,"about_ca_topic_score_gemma":0.000008641543,"teacher_disagreement_score":0.05248047,"about_ca_system_score_codex":7.508636e-7,"about_ca_system_score_gemma":0.0000133905405,"threshold_uncertainty_score":0.45551923},"labels":[],"label_agreement":null},{"id":"W2301483851","doi":"10.1021/acs.jpcb.6b00497","title":"Hexafluorobenzene under Extreme Conditions","year":2016,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Basic Energy Sciences; Canadian Institutes of Health Research; National Nuclear Security Administration; University of Nevada, Las Vegas; U.S. Department of Energy","keywords":"Diffraction; Phase transition; Raman spectroscopy; Amorphous solid; Hexafluorobenzene; Phase (matter); Ambient pressure; Analytical Chemistry (journal); Spectral line; Materials science; X-ray crystallography; Chemistry; Crystallography; Optics; Physics; Condensed matter physics; Thermodynamics; Molecule","score_opus":0.016888682295570973,"score_gpt":0.2191039631283536,"score_spread":0.20221528083278262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2301483851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960746,0.000059110047,0.00016594368,0.0008285215,0.00009197683,0.000022026463,0.000062408464,0.000006984858,0.0026884328],"genre_scores_gemma":[0.99849796,0.000018847682,0.000016120539,0.000054982942,0.0009365756,1.0051676e-7,0.0000031182933,0.0000024365936,0.00046986443],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99940705,0.000038308797,0.0001565215,0.000055287095,0.00020266797,0.00014014484],"domain_scores_gemma":[0.9993263,0.00024070677,0.00015117365,0.00013286238,0.00006109017,0.00008788139],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016289744,0.000078923134,0.00014579964,0.00000622785,0.000073398056,0.0000186993,0.00025136166,0.000022762264,0.0022598382],"category_scores_gemma":[0.000020698692,0.000034187142,0.00007895503,0.000046919406,0.00008660894,0.00012164064,0.000010161098,0.00007228066,0.00012212106],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030760497,0.000026565178,0.00012097127,0.0000074541294,0.00003299538,0.000003888104,0.000043107884,0.00040405418,0.9968844,0.00012805752,0.0013554207,0.0009623418],"study_design_scores_gemma":[0.00082147436,0.00017342839,0.029193671,0.00010577478,0.0001585816,0.000104128056,0.000092377,0.00018051406,0.9178436,0.04327443,0.007796219,0.00025582514],"about_ca_topic_score_codex":0.000026470401,"about_ca_topic_score_gemma":0.0000032458329,"teacher_disagreement_score":0.0790408,"about_ca_system_score_codex":0.0000027341534,"about_ca_system_score_gemma":0.000032936372,"threshold_uncertainty_score":0.9986522},"labels":[],"label_agreement":null},{"id":"W2306132221","doi":"10.1093/gji/ggw098","title":"Detecting lower-mantle slabs beneath Asia and the Aleutians","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismogram; Seismology; Slowness; Slab; Mantle (geology); Subduction; Transition zone; Reflection (computer programming); Seismic wave; Scattering; Geodesy; Geophysics; Tectonics; Physics; Optics","score_opus":0.006970482317417426,"score_gpt":0.2046872939782327,"score_spread":0.19771681166081528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2306132221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862712,0.00008298871,0.0008567903,0.0050578923,0.0021343755,0.00007209665,0.00008376997,0.000018842638,0.0054220147],"genre_scores_gemma":[0.9969709,0.000089702204,0.00014631222,0.00019739706,0.001702959,8.282696e-7,0.0000049239193,0.0000037387852,0.00088326057],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9990244,0.000079019395,0.00020378627,0.00015547851,0.00032450282,0.00021281542],"domain_scores_gemma":[0.9992936,0.00030734984,0.00012251368,0.00009650747,0.00007839694,0.000101595164],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032326687,0.00010868383,0.00014673588,0.000033369924,0.00023032361,0.00021712917,0.00030006125,0.00003345039,0.0011710364],"category_scores_gemma":[0.00007307863,0.00005071181,0.00008659528,0.000044182885,0.00015474755,0.00027030855,0.00003511757,0.00012808251,0.00036576862],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021713532,0.00013016784,0.03703025,0.000021513111,0.0010335948,0.0003571256,0.0010847534,0.00044344197,0.045130473,0.057293393,0.0063979896,0.8489059],"study_design_scores_gemma":[0.009040375,0.0006180798,0.6228334,0.00030041003,0.00019311017,0.0012272219,0.0002471526,0.0070095477,0.00918961,0.19316761,0.1551195,0.001054033],"about_ca_topic_score_codex":0.00022111599,"about_ca_topic_score_gemma":0.00007836626,"teacher_disagreement_score":0.84785193,"about_ca_system_score_codex":0.000004398528,"about_ca_system_score_gemma":0.000023174058,"threshold_uncertainty_score":0.99974203},"labels":[],"label_agreement":null},{"id":"W2306203856","doi":"10.1063/1.4944086","title":"High pressure structural changes in aluminium triiodide: A first principles study","year":2016,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); National Research Council Canada; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Compute Canada; University of Saskatchewan","keywords":"Monoclinic crystal system; Ambient pressure; Raman spectroscopy; Phase transition; Metadynamics; Crystallography; Aluminium; Triiodide; Chemistry; Chemical physics; Phase (matter); Structural stability; Raman scattering; Materials science; Crystal structure; Molecular dynamics; Thermodynamics; Computational chemistry; Physical chemistry; Physics; Optics; Metallurgy; Electrolyte","score_opus":0.018646568971826146,"score_gpt":0.22153364378046955,"score_spread":0.2028870748086434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2306203856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984461,0.00011050859,0.000011848043,0.0007952152,0.00035813544,0.00014603023,0.000053934564,0.0000064250803,0.00007177247],"genre_scores_gemma":[0.99889684,0.000034637465,0.00005453298,0.00004079325,0.000911762,5.372144e-7,0.0000023092105,0.000004343862,0.00005426004],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989201,0.00010583786,0.00031167487,0.000101239384,0.00033916254,0.00022197401],"domain_scores_gemma":[0.9990538,0.00032937265,0.00028816581,0.00018513037,0.00006915423,0.000074404554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042321376,0.00013428683,0.00031026758,0.000021963782,0.000049135586,0.000030374244,0.00044515255,0.00004095811,0.0002615237],"category_scores_gemma":[0.000053922984,0.00006045826,0.000050188577,0.00010739525,0.000086266395,0.00017529457,0.000034448873,0.000136121,0.00001727198],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.006448813,0.0012568437,0.34477296,0.00040851824,0.0016769572,0.0002104448,0.015518786,0.030912522,0.53265244,0.002013818,0.00698204,0.057145853],"study_design_scores_gemma":[0.007746468,0.0019471548,0.48788413,0.00043123812,0.00071346085,0.00008223326,0.00054896134,0.0011447527,0.45178342,0.035670664,0.011025305,0.0010221995],"about_ca_topic_score_codex":0.0002466899,"about_ca_topic_score_gemma":0.00017806621,"teacher_disagreement_score":0.14311117,"about_ca_system_score_codex":0.0000038607627,"about_ca_system_score_gemma":0.000029649273,"threshold_uncertainty_score":0.28635013},"labels":[],"label_agreement":null},{"id":"W2313506536","doi":"10.1139/cjp-2013-0496","title":"Lattice dynamics, thermodynamics, and elastic properties of Na<sub>2</sub>Se under pressure investigated by first principles method","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Thermodynamics; Physics; Lattice (music); Structural stability; High pressure","score_opus":0.015666818234144734,"score_gpt":0.18709441882452202,"score_spread":0.1714276005903773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2313506536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99437165,0.000814343,0.0035212862,0.00027344323,0.0003478679,0.000107542844,0.0003574971,0.000006083731,0.00020029092],"genre_scores_gemma":[0.9991241,0.000038706075,0.0005142896,0.00009207924,0.00015014797,3.588423e-7,0.0000300588,0.000010940908,0.00003930638],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988911,0.0001533713,0.00034595307,0.00015151991,0.00017978446,0.0002782776],"domain_scores_gemma":[0.99877656,0.000112529495,0.0003445239,0.00015586869,0.00017682773,0.00043371145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038464955,0.00016902888,0.00035377397,0.00006154356,0.00014716476,0.00008839853,0.00024445113,0.00007966486,0.000028043616],"category_scores_gemma":[0.00009414603,0.00013423256,0.000055509245,0.000114960356,0.00023116547,0.00023325978,0.000010301574,0.00017641416,0.0000055521487],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030227166,0.00017414094,0.0880283,0.002891779,0.0022751365,0.00006653713,0.0076490515,0.5291985,0.25107363,0.06404391,0.0028107213,0.05148598],"study_design_scores_gemma":[0.001918562,0.0010279474,0.11371652,0.0012125087,0.0010999511,0.00010165206,0.0005378634,0.7203193,0.10549336,0.04325827,0.009832643,0.0014814499],"about_ca_topic_score_codex":0.012147124,"about_ca_topic_score_gemma":0.04398406,"teacher_disagreement_score":0.19112073,"about_ca_system_score_codex":0.000009491615,"about_ca_system_score_gemma":0.00036284773,"threshold_uncertainty_score":0.9944311},"labels":[],"label_agreement":null},{"id":"W2314978389","doi":"10.1103/physreve.89.042304","title":"Predicting plasticity with soft vibrational modes: From dislocations to glasses","year":2014,"lang":"en","type":"article","venue":"Physical Review E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Phonon; Polarization (electrochemistry); Dislocation; Materials science; Plasticity; Molecular physics; Condensed matter physics; Soft modes; Molecular vibration; Chemical physics; Physics; Optics; Chemistry; Optoelectronics; Raman spectroscopy; Composite material","score_opus":0.01258490993226904,"score_gpt":0.2413953784834065,"score_spread":0.22881046855113746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314978389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9538974,0.00046353045,0.04026192,0.0010175902,0.00012568028,0.0003881977,0.00046242127,0.00007546129,0.0033077917],"genre_scores_gemma":[0.99725336,0.00007749589,0.0011393161,0.0007953801,0.000537358,0.00000952402,0.0001740641,0.0000033149875,0.000010196523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992315,0.00005883981,0.00013084195,0.00020979169,0.0002212004,0.00014778196],"domain_scores_gemma":[0.99926084,0.0003792744,0.000053996304,0.0001284362,0.000054925167,0.00012250217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000700343,0.00010407694,0.00022963638,0.000009233149,0.000102466285,0.000051243303,0.00013475635,0.00001057843,0.00035163193],"category_scores_gemma":[0.00017511802,0.00006856477,0.000034100874,0.000112990274,0.000026035768,0.00014963755,0.000012262766,0.0000483295,0.00049023767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041647372,0.001062424,0.3554209,0.004830016,0.0007201549,0.000012073931,0.002541839,0.20724015,0.044613793,0.12589508,0.015799195,0.24144791],"study_design_scores_gemma":[0.00056229514,0.00075635605,0.60553885,0.0033172416,0.00049889175,0.0000023701382,0.000043997923,0.31015292,0.0029712473,0.03719484,0.037885405,0.0010755814],"about_ca_topic_score_codex":0.0006223678,"about_ca_topic_score_gemma":0.00033157683,"teacher_disagreement_score":0.25011796,"about_ca_system_score_codex":0.0000012967454,"about_ca_system_score_gemma":0.000028366367,"threshold_uncertainty_score":0.6301177},"labels":[],"label_agreement":null},{"id":"W2316698056","doi":"10.1103/physrevb.85.214122","title":"Structural phase transitions in Si under hydrostatic and uniaxial compression","year":2012,"lang":"en","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Metastability; Materials science; Hydrostatic pressure; Hydrostatic equilibrium; Compression (physics); Phase (matter); Ambient pressure; Enthalpy; Phase transition; Condensed matter physics; Thermodynamics; Composite material; Chemistry; Physics","score_opus":0.023764108270210204,"score_gpt":0.30701866897247926,"score_spread":0.28325456070226906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316698056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99392897,0.0047828853,0.000024054367,0.0003361099,0.00010628612,0.0002512612,0.00009511535,0.000011019672,0.00046428034],"genre_scores_gemma":[0.99882174,0.00051277125,0.000044438675,0.0003384352,0.0001697659,0.000004852658,0.00009847292,0.0000021934056,0.0000073305387],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.999371,0.00009151967,0.00012777404,0.00010619135,0.00010705574,0.0001964636],"domain_scores_gemma":[0.99970514,0.000057342782,0.00003326572,0.00008465359,0.000007497503,0.00011208472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090961425,0.00009086568,0.0002314066,0.0000125059505,0.000053924792,0.000017498596,0.000054484077,0.0000125368415,0.00044401592],"category_scores_gemma":[0.000008286816,0.00006288476,0.000032455788,0.00008637232,0.00004290725,0.00021232944,0.0000064283045,0.000062900544,0.000071470065],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053226465,0.0026463678,0.043334555,0.014557317,0.00025738924,0.000064052685,0.00894334,0.0035213474,0.12082821,0.13377574,0.006401314,0.6651381],"study_design_scores_gemma":[0.005742971,0.0007991675,0.78269017,0.0053234664,0.0005600517,0.000042608,0.0001410035,0.060354024,0.0019632827,0.0875933,0.05285989,0.0019300573],"about_ca_topic_score_codex":0.00015264619,"about_ca_topic_score_gemma":0.00003693876,"teacher_disagreement_score":0.7393556,"about_ca_system_score_codex":0.0000011728937,"about_ca_system_score_gemma":0.000007571516,"threshold_uncertainty_score":0.4861663},"labels":[],"label_agreement":null},{"id":"W2318544485","doi":"10.1180/minmag.2012.076.4.14","title":"The effects of composition upon the high-pressure behaviour of amphiboles: compression of gedrite to 7 GPa and a comparison with anthophyllite and proto-amphibole","year":2012,"lang":"en","type":"article","venue":"Mineralogical Magazine","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique; University of Manitoba; American Museum of Natural History","keywords":"Amphibole; Orthorhombic crystal system; Monoclinic crystal system; Crystallography; Mineralogy; Analytical Chemistry (journal); Chemistry; Geology; Crystal structure; Materials science; Composite material","score_opus":0.006818708895989281,"score_gpt":0.2182022197738909,"score_spread":0.2113835108779016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2318544485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971793,0.0014384616,0.00006387953,0.0001599538,0.00010251993,0.000806391,0.00015803409,0.0000088209945,0.0000825981],"genre_scores_gemma":[0.99912375,0.000054977525,0.00063061825,0.000030552437,0.000064213484,0.000011541375,0.000056257693,0.000003803789,0.000024274013],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988826,0.00019814435,0.00030240702,0.00015714762,0.00024497806,0.00021473659],"domain_scores_gemma":[0.9990645,0.00035779213,0.00020258981,0.00019739619,0.00007492657,0.00010278856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028711787,0.00014838789,0.00037930594,0.000031103973,0.00011523971,0.00002700975,0.00014275195,0.000056849083,0.000028531824],"category_scores_gemma":[0.00002479714,0.00006702631,0.000027835995,0.00013213044,0.00024337797,0.00009098458,0.000052340445,0.00007839713,0.0000020846478],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007180911,0.00020656726,0.3410322,0.00045144977,0.00005131862,0.0000020806356,0.00055358623,0.00034300535,0.6517763,0.00068382744,0.0002913204,0.0038902026],"study_design_scores_gemma":[0.00050709693,0.00082474365,0.9833765,0.00015974461,0.0000875485,0.0000043965106,0.000020621395,0.0002962086,0.013347244,0.00010050734,0.001173891,0.000101483136],"about_ca_topic_score_codex":0.0004945783,"about_ca_topic_score_gemma":0.0001343083,"teacher_disagreement_score":0.6423443,"about_ca_system_score_codex":7.2145275e-7,"about_ca_system_score_gemma":0.0000055488226,"threshold_uncertainty_score":0.27332535},"labels":[],"label_agreement":null},{"id":"W2319778989","doi":"10.1017/s174392131202443x","title":"Modelling X-ray Pulse Profiles of Millisecond Pulsars","year":2012,"lang":"en","type":"article","venue":"Proceedings of the International Astronomical Union","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Millisecond pulsar; Neutron star; Physics; Millisecond; Astrophysics; RADIUS; Pulsar; Pulse (music); X-ray pulsar; Light curve; Accretion (finance); Doppler effect; Rotation (mathematics); Astronomy; Optics; Geometry; Detector","score_opus":0.012219916455796448,"score_gpt":0.19686321944095805,"score_spread":0.1846433029851616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319778989","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971511,0.000030056437,0.00006736161,0.00017523605,0.0005808357,0.000090029025,0.00020033153,0.0000030909866,0.0017019919],"genre_scores_gemma":[0.99735254,0.000003380167,0.0021887135,0.0000091570355,0.00025520255,0.0000010648827,0.00003662445,0.00000269412,0.00015060061],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993636,0.0000049492937,0.00022373226,0.000092913884,0.00017465942,0.0001401323],"domain_scores_gemma":[0.9996088,0.000023884048,0.00019281819,0.00004077326,0.000088301225,0.000045388497],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002499944,0.00007282952,0.00011832372,0.00003526096,0.000029317216,0.000021414471,0.00036665358,0.000030963332,0.00045631384],"category_scores_gemma":[0.00001690579,0.000049983566,0.00006342034,0.000039366012,0.000055273056,0.0003128503,0.000042196723,0.000055120607,0.000013279095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018021195,0.00014486346,0.80088127,0.00008000082,0.00014162772,2.7142455e-8,0.00029661471,0.07738607,0.10825298,0.0071048527,0.0007474031,0.0047841044],"study_design_scores_gemma":[0.00050988025,0.00008969389,0.6579963,0.00012753469,0.00005312171,0.0000020311807,0.00021288768,0.07148109,0.25861052,0.0033973674,0.0072462643,0.00027332755],"about_ca_topic_score_codex":0.0003841689,"about_ca_topic_score_gemma":0.0000021378132,"teacher_disagreement_score":0.15035753,"about_ca_system_score_codex":0.0000046147898,"about_ca_system_score_gemma":0.000009003821,"threshold_uncertainty_score":0.49963164},"labels":[],"label_agreement":null},{"id":"W2323398558","doi":"10.1103/physrevb.85.134202","title":"Evidence of fivefold-coordinated Ge atoms in amorphous GeO<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:msub><mml:mrow/><mml:mn>2</mml:mn></mml:msub></mml:math>under pressure using inelastic x-ray scattering","year":2012,"lang":"lv","type":"article","venue":"Physical Review B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Amorphous solid; Octahedron; Tetrahedron; Materials science; Physics; Crystallography; Chemistry; Crystal structure","score_opus":0.029140303904896067,"score_gpt":0.2649055024796842,"score_spread":0.23576519857478812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323398558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9739179,0.022761313,0.00022262214,0.00022734178,0.0012261268,0.00012762661,0.00033652087,0.00005442924,0.0011261016],"genre_scores_gemma":[0.99130446,0.006124894,0.00045049682,0.00048549566,0.001157082,0.000077726305,0.00026289598,0.000089798115,0.000047173315],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99563473,0.00036199146,0.0010543644,0.00078289985,0.00096261164,0.0012033876],"domain_scores_gemma":[0.99660844,0.00093538576,0.0009884865,0.0009190881,0.00008678452,0.0004618105],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011483864,0.000529892,0.0006254522,0.00009875361,0.00035000188,0.0002773436,0.00086006697,0.00035092732,0.0032520213],"category_scores_gemma":[0.0005067741,0.00061879185,0.00058313913,0.0006118001,0.00047020463,0.0011801673,0.00048977614,0.0005703628,0.0013492028],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000666657,0.000978267,0.00063766417,0.022691716,0.0011695126,0.00034663125,0.0020670604,0.009445843,0.055715322,0.89776415,0.0032350204,0.0052821287],"study_design_scores_gemma":[0.0010312637,0.0011875198,0.008127134,0.025429958,0.0034095147,0.00021614748,0.00020991213,0.88130474,0.06978603,0.00033475526,0.0070573986,0.0019056019],"about_ca_topic_score_codex":0.002615545,"about_ca_topic_score_gemma":0.00023666622,"teacher_disagreement_score":0.8974294,"about_ca_system_score_codex":0.000006437889,"about_ca_system_score_gemma":0.00028605887,"threshold_uncertainty_score":0.99962634},"labels":[],"label_agreement":null},{"id":"W2324154121","doi":"10.1093/gji/ggu355","title":"Flat versus normal subduction zones: a comparison based on 3-D regional traveltime tomography and petrological modelling of central Chile and western Argentina (29°–35°S)","year":2014,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Subduction; Geology; Seismic tomography; Seismology; Slab; Lithosphere; Forearc; Slab window; Trench; Induced seismicity; Mantle (geology); Episodic tremor and slip; Mantle wedge; Geophysics; Tectonics; Oceanic crust","score_opus":0.025716132489367893,"score_gpt":0.22621425945600987,"score_spread":0.200498126966642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2324154121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99257785,0.0000360634,0.005612206,0.0002895214,0.00092634564,0.00005870021,0.000074569485,0.0000123828495,0.00041235122],"genre_scores_gemma":[0.99792224,0.00003021537,0.0008525765,0.0000829953,0.00096203125,7.222809e-7,0.00012465053,0.000004248535,0.000020347157],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9986532,0.000094939336,0.0003134569,0.00023183627,0.00045079543,0.00025581976],"domain_scores_gemma":[0.99930966,0.00017197881,0.00019983064,0.000076591394,0.00006401523,0.00017791713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019726371,0.00015732313,0.00026108357,0.00010833849,0.00014173584,0.00012581832,0.0001369607,0.0000651022,0.00027232445],"category_scores_gemma":[0.000012707605,0.00012501454,0.00008846026,0.000060897157,0.0001300079,0.00020944826,0.000016608392,0.00022419455,0.00001413852],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009466943,0.0013339216,0.43561742,0.00013326528,0.0007731673,0.00007025659,0.0010517404,0.49918264,0.0058028144,0.011551411,0.0013126681,0.03370375],"study_design_scores_gemma":[0.0016988269,0.0009736786,0.5196745,0.00004531824,0.000049995768,0.00004255462,0.000026688991,0.47319666,0.0003019622,0.0017474801,0.002022021,0.0002203508],"about_ca_topic_score_codex":0.00019763818,"about_ca_topic_score_gemma":0.000023028455,"teacher_disagreement_score":0.08405706,"about_ca_system_score_codex":0.00000377944,"about_ca_system_score_gemma":0.000018733355,"threshold_uncertainty_score":0.50979453},"labels":[],"label_agreement":null},{"id":"W2325876585","doi":"10.1139/cjes-2013-0218","title":"Implications of metallic iron for diamonds and nitrogen in the sublithospheric mantle","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle (geology); Diamond; Kimberlite; Mineral redox buffer; Geology; Lithosphere; Metal; Geochemistry; Mantle plume; Transition zone; Materials science; Tectonics; Metallurgy; Paleontology","score_opus":0.0174132832002935,"score_gpt":0.21551800874832255,"score_spread":0.19810472554802905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325876585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99716085,0.0005649811,0.000050139937,0.00074006803,0.00012397331,0.00007463537,0.0000402542,5.748414e-7,0.001244517],"genre_scores_gemma":[0.9988647,0.00001861948,0.00093056395,0.00011085955,0.000059202725,5.1231683e-7,0.0000020000043,7.935911e-7,0.000012709644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994377,0.000053265085,0.0001735585,0.00007152048,0.00009378011,0.00017018232],"domain_scores_gemma":[0.999497,0.00014836108,0.00012007783,0.000066359826,0.00004239059,0.00012579054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010659193,0.000045245397,0.00011718215,0.000075237986,0.00014390927,0.00008465241,0.00027947186,0.00001715281,0.00013615175],"category_scores_gemma":[0.00006402839,0.000027239592,0.000029772213,0.00021268107,0.000201679,0.00016216702,0.0000018562737,0.000032975007,0.0000018222238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005742453,0.000005736635,0.9820945,0.000020839865,0.000008649845,0.0000017208264,0.000849464,0.00057021255,0.000529225,0.008906924,0.0002072037,0.006799726],"study_design_scores_gemma":[0.00011798335,0.00024721966,0.9606376,0.00001067694,0.0000144803,0.000016638163,0.00022188938,0.00027292207,0.00022861092,0.026190009,0.0119838165,0.000058108977],"about_ca_topic_score_codex":0.008964264,"about_ca_topic_score_gemma":0.12835518,"teacher_disagreement_score":0.11939091,"about_ca_system_score_codex":2.9727832e-7,"about_ca_system_score_gemma":0.00019956652,"threshold_uncertainty_score":0.9976351},"labels":[],"label_agreement":null},{"id":"W2326489194","doi":"10.1002/2015jb012460","title":"Structure and anisotropy of the crust in the Cyclades, Greece, using receiver functions constrained by in situ rock textural data","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Receiver function; Crust; CYCLADES; Anisotropy; Seismic anisotropy; Blueschist; Seismology; Petrology; Lithology; Magmatism; Subduction; Eclogite; Geophysics; Geochemistry; Mantle (geology); Tectonics","score_opus":0.049228167592121834,"score_gpt":0.31382110815581676,"score_spread":0.2645929405636949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2326489194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979935,0.00013021083,0.000028734057,0.0009652497,0.00015435021,0.00015414871,0.00043665583,0.000001320999,0.0001357863],"genre_scores_gemma":[0.9994263,0.00009436263,0.000083998064,0.00003818742,0.00024905408,1.7929194e-7,0.000011029855,0.00000300742,0.00009390151],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99784845,0.00056850247,0.00034419468,0.00017626827,0.0007116489,0.00035095174],"domain_scores_gemma":[0.998644,0.00062572025,0.00016479747,0.00033120858,0.00014076546,0.000093511175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00089329126,0.00010553417,0.00027656552,0.00009185065,0.00014293472,0.00008153562,0.0006883906,0.000060775423,0.0002158107],"category_scores_gemma":[0.00031426936,0.00004534547,0.000045312314,0.00038720996,0.00030548364,0.0004315353,0.000096834294,0.00042935772,0.0000079943],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000936457,0.00025961074,0.065323584,0.000090527035,0.00013472368,0.00010264219,0.0010994804,0.0010913837,0.88156223,0.0005494006,0.00827028,0.04057965],"study_design_scores_gemma":[0.0014382747,0.00045127174,0.9819405,0.00023351682,0.000026830028,0.000065083885,0.00041504117,0.0024908728,0.0040394524,0.005256522,0.00347791,0.0001647267],"about_ca_topic_score_codex":0.0017265946,"about_ca_topic_score_gemma":0.0013030033,"teacher_disagreement_score":0.9166169,"about_ca_system_score_codex":0.000005124408,"about_ca_system_score_gemma":0.00018150354,"threshold_uncertainty_score":0.26101062},"labels":[],"label_agreement":null},{"id":"W2329278892","doi":"10.1021/jp207170w","title":"Effects of High Pressure on Azobenzene and Hydrazobenzene Probed by Raman Spectroscopy","year":2011,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Ontario Ministry of Research and Innovation","keywords":"Azobenzene; Raman spectroscopy; Diamond anvil cell; Compression (physics); Chemistry; Molecule; High pressure; Spectroscopy; Photochemistry; Analytical Chemistry (journal); Materials science; Thermodynamics; Organic chemistry; Optics; Composite material","score_opus":0.004079129278995682,"score_gpt":0.17827653980402688,"score_spread":0.1741974105250312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2329278892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982993,0.00031771098,0.000015651744,0.000043328866,0.00006872835,0.00008475752,0.000029864012,0.000005889034,0.0011347575],"genre_scores_gemma":[0.9994582,0.000047014742,0.00006948372,0.000023304841,0.00032334687,2.887515e-7,0.0000035986325,0.0000048751167,0.00006990402],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99921095,0.000060148137,0.00020587487,0.00009971328,0.00025468515,0.00016864578],"domain_scores_gemma":[0.9992365,0.00017630213,0.0002943592,0.00014551857,0.000044445573,0.00010282782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017435096,0.0001378506,0.00031518293,0.000009674599,0.000052530002,0.000015985066,0.0002754232,0.000042959782,0.00018689808],"category_scores_gemma":[0.000024724288,0.00007939281,0.00006161685,0.00005541213,0.000077004646,0.000083071696,0.000017395983,0.00016826279,0.0000065586987],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030828314,0.00012842653,0.000117897805,0.00017704381,0.000081017555,0.000004796865,0.00032715918,0.00009139293,0.9979205,0.000049299764,0.00046884408,0.00032534904],"study_design_scores_gemma":[0.00041296807,0.00045513536,0.008221704,0.000057968635,0.00015435206,0.0000071516774,0.000011545717,0.000095910415,0.987593,0.0026513191,0.00024864534,0.00009030771],"about_ca_topic_score_codex":0.00022055962,"about_ca_topic_score_gemma":0.0000015038357,"teacher_disagreement_score":0.0103274975,"about_ca_system_score_codex":0.0000012891219,"about_ca_system_score_gemma":0.000017572156,"threshold_uncertainty_score":0.3237545},"labels":[],"label_agreement":null},{"id":"W2329721496","doi":"10.1107/s0108767308098656","title":"First-principles calculations of pressure-induced magnetic transition in siderite FeCO<sub>3</sub>","year":2008,"lang":"en","type":"article","venue":"Acta Crystallographica Section A Foundations of Crystallography","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences; University of Saskatchewan","funders":"","keywords":"Siderite; Transition (genetics); Materials science; Chemistry; Metallurgy","score_opus":0.018057106341720218,"score_gpt":0.21046304174466815,"score_spread":0.19240593540294793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2329721496","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99628997,0.00019281468,0.0007750678,0.0003119826,0.0003818561,0.00067652494,0.0003031819,0.00009133283,0.0009772942],"genre_scores_gemma":[0.9980115,0.0006808593,0.0007590304,0.000028724075,0.0000796945,0.000028477778,0.00038753983,0.000016661576,0.000007487138],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973674,0.00021872635,0.001006972,0.0004933006,0.0005006962,0.0004129053],"domain_scores_gemma":[0.99835765,0.0002490148,0.00046232546,0.00049101055,0.00029590895,0.00014409747],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00036718615,0.00031757556,0.0005479503,0.0014980028,0.00040070552,0.000048387225,0.00029986343,0.00024526197,0.00039173855],"category_scores_gemma":[0.000056944158,0.00033221525,0.00038595957,0.0022714618,0.00047036435,0.00066199113,0.000023524262,0.00022153962,0.0000011364851],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022162627,0.00050436676,0.0745542,0.0003194477,0.00026391647,0.000012587558,0.0013168291,0.05049033,0.87140596,0.0004832288,0.00009450294,0.0003330042],"study_design_scores_gemma":[0.0012153718,0.00060753577,0.9748722,0.00011022317,0.00018340445,0.00004273333,0.0001786854,0.0053345333,0.002468037,0.0021825382,0.012297674,0.00050708617],"about_ca_topic_score_codex":0.0029409323,"about_ca_topic_score_gemma":0.0114545105,"teacher_disagreement_score":0.90031797,"about_ca_system_score_codex":0.000005325471,"about_ca_system_score_gemma":0.00010218206,"threshold_uncertainty_score":0.999913},"labels":[],"label_agreement":null},{"id":"W2330983677","doi":"10.1130/g33523.1","title":"Deciphering high-pressure metamorphism in collisional context using microprobe mapping methods: Application to the Stak eclogitic massif (northwest Himalaya)","year":2012,"lang":"en","type":"article","venue":"Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"CHIST-ERA; Agence Nationale de la Recherche","keywords":"Context (archaeology); Massif; Metamorphism; Geology; Humanities; Cartography; Art; Geography; Paleontology","score_opus":0.025977014402664634,"score_gpt":0.265604309874823,"score_spread":0.23962729547215833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2330983677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9702798,0.0014018983,0.025666533,0.00069102144,0.0011341992,0.0005237429,0.00010686786,0.000030277972,0.00016561832],"genre_scores_gemma":[0.96749365,0.000014769973,0.031370815,0.00053885975,0.0003931873,0.000020949836,0.00008648295,0.000007557967,0.000073698706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981377,0.0004138676,0.00035924054,0.00032347662,0.0001571847,0.00060851756],"domain_scores_gemma":[0.9990081,0.00033384646,0.00014128577,0.0003287124,0.000053341955,0.00013471833],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010376297,0.00018764136,0.00035899575,0.00009701205,0.00020233422,0.000047872778,0.00035800354,0.00012587523,0.0009398937],"category_scores_gemma":[0.00007200851,0.00013722306,0.000048146416,0.0002786115,0.00008965594,0.00019102175,0.00008452959,0.00014882647,0.00024275793],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015690712,0.00009922379,0.7371874,0.00008313088,0.00020041974,0.00001802478,0.0021589866,0.111068815,0.09265154,0.0061382162,0.00049281906,0.04974454],"study_design_scores_gemma":[0.00035157648,0.000045885794,0.86774087,0.00001799772,0.00006246503,0.00002976567,0.00026419564,0.0055338973,0.0014811901,0.0014735206,0.12269293,0.00030567858],"about_ca_topic_score_codex":0.017068258,"about_ca_topic_score_gemma":0.0044665537,"teacher_disagreement_score":0.13055351,"about_ca_system_score_codex":0.0000083654295,"about_ca_system_score_gemma":0.000046388057,"threshold_uncertainty_score":0.99997336},"labels":[],"label_agreement":null},{"id":"W2332301513","doi":"10.1139/p11-105","title":"Analysis of elastic constants and thermal energy of ionic materials","year":2011,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Thermodynamics; Physics; Ionic bonding; Isothermal process; Thermal; Constant (computer programming); Thermal expansion; Volume (thermodynamics); Elastic modulus; Ion; Quantum mechanics","score_opus":0.014746891520527544,"score_gpt":0.17688945086611826,"score_spread":0.16214255934559071,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2332301513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982431,0.00020565199,0.00010549105,0.000004281357,0.00025890037,0.000016312013,0.00043975573,7.0436295e-7,0.0007257989],"genre_scores_gemma":[0.99977756,0.000023751727,0.00008813557,0.000015653424,0.00007176523,4.8748422e-8,0.00001098674,0.0000021453232,0.000009957673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993483,0.0000520697,0.00030194374,0.00006041661,0.000096608754,0.00014069212],"domain_scores_gemma":[0.99922997,0.000039123264,0.00034282304,0.00008799067,0.00010884141,0.00019127088],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015169906,0.000071212,0.00035416678,0.00012925411,0.000032549084,0.00001453588,0.00012892197,0.00003078324,0.0014272679],"category_scores_gemma":[0.000011652751,0.000056789617,0.000062902836,0.00019593452,0.00013161573,0.00010528533,0.0000030574322,0.000027589818,0.0000017035371],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004716702,0.00013173383,0.62130535,0.0003149536,0.008658711,0.0003283355,0.0091887945,0.009279345,0.22523713,0.066277996,0.00045845367,0.058347534],"study_design_scores_gemma":[0.00043265487,0.00040316087,0.88479024,0.00008272071,0.0015776759,0.000012067997,0.00017071523,0.000295047,0.10534387,0.006395239,0.0002559909,0.00024062766],"about_ca_topic_score_codex":0.03469105,"about_ca_topic_score_gemma":0.016608499,"teacher_disagreement_score":0.2634849,"about_ca_system_score_codex":0.000001914707,"about_ca_system_score_gemma":0.00026691073,"threshold_uncertainty_score":0.99948555},"labels":[],"label_agreement":null},{"id":"W2333531544","doi":"10.1103/physreve.87.063113","title":"Partial ionization in dense plasmas: Comparisons among average-atom density functional models","year":2013,"lang":"en","type":"article","venue":"Physical Review E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute for Microstructural Sciences","funders":"U.S. Department of Energy","keywords":"Ionization; Plasma; Atom (system on chip); Atomic physics; Statistical physics; Physics; Computational physics; Ion; Nuclear physics; Quantum mechanics; Computer science","score_opus":0.02529223022175873,"score_gpt":0.23216800487765013,"score_spread":0.2068757746558914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2333531544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955988,0.0007342181,0.0017574944,0.00018829515,0.00022799792,0.00039651204,0.000023637684,0.00003055219,0.0010424921],"genre_scores_gemma":[0.9985499,0.00061045244,0.00010324323,0.00028017833,0.00022864647,0.000012955489,0.00016689207,0.0000036877243,0.00004407229],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989266,0.00012850843,0.00023706892,0.00023695141,0.00024095921,0.00022995743],"domain_scores_gemma":[0.9994787,0.00009976945,0.000084881955,0.00016144257,0.00006044676,0.00011474424],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014025967,0.00013290334,0.00033932488,0.000021555634,0.000081375234,0.00006133965,0.00010529165,0.000028072332,0.001293904],"category_scores_gemma":[0.000026242218,0.000104236446,0.0000721141,0.000171457,0.00004646242,0.00041624738,0.000018005743,0.00010413885,0.0014973655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013413762,0.0010561981,0.5403877,0.002368523,0.00019609953,0.000048025577,0.00069518684,0.31087875,0.0028000632,0.041149702,0.06248988,0.037795752],"study_design_scores_gemma":[0.00029335165,0.000045520603,0.67360425,0.00039642895,0.00005479092,0.0000022461281,0.0000060221837,0.30457765,0.00038462252,0.015765348,0.0045373724,0.00033239162],"about_ca_topic_score_codex":0.0020257926,"about_ca_topic_score_gemma":0.0003984659,"teacher_disagreement_score":0.13321659,"about_ca_system_score_codex":0.0000039249203,"about_ca_system_score_gemma":0.000026723716,"threshold_uncertainty_score":0.99961907},"labels":[],"label_agreement":null},{"id":"W2334257424","doi":"10.1093/gji/ggw124","title":"Imaging anisotropic layering with Bayesian inversion of multiple data types","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Anisotropy; Seismic anisotropy; Lithosphere; Layering; Azimuth; Seismogram; Geophysics; Seismology; Mantle (geology); Tectonics; Geometry; Physics; Mathematics; Optics","score_opus":0.014046788522088606,"score_gpt":0.22348215171520716,"score_spread":0.20943536319311856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2334257424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905065,0.000030247142,0.006099841,0.0012113799,0.00088504836,0.00004776546,0.00031777017,0.000016242946,0.0008852241],"genre_scores_gemma":[0.9977333,0.000021735501,0.0014445509,0.000052492192,0.0006026298,1.3836325e-7,0.00004418438,0.0000034781356,0.000097516415],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99918133,0.000027253825,0.00016837569,0.0001581294,0.0003156434,0.0001492682],"domain_scores_gemma":[0.99942034,0.000103899,0.00013691165,0.00016599071,0.00009084387,0.00008198353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010085283,0.000083834195,0.00012320852,0.00004801177,0.000059447633,0.00006119329,0.00048920035,0.000016528407,0.0009295707],"category_scores_gemma":[0.000041366653,0.000047099056,0.000030959167,0.000047957892,0.000049760412,0.0005482813,0.000059452283,0.000064109074,0.00009478912],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061584584,0.0001532331,0.7143182,0.000029605055,0.0003785515,0.00017100625,0.00015321201,0.0011441135,0.11010287,0.0019197259,0.0035729518,0.16744064],"study_design_scores_gemma":[0.0026035595,0.00031035015,0.89519453,0.00041154207,0.00007978215,0.00015725286,0.00006008305,0.053810515,0.012285356,0.006413582,0.028178385,0.0004950374],"about_ca_topic_score_codex":0.00035462988,"about_ca_topic_score_gemma":0.00007006682,"teacher_disagreement_score":0.18087631,"about_ca_system_score_codex":0.000004238518,"about_ca_system_score_gemma":0.000035259745,"threshold_uncertainty_score":0.9999837},"labels":[],"label_agreement":null},{"id":"W2334333429","doi":"10.2138/am-2002-2-307","title":"X-ray spectroscopic investigations of fluids in the hydrothermal diamond anvil cell: The hydration structure of aqueous La <sup>3+</sup> up to 300 °C and 1600 bars","year":2002,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"X-ray absorption fine structure; Aqueous solution; Diamond anvil cell; Ion; Hydrothermal circulation; Chemistry; Analytical Chemistry (journal); Bond length; Absorption (acoustics); Crystallography; Microprobe; X-ray absorption spectroscopy; Extended X-ray absorption fine structure; Absorption spectroscopy; Materials science; Spectroscopy; Mineralogy; Crystal structure; Physical chemistry; Diffraction","score_opus":0.008259808707889053,"score_gpt":0.20073710123790456,"score_spread":0.1924772925300155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2334333429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959511,0.00017903582,0.000021331283,0.0007691008,0.00004236554,0.00021658924,0.0001697475,0.000005868393,0.0026448208],"genre_scores_gemma":[0.99889666,0.00004389785,0.00045874648,0.00032692886,0.00006725854,0.0000026883488,0.000036648842,0.0000038404705,0.00016334858],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99907064,0.0002174682,0.00022148353,0.00016148112,0.00016278465,0.00016611455],"domain_scores_gemma":[0.99941957,0.00018764881,0.000106281725,0.00022304463,0.000016342754,0.000047120368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000117488875,0.00011536436,0.00020460555,0.000046646306,0.00007111693,0.000041997446,0.00022149623,0.000028304996,0.00042951907],"category_scores_gemma":[0.000034122502,0.00006745313,0.000025689496,0.00029792095,0.0005504315,0.00007126651,0.000011798942,0.0000812293,0.000011535341],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000080461985,0.00012882824,0.19942595,0.00012677668,0.00007688563,0.00002964893,0.04388457,0.13229452,0.5947212,0.0026035549,0.012086695,0.014540917],"study_design_scores_gemma":[0.0008435655,0.0012835888,0.9288939,0.000048602615,0.000089506866,0.000019223397,0.0030475534,0.028036984,0.02413455,0.0017403397,0.011283895,0.0005782421],"about_ca_topic_score_codex":0.011760397,"about_ca_topic_score_gemma":0.0014901188,"teacher_disagreement_score":0.729468,"about_ca_system_score_codex":0.0000017029727,"about_ca_system_score_gemma":0.000015809297,"threshold_uncertainty_score":0.99482036},"labels":[],"label_agreement":null},{"id":"W2336735841","doi":"10.2138/am-2016-5425","title":"Some thermodynamic properties of larnite (β-Ca <sub>2</sub> SiO <sub>4</sub> ) constrained by high <i>T</i> / <i>P</i> experiment and/or theoretical simulation","year":2016,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Division of Materials Research; U.S. Department of Energy","keywords":"Bulk modulus; CASTEP; Pseudopotential; Heat capacity; Compressibility; Thermal expansion; Thermodynamics; Phonon; Isobaric process; Diamond anvil cell; Chemistry; Density functional theory; Materials science; Analytical Chemistry (journal); Crystallography; Condensed matter physics; Physics; High pressure; Computational chemistry","score_opus":0.007740100044726523,"score_gpt":0.20218268726109567,"score_spread":0.19444258721636914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2336735841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975153,0.00030596324,0.00023767947,0.00046217,0.00017544124,0.00030651147,0.0007539244,0.000054804506,0.00018817744],"genre_scores_gemma":[0.9988495,0.00038874557,0.00008347191,0.00033314852,0.00016276122,0.000011530764,0.00013282061,0.000015046572,0.000022948756],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9982456,0.00020339401,0.00041382934,0.0004228217,0.0002893971,0.00042497803],"domain_scores_gemma":[0.9989627,0.00026762544,0.00026132312,0.00028288766,0.00006557281,0.00015987644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018153852,0.0002925894,0.0004944,0.00005456616,0.00011289338,0.00005754132,0.00019121882,0.000069052876,0.00012984536],"category_scores_gemma":[0.000069270005,0.00016566167,0.000069662055,0.00013796295,0.0021920598,0.00022570314,0.000037943417,0.00006973801,0.000060685426],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027892075,0.000053546068,0.00051217404,0.000022183009,0.00003931965,0.00000832525,0.00010247764,0.00029844083,0.9753497,0.001321079,0.00021821601,0.021795573],"study_design_scores_gemma":[0.0013137846,0.0012427483,0.0074017555,0.00012379611,0.00008181393,0.0000121927715,0.00014940668,0.0042005195,0.9824079,0.0018264137,0.0005277956,0.00071186636],"about_ca_topic_score_codex":0.00095283927,"about_ca_topic_score_gemma":0.00013111375,"teacher_disagreement_score":0.021083707,"about_ca_system_score_codex":0.0000071725744,"about_ca_system_score_gemma":0.00005714022,"threshold_uncertainty_score":0.8076736},"labels":[],"label_agreement":null},{"id":"W2337691691","doi":"10.1021/acs.jpcc.5b12009","title":"Crystal Structure and Superconductivity of PH<sub>3</sub> at High Pressures","year":2016,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Basic Energy Sciences; Western Canada Research Grid; Specialized Research Fund for the Doctoral Program of Higher Education of China; National Key Research and Development Program of China; National Nuclear Security Administration; Office of Science; National Natural Science Foundation of China; Priority Academic Program Development of Jiangsu Higher Education Institutions; Natural Science Foundation of Jiangsu Province; National Science Foundation; Compute Canada; U.S. Department of Energy","keywords":"Monoclinic crystal system; Superconductivity; Crystal structure prediction; Crystal structure; Phase (matter); High pressure; Coupling (piping); Materials science; Crystallography; Condensed matter physics; Crystal (programming language); High-temperature superconductivity; Phonon; Chemical physics; Topology (electrical circuits); Chemistry; Physics; Thermodynamics","score_opus":0.006051598103393529,"score_gpt":0.18677518721447073,"score_spread":0.1807235891110772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2337691691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992338,0.00014031779,0.0000042010474,0.00014856689,0.00007619424,0.000033779732,0.00026635942,0.0000036464137,0.000093162875],"genre_scores_gemma":[0.999366,0.000042248455,0.000010263441,0.0000069985076,0.0005315153,6.52712e-8,0.0000031915267,0.0000031887662,0.00003654974],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999269,0.00006143025,0.00018000431,0.00008893561,0.00025457027,0.00014603588],"domain_scores_gemma":[0.99924815,0.00024714557,0.00020330495,0.00014324073,0.000069574875,0.00008856984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015411255,0.00011279216,0.00026240037,0.0000075915214,0.00006401444,0.0000138757805,0.00020443542,0.000043328775,0.00030728307],"category_scores_gemma":[0.00003802319,0.000052086998,0.00006193512,0.000038428294,0.0002085625,0.00017866373,0.000034503748,0.00009458429,0.000003128089],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011873338,0.000016642985,0.000634957,0.00005335032,0.000046081554,0.0000023846446,0.000115768955,0.00009291374,0.9976112,0.000010853503,0.00021378366,0.0010832985],"study_design_scores_gemma":[0.0002712783,0.00006725635,0.026023965,0.00003836523,0.00006727147,0.000032277432,0.000012839003,0.000015293432,0.97031397,0.0029231713,0.00015728067,0.00007703368],"about_ca_topic_score_codex":0.00005631176,"about_ca_topic_score_gemma":0.000008409889,"teacher_disagreement_score":0.027297264,"about_ca_system_score_codex":0.0000027118972,"about_ca_system_score_gemma":0.000026029045,"threshold_uncertainty_score":0.3364534},"labels":[],"label_agreement":null},{"id":"W2339084463","doi":"10.1103/physreve.94.053211","title":"Pair potentials for warm dense matter and their application to x-ray Thomson scattering in aluminum and beryllium","year":2016,"lang":"en","type":"article","venue":"Physical review. E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Université de Montréal; Regroupement Québécois sur les Matériaux de Pointe","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada","keywords":"Beryllium; Aluminium; X-ray; Scattering; Warm dense matter; Dense matter; Physics; Atomic physics; Thomson scattering; Nuclear physics; Materials science; Plasma; Astrophysics; Optics; Metallurgy; Neutron star","score_opus":0.009252151187755903,"score_gpt":0.25052185047524167,"score_spread":0.24126969928748576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339084463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930112,0.0011906592,0.0014334439,0.0034415696,0.00008528216,0.00066565024,0.00010639549,0.000012096097,0.000053751424],"genre_scores_gemma":[0.99799067,0.0006995004,0.00016449318,0.00083834864,0.00019230467,0.000042014548,0.00001657994,0.000005134609,0.000050951025],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9992564,0.00004796135,0.00016216855,0.00026937667,0.00006742889,0.00019666493],"domain_scores_gemma":[0.9995328,0.000154041,0.000051499002,0.00015033841,0.000018942288,0.00009236159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024529334,0.00012008678,0.0002876659,0.000020265157,0.00004217028,0.000032215412,0.000084655316,0.000018415349,0.000049342805],"category_scores_gemma":[0.000021633079,0.00006828551,0.0000367044,0.00005710228,0.000032738935,0.00011354108,0.000024081453,0.000022602211,0.00015689612],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076575656,0.00007704262,0.04173322,0.0016268692,0.00003271788,0.0000016815152,0.00038465564,0.000021678608,0.5197186,0.0003804683,0.0047664177,0.43118012],"study_design_scores_gemma":[0.0009912209,0.0003495889,0.72912705,0.0023762574,0.00012639895,0.000007792879,0.000026909647,0.0011328679,0.05075257,0.028064204,0.18603751,0.001007631],"about_ca_topic_score_codex":0.00015513804,"about_ca_topic_score_gemma":0.00005964167,"teacher_disagreement_score":0.68739384,"about_ca_system_score_codex":0.0000016869659,"about_ca_system_score_gemma":0.0000051322454,"threshold_uncertainty_score":0.27846023},"labels":[],"label_agreement":null},{"id":"W2339668439","doi":"10.1002/2016gl068688","title":"Linear analysis of melt band formation in a mid‐ocean ridge corner flow","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Asthenosphere; Streamlines, streaklines, and pathlines; Anisotropy; Porosity; Isotropy; Mineralogy; Lithosphere; Geophysics; Mechanics; Geotechnical engineering; Optics; Seismology","score_opus":0.03125748140665406,"score_gpt":0.2821310240945426,"score_spread":0.25087354268788853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339668439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971322,0.00001598671,0.00017252544,0.0017112055,0.00009514286,0.00016709956,0.00039158037,0.000013390155,0.00030086626],"genre_scores_gemma":[0.9993247,0.00002458566,0.000116954434,0.000116986805,0.00017266256,0.0000024464073,0.0001478222,0.000004121028,0.000089729416],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978199,0.00031128209,0.00030544546,0.00028699503,0.00073215965,0.00054424105],"domain_scores_gemma":[0.9988,0.0005815149,0.000068043104,0.00030429705,0.000105406245,0.00014076743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007200043,0.00011995729,0.00035482302,0.0004380509,0.000078173456,0.00004200262,0.0003034378,0.000052755604,0.0006596305],"category_scores_gemma":[0.0001483029,0.00007580971,0.0001294757,0.0011793858,0.00020594437,0.0003534226,0.000031016512,0.00013902792,0.00034545752],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007318509,0.00024048351,0.041826658,0.00015926763,0.00063318195,0.00011577829,0.0012601115,0.008007674,0.8983189,0.00038626997,0.011973369,0.03634646],"study_design_scores_gemma":[0.0013435768,0.00032050925,0.87772995,0.00010962838,0.00015983818,0.0000010263356,0.00005941893,0.03157137,0.08240845,0.0013306813,0.004537779,0.0004277476],"about_ca_topic_score_codex":0.0036725418,"about_ca_topic_score_gemma":0.00076516886,"teacher_disagreement_score":0.83590335,"about_ca_system_score_codex":0.000010111052,"about_ca_system_score_gemma":0.000026361307,"threshold_uncertainty_score":0.72224915},"labels":[],"label_agreement":null},{"id":"W2341747055","doi":"10.1016/j.tecto.2016.04.024","title":"Mica-dominated seismic properties of mid-crust beneath west Yunnan (China) and geodynamic implications","year":2016,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Mylonite; Mica; Lineation; Foliation (geology); Metamorphic rock; Anisotropy; Crust; Schist; Quartz; Gneiss; Shear wave splitting; Mineralogy; Shear (geology); Petrology; Geochemistry; Shear zone; Seismology; Tectonics","score_opus":0.009646002981275588,"score_gpt":0.18668584507164174,"score_spread":0.17703984209036616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2341747055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99769944,0.00016837982,0.00015963273,0.00047377244,0.00014433208,0.00021151167,0.00042419595,0.00005219,0.00066654664],"genre_scores_gemma":[0.9993681,0.000097568525,0.00014313943,0.00003122079,0.0000833627,0.000004843247,0.00003693632,0.0000083191835,0.00022651014],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991201,0.000040271716,0.0002147123,0.00026057288,0.0001127348,0.00025158277],"domain_scores_gemma":[0.9993846,0.00004201095,0.0001318772,0.00030421626,0.000056656303,0.00008064177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007483374,0.00016431106,0.00025896713,0.000045368673,0.0001227138,0.000035116216,0.00020722611,0.000054633765,0.00016303842],"category_scores_gemma":[0.000013792621,0.000103346094,0.000045686786,0.00013477296,0.00019443958,0.00019337147,0.000030761457,0.000048519294,0.00010286995],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044839613,0.000040151634,0.005307588,0.000068369285,0.0000431055,0.0000010999139,0.00018049142,0.00015339814,0.9585892,0.000747041,0.00007659801,0.034748103],"study_design_scores_gemma":[0.0009185616,0.00026624656,0.7640401,0.00017807382,0.00010176695,0.000009372218,0.00004047144,0.0017545534,0.22128615,0.009367628,0.0014995874,0.000537474],"about_ca_topic_score_codex":0.0023227544,"about_ca_topic_score_gemma":0.00018499866,"teacher_disagreement_score":0.75873256,"about_ca_system_score_codex":0.0000040142463,"about_ca_system_score_gemma":0.000048082686,"threshold_uncertainty_score":0.42143312},"labels":[],"label_agreement":null},{"id":"W2342126105","doi":"10.2172/1167485","title":"The LOFT perspective on neutron star thermonuclear bursts: White paper in support of the mission concept of the large observatory for X-ray timing","year":2015,"lang":"en","type":"report","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Los Alamos National Laboratory; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; U.S. Department of Energy","keywords":"Physics; Observatory; Neutron star; Thermonuclear fusion; Astronomy; Sky; Astrophysics; White dwarf; Stars; Nuclear physics","score_opus":0.03747363072811294,"score_gpt":0.2697535534158659,"score_spread":0.23227992268775294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342126105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7925087,0.0034993954,0.0000033471306,0.004469134,0.008848365,0.0049057202,0.005922675,0.000057087695,0.17978556],"genre_scores_gemma":[0.9882721,0.00022233374,0.000035194065,0.0003661497,0.00034900205,0.000005292511,0.00007255797,0.000023421193,0.010653998],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975402,0.0002498665,0.00051000685,0.0003350907,0.0010042056,0.00036065327],"domain_scores_gemma":[0.99784356,0.00027844778,0.00058422086,0.0006932343,0.00053847884,0.00006203256],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0019024438,0.00026180886,0.00048694303,0.00002867626,0.00021355916,0.000038933944,0.00076775195,0.00021063909,0.0009337667],"category_scores_gemma":[0.00022211121,0.000107693406,0.00024137311,0.00013285705,0.00019443131,0.00009443538,0.00007867319,0.00025972043,0.000007932952],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018722296,0.00061810034,0.038114585,0.001074948,0.0010770289,0.000018439257,0.028426886,0.008527517,0.010064032,0.008067039,0.8967393,0.005399887],"study_design_scores_gemma":[0.0005737484,0.00034955528,0.17138122,0.00022244122,0.0001191694,0.0000017423516,0.0042408183,0.00012478081,0.0006962341,0.00090494123,0.82108706,0.00029825448],"about_ca_topic_score_codex":0.0046944455,"about_ca_topic_score_gemma":0.002832112,"teacher_disagreement_score":0.19576333,"about_ca_system_score_codex":0.00004196456,"about_ca_system_score_gemma":0.0009128607,"threshold_uncertainty_score":0.9999795},"labels":[],"label_agreement":null},{"id":"W2342629655","doi":"10.1021/acs.analchem.6b00373","title":"STEM EDX Nitrogen Mapping of Nanoinclusions in Milky Diamonds from Juina, Brazil, Using a Windowless Silicon Drift Detector System","year":2016,"lang":"en","type":"article","venue":"Analytical Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada)","funders":"Deutsche Forschungsgemeinschaft","keywords":"Silicon; Silicon drift detector; Detector; Scanning transmission electron microscopy; Chemistry; Spectroscopy; Analytical Chemistry (journal); Milky Way; Transmission electron microscopy; Nanotechnology; Mineralogy; Optics; Materials science; Physics; Environmental chemistry","score_opus":0.014450900403563999,"score_gpt":0.21792170220589674,"score_spread":0.20347080180233273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342629655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978402,0.00018307297,0.0000926404,0.000044621625,0.000105221734,0.00008351535,0.00043825514,0.000027465267,0.0011849965],"genre_scores_gemma":[0.99953365,0.000006717835,0.00009812173,0.0000151429385,0.0001968059,0.0000011615182,0.000030241185,0.000006780468,0.00011138451],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99857825,0.000051200073,0.00042979058,0.00034130298,0.000257846,0.00034160007],"domain_scores_gemma":[0.99909765,0.00025228676,0.00013001259,0.0003054048,0.000046330137,0.000168347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018243035,0.00017658455,0.00042443562,0.000039565446,0.000075258984,0.000030436142,0.00027630496,0.00015251174,0.0006990485],"category_scores_gemma":[0.0000296911,0.0001257337,0.000104350715,0.00019783505,0.00009762461,0.000106572916,0.0000639164,0.00008024438,0.000045478977],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048666257,0.00003491581,0.1689388,0.0002248143,0.00007478463,0.00004932426,0.00009665123,0.000093179246,0.82895917,0.000028158156,0.000050023944,0.0014015366],"study_design_scores_gemma":[0.0015415947,0.000046962894,0.07164078,0.0013144063,0.00018796971,0.000014306489,0.00051763037,0.018303208,0.9041709,0.00066176977,0.0008471313,0.0007533676],"about_ca_topic_score_codex":0.0024074663,"about_ca_topic_score_gemma":0.00015542934,"teacher_disagreement_score":0.09729802,"about_ca_system_score_codex":0.000017661447,"about_ca_system_score_gemma":0.00007930895,"threshold_uncertainty_score":0.7654091},"labels":[],"label_agreement":null},{"id":"W2343519287","doi":"10.1021/acs.jctc.5b01194","title":"Impact of Short-Range Forces on Defect Production from High-Energy Collisions","year":2016,"lang":"en","type":"article","venue":"Journal of Chemical Theory and Computation","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Basic Energy Sciences; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Kinetic energy; Force field (fiction); Range (aeronautics); Coulomb; Molecular dynamics; Ab initio; Interatomic potential; Atomic physics; Field (mathematics); Energy (signal processing); Potential energy; Physics; Work (physics); Molecular physics; Materials science; Classical mechanics; Nuclear physics; Thermodynamics; Quantum mechanics; Electron","score_opus":0.010441247375181874,"score_gpt":0.23904800158165473,"score_spread":0.22860675420647286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2343519287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99676174,0.0000992747,0.0027005195,0.000046854228,0.00022895345,0.000026651769,0.00004852167,0.0000036443362,0.000083851635],"genre_scores_gemma":[0.99949205,0.00004383432,0.00015054653,0.000009618293,0.0002833409,1.3882538e-7,0.000011504012,0.0000017262605,0.000007243126],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99940944,0.000107357795,0.00020431018,0.00007944317,0.00013272063,0.00006670994],"domain_scores_gemma":[0.99925125,0.00042619475,0.00015622996,0.000042901615,0.000069706315,0.000053727723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027036268,0.000063865016,0.00016359938,0.000036651705,0.000026671256,0.000015226798,0.00005371719,0.00003604087,0.00013051333],"category_scores_gemma":[0.00006830852,0.0000332695,0.00008013144,0.000047212146,0.00004493639,0.00014813454,0.0000041378066,0.00003185555,0.0000020025582],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004408011,0.0001660999,0.021106554,0.000023471963,0.00039947385,0.000010063474,0.00032801693,0.00672169,0.7294907,0.009325154,0.0005271529,0.22749361],"study_design_scores_gemma":[0.0008492783,0.0012498245,0.2973113,0.0002452535,0.00013280718,0.000023307393,0.000026192612,0.00023517213,0.19994967,0.49971545,0.0000623795,0.00019935807],"about_ca_topic_score_codex":0.000063854844,"about_ca_topic_score_gemma":0.0000019094714,"teacher_disagreement_score":0.529541,"about_ca_system_score_codex":0.0000031630752,"about_ca_system_score_gemma":0.000016813092,"threshold_uncertainty_score":0.14290296},"labels":[],"label_agreement":null},{"id":"W2344343959","doi":"10.1002/2015jb012579","title":"Effects of olivine fabric, melt‐rock reaction, and hydration on the seismic properties of peridotites: Insight from the Luobusha ophiolite in the Tibetan Plateau","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"National Natural Science Foundation of China","keywords":"Olivine; Geology; Pyroxene; Anisotropy; Mantle (geology); Mineralogy; Ophiolite; Peridotite; Seismic anisotropy; Plateau (mathematics); Dissolution; Geochemistry; Tectonics; Chemistry; Seismology","score_opus":0.028416449492756873,"score_gpt":0.255240203018413,"score_spread":0.22682375352565612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2344343959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99615616,0.00042855242,0.000011005556,0.0027699308,0.00011509758,0.00030103893,0.000033260658,0.0000022557326,0.00018269786],"genre_scores_gemma":[0.99869347,0.00063893944,0.000006583415,0.00010402145,0.0004661849,0.0000024493886,0.0000023245395,0.0000043942186,0.000081665625],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99733526,0.00093971187,0.00040082342,0.0001467885,0.00090537587,0.00027202515],"domain_scores_gemma":[0.9961658,0.0030124255,0.00025626546,0.0002435685,0.0002511387,0.00007081183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014616541,0.0001234271,0.0003253152,0.000083649466,0.00017199675,0.00008000325,0.00043601196,0.00004940047,0.000047893693],"category_scores_gemma":[0.00071498804,0.000042206375,0.000081664766,0.00026621766,0.00025305004,0.0002834623,0.00003716984,0.00034049727,0.000033060955],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014469933,0.0003495928,0.0036525836,0.00018179906,0.0002202591,0.00003688668,0.008747533,0.00060676975,0.9654975,0.0013248104,0.0013481289,0.016587123],"study_design_scores_gemma":[0.0009093217,0.001740497,0.8124285,0.0009987064,0.00004565496,0.000010130131,0.0005258611,0.0023741536,0.17040576,0.00680207,0.0036054954,0.00015388938],"about_ca_topic_score_codex":0.002154355,"about_ca_topic_score_gemma":0.00018612019,"teacher_disagreement_score":0.8087759,"about_ca_system_score_codex":0.0000043784135,"about_ca_system_score_gemma":0.00010552702,"threshold_uncertainty_score":0.32567546},"labels":[],"label_agreement":null},{"id":"W2361820528","doi":"10.1002/2016jb012841","title":"A new back‐and‐forth iterative method for time‐reversed convection modeling: Implications for the Cenozoic evolution of 3‐D structure and dynamics of the mantle","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Université de Montréal","keywords":"Mantle convection; Mantle (geology); Geology; Buoyancy; Subduction; Hotspot (geology); Seismic tomography; Plate tectonics; Geophysics; Convection; Mantle plume; Tectonics; Seismology; Lithosphere; Mechanics; Physics","score_opus":0.028999999076375377,"score_gpt":0.32245101847555685,"score_spread":0.2934510193991815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2361820528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7986954,0.0001975017,0.19557396,0.0033104792,0.00016742026,0.00087097136,0.0011343892,0.0000026461546,0.000047267178],"genre_scores_gemma":[0.9952244,0.00006236072,0.0040874016,0.000010337854,0.00022724118,0.0000016140449,0.000005936398,0.0000038114429,0.0003768969],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99902093,0.00015075515,0.00026923098,0.00011564745,0.0002486329,0.00019477394],"domain_scores_gemma":[0.99792176,0.0011325083,0.00021535497,0.00014150815,0.00050109957,0.000087751636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066932675,0.000077184915,0.00023904092,0.000054843702,0.00018625802,0.000033759534,0.00018250148,0.00004735249,0.00006244938],"category_scores_gemma":[0.00022089445,0.0000347594,0.00009713934,0.00014005433,0.00012889718,0.00016678088,0.000027295047,0.00011121029,0.0000015675189],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0049868156,0.00022093223,0.011599574,0.0007543478,0.0012377279,8.936678e-7,0.0024654868,0.021264726,0.6335821,0.07831503,0.00546567,0.24010669],"study_design_scores_gemma":[0.0021969515,0.0017493804,0.19744721,0.00019735901,0.00016593568,0.00001845285,0.00018740959,0.53517765,0.010875963,0.25007513,0.0017256362,0.0001829041],"about_ca_topic_score_codex":0.0005431124,"about_ca_topic_score_gemma":0.00023700853,"teacher_disagreement_score":0.6227061,"about_ca_system_score_codex":0.000006824371,"about_ca_system_score_gemma":0.0001937101,"threshold_uncertainty_score":0.14325649},"labels":[],"label_agreement":null},{"id":"W2392172767","doi":"10.1002/2015jb012641","title":"Constraints on the heterogeneity spectrum of Earth's upper mantle","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Coda; Mantle (geology); Scattering; Geology; Seismic tomography; Geophysics; Computational physics; Tomography; Wavelength; Physics; Seismology; Optics","score_opus":0.043706299969368,"score_gpt":0.31023317636011216,"score_spread":0.2665268763907442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2392172767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934905,0.000039564864,0.000037184353,0.0022187692,0.000305323,0.00015126751,0.00013242471,0.000005099292,0.0036198532],"genre_scores_gemma":[0.9986032,0.00011967577,0.000066935536,0.00007075163,0.0006984057,5.568558e-7,0.0000016437775,0.0000056807726,0.0004331192],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9970362,0.00051515404,0.00043316412,0.00018737659,0.0012613987,0.0005666748],"domain_scores_gemma":[0.9975559,0.0013417596,0.00023042633,0.00032783725,0.00028842498,0.00025562514],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0017609008,0.0001432286,0.00039906023,0.00012732884,0.00017476759,0.00007560756,0.00054078834,0.00006194024,0.0039170785],"category_scores_gemma":[0.00038145416,0.000065211374,0.00021614769,0.00022409116,0.0007041244,0.00020055355,0.000047746107,0.00035535416,0.00086930004],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004440188,0.0016216309,0.051682197,0.00025414137,0.0013658712,0.0009889205,0.0010022584,0.0006499287,0.6562457,0.053161353,0.012728526,0.2158593],"study_design_scores_gemma":[0.00093859655,0.0027532824,0.6779854,0.00030284314,0.000024317407,0.000049616367,0.00007836277,0.00014351141,0.28719386,0.018937191,0.011353996,0.00023901531],"about_ca_topic_score_codex":0.00023109002,"about_ca_topic_score_gemma":0.00010610285,"teacher_disagreement_score":0.6263032,"about_ca_system_score_codex":0.0000027288102,"about_ca_system_score_gemma":0.00018193266,"threshold_uncertainty_score":0.9999086},"labels":[],"label_agreement":null},{"id":"W2404128530","doi":"10.2138/am-2000-0721","title":"<sup>VIII</sup> (Mg,Fe) <sub>0.85</sub> <sup>VI</sup> (Mg,Fe) <sub>4</sub> <sup>IV</sup> (Fe,Ge) <sub>3</sub> O <sub>12</sub> : A new tetragonal phase and its comparison with garnet","year":2000,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Tetragonal crystal system; Dodecahedron; Crystallography; Octahedron; Crystal structure; Bond length; Chemistry; X-ray crystallography; Space group; Phase (matter); Materials science; Diffraction; Physics","score_opus":0.013832673217120492,"score_gpt":0.2287904994397768,"score_spread":0.2149578262226563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2404128530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98494613,0.0023015423,0.0003276511,0.001628455,0.0004954626,0.0024589377,0.0038479508,0.00084959564,0.00314425],"genre_scores_gemma":[0.98558354,0.0030611646,0.00074150466,0.002294653,0.0029309087,0.00014526719,0.004459895,0.00033007332,0.00045297755],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.98346424,0.0014088055,0.0031927733,0.004342535,0.0028069667,0.004784661],"domain_scores_gemma":[0.99098945,0.0011847827,0.0016915676,0.0024471995,0.0005255596,0.0031614187],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","insufficient_payload"],"category_scores_codex":[0.0013897275,0.0033643758,0.004343074,0.0009970694,0.0016378531,0.0015979805,0.0023309216,0.00091441895,0.0010836232],"category_scores_gemma":[0.00031741144,0.0030722704,0.00089365395,0.0028091858,0.004632729,0.0020589917,0.00037141223,0.0020571318,0.002845983],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004366034,0.0021246774,0.009486046,0.00054821157,0.0014952042,0.0017212642,0.0047685164,0.0886765,0.5000116,0.00038379387,0.074727,0.31169116],"study_design_scores_gemma":[0.031819157,0.016204918,0.05503388,0.0016470766,0.004142222,0.0028911575,0.0051513687,0.23497005,0.52101237,0.0016054643,0.10768199,0.017840333],"about_ca_topic_score_codex":0.011316378,"about_ca_topic_score_gemma":0.006158574,"teacher_disagreement_score":0.2938508,"about_ca_system_score_codex":0.00016399682,"about_ca_system_score_gemma":0.001157297,"threshold_uncertainty_score":0.99982953},"labels":[],"label_agreement":null},{"id":"W2412979278","doi":"10.1093/gji/ggw207","title":"Lithospheric deformation in the Canadian Appalachians: evidence from shear wave splitting","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Lithosphere; Seismology; Rift; Shear wave splitting; Crust; Seismic anisotropy; Mantle (geology); Shear zone; Shear (geology); Tectonics; Geophysics; Paleontology","score_opus":0.022424895714182887,"score_gpt":0.225555747177616,"score_spread":0.20313085146343313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2412979278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98982763,0.00007140881,0.0005446736,0.0059453174,0.0011836115,0.00008623566,0.000108998705,0.000008651462,0.0022234477],"genre_scores_gemma":[0.99740094,0.00005089591,0.0005627033,0.0004596665,0.0013978591,0.0000015539417,0.000027186106,0.0000027664817,0.000096456206],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99868137,0.00014195226,0.00028325734,0.00014851805,0.00047091188,0.00027400345],"domain_scores_gemma":[0.99920344,0.00034473607,0.0001201139,0.000116648414,0.00008050819,0.00013457198],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00052391895,0.000105782085,0.00011707828,0.00005303314,0.00019843417,0.000327407,0.0004320011,0.000046804726,0.00184247],"category_scores_gemma":[0.0001313543,0.00005514496,0.00006752666,0.00010663752,0.000047236885,0.00075330166,0.000012854143,0.0001789505,0.0006046328],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031230386,0.00013785475,0.42450058,0.000018899393,0.00024127348,0.00050502986,0.006622283,0.001999377,0.005640124,0.0070050405,0.005236247,0.547781],"study_design_scores_gemma":[0.0002217613,0.000042597792,0.97673357,0.00015364772,0.000008879007,0.000036803358,0.00008835106,0.0021958328,0.00011860429,0.014635303,0.0056403372,0.00012434385],"about_ca_topic_score_codex":0.17166492,"about_ca_topic_score_gemma":0.08378959,"teacher_disagreement_score":0.552233,"about_ca_system_score_codex":0.000033163233,"about_ca_system_score_gemma":0.00012271416,"threshold_uncertainty_score":0.99907},"labels":[],"label_agreement":null},{"id":"W2414420081","doi":"10.3749/canmin.1400093","title":"HEAT TRANSPORT OF MICAS","year":2015,"lang":"en","type":"article","venue":"The Canadian Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology","score_opus":0.03369503745845067,"score_gpt":0.20925061688661517,"score_spread":0.1755555794281645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2414420081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94923913,0.00018546084,0.0000027086226,0.001728205,0.00047561433,0.00009446594,0.00044922132,0.000008449181,0.047816727],"genre_scores_gemma":[0.9984693,0.0000038023,0.000061841776,0.0003376414,0.0001318961,4.664452e-7,0.000121463,0.0000019521133,0.0008716691],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994572,0.00003217923,0.000115062685,0.000086333304,0.00010856796,0.00020066132],"domain_scores_gemma":[0.99948764,0.000017306638,0.000013699866,0.00017811121,0.000036370053,0.0002668716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022624446,0.00006616245,0.00011692528,0.00003061564,0.00006867797,0.000016903376,0.00020991506,0.000033332177,0.0006303921],"category_scores_gemma":[0.000012233427,0.00004165836,0.000027850894,0.000084229345,0.00013693336,0.000040531017,0.0000016579851,0.000039702663,0.00013613337],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003005031,0.000064324915,0.49205393,0.00014088771,0.00027867343,0.0005248071,0.0074214246,0.035146777,0.013693221,0.020391617,0.41864848,0.011335357],"study_design_scores_gemma":[0.000601276,0.00021702751,0.48551828,0.000017913277,0.00006655541,0.000031385753,0.00018663493,0.00078535854,0.0016075874,0.0048603774,0.5056953,0.0004123236],"about_ca_topic_score_codex":0.9192919,"about_ca_topic_score_gemma":0.9673,"teacher_disagreement_score":0.0870468,"about_ca_system_score_codex":0.0000046530868,"about_ca_system_score_gemma":0.0002584881,"threshold_uncertainty_score":0.69023514},"labels":[],"label_agreement":null},{"id":"W2415640937","doi":"10.1103/physrevlett.113.116404","title":"Metallization of Warm Dense<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:msub><mml:mrow><mml:mi>SiO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math>Studied by XANES Spectroscopy","year":2014,"lang":"lv","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Agence Nationale de la Recherche","keywords":"Nanosecond; Picosecond; Physics; Spectroscopy; Materials science; Laser; Atomic physics; Optics; Quantum mechanics","score_opus":0.014678724063654105,"score_gpt":0.2407769997019326,"score_spread":0.22609827563827847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2415640937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6756806,0.006345562,0.000836284,0.0025996596,0.003296152,0.00008329593,0.0007013277,0.0001735945,0.31028357],"genre_scores_gemma":[0.9774758,0.009292995,0.001281028,0.0051349294,0.0030556372,0.0005014623,0.002671917,0.0004072683,0.0001789265],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9907029,0.00075728184,0.0019080963,0.0017996432,0.0025689632,0.0022631052],"domain_scores_gemma":[0.99280405,0.0016774033,0.0022733423,0.0020736265,0.00015806082,0.0010135405],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001989546,0.0009418359,0.0006109179,0.00027769772,0.0011270875,0.0010293996,0.0020542874,0.0008776417,0.4434386],"category_scores_gemma":[0.0013016867,0.0015857441,0.0018870657,0.0011245495,0.0015329637,0.0013213329,0.0009955417,0.0011145239,0.0034294655],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009229093,0.00044026153,0.00002761143,0.0055181123,0.0020768915,0.0005556816,0.0013603918,0.0018212348,0.03556627,0.27306482,0.67619383,0.0024519686],"study_design_scores_gemma":[0.0011240079,0.0014325132,0.00022107044,0.0024565496,0.0025638707,0.00023283964,0.00027399533,0.025159748,0.9462258,0.000075420496,0.018660417,0.0015737241],"about_ca_topic_score_codex":0.0021869522,"about_ca_topic_score_gemma":0.00092571566,"teacher_disagreement_score":0.91065955,"about_ca_system_score_codex":0.00000735418,"about_ca_system_score_gemma":0.00066391897,"threshold_uncertainty_score":0.99865913},"labels":[],"label_agreement":null},{"id":"W2418381495","doi":"10.1038/ncomms11834","title":"Lasting mantle scars lead to perennial plate tectonics","year":2016,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Dalhousie University; Government of Ontario; Compute Canada","keywords":"Plate tectonics; Intraplate earthquake; Lithosphere; Geology; Mantle (geology); Subduction; Tectonics; Convergent boundary; Geophysics; Seismology; Mid-ocean ridge; Oceanic crust","score_opus":0.019453622579834715,"score_gpt":0.25856213095937963,"score_spread":0.23910850837954492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2418381495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94501233,0.001894532,0.0003572096,0.013039797,0.0014176312,0.0004147674,0.0009034587,0.00021642895,0.036743853],"genre_scores_gemma":[0.9928784,0.00014082977,0.0060756863,0.00016078478,0.0001182659,0.0000030738274,0.00006159709,0.0000046501063,0.00055674074],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992958,0.00007122193,0.00014114156,0.00015294683,0.00013322991,0.00020569432],"domain_scores_gemma":[0.99869984,0.0002445384,0.00005168986,0.0008490176,0.00007216616,0.00008277165],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018027516,0.000093533265,0.00011787501,0.000051298968,0.0002891781,0.00006178403,0.0008428793,0.000121813355,0.00046087676],"category_scores_gemma":[0.00007644772,0.000062009014,0.00003663146,0.00016016855,0.00005870687,0.00012695302,0.00010365055,0.00019548301,0.0009373107],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023015568,0.0002477564,0.11618225,0.000068749316,0.0003028703,0.000018384695,0.0028221505,0.0008947458,0.17944062,0.048589393,0.06594325,0.5852597],"study_design_scores_gemma":[0.00064046995,0.00013385367,0.24242604,0.00016678995,0.000056506906,0.000020822314,0.000089590874,0.0011608335,0.0052459044,0.0028360004,0.74658096,0.00064221944],"about_ca_topic_score_codex":0.00021363,"about_ca_topic_score_gemma":0.0045203334,"teacher_disagreement_score":0.6806377,"about_ca_system_score_codex":0.0000040780074,"about_ca_system_score_gemma":0.00003402729,"threshold_uncertainty_score":0.99984056},"labels":[],"label_agreement":null},{"id":"W2432779761","doi":"10.1002/2015jb012628","title":"Axial‐type olivine crystallographic preferred orientations: The effect of strain geometry on mantle texture","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Boston College; National Science Foundation","keywords":"Olivine; Geology; Seismic anisotropy; Mantle (geology); Peridotite; Electron backscatter diffraction; Anisotropy; Mineralogy; Deformation mechanism; Mantle wedge; Xenolith; Geometry; Geophysics; Subduction; Crystallography; Seismology; Microstructure; Physics; Tectonics; Chemistry; Optics","score_opus":0.025470888965173875,"score_gpt":0.31569457962657377,"score_spread":0.2902236906613999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2432779761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975687,0.00013696894,0.000026679425,0.0005249669,0.0004923999,0.0002637504,0.00018298905,0.0000070193714,0.0007965224],"genre_scores_gemma":[0.9983715,0.00015486917,0.000030581603,0.000025333686,0.0009313142,0.0000013548731,0.00001046319,0.000007137386,0.00046747932],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99674183,0.0008114852,0.00043139898,0.00019341374,0.0013326054,0.0004892589],"domain_scores_gemma":[0.9964191,0.0023720942,0.00026092742,0.00031680256,0.00041234744,0.00021876495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002155151,0.00016328182,0.00044058802,0.000270517,0.00019983268,0.000083794745,0.000534912,0.0000812683,0.00085318065],"category_scores_gemma":[0.0008917698,0.00007134764,0.00019439356,0.0007332848,0.00036899195,0.00024988962,0.000039343402,0.00042282994,0.00016013437],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01541253,0.0009790862,0.04094236,0.0007008971,0.0016244942,0.00045023614,0.0012962291,0.002813998,0.6778907,0.0047121234,0.016801076,0.23637624],"study_design_scores_gemma":[0.002113791,0.015839858,0.9316572,0.00047602152,0.00008095937,0.000032518066,0.000098088916,0.00016844118,0.026922997,0.011930306,0.010396189,0.00028362658],"about_ca_topic_score_codex":0.00023637322,"about_ca_topic_score_gemma":0.00006813139,"teacher_disagreement_score":0.8907148,"about_ca_system_score_codex":0.000004312108,"about_ca_system_score_gemma":0.0001245976,"threshold_uncertainty_score":0.934173},"labels":[],"label_agreement":null},{"id":"W2433263593","doi":"10.1002/2016jb012838","title":"Subduction beneath Laurentia modified the eastern North American cratonic edge: Evidence from <i>P</i> wave and <i>S</i> wave tomography","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Sight Research UK; Leverhulme Trust","keywords":"Geology; Archean; Proterozoic; Craton; Subduction; Laurentia; Lithosphere; Mantle (geology); Paleontology; Plate tectonics; Tectonics; Seismology; Earth science; Geophysics","score_opus":0.04862935299519951,"score_gpt":0.28404062132189284,"score_spread":0.23541126832669335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2433263593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970884,0.0005086445,0.00016111512,0.0013844506,0.00040486627,0.00019291644,0.00013066243,0.000011945753,0.00011705261],"genre_scores_gemma":[0.99664813,0.0013651031,0.0001741092,0.00007857025,0.0015022632,0.000002045683,0.0000087602775,0.000009328689,0.00021169776],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99661756,0.0006073031,0.00046468285,0.00035672117,0.001288949,0.00066478027],"domain_scores_gemma":[0.9970933,0.0013002643,0.000334914,0.00039110528,0.00049326825,0.0003871431],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010319309,0.0002181474,0.00048382956,0.00014682987,0.00034510714,0.00030204764,0.00041805446,0.000049715218,0.00015230555],"category_scores_gemma":[0.00024064236,0.00010999018,0.00018732571,0.00057109527,0.0007626669,0.00070903974,0.000089415786,0.00048310956,0.00011359208],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004397063,0.00056615326,0.35844612,0.00014790289,0.0012088628,0.0005913089,0.0029033634,0.00046996056,0.11447448,0.0005696241,0.008241558,0.5079836],"study_design_scores_gemma":[0.00066587905,0.0014912082,0.9788192,0.00025302728,0.00008515729,0.000024960222,0.00012587909,0.0017563498,0.008741682,0.0047260453,0.003011213,0.00029941084],"about_ca_topic_score_codex":0.0039403243,"about_ca_topic_score_gemma":0.0022036098,"teacher_disagreement_score":0.6203731,"about_ca_system_score_codex":0.000005938094,"about_ca_system_score_gemma":0.0001661002,"threshold_uncertainty_score":0.59566176},"labels":[],"label_agreement":null},{"id":"W2437570785","doi":"10.1093/gji/ggw225","title":"Present-day dynamic and residual topography in Central Anatolia","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lithosphere; Geodynamics; Volcanism; Isostasy; Mantle (geology); Ocean surface topography; Volcano; Tectonics; Crust; Geophysics; Seismology; Geoid; Geothermal gradient; Gravity anomaly; Gravimetry; Seismic tomography; Paleontology; Geodesy","score_opus":0.005570657542463054,"score_gpt":0.2200816612298232,"score_spread":0.21451100368736015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2437570785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943623,0.000086678345,0.00017751851,0.0027610403,0.0012727142,0.000058288948,0.00014474656,0.000012370881,0.0011243233],"genre_scores_gemma":[0.99839103,0.00017127692,0.00013737153,0.00007921452,0.00080337696,6.757677e-7,0.000022210617,0.0000034774973,0.00039134576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988099,0.00008846731,0.00024338315,0.00019472685,0.0003441867,0.0003193896],"domain_scores_gemma":[0.99948627,0.00013151574,0.0000882087,0.000078775796,0.000051133095,0.00016412728],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018428893,0.000117099546,0.0001543711,0.00012350235,0.0000692908,0.00014087133,0.00025091224,0.000044941764,0.00097330636],"category_scores_gemma":[0.00003071598,0.00007431902,0.00006131396,0.000083546554,0.00009046955,0.00039921186,0.0000290907,0.00012725846,0.00010760081],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004419268,0.00024416478,0.6926434,0.000019348434,0.00031194586,0.00053135114,0.0005407886,0.0003901701,0.015830947,0.009061563,0.0056920694,0.27429235],"study_design_scores_gemma":[0.0005514924,0.000057795885,0.96999454,0.00004078057,0.00000727371,0.000040062474,0.000016275342,0.0005420979,0.00023478214,0.020303944,0.008078395,0.00013253515],"about_ca_topic_score_codex":0.00032298072,"about_ca_topic_score_gemma":0.00022389814,"teacher_disagreement_score":0.27735117,"about_ca_system_score_codex":0.000007593476,"about_ca_system_score_gemma":0.000029604138,"threshold_uncertainty_score":0.9999399},"labels":[],"label_agreement":null},{"id":"W2462397653","doi":"10.1007/s00269-015-0794-1","title":"Equation of state of synthetic qandilite Mg2TiO4 at ambient temperature","year":2016,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Chemistry; Bulk modulus; Adiabatic process; Equation of state; Ringwoodite; Diffraction; Thermodynamics; Isothermal process; Crystallography; Mineralogy; Physics; Olivine","score_opus":0.008915833136597396,"score_gpt":0.18887991199779128,"score_spread":0.1799640788611939,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2462397653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846905,0.00016912934,0.000014127185,0.000055413202,0.00004114493,0.00005023692,0.00060788495,0.0000034079817,0.00058958784],"genre_scores_gemma":[0.9988002,0.00010989817,0.000043976816,0.0000042773095,0.00005068241,6.6141183e-7,0.000048045746,0.000002336587,0.0009398958],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993734,0.000014258986,0.00022464115,0.0001342174,0.00015037874,0.00010314844],"domain_scores_gemma":[0.99948126,0.000063051666,0.00019827308,0.00014603027,0.00006970626,0.00004169467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096827534,0.00008763386,0.00022714619,0.0000067611163,0.00002117172,0.0000052460928,0.00007210535,0.000028939812,0.0002600595],"category_scores_gemma":[0.000012018116,0.000056910892,0.000044418855,0.000044245902,0.00010119813,0.00005478553,0.000015194353,0.000017074679,0.0000028426182],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034621753,0.000021184294,0.0023635107,0.00020946686,0.000020418009,2.557385e-7,0.00008200301,0.00009860411,0.994206,0.000033158147,0.000099637095,0.0028311156],"study_design_scores_gemma":[0.00022139182,0.00003539996,0.0061469176,0.00009204717,0.000017825692,5.579862e-7,0.0000051701604,0.00006751847,0.9902528,0.0028168159,0.0002680521,0.00007551514],"about_ca_topic_score_codex":0.00013173783,"about_ca_topic_score_gemma":0.0000071270665,"teacher_disagreement_score":0.0039532366,"about_ca_system_score_codex":0.0000012582703,"about_ca_system_score_gemma":0.000013625112,"threshold_uncertainty_score":0.2847469},"labels":[],"label_agreement":null},{"id":"W2463654099","doi":"10.1002/2016gc006419","title":"Seismological structure of the 1.8 Ga Trans‐Hudson Orogen of North America","year":2016,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Industry Canada; Natural Environment Research Council; Leverhulme Trust","keywords":"Geology; Crust; Precambrian; Orogeny; Archean; Tectonics; Seismology; Proterozoic; Mantle (geology); Lithosphere; Geophysics; Paleontology","score_opus":0.005810141037338566,"score_gpt":0.17298658235572584,"score_spread":0.16717644131838727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2463654099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99496776,0.00010501402,0.00009656313,0.00011228248,0.0004089326,0.00020397408,0.0035606744,0.000023581188,0.00052121683],"genre_scores_gemma":[0.9992543,0.000018053463,0.000049072667,0.00003240514,0.00027954718,0.0000016223954,0.000116291885,0.0000064077403,0.00024234285],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9983466,0.000092039976,0.00045534992,0.00032787662,0.0004214719,0.00035660766],"domain_scores_gemma":[0.99862003,0.00012874644,0.00042279286,0.00060116383,0.00013161481,0.00009566315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007728339,0.00023633565,0.0004859336,0.000014834554,0.00008545718,0.00001540815,0.00060238625,0.00011345383,0.00075829384],"category_scores_gemma":[0.000027994553,0.00012382952,0.00019275864,0.00024680127,0.00023782786,0.00008255714,0.00003965558,0.00009341087,0.000027518323],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010922213,0.00008094929,0.12792405,0.0006783586,0.0001964726,0.000007203216,0.0003265482,0.000974736,0.8443972,0.00009280206,0.00058906025,0.02462339],"study_design_scores_gemma":[0.0008573274,0.00019228764,0.3746898,0.00024571217,0.00014577703,0.00002045699,0.000094962335,0.00018032464,0.6038223,0.0034819623,0.015662594,0.0006065437],"about_ca_topic_score_codex":0.0021071853,"about_ca_topic_score_gemma":0.00012661124,"teacher_disagreement_score":0.24676572,"about_ca_system_score_codex":0.0000037574525,"about_ca_system_score_gemma":0.00008051726,"threshold_uncertainty_score":0.8302786},"labels":[],"label_agreement":null},{"id":"W2488963759","doi":"10.48550/arxiv.1607.07511","title":"Theory of complex fluids in the warm-dense-matter regime, and application to an unusual phase-transitions in liquid carbon","year":2016,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Warm dense matter; Covalent bond; Carbon fibers; Atom (system on chip); Ionization; Phase (matter); Ionic bonding; Molecular dynamics; Atomic physics; Carbon atom; Density functional theory; Ion; Physics; Molecular physics; Chemistry; Materials science; Computational chemistry","score_opus":0.04024458639209213,"score_gpt":0.202743093003661,"score_spread":0.16249850661156887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2488963759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933475,0.000020357245,0.0030419827,0.0001950331,0.000075834425,0.00040992486,0.00030528384,0.000012721271,0.002591365],"genre_scores_gemma":[0.9995677,0.00002457615,0.000030265044,0.0001231712,0.000055204342,0.0000010572114,0.00013742763,0.0000042917072,0.00005631542],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9988542,0.00031509346,0.00017365089,0.00041246714,0.000062627245,0.00018194393],"domain_scores_gemma":[0.99932384,0.00009038204,0.000082182014,0.00040242943,0.000033796085,0.00006737816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041395845,0.0001500844,0.00024135626,0.00017056598,0.000046740995,0.0000222423,0.0003685566,0.00011362564,0.00011971712],"category_scores_gemma":[0.0000045077313,0.00011835912,0.000035585967,0.00020027024,0.00011650616,0.000091316884,0.000050903396,0.00012575022,0.000022820315],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.011584093,0.0023439424,0.18481211,0.0015464377,0.00048278086,0.0007081825,0.036990177,0.23879175,0.20076111,0.31106293,0.0011799694,0.009736502],"study_design_scores_gemma":[0.0059744027,0.0020264008,0.6040007,0.0007124187,0.00046042918,0.000017454822,0.0035047294,0.065563224,0.0051982724,0.30711406,0.0030702055,0.0023577271],"about_ca_topic_score_codex":0.0020535227,"about_ca_topic_score_gemma":0.0016823749,"teacher_disagreement_score":0.41918856,"about_ca_system_score_codex":0.0000064935107,"about_ca_system_score_gemma":0.000036703386,"threshold_uncertainty_score":0.48265448},"labels":[],"label_agreement":null},{"id":"W2492508807","doi":"10.1016/j.tecto.2016.07.017","title":"S-wave velocities and anisotropy of typical rocks from Yunkai metamorphic complex and constraints on the composition of the crust beneath Southern China","year":2016,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Underplating; Crust; Felsic; Mafic; Geochemistry; Adakite; Petrology; Oceanic crust; Diorite; Continental crust; Andesite; Seismology; Subduction; Tectonics; Zircon; Volcanic rock","score_opus":0.020268692694836346,"score_gpt":0.18501734294385982,"score_spread":0.16474865024902346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2492508807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99719656,0.00004089134,0.00019173807,0.0002841687,0.00007822882,0.00013450054,0.0015776646,0.000009036679,0.00048723916],"genre_scores_gemma":[0.99968725,0.00001809506,0.00012668835,0.00005924996,0.00007240997,7.962797e-7,0.000019291745,0.0000035090184,0.000012726503],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993546,0.00008962963,0.0001542613,0.00013890298,0.00014989336,0.00011270791],"domain_scores_gemma":[0.999405,0.00022027291,0.00013182408,0.00018345316,0.000028525561,0.000030927193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007785875,0.00011109687,0.00021510714,0.000011688344,0.000117254145,0.000021612375,0.0001152181,0.000037318063,0.00060781423],"category_scores_gemma":[0.000009424858,0.000050580045,0.000039731152,0.000045763692,0.00056531193,0.000044748438,0.000029734047,0.000053289183,0.000010285141],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006246642,0.00013640014,0.021655565,0.00009467502,0.0004315397,0.000004211914,0.0042970516,0.00022097876,0.84921175,0.03209494,0.00024292298,0.09098528],"study_design_scores_gemma":[0.00064128474,0.00021840198,0.89954424,0.000107676075,0.000097719974,0.0000025267864,0.00025252314,0.00057126884,0.06186236,0.036441974,0.00007714703,0.00018288943],"about_ca_topic_score_codex":0.00096145185,"about_ca_topic_score_gemma":0.00004675206,"teacher_disagreement_score":0.8778887,"about_ca_system_score_codex":0.0000013607824,"about_ca_system_score_gemma":0.000017331813,"threshold_uncertainty_score":0.665514},"labels":[],"label_agreement":null},{"id":"W2495774001","doi":"10.1017/s1743921310009774","title":"New advances in asteroseismology of pulsating hot subdwarf stars","year":2009,"lang":"en","type":"article","venue":"Proceedings of the International Astronomical Union","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Asteroseismology; Subdwarf; Stars; Physics; Astrophysics; Mode (computer interface); Astronomy; Computer science","score_opus":0.005799218719430488,"score_gpt":0.20381771290219974,"score_spread":0.19801849418276926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2495774001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971201,0.00003776944,0.000036406218,0.0006643948,0.00038222477,0.00006776836,0.000021398986,0.000003919066,0.0016660134],"genre_scores_gemma":[0.99804366,0.0000072252437,0.0016985742,0.000029872936,0.00009860957,2.2234093e-7,0.000008178612,0.0000012211171,0.00011243317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993902,0.000006080342,0.0002479143,0.00011348655,0.00013422468,0.00010810848],"domain_scores_gemma":[0.99966544,0.000028807857,0.00019991813,0.000031803935,0.00004611871,0.000027894765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016972532,0.00006372789,0.00013152322,0.0000471348,0.000014222623,0.0000170012,0.00036111375,0.00002745031,0.0001578835],"category_scores_gemma":[0.000033226923,0.000046785066,0.000037850114,0.000056439796,0.000030225225,0.0002602742,0.00002381583,0.00005863406,0.0000035530256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003531756,0.000062305386,0.7619726,0.000022732556,0.000024178833,1.5081005e-7,0.00020357809,0.0069574625,0.12499872,0.0119617805,0.00034488502,0.09309844],"study_design_scores_gemma":[0.00028181667,0.00011825796,0.9548985,0.00005135526,0.000004273857,8.765171e-7,0.000038218175,0.0008887318,0.03401325,0.007844215,0.0017977944,0.00006270864],"about_ca_topic_score_codex":0.00044242828,"about_ca_topic_score_gemma":0.000037447666,"teacher_disagreement_score":0.19292592,"about_ca_system_score_codex":0.0000054899724,"about_ca_system_score_gemma":0.000018593608,"threshold_uncertainty_score":0.19078395},"labels":[],"label_agreement":null},{"id":"W2497909704","doi":"10.1017/cbo9780511781773.003","title":"Internal structure of the Earth","year":2010,"lang":"en","type":"book-chapter","venue":"Cambridge University Press eBooks","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Earth (classical element); Thermal; Thermal energy; Internal energy; Internal heating; Geophysics; Geology; Astrobiology; Physics; Meteorology; Mechanics; Thermodynamics","score_opus":0.008166847909298643,"score_gpt":0.15548968640165012,"score_spread":0.14732283849235148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2497909704","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02546147,0.000037259822,0.000009842807,0.0000066768534,0.0012354308,0.00020386779,0.003103267,0.000021524273,0.96992064],"genre_scores_gemma":[0.15398164,0.000013046828,0.000055005105,0.000025657819,0.00020210397,1.0468717e-8,0.000056981433,0.000007103595,0.8456584],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991746,0.000029719076,0.00013977791,0.00024748954,0.0002410073,0.00016738618],"domain_scores_gemma":[0.99910647,0.000036034646,0.00025130608,0.0004464511,0.00007621198,0.000083558894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000041297615,0.00021424516,0.00028703207,0.000046716188,0.00013294135,0.00003188334,0.00070026825,0.00027589253,0.00020863958],"category_scores_gemma":[0.0000041643207,0.00016274035,0.00016094076,0.0000051315947,0.00027900308,0.000049633247,0.00012236592,0.00041699945,0.000013522093],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027160405,0.000010317545,0.0003500814,0.00028353467,0.00043579328,0.00012701406,0.00016117364,0.00005408887,0.01953182,0.96347,0.0112268785,0.0040776967],"study_design_scores_gemma":[0.00023086804,0.00003142133,0.0022253292,0.000078520956,0.00012261256,0.000008641934,0.0000041370113,0.000013465539,0.012125187,0.000076916156,0.98485833,0.00022455402],"about_ca_topic_score_codex":0.00191524,"about_ca_topic_score_gemma":0.00024076174,"teacher_disagreement_score":0.97363144,"about_ca_system_score_codex":0.0000024204965,"about_ca_system_score_gemma":0.00007110323,"threshold_uncertainty_score":0.6636359},"labels":[],"label_agreement":null},{"id":"W2511215906","doi":"10.1093/gji/ggw309","title":"Azimuthal seismic anisotropy in the Earth's upper mantle and the thickness of tectonic plates","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Science Foundation Ireland","keywords":"Geology; Lithosphere; Seismic anisotropy; Anisotropy; Azimuth; Geophysics; Mantle (geology); Crust; Seismogram; Seismology; Amplitude; Geodesy; Tectonics; Geometry; Physics","score_opus":0.006644302468225399,"score_gpt":0.21004879184059919,"score_spread":0.2034044893723738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2511215906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932798,0.00008410919,0.00020247724,0.004687223,0.00057630654,0.00008049996,0.00010231007,0.0000040628274,0.0009831951],"genre_scores_gemma":[0.9988752,0.0001245096,0.00007103675,0.00022600048,0.00049029035,0.0000011728791,0.000005637411,0.0000023846505,0.00020379039],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99898005,0.00015995877,0.00022894812,0.000113500304,0.00035036993,0.00016719142],"domain_scores_gemma":[0.999185,0.0004990592,0.00012245856,0.000098630735,0.000058615136,0.00003621042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004850401,0.00009241511,0.00015713728,0.000041905438,0.000097551085,0.00010253548,0.00040724495,0.000033027605,0.0006616265],"category_scores_gemma":[0.000044428736,0.00003605208,0.00007333991,0.000064353255,0.00023343103,0.00020463395,0.000027418027,0.00014667484,0.00006358064],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0064672465,0.00080951577,0.26231325,0.00011654012,0.0013717405,0.0004848377,0.010061995,0.0041150353,0.07831815,0.36193255,0.006312267,0.26769686],"study_design_scores_gemma":[0.0027699687,0.00014804215,0.870054,0.00009598083,0.000030664833,0.00032278316,0.00018209261,0.0027988052,0.0018127316,0.10966326,0.011935657,0.00018601814],"about_ca_topic_score_codex":0.00047302112,"about_ca_topic_score_gemma":0.000065972315,"teacher_disagreement_score":0.60774076,"about_ca_system_score_codex":0.0000021094424,"about_ca_system_score_gemma":0.000028459595,"threshold_uncertainty_score":0.7244347},"labels":[],"label_agreement":null},{"id":"W2512519495","doi":"10.1063/1.4959792","title":"High resolution x-ray Thomson scattering measurements from cryogenic hydrogen jets using the linac coherent light source","year":2016,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Physics; Thomson scattering; Scattering; Spectrometer; Cryogenics; Highly oriented pyrolytic graphite; Optics; Linear particle accelerator; Laser; Atomic physics; Beam (structure)","score_opus":0.03641722874851679,"score_gpt":0.23955768515410328,"score_spread":0.20314045640558648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2512519495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99164885,0.0047768094,0.00006481055,0.00032752054,0.002188673,0.0005544679,0.00023204315,0.000021870801,0.00018493657],"genre_scores_gemma":[0.9974808,0.0014453515,0.00048341532,0.00010243877,0.00016499213,0.000004616859,0.000071878036,0.000007812099,0.00023871344],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9972089,0.00026712776,0.00059327896,0.00047560452,0.0010600876,0.00039500694],"domain_scores_gemma":[0.99863356,0.000038511003,0.00044420408,0.0006157568,0.00015877085,0.00010921574],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017784133,0.00020910196,0.00038259945,0.00006193231,0.00042118682,0.0001237799,0.0005924905,0.000053302585,0.0016059303],"category_scores_gemma":[0.00006540454,0.00011238059,0.00013521822,0.00028512246,0.00018658533,0.0003070822,0.00008117381,0.000057209232,0.00034600106],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039299448,0.00007634449,0.01772414,0.0010202626,0.00021075518,0.0000019861673,0.00015889197,0.000114468814,0.7095757,0.000022956528,0.0014889509,0.26956624],"study_design_scores_gemma":[0.002412192,0.0002595368,0.07390963,0.038646404,0.0010293759,0.000014647962,0.0000725053,0.0020655948,0.5625748,0.0014662753,0.31596535,0.0015836833],"about_ca_topic_score_codex":0.0009525165,"about_ca_topic_score_gemma":0.00009523106,"teacher_disagreement_score":0.3144764,"about_ca_system_score_codex":0.000028392613,"about_ca_system_score_gemma":0.00008284561,"threshold_uncertainty_score":0.99930674},"labels":[],"label_agreement":null},{"id":"W2512852012","doi":"10.1103/physrevb.94.104107","title":"Role of quantum ion dynamics in the melting of lithium","year":2016,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Lawrence Livermore National Laboratory; Engineering and Physical Sciences Research Council; U.S. Department of Energy; National Science Foundation","keywords":"Ion; Quantum; Lithium (medication); Materials science; Melting curve analysis; Dynamics (music); Thermodynamics; Condensed matter physics; Physics; Chemistry; Quantum mechanics","score_opus":0.011721343705771737,"score_gpt":0.2987083023477244,"score_spread":0.28698695864195267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2512852012","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9532,0.036629643,0.00032283118,0.0025242444,0.00019946974,0.0013416006,0.00034560438,0.000029319292,0.005407314],"genre_scores_gemma":[0.95504147,0.04400659,0.000035140594,0.00050271285,0.00032358282,0.000017992958,0.00004860801,0.000010221158,0.000013691247],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99708825,0.0005837373,0.000807554,0.0004049768,0.00069064094,0.00042483895],"domain_scores_gemma":[0.99749494,0.0010251942,0.00056339183,0.0006747444,0.00012976093,0.000111970316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010500534,0.00030600646,0.001353027,0.00003521966,0.00005139867,0.000015082694,0.0007437035,0.000035727022,0.00012598048],"category_scores_gemma":[0.00056147896,0.00015163122,0.00045058687,0.0005781008,0.0001861569,0.0002340469,0.00005991067,0.00018792786,0.00024035362],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006501007,0.0009126646,0.0080268895,0.012571275,0.00010014554,0.000008124102,0.0003256287,0.000023480989,0.07048977,0.68271136,0.0015733945,0.22319226],"study_design_scores_gemma":[0.0012909085,0.0016250035,0.08919028,0.063858844,0.0013467774,0.000013416138,0.00015080869,0.044996038,0.030361349,0.7002177,0.065005586,0.0019432945],"about_ca_topic_score_codex":0.00045143144,"about_ca_topic_score_gemma":0.000068646696,"teacher_disagreement_score":0.22124895,"about_ca_system_score_codex":0.000010436356,"about_ca_system_score_gemma":0.00005210586,"threshold_uncertainty_score":0.6183342},"labels":[],"label_agreement":null},{"id":"W2515356698","doi":"10.1038/s41467-018-08238-y","title":"Earthquake lubrication and healing explained by amorphous nanosilica","year":2019,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Lubrication; Forensic engineering; Materials science; Composite material; Engineering","score_opus":0.00845212813981539,"score_gpt":0.22664126381779917,"score_spread":0.2181891356779838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515356698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9807223,0.0084676575,0.00001699896,0.003301564,0.00031819203,0.00032267813,0.00025377303,0.00007861462,0.00651819],"genre_scores_gemma":[0.9964064,0.0007952092,0.0013328462,0.00042274685,0.000034391986,0.0000039448973,0.0007037883,0.0000041725953,0.0002965228],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993171,0.00009918359,0.00014828662,0.00016900711,0.000118741475,0.00014766713],"domain_scores_gemma":[0.9987919,0.00019823849,0.00007641345,0.00081768073,0.00004695365,0.000068826426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001785334,0.0000901781,0.00012981177,0.00003501974,0.00022946867,0.00007462406,0.00043821914,0.00012998273,0.0002720954],"category_scores_gemma":[0.000027937349,0.000079887446,0.000023408707,0.000141113,0.000054024877,0.00014379321,0.000048611306,0.00024469933,0.0002365412],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018345955,0.00039490566,0.5725212,0.0002032964,0.0002608733,0.0000033561487,0.0030183322,0.00062135607,0.14883675,0.038753558,0.13999815,0.09520476],"study_design_scores_gemma":[0.00040391795,0.0000825253,0.4064152,0.000027264157,0.000027339483,0.00000737448,0.00010657118,0.0028164817,0.0015614788,0.0007199353,0.58752054,0.00031137993],"about_ca_topic_score_codex":0.00059016165,"about_ca_topic_score_gemma":0.0008233042,"teacher_disagreement_score":0.4475224,"about_ca_system_score_codex":0.000002075715,"about_ca_system_score_gemma":0.000019496953,"threshold_uncertainty_score":0.32577157},"labels":[],"label_agreement":null},{"id":"W2520291634","doi":"","title":"Variations in Grain Size and Viscosity Based on Vacancy Diffusion in Minerals, Seismic Tomography and Geodynamically Inferred Mantle Rheology","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Mantle (geology); Grain size; Geology; Rheology; Viscosity; Arrhenius equation; Seismic tomography; Diffusion creep; Mineralogy; Geophysics; Thermodynamics; Materials science; Grain boundary; Microstructure; Physics; Chemistry; Activation energy; Composite material","score_opus":0.008875623031422187,"score_gpt":0.21445042146183316,"score_spread":0.20557479843041096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2520291634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99722904,0.0001497378,0.00007864377,0.00049920694,0.00019761159,0.00017948008,0.00004950891,0.00001809177,0.0015987012],"genre_scores_gemma":[0.9986442,0.0000233087,0.00092348707,0.00022080271,0.000044599412,0.0000032105718,0.00006225832,0.000003899761,0.00007424398],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989233,0.00019777138,0.00022779046,0.0002643574,0.00013421132,0.00025258574],"domain_scores_gemma":[0.9994364,0.00023294106,0.00007465759,0.00011480054,0.000025134088,0.000116071686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006234983,0.00012879618,0.00022217035,0.00013433388,0.000055437173,0.000049594822,0.00008576268,0.000087875225,0.000016316266],"category_scores_gemma":[0.00017524255,0.000112196125,0.000016944781,0.00017035495,0.000043274405,0.000102630715,0.000029681352,0.000100969155,0.000007931866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008302633,0.000053765005,0.9917655,0.000025908168,0.000005015556,0.000021361184,0.00032675973,0.004584342,0.0018353491,0.00018050693,0.00017195876,0.0009465085],"study_design_scores_gemma":[0.0008600766,0.00010744535,0.82639897,0.00005803444,0.000006883635,0.0000019087756,0.00002750988,0.1706159,0.000012076071,0.001381535,0.00038528428,0.0001443744],"about_ca_topic_score_codex":0.033426534,"about_ca_topic_score_gemma":0.035084736,"teacher_disagreement_score":0.16603155,"about_ca_system_score_codex":0.0000040385207,"about_ca_system_score_gemma":0.00003578891,"threshold_uncertainty_score":0.9825224},"labels":[],"label_agreement":null},{"id":"W2520727429","doi":"10.1016/j.lithos.2016.09.011","title":"Carbonado revisited: Insights from neutron diffraction, high resolution orientation mapping and numerical simulations","year":2016,"lang":"en","type":"article","venue":"Lithos","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada)","funders":"Australian Research Council","keywords":"Grain boundary; Crystallography; Materials science; Nucleation; Annealing (glass); Anisotropy; Condensed matter physics; Neutron diffraction; Deformation (meteorology); Geology; Mineralogy; Crystal structure; Optics; Microstructure; Composite material; Chemistry; Physics; Thermodynamics","score_opus":0.009900519375721744,"score_gpt":0.20763505084238154,"score_spread":0.19773453146665979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2520727429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99620223,0.00016098871,0.0023497066,0.00029196191,0.00039910115,0.00011892282,0.0002130657,0.00004036632,0.00022367583],"genre_scores_gemma":[0.9985381,0.000030763043,0.000656955,0.000056458808,0.00037346993,0.0000012458285,0.00022987627,0.0000030331057,0.000110126166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999272,0.00008287641,0.00016285507,0.00022604202,0.00012987763,0.00012635445],"domain_scores_gemma":[0.9995209,0.0001640548,0.000077201104,0.00013307607,0.00003341734,0.00007136672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000041453644,0.00008512783,0.00012006481,0.00004104773,0.00014259056,0.000054112308,0.000047932997,0.000051371262,0.0004479989],"category_scores_gemma":[0.000029071121,0.000057086352,0.000016345208,0.00010002912,0.000025440188,0.00031020402,0.000008773148,0.00003539871,0.00008136416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022983075,0.00007157362,0.8396473,0.00005461895,0.00011269677,0.00001868631,0.0021519698,0.0014192242,0.10013853,0.0072027543,0.0010456512,0.04790718],"study_design_scores_gemma":[0.00023258093,0.000028179105,0.97814095,0.000028480657,0.000015429692,5.837581e-7,0.000019733989,0.0018417904,0.0002436058,0.0042429212,0.015105499,0.0001002717],"about_ca_topic_score_codex":0.009992206,"about_ca_topic_score_gemma":0.00019345758,"teacher_disagreement_score":0.13849364,"about_ca_system_score_codex":0.000004586782,"about_ca_system_score_gemma":0.000011120343,"threshold_uncertainty_score":0.99660033},"labels":[],"label_agreement":null},{"id":"W2521540026","doi":"10.1002/2016jb013460","title":"Identifying mantle lithosphere inheritance in controlling intraplate orogenesis","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Toronto; Canada Foundation for Innovation","keywords":"Lithosphere; Intraplate earthquake; Geology; Mantle (geology); Collision zone; Plate tectonics; Geophysics; Hotspot (geology); Tectonics; Seismology","score_opus":0.045762826280324194,"score_gpt":0.32314579051396985,"score_spread":0.27738296423364567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521540026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976289,0.0005675064,0.0002592799,0.00046214522,0.00036838412,0.00013574006,0.000031516167,0.000008687776,0.0005377988],"genre_scores_gemma":[0.9975941,0.00067923585,0.0004968374,0.000028196642,0.00074527453,0.0000011885312,0.0000014385682,0.000008260273,0.0004454702],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99711376,0.0003932328,0.00057326304,0.00023512795,0.00097558333,0.00070901366],"domain_scores_gemma":[0.998188,0.0007648516,0.00020902592,0.00020618636,0.00034938907,0.00028254284],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018956158,0.00015011092,0.00050615636,0.0001609598,0.00013926324,0.00016704758,0.00044560418,0.00008073983,0.00091945287],"category_scores_gemma":[0.00033906192,0.000091625414,0.00013855108,0.00042588927,0.00016210806,0.00061228406,0.000038790644,0.0003562336,0.00045387362],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033585299,0.0005410368,0.120583385,0.00030059094,0.0004207305,0.002358184,0.0013951192,0.0016523524,0.552971,0.0028590714,0.0014491504,0.3121108],"study_design_scores_gemma":[0.0034141506,0.0012871359,0.9055058,0.0010992365,0.00003212821,0.00005681239,0.00028644255,0.0016559693,0.04163167,0.036926858,0.0075873723,0.00051644363],"about_ca_topic_score_codex":0.00072834454,"about_ca_topic_score_gemma":0.0005582449,"teacher_disagreement_score":0.7849224,"about_ca_system_score_codex":0.000010200993,"about_ca_system_score_gemma":0.00016766104,"threshold_uncertainty_score":0.99999386},"labels":[],"label_agreement":null},{"id":"W2521983190","doi":"10.1073/pnas.1601254113","title":"Crystal structures and dynamical properties of dense CO <sub>2</sub>","year":2016,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Defense Sciences Office, DARPA; National Science Foundation; Advanced Research Projects Agency; Division of Materials Research; China Scholarship Council; U.S. Department of Energy","keywords":"Metastability; Metadynamics; Molecular dynamics; Ambient pressure; Materials science; Thermodynamics; Crystal structure; Crystallography; Structural stability; Phase (matter); Chemical physics; Diffraction; Chemistry; Computational chemistry; Physics","score_opus":0.020990171028177396,"score_gpt":0.22999761782869044,"score_spread":0.20900744680051303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521983190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985466,0.00013969779,3.33831e-7,0.0005982804,0.000022503764,0.00008738654,0.00008473903,0.000004503549,0.0005159295],"genre_scores_gemma":[0.99970984,0.00004437043,0.00014670189,0.00003564253,0.00004729827,5.892047e-7,1.1016066e-7,0.0000010308712,0.000014391902],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99886686,0.0000075168828,0.0002244918,0.00015149538,0.00063438073,0.00011527728],"domain_scores_gemma":[0.9995246,0.00006880884,0.0002489561,0.0000060164016,0.00012018012,0.000031457083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005355663,0.00006947548,0.00014388678,0.000064965825,0.00010334527,0.000019604251,0.00033624482,0.000049067254,0.000023824823],"category_scores_gemma":[0.00018394779,0.000031943066,0.000032729153,0.0001477097,0.0011120359,0.00032259402,0.000035682122,0.000038657032,0.0000010046709],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002286075,0.00000498989,0.013677173,0.000052418207,0.000007751914,3.0484177e-9,0.00007872104,0.000016862987,0.98020667,0.004937355,0.00007171428,0.0009234995],"study_design_scores_gemma":[0.00008350646,0.00003552077,0.24265583,0.00006841086,0.000005882234,0.0000035163923,0.000033717766,0.00012774169,0.732394,0.02452348,0.000023246816,0.000045175842],"about_ca_topic_score_codex":0.000024674964,"about_ca_topic_score_gemma":9.254639e-7,"teacher_disagreement_score":0.24781269,"about_ca_system_score_codex":0.000001701409,"about_ca_system_score_gemma":0.000022460794,"threshold_uncertainty_score":0.40973428},"labels":[],"label_agreement":null},{"id":"W2527712848","doi":"10.5772/64617","title":"Novel Pressure-Induced Molecular Transformations Probed by In Situ Vibrational Spectroscopy","year":2016,"lang":"en","type":"book-chapter","venue":"InTech eBooks","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Brookhaven National Laboratory; Ontario Ministry of Research and Innovation","keywords":"Raman spectroscopy; Characterization (materials science); Infrared spectroscopy; Fourier transform infrared spectroscopy; Spectroscopy; Chemical physics; Synchrotron; Intermolecular force; Molecule; Materials science; Molecular spectroscopy; In situ; Infrared; Chemistry; Nanotechnology; Optics; Organic chemistry; Physics","score_opus":0.011337310414893567,"score_gpt":0.21118393411932052,"score_spread":0.19984662370442696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2527712848","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0014396377,0.00017934707,0.020034315,0.00022719207,0.0005994439,0.00089638866,0.0018409045,0.00009203345,0.97469074],"genre_scores_gemma":[0.889861,0.000025642988,0.002353413,0.0002891477,0.00033923172,0.000029237714,0.0007796886,0.000042825206,0.10627981],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9985273,0.000019061192,0.00043616982,0.000361406,0.000352704,0.0003033928],"domain_scores_gemma":[0.99937075,0.000049144663,0.00015934807,0.00026542702,0.000057714013,0.000097597775],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014626385,0.0003255636,0.0003692701,0.00013878515,0.00007121332,0.00009603768,0.0003161392,0.00030805374,0.0015386268],"category_scores_gemma":[0.0000070554256,0.00026220566,0.000106164356,0.000014404799,0.000069746464,0.00012685204,0.00001537476,0.00025195547,0.00033672305],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031479023,0.000008384371,0.0000028384454,0.000036481633,0.00006062789,0.000007751832,0.00008875395,0.0000040550594,0.9816181,0.016288148,0.00023545821,0.0016179],"study_design_scores_gemma":[0.00046160497,0.00012767024,0.000037904967,0.00022194706,0.00005534903,0.0000082709785,0.0000027508056,0.000024938747,0.8693041,0.041596007,0.08767235,0.0004870836],"about_ca_topic_score_codex":0.00024968458,"about_ca_topic_score_gemma":0.0008218172,"teacher_disagreement_score":0.88842136,"about_ca_system_score_codex":0.000008301608,"about_ca_system_score_gemma":0.00014658527,"threshold_uncertainty_score":0.999983},"labels":[],"label_agreement":null},{"id":"W2527995534","doi":"10.1002/2016gc006509","title":"Spawning superplumes from the midmantle: The impact of spin transitions in the mantle","year":2016,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Directorate for Computer and Information Science and Engineering; National Science Foundation","keywords":"Geology; Spin transition; Upwelling; Transition zone; Mantle (geology); Silicate perovskite; Mantle plume; Lithosphere; Geophysics; Volcano; Hotspot (geology); Petrology; Geochemistry; Seismology; Tectonics; Oceanography; Condensed matter physics","score_opus":0.010097016907972642,"score_gpt":0.222138521955211,"score_spread":0.21204150504723834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2527995534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994236,0.0004306112,0.000045833003,0.0009786682,0.00022952264,0.00028817204,0.0021469228,0.000016916623,0.0016273645],"genre_scores_gemma":[0.9989316,0.000031819363,0.000009253913,0.000051391995,0.0006683534,0.000011477331,0.00018189508,0.000006238345,0.000107970365],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984137,0.00020582824,0.00036455554,0.00027342312,0.00034915365,0.0003933704],"domain_scores_gemma":[0.99842185,0.0005820529,0.00016695779,0.0007236572,0.000057903435,0.000047584766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005280124,0.00022356656,0.00029265104,0.000013473605,0.0002363587,0.00010362067,0.0008192333,0.00007929018,0.00084281876],"category_scores_gemma":[0.000031801275,0.00008413061,0.00020673135,0.00023974988,0.00017750051,0.00013748414,0.000024059078,0.00014192736,0.00015628184],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003207573,0.00040889674,0.21845917,0.0003521461,0.0009503084,0.00008873927,0.018827474,0.0050831106,0.7126092,0.0019353122,0.023772562,0.01719236],"study_design_scores_gemma":[0.0015105212,0.00020229901,0.9308948,0.0006933988,0.00019208065,0.00004248195,0.0050242087,0.0016982503,0.029936679,0.023346683,0.0055957274,0.00086290593],"about_ca_topic_score_codex":0.03160816,"about_ca_topic_score_gemma":0.0010427578,"teacher_disagreement_score":0.7124356,"about_ca_system_score_codex":0.0000061547325,"about_ca_system_score_gemma":0.000085994834,"threshold_uncertainty_score":0.97484046},"labels":[],"label_agreement":null},{"id":"W2528923963","doi":"10.1103/physrevb.96.184104","title":"Polymerization of sodium-doped liquid nitrogen under pressure","year":2017,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"U.S. Department of Energy","keywords":"Polymerization; Doping; Mixing (physics); Materials science; Nitrogen; Molecular dynamics; Phase transition; Sodium; Liquid nitrogen; Gibbs free energy; Phase (matter); Compression (physics); Thermodynamics; Chemical physics; Physical chemistry; Chemical engineering; Chemistry; Computational chemistry; Polymer; Organic chemistry; Physics; Composite material","score_opus":0.018866794284428376,"score_gpt":0.32600096981036725,"score_spread":0.30713417552593886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528923963","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85117865,0.12272525,0.0009911293,0.004891352,0.00089841825,0.0030922908,0.000899719,0.00016196634,0.015161225],"genre_scores_gemma":[0.9421557,0.054827172,0.000060933082,0.0015618148,0.0009913761,0.000028680846,0.00023523488,0.000023931412,0.000115123024],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9968669,0.00034617574,0.000716923,0.0006789495,0.00080856046,0.0005825118],"domain_scores_gemma":[0.99677414,0.00022484495,0.0009542124,0.0014975006,0.00021003924,0.00033926248],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004379341,0.00049276935,0.0017399791,0.00003192945,0.00035972573,0.000110734145,0.0012012586,0.000057938785,0.00070501305],"category_scores_gemma":[0.0004659484,0.000363814,0.00063308445,0.00023764477,0.00030443913,0.0006049459,0.00015104034,0.00025796925,0.00097289885],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008292781,0.0034229534,0.010679447,0.074181296,0.00215209,0.00006116476,0.00045050294,0.0003322425,0.28077012,0.44242918,0.026790282,0.15790142],"study_design_scores_gemma":[0.0027021572,0.0032962959,0.068513826,0.03847844,0.008894194,0.000023968645,0.000022247694,0.015565385,0.27206442,0.29166704,0.29369232,0.005079683],"about_ca_topic_score_codex":0.0005536807,"about_ca_topic_score_gemma":0.000024961613,"teacher_disagreement_score":0.26690206,"about_ca_system_score_codex":0.0000044646226,"about_ca_system_score_gemma":0.00010776189,"threshold_uncertainty_score":0.9998814},"labels":[],"label_agreement":null},{"id":"W2537108081","doi":"10.1190/1.3255258","title":"Laboratory measurements of static and dynamic bulk moduli in carbonate","year":2009,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Petrophysics; Carbonate; Calcite; Bulk modulus; Porosity; Modulus; Mineralogy; Materials science; Carbonate rock; Moduli; Geology; Composite material; Geotechnical engineering; Metallurgy; Physics","score_opus":0.010379647373603062,"score_gpt":0.21135581103465248,"score_spread":0.20097616366104942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2537108081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960279,0.0001804672,0.00000512407,0.00008240051,0.00007755886,0.0000720733,0.000044854885,0.000008116727,0.0035015203],"genre_scores_gemma":[0.99942553,0.000021825532,0.00038560797,0.000092705704,0.0000062852764,1.7437877e-7,0.000009742008,8.631701e-7,0.000057267454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99949986,0.00003231796,0.00012871939,0.0001011164,0.00012502656,0.00011295979],"domain_scores_gemma":[0.99981993,0.000013737254,0.000033561704,0.00007333025,0.00002204076,0.00003738396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017752853,0.00005740622,0.00012198608,0.000037367365,0.000013698686,0.000013187885,0.00005375295,0.000020369695,0.00019799743],"category_scores_gemma":[0.000007790723,0.000045282322,0.0000071551635,0.00008223019,0.000018622284,0.00007716892,0.0000026552989,0.000022787472,0.000010064058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028737774,0.0002856248,0.64357144,0.00037387462,0.0001154818,0.000060077302,0.002111568,0.032015305,0.25158164,0.0010520954,0.0005983006,0.06794725],"study_design_scores_gemma":[0.00034289787,0.000114665934,0.987393,0.00001743921,0.000007409155,3.3176477e-7,0.00001999032,0.006745631,0.0027876364,0.0023380218,0.00012487562,0.00010808212],"about_ca_topic_score_codex":0.001449204,"about_ca_topic_score_gemma":0.0011491297,"teacher_disagreement_score":0.34382161,"about_ca_system_score_codex":0.0000010466401,"about_ca_system_score_gemma":0.000018660412,"threshold_uncertainty_score":0.21907726},"labels":[],"label_agreement":null},{"id":"W2549464769","doi":"10.1016/j.epsl.2016.10.052","title":"Mid-mantle heterogeneities and iron spin transition in the lower mantle: Implications for mid-mantle slab stagnation","year":2016,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Directorate for Computer and Information Science and Engineering; National Science Foundation","keywords":"Transition zone; Spin transition; Mantle (geology); Geology; Core–mantle boundary; Mantle convection; Mantle wedge; Geophysics; Post-perovskite; Silicate perovskite; Petrology; Condensed matter physics; Subduction; Physics; Tectonics","score_opus":0.010943336722104798,"score_gpt":0.21022145444999024,"score_spread":0.19927811772788545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2549464769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887862,0.00021261028,0.000285697,0.009059123,0.00027981572,0.00034776903,0.00088784023,0.000014565522,0.0001263818],"genre_scores_gemma":[0.99766284,0.00013665769,0.0002898221,0.001542824,0.00011942575,0.0000057110947,0.00021148377,0.0000026146854,0.00002862758],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998886,0.00005766109,0.00017638829,0.00033562823,0.00019424636,0.00035011655],"domain_scores_gemma":[0.99949634,0.00018024008,0.000057068326,0.00016974582,0.00001622477,0.000080400176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052224554,0.00013195386,0.00012868429,0.00010878538,0.00032733072,0.00015917458,0.0002056604,0.00003695387,0.00014011051],"category_scores_gemma":[0.000013643477,0.0000800903,0.00002202058,0.00014723129,0.0003319402,0.0005438415,0.000007745566,0.000046815803,0.00002971656],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038746727,0.000090831156,0.1737523,0.00023019584,0.000034603945,0.000039222843,0.003550337,0.0026435698,0.7190355,0.0006416511,0.004444681,0.09514966],"study_design_scores_gemma":[0.0004954389,0.00021316684,0.98604953,0.000031901218,0.00001586466,0.000026690264,0.00007922926,0.00042723707,0.002917941,0.00041472435,0.009111109,0.0002171933],"about_ca_topic_score_codex":0.0006739051,"about_ca_topic_score_gemma":0.0012103034,"teacher_disagreement_score":0.8122972,"about_ca_system_score_codex":0.0000018490321,"about_ca_system_score_gemma":0.000022927885,"threshold_uncertainty_score":0.32659876},"labels":[],"label_agreement":null},{"id":"W2553863501","doi":"10.2138/am-2001-8-914","title":"Crystal structure of novel high-pressure perovskite K <sub>2/3</sub> Th <sub>1/3</sub> TiO <sub>3</sub> , a possible host for Th in the upper mantle","year":2001,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; Lakehead University","keywords":"Tetragonal crystal system; Crystallography; Perovskite (structure); Crystal structure; Rietveld refinement; Alkali metal; Mantle (geology); Materials science; Mineralogy; Chemistry; Geology; Geochemistry","score_opus":0.009867796456809356,"score_gpt":0.2156349911910544,"score_spread":0.20576719473424504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2553863501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99266285,0.0002853834,0.00027137352,0.0007138819,0.00057805737,0.00092191476,0.003949159,0.00006813048,0.000549247],"genre_scores_gemma":[0.9964908,0.00031162263,0.00055160845,0.00077738287,0.00070894026,0.000027604567,0.0010349347,0.00004238079,0.000054773576],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99635196,0.00023333612,0.0007576277,0.0008800836,0.0006697717,0.0011072336],"domain_scores_gemma":[0.99778175,0.00039647016,0.00059265917,0.00083137874,0.00017558466,0.0002221578],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00040407738,0.00063452544,0.00096777035,0.0002324666,0.00033454763,0.00025071757,0.0009338805,0.00020020174,0.00009780256],"category_scores_gemma":[0.00011077915,0.00045822366,0.00026797547,0.00088515284,0.0008409388,0.00041968867,0.00008536389,0.0003673165,0.00004758629],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028447658,0.00016668071,0.0151920235,0.00009412292,0.00011430501,0.0000417983,0.00059884775,0.0026267695,0.9726077,0.00041166414,0.0030531513,0.0048084627],"study_design_scores_gemma":[0.0027932618,0.0013894326,0.6145763,0.00013426575,0.00036188238,0.00016103795,0.00097441685,0.0019070138,0.36984998,0.0011461177,0.0052018464,0.0015044351],"about_ca_topic_score_codex":0.0078097424,"about_ca_topic_score_gemma":0.009460725,"teacher_disagreement_score":0.6027577,"about_ca_system_score_codex":0.000014193431,"about_ca_system_score_gemma":0.00015185571,"threshold_uncertainty_score":0.999787},"labels":[],"label_agreement":null},{"id":"W2555750105","doi":"10.1021/acs.jpcc.6b09434","title":"Dense Carbon Monoxide to 160 GPa: Stepwise Polymerization to Two-Dimensional Layered Solid","year":2016,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Steacie Institute for Molecular Sciences","funders":"Defense Sciences Office, DARPA; Division of Materials Research; Defense Threat Reduction Agency","keywords":"Carbon monoxide; Polymerization; Ionic bonding; Materials science; Phase (matter); Crystallography; Carbon fibers; Chemical engineering; Polymer; Composite number; Chemistry; Ion; Organic chemistry; Composite material; Catalysis","score_opus":0.007241453920611948,"score_gpt":0.2236224473456374,"score_spread":0.21638099342502545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2555750105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980763,0.00002233926,0.00006636272,0.0010344731,0.00013791837,0.000064443964,0.00005872858,0.000008456269,0.00053094066],"genre_scores_gemma":[0.99832517,0.0000020218204,0.0000611743,0.00016664456,0.0011197305,4.0816624e-7,0.000003442124,0.000005264426,0.0003161382],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99904126,0.000056844343,0.0002336787,0.00011136793,0.00033882988,0.00021800106],"domain_scores_gemma":[0.9991581,0.00017019674,0.00015335414,0.00017559878,0.00009362625,0.00024913534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020548575,0.0001259871,0.00022774587,0.00001700075,0.00006278304,0.000026145923,0.0002755498,0.000026567099,0.00026460196],"category_scores_gemma":[0.000058770318,0.00006460811,0.00006790594,0.00010863991,0.00003404229,0.00008076379,0.000029802939,0.00007311924,0.000068733105],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021739458,0.000024277551,0.000113203816,0.0000058017135,0.000025363013,0.0000071657923,0.00014643843,0.0074087316,0.9903082,0.0000048500765,0.0003094461,0.0014291026],"study_design_scores_gemma":[0.00036555584,0.00014938506,0.0030472614,0.000060534723,0.000043601325,0.000021347578,0.000018737777,0.00043852898,0.99479693,0.0005949324,0.00032236008,0.00014080365],"about_ca_topic_score_codex":0.00015085396,"about_ca_topic_score_gemma":0.000010230505,"teacher_disagreement_score":0.0069702026,"about_ca_system_score_codex":0.0000065935506,"about_ca_system_score_gemma":0.000054674983,"threshold_uncertainty_score":0.2897206},"labels":[],"label_agreement":null},{"id":"W2557709404","doi":"10.1107/s205327331409247x","title":"Structural Modifications of Cold and Dense Cesium, Calcium, Barium, and Selenium","year":2014,"lang":"en","type":"article","venue":"Acta Crystallographica Section A Foundations and Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Ottawa","funders":"","keywords":"Barium; Tetragonal crystal system; Orthorhombic crystal system; Selenium; Caesium; Materials science; Phase diagram; Phase (matter); Crystallography; Phase transition; Crystal structure; Chemistry; Thermodynamics; Inorganic chemistry; Metallurgy; Physics","score_opus":0.011190908848407182,"score_gpt":0.22686772329298172,"score_spread":0.21567681444457454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2557709404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99746275,0.00042196963,0.0008628503,0.0003235012,0.00022464948,0.00014842756,0.00009080955,0.000030601117,0.0004344132],"genre_scores_gemma":[0.99815506,0.00068977685,0.000918528,0.000037504364,0.000085280306,0.000004265984,0.00005870972,0.0000035077662,0.000047355603],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9992334,0.00006500568,0.00020406113,0.00024988392,0.000106032545,0.00014159702],"domain_scores_gemma":[0.9994373,0.0001454882,0.00012619702,0.000119418306,0.00007508752,0.00009656473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001425588,0.000119058794,0.00017279589,0.00012558365,0.0003958616,0.00012088347,0.000056276334,0.000055653512,0.00007191227],"category_scores_gemma":[0.000028510593,0.00010055898,0.000023814302,0.00021401317,0.0002843267,0.00058534543,0.000014336093,0.00006418177,2.2009228e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024420282,0.00011584823,0.29609203,0.00075513875,0.0002953228,0.000001801219,0.0012610686,0.0029606414,0.60751057,0.06464881,0.0002621677,0.025852434],"study_design_scores_gemma":[0.00070755545,0.00034679746,0.7573644,0.000030623178,0.00012047318,0.000035629142,0.0003379953,0.01074942,0.00043160713,0.009498489,0.21995175,0.00042526665],"about_ca_topic_score_codex":0.0005411911,"about_ca_topic_score_gemma":0.00112467,"teacher_disagreement_score":0.6070789,"about_ca_system_score_codex":9.0894e-7,"about_ca_system_score_gemma":0.000013047062,"threshold_uncertainty_score":0.41006762},"labels":[],"label_agreement":null},{"id":"W2557871031","doi":"10.1107/s2053273314091025","title":"Simple Binary Molecular Mixtures at High Density: the Methane-Nitrogen System","year":2014,"lang":"en","type":"article","venue":"Acta Crystallographica Section A Foundations and Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Methane; van der Waals force; Molecular solid; Miscibility; Chemistry; Tetragonal crystal system; Nitrogen; Solid solution; Thermodynamics; Phase (matter); Physical chemistry; Analytical Chemistry (journal); Organic chemistry; Molecule; Polymer","score_opus":0.005428996020395792,"score_gpt":0.2064448145970917,"score_spread":0.20101581857669593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2557871031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966436,0.00040589887,0.00076359976,0.00041656895,0.00055827375,0.00021149863,0.00006622007,0.000094987074,0.00083934335],"genre_scores_gemma":[0.9988298,0.00021782678,0.0002698388,0.0001628265,0.00020000956,0.000009773377,0.00026838057,0.000006091317,0.000035459183],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99888176,0.00020245227,0.00019953848,0.00029774592,0.00019540923,0.00022311797],"domain_scores_gemma":[0.99928296,0.00018880516,0.00013562552,0.00023945079,0.00006591962,0.000087235916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029938348,0.00015917237,0.00019036958,0.000104253144,0.00080170966,0.00016777219,0.00014465238,0.00006383165,0.0002171971],"category_scores_gemma":[0.00002895928,0.00010732597,0.00007139461,0.00031823624,0.00017287595,0.00030499778,0.000032178486,0.00008432322,0.0000042138804],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035241692,0.00012437532,0.08662441,0.0004753899,0.00067777507,0.000033260516,0.0005404449,0.006110863,0.8503599,0.022998584,0.0013001101,0.030402448],"study_design_scores_gemma":[0.0006157255,0.0003866875,0.07584972,0.000035746427,0.00022592564,0.000094675896,0.0004318108,0.0030575604,0.0016955193,0.029812563,0.88723236,0.0005616919],"about_ca_topic_score_codex":0.0013911832,"about_ca_topic_score_gemma":0.0020089957,"teacher_disagreement_score":0.88593227,"about_ca_system_score_codex":0.0000039538318,"about_ca_system_score_gemma":0.000013335213,"threshold_uncertainty_score":0.61661834},"labels":[],"label_agreement":null},{"id":"W2560087906","doi":"10.20381/ruor-493","title":"Lithospheric Structure Across the Northern Canadian Cordillera from Teleseismic Receiver Functions","year":2016,"lang":"en","type":"article","venue":"uO Research (University of Ottawa)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Receiver function; Seismology; Tectonics","score_opus":0.018987434961473468,"score_gpt":0.22465293757153987,"score_spread":0.2056655026100664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560087906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98529226,0.000038013226,0.00003810865,0.0023688274,0.0002327092,0.0001669673,0.004392983,0.000015393454,0.00745475],"genre_scores_gemma":[0.9931969,0.000052187643,0.00010471245,0.000030045005,0.00011289259,8.232102e-8,0.00008102566,0.0000038043468,0.006418334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857914,0.00020449377,0.00007672155,0.0002512707,0.0004049399,0.00048345412],"domain_scores_gemma":[0.99887615,0.00025950617,0.000049053666,0.000358056,0.0002132627,0.00024396222],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031696176,0.0000907517,0.0001469261,0.000055728462,0.0009106178,0.000050813534,0.0006340659,0.000086731176,0.016801959],"category_scores_gemma":[0.00003608373,0.000058973754,0.000053331132,0.0003293437,0.00041372742,0.00022016703,0.000047353584,0.00016491755,0.0007391305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003759532,0.000023528422,0.85658854,0.000018051122,0.0002366933,0.00008616886,0.002262658,0.00023556307,0.004626784,0.0003230205,0.021945484,0.11361594],"study_design_scores_gemma":[0.00022523089,0.000060367194,0.72714883,0.000013723983,0.000010343322,9.508793e-7,0.0012020776,0.000088110966,0.000099161494,0.0005752358,0.27048296,0.00009299147],"about_ca_topic_score_codex":0.48116285,"about_ca_topic_score_gemma":0.9134459,"teacher_disagreement_score":0.432283,"about_ca_system_score_codex":0.000022081982,"about_ca_system_score_gemma":0.00023724657,"threshold_uncertainty_score":0.9840968},"labels":[],"label_agreement":null},{"id":"W2560741233","doi":"10.1063/1.4969054","title":"Low temperature system for a large volume multi-anvil press","year":2016,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canada Foundation for Innovation","keywords":"Volume (thermodynamics); Liquid nitrogen; Materials science; Tungsten carbide; Carbide; Ambient pressure; Water cooling; Thermodynamics; Composite material; Chemistry; Physics","score_opus":0.014388390831253223,"score_gpt":0.23163168397635583,"score_spread":0.2172432931451026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560741233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9789739,0.0055963225,0.000079918995,0.00016785496,0.006094331,0.0018202653,0.006523317,0.00005647158,0.00068761443],"genre_scores_gemma":[0.99308455,0.0013375896,0.00062369974,0.00006886776,0.000106038045,0.00001794735,0.0002103009,0.00000603381,0.0045449613],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983519,0.00008005859,0.00043980763,0.00039204248,0.00036483747,0.00037136846],"domain_scores_gemma":[0.9990278,0.000028024398,0.00025313516,0.0004062472,0.00017425111,0.00011057444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010779535,0.00015536646,0.0003966487,0.00004268621,0.0002087628,0.00010374024,0.00039027454,0.000058880705,0.00061614625],"category_scores_gemma":[0.00005907174,0.0000894029,0.00013457992,0.00015473373,0.000079507976,0.00027756518,0.00003016775,0.000031852447,0.00029468504],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016415975,0.00065404724,0.021477874,0.12834483,0.0004535099,0.000015228406,0.00038493413,0.000006438097,0.18220836,0.0029293268,0.09727993,0.56608135],"study_design_scores_gemma":[0.002915308,0.00021568684,0.01253216,0.03792118,0.00021694181,0.000013299073,0.000045032688,0.0007121752,0.11096773,0.000080238824,0.83362126,0.0007589732],"about_ca_topic_score_codex":0.00006159902,"about_ca_topic_score_gemma":0.000022922708,"teacher_disagreement_score":0.73634136,"about_ca_system_score_codex":0.0000066291855,"about_ca_system_score_gemma":0.000058838665,"threshold_uncertainty_score":0.6746369},"labels":[],"label_agreement":null},{"id":"W2563482698","doi":"10.1016/j.epsl.2016.12.004","title":"Age-independent seismic anisotropy under oceanic plates explained by strain history in the asthenosphere","year":2016,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Cancer Institute; AGE-WELL; Natural Environment Research Council; Australian Government; Australian Research Council; Sight Research UK","keywords":"Geology; Anisotropy; Lithosphere; Asthenosphere; Seismic anisotropy; Geophysics; Dislocation creep; Mantle (geology); Seismology; Dislocation; Tectonics; Condensed matter physics","score_opus":0.008919125497694446,"score_gpt":0.17364895454394164,"score_spread":0.1647298290462472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2563482698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994554,0.0006574946,0.00012149315,0.0029637704,0.0004877436,0.00020347383,0.00030105634,0.000028427168,0.00068255264],"genre_scores_gemma":[0.9936729,0.0000846098,0.00016385969,0.0056294263,0.00010601156,0.0000010061059,0.000120580495,0.0000036693316,0.00021791467],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99808526,0.0001402229,0.00022102741,0.00046206467,0.0005044512,0.0005869653],"domain_scores_gemma":[0.9992852,0.00021092544,0.00008041539,0.0002577629,0.000008438048,0.00015726528],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007552756,0.00020687049,0.00019485402,0.00007563304,0.00021221404,0.0001260005,0.0005487777,0.000052749627,0.0016274008],"category_scores_gemma":[0.00001365988,0.000115919596,0.000029733254,0.00015836726,0.0005256411,0.0005439547,0.000017261984,0.00013249891,0.00020099996],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051956874,0.0001401968,0.271162,0.000108236345,0.000101042984,0.0015012764,0.006466149,0.0101429885,0.53776795,0.0015778535,0.12318373,0.047329027],"study_design_scores_gemma":[0.00078932766,0.00021777744,0.93998027,0.000038424205,0.000014029061,0.000070771974,0.00031579833,0.0009934242,0.00033984502,0.0006526967,0.056133974,0.00045367045],"about_ca_topic_score_codex":0.0017826434,"about_ca_topic_score_gemma":0.00083984964,"teacher_disagreement_score":0.6688183,"about_ca_system_score_codex":0.000008536825,"about_ca_system_score_gemma":0.00006746554,"threshold_uncertainty_score":0.9992852},"labels":[],"label_agreement":null},{"id":"W2564724042","doi":"10.1021/acs.jpcc.6b10916","title":"Contrasting Structural Stabilities and New Pressure-Induced Polymorphic Transitions of Scheelite- and Zircon-Type ZrGeO<sub>4</sub>","year":2016,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Scheelite; Tetragonal crystal system; Monoclinic crystal system; Raman spectroscopy; Zircon; Phase transition; Crystallography; Phase (matter); Materials science; Crystal structure; Chemical physics; Chemistry; Thermodynamics; Geology; Optics; Tungsten; Physics; Geochemistry","score_opus":0.012530342673580016,"score_gpt":0.20504838988755147,"score_spread":0.19251804721397145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2564724042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989058,0.00047028932,0.000022320164,0.00030437708,0.00006081394,0.000044782813,0.000097259486,0.0000049315513,0.00008944832],"genre_scores_gemma":[0.9994663,0.000033153476,0.000025003863,0.000011496147,0.00043715807,6.995074e-8,0.0000021292212,0.000003239183,0.000021435299],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992852,0.000054350166,0.0002339588,0.00008752395,0.00018193263,0.00015702259],"domain_scores_gemma":[0.99915135,0.00033506873,0.00019700524,0.000098944474,0.00008633181,0.0001313087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001829726,0.00011274038,0.0002646429,0.000010569027,0.000077614655,0.000026047948,0.00012053674,0.000037742517,0.00008862665],"category_scores_gemma":[0.00006576367,0.00005895679,0.000046804547,0.00004991877,0.00016655737,0.00018518908,0.0000118145035,0.00010400339,0.0000011186646],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011344537,0.000006598864,0.00032352537,0.000057369594,0.000054896063,0.0000011748822,0.0004148523,0.000036759666,0.9961453,0.00003530847,0.000018116032,0.0027926348],"study_design_scores_gemma":[0.0004954142,0.00014141607,0.016583513,0.00009349576,0.00014214938,0.000038878585,0.000101082514,0.000176837,0.97881544,0.0032590383,0.00005065551,0.000102086524],"about_ca_topic_score_codex":0.00008016499,"about_ca_topic_score_gemma":0.0000068311006,"teacher_disagreement_score":0.017329885,"about_ca_system_score_codex":0.0000013402823,"about_ca_system_score_gemma":0.000068011745,"threshold_uncertainty_score":0.2404188},"labels":[],"label_agreement":null},{"id":"W2565400120","doi":"10.1093/gji/ggw473","title":"Singular spectrum analysis and its applications in mapping mantle seismic structure","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Classification of discontinuities; Subduction; Seismology; Mantle (geology); Singular value decomposition; Seismogram; Seismic wave; Geophysics; Tectonics; Algorithm; Computer science; Mathematics; Mathematical analysis","score_opus":0.006750322414271067,"score_gpt":0.2122232067053403,"score_spread":0.20547288429106925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2565400120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926403,0.00006361199,0.005269668,0.0010794803,0.00028995093,0.0000677712,0.00020149164,0.000010409963,0.0003773105],"genre_scores_gemma":[0.9987524,0.000051773073,0.00022437738,0.00007609052,0.0005948354,8.102015e-7,0.000043255663,0.0000028478205,0.00025356846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909496,0.000040437346,0.00022291113,0.0001935723,0.00025061346,0.00019748647],"domain_scores_gemma":[0.99956554,0.000098411474,0.00011005875,0.00007845643,0.000046695437,0.000100853],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010310604,0.00010682775,0.00018042953,0.00020939801,0.0000943806,0.000121561534,0.0002178999,0.000040353487,0.001778929],"category_scores_gemma":[0.0000174458,0.000068591704,0.000074970194,0.00024129439,0.000031861113,0.0002585338,0.000023297274,0.000107816224,0.00007886027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018676577,0.00025541973,0.69636637,0.000048318816,0.0026792502,0.00023059774,0.000977229,0.008098306,0.14113036,0.016741063,0.00055468944,0.13273163],"study_design_scores_gemma":[0.0003636704,0.000027079224,0.94463664,0.00002686035,0.00006737082,0.00003053322,0.000029094239,0.0059194346,0.0022344487,0.039825343,0.0066501554,0.00018938266],"about_ca_topic_score_codex":0.00020556059,"about_ca_topic_score_gemma":0.00019835206,"teacher_disagreement_score":0.24827026,"about_ca_system_score_codex":0.000008864891,"about_ca_system_score_gemma":0.000020307576,"threshold_uncertainty_score":0.9991336},"labels":[],"label_agreement":null},{"id":"W2570244633","doi":"10.1016/j.epsl.2016.12.031","title":"Formation and properties of water from quartz and hydrogen at high pressure and temperature","year":2017,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China; China Scholarship Council; Science Foundation Ireland; National Science Foundation","keywords":"Quartz; Dissolution; Hydrogen; Geology; Mantle (geology); Chemical physics; Ambient pressure; Silicon; Brine; Mineralogy; Chemical engineering; Materials science; Geophysics; Thermodynamics; Chemistry","score_opus":0.007266539991505237,"score_gpt":0.15852637831157929,"score_spread":0.15125983832007406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2570244633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99670035,0.0014746998,4.0060564e-7,0.0012132934,0.00012553761,0.00014413841,0.00028049274,0.000008990719,0.000052078274],"genre_scores_gemma":[0.99917734,0.00018804609,0.00012151037,0.0002761939,0.00007516809,4.6423466e-7,0.000106552376,0.0000017270825,0.000052979627],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991109,0.000032151784,0.00013296082,0.0002870243,0.00019713001,0.00023983831],"domain_scores_gemma":[0.9995669,0.000021945423,0.00007515326,0.00018921426,0.00001263657,0.00013415577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002305137,0.00012997832,0.00018429266,0.000045021625,0.00071445224,0.00032855323,0.0001458165,0.000047669513,0.000085724605],"category_scores_gemma":[0.0000100039315,0.0000807835,0.000008442543,0.000019315632,0.0007107367,0.0009808756,0.00005459077,0.000062745705,0.000008019412],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000099457255,0.0000035789128,0.22064845,0.00012851728,0.000028300483,0.000012634683,0.001849894,0.00020429536,0.77372295,0.000010938999,0.00019248044,0.0030984867],"study_design_scores_gemma":[0.000289714,0.00007952263,0.9353414,0.000039688028,0.0000345836,0.000025974039,0.000034922272,0.0014853108,0.059961013,0.00007813512,0.0024574553,0.00017227317],"about_ca_topic_score_codex":0.005259487,"about_ca_topic_score_gemma":0.00082251494,"teacher_disagreement_score":0.71469295,"about_ca_system_score_codex":3.1593373e-7,"about_ca_system_score_gemma":0.000007455555,"threshold_uncertainty_score":0.7950806},"labels":[],"label_agreement":null},{"id":"W2575902678","doi":"10.1080/08957959.2016.1274979","title":"Diamond cleavage: importance to high pressure research","year":2017,"lang":"en","type":"article","venue":"High Pressure Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"St. Francis Xavier University; Northwestern University","keywords":"Cleavage (geology); Stereographic projection; Diamond; Principal stress; Geometry; Anisotropy; Crystallography; Materials science; High pressure; Composite material; Optics; Chemistry; Physics; Mathematics; Mechanics; Shear stress; Fracture (geology)","score_opus":0.08868285381240536,"score_gpt":0.372342980966571,"score_spread":0.2836601271541656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2575902678","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91179985,0.0037667835,0.000018834411,0.0070542414,0.0026693675,0.0031318006,0.0023320706,0.00022590587,0.06900117],"genre_scores_gemma":[0.97461873,0.00028241504,0.00048812293,0.000078686266,0.001947887,0.00006666658,0.00011703369,0.000038515405,0.022361942],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99096125,0.0014061047,0.0005480934,0.001393981,0.0033377435,0.0023528368],"domain_scores_gemma":[0.99379313,0.000915632,0.00018428799,0.003162967,0.0010070456,0.00093693694],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.007987735,0.00039153604,0.00066351995,0.00043822755,0.0036561014,0.002086538,0.0036418885,0.00038329352,0.005407691],"category_scores_gemma":[0.0013479531,0.00032917922,0.00010992192,0.0005564635,0.0008488311,0.0009220924,0.0008050276,0.00141667,0.004201116],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015488191,0.0003900076,0.1814941,0.0011512241,0.00075110525,0.00084147585,0.0016759651,0.0030440344,0.015902981,0.022632018,0.751213,0.019355284],"study_design_scores_gemma":[0.0004705078,0.00035744862,0.5076811,0.00008769241,0.000037847403,0.000004878715,0.000056823148,0.00014676286,0.0058065876,0.006346791,0.47860512,0.00039845804],"about_ca_topic_score_codex":0.03872226,"about_ca_topic_score_gemma":0.0044511952,"teacher_disagreement_score":0.32618698,"about_ca_system_score_codex":0.000010714863,"about_ca_system_score_gemma":0.00030298237,"threshold_uncertainty_score":0.999916},"labels":[],"label_agreement":null},{"id":"W2581281702","doi":"10.1063/1.4974149","title":"Rotary shear experiments under X-ray micro-computed tomography","year":2017,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Carbon Management Canada; University of Toronto; Canada Foundation for Innovation","keywords":"Shearing (physics); Materials science; Tomography; Shear (geology); Deformation (meteorology); Computed tomography; Sample (material); X-ray; Composite material; Mechanics; Optics; Physics","score_opus":0.022135126827149104,"score_gpt":0.2580554793642821,"score_spread":0.23592035253713298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2581281702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98630553,0.0048633968,0.0000083930245,0.00014636703,0.0034603893,0.0004966013,0.0002427376,0.000021863803,0.0044547287],"genre_scores_gemma":[0.9957931,0.0014474405,0.0015834083,0.0002299017,0.00008800695,0.0000032877638,0.00021955099,0.000005307404,0.0006300013],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99820024,0.00007825931,0.00044030245,0.00043112636,0.00050730136,0.00034279138],"domain_scores_gemma":[0.9984376,0.000012806071,0.00040613097,0.00090936525,0.0000958544,0.00013823455],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00072214083,0.00018250187,0.00040395983,0.0000922163,0.00070652994,0.0004720215,0.0008834024,0.000047443387,0.001706094],"category_scores_gemma":[0.000020337837,0.00014380061,0.00015554263,0.00016700578,0.0003534046,0.0006497385,0.000084588464,0.00006518546,0.0003495335],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012229907,0.00079097267,0.20123369,0.017621243,0.00090337754,0.000041957985,0.00048801585,0.00008409486,0.1357843,0.00157251,0.037774455,0.6035831],"study_design_scores_gemma":[0.0012404554,0.0001904746,0.79712313,0.010817866,0.00017511523,0.000009513754,0.000046977315,0.00040689146,0.058858313,0.0013806506,0.1288471,0.0009035128],"about_ca_topic_score_codex":0.00039623346,"about_ca_topic_score_gemma":0.000011824446,"teacher_disagreement_score":0.6026796,"about_ca_system_score_codex":0.0000034392874,"about_ca_system_score_gemma":0.000056077857,"threshold_uncertainty_score":0.9992065},"labels":[],"label_agreement":null},{"id":"W2585899355","doi":"10.1016/j.pepi.2017.01.005","title":"Thermal conductivity and Seebeck coefficient of Fe and Fe-Si alloys: Implications for variable Lorenz number","year":2017,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seebeck coefficient; Thermal conductivity; Wiedemann–Franz law; Condensed matter physics; Electrical resistivity and conductivity; Materials science; Thermoelectric materials; Thermodynamics; Thermoelectric effect; Physics; Composite material; Quantum mechanics","score_opus":0.019797348832244335,"score_gpt":0.23426906702843386,"score_spread":0.21447171819618954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2585899355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99701864,0.00012756257,0.000065742744,0.00019584697,0.00024727097,0.0002411378,0.0014860721,0.0000054401617,0.00061229296],"genre_scores_gemma":[0.99920535,0.000052545634,0.0004586794,0.00004366423,0.00008404385,0.0000013593268,0.00008232542,0.000003442376,0.00006857365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993904,0.00003630487,0.00016042026,0.00018207241,0.00007295687,0.00015785194],"domain_scores_gemma":[0.99925226,0.00012817104,0.00021678227,0.00030073104,0.0000357132,0.00006637012],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015511637,0.000121619014,0.00025117892,0.0000095107835,0.00026909658,0.0000719609,0.00020115208,0.00004003177,0.00004122356],"category_scores_gemma":[0.000021736163,0.000084470674,0.00003471457,0.000021341997,0.00030115971,0.00017505542,0.000056232868,0.00005583267,0.0000019439995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004440965,0.00009935158,0.8773273,0.00061232026,0.00032944768,8.618558e-7,0.0011647311,0.0021526013,0.089387365,0.0057557863,0.0004666279,0.022259483],"study_design_scores_gemma":[0.00043238082,0.00013397589,0.9834056,0.00006202682,0.00008675492,0.000007027655,0.000037324942,0.0025828972,0.0058527724,0.005289379,0.0019331828,0.00017666828],"about_ca_topic_score_codex":0.0036416512,"about_ca_topic_score_gemma":0.00041924455,"teacher_disagreement_score":0.10607828,"about_ca_system_score_codex":3.5850854e-7,"about_ca_system_score_gemma":0.000022768258,"threshold_uncertainty_score":0.5505112},"labels":[],"label_agreement":null},{"id":"W2592482134","doi":"10.1002/9781118944998.ch5","title":"Geodynamical Models for Continental Delamination and Ocean Lithosphere Peel Away in an Orogenic Setting","year":2017,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu; Dalhousie University","keywords":"Geology; Lithosphere; Subduction; Mantle (geology); Delamination (geology); Geophysics; Plate tectonics; Ocean surface topography; Collision zone; Asthenosphere; Seismology; Tectonics; Geodesy","score_opus":0.00903804905209905,"score_gpt":0.22693925699271517,"score_spread":0.21790120794061613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2592482134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9717168,0.0009287271,0.00045990825,0.00007307442,0.00076370867,0.0013426206,0.0022252065,0.00017217148,0.02231774],"genre_scores_gemma":[0.9837119,0.00012686041,0.0017970618,0.000039593717,0.0007959763,0.000014986805,0.0017640797,0.00009373576,0.011655825],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9984261,0.00007094321,0.00023527391,0.00059623,0.00020960797,0.0004618484],"domain_scores_gemma":[0.9991214,0.000074113406,0.00024384329,0.00036002704,0.000032946562,0.00016765315],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00016820041,0.00034465102,0.00052400987,0.000118258125,0.00015299591,0.00020327623,0.00032036658,0.0002958503,0.00014454346],"category_scores_gemma":[0.000013364461,0.0003082933,0.00013962321,0.000077693476,0.00015006117,0.00028431445,0.000034734414,0.00017049434,0.00001861947],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017509427,0.0019237461,0.18546522,0.0035701634,0.0015022709,0.0002616329,0.0031291388,0.0038417594,0.0018620156,0.019391302,0.12016526,0.65713656],"study_design_scores_gemma":[0.006218308,0.0016956269,0.42041177,0.0012762923,0.00060816,0.000017315315,0.00031808583,0.4120269,0.00009353199,0.071698025,0.08149208,0.0041438923],"about_ca_topic_score_codex":0.0045766486,"about_ca_topic_score_gemma":0.0057615764,"teacher_disagreement_score":0.65299267,"about_ca_system_score_codex":0.0000027971573,"about_ca_system_score_gemma":0.00002879064,"threshold_uncertainty_score":0.99993694},"labels":[],"label_agreement":null},{"id":"W2595409973","doi":"10.1103/physreve.95.043201","title":"Equation of state, phonons, and lattice stability of ultrafast warm dense matter","year":2017,"lang":"en","type":"article","venue":"Physical review. E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Université de Montréal; Regroupement Québécois sur les Matériaux de Pointe","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Compute Canada","keywords":"Density functional theory; Pseudopotential; Phonon; Physics; Condensed matter physics; Lattice (music); Electron; Equation of state; Fermi gas; Atomic physics; Quantum mechanics","score_opus":0.027757089368413083,"score_gpt":0.2875014171422908,"score_spread":0.25974432777387774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2595409973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975684,0.0006690039,0.000020611677,0.00015956217,0.00007270268,0.00018053192,0.00018298016,0.0000036563683,0.0011425295],"genre_scores_gemma":[0.99854475,0.0012272453,0.00008213222,0.000060719805,0.000045653294,0.000001212925,0.000021314714,0.0000019798065,0.0000150061005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993155,0.00007272313,0.00021126027,0.00014466,0.0001454231,0.000110452],"domain_scores_gemma":[0.9991809,0.00013569968,0.00024636742,0.00032569273,0.000057871635,0.000053436852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002851542,0.00008055145,0.00032521228,0.0000073998517,0.00006082802,0.000023245992,0.00014601207,0.00001208303,0.00036163494],"category_scores_gemma":[0.00010176406,0.000058452522,0.000047960864,0.000025709358,0.00012244927,0.000172262,0.000019323254,0.000038582166,0.00009091315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018786303,0.00043803596,0.70544857,0.0132825365,0.00014324568,0.0000041317185,0.0012066866,0.000048500176,0.20265746,0.0012979134,0.0011188583,0.07416621],"study_design_scores_gemma":[0.00018649637,0.00009410426,0.92476934,0.00040726588,0.00008207178,5.6352485e-7,0.000006925795,0.00037852646,0.06595011,0.006802433,0.0011772311,0.0001449518],"about_ca_topic_score_codex":0.0010552244,"about_ca_topic_score_gemma":0.000070519745,"teacher_disagreement_score":0.21932076,"about_ca_system_score_codex":7.307565e-7,"about_ca_system_score_gemma":0.0000157752,"threshold_uncertainty_score":0.3959649},"labels":[],"label_agreement":null},{"id":"W2603475914","doi":"10.1039/c7dt00539c","title":"New pressure-induced polymorphic transitions of anhydrous magnesium sulfate","year":2017,"lang":"en","type":"article","venue":"Dalton Transactions","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec)","funders":"Ministerio de Economía y Competitividad","keywords":"Anhydrous; Magnesium; Phase (matter); Sulfate; Polymorphism (computer science)","score_opus":0.017524827892593634,"score_gpt":0.2265151546229717,"score_spread":0.20899032673037807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2603475914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9415637,0.00030641045,0.029976606,0.002286157,0.003101176,0.00059397635,0.00321939,0.00015937455,0.018793162],"genre_scores_gemma":[0.99692345,0.000014224668,0.00053824764,0.000019644622,0.00016344203,0.0000023148093,0.0000634286,0.0000068641702,0.0022683833],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99900746,0.00004544511,0.00024720337,0.00023530234,0.00019914657,0.000265433],"domain_scores_gemma":[0.99907935,0.000028257746,0.0001383431,0.0005384541,0.000040297495,0.00017528208],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000112776215,0.00014897478,0.00024662566,0.00006780264,0.0006951878,0.00011616505,0.00035308214,0.000091558984,0.0037205904],"category_scores_gemma":[0.000004177278,0.00013787577,0.00011426884,0.00007093196,0.000070536946,0.0004171925,0.000002037433,0.000109626264,0.00013719658],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014145277,0.0010898212,0.0188536,0.0015749676,0.0016162512,0.00018805862,0.0075075324,0.044785555,0.6284736,0.006567105,0.003941057,0.28398797],"study_design_scores_gemma":[0.003438118,0.0008416409,0.7696413,0.00010387416,0.0014079561,0.000067525056,0.000118180506,0.0047454867,0.14961298,0.0046853763,0.063981496,0.0013560612],"about_ca_topic_score_codex":0.033693578,"about_ca_topic_score_gemma":0.010912406,"teacher_disagreement_score":0.75078773,"about_ca_system_score_codex":0.0000011398698,"about_ca_system_score_gemma":0.000079777456,"threshold_uncertainty_score":0.9971901},"labels":[],"label_agreement":null},{"id":"W2607227785","doi":"10.1021/acs.jpcc.7b01506","title":"Hydrogen-Doped Polymeric Carbon Monoxide at High Pressure","year":2017,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Division of Materials Research; Defense Advanced Research Projects Agency; National Nuclear Security Administration; Defense Threat Reduction Agency; National Science Foundation","keywords":"Materials science; Polymerization; Chemical engineering; Polymer; Anhydrous; Phase (matter); Carbon monoxide; Oxalic acid; Hydrogen; Carbon fibers; Doping; Inorganic chemistry; Organic chemistry; Chemistry; Composite material; Composite number; Catalysis","score_opus":0.007717894995128347,"score_gpt":0.20817983709060267,"score_spread":0.20046194209547433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2607227785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994403,0.00030840715,7.187553e-7,0.00030401497,0.00015124648,0.000040833726,0.000041363575,0.000006844251,0.0047435868],"genre_scores_gemma":[0.99727684,0.000027595617,0.000008240921,0.000023411434,0.0014552502,1.9943526e-7,0.0000049440882,0.0000050357157,0.0011984592],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999114,0.000047167563,0.00020211548,0.000101197555,0.00031680593,0.00021875529],"domain_scores_gemma":[0.99878734,0.00009225786,0.000504998,0.00043488626,0.000047941354,0.00013256805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002068148,0.00013953053,0.0002843305,0.0000062767017,0.00029792468,0.000073182055,0.00078812137,0.000042043004,0.0003191285],"category_scores_gemma":[0.00004066779,0.00008165879,0.00010710181,0.000027154822,0.00014481149,0.00013105784,0.000059172515,0.00016772495,0.000032671454],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015476561,0.00003145631,0.0010511946,0.000032323376,0.00010957592,0.000018148621,0.00013881594,0.0014996403,0.99612904,0.000010662414,0.00021503438,0.00060935016],"study_design_scores_gemma":[0.00033815904,0.000075261385,0.018936371,0.000023685203,0.00019343733,0.00003848649,0.0000148738645,0.0012175426,0.97613096,0.00081975356,0.0020652357,0.00014621326],"about_ca_topic_score_codex":0.00097303354,"about_ca_topic_score_gemma":0.000012298792,"teacher_disagreement_score":0.019998053,"about_ca_system_score_codex":0.0000032045757,"about_ca_system_score_gemma":0.000035964764,"threshold_uncertainty_score":0.34942335},"labels":[],"label_agreement":null},{"id":"W2607617830","doi":"10.1002/2016jb013599","title":"Seismic anisotropy of Precambrian lithosphere: Insights from Rayleigh wave tomography of the eastern Superior Craton","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"National Science Foundation","keywords":"Lithosphere; Geology; Craton; Archean; Precambrian; Proterozoic; Seismic anisotropy; Tectonics; Seismology; Geophysics; Plate tectonics; Paleontology; Mantle (geology)","score_opus":0.0325607555067306,"score_gpt":0.28620392599211797,"score_spread":0.25364317048538737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2607617830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974427,0.0002739787,0.000024367098,0.00024972085,0.0006116324,0.00021347936,0.00017893943,0.000003848427,0.0010013309],"genre_scores_gemma":[0.9984835,0.00012129558,0.0002824121,0.000018461746,0.00076764915,6.998628e-7,0.00000589398,0.000008757858,0.00031137402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99675906,0.00048689722,0.00063977326,0.00023664923,0.0014335201,0.0004441294],"domain_scores_gemma":[0.9971996,0.0003688134,0.00072659063,0.0007800324,0.00065033237,0.00027464275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060137967,0.00018713949,0.00067850086,0.000096238764,0.00041772178,0.0002325811,0.0011877262,0.00010839817,0.0003554497],"category_scores_gemma":[0.000285682,0.00011177384,0.00037613753,0.0002282139,0.0007128472,0.0005259508,0.00015658507,0.0005138959,0.000048459948],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0045897793,0.0014244567,0.5211214,0.00058071007,0.0016882588,0.0003060858,0.005324391,0.0016653442,0.40247092,0.0024168564,0.001950595,0.056461252],"study_design_scores_gemma":[0.0006815517,0.00085978047,0.9215753,0.00024088984,0.000042103064,0.0000044179646,0.000103957784,0.0027249998,0.06371494,0.00809599,0.0018237053,0.00013238304],"about_ca_topic_score_codex":0.009763133,"about_ca_topic_score_gemma":0.0007479159,"teacher_disagreement_score":0.40045393,"about_ca_system_score_codex":0.0000034056625,"about_ca_system_score_gemma":0.00028408368,"threshold_uncertainty_score":0.99683094},"labels":[],"label_agreement":null},{"id":"W2613130203","doi":"10.1093/gji/ggx198","title":"Spin transition-induced anomalies in the lower mantle: implications for mid-mantle partial layering","year":2017,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Directorate for Computer and Information Science and Engineering; National Science Foundation","keywords":"Transition zone; Mantle (geology); Geology; Spin transition; Mantle convection; Geophysics; Slab; Mantle wedge; Silicate perovskite; Petrology; Subduction; Condensed matter physics; Physics; Tectonics; Seismology","score_opus":0.03173665838268811,"score_gpt":0.29526618983511577,"score_spread":0.26352953145242763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2613130203","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850324,0.000013596837,0.0010522626,0.0097114025,0.0017656095,0.00016632375,0.00026774002,0.00000884401,0.0019818547],"genre_scores_gemma":[0.9972933,0.000014648504,0.00023754538,0.00027862546,0.0020313233,0.000009722882,0.000060248487,0.000004079031,0.00007052808],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9990919,0.00004281308,0.00024655764,0.0001647607,0.0002179182,0.00023605172],"domain_scores_gemma":[0.9993644,0.00011317356,0.00016582457,0.00020896403,0.000085270614,0.0000623692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029332584,0.00011011616,0.00014129996,0.00004328855,0.00055628957,0.00062411634,0.000718818,0.00004116306,0.0003828835],"category_scores_gemma":[0.000049309852,0.000076987344,0.00011918353,0.0000311815,0.000056424666,0.0004455278,0.0000170418,0.00014724345,0.00008369009],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029570314,0.0034142358,0.09794605,0.00017866792,0.0014888016,0.0005207921,0.008617395,0.016343677,0.33788928,0.13729839,0.022733713,0.37061197],"study_design_scores_gemma":[0.00072708225,0.00017792861,0.95697963,0.000036640675,0.000026884838,0.000050527968,0.00007484606,0.0026607716,0.0017848591,0.024293564,0.012987515,0.00019973845],"about_ca_topic_score_codex":0.0004686146,"about_ca_topic_score_gemma":0.00026223503,"teacher_disagreement_score":0.8590336,"about_ca_system_score_codex":0.000005322404,"about_ca_system_score_gemma":0.000036313362,"threshold_uncertainty_score":0.60183686},"labels":[],"label_agreement":null},{"id":"W2619150855","doi":"10.1002/2016jb013785","title":"Constraints on melt content of off‐axis magma lenses at the East Pacific Rise from analysis of 3‐D seismic amplitude variation with angle of incidence","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"BP (Canada); Shell (Canada); Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Courant Forschungszentrum Geobiologie, Georg-August-Universität Göttingen; Canada Foundation for Innovation; National Science Foundation","keywords":"Geology; Mantle (geology); Amplitude; Magma; Magma chamber; Mineralogy; Partial melting; Seismology; Petrology; Geochemistry; Volcano; Optics","score_opus":0.05882623067232355,"score_gpt":0.30742997354940327,"score_spread":0.2486037428770797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619150855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979857,0.00009620892,0.00008156997,0.00026792652,0.00009631894,0.0001657595,0.0008016755,0.0000019718464,0.0005028635],"genre_scores_gemma":[0.9994396,0.0001287903,0.00012267753,0.000010481099,0.00013494756,7.565951e-7,0.000020710397,0.000004286836,0.00013774377],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99692875,0.00043083722,0.0006082483,0.00021157536,0.0015026055,0.00031798417],"domain_scores_gemma":[0.9961756,0.0009566536,0.001135026,0.0005926632,0.00097374286,0.00016630547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00143636,0.00014413877,0.0007676403,0.00020752974,0.00026477524,0.000095358,0.0006446333,0.00005211845,0.0007119395],"category_scores_gemma":[0.00049690396,0.000082677165,0.00023982662,0.00030440066,0.0011393824,0.00027947966,0.00007328798,0.0002765652,0.000025776983],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013158359,0.0017881845,0.3400959,0.0003383784,0.009288796,0.00024364771,0.008219108,0.028595168,0.45679417,0.0012845221,0.0007048262,0.13948892],"study_design_scores_gemma":[0.0004957093,0.0011558554,0.9781328,0.00014286733,0.00024442447,0.0000024930093,0.00028028083,0.0025991441,0.016142637,0.000617274,0.00010093224,0.000085586085],"about_ca_topic_score_codex":0.0123630725,"about_ca_topic_score_gemma":0.0014856564,"teacher_disagreement_score":0.6380369,"about_ca_system_score_codex":0.000007433424,"about_ca_system_score_gemma":0.00020487777,"threshold_uncertainty_score":0.9942137},"labels":[],"label_agreement":null},{"id":"W2661761461","doi":"10.1002/2017jb014284","title":"Architecture of the crust and uppermost mantle in the northern Canadian Cordillera from receiver functions","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Ministry of Research, Innovation and Science; Agence Nationale de la Recherche; National Science Foundation","keywords":"Geology; Crust; Seismology; Mantle (geology); Lithosphere; Anisotropy; Receiver function; Seismic anisotropy; Crustal recycling; Geophysics; Tectonics; Continental crust; Petrology","score_opus":0.029057416687403113,"score_gpt":0.2816063291608422,"score_spread":0.2525489124734391,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2661761461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930855,0.000080810394,0.0000014770097,0.0028717602,0.00025553492,0.00013994168,0.00022616195,9.299429e-7,0.00333788],"genre_scores_gemma":[0.9990755,0.000062886764,0.000022672595,0.000072420546,0.00048014522,5.5728293e-7,0.000005503209,0.0000032450916,0.00027711134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99832374,0.0003335894,0.00022687716,0.00012648922,0.0006476527,0.00034165886],"domain_scores_gemma":[0.9986553,0.00038886146,0.00017356963,0.00040510317,0.0001952653,0.00018189459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073012576,0.000090973575,0.00024194938,0.00008339781,0.00065108424,0.0002220595,0.0007639668,0.00005263381,0.00044060004],"category_scores_gemma":[0.0003300791,0.000045460136,0.00008438011,0.00012823172,0.0003966622,0.00015886214,0.00004795561,0.0005957173,0.000047250214],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010021445,0.00039079285,0.8041588,0.00010671459,0.00046032545,0.00043469967,0.009407313,0.0031115713,0.019887,0.0005166791,0.0073368237,0.15318713],"study_design_scores_gemma":[0.00022618363,0.00015994649,0.9902136,0.000058344038,0.000012146546,0.000007219654,0.00022741256,0.00019915358,0.00022133111,0.0023905237,0.006228617,0.000055574346],"about_ca_topic_score_codex":0.2851451,"about_ca_topic_score_gemma":0.3975595,"teacher_disagreement_score":0.18605474,"about_ca_system_score_codex":0.000004232561,"about_ca_system_score_gemma":0.0003095349,"threshold_uncertainty_score":0.71961516},"labels":[],"label_agreement":null},{"id":"W267504818","doi":"10.1007/3-540-27946-6_8","title":"Synchronous vertical and horizontal tectonism during the late stage of Archean cratonization: An important process in gold mineralization?","year":2005,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Archean; Geology; Crust; Greenstone belt; Geochemistry; Tectonics; Mantle (geology); Petrology; Paleontology","score_opus":0.007798595397269296,"score_gpt":0.2092101973474797,"score_spread":0.2014116019502104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W267504818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9597842,0.00020971797,0.00001430301,0.00006537454,0.00010680826,0.00033180384,0.00023205024,0.000025715257,0.039230008],"genre_scores_gemma":[0.9553568,0.00018700995,0.00005311863,0.000028804401,0.0001659573,0.0000014410107,0.00020375306,0.000011900636,0.043991268],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99893403,0.000021648078,0.00039613942,0.00024039485,0.0002175636,0.00019022681],"domain_scores_gemma":[0.99956197,0.000026626754,0.00010082277,0.0001872319,0.000043273125,0.000080085316],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015144776,0.0001977486,0.00028553608,0.00006293341,0.00006482628,0.00006828991,0.00015451164,0.00012766103,0.001975292],"category_scores_gemma":[0.000006057144,0.00013250197,0.000027141416,0.00003650943,0.000114841045,0.00015860358,0.00001805755,0.00011422345,0.000008713056],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017049373,0.00064359943,0.39010513,0.0068314094,0.0011204617,0.00094710966,0.014566992,0.087793864,0.022718074,0.45403907,0.00033381424,0.019195555],"study_design_scores_gemma":[0.006738936,0.0033699605,0.81175494,0.0014410694,0.0006455786,0.0001726332,0.00076418207,0.07585087,0.019838903,0.03184764,0.04111212,0.0064631416],"about_ca_topic_score_codex":0.0008849716,"about_ca_topic_score_gemma":0.0063119954,"teacher_disagreement_score":0.4221914,"about_ca_system_score_codex":0.000004066343,"about_ca_system_score_gemma":0.00007241964,"threshold_uncertainty_score":0.998937},"labels":[],"label_agreement":null},{"id":"W2703371356","doi":"10.1038/nphys4156","title":"Spectroscopic evidence of a new energy scale for superconductivity in H3S","year":2017,"lang":"en","type":"article","venue":"Nature Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; Canadian Institute for Advanced Research; University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Superconductivity; Phonon; Hydrostatic pressure; Physics; Condensed matter physics; Hydride; Range (aeronautics); Photon energy; Photon; Atomic physics; Materials science; Quantum mechanics; Hydrogen; Thermodynamics","score_opus":0.029263637989350805,"score_gpt":0.28944198501665785,"score_spread":0.260178347027307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2703371356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967122,0.00085286575,0.0003893673,0.00026679967,0.000766903,0.00013456607,0.0000697625,0.000009393291,0.00079812005],"genre_scores_gemma":[0.998066,0.00007619779,0.00097040675,0.00004291586,0.00055642944,0.0000013642989,0.000016203263,0.000003210095,0.00026724726],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993272,0.00002108096,0.000115137846,0.00020302106,0.00014031761,0.00019327794],"domain_scores_gemma":[0.9993548,0.000089141016,0.000103183134,0.00036204985,0.000038043836,0.00005278627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012316993,0.00009921906,0.0002330305,0.000016734148,0.00010103307,0.00006392651,0.00034184175,0.0001077975,0.00007915615],"category_scores_gemma":[0.000060040165,0.00008261875,0.000056352306,0.000048487917,0.000055858032,0.000474322,0.000019425232,0.000117719464,0.000007925113],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007636969,0.000293263,0.30413437,0.00089446054,0.000105686915,0.000015028805,0.0015536457,0.0010984085,0.49985898,0.036119614,0.0070778937,0.14808495],"study_design_scores_gemma":[0.00083189365,0.00026313702,0.50625724,0.00034338442,0.000043104632,8.9202865e-7,0.000021361426,0.00087131665,0.34957692,0.135668,0.0057510324,0.00037172253],"about_ca_topic_score_codex":0.0067185955,"about_ca_topic_score_gemma":0.0031019682,"teacher_disagreement_score":0.20212287,"about_ca_system_score_codex":0.0000024158596,"about_ca_system_score_gemma":0.00008267281,"threshold_uncertainty_score":0.99989575},"labels":[],"label_agreement":null},{"id":"W2726667971","doi":"10.1002/2017jb014261","title":"Absolute reconstruction of the closing of the Mongol‐Okhotsk Ocean in the Mesozoic elucidates the genesis of the slab geometry underneath Eurasia","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Mantle (geology); Subduction; Convergent boundary; Fibrous joint; Paleontology; Paleomagnetism; Mesozoic; Stage (stratigraphy); Oceanic crust; Tectonics; Structural basin","score_opus":0.041839667581095204,"score_gpt":0.30977616861814083,"score_spread":0.26793650103704564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2726667971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959591,0.00021651448,0.0000025181573,0.0021713707,0.0005543995,0.00037175565,0.00007550259,0.0000016256757,0.00064723747],"genre_scores_gemma":[0.9991645,0.00022005632,0.000024380539,0.00003658515,0.0003995664,7.8950575e-7,8.8623256e-7,0.0000066404496,0.00014655104],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99595696,0.001220284,0.00065215176,0.00017500842,0.0015660945,0.00042950193],"domain_scores_gemma":[0.99645984,0.000944993,0.0010561027,0.001077073,0.0003936262,0.000068372705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003214276,0.0001578322,0.00043120945,0.00008684073,0.0008174711,0.00018031069,0.0026481592,0.00007876638,0.00008398347],"category_scores_gemma":[0.00079226436,0.000057303776,0.0003699811,0.000548925,0.0013019098,0.00029861185,0.00023735309,0.00072965026,0.000006747319],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013657218,0.00084546895,0.7016078,0.0006675851,0.0011202359,0.000033014378,0.01141453,0.014563881,0.17773679,0.0046361117,0.003680057,0.08232876],"study_design_scores_gemma":[0.0002792273,0.00016226523,0.9692429,0.00020096269,0.00004892606,0.000023147899,0.000589694,0.0010642214,0.022078954,0.005904046,0.0003365642,0.00006911258],"about_ca_topic_score_codex":0.0062687686,"about_ca_topic_score_gemma":0.0006993147,"teacher_disagreement_score":0.26763505,"about_ca_system_score_codex":0.000007039197,"about_ca_system_score_gemma":0.00028964694,"threshold_uncertainty_score":0.9476545},"labels":[],"label_agreement":null},{"id":"W2726858476","doi":"10.1002/2017gl074312","title":"Mantle flow through a tear in the Nazca slab inferred from shear wave splitting","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Division of Earth Sciences; National Science Foundation of Sri Lanka; Colorado College; National Science Foundation","keywords":"Geology; Slab; Shear wave splitting; Mantle wedge; Lithosphere; Mantle (geology); Seismology; Geophysics; Seismic anisotropy; Slab window; Shear (geology); Subduction; Petrology; Tectonics; Oceanic crust","score_opus":0.07471687260724563,"score_gpt":0.3188396457844851,"score_spread":0.24412277317723946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2726858476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98425555,0.00004200544,0.00003335748,0.009588318,0.00034288786,0.00035320685,0.00019103874,0.000021846803,0.005171814],"genre_scores_gemma":[0.99683726,0.000023976674,0.00077463203,0.000884267,0.0012358283,0.000011448492,0.000102795624,0.000008683637,0.00012111023],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9967672,0.0005240447,0.00024322252,0.00048956793,0.0010583509,0.00091759075],"domain_scores_gemma":[0.9978973,0.0008798714,0.00008033689,0.0009737961,0.00005527511,0.000113370705],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011593879,0.00018450058,0.00029204242,0.00005373065,0.0009389909,0.00086211826,0.0011508117,0.00007765647,0.0006281012],"category_scores_gemma":[0.00043577253,0.00012379342,0.00009493981,0.0001684261,0.0004397699,0.00055517344,0.00015407364,0.00062996784,0.0016889492],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024611864,0.001327568,0.13027047,0.00054986094,0.00077316264,0.0062206658,0.04705164,0.004947566,0.3626114,0.011514759,0.21603902,0.2162327],"study_design_scores_gemma":[0.000771381,0.00014994295,0.943404,0.00009430494,0.000014157231,0.0000024453902,0.00036185788,0.008065854,0.0013990544,0.015804918,0.029570652,0.00036140092],"about_ca_topic_score_codex":0.06574629,"about_ca_topic_score_gemma":0.0010441216,"teacher_disagreement_score":0.81313354,"about_ca_system_score_codex":0.000008408272,"about_ca_system_score_gemma":0.000055903198,"threshold_uncertainty_score":0.99908835},"labels":[],"label_agreement":null},{"id":"W2729214174","doi":"10.1016/j.epsl.2017.06.032","title":"Invariant electrical resistivity of Co along the melting boundary","year":2017,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Electrical resistivity and conductivity; Condensed matter physics; Materials science; Inner core; Thermal conductivity; Thermodynamics; Physics; Composite material","score_opus":0.01256436548448274,"score_gpt":0.2123332309642576,"score_spread":0.19976886547977485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2729214174","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952702,0.00020253615,0.000020645926,0.0017742704,0.00035288482,0.00013093252,0.00012411225,0.000012582329,0.002111833],"genre_scores_gemma":[0.9987479,0.000041357227,0.0003556299,0.0006134341,0.00016873695,3.2877136e-7,0.00003831482,0.0000016740745,0.00003262478],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985718,0.000084932726,0.00019511786,0.0003110242,0.0004261736,0.0004109188],"domain_scores_gemma":[0.9989995,0.0002221675,0.0001898683,0.00043232727,0.000018159473,0.00013797199],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0013184685,0.00012618315,0.00019616414,0.00006059381,0.001738105,0.0004768961,0.00068465696,0.00003292693,0.0002568758],"category_scores_gemma":[0.00014213882,0.00008135001,0.000029865394,0.00010127689,0.0013349155,0.00055645173,0.000035796034,0.00014632761,0.000047123267],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009948233,0.000010503299,0.94439864,0.000032229524,0.000026597152,0.00008467708,0.00033866908,0.0005703811,0.028597653,0.0002363803,0.0015928644,0.02401193],"study_design_scores_gemma":[0.00012248404,0.000056695124,0.9911588,0.000013556354,0.00001153475,0.000021344244,0.000010848966,0.0019445742,0.0015668325,0.000087637476,0.0048847366,0.00012094974],"about_ca_topic_score_codex":0.010173807,"about_ca_topic_score_gemma":0.0016319604,"teacher_disagreement_score":0.04676017,"about_ca_system_score_codex":8.7313316e-7,"about_ca_system_score_gemma":0.00008556358,"threshold_uncertainty_score":0.9995615},"labels":[],"label_agreement":null},{"id":"W2729958651","doi":"10.1144/sp460.10","title":"Seismic tomography of the Arctic region: inferences for the thermal structure and evolution of the lithosphere","year":2017,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Lithosphere; Seismic tomography; Geology; Arctic; Tomography; Seismology; The arctic; Geophysics; Oceanography; Tectonics; Medicine; Mantle (geology); Radiology","score_opus":0.01597531136903439,"score_gpt":0.21559990975493648,"score_spread":0.1996245983859021,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2729958651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848151,0.00031305832,0.00018876481,0.01245709,0.00049471797,0.000488657,0.0001922151,0.000009081966,0.0010412969],"genre_scores_gemma":[0.99893796,0.00005768315,0.00013155643,0.00010556934,0.0005433343,0.000007639879,0.000009040732,0.0000013890459,0.00020579579],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99927783,0.00006456075,0.000178919,0.00015621229,0.00016966306,0.00015279581],"domain_scores_gemma":[0.9987873,0.00021354613,0.00032930204,0.000492984,0.00014679799,0.000030103607],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018780296,0.0000861783,0.00013761398,0.0000048809816,0.0011239068,0.000109376386,0.0007787335,0.00010012421,0.00036111765],"category_scores_gemma":[0.0001671212,0.000035527748,0.00019526086,0.00014012652,0.0009865232,0.00013932244,0.00009474663,0.000109793764,8.340418e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012470797,0.000015267726,0.9716972,0.000019797975,0.00004476843,1.0804306e-8,0.000256958,0.0004550802,0.000099354635,0.022430455,0.0020401427,0.002928477],"study_design_scores_gemma":[0.00011786892,0.000026845522,0.9634766,0.000006830651,0.000037779802,9.20751e-7,0.00010248426,0.00053059746,0.00008161892,0.025505349,0.010064183,0.000048938553],"about_ca_topic_score_codex":0.0015364952,"about_ca_topic_score_gemma":0.00081487396,"teacher_disagreement_score":0.014122874,"about_ca_system_score_codex":0.0000025806187,"about_ca_system_score_gemma":0.00005701419,"threshold_uncertainty_score":0.86442965},"labels":[],"label_agreement":null},{"id":"W2731031470","doi":"10.1002/2017jb014259","title":"Constant electrical resistivity of Ni along the melting boundary up to 9 GPa","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Condensed matter physics; Materials science; Thermodynamics; Fermi liquid theory; Mineralogy; Analytical Chemistry (journal); Chemistry; Superconductivity; Physics","score_opus":0.047081064033482285,"score_gpt":0.34383908644732436,"score_spread":0.2967580224138421,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2731031470","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99488074,0.0001420311,0.000046243942,0.0014156187,0.0005587885,0.00020536775,0.000078747515,0.0000050328144,0.0026674515],"genre_scores_gemma":[0.9981823,0.00008870328,0.00020932604,0.000049852417,0.0009865224,8.230143e-7,0.0000026226712,0.0000060441785,0.00047381278],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9963851,0.00055126916,0.00054950773,0.00022249289,0.0015982073,0.0006934014],"domain_scores_gemma":[0.9967105,0.0011628473,0.0004583655,0.0005642823,0.0007149413,0.0003890754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0038759797,0.00015009442,0.0005497407,0.00013482876,0.0011334345,0.00050424883,0.00114497,0.00006750268,0.00029133382],"category_scores_gemma":[0.002543284,0.000090486814,0.00018187368,0.00024331521,0.0006323605,0.00037706952,0.00014753814,0.00072508794,0.00013186653],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.010885625,0.0011337337,0.17035647,0.00055135606,0.0015980682,0.0018210664,0.005661798,0.001629004,0.22845525,0.019297142,0.051188312,0.5074222],"study_design_scores_gemma":[0.0005366262,0.0013167957,0.96470684,0.00015740718,0.000032654618,0.000026380854,0.0001110155,0.00077349425,0.011454711,0.0075987317,0.013102818,0.00018252344],"about_ca_topic_score_codex":0.0051442403,"about_ca_topic_score_gemma":0.0009892035,"teacher_disagreement_score":0.7943504,"about_ca_system_score_codex":0.0000069293187,"about_ca_system_score_gemma":0.0005301701,"threshold_uncertainty_score":0.8717576},"labels":[],"label_agreement":null},{"id":"W2735575745","doi":"10.1002/2017jb014150","title":"Detailed crustal thickness variations beneath the Illinois Basin area: Implications for crustal evolution of the midcontinent","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of Illinois at Urbana-Champaign; Lilly Endowment; Purdue University; Eli Lilly and Company; National Science Foundation","keywords":"Geology; Crust; Precambrian; Underplating; Rift; Proterozoic; Structural basin; Seismology; Paleontology; Subduction; Tectonics; Geomorphology","score_opus":0.048795533543013636,"score_gpt":0.3242039333479002,"score_spread":0.27540839980488657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2735575745","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98855245,0.000092445785,0.0019343945,0.006960145,0.0005730153,0.00056858954,0.00053135835,0.0000050679987,0.0007825185],"genre_scores_gemma":[0.9983633,0.000046383517,0.00032992268,0.000026859125,0.00086935726,0.00000758512,0.000008781995,0.000006075053,0.0003417048],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978221,0.00030928568,0.00048439388,0.00018123488,0.0007518256,0.00045114357],"domain_scores_gemma":[0.9963866,0.00091274705,0.0006180513,0.0006726474,0.0012513482,0.00015862248],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0017928453,0.00013295127,0.000354295,0.00007708534,0.0016686282,0.00031236923,0.0011770416,0.00007744829,0.00011686968],"category_scores_gemma":[0.0013616078,0.0000695731,0.00031741624,0.00018955738,0.0004902518,0.0003924771,0.00010712182,0.0004082414,0.000017326332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038768596,0.0027865807,0.4089047,0.0006601739,0.0023532102,0.000031207783,0.0059115496,0.022558685,0.19744301,0.25581005,0.023006676,0.0766573],"study_design_scores_gemma":[0.0004565374,0.00026167888,0.9670166,0.00005295592,0.00005928656,0.0000075187722,0.00010678507,0.0027902892,0.0012623662,0.02469641,0.00320285,0.000086768785],"about_ca_topic_score_codex":0.0019780234,"about_ca_topic_score_gemma":0.0012226283,"teacher_disagreement_score":0.55811185,"about_ca_system_score_codex":0.000011961645,"about_ca_system_score_gemma":0.0005159356,"threshold_uncertainty_score":0.99963105},"labels":[],"label_agreement":null},{"id":"W2737418392","doi":"10.1103/physrevlett.120.096001","title":"Synthesis of Xenon and Iron-Nickel Intermetallic Compounds at Earth’s Core Thermodynamic Conditions","year":2018,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); University of Saskatchewan","funders":"Laboratory Directed Research and Development; Army Research Office; Basic Energy Sciences; Natural Sciences and Engineering Research Council of Canada; Office of Science; Western Canada Research Grid; Defense Advanced Research Projects Agency; Chinese Academy of Sciences; National Natural Science Foundation of China; National Science Foundation; Compute Canada; U.S. Department of Energy; University of Saskatchewan","keywords":"Intermetallic; Nickel; Xenon; Noble gas; Raman spectroscopy; Materials science; Earth (classical element); Synchrotron; Chemical physics; Physical chemistry; Chemistry; Atomic physics; Physics; Metallurgy; Nuclear physics","score_opus":0.015436463484747394,"score_gpt":0.25222013303999713,"score_spread":0.23678366955524974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2737418392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966369,0.0008979913,0.0000073518054,0.00067688356,0.00012893733,0.00019153295,0.00021513361,0.000016745671,0.0012284864],"genre_scores_gemma":[0.9970491,0.0010453596,0.000050665334,0.0015879621,0.0001571819,0.0000049571922,0.00007357525,0.000005293475,0.00002593387],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99913514,0.00008261755,0.00020881454,0.00022027692,0.000160955,0.0001922025],"domain_scores_gemma":[0.99932337,0.00021327761,0.00012936439,0.00022835104,0.000025401978,0.000080252576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012300399,0.00014245119,0.00040946796,0.000022642616,0.000099403034,0.000019213292,0.00016478627,0.000010790409,0.00076076214],"category_scores_gemma":[0.000025380548,0.00010566465,0.00010012002,0.000088739296,0.00037143004,0.00009948227,0.000032876385,0.000051935604,0.00039861543],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007928087,0.0001734836,0.006712585,0.0035613938,0.00027270848,0.00001554746,0.00041898538,0.00006865794,0.9629605,0.0021957452,0.009508537,0.014032573],"study_design_scores_gemma":[0.0011138655,0.00110563,0.86968786,0.0072682896,0.0018146837,0.00006288792,0.00004131087,0.023281965,0.028856011,0.0043440103,0.060219016,0.0022044494],"about_ca_topic_score_codex":0.00019246037,"about_ca_topic_score_gemma":0.000087620734,"teacher_disagreement_score":0.9341045,"about_ca_system_score_codex":0.000002430192,"about_ca_system_score_gemma":0.000008020679,"threshold_uncertainty_score":0.83298117},"labels":[],"label_agreement":null},{"id":"W2738587265","doi":"10.1063/1.4985548","title":"Electronic transition in solid Nb at high pressure and temperature","year":2017,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Electrical resistivity and conductivity; Isothermal process; Extrapolation; Condensed matter physics; Thermal conductivity; Thermodynamics; Materials science; Transition temperature; Chemistry; Superconductivity; Physics","score_opus":0.004923562163513693,"score_gpt":0.19947317175393484,"score_spread":0.19454960959042114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2738587265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99843705,0.00018828976,0.000008482843,0.00007938455,0.00019341764,0.0000822315,0.000055691202,0.00000332923,0.0009521084],"genre_scores_gemma":[0.99909395,0.00016885954,0.000063753534,0.000060495913,0.00056212366,3.2119894e-7,0.000018618195,0.0000037895913,0.000028105793],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99931955,0.000016688595,0.00018751407,0.00010739567,0.00017183457,0.00019702865],"domain_scores_gemma":[0.9994772,0.000020098929,0.0002640908,0.00014583812,0.00003239599,0.000060385428],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018694019,0.000103351995,0.00025021404,0.000020951195,0.00018643201,0.00012752977,0.00017799174,0.00006462459,0.00007320132],"category_scores_gemma":[0.0000027200251,0.00007988792,0.00003689533,0.000027859183,0.000047661357,0.00023575797,0.000010973916,0.00018696407,0.000008811896],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0048150113,0.00039873467,0.009873443,0.0005504245,0.00091656944,0.00014860758,0.01175034,0.28451863,0.6327609,0.018612202,0.0029675604,0.03268758],"study_design_scores_gemma":[0.007258656,0.0010346252,0.67620367,0.00026714648,0.000744546,0.000069324524,0.0003801616,0.0041000275,0.13339105,0.16324043,0.012117892,0.0011924603],"about_ca_topic_score_codex":0.00012789588,"about_ca_topic_score_gemma":0.00014383347,"teacher_disagreement_score":0.6663302,"about_ca_system_score_codex":0.0000029697003,"about_ca_system_score_gemma":0.00004218039,"threshold_uncertainty_score":0.32577348},"labels":[],"label_agreement":null},{"id":"W2744798548","doi":"10.1016/j.tecto.2017.07.025","title":"Contrasting upper-mantle shear wave anisotropy across the transpressive Queen Charlotte margin","year":2017,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"Natural Resources Canada; Chinese Academy of Sciences","keywords":"Geology; Seismology; Subduction; Shear wave splitting; Slab; Mantle (geology); Crust; Shear (geology); Anisotropy; Transition zone; Plate tectonics; Geophysics; Tectonics; Petrology; Physics","score_opus":0.017353193213928447,"score_gpt":0.2392147653269069,"score_spread":0.22186157211297844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2744798548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99065995,0.00008212486,0.0003692934,0.000758712,0.0008816965,0.00036684467,0.00075143727,0.00008589995,0.006044022],"genre_scores_gemma":[0.9982788,0.000043332675,0.0002771991,0.00016419085,0.0008053444,0.000005922081,0.000055267432,0.000013071406,0.0003568918],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99853694,0.000069344285,0.0002226692,0.00033674334,0.00026442055,0.0005698552],"domain_scores_gemma":[0.99873775,0.00013231543,0.0002345488,0.0007316803,0.000060339025,0.00010337503],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00024202208,0.00023521778,0.00031320055,0.000011321291,0.001499502,0.00053619297,0.00067163963,0.00007654663,0.00048555064],"category_scores_gemma":[0.00003647686,0.00015800091,0.000116084244,0.000047872985,0.0002708473,0.0003961993,0.000048647504,0.00019469175,0.00041315425],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015103631,0.00049738615,0.123427,0.0007826795,0.0017045952,0.00074316765,0.028166998,0.006494555,0.20630936,0.035646327,0.0070896377,0.58762795],"study_design_scores_gemma":[0.0015117275,0.00026772488,0.9171465,0.00012992707,0.00013125343,0.000010969325,0.00038383753,0.006143365,0.040553723,0.012043424,0.020740887,0.0009366733],"about_ca_topic_score_codex":0.0061553,"about_ca_topic_score_gemma":0.00017861648,"teacher_disagreement_score":0.7937195,"about_ca_system_score_codex":0.0000037181435,"about_ca_system_score_gemma":0.00003863777,"threshold_uncertainty_score":0.9998004},"labels":[],"label_agreement":null},{"id":"W2746322906","doi":"10.1103/physrevlett.119.075302","title":"Melting and High <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:mrow><mml:mi>P</mml:mi><mml:mtext>−</mml:mtext><mml:mi>T</mml:mi></mml:mrow></mml:math> Transitions of Hydrogen up to 300 GPa","year":2017,"lang":"lv","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"U.S. Department of Energy","keywords":"Diamond anvil cell; Raman spectroscopy; Phase transition; Classification of discontinuities; Phonon; Physics; Materials science; Spectral line; Lattice (music); High pressure; Thermodynamics; Condensed matter physics; Optics; Quantum mechanics","score_opus":0.018248185257317563,"score_gpt":0.24871907950723948,"score_spread":0.23047089424992193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2746322906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9769886,0.002325832,0.00016475028,0.003404618,0.0013764848,0.000074435375,0.00076022214,0.000059696027,0.014845374],"genre_scores_gemma":[0.98982614,0.0031405697,0.0006031447,0.0037499294,0.0016459802,0.00018038749,0.0006783092,0.00013139794,0.00004416389],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99542737,0.00026739045,0.0009997,0.0010044102,0.0011331395,0.0011679765],"domain_scores_gemma":[0.9961532,0.0006557252,0.0010818238,0.001391336,0.000068435664,0.00064951944],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000990499,0.0005158389,0.00044399794,0.000109737884,0.0011550231,0.00073486345,0.0012134943,0.0003434761,0.015715104],"category_scores_gemma":[0.0004581165,0.0007440052,0.0009025437,0.00033698382,0.0008178601,0.00088202365,0.00046821235,0.0005962049,0.0017294396],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041287407,0.00023175919,0.000022680066,0.005073103,0.0010684222,0.0005158175,0.0022830404,0.001850339,0.021144481,0.9102973,0.049803115,0.00729709],"study_design_scores_gemma":[0.0023714558,0.0023397363,0.0014159988,0.010422322,0.005023334,0.00045110617,0.000569122,0.12361179,0.815819,0.001020609,0.033774856,0.0031806636],"about_ca_topic_score_codex":0.0022465142,"about_ca_topic_score_gemma":0.00046347053,"teacher_disagreement_score":0.90927666,"about_ca_system_score_codex":0.0000032115402,"about_ca_system_score_gemma":0.00028352463,"threshold_uncertainty_score":0.9995011},"labels":[],"label_agreement":null},{"id":"W2747139564","doi":"10.1016/j.cplett.2017.08.053","title":"X-ray induced synthesis of a novel material: Stable, doped solid CO at ambient conditions","year":2017,"lang":"en","type":"article","venue":"Chemical Physics Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); University of Saskatchewan","funders":"Western Economic Diversification Canada; Basic Energy Sciences; Canadian Light Source; Natural Sciences and Engineering Research Council of Canada; National Nuclear Security Administration; National Science Foundation; Canadian Institutes of Health Research; National Research Council; American Pain Society; National Research Council Canada; National Sleep Foundation; U.S. Department of Energy; University of Saskatchewan; University of Nevada, Las Vegas","keywords":"Doping; Oxalate; Carbon monoxide; Absorption (acoustics); Infrared; Materials science; X-ray; Ambient pressure; Irradiation; Strontium; Analytical Chemistry (journal); Chemistry; Inorganic chemistry; Optoelectronics; Organic chemistry; Optics; Catalysis; Physics","score_opus":0.02448579679616333,"score_gpt":0.24872298762112724,"score_spread":0.2242371908249639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2747139564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99613833,0.0000018378914,0.000041076928,0.0004173425,0.00047235942,0.00015578973,0.0018095676,0.000028196542,0.00093550957],"genre_scores_gemma":[0.9987485,0.0000028370791,0.00022524523,0.0002890714,0.0003701754,0.0000075932626,0.00032112116,0.000009662577,0.000025794796],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.998852,0.00002344837,0.00025851387,0.00028883046,0.00025084877,0.00032635737],"domain_scores_gemma":[0.9989143,0.00010154077,0.00028911245,0.000535993,0.000038898717,0.00012014262],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010496248,0.00018282566,0.0003683373,0.000018827475,0.00026963346,0.00013234821,0.00046101672,0.00006752559,0.00054670335],"category_scores_gemma":[0.000044551594,0.00016114923,0.00009546274,0.000038346807,0.00020097617,0.00023661333,0.000062029285,0.00007471882,0.00012586146],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038545426,0.000055208,0.0006447596,0.00004481071,0.00004885986,0.0000032816579,0.000050288494,0.00016644545,0.9964321,0.000078205405,0.0023015519,0.00013591383],"study_design_scores_gemma":[0.00026968092,0.000014003987,0.013337665,0.00003712108,0.00004447245,8.4622604e-7,0.0000054832412,0.00013391425,0.985374,0.00014130081,0.00043370994,0.00020780764],"about_ca_topic_score_codex":0.0008788004,"about_ca_topic_score_gemma":0.00001046981,"teacher_disagreement_score":0.012692906,"about_ca_system_score_codex":0.000007996897,"about_ca_system_score_gemma":0.000020993186,"threshold_uncertainty_score":0.65714747},"labels":[],"label_agreement":null},{"id":"W2752555207","doi":"10.1039/c7ja00017k","title":"Effects of H<sub>2</sub>O- and O<sub>2</sub>-containing He carrier gases on the <sup>206</sup>Pb/<sup>238</sup>U system bias and down-hole fractionation in LA-ICPMS of zircon","year":2017,"lang":"en","type":"article","venue":"Journal of Analytical Atomic Spectrometry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Analytical Chemistry (journal); Fractionation; Chemistry; Isotope; Radiochemistry; Physics; Nuclear physics","score_opus":0.010473877294846666,"score_gpt":0.22185128724197803,"score_spread":0.21137740994713136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2752555207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983258,0.00041001724,0.00008809149,0.0002952749,0.00014022514,0.0001966645,0.000067673536,0.000008325669,0.00046791535],"genre_scores_gemma":[0.99923426,0.00031048706,0.000077132834,0.000045033652,0.00030766483,0.0000010812631,0.0000060286397,0.0000109257,0.0000073720507],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99766666,0.0003244642,0.0007896571,0.000286861,0.00059618766,0.00033618792],"domain_scores_gemma":[0.9966796,0.0018252018,0.000867679,0.00028973792,0.0001371407,0.0002006377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016188297,0.00025572896,0.00080686924,0.00043028028,0.00021463209,0.00020276244,0.00031641647,0.00016722608,0.000048582293],"category_scores_gemma":[0.000748043,0.00017400933,0.00016696009,0.00024607536,0.00027669704,0.00042775137,0.000048408972,0.00041179016,0.000010125079],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036490865,0.00058958994,0.2514785,0.00212263,0.0022414208,0.00082401576,0.0020945556,0.014998026,0.69046104,0.012973745,0.0012464143,0.017320994],"study_design_scores_gemma":[0.0024079832,0.0012643572,0.5551704,0.0010937337,0.000504062,0.00021340139,0.0010515553,0.037967604,0.3977778,0.001968653,0.00015428216,0.00042613636],"about_ca_topic_score_codex":0.00041334398,"about_ca_topic_score_gemma":0.000060534236,"teacher_disagreement_score":0.30369195,"about_ca_system_score_codex":0.000034611166,"about_ca_system_score_gemma":0.00010953688,"threshold_uncertainty_score":0.7095895},"labels":[],"label_agreement":null},{"id":"W2757809215","doi":"","title":"Water and Metasomatism in the Slave Cratonic Lithosphere (Canada): An FTIR Study","year":2017,"lang":"en","type":"article","venue":"NASA STI Repository (National Aeronautics and Space Administration)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Metasomatism; Craton; Geology; Kimberlite; Xenolith; Olivine; Geochemistry; Mantle (geology); Peridotite; Asthenosphere; Pyroxene; Lithosphere; Trace element; Partial melting; Paleontology","score_opus":0.014447745085128996,"score_gpt":0.24206520983678792,"score_spread":0.22761746475165892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2757809215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99485946,0.00009193927,0.0000047043804,0.0014902271,0.00026108924,0.00027248403,0.000057383757,0.0000072456323,0.0029554437],"genre_scores_gemma":[0.9990385,0.000010989093,0.00021499369,0.00010435701,0.00012842943,0.000006648723,0.00008290345,0.0000033534202,0.0004098327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998727,0.00012330078,0.00022908326,0.00026464032,0.0004839793,0.00017194523],"domain_scores_gemma":[0.99938303,0.00009080585,0.000111473186,0.00024826155,0.000079870086,0.00008658616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043873186,0.00014033995,0.000157195,0.00001665392,0.0008863392,0.0006815787,0.00021900077,0.00004827767,0.00006830742],"category_scores_gemma":[0.00003059971,0.000088847795,0.000014680063,0.000023241984,0.00009816213,0.00037034624,0.000022088854,0.00009723897,0.0000029211978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002298167,0.00063828804,0.95492536,0.000102091384,0.0002438419,0.0005035043,0.004480115,0.0005132471,0.0035051939,0.030791568,0.0008645037,0.0032024484],"study_design_scores_gemma":[0.00030398267,0.00028594732,0.99389386,0.0000064753935,0.00002811347,0.00003477659,0.00044774407,0.00082864665,0.00042395227,0.0013773452,0.002226907,0.0001422296],"about_ca_topic_score_codex":0.030822353,"about_ca_topic_score_gemma":0.31573027,"teacher_disagreement_score":0.28490794,"about_ca_system_score_codex":0.000007197976,"about_ca_system_score_gemma":0.0002677163,"threshold_uncertainty_score":0.9756315},"labels":[],"label_agreement":null},{"id":"W2758616366","doi":"","title":"The Interaction Between Supercontinent Cycles and Compositional Variations in the Deep Mantle","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Supercontinent; Earth science; Geophysics; Paleontology; Craton; Tectonics","score_opus":0.02363793294911021,"score_gpt":0.2501215858742155,"score_spread":0.2264836529251053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2758616366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940925,0.00021345614,0.000060369282,0.0015839767,0.0002669678,0.00010044811,0.000026410222,0.000009590718,0.0036462601],"genre_scores_gemma":[0.9992729,0.000017573791,0.0002560317,0.000062605235,0.0002860122,0.0000021865205,0.00008137403,0.0000015688194,0.000019766423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932694,0.00015662042,0.00014047069,0.00009437715,0.00015160574,0.00012998791],"domain_scores_gemma":[0.9994424,0.00036530884,0.000044625052,0.0000790713,0.000030141753,0.00003844978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008028738,0.000058499943,0.00007342262,0.00001841932,0.00019468504,0.00016242532,0.00012162118,0.000023094783,0.000009457533],"category_scores_gemma":[0.0000469932,0.00003308393,0.000013437794,0.000047613114,0.000029306195,0.00013962638,0.000014601272,0.00006556792,0.00005139998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021651704,0.00001511474,0.9882074,0.000007365791,0.000021920365,0.0000034017955,0.0026513995,0.0011992311,0.00023981853,0.0011760002,0.0016854575,0.004771237],"study_design_scores_gemma":[0.00021824529,0.000036585,0.9783134,0.00002167998,0.000018576498,0.0000059934105,0.00130503,0.004738142,0.00004137948,0.00341784,0.011788406,0.00009474401],"about_ca_topic_score_codex":0.009511264,"about_ca_topic_score_gemma":0.010392297,"teacher_disagreement_score":0.010102949,"about_ca_system_score_codex":0.000002380389,"about_ca_system_score_gemma":0.000012127283,"threshold_uncertainty_score":0.9970845},"labels":[],"label_agreement":null},{"id":"W2763686379","doi":"10.15273/ijge.2017.03.008","title":"Estimation of Quality Factor (Qβ) Using Accelerograms of Ahar-Varzaghan Earthquakes, Northwestern Iran","year":2017,"lang":"en","type":"article","venue":"International Journal of Georesources and Environment","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"International Institute of Earthquake Engineering and Seismology","keywords":"Aftershock; Seismic moment; Seismology; Attenuation; Source model; Scaling; Geology; Inversion (geology); Strong ground motion; Physics; Quality (philosophy); Magnitude (astronomy); Ground motion; Mathematics; Computational physics; Geometry; Fault (geology); Optics","score_opus":0.04120405298713877,"score_gpt":0.27577002862438876,"score_spread":0.23456597563724998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763686379","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998737,0.00013596375,0.00041461442,0.0000978531,0.0002862201,0.000053010684,0.00018999517,0.0000013398981,0.00008400804],"genre_scores_gemma":[0.9988411,0.00019173573,0.00076828257,0.000011922856,0.00014863646,1.4746705e-7,0.00001726957,0.000002644536,0.000018251605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99884826,0.000041372994,0.00046145264,0.00009434136,0.00045208907,0.00010247513],"domain_scores_gemma":[0.9986966,0.00004097165,0.0010206487,0.0001355654,0.00003333497,0.00007284396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029481354,0.00009033194,0.00022938137,0.000051337916,0.00007686202,0.00009246104,0.00033572607,0.00003711403,0.00034938348],"category_scores_gemma":[0.000017872117,0.00006976242,0.000078914316,0.000008706865,0.00014689342,0.00025082726,0.000041673426,0.000055415327,0.0000028582788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023513615,0.00009619248,0.6730402,0.000043786924,0.00025307626,0.0000139949825,0.0012789551,0.043782175,0.0029765014,0.00005768108,0.0000061087126,0.2782162],"study_design_scores_gemma":[0.0003917249,0.00011245909,0.9936809,0.000049174596,0.000026203219,0.000011861184,0.0000774611,0.0020818026,0.0017994038,0.00033522368,0.0013583077,0.00007548052],"about_ca_topic_score_codex":0.0028238692,"about_ca_topic_score_gemma":0.0001244621,"teacher_disagreement_score":0.3206407,"about_ca_system_score_codex":0.000004292564,"about_ca_system_score_gemma":0.000009158682,"threshold_uncertainty_score":0.4268864},"labels":[],"label_agreement":null},{"id":"W2765718194","doi":"10.1093/gji/ggx479","title":"Crust and uppermost-mantle structure of Greenland and the Northwest Atlantic from Rayleigh wave group velocity tomography","year":2017,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Lithosphere; Crust; Mantle (geology); Seismic tomography; Continental margin; Continental crust; Seismology; Tectonics; Geophysics","score_opus":0.008002158711329201,"score_gpt":0.20346357301364518,"score_spread":0.19546141430231598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765718194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99753803,0.00010711764,0.00004164321,0.00060795364,0.0007658002,0.00007075033,0.000570293,0.000004111263,0.0002942825],"genre_scores_gemma":[0.9985186,0.00014752222,0.00021815338,0.00007657152,0.0009079099,2.742366e-7,0.00010158899,0.0000030813399,0.00002629389],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990972,0.000060907223,0.00021673455,0.0001684762,0.0003083534,0.00014828674],"domain_scores_gemma":[0.999195,0.00017520685,0.00028608963,0.00016290115,0.00008235433,0.00009843966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012844203,0.00012611224,0.0002439062,0.000033892313,0.00042071156,0.00039944018,0.00033869626,0.000048528178,0.00047309362],"category_scores_gemma":[0.000040466875,0.000073926596,0.00007758599,0.000023242506,0.00042218453,0.0002943034,0.00006998039,0.0001853377,0.000005964403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009751788,0.00006409204,0.94711185,0.000026702754,0.0006949282,0.000084528896,0.00077071396,0.000049364255,0.0074326466,0.006409454,0.0003951478,0.035985418],"study_design_scores_gemma":[0.0009745902,0.00004472334,0.97361284,0.000026603737,0.00004545494,0.000040555664,0.000021840146,0.001214599,0.00022259391,0.023171542,0.00052908994,0.00009558041],"about_ca_topic_score_codex":0.012960854,"about_ca_topic_score_gemma":0.0020931223,"teacher_disagreement_score":0.035889838,"about_ca_system_score_codex":0.000001380265,"about_ca_system_score_gemma":0.000013744322,"threshold_uncertainty_score":0.99361193},"labels":[],"label_agreement":null},{"id":"W2765981451","doi":"10.2138/am-2017-6103","title":"Defect contributions to the heat capacities and stabilities of some chain, ring, and sheet silicates, with implications for mantle minerals","year":2017,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Western University","funders":"","keywords":"Enstatite; Alkali metal; Diopside; Chemistry; Dissociation (chemistry); Bond strength; Bond-dissociation energy; Oxygen; Natural bond orbital; Crystallography; Inorganic chemistry; Mineralogy; Physical chemistry; Meteorite; Computational chemistry; Density functional theory; Organic chemistry","score_opus":0.014670235034863753,"score_gpt":0.2577620342402911,"score_spread":0.24309179920542734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765981451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98294085,0.00035166342,0.00012528239,0.0112645505,0.00004497876,0.00039954734,0.004358128,0.000012333049,0.00050269265],"genre_scores_gemma":[0.9986645,0.000098863624,0.00045354286,0.00034763504,0.00008222347,0.000036752073,0.00008603663,0.0000036064218,0.00022682402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993766,0.000031563814,0.00013349044,0.00019522298,0.000057233112,0.00020590557],"domain_scores_gemma":[0.99917805,0.00021715595,0.00010002305,0.00034727334,0.000078748315,0.00007873304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015116627,0.00010754628,0.00023871535,0.0000248579,0.00046303298,0.00011519057,0.00016955518,0.0000139480435,0.000014756617],"category_scores_gemma":[0.000117384945,0.000064759915,0.000028379536,0.000034707587,0.0012842811,0.00011419365,0.000024142988,0.00002876493,0.0000017820523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005100456,0.00011005815,0.7675944,0.00027039947,0.00043264247,0.0000035049732,0.0037358108,0.0019029713,0.08963066,0.087671295,0.035722375,0.012415848],"study_design_scores_gemma":[0.0003979261,0.0007397349,0.9667674,0.000021445176,0.000070934744,0.000012527886,0.0006152804,0.00022766614,0.00091544323,0.0027577826,0.027222069,0.00025184077],"about_ca_topic_score_codex":0.03590088,"about_ca_topic_score_gemma":0.0107739195,"teacher_disagreement_score":0.19917296,"about_ca_system_score_codex":0.0000020151729,"about_ca_system_score_gemma":0.00002148999,"threshold_uncertainty_score":0.9705191},"labels":[],"label_agreement":null},{"id":"W2766985662","doi":"10.1002/2017gl075049","title":"Constraints on Inner Core Anisotropy Using Array Observations of P′P′","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; National Sleep Foundation; National Science Foundation","keywords":"Anisotropy; Inner core; Core (optical fiber); Geology; Polar; Rotation (mathematics); Geodesy; Sampling (signal processing); Geophysics; Phase (matter); Latitude; Physics; Computational physics; Geometry; Optics; Mathematics; Astronomy","score_opus":0.1509275144354192,"score_gpt":0.3458538752737842,"score_spread":0.19492636083836498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766985662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99591476,0.0000047633516,0.000084698484,0.0014181967,0.00031434224,0.00019465774,0.00022265577,0.000013422631,0.0018325119],"genre_scores_gemma":[0.99824405,0.000004911531,0.0009916212,0.00022195755,0.00040914328,0.0000017974787,0.00004389915,0.000005755808,0.00007688539],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9981523,0.00012456102,0.00019413156,0.0002967029,0.00071797246,0.00051429914],"domain_scores_gemma":[0.99863887,0.0003142869,0.00012417964,0.0006244245,0.00014263135,0.00015563618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041777667,0.00012620582,0.00024341546,0.00007879766,0.0007081272,0.00018515042,0.0006178163,0.000052124757,0.000627792],"category_scores_gemma":[0.00029686588,0.00010227803,0.00007698585,0.000120051685,0.0010471565,0.00025672975,0.000045282737,0.0002533378,0.00030019888],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096884854,0.00006762897,0.014027591,0.00003761972,0.000045168246,0.00003274668,0.00012968517,0.00061594293,0.9735777,0.006110617,0.0020615985,0.0031968222],"study_design_scores_gemma":[0.0004696726,0.00025092572,0.9725918,0.00009356199,0.000014707193,0.000001356669,0.000051159324,0.0013867782,0.018290354,0.004502463,0.0021055527,0.00024165871],"about_ca_topic_score_codex":0.005102302,"about_ca_topic_score_gemma":0.000088639084,"teacher_disagreement_score":0.9585642,"about_ca_system_score_codex":0.0000063429943,"about_ca_system_score_gemma":0.00007836748,"threshold_uncertainty_score":0.7713188},"labels":[],"label_agreement":null},{"id":"W2767779197","doi":"10.1038/s41467-017-01611-3","title":"Drip tectonics and the enigmatic uplift of the Central Anatolian Plateau","year":2017,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":154,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Istanbul Teknik Üniversitesi; Natural Sciences and Engineering Research Council of Canada; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu; Dalhousie University","keywords":"Lithosphere; Geology; Plateau (mathematics); Context (archaeology); Tectonics; Volcanism; Subsidence; Seismology; Geomorphology; Paleontology; Structural basin","score_opus":0.010312163187124579,"score_gpt":0.2412672477961664,"score_spread":0.23095508460904182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767779197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93847126,0.009038001,0.000009729884,0.025092794,0.0009961446,0.0006147143,0.00029345608,0.000025434036,0.025458453],"genre_scores_gemma":[0.99876374,0.0007155502,0.00025793933,0.00013733566,0.000026174432,0.0000016486107,0.00001748896,0.0000018115902,0.000078295576],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9994487,0.00012406668,0.00012764712,0.0000712632,0.00011040925,0.0001179037],"domain_scores_gemma":[0.9976455,0.00023365382,0.00017397695,0.0018803807,0.00003512758,0.00003138114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025883663,0.00006368253,0.00012267637,0.000010572086,0.0010297805,0.00011475234,0.0017373504,0.00008373984,0.00004712721],"category_scores_gemma":[0.00013167101,0.00003175917,0.00004417086,0.00004373904,0.0005571258,0.000085797765,0.0001253623,0.00028616795,0.0000065647605],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001072444,0.00006612861,0.4383185,0.00010320898,0.00028296505,0.00000125167,0.0052703335,0.00027673706,0.0007893403,0.52942973,0.006354462,0.01900008],"study_design_scores_gemma":[0.0003546044,0.0000061493038,0.9537879,0.000025928006,0.000046004494,0.0000029486819,0.000051670693,0.0020358434,0.0002874517,0.008666513,0.03466338,0.0000715772],"about_ca_topic_score_codex":0.0014321648,"about_ca_topic_score_gemma":0.007853,"teacher_disagreement_score":0.5207632,"about_ca_system_score_codex":9.413704e-7,"about_ca_system_score_gemma":0.000030763065,"threshold_uncertainty_score":0.79203427},"labels":[],"label_agreement":null},{"id":"W2768932471","doi":"10.1111/maps.12997","title":"Quartz–coesite–stishovite relations in shocked metaquartzites from the Vredefort impact structure, South Africa","year":2017,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Stishovite; Coesite; Quartz; Geology; Mineralogy; Geochemistry; Eclogite","score_opus":0.015884882406153825,"score_gpt":0.22883525131831997,"score_spread":0.21295036891216615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768932471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99261963,0.0008716643,0.00002701211,0.00020710024,0.00066140306,0.00019654764,0.003998944,0.000017115208,0.0014005521],"genre_scores_gemma":[0.998037,0.000036359903,0.001227288,0.00006648017,0.00020108062,7.788764e-7,0.00036227386,0.000003639044,0.00006514658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981999,0.00008453157,0.00028379905,0.0004690836,0.00045140865,0.0005113096],"domain_scores_gemma":[0.9985347,0.00040380462,0.00015679795,0.00065699394,0.000043668184,0.00020405294],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000766228,0.00021536658,0.0002894613,0.000093792194,0.001398659,0.0010040791,0.00088213966,0.00007263986,0.0009939199],"category_scores_gemma":[0.00020808441,0.00013523457,0.000048646623,0.00019984522,0.00068734144,0.00072731165,0.00005584789,0.00019730051,0.00007094947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004363092,0.000009664753,0.98950475,0.000006391873,0.000032189382,0.000034679837,0.0015098706,0.001591717,0.0021461973,0.00045366722,0.00027369484,0.0043935557],"study_design_scores_gemma":[0.00019085946,0.000102519916,0.98150814,0.000016371,0.000040422547,0.0000062633,0.00011601505,0.006502487,0.00014498094,0.009322068,0.0018363855,0.00021349701],"about_ca_topic_score_codex":0.01703959,"about_ca_topic_score_gemma":0.006386737,"teacher_disagreement_score":0.010652853,"about_ca_system_score_codex":0.000004411412,"about_ca_system_score_gemma":0.000116025316,"threshold_uncertainty_score":0.9999193},"labels":[],"label_agreement":null},{"id":"W2769152536","doi":"10.1021/acsearthspacechem.7b00100","title":"Structures and Transport Properties of CaCO<sub>3</sub> Melts under Earth’s Mantle Conditions","year":2017,"lang":"en","type":"article","venue":"ACS Earth and Space Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Science Foundation of Zhejiang Province; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Silicate; Carbonate; Mantle (geology); Calcium carbonate; Viscosity; Molecular dynamics; Diffusion; Ion; Mineralogy; Earth (classical element); Materials science; Chemical physics; Thermodynamics; Chemistry; Geology; Geochemistry; Physics; Composite material; Metallurgy; Organic chemistry","score_opus":0.011106988901301563,"score_gpt":0.19329358990927922,"score_spread":0.18218660100797765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2769152536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99727356,0.0005419983,0.000002303096,0.00018860772,0.000083917206,0.000080388905,0.00027736343,0.000014159553,0.0015377183],"genre_scores_gemma":[0.9991431,0.000311907,0.000031232765,0.00002628708,0.00008758322,9.557235e-7,0.00006295619,0.0000039773972,0.00033196874],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99934065,0.000009481554,0.00012440051,0.0002052781,0.00012930072,0.00019089243],"domain_scores_gemma":[0.99948853,0.000014296294,0.00010145219,0.00024050663,0.00003427333,0.00012094093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006691966,0.00013224063,0.00020372788,0.000011041539,0.00030662655,0.000088607325,0.00011647919,0.000085585365,0.00014400293],"category_scores_gemma":[0.000014342292,0.00010441821,0.000027541333,0.000016863718,0.00029678977,0.00016650095,0.000015616586,0.00007434111,0.000005475779],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026599095,0.000006365454,0.01673987,0.00017920807,0.00003007862,0.0000069142875,0.00013131097,0.000047826416,0.9822047,0.00007521893,0.000060383885,0.0004915209],"study_design_scores_gemma":[0.00019220704,0.000015044307,0.3067097,0.000028855226,0.000022594397,0.000009021955,0.0000667588,0.000015768659,0.6920645,0.00035729338,0.00041094577,0.000107254025],"about_ca_topic_score_codex":0.0006727036,"about_ca_topic_score_gemma":0.0006058765,"teacher_disagreement_score":0.29014015,"about_ca_system_score_codex":3.06155e-7,"about_ca_system_score_gemma":0.00003714409,"threshold_uncertainty_score":0.4258051},"labels":[],"label_agreement":null},{"id":"W2773329245","doi":"10.1002/chem.201705321","title":"Superconducting Hydrogen Sulfide","year":2017,"lang":"en","type":"review","venue":"Chemistry - A European Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Milestone; Superconductivity; Hydrogen sulfide; Sulfide; Cuprate; Room-temperature superconductor; Hydrogen; High-temperature superconductivity; Physics; Condensed matter physics; Materials science; Quantum mechanics; History; Sulfur; Metallurgy","score_opus":0.10498548092234283,"score_gpt":0.29525808662756586,"score_spread":0.19027260570522303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2773329245","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002146991,0.96966434,0.0000017603304,0.000010446687,0.00079684757,0.00009126898,0.0001963273,0.00003320208,0.027058825],"genre_scores_gemma":[0.00044151797,0.99184144,0.00009790325,0.000011236317,0.004324871,3.672272e-7,0.0002649455,0.00003385751,0.0029838393],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978168,0.00035720284,0.0007021713,0.00038024227,0.0002678529,0.00047574728],"domain_scores_gemma":[0.99811184,0.00006270402,0.0008152133,0.0005888419,0.00005264488,0.0003687776],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013122562,0.00043305475,0.0010784244,0.00003379402,0.0006544459,0.000816478,0.0013278469,0.00009930094,0.0054374347],"category_scores_gemma":[0.00015439784,0.0003204294,0.00048741206,0.000051464456,0.000099220866,0.00022825596,0.00007087006,0.0005723766,0.001776978],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000021141698,0.0000069097473,0.000009835388,0.002759234,0.00014603137,0.0011206721,0.00003354089,0.0000050893477,0.000111642694,4.6977263e-7,0.0014656482,0.9943388],"study_design_scores_gemma":[0.00009998306,0.000012595087,0.000007912783,0.0029283054,0.0002850609,0.0019740092,0.000010493088,0.0000051181205,0.00002965284,0.000016240616,0.994253,0.0003776315],"about_ca_topic_score_codex":0.000023274895,"about_ca_topic_score_gemma":0.000001264199,"teacher_disagreement_score":0.99396116,"about_ca_system_score_codex":0.0000073592046,"about_ca_system_score_gemma":0.00023508255,"threshold_uncertainty_score":0.9999248},"labels":[],"label_agreement":null},{"id":"W2773468726","doi":"10.1002/9781119227250.ch7","title":"Strength and Deformation of Zircon at Crustal and Mantle Pressures","year":2017,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; Western University","funders":"","keywords":"Zircon; Differential stress; Electron backscatter diffraction; Geology; Microstructure; Crystal twinning; Misorientation; Deformation (meteorology); Materials science; Mineralogy; Composite material; Geochemistry; Grain boundary","score_opus":0.00656798461060192,"score_gpt":0.1980761629600837,"score_spread":0.19150817834948178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2773468726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6675572,0.0042498372,0.000011331741,0.000035718855,0.000774828,0.0006232691,0.0023960236,0.00011260278,0.3242392],"genre_scores_gemma":[0.95260864,0.0013778334,0.000329732,0.000016889366,0.00044564652,0.00000401661,0.0004245773,0.000043398617,0.04474926],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9991943,0.000025114134,0.00014310043,0.00025574834,0.0001755642,0.00020614508],"domain_scores_gemma":[0.9993104,0.000029747864,0.00027274954,0.00027255295,0.000013800734,0.000100785284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005679687,0.00020923001,0.0003867465,0.00009915298,0.00011129429,0.000067127185,0.00014819548,0.00015713557,0.0006971019],"category_scores_gemma":[0.000005382251,0.0001652174,0.000060488608,0.000035940204,0.00024088117,0.00011297921,0.00005639831,0.000076634846,0.00003689568],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070770754,0.00039600173,0.09588738,0.005489344,0.0019081444,0.0000626746,0.0017482106,0.000062830164,0.006719505,0.004196831,0.53745866,0.3453627],"study_design_scores_gemma":[0.000807281,0.0003358293,0.5174667,0.0002936369,0.0002707711,0.000005964447,0.000031934735,0.00034406641,0.0014838675,0.0027217306,0.4755083,0.0007299064],"about_ca_topic_score_codex":0.0065109106,"about_ca_topic_score_gemma":0.0015521564,"teacher_disagreement_score":0.42157936,"about_ca_system_score_codex":5.644216e-7,"about_ca_system_score_gemma":0.000009315157,"threshold_uncertainty_score":0.98425925},"labels":[],"label_agreement":null},{"id":"W2783221544","doi":"10.1002/2017jb014846","title":"Inverse Problems in Geodynamics Using Machine Learning Algorithms","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Directorate for Computer and Information Science and Engineering; National Sleep Foundation; National Science Foundation","keywords":"Geodynamics; Geophysics; Algorithm; Machine learning; Mantle convection; Mantle (geology); Artificial intelligence; Geology; Computer science; Inverse; Mathematics; Geometry","score_opus":0.054135131629005795,"score_gpt":0.3293522305349888,"score_spread":0.275217098905983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783221544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830395,0.00008550337,0.00016356113,0.000096988246,0.00038642724,0.00014690675,0.00002456351,0.000008912233,0.00078321365],"genre_scores_gemma":[0.9964669,0.00012972044,0.0016104926,0.000030069203,0.0014289675,3.7853272e-7,0.0000114867735,0.00000938428,0.00031259714],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9969489,0.0005198306,0.00050866907,0.00022697341,0.0010588297,0.0007368272],"domain_scores_gemma":[0.9984718,0.000288957,0.00022429031,0.00017134276,0.0005338525,0.0003097614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022776567,0.00015895051,0.00043953446,0.00034103508,0.0002613945,0.00017137962,0.00040159115,0.0000891139,0.0006060855],"category_scores_gemma":[0.0003271852,0.00012190123,0.00011042717,0.00068019057,0.0003407284,0.0004716945,0.000069959766,0.00093162275,0.0002984566],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024342455,0.0018668118,0.41344804,0.00070856535,0.00073581113,0.00207297,0.009630773,0.21963395,0.21780145,0.0012823656,0.0011878908,0.12919714],"study_design_scores_gemma":[0.0012701228,0.0027789788,0.16812977,0.0002622736,0.000023372986,0.00006705758,0.00019498139,0.80738837,0.002553643,0.00787064,0.009099136,0.00036166568],"about_ca_topic_score_codex":0.008120667,"about_ca_topic_score_gemma":0.002908287,"teacher_disagreement_score":0.5877544,"about_ca_system_score_codex":0.000012767048,"about_ca_system_score_gemma":0.00024956683,"threshold_uncertainty_score":0.9984844},"labels":[],"label_agreement":null},{"id":"W2785097917","doi":"10.1038/s41561-017-0055-7","title":"Oxidized iron in garnets from the mantle transition zone","year":2018,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science and Technology Facilities Council; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; Natural Environment Research Council; Sight Research UK","keywords":"Mantle (geology); Transition zone; Geology; Oxidation state; Mineral redox buffer; Ringwoodite; Oxidizing agent; Mineralogy; Mössbauer spectroscopy; Oxygen; Geochemistry; Metal; Crystallography; Materials science; Chemistry","score_opus":0.005289262716376684,"score_gpt":0.20670154052971088,"score_spread":0.20141227781333418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2785097917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99599534,0.0004016752,0.00017030792,0.00090475957,0.0011603235,0.0001308564,0.00014862085,0.000022582304,0.00106555],"genre_scores_gemma":[0.99726367,0.000022763881,0.00055353966,0.0015110461,0.00042443984,9.606346e-7,0.000055762175,0.0000018324679,0.00016601072],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99894917,0.00007831418,0.00012641323,0.0002884323,0.0002870639,0.00027059828],"domain_scores_gemma":[0.9995559,0.00010483171,0.000045054076,0.00021325119,0.000029792993,0.00005119033],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038030837,0.00009614819,0.000113265065,0.000028911025,0.0001796992,0.00008331076,0.0003834475,0.000119751356,0.0014239881],"category_scores_gemma":[0.00003425527,0.00005947655,0.000025146712,0.0002946231,0.00019698507,0.0001967401,0.00001220354,0.00019524388,0.00030211933],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017092333,0.00047519515,0.18581977,0.0000906854,0.00006387916,0.0002860218,0.026248643,0.001669844,0.60536784,0.00792864,0.04309343,0.12724683],"study_design_scores_gemma":[0.00032972847,0.00008204246,0.96466917,0.00002484092,0.000008151459,0.0000029305413,0.00008216455,0.0021444287,0.0023613065,0.0018194804,0.028311875,0.00016385867],"about_ca_topic_score_codex":0.00931847,"about_ca_topic_score_gemma":0.011383531,"teacher_disagreement_score":0.7788494,"about_ca_system_score_codex":0.0000022123781,"about_ca_system_score_gemma":0.00003073916,"threshold_uncertainty_score":0.99948883},"labels":[],"label_agreement":null},{"id":"W2788237576","doi":"10.1103/physrevlett.121.047002","title":"Detecting Superconductivity in the High Pressure Hydrides and Metallic Hydrogen from Optical Properties","year":2018,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph; McMaster University; Canadian Institute for Advanced Research","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Superconductivity; Metallic hydrogen; Materials science; Condensed matter physics; Context (archaeology); Phonon; Hydrogen; Photon energy; Photon; Reflectivity; Absorption (acoustics); Band gap; Metal; Atomic physics; Physics; Optics","score_opus":0.024556492138177642,"score_gpt":0.23305989386796133,"score_spread":0.20850340172978368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788237576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905374,0.0062516653,0.0000032516705,0.0026939826,0.00009127527,0.00030333785,0.000027271559,0.0000174395,0.00007437554],"genre_scores_gemma":[0.9964115,0.0005309234,0.00007636379,0.0024463814,0.00050858513,0.000009211976,0.000010344676,0.0000042551305,0.0000024443098],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988134,0.0002564779,0.00016835131,0.00029176488,0.00022481295,0.00024519832],"domain_scores_gemma":[0.99944854,0.00020628078,0.00004452157,0.00023145702,0.000014649455,0.00005452562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003468887,0.00015368171,0.000345977,0.000013832347,0.00011036286,0.00007966085,0.00021905627,0.00001257818,0.00014008122],"category_scores_gemma":[0.000079242614,0.000084805026,0.000057421825,0.00011613365,0.00021472557,0.0002676544,0.000028479279,0.00013047016,0.00011489892],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007919413,0.00017929745,0.01106323,0.0017459977,0.00032934733,0.000043940672,0.0031039948,0.0002776611,0.9497288,0.0007334977,0.0008351776,0.03187987],"study_design_scores_gemma":[0.0016891902,0.00095857354,0.69990754,0.0057145543,0.0025934677,0.000052023533,0.0002937878,0.012686205,0.18415481,0.019399151,0.06940067,0.0031500536],"about_ca_topic_score_codex":0.0032970542,"about_ca_topic_score_gemma":0.00024131306,"teacher_disagreement_score":0.765574,"about_ca_system_score_codex":0.0000011563517,"about_ca_system_score_gemma":0.000007949513,"threshold_uncertainty_score":0.49841815},"labels":[],"label_agreement":null},{"id":"W2789788694","doi":"10.3847/1538-4357/aab767","title":"Habitability from Tidally Induced Tectonics","year":2018,"lang":"en","type":"article","venue":"The Astrophysical Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Toronto","funders":"","keywords":"Habitability; Terrestrial planet; Outgassing; Planet; Planetary habitability; Circumstellar habitable zone; Tectonics; Defrosting","score_opus":0.012324072058861251,"score_gpt":0.21305135177623213,"score_spread":0.2007272797173709,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789788694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969485,0.000017207787,0.00065028976,0.00050764193,0.0009124334,0.000067466695,0.00006182819,0.00002117649,0.0008134969],"genre_scores_gemma":[0.99481076,0.0000031147238,0.0014993788,0.0001534506,0.0034908643,3.247091e-7,0.000009168951,0.0000040132577,0.000028923603],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99882954,0.00017664963,0.00020846327,0.0001623066,0.00031586594,0.00030719585],"domain_scores_gemma":[0.99923587,0.00013225521,0.00011327319,0.0002781748,0.000091964066,0.00014849375],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00026749936,0.00012576766,0.00018579079,0.000014682372,0.000407694,0.0002070987,0.00046780176,0.00004069525,0.0022638363],"category_scores_gemma":[0.0000384102,0.00006997284,0.00009148595,0.000102416096,0.00018785034,0.00016629338,0.000031763375,0.0002907393,0.0012609584],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008570633,0.00025133594,0.024688229,0.000008514864,0.00035617297,0.00005759661,0.0015522604,0.000567497,0.7645301,0.0021428315,0.0038966802,0.20109168],"study_design_scores_gemma":[0.0003515502,0.0005909403,0.9589,0.0000139234835,0.00004727291,0.00001610362,0.000050826246,0.0011341771,0.008870242,0.026907457,0.0029301075,0.00018740249],"about_ca_topic_score_codex":0.000853622,"about_ca_topic_score_gemma":0.00014433106,"teacher_disagreement_score":0.9342118,"about_ca_system_score_codex":0.0000037304771,"about_ca_system_score_gemma":0.000068473375,"threshold_uncertainty_score":0.99951667},"labels":[],"label_agreement":null},{"id":"W2789876573","doi":"10.1002/2017jb014826","title":"Collisional Processes in the Crust of the Northern Tien Shan Inferred From Velocity and Attenuation Tomography Studies","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Population and Public Health; Russian Science Foundation; King Saud University; Russian Foundation for Basic Research","keywords":"Geology; Crust; Seismology; Kazakh; Attenuation; Shield; Seismic velocity; Anomaly (physics); Geophysics; Petrology","score_opus":0.06027908682772871,"score_gpt":0.3395020878383974,"score_spread":0.2792230010106687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789876573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983854,0.00033249336,0.0000030126466,0.0007021945,0.00015832728,0.00016325738,0.000081905935,0.0000016835885,0.00017172348],"genre_scores_gemma":[0.99908984,0.00014782183,0.000060031623,0.000052703155,0.00061876094,0.0000011603931,0.0000045991974,0.0000023577475,0.000022722805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978365,0.00041979805,0.00032608275,0.0001317638,0.0010413029,0.0002446039],"domain_scores_gemma":[0.9975588,0.0010705292,0.00020129736,0.00015675974,0.0009442339,0.00006839296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012903538,0.00009167957,0.0002744037,0.00009415001,0.00024124794,0.00008748836,0.00041762946,0.000039731713,0.000056724675],"category_scores_gemma":[0.0007937062,0.000044257307,0.000063046165,0.0006530708,0.0006310816,0.00023387352,0.000060149498,0.00028018933,0.000014755876],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018660073,0.0007589664,0.9098913,0.00035468716,0.00061983004,0.00005383945,0.03488244,0.0007845002,0.01097328,0.00043012793,0.0026971907,0.03668781],"study_design_scores_gemma":[0.00027591968,0.0005062435,0.9869988,0.00011774344,0.000014235766,0.0000022541622,0.00069418905,0.00029538324,0.0015599314,0.0086630955,0.00081477605,0.00005743199],"about_ca_topic_score_codex":0.0021525724,"about_ca_topic_score_gemma":0.006541002,"teacher_disagreement_score":0.077107474,"about_ca_system_score_codex":0.0000027455799,"about_ca_system_score_gemma":0.00022472,"threshold_uncertainty_score":0.3650033},"labels":[],"label_agreement":null},{"id":"W2790744183","doi":"10.1144/sp470.7","title":"Exploring the theory of plate tectonics: the role of mantle lithosphere structure","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Plate tectonics; Geology; Mantle (geology); Geophysics; Tectonics; Seismology","score_opus":0.026778693535835264,"score_gpt":0.21141984197471686,"score_spread":0.1846411484388816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790744183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9789242,0.00026563174,0.00011591255,0.0013683066,0.0003787952,0.0002568602,0.00027924028,0.00003154777,0.018379495],"genre_scores_gemma":[0.9976381,0.00011877431,0.00048716422,0.00011961003,0.0013406549,0.000006516119,0.00004425769,0.0000026117311,0.00024228888],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9990089,0.00011439651,0.0002520935,0.00018053812,0.0002184501,0.00022563133],"domain_scores_gemma":[0.998948,0.0003136721,0.00016976878,0.00036501372,0.00015850653,0.000045066678],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043161665,0.00010198815,0.0001713989,0.000008388514,0.00039109774,0.00005192098,0.000577674,0.00007160492,0.009083187],"category_scores_gemma":[0.00009002316,0.00004912529,0.00013601797,0.00032783343,0.0007219005,0.000167769,0.00006702663,0.00014177944,0.000055021024],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016757939,0.00014747222,0.08313486,0.000039075978,0.00037799336,4.120963e-7,0.008343068,0.00088317785,0.007744313,0.7587802,0.0110761095,0.12930577],"study_design_scores_gemma":[0.00013477466,0.000112453345,0.6566656,0.0000057323978,0.000039312024,0.0000019103845,0.001420611,0.00024828565,0.005006062,0.12781651,0.20842522,0.00012352451],"about_ca_topic_score_codex":0.0003901474,"about_ca_topic_score_gemma":0.00030192707,"teacher_disagreement_score":0.6309637,"about_ca_system_score_codex":0.0000022563827,"about_ca_system_score_gemma":0.000039609346,"threshold_uncertainty_score":0.99182266},"labels":[],"label_agreement":null},{"id":"W2791039182","doi":"10.1038/nature25972","title":"CaSiO3 perovskite in diamond indicates the recycling of oceanic crust into the lower mantle","year":2018,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":148,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of British Columbia","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Mantle (geology); Geology; Kimberlite; Geochemistry; Oceanic crust; Diamond; Crust; Mineralogy; Transition zone; Subduction; Basalt; Materials science; Paleontology; Metallurgy","score_opus":0.0056949604054295664,"score_gpt":0.22149538450384904,"score_spread":0.21580042409841946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791039182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937413,0.0013580702,0.0000010871869,0.0008262983,0.000834837,0.00011749639,0.00003250949,0.000007884811,0.0030805555],"genre_scores_gemma":[0.99881935,0.0000830968,0.000052819138,0.00046725062,0.00036006357,6.1177695e-7,0.000015244546,0.0000029293649,0.00019860637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993138,0.000067927656,0.00014009373,0.00014076252,0.00017356283,0.00016386576],"domain_scores_gemma":[0.9994907,0.00015707877,0.00007769306,0.00021489228,0.000034046167,0.000025586776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003862442,0.00008247289,0.000117090574,0.000030047617,0.00013938999,0.000041391726,0.000358829,0.00024537774,0.00081690546],"category_scores_gemma":[0.00006494322,0.000038899307,0.000033508724,0.00019278747,0.00014821692,0.00007318446,0.000026361531,0.00049019716,0.00011104269],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010529982,0.00039961527,0.66597193,0.00035894522,0.00038248187,0.00013712417,0.063530944,0.0009070292,0.05670997,0.0064838124,0.08683229,0.11723286],"study_design_scores_gemma":[0.0002761421,0.0001967765,0.9003933,0.00007440523,0.00003130453,0.000004330716,0.0005822946,0.00058099354,0.012956914,0.0057081166,0.0789848,0.00021064492],"about_ca_topic_score_codex":0.0012779684,"about_ca_topic_score_gemma":0.0021076144,"teacher_disagreement_score":0.23442134,"about_ca_system_score_codex":0.000001379201,"about_ca_system_score_gemma":0.000023389364,"threshold_uncertainty_score":0.8944542},"labels":[],"label_agreement":null},{"id":"W2791742501","doi":"10.1080/08957959.2018.1493476","title":"Decreasing electrical resistivity of gold along the melting boundary up to 5 GPa","year":2018,"lang":"en","type":"article","venue":"High Pressure Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Materials science; Phase boundary; Thermodynamics; Thermal conductivity; Melting temperature; Condensed matter physics; Phase (matter); Chemistry; Composite material; Physics","score_opus":0.04268776613893104,"score_gpt":0.318661848207255,"score_spread":0.27597408206832397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791742501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895563,0.0008335609,0.00010516636,0.00071459985,0.0005572059,0.0005066329,0.00015836881,0.000040436295,0.0075276894],"genre_scores_gemma":[0.99707276,0.000032445703,0.000538291,0.000055380493,0.0008806907,0.000005694774,0.00002099476,0.000009018055,0.001384726],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99641675,0.000973365,0.0003073783,0.00041905226,0.0011012016,0.0007822657],"domain_scores_gemma":[0.997481,0.001213461,0.00007835225,0.00055359,0.0004483458,0.00022527891],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0038852897,0.00014772554,0.0002909215,0.00015203295,0.0006781283,0.00024155814,0.0007362746,0.00010350872,0.0013028119],"category_scores_gemma":[0.00077917485,0.000098919845,0.0000579513,0.0007576196,0.00043854027,0.00016655886,0.00015022985,0.00033728883,0.00027948522],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005919497,0.0004067385,0.21379127,0.0010825321,0.0012360103,0.00018081606,0.00986896,0.0012646398,0.13077073,0.035390943,0.24500354,0.35508433],"study_design_scores_gemma":[0.000372935,0.0006296459,0.7186692,0.00013071935,0.00006168444,0.000009605406,0.00009508987,0.001402228,0.030648144,0.004451506,0.24320899,0.00032028608],"about_ca_topic_score_codex":0.026016418,"about_ca_topic_score_gemma":0.0033968291,"teacher_disagreement_score":0.5048779,"about_ca_system_score_codex":0.0000049461346,"about_ca_system_score_gemma":0.00020836978,"threshold_uncertainty_score":0.9996101},"labels":[],"label_agreement":null},{"id":"W2794129871","doi":"10.1126/science.aao3030","title":"Ice-VII inclusions in diamonds: Evidence for aqueous fluid in Earth’s deep mantle","year":2018,"lang":"en","type":"article","venue":"Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":231,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum","funders":"Office of the Director; U.S. Department of Energy","keywords":"Transition zone; Geology; Mantle (geology); Aqueous solution; Geochemistry; Mineralogy; High pressure; Chemistry; Thermodynamics","score_opus":0.03003866051164678,"score_gpt":0.2850431615020414,"score_spread":0.2550045009903946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794129871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960715,0.00047760355,0.00014583777,0.00024439482,0.0008361067,0.00030280772,0.000030532065,0.000019375739,0.0018718258],"genre_scores_gemma":[0.9981189,0.000060360908,0.0013048034,0.00019047271,0.00016867125,0.0000062734644,0.0000047311714,0.0000023693317,0.0001434442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852484,0.000042023683,0.00021783654,0.0004042551,0.00031003688,0.0005009785],"domain_scores_gemma":[0.9992865,0.00021674341,0.000050879422,0.00026149018,0.000069759844,0.00011465766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011888983,0.000101731435,0.00015991894,0.00017899965,0.00031041494,0.00011574519,0.00060052035,0.000040779374,0.0004916856],"category_scores_gemma":[0.00036141838,0.00008342334,0.000023912096,0.0007737018,0.0004650652,0.00064915355,0.000085075895,0.000057308058,0.0003288681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050430046,0.00023978959,0.5083972,0.00018929142,0.000010459287,0.00012195119,0.011846305,0.0050368025,0.28154445,0.002974772,0.0008813537,0.18825331],"study_design_scores_gemma":[0.00045152614,0.00044765236,0.9373809,0.00018061715,0.0000059489385,0.000006312528,0.00015928931,0.026721723,0.01494374,0.009645868,0.0096872505,0.00036916864],"about_ca_topic_score_codex":0.002655101,"about_ca_topic_score_gemma":0.018023014,"teacher_disagreement_score":0.4289837,"about_ca_system_score_codex":0.0000068716213,"about_ca_system_score_gemma":0.00017759236,"threshold_uncertainty_score":0.9998955},"labels":[],"label_agreement":null},{"id":"W2795786965","doi":"10.1063/1.5022273","title":"Strength and texture of sodium chloride to 56 GPa","year":2018,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Carnegie Institution of Washington; National Science Foundation","keywords":"Materials science; Phase (matter); Texture (cosmology); Sodium; Diffraction; Slip (aerodynamics); Crystallography; Analytical Chemistry (journal); Chemistry; Composite material; Thermodynamics; Metallurgy; Optics; Physics","score_opus":0.007999338187066406,"score_gpt":0.20628133367614174,"score_spread":0.19828199548907532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795786965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932173,0.000025750163,0.00010937964,0.00004322939,0.0004042473,0.00006706143,0.000062939136,0.0000037517304,0.006066357],"genre_scores_gemma":[0.99707216,0.000017495768,0.00088119326,0.00012182593,0.0018661363,1.5275049e-7,0.0000047219505,0.0000033802096,0.00003292255],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99930304,0.000008952531,0.00023939913,0.000091153495,0.00021447503,0.00014298278],"domain_scores_gemma":[0.99940145,0.00004362088,0.00023791024,0.000106219944,0.00009353772,0.000117262774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015774141,0.0000948721,0.0002516532,0.000029843235,0.000052440242,0.00003463262,0.00015400608,0.000035304725,0.00015891627],"category_scores_gemma":[0.000005478271,0.0000694881,0.000047889196,0.000110308276,0.00006402009,0.00008792421,0.000015986738,0.00008127619,0.00003183194],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0069390223,0.0006634719,0.014407975,0.0006158816,0.0012726894,0.000057891604,0.014016109,0.013887969,0.51206875,0.033336524,0.04262564,0.3601081],"study_design_scores_gemma":[0.0022485356,0.0022652808,0.10592888,0.00016378703,0.00032865597,0.00002399198,0.0005786029,0.0013428903,0.72281784,0.0668156,0.09668295,0.0008029888],"about_ca_topic_score_codex":0.00005822556,"about_ca_topic_score_gemma":0.000027713091,"teacher_disagreement_score":0.3593051,"about_ca_system_score_codex":0.0000011862809,"about_ca_system_score_gemma":0.00003847061,"threshold_uncertainty_score":0.28336427},"labels":[],"label_agreement":null},{"id":"W2796171267","doi":"","title":"Assessment of Symmetric Instability from Global Reanalysis Data","year":2017,"lang":"en","type":"article","venue":"21st Conference on Atmospheric and Oceanic Fluid Dynamics and the 19th Conference on Middle Atmosphere","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Instability; Geology; Climatology; Physics","score_opus":0.03210902773412067,"score_gpt":0.2567210085216745,"score_spread":0.22461198078755384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796171267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.916818,0.00058225106,0.00114665,0.00080777693,0.0005200516,0.0004957631,0.0022314002,0.000039480106,0.077358626],"genre_scores_gemma":[0.99388057,0.0031747795,0.0020182088,0.00014064384,0.000082836916,0.000003859645,0.00037478737,0.00001100038,0.00031331714],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9969477,0.00028024078,0.0006371452,0.0010501265,0.0006082107,0.00047658637],"domain_scores_gemma":[0.9960295,0.0003466297,0.0006540624,0.0024938823,0.00021349822,0.00026246044],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009163598,0.000495378,0.0009877207,0.0000034631548,0.0008125642,0.00077328784,0.0017450548,0.0001933172,0.0015651555],"category_scores_gemma":[0.00021722968,0.000328132,0.00011491488,0.00021746731,0.0010320374,0.00037837372,0.00039787398,0.00029008268,0.000029209905],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003829213,0.00013556969,0.12291943,0.000081206876,0.00035638813,0.000010941808,0.00009697501,0.00030729652,0.000015655865,0.7752511,0.000044822005,0.10039773],"study_design_scores_gemma":[0.0012000754,0.00020848612,0.37860492,0.000112361,0.00017514006,0.000001917993,0.0003757637,0.5995762,0.0000026776488,0.019344972,0.00010061076,0.00029691352],"about_ca_topic_score_codex":0.016224923,"about_ca_topic_score_gemma":0.0054983026,"teacher_disagreement_score":0.7559061,"about_ca_system_score_codex":0.000022667138,"about_ca_system_score_gemma":0.00029967245,"threshold_uncertainty_score":0.9999171},"labels":[],"label_agreement":null},{"id":"W2796526979","doi":"10.1002/2017gc007266","title":"The Sensitivity of Core Heat Flux to the Modeling of Plate‐Like Surface Motion","year":2018,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Heat flux; Convection; Rheology; Mechanics; Mantle convection; Mantle (geology); Geology; Inner core; Heat transfer; Geophysics; Convective heat transfer; Internal heating; Thermodynamics; Tectonics; Physics; Lithosphere","score_opus":0.015211802767913521,"score_gpt":0.21120243278770168,"score_spread":0.19599063001978817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2796526979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956124,0.00012218552,0.0008476168,0.000106415915,0.0009328316,0.00029668733,0.0005712986,0.000024692603,0.0014858881],"genre_scores_gemma":[0.9987964,0.000009225771,0.000056352597,0.000024036099,0.00065981824,0.0000018733956,0.00013960205,0.00000704642,0.00030563152],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983233,0.00011683617,0.0004341885,0.0003029979,0.00044155572,0.00038111085],"domain_scores_gemma":[0.99839807,0.00025717574,0.00018898159,0.0006896659,0.00037081575,0.0000953077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010128409,0.0002058558,0.00034744883,0.000011550051,0.00036361773,0.000059678972,0.0003563731,0.00009124856,0.00006942669],"category_scores_gemma":[0.00004629492,0.00012899967,0.0001066115,0.00024641718,0.00015198161,0.00008547613,0.00006244551,0.000108265755,0.00013222791],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002189538,0.000062464955,0.0040796706,0.0004554325,0.00018565184,0.000005529711,0.0014444256,0.31137034,0.67703706,0.00023651078,0.0021251203,0.002778815],"study_design_scores_gemma":[0.0003690208,0.00019334201,0.004814634,0.0002188142,0.00009633154,0.000019059478,0.00088478485,0.73856866,0.24908632,0.0017287892,0.0035187928,0.0005014551],"about_ca_topic_score_codex":0.011383156,"about_ca_topic_score_gemma":0.0009428966,"teacher_disagreement_score":0.42795077,"about_ca_system_score_codex":0.0000046210366,"about_ca_system_score_gemma":0.00006286788,"threshold_uncertainty_score":0.99520016},"labels":[],"label_agreement":null},{"id":"W2797512617","doi":"10.1139/cjes-2017-0277","title":"Surface-wave images of western Canada: lithospheric variations across the Cordillera–craton boundary","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"","keywords":"Geology; Craton; Lithosphere; Asthenosphere; Mantle (geology); Seismology; Archean; Low-velocity zone; Geophysics; Slab; Paleontology; Tectonics","score_opus":0.017931920173655403,"score_gpt":0.22092494760656003,"score_spread":0.20299302743290462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797512617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935993,0.0006960364,0.000039434486,0.00088474475,0.0017353249,0.00007241784,0.00032639896,0.0000020563982,0.0026442683],"genre_scores_gemma":[0.99866986,0.000019295241,0.0004993132,0.00024794685,0.00031072582,8.951337e-8,0.000002644543,0.0000021610674,0.0002479725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986363,0.000100622296,0.00034378452,0.00013020264,0.00037793466,0.00041113736],"domain_scores_gemma":[0.998766,0.00012938527,0.00032275825,0.0001435564,0.00029994422,0.00033837993],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009114759,0.00010314259,0.00021486907,0.000033114997,0.0008968038,0.00029985473,0.00047562894,0.000031660245,0.0019814437],"category_scores_gemma":[0.00008148565,0.00006432133,0.000045236786,0.00040626508,0.00097094756,0.0003344559,0.000008999209,0.00009633458,0.00001477275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026671303,0.000012698949,0.9785436,0.000025605716,0.000108317705,0.000120687444,0.003771279,0.003952381,0.001062854,0.00020932055,0.00609882,0.0060677826],"study_design_scores_gemma":[0.00010524698,0.00027479682,0.9670214,0.000035619414,0.000016775935,0.000049622147,0.0005299544,0.00031696225,0.0014941801,0.00024161336,0.029796548,0.00011730291],"about_ca_topic_score_codex":0.8540863,"about_ca_topic_score_gemma":0.994103,"teacher_disagreement_score":0.14001672,"about_ca_system_score_codex":0.0000027839708,"about_ca_system_score_gemma":0.0050562373,"threshold_uncertainty_score":0.9989309},"labels":[],"label_agreement":null},{"id":"W2802507608","doi":"10.1007/s00710-018-0570-2","title":"Diamonds from Orapa Mine show a clear subduction signature in SIMS stable isotope data","year":2018,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Diamond; Kimberlite; Isotopes of nitrogen; δ13C; Cathodoluminescence; Nitrogen; Population; Geochemistry; Subduction; Geology; Isotopic signature; Mantle (geology); δ15N; Craton; Mineralogy; Isotopes of carbon; Isotope; Analytical Chemistry (journal); Stable isotope ratio; Chemistry; Environmental chemistry; Materials science; Paleontology; Total organic carbon; Metallurgy; Tectonics","score_opus":0.017790644468071,"score_gpt":0.22356630532667982,"score_spread":0.20577566085860882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802507608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956107,0.0007973442,0.000028295899,0.0007145035,0.000923308,0.00008038423,0.0006626949,0.000019122923,0.0011636178],"genre_scores_gemma":[0.99572545,0.00009425191,0.00030875707,0.00053859793,0.00093971257,0.0000012731612,0.0018277437,0.000004284878,0.00055991014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988386,0.00016101783,0.00018033614,0.00043117255,0.0000706303,0.0003182488],"domain_scores_gemma":[0.99938864,0.00011194624,0.000055448,0.00034877157,0.000025586121,0.00006959978],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002625844,0.00013545019,0.0002746541,0.00007922595,0.00009324089,0.00003300218,0.00025995087,0.00020129827,0.0038451476],"category_scores_gemma":[0.000020870208,0.000111256195,0.000013969072,0.000118259435,0.00020038767,0.00022951815,0.00005451279,0.0001516799,0.00013848853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002932623,0.00016852425,0.8544763,0.000047077654,0.00020411778,0.00020299658,0.0014702538,0.00052608986,0.07789774,0.0010243508,0.048479717,0.01257026],"study_design_scores_gemma":[0.001384248,0.0011517295,0.7994059,0.000010609694,0.0000696147,0.000027637348,0.00007288079,0.00684379,0.00059116853,0.0038388062,0.1861986,0.00040506793],"about_ca_topic_score_codex":0.019696828,"about_ca_topic_score_gemma":0.0615021,"teacher_disagreement_score":0.13771889,"about_ca_system_score_codex":0.0000011949636,"about_ca_system_score_gemma":0.00002091724,"threshold_uncertainty_score":0.9970655},"labels":[],"label_agreement":null},{"id":"W2803909855","doi":"10.1016/j.epsl.2018.05.002","title":"Experimental constraints on the sound velocities of cementite Fe3C to core pressures","year":2018,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Materials Sciences and Engineering; Argonne National Laboratory; Alfred P. Sloan Foundation; U.S. Department of Energy; National Nuclear Security Administration; Alzheimer Society of B.C.; Office of Science; National Science Foundation","keywords":"Cementite; Inner core; Bulk modulus; Shear modulus; Carbide; Shear (geology); Core (optical fiber); Outer core; Diamond anvil cell; Geology; Materials science; Mineralogy; High pressure; Thermodynamics; Metallurgy; Composite material; Physics; Austenite","score_opus":0.02162637199174298,"score_gpt":0.22173913883076962,"score_spread":0.20011276683902665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803909855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944308,0.00007263254,0.000015555659,0.0006946134,0.0005823218,0.00020492398,0.00026143852,0.0000136372,0.0037240877],"genre_scores_gemma":[0.9962624,0.0000033870128,0.000269572,0.0031774114,0.00019200816,8.6463814e-7,0.000033385553,0.0000017706566,0.000059220107],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99879014,0.00003771622,0.0001538448,0.00027800194,0.00040289352,0.00033742795],"domain_scores_gemma":[0.99946064,0.00012011489,0.000062415405,0.00019702842,0.000022480219,0.0001373076],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038730408,0.00013017947,0.00014277475,0.00008199611,0.00040924142,0.00013460031,0.0003255241,0.00002168231,0.0028063916],"category_scores_gemma":[0.00002108331,0.00008495152,0.000020097114,0.00016710142,0.0017411541,0.00018687615,0.000025141506,0.0000593276,0.00020022543],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007639078,0.00008675235,0.24227463,0.00009653612,0.00016772222,0.00007451542,0.013672206,0.004295796,0.68513614,0.0052697742,0.033269193,0.014892802],"study_design_scores_gemma":[0.0003414149,0.0010595927,0.9018191,0.0000620245,0.000019961126,0.000020674022,0.0007155922,0.0007839789,0.08028518,0.00028380417,0.014194119,0.00041455528],"about_ca_topic_score_codex":0.0008611798,"about_ca_topic_score_gemma":0.0001834692,"teacher_disagreement_score":0.65954447,"about_ca_system_score_codex":7.926935e-7,"about_ca_system_score_gemma":0.000027864324,"threshold_uncertainty_score":0.99810517},"labels":[],"label_agreement":null},{"id":"W2804254254","doi":"10.1139/cjp-2018-0139","title":"Volume derivatives of the Grüneisen parameter in the limit of infinite pressure","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Limit (mathematics); Thermodynamics; Physics; Volume (thermodynamics); Zero (linguistics); Compression (physics); Grüneisen parameter; Order (exchange); Thermal; Mathematical analysis; Mathematics","score_opus":0.016952160312456634,"score_gpt":0.1989692044212089,"score_spread":0.18201704410875227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804254254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975059,0.00014653096,0.000026939393,0.00028488558,0.00039027724,0.00007955205,0.00015141875,5.4812136e-7,0.001413927],"genre_scores_gemma":[0.9993947,0.00000699911,0.00009381809,0.00013667934,0.00030604145,1.5074448e-7,0.000002096386,0.0000022601182,0.000057245597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923676,0.00013359619,0.00025586618,0.00005544839,0.00016085195,0.00015747744],"domain_scores_gemma":[0.9991944,0.000115241084,0.0002982299,0.00017749591,0.00013650127,0.000078138364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027580783,0.00007132383,0.00018463677,0.00003761971,0.000067427376,0.00002831619,0.0004573,0.000032092263,0.00023806619],"category_scores_gemma":[0.00007525706,0.000039046925,0.000072868104,0.00020700274,0.00027277187,0.00013518616,0.0000058051155,0.00010622922,0.0000075973508],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008333061,0.00005392223,0.93132144,0.00014411967,0.0002917545,0.00002414748,0.021978984,0.0056016906,0.0034556114,0.0035582632,0.010292147,0.023194563],"study_design_scores_gemma":[0.00019954654,0.00023811725,0.95664436,0.00009080614,0.00005929593,0.0000064836004,0.000276943,0.00028840848,0.0050093434,0.009810906,0.02728143,0.00009437493],"about_ca_topic_score_codex":0.012409016,"about_ca_topic_score_gemma":0.023829985,"teacher_disagreement_score":0.02532288,"about_ca_system_score_codex":0.000001533356,"about_ca_system_score_gemma":0.00030134976,"threshold_uncertainty_score":0.99416745},"labels":[],"label_agreement":null},{"id":"W2805797502","doi":"10.1029/2018jb015473","title":"Precambrian Plate Tectonics in Northern Hudson Bay: Evidence From <i>P</i> and <i>S</i> Wave Seismic Tomography and Analysis of Source Side Effects in Relative Arrival‐Time Data Sets","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Terrane; Geology; Precambrian; Lithosphere; Archean; Subduction; Seismology; Bay; Plate tectonics; Mantle (geology); Tectonics; Seismometer; Paleontology; Crust; Geophysics; Oceanography","score_opus":0.033324666137260185,"score_gpt":0.29970254532121193,"score_spread":0.2663778791839517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805797502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983853,0.0006745498,0.00009295087,0.00016959115,0.000067490306,0.00023389094,0.00024831502,0.0000048545585,0.00012302464],"genre_scores_gemma":[0.9986953,0.00035888178,0.0006559074,0.000036507805,0.00017095148,7.4829654e-7,0.000046087498,0.0000079328365,0.000027663928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966968,0.0008385296,0.00060514687,0.00045858772,0.0008798512,0.0005210632],"domain_scores_gemma":[0.9959755,0.0026947577,0.00032676442,0.00046152528,0.00025905526,0.000282413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022198432,0.00019970445,0.00087081915,0.0006336035,0.000106805135,0.00012538047,0.00046919016,0.00011148053,0.00003941784],"category_scores_gemma":[0.0007261628,0.0001563896,0.0000998808,0.0014793922,0.00047994786,0.00085943233,0.00020729825,0.0006022187,0.000020010666],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0032324733,0.00039757686,0.83767027,0.00028924574,0.0021462988,0.0005342549,0.0064534955,0.005652906,0.0669334,0.000028796812,0.00014844719,0.07651282],"study_design_scores_gemma":[0.0005958098,0.00088261627,0.8993595,0.00047020486,0.00017138098,0.000004712052,0.000054163113,0.094038956,0.0022641302,0.0018554142,0.00014013474,0.00016294443],"about_ca_topic_score_codex":0.009089902,"about_ca_topic_score_gemma":0.020348761,"teacher_disagreement_score":0.08838605,"about_ca_system_score_codex":0.0000072014464,"about_ca_system_score_gemma":0.00015428607,"threshold_uncertainty_score":0.9975273},"labels":[],"label_agreement":null},{"id":"W2806042432","doi":"10.1029/2017jb014894","title":"Shear Wave Tomography Beneath the United States Using a Joint Inversion of Surface and Body Waves","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"University of California, San Diego","keywords":"Geology; Lithosphere; Crust; Seismology; Seismic tomography; Mantle (geology); Geophysics; Surface wave; Tomography; Shear (geology); Seismic wave; Geodesy; Tectonics; Petrology; Physics","score_opus":0.058917526941551106,"score_gpt":0.3090273938239443,"score_spread":0.2501098668823932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806042432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989653,0.00012713503,0.0000322603,0.00036341994,0.00016786178,0.00013721902,0.00006093819,0.0000044271237,0.00014141272],"genre_scores_gemma":[0.9983905,0.0003151061,0.0007025899,0.000049015787,0.00047845434,9.710965e-8,0.000009211758,0.0000055504265,0.000049461916],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99754965,0.0004843584,0.0003928279,0.00016670335,0.00095473643,0.00045173775],"domain_scores_gemma":[0.99803364,0.0005242215,0.00022950709,0.00020762542,0.0007507813,0.0002541962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016104032,0.0001338051,0.00037849744,0.00022694562,0.00034537003,0.00013238528,0.00023686985,0.000056938705,0.00020309417],"category_scores_gemma":[0.00016476054,0.000078081466,0.00011777144,0.0006670101,0.0007937412,0.00025705647,0.00008084284,0.00036348266,0.000021388305],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0055580824,0.0012281262,0.051785074,0.0009243363,0.0019166893,0.0004988997,0.019464696,0.022373542,0.8639365,0.0030272466,0.009816297,0.019470517],"study_design_scores_gemma":[0.0016804414,0.008148486,0.5696226,0.0005927757,0.0001515962,0.00008103123,0.0020291635,0.25075236,0.12808329,0.030538738,0.007791414,0.00052813237],"about_ca_topic_score_codex":0.0056541157,"about_ca_topic_score_gemma":0.000079777885,"teacher_disagreement_score":0.7358532,"about_ca_system_score_codex":0.0000031098612,"about_ca_system_score_gemma":0.0001260943,"threshold_uncertainty_score":0.8547369},"labels":[],"label_agreement":null},{"id":"W2806375387","doi":"10.1126/sciadv.aat1602","title":"The growth of lithospheric diamonds","year":2018,"lang":"en","type":"article","venue":"Science Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Muséum National d'Histoire Naturelle; Campus France; Agence Nationale de la Recherche","keywords":"Lithosphere; Geology; Redox; Earth science; Diamond; Geochemistry; Paleontology; Chemistry; Materials science; Metallurgy; Inorganic chemistry","score_opus":0.005825406721933465,"score_gpt":0.22286967757601087,"score_spread":0.2170442708540774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806375387","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97688246,0.0012418424,0.00006284956,0.00014667927,0.002209852,0.000077210396,0.000017540164,0.000020633071,0.019340917],"genre_scores_gemma":[0.99859995,0.00009398045,0.0007415668,0.00003912734,0.00017332847,6.400871e-7,9.491609e-7,9.788544e-7,0.00034950138],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99908674,0.000019859332,0.0001289724,0.00017667723,0.0003209711,0.00026680194],"domain_scores_gemma":[0.99944,0.00009370702,0.000086007945,0.00018490819,0.00013454196,0.000060804243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055913936,0.00006158956,0.00008542579,0.000017988004,0.0005210372,0.00008273576,0.00057355594,0.000011426558,0.00024896022],"category_scores_gemma":[0.00010262656,0.000033443397,0.00001952531,0.0005579085,0.0018271245,0.0005612887,0.000021478989,0.00002499667,0.00012125223],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013310974,0.000045659326,0.34451863,0.00006231673,0.000020805412,0.0000047826006,0.0016953101,0.00025889976,0.09718342,0.020440612,0.0013901287,0.5342463],"study_design_scores_gemma":[0.0001579243,0.0005566675,0.5951844,0.0000252547,0.000010804856,0.000003081338,0.0003034507,0.0004591525,0.2608774,0.043046337,0.09910107,0.0002744364],"about_ca_topic_score_codex":0.00036417303,"about_ca_topic_score_gemma":0.00033315804,"teacher_disagreement_score":0.5339719,"about_ca_system_score_codex":9.724632e-7,"about_ca_system_score_gemma":0.00006821458,"threshold_uncertainty_score":0.67321163},"labels":[],"label_agreement":null},{"id":"W2806836148","doi":"10.1021/acsearthspacechem.8b00034","title":"Structures and Stability of Iron Halides at the Earth’s Mantle and Core Pressures: Implications for the Missing Halogen Paradox","year":2018,"lang":"en","type":"article","venue":"ACS Earth and Space Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"China Postdoctoral Science Foundation; Jilin University; Ministry of Science and Technology of the People's Republic of China; Ministry of Industry and Information Technology of the People's Republic of China; National Natural Science Foundation of China","keywords":"Halide; Halogen; Inner core; Mantle (geology); Chemistry; Outer core; Alkaline earth metal; Stoichiometry; Impurity; Inorganic chemistry; Chemical physics; Physical chemistry; Materials science; Metal; Geology; Geochemistry; Organic chemistry","score_opus":0.021250651623223055,"score_gpt":0.23736647035907238,"score_spread":0.2161158187358493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806836148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948082,0.0029417803,0.000017189193,0.0012162162,0.00004094773,0.00019532192,0.00045413955,0.000007632676,0.00031857105],"genre_scores_gemma":[0.9991703,0.00024203226,0.00016447506,0.00005650643,0.00012173251,0.0000026663788,0.000037319693,0.000002828428,0.00020215244],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994428,0.000016854738,0.00011092493,0.00020070089,0.00006908042,0.00015962006],"domain_scores_gemma":[0.9992505,0.0003183171,0.00007760989,0.0002430337,0.0000421639,0.00006837967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001734603,0.00010107204,0.00013101331,0.0000041654325,0.00043367845,0.000075883705,0.00009706957,0.0000552612,0.00015422361],"category_scores_gemma":[0.000057782334,0.00005670118,0.000018963245,0.000029173973,0.0005212148,0.000049067105,0.000035825145,0.000043007996,7.8225116e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020054632,0.000013128374,0.24783944,0.00052267587,0.000085332314,6.073147e-7,0.0014101428,0.000027409078,0.7334133,0.00036065315,0.0017240762,0.0144026885],"study_design_scores_gemma":[0.00025652483,0.000054620417,0.62326926,0.000015647398,0.00007471361,0.000016522818,0.00019614912,0.00018823134,0.35334522,0.0033649192,0.019079866,0.00013833148],"about_ca_topic_score_codex":0.00055656716,"about_ca_topic_score_gemma":0.0007179284,"teacher_disagreement_score":0.38006806,"about_ca_system_score_codex":3.9224085e-7,"about_ca_system_score_gemma":0.000019464354,"threshold_uncertainty_score":0.33355477},"labels":[],"label_agreement":null},{"id":"W2869678948","doi":"10.1029/2018gl078074","title":"Diverse Continental Subduction Scenarios Along the Arabia‐Eurasia Collision Zone","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"King Saud University; Institute of Population and Public Health; Deutsche Forschungsgemeinschaft","keywords":"Subduction; Geology; Collision zone; Continental collision; Lithosphere; Seismology; Mantle (geology); Convergent boundary; Slab; Eclogitization; Eurasian Plate; Slab window; Collision; Plate tectonics; Oceanic crust; Paleontology; Tectonics","score_opus":0.031529447381176044,"score_gpt":0.28286718660001586,"score_spread":0.25133773921883984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2869678948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926536,0.00003248872,0.00006541706,0.005125894,0.0009773162,0.00040705557,0.00007256945,0.00004491747,0.0006207189],"genre_scores_gemma":[0.99633765,0.000022426642,0.00007173271,0.00050980505,0.0025562795,0.0000062606837,0.00008451604,0.0000075723287,0.00040375598],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9970563,0.00044573017,0.00021345721,0.00043526766,0.0010665928,0.0007826349],"domain_scores_gemma":[0.998763,0.000387505,0.00006146156,0.00041564804,0.00017374076,0.00019864047],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0008867231,0.00016784247,0.00020761258,0.00008681748,0.00096644775,0.0002900172,0.0005312569,0.000059766902,0.0009353641],"category_scores_gemma":[0.00012485185,0.000109105604,0.00009316772,0.00044661303,0.0009550493,0.00032817875,0.00010078468,0.000362521,0.004095822],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018281871,0.00040581453,0.044918347,0.00012593962,0.0002779746,0.00032651983,0.0033603886,0.0010639499,0.5858968,0.0025526786,0.29327074,0.06597267],"study_design_scores_gemma":[0.0010898915,0.0008279797,0.870725,0.00007431016,0.000041042793,0.000012042456,0.0008086153,0.0045407773,0.017095527,0.0008356694,0.10340817,0.0005409754],"about_ca_topic_score_codex":0.02102233,"about_ca_topic_score_gemma":0.0020837223,"teacher_disagreement_score":0.8258067,"about_ca_system_score_codex":0.00001154866,"about_ca_system_score_gemma":0.000046080975,"threshold_uncertainty_score":0.9999779},"labels":[],"label_agreement":null},{"id":"W2881705875","doi":"10.1038/s41598-018-28921-w","title":"Electrical resistivity of liquid Fe to 12 GPa: Implications for heat flow in cores of terrestrial bodies","year":2018,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation; Natural Sciences and Engineering Research Council of Canada; Government of Canada","keywords":"Electrical resistivity and conductivity; Heat flow; Flow (mathematics); Materials science; Geology; Environmental science; Earth science; Soil science; Geophysics; Mechanics; Physics; Meteorology; Electrical engineering; Engineering","score_opus":0.023602327803481985,"score_gpt":0.2627979920953991,"score_spread":0.23919566429191713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2881705875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99562234,0.000041165506,0.00021184041,0.00016057666,0.0029041038,0.00041483133,0.00016435354,0.000011006464,0.00046976365],"genre_scores_gemma":[0.9983766,0.0000019470874,0.0011481324,0.000009024683,0.00018017391,0.000007573881,0.00010197911,0.0000022445383,0.00017231808],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99870026,0.00004138523,0.00046161457,0.00036855502,0.00019411591,0.00023405121],"domain_scores_gemma":[0.9991445,0.000109181936,0.00014630237,0.00040338858,0.000117600444,0.00007900364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010296847,0.0000797721,0.0002451578,0.00013578299,0.00013732913,0.000048647693,0.00013381732,0.00004285609,0.000094982475],"category_scores_gemma":[0.0003649085,0.00006499144,0.00005729972,0.00025710362,0.00021971378,0.00008635878,0.00002016557,0.00002569266,0.000005911519],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015959021,0.00028374713,0.19404292,0.00012731134,0.000055479693,0.00002036456,0.0012985463,0.0012613734,0.71784264,0.00041449643,0.07071195,0.012345239],"study_design_scores_gemma":[0.00030022443,0.00094590045,0.73109967,0.00006108848,0.000034181154,0.000012383691,0.0000148426625,0.0006588992,0.21056901,0.016742455,0.039313488,0.00024783495],"about_ca_topic_score_codex":0.0014663546,"about_ca_topic_score_gemma":0.0044270656,"teacher_disagreement_score":0.53705674,"about_ca_system_score_codex":0.000003224381,"about_ca_system_score_gemma":0.00013332593,"threshold_uncertainty_score":0.26502737},"labels":[],"label_agreement":null},{"id":"W2885165409","doi":"10.1063/1.5039329","title":"Setup for meV-resolution inelastic X-ray scattering measurements and X-ray diffraction at the Matter in Extreme Conditions endstation at the Linac Coherent Light Source","year":2018,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Fusion Energy Sciences; Volkswagen Foundation; Atomic Weapons Establishment; Engineering and Physical Sciences Research Council; U.S. Department of Energy","keywords":"Monochromator; Warm dense matter; Optics; Linear particle accelerator; Diffraction; Physics; Scattering; Resolution (logic); Silicon; X-ray; Laser; Beam (structure); Optoelectronics","score_opus":0.04415991678692219,"score_gpt":0.25464424454412327,"score_spread":0.21048432775720108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885165409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99525505,0.001138806,0.000039829458,0.0007078905,0.001259288,0.0010012259,0.00022153732,0.00000746169,0.00036891995],"genre_scores_gemma":[0.9975742,0.00036898383,0.00006465197,0.00021863586,0.00008334242,0.00003582558,0.00037895376,0.000004954968,0.0012704602],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984701,0.00016083066,0.0004114755,0.00031070242,0.00039945342,0.0002474145],"domain_scores_gemma":[0.99920094,0.00007233197,0.00029577257,0.00027270862,0.000109836896,0.000048394588],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012294301,0.00013566998,0.00020099037,0.00006135172,0.0007193676,0.00011108603,0.00017943692,0.00003304214,0.0018430545],"category_scores_gemma":[0.000044455966,0.0000792796,0.000052450523,0.00020726681,0.00028197517,0.00023061266,0.000055846405,0.000048171707,0.00031094922],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036288626,0.00034728914,0.24561734,0.009780239,0.00034365102,0.0000015113174,0.0030481115,0.0008931382,0.5324949,0.000087207314,0.06642443,0.1405993],"study_design_scores_gemma":[0.0009885177,0.00017066469,0.7868403,0.0037922147,0.00024292595,0.000008441072,0.00009786144,0.0046053724,0.0071360767,0.0002909227,0.19545883,0.0003678302],"about_ca_topic_score_codex":0.00016348422,"about_ca_topic_score_gemma":0.00075374375,"teacher_disagreement_score":0.541223,"about_ca_system_score_codex":0.000029722685,"about_ca_system_score_gemma":0.00002359543,"threshold_uncertainty_score":0.9990694},"labels":[],"label_agreement":null},{"id":"W2886204869","doi":"10.1029/2018gc007646","title":"Shear Wave Splitting Beneath Eastern North American Continent: Evidence for a Multilayered and Laterally Variable Anisotropic Structure","year":2018,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; Rutgers, The State University of New Jersey; National Science Foundation","keywords":"Lithosphere; Geology; Anisotropy; Tectonics; Shear wave splitting; Shear (geology); Seismology; Plate tectonics; Geophysics; Structural basin; Bay; Shear zone; Petrology; Geomorphology; Oceanography","score_opus":0.01940003281663583,"score_gpt":0.22852619738934243,"score_spread":0.2091261645727066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886204869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99676096,0.00017022986,0.00038932366,0.000051746185,0.000495221,0.00051164825,0.0013576547,0.000075517026,0.00018767249],"genre_scores_gemma":[0.9945568,0.000017568043,0.0025753682,0.00007953909,0.002006664,0.000011863902,0.00035230332,0.000017174738,0.0003827119],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99776536,0.00005754612,0.00044656664,0.0007247805,0.00030550332,0.00070026575],"domain_scores_gemma":[0.9984113,0.00020132784,0.00037903493,0.000490355,0.00028509425,0.00023288345],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00017830243,0.00038103992,0.00057060376,0.000028877765,0.0003674055,0.00030013334,0.00029390832,0.00009358554,0.00016745033],"category_scores_gemma":[0.0000672174,0.00034074753,0.000081682534,0.00022517072,0.00019290323,0.00027984983,0.00006629816,0.00012888914,0.000044490196],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011453329,0.00012983542,0.65460616,0.00400681,0.0006037688,0.00005591996,0.002817834,0.0016625961,0.29593316,0.0002846784,0.00090383895,0.03785005],"study_design_scores_gemma":[0.003759489,0.0018125277,0.71634454,0.0012855764,0.0005427071,0.00010774444,0.0005275501,0.2050297,0.047403768,0.0025487826,0.01745091,0.003186719],"about_ca_topic_score_codex":0.007959373,"about_ca_topic_score_gemma":0.0007368373,"teacher_disagreement_score":0.2485294,"about_ca_system_score_codex":0.00000800076,"about_ca_system_score_gemma":0.00008161635,"threshold_uncertainty_score":0.99990445},"labels":[],"label_agreement":null},{"id":"W2887867625","doi":"10.1029/2018je005633","title":"Penetrative Convection in Super‐Earth Planets: Consequences of MgSiO<sub>3</sub> Postperovskite Dissociation Transition and Implications for Super‐Earth GJ 876 d","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Planets","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; Directorate for Computer and Information Science and Engineering; National Science Foundation","keywords":"Mantle (geology); Layering; Mantle convection; Planet; Geology; Convection; Transition zone; Geophysics; Thermodynamics; Physics; Astrophysics; Lithosphere","score_opus":0.03471584756506839,"score_gpt":0.3068035038961811,"score_spread":0.2720876563311127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887867625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972308,0.00013756454,0.00007893973,0.00081666856,0.00017822407,0.00045559215,0.00090970605,0.0000070993815,0.00018537766],"genre_scores_gemma":[0.9986473,0.00032486,0.00017096197,0.00004331068,0.0004914195,0.0000049209966,0.00029626512,0.0000061591686,0.0000148192175],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978074,0.00040732988,0.00054776185,0.000255797,0.0005452513,0.00043648604],"domain_scores_gemma":[0.9976874,0.0011739578,0.00022907746,0.0001271923,0.00057992054,0.0002024717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012581717,0.00015641985,0.00042021976,0.00025486518,0.00026911517,0.0001074399,0.00018968593,0.00012330843,0.00008601469],"category_scores_gemma":[0.00024051267,0.00012648123,0.0000734395,0.00031045853,0.0004916982,0.00049972656,0.000012376339,0.00029825314,0.000024603354],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015799598,0.00019067276,0.020466864,0.000126576,0.000101450154,0.000016172306,0.0020413937,0.00015217153,0.9645233,0.0011270269,0.0006307836,0.009043629],"study_design_scores_gemma":[0.001101735,0.003221425,0.8979052,0.00013419527,0.00003259515,0.000043836193,0.00034259254,0.00080073084,0.087319046,0.008305051,0.0006067247,0.0001869175],"about_ca_topic_score_codex":0.0018423183,"about_ca_topic_score_gemma":0.0028633438,"teacher_disagreement_score":0.8774383,"about_ca_system_score_codex":0.000009565482,"about_ca_system_score_gemma":0.00022880049,"threshold_uncertainty_score":0.5157755},"labels":[],"label_agreement":null},{"id":"W2888885877","doi":"10.1029/2018tc004956","title":"A New Appraisal of Lithospheric Structures of the Cordillera‐Craton Boundary Region in Western Canada","year":2018,"lang":"en","type":"article","venue":"Tectonics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Geology; Craton; Lithosphere; Precambrian; Mantle (geology); Foreland basin; Mantle plume; Geophysics; Crust; Subduction; Terrane; Kimberlite; Paleontology; Geochemistry; Tectonics","score_opus":0.008073022786481341,"score_gpt":0.210994765832266,"score_spread":0.20292174304578467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888885877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968874,0.00024162931,0.000018797238,0.000067311805,0.0010509526,0.000094578056,0.000035088826,0.0000059912572,0.0015982881],"genre_scores_gemma":[0.9994756,0.000010914981,0.00020113656,0.000051939292,0.00009110091,2.0356732e-7,0.0000055622186,0.0000027564708,0.00016076742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993018,0.00004747903,0.00019373433,0.00011434054,0.0001951249,0.00014752118],"domain_scores_gemma":[0.9995113,0.000052518808,0.0001320451,0.00023208983,0.000034167166,0.000037906077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006968042,0.00008076894,0.00017926663,0.000011789345,0.000043477805,0.000014182092,0.00024277157,0.000040579976,0.0006111447],"category_scores_gemma":[0.000024027666,0.00005306095,0.000024785048,0.00018190416,0.000085159576,0.00004366819,0.000021635775,0.00005992705,0.0000029869416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037910746,0.00004216589,0.91153854,0.000281324,0.00011136533,0.000022714363,0.0020822966,0.002061358,0.007487469,0.0008472019,0.020754246,0.054392237],"study_design_scores_gemma":[0.000254013,0.00012513167,0.9630942,0.000042385705,0.000013484268,0.000004885853,0.000040374925,0.00027766047,0.010971193,0.0006756387,0.02438825,0.000112834656],"about_ca_topic_score_codex":0.6761618,"about_ca_topic_score_gemma":0.77835053,"teacher_disagreement_score":0.10218872,"about_ca_system_score_codex":0.0000036282695,"about_ca_system_score_gemma":0.0005819656,"threshold_uncertainty_score":0.6691606},"labels":[],"label_agreement":null},{"id":"W2889144529","doi":"10.1029/2018jb015771","title":"Seismic Imaging of the North American Midcontinent Rift Using <i>S</i>‐to‐<i>P</i> Receiver Functions","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"H2020 European Research Council; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Geology; Rift; Lithosphere; Underplating; Seismology; Discontinuity (linguistics); Tectonics; Fibrous joint; Gravity anomaly; Paleontology","score_opus":0.027605030819423466,"score_gpt":0.3028696462038336,"score_spread":0.27526461538441016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889144529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974974,0.000027072469,0.00020806547,0.0007719049,0.00069810345,0.00016700772,0.00008773661,0.0000057811267,0.000536919],"genre_scores_gemma":[0.9975075,0.0000197725,0.00043561828,0.00019334293,0.0015653181,4.334261e-7,0.0000029372268,0.000007719109,0.00026736586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972402,0.00039202377,0.00046756698,0.0002061182,0.001119214,0.0005748766],"domain_scores_gemma":[0.99777114,0.00027554668,0.00034502795,0.00033390537,0.000961124,0.00031323044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008872794,0.00014323046,0.0004109613,0.00017490787,0.00037432899,0.00010171623,0.00057518284,0.000021249632,0.00019880207],"category_scores_gemma":[0.00026139102,0.00009022828,0.00019416599,0.0010846263,0.0006867,0.00025695696,0.000095721065,0.00042599655,0.00019485985],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015753242,0.0005942165,0.7659054,0.00012081225,0.00045454202,0.00007128266,0.0023780644,0.027498698,0.13313986,0.00009410538,0.022244995,0.04592273],"study_design_scores_gemma":[0.00027624608,0.0006864178,0.9645016,0.000083434665,0.000038684197,0.000018648749,0.00013691736,0.0062724594,0.008394215,0.0002940447,0.019151134,0.00014617889],"about_ca_topic_score_codex":0.0050752256,"about_ca_topic_score_gemma":0.0010480937,"teacher_disagreement_score":0.19859625,"about_ca_system_score_codex":0.000007138545,"about_ca_system_score_gemma":0.0002742206,"threshold_uncertainty_score":0.7672257},"labels":[],"label_agreement":null},{"id":"W2889916649","doi":"10.1111/ter.12358","title":"Direct observation of dislocation nucleation in pyrite using combined electron channelling contrast imaging and electron backscatter diffraction","year":2018,"lang":"en","type":"article","venue":"Terra Nova","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Austrian Science Fund","keywords":"Channelling; Electron backscatter diffraction; Misorientation; Dislocation; Nucleation; Materials science; Crystal (programming language); Crystallography; Transmission electron microscopy; Grain boundary; Condensed matter physics; Geology; Composite material; Microstructure; Nanotechnology; Chemistry","score_opus":0.019867899135389045,"score_gpt":0.2459972149319999,"score_spread":0.22612931579661086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889916649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983486,0.00006315154,0.00058789604,0.00014170638,0.00025716177,0.00016126226,0.000008752615,0.000019479956,0.00041201813],"genre_scores_gemma":[0.9994026,0.000019039777,0.0001930719,0.00006505181,0.00018522116,6.901511e-7,0.00011825764,0.000005187578,0.000010886923],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99925244,0.000050459457,0.00022181224,0.0001787187,0.00010450983,0.00019206935],"domain_scores_gemma":[0.99965775,0.000034558023,0.00014106548,0.00008788216,0.00005546146,0.000023297893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023618834,0.000094424504,0.0001509415,0.00008626221,0.00007156272,0.000044503126,0.00004940864,0.000035102265,0.00016872243],"category_scores_gemma":[0.00001221866,0.000089994246,0.000013909937,0.00015504775,0.000043630364,0.00040078154,0.0000041686176,0.000049196722,0.000011032384],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026141584,0.00004358586,0.18224098,0.000060750062,0.000018223964,7.8654205e-7,0.0010617621,0.00061771605,0.80251765,0.0001063603,0.000039154675,0.013031645],"study_design_scores_gemma":[0.00039710524,0.00012970938,0.8525668,0.000059291207,0.000019920866,0.0000017465334,0.000042246305,0.06473507,0.0814346,0.00041813962,0.000058085952,0.00013727465],"about_ca_topic_score_codex":0.0035451457,"about_ca_topic_score_gemma":0.0011437665,"teacher_disagreement_score":0.72108305,"about_ca_system_score_codex":0.000008997645,"about_ca_system_score_gemma":0.000013801721,"threshold_uncertainty_score":0.53592235},"labels":[],"label_agreement":null},{"id":"W2890953917","doi":"10.1029/2018gl079081","title":"A Numerical Model for Twin Nucleation in Shocked Zircon and Comparison With Natural Samples","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Nucleation; Geology; Shock metamorphism; Metamorphism; Shock (circulatory); Impact structure; Crust; Metamictization; Stress (linguistics); Geophysics; Petrology; Meteorite; Geochemistry; Impact crater; Astrobiology; Physics; Thermodynamics","score_opus":0.052040792729096674,"score_gpt":0.3137940702999393,"score_spread":0.2617532775708426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890953917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99486065,0.000027045022,0.002887245,0.001601954,0.00007505332,0.00038530148,0.00004310722,0.000020495994,0.00009915079],"genre_scores_gemma":[0.99632233,0.00000322686,0.0029162061,0.00029187952,0.00033925154,0.000012451035,0.00006430075,0.0000067809433,0.000043556658],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983922,0.00012457989,0.0001598782,0.00035489385,0.00042249772,0.0005458975],"domain_scores_gemma":[0.9992164,0.00038884423,0.00003324644,0.00015221085,0.00008772381,0.00012159379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035171927,0.00012168415,0.00023777166,0.0000940848,0.00018467895,0.00012038102,0.00017434648,0.000040148556,0.000045871322],"category_scores_gemma":[0.000073395655,0.00008993447,0.000027868447,0.00023011408,0.0003382632,0.00021194978,0.000022930379,0.00020168048,0.00006419901],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.012711873,0.0007812215,0.10733292,0.00066966313,0.00029036144,0.000065735505,0.014387477,0.033354815,0.6484466,0.0111717135,0.03838517,0.1324024],"study_design_scores_gemma":[0.00089263916,0.0005809542,0.22779807,0.00004037885,0.000008496846,0.0000010802313,0.00008612257,0.7642537,0.0024752377,0.0025297147,0.0010892034,0.00024439368],"about_ca_topic_score_codex":0.003228702,"about_ca_topic_score_gemma":0.0009616839,"teacher_disagreement_score":0.73089886,"about_ca_system_score_codex":0.000007623683,"about_ca_system_score_gemma":0.00003723412,"threshold_uncertainty_score":0.4880853},"labels":[],"label_agreement":null},{"id":"W2893438849","doi":"10.1029/2018gl079406","title":"Upper Mantle Seismic Structure of Alaska From Rayleigh and <i>S</i> Wave Tomography","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Seismology; Subduction; Lithosphere; Terrane; Intraplate earthquake; Mantle (geology); Seismic tomography; Crust; Volcano; Rayleigh wave; Slab; Geophysics; Tectonics; Surface wave","score_opus":0.01651020926988033,"score_gpt":0.24663366682446122,"score_spread":0.23012345755458088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893438849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99722636,0.000081355895,0.000020195814,0.00094380975,0.00028801386,0.00018134258,0.0007100555,0.000019652814,0.00052919803],"genre_scores_gemma":[0.99790853,0.000019959245,0.00038727935,0.0005530256,0.0009370509,0.0000010894656,0.00012344438,0.000007561226,0.000062077655],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9979561,0.0002034087,0.00019373564,0.00041753188,0.00066029606,0.000568926],"domain_scores_gemma":[0.9989507,0.0003477569,0.0000534494,0.00033891486,0.00011125836,0.00019791366],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018423951,0.0001602482,0.00028107184,0.00012060726,0.00019710645,0.000098858494,0.0002699933,0.000074567826,0.001280685],"category_scores_gemma":[0.000036124096,0.00012320776,0.00007263881,0.0003347201,0.0008097157,0.00017884125,0.00007753326,0.00024717802,0.00020315773],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002871931,0.00004861804,0.024234125,0.00007114936,0.00014724371,0.00003717227,0.0008943604,0.000032288877,0.9472868,0.00031813688,0.018843397,0.007799513],"study_design_scores_gemma":[0.0006630502,0.00047553462,0.8028019,0.0000646901,0.000034943587,0.0000030482042,0.00010121858,0.0010918821,0.16240121,0.016182046,0.015788151,0.00039229591],"about_ca_topic_score_codex":0.007000728,"about_ca_topic_score_gemma":0.00015897809,"teacher_disagreement_score":0.7848856,"about_ca_system_score_codex":0.0000022891045,"about_ca_system_score_gemma":0.000028079105,"threshold_uncertainty_score":0.9996323},"labels":[],"label_agreement":null},{"id":"W2895378321","doi":"10.1039/c8ra06608f","title":"Vibrational properties of isotopically enriched materials: the case of calcite","year":2018,"lang":"en","type":"article","venue":"RSC Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Calcite; Chemistry; Mineralogy; Environmental chemistry; Geology; Geochemistry","score_opus":0.015567638908216854,"score_gpt":0.23115282157078043,"score_spread":0.21558518266256357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895378321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977505,0.0005775045,0.00017283237,0.00010284568,0.0004056299,0.000109743516,0.00012078796,0.000008064325,0.000752089],"genre_scores_gemma":[0.99880415,0.000042110798,0.00076206034,0.000042021176,0.0002731317,0.0000016279362,0.00000987438,0.0000015731167,0.00006344812],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994253,0.000062421816,0.0002099093,0.00009856738,0.00010011651,0.000103720966],"domain_scores_gemma":[0.9996006,0.000051686686,0.00012005926,0.00012562497,0.0000802508,0.000021777203],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001493494,0.000065427404,0.00014533066,0.000015424646,0.00008269694,0.000020032649,0.00012916498,0.0000231769,0.0011065815],"category_scores_gemma":[0.000034452147,0.00003504749,0.000021085225,0.00006396729,0.0002422858,0.00018072389,0.00001230719,0.00001774719,0.000028877694],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023637086,0.000040819254,0.003580022,0.00021937612,0.00005347009,0.00002605905,0.0012256465,0.00027956732,0.97210544,0.008891671,0.00015880374,0.0131827295],"study_design_scores_gemma":[0.00021865313,0.00030185614,0.01853794,0.00004102111,0.000027380222,0.000049297065,0.0002475862,0.0002965608,0.9646151,0.0062841694,0.009223328,0.00015709703],"about_ca_topic_score_codex":0.0010235846,"about_ca_topic_score_gemma":0.0007550022,"teacher_disagreement_score":0.014957919,"about_ca_system_score_codex":4.4990165e-7,"about_ca_system_score_gemma":0.000025393709,"threshold_uncertainty_score":0.9998065},"labels":[],"label_agreement":null},{"id":"W2899286368","doi":"10.1002/9781119249740.ch7","title":"Frayed Edges of Cratonic Mantle Keels","year":2018,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Craton; Geology; Lithosphere; Asthenosphere; Mantle (geology); Keel; Seismogram; Geophysics; Low-velocity zone; Downwelling; Seismology; Upwelling; Tectonics","score_opus":0.008640290109175,"score_gpt":0.20287011329748242,"score_spread":0.19422982318830742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899286368","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.041552458,0.0017550143,0.000108743996,0.0000413407,0.003029318,0.0008080415,0.0017032903,0.00031529108,0.9506865],"genre_scores_gemma":[0.49673146,0.0010660286,0.0019488087,0.00020188451,0.006721749,0.000032996464,0.0012870564,0.00034428493,0.49166575],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99845374,0.00007324256,0.00028475965,0.00044035134,0.00032779918,0.00042013306],"domain_scores_gemma":[0.99893224,0.00005872979,0.00028404628,0.00053943944,0.000041227933,0.00014429224],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00008783528,0.00034142303,0.0006638803,0.00019741125,0.00005830165,0.00004539067,0.00045765305,0.00027564357,0.019245232],"category_scores_gemma":[0.000007757749,0.00027491932,0.00025285542,0.00031256798,0.00031944792,0.000056388628,0.000036579582,0.000118714444,0.0040567247],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009475201,0.00018173363,0.004081663,0.0003975961,0.00054325577,0.000018344945,0.000092500624,0.000010768236,0.00089228596,0.0013456643,0.9587401,0.03360134],"study_design_scores_gemma":[0.00031883141,0.00043050217,0.028251553,0.0002156966,0.00014280842,9.74777e-7,0.00001351827,0.00004442496,0.0019134308,0.00543202,0.9626331,0.0006031914],"about_ca_topic_score_codex":0.004300214,"about_ca_topic_score_gemma":0.00044423813,"teacher_disagreement_score":0.45902076,"about_ca_system_score_codex":8.690619e-7,"about_ca_system_score_gemma":0.000040768115,"threshold_uncertainty_score":0.9999703},"labels":[],"label_agreement":null},{"id":"W2900498917","doi":"10.1002/anie.201704364","title":"Modulated Structure Calculated for Superconducting Hydrogen Sulfide","year":2017,"lang":"en","type":"article","venue":"Angewandte Chemie International Edition","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Superconductivity; Tetragonal crystal system; Metadynamics; Electron diffraction; Chemistry; Hydrogen; Anisotropy; Crystallography; Chemical physics; Electron; Condensed matter physics; Materials science; Crystal structure; Molecular dynamics; Diffraction; Computational chemistry; Physics","score_opus":0.02156155735169382,"score_gpt":0.25694114667753665,"score_spread":0.23537958932584283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900498917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927065,0.000029542576,0.0002561128,0.00062004605,0.00284414,0.00015328066,0.001655628,0.000039909,0.0016948783],"genre_scores_gemma":[0.9933614,0.000010590334,0.00028892088,0.00008968545,0.0021928796,0.0000033383478,0.0037549024,0.0000058238747,0.00029246573],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992251,0.000008291731,0.00016806573,0.00022705918,0.00019768265,0.00017383588],"domain_scores_gemma":[0.99940336,0.000040341285,0.00014473291,0.0001955689,0.00015514667,0.0000608262],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011128951,0.00011438308,0.00012554147,0.00003403735,0.0003336057,0.00022225555,0.0003175733,0.00009110882,0.0018151286],"category_scores_gemma":[0.00014154895,0.00010126132,0.00006284632,0.000019824416,0.00004820225,0.00057197874,0.0000185198,0.00006110788,0.00003146184],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010220513,0.00002006194,0.008178905,0.000032896183,0.00018492909,0.000012045003,0.00017550253,0.0012365282,0.9812845,0.00037495894,0.0053051133,0.003092357],"study_design_scores_gemma":[0.00046232075,0.000021827107,0.020452265,0.000023012542,0.000023843257,0.000007963137,0.000018185108,0.0020199353,0.959575,0.005858001,0.011379673,0.00015800381],"about_ca_topic_score_codex":0.0013796359,"about_ca_topic_score_gemma":0.00026834614,"teacher_disagreement_score":0.021709528,"about_ca_system_score_codex":0.0000074290742,"about_ca_system_score_gemma":0.000020813668,"threshold_uncertainty_score":0.99909735},"labels":[],"label_agreement":null},{"id":"W2900851192","doi":"10.1038/s41561-018-0263-9","title":"Basal continental mantle lithosphere displaced by flat-slab subduction","year":2018,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":194,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Compute Canada; National Science Foundation","keywords":"Geology; Subduction; Lithosphere; Mantle wedge; Slab window; Convergent boundary; Mantle (geology); Eclogitization; Slab; Asthenosphere; Collision zone; Continental collision; Continental crust; Obduction; Hotspot (geology); Plate tectonics; Oceanic crust; Geophysics; Seismology; Tectonics","score_opus":0.003141598381215959,"score_gpt":0.20779267678992913,"score_spread":0.20465107840871316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900851192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99071574,0.00042057695,0.0002004279,0.00042225505,0.003789081,0.0001458727,0.0003144109,0.000063926236,0.0039276895],"genre_scores_gemma":[0.9925243,0.000010935264,0.0007771374,0.00042247074,0.00067272654,0.0000011040001,0.00011602793,0.0000041679564,0.0054711136],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99854237,0.000048036767,0.00016021072,0.0004362639,0.0003970134,0.00041611594],"domain_scores_gemma":[0.9994211,0.00003927726,0.00008585002,0.0002371604,0.00007989542,0.00013670503],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031100897,0.00015702644,0.00015913765,0.00002765207,0.00033774803,0.00015489607,0.00038031323,0.00017843895,0.0025652645],"category_scores_gemma":[0.00005367647,0.00012130762,0.000040953324,0.00031388766,0.00028991894,0.0004054936,0.00002779534,0.00021244034,0.00072307186],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005509969,0.0001523567,0.26806736,0.00010000286,0.00005919303,0.00008990957,0.00094004895,0.000035375066,0.28338024,0.0021460005,0.40958455,0.03489394],"study_design_scores_gemma":[0.0008887759,0.00063601515,0.48637864,0.00005227165,0.000037623384,0.00005230668,0.00015073273,0.0028550471,0.057591494,0.0030893653,0.44740447,0.00086326344],"about_ca_topic_score_codex":0.0015872491,"about_ca_topic_score_gemma":0.00078923436,"teacher_disagreement_score":0.22578876,"about_ca_system_score_codex":0.0000037744971,"about_ca_system_score_gemma":0.00004028532,"threshold_uncertainty_score":0.9983465},"labels":[],"label_agreement":null},{"id":"W2902750392","doi":"10.1016/j.epsl.2018.11.025","title":"Diamond destruction and growth during mantle metasomatism: An experimental study of diamond resorption features","year":2018,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Eidgenössische Technische Hochschule Zürich; Dalhousie University","keywords":"Kimberlite; Geology; Dissolution; Mantle (geology); Metasomatism; Diamond; Silicate; Geochemistry; Carbonate; Mineralogy; Eclogite; Materials science; Subduction; Tectonics; Chemical engineering; Paleontology; Metallurgy","score_opus":0.008091639110741658,"score_gpt":0.20275047162854146,"score_spread":0.1946588325177998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902750392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989919,0.0001825686,0.0000026388498,0.000049212547,0.00036518226,0.00021514237,0.00006339729,0.000021078265,0.000108860724],"genre_scores_gemma":[0.9991048,0.0000178742,0.00054534123,0.00008461338,0.00018016632,8.5581786e-7,0.000050703107,0.0000026658377,0.000013000777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875295,0.000085534644,0.00017263216,0.00038581755,0.00032688509,0.00027616977],"domain_scores_gemma":[0.9995344,0.000030338673,0.00008831951,0.00016384326,0.000019392646,0.00016369714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002844683,0.00014323487,0.00017983078,0.00014242818,0.0004241446,0.00014731169,0.000159138,0.00003084223,0.00017863703],"category_scores_gemma":[0.00000897974,0.00011678632,0.000011756762,0.00018356099,0.00052550633,0.0008846752,0.000023162307,0.00006625314,0.0000118569305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013973302,0.000056292978,0.6501683,0.000028463908,0.000018414354,0.000023404555,0.0031982926,0.00013300286,0.3449503,0.000023358994,0.00006304402,0.0011973922],"study_design_scores_gemma":[0.00032473836,0.0007099352,0.9695348,0.0000086974915,0.000016035572,0.000037029047,0.00041759762,0.00026654036,0.028477307,0.000040399467,0.000021608525,0.00014529665],"about_ca_topic_score_codex":0.0045622005,"about_ca_topic_score_gemma":0.0010594013,"teacher_disagreement_score":0.3193665,"about_ca_system_score_codex":0.0000010362431,"about_ca_system_score_gemma":0.000010369996,"threshold_uncertainty_score":0.6896713},"labels":[],"label_agreement":null},{"id":"W2904193169","doi":"","title":"Laboratory Measurements of Static And Dynamic Bulk Moduli In Carbonate","year":2010,"lang":"en","type":"article","venue":"44th U.S. Rock Mechanics Symposium and 5th U.S.-Canada Rock Mechanics Symposium","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Materials science; Porosity; Static pressure; Composite material; Bulk modulus; Carbonate; Ultrasonic sensor; Mineralogy; Calcite; Modulus; Geology; Thermodynamics; Metallurgy; Acoustics; Physics","score_opus":0.006645968567277284,"score_gpt":0.19256618739568887,"score_spread":0.1859202188284116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904193169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9725364,0.0023628562,0.0048690056,0.0019001045,0.01003494,0.0025482418,0.0033426112,0.00020022625,0.0022056517],"genre_scores_gemma":[0.99809426,0.0007477258,0.00028453284,0.00036397736,0.00011049429,0.000020550442,0.00014048735,0.000052309217,0.00018567324],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99546427,0.00022588822,0.0010407387,0.0010508568,0.0011540467,0.00106418],"domain_scores_gemma":[0.997662,0.00016138524,0.00051276595,0.0007113356,0.00033354413,0.0006189372],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0009603498,0.00071929087,0.0010022373,0.0002955669,0.00038106582,0.00014304316,0.00061039644,0.00037576508,0.00024536805],"category_scores_gemma":[0.000062160325,0.0007004399,0.00008156868,0.00051290414,0.000014941896,0.00040456344,0.00019333603,0.00057892,0.000014004314],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038315725,0.0002500868,0.0039504673,0.0012630612,0.00033682867,0.000117038406,0.0009795015,0.08007932,0.9067468,0.004799365,0.00068905007,0.000405335],"study_design_scores_gemma":[0.0044109747,0.0010615382,0.0015078797,0.00037239157,0.0004944898,0.00008681327,0.0004483262,0.90386856,0.06641882,0.012976022,0.005528727,0.002825446],"about_ca_topic_score_codex":0.12597686,"about_ca_topic_score_gemma":0.51440775,"teacher_disagreement_score":0.840328,"about_ca_system_score_codex":0.00005327423,"about_ca_system_score_gemma":0.000996047,"threshold_uncertainty_score":0.9995447},"labels":[],"label_agreement":null},{"id":"W2904546999","doi":"10.3390/min8120591","title":"Equation of State of a Natural Chromian Spinel at Ambient Temperature","year":2018,"lang":"en","type":"article","venue":"Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Chinese Academy of Sciences; Argonne National Laboratory; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Spinel; Isothermal process; Equation of state; Diamond anvil cell; Bulk modulus; Materials science; Thermodynamics; Synchrotron; Volume (thermodynamics); Analytical Chemistry (journal); Diffraction; Mineralogy; Chemistry; High pressure; Metallurgy; Composite material; Physics","score_opus":0.011442328384002182,"score_gpt":0.21424351304108671,"score_spread":0.20280118465708452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904546999","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99807245,0.00016323478,0.000002608527,0.000069147485,0.00050411274,0.00010469061,0.0002286124,0.000008263585,0.00084691227],"genre_scores_gemma":[0.9972582,0.000011654524,0.00025545497,0.0000575989,0.00018944332,4.9735013e-7,0.00014092187,0.0000022153697,0.0020839984],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993212,0.000036488782,0.00021296775,0.00012648944,0.00016305552,0.00013980505],"domain_scores_gemma":[0.9995851,0.000019407431,0.00012664335,0.00014059887,0.00009013788,0.000038135786],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014251762,0.000080718506,0.00018353759,0.000037890342,0.000041012077,0.000013595578,0.00010113482,0.000029140509,0.00114903],"category_scores_gemma":[0.000017873095,0.000058497448,0.00003741987,0.00010150314,0.00007721706,0.00008424066,0.000013592941,0.000028052547,0.00007964637],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046712994,0.000009341765,0.0014191098,0.00003126528,0.00001404416,0.0000010795388,0.0002634185,0.00015326726,0.99496007,0.000031643453,0.0024265079,0.00064355775],"study_design_scores_gemma":[0.0003430045,0.00028338833,0.11407199,0.00004088837,0.000015415446,0.0000018517098,0.000009086821,0.0009547528,0.87879753,0.00039916532,0.0049495497,0.0001333876],"about_ca_topic_score_codex":0.0015885949,"about_ca_topic_score_gemma":0.0010331203,"teacher_disagreement_score":0.11616252,"about_ca_system_score_codex":0.0000017629178,"about_ca_system_score_gemma":0.000017740185,"threshold_uncertainty_score":0.999764},"labels":[],"label_agreement":null},{"id":"W2908729320","doi":"10.4095/213166","title":"Field-based feasibility study of teleseismic surveys at high northern latitudes, Northwest Territories and Nunavut","year":2002,"lang":"en","type":"book","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Latitude; Field (mathematics); Physical geography; Geography; Earth science; Geodesy","score_opus":0.015882287396198087,"score_gpt":0.20842898898519902,"score_spread":0.19254670158900092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908729320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98138124,0.00018143957,0.0000057687093,0.000028416238,0.0007014387,0.00075213664,0.0021845791,0.00004940491,0.014715599],"genre_scores_gemma":[0.9416539,0.00002730608,0.000045322275,0.00003797003,0.00026762704,0.0000028011323,0.0013654141,0.000011899175,0.05658773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979559,0.00027188548,0.0004996363,0.00055325736,0.00044687727,0.0002724515],"domain_scores_gemma":[0.9985218,0.00040985897,0.00027354274,0.00055283407,0.00011478838,0.00012715558],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047872143,0.0003734236,0.0007415821,0.00007336919,0.00015778685,0.00006830542,0.0003052688,0.00024384551,0.0038799362],"category_scores_gemma":[0.000025604482,0.00028986367,0.00007428047,0.000059822978,0.00010811668,0.000092098104,0.00005176706,0.00016020249,0.00006607684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047359852,0.00016037066,0.99655235,0.00018137897,0.00009235904,0.000020325946,0.00017123997,0.00018291445,0.000004888365,0.000014132725,0.0012015293,0.0013711591],"study_design_scores_gemma":[0.0007505539,0.0013813595,0.9885351,0.0000481803,0.00011586077,0.000001443673,0.000024122382,0.00007989715,0.00007016825,0.00056808046,0.0079589235,0.0004663222],"about_ca_topic_score_codex":0.16630058,"about_ca_topic_score_gemma":0.8197602,"teacher_disagreement_score":0.6534596,"about_ca_system_score_codex":0.000014169579,"about_ca_system_score_gemma":0.00012785503,"threshold_uncertainty_score":0.99995536},"labels":[],"label_agreement":null},{"id":"W2908797411","doi":"10.1029/2018jb016627","title":"<i>P</i> Wave Teleseismic Traveltime Tomography of the North American Midcontinent","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"National Science Foundation","keywords":"Geology; Seismology; Rift; Terrane; Mantle (geology); Subduction; Crust; Lithosphere; Bouguer anomaly; Geophysics; Tectonics; Paleontology; Gravity anomaly","score_opus":0.017837295537918567,"score_gpt":0.26188113630407267,"score_spread":0.2440438407661541,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908797411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974841,0.000069187176,0.000006610143,0.00041162022,0.00041375053,0.00025644645,0.000092111615,0.0000049586374,0.0012612344],"genre_scores_gemma":[0.9987074,0.00008009712,0.00016004092,0.000084649124,0.00048551738,5.617799e-7,0.0000057510074,0.000007370607,0.0004685827],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967148,0.0004294672,0.00054427,0.00020922242,0.0015056885,0.00059658044],"domain_scores_gemma":[0.99791944,0.0004605833,0.0004479916,0.00039779826,0.00051558914,0.00025858707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009352076,0.0001644436,0.00060319254,0.00018263412,0.00012378633,0.00008062942,0.00067116955,0.000037866903,0.00037580184],"category_scores_gemma":[0.000113775146,0.000095571624,0.00037723206,0.0009921718,0.0004633629,0.00020929551,0.000068944464,0.0006039173,0.00019052056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001901979,0.0010099577,0.80325645,0.0003824431,0.00088027155,0.00014579555,0.0017991002,0.0052827643,0.08402052,0.00065931556,0.006673772,0.0939876],"study_design_scores_gemma":[0.00038606368,0.0010398548,0.9834749,0.000057225687,0.00002097512,0.000011445303,0.00008340493,0.0008700483,0.006954776,0.00060125097,0.006375578,0.0001244807],"about_ca_topic_score_codex":0.0022790344,"about_ca_topic_score_gemma":0.00040341186,"teacher_disagreement_score":0.18021841,"about_ca_system_score_codex":0.0000034620289,"about_ca_system_score_gemma":0.00021795358,"threshold_uncertainty_score":0.41147664},"labels":[],"label_agreement":null},{"id":"W2909981771","doi":"10.1029/2018gl081011","title":"Crustal Structure in Alaska From Receiver Function Analysis","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Crust; Receiver function; Underplating; Seismology; Isostasy; Mantle (geology); Upper crust; Oceanic crust; Tectonics; Lithosphere; Subduction; Geophysics","score_opus":0.015178299849226057,"score_gpt":0.2532966569183458,"score_spread":0.23811835706911974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909981771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99751055,0.000029989702,0.000019093733,0.00067937624,0.00038500878,0.00022607596,0.00031805446,0.000021708041,0.00081013463],"genre_scores_gemma":[0.99833655,0.0000071700574,0.00008203929,0.00032610516,0.00040765284,0.0000019775496,0.0005496316,0.0000053181693,0.00028357888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975019,0.00033391884,0.00019600031,0.0005159269,0.0008310992,0.0006211343],"domain_scores_gemma":[0.99898565,0.00038541085,0.000042226802,0.00038048896,0.000058713344,0.00014748404],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00029871022,0.00014836923,0.00032612565,0.0002942518,0.00009275654,0.00015357902,0.00031594042,0.00008475356,0.008689089],"category_scores_gemma":[0.000040155333,0.00012102275,0.000116924035,0.0011936837,0.00010366634,0.00029441426,0.000044213743,0.00042491118,0.0024053296],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009262686,0.00010401835,0.6669839,0.00004957115,0.0008242586,0.00010216872,0.00075725716,0.025019635,0.28198013,0.00037287048,0.008249846,0.01463005],"study_design_scores_gemma":[0.0003008874,0.000085672364,0.9901373,0.000008775785,0.000042553056,1.01276655e-7,0.000054558986,0.0023770486,0.00057590124,0.0019562882,0.0042974744,0.00016344718],"about_ca_topic_score_codex":0.023952756,"about_ca_topic_score_gemma":0.0025084105,"teacher_disagreement_score":0.32315338,"about_ca_system_score_codex":0.000011859251,"about_ca_system_score_gemma":0.000036147885,"threshold_uncertainty_score":0.9983714},"labels":[],"label_agreement":null},{"id":"W2910387435","doi":"10.1029/2018jb016482","title":"Extrinsic Elastic Anisotropy in a Compositionally Heterogeneous Earth's Mantle","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"H2020 European Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Anisotropy; Geology; Layering; Seismic anisotropy; Mantle (geology); Isotropy; Geophysics; Basalt; Crust; Mineralogy; Seismology; Optics; Physics","score_opus":0.02331398454708357,"score_gpt":0.2945363944568419,"score_spread":0.2712224099097583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910387435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976337,0.00014554194,0.00003923161,0.00018155268,0.00043055258,0.00022273205,0.0000694757,0.00000810946,0.0012691044],"genre_scores_gemma":[0.9983214,0.00009326343,0.00044502725,0.000057431596,0.0005966704,8.583555e-7,0.000021104086,0.000008549171,0.00045567416],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99682844,0.00041318216,0.0005107288,0.00026335756,0.0013016823,0.0006825866],"domain_scores_gemma":[0.9983373,0.0006055401,0.00016714947,0.00024395029,0.00033954735,0.00030649477],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009775265,0.0001683098,0.0005129327,0.00029576579,0.00011222173,0.00017328827,0.00044150878,0.00007951846,0.0019268169],"category_scores_gemma":[0.00009120946,0.00013141107,0.00016601568,0.0004197402,0.00013095881,0.00035458338,0.000054973843,0.00060772523,0.0017839249],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0101729585,0.0037040906,0.16424166,0.0009942389,0.001083825,0.008201029,0.0019891267,0.17597096,0.5459947,0.015835082,0.003836713,0.06797559],"study_design_scores_gemma":[0.0024454985,0.0042576646,0.9412814,0.00031630447,0.000024295565,0.0002170363,0.00007425206,0.014521907,0.008554588,0.013981089,0.013852882,0.00047311166],"about_ca_topic_score_codex":0.00059960276,"about_ca_topic_score_gemma":0.00024151243,"teacher_disagreement_score":0.7770397,"about_ca_system_score_codex":0.000007728403,"about_ca_system_score_gemma":0.00024205164,"threshold_uncertainty_score":0.9989933},"labels":[],"label_agreement":null},{"id":"W2911229747","doi":"10.1107/s0108767318099075","title":"Magnetic moment fragmentation in Nd<sub>2</sub>ScNbO<sub>7</sub>","year":2018,"lang":"en","type":"article","venue":"Acta Crystallographica Section A Foundations and Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg; McMaster University; Brockhouse Institute for Materials Research; Canadian Institute for Advanced Research; University of Manitoba","funders":"","keywords":"Fragmentation (computing); Magnetic moment; Materials science; Atomic physics; Physics; Condensed matter physics; Computer science","score_opus":0.006940780778696715,"score_gpt":0.21811045083906933,"score_spread":0.2111696700603726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911229747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99637634,0.0004001256,0.0006510885,0.0003107515,0.0009419623,0.00033658487,0.00006158142,0.00006534098,0.00085621607],"genre_scores_gemma":[0.9968146,0.002215256,0.00024115016,0.00012137439,0.0003273312,0.000023780613,0.00023524353,0.000007765386,0.000013475323],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99857247,0.00009962143,0.00034812954,0.00042328727,0.00023726324,0.0003192161],"domain_scores_gemma":[0.9993829,0.00008159513,0.00015477241,0.00017633974,0.000090301575,0.00011404855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023406166,0.00020095658,0.00020467676,0.0003362501,0.000472711,0.00023447936,0.000108268745,0.00008537374,0.00027915154],"category_scores_gemma":[0.00001902135,0.00018663409,0.000053796884,0.0006917798,0.00026160319,0.0008750296,0.000018886285,0.000112716596,0.000012775587],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000098393386,0.000116975,0.029856376,0.00006293791,0.000039703118,0.000004950815,0.0004262526,0.00040074936,0.8873029,0.00040015197,0.00019425571,0.08109639],"study_design_scores_gemma":[0.0018051415,0.0016729856,0.7737439,0.00013418203,0.00011267972,0.00003627999,0.0008425883,0.0025515708,0.016942998,0.022221146,0.17890167,0.001034856],"about_ca_topic_score_codex":0.0002634083,"about_ca_topic_score_gemma":0.006665199,"teacher_disagreement_score":0.8703599,"about_ca_system_score_codex":0.000007689174,"about_ca_system_score_gemma":0.00003320031,"threshold_uncertainty_score":0.76107174},"labels":[],"label_agreement":null},{"id":"W2912400917","doi":"10.1139/cjes-2018-0232","title":"Crustal density structure of the northwestern Iranian Plateau","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Institute for Advanced Studies in Basic Sciences; Chinese Academy of Sciences","keywords":"Geology; Crust; Plateau (mathematics); Fibrous joint; Seismology; Tectonics; Continental crust; Fault (geology); Gravity anomaly; Receiver function; Structural basin; Geophysics; Geomorphology; Lithosphere; Paleontology","score_opus":0.008292054269181512,"score_gpt":0.1779468789565308,"score_spread":0.1696548246873493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912400917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967307,0.00011537939,0.0000015104699,0.00013720697,0.0017840863,0.00006945254,0.0001286371,0.000001189284,0.0010318767],"genre_scores_gemma":[0.99954313,0.0000026837297,0.00011290688,0.00010759407,0.000114743634,8.508326e-9,0.0000013564644,0.0000012804958,0.00011630836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999065,0.000052662108,0.00023037083,0.00010492851,0.00029060195,0.0002564528],"domain_scores_gemma":[0.9992519,0.000037547507,0.0002473505,0.00012537757,0.000089901376,0.00024794944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002749331,0.00008043044,0.00018039232,0.00009255629,0.00020200356,0.00010324011,0.0005324686,0.00004042644,0.0019054104],"category_scores_gemma":[0.00002119509,0.00004632951,0.00007106107,0.00024170795,0.00028065775,0.0002687191,0.0000069288653,0.000106676736,0.00002814823],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000004872401,0.0000010234298,0.9939717,0.00000808048,0.000008905015,0.000009581939,0.00043750167,0.0028717655,0.0022321464,0.000102343845,0.000036764835,0.00031529812],"study_design_scores_gemma":[0.000104372586,0.00011751058,0.99422324,0.00003302826,0.000009370295,0.00005256452,0.00016519339,0.00006442221,0.0027287544,0.00053074607,0.0019004773,0.00007030304],"about_ca_topic_score_codex":0.042449497,"about_ca_topic_score_gemma":0.5962536,"teacher_disagreement_score":0.5538041,"about_ca_system_score_codex":7.250707e-7,"about_ca_system_score_gemma":0.0008995779,"threshold_uncertainty_score":0.999007},"labels":[],"label_agreement":null},{"id":"W2913963901","doi":"10.1029/gm072p0081","title":"Numerical Calculation of Modes of Oscillation of the Earth's Core","year":2011,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Earth (classical element); Geology; Oscillation (cell signaling); Geophysics; Core (optical fiber); Inner core; Physics; Geodesy; Optics; Mathematical physics","score_opus":0.023530789250767733,"score_gpt":0.2002705991252273,"score_spread":0.17673980987445956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913963901","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.80141383,0.0003331952,0.00021119574,0.000024515908,0.00074478425,0.0007105944,0.0010294856,0.000030388233,0.195502],"genre_scores_gemma":[0.9969025,0.000038750346,0.00016347923,0.000007635862,0.00011180281,7.080247e-7,0.00010064913,0.000008551476,0.0026658685],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9987261,0.00003137118,0.00047440673,0.00022298156,0.00039394354,0.0001511944],"domain_scores_gemma":[0.9987194,0.000082641214,0.00061979145,0.00038611353,0.00013851906,0.00005353672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008822249,0.00020672026,0.00055085035,0.00008284613,0.00004489795,0.0000059505237,0.00025703644,0.00018466075,0.0004374478],"category_scores_gemma":[0.000009399063,0.00014128062,0.00036137248,0.00010281609,0.0003010896,0.000069705275,0.000027571215,0.00012316948,0.00002325274],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012993815,0.00045013256,0.08804927,0.0021738342,0.001646124,0.000007034189,0.0023150314,0.020671608,0.04180629,0.7522596,0.0011636871,0.08815802],"study_design_scores_gemma":[0.00043470738,0.0005921727,0.72910047,0.00042165825,0.00040939584,0.0000013912405,0.000008424872,0.0028677168,0.012158054,0.24840708,0.0049943,0.00060465944],"about_ca_topic_score_codex":0.002098328,"about_ca_topic_score_gemma":0.000054416356,"teacher_disagreement_score":0.6410512,"about_ca_system_score_codex":7.89078e-7,"about_ca_system_score_gemma":0.000036986257,"threshold_uncertainty_score":0.5761257},"labels":[],"label_agreement":null},{"id":"W2914555249","doi":"10.1007/s00269-019-01023-3","title":"Equations of state of Co2TiO4-Sp, Co2TiO4-CM, and Co2TiO4-CT, and their phase transitions: an experimental and theoretical study","year":2019,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Science Foundation","keywords":"Chemistry; Spinel; Isothermal process; Phase (matter); Synchrotron radiation; Analytical Chemistry (journal); Bulk modulus; Crystallography; Mineralogy; Thermodynamics; Optics; Materials science; Metallurgy; Physics","score_opus":0.01167281728185835,"score_gpt":0.2449488447229173,"score_spread":0.23327602744105896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914555249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99787664,0.00050659466,0.000036897334,0.000028632308,0.00002206216,0.0002223485,0.0009631117,0.0000052216096,0.00033851186],"genre_scores_gemma":[0.99967533,0.00006637092,0.000056721485,0.0000089903815,0.000032291144,0.0000028349948,0.000120097764,0.0000043502264,0.00003302217],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99923897,0.000039936906,0.00026297802,0.00021871431,0.00012145248,0.000117927164],"domain_scores_gemma":[0.99948245,0.00010257853,0.0001290424,0.00014435056,0.00005163797,0.000089963665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015744039,0.00014237547,0.00035527104,0.000012987748,0.00005257527,0.000027525279,0.000058685324,0.000019551373,0.0001718834],"category_scores_gemma":[0.00000560711,0.00011421701,0.000025089159,0.000048345908,0.00035849123,0.0001384486,0.000017931496,0.000042646807,3.783425e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000091703136,0.00040537416,0.0027593737,0.00020287876,0.000061029506,0.0000010242599,0.0019489088,0.000051746127,0.99177486,0.0012195508,0.00001018467,0.0014733875],"study_design_scores_gemma":[0.0033871643,0.0011124319,0.005130691,0.00008464987,0.00010620487,0.000010371375,0.003054217,0.0061846706,0.9693182,0.011225231,0.000052965304,0.00033320553],"about_ca_topic_score_codex":0.00017321958,"about_ca_topic_score_gemma":0.000008032564,"teacher_disagreement_score":0.022456642,"about_ca_system_score_codex":6.866086e-7,"about_ca_system_score_gemma":0.000016307604,"threshold_uncertainty_score":0.46576345},"labels":[],"label_agreement":null},{"id":"W2917203534","doi":"10.1029/2018jb016352","title":"Shear Wave Splitting Discloses Two Episodes of Collision‐Related Convergence in Western North America","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismic anisotropy; Shear wave splitting; Lithosphere; Anisotropy; Seismology; Crust; Mantle (geology); Foothills; Shear (geology); Geophysics; Tectonics; Petrology","score_opus":0.02845841047324545,"score_gpt":0.30994770144395184,"score_spread":0.2814892909707064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2917203534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983512,0.00012498241,0.000012703603,0.00016030307,0.00033900444,0.00024345885,0.000075104756,0.0000059052513,0.0006872977],"genre_scores_gemma":[0.9987495,0.00023390626,0.0002748851,0.000023278968,0.00022959373,6.7141855e-7,0.000016514052,0.000008079522,0.00046356404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99648154,0.00050654233,0.00082699384,0.00026656623,0.0012737692,0.0006445674],"domain_scores_gemma":[0.9976195,0.0009711621,0.00041372748,0.00028004567,0.00043530817,0.0002802717],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001188795,0.0001738392,0.00073244167,0.00026034037,0.00009256377,0.000085438514,0.00044695454,0.00006205098,0.00096095353],"category_scores_gemma":[0.0002937911,0.00012705875,0.00016319311,0.0007864364,0.00027978118,0.00047609457,0.000082042665,0.00062396476,0.0005518402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010415671,0.0005430488,0.91854143,0.00030750805,0.00021188257,0.000387128,0.002787225,0.03531043,0.021602305,0.0003738499,0.00023908193,0.018654542],"study_design_scores_gemma":[0.00094511034,0.0013156163,0.981995,0.00026542868,0.000014565887,0.000013162104,0.00026584146,0.008037319,0.0036582616,0.0018626561,0.001425381,0.0002016968],"about_ca_topic_score_codex":0.0036103025,"about_ca_topic_score_gemma":0.0004186381,"teacher_disagreement_score":0.063453525,"about_ca_system_score_codex":0.000007139294,"about_ca_system_score_gemma":0.0002394585,"threshold_uncertainty_score":0.9999523},"labels":[],"label_agreement":null},{"id":"W2917766788","doi":"10.1093/gji/ggz108","title":"Using commercial finite-element packages for the study of Glacial Isostatic Adjustment on a compressible self-gravitating spherical earth – 1: harmonic loads","year":2019,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Glaucoma Research Foundation","keywords":"Compressibility; Finite element method; Geology; Nonlinear system; Instability; Mechanics; Mathematical analysis; Physics; Mathematics","score_opus":0.03522343607873199,"score_gpt":0.2922649135741611,"score_spread":0.25704147749542916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2917766788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99503297,0.00003229966,0.0015413959,0.00018242338,0.002184277,0.0005811153,0.0001565999,0.000011439509,0.00027750782],"genre_scores_gemma":[0.99701774,0.000010379817,0.0016024857,0.00017189224,0.0010753195,0.0000054174247,0.000032862237,0.0000074582613,0.0000764246],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9982585,0.00014465138,0.00044031616,0.00020635259,0.0006719541,0.00027826047],"domain_scores_gemma":[0.9984935,0.00078393234,0.00033392568,0.00014572003,0.00015764927,0.00008527343],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029995877,0.00017191755,0.00029388125,0.000048711365,0.00022682892,0.00015337857,0.00041239857,0.000032212523,0.0009182708],"category_scores_gemma":[0.000033484896,0.000113001566,0.00014247086,0.00009312618,0.000037000133,0.0001554246,0.000043988584,0.00020774105,0.00007725176],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0055010915,0.009171196,0.17629173,0.0002735714,0.0049870033,0.000085758096,0.011436766,0.6267854,0.020990448,0.0056347507,0.0028821821,0.1359601],"study_design_scores_gemma":[0.0047001415,0.0041545746,0.78868806,0.00014761872,0.00027041294,0.000014205951,0.0016525808,0.1922385,0.0016851482,0.0030874663,0.0029311152,0.00043019227],"about_ca_topic_score_codex":0.00037802168,"about_ca_topic_score_gemma":0.000053124433,"teacher_disagreement_score":0.6123963,"about_ca_system_score_codex":0.00001227111,"about_ca_system_score_gemma":0.00006327483,"threshold_uncertainty_score":0.99999505},"labels":[],"label_agreement":null},{"id":"W2923944448","doi":"10.1038/s41598-019-41607-1","title":"Mechanism for the Structural Transformation to the Modulated Superconducting Phase of Compressed Hydrogen Sulfide","year":2019,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Western Canada Research Grid; Compute Canada; University of Saskatchewan","keywords":"Superconductivity; Crystal structure; Metastability; Metallic hydrogen; Materials science; Ambient pressure; Condensed matter physics; Hydrogen; Electronic structure; Crystallography; Thermodynamics; Chemistry; Physics; Metal","score_opus":0.021049184185798802,"score_gpt":0.24656572266065988,"score_spread":0.22551653847486108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923944448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99245185,0.00003690423,0.00043686075,0.0002882616,0.0055483887,0.0010139045,0.00008827114,0.000016662372,0.00011892141],"genre_scores_gemma":[0.9993757,6.4888883e-7,0.00012991886,0.000034609275,0.000060546405,0.0000046684236,0.00017506412,0.000002914019,0.00021592497],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99884963,0.000036775036,0.00035132366,0.0002556584,0.0003028195,0.0002038049],"domain_scores_gemma":[0.9991382,0.00008252066,0.00014780225,0.00045396303,0.00013045261,0.00004710446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010811787,0.00008694966,0.00014361387,0.000037879436,0.00035376695,0.00017102437,0.00021175013,0.000027938322,0.0004143512],"category_scores_gemma":[0.00003691587,0.000044888104,0.00006774456,0.00019070513,0.000050399678,0.00023098929,0.00001026285,0.00003642772,0.000026746566],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047033718,0.000011522275,0.00041463846,0.000053486405,0.00004955608,0.0000034890827,0.003426723,0.042764477,0.9470574,0.0010157553,0.0005827437,0.004573162],"study_design_scores_gemma":[0.0004641464,0.000119639735,0.0013792935,0.000024379126,0.00006512466,0.00004036517,0.00067808677,0.09934708,0.8627382,0.022509951,0.012425859,0.0002078993],"about_ca_topic_score_codex":0.00081165676,"about_ca_topic_score_gemma":0.00018976507,"teacher_disagreement_score":0.084319234,"about_ca_system_score_codex":0.0000015469997,"about_ca_system_score_gemma":0.00003691336,"threshold_uncertainty_score":0.45368552},"labels":[],"label_agreement":null},{"id":"W2924628040","doi":"10.1038/s41550-019-0721-3","title":"The dynamic geophysical environment of (101955) Bennu based on OSIRIS-REx measurements","year":2019,"lang":"en","type":"article","venue":"Nature Astronomy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":171,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Ontario Museum; University of Calgary; University of Toronto; University of Winnipeg; Canadian Space Agency; York University; University of British Columbia","funders":"Science and Technology Facilities Council; Canadian Space Agency; Jet Propulsion Laboratory; National Aeronautics and Space Administration; California Institute of Technology; Auburn University; Agence Nationale de la Recherche; Centre National d’Etudes Spatiales; Royal Astronomical Society","keywords":"Osiris; Geophysics; Astrobiology; Geology; Physics; Biology; Ecology","score_opus":0.004051312539339287,"score_gpt":0.18412426693645723,"score_spread":0.18007295439711793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2924628040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99146,0.00019306448,0.00015123421,0.00031675032,0.0008917647,0.0004560201,0.0001366074,0.000016581796,0.006377943],"genre_scores_gemma":[0.9986328,0.00000311518,0.00070243597,0.00008604659,0.00009488525,0.0000028724955,0.00010980154,0.000004973434,0.00036309776],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988024,0.00007361576,0.00017847163,0.00024836502,0.00042050172,0.00027659794],"domain_scores_gemma":[0.9993004,0.00012011436,0.00011726473,0.00038071632,0.000015707641,0.00006580165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023994946,0.00015252228,0.00019161541,0.000028254874,0.000092405724,0.000037609996,0.00031019986,0.00010176734,0.0007491772],"category_scores_gemma":[0.0000062304584,0.00009856584,0.00008604377,0.000053599204,0.00005443113,0.000067219575,0.000015079604,0.00023627652,0.0006924896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015567406,0.00071100186,0.5773763,0.00015377525,0.0006190216,0.0000065781073,0.0002406977,0.10225191,0.03474773,0.0013322303,0.006207396,0.27479663],"study_design_scores_gemma":[0.0008218184,0.0004660105,0.86940044,0.000033733566,0.000044342265,2.424717e-7,0.00003093924,0.004999675,0.004401989,0.0002670005,0.11927034,0.00026345506],"about_ca_topic_score_codex":0.00013292303,"about_ca_topic_score_gemma":0.000035935165,"teacher_disagreement_score":0.29202417,"about_ca_system_score_codex":0.0000073841393,"about_ca_system_score_gemma":0.000041253625,"threshold_uncertainty_score":0.8900784},"labels":[],"label_agreement":null},{"id":"W2927635446","doi":"10.5539/jmsr.v8n2p10","title":"Molecular Dynamics Study the Factors Effecting the Structure of MgSiO3 Bulk","year":2019,"lang":"en","type":"article","venue":"Journal of Materials Science Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Molecular dynamics; Materials science; Radial distribution function; Distribution (mathematics); Periodic boundary conditions; Coordination number; Thermodynamics; Distribution function; Computational chemistry; Boundary value problem; Physics; Chemistry; Quantum mechanics","score_opus":0.023387295583182185,"score_gpt":0.31397706078181864,"score_spread":0.29058976519863644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2927635446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99776304,0.000052255567,0.0000038063217,0.00015336023,0.0013849421,0.0004512879,0.000052668143,0.0000026461826,0.0001359959],"genre_scores_gemma":[0.99981606,0.000008403038,0.000026844398,0.00000809304,0.000114694776,1.839435e-7,0.0000015811803,0.0000036529557,0.00002050732],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9962712,0.0007965942,0.0004354215,0.0001762871,0.0018854917,0.0004350233],"domain_scores_gemma":[0.9980308,0.0006445697,0.00035111012,0.0003797959,0.0005031295,0.00009060816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009336079,0.00010853413,0.0002977917,0.00016888343,0.00042534125,0.00044981303,0.001583281,0.000037406968,0.00075532286],"category_scores_gemma":[0.0004546435,0.000045381672,0.0000511972,0.00064583146,0.00048558466,0.00031602525,0.00012592366,0.0002608061,0.000024151574],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006485716,0.000025306948,0.035085443,0.000028821038,0.000026059977,0.00000905613,0.0010522202,0.0022740185,0.9608399,0.00014629967,0.000011327417,0.00043668953],"study_design_scores_gemma":[0.00025087775,0.0008081941,0.39194402,0.000042066615,0.000018965675,0.000022614977,0.0029338258,0.00024732228,0.6024045,0.0011800732,0.000055035274,0.000092497576],"about_ca_topic_score_codex":0.0014105511,"about_ca_topic_score_gemma":0.00009207072,"teacher_disagreement_score":0.35843542,"about_ca_system_score_codex":0.00001656543,"about_ca_system_score_gemma":0.00037255324,"threshold_uncertainty_score":0.8270256},"labels":[],"label_agreement":null},{"id":"W2927868529","doi":"10.1063/1.5066103","title":"Electrical resistivity and thermal conductivity of W and Re up to 5 GPa and 2300 K","year":2019,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Thermal conductivity; Tungsten; Materials science; Wiedemann–Franz law; Rhenium; Condensed matter physics; Conductivity; Analytical Chemistry (journal); Chemistry; Metallurgy; Composite material; Physics","score_opus":0.0120503661902194,"score_gpt":0.2139592687663498,"score_spread":0.2019089025761304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2927868529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99858505,0.00008996711,0.000023226601,0.00003489729,0.00010090783,0.00009584799,0.000033468903,0.0000021753299,0.0010344746],"genre_scores_gemma":[0.9994666,0.000037534828,0.00026752867,0.00004399447,0.00015812475,1.4578484e-7,0.0000017731995,0.000002552846,0.000021761918],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994247,0.000027219525,0.00016001094,0.000112796704,0.00015808876,0.00011717615],"domain_scores_gemma":[0.99950635,0.00011529746,0.00016304785,0.000076649216,0.000039195183,0.00009943021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025711485,0.00008428243,0.00028736526,0.000023490376,0.000038819653,0.00003345032,0.0000595553,0.000035905476,0.000044002034],"category_scores_gemma":[0.0000071578484,0.0000628011,0.000020498592,0.00007119602,0.00005043846,0.00011510869,0.000018392027,0.00009974727,0.0000035126204],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024578841,0.00011096869,0.07770105,0.0002907513,0.00024232066,0.000012489282,0.0027111766,0.0032994845,0.7758994,0.007646039,0.001047913,0.1285805],"study_design_scores_gemma":[0.0013555475,0.0008107083,0.92970884,0.000045311805,0.00010658348,0.000016858257,0.00015755619,0.0013135292,0.049494073,0.014188636,0.0024753083,0.00032705904],"about_ca_topic_score_codex":0.00006407112,"about_ca_topic_score_gemma":0.00001010925,"teacher_disagreement_score":0.8520078,"about_ca_system_score_codex":0.00000111934,"about_ca_system_score_gemma":0.000026782447,"threshold_uncertainty_score":0.25609544},"labels":[],"label_agreement":null},{"id":"W2928694646","doi":"10.1029/2018jb016728","title":"Weak B‐Type Olivine Fabric Induced by Fast Compaction of Crystal Mush in a Crustal Magma Reservoir","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"National Natural Science Foundation of China","keywords":"Geology; Olivine; Peridotite; Ultramafic rock; Dislocation creep; Seismic anisotropy; Mafic; Petrology; Mineralogy; Geochemistry; Mantle (geology); Dislocation; Composite material; Materials science","score_opus":0.03163926346265882,"score_gpt":0.30938823547420385,"score_spread":0.277748972011545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2928694646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962552,0.00009360618,0.0000063014472,0.00022584248,0.00042973962,0.00024699362,0.000084335705,0.0000063393163,0.002651648],"genre_scores_gemma":[0.99855804,0.00007629689,0.000067869776,0.000016229182,0.0004197672,4.826898e-7,0.000026322372,0.000009255479,0.00082570594],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9964482,0.0005119421,0.0006536777,0.00024406317,0.0014758995,0.00066619116],"domain_scores_gemma":[0.998027,0.00047753297,0.0003225106,0.00027263036,0.00058644917,0.0003138338],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0015095234,0.00017798695,0.00066025025,0.00036766223,0.00008385161,0.00011374413,0.00046895945,0.00011338264,0.0014473035],"category_scores_gemma":[0.00027081193,0.00013881554,0.00014309186,0.00086543727,0.0001353227,0.00058671396,0.00006762791,0.00082972547,0.00033311424],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026274952,0.0007630555,0.030898683,0.00028568463,0.00015808266,0.00008318918,0.0008140224,0.0031607982,0.9466184,0.0002438174,0.005425345,0.008921455],"study_design_scores_gemma":[0.0022337222,0.005615301,0.9520542,0.00034829797,0.000022059732,0.000029414881,0.0007568684,0.0062388624,0.02355076,0.0019508803,0.006821739,0.00037787415],"about_ca_topic_score_codex":0.0053562503,"about_ca_topic_score_gemma":0.00048647504,"teacher_disagreement_score":0.9230676,"about_ca_system_score_codex":0.000014176149,"about_ca_system_score_gemma":0.00032444118,"threshold_uncertainty_score":0.9994655},"labels":[],"label_agreement":null},{"id":"W2937340070","doi":"10.1029/2019gl082406","title":"Seismic Evidence for Lithospheric Thinning and Heat in the northern Canadian Cordillera","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta; University of Ottawa","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; Northwestern University","keywords":"Lithosphere; Geology; Mantle (geology); Asthenosphere; Lithospheric flexure; Crust; Geophysics; Tectonics; Seismology","score_opus":0.04576985167864338,"score_gpt":0.2956939261187276,"score_spread":0.2499240744400842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937340070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98905003,0.0001740056,0.000010008457,0.009491242,0.00015184036,0.00067260896,0.000033992295,0.000008775641,0.00040750526],"genre_scores_gemma":[0.9977667,0.000024205166,0.000072125535,0.00175593,0.00023553599,0.000016556432,0.000022164997,0.0000055253267,0.00010131038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99810225,0.00026227007,0.00013375946,0.0003312021,0.00045666576,0.000713879],"domain_scores_gemma":[0.99813664,0.0013548918,0.000016498587,0.0002703321,0.000055470668,0.00016615396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009809419,0.00011377128,0.00017966279,0.00006446208,0.00023491782,0.0002325131,0.00040107832,0.000040923973,0.00019159704],"category_scores_gemma":[0.0001387777,0.00007615513,0.000040882962,0.00031307677,0.0001248229,0.00022685144,0.000023764966,0.00027607477,0.0003667814],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007622067,0.000110783854,0.86481553,0.0006749143,0.00013089822,0.00018089889,0.011181755,0.019396393,0.045238946,0.0010465435,0.01771932,0.03874182],"study_design_scores_gemma":[0.00038059932,0.00031711516,0.95920724,0.00013101385,0.000008130044,0.00000294108,0.00037790445,0.025817424,0.00010214404,0.0010722643,0.012331941,0.00025128032],"about_ca_topic_score_codex":0.4437776,"about_ca_topic_score_gemma":0.08688304,"teacher_disagreement_score":0.35689455,"about_ca_system_score_codex":0.000013147439,"about_ca_system_score_gemma":0.00012842624,"threshold_uncertainty_score":0.929779},"labels":[],"label_agreement":null},{"id":"W2938172839","doi":"10.1039/c9nr00562e","title":"Structure–property correlations in phase-pure B-doped Q-carbon high-temperature superconductor with a record <i>T</i><sub>c</sub> = 55 K","year":2019,"lang":"en","type":"article","venue":"Nanoscale","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centennial College","funders":"Division of Materials Research","keywords":"Condensed matter physics; Superconductivity; Materials science; Electrical resistivity and conductivity; Cooper pair; Fermi level; Doping; Magnetic susceptibility; Density of states; Magnetic moment; Phase (matter); Electron; Physics","score_opus":0.006638507056681398,"score_gpt":0.188154716980878,"score_spread":0.1815162099241966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2938172839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960829,0.00008853669,6.1186483e-7,0.00018880042,0.0014732743,0.0005385391,0.00051245285,0.000058248785,0.0010566536],"genre_scores_gemma":[0.9981649,0.000027175704,0.00020121699,0.00018357905,0.00025127147,0.000004757319,0.0004988074,0.00001518491,0.00065309904],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99844766,0.000112240516,0.0002787517,0.00046607738,0.0002924301,0.0004028527],"domain_scores_gemma":[0.99930215,0.000061924504,0.000081740174,0.0003615164,0.00006559307,0.00012708345],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011565316,0.00025812956,0.000392628,0.00009105024,0.000095348056,0.00010328897,0.00022949943,0.00020507455,0.0013710824],"category_scores_gemma":[0.000013955467,0.00015706453,0.00004456012,0.00035696197,0.00006809847,0.0003155544,0.000016421947,0.00028317914,0.0002908567],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000224971,0.00006576231,0.068090945,0.000040828923,0.000026823014,0.000023011162,0.0002742231,0.0004681376,0.92746216,0.000041942265,0.0012185964,0.0020625934],"study_design_scores_gemma":[0.008563161,0.0015921608,0.18815604,0.000307623,0.00013862483,0.00004768314,0.0003415658,0.0014996526,0.7738917,0.0011640529,0.022570394,0.0017273594],"about_ca_topic_score_codex":0.0027129096,"about_ca_topic_score_gemma":0.0078034815,"teacher_disagreement_score":0.15357047,"about_ca_system_score_codex":0.000007999621,"about_ca_system_score_gemma":0.000114629824,"threshold_uncertainty_score":0.9995418},"labels":[],"label_agreement":null},{"id":"W2939602882","doi":"10.1103/physrevc.99.055805","title":"Role of Landau-Rabi quantization of electron motion on the crust of magnetars within the nuclear energy density functional theory","year":2019,"lang":"en","type":"article","venue":"Physical review. C","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds De La Recherche Scientifique - FNRS; Bulgarian Academy of Sciences; European Cooperation in Science and Technology","keywords":"Magnetar; Physics; Landau quantization; Neutron star; Crust; Quantization (signal processing); Magnetic field; Electron; Condensed matter physics; Quantum electrodynamics; Quantum mechanics; Geophysics","score_opus":0.006623491249869843,"score_gpt":0.20366307352031135,"score_spread":0.1970395822704415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2939602882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99686587,0.0007042027,0.00003033909,0.000120770805,0.00008659903,0.00015377403,0.0000305717,0.0000046629193,0.002003182],"genre_scores_gemma":[0.9993022,0.00040379708,0.0000066668686,0.00014866926,0.00006512433,7.6212814e-7,0.000038425478,0.0000028117051,0.000031551474],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99913406,0.00023880217,0.00019160475,0.00010858476,0.00024484372,0.00008211629],"domain_scores_gemma":[0.99926037,0.00021758839,0.00023272543,0.00020660905,0.000065776694,0.000016916178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041156466,0.00007568809,0.00023550529,0.000011422107,0.000037658356,0.000005834308,0.00013660427,0.000017691951,0.000410791],"category_scores_gemma":[0.000050761202,0.00003776962,0.000085215106,0.000113116,0.00006470642,0.000051865056,0.0000104082355,0.000054993387,0.000056100067],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019543209,0.00013645361,0.004122378,0.00037344208,0.000068528454,1.0671027e-7,0.00020801276,0.0029474753,0.15178993,0.8327456,0.00034012308,0.00707253],"study_design_scores_gemma":[0.00040669282,0.0011913853,0.62345254,0.0007336937,0.00032862395,0.0000018272118,0.00010174344,0.013596052,0.1506635,0.20344424,0.0057545784,0.0003251247],"about_ca_topic_score_codex":0.0003720708,"about_ca_topic_score_gemma":0.000032074313,"teacher_disagreement_score":0.62930137,"about_ca_system_score_codex":0.0000011083578,"about_ca_system_score_gemma":0.000016820502,"threshold_uncertainty_score":0.44978732},"labels":[],"label_agreement":null},{"id":"W2939733642","doi":"10.1130/g46008.1","title":"Shock-produced high-pressure (La, Ce, Th)PO4 polymorph revealed by microstructural phase heritage of monazite","year":2019,"lang":"en","type":"article","venue":"Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Monazite; Library science; History; Art history; Archaeology; Geology; Geochemistry; Computer science","score_opus":0.0037999628196984073,"score_gpt":0.199992595660925,"score_spread":0.1961926328412266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2939733642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99380344,0.0012915737,0.000004874269,0.0003126542,0.0013059877,0.0002882322,0.0011060083,0.000040409457,0.0018468088],"genre_scores_gemma":[0.99352735,0.000035337373,0.00028144312,0.00017956656,0.0001756756,0.0000019677782,0.0006224829,0.00000876614,0.005167413],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9983514,0.00019977299,0.00035428995,0.00045164122,0.0001775036,0.00046536952],"domain_scores_gemma":[0.9990444,0.000115097435,0.00020311408,0.0004734251,0.000057622856,0.00010631151],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022886605,0.0002266758,0.0005270543,0.00005498511,0.00006958527,0.000030213965,0.00039997403,0.00019016248,0.009096207],"category_scores_gemma":[0.000023667979,0.00018701216,0.00007658174,0.00012596385,0.00016207181,0.0001545546,0.00005289461,0.00013913198,0.00044155153],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000545518,0.00007177975,0.13555148,0.00013856174,0.00018300938,0.00003409596,0.00033007102,0.00033057705,0.8449029,0.0011071786,0.013594583,0.0032102892],"study_design_scores_gemma":[0.0074178334,0.0015876956,0.67304164,0.0000537087,0.0002506188,0.00012934554,0.00015031836,0.00060718996,0.13809986,0.0064386297,0.1708889,0.0013342754],"about_ca_topic_score_codex":0.0046214974,"about_ca_topic_score_gemma":0.0001229238,"teacher_disagreement_score":0.706803,"about_ca_system_score_codex":0.0000012754894,"about_ca_system_score_gemma":0.000042596683,"threshold_uncertainty_score":0.9918096},"labels":[],"label_agreement":null},{"id":"W2940826215","doi":"10.1126/science.aaw9548","title":"Sulfur isotopes in diamonds reveal differences in continent construction","year":2019,"lang":"en","type":"article","venue":"Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Gemological Institute of America; Carnegie Institution for Science; University of Alberta; National Science Foundation","keywords":"Craton; Archean; Geology; Lithosphere; Geochemistry; Subduction; Mantle (geology); Earth science; Tectonics; Paleontology","score_opus":0.007669650381530352,"score_gpt":0.19528205061020973,"score_spread":0.18761240022867937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2940826215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947878,0.00006144405,0.0000026274156,0.00013478707,0.00093258877,0.00015434867,0.00001574534,0.000010367527,0.0039003082],"genre_scores_gemma":[0.99948394,0.00002039745,0.0001965837,0.00003997375,0.000034818302,0.0000011870936,0.0000041253397,8.311578e-7,0.00021812132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99897844,0.000036829562,0.00017229388,0.00027542855,0.00025170908,0.0002853198],"domain_scores_gemma":[0.99969476,0.00004529434,0.000051542414,0.00013211861,0.000021816017,0.000054441465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005393115,0.000074470874,0.00015624866,0.00013179982,0.00004910067,0.000096565585,0.0002804016,0.000026376001,0.0006202953],"category_scores_gemma":[0.00003181419,0.00005674897,0.000013440046,0.00047902553,0.00023182399,0.000378451,0.00002027135,0.00006198198,0.0002287378],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007912761,0.000006269035,0.9863693,0.0000066023736,4.1557593e-7,0.0000025659026,0.00016140444,0.00008528177,0.0096693095,0.00036373988,0.000008717706,0.0033184553],"study_design_scores_gemma":[0.00015665796,0.000040087776,0.9952799,0.000024200814,7.0371124e-7,0.0000016021604,0.000109166,0.0005404684,0.0021207728,0.0012393962,0.00039773984,0.00008931938],"about_ca_topic_score_codex":0.0025160527,"about_ca_topic_score_gemma":0.0014147095,"teacher_disagreement_score":0.008910559,"about_ca_system_score_codex":0.000004053915,"about_ca_system_score_gemma":0.00007663469,"threshold_uncertainty_score":0.67917985},"labels":[],"label_agreement":null},{"id":"W2948021141","doi":"10.1111/1755-6724.13913","title":"North American Earth Science Megaproject Continuum, Part 1: LITHOPROBE (1984‐2005)","year":2019,"lang":"en","type":"article","venue":"Acta Geologica Sinica - English Edition","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Megaproject; Engineering; Systems engineering","score_opus":0.010196681744852061,"score_gpt":0.20865305504544443,"score_spread":0.19845637330059238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948021141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9720902,0.000030592448,0.0000070861847,0.00029888665,0.0046923533,0.00047841942,0.00027201034,0.00022766941,0.02190277],"genre_scores_gemma":[0.99557817,0.00011369563,0.0005468845,0.00040470972,0.0022522674,0.000009900485,0.00043833765,0.000007438102,0.00064857135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99711347,0.00017387293,0.00043254445,0.0008005662,0.00060259574,0.0008769268],"domain_scores_gemma":[0.99815845,0.00032316943,0.00036010088,0.00059801043,0.00029879058,0.00026148363],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010378442,0.00028038173,0.00049409014,0.00013012903,0.0003379742,0.0002758258,0.0006623417,0.00009410452,0.0039652158],"category_scores_gemma":[0.0005246432,0.00021732392,0.00010154486,0.00071178965,0.00079183903,0.000951543,0.00008131991,0.00025679258,0.00079885777],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004895547,0.0004036835,0.8977758,0.00010200582,0.00014249004,0.000059733393,0.0014831832,0.00066747924,0.0074966573,0.00070595444,0.07384176,0.016831668],"study_design_scores_gemma":[0.0003269575,0.0005779129,0.73233175,0.000017123188,0.000027883612,0.000004065941,0.00011206004,0.00012414723,0.0013739555,0.00021375853,0.2645264,0.00036396366],"about_ca_topic_score_codex":0.00063628814,"about_ca_topic_score_gemma":0.0024432794,"teacher_disagreement_score":0.19068463,"about_ca_system_score_codex":0.000007511609,"about_ca_system_score_gemma":0.0001783916,"threshold_uncertainty_score":0.99997914},"labels":[],"label_agreement":null},{"id":"W2951332731","doi":"10.2110/jsr.2019.29","title":"A New Approach To Quantify the Ordering State of Protodolomite Using XRD, TEM, and Z-Contrast Imaging","year":2019,"lang":"en","type":"article","venue":"Journal of Sedimentary Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Contrast (vision); Geology; Mineralogy; Artificial intelligence; Computer science","score_opus":0.06347511855171091,"score_gpt":0.32367234476473095,"score_spread":0.26019722621302005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2951332731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99764365,0.0004019657,0.00023905866,0.00042252467,0.0002190847,0.0005742005,0.000023457489,0.0000021417638,0.00047394517],"genre_scores_gemma":[0.995236,0.00004007755,0.0042794375,0.0000674211,0.00023491091,8.4398823e-7,0.0000026452606,0.000005068647,0.00013363495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983897,0.00021640609,0.00033259953,0.00014190626,0.0006101629,0.0003091958],"domain_scores_gemma":[0.9992139,0.00019887676,0.00014355706,0.00014449384,0.00013678429,0.00016240517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026089777,0.00008617379,0.0002369858,0.00016222328,0.0001117208,0.00012153687,0.00029188028,0.000015890551,0.0003499075],"category_scores_gemma":[0.00002467243,0.0000528004,0.00003837813,0.0002307506,0.000059066882,0.00029784205,0.00005875906,0.00024250236,0.000022958093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021067346,0.00012327943,0.4889424,0.00049539574,0.00037993642,0.000054167824,0.0052043186,0.02152977,0.40230265,0.000082046005,0.0058337916,0.0729455],"study_design_scores_gemma":[0.0076130405,0.0031227598,0.7683108,0.0014879192,0.0002118584,0.0007024794,0.007889008,0.066123575,0.090164654,0.005665054,0.04754654,0.0011622985],"about_ca_topic_score_codex":0.0051848744,"about_ca_topic_score_gemma":0.000034439105,"teacher_disagreement_score":0.312138,"about_ca_system_score_codex":0.0000061856304,"about_ca_system_score_gemma":0.00014506043,"threshold_uncertainty_score":0.7838014},"labels":[],"label_agreement":null},{"id":"W2954094158","doi":"10.5194/sed-7-2663-2015","title":"Strain localization in ultramylonitic marbles by simultaneous activation of dislocation motion and grain boundary sliding (Syros, Greece)","year":2015,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Misorientation; Dislocation; Dislocation creep; Grain boundary; Grain Boundary Sliding; Materials science; Slip (aerodynamics); Crystallography; Grain boundary strengthening; Deformation (meteorology); Peierls stress; Deformation mechanism; Climb; Mineralogy; Composite material; Geometry; Microstructure; Geology; Chemistry; Physics; Thermodynamics","score_opus":0.013379353440695397,"score_gpt":0.2243569888984894,"score_spread":0.210977635457794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954094158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9659158,0.0003504393,0.030343791,0.00015600026,0.0005736756,0.00069411506,0.0011528069,0.000054304404,0.0007590824],"genre_scores_gemma":[0.99388206,0.000120358156,0.00035841877,0.000034601348,0.00007245622,0.0000033777192,0.0054175127,0.000007556074,0.00010367952],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985594,0.0001753915,0.0004246028,0.0003595855,0.000285206,0.00019578019],"domain_scores_gemma":[0.99924624,0.00013136452,0.00025787,0.00017227913,0.00011691871,0.00007532291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000533666,0.0002090632,0.0003102534,0.00012760657,0.00006814097,0.00015063459,0.0001260942,0.00022742589,0.00016821818],"category_scores_gemma":[0.00013602339,0.00019431382,0.000026452377,0.00013291075,0.00006704887,0.00022998023,0.000030472182,0.00014300499,0.0000058451737],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039324,0.00034590898,0.05505733,0.0034078534,0.00015975357,0.000019391728,0.005257248,0.6286514,0.045666873,0.0021838227,0.0023324632,0.2565247],"study_design_scores_gemma":[0.0011278396,0.00027696273,0.033535402,0.00066252565,0.00010664722,0.000006361767,0.00074129866,0.88066,0.011760866,0.06825619,0.0017566434,0.0011092718],"about_ca_topic_score_codex":0.009737332,"about_ca_topic_score_gemma":0.0015846627,"teacher_disagreement_score":0.25541544,"about_ca_system_score_codex":0.000015974076,"about_ca_system_score_gemma":0.00008711501,"threshold_uncertainty_score":0.9968569},"labels":[],"label_agreement":null},{"id":"W2955561921","doi":"10.1029/2019gc008385","title":"Spurious Transitions in Convective Regime Due to Viscosity Clipping: Ramifications for Modeling Planetary Secular Cooling","year":2019,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Convection; Mantle convection; Viscosity; Mechanics; Geophysics; Mantle (geology); Convective heat transfer; Thermodynamics; Thermal; Geology; Physics; Lithosphere","score_opus":0.010335670554684791,"score_gpt":0.2080238032034234,"score_spread":0.1976881326487386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955561921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98928976,0.00013470979,0.005331314,0.00017937926,0.000619747,0.0013088785,0.001747055,0.00007962713,0.001309519],"genre_scores_gemma":[0.996569,0.000004707874,0.00037394324,0.00009219714,0.00044364634,0.000047360252,0.0022407093,0.000014857317,0.0002136297],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9978981,0.00006598262,0.0004927656,0.0006686196,0.00027650158,0.0005980326],"domain_scores_gemma":[0.9988424,0.000119863995,0.0001418842,0.00054264284,0.00015502305,0.00019816287],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00036039107,0.0003031966,0.0005607572,0.000075546865,0.0002070559,0.00012426834,0.00034208767,0.00016563867,0.00014880979],"category_scores_gemma":[0.000022663153,0.00032440794,0.00014173675,0.00029680788,0.000026805188,0.00019284806,0.00002114545,0.00018886957,0.00037489025],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004104409,0.00018561103,0.0034784998,0.0013589822,0.00021971535,0.00005105314,0.002748877,0.85071576,0.1391049,0.0007030333,0.00033652762,0.00068660633],"study_design_scores_gemma":[0.0019490935,0.00022913185,0.006440502,0.0005273513,0.0001400784,0.000069878595,0.0015617273,0.9676815,0.011874406,0.0050097466,0.0030424683,0.0014740815],"about_ca_topic_score_codex":0.0037812106,"about_ca_topic_score_gemma":0.00048172762,"teacher_disagreement_score":0.12723051,"about_ca_system_score_codex":0.000018538414,"about_ca_system_score_gemma":0.00011855575,"threshold_uncertainty_score":0.9999208},"labels":[],"label_agreement":null},{"id":"W2956024631","doi":"10.2138/am-2019-6967","title":"Compressibility of synthetic Mg-Al tourmalines to 60 GPa","year":2019,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Tourmaline; Grossular; Compressibility; Crystallography; Octahedron; Anisotropy; Chemistry; Bulk modulus; Diamond anvil cell; Diopside; Analytical Chemistry (journal); Crystal structure; Mineralogy; Materials science; Thermodynamics; High pressure; Metallurgy","score_opus":0.008938002366775754,"score_gpt":0.2342119594742795,"score_spread":0.22527395710750375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2956024631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922586,0.000031969103,0.00003994138,0.00059389515,0.00040031268,0.0001942076,0.00033311173,0.000026583597,0.006121379],"genre_scores_gemma":[0.9978321,0.0000078357025,0.0010715219,0.00052746123,0.00008935675,0.0000014888839,0.00006889551,0.0000040731707,0.00039724927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998913,0.00008306463,0.00025970547,0.00029565106,0.00019004513,0.00025853462],"domain_scores_gemma":[0.99917716,0.000121696125,0.00014085157,0.00039168395,0.000051647134,0.000116943986],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014538383,0.00013479144,0.00037699437,0.000043323984,0.000034046912,0.000028689827,0.00027202757,0.000019868741,0.001743923],"category_scores_gemma":[0.000041097093,0.000103106446,0.0000630352,0.0001957669,0.00022988781,0.00006752029,0.000028252236,0.000048390866,0.00047076322],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043953912,0.00019302803,0.75660145,0.00014687418,0.00010638567,0.0000409476,0.0007843974,0.016655259,0.17452371,0.0006565644,0.016972207,0.03287964],"study_design_scores_gemma":[0.00024167051,0.0005873307,0.9653316,0.000027601613,0.000022811484,0.000005290608,0.00014475905,0.0012272208,0.0029749908,0.00022714163,0.028875284,0.00033429574],"about_ca_topic_score_codex":0.027317958,"about_ca_topic_score_gemma":0.0010856127,"teacher_disagreement_score":0.20873015,"about_ca_system_score_codex":0.0000018884807,"about_ca_system_score_gemma":0.000023239794,"threshold_uncertainty_score":0.99916863},"labels":[],"label_agreement":null},{"id":"W2963735633","doi":"10.48550/arxiv.1009.4185","title":"Singlet-Triplet Excitations in the Unconventional Spin-Peierls System TiOBr","year":2010,"lang":"en","type":"article","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oak Ridge National Laboratory; Nova scotia; Ridge; National laboratory; Singlet state; Physics; Library science; Research council; Neutron scattering; Engineering physics; Archaeology; Nuclear physics; Geography; Neutron; Cartography; Philosophy","score_opus":0.034852793130836945,"score_gpt":0.16252191500136873,"score_spread":0.12766912187053178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963735633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9871071,0.000008198532,0.0004248764,0.00008197223,0.0007202635,0.00013571448,0.00007752367,0.00003056712,0.011413795],"genre_scores_gemma":[0.9991841,0.0000034111204,0.00006474973,0.000057907197,0.00013237359,1.89446e-7,0.000056304267,0.0000021021203,0.0004988985],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9993151,0.00009652642,0.00011218555,0.0002177504,0.00007311465,0.00018532624],"domain_scores_gemma":[0.99951357,0.00011204489,0.00006509554,0.00021667358,0.00003792494,0.000054720163],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031625308,0.000088405526,0.00010359287,0.0000756952,0.00018003935,0.00006395394,0.0003141369,0.000053467054,0.0007549094],"category_scores_gemma":[0.000016827418,0.00007197201,0.00005321681,0.00033352667,0.000073146,0.0002088609,0.00001117204,0.00012868943,0.0004899371],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000088542976,0.00013457144,0.16038302,0.000097537864,0.00006121198,0.00044365381,0.00063830655,0.03412569,0.0026235844,0.79882604,0.0018559908,0.0007218878],"study_design_scores_gemma":[0.0011938912,0.00012518074,0.9130811,0.000047418038,0.0000851697,0.000028477338,0.0014285939,0.03340639,0.00012970791,0.02397999,0.026004288,0.0004898032],"about_ca_topic_score_codex":0.0012349695,"about_ca_topic_score_gemma":0.002883989,"teacher_disagreement_score":0.774846,"about_ca_system_score_codex":0.000004059926,"about_ca_system_score_gemma":0.00004242541,"threshold_uncertainty_score":0.8265729},"labels":[],"label_agreement":null},{"id":"W2964339032","doi":"10.1002/ctpp.201700202","title":"Theory of complex fluids in the warm dense matter regime and application to an unusual phase transition in liquid carbon","year":2018,"lang":"en","type":"article","venue":"Contributions to Plasma Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Warm dense matter; Materials science; Ion; Ionization; Phase (matter); Ionic bonding; Molecular dynamics; Atom (system on chip); Atomic physics; Electron; Scattering; Molecular physics; Thermodynamics; Physics","score_opus":0.012659857671900462,"score_gpt":0.26439386119665564,"score_spread":0.25173400352475517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964339032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906813,0.0000082648885,0.0070051313,0.00064136944,0.000058092555,0.00047060868,0.0008218535,0.000009855316,0.0003035454],"genre_scores_gemma":[0.9989742,0.000001975108,0.00012155831,0.000381576,0.00017970735,0.000016616836,0.00031609353,0.0000030268607,0.000005227146],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991176,0.00018091976,0.00019780922,0.00019389705,0.000116143696,0.00019359711],"domain_scores_gemma":[0.99949455,0.00010413039,0.00003909581,0.00021062559,0.00008412031,0.00006745582],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042606317,0.000098212724,0.00017155512,0.000057665882,0.00007881147,0.000030665164,0.00014063956,0.000042613516,0.000035166267],"category_scores_gemma":[0.000015469133,0.00007889798,0.000017499264,0.0002967559,0.00008681753,0.00010703452,0.000009287098,0.000054767428,0.000054906068],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0055054165,0.0013463278,0.0049373475,0.00010299753,0.00007138957,0.000016904509,0.032543685,0.007663418,0.8473242,0.06194993,0.0014069824,0.03713138],"study_design_scores_gemma":[0.010934761,0.009305996,0.34548753,0.00026655212,0.0002947695,0.000037180733,0.002468358,0.12417498,0.40191868,0.08466524,0.018499427,0.0019465404],"about_ca_topic_score_codex":0.0009765666,"about_ca_topic_score_gemma":0.0010134787,"teacher_disagreement_score":0.44540554,"about_ca_system_score_codex":0.0000061364794,"about_ca_system_score_gemma":0.000025052655,"threshold_uncertainty_score":0.32173663},"labels":[],"label_agreement":null},{"id":"W2969184124","doi":"10.1093/gji/ggz370","title":"Post-critical SsPmp and its applications to Virtual Deep Seismic Sounding (VDSS) – 2: 1-D imaging of the crust/mantle and joint constraints with receiver functions","year":2019,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Incorporated Research Institutions for Seismology","keywords":"Geology; Crust; Mantle (geology); Craton; Depth sounding; Lithosphere; Seismology; Receiver function; Geophysics; Tectonics","score_opus":0.007183633234181825,"score_gpt":0.21699954891450618,"score_spread":0.20981591568032434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969184124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99267966,0.000040616687,0.0029463808,0.0020099352,0.000665408,0.00017899786,0.0002195164,0.000010271922,0.0012492465],"genre_scores_gemma":[0.998861,0.000010205256,0.00020908267,0.00034832786,0.00031680698,0.0000023778214,0.000012936535,0.000004300839,0.0002349225],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99909234,0.000044808243,0.00020357917,0.00018393336,0.00030274317,0.00017260862],"domain_scores_gemma":[0.9993104,0.00017142935,0.00009169945,0.00008620491,0.0002048333,0.00013545912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014085347,0.000104704486,0.00015328736,0.00006220072,0.00018543424,0.00014459433,0.00015158374,0.000024249204,0.00061234325],"category_scores_gemma":[0.00005290063,0.000069034766,0.000044505516,0.000080060956,0.0001517418,0.00025741616,0.000048442744,0.00016740349,0.00013090005],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013679316,0.0007775308,0.2373636,0.00026776243,0.001392978,0.00009314331,0.004615234,0.025767336,0.3479742,0.14987402,0.002596516,0.22790973],"study_design_scores_gemma":[0.0013432925,0.00051062927,0.94376093,0.0002836081,0.00015356157,0.0009123286,0.0014272843,0.03250028,0.0029260924,0.0076949354,0.00792069,0.00056638656],"about_ca_topic_score_codex":0.000086836466,"about_ca_topic_score_gemma":0.000018433499,"teacher_disagreement_score":0.7063973,"about_ca_system_score_codex":0.0000059064614,"about_ca_system_score_gemma":0.000045052424,"threshold_uncertainty_score":0.6704729},"labels":[],"label_agreement":null},{"id":"W2970745978","doi":"10.1134/s0016702919090106","title":"Texture and Genesis of Polycrystalline Varieties of Diamond Based on Phase-Contrast and Diffraction Contrast Tomography","year":2019,"lang":"en","type":"article","venue":"Geochemistry International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stornoway Diamond (Canada)","funders":"","keywords":"Texture (cosmology); Diamond; Materials science; Phase contrast microscopy; Contrast (vision); Diffraction; Mineralogy; Crystallography; Phase (matter); Analytical Chemistry (journal); Chemistry; Metallurgy; Optics; Chromatography; Physics","score_opus":0.0038022091984537833,"score_gpt":0.19734079141957026,"score_spread":0.19353858222111647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970745978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99614125,0.00014283057,0.00010592639,0.000090023816,0.00017160985,0.0000679025,0.0011329489,0.000006177482,0.0021413052],"genre_scores_gemma":[0.9993198,0.00002795041,0.00008631664,0.000035529305,0.00008301392,8.358327e-7,0.0003480129,0.000002009613,0.00009656297],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994105,0.000011280842,0.0001610382,0.00014962691,0.00018441502,0.00008314544],"domain_scores_gemma":[0.9995885,0.00009844963,0.00012739091,0.00008344108,0.00006224444,0.000039984152],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000077460165,0.00008838477,0.0001512887,0.00003855044,0.00002027278,0.000023986982,0.00007592664,0.000056060297,0.0015347737],"category_scores_gemma":[0.000016282771,0.00007593559,0.000032464235,0.000034647164,0.0000698527,0.00006792143,0.0000071583645,0.000043120024,0.0000018028329],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000593311,0.00014440528,0.22835112,0.00017789897,0.00012583719,0.0000024830122,0.0000936267,0.00050614995,0.7631995,0.00016363549,0.00024505786,0.006396973],"study_design_scores_gemma":[0.0027115082,0.00029436534,0.734939,0.00009174781,0.000056431083,0.000007800108,0.000151275,0.019644406,0.23917516,0.00079029216,0.0018815307,0.00025649343],"about_ca_topic_score_codex":0.00041865258,"about_ca_topic_score_gemma":0.000015047701,"teacher_disagreement_score":0.52402437,"about_ca_system_score_codex":0.0000010273179,"about_ca_system_score_gemma":0.000014853829,"threshold_uncertainty_score":0.99937797},"labels":[],"label_agreement":null},{"id":"W2971402604","doi":"10.2138/am-2019-6937","title":"Goldschmidtite, (K,REE,Sr)(Nb,Cr)O3: A new perovskite supergroup mineral found in diamond from Koffiefontein, South Africa","year":2019,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Augite; Electron microprobe; Chromite; Mineralogy; Perovskite (structure); Analytical Chemistry (journal); Crystallography; Mineral; Geothermobarometry; Chemistry; Materials science; Metallurgy; Quartz","score_opus":0.010847692714144925,"score_gpt":0.19788470350603576,"score_spread":0.18703701079189083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971402604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.979323,0.0005952537,0.00003887964,0.00037193208,0.00087117084,0.0002670001,0.000556125,0.00007732981,0.017899295],"genre_scores_gemma":[0.9881468,0.000034877015,0.0015147608,0.00048337548,0.0007601258,0.0000055983983,0.0006571777,0.000021667614,0.00837566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997304,0.00016192616,0.0005060716,0.00078843243,0.0004010035,0.0008385735],"domain_scores_gemma":[0.9985369,0.00021638403,0.00022658033,0.00062761275,0.00005196071,0.00034057905],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016412696,0.00043055607,0.00076421624,0.00015761105,0.000082934755,0.00022712888,0.0005695133,0.000102289196,0.0030476893],"category_scores_gemma":[0.00006677619,0.00036158515,0.00014087491,0.00066841475,0.00030087662,0.0003664007,0.000063580126,0.00022905978,0.0018409304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043962823,0.00014142985,0.9280214,0.000044093842,0.00014477684,0.00021227737,0.005035209,0.002601238,0.023170644,0.0005271234,0.023714265,0.01594796],"study_design_scores_gemma":[0.0014694317,0.0006427357,0.9063029,0.000059199607,0.000051365732,0.0000057590805,0.0006583177,0.0016302739,0.00006541913,0.0006981596,0.08745905,0.00095735164],"about_ca_topic_score_codex":0.14905323,"about_ca_topic_score_gemma":0.03292114,"teacher_disagreement_score":0.116132095,"about_ca_system_score_codex":0.000014085732,"about_ca_system_score_gemma":0.00012059034,"threshold_uncertainty_score":0.9998836},"labels":[],"label_agreement":null},{"id":"W2971554026","doi":"10.2138/am-2019-7023","title":"Nixonite, Na2Ti6O13, a new mineral from a metasomatized mantle garnet pyroxenite from the western Rae Craton, Darby kimberlite field, Canada","year":2019,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Kimberlite; Isostructural; Craton; Geology; Geochemistry; Crystallography; Octahedron; Chemistry; Mantle (geology); Mineralogy; Crystal structure","score_opus":0.005997040407616688,"score_gpt":0.19073084423218828,"score_spread":0.18473380382457158,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971554026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987733,0.0005693236,0.000030335068,0.0028132738,0.0012011192,0.0003142318,0.002278521,0.00005123625,0.0050089736],"genre_scores_gemma":[0.9829287,0.000056331028,0.00083743705,0.0062175887,0.0009505315,0.00000475991,0.0018948577,0.000015665266,0.007094117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978539,0.00022081983,0.0004288674,0.00053929916,0.00042885178,0.00052827055],"domain_scores_gemma":[0.9978798,0.0008052834,0.0003086557,0.0007150621,0.000045489276,0.00024567734],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011228881,0.00034959128,0.0006228469,0.000030077646,0.00012640664,0.0002483821,0.00065728615,0.000057114125,0.004926147],"category_scores_gemma":[0.000055004715,0.00023375223,0.000108886845,0.00027017432,0.00015815359,0.00017892678,0.00005631476,0.00018459525,0.00053787936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031018344,0.00003513008,0.55108035,0.000013715718,0.00041113063,0.0001329705,0.0006510742,0.0006512555,0.011512471,0.00005062487,0.4121567,0.02299437],"study_design_scores_gemma":[0.0009387789,0.00017213199,0.53721714,0.000037982005,0.00011854574,0.0000053709414,0.00018374874,0.00057152926,0.0004366711,0.00031106544,0.45944294,0.00056411413],"about_ca_topic_score_codex":0.9937928,"about_ca_topic_score_gemma":0.9632749,"teacher_disagreement_score":0.047286242,"about_ca_system_score_codex":0.000009482877,"about_ca_system_score_gemma":0.00029716158,"threshold_uncertainty_score":0.9959835},"labels":[],"label_agreement":null},{"id":"W2977578445","doi":"10.1093/nsr/nwz144","title":"A chemical perspective on high pressure crystal structures and properties","year":2019,"lang":"en","type":"review","venue":"National Science Review","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"High pressure; Perspective (graphical); Materials science; Crystal (programming language); Chemical engineering; Chemical physics; Chemistry; Thermodynamics; Physics; Computer science; Engineering; Mathematics; Geometry","score_opus":0.046634574643082356,"score_gpt":0.3101334229372711,"score_spread":0.26349884829418874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2977578445","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000019260822,0.99466336,2.6834468e-7,0.00013985929,0.0003130552,0.00094027416,0.000428645,0.000018236811,0.0034770272],"genre_scores_gemma":[0.0014315664,0.99776137,0.00008183337,0.0002008243,0.00026094465,0.000012294224,0.000078652745,0.0000055079527,0.00016700581],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974743,0.00010685997,0.0003388394,0.00065511925,0.0011355832,0.00028929272],"domain_scores_gemma":[0.9990185,0.00012245924,0.0002511595,0.00019880143,0.00028505072,0.00012403882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007740882,0.00029983016,0.0010268845,0.000109508335,0.00017056418,0.00017964965,0.0005473892,0.000106979736,0.0008190778],"category_scores_gemma":[0.00037028664,0.00017350685,0.00013438733,0.00045228738,0.0003538514,0.0002611754,0.00005540628,0.00020726571,0.00022745963],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008891618,0.000029759069,0.0000045237525,0.08131499,0.00014552633,0.0000039303545,0.00005532326,0.000025583933,0.000030109246,0.06672543,0.0021985015,0.84945744],"study_design_scores_gemma":[0.000043767097,0.00003679612,0.000066075794,0.015373317,0.0003021128,0.00002492014,0.000002710123,0.000011107303,0.0000043696336,0.00126623,0.9825819,0.00028669782],"about_ca_topic_score_codex":0.00020881151,"about_ca_topic_score_gemma":0.0000063807934,"teacher_disagreement_score":0.9803834,"about_ca_system_score_codex":0.000027640499,"about_ca_system_score_gemma":0.000921349,"threshold_uncertainty_score":0.8968327},"labels":[],"label_agreement":null},{"id":"W2981456490","doi":"10.4095/220933","title":"Residual total magnetic field, 21O/16 - Charlo, New Brunswick","year":2005,"lang":"en","type":"report","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Residual; Biology; Mathematics; Algorithm","score_opus":0.017597768999082334,"score_gpt":0.23328556572318226,"score_spread":0.21568779672409993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981456490","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.030906808,0.008360178,0.000024287978,0.0015741069,0.009518157,0.00051049155,0.00030405595,0.00019116286,0.9486107],"genre_scores_gemma":[0.04797851,0.0056316606,0.001162356,0.0007515641,0.031229181,0.0000017285957,0.0016750523,0.00003259119,0.91153735],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99735177,0.00005925831,0.0005349261,0.00057321833,0.0009060471,0.00057478383],"domain_scores_gemma":[0.99874866,0.000110157365,0.00020746437,0.00050999876,0.000100803285,0.00032292434],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003644876,0.00040836792,0.000615615,0.00010417363,0.00011378368,0.00022517335,0.00038772443,0.00045763608,0.1534365],"category_scores_gemma":[0.000050947874,0.0003224077,0.00015693187,0.00011035949,0.000035878442,0.00015904539,0.000043912412,0.00029150618,0.0034785594],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003627928,0.000017540227,0.0021389502,0.00011041261,0.000058980888,0.000057655376,0.000047640548,0.0000628323,0.000022632574,0.00013785624,0.8171129,0.18019632],"study_design_scores_gemma":[0.00021528965,0.00036952685,0.054820202,0.000049373277,0.00009220718,0.00007655151,0.000015071763,0.00001638648,0.00013952084,0.00018098278,0.94348556,0.00053931866],"about_ca_topic_score_codex":0.2150085,"about_ca_topic_score_gemma":0.047917414,"teacher_disagreement_score":0.179657,"about_ca_system_score_codex":0.000009994907,"about_ca_system_score_gemma":0.002488434,"threshold_uncertainty_score":0.9999228},"labels":[],"label_agreement":null},{"id":"W2981604089","doi":"10.4095/220908","title":"Residual total magnetic field, 22B/11 - St-Jean-Bapt-Vianney, Quebec","year":2005,"lang":"en","type":"report","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Residual; Humanities; Mathematics; Art","score_opus":0.014203364225228611,"score_gpt":0.22806620312229284,"score_spread":0.21386283889706423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981604089","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12504682,0.0067470465,0.000035193654,0.0024514357,0.012211158,0.0011004527,0.003924855,0.0004118416,0.8480712],"genre_scores_gemma":[0.23220712,0.0018469824,0.0007510419,0.00059597724,0.010764803,0.000009586197,0.003632956,0.000043347463,0.7501482],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9966419,0.000111573056,0.00069779,0.00072518724,0.0011053553,0.00071821606],"domain_scores_gemma":[0.9983101,0.0003086477,0.00027267478,0.0006488089,0.00018029437,0.00027949284],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0005692557,0.0005204028,0.0007705034,0.00014225705,0.00017209045,0.0003328825,0.000495597,0.00056897546,0.12891653],"category_scores_gemma":[0.00015086462,0.00041346735,0.00020556168,0.0001362085,0.000077423036,0.00020617731,0.00005924367,0.00033375275,0.0022292188],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062169915,0.000059909267,0.0040058023,0.00032243386,0.00012367812,0.00026961445,0.00010198877,0.0005588553,0.00009680014,0.00016460413,0.8545841,0.13965006],"study_design_scores_gemma":[0.00023190536,0.000370051,0.034729093,0.000086383545,0.00014508486,0.000052686733,0.000034047192,0.00007985941,0.00027850101,0.00016629438,0.9630367,0.00078936416],"about_ca_topic_score_codex":0.4441145,"about_ca_topic_score_gemma":0.37210146,"teacher_disagreement_score":0.1388607,"about_ca_system_score_codex":0.000014059263,"about_ca_system_score_gemma":0.0009746395,"threshold_uncertainty_score":0.99983174},"labels":[],"label_agreement":null},{"id":"W2986204447","doi":"10.1139/cjp-2019-0326","title":"A modified Anderson–Grüneisen model for the pressure dependence of thermal expansivity","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Thermodynamics; Physics; Thermal; Equation of state; Volume (thermodynamics); Reciprocal","score_opus":0.022862759029234625,"score_gpt":0.2055680739637313,"score_spread":0.18270531493449668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2986204447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99104303,0.0005084106,0.0062630638,0.00017931488,0.0006242181,0.00026548383,0.00047560196,0.0000023345774,0.0006385425],"genre_scores_gemma":[0.99923736,0.000008087727,0.00019960466,0.00007859969,0.0002363165,5.0742733e-7,0.000005421375,0.000004278282,0.00022983953],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993087,0.00003164551,0.00019025555,0.00008739455,0.00015988143,0.00022209073],"domain_scores_gemma":[0.99915355,0.00012849341,0.0002218004,0.00016979543,0.00015203633,0.00017433986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002598376,0.000090959154,0.00021554927,0.000025496613,0.00009247123,0.00004590094,0.00034050096,0.00004251546,0.00014403927],"category_scores_gemma":[0.000018075807,0.00005943558,0.0001046527,0.00006083317,0.000058917525,0.0002181007,0.0000038347903,0.000095116404,0.000006837037],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007988323,0.000009631599,0.009002187,0.00008158611,0.00014985456,0.0000044808166,0.0015704515,0.9740865,0.0039914823,0.0019915695,0.00090404664,0.0081283115],"study_design_scores_gemma":[0.0012793068,0.00035732254,0.051012997,0.00010158402,0.0003280014,0.000013708083,0.00038794466,0.9213316,0.0058931056,0.016142191,0.002758413,0.00039383306],"about_ca_topic_score_codex":0.007636546,"about_ca_topic_score_gemma":0.009510308,"teacher_disagreement_score":0.052754924,"about_ca_system_score_codex":0.0000025830532,"about_ca_system_score_gemma":0.00059173984,"threshold_uncertainty_score":0.9989717},"labels":[],"label_agreement":null},{"id":"W2986259592","doi":"10.1130/ges02093.1","title":"A multicomponent Isabella anomaly: Resolving the physical state of the Sierra Nevada upper mantle from Vp/Vs anisotropy tomography","year":2019,"lang":"en","type":"article","venue":"Geosphere","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of South Carolina; National Science Foundation","keywords":"Lithosphere; Geology; Anomaly (physics); Anisotropy; Mantle (geology); Geophysics; Seismology; Volcanism; Seismic tomography; Tectonics; Physics; Condensed matter physics","score_opus":0.004631537050961645,"score_gpt":0.17942011628986476,"score_spread":0.17478857923890312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2986259592","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966831,0.00037653,0.000008551288,0.00021899863,0.0006834841,0.00032442436,0.00039627033,0.000022142527,0.0012864799],"genre_scores_gemma":[0.99860793,0.000022021606,0.0002612799,0.00014047623,0.0001682318,0.0000017629391,0.00003609438,0.000007804378,0.0007543823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987046,0.00013910593,0.00020891381,0.00028327893,0.00033380993,0.00033030097],"domain_scores_gemma":[0.99900514,0.0001741772,0.00014382326,0.00058063143,0.000035104018,0.00006111774],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012709931,0.0001729872,0.00026936963,0.000009046336,0.00015919116,0.00007963414,0.00051566726,0.000039854025,0.0024587119],"category_scores_gemma":[0.0000077613895,0.0000911084,0.00016323694,0.00016032372,0.00010915423,0.00010840021,0.000074477466,0.00013128966,0.0004357965],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000538399,0.00031415396,0.87246615,0.00015593106,0.0004267263,0.000016164471,0.0051036454,0.013193031,0.07686672,0.0010811132,0.0056099533,0.024228],"study_design_scores_gemma":[0.00044064163,0.00012063694,0.96423477,0.000053720298,0.000052284307,0.0000011673295,0.00019341639,0.006764559,0.0066759195,0.002939426,0.018299542,0.00022393465],"about_ca_topic_score_codex":0.015080158,"about_ca_topic_score_gemma":0.0010699583,"teacher_disagreement_score":0.091768585,"about_ca_system_score_codex":0.000002205621,"about_ca_system_score_gemma":0.000023212984,"threshold_uncertainty_score":0.9984532},"labels":[],"label_agreement":null},{"id":"W2988563457","doi":"10.1029/2019jb018653","title":"Influence of Upper Plate Structure on Flat‐Slab Depth: Numerical Modeling of Subduction Dynamics","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slab; Geology; Slab window; Subduction; Lithosphere; Craton; Mantle (geology); Seismology; Petrology; Geophysics; Oceanic crust; Tectonics","score_opus":0.019609645710791965,"score_gpt":0.2920404882237749,"score_spread":0.2724308425129829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2988563457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99885553,0.000036236557,0.00010700418,0.000090463465,0.000251381,0.00015353227,0.00010776715,0.0000045223837,0.00039356292],"genre_scores_gemma":[0.99914175,0.000055692977,0.0003707766,0.000014923527,0.0003101492,1.8655574e-7,0.00001640568,0.000007745121,0.000082391394],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.997094,0.0002485113,0.00060293195,0.0002129694,0.0013981292,0.00044351158],"domain_scores_gemma":[0.99812746,0.000340556,0.00033429905,0.00027660638,0.0007147885,0.00020631254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007144343,0.0001562112,0.000585865,0.00022689148,0.00007804769,0.000045540342,0.00040760174,0.000110065805,0.00030106108],"category_scores_gemma":[0.00020206437,0.00011304636,0.00016325885,0.00040367752,0.00013447739,0.00039260025,0.0000412505,0.00064973906,0.00010071351],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010401871,0.00009326506,0.015854685,0.00015309513,0.000107043874,0.000016842067,0.0002612756,0.91589296,0.06158147,0.0010195614,0.00003683606,0.0039427974],"study_design_scores_gemma":[0.001101426,0.003842013,0.38302758,0.0003913053,0.00004266865,0.000029242792,0.00017019895,0.55633384,0.034357294,0.020150352,0.00022244462,0.00033163812],"about_ca_topic_score_codex":0.0012012115,"about_ca_topic_score_gemma":0.000063509426,"teacher_disagreement_score":0.3671729,"about_ca_system_score_codex":0.000009070297,"about_ca_system_score_gemma":0.00019944948,"threshold_uncertainty_score":0.46098965},"labels":[],"label_agreement":null},{"id":"W2989963127","doi":"10.1029/2019gl085301","title":"Sound Velocities in Shock‐Synthesized Stishovite to 72 GPa","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"National Nuclear Security Administration; Princeton University; Washington State University; Carnegie Institution of Washington; U.S. Department of Energy","keywords":"Stishovite; Speed of sound; Geology; Rutile; Shear (geology); Mineralogy; Bulk modulus; Materials science; Thermodynamics; Composite material; Quartz; Petrology; Physics","score_opus":0.02937837099783221,"score_gpt":0.28317988689154583,"score_spread":0.25380151589371364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2989963127","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931943,0.000026994889,0.00002073927,0.0030262987,0.00039527303,0.00053692516,0.00013555224,0.00003565408,0.0026282559],"genre_scores_gemma":[0.9975109,0.000007819744,0.00021180799,0.0010340143,0.00041496454,0.000014315941,0.000058355155,0.000010655367,0.00073718233],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9966736,0.00036790752,0.00024961977,0.00052863546,0.0010027795,0.0011774855],"domain_scores_gemma":[0.99827516,0.0009276067,0.0000314137,0.0004208834,0.00006690488,0.0002780387],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009387301,0.000188816,0.00037059703,0.0002407746,0.00014949964,0.00027162491,0.00055819954,0.00006649807,0.0020751746],"category_scores_gemma":[0.00017569502,0.00016200384,0.00007771394,0.0005815049,0.00015494923,0.00027436108,0.000106409745,0.0003762252,0.008530924],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026883963,0.00045045099,0.17355296,0.00061261345,0.0002474014,0.0006939346,0.005826031,0.015235092,0.69265723,0.007735248,0.05639155,0.0439091],"study_design_scores_gemma":[0.0010975648,0.00048264395,0.94461286,0.00013644535,0.000009955308,0.0000025573815,0.0003547392,0.0013713295,0.0048239115,0.009781118,0.036566336,0.0007605134],"about_ca_topic_score_codex":0.008643571,"about_ca_topic_score_gemma":0.00091562746,"teacher_disagreement_score":0.77105993,"about_ca_system_score_codex":0.000013344052,"about_ca_system_score_gemma":0.00006463206,"threshold_uncertainty_score":0.99883705},"labels":[],"label_agreement":null},{"id":"W2989997968","doi":"","title":"Subcontinental sinking slab remnants in a spherical geometry mantle model","year":2012,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Slab; Geology; Mantle (geology); Transition zone; Slab window; Subduction; Lithosphere; Mantle wedge; Mantle convection; Geophysics; Seismology; Tectonics; Oceanic crust","score_opus":0.01843090144103167,"score_gpt":0.22600734095500494,"score_spread":0.20757643951397325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2989997968","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9808977,0.00031012902,0.0000131942315,0.000052283613,0.0005962372,0.00010549545,0.000028521075,0.000049539893,0.01794685],"genre_scores_gemma":[0.99672043,0.00002005867,0.0025818415,0.00010434898,0.0003396908,0.0000011373,0.000050484126,0.00000883295,0.00017315945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838597,0.000051027833,0.0003596405,0.00024285792,0.000282752,0.0006777795],"domain_scores_gemma":[0.9993655,0.0001290023,0.00013915506,0.00016835758,0.000019887964,0.00017807263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072982203,0.00017256099,0.00024895757,0.00006011857,0.00009933897,0.000080988146,0.0001991165,0.00010392862,0.00006542922],"category_scores_gemma":[0.00010688683,0.00015215242,0.000049669652,0.00016193026,0.00003322316,0.00035940937,0.00002909889,0.00016445325,0.00044184923],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003591648,0.00007637678,0.96210253,0.00003728423,0.000012512291,0.000034930934,0.00045252912,0.028295858,0.005806207,0.000028001952,0.00027784365,0.0028400216],"study_design_scores_gemma":[0.00031754162,0.000026567595,0.9883713,0.00009440997,0.000015123022,0.000011570603,0.00008938772,0.007169701,0.0021648451,0.0002948994,0.0011375382,0.00030711587],"about_ca_topic_score_codex":0.024791995,"about_ca_topic_score_gemma":0.0069428845,"teacher_disagreement_score":0.026268782,"about_ca_system_score_codex":0.0000060188254,"about_ca_system_score_gemma":0.000026323203,"threshold_uncertainty_score":0.98170197},"labels":[],"label_agreement":null},{"id":"W2990824274","doi":"","title":"The Unique Dynamics of the Pacific Hemisphere Mantle and its Signature on Seismic Anisotropy","year":2001,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Mantle (geology); Upwelling; Mantle convection; Seismic anisotropy; Mid-ocean ridge; Mantle wedge; Hotspot (geology); Core–mantle boundary; Southern Hemisphere; Geophysics; Seismology; Oceanography; Climatology; Tectonics; Subduction","score_opus":0.006930670504442461,"score_gpt":0.1929047940341259,"score_spread":0.18597412352968343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990824274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978958,0.00037048256,0.0000013592653,0.0007876344,0.0003562052,0.00014083117,0.00006112508,0.000019745454,0.019304583],"genre_scores_gemma":[0.9985809,0.0002875193,0.000036920435,0.00008735996,0.00008924018,7.2888577e-7,0.000019869043,0.0000052471955,0.00089226355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991289,0.000073568175,0.0001933785,0.00017340857,0.00019284588,0.00023794861],"domain_scores_gemma":[0.999251,0.00028304497,0.00016246797,0.00020612127,0.000040296483,0.00005703548],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030962826,0.00012558544,0.00012846255,0.000009717111,0.00028756497,0.00007518801,0.00025384536,0.00008898707,0.000015088681],"category_scores_gemma":[0.00006915556,0.00006910835,0.00003721037,0.00008688556,0.000057997247,0.00005726348,0.000020179248,0.00016701072,0.000028360839],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009446805,0.0003042554,0.47879136,0.0006680029,0.00040685522,0.00026944478,0.0025418592,0.38000312,0.047590666,0.010310803,0.009639032,0.068529926],"study_design_scores_gemma":[0.00071569806,0.00033018252,0.8854412,0.0005335562,0.0000909066,0.00006302989,0.0010707612,0.032124203,0.018391127,0.010858668,0.04965446,0.000726198],"about_ca_topic_score_codex":0.0037563108,"about_ca_topic_score_gemma":0.0072312164,"teacher_disagreement_score":0.40664986,"about_ca_system_score_codex":0.000002955054,"about_ca_system_score_gemma":0.00002801356,"threshold_uncertainty_score":0.56784433},"labels":[],"label_agreement":null},{"id":"W2994856919","doi":"10.23919/ursi-emts.2019.8931487","title":"Simple and Insightful Computation of Space-Time Crystal Dispersion Diagrams","year":2019,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Reciprocal lattice; Lattice (music); Sketch; Simple (philosophy); Computation; Dispersion (optics); Phase diagram; Space time; Spacetime; Space (punctuation); Computer science; Physics; Optics; Algorithm; Phase (matter); Quantum mechanics; Diffraction; Engineering","score_opus":0.004737070411591874,"score_gpt":0.18216311649258832,"score_spread":0.17742604608099644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994856919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99359345,0.00004898827,0.00010746797,0.000035454992,0.000110749184,0.00010499626,0.00003291995,0.000013812878,0.0059521664],"genre_scores_gemma":[0.9993394,0.000010100021,0.00018600911,0.000020756615,0.000028323157,8.735762e-8,0.00009868257,0.0000013535711,0.00031527475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99959016,0.000022969478,0.00009120061,0.0001078879,0.00009831673,0.000089479785],"domain_scores_gemma":[0.9997977,0.00004356121,0.000040267554,0.00005997977,0.0000171141,0.000041374347],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000066793626,0.000055492765,0.00012044239,0.000021102669,0.000026116628,0.000026711015,0.000038311387,0.00002621693,0.0020657496],"category_scores_gemma":[0.000003447029,0.00003950473,0.000016838543,0.00004749191,0.000022842201,0.000121628196,0.000010154585,0.00001709818,0.00026632493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016220911,0.00007433992,0.75258106,0.00026467035,0.00006977084,0.000005339199,0.0010553834,0.008776984,0.20542696,0.0023403126,0.003225571,0.02601738],"study_design_scores_gemma":[0.0005719879,0.00037697837,0.94002503,0.000020590402,0.00001906746,0.0000022131421,0.000113067435,0.042463683,0.00683769,0.003331659,0.006007519,0.00023051456],"about_ca_topic_score_codex":0.0014390466,"about_ca_topic_score_gemma":0.00011664549,"teacher_disagreement_score":0.19858927,"about_ca_system_score_codex":4.0827408e-7,"about_ca_system_score_gemma":0.000006848762,"threshold_uncertainty_score":0.9988465},"labels":[],"label_agreement":null},{"id":"W2995312363","doi":"10.1139/cjes-2019-0081","title":"Directions of lithosphere interactions in the Pamir – Hindu Kush junction inferred from anisotropic tomography","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Population and Public Health; King Saud University; National Natural Science Foundation of China; National Science Foundation","keywords":"Geology; Lithosphere; Seismology; Seismic tomography; Induced seismicity; Subduction; Anisotropy; Fibrous joint; Seismic anisotropy; Crust; Continental crust; Geophysics; Tectonics; Mantle (geology)","score_opus":0.014306391820668545,"score_gpt":0.21225535235364218,"score_spread":0.19794896053297364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995312363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923553,0.0005962019,0.000011556873,0.00033597354,0.0020665105,0.000080697595,0.00006187384,0.0000021259534,0.0044897553],"genre_scores_gemma":[0.99938715,0.000033783956,0.00027550774,0.000082033715,0.00012931622,2.6864117e-7,0.0000053651297,0.0000011170096,0.00008543699],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991165,0.00010522006,0.0002652748,0.00010624432,0.00021633224,0.0001904448],"domain_scores_gemma":[0.99936485,0.00013596739,0.00019497826,0.000104843675,0.00006888416,0.00013047957],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004290858,0.000070372145,0.00015480717,0.00020107588,0.00016543738,0.00013208773,0.0003165253,0.000024994682,0.002496695],"category_scores_gemma":[0.0000370988,0.000045446868,0.00006941365,0.00057632854,0.00014952091,0.000462598,0.0000028785216,0.00012501169,0.00003619674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006906038,0.000008713134,0.9940906,0.000003886932,0.000015252194,0.000007966166,0.0010728338,0.0013649982,0.0002904651,0.00022830938,0.00028344,0.0026266216],"study_design_scores_gemma":[0.00010740729,0.0001478381,0.9680853,0.00004904865,0.00001074644,0.000010618367,0.0011415153,0.00015394976,0.00013653371,0.00062985043,0.029467924,0.000059288897],"about_ca_topic_score_codex":0.14652058,"about_ca_topic_score_gemma":0.62415695,"teacher_disagreement_score":0.47763637,"about_ca_system_score_codex":0.0000011794517,"about_ca_system_score_gemma":0.0003914303,"threshold_uncertainty_score":0.9984152},"labels":[],"label_agreement":null},{"id":"W2997172280","doi":"10.1029/2019gc008799","title":"Improving Mass Conservation With the Tracer Ratio Method: Application to Thermochemical Mantle Flows","year":2020,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto; University of Saskatchewan","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"TRACER; Advection; Buoyancy; Thermal diffusivity; Geology; Conservation of mass; Mantle (geology); Convection; Mechanics; Entrainment (biomusicology); Thermal; Geophysics; Thermodynamics; Physics","score_opus":0.008030447380085801,"score_gpt":0.19864689231650645,"score_spread":0.19061644493642066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997172280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8848353,0.000083353974,0.10633374,0.0048484253,0.00018203948,0.0010548373,0.00030048427,0.0001516435,0.0022101712],"genre_scores_gemma":[0.9960662,0.0000015113101,0.001652525,0.0008205397,0.0008264749,0.00004947432,0.00040701902,0.000013008285,0.00016324408],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99841547,0.00007960767,0.0002781471,0.000500095,0.00037708724,0.00034957138],"domain_scores_gemma":[0.9989276,0.00013439114,0.00019870646,0.00040964366,0.00012844826,0.00020119085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002698106,0.00025112156,0.00029440297,0.000010550833,0.00023512193,0.00017765396,0.00039605383,0.00009686951,0.00021522799],"category_scores_gemma":[0.000024111194,0.00017158792,0.00006449578,0.00029221288,0.000035968857,0.00013892884,0.000026464852,0.00016397153,0.00031911864],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009119136,0.000010717472,0.000491809,0.00018141202,0.00004398567,0.0000036816964,0.0004602472,0.0044658673,0.9872973,0.00008026073,0.0012663676,0.0056071393],"study_design_scores_gemma":[0.0009571949,0.00020074866,0.0050130896,0.00006611332,0.00019537382,0.000017676113,0.0009793128,0.42641553,0.5292087,0.00070321007,0.0351164,0.0011266171],"about_ca_topic_score_codex":0.002158948,"about_ca_topic_score_gemma":0.00010207238,"teacher_disagreement_score":0.45808858,"about_ca_system_score_codex":0.0000063479088,"about_ca_system_score_gemma":0.000073049836,"threshold_uncertainty_score":0.69971526},"labels":[],"label_agreement":null},{"id":"W2997834924","doi":"10.1093/gji/ggz497","title":"The dynamics and impact of compositionally originating provinces in a mantle convection model featuring rheologically obtained plates","year":2019,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Canada Foundation for Innovation; Government of Ontario; Compute Canada","keywords":"Mantle (geology); Buoyancy; Geology; Mantle convection; Geophysics; Convection; Core–mantle boundary; Thermal; Mechanics; Physics; Thermodynamics; Subduction; Seismology; Tectonics","score_opus":0.0048966335874004886,"score_gpt":0.22952752898148213,"score_spread":0.22463089539408163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997834924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975545,0.000029817651,0.0003495912,0.00026110795,0.00029656585,0.00008732042,0.00006134434,0.0000062301137,0.0013535689],"genre_scores_gemma":[0.9990627,0.00003949735,0.00041434387,0.000013921223,0.00012671802,6.991063e-7,0.00003967203,0.0000022102465,0.00030021268],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991902,0.000047348363,0.00023119335,0.000121909165,0.00025339567,0.00015591967],"domain_scores_gemma":[0.999376,0.00023115502,0.00016979653,0.000049667866,0.00012738454,0.000046015866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025930424,0.0000904309,0.00014573248,0.000049583887,0.000104277904,0.0001434079,0.00018986655,0.00003475224,0.00011819026],"category_scores_gemma":[0.0000280065,0.000054256787,0.000060659768,0.00006566122,0.0000636208,0.00025444938,0.000024815628,0.00016588201,0.000013865533],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009765409,0.00016806478,0.5802416,0.00003796276,0.00034231239,0.000031556723,0.00034720765,0.30888003,0.018233372,0.06720377,0.00008931373,0.023448246],"study_design_scores_gemma":[0.00025264084,0.0001205093,0.45831236,0.000025461928,0.000003867442,0.000027246273,0.000024049901,0.5308479,0.00010187657,0.010216984,0.000008324079,0.000058785277],"about_ca_topic_score_codex":0.00051125424,"about_ca_topic_score_gemma":0.0001934796,"teacher_disagreement_score":0.22196786,"about_ca_system_score_codex":0.000020399308,"about_ca_system_score_gemma":0.00006713583,"threshold_uncertainty_score":0.22125275},"labels":[],"label_agreement":null},{"id":"W2997952198","doi":"10.1029/2019jb018837","title":"The Upper Mantle Structure of Northwestern Canada From Teleseismic Body Wave Tomography","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Ministry of Research, Innovation and Science","keywords":"Lithosphere; Geology; Craton; Seismology; Mantle (geology); Collision zone; Seismic tomography; Thrust fault; Crust; Geophysics; Tectonics","score_opus":0.018975202818169223,"score_gpt":0.25164305819732513,"score_spread":0.2326678553791559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997952198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99715,0.0002815572,0.000009384321,0.0012446742,0.0003515695,0.00012583875,0.0006388117,0.0000037359619,0.00019439615],"genre_scores_gemma":[0.9983864,0.00011738397,0.00008487809,0.00016457825,0.0011538763,2.0617755e-7,0.000027308013,0.0000066725656,0.00005870219],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99703765,0.00029567163,0.00047765288,0.000193043,0.0014811879,0.0005147713],"domain_scores_gemma":[0.9979151,0.0007437902,0.00025525002,0.00023291695,0.00042759327,0.00042538272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030492325,0.00015182969,0.00043181638,0.000056446373,0.0002455151,0.00013747643,0.000589568,0.0000566194,0.0005015242],"category_scores_gemma":[0.00013563818,0.00008909001,0.0001590932,0.0003733065,0.00021245683,0.00018309534,0.000060533966,0.0005984209,0.000027137192],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0069059925,0.0004913157,0.31718576,0.000622536,0.0034845606,0.0024745187,0.0069034086,0.008485554,0.47245604,0.0016991424,0.06700597,0.11228519],"study_design_scores_gemma":[0.0006187979,0.0010289935,0.91972005,0.00006886769,0.00004531742,0.000010636041,0.0004355268,0.002948267,0.028825913,0.0047802497,0.041278396,0.0002390068],"about_ca_topic_score_codex":0.35334256,"about_ca_topic_score_gemma":0.18753412,"teacher_disagreement_score":0.6025343,"about_ca_system_score_codex":0.000004254253,"about_ca_system_score_gemma":0.00063083536,"threshold_uncertainty_score":0.82729125},"labels":[],"label_agreement":null},{"id":"W2998633063","doi":"10.1021/acs.jpclett.9b03632","title":"Superconducting Zirconium Polyhydrides at Moderate Pressures","year":2020,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Engineering and Physical Sciences Research Council; Natural Sciences and Engineering Research Council of Canada; State Administration of Foreign Experts Affairs; Ministry of Science and Technology of the People's Republic of China; Ministry of Education of the People's Republic of China; National Natural Science Foundation of China; Royal Society","keywords":"Isostructural; Superconductivity; Diamond anvil cell; Zirconium; Materials science; High pressure; Crystal structure; Condensed matter physics; Diffraction; Synchrotron; Crystallography; Chemistry; Metallurgy; Engineering physics; Physics; Nuclear physics","score_opus":0.015509825982944196,"score_gpt":0.20009970581388964,"score_spread":0.18458987983094544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998633063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99274606,0.0001271676,0.000036391055,0.006578318,0.00009371577,0.00003752753,0.000029963187,0.000011952747,0.00033892423],"genre_scores_gemma":[0.9969704,0.000008681598,0.0000374163,0.00094772846,0.0019970755,1.2744097e-7,0.000005991507,0.0000052277505,0.000027307324],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99908805,0.00007043172,0.00022761743,0.0001078803,0.00028842824,0.00021760273],"domain_scores_gemma":[0.9993276,0.00017478004,0.00018942362,0.00011784141,0.000037446534,0.00015293354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016987638,0.00013672392,0.00025769367,0.0000057730144,0.00014111312,0.00005932507,0.0003808442,0.000025609654,0.00044457335],"category_scores_gemma":[0.000039843344,0.0000825863,0.00011443199,0.00006423549,0.00010345785,0.00020906382,0.000031845924,0.00021598383,0.000044648026],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012755522,0.000007922246,0.0002023192,0.000038376438,0.000055490524,0.000014521313,0.00085590547,0.023567857,0.97325504,0.0000020000846,0.0017828916,0.00009011578],"study_design_scores_gemma":[0.00024043332,0.000041876472,0.00065155263,0.000018022654,0.000094295065,0.000032318847,0.000098387594,0.0040518483,0.99311125,0.00009278741,0.0014228004,0.00014443703],"about_ca_topic_score_codex":0.00008336926,"about_ca_topic_score_gemma":0.000001959436,"teacher_disagreement_score":0.019856196,"about_ca_system_score_codex":0.000003241649,"about_ca_system_score_gemma":0.000019402887,"threshold_uncertainty_score":0.48677662},"labels":[],"label_agreement":null},{"id":"W2998670963","doi":"10.1007/s00190-019-01329-8","title":"Inertial modes of an Earth model with a compressible fluid core and elastic mantle and inner core","year":2019,"lang":"en","type":"article","venue":"Journal of Geodesy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge","funders":"","keywords":"Inner core; Mantle (geology); Physics; Inertial frame of reference; Dimensionless quantity; Normal mode; Nutation; Outer core; Core–mantle boundary; Classical mechanics; Mechanics; Geophysics; Quantum mechanics; Vibration","score_opus":0.014718072291419098,"score_gpt":0.21138419464894026,"score_spread":0.19666612235752115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998670963","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990018,0.00025661592,0.00015896936,0.000020436555,0.00008868286,0.00007236721,0.000052396543,0.0000035036483,0.00034521797],"genre_scores_gemma":[0.9977763,0.000058048667,0.0019300246,0.000031332773,0.000067832196,1.2009636e-7,0.000008308745,0.0000039464526,0.00012407741],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999309,0.000019965804,0.0002242649,0.00010608609,0.00020417401,0.00013650137],"domain_scores_gemma":[0.99947006,0.000043446933,0.00019213487,0.00009793482,0.00008265672,0.000113762224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016090524,0.000097982316,0.0002839003,0.00006347079,0.000040313837,0.00004374389,0.00009605018,0.000039423638,0.00013434271],"category_scores_gemma":[0.0000064194815,0.000061907725,0.000020485404,0.000049843664,0.00007432832,0.00030596988,0.00001446104,0.00008046858,0.0000036810586],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026800556,0.00013233906,0.21273783,0.0003488233,0.000190852,0.00006666888,0.0012086681,0.45571136,0.32049385,0.0010434825,0.0002947843,0.00509129],"study_design_scores_gemma":[0.0021072035,0.0020027305,0.20240258,0.0002196959,0.00009656784,0.00021561602,0.00015731466,0.7843408,0.005723062,0.002100315,0.00036429576,0.00026980732],"about_ca_topic_score_codex":0.00022933392,"about_ca_topic_score_gemma":0.00013466584,"teacher_disagreement_score":0.32862943,"about_ca_system_score_codex":6.591198e-7,"about_ca_system_score_gemma":0.00004876423,"threshold_uncertainty_score":0.25245237},"labels":[],"label_agreement":null},{"id":"W2999102200","doi":"10.1029/2019gc008726","title":"Long Wavelength Progressive Plateau Uplift in Eastern Anatolia Since 20 Ma: Implications for the Role of Slab Peel‐Back and Break‐Off","year":2020,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Türkiye Bilimler Akademisi","keywords":"Geology; Slab; Subduction; Lithosphere; Upwelling; Slab window; Plateau (mathematics); Mantle (geology); Tectonics; Seismology; Paleontology; Oceanic crust","score_opus":0.010412796270318906,"score_gpt":0.21395190810259943,"score_spread":0.20353911183228052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999102200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99224335,0.0026002913,0.000048028436,0.00085351686,0.00014577417,0.00089521596,0.0022217475,0.000030049647,0.00096200587],"genre_scores_gemma":[0.99878794,0.000054230593,0.00006659462,0.00004997473,0.00042317118,0.00003577916,0.00045622006,0.000011430715,0.00011465389],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99841213,0.000039043403,0.00044736863,0.0004721135,0.00020231563,0.000427032],"domain_scores_gemma":[0.9987342,0.00024052367,0.0003341573,0.00038486533,0.00014518018,0.00016108881],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016176642,0.00026158753,0.00043436888,0.00001846176,0.0001528322,0.00010987795,0.00042107893,0.00011736757,0.000068752706],"category_scores_gemma":[0.000030466956,0.00020670555,0.000087442815,0.00023051913,0.00011498974,0.00015522257,0.00006412258,0.00013981859,0.000048828853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00095053494,0.00040334897,0.6573529,0.0061382796,0.0008666996,0.00004414426,0.0063384906,0.0046612485,0.16515549,0.003377666,0.0022617325,0.15244944],"study_design_scores_gemma":[0.005844107,0.0007564539,0.5607702,0.0010375705,0.00058032025,0.00013242885,0.004221722,0.22874545,0.12228426,0.018276604,0.05419418,0.0031566638],"about_ca_topic_score_codex":0.001522763,"about_ca_topic_score_gemma":0.00022061977,"teacher_disagreement_score":0.2240842,"about_ca_system_score_codex":0.0000042868924,"about_ca_system_score_gemma":0.000088190434,"threshold_uncertainty_score":0.8429208},"labels":[],"label_agreement":null},{"id":"W2999578356","doi":"","title":"Thermochemical imaging of the lithosphere and upper mantle from geophysical observations: what can we really see?","year":2019,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"De Beers (Canada)","funders":"","keywords":"Geology; Lithosphere; Geophysics; Mantle (geology); Hotspot (geology); Seismology; Tectonics","score_opus":0.009948436734221596,"score_gpt":0.19580469447569845,"score_spread":0.18585625774147685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999578356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99537104,0.00063588796,2.3973692e-7,0.00086697354,0.00043324687,0.00014474317,0.000051212068,0.000020906542,0.0024757362],"genre_scores_gemma":[0.99887395,0.00013755553,0.0004252804,0.00018089903,0.00015100188,9.225725e-7,0.00005077929,0.000006355257,0.00017328496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99902093,0.000052572705,0.0002404786,0.00024920856,0.00021865542,0.00021815373],"domain_scores_gemma":[0.9991799,0.00028713065,0.00015980907,0.00026392526,0.00004265251,0.00006660604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001647555,0.00012988395,0.000194384,0.000008877722,0.0000871166,0.00014259072,0.00022369946,0.000054452656,0.00007317724],"category_scores_gemma":[0.000045553476,0.00008836602,0.000049654,0.00006390427,0.00006657117,0.0002520459,0.00004008111,0.000117087795,0.00006443786],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021479076,0.000023994902,0.9426667,0.000054896555,0.00003207789,0.000004330583,0.0009072392,0.0006241952,0.05055147,0.000066066976,0.00019694719,0.004850597],"study_design_scores_gemma":[0.0001445725,0.0000122156125,0.9897273,0.00027243665,0.000023648689,0.0000015746068,0.00033519013,0.0004095068,0.00620161,0.0021182199,0.00062550703,0.00012817404],"about_ca_topic_score_codex":0.049131077,"about_ca_topic_score_gemma":0.0033358592,"teacher_disagreement_score":0.04706064,"about_ca_system_score_codex":0.0000021094243,"about_ca_system_score_gemma":0.000036526424,"threshold_uncertainty_score":0.9572008},"labels":[],"label_agreement":null},{"id":"W3000104457","doi":"10.1029/2019gl085721","title":"Episodic Lithospheric Deformation in Eastern Tibet Inferred From Seismic Anisotropy","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Geology; Crust; Lithosphere; Seismology; Anisotropy; Plateau (mathematics); Upwelling; Geophysics; Seismic anisotropy; Mantle (geology); Tectonics","score_opus":0.03866680216127294,"score_gpt":0.27245319373371835,"score_spread":0.2337863915724454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000104457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913669,0.000052443396,0.00051345915,0.006978801,0.00017371408,0.00028528192,0.00013744534,0.000050572828,0.00044133083],"genre_scores_gemma":[0.99671555,0.000018798215,0.0003409305,0.0019493789,0.0006282631,0.000007005121,0.00029922987,0.000008414241,0.000032427946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997454,0.00038656805,0.00029056007,0.00041413613,0.00075753615,0.00069722167],"domain_scores_gemma":[0.99907386,0.00027536807,0.000057279205,0.0002388827,0.000048377555,0.0003062379],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029188322,0.00017205741,0.00029185845,0.000059901788,0.00012803669,0.00021029847,0.00043610384,0.00006771444,0.0008044014],"category_scores_gemma":[0.0001103643,0.00014779583,0.000067188616,0.000578495,0.00013952487,0.0004676322,0.000074571035,0.0004084779,0.004972683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002682521,0.00048622952,0.40092584,0.0005448693,0.00029110129,0.0009347806,0.015902622,0.04150998,0.3253912,0.0011561712,0.043310784,0.1668639],"study_design_scores_gemma":[0.0012635416,0.00042445248,0.82458353,0.00006300586,0.000013503253,8.5422135e-7,0.00022455321,0.14926124,0.0019327173,0.0049637402,0.016760627,0.0005082565],"about_ca_topic_score_codex":0.020233313,"about_ca_topic_score_gemma":0.00025367114,"teacher_disagreement_score":0.4236577,"about_ca_system_score_codex":0.000012134929,"about_ca_system_score_gemma":0.000059650192,"threshold_uncertainty_score":0.99580204},"labels":[],"label_agreement":null},{"id":"W3000132780","doi":"10.1103/physrevlett.125.217001","title":"Hydrogen Pentagraphenelike Structure Stabilized by Hafnium: A High-Temperature Conventional Superconductor","year":2020,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":159,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Program for Changjiang Scholars and Innovative Research Team in University; Gates Cambridge Trust; National Key Research and Development Program of China; Engineering and Physical Sciences Research Council; China Scholarship Council; Jilin University; Royal Society; Cambridge Trust; National Natural Science Foundation of China","keywords":"Hafnium; Materials science; Hydrogen; Superconductivity; High-temperature superconductivity; Condensed matter physics; Room-temperature superconductor; Engineering physics; Metallurgy; Chemistry; Physics; Zirconium","score_opus":0.010636643187028217,"score_gpt":0.22231476515158924,"score_spread":0.211678121964561,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000132780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9809962,0.0048867017,0.0000024854533,0.0116214445,0.0002579953,0.00042453498,0.0017358019,0.000053101085,0.00002176026],"genre_scores_gemma":[0.9687569,0.0011302866,0.000092526054,0.027828079,0.00060235785,0.0000052869173,0.0015665621,0.000010209993,0.00000774847],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983354,0.00017822233,0.00027895442,0.0004693514,0.00041131975,0.00032675243],"domain_scores_gemma":[0.9993068,0.00006938382,0.00009411441,0.00021872678,0.000034096443,0.00027689262],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008096365,0.000271553,0.00057172956,0.000013031231,0.0001006587,0.00007683294,0.0003381443,0.000023798018,0.0053972993],"category_scores_gemma":[0.000027095579,0.00020112646,0.00021820958,0.00022407442,0.00009184409,0.00025395543,0.000024181696,0.00020217156,0.00039508348],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003301329,0.000029743544,0.0010073858,0.00077057123,0.000094302966,0.000010576042,0.00010933997,0.00012805976,0.9161954,0.00017454602,0.08125782,0.00018922516],"study_design_scores_gemma":[0.0065231724,0.0011033202,0.025902143,0.0021004924,0.0019493278,0.00003626368,0.00013631112,0.0018694752,0.2005813,0.0036861734,0.7507719,0.0053401524],"about_ca_topic_score_codex":0.00021347275,"about_ca_topic_score_gemma":0.000011280312,"teacher_disagreement_score":0.71561414,"about_ca_system_score_codex":0.0000030655658,"about_ca_system_score_gemma":0.000026076084,"threshold_uncertainty_score":0.9955119},"labels":[],"label_agreement":null},{"id":"W3005091384","doi":"","title":"A new estimate of the effective elastic thickness of the Canadian shield from admittance analyses using the wavelet transform, and models of flexure and mantle convection","year":2013,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shield; Geology; Mantle (geology); Wavelet; Admittance; Wavelet transform; Geophysics; Geodesy; Electrical impedance; Computer science; Engineering; Petrology; Artificial intelligence","score_opus":0.01976478470234474,"score_gpt":0.237564860848034,"score_spread":0.21780007614568925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005091384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981764,0.0002583728,0.0000611558,0.0001815606,0.00016627459,0.0003023607,0.00009110564,0.0000033421295,0.00075942674],"genre_scores_gemma":[0.99957204,0.000012851177,0.00033790743,0.000028075161,0.000030997555,0.0000010330648,0.000003174262,0.000003092361,0.000010829622],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9992754,0.00008504966,0.00021307617,0.00012677906,0.00015453961,0.00014516956],"domain_scores_gemma":[0.9991652,0.00036334436,0.00020740097,0.0001475031,0.00005334547,0.00006323054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021686261,0.00009807739,0.00019134532,0.000021354446,0.00017139332,0.00003988496,0.00015055414,0.000063433436,0.000013724951],"category_scores_gemma":[0.00006782238,0.00004909593,0.00003592444,0.00009783761,0.00012542866,0.00012872624,0.000011612847,0.00009581915,6.8486645e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012959231,0.000033302284,0.19998711,0.0005816442,0.00043950704,0.0000035127944,0.01119491,0.6588774,0.10795623,0.00027006373,0.00012140002,0.020405352],"study_design_scores_gemma":[0.00017571726,0.000034112534,0.9305219,0.00024649402,0.0001351136,0.000003997216,0.00018804733,0.041011546,0.022735892,0.004847209,0.000010106476,0.00008988154],"about_ca_topic_score_codex":0.90608925,"about_ca_topic_score_gemma":0.68695784,"teacher_disagreement_score":0.7305348,"about_ca_system_score_codex":0.0000025754653,"about_ca_system_score_gemma":0.0000981226,"threshold_uncertainty_score":0.3187544},"labels":[],"label_agreement":null},{"id":"W3006637467","doi":"","title":"The Unique Bushveld Complex: Superheat-Dominant Impact Processes Beyond Sudbury","year":2006,"lang":"en","type":"article","venue":"M&PSA","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Earth science; Astrobiology","score_opus":0.010529443274508625,"score_gpt":0.22231924356621505,"score_spread":0.2117898002917064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006637467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9832957,0.00095045107,0.0000546435,0.0005055075,0.00041776538,0.0002483205,0.0004508069,0.00005024007,0.0140265655],"genre_scores_gemma":[0.99780005,0.00010123208,0.00010411591,0.00009993864,0.00039992548,0.0000033941708,0.000302111,0.0000061509027,0.0011830573],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9988481,0.00006989879,0.00022604206,0.00021433919,0.00021649827,0.00042516342],"domain_scores_gemma":[0.9992995,0.0002297772,0.00006665837,0.00024810035,0.00007363648,0.000082316925],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002980693,0.00017319612,0.00020815102,0.000028794933,0.0004150352,0.00023153279,0.00030732228,0.00005897967,0.0012573468],"category_scores_gemma":[0.000028545095,0.000097255535,0.00006057872,0.00018525802,0.00011713715,0.00016085259,0.00001832654,0.000079810365,0.00034728253],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011190063,0.0004475597,0.42970416,0.00068616436,0.00036650096,0.00029160193,0.0016273856,0.011879281,0.07882859,0.008987648,0.43006086,0.036001217],"study_design_scores_gemma":[0.000455657,0.00029843318,0.5971946,0.000030623767,0.00004354843,0.000028231478,0.00009070896,0.0006166148,0.011708866,0.009746149,0.37930033,0.00048621368],"about_ca_topic_score_codex":0.019315843,"about_ca_topic_score_gemma":0.008679328,"teacher_disagreement_score":0.16749047,"about_ca_system_score_codex":0.0000036207712,"about_ca_system_score_gemma":0.00012253405,"threshold_uncertainty_score":0.99965566},"labels":[],"label_agreement":null},{"id":"W3010751455","doi":"","title":"Modelling melting rates in upwelling mantle","year":2010,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Upwelling; Mantle (geology); Partial melting; Geology; Instability; Thermodynamics; Geophysics; Mechanics; Physics","score_opus":0.027716469776201447,"score_gpt":0.23612243341593991,"score_spread":0.20840596363973846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010751455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95493364,0.000022663846,0.0053841616,0.0002119063,0.00016296456,0.00028966035,0.00027807988,0.000038522296,0.038678415],"genre_scores_gemma":[0.9858898,0.0005679136,0.012058025,0.000006200718,0.0000647637,3.1011382e-8,0.00013865842,0.000007567203,0.0012670727],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9977548,0.00029549495,0.00015799819,0.0004884806,0.00053611497,0.0007670951],"domain_scores_gemma":[0.99859244,0.00046620384,0.00012229812,0.00036683612,0.00017540176,0.00027680153],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001115191,0.00018309915,0.00034982283,0.0006996098,0.0007645334,0.00005541122,0.0010748453,0.00012874186,0.0013786829],"category_scores_gemma":[0.000037553702,0.00022052976,0.0001250963,0.00070746266,0.00053383416,0.0006800931,0.00025738272,0.0007808778,0.00004932051],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0041383775,0.0006205956,0.6103109,0.0007591177,0.0004121054,0.0022465915,0.015636073,0.23581734,0.04256098,0.049642712,0.0022241855,0.035631023],"study_design_scores_gemma":[0.0028370114,0.00051600893,0.078280225,0.00021904416,0.000064397595,0.000013833193,0.01760426,0.6155,0.0011621438,0.019649236,0.2631691,0.0009847505],"about_ca_topic_score_codex":0.018619731,"about_ca_topic_score_gemma":0.02091714,"teacher_disagreement_score":0.5320307,"about_ca_system_score_codex":0.000015188995,"about_ca_system_score_gemma":0.0001850999,"threshold_uncertainty_score":0.9995342},"labels":[],"label_agreement":null},{"id":"W3012404287","doi":"","title":"Velocity Structure of the Crust and Uppermost Mantle Beneath Canada by Inversion of S, SP, SsPmP, and Shear-coupled PL waveforms","year":2006,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Crust; Shear (geology); Mantle (geology); Shear zone; Geophysics; Paleontology; Tectonics","score_opus":0.003997661473782398,"score_gpt":0.16224037819003168,"score_spread":0.1582427167162493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3012404287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806815,0.00021626565,1.9010177e-7,0.0001038173,0.00018042001,0.00010070191,0.00046444018,0.0000051620773,0.0008608722],"genre_scores_gemma":[0.9996403,0.000024424848,0.00010659282,0.00004370753,0.000045510536,1.0322406e-7,0.00007820237,0.000003226814,0.00005797306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991745,0.000021842037,0.00023412539,0.0001586132,0.0002281738,0.00018278859],"domain_scores_gemma":[0.9995214,0.00007506376,0.00018882289,0.00012193677,0.000034952467,0.000057871937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001253908,0.000112122485,0.00018813234,0.000013653595,0.00012933309,0.000025353565,0.000114546056,0.00006414501,0.000018863855],"category_scores_gemma":[0.000029524917,0.00007200567,0.000017357976,0.000057619294,0.00008148885,0.00007173566,0.000026516846,0.00007620371,5.3226813e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006710967,0.000025989488,0.8463594,0.00035351058,0.000044988876,0.000009453343,0.0003141877,0.007691188,0.13876398,0.00005425031,0.0040373644,0.0022786015],"study_design_scores_gemma":[0.00019349915,0.000025404332,0.97026783,0.000055217773,0.000019517223,0.0000032394255,0.000064974156,0.0009163082,0.02758657,0.0002549677,0.0005094848,0.00010297024],"about_ca_topic_score_codex":0.9456001,"about_ca_topic_score_gemma":0.7856024,"teacher_disagreement_score":0.1599977,"about_ca_system_score_codex":0.0000035308924,"about_ca_system_score_gemma":0.000074546806,"threshold_uncertainty_score":0.2936306},"labels":[],"label_agreement":null},{"id":"W3014364723","doi":"","title":"On the Relationships Between Slab dip, Back-arc Stress, Upper Plate Absolute Motion and Crustal Nature in Subduction Zones","year":2005,"lang":"en","type":"article","venue":"AGUFM","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Slab; Slab window; Seismology; Lithosphere; Convergent boundary; Volcanic arc; Seamount; Magnetic dip; Discontinuity (linguistics); Oceanic crust; Geophysics; Tectonics; Paleontology","score_opus":0.015358679679080287,"score_gpt":0.20704108395888077,"score_spread":0.1916824042798005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014364723","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957867,0.00021801132,0.000017786337,0.0017455373,0.00024249758,0.00014457302,0.00015078686,0.000016905784,0.0016771946],"genre_scores_gemma":[0.9988741,0.000055362456,0.00013081626,0.00006338154,0.00037245243,0.0000011868722,0.00016639549,0.0000034547124,0.00033281924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992333,0.000109895846,0.00014364341,0.0001801253,0.00014109939,0.00019194212],"domain_scores_gemma":[0.9995759,0.00017388059,0.00005443903,0.00013139976,0.000015453246,0.000048924336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003082931,0.00009792827,0.00010673644,0.000045690416,0.0001775944,0.00007155211,0.000084190564,0.00012553597,0.0007266762],"category_scores_gemma":[0.000040520008,0.000066125765,0.000020995385,0.000101328944,0.00004292772,0.00025204508,0.000010100039,0.00026436147,0.0003179301],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002313576,0.00011240726,0.8738194,0.00010205784,0.00012423925,0.000017587443,0.0032244327,0.03145635,0.0010072256,0.025031416,0.0046640085,0.060209487],"study_design_scores_gemma":[0.00015790945,0.000031669177,0.9887084,0.000023210334,0.00001177893,0.0000015057803,0.000059587685,0.0014426183,0.0003959382,0.0045578987,0.0044995197,0.000110010165],"about_ca_topic_score_codex":0.0010982571,"about_ca_topic_score_gemma":0.0024047827,"teacher_disagreement_score":0.11488892,"about_ca_system_score_codex":0.0000035327175,"about_ca_system_score_gemma":0.000008907538,"threshold_uncertainty_score":0.7956595},"labels":[],"label_agreement":null},{"id":"W3014431839","doi":"","title":"Lithospheric architecture beneath Hudson Bay","year":2015,"lang":"en","type":"article","venue":"Archipelago (Université du Québec à Montréal)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Craton; Lithosphere; Geology; Archean; Seismology; Precambrian; Asthenosphere; Proterozoic; Classification of discontinuities; Geophysics; Paleontology; Tectonics","score_opus":0.006809166023904644,"score_gpt":0.1536276442244627,"score_spread":0.14681847820055807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014431839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877605,0.0018657098,0.00092995446,0.0012669293,0.00041282797,0.00018510858,0.000093923,0.00013803168,0.007347008],"genre_scores_gemma":[0.9967196,0.00007626702,0.0019770868,0.00022039817,0.0002721377,7.937176e-7,0.00007716078,0.000011564065,0.0006449776],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985359,0.00012326254,0.00016857193,0.00038228947,0.00034630214,0.0004437229],"domain_scores_gemma":[0.99888986,0.0001148606,0.00010285425,0.00038309488,0.00006397562,0.000445337],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021146594,0.00024763294,0.00030095706,0.00007443007,0.00028044655,0.00007194216,0.0004762797,0.000082335784,0.0012547986],"category_scores_gemma":[0.000035929526,0.00021460012,0.00011339368,0.00024786475,0.000109619155,0.00025089114,0.000075262986,0.00017058339,0.00075862237],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016370538,0.00029533522,0.20690754,0.00012769752,0.0005177181,0.0014007716,0.23264189,0.04823179,0.0012577275,0.0051125386,0.023029888,0.47884005],"study_design_scores_gemma":[0.0030720232,0.0011169469,0.4776181,0.0000661381,0.00025592634,0.00015790501,0.014673768,0.0075179753,0.00028806686,0.013770774,0.47991335,0.0015490155],"about_ca_topic_score_codex":0.43584266,"about_ca_topic_score_gemma":0.50996304,"teacher_disagreement_score":0.47729105,"about_ca_system_score_codex":0.000018766248,"about_ca_system_score_gemma":0.00027097992,"threshold_uncertainty_score":0.99965817},"labels":[],"label_agreement":null},{"id":"W3014846542","doi":"10.1038/s41561-020-0560-y","title":"Iron isotope fractionation at the core–mantle boundary by thermodiffusion","year":2020,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Directorate for Geosciences","keywords":"Mantle (geology); Isotope fractionation; Geology; Isotope; Equilibrium fractionation; Core–mantle boundary; Fractionation; Mantle convection; Basalt; Outer core; Geochemistry; Isotopic signature; Inner core; Geophysics; Chemistry; Subduction","score_opus":0.009448338421837722,"score_gpt":0.21563253514214561,"score_spread":0.20618419672030788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014846542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98856556,0.0011536457,0.0001282863,0.0050322576,0.0010666248,0.00019279493,0.00027209183,0.0000446683,0.0035440645],"genre_scores_gemma":[0.99382555,0.00006599012,0.0000805565,0.0040857065,0.00024327276,0.0000014730867,0.00016803239,0.0000028884836,0.0015265179],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99882555,0.00004549003,0.000119481425,0.0003185637,0.00046598914,0.00022492342],"domain_scores_gemma":[0.9995193,0.00008860498,0.000087152854,0.00016779386,0.00003845405,0.000098727716],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002286722,0.00011024386,0.00009874874,0.000014638031,0.0006131817,0.00012622969,0.00038514135,0.00011643422,0.003139039],"category_scores_gemma":[0.00007331668,0.000066409295,0.000034052828,0.0002476521,0.00015186712,0.00025239005,0.00004622342,0.00024226106,0.00057334057],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031546678,0.00008604352,0.06394673,0.00007297816,0.000020679545,0.000023632507,0.00183601,0.001244182,0.5406261,0.0015076136,0.3382752,0.052045383],"study_design_scores_gemma":[0.00022898361,0.00013159197,0.25783873,0.000008275807,0.000013885549,0.000006659672,0.00006769389,0.008443129,0.0032026707,0.00089025806,0.7289128,0.00025536757],"about_ca_topic_score_codex":0.0005475356,"about_ca_topic_score_gemma":0.00017152823,"teacher_disagreement_score":0.53742343,"about_ca_system_score_codex":0.0000050811245,"about_ca_system_score_gemma":0.000040886494,"threshold_uncertainty_score":0.9977722},"labels":[],"label_agreement":null},{"id":"W3017796834","doi":"","title":"Geodynamic models of mature continental collision: Evolution of an orogen from lithospheric subduction to continental retreat/delamination","year":2011,"lang":"en","type":"article","venue":"AGUFM","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Subduction; Collision zone; Mantle (geology); Crust; Continental collision; Eclogitization; Continental crust; Crustal recycling; Convergent boundary; Geophysics; Delamination (geology); Plate tectonics; Seismology; Oceanic crust; Tectonics","score_opus":0.01022692255915019,"score_gpt":0.18857802640670757,"score_spread":0.17835110384755737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3017796834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968211,0.00018004673,0.0006407805,0.000014854279,0.00050712476,0.00022959679,0.0006411975,0.000022918843,0.00094235584],"genre_scores_gemma":[0.9966016,0.000012996149,0.0026585462,0.000008003733,0.00009123665,0.0000018031355,0.00052162766,0.00000496579,0.000099235214],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999084,0.000062952444,0.000275478,0.00022288306,0.00021195292,0.00014275387],"domain_scores_gemma":[0.9994274,0.000018740408,0.00017828746,0.00020055691,0.000102647165,0.000072378665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013607755,0.0001143417,0.00023014672,0.000041402036,0.000045814642,0.000013200032,0.00014789241,0.000091590824,0.0005947352],"category_scores_gemma":[0.000010009056,0.00009965234,0.000048563434,0.00017107007,0.000042600353,0.00038365714,0.000014471867,0.000041455954,0.000030023568],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005338938,0.0015833472,0.2655866,0.00034975208,0.00059619197,0.00007124626,0.02011866,0.064278334,0.5831632,0.014619247,0.0010250625,0.04326942],"study_design_scores_gemma":[0.0006597126,0.000638097,0.88326406,0.00006618241,0.000093969276,0.0000064902556,0.0006762668,0.059225053,0.048517503,0.006454794,0.00012304205,0.00027484194],"about_ca_topic_score_codex":0.041697543,"about_ca_topic_score_gemma":0.0022948482,"teacher_disagreement_score":0.61767745,"about_ca_system_score_codex":0.0000072791136,"about_ca_system_score_gemma":0.000022308852,"threshold_uncertainty_score":0.9646839},"labels":[],"label_agreement":null},{"id":"W3021167953","doi":"10.1016/j.pepi.2020.106485","title":"Effects of ongoing melting and buoyancy on melt band evolution in a compacting porous layer","year":2020,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Buoyancy; Porosity; Viscosity; Materials science; Amplitude; Volume viscosity; Thermodynamics; Isotropy; Porous medium; Instability; Mantle (geology); Permeability (electromagnetism); Mechanics; Mineralogy; Composite material; Geology; Geophysics; Chemistry; Physics; Optics","score_opus":0.00953812078731706,"score_gpt":0.18853656129097301,"score_spread":0.17899844050365596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021167953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99877036,0.00036258964,0.00001585662,0.00010043115,0.00015878963,0.00016242439,0.00007899346,0.000007719588,0.0003428303],"genre_scores_gemma":[0.99967206,0.000033467793,0.0000844761,0.00009107701,0.000092832866,2.914238e-7,0.000018821018,0.0000032252506,0.0000037505797],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992489,0.000089859284,0.00020846279,0.0001633065,0.00013186553,0.00015761277],"domain_scores_gemma":[0.99944454,0.00023807521,0.00015810489,0.00008370143,0.000011944595,0.00006360888],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106101106,0.0001233609,0.00028019675,0.000023432609,0.000056243967,0.00001926053,0.000106120635,0.00003232303,0.000023139606],"category_scores_gemma":[0.000034546072,0.00008932013,0.00003184975,0.000092219045,0.000059216767,0.00011084068,0.00002119662,0.00011336942,0.0000039920715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008854948,0.00007303205,0.75484765,0.0019621928,0.00017235322,0.000025475088,0.006687949,0.011400754,0.1864164,0.00032568641,0.00006494867,0.037138052],"study_design_scores_gemma":[0.0005860325,0.00037341943,0.9351415,0.00040321992,0.000043314492,0.000004335134,0.00011456807,0.006657033,0.05576052,0.0006872194,0.000052556818,0.00017627164],"about_ca_topic_score_codex":0.0029318128,"about_ca_topic_score_gemma":0.0003105579,"teacher_disagreement_score":0.18029386,"about_ca_system_score_codex":7.4418705e-7,"about_ca_system_score_gemma":0.000013131507,"threshold_uncertainty_score":0.44320434},"labels":[],"label_agreement":null},{"id":"W3023448308","doi":"10.1002/ange.201704364","title":"Modulated Structure Calculated for Superconducting Hydrogen Sulfide","year":2017,"lang":"en","type":"article","venue":"Angewandte Chemie","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Tetragonal crystal system; Superconductivity; Metadynamics; Electron diffraction; Crystallography; Chemistry; Chemical physics; Anisotropy; Electron; Crystal structure; Condensed matter physics; Proton; Hydrogen; Materials science; Diffraction; Molecular dynamics; Molecular physics; Computational chemistry; Physics","score_opus":0.025401181232909156,"score_gpt":0.24615795061892476,"score_spread":0.2207567693860156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3023448308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99702114,0.00016606209,0.000007366435,0.00017648708,0.0004784406,0.00020641137,0.0006328681,0.000048967093,0.0012622405],"genre_scores_gemma":[0.9981597,0.00001119274,0.0003275609,0.000071641225,0.00043611493,0.0000018097033,0.00055204256,0.000008562686,0.00043138253],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990833,0.000011167136,0.00016649604,0.00028269962,0.00012383582,0.00033250294],"domain_scores_gemma":[0.99924463,0.000039263203,0.00011293773,0.00043217163,0.00006314464,0.000107881955],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012948392,0.00015710625,0.0002277525,0.000020927318,0.0005419239,0.00020551037,0.00034996896,0.00011705262,0.0010117554],"category_scores_gemma":[0.00008939173,0.00012756021,0.000073309275,0.000032345895,0.00006471609,0.0003062238,0.000023562625,0.000067063665,0.00003684207],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036604706,0.0000064082424,0.010566363,0.000045633842,0.000078207195,0.00001091071,0.00016857675,0.00033392527,0.9863892,0.000046181576,0.0009194266,0.0013985425],"study_design_scores_gemma":[0.0004217414,0.000025582962,0.013829099,0.000014587699,0.00003893367,0.000005615316,0.000019584397,0.0003360781,0.9739879,0.0019493601,0.009161574,0.0002099746],"about_ca_topic_score_codex":0.002591453,"about_ca_topic_score_gemma":0.0005256592,"teacher_disagreement_score":0.012401351,"about_ca_system_score_codex":0.0000026963169,"about_ca_system_score_gemma":0.000027057244,"threshold_uncertainty_score":0.9999015},"labels":[],"label_agreement":null},{"id":"W3024006250","doi":"10.1039/c9cp05267d","title":"Stability and metallization of solid oxygen at high pressure","year":2020,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada; Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"Anharmonicity; Phase diagram; Thermodynamics; Oxygen; Solid oxygen; Lattice (music); Solid solution; Materials science; Phase (matter); Electronic structure; Metal; Molecular dynamics; Thermal; Atmospheric temperature range; Chemistry; Thermal stability; Condensed matter physics; Computational chemistry; Physics; Metallurgy","score_opus":0.014999633496841266,"score_gpt":0.20767468699985506,"score_spread":0.19267505350301378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024006250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979153,0.00006931113,0.00009997619,0.00016560472,0.000023698807,0.000106651205,0.00076661835,0.00004416864,0.00080866524],"genre_scores_gemma":[0.9987727,0.000008292953,0.00011452204,0.00006774125,0.0006301798,0.0000018387158,0.00037550862,0.000007797648,0.000021466161],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99885976,0.000023169083,0.00021867972,0.00039324697,0.00028129754,0.00022384086],"domain_scores_gemma":[0.99927586,0.0000951436,0.00013035769,0.00020590353,0.00006625281,0.00022645213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000041947984,0.00019734517,0.00041686802,0.0000019720233,0.00004687164,0.00001865618,0.00019818248,0.000071381764,0.00053304184],"category_scores_gemma":[0.000049814975,0.00017272102,0.000088769884,0.00012486646,0.00018114396,0.00013116858,0.00008533242,0.000115601564,0.000027244649],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007140779,0.000062816995,0.00044000862,0.000411826,0.00005583447,6.606263e-7,0.00021273163,0.0003845837,0.9977653,0.000090627684,0.00014084988,0.00036337267],"study_design_scores_gemma":[0.00023686336,0.000026287413,0.0008933584,0.000007671771,0.000093168754,3.6118664e-7,0.00000841691,0.006331629,0.98741734,0.0042951126,0.00049736747,0.00019244723],"about_ca_topic_score_codex":0.00008629366,"about_ca_topic_score_gemma":7.540837e-7,"teacher_disagreement_score":0.010347964,"about_ca_system_score_codex":0.0000028850068,"about_ca_system_score_gemma":0.00002032555,"threshold_uncertainty_score":0.70433587},"labels":[],"label_agreement":null},{"id":"W3024729862","doi":"","title":"Re-Os Isotopic Constraints on the Generation of the Low-Cr Megacryst Suite","year":2001,"lang":"en","type":"article","venue":"Eleventh Annual V. M. Goldschmidt Conference","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"De Beers (Canada)","funders":"","keywords":"Suite; Environmental science; Economics; Political science","score_opus":0.029037874770906615,"score_gpt":0.22099402257514825,"score_spread":0.19195614780424164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024729862","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9855068,0.000067651425,0.000113057285,0.001457658,0.0009417795,0.00044062134,0.0005506973,0.000024338862,0.010897445],"genre_scores_gemma":[0.9976079,0.000057194688,0.000027655788,0.0005887838,0.0003325791,0.0000055138767,0.00006118824,0.0000047108065,0.0013144693],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9984012,0.00025644887,0.00033488488,0.0002909366,0.00036800423,0.0003485019],"domain_scores_gemma":[0.9989075,0.00017140548,0.00020848638,0.00046580273,0.00015399716,0.00009280543],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038762295,0.00020200538,0.00023624029,0.00003285161,0.00024699958,0.00010084652,0.0005638318,0.000087695815,0.0075235344],"category_scores_gemma":[0.00010042016,0.00011135563,0.00009373153,0.00018879863,0.0002749462,0.00017290043,0.000035973775,0.00016624742,0.00020621798],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090053934,0.001007219,0.24831098,0.0004596443,0.0007926092,0.00014731642,0.018219685,0.0067692185,0.1768882,0.14120603,0.08271538,0.3225832],"study_design_scores_gemma":[0.0016083264,0.00085277844,0.7611859,0.00045708934,0.00011744237,0.000025306297,0.0022136793,0.005537614,0.09408463,0.00594747,0.1267038,0.0012659952],"about_ca_topic_score_codex":0.00057154393,"about_ca_topic_score_gemma":0.0012496256,"teacher_disagreement_score":0.5128749,"about_ca_system_score_codex":0.0000038642565,"about_ca_system_score_gemma":0.00013367935,"threshold_uncertainty_score":0.9933837},"labels":[],"label_agreement":null},{"id":"W3025164461","doi":"","title":"Stress Rotation Across the Cascadia Megathrust Requires a Weak Subduction Plate Boundary at Seismogenic Depths","year":2017,"lang":"en","type":"article","venue":"AGUFM","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Subduction; Seismology; Pacific Plate; Plate tectonics; Mantle (geology); Slip (aerodynamics); Episodic tremor and slip; Thrust; Convergent boundary; Thrust fault; Stress field; Focal mechanism; Fault (geology); Geophysics; Tectonics; Oceanic crust","score_opus":0.01691115476061601,"score_gpt":0.2522358878972768,"score_spread":0.2353247331366608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025164461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99346364,0.00040213988,0.000015318945,0.0005823644,0.0017615241,0.00020594154,0.00039542885,0.00003815984,0.0031354737],"genre_scores_gemma":[0.99616176,0.000096337935,0.000040690964,0.0000804317,0.00053059467,0.000004794279,0.00017703751,0.000006239057,0.002902144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890476,0.000071281385,0.00018347037,0.00026295325,0.00022960965,0.00034793283],"domain_scores_gemma":[0.9990651,0.000063097774,0.00021104545,0.00054054795,0.000039164202,0.00008104782],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00031715192,0.00014170159,0.00015346725,0.000014762411,0.0020880082,0.00061016675,0.00041584767,0.00007871686,0.0006247808],"category_scores_gemma":[0.000042625717,0.000095590454,0.000065866116,0.000038607373,0.00021323239,0.0005376512,0.000054951935,0.000086416985,0.0006114721],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014061833,0.00017204907,0.5338195,0.00039497332,0.0008793446,0.00034719682,0.017659372,0.03174133,0.061087463,0.0022042124,0.023832912,0.32645547],"study_design_scores_gemma":[0.00046626074,0.000088004555,0.90608037,0.000034101344,0.000055651122,0.000036731166,0.00030548134,0.0030408306,0.011762336,0.001465571,0.07633733,0.0003273641],"about_ca_topic_score_codex":0.021838197,"about_ca_topic_score_gemma":0.037730135,"teacher_disagreement_score":0.37226087,"about_ca_system_score_codex":0.000006532308,"about_ca_system_score_gemma":0.000035552825,"threshold_uncertainty_score":0.99921113},"labels":[],"label_agreement":null},{"id":"W3025829548","doi":"10.1021/acs.jpca.0c03330","title":"Formation of Stable Compounds of Potassium and Iron under Pressure","year":2020,"lang":"en","type":"article","venue":"The Journal of Physical Chemistry A","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Potassium; Chemistry; Organic chemistry","score_opus":0.011334602323439967,"score_gpt":0.2009070747457504,"score_spread":0.18957247242231043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025829548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983155,0.00016779464,0.00013687028,0.00036474317,0.00001347343,0.00002685693,0.000059972113,0.0000017994956,0.0009129967],"genre_scores_gemma":[0.9997278,0.000015290267,0.000021149379,0.000025914136,0.00018402841,3.3119125e-8,0.0000051693096,0.0000012675763,0.000019388406],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995157,0.000030449874,0.00017985364,0.00003467659,0.00017200942,0.000067280445],"domain_scores_gemma":[0.99948233,0.00007913516,0.00027382342,0.000057379566,0.000053199066,0.000054120614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011884015,0.00005398335,0.00018362829,0.0000036084107,0.00002481943,0.000009735245,0.00012965043,0.000019199702,0.00008537655],"category_scores_gemma":[0.000011726473,0.000032181888,0.000036662826,0.00004533496,0.000064264845,0.00012821778,0.00001289041,0.00007634625,0.0000011726453],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014349229,0.000024557816,0.00008555221,0.0003176649,0.000027002849,4.715827e-7,0.0006570889,0.016069189,0.98213506,0.000026717547,0.00038463154,0.00012856105],"study_design_scores_gemma":[0.00039756508,0.00023129069,0.0041725794,0.000044236258,0.00016407383,0.0000106211355,0.00026446523,0.013678212,0.9786852,0.0013237941,0.0009515497,0.00007643361],"about_ca_topic_score_codex":0.000038606842,"about_ca_topic_score_gemma":7.5131436e-7,"teacher_disagreement_score":0.004087027,"about_ca_system_score_codex":5.5243333e-7,"about_ca_system_score_gemma":0.000017496754,"threshold_uncertainty_score":0.13123393},"labels":[],"label_agreement":null},{"id":"W3026947625","doi":"10.1029/2019ea000881","title":"Toward a Unified Model for the Thermal State of the Planetary Mantle: Estimations From Mean Field Deep Learning","year":2020,"lang":"en","type":"article","venue":"Earth and Space Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Planet; Mantle (geology); Heat flux; Curvature; Artificial intelligence; Geology; Computer science; Geophysics; Physics; Mathematics; Geometry; Mechanics; Heat transfer","score_opus":0.022412240220328172,"score_gpt":0.20753842472991035,"score_spread":0.18512618450958218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3026947625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98488295,0.00025226004,0.010189459,0.0036647478,0.00016695059,0.00023380159,0.00013677221,0.000015284357,0.00045775325],"genre_scores_gemma":[0.99788934,0.000028992843,0.0015987146,0.00033396046,0.00004452796,8.844692e-7,0.0000087951885,0.0000014406337,0.00009334907],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99932647,0.000027416434,0.00009686563,0.0001710498,0.00019965098,0.00017856661],"domain_scores_gemma":[0.9994809,0.0002257038,0.0000650328,0.000118690514,0.000028544746,0.000081106344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021734707,0.00007038828,0.00009591156,0.000011997328,0.00038280088,0.00008871399,0.00030432676,0.000015650357,0.0001052172],"category_scores_gemma":[0.00008860376,0.0000377058,0.0000257928,0.00014383244,0.00019986033,0.00014455875,0.000031925774,0.00008128982,0.000007918478],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010857913,0.0000064027095,0.013856351,0.000031261927,0.00002198184,0.0000014351874,0.011800447,0.9186458,0.012358469,0.00054072856,0.00013395752,0.042494584],"study_design_scores_gemma":[0.00010634398,0.00005800542,0.087714024,0.0000059820422,0.000013213391,3.8178047e-7,0.00012056521,0.9082668,0.0024775132,0.0007137842,0.0004611315,0.00006225249],"about_ca_topic_score_codex":0.0011998769,"about_ca_topic_score_gemma":0.0007968679,"teacher_disagreement_score":0.07385767,"about_ca_system_score_codex":2.9667737e-7,"about_ca_system_score_gemma":0.00006155076,"threshold_uncertainty_score":0.29442334},"labels":[],"label_agreement":null},{"id":"W3026949239","doi":"10.1007/978-3-642-36197-5_375-1","title":"Receiver Functions with Artificial Sources","year":2016,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Computer science; Artificial intelligence","score_opus":0.014296637865348818,"score_gpt":0.17213900122428843,"score_spread":0.1578423633589396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3026949239","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012193843,0.00007570136,0.00011829561,0.00017135654,0.00072852644,0.00013241507,0.00059598684,0.00007267303,0.99688566],"genre_scores_gemma":[0.02189575,0.00003745617,0.00009212515,0.000092507275,0.0010657436,6.8792315e-7,0.00016804105,0.000010112444,0.9766376],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991355,0.000009369446,0.00016017044,0.00028572034,0.00021680548,0.0001924195],"domain_scores_gemma":[0.99949205,0.00005398431,0.00009945653,0.00021625895,0.000046483554,0.000091756025],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00006980852,0.00020879121,0.00023731477,0.000055803608,0.00013722929,0.00007952675,0.00012647088,0.00014346169,0.08898667],"category_scores_gemma":[0.0000020512955,0.000113631235,0.000057578436,0.000012456191,0.00010218167,0.00009178254,0.000008324121,0.000080870595,0.010442234],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00088255963,0.00003923128,0.0029464697,0.00015160044,0.0011688226,0.00018830327,0.000292916,0.00041641222,0.00070421136,0.5815358,0.1351123,0.27656132],"study_design_scores_gemma":[0.00007452732,0.00013138838,0.0006268376,0.00005192295,0.000068779584,0.0000047954645,0.000006471044,0.0000036892957,0.0000727858,0.021171601,0.97747576,0.00031142498],"about_ca_topic_score_codex":0.00031342433,"about_ca_topic_score_gemma":0.0016987069,"teacher_disagreement_score":0.8423635,"about_ca_system_score_codex":0.0000013625524,"about_ca_system_score_gemma":0.00004911123,"threshold_uncertainty_score":0.99032825},"labels":[],"label_agreement":null},{"id":"W3031321457","doi":"10.1111/maps.13494","title":"Shock metamorphism in plagioclase and selective amorphization","year":2020,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Austrian Science Fund; University of Glasgow","keywords":"Plagioclase; Shock metamorphism; Geology; Olivine; Geochemistry; Electron backscatter diffraction; Meteorite; Feldspar; Shock (circulatory); Mineral; Hypervelocity; Mineralogy; Materials science; Quartz; Astrobiology; Microstructure; Composite material; Thermodynamics","score_opus":0.011657846447652378,"score_gpt":0.18730128470887814,"score_spread":0.17564343826122575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3031321457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972211,0.0006132018,0.00007701175,0.00050794095,0.00019339735,0.00015313854,0.00021439829,0.000020851066,0.0009989735],"genre_scores_gemma":[0.9976792,0.00018952339,0.0013734505,0.0005605742,0.00009574711,5.7514296e-7,0.000086366934,0.0000022096933,0.000012370927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988134,0.000052497693,0.00018144827,0.0004016069,0.000255387,0.00029564102],"domain_scores_gemma":[0.9994664,0.00011826303,0.00004262192,0.00008494989,0.00003236075,0.00025539752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039547714,0.0001322341,0.00020536938,0.000094853036,0.00018243644,0.00015458344,0.00016183652,0.000042339212,0.00015821462],"category_scores_gemma":[0.00008940592,0.00011412905,0.000011072638,0.00044068406,0.00027788573,0.00040945603,0.0000262007,0.00010808549,0.000028646182],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024064773,0.00004856601,0.9152647,0.00024499747,0.000050614795,0.00036811913,0.0040242756,0.00709539,0.03619117,0.00833535,0.0008231841,0.027312987],"study_design_scores_gemma":[0.0004977002,0.0003577082,0.9142976,0.000018898325,0.000036070596,0.000035296314,0.00012023321,0.07442856,0.002161921,0.004131781,0.003512364,0.00040187032],"about_ca_topic_score_codex":0.0012911055,"about_ca_topic_score_gemma":0.00039547388,"teacher_disagreement_score":0.06733317,"about_ca_system_score_codex":0.0000017995059,"about_ca_system_score_gemma":0.00005701869,"threshold_uncertainty_score":0.46540475},"labels":[],"label_agreement":null},{"id":"W3032332838","doi":"","title":"Thermal conductivity and Seebeck coefficient of Fe and Fe-Si alloys: Implications for variable Lorenz number","year":2017,"lang":"en","type":"article","venue":"AGUFM","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Wiedemann–Franz law; Seebeck coefficient; Thermal conductivity; Electrical resistivity and conductivity; Condensed matter physics; Materials science; Thermoelectric materials; Thermodynamics; Thermoelectric effect; Physics; Composite material","score_opus":0.025127827167457456,"score_gpt":0.2559585232747105,"score_spread":0.23083069610725307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3032332838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961826,0.00007176854,0.00013509965,0.00025241758,0.00017653935,0.00018080206,0.00038399894,0.000008152125,0.002608579],"genre_scores_gemma":[0.99890846,0.000018324892,0.0006976802,0.000039635586,0.000070369104,0.000002952627,0.000035278536,0.0000023862642,0.00022489908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99955386,0.000016690161,0.000093263785,0.00015475466,0.00004790569,0.00013355182],"domain_scores_gemma":[0.99950385,0.00008226852,0.00009739213,0.00022277032,0.000037903494,0.000055805074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017220738,0.00006786869,0.00013976407,0.000007985467,0.0002702913,0.00009255102,0.00011118179,0.00003696925,0.00009316182],"category_scores_gemma":[0.000031342966,0.000053392996,0.000015816184,0.000015352845,0.00012195278,0.00014565846,0.00002411035,0.000023290515,0.000007857912],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021668339,0.00020506581,0.675198,0.0004170653,0.00024797607,0.0000025584184,0.0012457796,0.0029809868,0.24043821,0.05164301,0.0029545561,0.024450094],"study_design_scores_gemma":[0.0004911677,0.00008006577,0.9711139,0.000016440668,0.00005020458,0.0000040495497,0.000027627791,0.002320883,0.0042291456,0.005186747,0.016308466,0.00017129906],"about_ca_topic_score_codex":0.0047768867,"about_ca_topic_score_gemma":0.00041703397,"teacher_disagreement_score":0.2959159,"about_ca_system_score_codex":5.551516e-7,"about_ca_system_score_gemma":0.00002143712,"threshold_uncertainty_score":0.7221256},"labels":[],"label_agreement":null},{"id":"W3032682931","doi":"10.1029/2019jb019184","title":"Crustal Structure of the Niuafo'ou Microplate and Fonualei Rift and Spreading Center in the Northeastern Lau Basin, Southwestern Pacific","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Bundesministerium für Bildung und Forschung","keywords":"Geology; Crust; Seafloor spreading; Island arc; Rift; Oceanic crust; Seismology; Underplating; Volcano; Accretion (finance); Volcanic arc; Subduction; Back-arc basin; Mantle (geology); Geophysics; Tectonics","score_opus":0.026189131076280372,"score_gpt":0.2701834881361935,"score_spread":0.2439943570599131,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3032682931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99763054,0.00013428314,0.000004612146,0.0015508402,0.00012948559,0.00017546359,0.00021173159,0.0000020201269,0.00016103798],"genre_scores_gemma":[0.9993275,0.00007208083,0.000036290487,0.00012371772,0.0004001965,1.8883188e-7,0.0000043326722,0.000005219717,0.00003046767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978935,0.0004751791,0.00035238167,0.0001833392,0.0007199638,0.00037559654],"domain_scores_gemma":[0.9989959,0.00034153947,0.00017766267,0.00016239769,0.00013578114,0.00018671667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055584783,0.00013716739,0.00034655986,0.000065425316,0.00015393713,0.00019095097,0.00038584904,0.000057146357,0.000064397886],"category_scores_gemma":[0.00010774381,0.00007037497,0.0000832661,0.0002575282,0.0003015823,0.00022699567,0.00008619521,0.0005934827,0.000010300635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001246085,0.00016767802,0.8733538,0.00042638945,0.00018784974,0.00024715945,0.020046555,0.0004905992,0.087482885,0.00029907003,0.0005068543,0.015545089],"study_design_scores_gemma":[0.00076793955,0.0005532721,0.9904464,0.0001281892,0.000020626878,0.000058356458,0.0011682311,0.00078240404,0.0024481334,0.0011179601,0.002384652,0.00012386155],"about_ca_topic_score_codex":0.00076105754,"about_ca_topic_score_gemma":0.0005241457,"teacher_disagreement_score":0.11709259,"about_ca_system_score_codex":0.0000013967541,"about_ca_system_score_gemma":0.00007102786,"threshold_uncertainty_score":0.28698078},"labels":[],"label_agreement":null},{"id":"W3033178958","doi":"10.1103/physrevb.101.224103","title":"Compression behavior of dense <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"><mml:mrow><mml:msub><mml:mi mathvariant=\"normal\">H</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:mtext>−</mml:mtext><mml:mi>He</mml:mi></mml:mrow></mml:math> mixtures up to 160 GPa","year":2020,"lang":"lv","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Argonne National Laboratory; Army Research Office; National Nuclear Security Administration; Deutsches Elektronen-Synchrotron; U.S. Department of Energy; Division of Materials Research; Office of Science; National Science Foundation","keywords":"Crystallography; Physics; Lattice (music); Materials science; Chemistry","score_opus":0.0214558190136383,"score_gpt":0.27483910872731854,"score_spread":0.25338328971368024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033178958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.83578604,0.021141758,0.0006921545,0.0026222153,0.0034081815,0.00026410047,0.0016852939,0.00026161538,0.13413864],"genre_scores_gemma":[0.96367776,0.023774168,0.00083519146,0.0050667054,0.0034806288,0.0008687032,0.0017340934,0.00041299168,0.00014974407],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9889136,0.0009970722,0.0024356705,0.0021688365,0.0030716935,0.0024131555],"domain_scores_gemma":[0.99111867,0.0017382248,0.0024162002,0.0025104827,0.0002557353,0.001960692],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0017796778,0.0011791186,0.0010520344,0.00021702697,0.0012151101,0.0009696626,0.0027982532,0.0010399371,0.21215706],"category_scores_gemma":[0.0018919769,0.0017816713,0.0028358172,0.001579975,0.0012386892,0.0013688076,0.0017335862,0.0016900961,0.008225392],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00092430075,0.0006669195,0.000017121414,0.010168836,0.0010595118,0.0008991966,0.0012750956,0.00044044585,0.013363553,0.4799709,0.47808483,0.013129303],"study_design_scores_gemma":[0.0012167353,0.0025553748,0.00026076328,0.009773176,0.00441638,0.00031231414,0.00023765929,0.014935167,0.9246062,0.0009868834,0.038481817,0.0022175452],"about_ca_topic_score_codex":0.0015534303,"about_ca_topic_score_gemma":0.00036254473,"teacher_disagreement_score":0.9112426,"about_ca_system_score_codex":0.000008433919,"about_ca_system_score_gemma":0.0009923279,"threshold_uncertainty_score":0.99846315},"labels":[],"label_agreement":null},{"id":"W3033654543","doi":"10.1130/ges02213.1","title":"Advances in the thermal and petrologic modeling of subduction zones","year":2020,"lang":"en","type":"article","venue":"Geosphere","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Subduction; Mantle wedge; Mantle (geology); Geophysics; Slab; Crust; Eclogite; Metamorphic rock; Crustal recycling; Oceanic crust; Transition zone; Petrology; Forearc; Thermal; Eclogitization; Seismology; Continental crust; Tectonics","score_opus":0.013393459806774113,"score_gpt":0.19359445711920237,"score_spread":0.18020099731242825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033654543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99518967,0.0020737082,0.00008929367,0.00035797854,0.00006448004,0.00005457255,0.000010513997,0.000007073513,0.0021527044],"genre_scores_gemma":[0.99932677,0.00028518506,0.00018617934,0.00009742108,0.00009088599,5.024351e-7,0.000007625584,8.1237306e-7,0.0000046523164],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996259,0.000040643863,0.000085846026,0.000091139176,0.00007195704,0.000084503255],"domain_scores_gemma":[0.99987334,0.000023951092,0.00002894177,0.000048766018,0.00000813338,0.000016865159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009454955,0.0000451689,0.00008426144,0.000003208967,0.000032335178,0.000015109732,0.000080961036,0.00001944891,0.00033020403],"category_scores_gemma":[0.000008921468,0.000026797039,0.0000119959095,0.000057200767,0.000022749777,0.00012483192,0.0000053632043,0.000036788264,0.000012592534],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022776454,0.000032797045,0.19559462,0.00020050642,0.000012527089,0.00001638465,0.0036719674,0.70269054,0.0014455204,0.0012599048,0.00009706665,0.09475041],"study_design_scores_gemma":[0.00096109713,0.0009548095,0.42322275,0.00004293636,0.000049706992,0.000012767749,0.004225617,0.549547,0.000460673,0.0134311905,0.006631839,0.000459603],"about_ca_topic_score_codex":0.0005769506,"about_ca_topic_score_gemma":0.0004426026,"teacher_disagreement_score":0.22762813,"about_ca_system_score_codex":1.5047905e-7,"about_ca_system_score_gemma":0.0000036404424,"threshold_uncertainty_score":0.36155024},"labels":[],"label_agreement":null},{"id":"W3033953923","doi":"","title":"African cratonic lithosphere carved by mantle plumes","year":2018,"lang":"en","type":"article","venue":"RePEc: Research Papers in Economics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Craton; Lithosphere; Geology; Kimberlite; Archean; Mantle (geology); Mantle plume; Earth science; Geochemistry; Geophysics; Paleontology; Tectonics","score_opus":0.013594415797033866,"score_gpt":0.24947006293270055,"score_spread":0.2358756471356667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033953923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7978521,0.0001216457,5.532195e-7,0.00016347096,0.00029018553,0.00017437364,0.00015528502,0.00002277461,0.2012196],"genre_scores_gemma":[0.99379295,0.00076290587,0.00016286358,0.00005307724,0.00027596398,0.0000061423593,0.000055921402,0.000009435757,0.00488076],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983975,0.00014511631,0.00025101664,0.00040261244,0.00016527757,0.0006384502],"domain_scores_gemma":[0.9991634,0.00017679816,0.000055332952,0.00038063482,0.000052209893,0.00017166336],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00071251055,0.00013205523,0.00023261375,0.00006172098,0.00020417856,0.00014967637,0.00039104902,0.000095569114,0.0039031522],"category_scores_gemma":[0.000063092644,0.00012002315,0.0000453132,0.00013050523,0.00031066232,0.00015768669,0.000050583298,0.0001854836,0.0003613845],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046536783,0.00022642792,0.16467413,0.000119049684,0.00018414846,0.000078531935,0.00190236,0.00080693536,0.0057094283,0.0010176884,0.010622141,0.8141938],"study_design_scores_gemma":[0.0008055293,0.00072160445,0.084721744,0.00004726655,0.000009228538,0.000006379774,0.0009907044,0.0054553086,0.0050078505,0.0025567936,0.8990573,0.00062023033],"about_ca_topic_score_codex":0.0022003313,"about_ca_topic_score_gemma":0.005289783,"teacher_disagreement_score":0.88843524,"about_ca_system_score_codex":0.000021589432,"about_ca_system_score_gemma":0.00013077227,"threshold_uncertainty_score":0.9970074},"labels":[],"label_agreement":null},{"id":"W3034744427","doi":"10.1103/physrevb.101.220103","title":"Fermi surface studies of the low-temperature structure of sodium","year":2020,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Lawrence Livermore National Laboratory; High Magnetic Field Laboratory, Chinese Academy of Sciences; National High Magnetic Field Laboratory; Fusion Energy Sciences; U.S. Department of Energy; National Nuclear Security Administration; Division of Materials Research; Office of Science; National Science Foundation","keywords":"Fermi surface; Condensed matter physics; Materials science; Quantum oscillations; Sodium; Fermi level; Crystallite; Oscillation (cell signaling); Single crystal; Lattice (music); Physics; Nuclear magnetic resonance; Chemistry","score_opus":0.020691702986994912,"score_gpt":0.31793397186885153,"score_spread":0.2972422688818566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034744427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91849494,0.07543961,0.000003893233,0.0039635245,0.00029276244,0.0009804581,0.00055384176,0.000027485261,0.00024347194],"genre_scores_gemma":[0.94197816,0.053664304,0.000042568558,0.003588528,0.0006285049,0.0000035099786,0.000058771035,0.0000145017875,0.000021155147],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9970238,0.00045925533,0.000747422,0.00054257,0.00082291133,0.00040404574],"domain_scores_gemma":[0.99777645,0.00039131555,0.0006103765,0.00069253216,0.00029900193,0.0002303177],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0002074782,0.0004552595,0.0021172399,0.000010182547,0.00011309147,0.000021706264,0.0008926979,0.00004908581,0.00021878403],"category_scores_gemma":[0.0006344688,0.00025012624,0.0007215094,0.0008054018,0.00032751006,0.0001896394,0.00015561726,0.0003958226,0.00013693956],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000104491264,0.00038378118,0.0020101434,0.07135349,0.0006129433,0.000010139104,0.000847779,0.00037508085,0.85868496,0.027904352,0.03037589,0.0073369294],"study_design_scores_gemma":[0.0012885808,0.0012956286,0.028147247,0.041753463,0.0035769185,0.000009055289,0.000093363415,0.0022896817,0.7820864,0.07885705,0.05826266,0.0023399794],"about_ca_topic_score_codex":0.000057753245,"about_ca_topic_score_gemma":0.000014191736,"teacher_disagreement_score":0.076598614,"about_ca_system_score_codex":0.00000478872,"about_ca_system_score_gemma":0.000096990545,"threshold_uncertainty_score":0.9999951},"labels":[],"label_agreement":null},{"id":"W3036514308","doi":"10.1029/2020jb020337","title":"Femtosecond X‐Ray Diffraction of Laser‐Shocked Forsterite (Mg<sub>2</sub>SiO<sub>4</sub>) to 122 GPa","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"SLAC National Accelerator Laboratory; Los Alamos National Laboratory; Lawrence Livermore National Laboratory; Office of Science; Office of the Dean for Research, Princeton University; National Science Foundation; Česká geologická služba; Laboratory Directed Research and Development; Fusion Energy Sciences; U.S. Department of Energy; Princeton University; Deutsche Forschungsgemeinschaft","keywords":"Forsterite; Crystallite; Materials science; Amorphous solid; Laser; Diffraction; Phase (matter); Femtosecond; Silicate perovskite; Crystal (programming language); Periclase; Analytical Chemistry (journal); Electron diffraction; Mineralogy; Crystallography; Optics; Perovskite (structure); Chemistry; Metallurgy; Physics","score_opus":0.036423137982934756,"score_gpt":0.29107846559259726,"score_spread":0.2546553276096625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036514308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99688697,0.00006229036,0.000109905086,0.0013181069,0.0005209338,0.00038418098,0.0002772083,0.000019991117,0.00042039846],"genre_scores_gemma":[0.9972763,0.00022428212,0.00017774545,0.00032636066,0.0018880029,0.000002993506,0.00004413387,0.000021100166,0.000039076822],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99524343,0.00054121367,0.00092706154,0.00044791994,0.0018834522,0.00095692044],"domain_scores_gemma":[0.9966216,0.0006721713,0.0004744677,0.00034885586,0.0007154585,0.001167457],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012603587,0.0003131747,0.0009228736,0.00029263075,0.0002826158,0.00025127278,0.000652107,0.00015108135,0.00031064692],"category_scores_gemma":[0.0006413382,0.0002528721,0.00034374068,0.00082682644,0.00021306724,0.000746587,0.00013599069,0.0009190606,0.00086189527],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012854062,0.00023490372,0.0005910091,0.00015577975,0.00012880417,0.00012730196,0.000564611,0.0015655647,0.96672297,0.00003336261,0.002874349,0.025715923],"study_design_scores_gemma":[0.0019072924,0.0046748114,0.32521254,0.0002250435,0.00006984463,0.000023233013,0.00025659398,0.0027992257,0.6537645,0.0018785096,0.008693698,0.00049474486],"about_ca_topic_score_codex":0.00024181919,"about_ca_topic_score_gemma":0.00019644362,"teacher_disagreement_score":0.32462153,"about_ca_system_score_codex":0.000012983684,"about_ca_system_score_gemma":0.00031484844,"threshold_uncertainty_score":0.9999924},"labels":[],"label_agreement":null},{"id":"W3039447576","doi":"10.1103/physrevb.102.024501","title":"Optical properties of superconducting pressurized <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"><mml:msub><mml:mi>LaH</mml:mi><mml:mn>10</mml:mn></mml:msub></mml:math>","year":2020,"lang":"lv","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada; Compute Canada","keywords":"Superconductivity; London penetration depth; Condensed matter physics; Phonon; Physics; Thermodynamics; Materials science","score_opus":0.03359222466788885,"score_gpt":0.2722589351398665,"score_spread":0.23866671047197763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3039447576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9573203,0.027031656,0.0001003242,0.0024534974,0.00087073346,0.00028115744,0.00043323552,0.00014166176,0.011367461],"genre_scores_gemma":[0.9651908,0.028274009,0.00046324614,0.0023677738,0.0027094528,0.00030081518,0.00046527764,0.00016489222,0.000063682615],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99249667,0.0007327995,0.0017821431,0.0015352434,0.0019276014,0.0015255153],"domain_scores_gemma":[0.99499536,0.0009907786,0.0012394399,0.0014839374,0.00023173777,0.001058761],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001311587,0.00088269403,0.0013342537,0.00006856131,0.00063207705,0.00051971857,0.0016044788,0.00041841986,0.0071513304],"category_scores_gemma":[0.0023336858,0.0009990217,0.0018980067,0.0008569494,0.0010272851,0.0011263575,0.0009887007,0.0011329348,0.0055682715],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041499027,0.0005784344,0.000009979234,0.022117589,0.0008098792,0.00018168756,0.001009673,0.00020351725,0.039164916,0.9042576,0.023744604,0.007507109],"study_design_scores_gemma":[0.0012970425,0.0026686206,0.00011456829,0.020403594,0.005150941,0.00010788477,0.0002731764,0.12316975,0.7907055,0.0042816377,0.049392898,0.0024343727],"about_ca_topic_score_codex":0.0005663472,"about_ca_topic_score_gemma":0.000049634953,"teacher_disagreement_score":0.899976,"about_ca_system_score_codex":0.0000060957664,"about_ca_system_score_gemma":0.00060090085,"threshold_uncertainty_score":0.999246},"labels":[],"label_agreement":null},{"id":"W3040067670","doi":"10.2138/am-2020-7136ccby","title":"Elastic properties of majoritic garnet inclusions in diamonds and the seismic signature of pyroxenites in the Earth's upper mantle","year":2019,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Eclogite; Geology; Peridotite; Mantle (geology); Transition zone; Geochemistry; Olivine; Kimberlite; Seismology; Subduction; Tectonics","score_opus":0.00537737094345759,"score_gpt":0.18608550730271112,"score_spread":0.18070813635925354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040067670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99720615,0.000570574,0.0000016355293,0.0005676368,0.00006681213,0.00023968861,0.000058478614,0.0000033145184,0.0012857215],"genre_scores_gemma":[0.9994256,0.00010285674,0.000043696833,0.00022018113,0.00002660552,0.0000036249987,0.000018931154,0.000002683729,0.00015585736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99914163,0.00019852465,0.00021530771,0.00013422513,0.0001440565,0.00016624371],"domain_scores_gemma":[0.99937683,0.0003047216,0.0001020432,0.00017920908,0.000018662706,0.000018543646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025907066,0.000096656215,0.00028269328,0.000059903996,0.00003321392,0.000019767824,0.00021979945,0.0000258035,0.000101036225],"category_scores_gemma":[0.000054042088,0.000046237292,0.000030459887,0.0002511334,0.0007117892,0.000058892598,0.000033550445,0.00010694441,0.000011429068],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000488476,0.00015095368,0.90002567,0.00028373042,0.000053217813,0.000026053385,0.013338981,0.012966348,0.06464402,0.0035600602,0.00038905634,0.0040734485],"study_design_scores_gemma":[0.00090252934,0.0002698417,0.9871371,0.000098230485,0.000027395916,0.00000811613,0.0026313118,0.0059156506,0.0008471724,0.0011902647,0.0007914815,0.00018090787],"about_ca_topic_score_codex":0.026589204,"about_ca_topic_score_gemma":0.0032639299,"teacher_disagreement_score":0.087111436,"about_ca_system_score_codex":8.196538e-7,"about_ca_system_score_gemma":0.000021522295,"threshold_uncertainty_score":0.97989285},"labels":[],"label_agreement":null},{"id":"W3043268085","doi":"10.1103/physrevlett.125.075702","title":"Liquid-liquid Phase Transitions in Silicon","year":2020,"lang":"en","type":"preprint","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Supercooling; Silicon; Atom (system on chip); Atomic physics; Fermi liquid theory; Covalent bond; Ionization; Phase (matter); Scattering; Density functional theory; Molecular dynamics; Materials science; Molecular physics; Electron; Chemistry; Physics; Computational chemistry; Thermodynamics; Optics; Ion; Nuclear physics; Organic chemistry; Optoelectronics","score_opus":0.028850002112108874,"score_gpt":0.29404822254466473,"score_spread":0.26519822043255586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043268085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9553572,0.005633897,0.00009048643,0.035871033,0.00057148986,0.0009391534,0.0009609206,0.000077857585,0.00049795466],"genre_scores_gemma":[0.9762944,0.0039673923,0.000062112515,0.017626565,0.0008498337,0.000034408924,0.0011501819,0.000012506087,0.0000025814297],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979759,0.00025794117,0.0004567479,0.0006228311,0.00031470956,0.00037185958],"domain_scores_gemma":[0.9991154,0.00008348905,0.00016522987,0.0004099734,0.000021522701,0.0002043565],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00019768134,0.00036026625,0.0009749539,0.00004520529,0.00005080196,0.00006100906,0.00044587324,0.000038670747,0.0007592864],"category_scores_gemma":[0.00003606276,0.00031019218,0.0003394951,0.00020004732,0.000078467,0.00011474022,0.00006130544,0.0005190243,0.00071209646],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027686392,0.002696652,0.00026354386,0.069204316,0.0010504341,0.0015765493,0.0064754193,0.059921578,0.7405498,0.0025628933,0.082506426,0.030423721],"study_design_scores_gemma":[0.012212257,0.009608455,0.015561429,0.07696357,0.006349066,0.000039519953,0.00012701064,0.05925507,0.023659514,0.01034431,0.7690881,0.016791727],"about_ca_topic_score_codex":0.0005183049,"about_ca_topic_score_gemma":0.00007455143,"teacher_disagreement_score":0.71689034,"about_ca_system_score_codex":0.000006631102,"about_ca_system_score_gemma":0.00006400984,"threshold_uncertainty_score":0.99993503},"labels":[],"label_agreement":null},{"id":"W3043602218","doi":"","title":"Lithospheric Thickness and Thermal Regime in the Canadian Shield: Constraints from Heat Flux and S wave Travel Time Delays","year":2009,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shield; Lithosphere; Heat flux; Geology; Thermal; Flux (metallurgy); Geophysics; High heat; Seismology; Geodesy; Mechanics; Meteorology; Heat transfer; Petrology; Physics; Materials science","score_opus":0.010858212293591175,"score_gpt":0.18831593331030028,"score_spread":0.1774577210167091,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043602218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9781854,0.00032793835,9.734204e-7,0.00067860354,0.00010435488,0.00013312841,0.00003434549,0.000016109203,0.02051916],"genre_scores_gemma":[0.9987829,0.000018865197,0.0005549313,0.0004493346,0.00013403992,5.9613063e-7,0.000022225944,0.000003750457,0.000033388733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989312,0.00008332967,0.00020890287,0.0002609281,0.00015488909,0.0003607082],"domain_scores_gemma":[0.9993737,0.00024470227,0.000053097297,0.00015412252,0.000014276714,0.00016015356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000655067,0.00014983084,0.0001883038,0.000030974807,0.0002324445,0.00023935725,0.00013787091,0.00010574513,0.00012887026],"category_scores_gemma":[0.00005635397,0.00011177177,0.000018586994,0.00007247294,0.000098767254,0.000125733,0.0000073008964,0.00018498191,0.000042807314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026605104,0.00017622487,0.50284755,0.00018055302,0.00023256989,0.0031066588,0.040848073,0.02411835,0.11942092,0.0012665495,0.00065842835,0.30687806],"study_design_scores_gemma":[0.00017114557,0.00003342604,0.9974368,0.00007580283,0.000014626031,0.0000171095,0.0001514361,0.00077736616,0.00053130294,0.0004232626,0.00021163994,0.00015604253],"about_ca_topic_score_codex":0.52856946,"about_ca_topic_score_gemma":0.19549167,"teacher_disagreement_score":0.4945893,"about_ca_system_score_codex":0.000004017383,"about_ca_system_score_gemma":0.00006699867,"threshold_uncertainty_score":0.81918854},"labels":[],"label_agreement":null},{"id":"W3045809065","doi":"10.1002/jrs.5954","title":"Raman and infrared spectra to monitor the phase transition of natural kyanite under static compression","year":2020,"lang":"en","type":"article","venue":"Journal of Raman Spectroscopy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Key Research and Development Program of China; China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Kyanite; Raman spectroscopy; Phase transition; Bulk modulus; Natural bond orbital; Chemistry; Mineralogy; Analytical Chemistry (journal); Crystallography; Geology; Materials science; Condensed matter physics; Density functional theory; Computational chemistry; Composite material; Metamorphic rock; Optics; Geochemistry; Organic chemistry; Physics","score_opus":0.011164141169758224,"score_gpt":0.2535957076136146,"score_spread":0.24243156644385638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3045809065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99391544,0.00036133922,0.002258213,0.0027453066,0.00037243968,0.00015864156,0.0000650041,0.00000739284,0.00011622458],"genre_scores_gemma":[0.996066,0.00007122054,0.0027910536,0.00060716836,0.00043823602,2.0217489e-7,0.000010332414,0.0000043748914,0.000011443477],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989895,0.00009583545,0.000347647,0.00010794526,0.0002935071,0.00016552932],"domain_scores_gemma":[0.99936336,0.0000840808,0.0002426,0.00008707516,0.000059808663,0.00016309155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001854918,0.00011553615,0.00028421843,0.000051970495,0.00008850067,0.00009704823,0.00017948922,0.000029103672,0.0003242806],"category_scores_gemma":[0.000016158723,0.000070906404,0.000062032625,0.00013527238,0.000054378983,0.00020746331,0.000008664285,0.00017651278,0.000010621923],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018872072,0.0000855723,0.0005979175,0.00010188397,0.00012196416,0.000044807017,0.005256498,0.0034610718,0.98182595,0.00021326913,0.0044294894,0.0019743538],"study_design_scores_gemma":[0.009853262,0.010767456,0.16738456,0.0004993526,0.00053241185,0.00015556863,0.0041716457,0.016326116,0.768094,0.013931861,0.0074184015,0.00086534984],"about_ca_topic_score_codex":0.00006166543,"about_ca_topic_score_gemma":0.000014280457,"teacher_disagreement_score":0.21373194,"about_ca_system_score_codex":0.0000034405964,"about_ca_system_score_gemma":0.000027023843,"threshold_uncertainty_score":0.35506454},"labels":[],"label_agreement":null},{"id":"W3046235897","doi":"10.1029/2020gl090192","title":"Electrical Conductivity of Aqueous Magnesium Sulfate at High Pressure and Low Temperature With Application to Ganymede's Subsurface Ocean","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Aqueous solution; Magnesium; Conductivity; Conductance; Limiting; Analytical Chemistry (journal); Sulfate; Materials science; Mineralogy; Geology; Chemistry; Condensed matter physics; Physics; Environmental chemistry; Metallurgy; Physical chemistry","score_opus":0.0116349499030121,"score_gpt":0.2334152658545616,"score_spread":0.2217803159515495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046235897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896388,0.000079528385,0.000044497127,0.009285349,0.00004016917,0.00060801615,0.0002150945,0.000036107853,0.000052456613],"genre_scores_gemma":[0.9988018,0.0000065124873,0.00019192368,0.0005212737,0.00028277066,0.000006341335,0.00008855331,0.000011187799,0.000089637135],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9975448,0.0002756652,0.00017869298,0.00059565465,0.0008112703,0.0005938792],"domain_scores_gemma":[0.99878395,0.00027424967,0.000058408776,0.00028322617,0.00014362404,0.00045653927],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002710385,0.00019530747,0.00035773928,0.000056524965,0.00022754908,0.00009612892,0.00031010364,0.00008056759,0.000119138684],"category_scores_gemma":[0.00007167741,0.00014555591,0.00003688474,0.0005946438,0.00026527137,0.00016969207,0.00008433347,0.00034636378,0.0001434935],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00088692957,0.000048819154,0.003294445,0.00019396948,0.00004486427,0.000039261966,0.00025813715,0.0018375727,0.9882209,0.00019930085,0.0039577875,0.0010180713],"study_design_scores_gemma":[0.0016870826,0.0029422108,0.5341301,0.000054592318,0.00013214155,0.000016469414,0.000055723427,0.0064852303,0.4427523,0.0005045867,0.010239897,0.000999646],"about_ca_topic_score_codex":0.0029933292,"about_ca_topic_score_gemma":0.00014644608,"teacher_disagreement_score":0.5454685,"about_ca_system_score_codex":0.0000057244733,"about_ca_system_score_gemma":0.00004614845,"threshold_uncertainty_score":0.5935598},"labels":[],"label_agreement":null},{"id":"W3047501190","doi":"10.1038/s41586-020-2535-y","title":"A measurement of the equation of state of carbon envelopes of white dwarfs","year":2020,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":119,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"Laboratory Directed Research and Development; Fusion Energy Sciences; National Nuclear Security Administration; Office of Science; U.S. Department of Energy","keywords":"White dwarf; Equation of state; Physics; Astrophysics; Shock (circulatory); Stellar evolution; Stars; Thermodynamics","score_opus":0.01678685672086102,"score_gpt":0.19698062722863185,"score_spread":0.18019377050777083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047501190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977933,0.0006227115,0.000011077814,0.00031853767,0.00017145977,0.00011520851,0.0001825922,0.0000025777988,0.0007824966],"genre_scores_gemma":[0.9997931,0.000017524,0.00010147264,0.000044987453,0.000024156641,1.8048287e-7,0.000007360302,0.0000012581306,0.000009940713],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992268,0.000051980584,0.000197312,0.00007212599,0.00039196073,0.000059783757],"domain_scores_gemma":[0.99949247,0.000015867397,0.00022589814,0.000101199694,0.00014504435,0.000019519059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021305023,0.000050014154,0.00016609716,0.000014372722,0.000013013335,0.0000018307289,0.00014571166,0.00008571559,0.000060388084],"category_scores_gemma":[0.00006274309,0.000030935542,0.00003771992,0.00013693876,0.000032916458,0.000026607946,0.000015836675,0.00011719587,5.424991e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034116494,0.000058691538,0.15619959,0.001269793,0.00018560213,8.9312744e-7,0.0072962604,0.013422366,0.81041646,0.00033132615,0.00052338804,0.009954485],"study_design_scores_gemma":[0.00022871594,0.00013771198,0.4195402,0.00008967522,0.000038735372,9.912343e-8,0.000041868032,0.0007750416,0.57751375,0.0005561603,0.0010129481,0.000065073116],"about_ca_topic_score_codex":0.000492102,"about_ca_topic_score_gemma":0.00019480345,"teacher_disagreement_score":0.2633406,"about_ca_system_score_codex":7.2587886e-7,"about_ca_system_score_gemma":0.000051083858,"threshold_uncertainty_score":0.12615147},"labels":[],"label_agreement":null},{"id":"W3048691860","doi":"10.1073/pnas.2004269117","title":"Evidence for complex iron oxides in the deep mantle from FeNi(Cu) inclusions in superdeep diamond","year":2020,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca; Deutsche Forschungsgemeinschaft; FP7 Ideas: European Research Council; Alfred P. Sloan Foundation","keywords":"Diamond; Geology; Mantle (geology); Geochemistry; Materials science; Metallurgy","score_opus":0.11302128164812046,"score_gpt":0.3057269921046806,"score_spread":0.1927057104565601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048691860","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879227,0.00027799935,0.0000019038245,0.010609755,0.000021263773,0.000278174,0.00009261356,0.000003805838,0.0007917396],"genre_scores_gemma":[0.9977276,0.00005027773,0.0012366523,0.00087204477,0.00010107679,0.000005015227,0.0000016047942,0.0000011570272,0.00000460739],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99868315,0.000017302753,0.00027917803,0.0002105783,0.0006574586,0.0001523432],"domain_scores_gemma":[0.9990411,0.00070009887,0.00016280929,0.000008774253,0.00005789814,0.000029353449],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010841776,0.00007617149,0.00015429218,0.000057479385,0.0001723481,0.00004667842,0.0010289343,0.00004405542,0.000095214],"category_scores_gemma":[0.00062211615,0.000042823944,0.000042143343,0.0005025944,0.00032742647,0.00044016854,0.000075727934,0.000090480054,0.0000036585614],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018428032,0.00008431764,0.3500711,0.000240614,0.000015311212,8.8492975e-8,0.010108246,0.0053743785,0.6115714,0.017951746,0.0019087798,0.00248976],"study_design_scores_gemma":[0.00017692517,0.000059518676,0.91606414,0.00008842748,0.000008798439,5.3262426e-7,0.0008167076,0.01615273,0.013205831,0.053039934,0.000302029,0.000084442814],"about_ca_topic_score_codex":0.0005520973,"about_ca_topic_score_gemma":0.000045841887,"teacher_disagreement_score":0.59836555,"about_ca_system_score_codex":0.0000033156734,"about_ca_system_score_gemma":0.000020946954,"threshold_uncertainty_score":0.1912033},"labels":[],"label_agreement":null},{"id":"W3051391864","doi":"10.1063/5.0025557","title":"Composite pressure cell for pulsed magnets","year":2021,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Los Alamos National Laboratory; High Magnetic Field Laboratory, Chinese Academy of Sciences; Division of Materials Research; National High Magnetic Field Laboratory; National Science Foundation","keywords":"Materials science; Eddy current; Magnet; Magnetic field; Diamond anvil cell; Magnetic pressure; Composite material; Nuclear magnetic resonance; Mechanics; High pressure; Mechanical engineering; Magnetization; Electrical engineering; Physics","score_opus":0.012970341128845108,"score_gpt":0.22893006824639292,"score_spread":0.21595972711754782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3051391864","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9271053,0.039426126,0.00003273217,0.00033100107,0.0057618916,0.0013971205,0.0028060563,0.000035731322,0.023104016],"genre_scores_gemma":[0.9890078,0.0025707611,0.0017654652,0.00023630135,0.00007067451,0.000005738525,0.001121477,0.0000045809443,0.0052172025],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986524,0.00007159368,0.00035877785,0.0003330866,0.00033474877,0.00024937032],"domain_scores_gemma":[0.9991698,0.000030510026,0.0001803597,0.00033802752,0.00019486285,0.00008641441],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004675323,0.00011643886,0.00032293136,0.0000329934,0.0001472441,0.00011486761,0.000255803,0.000034945613,0.0030986152],"category_scores_gemma":[0.000026799085,0.0000958957,0.00011574258,0.00024823076,0.000077831304,0.00016110986,0.000028078082,0.000035213252,0.00015227312],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005606687,0.00051143294,0.009379416,0.048039116,0.00017893831,0.000013956878,0.0001688008,0.0000475329,0.3751006,0.0003720399,0.035360068,0.53077203],"study_design_scores_gemma":[0.00071008323,0.00012227945,0.010183446,0.0030658813,0.0002616357,0.000008091148,0.0000149021735,0.0005947613,0.25098923,0.0006045354,0.7331185,0.00032666427],"about_ca_topic_score_codex":0.0000339102,"about_ca_topic_score_gemma":0.000013513409,"teacher_disagreement_score":0.69775844,"about_ca_system_score_codex":0.0000015323543,"about_ca_system_score_gemma":0.000069026995,"threshold_uncertainty_score":0.9978127},"labels":[],"label_agreement":null},{"id":"W3083420293","doi":"10.5194/egusphere-egu2020-2032","title":"Slab Remnant Recycling and Mantle-Wide Convection: A Separation of Time Scales","year":2020,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Mantle (geology); Mantle convection; Geology; Slab; Mantle wedge; Geophysics; Convection; Mechanics; Subduction; Physics; Tectonics; Seismology","score_opus":0.013235264621257002,"score_gpt":0.21362781555500818,"score_spread":0.20039255093375116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3083420293","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987465,0.00012000355,0.00031360242,0.00085052947,0.00012477729,0.000091223475,0.000032132455,0.000029493363,0.010973202],"genre_scores_gemma":[0.9987014,0.000053705364,0.0005434258,0.00020053326,0.00009663429,2.2110291e-7,0.00003064041,0.0000012711513,0.00037215897],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99956626,0.000027614076,0.00013313953,0.00011899886,0.000078538134,0.000075436634],"domain_scores_gemma":[0.99977446,0.00005637705,0.000047728863,0.00004808458,0.000018518393,0.000054828695],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000092138274,0.000051585248,0.000120568155,0.000011606751,0.000043805776,0.000027666034,0.00003910132,0.00002604929,0.0018943136],"category_scores_gemma":[0.000019924253,0.000038871953,0.000015366892,0.000056293833,0.000027437618,0.00010341886,0.000006568994,0.000021653783,0.00019778174],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012120719,0.00007226862,0.34238702,0.0008074577,0.00028264552,0.000051580417,0.004261102,0.0056609274,0.5225604,0.0032478957,0.036548108,0.08290852],"study_design_scores_gemma":[0.0014292322,0.001036134,0.6235762,0.000075570715,0.00011279368,0.0000194827,0.00026489855,0.10452497,0.19401884,0.004251973,0.069907986,0.00078189466],"about_ca_topic_score_codex":0.0004493827,"about_ca_topic_score_gemma":0.00011963617,"teacher_disagreement_score":0.32854158,"about_ca_system_score_codex":2.8424228e-7,"about_ca_system_score_gemma":0.000008233206,"threshold_uncertainty_score":0.9990181},"labels":[],"label_agreement":null},{"id":"W3083477867","doi":"10.5194/egusphere-egu2020-5010","title":"Global and regional waveform tomography with massive datasets: new insights into the structure and evolution of the continents","year":2020,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Lithosphere; Archean; Geology; Craton; Seismic tomography; Mantle (geology); Crust; Seismology; Tectonics; Volcanism; Geophysics; Mantle plume; Intraplate earthquake; Earth science; Paleontology","score_opus":0.005685206364617544,"score_gpt":0.1762635531577658,"score_spread":0.17057834679314823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3083477867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99643064,0.0004607007,0.000053762655,0.002259229,0.00006260596,0.00013322795,0.00040755488,0.000005087287,0.00018721822],"genre_scores_gemma":[0.9992723,0.000022708184,0.00016295764,0.00036211906,0.000065505636,1.0207386e-7,0.00010311369,7.2917686e-7,0.000010481659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995626,0.00002431766,0.000077952805,0.00012282225,0.00014016498,0.00007213472],"domain_scores_gemma":[0.99974924,0.000016450158,0.00005758889,0.00009622414,0.00001572922,0.000064785476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000020935673,0.00007035858,0.00008685167,0.0000061960864,0.000095980206,0.000036122314,0.000116740586,0.000024128629,0.000080776765],"category_scores_gemma":[0.0000049787786,0.000027508071,0.000011868495,0.00013126378,0.00012324091,0.00011477763,0.000026876085,0.000029101348,8.854548e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046906222,0.000011072188,0.9432062,0.00009633972,0.00020729039,0.0000047869826,0.003335308,0.0004079408,0.0016661929,0.016447565,0.02730284,0.006845429],"study_design_scores_gemma":[0.00034148747,0.00010402543,0.978752,0.000013181877,0.00003386373,0.000003584188,0.00021554892,0.00044982074,0.00030871318,0.0081926305,0.0115085635,0.0000765608],"about_ca_topic_score_codex":0.0067561027,"about_ca_topic_score_gemma":0.0052642254,"teacher_disagreement_score":0.03554585,"about_ca_system_score_codex":7.7641573e-7,"about_ca_system_score_gemma":0.000029640405,"threshold_uncertainty_score":0.999858},"labels":[],"label_agreement":null},{"id":"W3084103887","doi":"10.1038/s41586-020-2677-y","title":"Evidence for supercritical behaviour of high-pressure liquid hydrogen","year":2020,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":171,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trinity College","funders":"Engineering and Physical Sciences Research Council","keywords":"Supercritical fluid; Phase diagram; Liquid hydrogen; Gas giant; Metallic hydrogen; Phase transition; Hydrogen; Chemical physics; Liquid water; Materials science; Planet; Phase (matter); Physics; Thermodynamics; Astrophysics","score_opus":0.027941421175464744,"score_gpt":0.26531501225350634,"score_spread":0.2373735910780416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084103887","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915291,0.003289281,0.000040368413,0.003196137,0.00039418542,0.00025151126,0.0011353471,0.000035086305,0.00012899456],"genre_scores_gemma":[0.9975294,0.00004239506,0.0007547776,0.0010241333,0.00049269875,0.000002464688,0.00011661025,0.0000050752737,0.00003244924],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990699,0.000041006584,0.00017598525,0.0002553395,0.00024045278,0.00021731351],"domain_scores_gemma":[0.9993971,0.00018817947,0.000021562586,0.00015596804,0.00009415517,0.00014305515],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013717244,0.00011483416,0.0002447457,0.000017028182,0.00005699754,0.000026090844,0.00030750487,0.00047662287,0.0011205992],"category_scores_gemma":[0.00025497694,0.00009254617,0.000079924255,0.00010020379,0.00004694626,0.00017548628,0.0000206391,0.0003683742,0.00004385484],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008732326,0.0003101155,0.14161222,0.0037329365,0.00071544613,0.00016675737,0.0033854218,0.005718415,0.7025965,0.027187591,0.09987906,0.005963216],"study_design_scores_gemma":[0.0018435383,0.0037236114,0.17741273,0.00035976517,0.00086280174,0.000014343643,0.0001628243,0.002081946,0.74290276,0.0036317909,0.065837145,0.0011667189],"about_ca_topic_score_codex":0.000321547,"about_ca_topic_score_gemma":0.00004798914,"teacher_disagreement_score":0.040306292,"about_ca_system_score_codex":6.1803945e-7,"about_ca_system_score_gemma":0.000040569415,"threshold_uncertainty_score":0.9997925},"labels":[],"label_agreement":null},{"id":"W3087086193","doi":"10.1038/s41586-020-2697-7","title":"Slow compression of crystalline ice at low temperature","year":2020,"lang":"en","type":"letter","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Compression (physics); Materials science; Geology; Composite material","score_opus":0.0061149338891757984,"score_gpt":0.19983245583373385,"score_spread":0.19371752194455805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087086193","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17492388,0.013177414,0.0000037987647,0.7778256,0.008895018,0.0011766221,0.01758974,0.0002660068,0.0061419033],"genre_scores_gemma":[0.35004538,0.000213537,0.00031686647,0.6195873,0.010402575,0.0000018570485,0.013748862,0.000030519204,0.0056530987],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982046,0.00011576283,0.00028851037,0.00046882333,0.00060709775,0.00031524504],"domain_scores_gemma":[0.9990795,0.000098203454,0.00026069992,0.00037134034,0.00010297852,0.000087269436],"candidate_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"consensus_categories":["research_integrity"],"category_scores_codex":[0.000069543195,0.0003413425,0.00059592584,0.000055922046,0.000115701434,0.00006443205,0.0005435654,0.0036637639,0.0026268943],"category_scores_gemma":[0.000030674113,0.00024636887,0.00015300735,0.00016890204,0.00006344772,0.000086827706,0.000058175854,0.004613105,0.00020209636],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007382857,0.0000054667366,0.000098972436,0.0005657021,0.000043922886,0.00024642766,0.000040799565,0.00011108934,0.014283124,0.000002875165,0.98439556,0.00013221298],"study_design_scores_gemma":[0.00020398793,0.000085528525,0.00117975,0.00024134862,0.000053482105,0.0000076722645,0.0000031313239,0.00006406991,0.0043360232,0.00014550527,0.99337363,0.00030584494],"about_ca_topic_score_codex":0.00013647627,"about_ca_topic_score_gemma":0.000045424196,"teacher_disagreement_score":0.1751215,"about_ca_system_score_codex":0.000003754678,"about_ca_system_score_gemma":0.000054617587,"threshold_uncertainty_score":0.99999887},"labels":[],"label_agreement":null},{"id":"W3087875723","doi":"10.5194/egusphere-egu2020-5380","title":"Thermochemical structure of cratons from Rayleigh wave phase velocities","year":2020,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Lithosphere; Archean; Craton; Geology; Proterozoic; Precambrian; Rift; Subduction; Mantle (geology); Kimberlite; Metasomatism; Mantle plume; Indian Shield; Geophysics; Petrology; Geochemistry; Tectonics; Seismology","score_opus":0.01933860446835513,"score_gpt":0.20692112485653777,"score_spread":0.18758252038818263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087875723","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99484706,0.0000827092,0.00006722552,0.0002977538,0.00014020484,0.000057695375,0.0011021084,0.000026433267,0.003378786],"genre_scores_gemma":[0.998186,0.0000063015723,0.00083734415,0.0003718995,0.00024170618,1.0687586e-7,0.00032083946,0.0000021824756,0.000033647677],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99944615,0.000023526316,0.00014120474,0.00014373877,0.00012745717,0.000117910575],"domain_scores_gemma":[0.99968946,0.000057825142,0.000044555283,0.000094973526,0.000020332305,0.00009286702],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000016405875,0.000086398606,0.00018002576,0.000007819665,0.000033419514,0.000025148125,0.000116908544,0.000049458486,0.024889138],"category_scores_gemma":[0.000013588732,0.000060143797,0.00003580353,0.0000542165,0.00005878607,0.00006568486,0.000011368898,0.000048794194,0.000051797433],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012105325,0.000015526102,0.0013870517,0.000023387911,0.00006309633,0.000009878882,0.0012261305,0.000057770234,0.98852,0.0005601895,0.0039222487,0.0040936135],"study_design_scores_gemma":[0.0007225677,0.00014277853,0.008369376,0.0000072108965,0.000035662604,7.39183e-7,0.00023050046,0.0015824308,0.97757167,0.0066282023,0.0045114546,0.00019742202],"about_ca_topic_score_codex":0.0011602195,"about_ca_topic_score_gemma":0.00007285793,"teacher_disagreement_score":0.02483734,"about_ca_system_score_codex":3.3524145e-7,"about_ca_system_score_gemma":0.000022608428,"threshold_uncertainty_score":0.9760023},"labels":[],"label_agreement":null},{"id":"W3087952801","doi":"10.1002/anie.202009897","title":"The Relative Thermodynamic Stability of Diamond and Graphite","year":2020,"lang":"en","type":"article","venue":"Angewandte Chemie International Edition","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Diamond; Graphite; Thermodynamics; Chemical stability; Density functional theory; Degenerate energy levels; Chemistry; Entropy (arrow of time); Materials science; Computational chemistry; Physics; Organic chemistry","score_opus":0.013226060360007032,"score_gpt":0.20885780993592723,"score_spread":0.1956317495759202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087952801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990023,0.00016577181,0.00043902316,0.002357533,0.0005435153,0.0000867079,0.00048696614,0.000014497739,0.0058829705],"genre_scores_gemma":[0.999196,0.00014149818,0.00004310222,0.00009137943,0.00030775092,0.0000014032313,0.00020128758,0.0000015061128,0.000016070468],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99951875,0.000019444877,0.0001243947,0.00011380229,0.00015699441,0.00006663775],"domain_scores_gemma":[0.9996203,0.00014134272,0.00008297815,0.00005328592,0.0000628209,0.000039279177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011262862,0.00005541773,0.00006966716,0.0000097825305,0.000063631225,0.000027084134,0.00010211199,0.000026100963,0.0003858029],"category_scores_gemma":[0.00006735723,0.00003737,0.000029399436,0.00004829018,0.00010325949,0.00018273585,0.0000126465575,0.00004830564,0.000008732384],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007488328,0.00007274065,0.12541476,0.00013027033,0.0004781061,0.000010116837,0.0048792046,0.00009581031,0.8327544,0.015192615,0.0053228964,0.0149003025],"study_design_scores_gemma":[0.00042868537,0.00011889043,0.30367744,0.00002379013,0.000032314314,0.0000019856188,0.00018587493,0.0017371536,0.6483192,0.033712376,0.011592638,0.0001696769],"about_ca_topic_score_codex":0.00017855977,"about_ca_topic_score_gemma":0.0000721649,"teacher_disagreement_score":0.18443517,"about_ca_system_score_codex":0.0000016810362,"about_ca_system_score_gemma":0.000009393629,"threshold_uncertainty_score":0.42242712},"labels":[],"label_agreement":null},{"id":"W3088005478","doi":"10.1038/s41467-020-18660-w","title":"Structural dynamics of basaltic melt at mantle conditions with implications for magma oceans and superplumes","year":2020,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Canada; Western Canada Research Grid; National Research Council Canada; National Natural Science Foundation of China; Compute Canada; Ministry of Education, Culture, Sports, Science and Technology; University of Saskatchewan","keywords":"Mantle (geology); Thermal diffusivity; Basalt; Viscosity; Geology; Magma; Geophysics; Chemical physics; Materials science; Geochemistry; Thermodynamics; Chemistry; Volcano; Physics","score_opus":0.01603435254451175,"score_gpt":0.25257149787970257,"score_spread":0.23653714533519082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088005478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95928913,0.0016579631,0.00014474576,0.02633819,0.00008264305,0.0005821019,0.010421494,0.000052882264,0.0014308452],"genre_scores_gemma":[0.99184275,0.00016687509,0.004641589,0.00029505396,0.000027264963,0.000008395227,0.0029745076,0.0000050804415,0.0000384664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994939,0.00003864937,0.0001475824,0.00013868786,0.00006384903,0.00011732945],"domain_scores_gemma":[0.99897844,0.0002701162,0.000078207755,0.0004814199,0.0001083183,0.00008347396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000048871745,0.000088196364,0.00014881426,0.00002559824,0.00034888173,0.00002951544,0.0004046781,0.00007931339,0.00012419069],"category_scores_gemma":[0.00003704315,0.000070305745,0.00003029709,0.00013412784,0.00018188637,0.00010724916,0.00005475946,0.00013000613,0.000005503006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001729115,0.00007523784,0.5978111,0.00029429828,0.00035275356,8.892316e-7,0.002283518,0.00084304065,0.007845915,0.3719998,0.012234763,0.0060857935],"study_design_scores_gemma":[0.000382519,0.00012580214,0.97171336,0.000013459381,0.00011289741,0.000008083355,0.00017849004,0.013001823,0.00020425451,0.003995682,0.010080663,0.00018293348],"about_ca_topic_score_codex":0.00011929438,"about_ca_topic_score_gemma":0.0066182483,"teacher_disagreement_score":0.3739023,"about_ca_system_score_codex":0.0000036006413,"about_ca_system_score_gemma":0.000033162072,"threshold_uncertainty_score":0.3693138},"labels":[],"label_agreement":null},{"id":"W3088110248","doi":"10.1111/maps.13572","title":"Ordinary chondrite shock stage quantification using in situ 2‐D X‐ray diffraction of olivine","year":2020,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Shock metamorphism; Petrography; Olivine; Chondrite; Geology; Shock (circulatory); Mosaicity; Full width at half maximum; Mineralogy; Diffraction; Meteorite; X-ray crystallography; Physics; Optics; Astronomy","score_opus":0.03287986327875412,"score_gpt":0.24204724786245296,"score_spread":0.20916738458369885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088110248","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99804443,0.00032042156,0.00031354348,0.00013365844,0.00036418758,0.00012619846,0.00025254095,0.000012366497,0.00043266785],"genre_scores_gemma":[0.9966851,0.000121954625,0.0028785774,0.0000931071,0.00008642627,2.2054809e-7,0.0001126196,0.0000021901753,0.000019806834],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99879706,0.000056589164,0.00027367257,0.00032290677,0.00030038346,0.00024939288],"domain_scores_gemma":[0.99946225,0.00011002283,0.000100089834,0.00013842947,0.000042067804,0.00014715875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045967483,0.000113921276,0.00021846913,0.00010869381,0.00013165602,0.00007787596,0.00020342585,0.00004126169,0.00019524983],"category_scores_gemma":[0.00006749319,0.000101382175,0.000017956992,0.0004514569,0.0002057752,0.00047382398,0.000021572812,0.000094477895,0.000015700718],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010310233,0.000038597515,0.16809322,0.00023649973,0.000011129087,0.00004068539,0.0006471742,0.026478875,0.7973479,0.00052166404,0.000034117587,0.0064470433],"study_design_scores_gemma":[0.00022612492,0.00020897678,0.8479161,0.000033589462,0.000019623312,0.000006827003,0.0001302712,0.14370124,0.005431855,0.00019014862,0.0019185552,0.00021669477],"about_ca_topic_score_codex":0.00272183,"about_ca_topic_score_gemma":0.0003692319,"teacher_disagreement_score":0.791916,"about_ca_system_score_codex":0.0000025609763,"about_ca_system_score_gemma":0.000062070496,"threshold_uncertainty_score":0.4134245},"labels":[],"label_agreement":null},{"id":"W3088168140","doi":"10.48550/arxiv.1704.05541","title":"On commutativity and near commutativity of translational and rotational averages: Analytical proofs and numerical examinations","year":2017,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Anisotropy; Commutative property; Elasticity (physics); Mathematical proof; Commutator; Perturbation (astronomy); Mathematics; Translational symmetry; Physics; Mathematical analysis; Mathematical physics; Pure mathematics; Geometry; Quantum mechanics; Algebra over a field","score_opus":0.06023871934605729,"score_gpt":0.20703245934985282,"score_spread":0.14679374000379553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088168140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99339867,0.000052615964,0.004316068,0.0001259659,0.00006590784,0.00021662386,0.000809273,0.000013137536,0.0010017683],"genre_scores_gemma":[0.99932146,0.000054082902,0.00032257725,0.000015351632,0.00001988218,2.7067657e-7,0.00019485285,0.0000034796249,0.000068042056],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904,0.00020744599,0.00013635991,0.00038234468,0.00010162734,0.00013219698],"domain_scores_gemma":[0.9988026,0.00061730086,0.00017500568,0.0002195804,0.00006755886,0.00011793088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026321938,0.0001709942,0.00031918177,0.000067705274,0.00034045096,0.00011241937,0.00015736466,0.00012271453,0.00011915604],"category_scores_gemma":[0.000057895413,0.00017086978,0.000040464292,0.000054848715,0.0005343676,0.00018665443,0.000088073495,0.00023157976,0.0000043036835],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005683876,0.00036948483,0.63553494,0.0007710643,0.0005322,0.00014706486,0.0024621852,0.19595355,0.00006351519,0.15074587,0.00013408082,0.012717685],"study_design_scores_gemma":[0.0003634108,0.000086567554,0.6777708,0.00004416607,0.00007830214,0.000002662099,0.00002025405,0.26746252,0.000013828647,0.05394537,0.000049671722,0.00016249111],"about_ca_topic_score_codex":0.0010731205,"about_ca_topic_score_gemma":0.00022697747,"teacher_disagreement_score":0.09680049,"about_ca_system_score_codex":0.0000034401342,"about_ca_system_score_gemma":0.00007984493,"threshold_uncertainty_score":0.69678676},"labels":[],"label_agreement":null},{"id":"W3088204411","doi":"10.5194/egusphere-egu2020-10638","title":"Mobile or not mobile: exploring the linkage between deep mantle composition and early Earth surface mobility","year":2020,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Mantle convection; Mantle (geology); Geology; Geophysics; Plate tectonics; Convection; Planetary differentiation; Earth's internal heat budget; Mantle wedge; Ocean surface topography; Tectonics; Petrology; Mechanics; Lithosphere; Physics; Geodesy; Paleontology","score_opus":0.040096719100456354,"score_gpt":0.2270407347583492,"score_spread":0.18694401565789287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088204411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806994,0.00012023257,0.00022875641,0.00011422051,0.00016897779,0.0004914149,0.00015280503,0.00007681356,0.0005768193],"genre_scores_gemma":[0.99879324,0.00007267512,0.0005002724,0.00017404876,0.0002574463,0.000010477203,0.000045877976,0.000004986844,0.00014100022],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989443,0.000109065055,0.00021628328,0.0002971606,0.00019451894,0.00023868862],"domain_scores_gemma":[0.9993621,0.00021106003,0.000052961455,0.00018909194,0.00002706963,0.00015768898],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024687155,0.00014151177,0.000230249,0.000010172353,0.00022318594,0.00017007126,0.00018784494,0.000042899443,0.001165969],"category_scores_gemma":[0.000007935685,0.00008345517,0.00003738446,0.00012320248,0.00007682102,0.0003094963,0.000034345783,0.00011158208,0.0002457553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015902827,0.00021506626,0.6841049,0.0009017302,0.00044942187,0.000116176074,0.028455932,0.04903928,0.08857517,0.0004375712,0.0010477522,0.14506672],"study_design_scores_gemma":[0.00052207056,0.0010890686,0.93658024,0.000020578647,0.00007451626,0.0000032139417,0.00065491424,0.0039422065,0.039985806,0.000095161,0.016592495,0.0004397012],"about_ca_topic_score_codex":0.0014022696,"about_ca_topic_score_gemma":0.00013961155,"teacher_disagreement_score":0.25247538,"about_ca_system_score_codex":9.322975e-7,"about_ca_system_score_gemma":0.000014227276,"threshold_uncertainty_score":0.9997471},"labels":[],"label_agreement":null},{"id":"W3088383102","doi":"10.1144/geosci2019-015","title":"What lies beneath: Thoughts on the lower mantle","year":2019,"lang":"en","type":"article","venue":"Geoscientist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Geophysics","score_opus":0.009880556870161738,"score_gpt":0.19614915337412153,"score_spread":0.1862685965039598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088383102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97206813,0.00016840769,0.0000061821224,0.0006691381,0.012606018,0.00019187188,0.00012618594,0.000028218716,0.0141358655],"genre_scores_gemma":[0.971778,0.000064147134,0.000038998813,0.0005025672,0.0004289299,0.0000011796177,0.000054757536,0.0000032166006,0.027128223],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.999016,0.000045733694,0.00010697717,0.0002615852,0.0002899618,0.00027974456],"domain_scores_gemma":[0.9994078,0.000098608936,0.000048251117,0.00036727783,0.000021926648,0.00005613587],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00027898798,0.00010736579,0.000116909076,0.000029417577,0.00023195235,0.00057852967,0.00031995142,0.000034268647,0.00558444],"category_scores_gemma":[0.000010487126,0.00006108483,0.00005002726,0.00013295234,0.000074878895,0.00031071148,0.000025377265,0.00006017984,0.01002652],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00079579564,0.00119259,0.15235424,0.00040364388,0.00039769273,0.0004169837,0.0064704735,0.008161984,0.03173628,0.10774362,0.5615512,0.12877548],"study_design_scores_gemma":[0.00020203546,0.00022638995,0.16796511,0.00006676121,0.000013787166,0.000005372574,0.00018834091,0.0005403682,0.0031644586,0.003757959,0.823596,0.0002733963],"about_ca_topic_score_codex":0.00040142177,"about_ca_topic_score_gemma":0.00048553955,"teacher_disagreement_score":0.2620448,"about_ca_system_score_codex":0.0000013429104,"about_ca_system_score_gemma":0.000015445414,"threshold_uncertainty_score":0.9953246},"labels":[],"label_agreement":null},{"id":"W3092373959","doi":"10.1016/j.ijhydene.2020.09.126","title":"The structural phase transition of ammonia borane under high pressure","year":2020,"lang":"en","type":"article","venue":"International Journal of Hydrogen Energy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"State Key Laboratory of Polymer Materials Engineering; China Academy of Engineering Physics; National Key Research and Development Program of China; Ministerio de Ciencia, Innovación y Universidades","keywords":"Ammonia borane; Borane; Hydrogen storage; Raman spectroscopy; Phonon; Phase transition; Density functional theory; Phase (matter); Chemistry; Ammonia; Hydrogen bond; Hydrogen; Thermodynamics; Materials science; Physical chemistry; Crystallography; Computational chemistry; Molecule; Condensed matter physics; Organic chemistry; Physics; Catalysis","score_opus":0.00896418646250125,"score_gpt":0.22724789687392938,"score_spread":0.21828371041142813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092373959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945119,0.00076433434,0.00061162916,0.0029311061,0.00082819455,0.000022021828,0.00021940953,0.0000048177194,0.00010656434],"genre_scores_gemma":[0.99870634,0.00011414935,0.000117382384,0.00029185344,0.00070162193,1.3683382e-7,0.000043181648,0.0000029475689,0.000022406435],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989968,0.000060786962,0.00033719555,0.00007480132,0.00043410284,0.0000963008],"domain_scores_gemma":[0.9993306,0.0000608573,0.000287788,0.000054221804,0.0001875139,0.00007901732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000109092354,0.000077332195,0.00014808524,0.000029008845,0.000049492246,0.00005098692,0.00038668918,0.000030339337,0.00044040542],"category_scores_gemma":[0.000013428453,0.000048729613,0.00008798148,0.00005110751,0.000050456936,0.00017954897,0.000008367907,0.00006021571,0.000004116224],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004465482,0.00013613097,0.0009905242,0.000038820817,0.0033384624,0.000318394,0.0015574901,0.69754624,0.18827331,0.02170502,0.0026929926,0.07893714],"study_design_scores_gemma":[0.010714773,0.002782083,0.01888483,0.00014200999,0.00067518756,0.00053348334,0.00041613524,0.080966026,0.580317,0.05295516,0.25077578,0.00083752157],"about_ca_topic_score_codex":0.00079525926,"about_ca_topic_score_gemma":0.00011875399,"teacher_disagreement_score":0.6165802,"about_ca_system_score_codex":0.0000018334315,"about_ca_system_score_gemma":0.0000443912,"threshold_uncertainty_score":0.48221305},"labels":[],"label_agreement":null},{"id":"W3093039332","doi":"","title":"Thermal expansivity and elastic properties of the lithospheric mantle: results from mineral physics of composites","year":2005,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Lithosphere; Mantle (geology); Geology; Archean; Thermal expansion; Geophysics; Thermal; Petrology; Seismology; Geochemistry; Thermodynamics; Physics; Tectonics","score_opus":0.013021058764091743,"score_gpt":0.18185303244063356,"score_spread":0.16883197367654182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093039332","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99805844,0.0003412175,0.0000020225145,0.000068592504,0.00016657932,0.00008492759,0.00006715327,0.000014638703,0.0011964028],"genre_scores_gemma":[0.9984075,0.000012955271,0.0013146385,0.000015407382,0.00021179215,3.49665e-7,0.0000053772437,0.0000039166052,0.00002806637],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9991466,0.000052280255,0.0003014131,0.00016334935,0.00017603606,0.00016034729],"domain_scores_gemma":[0.9993186,0.00016736341,0.00025754253,0.00018123927,0.00003764709,0.000037616363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019325456,0.000108062566,0.00019169539,0.0000071592717,0.00008053971,0.000030848732,0.00015477432,0.000036781137,0.000008726245],"category_scores_gemma":[0.000085390944,0.00006938304,0.000035540426,0.00005480107,0.000103068654,0.000113185095,0.00003275325,0.000072792325,0.000006873277],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008969011,0.000037692913,0.08914173,0.000075586526,0.000033798522,0.0000013835398,0.0012168091,0.13864808,0.76596993,0.0000075654957,0.0000118784,0.0047658915],"study_design_scores_gemma":[0.00017146276,0.000018512525,0.73295295,0.00018086794,0.000021788537,2.9594517e-7,0.000030466825,0.0021321226,0.26433605,0.000021472353,0.000059627702,0.00007440615],"about_ca_topic_score_codex":0.019695051,"about_ca_topic_score_gemma":0.0007407092,"teacher_disagreement_score":0.6438112,"about_ca_system_score_codex":0.0000012136512,"about_ca_system_score_gemma":0.000015739679,"threshold_uncertainty_score":0.98683286},"labels":[],"label_agreement":null},{"id":"W3093246739","doi":"10.1093/mnras/staa2615","title":"Chemical fingerprints of formation in rocky super-Earths’ data","year":2020,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; California Institute of Technology; National Aeronautics and Space Administration; Vanderbilt University; National Science Foundation","keywords":"Physics; Astrobiology; Astronomy","score_opus":0.019157220168711554,"score_gpt":0.1973449069095669,"score_spread":0.17818768674085536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093246739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99862725,0.000039639872,0.000013040817,0.00047809727,0.00009377487,0.00011591746,0.00042599425,0.0000067929836,0.00019952486],"genre_scores_gemma":[0.99826676,1.692061e-7,0.0014698259,0.000045742105,0.00009578324,4.163975e-7,0.000112927344,0.0000023529678,0.0000060345674],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991527,0.00004324123,0.00030461946,0.0001812106,0.00015064578,0.00016756497],"domain_scores_gemma":[0.99945176,0.00007707883,0.00013559098,0.00025921327,0.000014622565,0.000061716746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016177667,0.00008826077,0.00022308831,0.000004356032,0.000030191404,0.000018257833,0.0006828229,0.00005645292,0.00025338025],"category_scores_gemma":[0.000042190062,0.00006314311,0.00009840094,0.00006131549,0.00007932841,0.00017331052,0.00018646472,0.00010347809,0.000020329642],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009856739,0.000051595285,0.11857834,0.00011242578,0.00004241657,1.3494932e-7,0.0011001129,0.8743309,0.002056611,0.000009056296,0.0012222956,0.0023975428],"study_design_scores_gemma":[0.00028252482,0.000028489874,0.29287517,0.000019963376,0.000021936232,4.206735e-9,0.000118233744,0.6971183,0.008935036,0.000012019071,0.0005048119,0.000083546045],"about_ca_topic_score_codex":0.0010989011,"about_ca_topic_score_gemma":0.0001088506,"teacher_disagreement_score":0.17721263,"about_ca_system_score_codex":0.0000031088196,"about_ca_system_score_gemma":0.000019590194,"threshold_uncertainty_score":0.2774336},"labels":[],"label_agreement":null},{"id":"W3094954291","doi":"10.1103/physrevb.102.134120","title":"Two good metals make a semiconductor: A potassium-nickel compound under pressure","year":2020,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy","keywords":"Nickel; Ground state; Intermetallic; Materials science; Condensed matter physics; Potassium; Metal; Fermi level; Band gap; Electronic structure; Electronic band structure; Electron; Crystallography; Physics; Atomic physics; Chemistry; Metallurgy; Quantum mechanics","score_opus":0.03223535016174382,"score_gpt":0.32729219899541734,"score_spread":0.2950568488336735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094954291","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.51373464,0.41395813,0.0012951664,0.031537175,0.0015574762,0.0076781833,0.0032827063,0.00082966033,0.026126891],"genre_scores_gemma":[0.9336721,0.04100912,0.00020072474,0.021991828,0.002309128,0.00006384919,0.00050870684,0.000051541112,0.00019305463],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9945432,0.0008234517,0.0010315964,0.0013391563,0.0012292311,0.001033357],"domain_scores_gemma":[0.99656445,0.0005916214,0.00060502125,0.0010388382,0.0002025232,0.0009975719],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00054148404,0.00090840453,0.0029074724,0.00003434343,0.00023141902,0.00018122065,0.0012004611,0.00007207141,0.0015244744],"category_scores_gemma":[0.0003752174,0.0006658327,0.0011072665,0.0008828541,0.0002523384,0.00050258037,0.0002025099,0.00069380895,0.0052688885],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035106583,0.0032827961,0.0021748692,0.07703081,0.0038522407,0.00030595547,0.000889666,0.001617228,0.18840788,0.48591176,0.1656298,0.07054591],"study_design_scores_gemma":[0.0016636259,0.000955952,0.0038844037,0.008782055,0.0058112047,0.0000389334,0.000029082712,0.018503917,0.0061053545,0.07306086,0.8781156,0.0030490179],"about_ca_topic_score_codex":0.0003234634,"about_ca_topic_score_gemma":0.00003858168,"teacher_disagreement_score":0.7124858,"about_ca_system_score_codex":0.000011001882,"about_ca_system_score_gemma":0.0001608438,"threshold_uncertainty_score":0.9995793},"labels":[],"label_agreement":null},{"id":"W3098277841","doi":"10.1093/gji/ggaa541","title":"3-D and 5-D reconstruction of<i>P</i>receiver functions via multichannel singular spectrum analysis","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"University of Alberta; Incorporated Research Institutions for Seismology","keywords":"Classification of discontinuities; Algorithm; Computer science; Discontinuity (linguistics); Signal processing; Geology; Singular spectrum analysis; Data processing; Receiver function; Seismology; Mathematics; Telecommunications; Singular value decomposition; Mathematical analysis","score_opus":0.00979956962973113,"score_gpt":0.20027664050354954,"score_spread":0.1904770708738184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3098277841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9798489,0.000048740796,0.0162166,0.0017269107,0.0011104824,0.000049792558,0.00013563856,0.000016056369,0.00084688613],"genre_scores_gemma":[0.9978609,0.00003179534,0.00082186464,0.0001531349,0.0010030561,2.6453233e-7,0.000052221316,0.0000027004944,0.00007406528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999092,0.000050053666,0.00026500874,0.0001770924,0.00027612544,0.00013973183],"domain_scores_gemma":[0.9994391,0.000058441714,0.00017703522,0.000058692804,0.00009963193,0.00016708221],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009489283,0.00010225321,0.00022640904,0.00010056604,0.00010927546,0.00009321785,0.00014184201,0.000036477075,0.001986078],"category_scores_gemma":[0.000032012278,0.00008590573,0.00014774877,0.00023939402,0.000077672674,0.00027880524,0.000018328046,0.00014324687,0.000095051044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015387317,0.00046333866,0.40569112,0.00010247885,0.011789519,0.00020946297,0.0032850262,0.09099479,0.10219156,0.0027832736,0.0026430995,0.37830758],"study_design_scores_gemma":[0.001013132,0.0003997383,0.77329034,0.000027569216,0.0008945322,0.00015499858,0.00018697663,0.20320918,0.0043884898,0.011474137,0.0045307176,0.0004301727],"about_ca_topic_score_codex":0.0003730814,"about_ca_topic_score_gemma":0.00004255928,"teacher_disagreement_score":0.3778774,"about_ca_system_score_codex":0.0000032441678,"about_ca_system_score_gemma":0.000019362553,"threshold_uncertainty_score":0.9989262},"labels":[],"label_agreement":null},{"id":"W3100410436","doi":"10.1038/s41467-020-19541-y","title":"Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers","year":2020,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Geology; Forearc; Mantle wedge; Seismic anisotropy; Subduction; Seismology; Seafloor spreading; Mantle (geology); Anisotropy; Shear wave splitting; Geophysics; Slab; Shear (geology); Tectonics; Petrology; Physics","score_opus":0.06643625572188691,"score_gpt":0.263637697034273,"score_spread":0.19720144131238607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3100410436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9851899,0.0036254695,0.0012942769,0.0034914976,0.0004337518,0.00041473654,0.003011035,0.00007778789,0.0024615373],"genre_scores_gemma":[0.96966565,0.00021724765,0.028666386,0.00046657174,0.00009111568,0.000001405462,0.0008653403,0.0000066881566,0.0000196107],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99903256,0.00014162205,0.00026329551,0.00018382362,0.00018695254,0.00019176194],"domain_scores_gemma":[0.99872375,0.00020064581,0.00014418366,0.0007339761,0.00008178679,0.00011564372],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012004609,0.00012383224,0.00024618756,0.000052151718,0.00019408496,0.00005587543,0.0006379963,0.00014386886,0.00045400654],"category_scores_gemma":[0.00006193139,0.00011001838,0.00006755147,0.00029165766,0.00010417626,0.0001656925,0.0001371536,0.0003290194,0.000050265848],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072849105,0.0007343125,0.30388606,0.0007417081,0.0022287152,0.00008373464,0.033168536,0.013751222,0.54020876,0.023530679,0.03871198,0.0422258],"study_design_scores_gemma":[0.001795441,0.00028579554,0.5156091,0.0002640758,0.00030442956,0.000008885886,0.002149937,0.19238453,0.012593495,0.004359767,0.2691127,0.001131813],"about_ca_topic_score_codex":0.0029408382,"about_ca_topic_score_gemma":0.0004042104,"teacher_disagreement_score":0.52761525,"about_ca_system_score_codex":0.0000041983676,"about_ca_system_score_gemma":0.0000670829,"threshold_uncertainty_score":0.49710533},"labels":[],"label_agreement":null},{"id":"W3103251169","doi":"","title":"A note on the metallization of compressed liquid hydrogen","year":2016,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Lawrence Livermore National Laboratory; Natural Sciences and Engineering Research Council of Canada; Killam Trusts","keywords":"Schematic; Dissociation (chemistry); Phase diagram; Covalent bond; Molecular dynamics; Hydrogen; Materials science; Chemical physics; Hydrogen bond; Quadratic equation; Realization (probability); Metal; Nanotechnology; Molecule; Phase (matter); Chemistry; Computational chemistry; Physics; Physical chemistry; Metallurgy; Electronic engineering; Quantum mechanics; Mathematics; Engineering","score_opus":0.01473830838156121,"score_gpt":0.20543307585535103,"score_spread":0.19069476747378983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3103251169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98170656,0.000017433253,0.000796867,0.000883363,0.00013088154,0.00010920033,0.000072267445,0.000018375868,0.01626504],"genre_scores_gemma":[0.9992186,0.0000143288535,0.0000551186,0.00015730935,0.000045579833,5.717207e-7,0.000009101708,0.0000012669623,0.00049813825],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99956536,0.00004868958,0.000099101366,0.000081172875,0.00012065723,0.000085039275],"domain_scores_gemma":[0.9996008,0.00016684011,0.00004646824,0.00014186623,0.000020506059,0.000023475608],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001327914,0.000049821505,0.00008360012,0.000013339994,0.000037086877,0.000009563426,0.00012674951,0.00001933393,0.0053371675],"category_scores_gemma":[0.000018999559,0.000019450681,0.000026158245,0.000044878227,0.000033556178,0.000053837342,0.000005943239,0.000010466538,0.00035896897],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004860812,0.000069564085,0.0024068283,0.000032364613,0.00012225808,0.0000034035143,0.00033443017,0.002681096,0.9256506,0.053559467,0.0035078044,0.011146125],"study_design_scores_gemma":[0.0003276589,0.00040910632,0.0129217,0.000035211182,0.000028563376,6.6112335e-7,0.000009590359,0.00069929083,0.94312626,0.004143562,0.038138296,0.00016007607],"about_ca_topic_score_codex":0.00040960475,"about_ca_topic_score_gemma":0.00012080624,"teacher_disagreement_score":0.049415905,"about_ca_system_score_codex":3.4945737e-7,"about_ca_system_score_gemma":0.00000919359,"threshold_uncertainty_score":0.9955721},"labels":[],"label_agreement":null},{"id":"W3105087116","doi":"","title":"On generalized Born−Infeld electrodynamics","year":2016,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Physics; Quantum electrodynamics; Symmetry (geometry); Tensor (intrinsic definition); Mathematical physics; Quantum mechanics; Classical mechanics; Geometry","score_opus":0.005905911402771783,"score_gpt":0.18892697029011338,"score_spread":0.1830210588873416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3105087116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9520704,0.000018907944,0.00061949977,0.00068093254,0.00047227534,0.000077810524,0.00007820656,0.00006934386,0.045912612],"genre_scores_gemma":[0.9935279,0.000040317653,0.00034844366,0.0004956151,0.00016157614,6.5617684e-7,0.000025288566,0.0000025477566,0.0053976495],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99935985,0.000030008137,0.00010238401,0.00015870687,0.00012265629,0.00022637672],"domain_scores_gemma":[0.99964374,0.000082353625,0.000028387773,0.00016167504,0.000015831092,0.000068008834],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00009668565,0.00008538965,0.00010808885,0.000025289179,0.00005339009,0.000033620545,0.000118453754,0.00003656925,0.010638773],"category_scores_gemma":[0.000016452987,0.000043421765,0.00003275072,0.0000471369,0.00001973181,0.00008116096,0.000004702278,0.000021582007,0.0019377274],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005882713,0.00011280368,0.036182515,0.000032362434,0.0001756018,0.0000500414,0.000099009085,0.0012175255,0.19046466,0.5276753,0.087186575,0.15621535],"study_design_scores_gemma":[0.0037161794,0.0016568564,0.32359025,0.00007127659,0.00006938727,0.00001556316,0.0000110895435,0.004169962,0.07788285,0.24397363,0.3431435,0.0016994757],"about_ca_topic_score_codex":0.0007082993,"about_ca_topic_score_gemma":0.000611526,"teacher_disagreement_score":0.28740773,"about_ca_system_score_codex":0.0000013811766,"about_ca_system_score_gemma":0.000016750126,"threshold_uncertainty_score":0.9988394},"labels":[],"label_agreement":null},{"id":"W3106085707","doi":"","title":"Idealized Slab Plasma approach for the study of Warm Dense Matter","year":2005,"lang":"en","type":"article","venue":"CERN Document Server (European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; University of British Columbia","funders":"","keywords":"Warm dense matter; Plasma; Slab; Isochoric process; Physics; Dense matter; Equation of state; Opacity; Shock wave; Shock (circulatory); Ionization; Computational physics; Mechanics; Nuclear physics; Astrophysics; Geophysics; Neutron star; Thermodynamics; Ion; Optics; Quantum mechanics","score_opus":0.02663454103578545,"score_gpt":0.24940696904182996,"score_spread":0.22277242800604452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106085707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967777,0.00003133882,0.000029456314,0.00043963388,0.00012017827,0.0014332335,0.000025296713,0.000054488195,0.0010886638],"genre_scores_gemma":[0.9976989,0.000019733441,0.00008064429,0.00011380707,0.00020449396,0.0000011991111,0.00025176664,0.000065564614,0.0015638742],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984039,0.00030065072,0.00029706873,0.00029506767,0.00039768335,0.0003056308],"domain_scores_gemma":[0.9990494,0.00010882483,0.000115115974,0.00038158926,0.00025992523,0.00008511184],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010634799,0.00012630367,0.00016968674,0.000071764196,0.0006589671,0.00034474916,0.0006973602,0.00003069441,0.0069302376],"category_scores_gemma":[0.000070098096,0.00008942407,0.000047149006,0.0002459116,0.0000719555,0.00025029993,0.00014019554,0.00008364707,0.0011616522],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.011617614,0.010570713,0.09989143,0.004560492,0.0056827217,0.000059759666,0.1069563,0.2113184,0.007240414,0.13345793,0.3444312,0.06421302],"study_design_scores_gemma":[0.022886947,0.0055999933,0.3348132,0.00011002396,0.0007428123,0.000049012855,0.012159352,0.0052066282,0.011067806,0.008839408,0.5963267,0.0021980868],"about_ca_topic_score_codex":0.00031664327,"about_ca_topic_score_gemma":0.00003178996,"teacher_disagreement_score":0.25189552,"about_ca_system_score_codex":0.000010649371,"about_ca_system_score_gemma":0.00000901383,"threshold_uncertainty_score":0.9996161},"labels":[],"label_agreement":null},{"id":"W3106545159","doi":"10.1029/2020jb020574","title":"Variations in Seismic Wave Speed and <i>V</i><sub><i>P</i></sub>/<i>V</i><sub><i>S</i></sub> Ratio in the North American Lithosphere","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Geology; Rayleigh wave; P wave; Mantle (geology); Seismology; Tectonics; Mineralogy; Geometry; Geophysics; Wave propagation; Physics; Optics; Mathematics","score_opus":0.028966227016934368,"score_gpt":0.2674094895166785,"score_spread":0.23844326249974412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106545159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946672,0.00012435496,0.00009074694,0.004068728,0.00015170196,0.00044388714,0.00011518972,0.000013434473,0.00032481027],"genre_scores_gemma":[0.9968363,0.00085237407,0.00014231261,0.0010815361,0.0010265332,0.000003858469,0.000033939214,0.000016315624,0.0000067994692],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9951072,0.0011710731,0.0008402474,0.00045328017,0.0014846264,0.00094361574],"domain_scores_gemma":[0.99728835,0.0011761219,0.0003726359,0.0003119156,0.00032106182,0.0005299443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017930749,0.00030592302,0.0007715514,0.00019906939,0.0002700005,0.00040540248,0.0005916798,0.00008288506,0.000038886126],"category_scores_gemma":[0.0005397753,0.0002217349,0.0001632794,0.0018603907,0.0004259898,0.00062250026,0.00009733666,0.0013972794,0.0001773137],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0041701184,0.0017154989,0.13323615,0.00055789546,0.0005106463,0.003697221,0.02347733,0.034396976,0.611642,0.0011356977,0.010281627,0.17517881],"study_design_scores_gemma":[0.0012754884,0.0017099354,0.9457666,0.00008953248,0.00003901581,0.000044499113,0.0005883733,0.01939523,0.02688399,0.001907898,0.0019025351,0.0003968591],"about_ca_topic_score_codex":0.0013308295,"about_ca_topic_score_gemma":0.0037800285,"teacher_disagreement_score":0.8125305,"about_ca_system_score_codex":0.000012986259,"about_ca_system_score_gemma":0.00041582875,"threshold_uncertainty_score":0.90420866},"labels":[],"label_agreement":null},{"id":"W3110119943","doi":"10.1080/08927022.2020.1836370","title":"Considerations when calculating the mechanical properties of single crystals and bulk polycrystals from molecular dynamics simulations","year":2020,"lang":"en","type":"article","venue":"Molecular Simulation","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Molecular dynamics; Materials science; Interatomic potential; Elastic modulus; Crystallite; Crystal (programming language); Poisson distribution; Single crystal; Thermodynamics; Statistical physics; Stress (linguistics); Moduli; Tension (geology); Poisson's ratio; Orientation (vector space); Ultimate tensile strength; Physics; Computational chemistry; Mathematics; Chemistry; Crystallography; Composite material; Geometry; Computer science","score_opus":0.025395205217199835,"score_gpt":0.210753953709548,"score_spread":0.18535874849234815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3110119943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9569619,0.00029650744,0.04060041,0.0012911509,0.00006454404,0.000357085,0.00029258765,0.00003614264,0.000099620236],"genre_scores_gemma":[0.9976171,0.0000011351862,0.0016524161,0.00046857932,0.000050373183,0.0000013870236,0.00019546824,0.000009391916,0.000004131757],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998763,0.00017554419,0.00036371817,0.00025728653,0.00027200856,0.00016841166],"domain_scores_gemma":[0.99923825,0.00022363038,0.00015577975,0.00019538433,0.000099119665,0.000087850545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011262775,0.00014644394,0.00022350822,0.00002797789,0.00017919953,0.00013408056,0.000093107294,0.000076982134,0.00025111527],"category_scores_gemma":[0.000286424,0.00011227609,0.00005700743,0.000101694066,0.000076752105,0.00015607264,0.000035199704,0.000070920774,0.0000058287574],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000138232435,0.000008151938,0.00028330713,0.000012414804,0.000032604683,0.0000041869625,0.0005195693,0.5607015,0.43716058,0.0010139382,0.0000020669445,0.00024785363],"study_design_scores_gemma":[0.00024292197,0.00006791054,0.001091626,0.000024724994,0.00007576026,8.5394e-7,0.000073122814,0.92568046,0.06353982,0.00897535,0.000071763876,0.00015567006],"about_ca_topic_score_codex":0.0009104658,"about_ca_topic_score_gemma":0.00019278303,"teacher_disagreement_score":0.37362075,"about_ca_system_score_codex":0.0000050223553,"about_ca_system_score_gemma":0.00004226506,"threshold_uncertainty_score":0.45784858},"labels":[],"label_agreement":null},{"id":"W3112709350","doi":"10.1063/5.0040062","title":"Efficacy of the radial pair potential approximation for molecular dynamics simulations of dense plasmas","year":2021,"lang":"en","type":"article","venue":"Physics of Plasmas","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"Sandia National Laboratories","keywords":"Molecular dynamics; Microscale chemistry; Plasma; Range (aeronautics); Periodic boundary conditions; Boundary (topology); Boundary value problem; Power (physics)","score_opus":0.009854809904735215,"score_gpt":0.21055353142482913,"score_spread":0.2006987215200939,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112709350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888221,0.000027818449,0.008963268,0.00007201255,0.00038392656,0.00025588035,0.0012889368,0.000006757157,0.00017930895],"genre_scores_gemma":[0.99706113,0.0000024829096,0.00244581,0.000007725166,0.00008272792,0.0000011663554,0.00036499024,0.0000051648676,0.000028770808],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991279,0.000065187705,0.0003009729,0.00014353142,0.00023024711,0.00013213958],"domain_scores_gemma":[0.99903303,0.00024491598,0.00027792447,0.00024124426,0.00017229129,0.000030614272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009722749,0.000097275566,0.0002462273,0.00001948652,0.00006202619,0.000012998732,0.00016396325,0.000049415165,0.000040968065],"category_scores_gemma":[0.00008588893,0.00007957446,0.00016366338,0.00016447871,0.00008507325,0.00008804456,0.000022707398,0.00004313807,0.0000023399773],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017547427,0.00018784603,0.0029876386,0.000257124,0.00014802419,0.0000014222757,0.0003685651,0.86471397,0.11136042,0.016455663,0.00004373231,0.0033001292],"study_design_scores_gemma":[0.0011903477,0.00009245822,0.013591968,0.000051364488,0.00018482421,0.0000012461278,0.000047567897,0.43185854,0.5306983,0.02201891,0.00010758587,0.00015688274],"about_ca_topic_score_codex":0.00014610478,"about_ca_topic_score_gemma":0.0001048907,"teacher_disagreement_score":0.43285543,"about_ca_system_score_codex":0.0000029595597,"about_ca_system_score_gemma":0.00012776372,"threshold_uncertainty_score":0.32449526},"labels":[],"label_agreement":null},{"id":"W3122144885","doi":"","title":"Seismic velocities, anisotropy and shear-wave splitting of antigorite serpentinites and tectonic implications for subduction zones","year":2013,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Geology; Seismic anisotropy; Subduction; Forearc; Mantle (geology); Anisotropy; Shear wave splitting; Peridotite; Shear (geology); Olivine; Tectonite; Seismology; Mineralogy; Petrology; Tectonics; Geophysics; Geochemistry; Shear zone","score_opus":0.016560275036884457,"score_gpt":0.21071381828240404,"score_spread":0.1941535432455196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3122144885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971519,0.00025176612,0.0014307324,0.00035643025,0.00010694217,0.00030494403,0.00012353627,0.000022164582,0.00025156463],"genre_scores_gemma":[0.9925987,0.00014224391,0.0068381545,0.000032869888,0.00007373282,0.0000058962078,0.00007126222,0.0000028806417,0.00023422606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994665,0.000017041699,0.00016162399,0.00016262068,0.00004336234,0.00014884325],"domain_scores_gemma":[0.9995976,0.00013542241,0.00006661732,0.00009138207,0.000062201056,0.000046797188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011240653,0.00007715832,0.00013940793,0.000035548215,0.00013649702,0.00007667578,0.000037084792,0.00003428078,0.00028767082],"category_scores_gemma":[0.00001805829,0.00006255872,0.000018345132,0.000057934674,0.00006799126,0.000226317,0.000011535204,0.000022419452,0.000008485818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083407795,0.000081010134,0.59409815,0.0011241556,0.00021198032,6.149865e-7,0.0015080831,0.0005994122,0.21760984,0.026886355,0.0021747067,0.15562229],"study_design_scores_gemma":[0.0002386928,0.00011728083,0.9634351,0.00001498459,0.000025990403,0.00000783933,0.00022747988,0.012698158,0.0043315487,0.017584126,0.0011761859,0.00014261616],"about_ca_topic_score_codex":0.0038030287,"about_ca_topic_score_gemma":0.00007612405,"teacher_disagreement_score":0.36933693,"about_ca_system_score_codex":6.4069854e-7,"about_ca_system_score_gemma":0.000014110132,"threshold_uncertainty_score":0.5749067},"labels":[],"label_agreement":null},{"id":"W3127973157","doi":"10.1029/2020je006793","title":"Electrical Resistivity of FeS at High Pressures and Temperatures: Implications of Thermal Transport in the Core of Ganymede","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Planets","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Electrical conductor; Materials science; Impurity; Thermal; Adiabatic process; Dynamo theory; Dynamo; Thermal conductivity; Core (optical fiber); Convection; Thermodynamics; Chemistry; Composite material; Magnetic field; Electrical engineering; Physics","score_opus":0.036773201817248344,"score_gpt":0.3034044280339419,"score_spread":0.26663122621669355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127973157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979229,0.00078862417,0.0000011734996,0.00037587582,0.000038326034,0.00012304606,0.00042299123,0.0000012019121,0.00032586654],"genre_scores_gemma":[0.99937207,0.00031405987,0.00007514315,0.000014147647,0.00010980127,8.553705e-7,0.000055531113,0.0000027749743,0.000055605666],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99788785,0.0004288093,0.00047246332,0.00014399251,0.0008084104,0.00025848846],"domain_scores_gemma":[0.9974728,0.0016595882,0.00023408498,0.00021091566,0.00032864622,0.000093950366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010948757,0.0000941809,0.00043513317,0.00010094302,0.00007762233,0.000016254635,0.0003355852,0.00006688519,0.00013300612],"category_scores_gemma":[0.00023038452,0.00005740463,0.00007538003,0.00035439877,0.00027543976,0.00009374111,0.00002332471,0.00034541558,0.0000015386877],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001655362,0.00061488175,0.28300884,0.0003631522,0.00017847621,0.00023448515,0.001031014,0.00036993486,0.70376414,0.0029991996,0.0017412915,0.0040392177],"study_design_scores_gemma":[0.000303948,0.00042517702,0.973827,0.00005718719,0.000025982374,0.00002605306,0.00004805518,0.000026687365,0.022624988,0.0021695544,0.00041340635,0.000051937477],"about_ca_topic_score_codex":0.0021910088,"about_ca_topic_score_gemma":0.00086093735,"teacher_disagreement_score":0.6908182,"about_ca_system_score_codex":0.0000031785078,"about_ca_system_score_gemma":0.00021736501,"threshold_uncertainty_score":0.33121645},"labels":[],"label_agreement":null},{"id":"W3129103754","doi":"10.1029/2020jb020678","title":"Balanced Cross‐Sections and Numerical Modeling of the Lithospheric‐Scale Evolution of the Hindu Kush and Pamir","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Magmatism; Subduction; Lithosphere; Crust; Terrane; Mantle (geology); Seismology; Metamorphism; Continental crust; Delamination (geology); Geochemistry; Tectonics","score_opus":0.021993263609231303,"score_gpt":0.29388181751759584,"score_spread":0.2718885539083645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129103754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830717,0.0003762181,0.00026707278,0.00037273866,0.00024615452,0.00008984925,0.00004773308,0.0000020770797,0.0002909908],"genre_scores_gemma":[0.9992227,0.000095595635,0.00024228054,0.00001407832,0.00023215749,4.5061861e-7,9.1778327e-7,0.0000033121985,0.00018849368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980944,0.00038446946,0.0003510589,0.00014331055,0.00076704856,0.00025974243],"domain_scores_gemma":[0.99869674,0.0002659673,0.00018092211,0.00020989074,0.0005222734,0.0001242011],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000716875,0.000084779094,0.0002957056,0.000025667416,0.0002739813,0.00008379397,0.00024370675,0.000056555793,0.000057163317],"category_scores_gemma":[0.00030483236,0.000046639434,0.000120506644,0.00040848972,0.00033503305,0.00018409338,0.0001113133,0.00039749983,0.0000026477192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011147565,0.0008784543,0.62299734,0.00062699744,0.0004836769,0.000041940606,0.0037319579,0.13948976,0.21185525,0.0032378726,0.00064446375,0.014897558],"study_design_scores_gemma":[0.00033729733,0.00021995384,0.93348765,0.00010514672,0.000021958245,0.000024730623,0.00021050315,0.050280396,0.009275625,0.0057075517,0.00025924263,0.000069925125],"about_ca_topic_score_codex":0.0013747007,"about_ca_topic_score_gemma":0.00013430191,"teacher_disagreement_score":0.31049034,"about_ca_system_score_codex":0.000004735484,"about_ca_system_score_gemma":0.00026084838,"threshold_uncertainty_score":0.21072704},"labels":[],"label_agreement":null},{"id":"W3129695577","doi":"10.1002/pssb.202000588","title":"Solid Nitrogen and Nitrogen‐Rich Compounds as High‐Energy‐Density Materials","year":2021,"lang":"en","type":"article","venue":"physica status solidi (b)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Nitrogen; Solid nitrogen; Materials science; Diamond; High pressure; Nanotechnology; Realization (probability); Chemical engineering; Engineering physics; Chemistry; Organic chemistry; Composite material; Physics","score_opus":0.009748315130763388,"score_gpt":0.22747066159294846,"score_spread":0.21772234646218508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129695577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99489534,0.0003594109,0.000035894365,0.00021134771,0.0007910753,0.00011180173,0.0009495888,0.00008921336,0.002556338],"genre_scores_gemma":[0.99683654,0.00026574093,0.0003817369,0.00047623424,0.00071757764,0.000004917111,0.0010803789,0.000017859522,0.000219002],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.997734,0.00021792889,0.00033547517,0.00057656976,0.00037221535,0.00076381076],"domain_scores_gemma":[0.9988018,0.00011914722,0.00015931741,0.00042807419,0.00016665229,0.000324968],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014031258,0.00032858766,0.0006156211,0.000045905064,0.0003591823,0.00036342742,0.00018755643,0.00009356693,0.0013178583],"category_scores_gemma":[0.000027352096,0.00030163687,0.00007873496,0.00021620798,0.00013077828,0.00028175907,0.00010338155,0.00009635903,0.0004691661],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038867668,0.0003774415,0.027350428,0.00023088763,0.0007444323,0.00047458766,0.0010360248,0.00013245431,0.8953326,0.059228487,0.011477119,0.0032268672],"study_design_scores_gemma":[0.0006346321,0.00014583912,0.017890157,0.000024990464,0.00014148539,0.000046905407,0.0001103243,0.00006772223,0.7489412,0.22127509,0.010117637,0.00060403126],"about_ca_topic_score_codex":0.008276832,"about_ca_topic_score_gemma":0.00053353066,"teacher_disagreement_score":0.1620466,"about_ca_system_score_codex":0.0000071204445,"about_ca_system_score_gemma":0.00016528317,"threshold_uncertainty_score":0.99994355},"labels":[],"label_agreement":null},{"id":"W3130716649","doi":"10.1063/5.0047642","title":"Simple pair-potentials and pseudo-potentials for warm-dense matter applications","year":2021,"lang":"en","type":"article","venue":"Physics of Plasmas","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Density functional theory; Simple (philosophy); Warm dense matter; Ion; Tetrahedron; Molecular dynamics; Class (philosophy); Electron","score_opus":0.013336597338180614,"score_gpt":0.22390261642124518,"score_spread":0.21056601908306455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3130716649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9761556,0.00030060194,0.01830508,0.0004331382,0.00036879705,0.00062105467,0.0026831352,0.000039850613,0.0010927598],"genre_scores_gemma":[0.9948593,0.000052984244,0.0036875254,0.00013112128,0.00033747856,0.000019840732,0.00059800013,0.000008879542,0.00030488343],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990025,0.00004565974,0.0002635969,0.00029087876,0.00015830959,0.00023906196],"domain_scores_gemma":[0.99919087,0.00019423901,0.00014206689,0.00025915582,0.00012743544,0.00008626159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014925469,0.00013786787,0.00030017438,0.000019678851,0.0001392174,0.00007516449,0.00012547309,0.00005219606,0.0006620175],"category_scores_gemma":[0.000014349693,0.00012822525,0.00009158117,0.00010024218,0.00006873599,0.00015545532,0.00003004197,0.000041341424,0.0001601263],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033151984,0.0006770708,0.09327446,0.0022814258,0.0010242844,0.000030628496,0.0010595537,0.009902849,0.7332871,0.032104533,0.05174224,0.074284315],"study_design_scores_gemma":[0.0016848197,0.0001839709,0.052491922,0.000057924746,0.00049709657,0.000018849481,0.00019724577,0.0044184253,0.5633419,0.27879137,0.09737913,0.00093730335],"about_ca_topic_score_codex":0.00025112968,"about_ca_topic_score_gemma":0.000067514884,"teacher_disagreement_score":0.24668685,"about_ca_system_score_codex":0.0000010750373,"about_ca_system_score_gemma":0.00004204417,"threshold_uncertainty_score":0.7248627},"labels":[],"label_agreement":null},{"id":"W3133921129","doi":"","title":"The Feedback Between Surface Mobility and Mantle Compositional Heterogeneity: Implications for the Earth and Other Terrestrial Planets","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mantle (geology); Mantle convection; Geology; Upwelling; Lithosphere; Geophysics; Buoyancy; Convection; Planet; Tectonics; Mechanics; Physics; Seismology; Oceanography; Astrophysics","score_opus":0.026357479118949978,"score_gpt":0.24811705316705976,"score_spread":0.22175957404810978,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3133921129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971311,0.00018371953,0.000021656184,0.0009000679,0.00016841572,0.0002974309,0.00043479895,0.000018165667,0.00084463996],"genre_scores_gemma":[0.9991437,0.000020422443,0.00030075476,0.00009838664,0.00033449725,0.0000032721246,0.00007617881,0.0000038713256,0.000018869912],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992429,0.00007565727,0.00018791888,0.00019503877,0.000092472175,0.00020603149],"domain_scores_gemma":[0.99762374,0.0020149425,0.00010214097,0.00016917603,0.00001714546,0.000072848605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007526516,0.000099585726,0.000120358614,0.000006210095,0.00061746134,0.00020537026,0.00013857611,0.000045218825,0.00000382977],"category_scores_gemma":[0.000057605874,0.0000582471,0.000024011331,0.000021600978,0.00012429476,0.000054825217,0.000017715154,0.0000606976,0.0000136254685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000114091505,0.000021941247,0.9748826,0.000037650967,0.00010574474,3.1945746e-7,0.00015762652,0.0070691635,0.0022141573,0.00027759105,0.00072008546,0.014399036],"study_design_scores_gemma":[0.00022274863,0.00004627006,0.97412705,0.000008483127,0.000027419173,0.0000028738796,0.000011618849,0.0005358098,0.0003978509,0.001055562,0.023481648,0.000082654915],"about_ca_topic_score_codex":0.007504783,"about_ca_topic_score_gemma":0.008990729,"teacher_disagreement_score":0.022761563,"about_ca_system_score_codex":7.2654734e-7,"about_ca_system_score_gemma":0.000011902387,"threshold_uncertainty_score":0.9991043},"labels":[],"label_agreement":null},{"id":"W3134204943","doi":"10.1016/j.diamond.2020.107936","title":"WITHDRAWN: Automated FTIR mapping of boron distribution in diamond","year":2020,"lang":"en","type":"article","venue":"Diamond and Related Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"European Research Council; University of Alberta","keywords":"Diamond; Accidental; Fourier transform infrared spectroscopy; Computer science; Materials science; Library science; Engineering; Physics; Chemical engineering; Metallurgy","score_opus":0.007674113874358314,"score_gpt":0.18906295210171759,"score_spread":0.18138883822735927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134204943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968799,0.0004093037,0.000004035935,0.00023815267,0.00046428913,0.00022626616,0.00093949726,0.0001146177,0.0007239467],"genre_scores_gemma":[0.99860084,0.00023524654,0.00006451942,0.00005601977,0.000068997,0.0000020192372,0.0009271694,0.0000060851407,0.000039129118],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9987443,0.00011634475,0.00048028192,0.00026717884,0.00013414252,0.00025773255],"domain_scores_gemma":[0.99954927,0.000044015538,0.0001737028,0.00010500094,0.000026568698,0.00010141519],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000246022,0.00016488014,0.0004121967,0.000042363816,0.00006388999,0.00007119246,0.00010861889,0.00015155521,0.0008267155],"category_scores_gemma":[0.000043631233,0.00013190955,0.000029463357,0.00022846479,0.00008587257,0.00018636117,0.000025258325,0.000066778186,0.00006676075],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000256403,0.00006178242,0.026364299,0.00059389096,0.00011292339,0.00010287659,0.0024867603,0.0006501659,0.96485347,0.00063799554,0.00183709,0.0020423206],"study_design_scores_gemma":[0.001775048,0.00030455345,0.76669353,0.0002716327,0.000067635454,0.000011198491,0.00021538773,0.0025990598,0.22042647,0.0012990838,0.0057270913,0.0006092779],"about_ca_topic_score_codex":0.00090769096,"about_ca_topic_score_gemma":0.000023458186,"teacher_disagreement_score":0.744427,"about_ca_system_score_codex":0.0000021870883,"about_ca_system_score_gemma":0.000022971884,"threshold_uncertainty_score":0.90519553},"labels":[],"label_agreement":null},{"id":"W3134518932","doi":"10.1029/2020jb020924","title":"Lithospheric Structure and Flat‐Slab Subduction in the Northern Appalachians: Evidence From Rayleigh Wave Tomography","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Lithosphere; Subduction; Seismology; Terrane; Tectonics; Seismic tomography; Proterozoic; Geophysics; Paleontology; Mantle (geology)","score_opus":0.03367875215959434,"score_gpt":0.2860005344117303,"score_spread":0.252321782252136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134518932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99626863,0.002187409,0.000025614223,0.0008847533,0.00031421005,0.00013569274,0.000064661406,0.000004669756,0.00011435536],"genre_scores_gemma":[0.9974093,0.00074621907,0.0005578541,0.00006893479,0.0011351487,8.0161897e-7,0.000020457353,0.000005483593,0.000055802586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9968043,0.0009203174,0.00039026618,0.0002823321,0.0011475416,0.00045522515],"domain_scores_gemma":[0.9979179,0.0010427298,0.00015428866,0.0002895447,0.00040845483,0.00018709867],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011313392,0.00015650189,0.00038093427,0.0000927035,0.00020916606,0.00034592912,0.0003321564,0.000086379165,0.0005670965],"category_scores_gemma":[0.00038562043,0.00009721131,0.000121175995,0.00079274445,0.00020758084,0.0005098494,0.00004420797,0.0007945814,0.000031682517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021397336,0.00051162,0.61478996,0.00037030235,0.0006277834,0.0036216443,0.0180458,0.0029430883,0.1660852,0.0005668268,0.0019721116,0.18832594],"study_design_scores_gemma":[0.00036010583,0.0004280412,0.9718584,0.0001823424,0.000026755963,0.000058702513,0.0006032548,0.0007232382,0.004719569,0.019106165,0.001783359,0.0001501136],"about_ca_topic_score_codex":0.003947656,"about_ca_topic_score_gemma":0.004800863,"teacher_disagreement_score":0.3570684,"about_ca_system_score_codex":0.000004541129,"about_ca_system_score_gemma":0.00021488087,"threshold_uncertainty_score":0.6209309},"labels":[],"label_agreement":null},{"id":"W3134825266","doi":"","title":"Crustal and upper mantle anisotropy associated with fossilized transpression along the Denali Fault, northern Canadian Cordillera","year":2013,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transpression; Geology; Mantle (geology); Seismology; Fault (geology); Geophysics; Sinistral and dextral","score_opus":0.00852400879434837,"score_gpt":0.18939441641064936,"score_spread":0.180870407616301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134825266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99103826,0.00019613962,0.0000012901778,0.00038727128,0.00015852186,0.0003132732,0.00009252701,0.00004070123,0.0077719865],"genre_scores_gemma":[0.999281,0.000023552993,0.00013274985,0.00017270449,0.000091384456,0.0000049978453,0.00010092143,0.00001006247,0.00018266404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986569,0.0000962722,0.00023680057,0.00026502795,0.00026335855,0.0004816102],"domain_scores_gemma":[0.99913025,0.00021820582,0.00013446162,0.00016832966,0.00007982826,0.00026891349],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002629355,0.0001908968,0.0002115636,0.000037612765,0.00048317597,0.000277655,0.0001899818,0.00010282298,0.00024625298],"category_scores_gemma":[0.00006698179,0.00011273953,0.000034803194,0.000083623134,0.00009071494,0.0002174394,0.000007828544,0.00015957817,0.00012168598],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049350107,0.00002967932,0.98576427,0.00003058514,0.00012850303,0.00007968544,0.0012230977,0.0047659855,0.002507008,0.000009696371,0.00074812514,0.004664041],"study_design_scores_gemma":[0.00039091997,0.00006913901,0.9968678,0.00012755925,0.000042630596,0.000007763121,0.00021702345,0.0007442871,0.0003700597,0.0000754139,0.00087650283,0.00021090069],"about_ca_topic_score_codex":0.87488204,"about_ca_topic_score_gemma":0.9324948,"teacher_disagreement_score":0.0576128,"about_ca_system_score_codex":0.0000066691236,"about_ca_system_score_gemma":0.000097393575,"threshold_uncertainty_score":0.45973846},"labels":[],"label_agreement":null},{"id":"W3138733828","doi":"","title":"First-principles calculation of multi-phonon diffuse scattering in solids","year":2021,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Phonon; Brillouin zone; Scattering; Phonon scattering; Condensed matter physics; Diffraction; Intensity (physics); Crystal (programming language); Materials science; Physics; Optics; Computer science","score_opus":0.06963231801542216,"score_gpt":0.1842760032635213,"score_spread":0.11464368524809915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138733828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965124,0.00007118224,0.0022223396,0.000016319947,0.0005317513,0.00017438689,0.00009772464,0.000026463003,0.00034744205],"genre_scores_gemma":[0.9989903,0.00018297166,0.00033109795,0.000011826652,0.000056816312,1.9149059e-7,0.00021177442,0.000006018149,0.00020898085],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9988398,0.00009442037,0.00024405835,0.0005155997,0.00006929745,0.00023685637],"domain_scores_gemma":[0.9991779,0.000062000756,0.00020691747,0.00041548768,0.00005758641,0.000080124686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015969403,0.00019875506,0.00036789704,0.0001516911,0.000063935804,0.000053295968,0.0003463323,0.00019200309,0.00034264024],"category_scores_gemma":[0.00002025305,0.00022124391,0.000115271214,0.00020918605,0.00007132441,0.00016242627,0.0002116932,0.00018567096,0.000030553725],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025969302,0.000053043474,0.14278771,0.00018878016,0.000030170057,0.00009490219,0.0002751337,0.85605067,0.0002471689,0.00016315194,0.0000040848536,0.0000792083],"study_design_scores_gemma":[0.0005239579,0.000018418528,0.50955164,0.00020687674,0.0000459897,8.3855105e-7,0.000086015374,0.48815432,0.00065577915,0.0003518516,0.00012112439,0.00028319034],"about_ca_topic_score_codex":0.012336652,"about_ca_topic_score_gemma":0.012086462,"teacher_disagreement_score":0.36789638,"about_ca_system_score_codex":0.000014880683,"about_ca_system_score_gemma":0.00007430199,"threshold_uncertainty_score":0.9942403},"labels":[],"label_agreement":null},{"id":"W3155202518","doi":"10.1029/2021gl095413","title":"Structure and Stress Field of the Lithosphere Between Pamir and Tarim","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; Natural Environment Research Council; Sight Research UK","keywords":"Lithosphere; Geology; Slab; Induced seismicity; Seismology; Mantle (geology); Collision zone; Tarim basin; Stress field; Crust; Plateau (mathematics); Focal mechanism; Clockwise; Slab window; Geophysics; Subduction; Tectonics; Paleontology; Geometry","score_opus":0.01805791766745323,"score_gpt":0.2729232751220363,"score_spread":0.25486535745458305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3155202518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994824,0.0001738656,0.0000067349783,0.0041753515,0.00009984675,0.000105828374,0.00039625453,0.0000055843875,0.00021256175],"genre_scores_gemma":[0.99919516,0.00002730464,0.00010814152,0.00025556574,0.00026003807,6.83006e-7,0.000033068467,0.000002991992,0.00011702964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866194,0.00023268559,0.000119857534,0.00024925507,0.00042803204,0.00030825488],"domain_scores_gemma":[0.99894977,0.0005948306,0.000032150914,0.00024849866,0.000066232635,0.00010849686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015062289,0.00009058139,0.00018589402,0.000015742926,0.0001736927,0.000097465585,0.00019242136,0.00005484999,0.0003026404],"category_scores_gemma":[0.00012244537,0.000058402205,0.000034242352,0.00019837891,0.00025142977,0.00008909762,0.00012291248,0.00027720307,0.000007399318],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007304034,0.000037180245,0.8321775,0.00042843167,0.00015038057,0.00006290212,0.000943178,0.00010194182,0.110034436,0.00222378,0.0059165037,0.047850687],"study_design_scores_gemma":[0.00013994852,0.000060281804,0.9562147,0.000039195816,0.000012006245,0.0000012627229,0.00006472749,0.00006688723,0.038321745,0.0033192637,0.0016725803,0.00008735808],"about_ca_topic_score_codex":0.0032734526,"about_ca_topic_score_gemma":0.0003225202,"teacher_disagreement_score":0.1240372,"about_ca_system_score_codex":0.0000013147592,"about_ca_system_score_gemma":0.000041003885,"threshold_uncertainty_score":0.4948503},"labels":[],"label_agreement":null},{"id":"W3155750838","doi":"10.5194/egusphere-egu21-14473","title":"Slow subduction initiation drives fast mantle upwelling and lithosphere formation&amp;#160;","year":2021,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Subduction; Geology; Lithosphere; Mantle (geology); Slab; Plate tectonics; Eclogitization; Seismology; Tectonics; Geophysics; Oceanic crust","score_opus":0.019084567634425703,"score_gpt":0.2161739957684461,"score_spread":0.1970894281340204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3155750838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9796424,0.00071814546,0.008024594,0.00016705229,0.0013665549,0.00022308051,0.00011198294,0.00007897884,0.009667215],"genre_scores_gemma":[0.98901427,0.0009782175,0.005623959,0.00007186059,0.0004577639,0.000003837667,0.0026973034,0.0000060471466,0.0011467541],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9988926,0.000083307365,0.00029020023,0.00034000198,0.00020099343,0.00019287512],"domain_scores_gemma":[0.9993917,0.000043583957,0.00017000527,0.00022631725,0.000089964815,0.00007844651],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019272823,0.00019299157,0.0002553533,0.000042986074,0.00016551586,0.0005232463,0.00011301912,0.00018041205,0.0037372042],"category_scores_gemma":[0.000015345478,0.00017009978,0.000055182987,0.00006788823,0.000032422613,0.00046418214,0.000064889544,0.00016789872,0.00013811547],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047476665,0.00049398805,0.25912005,0.013407878,0.0014635276,0.00015266838,0.046458863,0.24981615,0.026721774,0.008858513,0.026193593,0.36683825],"study_design_scores_gemma":[0.0015824386,0.00020325149,0.7652853,0.0015055971,0.00062088884,0.00013280408,0.0057380493,0.08603037,0.025060626,0.036984347,0.07279729,0.0040590046],"about_ca_topic_score_codex":0.0016458787,"about_ca_topic_score_gemma":0.0016556383,"teacher_disagreement_score":0.50616527,"about_ca_system_score_codex":0.0000033614704,"about_ca_system_score_gemma":0.000045821977,"threshold_uncertainty_score":0.9971735},"labels":[],"label_agreement":null},{"id":"W3158795427","doi":"","title":"Investigating the lowermost mantle using migrations of long-period S-ScS data","year":2005,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Scattering; Slab; Core–mantle boundary; Discontinuity (linguistics); Mantle wedge; Transition zone; Geophysics; Seismology; Geometry; Subduction; Physics; Optics; Tectonics; Mathematical analysis","score_opus":0.05397915711092682,"score_gpt":0.262311514832599,"score_spread":0.2083323577216722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158795427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98177266,0.0000758592,0.0032921236,0.0010834729,0.000076009244,0.00036573867,0.0025167332,0.000024894714,0.010792524],"genre_scores_gemma":[0.98600954,0.00035018922,0.011918949,0.00001705887,0.00008233488,1.8271015e-8,0.00060331664,0.0000062661647,0.0010123178],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99788636,0.00040751958,0.00016570951,0.0004094367,0.00063088804,0.00050008047],"domain_scores_gemma":[0.99819136,0.00034819162,0.00019598688,0.00082583434,0.00022158041,0.00021703908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008743198,0.0001535874,0.00028890974,0.0002980605,0.0012280705,0.000048956488,0.0020916394,0.00007340054,0.0008949733],"category_scores_gemma":[0.0000797705,0.00015161127,0.000096761294,0.00069653906,0.00126353,0.0009241127,0.00071893237,0.00033398502,0.00001982778],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022308808,0.0011033454,0.66956323,0.0012029279,0.0018003035,0.00083305966,0.040419213,0.046934735,0.054766707,0.022462888,0.03692054,0.12176214],"study_design_scores_gemma":[0.0023084064,0.0006562927,0.37429452,0.0003179602,0.00029730648,0.000040567684,0.028935539,0.17513853,0.00091966346,0.0023874186,0.41385835,0.0008454352],"about_ca_topic_score_codex":0.009769578,"about_ca_topic_score_gemma":0.025548268,"teacher_disagreement_score":0.3769378,"about_ca_system_score_codex":0.000019523564,"about_ca_system_score_gemma":0.0003640057,"threshold_uncertainty_score":0.99682444},"labels":[],"label_agreement":null},{"id":"W3159126659","doi":"10.1093/gji/ggab169","title":"Optimal resolution tomography with error tracking and the structure of the crust and upper mantle beneath Ireland and Britain","year":2021,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Marine Institute; European Regional Development Fund; Geological Survey of Ireland; Science Foundation Ireland; Enterprise Ireland","keywords":"Tomography; Algorithm; Seismic tomography; Geodesy; Geology; Mathematics; Mantle (geology); Physics; Geophysics; Optics","score_opus":0.005485781677047991,"score_gpt":0.19784026916144792,"score_spread":0.19235448748439993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159126659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975927,0.00042023984,0.00006270162,0.0013361532,0.00022525921,0.000053624823,0.00012286632,0.000002430172,0.00018406044],"genre_scores_gemma":[0.9990448,0.00008580574,0.0004239027,0.00009622803,0.00026554312,1.7612291e-7,0.0000117595955,0.0000023541966,0.00006944384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99930406,0.000080255384,0.0001351547,0.0001252979,0.00024609387,0.00010914202],"domain_scores_gemma":[0.99959755,0.00009535128,0.000099823286,0.00006505889,0.000091975875,0.000050239778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011061519,0.0000821087,0.00013151,0.000022220594,0.0001995672,0.00018988563,0.000105387495,0.000030048202,0.00012294725],"category_scores_gemma":[0.000020278998,0.00004045706,0.000039758383,0.00006408272,0.00024816254,0.0001608924,0.0000366642,0.00015441004,4.842281e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036028938,0.00022490558,0.8063348,0.00017946675,0.0018710642,0.00023345782,0.00617835,0.014252021,0.04793163,0.05241668,0.0012620077,0.06551272],"study_design_scores_gemma":[0.0009671609,0.000058485875,0.98701215,0.00006120297,0.000057608722,0.00043976898,0.00018422793,0.003384655,0.0012671605,0.0057674083,0.00071126386,0.00008888626],"about_ca_topic_score_codex":0.00022607444,"about_ca_topic_score_gemma":0.00017137162,"teacher_disagreement_score":0.18067735,"about_ca_system_score_codex":0.000001282693,"about_ca_system_score_gemma":0.000023308563,"threshold_uncertainty_score":0.18310715},"labels":[],"label_agreement":null},{"id":"W3161147222","doi":"10.1103/physrevlett.126.196404","title":"Mechanisms for Pressure-Induced Isostructural Phase Transitions in EuO","year":2021,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Isostructural; Atomic orbital; Valence (chemistry); Condensed matter physics; Electronic structure; Valence electron; Atom (system on chip); Phase transition; Materials science; Density functional theory; Electronic band structure; Density of states; Crystallography; Crystal structure; Electron; Physics; Chemistry; Computational chemistry","score_opus":0.021075871225696197,"score_gpt":0.2873224847452358,"score_spread":0.2662466135195396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161147222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98176426,0.0028816285,0.0011741135,0.011850878,0.0005409604,0.0007916889,0.0007762167,0.000038352468,0.00018189613],"genre_scores_gemma":[0.99226743,0.00021658362,0.0006729245,0.0062603015,0.0001820856,0.000018066456,0.00036517275,0.000005417626,0.000012010387],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989912,0.00010152653,0.00020778237,0.00027478652,0.00015578403,0.00026893037],"domain_scores_gemma":[0.9995725,0.000077989534,0.0000532034,0.00018433975,0.000030305579,0.00008163475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001177752,0.0001400397,0.0003802683,0.00001774124,0.000064122774,0.000039296516,0.00013017486,0.000011848542,0.00050631264],"category_scores_gemma":[0.000029977962,0.000114739974,0.00015088884,0.00016372059,0.000018740704,0.00014812377,0.000006643246,0.000081313075,0.000070419905],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005018765,0.00017147187,0.00002732846,0.0017343449,0.00009446129,0.000055864024,0.0003284584,0.000987563,0.9718345,0.0041362015,0.0031429688,0.017436646],"study_design_scores_gemma":[0.020857103,0.002394583,0.046334285,0.0099089565,0.0043813693,0.00014819743,0.00022403483,0.10560295,0.3104981,0.10489053,0.387668,0.0070919003],"about_ca_topic_score_codex":0.0000903513,"about_ca_topic_score_gemma":0.00006820708,"teacher_disagreement_score":0.6613364,"about_ca_system_score_codex":0.0000017826017,"about_ca_system_score_gemma":0.00002687615,"threshold_uncertainty_score":0.55437684},"labels":[],"label_agreement":null},{"id":"W3161171435","doi":"10.1103/physreve.104.015201","title":"Ionization of carbon at 10–100 times the diamond density and in the<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"><mml:msup><mml:mrow><mml:mn>10</mml:mn></mml:mrow><mml:mn>6</mml:mn></mml:msup></mml:math> K temperature range","year":2021,"lang":"lv","type":"article","venue":"Physical review. E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Ionization; Ion; Density functional theory; Atom (system on chip); Coulomb; Atomic physics; Physics; Electron; Materials science; Quantum mechanics","score_opus":0.013986863423686895,"score_gpt":0.23716613330112482,"score_spread":0.2231792698774379,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161171435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94425875,0.011393193,0.000009468068,0.001216536,0.0008649986,0.00009875037,0.00052338396,0.000046184603,0.041588705],"genre_scores_gemma":[0.9856235,0.009893508,0.00013247896,0.000959215,0.001306512,0.00013521865,0.0014006434,0.00009306249,0.0004558772],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99536777,0.0006665755,0.00085130264,0.0009393043,0.0012584537,0.0009166109],"domain_scores_gemma":[0.9963921,0.0011135975,0.0007849304,0.001230595,0.00014712948,0.00033167677],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011793872,0.0005069349,0.00045754295,0.000080265796,0.00071502797,0.0005682099,0.000878967,0.0005430057,0.022608133],"category_scores_gemma":[0.0007734001,0.00055763504,0.00065061194,0.0007517284,0.0006521797,0.00052430294,0.0005460864,0.00065128144,0.0009967142],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00077288545,0.00047824398,0.00014361073,0.0048268037,0.0008580296,0.00081369583,0.0038541486,0.00060774584,0.012297808,0.8570279,0.11458471,0.003734448],"study_design_scores_gemma":[0.0017193434,0.0014302555,0.0031727494,0.003766097,0.0027983666,0.0005632126,0.00089787296,0.14246354,0.7861874,0.00060582766,0.054506496,0.0018888103],"about_ca_topic_score_codex":0.000931989,"about_ca_topic_score_gemma":0.0008326769,"teacher_disagreement_score":0.85642207,"about_ca_system_score_codex":0.000005156469,"about_ca_system_score_gemma":0.000440682,"threshold_uncertainty_score":0.99978113},"labels":[],"label_agreement":null},{"id":"W3163818932","doi":"10.3390/cryst11080875","title":"Thermal Convection in the Core of Ganymede Inferred from Liquid Eutectic Fe-FeS Electrical Resistivity at High Pressures","year":2021,"lang":"en","type":"article","venue":"Crystals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Eutectic system; Electrical resistivity and conductivity; Materials science; Thermal; Thermal conductivity; Convection; Thermodynamics; Core (optical fiber); Inner core; Composite material; Physics; Microstructure","score_opus":0.018548386115495256,"score_gpt":0.2237946467475005,"score_spread":0.20524626063200524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3163818932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972874,0.00088774675,0.000014311508,0.00017501575,0.0003121113,0.00015392201,0.00028550482,0.00001919602,0.00086482713],"genre_scores_gemma":[0.9992486,0.0000501495,0.000035606845,0.000090876405,0.00017578468,0.0000036175652,0.00018732369,0.000003861133,0.0002041644],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986765,0.00034495365,0.0002478085,0.0002409438,0.00026442303,0.00022540081],"domain_scores_gemma":[0.99898404,0.00053573644,0.00011642248,0.00026620165,0.00005425393,0.00004333377],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032836758,0.00012030825,0.00027126746,0.000034104778,0.0001094778,0.000054314,0.00017007155,0.000087354165,0.0013370267],"category_scores_gemma":[0.00015668162,0.000083406536,0.000054032145,0.00020785055,0.00007582359,0.000106643376,0.000028423943,0.00010272109,0.00002645904],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015079146,0.00018439643,0.047690157,0.00010058019,0.0001490098,0.00017582091,0.0017584662,0.002219557,0.93993694,0.00043345112,0.0028267808,0.0030169126],"study_design_scores_gemma":[0.0003158434,0.0001544871,0.9142066,0.000025280498,0.000044946948,0.000004305067,0.000046904108,0.00022055923,0.08028905,0.001300329,0.0032565023,0.0001351908],"about_ca_topic_score_codex":0.005717258,"about_ca_topic_score_gemma":0.0046342122,"teacher_disagreement_score":0.8665165,"about_ca_system_score_codex":0.0000044188573,"about_ca_system_score_gemma":0.00006539412,"threshold_uncertainty_score":0.9995759},"labels":[],"label_agreement":null},{"id":"W3164473332","doi":"","title":"The deep lithospheric structure of the Namibian volcanic margin","year":2010,"lang":"en","type":"article","venue":"EGU General Assembly Conference Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Lithosphere; Geophysics; Mantle (geology); Continental margin; Volcano; Geoid; Transition zone; Crust; Petrology; Seismology; Tectonics; Measured depth","score_opus":0.006583473789848935,"score_gpt":0.19720451726330213,"score_spread":0.19062104347345318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3164473332","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930609,0.000081485356,0.000008599921,0.0005750774,0.0024287417,0.00019685403,0.00009209873,0.00002021729,0.003536024],"genre_scores_gemma":[0.9982068,0.000025045161,0.0003688332,0.000108418906,0.0004069534,0.0000010936303,0.000028323582,0.0000059555323,0.0008485555],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99859625,0.00008108182,0.000328565,0.00025046192,0.00034727762,0.00039633326],"domain_scores_gemma":[0.9988668,0.000110921166,0.00026255683,0.0005248981,0.00012093715,0.000113896655],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024146559,0.00019225365,0.00020281193,0.000012292342,0.00034514887,0.00023258546,0.00081427704,0.00012481093,0.0011811943],"category_scores_gemma":[0.000066947025,0.00009990997,0.000081654696,0.00015167943,0.00015592374,0.00016045182,0.00004242944,0.00031051942,0.000072542214],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050630162,0.000032368833,0.032638054,0.00003854773,0.00007900196,0.000008488025,0.00042118743,0.0051317527,0.9056285,0.007216219,0.0013619136,0.04739335],"study_design_scores_gemma":[0.0001264661,0.00003791347,0.9414069,0.000010078671,0.000018875797,0.0000068014197,0.00004043159,0.0010850448,0.04086126,0.0037733621,0.012454452,0.000178399],"about_ca_topic_score_codex":0.0034732837,"about_ca_topic_score_gemma":0.048100296,"teacher_disagreement_score":0.90876883,"about_ca_system_score_codex":0.0000019090157,"about_ca_system_score_gemma":0.00017354666,"threshold_uncertainty_score":0.99973184},"labels":[],"label_agreement":null},{"id":"W3164484349","doi":"10.1029/2020av000304","title":"Slab Transport of Fluids to Deep Focus Earthquake Depths—Thermal Modeling Constraints and Evidence From Diamonds","year":2021,"lang":"en","type":"article","venue":"AGU Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Carnegie Institution for Science; University of Alberta; National Science Foundation","keywords":"Geology; Subduction; Mantle (geology); Transition zone; Slab; Deep-focus earthquake; Geophysics; Seismology; Tectonics; Petrology","score_opus":0.014690556903699442,"score_gpt":0.22495975822937514,"score_spread":0.2102692013256757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3164484349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98289114,0.012219769,0.0036810176,0.00010402436,0.00026527856,0.0000858793,0.00017827332,0.000017584982,0.00055705156],"genre_scores_gemma":[0.99451774,0.0007048567,0.004554706,0.000058087782,0.00010217196,0.0000016119851,0.000033237175,0.0000037147993,0.000023850806],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99901354,0.00004598882,0.00023989753,0.00029529035,0.00019407555,0.00021119737],"domain_scores_gemma":[0.9994589,0.00014680772,0.000047664602,0.00016290172,0.000063088424,0.00012064474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001234193,0.00012259779,0.00025643164,0.000024155206,0.00006804597,0.000028893808,0.00012384266,0.000042820313,0.00078315847],"category_scores_gemma":[0.000038760518,0.000106393345,0.00003935852,0.00011209381,0.00008326383,0.00036316155,0.000011676796,0.000048783568,0.0000296357],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016450336,0.00003258072,0.29083267,0.00012441703,0.00008251776,0.0001432394,0.0021541943,0.08511799,0.1230878,0.00014379255,0.000011817444,0.49810445],"study_design_scores_gemma":[0.0008867919,0.00036983844,0.81387603,0.0006605803,0.00016743795,0.000016000413,0.000920928,0.01700708,0.15768361,0.0056831795,0.0018070886,0.0009214476],"about_ca_topic_score_codex":0.0020567528,"about_ca_topic_score_gemma":0.0055629387,"teacher_disagreement_score":0.52304333,"about_ca_system_score_codex":7.9020623e-7,"about_ca_system_score_gemma":0.000045312067,"threshold_uncertainty_score":0.8575036},"labels":[],"label_agreement":null},{"id":"W3164933742","doi":"10.5194/egusphere-egu2020-3286","title":"Imaging Hales Discontinuity beneath India: Seismological and Petrological Model","year":2020,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Peridotite; Eclogite; Receiver function; Dharwar Craton; Seismology; Discontinuity (linguistics); Shield; Subduction; Geochemistry; Mineralogy; Craton; Geophysics; Lithosphere; Petrology; Tectonics","score_opus":0.018676875811364804,"score_gpt":0.20335496918127152,"score_spread":0.1846780933699067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3164933742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883389,0.0001324165,0.0026100054,0.002759641,0.000055697208,0.00007532143,0.00009931609,0.00006833905,0.0058603818],"genre_scores_gemma":[0.995535,0.00002321416,0.0019576757,0.0022337977,0.000113330534,6.050314e-7,0.000037516893,0.0000015228381,0.00009732772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992712,0.00003882509,0.00011942479,0.00025704346,0.00010407265,0.00020940547],"domain_scores_gemma":[0.9996899,0.00004515092,0.000029023557,0.00006399908,0.0000097352595,0.00016220023],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000100563615,0.00010440585,0.00018238217,0.000009980563,0.000089965855,0.00009479782,0.00011546236,0.000040970168,0.0010005205],"category_scores_gemma":[0.00002441939,0.000065113534,0.000029260187,0.00003933895,0.000083425395,0.00013360723,0.000040046067,0.00007686545,0.00006656465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012574402,0.000036019504,0.9538026,0.00003532543,0.00003164313,0.00015513504,0.00065054477,0.0086590275,0.001739463,0.009867726,0.0021902197,0.022706548],"study_design_scores_gemma":[0.00029179102,0.00012438666,0.6790621,0.0000028359495,0.000021771044,0.000011463685,0.00007052731,0.30934832,0.00019550092,0.008526272,0.0020970474,0.00024793934],"about_ca_topic_score_codex":0.0003053658,"about_ca_topic_score_gemma":0.000028703633,"teacher_disagreement_score":0.3006893,"about_ca_system_score_codex":4.1339408e-7,"about_ca_system_score_gemma":0.000010618398,"threshold_uncertainty_score":0.9999127},"labels":[],"label_agreement":null},{"id":"W3165222628","doi":"","title":"Structure of Canadian Lithosphere and Uppermost Mantle from P and S Receiver Functions","year":2016,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Geology; Mantle (geology); Receiver function; Geophysics; Seismology; Tectonics","score_opus":0.008310318326381275,"score_gpt":0.17695218677902608,"score_spread":0.1686418684526448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3165222628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992651,0.00026123755,4.69762e-7,0.00030521446,0.00025858812,0.000055418644,0.0011096668,0.000010956797,0.0053474596],"genre_scores_gemma":[0.99904794,0.00010657308,0.00036281487,0.000052117695,0.00010223012,1.475331e-7,0.000046394314,0.000003258531,0.00027852447],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993997,0.000022472805,0.00013857722,0.00017878498,0.000080563135,0.00017985133],"domain_scores_gemma":[0.999496,0.0001319255,0.00007124967,0.000103896644,0.000027558941,0.00016941206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007175763,0.00008831683,0.00012580003,0.000040338113,0.000101953476,0.0000380219,0.00006052646,0.00006843509,0.0002614119],"category_scores_gemma":[0.000049745,0.00005893326,0.000011842475,0.000057048277,0.000056268145,0.0001073415,0.000007660402,0.000041044947,0.000034430806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023870643,0.00000463639,0.9356633,0.000028983592,0.000045754856,0.000016561775,0.0003540608,0.0001372315,0.0400663,0.00002800472,0.0017637569,0.02186758],"study_design_scores_gemma":[0.0001336713,0.000024511522,0.9871554,0.00006977544,0.000018013812,0.0000029001942,0.00005069889,0.000008413702,0.0020188207,0.00049259193,0.009929055,0.000096141965],"about_ca_topic_score_codex":0.81292236,"about_ca_topic_score_gemma":0.83404535,"teacher_disagreement_score":0.05149215,"about_ca_system_score_codex":0.0000014931541,"about_ca_system_score_gemma":0.00003537361,"threshold_uncertainty_score":0.28622767},"labels":[],"label_agreement":null},{"id":"W3166281285","doi":"10.1116/6.0001074","title":"Zirconia-titania-doped tantala optical coatings for low mechanical loss Bragg mirrors","year":2021,"lang":"en","type":"article","venue":"Journal of Vacuum Science & Technology A Vacuum Surfaces and Films","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal; Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; California Institute of Technology; Fonds de recherche du Québec – Nature et technologies; Massachusetts Institute of Technology; Canada Foundation for Innovation; Polytechnique Montréal; Fonds Québécois de la Recherche sur la Nature et les Technologies; Gordon and Betty Moore Foundation; National Science Foundation","keywords":"Materials science; Cubic zirconia; Amorphous solid; Thin film; Crystallization; Dissipation factor; Composite material; Refractive index; Annealing (glass); Sputtering; Optoelectronics; Optics; Dielectric; Ceramic; Nanotechnology; Chemical engineering","score_opus":0.011116588991459328,"score_gpt":0.24150819711615232,"score_spread":0.230391608124693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3166281285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99423885,0.0006708615,0.00066658785,0.0028823265,0.0010709533,0.00018206418,0.000105161555,0.00004267352,0.00014051555],"genre_scores_gemma":[0.9772098,0.000300751,0.022118015,0.00015664504,0.00006724883,0.0000018556759,0.000005925424,0.0000083969435,0.00013137654],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9975137,0.00004334865,0.0007063516,0.00050139223,0.00053227326,0.00070290506],"domain_scores_gemma":[0.99821866,0.00023164332,0.0004523236,0.00029028708,0.0005152479,0.00029184207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001280116,0.0002570393,0.00064821553,0.0003186312,0.0005303472,0.0002604768,0.0007760143,0.00026528057,0.00038771855],"category_scores_gemma":[0.00028674022,0.00019526984,0.00013927386,0.0010717385,0.00089071586,0.0006435106,0.00013073816,0.0003642545,0.00002364272],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016779263,0.00014215292,0.01790595,0.00008037964,0.00007280066,0.00037336198,0.0001901538,0.000119234195,0.9680505,0.008301084,0.00039365832,0.004202979],"study_design_scores_gemma":[0.0027600112,0.002506668,0.028889474,0.000309011,0.00024229194,0.0025539808,0.00199971,0.0062243934,0.91293466,0.030467916,0.010091694,0.0010201877],"about_ca_topic_score_codex":0.000047639704,"about_ca_topic_score_gemma":0.0000837394,"teacher_disagreement_score":0.055115793,"about_ca_system_score_codex":0.000009386048,"about_ca_system_score_gemma":0.0004292469,"threshold_uncertainty_score":0.79628724},"labels":[],"label_agreement":null},{"id":"W3166730921","doi":"10.1063/5.0048141","title":"57Fe Mössbauer isomer shift of pure iron and iron oxides at high pressure—An experimental and theoretical study","year":2021,"lang":"en","type":"article","venue":"The Journal of Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Mössbauer spectroscopy; Density functional theory; Iron oxide; Chemistry; Synchrotron; Wüstite; Oxide; Oxygen; Materials science; Analytical Chemistry (journal); Crystallography; Computational chemistry; Metallurgy; Physics","score_opus":0.007597752319516053,"score_gpt":0.2212309090652065,"score_spread":0.21363315674569044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3166730921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984951,0.0010080511,0.0000064944834,0.00013222027,0.000112725524,0.000080228296,0.000033132656,0.0000035058167,0.00012853215],"genre_scores_gemma":[0.9994973,0.00004045551,0.00008068914,0.000050511222,0.0003008016,2.5248983e-7,0.0000081937,0.0000054395364,0.000016340437],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989805,0.00016003713,0.00026639574,0.00012602474,0.00031457242,0.00015243738],"domain_scores_gemma":[0.99933994,0.00016250505,0.0001652672,0.00016369825,0.000050162973,0.00011841028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026488482,0.00012968348,0.00030914013,0.000009427052,0.000061582745,0.000038940325,0.00016433587,0.000047113383,0.0004340409],"category_scores_gemma":[0.0000152032935,0.000078520934,0.00004119104,0.00004944402,0.00028462667,0.0001760289,0.00007109721,0.00013462659,0.0000028050456],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000488467,0.00038664014,0.0072522787,0.00005671696,0.00009937254,0.000016326294,0.0034156337,0.00015821047,0.98430943,0.0029637155,0.00016279846,0.0006903757],"study_design_scores_gemma":[0.0010595411,0.00068699446,0.023740433,0.000034490302,0.000342966,0.00004801305,0.0009741908,0.00011291556,0.95146286,0.02120926,0.000117064956,0.00021126759],"about_ca_topic_score_codex":0.00004552802,"about_ca_topic_score_gemma":0.0000042449433,"teacher_disagreement_score":0.0328466,"about_ca_system_score_codex":0.000001951495,"about_ca_system_score_gemma":0.000018408033,"threshold_uncertainty_score":0.47524437},"labels":[],"label_agreement":null},{"id":"W3168239742","doi":"10.3390/min11060607","title":"Compressibility and Phase Stability of Iron-Rich Ankerite","year":2021,"lang":"en","type":"article","venue":"Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministerio de Ciencia e Innovación; Generalitat Valenciana; Ministerio de Economía y Competitividad; Compute Canada; Yale University","keywords":"Ankerite; Dolomite; Bulk modulus; Phase (matter); Crystallography; Chemistry; Materials science; Thermodynamics; Mineralogy; Physics; Calcite","score_opus":0.02379151407556675,"score_gpt":0.2530194027308573,"score_spread":0.22922788865529056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3168239742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955865,0.0005773207,0.000010913697,0.000088283,0.0001662599,0.00008019605,0.00055005145,0.000011819528,0.002928645],"genre_scores_gemma":[0.99899745,0.000028157043,0.00055287906,0.000048367867,0.00005876312,5.6675225e-7,0.00013106642,0.0000014848725,0.00018127644],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99919766,0.000109688604,0.00021140184,0.00022108671,0.000118399104,0.00014174715],"domain_scores_gemma":[0.999477,0.000090947986,0.00005897608,0.00023785749,0.000063634136,0.00007156341],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023666756,0.000081740814,0.000229646,0.000011831704,0.000043386266,0.000032349344,0.00006759879,0.00003416669,0.0038453718],"category_scores_gemma":[0.0000452311,0.00006629035,0.000026861122,0.00008062951,0.00007989925,0.000101133825,0.00002077245,0.000035348086,0.000012944541],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006456352,0.00016324746,0.08796449,0.00019494636,0.000020425343,0.00001793068,0.00037744557,0.00006230842,0.9053486,0.00014120959,0.00089412235,0.004750718],"study_design_scores_gemma":[0.001960786,0.00027556263,0.48829657,0.00003779931,0.00006465919,0.0000120219975,0.0001410945,0.0016065717,0.4842316,0.0029169237,0.020038046,0.0004183617],"about_ca_topic_score_codex":0.00090731954,"about_ca_topic_score_gemma":0.00032067453,"teacher_disagreement_score":0.42111698,"about_ca_system_score_codex":6.8511105e-7,"about_ca_system_score_gemma":0.000026457948,"threshold_uncertainty_score":0.99706525},"labels":[],"label_agreement":null},{"id":"W3171082020","doi":"10.5194/egusphere-egu21-14987","title":"Radially and azimuthally anisotropic shear-wave velocity model of the Earth&amp;#8217;s upper mantle","year":2021,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Anisotropy; Azimuth; Lithosphere; Physics; Geometry; Geology; Seismology; Optics; Mathematics","score_opus":0.023855590581662412,"score_gpt":0.19932130233052026,"score_spread":0.17546571174885783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3171082020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98521006,0.00017281993,0.00045150478,0.00041484283,0.0002896842,0.00009590056,0.00015828293,0.000015030534,0.0131918965],"genre_scores_gemma":[0.98948574,0.00008519553,0.0055824057,0.00025865517,0.000071674935,4.437698e-7,0.000025036888,0.000003408451,0.0044874153],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99917066,0.00006949378,0.00016776241,0.00020380496,0.0001944653,0.0001938343],"domain_scores_gemma":[0.9995209,0.000047958572,0.000048622984,0.00025594467,0.000054756652,0.00007184444],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000118225245,0.00010224828,0.0001838898,0.000014415438,0.00011420048,0.000057604662,0.00011467833,0.00005800203,0.0023044758],"category_scores_gemma":[0.000021857213,0.00006629683,0.000055625733,0.000085732645,0.000080963255,0.00010030923,0.00004594078,0.00006330236,0.00005994801],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039832288,0.00046042452,0.30251065,0.00087963865,0.000714336,0.00010193818,0.006188357,0.07788119,0.44068345,0.097840615,0.013625132,0.05871596],"study_design_scores_gemma":[0.0008339132,0.00009186997,0.8836148,0.00004317196,0.00008997241,0.00003626076,0.00011290519,0.040015515,0.038524758,0.020721799,0.015425706,0.00048935716],"about_ca_topic_score_codex":0.0010537055,"about_ca_topic_score_gemma":0.0019135876,"teacher_disagreement_score":0.5811041,"about_ca_system_score_codex":7.802281e-7,"about_ca_system_score_gemma":0.00011221115,"threshold_uncertainty_score":0.9986076},"labels":[],"label_agreement":null},{"id":"W3175448650","doi":"10.5194/egusphere-egu21-6456","title":"Thermochemical structure of the lithosphere and upper mantle beneath Superior craton: Results from multi-observable probabilistic inversion","year":2021,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"De Beers (Canada); Université du Québec à Montréal","funders":"","keywords":"Craton; Lithosphere; Geology; Archean; Rift; Mantle (geology); Proterozoic; Dharwar Craton; Seismology; Geophysics; Petrology; Tectonics; Geochemistry","score_opus":0.011207494651400978,"score_gpt":0.18710419809097484,"score_spread":0.17589670343957386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175448650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976679,0.0002568323,0.0000027297776,0.00022886835,0.00022970243,0.00011238483,0.000814298,0.00001117791,0.00067609845],"genre_scores_gemma":[0.9967316,0.00002568819,0.002230346,0.000106795305,0.000058437403,2.2563896e-7,0.00018309112,0.0000029198409,0.0006609315],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99922734,0.00006046635,0.00017459813,0.00025375592,0.00014452903,0.00013932453],"domain_scores_gemma":[0.9994826,0.00008642273,0.00004855588,0.00027274914,0.000051368224,0.000058339683],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000049172617,0.00010289594,0.00016892118,0.000004021538,0.00009194927,0.000051536288,0.00014425901,0.00008067841,0.0033604838],"category_scores_gemma":[0.000060481492,0.000058571,0.00003716287,0.00008077883,0.00007665898,0.00008186168,0.000052267864,0.00006608494,0.00001070042],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023382764,0.00006878221,0.21156256,0.00013360335,0.00008205462,0.000018864042,0.0014794298,0.0006532325,0.7803679,0.00038288286,0.0018459023,0.003170927],"study_design_scores_gemma":[0.0008998932,0.000038043505,0.58879334,0.000066612345,0.000053999327,0.0000042033785,0.0003226905,0.004164591,0.40010253,0.0024356407,0.0029063488,0.00021210045],"about_ca_topic_score_codex":0.0041361246,"about_ca_topic_score_gemma":0.0024185374,"teacher_disagreement_score":0.3802654,"about_ca_system_score_codex":0.0000013378929,"about_ca_system_score_gemma":0.00004931339,"threshold_uncertainty_score":0.9975506},"labels":[],"label_agreement":null},{"id":"W3175484569","doi":"10.1016/j.epsl.2021.117053","title":"Adiabatic heat flow in Mercury's core from electrical resistivity measurements of liquid Fe-8.5 wt%Si to 24 GPa","year":2021,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Inner core; Adiabatic process; Convection; Thermal conductivity; Thermal; Materials science; Core–mantle boundary; Thermodynamics; Mercury (programming language); Phase boundary; Melting point; Geophysics; Geology; Mineralogy; Mantle (geology); Phase (matter); Composite material; Chemistry; Physics","score_opus":0.02200272820934462,"score_gpt":0.2078463654449925,"score_spread":0.18584363723564787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175484569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964993,0.0004811656,0.00002526379,0.0014458803,0.0005940023,0.00017498319,0.0004554209,0.000014514052,0.00030947372],"genre_scores_gemma":[0.9944743,0.000056490375,0.0027781583,0.0021989367,0.00011831435,9.989692e-7,0.0003474551,0.000003111551,0.000022218022],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978232,0.00013381576,0.0002992871,0.00055597414,0.00065274193,0.00053497375],"domain_scores_gemma":[0.9991275,0.00018415676,0.000051585375,0.00027628447,0.000045215147,0.00031523657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006214335,0.00018494861,0.00035263126,0.000162263,0.00016309737,0.00009735737,0.00029404653,0.000052954234,0.00086021307],"category_scores_gemma":[0.00014103942,0.0001643323,0.000032453197,0.00074954965,0.00019882568,0.00030110218,0.000029714587,0.00014666356,0.00008232437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004330435,0.000053703567,0.4987097,0.000043498167,0.00003770928,0.00025341962,0.0005849265,0.013458286,0.47153237,0.000007613448,0.0018068717,0.013078852],"study_design_scores_gemma":[0.000318457,0.00021792883,0.97511524,0.000050800918,0.000020092895,0.000009812827,0.000014980362,0.0033457847,0.017885583,0.00004532969,0.0027091983,0.00026677907],"about_ca_topic_score_codex":0.0066417316,"about_ca_topic_score_gemma":0.0062021296,"teacher_disagreement_score":0.47640556,"about_ca_system_score_codex":0.0000039975766,"about_ca_system_score_gemma":0.00015104153,"threshold_uncertainty_score":0.9999731},"labels":[],"label_agreement":null},{"id":"W3184973091","doi":"10.1126/science.abf8966","title":"Thickness and structure of the martian crust from InSight seismic data","year":2021,"lang":"en","type":"article","venue":"Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":271,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Space Agency; Institut Universitaire de France; Centre National de la Recherche Scientifique; Institut de Physique du Globe de Paris; Max-Planck-Gesellschaft; Nuclear Safety and Security Commission; Eidgenössische Technische Hochschule Zürich; H2020 Marie Skłodowska-Curie Actions; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Deutsches Zentrum für Luft- und Raumfahrt; Jet Propulsion Laboratory; Centre National d’Etudes Spatiales; Bundesministerium für Bildung und Forschung; National Aeronautics and Space Administration; Branco Weiss Fellowship – Society in Science; California Institute of Technology; European Commission; Agence Nationale de la Recherche; Belgian Federal Science Policy Office; National Science Foundation; European Space Agency; Staatssekretariat für Bildung, Forschung und Innovation; David and Lucile Packard Foundation; UK Space Agency","keywords":"Martian; Crust; Geology; Astrobiology; Geophysics; Earth science; Mars Exploration Program; Seismology; Physics","score_opus":0.01467982897155001,"score_gpt":0.21182998706917255,"score_spread":0.19715015809762254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184973091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996817,0.0003765187,0.000020818377,0.00030879237,0.0007766564,0.000040125822,0.0009994145,0.0000047795183,0.00065589935],"genre_scores_gemma":[0.9991768,0.000016705337,0.0004265057,0.00021359809,0.00006164944,3.563083e-8,0.00004544215,8.364392e-7,0.000058449146],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9992002,0.000040844705,0.00009067488,0.00027554645,0.00026033007,0.00013234954],"domain_scores_gemma":[0.9992463,0.000041407417,0.000049335118,0.0005679607,0.00004437321,0.0000506034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015094936,0.000053704367,0.000088419445,0.000013155382,0.00018874352,0.00010785574,0.00069112994,0.000023030869,0.000684825],"category_scores_gemma":[0.000066801345,0.000031871954,0.000008172281,0.00029691178,0.00039224912,0.00030956152,0.00019344664,0.00005110353,0.0000091587035],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020667676,0.00001800183,0.14291295,0.000049774655,0.000021044674,0.000018337361,0.0019770311,0.0016416367,0.82433254,0.00088191853,0.00070725096,0.027418861],"study_design_scores_gemma":[0.00009659267,0.000011282297,0.898849,0.000024667452,0.00001547177,0.000007620824,0.00012318196,0.0062203305,0.07504799,0.0063329744,0.013164542,0.00010632662],"about_ca_topic_score_codex":0.001161476,"about_ca_topic_score_gemma":0.0015636145,"teacher_disagreement_score":0.7559361,"about_ca_system_score_codex":5.998852e-7,"about_ca_system_score_gemma":0.00018069711,"threshold_uncertainty_score":0.7498354},"labels":[],"label_agreement":null},{"id":"W3187426502","doi":"10.1029/2021gl095075","title":"Coupling Between Lithosphere Removal and Mantle Flow in the Central Andes","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"ExxonMobil Research and Engineering Company; National Natural Science Foundation of China","keywords":"Lithosphere; Geology; Magmatism; Crust; Mantle (geology); Subduction; Geophysics; Lithospheric flexure; Seismology; Tectonics","score_opus":0.03658094016581815,"score_gpt":0.28593971049661465,"score_spread":0.2493587703307965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3187426502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942211,0.00024023246,0.000025105539,0.0043014484,0.00010922976,0.00014012479,0.00006477033,0.000011600145,0.00088638277],"genre_scores_gemma":[0.9984285,0.00006180028,0.00037550787,0.0002756828,0.00067460426,0.0000023798038,0.00008455149,0.000004263403,0.00009266183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979696,0.00026701036,0.00014981114,0.00032385008,0.0006076447,0.00068205607],"domain_scores_gemma":[0.99887127,0.0007033143,0.000019598216,0.00023610567,0.000042685602,0.00012701777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069450744,0.000108642125,0.00019320045,0.000029942614,0.00022638078,0.00028218084,0.00025845427,0.000045195266,0.00044141518],"category_scores_gemma":[0.0001010264,0.000074735646,0.00004242368,0.0003406108,0.00018938542,0.00014611852,0.000053328662,0.0003424842,0.00012372981],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049611606,0.00040061076,0.648652,0.0006918284,0.00031136218,0.008062928,0.00877692,0.0094258785,0.090700515,0.0044359323,0.03251654,0.19552937],"study_design_scores_gemma":[0.00028438235,0.00005296137,0.98496914,0.000029433608,0.000008663413,0.000008483053,0.00028558553,0.0038030406,0.0007578122,0.0015217094,0.008133378,0.00014540086],"about_ca_topic_score_codex":0.0029451633,"about_ca_topic_score_gemma":0.00042135018,"teacher_disagreement_score":0.33631715,"about_ca_system_score_codex":0.000004349701,"about_ca_system_score_gemma":0.00005198009,"threshold_uncertainty_score":0.48331866},"labels":[],"label_agreement":null},{"id":"W3188290860","doi":"10.1029/2021gc009910","title":"Focused Penetrative Plumes: A Possible Consequence of the Dissociation Transition of Post‐Perovskite at ∼0.9 TPa in Massive Rocky Super‐Earths","year":2021,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Compute Canada","keywords":"Mantle (geology); Mantle convection; Geology; Transition zone; Planet; Volcanism; Geophysics; Silicate; Convection; Mantle plume; Petrology; Tectonics; Geochemistry; Thermodynamics; Subduction; Lithosphere; Physics; Seismology","score_opus":0.006288600122603728,"score_gpt":0.1867905427611574,"score_spread":0.18050194263855365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3188290860","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956753,0.00032079514,0.000014588855,0.00017885023,0.00027102136,0.0002861267,0.0019387518,0.000013208325,0.0013013182],"genre_scores_gemma":[0.998798,0.00002950811,0.00003909075,0.000028944252,0.00010716534,0.000007471924,0.0006036859,0.0000066766656,0.0003794327],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99809504,0.00019719344,0.0005513199,0.0003711296,0.0004559181,0.00032941953],"domain_scores_gemma":[0.9985509,0.00018153533,0.00040831472,0.00041358924,0.0003751754,0.000070466805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021576625,0.00021930043,0.00048030232,0.000027058551,0.00012755423,0.000040416948,0.0002595096,0.00014815004,0.0003766523],"category_scores_gemma":[0.000069713016,0.00018199436,0.00017219436,0.00042400014,0.00012514992,0.00018613462,0.000037595928,0.0001345491,0.000022660535],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000092539514,0.00009087135,0.01646106,0.00063981774,0.00008359487,0.00003817594,0.0026821443,0.0035089394,0.9759317,0.000079103374,0.000042950767,0.0003490795],"study_design_scores_gemma":[0.0009205812,0.000092661576,0.15049425,0.00051298604,0.000071295,0.000023736371,0.0014945591,0.0018232759,0.84242195,0.00170281,0.000086538195,0.00035535175],"about_ca_topic_score_codex":0.0054860166,"about_ca_topic_score_gemma":0.0023969081,"teacher_disagreement_score":0.13403319,"about_ca_system_score_codex":0.000023224622,"about_ca_system_score_gemma":0.0003055907,"threshold_uncertainty_score":0.8293253},"labels":[],"label_agreement":null},{"id":"W3192719259","doi":"10.20944/preprints202108.0231.v1","title":"Thermobarometry of Diamond Inclusions: Evidence Mantle Evolution beneath Siberian Craton and Archean Cratons Worldwide.","year":2021,"lang":"en","type":"preprint","venue":"Preprints.org","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Science and Higher Education of the Russian Federation; Siberian Branch, Russian Academy of Sciences; Russian Foundation for Basic Research","keywords":"Craton; Kimberlite; Geology; Eclogite; Geochemistry; Archean; Mantle (geology); Lithosphere; Mantle plume; Earth science; Subduction; Tectonics; Paleontology","score_opus":0.07846285186770857,"score_gpt":0.3017556904081156,"score_spread":0.22329283854040705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3192719259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99240786,0.0033589778,0.0000862203,0.00023654131,0.0008727845,0.0005238182,0.00029729705,0.000059856186,0.0021566679],"genre_scores_gemma":[0.99747974,0.0012938504,0.00043291214,0.000047344514,0.00019831023,0.000015116312,0.00020760924,0.000015309948,0.00030980643],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970518,0.00040931476,0.0006331388,0.0010010224,0.000492208,0.0004125391],"domain_scores_gemma":[0.9977306,0.00032569224,0.00042642994,0.001121489,0.00016367492,0.00023208017],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010987476,0.0003833425,0.0006906402,0.0001984191,0.00022574546,0.000089515335,0.0006393807,0.00030190012,0.0037602284],"category_scores_gemma":[0.00037393326,0.00035505698,0.00016056004,0.0002851894,0.0002194048,0.00028197045,0.0014064893,0.000482667,0.00016791873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000064544576,0.00007432607,0.939999,0.00055551063,0.00013344277,0.000026461932,0.0011968173,0.0011935919,0.054728236,0.00015192958,0.000024171537,0.0018519765],"study_design_scores_gemma":[0.00013219252,0.0000298549,0.96613175,0.0007893037,0.00010298252,0.0000056950585,0.00016447861,0.00038528617,0.02675207,0.0049101356,0.00022713242,0.0003691013],"about_ca_topic_score_codex":0.008552936,"about_ca_topic_score_gemma":0.0023048555,"teacher_disagreement_score":0.027976166,"about_ca_system_score_codex":0.00001935494,"about_ca_system_score_gemma":0.00030722623,"threshold_uncertainty_score":0.99989015},"labels":[],"label_agreement":null},{"id":"W3192902513","doi":"10.1029/2021jb021960","title":"Surface‐Wave Tomography of the Northern Canadian Cordillera Using Earthquake Rayleigh Wave Group Velocities","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Ottawa; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Lithosphere; Crust; Asthenosphere; Craton; Low-velocity zone; Mantle (geology); Rayleigh wave; Seismic tomography; Group velocity; Geophysics; Surface wave; Tectonics","score_opus":0.05143600704837931,"score_gpt":0.27745415936504186,"score_spread":0.22601815231666256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3192902513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964804,0.00036895336,0.000007956461,0.00034192562,0.000642892,0.0001575157,0.00022049322,0.000004597593,0.0017752458],"genre_scores_gemma":[0.9984426,0.00011249137,0.00042279277,0.00007232858,0.00064478477,2.8405384e-7,0.00001537632,0.000011098633,0.000278235],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961316,0.0007186697,0.0005724979,0.00024281301,0.0015227144,0.0008116877],"domain_scores_gemma":[0.9970776,0.0004724291,0.00028170354,0.00039450935,0.0012498952,0.00052388303],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010786271,0.00019668897,0.00058687775,0.00018378,0.00047433344,0.00019932385,0.00040748002,0.00010762111,0.0011654831],"category_scores_gemma":[0.000249145,0.00013296031,0.00037576116,0.00092671765,0.00044421153,0.00028422754,0.00007498274,0.00069292716,0.000040440635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024761292,0.002088889,0.40501896,0.0014677738,0.005067858,0.0071964655,0.013657727,0.0516174,0.4010491,0.0062264125,0.006856704,0.09727659],"study_design_scores_gemma":[0.0008291047,0.00073914893,0.9546801,0.00034648535,0.00008442101,0.00012691885,0.00092748605,0.0046476084,0.024477422,0.0048184637,0.007931907,0.0003909694],"about_ca_topic_score_codex":0.069790944,"about_ca_topic_score_gemma":0.10505903,"teacher_disagreement_score":0.5496611,"about_ca_system_score_codex":0.000014265891,"about_ca_system_score_gemma":0.0013645183,"threshold_uncertainty_score":0.9997476},"labels":[],"label_agreement":null},{"id":"W3193573951","doi":"","title":"S receiver function imaging of the lithosphere-asthenosphere boundary (LAB) in western Canada","year":2020,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Asthenosphere; Geology; Lithosphere; Receiver function; Function (biology); Remote sensing; Boundary (topology); Geophysics; Seismology; Tectonics","score_opus":0.00858898199105398,"score_gpt":0.18118563970485008,"score_spread":0.1725966577137961,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193573951","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98974234,0.00033752457,0.000001557965,0.00088820077,0.0006478245,0.000111999805,0.000039716073,0.000017599401,0.008213231],"genre_scores_gemma":[0.9989765,0.000008871488,0.000074299904,0.0006734401,0.0001430914,5.4747625e-7,0.00001549912,0.0000054266065,0.000102310405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989007,0.00008360396,0.00030229276,0.00021038564,0.0002623141,0.00024070223],"domain_scores_gemma":[0.9994452,0.000097023774,0.00018914483,0.00014623198,0.00003685915,0.00008551944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002384687,0.00012041687,0.00017487547,0.0000063046555,0.00009552374,0.000058023023,0.00023027789,0.00003419839,0.00008002153],"category_scores_gemma":[0.00007950983,0.00008956692,0.000032729786,0.0001371318,0.00003829895,0.00013337279,0.000024456103,0.00013835389,0.000030736446],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003762805,0.0000070217393,0.9788506,0.000053801366,0.000010846535,0.000017608527,0.00039196466,0.015106937,0.00059967645,0.0000032520918,0.0011167023,0.0038039864],"study_design_scores_gemma":[0.00015752797,0.000020701877,0.98221445,0.000087358356,0.000013305638,0.0000014221155,0.00016575567,0.00030007953,0.00062898075,0.00008609371,0.016209297,0.00011505307],"about_ca_topic_score_codex":0.9180744,"about_ca_topic_score_gemma":0.94598395,"teacher_disagreement_score":0.027909564,"about_ca_system_score_codex":0.0000061445376,"about_ca_system_score_gemma":0.0002236717,"threshold_uncertainty_score":0.3652433},"labels":[],"label_agreement":null},{"id":"W3194041159","doi":"10.5194/egusphere-egu21-1417","title":"Adiabatic Heat Flow in Mercury with a Fe-8.5wt%Si Core","year":2021,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Thermal conductivity; Adiabatic process; Electrical resistivity and conductivity; Analytical Chemistry (journal); Thermodynamics; Chemistry; Materials science; Physics; Chromatography","score_opus":0.01205066154873556,"score_gpt":0.19558934259468713,"score_spread":0.18353868104595158,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194041159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98141336,0.00023444198,0.00003966883,0.0002932191,0.0002726844,0.000093449715,0.00006392587,0.000026671918,0.017562559],"genre_scores_gemma":[0.996282,0.000030136944,0.0017061397,0.00039255526,0.00008257137,0.0000014430872,0.00014918495,0.0000030475544,0.0013529302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992527,0.000038041966,0.00012708559,0.0002043115,0.00014857997,0.00022931707],"domain_scores_gemma":[0.99964786,0.000057122197,0.000014638413,0.00016805578,0.000027871993,0.00008447139],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000099201825,0.00009844681,0.00018317766,0.00002937068,0.000046103465,0.00006304917,0.00008798039,0.000036417245,0.0078009125],"category_scores_gemma":[0.000011622047,0.00006769768,0.00002176813,0.00019532315,0.000027072672,0.00011650102,0.000008960758,0.000055339824,0.00039290014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038679427,0.00033549315,0.8499463,0.0004682972,0.00026610272,0.0027887728,0.0030948434,0.044475358,0.024268378,0.0040885713,0.016687619,0.05319343],"study_design_scores_gemma":[0.0019155521,0.00048670114,0.88866377,0.00020542304,0.000081010614,0.00010612527,0.00063544314,0.043740872,0.009938662,0.003956275,0.049230166,0.0010399881],"about_ca_topic_score_codex":0.0036116254,"about_ca_topic_score_gemma":0.017065795,"teacher_disagreement_score":0.052153446,"about_ca_system_score_codex":0.0000014035087,"about_ca_system_score_gemma":0.00008129156,"threshold_uncertainty_score":0.99310607},"labels":[],"label_agreement":null},{"id":"W3194379528","doi":"10.1093/mnras/stab2460","title":"Cepheid metallicity in the Leavitt law (C-metall) survey – I. HARPS-N@TNG spectroscopy of 47 classical Cepheids and 1 BL Her variables","year":2021,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Istituto Nazionale di Astrofisica; Agenzia Spaziale Italiana; Institut sur la Nutrition et les Aliments Fonctionnels; Ministerio de Economía y Competitividad","keywords":"Cepheid variable; Physics; Metallicity; Astrophysics; Spectroscopy; Astronomy; Stars","score_opus":0.011272376717315891,"score_gpt":0.2002900896018332,"score_spread":0.1890177128845173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194379528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973452,0.00028803924,0.000014991374,0.00039950185,0.000234396,0.00016074975,0.00044140214,0.000006918339,0.0011088079],"genre_scores_gemma":[0.99736786,0.0000018620501,0.0022505429,0.00010550154,0.00011137331,0.0000018114644,0.00006495267,0.0000057136776,0.0000903985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981282,0.00052801153,0.00040765337,0.00031869652,0.0002812996,0.0003361559],"domain_scores_gemma":[0.99876434,0.0005689094,0.00020319592,0.00034559026,0.00004565109,0.00007229946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010170238,0.00019111206,0.00048298622,0.0000066915595,0.00013441588,0.000096343036,0.00052161,0.0001101883,0.00042769918],"category_scores_gemma":[0.000053013413,0.00011455112,0.00024641192,0.00013915628,0.0004291494,0.00012042788,0.00013015626,0.00022947093,0.000007000703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023418156,0.0004940291,0.5380391,0.00016516921,0.0005265922,0.0000019502415,0.0009927206,0.45094863,0.004599577,0.0020899365,0.0013170365,0.0005911258],"study_design_scores_gemma":[0.00037850876,0.000077107194,0.9517161,0.000022496415,0.00010511501,4.572958e-8,0.00018595964,0.04005407,0.005696931,0.00024431603,0.0013629815,0.00015636778],"about_ca_topic_score_codex":0.015515432,"about_ca_topic_score_gemma":0.0076398663,"teacher_disagreement_score":0.41367704,"about_ca_system_score_codex":0.000006864594,"about_ca_system_score_gemma":0.00006923447,"threshold_uncertainty_score":0.99104035},"labels":[],"label_agreement":null},{"id":"W3195764685","doi":"10.1029/2021gc010012","title":"Altered Mantle Fabric Beneath the Mid‐Continent Rift","year":2021,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Kingston Health Sciences Centre; University of Sudbury; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Lithosphere; Rift; Terrane; Mantle (geology); Seismology; Archean; Proterozoic; Geophysics; Paleontology; Tectonics","score_opus":0.008421719903583803,"score_gpt":0.18892766767587685,"score_spread":0.18050594777229304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195764685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97621953,0.0015768388,0.000062415435,0.0004988109,0.0022214542,0.00024115237,0.00081005326,0.00009596828,0.018273767],"genre_scores_gemma":[0.99221444,0.00005715406,0.000056744015,0.00014280758,0.002139989,0.000011142832,0.0010277284,0.000012736037,0.0043372624],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9977136,0.00011697898,0.0004370732,0.0005894907,0.0004965784,0.00064623187],"domain_scores_gemma":[0.99833935,0.00014092213,0.00023007227,0.00091630337,0.00019519227,0.00017817285],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00028045458,0.0003350221,0.0004355475,0.000016797294,0.00037073245,0.00031865895,0.0005313255,0.00012513583,0.0017187475],"category_scores_gemma":[0.000034027107,0.0002501434,0.00020180884,0.00030106844,0.000078093246,0.0001427921,0.00008145445,0.00021209747,0.0009061035],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019141364,0.00057635794,0.05853827,0.0024129394,0.0013480438,0.0007740184,0.0020895312,0.0065788524,0.84771794,0.0020344364,0.051255457,0.026482744],"study_design_scores_gemma":[0.0018475492,0.00012690517,0.11136233,0.00034673265,0.0003799399,0.00030506446,0.0013209973,0.004694379,0.4966321,0.008542686,0.37231195,0.002129379],"about_ca_topic_score_codex":0.002779506,"about_ca_topic_score_gemma":0.00027986756,"teacher_disagreement_score":0.35108584,"about_ca_system_score_codex":0.000006179358,"about_ca_system_score_gemma":0.00013918946,"threshold_uncertainty_score":0.99999505},"labels":[],"label_agreement":null},{"id":"W3196022491","doi":"10.1038/s41586-021-03595-z","title":"Unusual width of the superconducting transition in a hydride","year":2021,"lang":"en","type":"letter","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Superconductivity; Hydride; High pressure; Room-temperature superconductor; Superconducting transition temperature; Condensed matter physics; Transition temperature; Sulfur; High-temperature superconductivity; Physics; Materials science; Chemistry; Thermodynamics; Metallurgy; Metal","score_opus":0.009595284228986289,"score_gpt":0.2026959662525912,"score_spread":0.19310068202360492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3196022491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78321964,0.001427394,8.4227565e-7,0.20954235,0.0030456162,0.00021502138,0.00083323393,0.000013760873,0.0017021266],"genre_scores_gemma":[0.81959194,0.000027546108,0.00007369709,0.17649129,0.0024215484,9.4902305e-7,0.0010538215,0.0000073381716,0.0003318742],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99896777,0.00015440912,0.00018175357,0.00021879739,0.0002856162,0.00019163823],"domain_scores_gemma":[0.99958664,0.00008017521,0.00007494496,0.0002090475,0.00003547384,0.000013700272],"candidate_categories":["research_integrity"],"consensus_categories":["research_integrity"],"category_scores_codex":[0.000149514,0.00013557947,0.00025819245,0.000045505407,0.000042196087,0.000032813892,0.00024057107,0.001648357,0.0006503141],"category_scores_gemma":[0.000028822977,0.0000889426,0.00009499807,0.00019946533,0.000037158083,0.00008350228,0.00000983419,0.003050572,0.000008733861],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030979725,0.000028810953,0.006067991,0.001016633,0.00012715506,0.0006190034,0.002425097,0.00109862,0.01025584,0.000055569835,0.9742104,0.004063934],"study_design_scores_gemma":[0.0005178562,0.000056577694,0.04477283,0.000722732,0.00012365996,0.00004835442,0.00017228255,0.0001474367,0.012096447,0.0024632523,0.9382522,0.00062633416],"about_ca_topic_score_codex":0.0015580796,"about_ca_topic_score_gemma":0.0012150963,"teacher_disagreement_score":0.03870484,"about_ca_system_score_codex":0.0000022839874,"about_ca_system_score_gemma":0.000072213676,"threshold_uncertainty_score":0.99964774},"labels":[],"label_agreement":null},{"id":"W3198449896","doi":"","title":"Thermal and thermal-Hall conductivity study of SrCu 2 (BO 3 ) 2","year":2018,"lang":"de","type":"article","venue":"Verhandlungen der Deutschen Physikalischen Gesellschaft","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; Brockhouse Institute for Materials Research","funders":"","keywords":"Thermal conductivity; Materials science; Thermal; Physics; Thermodynamics; Composite material","score_opus":0.020387874419354163,"score_gpt":0.2400986104255708,"score_spread":0.21971073600621663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3198449896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98112816,0.010108585,0.00001760245,0.00012711683,0.0024091087,0.001407146,0.0005626722,0.00008302736,0.004156584],"genre_scores_gemma":[0.9948774,0.00030791442,0.00018633077,0.00017521129,0.0034640746,0.000018288616,0.00013673122,0.00006710258,0.0007669417],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9944945,0.0009554439,0.0009886429,0.0013860513,0.0009896411,0.0011856945],"domain_scores_gemma":[0.99675924,0.00031441,0.00067694945,0.0012916225,0.00043162808,0.0005261616],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011092303,0.00095295924,0.0014277567,0.00021774443,0.0005955159,0.00034236786,0.0009551922,0.00040410357,0.0035898879],"category_scores_gemma":[0.000044656583,0.0008142279,0.0002229638,0.0005330411,0.0008609308,0.0009170117,0.00039034267,0.00048109842,0.0010409948],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038684309,0.0072022933,0.17846093,0.001337427,0.018346934,0.00025268184,0.078080185,0.0013382402,0.6821811,0.0011054856,0.008351806,0.019474488],"study_design_scores_gemma":[0.0133330785,0.013254253,0.70870703,0.0004439584,0.010674757,0.000016982438,0.0040318146,0.0072866064,0.17190297,0.0011470941,0.06400472,0.0051967083],"about_ca_topic_score_codex":0.008493623,"about_ca_topic_score_gemma":0.0009261367,"teacher_disagreement_score":0.53024614,"about_ca_system_score_codex":0.000010764964,"about_ca_system_score_gemma":0.00018805158,"threshold_uncertainty_score":0.9997368},"labels":[],"label_agreement":null},{"id":"W3199430495","doi":"","title":"Rare earth titanates under high pressure: a neutron study","year":2002,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Atomic Energy (Canada); University of Waterloo","funders":"","keywords":"Earth (classical element); Geology; Physics","score_opus":0.01574201780955776,"score_gpt":0.19613931395605982,"score_spread":0.18039729614650207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3199430495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9746256,0.000549176,0.00000778237,0.00025513445,0.00056985125,0.0003334437,0.000083272025,0.00010805593,0.02346767],"genre_scores_gemma":[0.98902744,0.000029412895,0.00013369534,0.00016626246,0.0001807796,0.0000020344544,0.00002617061,0.00000436582,0.010429855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990029,0.000078172954,0.00015906373,0.00026069087,0.00022671565,0.00027249346],"domain_scores_gemma":[0.99953574,0.000052708176,0.00004128961,0.0002462098,0.000027586884,0.00009645297],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00010929865,0.00013734867,0.00018717539,0.000036886486,0.00012750954,0.00012777888,0.00019333861,0.00004282697,0.042820446],"category_scores_gemma":[0.000005248772,0.00009875576,0.000033546792,0.00011597748,0.000026423233,0.00019959704,0.000016600286,0.00006207715,0.0021373534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032685953,0.0026847846,0.71309155,0.0002678293,0.0016918796,0.0003904467,0.00504374,0.056618445,0.008572755,0.02006574,0.14449048,0.046755508],"study_design_scores_gemma":[0.0007221215,0.0004907636,0.94551843,0.0000063055413,0.00009117541,0.0000034824686,0.0002564132,0.0017846518,0.00048149232,0.0009436663,0.049348935,0.00035258246],"about_ca_topic_score_codex":0.0035967655,"about_ca_topic_score_gemma":0.0017647833,"teacher_disagreement_score":0.23242688,"about_ca_system_score_codex":4.2772095e-7,"about_ca_system_score_gemma":0.0000058597752,"threshold_uncertainty_score":0.9986396},"labels":[],"label_agreement":null},{"id":"W3199785057","doi":"10.1785/0120210076","title":"Multichannel Alignment of <i>S</i> Waves","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Waveform; Seismology; Residual; Geology; Induced seismicity; Redundancy (engineering); Algorithm; Geodesy; Computer science; Radar; Telecommunications","score_opus":0.011140419498115678,"score_gpt":0.19625301840372789,"score_spread":0.1851125989056122,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3199785057","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95463836,0.0013094589,0.0006415306,0.036184147,0.00067260826,0.0003223323,0.0005365037,0.000027261582,0.005667775],"genre_scores_gemma":[0.98326606,0.0002556034,0.011385135,0.0042023105,0.000044432836,7.328845e-7,0.000017421102,0.000002341965,0.00082595274],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990302,0.00012052505,0.0002815308,0.00015720737,0.00024897422,0.0001616186],"domain_scores_gemma":[0.99922323,0.0001890521,0.0002570555,0.00022016904,0.00007093932,0.000039548147],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015638376,0.000092497714,0.00032771105,0.000003299784,0.000053413223,0.000004861515,0.0002622933,0.00006348109,0.0030936764],"category_scores_gemma":[0.000054055774,0.000055352986,0.00030117112,0.00009606737,0.00041479463,0.0000068889767,0.00008139908,0.000058758233,0.000019233637],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036788272,0.001761578,0.023811616,0.0012231698,0.0012770504,0.00001921257,0.0045290915,0.034201734,0.155825,0.001005766,0.7266907,0.04928721],"study_design_scores_gemma":[0.00037046504,0.00027499406,0.047549758,0.00005670686,0.00006381232,0.0000044183566,0.00076914456,0.00039671132,0.13055453,0.0016898153,0.8180965,0.00017314973],"about_ca_topic_score_codex":0.004640912,"about_ca_topic_score_gemma":5.0379884e-7,"teacher_disagreement_score":0.0914058,"about_ca_system_score_codex":0.0000012081669,"about_ca_system_score_gemma":0.000023381,"threshold_uncertainty_score":0.99781764},"labels":[],"label_agreement":null},{"id":"W3200758836","doi":"10.1007/s00339-021-04911-0","title":"Fe-doped effects on phase transition and electronic structure of CeO2 under compressed conditions from ab initio calculations","year":2021,"lang":"en","type":"article","venue":"Applied Physics A","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Regroupement Québécois sur les Matériaux de Pointe","funders":"Royal Golden Jubilee (RGJ) Ph.D. Programme; Uppsala Universitet; Thailand Research Fund; Chulalongkorn University; Thailand Center of Excellence in Physics","keywords":"Orthorhombic crystal system; Band gap; Doping; Ab initio; Lattice constant; Materials science; Ab initio quantum chemistry methods; Electronic structure; Impurity; Phase transition; Phase (matter); Crystallography; Chemistry; Condensed matter physics; Crystal structure; Computational chemistry; Diffraction; Molecule","score_opus":0.007857064456260545,"score_gpt":0.22312780694661116,"score_spread":0.2152707424903506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200758836","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952263,0.00005465467,0.0013453201,0.00009017891,0.00008695292,0.00019998332,0.0022998292,0.000020784673,0.000675973],"genre_scores_gemma":[0.9947258,0.000015023501,0.000110828485,0.0003562635,0.00016491833,0.0000034187403,0.0046133245,0.000005764414,0.000004664983],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99929327,0.00004678836,0.00013443422,0.0002173818,0.00013933003,0.00016881572],"domain_scores_gemma":[0.99949896,0.00018718341,0.000067031055,0.00016200074,0.000029305678,0.000055487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000020347288,0.00012374934,0.00021537334,0.000017707787,0.00012437969,0.00004108203,0.000054194606,0.000051953393,0.0003601788],"category_scores_gemma":[0.0000016616053,0.00011764268,0.000036001395,0.00012642845,0.000046942096,0.000067568835,0.0000056076374,0.00009531678,0.000016978018],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006885615,0.00012145049,0.00003696149,0.000054858552,0.0001479302,0.0000045703405,0.00036606434,0.016779982,0.90027446,0.079869844,0.00014184412,0.0021332125],"study_design_scores_gemma":[0.002550502,0.00013346692,0.021515796,0.000038526883,0.00019064792,0.0000012813465,0.000064596905,0.0036228101,0.6881065,0.28307092,0.00041485496,0.00029015346],"about_ca_topic_score_codex":0.0003274292,"about_ca_topic_score_gemma":0.00015580471,"teacher_disagreement_score":0.21216798,"about_ca_system_score_codex":0.0000025811473,"about_ca_system_score_gemma":0.000053542226,"threshold_uncertainty_score":0.47973293},"labels":[],"label_agreement":null},{"id":"W3200944921","doi":"10.21203/rs.3.rs-967287/v1","title":"Absence of evidence of superconductivity in sulfur hydride in optical reflectance experiments","year":2021,"lang":"en","type":"preprint","venue":"Research Square","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Superconductivity; Hydride; Reflectivity; Phonon; Sulfur; Condensed matter physics; Infrared; Superconducting transition temperature; Chemistry; Materials science; Physics; Optics; Hydrogen; Organic chemistry","score_opus":0.2171475568586713,"score_gpt":0.42712392552482614,"score_spread":0.20997636866615485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200944921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956762,0.0028016586,0.000007568133,0.00009653654,0.00023609647,0.00047725812,0.00009129881,0.000006089003,0.00060727325],"genre_scores_gemma":[0.9982102,0.001127366,0.0004962206,0.0000027543683,0.000053037227,0.00001625803,0.000046391873,0.000005682401,0.00004207314],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9963842,0.00084470527,0.00054911815,0.00061317894,0.0010797143,0.0005290809],"domain_scores_gemma":[0.998048,0.00081386854,0.00010152945,0.0006415498,0.00028624572,0.00010881222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024286907,0.00017740164,0.00062787515,0.00029246332,0.000031858322,0.00006156586,0.0006219847,0.00021487787,0.0006971268],"category_scores_gemma":[0.00085261307,0.00014947321,0.00008035248,0.0005839798,0.000278159,0.0002910068,0.0003387837,0.0007267192,0.000016137143],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045572018,0.00038914985,0.3887622,0.0056725815,0.000037743313,0.00035796338,0.004602702,0.011805569,0.58489555,0.00027779504,0.000043343898,0.0026996564],"study_design_scores_gemma":[0.0002725636,0.00022374454,0.7671996,0.0070898784,0.0000037238085,0.0000019848053,0.0009802916,0.0011275215,0.22102132,0.0017763715,0.000021834316,0.00028118322],"about_ca_topic_score_codex":0.02515026,"about_ca_topic_score_gemma":0.0067198193,"teacher_disagreement_score":0.37843737,"about_ca_system_score_codex":0.00002467494,"about_ca_system_score_gemma":0.00055510487,"threshold_uncertainty_score":0.98134136},"labels":[],"label_agreement":null},{"id":"W3201411943","doi":"10.3389/feart.2021.732289","title":"Review of Electrical Resistivity Measurements and Calculations of Fe and Fe-Alloys Relating to Planetary Cores","year":2021,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Electrical resistivity and conductivity; Diamond anvil cell; Inner core; Materials science; Core (optical fiber); Mineralogy; Geology; Thermodynamics; Geophysics; High pressure; Physics; Composite material","score_opus":0.020766653418180132,"score_gpt":0.2361061482241281,"score_spread":0.21533949480594797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201411943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9809696,0.017020414,0.00035753642,0.00016126897,0.00029676637,0.00019449362,0.00006699358,0.0000056312165,0.00092730083],"genre_scores_gemma":[0.9785786,0.002292817,0.018936215,0.0001243839,0.00001440914,6.0558267e-7,0.000013894372,0.0000013225708,0.000037730257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989262,0.000080634694,0.0002376273,0.00024791746,0.00032449365,0.00018308313],"domain_scores_gemma":[0.9995412,0.00005641628,0.000085498155,0.00013590055,0.000082856684,0.00009807949],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00086414476,0.00006921406,0.0002437978,0.00008840947,0.000095742835,0.000021648006,0.00011233229,0.000024027031,0.000033245327],"category_scores_gemma":[0.00033737297,0.000060964496,0.000014622102,0.00058244605,0.00020220196,0.00015518455,0.000029527708,0.000053660675,0.0000012655427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022481983,0.00001802405,0.96636236,0.0005503686,0.000010265715,0.0000061812943,0.00016118718,0.00053537166,0.012998003,0.00006398644,0.0012102141,0.018061548],"study_design_scores_gemma":[0.00010712463,0.000052372583,0.99352103,0.00065223395,0.000013566475,0.0000032937241,0.000018592911,0.0019410732,0.0024421867,0.00022848336,0.0009353193,0.000084718304],"about_ca_topic_score_codex":0.0007754244,"about_ca_topic_score_gemma":0.0004964545,"teacher_disagreement_score":0.027158666,"about_ca_system_score_codex":0.0000018852277,"about_ca_system_score_gemma":0.00011708204,"threshold_uncertainty_score":0.248606},"labels":[],"label_agreement":null},{"id":"W3202190095","doi":"10.1103/physrevb.104.134102","title":"Evidence for mechanical softening-hardening dual anomaly in transition metals from shock-compressed vanadium","year":2021,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Science Challenge Project; NSAF Joint Fund; Natural Science Foundation of Jiangxi Province; China Postdoctoral Science Foundation; Tohoku University; National Natural Science Foundation of China; Canadian Association of Emergency Physicians","keywords":"Softening; Materials science; Vanadium; Hardening (computing); Phase transition; Compression (physics); Composite material; Thermodynamics; Flow stress; Bulk modulus; Mechanics; Condensed matter physics; Metallurgy; Strain rate; Physics","score_opus":0.04665139009314781,"score_gpt":0.341746515887476,"score_spread":0.2950951257943282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202190095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78145945,0.18735985,0.017983502,0.0068584904,0.00093722704,0.0033601795,0.0013373194,0.00018026719,0.0005237045],"genre_scores_gemma":[0.95050627,0.042266678,0.0010339448,0.0038589863,0.0013524167,0.00013544662,0.00078204216,0.000031220978,0.000032977954],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9952957,0.0007635458,0.0010285055,0.0012375355,0.0008284613,0.0008462492],"domain_scores_gemma":[0.99601126,0.0021753013,0.00035595856,0.0007642406,0.00026375602,0.000429503],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.000837649,0.0005978402,0.0023136388,0.000046574405,0.00017005063,0.00013694678,0.00055348297,0.00008237649,0.00082043227],"category_scores_gemma":[0.0013218445,0.00049596094,0.000953099,0.0006912397,0.00008144227,0.00065643794,0.00007589628,0.00042150982,0.00050490536],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001280343,0.0044444352,0.0015593872,0.056573283,0.0019641786,0.0012253925,0.0015639313,0.003807013,0.60745317,0.11935961,0.029978443,0.17079085],"study_design_scores_gemma":[0.0045456416,0.001957857,0.027984306,0.11375587,0.008434334,0.000065721695,0.00008129378,0.22080003,0.12208045,0.39185938,0.1019693,0.0064658234],"about_ca_topic_score_codex":0.00075810624,"about_ca_topic_score_gemma":0.00036065083,"teacher_disagreement_score":0.4853727,"about_ca_system_score_codex":0.00002106902,"about_ca_system_score_gemma":0.00019653952,"threshold_uncertainty_score":0.9997492},"labels":[],"label_agreement":null},{"id":"W3202264892","doi":"10.1007/s00269-021-01160-8","title":"In situ X-ray diffraction study of chrysotile at high P–T conditions: transformation to the 3.65 Å phase","year":2021,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of Saskatchewan","funders":"Ministry of Science and Higher Education of the Russian Federation","keywords":"Chrysotile; Phase (matter); Chemistry; Stishovite; Forsterite; Diamond anvil cell; X-ray crystallography; Diffraction; Intercalation (chemistry); Crystallography; Mineralogy; Analytical Chemistry (journal); Thermodynamics; High pressure; Materials science; Inorganic chemistry; Organic chemistry; Composite material; Optics","score_opus":0.011232222308022604,"score_gpt":0.24309626935136652,"score_spread":0.23186404704334393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202264892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99848694,0.0000547545,0.000009080668,0.00020615735,0.000066156834,0.00012794447,0.00024239114,0.0000028889501,0.00080370274],"genre_scores_gemma":[0.9993604,0.000025772,0.000013798141,0.000028862847,0.0000982664,0.0000043907608,0.00022531427,0.0000017118348,0.00024150783],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99944574,0.00002417386,0.0002006233,0.000114982155,0.00012928063,0.00008521302],"domain_scores_gemma":[0.9996825,0.00003745293,0.000080194,0.00012158947,0.0000459894,0.00003228129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007953448,0.00007207738,0.00017089474,0.000007263807,0.000049042985,0.000014321527,0.000058731668,0.000021564123,0.000347776],"category_scores_gemma":[0.0000069257194,0.000054824854,0.000023019635,0.00010253039,0.000020482932,0.00010660858,0.000009157114,0.000033723005,0.00000454748],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031891646,0.00026223165,0.00040160216,0.00007750156,0.000019094974,0.0000018818581,0.0010763912,0.002190203,0.99484956,0.00002755823,0.00038789105,0.00067419617],"study_design_scores_gemma":[0.0015571531,0.0001502436,0.03421257,0.00003626293,0.000050068043,0.0000022360007,0.0009266904,0.00037678162,0.95959514,0.0009273023,0.0020216254,0.00014390585],"about_ca_topic_score_codex":0.0006549568,"about_ca_topic_score_gemma":0.0003183366,"teacher_disagreement_score":0.035254396,"about_ca_system_score_codex":0.0000017684915,"about_ca_system_score_gemma":0.000012621499,"threshold_uncertainty_score":0.38079032},"labels":[],"label_agreement":null},{"id":"W3203050932","doi":"10.1016/j.mtphys.2021.100546","title":"Superconducting binary hydrides: Theoretical predictions and experimental progresses","year":2021,"lang":"en","type":"article","venue":"Materials Today Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Superconductivity; Metallic hydrogen; Hydrogen; Materials science; Hydride; Room-temperature superconductor; Periodic table; Critical field; Condensed matter physics; High-temperature superconductivity; Engineering physics; Metal; Physics; Metallurgy; Quantum mechanics","score_opus":0.01300353458919828,"score_gpt":0.23079837178869184,"score_spread":0.21779483719949355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203050932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965709,0.00038149336,0.000021612075,0.0001275441,0.001192065,0.00014183439,0.00035562352,0.00008196446,0.001126978],"genre_scores_gemma":[0.9980347,0.00004423532,0.0006165941,0.00007839692,0.00083225407,0.000007634535,0.0003163524,0.000009927379,0.000059871327],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988461,0.00013066485,0.00023003883,0.0003310695,0.00017665635,0.00028542703],"domain_scores_gemma":[0.99951494,0.00007240835,0.000053333228,0.00020986832,0.00004662936,0.000102849175],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015779815,0.00017492146,0.00026656952,0.000015114491,0.00023359004,0.00029100277,0.000098862634,0.00006239371,0.0044633336],"category_scores_gemma":[0.000023999417,0.00014790395,0.00003453888,0.00009351746,0.00021973254,0.0003241266,0.000055652898,0.000053336335,0.00010233426],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003712381,0.00010182228,0.0016537328,0.00007757908,0.000048166476,0.0000559266,0.00061984285,0.00019556619,0.98097306,0.015303725,0.0002782063,0.0006552686],"study_design_scores_gemma":[0.00024346472,0.00011065948,0.0037311974,0.000042606283,0.000035829868,0.000030333314,0.00041807012,0.00016175109,0.9861376,0.007899831,0.00094838644,0.00024023996],"about_ca_topic_score_codex":0.00013975239,"about_ca_topic_score_gemma":0.0000065984304,"teacher_disagreement_score":0.0074038943,"about_ca_system_score_codex":0.000002402269,"about_ca_system_score_gemma":0.00004512316,"threshold_uncertainty_score":0.9964467},"labels":[],"label_agreement":null},{"id":"W3203233221","doi":"10.1103/physrevd.104.089901","title":"Erratum: Sorkin-Johnston vacuum for a massive scalar field in the 2D causal diamond [Phys. Rev. D <b>100</b>, 045007 (2019)]","year":2021,"lang":"en","type":"erratum","venue":"Physical review. D/Physical review. D.","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institut Périmètre de physique théorique; Government of Canada; Ministry of Colleges and Universities; Innovation, Science and Economic Development Canada","keywords":"Attribution; License; Physics; Subject (documents); Cosmology; Theoretical physics; Citation; Diamond; Scalar (mathematics); Quantum mechanics; Psychology; Library science; Computer science; Law; Mathematics; Political science; Chemistry","score_opus":0.01739851760492807,"score_gpt":0.3616485115475431,"score_spread":0.344249993942615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203233221","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.024647748,0.8336529,0.000089729336,0.026196873,0.02905896,0.017571248,0.0057926956,0.00032446522,0.06266535],"genre_scores_gemma":[0.040302835,0.87902343,0.00024088919,0.029461665,0.024749026,0.0013584985,0.013917832,0.0002497651,0.010696044],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99084175,0.0015936112,0.0017836859,0.0021847954,0.0017588405,0.0018373213],"domain_scores_gemma":[0.9928565,0.0025399933,0.001254067,0.0023434404,0.0004431038,0.0005629136],"candidate_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow"],"category_scores_codex":[0.0016878869,0.0017131446,0.0051050438,0.00013265834,0.00040260964,0.00036736488,0.0024537088,0.0004450287,0.0004351294],"category_scores_gemma":[0.0015253192,0.0011464021,0.0023634501,0.0015479416,0.0002752356,0.00046113072,0.00026134233,0.0026310899,0.0013188716],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004365133,0.00048905326,0.00013342345,0.01633885,0.00019129929,0.00009590004,0.00011560495,0.000008907466,0.00039557897,0.0023205692,0.9645457,0.015321422],"study_design_scores_gemma":[0.0004277546,0.00062790845,0.0019214723,0.023355251,0.001735184,0.00001222669,0.000016345688,0.00046461378,0.00024802654,0.02463986,0.9449508,0.0016005259],"about_ca_topic_score_codex":0.0008183481,"about_ca_topic_score_gemma":0.0003544616,"teacher_disagreement_score":0.051969305,"about_ca_system_score_codex":0.000045091114,"about_ca_system_score_gemma":0.0006626106,"threshold_uncertainty_score":0.9996699},"labels":[],"label_agreement":null},{"id":"W3203923787","doi":"10.1029/2021gl094040","title":"Decadal to Centennial Timescale Mantle Viscosity Inferred From Modern Crustal Uplift Rates in Greenland","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Science Mission Directorate; Jet Propulsion Laboratory","keywords":"Geology; Centennial; Mantle (geology); Geophysics; History","score_opus":0.029953414179204708,"score_gpt":0.2945204347962906,"score_spread":0.26456702061708587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203923787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99507594,0.000059646296,0.00020635963,0.002950165,0.00030414786,0.00025549674,0.00040274902,0.000026537227,0.0007189824],"genre_scores_gemma":[0.99750996,0.00001205989,0.00034166613,0.0007287214,0.0006478882,0.0000074209433,0.00039599533,0.000009801222,0.00034649755],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99693877,0.00039375934,0.00025862688,0.00062548387,0.0008549727,0.0009284097],"domain_scores_gemma":[0.99865687,0.00045517107,0.000030223016,0.0003717163,0.00010386841,0.00038213603],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00036557982,0.0001942841,0.00035442112,0.00011427877,0.00019517083,0.00027520023,0.00039385975,0.00008062624,0.0014755982],"category_scores_gemma":[0.0001387145,0.0001738038,0.00008694461,0.00045010124,0.00013614834,0.0002495271,0.0001793813,0.00041098715,0.0015091621],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012056188,0.0005141203,0.13952571,0.00006565144,0.00014537816,0.0019110823,0.001596444,0.005815867,0.8044146,0.0003062495,0.024487037,0.020012269],"study_design_scores_gemma":[0.00088251743,0.00012820058,0.9632488,0.000059863003,0.00001060819,0.000002188896,0.00007206048,0.008716746,0.015338775,0.003968956,0.007178418,0.00039290407],"about_ca_topic_score_codex":0.025726518,"about_ca_topic_score_gemma":0.0060437126,"teacher_disagreement_score":0.8237231,"about_ca_system_score_codex":0.000015077221,"about_ca_system_score_gemma":0.00012263654,"threshold_uncertainty_score":0.9994372},"labels":[],"label_agreement":null},{"id":"W3204010624","doi":"10.1093/gji/ggab396","title":"Evidence for asthenospheric flow rotation in northwest Canada: insights from shear wave splitting","year":2021,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; McGill University; Geological Survey of Canada; University of Ottawa","funders":"National Science Foundation","keywords":"Lithosphere; Geology; Asthenosphere; Craton; Shear wave splitting; Seismology; Geophysics; North American Plate; Seismic anisotropy; Shear (geology); Mantle (geology); Slab; Plate tectonics; Tectonics; Paleontology","score_opus":0.028042126769695,"score_gpt":0.23515591405029826,"score_spread":0.20711378728060326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3204010624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947824,0.00026959006,0.0012955136,0.0008425858,0.0022039115,0.00008658202,0.00024302582,0.0000071378167,0.00026928555],"genre_scores_gemma":[0.99317163,0.000048452624,0.0042522107,0.00030608097,0.0017382266,0.0000026081307,0.00035975,0.00000485796,0.00011615815],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99868566,0.000077396646,0.00034172976,0.00023787694,0.00044313533,0.0002141791],"domain_scores_gemma":[0.99894273,0.00046096597,0.00014267073,0.00009204276,0.00024651943,0.00011504205],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010555293,0.00012121527,0.00019329255,0.000026103306,0.00012324432,0.00019662098,0.00019453025,0.00003860176,0.000999319],"category_scores_gemma":[0.00018011878,0.000106005915,0.000075224954,0.000118629054,0.000019400935,0.000408871,0.00002033195,0.00016736348,0.0000340477],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015408683,0.0006251038,0.24044923,0.00011744552,0.00097145286,0.0031677175,0.0033798874,0.22122657,0.033838082,0.004805224,0.0072301943,0.48264822],"study_design_scores_gemma":[0.0004953783,0.000050055158,0.9303292,0.00015763532,0.000018488812,0.000023872019,0.000118201,0.05250136,0.0012294479,0.01073837,0.0041420236,0.00019596101],"about_ca_topic_score_codex":0.27756846,"about_ca_topic_score_gemma":0.4674895,"teacher_disagreement_score":0.68987995,"about_ca_system_score_codex":0.00003549554,"about_ca_system_score_gemma":0.00046388598,"threshold_uncertainty_score":0.99991393},"labels":[],"label_agreement":null},{"id":"W3207241490","doi":"10.21203/rs.3.rs-1001084/v1","title":"Clear evidence against superconductivity in hydrides under high pressure","year":2021,"lang":"en","type":"preprint","venue":"Research Square","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Superconductivity; Condensed matter physics; High pressure; Physics; Materials science; Engineering physics","score_opus":0.0998023513460585,"score_gpt":0.3495184167839725,"score_spread":0.249716065437914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3207241490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887009,0.0072994027,0.000010714759,0.0007793843,0.00092348485,0.0008279625,0.00047383722,0.00005899311,0.0009252843],"genre_scores_gemma":[0.9950433,0.0031165534,0.0002029574,0.0000445856,0.0005171686,0.000026216314,0.0005434397,0.000018192643,0.0004876004],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9941556,0.0018444462,0.0004205909,0.0011366281,0.0014538001,0.0009889377],"domain_scores_gemma":[0.99723876,0.0009473544,0.0000855706,0.0010629945,0.0003958602,0.000269449],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0028362852,0.00034593695,0.00065086107,0.00031550004,0.00024794758,0.000803622,0.0009131884,0.00047468065,0.0038256827],"category_scores_gemma":[0.0005749746,0.0003090328,0.00014825584,0.0005174056,0.0002610095,0.00061322196,0.0006473736,0.0017206754,0.00032246686],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011437711,0.0009416113,0.3037945,0.02112719,0.00088561495,0.002379308,0.007045154,0.58762324,0.0350245,0.0021687618,0.008089007,0.02977734],"study_design_scores_gemma":[0.0003671273,0.00022351068,0.973522,0.005007983,0.000040007697,0.0000041133153,0.0012710867,0.0032970954,0.0037906244,0.007604296,0.003988242,0.0008838959],"about_ca_topic_score_codex":0.048086587,"about_ca_topic_score_gemma":0.01110589,"teacher_disagreement_score":0.6697275,"about_ca_system_score_codex":0.000024944755,"about_ca_system_score_gemma":0.0006884521,"threshold_uncertainty_score":0.99993616},"labels":[],"label_agreement":null},{"id":"W3208229143","doi":"10.1063/5.0064837","title":"Infrared imaging of samples in ultrahigh pressure diamond anvil cells","year":2021,"lang":"en","type":"article","venue":"Journal of Applied Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph; McMaster University; University of Waterloo","funders":"International Research Office; Natural Sciences and Engineering Research Council of Canada","keywords":"Diamond anvil cell; Micrometer; Materials science; Infrared; Diamond; Laser; Optics; Radiation; Superconductivity; Atmospheric temperature range; Optoelectronics; Analytical Chemistry (journal); Condensed matter physics; Chemistry; Diffraction; Physics; Composite material","score_opus":0.008764067408901222,"score_gpt":0.19524248064125208,"score_spread":0.18647841323235084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208229143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889468,0.0005954151,0.00023502835,0.000025161153,0.0005547326,0.000086797394,0.00021507968,0.0000054920997,0.009335507],"genre_scores_gemma":[0.9976626,0.00010665959,0.0017126151,0.00005850993,0.0003670496,2.7272455e-7,0.000025181022,0.000005027432,0.000062060215],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99893254,0.000038215025,0.00042992237,0.00012365608,0.00028673434,0.0001889572],"domain_scores_gemma":[0.9991464,0.0001348589,0.00038266927,0.00015340996,0.00011035925,0.00007232947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020680195,0.000117977645,0.00037717633,0.00004019237,0.00003260409,0.000049097616,0.00019327445,0.000037828373,0.00034760727],"category_scores_gemma":[0.000009039098,0.000100025594,0.00008346232,0.00020603661,0.000047742797,0.0001770918,0.000015685182,0.00015002293,0.000010418195],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036280276,0.000328461,0.03905204,0.00037344525,0.00026661405,0.00015232676,0.0028443332,0.26343238,0.6680992,0.0028605901,0.0038611365,0.01836665],"study_design_scores_gemma":[0.0013748114,0.00007584374,0.10828383,0.0001267768,0.00015744759,0.000013672617,0.0004898151,0.001434874,0.8058057,0.064861566,0.017004078,0.0003716],"about_ca_topic_score_codex":0.00009304471,"about_ca_topic_score_gemma":0.000024270334,"teacher_disagreement_score":0.26199752,"about_ca_system_score_codex":0.0000017626863,"about_ca_system_score_gemma":0.000111544505,"threshold_uncertainty_score":0.40789253},"labels":[],"label_agreement":null},{"id":"W3210183623","doi":"10.1093/gji/ggab418","title":"Global reference seismological data sets: multimode surface wave dispersion","year":2021,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"David and Lucile Packard Foundation; National Science Foundation","keywords":"Overtone; Dispersion (optics); Geology; Geodesy; Data quality; Metadata; Data set; Remote sensing; Computer science; Seismology; Optics; Physics; Artificial intelligence","score_opus":0.05809525781418893,"score_gpt":0.2894064535464444,"score_spread":0.23131119573225548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3210183623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986172,0.00013561572,0.0016161023,0.0022000268,0.0023814202,0.00005055496,0.0023350725,0.0000319881,0.0050771777],"genre_scores_gemma":[0.9921756,0.00012726392,0.003977289,0.0005257471,0.0008469419,1.7314225e-7,0.001840033,0.000003333725,0.0005036292],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99820065,0.00015055918,0.00030195614,0.00041150826,0.00062359555,0.00031174664],"domain_scores_gemma":[0.99898595,0.00011401998,0.00013255978,0.00033486035,0.00021206128,0.00022055926],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022329467,0.00016644817,0.00022668029,0.000015677651,0.00018554174,0.0003437139,0.0007445406,0.00008632196,0.0047069467],"category_scores_gemma":[0.00009739656,0.00012705923,0.00008194629,0.0001248897,0.000073105635,0.00055410207,0.00022007634,0.00024735896,0.0006067688],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021602057,0.002405599,0.29023182,0.00008922235,0.0021529107,0.010680882,0.00047714988,0.068328105,0.019300442,0.029337954,0.09736231,0.4774734],"study_design_scores_gemma":[0.0011196614,0.00016429299,0.76227176,0.00007686386,0.00007764473,0.0010847852,0.00012489637,0.10769861,0.0005163545,0.0282791,0.09799366,0.00059236394],"about_ca_topic_score_codex":0.0010906901,"about_ca_topic_score_gemma":0.00016959917,"teacher_disagreement_score":0.47688106,"about_ca_system_score_codex":0.000015623618,"about_ca_system_score_gemma":0.00014151291,"threshold_uncertainty_score":0.9962029},"labels":[],"label_agreement":null},{"id":"W3214102980","doi":"10.1139/cjp-2021-0184","title":"Nucleon–nucleus inelastic scattering by Manning–Rosen distorted nonlocal potential","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Scattering; Separable space; Nucleon; Inelastic scattering; Shell (structure); Quantum electrodynamics; Matrix (chemical analysis); Hadron; S-matrix; Quantum mechanics; Nuclear physics","score_opus":0.006735417959192687,"score_gpt":0.17377785304152846,"score_spread":0.16704243508233577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3214102980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99302465,0.00031434206,0.0024730356,0.0003113729,0.002332509,0.000040832147,0.00049491506,0.000007672255,0.0010006964],"genre_scores_gemma":[0.9983528,0.000009114917,0.00028285276,0.00018751384,0.00090826984,9.8908664e-8,0.00008566647,0.000008574361,0.00016507039],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99901605,0.00004859205,0.00026906145,0.0001375329,0.00019018225,0.00033860884],"domain_scores_gemma":[0.9989983,0.000023635866,0.00015891771,0.00013207254,0.00013695733,0.0005501049],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009992818,0.00012876368,0.00024160939,0.000040237806,0.00017735282,0.00018110807,0.00021841691,0.000050597897,0.0010039],"category_scores_gemma":[0.000022167473,0.00012291361,0.00009585831,0.0001475639,0.000084997366,0.0002357862,0.000007557568,0.00016193501,0.000099112636],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023464658,0.00024994402,0.09922254,0.00044725926,0.0014652648,0.015029268,0.0040859077,0.096177675,0.29999265,0.0018501185,0.22698095,0.2542638],"study_design_scores_gemma":[0.0046934406,0.0011877165,0.42378086,0.0008026903,0.0010140692,0.0017373927,0.0011781862,0.023670511,0.047118977,0.012504905,0.47907263,0.0032386119],"about_ca_topic_score_codex":0.0068697617,"about_ca_topic_score_gemma":0.0075277863,"teacher_disagreement_score":0.32455832,"about_ca_system_score_codex":0.00001424996,"about_ca_system_score_gemma":0.00056524185,"threshold_uncertainty_score":0.99990934},"labels":[],"label_agreement":null},{"id":"W3215112433","doi":"10.3390/min11121320","title":"Crystal Structure of an Anisotropic Pyrope Garnet That Contains Two Cubic Phases","year":2021,"lang":"en","type":"article","venue":"Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Basic Energy Sciences; Argonne National Laboratory; Natural Sciences and Engineering Research Council of Canada; Office of Science","keywords":"Pyrope; Crystallography; Electron microprobe; Materials science; Bond length; Phase (matter); Analytical Chemistry (journal); Crystal (programming language); Anisotropy; Crystal structure; Mineralogy; Chemistry; Optics; Physics","score_opus":0.01593030899969013,"score_gpt":0.2366346267173284,"score_spread":0.22070431771763827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3215112433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956051,0.00041630145,0.000011576638,0.00005398101,0.00038969162,0.00008142438,0.0010259,0.000021528745,0.002394498],"genre_scores_gemma":[0.9970697,0.000021930959,0.00053927675,0.00015578499,0.0002834728,3.2115295e-7,0.00072734116,0.0000044870035,0.001197684],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99908566,0.000098434706,0.00017866604,0.0002269715,0.0001846085,0.00022563676],"domain_scores_gemma":[0.99947566,0.00003982406,0.00008715702,0.00024060176,0.000059080663,0.000097698205],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000051969746,0.00013104359,0.00027620044,0.000028457369,0.000060510232,0.000075883996,0.00015026973,0.000044124066,0.010785647],"category_scores_gemma":[0.000016302285,0.00010251547,0.00004849018,0.000093107956,0.00005011984,0.0001982405,0.000015229885,0.000048447157,0.000019967925],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000274498,0.00003092788,0.008908309,0.000026434805,0.000032870463,0.000063701555,0.00014866494,0.0009647902,0.98729986,0.0003904042,0.0012757633,0.00083085307],"study_design_scores_gemma":[0.0018894599,0.0004842519,0.06645146,0.000046660432,0.00009834687,0.00005881662,0.0002321097,0.00073711306,0.8718338,0.004531195,0.053098977,0.0005377902],"about_ca_topic_score_codex":0.0029704592,"about_ca_topic_score_gemma":0.0048409356,"teacher_disagreement_score":0.115466006,"about_ca_system_score_codex":0.00000124488,"about_ca_system_score_gemma":0.000054020213,"threshold_uncertainty_score":0.9901186},"labels":[],"label_agreement":null},{"id":"W3216021946","doi":"10.1029/2021tc007031","title":"Geodynamics of East Anatolia‐Caucasus Domain: Inferences From 3D Thermo‐Mechanical Models, Residual Topography, and Admittance Function Analyses","year":2021,"lang":"en","type":"article","venue":"Tectonics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Geodynamics; Lithosphere; Tectonics; Mantle (geology); Ocean surface topography; Gravity anomaly; Geophysics; Seismic tomography; Plateau (mathematics); Massif; Seismology; Geodesy; Paleontology","score_opus":0.033406450074475,"score_gpt":0.24225274704702046,"score_spread":0.20884629697254548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216021946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99353915,0.0026725053,0.0013703443,0.00007019509,0.00033588056,0.000073246105,0.000504937,0.00003629459,0.0013974174],"genre_scores_gemma":[0.9965441,0.000522531,0.0025531813,0.000051529598,0.000090885354,0.0000011144518,0.00021130432,0.000004757522,0.000020590602],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9988118,0.00010268801,0.0002715665,0.0003241979,0.0002659065,0.00022388787],"domain_scores_gemma":[0.9993092,0.00010247195,0.0001248683,0.00027494074,0.000098019176,0.00009052627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014726832,0.0001555356,0.00031687648,0.00005266914,0.00010589151,0.00007389177,0.00014753491,0.0001133699,0.0006729944],"category_scores_gemma":[0.000020582685,0.00012964052,0.000062568666,0.00026859893,0.00008545609,0.00017695763,0.000037492337,0.00011149139,0.00000810804],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0035369752,0.00094426307,0.25076172,0.0010402582,0.004754745,0.00077191734,0.006075954,0.08533195,0.21423128,0.16421725,0.0014395589,0.26689413],"study_design_scores_gemma":[0.0018546598,0.0008091287,0.39789394,0.0002118717,0.0006690284,0.00003492862,0.001702491,0.13992415,0.012486063,0.43968755,0.003385255,0.001340907],"about_ca_topic_score_codex":0.002970156,"about_ca_topic_score_gemma":0.0062271752,"teacher_disagreement_score":0.27547032,"about_ca_system_score_codex":0.0000020147777,"about_ca_system_score_gemma":0.00010074339,"threshold_uncertainty_score":0.7368817},"labels":[],"label_agreement":null},{"id":"W3216781959","doi":"10.1016/s0967-0653(98)82917-7","title":"10.1016/s0967-0653(98)82917-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geoid; Geology; Asthenosphere; Lithosphere; Mantle (geology); Geophysics; Viscosity; Subduction; Gravity anomaly; Ocean surface topography; Geodesy; Seismology; Tectonics; Physics; Thermodynamics; Measured depth","score_opus":0.0056812020820698715,"score_gpt":0.15708811667917702,"score_spread":0.15140691459710715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216781959","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0045038466,0.000054069726,1.8073662e-7,0.00012701021,0.000008347289,0.00012918292,0.00015049946,0.000077432174,0.99494946],"genre_scores_gemma":[0.0014839798,5.230115e-7,0.000091477035,0.00004998346,0.0003184824,0.0000016787417,0.000107717264,0.000005347349,0.99794084],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991191,0.00004382481,0.00014901513,0.00021634872,0.00017629932,0.00029539058],"domain_scores_gemma":[0.9995288,0.000038643648,0.00002501411,0.00022304035,0.000020319692,0.00016415183],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001437962,0.00012608404,0.00017703978,0.000033956803,0.00009790808,0.00008948692,0.0002328478,0.000049928076,0.99978876],"category_scores_gemma":[0.00000941468,0.00010587261,0.0000389447,0.00012576433,0.000025819767,0.00012252475,0.000010030977,0.000051959047,0.9995906],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007274662,0.000014887256,6.399662e-7,0.000007016414,0.000016199327,0.000009309456,0.000020658015,0.0007065991,0.00003212318,0.000001460397,0.3470082,0.65211016],"study_design_scores_gemma":[0.00010830909,0.000103903236,0.00037594678,0.000007166997,0.000012314345,0.0000026215184,4.4265582e-7,0.00014038115,0.00012156694,0.000042328447,0.9989234,0.00016158263],"about_ca_topic_score_codex":0.0008284479,"about_ca_topic_score_gemma":0.0000074105205,"teacher_disagreement_score":0.6519486,"about_ca_system_score_codex":0.0000014448557,"about_ca_system_score_gemma":0.000019292458,"threshold_uncertainty_score":0.431736},"labels":[],"label_agreement":null},{"id":"W34642534","doi":"10.1007/978-1-4419-0346-4_1","title":"Geophysical and Experimental Petrological Studies of the Earth’s Interior","year":2009,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Silicate perovskite; Olivine; Stishovite; Mantle (geology); Ringwoodite; Geochemistry; Discontinuity (linguistics); Mineralogy; Geophysics; Petrology; Quartz; Paleontology","score_opus":0.024343350779764947,"score_gpt":0.23590897078434675,"score_spread":0.2115656200045818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W34642534","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46841687,0.0038774814,6.661787e-7,0.0002645001,0.0008827423,0.00033066198,0.00018198347,0.000036095877,0.526009],"genre_scores_gemma":[0.84182864,0.00015643856,0.00008297942,0.00019414909,0.00023850259,5.383647e-7,0.00001317406,0.000003864285,0.1574817],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.999187,0.000023515931,0.00021941988,0.00023585236,0.00019439518,0.00013982393],"domain_scores_gemma":[0.99956,0.00006574369,0.00011526671,0.00018431262,0.0000270914,0.00004760187],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000071636045,0.00020369749,0.00043548405,0.000020705267,0.00007554238,0.000025790678,0.0001771104,0.000106768275,0.0021090456],"category_scores_gemma":[0.000007079711,0.00010610969,0.000108170374,0.000009809255,0.00032278377,0.000043381217,0.00006562914,0.00011275657,0.00007649559],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018579707,0.000326405,0.004778812,0.00083985226,0.0034609328,0.0002672839,0.005013899,0.00015288811,0.07211384,0.70395213,0.028304752,0.17893124],"study_design_scores_gemma":[0.0022793394,0.006451377,0.15708034,0.0008438173,0.0006983868,0.000103324746,0.000601601,0.00020615026,0.047441877,0.15189497,0.6295272,0.002871629],"about_ca_topic_score_codex":0.00010549595,"about_ca_topic_score_gemma":0.00009661096,"teacher_disagreement_score":0.60122246,"about_ca_system_score_codex":0.0000010023051,"about_ca_system_score_gemma":0.0000138743335,"threshold_uncertainty_score":0.99880314},"labels":[],"label_agreement":null},{"id":"W4200028261","doi":"10.1130/2021.2553(30)","title":"Dense melt residues drive mid-ocean-ridge “hotspots”","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Mantle (geology); Geology; Hotspot (geology); Upwelling; Mid-ocean ridge; Plume; Buoyancy; Geophysics; Mantle convection; Mantle wedge; Mantle plume; Partial melting; Thermal; Petrology; Crust; Subduction; Lithosphere; Tectonics; Mechanics; Seismology; Thermodynamics; Oceanography; Physics","score_opus":0.017727884971023865,"score_gpt":0.20788701864502046,"score_spread":0.1901591336739966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200028261","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.032628443,0.002359029,0.000081030696,0.00051297655,0.00079354114,0.00056627736,0.0016341553,0.00019889978,0.9612256],"genre_scores_gemma":[0.17760658,0.0032736058,0.011740982,0.0048902887,0.0016253323,0.0000056149042,0.0018663668,0.00006452812,0.7989267],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99738085,0.000086202344,0.0006181358,0.0007679457,0.00058291195,0.0005639563],"domain_scores_gemma":[0.9981502,0.0003436721,0.00056222186,0.00051777327,0.00019063069,0.00023544735],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022485336,0.0005382074,0.0012013604,0.00003220035,0.00022016573,0.000064730986,0.0005150932,0.00063789514,0.009752072],"category_scores_gemma":[0.000029930208,0.00042357488,0.00080153963,0.000036386482,0.0011414847,0.000044172753,0.00015167127,0.00046992002,0.00029205007],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090474205,0.0003448984,0.009634603,0.002228333,0.0069980696,0.0012717362,0.0074217278,0.001337811,0.009378936,0.054073505,0.54211676,0.36428887],"study_design_scores_gemma":[0.0004916728,0.00074861135,0.010046745,0.00022685667,0.00035393273,0.000024172688,0.00031948363,0.000081153514,0.0016015059,0.029089788,0.95572126,0.0012948129],"about_ca_topic_score_codex":0.0010984854,"about_ca_topic_score_gemma":0.000042668562,"teacher_disagreement_score":0.4136045,"about_ca_system_score_codex":0.000007692134,"about_ca_system_score_gemma":0.00012744979,"threshold_uncertainty_score":0.9998216},"labels":[],"label_agreement":null},{"id":"W4200046331","doi":"10.1038/s41561-021-00871-5","title":"Internal structure of ultralow-velocity zones consistent with origin from a basal magma ocean","year":2021,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Science Foundation","keywords":"Geology; Mantle (geology); Geodynamics; Geophysics; Hotspot (geology); Shear velocity; Seismology; Shear (geology); Tectonics; Petrology; Mechanics","score_opus":0.0053767716639434825,"score_gpt":0.20221712931710223,"score_spread":0.19684035765315874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200046331","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99593174,0.0003560165,0.00027088847,0.00020968849,0.0011211459,0.000078514546,0.0015630631,0.000020750835,0.00044816415],"genre_scores_gemma":[0.9901529,0.000014858073,0.008859786,0.0003594265,0.00016280473,1.18481765e-7,0.00014396793,0.0000030893857,0.00030304573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985228,0.00006655914,0.00019575687,0.00042603843,0.0004994192,0.00028938794],"domain_scores_gemma":[0.9992007,0.00010670786,0.0001297938,0.00026860606,0.00017049305,0.0001237249],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010931849,0.0001631781,0.00026927792,0.000037932008,0.00011114563,0.00010059352,0.0003719521,0.00014029487,0.00154571],"category_scores_gemma":[0.00006742611,0.00011090771,0.000049859573,0.00032838804,0.00023654824,0.00020682921,0.000020857675,0.00028691892,0.000014767306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030995396,0.00007696909,0.7953464,0.00010681662,0.000118615804,0.00035779123,0.000697405,0.0010177405,0.194247,0.0020084307,0.0017718278,0.0039410307],"study_design_scores_gemma":[0.00046815345,0.00013858831,0.9307011,0.000093885756,0.00004474555,0.00003362807,0.00014455615,0.000734893,0.058506023,0.0045102336,0.0042908126,0.0003334325],"about_ca_topic_score_codex":0.0031794512,"about_ca_topic_score_gemma":0.0025047506,"teacher_disagreement_score":0.135741,"about_ca_system_score_codex":0.00000330505,"about_ca_system_score_gemma":0.0002054192,"threshold_uncertainty_score":0.999367},"labels":[],"label_agreement":null},{"id":"W4200046470","doi":"10.1016/j.tecto.2021.229192","title":"Seismic anisotropy evidence for modified lithosphere below the Bohai Sea region, eastern North China Craton","year":2021,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Craton; Lithosphere; Subduction; Seismology; Asthenosphere; Crust; Mantle (geology); Seismic anisotropy; Geophysics; Tectonics","score_opus":0.03314437156956823,"score_gpt":0.24055652568550864,"score_spread":0.2074121541159404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200046470","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870815,0.0007314796,0.009177918,0.0010127237,0.00071933685,0.00043721238,0.00019675055,0.00009534549,0.00054771744],"genre_scores_gemma":[0.99681526,0.00014566374,0.0005823313,0.00038547273,0.00065736874,0.000015440733,0.00017358319,0.000014186482,0.0012106833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850446,0.0001169863,0.00025622494,0.00044040318,0.00025853483,0.00042336222],"domain_scores_gemma":[0.99878055,0.0002113179,0.00014867204,0.0006082567,0.00014454164,0.000106680025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014483427,0.00024178321,0.00029903636,0.000011743798,0.00042366795,0.00022251437,0.00042691195,0.00006891015,0.00015740862],"category_scores_gemma":[0.00005205279,0.00017319038,0.00014354645,0.0003006727,0.000085460866,0.00032148583,0.000045052097,0.00014305052,0.00018229849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016543878,0.0006291615,0.36629018,0.001719864,0.0010833193,0.00037201095,0.00721604,0.27180427,0.010625706,0.012849276,0.04081004,0.28494576],"study_design_scores_gemma":[0.0014301854,0.0006346142,0.744747,0.00028928753,0.0003488282,0.00003335166,0.00020854175,0.16594064,0.01666287,0.042849895,0.02544757,0.0014072472],"about_ca_topic_score_codex":0.0020791334,"about_ca_topic_score_gemma":0.00085687556,"teacher_disagreement_score":0.37845677,"about_ca_system_score_codex":0.0000061282867,"about_ca_system_score_gemma":0.00017540692,"threshold_uncertainty_score":0.70624983},"labels":[],"label_agreement":null},{"id":"W4200387809","doi":"10.1002/essoar.10509005.1","title":"The Mantle Seismic Structure below Canada and Alaska Constrained by a New Absolute P-wavespeed Tomographic Model","year":2021,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; Natural Resources Canada; McGill University; Université du Québec à Montréal","funders":"European Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Electronic mail; World Wide Web; Computer science","score_opus":0.006185550931672435,"score_gpt":0.17507571681827788,"score_spread":0.16889016588660544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200387809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884199,0.0022445444,0.00038590236,0.0016671706,0.0013541568,0.00035987227,0.0039263885,0.00003917127,0.0016028939],"genre_scores_gemma":[0.99154216,0.00046190643,0.0007447491,0.00071767607,0.00014638527,0.0000011182607,0.0011876099,0.00000859024,0.00518979],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99840724,0.00006381377,0.00028856215,0.000502809,0.00032698712,0.00041056224],"domain_scores_gemma":[0.9990558,0.00009613984,0.0001394932,0.0004097177,0.000050705814,0.0002481272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012015509,0.00031772783,0.0003791512,0.00002651897,0.00025971196,0.00050374016,0.0003338923,0.00019069476,0.00087728706],"category_scores_gemma":[0.000011546741,0.00021211627,0.0000652747,0.0000825352,0.00011300044,0.00006302102,0.00012230454,0.00030268801,0.0000023043388],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001760062,0.000030196608,0.006717883,0.0006411277,0.0017029733,0.00025303452,0.0013810702,0.31336188,0.004897992,0.0007829901,0.6329446,0.037110254],"study_design_scores_gemma":[0.00174449,0.000114692026,0.051167853,0.0002578616,0.00052621134,0.00011752711,0.0006913149,0.8213185,0.002425802,0.047099587,0.07144846,0.0030876715],"about_ca_topic_score_codex":0.84624124,"about_ca_topic_score_gemma":0.9291209,"teacher_disagreement_score":0.56149614,"about_ca_system_score_codex":0.0000044102344,"about_ca_system_score_gemma":0.0013837661,"threshold_uncertainty_score":0.96056783},"labels":[],"label_agreement":null},{"id":"W4200499121","doi":"10.5194/gchron-2021-29-ac2","title":"Reply on RC2","year":2021,"lang":"en","type":"peer-review","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Scalable Vector Graphics; Span (engineering); Scroll; Glaucophane; Apatite; Geology; Computer science; Mineralogy; Engineering; Paleontology; World Wide Web; Structural engineering; Mechanical engineering","score_opus":0.026243478714668225,"score_gpt":0.2553907108561439,"score_spread":0.22914723214147567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200499121","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000168877,0.04505977,0.0000054942006,0.057737667,0.017385496,0.0004904461,0.0032518925,0.0001310044,0.8757694],"genre_scores_gemma":[0.00029987303,0.011802094,0.00020529874,0.03772064,0.0017794395,0.0000029709215,0.009882476,0.0000096216445,0.93829757],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985046,0.000092969756,0.00027931595,0.00045056385,0.00041059655,0.00026200185],"domain_scores_gemma":[0.99903846,0.00009929059,0.00012124552,0.0005508287,0.0000830909,0.00010708213],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00028825528,0.00023947941,0.0005679555,0.000033899138,0.00006420008,0.00010068046,0.00028941626,0.00011834594,0.1126456],"category_scores_gemma":[0.00006858554,0.00016832339,0.00014503147,0.000109613495,0.000021279377,0.000040773448,0.0000201151,0.00017853295,0.0050497036],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000023443706,0.000006374091,0.000014650486,0.0006548124,0.000026723817,0.000036529676,0.0000028286806,0.000007840179,0.000002013384,0.00007604282,0.9911245,0.008045324],"study_design_scores_gemma":[0.000040802617,0.00005563009,0.00044422963,0.0009871826,0.00005579209,0.000003826093,0.0000013363021,0.0000047477033,0.000044986653,0.00015588604,0.9979745,0.00023104451],"about_ca_topic_score_codex":0.006037819,"about_ca_topic_score_gemma":0.0011627151,"teacher_disagreement_score":0.1075959,"about_ca_system_score_codex":0.000001404084,"about_ca_system_score_gemma":0.00012314631,"threshold_uncertainty_score":0.995725},"labels":[],"label_agreement":null},{"id":"W4205104093","doi":"10.1130/geol.s.12573998.v1","title":"Supplemental Material: Seismic evidence for craton chiseling and displacement of lithospheric mantle by the Tintina fault in the northern Canadian Cordillera","year":2020,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Lithosphere; Seismology; Mantle (geology); Displacement (psychology); Geophysics; Tectonics","score_opus":0.024598165833506783,"score_gpt":0.25109641818675504,"score_spread":0.22649825235324827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205104093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896145,0.00039356988,0.00007204429,0.0034882554,0.0006704973,0.0013508486,0.004022436,0.0000094432335,0.00037839566],"genre_scores_gemma":[0.99777836,0.00020813862,0.00019432354,0.0004634663,0.00012550579,0.000032987846,0.0010585998,0.000007233433,0.00013141539],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864995,0.00012680356,0.0003462938,0.00034413277,0.00020688376,0.0003259405],"domain_scores_gemma":[0.9993062,0.00016828155,0.00016063213,0.00025202282,0.0000309403,0.00008194557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050142955,0.00020812097,0.00029047945,0.000018640858,0.00014604632,0.00020283245,0.00048473183,0.00007350488,0.0015556215],"category_scores_gemma":[0.000024132007,0.00011665203,0.000051722032,0.0000654926,0.000058984162,0.0000618601,0.00008062785,0.00013662665,0.000010659454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002530186,0.00038040977,0.60413414,0.009202109,0.0014456192,0.00009511074,0.040920448,0.037158474,0.028565092,0.001212739,0.19502778,0.079327896],"study_design_scores_gemma":[0.0035467895,0.0021632304,0.5078423,0.0022625604,0.0011399578,0.000037298774,0.017298829,0.16147894,0.021581464,0.00861377,0.26994607,0.0040887767],"about_ca_topic_score_codex":0.6163924,"about_ca_topic_score_gemma":0.48568013,"teacher_disagreement_score":0.13071226,"about_ca_system_score_codex":0.000008560779,"about_ca_system_score_gemma":0.00013302009,"threshold_uncertainty_score":0.9993571},"labels":[],"label_agreement":null},{"id":"W4205139822","doi":"10.1130/geol.s.12573998","title":"Supplemental Material: Seismic evidence for craton chiseling and displacement of lithospheric mantle by the Tintina fault in the northern Canadian Cordillera","year":2020,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Craton; Geology; Lithosphere; Mantle (geology); Seismology; Displacement (psychology); Fault (geology); Geochemistry; Tectonics","score_opus":0.024598165833506783,"score_gpt":0.25109641818675504,"score_spread":0.22649825235324827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205139822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896145,0.00039356988,0.00007204429,0.0034882554,0.0006704973,0.0013508486,0.004022436,0.0000094432335,0.00037839566],"genre_scores_gemma":[0.99777836,0.00020813862,0.00019432354,0.0004634663,0.00012550579,0.000032987846,0.0010585998,0.000007233433,0.00013141539],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99864995,0.00012680356,0.0003462938,0.00034413277,0.00020688376,0.0003259405],"domain_scores_gemma":[0.9993062,0.00016828155,0.00016063213,0.00025202282,0.0000309403,0.00008194557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00050142955,0.00020812097,0.00029047945,0.000018640858,0.00014604632,0.00020283245,0.00048473183,0.00007350488,0.0015556215],"category_scores_gemma":[0.000024132007,0.00011665203,0.000051722032,0.0000654926,0.000058984162,0.0000618601,0.00008062785,0.00013662665,0.000010659454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002530186,0.00038040977,0.60413414,0.009202109,0.0014456192,0.00009511074,0.040920448,0.037158474,0.028565092,0.001212739,0.19502778,0.079327896],"study_design_scores_gemma":[0.0035467895,0.0021632304,0.5078423,0.0022625604,0.0011399578,0.000037298774,0.017298829,0.16147894,0.021581464,0.00861377,0.26994607,0.0040887767],"about_ca_topic_score_codex":0.6163924,"about_ca_topic_score_gemma":0.48568013,"teacher_disagreement_score":0.13071226,"about_ca_system_score_codex":0.000008560779,"about_ca_system_score_gemma":0.00013302009,"threshold_uncertainty_score":0.9993571},"labels":[],"label_agreement":null},{"id":"W4205286966","doi":"10.1088/1742-6596/1609/1/011001","title":"Preface","year":2020,"lang":"en","type":"article","venue":"Journal of Physics Conference Series","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"China; Library science; Political science; Advisory committee; High pressure; Geography; Public administration; Engineering; Law; Engineering physics","score_opus":0.029947404223201878,"score_gpt":0.21029154557699112,"score_spread":0.18034414135378923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205286966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97658885,0.00025040287,0.007876398,0.0044746073,0.001192432,0.00012757495,0.00014083345,0.000034796867,0.009314113],"genre_scores_gemma":[0.99808884,0.00007005681,0.0008051476,0.00020340922,0.000748476,8.439949e-8,0.00000606823,0.000002450108,0.00007549667],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992947,0.000039744802,0.00022909977,0.00008295001,0.00021915289,0.00013437548],"domain_scores_gemma":[0.99936616,0.000026581798,0.00023788794,0.000069405156,0.00016391464,0.00013606036],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000087243185,0.00009437854,0.00023475109,0.000010267546,0.000053077052,0.00010971971,0.00023179184,0.000026132233,0.0009810649],"category_scores_gemma":[0.000027448628,0.00007019476,0.00006383451,0.00008793388,0.00005682549,0.0006175061,0.000011859199,0.00010964194,0.00011091592],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016884104,0.00016006603,0.041984364,0.0005245872,0.0006294095,0.00028912362,0.017766265,0.012941645,0.19252944,0.09206319,0.017650979,0.6217725],"study_design_scores_gemma":[0.001463528,0.003416096,0.09465734,0.00017414358,0.00020847973,0.00007700466,0.001811759,0.001086837,0.6568179,0.09813493,0.14115337,0.000998626],"about_ca_topic_score_codex":0.00003722609,"about_ca_topic_score_gemma":0.000013295416,"teacher_disagreement_score":0.6207739,"about_ca_system_score_codex":7.934205e-7,"about_ca_system_score_gemma":0.00010788092,"threshold_uncertainty_score":0.99993217},"labels":[],"label_agreement":null},{"id":"W4206244295","doi":"10.1002/essoar.10510179.1","title":"Cratonic Earthquakes in the Crust-Mantle Transition, Western Canada","year":2022,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Crust; Seismology; Mantle (geology); Lithosphere; Transition zone; Discontinuity (linguistics); Epicenter; Continental crust; Geophysics; Tectonics","score_opus":0.011707871345285678,"score_gpt":0.20143673272675405,"score_spread":0.18972886138146838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206244295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9807612,0.00035862916,0.000018894669,0.0024547232,0.0015058974,0.00038970122,0.0011348451,0.00002426003,0.013351873],"genre_scores_gemma":[0.99681866,0.00005944727,0.000028840792,0.001406951,0.000170382,0.000011572322,0.000737818,0.0000040841987,0.0007622681],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99849266,0.00025645067,0.0002593634,0.00031109373,0.0004097063,0.0002707444],"domain_scores_gemma":[0.9993898,0.00010513369,0.000071567294,0.00036761817,0.000017775963,0.00004805425],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00040558475,0.00017878035,0.00025007647,0.000038514638,0.00014655235,0.00014840851,0.0005536173,0.0000683248,0.016105706],"category_scores_gemma":[0.000005204673,0.000120437486,0.000053033255,0.0000982917,0.000026153433,0.000054509346,0.00004137242,0.00033689608,0.0000516346],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021793369,0.00025572037,0.14669816,0.0011561832,0.00036509792,0.0015207554,0.0150418505,0.6890652,0.0001294762,0.0021422864,0.13111073,0.012296552],"study_design_scores_gemma":[0.0003093498,0.0000769994,0.7260143,0.00004458863,0.000055984987,0.000012403438,0.0015624631,0.0013461491,0.00009223783,0.0030612743,0.2667407,0.0006834967],"about_ca_topic_score_codex":0.9452519,"about_ca_topic_score_gemma":0.98801047,"teacher_disagreement_score":0.6877191,"about_ca_system_score_codex":0.000006389978,"about_ca_system_score_gemma":0.0005819216,"threshold_uncertainty_score":0.9847937},"labels":[],"label_agreement":null},{"id":"W4206356931","doi":"10.1002/essoar.10507449.1","title":"Altered Mantle Fabric Beneath the Mid-Continent Rift","year":2021,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Vale (Canada); University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Lithosphere; Terrane; Rift; Seismology; Archean; Mantle (geology); Proterozoic; Anisotropy; Geophysics; Paleontology; Tectonics; Physics","score_opus":0.015652102320798063,"score_gpt":0.2104737331146487,"score_spread":0.19482163079385065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206356931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9531227,0.0019200336,0.00030746366,0.0014725142,0.00657737,0.0004674261,0.00049271336,0.00008951061,0.035550278],"genre_scores_gemma":[0.99281543,0.0002567882,0.0005142833,0.0003694315,0.00094438903,0.0000058001615,0.0009701489,0.0000069265225,0.004116802],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99846435,0.00012722041,0.00029440253,0.00047993168,0.00029824697,0.00033586047],"domain_scores_gemma":[0.9989571,0.00008310188,0.00014145856,0.00066448917,0.00005894403,0.00009489353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028500988,0.0002586062,0.00036753216,0.000032464715,0.00015022527,0.00050027494,0.00058347784,0.00014607709,0.012747211],"category_scores_gemma":[0.000015310909,0.0001529794,0.00016239748,0.00007263153,0.000047177695,0.00006397275,0.00020748719,0.00024760645,0.00044331735],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053188024,0.00091508066,0.2710282,0.0039594686,0.0050721113,0.0011439625,0.012411505,0.13990699,0.022898778,0.0073365015,0.3071784,0.22761711],"study_design_scores_gemma":[0.00063581776,0.00011031596,0.7159432,0.00024279795,0.00035991258,0.00002666504,0.00049304514,0.0054023033,0.013652992,0.0062103597,0.25536618,0.0015564215],"about_ca_topic_score_codex":0.01563663,"about_ca_topic_score_gemma":0.0035812187,"teacher_disagreement_score":0.444915,"about_ca_system_score_codex":0.0000017440941,"about_ca_system_score_gemma":0.00009409176,"threshold_uncertainty_score":0.99091834},"labels":[],"label_agreement":null},{"id":"W4212766476","doi":"10.1093/gji/ggac074","title":"The effects of discontinuity topography in the mantle transition zone on global geodynamic observables and mantle heterogeneity","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; Université du Québec à Montréal","funders":"Agence Nationale de la Recherche; University of Florida; Compute Canada; Université du Québec à Montréal; Mississippi State University; National Science Foundation","keywords":"Geology; Transition zone; Geodynamics; Seismic tomography; Mantle (geology); Classification of discontinuities; Geophysics; Core–mantle boundary; Ocean surface topography; Discontinuity (linguistics); Mantle convection; Observable; Subduction; Inversion (geology); Hotspot (geology); Seismology; Tectonics; Geodesy; Physics","score_opus":0.0049328634602136745,"score_gpt":0.21276926268514393,"score_spread":0.20783639922493025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212766476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973957,0.00014749984,0.00006808807,0.0008988257,0.00083401176,0.000109431516,0.00021816255,0.0000035178991,0.0003247679],"genre_scores_gemma":[0.99943906,0.000077054174,0.000019839446,0.00020929419,0.00019192515,0.0000038320736,0.000036696263,0.0000015673963,0.000020723699],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99886435,0.00023649533,0.00018580983,0.000120309596,0.00043567017,0.00015734963],"domain_scores_gemma":[0.99949276,0.00025450738,0.00010426954,0.00009003702,0.00002414785,0.000034300847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034451802,0.0000855015,0.000118447635,0.000026259124,0.00031158427,0.000104496015,0.00035105817,0.000015821235,0.00011113911],"category_scores_gemma":[0.000013329992,0.00004965937,0.00008739856,0.00010591621,0.000093053095,0.00010781628,0.000028454926,0.00017507651,0.0000054691504],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0062063984,0.0039176336,0.33537477,0.00038578192,0.001966124,0.0012751217,0.009044317,0.045378704,0.029319186,0.11199002,0.007404602,0.44773734],"study_design_scores_gemma":[0.0004592174,0.00038895008,0.9788183,0.000017155293,0.000020043199,0.000052754564,0.00021464669,0.0019375134,0.00021238325,0.015838401,0.0019512878,0.00008933873],"about_ca_topic_score_codex":0.00080392393,"about_ca_topic_score_gemma":0.0006359773,"teacher_disagreement_score":0.6434435,"about_ca_system_score_codex":0.0000073108076,"about_ca_system_score_gemma":0.000014036104,"threshold_uncertainty_score":0.23964858},"labels":[],"label_agreement":null},{"id":"W4212857539","doi":"10.1002/essoar.10507449.2","title":"Altered Mantle Fabric Beneath the Mid-Continent Rift","year":2021,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Vale (Canada); University of Manitoba","funders":"","keywords":"World Wide Web; Computer science","score_opus":0.015652102320798063,"score_gpt":0.2104737331146487,"score_spread":0.19482163079385065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212857539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9531227,0.0019200336,0.00030746366,0.0014725142,0.00657737,0.0004674261,0.00049271336,0.00008951061,0.035550278],"genre_scores_gemma":[0.99281543,0.0002567882,0.0005142833,0.0003694315,0.00094438903,0.0000058001615,0.0009701489,0.0000069265225,0.004116802],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99846435,0.00012722041,0.00029440253,0.00047993168,0.00029824697,0.00033586047],"domain_scores_gemma":[0.9989571,0.00008310188,0.00014145856,0.00066448917,0.00005894403,0.00009489353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028500988,0.0002586062,0.00036753216,0.000032464715,0.00015022527,0.00050027494,0.00058347784,0.00014607709,0.012747211],"category_scores_gemma":[0.000015310909,0.0001529794,0.00016239748,0.00007263153,0.000047177695,0.00006397275,0.00020748719,0.00024760645,0.00044331735],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053188024,0.00091508066,0.2710282,0.0039594686,0.0050721113,0.0011439625,0.012411505,0.13990699,0.022898778,0.0073365015,0.3071784,0.22761711],"study_design_scores_gemma":[0.00063581776,0.00011031596,0.7159432,0.00024279795,0.00035991258,0.00002666504,0.00049304514,0.0054023033,0.013652992,0.0062103597,0.25536618,0.0015564215],"about_ca_topic_score_codex":0.01563663,"about_ca_topic_score_gemma":0.0035812187,"teacher_disagreement_score":0.444915,"about_ca_system_score_codex":0.0000017440941,"about_ca_system_score_gemma":0.00009409176,"threshold_uncertainty_score":0.99091834},"labels":[],"label_agreement":null},{"id":"W4213080858","doi":"10.1063/5.0077343","title":"Evidence for multiple liquid–liquid phase transitions in carbon, and the Friedel ordering of its liquid state","year":2022,"lang":"en","type":"article","venue":"Physics of Plasmas","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Friedel oscillations; Physics; Ion; Atom (system on chip); Covalent bond; Fermi liquid theory; Phase transition; Electron; Atomic physics; Chemical physics; Molecular physics; Thermodynamics; Quantum mechanics","score_opus":0.0411156080936541,"score_gpt":0.26319349624486854,"score_spread":0.22207788815121443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213080858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99702173,0.00052047055,0.00023273088,0.000243723,0.0001742651,0.00047481645,0.001207776,0.000009687339,0.00011476814],"genre_scores_gemma":[0.9995699,0.00012033698,0.00012648855,0.0000294809,0.000049033108,0.000032039658,0.000053277003,0.0000057087063,0.0000137151455],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990051,0.00010719206,0.00030189866,0.00018777355,0.00019913344,0.00019893763],"domain_scores_gemma":[0.99904823,0.00054348866,0.0001534988,0.00015550827,0.000058472444,0.000040802373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045527372,0.00011298012,0.00029159678,0.000035704907,0.0001223468,0.000013131042,0.00019543964,0.000017183054,0.00004801925],"category_scores_gemma":[0.000060983486,0.000092372924,0.000060674447,0.00016931476,0.000107770706,0.00015968048,0.00003538912,0.0000850873,8.637247e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.042245556,0.00058978086,0.00077162933,0.0010730431,0.00025405418,0.000011450166,0.023761151,0.38394156,0.534737,0.010047633,0.000085156105,0.0024819868],"study_design_scores_gemma":[0.018258354,0.010034211,0.0010863653,0.00043257402,0.00032970528,0.0000074872314,0.0019820484,0.27129915,0.68468124,0.007832163,0.0029868926,0.0010698194],"about_ca_topic_score_codex":0.0013608992,"about_ca_topic_score_gemma":0.0006142613,"teacher_disagreement_score":0.14994423,"about_ca_system_score_codex":0.0000025382135,"about_ca_system_score_gemma":0.000065141176,"threshold_uncertainty_score":0.37668586},"labels":[],"label_agreement":null},{"id":"W4213155006","doi":"10.1002/pssb.202100644","title":"High‐Temperature, High‐Pressure Reactions of H<sub>2</sub> with CaCO<sub>3</sub> Melts","year":2022,"lang":"en","type":"article","venue":"physica status solidi (b)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Carbonate; Tetrahedron; Chemistry; Hydrogen; Diamondoid; Diamond anvil cell; Chemical reaction; Inorganic chemistry; High pressure; Molecule; Crystallography; Thermodynamics; Organic chemistry","score_opus":0.006224693740365918,"score_gpt":0.18627124619504595,"score_spread":0.18004655245468004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213155006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924384,0.00026159544,0.000010181857,0.00020552325,0.0011494564,0.00045572355,0.0047776964,0.00012395787,0.0005774658],"genre_scores_gemma":[0.9975899,0.00019577991,0.0001421848,0.00013950071,0.00053122645,0.00004135977,0.0012376036,0.00003460366,0.0000878486],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99686015,0.00028014815,0.0004606167,0.00067429553,0.0008630574,0.0008617074],"domain_scores_gemma":[0.9982695,0.00018221284,0.00040689617,0.00067704276,0.00017247425,0.00029187385],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00023170965,0.0004238287,0.0006950779,0.0001286821,0.00070828333,0.000115996605,0.0004131341,0.0000875141,0.0003579047],"category_scores_gemma":[0.000018863766,0.00036685026,0.00015425049,0.00064382714,0.00016910268,0.00041918067,0.000104848164,0.0004505498,0.00011918459],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034199384,0.00023439007,0.00047774086,0.00013035463,0.00030762103,0.0000352523,0.000461448,0.028887084,0.9590343,0.002009098,0.006361716,0.00171898],"study_design_scores_gemma":[0.000996269,0.00068782497,0.026579,0.000042533225,0.0003046562,0.000014445211,0.00019024867,0.00022793408,0.9496515,0.0027796426,0.017838936,0.00068700314],"about_ca_topic_score_codex":0.0051264353,"about_ca_topic_score_gemma":0.0006809177,"teacher_disagreement_score":0.02865915,"about_ca_system_score_codex":0.0000145784825,"about_ca_system_score_gemma":0.00026180205,"threshold_uncertainty_score":0.99987835},"labels":[],"label_agreement":null},{"id":"W4214708145","doi":"10.1051/epjconf/202226005001","title":"First measurement of<sup>25</sup>Al+p resonant scattering relevant to the astrophysical reaction<sup>22</sup>Mg(<i>α</i>,p)<sup>25</sup>Al","year":2022,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Physics; Proton; Reaction rate; Nuclear reaction; Atomic physics; Nuclear physics; Scattering; Resonance (particle physics); Thermonuclear fusion; Parity (physics); Excitation; Analytical Chemistry (journal); Plasma; Chemistry; Quantum mechanics","score_opus":0.021160790342250636,"score_gpt":0.21496531276006967,"score_spread":0.19380452241781904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214708145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98548496,0.00047041327,0.00016447066,0.0073808646,0.000670774,0.0008359447,0.0011240556,0.0000902517,0.0037782865],"genre_scores_gemma":[0.99787384,0.0001634035,0.0005060738,0.0004970463,0.00048752324,0.00005495299,0.0001406399,0.000023360255,0.0002531618],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.9945348,0.0005340052,0.0010461637,0.0008686008,0.0021539924,0.0008624233],"domain_scores_gemma":[0.99763817,0.00037452305,0.00046765432,0.0008717564,0.00033468136,0.00031324584],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016837543,0.0005281357,0.00093200896,0.00021722958,0.0008002888,0.00020805598,0.0013431862,0.00009980062,0.003955646],"category_scores_gemma":[0.00014801585,0.00039320998,0.00029522454,0.0004982657,0.00040471143,0.00033819696,0.00029717054,0.00047613037,0.0002998213],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0035464475,0.0018226086,0.06031462,0.0010606066,0.0020576583,0.00020362427,0.016064433,0.5671086,0.12098224,0.021474753,0.12943257,0.07593187],"study_design_scores_gemma":[0.0011145888,0.0017035846,0.056511816,0.0003010839,0.00021089165,0.000030789968,0.0036113362,0.047721554,0.002617695,0.00085258705,0.8843606,0.00096345524],"about_ca_topic_score_codex":0.0069172718,"about_ca_topic_score_gemma":0.0007670212,"teacher_disagreement_score":0.75492805,"about_ca_system_score_codex":0.000033938803,"about_ca_system_score_gemma":0.0008301216,"threshold_uncertainty_score":0.999852},"labels":[],"label_agreement":null},{"id":"W4220656124","doi":"10.3389/fphy.2022.838524","title":"Electron-Ion Temperature Relaxation in Warm Dense Hydrogen Observed With Picosecond Resolved X-Ray Scattering","year":2022,"lang":"en","type":"article","venue":"Frontiers in Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"SLAC National Accelerator Laboratory; Lawrence Livermore National Laboratory; Office of Science; Basic Energy Sciences; Ministerio de Economía y Competitividad; Deutsche Forschungsgemeinschaft; Fusion Energy Sciences; U.S. Department of Energy","keywords":"Warm dense matter; Ion; Atomic physics; Scattering; Relaxation (psychology); Picosecond; Electron; Hydrogen; X-ray; Thomson scattering; Materials science; Physics; Laser; Optics; Nuclear physics","score_opus":0.008555031162153368,"score_gpt":0.1785406663866248,"score_spread":0.16998563522447144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220656124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99824953,0.0003101997,0.00008888671,0.000084760046,0.00066602504,0.0002729681,0.00007901974,0.000026971404,0.00022165768],"genre_scores_gemma":[0.9983416,0.000023638555,0.0007491249,0.000116665266,0.00018341749,0.00001739367,0.0004165231,0.000010962528,0.00014067622],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.998694,0.00015934014,0.00021238907,0.00032454694,0.00025676418,0.00035292914],"domain_scores_gemma":[0.9995799,0.00002255977,0.00011016152,0.00022213852,0.00001619702,0.00004903549],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026378932,0.00016092393,0.00025444417,0.000077961835,0.00016512632,0.000055009037,0.00022501782,0.000047847596,0.00010999272],"category_scores_gemma":[0.0000056331414,0.00014988899,0.000034273162,0.00041966842,0.000032924807,0.00025267305,0.000027664564,0.00028487598,0.000008915713],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008234369,0.00018219383,0.45777872,0.000091478905,0.00008671913,0.00011475725,0.0028252401,0.4777241,0.048940975,0.00011277413,0.0042850827,0.007034538],"study_design_scores_gemma":[0.0069028717,0.0018299468,0.7894604,0.0002177283,0.00012608894,0.000021194779,0.0022260647,0.04950424,0.08779074,0.025737606,0.03358293,0.0026001432],"about_ca_topic_score_codex":0.0006593093,"about_ca_topic_score_gemma":0.0005412459,"teacher_disagreement_score":0.42821985,"about_ca_system_score_codex":0.000032063483,"about_ca_system_score_gemma":0.0000662592,"threshold_uncertainty_score":0.6112296},"labels":[],"label_agreement":null},{"id":"W4220689979","doi":"10.1029/2022je007180","title":"Low Thermal Conductivity of Carbon Dioxide at High Pressure: Implications for Icy Planetary Interiors","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Planets","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Institute of Biomedical Sciences, Academia Sinica; Ministry of Science and Technology, Taiwan; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Academia Sinica","keywords":"Thermal conductivity; Materials science; Carbon dioxide; Thermal; Thermal conduction; Thermodynamics; Planet; Analytical Chemistry (journal); Chemistry; Composite material; Physics; Astrophysics","score_opus":0.04015844956749759,"score_gpt":0.30048845164616794,"score_spread":0.26033000207867035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220689979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955234,0.00023140405,0.0000048016072,0.00067026645,0.00046397644,0.00037572562,0.0022973164,0.000008078857,0.00042502774],"genre_scores_gemma":[0.9987225,0.000027198115,0.000091393485,0.000030867246,0.0005242978,0.000009443289,0.00026914314,0.000008791253,0.00031635934],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973673,0.00051015744,0.00051152345,0.00024387232,0.0008618445,0.0005052738],"domain_scores_gemma":[0.9976554,0.0011998705,0.00038283772,0.0002916023,0.00023944589,0.00023083757],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013386264,0.00015444234,0.0004940429,0.0001695917,0.00032929707,0.000034147582,0.00065885956,0.000056404067,0.0009328861],"category_scores_gemma":[0.00014474038,0.00012407843,0.00013624268,0.0002276198,0.00019531895,0.00016555008,0.00013660148,0.0004894923,0.000012960734],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009176521,0.0010625891,0.047242913,0.0005763815,0.0009996389,0.00015380068,0.0009155351,0.026195271,0.8786029,0.0015354302,0.015517755,0.018021252],"study_design_scores_gemma":[0.0013594957,0.004320311,0.9400883,0.000049212198,0.00011071019,0.000095639116,0.00009502434,0.00089650915,0.021706896,0.006125775,0.024830788,0.0003213533],"about_ca_topic_score_codex":0.0032310071,"about_ca_topic_score_gemma":0.00021204,"teacher_disagreement_score":0.8928454,"about_ca_system_score_codex":0.000016945696,"about_ca_system_score_gemma":0.0002061332,"threshold_uncertainty_score":0.9999804},"labels":[],"label_agreement":null},{"id":"W4220770747","doi":"10.5194/egusphere-egu22-3062","title":"Heat flow in the cores of Earth, Mercury and Venus from resistivity experiments on Fe-Ni-Si","year":2022,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Electrical resistivity and conductivity; Thermal conductivity; Analytical Chemistry (journal); Venus; Mercury (programming language); Chemistry; Materials science; Inner core; Thermodynamics; Physics; Composite material; Environmental chemistry","score_opus":0.02498434643123465,"score_gpt":0.24475523003157776,"score_spread":0.2197708836003431,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220770747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914435,0.00075600593,0.0000020541506,0.00012705298,0.0010397143,0.00025854248,0.0016871784,0.0000107040905,0.00467524],"genre_scores_gemma":[0.9987924,0.0001469827,0.00017989137,0.0001327349,0.000115367766,0.0000080182235,0.00050965056,0.0000033346498,0.00011160183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986857,0.00030491955,0.00020280473,0.00033634747,0.0003166385,0.00015357441],"domain_scores_gemma":[0.9993018,0.00022333859,0.000051795796,0.00037618718,0.000009893074,0.00003697508],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034759013,0.0001589181,0.0003128168,0.000044285433,0.000086616375,0.00006561496,0.00030758706,0.00008013187,0.0031490803],"category_scores_gemma":[0.000019470826,0.000107610394,0.000043252894,0.000049833754,0.000060533814,0.00003602384,0.00012373007,0.00021387498,0.00001923469],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.006495804,0.002255309,0.62611645,0.001812884,0.001515302,0.0011106218,0.04898949,0.08562417,0.059294093,0.0028391979,0.04033835,0.12360835],"study_design_scores_gemma":[0.00026951465,0.00015890598,0.98426247,0.00007105153,0.000028732733,6.924108e-7,0.000258671,0.0010222022,0.003587376,0.002778523,0.007314976,0.00024691736],"about_ca_topic_score_codex":0.048096735,"about_ca_topic_score_gemma":0.0036603145,"teacher_disagreement_score":0.358146,"about_ca_system_score_codex":0.000001404659,"about_ca_system_score_gemma":0.000037237187,"threshold_uncertainty_score":0.9977622},"labels":[],"label_agreement":null},{"id":"W4220795982","doi":"10.1111/maps.13799","title":"Modeling the pressure–temperature–time evolution of in situ shock veins: A terrestrial case study from Vredefort","year":2022,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada; New Brunswick Innovation Foundation","keywords":"Stishovite; Shock (circulatory); Geology; Shock wave; Coesite; Equation of state; Mechanics; Thermodynamics; High pressure; Physics; Seismology; Subduction","score_opus":0.011935254254324228,"score_gpt":0.20868327422645203,"score_spread":0.1967480199721278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220795982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968181,0.0009663212,0.000011231566,0.000033383705,0.00077263796,0.0004080073,0.0008335645,0.000011993814,0.00014473342],"genre_scores_gemma":[0.99954534,0.000010991165,0.0001498624,0.00002766719,0.00013817023,0.000004035776,0.0001024041,0.0000026042228,0.000018915549],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9981422,0.00023639838,0.00033694762,0.00040178865,0.00057698204,0.00030572957],"domain_scores_gemma":[0.99935186,0.00017647327,0.00006877354,0.00029119127,0.000024769412,0.00008695269],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014087125,0.00014402547,0.0002578509,0.00012532293,0.00063646416,0.00012369671,0.00043492767,0.000031034044,0.00023154869],"category_scores_gemma":[0.000040753934,0.00010585122,0.000027415854,0.00041887388,0.00016873868,0.00024961605,0.00009219016,0.00020538126,0.0000047288804],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005440035,0.00042738378,0.1263448,0.000037345206,0.000113442045,0.0017814619,0.005764335,0.8280897,0.03332075,0.00015492649,0.000092036906,0.0033297902],"study_design_scores_gemma":[0.0013584796,0.001917399,0.1028486,0.00002286717,0.00018856872,0.00042664917,0.0064175758,0.88319224,0.00029395518,0.002213918,0.00059542235,0.00052435073],"about_ca_topic_score_codex":0.071774796,"about_ca_topic_score_gemma":0.005631594,"teacher_disagreement_score":0.06614321,"about_ca_system_score_codex":0.000006261692,"about_ca_system_score_gemma":0.00014380872,"threshold_uncertainty_score":0.93440634},"labels":[],"label_agreement":null},{"id":"W4220846757","doi":"10.5194/egusphere-egu22-8968","title":"The role of subducted fluids on the genesis of deep earthquakes: evidence from deep diamonds and subduction zone thermal modeling","year":2022,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Subduction; Geology; Mantle (geology); Slab; Eclogite; Lawsonite; Crust; Oceanic crust; Transition zone; Geochemistry; Seismology; Geophysics; Tectonics","score_opus":0.01788280585563457,"score_gpt":0.2062747239131961,"score_spread":0.18839191805756153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220846757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894505,0.008116335,0.000685165,0.00016803303,0.0006154448,0.0003361084,0.00020666714,0.000022974467,0.00039873863],"genre_scores_gemma":[0.99744487,0.0017956109,0.0003436614,0.000021182095,0.00020531262,0.000012118053,0.000117957185,0.0000082809465,0.00005102625],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99804777,0.00039431406,0.0004508672,0.00040090428,0.00047989291,0.0002262647],"domain_scores_gemma":[0.9982208,0.0007355249,0.00025663077,0.00063678,0.00009603286,0.000054204287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007759687,0.00022765077,0.00036401665,0.0000474617,0.00031084937,0.00010049644,0.00056111114,0.000114543225,0.0023773897],"category_scores_gemma":[0.000072591385,0.0001269387,0.00010746068,0.0001138075,0.00013820003,0.000102823935,0.00018056385,0.00023459026,0.000009115142],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006853219,0.00006569963,0.034681115,0.00013586626,0.00044492263,0.000003518786,0.0062941364,0.8138867,0.07071614,0.0010384099,0.000036961435,0.072011225],"study_design_scores_gemma":[0.00019664719,0.00026615182,0.1265056,0.00013759464,0.00026027227,0.0000015404686,0.004381234,0.8339277,0.023577992,0.009942678,0.0002920359,0.00051058613],"about_ca_topic_score_codex":0.045581914,"about_ca_topic_score_gemma":0.0022464935,"teacher_disagreement_score":0.09182449,"about_ca_system_score_codex":0.0000030930398,"about_ca_system_score_gemma":0.00005526577,"threshold_uncertainty_score":0.99853456},"labels":[],"label_agreement":null},{"id":"W4220855370","doi":"10.1016/j.xinn.2022.100226","title":"Theory-directed discovery of high-temperature superconductivity in clathrate hydrides at high pressure","year":2022,"lang":"en","type":"article","venue":"The Innovation","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Superconductivity; Room-temperature superconductor; Condensed matter physics; Physics; Materials science; High-temperature superconductivity; Chemistry","score_opus":0.009700427306986389,"score_gpt":0.19851385441972783,"score_spread":0.18881342711274143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220855370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978742,0.00012552607,0.0000054055763,0.0003600889,0.0006662481,0.0002164127,0.0005881472,0.000030175748,0.00013378372],"genre_scores_gemma":[0.9984221,0.000008585976,0.00003944617,0.00008704364,0.00008904345,0.0000074192258,0.0005513801,0.000004340373,0.0007906655],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988191,0.00034923613,0.00025350644,0.000181659,0.00024228987,0.00015421495],"domain_scores_gemma":[0.9994387,0.00013032027,0.00013519851,0.00023271555,0.000054150078,0.00000891866],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008603194,0.00010235976,0.00018581489,0.00009093431,0.0002223607,0.000041311294,0.00021234644,0.00004089913,0.0012187943],"category_scores_gemma":[0.000039055376,0.00007046864,0.000019151865,0.00082690374,0.000063881664,0.00035053727,0.000058351936,0.00016390976,0.000008482069],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006157726,0.00008218315,0.015008691,0.00007193095,0.00008524083,0.000007466749,0.0010797716,0.021745628,0.85766906,0.100354254,0.0013648401,0.0019151365],"study_design_scores_gemma":[0.0006608139,0.00016312937,0.71707904,0.000027004357,0.00004689227,0.000007308976,0.00017297933,0.0005222707,0.15536991,0.12312192,0.0025171738,0.0003115636],"about_ca_topic_score_codex":0.0042899493,"about_ca_topic_score_gemma":0.00054408633,"teacher_disagreement_score":0.7022992,"about_ca_system_score_codex":0.0000060161606,"about_ca_system_score_gemma":0.0000361658,"threshold_uncertainty_score":0.9996942},"labels":[],"label_agreement":null},{"id":"W4220884644","doi":"10.4006/0836-1398-35.1.39","title":"Newtonian gravitation derived by the elastic energy in the Earth’s interior","year":2022,"lang":"en","type":"article","venue":"Physics Essays","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Gravitation; Earth (classical element); Newtonian fluid; Classical mechanics; Gravitational energy; Energy (signal processing); Mechanics; Mathematical physics; Quantum mechanics","score_opus":0.00994644663412718,"score_gpt":0.1987285761475634,"score_spread":0.1887821295134362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220884644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9754583,0.00035337277,0.0018169883,0.0021702868,0.0017418879,0.00034899262,0.0005820237,0.00004423901,0.017483866],"genre_scores_gemma":[0.99869055,0.000010622942,0.000024551173,0.000647368,0.00018610983,0.000021299227,0.0002450811,0.0000042362417,0.00017019674],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9989298,0.00030096457,0.00013732952,0.00016170781,0.00026199638,0.0002081891],"domain_scores_gemma":[0.99950296,0.00018483632,0.00007236209,0.00020124274,0.000013150054,0.000025460318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026495272,0.00010215277,0.00011203098,0.000015780604,0.0003566196,0.00010484668,0.00040243118,0.000013662738,0.00039916812],"category_scores_gemma":[0.000007792962,0.00006286865,0.00004120106,0.00021191983,0.000051236584,0.00010543825,0.000034086086,0.00011956166,0.000042540658],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055512454,0.00063174684,0.018178321,0.00013044,0.00028136288,0.00010834784,0.04425859,0.09791111,0.19143987,0.3447745,0.077241965,0.22448862],"study_design_scores_gemma":[0.0016734859,0.00078069716,0.050103042,0.000034128156,0.0001346307,0.000030086085,0.004855545,0.027790124,0.0059592114,0.67906845,0.22842766,0.0011429528],"about_ca_topic_score_codex":0.0035749644,"about_ca_topic_score_gemma":0.00089070876,"teacher_disagreement_score":0.33429393,"about_ca_system_score_codex":0.0000025969005,"about_ca_system_score_gemma":0.00002559126,"threshold_uncertainty_score":0.54043007},"labels":[],"label_agreement":null},{"id":"W4220964493","doi":"10.1073/pnas.2112386119","title":"Metamorphism-facilitated faulting in deforming orthopyroxene: Implications for global intermediate-depth seismicity","year":2022,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Induced seismicity; Metamorphism; Subduction; Oceanic crust; Lithosphere; Seismology; Crust; Mantle (geology); Brittleness; Metamorphic rock; Petrology; Geophysics; Tectonics","score_opus":0.0417187676568197,"score_gpt":0.29251223745207433,"score_spread":0.25079346979525463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220964493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959595,0.00006381406,0.0000029876612,0.001518678,0.00005418595,0.00029093117,0.00062313635,0.000013374941,0.0014733901],"genre_scores_gemma":[0.99864835,0.000005166508,0.0010440834,0.00021603366,0.000034828918,0.000017593526,0.0000036921676,0.0000011938243,0.00002907527],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987159,0.000013090634,0.00035182387,0.00022213586,0.00050489657,0.00019215408],"domain_scores_gemma":[0.99935967,0.00013735985,0.00034611387,0.000008404711,0.00011857249,0.000029906783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001663481,0.000079300735,0.00016055474,0.00008913984,0.00038056477,0.000023907814,0.0007093991,0.00003117119,0.000042395066],"category_scores_gemma":[0.0002757642,0.000056848454,0.000068859394,0.0007678801,0.00025542345,0.00033577275,0.00009631197,0.00009233994,7.959218e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010775226,0.00010045965,0.8379346,0.00018001733,0.000048684124,1.7157811e-8,0.0010033575,0.02804774,0.08036211,0.042694606,0.0009542763,0.008566364],"study_design_scores_gemma":[0.00020442596,0.000060374445,0.8916334,0.000016430147,0.000011611371,0.000004310413,0.00035079537,0.0075770994,0.006428458,0.092897005,0.00072023505,0.00009587619],"about_ca_topic_score_codex":0.0002950183,"about_ca_topic_score_gemma":0.000006812201,"teacher_disagreement_score":0.07393365,"about_ca_system_score_codex":0.000016486989,"about_ca_system_score_gemma":0.00004792285,"threshold_uncertainty_score":0.29270348},"labels":[],"label_agreement":null},{"id":"W4220995090","doi":"10.5194/egusphere-egu22-13371","title":"Glaucophane plasticity and scale-dependent yield strength from nanoindentation experiments","year":2022,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Nanoindentation; Plasticity; Deformation (meteorology); Materials science; Slip (aerodynamics); Overburden pressure; Deformation mechanism; Grain boundary; Glaucophane; Geology; Cataclastic rock; Strain rate; Grain size; Composite material; Subduction; Geotechnical engineering; Tectonics; Seismology; Thermodynamics","score_opus":0.019596939865206248,"score_gpt":0.23678333826284653,"score_spread":0.21718639839764028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220995090","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903035,0.0003329654,0.00012759665,0.000032310672,0.0024658523,0.00030970262,0.0026430304,0.00006928153,0.0037157407],"genre_scores_gemma":[0.9960722,0.000114826675,0.0007735234,0.00009067107,0.00030855488,0.000011677786,0.0018621612,0.000007285792,0.00075913937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982926,0.00009718382,0.00029830076,0.00060021994,0.00046688595,0.00024476805],"domain_scores_gemma":[0.9992662,0.00016973891,0.00016690158,0.00023118054,0.000020754636,0.00014520778],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000121160534,0.00025959298,0.000337883,0.000056138208,0.00017537849,0.00024068465,0.00028213247,0.00014559303,0.045299005],"category_scores_gemma":[0.000016195254,0.00023098016,0.00005139053,0.000038391583,0.000039658888,0.00011026352,0.00028375507,0.00024137017,0.00014608161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001916298,0.000963188,0.8101359,0.00090973114,0.0017532308,0.00042043303,0.011055181,0.028187014,0.0800663,0.0005385765,0.013710767,0.050343357],"study_design_scores_gemma":[0.0013937934,0.00038860284,0.9105047,0.00014900116,0.0002840565,0.0000057839975,0.0014987271,0.004430375,0.07011021,0.006504616,0.0030853772,0.001644761],"about_ca_topic_score_codex":0.0453847,"about_ca_topic_score_gemma":0.0039397934,"teacher_disagreement_score":0.10036877,"about_ca_system_score_codex":0.0000066489342,"about_ca_system_score_gemma":0.00005894668,"threshold_uncertainty_score":0.9609722},"labels":[],"label_agreement":null},{"id":"W4221088633","doi":"10.5194/egusphere-egu22-1781","title":"Evidence for lithospheric and sublithospheric anisotropy of the eastern Canadian Shield and its margins","year":2022,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Lithosphere; Geology; Seismic anisotropy; Proterozoic; Archean; Seismic tomography; Craton; Geophysics; Seismology; Shear wave splitting; Continental margin; Plate tectonics; Mantle (geology); Paleontology; Tectonics","score_opus":0.045987831785500304,"score_gpt":0.24646357417272444,"score_spread":0.20047574238722413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221088633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988961,0.006201974,0.000056135836,0.00072163204,0.0010874472,0.0007882473,0.0008797558,0.00001365761,0.0012901975],"genre_scores_gemma":[0.99567163,0.00080871023,0.0011020809,0.00019645874,0.00009282504,0.00001586721,0.00003946825,0.000006949996,0.0020660146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99882036,0.000089196175,0.00022840696,0.0003929024,0.00018706886,0.00028203745],"domain_scores_gemma":[0.99917454,0.00014724999,0.00015242805,0.0003070152,0.000042331405,0.00017643791],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031185482,0.00019286873,0.00030846472,0.000021052892,0.00020220429,0.00013764626,0.00040642085,0.000106834465,0.0026403503],"category_scores_gemma":[0.00006160488,0.0001338423,0.00006329899,0.00010919432,0.000058636037,0.00010331225,0.00020437408,0.00015457123,0.00000394119],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000139829,0.00001783826,0.9804532,0.0015353127,0.00014649835,0.000008404201,0.0015777709,0.0016734911,0.00016633859,0.003507797,0.0012967535,0.009476748],"study_design_scores_gemma":[0.0002521345,0.0002144028,0.9616879,0.00021172478,0.0001332955,0.0000057979414,0.00033212942,0.013022218,0.00014515828,0.0037604999,0.019739266,0.00049547566],"about_ca_topic_score_codex":0.43508875,"about_ca_topic_score_gemma":0.24681382,"teacher_disagreement_score":0.18827493,"about_ca_system_score_codex":0.000005707118,"about_ca_system_score_gemma":0.00030827033,"threshold_uncertainty_score":0.99827135},"labels":[],"label_agreement":null},{"id":"W4224045844","doi":"10.1093/gji/ggac143","title":"Contrasts in 2-D and 3-D system behaviour in the modelling of compositionally originating LLSVPs and a mantle featuring dynamically obtained plates","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Ontario; University of Toronto; Canada Foundation for Innovation; Ontario Research Foundation","keywords":"Mantle (geology); Mantle convection; Geology; Geophysics; Plate tectonics; Convection; Transition zone; Shear (geology); Tectonics; Petrology; Physics; Mechanics; Seismology; Subduction","score_opus":0.008030821354180559,"score_gpt":0.20214544461301626,"score_spread":0.1941146232588357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224045844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986254,0.000068536574,0.00029962815,0.00030891836,0.00020115622,0.00008288094,0.00011633534,0.000004008106,0.00029311306],"genre_scores_gemma":[0.9993844,0.000010187434,0.00040285627,0.00003346741,0.00010877244,0.000002651961,0.000042167467,0.0000024210785,0.000013054332],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99899167,0.0001285188,0.0002624126,0.00012782957,0.00035031792,0.00013923994],"domain_scores_gemma":[0.9995476,0.00020909168,0.00012132758,0.000039992752,0.00004623005,0.00003577313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046186242,0.00007984177,0.00015630458,0.00008995946,0.00013648435,0.000095528725,0.00019365997,0.000018046134,0.00006178062],"category_scores_gemma":[0.000007673213,0.000060998093,0.000026026415,0.0000884718,0.00003678286,0.00014379674,0.00003688983,0.00024826106,0.0000010763231],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008279162,0.00046158183,0.37114355,0.00013323163,0.00017419041,0.0008113851,0.004738305,0.56903636,0.0064129177,0.038174838,0.00005438459,0.008031375],"study_design_scores_gemma":[0.00080754876,0.00011131335,0.67705566,0.00006971844,0.000010556729,0.00031455077,0.0007397106,0.31685433,0.000049975606,0.0038354772,0.000034860892,0.00011630451],"about_ca_topic_score_codex":0.0008504968,"about_ca_topic_score_gemma":0.00009521207,"teacher_disagreement_score":0.3059121,"about_ca_system_score_codex":0.000012887419,"about_ca_system_score_gemma":0.000024796745,"threshold_uncertainty_score":0.248743},"labels":[],"label_agreement":null},{"id":"W4224319962","doi":"10.1016/j.scib.2022.04.020","title":"Carbonate melts under lower mantle conditions","year":2022,"lang":"en","type":"article","venue":"Science Bulletin","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Zhejiang University of Technology; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Canada Research Chairs","keywords":"Carbonate; Geology; Mantle (geology); Geochemistry; Earth science; Materials science; Metallurgy","score_opus":0.007723770549816332,"score_gpt":0.20648158131399577,"score_spread":0.19875781076417945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224319962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93279934,0.000072935465,0.00000991188,0.002859955,0.002292633,0.00015195267,0.00036923253,0.000056641627,0.061387412],"genre_scores_gemma":[0.9966732,0.0000038187713,0.00011045034,0.0007672121,0.000075498414,0.0000049969817,0.000040789735,0.0000024299377,0.0023216056],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986488,0.00005445273,0.000121275254,0.0003022054,0.0005216871,0.0003515852],"domain_scores_gemma":[0.9995531,0.000041533644,0.00005076276,0.000210036,0.000033046137,0.00011155504],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000617185,0.00008268391,0.00009852589,0.00007876721,0.00096031075,0.000108058346,0.00046692282,0.000013147619,0.04880036],"category_scores_gemma":[0.000016757973,0.000072778144,0.000032076005,0.0003526284,0.00030316535,0.00007576206,0.00007807647,0.00008945379,0.0013140979],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035221822,0.0007238375,0.026947478,0.00008200298,0.000119876604,0.0006221849,0.003120049,0.34697995,0.14896825,0.11189098,0.351592,0.008601151],"study_design_scores_gemma":[0.00036208594,0.00025079888,0.15048525,0.0000065532276,0.000017574072,0.00003352617,0.00053537707,0.0014033089,0.0016131665,0.010053267,0.8347973,0.0004417955],"about_ca_topic_score_codex":0.0014778808,"about_ca_topic_score_gemma":0.00006372112,"teacher_disagreement_score":0.4832053,"about_ca_system_score_codex":0.000006920412,"about_ca_system_score_gemma":0.00011300152,"threshold_uncertainty_score":0.9994635},"labels":[],"label_agreement":null},{"id":"W4225472685","doi":"10.31223/x57s75","title":"The effect of a weak asthenospheric layer on surface kinematics, subduction dynamics and slab morphology in the lower mantle","year":2022,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Asthenosphere; Subduction; Lithosphere; Slab; Mantle (geology); Slab window; Transition zone; Geophysics; Mantle convection; Seismology; Trench; Geodynamics; Petrology; Oceanic crust; Tectonics; Layer (electronics)","score_opus":0.0072132071596844064,"score_gpt":0.21755146255572935,"score_spread":0.21033825539604495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225472685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918789,0.00022948663,0.00003120178,0.00044357943,0.0014391928,0.0005149608,0.00013392192,0.000011594816,0.005317146],"genre_scores_gemma":[0.9986604,0.00019164433,0.000106143634,0.000038916536,0.000047834128,0.000006338324,0.00012058823,0.0000052044848,0.0008229507],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99852395,0.0005506212,0.00024806056,0.00025190235,0.00023536163,0.00019011225],"domain_scores_gemma":[0.9987612,0.0006367223,0.00016411427,0.00040288293,0.000014190691,0.000020917298],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011588981,0.00017609955,0.00030758244,0.000018796503,0.00012393027,0.00007323195,0.00036707456,0.00009354873,0.0014715295],"category_scores_gemma":[0.000031209984,0.00008665558,0.0000535344,0.00009121011,0.00009279088,0.000025609384,0.00010085321,0.00029191576,0.000025865542],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026094674,0.0003675803,0.18356279,0.0019732642,0.00054388674,0.00013497178,0.0030137242,0.7554391,0.0021721183,0.0140634775,0.011963101,0.024156528],"study_design_scores_gemma":[0.0025742836,0.008360388,0.74976623,0.0002787808,0.0004781315,0.000090059526,0.0028186385,0.19275239,0.002701007,0.021651447,0.016647834,0.0018808269],"about_ca_topic_score_codex":0.0064566764,"about_ca_topic_score_gemma":0.0025170755,"teacher_disagreement_score":0.5662034,"about_ca_system_score_codex":0.0000046639684,"about_ca_system_score_gemma":0.000018878634,"threshold_uncertainty_score":0.99944127},"labels":[],"label_agreement":null},{"id":"W4225568533","doi":"10.1093/gji/ggac110","title":"Mapping the edge of subducted slabs in the lower mantle beneath southern Asia","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Agence Nationale de la Recherche; Deutscher Akademischer Austauschdienst; Deutsche Forschungsgemeinschaft; Providence Health Care","keywords":"Geology; Subduction; Seismology; Mantle (geology); Seismic tomography; Geophysics; Reflection (computer programming); Mantle wedge; Tectonics","score_opus":0.016975111855452318,"score_gpt":0.2139359113769007,"score_spread":0.1969607995214484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225568533","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925539,0.00006421541,0.000042539323,0.0022328133,0.0014838103,0.000087929555,0.00024929934,0.0000049585415,0.0032805307],"genre_scores_gemma":[0.9984349,0.000008173537,0.00003670267,0.00027183152,0.00077757076,0.0000026764228,0.000047912272,0.0000031245886,0.00041713341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861187,0.00021091131,0.00026565074,0.0001171859,0.0006124349,0.00018195985],"domain_scores_gemma":[0.99945724,0.00015184686,0.00016881061,0.00013082467,0.000059409365,0.00003189262],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005715488,0.00008896424,0.00012753851,0.00006196275,0.00025345135,0.000100765224,0.00080628856,0.000016695585,0.003723128],"category_scores_gemma":[0.000021160422,0.00004989778,0.00010088364,0.00018759322,0.000059362563,0.00010190664,0.00005775128,0.00032741125,0.00009423788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003668174,0.004432346,0.27258006,0.00013571259,0.0027650634,0.0024665445,0.09896895,0.11003784,0.10109678,0.0939372,0.090215616,0.21969572],"study_design_scores_gemma":[0.0011258213,0.00045202166,0.82541114,0.000039586546,0.000037777027,0.00033261158,0.007619805,0.006576421,0.0005067253,0.04318233,0.11433561,0.0003801228],"about_ca_topic_score_codex":0.0007926206,"about_ca_topic_score_gemma":0.0000874118,"teacher_disagreement_score":0.5528311,"about_ca_system_score_codex":0.0000066037283,"about_ca_system_score_gemma":0.000042511958,"threshold_uncertainty_score":0.9971876},"labels":[],"label_agreement":null},{"id":"W4225589044","doi":"10.48550/arxiv.2202.05162","title":"Do Magnetars' X-ray luminosities exceed their spin-down luminosities?","year":2022,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magnetar; Pulsar; Physics; Astrophysics; Neutron star; Spin (aerodynamics); Luminosity; Flux (metallurgy); Galaxy","score_opus":0.042664680190190055,"score_gpt":0.17105302527442462,"score_spread":0.12838834508423458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225589044","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96904343,0.0004922946,0.00019963436,0.00005839404,0.0028682277,0.0005126114,0.0018261697,0.0001990989,0.024800114],"genre_scores_gemma":[0.98884547,0.00047882533,0.00008897146,0.00014905595,0.00046058494,0.0000014053562,0.0009993252,0.000020690028,0.008955669],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.997175,0.00033856469,0.00034692395,0.0012266262,0.00021805198,0.0006948445],"domain_scores_gemma":[0.99805117,0.0001635117,0.00036401692,0.0010576369,0.00009539013,0.00026826732],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039167504,0.00059920264,0.0007233921,0.0002729706,0.00053184974,0.00030723496,0.001451081,0.00030302544,0.021017067],"category_scores_gemma":[0.000014250061,0.0006119525,0.0003592526,0.0003271658,0.00028660567,0.00033029154,0.00065818516,0.000674334,0.0005016732],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007126142,0.00027336745,0.10725804,0.0009566782,0.0010341387,0.0020472135,0.004201299,0.8492751,0.00060432724,0.021616833,0.009326504,0.0026939027],"study_design_scores_gemma":[0.004023666,0.0016872811,0.59695816,0.0005659788,0.0019559357,0.000044283715,0.012862131,0.08062692,0.0013932924,0.0984234,0.19294104,0.008517891],"about_ca_topic_score_codex":0.0068138666,"about_ca_topic_score_gemma":0.00050904846,"teacher_disagreement_score":0.76864815,"about_ca_system_score_codex":0.00003771737,"about_ca_system_score_gemma":0.00023497273,"threshold_uncertainty_score":0.99979985},"labels":[],"label_agreement":null},{"id":"W4226204252","doi":"10.21203/rs.3.rs-1001084/v2","title":"Clear evidence against superconductivity in hydrides under high pressure","year":2022,"lang":"en","type":"preprint","venue":"Research Square","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Superconductivity; Meissner effect; Condensed matter physics; Hydride; High pressure; Magnetic field; Physics; Sulfur; Materials science; Thermodynamics; Hydrogen; Quantum mechanics; Metallurgy","score_opus":0.10574697245734943,"score_gpt":0.3581630034515036,"score_spread":0.25241603099415416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226204252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98896927,0.004789397,0.000004274058,0.0008785805,0.001091307,0.0011477799,0.0012274481,0.00007582991,0.0018161313],"genre_scores_gemma":[0.9956279,0.0021599953,0.000104306266,0.00004732398,0.0004448494,0.000060103746,0.0005774723,0.000020432335,0.000957663],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9934825,0.0022133507,0.00041794038,0.0011051773,0.0017759237,0.0010051194],"domain_scores_gemma":[0.99733657,0.0010665588,0.00009804321,0.0010597716,0.00019620331,0.00024285064],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003849793,0.00033783584,0.00058685493,0.00042295127,0.00042516566,0.00044352555,0.0012475915,0.00031439326,0.013166717],"category_scores_gemma":[0.00042579838,0.00030829807,0.000138884,0.0005535047,0.0002495351,0.0004725174,0.0010105674,0.0022045588,0.00037923976],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011052379,0.00051481085,0.20583713,0.008490888,0.0004025096,0.00080029754,0.0033634442,0.7470809,0.00623918,0.002984458,0.010566096,0.012615025],"study_design_scores_gemma":[0.0004189006,0.00043783858,0.9406243,0.001717581,0.000038551214,0.0000029384084,0.0011312063,0.003442437,0.0008052296,0.022625348,0.027785912,0.0009697321],"about_ca_topic_score_codex":0.052238397,"about_ca_topic_score_gemma":0.0049151396,"teacher_disagreement_score":0.7436385,"about_ca_system_score_codex":0.000039435487,"about_ca_system_score_gemma":0.0005586266,"threshold_uncertainty_score":0.99993694},"labels":[],"label_agreement":null},{"id":"W4226277509","doi":"10.21203/rs.3.rs-1001084/v3","title":"Clear evidence against superconductivity in hydrides under high pressure","year":2022,"lang":"en","type":"preprint","venue":"Research Square","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Superconductivity; Meissner effect; Condensed matter physics; Hydride; High pressure; Physics; Engineering physics; Hydrogen; Quantum mechanics","score_opus":0.10574697245734943,"score_gpt":0.3581630034515036,"score_spread":0.25241603099415416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226277509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98896927,0.004789397,0.000004274058,0.0008785805,0.001091307,0.0011477799,0.0012274481,0.00007582991,0.0018161313],"genre_scores_gemma":[0.9956279,0.0021599953,0.000104306266,0.00004732398,0.0004448494,0.000060103746,0.0005774723,0.000020432335,0.000957663],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9934825,0.0022133507,0.00041794038,0.0011051773,0.0017759237,0.0010051194],"domain_scores_gemma":[0.99733657,0.0010665588,0.00009804321,0.0010597716,0.00019620331,0.00024285064],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.003849793,0.00033783584,0.00058685493,0.00042295127,0.00042516566,0.00044352555,0.0012475915,0.00031439326,0.013166717],"category_scores_gemma":[0.00042579838,0.00030829807,0.000138884,0.0005535047,0.0002495351,0.0004725174,0.0010105674,0.0022045588,0.00037923976],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011052379,0.00051481085,0.20583713,0.008490888,0.0004025096,0.00080029754,0.0033634442,0.7470809,0.00623918,0.002984458,0.010566096,0.012615025],"study_design_scores_gemma":[0.0004189006,0.00043783858,0.9406243,0.001717581,0.000038551214,0.0000029384084,0.0011312063,0.003442437,0.0008052296,0.022625348,0.027785912,0.0009697321],"about_ca_topic_score_codex":0.052238397,"about_ca_topic_score_gemma":0.0049151396,"teacher_disagreement_score":0.7436385,"about_ca_system_score_codex":0.000039435487,"about_ca_system_score_gemma":0.0005586266,"threshold_uncertainty_score":0.99993694},"labels":[],"label_agreement":null},{"id":"W4226435510","doi":"10.1093/nsr/nwac049","title":"A link between the destruction of the mantle root beneath the North China Craton and the Cretaceous Greenhouse","year":2022,"lang":"en","type":"article","venue":"National Science Review","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Cretaceous; Craton; China; Geology; Greenhouse; Mantle (geology); Earth science; Geochemistry; Paleontology; Biology; Geography; Archaeology; Botany; Tectonics","score_opus":0.013141554435348413,"score_gpt":0.2315666706308132,"score_spread":0.21842511619546479,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226435510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93622833,0.03561201,0.000010415377,0.024894293,0.00042729703,0.0009931729,0.0002614779,0.0000110083265,0.0015620029],"genre_scores_gemma":[0.9967894,0.0025063807,0.000016103208,0.00046791192,0.00015461839,0.000010539387,0.000009768245,0.0000014104526,0.000043881944],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9983424,0.00027713843,0.00019166904,0.00015364385,0.00090209884,0.00013304806],"domain_scores_gemma":[0.99927646,0.00022911542,0.00018349945,0.00020946465,0.00007509044,0.000026358779],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0027793692,0.000070038506,0.00013474446,0.000015584545,0.001472026,0.00006823016,0.00076504285,0.000009154279,0.00027548446],"category_scores_gemma":[0.00015226653,0.000024677889,0.000054940294,0.00065182644,0.0005932973,0.00011657336,0.000106762716,0.00012647799,0.000007941558],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066187764,0.00003929265,0.3597032,0.0007087208,0.00015977405,0.0000025436552,0.0021298286,0.011410893,0.0002229651,0.05196827,0.004265533,0.56932276],"study_design_scores_gemma":[0.00008899479,0.000023446364,0.94200164,0.000039566272,0.000057466317,0.000015635655,0.0000097582615,0.00053027965,0.000023021486,0.0060986904,0.051059738,0.00005178502],"about_ca_topic_score_codex":0.0005547354,"about_ca_topic_score_gemma":0.0004763431,"teacher_disagreement_score":0.5822984,"about_ca_system_score_codex":0.0000060108655,"about_ca_system_score_gemma":0.00016984202,"threshold_uncertainty_score":0.9998279},"labels":[],"label_agreement":null},{"id":"W4229032577","doi":"10.1038/s41598-022-11301-w","title":"Phase stability and dense polymorph of the BaCa(CO3)2 barytocalcite carbonate","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministerio de Ciencia e Innovación; Agencia Estatal de Investigación; Generalitat Valenciana; Compute Canada; Yale University","keywords":"Monoclinic crystal system; Crystallography; Carbonate; Phase transition; Phase (matter); Diffraction; Materials science; Powder diffraction; Chemistry; Single crystal; Crystal structure; Thermodynamics","score_opus":0.013665102059808526,"score_gpt":0.21431208653905234,"score_spread":0.2006469844792438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229032577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99188846,0.0002526336,0.0000022378665,0.000103399834,0.005709974,0.00025440074,0.00015882347,0.000015222515,0.0016148414],"genre_scores_gemma":[0.9991827,0.0000014069127,0.000031998698,0.000029459408,0.00003164308,0.000003374667,0.000051770865,0.0000024835188,0.0006651889],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9982853,0.00016980815,0.00034972056,0.00044005158,0.00053586863,0.00021926135],"domain_scores_gemma":[0.99893874,0.000044022774,0.0002475459,0.0006346532,0.000046705445,0.00008831489],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001720772,0.0000932778,0.00016697324,0.00004282511,0.0005930804,0.000111236106,0.00017949363,0.000019486231,0.0027346455],"category_scores_gemma":[0.0000535404,0.00006371258,0.00006296844,0.00031861133,0.00032788937,0.00010372435,0.00011577171,0.000084231695,0.0000037776647],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026638235,0.0006672694,0.46384886,0.00020404077,0.00011417932,0.0008021586,0.0038851365,0.002857788,0.49963003,0.0003987507,0.01305481,0.014270568],"study_design_scores_gemma":[0.0019858545,0.00076597347,0.41653028,0.000047522317,0.00022733709,0.0010513115,0.0010603502,0.005983251,0.27275467,0.059474275,0.23895045,0.0011687406],"about_ca_topic_score_codex":0.0015431978,"about_ca_topic_score_gemma":0.00020212987,"teacher_disagreement_score":0.22687538,"about_ca_system_score_codex":0.0000035141784,"about_ca_system_score_gemma":0.00012711031,"threshold_uncertainty_score":0.998177},"labels":[],"label_agreement":null},{"id":"W4234436235","doi":"10.1007/978-1-4614-8848-4_7","title":"Rocks and Minerals","year":2013,"lang":"en","type":"book-chapter","venue":"Astronomy and astrophysics library","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geochemistry; Geology","score_opus":0.005798801449767731,"score_gpt":0.1496622664210934,"score_spread":0.14386346497132566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234436235","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.063536316,0.0026030543,0.0010572574,0.00037828926,0.0007137528,0.00071403413,0.0021674458,0.00017117786,0.92865866],"genre_scores_gemma":[0.13664502,0.0008023513,0.037254717,0.00041400536,0.0040510306,0.000008683161,0.003920796,0.00010358698,0.8167998],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.998893,0.000016318412,0.00024387626,0.00043480587,0.00012315367,0.00028881675],"domain_scores_gemma":[0.9993316,0.000048732516,0.00016563818,0.00022396173,0.000011596211,0.00021846831],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00002315668,0.00038626642,0.00044831852,0.000054516004,0.0001342981,0.0003099988,0.00016204102,0.00014713872,0.0057775625],"category_scores_gemma":[5.8841664e-7,0.0003359903,0.0000733248,0.000015112581,0.00012880852,0.00079169724,0.00008800876,0.0002085978,0.00047261035],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050293864,0.000015630112,0.0015862698,0.00012612931,0.00026679496,0.000021716733,0.00007159435,0.00010798327,0.0002431653,0.04860085,0.020061875,0.9288477],"study_design_scores_gemma":[0.00020370197,0.0001583479,0.0026454532,0.0000780661,0.00006588593,0.000004239141,0.000009656804,0.000037737587,0.00010556708,0.020316929,0.9759265,0.00044788697],"about_ca_topic_score_codex":0.00011337649,"about_ca_topic_score_gemma":0.00000236521,"teacher_disagreement_score":0.95586467,"about_ca_system_score_codex":6.2547343e-7,"about_ca_system_score_gemma":0.000039490642,"threshold_uncertainty_score":0.9999092},"labels":[],"label_agreement":null},{"id":"W4236021129","doi":"10.1007/978-3-540-78697-9_134","title":"High-temperature cation ordering in olivine: an in situ Mössbauer study of synthetic (Mg0.55Fe0.45)2 SiO4","year":2008,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Mössbauer spectroscopy; Olivine; Octahedron; In situ; Metal; Crystallography; Spectral line; Analytical Chemistry (journal); Materials science; Chemistry; Mineralogy; Crystal structure; Metallurgy; Physics","score_opus":0.010667806912441175,"score_gpt":0.19916513827981738,"score_spread":0.1884973313673762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236021129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96745056,0.00016040674,4.8944037e-7,0.00002892028,0.00046752673,0.00059865153,0.000083305255,0.00002951469,0.031180618],"genre_scores_gemma":[0.9840878,0.00024953726,0.00008301982,0.000029947345,0.00016724966,0.000003553381,0.0002834362,0.000017178016,0.015078227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819964,0.00007991196,0.00057786034,0.0005063032,0.00036481736,0.0002714553],"domain_scores_gemma":[0.99914676,0.00007763727,0.00018932145,0.00043673307,0.00006209603,0.00008748093],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025050083,0.0003444559,0.00066827866,0.0002981135,0.000056673372,0.000049304872,0.00029442483,0.00030129333,0.002318096],"category_scores_gemma":[0.000013118406,0.00028554065,0.00004672439,0.00009321432,0.00004598009,0.00021109276,0.000030334912,0.00027847596,0.0001036677],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0042769485,0.011115102,0.2410892,0.006176633,0.0022633495,0.006416168,0.099205054,0.23641548,0.24089763,0.043349773,0.012945224,0.09584945],"study_design_scores_gemma":[0.006685739,0.0047113127,0.93328595,0.0020912495,0.0003736232,0.00007998556,0.001806941,0.0005823559,0.009718298,0.008195764,0.02695503,0.0055137365],"about_ca_topic_score_codex":0.016240925,"about_ca_topic_score_gemma":0.08249158,"teacher_disagreement_score":0.6921968,"about_ca_system_score_codex":0.000007562038,"about_ca_system_score_gemma":0.00007138327,"threshold_uncertainty_score":0.99995965},"labels":[],"label_agreement":null},{"id":"W4236213958","doi":"10.1002/jrs.1022","title":"Raman spectra of molecular crystals at high pressures: VIII—Boron tribromide","year":2003,"lang":"en","type":"article","venue":"Journal of Raman Spectroscopy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Raman spectroscopy; Chemistry; Tribromide; Bromine; Intermolecular force; Wavenumber; Boron; Analytical Chemistry (journal); Spectral line; Ambient pressure; Dissociation (chemistry); Crystallography; Thermodynamics; Molecule; Physical chemistry; Inorganic chemistry; Organic chemistry","score_opus":0.005488187864460924,"score_gpt":0.21124496714351598,"score_spread":0.20575677927905506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236213958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99193996,0.0016980381,0.0005943781,0.00013424575,0.0009198655,0.00019440388,0.00009110243,0.000014927579,0.004413067],"genre_scores_gemma":[0.9926355,0.00028937586,0.0063993502,0.000070661605,0.0002786294,4.51668e-7,0.000014975452,0.000013723478,0.00029735727],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9975722,0.0002582077,0.0008157411,0.000239694,0.00064959936,0.00046456262],"domain_scores_gemma":[0.99831295,0.00012604492,0.00085228024,0.000338844,0.00013087335,0.00023903287],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007677753,0.00025952086,0.000729543,0.00015831117,0.00011016829,0.00009845857,0.00040545376,0.00011259174,0.0045050597],"category_scores_gemma":[0.00009311352,0.00020524289,0.0002460628,0.00019604448,0.00010785177,0.0002836922,0.000017422239,0.00021388756,0.00005788389],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005114435,0.0001029256,0.0066388454,0.00009343596,0.00022980304,0.0002112564,0.00020353388,0.0022584705,0.9826938,0.0030090555,0.0039304146,0.000116996416],"study_design_scores_gemma":[0.0014153074,0.0010933013,0.023110617,0.00008375606,0.00016983126,0.00011883932,0.000053247226,0.00002170163,0.94936746,0.009643253,0.014636091,0.0002865636],"about_ca_topic_score_codex":0.00030271983,"about_ca_topic_score_gemma":0.00008934459,"teacher_disagreement_score":0.033326328,"about_ca_system_score_codex":0.000018185705,"about_ca_system_score_gemma":0.00012991286,"threshold_uncertainty_score":0.99640495},"labels":[],"label_agreement":null},{"id":"W4236250826","doi":"10.1130/geol.s.14347016.v1","title":"Supplemental Material: Protogenetic sulfide inclusions in diamonds date the diamond formation event using Re-Os isotopes","year":2021,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Diamond; Sulfide; Event (particle physics); Isotope; Geochemistry; Geology; Materials science; Mineralogy; Metallurgy; Nuclear physics; Physics","score_opus":0.024324541465939518,"score_gpt":0.2621348316908554,"score_spread":0.23781029022491587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236250826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921522,0.00012376746,0.00027382214,0.00038508343,0.0014483748,0.0028827752,0.00203163,0.000034579614,0.00066773634],"genre_scores_gemma":[0.99180335,0.00016013738,0.001495509,0.00014889742,0.00026541864,0.00012032279,0.0059074676,0.000011636326,0.00008725175],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9976597,0.00035940288,0.00069140375,0.00045906773,0.00039426,0.00043617844],"domain_scores_gemma":[0.9989714,0.000063320345,0.00026631847,0.0005572741,0.00004917032,0.00009254293],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067400315,0.0003208547,0.00040957384,0.00010476735,0.0002869233,0.00056606886,0.0005462567,0.0001658546,0.012938918],"category_scores_gemma":[0.000020126707,0.00021728099,0.0001041263,0.00015136084,0.00005705556,0.00029232338,0.0007753931,0.00021690807,0.000039430546],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007495559,0.00094564713,0.18095385,0.0045113266,0.00079077174,0.00056633906,0.02981038,0.42358223,0.31272367,0.0006648847,0.010902238,0.03379911],"study_design_scores_gemma":[0.0025733388,0.0003942811,0.4271549,0.0017460065,0.0005610197,0.000071773386,0.0058681387,0.14304504,0.35437283,0.008843384,0.0514104,0.003958896],"about_ca_topic_score_codex":0.028042378,"about_ca_topic_score_gemma":0.028287936,"teacher_disagreement_score":0.2805372,"about_ca_system_score_codex":0.000013930797,"about_ca_system_score_gemma":0.00016304119,"threshold_uncertainty_score":0.9894433},"labels":[],"label_agreement":null},{"id":"W4236254563","doi":"10.1007/978-1-4419-6688-9_1","title":"Introduction","year":2010,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Adiabatic process; Lattice (music); Crystal structure; Statistical physics; Superconductivity; Theoretical physics; Crystal system; Thermodynamics; Physics; Condensed matter physics; Chemistry; Crystallography","score_opus":0.007160309847066926,"score_gpt":0.1705252187693552,"score_spread":0.16336490892228828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236254563","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00024365982,0.000060190996,0.00001515309,0.0004224126,0.0035347764,0.0000869405,0.00011500631,0.000054545075,0.9954673],"genre_scores_gemma":[0.0027110775,0.00006089326,0.0005073093,0.000087262306,0.006242314,1.6675035e-7,0.0005021601,0.000005797699,0.989883],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99939305,0.0000037850539,0.0001263159,0.00022588935,0.00013623218,0.00011472296],"domain_scores_gemma":[0.99960697,0.000013981144,0.000066514425,0.00022697741,0.000028401028,0.00005715694],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000084952946,0.00013833503,0.00017142217,0.00003658088,0.00005955483,0.00005357717,0.000112913964,0.00020901595,0.20248328],"category_scores_gemma":[0.0000037301081,0.000104716055,0.000048438855,0.0000060194893,0.00004331925,0.000059493963,0.00000705532,0.00017508572,0.010405631],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005865343,0.00001014932,0.00011994449,0.00010670014,0.00017471406,0.00003584176,0.0000645884,0.00007084416,0.0041955113,0.60656404,0.27998835,0.10861066],"study_design_scores_gemma":[0.000026332298,0.00002243769,0.00028767504,0.0000030622746,0.000017699544,0.0000036563306,3.5650223e-7,0.000004614182,0.00031567996,0.03146652,0.9677088,0.00014313307],"about_ca_topic_score_codex":0.00035583554,"about_ca_topic_score_gemma":0.0008469481,"teacher_disagreement_score":0.6877205,"about_ca_system_score_codex":4.9398767e-7,"about_ca_system_score_gemma":0.000019710384,"threshold_uncertainty_score":0.9903649},"labels":[],"label_agreement":null},{"id":"W4239280626","doi":"10.5194/sed-3-713-2011","title":"Influence of the Ringwoodite-Perovskite transition on mantle convection in spherical geometry as a function of Clapeyron slope and Rayleigh number","year":2011,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Environment Research Council; Cardiff University","keywords":"Ringwoodite; Mantle convection; Rayleigh number; Geology; Convection; Transition zone; Mantle (geology); Geophysics; Phase transition; Natural convection; Thermodynamics; Tectonics; Lithosphere; Physics; Seismology","score_opus":0.008814590750529181,"score_gpt":0.19736962464654942,"score_spread":0.18855503389602024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239280626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99211866,0.000036116708,0.00006352085,0.00003096493,0.00047540833,0.00029171395,0.000066678615,0.00001312639,0.006903814],"genre_scores_gemma":[0.99953705,0.00008499405,0.000088539244,0.000076980556,0.000056988203,0.000003091655,0.000040999847,0.0000043107952,0.00010705357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988818,0.00012316799,0.0003387645,0.00029154384,0.00022328521,0.00014141615],"domain_scores_gemma":[0.9993968,0.000060823557,0.00021266528,0.00023933544,0.000050640007,0.000039740687],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024501095,0.00016283033,0.0003133777,0.000054042972,0.000036853493,0.00002082537,0.00013833384,0.00020339247,0.0018279897],"category_scores_gemma":[0.00001673667,0.00011173697,0.00006296334,0.00014539398,0.00010266454,0.000106200794,0.00003648229,0.00021903568,0.00004784926],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004656211,0.0007575733,0.59744745,0.0036557734,0.0004587441,0.000017767052,0.005243386,0.28155515,0.06783468,0.0061168964,0.0004423815,0.03181399],"study_design_scores_gemma":[0.00026701708,0.00017980846,0.9846871,0.00017565499,0.000045369154,0.0000025088177,0.000038062564,0.00026239935,0.009556616,0.004489318,0.0001447305,0.00015144302],"about_ca_topic_score_codex":0.014593834,"about_ca_topic_score_gemma":0.00080598285,"teacher_disagreement_score":0.38723963,"about_ca_system_score_codex":0.0000036899205,"about_ca_system_score_gemma":0.000038631613,"threshold_uncertainty_score":0.9990845},"labels":[],"label_agreement":null},{"id":"W4240539275","doi":"10.1002/ange.202009897","title":"The Relative Thermodynamic Stability of Diamond and Graphite","year":2020,"lang":"en","type":"article","venue":"Angewandte Chemie","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Diamond; Graphite; Thermodynamics; Chemical stability; Density functional theory; Degenerate energy levels; Chemistry; Materials science; Computational chemistry; Physics; Organic chemistry","score_opus":0.01513075334390134,"score_gpt":0.19623191635593448,"score_spread":0.18110116301203313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240539275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99393636,0.0008438089,0.000010093631,0.0005740213,0.000059434664,0.0000870622,0.00013861536,0.000012198456,0.004338405],"genre_scores_gemma":[0.9996092,0.00019280017,0.000037407513,0.00006974408,0.000047360572,7.1398244e-7,0.000021392254,0.0000018598573,0.000019544863],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99951816,0.000028235036,0.00011462927,0.0001318415,0.000092816976,0.000114335264],"domain_scores_gemma":[0.9995931,0.00015371929,0.000060246977,0.00010677715,0.00002208102,0.00006409494],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000131305,0.00006975485,0.00011806029,0.000005193918,0.000088246044,0.000020503992,0.000100606485,0.000028844792,0.00016864456],"category_scores_gemma":[0.000037575785,0.00004199909,0.000031681502,0.00008253476,0.00015016485,0.00008491392,0.000015316557,0.00004780929,0.000008870782],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023442204,0.000019635772,0.14070134,0.00014685896,0.00015267413,0.0000061873498,0.00469267,0.000013267349,0.8461512,0.0017763594,0.00062821846,0.0054771737],"study_design_scores_gemma":[0.0003029457,0.00012916124,0.23338969,0.000011566618,0.000043039247,8.2493784e-7,0.00019572873,0.00016969323,0.7491332,0.009473339,0.0069737355,0.00017705749],"about_ca_topic_score_codex":0.00027531188,"about_ca_topic_score_gemma":0.0001366489,"teacher_disagreement_score":0.09701797,"about_ca_system_score_codex":5.1605764e-7,"about_ca_system_score_gemma":0.000010988284,"threshold_uncertainty_score":0.18465398},"labels":[],"label_agreement":null},{"id":"W4240675769","doi":"10.1002/essoar.10505943.1","title":"Structural and thermal evolution of an infant subduction shear zone: Insights from sub-ophiolite metamorphic rocks recovered from Oman Drilling Project Site BT-1B","year":2021,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Ophiolite; Subduction; Geology; Shear zone; Drilling; Metamorphic rock; Geochemistry; Seismology; Earth science; Engineering; Tectonics","score_opus":0.013129172939993121,"score_gpt":0.20534098667225462,"score_spread":0.19221181373226148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240675769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99171937,0.0021297806,0.00029894413,0.000016222808,0.0019681205,0.0005057154,0.0031702898,0.000070057795,0.00012149158],"genre_scores_gemma":[0.9843323,0.00021327104,0.0019781943,0.00001804704,0.00087540265,0.0000040481304,0.0125367725,0.000014285569,0.000027664157],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9973255,0.0004179556,0.00061856676,0.0009232436,0.00041280212,0.00030195393],"domain_scores_gemma":[0.99860007,0.00010011805,0.00043386556,0.0005906887,0.00014163075,0.00013366078],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00018165923,0.00042127032,0.000787381,0.00015706653,0.00017429442,0.00033477673,0.00025008942,0.00039534742,0.0006692311],"category_scores_gemma":[0.000022444532,0.00033595346,0.0001418334,0.00013755464,0.00007380273,0.0006432299,0.00014811059,0.00034200374,0.000011524941],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012816265,0.00012510637,0.087967,0.00049476966,0.0015528222,0.00010024066,0.010419458,0.0880068,0.80006236,0.00022648949,0.000069424204,0.009693912],"study_design_scores_gemma":[0.00089491234,0.0002129825,0.8892032,0.00026728693,0.00046639022,0.000007804096,0.00048180192,0.06779266,0.033225514,0.0061203013,0.00028183972,0.0010453202],"about_ca_topic_score_codex":0.35508525,"about_ca_topic_score_gemma":0.029510247,"teacher_disagreement_score":0.8012362,"about_ca_system_score_codex":0.000013417914,"about_ca_system_score_gemma":0.0002010607,"threshold_uncertainty_score":0.9999092},"labels":[],"label_agreement":null},{"id":"W4241891622","doi":"10.1130/geol.s.14347016","title":"Supplemental Material: Protogenetic sulfide inclusions in diamonds date the diamond formation event using Re-Os isotopes","year":2021,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Diamond; Sulfide; Event (particle physics); Isotope; Geology; Geochemistry; Materials science; Nuclear physics; Metallurgy; Physics; Astrophysics","score_opus":0.024324541465939518,"score_gpt":0.2621348316908554,"score_spread":0.23781029022491587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241891622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921522,0.00012376746,0.00027382214,0.00038508343,0.0014483748,0.0028827752,0.00203163,0.000034579614,0.00066773634],"genre_scores_gemma":[0.99180335,0.00016013738,0.001495509,0.00014889742,0.00026541864,0.00012032279,0.0059074676,0.000011636326,0.00008725175],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9976597,0.00035940288,0.00069140375,0.00045906773,0.00039426,0.00043617844],"domain_scores_gemma":[0.9989714,0.000063320345,0.00026631847,0.0005572741,0.00004917032,0.00009254293],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00067400315,0.0003208547,0.00040957384,0.00010476735,0.0002869233,0.00056606886,0.0005462567,0.0001658546,0.012938918],"category_scores_gemma":[0.000020126707,0.00021728099,0.0001041263,0.00015136084,0.00005705556,0.00029232338,0.0007753931,0.00021690807,0.000039430546],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007495559,0.00094564713,0.18095385,0.0045113266,0.00079077174,0.00056633906,0.02981038,0.42358223,0.31272367,0.0006648847,0.010902238,0.03379911],"study_design_scores_gemma":[0.0025733388,0.0003942811,0.4271549,0.0017460065,0.0005610197,0.000071773386,0.0058681387,0.14304504,0.35437283,0.008843384,0.0514104,0.003958896],"about_ca_topic_score_codex":0.028042378,"about_ca_topic_score_gemma":0.028287936,"teacher_disagreement_score":0.2805372,"about_ca_system_score_codex":0.000013930797,"about_ca_system_score_gemma":0.00016304119,"threshold_uncertainty_score":0.9894433},"labels":[],"label_agreement":null},{"id":"W4242668350","doi":"10.1190/tle22030272.1","title":"Review","year":2003,"lang":"en","type":"article","venue":"The Leading Edge","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Humanities; Philosophy; Art history; Art","score_opus":0.024057026690617475,"score_gpt":0.23941838826216172,"score_spread":0.21536136157154423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242668350","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15730982,0.09985305,0.00014417375,0.0033512812,0.0045963936,0.0006789311,0.0000568511,0.00017468265,0.7338348],"genre_scores_gemma":[0.9876934,0.0034469706,0.00012675817,0.0031800729,0.00021742794,0.0000012637631,0.00001320208,0.0000031792638,0.0053177117],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995599,0.000084414314,0.000077171775,0.00007891131,0.00006135975,0.00013825702],"domain_scores_gemma":[0.99971104,0.000059595564,0.000027966476,0.00016247333,0.000009187834,0.000029767343],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004035704,0.000052572792,0.000099234894,0.0000068225736,0.00009526529,0.000026175087,0.00013359997,0.0000135156715,0.0019545406],"category_scores_gemma":[0.000043089683,0.00002940466,0.000026374983,0.00007429456,0.000024918136,0.000044529228,0.0000029480248,0.00004307752,0.004253765],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011568887,0.00002511322,0.009752701,0.00095860136,0.000072171904,0.00001664189,0.0006123144,0.00022433801,0.0024180068,0.031470235,0.89148754,0.06295077],"study_design_scores_gemma":[0.00003432534,0.000011556734,0.0022823587,0.000117226344,0.000016487287,0.0000056282674,0.0000035092373,0.000010044417,0.0004966461,0.0020198077,0.9949354,0.000067005305],"about_ca_topic_score_codex":0.0000771327,"about_ca_topic_score_gemma":0.000033373784,"teacher_disagreement_score":0.8303836,"about_ca_system_score_codex":5.446516e-7,"about_ca_system_score_gemma":0.000010957527,"threshold_uncertainty_score":0.9989578},"labels":[],"label_agreement":null},{"id":"W4244580903","doi":"10.1007/978-1-4614-3134-3_127","title":"Diapir (Mantle)","year":2015,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Diapir; Geology; Seismology; Tectonics","score_opus":0.03284927308960626,"score_gpt":0.207653310232562,"score_spread":0.17480403714295575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244580903","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00012796071,0.00074226246,0.000008292918,0.000064367654,0.0011319906,0.00011721664,0.00041250885,0.00006491407,0.9973305],"genre_scores_gemma":[0.010699878,0.00012218037,0.0001401638,0.00013646408,0.0007967514,2.657919e-7,0.0005235231,0.000009402185,0.98757136],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991053,0.000008396975,0.00017722484,0.00024755328,0.00027209672,0.00018944425],"domain_scores_gemma":[0.99942327,0.000031077463,0.00008326746,0.0002577792,0.00005166151,0.00015294808],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014502891,0.0002099774,0.00029601683,0.000042938063,0.000044635177,0.000064205524,0.00021059117,0.0001815618,0.071256205],"category_scores_gemma":[0.000004524516,0.00015366102,0.00006840771,0.00000875223,0.000046606976,0.00006832168,0.000018109113,0.000099419325,0.015082052],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044855435,0.000008475741,0.00024135478,0.00009304555,0.00018592262,0.00013667799,0.0000917878,0.00015594986,0.000034187702,0.31990615,0.6267583,0.0523433],"study_design_scores_gemma":[0.00006444323,0.000043615393,0.00024108979,0.0000161406,0.000026188298,0.0000026448124,0.0000012764924,0.000020392794,0.0000123394675,0.06332715,0.93601346,0.00023124862],"about_ca_topic_score_codex":0.00088841695,"about_ca_topic_score_gemma":0.00073479285,"teacher_disagreement_score":0.30925518,"about_ca_system_score_codex":0.0000015168143,"about_ca_system_score_gemma":0.00006298278,"threshold_uncertainty_score":0.9856848},"labels":[],"label_agreement":null},{"id":"W4254027871","doi":"10.1007/978-1-4614-9213-9_127-1","title":"Diapir (Mantle)","year":2014,"lang":"en","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Diapir; Geology; Mantle (geology); Geophysics; Seismology; Tectonics","score_opus":0.01096882194586454,"score_gpt":0.175656412927626,"score_spread":0.16468759098176144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254027871","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00017599108,0.00018958913,0.00007383166,0.00007052854,0.0010537774,0.0001075084,0.0001964304,0.00006571773,0.9980666],"genre_scores_gemma":[0.0293889,0.00012530769,0.00015118954,0.0003373967,0.0009519806,2.786962e-7,0.00038362484,0.000009841142,0.9686515],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99914443,0.000009998698,0.00018604733,0.00026459186,0.00020059418,0.00019434496],"domain_scores_gemma":[0.9994424,0.000058010988,0.000092491915,0.00027925358,0.00002467645,0.0001031427],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000117899945,0.00021529368,0.00031274543,0.00004275834,0.00006302025,0.00006952653,0.00021404741,0.00018207883,0.07858107],"category_scores_gemma":[0.0000036766467,0.0001582084,0.000088531306,0.000006900893,0.00004742204,0.00003455255,0.000014989409,0.0000979824,0.015751846],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031111605,0.0000051381035,0.00036277005,0.00016177306,0.00018231041,0.00005627711,0.000053456966,0.00011626145,0.000069787435,0.71769196,0.17327991,0.107989244],"study_design_scores_gemma":[0.000054489596,0.000042243762,0.0006836443,0.00002211568,0.000027237835,0.0000019976794,4.3273448e-7,0.0000404219,0.00003226865,0.028496213,0.9703492,0.0002497447],"about_ca_topic_score_codex":0.000650326,"about_ca_topic_score_gemma":0.00063807354,"teacher_disagreement_score":0.7970693,"about_ca_system_score_codex":7.6881514e-7,"about_ca_system_score_gemma":0.00002313356,"threshold_uncertainty_score":0.9850145},"labels":[],"label_agreement":null},{"id":"W4254135798","doi":"10.29173/ikc3167","title":"Mantle oxygen fugacity and diamond formation","year":2019,"lang":"en","type":"article","venue":"International Kimberlite Conference Extended Abstracts: 2003","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Mineral redox buffer; Fugacity; Mantle (geology); Diamond; Geology; Oxygen; Geochemistry; Materials science; Chemistry; Metallurgy; Physical chemistry","score_opus":0.011245236614599348,"score_gpt":0.21559765040483478,"score_spread":0.20435241379023544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254135798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9077295,0.00009264307,0.00013126277,0.00025599287,0.001451301,0.00023244864,0.0003771537,0.00004037845,0.089689285],"genre_scores_gemma":[0.99560016,0.00013343137,0.0005755241,0.00016676295,0.00014993911,0.000002587853,0.00044571608,0.0000043109394,0.0029215808],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99879354,0.00003443827,0.00032172317,0.00028438412,0.00032621485,0.00023970476],"domain_scores_gemma":[0.99925476,0.00004647961,0.00017004072,0.00016975938,0.0002437455,0.00011519559],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022102088,0.00016056278,0.00017414881,0.00007205118,0.000063835054,0.00028568914,0.00024078322,0.00008017322,0.0073916693],"category_scores_gemma":[0.000051352734,0.00014025913,0.00003135376,0.000082467435,0.00005042648,0.0008579607,0.000024246363,0.00011485032,0.0014815698],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016110064,0.0006883435,0.16712923,0.00075461925,0.00093889737,0.00037416077,0.0052195503,0.0058234017,0.057459615,0.14226422,0.01972896,0.598008],"study_design_scores_gemma":[0.00044288154,0.000061125706,0.903353,0.000046749803,0.000012744035,0.000033811753,0.00010575108,0.005296001,0.0017541632,0.006058358,0.08255145,0.0002839846],"about_ca_topic_score_codex":0.0007301452,"about_ca_topic_score_gemma":0.00032973292,"teacher_disagreement_score":0.73622376,"about_ca_system_score_codex":0.00000675859,"about_ca_system_score_gemma":0.0000535917,"threshold_uncertainty_score":0.9992959},"labels":[],"label_agreement":null},{"id":"W4254332257","doi":"10.1002/essoar.10501064.1","title":"Surface-Wave Images of Western Canada: Lithospheric Variations Across the Cordillera/Craton Boundary","year":2019,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"","keywords":"Geology; Craton; Lithosphere; Asthenosphere; Mantle (geology); Seismology; Slab; Low-velocity zone; Geophysics; Tectonics","score_opus":0.01529986452405085,"score_gpt":0.22299140359564557,"score_spread":0.2076915390715947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254332257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9754137,0.00082573184,0.00040417415,0.00064249965,0.004026166,0.00064000755,0.005500901,0.000037712234,0.012509129],"genre_scores_gemma":[0.993987,0.00013379518,0.00052093185,0.00021065527,0.00019068911,0.0000022831766,0.0005079444,0.000009090628,0.0044375905],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982012,0.00015771117,0.0004301696,0.00039410795,0.00044254828,0.00037425343],"domain_scores_gemma":[0.9984489,0.00024132016,0.0003464233,0.00072406145,0.00015609324,0.00008322324],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037949372,0.0002773958,0.0005156436,0.00000850284,0.00022499332,0.00029372808,0.0005057878,0.00015466141,0.004216364],"category_scores_gemma":[0.000020361049,0.00017711907,0.000091789494,0.00010134656,0.00011112621,0.00009447267,0.00020702815,0.00027014976,0.00008090769],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021830015,0.00018709643,0.60474336,0.0019153152,0.0018224479,0.00008779481,0.004130826,0.2927778,0.001834611,0.00043053558,0.07891164,0.012940242],"study_design_scores_gemma":[0.00021582861,0.000059329323,0.9672535,0.00008184087,0.00009740192,0.000004339546,0.00021644382,0.0036474825,0.0015066089,0.00063493854,0.02577192,0.00051035604],"about_ca_topic_score_codex":0.9126358,"about_ca_topic_score_gemma":0.8015697,"teacher_disagreement_score":0.36251014,"about_ca_system_score_codex":0.000009902349,"about_ca_system_score_gemma":0.0012891928,"threshold_uncertainty_score":0.9966939},"labels":[],"label_agreement":null},{"id":"W4254532584","doi":"10.22215/etd/2006-06520","title":"Thermal, density, seismological, and rheological structure of the lithospheric-sublithospheric mantle from combined petrological-geophysical modeling: insights on lithospheric stability and the initiation of subduction","year":2006,"lang":"en","type":"dissertation","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; Canadian Heritage","funders":"Natural Sciences and Engineering Research Council of Canada; European Science Foundation","keywords":"Lithosphere; Subduction; Geology; Mantle (geology); Geophysics; Rheology; Thermal; Seismology; Tectonics; Physics; Thermodynamics","score_opus":0.010900286939240422,"score_gpt":0.19322558435266918,"score_spread":0.18232529741342876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254532584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99685776,0.0005998795,0.000094453004,0.00012178415,0.0005437523,0.00063816196,0.00015577553,0.00003408822,0.000954357],"genre_scores_gemma":[0.99831176,0.00015791049,0.00042419796,0.00011047939,0.00012333652,0.0000050766394,0.0007107045,0.000009461531,0.00014704534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973044,0.0006823924,0.00066670834,0.0006078606,0.0004871603,0.00025149673],"domain_scores_gemma":[0.99816,0.0005371144,0.0005913225,0.00045379336,0.00018925004,0.00006854221],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025105715,0.00041195672,0.00090074755,0.000015964855,0.0002588731,0.00008784251,0.00035261645,0.00048544805,0.0007990328],"category_scores_gemma":[0.00011294749,0.00019037699,0.00015844803,0.00026203133,0.0005357837,0.0001284919,0.000062607425,0.00040283724,0.0000026213072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.05139889,0.0038370802,0.5799912,0.0029529927,0.0023063521,0.000055514833,0.016315412,0.073334105,0.122068435,0.11707628,0.00078468706,0.029879035],"study_design_scores_gemma":[0.0011185104,0.0005516031,0.9172909,0.00004987849,0.00022516011,0.0000015166971,0.00039752314,0.023756519,0.006498494,0.04973727,0.000032733395,0.00033987084],"about_ca_topic_score_codex":0.012209802,"about_ca_topic_score_gemma":0.0011107062,"teacher_disagreement_score":0.3372997,"about_ca_system_score_codex":0.0000054251327,"about_ca_system_score_gemma":0.00005276095,"threshold_uncertainty_score":0.99436796},"labels":[],"label_agreement":null},{"id":"W4255303613","doi":"10.1007/978-90-481-8702-7_40","title":"Mantle Viscosity","year":2011,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Viscosity; Thermodynamics; Physics","score_opus":0.019611061916522413,"score_gpt":0.21611295121729557,"score_spread":0.19650188930077317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255303613","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04757641,0.0021661718,0.000026648484,0.00011310593,0.0040399474,0.000829287,0.0010080812,0.000103166574,0.94413716],"genre_scores_gemma":[0.16734384,0.052818105,0.018570056,0.00025791462,0.0026172688,0.000018416114,0.0003163095,0.00010745877,0.7579506],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.991909,0.00017043887,0.0019932375,0.0018815646,0.0026090671,0.0014366361],"domain_scores_gemma":[0.9954792,0.0004699562,0.0020985215,0.0010019079,0.0003993332,0.0005510311],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0024334039,0.0011224065,0.0018844481,0.000833929,0.0010044514,0.00020063511,0.0030494835,0.00057832705,0.021159593],"category_scores_gemma":[0.0001882524,0.0009139878,0.00053680857,0.0008552555,0.0069962866,0.0020588683,0.00034091852,0.000553653,0.00080865994],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014593982,0.0010266115,0.27454773,0.0040475097,0.0012375658,0.0005441003,0.012292446,0.0065571796,0.0017235071,0.5960842,0.014896485,0.085583284],"study_design_scores_gemma":[0.0006575185,0.0045823585,0.08813055,0.00088101585,0.00034875754,0.00007154037,0.0003223282,0.00014455275,0.001560881,0.07205049,0.828517,0.002732959],"about_ca_topic_score_codex":0.00274524,"about_ca_topic_score_gemma":0.007126041,"teacher_disagreement_score":0.81362057,"about_ca_system_score_codex":0.0000021653625,"about_ca_system_score_gemma":0.0015011339,"threshold_uncertainty_score":0.9999693},"labels":[],"label_agreement":null},{"id":"W4255527042","doi":"10.1190/tle24040438.1","title":"Reviews","year":2005,"lang":"en","type":"article","venue":"The Leading Edge","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"College of Veterinarians of British Columbia","funders":"","keywords":"Interpretation (philosophy); Humanities; Philosophy; Art history; Art; Linguistics","score_opus":0.028717841890263513,"score_gpt":0.2449261900483946,"score_spread":0.2162083481581311,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255527042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7213638,0.0077149733,0.00016526415,0.0059635076,0.0024196254,0.00048779108,0.00004287137,0.00014532084,0.26169685],"genre_scores_gemma":[0.98869795,0.00024085268,0.00030015022,0.0007877334,0.0011771634,9.442724e-7,0.000011046633,0.00000202913,0.008782145],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995543,0.00005438451,0.00009975855,0.00008284946,0.00006130927,0.00014741949],"domain_scores_gemma":[0.9997167,0.0000454885,0.000035737303,0.00016491833,0.000005706224,0.00003147038],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00037204145,0.000057157376,0.00010622633,0.000010225604,0.00010688615,0.00004402653,0.00018612185,0.000017330847,0.0016725755],"category_scores_gemma":[0.000016681499,0.000031000298,0.00003074002,0.0000548774,0.000026690388,0.00007951993,0.000006504706,0.000047773883,0.015129252],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018299133,0.000016349559,0.0051766145,0.000042340766,0.00002290578,0.0000035290916,0.0016163845,0.000916017,0.0049309903,0.0029954682,0.37162155,0.61263955],"study_design_scores_gemma":[0.000035239293,0.000009463572,0.00643085,0.000009416694,0.000007289692,0.0000019599186,0.00000329369,0.00018395574,0.0006199988,0.00041524597,0.992227,0.000056291196],"about_ca_topic_score_codex":0.00011061086,"about_ca_topic_score_gemma":0.00019988813,"teacher_disagreement_score":0.62060547,"about_ca_system_score_codex":8.894744e-7,"about_ca_system_score_gemma":0.000005540856,"threshold_uncertainty_score":0.99924004},"labels":[],"label_agreement":null},{"id":"W4281885126","doi":"10.1016/j.saa.2022.121436","title":"Pressure- and temperature-dependent Raman spectra of Ca2Fe2O5 oxygen defect perovskite","year":2022,"lang":"en","type":"article","venue":"Spectrochimica Acta Part A Molecular and Biomolecular Spectroscopy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Raman spectroscopy; Phase transition; Isobaric process; Anharmonicity; Isothermal process; Chemistry; Phase (matter); Materials science; Analytical Chemistry (journal); Thermodynamics; Condensed matter physics; Organic chemistry","score_opus":0.0042204707995490386,"score_gpt":0.19929336450251364,"score_spread":0.1950728937029646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281885126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99073803,0.00508732,0.00014444446,0.000499284,0.00036800856,0.00062358147,0.0005217968,0.00007657418,0.0019409466],"genre_scores_gemma":[0.99769133,0.00033223032,0.0011490895,0.00029603206,0.000141415,0.000015654483,0.00022326216,0.000030255553,0.00012073335],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99691874,0.00033211542,0.000458288,0.0008884646,0.0006805429,0.00072185026],"domain_scores_gemma":[0.9988536,0.000041229763,0.00023061367,0.00055322103,0.000041934658,0.00027936895],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00041361712,0.0004607012,0.00063150167,0.00020404515,0.00047292886,0.00020064558,0.00042498685,0.000105408144,0.0011872746],"category_scores_gemma":[0.000022461887,0.00042816185,0.00022222665,0.00034173185,0.00021408088,0.00013158911,0.00019277072,0.00037743448,0.00001007194],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024090333,0.00007836831,0.0009179035,0.00007045597,0.00031591518,0.00012918434,0.00018793791,0.000059503458,0.9961518,0.0014874381,0.00029817308,0.00006240534],"study_design_scores_gemma":[0.0013878061,0.0015920663,0.011187132,0.000029154095,0.0005590358,0.00033602273,0.00016061962,0.00033415845,0.969558,0.0031226522,0.010853591,0.0008797858],"about_ca_topic_score_codex":0.00059902447,"about_ca_topic_score_gemma":0.00011728481,"teacher_disagreement_score":0.026593836,"about_ca_system_score_codex":0.000010620486,"about_ca_system_score_gemma":0.00009613191,"threshold_uncertainty_score":0.999817},"labels":[],"label_agreement":null},{"id":"W4282944701","doi":"10.1038/s41598-022-14130-z","title":"Resistivity of solid and liquid Fe–Ni–Si with applications to the cores of Earth, Mercury and Venus","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Research Council Canada; Canada Foundation for Innovation; Natural Sciences and Engineering Research Council of Canada; Government of Canada","keywords":"Electrical resistivity and conductivity; Thermal conductivity; Inner core; Materials science; Venus; Heat flux; Adiabatic process; Thermodynamics; Dynamo theory; Outer core; Analytical Chemistry (journal); Magnetic field; Condensed matter physics; Dynamo; Heat transfer; Chemistry; Physics; Composite material; Astrobiology","score_opus":0.010206502487288412,"score_gpt":0.2170353990015076,"score_spread":0.20682889651421918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4282944701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982056,0.00039889093,0.00002392722,0.00012842545,0.0005214964,0.00027116004,0.00019032517,0.0000059328167,0.00025422315],"genre_scores_gemma":[0.9994839,0.000007958106,0.00012724796,0.000012845471,0.000022272814,0.000010667532,0.00003484121,0.0000016425599,0.00029862975],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999136,0.00005011436,0.0001786307,0.00025581173,0.00027445485,0.00010498749],"domain_scores_gemma":[0.9993543,0.000038549246,0.00017164015,0.00033254366,0.000049299342,0.000053690776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008650955,0.000052979143,0.00012718952,0.000043032913,0.00035938487,0.00003843051,0.00008467985,0.000009998768,0.00010981594],"category_scores_gemma":[0.000019277659,0.000035164194,0.000012910373,0.00022374351,0.0002242851,0.00004624101,0.00005221435,0.000035332763,0.0000014982519],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014495145,0.00046152162,0.24351175,0.00083858205,0.00031534376,0.00040235615,0.013043638,0.020807471,0.62157655,0.002598432,0.03599202,0.059002817],"study_design_scores_gemma":[0.00017574284,0.00074875314,0.49062678,0.00003958884,0.00009486631,0.00023355546,0.00046275274,0.00020352064,0.056902748,0.0043670335,0.44584414,0.00030049376],"about_ca_topic_score_codex":0.0007880382,"about_ca_topic_score_gemma":0.0008717627,"teacher_disagreement_score":0.56467384,"about_ca_system_score_codex":5.3751086e-7,"about_ca_system_score_gemma":0.000061166946,"threshold_uncertainty_score":0.2764134},"labels":[],"label_agreement":null},{"id":"W4283209698","doi":"10.1088/1361-648x/ac7a82","title":"Theoretical methods for structural phase transitions in elemental solids at extreme conditions: statics and dynamics","year":2022,"lang":"en","type":"review","venue":"Journal of Physics Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Statics; Phase (matter); Phase transition; Statistical physics; Chemistry; Chemical physics; Materials science; Thermodynamics; Physics; Classical mechanics","score_opus":0.049888255725986146,"score_gpt":0.3757044840068902,"score_spread":0.32581622828090406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283209698","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.014433304,0.93444383,0.01511451,0.00045515702,0.00325289,0.0027532396,0.028931703,0.000024291558,0.0005910775],"genre_scores_gemma":[0.015794162,0.93841076,0.034394655,0.00090681575,0.0013996726,0.000060046783,0.008725495,0.00010985119,0.00019856951],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99804425,0.00042143956,0.00083662645,0.00020331852,0.00021490191,0.00027949063],"domain_scores_gemma":[0.99846923,0.00064239395,0.00058410765,0.00014067422,0.00005180339,0.0001117664],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00053729623,0.00028529836,0.0011326703,0.0001221423,0.00016711821,0.000094282084,0.00020621059,0.000090256406,0.008910281],"category_scores_gemma":[0.00001561927,0.00022422029,0.00032114063,0.00011394569,0.00018026307,0.00017576042,0.000027249624,0.00032581028,0.0000101149935],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002658449,0.00021390927,0.0000902984,0.007961624,0.0009586014,0.0001070267,0.0009857534,0.00018296215,0.00016720558,0.03559645,0.0026304342,0.9508399],"study_design_scores_gemma":[0.007598204,0.0017492418,0.00014524706,0.0025304127,0.005365589,0.0010613953,0.00063535536,0.014782714,0.000074858246,0.37882996,0.58523977,0.0019872303],"about_ca_topic_score_codex":0.000008955258,"about_ca_topic_score_gemma":0.00002189546,"teacher_disagreement_score":0.94885266,"about_ca_system_score_codex":0.000039339266,"about_ca_system_score_gemma":0.0001316254,"threshold_uncertainty_score":0.9919957},"labels":[],"label_agreement":null},{"id":"W4283710441","doi":"10.3749/canmin.2100063","title":"An <i>In Situ</i> Decarbonation Kinetic Study of Calcite Using Synchrotron Radiation XRD","year":2022,"lang":"en","type":"article","venue":"The Canadian Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Calcite; Nucleation; Mineralogy; Materials science; Isothermal process; Thermodynamics; Analytical Chemistry (journal); Chemical engineering; Chemistry","score_opus":0.018501454654545696,"score_gpt":0.23520860331196491,"score_spread":0.21670714865741922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283710441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830693,0.000080168575,0.0000026746761,0.00011743364,0.00026140042,0.000320949,0.00013832604,0.00000565775,0.000766457],"genre_scores_gemma":[0.9995524,0.0000012532778,0.000029053948,0.00014088475,0.00008172041,0.0000045795887,0.00016069114,0.0000033760225,0.000025982967],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990226,0.0002666159,0.00017517594,0.0001464594,0.00018735419,0.00020179158],"domain_scores_gemma":[0.99958813,0.00003007678,0.00007664337,0.00019708392,0.000018073135,0.00009000249],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038814655,0.000076127835,0.00012189684,0.00012048781,0.00025157776,0.00004073059,0.00022559095,0.000018878342,0.00028405362],"category_scores_gemma":[0.00000983778,0.00006316327,0.000015601961,0.00024882518,0.00003720982,0.00007752728,0.000007062036,0.00007618166,0.000003639339],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000537868,0.000102526916,0.14539546,0.000012453818,0.00002618617,0.0000571643,0.0031545293,0.7984959,0.046583295,0.00039109436,0.00038576615,0.0053418777],"study_design_scores_gemma":[0.00059549895,0.0004931162,0.95677215,0.0000037277296,0.00003843108,0.0000068705554,0.0008053417,0.038515944,0.0001779428,0.000394915,0.0019877756,0.00020827445],"about_ca_topic_score_codex":0.9123039,"about_ca_topic_score_gemma":0.9604696,"teacher_disagreement_score":0.8113767,"about_ca_system_score_codex":0.000038457278,"about_ca_system_score_gemma":0.00014450218,"threshold_uncertainty_score":0.3110188},"labels":[],"label_agreement":null},{"id":"W4283818999","doi":"10.2138/rmg.2022.88.15","title":"Carbon and Nitrogen in Mantle-Derived Diamonds","year":2022,"lang":"en","type":"article","venue":"Reviews in Mineralogy and Geochemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Mantle (geology); Nitrogen; Environmental science; Earth science; Carbon fibers; Geology; Geochemistry; Materials science; Chemistry; Composite material","score_opus":0.010317102047697884,"score_gpt":0.21340493355515114,"score_spread":0.20308783150745324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283818999","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96775615,0.029723143,1.0936462e-7,0.00010194528,0.00007209617,0.000109524626,0.000038602695,0.000004104831,0.0021943285],"genre_scores_gemma":[0.99484295,0.004718607,0.00005133974,0.00010801973,0.00004980354,0.000013502413,0.00010164958,0.0000018488522,0.00011227123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992388,0.00011153762,0.00020645317,0.00021426864,0.000055127504,0.00017382237],"domain_scores_gemma":[0.9997563,0.0000391147,0.00005040054,0.000108141794,0.0000035117364,0.00004254226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036906192,0.00009896584,0.00027026655,0.000028873334,0.000050835322,0.000010860964,0.000081699305,0.000041389554,0.00058276154],"category_scores_gemma":[0.000017045311,0.000088383924,0.000017800598,0.000090670976,0.000043792734,0.000027291704,0.00004029251,0.00013065671,0.0000029180067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006151284,0.00003730904,0.92170477,0.00037240854,0.000012791112,0.00011490104,0.00038634607,0.0000879873,0.061563693,0.00003711539,0.00039694543,0.0152242435],"study_design_scores_gemma":[0.0027909782,0.00025492618,0.7807044,0.00027173955,0.000101960395,0.00029972117,0.00038440854,0.0031429464,0.007935113,0.020554554,0.18212622,0.0014330709],"about_ca_topic_score_codex":0.0010656165,"about_ca_topic_score_gemma":0.00051413645,"teacher_disagreement_score":0.18172927,"about_ca_system_score_codex":0.0000021642245,"about_ca_system_score_gemma":0.000011760949,"threshold_uncertainty_score":0.63808304},"labels":[],"label_agreement":null},{"id":"W4285094441","doi":"10.1088/1361-6633/ac805b","title":"Glacial isostatic adjustment: physical models and observational constraints","year":2022,"lang":"en","type":"review","venue":"Reports on Progress in Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Toronto","funders":"","keywords":"Physics; Mantle (geology); Planet; Geophysics; Mantle convection; Convection; Glacial period; Phenomenology (philosophy); Geology; Mechanics; Astronomy; Seismology; Tectonics; Paleontology","score_opus":0.09553254536931917,"score_gpt":0.3229711025306434,"score_spread":0.22743855716132422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285094441","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.001614725,0.9920395,0.000007737668,0.00001255313,0.0012979343,0.0012893195,0.0007488961,0.00005841714,0.0029308866],"genre_scores_gemma":[0.009329725,0.98685116,0.00021261566,0.000045517278,0.0010874874,0.00013224817,0.0022476932,0.000032474218,0.00006110135],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99739367,0.00019854141,0.0006797027,0.0006959904,0.0006432263,0.00038887002],"domain_scores_gemma":[0.9985613,0.00026802762,0.00065462955,0.00037578578,0.000026248781,0.00011399083],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0003095906,0.0004465257,0.0012895846,0.00007381259,0.00014041485,0.00010466004,0.00018948181,0.00011065766,0.0004631676],"category_scores_gemma":[0.000017914306,0.00037119092,0.0002003303,0.0002767874,0.00025296534,0.00023635283,0.00006348155,0.00037253468,0.000018762095],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007295713,0.0001294086,0.00027166173,0.0020430668,0.00006959323,0.00029055227,0.000093203125,0.00028823625,1.734512e-8,0.0035557575,0.000065048465,0.9931862],"study_design_scores_gemma":[0.00033082234,0.00032772985,0.0019694995,0.0035024355,0.00054674,0.00018684726,0.000026106603,0.0026080697,0.000001111365,0.06724067,0.9219911,0.0012688888],"about_ca_topic_score_codex":0.000047024907,"about_ca_topic_score_gemma":0.000007858443,"teacher_disagreement_score":0.99191725,"about_ca_system_score_codex":0.000018762456,"about_ca_system_score_gemma":0.0003602125,"threshold_uncertainty_score":0.999874},"labels":[],"label_agreement":null},{"id":"W4285725666","doi":"10.1063/5.0091404","title":"Clear evidence against superconductivity in hydrides under high pressure","year":2022,"lang":"en","type":"article","venue":"Matter and Radiation at Extremes","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Superconductivity; Meissner effect; Condensed matter physics; Hydride; Lanthanum; High pressure; Critical field; Physics; Engineering physics; Hydrogen; Quantum mechanics; Nuclear physics","score_opus":0.01641248421840561,"score_gpt":0.2080656317065944,"score_spread":0.1916531474881888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285725666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99564797,0.001920273,0.0000055795967,0.0013076501,0.00039987842,0.00013313265,0.00010155775,0.000019427536,0.00046455444],"genre_scores_gemma":[0.99788135,0.00018058099,0.000029314577,0.0007559617,0.000078254576,0.0000054338343,0.000069021466,0.000003948858,0.0009961542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909365,0.00017210627,0.00014595434,0.0002377589,0.00017854945,0.00017199031],"domain_scores_gemma":[0.99967843,0.00009390278,0.00004523352,0.00012553271,0.000007837374,0.00004908825],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023119405,0.00009592702,0.0001396066,0.00006382549,0.00024122812,0.00006413374,0.00010098773,0.000025687814,0.008348749],"category_scores_gemma":[0.000007450339,0.00008443758,0.000021925043,0.000097087104,0.00003569685,0.00033120936,0.00004499209,0.00007735039,0.00011632047],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012896548,0.000042355015,0.92975473,0.00009757741,0.000037021782,0.000014818589,0.0013621207,0.036375087,0.011320315,0.00017368094,0.012176473,0.008516864],"study_design_scores_gemma":[0.00019493345,0.00003262095,0.97694623,0.000010650302,0.000011945223,0.0000037781865,0.00010213673,0.0013325803,0.00035387764,0.0006151854,0.020252684,0.00014336036],"about_ca_topic_score_codex":0.002350948,"about_ca_topic_score_gemma":0.0004256103,"teacher_disagreement_score":0.047191523,"about_ca_system_score_codex":0.000006540835,"about_ca_system_score_gemma":0.000014118828,"threshold_uncertainty_score":0.99255776},"labels":[],"label_agreement":null},{"id":"W4285820543","doi":"10.1039/d2cp02657k","title":"Predicted crystal structures of xenon and alkali metals under high pressures","year":2022,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Program for Jilin University Science and Technology Innovative Research Team; Department of Science and Technology of Jilin Province; National Natural Science Foundation of China","keywords":"Xenon; Electronegativity; Alkali metal; Chemistry; Crystal (programming language); Crystal structure; Chemical physics; Atomic orbital; Crystallography; High pressure; Metal; Thermodynamics; Physics; Nuclear physics; Organic chemistry","score_opus":0.00815338865975915,"score_gpt":0.19969028422147106,"score_spread":0.1915368955617119,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285820543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99649745,0.00011524081,0.000042396405,0.000049426064,0.00008906978,0.00013301839,0.0017941451,0.000057487174,0.0012217847],"genre_scores_gemma":[0.998363,0.0000050164504,0.00011823001,0.000050390972,0.0006072187,0.000008092481,0.00076283223,0.000013109799,0.00007210388],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99833834,0.0000556152,0.00026485574,0.0004422052,0.0005610555,0.0003379463],"domain_scores_gemma":[0.99911445,0.00017258342,0.00018529703,0.00031020943,0.000052315336,0.000165112],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007615427,0.0002642704,0.0004930358,0.00000976715,0.00014424026,0.000040725256,0.000352831,0.00005932445,0.0010106409],"category_scores_gemma":[0.000020601012,0.00023833105,0.000121891644,0.00018532482,0.00025635317,0.00013045815,0.00017035146,0.00027597972,0.0000029199693],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000101177095,0.00014342705,0.00021881676,0.00018149993,0.00012895156,0.0000030005624,0.00012396017,0.0066460413,0.990475,0.0010642892,0.00045435232,0.00045950335],"study_design_scores_gemma":[0.00050831534,0.00006822551,0.0026204018,0.000008189954,0.00014619606,0.0000053246026,0.00006203629,0.0025606311,0.9192066,0.07380308,0.0006548238,0.0003561666],"about_ca_topic_score_codex":0.0003789303,"about_ca_topic_score_gemma":0.0000011284608,"teacher_disagreement_score":0.07273879,"about_ca_system_score_codex":0.0000061287396,"about_ca_system_score_gemma":0.000041998854,"threshold_uncertainty_score":0.99990255},"labels":[],"label_agreement":null},{"id":"W4289188721","doi":"10.1051/0004-6361/201833605","title":"Crustal heating in accreting neutron stars from the nuclear energy-density functional theory","year":2018,"lang":"en","type":"article","venue":"Astronomy and Astrophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds De La Recherche Scientifique - FNRS; European Cooperation in Science and Technology","keywords":"Physics; Neutron star; Crust; Astrophysics; Pulsar; Nuclear matter; Stars; Nuclear astrophysics; Dense matter; Nuclear density; Nuclear physics; Geophysics; Nucleon","score_opus":0.00683334240653824,"score_gpt":0.16857750533711194,"score_spread":0.1617441629305737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289188721","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99361396,0.000030838582,0.0052021965,0.00006745533,0.00027641788,0.000052706626,0.00009873711,0.000018343417,0.00063934975],"genre_scores_gemma":[0.99531513,0.0000028633083,0.0032853025,0.00012623491,0.0011342567,6.9185836e-7,0.000109846864,0.0000053071167,0.000020358384],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991222,0.00011253866,0.0001509401,0.0002407347,0.00011470345,0.00025889257],"domain_scores_gemma":[0.99955493,0.00014507963,0.000074491596,0.00014420801,0.000023717195,0.000057600875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015518186,0.00013270184,0.00014659736,0.000014369077,0.0003320105,0.00011620128,0.00012435729,0.000033316363,0.00059294526],"category_scores_gemma":[0.000006058191,0.00009924243,0.00003613101,0.00006865948,0.0001525817,0.00021871232,0.00004613542,0.0001125615,0.00004967395],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007201452,0.000074403266,0.13507813,0.0000090471585,0.00014314118,0.000010376434,0.0016147092,0.001966671,0.015268591,0.034724288,0.00057944894,0.80981106],"study_design_scores_gemma":[0.0004019097,0.00017541529,0.97578627,0.000028878547,0.000027167278,0.0000010447725,0.00096771895,0.0011125432,0.0006654206,0.0054784156,0.015137922,0.00021730378],"about_ca_topic_score_codex":0.0041039987,"about_ca_topic_score_gemma":0.00039954187,"teacher_disagreement_score":0.84070814,"about_ca_system_score_codex":0.000002865219,"about_ca_system_score_gemma":0.000025551146,"threshold_uncertainty_score":0.64923346},"labels":[],"label_agreement":null},{"id":"W4289523175","doi":"10.1029/2022jb024494","title":"The Effect of a Weak Asthenospheric Layer on Surface Kinematics, Subduction Dynamics and Slab Morphology in the Lower Mantle","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Agence Nationale de la Recherche","keywords":"Slab; Subduction; Geology; Mantle (geology); Kinematics; Slab window; Seismology; Geophysics; Petrology; Tectonics; Oceanic crust; Physics","score_opus":0.016023547870523305,"score_gpt":0.2896933028158653,"score_spread":0.273669754945342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289523175","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978258,0.00014109454,0.000007420044,0.0009184618,0.00034567894,0.00021727307,0.00003131383,0.000001980847,0.0005109658],"genre_scores_gemma":[0.9994009,0.000109686225,0.000033040826,0.000022474693,0.00015032223,0.0000016863977,0.000004723325,0.000004405128,0.00027277722],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99672145,0.0015261924,0.00031642427,0.00012881815,0.00096018426,0.0003469101],"domain_scores_gemma":[0.9974956,0.0019465573,0.00018343811,0.00021096434,0.000095397874,0.00006807785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0037738392,0.00010204864,0.0003073446,0.00005328322,0.0003389338,0.00007756177,0.00041686106,0.000030571002,0.00023200126],"category_scores_gemma":[0.00021456635,0.00005185812,0.00007930751,0.00035670341,0.00022361305,0.00008973608,0.0000611451,0.00066396175,0.000025531359],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.036803976,0.0040295753,0.14624836,0.0012543933,0.0013540623,0.0023177604,0.010641236,0.46200383,0.11806541,0.02750573,0.028484331,0.16129133],"study_design_scores_gemma":[0.0032687178,0.040700562,0.8429861,0.00014247098,0.00008976762,0.0003038333,0.0027857188,0.07854976,0.0060146237,0.014970868,0.0097135315,0.00047401272],"about_ca_topic_score_codex":0.0009809124,"about_ca_topic_score_gemma":0.00021997269,"teacher_disagreement_score":0.69673777,"about_ca_system_score_codex":0.000007596366,"about_ca_system_score_gemma":0.00005604795,"threshold_uncertainty_score":0.28846204},"labels":[],"label_agreement":null},{"id":"W4291227706","doi":"10.1007/s10948-022-06365-8","title":"Evidence Against Superconductivity in Flux Trapping Experiments on Hydrides Under High Pressure","year":2022,"lang":"en","type":"article","venue":"Journal of Superconductivity and Novel Magnetism","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Superconductivity; Flux (metallurgy); Condensed matter physics; Magnetic flux; Trapping; Materials science; Flux pumping; High-temperature superconductivity; Flux pinning; Hydrogen; Physics; Magnetic field","score_opus":0.057055017373477096,"score_gpt":0.24430097251644345,"score_spread":0.18724595514296635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291227706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939651,0.0034264303,0.000036705893,0.00071751303,0.0012830608,0.00019817907,0.00012204209,0.000011130595,0.00023984673],"genre_scores_gemma":[0.99877876,0.00036981524,0.00024098544,0.00021383913,0.00019682608,0.0000040379273,0.0000098224355,0.000008819011,0.00017707574],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9979243,0.00033695498,0.0004659353,0.00035106816,0.0005682706,0.00035346742],"domain_scores_gemma":[0.9990951,0.00032965725,0.00016927741,0.00020234672,0.0000518676,0.00015179833],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011643308,0.0002379543,0.0005052851,0.00023730693,0.00030068096,0.00010928756,0.0003092025,0.00007894612,0.0023572205],"category_scores_gemma":[0.00007328986,0.0002095884,0.00009281769,0.00023244748,0.00013111618,0.0018266812,0.00006981295,0.00054592633,0.0000071950403],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038182715,0.0004915327,0.007110229,0.000113224094,0.00010320642,0.00011297027,0.001588018,0.020397302,0.96018,0.0007911298,0.00036588346,0.008364707],"study_design_scores_gemma":[0.003716999,0.0029085083,0.93506795,0.00069417426,0.00015713937,0.00039576474,0.0033188893,0.0008480325,0.03894226,0.0053424593,0.0074622417,0.0011455927],"about_ca_topic_score_codex":0.0017905394,"about_ca_topic_score_gemma":0.0001452809,"teacher_disagreement_score":0.9279577,"about_ca_system_score_codex":0.00001595672,"about_ca_system_score_gemma":0.000100706435,"threshold_uncertainty_score":0.99855477},"labels":[],"label_agreement":null},{"id":"W4292431773","doi":"10.1038/s41567-022-01693-x","title":"Absence of evidence of superconductivity in sulfur hydride in optical reflectance experiments","year":2022,"lang":"en","type":"article","venue":"Nature Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Superconductivity; Hydride; Reflectivity; Phonon; Sulfur; Condensed matter physics; Infrared; Superconducting transition temperature; Chemistry; Materials science; Atomic physics; Physics; Optics; Hydrogen; Organic chemistry","score_opus":0.05287595183293932,"score_gpt":0.3094850262464322,"score_spread":0.2566090744134929,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292431773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981684,0.0007996065,0.000008255591,0.000055959677,0.0003187877,0.00013124003,0.00005858938,0.0000053356794,0.00045382322],"genre_scores_gemma":[0.9995475,0.00003466318,0.00030571295,0.000031220134,0.000044692606,0.0000039587744,0.000012419341,0.0000029208156,0.000016931064],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9988697,0.0001194615,0.00023118102,0.00022624173,0.0003630503,0.0001903316],"domain_scores_gemma":[0.9994668,0.00017780015,0.00008688661,0.00020869313,0.00003020549,0.000029619903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003243604,0.00009621884,0.00026824902,0.0000434956,0.000031117772,0.0000066275634,0.00027951825,0.000056535555,0.00016579921],"category_scores_gemma":[0.000053839838,0.00008228895,0.000037337388,0.0004273014,0.00006450046,0.0002622557,0.000048564583,0.00034912553,0.0000035064586],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027558053,0.00023488858,0.10115608,0.00014623746,0.000012875736,0.000027312577,0.0015277634,0.01777094,0.8730919,0.003153495,0.00006412959,0.0025388259],"study_design_scores_gemma":[0.00064318406,0.00034330392,0.40010685,0.00024767232,0.000010340938,0.0000035178496,0.00034122446,0.002176308,0.5810994,0.014415095,0.00023767319,0.0003754279],"about_ca_topic_score_codex":0.0012232458,"about_ca_topic_score_gemma":0.00025025324,"teacher_disagreement_score":0.29895076,"about_ca_system_score_codex":0.000008882553,"about_ca_system_score_gemma":0.000064442516,"threshold_uncertainty_score":0.33556458},"labels":[],"label_agreement":null},{"id":"W4294718946","doi":"10.1016/j.xinn.2022.100309","title":"Evolving mantle convection from bottom up to top down","year":2022,"lang":"en","type":"article","venue":"The Innovation","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"National Natural Science Foundation of China; Chinese Academy of Sciences; National Science Foundation","keywords":"Geology; Mantle convection; Mantle (geology); Convection; Geophysics; Meteorology; Seismology; Lithosphere; Geography","score_opus":0.013862378399979445,"score_gpt":0.21538652452610632,"score_spread":0.20152414612612687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294718946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945914,0.000022245033,0.00037946753,0.0010855665,0.0019259165,0.00013534866,0.0001322851,0.000032629086,0.0016951512],"genre_scores_gemma":[0.99782854,9.386743e-7,0.00013426159,0.0007247937,0.0002690712,0.0000050359085,0.0003025475,0.000002023305,0.00073278486],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994217,0.00005644333,0.00013201023,0.00011327669,0.00017443046,0.00010211754],"domain_scores_gemma":[0.9997062,0.00004329492,0.00006061363,0.00013510999,0.000042480824,0.000012310476],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034495478,0.000049440372,0.00006154222,0.000051133367,0.0003188557,0.00006195032,0.00013368874,0.00001322718,0.0067640846],"category_scores_gemma":[0.000019997715,0.000037260434,0.000009608931,0.00047454442,0.000008936542,0.0000990289,0.000024759067,0.00007503131,0.000250072],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057836744,0.00006542294,0.08168734,0.000035092806,0.00017207429,0.000015026801,0.012718885,0.02259596,0.48903456,0.029674597,0.17681932,0.18660334],"study_design_scores_gemma":[0.00047153115,0.00024501563,0.67307127,0.000011818225,0.00003107711,0.0000056155827,0.0009062494,0.010023055,0.020403124,0.031505678,0.2629346,0.00039098793],"about_ca_topic_score_codex":0.0067891194,"about_ca_topic_score_gemma":0.00013624314,"teacher_disagreement_score":0.59138393,"about_ca_system_score_codex":0.0000047855187,"about_ca_system_score_gemma":0.000018915074,"threshold_uncertainty_score":0.99982476},"labels":[],"label_agreement":null},{"id":"W4295531925","doi":"10.1039/d2nr03441g","title":"Extreme structural stability of Ti<sub>0.5</sub>Sn<sub>0.5</sub>O<sub>2</sub> nanoparticles: synergistic effect in the cationic sublattice","year":2022,"lang":"en","type":"article","venue":"Nanoscale","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut interdisciplinaire d'innovation technologique; Université de Sherbrooke","funders":"","keywords":"Cationic polymerization; Materials science; Raman spectroscopy; Nanoscopic scale; Nanoparticle; Phase (matter); Phase transition; Chemical engineering; Crystallography; Chemical physics; Nanotechnology; Condensed matter physics; Chemistry; Optics; Physics; Polymer chemistry","score_opus":0.013622838459411247,"score_gpt":0.20684627945406078,"score_spread":0.19322344099464953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295531925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99640155,0.0004114801,0.000010252298,0.00017840158,0.0011711995,0.0008924847,0.0006388968,0.00007030611,0.00022540092],"genre_scores_gemma":[0.9992108,0.00004269217,0.000019536275,0.0001615408,0.00019224298,0.00005792495,0.00028997115,0.000021223566,0.000004066511],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99529964,0.0013553968,0.0008050296,0.0007318259,0.0009879099,0.0008202125],"domain_scores_gemma":[0.99748236,0.0010212576,0.00035957873,0.0008445253,0.00010993068,0.00018234612],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0016989815,0.00041339386,0.00063311664,0.00013288537,0.0005980538,0.00014725112,0.00077736384,0.00013680328,0.0003107502],"category_scores_gemma":[0.00023853428,0.00032690063,0.00019243483,0.0008406218,0.00029564742,0.00034500874,0.0001300905,0.00040625464,0.00015048891],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002022996,0.00007852402,0.01930688,0.000162043,0.000035900746,0.000024493196,0.0009900955,0.0017389568,0.97193044,0.00016185833,0.00027874226,0.0050897817],"study_design_scores_gemma":[0.0006954179,0.00042884695,0.21316054,0.000028083821,0.00010607896,0.000012200808,0.00024036226,0.0015966558,0.7817845,0.001398115,0.00016741437,0.00038183687],"about_ca_topic_score_codex":0.00074771314,"about_ca_topic_score_gemma":0.002536503,"teacher_disagreement_score":0.19385366,"about_ca_system_score_codex":0.000057366706,"about_ca_system_score_gemma":0.00023632219,"threshold_uncertainty_score":0.9999183},"labels":[],"label_agreement":null},{"id":"W4296293038","doi":"10.1038/s41567-022-01732-7","title":"Experimental observation of open structures in elemental magnesium at terapascal pressures","year":2022,"lang":"en","type":"article","venue":"Nature Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Lawrence Livermore National Laboratory; Engineering and Physical Sciences Research Council; Fusion Energy Sciences; U.S. Department of Energy; National Nuclear Security Administration; Office of Science; National Science Foundation","keywords":"Physics; Diffraction; Chemical physics; Phase (matter); Crystal (programming language); Magnesium; Alkali metal; Planet; Crystal structure; Nanosecond; State of matter; National Ignition Facility; Atomic physics; Molecular physics; Nanotechnology; Condensed matter physics; Crystallography; Laser; Materials science; Optics; Chemistry; Astrophysics; Quantum mechanics; Inertial confinement fusion","score_opus":0.015828398421096096,"score_gpt":0.2617174170889386,"score_spread":0.2458890186678425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296293038","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99619156,0.00039274193,0.0000014550195,0.00004975132,0.0006302516,0.00033235605,0.00057102845,0.000011355313,0.0018195035],"genre_scores_gemma":[0.99854887,0.000003251909,0.0002995672,0.00013987266,0.00015588463,0.0000104058745,0.0006553816,0.00000528046,0.00018149785],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989313,0.00010441664,0.0001945846,0.00023322795,0.0003529599,0.00018353942],"domain_scores_gemma":[0.99962133,0.00003408672,0.00012023692,0.00017286625,0.000017669237,0.00003382297],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013334658,0.000121985126,0.00020362959,0.000028481909,0.00015348522,0.000052041578,0.00049971475,0.000053537155,0.0023523457],"category_scores_gemma":[0.0000028799554,0.00011045484,0.00004062337,0.00017296326,0.00003201341,0.0002665013,0.00021982745,0.00019080294,0.000004798615],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011740122,0.00045346137,0.40595374,0.00013421154,0.00008298446,0.00002948896,0.0030825054,0.021926507,0.5377819,0.015606304,0.007658056,0.006116855],"study_design_scores_gemma":[0.0011357209,0.000305649,0.6995663,0.0000057492884,0.000021892849,0.000002920754,0.0003210643,0.0009050831,0.2808169,0.0069921864,0.009601313,0.00032521342],"about_ca_topic_score_codex":0.0025368207,"about_ca_topic_score_gemma":0.00029766324,"teacher_disagreement_score":0.29361257,"about_ca_system_score_codex":0.000011943488,"about_ca_system_score_gemma":0.000029945091,"threshold_uncertainty_score":0.99855965},"labels":[],"label_agreement":null},{"id":"W4297359859","doi":"10.1029/2022jb024130","title":"The Structure and Dynamics of the Uppermost Mantle of Southwestern Canada From a Joint Analysis of Geophysical Observations","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Asthenosphere; Mantle (geology); Lithosphere; Geology; Craton; Olivine; Geophysics; Low-velocity zone; Petrology; Geochemistry; Seismology; Tectonics","score_opus":0.025633101016576343,"score_gpt":0.2570106688271588,"score_spread":0.23137756781058244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297359859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956149,0.00009185858,0.0000072655325,0.0006445672,0.00020394185,0.00011816394,0.0032850038,0.0000010343015,0.000033248936],"genre_scores_gemma":[0.9996255,0.000033567176,0.000049244998,0.00002279238,0.000116597876,5.2401236e-7,0.000054820335,0.000004204995,0.00009274203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.996906,0.0004968697,0.0005866343,0.00014829618,0.0015666418,0.00029559806],"domain_scores_gemma":[0.9976592,0.0009034865,0.0005418557,0.00034778877,0.00042372587,0.00012392171],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006160207,0.00011200633,0.00056109816,0.00010284248,0.00038706674,0.00004233998,0.00060349883,0.000031221283,0.00021798926],"category_scores_gemma":[0.00017043663,0.00006363194,0.00021589857,0.000911114,0.0003445359,0.00009199592,0.0001889713,0.0004845942,5.011187e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017416648,0.00068841304,0.68828595,0.00028935354,0.007641135,0.000086275584,0.005255462,0.08622482,0.18447411,0.008443045,0.0017915821,0.015078215],"study_design_scores_gemma":[0.00019495045,0.0002479036,0.97667116,0.00001861868,0.00019444943,0.0000017691501,0.00058851164,0.015847458,0.0021076733,0.0037533643,0.00030799536,0.00006616849],"about_ca_topic_score_codex":0.40292645,"about_ca_topic_score_gemma":0.32820588,"teacher_disagreement_score":0.2883852,"about_ca_system_score_codex":0.000012459462,"about_ca_system_score_gemma":0.0006396063,"threshold_uncertainty_score":0.6840526},"labels":[],"label_agreement":null},{"id":"W4307712197","doi":"10.1144/sp531-2022-164","title":"Continents never forget: seismological record of lithospheric deformation 1 billion years ago","year":2022,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Geology; Seismology; Lithosphere; Seismogram; Receiver function; Mantle (geology); Crust; Seismic array; Geophysics; Tectonics","score_opus":0.015949704886971505,"score_gpt":0.21114380240541508,"score_spread":0.19519409751844358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307712197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902784,0.000072015064,0.00063838635,0.0030126073,0.00095592765,0.00038376043,0.00035368683,0.00009249599,0.004212711],"genre_scores_gemma":[0.9929777,0.000091567694,0.002089638,0.0010588826,0.0006825692,0.000036010344,0.0010566061,0.0000043544665,0.002002684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99844784,0.00015335208,0.0004118503,0.0002850834,0.00038083806,0.00032103987],"domain_scores_gemma":[0.9991977,0.00011107567,0.00025833488,0.00022494838,0.000102067126,0.000105840576],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046799617,0.00012644408,0.0002579089,0.000028642566,0.00039422463,0.000056271972,0.00038271977,0.000109650435,0.0148065435],"category_scores_gemma":[0.000072179566,0.00010316232,0.00020807082,0.0006107709,0.00014441775,0.0003420423,0.00011810053,0.00019936425,0.000104887215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002635286,0.0008554565,0.58719784,0.000048953152,0.00019968484,0.0000066661783,0.0014570748,0.008875777,0.00085581536,0.034237854,0.25389093,0.112110406],"study_design_scores_gemma":[0.00022574373,0.00015157505,0.5144051,9.618695e-7,0.00001248698,0.0000029387088,0.00011191264,0.0006903314,0.000017257045,0.004710439,0.47955787,0.0001134183],"about_ca_topic_score_codex":0.0013057144,"about_ca_topic_score_gemma":0.000050072533,"teacher_disagreement_score":0.22566696,"about_ca_system_score_codex":0.000013743534,"about_ca_system_score_gemma":0.00004674046,"threshold_uncertainty_score":0.98609406},"labels":[],"label_agreement":null},{"id":"W4309825461","doi":"10.48550/arxiv.cond-mat/0107110","title":"Effect of nearest neighbor repulsion on the low frequency phase diagram of a quarter-filled Hubbard-Holstein chain","year":2001,"lang":"en","type":"preprint","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quarter (Canadian coin); Phase diagram; k-nearest neighbors algorithm; Chain (unit); Condensed matter physics; Low frequency; Diagram; Phase (matter); Physics; Mathematics; Statistics; Quantum mechanics; Computer science; Geography; Artificial intelligence","score_opus":0.008277162670029583,"score_gpt":0.22131487083690385,"score_spread":0.21303770816687426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309825461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.977566,0.00043737714,0.00087828655,0.0015667394,0.0004266153,0.0009447224,0.0005819564,0.00006627222,0.017532023],"genre_scores_gemma":[0.9975425,0.00030655184,0.0006339082,0.00003109544,0.00004739143,0.000025960466,0.0008429741,0.000016169053,0.00055346376],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9905904,0.0072662383,0.00069417764,0.0005812135,0.00053533586,0.00033261534],"domain_scores_gemma":[0.99342865,0.002931513,0.0008759591,0.0020166934,0.00060968637,0.00013747734],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.006283644,0.0003554929,0.0006562725,0.00013409555,0.00022543583,0.00016878753,0.0011831832,0.0002401506,0.0010943416],"category_scores_gemma":[0.0011455254,0.00025020388,0.0002771589,0.00031708454,0.00026583215,0.00008275657,0.0001986872,0.00039760847,0.00005674687],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00204276,0.0057928613,0.042668596,0.005868127,0.0011940036,0.00011947987,0.027849434,0.0056489436,0.18683296,0.035797093,0.008879766,0.67730594],"study_design_scores_gemma":[0.0053670704,0.000121559024,0.04247835,0.010391702,0.00039908433,0.000013406041,0.00017822684,0.031200003,0.8920895,0.011821756,0.004265587,0.0016737564],"about_ca_topic_score_codex":0.008722412,"about_ca_topic_score_gemma":0.001306595,"teacher_disagreement_score":0.7052565,"about_ca_system_score_codex":0.000010224386,"about_ca_system_score_gemma":0.000119772776,"threshold_uncertainty_score":0.999995},"labels":[],"label_agreement":null},{"id":"W4310527564","doi":"10.2138/am-2022-8441","title":"Witness to strain: Subdomain boundary length and the apparent subdomain boundary density in large strained olivine grains","year":2022,"lang":"en","type":"article","venue":"American Mineralogist","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Olivine; Meteorite; Electron backscatter diffraction; Deformation (meteorology); Geology; Shock metamorphism; Shock (circulatory); Materials science; Mineralogy; Metallurgy; Microstructure; Physics; Astrobiology","score_opus":0.007615793300161861,"score_gpt":0.21651349744705592,"score_spread":0.20889770414689407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310527564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99194354,0.00022915086,0.0002841281,0.0031795285,0.00037884622,0.00057611824,0.0021256867,0.000047426336,0.001235574],"genre_scores_gemma":[0.99668795,0.000032285534,0.00036164385,0.0018689238,0.00018737184,0.000032087246,0.0005496912,0.000012112534,0.00026791327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972589,0.0006883262,0.00039248832,0.0005296313,0.00044244638,0.0006881812],"domain_scores_gemma":[0.9989005,0.0002899723,0.00017661238,0.00039995374,0.000028879402,0.00020408501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012966957,0.00028643498,0.00057232915,0.00012013239,0.00078778726,0.00020452513,0.0004532298,0.000027626946,0.00067460455],"category_scores_gemma":[0.0000862383,0.00021522655,0.00008123844,0.0005848441,0.0012565416,0.00012263804,0.00016834434,0.0002814268,0.000023414594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0063905865,0.0011793405,0.77002645,0.00023255349,0.0005245519,0.0021767379,0.022132857,0.007473677,0.009682333,0.08528689,0.020131353,0.07476266],"study_design_scores_gemma":[0.0023308059,0.0006024627,0.9509263,0.000010799297,0.000038983108,0.00007451294,0.0029874663,0.00077143684,0.00001825806,0.006946809,0.034706693,0.0005854584],"about_ca_topic_score_codex":0.03322197,"about_ca_topic_score_gemma":0.04874449,"teacher_disagreement_score":0.18089986,"about_ca_system_score_codex":0.00002159138,"about_ca_system_score_gemma":0.00013892558,"threshold_uncertainty_score":0.9732159},"labels":[],"label_agreement":null},{"id":"W4310679616","doi":"10.3390/cryst12121752","title":"Thermal Convection in Vesta’s Core from Experimentally-Based Conductive Heat Flow Estimates","year":2022,"lang":"en","type":"article","venue":"Crystals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Electrical resistivity and conductivity; Thermal conductivity; Heat flux; Materials science; Convection; Thermal; Core (optical fiber); Flux (metallurgy); Heat flow; Electrical conductor; Adiabatic process; Analytical Chemistry (journal); Thermodynamics; Condensed matter physics; Heat transfer; Composite material; Metallurgy; Chemistry; Physics","score_opus":0.022432168868389418,"score_gpt":0.23072612285248037,"score_spread":0.20829395398409095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310679616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99677026,0.0002977353,0.00003081128,0.00006526412,0.0006853838,0.00022052613,0.0009660534,0.00004202128,0.0009219384],"genre_scores_gemma":[0.99820226,0.0000015835822,0.0005201449,0.00019261448,0.000073992356,0.000017159373,0.00094351155,0.0000056079775,0.00004312917],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990864,0.00009324473,0.00017126773,0.0002475125,0.0001913188,0.00021030374],"domain_scores_gemma":[0.9996314,0.00010577567,0.000045159955,0.00014545591,0.000013503761,0.000058695994],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015119345,0.00012284656,0.00019479272,0.000048747916,0.0001855994,0.000054632223,0.0001272241,0.000029721627,0.013786476],"category_scores_gemma":[0.00000997805,0.000113971044,0.000035759695,0.00009993417,0.000058444708,0.00013537605,0.000023287655,0.00008566793,0.000053058742],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003370792,0.000113868264,0.042338073,0.000018311892,0.000043438748,0.000089997535,0.0019587702,0.2887959,0.6643303,0.000069575624,0.0010606291,0.00084408483],"study_design_scores_gemma":[0.0047548306,0.0013682713,0.47492278,0.00007430081,0.00008693429,0.000011765202,0.0057103606,0.22266082,0.26614296,0.0071096634,0.015647952,0.0015093606],"about_ca_topic_score_codex":0.007259656,"about_ca_topic_score_gemma":0.00021641987,"teacher_disagreement_score":0.4325847,"about_ca_system_score_codex":0.00001184957,"about_ca_system_score_gemma":0.000056772336,"threshold_uncertainty_score":0.9993511},"labels":[],"label_agreement":null},{"id":"W4311328695","doi":"10.4006/0836-1398-35.4.398","title":"Propagation of Newtonian gravitation derived by the elastic energy","year":2022,"lang":"en","type":"article","venue":"Physics Essays","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Newtonian fluid; Gravitation; Gravitational energy; Classical mechanics; Scalar theories of gravitation; Parameterized post-Newtonian formalism; Mechanics; Classical field theory","score_opus":0.008526113404008868,"score_gpt":0.1891736493405852,"score_spread":0.18064753593657634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311328695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9410703,0.0004213679,0.030016663,0.00087637274,0.0022537217,0.0005042965,0.0014723422,0.00008301172,0.023301935],"genre_scores_gemma":[0.99914414,0.000006199413,0.000051499046,0.00007335538,0.000117943404,0.000008806808,0.0004482697,0.0000034473385,0.00014631382],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9992726,0.000120304736,0.00012630923,0.000119011376,0.000239808,0.00012197523],"domain_scores_gemma":[0.9996138,0.00007831134,0.00012307549,0.00012970291,0.000030359504,0.0000247276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012687668,0.00007109025,0.000099846635,0.000011741408,0.00024932547,0.00002595819,0.00016866872,0.000010871105,0.0002902062],"category_scores_gemma":[0.0000060723232,0.000052825966,0.000031779276,0.0001500857,0.000041935724,0.00009169969,0.000019432791,0.00004836508,0.000012621864],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019467498,0.00028254613,0.0051567303,0.00012418373,0.00016473168,0.000004998684,0.003799484,0.14430152,0.4389664,0.2931873,0.018754026,0.095063396],"study_design_scores_gemma":[0.0011203138,0.0007416094,0.015599962,0.000022767217,0.00018304525,0.0000067595165,0.00075668195,0.06934216,0.07614055,0.8067553,0.028575761,0.0007551136],"about_ca_topic_score_codex":0.0017888672,"about_ca_topic_score_gemma":0.000071045804,"teacher_disagreement_score":0.513568,"about_ca_system_score_codex":0.0000024426301,"about_ca_system_score_gemma":0.000029286333,"threshold_uncertainty_score":0.31775546},"labels":[],"label_agreement":null},{"id":"W4312010699","doi":"10.1103/physrevmaterials.6.123604","title":"Internal mechanical dissipation mechanisms in amorphous silicon","year":2022,"lang":"en","type":"article","venue":"Physical Review Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Regroupement Québécois sur les Matériaux de Pointe","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada","keywords":"Materials science; Quantum decoherence; Relaxation (psychology); Amorphous solid; Silicon; Dissipation; Attenuation; Condensed matter physics; Quantum; Amorphous silicon; Optoelectronics; Physics; Crystalline silicon; Quantum mechanics; Crystallography; Chemistry","score_opus":0.013211461535957807,"score_gpt":0.25480363387121324,"score_spread":0.24159217233525543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312010699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99634427,0.0006954892,0.000043579483,0.00034765134,0.0010832883,0.0005256623,0.00045454083,0.000046046283,0.0004594711],"genre_scores_gemma":[0.99810994,0.00048575262,0.00006793851,0.0007440743,0.00021331254,0.000053965574,0.0002741898,0.00000813823,0.00004269021],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99812186,0.00046821465,0.00041074125,0.0003280441,0.00037709347,0.00029406341],"domain_scores_gemma":[0.9994317,0.00008129124,0.00016223786,0.00023504777,0.000016499089,0.000073182586],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00069908943,0.0001727453,0.0005512691,0.00003775738,0.000106391,0.00006144067,0.00033153247,0.000018351833,0.012780217],"category_scores_gemma":[0.00005653447,0.00014152576,0.00008276779,0.00017033433,0.00001900561,0.00014194132,0.00009334701,0.00010578751,0.00040895602],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026358108,0.000406418,0.0002946302,0.00130284,0.00004842265,0.000105615974,0.00018972924,0.00057347736,0.9479399,0.02580946,0.0022821452,0.020783795],"study_design_scores_gemma":[0.00273031,0.002492226,0.08654655,0.0023796416,0.00044574286,0.00010847808,0.0001053257,0.0033723686,0.47584534,0.35400602,0.06901997,0.0029480213],"about_ca_topic_score_codex":0.0013272006,"about_ca_topic_score_gemma":0.00006622544,"teacher_disagreement_score":0.47209457,"about_ca_system_score_codex":0.000010726582,"about_ca_system_score_gemma":0.000026358164,"threshold_uncertainty_score":0.9881222},"labels":[],"label_agreement":null},{"id":"W4313544928","doi":"10.1038/s41586-022-05392-8","title":"Extreme redox variations in a superdeep diamond from a subducted slab","year":2023,"lang":"en","type":"article","venue":"Nature","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Science Foundation","keywords":"Ringwoodite; Slab; Mantle (geology); Geology; Diamond; Silicate perovskite; Dehydration; Subduction; Transition zone; Olivine; Redox; Mineralogy; Geochemistry; Materials science; Chemistry; Geophysics; Composite material; Tectonics","score_opus":0.011503009315011055,"score_gpt":0.2128232817234476,"score_spread":0.20132027240843656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313544928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947559,0.0004208714,0.000005411175,0.00081409403,0.0010606876,0.00012179516,0.0008733986,0.00009152192,0.0018562865],"genre_scores_gemma":[0.9974397,0.000047278372,0.0002878591,0.00018819082,0.00030466498,0.0000021480894,0.0012264946,0.000003835023,0.0004998488],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99918044,0.000058317888,0.00013201522,0.00021996228,0.0001833953,0.00022589917],"domain_scores_gemma":[0.99957514,0.0001311546,0.000028311688,0.00018186973,0.00002714239,0.00005635538],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001423211,0.00009179697,0.00014457012,0.00008971453,0.00006539262,0.000063992025,0.00016793785,0.00039540656,0.0024386446],"category_scores_gemma":[0.00008449532,0.00007683784,0.000028506694,0.0005334756,0.00001624949,0.00013226832,0.000014160085,0.0004347727,0.0007749996],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033602855,0.0001921179,0.6868476,0.00011307087,0.0002622373,0.0008543425,0.009963243,0.0035850327,0.10959345,0.008489892,0.1478089,0.03195405],"study_design_scores_gemma":[0.000271248,0.000015570164,0.9622473,0.000013372875,0.000011499925,6.09338e-7,0.0000446013,0.0024963128,0.00042756362,0.009891796,0.024442341,0.00013776567],"about_ca_topic_score_codex":0.0045911,"about_ca_topic_score_gemma":0.0072260643,"teacher_disagreement_score":0.27539968,"about_ca_system_score_codex":0.0000020336176,"about_ca_system_score_gemma":0.000032906988,"threshold_uncertainty_score":0.9984733},"labels":[],"label_agreement":null},{"id":"W4317548797","doi":"10.1016/j.jsames.2023.104214","title":"Geophysical evidence for lithospheric scale asymmetry and inherited mantle in the SE Brazilian-Angola and Newfoundland-Iberia rifted margins","year":2023,"lang":"en","type":"article","venue":"Journal of South American Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Mantle (geology); Rift; Crust; Seismic tomography; Transition zone; Geophysics; Seismology; Petrology; Tectonics","score_opus":0.034466871479141625,"score_gpt":0.2892021740881043,"score_spread":0.25473530260896265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317548797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982536,0.00039283495,0.000033656866,0.0007437163,0.00022316372,0.00017795706,0.000051939816,0.000010967803,0.00011215817],"genre_scores_gemma":[0.9973212,0.00021334476,0.0019068627,0.0002572095,0.00023047355,0.0000016971637,0.0000030908445,0.0000035108258,0.00006263632],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851286,0.00015402923,0.00032215513,0.00024465538,0.00040717004,0.00035912296],"domain_scores_gemma":[0.9987536,0.0006328344,0.00031230893,0.00011116711,0.000055428583,0.00013465514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014309637,0.00013843772,0.00033901108,0.00012922783,0.00027787505,0.00030770738,0.00034025518,0.000029901898,0.00004280455],"category_scores_gemma":[0.00014724865,0.00008370766,0.000058590518,0.0012532115,0.00077565433,0.00043165128,0.000027383172,0.00013311775,0.000016282389],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022219431,0.000029786148,0.96823114,0.00005456306,0.000025495643,0.000035961617,0.008381854,0.00049912697,0.0011165793,0.000044954144,0.00027622376,0.02108211],"study_design_scores_gemma":[0.00026260567,0.00062503567,0.99095654,0.0000618801,0.000020672363,0.000028366278,0.003107971,0.0031148165,0.000024610114,0.00035460372,0.0013189845,0.00012393677],"about_ca_topic_score_codex":0.0026607185,"about_ca_topic_score_gemma":0.0013485036,"teacher_disagreement_score":0.022725366,"about_ca_system_score_codex":0.0000014216522,"about_ca_system_score_gemma":0.0000877745,"threshold_uncertainty_score":0.4022228},"labels":[],"label_agreement":null},{"id":"W4317564832","doi":"10.1130/g50675.1","title":"Diamonds reveal subducted slab harzburgite in the lower mantle","year":2023,"lang":"en","type":"article","venue":"Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; National Research Foundation","keywords":"Geology; Mantle (geology); Subduction; Diamond; Transition zone; Geochemistry; Lithosphere; Melt inclusions; Magnesite; Slab; Geophysics; Paleontology; Materials science; Tectonics","score_opus":0.012235959706650536,"score_gpt":0.21276548291745906,"score_spread":0.20052952321080852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317564832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906856,0.000079367375,0.0000019825948,0.0016144722,0.0010739615,0.000099514305,0.000045294204,0.000041693274,0.006358111],"genre_scores_gemma":[0.99665105,0.00003782139,0.000021072245,0.00042139203,0.00021196602,0.0000030659542,0.000189197,0.0000021823741,0.0024622486],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991326,0.00013115087,0.00013448096,0.00017192925,0.00010311319,0.00032677432],"domain_scores_gemma":[0.99958754,0.00013526274,0.000032399155,0.00020201897,0.00001324756,0.00002951516],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00038733994,0.000078228855,0.00013718587,0.00006458016,0.00006877047,0.000025969639,0.00024800672,0.00006406509,0.0023245926],"category_scores_gemma":[0.000026826188,0.000051140825,0.0000268904,0.00030893137,0.00006895345,0.000060398594,0.000020071375,0.00008277674,0.0030066445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024904922,0.00011245059,0.73783815,0.000073218966,0.000071392125,0.0015853057,0.003547027,0.0030739096,0.005848832,0.0051663583,0.22586124,0.016573079],"study_design_scores_gemma":[0.00017006093,0.00008387022,0.912632,0.0000029194248,0.0000052445143,0.000009389381,0.000050356964,0.0002783542,0.00008259883,0.00529106,0.08130176,0.00009241435],"about_ca_topic_score_codex":0.0024711578,"about_ca_topic_score_gemma":0.0017851611,"teacher_disagreement_score":0.17479382,"about_ca_system_score_codex":6.3633075e-7,"about_ca_system_score_gemma":0.000015960548,"threshold_uncertainty_score":0.9985874},"labels":[],"label_agreement":null},{"id":"W4317606097","doi":"10.1093/mnras/stad148","title":"Mantle mineralogy limits to rocky planet water inventories","year":2023,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Science and Technology Facilities Council; Vanderbilt University; National Aeronautics and Space Administration","keywords":"Planet; Mantle (geology); Geology; Transition zone; Astrobiology; Geochemistry; Geophysics; Physics; Astronomy","score_opus":0.010577451776285688,"score_gpt":0.19093085101273088,"score_spread":0.1803533992364452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317606097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971268,0.000017354747,0.0000010647265,0.000840639,0.00082214986,0.00014504055,0.0004479731,0.0000347409,0.0005642337],"genre_scores_gemma":[0.9978993,1.4251832e-7,0.00031406293,0.00010261106,0.00031070007,0.0000023819657,0.00025550716,0.00000502327,0.0011102782],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99898547,0.000049507824,0.00021442107,0.00020682029,0.00015991264,0.00038388718],"domain_scores_gemma":[0.999544,0.00007291565,0.000056608194,0.00020507607,0.000014921992,0.0001064648],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018592054,0.00012922924,0.00022167336,0.000011861699,0.0001312654,0.000047213027,0.0004116747,0.0000675014,0.00058133685],"category_scores_gemma":[0.000009764322,0.00007453379,0.000120514625,0.00006579188,0.00007483792,0.000057658144,0.00009494043,0.000079031706,0.00063257146],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003722086,0.000013040993,0.04201712,0.00002129559,0.00005090331,2.921436e-7,0.00050290115,0.9336537,0.00038481105,0.0000114969835,0.022993462,0.00031375725],"study_design_scores_gemma":[0.0003342623,0.00016150216,0.80470973,0.000017123015,0.00005856242,1.5143364e-8,0.00019810755,0.12081882,0.0057739406,0.00009875958,0.067558624,0.00027055127],"about_ca_topic_score_codex":0.0035983075,"about_ca_topic_score_gemma":0.000619165,"teacher_disagreement_score":0.81283486,"about_ca_system_score_codex":0.0000040745176,"about_ca_system_score_gemma":0.000013662942,"threshold_uncertainty_score":0.81306374},"labels":[],"label_agreement":null},{"id":"W4318482786","doi":"10.1103/physrevx.13.011010","title":"Bipolaronic High-Temperature Superconductivity","year":2023,"lang":"en","type":"article","venue":"Physical Review X","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"University of British Columbia; Max-Planck-Gesellschaft; National Natural Science Foundation of China; Division of Materials Research; Columbia University; Natural Sciences and Engineering Research Council of Canada; University of Tokyo; Stanford University; Stewart Blusson Quantum Matter Institute, University of British Columbia; Gordon and Betty Moore Foundation; National Science Foundation","keywords":"Superconductivity; Condensed matter physics; High-temperature superconductivity; Physics; Materials science","score_opus":0.015802488737621138,"score_gpt":0.2613292068359828,"score_spread":0.24552671809836168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318482786","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913561,0.006261134,2.9258808e-7,0.0009016187,0.00046150025,0.00020946092,0.00017088621,0.00012432462,0.000514719],"genre_scores_gemma":[0.9881513,0.0105291465,0.000016243417,0.00034449494,0.0005094264,0.0000047351946,0.00022713987,0.000005026305,0.0002124718],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99897593,0.00010894651,0.00013042628,0.00026047588,0.00022514457,0.00029909445],"domain_scores_gemma":[0.99946296,0.00010039312,0.000034662036,0.00026752445,0.00002688864,0.000107551816],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022978116,0.00014025693,0.00035553396,0.00002197171,0.00009731392,0.000044640034,0.00019655013,0.000026470761,0.0012171507],"category_scores_gemma":[0.00005525024,0.000097610646,0.00010671171,0.00043144982,0.000040529805,0.00021801739,0.000022085458,0.00012377395,0.006982503],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007230854,0.0005112777,0.012558324,0.015985617,0.00048031597,0.00023954142,0.0005894463,0.00090154714,0.5686882,0.09763854,0.13129249,0.17104238],"study_design_scores_gemma":[0.0006377396,0.00035987975,0.4805008,0.002551676,0.0003786797,0.000012363629,0.000025030606,0.00073161675,0.019030562,0.11045901,0.38368702,0.0016256587],"about_ca_topic_score_codex":0.0005610015,"about_ca_topic_score_gemma":0.00005625162,"teacher_disagreement_score":0.54965764,"about_ca_system_score_codex":0.0000016921858,"about_ca_system_score_gemma":0.000030653653,"threshold_uncertainty_score":0.9996959},"labels":[],"label_agreement":null},{"id":"W4318719278","doi":"10.48550/arxiv.2301.12919","title":"A strong X-ray polarization signal from the magnetar 1RXS J170849.0-400910","year":2023,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Goddard Space Flight Center; Agenzia Spaziale Italiana; Istituto Nazionale di Fisica Nucleare; Canadian Space Agency; Nuclear Safety and Security Commission; Istituto Nazionale di Astrofisica; Japan Society for the Promotion of Science; Marshall Space Flight Center; National Aeronautics and Space Administration","keywords":"Magnetar; Physics; Black-body radiation; Polarization (electrochemistry); Neutron star; Polarimetry; Astrophysics; Pulsar; Radiation; Computational physics; Optics; Scattering","score_opus":0.05994394604548386,"score_gpt":0.16164272992765788,"score_spread":0.10169878388217402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318719278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987239,0.00012930251,0.006655351,0.00021399303,0.0016915577,0.00041041797,0.0021973278,0.00019415515,0.0012688743],"genre_scores_gemma":[0.9946944,0.000113865426,0.00010915457,0.0000831078,0.0005447294,2.710118e-7,0.0017624738,0.0000132476,0.0026787592],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.998273,0.00024712158,0.00020618804,0.0007538589,0.00014815276,0.00037169133],"domain_scores_gemma":[0.9986859,0.00026286163,0.00022309061,0.0006235319,0.00006970763,0.00013490999],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002644787,0.00030127913,0.00032007167,0.00008037462,0.00029284696,0.00020688138,0.0009169339,0.00025737152,0.002684588],"category_scores_gemma":[0.000019997748,0.0002532102,0.00016073724,0.00028537464,0.000118715914,0.00020012766,0.00024560498,0.0003958687,0.001479255],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013153463,0.000036279416,0.13391691,0.0000586862,0.00031563686,0.00023882523,0.00034912874,0.8570378,0.00037320843,0.0044267066,0.0019798325,0.0011354605],"study_design_scores_gemma":[0.0007789763,0.00014308027,0.68384475,0.00016053714,0.0006514094,9.4845944e-7,0.000383852,0.23186971,0.00013301967,0.073084414,0.007823191,0.0011260984],"about_ca_topic_score_codex":0.029514855,"about_ca_topic_score_gemma":0.0038808472,"teacher_disagreement_score":0.6251681,"about_ca_system_score_codex":0.00001033818,"about_ca_system_score_gemma":0.00012847665,"threshold_uncertainty_score":0.999992},"labels":[],"label_agreement":null},{"id":"W4319078641","doi":"10.1103/physrevb.107.064101","title":"Effects of dispersion corrections on the theoretical description of bulk metals","year":2023,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Intermetallic; Bulk modulus; Dispersion (optics); Transferability; Density functional theory; Isotropy; Materials science; London dispersion force; Thermodynamics; Condensed matter physics; Chemistry; Physics; Computational chemistry; Quantum mechanics; Metallurgy; Molecule; Mathematics","score_opus":0.015925697908801672,"score_gpt":0.29764558284456083,"score_spread":0.28171988493575917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319078641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98126525,0.011280997,0.00031503083,0.0019105652,0.0005934045,0.0018325691,0.00015687305,0.00008240904,0.0025629082],"genre_scores_gemma":[0.94433147,0.054351237,0.0000140082,0.0007774364,0.00032421402,0.000042568463,0.00008886318,0.0000129356295,0.00005728368],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99722344,0.0006688194,0.00055452803,0.0004173586,0.0007484999,0.0003873538],"domain_scores_gemma":[0.99647534,0.0023148737,0.00034720192,0.000567514,0.00013202558,0.00016303013],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00076298317,0.00031887135,0.0012524332,0.000047063466,0.00013552346,0.00002243145,0.00047282391,0.000035747922,0.00037701897],"category_scores_gemma":[0.0012109397,0.00017722837,0.0006603828,0.0010256777,0.00039482035,0.00014705826,0.00006499866,0.00024592062,0.0013614099],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000870824,0.0008963116,0.00040727254,0.017447678,0.00025069635,0.000010533126,0.00019057238,0.00016849823,0.07983296,0.8495076,0.017917,0.033283796],"study_design_scores_gemma":[0.0009318874,0.002946654,0.06265741,0.044147987,0.0043774997,0.000005841244,0.000041760017,0.037383456,0.14285275,0.67013717,0.032797784,0.0017198084],"about_ca_topic_score_codex":0.00008843128,"about_ca_topic_score_gemma":0.000003472533,"teacher_disagreement_score":0.17937043,"about_ca_system_score_codex":0.0000055697346,"about_ca_system_score_gemma":0.00003550256,"threshold_uncertainty_score":0.9994162},"labels":[],"label_agreement":null},{"id":"W4319728782","doi":"10.1103/physrevb.107.064410","title":"Magnetoelastic interactions in <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"><mml:mrow><mml:msub><mml:mi>SrCu</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>BO</mml:mi><mml:mn>3</mml:mn></mml:msub><mml:mo>)</mml:mo></mml:mrow><mml:mn>2</mml:mn></mml:msub></mml:mrow></mml:math> studied by Raman scattering experiments and first principles calculations","year":2023,"lang":"lv","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; Brockhouse Institute for Materials Research","funders":"Natural Sciences and Engineering Research Council of Canada; Division of Materials Research; Office of Science; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; National High Magnetic Field Laboratory; U.S. Department of Energy; Florida Department of State; National Science Foundation","keywords":"Raman spectroscopy; Condensed matter physics; Magnetization; Phonon; Physics; Materials science; Raman scattering; Antiferromagnetism; Field (mathematics); Saturation (graph theory); Nuclear magnetic resonance; Magnetic field; Optics; Quantum mechanics; Combinatorics; Mathematics","score_opus":0.02684069092939916,"score_gpt":0.2830442107376026,"score_spread":0.25620351980820344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319728782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5963631,0.015611844,0.0010322422,0.0027030543,0.0065015475,0.0003300043,0.00262528,0.00074700837,0.37408587],"genre_scores_gemma":[0.9564648,0.02295297,0.0013255032,0.0032387348,0.00484044,0.0037765035,0.0055450825,0.0013721491,0.0004837691],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.97804034,0.0017777861,0.0046937256,0.0045532673,0.005274559,0.0056603476],"domain_scores_gemma":[0.9828691,0.0047181738,0.004424002,0.004281678,0.00046290597,0.0032441309],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"category_scores_codex":[0.0038971866,0.0023711922,0.0013862286,0.0010684459,0.003936285,0.0031544564,0.004699481,0.0025122482,0.46348435],"category_scores_gemma":[0.0043601505,0.0043736505,0.0043921364,0.003953094,0.0035009722,0.0035098698,0.004277054,0.003682686,0.00859325],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017007984,0.0012675311,0.000065001084,0.008405682,0.003631952,0.00184374,0.0027686192,0.0028322935,0.009209925,0.24533167,0.7157296,0.0072131655],"study_design_scores_gemma":[0.002963922,0.003055999,0.0003866746,0.009033855,0.0050517446,0.0010647291,0.0013856327,0.017357066,0.918237,0.0012940628,0.03563478,0.004534592],"about_ca_topic_score_codex":0.005075772,"about_ca_topic_score_gemma":0.0044309255,"teacher_disagreement_score":0.90902704,"about_ca_system_score_codex":0.00004813051,"about_ca_system_score_gemma":0.0022943923,"threshold_uncertainty_score":0.99921095},"labels":[],"label_agreement":null},{"id":"W4319763469","doi":"10.1016/j.icarus.2023.115472","title":"Electrical resistivity of liquid Fe-8wt%S-4.5wt%Si at high pressures with implications for heat flux through the cores of Io and sub-earth exoplanets","year":2023,"lang":"en","type":"article","venue":"Icarus","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Electrical resistivity and conductivity; Thermal conductivity; Heat flux; Dynamo theory; Materials science; Dynamo; Convection; RADIUS; Magnetic field; Thermodynamics; Heat transfer; Physics; Composite material","score_opus":0.017229003552880793,"score_gpt":0.23178768644313863,"score_spread":0.21455868289025784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319763469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964258,0.000694595,0.000023669765,0.00043944299,0.000082209415,0.00042340267,0.0014024882,0.000033514123,0.0004748566],"genre_scores_gemma":[0.9989115,0.0002461083,0.00015704706,0.000038478942,0.00008014409,0.000014629775,0.00030959866,0.000005652961,0.00023682069],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990778,0.00007247935,0.00019799013,0.00023432665,0.000169335,0.0002480823],"domain_scores_gemma":[0.99888486,0.0006114074,0.000094044895,0.00028761788,0.00006796862,0.000054106637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017986291,0.00012038319,0.000272987,0.000031672207,0.00019045487,0.000024793995,0.00018173814,0.000058056394,0.0000675355],"category_scores_gemma":[0.00004439505,0.000072971576,0.00003832349,0.0002107424,0.00018522872,0.00007315988,0.000029741088,0.00004767073,0.000011419788],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013514711,0.0003946557,0.20269531,0.0010656299,0.0011976435,0.000039269504,0.0029287525,0.010218205,0.63444316,0.027194666,0.08390091,0.022407101],"study_design_scores_gemma":[0.00038115907,0.00069598417,0.9193586,0.000017387472,0.00006297806,0.000008328128,0.000010812313,0.00015061979,0.06171175,0.0014618606,0.016010249,0.00013025348],"about_ca_topic_score_codex":0.0029219694,"about_ca_topic_score_gemma":0.001486792,"teacher_disagreement_score":0.7166633,"about_ca_system_score_codex":0.0000011579979,"about_ca_system_score_gemma":0.00004284661,"threshold_uncertainty_score":0.4417163},"labels":[],"label_agreement":null},{"id":"W4320482477","doi":"10.22541/essoar.167632445.53218675/v1","title":"Carbon storage in Earth's deep interior implied by carbonate-silicate-iron melt miscibility","year":2023,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Terramera (Canada)","funders":"European Commission; National Science Foundation","keywords":"Silicate; Mantle (geology); Carbonate; Geology; Mineralogy; Geochemistry; Thermodynamics; Materials science; Chemical engineering; Metallurgy","score_opus":0.016469389991005924,"score_gpt":0.22925172487848575,"score_spread":0.21278233488747983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320482477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9836508,0.00034199285,0.000014068569,0.00027535082,0.0024978984,0.0007694213,0.00087157456,0.00024804173,0.011330836],"genre_scores_gemma":[0.99633217,0.00011041465,0.0001393534,0.000078230245,0.00018649222,0.000023892233,0.0012790309,0.000023609404,0.0018268126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9966625,0.00025920308,0.0007024712,0.0012609913,0.00042070536,0.000694141],"domain_scores_gemma":[0.998359,0.00015325476,0.00022217706,0.0009886122,0.000047974878,0.00022894215],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008966685,0.0005089161,0.00083560636,0.0001619042,0.0000669049,0.00021886165,0.0007426496,0.00046230806,0.0017459593],"category_scores_gemma":[0.000055285327,0.00043657862,0.00014844518,0.00019625438,0.0001135746,0.00007769936,0.0003612288,0.00056811736,0.00032714388],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029928742,0.0010536396,0.50132036,0.00917832,0.0014267302,0.0013068296,0.012175659,0.18391429,0.18577494,0.00070973986,0.020427978,0.07971865],"study_design_scores_gemma":[0.0016057336,0.00035094656,0.884372,0.0003005029,0.0001802746,0.0000056973995,0.00035054152,0.07374971,0.015394226,0.011811124,0.00864737,0.0032318945],"about_ca_topic_score_codex":0.126973,"about_ca_topic_score_gemma":0.06775597,"teacher_disagreement_score":0.3830516,"about_ca_system_score_codex":0.000017628628,"about_ca_system_score_gemma":0.00012260147,"threshold_uncertainty_score":0.9998086},"labels":[],"label_agreement":null},{"id":"W4320484395","doi":"10.22541/essoar.167631321.13692671/v1","title":"Synthesis of the Seismic Structure of the Greater Alaska Region: Continental Lithosphere","year":2023,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Purdue University; National Aeronautics and Space Administration; National Science Foundation","keywords":"Terrane; Geology; Lithosphere; Seismology; Tectonics; Geodynamics; Crust; Mantle (geology); Continental margin; Plate tectonics; Continental crust; Collision zone; Geophysics","score_opus":0.014187477286016478,"score_gpt":0.19369051339631788,"score_spread":0.17950303611030138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320484395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99348956,0.00006143491,0.0000066422003,0.00082943,0.0022722068,0.00034009953,0.0013493636,0.000024013016,0.0016272601],"genre_scores_gemma":[0.9955859,0.000024511079,0.000055258442,0.00007024285,0.0001632562,0.0000014412598,0.000026852727,0.000007458222,0.0040650554],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987668,0.00015160145,0.0003292898,0.00027700159,0.00029961058,0.00017569913],"domain_scores_gemma":[0.9987082,0.00010762656,0.00035432176,0.00074328127,0.00005440369,0.00003215947],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010363053,0.00020109257,0.0003953893,0.000015185886,0.00007524277,0.000038626233,0.00083712017,0.00018991856,0.0016131534],"category_scores_gemma":[0.0000333226,0.000089958194,0.000237933,0.000105353334,0.00016805682,0.000030282947,0.00028204836,0.00018316874,0.000021818227],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016534375,0.000039355284,0.9162765,0.0019980217,0.0009064968,0.000015806425,0.0023593304,0.032499764,0.0034917707,0.00051229243,0.03606959,0.0056657395],"study_design_scores_gemma":[0.00009423359,0.000014437122,0.934158,0.00033013237,0.0001487116,0.0000057399698,0.00011739094,0.00040971086,0.059048045,0.004053214,0.0014226234,0.00019773294],"about_ca_topic_score_codex":0.008762151,"about_ca_topic_score_gemma":0.001239766,"teacher_disagreement_score":0.055556275,"about_ca_system_score_codex":0.0000016584805,"about_ca_system_score_gemma":0.00007301025,"threshold_uncertainty_score":0.9992995},"labels":[],"label_agreement":null},{"id":"W4321018330","doi":"10.1029/2022gl101213","title":"Global Variability of Density Contrast Across the 660‐km Discontinuity","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Jump; Geology; Mantle (geology); Discontinuity (linguistics); Subduction; Density contrast; Amplitude; Mantle convection; Classification of discontinuities; Geodesy; Geophysics; Seismology; Physics; Tectonics; Astrophysics; Optics","score_opus":0.028387482099605035,"score_gpt":0.31561072328622986,"score_spread":0.28722324118662484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321018330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940236,0.000007385988,0.00007594497,0.0035834496,0.0003716953,0.00034611108,0.0009951801,0.000053532916,0.0005430694],"genre_scores_gemma":[0.9991948,0.0000072195517,0.0000204541,0.00018003449,0.0004140259,0.0000057968928,0.00009308112,0.0000036891372,0.00008087695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9965203,0.00080451055,0.00026614152,0.0004157027,0.0010211075,0.000972259],"domain_scores_gemma":[0.9977241,0.0013118769,0.00006667454,0.0005659896,0.00015398447,0.00017734988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030012217,0.00014903829,0.00031918046,0.00002505199,0.00044402177,0.00015686861,0.00068002485,0.000060231763,0.00020450418],"category_scores_gemma":[0.000551564,0.00009468287,0.00013419421,0.00092587783,0.00094321574,0.00016795303,0.00018703903,0.00027078972,0.00075928215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010703194,0.00037469369,0.76003426,0.0003760985,0.00040309795,0.00022264972,0.0028647608,0.0032078093,0.12460225,0.012543038,0.05529502,0.039005987],"study_design_scores_gemma":[0.00020680255,0.00005696873,0.98818105,0.000011033607,0.00000802752,8.442554e-7,0.00010327282,0.0010330041,0.00077419484,0.007811433,0.0016984049,0.00011493423],"about_ca_topic_score_codex":0.017220955,"about_ca_topic_score_gemma":0.0016714797,"teacher_disagreement_score":0.2281468,"about_ca_system_score_codex":0.000010622618,"about_ca_system_score_gemma":0.00006704022,"threshold_uncertainty_score":0.98932344},"labels":[],"label_agreement":null},{"id":"W4321267594","doi":"10.1134/s0001433822100097","title":"Global Heat. Geofluids. Geodynamic Сatastrophes","year":2022,"lang":"en","type":"article","venue":"Izvestiya Atmospheric and Oceanic Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hydrogenics (Canada)","funders":"","keywords":"Environmental science; Astrobiology; Earth science; Geophysics; Geology; Physics","score_opus":0.005261466437805423,"score_gpt":0.18232428507574858,"score_spread":0.17706281863794315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321267594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925113,0.001181057,0.001329436,0.0000856965,0.00082134467,0.00018965405,0.0008114957,0.00010763477,0.002962423],"genre_scores_gemma":[0.99732006,0.000081997576,0.0014736213,0.00032659946,0.0003071931,0.000003896403,0.00023971059,0.000008909367,0.00023801376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984675,0.00009493932,0.00022225203,0.00041197537,0.00034035713,0.00046294334],"domain_scores_gemma":[0.99940944,0.000049231025,0.00006836691,0.00027302853,0.000022230024,0.00017773452],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014691544,0.00023786622,0.00029722354,0.0000019452016,0.00056268874,0.00009676062,0.00029925586,0.00003461649,0.0014018322],"category_scores_gemma":[0.000007297227,0.00022243953,0.000068591624,0.0003323352,0.00011740778,0.00020645453,0.000114399045,0.00012467643,0.00007861224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004837869,0.0005003218,0.48872736,0.00024767529,0.000514712,0.00035326267,0.0009194765,0.22872207,0.0014922465,0.04191155,0.024595553,0.211532],"study_design_scores_gemma":[0.0012767042,0.0009284116,0.7696545,0.000019500112,0.00017890414,0.00012152659,0.00041571137,0.12163391,0.00004106041,0.052289136,0.052289233,0.001151415],"about_ca_topic_score_codex":0.0022189415,"about_ca_topic_score_gemma":0.000044685006,"teacher_disagreement_score":0.28092712,"about_ca_system_score_codex":0.0000147729725,"about_ca_system_score_gemma":0.00009492651,"threshold_uncertainty_score":0.999511},"labels":[],"label_agreement":null},{"id":"W4321379019","doi":"10.1029/2022gc010678","title":"Penetrative Superplumes in the Mantle of Large Super‐Earth Planets: A Possible Mechanism for Active Tectonics in the Massive Super‐Earths","year":2023,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mantle (geology); Mantle convection; Geology; Planet; Core–mantle boundary; Geophysics; Plate tectonics; Planetary differentiation; Earth's internal heat budget; Transition zone; Mantle wedge; Volcanism; Hotspot (geology); Tectonics; Petrology; Subduction; Physics; Astrophysics; Seismology","score_opus":0.012228477491923628,"score_gpt":0.2319703190219387,"score_spread":0.21974184153001508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321379019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99160826,0.00011824679,0.000015277166,0.00026656265,0.0003016391,0.0011679543,0.0043817703,0.000035023768,0.0021052845],"genre_scores_gemma":[0.99754703,0.00005321843,0.000032127915,0.00011620888,0.00028886326,0.00011035774,0.0016436226,0.00001233713,0.00019622491],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9973522,0.00026613002,0.00051539944,0.0004907218,0.00057447195,0.0008011222],"domain_scores_gemma":[0.9982234,0.0008214364,0.000182535,0.00058193563,0.00012982577,0.000060840975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010365851,0.00033547834,0.0005254647,0.00008841468,0.00022994934,0.00013977564,0.0008290181,0.00018082335,0.00019268799],"category_scores_gemma":[0.000080750324,0.00022130439,0.00015448572,0.0007637967,0.00008476858,0.00022150193,0.00004371751,0.0002891474,0.00012389316],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028541181,0.0027961333,0.09052532,0.0103019755,0.0016291756,0.0014063745,0.19364394,0.018772662,0.57067984,0.083448336,0.017280709,0.0066614053],"study_design_scores_gemma":[0.010376707,0.0020695622,0.2495377,0.0012653788,0.00040290246,0.00014992496,0.17837219,0.066121385,0.36441296,0.10616145,0.017360793,0.0037690462],"about_ca_topic_score_codex":0.005096312,"about_ca_topic_score_gemma":0.0046374104,"teacher_disagreement_score":0.2062669,"about_ca_system_score_codex":0.0000070289684,"about_ca_system_score_gemma":0.00015775253,"threshold_uncertainty_score":0.9024531},"labels":[],"label_agreement":null},{"id":"W4321440665","doi":"10.1007/978-3-030-84936-8_9","title":"Thermodynamic Properties of Non-equilibrium Plasmas","year":2023,"lang":"es","type":"book-chapter","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Thermodynamic equilibrium; Plasma; Non-equilibrium thermodynamics; Thermodynamic state; Thermodynamics; Thermal equilibrium; Hydrogen; Thermodynamic process; Thermal; Argon; Equilibrium thermodynamics; Chemistry; Atomic physics; Physics; Material properties; Nuclear physics","score_opus":0.02320423362687797,"score_gpt":0.19617641453443543,"score_spread":0.17297218090755745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321440665","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4711192,0.0002688252,0.0000072127327,0.000149643,0.0027482798,0.0006412053,0.0016771453,0.00012707259,0.5232614],"genre_scores_gemma":[0.7565495,0.0004984042,0.000048089343,0.00002970764,0.0003431744,0.0000022971037,0.00019719452,0.000036781003,0.24229485],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978311,0.0000341466,0.000642265,0.000535524,0.00050833065,0.0004486564],"domain_scores_gemma":[0.99880457,0.00008775753,0.0003510271,0.00051303435,0.00010713386,0.00013646422],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00027063955,0.00050661527,0.00087123853,0.0001623902,0.000092800314,0.0001242533,0.00055190385,0.00036259094,0.006043988],"category_scores_gemma":[0.000012676896,0.0003567954,0.00023666154,0.00006064846,0.00031663105,0.00017882133,0.0001129096,0.00018641975,0.0043479623],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013436882,0.00016745775,0.0028085725,0.0087387,0.003209606,0.0002901344,0.0018180617,0.0040520304,0.77033687,0.18256137,0.004849081,0.019824456],"study_design_scores_gemma":[0.006336258,0.0076555316,0.11027822,0.014520036,0.0042779106,0.000105212006,0.0010691319,0.13927218,0.26339352,0.07758589,0.35787627,0.01762983],"about_ca_topic_score_codex":0.0034843462,"about_ca_topic_score_gemma":0.000463575,"teacher_disagreement_score":0.5069433,"about_ca_system_score_codex":0.0000028228578,"about_ca_system_score_gemma":0.00012608664,"threshold_uncertainty_score":0.9998884},"labels":[],"label_agreement":null},{"id":"W4321489077","doi":"10.5194/egusphere-egu23-5200","title":"High coseismic differential stress preserved in the lattice of seismically shocked garnets","year":2023,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Cataclastic rock; Differential stress; Geology; Electron backscatter diffraction; Slip (aerodynamics); Residual stress; Seismology; Gneiss; Fault plane; Mylonite; Fault (geology); Petrology; Materials science; Composite material; Tectonics; Metamorphic rock; Deformation (meteorology); Shear zone; Microstructure","score_opus":0.029702014350262797,"score_gpt":0.23385503490615003,"score_spread":0.20415302055588724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321489077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933591,0.000052541138,0.000081590144,0.000805191,0.0018588741,0.0006154776,0.0016483719,0.0000638445,0.001515029],"genre_scores_gemma":[0.9963186,0.00009545364,0.00019764809,0.00014438246,0.00037584722,0.000010791133,0.0015491782,0.000010022011,0.0012981176],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9976883,0.00039505336,0.0005573006,0.00047175493,0.0005117172,0.00037589457],"domain_scores_gemma":[0.9985252,0.00045241145,0.00023704272,0.00065884436,0.000057879945,0.00006864139],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004435551,0.00028602607,0.0005644722,0.000095786294,0.00005318731,0.00015737645,0.0011985988,0.00025598847,0.0029441775],"category_scores_gemma":[0.0000471019,0.00018077229,0.00012684705,0.00013858562,0.00008971331,0.000063886946,0.0002493274,0.00039062102,0.0002224062],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022959209,0.0019186067,0.26528662,0.009820865,0.0022153682,0.0006330239,0.009527827,0.5837733,0.0047595827,0.011907656,0.09287151,0.014989702],"study_design_scores_gemma":[0.0006626118,0.00011601034,0.95729476,0.00024460605,0.00013472197,0.0000010782658,0.00015712742,0.018244237,0.001438176,0.019410677,0.0017810891,0.000514924],"about_ca_topic_score_codex":0.062528275,"about_ca_topic_score_gemma":0.007506878,"teacher_disagreement_score":0.69200814,"about_ca_system_score_codex":0.000002337926,"about_ca_system_score_gemma":0.000082674494,"threshold_uncertainty_score":0.99796724},"labels":[],"label_agreement":null},{"id":"W4321995079","doi":"10.5194/egusphere-egu23-10229","title":"Outer Core Heat Flux in Small Terrestrial Bodies from Electrical Resistivity Measurements of Liquid Fe-8S-4.5Si at High Pressure","year":2023,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Electrical resistivity and conductivity; Electron microprobe; Materials science; Thermal conductivity; Mineralogy; Analytical Chemistry (journal); Outer core; Diamond anvil cell; Alloy; Inner core; Metallurgy; Chemistry; Thermodynamics; Composite material; High pressure; Physics","score_opus":0.07786443047341383,"score_gpt":0.2521187524329506,"score_spread":0.17425432195953677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321995079","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911581,0.0005344512,0.000032874614,0.00020868107,0.0035436256,0.000773814,0.0027141718,0.00012370088,0.0009105784],"genre_scores_gemma":[0.99296266,0.00009629158,0.0006554352,0.00005374648,0.0008612612,0.000017815802,0.0028398812,0.000020923932,0.002491997],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99648243,0.00037419517,0.0008421887,0.0010038357,0.0006841851,0.000613136],"domain_scores_gemma":[0.99836016,0.00037551002,0.0002690569,0.0007354283,0.000084133404,0.00017569716],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00073654676,0.0005104987,0.0011582639,0.00018575147,0.00010847673,0.000111667054,0.00073948584,0.000560152,0.002059388],"category_scores_gemma":[0.00018259953,0.0004168293,0.00021312272,0.00013314071,0.00010628566,0.00008907069,0.00044930063,0.000446472,0.0002761539],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.014404303,0.0006015919,0.85209966,0.0011759173,0.0023776377,0.00034876144,0.0013583561,0.031342376,0.04554727,0.00010287205,0.047843732,0.00279754],"study_design_scores_gemma":[0.001598924,0.00047064645,0.96200436,0.00037844083,0.00037046266,0.0000010457326,0.000009449384,0.0013216047,0.0239845,0.0050300593,0.0038596687,0.00097084796],"about_ca_topic_score_codex":0.13283248,"about_ca_topic_score_gemma":0.090419516,"teacher_disagreement_score":0.10990471,"about_ca_system_score_codex":0.000018933779,"about_ca_system_score_gemma":0.0001838401,"threshold_uncertainty_score":0.99982834},"labels":[],"label_agreement":null},{"id":"W4321995806","doi":"10.5194/egusphere-egu23-10733","title":"Asymptomatic lithospheric drip driving subsidence of Konya Basin, Central Anatolia","year":2023,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Crust; Structural basin; Isostasy; Geomorphology; Geophysics; Seismology; Tectonics","score_opus":0.018086020783703458,"score_gpt":0.22751471629252148,"score_spread":0.20942869550881804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321995806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99040866,0.00022277722,0.0005126262,0.00016938875,0.0036310959,0.00038101667,0.0002488831,0.00022201255,0.004203565],"genre_scores_gemma":[0.99471587,0.00023231903,0.0029637006,0.00004831758,0.0002513356,0.0000037386933,0.00022608701,0.000014316797,0.0015443118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99767643,0.00013196723,0.00060107803,0.0005396746,0.00048348735,0.0005673318],"domain_scores_gemma":[0.99855447,0.00021461332,0.00035321616,0.0006032744,0.00008260626,0.00019182754],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039048755,0.00032381614,0.00067820546,0.00007014114,0.000081506696,0.00017299813,0.0006850053,0.00022625894,0.0044826637],"category_scores_gemma":[0.000087945446,0.0002700667,0.0001777561,0.00024134002,0.000092698545,0.00014158542,0.00018539332,0.00022944451,0.00053208985],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024200626,0.00005314282,0.9605896,0.001671719,0.00028658428,0.00008614339,0.000884437,0.021265907,0.0004308127,0.0010458359,0.008300402,0.005361231],"study_design_scores_gemma":[0.000100457764,0.000039420687,0.980046,0.00036956725,0.00007349948,0.0000026201394,0.000069841364,0.0096008675,0.0012145574,0.0074244174,0.000654284,0.00040447383],"about_ca_topic_score_codex":0.021407109,"about_ca_topic_score_gemma":0.0031277207,"teacher_disagreement_score":0.019456409,"about_ca_system_score_codex":0.0000052848677,"about_ca_system_score_gemma":0.00018841929,"threshold_uncertainty_score":0.99997514},"labels":[],"label_agreement":null},{"id":"W4322504397","doi":"10.1029/2022jb025745","title":"A New P‐Wave Tomographic Model (CAP22) for North America: Implications for the Subduction and Cratonic Metasomatic Modification History of Western Canada and Alaska","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; Geological Survey of Canada; Université du Québec à Montréal","funders":"HORIZON EUROPE European Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Subduction; Geology; Craton; Seismology; Plate tectonics; Archean; Mantle (geology); Proterozoic; Seismometer; Volcanism; Crust; Tectonics; Intraplate earthquake; Paleontology","score_opus":0.08177245085894629,"score_gpt":0.30841789958218024,"score_spread":0.22664544872323394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322504397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938876,0.00057536404,0.0027490272,0.0018721463,0.00015878538,0.00045898565,0.00028066483,0.0000056787126,0.000011759121],"genre_scores_gemma":[0.99787134,0.00076645415,0.0006838012,0.000029055338,0.00021522955,0.00001224447,0.000041847128,0.0000058672526,0.0003741642],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99879086,0.00008362152,0.00031966882,0.00015498616,0.00036455962,0.00028631024],"domain_scores_gemma":[0.99812824,0.00092541665,0.00022327871,0.00017544675,0.00036234735,0.00018527613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005666695,0.00009299617,0.00028350562,0.00012854853,0.0001702917,0.00004665027,0.00016353448,0.000027859212,0.0000076158176],"category_scores_gemma":[0.00014125089,0.00006306624,0.000074785894,0.00027939247,0.00015058188,0.00018579068,0.000020120322,0.00013419379,0.0000012544601],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00292817,0.00047800693,0.07283754,0.0025711257,0.0024857908,0.000017993812,0.009888296,0.14538655,0.06482865,0.007341056,0.12054386,0.57069296],"study_design_scores_gemma":[0.000627365,0.00065991894,0.79168516,0.000036091,0.00013651706,0.000009013809,0.00015671195,0.18189688,0.00024905134,0.015904227,0.008480219,0.00015886876],"about_ca_topic_score_codex":0.048415318,"about_ca_topic_score_gemma":0.077502966,"teacher_disagreement_score":0.71884763,"about_ca_system_score_codex":0.000012060953,"about_ca_system_score_gemma":0.00084525405,"threshold_uncertainty_score":0.9579214},"labels":[],"label_agreement":null},{"id":"W4323076604","doi":"10.48550/arxiv.2303.01477","title":"Fundamental laws of chiral band crossings: local constraints, global constraints, and topological phase diagrams","year":2023,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Homogeneous space; Chern class; Constraint (computer-aided design); Topology (electrical circuits); Eigenvalues and eigenvectors; Phase space; Physics; Mathematics; Pure mathematics; Law; Quantum mechanics; Geometry; Combinatorics","score_opus":0.07117099735482599,"score_gpt":0.21495860381240064,"score_spread":0.14378760645757466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323076604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875483,0.00009382077,0.0034217457,0.000037593985,0.0008524479,0.00028122187,0.0041079503,0.000088520086,0.0035683818],"genre_scores_gemma":[0.99894655,0.00013441443,0.000097672586,0.000040387287,0.00010464995,1.9569706e-7,0.00038790028,0.000005319489,0.0002829194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99834144,0.00012719468,0.00028575107,0.0007265259,0.00011000141,0.00040908917],"domain_scores_gemma":[0.9990651,0.000110960165,0.00023592253,0.00028775525,0.000052419346,0.0002478288],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024624122,0.00031319272,0.0005389395,0.000055904467,0.00018033005,0.00013863719,0.0003718948,0.00031291667,0.0015038425],"category_scores_gemma":[0.000023757599,0.0002993371,0.00014834972,0.0001739801,0.0032315352,0.00012412145,0.00019747448,0.0002527253,0.00006751836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019907698,0.0009825606,0.73211634,0.0012791744,0.0015032269,0.004450114,0.0009406208,0.06083766,0.0006605135,0.13681205,0.0018095099,0.05661747],"study_design_scores_gemma":[0.017573498,0.002926043,0.49963588,0.0010641437,0.0016435024,0.00021665786,0.0053709364,0.068352334,0.0018990936,0.3927176,0.0037298694,0.004870447],"about_ca_topic_score_codex":0.0021862246,"about_ca_topic_score_gemma":0.0006728497,"teacher_disagreement_score":0.25590557,"about_ca_system_score_codex":0.00001615563,"about_ca_system_score_gemma":0.00014923663,"threshold_uncertainty_score":0.9999459},"labels":[],"label_agreement":null},{"id":"W4323349511","doi":"10.1016/j.epsl.2023.118081","title":"Dual origin of ferropericlase inclusions within super-deep diamonds","year":2023,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Argonne National Laboratory; H2020 European Research Council; Office of Science; Ministero dell’Istruzione, dell’Università e della Ricerca; U.S. Department of Energy; Academy of Pharmaceutical Sciences; University of Chicago; European Research Council; National Science Foundation","keywords":"Diamond; Geology; Mantle (geology); Silicate perovskite; Inclusion (mineral); Nucleation; Mineralogy; Materials science; Geochemistry; Thermodynamics; Composite material","score_opus":0.014091406228173857,"score_gpt":0.20954548149832955,"score_spread":0.19545407527015568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323349511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99683475,0.0000750992,0.000009741571,0.0008901199,0.0008125137,0.00013135823,0.00030302227,0.0000656072,0.00087781023],"genre_scores_gemma":[0.9982485,0.00004832532,0.0004402632,0.0006720317,0.00014799448,6.629896e-7,0.00030716366,0.000003321138,0.0001317019],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99830157,0.00006293807,0.00025839068,0.00038451425,0.00050554407,0.00048704457],"domain_scores_gemma":[0.99927574,0.00012456735,0.00007709064,0.00023846056,0.000021172456,0.0002629597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006909816,0.00016485271,0.00023256894,0.00023627872,0.00043395217,0.000103029815,0.00029776918,0.00004176526,0.00068793626],"category_scores_gemma":[0.00003948712,0.00012657806,0.000031762465,0.0008382842,0.0006165439,0.00046792626,0.000057618738,0.00011618101,0.00039826418],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017114413,0.000036627047,0.6924199,0.00013673792,0.000053047388,0.0006502731,0.0052510807,0.06999659,0.21269633,0.00042146727,0.0055160527,0.012650756],"study_design_scores_gemma":[0.00029385238,0.00017221137,0.97288954,0.000022596987,0.000017776303,0.000040385145,0.00017641865,0.01715329,0.002206038,0.00014730947,0.0065586893,0.00032188042],"about_ca_topic_score_codex":0.0025910463,"about_ca_topic_score_gemma":0.00069376186,"teacher_disagreement_score":0.28046966,"about_ca_system_score_codex":0.0000010306898,"about_ca_system_score_gemma":0.000066415065,"threshold_uncertainty_score":0.75324196},"labels":[],"label_agreement":null},{"id":"W4323841969","doi":"10.1038/s41598-023-31043-7","title":"Insights on the dissolution of water in an albite melt at high pressures and temperatures from a direct structural analysis","year":2023,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"Missouri Space Grant Consortium; Argonne National Laboratory; Natural Sciences and Engineering Research Council of Canada; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Albite; Dissolution; Materials science; Chemistry; Mineralogy; Chemical engineering; Metallurgy; Physical chemistry","score_opus":0.0094214346298111,"score_gpt":0.20957129653512757,"score_spread":0.20014986190531647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323841969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978067,0.00010505899,1.4047336e-7,0.000070959824,0.0015915789,0.00014890081,0.00010260632,0.00002424025,0.00014980922],"genre_scores_gemma":[0.998346,0.0000048974543,0.000009567691,0.000010215876,0.000048564896,0.0000023126731,0.0011177188,0.0000024123717,0.00045833155],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985131,0.00014736608,0.0002849155,0.0004836496,0.00036990803,0.00020104276],"domain_scores_gemma":[0.9992424,0.0000840499,0.000112286994,0.00046195564,0.000039558246,0.000059748625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051692367,0.00010983741,0.00023341781,0.0001932725,0.00028667238,0.00023596393,0.000114869996,0.0000416653,0.0004741078],"category_scores_gemma":[0.000028838524,0.000054063363,0.000049185568,0.00052619004,0.00015735847,0.00018169874,0.000037447073,0.00004698487,0.000014290548],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013680277,0.000029819072,0.47676837,0.000035183315,0.00034050862,0.0003623479,0.0068046604,0.02604068,0.4857629,0.000189437,0.0029789137,0.00055037165],"study_design_scores_gemma":[0.000048686074,0.000026491776,0.9071848,0.0000117395,0.000077333294,0.000001326112,0.000044066324,0.001955462,0.08213893,0.007462166,0.0009412433,0.00010775479],"about_ca_topic_score_codex":0.005971518,"about_ca_topic_score_gemma":0.011086464,"teacher_disagreement_score":0.4304164,"about_ca_system_score_codex":0.000002208443,"about_ca_system_score_gemma":0.00001162121,"threshold_uncertainty_score":0.90271884},"labels":[],"label_agreement":null},{"id":"W4323968144","doi":"10.1007/978-3-031-23313-5_7","title":"Constitutive Equations","year":2023,"lang":"en","type":"book-chapter","venue":"Springer geophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Constitutive equation; Physics; Thermodynamics; Finite element method","score_opus":0.028027444700077633,"score_gpt":0.21197988035300394,"score_spread":0.1839524356529263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323968144","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00061998796,0.00010962084,0.00015665723,0.000064233835,0.0032047026,0.00034353,0.0013892862,0.0002693917,0.9938426],"genre_scores_gemma":[0.109852076,0.0002052205,0.00024064477,0.00016856528,0.0018426583,0.000005071279,0.0015545036,0.00005493926,0.88607633],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9985008,0.000013860063,0.00029614096,0.000453801,0.00038306628,0.00035232992],"domain_scores_gemma":[0.99891925,0.0002050793,0.0002069079,0.00044092734,0.000098443816,0.00012937425],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0001249118,0.00035763666,0.000437695,0.000091717266,0.00020358077,0.00011526718,0.00030196918,0.00021777119,0.0029911974],"category_scores_gemma":[0.00002114857,0.00034173127,0.00017790814,0.000053031836,0.00019185965,0.0001317389,0.000054427306,0.0003081492,0.02632864],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012632763,0.000007766138,0.000102118145,0.000059222035,0.00021678957,0.00006761279,0.0000837266,0.0005847409,0.00007579222,0.988038,0.0019852875,0.008766318],"study_design_scores_gemma":[0.00027892186,0.00010614481,0.006729581,0.0002424001,0.0002918255,0.0000020811428,0.000011900212,0.00031652296,0.000110333494,0.57860214,0.41206834,0.0012398039],"about_ca_topic_score_codex":0.0016655282,"about_ca_topic_score_gemma":0.0010807437,"teacher_disagreement_score":0.41008306,"about_ca_system_score_codex":0.0000057955335,"about_ca_system_score_gemma":0.00017556289,"threshold_uncertainty_score":0.9999035},"labels":[],"label_agreement":null},{"id":"W4324056425","doi":"10.3390/geosciences13030079","title":"Shear-Wave Anisotropy Measurements in the Crust from Receiver Functions: An Interplay of Lower and Upper Crustal Anisotropy","year":2023,"lang":"en","type":"article","venue":"Geosciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Crust; Anisotropy; Seismology; Azimuth; Upper crust; Receiver function; Shear wave splitting; Shear (geology); Basin and Range Province; Seismic anisotropy; Upper and lower bounds; Geophysics; Geodesy; Geometry; Lithosphere; Tectonics; Petrology; Physics; Mantle (geology); Optics","score_opus":0.0358024294852964,"score_gpt":0.2513715023083866,"score_spread":0.21556907282309024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4324056425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972973,0.00013242269,0.00004309959,0.00017148202,0.0009961994,0.00015385634,0.00027964727,0.000024486975,0.0009015423],"genre_scores_gemma":[0.9990406,0.000091023016,0.0004042775,0.00012367652,0.00011241989,0.000002833805,0.00007245056,0.0000024485826,0.00015027981],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985237,0.00016111787,0.00022324178,0.0003347166,0.00046052245,0.00029669306],"domain_scores_gemma":[0.9994893,0.00011105293,0.000077471595,0.00021290737,0.000040086547,0.00006917095],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007043706,0.00012213273,0.00017474982,0.00010242839,0.00020599013,0.00015345917,0.00029882,0.00004945851,0.0012592988],"category_scores_gemma":[0.000050654035,0.00007692963,0.000032969016,0.0004665713,0.0002618024,0.00047676312,0.000030449579,0.00007327436,0.00012834204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044336746,0.00025389885,0.91370916,0.000045590208,0.00006734774,0.0000749711,0.009864125,0.0015062586,0.031705953,0.0005475222,0.007134451,0.03464734],"study_design_scores_gemma":[0.00022582134,0.00036873808,0.98920804,0.000025631178,0.000014972997,0.000003272335,0.0022645013,0.0018606228,0.00038045074,0.0017604636,0.0037401237,0.00014737612],"about_ca_topic_score_codex":0.015668541,"about_ca_topic_score_gemma":0.00321159,"teacher_disagreement_score":0.07549886,"about_ca_system_score_codex":0.0000023419307,"about_ca_system_score_gemma":0.000045735705,"threshold_uncertainty_score":0.9996537},"labels":[],"label_agreement":null},{"id":"W4327713835","doi":"10.1038/s43247-023-00722-8","title":"Tetracarbonates in silicate melts may be at the origin of a deep carbon reservoir in the deep Earth","year":2023,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca; Università degli Studi di Milano-Bicocca; National Natural Science Foundation of China; European Synchrotron Radiation Facility; Dipartimenti di Eccellenza","keywords":"Mantle (geology); Silicate; Carbonate; Geology; Carbon fibers; Mineralogy; Carbon cycle; Oxygen; Geochemistry; Materials science; Chemistry; Composite material","score_opus":0.03257767616639357,"score_gpt":0.24545914261158389,"score_spread":0.21288146644519032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4327713835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891833,0.0014775575,0.0000011665727,0.004595206,0.00004951691,0.00044719546,0.00006448723,0.000016336466,0.0041652145],"genre_scores_gemma":[0.996526,0.002620697,0.00015941219,0.00011423312,0.000017202548,0.000039496776,0.00022207478,0.0000056482145,0.00029520542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982723,0.00057631446,0.0003522269,0.00020863529,0.0003029716,0.00028754576],"domain_scores_gemma":[0.9974166,0.0006681743,0.00011040189,0.0017581283,0.0000067047145,0.00003999833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010958979,0.00013217254,0.00018693827,0.00008862605,0.00018808938,0.000030743857,0.0012276657,0.000056138284,0.00031607688],"category_scores_gemma":[0.00003302748,0.00008438723,0.000048301048,0.0003960634,0.0003079478,0.000063462445,0.00023009242,0.00020289073,0.00019035199],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014781013,0.0005016381,0.7405128,0.000084428684,0.0001145597,0.000031699085,0.01751303,0.20166437,0.011522336,0.0027035363,0.00033816698,0.024865614],"study_design_scores_gemma":[0.00023898149,0.00004864115,0.90886885,0.000014486251,0.000014709237,0.0000016195492,0.00047092035,0.016603095,0.0007076043,0.00064464594,0.07225842,0.00012805931],"about_ca_topic_score_codex":0.004524753,"about_ca_topic_score_gemma":0.03190698,"teacher_disagreement_score":0.18506128,"about_ca_system_score_codex":0.000006305472,"about_ca_system_score_gemma":0.0000157056,"threshold_uncertainty_score":0.9857582},"labels":[],"label_agreement":null},{"id":"W4360919297","doi":"10.1785/0320220044","title":"<i>P</i>/<i>SV</i>Amplitude Ratios of Shallow Isotropic Explosions and Earthquakes Could Be Indistinguishable at Local Distances: Insights from Single-Station Waveform Simulations","year":2023,"lang":"en","type":"article","venue":"The Seismic Record","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Seismology; Amplitude; Isotropy; Geology; Anisotropy; Seismic wave; Shear (geology); Shear waves; Waveform; Geophysics; Asymmetry; Love wave; Explosive material; Rayleigh wave; Wave propagation; Physics; Mechanical wave; Longitudinal wave; Optics","score_opus":0.0286194129560696,"score_gpt":0.2237688067922458,"score_spread":0.19514939383617622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360919297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99550337,0.00014578567,0.0013677046,0.00041801698,0.00047027942,0.00025780048,0.0011152698,0.00006329185,0.00065850414],"genre_scores_gemma":[0.997725,0.00010405163,0.00020588233,0.0002193461,0.00014236225,0.0000038546937,0.0011960585,0.00000742022,0.00039600726],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99887806,0.00008936366,0.00032647094,0.0002479996,0.00023708846,0.00022100727],"domain_scores_gemma":[0.998952,0.0004883057,0.00017569373,0.00025507036,0.00005527276,0.000073672774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009847235,0.0001468951,0.00023679271,0.000053220865,0.00037039173,0.000074293435,0.0001739756,0.000054651373,0.0003622517],"category_scores_gemma":[0.000049042577,0.00010074622,0.00004222596,0.0002449165,0.00015021884,0.0001990899,0.000038164522,0.00007884702,0.000088085464],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010823577,0.0003575172,0.1557836,0.0005510859,0.0006538425,0.000074713906,0.04521958,0.5517585,0.07738235,0.0026894265,0.017366312,0.1470807],"study_design_scores_gemma":[0.0016058065,0.0006078312,0.32898116,0.00026325724,0.00023220284,0.000004028348,0.0029429116,0.45502165,0.006939549,0.05943012,0.14305452,0.00091696205],"about_ca_topic_score_codex":0.0058014384,"about_ca_topic_score_gemma":0.012975055,"teacher_disagreement_score":0.17319757,"about_ca_system_score_codex":0.0000068664276,"about_ca_system_score_gemma":0.00003594092,"threshold_uncertainty_score":0.87700784},"labels":[],"label_agreement":null},{"id":"W4360952120","doi":"10.1038/s41467-023-37295-1","title":"Quantum structural fluxion in superconducting lanthanum polyhydride","year":2023,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Engineering and Physical Sciences Research Council; European Commission; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; University of Cambridge","keywords":"Superconductivity; Condensed matter physics; Lanthanum; Materials science; Chemistry; Physics; Inorganic chemistry","score_opus":0.02987496838384863,"score_gpt":0.2872800583807841,"score_spread":0.25740508999693545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360952120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99406886,0.00095795223,6.3639726e-7,0.0020251407,0.00064822525,0.00011102027,0.00014444446,0.00010599815,0.0019377401],"genre_scores_gemma":[0.99824363,0.00021510996,0.00034118388,0.00011003768,0.00009212654,0.0000023927116,0.00089020294,0.0000039169854,0.00010141816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99921846,0.00012566014,0.0001695547,0.00014075881,0.00012375166,0.00022181534],"domain_scores_gemma":[0.99898255,0.00023035528,0.000040586663,0.000672443,0.000028763156,0.00004530987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026938113,0.0000868322,0.00012630303,0.00011705051,0.00022733226,0.000055748453,0.00065909553,0.00012905557,0.0002549484],"category_scores_gemma":[0.00008630854,0.00007439073,0.000031648477,0.00048289902,0.000053403583,0.00020292308,0.000076214834,0.0004030268,0.00031510476],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054666867,0.00005757351,0.8574465,0.00007984906,0.000085557804,0.000038443643,0.004413115,0.0028940272,0.052025758,0.052603893,0.0136846,0.016616015],"study_design_scores_gemma":[0.00022040162,0.000021005288,0.9555338,0.000029986308,0.00001055273,0.000006613194,0.00049317896,0.012782767,0.00087383843,0.005332775,0.024466226,0.00022886416],"about_ca_topic_score_codex":0.002529358,"about_ca_topic_score_gemma":0.011525646,"teacher_disagreement_score":0.09808729,"about_ca_system_score_codex":0.0000031796524,"about_ca_system_score_gemma":0.00002635053,"threshold_uncertainty_score":0.6431581},"labels":[],"label_agreement":null},{"id":"W4361216979","doi":"10.1029/2022gl102057","title":"A Note on the Timing and Nature of the Moho Geometry and Upper Mantle Structure Beneath Southern New England","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Waterloo; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Fibrous joint; Paleontology; Laurentia; Lithosphere; Terrane; Devonian; Paleozoic; Magmatism; Carboniferous; Seismology; Structural basin; Tectonics","score_opus":0.021082228630068978,"score_gpt":0.2681510312038259,"score_spread":0.2470688025737569,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361216979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896104,0.00005425516,0.0000016404955,0.009587448,0.00014832319,0.00020465696,0.00026615482,0.000012949757,0.000114195806],"genre_scores_gemma":[0.9985424,0.00002287179,0.000033457276,0.0005719906,0.00043659884,0.0000011265137,0.00001905343,0.0000061744354,0.00036628975],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99843943,0.00019386668,0.000101432466,0.00026119853,0.00060573337,0.00039835516],"domain_scores_gemma":[0.9986809,0.0008664096,0.000034071145,0.00028352058,0.0000295089,0.00010558874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039393938,0.00011838257,0.00015513113,0.00007164357,0.00030908425,0.00011602906,0.00030461504,0.000081179445,0.00016386085],"category_scores_gemma":[0.00016681993,0.00005821796,0.000041892737,0.00042004063,0.00025292198,0.000057305042,0.0001147702,0.000525557,0.000077568606],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010055703,0.000082028826,0.08138898,0.0005277904,0.0004909722,0.00012941322,0.018363537,0.003061275,0.6597505,0.008402244,0.06475214,0.16204554],"study_design_scores_gemma":[0.0007663293,0.00019035987,0.96119803,0.00010232648,0.000030257499,0.00000441852,0.00036368557,0.0030499464,0.0085239755,0.012178429,0.013306672,0.00028554292],"about_ca_topic_score_codex":0.0021403893,"about_ca_topic_score_gemma":0.00018238396,"teacher_disagreement_score":0.8798091,"about_ca_system_score_codex":0.0000020354857,"about_ca_system_score_gemma":0.000029764362,"threshold_uncertainty_score":0.32356426},"labels":[],"label_agreement":null},{"id":"W4362660545","doi":"10.1093/gji/ggad152","title":"The coherence function and lithospheric elastic thickness of the Zagros fold and thrust belt","year":2023,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lithosphere; Bouguer anomaly; Seismology; Crust; Geodesy; Gravity anomaly; Geophysics; Tectonics","score_opus":0.008335098429142982,"score_gpt":0.2069080568763222,"score_spread":0.1985729584471792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362660545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958516,0.00010224362,0.0001169783,0.0011622937,0.00196824,0.000069376154,0.00004313778,0.000009584998,0.00067656755],"genre_scores_gemma":[0.99876344,0.0001122152,0.000025414174,0.000072292976,0.00045080605,9.751692e-7,0.000008136799,0.0000024488286,0.0005642756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907655,0.00007956642,0.00020751948,0.00011782698,0.00037265907,0.00014590599],"domain_scores_gemma":[0.99925625,0.00033739835,0.00016067398,0.00009175774,0.000096636235,0.00005728191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003261182,0.00008260112,0.00011160804,0.000015199755,0.00033714328,0.00020334506,0.00025264488,0.000030668107,0.00021084232],"category_scores_gemma":[0.00007559564,0.000041359042,0.00004895267,0.00013307208,0.00016098729,0.00015302289,0.00005691578,0.00015641988,0.000042740838],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000993977,0.000182427,0.4687538,0.00011981355,0.001008379,0.000044874505,0.0017460735,0.00527107,0.04911648,0.05950767,0.015278951,0.39797646],"study_design_scores_gemma":[0.00016318625,0.00006476197,0.96828175,0.000023984681,0.000020333493,0.000024367166,0.00007146248,0.0024914404,0.00012460815,0.02633013,0.0023456116,0.000058352533],"about_ca_topic_score_codex":0.00019254937,"about_ca_topic_score_gemma":0.00006137972,"teacher_disagreement_score":0.49952793,"about_ca_system_score_codex":0.0000019167157,"about_ca_system_score_gemma":0.00002743803,"threshold_uncertainty_score":0.2593068},"labels":[],"label_agreement":null},{"id":"W4366590978","doi":"10.3389/feart.2023.1187683","title":"Gravity inversion constrained by OBS receiver function reveals crustal structure in Ryukyu Trench","year":2023,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Subduction; Geology; Trench; Seismology; Gravity anomaly; Lithosphere; Seafloor spreading; Tectonics; Plate tectonics; Geophysics; Paleontology; Layer (electronics)","score_opus":0.006022235967516659,"score_gpt":0.19230208294579687,"score_spread":0.1862798469782802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366590978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952294,0.00009066598,0.00011605914,0.00010232032,0.0028545468,0.00021355778,0.0003053068,0.000046303314,0.001041798],"genre_scores_gemma":[0.998084,0.00005839547,0.0010318764,0.0000944742,0.000054847776,0.0000010892974,0.00014806484,0.0000026430973,0.0005245711],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99819255,0.000090899324,0.00024048593,0.00047793117,0.0004658607,0.0005322845],"domain_scores_gemma":[0.9995098,0.00003639382,0.00007994803,0.00020149437,0.000036381563,0.00013599738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077768526,0.0001441899,0.00023072898,0.0003613871,0.00019544778,0.0001093738,0.00034375663,0.000090462505,0.00044131023],"category_scores_gemma":[0.00008640178,0.00012687381,0.000028725572,0.0019097491,0.0004672059,0.0006059755,0.000031662,0.00016073394,0.00007559177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011080649,0.000019805784,0.8810963,0.00003299566,0.0000065175354,0.00003459022,0.00070114,0.0041018133,0.0409927,0.00008458852,0.03523104,0.037587695],"study_design_scores_gemma":[0.0004887353,0.00009631841,0.9767789,0.000033216613,0.0000053258655,0.0000015253538,0.00035257073,0.008076649,0.001641768,0.0053501097,0.006928812,0.00024605865],"about_ca_topic_score_codex":0.0014040165,"about_ca_topic_score_gemma":0.0009819383,"teacher_disagreement_score":0.095682606,"about_ca_system_score_codex":0.000009855319,"about_ca_system_score_gemma":0.000118034404,"threshold_uncertainty_score":0.51737636},"labels":[],"label_agreement":null},{"id":"W4366783150","doi":"10.1029/2022gc010807","title":"Manufacturing an Exact Solution for 2D Thermochemical Mantle Convection Models","year":2023,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle convection; Fortran; Python (programming language); Convection–diffusion equation; Convection; Mantle (geology); Advection; Exact solutions in general relativity; Correctness; Stream function; Mechanics; Thermodynamics; Computer science; Geology; Geophysics; Mathematical analysis; Algorithm; Mathematics; Physics; Lithosphere","score_opus":0.023209595969462878,"score_gpt":0.22555834136229055,"score_spread":0.20234874539282768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366783150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99383575,0.000046768087,0.0011222077,0.000052053292,0.0009890826,0.00043184022,0.0006057637,0.0003428606,0.0025736874],"genre_scores_gemma":[0.9945224,0.000016576614,0.000103576356,0.000022777544,0.0014180235,0.00003591705,0.0030927558,0.000017942619,0.00077004783],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9980967,0.000047149068,0.00033795217,0.00055817876,0.00032144165,0.00063857733],"domain_scores_gemma":[0.9989973,0.00010524644,0.00017319294,0.00045326437,0.000088271176,0.00018275804],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00035847904,0.00028177325,0.000343594,0.000043476404,0.00033568646,0.00015685422,0.00030942462,0.00018760255,0.00022170634],"category_scores_gemma":[0.000011654523,0.00026915094,0.00013954006,0.00015458812,0.00005050618,0.0004011734,0.000030397245,0.00012255476,0.0003495186],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025750964,0.00011887734,0.0006004988,0.0013682633,0.00020241768,0.000023915547,0.0007228932,0.02417255,0.9487281,0.0003796392,0.005059424,0.018365944],"study_design_scores_gemma":[0.0010363568,0.00016816103,0.0053623896,0.0001129538,0.0001041277,0.00002332003,0.00037316815,0.42675942,0.5268985,0.03339466,0.0047271554,0.0010397844],"about_ca_topic_score_codex":0.0018533126,"about_ca_topic_score_gemma":0.000059409675,"teacher_disagreement_score":0.42182955,"about_ca_system_score_codex":0.000011322069,"about_ca_system_score_gemma":0.00004823492,"threshold_uncertainty_score":0.99997604},"labels":[],"label_agreement":null},{"id":"W4367311569","doi":"10.3390/min13050619","title":"High-Pressure Experimental and DFT Structural Studies of Aurichalcite Mineral","year":2023,"lang":"en","type":"article","venue":"Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministerio de Ciencia e Innovación; Agencia Estatal de Investigación; Generalitat Valenciana; European Commission; Compute Canada","keywords":"Malachite; Monoclinic crystal system; Triclinic crystal system; Crystallography; Chemistry; Density functional theory; Ionic radius; Bulk modulus; Stoichiometry; Hydrogen bond; Crystal structure; Materials science; Copper; Molecule; Computational chemistry; Physical chemistry; Ion","score_opus":0.024325131274890104,"score_gpt":0.26976349931059773,"score_spread":0.24543836803570762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367311569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99554497,0.0028193956,3.6172636e-7,0.00014846782,0.000713037,0.00011823462,0.00030006174,0.000050727096,0.00030473658],"genre_scores_gemma":[0.9965659,0.0000655054,0.00025073267,0.00004627405,0.00026631515,0.0000024842982,0.00011211247,0.00000467467,0.0026860342],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99906814,0.000054157455,0.00022575588,0.00022010035,0.00018501592,0.00024682342],"domain_scores_gemma":[0.9995845,0.00008484802,0.00008071173,0.00014468706,0.00003813406,0.000067150184],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014663383,0.0001485879,0.00033088872,0.00007348408,0.000088098146,0.00003474068,0.000118973214,0.000043758522,0.0006018123],"category_scores_gemma":[0.000024372639,0.00010915775,0.00003842784,0.00016149045,0.000112525675,0.0001535174,0.000044068707,0.000036945712,0.000049350587],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078276345,0.000012941199,0.020431181,0.00018760818,0.0002865404,0.000037710393,0.0024432933,0.002824324,0.9481058,0.0014443275,0.023011744,0.0011362216],"study_design_scores_gemma":[0.003260477,0.0011845222,0.62964284,0.00017610232,0.00030698412,0.000036009496,0.0027642455,0.006521124,0.31322116,0.010898498,0.030374972,0.0016130791],"about_ca_topic_score_codex":0.0015255021,"about_ca_topic_score_gemma":0.00009886598,"teacher_disagreement_score":0.63488466,"about_ca_system_score_codex":7.755009e-7,"about_ca_system_score_gemma":0.000008031484,"threshold_uncertainty_score":0.6589423},"labels":[],"label_agreement":null},{"id":"W4378218246","doi":"10.1016/j.epsl.2023.118213","title":"On unusual conditions for the exhumation of subducted oceanic crustal rocks: How to make rocks hotter than models","year":2023,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Fundamental Research Funds for the Central Universities; National Key Research and Development Program of China; National University's Basic Research Foundation of China; National Natural Science Foundation of China","keywords":"Subduction; Geology; Eclogitization; Slab; Mantle wedge; Slab window; Mantle (geology); Geophysics; Asthenosphere; Metamorphic rock; Terrane; Petrology; Forearc; Seismology; Oceanic crust; Geochemistry; Tectonics","score_opus":0.01707036478627477,"score_gpt":0.21106215060233988,"score_spread":0.1939917858160651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378218246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926106,0.000025660229,0.0008595707,0.0040787105,0.00054018217,0.00045710505,0.0011712966,0.00004231527,0.00021458336],"genre_scores_gemma":[0.99729323,0.000013599287,0.00009918225,0.0016124742,0.00014295032,0.000003990411,0.00069625565,0.0000034745512,0.00013482179],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99867505,0.00003915194,0.00015993277,0.0003273399,0.00038553026,0.0004129979],"domain_scores_gemma":[0.99918956,0.00034995654,0.00007624109,0.00021064687,0.00003418271,0.00013944275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042503435,0.00014394664,0.0001656489,0.00019123087,0.0004848854,0.00017286799,0.0003004108,0.00003566089,0.00019422072],"category_scores_gemma":[0.000038624265,0.00009961005,0.00003907736,0.00044513508,0.00020424285,0.0003489232,0.000018382649,0.00007611889,0.00007274193],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041616915,0.00003118686,0.016800657,0.0001389027,0.00009686975,0.00003121906,0.0027558778,0.8753582,0.04952578,0.0008141117,0.044024426,0.010006554],"study_design_scores_gemma":[0.0004955063,0.00048235274,0.85439634,0.000046916906,0.00004260692,0.00001322462,0.00028830013,0.13755053,0.0023203562,0.0012645226,0.002711721,0.00038759934],"about_ca_topic_score_codex":0.0006386307,"about_ca_topic_score_gemma":0.0003646259,"teacher_disagreement_score":0.8375957,"about_ca_system_score_codex":0.0000012398722,"about_ca_system_score_gemma":0.000033451073,"threshold_uncertainty_score":0.406198},"labels":[],"label_agreement":null},{"id":"W4378421878","doi":"10.2139/ssrn.4459470","title":"Factory of Minerals. Dependence of the Geological Structure of the Deep Earth Interior on Earthquake Processes","year":2023,"lang":"en","type":"article","venue":"SSRN Electronic Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Earth (classical element); Factory (object-oriented programming); Geology; Geochemistry; Mining engineering; Seismology; Earth science; Physics","score_opus":0.008193534832695108,"score_gpt":0.2031473243792327,"score_spread":0.19495378954653758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378421878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988397,0.00037988968,0.000011395204,0.00013555076,0.00031310553,0.0001004894,0.000065566805,0.000005685009,0.00014861618],"genre_scores_gemma":[0.99925137,0.00032429025,0.000008137725,0.000024899857,0.00007691832,1.9906402e-7,0.0000034692498,0.000002810751,0.00030793095],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99857026,0.00013284072,0.00027415674,0.00011171135,0.0003399414,0.00057109847],"domain_scores_gemma":[0.9993016,0.000098862765,0.0003108356,0.00017447626,0.000086056614,0.00002817961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003783619,0.00010160467,0.0002057089,0.000037976457,0.00009643413,0.000013063671,0.00052751903,0.00005836093,0.00027982634],"category_scores_gemma":[0.00012473461,0.00004708144,0.0000921648,0.00028054876,0.00013918047,0.00006691852,0.00003392783,0.00043617137,0.0000062879685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007340202,0.000112750204,0.53828746,0.0005192315,0.00059876835,0.0000070509154,0.0024016218,0.029440835,0.3796635,0.014875529,0.00023068725,0.033128522],"study_design_scores_gemma":[0.0003401141,0.00062260055,0.869963,0.00011035194,0.00004636927,0.000055162946,0.00044271443,0.00011528983,0.08157935,0.04612179,0.0004603222,0.00014295265],"about_ca_topic_score_codex":0.00027949965,"about_ca_topic_score_gemma":0.0064937356,"teacher_disagreement_score":0.3316755,"about_ca_system_score_codex":0.000003858748,"about_ca_system_score_gemma":0.0005609407,"threshold_uncertainty_score":0.3623657},"labels":[],"label_agreement":null},{"id":"W4378938698","doi":"10.1007/s10948-023-06569-6","title":"On Magnetic Field Screening and Expulsion in Hydride Superconductors","year":2023,"lang":"en","type":"article","venue":"Journal of Superconductivity and Novel Magnetism","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Superconductivity; Condensed matter physics; Magnetic field; Magnetic flux; Meissner effect; Flux (metallurgy); Physics; Signature (topology); Materials science; Quantum mechanics","score_opus":0.021508060086368755,"score_gpt":0.22399857896265069,"score_spread":0.20249051887628194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378938698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997548,0.0006262342,0.000025426338,0.00084572355,0.0006354497,0.00008760743,0.000022176668,0.000011087687,0.00019831164],"genre_scores_gemma":[0.998594,0.0005994623,0.00042001816,0.00012395423,0.00013421469,4.7222866e-7,0.0000049059545,0.0000049406144,0.00011802912],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989481,0.000071264905,0.00030444397,0.00020138225,0.00022837316,0.00024644926],"domain_scores_gemma":[0.9992634,0.00041586178,0.00006195452,0.000099632416,0.000028725672,0.00013041048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061523996,0.00014549302,0.00031190616,0.0002694816,0.000089939036,0.00008039707,0.00010487098,0.000096950964,0.0005989122],"category_scores_gemma":[0.00013499499,0.000116112744,0.000042810647,0.00020928844,0.00007257144,0.00074503396,0.000027067204,0.00024977062,0.00001367766],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050551165,0.00019231712,0.08900199,0.00026302773,0.000053050244,0.0005351432,0.0029462497,0.0010049681,0.6684468,0.0015500514,0.0022665774,0.23323433],"study_design_scores_gemma":[0.0014967673,0.0019600142,0.9836822,0.00024081714,0.000030486448,0.00020926406,0.00074572227,0.0007012316,0.0031771618,0.0062649036,0.0011727328,0.00031870944],"about_ca_topic_score_codex":0.0016385695,"about_ca_topic_score_gemma":0.000432391,"teacher_disagreement_score":0.8946802,"about_ca_system_score_codex":0.0000020177818,"about_ca_system_score_gemma":0.000020058906,"threshold_uncertainty_score":0.65576684},"labels":[],"label_agreement":null},{"id":"W4379520449","doi":"10.1139/cjp-2022-0317","title":"Phase shift and cross section analysis of nucleon–nucleon and nucleon–nucleus scattering using second Pöschl–Teller potential","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Nucleon; Scattering; Cross section (physics); Phase (matter); Parameterized complexity; Nucleus; Scattering length; Nuclear physics; Atomic physics; Quantum mechanics","score_opus":0.01697124867387747,"score_gpt":0.24022312978423171,"score_spread":0.22325188111035424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379520449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983368,0.00011843045,0.00016307663,0.000061265186,0.0006571619,0.000058126556,0.0004674094,0.000007607963,0.00013013172],"genre_scores_gemma":[0.9993148,0.000020841435,0.0001487055,0.000040411334,0.00041260617,9.197636e-8,0.000029486853,0.000009850194,0.000023202989],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99892586,0.00005459225,0.00036280986,0.00018077236,0.00016809211,0.0003078973],"domain_scores_gemma":[0.99904627,0.000035887362,0.00029377302,0.0001272306,0.00009502859,0.00040180003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030617273,0.00014475266,0.00039251035,0.00033560002,0.00029339662,0.0002425217,0.00013772301,0.00007059636,0.00041953629],"category_scores_gemma":[0.000011840652,0.00014218569,0.00011776286,0.0005693875,0.00017784888,0.00046689942,0.000013422777,0.00012807095,0.000005975794],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063389697,0.00022529368,0.26663637,0.00085598225,0.006706738,0.00120122,0.016070751,0.26937562,0.3191398,0.0015332574,0.0021464704,0.11547458],"study_design_scores_gemma":[0.0021508485,0.0004294372,0.9269548,0.00010150144,0.0011582242,0.00006045461,0.00048834854,0.058355935,0.0039491737,0.0023005023,0.0034890848,0.00056167075],"about_ca_topic_score_codex":0.015060214,"about_ca_topic_score_gemma":0.016366556,"teacher_disagreement_score":0.66031843,"about_ca_system_score_codex":0.000007806365,"about_ca_system_score_gemma":0.0001926549,"threshold_uncertainty_score":0.9914986},"labels":[],"label_agreement":null},{"id":"W4381685270","doi":"10.1051/epjconf/202328502002","title":"The Münster cluster-jet target for the future PANDA experiment","year":2023,"lang":"en","type":"article","venue":"EPJ Web of Conferences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nozzle; Cluster (spacecraft); Jet (fluid); Storage ring; Physics; Beam (structure); Nuclear physics; Ring (chemistry); Work (physics); Aerospace engineering; Atomic physics; Mechanical engineering; Mechanics; Computer science; Optics; Engineering; Chemistry; Thermodynamics; Operating system","score_opus":0.018076481158725302,"score_gpt":0.2420696860742234,"score_spread":0.22399320491549812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381685270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9545753,0.0037099726,0.00017357945,0.0131126065,0.0086790975,0.0011873504,0.00083531876,0.00010460106,0.017622167],"genre_scores_gemma":[0.9978973,0.00040752193,0.00006970193,0.00009130352,0.00062069646,0.00001711046,0.00006372593,0.0000024933154,0.0008301335],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991523,0.00006280049,0.00019322778,0.00014132571,0.00021184432,0.00023849272],"domain_scores_gemma":[0.9990358,0.00056997617,0.00009618329,0.0002031588,0.000056040055,0.00003886063],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000491427,0.000106868305,0.00015975567,0.000019936135,0.00031657668,0.00014078242,0.0003952082,0.000041288306,0.0009302721],"category_scores_gemma":[0.00001819877,0.000046456797,0.00006798554,0.00009394029,0.00012029109,0.00006698594,0.000023563063,0.000043414744,0.00008924075],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012172913,0.00009589332,0.12319879,0.00032093358,0.0009585201,0.000009857048,0.0067969332,0.0034797692,0.006321715,0.08801084,0.47362694,0.2959625],"study_design_scores_gemma":[0.00024244467,0.00014857484,0.029088398,0.0000113672995,0.000016926237,4.3695417e-7,0.0013142645,0.003330783,0.0030158437,0.0042600734,0.9584646,0.000106240965],"about_ca_topic_score_codex":0.00031688382,"about_ca_topic_score_gemma":0.0008644499,"teacher_disagreement_score":0.4848377,"about_ca_system_score_codex":5.4701053e-7,"about_ca_system_score_gemma":0.00016064537,"threshold_uncertainty_score":0.999983},"labels":[],"label_agreement":null},{"id":"W4383373964","doi":"10.1029/2022gc010570","title":"The Thermal Regime of NW Canada and Alaska, and Tectonic and Seismicity Consequences","year":2023,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Lithosphere; Terrane; Crust; Craton; Asthenosphere; Mantle (geology); Forearc; Seismology; Underplating; Tectonophysics; Subduction; Tectonics; Geophysics; Petrology","score_opus":0.005813950046292168,"score_gpt":0.17441555454129862,"score_spread":0.16860160449500644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383373964","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972112,0.00096113235,4.4164884e-7,0.00027205033,0.00022409273,0.00013834002,0.00037208747,0.000025857342,0.00079475157],"genre_scores_gemma":[0.9990493,0.00024318614,0.000005018851,0.000028731642,0.0001356752,0.000003403766,0.00005879766,0.000004224952,0.00047164262],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988707,0.00005361787,0.0002351821,0.0002810656,0.00023340917,0.00032602638],"domain_scores_gemma":[0.9991284,0.00031313908,0.00015976343,0.00023162046,0.000054458622,0.000112644884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002981815,0.00016904033,0.00026847338,0.000012035734,0.00029646893,0.000097696466,0.00015371422,0.00006181623,0.000019852858],"category_scores_gemma":[0.000027115082,0.00012049702,0.000021548221,0.00013618717,0.00033317876,0.00007062593,0.00005353792,0.000089632835,0.0000053234817],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031151052,0.000047234786,0.43545237,0.0047221836,0.00094237225,0.00025099792,0.002579142,0.0016952094,0.49622175,0.0013580612,0.010311286,0.04610787],"study_design_scores_gemma":[0.0012774187,0.00020840038,0.8468057,0.00035791632,0.00018149604,0.0001597621,0.002337609,0.00865192,0.1077108,0.009632496,0.021327218,0.001349292],"about_ca_topic_score_codex":0.54841757,"about_ca_topic_score_gemma":0.07348928,"teacher_disagreement_score":0.47492832,"about_ca_system_score_codex":0.0000027745145,"about_ca_system_score_gemma":0.00017681789,"threshold_uncertainty_score":0.94341713},"labels":[],"label_agreement":null},{"id":"W4383908931","doi":"10.5194/ejm-35-461-2023","title":"Elasticity of mixtures and implications for piezobarometry of mixed-phase inclusions","year":2023,"lang":"en","type":"article","venue":"European Journal of Mineralogy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"H2020 European Research Council; Horizon 2020 Framework Programme; Japan Agency for Marine-Earth Science and Technology; European Commission","keywords":"Elasticity (physics); Isotropy; Entrapment; Phase (matter); Inclusion (mineral); Thermodynamics; Materials science; Mineralogy; Chemistry; Composite material; Physics","score_opus":0.022539891710893455,"score_gpt":0.2684550111949666,"score_spread":0.24591511948407316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383908931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974897,0.00020410217,0.0006973236,0.00035336142,0.0002939761,0.00005604466,0.00045156028,0.000004246642,0.00044967586],"genre_scores_gemma":[0.9984881,0.00008557546,0.0011526806,0.000024136461,0.00016803814,1.1242304e-7,0.00003356812,0.0000036948613,0.00004406421],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99923134,0.00013808589,0.0003761982,0.00007107449,0.000072705276,0.000110616],"domain_scores_gemma":[0.9991586,0.00026746813,0.0002972696,0.00008449627,0.00011821519,0.000073928335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058095716,0.00006126676,0.0002199887,0.00014451254,0.00005658488,0.000007685351,0.00015462213,0.000014684163,0.00007429428],"category_scores_gemma":[0.00016895575,0.000045575376,0.000056615292,0.0001550533,0.000072703624,0.000051231324,0.0000281184,0.000044389253,0.000006034896],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036228474,0.00017797833,0.030205378,0.00020784218,0.00020099449,0.000044213186,0.0006997238,0.0022098883,0.8913639,0.0016183394,0.02947712,0.043432314],"study_design_scores_gemma":[0.0010833851,0.0009885827,0.9859549,0.00003301056,0.00006874876,0.000042135427,0.000028623008,0.000122146,0.0032996105,0.0019422657,0.0063534267,0.00008315808],"about_ca_topic_score_codex":0.00003901959,"about_ca_topic_score_gemma":0.000021933203,"teacher_disagreement_score":0.9557495,"about_ca_system_score_codex":5.172388e-7,"about_ca_system_score_gemma":0.000022510649,"threshold_uncertainty_score":0.185851},"labels":[],"label_agreement":null},{"id":"W4384023593","doi":"10.1093/gji/ggad284","title":"Imaging the crustal structure at the northeast corner of the indenting Indian Plate in the Eastern Himalayan Syntaxis","year":2023,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Wadia Institute of Himalayan Geology","keywords":"Geology; Seismology; Crust; Fibrous joint; Tectonics; Anticline; Window (computing); Receiver function; Induced seismicity; Geophysics; Lithosphere","score_opus":0.008424778221786734,"score_gpt":0.2170486362117078,"score_spread":0.20862385798992109,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384023593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920729,0.000025177666,0.0000049589225,0.00538691,0.0015367153,0.00013064116,0.0002921343,0.000007034584,0.00054352265],"genre_scores_gemma":[0.9982454,0.000009109304,0.000004549015,0.00042771353,0.0009332808,0.0000014861431,0.000040458985,0.000005082193,0.00033288644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982683,0.00023456046,0.0003135413,0.00015026638,0.0007463315,0.0002870228],"domain_scores_gemma":[0.9991086,0.00029450163,0.00026808647,0.00021529516,0.000072694296,0.00004078607],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053165643,0.00013463135,0.00013362074,0.000051271185,0.00048092945,0.00028521125,0.0011797638,0.00003148518,0.00059522747],"category_scores_gemma":[0.000053613177,0.000052555155,0.00014241217,0.00028626106,0.00020061419,0.00019331231,0.00014226718,0.00044455458,0.00013108947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008992477,0.000031990035,0.9669134,0.00001109842,0.00012937153,0.00009024205,0.0045840275,0.00813877,0.0016026736,0.00063603144,0.0014165746,0.01635592],"study_design_scores_gemma":[0.0001923352,0.000013513142,0.98773336,0.00003697334,0.000016668286,0.00013457418,0.0007524334,0.0047495672,0.00015040363,0.004095592,0.0020416335,0.00008295487],"about_ca_topic_score_codex":0.0014740023,"about_ca_topic_score_gemma":0.0016428226,"teacher_disagreement_score":0.020819977,"about_ca_system_score_codex":0.000008807435,"about_ca_system_score_gemma":0.000045309844,"threshold_uncertainty_score":0.6517323},"labels":[],"label_agreement":null},{"id":"W4384938954","doi":"10.1134/s1028334x23600640","title":"Comparison of the I and IV Diamond Types (According to Orlov’s Classification) from the Snap Lake Deposit (Slave Craton, Canada)","year":2023,"lang":"en","type":"article","venue":"Doklady Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Kimberlite; Craton; Geology; Diamond; Geochemistry; Mantle (geology); Mineralogy; Paleontology; Materials science; Metallurgy; Tectonics","score_opus":0.03116192711799357,"score_gpt":0.24968877984668333,"score_spread":0.21852685272868977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384938954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952277,0.0001605302,0.000008763536,0.0017988725,0.0007940097,0.00016613808,0.00022457149,0.000016225316,0.0016032102],"genre_scores_gemma":[0.9994138,0.000014311365,0.00009496073,0.00023468069,0.00009970023,0.0000017543483,0.0000211675,0.0000018097153,0.00011785552],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998799,0.00008394419,0.00019966217,0.00024657237,0.0004365029,0.00023429429],"domain_scores_gemma":[0.99922067,0.0003562457,0.00010419443,0.00020720049,0.00003667555,0.00007503378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003720926,0.00009468883,0.00016533169,0.000028462879,0.00059174123,0.00018193667,0.00048917934,0.000026208209,0.00018807968],"category_scores_gemma":[0.000072845956,0.00004979024,0.000022828845,0.00051478134,0.00021863636,0.00012071658,0.00005435941,0.00006041515,0.000045383887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000049226496,0.0000033161182,0.9910915,0.000004706203,0.000009670005,8.927533e-7,0.00071608805,0.0014102344,0.001717033,0.00027355104,0.0019908578,0.0027772123],"study_design_scores_gemma":[0.000039074013,0.000028673767,0.98165673,0.000017502405,0.000011832898,4.4087153e-7,0.0011351886,0.0036672968,0.0027946278,0.00027401195,0.010292464,0.00008216725],"about_ca_topic_score_codex":0.21686806,"about_ca_topic_score_gemma":0.87402135,"teacher_disagreement_score":0.6571533,"about_ca_system_score_codex":9.0970525e-7,"about_ca_system_score_gemma":0.0001514719,"threshold_uncertainty_score":0.7883469},"labels":[],"label_agreement":null},{"id":"W4385325704","doi":"10.1007/978-3-662-65093-6_1864","title":"Asthenosphere","year":2023,"lang":"en","type":"book-chapter","venue":"Encyclopedia of Astrobiology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology","score_opus":0.009788377646374554,"score_gpt":0.19032352906810593,"score_spread":0.18053515142173138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385325704","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0028772182,0.0002468877,0.00001074436,0.000049465532,0.0024672146,0.00018027503,0.0013480694,0.000070492395,0.99274963],"genre_scores_gemma":[0.007277075,0.0013843108,0.0006260624,0.00003814668,0.0010642742,0.0000014361215,0.001548724,0.000028213415,0.98803174],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988631,0.000027634764,0.0003755583,0.00033274063,0.00011424775,0.00028671918],"domain_scores_gemma":[0.9991674,0.00014402685,0.0002789739,0.00028785475,0.00004622811,0.000075542135],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00013794549,0.00026214478,0.00055690296,0.00006191342,0.000040845887,0.000008448015,0.00031695943,0.00033298973,0.014425768],"category_scores_gemma":[0.000014948265,0.000218421,0.0001292708,0.000024237637,0.00015578813,0.00003622435,0.000038051116,0.00018483998,0.004161718],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058581616,0.00007968455,0.021168703,0.0009566001,0.0020754982,0.00045614695,0.0009196643,0.0032538099,0.00086701376,0.37400526,0.28837526,0.30725655],"study_design_scores_gemma":[0.00015818946,0.0003177951,0.007825118,0.000061427905,0.0000626832,0.0000052423534,0.000007669268,0.0000048631086,0.000017829763,0.024127452,0.9670934,0.000318342],"about_ca_topic_score_codex":0.0002811125,"about_ca_topic_score_gemma":0.00044057245,"teacher_disagreement_score":0.67871815,"about_ca_system_score_codex":0.0000014896691,"about_ca_system_score_gemma":0.00007538013,"threshold_uncertainty_score":0.9966137},"labels":[],"label_agreement":null},{"id":"W4385519594","doi":"10.22541/essoar.169111390.09109030/v1","title":"Structure, origin, and deformation of the lithosphere in the northern Canadian Cordillera from high-resolution, passive-source seismic velocity models","year":2023,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"National Science Foundation","keywords":"Geology; Lithosphere; Seismology; Craton; Mantle (geology); Crust; Seismic tomography; Seismic anisotropy; Shear wave splitting; Shear zone; Geophysics; Tectonics","score_opus":0.01518721983392326,"score_gpt":0.19069219744385588,"score_spread":0.1755049776099326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385519594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99430996,0.000114538154,0.000246686,0.0007472627,0.0007316696,0.0004476385,0.0029091116,0.000020682708,0.000472444],"genre_scores_gemma":[0.998482,0.00005777595,0.00017180333,0.00023189299,0.00012913859,0.0000038931366,0.0007966442,0.000006255204,0.00012058413],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9987369,0.00013407883,0.00031687468,0.00027521787,0.0002879056,0.00024898953],"domain_scores_gemma":[0.9991399,0.000080686674,0.00020442336,0.00042346993,0.0000754354,0.000076106255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018789683,0.00019836327,0.000280134,0.000041848583,0.00018719697,0.00012731261,0.00052843074,0.00019759651,0.00038737248],"category_scores_gemma":[0.000013589465,0.00010750074,0.000048387017,0.00014744407,0.000078137375,0.000111841946,0.00008000646,0.0002835743,0.000017229197],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019927751,0.00000688129,0.07891816,0.000092658534,0.00008193984,0.00000325461,0.0032567368,0.91101664,0.000010095766,0.00043280245,0.0011137992,0.0050471094],"study_design_scores_gemma":[0.00015224729,0.000012485899,0.7619429,0.00007167781,0.000043302927,9.939547e-7,0.00034054744,0.19023684,0.000051267718,0.04584459,0.0010905328,0.00021261796],"about_ca_topic_score_codex":0.95482767,"about_ca_topic_score_gemma":0.9376352,"teacher_disagreement_score":0.7207798,"about_ca_system_score_codex":0.000014345692,"about_ca_system_score_gemma":0.00029159331,"threshold_uncertainty_score":0.43837526},"labels":[],"label_agreement":null},{"id":"W4385855784","doi":"10.1093/mnras/stad2486","title":"A mineralogical reason why all exoplanets cannot be equally oxidizing","year":2023,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Science and Technology Facilities Council; Vanderbilt University; National Aeronautics and Space Administration","keywords":"Exoplanet; Planet; Mineral redox buffer; Physics; Silicate; Astrobiology; Outgassing; Mantle (geology); Astrophysics; Refractory (planetary science); Terrestrial planet; Stars; Oxygen; Astronomy; Geophysics","score_opus":0.020363479981411244,"score_gpt":0.20935966221038946,"score_spread":0.1889961822289782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385855784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960846,0.00007876178,0.000003021857,0.0018760647,0.0004998348,0.00017238958,0.00048463562,0.000061528364,0.0007392028],"genre_scores_gemma":[0.99761283,6.1421616e-7,0.0011819764,0.0003883013,0.00027649562,0.000002498855,0.00022232492,0.0000066576354,0.0003083062],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99850756,0.000112587666,0.0003115912,0.0003071424,0.00028445243,0.00047667837],"domain_scores_gemma":[0.99917376,0.00022125691,0.00017000908,0.00027218342,0.00002419578,0.00013861094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040454848,0.00018751762,0.00031313451,0.000011901227,0.00015540594,0.000078529345,0.0005598785,0.000116245814,0.00045419385],"category_scores_gemma":[0.000036488047,0.00012299021,0.00027358768,0.0001107788,0.00014646996,0.000087807064,0.00011552031,0.00015780985,0.00009122916],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005314603,0.00002965371,0.023565667,0.000030389343,0.00010128546,0.000001203958,0.00033145738,0.9388656,0.00050114753,0.000038048136,0.035848007,0.000634376],"study_design_scores_gemma":[0.00037571337,0.000118680575,0.6336824,0.000026883006,0.000080614576,2.9815027e-8,0.00014103582,0.32604647,0.0004548842,0.000077519144,0.038735695,0.00026006656],"about_ca_topic_score_codex":0.008964856,"about_ca_topic_score_gemma":0.0009071104,"teacher_disagreement_score":0.61281914,"about_ca_system_score_codex":0.000007920733,"about_ca_system_score_gemma":0.00003451687,"threshold_uncertainty_score":0.99763453},"labels":[],"label_agreement":null},{"id":"W4386444256","doi":"10.1007/s40766-023-00045-6","title":"Imperfections in natural diamond: the key to understanding diamond genesis and the mantle","year":2023,"lang":"en","type":"article","venue":"Rivista Del Nuovo Cimento","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Università degli Studi di Padova; University of Alberta","keywords":"Kimberlite; Diamond; Mantle (geology); Geology; Lithosphere; Geochemistry; Earth science; Tectonics; Transition zone; Paleontology; Chemistry","score_opus":0.01773867741473173,"score_gpt":0.2231874193308399,"score_spread":0.20544874191610818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386444256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99367034,0.00057685876,0.00007786848,0.0028701194,0.00059190305,0.0003874799,0.000085278545,0.000046169855,0.0016939681],"genre_scores_gemma":[0.9982415,0.0001313719,0.000022084045,0.00030147634,0.00010648491,0.000011429741,0.000027367267,0.0000054499847,0.0011528616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901205,0.00012361487,0.00015673634,0.00021438644,0.00018583875,0.00030738945],"domain_scores_gemma":[0.9993601,0.00031463537,0.000036616948,0.00020973329,0.0000086559985,0.00007027581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005464254,0.00011825202,0.00015599113,0.00008039248,0.0003726287,0.0002424459,0.00019507534,0.000028254186,0.00022170655],"category_scores_gemma":[0.000025519328,0.000065159285,0.000039928203,0.0004102331,0.00009431934,0.000108969856,0.000053009993,0.00007926545,0.00030122313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017505431,0.00020632628,0.41586232,0.0003621537,0.0010460585,0.00027312434,0.06931399,0.029056167,0.030825166,0.17983128,0.25533235,0.016140515],"study_design_scores_gemma":[0.0016281281,0.00010327807,0.9139344,0.000046671033,0.00009258844,0.000009945629,0.003355973,0.014119587,0.0006793023,0.018017214,0.047486663,0.0005262276],"about_ca_topic_score_codex":0.0064190025,"about_ca_topic_score_gemma":0.005050637,"teacher_disagreement_score":0.4980721,"about_ca_system_score_codex":0.000010251343,"about_ca_system_score_gemma":0.000018889868,"threshold_uncertainty_score":0.97036546},"labels":[],"label_agreement":null},{"id":"W4386742301","doi":"10.3847/1538-4357/acec3a","title":"Using Giant Pulses to Measure the Impulse Response of the Interstellar Medium","year":2023,"lang":"en","type":"article","venue":"The Astrophysical Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Institute for Theoretical Astrophysics; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Council for the Arts","keywords":"Physics; Impulse response; Impulse (physics); Deconvolution; Pulsar; Astrophysics; Computational physics; Optics; Mathematical analysis","score_opus":0.027987181357999255,"score_gpt":0.24362788018092824,"score_spread":0.21564069882292897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386742301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940139,0.000028028446,0.00033617474,0.0043907575,0.0009808115,0.00014362465,0.00005626357,0.000011062909,0.000039386785],"genre_scores_gemma":[0.99878114,0.0000071115987,0.00017798551,0.00019207469,0.0007424641,4.578964e-7,0.0000012822736,0.000005555683,0.000091944625],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9980922,0.0006909516,0.00024667615,0.00011521822,0.00053968263,0.0003152996],"domain_scores_gemma":[0.9989777,0.00035282937,0.00014571987,0.00033933177,0.000077280034,0.00010713994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011986106,0.00012201456,0.00018906983,0.000035027548,0.000463445,0.0001276881,0.00084104075,0.000026640797,0.00015660176],"category_scores_gemma":[0.00015007087,0.00004706068,0.00015550951,0.00042186902,0.00017678227,0.00007962016,0.00009677367,0.00025758482,0.00015550693],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012966348,0.000026335441,0.0008550353,0.000008843995,0.00013101465,0.000030879495,0.0019075165,0.038243275,0.9455262,0.00014348887,0.003071091,0.008759726],"study_design_scores_gemma":[0.0005754825,0.0006478629,0.92123,0.00021635268,0.0002315584,0.00017518825,0.0016980162,0.0075938664,0.059136383,0.003992859,0.004159476,0.00034294542],"about_ca_topic_score_codex":0.00019961187,"about_ca_topic_score_gemma":0.000024603418,"teacher_disagreement_score":0.920375,"about_ca_system_score_codex":0.000004620368,"about_ca_system_score_gemma":0.00010024137,"threshold_uncertainty_score":0.3564491},"labels":[],"label_agreement":null},{"id":"W4386925434","doi":"10.4006/0836-1398-36.3.256","title":"Dielectric constant and magnetic permeability in the Newtonian gravitational field derived by the elastic energy","year":2023,"lang":"en","type":"article","venue":"Physics Essays","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Newtonian fluid; Permeability (electromagnetism); Dielectric; Classical mechanics; Electromagnetic radiation; Electromagnetic field; Magnetic field; Gravitational field; Mechanics; Quantum electrodynamics; Quantum mechanics","score_opus":0.009381486127941069,"score_gpt":0.20409413376582794,"score_spread":0.19471264763788687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386925434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98690027,0.00053181406,0.00034482082,0.0021721958,0.00029418705,0.000197785,0.00019240612,0.000031454012,0.009335095],"genre_scores_gemma":[0.9992591,0.000098369084,0.000012252518,0.00036159484,0.000102662445,0.000007966136,0.00009748335,0.0000023370167,0.000058242073],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9991822,0.00014173125,0.00011798122,0.00016584802,0.00017867141,0.00021354941],"domain_scores_gemma":[0.99890065,0.0008738242,0.0000340949,0.00014275368,0.000017860777,0.000030818697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022896913,0.00009310882,0.00010639836,0.000016851965,0.000171733,0.00008675835,0.00017772669,0.000025916603,0.00011224292],"category_scores_gemma":[0.00003544144,0.00005362026,0.000024240448,0.00029862544,0.00008935824,0.000063652165,0.000014004009,0.00007706525,0.000030402236],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000295212,0.00033839495,0.13088821,0.00025010976,0.00013485386,0.000077712226,0.013479781,0.006951802,0.043902483,0.47362217,0.042454306,0.28760496],"study_design_scores_gemma":[0.0005017341,0.0003012885,0.1815365,0.000019416273,0.00004603932,0.0000065348427,0.00045429505,0.025508877,0.0007775516,0.78722227,0.0032880153,0.00033751002],"about_ca_topic_score_codex":0.0018919901,"about_ca_topic_score_gemma":0.00066936313,"teacher_disagreement_score":0.31360006,"about_ca_system_score_codex":0.0000013055474,"about_ca_system_score_gemma":0.000028287406,"threshold_uncertainty_score":0.28601354},"labels":[],"label_agreement":null},{"id":"W4386927461","doi":"10.1029/2023gl103994","title":"Thermal Conductivity of Hydrogen at High Pressure and High Temperature: Implications to Giant Planets","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Academia Sinica; Natural Sciences and Engineering Research Council of Canada; National Science and Technology Council","keywords":"Thermal conductivity; Planet; Hydrogen; Thermodynamics; Thermal; Materials science; Crystallization; Physics; Analytical Chemistry (journal); Chemistry; Astrophysics","score_opus":0.029937452325776527,"score_gpt":0.277511227766691,"score_spread":0.2475737754409145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386927461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99014235,0.000041256484,8.216606e-7,0.0078920815,0.00014028381,0.00041703944,0.0012138154,0.00005056477,0.000101769925],"genre_scores_gemma":[0.9986281,0.000016971386,0.0000578364,0.00025483474,0.0003124617,0.000017315038,0.0003438577,0.000008770341,0.00035986176],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99785656,0.00026220232,0.0001852209,0.00045631014,0.0005949197,0.0006447956],"domain_scores_gemma":[0.99869055,0.00049087533,0.000044264638,0.000406443,0.00008046152,0.00028740114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047474555,0.00015481147,0.00028733356,0.00013249094,0.00030829007,0.00007712266,0.00034202822,0.00007362347,0.00035547098],"category_scores_gemma":[0.00008108273,0.00012298637,0.000044257613,0.0005654067,0.00026687206,0.00014866839,0.00016555296,0.00022345583,0.0007598809],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009694752,0.000023949142,0.0018613084,0.0000527581,0.000067646724,0.00001750461,0.00017209222,0.002563446,0.98113567,0.0006350137,0.011980281,0.0013933614],"study_design_scores_gemma":[0.00026115926,0.00018205112,0.9379389,0.000018178369,0.00002301838,0.0000018814878,0.00001704761,0.00023297628,0.055325374,0.0010683617,0.0047274693,0.00020352405],"about_ca_topic_score_codex":0.008023793,"about_ca_topic_score_gemma":0.00021849394,"teacher_disagreement_score":0.93607765,"about_ca_system_score_codex":0.000004184047,"about_ca_system_score_gemma":0.000037899757,"threshold_uncertainty_score":0.9985819},"labels":[],"label_agreement":null},{"id":"W4386998048","doi":"10.1029/2023jb027274","title":"Modes of Mantle Convection, Their Stability, and What Controls Their Existence","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Geological Survey of Canada; Natural Resources Canada","funders":"David and Lucile Packard Foundation","keywords":"Mantle convection; Convection; Mantle (geology); Rayleigh number; Geophysics; Geology; Plate tectonics; Physics; Mechanics; Natural convection; Tectonics; Lithosphere","score_opus":0.07012139041216651,"score_gpt":0.31869705933074505,"score_spread":0.24857566891857852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386998048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981617,0.00043889176,0.000018300829,0.00044473773,0.0002509598,0.0001749717,0.00008348321,0.000012228885,0.0004147655],"genre_scores_gemma":[0.99747384,0.0019463492,0.000045951198,0.000022778162,0.00037810692,0.0000011228925,0.000008409014,0.0000053475906,0.00011808259],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99774563,0.0004190804,0.00043546455,0.0001984703,0.0007335868,0.0004677761],"domain_scores_gemma":[0.9974922,0.0012502118,0.00019510463,0.00022165067,0.0005905427,0.0002503009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021896984,0.00013480264,0.0005136456,0.00017006409,0.00017762261,0.00028139792,0.00031519565,0.00006112187,0.00028952552],"category_scores_gemma":[0.00025958603,0.00008562346,0.0001256168,0.00044121608,0.00043453518,0.00087897625,0.00006715755,0.0003362399,0.00008243097],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029002477,0.00063592574,0.025174508,0.0009291867,0.0007801699,0.00021565269,0.007910082,0.0024236457,0.797729,0.005771263,0.0018380065,0.15369232],"study_design_scores_gemma":[0.0020165714,0.0038968627,0.610243,0.0005400844,0.00004332193,0.000054082,0.008910363,0.026110832,0.22920091,0.11199587,0.0065070554,0.0004810236],"about_ca_topic_score_codex":0.0005257686,"about_ca_topic_score_gemma":0.0001123059,"teacher_disagreement_score":0.5850685,"about_ca_system_score_codex":0.0000029110765,"about_ca_system_score_gemma":0.0001443521,"threshold_uncertainty_score":0.34916234},"labels":[],"label_agreement":null},{"id":"W4387078932","doi":"10.1029/2023jb027428","title":"Variations of Crustal Thickness in Alaska and Northwestern Canada: Implications for Crustal Modification and Accretion of Tectonic Units","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Terrane; Subduction; Seismology; Tectonics; Accretion (finance); Craton; Crust; Continental margin; North American Plate; Plate tectonics; Continental crust; Paleontology","score_opus":0.058418629863625886,"score_gpt":0.32459378735528743,"score_spread":0.26617515749166154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387078932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984774,0.000048495876,0.00015376901,0.00055363885,0.00006401569,0.00022733536,0.00042309315,0.0000028512707,0.000049398157],"genre_scores_gemma":[0.99952066,0.00016326582,0.00011094941,0.0000057149537,0.000091856404,0.0000033443737,0.000058436846,0.0000036263166,0.000042175343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987265,0.00013228726,0.00038994988,0.00012855825,0.00037540856,0.00024732685],"domain_scores_gemma":[0.9981467,0.0007382434,0.00020955359,0.000117121235,0.00066756835,0.000120828794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083302765,0.00007377623,0.00026895566,0.00021640153,0.000108398846,0.000034852485,0.00014018496,0.000048340204,0.0000139769045],"category_scores_gemma":[0.00029185234,0.00006137299,0.000028658016,0.0006374357,0.00012897092,0.0002094455,0.000028919727,0.0001692456,0.0000012402534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002456702,0.00075528835,0.44706213,0.0025458164,0.000544443,0.000048542548,0.009144828,0.034391187,0.3484102,0.03057539,0.001851467,0.122214004],"study_design_scores_gemma":[0.0003683275,0.00027186744,0.9900075,0.000046952628,0.000013494994,0.0000042752918,0.00020755942,0.003972441,0.0011201048,0.0037665775,0.00016300523,0.000057872956],"about_ca_topic_score_codex":0.08387964,"about_ca_topic_score_gemma":0.11351342,"teacher_disagreement_score":0.5429454,"about_ca_system_score_codex":0.000006128819,"about_ca_system_score_gemma":0.00071543915,"threshold_uncertainty_score":0.9222209},"labels":[],"label_agreement":null},{"id":"W4387113880","doi":"10.1016/j.epsl.2023.118386","title":"The development of rifting and magmatism in the multiply rifted Turkana Depression, East Africa: Evidence from surface-wave analysis of crustal and uppermost mantle structure","year":2023,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Sight Research UK; Incorporated Research Institutions for Seismology; National Science Foundation","keywords":"Geology; Rift; Craton; East African Rift; Lithosphere; Mantle (geology); Crust; Paleontology; Proterozoic; Seismology; Structural basin; Tectonics","score_opus":0.01987942164117021,"score_gpt":0.20324845279639886,"score_spread":0.18336903115522865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387113880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981352,0.0008441107,0.000009876878,0.0003738507,0.0000904442,0.00014370547,0.00037392278,0.000007062693,0.000021814947],"genre_scores_gemma":[0.9985586,0.00009722435,0.0011362117,0.00006879091,0.000017170412,3.5850366e-7,0.00011468593,0.0000014412473,0.000005547372],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99859995,0.00011891281,0.0002891022,0.000300744,0.00040100684,0.00029030663],"domain_scores_gemma":[0.99893105,0.00066293176,0.00013459599,0.00017750125,0.000018374325,0.00007555792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008833698,0.00012643688,0.00022919755,0.00013342724,0.0003911722,0.00012455751,0.00023855636,0.000034367786,0.000053151754],"category_scores_gemma":[0.000065901644,0.000071248025,0.000017951224,0.0008270357,0.00045090783,0.00025811984,0.000046573892,0.00010021898,0.000002155574],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004223925,0.000002674545,0.9269973,0.000026360838,0.000064184496,0.000015952155,0.009642428,0.0066400017,0.046475656,0.0000029457822,0.00006253188,0.010027747],"study_design_scores_gemma":[0.00010002526,0.000014354458,0.97380346,0.00004246823,0.000045251796,0.000002663959,0.0006859951,0.02445319,0.0006311907,0.000023336464,0.000105337145,0.0000927494],"about_ca_topic_score_codex":0.003086645,"about_ca_topic_score_gemma":0.0056624087,"teacher_disagreement_score":0.046806157,"about_ca_system_score_codex":6.8928216e-7,"about_ca_system_score_gemma":0.000034386823,"threshold_uncertainty_score":0.46661043},"labels":[],"label_agreement":null},{"id":"W4387311910","doi":"10.1007/s10948-023-06622-4","title":"On Magnetic Field Screening and Trapping in Hydrogen-Rich High-Temperature Superconductors: Unpulling the Wool Over Readers’ Eyes","year":2023,"lang":"en","type":"article","venue":"Journal of Superconductivity and Novel Magnetism","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Diamagnetism; Superconductivity; Condensed matter physics; Room-temperature superconductor; Physics; High-temperature superconductivity; Magnetic field; Quantum mechanics","score_opus":0.02091687144071098,"score_gpt":0.22108777720677508,"score_spread":0.2001709057660641,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387311910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995503,0.0015131296,0.000008735993,0.0021297603,0.0006033608,0.00014562154,0.000037000093,0.000014508931,0.000044899432],"genre_scores_gemma":[0.9982399,0.0008887803,0.00020544496,0.00027195935,0.0002859693,0.0000010895118,0.000008052117,0.000008098487,0.000090705405],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99861246,0.00013022103,0.00036285276,0.00025867045,0.0003030004,0.0003327636],"domain_scores_gemma":[0.99895924,0.0006578691,0.00008525788,0.00014445938,0.000038528404,0.00011465639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008423994,0.00020916136,0.00037466464,0.00022828879,0.00021334017,0.00018404651,0.00017611266,0.00015322636,0.0004731302],"category_scores_gemma":[0.000118274125,0.00014180953,0.00005792992,0.00034506767,0.000118714466,0.0008160112,0.000029239069,0.000491934,0.0000063647176],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033650498,0.0001339076,0.025616268,0.00023830656,0.0001314604,0.00031021627,0.0071367067,0.002499961,0.9372961,0.0013597143,0.001813154,0.02312769],"study_design_scores_gemma":[0.0032961965,0.0024193358,0.9555783,0.00074982335,0.00015138197,0.00040790476,0.0057835705,0.001046805,0.019780787,0.008531631,0.0013781335,0.0008760777],"about_ca_topic_score_codex":0.0018128675,"about_ca_topic_score_gemma":0.00049977464,"teacher_disagreement_score":0.9299621,"about_ca_system_score_codex":0.0000032644257,"about_ca_system_score_gemma":0.000035020148,"threshold_uncertainty_score":0.5782825},"labels":[],"label_agreement":null},{"id":"W4387313520","doi":"10.25288/tjb.1318091","title":"A Discussion on Geodynamic Modeling Methodology: Inferences from Numerical Models in the Anatolian Plate","year":2023,"lang":"en","type":"article","venue":"Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto; Dalhousie University; Compute Canada; National Science Foundation","keywords":"Geology","score_opus":0.07249210961855303,"score_gpt":0.26934662271387827,"score_spread":0.19685451309532526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387313520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988513,0.00011589716,0.0011393082,0.00625573,0.00039101238,0.0003218847,0.00024204017,0.00010798011,0.0029131286],"genre_scores_gemma":[0.996539,0.00018430968,0.0020203064,0.0005479985,0.00012420447,0.000010908573,0.00032505035,0.0000069972675,0.00024120338],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99656516,0.0010819485,0.0006179608,0.00061530585,0.00048611086,0.00063349167],"domain_scores_gemma":[0.99770135,0.0015380875,0.00018627073,0.00041463735,0.000044721848,0.00011490768],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014702808,0.00031236382,0.00069623155,0.00014897776,0.00016787133,0.000055795485,0.00086772884,0.00028901425,0.0029792131],"category_scores_gemma":[0.000335502,0.00015123644,0.00015474737,0.00041223443,0.0002107979,0.000060396123,0.00012112358,0.00042664324,0.00086394994],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005502027,0.00006936954,0.010712036,0.000023464014,0.000045709192,0.0001476772,0.0011012256,0.97839427,0.00014056753,0.00311338,0.0013842796,0.004317819],"study_design_scores_gemma":[0.0006136314,0.00046732556,0.06644064,0.0000749733,0.000041054198,0.0000070519627,0.0006969237,0.7957056,0.00004354526,0.13251433,0.0029743793,0.0004204933],"about_ca_topic_score_codex":0.023696527,"about_ca_topic_score_gemma":0.00042282537,"teacher_disagreement_score":0.18268862,"about_ca_system_score_codex":0.000004192824,"about_ca_system_score_gemma":0.000030166248,"threshold_uncertainty_score":0.999914},"labels":[],"label_agreement":null},{"id":"W4387965088","doi":"10.1038/s41598-023-45240-x","title":"Unveiling the Enigma of Matter under Extreme Conditions: From Planetary Cores to Functional Materials","year":2023,"lang":"en","type":"editorial","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Astrobiology; Earth science; High pressure; Planetary science; Data science; Nanotechnology; Engineering physics; Physics; Computer science; Geology; Materials science","score_opus":0.02260292235655479,"score_gpt":0.2248441203389806,"score_spread":0.20224119798242582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387965088","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12435286,0.00012242283,0.00001769756,0.000118245596,0.8668318,0.00036361997,0.00780265,0.000055473178,0.00033528492],"genre_scores_gemma":[0.22431362,0.000027171662,0.00018817587,0.0001467125,0.6480646,0.00003787277,0.10361665,0.000056024997,0.02354917],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9959932,0.00016382363,0.0009583102,0.0009786652,0.0014746253,0.00043136012],"domain_scores_gemma":[0.996841,0.0010865842,0.0006700979,0.0010146035,0.00024296566,0.00014473891],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0016405275,0.00031568913,0.0005491031,0.0001857767,0.00045281975,0.0006588575,0.00040443733,0.0003047449,0.031551372],"category_scores_gemma":[0.00026799357,0.00021777143,0.00012060372,0.00032310636,0.0002917325,0.00016073904,0.000080113976,0.0001914127,0.0034176332],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031493448,0.0000101669775,0.0003871075,0.000051698087,0.00008443368,0.00008790427,0.00008121769,0.0020107257,0.010367179,0.0000050537997,0.9868554,0.000027650827],"study_design_scores_gemma":[0.000096959055,0.000031435877,0.021250319,0.0001739309,0.00011653847,0.000007909794,0.000068921574,0.000013181174,0.00503912,0.012495731,0.9603214,0.00038455654],"about_ca_topic_score_codex":0.0075241704,"about_ca_topic_score_gemma":0.0015200182,"teacher_disagreement_score":0.21876715,"about_ca_system_score_codex":0.0000072283,"about_ca_system_score_gemma":0.0003553194,"threshold_uncertainty_score":0.99908483},"labels":[],"label_agreement":null},{"id":"W4388497737","doi":"10.1186/s40645-023-00595-7","title":"Ancient slabs beneath Arctic and surroundings: Izanagi, Farallon, and in-betweens","year":2023,"lang":"en","type":"article","venue":"Progress in Earth and Planetary Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science London","keywords":"Geology; Subduction; Slab window; Seismology; Slab; Mantle (geology); Mantle wedge; Transition zone; Triple junction; Geophysics; Oceanic crust; Tectonics","score_opus":0.01244913162527609,"score_gpt":0.22308650337198405,"score_spread":0.21063737174670796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388497737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99494183,0.0039172573,6.954875e-7,0.0002252388,0.00029083935,0.00022878533,0.000095637064,0.000034387795,0.00026531407],"genre_scores_gemma":[0.99820566,0.0012164131,0.00030402435,0.00009696259,0.000047884194,0.0000022278466,0.00008353188,0.0000027543979,0.000040525007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99822605,0.000055825494,0.00022674123,0.0005443148,0.00032387688,0.00062318397],"domain_scores_gemma":[0.999401,0.00014131973,0.000056894296,0.00014624832,0.00002114813,0.00023343759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011359545,0.00016978937,0.00024495772,0.00032712737,0.00022170867,0.00026736906,0.00019174366,0.00005237236,0.0000566125],"category_scores_gemma":[0.000033168853,0.00014127743,0.000009861972,0.00069554104,0.00067711546,0.00047905796,0.00006055807,0.00012401624,0.000026527452],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024235542,0.0000044097237,0.97428286,0.000064124324,0.0000026147889,0.000077539116,0.00032355773,0.00014962004,0.00006507047,0.000080718375,0.000010875167,0.024914362],"study_design_scores_gemma":[0.00026691568,0.000103130595,0.9906419,0.000060964714,0.0000051906754,0.000024176614,0.00008359641,0.0067258202,0.00004242482,0.0005519428,0.0013051245,0.0001888371],"about_ca_topic_score_codex":0.001517674,"about_ca_topic_score_gemma":0.0027216154,"teacher_disagreement_score":0.024725525,"about_ca_system_score_codex":0.0000017819931,"about_ca_system_score_gemma":0.0000505912,"threshold_uncertainty_score":0.5761126},"labels":[],"label_agreement":null},{"id":"W4388733944","doi":"10.5194/egusphere-2023-2656","title":"Magma-poor continent-ocean transition zones of the southern North Atlantic: a wide-angle seismic synthesis of a new frontier","year":2023,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Transition zone; Tectonics; Mantle (geology); Seismology; Continental margin; Earth science; Paleontology; Geophysics","score_opus":0.01459227545053765,"score_gpt":0.18996531861651783,"score_spread":0.17537304316598018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388733944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99300873,0.00008147628,0.0013583115,0.0011122908,0.0010743857,0.00046586158,0.0024782645,0.000056832534,0.0003638652],"genre_scores_gemma":[0.99587184,0.000062350206,0.0004652959,0.000079778176,0.00018108365,0.0000020880889,0.00028698627,0.0000141748205,0.0030364168],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99838126,0.00013350064,0.0005187037,0.00035294465,0.0003630895,0.00025048992],"domain_scores_gemma":[0.9988459,0.00015885386,0.00038583108,0.00045531284,0.000076109216,0.0000780317],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023967253,0.00025556964,0.00064154086,0.00007475431,0.00006253047,0.00004856471,0.000508066,0.00015678519,0.0011516322],"category_scores_gemma":[0.000045839508,0.00016222063,0.0002891636,0.00013119171,0.00009228485,0.00005253161,0.00007800191,0.0001363139,0.00013923728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008472318,0.00029388734,0.7856999,0.0041605206,0.0021439462,0.00003743187,0.012283049,0.10747763,0.0012276248,0.00015257439,0.07325564,0.012420556],"study_design_scores_gemma":[0.0012878567,0.00020799036,0.92930293,0.0017115929,0.0020591465,0.0000072897074,0.0020426488,0.0253037,0.012037358,0.017414065,0.006958354,0.0016670931],"about_ca_topic_score_codex":0.09263339,"about_ca_topic_score_gemma":0.01397048,"teacher_disagreement_score":0.143603,"about_ca_system_score_codex":0.0000017800039,"about_ca_system_score_gemma":0.0001357698,"threshold_uncertainty_score":0.99976146},"labels":[],"label_agreement":null},{"id":"W4390014613","doi":"10.1029/2023jb026771","title":"Joint Inversion of SPREE Receiver Functions and Surface Wave Dispersion Curves for 3‐D Crustal and Upper Mantle Structure Beneath the U.S. Midcontinent Rift","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; Université du Québec à Montréal","funders":"","keywords":"Geology; Rift; Crust; Underplating; Mantle (geology); Seismology; Receiver function; Mafic; Continental crust; Petrology; Geophysics; Tectonics; Lithosphere","score_opus":0.041769417579681355,"score_gpt":0.28480460085322007,"score_spread":0.2430351832735387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390014613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99673116,0.0004815553,0.000012325066,0.0018306973,0.00023381844,0.00026051293,0.00035718453,0.000005032746,0.00008772148],"genre_scores_gemma":[0.99717134,0.0017204813,0.00013768581,0.000029833023,0.000282262,4.5920675e-7,0.000034500023,0.000005065182,0.0006183936],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984427,0.00017540247,0.0002653721,0.00017008322,0.00061587204,0.0003305848],"domain_scores_gemma":[0.99873465,0.0005034771,0.00013906641,0.00014177346,0.0003055072,0.00017552433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000873588,0.00011054565,0.00030649276,0.00009260512,0.0002915704,0.00007515923,0.00013244583,0.00005421933,0.00017754508],"category_scores_gemma":[0.00019932831,0.00006400422,0.00009974711,0.00023961629,0.0002523173,0.00023276493,0.000075872675,0.00027626668,0.000013975684],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005184566,0.0005188704,0.08684057,0.0038384178,0.0012856191,0.00019545243,0.0063354606,0.009403548,0.6289908,0.0021713064,0.16680393,0.08843142],"study_design_scores_gemma":[0.0011613112,0.001812283,0.94695836,0.0004760206,0.00009734688,0.000023785495,0.000965418,0.01761124,0.012598375,0.0060088,0.012057793,0.00022928056],"about_ca_topic_score_codex":0.00065956777,"about_ca_topic_score_gemma":0.00016143391,"teacher_disagreement_score":0.8601178,"about_ca_system_score_codex":0.000002324961,"about_ca_system_score_gemma":0.00006773198,"threshold_uncertainty_score":0.26100165},"labels":[],"label_agreement":null},{"id":"W4390064069","doi":"10.1063/5.0170100","title":"Effects of elevated-temperature deposition on the atomic structure of amorphous Ta2O5 films","year":2023,"lang":"en","type":"article","venue":"APL Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Science and ICT, South Korea; Gordon and Betty Moore Foundation; National Research Foundation of Korea; Fonds de recherche du Québec – Nature et technologies; National Research Foundation; Office of Naval Research; Polytechnique Montréal; National Science Foundation","keywords":"Amorphous solid; Materials science; Annealing (glass); Deposition (geology); Glass transition; Thin film; Atmospheric temperature range; Scattering; Atomic layer deposition; Composite material; Analytical Chemistry (journal); Condensed matter physics; Nanotechnology; Optics; Polymer; Crystallography; Thermodynamics; Chemistry","score_opus":0.004027229670211822,"score_gpt":0.17934858972262518,"score_spread":0.17532136005241336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390064069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99733174,0.00003466187,4.4246707e-7,0.00006350063,0.0011076997,0.0003269136,0.0010419885,0.000043319553,0.00004975606],"genre_scores_gemma":[0.9993036,0.00003693982,0.000030963856,0.00009422838,0.00013249344,0.0000024947396,0.00034333993,0.0000070630385,0.00004891003],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9989878,0.00017702272,0.0002619186,0.0001669491,0.00020837836,0.00019792828],"domain_scores_gemma":[0.99930316,0.00023705431,0.00017349147,0.00022110547,0.000036721794,0.000028465542],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018096673,0.00013867606,0.00029936736,0.000052973915,0.00007624447,0.00005079016,0.00020787043,0.00010161563,0.0013853832],"category_scores_gemma":[0.00004268373,0.00008313849,0.000042364016,0.0001918553,0.000054292468,0.000060421473,0.00001766416,0.000045623397,0.00015596602],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000082856524,0.000006796232,0.00021190848,0.00018031198,0.00003387368,0.000008570809,0.000098563236,0.00010467817,0.9965045,0.0005479301,0.0021650458,0.000055001332],"study_design_scores_gemma":[0.00016270358,0.00010654479,0.06524785,0.000066570225,0.000028210537,0.0000020973555,0.000013525874,0.000011293329,0.9326336,0.0015648563,0.00007629796,0.000086494365],"about_ca_topic_score_codex":0.00085090083,"about_ca_topic_score_gemma":0.000036316622,"teacher_disagreement_score":0.06503594,"about_ca_system_score_codex":0.0000010874107,"about_ca_system_score_gemma":0.000018491317,"threshold_uncertainty_score":0.9995275},"labels":[],"label_agreement":null},{"id":"W4390493313","doi":"10.5194/egusphere-2023-2656-rc2","title":"Comment on egusphere-2023-2656","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Mantle (geology); Crust; Earth science; Magmatism; Tectonics; Seismology; Transition zone; Paleontology; Petrology; Geophysics","score_opus":0.024690700807275135,"score_gpt":0.26087610124043004,"score_spread":0.2361854004331549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390493313","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000027404161,0.049029447,0.0000045208085,0.27684894,0.025327394,0.0007023845,0.0071132025,0.0001674232,0.6407793],"genre_scores_gemma":[0.00029103077,0.006360387,0.0001324075,0.06323122,0.0018338955,0.000009131524,0.007711414,0.000016392569,0.9204141],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981833,0.00008669149,0.00035395246,0.0005007087,0.0005205792,0.0003547285],"domain_scores_gemma":[0.99911237,0.0001220205,0.00009711281,0.00047680482,0.000046282752,0.00014541004],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003658338,0.00036113145,0.0006317937,0.000047148424,0.00007403087,0.00018118147,0.0004161729,0.0001747028,0.13537315],"category_scores_gemma":[0.000018432333,0.00023960213,0.00018465439,0.00014264647,0.000031467247,0.000038804883,0.000039175757,0.00029590647,0.035209917],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045887086,0.000010720683,0.0000028741233,0.0016889122,0.00006684838,0.000029611147,0.000005370892,0.000016637468,6.608485e-7,0.0003835805,0.98799014,0.009800048],"study_design_scores_gemma":[0.000051215484,0.00011786863,0.000054359552,0.0017318835,0.00014905585,0.0000021874657,0.0000024562662,0.000023962928,0.000016090462,0.000985924,0.9965485,0.00031654772],"about_ca_topic_score_codex":0.011027117,"about_ca_topic_score_gemma":0.0030818293,"teacher_disagreement_score":0.27963483,"about_ca_system_score_codex":0.0000046900814,"about_ca_system_score_gemma":0.000090888716,"threshold_uncertainty_score":0.99555856},"labels":[],"label_agreement":null},{"id":"W4391163342","doi":"10.1021/acs.cgd.3c01171","title":"Polymorphism and Phase Stability of Hydrated Magnesium Carbonate Nesquehonite MgCO<sub>3</sub>·3H<sub>2</sub>O: Negative Axial Compressibility and Thermal Expansion in a Cementitious Material","year":2024,"lang":"en","type":"article","venue":"Crystal Growth & Design","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Conselleria d'Educació, Investigació, Cultura i Esport; Agencia Estatal de Investigación; European Regional Development Fund; Generalitat Valenciana; Fundación para el Fomento en Asturias de la Investigación Científica Aplicada y la Tecnología; Ministerio de Ciencia e Innovación; European Commission; Compute Canada","keywords":"Thermodynamics; Thermal expansion; Magnesite; Materials science; Compressibility; Diamond anvil cell; Phase (matter); Thermal stability; Negative thermal expansion; Ambient pressure; Phase transition; Phase diagram; Polymorphism (computer science); Carbonate; Magnesium; Mineralogy; Crystallography; Chemistry; High pressure; Composite material; Metallurgy; Organic chemistry","score_opus":0.01365808403317375,"score_gpt":0.20961766519709615,"score_spread":0.1959595811639224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391163342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99626535,0.00054330286,0.00026003123,0.000035378496,0.000755592,0.00082150055,0.0011263548,0.0000809785,0.00011149934],"genre_scores_gemma":[0.99943334,0.00006272577,0.00010128056,0.000024992947,0.00016248251,0.00001571492,0.00017984286,0.000017178623,0.00000246728],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9973054,0.00061927666,0.00058356137,0.0006929108,0.00032861228,0.00047021997],"domain_scores_gemma":[0.9990627,0.00025815913,0.00014315275,0.00024148096,0.00010480123,0.00018969663],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00077286735,0.00035976127,0.00052079506,0.0001551749,0.00014229401,0.00025850398,0.00015401168,0.00015878446,0.00017067353],"category_scores_gemma":[0.000047327077,0.00031121823,0.000060846967,0.0003016052,0.0004112297,0.0005569242,0.0000705816,0.0001685019,0.000009330942],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011441647,0.000105369036,0.0012128501,0.00040928114,0.000030822262,0.00008758695,0.0009634746,0.000092433154,0.99349004,0.000040858286,0.000021205424,0.0024019375],"study_design_scores_gemma":[0.0016274045,0.0006113145,0.03974139,0.00009999965,0.000088529894,0.000011069437,0.00007987147,0.007913372,0.9458015,0.0036176976,0.000009648867,0.00039821013],"about_ca_topic_score_codex":0.0023757976,"about_ca_topic_score_gemma":0.00025822982,"teacher_disagreement_score":0.04768852,"about_ca_system_score_codex":0.000013854979,"about_ca_system_score_gemma":0.00013889637,"threshold_uncertainty_score":0.999934},"labels":[],"label_agreement":null},{"id":"W4391683917","doi":"10.1103/physrevlett.132.066003","title":"Resonant Ultrasound Spectroscopy for Irregularly Shaped Samples and Its Application to Uranium Ditelluride","year":2024,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Institute for Advanced Research","funders":"Maryland Quantum Materials Center; Basic Energy Sciences; Materials Research Science and Engineering Center, Harvard University; National Institute of Standards and Technology; University of Maryland; Gordon and Betty Moore Foundation; U.S. Department of Energy; National Institutes of Health; National Science Foundation","keywords":"Resonant ultrasound spectroscopy; Tensor (intrinsic definition); Spectroscopy; Elastic modulus; Materials science; Elasticity (physics); Superconductivity; Uranium; Physics; Condensed matter physics; Computational physics; Geometry; Nuclear physics; Mathematics; Composite material; Quantum mechanics","score_opus":0.016544328645854783,"score_gpt":0.266690023560216,"score_spread":0.2501456949143612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391683917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91024584,0.04902396,0.014922522,0.020771272,0.00067999016,0.0029685758,0.0010716567,0.00018066274,0.00013549793],"genre_scores_gemma":[0.9894333,0.0031151995,0.0007574702,0.005297942,0.0011170348,0.00006259364,0.00017546075,0.000011649063,0.000029379504],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99898994,0.00004012385,0.00017217688,0.00037697723,0.00016790844,0.00025285417],"domain_scores_gemma":[0.9993181,0.00035497622,0.00003375619,0.00015266438,0.000018125877,0.00012232941],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002004457,0.00015269326,0.00029271885,0.000024881221,0.00007696042,0.00013229718,0.00014185344,0.0000095702835,0.000101271595],"category_scores_gemma":[0.00004185362,0.0001126781,0.0000868391,0.00015281168,0.000024856312,0.00015220049,0.000010610426,0.000057009514,0.00040043765],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029441468,0.000018392559,0.00008246088,0.0025696883,0.000044471934,0.0000038035203,0.00014201787,0.000064507534,0.967894,0.003308908,0.012866663,0.012975599],"study_design_scores_gemma":[0.00023916762,0.00027590213,0.021728102,0.0018857195,0.00038368022,0.000011025091,0.0000071374825,0.014019524,0.01818504,0.00383185,0.9385971,0.00083574496],"about_ca_topic_score_codex":0.00009660026,"about_ca_topic_score_gemma":0.000021207052,"teacher_disagreement_score":0.949709,"about_ca_system_score_codex":0.0000033534475,"about_ca_system_score_gemma":0.000012573826,"threshold_uncertainty_score":0.5146949},"labels":[],"label_agreement":null},{"id":"W4392230579","doi":"10.22541/essoar.170914536.69257488/v1","title":"Inherited Crustal Features and Southern Alaska Tectonic History Constrained by Sp Receiver Functions","year":2024,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Geology; Terrane; Subduction; Seismology; Fault (geology); Tectonics; Induced seismicity","score_opus":0.010257127975212346,"score_gpt":0.19065370643744292,"score_spread":0.18039657846223056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392230579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87410486,0.016803168,0.000034748315,0.00068921084,0.0068078972,0.00062776176,0.008326815,0.0004586066,0.092146955],"genre_scores_gemma":[0.9301075,0.00019719894,0.00022129087,0.00021235098,0.00038039562,0.000007225212,0.0015738488,0.000017048938,0.06728315],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986362,0.000075329604,0.00023310778,0.00057408924,0.00020085617,0.00028045624],"domain_scores_gemma":[0.9993948,0.00006226089,0.00008912951,0.00026589027,0.00004181474,0.00014612124],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001597362,0.00030951004,0.00034646242,0.000090938855,0.000087982975,0.00018194546,0.00017207378,0.00031393033,0.015770106],"category_scores_gemma":[0.000014985691,0.00024495163,0.00009463822,0.00005842908,0.00021878532,0.000045518358,0.00012703182,0.0004915107,0.00074464065],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015054828,0.00005935211,0.0024849244,0.0008210118,0.0007294232,0.00008896883,0.0025633685,0.00072735385,0.0070024584,0.00028587092,0.966735,0.018351737],"study_design_scores_gemma":[0.0010165855,0.00031753155,0.027787445,0.0004061108,0.00080206024,0.000103860446,0.0013905116,0.0015667207,0.0004641869,0.01042074,0.9532616,0.002462633],"about_ca_topic_score_codex":0.01106358,"about_ca_topic_score_gemma":0.0022426601,"teacher_disagreement_score":0.056002654,"about_ca_system_score_codex":0.000013581061,"about_ca_system_score_gemma":0.00021095603,"threshold_uncertainty_score":0.9988838},"labels":[],"label_agreement":null},{"id":"W4392360705","doi":"10.1038/s41598-024-55846-4","title":"Nanoscale imaging of Fe-rich inclusions in single-crystal zircon using X-ray ptycho-tomography","year":2024,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada); University of Saskatchewan","funders":"Natural Environment Research Council; Sight Research UK; Diamond Light Source; NERC Environmental Bioinformatics Centre; National Science Foundation","keywords":"Zircon; Apatite; Magnetite; Geology; Remanence; Mineralogy; Materials science; Geochemistry; Magnetization; Magnetic field; Paleontology","score_opus":0.013068185006930534,"score_gpt":0.22571403994263492,"score_spread":0.2126458549357044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392360705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841714,0.0010389527,0.00017276319,0.00004668367,0.012078779,0.00018371952,0.0000445978,0.0000547344,0.002208385],"genre_scores_gemma":[0.9985552,0.0000032533853,0.0009225199,0.000008771772,0.00009803908,9.3915975e-7,0.000092064605,0.0000063922143,0.00031281545],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9979566,0.00006727847,0.000546687,0.00060875504,0.00046842397,0.0003523096],"domain_scores_gemma":[0.99921596,0.000058656202,0.00015317931,0.00040739836,0.000067066845,0.00009774506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012650642,0.00014112607,0.0002300859,0.000449555,0.0002359285,0.0004200911,0.00014918506,0.000046325113,0.00057076104],"category_scores_gemma":[0.000038924132,0.00011848196,0.00009582501,0.0011877714,0.00022904947,0.00040124997,0.000058428606,0.00008919384,0.000019382578],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000059120807,0.00005256425,0.08158796,0.00010941926,0.000014939729,0.000690399,0.00084744324,0.0021360037,0.9114091,0.000030139705,0.0011064005,0.0020097091],"study_design_scores_gemma":[0.00077382615,0.000246136,0.20347999,0.0028304055,0.0003273781,0.0010888386,0.0016120811,0.0514335,0.47527146,0.07557659,0.18471193,0.0026478756],"about_ca_topic_score_codex":0.0012715168,"about_ca_topic_score_gemma":0.0005575368,"teacher_disagreement_score":0.43613765,"about_ca_system_score_codex":0.0000054942875,"about_ca_system_score_gemma":0.0001311705,"threshold_uncertainty_score":0.6249433},"labels":[],"label_agreement":null},{"id":"W4392578126","doi":"10.5194/egusphere-egu24-11249","title":"The Adiabatic Heat Flux through the Top of the Core of Ancient Vesta from High-P,T Resistivity Experiments","year":2024,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Adiabatic process; Electrical resistivity and conductivity; Flux (metallurgy); Core (optical fiber); Heat flux; High heat; Astrophysics; Astrobiology; Materials science; Physics; Geology; Geophysics; Thermodynamics; Heat transfer; Optics; Composite material; Metallurgy","score_opus":0.026166461623700576,"score_gpt":0.24966529197178036,"score_spread":0.2234988303480798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392578126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9830297,0.0042203655,0.000012644391,0.00073666876,0.004534123,0.0005915035,0.0022633164,0.000020379042,0.004591282],"genre_scores_gemma":[0.9979713,0.000077670855,0.00015497005,0.0001507829,0.00021980025,0.000009025665,0.00014450934,0.000006655234,0.0012652955],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9981796,0.00021686417,0.00043394015,0.00037843763,0.00053563167,0.00025548204],"domain_scores_gemma":[0.9979619,0.00054186105,0.00020050394,0.0011903156,0.000063399006,0.000042036503],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004235855,0.00023560377,0.00039180377,0.000014060682,0.00023478759,0.00012922271,0.0010577157,0.000120909564,0.0013135719],"category_scores_gemma":[0.00005833726,0.00009337517,0.00016925044,0.00012592704,0.00035684902,0.000038358452,0.000542587,0.00026534608,0.00006616637],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016592828,0.0010576666,0.089378685,0.0045597865,0.0070798337,0.00005595281,0.046198178,0.068380415,0.14607377,0.12758514,0.48251924,0.025452055],"study_design_scores_gemma":[0.0003243114,0.00012617804,0.751182,0.00059093337,0.0004169527,7.0455786e-7,0.0006811057,0.0013253497,0.07067678,0.14797005,0.026192268,0.00051331683],"about_ca_topic_score_codex":0.048424076,"about_ca_topic_score_gemma":0.0022590915,"teacher_disagreement_score":0.66180336,"about_ca_system_score_codex":0.000005340358,"about_ca_system_score_gemma":0.00017959779,"threshold_uncertainty_score":0.99959934},"labels":[],"label_agreement":null},{"id":"W4392596333","doi":"10.5194/egusphere-egu24-330","title":"The Role of Upper Mantle Forces in Post-subduction Tectonics: Insights from 3D Thermo-mechanical Models in the East Anatolian Plateau","year":2024,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Subduction; Geology; Mantle (geology); Tectonics; Seismology; Plateau (mathematics); Geophysics","score_opus":0.008962343495111397,"score_gpt":0.19975843244943103,"score_spread":0.19079608895431963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392596333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98068714,0.0030549963,0.000011391633,0.00040137852,0.0009287321,0.00047414936,0.00040409272,0.000023394425,0.0140147],"genre_scores_gemma":[0.99897724,0.00031289665,0.00011743019,0.000055053464,0.00016580994,0.000012339242,0.00028345198,0.000008045516,0.00006772292],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99831885,0.00021638184,0.0004404512,0.00042717974,0.00033148652,0.00026564425],"domain_scores_gemma":[0.999167,0.00016490021,0.000121365825,0.00047267688,0.00003525349,0.000038781243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037119963,0.00023695007,0.0003366359,0.000102037666,0.00008568629,0.0002108987,0.00069131306,0.0002500971,0.00057262235],"category_scores_gemma":[0.000010449375,0.00011769247,0.00010224718,0.00014410653,0.000065993925,0.0001099771,0.00017020965,0.000491823,0.000081606304],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002146509,0.0005116129,0.007517603,0.0008898786,0.0014920445,0.00037832576,0.07382481,0.32299376,0.032836683,0.34626395,0.00090006826,0.21024477],"study_design_scores_gemma":[0.00017510448,0.0000635775,0.009088803,0.00015936226,0.000050635528,0.0000048052557,0.0028827703,0.1605276,0.0019450664,0.8232442,0.0015444166,0.00031363856],"about_ca_topic_score_codex":0.058495197,"about_ca_topic_score_gemma":0.04348398,"teacher_disagreement_score":0.4769803,"about_ca_system_score_codex":0.000005763649,"about_ca_system_score_gemma":0.00010434099,"threshold_uncertainty_score":0.97396994},"labels":[],"label_agreement":null},{"id":"W4392976422","doi":"10.4006/0836-1398-37.1.80","title":"Maxwell’s equations in the Newtonian gravitational field derived from the elastic energy","year":2024,"lang":"en","type":"article","venue":"Physics Essays","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Gravitational field; Newtonian fluid; Classical mechanics; Gravitational energy; Gravitation; Field equation; Mathematical physics; Mechanics","score_opus":0.016409968537402814,"score_gpt":0.22243862799680292,"score_spread":0.2060286594594001,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392976422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49190074,0.0072134254,0.2596593,0.0546229,0.015091238,0.0013641665,0.0050223754,0.00041567162,0.1647102],"genre_scores_gemma":[0.99758637,0.000028035798,0.00010383447,0.0007926328,0.0008213727,0.0000073451024,0.0005846132,0.0000034086067,0.00007238544],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99925077,0.00010803465,0.00012281677,0.00016064753,0.0002027494,0.00015500806],"domain_scores_gemma":[0.99799794,0.0017709483,0.000025002051,0.00016712701,0.0000152292705,0.00002377716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013721104,0.00009184993,0.00008407125,0.000013567614,0.00014485978,0.00023083392,0.00026907978,0.000028007697,0.0004373788],"category_scores_gemma":[0.000025966337,0.000051700612,0.000045677647,0.00018747139,0.00003571994,0.00013310772,0.000011423262,0.0000955499,0.0001566338],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002433311,0.00005568997,0.002956894,0.000026053933,0.00009686245,0.00003346151,0.0054209353,0.017105717,0.0029260232,0.9191037,0.0137990825,0.038451273],"study_design_scores_gemma":[0.000098717486,0.000032543114,0.013735096,0.000035546476,0.000040050483,7.4313834e-7,0.00016265546,0.028931456,0.00033349788,0.94382846,0.012654914,0.00014633339],"about_ca_topic_score_codex":0.0066572013,"about_ca_topic_score_gemma":0.0026292668,"teacher_disagreement_score":0.5056856,"about_ca_system_score_codex":0.00000164702,"about_ca_system_score_gemma":0.000050092887,"threshold_uncertainty_score":0.99995756},"labels":[],"label_agreement":null},{"id":"W4393032697","doi":"10.1103/physrevb.109.094113","title":"Thermal equation of state of rhodium to 191 GPa and 2700 K using double-sided flash laser heating in a diamond anvil cell","year":2024,"lang":"fi","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Deutsches Elektronen-Synchrotron; Engineering and Physical Sciences Research Council; European Synchrotron Radiation Facility; Environmental Studies Research Funds; Helmholtz-Gemeinschaft","keywords":"Flash (photography); Laser; Rhodium; Materials science; Diamond anvil cell; Equation of state; Diamond; Thermal; Atomic physics; Optics; Physics; Thermodynamics; Diffraction; Chemistry; Composite material","score_opus":0.03196165044445204,"score_gpt":0.3310536136534334,"score_spread":0.29909196320898135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393032697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91724485,0.07834331,0.00026608433,0.0005587843,0.0003407582,0.001902935,0.0005700223,0.00002595272,0.00074729306],"genre_scores_gemma":[0.94170403,0.05675539,0.00027593723,0.00046565724,0.00051639107,0.000033866487,0.00013103895,0.00003966878,0.00007803211],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99518186,0.00068877137,0.001517981,0.00096173794,0.0008826907,0.0007669855],"domain_scores_gemma":[0.99719423,0.0010387456,0.00056283467,0.00060853775,0.00018151898,0.00041415272],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0013068342,0.0006608866,0.0025247193,0.00012680772,0.00008877717,0.00011754942,0.0004338511,0.00006589995,0.00018733823],"category_scores_gemma":[0.0002590112,0.00052213145,0.0005090073,0.0013745268,0.00020822117,0.00062998093,0.00020010339,0.00044739246,0.00030793322],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005406226,0.0020616646,0.002029326,0.19860086,0.0004473642,0.00011771249,0.003948331,0.01161976,0.47684887,0.014797027,0.0016591564,0.2873293],"study_design_scores_gemma":[0.0029579962,0.003044161,0.013186731,0.23657548,0.004588959,0.000010365687,0.000060752394,0.42042094,0.24161948,0.041687343,0.03169135,0.0041564154],"about_ca_topic_score_codex":0.0013877855,"about_ca_topic_score_gemma":0.000085751,"teacher_disagreement_score":0.4088012,"about_ca_system_score_codex":0.000025220683,"about_ca_system_score_gemma":0.0002181236,"threshold_uncertainty_score":0.999723},"labels":[],"label_agreement":null},{"id":"W4394718096","doi":"10.7185/geochemlet.2412","title":"Comparative 142Nd and 182W study of MORBs and the 4.5 Gyr evolution of the upper mantle","year":2024,"lang":"en","type":"article","venue":"Geochemical Perspectives Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Ottawa; Carnegie Institution of Washington","keywords":"Mantle (geology); Geology; Astrobiology; Physics; Geochemistry","score_opus":0.006676448484182955,"score_gpt":0.2123825562901017,"score_spread":0.20570610780591875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394718096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960206,0.0017655316,0.000010280783,0.0012849199,0.00012091118,0.0002531774,0.000051723677,0.000008016803,0.00048480715],"genre_scores_gemma":[0.99983096,0.00001731531,0.000024717754,0.000034635796,0.00006616008,0.0000018259232,0.000002199924,0.0000016303449,0.000020556015],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99933857,0.00009878088,0.00012359885,0.00018803042,0.00014822093,0.0001028003],"domain_scores_gemma":[0.9996188,0.00016766004,0.00004270391,0.0001259752,0.000022317307,0.000022518687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001443004,0.000084350955,0.00018944255,0.000022583698,0.000069022164,0.000035050653,0.000107860156,0.000021487253,0.00007574883],"category_scores_gemma":[0.000015854757,0.000043153337,0.000036910635,0.0001048628,0.00051126775,0.00007317077,0.000036086632,0.00008833536,0.0000031634759],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00077175593,0.00032134284,0.16097498,0.00036840286,0.0010466505,0.000010039959,0.19566028,0.0011896611,0.61574054,0.015456666,0.007822686,0.00063698384],"study_design_scores_gemma":[0.0014951838,0.00019378653,0.94087654,0.00008757497,0.00024669946,0.000013233871,0.035562396,0.0036992938,0.011513252,0.005605121,0.00047633954,0.00023055835],"about_ca_topic_score_codex":0.0019743145,"about_ca_topic_score_gemma":0.000086383545,"teacher_disagreement_score":0.77990156,"about_ca_system_score_codex":0.0000037173836,"about_ca_system_score_gemma":0.000010133194,"threshold_uncertainty_score":0.2984586},"labels":[],"label_agreement":null},{"id":"W4395082450","doi":"10.1103/physrevb.109.165146","title":"Strontium ferrite under pressure: Potential analog to strontium ruthenate","year":2024,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke; Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Flatiron Health; Alliance de recherche numérique du Canada; Canada First Research Excellence Fund; Canada Foundation for Innovation; Simons Foundation","keywords":"Strontium; Isostructural; Ferrite (magnet); Materials science; Condensed matter physics; Metal; Electronic structure; Density functional theory; Physics; Chemistry; Crystal structure; Crystallography; Metallurgy; Quantum mechanics; Composite material; Nuclear physics","score_opus":0.011824505261429254,"score_gpt":0.3195739370883937,"score_spread":0.30774943182696446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395082450","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.25842023,0.63991696,0.035525117,0.026444707,0.0076291207,0.009288247,0.0044797934,0.001432216,0.016863622],"genre_scores_gemma":[0.95680207,0.03494823,0.00016463574,0.0039180466,0.002907113,0.00007111642,0.0004184496,0.000051877665,0.00071848964],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9949604,0.00049012963,0.0008441396,0.0013438539,0.0012056412,0.0011557918],"domain_scores_gemma":[0.99753207,0.00026985875,0.00020810786,0.0010380205,0.00017374424,0.000778227],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00067571684,0.0007998848,0.001916763,0.0000886307,0.00020966852,0.00034853746,0.0009935058,0.00007309913,0.0013380192],"category_scores_gemma":[0.00015619588,0.00058218854,0.0010089575,0.00096121203,0.00014680027,0.0006158646,0.00017398832,0.0005935262,0.006883627],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002498099,0.0016981657,0.0003943552,0.05808572,0.002520122,0.00039927365,0.00042747275,0.010039451,0.025301231,0.3955138,0.32010737,0.18526323],"study_design_scores_gemma":[0.00041928067,0.000785222,0.010929587,0.01594558,0.0036394359,0.000022961049,0.00001257312,0.053089317,0.0010836875,0.0840971,0.8277875,0.0021877517],"about_ca_topic_score_codex":0.00044646586,"about_ca_topic_score_gemma":0.000058495778,"teacher_disagreement_score":0.6983818,"about_ca_system_score_codex":0.000017602943,"about_ca_system_score_gemma":0.00014730026,"threshold_uncertainty_score":0.99966294},"labels":[],"label_agreement":null},{"id":"W4395450538","doi":"10.1038/s41467-024-47887-0","title":"Seismic evidence for melt-rich lithosphere-asthenosphere boundary beneath young slab at Cascadia","year":2024,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Institute of Geology and Geophysics, Chinese Academy of Sciences; National Natural Science Foundation of China; Chinese Academy of Sciences; National Science Foundation","keywords":"Subduction; Asthenosphere; Geology; Lithosphere; Slab; Mantle (geology); Seismology; Slab window; Geophysics; Oceanic crust; Tectonics","score_opus":0.0296987365516227,"score_gpt":0.2962280993311075,"score_spread":0.2665293627794848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395450538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.57403255,0.39434814,0.00051602186,0.008295872,0.004363079,0.0013867212,0.002448864,0.00052369403,0.014085078],"genre_scores_gemma":[0.98653114,0.0025713686,0.0061898935,0.0002888539,0.00024730797,0.00002856153,0.00063091953,0.00001514012,0.0034968099],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99876404,0.00012322329,0.00025223914,0.0003344683,0.00021253027,0.00031349756],"domain_scores_gemma":[0.9974827,0.0009163351,0.00006714539,0.0013095252,0.000115255,0.00010903939],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039906838,0.00018904924,0.00021116258,0.000033575874,0.0007306507,0.00036382786,0.0011860323,0.00024844278,0.00082269945],"category_scores_gemma":[0.00009210901,0.00015722589,0.000109596374,0.00032289626,0.00012534225,0.00037391018,0.0001381144,0.0004447599,0.00043670615],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048058844,0.00028170118,0.113166794,0.0014761597,0.0013008233,0.0000596173,0.011049787,0.004558599,0.007264047,0.057343993,0.62333256,0.17968531],"study_design_scores_gemma":[0.00013470631,0.00007643551,0.044307634,0.00019195865,0.00012945116,0.000025722735,0.00007382102,0.015456578,0.00036908954,0.0026170115,0.9362973,0.00032029249],"about_ca_topic_score_codex":0.0014335647,"about_ca_topic_score_gemma":0.015783159,"teacher_disagreement_score":0.41249862,"about_ca_system_score_codex":0.000022819679,"about_ca_system_score_gemma":0.00017472345,"threshold_uncertainty_score":0.90079826},"labels":[],"label_agreement":null},{"id":"W4396801265","doi":"10.1107/s2053273323095438","title":"Structure and magnetism of doped SrCu<sub>2</sub>(BO<sub>3</sub>)<sub>2</sub>","year":2023,"lang":"en","type":"article","venue":"Acta Crystallographica Section A Foundations and Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada)","funders":"","keywords":"Magnetism; Doping; Materials science; Condensed matter physics; Physics","score_opus":0.006894372524614231,"score_gpt":0.20848438664450858,"score_spread":0.20159001411989436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396801265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99633646,0.0007061804,0.00014008423,0.0003456736,0.0010635977,0.00043399516,0.0006242882,0.0001674375,0.00018227195],"genre_scores_gemma":[0.98861486,0.0100898435,0.00014658291,0.000070691414,0.00029924858,0.00001606388,0.0007318766,0.000019053105,0.000011777954],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9978127,0.00014831222,0.0005236821,0.0006619825,0.00036612988,0.00048720633],"domain_scores_gemma":[0.99874264,0.00023360756,0.0003400849,0.00031237173,0.00015164302,0.00021967631],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00029431516,0.0003659009,0.00045402054,0.00050196704,0.0007517401,0.000316328,0.000188058,0.00019863233,0.000096449716],"category_scores_gemma":[0.00006076727,0.00032873813,0.00011716725,0.0012903713,0.00043451434,0.0010902005,0.000060657036,0.00023497574,0.0000063839916],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005924492,0.000031197953,0.005633763,0.00013339218,0.00007924999,0.0000066072453,0.000185447,0.0003637932,0.96063924,0.00018990938,0.00022459576,0.032453585],"study_design_scores_gemma":[0.002260856,0.0011555301,0.68937546,0.00022177679,0.0003771497,0.00012331957,0.0007579084,0.0014202446,0.18979512,0.03189632,0.080951355,0.0016649646],"about_ca_topic_score_codex":0.00019236708,"about_ca_topic_score_gemma":0.0033597162,"teacher_disagreement_score":0.7708441,"about_ca_system_score_codex":0.000004697925,"about_ca_system_score_gemma":0.000061236926,"threshold_uncertainty_score":0.9999165},"labels":[],"label_agreement":null},{"id":"W4396852054","doi":"10.31223/x52d86","title":"Direct observations of transient weakening during phase transformations in quartz and olivine","year":2024,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"","keywords":"Geology; Geophysics; Slab; Subduction; Olivine; Mantle convection; Ringwoodite; Coesite; Phase (matter); Mantle (geology); Synchrotron radiation; Transition zone; Convection; Stishovite; Petrology; Geochemistry; Mechanics; Quartz; Seismology; Tectonics; Paleontology; Physics","score_opus":0.021557910702112836,"score_gpt":0.23991912696814396,"score_spread":0.21836121626603114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396852054","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99093,0.00067415135,0.00006744933,0.0002484167,0.00039439125,0.0002902018,0.0010875373,0.000042862797,0.006264939],"genre_scores_gemma":[0.99874794,0.0002546348,0.00047168025,0.000008775004,0.000067257184,0.000006432139,0.0002708271,0.000004075326,0.00016838055],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9990255,0.00004110809,0.00040572634,0.000226717,0.00013736861,0.00016355986],"domain_scores_gemma":[0.9996663,0.000057141653,0.00005785457,0.00013883183,0.00002280883,0.000057087975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002007188,0.00014815138,0.0003069611,0.0001514691,0.000050257353,0.00007336434,0.000100272,0.0000850099,0.0004943724],"category_scores_gemma":[0.0000066909824,0.00012403927,0.000060530878,0.00013902695,0.000032958476,0.00009803642,0.000022292987,0.00016282343,0.000011691088],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008836198,0.0015940007,0.06360282,0.03850721,0.0017235938,0.00024028069,0.1179707,0.4491298,0.24057601,0.012218599,0.0020765103,0.071476854],"study_design_scores_gemma":[0.002752997,0.00031487914,0.8902653,0.0023312708,0.00043606505,0.000013101757,0.0007627255,0.061988134,0.02565355,0.00945237,0.0046733506,0.001356252],"about_ca_topic_score_codex":0.0043517533,"about_ca_topic_score_gemma":0.0056820447,"teacher_disagreement_score":0.8266625,"about_ca_system_score_codex":0.0000021248427,"about_ca_system_score_gemma":0.00005223967,"threshold_uncertainty_score":0.65785784},"labels":[],"label_agreement":null},{"id":"W4398206906","doi":"10.5539/ijc.v16n2p34","title":"The Paradox of Thermodynamic Instability","year":2024,"lang":"en","type":"article","venue":"International Journal of Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Chemistry; Instability; Thermodynamics; Mechanics","score_opus":0.005385554250555684,"score_gpt":0.2252962271431247,"score_spread":0.21991067289256902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398206906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923985,0.000831845,0.000031024796,0.0004463334,0.0013001747,0.000012400683,0.000081674225,0.0000037421244,0.0048942952],"genre_scores_gemma":[0.999431,0.00012708601,0.000024249719,0.000012037138,0.00028604642,8.224697e-8,0.000008068432,0.0000012185013,0.00011022556],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993681,0.00001318716,0.00023820945,0.00004819495,0.00027607038,0.000056271765],"domain_scores_gemma":[0.999514,0.00017067118,0.00011007036,0.00006062373,0.00011899035,0.000025680712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028424535,0.00004212012,0.000078716635,0.0000129905575,0.000018582146,0.00007294341,0.00033310655,0.000021902712,0.00074619584],"category_scores_gemma":[0.00004317329,0.000024202734,0.000071965405,0.000034666733,0.00005657298,0.00008611579,0.000008968603,0.000075729506,0.0000077012355],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057424547,0.000100492434,0.017276777,0.0002097122,0.0018005949,0.00026245738,0.00082153187,0.0037770323,0.741187,0.0021652193,0.002858975,0.22896601],"study_design_scores_gemma":[0.0009823199,0.00017788821,0.3220898,0.0007523167,0.000243794,0.00055878714,0.000425867,0.028826,0.34443435,0.06606606,0.23492007,0.0005227545],"about_ca_topic_score_codex":0.0000454919,"about_ca_topic_score_gemma":0.000009637541,"teacher_disagreement_score":0.3967526,"about_ca_system_score_codex":0.0000041949443,"about_ca_system_score_gemma":0.00007428754,"threshold_uncertainty_score":0.81703216},"labels":[],"label_agreement":null},{"id":"W4398208950","doi":"10.1029/2023jb027012","title":"High‐Resolution Mantle Transition Zone Imaging Using Multi‐Dimensional Reconstruction of SS Precursors","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada; Natural Resources Canada","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Transition zone; Geology; Mantle (geology); High resolution; Seismology; Remote sensing; Geophysics","score_opus":0.03505399528567535,"score_gpt":0.31276024940219277,"score_spread":0.2777062541165174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398208950","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955499,0.0005018684,0.0019266587,0.00021432606,0.001484628,0.00013404693,0.000110572364,0.000013429849,0.00006455925],"genre_scores_gemma":[0.9951713,0.00008419295,0.003684861,0.000009468758,0.00091233006,3.9168378e-7,0.000019759154,0.000007831282,0.000109836634],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99758726,0.00034319118,0.000498291,0.00021320092,0.00095264014,0.00040539005],"domain_scores_gemma":[0.998816,0.00028512583,0.00015316842,0.00012402296,0.00044035152,0.00018132124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013144325,0.00013044958,0.00035318604,0.00032608683,0.0001692155,0.00012983529,0.00016394704,0.00006252628,0.00047768024],"category_scores_gemma":[0.00007238411,0.00010224096,0.00017032133,0.000417679,0.00023587754,0.0006903252,0.000019304183,0.00045455352,0.00008001333],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019142461,0.00053345656,0.0015072682,0.0009126401,0.0005363626,0.00059650757,0.0018802899,0.13674197,0.70771706,0.0017036976,0.001174576,0.14478192],"study_design_scores_gemma":[0.001296534,0.0011340986,0.09332711,0.0016211317,0.00015346734,0.00046221423,0.00034240808,0.8285239,0.061756555,0.009624754,0.0013245803,0.0004332926],"about_ca_topic_score_codex":0.0025268968,"about_ca_topic_score_gemma":0.00007096385,"teacher_disagreement_score":0.6917819,"about_ca_system_score_codex":0.000012266512,"about_ca_system_score_gemma":0.00024437354,"threshold_uncertainty_score":0.52302635},"labels":[],"label_agreement":null},{"id":"W4399343663","doi":"10.1007/s10853-024-09823-x","title":"Twinning dominated microstructural evolution in tungsten under impact loading","year":2024,"lang":"en","type":"article","venue":"Journal of Materials Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"National Natural Science Foundation of China","keywords":"Materials science; Crystal twinning; Solid mechanics; Tungsten; Metallurgy; Composite material; Microstructure; Crystallography","score_opus":0.008853328945517972,"score_gpt":0.25221527668704813,"score_spread":0.24336194774153017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399343663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956843,0.0004423442,0.000060676848,0.000084699146,0.003482964,0.00006187087,0.000042650718,0.000012516268,0.00012796739],"genre_scores_gemma":[0.9992377,0.000016022555,0.00038641022,0.000020203244,0.00031245517,1.2384747e-7,0.000003180856,0.0000032883286,0.000020622494],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985726,0.000074084404,0.00045212515,0.0001788053,0.0003781222,0.0003442475],"domain_scores_gemma":[0.99947083,0.000060969218,0.00017876118,0.0000900049,0.000092209135,0.00010720581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019397187,0.000118439566,0.00025310807,0.00035429155,0.00010683029,0.0007110366,0.00035276188,0.00004182797,0.0007462817],"category_scores_gemma":[0.00005807037,0.00007712524,0.00005260733,0.000546073,0.00016816639,0.0012399711,0.000023513852,0.000094403644,0.00006288694],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051688414,0.0000031020597,0.0025808117,0.000021508533,0.0000086832715,0.000057499234,0.0001839585,0.0031851833,0.993349,0.00016315018,0.000046740843,0.00034866208],"study_design_scores_gemma":[0.0002908245,0.00018887747,0.68819135,0.00034016918,0.000025882864,0.00042645278,0.00012358153,0.0009461917,0.30506158,0.0041122064,0.00009169351,0.00020122388],"about_ca_topic_score_codex":0.0009868637,"about_ca_topic_score_gemma":0.000032049775,"teacher_disagreement_score":0.68828744,"about_ca_system_score_codex":0.000045800578,"about_ca_system_score_gemma":0.0003087624,"threshold_uncertainty_score":0.81712615},"labels":[],"label_agreement":null},{"id":"W4399365424","doi":"10.1016/j.physleta.2024.129643","title":"Theoretical exploration of novel compounds in Sr(B,C) (x = 7,8) at high pressure","year":2024,"lang":"en","type":"article","venue":"Physics Letters A","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"High pressure; Chemistry; Materials science; Thermodynamics; Physics","score_opus":0.017943678514633993,"score_gpt":0.21972721241732746,"score_spread":0.20178353390269346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399365424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926304,0.00019798843,0.002757484,0.0017831527,0.0007669639,0.00016960637,0.0003107618,0.000044693934,0.00133892],"genre_scores_gemma":[0.99895084,0.000014500126,0.00030175253,0.00020055595,0.0003305425,0.0000028645065,0.0001637533,0.0000058297223,0.000029336732],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9991631,0.000041829782,0.00018248196,0.00021692477,0.00021140545,0.00018426093],"domain_scores_gemma":[0.9996372,0.000116394454,0.000037831353,0.00015496882,0.000016539314,0.00003705923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014618736,0.0001117195,0.00018579942,0.000036558093,0.000034743458,0.0000637822,0.00013018683,0.00003465406,0.0004460595],"category_scores_gemma":[0.0000056587223,0.00009233418,0.000047905574,0.0001679641,0.00011925413,0.00033865104,0.000021452433,0.000079790756,0.00008692869],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012912974,0.0001365504,0.0035266702,0.00044152525,0.00012624377,0.000031948854,0.0022506549,0.041310553,0.39498007,0.54836226,0.0048789736,0.0038254324],"study_design_scores_gemma":[0.0039742934,0.00066584774,0.10055907,0.0011213225,0.0005640453,0.000019649548,0.00016037213,0.3090089,0.17975225,0.35878673,0.042752925,0.0026345893],"about_ca_topic_score_codex":0.00047136168,"about_ca_topic_score_gemma":0.00006275315,"teacher_disagreement_score":0.26769835,"about_ca_system_score_codex":0.0000034064444,"about_ca_system_score_gemma":0.000015517382,"threshold_uncertainty_score":0.4884039},"labels":[],"label_agreement":null},{"id":"W4399384714","doi":"10.3847/1538-4357/ad40a2","title":"Evolution of the Disk in the Be Binary δ Scorpii Probed during Three Periastron Passages","year":2024,"lang":"en","type":"article","venue":"The Astrophysical Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ciência sem Fronteiras; Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Fundação de Amparo à Pesquisa do Estado de São Paulo","keywords":"Binary number; Physics; Astrophysics; Mathematics; Arithmetic","score_opus":0.00862363955681327,"score_gpt":0.19974810399858225,"score_spread":0.19112446444176898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399384714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969054,0.00026102067,0.00015620285,0.0017803333,0.0005931996,0.00015860151,0.000044962773,0.000009331162,0.00009098882],"genre_scores_gemma":[0.99902695,0.000014219382,0.000074630276,0.000017601282,0.0008126337,0.0000019049454,0.0000027333917,0.00000410367,0.00004521662],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99875444,0.0002734822,0.00021338116,0.00012203961,0.00038811853,0.0002485365],"domain_scores_gemma":[0.9995345,0.00010524955,0.00008692341,0.00021849768,0.000019879237,0.000034945177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003833907,0.00011344058,0.00014358448,0.00002912803,0.0002813409,0.0001798227,0.0005571712,0.000025189884,0.00016062599],"category_scores_gemma":[0.000014005013,0.000044566557,0.0001257392,0.00023703132,0.0001588957,0.0001815137,0.00004196513,0.00036677739,0.000032645516],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008309162,0.00037220586,0.06607687,0.00027776154,0.0003070641,0.0001981614,0.0068295454,0.058550857,0.8281912,0.01395914,0.002199701,0.022206573],"study_design_scores_gemma":[0.00014723447,0.00013480711,0.99116826,0.00010585869,0.000039658702,0.000037762697,0.00022192752,0.0019497519,0.0007489168,0.0051794252,0.00019797738,0.00006839346],"about_ca_topic_score_codex":0.00033910776,"about_ca_topic_score_gemma":0.00011387725,"teacher_disagreement_score":0.92509145,"about_ca_system_score_codex":0.000007827409,"about_ca_system_score_gemma":0.00006443077,"threshold_uncertainty_score":0.21638753},"labels":[],"label_agreement":null},{"id":"W4399781488","doi":"10.1038/s41550-024-02295-8","title":"Complex rotational dynamics of the neutron star in Hercules X-1 revealed by X-ray polarization","year":2024,"lang":"en","type":"article","venue":"Nature Astronomy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Nuclear Physics; Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Goddard Space Flight Center; National Aeronautics and Space Administration; Marshall Space Flight Center; Deutscher Akademischer Austauschdienst; Compute Canada; Istituto Nazionale di Astrofisica","keywords":"Neutron star; Physics; Astrophysics; Pulsar; X-ray pulsar; Astronomy; X-ray burster; X-ray binary; Accretion (finance); Precession; Stars; Stellar evolution; Stellar mass loss","score_opus":0.004397252211676161,"score_gpt":0.20283176134277336,"score_spread":0.1984345091310972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399781488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958485,0.00058764993,0.00024673413,0.0008457343,0.0005132629,0.0002099889,0.001040006,0.000014459379,0.0006936702],"genre_scores_gemma":[0.9968265,0.0000025556985,0.0017108276,0.000047647543,0.000082260514,0.0000011863283,0.0011061638,0.0000028995264,0.0002199038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993836,0.00006235513,0.00014987524,0.00013840933,0.00014343993,0.00012228663],"domain_scores_gemma":[0.99976164,0.000052461703,0.000044898257,0.00009644068,0.000022328559,0.000022215196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012602535,0.00007753146,0.00010491562,0.000036147794,0.0000384724,0.000044133354,0.00015023194,0.00008257345,0.0004685118],"category_scores_gemma":[0.0000062661697,0.00005408979,0.00003551279,0.0001658686,0.00003367319,0.00012274392,0.000009981061,0.00018989043,0.000016708971],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011070835,0.00010097951,0.85364157,0.0002981724,0.00015942934,0.0000049724913,0.0005533954,0.027821485,0.044065814,0.023010798,0.014710589,0.035522092],"study_design_scores_gemma":[0.00010575369,0.000019115965,0.96467537,0.000030454386,0.0000103795255,3.5372358e-7,0.000029288587,0.008027892,0.00009311254,0.0004708066,0.02646902,0.00006843071],"about_ca_topic_score_codex":0.0005539705,"about_ca_topic_score_gemma":0.0007826492,"teacher_disagreement_score":0.11103383,"about_ca_system_score_codex":0.0000068915297,"about_ca_system_score_gemma":0.00005585935,"threshold_uncertainty_score":0.51298755},"labels":[],"label_agreement":null},{"id":"W4399803171","doi":"10.3390/cryst14060565","title":"The Electrical Resistivity of Liquid Fe-16wt%S-2wt%Si at High Pressures and the Effect of S and Si on the Dynamo in the Ancient Vestan Core","year":2024,"lang":"en","type":"article","venue":"Crystals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Dynamo; Electrical resistivity and conductivity; Core (optical fiber); Materials science; Condensed matter physics; Physics; Magnetic field; Electrical engineering; Composite material; Engineering","score_opus":0.007871183825641852,"score_gpt":0.2178573585918852,"score_spread":0.20998617476624334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399803171","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921034,0.0052661593,0.0000024979686,0.0010790331,0.00016956213,0.0005325081,0.00014567203,0.000008820833,0.00069236534],"genre_scores_gemma":[0.99943465,0.00029637953,0.0000026967052,0.00007607203,0.000060888215,0.000009914725,0.0000092123055,0.0000036290974,0.00010657951],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99836314,0.000687118,0.00021569354,0.00020690775,0.00031120324,0.0002159123],"domain_scores_gemma":[0.9944431,0.0051131183,0.00008527621,0.00030733744,0.000018570217,0.000032575255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024805958,0.0001326577,0.0002541007,0.00002586015,0.00026443132,0.00012478464,0.0002643243,0.000048043235,0.00004051051],"category_scores_gemma":[0.00025637372,0.000045383047,0.00004894944,0.00018155426,0.0005135634,0.0000455343,0.000047105415,0.00012810537,0.0000030213807],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.04831356,0.00042304012,0.08585375,0.0052120895,0.001929456,0.00038883503,0.029902775,0.007232109,0.33187136,0.31347364,0.087737545,0.08766184],"study_design_scores_gemma":[0.0019305629,0.004646364,0.88094896,0.0004397065,0.00040956002,0.000033878918,0.000289016,0.01102162,0.027949868,0.013449189,0.058383737,0.0004975248],"about_ca_topic_score_codex":0.00082906167,"about_ca_topic_score_gemma":0.0007556875,"teacher_disagreement_score":0.7950952,"about_ca_system_score_codex":0.0000027879712,"about_ca_system_score_gemma":0.000023612958,"threshold_uncertainty_score":0.20338187},"labels":[],"label_agreement":null},{"id":"W4399883802","doi":"10.1029/2023jb028014","title":"Depth‐Dependent Anisotropy Along Northwest Segment of the North Anatolian Fault Zone: Evidence for Paleo‐Tectonic Structures Contributing to Overall Complexity","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Bilimsel Araştırma Projeleri Birimi, İstanbul Teknik Üniversitesi","keywords":"Geology; Seismology; Seismic anisotropy; Crust; Anisotropy; Shear zone; North Anatolian Fault; Tectonics; Mantle (geology); Receiver function; Shear (geology); Lithosphere; Geophysics; Petrology","score_opus":0.07277847746761351,"score_gpt":0.35844469306906696,"score_spread":0.28566621560145344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399883802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959997,0.0005291454,0.00065336167,0.000829002,0.00071636384,0.00062797416,0.00058877846,0.000012569682,0.000043096046],"genre_scores_gemma":[0.99823,0.00010382413,0.0006401934,0.00006665125,0.00084406516,0.0000035896003,0.000019955865,0.000010228519,0.000081521226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9959162,0.00040047226,0.0007032834,0.00034304295,0.0016985512,0.00093847193],"domain_scores_gemma":[0.99694306,0.0013033993,0.00024658107,0.00035156446,0.00076454045,0.00039087253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017015325,0.00022042055,0.0005800797,0.0001602738,0.00043740467,0.0003403851,0.0008265293,0.00007080091,0.00017895289],"category_scores_gemma":[0.00063360797,0.00013613414,0.000335786,0.00051631307,0.00024275297,0.00035778387,0.00015589129,0.00060438085,0.000042305877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00683785,0.000631786,0.64538765,0.0036881394,0.0025323764,0.0009953291,0.005225881,0.09290943,0.09761737,0.026419125,0.004606193,0.11314883],"study_design_scores_gemma":[0.000426201,0.0010587891,0.9793743,0.0004037068,0.000053582422,0.00002346072,0.00007257015,0.0036020256,0.008740365,0.004499722,0.0015636988,0.00018157392],"about_ca_topic_score_codex":0.0063323057,"about_ca_topic_score_gemma":0.015527568,"teacher_disagreement_score":0.33398664,"about_ca_system_score_codex":0.000023620942,"about_ca_system_score_gemma":0.0005264977,"threshold_uncertainty_score":0.9572595},"labels":[],"label_agreement":null},{"id":"W4400064058","doi":"10.1029/2024gc011454","title":"Thermochemical Structure of the Superior Craton and Environs: Implications for the Evolution and Preservation of Cratonic Lithosphere","year":2024,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; Geological Survey of Canada","funders":"","keywords":"Craton; Geology; Lithosphere; Archean; Proterozoic; Mantle (geology); Kimberlite; Terrane; Precambrian; Geochemistry; Petrology; Paleontology; Tectonics","score_opus":0.006200791176611026,"score_gpt":0.197532705674391,"score_spread":0.19133191449777998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400064058","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926091,0.0050905505,0.00013602697,0.000301201,0.00018382893,0.00041462356,0.0011567315,0.000014182951,0.000093778246],"genre_scores_gemma":[0.9994838,0.00006469226,0.00003941365,0.000006214433,0.00018587134,0.000011288577,0.0000922528,0.000005437243,0.00011100644],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99921626,0.000029564942,0.0002448242,0.00023279742,0.00012586295,0.00015070713],"domain_scores_gemma":[0.99918187,0.00026538683,0.000113970455,0.0003361608,0.00006816626,0.00003445781],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011928393,0.00012922524,0.00018317548,0.0000072914177,0.00015731837,0.00006483611,0.00020119746,0.00009346639,0.000045366363],"category_scores_gemma":[0.000029765393,0.00007631628,0.000063283216,0.0001348534,0.00017639776,0.00011756359,0.00003814987,0.000083794184,7.7642e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000197712,0.000010211951,0.017968155,0.0011764679,0.00008655238,7.4491595e-8,0.000311202,0.00017505483,0.97454166,0.0029753842,0.00017249364,0.0025629804],"study_design_scores_gemma":[0.0004298828,0.00009226914,0.65607303,0.00046309002,0.00037159686,0.0000231335,0.00059110567,0.018029105,0.26637855,0.053953294,0.0031898355,0.00040507945],"about_ca_topic_score_codex":0.001175056,"about_ca_topic_score_gemma":0.00009482395,"teacher_disagreement_score":0.7081631,"about_ca_system_score_codex":0.000004634856,"about_ca_system_score_gemma":0.00007821008,"threshold_uncertainty_score":0.31120878},"labels":[],"label_agreement":null},{"id":"W4400244264","doi":"10.1063/5.0198531","title":"A novel means to generate high pressure","year":2024,"lang":"en","type":"article","venue":"Review of Scientific Instruments","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada)","funders":"Basic Energy Sciences; Natural Sciences and Engineering Research Council of Canada; Canadian Institutes of Health Research; Canadian Light Source; U.S. Department of Energy","keywords":"Gasket; Materials science; Diamond anvil cell; Diamond; Cylinder; Optics; Aperture (computer memory); Laser; Diffraction; Composite material; Physics; Acoustics","score_opus":0.017318428694558533,"score_gpt":0.23976905085316286,"score_spread":0.22245062215860434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400244264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95591384,0.022386752,0.00012164209,0.0007793183,0.011855029,0.0010533015,0.0026981921,0.0000904146,0.005101485],"genre_scores_gemma":[0.99105394,0.0022094995,0.0023575826,0.0003189718,0.00017081888,0.0000057934562,0.0002606873,0.0000062536255,0.0036164653],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984367,0.000042067033,0.00035558475,0.00042787284,0.00047274126,0.00026502897],"domain_scores_gemma":[0.9993694,0.000017220873,0.000065294735,0.00034007648,0.0000785659,0.0001294381],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00084930944,0.00013707494,0.00028770475,0.00009680609,0.00011969987,0.00025445377,0.00034280855,0.000031473355,0.0031758994],"category_scores_gemma":[0.0000271158,0.00009983103,0.00008172991,0.000586583,0.00007073829,0.00022675941,0.000037729988,0.000053602384,0.0011621929],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001838202,0.00009479956,0.0008466465,0.024788838,0.0003056606,0.000013667847,0.00033866236,0.0002971373,0.07311769,0.005774646,0.046905424,0.8474985],"study_design_scores_gemma":[0.000117241754,0.000068228226,0.003626311,0.006687247,0.0001385449,0.000007611801,0.0000051013512,0.0016333658,0.011786937,0.0003411006,0.9753346,0.00025374882],"about_ca_topic_score_codex":0.00038378622,"about_ca_topic_score_gemma":0.00003884237,"teacher_disagreement_score":0.9284291,"about_ca_system_score_codex":0.0000024473804,"about_ca_system_score_gemma":0.00008376734,"threshold_uncertainty_score":0.9996155},"labels":[],"label_agreement":null},{"id":"W4400454642","doi":"10.1016/j.pepi.2024.107228","title":"Hydrogenation of calcite and change in chemical bonding at high pressure: Diamond formation above 100 GPa","year":2024,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Calcite; High pressure; Diamond; Diamond anvil cell; Geology; Materials science; Chemical engineering; Mineralogy; Geochemistry; Thermodynamics; Metallurgy","score_opus":0.012222351974836876,"score_gpt":0.20784798341566021,"score_spread":0.19562563144082334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400454642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970392,0.0014547296,0.0000056004724,0.0001029255,0.0002943361,0.00017384457,0.0007698616,0.000009099197,0.00015037516],"genre_scores_gemma":[0.99940133,0.00014357676,0.00004521274,0.00002852074,0.000110058,0.0000013243299,0.00022128022,0.0000031983086,0.000045483008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933136,0.00004115903,0.00020698301,0.0001457615,0.0001383841,0.0001363725],"domain_scores_gemma":[0.9996837,0.00008068419,0.00008156153,0.00010218898,0.000010732629,0.00004116962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011895272,0.00010896327,0.00019321022,0.000043573105,0.000034093737,0.000030235835,0.000095242096,0.00004590182,0.00009187754],"category_scores_gemma":[0.000005987956,0.00007807302,0.00003336641,0.00010350283,0.00007365051,0.0003125258,0.000036718393,0.000073284,0.000005776203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010285616,0.00010312012,0.38949805,0.005939504,0.00056883594,0.000037716833,0.032817435,0.0036838192,0.380366,0.005241806,0.00082732615,0.17988783],"study_design_scores_gemma":[0.00068538176,0.00025144892,0.73789513,0.0008241474,0.00019929472,0.000034708057,0.00008173442,0.06866797,0.17937824,0.0069887633,0.0044981623,0.00049500517],"about_ca_topic_score_codex":0.0035928222,"about_ca_topic_score_gemma":0.00068609905,"teacher_disagreement_score":0.34839708,"about_ca_system_score_codex":0.0000012863028,"about_ca_system_score_gemma":0.000007893856,"threshold_uncertainty_score":0.5431296},"labels":[],"label_agreement":null},{"id":"W4400580295","doi":"10.1038/s41561-024-01478-2","title":"Contributions of core, mantle and climatological processes to Earth’s polar motion","year":2024,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Eidgenössische Technische Hochschule Zürich; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Polar motion; Geology; Polar; Mantle (geology); Geophysics; Core (optical fiber); Earth's rotation; Climatology; Earth science; Geodesy; Physics","score_opus":0.008720108795048242,"score_gpt":0.2512976242241654,"score_spread":0.24257751542911715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400580295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99396634,0.0023674055,0.00061730674,0.0005194964,0.0007251251,0.000150855,0.0009017401,0.00004590186,0.0007058363],"genre_scores_gemma":[0.9988774,0.00006693187,0.0006572234,0.00014011608,0.00006578158,0.0000010869545,0.00003726697,0.000001217313,0.00015296304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992068,0.000018836226,0.00011973559,0.0002514772,0.00020322177,0.0001999756],"domain_scores_gemma":[0.99960065,0.00010698944,0.000025333287,0.00008893699,0.000084674466,0.0000934322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025666677,0.00007604627,0.00012699251,0.00006344365,0.00010871688,0.000088740606,0.00014243482,0.00010121011,0.0001855481],"category_scores_gemma":[0.00022129208,0.000052617797,0.000017605682,0.00045881534,0.00011033322,0.00017765618,0.000021625063,0.00012797136,0.00006954061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025265795,0.00024583246,0.510339,0.0026384008,0.00008787083,0.00026897376,0.0018174732,0.00085581315,0.19403107,0.230514,0.00803958,0.050909296],"study_design_scores_gemma":[0.00018151371,0.00036697547,0.87384033,0.00019798701,0.000040571325,0.000076129414,0.000067795394,0.0029598617,0.012808243,0.008020833,0.10107669,0.00036304345],"about_ca_topic_score_codex":0.00026674088,"about_ca_topic_score_gemma":0.00017355297,"teacher_disagreement_score":0.36350134,"about_ca_system_score_codex":7.330588e-7,"about_ca_system_score_gemma":0.00005595338,"threshold_uncertainty_score":0.21456915},"labels":[],"label_agreement":null},{"id":"W4400773532","doi":"10.1016/j.jseaes.2024.106258","title":"The crustal structure of southeast Tibet from joint inversion of surface wave dispersion and gravity anomaly data","year":2024,"lang":"en","type":"article","venue":"Journal of Asian Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Geology; Seismology; Inversion (geology); Geophysics; Gravity anomaly; Geodesy; Surface wave; Joint (building); Anomaly (physics); Tectonics; Paleontology; Optics","score_opus":0.02197319916957371,"score_gpt":0.2199810157102532,"score_spread":0.19800781654067948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400773532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996294,0.0011739496,0.000020476089,0.0006265873,0.00069521007,0.000047364676,0.0009289518,0.0000025968195,0.00021082743],"genre_scores_gemma":[0.99868786,0.00014389033,0.0010095587,0.0000075565113,0.0001165901,4.4086637e-9,0.000013772808,0.0000013494958,0.000019422432],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988391,0.00008690596,0.00031330797,0.00016377422,0.00045725665,0.00013965458],"domain_scores_gemma":[0.9993305,0.00010639664,0.00026225104,0.00016549345,0.00005260758,0.00008273899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007041717,0.00008319452,0.00020875943,0.00005305311,0.00017085613,0.00015924548,0.00037758242,0.000036059722,0.00018285215],"category_scores_gemma":[0.000037183057,0.00004311871,0.000045044148,0.0001901172,0.00045036184,0.0004996218,0.000063655054,0.000104652085,0.0000029390706],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000678062,0.0000976798,0.2330792,0.00049871544,0.00048138536,0.00016604307,0.011900696,0.004656455,0.6012689,0.0016748632,0.0047025573,0.14079545],"study_design_scores_gemma":[0.00033759107,0.0008591761,0.9374848,0.0004189877,0.00012393818,0.00006179185,0.00464564,0.020732796,0.022877533,0.0077620107,0.0044691,0.00022662619],"about_ca_topic_score_codex":0.0009978383,"about_ca_topic_score_gemma":0.00067055266,"teacher_disagreement_score":0.7044056,"about_ca_system_score_codex":6.307428e-7,"about_ca_system_score_gemma":0.00012818692,"threshold_uncertainty_score":0.20021027},"labels":[],"label_agreement":null},{"id":"W4400850187","doi":"10.1007/s00269-024-01275-8","title":"Pressure–volume equation of state of Fe18Pt82","year":2024,"lang":"en","type":"article","venue":"Physics and Chemistry of Minerals","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Chemistry; Equation of state; Volume (thermodynamics); Thermodynamics","score_opus":0.012004033587027757,"score_gpt":0.2071671727753433,"score_spread":0.19516313918831554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400850187","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949658,0.001483356,0.00009116139,0.000029314975,0.00007738614,0.000049046746,0.00061048154,0.00000770367,0.0026857594],"genre_scores_gemma":[0.9981333,0.00009540426,0.00011440284,0.0000025722059,0.00009602903,5.496675e-7,0.00008764799,0.000002781144,0.0014672935],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994085,0.000010244654,0.00021974072,0.00012599872,0.00014524051,0.00009031103],"domain_scores_gemma":[0.999654,0.000042867512,0.00010945419,0.00011002243,0.000051266208,0.000032381835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000107791755,0.00007962408,0.0002139532,0.0000083998275,0.000012667193,0.000015106603,0.00007599971,0.00002459917,0.00028983844],"category_scores_gemma":[0.0000069705475,0.000066995584,0.0000449952,0.000069927526,0.00007140701,0.00007938225,0.00001122025,0.00003078291,0.0000031571708],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001670366,0.000021675898,0.0011486269,0.0014409953,0.00007564661,7.411179e-7,0.00020564314,0.0019062794,0.9841633,0.00016485965,0.00057612016,0.01027945],"study_design_scores_gemma":[0.0001411942,0.000051065916,0.0039092936,0.00013606493,0.000078483296,7.6574304e-7,0.000012789546,0.014172732,0.96681184,0.010600502,0.0039570476,0.00012820384],"about_ca_topic_score_codex":0.00050690817,"about_ca_topic_score_gemma":0.0000037452508,"teacher_disagreement_score":0.0173514,"about_ca_system_score_codex":3.3262626e-7,"about_ca_system_score_gemma":0.000024425128,"threshold_uncertainty_score":0.31735277},"labels":[],"label_agreement":null},{"id":"W4400864943","doi":"10.1002/advs.202405561","title":"Prediction of Room‐Temperature Superconductivity in Quasi‐Atomic H<sub>2</sub>‐Type Hydrides at High Pressure","year":2024,"lang":"en","type":"article","venue":"Advanced Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Key Research and Development Program of China; Fundamental Research Funds for the Central Universities; Jilin University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Superconductivity; Antibonding molecular orbital; Condensed matter physics; High pressure; Fermi level; Materials science; Metallic hydrogen; Electron; Physics; Atomic orbital; Metal; Thermodynamics; Metallurgy; Nuclear physics","score_opus":0.009276245751967348,"score_gpt":0.21013309003255107,"score_spread":0.20085684428058373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400864943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99545395,0.0015268311,0.0000097736565,0.00007384787,0.0021603669,0.00020897512,0.0003342063,0.00006950834,0.00016252378],"genre_scores_gemma":[0.9993578,0.00023037633,0.00016119011,0.000018711386,0.00009128334,0.000002763055,0.000044861226,0.000005236348,0.00008778722],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99834406,0.00005882549,0.00025074606,0.0005529116,0.00042550612,0.00036795603],"domain_scores_gemma":[0.99937695,0.00010517448,0.000051490795,0.0002874822,0.000077991026,0.00010091012],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055317796,0.00015874638,0.00023672874,0.00016505203,0.00016805352,0.0001001191,0.00032474517,0.00007634206,0.0001407901],"category_scores_gemma":[0.00008547847,0.00012866808,0.00003733414,0.001007545,0.00028923532,0.0014557461,0.000045576253,0.00015263587,0.00008248575],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035862286,0.000017298396,0.0053838245,0.0000866197,0.00000690584,0.000009275002,0.00023096486,0.008347538,0.98278207,0.00038951891,0.000069542075,0.0026405905],"study_design_scores_gemma":[0.00019035775,0.00017376758,0.18004256,0.00016343714,0.000020844123,0.000010620799,0.000043591303,0.005508882,0.8094116,0.002908201,0.0013222686,0.00020387376],"about_ca_topic_score_codex":0.00046560087,"about_ca_topic_score_gemma":0.0006143596,"teacher_disagreement_score":0.17465875,"about_ca_system_score_codex":0.000014434581,"about_ca_system_score_gemma":0.00017219699,"threshold_uncertainty_score":0.5246932},"labels":[],"label_agreement":null},{"id":"W4400902982","doi":"10.1029/2024gl109758","title":"Seismic Azimuthal Anisotropy Beneath the Alaska Subduction Zone","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Division of Earth Sciences; Jackson School of Geosciences,University of Texas at Austin","keywords":"Subduction; Geology; Forearc; Trench; Seismology; Slab; Anisotropy; Seismic anisotropy; Oceanic crust; Geophysics; Mantle (geology); Tectonics","score_opus":0.02716272558627448,"score_gpt":0.281999108938103,"score_spread":0.2548363833518285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400902982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9840957,0.00023366809,0.00043207084,0.01280837,0.0012118483,0.00027477884,0.00012457774,0.000108736735,0.0007102406],"genre_scores_gemma":[0.995646,0.000057780235,0.00007604492,0.00038721552,0.002362465,0.000010252366,0.00009816446,0.000011618216,0.0013504572],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.99720234,0.0003617862,0.0001833529,0.00048392502,0.00097597594,0.0007926098],"domain_scores_gemma":[0.9988239,0.0005402936,0.000021251159,0.00038431794,0.000058519847,0.0001717225],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00077029417,0.00017367754,0.00018486645,0.00010896107,0.00046664575,0.0005783168,0.00046906734,0.000058587317,0.0010383457],"category_scores_gemma":[0.000041466195,0.000109056615,0.000120206096,0.00053400715,0.00037542608,0.00032099782,0.0000617227,0.0005409171,0.00497353],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000559791,0.00024156163,0.004422786,0.00068601826,0.0005602573,0.0008484186,0.003449928,0.017696561,0.46763784,0.020823827,0.3745878,0.10848519],"study_design_scores_gemma":[0.00066548644,0.00084852753,0.2252438,0.000180207,0.00009419855,0.00005215033,0.0004274511,0.06753449,0.019501114,0.020253835,0.664158,0.0010407438],"about_ca_topic_score_codex":0.004841074,"about_ca_topic_score_gemma":0.0001071148,"teacher_disagreement_score":0.44813672,"about_ca_system_score_codex":0.000012878,"about_ca_system_score_gemma":0.00007924944,"threshold_uncertainty_score":0.99987483},"labels":[],"label_agreement":null},{"id":"W4401046357","doi":"10.1016/j.epsl.2024.118894","title":"Strength of continental lithosphere governed by the time since the last orogeny","year":2024,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"National Key Research and Development Program of China; Key Technologies Research and Development Program; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Lithosphere; Geology; Supercontinent; Orogeny; Craton; Continental collision; Obduction; Collision zone; Continental crust; Geodynamics; Geophysics; Delamination (geology); Tectonics; Mantle (geology); Seismology; Subduction; Oceanic crust","score_opus":0.003634793101600878,"score_gpt":0.16839187804609596,"score_spread":0.16475708494449506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401046357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917478,0.0019950608,0.0000051872676,0.0038574785,0.00047418525,0.00015158654,0.00083315634,0.000027480855,0.00090804545],"genre_scores_gemma":[0.99825746,0.00006127722,0.00006964314,0.0010174384,0.00013627132,4.818597e-7,0.0001637697,0.0000025189804,0.00029111444],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99874693,0.000065792054,0.00016964265,0.00028870057,0.0004065228,0.00032241366],"domain_scores_gemma":[0.99935824,0.00027848314,0.000054371085,0.00020609712,0.000009914747,0.00009290252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051632256,0.00013754013,0.00014108646,0.00002129406,0.00030212392,0.00029608211,0.0004358403,0.000026163198,0.0008286732],"category_scores_gemma":[0.000015774065,0.000069988906,0.00003493262,0.00027620042,0.0007796455,0.00031643955,0.000025145759,0.00012339072,0.0003001952],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027969448,0.00006855198,0.29315463,0.000329193,0.00032851438,0.0002409695,0.004048576,0.0048257043,0.42772081,0.0012759388,0.18083242,0.086895026],"study_design_scores_gemma":[0.00027904555,0.00022305863,0.71089774,0.000086353095,0.00006673905,0.000103767095,0.00019351098,0.019002706,0.0065037683,0.00009035765,0.26212958,0.0004233645],"about_ca_topic_score_codex":0.0018774266,"about_ca_topic_score_gemma":0.000410417,"teacher_disagreement_score":0.42121702,"about_ca_system_score_codex":9.2655574e-7,"about_ca_system_score_gemma":0.00004512628,"threshold_uncertainty_score":0.90733904},"labels":[],"label_agreement":null},{"id":"W4401242636","doi":"10.1139/cjes-2024-0082","title":"Serpentinization of the forearc mantle wedge in subduction zones: revisiting Roy D. Hyndman’s seminal contributions 25 years later","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Forearc; Geology; Subduction; Mantle (geology); Mantle wedge; Seismology; Wedge (geometry); Tectonics; Paleontology; Geometry","score_opus":0.010472954253560488,"score_gpt":0.21951413597681618,"score_spread":0.2090411817232557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401242636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962261,0.00082168495,0.000031673477,0.00058569823,0.001278295,0.000071437666,0.000095972835,0.0000023882963,0.0008867773],"genre_scores_gemma":[0.99945647,0.000027176735,0.00010327093,0.00002499111,0.00021291508,1.468997e-7,0.000005258164,0.0000014160222,0.00016837675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991726,0.00007018554,0.00026263137,0.00009770964,0.00018782154,0.00020905198],"domain_scores_gemma":[0.9995866,0.000051391497,0.00011220668,0.000060062197,0.00007819676,0.00011157232],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009533768,0.00005450343,0.000117316544,0.00019027185,0.00015632602,0.00017438078,0.00021315277,0.000030211726,0.00078516896],"category_scores_gemma":[0.000082369916,0.000036833342,0.000050998424,0.00049711706,0.00017302872,0.00036100682,0.00000504567,0.00009352588,0.000022818243],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014567431,0.000009379678,0.960228,0.00013845536,0.000043765092,0.00014846982,0.0029033513,0.013328966,0.002360671,0.0056889765,0.0015160483,0.013619308],"study_design_scores_gemma":[0.000087110064,0.000059120288,0.9836078,0.00033161655,0.000018382312,0.00006409629,0.00025438963,0.0019089163,0.0008289536,0.0014012569,0.011362504,0.000075820026],"about_ca_topic_score_codex":0.009667661,"about_ca_topic_score_gemma":0.072652385,"teacher_disagreement_score":0.06298472,"about_ca_system_score_codex":0.0000023711418,"about_ca_system_score_gemma":0.00057352625,"threshold_uncertainty_score":0.996927},"labels":[],"label_agreement":null},{"id":"W4401541608","doi":"10.1103/physrevmaterials.8.084805","title":"Strong correlation between ionic bonding strength and superconductivity in compressed hydrides","year":2024,"lang":"en","type":"article","venue":"Physical Review Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Key Research and Development Program of China; Natural Science Foundation of Hebei Province; National Natural Science Foundation of China","keywords":"Superconductivity; Ionic bonding; Materials science; Condensed matter physics; Chemical bond; Valence (chemistry); Superconducting transition temperature; Ion; Chemistry; Physics","score_opus":0.025083615228333862,"score_gpt":0.282807612791317,"score_spread":0.25772399756298314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401541608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9904001,0.008013,0.000012845152,0.00019797073,0.00043814117,0.0003156496,0.0003266184,0.000050450915,0.0002452568],"genre_scores_gemma":[0.99727994,0.0020079485,0.000032189128,0.000026928705,0.0003783795,0.000006186806,0.00023856356,0.000006403681,0.00002347583],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99879897,0.00020772197,0.0002946289,0.0003082083,0.00015878503,0.00023168506],"domain_scores_gemma":[0.9994532,0.00028866442,0.000049187995,0.00013645303,0.000011774456,0.000060761522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043262323,0.00016436042,0.00051917153,0.000042064636,0.0000547838,0.00019708964,0.000083523366,0.000031180833,0.00064084854],"category_scores_gemma":[0.0000451156,0.00012507314,0.000042464973,0.00014221242,0.00004801749,0.00045944896,0.000025705483,0.00008278785,0.00018537838],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008518584,0.00025646487,0.05399153,0.032612514,0.00035338383,0.0001349703,0.0012090894,0.00063116575,0.7314706,0.06199298,0.0028380582,0.11442408],"study_design_scores_gemma":[0.00089046365,0.00036141026,0.79538363,0.019815892,0.0007853836,0.000018165625,0.000049516766,0.006755674,0.09173173,0.051748905,0.030575337,0.0018838657],"about_ca_topic_score_codex":0.0008004923,"about_ca_topic_score_gemma":0.000037963848,"teacher_disagreement_score":0.74139214,"about_ca_system_score_codex":0.000004528545,"about_ca_system_score_gemma":0.000021376725,"threshold_uncertainty_score":0.70168424},"labels":[],"label_agreement":null},{"id":"W4401718559","doi":"10.1109/icops58192.2024.10627131","title":"Transport of Dispersed Tungsten Dust in the STOR-M Plasma","year":2024,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Tungsten; Plasma; Materials science; Environmental science; Metallurgy; Physics","score_opus":0.010510356002992174,"score_gpt":0.20027198306983232,"score_spread":0.18976162706684013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401718559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96498775,0.00010483426,0.000010854745,0.0003473433,0.00036216472,0.000091565606,0.00010752511,0.000017847531,0.033970118],"genre_scores_gemma":[0.9988421,0.000015405447,0.00004138419,0.000049913553,0.00006614447,6.879661e-7,0.00004096974,0.0000013918942,0.00094197004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99949896,0.000027847009,0.00012429892,0.00010404421,0.00013397001,0.000110902736],"domain_scores_gemma":[0.9997952,0.000072776085,0.000011127276,0.00009534185,0.000005388959,0.000020158071],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022452694,0.00005638158,0.00009637342,0.000030052115,0.000018612393,0.000025134485,0.00014324355,0.00002639291,0.003031967],"category_scores_gemma":[0.0000022882145,0.000029663688,0.000034549666,0.0001260684,0.000030015708,0.000083437146,0.0000016192449,0.000045251505,0.00013197261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005947839,0.0004019802,0.6545944,0.002101894,0.00050382066,0.0014078099,0.050157703,0.012582772,0.034227423,0.09632633,0.048865445,0.09823563],"study_design_scores_gemma":[0.0002841569,0.00011925925,0.8756956,0.000062696054,0.000043940257,0.000008356083,0.0010002941,0.0057215816,0.0016935052,0.0010068024,0.114142075,0.00022175757],"about_ca_topic_score_codex":0.0034711896,"about_ca_topic_score_gemma":0.0043863766,"teacher_disagreement_score":0.22110116,"about_ca_system_score_codex":4.569484e-7,"about_ca_system_score_gemma":0.000020638017,"threshold_uncertainty_score":0.9978794},"labels":[],"label_agreement":null},{"id":"W4401867699","doi":"10.1093/gji/ggae269","title":"Structure of the crust and upper mantle in Greenland and northeastern Canada: insights from anisotropic Rayleigh-wave tomography","year":2024,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Ottawa","funders":"University of Ottawa; Natural Sciences and Engineering Research Council of Canada; Discovery Eye Foundation","keywords":"Geology; Lithosphere; Craton; Crust; Mantle (geology); Seismology; Seismic tomography; Tectonics; Geophysics","score_opus":0.004965504968077334,"score_gpt":0.17557742587363268,"score_spread":0.17061192090555535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401867699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99709475,0.00055914966,0.000010617891,0.00042625723,0.001213948,0.000046705118,0.0004572276,0.0000029465552,0.00018842502],"genre_scores_gemma":[0.99926704,0.000049580078,0.000050356775,0.00008187472,0.00047258646,1.628596e-7,0.00002396723,0.0000028080192,0.00005161959],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992369,0.000043798947,0.0001818462,0.00014664566,0.00028182726,0.00010901401],"domain_scores_gemma":[0.99970114,0.0000798644,0.000056044322,0.000063154446,0.00003393309,0.000065855136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00002355039,0.000096493604,0.00013945621,0.000053367934,0.000058658046,0.00012778453,0.00013384616,0.000033261596,0.00030747533],"category_scores_gemma":[0.0000059624003,0.000057504338,0.000037284924,0.000081644575,0.000064578715,0.00015230967,0.000033068955,0.00017254378,0.0000020395503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016521127,0.000046258556,0.9443752,0.00006395255,0.00045888155,0.0003325293,0.0012177904,0.0005835072,0.019869734,0.004997216,0.00081351283,0.027076202],"study_design_scores_gemma":[0.00017866847,0.000021690654,0.9825236,0.00006863067,0.000015703165,0.000032557986,0.000033061187,0.0020867984,0.0005243047,0.012470704,0.0019703978,0.000073874304],"about_ca_topic_score_codex":0.16317591,"about_ca_topic_score_gemma":0.28005618,"teacher_disagreement_score":0.11688026,"about_ca_system_score_codex":0.0000048161046,"about_ca_system_score_gemma":0.00007865526,"threshold_uncertainty_score":0.84239656},"labels":[],"label_agreement":null},{"id":"W4401883938","doi":"10.1103/physrevb.110.064106","title":"<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mrow> <mml:mi>ε</mml:mi> <mml:mo>−</mml:mo> <mml:mi>ζ</mml:mi> </mml:mrow> </mml:math> transition in solid oxygen","year":2024,"lang":"lv","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"King Fahd University of Petroleum and Minerals; U.S. Department of Energy","keywords":"Crystallography; Physics; Algorithm; Materials science; Chemistry; Mathematics","score_opus":0.017953637363074218,"score_gpt":0.27787838738148724,"score_spread":0.25992475001841303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401883938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9115341,0.039902158,0.00044106133,0.002576599,0.0023957319,0.00024955708,0.0008339116,0.0002390241,0.04182791],"genre_scores_gemma":[0.931035,0.059529673,0.00026006243,0.0033723307,0.003669007,0.00054789166,0.0012579012,0.00024539736,0.00008277613],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99163735,0.00073381787,0.001807009,0.0018342921,0.002094661,0.0018928825],"domain_scores_gemma":[0.9950505,0.0013126576,0.0010210014,0.0015170986,0.00013616798,0.0009626053],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001867023,0.0009556234,0.0009715912,0.00017774224,0.00068476156,0.00093372795,0.0015659191,0.0006649065,0.014630917],"category_scores_gemma":[0.00083326246,0.0012692473,0.002307369,0.001383139,0.0007916616,0.0013127,0.00055491657,0.0014426017,0.012751959],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022418352,0.00043951848,0.0000028154907,0.012064527,0.00061963516,0.0005201558,0.00081580284,0.00034385888,0.0042214845,0.9056819,0.058262613,0.016803496],"study_design_scores_gemma":[0.0020539842,0.00442715,0.000436129,0.047675133,0.008191711,0.0006009647,0.0004116439,0.3283861,0.40744412,0.032030597,0.16316938,0.0051730806],"about_ca_topic_score_codex":0.001431488,"about_ca_topic_score_gemma":0.00033576693,"teacher_disagreement_score":0.8736513,"about_ca_system_score_codex":0.000012261597,"about_ca_system_score_gemma":0.0007544033,"threshold_uncertainty_score":0.99897575},"labels":[],"label_agreement":null},{"id":"W4402167349","doi":"10.22541/au.172538614.44654756/v1","title":"No temporal change seen in high-frequency waves scattered near the Core-Mantle Boundary","year":2024,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mantle (geology); Geology; Observable; Cosmic microwave background; Core–mantle boundary; Diffraction; Scattering; Geophysics; Seismology; Inner core; Seismic wave; Travel time; Core (optical fiber); Physics; Optics","score_opus":0.032714564485852936,"score_gpt":0.24127475501712553,"score_spread":0.2085601905312726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402167349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9650344,0.0019619272,0.0000025727331,0.0019131724,0.0069231642,0.00090893277,0.0017586891,0.00013592308,0.021361165],"genre_scores_gemma":[0.99303705,0.000110556364,0.0006414082,0.0005992323,0.0014072692,0.000025553203,0.001173797,0.000015941794,0.0029891825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99803054,0.00011918332,0.0004258046,0.0006219931,0.00034206186,0.00046042012],"domain_scores_gemma":[0.998993,0.000080414866,0.0001320198,0.00065050926,0.00004426063,0.000099836434],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00051904237,0.00035905754,0.00046735996,0.000086254084,0.0002076272,0.0010601514,0.0007437976,0.0002471546,0.005922102],"category_scores_gemma":[0.000014635762,0.00021966304,0.000120593475,0.00015658666,0.00024868583,0.0001242353,0.00036294866,0.00054466707,0.00461414],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00068839325,0.0005304269,0.6824874,0.009752853,0.0018347274,0.002490036,0.020278957,0.002888834,0.00328844,0.023197057,0.19791786,0.05464498],"study_design_scores_gemma":[0.0005645242,0.00023752429,0.6584932,0.0007381638,0.00018020914,0.000016358199,0.00011161467,0.005864202,0.00021226886,0.23227456,0.099651664,0.001655696],"about_ca_topic_score_codex":0.15548745,"about_ca_topic_score_gemma":0.01768517,"teacher_disagreement_score":0.2090775,"about_ca_system_score_codex":0.000007668821,"about_ca_system_score_gemma":0.0002681543,"threshold_uncertainty_score":0.9999769},"labels":[],"label_agreement":null},{"id":"W4402513884","doi":"10.1038/s41524-024-01390-8","title":"A unified moment tensor potential for silicon, oxygen, and silica","year":2024,"lang":"en","type":"article","venue":"npj Computational Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; École de Technologie Supérieure; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Alliance de recherche numérique du Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Nuclear Waste Management Organization","keywords":"Silicon; Oxygen; Moment (physics); Tensor (intrinsic definition); Materials science; Physics; Mathematics; Optoelectronics; Geometry; Classical mechanics; Quantum mechanics","score_opus":0.010277468761060784,"score_gpt":0.22441309057789516,"score_spread":0.21413562181683438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402513884","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921903,0.00030669762,0.002291071,0.000858021,0.001742899,0.000430488,0.0019063749,0.00009427761,0.00017986257],"genre_scores_gemma":[0.9962992,0.0000140052425,0.0019187292,0.00020319199,0.0005410619,0.000012919064,0.0007623598,0.000007355601,0.00024119356],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9990208,0.000050489005,0.00025882243,0.0002932414,0.00017416805,0.00020248412],"domain_scores_gemma":[0.99960506,0.0001511225,0.00004200468,0.000073585674,0.00006297061,0.00006528485],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002554994,0.00013440565,0.00020008757,0.00006087507,0.00012022899,0.0003940183,0.00008629762,0.000052857245,0.0014164454],"category_scores_gemma":[0.000012743517,0.000109471315,0.000036358786,0.000059478643,0.00004464055,0.00013178447,0.00001577,0.000023406139,0.0001747466],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010382293,0.00013559783,0.00046294348,0.0020356227,0.00066952116,0.00012545263,0.001085397,0.15491898,0.68084043,0.096549585,0.032100152,0.0300381],"study_design_scores_gemma":[0.002687458,0.0011068524,0.29041263,0.00022160652,0.00039427046,0.00016069118,0.00012323538,0.1410727,0.033845514,0.34930503,0.17893709,0.0017329128],"about_ca_topic_score_codex":0.00017945278,"about_ca_topic_score_gemma":0.000009240452,"teacher_disagreement_score":0.6469949,"about_ca_system_score_codex":0.0000027039962,"about_ca_system_score_gemma":0.000049565664,"threshold_uncertainty_score":0.9994964},"labels":[],"label_agreement":null},{"id":"W4402694859","doi":"10.1029/2024jb029387","title":"A Reference Model of Crustal Thickness and <i>V</i><sub><i>p</i></sub>/<i>V</i><sub><i>s</i></sub> of Western Canada","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Alberta; University of Ottawa","funders":"","keywords":"Geology; Geodesy; Geometry; Mathematics","score_opus":0.03338480330981208,"score_gpt":0.27936204791538355,"score_spread":0.24597724460557147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402694859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970135,0.000765776,0.0001257344,0.0003282444,0.00039858383,0.00022202068,0.00063771644,0.000013624903,0.0004947989],"genre_scores_gemma":[0.998029,0.0012153946,0.00012842871,0.00007041314,0.00045805657,0.0000021125786,0.00002240349,0.000020194191,0.000054009965],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9950996,0.00041785117,0.0009726562,0.0004326913,0.002233891,0.00084329443],"domain_scores_gemma":[0.99685836,0.0009496541,0.00036295448,0.0003720039,0.00088518544,0.0005718483],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0017661612,0.0003173826,0.00094618375,0.0002877834,0.00017374389,0.00019797793,0.0005979861,0.00015755337,0.000035019464],"category_scores_gemma":[0.00023125167,0.0002476124,0.00018746438,0.00062529417,0.0005067209,0.00061195943,0.00015007018,0.0010389175,0.000029796287],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053494,0.00012445713,0.0007678721,0.0007921301,0.00020530722,0.00022334173,0.00045865736,0.004670954,0.9750909,0.0005328972,0.0016460933,0.014952429],"study_design_scores_gemma":[0.0008882522,0.0015413053,0.036502916,0.0010716759,0.0001378609,0.000106294356,0.00020239952,0.019433437,0.9297925,0.007937795,0.0018247229,0.0005608226],"about_ca_topic_score_codex":0.0352557,"about_ca_topic_score_gemma":0.05078608,"teacher_disagreement_score":0.0452984,"about_ca_system_score_codex":0.000015775882,"about_ca_system_score_gemma":0.0023721624,"threshold_uncertainty_score":0.9999976},"labels":[],"label_agreement":null},{"id":"W4402903905","doi":"10.1126/sciadv.ado1219","title":"Mesozoic intraoceanic subduction shaped the lower mantle beneath the East Pacific Rise","year":2024,"lang":"en","type":"article","venue":"Science Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Subduction; Geology; Mantle (geology); Transition zone; Mesozoic; Paleontology; Downwelling; Triple junction; Slab; Seismology; Ridge; East Asia; Oceanography; Tectonics; Geophysics; Upwelling; Geography","score_opus":0.008501568632576367,"score_gpt":0.22080664478402207,"score_spread":0.2123050761514457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402903905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9696698,0.01062608,0.00015742912,0.0032606418,0.008485437,0.00033647512,0.00009979075,0.00013441051,0.00722993],"genre_scores_gemma":[0.99833775,0.00025467822,0.00008137614,0.00006888671,0.00047720122,0.000003244816,0.0000063628054,0.0000033058911,0.0007671815],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985714,0.000051590217,0.0001534794,0.00038194534,0.0004681268,0.00037347557],"domain_scores_gemma":[0.9994355,0.00010057526,0.000046010202,0.0003074027,0.000041895695,0.00006861739],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00094053237,0.00012635998,0.00010157658,0.000053630512,0.00079338375,0.0006235961,0.00067917,0.000021766527,0.001086018],"category_scores_gemma":[0.000033888213,0.000057860885,0.000048158225,0.00077654957,0.0008088707,0.0010670146,0.000030032463,0.00011549383,0.00068323774],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013845126,0.00009969942,0.0070826737,0.00016801833,0.00007375421,0.00008820289,0.00666182,0.008175968,0.041855026,0.016372718,0.005188589,0.9140951],"study_design_scores_gemma":[0.00021606922,0.00047008914,0.07410498,0.00014354243,0.000102157115,0.00008225484,0.0036727304,0.025034023,0.008628406,0.040780667,0.8459906,0.0007745097],"about_ca_topic_score_codex":0.0001562928,"about_ca_topic_score_gemma":0.00028534664,"teacher_disagreement_score":0.91332054,"about_ca_system_score_codex":0.0000046811288,"about_ca_system_score_gemma":0.000104214036,"threshold_uncertainty_score":0.99982715},"labels":[],"label_agreement":null},{"id":"W4402907838","doi":"10.1016/j.commatsci.2024.113419","title":"Emergent superconductivity in clathrate Sr(B,C)9 at low pressures","year":2024,"lang":"en","type":"article","venue":"Computational Materials Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Clathrate hydrate; Superconductivity; Condensed matter physics; Materials science; Physics; Chemistry; Hydrate","score_opus":0.015902360334999307,"score_gpt":0.24508968324761402,"score_spread":0.2291873229126147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402907838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949972,0.00035709905,0.00012294581,0.00018221737,0.003396481,0.0001790239,0.00031390114,0.00006841838,0.00038269765],"genre_scores_gemma":[0.99887186,0.000028286358,0.0006513141,0.000047740705,0.00018469372,0.000003992362,0.000091154725,0.000004325163,0.000116621944],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9982791,0.00008732027,0.00028854283,0.00049974624,0.0004857769,0.00035951982],"domain_scores_gemma":[0.99953854,0.000112015965,0.000039373786,0.0001418449,0.00006249943,0.000105732746],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0008852448,0.00014485365,0.00019261223,0.00016395736,0.00022070535,0.00044130324,0.00032970886,0.000039031944,0.004986582],"category_scores_gemma":[0.000037837046,0.000118613374,0.00002787836,0.00044396386,0.00029811217,0.00078827416,0.00007257747,0.00004858704,0.00090742734],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005167791,0.00004147901,0.0042882026,0.00025839344,0.000014669656,0.000077017125,0.000743783,0.121366344,0.8623651,0.007921759,0.00091376185,0.0019577679],"study_design_scores_gemma":[0.00030304142,0.00009736198,0.7476353,0.00025623187,0.000018777659,0.000039969218,0.00003855278,0.039055336,0.15890114,0.04971763,0.0032794073,0.00065725413],"about_ca_topic_score_codex":0.00069992663,"about_ca_topic_score_gemma":0.00015458961,"teacher_disagreement_score":0.7433471,"about_ca_system_score_codex":0.000015742899,"about_ca_system_score_gemma":0.00019670509,"threshold_uncertainty_score":0.9998705},"labels":[],"label_agreement":null},{"id":"W4403574249","doi":"10.1016/j.jseaes.2024.106375","title":"A shallow mantle seismic discontinuity beneath northeast India: Evidence from receiver function analyses","year":2024,"lang":"en","type":"article","venue":"Journal of Asian Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Ministry of Earth Sciences","keywords":"Geology; Receiver function; Discontinuity (linguistics); Seismology; Mantle (geology); Geophysics; Lithosphere; Tectonics","score_opus":0.03630664276881858,"score_gpt":0.27724022313793273,"score_spread":0.24093358036911416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403574249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915042,0.0029435565,0.0005096363,0.0008137995,0.0021738177,0.00007180544,0.0001025094,0.000020207432,0.0018604937],"genre_scores_gemma":[0.997834,0.0002607885,0.00079872285,0.000079705605,0.00077657774,2.334732e-7,0.0000071686954,0.000002934573,0.00023984158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982748,0.00012137271,0.00039791322,0.00028495234,0.00064643973,0.0002745383],"domain_scores_gemma":[0.9992392,0.00017243475,0.000235463,0.00012356215,0.00007173288,0.00015759392],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009005796,0.0001484597,0.0002874974,0.00020982177,0.00023139275,0.00064098113,0.00041035633,0.00005369423,0.0020291016],"category_scores_gemma":[0.000053852636,0.00009430639,0.00015254632,0.0005266992,0.000197883,0.0016212313,0.000018750257,0.00018018878,0.00021117873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003713918,0.000097649216,0.72234476,0.00014172606,0.0005702677,0.00072773447,0.005749432,0.018561825,0.015163423,0.00018228962,0.0034789084,0.23261058],"study_design_scores_gemma":[0.00009770976,0.00047277063,0.9864187,0.00042636998,0.0001263621,0.00004294384,0.00047681542,0.0042566834,0.00068236113,0.0021573955,0.0046687433,0.00017314962],"about_ca_topic_score_codex":0.0015035793,"about_ca_topic_score_gemma":0.0020106635,"teacher_disagreement_score":0.2640739,"about_ca_system_score_codex":0.000002686839,"about_ca_system_score_gemma":0.00023211766,"threshold_uncertainty_score":0.9988832},"labels":[],"label_agreement":null},{"id":"W4403586062","doi":"10.48550/arxiv.2409.03941","title":"White dwarf fundamentals","year":2024,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute for Theoretical Astrophysics","keywords":"White dwarf; White (mutation); Mathematics; Physics; Biology; Astrophysics; Genetics; Stars","score_opus":0.04780188370445926,"score_gpt":0.16837835539426566,"score_spread":0.1205764716898064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403586062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9619682,0.00030123087,0.00016162719,0.000094868155,0.002959553,0.00025772088,0.00093963795,0.0001899651,0.033127185],"genre_scores_gemma":[0.98876417,0.00017971676,0.00006104719,0.000078602054,0.00032194037,1.6601454e-7,0.00029950996,0.000010254303,0.010284587],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9985126,0.00008706832,0.00017156158,0.00078858226,0.00009061163,0.00034956785],"domain_scores_gemma":[0.999121,0.000042374948,0.00011581322,0.000506344,0.000039586153,0.0001748611],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00018626342,0.0002926355,0.00033726217,0.00013844222,0.00011532618,0.00021376146,0.0005500361,0.00022728075,0.0049731974],"category_scores_gemma":[0.000005377733,0.00028933695,0.00018642005,0.00022882933,0.00009538327,0.00010536037,0.00038430185,0.00037608898,0.0041542295],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030508483,0.00014370955,0.15419815,0.0017965143,0.0011781954,0.0034247972,0.0010618662,0.7669803,0.00027742647,0.03955649,0.02684275,0.0042347154],"study_design_scores_gemma":[0.0012420627,0.00036346307,0.13820988,0.0008980285,0.001496774,0.000022777782,0.0006014115,0.13044535,0.0008249887,0.65584755,0.06641727,0.0036304211],"about_ca_topic_score_codex":0.0019472362,"about_ca_topic_score_gemma":0.0006390787,"teacher_disagreement_score":0.6365349,"about_ca_system_score_codex":0.0000134589445,"about_ca_system_score_gemma":0.00011054034,"threshold_uncertainty_score":0.9999559},"labels":[],"label_agreement":null},{"id":"W4403709751","doi":"10.48550/arxiv.2409.11459","title":"Thermal Evolution of Lava Planets","year":2024,"lang":"en","type":"preprint","venue":"arXiv (Cornell University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Astrobiology; Lava; Planet; Geology; Thermal; Physics; Astronomy; Meteorology; Volcano; Paleontology","score_opus":0.03206722866039464,"score_gpt":0.15316197592626243,"score_spread":0.1210947472658678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403709751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98369247,0.00033635448,0.00017966353,0.000016648919,0.0013159169,0.00014730408,0.0007118213,0.00006686213,0.01353299],"genre_scores_gemma":[0.9983918,0.000061806655,0.000028858656,0.0000074843165,0.00017916723,5.7291263e-8,0.00018461759,0.0000052266437,0.0011409597],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99906594,0.00007501496,0.00014631057,0.00043493783,0.00007295985,0.00020481895],"domain_scores_gemma":[0.9993678,0.000045774384,0.00012998909,0.00033623326,0.000041605614,0.00007859619],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014248157,0.00017863957,0.00026159463,0.00011246552,0.000048172875,0.000035907233,0.0003711313,0.00019232718,0.0011650033],"category_scores_gemma":[0.0000055901496,0.0001710257,0.00011096161,0.0001508228,0.00008257712,0.00006289701,0.00017482949,0.00023576053,0.00061313296],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001544398,0.000039249036,0.025421545,0.0006174199,0.00025847674,0.00031381514,0.00021033797,0.9372552,0.0010381895,0.0328088,0.0011812394,0.0007013041],"study_design_scores_gemma":[0.001014128,0.00038927593,0.3349615,0.00074955507,0.0011409365,0.00000806618,0.00029458228,0.33544302,0.0022492518,0.31429976,0.007555266,0.0018946803],"about_ca_topic_score_codex":0.0069147134,"about_ca_topic_score_gemma":0.00062751386,"teacher_disagreement_score":0.6018122,"about_ca_system_score_codex":0.000010097191,"about_ca_system_score_gemma":0.00012590032,"threshold_uncertainty_score":0.99974805},"labels":[],"label_agreement":null},{"id":"W4403908216","doi":"10.1029/2024je008466","title":"Phase Transitions and Thermal Equation of State of Fe‐9wt.%Si Applied to the Moon and Mercury","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Planets","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; Office of Science; National Science Foundation","keywords":"Mercury (programming language); Thermal; Equation of state; Physics; Thermodynamics; Astrobiology; Materials science; Computer science","score_opus":0.043025251894651076,"score_gpt":0.3215179684818141,"score_spread":0.278492716587163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403908216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997726,0.00036493887,0.00012079423,0.0007879843,0.0000921452,0.00017472051,0.00035958813,0.0000030432577,0.00037078655],"genre_scores_gemma":[0.9995197,0.000135791,0.00008560745,0.000016269989,0.00018655001,8.693121e-7,0.000022077022,0.000003093269,0.000030009229],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9986851,0.00015142596,0.0002808182,0.0001125612,0.0005734607,0.00019660124],"domain_scores_gemma":[0.99900144,0.00058836944,0.00006993275,0.00008978696,0.00010817599,0.00014228828],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001034235,0.00007598253,0.00022286974,0.00012215873,0.00007888026,0.000075473785,0.00013617911,0.00002652637,0.00010212641],"category_scores_gemma":[0.000038479968,0.000045063684,0.000034668243,0.00019799317,0.0001404829,0.00015727377,0.0000162417,0.00022099777,0.00002103599],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014809852,0.0003044076,0.0001492693,0.00047976788,0.0002675778,0.000082081555,0.0047609448,0.00309196,0.6625926,0.0030598005,0.0014334266,0.3222972],"study_design_scores_gemma":[0.0073778923,0.021708438,0.65296715,0.0015711312,0.00057416357,0.0002231728,0.0016841518,0.08519096,0.11641184,0.073550776,0.03758274,0.001157587],"about_ca_topic_score_codex":0.0005414763,"about_ca_topic_score_gemma":0.00009283436,"teacher_disagreement_score":0.6528179,"about_ca_system_score_codex":0.0000017915999,"about_ca_system_score_gemma":0.000079447964,"threshold_uncertainty_score":0.18376437},"labels":[],"label_agreement":null},{"id":"W4404145151","doi":"10.3390/geosciences14110301","title":"Non-Linear Effects of Gravity Change on Mantle Dynamics","year":2024,"lang":"en","type":"article","venue":"Geosciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Mantle (geology); Dynamics (music); Geophysics; Geodesy; Physics","score_opus":0.011785184723714147,"score_gpt":0.2288340840358824,"score_spread":0.21704889931216825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404145151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936478,0.00036680413,0.00010449743,0.00015056433,0.0030746695,0.0001742459,0.00017071719,0.000037863727,0.0022728334],"genre_scores_gemma":[0.99912447,0.00008124632,0.00013971295,0.000065885746,0.00022290193,0.0000022705626,0.000030950585,0.0000019420008,0.00033061032],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9991437,0.000023003098,0.0001126919,0.00023782381,0.00026336862,0.00021941261],"domain_scores_gemma":[0.999645,0.00011574335,0.0000338368,0.00013025357,0.0000146680795,0.0000604799],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025226964,0.0000930273,0.00014260384,0.00007430521,0.000088301844,0.00006673699,0.00022858856,0.00003633364,0.00017876853],"category_scores_gemma":[0.000014877166,0.00006349591,0.000043366297,0.00027820186,0.00012393689,0.00022916582,0.000015001755,0.000052014024,0.00031229437],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018929307,0.00045448577,0.17732763,0.005882461,0.00019395756,0.0006648522,0.0072359927,0.002595938,0.02012111,0.05122911,0.0058141984,0.728291],"study_design_scores_gemma":[0.0002714833,0.0014471955,0.7733613,0.0005332675,0.000068051886,0.000008919889,0.00013321429,0.17487158,0.01761522,0.011430665,0.01963849,0.00062057446],"about_ca_topic_score_codex":0.0044233347,"about_ca_topic_score_gemma":0.0008006877,"teacher_disagreement_score":0.7276704,"about_ca_system_score_codex":0.0000017418521,"about_ca_system_score_gemma":0.000027729538,"threshold_uncertainty_score":0.6686788},"labels":[],"label_agreement":null},{"id":"W4404303408","doi":"10.1007/s12210-024-01280-7","title":"The oxidation of iron in amphiboles at high temperatures: a review and implications for large-scale Earth processes","year":2024,"lang":"en","type":"review","venue":"RENDICONTI LINCEI","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Amphibole; Earth (classical element); Earth science; Scale (ratio); Astrobiology; Geology; Geochemistry; Materials science; Environmental science; Metallurgy; Geography; Physics","score_opus":0.01686591348799206,"score_gpt":0.28481898665538846,"score_spread":0.2679530731673964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404303408","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003815138,0.9950317,0.0000040904224,0.00024079031,0.00019752004,0.0012388383,0.002823323,0.000017622166,0.000064565545],"genre_scores_gemma":[0.0008158801,0.9965474,0.000087310626,0.000029556722,0.00013837407,0.00009586049,0.0017305498,0.000010202611,0.0005448501],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987101,0.00008939446,0.0005345083,0.00034157422,0.00009921364,0.00022518472],"domain_scores_gemma":[0.99901664,0.0003138688,0.00029623,0.00026736842,0.000057109803,0.00004876818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004424503,0.0002227896,0.0008803764,0.00006701594,0.00015360159,0.000091713635,0.00022769782,0.000113103044,0.000041692343],"category_scores_gemma":[0.00008134584,0.00012546954,0.00011202912,0.00029934317,0.000055827077,0.00009543049,0.000033040225,0.00010149571,0.000026386304],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002251506,0.00006065884,0.00027008884,0.41265884,0.00022531547,0.0000024961794,0.00020923531,0.0000025875668,0.000057978374,0.0040336447,0.008137008,0.5743196],"study_design_scores_gemma":[0.000070153736,0.000035616624,0.00043796384,0.0121263815,0.0007000313,0.0000048463303,0.0000049922305,0.0000013499715,0.000008685819,0.0004602966,0.98599887,0.0001508161],"about_ca_topic_score_codex":0.00011554157,"about_ca_topic_score_gemma":0.0036830488,"teacher_disagreement_score":0.9778619,"about_ca_system_score_codex":0.00000413178,"about_ca_system_score_gemma":0.00015286963,"threshold_uncertainty_score":0.51164997},"labels":[],"label_agreement":null},{"id":"W4404681254","doi":"","title":"OSSOS measures the orbital ne structure of main-belt TNOs","year":2023,"lang":"en","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Herzberg Institute of Astrophysics; University of British Columbia","funders":"","keywords":"Computer science; Geology; Orbital Fracture; Medicine","score_opus":0.010392390645954331,"score_gpt":0.1957786838801697,"score_spread":0.18538629323421538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404681254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841423,0.00021351565,0.0005355354,0.0033804807,0.00027824478,0.00021003257,0.00039969885,0.000097131866,0.010743065],"genre_scores_gemma":[0.9964902,0.000057116475,0.00078644144,0.000042893473,0.000041934654,0.000001722815,0.00035903402,0.00000691267,0.0022137759],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99734306,0.0015125368,0.000270575,0.0002477812,0.00036277945,0.0002632818],"domain_scores_gemma":[0.99774766,0.0008523206,0.00017862728,0.00073570886,0.0004024391,0.00008324292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019674285,0.00013147242,0.00018824701,0.000063955384,0.00030715464,0.00014305851,0.0006765713,0.00006903104,0.00066520035],"category_scores_gemma":[0.0003564619,0.000093458584,0.000077004355,0.0004696179,0.00018360784,0.000111973946,0.00008543423,0.00012160431,0.000115823066],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013407032,0.0003102932,0.06325074,0.000346305,0.0004424885,0.000045720964,0.033665236,0.0032240744,0.5654554,0.121491894,0.03340799,0.17822579],"study_design_scores_gemma":[0.0009790385,0.000003580536,0.45660266,0.00041019206,0.00009856436,0.000027613336,0.00065619167,0.009810614,0.44303927,0.0213597,0.066306114,0.00070648384],"about_ca_topic_score_codex":0.003437468,"about_ca_topic_score_gemma":0.005486274,"teacher_disagreement_score":0.3933519,"about_ca_system_score_codex":0.000003068689,"about_ca_system_score_gemma":0.00007197528,"threshold_uncertainty_score":0.7283477},"labels":[],"label_agreement":null},{"id":"W4405008350","doi":"10.1029/2024gl112155","title":"No Temporal Change Seen in High‐Frequency Waves Scattered Near the Core‐Mantle Boundary","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Institute of Geology and Geophysics, Chinese Academy of Sciences; National Science Foundation","keywords":"Mantle (geology); Geology; Core–mantle boundary; Geophysics; Cosmic microwave background; Scattering; Observable; Diffraction; Seismology; Inner core; Seismic wave; Travel time; Core (optical fiber); Physics; Optics; Anisotropy","score_opus":0.0580636621930575,"score_gpt":0.30142733782046144,"score_spread":0.24336367562740394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405008350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853027,0.00043769708,0.000003897799,0.011175861,0.0010703491,0.00053619937,0.00025225116,0.000071077775,0.0011499759],"genre_scores_gemma":[0.9961211,0.000034651184,0.00012378341,0.0010812194,0.0018704751,0.000033570897,0.000203994,0.000015405141,0.0005157743],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99689794,0.00037518903,0.00026977566,0.0005485458,0.0009287069,0.0009798587],"domain_scores_gemma":[0.9986818,0.00059189944,0.000030527597,0.0004549404,0.00006271505,0.00017812662],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010370581,0.00021307642,0.0002745927,0.00014067393,0.00048709713,0.0011228392,0.00067280926,0.00007479072,0.0011239371],"category_scores_gemma":[0.00007385451,0.00013803512,0.00010193016,0.00069589564,0.00083254173,0.0004767513,0.00010138093,0.0006621131,0.006964353],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012556185,0.00072479073,0.14091629,0.0025902125,0.00078295317,0.0067961416,0.015240892,0.00043567325,0.34902585,0.02628772,0.3431022,0.11284167],"study_design_scores_gemma":[0.00053191924,0.0004348231,0.8275734,0.00029910626,0.000024558623,0.000009257202,0.000083675244,0.0066195745,0.00051989587,0.018185165,0.14505145,0.00066716515],"about_ca_topic_score_codex":0.055835195,"about_ca_topic_score_gemma":0.001331258,"teacher_disagreement_score":0.68665713,"about_ca_system_score_codex":0.000017741484,"about_ca_system_score_gemma":0.00016307943,"threshold_uncertainty_score":0.9999141},"labels":[],"label_agreement":null},{"id":"W4405357844","doi":"10.1002/9781394195947.ch7","title":"Structure, Origin, and Deformation of the Lithosphere in the Northern Canadian Cordillera From High‐Resolution, Passive‐Source Seismic Velocity Models","year":2024,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"National Science Foundation","keywords":"Lithosphere; Geology; Seismology; Deformation (meteorology); High resolution; Seismic velocity; Geophysics; Geodesy; Tectonics; Remote sensing","score_opus":0.006043762369900577,"score_gpt":0.1742056420206501,"score_spread":0.16816187965074952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405357844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9758161,0.0013810504,0.00005106613,0.00036935013,0.0009598855,0.0007052691,0.005124014,0.000051380346,0.015541898],"genre_scores_gemma":[0.9968202,0.00007824381,0.0000780219,0.00019000565,0.0003545707,0.000005604088,0.00037398667,0.000038301303,0.002061037],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9987149,0.0001074772,0.00024592425,0.00031878555,0.00030389827,0.0003090108],"domain_scores_gemma":[0.9992635,0.000042302385,0.00017196685,0.00039445958,0.000030583702,0.0000971495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000067109606,0.0002699216,0.00035590827,0.00009475579,0.0001047945,0.0001047628,0.00042640237,0.00021148076,0.0004654042],"category_scores_gemma":[0.000004258985,0.00015173267,0.000103014674,0.00039235794,0.00016699827,0.00008874851,0.000029448627,0.00029516759,0.00006135202],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037969826,0.00039246195,0.14227597,0.0025097833,0.0033250826,0.00011148764,0.026198128,0.09620023,0.000180695,0.0144010335,0.5000887,0.21393673],"study_design_scores_gemma":[0.0007871861,0.00014952788,0.5834687,0.0007630166,0.00049016514,0.0000051405113,0.0005806543,0.05124795,0.000047397476,0.15841576,0.2027998,0.0012447524],"about_ca_topic_score_codex":0.81349564,"about_ca_topic_score_gemma":0.6109037,"teacher_disagreement_score":0.4411927,"about_ca_system_score_codex":0.0000068354543,"about_ca_system_score_gemma":0.000095807525,"threshold_uncertainty_score":0.6187479},"labels":[],"label_agreement":null},{"id":"W4405760258","doi":"10.4006/0836-1398-37.4.330","title":"Gravitational waves derived from the elastic energy","year":2024,"lang":"en","type":"article","venue":"Physics Essays","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Gravitational field; Gravitational energy; Classical mechanics; Maxwell's equations; Gravitation; Gravitational wave; Gravitational acceleration; Gravitational redshift; Context (archaeology); Classical field theory; Gravitational potential; Mechanics; Quantum electrodynamics; Quantum mechanics","score_opus":0.012434575472982755,"score_gpt":0.2069864052997089,"score_spread":0.19455182982672614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405760258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84314513,0.0056248005,0.036676034,0.0031059624,0.014333697,0.00036491797,0.00597459,0.00052947656,0.090245396],"genre_scores_gemma":[0.99719816,0.000038182796,0.00018897043,0.00019354136,0.00159558,0.0000025587487,0.0006147036,0.000005268773,0.00016305955],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99928236,0.00005379374,0.00010647541,0.00019625197,0.00019671004,0.00016439929],"domain_scores_gemma":[0.99925977,0.00050915877,0.00002488761,0.00013975477,0.000022221895,0.00004418125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006888186,0.000107211876,0.00010443582,0.000009421462,0.00013608976,0.0002173358,0.00017960859,0.000025465037,0.0008172606],"category_scores_gemma":[0.0000092390455,0.000067543006,0.000055122608,0.0001120846,0.00005951878,0.00015740236,0.000014238974,0.00005976661,0.0005214993],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037318532,0.00004401984,0.003804053,0.000050910126,0.00032421437,0.000042556574,0.0016100842,0.008950696,0.01828727,0.8812795,0.01749422,0.06807511],"study_design_scores_gemma":[0.00007897294,0.000022030134,0.0195279,0.000031714626,0.00005114935,9.0086627e-7,0.00003663439,0.012145613,0.0015272882,0.95505613,0.011349184,0.00017246495],"about_ca_topic_score_codex":0.0024166633,"about_ca_topic_score_gemma":0.0002672661,"teacher_disagreement_score":0.154053,"about_ca_system_score_codex":0.0000013456443,"about_ca_system_score_gemma":0.000042436503,"threshold_uncertainty_score":0.89484304},"labels":[],"label_agreement":null},{"id":"W4406366495","doi":"10.1103/physreve.111.015205","title":"Ionic structure, liquid-liquid phase transitions, x-ray diffraction, and x-ray Thomson scattering in shock-compressed liquid silicon in the 100–200 GPa regime","year":2025,"lang":"en","type":"article","venue":"Physical review. E","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; National Research Council Canada","funders":"Engineering and Physical Sciences Research Council","keywords":"X-ray; Diffraction; Silicon; Materials science; Scattering; Phase (matter); Shock (circulatory); X-ray crystallography; Ionic liquid; Phase transition; Crystallography; Condensed matter physics; Optics; Physics; Chemistry; Metallurgy","score_opus":0.012162858485054197,"score_gpt":0.293030626093283,"score_spread":0.2808677676082288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406366495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887123,0.0069951857,0.000032815966,0.002780373,0.0002222556,0.000677705,0.00013436373,0.000028031618,0.0004169617],"genre_scores_gemma":[0.99416524,0.0040298323,0.000024386347,0.0013588833,0.00021633289,0.000024863166,0.00015064234,0.0000067997653,0.000023013752],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981078,0.00041318688,0.00044285948,0.00044428007,0.00022702666,0.00036486684],"domain_scores_gemma":[0.9991072,0.0002793397,0.00010923908,0.00039205363,0.000033260876,0.000078918514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004192159,0.00026399127,0.00057407987,0.00009496321,0.00014734754,0.000090375426,0.00033205785,0.000059228638,0.0002132023],"category_scores_gemma":[0.000059279075,0.00018331784,0.000101121106,0.00048719696,0.0000972508,0.00030930035,0.00002367111,0.00028454317,0.00002874679],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0032014088,0.0013746999,0.00094958814,0.0047511156,0.00016658005,0.000080079706,0.0031710542,0.0069605745,0.94900537,0.0052026147,0.0025391844,0.022597745],"study_design_scores_gemma":[0.016716313,0.01068833,0.37489492,0.024368761,0.0019501057,0.000066196415,0.0010782161,0.021500384,0.079746425,0.02351217,0.43940514,0.0060730292],"about_ca_topic_score_codex":0.0006685313,"about_ca_topic_score_gemma":0.00036929987,"teacher_disagreement_score":0.86925894,"about_ca_system_score_codex":0.0000089354335,"about_ca_system_score_gemma":0.000049243696,"threshold_uncertainty_score":0.74754846},"labels":[],"label_agreement":null},{"id":"W4406392237","doi":"10.1016/s0967-0653(98)82918-9","title":"10.1016/s0967-0653(98)82918-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Shear (geology); Seismology; Mantle (geology); Velocity gradient; Geodesy; Geophysics; Petrology; Mechanics; Physics","score_opus":0.005462940383051636,"score_gpt":0.1560333030631282,"score_spread":0.15057036268007656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406392237","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004819978,0.00005407158,1.8411674e-7,0.0001272453,0.000008324387,0.00012951194,0.00015266807,0.000077521545,0.9946305],"genre_scores_gemma":[0.0014921387,5.349522e-7,0.000088602355,0.00005185381,0.00031761444,0.0000016829346,0.00011125802,0.000005349377,0.99793094],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991188,0.000043756776,0.00014859569,0.00021615747,0.0001775102,0.00029514628],"domain_scores_gemma":[0.9995291,0.000038744423,0.00002494846,0.00022286092,0.000020419757,0.00016392936],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014442984,0.00012604585,0.00017688352,0.000033999364,0.00009815593,0.000090072324,0.00023297154,0.0000498936,0.99978334],"category_scores_gemma":[0.000009427589,0.00010589854,0.000038926013,0.00012559514,0.000025774028,0.00012504544,0.000010047842,0.00005179684,0.99959487],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000737843,0.000015052396,6.1454244e-7,0.0000069773314,0.000016557986,0.000009201626,0.000021983338,0.0007041219,0.000034384044,0.000001339169,0.37422106,0.6248949],"study_design_scores_gemma":[0.00010855297,0.00010399872,0.0003835749,0.000007078475,0.000012364292,0.0000026201365,4.5479547e-7,0.00013867776,0.00014806811,0.000042277516,0.9988907,0.0001616451],"about_ca_topic_score_codex":0.00082322786,"about_ca_topic_score_gemma":0.000007164652,"teacher_disagreement_score":0.62473327,"about_ca_system_score_codex":0.000001457042,"about_ca_system_score_gemma":0.000019570887,"threshold_uncertainty_score":0.4318417},"labels":[],"label_agreement":null},{"id":"W4406398300","doi":"10.1016/0967-0653(94)91381-1","title":"10.1016/0967-0653(94)91381-1","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Isostasy; Geology; Crest; Mantle (geology); Geodesy; Geophysics; Seismology; Physics; Tectonics","score_opus":0.005263335518847099,"score_gpt":0.15281664099725112,"score_spread":0.147553305478404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406398300","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008422647,0.00006517257,2.1778446e-7,0.00012336479,0.000009459537,0.00013311718,0.00018626457,0.000079334925,0.99098045],"genre_scores_gemma":[0.003180262,4.810783e-7,0.000085601794,0.000056685494,0.00031217726,0.0000017198423,0.00013624056,0.000005402623,0.9962214],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99910176,0.00004470542,0.00015147401,0.00022092956,0.00017885423,0.0003022965],"domain_scores_gemma":[0.9995183,0.00004029196,0.000025312,0.00022769037,0.000020552183,0.0001678874],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014528279,0.00012771417,0.00017382005,0.00003425495,0.00010296967,0.00009184808,0.00023784049,0.000050331888,0.99946916],"category_scores_gemma":[0.000009705165,0.00010756548,0.00003907943,0.00012941705,0.000026363017,0.00012869218,0.000010080685,0.000052076804,0.9986386],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074297044,0.000016546654,0.0000020301275,0.000007513798,0.000016992224,0.000010555135,0.000023715502,0.000843334,0.000064257314,0.0000016041447,0.2441666,0.75477254],"study_design_scores_gemma":[0.00010465937,0.00010833033,0.00074095296,0.000007049389,0.000012062749,0.0000030463923,4.4495022e-7,0.00014654225,0.00012336868,0.000042820175,0.99854636,0.00016437937],"about_ca_topic_score_codex":0.0006619728,"about_ca_topic_score_gemma":0.000006633181,"teacher_disagreement_score":0.75460815,"about_ca_system_score_codex":0.0000014243826,"about_ca_system_score_gemma":0.000019710737,"threshold_uncertainty_score":0.4386393},"labels":[],"label_agreement":null},{"id":"W4406398785","doi":"10.1039/d4cp04200j","title":"Pressure-driven phase transformations on Mg<sub>3</sub>Ca(CO<sub>3</sub>)<sub>4</sub> huntite carbonate","year":2025,"lang":"en","type":"article","venue":"Physical Chemistry Chemical Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Conselleria d'Educació, Investigació, Cultura i Esport; Agencia Estatal de Investigación; Ministerio de Ciencia y Tecnología; Fundación para el Fomento en Asturias de la Investigación Científica Aplicada y la Tecnología; Generalitat Valenciana; Conselleria de Cultura, Educación y Ciencia, Generalitat Valenciana; Gobierno del Principado de Asturias; Compute Canada; European Commission; Yale University","keywords":"Carbonate; Phase (matter); Materials science; Mineralogy; Chemistry; Metallurgy; Organic chemistry","score_opus":0.008067628580515795,"score_gpt":0.23025974546110542,"score_spread":0.22219211688058962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406398785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986604,0.00006219281,0.00029529494,0.00038991953,0.0003324431,0.0006479637,0.0026431764,0.00028039236,0.008744625],"genre_scores_gemma":[0.99512255,0.00006474498,0.00004461799,0.00048935186,0.0017604575,0.00006963039,0.0023687673,0.000048833506,0.000031063464],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9957176,0.00009097207,0.0007716769,0.0012324213,0.0009599242,0.0012274251],"domain_scores_gemma":[0.99749726,0.00037543935,0.00027171604,0.00094704324,0.00020923163,0.00069932564],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016666879,0.0009153837,0.0010961788,0.00006552962,0.0003719719,0.00028420138,0.00091971527,0.00034483688,0.000049078473],"category_scores_gemma":[0.000082071354,0.0009012224,0.0005532557,0.00082761835,0.00034104576,0.0005128334,0.000113510185,0.00086478365,0.00077960215],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025679567,0.0007843965,0.000034592318,0.00049175316,0.00025261342,0.0000115329,0.00021530829,0.0043953243,0.9798782,0.0002500564,0.0037006002,0.009728849],"study_design_scores_gemma":[0.0014229155,0.0000984107,0.00020326507,0.00018319783,0.0003323477,0.0000023761897,0.000015524556,0.011436025,0.97665244,0.0056521012,0.003050861,0.0009505293],"about_ca_topic_score_codex":0.000055193606,"about_ca_topic_score_gemma":0.000008878362,"teacher_disagreement_score":0.00877832,"about_ca_system_score_codex":0.00004410594,"about_ca_system_score_gemma":0.00021448245,"threshold_uncertainty_score":0.9999984},"labels":[],"label_agreement":null},{"id":"W4406416038","doi":"10.1016/s0967-0653(97)80314-6","title":"10.1016/s0967-0653(97)80314-6","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Mantle (geology); Seismology; Anisotropy; Geophysics; Tectonics","score_opus":0.006198259387259625,"score_gpt":0.15605645797281897,"score_spread":0.14985819858555935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406416038","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0031146961,0.00006610511,1.9229607e-7,0.00010382438,0.000008549827,0.00013400482,0.00015254505,0.000078946345,0.9963411],"genre_scores_gemma":[0.00088243285,5.6657973e-7,0.0000919992,0.00005259471,0.00031076802,0.0000017638897,0.000111369656,0.0000054507,0.9985431],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990966,0.000045359317,0.00015295601,0.00022188797,0.00017995996,0.00030328715],"domain_scores_gemma":[0.99951786,0.000040359922,0.000025720665,0.00022793334,0.000021026603,0.0001671048],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014721276,0.00012991586,0.00017528662,0.00003476478,0.0000995463,0.0000926929,0.00023840682,0.000050968152,0.9997242],"category_scores_gemma":[0.000009804688,0.000109067216,0.000040086154,0.00012946542,0.000026520082,0.00012898579,0.000010140001,0.00005303897,0.99979603],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006329371,0.0000124429835,6.200813e-7,0.0000057681436,0.000012854365,0.000007909415,0.000019421526,0.00055380486,0.000019596444,9.5324594e-7,0.05867172,0.9406316],"study_design_scores_gemma":[0.0001164014,0.00010984551,0.00013977046,0.0000072721537,0.000012134165,0.0000028722825,4.902612e-7,0.00013623488,0.00014845858,0.00005739289,0.99910283,0.00016628977],"about_ca_topic_score_codex":0.0008098826,"about_ca_topic_score_gemma":0.000006226156,"teacher_disagreement_score":0.94046533,"about_ca_system_score_codex":0.0000014256924,"about_ca_system_score_gemma":0.00001926021,"threshold_uncertainty_score":0.4447632},"labels":[],"label_agreement":null},{"id":"W4406436435","doi":"10.1016/0967-0653(96)82011-4","title":"10.1016/0967-0653(96)82011-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Attenuation; Seismology; Shear (geology); Mantle (geology); Geophysics; Geodesy; Petrology; Physics; Optics","score_opus":0.005500798893804367,"score_gpt":0.15228167201632192,"score_spread":0.14678087312251756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406436435","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008664088,0.000059495633,2.0856204e-7,0.00013000233,0.000009558196,0.00012929467,0.00017199529,0.00007698242,0.99075836],"genre_scores_gemma":[0.0028163362,5.2009807e-7,0.00008088973,0.000052657702,0.00029884474,0.0000016502697,0.00012683476,0.000005298348,0.99661696],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.999126,0.00004366145,0.0001476143,0.00021524972,0.000171482,0.0002959812],"domain_scores_gemma":[0.99952424,0.00003690547,0.000025337897,0.00022720714,0.000020286016,0.00016599862],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014352889,0.00012537804,0.00016969471,0.000033480737,0.00009919345,0.00008611022,0.00023647967,0.000050002836,0.9995755],"category_scores_gemma":[0.000008617534,0.00010479777,0.000038264658,0.00011320729,0.00002615442,0.00012912486,0.0000099607905,0.00005042027,0.9989302],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000718152,0.000016029771,0.0000025974032,0.0000070510805,0.00001590131,0.000009117345,0.000023873885,0.0006333946,0.000057457513,0.0000015278434,0.2858522,0.71330905],"study_design_scores_gemma":[0.00010104165,0.00010927409,0.0006646507,0.0000066211405,0.000011788532,0.0000029692835,4.2589576e-7,0.00013257709,0.00014172477,0.000044560147,0.998623,0.0001613313],"about_ca_topic_score_codex":0.00081318436,"about_ca_topic_score_gemma":0.000006462263,"teacher_disagreement_score":0.7131477,"about_ca_system_score_codex":0.0000013309158,"about_ca_system_score_gemma":0.000019025507,"threshold_uncertainty_score":0.4273529},"labels":[],"label_agreement":null},{"id":"W4406471232","doi":"10.1016/0967-0653(93)93842-f","title":"10.1016/0967-0653(93)93842-f","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Attenuation; Mantle (geology); Seismology; Pacific ocean; Geophysics; Oceanography; Physics; Optics","score_opus":0.00484750526709518,"score_gpt":0.1486513858233058,"score_spread":0.14380388055621063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406471232","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008701406,0.000058601952,2.3161161e-7,0.00012759665,0.000009501705,0.00013315077,0.0001767045,0.00008020384,0.9907126],"genre_scores_gemma":[0.003213479,4.922927e-7,0.00008909653,0.000057026446,0.000307965,0.0000017165611,0.0001341787,0.0000054113248,0.9961906],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991004,0.000044585122,0.00015201312,0.00022100647,0.00017927698,0.00030271232],"domain_scores_gemma":[0.9995176,0.000040374594,0.000025366302,0.00022790044,0.000020500822,0.00016826107],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014553366,0.00012820306,0.00017407774,0.00003424821,0.00010292,0.00009218957,0.00023773655,0.000050376028,0.9994667],"category_scores_gemma":[0.000009605094,0.00010768616,0.000039505318,0.0001285622,0.000026346564,0.00012905747,0.0000100758725,0.000052067404,0.99860173],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007613238,0.000016682678,0.000002052848,0.000007623601,0.00001720406,0.000010229539,0.000025153558,0.0009231058,0.000059359845,0.0000016531137,0.21080378,0.788057],"study_design_scores_gemma":[0.00010501778,0.00010935039,0.00070120074,0.000007039749,0.000012024297,0.0000031039478,4.7595546e-7,0.00016047076,0.00012939554,0.00004280035,0.99856454,0.00016457724],"about_ca_topic_score_codex":0.00073504576,"about_ca_topic_score_gemma":0.0000064911565,"teacher_disagreement_score":0.78789246,"about_ca_system_score_codex":0.0000014169319,"about_ca_system_score_gemma":0.000019609548,"threshold_uncertainty_score":0.4391314},"labels":[],"label_agreement":null},{"id":"W4406477335","doi":"10.1016/s0967-0653(97)84655-8","title":"10.1016/s0967-0653(97)84655-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Seismology; Geophysics","score_opus":0.006157605772078298,"score_gpt":0.15555277825834385,"score_spread":0.14939517248626555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406477335","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.003173277,0.00006398275,2.2879726e-7,0.00012433494,0.000008441614,0.00013524249,0.00015671321,0.00007879733,0.996259],"genre_scores_gemma":[0.00097278063,5.7354913e-7,0.000094018884,0.000050248058,0.00031240436,0.0000017662156,0.000110908935,0.0000054421116,0.9984518],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99909914,0.000045357283,0.00015253025,0.00022142474,0.00017957893,0.0003019861],"domain_scores_gemma":[0.9995167,0.000040996896,0.00002568973,0.00022724137,0.000021017871,0.0001683469],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014544399,0.00012964326,0.00017493224,0.000034785637,0.00010329818,0.000092649716,0.00023772662,0.000050894952,0.9997335],"category_scores_gemma":[0.000010080747,0.00010884829,0.00004001096,0.00012724577,0.000026496546,0.0001289331,0.000010112409,0.000052875996,0.99979323],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059940347,0.00001178075,6.947495e-7,0.000005382314,0.000011931899,0.000007483596,0.000016551085,0.0005651062,0.00001647632,9.35087e-7,0.049957976,0.94934577],"study_design_scores_gemma":[0.00011723902,0.00011102674,0.00018466529,0.0000072298526,0.000012233377,0.0000029765572,5.0188356e-7,0.00013742472,0.00014067601,0.000041317064,0.99907976,0.00016492105],"about_ca_topic_score_codex":0.0006471975,"about_ca_topic_score_gemma":0.000006457171,"teacher_disagreement_score":0.94918084,"about_ca_system_score_codex":0.0000014312793,"about_ca_system_score_gemma":0.000019708423,"threshold_uncertainty_score":0.44387046},"labels":[],"label_agreement":null},{"id":"W4406495420","doi":"10.1016/0967-0653(96)80560-6","title":"10.1016/0967-0653(96)80560-6","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Anisotropy; Mantle wedge; Seismology; Shear (geology); Mantle (geology); Geophysics; Subduction; Petrology; Tectonics; Optics; Physics","score_opus":0.005300355979070946,"score_gpt":0.15275907679759976,"score_spread":0.14745872081852882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406495420","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009247624,0.000055077886,2.0660741e-7,0.00014911778,0.0000093680665,0.0001320661,0.00017599559,0.00007967862,0.99015087],"genre_scores_gemma":[0.0032349052,4.8199604e-7,0.000092186725,0.000058008685,0.00030430718,0.0000017046044,0.0001337102,0.000005391315,0.9961693],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99910253,0.000044793287,0.00015145243,0.00022073922,0.00017848014,0.00030201528],"domain_scores_gemma":[0.99951816,0.000040688123,0.000025300575,0.00022741052,0.000020459409,0.00016798338],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000145428,0.00012800304,0.00017368403,0.000034273162,0.00010271658,0.0000917266,0.00023706317,0.00005029829,0.99949837],"category_scores_gemma":[0.000009723141,0.00010762373,0.000039414987,0.00012873372,0.000026027259,0.0001284919,0.000010047218,0.00005183676,0.99863976],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007568774,0.00001693293,0.0000026406515,0.000007786172,0.000017480024,0.000010462287,0.00002467449,0.0008119856,0.000067879904,0.0000015936545,0.24939206,0.7495708],"study_design_scores_gemma":[0.00010432695,0.000107546046,0.0006634878,0.0000070680285,0.00001196985,0.0000030945916,4.7533695e-7,0.00015036885,0.00015655637,0.00004455277,0.99858606,0.00016448012],"about_ca_topic_score_codex":0.0007373947,"about_ca_topic_score_gemma":0.0000060568027,"teacher_disagreement_score":0.74940634,"about_ca_system_score_codex":0.0000013933558,"about_ca_system_score_gemma":0.000019406622,"threshold_uncertainty_score":0.43887684},"labels":[],"label_agreement":null},{"id":"W4406498221","doi":"10.1016/0967-0653(96)85840-6","title":"10.1016/0967-0653(96)85840-6","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Classification of discontinuities; Geology; Geodesy; Seismology; Mathematics; Mathematical analysis","score_opus":0.0052660935018230175,"score_gpt":0.15232143468337184,"score_spread":0.1470553411815488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406498221","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009969805,0.000058596233,2.2586859e-7,0.00013613734,0.000008402124,0.00013187491,0.00018453744,0.00008013552,0.9894303],"genre_scores_gemma":[0.00312934,4.921471e-7,0.00008698506,0.000055307486,0.00031359866,0.0000017060637,0.00013431109,0.0000052871915,0.996273],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991033,0.000044854147,0.00015128255,0.00022074953,0.00017810847,0.000301703],"domain_scores_gemma":[0.99951917,0.000040405976,0.000025081683,0.00022714803,0.000020437361,0.00016773648],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014566445,0.00012758948,0.00017358165,0.000034288027,0.00010251346,0.00009170474,0.00023676868,0.000050248585,0.99947214],"category_scores_gemma":[0.000009679391,0.00010759358,0.000039401777,0.00012858982,0.000026311543,0.00012828111,0.000010051497,0.000052032756,0.99862474],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000731849,0.000016265089,0.000002417461,0.000007640964,0.000016859085,0.000010224246,0.000024073492,0.00087681384,0.00007292697,0.0000015033105,0.23199986,0.7668982],"study_design_scores_gemma":[0.000103942504,0.0001079339,0.00064828905,0.0000070142646,0.000011838959,0.0000030620008,4.5821972e-7,0.0001512932,0.00017585051,0.00004280547,0.99858314,0.00016435164],"about_ca_topic_score_codex":0.00071313186,"about_ca_topic_score_gemma":0.000006077176,"teacher_disagreement_score":0.7667339,"about_ca_system_score_codex":0.0000014199127,"about_ca_system_score_gemma":0.000019539762,"threshold_uncertainty_score":0.4387539},"labels":[],"label_agreement":null},{"id":"W4406504343","doi":"10.1016/s0967-0653(97)87080-9","title":"10.1016/s0967-0653(97)87080-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Classification of discontinuities; Seismology; Mantle (geology); Geophysics","score_opus":0.0061847306782111915,"score_gpt":0.15589071342483568,"score_spread":0.1497059827466245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406504343","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0029156213,0.00006583036,2.1808539e-7,0.00012209476,0.000008529814,0.00013436371,0.00015651745,0.00007901449,0.99651784],"genre_scores_gemma":[0.00093863194,5.864024e-7,0.00009038486,0.000051996052,0.00031503083,0.0000017689707,0.00011269781,0.0000054490342,0.9984835],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990956,0.00004526566,0.00015320322,0.00022224456,0.00018022594,0.00030343124],"domain_scores_gemma":[0.99951524,0.000041066585,0.000025739071,0.00022793296,0.000021084863,0.00016893607],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014724338,0.00012997989,0.00017542408,0.00003482167,0.00010360898,0.00009426727,0.00023898386,0.000051009243,0.9997199],"category_scores_gemma":[0.000009973214,0.00010908959,0.000040081726,0.00012872915,0.000026621728,0.0001298856,0.000010312071,0.000053119584,0.9997996],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062093146,0.000012152996,7.0747876e-7,0.000005631986,0.000012511946,0.000007727736,0.000017566514,0.000579204,0.000017017146,0.0000010429113,0.059829496,0.93945485],"study_design_scores_gemma":[0.00011689515,0.00011030117,0.00018060548,0.000007214026,0.0000122481915,0.0000028733243,4.926172e-7,0.00014030434,0.00012546974,0.000042509513,0.99909484,0.0001662238],"about_ca_topic_score_codex":0.0007072946,"about_ca_topic_score_gemma":0.0000064315473,"teacher_disagreement_score":0.9392886,"about_ca_system_score_codex":0.0000014475685,"about_ca_system_score_gemma":0.00001958948,"threshold_uncertainty_score":0.44485444},"labels":[],"label_agreement":null},{"id":"W4406504505","doi":"10.1016/s0967-0653(97)87071-8","title":"10.1016/s0967-0653(97)87071-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Petrology; Earth science; Geochemistry","score_opus":0.006171564149555711,"score_gpt":0.15573729976459438,"score_spread":0.14956573561503866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406504505","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0028790014,0.00006598081,2.1470201e-7,0.00012343566,0.000008631679,0.00013400082,0.00015755412,0.000078688725,0.99655247],"genre_scores_gemma":[0.0009159339,6.0873833e-7,0.00008745995,0.000050645613,0.000322837,0.0000017689939,0.00011416631,0.000005444672,0.9985011],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99909717,0.000045239736,0.0001529455,0.00022160665,0.00018014685,0.00030291808],"domain_scores_gemma":[0.99951714,0.000041027302,0.000025706426,0.0002262209,0.000021070618,0.00016884471],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014677105,0.00012981983,0.00017488566,0.000034797682,0.00010334777,0.00009291902,0.00023812613,0.000051210558,0.9997017],"category_scores_gemma":[0.000009796955,0.00010899603,0.000040059957,0.00012832652,0.00002662699,0.00012940206,0.000010277369,0.000053231204,0.99979025],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006143909,0.0000119542165,7.0311546e-7,0.0000055326022,0.0000122509555,0.0000075296653,0.000018052237,0.0005701624,0.00001668699,9.5672e-7,0.06806991,0.9312248],"study_design_scores_gemma":[0.00011718751,0.000108802975,0.00017665702,0.0000072283087,0.0000120514305,0.0000028362756,5.138801e-7,0.00014098773,0.00012445859,0.000041741754,0.99910146,0.00016607462],"about_ca_topic_score_codex":0.00070379657,"about_ca_topic_score_gemma":0.000005503816,"teacher_disagreement_score":0.93105876,"about_ca_system_score_codex":0.000001441605,"about_ca_system_score_gemma":0.000019484401,"threshold_uncertainty_score":0.4444729},"labels":[],"label_agreement":null},{"id":"W4406513094","doi":"10.1016/s0967-0653(98)82957-8","title":"10.1016/s0967-0653(98)82957-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Discontinuity (linguistics); Mantle (geology); Structural basin; Pacific basin; Seismology; Paleontology; Oceanography","score_opus":0.005452443325795863,"score_gpt":0.15591651807308773,"score_spread":0.15046407474729187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406513094","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.005293884,0.000053159998,1.8682783e-7,0.000121287965,0.000008181028,0.00012804367,0.00014915915,0.00007713211,0.99416894],"genre_scores_gemma":[0.001609766,5.4360635e-7,0.00008923109,0.000048920658,0.0003125618,0.0000016726076,0.00010697434,0.0000053315016,0.997825],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991255,0.000044680586,0.00014753405,0.0002148044,0.00017505871,0.00029242338],"domain_scores_gemma":[0.9995313,0.000039640105,0.000024820758,0.00022137599,0.000020089028,0.00016276217],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014492118,0.0001254503,0.00017599143,0.000033906803,0.00009715971,0.00009009025,0.00023190149,0.00005005575,0.99979806],"category_scores_gemma":[0.000009445859,0.000105335115,0.000038755268,0.00012521139,0.000025958916,0.00012431612,0.000010019073,0.000051828658,0.99959236],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007403975,0.000015087698,6.3296466e-7,0.000007050641,0.000016386024,0.000009552705,0.000022076294,0.0007093181,0.000033184664,0.0000017001518,0.3274244,0.6716866],"study_design_scores_gemma":[0.00010949736,0.00010254891,0.00036867024,0.000007124727,0.000012259357,0.0000026734758,4.4559292e-7,0.00013695366,0.00012091127,0.00003985237,0.99893844,0.00016064208],"about_ca_topic_score_codex":0.0007210693,"about_ca_topic_score_gemma":0.0000068154345,"teacher_disagreement_score":0.6715259,"about_ca_system_score_codex":0.0000013980288,"about_ca_system_score_gemma":0.000019388042,"threshold_uncertainty_score":0.42954415},"labels":[],"label_agreement":null},{"id":"W4406530201","doi":"10.1016/0967-0653(94)93620-x","title":"10.1016/0967-0653(94)93620-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mediterranean climate; Tomography; Mantle (geology); Seismology; Geography; Geophysics; Archaeology; Radiology; Medicine","score_opus":0.00528183105760906,"score_gpt":0.15294830875507898,"score_spread":0.1476664776974699,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406530201","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007620339,0.000064457476,2.1041731e-7,0.00012170051,0.000009405549,0.00013242001,0.00017491312,0.000079978134,0.99179655],"genre_scores_gemma":[0.0028650337,4.7802763e-7,0.000086347856,0.00005632407,0.0003145104,0.0000017138091,0.00013285488,0.0000054074103,0.9965373],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991006,0.000044738572,0.00015180174,0.00022118827,0.00017907648,0.00030257186],"domain_scores_gemma":[0.9995177,0.00004029501,0.000025347603,0.00022799977,0.000020509478,0.00016816052],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014537392,0.00012783257,0.00017443358,0.000034355446,0.000102963684,0.000092914204,0.00023812377,0.000050379265,0.9995586],"category_scores_gemma":[0.000009673398,0.00010771549,0.000039473576,0.00012915154,0.000026364038,0.00012979952,0.000010078081,0.00005242795,0.99864686],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007370591,0.000016418968,0.0000019888844,0.0000075042653,0.000016839302,0.000010463847,0.00002452289,0.00083914184,0.000062136416,0.0000015483679,0.27768672,0.72125906],"study_design_scores_gemma":[0.00010485623,0.000108481254,0.00071198674,0.0000070979772,0.0000119747265,0.000002994425,4.4701088e-7,0.00014618608,0.00012503697,0.000043395652,0.99857295,0.00016461308],"about_ca_topic_score_codex":0.00072058395,"about_ca_topic_score_gemma":0.00000650409,"teacher_disagreement_score":0.7210944,"about_ca_system_score_codex":0.0000014309458,"about_ca_system_score_gemma":0.00001967417,"threshold_uncertainty_score":0.439251},"labels":[],"label_agreement":null},{"id":"W4406530252","doi":"10.1016/0967-0653(95)90572-g","title":"10.1016/0967-0653(95)90572-g","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Subduction; Geology; Seismology; Tectonics","score_opus":0.005320601203518116,"score_gpt":0.1530247095182842,"score_spread":0.14770410831476607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406530252","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010051668,0.00011263453,1.8786727e-7,0.00011027695,0.000009462773,0.00013681281,0.00017637043,0.000080419784,0.9893222],"genre_scores_gemma":[0.0030971537,9.1631097e-7,0.00008368921,0.000049253977,0.0003063524,0.000001797318,0.00013427825,0.000005411146,0.99632114],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99910086,0.000045872646,0.00015222868,0.00022168514,0.0001788847,0.00030045043],"domain_scores_gemma":[0.99951917,0.000041301242,0.000025519514,0.0002256953,0.000020454767,0.00016788369],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014932167,0.00012794088,0.00017585472,0.000027065878,0.000101847465,0.00009231518,0.00023604292,0.000050345654,0.9994677],"category_scores_gemma":[0.0000096394415,0.000107364096,0.000039972016,0.00012839708,0.000026113941,0.00012777065,0.000009982267,0.000052037012,0.9986039],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008397482,0.000017894732,0.0000025781496,0.000008299103,0.000018341374,0.000013344567,0.00001988892,0.00088405795,0.000055874025,0.0000016842448,0.2957793,0.7031148],"study_design_scores_gemma":[0.000115343515,0.00010710766,0.0008485213,0.000007283299,0.000012559872,0.0000030093238,4.351433e-7,0.00018300128,0.00010606697,0.000042913398,0.9984096,0.00016411045],"about_ca_topic_score_codex":0.0007434362,"about_ca_topic_score_gemma":0.000006339791,"teacher_disagreement_score":0.70295066,"about_ca_system_score_codex":0.0000013963561,"about_ca_system_score_gemma":0.000019325567,"threshold_uncertainty_score":0.43781808},"labels":[],"label_agreement":null},{"id":"W4406557755","doi":"10.1016/0967-0653(93)93836-g","title":"10.1016/0967-0653(93)93836-g","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Plume; Geology; Mantle (geology); Mantle plume; Geochemistry; Paleontology; Geography; Meteorology; Tectonics","score_opus":0.00484750526709518,"score_gpt":0.1486513858233058,"score_spread":0.14380388055621063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406557755","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008785143,0.000060354818,2.2121144e-7,0.00012687371,0.00000963197,0.00013276529,0.00017203242,0.00008015985,0.99063283],"genre_scores_gemma":[0.0031711976,4.6681404e-7,0.00008849636,0.000055735934,0.0003206625,0.0000017666933,0.00013566988,0.000005408966,0.9962206],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99910235,0.000044412056,0.00015145371,0.00022099503,0.00017881831,0.00030194773],"domain_scores_gemma":[0.99951845,0.00003997012,0.000025266643,0.0002278057,0.00002042044,0.00016807966],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014333928,0.00012805291,0.00017359143,0.000034215907,0.00010254261,0.00009213023,0.00023737509,0.00005035159,0.99948394],"category_scores_gemma":[0.00000953963,0.00010761176,0.00003944767,0.0001284919,0.000026316551,0.00012843704,0.000010052421,0.00005200575,0.9986264],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007684862,0.000017064289,0.0000021805458,0.000007628431,0.000017426872,0.000010416293,0.00002645313,0.00089447,0.00006522481,0.0000017234032,0.23306231,0.76581824],"study_design_scores_gemma":[0.000104777864,0.000108379005,0.0007102089,0.0000069099347,0.000011845112,0.0000030380784,4.902444e-7,0.00015315386,0.00013616767,0.000042606684,0.99855787,0.0001645362],"about_ca_topic_score_codex":0.0007127463,"about_ca_topic_score_gemma":0.0000063271195,"teacher_disagreement_score":0.7656537,"about_ca_system_score_codex":0.0000014099443,"about_ca_system_score_gemma":0.000019096202,"threshold_uncertainty_score":0.43882802},"labels":[],"label_agreement":null},{"id":"W4406618462","doi":"10.3847/1538-3881/ad9f26","title":"Lessons from the High-resolution Spectroscopy of AW UMa and ϵ CrA: Is the Lucy Model Valid?","year":2025,"lang":"en","type":"article","venue":"The Astronomical Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Physics; Spectroscopy; High resolution; Astronomy; Astrophysics; Remote sensing; Geography","score_opus":0.014360304959114473,"score_gpt":0.24152914823886992,"score_spread":0.22716884327975545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406618462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98124003,0.0003447115,0.0036777358,0.013825165,0.00033229066,0.00008382755,0.0001973402,0.0000043248224,0.00029459898],"genre_scores_gemma":[0.99831814,0.00007257189,0.0009426634,0.00022585606,0.0003430293,5.09179e-7,0.0000076105052,0.0000020099217,0.000087640445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9992231,0.0001475822,0.00020934042,0.000109051616,0.00011999229,0.00019092334],"domain_scores_gemma":[0.9993496,0.00026277092,0.000118648124,0.00020597299,0.000019910485,0.000043086377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042899093,0.00009117428,0.00015439674,0.00001336116,0.00038854545,0.0001477335,0.00041606405,0.000030996336,0.00032585024],"category_scores_gemma":[0.000013102243,0.000039476537,0.00006262864,0.000044467655,0.00018792675,0.000080781625,0.000045883182,0.00020901121,0.00002020715],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022947213,0.00024288756,0.18165962,0.000037172274,0.001966675,0.000004124107,0.005526891,0.4349699,0.10863379,0.08249831,0.112407945,0.06975795],"study_design_scores_gemma":[0.0006020791,0.000078455916,0.83637565,0.000044666656,0.00020484568,0.000004380541,0.00022110973,0.0665923,0.0064059915,0.08692374,0.0024173683,0.00012941638],"about_ca_topic_score_codex":0.0015795806,"about_ca_topic_score_gemma":0.000105898784,"teacher_disagreement_score":0.654716,"about_ca_system_score_codex":0.0000038127725,"about_ca_system_score_gemma":0.000068448215,"threshold_uncertainty_score":0.35678315},"labels":[],"label_agreement":null},{"id":"W4406916531","doi":"10.1029/2024jb030213","title":"Alteration's Control on Frictional Behavior and the Depth of the Ductile Shear Zone in Geothermal Reservoirs in Volcanic Arcs","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"European Research Council","keywords":"Shear zone; Geology; Geothermal gradient; Volcano; Shear (geology); Petrology; Geotechnical engineering; Seismology; Tectonics; Paleontology","score_opus":0.017864841676313775,"score_gpt":0.294906595479753,"score_spread":0.2770417538034392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406916531","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965837,0.00012350695,0.00001498779,0.0020311712,0.00026606832,0.00032595155,0.00003323145,0.0000015140969,0.00061985035],"genre_scores_gemma":[0.99925077,0.00007028589,0.00002085109,0.000093683295,0.00023850074,0.0000047449234,0.0000017711781,0.000002795232,0.0003165856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975698,0.00080103456,0.00042009313,0.00014242982,0.0007551277,0.0003115357],"domain_scores_gemma":[0.99841195,0.0010033842,0.00013188376,0.00019079511,0.00019155473,0.00007044207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019013915,0.0000951713,0.0003397168,0.0001868453,0.00015592675,0.00007958732,0.0003427734,0.000049741477,0.00013193503],"category_scores_gemma":[0.00031566533,0.000050589202,0.00009213036,0.00046749244,0.00032197143,0.0001657128,0.000039698425,0.0006110484,0.00001168863],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.02305886,0.002979297,0.6801029,0.00040493545,0.00057749596,0.00033919088,0.004900063,0.13994505,0.03844739,0.066411875,0.004495274,0.038337704],"study_design_scores_gemma":[0.0020318157,0.00027291387,0.98852545,0.0001035189,0.000013061706,0.000004188932,0.000093894276,0.004229305,0.00067947427,0.0033526176,0.0006431356,0.000050618582],"about_ca_topic_score_codex":0.0034203934,"about_ca_topic_score_gemma":0.0025865897,"teacher_disagreement_score":0.30842257,"about_ca_system_score_codex":0.00000771567,"about_ca_system_score_gemma":0.00024187237,"threshold_uncertainty_score":0.51706344},"labels":[],"label_agreement":null},{"id":"W4407357763","doi":"10.1029/2024gc011724","title":"The Lithosphere‐Asthenosphere System Beneath the North Atlantic and Surroundings: Results From Multi‐Observable Probabilistic Inversions","year":2025,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Asthenosphere; Lithosphere; Observable; Probabilistic logic; Geophysics; Seismology; Tectonics","score_opus":0.009197390489564765,"score_gpt":0.18680575899028945,"score_spread":0.17760836850072467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407357763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99212724,0.001184807,0.000036418507,0.00026306018,0.001158858,0.0006584016,0.0013745786,0.000120293764,0.0030763191],"genre_scores_gemma":[0.9960896,0.000086761094,0.000078853394,0.00004613397,0.0004267649,0.000023995122,0.0007234387,0.000010485056,0.0025140184],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99752134,0.00018002554,0.0006131561,0.0006772895,0.00038293525,0.00062527764],"domain_scores_gemma":[0.99725467,0.001063724,0.00033987826,0.0010135524,0.00017499874,0.00015316886],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00056136854,0.00038279622,0.00045244614,0.000010571658,0.0014723988,0.0006330002,0.0007888637,0.00014238487,0.000035129997],"category_scores_gemma":[0.00013881536,0.00023078104,0.00011718149,0.00037853455,0.00022760704,0.00015242139,0.0001336687,0.00026687206,0.00011834978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018308458,0.00047209964,0.8943787,0.006858527,0.0028344735,0.0001945499,0.006330475,0.020719709,0.008229659,0.0106547,0.03660159,0.0108946515],"study_design_scores_gemma":[0.0068881367,0.00025866597,0.64324707,0.003549591,0.0014233475,0.00005051096,0.01670326,0.17622922,0.002513396,0.008995346,0.13706346,0.0030779678],"about_ca_topic_score_codex":0.05490454,"about_ca_topic_score_gemma":0.00800313,"teacher_disagreement_score":0.25113162,"about_ca_system_score_codex":0.0000223415,"about_ca_system_score_gemma":0.0001671507,"threshold_uncertainty_score":0.99982756},"labels":[],"label_agreement":null},{"id":"W4407395835","doi":"10.1139/cjes-2024-0121","title":"Structure and serpentinization of the northern Cascadia mantle wedge corner from receiver function modelling","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Statistics Canada; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Receiver function; Mantle (geology); Seismology; Mantle wedge; Wedge (geometry); Subduction; Geophysics; Lithosphere; Geometry; Tectonics","score_opus":0.010253332717250624,"score_gpt":0.17613973119397197,"score_spread":0.16588639847672135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407395835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967564,0.0006191151,0.0002217288,0.00015551763,0.001294528,0.00004691396,0.00011042763,9.622669e-7,0.0007944415],"genre_scores_gemma":[0.9995241,0.000017991588,0.00014662347,0.00007826561,0.00007346274,2.7863239e-8,0.000003910706,8.2411435e-7,0.00015476704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994544,0.000044595203,0.00016680775,0.00008931409,0.0001225704,0.00012232982],"domain_scores_gemma":[0.9995656,0.000038261558,0.00014521166,0.00006343667,0.00009145527,0.000096008036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019934768,0.00005383334,0.00010458213,0.000084999665,0.00024389535,0.00008953223,0.00018102679,0.000033125907,0.00058217894],"category_scores_gemma":[0.000021838714,0.00003312528,0.000026062948,0.00024208768,0.00015206855,0.0001991833,0.0000041832313,0.000060522747,0.000002742975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010858748,0.0000012839782,0.8922569,0.000008809293,0.000021564938,0.0000023461714,0.00042450763,0.10376567,0.0004192414,0.00023031069,0.00013705238,0.0027214705],"study_design_scores_gemma":[0.00011791668,0.00003934719,0.981328,0.00006628267,0.000035344274,0.0000038966627,0.00013956151,0.0090109855,0.0008401086,0.004662775,0.0036944812,0.00006126652],"about_ca_topic_score_codex":0.04021245,"about_ca_topic_score_gemma":0.36242956,"teacher_disagreement_score":0.3222171,"about_ca_system_score_codex":6.8509814e-7,"about_ca_system_score_gemma":0.00044555616,"threshold_uncertainty_score":0.96617883},"labels":[],"label_agreement":null},{"id":"W4408422897","doi":"10.5194/egusphere-egu25-2878","title":"The heat flux through the cores of small terrestrial planetary bodies from electrical resistivity measurements of liquid Fe-S-Si at high pressures","year":2025,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Electrical resistivity and conductivity; Flux (metallurgy); High heat; Materials science; Heat flux; Astrobiology; Geology; Geophysics; Physics; Mechanics; Heat transfer; Composite material; Metallurgy","score_opus":0.040642921570755275,"score_gpt":0.23941020005106153,"score_spread":0.19876727848030626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408422897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9713967,0.0080213435,0.00006156366,0.00070968934,0.004041273,0.0012676439,0.00616259,0.00006629057,0.008272934],"genre_scores_gemma":[0.99464095,0.0007846819,0.0005794523,0.00009668491,0.00065589545,0.000014458603,0.0017026188,0.000008063652,0.0015171714],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99640745,0.0008007344,0.0008648532,0.0006223149,0.000839426,0.0004652256],"domain_scores_gemma":[0.9963563,0.0019883784,0.00044600022,0.0010225041,0.00011603894,0.000070768205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007470401,0.00044914667,0.00092815136,0.000047047022,0.00042224326,0.000119817276,0.0013833331,0.0003265291,0.00048052164],"category_scores_gemma":[0.000231461,0.00023647552,0.00024990816,0.000092328635,0.00041356738,0.00006708214,0.0004767781,0.00037955376,0.000015671345],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.084389314,0.0013914126,0.27627927,0.0034571544,0.020301495,0.000095748575,0.0066376654,0.14185028,0.053458888,0.0029286102,0.38758707,0.021623097],"study_design_scores_gemma":[0.0023956231,0.0013733008,0.718314,0.00085112924,0.0021385434,0.0000026456567,0.000092065944,0.0022360187,0.18714797,0.025329355,0.058566444,0.0015529217],"about_ca_topic_score_codex":0.18767068,"about_ca_topic_score_gemma":0.04998477,"teacher_disagreement_score":0.44203472,"about_ca_system_score_codex":0.000009141342,"about_ca_system_score_gemma":0.00027482316,"threshold_uncertainty_score":0.96735054},"labels":[],"label_agreement":null},{"id":"W4408444312","doi":"10.5194/egusphere-egu25-915","title":"Is the mantle transition zone uniform beneath Precambrian shields?","year":2025,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transition zone; Precambrian; Geology; Mantle (geology); Discontinuity (linguistics); Shields; Core–mantle boundary; Classification of discontinuities; Baltic Shield; Shield; Geophysics; Petrology; Geochemistry","score_opus":0.014473332887121123,"score_gpt":0.21963148381007003,"score_spread":0.2051581509229489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408444312","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43991575,0.0012428656,0.009023625,0.015672887,0.008132359,0.0023681403,0.00987055,0.00035441405,0.5134194],"genre_scores_gemma":[0.97781885,0.0003501721,0.000748561,0.0020012727,0.0005387731,0.000008215363,0.0011125313,0.000004447013,0.017417198],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99883914,0.00006797575,0.00024661212,0.00036354392,0.00022996572,0.00025275588],"domain_scores_gemma":[0.99925447,0.00007358731,0.00008314361,0.0004866815,0.000039732186,0.000062396626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027826437,0.00021931854,0.00027020468,0.00004980408,0.0001799896,0.00021845683,0.00045641878,0.00022474889,0.008880408],"category_scores_gemma":[0.0000038289186,0.00013539872,0.00013276472,0.00008819174,0.000045423803,0.000080950085,0.0000634546,0.00024657813,0.0003378543],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010416725,0.0004717896,0.0076393913,0.0056145526,0.0030605705,0.00013343904,0.027872397,0.12351926,0.0010664861,0.047669344,0.34982356,0.43208754],"study_design_scores_gemma":[0.001577063,0.0004638165,0.18407673,0.0011283784,0.0012558448,0.000018606635,0.0011715746,0.06052551,0.015010331,0.0815768,0.6501381,0.003057245],"about_ca_topic_score_codex":0.017346831,"about_ca_topic_score_gemma":0.0059980596,"teacher_disagreement_score":0.5379031,"about_ca_system_score_codex":0.000002457649,"about_ca_system_score_gemma":0.00009938939,"threshold_uncertainty_score":0.9920256},"labels":[],"label_agreement":null},{"id":"W4408967685","doi":"10.22541/essoar.174326672.28941810/v1","title":"The role of dislocations in the anelasticity of the upper mantle","year":2025,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"","keywords":"Geology; Mantle (geology); Dislocation; Geophysics; Condensed matter physics; Physics","score_opus":0.006994165136135152,"score_gpt":0.2072778669705415,"score_spread":0.20028370183440636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408967685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9045089,0.0006333361,0.000062440566,0.0013665387,0.0010745287,0.00062457327,0.0010158743,0.000008045154,0.09070579],"genre_scores_gemma":[0.999026,0.00007149257,0.000039269642,0.000042965952,0.000039304738,0.000003939371,0.000026110916,7.38966e-7,0.0007501958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923813,0.00015513356,0.00021922322,0.00011245911,0.00017059786,0.00010446482],"domain_scores_gemma":[0.99901664,0.000381445,0.00011301019,0.00044348184,0.000035907007,0.000009523359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034994728,0.000078520774,0.00013951135,0.0000171096,0.0000983147,0.00003429031,0.0007431891,0.000055993263,0.00030040732],"category_scores_gemma":[0.000041388634,0.00002989273,0.00006627848,0.00010193417,0.000109374174,0.000016977643,0.00010628295,0.00012850588,0.000009195342],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011869593,0.000300341,0.653255,0.00070198084,0.0003191882,0.0000012899076,0.007840903,0.091563284,0.0016899778,0.21065389,0.0058767865,0.02767865],"study_design_scores_gemma":[0.000054916203,0.000013098457,0.9301807,0.00007171123,0.000047274767,3.000187e-7,0.00056538783,0.0026319122,0.002791532,0.051429566,0.012128931,0.00008463393],"about_ca_topic_score_codex":0.0126706315,"about_ca_topic_score_gemma":0.0073876074,"teacher_disagreement_score":0.2769257,"about_ca_system_score_codex":7.5011366e-7,"about_ca_system_score_gemma":0.0000896638,"threshold_uncertainty_score":0.99390405},"labels":[],"label_agreement":null},{"id":"W4409218598","doi":"10.1103/physrevd.111.l081901","title":"Dressing factors for mixed-flux <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi>AdS</mml:mi> </mml:mrow> <mml:mrow> <mml:mn>3</mml:mn> </mml:mrow> </mml:msub> <mml:mo>×</mml:mo> <mml:msup> <mml:mrow> <mml:mi>S</mml:mi> </mml:mrow> <mml:mrow> <mml:mn>3</mml:mn> </mml:mrow> </mml:msup> <mml:mo>×</mml:mo> <mml:msup> <mml:mrow> <mml:mi>T</mml:mi> </mml:mrow> <mml:mrow> <mml:mn>4</mml:mn> </mml:mrow> </mml:msup> </mml:mrow> </mml:math> superstrings","year":2025,"lang":"lv","type":"article","venue":"Physical review. D/Physical review. D.","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trinity College","funders":"NextGenerationEU; Instituto Nazionale di Fisica Nucleare; Fondazione Cariplo; Università degli Studi di Padova; Deutsche Forschungsgemeinschaft; Fondazione Cassa di Risparmio di Padova e Rovigo","keywords":"Computer science","score_opus":0.018700435561180936,"score_gpt":0.2847188212198074,"score_spread":0.26601838565862646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409218598","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32509813,0.014695468,0.0013539712,0.003442543,0.010629109,0.0003745509,0.00411175,0.0011467418,0.6391477],"genre_scores_gemma":[0.93193144,0.021602282,0.0037614962,0.0069883685,0.011090829,0.0066239005,0.01289721,0.0036640563,0.0014404453],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.95583653,0.0034824442,0.008993941,0.008996027,0.011022712,0.011668329],"domain_scores_gemma":[0.9640632,0.009401156,0.009373503,0.009401624,0.0012128734,0.0065476443],"candidate_categories":["metaresearch","metaepi_narrow","metaepi_broad","sts","scholarly_communication","open_science","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","sts","open_science","research_integrity","insufficient_payload"],"category_scores_codex":[0.008093576,0.0051372256,0.0025574067,0.0024454305,0.006975317,0.0076028053,0.0117627,0.008275145,0.76277274],"category_scores_gemma":[0.009613695,0.009693397,0.01188575,0.0069627427,0.008168069,0.0077622677,0.00832251,0.008308631,0.011030795],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004127404,0.0017013922,0.00006594297,0.010312719,0.00643393,0.0034829546,0.0028235049,0.0022162013,0.00851968,0.31240216,0.6385406,0.009373513],"study_design_scores_gemma":[0.0060405126,0.005858359,0.0003247719,0.010491206,0.010960015,0.0031303167,0.003265636,0.01817778,0.88523537,0.0007697662,0.04732032,0.008425955],"about_ca_topic_score_codex":0.0085400455,"about_ca_topic_score_gemma":0.0047557605,"teacher_disagreement_score":0.87671566,"about_ca_system_score_codex":0.00010020616,"about_ca_system_score_gemma":0.0076242094,"threshold_uncertainty_score":0.999698},"labels":[],"label_agreement":null},{"id":"W4409888918","doi":"10.1139/cjes-2025-0007","title":"Geophysical studies of the lithosphere and plate boundaries: special issue in honour of Roy D. Hyndman","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Lithosphere; Honour; Geophysics; Plate tectonics; Seismology; Tectonics; Archaeology","score_opus":0.01324444138968375,"score_gpt":0.2316983182419958,"score_spread":0.21845387685231205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409888918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927213,0.0019136551,9.41142e-7,0.00066756696,0.0013787681,0.000062534404,0.000043408232,6.1604106e-7,0.0032112116],"genre_scores_gemma":[0.9991181,0.00007638222,0.00015524904,0.00006161519,0.00028821078,8.719223e-8,2.7142605e-7,7.759392e-7,0.00029929416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99910057,0.00007803743,0.0003277436,0.00010338044,0.00018277187,0.00020747822],"domain_scores_gemma":[0.9993959,0.00011364381,0.00020840304,0.0000761764,0.00009580934,0.000110071356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006416778,0.0000773267,0.0002893542,0.00011303957,0.00029491226,0.00010456721,0.0003279439,0.000029900102,0.00028482144],"category_scores_gemma":[0.00015953422,0.00004771698,0.00004686949,0.00041294176,0.0013613139,0.00019316797,0.000013192396,0.00010145861,0.0000023083742],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006148291,0.000020795036,0.9628861,0.00016718105,0.000116889445,0.00005634298,0.008676054,0.002675986,0.00043605978,0.0059753074,0.0032209167,0.015706861],"study_design_scores_gemma":[0.00020454191,0.00018772206,0.9562151,0.00026487364,0.000020351137,0.00000835106,0.0018727838,0.00007647311,0.0011372714,0.0068030898,0.03313189,0.00007756681],"about_ca_topic_score_codex":0.024732877,"about_ca_topic_score_gemma":0.32110268,"teacher_disagreement_score":0.29636982,"about_ca_system_score_codex":0.0000011508756,"about_ca_system_score_gemma":0.0012428022,"threshold_uncertainty_score":0.9817615},"labels":[],"label_agreement":null},{"id":"W4409951988","doi":"10.1038/s41467-025-58255-x","title":"Taking three-dimensional x-ray diffraction (3DXRD) from the synchrotron to the laboratory scale","year":2025,"lang":"en","type":"article","venue":"Nature Communications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor; PROTO Manufacturing (Canada)","funders":"Lawrence Livermore National Laboratory; Basic Energy Sciences; National Science Foundation; Division of Civil, Mechanical and Manufacturing Innovation; Division of Materials Research; U.S. Department of Energy","keywords":"Synchrotron; Diffraction; Scale (ratio); X-ray crystallography; Crystallography; Physics; Computer science; Optics; Chemistry","score_opus":0.010875746644288585,"score_gpt":0.25399003685664506,"score_spread":0.24311429021235648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409951988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.887039,0.015660912,0.00022471287,0.08436443,0.002956303,0.000865391,0.0013863071,0.00012025395,0.007382681],"genre_scores_gemma":[0.9947187,0.00005587357,0.0012693743,0.0034055023,0.00018452088,0.000012061711,0.00026300503,0.0000027265617,0.00008827263],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99919546,0.00021058846,0.00014122871,0.0001482735,0.000169068,0.00013540835],"domain_scores_gemma":[0.997666,0.0008115855,0.000083375075,0.0013070466,0.00009806667,0.000033896522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031508697,0.00009140088,0.00009923001,0.000025842402,0.0009191366,0.000118949094,0.0011497944,0.00010998622,0.00032745517],"category_scores_gemma":[0.00011411295,0.000051330757,0.000037290218,0.00033991985,0.00008183759,0.000099853256,0.00013040946,0.00047876587,0.00020450455],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024644323,0.00037702124,0.34051973,0.00003273764,0.0006716032,0.0000032588105,0.0024562466,0.027512211,0.035538774,0.029089777,0.45750698,0.10604521],"study_design_scores_gemma":[0.000053187734,0.0000061680316,0.7056096,0.000023707282,0.000027999542,1.131412e-7,0.0000359896,0.001315436,0.00009215375,0.0006257941,0.29215258,0.000057270176],"about_ca_topic_score_codex":0.0038055168,"about_ca_topic_score_gemma":0.051303048,"teacher_disagreement_score":0.36508986,"about_ca_system_score_codex":0.000005726038,"about_ca_system_score_gemma":0.00007206435,"threshold_uncertainty_score":0.9660082},"labels":[],"label_agreement":null},{"id":"W4410098741","doi":"10.1080/08957959.2025.2498496","title":"Brillouinview for Brillouin spectroscopy data processing and single crystal elasticity modelling","year":2025,"lang":"en","type":"article","venue":"High Pressure Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds de recherche du Québec – Nature et technologies; National Coordination Office; National Aeronautics and Space Administration","keywords":"Brillouin Spectroscopy; Elasticity (physics); Spectroscopy; Materials science; Single crystal; Brillouin scattering; Biological system; Crystallography; Optics; Chemistry; Physics; Composite material; Laser","score_opus":0.10920787472072511,"score_gpt":0.3459684469859749,"score_spread":0.23676057226524977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410098741","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.70289093,0.052211564,0.20763718,0.0029995178,0.002086371,0.0051963422,0.0069913375,0.00040428303,0.019582478],"genre_scores_gemma":[0.990515,0.00031323248,0.0070707677,0.000046282126,0.00036928142,0.000009184596,0.0003593001,0.000010605314,0.0013063615],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99754906,0.00021730376,0.00029114648,0.0007351304,0.0004932348,0.0007141115],"domain_scores_gemma":[0.99845093,0.00054313184,0.000062613486,0.00057011424,0.00022875979,0.00014447296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016461036,0.00018276882,0.00035699966,0.00015144605,0.00061012525,0.00053257315,0.00065892015,0.00011771421,0.00021833497],"category_scores_gemma":[0.00016215439,0.00015698935,0.000030930103,0.00033912197,0.00021833071,0.000431316,0.00023253028,0.00022904116,0.000018477966],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005340266,0.0013821878,0.034547996,0.030741652,0.0021851405,0.00014081266,0.0025077562,0.1854718,0.28405055,0.044466097,0.15681352,0.2523522],"study_design_scores_gemma":[0.0013425874,0.00045668913,0.009806749,0.00074485684,0.00026369782,0.000008360457,0.0000910907,0.49712434,0.012285107,0.031341497,0.44584447,0.0006905336],"about_ca_topic_score_codex":0.0028101557,"about_ca_topic_score_gemma":0.00041559542,"teacher_disagreement_score":0.31165254,"about_ca_system_score_codex":0.0000039558263,"about_ca_system_score_gemma":0.00017273519,"threshold_uncertainty_score":0.640184},"labels":[],"label_agreement":null},{"id":"W4410111538","doi":"10.1029/2024jb030712","title":"Mapping Crustal Vp/Vs in North America With a Machine Learning Approach","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Artificial intelligence; Computer science","score_opus":0.02244884239106559,"score_gpt":0.28187942337199123,"score_spread":0.25943058098092564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410111538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932984,0.0001888066,0.00047750375,0.00030471443,0.0001114077,0.00019744907,0.000025826337,0.000012155456,0.005383752],"genre_scores_gemma":[0.9974235,0.00014678758,0.0011152332,0.000068237845,0.00031110755,0.0000019155184,0.000030142002,0.0000066347484,0.0008964181],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970257,0.0005132435,0.00046480325,0.00027274727,0.0010078282,0.0007156396],"domain_scores_gemma":[0.998647,0.00041523515,0.00019015105,0.00019248767,0.00031632438,0.00023883095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009914447,0.00018275039,0.0005866244,0.00052329554,0.00024285229,0.00020081636,0.00045784464,0.000058705547,0.00020207725],"category_scores_gemma":[0.00024141949,0.00012550803,0.00010989876,0.0015622275,0.00024463554,0.00033587072,0.00006742052,0.0012222921,0.000085546766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0061883796,0.0014997752,0.6529785,0.00082715787,0.00076151476,0.0015378721,0.005775883,0.19680072,0.004813201,0.0007361763,0.0018004795,0.12628035],"study_design_scores_gemma":[0.001422788,0.0017301132,0.9274106,0.00021574496,0.000018893767,0.00002332206,0.00068734866,0.038987968,0.00026856404,0.00080320286,0.02814441,0.00028702794],"about_ca_topic_score_codex":0.0032124352,"about_ca_topic_score_gemma":0.0009368243,"teacher_disagreement_score":0.27443212,"about_ca_system_score_codex":0.000009942454,"about_ca_system_score_gemma":0.00035951848,"threshold_uncertainty_score":0.5310319},"labels":[],"label_agreement":null},{"id":"W4410147088","doi":"10.1029/2024jb030831","title":"The Heterogeneous Mantle Transition Zone Beneath the Tarim Craton and Adjacent Region: Insight Into the Thermal Processes by the Cenozoic Reactivation","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Craton; Transition zone; Geology; Cenozoic; Mantle (geology); Tarim basin; Geophysics; Paleontology; Tectonics","score_opus":0.01846860517254584,"score_gpt":0.27601716817935407,"score_spread":0.25754856300680823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410147088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9771002,0.0027341826,0.00011737328,0.018857097,0.00023165577,0.0003745005,0.000015353982,0.000006544926,0.00056308036],"genre_scores_gemma":[0.99667466,0.0020631866,0.000008824771,0.00031150677,0.0005174669,0.0000052787623,0.000010926601,0.0000049779283,0.00040316366],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99757653,0.0007011153,0.00032594596,0.00017808941,0.0008313627,0.00038696598],"domain_scores_gemma":[0.9975297,0.0014963252,0.00017105718,0.000298395,0.0004137577,0.000090785376],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0014234252,0.00014431406,0.00020984522,0.00004487056,0.0016322351,0.0005080759,0.0005725881,0.000056818597,0.000030442365],"category_scores_gemma":[0.0001869944,0.000053333006,0.00008205224,0.0004485534,0.0005164681,0.00026242185,0.000050108432,0.0005904002,0.000014189844],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0073599643,0.0010292972,0.0027167958,0.0006060223,0.0017908892,0.00025238853,0.048196282,0.012432276,0.10280837,0.0069362298,0.03556827,0.78030324],"study_design_scores_gemma":[0.0023270987,0.003563514,0.24899209,0.0006281325,0.0003229681,0.00020212037,0.0037559248,0.011354604,0.118440054,0.034703795,0.57499033,0.0007193692],"about_ca_topic_score_codex":0.002027773,"about_ca_topic_score_gemma":0.0010129507,"teacher_disagreement_score":0.7795839,"about_ca_system_score_codex":0.0000075979847,"about_ca_system_score_gemma":0.00024517518,"threshold_uncertainty_score":0.9996675},"labels":[],"label_agreement":null},{"id":"W4410621472","doi":"10.1038/s41561-025-01703-6","title":"Direct observations of transient weakening during phase transformations in quartz and olivine","year":2025,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"","keywords":"Olivine; Quartz; Geology; Transient (computer programming); Phase (matter); Geophysics; Mineralogy; Physics; Paleontology","score_opus":0.007212672397467048,"score_gpt":0.23711824299737597,"score_spread":0.22990557059990893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410621472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966062,0.000545856,0.00018264614,0.00034351848,0.00028109405,0.00013988889,0.00015381117,0.000015207353,0.0017317849],"genre_scores_gemma":[0.9991783,0.00006071004,0.0005098771,0.000057656038,0.000016299613,0.0000018076657,0.000019107936,8.334161e-7,0.0001554437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992797,0.000029920899,0.00020304145,0.00016764305,0.00014515671,0.00017456897],"domain_scores_gemma":[0.9997158,0.00007496837,0.000039432,0.00009915378,0.0000319624,0.000038684466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002453099,0.000074210024,0.00014287805,0.00013983218,0.00013818101,0.000033361805,0.00013725925,0.00006467576,0.0000499611],"category_scores_gemma":[0.000041586274,0.000062400686,0.000022192255,0.00060983736,0.00007763742,0.0002934016,0.0000055041874,0.000119133314,0.000001371284],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029322857,0.00051443523,0.48732197,0.0010374589,0.00005677965,0.000025541025,0.010141003,0.011220692,0.4444326,0.011584293,0.0003315991,0.033040397],"study_design_scores_gemma":[0.00046994176,0.00003617874,0.9908066,0.00008021587,0.000009608456,0.0000011974557,0.00007649066,0.0027403398,0.0037972885,0.0002084405,0.0016921673,0.00008153427],"about_ca_topic_score_codex":0.000707757,"about_ca_topic_score_gemma":0.00175807,"teacher_disagreement_score":0.5034846,"about_ca_system_score_codex":0.0000020148764,"about_ca_system_score_gemma":0.00004632241,"threshold_uncertainty_score":0.2544626},"labels":[],"label_agreement":null},{"id":"W4410944116","doi":"10.1016/j.jnoncrysol.2025.123668","title":"Universal correlation between boson peak and quasi-localized modes in solids","year":2025,"lang":"en","type":"article","venue":"Journal of Non-Crystalline Solids","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Outstanding Youth Science Fund Project of National Natural Science Foundation of China; China Postdoctoral Science Foundation; National Natural Science Foundation of China; Canadian Anesthesiologists' Society","keywords":"Boson; Correlation; Physics; Statistical physics; Theoretical physics; Condensed matter physics; Quantum mechanics; Mathematics; Geometry","score_opus":0.00929836340688944,"score_gpt":0.24083402461945283,"score_spread":0.2315356612125634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410944116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9835802,0.00029226206,0.013553134,0.00038500052,0.00032264224,0.000106391715,0.000045170877,0.000008196695,0.001707046],"genre_scores_gemma":[0.9980617,0.00017993487,0.0010249288,0.00005454621,0.00030442595,1.7378315e-7,0.000029420227,0.0000038666053,0.00034099072],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99881727,0.00010153262,0.0005050869,0.00013528863,0.00022017899,0.00022062847],"domain_scores_gemma":[0.9993199,0.0001534094,0.00023909198,0.00009502,0.000090439244,0.00010213759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005378401,0.00013977851,0.0004137183,0.00023807016,0.000076719225,0.00007971191,0.00014428704,0.00010241294,0.000132763],"category_scores_gemma":[0.00003707983,0.0001155379,0.00007096918,0.00022105167,0.00006282469,0.0003431874,0.000020871037,0.00020576852,0.0000073542374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020265235,0.0003629629,0.79641753,0.00052183843,0.00060301315,0.00047519742,0.0027175385,0.13043745,0.02634697,0.0019871776,0.0063459715,0.031757813],"study_design_scores_gemma":[0.0054852995,0.00096453825,0.8125838,0.0005919935,0.00030067956,0.00004333595,0.0008062515,0.14766209,0.000910454,0.011816048,0.01826785,0.00056766236],"about_ca_topic_score_codex":0.0006930041,"about_ca_topic_score_gemma":0.00022758654,"teacher_disagreement_score":0.031190151,"about_ca_system_score_codex":0.000010108341,"about_ca_system_score_gemma":0.00012977267,"threshold_uncertainty_score":0.4711499},"labels":[],"label_agreement":null},{"id":"W4410963716","doi":"10.1063/5.0260921","title":"Evaluating nonlocal heat transport in directly driven chromium spheres using x-ray spectroscopy","year":2025,"lang":"en","type":"article","venue":"Physics of Plasmas","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"U.S. Department of Energy","keywords":"Physics; SPHERES; Chromium; Spectroscopy; X-ray spectroscopy; Plasma; Atomic physics; Computational physics; Nuclear physics; Quantum mechanics; Astronomy","score_opus":0.027199170981423392,"score_gpt":0.29228813012432114,"score_spread":0.26508895914289776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410963716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99449706,0.00008977203,0.0011213579,0.000032837725,0.00052813516,0.0001944282,0.00011475772,0.000022326232,0.003399325],"genre_scores_gemma":[0.99300385,0.000011288835,0.0066835205,0.000024981811,0.0001583018,0.0000013625531,0.000059449936,0.0000053251447,0.000051900537],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.998779,0.000071784045,0.00032346466,0.0002759066,0.0002478408,0.00030201842],"domain_scores_gemma":[0.99952054,0.00012362683,0.000073744486,0.00019378672,0.000040775558,0.000047533278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020181433,0.00016639117,0.00038267343,0.000049258,0.000074390264,0.000025878162,0.00020802049,0.000055356435,0.00030529307],"category_scores_gemma":[0.000013442014,0.00015471406,0.00007754986,0.00028915814,0.000077259625,0.00018212502,0.00001332506,0.000107815,0.000023100274],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013464925,0.0000913645,0.094335765,0.00016777984,0.00006520041,0.000009849704,0.0003022356,0.4179167,0.48418984,0.0006288378,0.00006138168,0.0020964202],"study_design_scores_gemma":[0.0013484308,0.00025093192,0.11863661,0.00038732943,0.00014457839,8.629967e-7,0.00015452187,0.4644747,0.4068616,0.006976842,0.00027905017,0.00048452473],"about_ca_topic_score_codex":0.0059148376,"about_ca_topic_score_gemma":0.0024980647,"teacher_disagreement_score":0.077328235,"about_ca_system_score_codex":0.000008112866,"about_ca_system_score_gemma":0.0001492067,"threshold_uncertainty_score":0.8941505},"labels":[],"label_agreement":null},{"id":"W4411609292","doi":"10.4006/0836-1398-38.2.143","title":"Local variation in the Newtonian gravitational field derived from the elastic energy","year":2025,"lang":"en","type":"article","venue":"Physics Essays","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Physics; Gravitational field; Gravitational energy; Newtonian fluid; Variation (astronomy); Classical mechanics; Gravitation; Mechanics; Astrophysics","score_opus":0.007757841527174735,"score_gpt":0.20450344382767746,"score_spread":0.19674560230050273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411609292","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.39915282,0.0005541852,0.52280915,0.01355137,0.003876377,0.00048407388,0.000573562,0.0000674726,0.058930967],"genre_scores_gemma":[0.99776685,0.000011467205,0.00011307121,0.0016095726,0.00028551233,0.000004916252,0.00016793731,0.0000014616547,0.000039200368],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9993245,0.00013305144,0.00011985208,0.00013657789,0.00015519062,0.00013080455],"domain_scores_gemma":[0.998802,0.0009589131,0.000041392475,0.00016076643,0.000022154496,0.000014790613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001322234,0.00007993862,0.00009076862,0.000011732424,0.00014102735,0.00009172226,0.00026022675,0.00003274361,0.00015998288],"category_scores_gemma":[0.000023773211,0.000046978894,0.000031023166,0.00017385554,0.0000352341,0.00008968104,0.000012206105,0.00007337076,0.000036435136],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000109353874,0.00011159628,0.01727734,0.000021733267,0.00011410214,0.0000094032985,0.0038661943,0.044742264,0.0042780815,0.87167495,0.008625893,0.049169097],"study_design_scores_gemma":[0.00019596543,0.000021438953,0.22672209,0.000017774699,0.000027336358,1.6192197e-7,0.00010410858,0.013123118,0.00042053012,0.7571666,0.0021129067,0.00008792896],"about_ca_topic_score_codex":0.0133799305,"about_ca_topic_score_gemma":0.003208315,"teacher_disagreement_score":0.59861404,"about_ca_system_score_codex":0.0000020110779,"about_ca_system_score_gemma":0.000048956685,"threshold_uncertainty_score":0.99319005},"labels":[],"label_agreement":null},{"id":"W4411635804","doi":"10.1088/1361-648x/ade83d","title":"Pressure-induced reactions in minerals: a condensed matter physics perspective","year":2025,"lang":"en","type":"review","venue":"Journal of Physics Condensed Matter","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Diamondoid; Perspective (graphical); Scale (ratio); Statistical physics; Molecular dynamics; Nanotechnology; Computer science; Physics; Chemistry; Materials science; Artificial intelligence; Computational chemistry","score_opus":0.032479454997332805,"score_gpt":0.29998910737509604,"score_spread":0.26750965237776325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411635804","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0014709273,0.9719574,0.00018405903,0.0005490792,0.004439493,0.0015983327,0.0011895947,0.000040181956,0.018570937],"genre_scores_gemma":[0.02013099,0.9431632,0.0008044493,0.0024586758,0.0075032995,0.000049879025,0.0004372917,0.00017921832,0.025272999],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9961624,0.00059760554,0.0015269093,0.0005447843,0.0005846274,0.00058366026],"domain_scores_gemma":[0.99633956,0.0006523155,0.0017876849,0.00057947,0.00046086346,0.00018010836],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004932923,0.0007276919,0.0027857227,0.00032801213,0.00011613147,0.00027681314,0.0006999602,0.0003709528,0.0033120513],"category_scores_gemma":[0.00004879789,0.0005789387,0.00092058856,0.00058039685,0.000098725206,0.00053373794,0.000059114976,0.0010838403,0.0012663072],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010003691,0.002766413,0.0037377337,0.12053679,0.01631099,0.0019234526,0.00594052,0.003564112,0.0047144573,0.006838749,0.50073457,0.33193183],"study_design_scores_gemma":[0.0019556517,0.00025926623,0.0010191782,0.018794028,0.0042258287,0.00021524286,0.00022465998,0.00005965464,0.0002413166,0.01771528,0.9534935,0.0017964166],"about_ca_topic_score_codex":0.00081663526,"about_ca_topic_score_gemma":0.00006560307,"teacher_disagreement_score":0.45275888,"about_ca_system_score_codex":0.00004763859,"about_ca_system_score_gemma":0.00071689795,"threshold_uncertainty_score":0.9996662},"labels":[],"label_agreement":null},{"id":"W4411946695","doi":"10.1103/hw9y-y2cn","title":"Dynamics of the transition from the metastable tetragonal st12 to the diamond-cubic phase in germanium characterized by neutron spectroscopy","year":2025,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Light Source (Canada)","funders":"Oak Ridge National Laboratory; Office of Science; University of Illinois at Urbana-Champaign; California Institute of Technology; U.S. Department of Energy","keywords":"Tetragonal crystal system; Metastability; Germanium; Materials science; Phase transition; Spectroscopy; Crystallography; Diamond; Neutron spectroscopy; Phase (matter); Neutron; Neutron diffraction; Condensed matter physics; Neutron scattering; Chemistry; Crystal structure; Physics; Optoelectronics; Metallurgy; Nuclear physics; Silicon","score_opus":0.007780184853949873,"score_gpt":0.30314416800290933,"score_spread":0.29536398314895945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411946695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92819434,0.03284772,0.0012347159,0.029201983,0.0005824304,0.0038649787,0.0032481689,0.000034889767,0.00079077616],"genre_scores_gemma":[0.96418613,0.026368825,0.000022330567,0.008172965,0.00049643434,0.000117870106,0.000577215,0.000013419125,0.00004480161],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9969079,0.0008114146,0.0006708126,0.0005231859,0.0005897356,0.0004969449],"domain_scores_gemma":[0.9979577,0.0007046897,0.00029156797,0.0008514787,0.00007263664,0.0001219253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063712517,0.0003936875,0.0012341784,0.000022439204,0.00019097558,0.00007219286,0.001075252,0.000034243614,0.00019325627],"category_scores_gemma":[0.00007414548,0.00018940914,0.0005345775,0.0009701349,0.00016113323,0.00021934735,0.00008341813,0.0004396498,0.0001701745],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007525863,0.0040446892,0.00145653,0.008806042,0.0007695371,0.000013473691,0.000856943,0.00032781114,0.7029203,0.10752393,0.04543628,0.12709187],"study_design_scores_gemma":[0.0056700995,0.0014104289,0.10339648,0.027981201,0.0062915226,0.0000054630764,0.00009648506,0.036695443,0.13847008,0.09291756,0.5840947,0.0029705225],"about_ca_topic_score_codex":0.00074428035,"about_ca_topic_score_gemma":0.0003128348,"teacher_disagreement_score":0.5644502,"about_ca_system_score_codex":0.00002073131,"about_ca_system_score_gemma":0.00009514202,"threshold_uncertainty_score":0.77238804},"labels":[],"label_agreement":null},{"id":"W4412121878","doi":"10.5194/epsc-dps2025-1627","title":"Self-consistent formation and thermochemical evolution of Mars’ basal mantle layer","year":2025,"lang":"en","type":"preprint","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Mars Exploration Program; Mantle (geology); Astrobiology; Geology; Basal (medicine); Earth science; Geochemistry; Physics; Biology","score_opus":0.011124882221677625,"score_gpt":0.2075099217965737,"score_spread":0.1963850395748961,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412121878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95256746,0.00051999267,0.0007087259,0.0001635212,0.0007521217,0.0003491584,0.00043668045,0.00005386204,0.044448473],"genre_scores_gemma":[0.9971193,0.00009984157,0.0021192834,0.00003535753,0.000069006404,0.000002110747,0.00020644671,0.0000013459702,0.00034728344],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992796,0.000046613084,0.00023409992,0.00018293061,0.00013824835,0.00011847805],"domain_scores_gemma":[0.99958557,0.000046226167,0.00010992588,0.00017073548,0.000049837974,0.000037721533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016420023,0.00011771087,0.0002157576,0.000048595102,0.000037199483,0.000037135655,0.00011489523,0.00014767352,0.00066932786],"category_scores_gemma":[0.0000077614895,0.00009148313,0.000049318285,0.000034544435,0.000029735489,0.000070573326,0.00008290384,0.00008929838,0.000022209297],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024009924,0.0015652594,0.33780336,0.056658518,0.004660025,0.00007021775,0.013272814,0.016429173,0.18313089,0.12871064,0.10707184,0.14822626],"study_design_scores_gemma":[0.002014578,0.0003439513,0.5318345,0.0011213659,0.0010038005,0.000020474072,0.00062765734,0.13401422,0.15292767,0.14720114,0.026733372,0.0021573196],"about_ca_topic_score_codex":0.0015023152,"about_ca_topic_score_gemma":0.00015716451,"teacher_disagreement_score":0.1940311,"about_ca_system_score_codex":0.00000467213,"about_ca_system_score_gemma":0.000059645598,"threshold_uncertainty_score":0.73286706},"labels":[],"label_agreement":null},{"id":"W4412403374","doi":"10.1103/l1qh-5c44","title":"Melting curve of tin to 61 GPa: Resolving discrepancies through shock experiments and simulations","year":2025,"lang":"en","type":"article","venue":"Physical review. B./Physical review. B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Association of Emergency Physicians","funders":"National Natural Science Foundation of China","keywords":"Tin; Materials science; Melting curve analysis; Shock (circulatory); Thermodynamics; Mechanics; Physics; Metallurgy; Chemistry; Medicine","score_opus":0.023277273694101364,"score_gpt":0.3761502869712268,"score_spread":0.35287301327712545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412403374","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9125647,0.07381314,0.0013920813,0.0027975643,0.0003471834,0.0021042093,0.00041656895,0.000088190165,0.006476398],"genre_scores_gemma":[0.98172253,0.01505338,0.00060404855,0.002072421,0.0002974835,0.000030935116,0.00009964056,0.000012574709,0.00010697087],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99736345,0.0003117047,0.00072339125,0.0006321168,0.0004919241,0.0004774091],"domain_scores_gemma":[0.9980469,0.000732594,0.0002867433,0.0005883967,0.000150555,0.00019482146],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00037178272,0.00038436157,0.0014257486,0.00004089858,0.00024300431,0.000078286896,0.0004024686,0.00003321937,0.00016137936],"category_scores_gemma":[0.0008403704,0.00028866093,0.000304319,0.0007360423,0.00015891794,0.00035172343,0.00017738527,0.00018841164,0.0001318017],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002153364,0.0021164576,0.030157885,0.054723073,0.0010008088,0.000028516963,0.0043475367,0.0016967846,0.10509452,0.6086368,0.02986592,0.16211636],"study_design_scores_gemma":[0.0015917026,0.0012254842,0.05496542,0.08317743,0.0029364207,0.0000055943324,0.00018436593,0.038133156,0.06093182,0.2542565,0.4990928,0.003499316],"about_ca_topic_score_codex":0.00047849515,"about_ca_topic_score_gemma":0.00006707228,"teacher_disagreement_score":0.46922687,"about_ca_system_score_codex":0.000009381518,"about_ca_system_score_gemma":0.00007255779,"threshold_uncertainty_score":0.99995655},"labels":[],"label_agreement":null},{"id":"W4412900458","doi":"10.1038/s41550-025-02617-4","title":"The role of interior dynamics and differentiation on the surface and in the atmosphere of lava planets","year":2025,"lang":"en","type":"article","venue":"Nature Astronomy","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Montreal Clinical Research Institute; McGill University; York University","funders":"Agence Nationale de la Recherche","keywords":"Astrobiology; Atmosphere (unit); Planet; Lava; Geology; Earth science; Atmospheric sciences; Astronomy; Physics; Meteorology; Paleontology; Volcano","score_opus":0.0017963534125523197,"score_gpt":0.17880641319471427,"score_spread":0.17701005978216194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412900458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967303,0.0008299976,0.00000995775,0.0004234385,0.000090669746,0.00013118215,0.000062031606,0.0000014883226,0.0017209103],"genre_scores_gemma":[0.99981445,0.000024478648,0.000050973184,0.000025887699,0.000012113975,6.165207e-7,0.000022780247,6.9773415e-7,0.000047983835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99965173,0.000055074786,0.00009145669,0.000069485926,0.00006243941,0.00006982805],"domain_scores_gemma":[0.9995533,0.00027135375,0.00005552662,0.00010224109,0.000010400516,0.000007164979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016226442,0.00005238373,0.000080401085,0.0000037756326,0.00005568684,0.000031522402,0.00012769447,0.000043673885,0.000021950284],"category_scores_gemma":[0.000008000387,0.000023236695,0.000010921971,0.00004583651,0.000054618817,0.000025342884,0.000012796157,0.00011591678,5.5059485e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024821152,0.000019177824,0.8957916,0.00004260689,0.00007904515,3.8797282e-7,0.0006813455,0.0010183665,0.0013782223,0.032908857,0.00029870518,0.0675335],"study_design_scores_gemma":[0.00013511105,0.000045332858,0.9873283,0.000030109244,0.000013814201,2.4996828e-7,0.00074229046,0.0030806263,0.001335887,0.0017676115,0.0054842,0.00003645068],"about_ca_topic_score_codex":0.0003534926,"about_ca_topic_score_gemma":0.0019348137,"teacher_disagreement_score":0.09153674,"about_ca_system_score_codex":9.066478e-7,"about_ca_system_score_gemma":0.000010497622,"threshold_uncertainty_score":0.107967146},"labels":[],"label_agreement":null},{"id":"W4413148050","doi":"10.1103/493p-85fd","title":"Atomistic study of atomic diffusion in <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\"> <mml:mrow> <mml:mi mathvariant=\"normal\">L</mml:mi> <mml:msub> <mml:mn>1</mml:mn> <mml:mn>2</mml:mn> </mml:msub> <mml:mtext>−</mml:mtext> <mml:msub> <mml:mi>FeNi</mml:mi> <mml:mn>3</mml:mn> </mml:msub> </mml:mrow> </mml:math> : Magnetochemical excitations and compositional effects","year":2025,"lang":"lv","type":"article","venue":"Physical Review Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Structural Genomics Consortium; University of Toronto","funders":"Canada First Research Excellence Fund","keywords":"Materials science; Diffusion; Chemical physics; Condensed matter physics; Thermodynamics; Physics","score_opus":0.012748191425582011,"score_gpt":0.24529811205427687,"score_spread":0.23254992062869487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413148050","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8834033,0.0049885996,0.00035928594,0.00090726116,0.004632086,0.00030600905,0.0026535587,0.00029352796,0.102456346],"genre_scores_gemma":[0.97999036,0.005454177,0.0013942793,0.0018806779,0.0027687924,0.0020594697,0.0055468986,0.00064037344,0.00026495926],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.98422754,0.0019001096,0.0038471066,0.0030794707,0.0034826654,0.0034631027],"domain_scores_gemma":[0.98784643,0.0038416141,0.003249006,0.0030923467,0.00033339864,0.0016372269],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.0036080559,0.0017000271,0.001280064,0.00077670225,0.0022538195,0.0023221548,0.0031630283,0.0021903398,0.3038919],"category_scores_gemma":[0.0019901611,0.002882756,0.0020621098,0.0019868673,0.0022060107,0.00204419,0.0026001674,0.0018544461,0.003242161],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004283634,0.00225728,0.00007180541,0.014033342,0.0032391723,0.0022698448,0.003285562,0.0010269065,0.077531695,0.41396263,0.47385398,0.0041841688],"study_design_scores_gemma":[0.003992614,0.0028381154,0.000740232,0.0061281794,0.0040162527,0.00074242335,0.0008427869,0.0051700976,0.9650473,0.0018038775,0.005824709,0.0028533845],"about_ca_topic_score_codex":0.004014753,"about_ca_topic_score_gemma":0.0016815369,"teacher_disagreement_score":0.88751566,"about_ca_system_score_codex":0.000028605691,"about_ca_system_score_gemma":0.0019030792,"threshold_uncertainty_score":0.9995746},"labels":[],"label_agreement":null},{"id":"W4413908565","doi":"10.1038/s41598-025-14903-2","title":"A rapid tectonic plate reorganization event driven by changes at subduction locations in a mantle convection model","year":2025,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; The Scarborough Hospital","funders":"Natural Sciences and Engineering Research Council of Canada; Academia Sinica","keywords":"Subduction; Plate tectonics; Mantle convection; Mantle (geology); Geology; Tectonics; Seismology; Hotspot (geology); Geophysics","score_opus":0.007992505098065828,"score_gpt":0.20629132606574743,"score_spread":0.19829882096768162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413908565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908926,0.0002793689,0.0012992783,0.00046220707,0.00559098,0.0003740778,0.000028350985,0.00005854794,0.0010146211],"genre_scores_gemma":[0.9909461,0.000042734187,0.000093899675,0.000025518715,0.000031607153,0.000008129044,0.00068579963,0.0000032680473,0.008162903],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987954,0.000046420846,0.0002806775,0.00046241414,0.00021107437,0.00020401603],"domain_scores_gemma":[0.99939424,0.000013827775,0.00015747164,0.00031194038,0.000078074074,0.000044467062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058341195,0.00009571419,0.00013038485,0.00019258153,0.00032198156,0.00014258648,0.00007488793,0.000060114184,0.00055905967],"category_scores_gemma":[0.00003427587,0.00008918995,0.000024016097,0.0005978686,0.00007246518,0.00017472243,0.000020978392,0.000049510116,0.00005951611],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008148638,0.00020945078,0.0660496,0.00021363136,0.00007160901,0.00006966087,0.0019099853,0.20025794,0.623899,0.00039183765,0.09340022,0.013445571],"study_design_scores_gemma":[0.00082786113,0.00013774856,0.080027856,0.00026851497,0.00013017851,0.00012412405,0.00026068714,0.3694355,0.3941161,0.03298373,0.12074509,0.00094258314],"about_ca_topic_score_codex":0.000635791,"about_ca_topic_score_gemma":0.0038289656,"teacher_disagreement_score":0.22978288,"about_ca_system_score_codex":0.000027152411,"about_ca_system_score_gemma":0.000101153935,"threshold_uncertainty_score":0.6121311},"labels":[],"label_agreement":null},{"id":"W4413991276","doi":"10.1029/2025gl115773","title":"Lithospheric Structures of Marginal Sea Basins in and Around the Philippine Sea Plate Shaped by Eastward Mantle Flow","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Nutrition Obesity Research Center, University of North Carolina","keywords":"Geology; Lithosphere; Mantle (geology); Heat flow; Seismology; Geophysics; Oceanography; Tectonics; Thermal; Meteorology","score_opus":0.016462482745516333,"score_gpt":0.2661167450585255,"score_spread":0.24965426231300916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413991276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926538,0.00031272322,0.00007533856,0.00546017,0.00016021555,0.00030396238,0.0005251989,0.00001302,0.00049559854],"genre_scores_gemma":[0.9987042,0.00007548885,0.00019643563,0.0004493718,0.00016700433,0.0000063523103,0.000086600805,0.0000052334203,0.00030931277],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99790543,0.000325684,0.00022825383,0.0003606039,0.00057459244,0.00060542254],"domain_scores_gemma":[0.99899596,0.0005162927,0.00004359843,0.0002821354,0.00005484257,0.000107186424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005800673,0.0001628815,0.00029505722,0.00008017864,0.00018893988,0.00013580875,0.00040619526,0.00005714102,0.00041622788],"category_scores_gemma":[0.00008051947,0.00010980772,0.00005254693,0.0005600495,0.0004633017,0.00014569974,0.000093381226,0.00036889815,0.00004100929],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036852527,0.0005609345,0.31993246,0.0017206979,0.0007484628,0.00033176976,0.0028406598,0.0074994983,0.38127863,0.0049524554,0.09659963,0.17984955],"study_design_scores_gemma":[0.0008417127,0.0001885813,0.946523,0.00008629967,0.00001830119,0.0000021412989,0.0001648588,0.022545792,0.0020284909,0.0065798867,0.020765506,0.00025540593],"about_ca_topic_score_codex":0.0065628868,"about_ca_topic_score_gemma":0.00071899925,"teacher_disagreement_score":0.62659055,"about_ca_system_score_codex":0.000007650345,"about_ca_system_score_gemma":0.000067141096,"threshold_uncertainty_score":0.9921165},"labels":[],"label_agreement":null},{"id":"W4414602670","doi":"10.1029/2025jb031674","title":"The Role of Dislocations in the Anelasticity of the Upper Mantle","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Division of Earth Sciences; Royal Commission for the Exhibition of 1851; University of Minnesota; National Science Foundation","keywords":"Viscoelasticity; Attenuation; Anisotropy; Grain Boundary Sliding; Grain boundary; Dislocation; Crystallite; Dissipation; Extrapolation","score_opus":0.016320015740513477,"score_gpt":0.3046752142949873,"score_spread":0.2883551985544738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414602670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943601,0.00026908927,0.000012236303,0.0014352753,0.00017843048,0.00015790436,0.00003296335,9.4279704e-7,0.003553098],"genre_scores_gemma":[0.9994285,0.000109984016,0.000020993213,0.000027184073,0.00013909064,9.956036e-7,0.0000011032754,0.0000014288381,0.00027068818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979421,0.00057024334,0.00037147722,0.00007974111,0.00076805236,0.000268405],"domain_scores_gemma":[0.9975405,0.0016761747,0.00016016843,0.00027852334,0.00030150497,0.000043130283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017035014,0.00006630528,0.00020933995,0.00007117153,0.00024829555,0.000062409395,0.00081598165,0.00003246705,0.00006655967],"category_scores_gemma":[0.00051267154,0.00002739958,0.00012139742,0.0005816746,0.00039641335,0.000097247124,0.000056017463,0.00039528578,0.000015882097],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002427337,0.0025149041,0.45276043,0.00053324935,0.0008372813,0.00004573348,0.010117614,0.01979732,0.13265255,0.23169245,0.01038702,0.1362341],"study_design_scores_gemma":[0.00016108772,0.00017045751,0.9436716,0.00007988679,0.00001522827,0.0000019065467,0.00060838147,0.001363535,0.008048126,0.038665086,0.007179169,0.000035559107],"about_ca_topic_score_codex":0.0015421561,"about_ca_topic_score_gemma":0.00063732534,"teacher_disagreement_score":0.49091113,"about_ca_system_score_codex":0.0000023323694,"about_ca_system_score_gemma":0.00024418914,"threshold_uncertainty_score":0.2331289},"labels":[],"label_agreement":null},{"id":"W4414768015","doi":"10.1029/2025gl119220","title":"Formation and Arrest of a Surface Density Front via Strain‐Driven Frontogenesis","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Frontogenesis; Front (military); Mixed layer; Layer (electronics); Surface (topology); Biogeochemical cycle","score_opus":0.021344891904081016,"score_gpt":0.2699559622696808,"score_spread":0.24861107036559982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414768015","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99630696,0.0000787535,0.0010848687,0.0014615098,0.0001797346,0.0002430157,0.00013782378,0.000016550784,0.0004907972],"genre_scores_gemma":[0.9990556,0.000028303884,0.00049753406,0.00015468399,0.00009506287,0.000001880133,0.00006473676,0.0000026405094,0.000099546385],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9984559,0.00024299895,0.00019729244,0.00025197465,0.00045212146,0.0003997406],"domain_scores_gemma":[0.99919873,0.00031715262,0.00004770256,0.00022557059,0.000099692945,0.00011115835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041953853,0.00011087924,0.00024333718,0.000076531556,0.00018153134,0.000072604205,0.00021412151,0.000050263552,0.00012515888],"category_scores_gemma":[0.000060173057,0.00009366739,0.000050906485,0.00018002668,0.00024113979,0.00022458253,0.00005906157,0.00014822611,0.0001139765],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002592215,0.00007605987,0.017732268,0.0003102753,0.00010507857,0.000021871896,0.0006547767,0.001741545,0.94814104,0.0007382213,0.007308904,0.022910748],"study_design_scores_gemma":[0.00058076147,0.00016009806,0.9466727,0.0000879681,0.00003457709,9.504365e-7,0.00014315732,0.013612835,0.031004148,0.0046551465,0.00279983,0.00024785375],"about_ca_topic_score_codex":0.009046582,"about_ca_topic_score_gemma":0.0010312031,"teacher_disagreement_score":0.9289404,"about_ca_system_score_codex":0.0000073077003,"about_ca_system_score_gemma":0.00004189881,"threshold_uncertainty_score":0.9975523},"labels":[],"label_agreement":null},{"id":"W4414768454","doi":"10.1029/2025je009203","title":"Electrical Resistivity of Liquid Fe‐16S‐2Si up to 13 GPa With Implications for the Adiabatic Heat Flux Through the Core of Exoplanet TRAPPIST‐1h","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Planets","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Electrical resistivity and conductivity; Liquidus; Heat flux; Convection; Thermal conductivity; Dynamo; Adiabatic process; Thermal; Core (optical fiber)","score_opus":0.057275012256531845,"score_gpt":0.3414380239794479,"score_spread":0.284163011722916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414768454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910096,0.0004842322,0.00075781037,0.004648262,0.00021750256,0.000945586,0.0009683985,0.0000065548575,0.0009620307],"genre_scores_gemma":[0.9987576,0.00009669872,0.00020937134,0.00012177968,0.00026490778,0.000012160495,0.00006886341,0.000005383635,0.00046321884],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9977746,0.00028264822,0.0005142799,0.00020934484,0.0007347747,0.00048436105],"domain_scores_gemma":[0.99323165,0.0054992056,0.00019275141,0.00041138998,0.00051146146,0.00015356373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001246675,0.00015557445,0.000494668,0.00011855716,0.00033249854,0.00006596204,0.000828072,0.00007138582,0.00010124197],"category_scores_gemma":[0.00048404626,0.00007727812,0.00012014433,0.0006883449,0.00034190778,0.000115956194,0.00003848709,0.00041339634,0.000013721704],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.05080847,0.001977973,0.027206225,0.0019827632,0.0037402802,0.000102705955,0.0052488167,0.024469923,0.22794543,0.060268644,0.5336917,0.062557034],"study_design_scores_gemma":[0.0013621097,0.0073683206,0.9125342,0.00030982133,0.00025824926,0.000039935767,0.00024585635,0.0014467206,0.008925968,0.01585777,0.051378515,0.00027256407],"about_ca_topic_score_codex":0.0032396824,"about_ca_topic_score_gemma":0.0008590591,"teacher_disagreement_score":0.88532794,"about_ca_system_score_codex":0.000009700147,"about_ca_system_score_gemma":0.0004742752,"threshold_uncertainty_score":0.48974523},"labels":[],"label_agreement":null},{"id":"W4414774506","doi":"10.1002/cjoc.70233","title":"Hydrogen‐Based Superconductors: Superconducting Mechanisms under Pressure Tuning and Future Development","year":2025,"lang":"en","type":"article","venue":"Chinese Journal of Chemistry","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Superconductivity; Hydride; Ambient pressure; Doping; High pressure","score_opus":0.007273322664685952,"score_gpt":0.21326734595333388,"score_spread":0.20599402328864794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414774506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99619085,0.0018908245,0.00017123901,0.00038622497,0.00053874793,0.000043749285,0.000013551294,0.000012505464,0.000752304],"genre_scores_gemma":[0.99730337,0.000030788193,0.0017456887,0.00012684728,0.0005398653,3.3349465e-7,0.00002031089,0.0000045607517,0.00022823352],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9990527,0.00003093864,0.0003594652,0.000158386,0.00020963242,0.00018885458],"domain_scores_gemma":[0.99945945,0.0000661187,0.00013378695,0.00012230463,0.00009983153,0.00011848476],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034109087,0.0001839365,0.00031047288,0.00004667509,0.00015049058,0.000091156086,0.00021156746,0.00010946195,0.0009767852],"category_scores_gemma":[0.000034965535,0.00012478254,0.00006363284,0.00013128735,0.000037060283,0.0002581247,0.000020910766,0.00020334129,0.0000025191441],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046754918,0.0000305401,0.014321507,0.0004111969,0.00022559683,0.000028916233,0.0004322792,0.0011888964,0.98100525,0.00003599772,0.00016900257,0.002104033],"study_design_scores_gemma":[0.0016767143,0.000054461034,0.035732888,0.00037615956,0.00022708956,0.00017506476,0.0014999851,0.0007526778,0.9310749,0.0062199943,0.02160198,0.00060807844],"about_ca_topic_score_codex":0.000024036828,"about_ca_topic_score_gemma":0.000008567263,"teacher_disagreement_score":0.04993037,"about_ca_system_score_codex":0.0000042121455,"about_ca_system_score_gemma":0.00021648004,"threshold_uncertainty_score":0.99993646},"labels":[],"label_agreement":null},{"id":"W4414798349","doi":"10.1073/pnas.2510213122","title":"Electronic origin of the anomalous melting of sodium under pressure","year":2025,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Fundamental Research Funds for the Central Universities; Jilin University; Program for Jilin University Science and Technology Innovative Research Team; National Natural Science Foundation of China","keywords":"Molecular dynamics; Electron; Electronic structure; Melting point; Melting temperature; Ab initio","score_opus":0.018127947521173995,"score_gpt":0.2603138887249059,"score_spread":0.2421859412037319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414798349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98451626,0.00039445728,5.18647e-7,0.0014612563,0.00006965165,0.00015158724,0.000052755746,0.0000037140887,0.013349777],"genre_scores_gemma":[0.99937654,0.00002067923,0.00013029088,0.00010316674,0.00003548439,7.688752e-7,1.9117392e-7,8.6493986e-7,0.00033202424],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99871176,0.000011835036,0.00029408012,0.00014834359,0.00066170126,0.00017229623],"domain_scores_gemma":[0.9992545,0.00011191254,0.00041003153,0.00001289375,0.00019375792,0.000016858925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011000506,0.00007070644,0.00016447183,0.00009421853,0.00016293666,0.000016108961,0.0009468409,0.000060012193,0.00006396847],"category_scores_gemma":[0.00015152003,0.000038398593,0.00006877803,0.00067297305,0.0005378309,0.00020295745,0.000057563004,0.00009808038,7.4438435e-7],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048647875,0.000050121085,0.19043292,0.0004677484,0.00012481006,2.9412548e-9,0.00038756483,0.0036004866,0.384717,0.4183069,0.0011187305,0.00074507995],"study_design_scores_gemma":[0.00012581395,0.00003849196,0.47010115,0.00012012958,0.00004224788,8.8286527e-7,0.000111949485,0.0012407503,0.39156055,0.13530874,0.0012840362,0.000065257154],"about_ca_topic_score_codex":0.00084501004,"about_ca_topic_score_gemma":0.000012826212,"teacher_disagreement_score":0.28299814,"about_ca_system_score_codex":0.0000033692106,"about_ca_system_score_gemma":0.00015497311,"threshold_uncertainty_score":0.19816604},"labels":[],"label_agreement":null},{"id":"W4414998900","doi":"10.1016/j.gsf.2025.102173","title":"Modelling 4.5 billion years of Earth’s thermal evolution: Insights from core-mantle coupling, lithospheric viscosity, grain-size-dependent rheology, and surface boundary conditions","year":2025,"lang":"en","type":"article","venue":"Geoscience Frontiers","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; Université du Québec à Montréal","funders":"Alliance de recherche numérique du Canada; Institut de Physique du Globe de Paris; Queen's University; Université du Québec à Montréal","keywords":"Mantle (geology); Lithosphere; Viscosity; Hotspot (geology); Mantle convection; Thermal; Rheology; Boundary value problem","score_opus":0.008441063579004706,"score_gpt":0.20673797519712045,"score_spread":0.19829691161811575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414998900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9604297,0.002644677,0.033837866,0.00006235374,0.002079556,0.0001931109,0.00028942173,0.00003637489,0.000426885],"genre_scores_gemma":[0.9937712,0.00019158778,0.00504348,0.000056702298,0.00004265967,0.0000013509194,0.00005903038,0.0000034027466,0.00083057565],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99871206,0.000047389793,0.0002616737,0.00041146931,0.00026972225,0.00029765346],"domain_scores_gemma":[0.999369,0.00009995524,0.00013050291,0.00023869683,0.00006128538,0.00010051813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002287903,0.00014488694,0.0002810526,0.000060703915,0.00035959907,0.00010281223,0.00029498126,0.00009512531,0.00016688363],"category_scores_gemma":[0.00002416136,0.00013360323,0.000048290807,0.00032967393,0.00065196265,0.00032019115,0.00006070103,0.000107045176,0.000020036827],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001599871,0.000114272996,0.31878027,0.000064605236,0.00013645817,0.000029675299,0.0012883072,0.65255785,0.018378727,0.0050208746,0.0017285548,0.0017404127],"study_design_scores_gemma":[0.00046337294,0.00011165464,0.5393189,0.00006554594,0.000067320136,0.0000017660567,0.00038811372,0.43860322,0.0008484529,0.017589761,0.0022501915,0.00029165257],"about_ca_topic_score_codex":0.013098468,"about_ca_topic_score_gemma":0.0005373336,"teacher_disagreement_score":0.22053865,"about_ca_system_score_codex":0.0000063230286,"about_ca_system_score_gemma":0.00016780573,"threshold_uncertainty_score":0.9934734},"labels":[],"label_agreement":null},{"id":"W4415221290","doi":"10.1126/sciadv.adt9106","title":"Onset of slab mantle melting in Earth’s lower mantle: Evidence from ferropericlase in superdeep diamonds","year":2025,"lang":"en","type":"article","venue":"Science Advances","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Slab; Diamond; Mantle (geology); Inclusion (mineral); Crystallization; Melt inclusions; Lithosphere","score_opus":0.011222780856078479,"score_gpt":0.2570862929798344,"score_spread":0.2458635121237559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415221290","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99440575,0.0024890732,0.00002988667,0.00013276693,0.000839688,0.0001415213,0.00007465179,0.0000128642505,0.0018738197],"genre_scores_gemma":[0.99816525,0.00031599973,0.0012319483,0.00007437447,0.000026677695,0.000002750449,0.0000075139637,0.0000018595119,0.00017361094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99837136,0.000073138865,0.0003464483,0.00044445766,0.00036017835,0.00040443044],"domain_scores_gemma":[0.9992659,0.0002630917,0.00008114638,0.00027772112,0.00004953165,0.00006260027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007822663,0.00012983609,0.00026859445,0.00023546733,0.00010814113,0.000082651066,0.0005938527,0.00003577012,0.00057922956],"category_scores_gemma":[0.0002955456,0.00010427288,0.000028155138,0.0012538766,0.00044269816,0.0012731667,0.0000633234,0.00009688243,0.00006204466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001421193,0.000068913534,0.84627175,0.00008085581,0.000005263065,0.0000800625,0.0010747134,0.01021244,0.1052686,0.00018231836,0.000037880145,0.036575064],"study_design_scores_gemma":[0.00031120778,0.00009531069,0.88858134,0.00057265116,0.0000074628374,0.0000010170927,0.00056239334,0.0038150472,0.10163903,0.0027722213,0.0013986393,0.0002436897],"about_ca_topic_score_codex":0.0071066758,"about_ca_topic_score_gemma":0.012387885,"teacher_disagreement_score":0.042309552,"about_ca_system_score_codex":0.000006450698,"about_ca_system_score_gemma":0.00017676782,"threshold_uncertainty_score":0.9995051},"labels":[],"label_agreement":null},{"id":"W4415504882","doi":"10.15302/planet.2025.25005","title":"Quantification of shock in enstatite chondrites using micro-X-ray diffraction","year":2025,"lang":"en","type":"article","venue":"Planet","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Enstatite; Chondrite; Shock metamorphism; Meteorite; Shock (circulatory); Petrography; Metamorphic rock","score_opus":0.015418624228209572,"score_gpt":0.2373623051993614,"score_spread":0.22194368097115183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415504882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981258,0.00015673423,0.00013486847,0.000032335105,0.0003961906,0.000088930814,0.00032928426,0.000009476317,0.0007263631],"genre_scores_gemma":[0.9979528,0.000033931785,0.0009428484,0.000028561903,0.000027893537,3.4227853e-7,0.00091689994,0.0000010776785,0.00009563586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99949855,0.000040699593,0.00017319575,0.000115329334,0.00006817395,0.00010403887],"domain_scores_gemma":[0.99972516,0.00008668823,0.00006691618,0.00009378512,0.000011933397,0.000015503476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010898554,0.000057421432,0.000119010205,0.00008383181,0.000030713796,0.000024205257,0.000068038054,0.000037203088,0.00035820922],"category_scores_gemma":[0.000012438624,0.000051401134,0.000009380108,0.00011421185,0.000018719364,0.000088124725,0.0000037919103,0.00003913882,0.000040364317],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066649205,0.000043157805,0.5945552,0.00014170258,0.000023439636,0.0000037473478,0.00017902654,0.02617471,0.37364626,0.00037969375,0.001508886,0.0032774988],"study_design_scores_gemma":[0.0001684502,0.000016728553,0.9700272,0.000034925688,0.000013863447,6.091799e-7,0.000046400797,0.009037827,0.006249381,0.0004148159,0.013906174,0.00008362662],"about_ca_topic_score_codex":0.008022989,"about_ca_topic_score_gemma":0.0015044002,"teacher_disagreement_score":0.37547198,"about_ca_system_score_codex":0.0000017211202,"about_ca_system_score_gemma":0.000020586953,"threshold_uncertainty_score":0.99858266},"labels":[],"label_agreement":null},{"id":"W4415995000","doi":"10.1038/s43017-025-00735-1","title":"Earth’s past and present mantle oxygen fugacity","year":2025,"lang":"en","type":"article","venue":"Nature Reviews Earth & Environment","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Agence Nationale de la Recherche","keywords":"Mineral redox buffer; Mantle (geology); Planetary differentiation; Fugacity; Mantle plume; Transition zone; Mantle wedge; Early Earth; Crustal recycling","score_opus":0.007790323367191154,"score_gpt":0.21308974031999434,"score_spread":0.20529941695280318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415995000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.57610196,0.3761488,0.0004376484,0.00421564,0.0023891039,0.003800152,0.0004843419,0.000109491935,0.03631287],"genre_scores_gemma":[0.90672743,0.07957583,0.0027607318,0.0018098097,0.0006836178,0.000024944236,0.00021697878,0.000010931351,0.0081897145],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985619,0.0001676457,0.0003106036,0.000423861,0.0002319782,0.00030401623],"domain_scores_gemma":[0.9993274,0.000049192968,0.000101303645,0.0003925107,0.0000062622344,0.00012329652],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043472304,0.00021909547,0.00040348832,0.00004578132,0.0001479857,0.00008059065,0.0001867651,0.00016906971,0.00225882],"category_scores_gemma":[0.000014719104,0.00016016145,0.000089144974,0.00008646549,0.00007667352,0.000119951015,0.00006008079,0.0002711587,0.00075908046],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011265777,0.00019661062,0.07143107,0.0010931036,0.0002398376,0.00005140768,0.00023202016,0.00086226413,0.0055872933,0.0020921826,0.038212303,0.87988925],"study_design_scores_gemma":[0.00012509321,0.00002871097,0.2656567,0.000053483156,0.00003310766,0.0000018679962,0.0000029661599,0.000059385147,0.00040392845,0.00021382404,0.733299,0.00012190461],"about_ca_topic_score_codex":0.00009894392,"about_ca_topic_score_gemma":0.00009028368,"teacher_disagreement_score":0.87976736,"about_ca_system_score_codex":0.000002397919,"about_ca_system_score_gemma":0.000012800216,"threshold_uncertainty_score":0.99865323},"labels":[],"label_agreement":null},{"id":"W4416247275","doi":"10.1016/j.diamond.2025.113060","title":"Spatial distribution of nitrogen and hydrogen in natural lithospheric diamonds by in situ synchrotron infrared microspectroscopy","year":2025,"lang":"en","type":"article","venue":"Diamond and Related Materials","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ural Branch, Russian Academy of Sciences; Sapienza Università di Roma; Chinese Academy of Sciences; Canadian Anesthesiologists' Society; Diamond Light Source","keywords":"Chromite; Synchrotron; Diamond; Hydrogen; Nitrogen; Chemical composition; Infrared; Absorption (acoustics); Analytical Chemistry (journal); Mineral","score_opus":0.0016457098847977628,"score_gpt":0.1828276606487254,"score_spread":0.18118195076392765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416247275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99426067,0.0041996785,0.0000028250513,0.00004462718,0.0004201546,0.00026708393,0.00044816273,0.000015881029,0.00034092407],"genre_scores_gemma":[0.9982078,0.00071694993,0.000026560689,0.00002099192,0.000019806743,0.0000047566164,0.0008420802,0.000003971996,0.00015709772],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9988566,0.00010768709,0.00042417028,0.00026534154,0.000083710045,0.00026249603],"domain_scores_gemma":[0.9996806,0.00004719751,0.000108905704,0.000106901025,0.000015714524,0.000040691117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000237651,0.0001651528,0.00039860932,0.000058082318,0.00005004475,0.000066612716,0.00008745784,0.00016000334,0.00013049712],"category_scores_gemma":[0.00002306866,0.00013828058,0.0000221794,0.00020681108,0.00010267943,0.0001401605,0.00003154835,0.00008489006,0.0000046990467],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015522397,0.000036135312,0.12295034,0.00012278608,0.000035302306,0.000011972276,0.00017072738,0.000020252279,0.8752738,0.000119820375,0.00021158037,0.00089203793],"study_design_scores_gemma":[0.0010887254,0.00008245992,0.5102053,0.00014238284,0.00003228913,0.000002818156,0.000028565464,0.00010419023,0.48237026,0.00525221,0.00047837052,0.00021241883],"about_ca_topic_score_codex":0.0038087498,"about_ca_topic_score_gemma":0.0002845178,"teacher_disagreement_score":0.39290354,"about_ca_system_score_codex":0.0000063979573,"about_ca_system_score_gemma":0.00002617197,"threshold_uncertainty_score":0.5757716},"labels":[],"label_agreement":null},{"id":"W4416593840","doi":"10.48550/arxiv.2511.16859","title":"Constructing Earth Formation History Using Deep Mantle Noble Gas Reservoirs","year":2025,"lang":"","type":"preprint","venue":"ArXiv.org","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Kavli Institute for Theoretical Physics, University of California, Santa Barbara; Fonds de recherche du Québec – Nature et technologies; Alliance de recherche numérique du Canada; Natural Sciences and Engineering Research Council of Canada; McGill University; National Science Foundation","keywords":"Mantle (geology); Noble gas; Neon; Formation and evolution of the Solar System; Accretion (finance); Krypton; Crust; Volcano; Radiogenic nuclide; Solar System","score_opus":0.05622177623760073,"score_gpt":0.23891610617130854,"score_spread":0.18269432993370782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416593840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96607107,0.0021077849,0.0013367985,0.00015934394,0.009920357,0.00068988296,0.00040099627,0.00009028502,0.019223478],"genre_scores_gemma":[0.99132836,0.00080504175,0.0033553205,0.0001825597,0.00094532606,0.000008474144,0.00075034116,0.000019627658,0.0026049723],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9959712,0.00041988277,0.0011590079,0.0009787766,0.0005362392,0.00093491486],"domain_scores_gemma":[0.9973687,0.00023878527,0.0009281641,0.0009401564,0.0002567098,0.0002674653],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009668774,0.0006304374,0.00091523095,0.00027989878,0.0006245244,0.0002158086,0.0008072647,0.00050674164,0.005679324],"category_scores_gemma":[0.00012438945,0.0006572993,0.000273667,0.0002456596,0.00030122255,0.0008701127,0.0004530742,0.0007145474,0.000870849],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055409817,0.00019511835,0.8573408,0.0066847843,0.00082291034,0.00020000807,0.0066427095,0.088129595,0.013798687,0.002186124,0.0029255925,0.02051953],"study_design_scores_gemma":[0.0035287044,0.0005325217,0.15966615,0.0053888136,0.0020052444,0.00019158007,0.0057818666,0.3415722,0.039238345,0.0059864004,0.4298383,0.0062698806],"about_ca_topic_score_codex":0.009157229,"about_ca_topic_score_gemma":0.0027424642,"teacher_disagreement_score":0.6976747,"about_ca_system_score_codex":0.000117340365,"about_ca_system_score_gemma":0.0006660038,"threshold_uncertainty_score":0.9999071},"labels":[],"label_agreement":null},{"id":"W4416985230","doi":"10.1088/1674-1056/ae27b7","title":"Superconducting and dynamically stable polymorphs of elemental calcium predicted under high pressure","year":2025,"lang":"","type":"article","venue":"Chinese Physics B","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Superconductivity; Calcium; High pressure; Polymorphism (computer science); Phase (matter); Metal; Crystal structure","score_opus":0.008574404934297028,"score_gpt":0.23433266960388247,"score_spread":0.22575826466958543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416985230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98948044,0.0017515753,0.00058260054,0.0002983638,0.001943388,0.0005144571,0.0037592803,0.00004247163,0.0016274293],"genre_scores_gemma":[0.99708104,0.00011776897,0.00024476717,0.000121120924,0.00048267806,0.000004746402,0.00064556015,0.000017390237,0.001284898],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9974308,0.00017526794,0.00069766946,0.00067239144,0.00041047577,0.0006133925],"domain_scores_gemma":[0.9986684,0.00023677951,0.00025191065,0.0004915224,0.00016581641,0.00018560073],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002850162,0.00049210084,0.00083880505,0.00008808418,0.00033520305,0.00019941574,0.00041098866,0.00018308406,0.000972464],"category_scores_gemma":[0.00004052173,0.00041114568,0.00012529243,0.000592944,0.00034645197,0.0006193205,0.00021939931,0.0002749499,0.000014711374],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007689219,0.0010696887,0.3562627,0.003948169,0.0030641938,0.000019641895,0.0025407283,0.017716642,0.5720291,0.03149771,0.0015343967,0.009548076],"study_design_scores_gemma":[0.0049164114,0.00069133483,0.7907988,0.00082889246,0.0017733652,0.000008438704,0.00090560253,0.058350872,0.04525515,0.093248524,0.0014193449,0.0018032708],"about_ca_topic_score_codex":0.0075151734,"about_ca_topic_score_gemma":0.00019291198,"teacher_disagreement_score":0.5267739,"about_ca_system_score_codex":0.0000081261705,"about_ca_system_score_gemma":0.00024406386,"threshold_uncertainty_score":0.99994075},"labels":[],"label_agreement":null},{"id":"W4417062586","doi":"10.1139/cjes-2025-0012","title":"Receiver function insights into crust and lithospheric fabric in Northern Canada","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"","keywords":"Receiver function; Lithosphere; Bouguer anomaly; Crust; Upper crust; Density contrast; Inversion (geology); Tectonics","score_opus":0.0061971136088881515,"score_gpt":0.17478840042950633,"score_spread":0.1685912868206182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417062586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99156505,0.0027859877,0.000015770589,0.00040862325,0.0012375015,0.000047025358,0.0000050194617,0.0000013517702,0.003933687],"genre_scores_gemma":[0.9992498,0.00005257271,0.00012328081,0.00029890612,0.000062878076,1.2749858e-7,0.0000012761739,8.7868267e-7,0.00021023511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992171,0.000052815412,0.00021833013,0.00012844539,0.00016062384,0.00022268317],"domain_scores_gemma":[0.9994726,0.00005457683,0.00009482581,0.00005627173,0.00007127214,0.00025042225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029663419,0.000076845805,0.00015157992,0.00017142398,0.00025059047,0.00013390489,0.00018961087,0.000030661795,0.0002571354],"category_scores_gemma":[0.000052595904,0.000058290938,0.000016873812,0.000561663,0.00015962153,0.00028027457,0.0000038084547,0.00008680048,0.0000046924333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009441812,0.0000017657587,0.98357207,0.00001148687,0.000009405989,0.00005563317,0.00035609058,0.002806717,0.00004675366,0.0001811352,0.00038940477,0.012560116],"study_design_scores_gemma":[0.00011130383,0.00008155508,0.9528518,0.000046094323,0.000007224925,0.000005422722,0.00031213116,0.00025940867,0.000039810882,0.0015638226,0.044646844,0.00007458616],"about_ca_topic_score_codex":0.9494336,"about_ca_topic_score_gemma":0.999757,"teacher_disagreement_score":0.050323386,"about_ca_system_score_codex":0.00000450969,"about_ca_system_score_gemma":0.0033871008,"threshold_uncertainty_score":0.60085714},"labels":[],"label_agreement":null},{"id":"W4417144583","doi":"10.21203/rs.3.rs-8302131/v1","title":"Viscous coupling at mid-oceanic ridges explaining puzzling Pacific Plate motions","year":2025,"lang":"","type":"preprint","venue":"Research Square","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"Nederlandse Organisatie voor Wetenschappelijk Onderzoek","keywords":"Ridge push; Plate tectonics; Mid-ocean ridge; Ridge; Slab window; Slab; Pacific Plate; Convergent boundary; Mantle (geology)","score_opus":0.06148317994281278,"score_gpt":0.33803064604201855,"score_spread":0.2765474660992058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417144583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9473852,0.008670563,0.00051979686,0.0010151997,0.0071850517,0.0034526505,0.009401628,0.000300579,0.022069313],"genre_scores_gemma":[0.9720551,0.010049369,0.00035646715,0.000019670591,0.0015941418,0.00008800003,0.0027778836,0.000048519054,0.013010858],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.98883486,0.0011177756,0.0015059432,0.0025240013,0.0029039853,0.003113429],"domain_scores_gemma":[0.9932676,0.0023062401,0.00047897125,0.0019338779,0.0010808734,0.00093245116],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.006735172,0.0010375917,0.001488457,0.0011696327,0.004645753,0.0019428367,0.0020380728,0.0009774853,0.007232648],"category_scores_gemma":[0.0007097547,0.0010169355,0.0005550056,0.0014194188,0.0006513299,0.00049445673,0.0021311366,0.00289033,0.0028098833],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014507718,0.00081554503,0.0328665,0.019588612,0.002093068,0.0013887256,0.01585389,0.87720853,0.018713344,0.002660335,0.014636433,0.0127242645],"study_design_scores_gemma":[0.005070629,0.0025342526,0.12208421,0.03396252,0.000959253,0.00010623042,0.021438908,0.5606427,0.027522506,0.013556608,0.20373718,0.008385009],"about_ca_topic_score_codex":0.0033041858,"about_ca_topic_score_gemma":0.0007977273,"teacher_disagreement_score":0.3165658,"about_ca_system_score_codex":0.00018839212,"about_ca_system_score_gemma":0.0014379132,"threshold_uncertainty_score":0.99941003},"labels":[],"label_agreement":null},{"id":"W4417503897","doi":"10.1038/s41598-025-28606-1","title":"Cenozoic evolution of earth’s strongest geoid low illuminates mantle dynamics beneath Antarctica","year":2025,"lang":"en","type":"article","venue":"Scientific Reports","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; Université du Québec à Montréal; Geological Survey of Canada","funders":"Institut de Physique du Globe de Paris; Queen's University; Agence Nationale de la Recherche; National Science Foundation","keywords":"Geoid; Mantle (geology); Transition zone; Ocean surface topography; Geodynamics; Post-glacial rebound; Buoyancy; Subduction","score_opus":0.0037874810247728687,"score_gpt":0.19252384066641168,"score_spread":0.18873635964163882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417503897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98475885,0.0003369416,0.00019686647,0.00008854973,0.007949275,0.00021146006,0.000109543405,0.000036064543,0.0063124727],"genre_scores_gemma":[0.994754,0.000010717283,0.00027203994,0.0000074810414,0.000048766477,0.0000013548794,0.00033639756,0.000003049613,0.00456616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983438,0.00004579622,0.0004247908,0.00050017086,0.00035747615,0.0003279262],"domain_scores_gemma":[0.99893254,0.00004166523,0.0002264213,0.0005705088,0.00015016928,0.00007868489],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007543691,0.0001320363,0.00023530332,0.00016551385,0.00027206968,0.00016667506,0.00017329221,0.0000656231,0.000750602],"category_scores_gemma":[0.000058574187,0.000113115675,0.000073386866,0.00043319678,0.00029622635,0.00020593352,0.000037326816,0.0000671263,0.000052444913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012763427,0.00043557485,0.8359335,0.0010655675,0.0002521826,0.0005505876,0.0006692216,0.01295772,0.09703073,0.011227537,0.017172998,0.022576729],"study_design_scores_gemma":[0.00034619932,0.00016718569,0.82194316,0.0003244514,0.00016130957,0.00007677902,0.00047126712,0.016824238,0.073744975,0.049273778,0.036044717,0.00062196155],"about_ca_topic_score_codex":0.002173781,"about_ca_topic_score_gemma":0.0022847103,"teacher_disagreement_score":0.03804624,"about_ca_system_score_codex":0.000009160107,"about_ca_system_score_gemma":0.00019884761,"threshold_uncertainty_score":0.82185656},"labels":[],"label_agreement":null},{"id":"W567514250","doi":"","title":"Deux aspects de l'influence des continents sur le manteau terrestre : initiation de la subduction : effet thermique des racines continentales","year":2009,"lang":"fr","type":"dissertation","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Humanities; Geology; Lithosphere; Physics; Philosophy; Tectonics; Seismology","score_opus":0.009612915817854586,"score_gpt":0.2157585144808598,"score_spread":0.20614559866300522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W567514250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9742275,0.002350868,0.0028609158,0.00094872824,0.0003293293,0.0005150955,0.00017519646,0.00015185984,0.018440539],"genre_scores_gemma":[0.9811856,0.0024169066,0.005940105,0.00006746651,0.00009756796,0.000028271219,0.00283514,0.000037866488,0.007391055],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99003994,0.007461881,0.0006928361,0.0007031414,0.0003881824,0.00071402424],"domain_scores_gemma":[0.9951389,0.0017343272,0.00074436434,0.0007172901,0.0013746929,0.0002904445],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.004507036,0.0005353082,0.00054911134,0.00020037119,0.0010491633,0.00080668565,0.0008046094,0.00045036105,0.00036917685],"category_scores_gemma":[0.00167486,0.00056242716,0.0002052575,0.0004245836,0.00070060743,0.00080420275,0.00006402089,0.00040882558,0.00007787266],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041290672,0.0019657398,0.36460707,0.0017997072,0.0003311499,0.00012477324,0.056302395,0.0024291999,0.38093024,0.026938213,0.0010418771,0.16311671],"study_design_scores_gemma":[0.00090659515,0.000004776956,0.79687834,0.0031632418,0.00013484359,0.000060883744,0.0005546776,0.0035310143,0.1819498,0.009009302,0.0032192324,0.00058729976],"about_ca_topic_score_codex":0.0497813,"about_ca_topic_score_gemma":0.064515226,"teacher_disagreement_score":0.43227127,"about_ca_system_score_codex":0.00007343764,"about_ca_system_score_gemma":0.00058261934,"threshold_uncertainty_score":0.9996827},"labels":[],"label_agreement":null},{"id":"W56906572","doi":"10.1007/978-3-540-85181-3_107","title":"On the ongoing quest to pinpoint the location of RR-MR transition in blast wave reflections","year":2009,"lang":"en","type":"book-chapter","venue":"Shock Waves","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Explosive material; Reflection (computer programming); Blast wave; Reduction (mathematics); Range (aeronautics); Ranging; Mechanics; Scale (ratio); Physics; Computer science; Engineering; Aerospace engineering; Mathematics; Geography; Shock wave; Telecommunications; Quantum mechanics; Geometry","score_opus":0.022028656326783712,"score_gpt":0.22656479561690115,"score_spread":0.20453613929011744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W56906572","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10259576,0.0005085093,0.00029804077,0.008923888,0.0014476469,0.0019304297,0.0005822886,0.000076562545,0.8836369],"genre_scores_gemma":[0.9837334,0.00008853317,0.000056250847,0.00056182063,0.00030570294,0.0000028844104,0.00012792615,0.000008208702,0.0151152825],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9990631,0.000059651265,0.00027711494,0.0002197979,0.00022393283,0.00015644527],"domain_scores_gemma":[0.99933964,0.00016237466,0.00011389086,0.00028162228,0.000064684195,0.000037790607],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002853697,0.00017396918,0.0002138329,0.000094984796,0.00014750296,0.000051566705,0.00015161901,0.000105546365,0.0005337301],"category_scores_gemma":[0.00002389724,0.00010213714,0.00005803778,0.00008762166,0.00005653487,0.000056010158,0.0000068463446,0.00017516341,0.00014619391],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008372713,0.00019053668,0.000046039055,0.0004960264,0.00034750922,0.000050333205,0.019236738,0.09960736,0.00980451,0.7644543,0.010394208,0.09453516],"study_design_scores_gemma":[0.0009770916,0.003790745,0.052744593,0.0050375247,0.00043879618,0.00004643102,0.0010084556,0.004076889,0.011900179,0.67132306,0.24620596,0.0024502673],"about_ca_topic_score_codex":0.0010176145,"about_ca_topic_score_gemma":0.0077019744,"teacher_disagreement_score":0.8811376,"about_ca_system_score_codex":0.0000081722355,"about_ca_system_score_gemma":0.000058308287,"threshold_uncertainty_score":0.584397},"labels":[],"label_agreement":null},{"id":"W58395576","doi":"","title":"La structure thermique de la lithosphère continentale : à l'heure actuelle et dans le passé","year":2005,"lang":"fr","type":"dissertation","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Humanities; Physics; Lithosphere; Geology; Philosophy; Tectonics; Seismology","score_opus":0.004092831188727062,"score_gpt":0.21983550676573885,"score_spread":0.2157426755770118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W58395576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.83485174,0.0009327868,0.00007607049,0.00057913363,0.0008951359,0.00030863038,0.0014221184,0.00006629134,0.1608681],"genre_scores_gemma":[0.942082,0.0008170585,0.0012860802,0.0002790643,0.00047915932,0.0000059868516,0.0038864724,0.000031517222,0.051132668],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.997391,0.0009469887,0.0003783617,0.0005034628,0.0002730377,0.00050717127],"domain_scores_gemma":[0.99875593,0.00041221667,0.0002496371,0.00030456646,0.00006360988,0.0002140508],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005416559,0.00049614004,0.0005227666,0.00005174725,0.00031758472,0.00040714987,0.00044307887,0.0008547923,0.011638312],"category_scores_gemma":[0.000038001985,0.00040746565,0.00017279845,0.00012824478,0.00016719066,0.00029199343,0.000024156283,0.0005396664,0.00016384116],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010601191,0.0010581713,0.21144512,0.002879933,0.0015148651,0.0010298184,0.086429924,0.015384789,0.26369116,0.2641512,0.040490095,0.110864826],"study_design_scores_gemma":[0.0007876607,0.00012901425,0.5002021,0.00024134127,0.00019097622,0.00009857816,0.0060032327,0.0006898185,0.038464494,0.0037165077,0.44848606,0.0009902181],"about_ca_topic_score_codex":0.026168806,"about_ca_topic_score_gemma":0.05421851,"teacher_disagreement_score":0.40799597,"about_ca_system_score_codex":0.000010188836,"about_ca_system_score_gemma":0.0004703707,"threshold_uncertainty_score":0.9998377},"labels":[],"label_agreement":null},{"id":"W6884308082","doi":"10.1016/j.pepi.2025.107418","title":"Rutile's pressure-temperature-time evolution dictates its role as a depth-dependent subduction-zone water regulator","year":2025,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Anesthesiologists' Society","keywords":"Rutile; Subduction; Hydrogen; Crystallinity; Raman spectroscopy; Fourier transform infrared spectroscopy; Amorphous solid","score_opus":0.0028827324489229997,"score_gpt":0.17472998277433036,"score_spread":0.17184725032540735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6884308082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99464977,0.0014610693,0.000008283099,0.00033603667,0.0010696518,0.00031414346,0.00048706078,0.00003877492,0.0016352191],"genre_scores_gemma":[0.99505836,0.000058117563,0.00003775354,0.00009339858,0.00023786761,0.0000023378334,0.00030563236,0.0000057606244,0.0042007514],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99866694,0.00013334454,0.00029748812,0.0003203416,0.00025616123,0.00032569794],"domain_scores_gemma":[0.9993554,0.00006064848,0.00010883369,0.0003264633,0.000061030583,0.00008766154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016731209,0.00023943017,0.00034490204,0.000066204135,0.00022376429,0.000097275784,0.0003262276,0.00009673921,0.00072997215],"category_scores_gemma":[0.000013079232,0.00014895177,0.00009666121,0.00015018106,0.00011913828,0.0002765384,0.00006753226,0.00016165724,0.00020442742],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014471496,0.00016695965,0.046084367,0.0006312563,0.0011693939,0.000012912434,0.001554939,0.016030058,0.91819626,0.0023076385,0.002378299,0.010020753],"study_design_scores_gemma":[0.00092706736,0.00030311552,0.34732622,0.0003161842,0.00045882966,0.000036709218,0.0001365261,0.006302107,0.6142911,0.012127743,0.01711931,0.00065511337],"about_ca_topic_score_codex":0.0017754335,"about_ca_topic_score_gemma":0.00026768644,"teacher_disagreement_score":0.30390522,"about_ca_system_score_codex":0.000001809239,"about_ca_system_score_gemma":0.000044017,"threshold_uncertainty_score":0.7992683},"labels":[],"label_agreement":null},{"id":"W6884499442","doi":"10.1021/jp401847s.s001","title":"A Drude Polarizable Model for Liquid Hydrogen Sulfide","year":2016,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Polarizability; Dipole; Enthalpy; Harmonic oscillator; Lone pair; Moment (physics); Point particle; Dielectric; Radial distribution function; Force field (fiction)","score_opus":0.02972386663569551,"score_gpt":0.2197369449390025,"score_spread":0.190013078303307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6884499442","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027596269,0.00021666393,0.00008577835,0.00025264802,0.00010854644,0.0003630539,0.9675253,0.000091274276,0.0037604715],"genre_scores_gemma":[0.94518614,0.0000035835462,0.00037221564,0.00023799475,0.00028109373,0.000030775576,0.051137947,0.000008526375,0.0027416986],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99927706,0.000013403583,0.00011727563,0.00019598694,0.00010915549,0.00028711636],"domain_scores_gemma":[0.99952596,0.0001026587,0.000050214603,0.00017595947,0.000044724253,0.00010047314],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000051662384,0.000100009616,0.00012654501,0.000022649554,0.00009251099,0.00004374582,0.0002109138,0.00005962789,0.15250775],"category_scores_gemma":[0.0001371787,0.00006395113,0.00005869569,0.000041739895,0.000004412891,0.00019800162,0.000018310186,0.000020499965,0.004155945],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004080539,0.000044644632,0.0003592472,0.0003277491,0.000098753335,0.000015872753,0.0002950904,0.0060647326,0.037492722,0.00046460898,0.9423493,0.012079192],"study_design_scores_gemma":[0.00093296246,0.00031704886,0.000944404,0.00064428314,0.000027175636,0.000005015172,0.0000059120675,0.043689582,0.05900999,0.0056324084,0.88814914,0.0006420831],"about_ca_topic_score_codex":0.00010225542,"about_ca_topic_score_gemma":0.00012522421,"teacher_disagreement_score":0.9175899,"about_ca_system_score_codex":0.0000018263347,"about_ca_system_score_gemma":0.00005713294,"threshold_uncertainty_score":0.99661946},"labels":[],"label_agreement":null},{"id":"W6887815365","doi":"10.17611/dp/11246027","title":"Moment Tensor for September 19, 2015 MW 4.7 (GCMT) VANCOUVER ISLAND, CANADA REGION","year":2015,"lang":"en","type":"other","venue":"NSF Seismological Facility for the Advancement of Geoscience (SAGE)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Moment (physics); Earth structure; Tensor (intrinsic definition); Field (mathematics); Intersection (aeronautics)","score_opus":0.025442253096576124,"score_gpt":0.24591963860198604,"score_spread":0.2204773855054099,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6887815365","genre_codex":"methods","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010077568,0.0024376288,0.943531,0.0021963695,0.0055854996,0.0049532414,0.036250066,0.00010097784,0.0039374814],"genre_scores_gemma":[0.004213389,0.00031046936,0.0013412992,0.0011457974,0.00026442093,0.00010152633,0.00074265746,0.000023547278,0.9918569],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99708545,0.000092055634,0.00051719917,0.000760576,0.0008132934,0.0007314302],"domain_scores_gemma":[0.9982257,0.000328843,0.00043837656,0.0006172393,0.00014150761,0.00024835736],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00082859315,0.0004252533,0.0006892167,0.000054200726,0.00026331752,0.00004372992,0.0007758488,0.00020013233,0.0022401018],"category_scores_gemma":[0.0001372406,0.00025291403,0.00016342638,0.0001821871,0.00038547398,0.00011394609,0.000075798824,0.00012528902,0.000033058262],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064889813,0.0002030567,0.0010189537,0.0006320282,0.00019012298,0.000019010775,0.000100735124,0.0058608474,0.00005478305,0.00016962017,0.6490379,0.34206402],"study_design_scores_gemma":[0.0006133643,0.0004512989,0.00034426668,0.000046152767,0.00007305684,0.0000019258498,0.000076217955,0.00053315057,0.00003693736,0.00081974815,0.9966537,0.00035017563],"about_ca_topic_score_codex":0.20765531,"about_ca_topic_score_gemma":0.38092864,"teacher_disagreement_score":0.9879194,"about_ca_system_score_codex":0.000048772225,"about_ca_system_score_gemma":0.00044770708,"threshold_uncertainty_score":0.9999923},"labels":[],"label_agreement":null},{"id":"W6889169258","doi":"10.25394/pgs.24302335","title":"Investigating the Effect of Mantle Flow on Surface Deformation in Alaska, Northwestern Canada, and the Bering Sea Using 3-D Geodynamic Models","year":2023,"lang":"en","type":"dissertation","venue":"Purdue","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Mantle (geology); Plate tectonics; Crust; Slab; Tectonics; Lithosphere; Geodynamics; Mid-ocean ridge","score_opus":0.007753763515885715,"score_gpt":0.19894125625692344,"score_spread":0.19118749274103772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6889169258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998533,0.00010379372,0.0000046980313,0.000024733028,0.00053117645,0.00036554766,0.00020444983,0.000008191978,0.00022438088],"genre_scores_gemma":[0.99870294,0.000024441819,0.000029492454,0.000015188385,0.000042029096,0.0000031996824,0.0010200685,0.000008126515,0.00015449949],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99901026,0.00016340002,0.0002492453,0.00014757954,0.00024882596,0.00018067703],"domain_scores_gemma":[0.9992368,0.00037627606,0.00018876893,0.00014855448,0.000018612312,0.000030992083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005370217,0.00015466019,0.0002667803,0.000033393197,0.00013855434,0.00006125306,0.00014732873,0.00006560312,0.000009838037],"category_scores_gemma":[0.00002640858,0.00008705421,0.00002923187,0.000121321755,0.00003439633,0.0001039026,0.000010928641,0.0001423135,0.000005257992],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056282766,9.587984e-7,0.02480932,0.00034313652,0.000026782393,0.0000019988079,0.0019330756,0.9707813,0.00011165457,0.000009756786,0.000013626023,0.001912061],"study_design_scores_gemma":[0.00038845133,0.000031589876,0.20925747,0.0003461804,0.00006105271,0.0000018820025,0.00026150743,0.7884567,0.0005517709,0.000457878,0.000012157149,0.00017336647],"about_ca_topic_score_codex":0.88596576,"about_ca_topic_score_gemma":0.9793783,"teacher_disagreement_score":0.18444814,"about_ca_system_score_codex":0.000008415689,"about_ca_system_score_gemma":0.000101858546,"threshold_uncertainty_score":0.35499677},"labels":[],"label_agreement":null},{"id":"W6898696708","doi":"10.57757/iugg23-3635","title":"Improved Greenland glacial isostatic adjustment models with 3D Earth structure inferred from the joint inversion of regional data sets","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Post-glacial rebound; Lithosphere; Geodetic datum; Inversion (geology); Ice sheet; Sea level; Data set; Earth model; Ice-sheet model","score_opus":0.07702331965584748,"score_gpt":0.30785355882860893,"score_spread":0.23083023917276146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6898696708","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.80167675,0.0001548557,0.001634793,0.011095091,0.0005626542,0.0024688202,0.18217354,0.00009585749,0.00013765159],"genre_scores_gemma":[0.8150856,0.00022512031,0.0049836696,0.00036193305,0.00041605264,0.000027585224,0.17851019,0.000014760798,0.00037507794],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9964406,0.0003029547,0.00038132365,0.00076480047,0.00140313,0.00070719386],"domain_scores_gemma":[0.99706155,0.0006170231,0.00023896781,0.0012883084,0.00053143495,0.00026268928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002000537,0.00018326158,0.00023252472,0.0002252976,0.00060358056,0.00029599178,0.0014900444,0.000060969593,0.0007203425],"category_scores_gemma":[0.00036624994,0.0001136073,0.000036337628,0.0011610128,0.00046618812,0.0015859418,0.00038242954,0.00019264666,0.000053400596],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019541758,0.00037652248,0.03184148,0.00071698456,0.00037564363,0.000018527906,0.0070186635,0.004449962,0.014320074,0.007298304,0.8186074,0.113022275],"study_design_scores_gemma":[0.0014015689,0.00021494195,0.16537377,0.00010056808,0.00004757561,0.000002852558,0.0006097967,0.7517509,0.00072236377,0.0060802996,0.07333967,0.00035569773],"about_ca_topic_score_codex":0.014425804,"about_ca_topic_score_gemma":0.013471307,"teacher_disagreement_score":0.7473009,"about_ca_system_score_codex":0.0000094812285,"about_ca_system_score_gemma":0.0005179888,"threshold_uncertainty_score":0.9921372},"labels":[],"label_agreement":null},{"id":"W6901795225","doi":"10.60692/v6m6e-hcs92","title":"Vaccine-associated enhanced disease: Case definition and guidelines for data collection, analysis, and presentation of immunization safety data","year":2021,"lang":"en","type":"article","venue":"Greater South Information System","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University Health Centre","funders":"","keywords":"Context (archaeology); Presentation (obstetrics); Preparedness; Term (time); Immunization; Case presentation","score_opus":0.08251177781885528,"score_gpt":0.26980681989812,"score_spread":0.18729504207926473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6901795225","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8726136,0.0000828748,0.11155846,0.00008371179,0.00023578429,0.00041957898,0.014878774,0.00003995329,0.000087257446],"genre_scores_gemma":[0.96947587,0.000014674837,0.0016193703,0.000025367515,0.000030970095,0.00000353326,0.028807081,0.0000019616891,0.000021201686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99893224,0.00009336139,0.0005583812,0.00018350496,0.00013956278,0.00009292078],"domain_scores_gemma":[0.9985065,0.000037118487,0.00035236706,0.00047965406,0.00056973036,0.000054659522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048884,0.00008885936,0.0002109615,0.00011586925,0.00019560813,0.00015224352,0.000115171904,0.00004400738,0.00003359029],"category_scores_gemma":[0.00023701301,0.000077351186,0.000017301069,0.0003930912,0.000011087176,0.001091496,0.00006741931,0.000017779646,0.0000037068976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00097357854,0.00001611333,0.9614267,0.0026996643,0.0019583139,0.00002903535,0.016725626,0.005921221,0.00012513457,0.00026975526,0.0023890808,0.0074657947],"study_design_scores_gemma":[0.0014038315,0.000030893418,0.637584,0.00010837141,0.0010188918,0.0000417109,0.0032031764,0.35563836,0.0005689275,0.000018584109,0.00017633369,0.00020692778],"about_ca_topic_score_codex":0.00048359326,"about_ca_topic_score_gemma":0.00017137021,"teacher_disagreement_score":0.34971714,"about_ca_system_score_codex":0.000003627412,"about_ca_system_score_gemma":0.00004884502,"threshold_uncertainty_score":0.31542897},"labels":[],"label_agreement":null},{"id":"W6903198140","doi":"10.7939/r3-ee96-7t52","title":"Hydrous Silicate Melts: A new Growth Medium for Diamond?","year":2009,"lang":"en","type":"dissertation","venue":"University of Alberta Library","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Halide; Alkali metal; Diamond; Silicate; Mantle (geology); Carbonate","score_opus":0.005278483855174162,"score_gpt":0.16558044704342545,"score_spread":0.1603019631882513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6903198140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85005176,0.0007307597,0.000020827152,0.0015010999,0.0012956295,0.0008359703,0.00054051244,0.00010191903,0.14492151],"genre_scores_gemma":[0.56761944,0.001194146,0.003434205,0.0003718971,0.00096193375,3.0659479e-7,0.041236,0.000041597334,0.38514045],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990657,0.000032331685,0.00016626566,0.0003283882,0.00016485326,0.00024248881],"domain_scores_gemma":[0.9991527,0.00019781568,0.0002356792,0.00020740245,0.000025777044,0.00018060952],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00003506371,0.00021463558,0.0004054933,0.000118738855,0.00011939541,0.00003988431,0.0005387089,0.00023384,0.0024063017],"category_scores_gemma":[0.000015886335,0.00022456494,0.0001691959,0.00011666458,0.000033645403,0.0005814424,0.000013241567,0.000092922644,0.00011712026],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0060278615,0.00030786323,0.011373777,0.002227271,0.0011029306,0.00012103936,0.024725245,0.00031725303,0.0015890644,0.0065972144,0.90511066,0.04049982],"study_design_scores_gemma":[0.002836834,0.0011594864,0.20129381,0.00050731713,0.0009023687,0.000004313389,0.0016361616,0.00044656423,0.014345351,0.032795917,0.7422297,0.0018421814],"about_ca_topic_score_codex":0.027586749,"about_ca_topic_score_gemma":0.011898207,"teacher_disagreement_score":0.28243232,"about_ca_system_score_codex":0.0000014665666,"about_ca_system_score_gemma":0.00025776256,"threshold_uncertainty_score":0.99850565},"labels":[],"label_agreement":null},{"id":"W6911969788","doi":"10.5281/zenodo.14740086","title":"Playing with Edges: The Influence of Arbitrary Definitions on Hotspot–LLSVP Correlations","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Agence Nationale de la Recherche","keywords":"Hotspot (geology); Mantle plume; Plume; Mantle (geology); Merge (version control); Volcanism; Geodynamics; Seismic tomography","score_opus":0.02787660674135729,"score_gpt":0.21028098096698075,"score_spread":0.18240437422562347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6911969788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79150885,0.000040736897,0.00048879953,0.00053393433,0.00008762417,0.00028723682,0.0005252229,0.00015300546,0.2063746],"genre_scores_gemma":[0.9988161,0.00004022678,0.000115516734,0.00017998714,0.000032148255,2.0734513e-8,0.0005547178,0.000056469227,0.00020483861],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99916613,0.00015058556,0.00015333774,0.00017437029,0.00018966959,0.00016589448],"domain_scores_gemma":[0.99932873,0.00009737362,0.00007221684,0.00026844608,0.00018544534,0.00004779872],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00025880226,0.00007932206,0.000093706905,0.000108548105,0.0016764782,0.00022775137,0.00046659596,0.000028954128,0.0033486788],"category_scores_gemma":[0.00014717325,0.000056569905,0.000022670958,0.00045665583,0.00017032039,0.00014767336,0.00007855163,0.00013761147,0.0015040627],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013181964,0.00073809165,0.0053694253,0.0006345076,0.00070278696,0.000059141243,0.007981121,0.19532157,0.016991166,0.46713838,0.1829455,0.12080011],"study_design_scores_gemma":[0.00068279705,0.0005367798,0.5034077,0.0002549317,0.00007184757,0.000029159037,0.00044665558,0.00097574317,0.00093907275,0.0043044705,0.48806685,0.0002839765],"about_ca_topic_score_codex":0.00012892365,"about_ca_topic_score_gemma":0.000004192195,"teacher_disagreement_score":0.4980383,"about_ca_system_score_codex":0.000004910567,"about_ca_system_score_gemma":0.000008088325,"threshold_uncertainty_score":0.9996232},"labels":[],"label_agreement":null},{"id":"W6920589467","doi":"10.60692/behwn-tkp10","title":"Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Greater South Information System","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Volcano; Impact crater; Induced seismicity; Spectral analysis; Polarization (electrochemistry); Unrest","score_opus":0.016592121881004274,"score_gpt":0.17275423043930718,"score_spread":0.1561621085583029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920589467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917449,0.0000030770764,0.0046552513,0.00010481516,0.00063054165,0.00036099897,0.00082800403,0.00008273678,0.0015896846],"genre_scores_gemma":[0.9991675,8.50062e-8,0.000052061867,0.000309333,0.00007504029,0.000013566173,0.0002822429,0.0000023308392,0.00009784753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990882,0.00010331431,0.00033923343,0.00011845999,0.00019786794,0.00015291623],"domain_scores_gemma":[0.99953204,0.000009760168,0.00017125954,0.00015526547,0.00004904705,0.00008263072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040627868,0.00011030281,0.00014087307,0.000117694464,0.00038002426,0.00018363273,0.000101167,0.00003292907,0.00024423853],"category_scores_gemma":[0.0000075202315,0.00008765931,0.000021925754,0.00016484412,0.000010964706,0.00055504905,0.000034501234,0.000058146656,0.00042111034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027515515,0.0000029368764,0.80654144,0.00031570188,0.000054634926,0.0000050939498,0.10981287,0.07779947,0.000032346943,0.00044277014,0.0014262706,0.0032912923],"study_design_scores_gemma":[0.0003756199,0.00011653081,0.968727,0.000022160762,0.000011685552,0.00003265835,0.0048555285,0.019215513,0.00024825486,0.000008290818,0.006172206,0.00021455593],"about_ca_topic_score_codex":0.00030175585,"about_ca_topic_score_gemma":0.000006870727,"teacher_disagreement_score":0.16218553,"about_ca_system_score_codex":0.0000138152745,"about_ca_system_score_gemma":0.000023154042,"threshold_uncertainty_score":0.5412662},"labels":[],"label_agreement":null},{"id":"W6921631654","doi":"10.7907/xqhn-dj49","title":"Shear Velocity Structure of the Mantle Beneath the North American Plate","year":2019,"lang":"en","type":"article","venue":"CaltechTHESIS (California Institute of Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Classification of discontinuities; Seismogram; Shear (geology); Mantle (geology); Tectonics; Discontinuity (linguistics); Velocity gradient; Shear zone","score_opus":0.005831603499711767,"score_gpt":0.18337665968230984,"score_spread":0.17754505618259808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6921631654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99658734,0.00008636604,0.00003005579,0.0007479499,0.00046194604,0.00035519025,0.0012898755,0.00005479018,0.00038646098],"genre_scores_gemma":[0.9984386,0.000040411007,0.0013219338,0.000095870026,0.000039935738,0.0000013780535,0.000024321724,0.000006206657,0.00003135457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883443,0.00003299328,0.0003331205,0.00025688528,0.000259446,0.00028312017],"domain_scores_gemma":[0.9987416,0.00003951403,0.0003439879,0.0007717353,0.000064256696,0.000038857826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012778406,0.0001815101,0.00039870266,0.000096501484,0.00014182941,0.000015681737,0.0010147786,0.00012169856,0.00032208173],"category_scores_gemma":[0.00006493537,0.00009608758,0.0001098853,0.000728005,0.00089129526,0.000077255805,0.00010193286,0.00022948574,0.00014852683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017734143,0.000061596824,0.8914643,0.00022005527,0.00025289026,0.0000069456587,0.00009976539,0.0074947625,0.02513099,0.005612833,0.00074179407,0.06873674],"study_design_scores_gemma":[0.00037161118,0.00020532272,0.7458373,0.00007204006,0.00011888416,0.000015959413,0.000081443715,0.0006352641,0.13125761,0.0046490952,0.11639957,0.00035594302],"about_ca_topic_score_codex":0.0009773597,"about_ca_topic_score_gemma":0.001284747,"teacher_disagreement_score":0.14562704,"about_ca_system_score_codex":0.00000520089,"about_ca_system_score_gemma":0.00007094594,"threshold_uncertainty_score":0.39183378},"labels":[],"label_agreement":null},{"id":"W6923789032","doi":"10.14288/1.0177104","title":"The Cumberland News","year":2012,"lang":"en","type":"article","venue":"Open Collections","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"News bureau; News media; Postal service; Newspaper","score_opus":0.016377767486661688,"score_gpt":0.2334931895115105,"score_spread":0.2171154220248488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6923789032","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011082127,0.00016308992,0.000031600823,0.00028840403,0.0021044998,0.00028516346,0.0000737779,0.000017522443,0.9859538],"genre_scores_gemma":[0.55011195,0.00010345982,0.00026098205,0.0001463714,0.00067565247,0.000013981782,0.000027636102,0.0000031050706,0.44865686],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995468,0.000048704864,0.00007721169,0.00006592467,0.00006611134,0.00019523047],"domain_scores_gemma":[0.9996534,0.00009844902,0.000027013692,0.00013290424,0.000015240089,0.00007301507],"candidate_categories":["sts","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000186892,0.000046352503,0.00006180538,0.0000062281974,0.0027717352,0.0011957714,0.00021321673,0.000018797053,0.0042547625],"category_scores_gemma":[0.000016530352,0.000027933589,0.000018640927,0.00021866395,0.000024044064,0.00023202317,0.000022343398,0.000035778827,0.00034395515],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017154818,0.000016229604,0.010186954,0.0000011153351,0.000021464028,3.3020518e-7,0.00008858844,0.00007062044,0.000022645198,0.00033100022,0.985502,0.0037419028],"study_design_scores_gemma":[0.00008409184,0.00001795821,0.018834066,0.0000012748243,0.000008567128,0.0000040879427,0.00006377252,0.000046669313,0.00006513592,0.0012703277,0.9795486,0.00005550492],"about_ca_topic_score_codex":0.070166655,"about_ca_topic_score_gemma":0.037692506,"teacher_disagreement_score":0.53902984,"about_ca_system_score_codex":0.0000012773236,"about_ca_system_score_gemma":0.000028730094,"threshold_uncertainty_score":0.9998411},"labels":[],"label_agreement":null},{"id":"W6926368740","doi":"10.25316/ir-14291","title":"Nanaimo Free Press [Saturday, October 23, 1880]","year":2020,"lang":"en","type":"other","venue":"VIUSpace (Vancouver Island University Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"","score_opus":0.006551046779647238,"score_gpt":0.16150109822956885,"score_spread":0.1549500514499216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6926368740","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006451479,0.0006409348,0.000051881794,0.00045678293,0.0024710489,0.00037668648,0.0050448393,0.0004873643,0.9904059],"genre_scores_gemma":[0.0012503962,0.0009327278,0.00086865865,0.00027975012,0.0010324449,2.3075522e-7,0.00024873068,0.00011920257,0.99526787],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99810725,0.00014449954,0.00015888127,0.0006959726,0.00039123476,0.00050215225],"domain_scores_gemma":[0.9986447,0.000063829284,0.00025540215,0.0006847665,0.000013369464,0.00033789864],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0000310633,0.00049726176,0.0006187277,0.00018269845,0.00015842558,0.00015870019,0.0011545982,0.00043447068,0.020130446],"category_scores_gemma":[0.000010358897,0.00045347528,0.00018697181,0.00029880376,0.00012358965,0.00059672596,0.00024278066,0.00032162687,0.0008127839],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000088319044,0.000019589745,0.00014703698,0.000118111995,0.00015771258,0.00026412067,0.00013262294,0.000042477375,0.0000056574863,0.00029591986,0.9984864,0.00024201993],"study_design_scores_gemma":[0.0007741676,0.00007982735,0.000273799,0.000093774725,0.0001238356,9.869124e-7,0.00007112324,0.000054550936,0.000072539064,0.00018515371,0.99765927,0.00061095605],"about_ca_topic_score_codex":0.009783104,"about_ca_topic_score_gemma":0.44334224,"teacher_disagreement_score":0.43355915,"about_ca_system_score_codex":0.000004938768,"about_ca_system_score_gemma":0.0001323366,"threshold_uncertainty_score":0.9999652},"labels":[],"label_agreement":null},{"id":"W6930467626","doi":"10.5281/zenodo.14186472","title":"Conolidine Reviews, Cost, Work, Price, Update & Benefits","year":2024,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pain relief; Recipe; Competitor analysis; Alternative medicine; Instant","score_opus":0.03598499770753866,"score_gpt":0.2300673711853081,"score_spread":0.19408237347776944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6930467626","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006931958,0.008707443,0.00006745711,0.0002881972,0.0007416404,0.00087331206,0.0030113372,0.00095387775,0.9852874],"genre_scores_gemma":[0.005862136,0.01944475,0.00045603287,0.00056616054,0.0027041466,1.23583e-7,0.028334718,0.0078034378,0.9348285],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982056,0.00024164448,0.00029229102,0.0005478843,0.00029283794,0.00041971277],"domain_scores_gemma":[0.9989961,0.000010395606,0.00018542152,0.0005027153,0.000097694865,0.00020772296],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00057077815,0.0002610521,0.00035760185,0.00024370197,0.0004156645,0.0009992897,0.0009297707,0.00014158165,0.30267397],"category_scores_gemma":[0.000101076985,0.00022958285,0.00007562355,0.00048587067,0.00009479854,0.0000980654,0.00031983486,0.00025781052,0.2823621],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013383418,0.000013451806,0.0000010898201,0.00020017392,0.00004858094,0.000013181355,0.00005282385,0.000014313971,0.000015337146,0.00084396487,0.92647046,0.07231325],"study_design_scores_gemma":[0.00012909198,0.000055166867,0.000089719986,0.0002963221,0.00003567503,0.000016959633,0.0000062615486,0.000016092352,0.0000137685865,0.00011989041,0.9989589,0.0002621556],"about_ca_topic_score_codex":0.00011639318,"about_ca_topic_score_gemma":0.0000047932836,"teacher_disagreement_score":0.07248845,"about_ca_system_score_codex":0.000011160147,"about_ca_system_score_gemma":0.0000034970585,"threshold_uncertainty_score":0.9636173},"labels":[],"label_agreement":null},{"id":"W6939483196","doi":"10.6084/m9.figshare.25001664.v1","title":"Additional file 1 of What do primary care providers want to know when caring for patients living with frailty? An analysis of eConsult communications between primary care providers and specialists","year":2024,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ottawa Hospital; Bruyère; University of Ottawa","funders":"","keywords":"Primary care; MEDLINE; Primary health care; Need to know; Qualitative research","score_opus":0.01928641956612191,"score_gpt":0.22758307201128203,"score_spread":0.20829665244516013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939483196","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01358494,0.00077557267,5.0061493e-7,0.000020684438,0.000027083539,0.00056108483,0.98444027,0.000022972132,0.000566867],"genre_scores_gemma":[0.16809349,0.000008232525,0.0015622686,0.000027979742,0.0000657466,0.000120820216,0.8300861,0.000008134861,0.000027202668],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9990084,0.000050087463,0.0002480024,0.00029958237,0.00022174224,0.00017215032],"domain_scores_gemma":[0.99809194,0.0010266618,0.00013133258,0.0003448844,0.0002996992,0.00010547404],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000028397875,0.00014149657,0.00032577524,0.0001644427,0.00012972108,0.00025480773,0.00028525703,0.000059367125,0.2381168],"category_scores_gemma":[0.00015582709,0.00012094348,0.00007459253,0.00023263105,0.000029492212,0.00068537705,0.00008546545,0.00006127888,0.000020685073],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005676681,0.000058950165,0.016724557,0.007613478,0.0009998006,0.0000030496983,0.023575207,0.0007340751,0.000020946478,0.000005685214,0.79931086,0.15089662],"study_design_scores_gemma":[0.00019432219,0.0004652735,0.5918443,0.012217907,0.00051604,4.0143397e-7,0.003979391,0.000294538,0.00004850812,0.000024857203,0.3899846,0.00042984486],"about_ca_topic_score_codex":0.00034614632,"about_ca_topic_score_gemma":0.0028408333,"teacher_disagreement_score":0.57511973,"about_ca_system_score_codex":0.000019156148,"about_ca_system_score_gemma":0.00024056432,"threshold_uncertainty_score":0.7625797},"labels":[],"label_agreement":null},{"id":"W6939996337","doi":"10.6084/m9.figshare.c.7747526.v1","title":"ASFV pS183L protein negatively regulates RLR-mediated antiviral signalling by blocking MDA5 oligomerisation","year":2025,"lang":"en","type":"other","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"MDA5; RIG-I; Blocking (statistics); Helicase; HEK 293 cells; Receptor; Gene; TSG101","score_opus":0.011416550188130793,"score_gpt":0.20343013616776545,"score_spread":0.19201358597963467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939996337","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0007877933,0.0016295814,0.0000041187695,0.000051556483,0.0003051886,0.0010456904,0.717993,0.0003700548,0.277813],"genre_scores_gemma":[0.07345616,0.000031755786,0.0002247432,0.00012545835,0.0009009901,0.00005686356,0.6465288,0.000114798175,0.27856043],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99851793,0.00010495248,0.00026032547,0.0004560159,0.00029640103,0.00036439107],"domain_scores_gemma":[0.99921983,0.0001024231,0.00034761697,0.00020162108,0.000055205346,0.00007332842],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00006684471,0.00034370387,0.00042312418,0.00014653665,0.00011355808,0.00019023735,0.0003218469,0.00032384013,0.33815685],"category_scores_gemma":[0.0001929309,0.0003076082,0.00007984918,0.0002234193,0.000014904612,0.00011558177,0.000034767385,0.00017523224,0.004078311],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009435946,0.000009500655,0.00003240014,0.00035659858,0.00007240725,0.000007157265,0.000042855514,0.00003554533,0.0020214778,0.0000032680741,0.9948181,0.0025912644],"study_design_scores_gemma":[0.00022947819,0.000053536594,0.00054813473,0.00461012,0.000028181268,3.9738154e-7,0.000012709949,0.0005016888,0.011780295,0.00013473525,0.98155,0.0005507722],"about_ca_topic_score_codex":0.0015556546,"about_ca_topic_score_gemma":0.00036082955,"teacher_disagreement_score":0.33407855,"about_ca_system_score_codex":0.0000043711834,"about_ca_system_score_gemma":0.000114061884,"threshold_uncertainty_score":0.9999376},"labels":[],"label_agreement":null},{"id":"W6940359487","doi":"10.7275/55287","title":"Seismic Imaging of the Middle American Subduction Zone and Alaska-Northwestern Canada: News Insights into Subduction Dynamics and Tectonic Evolution","year":2025,"lang":"en","type":"dissertation","venue":"ScholarWorks@UMassAmherst (University of Massachusetts Amherst)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Tectonics; Geophysical imaging; Seismic tomography; Plate tectonics; Geodynamics","score_opus":0.00513572091116144,"score_gpt":0.1656964165668884,"score_spread":0.16056069565572698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6940359487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99474996,0.0017518504,0.00036546058,0.00045372205,0.0014029625,0.00043149944,0.00021357222,0.000030928553,0.0006000231],"genre_scores_gemma":[0.9960334,0.000572268,0.00023908018,0.00002394172,0.00006752258,5.056827e-7,0.00086727605,0.000014806495,0.0021812478],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782693,0.00028608882,0.00036297654,0.0006448181,0.0005365132,0.00034264286],"domain_scores_gemma":[0.9981803,0.00009412355,0.00088544836,0.00046070106,0.00023637286,0.00014300067],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0002552982,0.0003936386,0.00065356574,0.00028806168,0.000662012,0.00008841344,0.00044485135,0.00024093437,0.00006841797],"category_scores_gemma":[0.00002761686,0.00039377864,0.00012708176,0.0006451047,0.00035832875,0.00064736785,0.00007230613,0.00055735884,0.0000021842227],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014360973,0.00016869033,0.86645484,0.0027626667,0.0011874975,0.000042879466,0.011574439,0.008663924,0.0022645544,0.00056197494,0.0022919716,0.10259045],"study_design_scores_gemma":[0.0009220051,0.00012219635,0.94625896,0.0006995857,0.0007123652,0.000008394503,0.037990324,0.00942396,0.0001943266,0.00053486007,0.0024293072,0.00070370606],"about_ca_topic_score_codex":0.7903519,"about_ca_topic_score_gemma":0.96783745,"teacher_disagreement_score":0.17748557,"about_ca_system_score_codex":0.000184003,"about_ca_system_score_gemma":0.0006771726,"threshold_uncertainty_score":0.9998514},"labels":[],"label_agreement":null},{"id":"W6943695731","doi":"10.17605/osf.io/7mbpk","title":"Post-critical SsPmp and its Applications to Virtual Deep Seismic Sounding (VDSS) 2: 1D Imaging of the Crust/Mantle and Joint Constraints with Receiver Function","year":2019,"lang":"en","type":"article","venue":"OSF Preprints (OSF Preprints)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Joint (building); Receiver function; Depth sounding; Crust; Lithosphere; Reflection (computer programming); Waveform","score_opus":0.007557297481035687,"score_gpt":0.20831391227228607,"score_spread":0.2007566147912504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6943695731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.962597,0.0000052178348,0.0033782367,0.00034493834,0.0002502352,0.0008464314,0.00008411024,0.000034380104,0.032459423],"genre_scores_gemma":[0.99683285,0.000015287134,0.00033052848,0.00019550072,0.000042409953,0.000017127282,0.000011030025,0.000007734227,0.002547507],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982997,0.00017151643,0.0002666358,0.00077817985,0.00023126889,0.00025266022],"domain_scores_gemma":[0.9986343,0.00029869055,0.00010865821,0.0006914392,0.000117725605,0.00014921694],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001001914,0.00015859804,0.000239375,0.000062340216,0.00018545677,0.000106068204,0.00023329478,0.000059182148,0.043104347],"category_scores_gemma":[0.00028833098,0.0001240102,0.00003957621,0.00011266012,0.00021177463,0.00023501116,0.00021647784,0.00014769084,0.038133442],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008897695,0.00026869238,0.45163277,0.0007361868,0.00038556627,0.000014137221,0.0057101944,0.017816447,0.37573475,0.023170967,0.0010615854,0.122578934],"study_design_scores_gemma":[0.0011637997,0.000026976111,0.93384033,0.00030165596,0.00024078204,0.00015076176,0.001531994,0.013433909,0.029757349,0.005508369,0.013265701,0.00077838736],"about_ca_topic_score_codex":0.00032926202,"about_ca_topic_score_gemma":0.00007117496,"teacher_disagreement_score":0.48220754,"about_ca_system_score_codex":0.000008100062,"about_ca_system_score_gemma":0.0000562036,"threshold_uncertainty_score":0.9626155},"labels":[],"label_agreement":null},{"id":"W6948795132","doi":"10.5281/zenodo.10927348","title":"Understanding the influence of seismic mantle structures at the core-mantle boundary on intense magnetic flux regions","year":2024,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Core–mantle boundary; Mantle (geology); Seismogram; Seismic anisotropy; Anisotropy; Shear wave splitting; Seismic wave; Shear (geology)","score_opus":0.05263949895427165,"score_gpt":0.2323892025730577,"score_spread":0.17974970361878606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6948795132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.963211,0.0004890816,0.00041551274,0.0015416074,0.00037096784,0.00040330598,0.00077919115,0.00022861619,0.03256074],"genre_scores_gemma":[0.99752283,0.00007971588,0.0000062154845,0.00018209583,0.00008044,1.2506119e-8,0.00036890502,0.00009829445,0.0016615049],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989578,0.00018017212,0.00015398617,0.00021909384,0.00027713703,0.0002117824],"domain_scores_gemma":[0.99938965,0.00009560824,0.000050118993,0.0003255643,0.00008362216,0.000055427412],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004074602,0.000096211275,0.00009084635,0.0000703424,0.0016178761,0.0005521379,0.0005889464,0.000026196465,0.013514594],"category_scores_gemma":[0.00009955484,0.00005737273,0.00003717899,0.00028698647,0.00036652863,0.000108506305,0.00020985116,0.00015552966,0.003420543],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040431847,0.000043332973,0.00008103576,0.0004033635,0.00019984963,0.000102890095,0.01031145,0.035805497,0.021074466,0.0811633,0.81737405,0.033036426],"study_design_scores_gemma":[0.00015034046,0.000314806,0.009848001,0.000087613065,0.000036648442,0.00010461308,0.0006531913,0.0043383534,0.0005574119,0.01318815,0.97056067,0.00016020179],"about_ca_topic_score_codex":0.00016766804,"about_ca_topic_score_gemma":0.000010258695,"teacher_disagreement_score":0.15318659,"about_ca_system_score_codex":0.000020956639,"about_ca_system_score_gemma":0.0000061978076,"threshold_uncertainty_score":0.9996819},"labels":[],"label_agreement":null},{"id":"W6948978275","doi":"10.5281/zenodo.12658821","title":"Investigation of seismic anisotropy in the D'' layer and at the CMB regarding intense magnetic flux regions","year":2024,"lang":"en","type":"article","venue":"Open MIND","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Shear wave splitting; Core–mantle boundary; Seismic anisotropy; Mantle (geology); Anisotropy; Shear (geology); Shear waves; Seismic wave","score_opus":0.0397421190529265,"score_gpt":0.2508985547685594,"score_spread":0.21115643571563286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6948978275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99404573,0.0005103043,0.000004321017,0.0017472861,0.00014652795,0.0002106406,0.000069356705,9.050757e-7,0.0032649369],"genre_scores_gemma":[0.9979557,0.0000373908,0.00018236053,0.0001226989,0.000041299474,0.0000018098492,0.000044545148,0.000001748949,0.0016124665],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994493,0.00011381537,0.00011741064,0.00013798365,0.00008743856,0.000094045135],"domain_scores_gemma":[0.99965024,0.00014613598,0.000027900282,0.00014304953,0.000011092993,0.000021587242],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045805256,0.000057205052,0.00008537874,0.000022815082,0.00008233957,0.0002001202,0.00020106549,0.00002049738,0.0011248763],"category_scores_gemma":[0.000014027675,0.000029550192,0.000015016297,0.000121822195,0.000090907175,0.00013054973,0.00004184214,0.000053399817,0.00012698726],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005612764,0.000041028292,0.1535938,0.000428802,0.00023077,0.0004376254,0.108936846,0.003848308,0.26205572,0.0050108726,0.14163423,0.32322073],"study_design_scores_gemma":[0.0009832687,0.00058424595,0.38257092,0.0006151714,0.00025586822,0.00018821412,0.004572203,0.020572579,0.042127546,0.024542382,0.52236146,0.0006261537],"about_ca_topic_score_codex":0.001925239,"about_ca_topic_score_gemma":0.001735268,"teacher_disagreement_score":0.3807272,"about_ca_system_score_codex":0.0000014376736,"about_ca_system_score_gemma":0.00002572938,"threshold_uncertainty_score":0.9997882},"labels":[],"label_agreement":null},{"id":"W6950198441","doi":"10.5281/zenodo.4216198","title":"ReGaRder L'un des nôtres (2020) Streaming VF Film Complet Gratuit en Vostfr cmj","year":2020,"lang":"fr","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Historical heritage; Motor area; Mental deficiency","score_opus":0.03296267298961506,"score_gpt":0.21547722110225803,"score_spread":0.18251454811264298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950198441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5707307,0.011858887,0.005230267,0.03880788,0.0033801533,0.0027009377,0.022226868,0.002794619,0.34226972],"genre_scores_gemma":[0.98092455,0.0015105779,0.0012708536,0.00079117133,0.0016952896,3.250787e-8,0.006679821,0.00082639843,0.0063013383],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9968104,0.0009271744,0.00039667822,0.00064576213,0.0004929325,0.0007270592],"domain_scores_gemma":[0.998472,0.00009013498,0.00015826692,0.0003823061,0.00036783403,0.0005294954],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0006165612,0.00028981126,0.0003312173,0.00008272029,0.0025471828,0.0016565181,0.0011888568,0.00012999939,0.15437283],"category_scores_gemma":[0.000622745,0.00029883452,0.00009188605,0.0006080569,0.0004047439,0.0004972086,0.00069048576,0.0003502268,0.0307349],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019492819,0.00014680541,0.00013036485,0.0005643806,0.00022199916,0.00022217489,0.008659886,0.0018696529,0.0061744126,0.0034808076,0.7226159,0.2557187],"study_design_scores_gemma":[0.000457042,0.00047340975,0.005389794,0.00007698898,0.000057059853,0.00007275799,0.0005357815,0.0023820938,0.0006439019,0.0005194684,0.9890493,0.0003423764],"about_ca_topic_score_codex":0.0006645708,"about_ca_topic_score_gemma":0.000014748252,"teacher_disagreement_score":0.41019383,"about_ca_system_score_codex":0.000026458461,"about_ca_system_score_gemma":0.000011006306,"threshold_uncertainty_score":0.99994636},"labels":[],"label_agreement":null},{"id":"W6955027572","doi":"10.57907/mirri/0ao9bb","title":"MIRRI0052244","year":2022,"lang":"en","type":"dataset","venue":"Entrepôt pour orphelin","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Organism; Taxon; Identification (biology); Segmented filamentous bacteria","score_opus":0.010488613788732159,"score_gpt":0.20914045775859166,"score_spread":0.1986518439698595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6955027572","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011274479,0.00064664136,0.0000015419032,0.00023172086,0.0033113249,0.00021851693,0.9943235,0.00005673669,0.00008255838],"genre_scores_gemma":[0.00016643447,0.00039147062,0.000078433055,0.00043005685,0.0009577344,0.000005539086,0.99559623,0.000009041695,0.002365035],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979092,0.00021022258,0.00038126935,0.000525531,0.0005034907,0.0004703],"domain_scores_gemma":[0.9987581,0.00016175924,0.0002474976,0.0006265006,0.000029089328,0.00017705064],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033109292,0.00034300046,0.00042788757,0.000105966676,0.00022136011,0.00014272299,0.0006979644,0.00017425179,0.99540114],"category_scores_gemma":[0.00005307252,0.00030239733,0.00015498008,0.00012718397,0.000040240633,0.00008120536,0.00009194694,0.0003571405,0.40436858],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023787037,0.000033402463,0.000113362075,0.000049850423,0.00005236116,0.00013336902,0.000013242067,0.00025640664,0.000019318697,0.000005074465,0.9984413,0.00085856154],"study_design_scores_gemma":[0.00021086239,0.00005451786,0.00048475267,0.00001439605,0.00007987624,0.000012384377,0.000018647905,0.000014808136,0.00004362817,0.000257652,0.99844086,0.00036761022],"about_ca_topic_score_codex":0.009907269,"about_ca_topic_score_gemma":0.001761639,"teacher_disagreement_score":0.59103256,"about_ca_system_score_codex":0.000007014971,"about_ca_system_score_gemma":0.00016705066,"threshold_uncertainty_score":0.99994284},"labels":[],"label_agreement":null},{"id":"W6955031182","doi":"10.58066/h21j-yp79","title":"72nd Tug of War Team [Wills Photograph Album Page 51]","year":2023,"lang":"en","type":"other","venue":"UVic’s Research and Learning Repository (University of Victoria)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tug of war; Photography; Photojournalism; Period (music)","score_opus":0.015528136295479902,"score_gpt":0.22940178912182085,"score_spread":0.21387365282634097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6955031182","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.29774317,0.005199721,0.000018500124,0.00006163612,0.0034714914,0.0010179055,0.0006761748,0.0005174904,0.6912939],"genre_scores_gemma":[0.46268806,0.004841448,0.00031007727,0.0000031977443,0.0010761144,5.642941e-7,0.00020599396,0.00015719906,0.5307173],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99754936,0.00055007637,0.00018381902,0.00047716222,0.00077894056,0.0004606619],"domain_scores_gemma":[0.9985031,0.00046916967,0.00027529194,0.00034909125,0.00016322151,0.00024016346],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00096501823,0.00020976768,0.000531925,0.0005020523,0.00042309827,0.00004531758,0.0004587146,0.00032589916,0.0021068489],"category_scores_gemma":[0.00008974114,0.00021813724,0.00012174988,0.00046588192,0.0005045579,0.000115186696,0.000108438624,0.0006026985,0.0001642654],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012863358,0.0003603028,0.15220872,0.003921154,0.002012665,0.0009022738,0.008700319,0.0003804991,0.030966187,0.00020285718,0.78527224,0.013786432],"study_design_scores_gemma":[0.0005426382,0.0006741252,0.034690276,0.0005444019,0.00006447018,0.000005025279,0.0015687149,0.00014197422,0.00033787463,0.000091373266,0.9609811,0.00035803256],"about_ca_topic_score_codex":0.043601472,"about_ca_topic_score_gemma":0.0032385245,"teacher_disagreement_score":0.17570885,"about_ca_system_score_codex":0.000008687186,"about_ca_system_score_gemma":0.00011914468,"threshold_uncertainty_score":0.99880534},"labels":[],"label_agreement":null},{"id":"W6955069091","doi":"10.57907/mirri/wqnmy0","title":"MIRRI0041724","year":2022,"lang":"en","type":"dataset","venue":"Entrepôt pour orphelin","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Organism; Taxon; Mucor; Identification (biology)","score_opus":0.010276320889432249,"score_gpt":0.2090491851650107,"score_spread":0.19877286427557844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6955069091","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010867098,0.00073454896,0.0000015695132,0.0002386833,0.0034563588,0.00022136363,0.99412936,0.00005770857,0.00007368782],"genre_scores_gemma":[0.0001544118,0.00038462432,0.00008183468,0.00044430906,0.0009690087,0.0000063878692,0.99558634,0.000009090787,0.0023639908],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979102,0.00020765595,0.00038043162,0.00052689854,0.0005073011,0.00046748327],"domain_scores_gemma":[0.99876887,0.0001552149,0.00024203009,0.00062944845,0.00002909736,0.0001753493],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00033383243,0.00034301484,0.0004268515,0.00010646178,0.00022006921,0.00014437288,0.0006985157,0.00017193802,0.9956297],"category_scores_gemma":[0.00005020705,0.00030178894,0.00015754644,0.00012966906,0.000040056242,0.00008035253,0.00009203219,0.00035902107,0.39201397],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023452427,0.00003360014,0.00010779332,0.000053470267,0.000053985907,0.00014172494,0.000013373727,0.00025220474,0.000017653683,0.000005312247,0.9983176,0.0009798411],"study_design_scores_gemma":[0.00020742835,0.000055690783,0.000442338,0.0000150111355,0.00008339768,0.000012739659,0.000018721616,0.000014463661,0.000037032816,0.0002960075,0.99844813,0.00036903523],"about_ca_topic_score_codex":0.010738051,"about_ca_topic_score_gemma":0.0016156886,"teacher_disagreement_score":0.60361576,"about_ca_system_score_codex":0.0000070579345,"about_ca_system_score_gemma":0.00016731452,"threshold_uncertainty_score":0.99994344},"labels":[],"label_agreement":null},{"id":"W6955326608","doi":"10.58066/rcpj-nw78","title":"Explaining mortar (civilian technicians)","year":2023,"lang":"en","type":"other","venue":"UVic’s Research and Learning Repository (University of Victoria)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Newspaper; Photography; Mortar; Harbour","score_opus":0.021965498181640414,"score_gpt":0.243390280803443,"score_spread":0.22142478262180257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6955326608","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06365305,0.001863599,0.000038928258,0.00010001811,0.0022457887,0.00056570134,0.00014136046,0.00092327804,0.93046826],"genre_scores_gemma":[0.27320555,0.0015215467,0.0003332379,0.000003038992,0.0011562873,4.4771087e-7,0.00010482004,0.00015314137,0.72352195],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99786943,0.00034730165,0.00013885707,0.00048926246,0.0006759232,0.00047922437],"domain_scores_gemma":[0.9989052,0.0002793237,0.0001808138,0.00030695205,0.00010560507,0.0002221185],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00074512034,0.00019565731,0.0004032231,0.0004003697,0.0006581176,0.00008762483,0.00042233834,0.00032344245,0.0021278388],"category_scores_gemma":[0.00007251265,0.00021700693,0.00007277991,0.00037103577,0.00034323378,0.00011966797,0.00009787132,0.0007301752,0.00039551943],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070742425,0.00020161939,0.15975209,0.0023777909,0.0014911488,0.0031485716,0.009189214,0.0008377961,0.0071310108,0.0009604192,0.7784693,0.03573358],"study_design_scores_gemma":[0.0002895342,0.00042421272,0.01945763,0.00044840804,0.000034327557,0.000006062488,0.0019514946,0.00021333364,0.000043596407,0.000088832334,0.9767358,0.00030676823],"about_ca_topic_score_codex":0.03229353,"about_ca_topic_score_gemma":0.009478559,"teacher_disagreement_score":0.20955251,"about_ca_system_score_codex":0.000011263076,"about_ca_system_score_gemma":0.0001048821,"threshold_uncertainty_score":0.99878436},"labels":[],"label_agreement":null},{"id":"W6955498224","doi":"10.58079/jij","title":"Ambiances en acte(s)","year":2011,"lang":"en","type":"other","venue":"OpenEdition (OpenEdition)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nature versus nurture; Work (physics); Architecture; Field (mathematics)","score_opus":0.017033769485134288,"score_gpt":0.20994974095954774,"score_spread":0.19291597147441344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6955498224","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00028379363,0.0007384622,0.00011954866,0.001288018,0.006636381,0.0007036288,0.0048887893,0.0003219944,0.9850194],"genre_scores_gemma":[0.043716285,0.0019536596,0.0021412764,0.009483847,0.008308164,0.00010587631,0.018642023,0.00027188085,0.91537696],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976155,0.00022075845,0.00042317167,0.00069554773,0.00053637003,0.0005086575],"domain_scores_gemma":[0.9985763,0.00008744047,0.0004539865,0.0005554791,0.00007129772,0.00025548702],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00032995615,0.0004929524,0.00061577786,0.00022334546,0.00021365687,0.00028674176,0.0007235475,0.00045926255,0.35573587],"category_scores_gemma":[0.000035015306,0.00044171643,0.00014933107,0.00020076617,0.00014826369,0.0031201816,0.000054632448,0.00024287213,0.035327744],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004544936,0.00006366217,0.00021016019,0.00013800059,0.00013608151,0.00005738977,0.0000440938,0.000015084905,0.000057990652,0.010281215,0.9817811,0.0071697193],"study_design_scores_gemma":[0.00034972394,0.00012625857,0.021628747,0.00024022679,0.00008712615,0.000011567877,0.000022018432,0.000007833616,0.00038701552,0.001632083,0.9748836,0.0006237696],"about_ca_topic_score_codex":0.00449217,"about_ca_topic_score_gemma":0.016919667,"teacher_disagreement_score":0.3204081,"about_ca_system_score_codex":0.000008310687,"about_ca_system_score_gemma":0.00010941953,"threshold_uncertainty_score":0.9998035},"labels":[],"label_agreement":null},{"id":"W6957797564","doi":"10.60692/5x207-hve57","title":"Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Greater South Information System","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Volcano; Impact crater; Induced seismicity; Spectral analysis; Polarization (electrochemistry); Unrest","score_opus":0.016592121881004274,"score_gpt":0.17275423043930718,"score_spread":0.1561621085583029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6957797564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917449,0.0000030770764,0.0046552513,0.00010481516,0.00063054165,0.00036099897,0.00082800403,0.00008273678,0.0015896846],"genre_scores_gemma":[0.9991675,8.50062e-8,0.000052061867,0.000309333,0.00007504029,0.000013566173,0.0002822429,0.0000023308392,0.00009784753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990882,0.00010331431,0.00033923343,0.00011845999,0.00019786794,0.00015291623],"domain_scores_gemma":[0.99953204,0.000009760168,0.00017125954,0.00015526547,0.00004904705,0.00008263072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040627868,0.00011030281,0.00014087307,0.000117694464,0.00038002426,0.00018363273,0.000101167,0.00003292907,0.00024423853],"category_scores_gemma":[0.0000075202315,0.00008765931,0.000021925754,0.00016484412,0.000010964706,0.00055504905,0.000034501234,0.000058146656,0.00042111034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027515515,0.0000029368764,0.80654144,0.00031570188,0.000054634926,0.0000050939498,0.10981287,0.07779947,0.000032346943,0.00044277014,0.0014262706,0.0032912923],"study_design_scores_gemma":[0.0003756199,0.00011653081,0.968727,0.000022160762,0.000011685552,0.00003265835,0.0048555285,0.019215513,0.00024825486,0.000008290818,0.006172206,0.00021455593],"about_ca_topic_score_codex":0.00030175585,"about_ca_topic_score_gemma":0.000006870727,"teacher_disagreement_score":0.16218553,"about_ca_system_score_codex":0.0000138152745,"about_ca_system_score_gemma":0.000023154042,"threshold_uncertainty_score":0.5412662},"labels":[],"label_agreement":null},{"id":"W6958946674","doi":"10.6084/m9.figshare.c.6962497","title":"Efficacy and safety comparison of infrared laser moxibustion and traditional moxibustion in knee osteoarthritis: study protocol for a Zelen-design randomized controlled non-inferiority clinical trial","year":2024,"lang":"en","type":"other","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Moxibustion; Osteoarthritis; Clinical trial; Randomized controlled trial; Protocol (science); Visual analogue scale; Adverse effect","score_opus":0.08499203973464409,"score_gpt":0.3496287497551338,"score_spread":0.2646367100204897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6958946674","genre_codex":"protocol","genre_gemma":"protocol","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"protocol","genre_consensus":"protocol","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0014057467,0.0003875745,0.000036530528,0.000016719883,0.0006981128,0.792697,0.19692323,0.0001159254,0.00771918],"genre_scores_gemma":[0.10997914,0.000027736065,0.0009488527,0.00005372481,0.0047220928,0.74025095,0.12499652,0.0002957046,0.018725315],"study_design_codex":"randomized_trial","study_design_gemma":"randomized_trial","domain_scores_codex":[0.9971715,0.00073148205,0.0011410217,0.00047878758,0.00027577797,0.00020138508],"domain_scores_gemma":[0.99737185,0.0017313194,0.0005838047,0.00015947034,0.000059695914,0.00009388557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011159052,0.00031429194,0.0021032079,0.00016922998,0.000048074737,0.00011893127,0.00010295517,0.0003667561,0.024709713],"category_scores_gemma":[0.0011101762,0.00024097688,0.00018518676,0.00009290143,0.00004445125,0.00008634277,0.000023307697,0.0002261283,0.000075403645],"study_design_candidate":"randomized_trial","study_design_consensus":"randomized_trial","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.82731026,0.00047751158,0.000060522747,0.0011654609,0.00027851597,0.000008548486,0.0001478838,0.00021691003,0.0000014762616,0.000006121937,0.1658755,0.0044512805],"study_design_scores_gemma":[0.9698372,0.0033900081,0.0023716334,0.0032776769,0.00022943762,8.920516e-7,0.00003006676,0.0030690234,0.0000033734373,0.00026481602,0.017191457,0.00033444347],"about_ca_topic_score_codex":0.000094055205,"about_ca_topic_score_gemma":0.00023643747,"teacher_disagreement_score":0.14868404,"about_ca_system_score_codex":0.0000036592155,"about_ca_system_score_gemma":0.0001227081,"threshold_uncertainty_score":0.9826752},"labels":[],"label_agreement":null},{"id":"W6966869922","doi":"10.48380/dggv-stpw-7x38","title":"Cenozoic evolution of the Icelandic Plume and its influence upon the topographic evolution of Northwest Europe","year":2021,"lang":"en","type":"article","venue":"dggv-e-publications","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Plume; Upwelling; Cenozoic; Mantle plume; Convection; Sill; Seafloor spreading; Gravity anomaly; Mantle (geology)","score_opus":0.007877860765630554,"score_gpt":0.19284541986083023,"score_spread":0.18496755909519969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6966869922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99489903,0.0013965319,0.000051687715,0.0013923339,0.00018505506,0.00018557122,0.00039800617,0.000019416086,0.0014723747],"genre_scores_gemma":[0.9993919,0.00012740628,0.000028413695,0.000033921777,0.00004905091,0.000004601919,0.000104106664,0.0000028303157,0.00025774876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904054,0.00015648508,0.00025151973,0.00018265155,0.00021932424,0.0001495044],"domain_scores_gemma":[0.9988641,0.00010250437,0.00020067234,0.00039082952,0.00039374497,0.000048109632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024614838,0.00008456555,0.00012392197,0.00006938582,0.00026028143,0.000048882845,0.00028408656,0.00004505033,0.00020574575],"category_scores_gemma":[0.00016807695,0.000053190866,0.000046150813,0.0010486261,0.00011457829,0.00023396204,0.00004201891,0.00008140146,0.000020634083],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001171223,0.000075099444,0.89778626,0.00008223938,0.000055268258,3.813178e-7,0.0004546347,0.0020096118,0.02461835,0.07396659,0.00038369754,0.0005561338],"study_design_scores_gemma":[0.00009323463,0.000021417825,0.98777163,0.000017545453,0.000037950285,0.0000049431046,0.00005884796,0.00046804184,0.0007019256,0.0009512235,0.009810174,0.000063037856],"about_ca_topic_score_codex":0.0027775725,"about_ca_topic_score_gemma":0.0052470425,"teacher_disagreement_score":0.08998538,"about_ca_system_score_codex":0.000004286399,"about_ca_system_score_gemma":0.00017531568,"threshold_uncertainty_score":0.41988772},"labels":[],"label_agreement":null},{"id":"W6966915962","doi":"10.48550/arxiv.1710.04191","title":"Isochoric, isobaric and ultrafast conductivities of aluminum, lithium and carbon in the warm dense matter (WDM) regime","year":2017,"lang":"en","type":"preprint","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Warm dense matter; Isochoric process; Isobaric process; Lithium (medication); Carbon fibers; Ion; Thermodynamic equilibrium; Ultrashort pulse","score_opus":0.017833975790131865,"score_gpt":0.22053006392461477,"score_spread":0.20269608813448292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6966915962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9736899,0.0005268255,0.0000010241777,0.0009415897,0.0005510895,0.00027317388,0.00022212508,0.000007550062,0.023786707],"genre_scores_gemma":[0.99863034,0.00038041678,0.00010259425,0.00010470849,0.00021030959,0.0000060342577,0.000041271236,0.000005372859,0.00051896024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998848,0.00015333225,0.00022341375,0.0003456083,0.00020577549,0.00022386927],"domain_scores_gemma":[0.9991052,0.00014484323,0.00021330435,0.00045476516,0.000032305106,0.000049592392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046754882,0.00020577224,0.0004095904,0.00006325843,0.000088236484,0.00019218723,0.0003207565,0.00016527396,0.00027322883],"category_scores_gemma":[0.000023931336,0.00014104604,0.000035932488,0.000029382592,0.00023472402,0.00008684698,0.00009113341,0.00026277374,0.000010809982],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051801035,0.00022651177,0.8014673,0.004522771,0.00052491704,0.00025917238,0.05510986,0.00034067573,0.103131145,0.0012188961,0.018912861,0.01376791],"study_design_scores_gemma":[0.0007289195,0.00020596535,0.9227411,0.0004245995,0.0002172206,0.00007556336,0.001042754,0.0005928101,0.008824575,0.056187637,0.008082283,0.00087658473],"about_ca_topic_score_codex":0.006639365,"about_ca_topic_score_gemma":0.00071001257,"teacher_disagreement_score":0.121273816,"about_ca_system_score_codex":0.0000017573666,"about_ca_system_score_gemma":0.000045755787,"threshold_uncertainty_score":0.9999755},"labels":[],"label_agreement":null},{"id":"W6968248803","doi":"10.5281/zenodo.12658820","title":"Investigation of seismic anisotropy in the D'' layer and at the CMB regarding intense magnetic flux regions","year":2024,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Shear wave splitting; Core–mantle boundary; Seismic anisotropy; Mantle (geology); Anisotropy; Shear (geology); Shear waves; Seismic wave","score_opus":0.03305017705193835,"score_gpt":0.21575248134376296,"score_spread":0.1827023042918246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6968248803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9843494,0.0005762332,0.00011702609,0.0029268241,0.00013240063,0.00029998441,0.00023553424,0.00009994164,0.01126262],"genre_scores_gemma":[0.9985456,0.00011925092,0.000031543997,0.00015555734,0.00006529151,1.7619083e-8,0.00043698077,0.00006335733,0.0005824413],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99900156,0.0003463384,0.0001424408,0.0001803412,0.00018024122,0.00014905368],"domain_scores_gemma":[0.9995807,0.00007183191,0.00003525898,0.00020069265,0.000070581,0.000040927993],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007038028,0.00006797203,0.00007589463,0.00007471427,0.00060670037,0.00040437136,0.00033093372,0.000022258673,0.0032804685],"category_scores_gemma":[0.00009642711,0.000042420717,0.000020067218,0.0003202979,0.00018176506,0.00013507906,0.00013762328,0.000109545974,0.00082148093],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025155954,0.00003347466,0.0011560089,0.00059930596,0.00010539453,0.000116896525,0.033347,0.0015705966,0.10107417,0.028154582,0.73179156,0.10179948],"study_design_scores_gemma":[0.00023040135,0.00023020073,0.026498282,0.00008893769,0.000030512454,0.00013914112,0.0008181442,0.0048766066,0.001517805,0.0037134283,0.9617168,0.00013976343],"about_ca_topic_score_codex":0.00026706705,"about_ca_topic_score_gemma":0.000014136974,"teacher_disagreement_score":0.22992525,"about_ca_system_score_codex":0.0000067511596,"about_ca_system_score_gemma":0.000003077467,"threshold_uncertainty_score":0.9999565},"labels":[],"label_agreement":null},{"id":"W6976257584","doi":"10.6068/dp15e7926249a83","title":"Trend 1961 - 2050. Food and Agriculture Organization of the United Nations. Food and Agriculture Organization Statistics: Emissions, Agriculture - Manure Applied to Soils | Country: Canada | Item: Chickens, broilers | Element: Stocks - Head, 1961-2050. Data-Planet™ Statistical Ready Reference by Conquest Systems, Inc. Dataset-ID: 067-001-035.","year":2017,"lang":"en","type":"other","venue":"Data Planet","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Agriculture; Manure; European union; Agency (philosophy); Food processing; Soil water; Food security","score_opus":0.01072654739806863,"score_gpt":0.20712882974776092,"score_spread":0.1964022823496923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6976257584","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00008846971,0.00074515794,0.0000033768981,0.000034424385,0.00043886158,0.0012299049,0.99622136,0.000056960936,0.0011815096],"genre_scores_gemma":[0.0022018214,0.0013592069,0.00013763862,0.00016986513,0.00035209072,0.000006351995,0.99435467,0.00005600962,0.0013623674],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9969398,0.00022838691,0.00058274827,0.0009996294,0.00079178624,0.00045766676],"domain_scores_gemma":[0.997037,0.00024177383,0.0008781725,0.0014015986,0.000078235345,0.0003632536],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020893147,0.0006386808,0.00071557943,0.00014903488,0.00063078164,0.00054655306,0.0014996594,0.00054459064,0.002196901],"category_scores_gemma":[0.00007753288,0.00039233922,9.4168223e-7,0.00036417242,0.00013769335,0.00023722519,0.0003597798,0.00042891272,0.000055349632],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017706838,0.000042302054,0.00006794473,0.00046832563,0.00023770881,0.0000101576115,0.000023877486,0.000067964276,0.0002088599,0.0006505113,0.9980916,0.0001130814],"study_design_scores_gemma":[0.000497367,0.00010307886,0.0008298772,0.000081830636,0.00040089642,0.000046242658,0.00019762797,0.000056709287,0.000003271988,0.0000013126268,0.99719316,0.0005886449],"about_ca_topic_score_codex":0.85765165,"about_ca_topic_score_gemma":0.892878,"teacher_disagreement_score":0.035226345,"about_ca_system_score_codex":0.00001738902,"about_ca_system_score_gemma":0.00017479369,"threshold_uncertainty_score":0.99985284},"labels":[],"label_agreement":null},{"id":"W6977163161","doi":"10.6084/m9.figshare.26748875.v1","title":"Additional file 6 of SurvdigitizeR: an algorithm for automated survival curve digitization","year":2024,"lang":"en","type":"dataset","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"SickKids Foundation; Hospital for Sick Children; McMaster University; York University; University of Toronto","funders":"","keywords":"Digitization; Curve fitting; Data file; Area under curve; Receiver operating characteristic","score_opus":0.02126943220876412,"score_gpt":0.24208854076685543,"score_spread":0.2208191085580913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6977163161","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[9.565275e-8,0.000026445388,2.9944619e-7,0.0000022918894,0.00038787676,0.0003057579,0.9988284,0.00015843105,0.00029041988],"genre_scores_gemma":[4.454842e-7,0.0000024692135,0.0002770044,0.000022284605,0.00080326427,0.00017696414,0.9984153,0.000011778678,0.00029052488],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99868965,0.000059371916,0.00030629785,0.0003764007,0.00031642988,0.00025187625],"domain_scores_gemma":[0.99785364,0.0013462417,0.0002290737,0.00026118397,0.00020347376,0.00010637427],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000045793826,0.00024413622,0.00035961228,0.00009345382,0.00007403728,0.00023120969,0.00033521757,0.00023477676,0.99607575],"category_scores_gemma":[0.00067053776,0.00022101434,0.00011303735,0.00015909517,0.000012775307,0.0002413339,0.000031899377,0.00009971959,0.019093253],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000040687905,0.000015766638,5.177284e-8,0.0004170036,0.000040252617,0.000008235699,0.0000020431685,0.00003207956,7.719392e-8,1.698027e-7,0.99683267,0.0026475883],"study_design_scores_gemma":[0.00006268295,0.00009641199,0.00019500096,0.0012639472,0.000021834476,0.0000022692577,0.0000026294647,0.005012911,0.0000035341402,0.00006629854,0.9930121,0.00026040632],"about_ca_topic_score_codex":0.00019110163,"about_ca_topic_score_gemma":0.00053246116,"teacher_disagreement_score":0.97698253,"about_ca_system_score_codex":0.0000032061698,"about_ca_system_score_gemma":0.00024575234,"threshold_uncertainty_score":0.9816705},"labels":[],"label_agreement":null},{"id":"W6977728028","doi":"10.6084/m9.figshare.c.3812578.v1","title":"Understanding factors affecting collaboration between midwives and other health care professionals in a birth center and its affiliated Quebec hospital: a case study","year":2017,"lang":"en","type":"other","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Thematic analysis; Multidisciplinary approach; Scope (computer science); Health care; Scope of practice; Qualitative research; Variety (cybernetics); Work (physics)","score_opus":0.07651114889420858,"score_gpt":0.31287517443539475,"score_spread":0.23636402554118618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6977728028","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47378305,0.0023523027,9.533095e-8,0.000037669695,0.00029553802,0.0023259157,0.5182524,0.00006996276,0.0028830925],"genre_scores_gemma":[0.97228396,0.000005639265,0.0000057594034,0.000019795258,0.00015831568,0.000010408213,0.021732269,0.000045900808,0.005737982],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988805,0.00019213477,0.00016114666,0.00037415812,0.00014798439,0.00024407347],"domain_scores_gemma":[0.9992578,0.00010593719,0.00035819586,0.00014459893,0.000023741946,0.00010971348],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000077111705,0.00024743925,0.00040364926,0.00014653767,0.0002450119,0.0002240837,0.000095721065,0.00015377173,0.014204233],"category_scores_gemma":[0.00007927656,0.0001961679,0.000018218807,0.00008416073,0.000009296906,0.00013941513,0.000039000075,0.0001161835,0.000030917818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047840982,0.00021034294,0.46684277,0.0070457067,0.00043440232,0.0009262972,0.12571594,0.000010374296,0.0000034527707,0.000005039808,0.3965522,0.0022056096],"study_design_scores_gemma":[0.0053783143,0.001833502,0.5275693,0.035384882,0.00012056467,0.000038649894,0.23322952,0.00008513037,0.00004655135,0.000014171932,0.19325705,0.0030423882],"about_ca_topic_score_codex":0.022030061,"about_ca_topic_score_gemma":0.35850626,"teacher_disagreement_score":0.49850088,"about_ca_system_score_codex":0.000017719447,"about_ca_system_score_gemma":0.00013656162,"threshold_uncertainty_score":0.9866969},"labels":[],"label_agreement":null},{"id":"W6983259340","doi":"","title":"Manif d'art 9 : La biennale de Québec : Si petits entre les étoiles","year":2019,"lang":"fr","type":"book","venue":"E-Artexte (Artexte)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Narrative; Perspective (graphical); Subject (documents); Feature (linguistics); Context (archaeology); Object (grammar); Government (linguistics)","score_opus":0.011140729527616014,"score_gpt":0.194630041603531,"score_spread":0.18348931207591498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6983259340","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.102961645,0.011443987,0.00015142832,0.0026534763,0.006567754,0.0014552706,0.003281646,0.0003114244,0.8711734],"genre_scores_gemma":[0.12717523,0.002053601,0.00035544546,0.00056510867,0.002633557,0.000020559315,0.0015030184,0.00011127843,0.8655822],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.993462,0.00089628244,0.0011503123,0.0015939773,0.0010060186,0.0018914024],"domain_scores_gemma":[0.99580646,0.0012046112,0.0007215378,0.0012503027,0.00021865549,0.00079843035],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.0012115034,0.0013684172,0.0016111229,0.00028492324,0.0008288943,0.00076269463,0.001388127,0.0010997027,0.11242217],"category_scores_gemma":[0.00010886826,0.0013063293,0.0006640211,0.00025836,0.0008156392,0.0006542797,0.00020671841,0.000986211,0.080101706],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038397283,0.0005678571,0.012506808,0.0026328412,0.0012339307,0.0012202297,0.0053082407,0.0019604885,0.0034973682,0.027942318,0.8221751,0.12057085],"study_design_scores_gemma":[0.00072841946,0.0003779812,0.024432883,0.0008369592,0.00044432873,0.00014694313,0.00014125969,0.0004438823,0.00020259083,0.001724171,0.9690679,0.0014527194],"about_ca_topic_score_codex":0.026303215,"about_ca_topic_score_gemma":0.061077766,"teacher_disagreement_score":0.14689277,"about_ca_system_score_codex":0.00009909807,"about_ca_system_score_gemma":0.0023866463,"threshold_uncertainty_score":0.99990666},"labels":[],"label_agreement":null},{"id":"W6987460225","doi":"","title":"Structural and electronic properties of dense liquid and amorphous nitrogen","year":2011,"lang":"en","type":"article","venue":"University of North Texas Digital Library (University of North Texas)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Killam Trusts; Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"Amorphous solid; Liquid phase; Liquid nitrogen; Phase (matter); Electronic structure; Nitrogen; Conductivity; Range (aeronautics); Electrical resistivity and conductivity","score_opus":0.010098996285428003,"score_gpt":0.1348557034649107,"score_spread":0.12475670717948269,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6987460225","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99720496,0.0003154211,0.0000066535454,0.000021426074,0.00003174097,0.00016992536,0.0009683459,0.000037880367,0.0012436656],"genre_scores_gemma":[0.99894303,0.00026801415,0.00018317782,0.00000938821,0.000011777245,2.9220903e-9,0.00012832401,0.000005665157,0.00045061234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990763,0.00004292026,0.00014300061,0.00028329942,0.00018018874,0.00027427264],"domain_scores_gemma":[0.9993263,0.000028099716,0.00023843745,0.00019358542,0.00005655691,0.00015704855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00003425655,0.00017948741,0.0003833876,0.00015031754,0.00014425586,0.000020834703,0.000412526,0.000060679475,0.0005137585],"category_scores_gemma":[0.0000047257467,0.00019324382,0.000089301626,0.0001951098,0.0006382425,0.0018099557,0.00020228795,0.000095573094,0.000018420456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008361607,0.000029566167,0.99617183,0.00011560366,0.00011117371,0.000037823105,0.000252149,0.000020354384,0.0000045246175,0.00008041108,0.00005849512,0.0022818882],"study_design_scores_gemma":[0.00047228546,0.0005670726,0.99691397,0.000033368156,0.00006773678,0.000010700694,0.000091666494,0.000064491156,0.00027211633,0.00019577619,0.0010986654,0.0002121241],"about_ca_topic_score_codex":0.0031634404,"about_ca_topic_score_gemma":0.0029866416,"teacher_disagreement_score":0.002069764,"about_ca_system_score_codex":0.000003016175,"about_ca_system_score_gemma":0.000104064755,"threshold_uncertainty_score":0.78802544},"labels":[],"label_agreement":null},{"id":"W6992011087","doi":"","title":"Isolation thermique haute performance : toujours plus","year":2010,"lang":"fr","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Energy consumption; Vacuum insulated panel; Thermal insulation; Efficient energy use; Energy (signal processing)","score_opus":0.01189152093309886,"score_gpt":0.20144648166377543,"score_spread":0.18955496073067657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6992011087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.922823,0.00017281345,0.00012225549,0.002771206,0.008178599,0.00015811088,0.00012494564,0.000033951474,0.065615125],"genre_scores_gemma":[0.9813601,0.0002458631,0.0021338402,0.00020191846,0.0014585182,0.0000021384653,0.00006098231,0.000007662586,0.014528985],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989186,0.00006647621,0.00020389786,0.00023319098,0.00018709266,0.0003907232],"domain_scores_gemma":[0.99938095,0.00006220128,0.00009970663,0.000258473,0.00005136989,0.00014729668],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00036251865,0.00016287643,0.00020187422,0.000035140452,0.00021275545,0.00014730396,0.00023448464,0.00017486271,0.025781408],"category_scores_gemma":[0.00001816872,0.00014445881,0.000052267587,0.00010540467,0.000119193355,0.0004256044,0.00002037386,0.00027807232,0.001994016],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015115565,0.000101646794,0.05141031,0.00037989154,0.00010996134,0.000046891884,0.0030962885,0.0065405937,0.5421523,0.02072591,0.034175295,0.34110975],"study_design_scores_gemma":[0.00055275677,0.00025699436,0.28426126,0.00008947591,0.00007575868,0.000040130883,0.000054880322,0.082622305,0.014338687,0.008205821,0.6089058,0.0005961485],"about_ca_topic_score_codex":0.0010115242,"about_ca_topic_score_gemma":0.00085806043,"teacher_disagreement_score":0.5747305,"about_ca_system_score_codex":0.0000034463224,"about_ca_system_score_gemma":0.0001256361,"threshold_uncertainty_score":0.99878305},"labels":[],"label_agreement":null},{"id":"W6992591005","doi":"","title":"Lo permanente en lo efímero: Pabellones de Exposiciones Universales, hitos de la arquitectura de la segunda posguerra","year":2015,"lang":"es","type":"other","venue":"Tesis Doctorals en Xarxa (Consorci de Serveis Universitaris de Catalunya)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Context (archaeology); Gnosticism; Base (topology)","score_opus":0.007559813062807181,"score_gpt":0.23785969152293784,"score_spread":0.23029987846013067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6992591005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94936615,0.005022588,0.00015652401,0.00069033593,0.0006929246,0.00084893877,0.0056538377,0.00048661922,0.037082054],"genre_scores_gemma":[0.94124186,0.003462414,0.0026747049,0.00044195665,0.0012849437,0.000009570728,0.0024716053,0.00027690717,0.048136055],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9910064,0.004108309,0.0006754373,0.0013119638,0.00075926847,0.0021386244],"domain_scores_gemma":[0.9945203,0.0020678132,0.0007172355,0.0011486916,0.00022794696,0.0013180274],"candidate_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow"],"category_scores_codex":[0.0026805054,0.0013854407,0.0015367162,0.0007891751,0.0006280867,0.0010016226,0.0021962423,0.001986215,0.0064495527],"category_scores_gemma":[0.00024653145,0.0014743361,0.00051574357,0.0007071053,0.00096697925,0.0007385631,0.00040770436,0.0011727801,0.00076184975],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021443646,0.0012320663,0.35825735,0.0036705406,0.005785163,0.009912898,0.033420045,0.015897842,0.07001293,0.0059436285,0.48897746,0.0047457097],"study_design_scores_gemma":[0.0028537298,0.00050290156,0.08162496,0.0010317184,0.0023636061,0.0006597791,0.0047621047,0.0009763606,0.0042961347,0.0009940853,0.89701754,0.0029170979],"about_ca_topic_score_codex":0.050221123,"about_ca_topic_score_gemma":0.0020872517,"teacher_disagreement_score":0.40804005,"about_ca_system_score_codex":0.0007500584,"about_ca_system_score_gemma":0.0022643271,"threshold_uncertainty_score":0.9998896},"labels":[],"label_agreement":null},{"id":"W6993093806","doi":"","title":"The âNYSE Premiumâ: Decomposing the âUS Premiumâ in compensation for CEOs of cross-listed firms","year":2016,"lang":"en","type":"article","venue":"e-publications@bond (Bond University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; Hyporeflexia; Fusible alloy; TSG101; Demotion; Hemopericardium","score_opus":0.019057000340816786,"score_gpt":0.2314745536899677,"score_spread":0.2124175533491509,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6993093806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9636761,0.00012011765,0.001095631,0.003517693,0.0005340114,0.0009952686,0.00054496346,0.000066457265,0.029449739],"genre_scores_gemma":[0.99125326,0.00004628541,0.00050473626,0.000033418368,0.00008499554,0.0000026461546,0.00012524567,0.0000047770473,0.007944627],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9989947,0.00008061664,0.00025347614,0.00024129072,0.00017243421,0.00025744934],"domain_scores_gemma":[0.9982519,0.0007912313,0.00023360323,0.00040675318,0.00025177363,0.00006471627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043920332,0.000116688585,0.00015109662,0.0001467412,0.0005278008,0.00015380178,0.00057401665,0.00007124909,0.00020106572],"category_scores_gemma":[0.00013087886,0.00006749251,0.00006882645,0.0005090935,0.00022874621,0.000528586,0.00003864504,0.00006082537,0.000028135068],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001248099,0.00036894015,0.3442165,0.00019628603,0.0002957147,0.0000052213272,0.002731995,0.001530923,0.032485284,0.5043963,0.042336557,0.0701882],"study_design_scores_gemma":[0.0009903128,0.00006625383,0.5130153,0.000035731344,0.000035482793,0.0000019502972,0.00013271833,0.00053177227,0.0031093068,0.0028151765,0.47908157,0.00018446596],"about_ca_topic_score_codex":0.0005237568,"about_ca_topic_score_gemma":0.0017392692,"teacher_disagreement_score":0.50158113,"about_ca_system_score_codex":0.000018159271,"about_ca_system_score_gemma":0.00010989924,"threshold_uncertainty_score":0.40594706},"labels":[],"label_agreement":null},{"id":"W6996822185","doi":"","title":"Texture and elastic anisotropy of a mylonitic anorthosite from the Morin Shear Zone (Quebec, Canada)","year":2015,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mylonite; Anisotropy; Seismic anisotropy; Anorthosite; Granulite; Shear zone; Gneiss; Plagioclase","score_opus":0.00943536199617242,"score_gpt":0.170751765339287,"score_spread":0.16131640334311456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6996822185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98546964,0.0008205539,0.00008242376,0.0006706528,0.00023027118,0.00016777891,0.010615863,0.000044257606,0.0018985646],"genre_scores_gemma":[0.9976351,0.000013489009,0.00020686637,0.0003894963,0.00021605732,0.0000014363804,0.0010750735,0.000012874922,0.00044958058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986116,0.00009362145,0.00028651857,0.00028136608,0.0004149836,0.00031187723],"domain_scores_gemma":[0.9989898,0.00026169058,0.00010953967,0.00027507747,0.00003466401,0.00032921208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009869979,0.0002089297,0.00027403198,0.000027965416,0.00010519161,0.00062656944,0.00033595148,0.00007619648,0.0006522265],"category_scores_gemma":[0.00009495842,0.00013995143,0.000044568907,0.00018102533,0.000119007665,0.0011896996,0.00006831628,0.00018341193,0.00020447664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023968336,0.000044514487,0.98052627,0.000046140372,0.000092641334,0.00009324996,0.00010655621,0.0002474589,0.00016042619,0.0005211031,0.010299865,0.007622101],"study_design_scores_gemma":[0.0007400305,0.0001460804,0.7483822,0.00009334968,0.00006935643,0.000009993587,0.00013002666,0.00049482693,0.0009024226,0.00688443,0.24164924,0.0004980115],"about_ca_topic_score_codex":0.16103971,"about_ca_topic_score_gemma":0.1467197,"teacher_disagreement_score":0.23214403,"about_ca_system_score_codex":0.0000046172686,"about_ca_system_score_gemma":0.00037787578,"threshold_uncertainty_score":0.86885047},"labels":[],"label_agreement":null},{"id":"W6997255138","doi":"","title":"Variations of the lithospheric strength and elastic thickness in North America","year":2015,"lang":"","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Craton; Crust; Seismic tomography; Proterozoic; Lithospheric flexure; Mantle (geology)","score_opus":0.03800263403686712,"score_gpt":0.30183799423047175,"score_spread":0.26383536019360465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6997255138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9381572,0.0011340688,0.0017040212,0.014458912,0.0021781859,0.0038958436,0.037435066,0.000045880253,0.000990804],"genre_scores_gemma":[0.99296004,0.00041614939,0.001739996,0.00012664586,0.00023873511,0.00006564246,0.0034230703,0.000012874572,0.00101685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9941291,0.0010209362,0.00082704856,0.000958042,0.0018547882,0.0012100484],"domain_scores_gemma":[0.99488926,0.0013504819,0.00048841175,0.0011049444,0.0014885452,0.00067837257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004551665,0.00028281356,0.0004045305,0.00035061658,0.00079761795,0.00067816686,0.0016647903,0.00010722051,0.0006596154],"category_scores_gemma":[0.0041197897,0.0002098296,0.00007471368,0.004320492,0.0013362349,0.0015804938,0.00049896486,0.0004060341,0.00007750159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00092193496,0.0035935913,0.67712224,0.0023704018,0.00018315899,0.000014424156,0.03099573,0.0041750763,0.00086559553,0.037510287,0.12632895,0.11591861],"study_design_scores_gemma":[0.0016224239,0.0003536816,0.5157422,0.00016030813,0.00007455657,0.0000064457854,0.0022487827,0.09855679,0.00018807127,0.0023022634,0.37813073,0.00061378645],"about_ca_topic_score_codex":0.015320684,"about_ca_topic_score_gemma":0.01675721,"teacher_disagreement_score":0.2518018,"about_ca_system_score_codex":0.000041663974,"about_ca_system_score_gemma":0.0017042427,"threshold_uncertainty_score":0.9912364},"labels":[],"label_agreement":null},{"id":"W7001950610","doi":"","title":"Mixed-integer Programming Models for Maintenance Scheduling in Power Transmission Systems","year":2023,"lang":"fr","type":"other","venue":"PolyPublie (École Polytechnique de Montréal)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Rail transportation; Scheduling (production processes); Transmission channel; Transport system; Power grid","score_opus":0.016759323939613435,"score_gpt":0.21479335508880082,"score_spread":0.19803403114918738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7001950610","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007940932,0.013595377,0.9585564,0.001900429,0.0037872694,0.0058057,0.0013008197,0.0012803096,0.0058327685],"genre_scores_gemma":[0.62849027,0.0041912277,0.15553415,0.0006041409,0.0017090657,0.0024735222,0.00060457917,0.001328888,0.20506416],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9949075,0.00030324073,0.0011530747,0.001163724,0.00054287317,0.0019295992],"domain_scores_gemma":[0.9975749,0.00040684853,0.00055285986,0.0007845396,0.00015283542,0.0005280141],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0017357509,0.00090665166,0.0012929124,0.00070504274,0.00029455818,0.00059479324,0.0008681045,0.001157714,0.0005833078],"category_scores_gemma":[0.00014563656,0.0008326973,0.0004061512,0.0007007897,0.000153243,0.0005003181,0.00007834248,0.00065512373,0.00018940464],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048813052,0.00034281475,0.004007681,0.0017822469,0.00028370493,0.00030542375,0.000969811,0.78594416,0.0013281214,0.092702545,0.008540886,0.10330446],"study_design_scores_gemma":[0.0007527055,0.0002693348,0.00147746,0.0025306104,0.00009150882,0.00003251175,0.00023840148,0.7427319,0.00025139636,0.0027610776,0.24783212,0.0010309675],"about_ca_topic_score_codex":0.088102005,"about_ca_topic_score_gemma":0.038356636,"teacher_disagreement_score":0.80302227,"about_ca_system_score_codex":0.0001784456,"about_ca_system_score_gemma":0.00039504978,"threshold_uncertainty_score":0.99941236},"labels":[],"label_agreement":null},{"id":"W7001955573","doi":"","title":"Lithospheric structure of Eastern Canada and the NE USA from earthquake and ambient noise seismology","year":2022,"lang":"fr","type":"other","venue":"Archipelago (University of Quebec in Montreal)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Terrane; Bathymetry; Seismic zone; Craton; Lithosphere","score_opus":0.0042636300205549415,"score_gpt":0.14591517643386775,"score_spread":0.14165154641331282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7001955573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923588,0.0016460833,0.000012712946,0.00045341504,0.00035512366,0.00030435977,0.0024022816,0.0000029728972,0.0024642546],"genre_scores_gemma":[0.97019213,0.0004947946,0.00024914424,0.00009076987,0.000047721776,1.3001535e-7,0.00018932657,0.000011037361,0.028724926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99840057,0.0004974808,0.00020853552,0.00037360284,0.00024876816,0.0002710296],"domain_scores_gemma":[0.9988639,0.00037283948,0.00033301715,0.00029417002,0.00002066175,0.0001154108],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013331218,0.0002327162,0.00067229074,0.00006158497,0.00015453687,0.000015931835,0.0003669195,0.000126497,0.014847977],"category_scores_gemma":[0.000012354711,0.00020802532,0.000055530258,0.00013001979,0.0007409282,0.000065775996,0.00019987789,0.0002399537,0.0000047942112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002180728,0.000100091216,0.46275872,0.0005399721,0.0006906614,0.00057010696,0.06081742,0.0043818713,0.00031662532,0.0038956604,0.001685305,0.46206287],"study_design_scores_gemma":[0.0014927678,0.00008552105,0.97138745,0.000059266647,0.00013952416,0.0000056107206,0.0045916736,0.0011238575,0.0000046828627,0.0043263845,0.016571473,0.00021181788],"about_ca_topic_score_codex":0.9997456,"about_ca_topic_score_gemma":0.9999591,"teacher_disagreement_score":0.5086287,"about_ca_system_score_codex":0.000012890086,"about_ca_system_score_gemma":0.0002535069,"threshold_uncertainty_score":0.9860526},"labels":[],"label_agreement":null},{"id":"W7006405168","doi":"","title":"Understanding the composition, origin, and evolution of the continental crust: Case studies in the southern Rio Grande rift, New Mexico, United States of Americaand the Coast Plutonic Complex, British Columbia, Canada","year":2006,"lang":"en","type":"article","venue":"scholarworks - UTEP (The University of Texas at El Paso)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pluton; Continental crust; Peridotite; Granulite; Crust; Mafic; Rift; Batholith; Volcano; Metallogeny; Gneiss","score_opus":0.022365377648403375,"score_gpt":0.19826968823145183,"score_spread":0.17590431058304845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7006405168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99697536,0.0007547839,0.00010844109,0.000839617,0.0001228533,0.0003537677,0.0007060768,0.0000057036705,0.0001333953],"genre_scores_gemma":[0.9994416,0.00012268987,0.000017226794,0.000087618275,0.00002848422,1.3227516e-7,0.00006932741,0.0000032955984,0.0002296309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986344,0.00045393768,0.00022353807,0.00015932613,0.00032504072,0.0002037492],"domain_scores_gemma":[0.9988363,0.00048318258,0.00030300426,0.0002558383,0.000088409404,0.000033316086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005143449,0.0001117362,0.00025191557,0.000024652452,0.001156881,0.000086505715,0.00045910818,0.000041447216,0.00011982559],"category_scores_gemma":[0.000016962524,0.00007115867,0.00006484892,0.00039019852,0.00095650234,0.00010712459,0.00009300256,0.00020630707,0.0000010441631],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021922441,0.0000736577,0.93183047,0.000078381,0.00037251174,0.000116284304,0.0076985843,0.029743316,0.00026762648,0.0004113962,0.028936522,0.00025202104],"study_design_scores_gemma":[0.0014783626,0.00007352388,0.93881184,0.00016156079,0.0002867892,0.00016859615,0.04763588,0.0024204596,0.000021038464,0.0018681389,0.006875183,0.00019862811],"about_ca_topic_score_codex":0.9618971,"about_ca_topic_score_gemma":0.9855928,"teacher_disagreement_score":0.039937295,"about_ca_system_score_codex":0.00004913914,"about_ca_system_score_gemma":0.0001157215,"threshold_uncertainty_score":0.8897911},"labels":[],"label_agreement":null},{"id":"W7006418589","doi":"","title":"The thermal structure of the continental lithosphere (past and present)","year":2005,"lang":"fr","type":"other","venue":"OpenGrey (Institut de l'Information Scientifique et Technique)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Heat flux; Convection; Thermal; Continental crust","score_opus":0.007955159002764252,"score_gpt":0.21647098348911345,"score_spread":0.2085158244863492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7006418589","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15689287,0.0025696817,0.0042640325,0.007582661,0.008360035,0.022164138,0.004926825,0.00022035318,0.7930194],"genre_scores_gemma":[0.69159967,0.000986543,0.0076608337,0.001012575,0.0012764393,0.00018968902,0.0006066945,0.00007675206,0.29659078],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99739116,0.0003811052,0.0007546672,0.00031829023,0.0006360957,0.0005186932],"domain_scores_gemma":[0.99789596,0.00015114134,0.00084653636,0.00073104736,0.0002161376,0.00015918948],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014870788,0.00041134146,0.00040463425,0.00008679122,0.00079497613,0.0011125115,0.0012162066,0.0003991586,0.007773557],"category_scores_gemma":[0.00012748182,0.000240222,0.00014644032,0.00034924768,0.0009830451,0.0013594351,0.00027736995,0.00046420228,0.00013151363],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026806846,0.0001204503,0.017765936,0.0023168998,0.00038733636,0.000011129904,0.008133848,0.0048914975,0.031331852,0.07510395,0.17626551,0.68340355],"study_design_scores_gemma":[0.000271529,0.000027249125,0.019908765,0.00052805507,0.0000493869,0.000023128818,0.00008312498,0.00065454026,0.018756576,0.00024056231,0.95914626,0.0003108402],"about_ca_topic_score_codex":0.0018723877,"about_ca_topic_score_gemma":0.004362171,"teacher_disagreement_score":0.7828807,"about_ca_system_score_codex":0.000026824377,"about_ca_system_score_gemma":0.0003964304,"threshold_uncertainty_score":0.9999244},"labels":[],"label_agreement":null},{"id":"W7015477520","doi":"","title":"Surface and Crustal Response to Lithospheric Removal Processes: Insights From Numerical and Analogue Modeling","year":2010,"lang":"en","type":"dissertation","venue":"Library and Archives Canada (Government of Canada)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lithosphere; Subduction; Mantle (geology); Delamination (geology); Plate tectonics; Crust; Asthenosphere; Convergent boundary; Oceanic crust","score_opus":0.003505791743060484,"score_gpt":0.1522080896285912,"score_spread":0.14870229788553072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7015477520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893624,0.0013043787,0.000025235759,0.0003115457,0.00033037132,0.00017649033,0.0010067637,0.000007728668,0.0074750674],"genre_scores_gemma":[0.9948662,0.00025744698,0.002178756,0.00022755924,0.00007933182,0.0000013215864,0.00028009247,0.00001252312,0.0020967647],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9981914,0.000068940346,0.000268087,0.00039601038,0.0008455436,0.00023001959],"domain_scores_gemma":[0.99908984,0.0002661073,0.00013237302,0.00014264934,0.0000018583094,0.00036714663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000014877964,0.0002522067,0.00037521552,0.00001598012,0.00019138391,0.00008571776,0.00015904664,0.00007734797,0.00006299562],"category_scores_gemma":[0.000010794563,0.00022292684,0.000013772538,0.00008494249,0.000032981756,0.0002674601,0.000036156936,0.00017628966,9.298913e-9],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0871372,0.00025026937,0.10489785,0.00852455,0.0015695336,0.0035950234,0.018369496,0.0353314,0.6229279,0.010756402,0.0021564462,0.1044839],"study_design_scores_gemma":[0.0017847053,0.0009054551,0.7378982,0.001429966,0.00037937812,0.00004213779,0.018442407,0.08575236,0.068573095,0.009901327,0.071479075,0.0034119487],"about_ca_topic_score_codex":0.063212335,"about_ca_topic_score_gemma":0.30135608,"teacher_disagreement_score":0.6330003,"about_ca_system_score_codex":8.631471e-7,"about_ca_system_score_gemma":0.0014049362,"threshold_uncertainty_score":0.9430258},"labels":[],"label_agreement":null},{"id":"W7017476298","doi":"","title":"Archean high-pressure metamorphism in the western Canadian shield","year":2010,"lang":"en","type":"article","venue":"Scholarworks (University of Massachusetts Amherst)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archean; Metamorphism; Shield; Precambrian; Proterozoic","score_opus":0.010147760482776332,"score_gpt":0.18280264683425898,"score_spread":0.17265488635148266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7017476298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98642355,0.00012189139,0.000037073794,0.005778393,0.0006119113,0.00025468942,0.00028642776,0.00002543431,0.0064606424],"genre_scores_gemma":[0.9980839,0.000021563385,0.00056159066,0.00040550143,0.00011355013,1.5735863e-7,0.000092953676,0.00000540971,0.00071538566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985136,0.00022955619,0.00014530857,0.00031297316,0.00034633122,0.00045226648],"domain_scores_gemma":[0.998962,0.00013675808,0.00010841938,0.0005160695,0.000045245783,0.00023152136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001022204,0.00017231719,0.00027670927,0.00020746829,0.00033349212,0.00012131564,0.0010895791,0.00023063635,0.0028538592],"category_scores_gemma":[0.00003316581,0.00015144424,0.000088571964,0.00033298458,0.00019881754,0.0005561612,0.000034222747,0.0008022428,0.00018747353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029946683,0.00018494406,0.92256415,0.00014955494,0.00043933163,0.0008242299,0.013282976,0.0033780169,0.0040157246,0.0061215023,0.026853668,0.02188646],"study_design_scores_gemma":[0.0005761538,0.000058907077,0.8626251,0.000024653635,0.000103367645,0.000007982334,0.0010758304,0.00020964837,0.000053735894,0.0011877727,0.13379006,0.00028675052],"about_ca_topic_score_codex":0.47958195,"about_ca_topic_score_gemma":0.7850807,"teacher_disagreement_score":0.3054987,"about_ca_system_score_codex":0.000004629548,"about_ca_system_score_gemma":0.0001328619,"threshold_uncertainty_score":0.99805766},"labels":[],"label_agreement":null},{"id":"W7018960792","doi":"","title":"Elastic behavior and high &#13;\\npressure-induced phase transition in chabazite: new data from a sample from Nova Scotia","year":2012,"lang":"en","type":"article","venue":"IRIS UNIMORE (University of Modena and Reggio Emilia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sample (material); Nova scotia; Phase (matter); Phase transition; Work (physics)","score_opus":0.04326525631401768,"score_gpt":0.23916501772946522,"score_spread":0.19589976141544754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7018960792","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99219406,0.00081088376,0.0017931443,0.00020943453,0.0002628285,0.00018440546,0.0044849226,0.000019741388,0.000040555857],"genre_scores_gemma":[0.9956679,0.00020906272,0.0017273469,0.000024384408,0.00014742583,4.337207e-8,0.0021895487,0.000005043903,0.000029258543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998974,0.00007359443,0.00013749373,0.00036951955,0.00018688475,0.00025850648],"domain_scores_gemma":[0.99915147,0.00014427285,0.00009371751,0.0003538744,0.000022847706,0.00023382557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012739214,0.00016115987,0.00033730955,0.00009154252,0.00009951284,0.000028521037,0.0002912023,0.00014080995,0.00081143045],"category_scores_gemma":[0.000012411008,0.0001675904,0.000029407827,0.00012316265,0.00011463221,0.0007193234,0.00007164198,0.000115108785,0.000018601346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036526357,0.0015659067,0.5723351,0.00031261158,0.00069725077,0.00035065017,0.039071325,0.0010107371,0.17846203,0.00023486522,0.010221802,0.19208507],"study_design_scores_gemma":[0.0037574589,0.00017366583,0.98239964,0.000111824906,0.0004154009,0.000004116237,0.0010642598,0.009019894,0.00053318485,0.0009256635,0.0011848207,0.00041005798],"about_ca_topic_score_codex":0.34307602,"about_ca_topic_score_gemma":0.04584263,"teacher_disagreement_score":0.41006452,"about_ca_system_score_codex":0.0000033352644,"about_ca_system_score_gemma":0.00003949734,"threshold_uncertainty_score":0.9715682},"labels":[],"label_agreement":null},{"id":"W7019102114","doi":"","title":"Experimental, geochemical and isotopic insights on melting and degassing behavior on Earth","year":2022,"lang":"en","type":"dissertation","venue":"DSpace@MIT (Massachusetts Institute of Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Supercritical fluid; Geothermal gradient; Hydrothermal circulation; Mantle (geology); Igneous rock; Isotope geochemistry; Meteorite; Fluid inclusions; Geochemical modeling","score_opus":0.01094202609969316,"score_gpt":0.2426591827287778,"score_spread":0.23171715662908463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7019102114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99199045,0.0020619961,7.4892307e-7,0.00015428287,0.0012577702,0.0004623426,0.00020020308,0.0001266799,0.0037455151],"genre_scores_gemma":[0.9975096,0.00015508496,0.00073079346,0.000052448522,0.000081426304,0.000035348414,0.00073824124,0.000018069535,0.00067898084],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9982142,0.00003610789,0.00036697742,0.0006662925,0.00037460733,0.00034185493],"domain_scores_gemma":[0.9991004,0.000040311385,0.0003315129,0.0003959024,0.000035661014,0.000096213575],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0000951075,0.0004086625,0.00058922503,0.0005023915,0.00040053204,0.00008063432,0.00031140083,0.00051182864,0.0003087118],"category_scores_gemma":[0.00005602719,0.0003763261,0.00006731517,0.00024768352,0.00025843614,0.00017455585,0.000062094645,0.0005473926,0.000013253961],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001390317,0.0014141464,0.0480852,0.0015375768,0.0009663424,0.0010694849,0.0055864723,0.00037948982,0.68896574,0.027556716,0.0021019669,0.22094658],"study_design_scores_gemma":[0.002020771,0.002173457,0.05563985,0.0008578755,0.00041322462,0.000045669593,0.0019463216,0.00013930145,0.7018149,0.0012291431,0.2319343,0.0017851974],"about_ca_topic_score_codex":0.00036132708,"about_ca_topic_score_gemma":0.00042955118,"teacher_disagreement_score":0.22983232,"about_ca_system_score_codex":0.000011673483,"about_ca_system_score_gemma":0.000069041314,"threshold_uncertainty_score":0.99986887},"labels":[],"label_agreement":null},{"id":"W7023522268","doi":"","title":"2021 OCT 02 OAN Ivermectin DEFEATS Co V 19 In Uttar Pradesh India Population 241m People Co V 19 Free","year":2021,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ivermectin; Uttar pradesh; Population; State (computer science); Coronavirus disease 2019 (COVID-19)","score_opus":0.005794069890405255,"score_gpt":0.1884765013933507,"score_spread":0.18268243150294544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7023522268","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0072518885,0.0005210871,1.796051e-7,0.00007305366,0.0006540447,0.0005781645,0.001805402,0.00006884,0.98904735],"genre_scores_gemma":[0.031034397,0.00041463925,0.0005064487,0.00019532272,0.00039494145,0.000007041441,0.008971303,0.00004858989,0.9584273],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99764735,0.00022467661,0.00075136655,0.00034868324,0.0005854695,0.00044246152],"domain_scores_gemma":[0.99838406,0.00017488192,0.00067365286,0.0004966419,0.000069521215,0.00020125543],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00037900198,0.00040636788,0.00067203643,0.00015723333,0.00011164132,0.00014082338,0.00044140944,0.00047670925,0.6322054],"category_scores_gemma":[0.0001822736,0.0004072051,0.00014545536,0.00003217563,0.00006510414,0.0000011549627,0.000048539558,0.00028568163,0.006450485],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006135933,0.000029652367,0.0028155923,0.00044877088,0.000051673753,0.00005029354,0.00028637244,0.0011541174,0.0000012190984,0.000013191971,0.9942609,0.0008268415],"study_design_scores_gemma":[0.00063109305,0.000096294556,0.014398962,0.00020329625,0.000040205232,0.000040423078,0.00011660348,0.000032373286,0.0000104132,0.000035233006,0.9839617,0.0004334035],"about_ca_topic_score_codex":0.14494154,"about_ca_topic_score_gemma":0.08238593,"teacher_disagreement_score":0.62575495,"about_ca_system_score_codex":0.000023434595,"about_ca_system_score_gemma":0.00009000714,"threshold_uncertainty_score":0.999838},"labels":[],"label_agreement":null},{"id":"W7023649996","doi":"","title":"The optimal point of international taxation and its economic impact in productive internationalization : a study of the cost-benefit ratio from the perspective of the Brazilian and French regimes","year":2020,"lang":"fr","type":"article","venue":"theses.fr (ABES)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Internationalization; International taxation; Perspective (graphical); Double taxation","score_opus":0.016143601940528638,"score_gpt":0.2434587356722944,"score_spread":0.22731513373176576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7023649996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98818034,0.0014427664,0.000012156343,0.0072295475,0.00056789006,0.0010285367,0.0008525921,0.0000026662508,0.00068352954],"genre_scores_gemma":[0.99933946,0.00031857355,0.000010967186,0.000037885275,0.00020037736,0.000008253518,0.000017531955,0.000005130965,0.000061845625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986526,0.00034879489,0.00037241893,0.000251215,0.0002570732,0.00011791975],"domain_scores_gemma":[0.99841803,0.00046946364,0.00068223587,0.00021667525,0.00018214603,0.0000314594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046084658,0.00014102765,0.00022140545,0.000024307908,0.00012387865,0.00007923056,0.00046604886,0.00004299287,0.00024094548],"category_scores_gemma":[0.00039258035,0.00006899121,0.00005463584,0.00013758535,0.00026831022,0.000284098,0.00013919207,0.000115219395,0.0000027934211],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007961468,0.00033188038,0.4630977,0.00006389592,0.0012112783,0.0000012400164,0.32675913,0.09347417,0.00512693,0.10447114,0.00036378775,0.0043026987],"study_design_scores_gemma":[0.00065818,0.00024989643,0.94627184,0.00009918952,0.00008947113,0.0000019650554,0.020140026,0.022512002,0.005059692,0.0043349494,0.00047944483,0.00010333209],"about_ca_topic_score_codex":0.054535426,"about_ca_topic_score_gemma":0.011116637,"teacher_disagreement_score":0.48317415,"about_ca_system_score_codex":0.00003165421,"about_ca_system_score_gemma":0.00011542206,"threshold_uncertainty_score":0.95176053},"labels":[],"label_agreement":null},{"id":"W7024587117","doi":"","title":"Studies Of Earthquakes Stress Drops, Seismic Scattering, And Dynamic Triggering In North America","year":2010,"lang":"en","type":"article","venue":"scholarworks - UTEP (The University of Texas at El Paso)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic moment; Focal mechanism; Attenuation; Deconvolution; Tectonics; Seismogram; Drop (telecommunication); Stress (linguistics)","score_opus":0.007060146280898558,"score_gpt":0.201869636973726,"score_spread":0.19480949069282744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7024587117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985236,0.0005500547,0.000018693549,0.00015854828,0.000234667,0.00014508734,0.00014533769,0.000014939024,0.00020906859],"genre_scores_gemma":[0.9988779,0.0005254714,0.00027812895,0.000022572296,0.000023012071,6.9396194e-8,0.000030447092,0.000003818686,0.0002385767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99909794,0.000084999294,0.00017489806,0.00023960091,0.00017683346,0.00022569613],"domain_scores_gemma":[0.9993001,0.00013581531,0.00017790133,0.00027250528,0.00004682218,0.00006682862],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021813248,0.00014103657,0.00032413055,0.00009164797,0.00022661684,0.000024430477,0.0003533859,0.00006757534,0.00033489423],"category_scores_gemma":[0.000026303804,0.0001179256,0.000057001726,0.00021683516,0.00048361413,0.00025595864,0.00012704384,0.00025483963,0.00003249362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021458439,0.00006420386,0.94442195,0.00024378514,0.00021175652,0.000042590458,0.0035061918,0.012449576,0.006106308,0.000026922617,0.00014898567,0.032563157],"study_design_scores_gemma":[0.0004213985,0.00007051825,0.99061126,0.00006946382,0.00004887172,0.0000031166,0.00082976074,0.002499496,0.00035168705,0.000083123974,0.004839673,0.00017165486],"about_ca_topic_score_codex":0.0023654988,"about_ca_topic_score_gemma":0.021708293,"teacher_disagreement_score":0.046189297,"about_ca_system_score_codex":0.000004906015,"about_ca_system_score_gemma":0.000021717231,"threshold_uncertainty_score":0.996143},"labels":[],"label_agreement":null},{"id":"W7025008644","doi":"","title":"UFP Reports Record Fourth Quarter and Annual Results","year":2017,"lang":"en","type":"other","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quarter (Canadian coin); Historical record; Period (music); Data collection","score_opus":0.008626850202245418,"score_gpt":0.2087179722542013,"score_spread":0.2000911220519559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7025008644","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00068743026,0.0003073296,0.0000108170925,0.00012968545,0.0022989654,0.00018855563,0.0013747048,0.00009797848,0.9949045],"genre_scores_gemma":[0.009152689,0.00026975875,0.00091980863,0.00007298795,0.0012252795,9.746872e-7,0.00042371286,0.00003324252,0.98790157],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989308,0.000036006175,0.00020607295,0.00042822142,0.00016494073,0.00023396629],"domain_scores_gemma":[0.99892277,0.000027243892,0.00035905032,0.00055405643,0.000017943572,0.00011895352],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022309145,0.00020648615,0.00033018095,0.00006393042,0.000090487825,0.00014874747,0.00014446088,0.00019881017,0.007866729],"category_scores_gemma":[0.000027802904,0.00014806056,0.000038879676,0.000016852022,0.000065328204,0.000090175534,0.000018050101,0.00007620362,0.00038197153],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018014556,0.0000031969694,0.00081588124,0.00002438184,0.000028233593,0.00012839952,0.000034833356,6.658131e-7,0.000002189124,0.000009953349,0.9868266,0.012107673],"study_design_scores_gemma":[0.00013317328,0.000071503804,0.0057453047,0.00006518817,0.00002082259,0.000020569838,0.00000941752,0.000009251418,0.000004795563,0.0002752327,0.9934147,0.00023006239],"about_ca_topic_score_codex":0.031980842,"about_ca_topic_score_gemma":0.02230768,"teacher_disagreement_score":0.01187761,"about_ca_system_score_codex":4.6838974e-7,"about_ca_system_score_gemma":0.000030804094,"threshold_uncertainty_score":0.99553263},"labels":[],"label_agreement":null},{"id":"W7030375350","doi":"","title":"New Insight Into Relative Sea Level Change and Its Constraints on Mantle Viscosity and Deglaciation History Since the Last Glacial Maximum","year":2023,"lang":"en","type":"dissertation","venue":"CU Scholar (University of Colorado Boulder)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Deglaciation; Post-glacial rebound; Mantle (geology); Last Glacial Maximum; Lithosphere; Ice sheet; Glacial period","score_opus":0.03856585332670854,"score_gpt":0.21940028389387622,"score_spread":0.1808344305671677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7030375350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99412405,0.0010343735,0.00003114124,0.00033247547,0.00096514245,0.0004660445,0.000352647,0.00003520505,0.0026589278],"genre_scores_gemma":[0.9957987,0.00057527726,0.00016312858,0.00006199572,0.00012316385,3.5358067e-7,0.0008752347,0.000009210107,0.0023929523],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9989044,0.00016103247,0.00012410794,0.00034205473,0.00028946644,0.00017894637],"domain_scores_gemma":[0.9992507,0.000110121655,0.00027333194,0.0001351277,0.0001041645,0.00012656537],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002786564,0.00020077523,0.00031045207,0.00014911091,0.00055169687,0.000056872752,0.00022240296,0.0002732381,0.00037222274],"category_scores_gemma":[0.000049745937,0.00019779512,0.00005201504,0.00015082056,0.00014066823,0.00063784915,0.00003587594,0.0003779061,0.00010913671],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00634553,0.0003421313,0.044233717,0.00344024,0.0018188255,0.00061808794,0.39170018,0.00011715953,0.010026587,0.022252848,0.026103502,0.4930012],"study_design_scores_gemma":[0.000636329,0.00021703653,0.9736505,0.00018129798,0.00017405093,0.0000020589216,0.002795998,0.00017268983,0.0001269837,0.001224461,0.020496022,0.00032256934],"about_ca_topic_score_codex":0.0041496777,"about_ca_topic_score_gemma":0.025082622,"teacher_disagreement_score":0.9294168,"about_ca_system_score_codex":0.000029663572,"about_ca_system_score_gemma":0.00019372892,"threshold_uncertainty_score":0.9927071},"labels":[],"label_agreement":null},{"id":"W7034526367","doi":"","title":"West Fraser Timber Co. Ltd. (NYSE:WFG) Short Interest Down 30.3% in December","year":2023,"lang":"en","type":"other","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Interest rate; Work (physics); Feature (linguistics); Quarter (Canadian coin)","score_opus":0.020484166185907374,"score_gpt":0.2505490161023363,"score_spread":0.23006484991642895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7034526367","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021664517,0.00019039931,0.000004661974,0.00007869293,0.0020230405,0.00036816098,0.00077967724,0.00041904877,0.9744718],"genre_scores_gemma":[0.11839181,0.00030756032,0.00016995794,0.00034173907,0.0011221203,0.000010097993,0.0009374127,0.00026723914,0.87845206],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982327,0.00007652351,0.00035335263,0.00055262045,0.00027401192,0.000510778],"domain_scores_gemma":[0.9991869,0.00010118439,0.00008398438,0.00044482373,0.000017658722,0.0001654862],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022667315,0.00039209318,0.00055363734,0.00022587141,0.000040705218,0.00013805644,0.00039607263,0.00038651918,0.39876205],"category_scores_gemma":[0.00001797952,0.0003007513,0.00009208958,0.00019826238,0.000080440936,0.00008741869,0.000041245687,0.00022228,0.044216152],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012043373,0.000023741779,0.020487553,0.00005225552,0.00006704726,0.00013349301,0.000031084546,0.000051790295,0.00001828762,0.00007094472,0.976779,0.0022727798],"study_design_scores_gemma":[0.00019691346,0.00003666359,0.035762094,0.00014367708,0.000024984383,0.0000020994173,0.000024871628,0.000052292424,0.00006746425,0.00010968222,0.9631052,0.00047407314],"about_ca_topic_score_codex":0.024890937,"about_ca_topic_score_gemma":0.28591096,"teacher_disagreement_score":0.3545459,"about_ca_system_score_codex":0.0000046946966,"about_ca_system_score_gemma":0.00005823552,"threshold_uncertainty_score":0.99994445},"labels":[],"label_agreement":null},{"id":"W7039722942","doi":"","title":"Neutron Scattering in Earth Sciences","year":2007,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"","score_opus":0.014936848699655239,"score_gpt":0.22677130676462845,"score_spread":0.2118344580649732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7039722942","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9264296,0.000025153438,0.000016006197,0.00012712007,0.00032199858,0.000051187257,0.0000067825454,0.000017385806,0.07300472],"genre_scores_gemma":[0.99847585,0.0000066427942,0.001123143,0.00011786111,0.00013184016,2.1796485e-7,0.000004970348,0.0000012412551,0.00013824011],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992815,0.000018450104,0.0001210865,0.0001532363,0.00014074198,0.0002849541],"domain_scores_gemma":[0.9997924,0.00004741615,0.000026105141,0.00007619506,0.0000065013237,0.00005138158],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000592695,0.00005969771,0.00008729085,0.00006784036,0.00008139417,0.00005404512,0.00014286756,0.000023974631,0.0018941642],"category_scores_gemma":[0.000006753187,0.00004866419,0.000015499614,0.00016560833,0.00007293731,0.00013835722,0.000009831035,0.000043309148,0.0002681537],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054395125,0.000031985794,0.5549605,0.00003465188,0.0000071442214,0.00006896422,0.00047982828,0.0020524948,0.37849477,0.0038524733,0.00040860393,0.059554223],"study_design_scores_gemma":[0.000099801226,0.000049159087,0.9854561,0.000011101448,0.0000014247028,0.000002314286,0.000030611332,0.000297774,0.0056205564,0.0024072167,0.0059344578,0.00008948891],"about_ca_topic_score_codex":0.0007441773,"about_ca_topic_score_gemma":0.0023384846,"teacher_disagreement_score":0.43049562,"about_ca_system_score_codex":5.8767927e-7,"about_ca_system_score_gemma":0.00001636288,"threshold_uncertainty_score":0.99901825},"labels":[],"label_agreement":null},{"id":"W7040434596","doi":"","title":"EXD-16-04-10","year":2016,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Feature (linguistics); Set (abstract data type); Punk; Panama","score_opus":0.004949471656025455,"score_gpt":0.1717107441800623,"score_spread":0.16676127252403683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7040434596","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00004422894,0.0002606894,2.9247076e-7,0.00008469631,0.0007497868,0.0002679957,0.0010941076,0.00013282227,0.99736536],"genre_scores_gemma":[0.0009635865,0.00025181661,0.00023115502,0.00014608238,0.00048516082,0.000002308418,0.00050708983,0.00003826117,0.99737453],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99859554,0.000064201064,0.00045716378,0.00019228131,0.00036918826,0.00032164334],"domain_scores_gemma":[0.99891293,0.00008864886,0.00046184665,0.00033391805,0.000071639886,0.00013103086],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00017757443,0.00029486883,0.0004092965,0.00005772647,0.000058771846,0.00006666687,0.00035587116,0.0003042077,0.9603855],"category_scores_gemma":[0.00003643833,0.00022485896,0.00012069497,0.000004394301,0.0001077726,2.527406e-7,0.000029908984,0.00009968882,0.17685786],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000450122,0.000008186343,0.000005803269,0.00020272349,0.000042583706,0.000007933566,0.000020851565,0.00003630478,4.0442174e-7,0.000021783162,0.99508435,0.0045240624],"study_design_scores_gemma":[0.0002789923,0.00008174449,0.000037273192,0.0001465569,0.000033871318,0.000013253999,0.000010915745,0.000002714144,0.0000121589,0.000038898055,0.999045,0.00029857905],"about_ca_topic_score_codex":0.017813724,"about_ca_topic_score_gemma":0.004654738,"teacher_disagreement_score":0.7835276,"about_ca_system_score_codex":0.000005328802,"about_ca_system_score_gemma":0.000028635728,"threshold_uncertainty_score":0.98872674},"labels":[],"label_agreement":null},{"id":"W7042379995","doi":"","title":"1-800-769-28O5 norton antivirus tech support phone number","year":2016,"lang":"en","type":"other","venue":"OSF Preprints (OSF Preprints)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Phone; The Internet; Mobile phone; Service (business); Mobile phone tracking; Smart phone","score_opus":0.009700576315994197,"score_gpt":0.2326844957367555,"score_spread":0.22298391942076132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7042379995","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0038725305,0.0000040780933,0.00019635212,0.000087951186,0.0021955066,0.0009396849,0.0010820153,0.00039857454,0.99122334],"genre_scores_gemma":[0.026804907,0.0004716994,0.0005743574,0.00013101373,0.00087997504,0.000037537928,0.00038991641,0.00018633578,0.97052425],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99457103,0.0004851096,0.00070700696,0.0025935895,0.0007352646,0.0009079853],"domain_scores_gemma":[0.9950675,0.00024261643,0.0006350387,0.0035947107,0.00008263281,0.00037752066],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0022806544,0.00073353265,0.0009991458,0.0002151418,0.00017343705,0.00021929936,0.0016650755,0.00071809255,0.9874212],"category_scores_gemma":[0.00025797237,0.00063659507,0.0003030038,0.00019044918,0.00027677725,0.00023493072,0.0005159455,0.00043331727,0.9885882],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000092843286,0.00012171863,0.029926294,0.0002003466,0.00033201242,0.00011872285,0.0001350711,0.00002051746,0.0016885275,0.00019296592,0.94304246,0.024128517],"study_design_scores_gemma":[0.00050219364,0.0000012449815,0.009132896,0.00018297695,0.00010934502,0.00003512812,0.000010285352,0.000010621608,0.003592342,0.0014872458,0.98411906,0.0008166451],"about_ca_topic_score_codex":0.0069546946,"about_ca_topic_score_gemma":0.001749447,"teacher_disagreement_score":0.04107661,"about_ca_system_score_codex":0.000025274026,"about_ca_system_score_gemma":0.00023937025,"threshold_uncertainty_score":0.9996581},"labels":[],"label_agreement":null},{"id":"W7042614567","doi":"","title":"Rayleigh-Taylor instability of a thin elastic solid loaded by a shock wave","year":2024,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Instability; Shock wave; Shock (circulatory); Work (physics); Stability (learning theory)","score_opus":0.012768038168398744,"score_gpt":0.21974440440160747,"score_spread":0.20697636623320873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7042614567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9401411,0.0008417136,2.5548815e-7,0.000013394054,0.0041208374,0.00077703333,0.015481296,0.0001932428,0.038431138],"genre_scores_gemma":[0.9873808,0.00010089534,0.00017752073,0.000068455214,0.00011709674,0.000027306845,0.007850987,0.00006742038,0.004209537],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9949585,0.00042768143,0.0013354591,0.0013603092,0.0010658278,0.00085220207],"domain_scores_gemma":[0.9973335,0.00043870482,0.000655672,0.00085921213,0.00030544878,0.00040741274],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010392326,0.00087927276,0.0013120406,0.0002825623,0.00052361656,0.00019366974,0.0007614947,0.000838177,0.003057846],"category_scores_gemma":[0.0005066932,0.00078477315,0.0004509664,0.00057842204,0.00011761819,0.0006065419,0.00007539191,0.0011412788,0.0012177675],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031664183,0.0011238544,0.00031666923,0.012077757,0.0027287942,0.001238892,0.00033983524,0.00128011,0.83095294,0.028884908,0.0006683381,0.11722149],"study_design_scores_gemma":[0.0021542443,0.0011771315,0.0077679283,0.0017124299,0.0018330537,0.00007580734,0.0008476024,0.0009789548,0.75491834,0.11256689,0.11178589,0.0041817226],"about_ca_topic_score_codex":0.0034041868,"about_ca_topic_score_gemma":0.0057262355,"teacher_disagreement_score":0.11303976,"about_ca_system_score_codex":0.00005697433,"about_ca_system_score_gemma":0.00010575404,"threshold_uncertainty_score":0.9995599},"labels":[],"label_agreement":null},{"id":"W7043524763","doi":"","title":"+91 7073778243 strong vashikaran mantra for husband in Solapur Thane","year":2021,"lang":"en","type":"other","venue":"OSF Preprints (OSF Preprints)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tamil; Girl; Wife; Dowry; Agra; Caste; Mantra","score_opus":0.015555560260851736,"score_gpt":0.23580179100697546,"score_spread":0.22024623074612373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7043524763","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0075253695,0.00004351812,0.0004528561,0.0001001844,0.0015175877,0.0016150939,0.00077161606,0.0001241326,0.98784965],"genre_scores_gemma":[0.036917176,0.00037331638,0.0014239049,0.00008146875,0.0006552185,0.00008934665,0.001047449,0.00014108678,0.959271],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99555635,0.0004162744,0.0006120985,0.0022227273,0.00041082746,0.0007817417],"domain_scores_gemma":[0.99667,0.00034080152,0.0003754419,0.0023152088,0.000055973345,0.00024255474],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0021232434,0.00053811056,0.00092594617,0.00023910227,0.000107945554,0.00023945422,0.0010992637,0.00054553925,0.83350575],"category_scores_gemma":[0.00033590876,0.0005530767,0.00025934368,0.00018290713,0.00011671086,0.000121352634,0.00025156632,0.000391354,0.2654011],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006823475,0.00068885396,0.062449135,0.0033189724,0.0014358693,0.00042545967,0.0015157085,0.00492333,0.005389544,0.002425704,0.8503158,0.06642925],"study_design_scores_gemma":[0.0012727907,0.000004013391,0.026927525,0.0005312866,0.00012811394,0.000016873879,0.00007530295,0.00050453807,0.0016676133,0.0019460212,0.96599954,0.0009263997],"about_ca_topic_score_codex":0.0067462176,"about_ca_topic_score_gemma":0.010658389,"teacher_disagreement_score":0.5681046,"about_ca_system_score_codex":0.000020467047,"about_ca_system_score_gemma":0.00023226444,"threshold_uncertainty_score":0.9998679},"labels":[],"label_agreement":null},{"id":"W7043551526","doi":"","title":"Surface-Wave Tomography of Western Canada Using a Two-station Approach","year":2017,"lang":"en","type":"dissertation","venue":"Mspace (University of Manitoba)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Seismic tomography; Precambrian; Travel time; Slab; Dispersion (optics); Perturbation (astronomy)","score_opus":0.02195842038345291,"score_gpt":0.1968797750902036,"score_spread":0.1749213547067507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7043551526","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909694,0.00010837627,0.00005805151,0.00001450733,0.0005758152,0.0001914541,0.00073699973,0.000009221426,0.007336179],"genre_scores_gemma":[0.9963405,0.000032020354,0.0010718689,0.0000031157067,0.00004528651,2.0343895e-8,0.001674993,0.0000058359324,0.00082634395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903184,0.00006681799,0.00011352716,0.00024235871,0.00036009765,0.00018537439],"domain_scores_gemma":[0.99888986,0.000029583982,0.00059193216,0.00027720327,0.00014171685,0.00006972499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012755036,0.00016874689,0.0003937077,0.00009209677,0.0002383144,0.00003108314,0.0003122852,0.000114362774,0.00004787174],"category_scores_gemma":[0.000005136784,0.00020120581,0.00008822403,0.000092462724,0.000061677565,0.00019763461,0.000012122994,0.000095913805,0.0000037259574],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012166236,0.00015027374,0.9130545,0.0044581234,0.0012583435,0.00024422683,0.0038400018,0.052380197,0.01213537,0.00024610508,0.004865979,0.00615026],"study_design_scores_gemma":[0.0004990444,0.00006657815,0.9822167,0.0001779067,0.00029124762,0.0000022937243,0.009489364,0.0039643613,0.0008893762,0.000078205245,0.0019330373,0.0003918486],"about_ca_topic_score_codex":0.9598547,"about_ca_topic_score_gemma":0.998586,"teacher_disagreement_score":0.06916224,"about_ca_system_score_codex":0.00001342161,"about_ca_system_score_gemma":0.0003985446,"threshold_uncertainty_score":0.8204935},"labels":[],"label_agreement":null},{"id":"W7066032598","doi":"","title":"Geodetic and paleo-shoreline evidence of glacial-isostatic adjustment in the Churchill regioon, Canada: data reanalysis and inversion in terms of mantle viscosity","year":2005,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geodetic datum; Inversion (geology); Mantle (geology); Inverse theory; Viscosity","score_opus":0.05545676759041785,"score_gpt":0.31682991351593903,"score_spread":0.2613731459255212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7066032598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98475164,0.00073667965,0.00006232971,0.009170884,0.000053611646,0.00082316564,0.0043083117,0.0000039488905,0.00008942913],"genre_scores_gemma":[0.99551934,0.001113477,0.00053343567,0.00011849899,0.000044786855,0.000007327996,0.002619588,0.000002180349,0.000041376956],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973708,0.00036594944,0.000447251,0.00050401775,0.0009001969,0.00041182712],"domain_scores_gemma":[0.99794775,0.00078570493,0.00018626924,0.00079035887,0.00015831892,0.00013157887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0045405873,0.00010807512,0.00022461942,0.0002903969,0.00015817594,0.00008236533,0.00092162,0.00002981952,0.00013765147],"category_scores_gemma":[0.00093723286,0.00007622659,0.000015480757,0.000856166,0.00034512096,0.00088196964,0.00022130618,0.00011826775,0.0000019585652],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005645375,0.00059062726,0.80276036,0.0016930471,0.00005817267,0.000015410365,0.0044884407,0.000556974,0.0026678888,0.0026740325,0.07042859,0.11350189],"study_design_scores_gemma":[0.0005217846,0.00009596267,0.88765943,0.00022414482,0.000031391595,0.0000030854724,0.0005364791,0.09186801,0.00039966387,0.00047020701,0.018017922,0.0001719186],"about_ca_topic_score_codex":0.38101682,"about_ca_topic_score_gemma":0.8147136,"teacher_disagreement_score":0.43369678,"about_ca_system_score_codex":0.00001745614,"about_ca_system_score_gemma":0.00028078316,"threshold_uncertainty_score":0.62310505},"labels":[],"label_agreement":null},{"id":"W7067163201","doi":"","title":"The leading Clydesdale sires in Canada","year":2010,"lang":"en","type":"article","venue":"University Library - University of Saskatchewan (University of Saskatchewan)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"","score_opus":0.004164855832086318,"score_gpt":0.13483756408401373,"score_spread":0.13067270825192742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7067163201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936379,0.000052077492,0.000056691213,0.0008158885,0.00044932106,0.00024048389,0.0006719863,0.00005830155,0.0040173214],"genre_scores_gemma":[0.98553675,0.00014876811,0.0017611429,0.000029427665,0.00004145456,3.2672092e-9,0.00010652862,0.000009163065,0.012366738],"study_design_codex":"observational","study_design_gemma":"qualitative","domain_scores_codex":[0.99811625,0.0001809165,0.00020657608,0.00048287326,0.00044401133,0.00056939264],"domain_scores_gemma":[0.99830014,0.0003881283,0.00036862932,0.000552844,0.0000886725,0.0003015883],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023483027,0.00028274668,0.0005486832,0.00023862073,0.00073919375,0.000031300413,0.0016839568,0.00019853663,0.002477675],"category_scores_gemma":[0.000009359277,0.00033322984,0.00019749207,0.0006810708,0.000777244,0.0014254941,0.00026563636,0.00048029667,0.00006148742],"study_design_candidate":"qualitative","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036942228,0.0003666865,0.7053481,0.0004713957,0.0008040875,0.0026597132,0.2198262,0.003996589,0.015335413,0.0006319184,0.009097165,0.03776855],"study_design_scores_gemma":[0.0016082143,0.00011497119,0.16216233,0.00007455554,0.00011173873,0.0000067984843,0.77700573,0.0005285682,0.0011565144,0.00041587025,0.056228194,0.00058650563],"about_ca_topic_score_codex":0.9681637,"about_ca_topic_score_gemma":0.99494404,"teacher_disagreement_score":0.5571795,"about_ca_system_score_codex":0.000049697912,"about_ca_system_score_gemma":0.002687941,"threshold_uncertainty_score":0.99991196},"labels":[],"label_agreement":null},{"id":"W7067850781","doi":"","title":"Mantle velocity variations under the northern Canadian Cordillera through body wave tomography","year":2020,"lang":"en","type":"article","venue":"Digital Collections of Colorado (Colorado State University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic tomography; Tomography; Mantle (geology); Wave velocity; Surface wave","score_opus":0.014120434367781973,"score_gpt":0.16509775161165918,"score_spread":0.1509773172438772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7067850781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.796417,0.000042952295,0.0021508227,0.0047560656,0.00063418085,0.00107758,0.006434593,0.00015935424,0.18832746],"genre_scores_gemma":[0.9971811,0.00003274917,0.00011526066,0.00023938954,0.00004849617,8.152852e-7,0.0001717431,0.000007889353,0.002202559],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.99884677,0.000079199,0.00021069405,0.00029101517,0.00022088377,0.00035141138],"domain_scores_gemma":[0.99902177,0.00014569468,0.00014185318,0.00021320173,0.00022274478,0.0002547323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057276036,0.00018350375,0.00026085766,0.0002282722,0.0009991251,0.0002525909,0.00035419324,0.000074063646,0.00082700356],"category_scores_gemma":[0.000025513295,0.00014900124,0.00013377548,0.0024095194,0.00021836015,0.00065125746,0.000040446852,0.00014633097,0.00008307075],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008019729,0.0030619772,0.20686536,0.0008160221,0.012875387,0.0020072781,0.049916957,0.35449794,0.0020356097,0.121580094,0.21759747,0.02072616],"study_design_scores_gemma":[0.0024692365,0.0021149504,0.14659716,0.000043746746,0.00046065685,0.000018380699,0.008532986,0.014686823,0.0006349959,0.010276721,0.8126923,0.0014720437],"about_ca_topic_score_codex":0.050738934,"about_ca_topic_score_gemma":0.19784397,"teacher_disagreement_score":0.5950948,"about_ca_system_score_codex":0.00003466482,"about_ca_system_score_gemma":0.00050489546,"threshold_uncertainty_score":0.95558226},"labels":[],"label_agreement":null},{"id":"W7071707059","doi":"","title":"Understanding Public Responses to Domestic Threats","year":2007,"lang":"en","type":"article","venue":"Defense Technical Information Center (DTIC)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Affect (linguistics); Normative; Anger; Public opinion; Risk assessment; Estimation; Trait; Compliance (psychology)","score_opus":0.09107655789091339,"score_gpt":0.2841340839966967,"score_spread":0.1930575261057833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071707059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6662855,0.00005788327,0.20526654,0.0028802892,0.002003472,0.0012321604,0.00064641656,0.00087848376,0.12074925],"genre_scores_gemma":[0.99682575,0.000011998845,0.0014574568,0.0013348007,0.000079266094,0.0000021000128,0.00021107851,0.0000036795739,0.000073870324],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99851584,0.00004079706,0.0004786673,0.00014228135,0.00035701523,0.00046538623],"domain_scores_gemma":[0.9990189,0.00026106453,0.00010698229,0.0002592704,0.00006973513,0.0002840527],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008989162,0.00015097327,0.00018182106,0.00025854062,0.00018490998,0.00028116175,0.00023236273,0.000101049896,0.0006626586],"category_scores_gemma":[0.00022150893,0.0001236715,0.00006004558,0.00034585598,0.00006056131,0.0008875183,0.000041250045,0.0001141316,0.0015745533],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0061359066,0.0006834325,0.31732112,0.00071170134,0.00041403083,0.00041584033,0.0062536886,0.002893284,0.0054786187,0.432789,0.09643693,0.13046643],"study_design_scores_gemma":[0.0024034348,0.0008531247,0.6312381,0.00018618107,0.000074862604,0.0003230743,0.0007984813,0.0009611512,0.0010166581,0.028076071,0.33258265,0.0014861884],"about_ca_topic_score_codex":0.00006738974,"about_ca_topic_score_gemma":0.00019353736,"teacher_disagreement_score":0.40471292,"about_ca_system_score_codex":0.000027279273,"about_ca_system_score_gemma":0.000036540012,"threshold_uncertainty_score":0.99920285},"labels":[],"label_agreement":null},{"id":"W7071741379","doi":"","title":"Ãtudes des fuites excitoniques dans des familles de boîtes quantiques d'InAs/InP par PLRT par addition de fréquences","year":2012,"lang":"fr","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Limiting; Work (physics); Derogation; Nucleofection","score_opus":0.005283750478946504,"score_gpt":0.14569509049818827,"score_spread":0.14041134001924177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071741379","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.62165385,0.010440903,0.0002176776,0.0007477173,0.0006173236,0.0003980884,0.005505211,0.00005018978,0.36036903],"genre_scores_gemma":[0.9481774,0.009220422,0.012955066,0.00048997137,0.0006366958,0.000019177567,0.00021175828,0.00006724527,0.02822227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99649197,0.0004463781,0.0005103957,0.0004756573,0.0010634571,0.0010121384],"domain_scores_gemma":[0.99795455,0.0007130406,0.00041298917,0.00026665567,0.0000028339184,0.0006499393],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006561746,0.0005879755,0.0006797214,0.000054782115,0.0006481092,0.00018922286,0.00052669307,0.0001557636,0.0031543793],"category_scores_gemma":[0.000018039073,0.0005243122,0.00008750379,0.000098419536,0.0009721674,0.0008647461,0.00009974197,0.0002087989,1.5632655e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048200926,0.00013915183,0.79735875,0.002986773,0.0007175213,0.00026301548,0.0030630233,0.00025945995,0.069832094,0.071695216,0.010126869,0.04307611],"study_design_scores_gemma":[0.00019927566,0.00027297923,0.60854316,0.0013655837,0.00016963277,0.000024692068,0.0031902764,0.0003972434,0.2275292,0.019911448,0.13750874,0.00088777154],"about_ca_topic_score_codex":0.12983896,"about_ca_topic_score_gemma":0.3377605,"teacher_disagreement_score":0.33214673,"about_ca_system_score_codex":0.000012584138,"about_ca_system_score_gemma":0.001829498,"threshold_uncertainty_score":0.9997209},"labels":[],"label_agreement":null},{"id":"W7072108027","doi":"","title":"Victory Square Technologies Reports Record 6th Consecutive Quarter With Positive Net Income &amp;amp; Earnings Per Share \\n\\n\\tTamar Securities Financial Portal","year":2021,"lang":"en","type":"other","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Earnings; Quarter (Canadian coin); Net income; Square (algebra); Net worth","score_opus":0.006716158438312287,"score_gpt":0.19862378876910167,"score_spread":0.1919076303307894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072108027","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13038214,0.003792378,0.00013900684,0.00031471928,0.0032719085,0.0015010254,0.0072494647,0.0014961183,0.85185325],"genre_scores_gemma":[0.27025053,0.000375524,0.0037310692,0.0003916995,0.0011164052,0.00005585351,0.015171117,0.00023333222,0.7086745],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9973376,0.00012924963,0.00048630856,0.00094785163,0.00048808518,0.0006109387],"domain_scores_gemma":[0.99839544,0.000088601264,0.0006065179,0.0006260564,0.00016522344,0.000118136886],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016516777,0.0006508972,0.0009263217,0.00025388104,0.00019560852,0.00023858958,0.00029091258,0.00065432827,0.08516077],"category_scores_gemma":[0.00006944825,0.0004945311,0.00015284219,0.00021379282,0.00036875295,0.00015733183,0.00007851918,0.00046435025,0.0004456404],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001787288,0.00006803798,0.101714715,0.0006142542,0.00047944047,0.0022975528,0.00225264,0.000019197942,0.00007422511,0.00023794119,0.8907502,0.0013130313],"study_design_scores_gemma":[0.00023778954,0.00022692054,0.044073876,0.0009776298,0.000096636824,0.00023022582,0.00090369105,0.0000015249317,0.00005794562,0.0003034251,0.9518705,0.0010198598],"about_ca_topic_score_codex":0.01131007,"about_ca_topic_score_gemma":0.059790853,"teacher_disagreement_score":0.14317878,"about_ca_system_score_codex":0.000010265522,"about_ca_system_score_gemma":0.0004638642,"threshold_uncertainty_score":0.9997506},"labels":[],"label_agreement":null},{"id":"W7072189319","doi":"","title":"Two-station Rayleigh wave tomography of Canada","year":2022,"lang":"en","type":"dissertation","venue":"Mspace (University of Manitoba)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Seismic tomography; Mantle (geology); Tectonics; Crust; Rayleigh wave; Seismic anisotropy; Anisotropy; Tomography","score_opus":0.007229044862608859,"score_gpt":0.16657966164719296,"score_spread":0.1593506167845841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072189319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9786367,0.00016018646,0.000005627871,0.00006419416,0.00103872,0.00016765381,0.001211159,0.000012328278,0.018703429],"genre_scores_gemma":[0.99422354,0.000060922193,0.00026081083,0.000009812217,0.000041228708,8.576086e-8,0.0036611957,0.000005082993,0.0017373366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989987,0.00007570856,0.0001096573,0.00020652593,0.00043562683,0.00017375655],"domain_scores_gemma":[0.9992535,0.000054940112,0.00035372627,0.00017646002,0.00009781627,0.00006352137],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011689259,0.00013636728,0.00030434877,0.00014086287,0.00020683449,0.000009824251,0.0002497172,0.000064874126,0.0012325374],"category_scores_gemma":[0.000005937234,0.00017027275,0.00009150442,0.00021965006,0.000033126325,0.00010493537,0.000015136722,0.00011073645,0.0000053011163],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.007394444,0.0006816068,0.5389053,0.009874242,0.0045194915,0.0017880114,0.01850042,0.038873836,0.02327665,0.013210444,0.30206957,0.040905926],"study_design_scores_gemma":[0.00047752078,0.0001481733,0.9455507,0.0000563435,0.00018800116,0.0000011955642,0.02930788,0.00027912296,0.0010061127,0.00037637277,0.022263886,0.00034472972],"about_ca_topic_score_codex":0.91779995,"about_ca_topic_score_gemma":0.9990327,"teacher_disagreement_score":0.40664533,"about_ca_system_score_codex":0.0000120410905,"about_ca_system_score_gemma":0.00033342425,"threshold_uncertainty_score":0.99968046},"labels":[],"label_agreement":null},{"id":"W7072255106","doi":"","title":"2021-11-14 Vulgar Royalty","year":2021,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"West virginia; Collectable; Quarter (Canadian coin); George (robot)","score_opus":0.005349378629332009,"score_gpt":0.17088574864299533,"score_spread":0.1655363700136633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072255106","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00015923665,0.0008384278,2.2530897e-7,0.00008327508,0.0011577976,0.00026841948,0.0008281097,0.00007458243,0.9965899],"genre_scores_gemma":[0.0009779878,0.0004032933,0.0006415003,0.00018325119,0.0005418051,0.0000025667298,0.0017045343,0.00004113202,0.9955039],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99827886,0.00010337676,0.00054410845,0.00025643353,0.0004582024,0.00035899744],"domain_scores_gemma":[0.99875337,0.000084372565,0.00047149928,0.0004157645,0.00011852402,0.00015646563],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00021888727,0.0003406341,0.000534327,0.00005544876,0.00007645283,0.00010758703,0.0003569105,0.00037478103,0.93296725],"category_scores_gemma":[0.000063110405,0.00031241684,0.00015454464,0.000010490951,0.0000945129,2.0484904e-7,0.000044631244,0.0001717861,0.026515009],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021449941,0.000015494637,0.000026769027,0.00037082797,0.00005663147,0.000033014752,0.00003814024,0.0004595481,4.8870265e-7,0.000016228041,0.9970341,0.0019273425],"study_design_scores_gemma":[0.00026105196,0.00006407545,0.0001373321,0.0002002481,0.00004939457,0.000020436868,0.000027624857,0.000023411105,0.000014099029,0.0000133864305,0.9988395,0.00034942778],"about_ca_topic_score_codex":0.040401507,"about_ca_topic_score_gemma":0.020283278,"teacher_disagreement_score":0.90645224,"about_ca_system_score_codex":0.0000046468153,"about_ca_system_score_gemma":0.000051426396,"threshold_uncertainty_score":0.99993277},"labels":[],"label_agreement":null},{"id":"W7072322472","doi":"","title":"« Vous avez bien là dequoy vous contenter les yeux, l'odorat & l'appetit ». Usages, fonctions et enjeux du lexique des perceptions sensorielles dans les récits de voyages français en Amérique (1545-1618)","year":2023,"lang":"en","type":"dissertation","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Narrative; Sensibility; Romance; Perception; Travel writing; Lexicon","score_opus":0.01894374618606841,"score_gpt":0.2357830527715228,"score_spread":0.2168393065854544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072322472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9423256,0.0009286725,0.011244664,0.0025169337,0.00069183076,0.0006908952,0.0013387699,0.00053103745,0.039731592],"genre_scores_gemma":[0.9327444,0.004650456,0.0042396304,0.000100740144,0.00014409973,0.00006503547,0.008238435,0.000077258526,0.04973994],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9933595,0.003934627,0.0006894572,0.0008575945,0.00049404486,0.00066476746],"domain_scores_gemma":[0.9949495,0.0016926947,0.0004453472,0.0010382412,0.001572852,0.00030133873],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0026371235,0.00058378844,0.0005948972,0.00031505275,0.0013602102,0.0007229565,0.0010241416,0.00055770687,0.0012378264],"category_scores_gemma":[0.0012209966,0.0005721375,0.00031338446,0.00050799,0.00033577473,0.00033927552,0.00011368153,0.00062580185,0.00041670553],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035128437,0.0015895722,0.22972113,0.0021591566,0.0013400447,0.0002625432,0.40950412,0.0037872577,0.16237636,0.029767489,0.023459964,0.1356811],"study_design_scores_gemma":[0.001123123,0.000013614606,0.85349774,0.0034318385,0.00038677343,0.00008132321,0.014112677,0.0044210097,0.037191525,0.0035700963,0.08021345,0.0019568496],"about_ca_topic_score_codex":0.08317486,"about_ca_topic_score_gemma":0.45227855,"teacher_disagreement_score":0.6237766,"about_ca_system_score_codex":0.000050959745,"about_ca_system_score_gemma":0.00033298187,"threshold_uncertainty_score":0.99993986},"labels":[],"label_agreement":null},{"id":"W7072461351","doi":"","title":"إن الشرك لظلم عظيم 360 ان الشرک لظلم عظیم","year":2022,"lang":"ar","type":"other","venue":"Internet Archive (Internet Archive)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Brother; Islam; State (computer science); Supporter; Hinduism","score_opus":0.011179773642287042,"score_gpt":0.21106566753490397,"score_spread":0.19988589389261693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072461351","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.028678764,0.0019433122,0.00067040446,0.00035121164,0.01285217,0.0021043445,0.016859382,0.00041307876,0.9361273],"genre_scores_gemma":[0.19318835,0.0008776615,0.0010006599,0.0010184952,0.0045803995,0.00010857849,0.009398698,0.00043426763,0.7893929],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9875614,0.0022695067,0.0021613454,0.003410973,0.0018171346,0.0027796603],"domain_scores_gemma":[0.993532,0.0013583025,0.0015800229,0.002173202,0.00008643963,0.0012700186],"candidate_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.0010696666,0.0024382279,0.0026423328,0.0012457116,0.00035828422,0.0010187991,0.005073167,0.00048201953,0.60714096],"category_scores_gemma":[0.00017272195,0.0022721763,0.0014155427,0.0004091579,0.0012824403,0.00033004826,0.0023110984,0.002465476,0.074512936],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010944644,0.0002846641,0.0068445387,0.000472964,0.0016702372,0.0011106934,0.008283769,0.00036147318,0.0008379593,0.004460257,0.973104,0.0014750054],"study_design_scores_gemma":[0.0015068789,0.001636185,0.0073662354,0.0009098818,0.00044859227,0.00018566426,0.00032352054,0.0030110176,0.00040062916,0.0055152457,0.9761958,0.0025003613],"about_ca_topic_score_codex":0.107089095,"about_ca_topic_score_gemma":0.06795581,"teacher_disagreement_score":0.532628,"about_ca_system_score_codex":0.000064353706,"about_ca_system_score_gemma":0.00040303794,"threshold_uncertainty_score":0.99983585},"labels":[],"label_agreement":null},{"id":"W7072480478","doi":"","title":"The wider international context","year":2025,"lang":"en","type":"book-chapter","venue":"Åbo Akademi University Research Portal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"","score_opus":0.033726709077861995,"score_gpt":0.2632151217056627,"score_spread":0.2294884126278007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072480478","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00040502046,0.000381073,0.0000053169974,0.0014469108,0.0011760626,0.0002551906,0.0009985648,0.00003249582,0.99529934],"genre_scores_gemma":[0.05256291,0.0013448966,0.000014908274,0.00006244006,0.0004054498,1.4567814e-7,0.00045247716,0.000005381492,0.9451514],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99810445,0.00009455158,0.0001783505,0.0003711778,0.00084254344,0.00040891956],"domain_scores_gemma":[0.9985442,0.0005583249,0.000100735655,0.0003347736,0.00030617617,0.00015578285],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007952868,0.00017960001,0.00022099224,0.00018406045,0.00071617594,0.00015416513,0.001081498,0.00026769022,0.011923882],"category_scores_gemma":[0.000055956516,0.00014323596,0.00013050083,0.00006352717,0.00049130025,0.00016176178,0.00018498457,0.0007576428,0.0010172434],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018555774,0.00000806099,0.0010600504,0.00002679696,0.00036786508,0.0005531399,0.000095926924,0.000013976331,0.000011170384,0.43468052,0.5341907,0.028806217],"study_design_scores_gemma":[0.000155062,0.000035054087,0.0009078898,0.000057256857,0.000020726135,0.0000037277819,0.0001887679,0.000042849133,0.00000987821,0.005091178,0.9933394,0.0001482131],"about_ca_topic_score_codex":0.001859448,"about_ca_topic_score_gemma":0.003771117,"teacher_disagreement_score":0.45914868,"about_ca_system_score_codex":0.000014361382,"about_ca_system_score_gemma":0.0003730867,"threshold_uncertainty_score":0.99976057},"labels":[],"label_agreement":null},{"id":"W7072534438","doi":"","title":"イギリスの成年後見制度にみる市民社会の構想¹⁾","year":2011,"lang":"en","type":"article","venue":"Hosei University Repository (Hosei University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Legal guardian; Dignity; Autonomy; Realm; Legislation; Guardian; Civil society; State (computer science); Legislature","score_opus":0.012688849621135036,"score_gpt":0.12733888104444843,"score_spread":0.1146500314233134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072534438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.61320263,0.000037176054,0.00017672732,0.000027751756,0.0008857043,0.00016495254,0.00008860212,0.00020624153,0.38521022],"genre_scores_gemma":[0.95279634,0.00006803646,0.00070298085,0.000038410024,0.00014092267,1.8778376e-8,0.00004253622,0.0000080791,0.04620268],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99835145,0.00020322796,0.00015193399,0.00054143334,0.00027004138,0.00048190693],"domain_scores_gemma":[0.9988374,0.000054547392,0.00016730513,0.0004819868,0.000116815805,0.0003419603],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000116530995,0.00026473077,0.00030687574,0.00033450813,0.0007182722,0.00005063813,0.0007911748,0.00018524712,0.0015033218],"category_scores_gemma":[0.0000065998606,0.00030135916,0.00017831555,0.00055818894,0.00024619876,0.00077328034,0.00010177695,0.00018981559,0.00055268395],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00557985,0.0014058541,0.79691625,0.00043466783,0.0020542056,0.037790112,0.0173801,0.0010383064,0.021240829,0.06971068,0.029187353,0.01726179],"study_design_scores_gemma":[0.0015782771,0.00046527348,0.329648,0.000057232122,0.00035115864,0.00007134262,0.0033959395,0.00023555134,0.0070121265,0.0003084761,0.65575105,0.0011255798],"about_ca_topic_score_codex":0.008106502,"about_ca_topic_score_gemma":0.00046357614,"teacher_disagreement_score":0.62656367,"about_ca_system_score_codex":0.00003461757,"about_ca_system_score_gemma":0.00013388274,"threshold_uncertainty_score":0.99994385},"labels":[],"label_agreement":null},{"id":"W7072563301","doi":"","title":"مثاني تقدم: ❖ مرئي: ما هو هدف التحالف الصليبي جمادى الآخرة 1444 هـ ISLAMIC STATE VIDEO اصدار الدولة الإسلامية","year":2020,"lang":"ar","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Islam; Brother; State (computer science); Supporter","score_opus":0.005204237839731314,"score_gpt":0.164352820208625,"score_spread":0.15914858236889368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072563301","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004536637,0.0012867824,0.000001306636,0.0007349969,0.0027346222,0.0012949592,0.004338744,0.00026331635,0.9848086],"genre_scores_gemma":[0.030379238,0.0026073195,0.00074748264,0.0012076867,0.0010612174,0.000015801756,0.0021324498,0.00013953206,0.96170926],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99359393,0.0004633453,0.0022567858,0.00092965754,0.0014158685,0.0013403975],"domain_scores_gemma":[0.9957774,0.0004254703,0.001912519,0.0010105816,0.00031647732,0.0005575082],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["metaepi_narrow","insufficient_payload"],"category_scores_codex":[0.00077953335,0.0013123216,0.0017495757,0.00018637037,0.00041173762,0.00055479514,0.0014404696,0.0008578493,0.7235794],"category_scores_gemma":[0.0002210637,0.0012501727,0.0005634102,0.000052996653,0.00045711006,0.000003713078,0.0002590422,0.0008309405,0.25229642],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045315866,0.00006897221,0.000027668493,0.001463943,0.00035510404,0.00015481854,0.0012679038,0.0044483165,0.000024687706,0.00004638908,0.98855805,0.0031309745],"study_design_scores_gemma":[0.0011742089,0.00069313083,0.0002980432,0.00060830056,0.00027676165,0.00008664773,0.00022351378,0.0003291171,0.00014162424,0.00016389761,0.99465734,0.0013474316],"about_ca_topic_score_codex":0.029002333,"about_ca_topic_score_gemma":0.007453661,"teacher_disagreement_score":0.471283,"about_ca_system_score_codex":0.000038590646,"about_ca_system_score_gemma":0.000235286,"threshold_uncertainty_score":0.9999628},"labels":[],"label_agreement":null},{"id":"W7072611731","doi":"","title":"Waste Heat-to-Power Capture Pilot Launched in Ontario","year":2022,"lang":"en","type":"other","venue":"Power","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Launched; Thermal power station; Municipal solid waste; Power station; Waste disposal","score_opus":0.010545584531729645,"score_gpt":0.19354931661395683,"score_spread":0.18300373208222717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072611731","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02533474,0.00042226518,0.00000234483,0.00016930066,0.003298738,0.0004485667,0.0006099331,0.00007386502,0.96964025],"genre_scores_gemma":[0.23048916,0.000009063557,0.00014658833,0.0009482413,0.00020008264,0.000011208447,0.00058700703,0.00008912142,0.76751953],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985319,0.00007440004,0.00020228678,0.00044737695,0.00033188344,0.00041217532],"domain_scores_gemma":[0.9993583,0.000025829831,0.000058902788,0.00040076274,0.000009908324,0.00014627787],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00017606052,0.00028661368,0.00041978213,0.00018404145,0.0000474846,0.00006327728,0.00035988886,0.00013248855,0.46190664],"category_scores_gemma":[0.000009225017,0.00024407344,0.000059944654,0.00014724613,0.0000236021,0.00003990074,0.000053695876,0.0003203941,0.0025208783],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009451252,0.00006749632,0.018430449,0.000024482026,0.00006461543,0.00013715819,0.0013003588,0.00035175838,0.00012929419,0.00010414189,0.9792273,0.00006842987],"study_design_scores_gemma":[0.00022643356,0.00019278715,0.021686886,0.000030203042,0.000011650919,0.0000020147759,0.000051873572,0.0000014124305,0.000006292645,0.00006942449,0.97739375,0.0003273036],"about_ca_topic_score_codex":0.49714714,"about_ca_topic_score_gemma":0.7916897,"teacher_disagreement_score":0.45938575,"about_ca_system_score_codex":0.000018319257,"about_ca_system_score_gemma":0.00013343901,"threshold_uncertainty_score":0.9982558},"labels":[],"label_agreement":null},{"id":"W7072684913","doi":"","title":"والعاقبة للمتقين ولاية غرب إفريقية","year":2022,"lang":"ar","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Brother; Islam; State (computer science); Supporter; Spanish Civil War","score_opus":0.005421093466083085,"score_gpt":0.16490339402044185,"score_spread":0.15948230055435877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072684913","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0017101252,0.00090906175,6.8405214e-8,0.0002458166,0.002286918,0.00074396183,0.0024528618,0.0001241316,0.9915271],"genre_scores_gemma":[0.008404634,0.000806742,0.00035657175,0.00053457025,0.0006570356,0.000013231693,0.0019988022,0.000067645626,0.98716074],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9960537,0.0003429014,0.0012686774,0.00049933814,0.0010444168,0.00079099316],"domain_scores_gemma":[0.9973281,0.00027826815,0.0011559472,0.00074279786,0.00016306444,0.00033184068],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007403588,0.0006963746,0.000957462,0.00011820617,0.00039569577,0.00023214743,0.00097546325,0.0004895528,0.9823218],"category_scores_gemma":[0.00011850529,0.0006746441,0.00034814293,0.000022420712,0.00024091711,7.2890776e-7,0.00019377192,0.00052260834,0.2235294],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018753225,0.000050857423,0.000039577375,0.0006735696,0.00016745871,0.000060752016,0.00048675013,0.003695725,0.0000012998552,0.000058617483,0.9924686,0.002109271],"study_design_scores_gemma":[0.00061901455,0.00043358354,0.00015907522,0.00013101986,0.00016046371,0.0000665516,0.00030030322,0.000071292314,0.000011901442,0.000038595943,0.9972596,0.0007485562],"about_ca_topic_score_codex":0.027613038,"about_ca_topic_score_gemma":0.0033648966,"teacher_disagreement_score":0.7587924,"about_ca_system_score_codex":0.000026604783,"about_ca_system_score_gemma":0.00010918156,"threshold_uncertainty_score":0.9995705},"labels":[],"label_agreement":null},{"id":"W7073089441","doi":"","title":"成層圏惑星規模波の下方伝播が北太平洋ブロッキングの形成に及ぼす影響","year":2013,"lang":"en","type":"article","venue":"Kyoto University Research Information Repository (Kyoto University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Blocking (statistics); Ridge; Trough (economics); Stratosphere; Sudden stratospheric warming; Reflection (computer programming)","score_opus":0.015278314783408537,"score_gpt":0.19284687979367665,"score_spread":0.1775685650102681,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073089441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5274033,0.0000067663764,0.00006733156,0.00022402771,0.00027202984,0.0006084831,0.00003925269,0.00012535545,0.47125348],"genre_scores_gemma":[0.95151746,0.00005581802,0.0001872072,0.00009510203,0.00009828097,3.350918e-7,0.00012271105,0.0000043988425,0.04791867],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976231,0.00039191465,0.00022046044,0.00029246171,0.0008252796,0.0006468246],"domain_scores_gemma":[0.9979375,0.00016884084,0.00014403097,0.00045393652,0.0007941341,0.0005015586],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00039058883,0.0001975066,0.00022008117,0.0009757612,0.001348439,0.0004245905,0.000967877,0.00018489762,0.0057689664],"category_scores_gemma":[0.000062804975,0.00021395173,0.00011126657,0.0011177828,0.00032152218,0.0053344127,0.00016837676,0.00035838343,0.014489031],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00436678,0.00075060024,0.3163672,0.0012600821,0.001458767,0.004654168,0.01895785,0.01165264,0.014271199,0.2404594,0.33334038,0.052460928],"study_design_scores_gemma":[0.00100543,0.00035358267,0.06531097,0.00003937825,0.000027751863,0.000042661748,0.0075643896,0.0011841693,0.0015883403,0.0006747719,0.9217442,0.0004643082],"about_ca_topic_score_codex":0.035479777,"about_ca_topic_score_gemma":0.00021899593,"teacher_disagreement_score":0.5884039,"about_ca_system_score_codex":0.00008218844,"about_ca_system_score_gemma":0.00037257615,"threshold_uncertainty_score":0.99995166},"labels":[],"label_agreement":null},{"id":"W7073524567","doi":"","title":"Implant-prosthetic rehabilitation after excision of hard palate gland carcinoma","year":2004,"lang":"en","type":"article","venue":"BOA (University of Milano-Bicocca)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Diafiltration; Liquation; Hyporeflexia; Fusible alloy; Dysgeusia","score_opus":0.006217878442665752,"score_gpt":0.16248562239533265,"score_spread":0.1562677439526669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073524567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982282,0.00010651806,0.00007224805,0.00023320493,0.00019969452,0.0001643863,0.0004015076,0.000016381473,0.000577895],"genre_scores_gemma":[0.9977702,0.0000339146,0.0019008329,0.00001507106,0.00002818208,8.562501e-8,0.00008974463,0.0000030432104,0.00015895824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919057,0.000052013496,0.00014326729,0.0002175451,0.00021276959,0.00018384811],"domain_scores_gemma":[0.99943256,0.00006089201,0.00012880594,0.00022645177,0.00007012081,0.000081185695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016627001,0.000109579254,0.00025035223,0.0000930903,0.00008774235,0.000010662337,0.0001882921,0.00007978805,0.00072442676],"category_scores_gemma":[0.000010114125,0.000109003966,0.000096642565,0.00011608977,0.00012481686,0.00018362331,0.000026040838,0.000049755254,0.00009283568],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024238655,0.00023076565,0.91900945,0.00069261034,0.00011967773,0.00023933972,0.010512771,0.003115428,0.049826566,0.00073409505,0.0021102508,0.010985211],"study_design_scores_gemma":[0.00087708974,0.00038200113,0.99311286,0.000058928777,0.000040793613,0.0000067664,0.000416102,0.00007970338,0.0006435238,0.0017692746,0.0024762782,0.00013667645],"about_ca_topic_score_codex":0.0057631186,"about_ca_topic_score_gemma":0.0014784323,"teacher_disagreement_score":0.074103445,"about_ca_system_score_codex":0.000005202541,"about_ca_system_score_gemma":0.000046282847,"threshold_uncertainty_score":0.871215},"labels":[],"label_agreement":null},{"id":"W7073524647","doi":"","title":"Helicobacter canadensis sp. nov. Isolated from Humans with Diarrhea as an Example of an Emerging Pathogen","year":2000,"lang":"en","type":"article","venue":"PubMed Central","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Helicobacter; Pathogen; Helicobacter pylori; Restriction fragment length polymorphism; Diarrhea; 16S ribosomal RNA; Nalidixic acid","score_opus":0.013296942707510353,"score_gpt":0.1889964234468147,"score_spread":0.17569948073930433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073524647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976548,0.000047183534,0.0000069878083,0.000044058797,0.00030397763,0.00021072703,0.0008484977,0.00003905768,0.000844726],"genre_scores_gemma":[0.9979259,0.000024493076,0.0001929752,0.00012794005,0.00040107925,0.0000040311565,0.001169908,0.00000918687,0.0001445117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99820256,0.00009678153,0.00021688841,0.0003442357,0.00023029267,0.00090923265],"domain_scores_gemma":[0.99906766,0.000021591692,0.00006997931,0.00030631782,0.000024362906,0.0005100626],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016640096,0.00016422558,0.00024278926,0.000033688753,0.00010973378,0.00008443423,0.00021860763,0.00006288989,0.008529407],"category_scores_gemma":[0.0000038391886,0.0001309781,0.0000337903,0.00011481618,0.000049326514,0.00036287424,0.000005310519,0.000070566224,0.000051151084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014307658,0.00034853368,0.76647574,0.00006034065,0.00046331345,0.00032449604,0.012756558,0.0056894035,0.011688281,0.00017737111,0.00047671612,0.2001085],"study_design_scores_gemma":[0.000349565,0.00011925488,0.98734033,0.000008581302,0.00005088192,0.000003903917,0.000059019574,0.0005057683,0.0022393414,0.00020035142,0.008889055,0.00023392304],"about_ca_topic_score_codex":0.345527,"about_ca_topic_score_gemma":0.121225886,"teacher_disagreement_score":0.22430113,"about_ca_system_score_codex":0.000005993198,"about_ca_system_score_gemma":0.000071451264,"threshold_uncertainty_score":0.9923769},"labels":[],"label_agreement":null},{"id":"W7073539540","doi":"","title":"Pneumonia care and the nursing home:a qualitative descriptive study of resident and family member perspectives","year":2006,"lang":"en","type":"article","venue":"Research Portal (Queen's University Belfast)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Descriptive research; Qualitative research; Pneumonia; Family member; Pandemic; Government (linguistics); MEDLINE; Coronavirus disease 2019 (COVID-19)","score_opus":0.02339484757437713,"score_gpt":0.28637653703636673,"score_spread":0.2629816894619896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073539540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886963,0.00039045245,0.000004468079,0.00025339256,0.000045776047,0.0005468658,0.00015101235,0.000014491843,0.009897247],"genre_scores_gemma":[0.99885005,0.00017741017,0.00005480623,0.0000017411028,0.000047290632,5.2485365e-7,0.000020115076,0.0000042881966,0.0008437475],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.99746585,0.00109565,0.00015534552,0.00035722638,0.0005923015,0.00033361133],"domain_scores_gemma":[0.9988668,0.00040901566,0.00008774397,0.00018570482,0.00034611157,0.00010465687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008007865,0.0001370581,0.000284378,0.00018042799,0.00058138685,0.00008506194,0.00020043222,0.00005180377,0.00009378023],"category_scores_gemma":[0.000034596524,0.00010350438,0.000040475665,0.00030319908,0.0010334443,0.0002856871,0.00007658487,0.00021087113,0.0000054065217],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022777943,0.00040973743,0.06571205,0.00015650425,0.00036683222,0.00050570414,0.8820852,0.00030438538,0.00094672904,0.043941163,0.0018866952,0.0014071772],"study_design_scores_gemma":[0.0010132337,0.00040738576,0.34453914,0.000035100988,0.00003704908,0.0000013517575,0.6523153,0.00001396036,0.0000512079,0.0013199578,0.00016313053,0.0001031665],"about_ca_topic_score_codex":0.116718546,"about_ca_topic_score_gemma":0.0026857422,"teacher_disagreement_score":0.27882707,"about_ca_system_score_codex":0.000019150259,"about_ca_system_score_gemma":0.00009635439,"threshold_uncertainty_score":0.8891633},"labels":[],"label_agreement":null},{"id":"W7073550071","doi":"","title":"Use of transcranial magnetic stimulation in the treatment of selected movement disorders","year":2014,"lang":"en","type":"review","venue":"Dove Medical Press (Taylor and Francis Group)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transcranial magnetic stimulation; Movement disorders; Neurophysiology; Rehabilitation; Deep transcranial magnetic stimulation; Neurorehabilitation; Disease; Neurological disorder","score_opus":0.026580734095990283,"score_gpt":0.25497119186172146,"score_spread":0.22839045776573116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073550071","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0015191953,0.99254984,0.003612701,0.000021927362,0.0003860199,0.0012164966,0.000560312,0.000009834264,0.0001236831],"genre_scores_gemma":[0.31663197,0.68227535,0.00006348511,0.0000496905,0.00023181441,0.000034869725,0.0006988022,0.000011445411,0.000002545336],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978985,0.00038483643,0.0006897306,0.00028585258,0.00051108876,0.00022996432],"domain_scores_gemma":[0.99871594,0.0007146966,0.00021170916,0.00023690758,0.000024313516,0.000096433025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033231685,0.00027412942,0.0011562305,0.00006780072,0.00003680794,0.000030664523,0.00023615899,0.00021907582,0.00063597254],"category_scores_gemma":[0.000053285275,0.00015015279,0.00016853765,0.00018460966,0.00015475957,0.000061015126,0.00000671298,0.000115920535,0.000003465032],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038169757,0.00016535874,0.00033108052,0.0021765586,0.00004817873,0.0000028227048,0.00033137872,0.000044020195,0.0000017394749,0.00007285822,0.0000032477296,0.99678457],"study_design_scores_gemma":[0.0043994994,0.0060218987,0.02740365,0.000578871,0.0027342096,0.0000052965643,0.000036144305,0.12367431,0.000008873828,0.0017451451,0.83221954,0.0011725425],"about_ca_topic_score_codex":0.0057713385,"about_ca_topic_score_gemma":0.0019519166,"teacher_disagreement_score":0.995612,"about_ca_system_score_codex":0.0000026895818,"about_ca_system_score_gemma":0.0000040168484,"threshold_uncertainty_score":0.87245756},"labels":[],"label_agreement":null},{"id":"W7073553619","doi":"","title":"Source attribution of Arctic black carbon constrained by aircraft and surface measurements","year":2017,"lang":"en","type":"article","venue":"CU Scholar (University of Colorado Boulder)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Arctic; The arctic; Carbon fibers; Carbon black; Surface (topology)","score_opus":0.02053207685011504,"score_gpt":0.20581589801646372,"score_spread":0.18528382116634867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073553619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981346,0.00015698072,0.00017481047,0.0002619218,0.00011311612,0.00015568484,0.00019480425,0.000013108026,0.0007949776],"genre_scores_gemma":[0.99927616,0.000057045254,0.00032016294,0.000009704294,0.000012595452,1.4932809e-8,0.00004504119,0.0000024157378,0.00027686724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991803,0.00009713571,0.000107632,0.00019479298,0.00024630246,0.00017384755],"domain_scores_gemma":[0.9992028,0.000028224824,0.00026725378,0.00025971275,0.0001363133,0.00010571045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045979273,0.000102303195,0.00025698758,0.000031158772,0.0004402049,0.000062366875,0.0003033017,0.00009649556,0.00019797898],"category_scores_gemma":[0.00004764191,0.000116805815,0.00004291623,0.00005001439,0.0004861771,0.0003845425,0.000045952886,0.00011544834,0.000012995817],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002846845,0.0000844558,0.891566,0.00026457533,0.00018938293,0.000009196863,0.0010368522,0.0005658364,0.10232409,0.00011059071,0.0006936873,0.0028706503],"study_design_scores_gemma":[0.0016941561,0.00026947446,0.9828361,0.00009304011,0.00016090267,0.0000031711431,0.00072553643,0.0015520673,0.0056316257,0.00032114462,0.0064380975,0.00027466763],"about_ca_topic_score_codex":0.0069168974,"about_ca_topic_score_gemma":0.0005752412,"teacher_disagreement_score":0.096692465,"about_ca_system_score_codex":0.000005015396,"about_ca_system_score_gemma":0.000050315663,"threshold_uncertainty_score":0.99969614},"labels":[],"label_agreement":null},{"id":"W7073554429","doi":"","title":"The consequences of the new European reclassification of non-invasive brain stimulation devices and the medical device regulations pose an existential threat to research and treatment:An invited opinion paper","year":2024,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Transcranial direct-current stimulation; Medical device; Constructive; Brain stimulation; Bureaucracy; Electrical brain stimulation; Transcranial magnetic stimulation; Neuroethics","score_opus":0.05334544843860975,"score_gpt":0.2945301060176578,"score_spread":0.24118465757904803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073554429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9836618,0.0001151281,0.0003424493,0.011137271,0.00008287044,0.00070305046,0.00030047278,0.0000126059595,0.003644381],"genre_scores_gemma":[0.99744517,0.0012187276,0.00046478503,0.000018529292,0.00006000713,1.2388344e-7,0.0001366727,0.0000045145102,0.000651461],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9967343,0.0017987674,0.00015300828,0.00033226234,0.000711911,0.00026972452],"domain_scores_gemma":[0.99693274,0.0020731052,0.00009673102,0.000379612,0.0002768965,0.00024089662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021106768,0.000109393324,0.00019377182,0.00025258336,0.001271911,0.00009233593,0.00075237954,0.000058065267,0.00009734105],"category_scores_gemma":[0.0001602301,0.000071075396,0.000059401595,0.00069443294,0.0025098273,0.000544817,0.0002464979,0.00020834866,0.000001929823],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.021065217,0.0007030341,0.12626071,0.001092771,0.0016748607,0.00020297142,0.12185045,0.002772205,0.07226375,0.20957392,0.010069224,0.4324709],"study_design_scores_gemma":[0.0025182315,0.0025706575,0.8335675,0.00049359055,0.00011461311,0.000014795535,0.027778905,0.018355073,0.00053811306,0.015852204,0.097929,0.0002673476],"about_ca_topic_score_codex":0.016520275,"about_ca_topic_score_gemma":0.049208134,"teacher_disagreement_score":0.70730674,"about_ca_system_score_codex":0.000017906415,"about_ca_system_score_gemma":0.00038549874,"threshold_uncertainty_score":0.9900288},"labels":[],"label_agreement":null},{"id":"W7073555992","doi":"","title":"The incidence of negative intraoperative findings after unsuccessful hydrostatic reduction of ileocolic intussusception in children: A retrospective analysis","year":2019,"lang":"en","type":"article","venue":"EUR Research Repository (Erasmus University Rotterdam)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pediatric Oncology Group","funders":"","keywords":"Incidence (geometry); Reduction (mathematics); Intussusception (medical disorder); Retrospective cohort study; Endoscopy","score_opus":0.005732240996989612,"score_gpt":0.2234969133566201,"score_spread":0.2177646723596305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073555992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99749047,0.000028002496,0.0000092904675,0.00009062659,0.00013116856,0.0007977994,0.00007898028,0.000009264651,0.0013644135],"genre_scores_gemma":[0.99917525,0.000052391413,0.00004077139,0.0000046669684,0.000045417157,0.0000022578467,0.000023836708,0.0000036678346,0.0006517642],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973603,0.0009582305,0.0003031646,0.0003899794,0.00065666344,0.00033169385],"domain_scores_gemma":[0.99877995,0.00025927776,0.00018328762,0.00035199488,0.00034922655,0.00007624352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009349238,0.00013574994,0.00034039686,0.0005278374,0.0002850056,0.00007555385,0.00040908103,0.00007621708,0.00023618604],"category_scores_gemma":[0.000059817186,0.000111254165,0.0001037548,0.0016615528,0.0004492154,0.00049707916,0.000081462786,0.00032421004,0.000022200818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007320895,0.0000468106,0.9757037,0.000029943261,0.00025344844,0.000018687466,0.0039934735,0.0017968684,0.017104164,0.00015015477,0.00004855163,0.00012208176],"study_design_scores_gemma":[0.0005181475,0.00035870864,0.980345,0.000049210692,0.000056104054,0.000004054708,0.0012808535,0.0008956501,0.016159903,0.00016762075,0.000046251622,0.00011847046],"about_ca_topic_score_codex":0.014585249,"about_ca_topic_score_gemma":0.0017210715,"teacher_disagreement_score":0.012864178,"about_ca_system_score_codex":0.000064063555,"about_ca_system_score_gemma":0.00012414377,"threshold_uncertainty_score":0.99197674},"labels":[],"label_agreement":null},{"id":"W7073556180","doi":"","title":"Seroprevalence of Lawsonia intracellularis in different swine populations in 3 provinces in Canada","year":2007,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seroprevalence; Lawsonia intracellularis; Herd; Pig farming; Serology; Indirect immunofluorescence","score_opus":0.01482681561458943,"score_gpt":0.19511165033327807,"score_spread":0.18028483471868864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073556180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980613,0.0003031997,0.000008147492,0.00014357708,0.0005629581,0.00035577826,0.00008188506,0.0000072950716,0.00047584303],"genre_scores_gemma":[0.9995854,0.000082825354,0.00010215021,0.000026515152,0.00007321976,0.0000024850212,0.000041743206,0.0000047820263,0.00008089318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99820143,0.00011904667,0.0004943018,0.0002409885,0.00025254115,0.0006916957],"domain_scores_gemma":[0.9995019,0.000064979045,0.00011102075,0.00016517419,0.000019082574,0.00013785603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004032565,0.00013941103,0.00025864836,0.00010369117,0.000020564923,0.000020155554,0.00023129121,0.000033233122,0.00020741252],"category_scores_gemma":[0.00006572043,0.00011413276,0.000017437293,0.00040501126,0.000028976594,0.00012381696,0.00001930498,0.00013721269,0.0000055140604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038938648,0.000037772556,0.9912557,0.000043250377,0.0000025832694,0.000087885994,0.00062396604,0.0031220024,0.0005101796,0.000080696234,0.000026146668,0.0041708658],"study_design_scores_gemma":[0.0002815827,0.00001589042,0.99633867,0.000045612273,0.0000037178772,9.70131e-7,0.00006289645,0.00044013694,0.0018451177,0.000074680924,0.00076565996,0.00012506802],"about_ca_topic_score_codex":0.85471725,"about_ca_topic_score_gemma":0.9907415,"teacher_disagreement_score":0.13602424,"about_ca_system_score_codex":0.000049445975,"about_ca_system_score_gemma":0.00022398254,"threshold_uncertainty_score":0.4654199},"labels":[],"label_agreement":null},{"id":"W7073563564","doi":"","title":"Masculinities Ageing between Cultures : Relationality, Kinship and Care in Dialogue","year":2024,"lang":"en","type":"book","venue":"BiblioBoard Library Catalog (Open Research Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Trường Đại học Kinh tế - Luật, Đại học Quốc gia Thành phố Hồ Chí Minh; Universität Rostock; Fundamental Research Funds for the Central Universities; Zhongnan University of Economics and Law; Austrian Science Fund; Social Sciences and Humanities Research Council of Canada","keywords":"Kinship; Diaspora; Context (archaeology); Masculinity; Queer; Intersectionality; Intersection (aeronautics)","score_opus":0.07613439044431111,"score_gpt":0.31416595515801576,"score_spread":0.23803156471370465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073563564","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015284374,0.026233325,4.565997e-7,0.0029294752,0.0006812608,0.001998267,0.013891319,0.00028838732,0.9386931],"genre_scores_gemma":[0.114075564,0.010885914,0.0008083987,0.00037144677,0.0040092217,0.00008532181,0.10720757,0.0001992526,0.7623573],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99450403,0.0009866467,0.0008572648,0.0013805322,0.0012277043,0.0010438235],"domain_scores_gemma":[0.99707466,0.0013755711,0.00017595472,0.00079030514,0.000057756064,0.0005257547],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009454985,0.00063943473,0.001041648,0.004620976,0.0004449991,0.006473112,0.0025318214,0.00076838746,0.0051358533],"category_scores_gemma":[0.00007494519,0.0005345853,0.0001810828,0.0030791548,0.0006842855,0.008346162,0.0021959317,0.0018298855,0.0015277661],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001870387,0.000019503108,0.042301886,0.001999474,0.00020066192,0.0015472953,0.001458169,0.000025124355,0.0000031533539,0.037175488,0.9095701,0.0055120913],"study_design_scores_gemma":[0.00035588726,0.00024315578,0.08085785,0.0008657839,0.000042806656,0.0000060965936,0.00016698817,0.000006298184,0.00006568358,0.17594314,0.7407987,0.0006476006],"about_ca_topic_score_codex":0.0027212936,"about_ca_topic_score_gemma":0.0007618621,"teacher_disagreement_score":0.17633583,"about_ca_system_score_codex":0.000013693508,"about_ca_system_score_gemma":0.0018404188,"threshold_uncertainty_score":0.99971056},"labels":[],"label_agreement":null},{"id":"W7073564814","doi":"","title":"Project History as a Group Memory: Learning From the Past","year":2004,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Team software process; Software development; Project team; Software; Software development process; Software project management; Work (physics)","score_opus":0.009875247911133823,"score_gpt":0.15048822602546572,"score_spread":0.1406129781143319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073564814","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99380475,0.0003796104,0.00004154995,0.00009248855,0.0003465614,0.00016570698,0.00014429573,0.00004951633,0.0049754903],"genre_scores_gemma":[0.998602,0.00008235715,0.00016752986,0.00007496578,0.00012148513,1.08008074e-7,0.00011460661,0.000003643123,0.0008333493],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99920475,0.00008129305,0.0000732195,0.0002493157,0.00020477826,0.0001866304],"domain_scores_gemma":[0.99958503,0.00005386982,0.00009762759,0.00016482563,0.000040273393,0.00005834508],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001549861,0.000038241575,0.00016837582,0.000013947796,0.00026847975,0.00007542782,0.0003249167,0.000058412614,0.0012312686],"category_scores_gemma":[0.000015197296,0.00009425419,0.00007309435,0.00009629856,0.00019130598,0.00023154724,0.00003517764,0.00011493426,0.00018200325],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011264734,0.00020609245,0.17461473,0.00012134181,0.00027781512,0.0009356779,0.006539211,0.0018743454,0.0018723301,0.000021831851,0.042475425,0.7709486],"study_design_scores_gemma":[0.00050742377,0.00009315167,0.98050046,0.000048622762,0.00003352587,0.000011332257,0.0011382531,0.000032008636,4.8910414e-7,0.00050727336,0.017001979,0.00012547192],"about_ca_topic_score_codex":0.88124317,"about_ca_topic_score_gemma":0.64468724,"teacher_disagreement_score":0.80588573,"about_ca_system_score_codex":0.000016912465,"about_ca_system_score_gemma":0.0001033564,"threshold_uncertainty_score":0.9996818},"labels":[],"label_agreement":null},{"id":"W7073564975","doi":"","title":"The Adherence Gap: A Longitudinal Examination of Men's and Women's Antiretroviral Therapy Adherence in British Columbia, 2000-2014","year":2017,"lang":"en","type":"article","venue":"Summit (Simon Fraser University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cart; Antiretroviral therapy; Observational study; Confounding; Human immunodeficiency virus (HIV); Odds ratio; Confidence interval; Odds; Pharmacy; Generalized estimating equation; Men who have sex with men","score_opus":0.014124472689225256,"score_gpt":0.19865930953585345,"score_spread":0.1845348368466282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073564975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947749,0.00016426193,0.0000038693474,0.0000133495905,0.00016800028,0.00017089593,0.000099728226,0.000011171732,0.004593856],"genre_scores_gemma":[0.9964592,0.0008933405,0.00001932896,0.0000075026906,0.000031534062,4.923635e-7,0.000013559742,0.0000027653284,0.0025722734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990481,0.00011521843,0.00013188645,0.0002571665,0.0001805773,0.00026702005],"domain_scores_gemma":[0.9993069,0.000091024485,0.00018982383,0.00027730022,0.000058899608,0.00007601694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033021922,0.00008793079,0.00018977559,0.000044126304,0.0005033285,0.00042433263,0.00048007065,0.00006579928,0.0005425685],"category_scores_gemma":[0.000029219118,0.00010410232,0.000028686016,0.000113612376,0.00029829564,0.00049893634,0.00004644318,0.000087361186,0.000016177619],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004049499,0.000017655131,0.94567066,0.000012135898,0.000013966284,0.00005019791,0.00004693241,0.000006808836,0.000021649501,0.000023961264,0.00049781945,0.05359771],"study_design_scores_gemma":[0.0007175238,0.00036224202,0.990835,0.000033629753,0.000006944919,2.2018527e-8,0.002370903,0.00012260467,0.000081672246,0.00026798446,0.0050635086,0.00013797761],"about_ca_topic_score_codex":0.095165566,"about_ca_topic_score_gemma":0.69458735,"teacher_disagreement_score":0.5994218,"about_ca_system_score_codex":0.000010149197,"about_ca_system_score_gemma":0.00005927547,"threshold_uncertainty_score":0.9108598},"labels":[],"label_agreement":null},{"id":"W7073574300","doi":"","title":"Civic tradition &amp; planning processes : a comparative study of two resource communities in Northern Ontario","year":2009,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Resource (disambiguation); Population; Capital (architecture); Context (archaeology); Plan (archaeology)","score_opus":0.028241266336264278,"score_gpt":0.20357540998184595,"score_spread":0.17533414364558167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073574300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971572,0.00006718323,0.0000112945545,0.000008417462,0.000029250486,0.00022431888,0.000119415134,0.000016775904,0.0023661484],"genre_scores_gemma":[0.9996883,0.000003556188,0.0000665595,0.000009544798,0.000011321866,1.0709917e-7,0.00013693057,0.0000014654076,0.00008218045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992858,0.00011490458,0.00013507948,0.00014417982,0.00017877227,0.0001412674],"domain_scores_gemma":[0.99952465,0.0000671629,0.00013712712,0.00014675876,0.00008009896,0.000044178218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015248706,0.00004150177,0.00029163403,0.000046651912,0.00015833945,0.000053944783,0.00023966254,0.000031482577,0.0001820279],"category_scores_gemma":[0.0000034959667,0.00011467189,0.000027145703,0.00020262171,0.000094127456,0.00024572425,0.000013327814,0.000097733355,0.0000062019103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052505926,0.00037174547,0.93601274,0.000054281947,0.000029847228,0.00004365212,0.045506127,0.004846553,0.000031761865,3.351926e-7,0.00018338347,0.012867087],"study_design_scores_gemma":[0.00087942794,0.00030562756,0.9745231,0.00015346005,0.000021513424,0.0000053171643,0.023543537,0.000038043996,4.8834323e-7,0.00026694324,0.00015091636,0.00011160782],"about_ca_topic_score_codex":0.91266364,"about_ca_topic_score_gemma":0.99943316,"teacher_disagreement_score":0.086769484,"about_ca_system_score_codex":0.000009725616,"about_ca_system_score_gemma":0.00008509563,"threshold_uncertainty_score":0.4676184},"labels":[],"label_agreement":null},{"id":"W7073575177","doi":"","title":"4-Dimensional Electrical Resistivity Tomography for continuous, near-real time monitoring of a landslide affecting transport infrastructure in British Columbia, Canada","year":2021,"lang":"en","type":"article","venue":"Arrow@dit (Dublin Institute of Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Electrical resistivity tomography; Landslide; Serviceability (structure); Hydrogeology; Continuous monitoring; GNSS applications; Global Positioning System; Environmental geology","score_opus":0.003879504987655797,"score_gpt":0.18371138190057387,"score_spread":0.17983187691291808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073575177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979347,0.00022838532,0.000017107404,0.00008489649,0.0006862057,0.00024578816,0.0006202945,0.00004741095,0.00013523498],"genre_scores_gemma":[0.9918999,0.000025283181,0.0077214963,0.000009943947,0.00008084356,0.000006052297,0.00018614299,0.000006143852,0.0000641852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860543,0.000026634885,0.0004279809,0.00034000262,0.00024750832,0.00035243016],"domain_scores_gemma":[0.9992663,0.00009567263,0.00019008832,0.00021092374,0.00017279018,0.00006421544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023804001,0.00012323937,0.0005212476,0.00010385232,0.00013712588,0.000044512628,0.00024179144,0.00022549511,0.00010522574],"category_scores_gemma":[0.00017080983,0.00016870593,0.000085627944,0.0007567911,0.00017433643,0.00015606913,0.000021376207,0.00019260136,7.21571e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042607782,0.00004488682,0.973407,0.00010109333,0.000067367786,0.00017265965,0.000016303886,0.0009597693,0.013320496,0.000051460996,0.0007738356,0.011042531],"study_design_scores_gemma":[0.00083302736,0.00012292672,0.97941166,0.0001852687,0.0000429583,0.00003449854,0.000032319218,0.00020240044,0.01197544,0.0008453726,0.006083675,0.00023047584],"about_ca_topic_score_codex":0.6677835,"about_ca_topic_score_gemma":0.9182348,"teacher_disagreement_score":0.2504513,"about_ca_system_score_codex":0.000013224051,"about_ca_system_score_gemma":0.0007146406,"threshold_uncertainty_score":0.6879628},"labels":[],"label_agreement":null},{"id":"W7073585229","doi":"","title":"Using a patient-generated mental-health measure 'PSYCHLOPS' to explore problems in patients with coronary heart disease","year":2014,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute of Population and Public Health","funders":"","keywords":"Confounding; Distress; Psychological distress; Psychometrics; Coronary heart disease; Heart disease; Social support; Ethnic group","score_opus":0.05266313784120553,"score_gpt":0.23612717102379538,"score_spread":0.18346403318258986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073585229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89910764,0.00010715842,0.0000015060041,0.0002315021,0.00016942373,0.0010807922,0.09913948,0.00004577995,0.000116706186],"genre_scores_gemma":[0.92111987,3.4930542e-7,0.0001841862,0.0008585324,0.00005317297,0.000021783619,0.07774181,0.00000985249,0.000010457841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986604,0.000117578005,0.00020818113,0.00032122034,0.00033264,0.00036002396],"domain_scores_gemma":[0.9992887,0.00001602042,0.00008617018,0.0002074943,0.00007172178,0.00032988604],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006126277,0.00017110088,0.00020996293,0.00006366906,0.00013880839,0.00006854128,0.00013110401,0.00003377385,0.016563827],"category_scores_gemma":[0.00004181861,0.00013361884,0.00002253694,0.00021728603,0.0000052149885,0.00018184041,0.000022676168,0.000062387844,0.0005655141],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008046901,0.00037946648,0.7551925,0.0005637392,0.000040708048,0.000009494401,0.0029631492,0.042399924,0.00013242483,0.0000030165627,0.18500084,0.012510018],"study_design_scores_gemma":[0.00070835906,0.00054442266,0.97019094,0.001275193,0.0000040766304,5.7030155e-7,0.000026057642,0.0010245076,0.000028170554,0.000032232885,0.025860628,0.00030483794],"about_ca_topic_score_codex":0.00033030426,"about_ca_topic_score_gemma":0.0003261737,"teacher_disagreement_score":0.21499841,"about_ca_system_score_codex":0.000010024695,"about_ca_system_score_gemma":0.00009180155,"threshold_uncertainty_score":0.9843352},"labels":[],"label_agreement":null},{"id":"W7073587463","doi":"","title":"Effect of the COVID-19 Pandemic on Patient Volumes, Acuity, and Outcomes in Pediatric Emergency Departments: A Nationwide Study","year":2021,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Triage; Emergency department; Pandemic; Confidence interval; Observational study; Intensive care unit; Pediatric intensive care unit","score_opus":0.049671497072411065,"score_gpt":0.30439602532249976,"score_spread":0.2547245282500887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073587463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867636,0.000080615806,0.000002449628,0.000065329,0.00046477327,0.00050181826,0.00012904973,0.000024370776,0.00005523117],"genre_scores_gemma":[0.99933136,0.00009654051,0.0000014953223,0.0001114223,0.000025918955,8.882927e-7,0.00002494495,0.0000053889535,0.00040204666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99775684,0.0009775134,0.0002609299,0.0003821085,0.00038259325,0.00024004478],"domain_scores_gemma":[0.9990214,0.00026510024,0.00018447213,0.0003248179,0.000050703282,0.00015352106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049812515,0.00019817703,0.0003219985,0.00017987462,0.00017420076,0.0000655203,0.00034246728,0.00007801079,0.00010609847],"category_scores_gemma":[0.00017177784,0.0001508232,0.00007686404,0.00044596734,0.00003585305,0.00038019544,0.0001566016,0.00018826178,0.000027815831],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007938668,0.000110090696,0.9986849,0.00006699431,0.000036902184,0.00008679017,0.00033196306,0.00015595535,0.000033271892,0.000002586749,6.4637976e-7,0.0004105488],"study_design_scores_gemma":[0.0010431131,0.0004430357,0.9977095,0.000008249898,0.00009901447,0.0000052348823,0.00008062814,3.7898056e-7,0.00021546056,0.000064694024,0.0001796292,0.00015103075],"about_ca_topic_score_codex":0.00012731279,"about_ca_topic_score_gemma":0.030074067,"teacher_disagreement_score":0.029946756,"about_ca_system_score_codex":0.000022305992,"about_ca_system_score_gemma":0.00009182591,"threshold_uncertainty_score":0.9876245},"labels":[],"label_agreement":null},{"id":"W7073590650","doi":"","title":"Profiling Academic Research on Massively Multiplayer On-line Role-Play Gaming (MMORPG) 2000-2009: Horizons for Educational Research","year":2013,"lang":"en","type":"article","venue":"DOAJ (DOAJ: Directory of Open Access Journals)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Profiling (computer programming); Educational research; Architecture; Research methodology; Research data","score_opus":0.47488966548381156,"score_gpt":0.5855772617304632,"score_spread":0.11068759624665164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073590650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98365897,0.003498902,0.00003518423,0.001197051,0.0011066075,0.002099252,0.000702085,0.000020554913,0.007681409],"genre_scores_gemma":[0.9932449,0.0014886338,0.0006600485,0.00015969021,0.0015773025,0.00017564897,0.00019323928,0.00003521017,0.0024653615],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99434626,0.00093640474,0.0008946379,0.0007746475,0.0018870798,0.0011609567],"domain_scores_gemma":[0.99235606,0.004932597,0.00044782963,0.00051666645,0.0012238977,0.00052291824],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0060774526,0.0003395072,0.0006395771,0.0013663119,0.0011321378,0.0016572967,0.0030301923,0.00024814496,0.02591563],"category_scores_gemma":[0.0014544935,0.0002747783,0.00014154518,0.001155756,0.00027017473,0.0018652703,0.000298666,0.0013702812,0.00083911914],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014758445,0.00060974486,0.26654497,0.00028307797,0.00032686323,0.000019337358,0.00058989046,0.012775846,0.43565997,0.0018558722,0.23828162,0.041576978],"study_design_scores_gemma":[0.0010899203,0.00028047187,0.8150865,0.0009298629,0.00004009419,0.000008425485,0.00038923832,0.003152356,0.11330151,0.03518485,0.029731466,0.00080532575],"about_ca_topic_score_codex":0.005498723,"about_ca_topic_score_gemma":0.00014245206,"teacher_disagreement_score":0.54854155,"about_ca_system_score_codex":0.000052375548,"about_ca_system_score_gemma":0.0006938616,"threshold_uncertainty_score":0.99997044},"labels":[],"label_agreement":null},{"id":"W7073605791","doi":"","title":"Can Food Banks Sustain Nutrient Requirements? A Case Study in Southwestern Ontario","year":2007,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Food energy; Food supply; Nutrient; Food group; Food products; Dairy foods; Food guide; Food processing","score_opus":0.07865732746257033,"score_gpt":0.2857376629502475,"score_spread":0.20708033548767718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073605791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99789894,0.000029967405,0.000064848056,0.00004003539,0.0005507707,0.00094389566,0.00011705422,0.0000920829,0.000262417],"genre_scores_gemma":[0.99761415,0.0000032756147,0.000017200868,0.00011317806,0.00011266456,7.270834e-7,0.00006338481,0.000018510602,0.0020568934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9967491,0.00033338412,0.0005291867,0.0008134734,0.0005754456,0.000999394],"domain_scores_gemma":[0.998432,0.000122832,0.00024781746,0.0006282832,0.000120029086,0.00044908456],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.001234321,0.00043885302,0.0004992091,0.0006600257,0.00032825748,0.00037368172,0.00069538306,0.00019923516,0.0002747525],"category_scores_gemma":[0.00001711739,0.00046069105,0.00011446429,0.0006206947,0.00009088761,0.0011475271,0.00017390611,0.0005407697,0.00014381703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023392767,0.0002510183,0.9745613,0.000028620114,0.00007716351,0.01911101,0.00511727,0.00007022403,0.0000441774,0.000020553907,2.413748e-7,0.00048454895],"study_design_scores_gemma":[0.002354722,0.0008336962,0.9895175,0.00005926524,0.00008779037,0.00022699356,0.005391737,2.3315975e-7,0.00026319464,0.00012715835,0.000614163,0.0005235149],"about_ca_topic_score_codex":0.025509426,"about_ca_topic_score_gemma":0.9721936,"teacher_disagreement_score":0.9466841,"about_ca_system_score_codex":0.00017517632,"about_ca_system_score_gemma":0.0002470348,"threshold_uncertainty_score":0.99978447},"labels":[],"label_agreement":null},{"id":"W7073608969","doi":"","title":"The predictive utility of micro indicators of concern about smoking: findings from the International Tobacco Control Four Country study","year":2014,"lang":"en","type":"article","venue":"Deakin Research Online (Deakin University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tobacco control; Logistic regression; Quit smoking; Control (management); Association (psychology); Smoking cessation; Survey data collection; Regression analysis","score_opus":0.031231237923207335,"score_gpt":0.27465873517394807,"score_spread":0.24342749725074073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073608969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941277,0.000033668315,0.00008804688,0.00034918857,0.0003378533,0.00049344817,0.002822772,0.000014452651,0.0017328646],"genre_scores_gemma":[0.9994735,0.00003043696,0.00003338592,0.0000336196,0.00018979919,5.92481e-7,0.0001369514,0.000004664789,0.00009700935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99719465,0.00083679863,0.00029935324,0.00032685083,0.0009916633,0.00035068038],"domain_scores_gemma":[0.9963027,0.0025536574,0.00023209523,0.0004354617,0.0003825285,0.000093538176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021397776,0.00013887942,0.00027955082,0.00018106915,0.00041621967,0.00008119064,0.0016336088,0.00008895352,0.00042599006],"category_scores_gemma":[0.0004646242,0.000091094174,0.000077683384,0.00056695525,0.00066682644,0.00014793914,0.00018468771,0.00036405408,0.000009227397],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006683373,0.00014036347,0.99318254,0.000007181329,0.00030983821,0.000012384186,0.00033310681,0.00011133625,0.00026116567,0.0022679486,0.000708344,0.0019974515],"study_design_scores_gemma":[0.001050744,0.00023332481,0.88930875,0.00002969207,0.000046912017,3.789195e-7,0.0009147002,0.0011079747,0.0002894378,0.00030290382,0.106629424,0.000085757056],"about_ca_topic_score_codex":0.027579907,"about_ca_topic_score_gemma":0.007817021,"teacher_disagreement_score":0.105921075,"about_ca_system_score_codex":0.000015715314,"about_ca_system_score_gemma":0.0002010499,"threshold_uncertainty_score":0.97889555},"labels":[],"label_agreement":null},{"id":"W7073616391","doi":"","title":"Constraints on non-Standard Model Higgs boson interactions in an effective field theory using differential cross sections measured in the $H \\\\rightarrow \\\\gamma\\\\gamma$ decay channel at $\\\\sqrt{s} = 8$ TeV with the ATLAS detector","year":2015,"lang":"en","type":"other","venue":"DESY (CERN, DESY, Fermilab, IHEP, and SLAC)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fundação para a Ciência e a Tecnologia; Institut National de Physique Nucléaire et de Physique des Particules; Agencia Nacional de Promoción Científica y Tecnológica; Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; H. Lundbeck A/S; Centre National pour la Recherche Scientifique et Technique; Georgian National Science Foundation; National Research Center \"Kurchatov Institute\"; Centre National de la Recherche Scientifique; Max-Planck-Gesellschaft; Israel Science Foundation; Israeli Centers for Research Excellence; Joint Institute for Nuclear Research; Japan Society for the Promotion of Science; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Lundbeckfonden; Bundesministerium für Wissenschaft, Forschung und Wirtschaft; Leverhulme Trust; General Secretariat for Research and Technology; Ministry of Education, Culture, Sports, Science and Technology; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Austrian Science Fund; Bundesministerium für Bildung und Forschung; National Science Council; U.S. Department of Energy; National Natural Science Foundation of China; Fundação de Amparo à Pesquisa do Estado de São Paulo; Javna Agencija za Raziskovalno Dejavnost RS; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Ministerstwo Edukacji i Nauki; CERN; Departamento Administrativo de Ciencia, Tecnología e Innovación (COLCIENCIAS); Deutsche Forschungsgemeinschaft; European Commission; Comisión Nacional de Investigación Científica y Tecnológica; Danmarks Grundforskningsfond; TRIUMF; Alexander von Humboldt-Stiftung; Services Fédéraux des Affaires Scientifiques, Techniques et Culturelles; Department of Science and Technology, Ministry of Science and Technology, India; National Science Foundation; Türkiye Atom Enerjisi Kurumu","keywords":"Nucleofection; TSG101; Gestational period; Hyporeflexia; Proteogenomics; Fusible alloy; Dysgeusia","score_opus":0.0221958803237498,"score_gpt":0.25617539533175315,"score_spread":0.23397951500800335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073616391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97782904,0.00030562782,0.00079433876,0.000106559884,0.0010026674,0.0013491046,0.0012624094,0.000078906574,0.017271359],"genre_scores_gemma":[0.99534345,0.00006556424,0.000045571713,0.000100154066,0.00059476745,0.000034590917,0.00023907231,0.00010095305,0.0034758619],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970009,0.0006949573,0.00037665895,0.0007438511,0.0005631057,0.00062054716],"domain_scores_gemma":[0.99848264,0.0003656112,0.00027636834,0.0005708042,0.00010026198,0.00020432207],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007233969,0.0006233665,0.0007045302,0.00029485897,0.00056864,0.00042381792,0.0005117418,0.0003504212,0.0010645958],"category_scores_gemma":[0.00003865015,0.0003644675,0.0001160235,0.00028162153,0.00047996445,0.00022336244,0.000056055826,0.00062749727,0.000040721683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.07480374,0.0045821927,0.19857916,0.003631848,0.007164612,0.0032038426,0.1298432,0.16435914,0.055175204,0.0040153423,0.18992627,0.16471545],"study_design_scores_gemma":[0.0523577,0.017725734,0.2744117,0.0120944735,0.005715404,0.0020811853,0.010270508,0.1986049,0.16514729,0.023965245,0.2156344,0.021991434],"about_ca_topic_score_codex":0.004627628,"about_ca_topic_score_gemma":0.05564848,"teacher_disagreement_score":0.14272402,"about_ca_system_score_codex":0.000061102626,"about_ca_system_score_gemma":0.00013305507,"threshold_uncertainty_score":0.99988073},"labels":[],"label_agreement":null},{"id":"W7073618091","doi":"","title":"Meaningful patient representation informing Canada’s cancer drug funding decisions: views of patient representatives on the Pan-Canadian Oncology Drug Review","year":2023,"lang":"en","type":"other","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cancer drugs; Representation (politics); Drug; Cancer; Alternative medicine; MEDLINE; Patient advocacy","score_opus":0.04497093087258256,"score_gpt":0.29820192038088844,"score_spread":0.25323098950830586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073618091","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009169902,0.020670183,0.0000035253518,0.0049538696,0.0059426525,0.003687997,0.0027340944,0.00014937053,0.9526884],"genre_scores_gemma":[0.20645596,0.23737009,0.0009281342,0.018590653,0.0016734385,0.0005387182,0.0023017814,0.00078776403,0.5313535],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997263,0.0003753031,0.0007639179,0.00045303372,0.0006582213,0.00048649186],"domain_scores_gemma":[0.9972343,0.001043762,0.0008404247,0.00056818454,0.00008326586,0.00023010047],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005241712,0.0003164663,0.00069811783,0.00020315665,0.00019315952,0.000042358544,0.00039698093,0.000091390466,0.013684309],"category_scores_gemma":[0.00044143293,0.00019548004,0.00011426612,0.0003590642,0.00007031032,0.000091305,0.000048530295,0.00019048694,0.00018625495],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010059171,0.0000069059674,0.00069023744,0.00013134435,0.00009907722,0.000021655904,0.0009657989,0.00016327556,0.0000022591162,0.0002242615,0.89466405,0.103021085],"study_design_scores_gemma":[0.00007589793,0.000050756866,0.0010626313,0.0030627775,0.00006707184,0.0000012002002,0.0012257296,0.000030479041,0.00012949624,0.0001120954,0.9939184,0.0002634655],"about_ca_topic_score_codex":0.9961184,"about_ca_topic_score_gemma":0.9993959,"teacher_disagreement_score":0.42133492,"about_ca_system_score_codex":0.00008311923,"about_ca_system_score_gemma":0.0015504281,"threshold_uncertainty_score":0.9872173},"labels":[],"label_agreement":null},{"id":"W7073621507","doi":"","title":"The Canadian Medical Association Journal","year":2006,"lang":"en","type":"other","venue":"DigitalGeorgetown (Georgetown University Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"","score_opus":0.002661555759326553,"score_gpt":0.13983521782484862,"score_spread":0.13717366206552206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073621507","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003156126,0.00044741415,0.0000027394199,0.005913013,0.002447618,0.0002317647,0.001533305,0.0002640419,0.9888445],"genre_scores_gemma":[0.003358515,0.000660599,0.00007362265,0.00037129974,0.0018558601,1.8024816e-7,0.000996403,0.00010332097,0.9925802],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9968007,0.00021394959,0.00032187192,0.00040752417,0.0013076616,0.0009482646],"domain_scores_gemma":[0.9979311,0.00020538665,0.00044994513,0.00038392577,0.000071528826,0.000958081],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00039050134,0.00041283233,0.0004342545,0.00035800447,0.00106927,0.0013128989,0.0013751496,0.00096954906,0.029826615],"category_scores_gemma":[0.00009080858,0.00032106493,0.00023981532,0.00042421583,0.00018772483,0.00075911434,0.000081329825,0.0007234229,0.0019182101],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012033077,0.000011083752,0.0090641985,0.000010731152,0.00014577767,0.00035762845,0.00001093236,0.0000068911077,1.6017324e-7,0.0014918969,0.9847242,0.004164451],"study_design_scores_gemma":[0.00026774715,0.000028939516,0.0064439257,0.000055403758,0.0000439363,0.000016816708,0.0000270637,0.000018582654,0.00000540961,0.00057393505,0.99210125,0.0004170095],"about_ca_topic_score_codex":0.14561161,"about_ca_topic_score_gemma":0.5191702,"teacher_disagreement_score":0.3735586,"about_ca_system_score_codex":0.000053696353,"about_ca_system_score_gemma":0.0020928197,"threshold_uncertainty_score":0.9999241},"labels":[],"label_agreement":null},{"id":"W7073625043","doi":"","title":"Canadian philanthropy and higher education : funding shifts, organizational restructuring and the repositioning of academic culture in university museums","year":2011,"lang":"en","type":"other","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Higher education; Restructuring; Receipt; Element (criminal law); Academic community; Work (physics); Participant observation","score_opus":0.005955758989693207,"score_gpt":0.15633588500561996,"score_spread":0.15038012601592676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073625043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9315127,0.001413557,0.0000038309618,0.00011146904,0.00035892945,0.00026430393,0.0008115622,0.00002049593,0.06550314],"genre_scores_gemma":[0.9795668,0.0010796605,0.00013242303,0.000012835585,0.000055132914,2.0799002e-8,0.00012319972,0.0000100329235,0.01901988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99945414,0.00007301482,0.00007051871,0.00019962933,0.000086703185,0.00011598172],"domain_scores_gemma":[0.9996255,0.000019677376,0.00015529236,0.00008865869,0.00003219643,0.00007869909],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010216913,0.00004258093,0.00019027184,0.00007956593,0.00017623203,0.000031685147,0.00015298813,0.00016589698,0.0013949001],"category_scores_gemma":[0.000006328488,0.00009444029,0.000017779594,0.00014497581,0.0002585632,0.00011405226,0.000028025122,0.00013194965,0.0000024013991],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012872793,0.000060620154,0.8097601,0.0013263054,0.0003829954,0.0002463393,0.0062047825,0.000028399125,0.00021388955,0.0015386919,0.07749,0.10261918],"study_design_scores_gemma":[0.00034337788,0.000010376943,0.99217105,0.00031664892,0.00003977737,0.000011831955,0.00053197675,0.000005178746,2.2357632e-7,0.00065656507,0.005808114,0.000104865794],"about_ca_topic_score_codex":0.9552683,"about_ca_topic_score_gemma":0.953142,"teacher_disagreement_score":0.182411,"about_ca_system_score_codex":0.000012223828,"about_ca_system_score_gemma":0.00015897596,"threshold_uncertainty_score":0.999518},"labels":[],"label_agreement":null},{"id":"W7073625750","doi":"","title":"Physiologically regulated transgenic ABCA1 does not reduce amyloid burden or amyloid‐beta peptide levels in vivo","year":2007,"lang":"en","type":"article","venue":"Portuguese National Funding Agency for Science, Research and Technology (RCAAP Project by FCT)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"ABCA1; Genetically modified mouse; Transgene; In vivo; Amyloid (mycology); Amyloid precursor protein; Messenger RNA","score_opus":0.06437794182273959,"score_gpt":0.34562775184514344,"score_spread":0.28124981002240385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073625750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99137,0.00036754675,0.00008765843,0.001063866,0.00032273354,0.0013576674,0.000833266,0.00015757134,0.004439689],"genre_scores_gemma":[0.99278075,0.00038407315,0.0013936036,0.000038468446,0.00019525642,0.00005935896,0.0001007633,0.000011721401,0.005036009],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9949628,0.000096634154,0.00067514624,0.0011428939,0.0015145977,0.0016079245],"domain_scores_gemma":[0.99776393,0.00068809907,0.00017484235,0.00032287333,0.00080718263,0.00024307887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0083176335,0.000299011,0.00042867305,0.0020895058,0.0009957405,0.00018422729,0.001184842,0.00033487033,0.00043905823],"category_scores_gemma":[0.0011796185,0.00019968055,0.00006951215,0.0040429467,0.0019456974,0.00063343736,0.00012357021,0.0004889266,0.000024649758],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006245035,0.00015664351,0.004186165,0.00010953169,0.000053590764,0.000047637703,0.00035286008,0.00003430165,0.9471363,0.00855123,0.0015280601,0.037219208],"study_design_scores_gemma":[0.0033582924,0.0040681534,0.19115195,0.0002949595,0.00003853718,0.00010445819,0.0013581488,0.0030804148,0.6477455,0.12110412,0.025885647,0.0018097933],"about_ca_topic_score_codex":0.00095438573,"about_ca_topic_score_gemma":0.0007227581,"teacher_disagreement_score":0.29939076,"about_ca_system_score_codex":0.00006461509,"about_ca_system_score_gemma":0.0009879547,"threshold_uncertainty_score":0.81427366},"labels":[],"label_agreement":null},{"id":"W7073628174","doi":"","title":"Comparison of deferral rates using a computerized versus written blood donor questionnaire:a randomized, cross-over study [ISRCTN84429599]","year":2002,"lang":"en","type":"article","venue":"Research Portal (Queen's University Belfast)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Blood donor; Donation; Deferral; Randomized controlled trial; Blood donations; Crossover study","score_opus":0.05581836716760888,"score_gpt":0.32956157134716757,"score_spread":0.27374320417955866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073628174","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962134,0.000058752466,0.000071658455,0.000099966666,0.00038980396,0.0009136142,0.00016415272,0.000058545553,0.0020301498],"genre_scores_gemma":[0.99858356,0.000058028058,0.00041032207,0.0000060953093,0.00015001938,8.07244e-7,0.00006584016,0.000009779023,0.00071553345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99614,0.0011888173,0.0004832061,0.00051956443,0.0009902972,0.00067810353],"domain_scores_gemma":[0.99809605,0.00049684756,0.0002482932,0.00039904844,0.00046456917,0.00029518895],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001190506,0.000263096,0.00088987424,0.00034143013,0.0006293162,0.00019707062,0.0005934223,0.00013613803,0.0027137254],"category_scores_gemma":[0.00015479005,0.00024518138,0.00020766657,0.0006028491,0.00075718143,0.00055097736,0.00017087894,0.00036099055,0.000094302064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.046280246,0.0021633795,0.9345853,0.00023182016,0.0015033295,0.00095044484,0.003190693,0.004816093,0.0007784816,0.0030552205,0.0017596487,0.0006853748],"study_design_scores_gemma":[0.33542612,0.004360803,0.5969864,0.00035883856,0.001148488,0.000017755274,0.005848083,0.0497654,0.0017969203,0.00055861817,0.0018703144,0.0018622078],"about_ca_topic_score_codex":0.032496344,"about_ca_topic_score_gemma":0.00070839626,"teacher_disagreement_score":0.33759883,"about_ca_system_score_codex":0.000016191416,"about_ca_system_score_gemma":0.00010008025,"threshold_uncertainty_score":0.99982065},"labels":[],"label_agreement":null},{"id":"W7073632137","doi":"","title":"High fracture probability with FRAX® usually indicates densitometric osteoporosis: Implications for clinical practice","year":2012,"lang":"en","type":"article","venue":"Research Bank (Australian Catholic University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Femoral neck; Fracture (geology); Osteoporosis; Bone mineral; Population; Risk factor","score_opus":0.114970218176408,"score_gpt":0.36886506286016363,"score_spread":0.2538948446837556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073632137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922202,0.00010568373,0.00012937217,0.0042559,0.00018983649,0.0010419805,0.00052824675,0.0000656394,0.0014631317],"genre_scores_gemma":[0.98894083,0.00014810023,0.008434923,0.000107483844,0.00050836196,0.0000042318757,0.00025122566,0.00000965035,0.0015951885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971662,0.0006347244,0.0002763848,0.00049355446,0.0004937733,0.00093533803],"domain_scores_gemma":[0.9965482,0.0015553138,0.00018487373,0.0005107634,0.00062844536,0.00057245675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026820847,0.00019327867,0.00032231098,0.0004094268,0.00059572957,0.00015587828,0.0005885511,0.00024076023,0.00034722773],"category_scores_gemma":[0.0006737181,0.00016085233,0.000097571465,0.0017192239,0.00040596182,0.0009997927,0.000058017526,0.00048408835,0.00016662534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014292006,0.0013514333,0.94315016,0.0003558476,0.0005276031,0.000080705264,0.0039282,0.00045764548,0.0005043316,0.007922006,0.02219089,0.018101973],"study_design_scores_gemma":[0.00040130905,0.00033123823,0.60264134,0.000012665551,0.00008274979,0.000013930926,0.0002787813,0.0000022822758,0.000219995,0.00023326019,0.3956037,0.0001787449],"about_ca_topic_score_codex":0.00273268,"about_ca_topic_score_gemma":0.00024653494,"teacher_disagreement_score":0.3734128,"about_ca_system_score_codex":0.0000328273,"about_ca_system_score_gemma":0.00031289307,"threshold_uncertainty_score":0.6559368},"labels":[],"label_agreement":null},{"id":"W7073640580","doi":"","title":"Isolated Frontopolar Cortex Lesion: A Case Study","year":2012,"lang":"en","type":"article","venue":"Journal of International Crisis and Risk Communication Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ideology; Variance (accounting); Enforcement; Proxy (statistics); Economic Justice; Variation (astronomy); Procedural justice","score_opus":0.06706529547926555,"score_gpt":0.3784353293235698,"score_spread":0.3113700338443043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073640580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99457467,0.0038243853,0.0000726723,0.00042111924,0.00033124597,0.000117058065,0.00003307466,0.000004168967,0.00062163104],"genre_scores_gemma":[0.99362695,0.0054677892,0.0005411142,0.000021217444,0.0002466516,8.8212414e-7,0.000009658833,0.000003023829,0.00008268606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997931,0.00085233327,0.00039021973,0.000079458914,0.0005709023,0.00017610425],"domain_scores_gemma":[0.99830645,0.0003668479,0.0002638806,0.00024468102,0.0006611515,0.0001569623],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0039755544,0.000071682865,0.00015824397,0.00019670457,0.00038495735,0.00016685204,0.00042870216,0.000043732507,0.0009783641],"category_scores_gemma":[0.00012871197,0.00004994292,0.00004576722,0.00012410525,0.00006255882,0.0004905866,0.00008134109,0.00040075966,0.000034934434],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020186228,0.00040987207,0.97395104,0.000006363634,0.00027090704,0.00014091648,0.0045337975,0.000044379718,0.00011834314,0.00019331758,0.0057327556,0.014396414],"study_design_scores_gemma":[0.0009576976,0.0006495987,0.9374107,0.000033507786,0.00007021298,0.0014760889,0.025316413,0.0017094385,0.000054637494,0.0008963999,0.03127309,0.00015222101],"about_ca_topic_score_codex":0.013092264,"about_ca_topic_score_gemma":0.0010976801,"teacher_disagreement_score":0.036540378,"about_ca_system_score_codex":0.000008694994,"about_ca_system_score_gemma":0.000034703644,"threshold_uncertainty_score":0.99993485},"labels":[],"label_agreement":null},{"id":"W7073640601","doi":"","title":"Acetylcholinesterase-positive afferent axons in mucosa of urinary bladder of adult cats: retrograde tracing and degeneration studies","year":2011,"lang":"en","type":"article","venue":"Digitum: Institutional Repository of the University of Murcia (University of Murcia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of British Columbia","keywords":"Axon; Retrograde tracing; Dorsal root ganglion; Urinary bladder; Wheat germ agglutinin; Ganglion; Synaptic vesicle; Free nerve ending; Population; Horseradish peroxidase","score_opus":0.0240928867758268,"score_gpt":0.18317697938903416,"score_spread":0.15908409261320736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073640601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99717814,0.00023189762,0.00009576671,0.00004963186,0.00017737814,0.0001698295,0.00024949556,0.0000062329013,0.0018416495],"genre_scores_gemma":[0.99883693,0.00015166496,0.0008687255,0.0000041666053,0.000015877582,2.019542e-8,0.000025697773,0.0000017730681,0.00009511558],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904925,0.00011278232,0.00022329575,0.00019904587,0.00029445023,0.00012120437],"domain_scores_gemma":[0.998934,0.00007711425,0.00045848705,0.00019328849,0.00028564845,0.000051488016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013032855,0.00012125582,0.0003960736,0.00015583493,0.00025850983,0.0000033252409,0.0003189183,0.000084515894,0.000024504827],"category_scores_gemma":[0.000026814265,0.00012418217,0.00013044149,0.00018138273,0.0011317779,0.00038418963,0.00010095092,0.00008030879,6.3767186e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033402615,0.0016776028,0.833575,0.0016749714,0.0014762635,0.00019994138,0.060089763,0.0103521105,0.07339616,0.01032175,0.00037091857,0.0035252685],"study_design_scores_gemma":[0.0009813913,0.00024037779,0.9605371,0.00055435335,0.00020701913,0.00001525015,0.006209685,0.00030471527,0.030485887,0.00021521866,0.00008505241,0.00016396571],"about_ca_topic_score_codex":0.005401475,"about_ca_topic_score_gemma":0.0015331649,"teacher_disagreement_score":0.1269621,"about_ca_system_score_codex":0.000019152732,"about_ca_system_score_gemma":0.0001384556,"threshold_uncertainty_score":0.81654507},"labels":[],"label_agreement":null},{"id":"W7073644244","doi":"","title":"Expansion of the Parkinson disease-associated SNCA-Rep1 allele upregulates human alpha-synuclein in transgenic mouse brain.","year":2009,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Human Genome Research Institute; National Institutes of Health; University of Ottawa","keywords":"Allele; Gene; Disease; Frameshift mutation; Mutation","score_opus":0.009897968024190854,"score_gpt":0.19219683843832422,"score_spread":0.18229887041413337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073644244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99326175,0.00020119258,0.0000017758772,0.0009253491,0.00008418966,0.00034099925,0.0034898457,0.00011412267,0.0015807708],"genre_scores_gemma":[0.99748135,0.000014134651,0.00003450175,0.00046165363,0.000062619234,0.0000023201806,0.0013309461,0.000018246254,0.0005942111],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99794483,0.00019697576,0.0005414824,0.0004099438,0.00043183347,0.00047492096],"domain_scores_gemma":[0.99900395,0.0001064007,0.0001944035,0.0004315725,0.00002149533,0.0002422025],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023341693,0.0002835173,0.00036378743,0.00009268644,0.00017214687,0.00045554034,0.00065461727,0.00013141287,0.0010613445],"category_scores_gemma":[0.00010101802,0.0002073536,0.00022113645,0.00039552271,0.00009659929,0.0017567099,0.00004128952,0.00022346094,0.00019060752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046281563,0.0005117294,0.96089596,0.00009087175,0.000093369825,0.000032569274,0.00019043373,0.0010588712,0.021978086,0.0007669598,0.004466595,0.009451737],"study_design_scores_gemma":[0.00075148564,0.00014550317,0.9428206,0.00010393426,0.000023564246,6.150292e-7,0.000011852858,0.0001493042,0.018739954,0.013647251,0.023236409,0.00036953067],"about_ca_topic_score_codex":0.00007409171,"about_ca_topic_score_gemma":0.000066461886,"teacher_disagreement_score":0.018769814,"about_ca_system_score_codex":0.000005547557,"about_ca_system_score_gemma":0.00007394153,"threshold_uncertainty_score":0.9998518},"labels":[],"label_agreement":null},{"id":"W7073645630","doi":"","title":"Congenital cytomegalovirus infection in Canada: Active surveillance for cases diagnosed by paediatricians","year":2014,"lang":"en","type":"article","venue":"PubMed Central","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cytomegalovirus; Cytomegalovirus infection; Cytomegalovirus infections; Betaherpesvirinae; Human cytomegalovirus","score_opus":0.0073173644847159165,"score_gpt":0.17651135965986464,"score_spread":0.16919399517514871,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073645630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99546385,0.00008145398,0.000041814743,0.00007127401,0.0016821206,0.0003931179,0.0019673798,0.000016234084,0.0002827447],"genre_scores_gemma":[0.9989572,0.000059079885,0.000009308278,0.00012344519,0.00044597988,0.000030255225,0.00035331468,0.0000041213134,0.000017265847],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986187,0.00007575293,0.00015687225,0.00019384005,0.00013035594,0.00082443404],"domain_scores_gemma":[0.9992676,0.0003774903,0.00006672627,0.00007997537,0.000012886932,0.00019534689],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021170238,0.00011223479,0.00018311238,0.000029181556,0.00006458619,0.00004103354,0.00008016261,0.000039497896,0.00007634298],"category_scores_gemma":[0.00018979768,0.00010266154,0.000031648047,0.000104857856,0.000018671148,0.0001325976,0.000004715032,0.000053387444,0.000005538636],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007008553,0.000013367104,0.97021204,0.000012120527,0.000015186426,0.000009724376,0.00003824489,0.00075922295,0.000029475805,0.0000136996,0.003421539,0.02540528],"study_design_scores_gemma":[0.0004287444,0.000031016494,0.97530633,0.0000010587856,0.000006667617,0.0000016823543,0.000010343652,0.00035333095,0.00048663394,0.000034114408,0.02320219,0.00013788504],"about_ca_topic_score_codex":0.94266677,"about_ca_topic_score_gemma":0.99256736,"teacher_disagreement_score":0.049900554,"about_ca_system_score_codex":0.000056399276,"about_ca_system_score_gemma":0.0002314494,"threshold_uncertainty_score":0.41864163},"labels":[],"label_agreement":null},{"id":"W7073652694","doi":"","title":"The IceCube Neutrino Observatory - Contributions to ICRC 2015 Part V:\\n Neutrino Oscillations and Supernova Searches","year":2015,"lang":"en","type":"other","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Marsden Fund; Japan Society for the Promotion of Science; Vetenskapsrådet; Natural Sciences and Engineering Research Council of Canada; Knut och Alice Wallenbergs Stiftelse; National Research Foundation of Korea; Fonds Wetenschappelijk Onderzoek; Bundesministerium für Bildung und Forschung; Helmholtz Alliance for Astroparticle Physics; Danmarks Grundforskningsfond; Belgian Federal Science Policy Office; Deutsche Forschungsgemeinschaft; National Research Foundation; University of Oxford; National Science Foundation; Compute Canada; Western Canada Research Grid; Office of Polar Programs; Vlaamse regering; Fonds De La Recherche Scientifique - FNRS; Polarforskningssekretariatet; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; U.S. Department of Energy","keywords":"Supernova; Neutrino; Observatory; Neutrino oscillation; Neutrino detector; Neutrino astronomy; Solar neutrino problem","score_opus":0.03672304685188489,"score_gpt":0.25724778372768736,"score_spread":0.22052473687580249,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073652694","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.046859186,0.0013961595,0.0004311348,0.0055478606,0.0007670212,0.0027605798,0.041322503,0.0002694708,0.9006461],"genre_scores_gemma":[0.038790517,0.021910831,0.0022486786,0.00010127825,0.00089542737,9.540231e-7,0.004456657,0.00015169343,0.931444],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9962676,0.00081014395,0.00018725594,0.00069254165,0.001027029,0.0010153959],"domain_scores_gemma":[0.9968385,0.0007186303,0.00018079927,0.00075408904,0.0006150151,0.00089294766],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0013514408,0.00034176846,0.000593768,0.0007267521,0.0016388544,0.00012813641,0.0015331975,0.00026159227,0.0013248331],"category_scores_gemma":[0.00010050282,0.00034178112,0.00015387761,0.0009551718,0.0014565644,0.0003333411,0.000776783,0.0006784125,0.00014462616],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065483956,0.00007827229,0.009979355,0.00015778841,0.00035228726,0.00014648089,0.00079502224,0.00011254441,0.00015307139,0.008394974,0.9757181,0.0034572976],"study_design_scores_gemma":[0.0007951032,0.0003211738,0.026798628,0.00010492852,0.000073630916,0.000004056377,0.0020778594,0.00010812436,0.000005910914,0.0007207629,0.968648,0.00034178473],"about_ca_topic_score_codex":0.017723944,"about_ca_topic_score_gemma":0.05039406,"teacher_disagreement_score":0.036865845,"about_ca_system_score_codex":0.00007192732,"about_ca_system_score_gemma":0.00092075707,"threshold_uncertainty_score":0.99990344},"labels":[],"label_agreement":null},{"id":"W7073653196","doi":"","title":"All About Birds Midwest: Midwest US and Canada","year":2022,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Work (physics); Natural (archaeology); Population","score_opus":0.010682063718341423,"score_gpt":0.17930442544771366,"score_spread":0.16862236172937223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073653196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89168036,0.000007894249,0.0000045969346,0.00018617927,0.0006320612,0.0002450819,0.0008550858,0.000062281884,0.106326476],"genre_scores_gemma":[0.99236804,0.006702132,0.00010359143,0.00042587647,0.00009492841,7.426683e-7,0.00018193512,0.0000077598925,0.000114968025],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986887,0.00015998117,0.00012130542,0.0003575294,0.00029813257,0.00037437078],"domain_scores_gemma":[0.99945176,0.00007109782,0.00008752781,0.00022547308,0.00003220434,0.0001319243],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014287361,0.00017591253,0.00020892583,0.00095743395,0.0004569768,0.000061873434,0.0003631838,0.000039684586,0.0009427611],"category_scores_gemma":[0.000009991267,0.00018419603,0.000041012023,0.0014408649,0.000056134144,0.00021448702,0.0001263322,0.000159805,0.000014961605],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031926662,0.0009867277,0.71457374,0.0011446823,0.0021826837,0.016013885,0.024438202,0.022421185,0.0007789791,0.007919544,0.05128553,0.15506217],"study_design_scores_gemma":[0.00038716203,0.00009952153,0.019453142,0.000005282495,0.000047504163,0.000018351131,0.00022614852,0.00021857105,0.00009351773,0.0000014016002,0.9792027,0.00024673456],"about_ca_topic_score_codex":0.9965118,"about_ca_topic_score_gemma":0.98851687,"teacher_disagreement_score":0.9279171,"about_ca_system_score_codex":0.00003466112,"about_ca_system_score_gemma":0.00058165105,"threshold_uncertainty_score":0.9999705},"labels":[],"label_agreement":null},{"id":"W7073653373","doi":"","title":"Bacterial contaminants in cosmetic products from a patient with cystic fibrosis","year":2006,"lang":"en","type":"article","venue":"Research Portal (Queen's University Belfast)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute of Infection and Immunity","funders":"","keywords":"Cystic fibrosis; Contamination; Fibrosis; Bacteria","score_opus":0.009714906710954771,"score_gpt":0.20529823093105476,"score_spread":0.1955833242201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073653373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99470794,0.000014251247,0.0000078737,0.00023690143,0.000159515,0.00045960717,0.00082081405,0.000030296847,0.0035628222],"genre_scores_gemma":[0.99767745,0.00001614047,0.0003503491,0.0000056189556,0.00015636165,7.3685686e-7,0.00070549274,0.000006754646,0.0010811073],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976554,0.0003565647,0.00019078626,0.00049053517,0.0006664663,0.0006402547],"domain_scores_gemma":[0.9991077,0.00018298686,0.00008275251,0.00028836716,0.00017880641,0.00015935815],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003106117,0.00017348398,0.00028534586,0.00023989257,0.00024230708,0.00010027064,0.00029346155,0.00008529558,0.0016118365],"category_scores_gemma":[0.000040180683,0.00015126044,0.00003373275,0.0005806252,0.00020466224,0.00034112931,0.00006764729,0.00021799887,0.00018746176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.012328326,0.0019698436,0.86145544,0.000594405,0.0004308865,0.02628398,0.0029267927,0.004262601,0.037371,0.00489902,0.03456224,0.012915475],"study_design_scores_gemma":[0.0015539821,0.0009422497,0.9636972,0.00014588756,0.000033505297,0.0000064808846,0.0007224049,0.00007671042,0.0040493403,0.00038126056,0.027977828,0.00041317422],"about_ca_topic_score_codex":0.13294186,"about_ca_topic_score_gemma":0.0069954135,"teacher_disagreement_score":0.12594645,"about_ca_system_score_codex":0.000021125643,"about_ca_system_score_gemma":0.00023641872,"threshold_uncertainty_score":0.99930084},"labels":[],"label_agreement":null},{"id":"W7073656766","doi":"","title":"Indoor and outdoor levels and sources of submicron particles (PM1) at homes in Edmonton, Canada","year":2015,"lang":"en","type":"article","venue":"Research Bank (Australian Catholic University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Smoke; Biomass burning; Biomass (ecology); Indoor air quality; Air pollution; Air pollutants; Coal","score_opus":0.0688331515197596,"score_gpt":0.2551947186229529,"score_spread":0.1863615671031933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073656766","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981415,0.00018875947,1.5792631e-7,0.0004888189,0.000039798124,0.00014165627,0.00022363999,0.0000061367523,0.0007695225],"genre_scores_gemma":[0.996025,0.000068717214,0.00004734964,0.000007987027,0.00002904143,1.5394633e-7,0.000012574655,0.0000027317606,0.0038064378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986852,0.00022487818,0.00012521722,0.00023396131,0.00032127774,0.00040948868],"domain_scores_gemma":[0.9993234,0.00010727057,0.000045155903,0.00013849704,0.000087409746,0.00029824796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057503005,0.0000987963,0.00020505629,0.00020436085,0.000112305344,0.000045203717,0.00018502928,0.000059679594,0.00010739046],"category_scores_gemma":[0.000046670222,0.00009262832,0.000013497757,0.00031355207,0.0002855641,0.00019156442,0.00008001601,0.00011547611,0.000007917416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018930958,0.000024538245,0.9843672,0.00011576534,0.00002762324,0.000340341,0.004369193,0.00009025891,0.00584243,0.00023040434,0.0015637785,0.0028391394],"study_design_scores_gemma":[0.000663415,0.00011406853,0.91625696,0.000031374315,0.000010543385,0.000010299818,0.0015342324,0.000025772259,0.008431599,0.00010938802,0.07265715,0.00015520632],"about_ca_topic_score_codex":0.713531,"about_ca_topic_score_gemma":0.77077127,"teacher_disagreement_score":0.07109337,"about_ca_system_score_codex":0.00003220003,"about_ca_system_score_gemma":0.00032262478,"threshold_uncertainty_score":0.3777273},"labels":[],"label_agreement":null},{"id":"W7073657553","doi":"","title":"Because This Land is Who We Are : Indigenous Practices of Environmental Repossession","year":2024,"lang":"en","type":"book","venue":"BiblioBoard Library Catalog (Open Research Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Indigenous; Aotearoa; Land rights; Indigenous rights; Community engagement; Traditional knowledge","score_opus":0.0613148882231356,"score_gpt":0.3098178441186661,"score_spread":0.24850295589553048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073657553","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.035364382,0.040978342,3.8865718e-7,0.00580338,0.0013092185,0.0035804417,0.04336133,0.0003291537,0.86927336],"genre_scores_gemma":[0.007915303,0.034640368,0.00034285407,0.0004427395,0.0012143898,0.00003629517,0.014423594,0.00016354049,0.94082093],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9935367,0.000777765,0.0010536313,0.0015819038,0.0019222525,0.0011277102],"domain_scores_gemma":[0.9954089,0.0009538678,0.001311887,0.0016555048,0.000034986515,0.0006348804],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000925323,0.00072312314,0.0012638562,0.004105697,0.0005007434,0.004191179,0.0039654667,0.0007851489,0.05286882],"category_scores_gemma":[0.000057591285,0.0005706441,0.00028272337,0.0027240056,0.0006168812,0.011878316,0.0025276246,0.0015624436,0.005531941],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034964044,0.00011288254,0.018305426,0.0011882974,0.00030288036,0.0010414914,0.00068413606,0.0000021964463,0.00013412046,0.00026428016,0.9750109,0.002603749],"study_design_scores_gemma":[0.000337184,0.00053979724,0.017670076,0.0013797136,0.00009325074,0.00002861264,0.0000884081,0.000011756445,0.0030400143,0.010658395,0.9654628,0.00068997947],"about_ca_topic_score_codex":0.0017035184,"about_ca_topic_score_gemma":0.0000697991,"teacher_disagreement_score":0.071547545,"about_ca_system_score_codex":0.000012489544,"about_ca_system_score_gemma":0.0022217303,"threshold_uncertainty_score":0.9996745},"labels":[],"label_agreement":null},{"id":"W7073661807","doi":"","title":"A sensitive radioimmunoprecipitation assay for assessing the clinical relevance of antibodies to IFN beta.","year":2003,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Fusible alloy; Proteogenomics; TSG101; Sulfinpyrazone; Diafiltration","score_opus":0.04115683891647297,"score_gpt":0.30091161914331305,"score_spread":0.25975478022684007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073661807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94020426,0.000046957623,0.03634975,0.0006784903,0.00024237279,0.0008960827,0.00094969576,0.000024131408,0.020608261],"genre_scores_gemma":[0.9731817,0.0005945564,0.02475729,0.000020139345,0.000042419284,9.2818766e-8,0.0001265631,0.000006648814,0.001270541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9969168,0.0013952148,0.00022094822,0.00041982252,0.0005271426,0.000520081],"domain_scores_gemma":[0.99551857,0.0030937581,0.00023423164,0.00039540592,0.0005646964,0.00019334229],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030117675,0.00015920542,0.0004416098,0.00031581012,0.0009728989,0.0000458723,0.0007238751,0.000093195755,0.00012870193],"category_scores_gemma":[0.0005027799,0.00015526837,0.00022522929,0.00058072794,0.00087828655,0.0005322339,0.00014693863,0.0003006814,0.000010463268],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01164044,0.001364215,0.4817533,0.0014813099,0.0030021693,0.00047491834,0.04243397,0.011622047,0.041568488,0.12064225,0.03424231,0.2497746],"study_design_scores_gemma":[0.0019246781,0.0012212101,0.5690716,0.0001943248,0.0001564237,0.00000609439,0.025954008,0.002666959,0.0013303233,0.006384071,0.3906468,0.0004435006],"about_ca_topic_score_codex":0.001557539,"about_ca_topic_score_gemma":0.00204325,"teacher_disagreement_score":0.35640448,"about_ca_system_score_codex":0.000020204243,"about_ca_system_score_gemma":0.0003172382,"threshold_uncertainty_score":0.748285},"labels":[],"label_agreement":null},{"id":"W7073664002","doi":"","title":"Click chemistry as a route to the synthesis of structurally new and magnetically interesting coordination clusters: a {Ni} complex with a trapezoidal prismatic topology.","year":2019,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Office of Science; Basic Energy Sciences; Ministerio de Economía y Competitividad; U.S. Department of Energy","keywords":"Click chemistry; Coordination complex; Cluster (spacecraft); Ion; Solvent; Chelation","score_opus":0.008627987559885298,"score_gpt":0.19019383036226867,"score_spread":0.18156584280238336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073664002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98979837,0.000032858243,0.00003684024,0.0016339143,0.000054353855,0.00036924367,0.0008323489,0.000046981182,0.007195119],"genre_scores_gemma":[0.9971977,0.0000013793948,0.0014528009,0.00036099917,0.00007437721,0.0000025853383,0.00017519404,0.000011736979,0.00072326517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988265,0.00006265818,0.00031734703,0.00029462777,0.00022669608,0.00027216156],"domain_scores_gemma":[0.9991125,0.000284206,0.0001398295,0.00023606396,0.000025291352,0.00020211063],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011565871,0.00019685105,0.00028858896,0.00003834671,0.00007005339,0.0006353941,0.00036400266,0.00007257947,0.001988308],"category_scores_gemma":[0.00012838327,0.00012486594,0.00004396949,0.00017383207,0.00009182909,0.0008343046,0.00008020993,0.00013901315,0.00034497955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023648378,0.000115533614,0.838826,0.0012125967,0.00035488358,0.000049267932,0.0009738044,0.00081283826,0.010965083,0.0011112449,0.0020925654,0.14112134],"study_design_scores_gemma":[0.0023636715,0.0018640314,0.911021,0.0009044387,0.00023021127,0.00023434806,0.00073855545,0.0035534557,0.016262613,0.01364544,0.047614682,0.0015675303],"about_ca_topic_score_codex":0.00011057756,"about_ca_topic_score_gemma":0.000041059,"teacher_disagreement_score":0.13955382,"about_ca_system_score_codex":0.0000023323446,"about_ca_system_score_gemma":0.000078850935,"threshold_uncertainty_score":0.998924},"labels":[],"label_agreement":null},{"id":"W7073664914","doi":"","title":"Mycobacterium branderi from Both a Hand Infection and a Case of Pulmonary Disease","year":2000,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"16S ribosomal RNA; Pathogen; Antibiotics; Gene; Identification (biology); Ribosomal RNA; Mycolic acid; Human pathogen","score_opus":0.006710505114449338,"score_gpt":0.19063789693933467,"score_spread":0.18392739182488532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073664914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99621195,0.00016001615,0.000020658494,0.000031112904,0.00011382506,0.00008075639,0.00036016482,0.00001649183,0.0030050378],"genre_scores_gemma":[0.99918336,0.00009384618,0.000052433774,0.0000479099,0.00009689091,6.561596e-7,0.00010210322,0.0000017664215,0.0004210069],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99955434,0.00003367609,0.00011220138,0.00014270568,0.000056323162,0.000100745034],"domain_scores_gemma":[0.999719,0.000033208238,0.000026350799,0.000099896206,0.000008770439,0.00011276111],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00004733439,0.000073491006,0.00011595539,0.000017969714,0.00007683698,0.00005835613,0.000025595611,0.000025772102,0.012052806],"category_scores_gemma":[0.0000031285485,0.000055917288,0.000022382206,0.000042328935,0.000052761065,0.00016075176,0.000004401439,0.000021471256,0.000050211365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012326554,0.0001634551,0.7351404,0.0002177479,0.00009479766,0.0017974935,0.00074268103,0.0005938907,0.017481746,0.00008639197,0.0006372659,0.24181148],"study_design_scores_gemma":[0.0002172401,0.00003980918,0.9915344,0.000010812426,0.000037862806,0.000055841945,0.00000827021,0.0022113286,0.0005559593,0.0010129387,0.004200185,0.000115342846],"about_ca_topic_score_codex":0.039533027,"about_ca_topic_score_gemma":0.0018613393,"teacher_disagreement_score":0.25639403,"about_ca_system_score_codex":3.6196025e-7,"about_ca_system_score_gemma":0.000013205796,"threshold_uncertainty_score":0.9888503},"labels":[],"label_agreement":null},{"id":"W7073668745","doi":"","title":"The challenge of establishing, growing and sustaining a large biobank. A personal perspective","year":2014,"lang":"en","type":"article","venue":"Research Bank (Australian Catholic University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Perspective (graphical); Quality (philosophy); Interpretation (philosophy); Creativity; Value (mathematics); Ethnic group","score_opus":0.03137054457400675,"score_gpt":0.27253376561740833,"score_spread":0.24116322104340157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073668745","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9743884,0.00018772992,0.000011139323,0.003090947,0.000097005905,0.00019733989,0.0001219739,0.000024751696,0.0218807],"genre_scores_gemma":[0.9963425,0.00022561033,0.00005267245,0.000009247391,0.0001395275,2.167496e-7,0.000011112079,0.0000042236525,0.0032148983],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980298,0.00047910077,0.00011200522,0.0003152296,0.0004309142,0.00063294626],"domain_scores_gemma":[0.9988461,0.00044653346,0.000060974282,0.000207778,0.00025781305,0.00018081277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019210166,0.000116145595,0.00018114534,0.0002539504,0.0007843321,0.00017372171,0.0003934694,0.000078898825,0.00021065591],"category_scores_gemma":[0.00022878846,0.00009260645,0.000055026834,0.00048728025,0.00040147765,0.00046506285,0.000092832815,0.00029906604,0.000019755978],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008787008,0.00026009578,0.036521655,0.0006209392,0.00045690264,0.0005629731,0.13473688,0.00015870339,0.0048267366,0.780391,0.0031449446,0.03744046],"study_design_scores_gemma":[0.0012635385,0.0007175955,0.065408096,0.0001215437,0.000054145417,0.000013016551,0.04582733,0.0011246996,0.00067855546,0.0043595615,0.87998873,0.00044318204],"about_ca_topic_score_codex":0.007472567,"about_ca_topic_score_gemma":0.001447276,"teacher_disagreement_score":0.8768438,"about_ca_system_score_codex":0.000020290308,"about_ca_system_score_gemma":0.00011838471,"threshold_uncertainty_score":0.99913675},"labels":[],"label_agreement":null},{"id":"W7073677040","doi":"","title":"Development of measures to assess listening-related effort and fatigue in daily life among hearing aid users:protocol for a quantitative field trial","year":2024,"lang":"en","type":"article","venue":"Technical University of Denmark, DTU Orbit (Technical University of Denmark, DTU)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Hearing aid; Field (mathematics); Hearing loss; Quality of life (healthcare)","score_opus":0.061353493383206496,"score_gpt":0.28409485799452633,"score_spread":0.22274136461131983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073677040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9623044,0.000053038482,0.014540411,0.00026814637,0.00015845042,0.018415187,0.0001533445,0.00012218484,0.0039848196],"genre_scores_gemma":[0.9643884,0.000018517212,0.035188325,0.000017220867,0.000018110804,0.000020475185,0.00002427361,0.000012661498,0.00031201745],"study_design_codex":"randomized_trial","study_design_gemma":"observational","domain_scores_codex":[0.99758095,0.00014741502,0.00062792806,0.0006612932,0.00055076834,0.00043166714],"domain_scores_gemma":[0.99791974,0.00091396004,0.0003105746,0.00034410268,0.0001996273,0.0003119829],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0011503196,0.00030603784,0.0008943085,0.0004688633,0.00021142368,0.000038943766,0.0007900474,0.00046255047,0.00056193466],"category_scores_gemma":[0.0002939527,0.00033599683,0.0002558447,0.0007439908,0.00043692946,0.00041300975,0.00031771138,0.00039903217,0.000017443286],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.39833698,0.005793188,0.21204,0.015848704,0.0054066875,0.0023685326,0.019542173,0.010380565,0.18133622,0.044291187,0.03457282,0.070082925],"study_design_scores_gemma":[0.08170153,0.015741272,0.7494887,0.010012563,0.0015058187,0.00005119787,0.00860563,0.009639549,0.01894003,0.0036146198,0.09571048,0.004988621],"about_ca_topic_score_codex":0.0023884862,"about_ca_topic_score_gemma":0.007356622,"teacher_disagreement_score":0.5374487,"about_ca_system_score_codex":0.0000499744,"about_ca_system_score_gemma":0.0003687176,"threshold_uncertainty_score":0.9999092},"labels":[],"label_agreement":null},{"id":"W7073678119","doi":"","title":"Esthetics and Smile Characteristics Evaluated by Laypersons: A comparison of Canadian and US data","year":2010,"lang":"en","type":"dissertation","venue":"Mspace (University of Manitoba)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Wilcoxon signed-rank test; Preference; Ideal (ethics); Perception; Face (sociological concept); Paired comparison","score_opus":0.02370447033997231,"score_gpt":0.21850129955639175,"score_spread":0.19479682921641944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073678119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99335325,0.0003393743,0.0000016268034,0.00012177831,0.00027642254,0.00014483,0.004856251,0.0000068677937,0.0008996156],"genre_scores_gemma":[0.9899448,0.00050511776,0.0002845098,0.000007598974,0.000022906457,2.5476101e-8,0.008924666,0.0000048833895,0.00030549528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993088,0.000042790994,0.00009495838,0.00023552447,0.00016546187,0.00015241464],"domain_scores_gemma":[0.9992469,0.00003599289,0.00022791229,0.0002691853,0.000079310834,0.00014071916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014574794,0.000129652,0.00035368223,0.00016496268,0.00015001293,0.000029612276,0.00030838195,0.00020112962,0.00007986935],"category_scores_gemma":[0.000016969167,0.00015198678,0.00001697472,0.000102991544,0.00010212087,0.0001100462,0.000025745683,0.00014670975,0.000009837306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034538336,0.000096327756,0.9285236,0.0011796817,0.00030862822,0.00004420449,0.0038149992,0.000020727983,0.0071043344,0.00008519354,0.037967812,0.020509133],"study_design_scores_gemma":[0.00024930487,0.000111395915,0.94140846,0.000076983095,0.00024906103,0.0000017140227,0.005483047,0.0037657972,0.00011318329,0.000020061041,0.048300236,0.00022076104],"about_ca_topic_score_codex":0.5739574,"about_ca_topic_score_gemma":0.990375,"teacher_disagreement_score":0.41641757,"about_ca_system_score_codex":0.0000024329236,"about_ca_system_score_gemma":0.00011319841,"threshold_uncertainty_score":0.6197841},"labels":[],"label_agreement":null},{"id":"W7073680674","doi":"","title":"Experiences of Visible Minority Librarians and Students in Canada from the ViMLoC Mentorship Program","year":2023,"lang":"en","type":"article","venue":"Scholars Commons (Wilfrid Laurier University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mentorship; Helpfulness; Empirical research; Perception; Qualitative research; Empirical evidence","score_opus":0.01243848657870434,"score_gpt":0.20254714583313854,"score_spread":0.1901086592544342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073680674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969698,0.00011637479,4.5717402e-7,0.00018749957,0.0003125248,0.0002310533,0.00027188286,0.000030368272,0.0018800375],"genre_scores_gemma":[0.9994533,0.000050952942,0.0000567683,0.00003773515,0.000027028505,9.306705e-7,0.00007730147,0.0000023489501,0.00029364196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988559,0.00021485655,0.00013909917,0.00022286366,0.0003103708,0.0002569339],"domain_scores_gemma":[0.99936515,0.00019820122,0.00006888102,0.00023724698,0.000020716825,0.000109788314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023003314,0.00011243045,0.00018596277,0.00009502586,0.00020547764,0.0001208879,0.00063781854,0.000041419407,0.0002720673],"category_scores_gemma":[0.000019375731,0.00009155334,0.000026098327,0.00071660994,0.00010423598,0.00042131537,0.00011722249,0.00013868505,0.00000957764],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003911455,0.000023328117,0.9943641,0.000007829894,0.00003287169,0.000062474835,0.0025417202,0.00005029768,0.000040279414,0.00018487009,0.0008792149,0.0017739298],"study_design_scores_gemma":[0.00035468317,0.000051652136,0.953899,0.0000235984,0.00002270098,3.5169677e-7,0.011318153,0.0001020078,0.0003071868,0.0002409953,0.033538774,0.00014084572],"about_ca_topic_score_codex":0.80294186,"about_ca_topic_score_gemma":0.91408294,"teacher_disagreement_score":0.11114104,"about_ca_system_score_codex":0.000011957079,"about_ca_system_score_gemma":0.00026280907,"threshold_uncertainty_score":0.37334368},"labels":[],"label_agreement":null},{"id":"W7073682604","doi":"","title":"Modes of innovation in an emerging economy : a firm-level analysis from Mexico","year":2020,"lang":"en","type":"article","venue":"tub.dok (Hamburg University of Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Emerging markets; Mode (computer interface); Product (mathematics); Core (optical fiber); Process (computing); Product innovation; Point (geometry)","score_opus":0.024758214071221328,"score_gpt":0.20524045297889412,"score_spread":0.1804822389076728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073682604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971508,0.00003231926,0.0010361467,0.0006104327,0.000019515694,0.00007587831,0.0002099164,0.000043160806,0.0008218573],"genre_scores_gemma":[0.9969331,0.00001099718,0.0028331927,0.000031501444,0.0000089154155,5.5132414e-8,0.0001479199,0.0000016013925,0.000032702214],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99930274,0.000022784792,0.00023077025,0.00023452663,0.00007591073,0.00013328275],"domain_scores_gemma":[0.99945945,0.00001659035,0.00021109232,0.0001949314,0.00008389809,0.00003403456],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010326415,0.00009016416,0.00034218642,0.0005236212,0.000046334895,0.000006686652,0.00034202635,0.000117843076,0.0011443739],"category_scores_gemma":[0.000015684278,0.00010228584,0.000045509638,0.0015913448,0.000111830115,0.00025217782,0.000046000372,0.00009130437,0.000012590451],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011615007,0.0000477262,0.96411073,0.000027650669,0.00029768122,0.000024222312,0.0013577415,0.012152873,0.014135673,0.0017443572,0.00013375895,0.0058514397],"study_design_scores_gemma":[0.0011923434,0.00033950194,0.9142038,0.00004050074,0.00045097905,4.9686474e-7,0.0033565543,0.037673026,0.023781933,0.010993307,0.0074783387,0.00048917515],"about_ca_topic_score_codex":0.024900898,"about_ca_topic_score_gemma":0.010148518,"teacher_disagreement_score":0.049906883,"about_ca_system_score_codex":0.000005637452,"about_ca_system_score_gemma":0.000053101405,"threshold_uncertainty_score":0.99976873},"labels":[],"label_agreement":null},{"id":"W7073683259","doi":"","title":"Type-1 Collagen Differentially Alters Beta-catenin Accumulation in Primary Dupuytren's Disease Cord and Adjacent Palmar Fascia Cells","year":2009,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Musculoskeletal Health and Arthritis; Canadian Institutes of Health Research; Lawson Health Research Institute","keywords":"Myofibroblast; Fibrosis; Fibroblast; Immunofluorescence; In vitro; In vivo; Extracellular matrix; Transforming growth factor; Cell culture","score_opus":0.06159831917570883,"score_gpt":0.2721574442571607,"score_spread":0.2105591250814519,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073683259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99851614,0.00012983229,0.000034057644,0.00016507815,0.00042905135,0.00036707256,0.00014174693,0.000062270934,0.00015477014],"genre_scores_gemma":[0.9980503,0.00018216402,0.000032762742,0.00025164548,0.000084508414,1.9106614e-7,0.0002971056,0.000009148199,0.0010921763],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99818605,0.00024811973,0.0002553755,0.0005380821,0.0003309717,0.0004413791],"domain_scores_gemma":[0.99904954,0.000065633285,0.00015826992,0.00029386807,0.00006317709,0.0003694843],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00021202331,0.00029176087,0.00035631124,0.00027752892,0.00017491032,0.0002775524,0.00039598666,0.000121040706,0.00012484407],"category_scores_gemma":[0.000009120835,0.00029367066,0.0000681526,0.000333589,0.00008311398,0.0010291779,0.00007337173,0.00015222204,0.00013840012],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006021664,0.000056377623,0.99174035,0.000042985164,0.000024465417,0.00021155026,0.00015977434,0.00037717813,0.0046880334,0.00001675501,0.000002360255,0.0020779883],"study_design_scores_gemma":[0.0008331611,0.00018350176,0.99674827,0.00007255,0.00008376176,0.000001869118,0.000032947522,0.000006302412,0.0009792373,0.000111234964,0.0006038917,0.00034328594],"about_ca_topic_score_codex":0.000042273554,"about_ca_topic_score_gemma":0.0016037337,"teacher_disagreement_score":0.005007891,"about_ca_system_score_codex":0.000031684118,"about_ca_system_score_gemma":0.00008766023,"threshold_uncertainty_score":0.99995154},"labels":[],"label_agreement":null},{"id":"W7073685434","doi":"","title":"Constraints on non-Standard Model Higgs boson interactions in an effective Lagrangian using differential cross sections measured in the $H \\rightarrow \\gamma\\gamma$ decay channel at $\\sqrt{s} = 8$ TeV with the ATLAS detector","year":2016,"lang":"en","type":"article","venue":"DESY Publication Database (PUBDB) (Deutsches Elektronen-Synchrotron)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"H2020 Marie Skłodowska-Curie Actions; Institut National de Physique Nucléaire et de Physique des Particules; Fundação para a Ciência e a Tecnologia; Agencia Nacional de Promoción Científica y Tecnológica; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Science and Technology Facilities Council; Bundesministerium für Bildung und Forschung; Ministry of Education, Culture, Sports, Science and Technology; Natural Sciences and Engineering Research Council of Canada; Department of Science and Technology, Ministry of Science and Technology, India; H. Lundbeck A/S; Fondation Partager le Savoir; European Social Fund; Centre National pour la Recherche Scientifique et Technique; Georgian National Science Foundation; Japan Society for the Promotion of Science; National Research Center \"Kurchatov Institute\"; British Columbia Knowledge Development Fund; Centre National de la Recherche Scientifique; Max-Planck-Gesellschaft; Israel Science Foundation; U.S. Department of Energy; Israeli Centers for Research Excellence; Comisión Nacional de Investigación Científica y Tecnológica; Türkiye Atom Enerjisi Kurumu; Joint Institute for Nuclear Research; Ministerstwo Edukacji i Nauki; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Bundesministerium für Wissenschaft, Forschung und Wirtschaft; Fonds Québécois de la Recherche sur la Nature et les Technologies; Austrian Science Fund; Ontario Innovation Trust; National Natural Science Foundation of China; European Commission; Leverhulme Trust; Fundação de Amparo à Pesquisa do Estado de São Paulo; Javna Agencija za Raziskovalno Dejavnost RS; Deutsche Forschungsgemeinschaft; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Agence Nationale de la Recherche; Services Fédéraux des Affaires Scientifiques, Techniques et Culturelles; General Secretariat for Research and Technology; National Science Foundation; Lundbeckfonden; Compute Canada; Alexander von Humboldt-Stiftung; TRIUMF; Departamento Administrativo de Ciencia, Tecnología e Innovación (COLCIENCIAS); CERN; Danmarks Grundforskningsfond; Canarie","keywords":"Higgs boson; Atlas (anatomy); Large Hadron Collider; Kinematics; Lagrangian; Standard Model (mathematical formulation); Boson; Detector; Tensor (intrinsic definition)","score_opus":0.02435073845266146,"score_gpt":0.2598394081362846,"score_spread":0.23548866968362314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073685434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824229,0.00003242535,0.010083704,0.0014540937,0.00031459393,0.0023392711,0.0030717757,0.00008809046,0.00019315412],"genre_scores_gemma":[0.9976266,0.000010698446,0.00027772263,0.000081084865,0.0003607078,0.00037313803,0.0011807018,0.000032698325,0.000056630794],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9959048,0.0008512983,0.00059693237,0.000971741,0.00080778176,0.0008674197],"domain_scores_gemma":[0.9973698,0.0005160866,0.00039122644,0.0011712972,0.0003041398,0.00024741894],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0012626686,0.0005282713,0.00048865046,0.00040415267,0.00086575025,0.0006047717,0.0008596357,0.00012968389,0.0005195866],"category_scores_gemma":[0.00011093273,0.00028709625,0.00011996273,0.0006975745,0.0004820707,0.002071733,0.000077630684,0.0004352298,0.000110524226],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009964692,0.0031627791,0.29856092,0.0002521356,0.00092060334,0.000109816036,0.011035449,0.041881643,0.58428746,0.0022988743,0.0026748457,0.044850767],"study_design_scores_gemma":[0.010896869,0.0017760469,0.6622152,0.0005051744,0.00042956672,0.00011616236,0.0011993283,0.06292305,0.25169817,0.00024945763,0.005767139,0.002223852],"about_ca_topic_score_codex":0.0025834714,"about_ca_topic_score_gemma":0.03354508,"teacher_disagreement_score":0.36365426,"about_ca_system_score_codex":0.00016483413,"about_ca_system_score_gemma":0.00021134946,"threshold_uncertainty_score":0.9999581},"labels":[],"label_agreement":null},{"id":"W7073686702","doi":"","title":"Modest impact on risk for autism spectrum disorder of rare copy number variants at 15q11.2, specifically breakpoints 1 to 2.","year":2014,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; National Institutes of Health; Simons Foundation Autism Research Initiative; Howard Hughes Medical Institute","keywords":"Copy-number variation; Penetrance; Autism; Transmission disequilibrium test; Proband; Breakpoint; Autism spectrum disorder; Genome-wide association study; Chromosome","score_opus":0.008024372458314416,"score_gpt":0.2069104690933681,"score_spread":0.1988860966350537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073686702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9357452,0.000017720444,0.0006088402,0.0004952201,0.00033600337,0.00056072976,0.04040047,0.0001167069,0.02171914],"genre_scores_gemma":[0.9955284,0.000010523347,0.00083596923,0.00027013206,0.00025732047,0.0000070058104,0.00205059,0.000041567262,0.0009984899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99767804,0.00013253873,0.0005267084,0.0005941666,0.00041189953,0.00065664074],"domain_scores_gemma":[0.9982508,0.00043308185,0.00023294098,0.00053814444,0.000022952885,0.0005221193],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0002911017,0.0004000835,0.00054085517,0.000098365825,0.00020607002,0.0006643513,0.00055965554,0.00015922058,0.0069926577],"category_scores_gemma":[0.0001683772,0.00030163134,0.00026372512,0.0002703792,0.000072626244,0.0013433597,0.00009400678,0.00018607812,0.007936312],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020724973,0.00025545436,0.9734922,0.0000911773,0.00012979897,0.000011996017,0.000051248073,0.002141855,0.00023048076,0.0045168097,0.009386457,0.0076200403],"study_design_scores_gemma":[0.0013530274,0.00091524963,0.78025144,0.00011401431,0.000046598412,0.000010602439,0.0000061914666,0.0011120134,0.00275777,0.070453435,0.1421874,0.0007922675],"about_ca_topic_score_codex":0.00021026866,"about_ca_topic_score_gemma":0.0000492641,"teacher_disagreement_score":0.19324076,"about_ca_system_score_codex":0.0000089559535,"about_ca_system_score_gemma":0.000057127912,"threshold_uncertainty_score":0.99994355},"labels":[],"label_agreement":null},{"id":"W7073692343","doi":"","title":"Updated Survey of the Geriatrics Content of Canadian Undergraduate and Postgraduate Medical Curricula","year":2011,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geriatrics; Curriculum; Content (measure theory); MEDLINE; Content analysis","score_opus":0.0372401799963567,"score_gpt":0.18830974521895325,"score_spread":0.15106956522259654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073692343","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957133,0.00023859476,0.0000031823618,0.00036254743,0.0009266167,0.00024669818,0.00059963693,0.0000097334905,0.0018996709],"genre_scores_gemma":[0.99909586,0.00050756574,0.000036309066,0.000093050476,0.000034582932,7.5450845e-7,0.000086830565,0.0000059719,0.00013909987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982348,0.0003710621,0.00034065192,0.00019805651,0.00032805692,0.00052736787],"domain_scores_gemma":[0.9989114,0.00005251217,0.00017678716,0.00024059389,0.00013961854,0.0004791367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007262457,0.00013220691,0.00024310575,0.000090740024,0.0000662957,0.000020050185,0.000369579,0.00005468657,0.0003732191],"category_scores_gemma":[0.00026170487,0.00008333144,0.000038924547,0.0005876717,0.00018094,0.00007054606,0.000035598812,0.00009565333,0.000014419838],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004718517,0.000030493047,0.9934179,0.000026203985,0.00005689539,0.000024755565,0.0006000943,0.000010891334,0.00014055514,0.00061506947,0.0012278903,0.0038020425],"study_design_scores_gemma":[0.00022515314,0.000028969844,0.9957371,0.000014009394,0.000027725504,0.0000062575896,0.000008515687,0.000043069234,0.0012667503,0.0001038388,0.002437126,0.000101534686],"about_ca_topic_score_codex":0.531787,"about_ca_topic_score_gemma":0.21223922,"teacher_disagreement_score":0.31954774,"about_ca_system_score_codex":0.000003174186,"about_ca_system_score_gemma":0.00021364524,"threshold_uncertainty_score":0.80213535},"labels":[],"label_agreement":null},{"id":"W7073694327","doi":"","title":"Sex differences in clinical phenotypes of behavioral variant frontotemporal dementia","year":2024,"lang":"en","type":"article","venue":"DZNE Pub","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Institute on Aging; NIHR Cambridge Biomedical Research Centre; Medical Research Council; Alzheimer Nederland; Demensförbundet; Vetenskapsrådet; Ministero della Salute; National Institute of Neurological Disorders and Stroke; National Institute for Health and Care Research; Bundesministerium für Bildung und Forschung; Brain Research UK; Deutsche Forschungsgemeinschaft; University College London; Stichting Dioraphte; University of Cambridge; Instituto de Salud Carlos III; ZonMw; Weston Brain Institute","keywords":"Frontotemporal dementia; Phenotype; Genetic testing; Dementia; Genetic variants; Genetic model","score_opus":0.034718974813067106,"score_gpt":0.2793608070273975,"score_spread":0.24464183221433042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073694327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952774,0.0009739162,0.000057501595,0.00007023982,0.0013256517,0.00009275135,0.00017306313,0.000027455262,0.002001994],"genre_scores_gemma":[0.99913216,0.000038017366,0.00032606165,0.000017647953,0.00019688295,0.0000012023648,0.00007204346,0.0000026995178,0.00021330731],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989957,0.00009475404,0.00036111198,0.00021230032,0.00015287581,0.00018325886],"domain_scores_gemma":[0.9996868,0.000074426134,0.000048375758,0.00012060593,0.000011537838,0.000058274993],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004577381,0.000090087975,0.00025235343,0.00004688155,0.000023299863,0.0000753936,0.00015772427,0.00006196208,0.002100365],"category_scores_gemma":[0.0000069679713,0.00006681301,0.000057088924,0.000091101945,0.000056946115,0.00013871615,0.00001740861,0.00008370489,0.00010676824],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002781175,0.000079438585,0.9644021,0.000052078707,0.000056031164,0.00006719963,0.00040921583,0.000020215617,0.0001288372,0.0009954027,0.00084126776,0.0329204],"study_design_scores_gemma":[0.00015176176,0.00014412455,0.99175775,0.00003322454,0.000048607213,0.000001328104,0.000050938597,0.00134758,0.00010741782,0.0021750343,0.004061606,0.00012062726],"about_ca_topic_score_codex":0.0089751985,"about_ca_topic_score_gemma":0.002531491,"teacher_disagreement_score":0.032799773,"about_ca_system_score_codex":9.451056e-7,"about_ca_system_score_gemma":0.00004838313,"threshold_uncertainty_score":0.99881184},"labels":[],"label_agreement":null},{"id":"W7073694434","doi":"","title":"Of National Immunization Technical Advisory Groups (NITAGs), Evidence, and Decisions on Public Vaccination Programs: Lessons from Canada","year":2020,"lang":"en","type":"article","venue":"Portuguese National Funding Agency for Science, Research and Technology (RCAAP Project by FCT)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Public Health Ontario; Toronto Public Health","funders":"","keywords":"Immunization; Vaccination; Public health; Government (linguistics); Advisory committee","score_opus":0.11034156422553526,"score_gpt":0.35551909348457195,"score_spread":0.2451775292590367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073694434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9781365,0.0021059557,0.00046977785,0.013029549,0.00023106598,0.0016496446,0.0015348695,0.00012727558,0.002715352],"genre_scores_gemma":[0.99757856,0.00058907806,0.0010694774,0.00006077154,0.00007299038,0.000067673966,0.0004953648,0.0000066488938,0.000059440146],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99642235,0.00008615993,0.0004097772,0.0006624445,0.0018926419,0.0005266216],"domain_scores_gemma":[0.9966628,0.0011360015,0.00017661738,0.00015364376,0.0016703551,0.0002005995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026462174,0.00016151046,0.000235635,0.0009369131,0.0008516275,0.00015906461,0.00065160106,0.00015411705,0.00006627198],"category_scores_gemma":[0.0067434097,0.0001388971,0.000027225862,0.002989918,0.00064963615,0.0006893958,0.00014727257,0.00028993495,0.0000034380757],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047728486,0.0006237633,0.14701799,0.00024632053,0.00016940727,0.000017588445,0.00053729076,0.00007620635,0.058806207,0.3631371,0.0186438,0.41024706],"study_design_scores_gemma":[0.0023891432,0.0051197764,0.6083957,0.0004889439,0.00004853593,0.000037165235,0.0013564051,0.022161668,0.012972953,0.32412753,0.021535153,0.0013670205],"about_ca_topic_score_codex":0.011790428,"about_ca_topic_score_gemma":0.012073798,"teacher_disagreement_score":0.46137774,"about_ca_system_score_codex":0.000068063644,"about_ca_system_score_gemma":0.0026124888,"threshold_uncertainty_score":0.99479014},"labels":[],"label_agreement":null},{"id":"W7073694726","doi":"","title":"The Global Kidney Patient Trials Network and the CAPTIVATE Platform Clinical Trial Design: A Trial Protocol","year":2024,"lang":"en","type":"article","venue":"UCL Discovery (University College London)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Clinical trial; Kidney disease; Randomized controlled trial; Renal function; Protocol (science)","score_opus":0.043289255852904544,"score_gpt":0.2752841668374662,"score_spread":0.23199491098456165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073694726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6305485,0.00071429583,0.003536215,0.0074431524,0.025681678,0.3090852,0.010328713,0.00039716053,0.012265096],"genre_scores_gemma":[0.9768697,0.00046043322,0.000859483,0.0011685244,0.008068443,0.001720998,0.00022688115,0.000034623372,0.010590915],"study_design_codex":"randomized_trial","study_design_gemma":"not_applicable","domain_scores_codex":[0.99618924,0.0017566186,0.000638767,0.0004895109,0.0004387176,0.00048715298],"domain_scores_gemma":[0.99588144,0.003190099,0.00028844908,0.00036078392,0.00004063973,0.00023860032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0045410967,0.00026859678,0.000697486,0.00003468584,0.0011017296,0.00066783454,0.0005018733,0.00016117992,0.0002649508],"category_scores_gemma":[0.00044282322,0.0001450551,0.00040162064,0.00046106108,0.0004976721,0.0007933286,0.00014153836,0.00024111907,0.000093435825],"study_design_candidate":"randomized_trial","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.8702669,0.00007024082,0.00011558841,0.000038136914,0.00045365773,0.00016826093,0.00015986772,0.0005906526,0.0000010378958,0.05696568,0.06330563,0.007864323],"study_design_scores_gemma":[0.28709626,0.0033831748,0.00069166993,0.00012168301,0.00047230153,0.0000151760405,0.00047140254,0.009721044,0.0000059925105,0.021660207,0.67584383,0.0005172216],"about_ca_topic_score_codex":0.0010051638,"about_ca_topic_score_gemma":0.0005465553,"teacher_disagreement_score":0.6125382,"about_ca_system_score_codex":0.000022374805,"about_ca_system_score_gemma":0.0005965745,"threshold_uncertainty_score":0.8473725},"labels":[],"label_agreement":null},{"id":"W7073698843","doi":"","title":"Pregnancy, fetal, and neonatal outcomes after a first booster dose of covid-19 vaccine during pregnancy in Ontario, Canada: population based, retrospective cohort study","year":2023,"lang":"en","type":"other","venue":"Duo Research Archive (University of Oslo)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Retrospective cohort study; Pregnancy; Population; Cohort study; Booster dose; Booster (rocketry)","score_opus":0.017212217945412146,"score_gpt":0.23324600332778225,"score_spread":0.2160337853823701,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073698843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896582,0.0003127493,0.000018005258,0.00013583708,0.00016270617,0.002246889,0.0033215655,0.000040951,0.0041030925],"genre_scores_gemma":[0.9779313,0.00014332283,0.00012052891,0.000004019866,0.000016622267,0.0000034170687,0.00032995045,0.000041276584,0.021409517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782985,0.00027891478,0.00019478191,0.00053510873,0.00077332556,0.00038800068],"domain_scores_gemma":[0.99895966,0.00024007789,0.00018026445,0.0003553237,0.000054000895,0.00021067755],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002822244,0.00020895922,0.00060564035,0.0005786478,0.00017174795,0.00002003902,0.00033143564,0.000089074696,0.0040317182],"category_scores_gemma":[0.00008212944,0.0002125668,0.00006158624,0.000251792,0.000115616254,0.00013260284,0.00018573276,0.000309909,0.000010002999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029027846,0.00005016767,0.99581814,0.00041430106,0.00011134137,0.000694623,0.0011965461,0.000048806618,0.000001937167,0.0000056059107,0.0012105585,0.00015766692],"study_design_scores_gemma":[0.0013303595,0.00016710152,0.9961109,0.0006496716,0.000033317814,0.0000012708896,0.00032203257,0.00005845698,7.784326e-7,0.00011100722,0.0010289883,0.00018612],"about_ca_topic_score_codex":0.9956534,"about_ca_topic_score_gemma":0.9998299,"teacher_disagreement_score":0.017306425,"about_ca_system_score_codex":0.000118780146,"about_ca_system_score_gemma":0.0006336929,"threshold_uncertainty_score":0.99687874},"labels":[],"label_agreement":null},{"id":"W7073701879","doi":"","title":"Date of Service Provision and Date of Payment in Claims Data: Dealing with Time Differences","year":2020,"lang":"en","type":"article","venue":"Kölner Universitäts PublikationsServer (Universität zu Köln)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Medical prescription; Payment; Quarter (Canadian coin); Service (business); Statutory law; Health care; Payment by Results; Inpatient care","score_opus":0.025913000490970454,"score_gpt":0.18117543740988765,"score_spread":0.1552624369189172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073701879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923833,0.00008202496,0.00026989245,0.0028777195,0.000056197114,0.00030370496,0.0007886654,0.000033347584,0.003205161],"genre_scores_gemma":[0.99726105,0.000055230423,0.0014950745,0.000111355,0.000022595852,1.4366445e-7,0.00089780625,0.000005883966,0.0001508421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99862933,0.00009967686,0.00024023368,0.00046428235,0.00033097854,0.00023548039],"domain_scores_gemma":[0.99894637,0.00008735684,0.00027068728,0.00038529502,0.00014325448,0.0001670271],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020812423,0.00018662994,0.0003653043,0.00022264874,0.00014300006,0.000059541788,0.0007022497,0.000076415556,0.00095666345],"category_scores_gemma":[0.000009291251,0.00016702393,0.000026978027,0.0007661739,0.000105586034,0.0040700315,0.00024351628,0.00010818071,0.000026930804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0048854337,0.00083889975,0.72074753,0.0031343515,0.0021590472,0.00052127114,0.027882926,0.029839614,0.022589935,0.15230365,0.0024444612,0.032652877],"study_design_scores_gemma":[0.007631467,0.0014370969,0.8415495,0.000583744,0.00090700324,0.000012193824,0.011384826,0.109661154,0.0020669217,0.001026978,0.022096045,0.0016430282],"about_ca_topic_score_codex":0.00415604,"about_ca_topic_score_gemma":0.00253018,"teacher_disagreement_score":0.15127666,"about_ca_system_score_codex":0.000002861928,"about_ca_system_score_gemma":0.00011605981,"threshold_uncertainty_score":0.9999566},"labels":[],"label_agreement":null},{"id":"W7073703442","doi":"","title":"Astragalus-containing Chinese herbal combinations for advanced non-small-cell lung cancer: a meta-analysis of 65 clinical trials enrolling 4751 patients","year":2010,"lang":"en","type":"article","venue":"Dove Medical Press (Taylor and Francis Group)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Clinical trial; Lung cancer; Randomized controlled trial; Psychological intervention; Relative risk; Alternative medicine; Confidence interval; Clinical research","score_opus":0.046112784030952855,"score_gpt":0.34291581979445984,"score_spread":0.296803035763507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073703442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9111597,0.002085452,0.08007818,0.00012859573,0.0023498342,0.0012282209,0.002473879,0.000033485358,0.0004626683],"genre_scores_gemma":[0.99778545,0.000016480637,0.001073478,0.00019595852,0.0003404144,0.000079303565,0.00049210043,0.000010867474,0.0000059250146],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9965893,0.00036674022,0.0014823412,0.00055497,0.0005992304,0.00040743794],"domain_scores_gemma":[0.9954596,0.0029257282,0.00065280934,0.00032612958,0.00020636215,0.0004293817],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0044797543,0.0003007906,0.0021808217,0.00011656959,0.00019311604,0.00008566295,0.00040905218,0.0002834933,0.0018834979],"category_scores_gemma":[0.001469352,0.00020034127,0.0009861938,0.00027907424,0.00016965847,0.0001963177,0.00004746911,0.00036747713,0.0000023835512],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016650374,0.0014518793,0.49579602,0.00070929667,0.051455166,0.000015086628,0.001740293,0.0040050354,0.0016004263,0.0006762054,0.00005905548,0.4408265],"study_design_scores_gemma":[0.007255399,0.0005452539,0.10676081,0.000003456337,0.047651015,4.9473016e-7,0.000050305447,0.8358567,0.00023307589,0.0006662811,0.00044559524,0.0005316675],"about_ca_topic_score_codex":0.002014773,"about_ca_topic_score_gemma":0.0025561159,"teacher_disagreement_score":0.8318516,"about_ca_system_score_codex":0.0000018550531,"about_ca_system_score_gemma":0.000009358506,"threshold_uncertainty_score":0.9990289},"labels":[],"label_agreement":null},{"id":"W7073708710","doi":"","title":"Recommendations for improved acute pain services: Canadian collaborative acute pain initiative.","year":2004,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Acute pain; Multidisciplinary approach; Pain management; Acute care; Acute hospital; MEDLINE; Outcome (game theory); Epidemiology; Acute stroke","score_opus":0.01193119460286485,"score_gpt":0.20598292208595956,"score_spread":0.1940517274830947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073708710","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.27446768,0.00036769855,0.004049952,0.041317586,0.0015946482,0.0042686234,0.6510649,0.00084514497,0.022023806],"genre_scores_gemma":[0.9356954,0.00005918028,0.007400308,0.012327931,0.00037587003,0.00005736782,0.043544978,0.00005133182,0.0004876373],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980132,0.00023688245,0.00042564818,0.00047383428,0.00015965615,0.0006907967],"domain_scores_gemma":[0.99847,0.00034136765,0.00017654813,0.0002848178,0.00010269333,0.00062457955],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00062727917,0.00033860514,0.0003467717,0.00016572047,0.00046979295,0.0017798196,0.00050248083,0.00016766613,0.0012201394],"category_scores_gemma":[0.000114564245,0.00030094403,0.0001199367,0.00055142783,0.00006638535,0.0037722506,0.000035074798,0.00019930494,0.0008558553],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004812481,0.001721835,0.25003767,0.0019915074,0.010058232,0.0009820742,0.007003927,0.0019789983,0.006372627,0.030039918,0.23099807,0.45400268],"study_design_scores_gemma":[0.0012985271,0.00055877905,0.0030914869,0.00012361005,0.00009780283,0.0000043042332,0.00027211587,0.00059844804,0.0017747971,0.04897828,0.9423842,0.00081768364],"about_ca_topic_score_codex":0.0029987148,"about_ca_topic_score_gemma":0.01269066,"teacher_disagreement_score":0.7113861,"about_ca_system_score_codex":0.000019468678,"about_ca_system_score_gemma":0.00062229304,"threshold_uncertainty_score":0.99994427},"labels":[],"label_agreement":null},{"id":"W7073710746","doi":"","title":"[Environment and the \"Health in All Policies\" approach-an overview].","year":2018,"lang":"en","type":"article","venue":"Data Archiving and Networked Services (DANS)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Public health; Joint (building); Global health; Quarter (Canadian coin); Burden of disease; Occupational safety and health","score_opus":0.04490880600083988,"score_gpt":0.2672907380918401,"score_spread":0.22238193209100024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073710746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99385667,0.0026411044,0.0001387365,0.00064059615,0.00016251554,0.00030404015,0.00070389034,0.000025941112,0.0015265194],"genre_scores_gemma":[0.99060476,0.0043793153,0.0009377518,0.0017190521,0.00047543438,0.0000023761668,0.0018408607,0.0000065804275,0.000033858923],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99848706,0.0003617342,0.00022961195,0.00041296467,0.00013480894,0.00037384883],"domain_scores_gemma":[0.99899864,0.00012278902,0.00009814258,0.0006353412,0.0000036844183,0.00014142987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011108234,0.00015650052,0.00025913634,0.00003065482,0.0002729199,0.00015167301,0.00066341815,0.000029296862,0.00004596029],"category_scores_gemma":[0.0000022487225,0.00009665714,0.000012613819,0.00007331817,0.00026177402,0.0002626806,0.00024292119,0.00009774049,0.000016042724],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022789536,0.00041008796,0.3850071,0.0017716546,0.0004896496,0.000019800045,0.15453589,0.010815334,0.00039968177,0.010211259,0.004207972,0.4298526],"study_design_scores_gemma":[0.0007600167,0.00015948074,0.61084837,0.0000799651,0.000030286988,0.000011782573,0.00068490824,0.3451842,0.0000024074516,0.003603066,0.03838909,0.00024644096],"about_ca_topic_score_codex":0.035615698,"about_ca_topic_score_gemma":0.017741086,"teacher_disagreement_score":0.42960617,"about_ca_system_score_codex":0.0000016449967,"about_ca_system_score_gemma":0.000013181918,"threshold_uncertainty_score":0.9899943},"labels":[],"label_agreement":null},{"id":"W7073716331","doi":"","title":"Insights into Canadians’ Perceptions of Service Dogs in Public Spaces","year":2023,"lang":"en","type":"article","venue":"University Library (University of Saskatchewan)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Perception; Service (business); Public health; Phase (matter); Public service; Qualitative research","score_opus":0.008262194862323349,"score_gpt":0.15375912300606256,"score_spread":0.1454969281437392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073716331","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924815,0.000019231473,0.000013916286,0.0023316373,0.00011280048,0.00010466324,0.0002676311,0.00007021664,0.0045983954],"genre_scores_gemma":[0.996354,0.00007974662,0.0005091089,0.000052454343,0.000019629788,6.5742016e-9,0.00032331585,0.0000034316715,0.0026583401],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99919677,0.000096532225,0.00009328168,0.00022686682,0.0001648801,0.00022167171],"domain_scores_gemma":[0.9994197,0.00006791774,0.00009491748,0.00020466662,0.00004317776,0.0001696254],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00005614161,0.00010979473,0.00024542073,0.0005325865,0.00018689872,0.000019624258,0.00053478405,0.0001032691,0.0025976517],"category_scores_gemma":[0.0000026067348,0.00013717478,0.00006751921,0.0014393841,0.00015480943,0.0015358188,0.000102649305,0.00009079597,0.00019987737],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024994276,0.00012416486,0.78968036,0.0004482991,0.00017896743,0.00052105123,0.19108707,0.0029892798,0.0039128833,0.0023316632,0.005243081,0.0032332437],"study_design_scores_gemma":[0.00062300917,0.00007033769,0.7279252,0.000049957194,0.0000319881,6.8555073e-7,0.25188404,0.00082851714,0.000099870034,0.0016581756,0.016572658,0.00025556312],"about_ca_topic_score_codex":0.3169653,"about_ca_topic_score_gemma":0.52310747,"teacher_disagreement_score":0.20614217,"about_ca_system_score_codex":0.000008024035,"about_ca_system_score_gemma":0.00033274706,"threshold_uncertainty_score":0.9983141},"labels":[],"label_agreement":null},{"id":"W7073722799","doi":"","title":"INFORMAS (International Network for Food and Obesity/non-communicable diseases Research, Monitoring and Action Support): overview and key principles","year":2013,"lang":"en","type":"article","venue":"Research Online (University of Wollongong)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Accountability; Benchmarking; Key (lock); Food safety; Action (physics); Private sector; Food supply; Monitoring and evaluation","score_opus":0.12310204083694036,"score_gpt":0.3317379305760578,"score_spread":0.20863588973911745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073722799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970184,0.000883609,0.000013169305,0.00066749094,0.00008595446,0.0004454242,0.0004360371,0.00001261516,0.00043728983],"genre_scores_gemma":[0.9889825,0.0073838257,0.0023510836,0.0000047353565,0.00018764105,0.0000010091707,0.00016345983,0.000003829296,0.0009219442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875945,0.0001401224,0.000113813,0.00020440463,0.00040643994,0.0003757518],"domain_scores_gemma":[0.9987945,0.00043282617,0.00005824877,0.00018305282,0.00030855305,0.0002228443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008723679,0.00008533449,0.00020206562,0.00015767384,0.0006279906,0.00014133702,0.00029073592,0.00006453833,0.00023295778],"category_scores_gemma":[0.00009869355,0.00008580005,0.000029847237,0.0001796869,0.0003163057,0.00076032436,0.00029447192,0.0001856229,0.000008554616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062984484,0.0002664163,0.9220486,0.0014507244,0.0004165593,0.000016720036,0.0027795583,0.00060431,0.0012933939,0.0027244065,0.007776343,0.05999307],"study_design_scores_gemma":[0.0005399298,0.00045962792,0.96201926,0.00012172959,0.000016927374,0.000002957813,0.0022160416,0.00503335,0.000059534344,0.001806983,0.027600508,0.00012314387],"about_ca_topic_score_codex":0.0058805854,"about_ca_topic_score_gemma":0.00370552,"teacher_disagreement_score":0.059869926,"about_ca_system_score_codex":0.000007896978,"about_ca_system_score_gemma":0.00007500775,"threshold_uncertainty_score":0.8889725},"labels":[],"label_agreement":null},{"id":"W7073726977","doi":"","title":"A neonatal pneumococcal conjugate vaccine trial in Papua New Guinea: study population, methods and operational challenges","year":2010,"lang":"en","type":"article","venue":"UWA Profiles and Research Repository (UWA)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centre for Global Health Research","funders":"","keywords":"Pneumococcal conjugate vaccine; Pneumococcal vaccine; Pneumococcal disease; Vaccination; Clinical trial; Pandemic","score_opus":0.04338705817725534,"score_gpt":0.3569860263572188,"score_spread":0.31359896817996347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073726977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99554116,0.0011752689,0.0000052077175,0.0006889745,0.0008267781,0.0011505325,0.000025372568,0.000021963573,0.00056471775],"genre_scores_gemma":[0.99631786,0.0002003107,0.0013561302,0.000010944222,0.0012507846,0.000027911256,0.00005975667,0.000007744274,0.00076854613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974824,0.00077006326,0.00039302546,0.00051343534,0.00046038692,0.00038066757],"domain_scores_gemma":[0.9989378,0.0003633515,0.00006894373,0.00024815212,0.00012078261,0.00026100955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023307765,0.00017122675,0.0003273649,0.00015334561,0.00045114296,0.00031823295,0.00019366964,0.00013217152,0.00018434544],"category_scores_gemma":[0.00017523945,0.00012563671,0.000029681698,0.00014037406,0.00009020715,0.0002923714,0.00008825621,0.00041617587,0.000009490668],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.014642976,0.00084672234,0.46776095,0.0004743673,0.00033113462,0.0005314274,0.008932879,0.00013770026,0.31773993,0.008039584,0.0014677763,0.17909455],"study_design_scores_gemma":[0.00794999,0.0012046474,0.96703887,0.000027552556,0.000017479828,0.00004195901,0.00062011305,0.0011392403,0.014090764,0.0016891501,0.005917931,0.00026228666],"about_ca_topic_score_codex":0.007481542,"about_ca_topic_score_gemma":0.0004474569,"teacher_disagreement_score":0.49927795,"about_ca_system_score_codex":0.00000335342,"about_ca_system_score_gemma":0.00012411515,"threshold_uncertainty_score":0.99912775},"labels":[],"label_agreement":null},{"id":"W7073730451","doi":"","title":"Bisphosphonates and cancer:More data using same database","year":2010,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute of Population and Public Health","funders":"","keywords":"MEDLINE; Patient data; Key (lock); Work (physics)","score_opus":0.03455599284424942,"score_gpt":0.2741943430688166,"score_spread":0.2396383502245672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073730451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995442,0.00040441303,0.00002257471,0.00022934342,0.0008801034,0.00007095766,0.0023935528,0.000027742308,0.0005293482],"genre_scores_gemma":[0.99252677,0.00017493496,0.0057607666,0.00028383482,0.00021253481,3.0003102e-7,0.0007387362,0.000003225668,0.0002989192],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993578,0.000010482656,0.00009480161,0.00025786334,0.000106167514,0.00017283681],"domain_scores_gemma":[0.99939364,0.000044653745,0.000033280317,0.00041544822,0.00001631552,0.00009665521],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016041519,0.00008591878,0.00011113284,0.000018256596,0.000106007305,0.00010330395,0.0002803933,0.000033957487,0.0058038738],"category_scores_gemma":[0.000018820185,0.0000618802,0.000007060683,0.000060879727,0.00007236886,0.00038081894,0.00008062724,0.00007246306,0.00004398253],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000942417,0.000048862425,0.46769223,0.00016081361,0.00011204801,0.000057309928,0.000400247,0.00037670764,0.36159107,0.0018379138,0.016213294,0.15141526],"study_design_scores_gemma":[0.0009061044,0.000061173705,0.40216538,0.000059097918,0.00015844844,0.000047841135,0.00023217933,0.12758042,0.038765877,0.0016772932,0.42725304,0.0010931293],"about_ca_topic_score_codex":0.08443072,"about_ca_topic_score_gemma":0.019443642,"teacher_disagreement_score":0.41103974,"about_ca_system_score_codex":2.7506368e-7,"about_ca_system_score_gemma":0.00004031015,"threshold_uncertainty_score":0.99844897},"labels":[],"label_agreement":null},{"id":"W7073732984","doi":"","title":"ATP1A2- and ATP1A3-associated early profound epileptic encephalopathy and polymicrogyria","year":2021,"lang":"en","type":"article","venue":"University of Southern Denmark Research Portal (University of Southern Denmark)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Hospital for Sick Children","funders":"","keywords":"Polymicrogyria; Epilepsy; Encephalopathy; Disease; Central nervous system disease","score_opus":0.01659223611714569,"score_gpt":0.2060241987498724,"score_spread":0.1894319626327267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073732984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98882324,0.0005721637,0.000022941964,0.00013861922,0.00006652595,0.00027173455,0.0022161112,0.000025014502,0.007863624],"genre_scores_gemma":[0.9895772,0.0003229763,0.00036940275,0.00000892738,0.0000349568,2.997287e-8,0.00010138779,0.000012421897,0.0095727015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972899,0.00052792433,0.00021091131,0.00061330444,0.00074946706,0.0006085083],"domain_scores_gemma":[0.9982309,0.0002937218,0.00027188772,0.00036546084,0.0004734763,0.00036458706],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010711777,0.00023884709,0.0005366519,0.00026216783,0.0006980854,0.00006988726,0.00051599374,0.00025170762,0.011218547],"category_scores_gemma":[0.00009095354,0.00028702014,0.00014245385,0.0005339356,0.0013490039,0.00026098036,0.00030912407,0.00034682147,0.00064209313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011445504,0.00031550069,0.9258847,0.00041645975,0.0008242589,0.002281521,0.041943084,0.00002289521,0.01603359,0.00037493467,0.001098074,0.009660429],"study_design_scores_gemma":[0.004652092,0.00077886565,0.6534843,0.00050252106,0.0004411698,0.0000777131,0.3314643,0.0005549121,0.0005503273,0.002890409,0.00346348,0.0011399264],"about_ca_topic_score_codex":0.016397092,"about_ca_topic_score_gemma":0.01418909,"teacher_disagreement_score":0.2895212,"about_ca_system_score_codex":0.000012167702,"about_ca_system_score_gemma":0.00027525093,"threshold_uncertainty_score":0.9999582},"labels":[],"label_agreement":null},{"id":"W7073737335","doi":"","title":"Contribution of the PALB2 c.2323C>T [p.Q775X] founder mutation in well-defined breast and/or ovarian cancer families and unselected ovarian cancer cases of French Canadian descent.","year":2013,"lang":"en","type":"article","venue":"Apollo (University of Cambridge)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"PALB2; Ovarian cancer; Breast cancer; Serous fluid; BRCA mutation; Cancer; Founder effect","score_opus":0.006900293882102506,"score_gpt":0.17747471367892223,"score_spread":0.17057441979681973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073737335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975315,0.00018303272,0.000024403782,0.000678783,0.00013425478,0.00028264723,0.0009268612,0.000005151167,0.00023341338],"genre_scores_gemma":[0.9993703,0.000212673,0.000061803104,0.000036680864,0.0000176785,3.827062e-7,0.00007087008,0.0000024346891,0.00022722367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992851,0.00008231265,0.00014076535,0.0001588638,0.00013308556,0.00019985672],"domain_scores_gemma":[0.9994002,0.00007423014,0.00015829693,0.00010913945,0.00016291958,0.000095215764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009427313,0.00010056216,0.00023873064,0.0001100263,0.00012509589,0.000016529546,0.0001174122,0.00007291803,0.0005462449],"category_scores_gemma":[0.000017362949,0.00008467785,0.000029225104,0.0002785842,0.00016675453,0.00021533604,0.000015519308,0.000053294774,0.0000026540695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025232174,0.000039313836,0.97772497,0.00017284238,0.00016633245,0.000022198703,0.0020199432,0.00043260658,0.0059492695,0.0012278967,0.0012884886,0.010703811],"study_design_scores_gemma":[0.00076696096,0.000046820085,0.9967325,0.00007112292,0.000057158526,0.000009559299,0.0004986313,0.0009212293,0.0004268219,0.000071757815,0.00029855152,0.00009891596],"about_ca_topic_score_codex":0.9754981,"about_ca_topic_score_gemma":0.90707207,"teacher_disagreement_score":0.068426,"about_ca_system_score_codex":0.000016725045,"about_ca_system_score_gemma":0.00027976563,"threshold_uncertainty_score":0.5980999},"labels":[],"label_agreement":null},{"id":"W7073738924","doi":"","title":"HLA-DQA1-HLA-DRB1 polymorphism is a major predictor of azathioprine-induced pancreatitis in patients with inflammatory bowel disease","year":2018,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Inflammatory bowel disease; Azathioprine; Thiopurine methyltransferase; Pancreatitis; Genotype; Crohn's disease; Single-nucleotide polymorphism; Pharmacogenomics; Autoimmune pancreatitis","score_opus":0.02156305498909346,"score_gpt":0.22633073456665084,"score_spread":0.20476767957755737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073738924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981814,0.000030226793,0.00001168971,0.000051385203,0.0003489157,0.0004652844,0.00066489907,0.00006766791,0.00017851012],"genre_scores_gemma":[0.99869055,0.000013067782,0.000025572323,0.00014435606,0.0001571201,7.731516e-7,0.00012872649,0.000019929308,0.0008199078],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977398,0.00020373335,0.0003567787,0.00058670226,0.0005780841,0.00053490285],"domain_scores_gemma":[0.99842507,0.000053567717,0.0002981148,0.00059830915,0.00020240109,0.0004225363],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00021511265,0.00035064758,0.00041332547,0.00039795216,0.00017193823,0.00012928847,0.0006718928,0.00015618069,0.00047525004],"category_scores_gemma":[0.000022667435,0.000328362,0.00008869054,0.00038862746,0.00021400549,0.0013636191,0.00012347006,0.00023354353,0.0002651119],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007381533,0.00008755495,0.998145,0.00008751374,0.000066981454,0.00014908044,0.00034917018,0.0000111626605,0.00019729258,0.000019299752,0.0000014448542,0.00014738397],"study_design_scores_gemma":[0.0021746187,0.0004388036,0.9951347,0.00024196276,0.00010067362,0.0000017488908,0.00003058321,0.0000018057383,0.0011488931,0.000065475906,0.00027662955,0.00038408945],"about_ca_topic_score_codex":0.00018922282,"about_ca_topic_score_gemma":0.0035749436,"teacher_disagreement_score":0.0033857208,"about_ca_system_score_codex":0.000025476673,"about_ca_system_score_gemma":0.00017294392,"threshold_uncertainty_score":0.99991685},"labels":[],"label_agreement":null},{"id":"W7073755102","doi":"","title":"Photoanode development for photoelectrochemical water splitting","year":2020,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Water splitting; Photocathode; Photocurrent; Photoelectrochemical cell; Photoelectrochemistry; Oxygen evolution; Polarization (electrochemistry); Reversible hydrogen electrode","score_opus":0.009566652240516633,"score_gpt":0.15344555880195798,"score_spread":0.14387890656144134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073755102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980397,0.000027105483,0.0007538277,0.00009660454,0.00007243957,0.00019899821,0.00018825954,0.000038229384,0.00058483984],"genre_scores_gemma":[0.99733526,0.000006627062,0.002158089,0.000121419864,0.000058099507,1.980413e-7,0.0001775852,0.0000035169326,0.00013918277],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9992519,0.000015544781,0.0000977353,0.00025410575,0.00012723678,0.00025350365],"domain_scores_gemma":[0.99967843,0.00002487456,0.00004451906,0.00007085254,0.000057832553,0.00012347814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000099105586,0.000034312325,0.00018530026,0.000008091926,0.0001768695,0.00006830345,0.00020852276,0.000052369847,0.0007991481],"category_scores_gemma":[0.0000104793935,0.00009183268,0.000059952938,0.00005827593,0.00005249583,0.00012373079,0.000028036424,0.0000458777,0.00007065042],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021200338,0.000104330866,0.02697082,0.0007486748,0.00022536691,0.00013902991,0.002978958,0.000114246155,0.27484408,0.0000027429135,0.01194477,0.68171495],"study_design_scores_gemma":[0.0014488751,0.00019559906,0.96026987,0.00006756757,0.00005614681,0.00001363842,0.0004934418,0.0016735005,0.007548576,0.00039929192,0.027373852,0.00045963807],"about_ca_topic_score_codex":0.023808593,"about_ca_topic_score_gemma":0.034828864,"teacher_disagreement_score":0.93329906,"about_ca_system_score_codex":0.0000034242344,"about_ca_system_score_gemma":0.000042162214,"threshold_uncertainty_score":0.982783},"labels":[],"label_agreement":null},{"id":"W7073757376","doi":"","title":"The health outcomes and physical activity in preschoolers (HOPP) study: rationale and design","year":2012,"lang":"en","type":"article","venue":"Queensland's institutional digital repository (The University of Queensland)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Physical activity; Overweight; Test (biology); Quality of life (healthcare); Cohort; Early childhood; Waist; Physical activity level; Motor activity; Child development","score_opus":0.017844187026561292,"score_gpt":0.2162927601815294,"score_spread":0.1984485731549681,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073757376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99695504,0.00018478981,0.00021245617,0.00037826857,0.00017622439,0.00043649581,0.00007734214,0.0000136724075,0.0015656942],"genre_scores_gemma":[0.9994583,0.000036716498,0.000046593406,0.000018464747,0.00007502206,5.089499e-7,0.000012793818,0.0000019882243,0.00034960586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903256,0.00018550044,0.00012587482,0.00017421343,0.0002634357,0.0002184068],"domain_scores_gemma":[0.9991592,0.00043486708,0.000116414805,0.00014007324,0.00003513898,0.00011426525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030908285,0.00012632477,0.00021621225,0.000037288915,0.0007111128,0.000092679504,0.0001336039,0.000034057564,0.0000060650973],"category_scores_gemma":[0.000036019854,0.00008042188,0.000041477044,0.00007355052,0.00039669668,0.00060970057,0.00004522196,0.00011100187,0.000008999484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032537107,0.00018470806,0.99008495,0.000019877589,0.00008129252,0.00001130964,0.0018237473,0.0008926992,0.0000341588,0.0012451579,0.00038033383,0.004916378],"study_design_scores_gemma":[0.00049596524,0.00012958916,0.99460655,0.000014267589,0.000015904692,0.000011782819,0.00052135624,0.0004841152,0.00001864015,0.0003117214,0.0032894195,0.0001006711],"about_ca_topic_score_codex":0.0026905986,"about_ca_topic_score_gemma":0.0004977749,"teacher_disagreement_score":0.004815707,"about_ca_system_score_codex":0.000012466133,"about_ca_system_score_gemma":0.00012369615,"threshold_uncertainty_score":0.54693764},"labels":[],"label_agreement":null},{"id":"W7073758995","doi":"","title":"An analytical approach to study educational inequalities: 10 hypothesis tests in PIRLS 2006","year":2012,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Diafiltration; Hyporeflexia; Dysgeusia; Proteogenomics; Liquation","score_opus":0.05468763972040508,"score_gpt":0.2766725516507347,"score_spread":0.2219849119303296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073758995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94317317,0.000012785459,0.00039585656,0.00025073148,0.000060586393,0.00058826717,0.0007655047,0.00002264193,0.054730434],"genre_scores_gemma":[0.99109596,0.00003757602,0.005618899,0.000017495915,0.00010000715,2.075576e-7,0.00021137205,0.00000698031,0.0029114739],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99679595,0.0009270667,0.00017175723,0.00047896293,0.00076611456,0.0008601698],"domain_scores_gemma":[0.99789983,0.000672185,0.00008438614,0.0004825401,0.00019345904,0.00066760625],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014697711,0.00019615491,0.0003910603,0.0009318575,0.0005363069,0.00004897944,0.0011653799,0.0000838503,0.0025583815],"category_scores_gemma":[0.00011540825,0.00022620814,0.00009391264,0.0010740715,0.00035908428,0.0009356634,0.00023733643,0.00029787733,0.00009654941],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013156177,0.0026894412,0.9638632,0.00008976867,0.00015733851,0.00004609832,0.013367706,0.0011079208,0.00023206093,0.007602306,0.003586476,0.0059420574],"study_design_scores_gemma":[0.00079481304,0.00064942765,0.9436901,0.000018075852,0.000036370286,0.0000023026796,0.023729876,0.0011890581,0.000009925795,0.0011358457,0.0284599,0.00028428185],"about_ca_topic_score_codex":0.010287027,"about_ca_topic_score_gemma":0.00497753,"teacher_disagreement_score":0.05181896,"about_ca_system_score_codex":0.00004472532,"about_ca_system_score_gemma":0.00026639563,"threshold_uncertainty_score":0.9983534},"labels":[],"label_agreement":null},{"id":"W7073759164","doi":"","title":"TOWARDS A RADIOCARBON CALIBRATION FOR OXYGEN ISOTOPE STAGE 3 USING NEW ZEALAND KAURI (AGATHIS AUSTRALIS)","year":2010,"lang":"en","type":"article","venue":"Research Commons (University of Waikato)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Queen's University; University of Wollongong","keywords":"Radiocarbon dating; Calibration curve; Subfossil; Calibration; Holocene; Stage (stratigraphy); Measure (data warehouse); Isotopes of oxygen","score_opus":0.06717132198228806,"score_gpt":0.2909221223064517,"score_spread":0.22375080032416364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073759164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99556583,0.000030415056,0.0005028384,0.001184381,0.00019421181,0.00042495684,0.00052784325,0.00002486117,0.0015446804],"genre_scores_gemma":[0.9896234,0.000025566931,0.0054199398,0.000010081762,0.00015603889,1.4587246e-7,0.0001469297,0.0000056600743,0.004612203],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986736,0.00015013332,0.0001160271,0.00023972355,0.00042270627,0.00039780652],"domain_scores_gemma":[0.99902016,0.00019533202,0.00007382239,0.00031093362,0.00014424606,0.00025549295],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00084956514,0.00010295738,0.0002260472,0.00019166843,0.00038664276,0.00008629872,0.00046755307,0.00012600662,0.0019086219],"category_scores_gemma":[0.00006337706,0.00010849996,0.000080912905,0.00031632258,0.00018997498,0.00039539425,0.00006329164,0.00025179578,0.000023157096],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0032054028,0.00048937334,0.13931891,0.0009063411,0.0007431614,0.00027188525,0.016085746,0.0067479042,0.58158785,0.025719536,0.16240817,0.062515706],"study_design_scores_gemma":[0.0051673916,0.0013746542,0.24004856,0.00014692788,0.00017631498,0.000021071659,0.0025810755,0.092396,0.024473919,0.014325152,0.6180868,0.0012021292],"about_ca_topic_score_codex":0.08775167,"about_ca_topic_score_gemma":0.028084856,"teacher_disagreement_score":0.55711395,"about_ca_system_score_codex":0.000008106839,"about_ca_system_score_gemma":0.0003383838,"threshold_uncertainty_score":0.99900377},"labels":[],"label_agreement":null},{"id":"W7073764301","doi":"","title":"Characteristics of high-quality guidelines: evaluation of 86 clinical guidelines developed in ten European countries and Canada.","year":2003,"lang":"en","type":"article","venue":"Explore Bristol Research","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Guideline; Agency (philosophy); Scope (computer science); Quality (philosophy); Clinical Practice; Quality assurance","score_opus":0.4139184831209174,"score_gpt":0.4648083088601124,"score_spread":0.05088982573919498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073764301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99743384,0.0004581327,0.000018082945,0.00037990845,0.0003114835,0.00027788203,0.00029141878,0.0000048703278,0.00082440465],"genre_scores_gemma":[0.9979563,0.0006278539,0.0009815001,0.000074387826,0.0001240099,0.000002851692,0.00012233651,0.000006294756,0.00010449903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99421245,0.0023786423,0.0013988811,0.00029712636,0.0014158105,0.00029710963],"domain_scores_gemma":[0.99601394,0.00056293793,0.00025734951,0.00028464678,0.002769942,0.00011117803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.021031456,0.00011323158,0.00042765302,0.00010251117,0.00007965303,0.000034444733,0.0002388076,0.000049776467,0.00024751297],"category_scores_gemma":[0.00807527,0.00009389662,0.000023566545,0.00023046554,0.00022298265,0.00010967268,0.00003898821,0.00014400108,0.000014851798],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002821858,0.000076852266,0.8819236,0.00028916803,0.00005953135,0.00003227035,0.0004942115,0.0002362174,0.00042948037,0.0008822924,0.02944117,0.08585301],"study_design_scores_gemma":[0.0005323176,0.000072174786,0.9721446,0.00008107715,0.000013932891,0.0000014539349,0.00023664098,0.00024467878,0.0006660041,0.00083079987,0.025044817,0.0001315224],"about_ca_topic_score_codex":0.48510224,"about_ca_topic_score_gemma":0.4214864,"teacher_disagreement_score":0.090220965,"about_ca_system_score_codex":0.000013984688,"about_ca_system_score_gemma":0.001642546,"threshold_uncertainty_score":0.9667436},"labels":[],"label_agreement":null},{"id":"W7073767334","doi":"","title":"Guidelines for Evaluating Artificial Light to Mitigate Unwanted Fisheries Bycatch","year":2024,"lang":"en","type":"article","venue":"Technical University of Denmark, DTU Orbit (Technical University of Denmark, DTU)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"International Council for the Exploration of the Sea","keywords":"Bycatch; Fishing; Artificial light; Work (physics)","score_opus":0.054090670955291485,"score_gpt":0.2766829525874307,"score_spread":0.2225922816321392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073767334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90144557,0.0011459455,0.042278267,0.019094026,0.0015411435,0.0035014045,0.0032503444,0.0010039231,0.02673939],"genre_scores_gemma":[0.966211,0.00019683216,0.028660951,0.0001146404,0.00016722803,4.374695e-7,0.00014722791,0.000026014639,0.0044756327],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9966559,0.00020104939,0.0006674883,0.0009694815,0.0008004292,0.00070565485],"domain_scores_gemma":[0.9970521,0.0007477607,0.00030328459,0.0006793414,0.0007890333,0.00042848758],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012717403,0.00043776442,0.0009616237,0.00039608515,0.00048009545,0.00008290436,0.0014773346,0.0005246747,0.003451316],"category_scores_gemma":[0.00052063656,0.00048371617,0.0005639747,0.0010762963,0.00060603267,0.0004953387,0.00038661432,0.0004038972,0.00039238913],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00801609,0.0008503876,0.0033612086,0.0022252898,0.0011912716,0.0010411702,0.0013388479,0.0027856114,0.50597334,0.012531187,0.38862187,0.07206375],"study_design_scores_gemma":[0.0047394214,0.0063039125,0.0524499,0.003539576,0.0028957578,0.00016402222,0.0043934477,0.019825995,0.034966324,0.024480402,0.8416599,0.004581317],"about_ca_topic_score_codex":0.0018048115,"about_ca_topic_score_gemma":0.004161891,"teacher_disagreement_score":0.47100702,"about_ca_system_score_codex":0.00006057295,"about_ca_system_score_gemma":0.00038130753,"threshold_uncertainty_score":0.99976146},"labels":[],"label_agreement":null},{"id":"W7073767712","doi":"","title":"Staff, space, and time as dimensions of organizational slack: A psychometric assessment","year":2011,"lang":"en","type":"preprint","venue":"UVic’s Research and Learning Repository (University of Victoria)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Variance (accounting); Bivariate analysis; Reliability (semiconductor); Context (archaeology); Psychometrics; Measure (data warehouse); Organizational commitment; Health care; Likert scale","score_opus":0.021368485868128555,"score_gpt":0.2526798206816068,"score_spread":0.23131133481347826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073767712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9789891,0.0005210361,0.00004479119,0.00007006023,0.0004231024,0.00025889318,0.00007061416,0.000026835289,0.01959552],"genre_scores_gemma":[0.9922422,0.00071812264,0.0011455631,0.000001149441,0.0001347906,1.6534986e-7,0.00012997427,0.000007892973,0.005620152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978687,0.0005036743,0.0001827875,0.00046530372,0.00069563056,0.00028391086],"domain_scores_gemma":[0.99833995,0.00035356748,0.00025556376,0.00027185434,0.0005364547,0.00024259725],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00082433503,0.00016544001,0.00041570168,0.00043519854,0.0005697247,0.000082239625,0.00030271322,0.00022807994,0.001369267],"category_scores_gemma":[0.00010541721,0.00016144752,0.00005222567,0.00044036622,0.00037459872,0.00012984485,0.00034083295,0.0007030109,0.000038837476],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016890687,0.0010837482,0.8737185,0.0031432991,0.0020377103,0.0003403713,0.017339937,0.0030272908,0.07176628,0.011282707,0.009460136,0.0051109465],"study_design_scores_gemma":[0.001765464,0.0039660507,0.92449456,0.00063782017,0.00026455594,0.000038097056,0.003307873,0.0036113018,0.0012069651,0.014304941,0.045406092,0.0009962752],"about_ca_topic_score_codex":0.0058472594,"about_ca_topic_score_gemma":0.00005318881,"teacher_disagreement_score":0.070559315,"about_ca_system_score_codex":0.000012291863,"about_ca_system_score_gemma":0.00034775594,"threshold_uncertainty_score":0.9995436},"labels":[],"label_agreement":null},{"id":"W7073770411","doi":"","title":"Mass schooling, empowerment, and demographc and economic outcomes: a note of dissent. Vienna Yearbook of Population Research|Vienna Yearbook of Population Research 2010 8|","year":2010,"lang":"en","type":"other","venue":"Oesterreichisches Musiklexikon online (Institut für kunst- und musikhistorische Forschungen der  Österreichischen Akademie der Wissenschaften)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mantra; Yearbook; Population; Subject (documents); Quarter (Canadian coin); Lament","score_opus":0.036488577306846806,"score_gpt":0.35201510686402465,"score_spread":0.31552652955717786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073770411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9162165,0.025196565,0.00015552832,0.00050300825,0.0058723944,0.0049078693,0.0031651412,0.00025620093,0.043726776],"genre_scores_gemma":[0.94361097,0.0023984679,0.014100325,0.000095926196,0.0019919586,0.000063457526,0.0033448413,0.0005487731,0.033845276],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9911162,0.0010018939,0.0025774403,0.0019710327,0.0018315625,0.001501819],"domain_scores_gemma":[0.9941878,0.0005890515,0.0021133707,0.0018989302,0.0004003149,0.0008105539],"candidate_categories":["metaepi_narrow","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow","research_integrity"],"category_scores_codex":[0.0031619552,0.0013261137,0.0026727482,0.0027831385,0.00044907889,0.00017323502,0.0011947249,0.0018102353,0.001007923],"category_scores_gemma":[0.00040367251,0.0012169607,0.00049584924,0.0007357663,0.0017477528,0.0008466821,0.0004726872,0.0023896154,0.00008955527],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036850902,0.0020877572,0.7576728,0.01326182,0.008633827,0.00027261878,0.009620429,0.00082153577,0.1020816,0.007956601,0.056797583,0.03710836],"study_design_scores_gemma":[0.006217568,0.0017026826,0.3178902,0.0056018964,0.0033764383,0.000110610585,0.00082159037,0.0024335627,0.002450616,0.0034120632,0.65113264,0.004850149],"about_ca_topic_score_codex":0.046063,"about_ca_topic_score_gemma":0.042692106,"teacher_disagreement_score":0.594335,"about_ca_system_score_codex":0.00009494717,"about_ca_system_score_gemma":0.00047766275,"threshold_uncertainty_score":0.99994904},"labels":[],"label_agreement":null},{"id":"W7073772168","doi":"","title":"Impact of nonoptimal intakes of saturated, polyunsaturated, and trans fat on global burdens of coronary heart disease","year":2016,"lang":"en","type":"article","venue":"Dépôt institutionnel de l'Université libre de Bruxelles (Université Libre de Bruxelles)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Coronary heart disease; Trans fat; Proportional hazards model; Polyunsaturated fat; Polyunsaturated fatty acid; Prospective cohort study; Risk assessment","score_opus":0.007048828565205768,"score_gpt":0.19278924673161035,"score_spread":0.18574041816640458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073772168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914888,0.00091242435,0.0012142272,0.00055157335,0.00016776158,0.0003179544,0.003909848,0.000076925804,0.0013604857],"genre_scores_gemma":[0.99791014,0.0007327819,0.0007895394,0.00006502295,0.0000857904,4.284386e-7,0.00016190596,0.000014376315,0.00024002929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979176,0.00021090887,0.00038434696,0.0005021438,0.0003609433,0.00062406407],"domain_scores_gemma":[0.9983197,0.00019364014,0.0003371425,0.00042042113,0.00016587214,0.000563232],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00016122966,0.00042554506,0.0006353734,0.0002702134,0.0002935975,0.00004051419,0.00061206106,0.000284986,0.0008070273],"category_scores_gemma":[0.000030343972,0.00035989608,0.00034317814,0.00057769165,0.00070234697,0.00085238606,0.00010091843,0.00016595364,0.00002356262],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.039918922,0.0009394571,0.70694524,0.00077861216,0.0015242705,0.0013657252,0.0064577577,0.045617305,0.1412909,0.017320951,0.008932782,0.028908083],"study_design_scores_gemma":[0.005027702,0.0009459155,0.98284906,0.00048580774,0.00032660688,0.00015132074,0.0014527625,0.0015633942,0.0039780145,0.000685477,0.0019584203,0.0005755406],"about_ca_topic_score_codex":0.0048163002,"about_ca_topic_score_gemma":0.00034919017,"teacher_disagreement_score":0.27590382,"about_ca_system_score_codex":0.00010592211,"about_ca_system_score_gemma":0.00066981086,"threshold_uncertainty_score":0.9998853},"labels":[],"label_agreement":null},{"id":"W7073774864","doi":"","title":"CCA Young Investigator Award","year":2010,"lang":"en","type":"article","venue":"Le dépôt institutionnel (Université du Québec à Trois-Rivières)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Chiropractic; Association (psychology); MEDLINE; Alternative medicine","score_opus":0.008366515341756215,"score_gpt":0.1726735219836592,"score_spread":0.16430700664190298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073774864","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9851258,0.00007798452,0.002028467,0.0032456643,0.0023852338,0.00023433942,0.00019766716,0.00021684726,0.00648802],"genre_scores_gemma":[0.9965344,0.000020573674,0.0007265128,0.00030471786,0.00065804506,0.0000022375264,0.00012725104,0.000010395246,0.0016158874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984054,0.00006912047,0.00024639152,0.00046779358,0.00033732594,0.00047397494],"domain_scores_gemma":[0.9987154,0.00007231215,0.00014608371,0.00046430496,0.00011158564,0.0004902891],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00022639666,0.0002859106,0.0003193035,0.00016106728,0.00095149095,0.00015510012,0.000636611,0.00017184032,0.0032461686],"category_scores_gemma":[0.00013054226,0.0002658288,0.00014273188,0.0003157071,0.00042025757,0.0009295237,0.00007220736,0.00032393282,0.0016044672],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038048634,0.00036406418,0.7806206,0.00019117566,0.00039767535,0.0006419837,0.011569084,0.022381408,0.042392567,0.10763697,0.023970082,0.009453947],"study_design_scores_gemma":[0.0023091359,0.00018552881,0.81510955,0.00004327489,0.00015472536,0.00014658786,0.0009883884,0.015737021,0.0029177787,0.0017900998,0.15946774,0.0011501644],"about_ca_topic_score_codex":0.5220673,"about_ca_topic_score_gemma":0.70585567,"teacher_disagreement_score":0.18378836,"about_ca_system_score_codex":0.000017984981,"about_ca_system_score_gemma":0.0007250665,"threshold_uncertainty_score":0.9999794},"labels":[],"label_agreement":null},{"id":"W7073780325","doi":"","title":"The role of SMEs in promoting sustainable procurement","year":2015,"lang":"en","type":"book-chapter","venue":"Research Publications (Maastricht University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Montreal Council on Foreign Relations","funders":"","keywords":"Procurement; Production (economics); Sustainability; Work (physics); Government (linguistics)","score_opus":0.04691914636703712,"score_gpt":0.2582870644307032,"score_spread":0.2113679180636661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073780325","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010544168,0.0010755601,0.000004344293,0.0006460502,0.000035662066,0.00089624815,0.00012943691,0.000029215496,0.9961291],"genre_scores_gemma":[0.11150828,0.00040305863,0.00007944932,0.0000014365011,0.00008716652,0.0000021227977,0.00019993864,0.00000863801,0.8877099],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981019,0.00014362029,0.00022161676,0.00029087262,0.00074113416,0.00050088164],"domain_scores_gemma":[0.9976812,0.00027736608,0.0001712378,0.00042346647,0.0012896719,0.0001570397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018101155,0.00013026272,0.00019576437,0.00094507285,0.00041074987,0.00015392428,0.00085308723,0.0001286274,0.0004322976],"category_scores_gemma":[0.00021547829,0.00010655079,0.000047630976,0.0007188396,0.00022752225,0.0003053381,0.00016145373,0.00035728674,0.00008710883],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038207872,0.000038368555,0.0017699157,0.00007661045,0.000067424946,0.000015780668,0.00023107431,0.000085182546,0.000035192326,0.9770865,0.007850998,0.012704733],"study_design_scores_gemma":[0.00012403923,0.000079291975,0.00093902857,0.000030344687,0.00001149198,5.832399e-7,0.00063310657,0.00010257517,0.00003432945,0.027721312,0.9702232,0.00010068133],"about_ca_topic_score_codex":0.0016428808,"about_ca_topic_score_gemma":0.0008279911,"teacher_disagreement_score":0.96237224,"about_ca_system_score_codex":0.00006596442,"about_ca_system_score_gemma":0.0010821536,"threshold_uncertainty_score":0.47333553},"labels":[],"label_agreement":null},{"id":"W7073782846","doi":"","title":"Myocardial perfusion grade after late infarct artery recanalization is associated with global and regional left ventricular function at one year: analysis from the Total Occlusion Study of Canada-2.","year":2010,"lang":"en","type":"article","venue":"The Institutional Repository of Hospital Prof. Dr. Fernando Fonseca (Hospital Prof. Dr. Fernando Fonseca)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ejection fraction; Myocardial infarction; Conventional PCI; Thrombolysis; Perfusion; Artery; Percutaneous coronary intervention; Ventricular function; Stroke volume; Occlusion","score_opus":0.004895068952413218,"score_gpt":0.17625229637731013,"score_spread":0.17135722742489692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073782846","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99265087,0.0005136686,0.000045212168,0.002207507,0.0019522979,0.0014874839,0.000880937,0.000036763708,0.00022524771],"genre_scores_gemma":[0.99837947,0.000034540328,0.000013524322,0.000080768186,0.00036936515,0.000024308842,0.00041107723,0.00001567312,0.0006712775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99582785,0.00037086412,0.00083944475,0.0007262466,0.0017498509,0.00048574433],"domain_scores_gemma":[0.99758893,0.00028297634,0.00084854924,0.00061180134,0.00045560516,0.00021212258],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.0006270399,0.000471739,0.00073469646,0.00009152368,0.0013011822,0.00015245749,0.00047374092,0.00022267661,0.0001776184],"category_scores_gemma":[0.00013852789,0.00030380898,0.0002626757,0.0005376008,0.0006029907,0.0004327878,0.00019468862,0.00040597055,0.0000048500415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023752756,0.00083115505,0.98584807,0.000036452308,0.002560498,0.00018559056,0.0016336393,0.0022372326,0.001799485,0.00017418145,0.002155816,0.00016258493],"study_design_scores_gemma":[0.0021916695,0.0013599343,0.991617,0.0001120747,0.0012840475,0.000037623147,0.00020815975,0.0009829866,0.0006959345,0.0004882422,0.0005799067,0.00044242296],"about_ca_topic_score_codex":0.14200753,"about_ca_topic_score_gemma":0.0859573,"teacher_disagreement_score":0.056050222,"about_ca_system_score_codex":0.00009915646,"about_ca_system_score_gemma":0.0007255679,"threshold_uncertainty_score":0.999999},"labels":[],"label_agreement":null},{"id":"W7073785430","doi":"","title":"Human cathepsin X. A novel cysteine protease with unique specificity","year":2000,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cathepsin H; Cathepsin E; Cysteine; Enzyme; Protease; Cathepsin O; Cathepsin; Cathepsin A","score_opus":0.01259134268455239,"score_gpt":0.20197699473761166,"score_spread":0.18938565205305927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073785430","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9025179,0.0000072361286,0.000039673996,0.00015039177,0.000043921227,0.0002573323,0.00015152393,0.0000479273,0.09678407],"genre_scores_gemma":[0.99366885,0.0000026894625,0.0018767178,0.00009015187,0.00019229604,0.0000038536164,0.00006412811,0.000004585782,0.0040967297],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992327,0.000035042027,0.00012725893,0.00020811471,0.0001711212,0.00022573152],"domain_scores_gemma":[0.999604,0.000011577038,0.000038848062,0.00021916561,0.000021000045,0.000105448715],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013790319,0.00011705577,0.00015274428,0.0000227935,0.0001376306,0.00006364205,0.00015475102,0.00003848906,0.018835409],"category_scores_gemma":[0.0000025060504,0.00008194537,0.000023821845,0.00009723541,0.000059983235,0.000086051026,0.0000043919363,0.000069865164,0.00044812929],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010862311,0.0008236858,0.032191403,0.00028720085,0.0001994405,0.00039557207,0.0022357167,0.0053244457,0.8705765,0.017846141,0.010698791,0.0583349],"study_design_scores_gemma":[0.0041095004,0.0028931252,0.43189597,0.00025384995,0.00012930411,0.00013415563,0.000102163074,0.0021263172,0.06674185,0.021341622,0.46829477,0.0019773864],"about_ca_topic_score_codex":0.002314601,"about_ca_topic_score_gemma":0.0007715724,"teacher_disagreement_score":0.8038346,"about_ca_system_score_codex":0.0000017464281,"about_ca_system_score_gemma":0.00003082277,"threshold_uncertainty_score":0.9820615},"labels":[],"label_agreement":null},{"id":"W7073786525","doi":"","title":"A moral profession: Nurse educators’ selected narratives of care and compassion","year":2017,"lang":"en","type":"article","venue":"Bucks New University Repository (Bucks New University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Compassion; Narrative; Abandonment (legal); Kindness; Context (archaeology); Empathy; Perception; Nursing care; Health care","score_opus":0.008291060730556705,"score_gpt":0.19518928936150653,"score_spread":0.18689822863094982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073786525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9526028,0.00012803571,0.0000607089,0.000318834,0.00096811075,0.0002770659,0.000059709746,0.000069606016,0.045515105],"genre_scores_gemma":[0.9705416,0.000040432184,0.00071166194,0.000008548565,0.00022865615,1.6462062e-8,0.000046426827,0.0000061752216,0.028416472],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986329,0.00018426967,0.00015267277,0.00046865176,0.00025188498,0.00030960052],"domain_scores_gemma":[0.9984102,0.00004358772,0.00038048145,0.0005219684,0.00018592116,0.0004578457],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00004895234,0.0002488567,0.00040507282,0.00022010577,0.0014049733,0.00010775047,0.0007028304,0.0001844954,0.00022810082],"category_scores_gemma":[0.000014589511,0.00025690178,0.00009805845,0.00024279229,0.000302461,0.00079001725,0.00012153317,0.0001859751,0.0000144168625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0041663293,0.00027584864,0.8472085,0.0004845365,0.0005756707,0.0014766003,0.051604368,0.00034277554,0.019770404,0.006379523,0.047074445,0.020641008],"study_design_scores_gemma":[0.0040697325,0.0009176547,0.787131,0.00044721793,0.0003439189,0.000041608357,0.04953313,0.00009109348,0.010031098,0.00029322895,0.14613833,0.0009619532],"about_ca_topic_score_codex":0.009616001,"about_ca_topic_score_gemma":0.0017381511,"teacher_disagreement_score":0.09906388,"about_ca_system_score_codex":0.000034305125,"about_ca_system_score_gemma":0.0007768542,"threshold_uncertainty_score":0.9999883},"labels":[],"label_agreement":null},{"id":"W7073787403","doi":"","title":"Alcohol Intake as a Risk Factor for Acute Stroke:The INTERSTROKE Study","year":2023,"lang":"en","type":"article","venue":"UWA Profiles and Research Repository (University of Western Australia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Risk factor; Alcohol intake; Alcohol consumption; Risk assessment; Alcohol","score_opus":0.0848682166202757,"score_gpt":0.3330984783487985,"score_spread":0.2482302617285228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073787403","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971957,0.000018028393,0.000010307637,0.0002291911,0.00027038742,0.0009321172,0.0011343644,0.00003604914,0.00017383594],"genre_scores_gemma":[0.9781849,0.00007081503,0.000054756445,0.0000028872942,0.00011054141,0.0000015983707,0.000030598178,0.0000047761328,0.021539124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983754,0.00030070293,0.00014629528,0.0003346922,0.0004482047,0.00039468036],"domain_scores_gemma":[0.99908715,0.00024130195,0.00011582008,0.00027350287,0.00013595434,0.00014626537],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066517765,0.00012284538,0.00023463719,0.00012839053,0.00077843986,0.00013565336,0.0004570298,0.0000783184,0.00017320202],"category_scores_gemma":[0.000019904128,0.00009550314,0.0000861794,0.00019422315,0.00030428002,0.00021325902,0.000121968485,0.00022131724,0.00010997566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011652366,0.00015331934,0.9436478,0.00022917303,0.0011772594,0.0003435116,0.013489833,0.00008833526,0.028236922,0.00009703437,0.0037832253,0.0075883637],"study_design_scores_gemma":[0.00080921303,0.0013721874,0.9741653,0.000033690372,0.00012072616,0.000010011873,0.013743397,0.00025531475,0.005225657,0.00010547187,0.003996917,0.00016208849],"about_ca_topic_score_codex":0.009743015,"about_ca_topic_score_gemma":0.00050805457,"teacher_disagreement_score":0.030517539,"about_ca_system_score_codex":0.0000054762945,"about_ca_system_score_gemma":0.00004681476,"threshold_uncertainty_score":0.9968512},"labels":[],"label_agreement":null},{"id":"W7073800004","doi":"","title":"Facilitators and barriers to implementation of Alberta family integrated care (FICare) in level II neonatal intensive care units: a qualitative process evaluation substudy of a multicentre cluster-randomised controlled trial using the consolidated framework for implementation research","year":2021,"lang":"en","type":"other","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Integrated care; Qualitative research; Intensive care; Process (computing); Randomized controlled trial; Neonatal intensive care unit","score_opus":0.10072622528844273,"score_gpt":0.437977001491552,"score_spread":0.3372507762031093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073800004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.974396,0.00071638456,0.00031533925,0.00004527852,0.0003174337,0.01826336,0.005804173,0.000007485616,0.00013454049],"genre_scores_gemma":[0.99407685,0.00001692904,0.0006646783,0.000045341054,0.000041756226,0.00039046936,0.004526459,0.000031308144,0.0002061868],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.99558955,0.0020694544,0.0008561435,0.0004685824,0.0006825582,0.0003336963],"domain_scores_gemma":[0.9929815,0.0018457914,0.00051625865,0.00021868208,0.0043218066,0.00011594416],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014800569,0.0002878136,0.00088117504,0.0003735199,0.00018099211,0.000058281254,0.00019638745,0.00019044173,0.0018174709],"category_scores_gemma":[0.0023203425,0.00020105291,0.00008094793,0.00070467504,0.00014449834,0.00007779108,0.000039390117,0.00016613227,5.811147e-7],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.08444555,0.00000989558,0.0012302998,0.000599147,0.0006091038,7.5027674e-7,0.9093025,0.00027998,0.00040820497,0.000058432008,0.0005385711,0.0025175824],"study_design_scores_gemma":[0.146404,0.00046889362,0.00027250542,0.00028467018,0.00023701823,1.5970895e-7,0.85097456,0.0003328223,0.00056311063,0.00006352281,0.00021151423,0.00018724795],"about_ca_topic_score_codex":0.14851582,"about_ca_topic_score_gemma":0.324539,"teacher_disagreement_score":0.17602319,"about_ca_system_score_codex":0.00004133364,"about_ca_system_score_gemma":0.0013930154,"threshold_uncertainty_score":0.999095},"labels":[],"label_agreement":null},{"id":"W7073800984","doi":"","title":"Understanding collaborative approaches to research: A synthesis of the research partnership literature","year":2018,"lang":"en","type":"other","venue":"OSF Preprints (OSF Preprints)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"General partnership; Systematic review; Context (archaeology); MEDLINE; Health services research","score_opus":0.3089262806671904,"score_gpt":0.32819094977494595,"score_spread":0.01926466910775554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073800984","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013750605,0.000013198868,0.000039732568,0.00048960897,0.00043265583,0.0018360954,0.0005001386,0.000052992495,0.99526054],"genre_scores_gemma":[0.13349947,0.00011079402,0.0005173941,0.000023591474,0.00050932413,0.000101815735,0.000047517635,0.00009025211,0.86509985],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9905275,0.00476754,0.00044849035,0.001905203,0.0015173695,0.0008338778],"domain_scores_gemma":[0.99346787,0.0020776389,0.00028060205,0.0035668549,0.00031090408,0.00029614955],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.01550175,0.00035862284,0.0006210331,0.0005792135,0.00045804627,0.0004106867,0.0023744805,0.00054798037,0.48215294],"category_scores_gemma":[0.004679155,0.00026885018,0.00015155842,0.0017477592,0.00096205395,0.00011481874,0.0009414297,0.0007690868,0.3850311],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021152258,0.000088834764,0.003401336,0.00047222007,0.00027372813,0.000012762546,0.0039824513,0.00017330387,0.00025986627,0.007885253,0.9822006,0.0010381065],"study_design_scores_gemma":[0.0001741355,0.000006871539,0.002483799,0.0016924328,0.000055912267,0.000004221468,0.0011589184,0.00006690216,0.0058032568,0.017113043,0.97099364,0.00044687418],"about_ca_topic_score_codex":0.0018560281,"about_ca_topic_score_gemma":0.003218565,"teacher_disagreement_score":0.13212441,"about_ca_system_score_codex":0.00006747134,"about_ca_system_score_gemma":0.0004658317,"threshold_uncertainty_score":0.9999764},"labels":[],"label_agreement":null},{"id":"W7073803165","doi":"","title":"Practising Femininity: Domestic Realism and the Performance of Gender in Early Canadian Fiction","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Realism; Narrative; Perspective (graphical); Government (linguistics); Order (exchange)","score_opus":0.01900665889387148,"score_gpt":0.20716303475075076,"score_spread":0.18815637585687928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073803165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9055876,0.000001410761,0.0000016677623,0.000069551264,0.00015815556,0.00019034218,0.00005846923,0.000022409553,0.093910374],"genre_scores_gemma":[0.98686,0.0130018955,0.00003281991,0.000020882224,0.000032750275,2.5682368e-7,0.00003108668,0.000002727142,0.000017600485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932516,0.00010884544,0.00009486336,0.00015073796,0.00010790132,0.00021248122],"domain_scores_gemma":[0.99958354,0.00014038292,0.000067696405,0.0001272599,0.000027269598,0.000053862605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031863732,0.000079143014,0.00013608934,0.0023401338,0.00014409967,0.000035849527,0.00012752615,0.000049496695,0.000026983405],"category_scores_gemma":[0.000028788385,0.000063916814,0.000020897442,0.0026359167,0.0000844362,0.00027281768,0.00001985318,0.0000878278,0.000015249831],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022824865,0.00009047791,0.72982675,0.00075456116,0.00038288624,0.0013039546,0.15438956,0.009113826,0.00011177578,0.007006566,0.0012158639,0.093521304],"study_design_scores_gemma":[0.0014832396,0.00012425025,0.5599022,0.00005672713,0.000067452886,0.000014941451,0.0009883071,0.0062216967,0.00008184426,0.00001354386,0.43081012,0.0002356818],"about_ca_topic_score_codex":0.90502715,"about_ca_topic_score_gemma":0.50415266,"teacher_disagreement_score":0.42959425,"about_ca_system_score_codex":0.000009734354,"about_ca_system_score_gemma":0.00021243261,"threshold_uncertainty_score":0.50489527},"labels":[],"label_agreement":null},{"id":"W7073804889","doi":"","title":"International Tax Avoidance -- Introduction","year":2017,"lang":"","type":"article","venue":"eYLS (Yale Law School)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tax avoidance; Tax reform; Indirect tax; Statutory law; Direct tax; Scope (computer science); Revenue; Evasion (ethics); Double taxation","score_opus":0.012242822035404008,"score_gpt":0.2334295243076435,"score_spread":0.2211867022722395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073804889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.72973675,0.0014621832,0.00020243168,0.023501208,0.07861628,0.0008012014,0.002269802,0.00014041187,0.16326974],"genre_scores_gemma":[0.96008486,0.000660313,0.00064121676,0.00038746715,0.01713938,0.0000064414508,0.0002192755,0.000015605312,0.020845424],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9972433,0.00014819333,0.0005278033,0.00082774734,0.0006261297,0.00062686787],"domain_scores_gemma":[0.9974138,0.000053041917,0.0006161876,0.001344769,0.00018391783,0.00038825406],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00074747385,0.00036408156,0.00042997504,0.00005426674,0.0018374244,0.0024303326,0.0016110849,0.00020635939,0.030874424],"category_scores_gemma":[0.00028899589,0.00035094,0.00015371399,0.00005993628,0.00045252955,0.0019822256,0.00018232792,0.00039414587,0.008960843],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018839393,0.0007975355,0.11363436,0.0006580989,0.0016899745,0.0004288794,0.0012369528,0.006374516,0.05751988,0.22214873,0.47867054,0.11495661],"study_design_scores_gemma":[0.0005673824,0.00010789656,0.06359693,0.000058942584,0.000052399828,0.000013007562,0.000026207277,0.0005192759,0.0034964937,0.003268302,0.9278483,0.0004449029],"about_ca_topic_score_codex":0.015020059,"about_ca_topic_score_gemma":0.004343232,"teacher_disagreement_score":0.44917774,"about_ca_system_score_codex":0.000017401688,"about_ca_system_score_gemma":0.000098865734,"threshold_uncertainty_score":0.99989426},"labels":[],"label_agreement":null},{"id":"W7073807646","doi":"","title":"History of Canadian Surgery: Dr. John Mackieson (1795-1885), Strangulated Hernia in the Early 19th Century","year":2009,"lang":"en","type":"article","venue":"TSpace (University of Toronto)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"History of medicine; Work (physics); Late 19th century; MEDLINE","score_opus":0.013166635160675264,"score_gpt":0.17620367027378592,"score_spread":0.16303703511311066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073807646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9420043,0.0012952628,0.0000011145695,0.00065405405,0.0002582503,0.00011407873,0.00010908265,0.000010736992,0.055553075],"genre_scores_gemma":[0.99844074,0.00037403242,0.00004734741,0.000049990063,0.000025391677,1.4084976e-8,0.000047437316,0.0000016974257,0.0010133524],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9992434,0.000103862934,0.00008992562,0.00013964971,0.00018532523,0.00023786658],"domain_scores_gemma":[0.99951607,0.000047205394,0.000104422776,0.00019504079,0.000034142777,0.000103139],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002473976,0.00009416013,0.00023269384,0.00009555531,0.000059512666,0.000008298247,0.00028545503,0.000072618415,0.012335825],"category_scores_gemma":[0.0000055728665,0.00009001904,0.00006903981,0.00010369874,0.000072284936,0.00024379598,0.000005112039,0.00006030435,0.000022792474],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017884622,0.00047848828,0.2680912,0.00035598647,0.00039588066,0.0009372393,0.25478286,0.0011709188,0.010010827,0.0033841457,0.14774746,0.31085652],"study_design_scores_gemma":[0.0001545633,0.00007331482,0.9572089,0.000016977408,0.000018886725,7.527938e-7,0.0015007476,0.000051421437,0.000011843635,0.000018544868,0.040846467,0.00009758818],"about_ca_topic_score_codex":0.98486316,"about_ca_topic_score_gemma":0.9607401,"teacher_disagreement_score":0.68911767,"about_ca_system_score_codex":0.000052450134,"about_ca_system_score_gemma":0.00020073375,"threshold_uncertainty_score":0.98856705},"labels":[],"label_agreement":null},{"id":"W7073812083","doi":"","title":"Characterization of the phosphocholine-substituted oligosaccharide in lipopolysaccharides of type b Haemophilus influenzae","year":2000,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Heptose; Oligosaccharide; Phase variation; Phosphocholine; Haemophilus influenzae; Mutant; Epitope; Lipid A; Lipopolysaccharide","score_opus":0.010917058843382895,"score_gpt":0.20847222955200007,"score_spread":0.19755517070861717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073812083","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973299,0.000032057113,0.000001761063,0.000078040954,0.00032126065,0.00014339328,0.0001484303,0.0000097286475,0.0019354514],"genre_scores_gemma":[0.9995271,0.00009506892,0.00008128467,0.000075743425,0.000059377602,8.332022e-7,0.00004453646,0.0000028970026,0.0001131556],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9992137,0.000042401574,0.0002991785,0.00012761082,0.00017132366,0.00014581959],"domain_scores_gemma":[0.99955726,0.000025011555,0.000118544136,0.00022119214,0.000046380854,0.000031626107],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013669848,0.00008776223,0.0001972123,0.000040373154,0.000035667086,0.000013363277,0.00024324695,0.0000536613,0.0050885337],"category_scores_gemma":[0.00002527041,0.000061903644,0.000036588637,0.00033305804,0.000072837734,0.00013982126,0.000010718489,0.000060315535,0.00005587926],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012344317,0.000030189502,0.03691651,0.000034642457,0.000013360678,0.0000018419878,0.00036722998,0.0011615871,0.9498123,0.0002829712,0.000030036772,0.011225868],"study_design_scores_gemma":[0.00026986722,0.000033292315,0.6095614,0.000060357917,0.000015275262,0.0000017202746,0.000006878742,0.00088980584,0.3855217,0.0019551194,0.001574839,0.00010974977],"about_ca_topic_score_codex":0.0019073549,"about_ca_topic_score_gemma":0.00030829365,"teacher_disagreement_score":0.5726449,"about_ca_system_score_codex":0.0000017184605,"about_ca_system_score_gemma":0.00005092687,"threshold_uncertainty_score":0.99582094},"labels":[],"label_agreement":null},{"id":"W7073819962","doi":"","title":"A data set of worldwide glacier fluctuations","year":2014,"lang":"en","type":"article","venue":"Utrecht University Repository (Utrecht University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Glacier; Arctic; Climate change; Data set; Glacier mass balance; Glacier terminus; Series (stratigraphy); Glaciology","score_opus":0.018027003274909047,"score_gpt":0.1846901082748879,"score_spread":0.16666310499997886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073819962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6840134,0.00005475465,0.0026422937,0.000324019,0.0014136479,0.00035119095,0.0015045286,0.00023108903,0.30946505],"genre_scores_gemma":[0.9602,0.00004526872,0.001492609,0.000027193557,0.00018906464,1.6471981e-8,0.0005199434,0.0000064530045,0.037519444],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983033,0.00033423404,0.00019279805,0.0005438825,0.0003066186,0.00031914646],"domain_scores_gemma":[0.9981803,0.00026354202,0.00023564057,0.0009867399,0.00012491069,0.00020885105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031152798,0.00020294508,0.00033838098,0.0003490334,0.00043539298,0.00003755916,0.0013014107,0.00014402252,0.0006933532],"category_scores_gemma":[0.000039158804,0.00022524815,0.000099760495,0.00070858066,0.00023148564,0.0006922536,0.00021621298,0.00015935401,0.00009966458],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0046318197,0.0014791542,0.4401783,0.0014038662,0.004828015,0.0041760956,0.009285061,0.017065167,0.0692588,0.115816355,0.11239321,0.21948417],"study_design_scores_gemma":[0.0010316868,0.00014052658,0.035238598,0.000061675935,0.00035536737,0.000019679273,0.0009834828,0.0028509628,0.0023787133,0.00029652007,0.95617235,0.00047046258],"about_ca_topic_score_codex":0.0037695984,"about_ca_topic_score_gemma":0.0012638036,"teacher_disagreement_score":0.84377915,"about_ca_system_score_codex":0.000025577132,"about_ca_system_score_gemma":0.00016789991,"threshold_uncertainty_score":0.9185353},"labels":[],"label_agreement":null},{"id":"W7073832890","doi":"","title":"Structural analysis with mixed frequencies : monetary policy, uncertainty and gross capital flows","year":2016,"lang":"en","type":"other","venue":"Archivio Istituzionale della Ricerca (Universita Degli Studi Di Milano)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shock (circulatory); Monetary policy; Capital (architecture); Lag; Quarter (Canadian coin); Capital flows; Net capital rule; Capital formation; Capital account","score_opus":0.008421963262190921,"score_gpt":0.1934875936560626,"score_spread":0.1850656303938717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073832890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6534008,0.0028261477,0.00021756362,0.0002915334,0.0006072761,0.00068666146,0.014528131,0.0002164431,0.32722548],"genre_scores_gemma":[0.86482984,0.0010325743,0.0010102056,0.00007438134,0.0007489297,0.0000033173465,0.0026673735,0.00007973327,0.12955365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974511,0.00014637764,0.00024884916,0.00088471826,0.00059032167,0.00067860546],"domain_scores_gemma":[0.9986236,0.00020835847,0.00027707947,0.0004969335,0.00006840165,0.0003256047],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000108796776,0.000619824,0.00089681253,0.00078267744,0.00046325228,0.00010701375,0.00056698587,0.00017588308,0.003978672],"category_scores_gemma":[0.000010614151,0.00045473804,0.00020934345,0.00055882573,0.0005247133,0.00019199938,0.00014625154,0.00018963238,0.00025564627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021990265,0.00031460903,0.61360186,0.0015120661,0.04740949,0.004026335,0.0096568735,0.029428964,0.00084799685,0.036984958,0.22786702,0.026150784],"study_design_scores_gemma":[0.002407351,0.00043205803,0.86715734,0.0002642432,0.0042813974,0.0000832722,0.001223388,0.002699925,0.000008402242,0.0023673219,0.11642648,0.0026488078],"about_ca_topic_score_codex":0.045125455,"about_ca_topic_score_gemma":0.1081005,"teacher_disagreement_score":0.25355548,"about_ca_system_score_codex":0.000028811573,"about_ca_system_score_gemma":0.00020746111,"threshold_uncertainty_score":0.99979043},"labels":[],"label_agreement":null},{"id":"W7073836740","doi":"","title":"Psychometric properties of the Montreal Cognitive Assessment (MoCA) in healthy participants aged 18-70","year":2020,"lang":"en","type":"article","venue":"Data Archiving and Networked Services (DANS)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Montreal Cognitive Assessment; Normative; Cognition; Reliability (semiconductor); Equivalence (formal languages); Psychometrics","score_opus":0.06336197217922025,"score_gpt":0.27243174422883304,"score_spread":0.2090697720496128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073836740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969847,0.0006114147,0.0000389783,0.0003021761,0.00019191032,0.0002767058,0.000854305,0.000018917499,0.0007208925],"genre_scores_gemma":[0.9985313,0.00034164055,0.000072404124,0.0005103959,0.00014836456,0.000003481159,0.00037919424,0.000005395662,0.000007819039],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99839973,0.00030252285,0.00031496014,0.00038230506,0.0002361493,0.00036432143],"domain_scores_gemma":[0.9992037,0.00015789109,0.00015120902,0.00032736777,0.00001470918,0.00014516286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044813263,0.00015179934,0.00029307304,0.00004545306,0.00016925487,0.000076076445,0.00068212854,0.000031931497,0.000049009992],"category_scores_gemma":[0.000019219047,0.00009449083,0.000024328641,0.0004311433,0.00008609949,0.00021899847,0.00019139382,0.00015351397,0.0000064855312],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007060442,0.000083867264,0.96382797,0.00062781724,0.00009444968,0.0000061357796,0.007276861,0.0027938695,0.0013887668,0.000008974227,0.00022915818,0.022956058],"study_design_scores_gemma":[0.00044244612,0.00012585027,0.9260331,0.00021434751,0.00003913919,8.647552e-7,0.00061061006,0.07210038,0.0000736387,0.00007579518,0.00016244593,0.0001213851],"about_ca_topic_score_codex":0.0106326435,"about_ca_topic_score_gemma":0.018314896,"teacher_disagreement_score":0.06930651,"about_ca_system_score_codex":0.0000014363624,"about_ca_system_score_gemma":0.00004475002,"threshold_uncertainty_score":0.9995983},"labels":[],"label_agreement":null},{"id":"W7073837147","doi":"","title":"Gender differences in descriptions of angina symptoms and health problems immediately prior to angiography: the ACRE study. Appropriateness of Coronary Revascularisation study","year":2001,"lang":"en","type":"article","venue":"UCL Discovery (University College London)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Angina; Coronary artery disease; Chest pain; Coronary angiography; Acre; Coronary heart disease; Neck pain; Canadian Cardiovascular Society","score_opus":0.027839154008319746,"score_gpt":0.2117538001464415,"score_spread":0.18391464613812175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073837147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969852,0.0003082842,0.00014283777,0.00014782217,0.00013713304,0.0017412262,0.00047370492,0.000011227671,0.000052554173],"genre_scores_gemma":[0.999623,0.00012806462,0.00005188799,0.00001951981,0.0000163618,0.0000021821288,0.000034901797,0.0000035099208,0.000120553224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99866176,0.00029324953,0.00022800837,0.00029035172,0.00030061993,0.00022601639],"domain_scores_gemma":[0.9994039,0.000059755967,0.00016139788,0.00024409445,0.00005455946,0.00007628474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051821966,0.00014139629,0.00037049642,0.00025415397,0.00022975358,0.000028311091,0.0002764703,0.000038933333,0.000046278336],"category_scores_gemma":[0.0000059193935,0.0001096277,0.00008206512,0.0008399028,0.000088256675,0.0004699528,0.00007029188,0.00006846687,0.0000024454016],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019063955,0.00039498392,0.9910434,0.000054400225,0.00013719486,0.000019701243,0.006596233,0.00050820765,0.000056614295,0.00023423095,0.000026841715,0.00073756976],"study_design_scores_gemma":[0.00096814265,0.00070717616,0.9785372,0.000029539262,0.00007341355,0.0000023767182,0.019229118,0.00017044359,0.0000026521268,0.0001263084,0.00003645445,0.00011715055],"about_ca_topic_score_codex":0.01649624,"about_ca_topic_score_gemma":0.016123679,"teacher_disagreement_score":0.012632885,"about_ca_system_score_codex":0.000010094265,"about_ca_system_score_gemma":0.000091935886,"threshold_uncertainty_score":0.990053},"labels":[],"label_agreement":null},{"id":"W7073841611","doi":"","title":"Cognitive impairment in patients with heart failure: an international study.","year":2020,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cognition; Montreal Cognitive Assessment; Cognitive impairment; Heart failure; Population; Cross-sectional study; Activities of daily living; Cognitive test","score_opus":0.009346984997440428,"score_gpt":0.21144033089046088,"score_spread":0.20209334589302044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073841611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984228,7.601821e-7,0.0000086040845,0.0003421357,0.00009381139,0.00030554057,0.00008952265,0.000018603527,0.00071823987],"genre_scores_gemma":[0.9990818,2.0466655e-7,0.00019299219,0.00046972974,0.00006541344,0.0000015976814,0.0001732842,0.00000170441,0.0000132980595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993781,0.000041288236,0.00009731934,0.00017398068,0.00019969147,0.000109654145],"domain_scores_gemma":[0.99979526,0.000014891988,0.000021903963,0.00004641873,0.000035606427,0.00008592257],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000060868162,0.00006865072,0.00009503959,0.000019753243,0.000025160023,0.00005602093,0.00009335522,0.0000127271005,0.0029538332],"category_scores_gemma":[0.0000056912454,0.000046554072,0.000008952576,0.00007089248,0.000012314178,0.00025026614,0.000009948491,0.000035585126,0.0001732595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016517834,0.00012966983,0.9987749,0.0000014807741,0.000011922929,0.0000021973094,0.00040434444,0.000104897656,0.0000036171032,0.000006642667,0.00015311033,0.00024203732],"study_design_scores_gemma":[0.0010567495,0.0012142267,0.9965381,0.0000035654102,0.0000047110866,7.092904e-8,0.00035347918,0.00016034204,0.000033154676,0.000012304654,0.0005464197,0.00007687388],"about_ca_topic_score_codex":0.0010781807,"about_ca_topic_score_gemma":0.0015394092,"teacher_disagreement_score":0.0027805737,"about_ca_system_score_codex":0.0000010003961,"about_ca_system_score_gemma":0.000013506111,"threshold_uncertainty_score":0.9979576},"labels":[],"label_agreement":null},{"id":"W7073844636","doi":"","title":"Clinical drugs that interact with St. John's Wort and implication in drug development","year":2008,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Drug; Pharmacokinetics; Pharmacodynamics; Drug interaction; Tolbutamide; Antimicrobial","score_opus":0.03714420535902893,"score_gpt":0.25361644249615617,"score_spread":0.21647223713712724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073844636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856297,0.00010222106,3.2463873e-7,0.00005084281,0.00005795036,0.00016703372,0.011699898,0.000022311426,0.0022697581],"genre_scores_gemma":[0.9764375,0.000015924335,0.00023720827,0.00008011741,0.00006221222,0.000009150585,0.02298425,0.0000027877613,0.00017085092],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993447,0.00003466133,0.00016001696,0.00019880477,0.00011727999,0.00014451459],"domain_scores_gemma":[0.9996329,0.00009986365,0.00006714662,0.000106846026,0.000021298783,0.00007194296],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008484164,0.00008451288,0.00013517604,0.000029500157,0.00006908705,0.000036341615,0.0001020176,0.000033152155,0.028776977],"category_scores_gemma":[0.000026103578,0.00006154541,0.000013177825,0.000063707856,0.000009476175,0.00016152284,0.000019386629,0.00007346016,0.0005946815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017686443,0.00009281995,0.6731582,0.00018873501,0.00005532767,0.00014152472,0.003899917,0.000098723474,0.000024871279,0.000008725423,0.23348843,0.08866581],"study_design_scores_gemma":[0.00015412488,0.000018192375,0.84126055,0.0001667007,0.000001384765,0.0000068068653,0.000023566943,0.000026187656,0.00019595303,0.000011722104,0.15803784,0.00009696338],"about_ca_topic_score_codex":0.00021808677,"about_ca_topic_score_gemma":0.0006383365,"teacher_disagreement_score":0.1681023,"about_ca_system_score_codex":0.000001949036,"about_ca_system_score_gemma":0.000063298365,"threshold_uncertainty_score":0.97211087},"labels":[],"label_agreement":null},{"id":"W7073845775","doi":"","title":"Utility of Gram stain in the clinical management of suspected ventilator-associated pneumonia. Secondary analysis of a multicenter randomized trial.","year":2008,"lang":"en","type":"article","venue":"TSpace","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Canadian Institutes of Health Research; AstraZeneca","keywords":"Gram staining; Gram; Pneumonia; Pathogenic bacteria; Stain; Bronchoalveolar lavage; Microbiological culture; Gram-negative bacteria","score_opus":0.0327652114643878,"score_gpt":0.3197261495166803,"score_spread":0.2869609380522925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073845775","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972672,0.00010665915,0.000012579661,0.000048773887,0.00014693469,0.00071292324,0.0001110063,0.0000071169575,0.0015868472],"genre_scores_gemma":[0.99950397,0.00014714847,0.00010229336,0.00001346386,0.000012011558,0.0000030992765,0.00009204604,0.0000019038126,0.00012403683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99755776,0.0009983092,0.00079911423,0.00017776404,0.0003044618,0.00016261423],"domain_scores_gemma":[0.9984311,0.0006611574,0.0005063507,0.00029902582,0.00006969941,0.000032709628],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025942484,0.000100107725,0.00096052774,0.0001086205,0.000030474443,0.00000657453,0.00023629153,0.00006058407,0.000955402],"category_scores_gemma":[0.00011883028,0.00006599139,0.00034521555,0.00060626963,0.0002124359,0.00003904139,0.000019998011,0.0000890387,0.0000030004176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.4425331,0.0024608828,0.5319778,0.0003501335,0.008361936,0.00008946148,0.0097603565,0.0007979904,0.00046143937,0.00038197034,0.0005724907,0.0022524858],"study_design_scores_gemma":[0.12347912,0.000110787005,0.8720517,0.000019659356,0.0007841071,1.0920456e-7,0.00048130282,0.0026237278,0.00019703578,0.00010264015,0.00007930102,0.000070465925],"about_ca_topic_score_codex":0.0043549417,"about_ca_topic_score_gemma":0.0013093065,"teacher_disagreement_score":0.340074,"about_ca_system_score_codex":0.0000013657456,"about_ca_system_score_gemma":0.00003771341,"threshold_uncertainty_score":0.99995786},"labels":[],"label_agreement":null},{"id":"W7073850902","doi":"","title":"Factors affecting the psychological functioning of Australian adults with chronic pain","year":2012,"lang":"en","type":"article","venue":"ResearchOnline at James Cook University (James Cook University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Psychological intervention; Chronic pain; Anxiety; Coping (psychology); Mental health; Quality of life (healthcare); Psychological resilience; Depression (economics)","score_opus":0.029386753454436365,"score_gpt":0.2314387022157232,"score_spread":0.20205194876128685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073850902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99470824,0.00010823858,0.0001444553,0.00029137297,0.00014599698,0.0003481958,0.00017454065,0.000071600865,0.0040073306],"genre_scores_gemma":[0.98406214,0.00013055498,0.00018178881,0.000023120596,0.00016439265,4.1618286e-8,0.00016856402,0.000007696927,0.015261682],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975208,0.00072543375,0.00014510595,0.00038174927,0.00047295346,0.0007539655],"domain_scores_gemma":[0.99827397,0.0006899873,0.00018111864,0.0003868808,0.0001397673,0.00032829057],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006018701,0.0002526096,0.00032517998,0.0002842216,0.0010191364,0.00006074279,0.00063585205,0.00014654672,0.0032987907],"category_scores_gemma":[0.00006500913,0.00018442201,0.00013953136,0.0008051221,0.0007766133,0.00052668207,0.00015006313,0.000361764,0.000067649395],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0052282293,0.00056330604,0.928778,0.00042118336,0.0007819111,0.0003677244,0.0069222967,0.00547538,0.0021914488,0.0013385445,0.009076349,0.03885561],"study_design_scores_gemma":[0.002277311,0.0015940388,0.3774712,0.00021286098,0.00015869128,0.000014162206,0.014734938,0.00076647644,0.0010315119,0.000008835442,0.60111886,0.00061112014],"about_ca_topic_score_codex":0.002921503,"about_ca_topic_score_gemma":0.002066007,"teacher_disagreement_score":0.5920425,"about_ca_system_score_codex":0.00009339102,"about_ca_system_score_gemma":0.00013567321,"threshold_uncertainty_score":0.99761236},"labels":[],"label_agreement":null},{"id":"W7073852540","doi":"","title":"Sowing the Seeds of Hope: Keeping children safe with families","year":2025,"lang":"en","type":"report","venue":"Issue Lab (Candid)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Plan (archaeology); Quarter (Canadian coin); Key (lock); Best practice; Agriculture","score_opus":0.00930167853416135,"score_gpt":0.22544898307148553,"score_spread":0.21614730453732417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073852540","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.35320154,0.014179852,0.00004705337,0.00076251314,0.004407033,0.0015162895,0.0040113027,0.00015897567,0.6217154],"genre_scores_gemma":[0.966734,0.0039039373,0.00018443723,0.00020598265,0.0018822866,0.000007885859,0.0014365743,0.000024030569,0.02562085],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979344,0.000107634325,0.00043760694,0.00039896593,0.0007314939,0.00038989508],"domain_scores_gemma":[0.9986924,0.00015974623,0.00035502468,0.00055482035,0.0001677351,0.00007025892],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006069018,0.00033831174,0.000732404,0.0001217671,0.00024202846,0.00013003078,0.0005435621,0.00020147148,0.001275055],"category_scores_gemma":[0.000047971353,0.0002033983,0.00011334354,0.00030770234,0.00015461617,0.00010571815,0.00006123889,0.00026653157,0.000077862525],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005958903,0.00015365957,0.508399,0.0044286856,0.005151037,0.00022586477,0.005905648,0.007062108,0.00062777766,0.000530371,0.24843562,0.21848431],"study_design_scores_gemma":[0.0003831379,0.00015221347,0.22898908,0.00091032847,0.00044378318,0.000026152393,0.00015206699,0.0000339508,0.00060641335,0.0001636293,0.7676188,0.0005204835],"about_ca_topic_score_codex":0.06049288,"about_ca_topic_score_gemma":0.006178446,"teacher_disagreement_score":0.6135325,"about_ca_system_score_codex":0.000007761317,"about_ca_system_score_gemma":0.0005599418,"threshold_uncertainty_score":0.9996379},"labels":[],"label_agreement":null},{"id":"W7073856104","doi":"","title":"Short Report: Stable Prevalence of Powassan Virus in Ixodes scapularis in a Northern Wisconsin Focus","year":2008,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Enzootic; Ixodes scapularis; Ixodes; Transmission (telecommunications); Encephalitis; Flavivirus","score_opus":0.017811081410453938,"score_gpt":0.21567499060777678,"score_spread":0.19786390919732286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073856104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99188215,0.00033981985,0.000025038007,0.000032894884,0.00011555921,0.00018520822,0.00007289596,0.000016126822,0.007330286],"genre_scores_gemma":[0.99873775,0.0001272243,0.0004235223,0.000013079574,0.000027052829,0.0000018632442,0.000021232265,0.0000034572063,0.00064484327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987033,0.000074331685,0.00044364572,0.00026941687,0.00023431965,0.00027499144],"domain_scores_gemma":[0.99950683,0.000054182077,0.000081402955,0.00026372806,0.000033830653,0.000060034974],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038322172,0.00011957816,0.00028167522,0.00009789264,0.000038868977,0.000016084885,0.00016539839,0.0000626577,0.00095655635],"category_scores_gemma":[0.000037036625,0.00009765753,0.000035759513,0.00022355012,0.00008510991,0.00022102744,0.00001792191,0.00007392237,0.00004855264],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027163947,0.00004391212,0.9940003,0.000038704937,0.0000061080136,0.0003550442,0.00024955886,0.0009548653,0.0029537587,0.000030181942,0.000064764405,0.0012756387],"study_design_scores_gemma":[0.00014630819,0.00004461281,0.98500776,0.000033963905,0.0000057664643,0.000041888976,0.000033889017,0.00025533224,0.013368976,0.0006046085,0.0003125664,0.00014432639],"about_ca_topic_score_codex":0.057183422,"about_ca_topic_score_gemma":0.16878581,"teacher_disagreement_score":0.11160239,"about_ca_system_score_codex":0.0000033992264,"about_ca_system_score_gemma":0.00008482751,"threshold_uncertainty_score":0.9999567},"labels":[],"label_agreement":null},{"id":"W7073867394","doi":"","title":"Practices and principles of combative syndicalism in the 2012 Quebec student strike","year":2015,"lang":"en","type":"other","venue":"Redalyc (Universidad Autónoma del Estado de México)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Diafiltration; Dysgeusia; Liquation; Fusible alloy; Hyporeflexia; Demotion","score_opus":0.02438766735271979,"score_gpt":0.256407058200504,"score_spread":0.23201939084778422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073867394","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4799725,0.006292904,0.00005917234,0.00071389135,0.0005986329,0.0012197084,0.0017024437,0.00010281046,0.5093379],"genre_scores_gemma":[0.73810375,0.0013213438,0.0011063209,0.00016310536,0.00040764624,0.0000051802,0.00061763666,0.00009332875,0.25818166],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981232,0.00044061325,0.0002538246,0.000360444,0.00048202986,0.00033986598],"domain_scores_gemma":[0.99834114,0.0002618792,0.0008330521,0.0003731785,0.000047551428,0.00014319793],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00071401004,0.00027894054,0.0004977619,0.00029158,0.00007320145,0.00010718441,0.0006026588,0.00027734658,0.0014037197],"category_scores_gemma":[0.000058265046,0.00021162233,0.000056297573,0.00029217437,0.00025430927,0.0002697042,0.00007884919,0.0002546243,0.000048945472],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009546624,0.0017522591,0.18515989,0.0026038247,0.0026634955,0.0036738892,0.052017666,0.0016581588,0.0005723339,0.06628536,0.64521855,0.037439916],"study_design_scores_gemma":[0.00090429775,0.00023060024,0.23163398,0.00027882803,0.00023272874,0.000029250885,0.006172331,0.0003943162,0.000013033542,0.00034952138,0.75928986,0.0004712889],"about_ca_topic_score_codex":0.075764656,"about_ca_topic_score_gemma":0.08991495,"teacher_disagreement_score":0.25813127,"about_ca_system_score_codex":0.00001908639,"about_ca_system_score_gemma":0.00033725137,"threshold_uncertainty_score":0.99950916},"labels":[],"label_agreement":null},{"id":"W7073867507","doi":"","title":"Canadian recommendations on the prevention and treatment of Zika virus: Update","year":2016,"lang":"en","type":"article","venue":"PubMed Central","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Zika virus; MEDLINE; Public health; Disease prevention","score_opus":0.01643028895254569,"score_gpt":0.19873954806795469,"score_spread":0.182309259115409,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073867507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914204,0.00004599085,0.000007456252,0.006064447,0.00044223375,0.00021903423,0.0005956731,0.0000056841536,0.0011990715],"genre_scores_gemma":[0.9989696,0.000357245,0.000026059892,0.00007497418,0.00010268086,0.000007179834,0.000049807422,0.0000012318912,0.00041117796],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99941623,0.00004787297,0.00007942636,0.0000843719,0.00004926273,0.0003228487],"domain_scores_gemma":[0.9996693,0.00004527375,0.000033563712,0.00008629264,0.0000059594404,0.00015961353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00010980985,0.000051237166,0.0000658127,0.000021207801,0.00007128345,0.000021030928,0.000048861013,0.000017005877,0.0013197587],"category_scores_gemma":[0.000010232585,0.000024526596,0.000019125933,0.000030082823,0.000022661454,0.000060833358,0.0000016942843,0.0000088236475,0.000038383947],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005526722,0.000060838636,0.09027666,0.000005186292,0.000095397554,0.0000029174637,0.0003789816,0.000024252933,0.00052219955,0.005675834,0.004955495,0.89794695],"study_design_scores_gemma":[0.00022877289,0.000085668544,0.8099006,0.000009312673,0.000018476256,6.8290313e-7,0.000015276883,0.000013127705,0.003555028,0.0017026004,0.18440545,0.00006501043],"about_ca_topic_score_codex":0.05035897,"about_ca_topic_score_gemma":0.25911042,"teacher_disagreement_score":0.897882,"about_ca_system_score_codex":0.000012847344,"about_ca_system_score_gemma":0.00004932886,"threshold_uncertainty_score":0.9995932},"labels":[],"label_agreement":null},{"id":"W7073875426","doi":"","title":"Integrating Circadian Activity and Gene Expression Profiles to Predict Chronotoxicity of Drosophila suzukii Response to Insecticides","year":2013,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Drosophila suzukii; Circadian rhythm; Drosophila (subgenus); photoperiodism; Gene expression; Gene","score_opus":0.010326255937615528,"score_gpt":0.21322995801624947,"score_spread":0.20290370207863395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073875426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978141,0.000016883958,0.00027271654,0.00034554917,0.00013688477,0.0006266533,0.000114483606,0.00003577038,0.0006369256],"genre_scores_gemma":[0.995268,0.0000033004223,0.0043254145,0.00013462926,0.00009955466,0.000013714861,0.000010322748,0.0000044147805,0.00014067955],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9989644,0.00013978346,0.00019658376,0.00028213722,0.00017436477,0.00024267683],"domain_scores_gemma":[0.9992012,0.00020520313,0.00006780526,0.00020297906,0.00005967119,0.00026315774],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038972328,0.00014062291,0.00023592438,0.00009517354,0.00011624189,0.000091665876,0.00014616335,0.00006338935,0.001201498],"category_scores_gemma":[0.0001917914,0.00010196216,0.000025493851,0.00013949009,0.000044720222,0.00028761855,0.00004793073,0.00006212927,0.00009908492],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020369071,0.000013981698,0.02508499,0.00002183597,0.000006304268,0.0000010886281,0.0004557917,0.00012881082,0.9694221,0.000013502169,0.00028906105,0.0043588663],"study_design_scores_gemma":[0.00007243982,0.0002284385,0.51843226,0.00002805375,0.0000029311611,0.0000010804008,0.000037368238,0.00021625662,0.48066533,0.00013569363,0.0000928162,0.00008737013],"about_ca_topic_score_codex":0.01291358,"about_ca_topic_score_gemma":0.00092985586,"teacher_disagreement_score":0.49334726,"about_ca_system_score_codex":0.0000036833808,"about_ca_system_score_gemma":0.00004575586,"threshold_uncertainty_score":0.9997115},"labels":[],"label_agreement":null},{"id":"W7073878089","doi":"","title":"Experimental and Theoretical Investigation of the Reaction of C₂H with Formaldehyde (CH₂O) at Very Low Temperatures and Application to Astrochemical Models","year":2024,"lang":"en","type":"other","venue":"White Rose Research Online (University of Leeds, The University of Sheffield, University of York)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Science and Technology Facilities Council; European Commission","keywords":"Atmospheric temperature range; Formaldehyde; Yield (engineering); Activation energy; Photodissociation; Radical; Work (physics); Range (aeronautics); Nozzle; Branching (polymer chemistry)","score_opus":0.010791924168398572,"score_gpt":0.2041354376385584,"score_spread":0.19334351347015982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073878089","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890007,0.00035282856,0.00039036878,0.0006672102,0.00003800982,0.0005407427,0.000850851,0.000017093182,0.008142212],"genre_scores_gemma":[0.99171424,0.00034291294,0.0011159532,0.0000049045525,0.000021656153,1.0457147e-8,0.00009791626,0.000011870095,0.0066905282],"study_design_codex":"bench_or_experimental","study_design_gemma":"qualitative","domain_scores_codex":[0.99875474,0.00017212938,0.00010445038,0.00029832573,0.00048703654,0.00018330649],"domain_scores_gemma":[0.9990646,0.00011216473,0.00022629349,0.00032592882,0.00015288833,0.000118126896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031004255,0.0001510652,0.00037197393,0.0002597621,0.00020662074,0.000006839735,0.0005421288,0.00021895465,0.00029704714],"category_scores_gemma":[0.0000075613557,0.00013380211,0.00009086637,0.00033883716,0.002155735,0.00014050245,0.00037259492,0.00029045512,0.0000032782298],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.018255018,0.0012081474,0.017247625,0.009006611,0.0029881129,0.00010133175,0.09865101,0.005055321,0.71741956,0.036520205,0.087318085,0.0062289755],"study_design_scores_gemma":[0.020128569,0.011595203,0.13339692,0.017955502,0.005044816,0.00013511823,0.5217958,0.044405885,0.120899245,0.009705241,0.11018985,0.004747821],"about_ca_topic_score_codex":0.009735674,"about_ca_topic_score_gemma":0.003511078,"teacher_disagreement_score":0.5965203,"about_ca_system_score_codex":0.00002068967,"about_ca_system_score_gemma":0.000106689295,"threshold_uncertainty_score":0.9968586},"labels":[],"label_agreement":null},{"id":"W7073882120","doi":"","title":"Weight status in individuals with autism spectrum disorder: a study protocol for systematic review and meta-analysis","year":2019,"lang":"en","type":"article","venue":"Queensland's institutional digital repository (The University of Queensland)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Checklist; Observational study; Population; Epidemiology; Systematic review; Public health","score_opus":0.012083651269179554,"score_gpt":0.2194030934075132,"score_spread":0.20731944213833364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073882120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.51523757,0.0024528578,0.0010578424,0.0016190815,0.00019177115,0.45581827,0.0037598377,0.00014638626,0.019716391],"genre_scores_gemma":[0.99793804,0.00001387942,0.00009639627,0.00004036162,0.000011575105,0.00059252355,0.00009622404,0.0000044024423,0.001206602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984936,0.00015920158,0.00036336473,0.00035778005,0.00038434006,0.00024169944],"domain_scores_gemma":[0.9990236,0.00020084502,0.00031271778,0.00032292074,0.000054370896,0.00008552216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028799745,0.00021866476,0.0011075842,0.0001343959,0.00023183555,0.00009246141,0.00025576056,0.000050983366,0.0001994058],"category_scores_gemma":[0.000015818507,0.0001288809,0.000246139,0.0003118201,0.0001748934,0.00042017052,0.00003833532,0.0000865172,0.000021707727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030999197,0.0003341381,0.9476356,0.019261675,0.026288936,0.00005960217,0.0006795243,0.0028596004,0.0000019300514,0.0024099227,0.00014695866,0.0000121079065],"study_design_scores_gemma":[0.0049568545,0.0015735984,0.87756073,0.00175176,0.10401155,0.000059192113,0.00070739456,0.00045644358,0.000011769791,0.0012556954,0.0067538638,0.00090115593],"about_ca_topic_score_codex":0.0025597785,"about_ca_topic_score_gemma":0.0018162539,"teacher_disagreement_score":0.4827005,"about_ca_system_score_codex":0.0000111995805,"about_ca_system_score_gemma":0.00012852855,"threshold_uncertainty_score":0.5255611},"labels":[],"label_agreement":null},{"id":"W7073889129","doi":"","title":"Modelling the impact of compliance with dietary recommendations on cancer and cardiovascular disease mortality in Canada","year":2014,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Disease; Guideline; Dietary salt; Compliance (psychology); Cancer; Risk assessment; Relative risk; Estimation","score_opus":0.0488745575479854,"score_gpt":0.25250714621007336,"score_spread":0.20363258866208797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073889129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99339896,0.00006454808,0.0013071154,0.0002815324,0.000026049254,0.00026001595,0.0014513487,0.0000051249954,0.0032052787],"genre_scores_gemma":[0.99819726,0.0012208391,0.00038479976,0.0000051731777,0.000013083765,7.098387e-8,0.000095299656,0.0000030043573,0.00008049869],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9984701,0.00037522588,0.00008396042,0.00029013565,0.00044882708,0.00033172473],"domain_scores_gemma":[0.9989234,0.00029515897,0.00007339892,0.0003811971,0.00011707073,0.00020972516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004873811,0.00011852895,0.00028605977,0.00014635018,0.00040618115,0.00001277117,0.00047670724,0.000021786402,0.00016340501],"category_scores_gemma":[0.000011584876,0.000099175726,0.00010149503,0.00034053254,0.00038442272,0.00021402737,0.000100677076,0.00022247815,6.6761146e-7],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007634257,0.00003672874,0.36468202,0.00008661305,0.00034097303,0.000042486972,0.00043849417,0.6271227,0.000014103997,0.00043515212,0.0002535709,0.0057837428],"study_design_scores_gemma":[0.00062598946,0.0002120529,0.7761788,0.00014187366,0.00006527663,5.634798e-7,0.0016475553,0.21384613,0.0000043727423,0.00076182577,0.006363866,0.00015170542],"about_ca_topic_score_codex":0.9615874,"about_ca_topic_score_gemma":0.8262981,"teacher_disagreement_score":0.41327655,"about_ca_system_score_codex":0.000048592265,"about_ca_system_score_gemma":0.00065447594,"threshold_uncertainty_score":0.40442687},"labels":[],"label_agreement":null},{"id":"W7073891157","doi":"","title":"Malignant Hyperthermia in the Post-Genomics Era: New Perspectives on an Old Concept","year":2018,"lang":"en","type":"article","venue":"White Rose Research Online (University of Leeds, The University of Sheffield, University of York)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Institutes of Health; University of Toronto; Johns Hopkins University","keywords":"Malignant hyperthermia; Malignant disease; Malignant cells; Cancer; Connection (principal bundle); MEDLINE","score_opus":0.029862732569893656,"score_gpt":0.23655633540758517,"score_spread":0.2066936028376915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073891157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894778,0.00014809347,0.0001395391,0.003994872,0.00007814211,0.00039942886,0.0005459878,0.000020266898,0.005195876],"genre_scores_gemma":[0.9953684,0.0006204546,0.0010555421,0.000043327225,0.000102138074,2.2836153e-9,0.00009220892,0.0000054806687,0.0027124155],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.9975898,0.00071082026,0.00013733552,0.00044085176,0.00066353363,0.00045764577],"domain_scores_gemma":[0.99804896,0.00040866967,0.00021134864,0.0006720994,0.00047161456,0.0001872968],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010065708,0.0001931391,0.0004234642,0.00036627604,0.0008466876,0.000022011367,0.0021495582,0.00020180774,0.002403837],"category_scores_gemma":[0.000035607685,0.00018063943,0.00018552512,0.0006879735,0.0020567388,0.00038145925,0.00022687238,0.0005264031,0.000054810087],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01424815,0.0030421556,0.03477055,0.00033223978,0.001051645,0.0008032124,0.8332645,0.0093413405,0.01786568,0.014878723,0.02058087,0.049820926],"study_design_scores_gemma":[0.0031830987,0.0034730562,0.22610272,0.00022056254,0.00016909133,0.000010920713,0.7300461,0.0030350252,0.0002851932,0.00040182174,0.032570504,0.0005019215],"about_ca_topic_score_codex":0.08805369,"about_ca_topic_score_gemma":0.0517647,"teacher_disagreement_score":0.19133218,"about_ca_system_score_codex":0.00003963442,"about_ca_system_score_gemma":0.0003817723,"threshold_uncertainty_score":0.9985081},"labels":[],"label_agreement":null},{"id":"W7073900555","doi":"","title":"Sleep characteristics and health-related quality of life in 9- to 11-year-old children from 12 countries","year":2020,"lang":"","type":"article","venue":"Civil War Book Review","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sleep (system call); Actigraphy; Multilevel model; Sleep debt; Quality of life (healthcare); Association (psychology); Insomnia","score_opus":0.03028189926335788,"score_gpt":0.2530591062132791,"score_spread":0.2227772069499212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073900555","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.33629817,0.6445945,0.000009546247,0.01269588,0.00043042493,0.0014935918,0.004297719,0.00002368075,0.00015651301],"genre_scores_gemma":[0.52244735,0.44974875,0.000059197762,0.026790915,0.0002609402,0.0000057213438,0.0005943094,0.00001512817,0.000077675475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.995748,0.0006278658,0.0020847495,0.000648308,0.00041268417,0.00047838088],"domain_scores_gemma":[0.9977339,0.00018434129,0.0008812631,0.00041941923,0.0000724451,0.00070866646],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014333287,0.00037538126,0.0022020475,0.000041402058,0.00011221191,0.00006429225,0.00036836954,0.00013622075,0.006941057],"category_scores_gemma":[0.00034124157,0.00034063275,0.00012345775,0.0002606384,0.0001362983,0.00022171055,0.00010976333,0.00020900201,0.0005210087],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002575094,0.00012021028,0.9047926,0.02171007,0.00031855085,0.00001382862,0.0032583151,0.000026224086,0.00007495217,0.0005561098,0.056968987,0.011902636],"study_design_scores_gemma":[0.0005565511,0.00023769423,0.8372364,0.004197622,0.000112060006,8.468159e-7,0.000013587187,0.00005179809,0.000012509583,0.00006312069,0.15708867,0.00042913167],"about_ca_topic_score_codex":0.015680347,"about_ca_topic_score_gemma":0.0023513306,"teacher_disagreement_score":0.1948457,"about_ca_system_score_codex":0.000008027834,"about_ca_system_score_gemma":0.00019910798,"threshold_uncertainty_score":0.9999046},"labels":[],"label_agreement":null},{"id":"W7073902070","doi":"","title":"An investigation into a sustainable AMS food delivery system","year":2014,"lang":"en","type":"report","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sustainability; Environmentally friendly; Certification; Food delivery; Stakeholder; Food systems; Delivery system; Greenwashing","score_opus":0.008351581068483023,"score_gpt":0.1630622818282211,"score_spread":0.15471070075973808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073902070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99277264,0.0003587617,0.00006326237,0.0000086780265,0.0006928377,0.00037314137,0.0007856243,0.000113478534,0.0048315492],"genre_scores_gemma":[0.99602246,0.00019405536,0.00023335167,0.000012043264,0.00028159958,3.0241017e-7,0.0011922695,0.000012003047,0.0020519414],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99799645,0.0001827125,0.00022935633,0.0005674517,0.0006504208,0.0003736051],"domain_scores_gemma":[0.99812,0.00004192233,0.0004314693,0.0004408162,0.0007087729,0.00025701127],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00075271085,0.000097009026,0.0005880786,0.00008003191,0.00042105064,0.00033230858,0.00053929293,0.000342304,0.00027392025],"category_scores_gemma":[0.000024049683,0.00030853704,0.00013695857,0.0002158671,0.00021952324,0.00054337183,0.000057066627,0.00016104685,0.00006951631],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006820006,0.00015860824,0.14847927,0.020290809,0.00077184796,0.0018380149,0.0018453967,0.00094526,0.00039232316,0.00002839173,0.07578528,0.74939656],"study_design_scores_gemma":[0.0003062138,0.00036315777,0.9877408,0.00046926393,0.00016324091,0.00006039313,0.0023559057,0.0003313808,0.0000012477311,0.00037406382,0.0074350117,0.00039930313],"about_ca_topic_score_codex":0.9119993,"about_ca_topic_score_gemma":0.75362545,"teacher_disagreement_score":0.83926153,"about_ca_system_score_codex":0.000055237266,"about_ca_system_score_gemma":0.00073175365,"threshold_uncertainty_score":0.9999367},"labels":[],"label_agreement":null},{"id":"W7073902228","doi":"","title":"Ethnic Background Is a Potential Barrier to Living Donor Kidney Transplantation in Canada: A Single-Center Retrospective Cohort Study","year":2017,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Astellas Pharma","keywords":"Ethnic group; Retrospective cohort study; Referral; Kidney transplantation; Transplantation; Proportional hazards model; Cohort study; Cohort","score_opus":0.01574603100716825,"score_gpt":0.21053770022890614,"score_spread":0.19479166922173788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073902228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97920406,0.000017032955,0.00001749446,0.0002826147,0.00054682454,0.00073750265,0.01294445,0.000040147163,0.0062098894],"genre_scores_gemma":[0.998141,0.000006676436,0.00006291237,0.00076031574,0.00018374716,0.000012010148,0.00050391327,0.000020243448,0.0003091807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99787027,0.000110608555,0.00040671765,0.00058268034,0.00051303353,0.0005166885],"domain_scores_gemma":[0.99877805,0.000061690196,0.0001590243,0.00046853526,0.000033947388,0.00049873424],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025409658,0.0002780572,0.00037796827,0.00009967845,0.0003130968,0.0020941228,0.00061674166,0.0000775319,0.0028051126],"category_scores_gemma":[0.00012838258,0.00025338313,0.0000734696,0.00015762194,0.000040071376,0.0032717176,0.00007989732,0.00024124517,0.0005967145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012954048,0.000093449686,0.9978507,0.000023121092,0.00004494123,0.00012966801,0.00013149015,0.000026640446,0.000092655275,0.0000062324175,0.000643833,0.00082769303],"study_design_scores_gemma":[0.00048339937,0.000134761,0.9961775,0.000088003806,0.000026117603,0.000006674879,0.0000734364,0.00007224115,0.00018242546,0.0002562412,0.0021592253,0.00034000157],"about_ca_topic_score_codex":0.18981254,"about_ca_topic_score_gemma":0.33573815,"teacher_disagreement_score":0.14592561,"about_ca_system_score_codex":0.000045276436,"about_ca_system_score_gemma":0.0003896599,"threshold_uncertainty_score":0.99999183},"labels":[],"label_agreement":null},{"id":"W7073905388","doi":"","title":"Microarray analysis for identification of Plasmodium-refractoriness candidate genes in mosquitoes","year":2004,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Expressed sequence tag; Anopheles; Gene; Aedes aegypti; Complementary DNA; Population; Transcriptome; Malaria; Parasite hosting; cDNA library","score_opus":0.010683444806928958,"score_gpt":0.20802935146804327,"score_spread":0.19734590666111432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073905388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98468333,0.00016081946,0.0004633345,0.000119269615,0.00021066943,0.00025872493,0.013712086,0.00004495948,0.00034678972],"genre_scores_gemma":[0.99536186,0.000026285426,0.00040865826,0.000033834753,0.000098695265,0.000007910066,0.0039275796,0.000011168593,0.00012400873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99855214,0.00003376064,0.0005565822,0.00034600138,0.00020779273,0.00030369303],"domain_scores_gemma":[0.9992574,0.00009389912,0.00022590237,0.000269227,0.00003889742,0.00011466295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019781203,0.00018344706,0.00035747906,0.0002665026,0.00007063829,0.00051674014,0.00036101704,0.00009193671,0.00026179344],"category_scores_gemma":[0.000056474943,0.00015649073,0.00015438143,0.000715839,0.000056328772,0.001954751,0.000025992911,0.000078559184,0.0001907976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023421472,0.00011778804,0.9668921,0.00013171001,0.0002014367,0.0000073407714,0.000060492628,0.014606815,0.01394916,0.00043623612,0.00004404425,0.0033186413],"study_design_scores_gemma":[0.0010520575,0.000091843154,0.8047885,0.000044332508,0.00015811338,0.0000015081827,0.00003728139,0.0003354698,0.15872467,0.01567575,0.018601548,0.0004889396],"about_ca_topic_score_codex":0.0003246623,"about_ca_topic_score_gemma":0.00020977759,"teacher_disagreement_score":0.16210364,"about_ca_system_score_codex":0.0000049877326,"about_ca_system_score_gemma":0.00007675377,"threshold_uncertainty_score":0.6381507},"labels":[],"label_agreement":null},{"id":"W7073912810","doi":"","title":"PCV-2 genotype definition and nomenclature","year":2008,"lang":"en","type":"article","venue":"Ghent University Academic Bibliography (Ghent University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Nomenclature; Genotype; Identification (biology); Association (psychology)","score_opus":0.02248631109573826,"score_gpt":0.16804875308446054,"score_spread":0.14556244198872229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073912810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97251004,0.0006449791,0.00041558951,0.0002724628,0.00037996742,0.00023728222,0.00039814075,0.00015702566,0.024984518],"genre_scores_gemma":[0.9700591,0.027912114,0.000648361,0.00014551001,0.00011370475,3.080931e-8,0.00018489263,0.0000058911505,0.0009304284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984512,0.00013297917,0.00013980136,0.0004942427,0.00033262226,0.00044920153],"domain_scores_gemma":[0.9991493,0.000082956176,0.00014597032,0.00021676043,0.00008272198,0.00032226124],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00013469238,0.0002469475,0.00026874527,0.0068556922,0.0007447241,0.000030401654,0.00047202074,0.0003233621,0.00064230623],"category_scores_gemma":[0.0000038015519,0.00027483396,0.00015757767,0.008150541,0.00035397717,0.0008270923,0.00009977871,0.00043314398,0.00010206545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00076553103,0.000105954095,0.93041795,0.00010599382,0.0003983707,0.0009678355,0.0011513624,0.00025292332,0.0020038,0.028680399,0.033719074,0.001430821],"study_design_scores_gemma":[0.0012579157,0.00016454494,0.63228387,0.00003988843,0.00018961345,0.000038208906,0.0004947019,0.00006932186,0.00010203129,0.0020698595,0.36272022,0.00056982494],"about_ca_topic_score_codex":0.0012645954,"about_ca_topic_score_gemma":0.00009484534,"teacher_disagreement_score":0.32900116,"about_ca_system_score_codex":0.000010290845,"about_ca_system_score_gemma":0.000049911916,"threshold_uncertainty_score":0.9999704},"labels":[],"label_agreement":null},{"id":"W7073924904","doi":"","title":"Quantifying the surface properties of enzymatically-made porous starches by using a surface energy analyzer","year":2018,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Porosity; Surface (topology); Spectrum analyzer; Surface energy; Energy (signal processing); Surface roughness","score_opus":0.051555478948202685,"score_gpt":0.2424029394600389,"score_spread":0.1908474605118362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073924904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99722385,0.00065071497,0.00050297385,0.00017625249,0.00018240647,0.00008701186,0.00006038616,0.000027317128,0.001089102],"genre_scores_gemma":[0.9975647,0.00003256998,0.0016371228,0.000108921486,0.0000758545,1.5765144e-7,0.000013497356,0.0000052275122,0.0005619888],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9987817,0.00015648843,0.0002870352,0.00019743473,0.0002789897,0.0002983605],"domain_scores_gemma":[0.9993843,0.00009804552,0.00010854001,0.00025200908,0.00009307813,0.00006403979],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042258497,0.00013905387,0.00024464662,0.000015203942,0.00019838731,0.000096399155,0.0002762757,0.000049935566,0.001224412],"category_scores_gemma":[0.000027094618,0.00007462052,0.000042053704,0.00015179256,0.00028697783,0.00016613655,0.00003126443,0.00004522077,0.000042257743],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009168498,0.000039170696,0.012370425,0.000077959456,0.00011795569,0.0000020311647,0.0011691868,0.00574178,0.9772569,0.00077364745,0.001468397,0.00089084776],"study_design_scores_gemma":[0.00027785887,0.00026929798,0.00467009,0.00009354508,0.000094942814,0.000007350621,0.0008366778,0.07972276,0.9054488,0.00052677206,0.0075703934,0.00048152363],"about_ca_topic_score_codex":0.036811844,"about_ca_topic_score_gemma":0.0025569366,"teacher_disagreement_score":0.07398099,"about_ca_system_score_codex":0.0000019246415,"about_ca_system_score_gemma":0.00005646098,"threshold_uncertainty_score":0.9996886},"labels":[],"label_agreement":null},{"id":"W7073933527","doi":"","title":"Prediction of Women's Utilization of Resistance Strategies in a Sexual Assault Situation A Prospective Study","year":2008,"lang":"en","type":"article","venue":"University of New Hampshire Scholars Repository (University of New Hampshire at Manchester)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sexual assault; Interim; Resistance (ecology); Assertiveness; Aggression; Poison control; Quarter (Canadian coin); Human factors and ergonomics","score_opus":0.028697879129475454,"score_gpt":0.19788274077488718,"score_spread":0.16918486164541174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073933527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974944,0.00010540041,0.0003400463,0.000030525884,0.00013476334,0.0005456236,0.00010805896,0.00003420244,0.0012069849],"genre_scores_gemma":[0.9960372,0.000056069537,0.00078072323,0.000002920384,0.000031394997,5.249484e-8,0.000065139095,0.000006255002,0.0030202884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979757,0.00024092406,0.00037061409,0.00047269437,0.0006598973,0.00028017105],"domain_scores_gemma":[0.9982317,0.00008929017,0.00078375655,0.00041070214,0.00030184395,0.00018271733],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00036806377,0.00021732943,0.00061047607,0.0002622376,0.00030578746,0.00001668595,0.00045668645,0.00019909287,0.00018236804],"category_scores_gemma":[0.00003463918,0.00028101946,0.00010444767,0.0005649202,0.00030692253,0.0015166916,0.00009425811,0.00018549174,0.000006510191],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029877636,0.00051660446,0.84243804,0.00032826507,0.00028189938,0.000172678,0.1207652,0.0021870665,0.028662875,0.00008036721,0.00071423664,0.0008650013],"study_design_scores_gemma":[0.002278733,0.0006913259,0.9359065,0.00012228818,0.000080409496,0.0000080680165,0.05874357,0.00016199624,0.0010145772,0.00014790423,0.0006536851,0.00019093209],"about_ca_topic_score_codex":0.011506732,"about_ca_topic_score_gemma":0.011021917,"teacher_disagreement_score":0.09346847,"about_ca_system_score_codex":0.00012080364,"about_ca_system_score_gemma":0.000561603,"threshold_uncertainty_score":0.9999642},"labels":[],"label_agreement":null},{"id":"W7073941403","doi":"","title":"Nunaup rkuanguniata mikhanut unikkat : Frozen-Ground Cartoons ; an international collaboration between artists and permafrost scientists","year":2020,"lang":"iu","type":"book","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Outreach; Circumpolar star; Climate change; Multidisciplinary approach; Work (physics); The arts; Craft; Global warming","score_opus":0.052765029260773776,"score_gpt":0.33927050645193224,"score_spread":0.2865054771911585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073941403","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17687517,0.00077499123,0.0007335094,0.031468995,0.0061707594,0.0072451085,0.76728415,0.00027744175,0.009169877],"genre_scores_gemma":[0.17027062,0.0014825027,0.0032338444,0.0007372473,0.00637738,0.00020524397,0.7493853,0.000107180385,0.06820066],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.98882544,0.0010761281,0.0012989059,0.002955729,0.003854104,0.0019897083],"domain_scores_gemma":[0.9910626,0.0011658557,0.00083907566,0.0017241219,0.0032093804,0.0019989721],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.005908686,0.0007702863,0.00085728616,0.001233858,0.0028694645,0.006820323,0.0035255025,0.00042660366,0.0031516855],"category_scores_gemma":[0.002023012,0.0007594743,0.00015189614,0.002151812,0.0020116006,0.0065001864,0.0009497008,0.00083149294,0.00080117176],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006729059,0.000837503,0.051610723,0.0018137317,0.0004963413,0.0001005608,0.008651105,0.00005621203,0.0050646383,0.055614065,0.8473388,0.027743403],"study_design_scores_gemma":[0.0009865871,0.00032617393,0.04588663,0.00017672301,0.00011448067,0.000010839179,0.0005471981,0.008063259,0.0002768688,0.0015652409,0.9411734,0.00087259937],"about_ca_topic_score_codex":0.005063057,"about_ca_topic_score_gemma":0.010037665,"teacher_disagreement_score":0.093834594,"about_ca_system_score_codex":0.00019790263,"about_ca_system_score_gemma":0.0033178588,"threshold_uncertainty_score":0.9999768},"labels":[],"label_agreement":null},{"id":"W7073943277","doi":"","title":"Role of Indigenous health workers in the delivery of comprehensive primary health care in Canada, Australia, and New Zealand: a scoping review protocol","year":2021,"lang":"en","type":"article","venue":"ResearchOnline - JCU (James Cook University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Indigenous; Health care; Workforce; Mainstream; Government (linguistics); Population health; Health policy; HRHIS; Primary health care","score_opus":0.029206744399252228,"score_gpt":0.2926791317574523,"score_spread":0.26347238735820006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073943277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9671383,0.010029616,8.161247e-7,0.0014940571,0.000027815135,0.02063025,0.00042352258,0.0000049322216,0.0002507211],"genre_scores_gemma":[0.92787313,0.053292766,0.0044314493,0.0063160574,0.00034496785,0.00028417064,0.002909382,0.000048878064,0.0044991947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982393,0.0005680467,0.00029754496,0.00020878114,0.0003397758,0.0003465546],"domain_scores_gemma":[0.9992275,0.00016596734,0.00016866946,0.00019250749,0.0000978912,0.00014744239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025911108,0.00010107386,0.00044434695,0.00014435321,0.00007904524,0.000015095169,0.0002409894,0.000028720846,0.000118013515],"category_scores_gemma":[0.000011966044,0.000086619504,0.00003008089,0.00060062227,0.00007262225,0.00008826957,0.000053295676,0.00017569865,9.636311e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002050432,0.00033492956,0.7347743,0.063646436,0.00017886052,0.0010616735,0.018488733,0.0031847209,0.0005242368,0.00008632174,0.013129149,0.1625402],"study_design_scores_gemma":[0.003449929,0.0012681544,0.8022842,0.027060617,0.000023387545,0.00002059911,0.017525641,0.000047704933,0.00019266552,0.000048090882,0.14762612,0.00045290985],"about_ca_topic_score_codex":0.9460107,"about_ca_topic_score_gemma":0.9678499,"teacher_disagreement_score":0.16208729,"about_ca_system_score_codex":0.00007875798,"about_ca_system_score_gemma":0.009920339,"threshold_uncertainty_score":0.9956925},"labels":[],"label_agreement":null},{"id":"W7073948440","doi":"","title":"Obesity in Canadian children","year":2001,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Obesity; Population; Disease; Overweight; Public health","score_opus":0.008159659866415047,"score_gpt":0.17247444897551628,"score_spread":0.16431478910910124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073948440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97975075,0.00020667203,0.0000013586169,0.00028442117,0.0006798227,0.00024684062,0.00012504421,0.00003155415,0.01867352],"genre_scores_gemma":[0.99835384,0.0002579515,0.000032452568,0.00023866213,0.00031020396,0.0000016131023,0.0001163139,0.0000056258496,0.00068334624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99818945,0.000096708165,0.00016528154,0.0002525063,0.00014339035,0.0011526449],"domain_scores_gemma":[0.999123,0.000015928808,0.000035200253,0.00019925095,0.000016334105,0.00061029353],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002822904,0.00012677714,0.00014965421,0.0000801001,0.00008489785,0.00008766364,0.00026652886,0.000042217773,0.0018845488],"category_scores_gemma":[0.00004316986,0.00011182099,0.000027393362,0.00030169202,0.000029826104,0.00015078185,0.000010350063,0.000099801946,0.0007328621],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008633371,0.000011427037,0.9923529,0.0000022031268,0.0000067784495,0.00009388815,0.00022254177,0.00020291598,0.00001362722,0.00008148103,0.00076467334,0.006238953],"study_design_scores_gemma":[0.00015234301,0.000009973805,0.89259326,0.000004570795,0.000004812506,0.000009761417,0.000002790454,0.00002752762,0.00007350659,0.0000795093,0.106910855,0.00013106971],"about_ca_topic_score_codex":0.5849902,"about_ca_topic_score_gemma":0.64034843,"teacher_disagreement_score":0.10614618,"about_ca_system_score_codex":0.000011912546,"about_ca_system_score_gemma":0.00012925535,"threshold_uncertainty_score":0.99902785},"labels":[],"label_agreement":null},{"id":"W7073948448","doi":"","title":"Health-related Quality of Life in Canadian Adolescents and Young Adults: Normative Data Using the SF-36","year":2009,"lang":"en","type":"article","venue":"PubMed Central","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Normative; Quality of life (healthcare); Quality (philosophy); Young adult","score_opus":0.03418713250127116,"score_gpt":0.24131957782015154,"score_spread":0.20713244531888036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073948448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968141,0.00055166945,0.0000036282515,0.0008043497,0.0004322664,0.00031168424,0.00091472437,0.000005915837,0.0001616922],"genre_scores_gemma":[0.9992525,0.000061286475,0.000035322933,0.0003677993,0.00005886093,4.033714e-7,0.0002187964,0.000001427996,0.0000036178922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99830925,0.00020412818,0.00036011075,0.0001704049,0.00014501438,0.0008110981],"domain_scores_gemma":[0.99913156,0.00002056309,0.00014869864,0.00022741246,0.000013767643,0.00045798006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095938606,0.00008578882,0.00022174846,0.00003912818,0.00009629437,0.000041298437,0.0002611773,0.000038809078,0.000036408794],"category_scores_gemma":[0.00009735877,0.000062309045,0.000013527543,0.00013429469,0.000049240327,0.00023831712,0.000014357923,0.00008987202,0.0000023281991],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078564,0.000014676786,0.98897743,0.00003903873,0.000010615075,0.0000020694865,0.0014765662,0.00026542126,0.0000053986523,0.00005175459,0.00015342016,0.008925026],"study_design_scores_gemma":[0.00030795296,0.0000109579,0.9966672,0.00003663414,0.0000037572224,0.000001291622,0.00013107112,0.0025021594,0.000004899573,0.000096739655,0.00016580422,0.00007152791],"about_ca_topic_score_codex":0.8641696,"about_ca_topic_score_gemma":0.8071064,"teacher_disagreement_score":0.057063226,"about_ca_system_score_codex":0.000016028876,"about_ca_system_score_gemma":0.00027234765,"threshold_uncertainty_score":0.2540889},"labels":[],"label_agreement":null},{"id":"W7073952409","doi":"","title":"Epithelial Mesenchymal Transition in Respiratory Disease:Fact or Fiction","year":2020,"lang":"en","type":"article","venue":"UWA Profiles and Research Repository (UWA)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centre for Global Health Research","funders":"","keywords":"Wound healing; Epithelial–mesenchymal transition; Fibrosis; Extracellular matrix; Pulmonary fibrosis; Mesenchymal stem cell; Regeneration (biology); Lung; Bronchiolitis obliterans","score_opus":0.05074906728092715,"score_gpt":0.28581876683968893,"score_spread":0.23506969955876178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073952409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952577,0.0006484586,0.00001739725,0.0009467103,0.000334,0.00047668078,0.00019062366,0.000045206776,0.0020832224],"genre_scores_gemma":[0.9982823,0.00013584986,0.00004802816,0.00012094971,0.00095629325,0.000014916226,0.00006393711,0.0000076171486,0.0003700914],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.997738,0.0005290688,0.0002828214,0.00044722806,0.0005761159,0.00042677647],"domain_scores_gemma":[0.9991698,0.00013860098,0.000050875697,0.00016859264,0.00008062504,0.0003914773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000636825,0.00014553226,0.00021603022,0.000108958724,0.00040790683,0.00019963783,0.00017018095,0.00009935596,0.00037619402],"category_scores_gemma":[0.00007602713,0.00010471722,0.000050424824,0.00026778886,0.00016870549,0.0003042955,0.000027613527,0.00028275658,0.00006143898],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008012641,0.00035108218,0.08305021,0.0022764932,0.00016667224,0.0030091607,0.008128125,0.0025853335,0.8457861,0.0010826637,0.01684535,0.028706174],"study_design_scores_gemma":[0.0013816997,0.0014312809,0.65671366,0.00020850908,0.00003659149,0.000013836073,0.0009633083,0.009773,0.27342921,0.00050950097,0.05496989,0.0005694916],"about_ca_topic_score_codex":0.0009829383,"about_ca_topic_score_gemma":0.000010329259,"teacher_disagreement_score":0.5736635,"about_ca_system_score_codex":0.0000072673784,"about_ca_system_score_gemma":0.00018396998,"threshold_uncertainty_score":0.42702442},"labels":[],"label_agreement":null},{"id":"W7073952555","doi":"","title":"The dangers of substance abuse in adolescents with chronic kidney disease: a review of the literature","year":2012,"lang":"en","type":"article","venue":"Rare & Special e-Zone (The Hong Kong University of Science and Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Public health; Substance abuse; Kidney disease; Drug; Nephrology; Addiction; Polysubstance dependence; Alcohol abuse; Obligation","score_opus":0.003569100541092265,"score_gpt":0.16635727913414117,"score_spread":0.1627881785930489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073952555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899777,0.008354783,0.0000028112804,0.0009968301,0.00017536202,0.00024633305,0.000050317853,0.0000072328235,0.00018860651],"genre_scores_gemma":[0.99174535,0.00808198,0.000025595773,0.000032367654,0.000053517575,1.212885e-7,0.0000019060072,0.0000012266764,0.00005793731],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991687,0.000036004814,0.0001107196,0.00014448978,0.00031168037,0.00022842674],"domain_scores_gemma":[0.99929744,0.000016413202,0.00017632688,0.00031459253,0.00012865916,0.000066551365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042830216,0.0000807043,0.00016727406,0.00007638454,0.00032015363,0.000012790195,0.00074812584,0.00004013075,0.000031674284],"category_scores_gemma":[0.000034977606,0.00004241331,0.000028487935,0.0014548554,0.0027024478,0.00027459516,0.00003391637,0.00011984874,0.0000020990872],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032645173,0.0001458941,0.95148826,0.0027847285,0.00004284817,0.000024579866,0.005761699,0.000028347305,0.004981342,0.005171746,0.0014499584,0.027794126],"study_design_scores_gemma":[0.0005507659,0.00010280662,0.9587342,0.010433739,0.000076297016,0.0000051285338,0.0009315069,0.000021276104,0.0024848005,0.00028649293,0.026183622,0.00018933328],"about_ca_topic_score_codex":0.00014210229,"about_ca_topic_score_gemma":0.000837922,"teacher_disagreement_score":0.027604792,"about_ca_system_score_codex":0.000009615872,"about_ca_system_score_gemma":0.00016333297,"threshold_uncertainty_score":0.99572814},"labels":[],"label_agreement":null},{"id":"W7073959718","doi":"","title":"A Multiparous Woman with Lately Diagnosed Multilevel Left Ventricular Obstruction","year":2017,"lang":"en","type":"report","venue":"eCommons - AKU (Aga Khan University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Stenosis; Coarctation of the aorta; Blood pressure; Ventricular pressure; Cardiac catheterization; Unstable angina; Heart murmur; Aortography","score_opus":0.024552294945941182,"score_gpt":0.21147787634018406,"score_spread":0.18692558139424287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073959718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8964473,0.00037037264,0.00006568352,0.00009252347,0.0038709724,0.00091829716,0.0024393264,0.00025363077,0.095541894],"genre_scores_gemma":[0.9726141,0.0006550695,0.0004793703,0.000014860427,0.00062729296,7.032926e-7,0.0017193703,0.000029960933,0.023859235],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.997644,0.00015409745,0.0002799327,0.0007224485,0.00060165225,0.0005978564],"domain_scores_gemma":[0.99779654,0.0001315285,0.00066478853,0.00087582436,0.00023213432,0.0002991765],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025831,0.0005055108,0.00076317345,0.00043749815,0.00082631194,0.00024625484,0.00087473856,0.0004183127,0.0011652417],"category_scores_gemma":[0.00006513605,0.00046242963,0.00021314123,0.00015775443,0.00018828761,0.00045047174,0.000100577236,0.00041430077,0.00033025327],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020360472,0.00097428187,0.7064668,0.0018910777,0.0050486764,0.07499261,0.0023471604,0.011147945,0.00021944096,0.0003011166,0.09761372,0.096961126],"study_design_scores_gemma":[0.00094341865,0.00019986347,0.27724344,0.0002030081,0.00033169083,0.00014980944,0.00007692765,0.00018046846,0.00010060628,0.000033636912,0.7198162,0.0007208966],"about_ca_topic_score_codex":0.018443558,"about_ca_topic_score_gemma":0.020629328,"teacher_disagreement_score":0.6222025,"about_ca_system_score_codex":0.00006383588,"about_ca_system_score_gemma":0.0006026508,"threshold_uncertainty_score":0.99978274},"labels":[],"label_agreement":null},{"id":"W7073960452","doi":"","title":"The posteromedial corner of the knee: an international expert consensus statement on diagnosis, classification, treatment, and rehabilitation","year":2020,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fowler Kennedy Sport Medicine Clinic","funders":"","keywords":"Rehabilitation; Delphi method; Statement (logic); Delphi; Arthroscopy; Inclusion (mineral); MEDLINE","score_opus":0.08969887026497006,"score_gpt":0.30049745132498495,"score_spread":0.2107985810600149,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073960452","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99479246,0.000033222288,0.00000365625,0.0040072855,0.0004837864,0.0003143367,0.0002479004,0.000021358876,0.00009596634],"genre_scores_gemma":[0.9992192,0.00013569323,0.000016026843,0.00028043863,0.00010721027,0.0000014092366,0.000059330323,0.000005035554,0.00017566077],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99880177,0.0003206893,0.00020651748,0.0002853902,0.00022891513,0.00015670621],"domain_scores_gemma":[0.99897337,0.00036315565,0.00018555838,0.00026204443,0.00008568277,0.00013016495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017638814,0.00013994507,0.00014015098,0.000046101588,0.00024275458,0.000159381,0.00036256356,0.0000529536,0.000046424993],"category_scores_gemma":[0.0000640754,0.00009004171,0.000050445957,0.00011755053,0.00020444245,0.00036459844,0.000043560914,0.00008637576,0.000027106196],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002442857,0.000041386076,0.9952371,0.0000074432355,0.000043468724,0.0000043684754,0.0013095514,0.000046393026,0.00064988737,0.00012919377,0.0000066243397,0.002280279],"study_design_scores_gemma":[0.00061014557,0.0006394359,0.98334455,0.000023929415,0.000025009796,0.0000012816183,0.0005635679,0.0000059738913,0.000770124,0.00006154385,0.013851475,0.00010294802],"about_ca_topic_score_codex":0.000054598786,"about_ca_topic_score_gemma":0.0018740519,"teacher_disagreement_score":0.0138448505,"about_ca_system_score_codex":0.000018460196,"about_ca_system_score_gemma":0.000048469417,"threshold_uncertainty_score":0.36717942},"labels":[],"label_agreement":null},{"id":"W7073966650","doi":"","title":"Search for ZH -> l+l- bbar production in 9.7 fb-1 of ppbar collisions with the D0 detector","year":2013,"lang":"en","type":"article","venue":"Lancaster EPrints (Lancaster University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; Fundação para o Desenvolvimento da UNESP; Centre National de la Recherche Scientifique; Institut National de Physique Nucléaire et de Physique des Particules; Vetenskapsrådet; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Bundesministerium für Bildung und Forschung; Russian Foundation for Basic Research; Fundação Carlos Chagas Filho de Amparo à Pesquisa do Estado do Rio de Janeiro; Korea Science and Engineering Foundation; Department of Science and Technology, Ministry of Science and Technology, India; Grantová Agentura České Republiky; Federal Agency for Science and Innovation; Deutsche Forschungsgemeinschaft; Secretaría de Ciencia y Técnica, Universidad de Buenos Aires; National Science Foundation; Science Foundation Ireland; Departamento Administrativo de Ciencia, Tecnología e Innovación (COLCIENCIAS); Fermilab; Consejo Nacional de Investigaciones Científicas y Técnicas; Fundação de Amparo à Pesquisa do Estado de São Paulo; U.S. Department of Energy","keywords":"Tevatron; Higgs boson; Fermilab; Collider; Branching fraction; Detector; Collider Detector at Fermilab; Standard Model (mathematical formulation)","score_opus":0.014473814040059488,"score_gpt":0.18353475172094827,"score_spread":0.16906093768088878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073966650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99515975,0.000013082514,0.00042190045,0.00040090346,0.00016417309,0.00073193427,0.00006361758,0.000012462079,0.0030322021],"genre_scores_gemma":[0.9960381,0.000007750511,0.00068708207,0.000038313057,0.00009843491,0.0000020969806,0.00001987265,0.0000057651837,0.003102633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99900186,0.00009637226,0.0001381558,0.00029562693,0.00017161045,0.00029639638],"domain_scores_gemma":[0.9993395,0.00008924704,0.00007848775,0.0003126741,0.00010911214,0.00007096202],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001792548,0.00013173152,0.00021420015,0.00014058723,0.00010471506,0.000046349836,0.0003067781,0.000054668606,0.0010920083],"category_scores_gemma":[0.0000053842446,0.00008805422,0.000043344986,0.00033822554,0.00009763933,0.00029758445,0.000042624135,0.00009656962,0.0003013533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006154182,0.00009007113,0.97780806,0.00018130335,0.00009931501,0.000026849259,0.0016765015,0.00027164808,0.0071654688,0.00032788856,0.00067208894,0.011065384],"study_design_scores_gemma":[0.00063501677,0.00015959679,0.9735054,0.00004706569,0.000022575572,0.0000045597253,0.00060819904,0.00042916316,0.0064044567,0.000048230766,0.017977655,0.00015810801],"about_ca_topic_score_codex":0.0011486409,"about_ca_topic_score_gemma":0.001105928,"teacher_disagreement_score":0.017305566,"about_ca_system_score_codex":0.0000067298556,"about_ca_system_score_gemma":0.000037485082,"threshold_uncertainty_score":0.9998211},"labels":[],"label_agreement":null},{"id":"W7073971294","doi":"","title":"Factors Associated with Higher Body Mass Index, Weight Concern, and Weight Gain in a Multinational Cohort Study of Smokers Intending to Quit","year":2009,"lang":"en","type":"article","venue":"RePEc: Research Papers in Economics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Weight gain; Body mass index; Baseline (sea); Cohort study; Cohort; Longitudinal study; Obesity; Body weight; Weight loss","score_opus":0.029522194777278236,"score_gpt":0.2801048849534948,"score_spread":0.25058269017621654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073971294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99380326,0.000011338252,4.9814156e-7,0.00007378001,0.000105518964,0.0005755823,0.00007070444,0.000009784088,0.0053495383],"genre_scores_gemma":[0.9995493,0.00005201879,0.000024021629,0.000029119408,0.00003699954,0.000008458286,0.000058061,0.000006297848,0.00023567371],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99833494,0.0002070808,0.000355831,0.00039487696,0.00028341147,0.00042386365],"domain_scores_gemma":[0.9991458,0.00038570774,0.00010411836,0.00017420619,0.00005398023,0.00013620236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010473299,0.00015231721,0.00036655087,0.00029809136,0.00008238636,0.00006339812,0.00021652244,0.000083554376,0.00026305125],"category_scores_gemma":[0.000114159884,0.00012375526,0.000021124586,0.00022755176,0.00009238327,0.0001623529,0.000030107523,0.00021306453,0.0000017279417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000978925,0.000101527265,0.99349374,0.0000051976153,0.000050277078,0.000011633713,0.0004644523,0.0028202252,0.00023213109,0.00006104105,0.000010337175,0.0026515375],"study_design_scores_gemma":[0.00086457294,0.00043882834,0.99563545,0.00004005874,0.0000051234224,2.0897436e-7,0.0006163561,0.0016924923,0.00011771918,0.00014242006,0.0002944451,0.0001523105],"about_ca_topic_score_codex":0.0010471672,"about_ca_topic_score_gemma":0.0050808946,"teacher_disagreement_score":0.0057460945,"about_ca_system_score_codex":0.000060837327,"about_ca_system_score_gemma":0.00006998465,"threshold_uncertainty_score":0.5046593},"labels":[],"label_agreement":null},{"id":"W7073971510","doi":"","title":"Teaching students the repair of resin-based composite restorations - A survey of North American dental schools","year":2003,"lang":"en","type":"article","venue":"Bristol Research (University of Bristol)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dental education; MEDLINE; Class (philosophy); Educational measurement","score_opus":0.040667677954665936,"score_gpt":0.2913718685472675,"score_spread":0.2507041905926016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073971510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99797684,0.00009239003,0.00013752209,0.000069194815,0.000054010092,0.00029993532,0.0006320925,0.000015716287,0.0007222916],"genre_scores_gemma":[0.99875844,0.000018391262,0.00078538444,0.0000086295595,0.0000097863385,1.5914964e-7,0.00013011221,0.0000044104822,0.00028471957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961023,0.0020626883,0.0002467471,0.0002583647,0.0010396026,0.00029031743],"domain_scores_gemma":[0.9981107,0.00051980186,0.00031497196,0.00047385125,0.00044735058,0.00013329885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027329389,0.00010496582,0.0003518294,0.00021393951,0.00055747,0.000029615318,0.00080189505,0.000032283722,0.00008383058],"category_scores_gemma":[0.00033188637,0.000101601814,0.00010568842,0.0007632266,0.00082095974,0.0001671853,0.00006810208,0.00029562952,0.000026916188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024085985,0.00014680167,0.99464524,0.000052875585,0.00006286186,0.000018152712,0.00026699042,0.0005041598,0.0005002627,0.000059873924,0.0026813168,0.0008205966],"study_design_scores_gemma":[0.0003229752,0.00027505096,0.996082,0.000031363565,0.000023043078,0.0000012070154,0.0007477705,0.0003778936,0.00013354217,0.000022069835,0.0018885983,0.0000944674],"about_ca_topic_score_codex":0.29272702,"about_ca_topic_score_gemma":0.1457037,"teacher_disagreement_score":0.1470233,"about_ca_system_score_codex":0.000021375017,"about_ca_system_score_gemma":0.00032557372,"threshold_uncertainty_score":0.86988497},"labels":[],"label_agreement":null},{"id":"W7073977670","doi":"","title":"Commonality and Biosynthesis of the O-Methyl Phosphoramidate Capsule Modification in Campylobacter jejuni","year":2007,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Campylobacter jejuni; Biosynthesis; Complementation; Strain (injury); Mutant; Bacterial capsule","score_opus":0.013142304900703079,"score_gpt":0.21709900173696778,"score_spread":0.2039566968362647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073977670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99455607,0.000044862474,0.00001372813,0.00022492396,0.000119592594,0.00009353162,0.00010270651,0.000005250629,0.004839359],"genre_scores_gemma":[0.9995952,0.000020348358,0.00025716744,0.000048673162,0.00002210623,3.281031e-7,0.000012976716,0.0000013777066,0.000041779906],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994229,0.00006156368,0.00016089994,0.000109403125,0.00011402686,0.00013122727],"domain_scores_gemma":[0.9996306,0.00007337075,0.00006868159,0.00017450548,0.000019157049,0.000033689474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005267781,0.00005821484,0.00011107973,0.000022326789,0.00004448891,0.000017396707,0.00012856758,0.000038423117,0.0004583658],"category_scores_gemma":[0.000024330091,0.00003818219,0.000019056157,0.000116084186,0.00008214772,0.000059763533,0.000013823082,0.00004429782,0.000012077753],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009313742,0.00008393778,0.39307216,0.00006828698,0.000023730074,0.0000030910942,0.00080562395,0.000114347196,0.5459771,0.003247566,0.00025931344,0.056251712],"study_design_scores_gemma":[0.000074794036,0.000009904239,0.8659826,0.000008785824,0.000005728254,4.6722218e-7,0.000028713554,0.00016838856,0.12799074,0.0045097573,0.0011700165,0.000050101302],"about_ca_topic_score_codex":0.0035233567,"about_ca_topic_score_gemma":0.0017262378,"teacher_disagreement_score":0.47291043,"about_ca_system_score_codex":0.000001641697,"about_ca_system_score_gemma":0.000009467388,"threshold_uncertainty_score":0.53262854},"labels":[],"label_agreement":null},{"id":"W7073978500","doi":"","title":"Mass spectrometric analysis and mutagenesis predict involvement of multiple cysteines in redox regulation of the skeletal muscle ryanodine receptor ion channel complex","year":2011,"lang":"en","type":"other","venue":"Dove Medical Press (Taylor and Francis Group)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ryanodine receptor; RYR1; Cysteine; Skeletal muscle; Mutagenesis; Glutathione; Mutant; Protein subunit","score_opus":0.014680399314962253,"score_gpt":0.19918667859929687,"score_spread":0.1845062792843346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073978500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6891507,0.054919112,0.12638485,0.0005770554,0.010578272,0.0097657805,0.024112971,0.00040545914,0.08410579],"genre_scores_gemma":[0.99865574,0.00009006424,0.00023229957,0.000016498543,0.00029910682,0.000008024371,0.0004856125,0.000024300722,0.00018835832],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9980342,0.00018073464,0.00052818155,0.00040231497,0.00062184106,0.00023275771],"domain_scores_gemma":[0.9989403,0.00013436601,0.00042505658,0.00032448088,0.00003532395,0.00014046117],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045186977,0.00024855128,0.0007616385,0.0003966734,0.000043562522,0.00001737149,0.00028980605,0.00026731024,0.0043492015],"category_scores_gemma":[0.00011233425,0.0001649943,0.00012783479,0.00062832487,0.00028352157,0.000056400466,0.00006721992,0.00012347873,0.0000030678757],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081922713,0.0009842472,0.36087623,0.007776855,0.004818651,0.000033854754,0.0028243584,0.00057484745,0.051832862,0.00087795756,0.0029475393,0.56563336],"study_design_scores_gemma":[0.0018070259,0.00031113147,0.8983106,0.00006240724,0.0007025155,0.0000010768763,0.00006197627,0.09230351,0.0011245131,0.00049997127,0.0043661785,0.0004491046],"about_ca_topic_score_codex":0.017471738,"about_ca_topic_score_gemma":0.0047691856,"teacher_disagreement_score":0.5651843,"about_ca_system_score_codex":0.0000031385482,"about_ca_system_score_gemma":0.0000022528777,"threshold_uncertainty_score":0.99656093},"labels":[],"label_agreement":null},{"id":"W7073982838","doi":"","title":"Paleogene Newfoundland sediment drifts","year":2012,"lang":"en","type":"article","venue":"Open Research Online (The Open University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Paleogene; Sedimentary rock; Drilling; Deposition (geology); Sediment; Deep sea; Ocean current; Current (fluid); Contourite","score_opus":0.11564365817894268,"score_gpt":0.3408574999797622,"score_spread":0.22521384180081955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073982838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.62075543,0.00018468227,0.000013433201,0.0032833056,0.00051672064,0.0018195375,0.00039757908,0.00001723184,0.3730121],"genre_scores_gemma":[0.951365,0.00024153889,0.0009288118,0.00016731389,0.00043601342,0.000001094491,0.00035931915,0.0000072991547,0.046493616],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99780667,0.00061461376,0.00012774511,0.0002908052,0.00046916233,0.0006909889],"domain_scores_gemma":[0.9987359,0.00022691465,0.000059607133,0.00050946843,0.0001303183,0.0003378081],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0020811495,0.00012792276,0.00021389032,0.000114298295,0.00089386536,0.0007391076,0.0034143575,0.000058682916,0.009547764],"category_scores_gemma":[0.000036094105,0.00008963295,0.000038167367,0.0006263421,0.00016232605,0.0012200758,0.0012077519,0.00023973457,0.0011637226],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038482316,0.0022466567,0.6332899,0.000118692486,0.0009614692,0.0005304398,0.003692666,0.0018040575,0.0043796063,0.04623229,0.10945088,0.19344513],"study_design_scores_gemma":[0.00054977724,0.000113505535,0.10251078,0.000016374477,0.00001647406,0.0000030790688,0.00047456636,0.00010443998,0.00014593409,0.0002298144,0.8956858,0.00014949121],"about_ca_topic_score_codex":0.03155509,"about_ca_topic_score_gemma":0.014437128,"teacher_disagreement_score":0.7862349,"about_ca_system_score_codex":0.000017045575,"about_ca_system_score_gemma":0.00020254051,"threshold_uncertainty_score":0.999614},"labels":[],"label_agreement":null},{"id":"W7073988784","doi":"","title":"Screening of cognitive impairment in patients with Parkinson's disease: diagnostic validity of the Brazilian versions of the Montreal Cognitive Assessment and the Addenbrooke's Cognitive Examination-Revised","year":2015,"lang":"en","type":"article","venue":"LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Montreal Cognitive Assessment; Dementia; Cognitive impairment; Cognition; Neuropsychology; Rating scale; Neuropsychological assessment; Cognitive Assessment System; Psychometrics","score_opus":0.016556329902036968,"score_gpt":0.22901751289747158,"score_spread":0.2124611829954346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073988784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944571,0.00010959604,0.00014217423,0.0005379462,0.00019543734,0.0011242377,0.00088352157,0.000009703482,0.0025402731],"genre_scores_gemma":[0.9995848,0.000027341117,0.00006480471,0.000034939214,0.00004691189,0.000039808743,0.00018345736,0.0000066298257,0.000011314562],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972906,0.0009960743,0.00041320254,0.0002891411,0.0007754831,0.00023546488],"domain_scores_gemma":[0.9965861,0.0019390475,0.00053206476,0.00020612677,0.0005732361,0.000163424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007352122,0.00020090693,0.000346603,0.00008563242,0.0002651026,0.00004406794,0.00029318384,0.000081134385,0.00002264041],"category_scores_gemma":[0.0011864076,0.00010845819,0.00009786237,0.00037910655,0.00016343564,0.00020291444,0.00011915053,0.00018783346,4.373441e-7],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018984549,0.0006183413,0.9803093,0.000113184884,0.00022808318,0.000009208288,0.0032991925,0.00026624344,0.000012374913,0.010452515,0.000044318793,0.0027487886],"study_design_scores_gemma":[0.0042861286,0.00014949223,0.99220943,0.00071147684,0.0002430963,0.0000038245535,0.0010150921,0.00034627132,0.0001617401,0.00014232371,0.00059887103,0.00013223938],"about_ca_topic_score_codex":0.000064543034,"about_ca_topic_score_gemma":0.00082889845,"teacher_disagreement_score":0.01190015,"about_ca_system_score_codex":0.00002766096,"about_ca_system_score_gemma":0.0003957228,"threshold_uncertainty_score":0.44227967},"labels":[],"label_agreement":null},{"id":"W7073990219","doi":"","title":"Canadian-American Planning: The Seventh Annual Conference on Canadian-American Relations, 1965","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Exposition (narrative); Work (physics); Period (music)","score_opus":0.01755151322949746,"score_gpt":0.21486696802849267,"score_spread":0.1973154547989952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073990219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.58192366,0.0000013380409,0.000008127432,0.0018399055,0.0004040614,0.00041124274,0.0018995369,0.00013858898,0.41337353],"genre_scores_gemma":[0.9963747,0.0023090942,0.000051037085,0.00038511615,0.00009051636,9.574014e-7,0.00029332223,0.0000093730705,0.00048585588],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983876,0.00019002368,0.00012971526,0.00037271314,0.00023540598,0.0006845416],"domain_scores_gemma":[0.99892217,0.00014647529,0.00011704766,0.00034090295,0.0000816994,0.00039169632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020760846,0.00020730907,0.00023062016,0.0042094025,0.0006313961,0.00011396613,0.0005520992,0.000054552158,0.00034554795],"category_scores_gemma":[0.000039873263,0.00017631074,0.00006562848,0.006441686,0.00020738693,0.00021412766,0.000026966141,0.00020571669,0.00074289617],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006771697,0.0001528706,0.5162962,0.00009005702,0.0010423982,0.0060383906,0.07999661,0.023690086,0.000020479643,0.016643832,0.09563071,0.2597212],"study_design_scores_gemma":[0.0001361274,0.00015230148,0.069664046,0.00001863918,0.000029840654,0.000003126492,0.0026976815,0.00086458714,0.000009811168,0.00000449987,0.9261779,0.00024145075],"about_ca_topic_score_codex":0.99848384,"about_ca_topic_score_gemma":0.9960929,"teacher_disagreement_score":0.83054715,"about_ca_system_score_codex":0.00007191758,"about_ca_system_score_gemma":0.0020262285,"threshold_uncertainty_score":0.9548675},"labels":[],"label_agreement":null},{"id":"W7073991106","doi":"","title":"Carcinogenicity of saccharin in laboratory animals and humans: letter to Dr. Harry Conacher of Health Canada","year":2007,"lang":"en","type":"article","venue":"AUSpace (Athabasca University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Saccharin; Public health; Human health; Unit (ring theory); Sweetening agents; Public interest","score_opus":0.011236288171324067,"score_gpt":0.1974373068514713,"score_spread":0.1862010186801472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073991106","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979804,0.00021405015,0.000034253626,0.00061472337,0.00009516423,0.00013495031,0.00026182662,0.0000052375267,0.0006593868],"genre_scores_gemma":[0.99923694,0.000016996804,0.00013709134,0.00025635274,0.000024092047,3.0907568e-8,0.000008383066,0.000002275644,0.0003178324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991901,0.00008291049,0.00016136067,0.00018074916,0.00015588195,0.00022901769],"domain_scores_gemma":[0.9995195,0.00007062484,0.00011541053,0.00013074827,0.00005208677,0.00011159674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004056554,0.00009054279,0.00025657794,0.00014316563,0.000046729525,0.000006144332,0.00015684897,0.00004223935,0.00018032386],"category_scores_gemma":[0.00001246527,0.00009434598,0.000018708737,0.00027942593,0.000049947488,0.000103902836,0.000031884712,0.00006241406,0.0000025266977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001273996,0.000028351287,0.9695008,0.0001397675,0.000040068713,0.00008518702,0.0020741092,0.00008798237,0.019258099,0.0007696606,0.0072193914,0.0006692185],"study_design_scores_gemma":[0.00028063206,0.0001000927,0.935725,0.000030188698,0.000008160555,2.9731223e-7,0.0006611441,0.0000040526497,0.007471385,0.000015723828,0.05558409,0.00011928415],"about_ca_topic_score_codex":0.8508129,"about_ca_topic_score_gemma":0.94065183,"teacher_disagreement_score":0.08983887,"about_ca_system_score_codex":0.000019242732,"about_ca_system_score_gemma":0.0002625504,"threshold_uncertainty_score":0.38473174},"labels":[],"label_agreement":null},{"id":"W7073992235","doi":"","title":"Politics and Independence- the Collapse of the Canadian Medical Association Journal","year":2006,"lang":"en","type":"other","venue":"DigitalGeorgetown (Georgetown University Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Politics; Association (psychology); Government (linguistics); Field (mathematics)","score_opus":0.003011836118104954,"score_gpt":0.14326964132836387,"score_spread":0.1402578052102589,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073992235","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.013398812,0.00028890933,0.0000010978623,0.006199811,0.0013334849,0.00033098168,0.0024378814,0.00006432086,0.9759447],"genre_scores_gemma":[0.13787194,0.00025608664,0.00003883481,0.00043531603,0.00058760814,1.2496201e-7,0.00018383063,0.00005130301,0.86057496],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99766034,0.00021460144,0.00026195793,0.0002598131,0.001104531,0.00049876276],"domain_scores_gemma":[0.99857,0.00014732004,0.00045832703,0.00032229713,0.000073957985,0.0004280606],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028418525,0.00027105078,0.00036603553,0.00021219124,0.00052364334,0.00034377121,0.0010266774,0.00069759664,0.0064381706],"category_scores_gemma":[0.00008686819,0.0001758391,0.00014579798,0.00038658202,0.00032723797,0.0004162934,0.00012762132,0.0005582866,0.00005952515],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000056102535,0.000011913078,0.09919165,0.00002512899,0.000110791036,0.00005786005,0.000051310144,0.0000080296395,4.890184e-7,0.0029953148,0.8971407,0.00040122878],"study_design_scores_gemma":[0.0002216807,0.000021515185,0.042498615,0.00007869815,0.000060436734,0.000018322356,0.00006390145,0.0000137727775,0.000021064685,0.00085846556,0.9559302,0.00021335542],"about_ca_topic_score_codex":0.13541456,"about_ca_topic_score_gemma":0.2703992,"teacher_disagreement_score":0.13498464,"about_ca_system_score_codex":0.000022194792,"about_ca_system_score_gemma":0.0018692935,"threshold_uncertainty_score":0.99447006},"labels":[],"label_agreement":null},{"id":"W7073995092","doi":"","title":"A 10-year retrospective review of Salmonella infections at the Children's Hospital in London, Ontario","year":2010,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Epidemiology; Antibiotics; Salmonella; Retrospective cohort study; Public health; Medical record; Risk factor","score_opus":0.018271757824095514,"score_gpt":0.23483117815959326,"score_spread":0.21655942033549774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073995092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972065,0.00025912927,0.0000017134586,0.00013533041,0.00040142136,0.00043808244,0.00016356912,0.00003068067,0.0013635353],"genre_scores_gemma":[0.9929447,0.00034515795,0.000008327312,0.00007938483,0.00007951847,5.1681286e-7,0.000101709564,0.000008138444,0.006432529],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985641,0.00016644553,0.00025543268,0.00038909868,0.00030512217,0.00031977924],"domain_scores_gemma":[0.9989503,0.000075230244,0.00022688124,0.00050350005,0.00011972812,0.00012438606],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00043465698,0.00021385957,0.00035496688,0.00014894152,0.00020066474,0.000081852115,0.0005454641,0.00012808671,0.004027216],"category_scores_gemma":[0.00005028588,0.00017729565,0.00012955614,0.00041572863,0.00017224108,0.0006083065,0.00012873272,0.00051094155,0.0007593732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003917672,0.00005160979,0.9993534,0.00006976989,0.00003401557,0.000021521297,0.00014087601,0.000009964879,0.0001515292,0.000027393891,0.00000872324,0.00009201773],"study_design_scores_gemma":[0.00042511645,0.00019310997,0.9939771,0.00032536575,0.00006021163,0.000012266606,0.0000115237835,4.227904e-8,0.00050832727,0.000072859795,0.004201728,0.00021233647],"about_ca_topic_score_codex":0.003185644,"about_ca_topic_score_gemma":0.4902805,"teacher_disagreement_score":0.48709488,"about_ca_system_score_codex":0.000040496103,"about_ca_system_score_gemma":0.00011964827,"threshold_uncertainty_score":0.9968832},"labels":[],"label_agreement":null},{"id":"W7074001598","doi":"","title":"Neuro-ophthalmological manifestations of tuberous sclerosis: current perspectives","year":2019,"lang":"en","type":"review","venue":"Dove Medical Press (Taylor and Francis Group)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tuberous sclerosis; Vigabatrin; Visual field; Optic nerve; Disease; Retinal; Visual system; Multiple sclerosis","score_opus":0.07784057425795271,"score_gpt":0.3028024031241409,"score_spread":0.2249618288661882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074001598","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00020382191,0.99403256,0.0014255666,0.000017536968,0.0016566887,0.0006365096,0.0010136225,0.000034887435,0.0009788336],"genre_scores_gemma":[0.15583405,0.84279424,0.00006390092,0.00003203305,0.0006990297,0.00002954576,0.00052147114,0.000020688523,0.0000050154486],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9971434,0.00026239862,0.0007481057,0.00070710405,0.00071422075,0.0004247868],"domain_scores_gemma":[0.9981914,0.0006750256,0.000331298,0.00039051977,0.00006377163,0.0003479899],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042782613,0.00045106228,0.0016535026,0.0000892564,0.00010653625,0.000082779305,0.0005583602,0.00036916923,0.002523172],"category_scores_gemma":[0.00021639321,0.00029938944,0.0003341481,0.00015214154,0.00035465628,0.00016382542,0.00009975704,0.000546318,0.00013483006],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014795824,0.000099090525,0.00014370724,0.0057223807,0.00009038233,0.00006315077,0.00012927997,0.0000033598612,4.911795e-7,0.00061317446,0.000028536855,0.99309164],"study_design_scores_gemma":[0.0024329145,0.0018664557,0.012449831,0.0024366966,0.004613872,0.0014705989,0.00027612908,0.015586653,0.000002915096,0.003284433,0.9523137,0.0032657688],"about_ca_topic_score_codex":0.00064441387,"about_ca_topic_score_gemma":0.000024212963,"teacher_disagreement_score":0.9898259,"about_ca_system_score_codex":0.0000036572103,"about_ca_system_score_gemma":0.0000082771,"threshold_uncertainty_score":0.9999458},"labels":[],"label_agreement":null},{"id":"W7074009480","doi":"","title":"Land, land banks and land back: Accounting, social reproduction and Indigenous resurgence","year":2021,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Indigenous; Commodification; Aotearoa; Social reproduction; Reproduction; Capitalism; Vanguard; Privilege (computing)","score_opus":0.021053532743200883,"score_gpt":0.21728512822475246,"score_spread":0.19623159548155159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074009480","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9388067,0.0015500115,1.4671912e-7,0.00012497803,0.00020686354,0.00010991422,0.057418343,0.000027281285,0.0017557631],"genre_scores_gemma":[0.96328795,0.00007888976,0.00004468442,0.00009446696,0.0007951517,0.0000031045508,0.03512929,0.0000052326614,0.0005612564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992288,0.0000424567,0.000112828086,0.00030658045,0.00012143115,0.00018795679],"domain_scores_gemma":[0.99965805,0.000045512235,0.000065557455,0.000117424155,0.000058971567,0.000054463926],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009689805,0.00009304247,0.00014191661,0.000020543335,0.00022455584,0.0001899188,0.00005722705,0.00007263605,0.05391869],"category_scores_gemma":[0.00012512036,0.00008156329,0.000017430886,0.00008574609,0.000010052256,0.00016619741,0.000032635584,0.000070552356,0.00050066283],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072252835,0.000029949137,0.83953756,0.0006838398,0.0000686231,0.000149723,0.0022279967,0.00006609674,0.00049435004,0.0000060373495,0.11323318,0.043430414],"study_design_scores_gemma":[0.00017720688,0.000021241436,0.83220154,0.00008932493,0.000009944128,0.000033027904,0.000018810662,0.00003327499,0.0005091668,0.00010287483,0.16664448,0.00015910705],"about_ca_topic_score_codex":0.0007339665,"about_ca_topic_score_gemma":0.0013415405,"teacher_disagreement_score":0.053418025,"about_ca_system_score_codex":0.0000010225024,"about_ca_system_score_gemma":0.00004268991,"threshold_uncertainty_score":0.94694614},"labels":[],"label_agreement":null},{"id":"W7074009642","doi":"","title":"High Quantile Estimation for some Stochastic Volatility Models","year":2011,"lang":"en","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Stochastic volatility; Volatility (finance); Quantile; Financial models with long-tailed distributions and volatility clustering; Estimation; Central limit theorem; Rate of convergence; Asymptotic distribution","score_opus":0.0062938895947004464,"score_gpt":0.14316409464267027,"score_spread":0.13687020504796982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074009642","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011083825,0.0013184558,0.008391769,0.0005267653,0.0029439514,0.0016358488,0.026993556,0.000080427504,0.9470254],"genre_scores_gemma":[0.85187346,0.00006836399,0.0040059546,0.000258995,0.00023676218,0.000007458268,0.0003392793,0.000056636436,0.14315306],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986258,0.000030721152,0.00021292843,0.0002459744,0.00064871716,0.00023584855],"domain_scores_gemma":[0.99932057,0.00012799175,0.00021777519,0.00017752814,3.2386114e-7,0.00015581469],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000010326784,0.0002017881,0.00032926857,0.000021871654,0.00008336678,0.000020594856,0.00018338142,0.000041992145,0.0012015847],"category_scores_gemma":[0.0000016940245,0.00017923498,0.000026020954,0.000023119585,0.000049415656,0.00023913631,0.00002424993,0.00005640134,2.255264e-8],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021501451,0.00010296745,0.0021851226,0.0039116475,0.00084168866,0.000062214036,0.00021021378,0.027249493,0.0010974797,0.68538016,0.22640923,0.05039967],"study_design_scores_gemma":[0.0017450184,0.00053249183,0.025020387,0.0010130949,0.00037230266,0.00000582861,0.00035242274,0.5243916,0.008859954,0.2276467,0.20778392,0.0022763123],"about_ca_topic_score_codex":0.07772726,"about_ca_topic_score_gemma":0.12024912,"teacher_disagreement_score":0.8407897,"about_ca_system_score_codex":6.163638e-7,"about_ca_system_score_gemma":0.0006060637,"threshold_uncertainty_score":0.99971145},"labels":[],"label_agreement":null},{"id":"W7074013687","doi":"","title":"A medicina preventiva","year":2008,"lang":"pt","type":"article","venue":"Revista Portuguesa de Clínica Geral","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Charter; Context (archaeology); Relevance (law); Clinical Practice; Ethical issues; Medical practice; Reflection (computer programming); Medical ethics; Promotion (chess)","score_opus":0.02564761239611017,"score_gpt":0.24191189678059322,"score_spread":0.21626428438448306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074013687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9707886,0.014008683,0.0001802384,0.0011341949,0.0018676682,0.0007907962,0.000712676,0.00015108055,0.010366068],"genre_scores_gemma":[0.96644187,0.004940634,0.0003272951,0.00058207364,0.0016087265,0.0000069111916,0.00045370427,0.000028205362,0.025610596],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9961242,0.00043755426,0.0009374119,0.0007352371,0.00067346654,0.0010921],"domain_scores_gemma":[0.9977982,0.00018184472,0.00043500276,0.00080342294,0.00009742649,0.00068410876],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009808528,0.0004945063,0.0009553456,0.00010545804,0.0004432277,0.00015971097,0.00066691876,0.00027866592,0.010203958],"category_scores_gemma":[0.00013945563,0.00043395304,0.00035366803,0.0003294699,0.00033075013,0.0003098729,0.000082963794,0.000375269,0.0014172429],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00093183154,0.0009476167,0.26685447,0.002407679,0.0011541215,0.008846512,0.0068703964,0.00027192687,0.0054794657,0.0043108324,0.6741674,0.027757736],"study_design_scores_gemma":[0.000935871,0.0004857174,0.28178254,0.0004322841,0.00027818585,0.0005805419,0.00006832415,0.0006145198,0.00015509757,0.00028813008,0.7134949,0.0008838915],"about_ca_topic_score_codex":0.001215759,"about_ca_topic_score_gemma":0.00006327463,"teacher_disagreement_score":0.03932749,"about_ca_system_score_codex":0.00002159945,"about_ca_system_score_gemma":0.0005856033,"threshold_uncertainty_score":0.99981123},"labels":[],"label_agreement":null},{"id":"W7074016878","doi":"","title":"Prevalence and Predictors of Neurocognitive Impairment in Ethiopian Population Living with HIV","year":2020,"lang":"en","type":"other","venue":"Dove Medical Press (Taylor and Francis Group)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Neurocognitive; Psychosocial; Logistic regression; Public health; Human immunodeficiency virus (HIV); Dementia; Population; Disease","score_opus":0.006423742656737126,"score_gpt":0.19763009625936076,"score_spread":0.19120635360262364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074016878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.50336075,0.058226533,0.048766028,0.0017379887,0.009420236,0.014746065,0.017331142,0.0011795686,0.3452317],"genre_scores_gemma":[0.99904037,0.000094182615,0.000083831306,0.00012470955,0.00034418318,0.000008607064,0.00013144397,0.00003279023,0.00013987925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983944,0.00014496814,0.00028987497,0.00043489342,0.00050379767,0.00023205232],"domain_scores_gemma":[0.9992285,0.00019727073,0.00018147977,0.00012637486,0.000012688575,0.0002536906],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024187045,0.00024035067,0.00046000403,0.00007379783,0.000031943742,0.00003423691,0.00015445797,0.00023521,0.0019687705],"category_scores_gemma":[0.00010896619,0.00017279117,0.000028131357,0.00008108239,0.00017975317,0.00008117094,0.000048198817,0.00025605832,0.0000051655184],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016251134,0.00009212627,0.9112332,0.0031338527,0.00012707611,0.00008035876,0.0014420847,0.0000165081,0.000016316018,0.00012681102,0.00036605468,0.08320314],"study_design_scores_gemma":[0.00083918555,0.00050136854,0.9816603,0.00026508994,0.00012403946,0.000007667012,0.00004099797,0.014310381,0.000007814432,0.00010183008,0.001769054,0.00037225656],"about_ca_topic_score_codex":0.005522183,"about_ca_topic_score_gemma":0.0016270201,"teacher_disagreement_score":0.49567965,"about_ca_system_score_codex":0.0000013518014,"about_ca_system_score_gemma":0.0000022262655,"threshold_uncertainty_score":0.99894357},"labels":[],"label_agreement":null},{"id":"W7074018504","doi":"","title":"Chasse aux phoques à l'OMC : bien-être animal et moralité publique en débat","year":2013,"lang":"fr","type":"article","venue":"LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Context (archaeology); Limiting; Public policy","score_opus":0.021014638939616984,"score_gpt":0.24149500210879327,"score_spread":0.2204803631691763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074018504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.62960154,0.0052161966,0.0005234351,0.22748208,0.007619938,0.0020519232,0.0012939925,0.0007429547,0.12546796],"genre_scores_gemma":[0.98781955,0.001019964,0.0028335105,0.0015087236,0.002239084,0.0001707164,0.00085279054,0.000065989356,0.0034896578],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99289304,0.001545615,0.0011787821,0.0013050127,0.0014084425,0.0016691025],"domain_scores_gemma":[0.9955649,0.00056681194,0.0005925121,0.00090574665,0.0011705961,0.0011994381],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0016872099,0.00092178024,0.0009603481,0.00048354178,0.0009474711,0.0016172373,0.0012530789,0.0010680541,0.0023099398],"category_scores_gemma":[0.00077579456,0.0008622975,0.0003525975,0.0010481683,0.000091563226,0.0027637521,0.00032467308,0.0009973961,0.0005719411],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019832166,0.00062550843,0.0020142896,0.0003341603,0.00030433133,0.00028701252,0.0026734371,0.00020788374,0.008125429,0.95919245,0.02130237,0.0047348156],"study_design_scores_gemma":[0.0008756005,0.0002780818,0.06156276,0.00023499533,0.00012894004,0.00071746454,0.00033906792,0.0014403181,0.0013068906,0.0025893995,0.9295584,0.0009680978],"about_ca_topic_score_codex":0.00049415964,"about_ca_topic_score_gemma":0.001761687,"teacher_disagreement_score":0.95660305,"about_ca_system_score_codex":0.00023407621,"about_ca_system_score_gemma":0.0019076564,"threshold_uncertainty_score":0.99941915},"labels":[],"label_agreement":null},{"id":"W7074020301","doi":"","title":"Respiratory impedance and bronchodilator response in healthy Italian preschool children","year":2010,"lang":"en","type":"article","venue":"UWA Profiles and Research Repository (University of Western Australia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centre for Global Health Research","funders":"","keywords":"Percentile; Bronchodilator; Salbutamol; Supine position; Repeatability; Population; Limits of agreement; Lung function","score_opus":0.03244190111824727,"score_gpt":0.2832478057513175,"score_spread":0.2508059046330703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074020301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880236,0.00015482015,0.0000010406355,0.0002442998,0.00014896327,0.00038379876,0.00009855332,0.00001526346,0.00015089152],"genre_scores_gemma":[0.9979681,0.000051871022,0.00018569549,0.000010727295,0.00009876122,4.2344325e-7,0.000009773463,0.0000042598076,0.0016703951],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983011,0.00042515036,0.00016917466,0.00038406573,0.00034132594,0.00037916738],"domain_scores_gemma":[0.9991437,0.00014501321,0.000092615795,0.00026706548,0.000079876605,0.00027168595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011807155,0.00011957694,0.00022802688,0.00015611127,0.0003324222,0.00009039604,0.00026821715,0.00015246966,0.00010854407],"category_scores_gemma":[0.000033124874,0.000118981035,0.000030680327,0.00014994874,0.0005084752,0.00036061264,0.00008121494,0.00041801995,0.00002087516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015662677,0.000031680513,0.93708277,0.00010908724,0.000019354044,0.00007235434,0.00061610324,0.000007040719,0.059356418,0.00006362625,0.00032831216,0.0007469844],"study_design_scores_gemma":[0.0005420951,0.0005120059,0.99284035,0.000045528872,0.000006820704,0.00001954355,0.00029000654,0.000034038,0.0037573578,0.000056252735,0.001764497,0.00013148622],"about_ca_topic_score_codex":0.010090639,"about_ca_topic_score_gemma":0.000848162,"teacher_disagreement_score":0.055757597,"about_ca_system_score_codex":0.0000052759915,"about_ca_system_score_gemma":0.00010867837,"threshold_uncertainty_score":0.99650127},"labels":[],"label_agreement":null},{"id":"W7074020454","doi":"","title":"Design, Synthesis, and Evaluation of New 1H-Benzo[d]imidazole Based PqsR Inhibitors as Adjuvant Therapy for Pseudomonas aeruginosa Infections","year":2024,"lang":"en","type":"article","venue":"White Rose Research Online (University of Leeds, The University of Sheffield, University of York)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Novartis Pharma; Uppsala Universitet; Université Laval","keywords":"Pseudomonas aeruginosa; Quorum sensing; Virulence; Biofilm; Adjuvant; Potency; Pseudomonadales; Economic shortage; Cell","score_opus":0.0654339633763149,"score_gpt":0.27645790156505484,"score_spread":0.21102393818873993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074020454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98844683,0.00091541145,0.0053098025,0.002475752,0.00013737565,0.0009536787,0.00068140036,0.00003836968,0.0010413787],"genre_scores_gemma":[0.9951814,0.0014362965,0.0025477568,0.000005948639,0.000043631044,1.9870136e-8,0.00008075161,0.000006188649,0.0006980115],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99779546,0.00057817873,0.00015795892,0.00036949755,0.0007850118,0.00031390903],"domain_scores_gemma":[0.9973807,0.001269265,0.00019747792,0.0003476488,0.0006280958,0.00017684972],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018854464,0.00017385696,0.00043576563,0.0005318622,0.0005958163,0.000021308859,0.00065515353,0.00020020377,0.0015495508],"category_scores_gemma":[0.00008256825,0.00018700176,0.00022149495,0.00068297464,0.0008629991,0.00036486724,0.00013180544,0.00027461044,0.0000111119425],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.018005624,0.0034517027,0.028866999,0.004263287,0.0047206557,0.0002490337,0.09375743,0.19745688,0.08708262,0.0046785683,0.060368735,0.49709845],"study_design_scores_gemma":[0.018553648,0.00890001,0.16476443,0.00434292,0.0043134876,0.000033227017,0.2085229,0.43078214,0.03002285,0.006355077,0.12088549,0.0025237894],"about_ca_topic_score_codex":0.028837895,"about_ca_topic_score_gemma":0.0061904844,"teacher_disagreement_score":0.49457467,"about_ca_system_score_codex":0.000032749347,"about_ca_system_score_gemma":0.0008557094,"threshold_uncertainty_score":0.9993632},"labels":[],"label_agreement":null},{"id":"W7074021605","doi":"","title":"Neoadjuvant or Adjuvant Therapy for Resectable Esophageal Cancer: A Clinical Practice Guideline","year":2004,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Guideline; Clinical Practice; Systematic review; MEDLINE; Adjuvant therapy; Neoadjuvant therapy; Evidence-based medicine","score_opus":0.1223539342831005,"score_gpt":0.3798381145199753,"score_spread":0.2574841802368748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074021605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99348456,0.0008067961,0.0010837956,0.0012946723,0.0014712466,0.00084183435,0.00061535655,0.00014764271,0.00025411995],"genre_scores_gemma":[0.9871644,0.0017873172,0.002439262,0.002779609,0.0011891177,0.0000036075555,0.00028352262,0.000036440728,0.0043167663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9970264,0.00034220846,0.0006457601,0.0007815876,0.00047437468,0.0007296895],"domain_scores_gemma":[0.9977855,0.00045721076,0.00041136492,0.000551025,0.0003872961,0.00040760607],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0013439248,0.00036966795,0.00060869,0.00018708418,0.0004259435,0.00035412807,0.00088369707,0.0002590603,0.0004137309],"category_scores_gemma":[0.00020954764,0.00030765333,0.00021129928,0.00039441584,0.00013427268,0.002025841,0.00009087821,0.0003929537,0.00025862682],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00749485,0.00044092693,0.95874757,0.00009547738,0.0004323171,0.0013515175,0.00046580881,0.0036587014,0.000670527,0.00021098577,0.00009304659,0.026338305],"study_design_scores_gemma":[0.007911328,0.0018211916,0.68538713,0.00017590057,0.00022619448,0.000060977898,0.00022671232,0.0000055692126,0.0020544853,0.0006610337,0.30068246,0.0007870277],"about_ca_topic_score_codex":0.0006088811,"about_ca_topic_score_gemma":0.011812677,"teacher_disagreement_score":0.3005894,"about_ca_system_score_codex":0.0000378637,"about_ca_system_score_gemma":0.0005499632,"threshold_uncertainty_score":0.99993753},"labels":[],"label_agreement":null},{"id":"W7074030549","doi":"","title":"Improving mobility &amp; mobility equity : a study on public transportation mode choice in response to fare changes in Metro Vancouver","year":2016,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Public transport; Payment; TRIPS architecture; Mode (computer interface); Equity (law); Pledge; Order (exchange)","score_opus":0.019486230440701705,"score_gpt":0.21866025037733844,"score_spread":0.19917401993663675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074030549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975224,0.000009286146,0.00009511584,0.00012561586,0.0001718347,0.0007018187,0.0012947045,0.000030998355,0.000048202604],"genre_scores_gemma":[0.99975574,0.0000034206878,0.000078476995,0.000025504909,0.000015973512,0.0000017737777,0.000022188678,0.00000379433,0.00009313653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99835724,0.0003045006,0.00017385453,0.0005275062,0.00030904263,0.0003278452],"domain_scores_gemma":[0.999123,0.00022061502,0.00009818984,0.00032767074,0.00009285558,0.00013767192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011082193,0.00006393544,0.00030827938,0.00011185425,0.0001032241,0.00006400817,0.00032388425,0.00007838622,0.0003575749],"category_scores_gemma":[0.00015477749,0.00013802144,0.000047636076,0.00040610225,0.00007098744,0.00042805873,0.00003448963,0.000081622704,0.000019072988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030359905,0.00040131755,0.79025465,0.000044102788,0.000010272606,0.000035164885,0.000632079,0.00012087494,0.0020378479,1.3321959e-7,0.00008177577,0.2060782],"study_design_scores_gemma":[0.0011063527,0.00031138666,0.99674875,0.000057697078,0.000009837429,1.2821948e-7,0.0013163768,0.00004155261,0.0000044926796,0.000100403035,0.00014003966,0.00016298624],"about_ca_topic_score_codex":0.6370927,"about_ca_topic_score_gemma":0.9986022,"teacher_disagreement_score":0.36150947,"about_ca_system_score_codex":0.00005033871,"about_ca_system_score_gemma":0.00008036702,"threshold_uncertainty_score":0.5628351},"labels":[],"label_agreement":null},{"id":"W7074031140","doi":"","title":"Posterolateral corner of the knee: an expert consensus statement on diagnosis, classification, treatment, and rehabilitation","year":2019,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fowler Kennedy Sport Medicine Clinic","funders":"","keywords":"Rehabilitation; Statement (logic); Delphi method; Delphi; International Classification of Functioning, Disability and Health; Consensus conference","score_opus":0.06355648322090422,"score_gpt":0.28997570553191765,"score_spread":0.2264192223110134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074031140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841464,0.000032576245,0.0000012869392,0.00037166206,0.0003583876,0.00047937248,0.00018766423,0.000024965942,0.00012942564],"genre_scores_gemma":[0.9987597,0.000036903868,0.000019798365,0.00013748604,0.00003185347,9.840303e-7,0.00005896439,0.0000066468447,0.00094765454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986914,0.00035432685,0.00021235298,0.00035468113,0.00018488205,0.00020235099],"domain_scores_gemma":[0.9990042,0.00019904113,0.00018867606,0.00042485818,0.000073502,0.00010971518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018833167,0.00017669146,0.0002137771,0.00010364636,0.00012861428,0.00010802583,0.0002262955,0.00007766963,0.00012397124],"category_scores_gemma":[0.000012604928,0.00013009283,0.000056558565,0.00012453544,0.00011086634,0.0004579345,0.00003144677,0.00008153954,0.000082337654],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017565736,0.00006849337,0.99637747,0.000020854715,0.00003050016,0.0000035087655,0.0007085522,0.00007484794,0.0016999863,0.00007106696,0.00000174701,0.00076730223],"study_design_scores_gemma":[0.0008224662,0.0010027996,0.9934809,0.0000620148,0.000029280123,0.0000023354073,0.0002757039,0.0000031092025,0.0014218352,0.000077160475,0.002672942,0.00014941748],"about_ca_topic_score_codex":0.00013539002,"about_ca_topic_score_gemma":0.002066143,"teacher_disagreement_score":0.0028965473,"about_ca_system_score_codex":0.000022441829,"about_ca_system_score_gemma":0.000042929114,"threshold_uncertainty_score":0.53050315},"labels":[],"label_agreement":null},{"id":"W7074038371","doi":"","title":"Paraneoplastic hypoglycemia in a diabetic dog with an insulin growth factor-2-producing mammary carcinoma","year":2010,"lang":"en","type":"article","venue":"Murdoch Research Repository (Murdoch University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mammary carcinoma; Hypoglycemia; Insulin; Diabetes mellitus; Immunohistochemistry; Mammary tumor","score_opus":0.01809441918076496,"score_gpt":0.22356924618356463,"score_spread":0.20547482700279968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074038371","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98724115,0.00006762403,0.00003317591,0.00008497785,0.00054569304,0.00048885273,0.00005016555,0.00009747093,0.0113908695],"genre_scores_gemma":[0.99733675,0.000028734701,0.00052291394,0.000013671313,0.00034960321,0.0000021960973,0.00006347511,0.0000174122,0.0016652365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9959204,0.00070097105,0.0003013311,0.001023792,0.00093973795,0.001113727],"domain_scores_gemma":[0.9976366,0.0004386426,0.00010983899,0.0008979622,0.00033529595,0.00058164616],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00066458323,0.00033262288,0.00042446717,0.0008957414,0.0006683132,0.00037862713,0.0011321384,0.00022732838,0.00025906743],"category_scores_gemma":[0.000118338314,0.00030045173,0.00006779256,0.0013848473,0.00041262867,0.001153665,0.00013128955,0.0011149691,0.00010998178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014560843,0.00035739836,0.88348085,0.00033343863,0.00010579852,0.009142861,0.0021439395,0.00063130824,0.095608324,0.0029272705,0.00016825051,0.0036444531],"study_design_scores_gemma":[0.0015771353,0.0010708648,0.97640306,0.00007727555,0.000027260603,0.00011603657,0.0003202272,0.0016619902,0.015133448,0.00047261792,0.0024988868,0.0006411954],"about_ca_topic_score_codex":0.018022941,"about_ca_topic_score_gemma":0.0061847647,"teacher_disagreement_score":0.09292219,"about_ca_system_score_codex":0.000043721022,"about_ca_system_score_gemma":0.00058143836,"threshold_uncertainty_score":0.99994475},"labels":[],"label_agreement":null},{"id":"W7074040886","doi":"","title":"Long-term follow-up of anatomic graduated component total knee arthroplasty:a 15- to 20-year survival analysis","year":2012,"lang":"en","type":"article","venue":"University of Groningen research database (University of Groningen / Centre for Information Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Survival analysis; Prosthesis; Total knee arthroplasty; Survival rate; Osteoarthritis; Arthroplasty; Overall survival","score_opus":0.021470001160955928,"score_gpt":0.23314822392571202,"score_spread":0.2116782227647561,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074040886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893136,0.00007707066,0.0049099377,0.00020639489,0.00019647935,0.00058335636,0.0042717927,0.000056266195,0.00038511248],"genre_scores_gemma":[0.9927139,0.0000924837,0.0036630384,0.0000026045284,0.000016370004,8.306682e-8,0.0032271084,0.0000043151567,0.0002800724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99806064,0.0001395635,0.00027619427,0.00024826816,0.0006188774,0.0006564623],"domain_scores_gemma":[0.9981206,0.00015328346,0.00037982318,0.0004879181,0.0006032495,0.00025510654],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010408428,0.00017916197,0.0005206092,0.001832127,0.0005178878,0.00001936689,0.00059631566,0.0001780383,0.0010568546],"category_scores_gemma":[0.00009304785,0.00022161554,0.00019707248,0.0016735157,0.00050970557,0.0015249968,0.00035154802,0.00023318028,0.00012444291],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003829668,0.0004358118,0.93463486,0.0009711553,0.0038321174,0.000024702449,0.011920389,0.0040454348,0.0051062736,0.01005018,0.0060777375,0.01907167],"study_design_scores_gemma":[0.0084668035,0.001366182,0.88862836,0.0003271892,0.0017093398,0.000006329546,0.053638276,0.007433676,0.006029061,0.00012027113,0.031115772,0.0011587071],"about_ca_topic_score_codex":0.0046768524,"about_ca_topic_score_gemma":0.0052530426,"teacher_disagreement_score":0.046006467,"about_ca_system_score_codex":0.000047809306,"about_ca_system_score_gemma":0.00013116768,"threshold_uncertainty_score":0.9998563},"labels":[],"label_agreement":null},{"id":"W7074041853","doi":"","title":"Both common variations and rare non-synonymous substitutions and small insertion/deletions in CLU are associated with increased Alzheimer risk","year":2012,"lang":"en","type":"article","venue":"VUBIR (Vrije Universiteit Brussel)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Clusterin; Single-nucleotide polymorphism; SNP; Genetic association; Genome-wide association study; Locus (genetics); Exon; Genetic variation","score_opus":0.011430117000918021,"score_gpt":0.17475990971984545,"score_spread":0.16332979271892742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074041853","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963508,0.00045587422,0.00019235649,0.00012928738,0.00010171518,0.0002758404,0.0008113438,0.000058143065,0.0016246085],"genre_scores_gemma":[0.99883205,0.0001364698,0.0004017006,0.00007511741,0.00006411281,0.0000015445064,0.00041991158,0.000007069193,0.000062016145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989133,0.00017952092,0.00016901846,0.00024413322,0.00013852418,0.00035549316],"domain_scores_gemma":[0.99916846,0.000205707,0.00016585995,0.00017694302,0.00005718223,0.00022583992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025924953,0.00018556813,0.0002553642,0.00019522694,0.00053335313,0.00008218099,0.00011625699,0.00011616349,0.00026470382],"category_scores_gemma":[0.000033987802,0.00016621854,0.000028530381,0.00039299997,0.0001306404,0.0005204521,0.000030368026,0.00016262355,0.00003232424],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007518809,0.00010866615,0.99616945,0.000011476151,0.00015679174,0.000027250528,0.0010692035,0.00062716444,0.00022521846,0.0007726297,0.0001955142,0.0005614646],"study_design_scores_gemma":[0.00088168477,0.00007445888,0.99479973,0.000047079448,0.00027357214,0.000008917132,0.00037637277,0.0014874379,0.000046266225,0.00010488957,0.0016504866,0.0002490721],"about_ca_topic_score_codex":0.018753946,"about_ca_topic_score_gemma":0.026273735,"teacher_disagreement_score":0.0075197876,"about_ca_system_score_codex":0.000012879086,"about_ca_system_score_gemma":0.000057981313,"threshold_uncertainty_score":0.99149424},"labels":[],"label_agreement":null},{"id":"W7074047065","doi":"","title":"Hockey Fans in Training: A Pilot Pragmatic 1 Randomized Controlled Trial","year":2017,"lang":"en","type":"other","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Randomized controlled trial; Pedometer; Overweight; Body mass index; Weight loss; Intervention (counseling); Obesity; Clinical trial","score_opus":0.07527031337109891,"score_gpt":0.2896829398719732,"score_spread":0.21441262650087428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074047065","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8131666,0.0006223008,0.000066767774,0.00012506341,0.0040657916,0.008568929,0.00062769384,0.00036552193,0.1723913],"genre_scores_gemma":[0.42977175,0.00037091452,0.000035691697,0.00009781695,0.0008675798,0.000013568628,0.00036560497,0.00014384264,0.5683332],"study_design_codex":"randomized_trial","study_design_gemma":"randomized_trial","domain_scores_codex":[0.9955219,0.0016458457,0.00061986235,0.0008371754,0.0006142631,0.0007609715],"domain_scores_gemma":[0.9968591,0.00057294004,0.0012798649,0.00091550016,0.000054301672,0.00031833464],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0017918552,0.00073276524,0.003342689,0.0009848688,0.00022081811,0.0006223624,0.0014974753,0.0005201047,0.0018932769],"category_scores_gemma":[0.00030317053,0.0006337013,0.00050663424,0.00019191505,0.0003135721,0.00065772247,0.00010242398,0.00063355087,0.0007693702],"study_design_candidate":"randomized_trial","study_design_consensus":"randomized_trial","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.95014143,0.00029379406,0.044314645,0.00037817145,0.0013693476,0.0013340426,0.00092269544,0.000057106252,0.000033536347,0.00012204144,0.00020945696,0.00082372664],"study_design_scores_gemma":[0.9436292,0.0004117155,0.0127606,0.0010416897,0.0006330497,0.000008901393,0.00005972116,0.0000018721674,0.0000064106134,0.0002604494,0.040236343,0.0009500513],"about_ca_topic_score_codex":0.0006063635,"about_ca_topic_score_gemma":0.05535952,"teacher_disagreement_score":0.39594194,"about_ca_system_score_codex":0.000023221257,"about_ca_system_score_gemma":0.0003266621,"threshold_uncertainty_score":0.99961144},"labels":[],"label_agreement":null},{"id":"W7074048574","doi":"","title":"Houston, We Have AI Problem! Quality Issues with Neuroimaging-Based Artificial Intelligence in Parkinson's Disease: A Systematic Review.","year":2024,"lang":"en","type":"article","venue":"DZNE Pub","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft; Canadian Institutes of Health Research; Jazz Pharmaceuticals; Tourette Association of America; National Institutes of Health; H. Lundbeck A/S; Lundbeckfonden; U.S. Department of Defense","keywords":"Neuroimaging; Variety (cybernetics); Systematic review; Intervention (counseling); Applications of artificial intelligence; Quality (philosophy); Disease","score_opus":0.02317043863458699,"score_gpt":0.28707994862747943,"score_spread":0.2639095099928924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074048574","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19866762,0.6210576,0.017876307,0.1289837,0.0048543387,0.018777033,0.0038841772,0.002100366,0.0037988026],"genre_scores_gemma":[0.99747396,0.0009478896,0.0002943344,0.0007971819,0.000127492,0.000048111597,0.000121214885,0.00001096888,0.00017886599],"study_design_codex":"systematic_review","study_design_gemma":"systematic_review","domain_scores_codex":[0.99803936,0.00032722164,0.00050706224,0.0004309148,0.00037218432,0.00032327397],"domain_scores_gemma":[0.9992216,0.00014416232,0.00010050767,0.00034524497,0.000047583853,0.00014085071],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00089650124,0.00020411867,0.00047875982,0.00008930372,0.00006335913,0.00032080186,0.00024725855,0.000029907473,0.0003940942],"category_scores_gemma":[0.00007968543,0.000139595,0.00006500427,0.0003144059,0.00007347112,0.00023593791,0.000013556389,0.00014019782,0.00031475927],"study_design_candidate":"systematic_review","study_design_consensus":"systematic_review","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044751365,0.00030513486,0.030478725,0.92337805,0.0001617789,0.0013269628,0.0014629408,0.014319082,0.00017734694,0.0071577555,0.0073796436,0.013405087],"study_design_scores_gemma":[0.0005649856,0.0010954832,0.0729423,0.4165899,0.0018846304,0.000050656683,0.0005837959,0.2972525,0.0020983897,0.056176554,0.14610076,0.0046600588],"about_ca_topic_score_codex":0.0014329394,"about_ca_topic_score_gemma":0.0013360002,"teacher_disagreement_score":0.7988063,"about_ca_system_score_codex":0.00000536164,"about_ca_system_score_gemma":0.000121358134,"threshold_uncertainty_score":0.5692519},"labels":[],"label_agreement":null},{"id":"W7074048632","doi":"","title":"Richard Wagamese’s Indian Horse: Stolen Memories and Recovered Histories","year":2019,"lang":"en","type":"article","venue":"LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Narrative; Rewriting; Indigenous; Accident (philosophy)","score_opus":0.011963859708658185,"score_gpt":0.20773670347310882,"score_spread":0.19577284376445064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074048632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9129456,0.00096326065,0.000072948525,0.005076148,0.0032927252,0.0005954007,0.00041556818,0.00026231838,0.07637601],"genre_scores_gemma":[0.9967403,0.00016793232,0.0009961391,0.00014716078,0.00052243826,0.000018567644,0.00037316704,0.000019460937,0.0010148557],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99741167,0.00024763745,0.0004690641,0.0006622862,0.0005836587,0.0006256716],"domain_scores_gemma":[0.99847597,0.00018708654,0.0002746619,0.00047088065,0.00018652373,0.00040487677],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0004943266,0.00037578956,0.0005034418,0.00023423717,0.00046369666,0.0003236748,0.00043336087,0.00032446763,0.00048983743],"category_scores_gemma":[0.00017095532,0.00033544414,0.00011117896,0.00034581416,0.000032289576,0.0006632177,0.00009136568,0.00032519392,0.00010700071],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013662232,0.00045015325,0.07738274,0.00089193,0.0007069835,0.0005579722,0.01564613,0.000625983,0.01498753,0.860525,0.0077157756,0.019143555],"study_design_scores_gemma":[0.0006651903,0.00012210011,0.041539263,0.00005744594,0.000044669392,0.00027253095,0.00040706436,0.00012862353,0.0007629063,0.00091386435,0.9546058,0.0004805283],"about_ca_topic_score_codex":0.000021294127,"about_ca_topic_score_gemma":0.0006306004,"teacher_disagreement_score":0.94689006,"about_ca_system_score_codex":0.00007113179,"about_ca_system_score_gemma":0.0003068945,"threshold_uncertainty_score":0.99990976},"labels":[],"label_agreement":null},{"id":"W7074050800","doi":"","title":"Fruit, vegetables and the prevention of cancer: research challenges","year":2007,"lang":"en","type":"article","venue":"AUSpace (Athabasca University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"","keywords":"Cohort; Confounding; Socioeconomic status; Consumption (sociology); Cohort study; Whole grains; Serving size","score_opus":0.03434468390860534,"score_gpt":0.26607259611495004,"score_spread":0.2317279122063447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074050800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9703072,0.0036575103,0.000033521053,0.0010222679,0.00014759433,0.00018328386,0.000026100572,0.000013734187,0.024608826],"genre_scores_gemma":[0.99202675,0.0037222505,0.000100158235,0.0000057846023,0.00006899065,1.04758165e-7,0.000004769108,0.0000018366082,0.0040693358],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9991761,0.00016198371,0.00007333193,0.00015739967,0.0002118878,0.00021932342],"domain_scores_gemma":[0.99934274,0.0003147085,0.000062252904,0.00014547483,0.00007652082,0.000058285183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010834057,0.000065885026,0.00014003196,0.00012822695,0.0001817257,0.000020038638,0.00021271213,0.000047491692,0.000237674],"category_scores_gemma":[0.000020862135,0.000047826306,0.000034910066,0.0002057052,0.0002654141,0.00017738172,0.000045207635,0.00008487059,0.000012803362],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0047164005,0.00029029758,0.15517196,0.001068134,0.0010026159,0.00023858515,0.03458544,0.00058086694,0.01141086,0.54984844,0.004905397,0.23618104],"study_design_scores_gemma":[0.0031972337,0.00041982168,0.6284833,0.00021349842,0.00015832696,0.0000047593257,0.011238174,0.00012460057,0.013046241,0.013271616,0.32945663,0.00038580713],"about_ca_topic_score_codex":0.014130829,"about_ca_topic_score_gemma":0.040367864,"teacher_disagreement_score":0.5365768,"about_ca_system_score_codex":0.0000039187025,"about_ca_system_score_gemma":0.000040854116,"threshold_uncertainty_score":0.99243414},"labels":[],"label_agreement":null},{"id":"W7074051064","doi":"","title":"Time to resolution of symptoms and recovery after mild traumatic brain injury: protocol for a systematic review and meta-analysis.","year":2023,"lang":"en","type":"article","venue":"Apollo (University of Cambridge)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Rosetrees Trust; Department of Health and Social Care; National Institute for Health and Care Research","keywords":"Protocol (science); MEDLINE; Reporting bias; Cohort; Clinical trial; Traumatic brain injury; Systematic review; Cohort study","score_opus":0.03062527905065419,"score_gpt":0.25496622525601453,"score_spread":0.22434094620536035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074051064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6021689,0.0030817285,0.001269304,0.009466599,0.00008444579,0.37163305,0.010494136,0.00020034508,0.0016014513],"genre_scores_gemma":[0.9198541,0.00027691753,0.0054003503,0.0030144374,0.000087852015,0.006818687,0.0007357108,0.00004897886,0.06376295],"study_design_codex":"systematic_review","study_design_gemma":"meta_analysis","domain_scores_codex":[0.99918777,0.0001291698,0.00021129011,0.00019147128,0.0001466859,0.00013361638],"domain_scores_gemma":[0.99934286,0.00014962604,0.00018872505,0.00019268779,0.00005192247,0.00007419032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006355195,0.00010225551,0.0009797674,0.00016656947,0.000062017025,0.000013797302,0.00011184032,0.000037244645,0.00035254363],"category_scores_gemma":[0.00003894995,0.000087342414,0.00022417963,0.00042259795,0.000057294972,0.00014688574,0.000027420836,0.000020793617,0.0000517516],"study_design_candidate":"meta_analysis","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023275588,0.0001499792,0.00072627375,0.7932349,0.09409322,0.000022165055,0.0029011955,0.0007787519,0.0013928735,0.00060611026,0.103061564,0.00070544594],"study_design_scores_gemma":[0.004393565,0.0052551026,0.15075734,0.013637712,0.7922829,0.000012459275,0.0012864894,0.016580695,0.00038757786,0.00079860375,0.012064536,0.0025430657],"about_ca_topic_score_codex":0.0006475238,"about_ca_topic_score_gemma":0.00016134475,"teacher_disagreement_score":0.77959716,"about_ca_system_score_codex":0.000002001188,"about_ca_system_score_gemma":0.000016383648,"threshold_uncertainty_score":0.38601056},"labels":[],"label_agreement":null},{"id":"W7074051251","doi":"","title":"A Companion to Nordic Cinema","year":2016,"lang":"en","type":"other","venue":"Lincoln Repository (University of Lincoln)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Movie theater; Filmmaking; Icelandic; National cinema; Danish; Indigenous; Film industry","score_opus":0.005364820033365172,"score_gpt":0.1766668733841439,"score_spread":0.17130205335077875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074051251","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01619082,0.00037751702,0.00047623116,0.00025039725,0.00339135,0.00085965736,0.0008111592,0.00025828666,0.97738457],"genre_scores_gemma":[0.08103848,0.00009203176,0.002067426,0.00006342173,0.001435164,3.4376066e-7,0.000108539534,0.00006392976,0.9151307],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985071,0.0001252265,0.00021142422,0.0004800254,0.00037140842,0.00030483495],"domain_scores_gemma":[0.99868786,0.0000730584,0.00039662997,0.000495666,0.00007357605,0.00027323104],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00014072475,0.0002759311,0.00061856356,0.00023496026,0.0001887347,0.00003299154,0.0006126093,0.0003186236,0.010158537],"category_scores_gemma":[0.0000062935123,0.0002653666,0.00016699162,0.00017426016,0.00012283353,0.00009469987,0.00008435146,0.000115540344,0.0024244746],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029564678,0.00013209881,0.017096283,0.00051451486,0.00038002862,0.00048618834,0.00057688216,0.0001979941,0.0020058285,0.00026060882,0.96880394,0.009250005],"study_design_scores_gemma":[0.00051842735,0.00018191595,0.018393088,0.00041851244,0.000113229515,0.000009857074,0.000114798866,0.00005929229,0.000087796005,0.0000548576,0.97962964,0.00041856978],"about_ca_topic_score_codex":0.014217632,"about_ca_topic_score_gemma":0.0041113775,"teacher_disagreement_score":0.06484766,"about_ca_system_score_codex":0.000012751305,"about_ca_system_score_gemma":0.00013920698,"threshold_uncertainty_score":0.99997985},"labels":[],"label_agreement":null},{"id":"W7074052111","doi":"","title":"Labor Down or Bear Down: A Strategy to Translate Second-Stage Labor Evidence to Perinatal Practice","year":2014,"lang":"en","type":"article","venue":"e-Publications@Marquette (Marquette University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; Hyporeflexia; TSG101; Diafiltration; Articular cartilage damage","score_opus":0.01820664176692577,"score_gpt":0.24166080074326549,"score_spread":0.22345415897633972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074052111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8256032,0.00015398645,0.0017733177,0.08005631,0.001022549,0.0025034586,0.014906069,0.00080731814,0.073173806],"genre_scores_gemma":[0.7464735,0.00021773989,0.012158832,0.02016963,0.0008679807,0.000022953613,0.0018124399,0.000052488962,0.21822444],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99673885,0.00049256143,0.00042923127,0.0009886457,0.0005458895,0.0008048104],"domain_scores_gemma":[0.9966663,0.00068788894,0.00023546166,0.0009642084,0.00066158135,0.0007845297],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0008729089,0.00042699138,0.0004581486,0.00071094214,0.0006087438,0.0005744574,0.0012515903,0.00019663996,0.020462167],"category_scores_gemma":[0.0006430916,0.00040784694,0.00010785962,0.0027942192,0.00011517678,0.0025597767,0.00010872735,0.00033898934,0.0027700556],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0076421397,0.0010097843,0.014798635,0.0014111693,0.0014500989,0.0008450904,0.012153322,0.014894143,0.03964995,0.08613756,0.74451494,0.07549315],"study_design_scores_gemma":[0.0004647966,0.00049341575,0.024683973,0.0000485579,0.00007419717,0.000015024636,0.00032878527,0.00011905879,0.00058231724,0.000040859923,0.9725582,0.0005908101],"about_ca_topic_score_codex":0.0018574012,"about_ca_topic_score_gemma":0.005524141,"teacher_disagreement_score":0.22804324,"about_ca_system_score_codex":0.00004311548,"about_ca_system_score_gemma":0.00044682328,"threshold_uncertainty_score":0.99983734},"labels":[],"label_agreement":null},{"id":"W7074053530","doi":"","title":"Doctors and Doctrines: The Ideology of Medical Care in Canada","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ideology; Medical care; Subject (documents); MEDLINE; Health care","score_opus":0.010497810087234726,"score_gpt":0.19832425030338843,"score_spread":0.18782644021615372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074053530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9751074,0.0000060539305,9.929282e-7,0.00029012654,0.0002554157,0.00014158658,0.000096835895,0.00001704594,0.024084577],"genre_scores_gemma":[0.9835768,0.01629221,0.000007216294,0.000046109817,0.00003408211,1.6708093e-7,0.00003597794,0.000001733691,0.000005755715],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991852,0.00010462797,0.00010779144,0.0001578859,0.00023976885,0.00020474331],"domain_scores_gemma":[0.9995803,0.00016765215,0.000045484492,0.00012707982,0.00002582887,0.00005364358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001489237,0.00008067616,0.00015818975,0.000858723,0.000060561488,0.000009958896,0.00029922588,0.000049737533,0.00017338309],"category_scores_gemma":[0.00003192486,0.000058953014,0.000019664756,0.0025448166,0.00007129316,0.00007265294,0.000063497566,0.000084206236,0.0000071114487],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024606907,0.000023052338,0.8771889,0.00033899874,0.00011634325,0.0016102755,0.015387135,0.0010623459,0.000010739455,0.0027037256,0.0010029675,0.10030945],"study_design_scores_gemma":[0.0003960649,0.0000489414,0.1136048,0.000020282552,0.000015962392,0.000003860959,0.0025062219,0.00038493096,0.00007477744,0.0000025129777,0.88283706,0.00010456211],"about_ca_topic_score_codex":0.99780047,"about_ca_topic_score_gemma":0.9987519,"teacher_disagreement_score":0.8818341,"about_ca_system_score_codex":0.000013247656,"about_ca_system_score_gemma":0.0008878852,"threshold_uncertainty_score":0.24040341},"labels":[],"label_agreement":null},{"id":"W7074061075","doi":"","title":"Separating Birth from Community: Colonialism and Historical Institutionalism in Indigenous Pregnancy Evacuation Policies","year":2024,"lang":"en","type":"article","venue":"DOAJ (DOAJ: Directory of Open Access Journals)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Indigenous; Colonialism; Norm (philosophy); Health care; Maternity care","score_opus":0.2077933180516097,"score_gpt":0.4808720953565009,"score_spread":0.27307877730489116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074061075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9642841,0.032812335,0.000032539498,0.00014926428,0.0010599712,0.0003011985,0.00037595184,0.00003060846,0.00095398276],"genre_scores_gemma":[0.9954891,0.0037982163,0.00011846182,0.00009791837,0.00021568697,0.000008007507,0.00011986408,0.000008532486,0.00014416873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981399,0.00044198366,0.0005398024,0.00023491275,0.00039154122,0.00025184246],"domain_scores_gemma":[0.99888927,0.00047151695,0.00023546108,0.0002038342,0.000072156894,0.00012773731],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000837987,0.00018941949,0.0004556848,0.00041338286,0.00040067377,0.0013957554,0.00084218703,0.00009706287,0.002290908],"category_scores_gemma":[0.0001055194,0.00016397343,0.000052724317,0.00047678198,0.000088421795,0.0016782851,0.00018305412,0.00034943986,0.000018891556],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000116782234,0.00016842913,0.91514194,0.0003179965,0.00020245742,0.00013711004,0.009500247,0.0019524652,0.025982581,0.0010358389,0.004739573,0.04070458],"study_design_scores_gemma":[0.00020749944,0.000014421428,0.9553889,0.00068349385,0.000036925918,0.0000071100662,0.00003765589,0.00030839312,0.0009288369,0.027223255,0.014924757,0.00023875033],"about_ca_topic_score_codex":0.15093717,"about_ca_topic_score_gemma":0.005442353,"teacher_disagreement_score":0.14549482,"about_ca_system_score_codex":0.00004841751,"about_ca_system_score_gemma":0.00019888433,"threshold_uncertainty_score":0.9996409},"labels":[],"label_agreement":null},{"id":"W7074065805","doi":"","title":"Personal Health Data: Patient Consent in Information Age","year":2011,"lang":"en","type":"other","venue":"TU/e Research Portal (Eindhoven University of Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Custodians; Confidentiality; Public health; Set (abstract data type); Informed consent; Health information; Personally identifiable information; Masking (illustration)","score_opus":0.06149111401642309,"score_gpt":0.27618011466287984,"score_spread":0.21468900064645674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074065805","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.071352914,0.0020458777,0.000037651374,0.0015613454,0.0006014594,0.002195406,0.011016346,0.00037473335,0.9108143],"genre_scores_gemma":[0.87563187,0.0053090453,0.003261429,0.00009619965,0.00016627833,0.0000013145975,0.009940197,0.00008494325,0.10550872],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984205,0.00010616652,0.00022421121,0.00030471405,0.00047887332,0.0004655837],"domain_scores_gemma":[0.9989709,0.000031231626,0.00029221998,0.0005376726,0.000057936828,0.00011001864],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005906655,0.00015201299,0.00039316204,0.0011717179,0.000100190395,0.000016710517,0.0008902116,0.00034389194,0.008169965],"category_scores_gemma":[0.000048530324,0.0001571354,0.000038632188,0.00043565666,0.0004608295,0.00021405189,0.00029160094,0.00045136383,0.00052676705],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012157009,0.00013534681,0.0062575247,0.0005130252,0.00014932232,0.00062630366,0.0011463338,0.000004821497,0.000022137358,0.0012084745,0.9406278,0.049187355],"study_design_scores_gemma":[0.00041731508,0.00039009892,0.0053023333,0.00031898342,0.000009953105,0.0000075215853,0.0022448346,0.000033497698,0.000022031543,0.0004000577,0.9906326,0.00022075049],"about_ca_topic_score_codex":0.07883586,"about_ca_topic_score_gemma":0.04578533,"teacher_disagreement_score":0.80530554,"about_ca_system_score_codex":0.000014453966,"about_ca_system_score_gemma":0.00048371605,"threshold_uncertainty_score":0.9927367},"labels":[],"label_agreement":null},{"id":"W7074065991","doi":"","title":"Peace is Essential Prerequisite of Health: Linkage in Canadian Indigenous Peoples","year":2006,"lang":"en","type":"article","venue":"PubMed Central","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Indigenous; Linkage (software); Traditional knowledge; Ethnic group","score_opus":0.006778721831712134,"score_gpt":0.18899838544685005,"score_spread":0.18221966361513792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074065991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958198,0.0011043672,0.0000064531987,0.0002874907,0.0006964726,0.00032278226,0.0005993591,0.000012220676,0.0011510641],"genre_scores_gemma":[0.99896663,0.00009353402,0.000058173275,0.0001230659,0.00031882979,0.0000032548996,0.00025505564,0.0000037729899,0.00017766625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9977847,0.00007729777,0.000302342,0.00018913901,0.00017171893,0.0014748292],"domain_scores_gemma":[0.999383,0.00002775406,0.000103342085,0.00013544812,0.000013252036,0.00033723746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042044948,0.00010645764,0.0002278355,0.0000998443,0.00008505772,0.000050853465,0.00017329067,0.000059167785,0.0006018991],"category_scores_gemma":[0.000011013496,0.000100363955,0.000040329185,0.00015640218,0.00003446887,0.000113690774,0.0000066935604,0.00006707398,0.000029922425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012667899,0.000029822228,0.99050725,0.00008504848,0.00001099354,0.000020809775,0.0025825407,0.0010455857,0.0000577217,0.00016452374,0.00093298807,0.004550049],"study_design_scores_gemma":[0.00017420478,0.000017576636,0.9939005,0.000010479057,0.000004696877,0.0000019414508,0.000039870087,0.000056678215,0.0005668009,0.00022592138,0.0048980387,0.00010333444],"about_ca_topic_score_codex":0.9310542,"about_ca_topic_score_gemma":0.9457886,"teacher_disagreement_score":0.014734448,"about_ca_system_score_codex":0.00002364098,"about_ca_system_score_gemma":0.0006148611,"threshold_uncertainty_score":0.6590373},"labels":[],"label_agreement":null},{"id":"W7074066884","doi":"","title":"Are We Doing Any Good? A Value-Added Analysis of UBC’s Science One Program","year":2012,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Academic program; Degree program; Program evaluation; Work (physics); Experimental science","score_opus":0.09010164834669149,"score_gpt":0.3031234038039493,"score_spread":0.21302175545725782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074066884","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978731,0.00018918714,0.000082594175,0.000066074565,0.00039370643,0.00031577493,0.00025433346,0.00012043324,0.0007047517],"genre_scores_gemma":[0.9988263,0.00005167424,0.00030872374,0.000066376415,0.00012074138,4.9624e-7,0.000060590493,0.000009384729,0.0005557115],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972837,0.00023850135,0.0003249984,0.0005264809,0.0007666392,0.0008597105],"domain_scores_gemma":[0.9981004,0.00010214745,0.00052376144,0.0005950797,0.00018842047,0.0004902074],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0010065588,0.0002806143,0.0006038781,0.0010290481,0.00037369665,0.00030576016,0.0010182748,0.00013531013,0.00025328013],"category_scores_gemma":[0.0000329263,0.00028065007,0.00021193078,0.0028163937,0.0003677709,0.0026598074,0.00017187477,0.00023897408,0.00014535585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005116133,0.00014626823,0.99496204,0.000056078272,0.00030460153,0.00002202061,0.00048480651,0.00029637097,0.002242918,0.000099789475,2.5360598e-7,0.0013337015],"study_design_scores_gemma":[0.00033147508,0.00010373929,0.99215615,0.00009756458,0.0008583265,0.000002882603,0.00021509243,0.000009272324,0.003643149,0.000030068259,0.0022187508,0.00033356043],"about_ca_topic_score_codex":0.00009474,"about_ca_topic_score_gemma":0.0022108706,"teacher_disagreement_score":0.0028059115,"about_ca_system_score_codex":0.000027643731,"about_ca_system_score_gemma":0.00010231903,"threshold_uncertainty_score":0.9999646},"labels":[],"label_agreement":null},{"id":"W7074071186","doi":"","title":"Measurement of single top-quark production in association with a $W$ boson in the single-lepton channel at $\\sqrt{s} = 8$ TeV with the ATLAS detector","year":2020,"lang":"en","type":"article","venue":"DESY (CERN, DESY, Fermilab, IHEP, and SLAC)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"H2020 Marie Skłodowska-Curie Actions; European Regional Development Fund; Max-Planck-Gesellschaft; Centre National de la Recherche Scientifique; British Columbia Knowledge Development Fund; Fundação para a Ciência e a Tecnologia; Institut National de Physique Nucléaire et de Physique des Particules; Agencia Nacional de Promoción Científica y Tecnológica; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Science and Technology Facilities Council; Bundesministerium für Bildung und Forschung; Ministry of Education, Culture, Sports, Science and Technology; Natural Sciences and Engineering Research Council of Canada; European Social Fund; Royal Society; Centre National pour la Recherche Scientifique et Technique; Japan Society for the Promotion of Science; National Research Center \"Kurchatov Institute\"; Israel Science Foundation; Comisión Nacional de Investigación Científica y Tecnológica; Türkiye Atom Enerjisi Kurumu; Joint Institute for Nuclear Research; Ministerstwo Edukacji i Nauki; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Bundesministerium für Wissenschaft, Forschung und Wirtschaft; Generalitat de Catalunya; Generalitat Valenciana; Austrian Science Fund; U.S. Department of Energy; National Natural Science Foundation of China; European Commission; Leverhulme Trust; Fundação de Amparo à Pesquisa do Estado de São Paulo; Javna Agencija za Raziskovalno Dejavnost RS; Deutsche Forschungsgemeinschaft; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Agence Nationale de la Recherche; Services Fédéraux des Affaires Scientifiques, Techniques et Culturelles; Department of Science and Technology, Ministry of Science and Technology, India; General Secretariat for Research and Technology; National Science Foundation; Compute Canada; Alexander von Humboldt-Stiftung; TRIUMF; Departamento Administrativo de Ciencia, Tecnología e Innovación (COLCIENCIAS); Canarie; Centres de Recerca de Catalunya; CERN; Danmarks Grundforskningsfond","keywords":"Large Hadron Collider; Luminosity; Atlas (anatomy); Detector; Top quark; ATLAS experiment; Lepton; Invariant mass","score_opus":0.02497107149397467,"score_gpt":0.18147405769869113,"score_spread":0.15650298620471645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074071186","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960782,0.00045263383,0.000018598292,0.0021223426,0.00015186243,0.000560953,0.000029902689,0.00002431491,0.0005611823],"genre_scores_gemma":[0.999488,0.000053592077,0.000034338434,0.00011651992,0.00021026556,0.00000829049,0.00002856457,0.00001142806,0.000049001406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99811643,0.00026045268,0.00027966418,0.00037582993,0.0006334437,0.00033415292],"domain_scores_gemma":[0.9993121,0.000075706084,0.00023525541,0.00020793211,0.00009850378,0.00007052243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077629683,0.00021461573,0.00030913702,0.00005560253,0.0001869684,0.000120194,0.00021001605,0.00008820796,0.000064614185],"category_scores_gemma":[0.00008257407,0.000119159624,0.000036437857,0.00038090447,0.000077530465,0.00018908281,0.000022183076,0.0001448708,0.000014866578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033775577,0.0005307381,0.70369595,0.0005421777,0.00024330903,0.00006776272,0.025374439,0.0047356873,0.24261758,0.000054317716,0.0023321519,0.01642831],"study_design_scores_gemma":[0.0027792961,0.0035253451,0.60725105,0.00038653752,0.00023773291,0.000036953847,0.0020863563,0.0012447973,0.36769047,0.00024937556,0.0136116035,0.0009004557],"about_ca_topic_score_codex":0.0016823922,"about_ca_topic_score_gemma":0.009291667,"teacher_disagreement_score":0.12507291,"about_ca_system_score_codex":0.000043796037,"about_ca_system_score_gemma":0.000038617534,"threshold_uncertainty_score":0.5184968},"labels":[],"label_agreement":null},{"id":"W7074074812","doi":"","title":"Psychophysical distress and alexithymic traits in chronic fatigue syndrome with and without comorbid depression","year":2011,"lang":"en","type":"article","venue":"Cineca Institutional Research Information System (Tor Vergata University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Depression (economics); Distress; Chronic fatigue syndrome; Anxiety; Alexithymia","score_opus":0.051672208290983256,"score_gpt":0.24917243406526235,"score_spread":0.1975002257742791,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074074812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9837731,0.0000414543,0.0003553537,0.0000186012,0.00007759194,0.00032745508,0.00026392684,0.000028635715,0.015113856],"genre_scores_gemma":[0.9995898,0.000027744034,0.00014053528,0.0000052475475,0.000030960513,0.0000014691421,0.00015224006,0.0000019927493,0.000049998896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99882686,0.000108330845,0.00017911667,0.00019568206,0.00042828766,0.00026172525],"domain_scores_gemma":[0.9994576,0.000039157243,0.00007168987,0.00013338537,0.00011443445,0.0001837304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028403796,0.0001216937,0.0001803161,0.000361919,0.0003364055,0.00008113934,0.00020697086,0.00007003489,0.0001004447],"category_scores_gemma":[0.000015216349,0.000098561904,0.000014337799,0.00039533884,0.00032528676,0.0017842867,0.000051027175,0.0001625017,0.00005856457],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0048371013,0.00019143046,0.6948989,0.004818238,0.00028971513,0.0009865524,0.006531368,0.0062053236,0.0012419728,0.2580599,0.0004872073,0.021452285],"study_design_scores_gemma":[0.0018410631,0.0002703938,0.9880427,0.0004831023,0.000012075376,0.00012982287,0.00060774485,0.0039764233,0.00012468711,0.00005527719,0.0042450125,0.00021170164],"about_ca_topic_score_codex":0.0018618584,"about_ca_topic_score_gemma":0.0004939345,"teacher_disagreement_score":0.29314378,"about_ca_system_score_codex":0.00005887589,"about_ca_system_score_gemma":0.00020879462,"threshold_uncertainty_score":0.4019238},"labels":[],"label_agreement":null},{"id":"W7074075081","doi":"","title":"Fashioning the Canadian Landscape: Essays on Travel Writing, Tourism, and National Identity in the Pre-Automobile Era","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Dysgeusia; Liquation; Diafiltration; Emperipolesis; Triacetin; Demotion","score_opus":0.015134710704307955,"score_gpt":0.22063073805939568,"score_spread":0.2054960273550877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074075081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.76269466,0.0000014271021,0.0000040114237,0.00045726716,0.00013357626,0.00028449297,0.00019672794,0.000031474585,0.23619637],"genre_scores_gemma":[0.9978026,0.0017440283,0.000015585589,0.00017717372,0.00011246102,0.0000011780173,0.00009667206,0.0000032279643,0.000047042326],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989703,0.00016920408,0.00009130552,0.00020815154,0.00028626746,0.0002747404],"domain_scores_gemma":[0.99953324,0.00020286861,0.000045161032,0.00012864088,0.000036588324,0.00005352093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006114749,0.00010425181,0.00010227574,0.0017479177,0.00052163645,0.00021592026,0.00034761918,0.000058316422,0.000109931774],"category_scores_gemma":[0.000034219996,0.00007223214,0.000032022286,0.0027477716,0.00005200453,0.00029378923,0.0000260348,0.00017211649,0.00005215842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006150772,0.00043124345,0.44084752,0.00046812333,0.0005671581,0.004772932,0.17306745,0.026766025,0.00007906476,0.23695509,0.023276769,0.09215356],"study_design_scores_gemma":[0.0004933742,0.00008624891,0.54094005,0.000035579385,0.000024890911,0.000008839796,0.0021087248,0.0032916176,0.000018760104,0.00008418257,0.45268697,0.00022078284],"about_ca_topic_score_codex":0.7069339,"about_ca_topic_score_gemma":0.9215651,"teacher_disagreement_score":0.4294102,"about_ca_system_score_codex":0.000014654944,"about_ca_system_score_gemma":0.00030091926,"threshold_uncertainty_score":0.40120587},"labels":[],"label_agreement":null},{"id":"W7074076436","doi":"","title":"Mycoplasma genitalium in Toronto, Ont: Estimates of prevalence and macrolide resistance","year":2016,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mycoplasma genitalium; Macrolide Antibiotics; Drug resistance; Antibiotic resistance; Antibiotics","score_opus":0.007529773944489517,"score_gpt":0.19113630230558057,"score_spread":0.18360652836109106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074076436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897632,0.002364197,0.000012833924,0.00012492728,0.00040645324,0.00023266183,0.00029206902,0.000024787254,0.0067788437],"genre_scores_gemma":[0.99680585,0.0013524821,0.00041323894,0.000024492541,0.00008384053,0.0000039562815,0.000006938427,0.0000065612235,0.00130265],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860066,0.000088540306,0.00027219512,0.00029190746,0.00017840171,0.0005682848],"domain_scores_gemma":[0.99935085,0.00012999313,0.00010364462,0.00021618431,0.000031802378,0.00016755136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027777933,0.00014291954,0.00021218722,0.000022331362,0.000036216792,0.000044061173,0.00021096207,0.00003634851,0.00086434325],"category_scores_gemma":[0.00012773128,0.0000964916,0.000023099834,0.00008058128,0.000096720585,0.0003081561,0.000025809653,0.000034309436,0.000037781054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021728188,0.000031463736,0.97664106,0.00024443128,0.000022684539,0.0000513266,0.0010818973,0.000014072776,0.007900137,0.0006167101,0.0004879298,0.01269099],"study_design_scores_gemma":[0.00039260436,0.000030090672,0.98285097,0.000099088924,0.00001494163,0.0000048574025,0.00001198536,0.000014177384,0.0077795777,0.000375312,0.008268325,0.00015807911],"about_ca_topic_score_codex":0.0018896227,"about_ca_topic_score_gemma":0.007987624,"teacher_disagreement_score":0.012532911,"about_ca_system_score_codex":0.000010486294,"about_ca_system_score_gemma":0.000030832718,"threshold_uncertainty_score":0.9463952},"labels":[],"label_agreement":null},{"id":"W7074078030","doi":"","title":"Los Tellos de Meneses de Lope de Vega en la conformación del ideal de labrador digno","year":2011,"lang":"es","type":"article","venue":"LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ideal (ethics); Order (exchange); Context (archaeology)","score_opus":0.020521547107467245,"score_gpt":0.23347185220844194,"score_spread":0.21295030510097468,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074078030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8556827,0.0012228716,0.002979676,0.0022403349,0.0016028144,0.00091927935,0.0012147613,0.0004412391,0.13369635],"genre_scores_gemma":[0.9895973,0.0010103091,0.006598965,0.00051012245,0.0013135399,0.00009324099,0.00035173222,0.000067185625,0.00045760177],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99364024,0.0014145673,0.0010707395,0.0009633705,0.0009155776,0.0019954832],"domain_scores_gemma":[0.9961917,0.00076818647,0.00059743057,0.0007545641,0.00034462777,0.0013435222],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0021522122,0.00085282896,0.00088732195,0.0004129129,0.0010315512,0.000848865,0.0013996849,0.0010480431,0.00052113517],"category_scores_gemma":[0.0006304945,0.00080731657,0.0003495784,0.0005791661,0.00010590483,0.0009496888,0.00026360655,0.00086965284,0.00010774601],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001074639,0.0010694194,0.037311904,0.00086915924,0.00071163103,0.0017338272,0.012082368,0.0010607657,0.020823484,0.9148541,0.0024701,0.0059385654],"study_design_scores_gemma":[0.0016377785,0.0002720658,0.094118744,0.0004266343,0.000420544,0.0022579741,0.00069281016,0.00256892,0.015992442,0.0029611222,0.87732506,0.0013259321],"about_ca_topic_score_codex":0.00035418963,"about_ca_topic_score_gemma":0.00075337663,"teacher_disagreement_score":0.911893,"about_ca_system_score_codex":0.00036369552,"about_ca_system_score_gemma":0.0025413688,"threshold_uncertainty_score":0.99943775},"labels":[],"label_agreement":null},{"id":"W7074078917","doi":"","title":"Ethnic specific recommendations in clinical practice guidelines: a first exploratory comparison between guidelines from the USA, Canada, the UK, and the Netherlands","year":2003,"lang":"en","type":"article","venue":"Data Archiving and Networked Services (DANS)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ethnic group; Guideline; Clinical Practice; Primary care; Foundation (evidence); MEDLINE; Scientific literature","score_opus":0.1434938705162691,"score_gpt":0.3554102143050123,"score_spread":0.2119163437887432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074078917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96514994,0.012050116,0.0005062954,0.017234473,0.0012679364,0.0005173991,0.0024156524,0.000020119593,0.0008380713],"genre_scores_gemma":[0.9780736,0.010718669,0.0023452758,0.0048510544,0.0016774543,0.000008329301,0.002264303,0.000011384082,0.000049932987],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99668956,0.00139783,0.0009030393,0.0004421742,0.0002569284,0.00031044811],"domain_scores_gemma":[0.9911531,0.0074445694,0.0003142928,0.0009125755,0.00007628359,0.000099164354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0048432825,0.0002048913,0.00036158494,0.000015403537,0.00068050926,0.00024598418,0.001104124,0.000054041982,0.0001076176],"category_scores_gemma":[0.00033598332,0.00009832082,0.000028592918,0.00020243418,0.00019613284,0.00025726808,0.00019018921,0.00035010633,0.000010118247],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015673258,0.000015625641,0.85417205,0.000021124746,0.00015343638,0.0000058689425,0.0044051725,0.0043014046,0.0000016244902,0.00013549956,0.0998937,0.03673776],"study_design_scores_gemma":[0.00047251277,0.000016807931,0.46294802,0.000103477556,0.00008332763,0.0000028829043,0.0032246253,0.02527956,5.516298e-7,0.0004462947,0.5072705,0.00015139898],"about_ca_topic_score_codex":0.58924663,"about_ca_topic_score_gemma":0.9684634,"teacher_disagreement_score":0.40737683,"about_ca_system_score_codex":0.0000033589758,"about_ca_system_score_gemma":0.000121795245,"threshold_uncertainty_score":0.5233996},"labels":[],"label_agreement":null},{"id":"W7074079058","doi":"","title":"La ruée vers l’or rose : Regards croisés sur la pêche crevettière traditionnelle à Madagascar","year":2002,"lang":"fr","type":"book","venue":"Directory of Open access Books (OAPEN Foundation)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Population; Western europe; Period (music)","score_opus":0.0955115332977263,"score_gpt":0.32413639493940477,"score_spread":0.22862486164167847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074079058","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.029802844,0.0006095246,0.000055491633,0.00036761927,0.003540409,0.002090425,0.0006500748,0.00010932241,0.9627743],"genre_scores_gemma":[0.108251445,0.0016926056,0.0007023414,0.0002792344,0.0009772555,0.00008630012,0.0045721275,0.0001168458,0.8833218],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99414766,0.0011959574,0.0014503519,0.0013133197,0.0011010241,0.00079171325],"domain_scores_gemma":[0.9944609,0.0021522793,0.0014128046,0.0011010595,0.00040717804,0.00046578146],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0018833682,0.000997307,0.0017142667,0.00035338974,0.0008347607,0.0047351527,0.0045640036,0.00052081636,0.16598906],"category_scores_gemma":[0.00024949835,0.0009381773,0.00042078164,0.00034384348,0.0011618355,0.0058492804,0.000636112,0.0006734418,0.004303166],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0030914932,0.0014405003,0.008452477,0.0046078977,0.003408452,0.0012011785,0.002148089,0.0027844475,0.0010330032,0.117400885,0.30439898,0.5500326],"study_design_scores_gemma":[0.0012914805,0.00016294798,0.03222924,0.0007947679,0.00038415563,0.000042383326,0.000040533916,0.00028047958,0.0005143594,0.003680873,0.9594452,0.0011335994],"about_ca_topic_score_codex":0.012410633,"about_ca_topic_score_gemma":0.0038365785,"teacher_disagreement_score":0.65504616,"about_ca_system_score_codex":0.00011708591,"about_ca_system_score_gemma":0.0016285183,"threshold_uncertainty_score":0.99930686},"labels":[],"label_agreement":null},{"id":"W7074082122","doi":"","title":"French &amp; English in Dieppe, New-Brunswick","year":2016,"lang":"fr","type":"other","venue":"reroDoc Digital Library","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"French; Relation (database); Portrait; Linguistic analysis","score_opus":0.009508278389516438,"score_gpt":0.18411469276334208,"score_spread":0.17460641437382565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074082122","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.029457124,0.0038865888,0.000016338807,0.0006763947,0.0046861097,0.0004599111,0.0043843742,0.00021915925,0.956214],"genre_scores_gemma":[0.022171896,0.00091871707,0.00034538738,0.000245941,0.005517268,0.0000020960722,0.0027643172,0.00014023548,0.96789414],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9970544,0.0001219002,0.0006410219,0.00086030876,0.000381519,0.00094085356],"domain_scores_gemma":[0.99818707,0.00030352976,0.00027936508,0.00066222146,0.000019942687,0.0005478782],"candidate_categories":["metaepi_narrow","scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00009765062,0.00065212615,0.00081361696,0.0002526147,0.00006492479,0.001196108,0.00084415305,0.00049610855,0.19372651],"category_scores_gemma":[0.000097131124,0.00051130156,0.00020254412,0.00031016665,0.00019435397,0.002779047,0.00019407649,0.00028085386,0.038218513],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006117073,0.00010894657,0.1547836,0.00021463791,0.000102830585,0.00011383559,0.00028926917,0.000023968265,0.000016248767,0.0061716177,0.7582796,0.07983424],"study_design_scores_gemma":[0.00041430377,0.00007826066,0.052399676,0.0005518255,0.000017417298,0.000004414262,0.0000048389347,0.0000025692143,0.00003278095,0.0050945296,0.94073117,0.0006682189],"about_ca_topic_score_codex":0.0033795764,"about_ca_topic_score_gemma":0.0028829894,"teacher_disagreement_score":0.18245155,"about_ca_system_score_codex":0.00000759115,"about_ca_system_score_gemma":0.00079279393,"threshold_uncertainty_score":0.99984074},"labels":[],"label_agreement":null},{"id":"W7074084889","doi":"","title":"Fuzzy logic: principles, applications and perspectives","year":2011,"lang":"en","type":"other","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Dysgeusia; Liquation; Diafiltration; Emperipolesis; Triacetin; Demotion","score_opus":0.01586282891013545,"score_gpt":0.16522541703537835,"score_spread":0.1493625881252429,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074084889","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.024255058,0.0035059233,0.000119305936,0.000022488079,0.00014896216,0.0005359572,0.0031960546,0.00013095274,0.9680853],"genre_scores_gemma":[0.5450404,0.004332578,0.0024843616,0.000025189436,0.00027884278,8.0965333e-7,0.00035655766,0.00005427891,0.44742694],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9992928,0.000030054662,0.00006376059,0.00034799794,0.00011183998,0.00015352965],"domain_scores_gemma":[0.99950266,0.000012729096,0.00014537235,0.00020878953,0.000038271643,0.00009215134],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006561499,0.00005108978,0.0002551662,0.000038615926,0.00011561341,0.00006179268,0.0002433058,0.00014897094,0.005428412],"category_scores_gemma":[0.0000031490229,0.00015538245,0.000049171493,0.00008163802,0.0002775988,0.00006972628,0.000041969164,0.00006909769,0.00017605569],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014595879,0.00016299343,0.019069698,0.0006078591,0.00031882056,0.00013782181,0.00073306245,0.000004748634,0.00003218118,0.00040232367,0.19369358,0.7848223],"study_design_scores_gemma":[0.00016982316,0.000033949946,0.8232997,0.00006872492,0.00004811488,0.000010615439,0.00041831215,0.000002508573,4.1053116e-8,0.0012436579,0.17452174,0.00018280996],"about_ca_topic_score_codex":0.43807092,"about_ca_topic_score_gemma":0.60807973,"teacher_disagreement_score":0.80423,"about_ca_system_score_codex":0.0000024532203,"about_ca_system_score_gemma":0.000036642625,"threshold_uncertainty_score":0.9954808},"labels":[],"label_agreement":null},{"id":"W7074085193","doi":"","title":"Structural analysis of the lipopolysaccharide from nontypeable Haemophilus influenzae strain 1003","year":2002,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Strain (injury); Haemophilus influenzae; Lipopolysaccharide; Pasteurellaceae","score_opus":0.018120943352488005,"score_gpt":0.20547076347654816,"score_spread":0.18734982012406015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074085193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907221,0.0000843759,0.0000049044356,0.00015642056,0.0003814348,0.00007809604,0.0014039709,0.000015145108,0.0071535395],"genre_scores_gemma":[0.99906605,0.0000081293065,0.00027877063,0.00015516201,0.000115335795,4.57439e-7,0.000059425074,0.0000024894264,0.00031415318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999101,0.000064385575,0.00021333684,0.00017959032,0.00024561674,0.00019607795],"domain_scores_gemma":[0.9993887,0.000067568304,0.00011690681,0.00033648472,0.000030290836,0.00006004603],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009171616,0.00010490091,0.00025961726,0.00005629857,0.000106580446,0.000047489502,0.00032894913,0.00005035276,0.029045494],"category_scores_gemma":[0.000023462857,0.00006684108,0.00012252369,0.00030744416,0.000068998444,0.00010915096,0.000021379106,0.00006805308,0.00010035681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009270336,0.000058512793,0.50568897,0.000044216536,0.0029916116,0.000023051267,0.0031068604,0.050168324,0.37738302,0.0033017201,0.005602769,0.05153824],"study_design_scores_gemma":[0.00028763321,0.000043079846,0.9246305,0.000012164391,0.00073239673,8.869904e-7,0.00005404138,0.049371116,0.010982983,0.011379504,0.0022498248,0.00025587148],"about_ca_topic_score_codex":0.0066261715,"about_ca_topic_score_gemma":0.0024898238,"teacher_disagreement_score":0.41894153,"about_ca_system_score_codex":0.000001725577,"about_ca_system_score_gemma":0.000011403198,"threshold_uncertainty_score":0.9999888},"labels":[],"label_agreement":null},{"id":"W7074086629","doi":"","title":"Personal, Cultural, and Educational Implications of Language Loss/Transformation: A Canadian Context","year":2013,"lang":"en","type":"article","venue":"PDXScholar  (Portland State University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"German; Context (archaeology); Face (sociological concept); Cultural diversity; Character (mathematics); Diversity (politics); Language industry; Linguistic diversity","score_opus":0.009599320082986345,"score_gpt":0.19133728122163138,"score_spread":0.18173796113864504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074086629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847412,0.00012825453,0.000011306743,0.001122547,0.000055928467,0.0001469418,0.00063128304,0.000007993861,0.01315456],"genre_scores_gemma":[0.99793404,0.00016720324,0.00007098728,0.000074451,0.000021721202,2.7790395e-7,0.00035415086,0.0000015083302,0.0013756711],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995453,0.000026803356,0.000095784344,0.0001126852,0.00007350972,0.00014595513],"domain_scores_gemma":[0.99955523,0.00002622959,0.00005172006,0.00007333271,0.000104253995,0.00018925204],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000056862005,0.00007169437,0.000100138124,0.00010668561,0.00018172333,0.00006738375,0.00009706891,0.000025045245,0.002380217],"category_scores_gemma":[0.0000066754915,0.00006309307,0.000024451645,0.00012767238,0.000061638275,0.00061204605,0.0000047266517,0.00005569324,0.00009362167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006228498,0.000072913,0.9134329,0.0002019656,0.00024710735,0.000047532445,0.030561317,0.00015519527,0.003218596,0.011294449,0.010249548,0.030456187],"study_design_scores_gemma":[0.00032721594,0.000035798443,0.9150311,0.000013241084,0.000025470084,0.000014955404,0.0026357975,0.000106824,0.0001203842,0.00035712373,0.08116892,0.0001632072],"about_ca_topic_score_codex":0.18694365,"about_ca_topic_score_gemma":0.106201045,"teacher_disagreement_score":0.08074261,"about_ca_system_score_codex":0.0000058674623,"about_ca_system_score_gemma":0.00012573588,"threshold_uncertainty_score":0.99853176},"labels":[],"label_agreement":null},{"id":"W7074089145","doi":"","title":"The first 20 years of the Canadian Respiratory Journal","year":2014,"lang":"en","type":"article","venue":"PubMed Central","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Respiratory system; MEDLINE","score_opus":0.008988241681218239,"score_gpt":0.16485464642054656,"score_spread":0.15586640473932833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074089145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889201,0.00017428854,0.0000013359014,0.0013089118,0.0035828194,0.00012432563,0.00005604594,0.0000043923887,0.0058278],"genre_scores_gemma":[0.9988439,0.0000107358255,0.0000057052407,0.0003636236,0.0006244405,8.817454e-7,0.0000019033547,0.0000017007768,0.00014712666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99896735,0.00007402712,0.00011951866,0.000061969746,0.000173312,0.000603822],"domain_scores_gemma":[0.99945384,0.00005667236,0.000065882356,0.00014978397,0.000016872105,0.0002569715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006962166,0.000046769168,0.00006602212,0.000014044268,0.00040129584,0.0001188253,0.00033723115,0.000029530127,0.0001421304],"category_scores_gemma":[0.00008732467,0.00002567852,0.00004340766,0.000060521914,0.000086949454,0.000051857463,0.000007350019,0.00008805716,0.000023865718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027474458,0.000008141737,0.8440975,0.000010700996,0.000061457904,0.0000066866437,0.0005059752,0.0016578662,0.00003404842,0.0020481013,0.041543312,0.10999877],"study_design_scores_gemma":[0.00004280991,0.0000046454365,0.57591087,0.0000014184807,0.0000039374236,0.0000011604516,0.0000036280442,0.000020018346,0.00006034703,0.0002816758,0.4236469,0.000022585287],"about_ca_topic_score_codex":0.03994096,"about_ca_topic_score_gemma":0.67750186,"teacher_disagreement_score":0.6375609,"about_ca_system_score_codex":0.000008254412,"about_ca_system_score_gemma":0.00017534384,"threshold_uncertainty_score":0.9664522},"labels":[],"label_agreement":null},{"id":"W7074089912","doi":"","title":"Deletion of GSK-3beta in mice leads to hypertrophic cardiomyopathy secondary to cardiomyoblast hyperproliferation.","year":2008,"lang":"en","type":"article","venue":"The Medicine Forum","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; National Institutes of Health; Paavo Nurmen Säätiö; American Heart Association","keywords":"Hypertrophic cardiomyopathy; Regulator; Muscle hypertrophy; Heart disease; Embryoid body; Heart failure; Diabetic cardiomyopathy; Embryogenesis; Cardiomyopathy","score_opus":0.011672552100002665,"score_gpt":0.20916646355469914,"score_spread":0.19749391145469647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074089912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98895293,0.00038675423,0.00014623109,0.005550201,0.00062856404,0.0003838898,0.00006831825,0.000018195089,0.0038649268],"genre_scores_gemma":[0.99772084,0.000041011444,0.00014687692,0.0013474703,0.00046306592,0.000007192052,0.0000484461,0.0000057075317,0.00021936891],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873364,0.000111577036,0.00031331362,0.00021353732,0.0003258043,0.00030212133],"domain_scores_gemma":[0.9994115,0.0000764254,0.000056789602,0.00026978532,0.000066149245,0.00011931257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000495284,0.00013881488,0.00038749585,0.0001319715,0.00012930277,0.000008118117,0.00025490538,0.000042191325,0.00032341754],"category_scores_gemma":[0.00006429314,0.000086771026,0.000047782272,0.00034913857,0.00009222542,0.000080669124,0.000028632334,0.00009794507,0.00020488452],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017237456,0.0001247121,0.41803882,0.00030860407,0.00023147746,0.00031685588,0.015749542,0.09212078,0.32427847,0.0010837454,0.097112924,0.048910327],"study_design_scores_gemma":[0.001960928,0.0023822077,0.8870357,0.00024443175,0.00011987297,0.0003001223,0.0009064284,0.00091198494,0.01939872,0.0010788683,0.08499707,0.0006636281],"about_ca_topic_score_codex":0.00508484,"about_ca_topic_score_gemma":0.0012168398,"teacher_disagreement_score":0.46899694,"about_ca_system_score_codex":0.000004954799,"about_ca_system_score_gemma":0.00005960531,"threshold_uncertainty_score":0.76867914},"labels":[],"label_agreement":null},{"id":"W7074091142","doi":"","title":"Has mortality from acute respiratory distress syndrome decreased over time?: A systematic review.","year":2009,"lang":"en","type":"article","venue":"TSpace","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Hospital for Sick Children; University of Toronto","keywords":"Observational study; ARDS; Odds ratio; Confidence interval; Randomized controlled trial; Mortality rate; Meta-analysis; Risk of mortality; Acute respiratory distress","score_opus":0.020008172885791764,"score_gpt":0.2780511234058955,"score_spread":0.25804295052010373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074091142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902422,0.006269405,0.000018830573,0.00026887626,0.00018653605,0.0006368673,0.00065299147,0.000090271446,0.0016340342],"genre_scores_gemma":[0.997355,0.00014189744,0.0000802631,0.0012084867,0.000085424654,0.000004603187,0.00035550699,0.0000051029533,0.00076372764],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9985599,0.00021327025,0.00032395948,0.0002980288,0.0003390882,0.00026578084],"domain_scores_gemma":[0.9989432,0.00008795236,0.00018693993,0.00057016814,0.000029322455,0.00018240526],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003332926,0.00019369107,0.00062409305,0.000023812125,0.000114718576,0.00012740087,0.0002901024,0.00006282886,0.0038567604],"category_scores_gemma":[0.000060300314,0.00014527407,0.00009825676,0.00012678216,0.000043802986,0.00014501096,0.0000112188245,0.00007161054,0.0013720995],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011149679,0.0019530489,0.09479813,0.3430934,0.009097227,0.013862393,0.008827874,0.0009289963,0.11481407,0.0016670485,0.40687,0.0029728583],"study_design_scores_gemma":[0.0010906567,0.00050173217,0.9534453,0.032189578,0.00290846,0.000040820083,0.00005217134,0.00084978645,0.001342641,0.0022093514,0.0039584194,0.0014110429],"about_ca_topic_score_codex":0.0029226793,"about_ca_topic_score_gemma":0.00014596971,"teacher_disagreement_score":0.8586472,"about_ca_system_score_codex":0.0000041019,"about_ca_system_score_gemma":0.00004066709,"threshold_uncertainty_score":0.99940544},"labels":[],"label_agreement":null},{"id":"W7074095876","doi":"","title":"Supportive communication with parents moderates the negative effects of electronic media use on life satisfaction during adolescence","year":2014,"lang":"en","type":"article","venue":"Utrecht University Repository (Utrecht University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Electronic media; Life satisfaction; Electronic communication; Media use; Sample (material); Computer-mediated communication","score_opus":0.004304121190653929,"score_gpt":0.14140441424067632,"score_spread":0.1371002930500224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074095876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960178,0.000021237689,0.00020293945,0.000056090717,0.00016441806,0.00027437267,0.00003196831,0.000060335078,0.0031708211],"genre_scores_gemma":[0.9985088,0.00013732899,0.00013248117,0.000018848968,0.000036067468,8.891208e-8,0.000033128686,0.0000053207127,0.0011279084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983771,0.0006012886,0.00012963734,0.0003213341,0.00028154792,0.00028911172],"domain_scores_gemma":[0.9982643,0.00075075193,0.00029521793,0.00042680823,0.00013125433,0.00013162811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012740944,0.0001956524,0.00025625725,0.00016621692,0.000614813,0.000044455526,0.0004122708,0.000103578954,0.000036693258],"category_scores_gemma":[0.000050827937,0.00016233495,0.000067816276,0.0003738917,0.00024622388,0.0005584038,0.000051003633,0.00024664737,0.000013216875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008216148,0.00055640296,0.9120545,0.000461754,0.0015586275,0.00041489833,0.010902789,0.021830775,0.012046966,0.0154424915,0.00062270416,0.015891936],"study_design_scores_gemma":[0.0019679628,0.00056908245,0.9517538,0.000334915,0.00035092985,0.000010608338,0.002072962,0.0013420872,0.039490063,0.00021875396,0.0014267501,0.00046208996],"about_ca_topic_score_codex":0.0067776283,"about_ca_topic_score_gemma":0.0022002717,"teacher_disagreement_score":0.039699286,"about_ca_system_score_codex":0.00005820871,"about_ca_system_score_gemma":0.0001349183,"threshold_uncertainty_score":0.9998363},"labels":[],"label_agreement":null},{"id":"W7074098028","doi":"","title":"A sustainable identity: The creativity of an everyday designer","year":2009,"lang":"en","type":"article","venue":"Summit (Simon Fraser University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Social Sciences and Humanities Research Council of Canada","keywords":"Cognitive reframing; Creativity; Everyday life; Sustainability; Sustainable design; Set (abstract data type); Ethnography; Identity (music); Work (physics)","score_opus":0.010038511786467644,"score_gpt":0.1989374010111893,"score_spread":0.18889888922472167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074098028","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859503,0.00004390322,0.00027570612,0.00012891882,0.000088878165,0.00016100396,0.000050439132,0.00003160649,0.01326927],"genre_scores_gemma":[0.99473226,0.000020482757,0.000102105165,0.00008122552,0.000051605744,4.2804654e-8,0.000032225107,0.0000018911414,0.0049781497],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990772,0.00017197122,0.00009587377,0.00019167562,0.00020249964,0.00026078656],"domain_scores_gemma":[0.99939793,0.000066862995,0.00008126098,0.00027890503,0.00008430604,0.00009075134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002821164,0.000107658285,0.0001675475,0.00010126882,0.00023320477,0.000067690075,0.00043411306,0.000056960842,0.00079327007],"category_scores_gemma":[0.000018814597,0.00008258198,0.000058972415,0.00043940227,0.00008386456,0.0010416249,0.00002104548,0.00007024002,0.000044434037],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073438126,0.0003825189,0.91554046,0.00010038403,0.00016475671,0.0008273577,0.0003497056,0.005806374,0.00044634927,0.046385914,0.014850287,0.014411535],"study_design_scores_gemma":[0.0017903583,0.0013292657,0.5785948,0.000043593434,0.0003437748,4.7287646e-8,0.02819443,0.0012553757,0.013664843,0.030464265,0.34342998,0.0008892441],"about_ca_topic_score_codex":0.006422298,"about_ca_topic_score_gemma":0.036745634,"teacher_disagreement_score":0.33694562,"about_ca_system_score_codex":0.000005950309,"about_ca_system_score_gemma":0.000059540085,"threshold_uncertainty_score":0.98083127},"labels":[],"label_agreement":null},{"id":"W7074099111","doi":"","title":"The sun doesn't shine so brightly any more","year":2024,"lang":"en","type":"other","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"The Holocaust; Persecution; Nazism; Refugee; World War II; Nazi Germany; Power (physics); Judaism","score_opus":0.005872344395016856,"score_gpt":0.2085956510867282,"score_spread":0.20272330669171135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074099111","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00020050943,0.0054147257,0.000007071408,0.0010798102,0.0037131,0.0002052678,0.00072108937,0.00023904233,0.98841935],"genre_scores_gemma":[0.0017744208,0.00052809116,0.00012547158,0.000345751,0.0016284456,0.000001611761,0.00019696348,0.00006420583,0.99533504],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989703,0.000032410175,0.00015413327,0.0003037297,0.00023857932,0.0003008171],"domain_scores_gemma":[0.9994399,0.00004541777,0.000064574066,0.00035492977,0.000010040533,0.00008517105],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00016707109,0.00022032022,0.00023425234,0.00004549868,0.000103078615,0.00046595515,0.00037226535,0.0001494279,0.0609722],"category_scores_gemma":[0.0000054644465,0.00010285915,0.00007816272,0.000087878245,0.00011842075,0.000032684526,0.000025686453,0.000121027806,0.013377725],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000037582004,0.000002528568,0.00010890229,0.000050570496,0.00006715579,0.00002288047,0.000030164627,0.000002701717,0.000008357559,0.0013540772,0.99640423,0.0019446613],"study_design_scores_gemma":[0.000042550993,0.000017281089,0.0011044439,0.000043403554,0.000035244993,0.000002433024,0.00001017746,0.000033386914,0.000023116552,0.002493234,0.99601424,0.0001804867],"about_ca_topic_score_codex":0.019072516,"about_ca_topic_score_gemma":0.023600735,"teacher_disagreement_score":0.047594473,"about_ca_system_score_codex":6.5520203e-7,"about_ca_system_score_gemma":0.000044600372,"threshold_uncertainty_score":0.994216},"labels":[],"label_agreement":null},{"id":"W7074103443","doi":"","title":"Shock Tubes: Proceedings of the Seventh International Shock Tube Symposium held at University of Toronto, Toronto, Canada 23-25 June 1969","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shock (circulatory); Shock tube; Tube (container); Shock wave","score_opus":0.0074560193947675575,"score_gpt":0.17565144312874,"score_spread":0.16819542373397245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074103443","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6668653,0.0000075953376,0.0000015853012,0.00023949763,0.001152318,0.00035019932,0.00086348143,0.00005230222,0.33046773],"genre_scores_gemma":[0.9847337,0.012773063,0.00004394451,0.00003313857,0.00009586061,1.4325377e-7,0.000118073265,0.00000765106,0.0021944456],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986834,0.00004349794,0.00017727492,0.00032818876,0.0004525509,0.00031511538],"domain_scores_gemma":[0.9993136,0.00006177435,0.00015433917,0.00019564148,0.00018480643,0.00008983709],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014189487,0.00018492933,0.00027292268,0.00030051867,0.00021140768,0.000021586819,0.0008509037,0.00010806644,0.0012144019],"category_scores_gemma":[0.000015591735,0.0001676996,0.00011984709,0.001028933,0.00009038803,0.00051502377,0.00024895443,0.000090782334,0.00001369229],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.006026873,0.0014521449,0.5799018,0.0039025168,0.0054134806,0.00084495975,0.084654056,0.0072804606,0.023100184,0.014991122,0.25711995,0.015312426],"study_design_scores_gemma":[0.0005040543,0.00008259903,0.016471632,0.0000601801,0.000088636734,0.0000036696204,0.0018895733,0.0006539382,0.0021521198,0.0000011462828,0.9778732,0.00021922331],"about_ca_topic_score_codex":0.9811714,"about_ca_topic_score_gemma":0.99073935,"teacher_disagreement_score":0.72075325,"about_ca_system_score_codex":0.00020010766,"about_ca_system_score_gemma":0.00054591853,"threshold_uncertainty_score":0.99969864},"labels":[],"label_agreement":null},{"id":"W7074105068","doi":"","title":"Francophone Poetics in Tension: Intuition, Relation, and Exiguity from Senghor to Canadian Minority Voices","year":2025,"lang":"en","type":"article","venue":"Journals & Books Hosting (International Knowledge Sharing Platform)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"French; Poetics; Intuition; Transculturation; Cognitive dissonance; Postcolonialism (international relations)","score_opus":0.022473437057219693,"score_gpt":0.2668898445399881,"score_spread":0.2444164074827684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074105068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95863104,0.0008909948,0.00015716418,0.0007709086,0.0027245646,0.00019650074,0.00027233758,0.00003322177,0.03632329],"genre_scores_gemma":[0.9966207,0.00007159803,0.0009397574,0.0004055637,0.000684609,0.0000026483492,0.000122040445,0.0000057143925,0.0011473283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842775,0.000029886753,0.0005639201,0.00038368328,0.00024929232,0.00034547749],"domain_scores_gemma":[0.9988367,0.0002467765,0.0001539216,0.00016983796,0.00031001717,0.00028274194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067990634,0.00019598928,0.00027679658,0.0004907211,0.00033937153,0.00037944267,0.0003555562,0.0001257615,0.0006990799],"category_scores_gemma":[0.0004280935,0.00018873821,0.000047927973,0.00027088137,0.000034218214,0.0004237007,0.00008507224,0.00029869907,0.00012102306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000118149466,0.00004908588,0.95743215,0.000075676726,0.00016117217,0.00009502605,0.0035806322,0.0021179602,0.0025470597,0.001800155,0.0064265165,0.0255964],"study_design_scores_gemma":[0.00047827142,0.00002838855,0.94097686,0.00066308805,0.00002116021,0.00001227529,0.0001356835,0.009551334,0.0003262131,0.020611439,0.0269173,0.00027796332],"about_ca_topic_score_codex":0.13786122,"about_ca_topic_score_gemma":0.38351,"teacher_disagreement_score":0.24564876,"about_ca_system_score_codex":0.000064185275,"about_ca_system_score_gemma":0.00023451462,"threshold_uncertainty_score":0.8678798},"labels":[],"label_agreement":null},{"id":"W7074124714","doi":"","title":"Transfusion Camp: The UK experience and its value in improving knowledge of transfusion medicine among postgraduate trainees","year":2024,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transfusion medicine; SAFER; Excellence; Blood transfusion; Likert scale; Confidence interval","score_opus":0.02151587658159618,"score_gpt":0.24030142521595016,"score_spread":0.21878554863435398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074124714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990451,0.00046463872,0.0007055378,0.00053670106,0.00011855349,0.0004903014,0.00031282776,0.000024598088,0.00689586],"genre_scores_gemma":[0.99274665,0.006384484,0.0001756551,0.0000031714728,0.00003320236,9.005169e-8,0.00005239339,0.0000053688705,0.0005989752],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9980822,0.00044193116,0.00016818017,0.0004346582,0.0004300921,0.00044289764],"domain_scores_gemma":[0.9988602,0.00055273576,0.000059391103,0.00021863867,0.00012459181,0.00018447448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096845377,0.00017080811,0.0003372251,0.0005917759,0.00050615135,0.000025791578,0.0006954003,0.00008350077,0.0004915992],"category_scores_gemma":[0.000039748502,0.00014595874,0.00009708353,0.00089068466,0.0010908695,0.0004826326,0.00013981845,0.0003840666,0.0000032155108],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0045407857,0.00037167754,0.15720959,0.0033277702,0.00040312085,0.0011286064,0.4295731,0.0018512378,0.22449431,0.030793615,0.0009125354,0.14539365],"study_design_scores_gemma":[0.0033555853,0.0022661549,0.7724773,0.0015422027,0.0001821167,0.000024686124,0.09230408,0.089802414,0.002219253,0.004550408,0.030525666,0.00075008237],"about_ca_topic_score_codex":0.03456841,"about_ca_topic_score_gemma":0.025884716,"teacher_disagreement_score":0.61526775,"about_ca_system_score_codex":0.000017500495,"about_ca_system_score_gemma":0.00015649221,"threshold_uncertainty_score":0.9918904},"labels":[],"label_agreement":null},{"id":"W7074132002","doi":"","title":"What can we learn from 25 years of PUS survey research? Liberating and expanding the agenda","year":2007,"lang":"en","type":"article","venue":"London School of Economics and Political Science Research Online (London School of Economics and Political Science)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Rhetoric; Science communication; Public awareness of science; Perception; Relation (database); Survey data collection; Quarter (Canadian coin); Period (music)","score_opus":0.07965842614379956,"score_gpt":0.359498344258387,"score_spread":0.2798399181145874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074132002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935679,0.00075995945,0.0000041924577,0.0026859704,0.00038740766,0.00038104987,0.0009127561,0.0000060085076,0.0012947833],"genre_scores_gemma":[0.9937022,0.0050634188,0.0005624205,0.00018624995,0.0003531333,0.0000019497572,0.000028897432,0.000011216416,0.000090548856],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9939383,0.0004114035,0.0011809805,0.0010058045,0.0006159712,0.002847539],"domain_scores_gemma":[0.9909725,0.004704298,0.00025813593,0.0006000285,0.0006135553,0.0028514361],"candidate_categories":["sts","scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.022818498,0.00026509803,0.0007345154,0.0007333518,0.0008111335,0.0012131635,0.0012364214,0.00017060785,0.000244247],"category_scores_gemma":[0.0035135928,0.00021200551,0.00008433299,0.00085386675,0.00999643,0.001498555,0.00066482247,0.0007300206,0.000017061666],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003754057,0.00019766092,0.24648389,0.00013237473,0.00007277426,0.000011782671,0.0006490839,0.00023238416,0.008676776,0.7218394,0.000090044305,0.021238387],"study_design_scores_gemma":[0.00075599254,0.0006272387,0.86924154,0.00014036281,0.000018165121,0.000013711999,0.002898709,0.004561701,0.009048723,0.11109811,0.0012088452,0.0003869048],"about_ca_topic_score_codex":0.060787734,"about_ca_topic_score_gemma":0.011334597,"teacher_disagreement_score":0.6227576,"about_ca_system_score_codex":0.00011406987,"about_ca_system_score_gemma":0.0019913253,"threshold_uncertainty_score":0.9998237},"labels":[],"label_agreement":null},{"id":"W7074136844","doi":"","title":"A rapid screening test to distinguish between Candida albicans and Candida dubliniensis using NMR spectroscopy","year":2005,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Candida dubliniensis; Candida albicans; Nuclear magnetic resonance spectroscopy; Screening test","score_opus":0.021916400795198764,"score_gpt":0.24265676884096307,"score_spread":0.2207403680457643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074136844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902035,0.00007209106,0.000408446,0.0006148929,0.00014580895,0.00017899217,0.00056365406,0.000047315,0.007765314],"genre_scores_gemma":[0.9746077,0.000014713599,0.023684965,0.00027732807,0.001204026,0.0000010949037,0.000065843604,0.000008234802,0.00013607828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869394,0.00004312551,0.00023782325,0.00034149876,0.0002255383,0.0004580889],"domain_scores_gemma":[0.99918276,0.00020004854,0.00007913195,0.00018976041,0.000040809897,0.00030746032],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026338408,0.00017470363,0.0002956249,0.0000778233,0.00027516918,0.0001935761,0.00015844221,0.00005367331,0.0021871724],"category_scores_gemma":[0.00012289018,0.00015451224,0.00003496227,0.00019907467,0.000061777944,0.00013976237,0.00003361747,0.00009263836,0.00006135067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006706122,0.000028216778,0.8607102,0.000043728724,0.00007935337,0.00003212148,0.0012130097,0.00096320896,0.04140114,0.00007702353,0.004143405,0.091241516],"study_design_scores_gemma":[0.0009291373,0.00046257259,0.8584962,0.00012999077,0.00016967775,0.000021949769,0.00014098464,0.008527911,0.011787853,0.00082796265,0.11759114,0.00091462943],"about_ca_topic_score_codex":0.008067241,"about_ca_topic_score_gemma":0.0042578136,"teacher_disagreement_score":0.11344773,"about_ca_system_score_codex":0.0000060495945,"about_ca_system_score_gemma":0.00005070571,"threshold_uncertainty_score":0.99872494},"labels":[],"label_agreement":null},{"id":"W7074139268","doi":"","title":"Towards Principled Oceans Governance","year":2006,"lang":"en","type":"book","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Social Sciences and Humanities Research Council of Canada; Natural Sciences and Engineering Research Council of Canada; Dalhousie University; Industry Canada; Australian Government; Transport Canada","keywords":"Operationalization; Corporate governance; International waters; Marine conservation; Key (lock); Indian ocean; Maritime boundary; International relations","score_opus":0.008312901706742157,"score_gpt":0.18831245726457968,"score_spread":0.17999955555783753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074139268","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004083104,0.00034802838,0.00003101023,0.00007368523,0.0010766698,0.00019763291,0.0013988408,0.00009185717,0.99637395],"genre_scores_gemma":[0.004036329,0.000097034164,0.00040629428,0.00016140928,0.0010917772,7.0040505e-7,0.0013242989,0.000010512568,0.99287164],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99863833,0.00002133683,0.00027485585,0.00035929782,0.00039303288,0.0003131735],"domain_scores_gemma":[0.9993344,0.000035444868,0.0001801231,0.00032051155,0.000040802766,0.00008872267],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00012918538,0.00027809828,0.00039286516,0.000022915587,0.000074901574,0.0001040017,0.00036484512,0.0002241235,0.01647706],"category_scores_gemma":[0.0000066059665,0.00021363133,0.000111950896,0.000036462883,0.000052351952,0.00009526704,0.000023745899,0.0001424019,0.002628523],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016514745,0.000010568002,0.00038233752,0.000092825445,0.00005173691,0.000052543925,0.000018696359,0.00031773085,0.0000063182692,0.022844367,0.96788853,0.008317799],"study_design_scores_gemma":[0.000106930114,0.000036369576,0.017572267,0.000030655818,0.000030103987,0.000002369733,3.5664462e-7,0.00008175525,0.000025297315,0.00798567,0.9738169,0.0003113755],"about_ca_topic_score_codex":0.0035251032,"about_ca_topic_score_gemma":0.0027290133,"teacher_disagreement_score":0.017189931,"about_ca_system_score_codex":0.000007545489,"about_ca_system_score_gemma":0.00029288526,"threshold_uncertainty_score":0.998148},"labels":[],"label_agreement":null},{"id":"W7074142324","doi":"","title":"17BIPHE2, an engineered cathelicidin antimicrobial peptide with low susceptibility to proteases, is an effective spermicide and microbicide against Neisseria gonorrhoeae","year":2022,"lang":"en","type":"article","venue":"NOVA (University of Newcastle Australia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Spermicide; Cathelicidin; Neisseria gonorrhoeae; Sperm; In vivo; Antimicrobial; Sperm motility; Peptide; In vitro","score_opus":0.02983294283039603,"score_gpt":0.23157000918041928,"score_spread":0.20173706635002325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074142324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971493,0.0000058590485,0.000065796994,0.00016785288,0.0001414394,0.00079935684,0.001547283,0.000041561285,0.00008153237],"genre_scores_gemma":[0.99720967,0.0000021645917,0.001879935,0.00012202651,0.000061118204,5.6778424e-7,0.0003486236,0.000009912916,0.0003659898],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.998638,0.00016255576,0.00014464036,0.00055686303,0.00012466892,0.00037328983],"domain_scores_gemma":[0.99910516,0.000029252116,0.00012049382,0.00039255555,0.00008019716,0.00027237344],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002530425,0.0002296843,0.00035701803,0.00012563656,0.0003294927,0.000049874656,0.00037615877,0.00006210956,0.0025929708],"category_scores_gemma":[0.0000061339492,0.00025465322,0.000058381338,0.0003068763,0.00012412397,0.0004404285,0.00007930807,0.0001688745,0.000051491625],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016257017,0.00032295758,0.038015634,0.00015869686,0.00012369266,0.00009503505,0.0077963634,0.018729536,0.92600435,0.000020697431,0.0020200415,0.0050873244],"study_design_scores_gemma":[0.0026044708,0.0041171913,0.92945623,0.000087977816,0.0001819352,0.000113655115,0.005476729,0.0012543381,0.049815435,0.000055850494,0.00563117,0.001205036],"about_ca_topic_score_codex":0.0438139,"about_ca_topic_score_gemma":0.015176015,"teacher_disagreement_score":0.8914406,"about_ca_system_score_codex":0.000023358085,"about_ca_system_score_gemma":0.000063125015,"threshold_uncertainty_score":0.9999906},"labels":[],"label_agreement":null},{"id":"W7074144125","doi":"","title":"Shaping policy: the Canadian Cancer Society and the Hormone Receptor Testing Inquiry","year":2011,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cancer; Receptor; Hormone receptor; Hormone; MEDLINE; Disease","score_opus":0.054998652591449995,"score_gpt":0.2158708700236402,"score_spread":0.1608722174321902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074144125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9806003,0.002481524,0.000005130248,0.0036242867,0.0013043422,0.00053632364,0.00016508711,0.000050343366,0.011232646],"genre_scores_gemma":[0.9960125,0.0007433617,0.00021435332,0.0015282528,0.0012039514,0.000011451866,0.000012000339,0.000008998496,0.00026514434],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984815,0.00016396254,0.00016702122,0.00022146326,0.00016020745,0.0008058104],"domain_scores_gemma":[0.9992408,0.000109375724,0.00008788497,0.00020720845,0.0000472011,0.0003075032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006826473,0.00014182673,0.00014589849,0.00002044977,0.0006057156,0.0001857531,0.0003319876,0.000041123563,0.00028633815],"category_scores_gemma":[0.00016062058,0.00007542779,0.00004099062,0.0002826093,0.0003412817,0.00012710594,0.00003276352,0.00015281094,0.00005764641],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002706173,0.00003997827,0.45235234,0.000106078885,0.0005623987,0.000043078286,0.24878111,0.0004636366,0.0014372183,0.007787993,0.061878465,0.22627708],"study_design_scores_gemma":[0.0003400585,0.000014523207,0.91483194,0.000012193427,0.000031327538,0.0000040481245,0.0001822925,0.00023379333,0.000137563,0.00035470445,0.08369657,0.000161011],"about_ca_topic_score_codex":0.56136775,"about_ca_topic_score_gemma":0.10451219,"teacher_disagreement_score":0.4624796,"about_ca_system_score_codex":0.000012923058,"about_ca_system_score_gemma":0.00029143016,"threshold_uncertainty_score":0.9118281},"labels":[],"label_agreement":null},{"id":"W7074145292","doi":"","title":"Multiproxy bioarchaeological data reveals interplay between growth, diet and population dynamics across the transition to farming in the central Mediterranean","year":2023,"lang":"en","type":"article","venue":"Apollo (University of Cambridge)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Arts and Humanities Research Council; Isaac Newton Trust; Leverhulme Trust","keywords":"Scholarship; Prehistory; Maltese; Research council; Population; White (mutation); General partnership","score_opus":0.02725647668791081,"score_gpt":0.2597935796013979,"score_spread":0.23253710291348706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074145292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99351054,0.000010786001,0.0004574823,0.0037553075,0.00013050428,0.00022886593,0.0018536925,0.00001776066,0.000035033503],"genre_scores_gemma":[0.99792737,0.000035008732,0.00011190271,0.000076373115,0.000074692434,8.889404e-8,0.0017414739,0.0000017328441,0.00003134781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991275,0.00015124623,0.00010772552,0.00020540596,0.00017268762,0.00023541159],"domain_scores_gemma":[0.9994755,0.00019417601,0.000051309133,0.00021207666,0.000015012734,0.000051958614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006614577,0.00007742691,0.0001540517,0.00004582596,0.00021290132,0.000026712516,0.0004894991,0.000049563023,0.000012273578],"category_scores_gemma":[0.00002748391,0.000055112938,0.000026019912,0.0002598484,0.00015199005,0.0002255917,0.00009938826,0.00007958259,0.000011145203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041777588,0.000025109764,0.91672754,0.000113948634,0.00006573788,0.000081217775,0.04487023,0.00045199515,0.00035353497,0.00086506,0.0013478961,0.034679946],"study_design_scores_gemma":[0.00018321307,0.00007498812,0.9872344,0.000018938814,0.000018010121,0.00000180954,0.0038135785,0.008142007,0.000004114554,0.00017641131,0.0002589759,0.00007356665],"about_ca_topic_score_codex":0.031179167,"about_ca_topic_score_gemma":0.0128870085,"teacher_disagreement_score":0.07050684,"about_ca_system_score_codex":0.0000037691198,"about_ca_system_score_gemma":0.0000067640963,"threshold_uncertainty_score":0.9752723},"labels":[],"label_agreement":null},{"id":"W7074152960","doi":"","title":"The genome of Eucalyptus grandis","year":2014,"lang":"en","type":"article","venue":"Americanae (AECID Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Genome; Reference genome; Eucalyptus; Inbreeding; Genome size; Perennial plant; Adaptability; Comparative genomics","score_opus":0.003072355191708602,"score_gpt":0.15584456619499487,"score_spread":0.15277221100328628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074152960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97532284,0.00039355003,0.00013935428,0.0008426583,0.00044805353,0.000114874834,0.00010293797,0.000052201583,0.022583548],"genre_scores_gemma":[0.99795365,0.00018834259,0.00042904948,0.00034522504,0.00021018564,0.0000013998516,0.000064998785,0.000006275355,0.0008008657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907404,0.000110165856,0.00021349356,0.00016862527,0.00017257576,0.00026111607],"domain_scores_gemma":[0.99920076,0.00022987663,0.0001366124,0.0003147575,0.00001163503,0.00010636109],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012749266,0.0001093982,0.00021694983,0.000031914406,0.0001533727,0.000039541777,0.0003974656,0.000025260224,0.0020985696],"category_scores_gemma":[0.000022529866,0.00006748219,0.0000674911,0.00022529309,0.00023127902,0.00023854944,0.000025067882,0.0000516265,0.00022706641],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019514518,0.000054667657,0.7346681,0.000051068848,0.00020549486,0.000011963753,0.00041475758,0.001117072,0.0032522879,0.015623767,0.023197792,0.22120793],"study_design_scores_gemma":[0.000116534364,0.00014487623,0.8512747,0.0000033881531,0.000013502823,7.4213773e-7,0.000025126545,0.00021796925,0.0006989528,0.0023331752,0.14505018,0.000120833494],"about_ca_topic_score_codex":0.019030482,"about_ca_topic_score_gemma":0.000101103,"teacher_disagreement_score":0.2210871,"about_ca_system_score_codex":4.676991e-7,"about_ca_system_score_gemma":0.000028806204,"threshold_uncertainty_score":0.9988136},"labels":[],"label_agreement":null},{"id":"W7074162762","doi":"","title":"Integrating Acupuncture with Exercise-based Physical Therapy for Knee Osteoarthritis: A Randomized Controlled Trial","year":2013,"lang":"en","type":"article","venue":"Journal of Bioresource Management","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Acupuncture; Osteoarthritis; Randomized controlled trial; Logistic regression; Adverse effect; Electroacupuncture","score_opus":0.0049761894717796065,"score_gpt":0.19770822704982452,"score_spread":0.1927320375780449,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074162762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864584,0.00048561336,0.0026332622,0.0003711009,0.00062078924,0.0081728175,0.000016182548,0.000022273358,0.0012195535],"genre_scores_gemma":[0.9938049,0.000030375713,0.0044678957,0.00022636924,0.00095792295,0.00018242108,0.00001535627,0.000010519587,0.0003042757],"study_design_codex":"randomized_trial","study_design_gemma":"randomized_trial","domain_scores_codex":[0.9983465,0.00019128565,0.00057905767,0.00017148026,0.00044211338,0.00026954946],"domain_scores_gemma":[0.9984647,0.00045868,0.0006499646,0.00015432532,0.00015689076,0.00011542737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00089120143,0.00026640584,0.0014095948,0.00013250641,0.00011499097,0.00026985767,0.00022827758,0.000047138336,0.00040289777],"category_scores_gemma":[0.000033354172,0.000114232455,0.00055425783,0.00010104339,0.00008532058,0.0001334975,0.000008996382,0.000108788365,0.000019172852],"study_design_candidate":"randomized_trial","study_design_consensus":"randomized_trial","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.89611787,0.00015069118,0.000047165766,0.00004056842,0.00045782138,0.000015938562,0.0002468319,0.0021630942,0.00009617506,0.00009675206,0.00072250393,0.09984458],"study_design_scores_gemma":[0.9859062,0.0045419573,0.0002824037,0.00017982748,0.00036343484,0.0000026740506,0.00021152322,0.0041158926,0.0001465843,0.00063195784,0.003419391,0.00019816207],"about_ca_topic_score_codex":0.00006762169,"about_ca_topic_score_gemma":0.000009606898,"teacher_disagreement_score":0.09964643,"about_ca_system_score_codex":0.000003820374,"about_ca_system_score_gemma":0.000029686636,"threshold_uncertainty_score":0.46582642},"labels":[],"label_agreement":null},{"id":"W7074165314","doi":"","title":"The Burgess Shale anomalocaridid Hurdia and its significance for early euarthropod evolution.","year":2009,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Carapace; Arthropod; Oil shale; Morphology (biology); Assemblage (archaeology); Taphonomy; Faunal assemblage","score_opus":0.01858027092073551,"score_gpt":0.22688594871770928,"score_spread":0.2083056777969738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074165314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9802105,0.00039052079,0.0037369088,0.0011135826,0.00014006467,0.0009082692,0.0013102605,0.000048200338,0.012141695],"genre_scores_gemma":[0.99408185,0.0012609988,0.00095543015,0.00001143339,0.00006946288,1.14918706e-7,0.00009034134,0.000004832718,0.0035255388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979225,0.00029760762,0.00012439082,0.00046119775,0.0004757148,0.00071862334],"domain_scores_gemma":[0.998352,0.0005858038,0.00012284527,0.00032952463,0.00030946257,0.00030039015],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00071454595,0.00017677496,0.00029175912,0.00023947516,0.0021733916,0.0000807485,0.0009033636,0.000089894114,0.00015910996],"category_scores_gemma":[0.000054961216,0.00017674487,0.00013129872,0.0004407925,0.00070277246,0.00059855153,0.00014131807,0.00026708242,0.000013873621],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.01652852,0.0008260835,0.4311303,0.00073674665,0.0012072072,0.000830667,0.011332612,0.001383723,0.017752552,0.36477455,0.033487223,0.12000981],"study_design_scores_gemma":[0.0016262964,0.0016299537,0.7573025,0.000056075743,0.00006709663,0.0000051697316,0.0046725385,0.004790479,0.00014640075,0.014709803,0.21457073,0.00042293922],"about_ca_topic_score_codex":0.0025701318,"about_ca_topic_score_gemma":0.001979771,"teacher_disagreement_score":0.35006475,"about_ca_system_score_codex":0.000024886733,"about_ca_system_score_gemma":0.0002265941,"threshold_uncertainty_score":0.99912566},"labels":[],"label_agreement":null},{"id":"W7074166037","doi":"","title":"Typhoid and Malaria Co-Infection – An Interesting Finding in the Investigation of a Tropical Fever","year":2006,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Typhoid fever; Malaria; Salmonella typhi; Vivax malaria; Dengue fever; Vector (molecular biology); Plasmodium vivax; Enteric fever","score_opus":0.0197407096402078,"score_gpt":0.2091836366819772,"score_spread":0.1894429270417694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074166037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841887,0.000034736782,0.00002431301,0.00009760922,0.00022647079,0.00016524005,0.000017710012,0.000014115043,0.0010009394],"genre_scores_gemma":[0.99953043,0.000013503874,0.00013270119,0.000045112993,0.00019083802,0.0000017192414,0.000052130497,0.000003016762,0.0000305506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99907696,0.00022668303,0.0001791362,0.0001461606,0.000114426046,0.0002566142],"domain_scores_gemma":[0.9997088,0.000057700716,0.000074355325,0.00009193437,0.0000139324775,0.000053289095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030320112,0.00007585038,0.00009889415,0.000039375594,0.000056510322,0.00007583178,0.00008616313,0.000029178014,0.00007017231],"category_scores_gemma":[0.000045881377,0.00005336132,0.000013317012,0.00014223893,0.000052945685,0.00018833615,0.000006904948,0.00007748923,0.000008212585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001446622,0.000009234034,0.9948273,0.000014988474,0.0000026164378,0.0000062646577,0.00079679705,0.0001778331,0.0020571793,0.00048266037,0.000081243044,0.0015294196],"study_design_scores_gemma":[0.00016283472,0.00003104816,0.9965337,0.000013103279,0.000008092145,0.0000060484235,0.000015704032,0.0002899611,0.0014543687,0.00039086884,0.0010313347,0.00006296134],"about_ca_topic_score_codex":0.0023724283,"about_ca_topic_score_gemma":0.00096497586,"teacher_disagreement_score":0.0017063767,"about_ca_system_score_codex":0.0000025851552,"about_ca_system_score_gemma":0.00001489455,"threshold_uncertainty_score":0.35864177},"labels":[],"label_agreement":null},{"id":"W7074169586","doi":"","title":"Helicobacter pylori in First Nations and recent immigrant populations in Canada","year":2012,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Helicobacter pylori; Epidemiology; Immigration; Spirillaceae; Helicobacter pylori infection; Public health","score_opus":0.019198967686833344,"score_gpt":0.19400162955889974,"score_spread":0.1748026618720664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074169586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952369,0.0005453429,0.0000017670765,0.00079700176,0.001314419,0.00024191597,0.00014858418,0.000009800668,0.001704293],"genre_scores_gemma":[0.99876916,0.000710714,0.00006216238,0.000101943464,0.00016145539,0.000006487803,0.00009943571,0.000004716591,0.000083947896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99872035,0.000079200414,0.00022711685,0.00015807351,0.0001478785,0.00066737283],"domain_scores_gemma":[0.9995284,0.000058604535,0.0000465627,0.00011879443,0.000017082957,0.00023054008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001976894,0.00010665592,0.00013322513,0.00007529651,0.000086531996,0.000040912662,0.000096592536,0.000022318707,0.0004324887],"category_scores_gemma":[0.00008172603,0.00009252835,0.0000107360365,0.00033470857,0.000015636291,0.00022453148,0.0000142061635,0.00007946524,0.000029387304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009279327,0.000017515309,0.99497575,0.000011029035,0.000003905429,0.000008377868,0.0009748188,0.00036880007,0.000017115468,0.00021293254,0.00028542642,0.0031150556],"study_design_scores_gemma":[0.00017040929,0.0000037429047,0.88818735,0.000011258541,0.000004486852,0.000002004864,0.000038697446,0.00004772235,0.00005621687,0.000023335924,0.11134939,0.00010539075],"about_ca_topic_score_codex":0.8073792,"about_ca_topic_score_gemma":0.9903798,"teacher_disagreement_score":0.18300061,"about_ca_system_score_codex":0.00003150887,"about_ca_system_score_gemma":0.00011522432,"threshold_uncertainty_score":0.47354484},"labels":[],"label_agreement":null},{"id":"W7074175630","doi":"","title":"CD4+CD25+ T regulatory cells and TGF-beta in mucosal immune system: the good and the bad.","year":2007,"lang":"en","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute of Infection and Immunity","funders":"","keywords":"Immune system; Immunity; Component (thermodynamics); T lymphocyte","score_opus":0.004512161737691059,"score_gpt":0.17182030681692356,"score_spread":0.1673081450792325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074175630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96282285,0.0034651814,0.00083416875,0.0034401738,0.00026415655,0.00038745726,0.000042911182,0.00004909432,0.028694026],"genre_scores_gemma":[0.99778134,0.00024942684,0.00055410346,0.000057906786,0.000025864367,0.0000029107696,0.000036167425,0.000005650969,0.001286607],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99691224,0.0020270692,0.00031622287,0.00026302715,0.00021920782,0.0002622605],"domain_scores_gemma":[0.997344,0.0015755354,0.00016303535,0.0006785672,0.00015629709,0.00008252122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008829436,0.00013376898,0.00020677326,0.000049506547,0.0003814808,0.00024133424,0.00043250652,0.000067130684,0.00006471084],"category_scores_gemma":[0.00009236038,0.000082616716,0.000041709056,0.0001994734,0.0003982133,0.00012295815,0.00010750017,0.00014738133,0.000022853095],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003338622,0.00027105288,0.08294067,0.00042095518,0.00018502255,0.00003483021,0.03419482,0.00016278354,0.03452949,0.69712037,0.0008677834,0.14893839],"study_design_scores_gemma":[0.0022740404,0.0000016675349,0.8837053,0.00051538664,0.00007168298,0.000036310477,0.0011116408,0.008698307,0.07662307,0.0019712108,0.024550814,0.0004405743],"about_ca_topic_score_codex":0.0066040177,"about_ca_topic_score_gemma":0.00812953,"teacher_disagreement_score":0.8007646,"about_ca_system_score_codex":0.0000051802117,"about_ca_system_score_gemma":0.000034279772,"threshold_uncertainty_score":0.9983343},"labels":[],"label_agreement":null},{"id":"W7074175948","doi":"","title":"Précisions nécessaires dans la loi du Canada sur l’aide médicale à mourir","year":2018,"lang":"fr","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Legislation; Context (archaeology); Work (physics); Public policy","score_opus":0.01342908376185001,"score_gpt":0.1790977739878969,"score_spread":0.16566869022604688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074175948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9325509,0.003316744,0.000048963124,0.0052057505,0.013026446,0.00048265647,0.0019131254,0.000084463085,0.043370932],"genre_scores_gemma":[0.9532577,0.0016570076,0.00019666781,0.00063709565,0.004061356,0.000008200715,0.00014765986,0.00003653856,0.039997812],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99534714,0.0007075682,0.0005632946,0.0006886457,0.00070373283,0.0019896273],"domain_scores_gemma":[0.9974505,0.00038675166,0.0002049145,0.00058496493,0.0001744308,0.0011984484],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007402693,0.00042784828,0.00045891516,0.00005253747,0.00048983487,0.0003627359,0.0008385755,0.000150737,0.0060297726],"category_scores_gemma":[0.0004575713,0.00037789394,0.00009929303,0.00047623907,0.00062445464,0.00039642613,0.00012621185,0.00028056256,0.00067383493],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002342948,0.00038828832,0.20015071,0.00027604244,0.00029349438,0.0024509772,0.0061282795,0.0010297706,0.0011538351,0.0033278407,0.73608196,0.0484845],"study_design_scores_gemma":[0.0002824297,0.000058613456,0.3295709,0.000055305638,0.00006425331,0.00004363041,0.000056844605,0.00018696803,0.0016407578,0.00011049612,0.667604,0.00032580647],"about_ca_topic_score_codex":0.57784736,"about_ca_topic_score_gemma":0.686309,"teacher_disagreement_score":0.12942016,"about_ca_system_score_codex":0.00004736771,"about_ca_system_score_gemma":0.0015697901,"threshold_uncertainty_score":0.9998673},"labels":[],"label_agreement":null},{"id":"W7074176511","doi":"","title":"Identification of lysophosphatidylcholine (LPC) and platelet activating factor (PAF) from PC12 cells and mouse cortex using liquid chromatography/multi-stage mass spectrometry (LC/MS(3))","year":2008,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lysophosphatidylcholine; Mass spectrometry; Platelet-activating factor; Identification (biology); Liquid chromatography–mass spectrometry; In vitro","score_opus":0.02664825137007673,"score_gpt":0.23417276248853355,"score_spread":0.20752451111845682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074176511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99701804,0.0003134219,0.0007897942,0.00001052341,0.0001992947,0.00018985345,0.0013567978,0.000031705822,0.00009058853],"genre_scores_gemma":[0.9916019,0.000327369,0.0077726296,0.000016756372,0.00009414898,7.4606135e-7,0.000099935474,0.000009536013,0.0000769817],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99874127,0.000058014575,0.00038501318,0.0003370413,0.00023316572,0.00024552573],"domain_scores_gemma":[0.9992045,0.000109744025,0.00031151008,0.00021020361,0.000043397507,0.00012063082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001340228,0.00018021799,0.0003257303,0.00011086881,0.00018415556,0.00006856327,0.00012615422,0.00008944441,0.00076226663],"category_scores_gemma":[0.000020884718,0.00016472973,0.00004204007,0.0001854598,0.00013066604,0.00031330364,0.000022083239,0.00009265951,0.00001005],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005838807,0.000022542015,0.014107088,0.000040544648,0.00004215867,0.000009239883,0.00034278087,0.000058992424,0.98491496,0.000008259708,0.000013318214,0.000381732],"study_design_scores_gemma":[0.00043976857,0.000072351206,0.20324793,0.000019781633,0.000012439467,0.0000039862475,0.00004510607,0.0043218797,0.79141515,0.000109900044,0.00012304205,0.00018863045],"about_ca_topic_score_codex":0.0015424959,"about_ca_topic_score_gemma":0.000060954488,"teacher_disagreement_score":0.19349977,"about_ca_system_score_codex":0.0000030085873,"about_ca_system_score_gemma":0.000026046751,"threshold_uncertainty_score":0.8346285},"labels":[],"label_agreement":null},{"id":"W7074181831","doi":"","title":"Streamflow hydrograph classification using functional data analysis","year":2015,"lang":"en","type":"article","venue":"LillOA (Université de Lille (University Of Lille))","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hydrograph; Streamflow; Flood myth; Functional data analysis; Representation (politics)","score_opus":0.0836193157922765,"score_gpt":0.20545719224565245,"score_spread":0.12183787645337596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074181831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98175263,0.00016113596,0.005040276,0.0002929057,0.00025732443,0.00012792538,0.0009218902,0.00006923996,0.011376679],"genre_scores_gemma":[0.99161756,0.000079710815,0.005128906,0.000027096035,0.000074401454,1.8769889e-8,0.0016875203,0.000005156426,0.0013796389],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985109,0.00012531878,0.00013320275,0.0004953352,0.00041541804,0.00031984734],"domain_scores_gemma":[0.99851876,0.00006366133,0.0002441608,0.00071859115,0.000133812,0.00032099537],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035710813,0.00016970282,0.00035536403,0.00044206693,0.0004413227,0.000029944007,0.0007595695,0.00014505771,0.0026151529],"category_scores_gemma":[0.000014857694,0.0002042721,0.00016738963,0.0011861172,0.00018404247,0.00074495893,0.00022530243,0.00009701998,0.000104893414],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002068717,0.00044441095,0.8153541,0.00014527085,0.0059347237,0.00039931337,0.009003155,0.103786096,0.010365297,0.0040029343,0.02793152,0.020564478],"study_design_scores_gemma":[0.0020103958,0.00020767667,0.60622686,0.000023847415,0.002531891,0.000022593113,0.012791358,0.32253194,0.000114330796,0.0005084908,0.052315373,0.00071526057],"about_ca_topic_score_codex":0.014417685,"about_ca_topic_score_gemma":0.006998611,"teacher_disagreement_score":0.21874584,"about_ca_system_score_codex":0.000044172342,"about_ca_system_score_gemma":0.00014605312,"threshold_uncertainty_score":0.9982966},"labels":[],"label_agreement":null},{"id":"W7074185819","doi":"","title":"Autism spectrum disorders are associated with fetal growth extremely below or above average for gestational age","year":2013,"lang":"en","type":"article","venue":"UWA Profiles and Research Repository (University of Western Australia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centre for Global Health Research","funders":"","keywords":"Autism; Fetal growth; Fetus; Gestational age; Small for gestational age; Pregnancy","score_opus":0.04177060981827367,"score_gpt":0.24922480916147993,"score_spread":0.20745419934320625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074185819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99759614,0.000026493673,0.00008170183,0.00093742623,0.00009808038,0.0006292117,0.00029968563,0.000022316768,0.00030891848],"genre_scores_gemma":[0.9800611,0.000038144968,0.00034826386,0.0000050677727,0.00004861833,0.0000015617761,0.00014738197,0.000005598044,0.019344239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99860775,0.00014425795,0.00012247992,0.00030796963,0.00042692886,0.00039063056],"domain_scores_gemma":[0.99928176,0.00019383765,0.00013959223,0.00012531034,0.000094580835,0.00016491907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025347873,0.00012963302,0.00022944178,0.00008984952,0.00052631163,0.00013923412,0.00022496404,0.00009948651,0.00042440253],"category_scores_gemma":[0.000015126312,0.00010512056,0.000049432587,0.00014025836,0.0003701204,0.0004242022,0.000036432477,0.00014715923,0.000024003488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001092987,0.00028398848,0.98108065,0.00075261295,0.00052174786,0.00046309587,0.0024042123,0.00025080977,0.0059168045,0.0018138743,0.004233492,0.0011857148],"study_design_scores_gemma":[0.000702561,0.00051606435,0.99494755,0.000098729215,0.000024280023,0.000007264686,0.00057896995,0.0003892276,0.00080142944,0.0014047805,0.00035761658,0.00017150758],"about_ca_topic_score_codex":0.012449537,"about_ca_topic_score_gemma":0.002746635,"teacher_disagreement_score":0.01903532,"about_ca_system_score_codex":0.000009345585,"about_ca_system_score_gemma":0.00006816706,"threshold_uncertainty_score":0.9941266},"labels":[],"label_agreement":null},{"id":"W7074187200","doi":"","title":"CGM accuracy: Contrasting CE marking with the governmental controls of the USA (FDA) and Australia (TGA) - A narrative review.","year":2022,"lang":"en","type":"article","venue":"UWA Profiles and Research Repository (University of Western Australia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centre for Global Health Research","funders":"","keywords":"Food and drug administration; Excellence; Continuous glucose monitoring; Process (computing); Conformity; Narrative review; Protocol (science); Comparability","score_opus":0.04585959455772375,"score_gpt":0.2812045155005037,"score_spread":0.23534492094277992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074187200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99758464,0.0003732987,0.0000028839197,0.00081768306,0.000083622705,0.00060651,0.00019269179,0.0000040418636,0.00033460552],"genre_scores_gemma":[0.995285,0.00014111708,0.000030274794,0.000018770172,0.000036728514,0.0000013334924,0.000008069214,0.0000026393193,0.004476119],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980712,0.0005937903,0.00014092619,0.0002413256,0.0006953719,0.00025738234],"domain_scores_gemma":[0.99910367,0.0002848577,0.00025317777,0.00020037139,0.00008061456,0.00007730254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083671923,0.000107519256,0.0002487169,0.000024910763,0.0011517719,0.00005612836,0.00037944308,0.00003308955,0.00030877997],"category_scores_gemma":[0.000019027617,0.00006892985,0.00004792302,0.00015598795,0.00066731597,0.00018493891,0.0001878507,0.00028529167,0.0000016051619],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063998415,0.00006193523,0.93354857,0.0009485941,0.00026199795,0.00010274823,0.004628181,0.00010009124,0.055249862,0.00034134515,0.0034891975,0.00062749686],"study_design_scores_gemma":[0.0006443023,0.00049603987,0.9771379,0.00040349018,0.00008163974,0.00007029216,0.013269477,0.000096615935,0.0036558104,0.000027956443,0.003963602,0.00015282641],"about_ca_topic_score_codex":0.010339874,"about_ca_topic_score_gemma":0.000564167,"teacher_disagreement_score":0.051594052,"about_ca_system_score_codex":0.000013079959,"about_ca_system_score_gemma":0.000055167508,"threshold_uncertainty_score":0.99625033},"labels":[],"label_agreement":null},{"id":"W7074188203","doi":"","title":"Hippocampal volume in early onset depression","year":2004,"lang":"en","type":"article","venue":"NPARC","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"","score_opus":0.007824887359332471,"score_gpt":0.1985304354063724,"score_spread":0.19070554804703993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074188203","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98742825,0.00003250261,0.00003117023,0.00010653969,0.00032338718,0.00008131165,0.000057600362,0.000025275485,0.011913969],"genre_scores_gemma":[0.99884075,0.000008942499,0.0007472666,0.000078422585,0.00010156139,0.0000011269977,0.00004762517,0.0000023569178,0.00017193829],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99932426,0.000033721728,0.000120022996,0.00016120679,0.00014221924,0.00021854883],"domain_scores_gemma":[0.9997385,0.000017178187,0.000029111703,0.00013333457,0.000009979668,0.00007189374],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00013470894,0.00007583353,0.00011317668,0.00003848141,0.00005113442,0.000046856512,0.00013309179,0.000048466805,0.0021124966],"category_scores_gemma":[0.000010124939,0.000062043764,0.000022882032,0.00009047499,0.00002675702,0.0001303904,0.000010077153,0.00006574976,0.0010788627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006239492,0.000033460252,0.97909117,0.000015794041,0.000006171823,0.00006322284,0.0004925348,0.002000439,0.004288319,0.0001591023,0.0008541144,0.012933281],"study_design_scores_gemma":[0.0003412487,0.000052129646,0.9679325,0.000024991314,0.0000032650794,0.0000034172313,0.000009395482,0.00010880387,0.0014538575,0.027590005,0.0023724746,0.000107894906],"about_ca_topic_score_codex":0.0029639653,"about_ca_topic_score_gemma":0.00093611935,"teacher_disagreement_score":0.027430903,"about_ca_system_score_codex":0.0000023226846,"about_ca_system_score_gemma":0.00003167799,"threshold_uncertainty_score":0.99969894},"labels":[],"label_agreement":null},{"id":"W7074190829","doi":"","title":"La diversidad como problema","year":2001,"lang":"es","type":"article","venue":"RECERCAT (Consorci de Serveis Universitaris de Catalunya)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Diversity (politics); Cultural diversity; Ideology; Representation (politics)","score_opus":0.011379315462543109,"score_gpt":0.2117854804689742,"score_spread":0.20040616500643108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074190829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9360178,0.0015457816,0.00010923409,0.0018389036,0.00059001276,0.0004922844,0.0015823281,0.00018044478,0.057643194],"genre_scores_gemma":[0.986768,0.0053193523,0.0005890848,0.00029529174,0.00031214737,0.0000020768846,0.00072537165,0.000034380362,0.005954267],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99625003,0.00074377534,0.000421464,0.00082361395,0.00046339433,0.0012977142],"domain_scores_gemma":[0.99762386,0.0004251419,0.00029146142,0.0007489614,0.00017488869,0.0007356805],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009935251,0.0005803957,0.0006907989,0.0004053856,0.0007036786,0.00050691376,0.0011639621,0.0006348103,0.0058668493],"category_scores_gemma":[0.00006258676,0.0006271321,0.0003047378,0.00093157386,0.00040512058,0.0008754037,0.00025483928,0.00056570786,0.0016552256],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011183225,0.00052319095,0.90494287,0.0011002911,0.0012584404,0.0037965889,0.005203703,0.005557097,0.003639812,0.010078534,0.039105155,0.02367598],"study_design_scores_gemma":[0.0017057828,0.0003726711,0.24898294,0.00035516935,0.0006841136,0.00037246844,0.0020658295,0.0014384995,0.0013282651,0.0010847591,0.7403678,0.0012416791],"about_ca_topic_score_codex":0.018416299,"about_ca_topic_score_gemma":0.0011873613,"teacher_disagreement_score":0.70126265,"about_ca_system_score_codex":0.00018029514,"about_ca_system_score_gemma":0.00055608596,"threshold_uncertainty_score":0.999618},"labels":[],"label_agreement":null},{"id":"W7074191962","doi":"","title":"The Psychophysical Assessment of Hierarchical Magno-, Parvo- and Konio-Cellular Visual Stream Dysregulations in Migraineurs","year":2019,"lang":"en","type":"other","venue":"Dove Medical Press (Taylor and Francis Group)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Parvocellular cell; Migraine; Contrast (vision); Visual system; Aura; Visual processing; Pupillometry; Achromatic lens; Illusion","score_opus":0.006505719778478763,"score_gpt":0.24590424141758957,"score_spread":0.2393985216391108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074191962","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14922042,0.04763361,0.05725455,0.004907498,0.015037399,0.00894247,0.007393315,0.0004941587,0.7091166],"genre_scores_gemma":[0.9977207,0.00012863983,0.00012873649,0.00009390319,0.00063518033,0.000014816605,0.00027699076,0.000045411347,0.000955616],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9976738,0.00023798231,0.00045073222,0.00050872704,0.0007347785,0.00039395352],"domain_scores_gemma":[0.99861825,0.00057005545,0.0001833879,0.00033333024,0.000018812603,0.00027618944],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046081468,0.00030828867,0.0006395247,0.000085427564,0.00008934991,0.000087857545,0.00032793236,0.00034761708,0.0014559651],"category_scores_gemma":[0.00006225554,0.0002021254,0.00008804783,0.00011013616,0.0005755634,0.000057227906,0.00007007999,0.00042726396,0.000015810378],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024359643,0.00054643233,0.029673237,0.00087307754,0.00035119336,0.00008681066,0.00031550668,0.00006394575,0.00036802923,0.0117508285,0.005700965,0.9500264],"study_design_scores_gemma":[0.006117994,0.0012148303,0.25837225,0.00014412048,0.00034730425,0.000016774507,0.00013275554,0.5168597,0.000050319784,0.006396715,0.20872752,0.0016196737],"about_ca_topic_score_codex":0.0032368489,"about_ca_topic_score_gemma":0.0014536992,"teacher_disagreement_score":0.9484067,"about_ca_system_score_codex":0.0000021497985,"about_ca_system_score_gemma":0.0000063809425,"threshold_uncertainty_score":0.9994568},"labels":[],"label_agreement":null},{"id":"W7074192286","doi":"","title":"La création de revenu et ses répercussions sur le capital universitaire, les valeurs de l'université et l'autonomie des établissements : éclairages canadiens","year":2007,"lang":"fr","type":"other","venue":"Cairn.info","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Capital (architecture); Context (archaeology); Inequality; Consumption (sociology); Production (economics)","score_opus":0.015457601780095056,"score_gpt":0.20782086366649002,"score_spread":0.19236326188639497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074192286","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7161611,0.0009526394,0.00031350655,0.000808273,0.00054714817,0.00025278056,0.0018261931,0.00006900551,0.27906936],"genre_scores_gemma":[0.6101173,0.0018098117,0.0013005475,0.00025200236,0.00022760125,0.000001627788,0.0006753533,0.0000523184,0.38556343],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99794984,0.00039739162,0.00026304912,0.00042636003,0.00022991703,0.000733423],"domain_scores_gemma":[0.9986373,0.00029810957,0.00023714938,0.00029872605,0.00009576655,0.00043295455],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006584496,0.0004046871,0.00040971185,0.00032052433,0.0005361201,0.00018092143,0.0004642763,0.0004380475,0.015233109],"category_scores_gemma":[0.000089888235,0.00041524097,0.00014837102,0.0002270944,0.00031880024,0.0005291179,0.00008163907,0.0002893132,0.00030291948],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028084312,0.0005090669,0.33236384,0.0014651284,0.0014247033,0.0028169553,0.09152086,0.022228403,0.004867331,0.07163084,0.38736212,0.0835299],"study_design_scores_gemma":[0.00048440654,0.00013147025,0.28358024,0.0003508153,0.00021813205,0.000039419476,0.0026307965,0.0001542507,0.0002944935,0.0003810731,0.71120477,0.00053011597],"about_ca_topic_score_codex":0.47284067,"about_ca_topic_score_gemma":0.4554441,"teacher_disagreement_score":0.32384264,"about_ca_system_score_codex":0.00040373552,"about_ca_system_score_gemma":0.001380452,"threshold_uncertainty_score":0.99982995},"labels":[],"label_agreement":null},{"id":"W7074203597","doi":"","title":"Another Canadian in Japan during the bombing","year":2013,"lang":"en","type":"article","venue":"Europe PMC (PubMed Central)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Terrorism; Work (physics); Feature (linguistics)","score_opus":0.008050684581048958,"score_gpt":0.1596415741323965,"score_spread":0.15159088955134753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074203597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98411745,0.00010508751,3.7730308e-7,0.0007778273,0.0006727362,0.00034726533,0.000030968426,0.000022953485,0.0139253335],"genre_scores_gemma":[0.99753404,0.000041659812,0.000016456657,0.00037397537,0.00022556708,0.0000075998414,0.000011751595,0.000007891969,0.0017810753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99850476,0.000100270365,0.00015946341,0.00019634099,0.0001293557,0.0009097929],"domain_scores_gemma":[0.99946105,0.000026540663,0.000038549424,0.00021371107,0.000017036451,0.00024313704],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000197252,0.00011487192,0.00011310002,0.000053375057,0.00013527824,0.00019237495,0.00028938372,0.000030074905,0.003526891],"category_scores_gemma":[0.000032090975,0.00007698761,0.000024264033,0.00019979134,0.00003756978,0.0001945343,0.000012253935,0.000103902996,0.0010546716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008489189,0.0000106909165,0.9820607,0.00001858869,0.000018064527,0.000036327623,0.0027550154,0.00059255736,0.001199406,0.0001237756,0.0021990016,0.010977415],"study_design_scores_gemma":[0.00013038429,0.000005513304,0.9546371,0.0000075082535,0.000002983312,0.000002749251,0.000040813527,0.000054448235,0.00045578266,0.0000742625,0.044478666,0.000109762026],"about_ca_topic_score_codex":0.3406793,"about_ca_topic_score_gemma":0.19521715,"teacher_disagreement_score":0.14546213,"about_ca_system_score_codex":0.000009724213,"about_ca_system_score_gemma":0.000057526744,"threshold_uncertainty_score":0.99972314},"labels":[],"label_agreement":null},{"id":"W7074203788","doi":"","title":"COVID-19 Policy Response and the Rise of the Sub-National Governments","year":2021,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Politics; Context (archaeology); Latin Americans; Diplomacy; Public policy","score_opus":0.015430124520421501,"score_gpt":0.2201266767836682,"score_spread":0.2046965522632467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074203788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8967994,0.000009476207,0.000024714,0.0029574283,0.0001831354,0.00028974455,0.00071172643,0.0000187771,0.099005625],"genre_scores_gemma":[0.9921476,0.007140448,0.000043994238,0.00046695617,0.00006216672,2.3620416e-7,0.000011559265,0.0000024231488,0.00012461188],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99872035,0.0005527461,0.000095474184,0.0001752662,0.00031264237,0.00014355154],"domain_scores_gemma":[0.9991907,0.00037134148,0.000099852,0.00019649095,0.000066496075,0.000075132244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042290354,0.00008872233,0.0001307772,0.00048230443,0.00023598688,0.00003913344,0.00025951277,0.00004064951,0.0001395151],"category_scores_gemma":[0.000514818,0.00005685764,0.00006410128,0.0019326505,0.00022624012,0.00012872783,0.00009927171,0.00006540152,0.0000086245545],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.06269556,0.0016002161,0.32520685,0.0017416347,0.003514981,0.0017174042,0.108228676,0.01223215,0.009428199,0.392022,0.023220848,0.058391448],"study_design_scores_gemma":[0.001213131,0.000023504343,0.02171754,0.000007646248,0.000035586192,0.000008471145,0.00021567676,0.00017207213,0.0009958193,0.000051808114,0.9754758,0.00008294195],"about_ca_topic_score_codex":0.07567596,"about_ca_topic_score_gemma":0.012632789,"teacher_disagreement_score":0.95225495,"about_ca_system_score_codex":0.000027236007,"about_ca_system_score_gemma":0.0015123524,"threshold_uncertainty_score":0.93047917},"labels":[],"label_agreement":null},{"id":"W7074211256","doi":"","title":"Role of Belinda in H. Purcell’s Dido &amp; Aeneas","year":2009,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University","keywords":"Opera; DIDO; Criticism; Degree (music)","score_opus":0.005292149643239631,"score_gpt":0.15304547843832025,"score_spread":0.14775332879508063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074211256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99465287,0.00023613655,0.000010987351,0.00003551328,0.00007802022,0.00010706696,0.00029841455,0.000015789054,0.0045652296],"genre_scores_gemma":[0.9991352,0.000090637994,0.0002982198,0.000021284448,0.000025257963,2.0023888e-8,0.000065096,0.0000016937984,0.00036259947],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9992727,0.000041903815,0.000121044366,0.00020172563,0.00017508384,0.00018756729],"domain_scores_gemma":[0.9995861,0.000022655491,0.000097395045,0.00016679024,0.000052730895,0.000074336334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014761683,0.00003305942,0.00023641712,0.000035215206,0.000060536797,0.000038228492,0.00025491227,0.00006914178,0.00087310205],"category_scores_gemma":[0.000008972244,0.00010381532,0.00006115058,0.0001808009,0.00008877086,0.00018904243,0.000017099415,0.000058161335,0.000056778663],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032384778,0.0001245788,0.13396338,0.00004365268,0.000018982619,0.000048217684,0.00049993163,0.0003992172,0.0056972904,0.000004845324,0.0010026592,0.85816485],"study_design_scores_gemma":[0.00038292803,0.00007035073,0.9952907,0.000049284707,0.000011645098,0.00000489778,0.0001893357,0.00009333676,0.000009660971,0.001620443,0.0021703134,0.000107113265],"about_ca_topic_score_codex":0.35403165,"about_ca_topic_score_gemma":0.6177032,"teacher_disagreement_score":0.8613273,"about_ca_system_score_codex":0.0000030298927,"about_ca_system_score_gemma":0.000037460013,"threshold_uncertainty_score":0.95598555},"labels":[],"label_agreement":null},{"id":"W7074215229","doi":"","title":"Beta-cell replacement strategies for diabetes","year":2018,"lang":"en","type":"article","venue":"Institutional Repositories DataBase (IRDB)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Embryonic stem cell; Induced pluripotent stem cell; Progenitor cell; Stem cell; Diabetes mellitus; Transplantation; Regenerative medicine; Insulin","score_opus":0.015996156982488324,"score_gpt":0.23523871543791283,"score_spread":0.2192425584554245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074215229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9584034,0.00035063017,0.0027718956,0.00022299973,0.007795505,0.0005319574,0.0051070037,0.00012306147,0.024693545],"genre_scores_gemma":[0.99019206,0.00001348764,0.0039443723,0.00017102875,0.002750012,0.000020600495,0.0024257572,0.0000052232444,0.0004774418],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99853086,0.000037788817,0.00031517202,0.00039887318,0.0003603917,0.00035689046],"domain_scores_gemma":[0.99902934,0.00012606221,0.00012370116,0.00038371937,0.0002125892,0.00012457078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029435608,0.00018834663,0.00020329641,0.00004600894,0.00072358607,0.0003243713,0.00025349407,0.00004999616,0.00051944476],"category_scores_gemma":[0.000049344388,0.0001560994,0.00006487778,0.00011603132,0.0003442945,0.0008733234,0.00004025965,0.00006153733,0.00021849947],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024069753,0.00078106346,0.14397606,0.0016558105,0.000813802,0.00017485383,0.0013287156,0.0037783883,0.2032323,0.43155628,0.2064782,0.0038175448],"study_design_scores_gemma":[0.00081280834,0.00066656736,0.012199666,0.000092555136,0.00009789256,0.000013228755,0.0001385857,0.00084882573,0.102003224,0.0032530858,0.87934345,0.0005300819],"about_ca_topic_score_codex":0.0010471953,"about_ca_topic_score_gemma":0.00047904594,"teacher_disagreement_score":0.6728653,"about_ca_system_score_codex":0.0000098983965,"about_ca_system_score_gemma":0.0003529619,"threshold_uncertainty_score":0.6365549},"labels":[],"label_agreement":null},{"id":"W7074221496","doi":"","title":"Nicotine metabolism in the cabbage looper Trichoplusia ni (Hübner) - a toxicogenomic approach","year":2021,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"University of British Columbia","keywords":"Cabbage looper; Trichoplusia; Detoxification (alternative medicine); Xenobiotic; Cytochrome P450; Nicotine; Glutathione; Enzyme; Insect","score_opus":0.007821990487840848,"score_gpt":0.155140866915393,"score_spread":0.14731887642755215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074221496","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915076,0.0007820978,0.000042285665,0.00007300485,0.00020640483,0.00017178504,0.00043513675,0.000017012328,0.0067646964],"genre_scores_gemma":[0.998099,0.00022770611,0.00039567146,0.00008530883,0.00007286283,1.9104867e-7,0.00016032382,0.0000038241155,0.0009551061],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99886006,0.00018977543,0.00012986705,0.00033090558,0.00022903734,0.00026034817],"domain_scores_gemma":[0.9994605,0.00004602535,0.000079061974,0.00028021075,0.00006557723,0.00006857838],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00033376052,0.000049681203,0.00028670946,0.000030072682,0.00018153717,0.00017500966,0.0004275352,0.000075804506,0.0010289657],"category_scores_gemma":[0.000017633914,0.00011585103,0.00008847453,0.00041413735,0.0001121865,0.00023555555,0.00005021896,0.000115069925,0.000067360554],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010336166,0.001082331,0.15305465,0.00040869624,0.0003310387,0.0017914085,0.0058673453,0.0020313642,0.011788225,0.00006999201,0.02018412,0.80328745],"study_design_scores_gemma":[0.00064755016,0.000018646086,0.99434114,0.000015749834,0.000043377968,0.000060000686,0.0011322225,0.00025457487,0.0000065748272,0.00016361216,0.0031709592,0.00014560841],"about_ca_topic_score_codex":0.29713914,"about_ca_topic_score_gemma":0.465257,"teacher_disagreement_score":0.8412865,"about_ca_system_score_codex":0.0000044802077,"about_ca_system_score_gemma":0.000095909716,"threshold_uncertainty_score":0.99988425},"labels":[],"label_agreement":null},{"id":"W7074238820","doi":"","title":"Concurrent Bering Sea and Labrador Sea ice melt extremes in March 2023: A confluence of meteorological events aligned with stratosphere-troposphere interactions","year":2024,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sea ice; Arctic ice pack; Drift ice; Antarctic sea ice; Arctic; Lead (geology); Arctic sea ice decline; Cryosphere","score_opus":0.023424357263113847,"score_gpt":0.2548088227809404,"score_spread":0.23138446551782657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074238820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8556937,0.002280378,0.0000037748728,0.00009937587,0.00017562057,0.00033957098,0.13992155,0.00004605492,0.0014400067],"genre_scores_gemma":[0.9924435,0.000019353869,0.00009948805,0.0000218817,0.000045663008,0.000014492559,0.007227922,0.0000043772616,0.00012333208],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.999095,0.000068850466,0.00018640132,0.00027148455,0.00017328301,0.00020493627],"domain_scores_gemma":[0.9995274,0.00019611762,0.00005142406,0.00010251481,0.000043201755,0.00007934326],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000059432245,0.00013268951,0.00020635246,0.000024134677,0.000042189044,0.00008061213,0.00012476499,0.000046767032,0.104510255],"category_scores_gemma":[0.000044298966,0.00009626712,0.000028152079,0.00017474675,0.000019428155,0.00022551279,0.00003236633,0.000095204465,0.00020667285],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014910497,0.00085055665,0.23772147,0.020437673,0.0021629706,0.0032419064,0.0053050653,0.014181688,0.0344801,0.0015648479,0.18852557,0.4900371],"study_design_scores_gemma":[0.0011825921,0.0010218683,0.86694556,0.0077451384,0.00011207475,0.00008394024,0.00060781406,0.020273272,0.0063516814,0.00047103202,0.09423561,0.0009694482],"about_ca_topic_score_codex":0.001511528,"about_ca_topic_score_gemma":0.003908384,"teacher_disagreement_score":0.62922406,"about_ca_system_score_codex":0.0000034191671,"about_ca_system_score_gemma":0.000060872837,"threshold_uncertainty_score":0.89630836},"labels":[],"label_agreement":null},{"id":"W7074244437","doi":"","title":"Intertwined Histories: Plants in Their Social Contexts","year":2019,"lang":"en","type":"book","venue":"Libraries and Cultural Resources (University of Calgary)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Creatures; Interdependence; Social life; Atmosphere (unit); Plant life; Globe","score_opus":0.008693502325768014,"score_gpt":0.1560509648131101,"score_spread":0.14735746248734208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074244437","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42041668,0.0035576862,0.000009237298,0.00032859447,0.0005989561,0.00037005811,0.00061802194,0.00005664877,0.5740441],"genre_scores_gemma":[0.15084532,0.00044099404,0.00010238835,0.00010922985,0.00021851208,9.357927e-8,0.0010494329,0.000010520474,0.8472235],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991254,0.000052156753,0.00015854553,0.00027705342,0.00017126276,0.00021556196],"domain_scores_gemma":[0.9995059,0.00008438451,0.00019744184,0.000111502835,0.000025598638,0.000075172036],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000054775024,0.000224674,0.0005500604,0.00007563333,0.0001759657,0.00007813546,0.00033348412,0.00026074503,0.0014429962],"category_scores_gemma":[0.000004551164,0.00018620618,0.00010288527,0.00004715742,0.00033497898,0.0004154365,0.00008466316,0.00018311953,0.000028785316],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0059814695,0.00011295309,0.013318361,0.002769115,0.0011620483,0.0005039234,0.26329553,0.00002805867,0.00041961198,0.049076892,0.47934103,0.18399103],"study_design_scores_gemma":[0.0005219538,0.000121554855,0.018087415,0.00012717392,0.000030295134,0.0000022162315,0.0019235315,0.00008938613,0.000006997437,0.0017740153,0.9770131,0.0003023678],"about_ca_topic_score_codex":0.0020257083,"about_ca_topic_score_gemma":0.0011183388,"teacher_disagreement_score":0.49767208,"about_ca_system_score_codex":0.000007881712,"about_ca_system_score_gemma":0.00007444755,"threshold_uncertainty_score":0.9994698},"labels":[],"label_agreement":null},{"id":"W7074245304","doi":"","title":"Composition and cytotoxic activity of the leaf essential oil of Comptonia peregrina (L.) Coulter","year":2007,"lang":"en","type":"other","venue":"Constellation (Université du Québec à Chicoutimi)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Essential oil; Cytotoxic T cell; Chemical composition; Fraction (chemistry); Composition (language); Cell culture; Human lung","score_opus":0.00639133859438158,"score_gpt":0.17835782425000818,"score_spread":0.1719664856556266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074245304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5703124,0.00031252505,0.00013339013,0.00012712427,0.00041991874,0.00017321276,0.00042831688,0.000033087686,0.42806005],"genre_scores_gemma":[0.9852034,0.00010584611,0.00005013069,0.000017525073,0.00010199402,5.314981e-8,0.00006127092,0.000017228404,0.014442561],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9991812,0.000086257416,0.00015739787,0.00021166721,0.0002331659,0.00013027992],"domain_scores_gemma":[0.9991429,0.00009665821,0.0004305718,0.000226186,0.000050808958,0.000052885956],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011113722,0.00017424593,0.0003366683,0.00014755245,0.00011624929,0.000017105422,0.00018076863,0.00017621557,0.030054983],"category_scores_gemma":[0.000002926834,0.00014249489,0.000086770706,0.00013125682,0.0004356262,0.00006861708,0.00004109376,0.00010592234,0.000014913286],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00210362,0.0007313435,0.3442413,0.0047050905,0.0024116985,0.00006188142,0.0072199716,0.0062568127,0.16767901,0.0038524878,0.34455743,0.11617936],"study_design_scores_gemma":[0.0037891413,0.00022657473,0.798882,0.001275895,0.0011385741,0.00006768454,0.00037132122,0.0070419484,0.02087596,0.00005297599,0.16475089,0.0015269961],"about_ca_topic_score_codex":0.018176429,"about_ca_topic_score_gemma":0.007591361,"teacher_disagreement_score":0.45464075,"about_ca_system_score_codex":0.00000800067,"about_ca_system_score_gemma":0.0001549727,"threshold_uncertainty_score":0.9883616},"labels":[],"label_agreement":null},{"id":"W7074246654","doi":"","title":"From Arm's Length to Hands-On: The Formative Years of Ontario's Public Service, 1867-1940","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Formative assessment; Curriculum; Work (physics)","score_opus":0.03163106961671409,"score_gpt":0.2011593533155252,"score_spread":0.16952828369881112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074246654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87925494,2.2636057e-7,0.000007778315,0.00052524917,0.00028004273,0.00032910908,0.00042025422,0.00007532902,0.11910707],"genre_scores_gemma":[0.9985056,0.00069704006,0.00007734473,0.00032282865,0.000095418705,8.9497405e-7,0.00019446024,0.000005883719,0.000100519384],"study_design_codex":"qualitative","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988984,0.000110243665,0.00014021629,0.00025981458,0.0002716475,0.0003196677],"domain_scores_gemma":[0.9991681,0.00021904288,0.000100705656,0.00033475796,0.00008212213,0.00009529814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019579763,0.00014899147,0.00022159645,0.0020436218,0.00017266543,0.00008280521,0.00055833993,0.000066053515,0.0008693116],"category_scores_gemma":[0.000027425114,0.0001211382,0.00007002195,0.004695005,0.000043193293,0.00035321983,0.00010539441,0.00012892953,0.00068311696],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029236772,0.0008846821,0.044498764,0.00034494544,0.0023966916,0.0009753339,0.61204547,0.0055687595,0.00031257045,0.017538581,0.0371036,0.27540693],"study_design_scores_gemma":[0.0004343809,0.00029473644,0.021832211,0.000029036924,0.00003152754,4.574183e-7,0.00093702576,0.00016217656,0.00036325006,0.000025710384,0.9757161,0.00017335238],"about_ca_topic_score_codex":0.7156781,"about_ca_topic_score_gemma":0.60492975,"teacher_disagreement_score":0.9386125,"about_ca_system_score_codex":0.000024197547,"about_ca_system_score_gemma":0.0003817921,"threshold_uncertainty_score":0.9518353},"labels":[],"label_agreement":null},{"id":"W7074251543","doi":"","title":"Food insecurity during the COVID-19 pandemic who use drugs in Vancouver, Canada","year":2023,"lang":"en","type":"other","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pandemic; Food insecurity; Coronavirus disease 2019 (COVID-19); Food security; Population; Poverty","score_opus":0.018756644804665774,"score_gpt":0.21010558692757816,"score_spread":0.1913489421229124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074251543","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6487998,0.0014106216,0.000007665511,0.00051674666,0.019315097,0.002105325,0.0116136605,0.001370144,0.31486097],"genre_scores_gemma":[0.38510507,0.0006945859,0.000013185068,0.0010393683,0.00053409836,0.000007470345,0.000104281,0.00012098511,0.6123809],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99873346,0.00010573916,0.0002013113,0.0003107105,0.00030221697,0.0003465668],"domain_scores_gemma":[0.99916613,0.00025142435,0.00011107,0.00031173122,0.0000076687,0.0001519728],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020839661,0.00021472955,0.00030637166,0.00007818036,0.000095398915,0.00007327045,0.00033818712,0.00014032774,0.006892264],"category_scores_gemma":[0.000062239014,0.00013916295,0.000037458674,0.00018236958,0.000042483975,0.00006641841,0.000034487897,0.00017076296,0.00008016068],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016277183,0.00000407102,0.10316835,0.00012531354,0.000047091726,0.000029042088,0.00023402451,0.00024487555,0.0000015900772,0.000052529256,0.89593786,0.00013898412],"study_design_scores_gemma":[0.0002313814,0.000015816959,0.040167205,0.000032417818,0.000010210115,0.0000012416152,0.00008362113,0.0000220042,0.0000026975677,0.00017313816,0.95901334,0.00024693293],"about_ca_topic_score_codex":0.9930224,"about_ca_topic_score_gemma":0.99987036,"teacher_disagreement_score":0.29751998,"about_ca_system_score_codex":0.000024453862,"about_ca_system_score_gemma":0.00052318955,"threshold_uncertainty_score":0.9940156},"labels":[],"label_agreement":null},{"id":"W7074255864","doi":"","title":"Waiting Time for Radiation Therapy in Breast Cancer Patients in Quebec from 1992 to 1998: A study of surgically treated breast cancer patients in Quebec documents and helps to explain increased waiting times for radiation therapy.","year":2006,"lang":"en","type":"article","venue":"PubMed Central","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Radiation therapy; Breast cancer; Confidence interval; Chemotherapy; Breast-conserving surgery; Cancer; Systemic therapy; Retrospective cohort study; Mastectomy; Cancer registry","score_opus":0.0057827884757929065,"score_gpt":0.20191766877434827,"score_spread":0.19613488029855536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074255864","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918026,0.00008322411,0.0000011860393,0.00014758835,0.00017701351,0.0035675052,0.004197766,0.000014245152,0.000008917688],"genre_scores_gemma":[0.9974314,0.000059522936,0.000015825719,0.000087622255,0.0001954338,0.0005241307,0.0016367874,0.000014154769,0.00003509864],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99771905,0.00019596587,0.0005879223,0.00043166327,0.00026172667,0.00080368744],"domain_scores_gemma":[0.9992642,0.00018808048,0.00022059087,0.000096689175,0.00005074489,0.00017972103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035984124,0.00023588409,0.00042111397,0.0001996511,0.000070615235,0.000116560426,0.00013416036,0.00007697923,0.00009117236],"category_scores_gemma":[0.000020858173,0.0002065367,0.000040547788,0.00029646364,0.00001395732,0.0003871589,0.000012267464,0.00005115307,0.0000015115548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015207271,0.00043339605,0.862802,0.000011568629,0.000029640249,8.493859e-7,0.0016120578,0.0024949783,0.00019008978,0.0000014641108,0.00008534954,0.13081785],"study_design_scores_gemma":[0.007536403,0.00014984906,0.98848253,0.000053238153,0.000011608348,5.9724584e-8,0.00007388319,0.002942404,0.00032809481,0.000020647065,0.00017132482,0.00022992323],"about_ca_topic_score_codex":0.94688326,"about_ca_topic_score_gemma":0.77665347,"teacher_disagreement_score":0.17022978,"about_ca_system_score_codex":0.00013569393,"about_ca_system_score_gemma":0.000091427246,"threshold_uncertainty_score":0.8422322},"labels":[],"label_agreement":null},{"id":"W7074256559","doi":"","title":"Physicians' tacit and stated policies for determining patient benefit and referral to cardiac rehabilitation.","year":2013,"lang":"en","type":"article","venue":"Digital Commons - University of South Florida (University of South Florida)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Referral; Rehabilitation; Clinical judgment; Patient referral; Tacit knowledge","score_opus":0.010353855226630904,"score_gpt":0.1696583502564146,"score_spread":0.1593044950297837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074256559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932906,0.000029755423,0.0003015046,0.00019372962,0.00018395737,0.00050102914,0.0045081396,0.000039214654,0.0009520386],"genre_scores_gemma":[0.9979044,0.0000062963977,0.0016747421,0.000016729513,0.000036115598,1.3307064e-7,0.00016225946,0.0000067794444,0.0001925319],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989159,0.000030204903,0.00015777878,0.00034658684,0.00023543424,0.00031406354],"domain_scores_gemma":[0.9989296,0.000187128,0.0001965707,0.00023866525,0.0002311557,0.0002168877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000085361935,0.0001987533,0.00045996162,0.00019651826,0.0004040651,0.00008123658,0.0002553552,0.00008507186,0.000066805085],"category_scores_gemma":[0.000028586452,0.00024453492,0.00012458743,0.00023116333,0.00036134577,0.00087583996,0.0001432108,0.000078074336,0.00002514249],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015979488,0.00010913495,0.6881887,0.000660403,0.0006769833,0.000018377496,0.24741665,0.0026229525,0.0011974896,0.0019910876,0.0024586394,0.05306167],"study_design_scores_gemma":[0.0013042284,0.0013490928,0.8612266,0.00014141013,0.0001782515,9.613726e-7,0.12753285,0.0009861662,0.00009657217,0.00092951715,0.0056276573,0.0006266524],"about_ca_topic_score_codex":0.002973098,"about_ca_topic_score_gemma":0.00032194747,"teacher_disagreement_score":0.17303798,"about_ca_system_score_codex":0.000009766554,"about_ca_system_score_gemma":0.00003142873,"threshold_uncertainty_score":0.99718446},"labels":[],"label_agreement":null},{"id":"W7074547525","doi":"","title":"Ontario's Cattle Kingdom: Purebred Breeders and Their World, 1870-1920","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Purebred; Beef cattle; Livestock; Dairy cattle; Animal breeding","score_opus":0.02303222034880904,"score_gpt":0.19924006087641932,"score_spread":0.1762078405276103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074547525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78800935,0.000002202854,0.000024000772,0.00015702266,0.00052290614,0.0003157782,0.00017706235,0.00020942677,0.21058227],"genre_scores_gemma":[0.99589425,0.0027765902,0.00011474744,0.000094022645,0.00011625662,5.2325623e-7,0.00018676152,0.000009212575,0.0008076465],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987738,0.00008387306,0.0001274052,0.00040972405,0.00015998029,0.00044517667],"domain_scores_gemma":[0.999382,0.00010972823,0.000079094156,0.00026074972,0.000041022126,0.00012737214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017174798,0.00022189163,0.00026306557,0.0035965107,0.00029203465,0.00012857818,0.00031917836,0.00007628207,0.00065864646],"category_scores_gemma":[0.000011918679,0.00019618968,0.00007575066,0.004086934,0.00010780801,0.0003607955,0.00008765612,0.00014134555,0.0002757154],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001956668,0.00045550082,0.6036045,0.00074624224,0.0019092205,0.0021079192,0.099566214,0.0033896067,0.00089360256,0.00943995,0.03712864,0.23880196],"study_design_scores_gemma":[0.00048723505,0.00007173772,0.038313683,0.000020252774,0.000035215442,0.0000048405263,0.00031842446,0.0001719805,0.00022234715,0.00001055594,0.96008027,0.00026347226],"about_ca_topic_score_codex":0.8218526,"about_ca_topic_score_gemma":0.8928627,"teacher_disagreement_score":0.92295164,"about_ca_system_score_codex":0.000020108862,"about_ca_system_score_gemma":0.00024255518,"threshold_uncertainty_score":0.8000383},"labels":[],"label_agreement":null},{"id":"W7074548925","doi":"","title":"THE OXFORD HANDBOOK OF THE HISTORY OF EUGENICS","year":2010,"lang":"en","type":"other","venue":"DigitalGeorgetown (Georgetown University Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Eugenics; Ceylon; Galton's problem; Subject (documents); Ridiculous; Dehumanization","score_opus":0.004202254099377747,"score_gpt":0.131513434506481,"score_spread":0.12731118040710326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074548925","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0032490175,0.0026474367,0.000007575776,0.00041006028,0.004672515,0.0005056964,0.0020951745,0.00014714812,0.98626536],"genre_scores_gemma":[0.0066336934,0.0014627343,0.0001970556,0.000054006134,0.00020799549,2.7633737e-7,0.00026552635,0.00008370274,0.991095],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99826556,0.00012723183,0.00035254497,0.00038249182,0.0004567355,0.00041541582],"domain_scores_gemma":[0.9978243,0.00019006233,0.00078344974,0.0010169642,0.00004752428,0.00013770908],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011968603,0.00037779688,0.0005592055,0.00015777467,0.00015153989,0.00005421031,0.0018453335,0.00040769152,0.0064495816],"category_scores_gemma":[0.00003460947,0.00024310318,0.0003836887,0.00028385854,0.0009902697,0.00040167087,0.00026188968,0.00035292376,0.000055225588],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070287235,0.000036521604,0.0049121636,0.00010923871,0.00018118962,0.000008427692,0.00010370795,0.000006067809,0.00018541727,0.0033813913,0.9876724,0.0033331953],"study_design_scores_gemma":[0.00023299412,0.00004499983,0.0026149605,0.00013254432,0.00008597447,0.0000012972115,0.00003316899,0.000010559674,0.00085050863,0.00072755176,0.99497646,0.00028899117],"about_ca_topic_score_codex":0.0012994176,"about_ca_topic_score_gemma":0.0010628129,"teacher_disagreement_score":0.007304058,"about_ca_system_score_codex":0.000011658835,"about_ca_system_score_gemma":0.0006270897,"threshold_uncertainty_score":0.9944587},"labels":[],"label_agreement":null},{"id":"W7074580089","doi":"","title":"Associations of process-and hybrid-oriented motor competence assessment in spanish adolescents","year":2025,"lang":"en","type":"article","venue":"Dialnet (Universidad de la Rioja)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Agencia Estatal de Investigación; European Regional Development Fund","keywords":"Gross motor skill; Motor skill; Competence (human resources); Test (biology); Correlation; Psychomotor learning","score_opus":0.005739885794716508,"score_gpt":0.237939394579575,"score_spread":0.23219950878485848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074580089","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915587,0.000042523323,0.00014103352,0.00009682682,0.00016859657,0.00016087867,0.00036499073,0.000017163151,0.0074492865],"genre_scores_gemma":[0.9993481,0.000027772088,0.00034208247,0.00005394976,0.000018591849,8.029041e-7,0.00008119703,0.000001939912,0.00012553923],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923545,0.00011877976,0.0001399364,0.00017319724,0.00014849978,0.00018415233],"domain_scores_gemma":[0.99958074,0.00011381782,0.00010033985,0.00010172296,0.00004825289,0.000055118504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021933735,0.00008686749,0.00020275627,0.00012737805,0.00008176702,0.000037909653,0.00014658607,0.000053400832,0.000120403296],"category_scores_gemma":[0.00003420528,0.000092055656,0.00002904779,0.00025620576,0.00007870033,0.00015508811,0.000022275284,0.00010125946,0.0000053815475],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002819393,0.000060359933,0.9924363,0.000074190575,0.000027240485,0.00001877529,0.0003121735,0.0003808956,0.0012667039,0.004054881,0.00016437995,0.0011758923],"study_design_scores_gemma":[0.0004964679,0.000031211293,0.994648,0.00007934017,0.000023683308,5.4515084e-7,0.00018469921,0.001732445,0.00021204632,0.0018654924,0.0006407711,0.00008529357],"about_ca_topic_score_codex":0.0034679237,"about_ca_topic_score_gemma":0.0012326502,"teacher_disagreement_score":0.007789424,"about_ca_system_score_codex":0.000013015066,"about_ca_system_score_gemma":0.00016404934,"threshold_uncertainty_score":0.52424866},"labels":[],"label_agreement":null},{"id":"W7074580496","doi":"","title":"Metabolic Characteristics of Primary Muscle Cells of Diet Sensitive and Diet Resistant Obese Patients","year":2012,"lang":"en","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Myogenesis; Skeletal muscle; Myocyte; Mitochondrion; Basal (medicine); Ex vivo; In vivo; Reactive oxygen species","score_opus":0.002434954775246214,"score_gpt":0.12068857766613339,"score_spread":0.11825362289088717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074580496","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4159263,0.0016732512,0.000002170567,0.000078093515,0.0007341102,0.00036265564,0.027579961,0.000007815917,0.55363566],"genre_scores_gemma":[0.9800603,0.0012851531,0.0003423741,0.00012663842,0.00010880986,7.6322465e-7,0.00022346604,0.00003272877,0.017819766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99835354,0.000076391574,0.00030670734,0.00018970302,0.00084724673,0.00022642416],"domain_scores_gemma":[0.9990604,0.00012679675,0.0004582808,0.00017176126,0.0000012051056,0.00018157704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000015286405,0.00020687727,0.0005719642,0.000028590171,0.000041231397,0.000009103034,0.00012587704,0.000046221372,0.00024951622],"category_scores_gemma":[0.0000018900389,0.00017682128,0.000026377096,0.000038339043,0.00012052334,0.00010761878,0.0000640145,0.0000658645,8.593682e-9],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.018417068,0.00083015306,0.46060854,0.02474909,0.003646958,0.00031360544,0.0018656095,0.000038184382,0.23950137,0.029293915,0.08183659,0.13889892],"study_design_scores_gemma":[0.0002560013,0.00019262012,0.84810793,0.00026011866,0.00009455499,1.8093807e-7,0.00011024192,0.000015580128,0.01282863,0.000091652015,0.1377867,0.00025576123],"about_ca_topic_score_codex":0.023736179,"about_ca_topic_score_gemma":0.025208019,"teacher_disagreement_score":0.564134,"about_ca_system_score_codex":5.951842e-7,"about_ca_system_score_gemma":0.00035004623,"threshold_uncertainty_score":0.9925794},"labels":[],"label_agreement":null},{"id":"W7074609096","doi":"","title":"The Short-a Nasal System: how does it get so tense?","year":2014,"lang":"en","type":"other","venue":"Memorial University Research Repository (Memorial University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nasalization; Dysgeusia; Nucleofection; Noise (video); Auscultation","score_opus":0.01607910638877233,"score_gpt":0.2143499794890983,"score_spread":0.19827087310032598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074609096","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0072613284,0.00015356655,0.00008416738,0.00053085695,0.044031896,0.0015711099,0.0008188684,0.0005820252,0.9449662],"genre_scores_gemma":[0.09398253,0.00037266302,0.00007724353,0.000009757186,0.02333934,3.343534e-7,0.00020975983,0.00011129468,0.8818971],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99264896,0.0026165522,0.0002877478,0.001243359,0.0018386296,0.0013647231],"domain_scores_gemma":[0.99635714,0.0008559996,0.000323854,0.0013379933,0.00046702274,0.00065799773],"candidate_categories":["metaepi_narrow","sts","scholarly_communication"],"consensus_categories":[],"category_scores_codex":[0.0015936848,0.00062664074,0.0008994761,0.0009317606,0.003656178,0.0010860299,0.0029912505,0.00088345,0.0006753612],"category_scores_gemma":[0.00013608787,0.00048289727,0.00038915535,0.0009546877,0.0014589839,0.0004018299,0.00048356975,0.0010430855,0.0006087169],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024067925,0.00006325394,0.0009618217,0.00042644583,0.0007892402,0.003765782,0.00024919957,0.00006486181,0.00087347225,0.006892055,0.98231214,0.0011949547],"study_design_scores_gemma":[0.0011360797,0.00026509757,0.00019411862,0.00018773695,0.00021698257,0.000017950822,0.0020384341,0.000110136396,0.00028226373,0.000033713615,0.99488705,0.00063044886],"about_ca_topic_score_codex":0.0201623,"about_ca_topic_score_gemma":0.0148405675,"teacher_disagreement_score":0.086721204,"about_ca_system_score_codex":0.00020130882,"about_ca_system_score_gemma":0.00095932436,"threshold_uncertainty_score":0.99995095},"labels":[],"label_agreement":null},{"id":"W7074618550","doi":"","title":"Mediadores inflamatórios na dor pélvica crônica identificação de possíveis marcadores séricos da doença","year":2010,"lang":"pt","type":"article","venue":"Americanae (AECID Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Filter (signal processing); Feature (linguistics); Noise (video); Work (physics)","score_opus":0.007192273958647782,"score_gpt":0.21244640004208223,"score_spread":0.20525412608343446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074618550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9823297,0.0008083461,0.000049466602,0.003502632,0.0054140687,0.00075960654,0.0019110495,0.00037262365,0.0048525],"genre_scores_gemma":[0.98593533,0.00074669544,0.0020402318,0.0022280386,0.0018669451,0.000035670415,0.00083584466,0.0001057797,0.0062054703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99395305,0.00051281165,0.0012257166,0.0013882358,0.0010306496,0.0018895419],"domain_scores_gemma":[0.99528795,0.00079841085,0.00080304296,0.0016416953,0.00008584796,0.0013830701],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00051112886,0.00094245526,0.0012570058,0.00041943332,0.00065743213,0.0010320903,0.0023988714,0.00046127234,0.043122217],"category_scores_gemma":[0.00021349959,0.0008353362,0.0004342377,0.001226635,0.0011595621,0.0022964259,0.00040602457,0.001051257,0.0035933445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046773066,0.00039208226,0.66670513,0.00031453467,0.0006822877,0.00083899533,0.0025114126,0.0002050698,0.030748604,0.0016494233,0.23385309,0.061631616],"study_design_scores_gemma":[0.00074677786,0.00048016015,0.8881931,0.00009279995,0.00025292917,0.00004149208,0.00044507958,0.0011578962,0.0069639552,0.0009744123,0.099227,0.0014244129],"about_ca_topic_score_codex":0.062495783,"about_ca_topic_score_gemma":0.0016437015,"teacher_disagreement_score":0.22148792,"about_ca_system_score_codex":0.000010673515,"about_ca_system_score_gemma":0.00071485253,"threshold_uncertainty_score":0.99940974},"labels":[],"label_agreement":null},{"id":"W7074646858","doi":"","title":"“DISTANCE LEARNING” IN THE NINTH CENTURY?: MICRO-CLUSTER ANALYSIS OF THE EPISTOLARY NETWORK OF ALCUIN AFTER 796","year":2020,"lang":"en","type":"article","venue":"UKnowledge (University of Kentucky)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto; University of Cambridge","keywords":"Interpretation (philosophy); Ninth; Interpreter; Period (music); Intellectual history; Order (exchange)","score_opus":0.006163608040631881,"score_gpt":0.1598141556684232,"score_spread":0.15365054762779132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074646858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99475753,0.00070931244,0.0001295261,0.00076346484,0.00015975442,0.00014490377,0.000102153914,0.0000064246206,0.0032269424],"genre_scores_gemma":[0.99935293,0.000100509984,0.00013032187,0.00009140302,0.000040823314,6.2279106e-8,0.000033246135,0.0000020275604,0.00024868964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898475,0.00029656242,0.00017410296,0.0001848554,0.00019111627,0.00016863774],"domain_scores_gemma":[0.99931407,0.00010855242,0.00022844828,0.00023347621,0.00007136724,0.00004406178],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031041956,0.00009502697,0.0003324612,0.00005330415,0.00008815001,0.000008053972,0.0005365185,0.000054619137,0.00095240126],"category_scores_gemma":[0.000026841968,0.000070158574,0.00019602843,0.0010012314,0.00018167945,0.00008773699,0.00007056522,0.00013055938,0.000019666288],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005983058,0.00008455061,0.9565551,0.00021511775,0.0004903549,0.000018183218,0.019996565,0.013512701,0.0010695077,0.00033486134,0.0052500986,0.0018746068],"study_design_scores_gemma":[0.00032345956,0.00007299819,0.9536775,0.00005310828,0.0004162831,2.967528e-7,0.0011578916,0.003308535,0.0001561694,0.00008701961,0.04062864,0.00011814265],"about_ca_topic_score_codex":0.0010283466,"about_ca_topic_score_gemma":0.0043841796,"teacher_disagreement_score":0.035378546,"about_ca_system_score_codex":0.0000036476497,"about_ca_system_score_gemma":0.00003552427,"threshold_uncertainty_score":0.99996084},"labels":[],"label_agreement":null},{"id":"W7074648785","doi":"","title":"Acupuncture therapy in treating migraine: results of a magnetic resonance spectroscopy imaging study","year":2018,"lang":"en","type":"other","venue":"Dove Medical Press (Taylor and Francis Group)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Migraine; Acupuncture; Aura; Magnetic resonance imaging; Proton magnetic resonance; Functional magnetic resonance imaging; Migraine with aura","score_opus":0.007361946197143422,"score_gpt":0.22890616959077195,"score_spread":0.22154422339362853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074648785","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07606251,0.25560993,0.005080512,0.00062174705,0.007710781,0.008346665,0.00676701,0.0005773884,0.63922346],"genre_scores_gemma":[0.99567044,0.00023923576,0.0004370191,0.0001861975,0.0015507874,0.000020007667,0.00023436459,0.000086059656,0.001575881],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974083,0.00022223743,0.00055840006,0.0006731099,0.0006952509,0.00044272162],"domain_scores_gemma":[0.9988713,0.0002338527,0.0002476707,0.00042437194,0.000027749886,0.00019504013],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006842338,0.00044663207,0.00087335805,0.00013742482,0.000053628024,0.000061657505,0.0004340804,0.00024881223,0.005642465],"category_scores_gemma":[0.0001744836,0.0002745343,0.00008426463,0.00017665504,0.00030096204,0.000060556285,0.000048107402,0.00026694627,0.00003016971],"study_design_candidate":"design_other","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00093250023,0.00033685198,0.06557433,0.00022749667,0.0000757523,0.00022176625,0.0018537423,0.0000021863862,0.00020936734,0.000024017627,0.009333435,0.92120856],"study_design_scores_gemma":[0.025289305,0.005970817,0.27200568,0.0004016863,0.00033133122,0.000037992213,0.00073650933,0.045237605,0.00048012013,0.0014417605,0.645227,0.0028401688],"about_ca_topic_score_codex":0.02237658,"about_ca_topic_score_gemma":0.0069485316,"teacher_disagreement_score":0.91960794,"about_ca_system_score_codex":0.000002522153,"about_ca_system_score_gemma":0.0000036068407,"threshold_uncertainty_score":0.9999707},"labels":[],"label_agreement":null},{"id":"W7074670411","doi":"","title":"Aboriginal post-secondary education in British Columbia : Nicola Valley Institute of Technology","year":2012,"lang":"en","type":"other","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Indigenous; Circumstantial evidence; Population; Frugality; Pretext","score_opus":0.0033765545852026163,"score_gpt":0.17035953294806747,"score_spread":0.16698297836286485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074670411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9239895,0.0025051266,0.000005471866,0.000023471246,0.0013948906,0.00045714472,0.003602244,0.000073546464,0.067948654],"genre_scores_gemma":[0.83523405,0.0020798629,0.0012275174,0.000036092817,0.0002320751,8.7010244e-7,0.0010318044,0.000052806692,0.16010493],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987597,0.000052449832,0.00021435402,0.00041178465,0.0002265414,0.00033519117],"domain_scores_gemma":[0.9990643,0.0000138518635,0.00036410792,0.00031088156,0.00012952527,0.000117331176],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015624677,0.000072491595,0.00056766404,0.00014984971,0.000099002755,0.0001428278,0.0005352196,0.00044415565,0.012590966],"category_scores_gemma":[0.00000910492,0.0003071765,0.000097502394,0.00035361835,0.0004214139,0.0003155275,0.000036920843,0.00021966035,0.00008927969],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000059592767,0.00018759219,0.12352801,0.00047018362,0.0000706503,0.00009100344,0.000048424354,0.0000022343493,0.00006421015,0.0000021971562,0.12083083,0.7546987],"study_design_scores_gemma":[0.0003938879,0.00006198212,0.7414563,0.00050551107,0.00004571957,0.00004216602,0.00018514329,0.0000017728702,1.8135003e-7,0.00016560298,0.25691777,0.00022397166],"about_ca_topic_score_codex":0.96732503,"about_ca_topic_score_gemma":0.9966477,"teacher_disagreement_score":0.75447476,"about_ca_system_score_codex":0.000013331008,"about_ca_system_score_gemma":0.00088633405,"threshold_uncertainty_score":0.999938},"labels":[],"label_agreement":null},{"id":"W7074681568","doi":"","title":"Canadian Conference on Medical Education 2022 abstracts","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Continuing medical education; MEDLINE; Curriculum; Accreditation","score_opus":0.0222512944757124,"score_gpt":0.22737738371483618,"score_spread":0.2051260892391238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074681568","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.064452395,0.00018683333,2.3051648e-8,0.0030372883,0.0015833152,0.0002995727,0.69684225,0.000053005126,0.23354529],"genre_scores_gemma":[0.85943604,0.000001214099,0.0000029065322,0.0013360474,0.00014773641,0.00001662788,0.13819282,0.0000018164229,0.0008648023],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992742,0.000040061856,0.00008314732,0.00013282575,0.0002997225,0.00017003421],"domain_scores_gemma":[0.99954236,0.000030365383,0.00003565057,0.0001098359,0.000023660157,0.00025812886],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000068040215,0.000057038884,0.00006182134,0.000042883534,0.00021594837,0.000047930593,0.0002332749,0.000028750706,0.94185925],"category_scores_gemma":[0.00015060912,0.000054028107,0.00001642635,0.00007341701,0.0000022563397,0.000047964142,0.00001450329,0.00011907478,0.0058146096],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000043692703,0.000014958713,0.00018601002,0.000014146897,0.0000037616878,0.000027039405,0.00006872251,0.00036632063,0.000005379289,0.00014407151,0.98613936,0.013025836],"study_design_scores_gemma":[0.00005047111,0.00005253744,0.05393766,0.00005749439,0.0000016004504,0.0000068357363,0.000046161294,0.00033487103,0.0000340423,0.00036401418,0.94500434,0.00010998345],"about_ca_topic_score_codex":0.09369789,"about_ca_topic_score_gemma":0.14903532,"teacher_disagreement_score":0.93604463,"about_ca_system_score_codex":0.000008951208,"about_ca_system_score_gemma":0.0014345042,"threshold_uncertainty_score":0.9949595},"labels":[],"label_agreement":null},{"id":"W7074688341","doi":"","title":"Loneliness and social isolation in the COVID-19 pandemic among the over 70s. Data from The Irish Longitudinal Study on Ageing","year":2020,"lang":"en","type":"report","venue":"Arrow@dit (Dublin Institute of Technology)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trinity College","funders":"","keywords":"Loneliness; Social isolation; Longitudinal study; Pandemic; Irish; Isolation (microbiology); Longitudinal data","score_opus":0.1422718445035927,"score_gpt":0.3342868153319713,"score_spread":0.1920149708283786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074688341","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98718834,0.0006566996,0.000107315595,0.0062791007,0.002005794,0.0011458202,0.0019003643,0.00009971301,0.00061683205],"genre_scores_gemma":[0.99648684,0.00041136428,0.000041163767,0.0003775936,0.0010053037,0.000018265944,0.0016232337,0.000011135738,0.000025083247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972341,0.00020862247,0.0006851392,0.0007727807,0.0007910825,0.00030828782],"domain_scores_gemma":[0.9975988,0.00041356907,0.0006788621,0.0011752703,0.000089106215,0.00004434904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021207822,0.00035303354,0.0006138762,0.00016866474,0.0005744584,0.0002084979,0.0024224888,0.000474004,0.0001110928],"category_scores_gemma":[0.0009532998,0.0001880538,0.00006913593,0.00061548204,0.00079593505,0.00037351885,0.0003722127,0.00095197535,0.000018970683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009808071,0.00009430097,0.9466592,0.00008889023,0.0002675167,0.00017455278,0.0010063178,0.00036932091,0.00003456461,0.0001443177,0.04786175,0.0032011669],"study_design_scores_gemma":[0.00062209496,0.00012741034,0.8266025,0.0000719072,0.00027614544,0.000016676935,0.0009211757,0.00036776508,0.0000039188117,0.0014728372,0.16921584,0.0003017175],"about_ca_topic_score_codex":0.030898282,"about_ca_topic_score_gemma":0.0515172,"teacher_disagreement_score":0.121354096,"about_ca_system_score_codex":0.00001980266,"about_ca_system_score_gemma":0.00048365653,"threshold_uncertainty_score":0.97555506},"labels":[],"label_agreement":null},{"id":"W7074690926","doi":"","title":"Review of Anna C. Korteweg and Jennifer A. Selby (eds.), &lt;i&gt;Debating Sharia: Islam, Gender Politics, and Family Law&lt;/i&gt;, Toronto: University of Toronto Press 2012","year":2014,"lang":"en","type":"other","venue":"Utrecht University Repository (Utrecht University)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Dysgeusia; Diafiltration; Liquation; Triacetin; Emperipolesis; Fusible alloy","score_opus":0.008657084616151757,"score_gpt":0.1756248811614237,"score_spread":0.16696779654527194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074690926","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0027756803,0.08998805,0.00008773781,0.000027989301,0.0008344709,0.0006764527,0.0013401841,0.00016322841,0.9041062],"genre_scores_gemma":[0.02003817,0.23550375,0.0016054377,0.00012783294,0.00046224965,1.02322964e-7,0.00049260753,0.000119889824,0.74165],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99713355,0.0005463539,0.0003651237,0.0009264095,0.00046138963,0.00056718336],"domain_scores_gemma":[0.9975283,0.00018695525,0.0008616612,0.00076619576,0.0002404179,0.00041644822],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003523237,0.0005870155,0.0012292619,0.000114385766,0.00041153526,0.00003546334,0.0008250188,0.0006493939,0.0022808295],"category_scores_gemma":[0.000015850388,0.0006852506,0.00023921304,0.00014146877,0.00063387956,0.0007366659,0.0003292973,0.00021722642,0.000013708435],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065377995,0.0005641563,0.0023211797,0.022385668,0.0043806746,0.0011158482,0.003164473,0.00003917455,0.0075646215,0.05278849,0.8928808,0.012141163],"study_design_scores_gemma":[0.00094133016,0.00016537058,0.002052334,0.0020477665,0.0011146365,0.000019051602,0.000397205,0.00005533842,0.00008934053,0.00003096816,0.99238646,0.0007001989],"about_ca_topic_score_codex":0.09489042,"about_ca_topic_score_gemma":0.03177039,"teacher_disagreement_score":0.16245624,"about_ca_system_score_codex":0.00010862136,"about_ca_system_score_gemma":0.00022390415,"threshold_uncertainty_score":0.9995599},"labels":[],"label_agreement":null},{"id":"W7074701115","doi":"","title":"Using a Delphi Consensus Method to Examine Behavior Change Theories Taught to Canadian Undergraduate Students","year":2019,"lang":"en","type":"other","venue":"OSF Preprints (OSF Preprints)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Behaviour change; Behavior change; Delphi method; Field (mathematics); Theory of planned behavior; Theory of change","score_opus":0.03884625659129643,"score_gpt":0.30410359659767455,"score_spread":0.26525734000637813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074701115","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03240876,0.000011135675,0.0010388235,0.00065505016,0.0030498207,0.007240913,0.0026994692,0.0002197001,0.95267636],"genre_scores_gemma":[0.0389156,0.000034179244,0.011393623,0.0008808969,0.00056152185,0.00022863703,0.00021790502,0.00020194585,0.9475657],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.994818,0.00081711647,0.00052547577,0.0022363046,0.000680024,0.00092309184],"domain_scores_gemma":[0.9956397,0.00025085575,0.00030259823,0.002729871,0.00011590095,0.00096107676],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0027292483,0.0006275462,0.00088524254,0.00056897197,0.0001901397,0.00034195112,0.001649036,0.00041880013,0.37810394],"category_scores_gemma":[0.00035778744,0.0006330995,0.00014907662,0.00035024312,0.00008187931,0.00008662789,0.0005633771,0.00029599876,0.6291879],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005690904,0.0005868641,0.1618785,0.0010346384,0.002194552,0.0012088995,0.007442788,0.0063588675,0.006214775,0.004612899,0.6977684,0.11012976],"study_design_scores_gemma":[0.00041918838,0.0000063545554,0.032639638,0.00032188033,0.00029204463,0.000036534646,0.000107707325,0.00008639594,0.0005176606,0.00087274396,0.9636227,0.0010771839],"about_ca_topic_score_codex":0.57326984,"about_ca_topic_score_gemma":0.3683501,"teacher_disagreement_score":0.2658543,"about_ca_system_score_codex":0.00008158396,"about_ca_system_score_gemma":0.0003803434,"threshold_uncertainty_score":0.99961203},"labels":[],"label_agreement":null},{"id":"W7074703161","doi":"","title":"The rise of the graphic novel computational criticism and the evolution of literary value","year":2023,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Comics; Argument (complex analysis); Style (visual arts); Periodization; Representation (politics); Graphic design; Literary criticism; Value (mathematics); Comic strip","score_opus":0.006433769760262368,"score_gpt":0.19405834885001713,"score_spread":0.18762457908975477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074703161","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995204,0.00059734134,0.00023784088,0.0013771803,0.000397089,0.00015257679,0.00017145537,0.000010901366,0.0018516629],"genre_scores_gemma":[0.99951804,0.0000273916,0.00008812905,0.00004379401,0.000033089545,7.586092e-7,0.0000069034304,8.9736886e-7,0.00028101652],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9994705,0.00008634152,0.00013720209,0.00006320998,0.00016335405,0.00007944264],"domain_scores_gemma":[0.9992669,0.0005238359,0.000051693467,0.00010502923,0.000039002734,0.000013534653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045545236,0.000040835297,0.0000760262,0.000017522056,0.0001766561,0.000025836593,0.00014258687,0.000015919895,0.00004512121],"category_scores_gemma":[0.000028820456,0.000015860665,0.000036454112,0.00018084238,0.00030411422,0.000048642196,0.000021385022,0.000029232375,0.0000066099165],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001465241,0.000027427692,0.034378015,0.000097377684,0.00009529558,5.9437883e-7,0.001688084,0.02210303,0.0024814568,0.9342231,0.0021199908,0.0026391172],"study_design_scores_gemma":[0.0003247401,0.000017710925,0.7394067,0.000012777912,0.000016066762,0.0000014818708,0.00012169085,0.050707128,0.00012860258,0.20825234,0.00097396714,0.000036808913],"about_ca_topic_score_codex":0.0013649571,"about_ca_topic_score_gemma":0.00012825885,"teacher_disagreement_score":0.72597075,"about_ca_system_score_codex":3.73277e-7,"about_ca_system_score_gemma":0.000023530127,"threshold_uncertainty_score":0.20634158},"labels":[],"label_agreement":null},{"id":"W7074722543","doi":"","title":"Training in the solid wood manufacturing industry : a comparison between interior British Columbia, Alberta and New Zealand","year":2001,"lang":"en","type":"other","venue":"cIRcle (University of British Columbia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Training (meteorology); Productivity; Investment (military); Manufacturing; Population; Sample (material); Wood industry","score_opus":0.017076983380244482,"score_gpt":0.1942440943333289,"score_spread":0.1771671109530844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074722543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9694877,0.00028678324,0.00000680265,0.000049791008,0.00022072766,0.0003658278,0.0009936639,0.000036900492,0.02855175],"genre_scores_gemma":[0.85750103,0.0001918208,0.000084716296,0.000037348473,0.00027338447,2.3161148e-7,0.00022558079,0.000031807038,0.14165406],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9985447,0.00011908119,0.00020981228,0.0004743556,0.00025387853,0.00039816246],"domain_scores_gemma":[0.99921477,0.00009821691,0.0002622634,0.00023565117,0.00001431527,0.00017478211],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020374426,0.00009230279,0.00067337044,0.000050453287,0.00016915737,0.00077640335,0.0005387642,0.00047357258,0.005796444],"category_scores_gemma":[0.000011833323,0.0002912273,0.00007775113,0.00014064144,0.00019790651,0.00015908675,0.000068295245,0.00043971042,0.000024671011],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000030933422,0.000015918946,0.20222908,0.00008488203,0.00008256655,0.0002303141,0.0008841405,0.0000041007606,0.0000020175669,2.1097232e-8,0.15584272,0.6406211],"study_design_scores_gemma":[0.0006583775,0.0000707664,0.91617554,0.0007463573,0.00007929911,0.00007726406,0.0016349661,0.000009539028,1.1516478e-7,0.0001002974,0.08014761,0.00029983657],"about_ca_topic_score_codex":0.9911958,"about_ca_topic_score_gemma":0.99852425,"teacher_disagreement_score":0.71394646,"about_ca_system_score_codex":0.0000066826024,"about_ca_system_score_gemma":0.00009878875,"threshold_uncertainty_score":0.999954},"labels":[],"label_agreement":null},{"id":"W7074724334","doi":"","title":"Dalitz plot analysis of the decay B±→K±K±K","year":2006,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"SLAC National Accelerator Laboratory; Institut National de Physique Nucléaire et de Physique des Particules; U.S. Department of Energy; European Commission; Institute of High Energy Physics; Centre National de la Recherche Scientifique; Bundesministerium für Bildung und Forschung; Alfred P. Sloan Foundation; Natural Sciences and Engineering Research Council of Canada; Alexander von Humboldt-Stiftung; Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Dalitz plot; Isobar; Branching fraction; Measure (data warehouse); Asymmetry; CP violation; Particle decay","score_opus":0.008118030416358946,"score_gpt":0.18120056412077898,"score_spread":0.17308253370442003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074724334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9488971,0.00014154946,0.00002289299,0.00019390057,0.00018774324,0.00013240233,0.010643972,0.00008026877,0.039700173],"genre_scores_gemma":[0.9972889,0.0000035638545,0.000100097815,0.00013051939,0.00013352075,0.0000012039878,0.0015301425,0.000010204148,0.0008018376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99851066,0.0000911465,0.000417554,0.00028348295,0.00038018066,0.00031698705],"domain_scores_gemma":[0.99911445,0.00013634781,0.00018105454,0.0004389063,0.000025016021,0.000104241655],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014410785,0.00018740498,0.00033566717,0.00013728393,0.00012775617,0.00059217,0.00059421617,0.000081169994,0.0027810484],"category_scores_gemma":[0.000029479555,0.00012025085,0.00029494203,0.0011614852,0.00011374044,0.0010279,0.000069637055,0.00012261546,0.00068536674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034298784,0.000043264623,0.99260503,0.000018650982,0.00020234837,0.0000047917124,0.0000076164342,0.0013292766,0.00040623074,0.0031142908,0.0010795706,0.0011546112],"study_design_scores_gemma":[0.00017031869,0.000028648295,0.8901764,0.00001690584,0.00025090046,0.0000011291216,0.000006490993,0.0002894696,0.00878317,0.010287892,0.08974184,0.0002468055],"about_ca_topic_score_codex":0.00030250836,"about_ca_topic_score_gemma":0.00011076764,"teacher_disagreement_score":0.102428615,"about_ca_system_score_codex":0.0000016675866,"about_ca_system_score_gemma":0.000049905782,"threshold_uncertainty_score":0.99813056},"labels":[],"label_agreement":null},{"id":"W7074725941","doi":"","title":"A Multidimensional Decisions Modelling Framework for Built Space Supply","year":2012,"lang":"en","type":"article","venue":"Infoscience (Ecole Polytechnique Fédérale de Lausanne)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Profit (economics); Space (punctuation); Zoning; Work (physics); Supply and demand; Econometric model; Distribution (mathematics); Spatial analysis","score_opus":0.03240635695104065,"score_gpt":0.2731663388272379,"score_spread":0.24075998187619724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074725941","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43936035,0.0002543222,0.5567334,0.00042841514,0.0009955392,0.00076544617,0.0003500028,0.00020324862,0.0009092636],"genre_scores_gemma":[0.64206415,0.00006308771,0.3567792,0.00042308038,0.00034198607,0.00004512061,0.00004026933,0.000009556885,0.00023354337],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9975311,0.00007476092,0.00038511693,0.00041071247,0.00042471322,0.0011736061],"domain_scores_gemma":[0.99787945,0.0008827198,0.0001766925,0.00046827926,0.000106756204,0.00048611342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001171654,0.00026974076,0.00031799253,0.0001640598,0.00051230314,0.00013878696,0.00056871463,0.00025214147,0.0007045928],"category_scores_gemma":[0.0003566406,0.00024255709,0.0001393857,0.0004188893,0.00018577364,0.00079473463,0.00006931716,0.0002317048,0.00021203134],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063506654,0.000795461,0.26104665,0.00018652497,0.00010722755,0.000038984937,0.004003589,0.2394734,0.078021415,0.36040008,0.02066109,0.03463052],"study_design_scores_gemma":[0.0011137851,0.0008498928,0.090201706,0.0008210362,0.00013396009,0.00010390273,0.00036378606,0.4141441,0.17310108,0.15366842,0.16279453,0.002703813],"about_ca_topic_score_codex":0.0015462793,"about_ca_topic_score_gemma":0.00014620843,"teacher_disagreement_score":0.20673165,"about_ca_system_score_codex":0.000015735284,"about_ca_system_score_gemma":0.00016857954,"threshold_uncertainty_score":0.98911905},"labels":[],"label_agreement":null},{"id":"W7074741994","doi":"","title":"Psychometric Validation and Demographic Differences in Two Recently Developed Trait Mindfulness Measures","year":2012,"lang":"en","type":"article","venue":"ResearchArchive–Te Puna Rangahau (Victoria University of Wellington)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mindfulness; Trait; Facet (psychology); Context (archaeology); Happiness; Psychometrics; Self-report study; Depression (economics); Construct validity; Young adult","score_opus":0.03440385587139878,"score_gpt":0.24286340926023586,"score_spread":0.2084595533888371,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074741994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99603015,0.0004895627,0.001246721,0.00014246129,0.00046546527,0.00034075166,0.00019213225,0.000025181469,0.001067583],"genre_scores_gemma":[0.9984209,0.0005764705,0.0005688401,0.0000065060844,0.00016263966,5.14615e-7,0.00010577981,0.0000068588693,0.00015147805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976658,0.00047546305,0.00025224508,0.00035253837,0.0006232973,0.00063063146],"domain_scores_gemma":[0.9987868,0.0004456436,0.0001390708,0.00020580516,0.000101262005,0.00032140396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013205375,0.00020161344,0.0004002773,0.00081361254,0.00027051207,0.000056692934,0.00046380606,0.00007551082,0.0005057546],"category_scores_gemma":[0.0000865873,0.00019441897,0.000077169185,0.0009796295,0.00028163067,0.00050415646,0.000053982476,0.00024940606,0.00003905554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007432376,0.00015185917,0.89623725,0.00017950122,0.00011920855,0.0000068452855,0.0038203546,0.00007044792,0.001886783,0.0019351062,0.00009355973,0.09475583],"study_design_scores_gemma":[0.0016514465,0.000114480754,0.978968,0.00010040223,0.000044900993,0.0000031458994,0.0006608563,0.00040468771,0.004889761,0.0034143457,0.009381388,0.00036656152],"about_ca_topic_score_codex":0.007825413,"about_ca_topic_score_gemma":0.0028859787,"teacher_disagreement_score":0.09438927,"about_ca_system_score_codex":0.00000936553,"about_ca_system_score_gemma":0.00008565612,"threshold_uncertainty_score":0.99878156},"labels":[],"label_agreement":null},{"id":"W7074747943","doi":"","title":"Using a WebCT to Develop a Research Skills Module","year":2003,"lang":"en","type":"other","venue":"E-LIS Repository (University of Naples Federico II)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Session (web analytics); Presentation (obstetrics); Tracking (education); Process (computing); Postgraduate research","score_opus":0.0319926829371612,"score_gpt":0.24567278936195852,"score_spread":0.21368010642479732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074747943","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13680397,0.00088324735,0.00044024718,0.00008555957,0.0017297302,0.0007766967,0.00043792528,0.00015572639,0.8586869],"genre_scores_gemma":[0.04920878,0.0001527495,0.018976655,0.0000438837,0.00043027624,3.1902528e-7,0.00012404709,0.000086010084,0.9309773],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978365,0.00030175192,0.00018537941,0.00056330103,0.0006244073,0.0004886689],"domain_scores_gemma":[0.99875903,0.00006095865,0.00023428345,0.00046371587,0.00023510787,0.000246915],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035877846,0.0002639493,0.00053870736,0.00038312087,0.00084659207,0.000109495646,0.0006751691,0.00030109967,0.005998245],"category_scores_gemma":[0.00004159156,0.0002943291,0.00009801677,0.00090901967,0.00018191307,0.0001406583,0.00016443813,0.0002076125,0.00038495046],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000106672014,0.00016626531,0.0020958674,0.00029798842,0.00035901883,0.00037805934,0.0019698294,0.00039392035,0.0062865405,0.0001689223,0.9857462,0.0020307112],"study_design_scores_gemma":[0.00025549807,0.00015788914,0.0032531982,0.00023785127,0.00005030757,0.000020628398,0.00060634257,0.00008537481,0.0005149772,0.00003914696,0.9943503,0.00042844194],"about_ca_topic_score_codex":0.028019,"about_ca_topic_score_gemma":0.003154951,"teacher_disagreement_score":0.087595195,"about_ca_system_score_codex":0.000028388247,"about_ca_system_score_gemma":0.00041975506,"threshold_uncertainty_score":0.9999509},"labels":[],"label_agreement":null},{"id":"W7075270998","doi":"","title":"Implementation and removal of an affrmative-action quota: The impact on task assignment and workers' skill acquisition","year":2013,"lang":"en","type":"article","venue":"Figshare","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Affirmative action; Repeal; Legislation; Task (project management); Equity (law); Action (physics); Public policy; Employment discrimination","score_opus":0.021032878098099707,"score_gpt":0.28092303217094744,"score_spread":0.2598901540728477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7075270998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97104806,0.000061680104,0.0000015373631,0.00004970762,0.00003863103,0.00026072044,0.028108789,0.000008847373,0.00042201453],"genre_scores_gemma":[0.9845274,0.000005033848,0.000031636737,0.000038443686,0.00006790335,0.000008525489,0.015303639,0.0000018609518,0.000015545857],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9995238,0.0000708132,0.00009531019,0.00010452874,0.00010711839,0.00009839117],"domain_scores_gemma":[0.99969536,0.00006075667,0.000089524365,0.00008022324,0.000026449332,0.000047690897],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000059497666,0.00007300785,0.00007752923,0.000019146302,0.00008792388,0.000090143214,0.00004348462,0.000025859601,0.07346535],"category_scores_gemma":[0.000008380734,0.000043458433,0.000015095731,0.000038003804,0.000007944879,0.0003221063,0.00000857898,0.00002928129,0.00014182407],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039005734,0.00012899391,0.029534616,0.00048771797,0.00028346822,0.000024922441,0.009271561,0.003710542,0.027919091,0.000048267775,0.2522237,0.67597705],"study_design_scores_gemma":[0.00017542964,0.00025303554,0.99458563,0.000081400845,0.0000056942345,0.00000764356,0.0004995787,0.0005915184,0.00241094,0.00030465273,0.0010088175,0.00007566429],"about_ca_topic_score_codex":0.0013891336,"about_ca_topic_score_gemma":0.00009458126,"teacher_disagreement_score":0.965051,"about_ca_system_score_codex":0.000002480053,"about_ca_system_score_gemma":0.000009988662,"threshold_uncertainty_score":0.92738163},"labels":[],"label_agreement":null},{"id":"W7075576738","doi":"","title":"Full Genome of Phialocephala scopiformis DAOMC 229536, a Fungal Endophyte of Spruce Producing the Potent Anti-Insectan Compound Rugulosin.","year":2016,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Endophyte; Genome; Genomics; Genotyping; Whole genome sequencing; Reference genome; Inoculation","score_opus":0.010938034494354782,"score_gpt":0.19325976231844713,"score_spread":0.18232172782409234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7075576738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99314153,0.00030529717,0.00016692563,0.00029026106,0.000531823,0.00034238317,0.00037036635,0.000025256855,0.004826156],"genre_scores_gemma":[0.9989584,0.000096720454,0.00031152682,0.000044122742,0.00030039763,0.0000014285491,0.000017804648,0.0000060808025,0.00026352212],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9985051,0.000090449845,0.00043374702,0.0002959501,0.00034521683,0.0003295073],"domain_scores_gemma":[0.9989869,0.0001428269,0.0002452907,0.00044461913,0.000099352794,0.00008098633],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045762543,0.00017615056,0.0003756227,0.000059581038,0.00011971028,0.000034957757,0.0003847932,0.00004719645,0.0015255588],"category_scores_gemma":[0.000027221915,0.0000861142,0.000093861716,0.00016248906,0.00018791134,0.0001979023,0.000040958774,0.000050637653,0.00009089908],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024773087,0.000082614126,0.028054899,0.00021093052,0.00013039797,0.00001418996,0.00052357704,0.00036716534,0.9635708,0.0008791181,0.00024129527,0.0056773364],"study_design_scores_gemma":[0.001377376,0.0008651512,0.6825973,0.00022466626,0.00011866866,0.00005798517,0.00011746364,0.00018325842,0.30770776,0.0018238359,0.0044012256,0.0005253431],"about_ca_topic_score_codex":0.002665268,"about_ca_topic_score_gemma":0.00047699758,"teacher_disagreement_score":0.655863,"about_ca_system_score_codex":0.0000029422906,"about_ca_system_score_gemma":0.000071574796,"threshold_uncertainty_score":0.9993872},"labels":[],"label_agreement":null},{"id":"W7075579378","doi":"","title":"Annual survival of Red Knots (&lt;i&gt;Calidris canutus rufa&lt;/i&gt;) using the San Antonio Oeste stopover site is reduced by domino effects involving late arrival and food depletion in Delaware Bay","year":2006,"lang":"en","type":"article","venue":"Digital Library .UBAExacts (University of Buenos Aires)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Bay; Flyway; Population; Population decline; Overwintering; Netting; Mark and recapture","score_opus":0.005058206482387468,"score_gpt":0.15499313728336817,"score_spread":0.1499349308009807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7075579378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917395,0.0005145504,0.000035403365,0.000133259,0.0001735384,0.00030392708,0.005774069,0.000044718,0.0012810433],"genre_scores_gemma":[0.99858975,0.00006911672,0.00014947473,0.00003013355,0.000060064005,1.2906915e-7,0.0006968664,0.000014006083,0.0003904666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984533,0.00016136657,0.00026741796,0.00039621154,0.0003446092,0.00037707697],"domain_scores_gemma":[0.9990524,0.00021861076,0.00027664733,0.0002722896,0.000043759446,0.00013628167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012983222,0.00024267478,0.00043901842,0.00015315041,0.0002487132,0.00016173066,0.0003265892,0.00014060804,0.00011378788],"category_scores_gemma":[0.000017876322,0.00023529684,0.000100561665,0.00036052807,0.0002845265,0.00234582,0.00013331394,0.00011059486,0.00000769991],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002544665,0.00073682406,0.5238799,0.0015245676,0.0006243283,0.0005049605,0.0102280285,0.008309534,0.40595362,0.0015726172,0.031619973,0.012501021],"study_design_scores_gemma":[0.0023674523,0.00062513707,0.96510315,0.00037837616,0.00013025194,0.000012269325,0.00047568663,0.0033389127,0.010079361,0.0011182798,0.015609844,0.000761308],"about_ca_topic_score_codex":0.0035454808,"about_ca_topic_score_gemma":0.002839052,"teacher_disagreement_score":0.44122326,"about_ca_system_score_codex":0.000011119062,"about_ca_system_score_gemma":0.00010456355,"threshold_uncertainty_score":0.9595127},"labels":[],"label_agreement":null},{"id":"W7075600503","doi":"","title":"Male condition, female choice, and extreme variation in repeated mating in a scaly cricket, Ornebius aperta (Orthoptera: Gryllidae: Mogoplistinae)","year":2000,"lang":"en","type":"article","venue":"TSpace","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Spermatophore; Mating; Courtship; Cricket; Reproduction; Variation (astronomy); Female sperm storage","score_opus":0.018186716595515517,"score_gpt":0.25340582379601495,"score_spread":0.23521910720049943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7075600503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98321825,0.00015134734,0.000017956856,0.00016950585,0.00008534276,0.0002064085,0.000028908025,0.000031701336,0.016090583],"genre_scores_gemma":[0.99563766,0.00004777403,0.0005338131,0.000096639094,0.00008294994,0.000005281467,0.000119735334,0.0000052066707,0.003470952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99888223,0.000108999775,0.00027312836,0.0003119274,0.00014496918,0.00027875302],"domain_scores_gemma":[0.9995466,0.00011834496,0.00007769569,0.0001620267,0.00002388484,0.000071462055],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030555908,0.00013912198,0.00021940532,0.00008701528,0.00008603869,0.00010821231,0.00009008213,0.000071995346,0.006764099],"category_scores_gemma":[0.000055688884,0.00013026354,0.000018927409,0.00027643295,0.00003152161,0.00023973447,0.000009209427,0.00009263303,0.00017983434],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072502924,0.000060467613,0.97428143,0.00009769838,0.000012825365,0.000088418325,0.0044751638,0.0033947602,0.002797826,0.00011770194,0.00026960683,0.014331627],"study_design_scores_gemma":[0.00050869305,0.00003756941,0.99111295,0.000058052967,0.000008838263,0.000019484125,0.00010431917,0.005510608,0.00007262903,0.0002382747,0.0021504194,0.00017816393],"about_ca_topic_score_codex":0.0239437,"about_ca_topic_score_gemma":0.008080169,"teacher_disagreement_score":0.016831545,"about_ca_system_score_codex":0.000005320882,"about_ca_system_score_gemma":0.000021927137,"threshold_uncertainty_score":0.99414384},"labels":[],"label_agreement":null},{"id":"W7075616371","doi":"","title":"Les enjeux et défis de la gouvernance biculturelle : l’exemple du gouvernement régional de l’Eeyou-Istchee-Baie-James","year":2021,"lang":"fr","type":"article","venue":"Industrias Culturais (Universidade de Coimbra)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Context (archaeology); Government (linguistics); Convention; Delegation; Legislation","score_opus":0.024054083589023823,"score_gpt":0.23756417351228487,"score_spread":0.21351008992326104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7075616371","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88101333,0.0064912564,0.000414973,0.058842078,0.0021324598,0.0004262828,0.003711183,0.00017633164,0.04679212],"genre_scores_gemma":[0.94688004,0.0025334994,0.0022779277,0.001311408,0.0012300079,0.000008008774,0.0009129806,0.00003406355,0.04481208],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99546367,0.0014676943,0.00042617082,0.0007935591,0.00062985305,0.0012190581],"domain_scores_gemma":[0.99755126,0.0006970703,0.00037813117,0.0004192212,0.0003313156,0.00062298053],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010719036,0.0005745194,0.0006157322,0.0000941574,0.0008010323,0.0006818144,0.0007728124,0.0010140283,0.011479665],"category_scores_gemma":[0.00047136933,0.0005792437,0.0003393516,0.0007135439,0.00046501507,0.0007073548,0.00021294566,0.00096147426,0.00028170287],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020370886,0.00050738576,0.04149142,0.00021434332,0.0007445966,0.0028682307,0.009198084,0.008264423,0.024769368,0.034159362,0.8688613,0.008717736],"study_design_scores_gemma":[0.0014087826,0.0001073893,0.3614014,0.0002721634,0.00025139604,0.00028122784,0.004117011,0.00043521475,0.0071092965,0.0012147272,0.6227249,0.0006765133],"about_ca_topic_score_codex":0.060932446,"about_ca_topic_score_gemma":0.00357653,"teacher_disagreement_score":0.31991,"about_ca_system_score_codex":0.00038126917,"about_ca_system_score_gemma":0.0016389813,"threshold_uncertainty_score":0.9996659},"labels":[],"label_agreement":null},{"id":"W7075711598","doi":"","title":"Factors influencing visor use among players in the National Hockey League (NHL)","year":2014,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"League; Confidence interval; Quarter (Canadian coin)","score_opus":0.03116916143740261,"score_gpt":0.22070083125824372,"score_spread":0.1895316698208411,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7075711598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932535,0.0000037272207,0.000032122414,0.000055427125,0.00018584087,0.00009297681,0.000032348817,0.000020240284,0.0063237846],"genre_scores_gemma":[0.99910784,0.0000017599217,0.000057833502,0.00045374196,0.000108441316,9.2883886e-7,0.000047127025,0.0000019088454,0.00022040046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99913484,0.00010042868,0.0001510896,0.00014578979,0.00028128485,0.00018656933],"domain_scores_gemma":[0.9994287,0.00036776622,0.000046098332,0.00008876563,0.000026050293,0.00004262303],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040949282,0.000094951094,0.00011217247,0.000050595216,0.00009940333,0.00016350958,0.00020088503,0.000043055385,0.0006985276],"category_scores_gemma":[0.00010261552,0.000053095802,0.000029965582,0.00010668002,0.00003865506,0.00036536434,0.000008066608,0.00007043454,0.000114860406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000063386124,0.000008493262,0.9891218,0.000005860454,0.000007872406,8.80488e-7,0.0011173823,0.0066204276,0.0003490059,0.0011821262,0.001189215,0.00039057707],"study_design_scores_gemma":[0.00009375447,0.000023447981,0.99235976,0.0000048183597,0.000002976383,2.7869197e-7,0.00016674108,0.0021688675,0.0003265385,0.00046363668,0.004296909,0.00009224599],"about_ca_topic_score_codex":0.013964355,"about_ca_topic_score_gemma":0.008971955,"teacher_disagreement_score":0.0061033843,"about_ca_system_score_codex":0.0000019910283,"about_ca_system_score_gemma":0.00001933056,"threshold_uncertainty_score":0.99260175},"labels":[],"label_agreement":null},{"id":"W7087811712","doi":"10.5281/zenodo.17314023","title":"bilby-dev/bilby: v2.7.0rc0","year":2025,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Semtech (Canada); Canadian Institute for Theoretical Astrophysics","funders":"","keywords":"Waveform; JSON; Interface (matter); Float (project management); Extension (predicate logic); Generator (circuit theory); State (computer science); Filter (signal processing)","score_opus":0.018459519024718235,"score_gpt":0.21157399841956018,"score_spread":0.19311447939484194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7087811712","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00014479895,0.00039424867,0.00029782197,0.0002505578,0.00065634894,0.00044278218,0.0030511944,0.0010924595,0.9936698],"genre_scores_gemma":[0.023023473,0.00091899745,0.00048458664,0.00040112986,0.001620093,3.3303618e-8,0.017403603,0.0038431727,0.9523049],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99806845,0.00029684274,0.00024525478,0.00055554596,0.00039112664,0.00044277488],"domain_scores_gemma":[0.99887395,0.000025703994,0.00016248909,0.0005880584,0.00016810706,0.00018166442],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00040397848,0.00025475444,0.0003065898,0.00033963867,0.00090556627,0.0008244423,0.0012045507,0.0001848061,0.3202181],"category_scores_gemma":[0.00018272233,0.00023779993,0.00007319987,0.000417559,0.00013877095,0.000099701094,0.0003453383,0.0002425449,0.053529836],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001886293,0.00002614406,0.000004473611,0.00012797947,0.00006800935,0.000015208721,0.00007734814,0.000025031553,0.000107586246,0.0012040773,0.9478066,0.050518688],"study_design_scores_gemma":[0.00021870533,0.00009109549,0.00037230254,0.000094230905,0.000030727097,0.0000100068755,0.000027473528,0.000048060814,0.000053319687,0.0003048069,0.9984871,0.00026215918],"about_ca_topic_score_codex":0.0011187465,"about_ca_topic_score_gemma":0.000018742498,"teacher_disagreement_score":0.26668826,"about_ca_system_score_codex":0.000011932646,"about_ca_system_score_gemma":0.000011773499,"threshold_uncertainty_score":0.96971995},"labels":[],"label_agreement":null},{"id":"W7090618877","doi":"","title":"Patrimonialiser la culture selon l’UNESCO","year":2015,"lang":"fr","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Heritage","funders":"","keywords":"","score_opus":0.015519089614656839,"score_gpt":0.20848570867373248,"score_spread":0.19296661905907564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7090618877","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42501348,0.028834071,0.007816156,0.0433852,0.0047975937,0.0008775038,0.0013918661,0.00038101827,0.4875031],"genre_scores_gemma":[0.82001096,0.0025184704,0.0154989455,0.0002962827,0.00029888208,0.000010539472,0.0011264005,0.000034507742,0.16020498],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99129575,0.0066669947,0.00043351643,0.0005582924,0.0005148519,0.0005305931],"domain_scores_gemma":[0.99613583,0.00071999116,0.0002958717,0.0009972748,0.001340782,0.00051026716],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.004842838,0.00031951425,0.00036741977,0.00007663041,0.0003965053,0.0007074319,0.0008317023,0.00031383237,0.0008568118],"category_scores_gemma":[0.0007407315,0.0003030612,0.00014283553,0.0004634348,0.0003405013,0.00047304793,0.00017644648,0.0003092334,0.0018873337],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017174707,0.0017759565,0.034589037,0.0006374583,0.00039360605,0.00017126011,0.08024374,0.00090407796,0.011319273,0.29431584,0.3943852,0.1810928],"study_design_scores_gemma":[0.0008219857,0.0000019764698,0.008425414,0.0005865902,0.00008899954,0.000029783932,0.00034044098,0.0028042046,0.013804769,0.00565669,0.96692884,0.0005103113],"about_ca_topic_score_codex":0.021530978,"about_ca_topic_score_gemma":0.0066954633,"teacher_disagreement_score":0.5725436,"about_ca_system_score_codex":0.000021425374,"about_ca_system_score_gemma":0.00032487273,"threshold_uncertainty_score":0.9999421},"labels":[],"label_agreement":null},{"id":"W7093457063","doi":"","title":"In-situ Synchrotron XRPD&#13;\\n study of HP-induced phase transition in chabazite from Nova Scotia","year":2012,"lang":"en","type":"article","venue":"IRIS UNIMORE (University of Modena and Reggio Emilia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Chabazite; Phase transition; Phase (matter); Flattening; Synchrotron; Substructure; X-ray crystallography; Diffraction","score_opus":0.02054275507393045,"score_gpt":0.22500412947519374,"score_spread":0.2044613744012633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7093457063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99861187,0.00019840014,0.00006370743,0.00012116099,0.00018679138,0.0002793812,0.000117504285,0.000008652059,0.00041250925],"genre_scores_gemma":[0.99968344,0.00006272791,0.000093105664,0.000013955011,0.00004988414,5.6609426e-8,0.00006616284,0.0000032738399,0.000027397287],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990696,0.00011189556,0.00016955358,0.00022312407,0.00019356784,0.00023228842],"domain_scores_gemma":[0.9995328,0.000043235563,0.00011218372,0.00018111669,0.00003207127,0.0000985907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020906507,0.00012949368,0.00036076226,0.0001862212,0.00005105165,0.0000075442754,0.00016263557,0.00010106777,0.00021410164],"category_scores_gemma":[0.0000036121019,0.00013514457,0.000042705968,0.00021920327,0.00008308905,0.0004922045,0.000022567276,0.000102594786,0.000011833985],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026336664,0.0037414522,0.39767903,0.00034586937,0.00029405966,0.00026081983,0.12298568,0.0031395599,0.4500705,0.00011087191,0.0006876599,0.018050823],"study_design_scores_gemma":[0.0055623623,0.0006846018,0.97737193,0.00013539262,0.00011501038,0.0000027737733,0.009548143,0.0024165036,0.0034998208,0.00024055112,0.00011232103,0.0003105789],"about_ca_topic_score_codex":0.08210094,"about_ca_topic_score_gemma":0.05571336,"teacher_disagreement_score":0.5796929,"about_ca_system_score_codex":0.000005838502,"about_ca_system_score_gemma":0.000022595295,"threshold_uncertainty_score":0.9615174},"labels":[],"label_agreement":null},{"id":"W7096114792","doi":"","title":"Seismic structure of the crust and uppermost mantle of North America and adjacent oceanic basins: a synthesis, Bull. seism","year":2002,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Crust; Seafloor spreading; Oceanic crust; Precambrian; Continental crust; Mantle (geology); Paleozoic","score_opus":0.006310542292154717,"score_gpt":0.1588823876600409,"score_spread":0.15257184536788618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7096114792","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973732,0.00052563444,0.000007512127,0.00021457917,0.000107996784,0.00012377661,0.00083136273,0.000007305558,0.00080858386],"genre_scores_gemma":[0.9989311,0.00053000334,0.00012766062,0.00016074051,0.00002867455,2.1183529e-7,0.000008428254,0.0000028384293,0.00021034594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999357,0.00004663989,0.000165239,0.00015449619,0.00013604692,0.00014060979],"domain_scores_gemma":[0.99958014,0.00006971067,0.00010253332,0.00017375307,0.000021262047,0.000052596715],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000027541926,0.00010429797,0.00021086079,0.000021956883,0.00007117053,0.000020185304,0.00012526801,0.00003186807,0.0021659832],"category_scores_gemma":[0.000015858765,0.000060773684,0.000026858137,0.000094575895,0.00014364683,0.00005986299,0.000028238941,0.00004480128,0.00000877186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013022318,0.00015975346,0.76888716,0.000931587,0.00034052355,0.000011734901,0.002575066,0.0032803577,0.022436662,0.00034024986,0.014365406,0.18654126],"study_design_scores_gemma":[0.00013019869,0.00005899073,0.9781047,0.000029078858,0.000047436068,0.000009403386,0.00007448732,0.005741482,0.0047778236,0.00010086103,0.010805254,0.00012025206],"about_ca_topic_score_codex":0.0011972159,"about_ca_topic_score_gemma":0.00035206,"teacher_disagreement_score":0.20921756,"about_ca_system_score_codex":6.467904e-7,"about_ca_system_score_gemma":0.000009279709,"threshold_uncertainty_score":0.99874616},"labels":[],"label_agreement":null},{"id":"W7096666789","doi":"","title":"A mode-converted (P-SV) synthetic seismogram","year":2015,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Amplitude; Seismogram; Offset (computer science); Waveform; Computation; Reflection (computer programming); Synthetic seismogram; Synthetic data","score_opus":0.02082795440513821,"score_gpt":0.21842890806315604,"score_spread":0.19760095365801783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7096666789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89694834,0.000100904836,0.0007646702,0.00042325156,0.0011243159,0.0001829293,0.00008409422,0.00018165911,0.10018982],"genre_scores_gemma":[0.9965327,0.000004867526,0.0005124415,0.00030082415,0.000107309315,0.0000010045821,0.000056355904,0.0000027059793,0.0024818012],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99926615,0.000042306092,0.00011965743,0.00016891307,0.00017982625,0.00022314621],"domain_scores_gemma":[0.9995301,0.000029572395,0.000028305023,0.00018316026,0.000039176757,0.00018971559],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00015571833,0.000094383024,0.00013925572,0.000029082212,0.00004337918,0.000074462856,0.00015247554,0.00004427295,0.003137101],"category_scores_gemma":[0.000018854507,0.00006733432,0.000031935055,0.000090481306,0.00003400717,0.0001275507,0.000010173704,0.000037121004,0.0026416567],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008398349,0.00057309953,0.15736085,0.00025538492,0.0005993991,0.00037363393,0.006017491,0.04475524,0.0062375935,0.026415605,0.31448328,0.44208857],"study_design_scores_gemma":[0.0022827254,0.0007679363,0.059209485,0.000044463122,0.0001396019,0.000059683833,0.00051719794,0.26194254,0.008368037,0.052890155,0.61228836,0.0014898079],"about_ca_topic_score_codex":0.007391754,"about_ca_topic_score_gemma":0.00039775512,"teacher_disagreement_score":0.4405988,"about_ca_system_score_codex":0.0000010575451,"about_ca_system_score_gemma":0.000039992243,"threshold_uncertainty_score":0.9992181},"labels":[],"label_agreement":null},{"id":"W7096738371","doi":"","title":"Topography of Earth’s inner core boundary from high-quality waveform","year":2012,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Inner core; Waveform; Boundary (topology); Core (optical fiber); Rotation (mathematics); Earth's rotation; Reflection (computer programming)","score_opus":0.023989134332418754,"score_gpt":0.23799931670744523,"score_spread":0.21401018237502648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7096738371","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.980886,0.00022771602,0.000043983087,0.00005113738,0.0011190433,0.00008676541,0.0006237752,0.000033821412,0.016927795],"genre_scores_gemma":[0.9972373,0.000018699362,0.0014461611,0.00017684011,0.0003805382,5.8107605e-7,0.00035606127,0.0000027302885,0.00038106184],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99903315,0.000044822853,0.00026807596,0.00013915027,0.00022831159,0.00028649473],"domain_scores_gemma":[0.99940246,0.00008722237,0.00009892873,0.00024345952,0.000035732417,0.00013222307],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030467907,0.000113125374,0.00024300544,0.000040410327,0.00007734408,0.000034077668,0.00014972789,0.00006766206,0.012916296],"category_scores_gemma":[0.000010666383,0.00007827652,0.00007153784,0.00012108257,0.00009334908,0.00030269226,0.000018385226,0.000054562806,0.00033867522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009045336,0.00008984176,0.9596567,0.000043025626,0.00010746789,0.0000017029006,0.0005944474,0.000023594199,0.013109839,0.011783571,0.0018152238,0.012684147],"study_design_scores_gemma":[0.00016308652,0.000040759653,0.95974255,0.0000052601254,0.000015823567,3.5541268e-7,0.00005179214,0.000010457959,0.01037801,0.005595645,0.023860186,0.00013608883],"about_ca_topic_score_codex":0.029440023,"about_ca_topic_score_gemma":0.0016613799,"teacher_disagreement_score":0.027778642,"about_ca_system_score_codex":4.5082663e-7,"about_ca_system_score_gemma":0.000020166632,"threshold_uncertainty_score":0.987986},"labels":[],"label_agreement":null},{"id":"W7097522266","doi":"","title":"2009), Spatial variations of P wave attenuation in the mantle beneath North","year":2016,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismometer; Attenuation; Subduction; Amplitude; P wave; Tectonics; Mantle (geology); S-wave; Crust","score_opus":0.014929569962896443,"score_gpt":0.19177988936736534,"score_spread":0.1768503194044689,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097522266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99067754,0.000011205149,0.0021450394,0.00055707735,0.00017204272,0.00011394782,0.0002483575,0.0000061716387,0.00606863],"genre_scores_gemma":[0.9994014,0.000009331134,0.00017445967,0.000069371265,0.00008671608,8.7226994e-7,0.0000471494,7.482644e-7,0.0002099316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995566,0.000046085406,0.00011903018,0.000074150455,0.00011618761,0.00008795945],"domain_scores_gemma":[0.9997207,0.00009554115,0.000043057,0.00010704153,0.000019711346,0.0000139663525],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015756887,0.000040129464,0.00006484887,0.000023128094,0.000031214906,0.000012615647,0.00008158979,0.00001731656,0.002456043],"category_scores_gemma":[0.000014044426,0.000018268416,0.000015206593,0.000067917645,0.000015993608,0.00008335048,0.0000038644835,0.000013390657,0.00014535907],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007688198,0.00012560541,0.73407996,0.000027530059,0.000043857497,0.000011468478,0.0019416185,0.0016338902,0.0058260355,0.014291645,0.0058096545,0.23613186],"study_design_scores_gemma":[0.00012864596,0.000033441138,0.99562556,0.0000040293853,0.0000055040246,4.9611134e-7,0.0000118338885,0.0007905822,0.00039296504,0.0014474624,0.0015203648,0.000039126913],"about_ca_topic_score_codex":0.011122574,"about_ca_topic_score_gemma":0.02768777,"teacher_disagreement_score":0.2615456,"about_ca_system_score_codex":5.821599e-7,"about_ca_system_score_gemma":0.000015200945,"threshold_uncertainty_score":0.9984558},"labels":[],"label_agreement":null},{"id":"W7097534622","doi":"","title":"Anisotropy of the flexural response of the lithosphere","year":2004,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Bouguer anomaly; Anisotropy; Coherence (philosophical gambling strategy); Perpendicular; Tectonics; Shield; Lithospheric flexure","score_opus":0.0071255850032693096,"score_gpt":0.1907342163546337,"score_spread":0.18360863135136438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097534622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960294,0.00005551529,0.000014180748,0.00052640645,0.00036719686,0.000090815454,0.00005988159,0.0000059564672,0.0028506974],"genre_scores_gemma":[0.99830455,0.0000045555826,0.00039307307,0.00008529412,0.000027747086,1.7516321e-7,0.0000010822782,0.0000011159918,0.001182391],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9994688,0.000089387744,0.00012657091,0.00006801295,0.00015289911,0.00009433769],"domain_scores_gemma":[0.9995875,0.000047869027,0.000072713454,0.00024895454,0.00002413676,0.000018850193],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014239374,0.00005063859,0.000092343405,0.0000041244884,0.00005989903,0.000010011131,0.00028303664,0.00002498048,0.0012768762],"category_scores_gemma":[0.000027717871,0.000021286669,0.000059451973,0.00010656691,0.00009446394,0.000043278575,0.000021426806,0.00002927942,0.00002619617],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026914894,0.00020540139,0.43784118,0.00019009532,0.00017782787,0.000006890408,0.0038046504,0.037196387,0.4419391,0.0628901,0.005030426,0.008026469],"study_design_scores_gemma":[0.0001869743,0.00006589404,0.86382204,0.000016561191,0.000009921176,0.0000013795216,0.000059161597,0.000020780657,0.12760954,0.0058104927,0.0023510766,0.000046150595],"about_ca_topic_score_codex":0.0038277165,"about_ca_topic_score_gemma":0.0005877349,"teacher_disagreement_score":0.4259809,"about_ca_system_score_codex":8.2007745e-7,"about_ca_system_score_gemma":0.00006311638,"threshold_uncertainty_score":0.9996361},"labels":[],"label_agreement":null},{"id":"W7097712388","doi":"","title":"Modeling S wave amplitude patterns for events in the Kurile slab using three-dimensional Gaussian beams","year":2016,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Slab; Amplitude; Residual; Subduction; Seismometer; Hypocenter; Ray tracing (physics); Discontinuity (linguistics); Deep-focus earthquake","score_opus":0.04151133876854171,"score_gpt":0.2446094779922176,"score_spread":0.2030981392236759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097712388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9720303,0.000025034715,0.026646867,0.00030952916,0.00032880946,0.0002739844,0.0002073596,0.000012752982,0.0001653565],"genre_scores_gemma":[0.997893,0.0000024558074,0.0015865451,0.00020477596,0.00019341346,0.0000035721707,0.000044116077,0.000003643525,0.00006847592],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991055,0.00003985522,0.000183912,0.00020069299,0.00018794935,0.00028205363],"domain_scores_gemma":[0.9996226,0.00011450565,0.000033863285,0.00016435819,0.00002136643,0.000043326876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035083626,0.000104129074,0.00013094928,0.000029344605,0.00011133936,0.000030239511,0.00015636622,0.000041348412,0.0008374265],"category_scores_gemma":[0.000009808365,0.000048736332,0.000046146197,0.000042910844,0.000012942753,0.00015181534,0.000014443153,0.000029454177,0.000042892814],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008342116,0.00042150114,0.5207965,0.00028528323,0.0002989801,0.00006614555,0.0021393208,0.3403487,0.04257183,0.009754178,0.0011610369,0.08132237],"study_design_scores_gemma":[0.0017482007,0.00019741061,0.18475637,0.00021959622,0.00005081403,0.000017471864,0.00011323777,0.763144,0.0012996828,0.046591077,0.0012153101,0.00064680737],"about_ca_topic_score_codex":0.006412609,"about_ca_topic_score_gemma":0.005183986,"teacher_disagreement_score":0.42279536,"about_ca_system_score_codex":0.0000025411566,"about_ca_system_score_gemma":0.000025052095,"threshold_uncertainty_score":0.969399},"labels":[],"label_agreement":null},{"id":"W7100058583","doi":"","title":"Toronto, ON M5G 2N2, Canada • Inclusion in PubMed and all major indexing services • Maximum visibility for your research","year":2016,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Visibility; Search engine indexing; Inclusion (mineral); Order (exchange)","score_opus":0.035030536306167835,"score_gpt":0.2798983969201699,"score_spread":0.24486786061400204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7100058583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99377596,0.00012439639,0.000007096418,0.0007760065,0.0002768964,0.00048505064,0.0003129831,0.00001108033,0.0042305146],"genre_scores_gemma":[0.99873376,0.000032389467,0.00008807573,0.00028928995,0.000099372075,0.000010728097,0.00004277059,0.0000033165977,0.00070032635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99848384,0.0001411812,0.00018902884,0.0003331136,0.00037587134,0.00047695354],"domain_scores_gemma":[0.9991348,0.00042227854,0.000036318062,0.00019340715,0.00006288748,0.00015033274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001779506,0.00010233126,0.00016161136,0.000033533674,0.00021338167,0.000068313704,0.00023895255,0.0000619175,0.0006731466],"category_scores_gemma":[0.000053762564,0.000060537233,0.000012587982,0.00005992875,0.000029289906,0.00023911065,0.00017913552,0.0000472782,0.000007133212],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020049384,0.0001343871,0.5552628,0.00054431695,0.00008736833,0.00003235978,0.0019878838,0.00007407334,0.006041181,0.0010660164,0.0062979045,0.42646676],"study_design_scores_gemma":[0.000692789,0.00012537181,0.9715766,0.00003876799,0.0000039236543,4.919151e-7,0.00013620906,0.00025361186,0.0016840744,0.008854249,0.01646453,0.00016944093],"about_ca_topic_score_codex":0.9690619,"about_ca_topic_score_gemma":0.9962436,"teacher_disagreement_score":0.4262973,"about_ca_system_score_codex":0.000033214397,"about_ca_system_score_gemma":0.00011584784,"threshold_uncertainty_score":0.7370484},"labels":[],"label_agreement":null},{"id":"W7100124151","doi":"","title":"Toronto Hydro Energy Services","year":2006,"lang":"en","type":"article","venue":"","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Housekeeping; Work (physics); Service (business); Energy (signal processing)","score_opus":0.0027129122591220732,"score_gpt":0.16132608326187967,"score_spread":0.1586131710027576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7100124151","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46828362,0.0005497771,0.00006670751,0.000065934335,0.0004886556,0.000029715797,0.000044226756,0.000077216784,0.53039414],"genre_scores_gemma":[0.99299854,0.000019067302,0.00022405786,0.00022355064,0.00037164407,3.6850136e-7,0.00012722718,0.0000015014396,0.0060340553],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99951476,0.000015115188,0.00009355052,0.00011975304,0.00010119811,0.00015563524],"domain_scores_gemma":[0.9998059,0.000014772311,0.000023789118,0.00010689363,0.000010854467,0.00003774995],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000044336648,0.00006746721,0.000083331164,0.000006402653,0.000056942037,0.00006139473,0.00011380947,0.000028454102,0.0132518355],"category_scores_gemma":[2.573615e-7,0.00004871337,0.000021968734,0.000024462777,0.000010029424,0.00019169982,0.000005984677,0.000008652896,0.00030637838],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023876534,0.0003566889,0.2883696,0.0003586739,0.00022851651,0.00015619189,0.0006691405,0.01820746,0.054617632,0.3293947,0.1453662,0.16203643],"study_design_scores_gemma":[0.00021350784,0.00006665697,0.19474518,0.000006844046,0.000014705939,0.000003229652,0.00004993819,0.0031143231,0.007900323,0.013866306,0.77971363,0.0003053677],"about_ca_topic_score_codex":0.42131335,"about_ca_topic_score_gemma":0.23803093,"teacher_disagreement_score":0.6343474,"about_ca_system_score_codex":8.840641e-7,"about_ca_system_score_gemma":0.000006102893,"threshold_uncertainty_score":0.9876502},"labels":[],"label_agreement":null},{"id":"W7101433355","doi":"10.2139/ssrn.5654378","title":"&lt;p&gt;Petrology, Geochemistry, and U–Pb Zircon Geochronology of the Lalla Tittaf Magmatic Rocks (Rehamna Massif, Morocco): Implications for the Evolution of the South-Western Variscan Belt&lt;/p&gt;","year":2025,"lang":"","type":"preprint","venue":"SSRN Electronic Journal","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Zircon; Carboniferous; Metamorphism; Geochronology; Terrane; Craton; Gondwana; Mafic; Igneous rock; Basement","score_opus":0.006530892547177519,"score_gpt":0.2157984727459418,"score_spread":0.2092675801987643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7101433355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9050603,0.037435647,0.035559077,0.010816441,0.0035502575,0.0028309277,0.0030920077,0.000029467094,0.0016259073],"genre_scores_gemma":[0.99140537,0.0054609845,0.000094872885,0.000066470624,0.00053542457,0.00005310394,0.00006911657,0.000018609333,0.0022960457],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9947485,0.0005971319,0.0013777826,0.0007088944,0.00042074622,0.002146962],"domain_scores_gemma":[0.9951755,0.0006797041,0.0022768888,0.0013515402,0.00039837408,0.000118019525],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.002691495,0.00059484324,0.0009850744,0.0001278884,0.0012716996,0.0001397765,0.0024528846,0.0006212184,0.00016534864],"category_scores_gemma":[0.00020396918,0.00034916797,0.0005913634,0.00031936142,0.0008519678,0.000117276424,0.00064164033,0.0020204112,0.0000055034807],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018837882,0.0009583605,0.16435586,0.004090239,0.01308936,0.0000024023216,0.0052283276,0.06310475,0.5397706,0.15371063,0.002749392,0.051056307],"study_design_scores_gemma":[0.003084547,0.0011825595,0.37659445,0.0007453086,0.004449989,0.0006392222,0.0012155048,0.005545911,0.006006288,0.5891587,0.010168132,0.0012094014],"about_ca_topic_score_codex":0.0015751404,"about_ca_topic_score_gemma":0.01972847,"teacher_disagreement_score":0.5337643,"about_ca_system_score_codex":0.00024647446,"about_ca_system_score_gemma":0.0058605243,"threshold_uncertainty_score":0.99989605},"labels":[],"label_agreement":null},{"id":"W7102413631","doi":"10.1016/j.pepi.2025.107463","title":"The Earth’s magma ocean: Processes and current interpretations from an interdisciplinary perspective","year":2025,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle (geology); Magma; Context (archaeology); Early Earth; Volcanology; Silicate; Plate tectonics","score_opus":0.006964218271563493,"score_gpt":0.25323852348087705,"score_spread":0.24627430520931357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7102413631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920978,0.0036281743,0.00006683168,0.0007390616,0.0009875327,0.00023900936,0.0009477018,0.000020344149,0.0012735493],"genre_scores_gemma":[0.99910396,0.0003464828,0.00006808382,0.00008676939,0.00014093856,0.0000012260408,0.00014059962,0.0000035493083,0.00010837946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990598,0.000117856674,0.00022640076,0.00027043608,0.00013268446,0.0001928531],"domain_scores_gemma":[0.9991535,0.00030886332,0.00012127954,0.00027259678,0.00007290525,0.00007087856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112697984,0.0001783021,0.00022773072,0.000029347386,0.0004105371,0.00015053537,0.00033855144,0.000034155473,0.00006192193],"category_scores_gemma":[0.000031612766,0.00010491432,0.000048130638,0.00013102834,0.0003111588,0.00026442803,0.00013386544,0.000162173,0.00000911544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029206509,0.00041987133,0.46361634,0.0013640457,0.0017352168,0.000017709224,0.048561253,0.0038366348,0.0043724603,0.01323656,0.0042007035,0.45571855],"study_design_scores_gemma":[0.0005963758,0.00044246716,0.85458887,0.00067280565,0.0002697197,0.000008577202,0.00406496,0.008092746,0.0036466096,0.12084417,0.006267599,0.00050512113],"about_ca_topic_score_codex":0.0017160287,"about_ca_topic_score_gemma":0.0036891461,"teacher_disagreement_score":0.45521343,"about_ca_system_score_codex":0.0000011957613,"about_ca_system_score_gemma":0.0000660302,"threshold_uncertainty_score":0.42782816},"labels":[],"label_agreement":null},{"id":"W7105998365","doi":"10.7939/83411","title":"S receiver function imaging of lithospheric structure beneath Southwestern Canada","year":2025,"lang":"en","type":"dissertation","venue":"University of Alberta Library","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Craton; Precambrian; Lithosphere; Receiver function; Fibrous joint; Shear zone; Shear (geology)","score_opus":0.002431639961365265,"score_gpt":0.13671434397591856,"score_spread":0.13428270401455328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7105998365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9659352,0.00030016818,0.0000028125764,0.000045722358,0.0014262759,0.00010888668,0.00059902563,0.000010789267,0.031571165],"genre_scores_gemma":[0.9345146,0.000067483976,0.00019084384,0.000036363523,0.000052488922,1.4592423e-8,0.0073583727,0.0000055149017,0.057774357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992966,0.000038848608,0.00014372393,0.00022106267,0.00016689445,0.00013285925],"domain_scores_gemma":[0.99939984,0.00007993464,0.00024811804,0.00018052029,0.00003701245,0.000054590615],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000014628716,0.00015508196,0.0002976326,0.00005761214,0.00007978707,0.000017016728,0.00028215375,0.00010493931,0.0058118533],"category_scores_gemma":[0.0000043505984,0.00016401202,0.00006618337,0.00015093159,0.000022282962,0.00033871268,0.000017081122,0.000094315874,0.000004105691],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028637112,0.000070171205,0.86453253,0.00376186,0.001134647,0.00009431933,0.01232141,0.0043904125,0.000990882,0.0011473191,0.07328935,0.035403382],"study_design_scores_gemma":[0.0004397046,0.00006649819,0.9173875,0.00039591262,0.00037806516,7.58085e-7,0.0032736491,0.00030682966,0.001364778,0.000632635,0.07530767,0.00044601303],"about_ca_topic_score_codex":0.87840843,"about_ca_topic_score_gemma":0.88896376,"teacher_disagreement_score":0.052854955,"about_ca_system_score_codex":0.0000030449562,"about_ca_system_score_gemma":0.0006323623,"threshold_uncertainty_score":0.995097},"labels":[],"label_agreement":null},{"id":"W7113452556","doi":"","title":"Seismic heterogeneity and anisotropy in the Superios Province, Canada: Insights into the evolution of an Archaean craton","year":2002,"lang":"en","type":"book-chapter","venue":"Bristol Research (University of Bristol)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archean; Anisotropy; Craton; Seismic anisotropy","score_opus":0.020140547880621133,"score_gpt":0.20762757350076438,"score_spread":0.18748702562014324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7113452556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.982224,0.0020955992,0.00002931085,0.00035331643,0.00008288353,0.0007033052,0.000444379,0.000008465631,0.014058744],"genre_scores_gemma":[0.99392325,0.00055450347,0.00006078621,0.000016389191,0.00005344572,2.2993353e-7,0.00012058935,0.000007714533,0.0052630804],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976267,0.00043626814,0.00022455085,0.00041523718,0.0009774811,0.00031973884],"domain_scores_gemma":[0.99873054,0.00018884362,0.00019331244,0.0005422629,0.00021409612,0.00013092576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007577237,0.00019865367,0.0004087587,0.00022246581,0.00051249564,0.00003830179,0.0009667255,0.00016279584,0.00014411066],"category_scores_gemma":[0.000025478297,0.00015916482,0.00006790198,0.00014396863,0.0010541703,0.00021606995,0.0001296581,0.000455112,0.000009706141],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00829274,0.0018886116,0.09067553,0.010260577,0.0026521122,0.010553088,0.11252573,0.010050565,0.007975437,0.26118287,0.11870663,0.3652361],"study_design_scores_gemma":[0.0015274478,0.0017626522,0.29728687,0.00041707105,0.00016659775,0.000061538354,0.0062468904,0.015761608,0.00016175791,0.022053363,0.6534725,0.001081723],"about_ca_topic_score_codex":0.8974511,"about_ca_topic_score_gemma":0.96778375,"teacher_disagreement_score":0.53476584,"about_ca_system_score_codex":0.00010745811,"about_ca_system_score_gemma":0.00092441065,"threshold_uncertainty_score":0.6490553},"labels":[],"label_agreement":null},{"id":"W7116598230","doi":"","title":"Elastic behavior and high pressure-induced phase transition in chabazite: new data from a sample from Nova Scotia","year":2012,"lang":"en","type":"article","venue":"IRIS UNIMORE (University of Modena and Reggio Emilia)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sample (material); Nova scotia; Phase (matter); Phase transition; Work (physics)","score_opus":0.0436051571611307,"score_gpt":0.2390781851288773,"score_spread":0.1954730279677466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116598230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922047,0.0008663946,0.0015984019,0.00018991993,0.00023187831,0.00018681969,0.004660873,0.000017962251,0.000043002816],"genre_scores_gemma":[0.9959334,0.0001594552,0.0017945496,0.000020141393,0.00013470592,4.0547892e-8,0.0019113856,0.0000044752105,0.000041805197],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990521,0.00006799227,0.00012577156,0.0003452921,0.00017167925,0.00023716135],"domain_scores_gemma":[0.99922246,0.00012644826,0.000086946784,0.00032998298,0.000020885185,0.00021327531],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011748172,0.00014682522,0.00030741913,0.00008381557,0.00008943808,0.000025787336,0.0002660894,0.00012855379,0.0007815506],"category_scores_gemma":[0.0000116060555,0.00015204292,0.000025979127,0.00010909262,0.00010344122,0.00068280223,0.00006507357,0.00010335407,0.000015248518],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00454315,0.0019584242,0.5437424,0.0004497952,0.0010208251,0.00032937076,0.04915694,0.0014037978,0.21692541,0.00046962386,0.012204112,0.16779615],"study_design_scores_gemma":[0.0041003935,0.00019938384,0.97680485,0.00012081547,0.0005865547,0.000004204273,0.0010332444,0.013404585,0.0005903376,0.0009927166,0.0017235499,0.00043933332],"about_ca_topic_score_codex":0.27291137,"about_ca_topic_score_gemma":0.023664502,"teacher_disagreement_score":0.4330625,"about_ca_system_score_codex":0.0000025317956,"about_ca_system_score_gemma":0.000038528768,"threshold_uncertainty_score":0.99415106},"labels":[],"label_agreement":null},{"id":"W7116861021","doi":"10.1002/ctpp.70072","title":"A Study of the Electronic and Ionic Structure, for Competing States of Fully and Partially Ionized Hydrogen, Using the Neutral Pseudo‐Atom Method as Well as a Classical Map for the Electron Subsystem","year":2025,"lang":"en","type":"article","venue":"Contributions to Plasma Physics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; National Research Council Canada","funders":"","keywords":"Ionization; Thomson scattering; Warm dense matter; Electron; Ab initio; Ab initio quantum chemistry methods; Density functional theory; Measure (data warehouse); Monte Carlo method","score_opus":0.009458923874322548,"score_gpt":0.28135418347808056,"score_spread":0.271895259603758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116861021","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988139,0.0002630418,0.007790503,0.0006782826,0.00017288877,0.0021644703,0.00077083317,0.000010311734,0.000010694984],"genre_scores_gemma":[0.99950254,0.000010688872,0.00022169466,0.00006358788,0.00008929707,0.00003488958,0.00003757829,0.000005249587,0.0000344965],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99862874,0.00027687458,0.0003337837,0.00024179625,0.00013894607,0.00037985714],"domain_scores_gemma":[0.9978251,0.0014683413,0.0002066051,0.0002513953,0.00020496256,0.000043586526],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058192323,0.00016298365,0.00035772784,0.000023670022,0.0006467283,0.00009077986,0.00026076447,0.00005039971,0.0000058184187],"category_scores_gemma":[0.0000741408,0.00008924556,0.00008711613,0.00024220857,0.00010203668,0.00006129221,0.000048766142,0.000120925426,9.3206114e-7],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0041659265,0.0005350457,0.009823779,0.00064456015,0.0028006586,0.0000017853188,0.0046599433,0.2499832,0.1801417,0.5428447,0.0007282137,0.0036704408],"study_design_scores_gemma":[0.007964926,0.0028368381,0.009330902,0.0002099366,0.0026988217,0.000026503645,0.0029822853,0.3767958,0.42146325,0.16020586,0.014836308,0.00064858294],"about_ca_topic_score_codex":0.00060013373,"about_ca_topic_score_gemma":0.0017007319,"teacher_disagreement_score":0.38263887,"about_ca_system_score_codex":0.000012403292,"about_ca_system_score_gemma":0.00028040513,"threshold_uncertainty_score":0.49741766},"labels":[],"label_agreement":null},{"id":"W7117445735","doi":"","title":"A viable Labrador Sea rifting origin of the Northern Appalachian and related seismic anomalies","year":2025,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Continental margin; Rift; Anomaly (physics); Breakup; Asthenosphere; Seafloor spreading; Magnetic anomaly; Passive margin; Upwelling","score_opus":0.020263525977490787,"score_gpt":0.2862433370794003,"score_spread":0.2659798111019095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7117445735","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9828497,0.00023448902,0.00015110697,0.007485679,0.00046917883,0.0010791832,0.0051471256,0.000045334025,0.002538194],"genre_scores_gemma":[0.99359787,0.00004005241,0.00045772485,0.00013380064,0.000056423225,0.000018732346,0.001507216,0.0000049133205,0.0041832603],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975595,0.0002959751,0.0003763408,0.0005125183,0.0006325194,0.0006231636],"domain_scores_gemma":[0.9981318,0.00044829556,0.00017562919,0.0006087793,0.00048085925,0.00015463457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002730789,0.00013909115,0.00019325002,0.00027313348,0.00087035354,0.00034821834,0.0008674896,0.00006115647,0.0003931091],"category_scores_gemma":[0.0007015348,0.00009744236,0.00005248661,0.0015336543,0.0005192662,0.00070039555,0.00019138498,0.0001816614,0.00003798173],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015397144,0.00027960326,0.85417986,0.0009743254,0.0001241923,0.0000034587206,0.002498132,0.000528532,0.0033820786,0.037532855,0.05328467,0.04705833],"study_design_scores_gemma":[0.0009995098,0.00008364121,0.38822007,0.00018878619,0.000046307923,0.0000058394003,0.0008462063,0.076607876,0.0029573247,0.0075221574,0.52214426,0.00037801755],"about_ca_topic_score_codex":0.01342874,"about_ca_topic_score_gemma":0.006618832,"teacher_disagreement_score":0.4688596,"about_ca_system_score_codex":0.000011677108,"about_ca_system_score_gemma":0.0004272984,"threshold_uncertainty_score":0.99314094},"labels":[],"label_agreement":null},{"id":"W7118478401","doi":"10.5281/zenodo.18153016","title":"Relative Moment Tensors Rejuvenated","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Geological Survey of Canada; Carbon Management Canada","funders":"European Commission","keywords":"Amplitude; Moment (physics); Seismogram; Python (programming language); Waveform; Software; Algebraic number","score_opus":0.018138092625216706,"score_gpt":0.21828199822558703,"score_spread":0.20014390560037032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7118478401","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18617582,0.00020479466,0.0022779924,0.002578758,0.000534084,0.00069093105,0.00076211203,0.00091486983,0.80586064],"genre_scores_gemma":[0.99282783,0.000051954554,0.00017496408,0.00018915588,0.000065484805,8.491883e-9,0.001523262,0.000118413154,0.005048931],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99891895,0.0001864488,0.00017483415,0.00026891,0.00019713893,0.0002537172],"domain_scores_gemma":[0.99937236,0.000021422387,0.000058319616,0.00024534593,0.00021429699,0.00008823009],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004013664,0.00009595189,0.00012092477,0.00013652802,0.0012443031,0.00039263687,0.00048243816,0.000045094894,0.02501644],"category_scores_gemma":[0.00012833957,0.00008716584,0.000032045853,0.00043094176,0.000087584456,0.00019590753,0.00016290376,0.00012195603,0.008807612],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033647442,0.0001901376,0.0002661889,0.00016865028,0.00032906907,0.00005608811,0.002221503,0.0029274465,0.008351199,0.06540536,0.66859835,0.25114956],"study_design_scores_gemma":[0.000247011,0.00009299221,0.009664273,0.000023208488,0.000012912476,0.0000053306294,0.00008051959,0.00053342065,0.00049101736,0.0016211031,0.98712534,0.00010290388],"about_ca_topic_score_codex":0.00014506867,"about_ca_topic_score_gemma":0.0000015100301,"teacher_disagreement_score":0.806652,"about_ca_system_score_codex":0.000013651491,"about_ca_system_score_gemma":0.0000034128147,"threshold_uncertainty_score":0.99196416},"labels":[],"label_agreement":null},{"id":"W7118739408","doi":"10.5281/zenodo.18153017","title":"Relative Moment Tensors Rejuvenated","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Geological Survey of Canada; Carbon Management Canada","funders":"European Commission","keywords":"Amplitude; Moment (physics); Seismogram; Python (programming language); Waveform; Software; Algebraic number","score_opus":0.018138092625216706,"score_gpt":0.21828199822558703,"score_spread":0.20014390560037032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7118739408","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18617582,0.00020479466,0.0022779924,0.002578758,0.000534084,0.00069093105,0.00076211203,0.00091486983,0.80586064],"genre_scores_gemma":[0.99282783,0.000051954554,0.00017496408,0.00018915588,0.000065484805,8.491883e-9,0.001523262,0.000118413154,0.005048931],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99891895,0.0001864488,0.00017483415,0.00026891,0.00019713893,0.0002537172],"domain_scores_gemma":[0.99937236,0.000021422387,0.000058319616,0.00024534593,0.00021429699,0.00008823009],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0004013664,0.00009595189,0.00012092477,0.00013652802,0.0012443031,0.00039263687,0.00048243816,0.000045094894,0.02501644],"category_scores_gemma":[0.00012833957,0.00008716584,0.000032045853,0.00043094176,0.000087584456,0.00019590753,0.00016290376,0.00012195603,0.008807612],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033647442,0.0001901376,0.0002661889,0.00016865028,0.00032906907,0.00005608811,0.002221503,0.0029274465,0.008351199,0.06540536,0.66859835,0.25114956],"study_design_scores_gemma":[0.000247011,0.00009299221,0.009664273,0.000023208488,0.000012912476,0.0000053306294,0.00008051959,0.00053342065,0.00049101736,0.0016211031,0.98712534,0.00010290388],"about_ca_topic_score_codex":0.00014506867,"about_ca_topic_score_gemma":0.0000015100301,"teacher_disagreement_score":0.806652,"about_ca_system_score_codex":0.000013651491,"about_ca_system_score_gemma":0.0000034128147,"threshold_uncertainty_score":0.99196416},"labels":[],"label_agreement":null},{"id":"W7126545515","doi":"","title":"The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data.","year":2008,"lang":"en","type":"article","venue":"Research at the University of Copenhagen (University of Copenhagen)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Crust; Upper crust; Seismic refraction; Bouguer anomaly; Block (permutation group theory); Submarine pipeline; Refraction; Seismic velocity","score_opus":0.02750996610243557,"score_gpt":0.217908080164082,"score_spread":0.19039811406164642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7126545515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99036235,0.0015604821,0.000056343113,0.00038773598,0.00007583117,0.00047596951,0.0029105982,0.000006952105,0.004163722],"genre_scores_gemma":[0.95757234,0.00036898305,0.00017301922,0.0000069433327,0.000020751178,1.1068245e-8,0.0001061179,0.0000043183386,0.041747488],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99779195,0.00075478625,0.00016442178,0.000305633,0.0007094891,0.00027372048],"domain_scores_gemma":[0.9979333,0.00057905336,0.0003640525,0.0007881331,0.0002467669,0.00008868676],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007086642,0.00012972581,0.00031444154,0.000052142066,0.0014539455,0.00001955441,0.0018370542,0.00009593685,0.044191074],"category_scores_gemma":[0.000059389087,0.00009076163,0.00008184249,0.00033947921,0.0018087379,0.00041641743,0.0007185562,0.00021942069,0.0008545814],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004511766,0.00014218247,0.0011229177,0.0003663387,0.0009341825,0.00011210562,0.025466543,0.0016705138,0.11076339,0.00011083165,0.83369887,0.02110036],"study_design_scores_gemma":[0.002026517,0.00048200184,0.32746524,0.00015652993,0.00028749363,0.0000175397,0.050069574,0.0032749323,0.025188446,0.00016296114,0.5904806,0.00038812004],"about_ca_topic_score_codex":0.053463053,"about_ca_topic_score_gemma":0.026509982,"teacher_disagreement_score":0.3263423,"about_ca_system_score_codex":0.000017258692,"about_ca_system_score_gemma":0.00034105906,"threshold_uncertainty_score":0.99992335},"labels":[],"label_agreement":null},{"id":"W7132870221","doi":"","title":"The solution behaviour of siderophile elements during earth differentiation: An experimental study","year":2007,"lang":"","type":"dissertation","venue":"TSpace","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bank of Canada; University of Toronto","funders":"","keywords":"Mineral redox buffer; Silicate; Outer core; Trace element; Oxygen; Metal; Earth (classical element); Impurity; Liquid metal","score_opus":0.02094034538189379,"score_gpt":0.31815521021108645,"score_spread":0.2972148648291927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7132870221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99500364,0.0006694677,0.000006135484,0.000012419707,0.002558552,0.001143873,0.00008232702,0.000024689576,0.0004988808],"genre_scores_gemma":[0.9947999,0.00008317367,0.000048770762,0.0000036522292,0.00039131043,0.000015344358,0.0011982649,0.000019122666,0.003440463],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9968434,0.0003173397,0.00081868214,0.0005521755,0.0009000647,0.0005683386],"domain_scores_gemma":[0.9982598,0.00006968691,0.00082122744,0.00052219053,0.00015242724,0.00017465567],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005974495,0.00042096272,0.00046998222,0.00010989376,0.0011760567,0.00026008883,0.00043947418,0.0001782156,0.0026705954],"category_scores_gemma":[0.000014407498,0.0003342803,0.00012206094,0.0001859544,0.000078409495,0.00028434774,0.00004112628,0.00020878734,0.000076675715],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0034734162,0.0061073047,0.30397666,0.00041456422,0.000820776,0.00007281565,0.11931458,0.0008585393,0.5610249,0.00015222134,0.000111468784,0.003672753],"study_design_scores_gemma":[0.0009899694,0.0016495703,0.7908479,0.000061095496,0.00021238092,0.0000016444977,0.04368288,0.00024442922,0.16179505,0.000019723528,0.00007244176,0.00042290078],"about_ca_topic_score_codex":0.005995279,"about_ca_topic_score_gemma":0.0069869473,"teacher_disagreement_score":0.48687124,"about_ca_system_score_codex":0.000010277676,"about_ca_system_score_gemma":0.00007756361,"threshold_uncertainty_score":0.99991095},"labels":[],"label_agreement":null},{"id":"W7132935241","doi":"","title":"Convection in earth&apos;s mantle: Impacts of solid-solid phase transformations and crystalline rheology","year":2001,"lang":"en","type":"dissertation","venue":"TSpace","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto","keywords":"Convection; Péclet number; Boundary layer; Mass flux; Heat flux; Convective heat transfer; Thermal; Endothermic process; Natural convection","score_opus":0.016487784966199563,"score_gpt":0.34593782200386153,"score_spread":0.32945003703766196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7132935241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916999,0.0005208831,0.000103848404,0.000072417715,0.0004417545,0.00029220214,0.00030896216,0.000019795089,0.006540263],"genre_scores_gemma":[0.990425,0.0013265776,0.00006499387,0.000019670819,0.00008934748,0.0000028421396,0.0027756225,0.000006721754,0.0052892324],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9990226,0.000064914464,0.00034168074,0.00019025631,0.00013772787,0.00024281476],"domain_scores_gemma":[0.99948823,0.000053681404,0.00019764337,0.00011953458,0.000056642682,0.000084243155],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017580156,0.00017948823,0.00040184145,0.00017445892,0.00006128932,0.000025532843,0.00008402757,0.00019923426,0.0021093797],"category_scores_gemma":[0.0000181082,0.00016625295,0.00004207801,0.00016401072,0.000041634827,0.0001531288,0.0000025263412,0.00013526854,0.000035613608],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.010017724,0.0019553609,0.012421767,0.009823209,0.001243411,0.0004680919,0.16474319,0.015557154,0.6642815,0.005153038,0.006743989,0.107591555],"study_design_scores_gemma":[0.02627663,0.007843937,0.49004936,0.0027811625,0.0014994451,0.00035490454,0.027080083,0.051916137,0.29738015,0.0130991265,0.076219335,0.0054997094],"about_ca_topic_score_codex":0.0057230885,"about_ca_topic_score_gemma":0.026785308,"teacher_disagreement_score":0.4776276,"about_ca_system_score_codex":0.0000019800493,"about_ca_system_score_gemma":0.000072101575,"threshold_uncertainty_score":0.99880284},"labels":[],"label_agreement":null},{"id":"W7132978415","doi":"","title":"Development of New Methods to Control Redox Conditions in High-pressure Experiments and their Application to Study Ore Metal Solubilities in Sulfur-bearing Magmatic Fluids","year":2021,"lang":"","type":"dissertation","venue":"TSpace","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Hydrogen; Silicate; Redox; Saturation (graph theory); Metal; Analytical Chemistry (journal); Alloy; Bar (unit); Argon; Partition coefficient","score_opus":0.022758849984046627,"score_gpt":0.3358657232135456,"score_spread":0.3131068732294989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7132978415","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99144155,0.0013423177,0.0033358946,0.00009488132,0.00051304285,0.0029641292,0.00013491993,0.00001639142,0.00015687407],"genre_scores_gemma":[0.9733652,0.00002178028,0.024449043,0.000039559494,0.00006449222,0.00025899766,0.000675256,0.000021620755,0.0011040599],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99645436,0.0006507469,0.0011341701,0.00087239733,0.0003865687,0.00050177926],"domain_scores_gemma":[0.99845344,0.00032253095,0.00030195608,0.0004912511,0.00013814658,0.00029265496],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.001319448,0.00052107335,0.0013078606,0.0004074419,0.00019312669,0.00015247194,0.00037023582,0.00020426723,0.0008862544],"category_scores_gemma":[0.00013532258,0.0004916968,0.00006398719,0.00063723593,0.000037115835,0.00018440712,0.000093570954,0.00020630748,0.000022700604],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046220093,0.0005093796,0.006244324,0.0006320695,0.00055247906,0.000009075026,0.42937145,0.0053324103,0.53939307,0.00020954682,0.000047223955,0.01723674],"study_design_scores_gemma":[0.0029402482,0.0005289857,0.42465082,0.00073202857,0.00032379295,0.000002155741,0.2913275,0.0011364868,0.27542564,0.0006777793,0.0011020795,0.001152473],"about_ca_topic_score_codex":0.015370157,"about_ca_topic_score_gemma":0.013876386,"teacher_disagreement_score":0.41840652,"about_ca_system_score_codex":0.000019181498,"about_ca_system_score_gemma":0.00039046496,"threshold_uncertainty_score":0.9997535},"labels":[],"label_agreement":null},{"id":"W7143582907","doi":"","title":"Abschlussbericht SO294 - CLOCKS: Die Cascadia Subduktionszone vor Vancouver Island: Ausdehnung der seismogenen Zone, Bruchverhalten an der Deformationsfront, und nördliche Begrenzung der Subduktion - Förderkennzeichen: 03G0294A BMBF","year":2025,"lang":"en","type":"book","venue":"Helmholtz Centre for Ocean Research Kiel (GEOMAR)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Context (archaeology); Field (mathematics); Interpretation (philosophy); Identification (biology)","score_opus":0.02600687586247801,"score_gpt":0.29306703363747827,"score_spread":0.26706015777500025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7143582907","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07827332,0.10478549,0.048105344,0.009739899,0.039647166,0.049605947,0.1033141,0.0039745164,0.56255424],"genre_scores_gemma":[0.02169575,0.0027852326,0.004328802,0.0009414549,0.0038805848,0.000119435506,0.028820071,0.00024623188,0.9371824],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99038553,0.0008683459,0.0016229317,0.0019801988,0.0021959185,0.00294709],"domain_scores_gemma":[0.99349135,0.0014602332,0.0006329483,0.0018555445,0.0013921709,0.0011677743],"candidate_categories":["metaepi_narrow","sts","scholarly_communication","research_integrity","insufficient_payload"],"consensus_categories":["metaepi_narrow"],"category_scores_codex":[0.0027704444,0.0013227711,0.0015201061,0.0011758542,0.0020378327,0.0010895673,0.0018939445,0.0013643744,0.0028490003],"category_scores_gemma":[0.00036910485,0.0011961889,0.00062672707,0.0007067431,0.00045438667,0.0016234828,0.00037754286,0.0014679873,0.00069734664],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057123165,0.0003344585,0.0033407437,0.0017596927,0.0019628538,0.00021338052,0.0013181578,0.0022531203,0.000063528714,0.0014192818,0.9764489,0.01031465],"study_design_scores_gemma":[0.0021842674,0.0003805382,0.0041417237,0.0005133846,0.00091169984,0.000023035022,0.0003395514,0.006893734,0.00035411463,0.0067873304,0.9757353,0.0017352964],"about_ca_topic_score_codex":0.0065307673,"about_ca_topic_score_gemma":0.052392777,"teacher_disagreement_score":0.37462822,"about_ca_system_score_codex":0.0003257595,"about_ca_system_score_gemma":0.0026937858,"threshold_uncertainty_score":0.9999524},"labels":[],"label_agreement":null},{"id":"W7164921626","doi":"10.5281/zenodo.20715474","title":"D2.1 - Report on solid-state phase transition and transformation as a function of temperature","year":2024,"lang":"","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Safran Electronics (Canada)","funders":"European Commission","keywords":"Transformation (genetics); Function (biology); Phase transition; Phase (matter); Work (physics)","score_opus":0.016576187130332747,"score_gpt":0.2427544150987972,"score_spread":0.22617822796846446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7164921626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96545,0.0006411549,0.0016155966,0.0012912698,0.00092089374,0.00091040885,0.0027294357,0.00039928293,0.026041975],"genre_scores_gemma":[0.9931084,0.0006797447,0.000015136319,0.00008384508,0.0002276352,2.9446937e-8,0.0051405043,0.00026364246,0.00048109054],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977786,0.00035385237,0.00052800466,0.0005189273,0.00049222156,0.0003283725],"domain_scores_gemma":[0.9990689,0.00003348194,0.00012709909,0.00027779862,0.00029546945,0.00019725507],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010232809,0.00022281404,0.00025797894,0.00029226037,0.0012653716,0.0014169514,0.00025362766,0.00011953733,0.013882594],"category_scores_gemma":[0.00008017557,0.00021098509,0.00007827851,0.00052431074,0.00014218847,0.0007529035,0.000050048402,0.00028740283,0.0025003674],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002778901,0.0005510181,9.073173e-7,0.002718435,0.00048019647,0.00045841318,0.021190854,0.0033919779,0.26120165,0.007035756,0.038087998,0.6621039],"study_design_scores_gemma":[0.001218973,0.0036073932,0.00051045086,0.0004558853,0.00017509647,0.0005274614,0.0004905051,0.007502798,0.010863087,0.0014926561,0.9727575,0.00039815434],"about_ca_topic_score_codex":0.00008635246,"about_ca_topic_score_gemma":0.0000013942656,"teacher_disagreement_score":0.93466955,"about_ca_system_score_codex":0.000017521428,"about_ca_system_score_gemma":0.00001406129,"threshold_uncertainty_score":0.99961966},"labels":[],"label_agreement":null},{"id":"W7164967665","doi":"10.5281/zenodo.20715475","title":"D2.1 - Report on solid-state phase transition and transformation as a function of temperature","year":2024,"lang":"","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Safran Electronics (Canada)","funders":"European Commission","keywords":"Transformation (genetics); Function (biology); Phase transition; Phase (matter); Work (physics)","score_opus":0.016576187130332747,"score_gpt":0.2427544150987972,"score_spread":0.22617822796846446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7164967665","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96545,0.0006411549,0.0016155966,0.0012912698,0.00092089374,0.00091040885,0.0027294357,0.00039928293,0.026041975],"genre_scores_gemma":[0.9931084,0.0006797447,0.000015136319,0.00008384508,0.0002276352,2.9446937e-8,0.0051405043,0.00026364246,0.00048109054],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977786,0.00035385237,0.00052800466,0.0005189273,0.00049222156,0.0003283725],"domain_scores_gemma":[0.9990689,0.00003348194,0.00012709909,0.00027779862,0.00029546945,0.00019725507],"candidate_categories":["scholarly_communication","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010232809,0.00022281404,0.00025797894,0.00029226037,0.0012653716,0.0014169514,0.00025362766,0.00011953733,0.013882594],"category_scores_gemma":[0.00008017557,0.00021098509,0.00007827851,0.00052431074,0.00014218847,0.0007529035,0.000050048402,0.00028740283,0.0025003674],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002778901,0.0005510181,9.073173e-7,0.002718435,0.00048019647,0.00045841318,0.021190854,0.0033919779,0.26120165,0.007035756,0.038087998,0.6621039],"study_design_scores_gemma":[0.001218973,0.0036073932,0.00051045086,0.0004558853,0.00017509647,0.0005274614,0.0004905051,0.007502798,0.010863087,0.0014926561,0.9727575,0.00039815434],"about_ca_topic_score_codex":0.00008635246,"about_ca_topic_score_gemma":0.0000013942656,"teacher_disagreement_score":0.93466955,"about_ca_system_score_codex":0.000017521428,"about_ca_system_score_gemma":0.00001406129,"threshold_uncertainty_score":0.99961966},"labels":[],"label_agreement":null},{"id":"W83403527","doi":"10.1023/a:1017999626693","title":"Lateral stress measurements in a shock loaded alumina: Shear strength and delayed failure","year":2001,"lang":"en","type":"article","venue":"Journal of Materials Science","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Military College of Canada","funders":"","keywords":"Manganin; Materials science; Brittleness; Silicon carbide; Composite material; Shock (circulatory); Stress (linguistics); Solid mechanics; Grain boundary; Front (military); Microstructure; Acceleration; Geology","score_opus":0.017586162679748357,"score_gpt":0.22901158875330258,"score_spread":0.21142542607355422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W83403527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99851596,0.00012565467,0.000007866557,0.00018186345,0.0008534606,0.00009675824,0.000057248468,0.000006164243,0.00015501361],"genre_scores_gemma":[0.9989507,0.000060163413,0.0007028007,0.00004774427,0.00020168099,3.539623e-7,0.0000039576335,0.0000031017673,0.000029448742],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9981546,0.00011092296,0.0005089482,0.00021051469,0.0006318768,0.00038315143],"domain_scores_gemma":[0.999222,0.00003830823,0.00029383972,0.0001295596,0.00013370995,0.00018261225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016004975,0.00014143788,0.00032710432,0.00019266612,0.00012927156,0.0003630944,0.00040936653,0.000048711652,0.0006885699],"category_scores_gemma":[0.00008075213,0.000102915,0.000025905074,0.0002772895,0.00019309513,0.00086663896,0.0000344305,0.00007956828,0.000021721557],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035478914,0.00007533655,0.083477154,0.00003706787,0.000021145437,0.00014209065,0.0006437378,0.0009353289,0.9125821,0.000032320768,0.00018790262,0.0015110062],"study_design_scores_gemma":[0.0014025937,0.00057985156,0.59403,0.00021696654,0.000036303645,0.0002933314,0.0002531549,0.00014973666,0.40104964,0.00067646476,0.0009575529,0.00035440823],"about_ca_topic_score_codex":0.0007912365,"about_ca_topic_score_gemma":0.00038509868,"teacher_disagreement_score":0.5115325,"about_ca_system_score_codex":0.000009947956,"about_ca_system_score_gemma":0.00012960276,"threshold_uncertainty_score":0.75393575},"labels":[],"label_agreement":null},{"id":"W940326584","doi":"10.1007/978-1-4614-9616-8_3","title":"Normalization Analysis for Possibly-Unstable Triple Junction Zones","year":2014,"lang":"en","type":"book-chapter","venue":"SpringerBriefs in earth sciences","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nova Scotia Department of Energy","funders":"","keywords":"Normalization (sociology); Triple junction; Geology; Geometry; Mathematics; Sociology; Geophysics","score_opus":0.019397170290660175,"score_gpt":0.21883106786284656,"score_spread":0.19943389757218638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W940326584","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05933146,0.002680945,0.038571194,0.00038609855,0.010268621,0.0026716627,0.00093012647,0.0003245888,0.8848353],"genre_scores_gemma":[0.629321,0.0006736661,0.0073519666,0.00032874823,0.0016625283,0.000018280733,0.0009789614,0.000033098822,0.3596318],"study_design_codex":"simulation_or_modeling","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977637,0.000037603273,0.00051582296,0.0006940186,0.0005213082,0.0004675552],"domain_scores_gemma":[0.9990081,0.00013449267,0.0003651162,0.00028974863,0.00009804988,0.000104455234],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0012642632,0.0003073109,0.0006058125,0.00065609603,0.00039040318,0.00032444173,0.00040869202,0.00021344508,0.0022352845],"category_scores_gemma":[0.00004946675,0.0002642642,0.00021524337,0.00044966306,0.00026550848,0.00031820763,0.000027354097,0.0001174704,0.00016343468],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036449727,0.00007277889,0.16122891,0.00082761986,0.0010194313,0.000023347733,0.0008951797,0.38910997,0.00030806425,0.3802088,0.0020042427,0.063937165],"study_design_scores_gemma":[0.0009023086,0.00076527026,0.14010283,0.0002686725,0.0008104171,0.000004397231,0.000040707167,0.049847785,0.0005707901,0.043291815,0.7616736,0.0017213855],"about_ca_topic_score_codex":0.0026636356,"about_ca_topic_score_gemma":0.015706794,"teacher_disagreement_score":0.75966936,"about_ca_system_score_codex":0.0000038757903,"about_ca_system_score_gemma":0.00012185634,"threshold_uncertainty_score":0.999981},"labels":[],"label_agreement":null},{"id":"W96580940","doi":"","title":"Equation of state experiments in extreme magnetic fields","year":2004,"lang":"en","type":"paratext","venue":"OSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information)","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Douglas College","funders":"","keywords":"Isentropic process; Explosive material; Microsecond; Equation of state; Pulsed power; Mechanics; Capacitor; Compression (physics); Physics; Voltage; Computational physics; Power (physics); Thermodynamics; Optics; Chemistry","score_opus":0.024365091531374,"score_gpt":0.22704694583840304,"score_spread":0.20268185430702904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W96580940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.74398875,0.0027330867,0.002520595,0.00008980298,0.0032864923,0.0008611735,0.0037444008,0.00003428032,0.24274142],"genre_scores_gemma":[0.99010813,0.000301149,0.00074757147,0.000022546297,0.000020691432,0.000007924242,0.007132427,0.000003552601,0.0016559822],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9979836,0.000039959636,0.0009835893,0.00022303066,0.00053715444,0.00023270164],"domain_scores_gemma":[0.99874437,0.00008639895,0.0006454734,0.00028026945,0.00016236567,0.00008111719],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037326882,0.00020555526,0.0004659492,0.00032854712,0.00006477928,0.000069513386,0.00027781146,0.00019045304,0.001990927],"category_scores_gemma":[0.000032469496,0.00018016067,0.00007447421,0.00032942928,0.00032696666,0.0005069009,0.00005682353,0.00009081543,0.000111738875],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005945511,0.0062661255,0.015522722,0.017555472,0.0012037192,0.000048479465,0.0010797753,0.37436765,0.04858854,0.071022004,0.25373507,0.20466493],"study_design_scores_gemma":[0.007664401,0.005116269,0.44589454,0.0035749124,0.00039432535,0.000025997027,0.000073344985,0.0008397719,0.13441296,0.008959836,0.38985327,0.0031903898],"about_ca_topic_score_codex":0.0015924529,"about_ca_topic_score_gemma":0.00030419137,"teacher_disagreement_score":0.4303718,"about_ca_system_score_codex":0.000009461909,"about_ca_system_score_gemma":0.00018139461,"threshold_uncertainty_score":0.9989214},"labels":[],"label_agreement":null}]}