{"meta":{"query_hash":"9de789315c64","filters":{"venue":"Journal of Metamorphic Geology"},"cohort_total":146,"direct_labels_cover":0,"predictions_cover":146,"exported":146,"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/9de789315c64","api":"https://metacan.xera.ac/api/v1/cohort?venue=Journal+of+Metamorphic+Geology"},"results":[{"id":"W1497274899","doi":"10.1111/j.1525-1314.2011.00933.x","title":"Garnet growth during crustal thickening in the Cascades Crystalline Core, Washington, USA","year":2011,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Laurentian University","funders":"","keywords":"Geology; Batholith; Geochemistry; Pluton; Metamorphism; Gneiss; Plutonism; Metamorphic rock; Petrology; Schist; Tectonics; Seismology","score_opus":0.04376679083399094,"score_gpt":0.21212684692813602,"score_spread":0.1683600560941451,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1497274899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99581194,0.00007702232,0.000022721204,0.000037306312,0.0000017054447,0.000006671834,0.00080626225,0.000006905497,0.0032295887],"genre_scores_gemma":[0.9959812,0.00020830944,0.00010681465,0.000021443453,0.0000021618098,0.000005766377,0.001084915,0.0000034714583,0.002585996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999691,0.0000014929177,0.0000020358727,0.000010869886,0.000009345136,0.000007232996],"domain_scores_gemma":[0.99991906,0.0000057770035,0.000022523152,0.000003952912,0.000030801504,0.000017904387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057366473,0.00014150348,0.000050874547,0.00065744,0.00050154247,0.00025942377,0.00015055017,0.00009881189,0.0013921665],"category_scores_gemma":[0.00013951935,0.000112672686,0.000051368435,0.00047373513,0.00013104928,0.00020236624,0.00022766074,0.00013513443,0.00016506293],"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":[0.00012444904,0.000051378578,0.96287096,0.000031055697,0.00004364437,0.0004511615,0.0011122508,0.0001946949,0.015452665,0.00011891964,0.0014299954,0.018118884],"study_design_scores_gemma":[0.000001289722,0.000006337871,0.9977889,0.0000074504446,0.000005472582,0.00003030714,0.000319177,0.00011589993,0.00072342023,0.000009973962,0.0009907082,0.0000010836089],"about_ca_topic_score_codex":0.38668776,"about_ca_topic_score_gemma":0.8393493,"teacher_disagreement_score":0.38668776,"about_ca_system_score_codex":0.0014138779,"about_ca_system_score_gemma":0.0005855483,"threshold_uncertainty_score":0.76887393},"labels":[],"label_agreement":null},{"id":"W1503780069","doi":"10.1111/jmg.12067","title":"A new thermodynamic model for sapphirine: calculated phase equilibria in K<sub>2</sub>O–FeO–MgO–Al<sub>2</sub>O<sub>3</sub>–SiO<sub>2</sub>–H<sub>2</sub>O–TiO<sub>2</sub>–Fe<sub>2</sub>O<sub>3</sub>","year":2013,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":84,"is_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":"Granulite; Quartz; Geology; Metamorphism; Metamorphic rock; Thermodynamics; Phase (matter); Context (archaeology); Phase diagram; Mineralogy; Geochemistry; Chemistry; Physics","score_opus":0.015700020598415652,"score_gpt":0.22608878555244813,"score_spread":0.21038876495403247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1503780069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8427632,0.00013401805,0.13453667,0.0001426642,0.000016158227,0.00010408898,0.0010383888,0.0004702442,0.020794531],"genre_scores_gemma":[0.9857334,0.00007524149,0.011628153,0.000013811572,0.0000036072338,0.00007865189,0.0002748676,0.00006111545,0.0021310945],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999959,0.000005373329,0.000002360733,0.000009467703,0.000017493152,0.0000062361205],"domain_scores_gemma":[0.99993575,0.000018755953,0.0000067296946,0.000008688896,0.000023503955,0.0000066770563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013672127,0.00028129504,0.0003074504,0.0003073698,0.0004583618,0.00052706606,0.0009642444,0.00056236703,0.0020156903],"category_scores_gemma":[0.00037008338,0.00026794584,0.0002703892,0.00033298437,0.00034241797,0.00064742356,0.00025787533,0.00024244077,0.00028795013],"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":[0.00003276147,0.000025312189,0.002897871,0.00004661773,0.000011126635,0.00010723004,0.000063552296,0.9736582,0.016132958,0.0033201184,0.0002291089,0.0034750914],"study_design_scores_gemma":[0.000009323816,0.000008804835,0.00093094003,0.0000028232694,0.000003430616,0.000019232535,0.0000193505,0.9957639,0.0021817402,0.00053251965,0.0005241172,0.000003837684],"about_ca_topic_score_codex":0.03747595,"about_ca_topic_score_gemma":0.04040821,"teacher_disagreement_score":0.03747595,"about_ca_system_score_codex":0.0011102934,"about_ca_system_score_gemma":0.0011807323,"threshold_uncertainty_score":0.07451564},"labels":[],"label_agreement":null},{"id":"W1505164167","doi":"10.1046/j.1525-1314.2003.00439.x","title":"Measurement and correlation of microstructures: the case of foliation intersection axes","year":2003,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geophysical Studies Worldwide","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 British Columbia","funders":"","keywords":"Geology; Intersection (aeronautics); Correlation; Orientation (vector space); Foliation (geology); Schist; Data set; Geometry; Statistics; Mathematics; Petrology; Cartography; Geography; Metamorphic rock","score_opus":0.01616474350102563,"score_gpt":0.20068561481189803,"score_spread":0.18452087131087241,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1505164167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9726093,0.00021829801,0.025227057,0.000024018611,0.000006551017,0.000032576023,0.0002864989,0.00012487118,0.0014706976],"genre_scores_gemma":[0.9946807,0.000033622677,0.0050615002,0.0000021257745,0.0000024151966,0.000013666016,0.00012640283,0.000009175769,0.000070396854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869376,0.00036686228,0.00013467939,0.00033367053,0.0003384532,0.00013256405],"domain_scores_gemma":[0.993244,0.002506741,0.0016892464,0.00090566074,0.0015038045,0.00015046427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026717414,0.00031011458,0.00030453198,0.0031917333,0.0004721689,0.0008807317,0.0003000185,0.00028554816,0.00095625565],"category_scores_gemma":[0.008627208,0.0002997632,0.0002483951,0.0019823236,0.0008096845,0.0006112908,0.00058103015,0.00029577402,0.00013974024],"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":[0.0003391527,0.000032497468,0.84849995,0.00012743798,0.00012591975,0.0002425762,0.0006830972,0.008448981,0.10615368,0.001381647,0.0001761731,0.033788968],"study_design_scores_gemma":[0.00000574276,0.000115248346,0.94290924,0.00001608698,0.00004910191,0.00035364638,0.00023095513,0.033042327,0.021831645,0.00072592014,0.0006813875,0.000038631202],"about_ca_topic_score_codex":0.008457351,"about_ca_topic_score_gemma":0.012193851,"teacher_disagreement_score":0.008457351,"about_ca_system_score_codex":0.0006589775,"about_ca_system_score_gemma":0.00042448178,"threshold_uncertainty_score":0.016816258},"labels":[],"label_agreement":null},{"id":"W1514715288","doi":"10.1111/jmg.12015","title":"Short‐duration contact metamorphism of calcareous sedimentary rocks by Neoproterozoic Franklin gabbro sills and dykes on Victoria Island, Canada","year":2012,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"McGill University; Geological Survey of Canada","funders":"","keywords":"Geology; Metamorphism; Sill; Geochemistry; Massif; Protolith; Gabbro; Igneous rock; Petrology","score_opus":0.0072967460811029046,"score_gpt":0.18561198185070643,"score_spread":0.17831523576960354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1514715288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988588,0.00009215661,0.000019378645,0.000009784601,6.683667e-7,0.000003916915,0.00021050061,0.0000033894196,0.0008014035],"genre_scores_gemma":[0.9988537,0.00008093376,0.00005090709,0.000005288058,5.0582463e-7,0.0000020810328,0.00022070136,0.0000021560013,0.0007837818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998155,0.0000062413533,0.000008427921,0.000037580277,0.000057130866,0.00007511516],"domain_scores_gemma":[0.99969006,0.000011009028,0.00004854762,0.0000091388765,0.00015107107,0.00009020478],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013361289,0.00024049103,0.00018551455,0.0016984215,0.001966549,0.00088123913,0.00043085415,0.00020899666,0.0012192468],"category_scores_gemma":[0.00032400744,0.0002571366,0.00016971391,0.0012114916,0.00054380024,0.0001970572,0.00072232995,0.00018144076,0.00020409783],"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":[0.00014834038,0.000015825206,0.96641344,0.0000434706,0.000046843303,0.00037398151,0.0032925021,0.00026933616,0.019876758,0.00012167679,0.00023055432,0.009167308],"study_design_scores_gemma":[9.081498e-7,0.0000060034104,0.9982765,0.000005661291,0.000004103884,0.00003174817,0.00088004913,0.000096207856,0.00028824218,0.0000040080145,0.00040465832,0.0000020484722],"about_ca_topic_score_codex":0.94030493,"about_ca_topic_score_gemma":0.9873942,"teacher_disagreement_score":0.059695065,"about_ca_system_score_codex":0.008983908,"about_ca_system_score_gemma":0.0045027747,"threshold_uncertainty_score":0.12009317},"labels":[],"label_agreement":null},{"id":"W1520252426","doi":"10.1046/j.0263-4929.2000.00300.x","title":"Metamorphism at a late Mesozoic accretionary margin: a study from the Coast Belt of the North American Cordillera","year":2001,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Batholith; Metamorphic rock; Geochemistry; Mesozoic; Subduction; Metamorphic core complex; Doming; Back-arc basin; Paleontology; Geomorphology; Tectonics; Extensional definition","score_opus":0.015976762672612298,"score_gpt":0.20119647626743598,"score_spread":0.18521971359482367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1520252426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994747,0.00008602642,0.000012519258,0.000010161142,8.728893e-7,0.0000053456574,0.00008215942,0.0000017150819,0.00032648473],"genre_scores_gemma":[0.9989993,0.00015019179,0.000108657405,0.000017221882,0.0000042037414,0.000008646049,0.000295422,0.0000021266987,0.0004143592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987423,0.0000120567865,0.000009620734,0.000038856033,0.000026527903,0.00003858624],"domain_scores_gemma":[0.9996296,0.000022834582,0.00010266056,0.000019234056,0.00014010466,0.000085589556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016465689,0.00032060774,0.00026205988,0.0021633522,0.0013391828,0.00066962896,0.0004288629,0.00038269465,0.0013206946],"category_scores_gemma":[0.00036965217,0.000206528,0.00017230817,0.0018749965,0.00040924392,0.00028380382,0.0005506444,0.00017296,0.00032617166],"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":[0.00007865401,0.000041137406,0.9882366,0.000029633551,0.000022810369,0.0006355392,0.0025486916,0.000025623407,0.002793298,0.000024694838,0.00007654041,0.0054867635],"study_design_scores_gemma":[8.1536035e-7,0.000014132417,0.9990722,0.0000036692845,0.0000028723196,0.00008893475,0.00055667304,0.000026086745,0.00005549135,0.0000023281568,0.00017606126,7.571246e-7],"about_ca_topic_score_codex":0.25999203,"about_ca_topic_score_gemma":0.48919794,"teacher_disagreement_score":0.740008,"about_ca_system_score_codex":0.0014420259,"about_ca_system_score_gemma":0.00072961417,"threshold_uncertainty_score":0.5169574},"labels":[],"label_agreement":null},{"id":"W1522340574","doi":"10.1046/j.1525-1314.2002.00407.x","title":"Numerical simulations of spiral‐shaped inclusion trails: can 3D geometry distinguish between end‐member models of spiral formation?","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"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":"Japan Society for the Promotion of Science; Shizuoka University; Canadian Imperial Bank of Commerce","keywords":"Spiral (railway); Foliation (geology); Geometry; Rotation (mathematics); Curvature; Smoothness; Geology; Principal curvature; Mathematics; Paleontology; Mathematical analysis","score_opus":0.049185305699795887,"score_gpt":0.2404672178320717,"score_spread":0.1912819121322758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1522340574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877951,0.00004947859,0.0077082193,0.00016558394,0.000013850018,0.00003157549,0.00029988124,0.00008540545,0.0038508342],"genre_scores_gemma":[0.99592847,0.000033062428,0.003584699,0.000016962447,0.0000020624188,0.000025882164,0.000117261094,0.000017875775,0.00027381486],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985325,0.00004066442,0.000011304989,0.000018337214,0.000041022773,0.00003543122],"domain_scores_gemma":[0.99875224,0.00075860537,0.00012168851,0.00013000592,0.00014089308,0.00009667284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004962698,0.00025891227,0.00050676323,0.00039342104,0.00047169568,0.0008180486,0.0007117464,0.00093621726,0.0016764652],"category_scores_gemma":[0.0030402015,0.00029865038,0.0004290602,0.00041615838,0.00082431175,0.000558551,0.00046971312,0.0003876675,0.00014161902],"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":[0.000069564485,0.000040875355,0.0058378126,0.000022793865,0.000012085659,0.000068543486,0.0000865196,0.98977506,0.0012240793,0.0016351609,0.000086761196,0.0011407356],"study_design_scores_gemma":[0.000018412096,0.000019448571,0.00077009515,0.0000043926384,0.0000030924293,0.000009492968,0.000040829782,0.99805874,0.00043995984,0.0004826022,0.00014678529,0.0000062071026],"about_ca_topic_score_codex":0.013105863,"about_ca_topic_score_gemma":0.0076059485,"teacher_disagreement_score":0.013105863,"about_ca_system_score_codex":0.0007915398,"about_ca_system_score_gemma":0.00067540404,"threshold_uncertainty_score":0.02605915},"labels":[],"label_agreement":null},{"id":"W1537067100","doi":"10.1046/j.1525-1314.2003.00436.x","title":"Large‐scale melt‐depletion in granulite terranes: an example from the Archean Ashuanipi Subprovince of Quebec","year":2003,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":161,"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 Chicoutimi","funders":"","keywords":"Geology; Granulite; Geochemistry; Terrane; Biotite; Anatexis; Protolith; Archean; Plagioclase; Partial melting; Outcrop; Migmatite; Petrology; Facies; Quartz; Basalt; Metamorphic rock; Gneiss; Geomorphology; Tectonics","score_opus":0.02772210122942013,"score_gpt":0.21068921865593127,"score_spread":0.18296711742651114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1537067100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948397,0.0001850635,0.00015914965,0.000071157534,0.0000024696758,0.000027270746,0.00094974885,0.00001935252,0.00374605],"genre_scores_gemma":[0.9970214,0.00010610037,0.00034233552,0.000039476578,0.00000202082,0.0000072507473,0.0007534029,0.0000073398705,0.0017206286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998597,0.000007120568,0.000004171126,0.000029933231,0.000041581166,0.00005749858],"domain_scores_gemma":[0.9997329,0.000021832326,0.000033246666,0.000012733178,0.00014232541,0.0000569937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010868414,0.00026695468,0.00021938368,0.0015403954,0.0022430527,0.0008157891,0.00057953247,0.00029259518,0.001986039],"category_scores_gemma":[0.00029618153,0.00016440384,0.00017064418,0.0022429554,0.00058158755,0.00019647992,0.00035606994,0.00027244564,0.00016712333],"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":[0.0001912992,0.00008591863,0.94147086,0.00008635499,0.000115615396,0.0026577646,0.005280885,0.00095838564,0.015401264,0.00046811416,0.0017310525,0.0315524],"study_design_scores_gemma":[0.0000061567857,0.000014768571,0.9934182,0.000013147973,0.000013565283,0.00024705796,0.002033618,0.0006622133,0.00055289717,0.000024164128,0.003004763,0.000009487342],"about_ca_topic_score_codex":0.9845812,"about_ca_topic_score_gemma":0.9957995,"teacher_disagreement_score":0.0154188275,"about_ca_system_score_codex":0.009124663,"about_ca_system_score_gemma":0.0044011073,"threshold_uncertainty_score":0.06620437},"labels":[],"label_agreement":null},{"id":"W1537134122","doi":"10.1111/j.1525-1314.2010.00902.x","title":"Episodic growth of zircon in UHP orthogneisses from the North Dabie Terrane of east‐central China: implications for crustal architecture of a collisional orogen","year":2010,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Geological Survey of Canada","funders":"Chinese Academy of Geological Sciences; China University of Geosciences; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Zircon; Protolith; Geology; Terrane; Metamorphism; Geochemistry; Subduction; Plagioclase; Mantle (geology); Eclogite; Petrology; Seismology; Paleontology; Quartz; Tectonics","score_opus":0.013469992126410516,"score_gpt":0.20977462011831868,"score_spread":0.19630462799190818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1537134122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994286,0.00006237162,0.00003560796,0.000004527869,7.441307e-7,0.0000021415162,0.000077717705,0.0000019283602,0.00038633595],"genre_scores_gemma":[0.9994136,0.000053115364,0.000061992054,0.0000043450973,0.0000011366884,0.0000021702015,0.00015993079,0.000001702514,0.00030185256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999144,0.000003972719,0.000007170678,0.000030467869,0.000019198005,0.000024832596],"domain_scores_gemma":[0.9999074,0.0000070767405,0.000025078194,0.000008838825,0.00003180025,0.000019787769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017996038,0.00029838513,0.00030226365,0.0014188173,0.0006792422,0.0005735447,0.0002518998,0.0002228889,0.00061429135],"category_scores_gemma":[0.00015738688,0.00023800033,0.00015585004,0.000984783,0.00037660988,0.00015828371,0.00043271438,0.000110816,0.00012605415],"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":[0.00016713512,0.00001960306,0.8968173,0.00004789191,0.00005418719,0.00041216976,0.0011562002,0.00022429143,0.09351493,0.000114385904,0.00004672119,0.0074250824],"study_design_scores_gemma":[0.000001793507,0.000010845587,0.99873525,0.0000012798513,0.000005846393,0.00004570964,0.00018494634,0.00007731697,0.00074306334,0.0000049266514,0.00018772755,0.0000013306291],"about_ca_topic_score_codex":0.05977246,"about_ca_topic_score_gemma":0.09961699,"teacher_disagreement_score":0.05977246,"about_ca_system_score_codex":0.00071164966,"about_ca_system_score_gemma":0.00037099406,"threshold_uncertainty_score":0.1188491},"labels":[],"label_agreement":null},{"id":"W1543336708","doi":"10.1111/jmg.12168","title":"CONSONORM_HG: a new method of norm calculation for mid‐ to high‐grade metamorphic rocks","year":2015,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Université du Québec à Chicoutimi","funders":"Canada Economic Development for Quebec Regions; Ministère de l'Énergie et des Ressources Naturelles","keywords":"Metamorphic rock; Greenschist; Geology; Geochemistry; Metamorphic facies; Silicate; Mineralogy; Carbonate; Silicate minerals; Protolith; Petrography; Mineral; Quartz; Facies; Chemistry; Materials science; Metallurgy; Geomorphology","score_opus":0.049440352797685445,"score_gpt":0.27815570662794,"score_spread":0.22871535383025454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1543336708","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009370546,0.00011524792,0.9705239,0.00004997448,0.00012621563,0.00010861951,0.0015494089,0.013196153,0.0049600075],"genre_scores_gemma":[0.040374905,0.00006952745,0.9499218,0.00003838861,0.00002898664,0.00022829525,0.003035479,0.0031355605,0.0031670863],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9973853,0.00041406753,0.00032722153,0.00058913784,0.0011417266,0.00014253159],"domain_scores_gemma":[0.9970673,0.00048019507,0.00031927667,0.0004948266,0.001545134,0.00009334031],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026967558,0.0014057531,0.0007619304,0.0033920396,0.00073317555,0.0023725778,0.0021505265,0.0007565392,0.011770869],"category_scores_gemma":[0.007868878,0.00064665644,0.0010224034,0.0025708913,0.0007997893,0.0013918133,0.0018419675,0.0012141446,0.0049643763],"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":[0.0003145956,0.0001151547,0.010578544,0.00055447244,0.00013793232,0.0001945048,0.00036866727,0.025922459,0.05334186,0.02834158,0.034993447,0.8451367],"study_design_scores_gemma":[0.00010731844,0.00025261345,0.020804357,0.00016497754,0.00009239991,0.0009068107,0.0003852604,0.61173236,0.13467483,0.03159729,0.19899246,0.000289273],"about_ca_topic_score_codex":0.0041875057,"about_ca_topic_score_gemma":0.00511265,"teacher_disagreement_score":0.011770869,"about_ca_system_score_codex":0.0009026853,"about_ca_system_score_gemma":0.0016979753,"threshold_uncertainty_score":0.03937751},"labels":[],"label_agreement":null},{"id":"W1579112697","doi":"10.1046/j.0263-4929.2001.00323.x","title":"Chromium and manganese zoning in pelitic garnet and kyanite: Spiral, overprint, and oscillatory (?) zoning patterns and the role of growth rate","year":2001,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Kyanite; Geology; Metamorphic facies; Pelite; Metamorphic rock; Zoning; Geochemistry; Chlorite; Quartz; Mineralogy; Facies; Geomorphology; Paleontology","score_opus":0.006187140128742341,"score_gpt":0.17593641972780613,"score_spread":0.1697492795990638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1579112697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942964,0.000070070215,0.000093234834,0.000003891971,4.0264462e-7,0.000002580638,0.00010658034,0.000011576398,0.00028201885],"genre_scores_gemma":[0.99924386,0.000034783243,0.00016474255,0.0000023544642,5.9924633e-7,0.0000037304392,0.00015298615,0.000008211824,0.00038879167],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992704,0.000005400586,0.0000068602526,0.00002538491,0.000012535356,0.000022786744],"domain_scores_gemma":[0.99976414,0.000036715373,0.00007089584,0.000018058165,0.00006745402,0.000042670017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010770023,0.00017908585,0.00021015984,0.0012301556,0.00016518668,0.0004285445,0.0001924962,0.00019982952,0.0008754114],"category_scores_gemma":[0.00023476708,0.00024613334,0.00014583713,0.0004891379,0.00032543272,0.00017574054,0.00023901706,0.00007596363,0.00015210248],"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":[0.00062566984,0.000017770406,0.18239442,0.000058826823,0.000027720118,0.00014458479,0.00028266647,0.00042034796,0.810881,0.000116252835,0.00002724495,0.0050034523],"study_design_scores_gemma":[0.00000714368,0.000065382614,0.9696796,0.0000031908198,0.000012452467,0.00018549425,0.00015039199,0.0008912266,0.028641045,0.000036552676,0.0003205637,0.0000068886416],"about_ca_topic_score_codex":0.014692757,"about_ca_topic_score_gemma":0.023100156,"teacher_disagreement_score":0.014692757,"about_ca_system_score_codex":0.00045237943,"about_ca_system_score_gemma":0.0002014466,"threshold_uncertainty_score":0.029214442},"labels":[],"label_agreement":null},{"id":"W1584063203","doi":"10.1111/j.1525-1314.2012.00975.x","title":"Major element distribution in Archean banded iron formation (BIF): influence of metamorphic differentiation","year":2012,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Queen's University","funders":"","keywords":"Metamorphic rock; Amphibole; Geology; Metamorphism; Banded iron formation; Archean; Geochemistry; Hornblende; Metamorphic facies; Greenstone belt; Quartz; Facies; Geomorphology; Biotite; Paleontology","score_opus":0.014211785172100143,"score_gpt":0.20850143807856455,"score_spread":0.1942896529064644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1584063203","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992047,0.00009171498,0.000041656855,0.0000055346513,5.0900945e-7,0.0000019298063,0.00021565452,0.0000049594364,0.0004334105],"genre_scores_gemma":[0.99948454,0.000027704591,0.000057295038,0.0000026190448,3.0077433e-7,9.4862116e-7,0.00018816245,0.0000019976794,0.00023639084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998894,0.000007990881,0.000006825844,0.00003384348,0.000027054804,0.00003492298],"domain_scores_gemma":[0.99977857,0.000015246187,0.00003763139,0.000009170786,0.00012192199,0.000037489186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014999179,0.00016005088,0.00014958259,0.0017647041,0.00040155393,0.00051047123,0.00022662143,0.00020670057,0.0009965455],"category_scores_gemma":[0.00038635352,0.00013876204,0.00010085066,0.0006588032,0.00036004232,0.0001507832,0.00026009715,0.0001171841,0.0001319448],"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":[0.00045188447,0.000017436041,0.953019,0.000024384637,0.000037710906,0.000109510234,0.00016226832,0.00063157105,0.04003464,0.00013085865,0.00009602736,0.0052847858],"study_design_scores_gemma":[0.0000027543415,0.000014888665,0.99777836,0.0000023596951,0.0000061913847,0.000050485334,0.00010369227,0.0005105346,0.001285263,0.000018035451,0.00022546733,0.0000018392896],"about_ca_topic_score_codex":0.31172392,"about_ca_topic_score_gemma":0.3726133,"teacher_disagreement_score":0.31172392,"about_ca_system_score_codex":0.001922405,"about_ca_system_score_gemma":0.00050847145,"threshold_uncertainty_score":0.6198189},"labels":[],"label_agreement":null},{"id":"W1584393996","doi":"10.1111/j.1525-1314.2010.00913.x","title":"Initiation and development of the Twelve Mile Bay shear zone: the low viscosity sole of a granulite nappe","year":2010,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Western University; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Geological Society of America; National Science Foundation","keywords":"Granulite; Geology; Shear zone; Geochemistry; Pegmatite; Nappe; Metamorphism; Shear (geology); Mylonite; Pyroxene; Metamorphic facies; Petrology; Geomorphology; Facies; Tectonics; Seismology","score_opus":0.010159477136424415,"score_gpt":0.18991150906148097,"score_spread":0.17975203192505654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1584393996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891055,0.000030641124,0.0001735456,0.0000058302803,6.733417e-7,0.000006329228,0.000048465557,0.000009598555,0.00081442075],"genre_scores_gemma":[0.9989491,0.00002625158,0.0003150203,0.00000663811,7.0571355e-7,0.0000043419554,0.00008740985,0.0000032444036,0.0006073363],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.0000022435736,0.0000026927426,0.000020293379,0.0000132634,0.000011995083],"domain_scores_gemma":[0.9999213,0.000005271041,0.000032008018,0.0000075325734,0.000012900873,0.000020938547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006999895,0.00018422338,0.00011176206,0.00041471128,0.000267592,0.00041480322,0.00016921735,0.00019697906,0.0009473568],"category_scores_gemma":[0.00018679824,0.00022730327,0.000116182724,0.00018068097,0.00055155496,0.00016248909,0.00052607927,0.00022905417,0.00022690573],"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":[0.00031190395,0.000028798338,0.27677757,0.000073411604,0.000018754454,0.0009888146,0.0010086566,0.000504159,0.7089099,0.0005995067,0.000075412405,0.010703045],"study_design_scores_gemma":[0.0000062696226,0.00007883456,0.9850611,0.000005397387,0.000004808279,0.00030309273,0.00021681606,0.00030035456,0.0131188985,0.00005877755,0.000841738,0.0000039028077],"about_ca_topic_score_codex":0.013484504,"about_ca_topic_score_gemma":0.020568147,"teacher_disagreement_score":0.013484504,"about_ca_system_score_codex":0.00037991896,"about_ca_system_score_gemma":0.00028147802,"threshold_uncertainty_score":0.026812017},"labels":[],"label_agreement":null},{"id":"W1588936869","doi":"10.1111/j.1525-1314.2010.00926.x","title":"Metamorphic evolution of sapphirine- and orthoamphibole-cordierite-bearing gneiss, Okanogan dome, Washington, USA","year":2011,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_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; Kyanite; Migmatite; Gneiss; Metamorphic rock; Geochemistry; Staurolite; Andalusite; Cordierite; Petrology","score_opus":0.023540630038340556,"score_gpt":0.19604737233921388,"score_spread":0.17250674230087332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1588936869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973726,0.00012880447,0.000020749187,0.000013723297,0.0000014495374,0.0000040945883,0.00046873555,0.0000056405333,0.0019841685],"genre_scores_gemma":[0.9975375,0.00012690871,0.00010987885,0.000010610979,7.892012e-7,0.00000394397,0.00073342986,0.000003197823,0.0014735779],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999409,0.0000029105136,0.000005494751,0.000024451609,0.0000106007265,0.000015658821],"domain_scores_gemma":[0.9998654,0.000005400315,0.00002765226,0.000005431159,0.000059573067,0.000036503283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008682467,0.00025574322,0.00010082239,0.0011763049,0.0006082124,0.0005984409,0.00021271325,0.00018579939,0.001248459],"category_scores_gemma":[0.00014573424,0.00016078711,0.00009874333,0.00081599015,0.00029965746,0.00019936914,0.00034384517,0.00015573714,0.00027087194],"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":[0.00010565667,0.000023350603,0.9732242,0.000025546686,0.000052347707,0.0002542006,0.00066255894,0.00020695156,0.01621181,0.00008391892,0.000366418,0.008782964],"study_design_scores_gemma":[7.515371e-7,0.0000036335841,0.99909496,0.0000026824684,0.000003951481,0.000025461333,0.00024647618,0.00005378426,0.00022593026,0.000002306917,0.00033933183,8.380621e-7],"about_ca_topic_score_codex":0.45027965,"about_ca_topic_score_gemma":0.80062777,"teacher_disagreement_score":0.45027965,"about_ca_system_score_codex":0.00216838,"about_ca_system_score_gemma":0.00067763746,"threshold_uncertainty_score":0.89531744},"labels":[],"label_agreement":null},{"id":"W1589807587","doi":"10.1111/j.1525-1314.2012.00972.x","title":"Trace element systematics in granulite facies rutile: implications for Zr geothermometry and provenance studies","year":2012,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":114,"is_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":"Granulite; Rutile; Geology; Geochemistry; Trace element; Mineralogy; Provenance; Facies; Zircon","score_opus":0.048949810826377095,"score_gpt":0.27631173000013654,"score_spread":0.22736191917375945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1589807587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980628,0.00015675231,0.0007856329,0.000010885478,7.6800615e-7,0.00001260192,0.0002669169,0.000025533947,0.000678011],"genre_scores_gemma":[0.9987029,0.00006618097,0.0007348202,0.000006406254,5.678877e-7,0.000005654276,0.00023218429,0.000012914975,0.00023830797],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997831,0.00003393454,0.000016064432,0.000070726936,0.00005208372,0.00004412063],"domain_scores_gemma":[0.9994574,0.00008909496,0.00013760466,0.00008452986,0.00020106813,0.000030206493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043613228,0.0002470743,0.00032968377,0.0017049569,0.000377039,0.00048182902,0.0004966221,0.00020034959,0.00083799375],"category_scores_gemma":[0.00079516176,0.0001909848,0.00019448258,0.0010789823,0.00062080676,0.00019258799,0.0004373065,0.00012881929,0.00018037303],"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":[0.00033932755,0.000018590395,0.79373634,0.000108487366,0.0001055614,0.00032900297,0.001377879,0.0007906082,0.18534923,0.00023312744,0.00005328613,0.017558577],"study_design_scores_gemma":[0.0000030590193,0.00003372608,0.99227303,0.000008253069,0.000020574484,0.00014522522,0.0003306182,0.00035884537,0.006375912,0.00003655562,0.00040993607,0.0000042334646],"about_ca_topic_score_codex":0.1606486,"about_ca_topic_score_gemma":0.26819378,"teacher_disagreement_score":0.1606486,"about_ca_system_score_codex":0.0011437355,"about_ca_system_score_gemma":0.00056999916,"threshold_uncertainty_score":0.319427},"labels":[],"label_agreement":null},{"id":"W1596863264","doi":"10.1111/j.1525-1314.2012.00979.x","title":"Coupled role of deformation and metamorphism in the construction of inverted metamorphic sequences: an example from far‐northwest Nepal","year":2012,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":92,"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; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphic rock; Metamorphism; Kyanite; Sillimanite; Shear zone; Main Central Thrust; Metamorphic core complex; Gneiss; Schist; Foreland basin; Migmatite; Geothermobarometry; Shearing (physics); Geochemistry; Petrology; Quartz; Tectonics; Seismology; Paleontology; Biotite; Extensional definition; Geotechnical engineering","score_opus":0.02681775859813567,"score_gpt":0.20234153540643254,"score_spread":0.17552377680829687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1596863264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99715,0.000048314203,0.00028111783,0.000023703864,4.3839142e-7,0.0000048947695,0.000033741235,0.0000045379097,0.0024532387],"genre_scores_gemma":[0.9994579,0.000029645065,0.0002559351,0.0000067240157,5.9686374e-7,0.0000018200357,0.000032832595,0.0000016544042,0.00021288096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999298,0.000014461016,0.0000052994324,0.00001944883,0.000015157876,0.000015928277],"domain_scores_gemma":[0.99985695,0.00004209528,0.000028752953,0.000017215509,0.000039989176,0.000014934345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009675039,0.00013844999,0.0001262607,0.0006295713,0.0006805806,0.0006989977,0.00031307008,0.00025471143,0.0010896968],"category_scores_gemma":[0.0005007156,0.00015033945,0.00010969713,0.0007755772,0.00075652834,0.00026656376,0.00059208914,0.00024312365,0.00012580257],"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":[0.00030205137,0.00007968587,0.80993503,0.00032980109,0.00018451101,0.016626982,0.015303166,0.0074352943,0.090118185,0.0048308913,0.00028269883,0.05457169],"study_design_scores_gemma":[0.000011313137,0.000049545553,0.98145974,0.000028566676,0.00003740451,0.0024416088,0.0037742646,0.006007469,0.0032157395,0.0010768302,0.0018763362,0.000021091224],"about_ca_topic_score_codex":0.022624185,"about_ca_topic_score_gemma":0.0386399,"teacher_disagreement_score":0.022624185,"about_ca_system_score_codex":0.00043951557,"about_ca_system_score_gemma":0.00029654006,"threshold_uncertainty_score":0.044984996},"labels":[],"label_agreement":null},{"id":"W1598473770","doi":"10.1111/j.1525-1314.2011.00954.x","title":"Stability of sapphirine + quartz in the oxidized rocks of the Wilson Lake terrane, Labrador: calculated equilibria in NCKFMASHTO","year":2011,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Graduate School, University of Minnesota; Geological Society of America; U.S. Department of Education","keywords":"Quartz; Geology; Terrane; Metamorphism; Feldspar; Biotite; Mineralogy; Geochemistry","score_opus":0.035029160543929926,"score_gpt":0.20647750024537134,"score_spread":0.1714483397014414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1598473770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990274,0.000029684337,0.000057369907,0.000005046917,3.810109e-7,0.000003481053,0.00026775847,0.000010200995,0.00059864536],"genre_scores_gemma":[0.9995171,0.000020416477,0.000084165746,0.0000025721383,5.111068e-7,0.0000030329547,0.00023580974,0.0000046682894,0.00013173708],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998776,0.0000072562652,0.000007741127,0.000039090355,0.0000358264,0.00003249496],"domain_scores_gemma":[0.9999052,0.000019307072,0.000017644594,0.0000073957067,0.00003541796,0.000015020798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001463008,0.00022181404,0.00018532362,0.00067850493,0.00065065926,0.0005513072,0.0006118375,0.00028552717,0.0021036412],"category_scores_gemma":[0.0003691977,0.00020764617,0.00014546103,0.00051173934,0.00033109926,0.00037191177,0.00025171638,0.00018194508,0.0002307046],"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":[0.0015039941,0.00018561666,0.52489656,0.00035168655,0.00034170636,0.0011489487,0.0010598828,0.0312609,0.41940343,0.0011059257,0.00074854976,0.01799272],"study_design_scores_gemma":[0.00008453412,0.0002650914,0.87392384,0.000020391422,0.00007348361,0.00018751119,0.001048439,0.04254494,0.079357065,0.00023013362,0.002225325,0.00003926548],"about_ca_topic_score_codex":0.15561378,"about_ca_topic_score_gemma":0.1845318,"teacher_disagreement_score":0.8443862,"about_ca_system_score_codex":0.0015489764,"about_ca_system_score_gemma":0.00036142874,"threshold_uncertainty_score":0.309416},"labels":[],"label_agreement":null},{"id":"W1607860939","doi":"10.1111/j.1525-1314.2010.00873.x","title":"Diachronous Palaeoproterozoic deformation and metamorphism in the Committee Bay belt, Rae Province, Nunavut: insights from <sup>40</sup>Ar–<sup>39</sup>Ar cooling ages and thermal modelling","year":2010,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of Manitoba; Government of Newfoundland and Labrador; Geological Survey of Canada","funders":"","keywords":"Geology; Monazite; Migmatite; Hornblende; Archean; Geochemistry; Metamorphism; Metamorphic facies; Metamorphic rock; Biotite; Diachronous; Schist; Radiogenic nuclide; Craton; Tectonics; Geomorphology; Gneiss; Zircon; Facies; Paleontology; Quartz; Mantle (geology)","score_opus":0.011036179861565451,"score_gpt":0.1833075397170338,"score_spread":0.17227135985546838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607860939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99612856,0.00036107615,0.00015433312,0.00008833384,0.0000039242436,0.00001061844,0.00084237836,0.0000212709,0.002389427],"genre_scores_gemma":[0.9987092,0.00016598601,0.00023923331,0.000011726233,0.0000015146065,0.0000047894528,0.00046827903,0.000008988672,0.00039022416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998764,0.000015733613,0.000007844957,0.00003966513,0.000028611492,0.000031716703],"domain_scores_gemma":[0.9998282,0.000025100064,0.000030945594,0.000013029792,0.00007616554,0.00002642024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002973764,0.00034079514,0.00021837486,0.0011340441,0.0006649249,0.0010890694,0.00057478755,0.00030288013,0.0013178248],"category_scores_gemma":[0.0005639411,0.00026736577,0.00029075734,0.0012611703,0.00060031004,0.00026129044,0.00047270322,0.00023654186,0.00018574996],"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":[0.00011866123,0.000030577517,0.9681119,0.00006684938,0.000094812625,0.00022142846,0.0015114669,0.008427885,0.009987758,0.0005857221,0.0003517139,0.010491204],"study_design_scores_gemma":[0.000005682968,0.000007350367,0.9935649,0.000019805757,0.00001821306,0.000036438087,0.000816776,0.004227523,0.00031573433,0.00007205095,0.00090704474,0.000008545706],"about_ca_topic_score_codex":0.88440424,"about_ca_topic_score_gemma":0.9291179,"teacher_disagreement_score":0.11559576,"about_ca_system_score_codex":0.0053643514,"about_ca_system_score_gemma":0.0027858526,"threshold_uncertainty_score":0.232553},"labels":[],"label_agreement":null},{"id":"W1735826244","doi":"10.1111/jmg.12004","title":"Discovery of coesite–eclogite from the Nordøyane UHP domain, Western Gneiss Region, Norway: field relations, metamorphic history, and tectonic significance","year":2012,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Eclogite; Geology; Geochemistry; Coesite; Gneiss; Phengite; Omphacite; Metamorphism; Metamorphic rock; Continental crust; Metamorphic facies; Partial melting; Petrology; Subduction; Basalt; Crust; Geomorphology; Tectonics; Facies; Paleontology","score_opus":0.01890220361105494,"score_gpt":0.19523446537056138,"score_spread":0.17633226175950645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1735826244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986619,0.000109918816,0.00016341955,0.000010302716,0.0000042882425,0.0000071691716,0.00014344265,0.000007295172,0.0008922349],"genre_scores_gemma":[0.99923456,0.00004320234,0.00028411404,0.000010598281,0.000002886969,0.000004118068,0.00017363255,0.0000038298613,0.00024310162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998468,0.000008575331,0.000013086173,0.000068744994,0.00003557981,0.000027147575],"domain_scores_gemma":[0.9998254,0.00002350952,0.00005023593,0.00001535283,0.00004628008,0.00003933261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020340622,0.00020236122,0.00018124675,0.0013100996,0.00052932155,0.00060965755,0.0002788518,0.00029792124,0.0005292837],"category_scores_gemma":[0.0002590839,0.0001753579,0.00014250359,0.0006613633,0.00071348116,0.00021816342,0.0006465772,0.00015466807,0.00012137604],"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":[0.00014649582,0.000040916053,0.86348444,0.000077649165,0.000045835823,0.0025334188,0.0023648394,0.0001544459,0.11794962,0.00013551414,0.00017195083,0.012894837],"study_design_scores_gemma":[0.0000058604055,0.000031651463,0.99690646,0.000008632092,0.000007638513,0.0005371004,0.0005282438,0.00010489448,0.001018439,0.000014920581,0.0008344276,0.0000018646822],"about_ca_topic_score_codex":0.028425517,"about_ca_topic_score_gemma":0.049430568,"teacher_disagreement_score":0.028425517,"about_ca_system_score_codex":0.00041966233,"about_ca_system_score_gemma":0.00032266375,"threshold_uncertainty_score":0.056520104},"labels":[],"label_agreement":null},{"id":"W1748073762","doi":"10.1111/j.1525-1314.2010.00887.x","title":"Formation of gold deposits: a metamorphic devolatilization model","year":2010,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":622,"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":"Newmont Corporation; Barrick Gold Corporation","keywords":"Metamorphic rock; Greenschist; Geology; Geochemistry; Metamorphic facies; Shear zone; Metamorphism; Archean; Magnetite; Metasomatism; Mineralogy; Facies; Mantle (geology); Geomorphology","score_opus":0.0186278660773911,"score_gpt":0.22624159640740982,"score_spread":0.20761373033001873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1748073762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6505802,0.0016565737,0.12958105,0.0079715345,0.0003190889,0.00028824157,0.0010708433,0.0005433911,0.20798911],"genre_scores_gemma":[0.96247923,0.0005607619,0.008086203,0.00024417354,0.000053158514,0.000118520235,0.00017876798,0.00007672645,0.028202554],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999049,0.00001916632,0.0000066119005,0.00002403486,0.000017524664,0.000027807291],"domain_scores_gemma":[0.9997938,0.00003704083,0.000045613917,0.000020179317,0.000044463166,0.00005885886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003328409,0.00045420698,0.00031326473,0.0007711969,0.0007554362,0.0010728135,0.0012892424,0.0013998762,0.0073910896],"category_scores_gemma":[0.000692313,0.00033838805,0.0006652758,0.0002447914,0.0014887666,0.0015149855,0.0011571164,0.0005414968,0.0010451],"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":[0.00016947549,0.00014721365,0.0112689985,0.00021622637,0.00007232443,0.002173013,0.0006337757,0.41683,0.018023431,0.53079826,0.0048150024,0.014852169],"study_design_scores_gemma":[0.00013573046,0.000120746045,0.0035367282,0.000041894793,0.000035320027,0.00082466955,0.0002476308,0.8477127,0.0015996153,0.13644053,0.009255264,0.000049194805],"about_ca_topic_score_codex":0.0065677515,"about_ca_topic_score_gemma":0.0034409969,"teacher_disagreement_score":0.0073910896,"about_ca_system_score_codex":0.0014191584,"about_ca_system_score_gemma":0.00060913106,"threshold_uncertainty_score":0.024725676},"labels":[],"label_agreement":null},{"id":"W1844977582","doi":"10.1111/j.1525-1314.2010.00886.x","title":"Dependence of reaction kinetics on H<sub>2</sub>O activity as inferred from rates of intergranular diffusion of aluminium","year":2010,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":68,"is_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":"Metamorphic rock; Geology; Intergranular corrosion; Diffusion; Anhydrous; Mineralogy; Pluton; Geochemistry; Thermodynamics; Materials science; Chemistry; Tectonics; Metallurgy; Microstructure; Seismology","score_opus":0.013061858451677906,"score_gpt":0.22204599842125947,"score_spread":0.20898413996958157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1844977582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99778664,0.000084126434,0.0012410519,0.000009648773,0.0000010434487,0.0000050549515,0.00013379786,0.000022042219,0.0007164703],"genre_scores_gemma":[0.999355,0.000052360825,0.00027032805,0.0000024290912,5.099611e-7,0.0000031669206,0.00011165228,0.0000057268903,0.0001987968],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999008,0.000009293821,0.0000052977325,0.00003912647,0.000026216065,0.00001930986],"domain_scores_gemma":[0.99961084,0.00018401511,0.00009606545,0.000034083812,0.000051645806,0.000023482877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021025144,0.00017767565,0.00009448505,0.00032926662,0.00009878486,0.00042881013,0.0001945067,0.0001438541,0.0007849232],"category_scores_gemma":[0.0005844454,0.00019054719,0.0001260831,0.000121935765,0.00023516476,0.0003815119,0.00011645435,0.00017726092,0.00022842303],"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":[0.0004225714,0.000026688722,0.06679787,0.000049270988,0.00003749004,0.00006688149,0.0001375415,0.0034640746,0.92382246,0.0003625217,0.000051655545,0.0047610905],"study_design_scores_gemma":[0.000013157501,0.00011915055,0.22375722,0.0000060517436,0.000021874455,0.000084691834,0.00014540607,0.033445645,0.7411518,0.00021786505,0.0010227001,0.000014433526],"about_ca_topic_score_codex":0.0059075225,"about_ca_topic_score_gemma":0.005574747,"teacher_disagreement_score":0.0059075225,"about_ca_system_score_codex":0.00039389465,"about_ca_system_score_gemma":0.00013063432,"threshold_uncertainty_score":0.011746287},"labels":[],"label_agreement":null},{"id":"W1867751414","doi":"10.1111/jmg.12150","title":"Monazite as a monitor of melting, garnet growth and feldspar recrystallization in continental lower crust","year":2015,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"University of Massachusetts; University of Arkansas","keywords":"Monazite; Geology; Granulite; Geochemistry; Felsic; Partial melting; Continental crust; Grossular; Mafic; Plagioclase; Petrology; Zircon; Crust; Metamorphic rock; Quartz; Geomorphology; Facies","score_opus":0.018432722487226747,"score_gpt":0.21454978703393845,"score_spread":0.1961170645467117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1867751414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987531,0.000117070434,0.00007483288,0.0000040206005,5.8212356e-7,0.0000033492513,0.00041328164,0.000023565073,0.0006101724],"genre_scores_gemma":[0.99911946,0.00003596809,0.00018816136,0.0000039187594,5.5700224e-7,0.0000022170616,0.0003619461,0.0000045299057,0.00028307716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992764,0.000005769631,0.000005894918,0.00002209095,0.000024111447,0.000014618056],"domain_scores_gemma":[0.99985325,0.000008786787,0.000043406482,0.00001632852,0.000046071927,0.000032148946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010851245,0.00020371443,0.00010939941,0.000986934,0.00019905726,0.00037445992,0.00014200184,0.00017059848,0.0006768039],"category_scores_gemma":[0.00025759643,0.00011617995,0.000113312904,0.0006821498,0.00012294522,0.00011696573,0.00022107128,0.000116079726,0.00015639639],"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":[0.00020464603,0.00002262812,0.90051705,0.000031131895,0.000061413775,0.0000847098,0.0002008682,0.00042618613,0.0906756,0.000039029528,0.00007198613,0.0076647294],"study_design_scores_gemma":[0.00000109354,0.000017887101,0.9962089,0.0000014999641,0.0000061380224,0.00003235518,0.000043553853,0.00019981782,0.0032854283,0.000004318391,0.00019778937,0.0000012779659],"about_ca_topic_score_codex":0.04845304,"about_ca_topic_score_gemma":0.10316984,"teacher_disagreement_score":0.04845304,"about_ca_system_score_codex":0.00056150445,"about_ca_system_score_gemma":0.0001688138,"threshold_uncertainty_score":0.09634203},"labels":[],"label_agreement":null},{"id":"W1870803485","doi":"10.1046/j.1525-1314.2003.00445.x","title":"Exhumation of the Main Central Thrust from Lower Crustal Depths, Eastern Bhutan Himalaya","year":2003,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":241,"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; National Science Foundation","keywords":"Kyanite; Geology; Monazite; Leucogranite; Staurolite; Metamorphism; Schist; Metamorphic rock; Geochemistry; Sillimanite; Gneiss; Main Central Thrust; Migmatite; Zircon; Paleontology; Biotite","score_opus":0.012788609613674546,"score_gpt":0.1829668534396791,"score_spread":0.17017824382600458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1870803485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970011,0.0001695713,0.000068552545,0.000025326975,0.00000335739,0.0000048471625,0.00025346997,0.000010032716,0.0024637422],"genre_scores_gemma":[0.9988331,0.00006449252,0.000066230205,0.000012759797,0.000003868606,0.0000018328036,0.00025725638,0.0000024060844,0.00075813045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991965,0.0000066079133,0.0000049754294,0.000018973933,0.00002266685,0.000027097069],"domain_scores_gemma":[0.999876,0.000014110241,0.000025568872,0.000008968673,0.000044739816,0.000030590374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007877806,0.0001952654,0.00016305436,0.0012544368,0.000756921,0.00058056874,0.00018174395,0.00016150206,0.0026570647],"category_scores_gemma":[0.00017389398,0.00016063127,0.00010073417,0.0016005208,0.00031907033,0.00021589095,0.00038536493,0.00017575898,0.00036960305],"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":[0.0003522379,0.00004744458,0.80487293,0.00027711983,0.00013311657,0.0023525937,0.0061088707,0.0009836532,0.12850176,0.00043681992,0.0005993352,0.05533424],"study_design_scores_gemma":[0.000002144402,0.000009758433,0.9984332,0.0000047286912,0.0000053187505,0.00010703382,0.0002450825,0.00011749682,0.00060435163,0.000013397824,0.00045563918,0.000001949014],"about_ca_topic_score_codex":0.08833675,"about_ca_topic_score_gemma":0.15019593,"teacher_disagreement_score":0.08833675,"about_ca_system_score_codex":0.0007830946,"about_ca_system_score_gemma":0.00035344975,"threshold_uncertainty_score":0.17564517},"labels":[],"label_agreement":null},{"id":"W1931141686","doi":"10.1111/j.1525-1314.2010.00893.x","title":"Metamorphic history of a syn‐convergent orogen‐parallel detachment: The South Tibetan detachment system, Bhutan Himalaya","year":2010,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Monazite; Metamorphism; Metamorphic rock; Geochemistry; Geochronology; Sillimanite; Detachment fault; Geothermobarometry; Kyanite; Clockwise; Zircon; Petrology; Seismology; Paleontology; Tectonics; Fold (higher-order function); Extensional definition; Biotite; Quartz","score_opus":0.01417565157659682,"score_gpt":0.18891371206110302,"score_spread":0.1747380604845062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1931141686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846494,0.000092429684,0.000035095403,0.000012837786,0.0000013786462,0.0000038710878,0.000082939674,0.0000042891224,0.0013021083],"genre_scores_gemma":[0.9994326,0.000052220963,0.000036623827,0.0000065874965,0.0000014971198,0.0000012337894,0.00012187364,0.000001434369,0.00034587074],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999198,0.000009864147,0.0000072444154,0.000021992482,0.000017660741,0.00002344884],"domain_scores_gemma":[0.9999083,0.0000059571958,0.000022201148,0.000007186483,0.000027236976,0.000029003844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013273313,0.00021466453,0.00014301474,0.0012259597,0.0008572678,0.00077735493,0.00019935337,0.00016469456,0.0018691149],"category_scores_gemma":[0.0002054086,0.00017425648,0.00009909336,0.0015952847,0.0005597021,0.00017308192,0.0005172749,0.0001743236,0.00024277596],"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":[0.0002907127,0.00004957748,0.9298032,0.00009836096,0.000106566054,0.0016078416,0.004685576,0.0011017717,0.040814944,0.00064520474,0.00027434525,0.020521956],"study_design_scores_gemma":[0.0000049063237,0.00002671449,0.99821967,0.000004902572,0.000009458567,0.00018196316,0.0005560964,0.00023374784,0.00026748306,0.000029561108,0.00046232005,0.0000030963631],"about_ca_topic_score_codex":0.07465908,"about_ca_topic_score_gemma":0.1364611,"teacher_disagreement_score":0.07465908,"about_ca_system_score_codex":0.0011701605,"about_ca_system_score_gemma":0.00046422897,"threshold_uncertainty_score":0.148449},"labels":[],"label_agreement":null},{"id":"W1943489223","doi":"10.1046/j.1525-1314.2003.00447.x","title":"Schlieren formation in diatexite migmatite: examples from the St Malo migmatite terrane, France","year":2003,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Université du Québec à Chicoutimi","funders":"","keywords":"Biotite; Plagioclase; Geology; Geochemistry; Mineralogy; Paleontology","score_opus":0.018642365958291003,"score_gpt":0.19486616148083524,"score_spread":0.17622379552254425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1943489223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996756,0.00029167766,0.00010836699,0.000023360808,0.0000026654095,0.000013421432,0.00016063926,0.000015335536,0.0026286163],"genre_scores_gemma":[0.9974989,0.00011395955,0.00040794275,0.000011540335,0.000004357024,0.000004287127,0.0003397086,0.0000068904637,0.0016124735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980193,0.000015130924,0.000011144063,0.000061925064,0.000058374226,0.000051411025],"domain_scores_gemma":[0.99992037,0.000009856818,0.00002983279,0.000008010617,0.000021639107,0.000010265786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001433763,0.00036278213,0.00022614654,0.0026281895,0.00082350697,0.00064064236,0.0003896722,0.0004832146,0.0012800541],"category_scores_gemma":[0.00017960297,0.00016191314,0.00024232201,0.0011328986,0.00048800017,0.00017231768,0.0004793658,0.00013541938,0.00021386838],"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":[0.00042203546,0.00013138508,0.860508,0.0001617646,0.00012283561,0.0071611777,0.0031589665,0.0020651233,0.07803102,0.00069859554,0.0007944057,0.046744756],"study_design_scores_gemma":[0.000008079651,0.000050278595,0.9900525,0.000009379802,0.000011085918,0.001308141,0.00049330294,0.00057668233,0.0027804929,0.000044776403,0.004658197,0.000007152912],"about_ca_topic_score_codex":0.054177213,"about_ca_topic_score_gemma":0.11979806,"teacher_disagreement_score":0.054177213,"about_ca_system_score_codex":0.0012251892,"about_ca_system_score_gemma":0.00029087407,"threshold_uncertainty_score":0.10772377},"labels":[],"label_agreement":null},{"id":"W1966026303","doi":"10.1111/j.1525-1314.2008.00783.x","title":"The role of heterogeneous strain in the development and preservation of a polymetamorphic record in high‐<i>P</i> granulites, western Canadian Shield","year":2008,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":59,"is_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":"Granulite; Mafic; Geology; Geochemistry; Zircon; Amphibole; Facies; Metamorphic rock; Metamorphic facies; Baltic Shield; Crust; Geomorphology; Paleontology","score_opus":0.01727475507218083,"score_gpt":0.18497113045070798,"score_spread":0.16769637537852716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966026303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835277,0.000059259914,0.00006294368,0.000012307257,4.1561083e-7,0.0000043329,0.00020406986,0.000009749555,0.0012940994],"genre_scores_gemma":[0.9996499,0.000023974118,0.00006113633,0.0000042560837,4.5036987e-7,0.000001649938,0.00012610597,0.0000027828062,0.00012982007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984694,0.000003957228,0.0000064553324,0.000039158742,0.00005330695,0.000050223505],"domain_scores_gemma":[0.9997776,0.000015376672,0.00005714734,0.000014223334,0.00009440748,0.000041289615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116903626,0.00016977281,0.00013153015,0.0015064777,0.0012531005,0.00077868014,0.0005179232,0.0002104506,0.0008922342],"category_scores_gemma":[0.00037259966,0.00019618432,0.00012194355,0.0011161466,0.0010643774,0.00017017881,0.00041700184,0.00016636479,0.00009665798],"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":[0.00018190136,0.00001935343,0.9084845,0.00004867944,0.000058182883,0.00035872567,0.0012774764,0.0009278345,0.07602637,0.000524209,0.00026911215,0.011823585],"study_design_scores_gemma":[7.888106e-7,0.0000035160185,0.99914265,0.0000012972042,0.0000029776897,0.000036095615,0.00010255439,0.000113210546,0.0004344688,0.000010488297,0.00015017283,0.000001759716],"about_ca_topic_score_codex":0.82982,"about_ca_topic_score_gemma":0.91358155,"teacher_disagreement_score":0.17018002,"about_ca_system_score_codex":0.0038872932,"about_ca_system_score_gemma":0.0020846594,"threshold_uncertainty_score":0.34236443},"labels":[],"label_agreement":null},{"id":"W1971728771","doi":"10.1111/jmg.12030","title":"Integrated pressure–temperature–time constraints for the <scp>T</scp>so <scp>M</scp>orari dome (<scp>N</scp>orthwest <scp>I</scp>ndia): implications for the burial and exhumation path of <scp>UHP</scp> units in the western <scp>H</scp>imalaya","year":2012,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":160,"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; Eclogite; Coesite; Zircon; Omphacite; Geochemistry; Mafic; Metamorphism; Gneiss; Lawsonite; Pyrope; Phengite; Protolith; Grossular; Metamorphic rock; Petrology; Subduction; Tectonics","score_opus":0.025543659437366164,"score_gpt":0.23211345542545905,"score_spread":0.20656979598809289,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971728771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736834,0.000038513073,0.0004619434,0.000014712878,0.0000016029095,0.0000046757186,0.00039790347,0.000018392184,0.001693866],"genre_scores_gemma":[0.99913675,0.000021638712,0.00025717754,0.0000035815992,0.0000015656998,0.0000055491523,0.00040822735,0.000009228503,0.00015624393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992526,0.0000035822864,0.0000051985094,0.000027312455,0.000021567,0.00001705272],"domain_scores_gemma":[0.99988675,0.000015552192,0.000032568667,0.000010903167,0.000034652738,0.000019579824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011890628,0.00019761153,0.00019703241,0.00077017065,0.00041149626,0.00057101954,0.0003178374,0.00023344302,0.001029644],"category_scores_gemma":[0.00029908947,0.0003074164,0.0002597975,0.00073125487,0.0003455695,0.00033076358,0.00038826556,0.00024045986,0.00025473206],"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":[0.00040197204,0.000084861684,0.67565507,0.000087123444,0.00011804406,0.00041953588,0.00054634834,0.012034542,0.297378,0.0007808746,0.00035608167,0.012137538],"study_design_scores_gemma":[0.000012750957,0.000024821298,0.97624546,0.0000038907137,0.00002213234,0.000079931495,0.0001291567,0.010720639,0.012130373,0.00010007382,0.0005230463,0.000007697915],"about_ca_topic_score_codex":0.03341908,"about_ca_topic_score_gemma":0.048690915,"teacher_disagreement_score":0.03341908,"about_ca_system_score_codex":0.0007213053,"about_ca_system_score_gemma":0.0006023228,"threshold_uncertainty_score":0.066449106},"labels":[],"label_agreement":null},{"id":"W1973970442","doi":"10.1111/jmg.12112","title":"Quantifying the <i>P–T–t</i> conditions of north–south Lhasa terrane accretion: new insight into the pre‐Himalayan architecture of the Tibetan plateau","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Geological Survey of Canada","funders":"Natural Environment Research Council; Natural Resources Canada","keywords":"Geology; Terrane; Zircon; Metamorphism; Overprinting; Metamorphic rock; Monazite; Geochemistry; Geochronology; Continental collision; Schist; Plateau (mathematics); Gondwana; Tectonics; Paleontology; Subduction","score_opus":0.020668995476992677,"score_gpt":0.2160664174356549,"score_spread":0.19539742195866222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973970442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984676,0.00008405517,0.00031712654,0.000010249698,8.558583e-7,0.0000024304197,0.00010589182,0.000009352093,0.0010024513],"genre_scores_gemma":[0.99965227,0.000028529286,0.00013153256,0.0000029995294,0.0000018210981,0.0000015314635,0.000085857435,0.0000024203591,0.00009302342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.000006954709,0.0000038719936,0.000014545651,0.000009329917,0.000007812979],"domain_scores_gemma":[0.99991536,0.000015415411,0.000020590815,0.000007715608,0.000027942335,0.000013003691],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019203038,0.00015961792,0.00008827758,0.0008624241,0.00028462618,0.00069978886,0.00014505838,0.00015338737,0.00095942774],"category_scores_gemma":[0.00022666744,0.0001084145,0.000102961334,0.000755008,0.0003019408,0.0002575473,0.0001794364,0.00010963595,0.00013680148],"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":[0.00013966409,0.00001707502,0.9002614,0.00006444046,0.00007383866,0.00019774503,0.00054736057,0.0022339416,0.08212295,0.00023726688,0.00012778927,0.013976449],"study_design_scores_gemma":[0.000003031488,0.000019044463,0.99600285,0.000004127706,0.000012245007,0.000047539994,0.00026906462,0.002062941,0.0012887155,0.00005900192,0.00022768871,0.0000036733588],"about_ca_topic_score_codex":0.020230656,"about_ca_topic_score_gemma":0.03143575,"teacher_disagreement_score":0.020230656,"about_ca_system_score_codex":0.00033491946,"about_ca_system_score_gemma":0.0002451076,"threshold_uncertainty_score":0.040225804},"labels":[],"label_agreement":null},{"id":"W1974131317","doi":"10.1046/j.1525-1314.2003.00417.x","title":"Regional‐scale Grenvillian‐age UHT metamorphism in the Mollendo–Camana block (basement of the Peruvian Andes)","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Geology; Metamorphism; Geochemistry; Biotite; Sillimanite; Migmatite; Monazite; Zircon; Cordierite; Kyanite; Precambrian; Metamorphic rock; Gneiss; Quartz; Chemistry; Paleontology","score_opus":0.02985007414169127,"score_gpt":0.19343461176029583,"score_spread":0.16358453761860456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974131317","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99794906,0.00017586334,0.000040123537,0.000029496838,9.1816275e-7,0.000007312741,0.0002683865,0.000014688195,0.0015141858],"genre_scores_gemma":[0.9992945,0.00006189028,0.000088922905,0.000005976099,0.000002017581,0.000004523619,0.00024579276,0.0000030342292,0.00029334024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992085,0.000010821266,0.0000035683695,0.000024819452,0.000013140142,0.000026827294],"domain_scores_gemma":[0.9998853,0.000008866482,0.000045614044,0.000012034943,0.000029420098,0.000018685381],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012903824,0.0001638114,0.000118406635,0.00086642016,0.00036052198,0.00045533717,0.00022716072,0.00028711703,0.0020149932],"category_scores_gemma":[0.00030750112,0.00011070171,0.00012950123,0.0006138196,0.00032536944,0.00017613563,0.0005009856,0.00010747288,0.00037366487],"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":[0.00020099584,0.000022086835,0.9304655,0.0001054291,0.00009578561,0.00089132274,0.0018753178,0.00038449749,0.044189505,0.00027180577,0.00043556892,0.021062195],"study_design_scores_gemma":[0.0000021263825,0.000010366468,0.99867934,0.000005439465,0.000004556361,0.00008436084,0.0001659676,0.00007840143,0.0001926187,0.000005793407,0.00076986814,0.0000011311391],"about_ca_topic_score_codex":0.05482678,"about_ca_topic_score_gemma":0.1225953,"teacher_disagreement_score":0.05482678,"about_ca_system_score_codex":0.00074617326,"about_ca_system_score_gemma":0.00015881071,"threshold_uncertainty_score":0.109015346},"labels":[],"label_agreement":null},{"id":"W1976003055","doi":"10.1111/jmg.12128","title":"Petrology of metapelites in the Bugaboo aureole, British Columbia, Canada","year":2015,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Andalusite; Geology; Sillimanite; Geochemistry; Schist; Greenschist; Metamorphism; Cordierite; Metamorphic rock; Hornfels; Muscovite; Biotite; Quartz; Paleontology","score_opus":0.014540021146392969,"score_gpt":0.1774800774918221,"score_spread":0.16294005634542913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976003055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833875,0.00063706207,0.00021011784,0.00010421962,0.000007371994,0.00005947936,0.0017476564,0.000049288632,0.013797355],"genre_scores_gemma":[0.9918248,0.00033332643,0.00040809036,0.00003490169,0.000001717823,0.00001570735,0.00058157585,0.000017367689,0.0067825112],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998017,0.0000054320976,0.00000682768,0.000043199787,0.00007592333,0.00006698562],"domain_scores_gemma":[0.99962103,0.000016200916,0.000037873975,0.000012055491,0.00023261017,0.00008023329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011648313,0.00034416743,0.00020169378,0.0028549577,0.0035560457,0.0010806147,0.00069497345,0.00036660963,0.0039678877],"category_scores_gemma":[0.00040611307,0.0003438383,0.00013256742,0.0023656725,0.00059678056,0.00025670277,0.00084086607,0.00031874684,0.0004592818],"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":[0.0001850513,0.00003954323,0.9190686,0.00014485694,0.000052017822,0.0019517373,0.004772368,0.0005101436,0.021526037,0.00045576657,0.0024456028,0.048848286],"study_design_scores_gemma":[0.0000026200591,0.000008819959,0.99118453,0.000042322805,0.000007913915,0.0002082403,0.0025078843,0.0002193691,0.00045065046,0.000019684618,0.0053400244,0.000007855564],"about_ca_topic_score_codex":0.9819885,"about_ca_topic_score_gemma":0.9975683,"teacher_disagreement_score":0.01801151,"about_ca_system_score_codex":0.010304433,"about_ca_system_score_gemma":0.0071969284,"threshold_uncertainty_score":0.07476425},"labels":[],"label_agreement":null},{"id":"W1976187498","doi":"10.1111/j.1525-1314.2008.00787.x","title":"Coupling forward modelling of garnet growth with monazite geochronology: an application to the Rappold Complex (Austroalpine crystalline basement)","year":2008,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Austrian Science Fund","keywords":"Monazite; Metamorphism; Geology; Geochemistry; Metamorphic rock; Geochronology; Orogeny; Sillimanite; Kyanite; Zircon; Biotite; Paleontology; Tectonics","score_opus":0.038729925178990085,"score_gpt":0.20933225358672217,"score_spread":0.1706023284077321,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976187498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9485292,0.0001088656,0.04504154,0.00013191924,0.00003187517,0.0000670378,0.00059454306,0.001318231,0.0041767415],"genre_scores_gemma":[0.98507255,0.000049200447,0.013344659,0.00001434867,0.0000065385548,0.000035402896,0.00027219218,0.00011105144,0.0010940469],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998956,0.00003105322,0.000007645651,0.000027907588,0.00002447509,0.000013379523],"domain_scores_gemma":[0.9996039,0.00021998404,0.00003767505,0.00003110103,0.00008094559,0.000026443904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043733793,0.00074256165,0.00063421065,0.00050820084,0.0004319857,0.0010212341,0.0008688382,0.001170534,0.0021932097],"category_scores_gemma":[0.0011345682,0.00059769873,0.0008430395,0.00042453967,0.00040215557,0.0003081265,0.0004756267,0.0005379369,0.0002884117],"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":[0.000030046154,0.00001988433,0.0018456758,0.000014376282,0.000026703554,0.000037387872,0.000023200717,0.99418455,0.0013784013,0.00013745806,0.00003963824,0.0022626226],"study_design_scores_gemma":[0.0000061978603,0.000006414838,0.000467122,0.0000010315867,0.0000034837044,0.00000392341,0.0000051518086,0.99913067,0.00026375373,0.00003618669,0.000073226605,0.0000027756112],"about_ca_topic_score_codex":0.08675212,"about_ca_topic_score_gemma":0.05659403,"teacher_disagreement_score":0.08675212,"about_ca_system_score_codex":0.0009651671,"about_ca_system_score_gemma":0.0014933335,"threshold_uncertainty_score":0.17249435},"labels":[],"label_agreement":null},{"id":"W1984094358","doi":"10.1111/j.1525-1314.2006.00683.x","title":"Multiple metasomatism in Sulu ultrahigh‐P garnet peridotite constrained by petrological and geochemical investigations","year":2007,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Saskatchewan","funders":"","keywords":"Phlogopite; Peridotite; Geology; Geochemistry; Lile; Metasomatism; Mantle (geology); Carbonatite; Primitive mantle; Partial melting","score_opus":0.011043360013740539,"score_gpt":0.19808303120579918,"score_spread":0.18703967119205864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984094358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995347,0.000048649537,0.00005612883,0.0000057620755,6.3244283e-7,0.0000018974035,0.0000496816,0.000005403582,0.0002971144],"genre_scores_gemma":[0.9996697,0.000026054719,0.00008340468,0.00000350702,9.343224e-7,0.000001133661,0.000073302734,0.0000017943258,0.00014010012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999347,0.000003935783,0.0000041685435,0.000024836749,0.000014055464,0.000018288913],"domain_scores_gemma":[0.99992573,0.0000053641807,0.000027100617,0.0000061303645,0.00001984394,0.000015946971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105136925,0.0003190466,0.00016211194,0.0017118711,0.00039004945,0.0005004637,0.00026106957,0.00031535662,0.00073003396],"category_scores_gemma":[0.00010862322,0.0002347165,0.00016265527,0.0007477447,0.00038695565,0.00020687644,0.00039503517,0.00010172106,0.00015998665],"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":[0.00024250097,0.000031695225,0.75640774,0.000048693728,0.00006320034,0.001948931,0.000624306,0.00032459578,0.23472066,0.00021233728,0.00006301575,0.0053122337],"study_design_scores_gemma":[0.000005119217,0.00003733985,0.9912896,0.000004282053,0.00001895642,0.0006936768,0.0004155089,0.0009131254,0.0059262295,0.00005956975,0.00063234573,0.000004266222],"about_ca_topic_score_codex":0.009189169,"about_ca_topic_score_gemma":0.020550882,"teacher_disagreement_score":0.009189169,"about_ca_system_score_codex":0.00040395051,"about_ca_system_score_gemma":0.00019908344,"threshold_uncertainty_score":0.018271327},"labels":[],"label_agreement":null},{"id":"W1998427043","doi":"10.1046/j.1525-1314.2003.00481.x","title":"Stable isotope constraints on the Al<sub>2</sub>SiO<sub>5</sub>‘triple‐point’ rocks from the Proterozoic Priest pluton contact aureole, New Mexico, USA","year":2003,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Western University","funders":"","keywords":"Geology; Schist; Kyanite; Andalusite; Sillimanite; Staurolite; Geochemistry; Metamorphism; Isograd; Pluton; Pelite; Metamorphic rock; Grossular; Muscovite; Quartz; Biotite; Metamorphic facies; Geomorphology; Paleontology","score_opus":0.017927029304021565,"score_gpt":0.1968107922758716,"score_spread":0.17888376297185002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998427043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979966,0.0000779248,0.00006208418,0.000028286437,0.0000012192448,0.000003859046,0.0003402113,0.00000841982,0.001481362],"genre_scores_gemma":[0.9989021,0.000048742517,0.00022289353,0.000009320069,0.0000019814656,0.0000049964196,0.00046424023,0.000004240378,0.00034146124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999604,0.0000017641805,0.0000032630307,0.000015844846,0.000010584346,0.000008160795],"domain_scores_gemma":[0.99989855,0.0000086112195,0.000032478853,0.0000064276096,0.000040112227,0.000013781231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009965416,0.00015875258,0.0001285513,0.0011307094,0.0006594274,0.00052053685,0.00022948242,0.00022964615,0.001684245],"category_scores_gemma":[0.00015726942,0.00015414614,0.000102887716,0.00062635174,0.00027057304,0.00016047021,0.00024569043,0.00015679476,0.00022444996],"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":[0.00034953404,0.00004282368,0.8270305,0.00007932233,0.0001018851,0.00041749535,0.0009487915,0.0007029734,0.15301578,0.00029565464,0.00043811364,0.016577078],"study_design_scores_gemma":[0.0000057793586,0.000011595014,0.9963613,0.0000049924356,0.000011410373,0.00004846341,0.0001667719,0.00026346324,0.0020673284,0.000014465308,0.0010431374,0.000001340918],"about_ca_topic_score_codex":0.09861722,"about_ca_topic_score_gemma":0.2744522,"teacher_disagreement_score":0.09861722,"about_ca_system_score_codex":0.0011957313,"about_ca_system_score_gemma":0.00033905328,"threshold_uncertainty_score":0.1960864},"labels":[],"label_agreement":null},{"id":"W2009478634","doi":"10.1111/j.1525-1314.2005.00577.x","title":"Borosilicate‐ and phengite‐bearing veins from the Grenville Province of Labrador: evidence for rapid uplift","year":2005,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Graduate School, University of Minnesota; Geological Society of America; U.S. Department of Education","keywords":"Geology; Phengite; Kyanite; Geochemistry; Pseudomorph; Vein; Igneous rock; Metamorphic rock; Migmatite; Quartz; Gneiss; Paleontology; Eclogite; Subduction","score_opus":0.03649489876945081,"score_gpt":0.23278193985709075,"score_spread":0.19628704108763995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009478634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99707544,0.00019051059,0.00005015192,0.00004945351,0.0000031599016,0.000012751053,0.0005120572,0.000022087086,0.0020842978],"genre_scores_gemma":[0.9987888,0.000042981494,0.0001364215,0.000025725436,0.000002770584,0.000007167615,0.0006673218,0.0000104101055,0.00031843976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994856,0.000049409082,0.000045567813,0.00014389926,0.000120944664,0.00015463422],"domain_scores_gemma":[0.99936014,0.00006283643,0.00023906208,0.00005514276,0.00019602301,0.00008675521],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028715862,0.00028871297,0.0003992797,0.0020529814,0.0007871861,0.0016716549,0.0011159787,0.00044068883,0.0016631269],"category_scores_gemma":[0.00087812735,0.00033821585,0.00020885939,0.0016848248,0.0008967184,0.00034640037,0.00080097996,0.00026455472,0.00039419404],"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":[0.0001940422,0.00005389344,0.948329,0.00011157379,0.00008943609,0.0005857673,0.0019891658,0.00028919292,0.033789467,0.0002315879,0.00039747328,0.013939385],"study_design_scores_gemma":[0.000013238615,0.000023256705,0.9968471,0.000018551307,0.0000113116175,0.00019968991,0.0008055266,0.00014782278,0.00074595335,0.000015793059,0.0011641268,0.000007605045],"about_ca_topic_score_codex":0.3476749,"about_ca_topic_score_gemma":0.57597095,"teacher_disagreement_score":0.6523251,"about_ca_system_score_codex":0.0018355856,"about_ca_system_score_gemma":0.0012393142,"threshold_uncertainty_score":0.6913024},"labels":[],"label_agreement":null},{"id":"W2012622731","doi":"10.1111/j.1525-1314.2007.00746.x","title":"Establishing the <i>P–T</i> path for Alpine Schist, Southern Alps near Hokitika, New Zealand","year":2007,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Victoria University; University of Melbourne; University of Victoria","keywords":"Schist; Geology; Albite; Metamorphic rock; Geochemistry; Mineralogy; Geomorphology; Quartz; Paleontology","score_opus":0.013906223559373338,"score_gpt":0.20550871191843276,"score_spread":0.1916024883590594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012622731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99775296,0.000037716272,0.00024798763,0.000019830828,0.0000011842155,0.00001863318,0.00037120612,0.000013047092,0.0015374654],"genre_scores_gemma":[0.9990031,0.000028447315,0.00045518222,0.000002575682,9.1825115e-7,0.0000090151525,0.00029172614,0.000003838425,0.00020514929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989843,0.0000071060686,0.000008444003,0.000030076177,0.000028489922,0.000027420607],"domain_scores_gemma":[0.99969983,0.000026284262,0.00009761636,0.000012783042,0.00012464121,0.00003888202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013111066,0.00017955262,0.0001115521,0.00168163,0.00071724807,0.00073947175,0.00028548745,0.00025884144,0.0016930358],"category_scores_gemma":[0.00059162773,0.0002166401,0.00021955844,0.0011999564,0.00059195206,0.00030532098,0.00047506593,0.00021580247,0.00035589247],"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":[0.0002471433,0.000047258447,0.91777575,0.000144957,0.000041934516,0.0010007505,0.0016044069,0.0018011716,0.053939857,0.00030651304,0.0003272397,0.02276296],"study_design_scores_gemma":[0.000006313159,0.000036013153,0.9972166,0.0000083615105,0.000005025078,0.00011813732,0.00043938195,0.001106914,0.0005573528,0.000032445038,0.00046943675,0.000004056181],"about_ca_topic_score_codex":0.25196004,"about_ca_topic_score_gemma":0.33011553,"teacher_disagreement_score":0.25196004,"about_ca_system_score_codex":0.001161448,"about_ca_system_score_gemma":0.00088247476,"threshold_uncertainty_score":0.50098693},"labels":[],"label_agreement":null},{"id":"W2023565929","doi":"10.1111/jmg.12086","title":"High to ultrahigh temperature contact metamorphism and dry partial melting of the Tasiuyak paragneiss, Northern Labrador","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Government of Newfoundland and Labrador; Memorial University of Newfoundland; Carleton University","funders":"University of Michigan","keywords":"Geology; Sillimanite; Geochemistry; Granulite; Cordierite; Metamorphism; Gneiss; Partial melting; Migmatite; Pseudomorph; Biotite; Plagioclase; Feldspar; Metamorphic facies; Mineral; Metamorphic rock; Quartz; Facies; Geomorphology; Crust; Chemistry","score_opus":0.006291968682112307,"score_gpt":0.17769365062454132,"score_spread":0.171401681942429,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023565929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991517,0.000035070938,0.00002509636,0.000005083656,5.651809e-7,0.0000034393934,0.0001645573,0.0000071376753,0.0006073065],"genre_scores_gemma":[0.9993569,0.0000193289,0.0000479815,0.000004433403,8.159413e-7,0.0000030807225,0.00020636339,0.00000485379,0.00035618688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999039,0.0000049507294,0.0000054433312,0.000039532082,0.000017080823,0.00002906638],"domain_scores_gemma":[0.9999459,0.000002866722,0.000020800775,0.00000499381,0.000014103908,0.000011481211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007468445,0.00021794885,0.00022918811,0.0008828549,0.0007430398,0.00054077595,0.00031596966,0.00019771517,0.0011898879],"category_scores_gemma":[0.0001078652,0.00020238748,0.00015514604,0.000897669,0.00054273097,0.00020215199,0.00037328745,0.00014943945,0.00023005705],"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":[0.00039374424,0.000053208933,0.8479079,0.00007605381,0.000102167425,0.00123104,0.004249633,0.0004225341,0.13143362,0.00019445336,0.00023591616,0.013699683],"study_design_scores_gemma":[0.000002035355,0.000018157572,0.99829537,0.0000020902496,0.0000064241985,0.00009661783,0.00045063015,0.00006777174,0.0007079698,0.000004391598,0.00034685052,0.0000015838334],"about_ca_topic_score_codex":0.17440234,"about_ca_topic_score_gemma":0.35027036,"teacher_disagreement_score":0.82559764,"about_ca_system_score_codex":0.0015463016,"about_ca_system_score_gemma":0.00057779346,"threshold_uncertainty_score":0.34677446},"labels":[],"label_agreement":null},{"id":"W2023661439","doi":"10.1111/jmg.12088","title":"The inception and growth of leucosomes: microstructure at the start of melt segregation in migmatites","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":60,"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 Chicoutimi","funders":"Natural Sciences and Engineering Research Council of Canada; University of Minnesota","keywords":"Plagioclase; Cordierite; Migmatite; Geology; Geochemistry; Partial melting; Feldspar; Mineralogy; Metamorphic rock; Quartz; Gneiss; Materials science; Basalt; Composite material","score_opus":0.006974982696636615,"score_gpt":0.18099001903194206,"score_spread":0.17401503633530543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023661439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907136,0.0000622377,0.00017925406,0.000003433349,6.733736e-7,0.0000035760065,0.000097807155,0.0000139347085,0.0005676882],"genre_scores_gemma":[0.99918646,0.000021372021,0.00020708557,0.0000032536593,8.8013286e-7,0.0000027997412,0.00011328398,0.000007661768,0.00045710517],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995124,0.0000031295724,0.0000033019367,0.000018324186,0.000011671879,0.0000122313595],"domain_scores_gemma":[0.9999081,0.000011096839,0.000024488985,0.0000064196515,0.000025902575,0.00002412491],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000073778174,0.00009302149,0.000099254336,0.0005148413,0.00021182415,0.00044992514,0.0001341061,0.00022665426,0.0006093392],"category_scores_gemma":[0.00015270193,0.00016251853,0.00009631222,0.00016873286,0.00024440518,0.00018778471,0.00018896458,0.00015347017,0.0001508216],"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":[0.0002851305,0.000015912632,0.06220962,0.000032318807,0.000013626276,0.00018548276,0.00035057787,0.00031030067,0.93285996,0.00012981548,0.00003392232,0.0035732065],"study_design_scores_gemma":[0.0000064390247,0.00010610483,0.92119235,0.000005705557,0.000012937721,0.00027436067,0.0002591177,0.0009403973,0.075877585,0.000042678585,0.001275636,0.0000065937397],"about_ca_topic_score_codex":0.005135317,"about_ca_topic_score_gemma":0.0073039047,"teacher_disagreement_score":0.005135317,"about_ca_system_score_codex":0.00043194272,"about_ca_system_score_gemma":0.000105682724,"threshold_uncertainty_score":0.010210872},"labels":[],"label_agreement":null},{"id":"W2028598478","doi":"10.1111/jmg.12085","title":"Phase equilibria modelling of retrograde amphibole and clinozoisite in mafic eclogite from the Tso Morari massif, northwest India: constraining the <i>P</i>–<i>T</i>–<i>M</i>(H<sub>2</sub>O) conditions of exhumation","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Environment Research Council","keywords":"Amphibole; Eclogite; Mafic; Geology; Geochemistry; Massif; Metamorphic rock; Omphacite; Phengite; Petrology; Subduction; Paleontology; Tectonics","score_opus":0.024924444053782874,"score_gpt":0.21721955875617593,"score_spread":0.19229511470239305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028598478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983677,0.000012678736,0.0007537454,0.000014215988,0.0000011638252,0.000009833219,0.00022365198,0.000039057948,0.000577977],"genre_scores_gemma":[0.9988416,0.00001362821,0.00070619775,0.0000035916835,7.881827e-7,0.000008416138,0.00024582172,0.000009249316,0.00017068884],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996245,0.000004640295,0.0000026339817,0.00001050266,0.000007986452,0.000011749999],"domain_scores_gemma":[0.99992645,0.000025162306,0.000014232195,0.0000056628232,0.000020029025,0.000008495344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009717868,0.00039474736,0.00019655225,0.0005952243,0.00034615723,0.0005288404,0.0005453736,0.0005150258,0.0012982164],"category_scores_gemma":[0.00029329173,0.00029499846,0.0005456697,0.00044415865,0.0002889652,0.00020249789,0.00021692636,0.00021418551,0.00013259613],"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":[0.00040031393,0.00012355662,0.07717632,0.000094893294,0.00008158981,0.00038704296,0.00028758505,0.86970776,0.0453392,0.00056209095,0.00017186807,0.005667754],"study_design_scores_gemma":[0.00004567124,0.00007041843,0.029879276,0.000005006301,0.000020984491,0.00003924549,0.00019183545,0.9634915,0.005777894,0.00015650496,0.00031077478,0.000010956593],"about_ca_topic_score_codex":0.046486966,"about_ca_topic_score_gemma":0.037506785,"teacher_disagreement_score":0.046486966,"about_ca_system_score_codex":0.00077908055,"about_ca_system_score_gemma":0.0005819946,"threshold_uncertainty_score":0.0924328},"labels":[],"label_agreement":null},{"id":"W2028913654","doi":"10.1111/jmg.12082","title":"An electron‐optical study of melt‐related microstructures in granulite facies rocks from the Torngat Orogen","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Memorial University of Newfoundland","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Natural Sciences and Engineering Research Council of Canada","keywords":"Cordierite; Plagioclase; Quartz; Geology; Granulite; Metamorphism; Gneiss; Sillimanite; Mineralogy; Geochemistry; Crystallization; Mineral; Metamorphic rock; Materials science; Facies; Composite material; Chemical engineering; Metallurgy; Ceramic","score_opus":0.007128996489774067,"score_gpt":0.20229703392095305,"score_spread":0.195168037431179,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028913654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909043,0.00006273559,0.00008729958,0.000003260127,6.595634e-7,0.000004349425,0.000100059005,0.0000074796185,0.0006437659],"genre_scores_gemma":[0.99875975,0.00005592716,0.00033233175,0.000005517997,0.0000022262896,0.000003055283,0.0003065504,0.000007571452,0.0005271361],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994814,0.0000024160636,0.0000021942,0.000018072931,0.000012897702,0.000016391938],"domain_scores_gemma":[0.9999199,0.000010519715,0.000022921427,0.0000064086194,0.000024622783,0.000015651522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007893093,0.0002072233,0.0001356634,0.0010121559,0.0003912497,0.00033288373,0.00018969462,0.00019887816,0.0013422046],"category_scores_gemma":[0.000116344796,0.0001727543,0.00012949678,0.00041282328,0.00033837953,0.0001493537,0.00019475594,0.00010943218,0.00022110924],"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":[0.00033701764,0.000046897014,0.21198015,0.00008385833,0.000055395267,0.00091421197,0.0012815443,0.00017661216,0.7759876,0.00009123176,0.00006230402,0.008983149],"study_design_scores_gemma":[0.000002265221,0.000044462187,0.99351597,0.0000021622536,0.000008892472,0.00028744328,0.00021078391,0.00013538991,0.0053543337,0.0000069563766,0.00042975275,0.000001508715],"about_ca_topic_score_codex":0.014542151,"about_ca_topic_score_gemma":0.02485612,"teacher_disagreement_score":0.014542151,"about_ca_system_score_codex":0.000441401,"about_ca_system_score_gemma":0.00014343196,"threshold_uncertainty_score":0.028915048},"labels":[],"label_agreement":null},{"id":"W2045994816","doi":"10.1111/j.1525-1314.2006.00668.x","title":"Oxidized eclogites and garnet‐blueschists from Oman: <i>P–T</i> path modelling in the NCFMASHO system","year":2006,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":93,"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 Environment Research Council; Killam Trusts; Dalhousie University","keywords":"Eclogite; Omphacite; Geology; Lawsonite; Glaucophane; Blueschist; Amphibole; Phengite; Pyroxene; Epidote; Metamorphic rock; Geochemistry; Mafic; Albite; Mineral; Subduction; Quartz; Olivine; Seismology; Tectonics; Chlorite; Paleontology","score_opus":0.010662254032380613,"score_gpt":0.1638191234112194,"score_spread":0.1531568693788388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045994816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980896,0.00001419446,0.000428516,0.000009828418,0.0000016355204,0.000010609059,0.0004949097,0.000030448426,0.00092017255],"genre_scores_gemma":[0.9973792,0.000028948256,0.0013691903,0.0000064163996,0.0000018477062,0.000031929565,0.0008146704,0.00001780001,0.0003498593],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999553,0.00000742688,0.0000029688358,0.000012863129,0.000008778445,0.000012609174],"domain_scores_gemma":[0.9999281,0.000025363765,0.000010250721,0.0000075283374,0.000019857958,0.00000879776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014493409,0.0003970045,0.00022805916,0.00048550416,0.00052386307,0.00046301738,0.000514352,0.0005874145,0.0016393336],"category_scores_gemma":[0.00027808954,0.00025130154,0.0005403895,0.00046204365,0.0002497854,0.00026113456,0.00029473478,0.00015382795,0.00022281434],"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":[0.00033560937,0.000119758755,0.10027373,0.00016985883,0.00010386639,0.0003729409,0.0003955314,0.8663727,0.02292879,0.0010145917,0.00042762168,0.0074850377],"study_design_scores_gemma":[0.00006235896,0.00006834704,0.045457657,0.000008734041,0.00002836733,0.00005165831,0.00016479532,0.94987917,0.0029075323,0.00023810868,0.001116539,0.000016702046],"about_ca_topic_score_codex":0.05806996,"about_ca_topic_score_gemma":0.055148114,"teacher_disagreement_score":0.05806996,"about_ca_system_score_codex":0.0011604141,"about_ca_system_score_gemma":0.00073083484,"threshold_uncertainty_score":0.11546385},"labels":[],"label_agreement":null},{"id":"W2052188270","doi":"10.1046/j.1525-1314.2003.00413.x","title":"Petrological and geochronological constraints on high pressure, high temperature metamorphism in the Snowbird tectonic zone, Canada","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":108,"is_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":"Granulite; Metamorphism; Zircon; Geology; Mafic; Geochemistry; Petrology; Geomorphology; Facies","score_opus":0.011216618415422937,"score_gpt":0.1710529901786304,"score_spread":0.15983637176320747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052188270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916152,0.00028393086,0.00012957443,0.000079413134,0.0000037674502,0.0000113046735,0.0018264744,0.000019374029,0.0060310946],"genre_scores_gemma":[0.9974606,0.00014939735,0.00025157904,0.000011390035,0.0000011536531,0.0000033440176,0.0008212957,0.000007841048,0.0012933648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998306,0.0000065539684,0.000006102379,0.000029133818,0.000059466383,0.000068119014],"domain_scores_gemma":[0.99955374,0.000017845523,0.000049806364,0.000011458511,0.00028822015,0.00007886755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015398189,0.0002443686,0.00016255496,0.0022383824,0.002237871,0.0010269597,0.0004907451,0.00018458822,0.0021457963],"category_scores_gemma":[0.00042637123,0.00020106397,0.00018727797,0.0027118023,0.0006215382,0.00019500473,0.0004577909,0.00021249312,0.00023966971],"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":[0.0001783882,0.000021660748,0.96777076,0.00005245284,0.000073620315,0.0003572698,0.0016072673,0.0012528719,0.011469851,0.00084009394,0.0012333769,0.01514232],"study_design_scores_gemma":[0.0000034205984,0.000004850712,0.9968733,0.0000115539815,0.000007410926,0.00004146354,0.00069898367,0.00040838716,0.00031339942,0.000027252787,0.0016063,0.0000037534835],"about_ca_topic_score_codex":0.9909807,"about_ca_topic_score_gemma":0.99797314,"teacher_disagreement_score":0.017601147,"about_ca_system_score_codex":0.017601147,"about_ca_system_score_gemma":0.01151612,"threshold_uncertainty_score":0.12770587},"labels":[],"label_agreement":null},{"id":"W2053262695","doi":"10.1111/j.1525-1314.2006.00647.x","title":"Shape, size, spatial distribution and composition of garnet crystals in highly deformed gneiss of the Otter Lake area, Québec, and a model for garnet crystallization","year":2006,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Gneiss; Geology; Crystallization; Nucleation; Kyanite; Mineralogy; Metamorphic rock; Geochemistry; Crystallography; Chemistry","score_opus":0.009431427710597856,"score_gpt":0.18471017366180023,"score_spread":0.17527874595120238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053262695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891996,0.000048633017,0.0001808189,0.000016822596,7.079748e-7,0.000009505375,0.000245402,0.00000994634,0.00056828733],"genre_scores_gemma":[0.9989735,0.000027333026,0.00022877283,0.0000061422966,4.6061203e-7,0.0000042132733,0.0002800469,0.000003998344,0.00047545903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999131,0.0000059985678,0.0000036179008,0.000032661377,0.000020469672,0.000024196599],"domain_scores_gemma":[0.9998429,0.000025085596,0.000029624967,0.000009194759,0.000066671375,0.000026557193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013390779,0.00026267272,0.00019094239,0.0010271505,0.0007732976,0.0006055067,0.0006161145,0.0002733167,0.0014893387],"category_scores_gemma":[0.00027801294,0.00014312852,0.00019383723,0.0007261636,0.00081890257,0.00020015101,0.00015529065,0.0001138665,0.00015675859],"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":[0.00042826834,0.00004987132,0.7870352,0.00007463389,0.00006410179,0.0006135626,0.0010410137,0.006703324,0.19691958,0.00048389682,0.00035801693,0.006228377],"study_design_scores_gemma":[0.000008065601,0.000028520222,0.98715997,0.000003957611,0.00001138439,0.00007944763,0.0004895985,0.0083023,0.0033711188,0.000046331978,0.00048831874,0.000010980007],"about_ca_topic_score_codex":0.9043705,"about_ca_topic_score_gemma":0.93738955,"teacher_disagreement_score":0.09562951,"about_ca_system_score_codex":0.008650039,"about_ca_system_score_gemma":0.0019654986,"threshold_uncertainty_score":0.19238532},"labels":[],"label_agreement":null},{"id":"W2053601550","doi":"10.1111/jmg.12104","title":"A comment on diffusion and the displacement of atoms in metamorphic transformations","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Plagioclase; Geology; Olivine; Hornblende; Metamorphic rock; Crystallization; Spinel; Geochemistry; Mineralogy; Biotite; Quartz; Thermodynamics","score_opus":0.009626707746907399,"score_gpt":0.19556280654269886,"score_spread":0.18593609879579145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053601550","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021962387,0.057299044,0.058698904,0.73999274,0.07081074,0.000063466105,0.0017219912,0.0008914045,0.04855938],"genre_scores_gemma":[0.49465665,0.039327428,0.027762596,0.24165572,0.09980438,0.0002776977,0.0005426922,0.0011326112,0.09484021],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9977945,0.0004534008,0.00027006143,0.0006916145,0.00061463594,0.00017586043],"domain_scores_gemma":[0.99395645,0.004444385,0.00034377887,0.00047737686,0.00063361356,0.00014446415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003187067,0.0005933894,0.0008433448,0.00075001974,0.0024428312,0.0018232466,0.004409527,0.005450797,0.006418854],"category_scores_gemma":[0.012224705,0.00047888554,0.0012449909,0.00094860815,0.009755488,0.009175096,0.0017547456,0.009483786,0.0016453008],"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":[0.00025749695,0.000022764512,0.0020155169,0.00089943263,0.000053442127,0.0009469158,0.0016895521,0.0021718282,0.004940619,0.76983833,0.18893737,0.028226681],"study_design_scores_gemma":[0.000055762433,0.00010427247,0.002890693,0.00029476505,0.000024694265,0.0014121014,0.00052366225,0.0038590054,0.0038970355,0.15408564,0.8327571,0.00009524869],"about_ca_topic_score_codex":0.01475819,"about_ca_topic_score_gemma":0.006437666,"teacher_disagreement_score":0.01475819,"about_ca_system_score_codex":0.004009257,"about_ca_system_score_gemma":0.0011141076,"threshold_uncertainty_score":0.029344618},"labels":[],"label_agreement":null},{"id":"W2054302767","doi":"10.1046/j.1525-1314.2000.00235.x","title":"Microstructural tectonometamorphic processes and the development of gneissic layering: a mechanism for metamorphic segregation","year":2000,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Plagioclase; Geology; Igneous rock; Geochemistry; Granulite; Metamorphic rock; Phenocryst; Recrystallization (geology); Feldspar; Hornblende; Quartz; Layering; Partial melting; Crust; Petrology; Melt inclusions; Mantle (geology); Biotite; Facies; Geomorphology","score_opus":0.016523403619100756,"score_gpt":0.20258062196281995,"score_spread":0.1860572183437192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054302767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966433,0.00015923972,0.00071334484,0.000046126144,0.0000011513168,0.000013361402,0.00010235407,0.000027525166,0.0022935255],"genre_scores_gemma":[0.9988661,0.00004878308,0.00034763393,0.000007717279,5.792393e-7,0.000004048139,0.00005063425,0.00000437704,0.00067012],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999201,0.000007627682,0.0000070495435,0.000028963084,0.000014660135,0.00002159618],"domain_scores_gemma":[0.99987566,0.000010271398,0.000045336394,0.000015010817,0.000034877175,0.000018815506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011615735,0.00021240237,0.00014675222,0.0007856487,0.00043024198,0.00078178616,0.00044853255,0.00034185237,0.0008692979],"category_scores_gemma":[0.0002648053,0.00025525672,0.00010833492,0.0005712387,0.0009687916,0.0003444781,0.00045006344,0.00018035616,0.0001919449],"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":[0.00035354224,0.000032658936,0.47324464,0.00012496105,0.00007698407,0.0010347357,0.0014102741,0.0042566005,0.49684614,0.0039860443,0.000180591,0.018452844],"study_design_scores_gemma":[0.000010256138,0.000035905206,0.9876699,0.000008584244,0.000014518405,0.00023461998,0.00045754787,0.001864853,0.008399401,0.0004288499,0.0008634278,0.000012317135],"about_ca_topic_score_codex":0.076592475,"about_ca_topic_score_gemma":0.15939969,"teacher_disagreement_score":0.076592475,"about_ca_system_score_codex":0.002192999,"about_ca_system_score_gemma":0.0008119472,"threshold_uncertainty_score":0.15229332},"labels":[],"label_agreement":null},{"id":"W2055139052","doi":"10.1046/j.1525-1314.2003.00414.x","title":"Metamorphic textures and <i>P–T</i> evolution of high‐<i>P</i> granulites from the Lelukuau terrane, NE Grenville Province","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Kyanite; Granulite; Geology; Geochemistry; Plagioclase; Anorthosite; Igneous rock; Metamorphic rock; Metamorphism; Terrane; Petrology; Quartz; Geomorphology; Tectonics; Facies; Paleontology","score_opus":0.011372174644678558,"score_gpt":0.16579436692577187,"score_spread":0.15442219228109333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055139052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982175,0.000052553016,0.000039518778,0.0000097821985,7.806881e-7,0.000005831088,0.00024550935,0.00002099315,0.0014074731],"genre_scores_gemma":[0.99914443,0.00002079733,0.00009318236,0.0000066208563,7.6036036e-7,0.0000039798565,0.00037953013,0.0000091257125,0.00034154585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988484,0.000006618279,0.0000070804153,0.000049211423,0.00002573533,0.000026568974],"domain_scores_gemma":[0.99989426,0.000010621736,0.000033516222,0.000008040472,0.000029814806,0.000023729279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009476721,0.00017638116,0.00011978096,0.0010166576,0.00039173447,0.00068149477,0.00037066478,0.0002773508,0.0013618798],"category_scores_gemma":[0.0001786528,0.00014179171,0.00011817212,0.00046084172,0.00042785672,0.00016102337,0.00024802948,0.00017359643,0.0003438121],"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":[0.0003418571,0.000054342046,0.5786249,0.00006711589,0.00007341744,0.0008460775,0.0011584974,0.0007557209,0.40587148,0.00019797565,0.00036526332,0.011643365],"study_design_scores_gemma":[0.0000039687447,0.0000151867625,0.9972275,0.000002500775,0.0000036378012,0.00013299794,0.00013663407,0.00013859766,0.0018503929,0.0000058835594,0.0004799815,0.0000027174044],"about_ca_topic_score_codex":0.10576863,"about_ca_topic_score_gemma":0.15968713,"teacher_disagreement_score":0.10576863,"about_ca_system_score_codex":0.0011565093,"about_ca_system_score_gemma":0.00024392632,"threshold_uncertainty_score":0.21030593},"labels":[],"label_agreement":null},{"id":"W2057104287","doi":"10.1111/j.1525-1314.2005.00611.x","title":"Calcite–graphite isotope thermometry in amphibolite facies marble, Bancroft, Ontario","year":2005,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"University of Massachusetts","keywords":"Calcite; Geology; Hornblende; Dolomite; Biotite; Metamorphic rock; Tremolite; Geochemistry; Metamorphic facies; Quartz; Mineralogy; Titanite; Facies; Materials science; Geomorphology; Asbestos","score_opus":0.012677456618610316,"score_gpt":0.19601999727424974,"score_spread":0.18334254065563943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057104287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99396694,0.00023047999,0.00026226626,0.000025241618,0.0000019905674,0.000013751509,0.000804732,0.000022100276,0.004672467],"genre_scores_gemma":[0.9958045,0.00013348254,0.00032025986,0.000008590999,9.724685e-7,0.00000599347,0.00044468345,0.000009413912,0.0032721008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984527,0.00000594759,0.000004490723,0.000038395276,0.00006952022,0.000036390105],"domain_scores_gemma":[0.9997445,0.000012476661,0.000034602403,0.000010303131,0.00016019303,0.000037995553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011039001,0.00020833312,0.0001675551,0.0013201438,0.001396395,0.0005943613,0.0003992896,0.0001042509,0.0019058862],"category_scores_gemma":[0.00026930735,0.00020619942,0.0001232027,0.0010531733,0.00047276876,0.00013748961,0.00023374884,0.00011077193,0.00027374463],"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":[0.00033582334,0.000019740823,0.8840199,0.00010898753,0.00007548942,0.00048241107,0.0033350405,0.0003975599,0.08775179,0.00031487734,0.0006143518,0.022543993],"study_design_scores_gemma":[0.000002645606,0.00001014922,0.9954964,0.000007242675,0.000006379003,0.00005862437,0.0004840682,0.00011879018,0.00175714,0.000012377382,0.0020430563,0.0000031549155],"about_ca_topic_score_codex":0.9460394,"about_ca_topic_score_gemma":0.99165994,"teacher_disagreement_score":0.05396062,"about_ca_system_score_codex":0.0062207407,"about_ca_system_score_gemma":0.0033246027,"threshold_uncertainty_score":0.10855675},"labels":[],"label_agreement":null},{"id":"W2060298519","doi":"10.1111/jmg.12108","title":"Constraining the conditions of Barrovian metamorphism in Sikkim, India: <i>P</i>–<i>T</i>–<i>t</i> paths of garnet crystallization in the Lesser Himalayan Belt","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; Ruhr-Universität Bochum","keywords":"Metamorphic rock; Metamorphism; Staurolite; Geology; Isograd; Main Central Thrust; Geochemistry; Clockwise; Mineralogy; Kyanite; Fold (higher-order function); Geomorphology; Metamorphic facies; Structural basin","score_opus":0.011568893501299523,"score_gpt":0.20373003893767064,"score_spread":0.1921611454363711,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060298519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948573,0.000009298623,0.00014940258,0.000006693428,3.8932643e-7,0.000002736007,0.000053317992,0.000010458312,0.0002820656],"genre_scores_gemma":[0.9997689,0.000008693355,0.000114648756,0.0000014767438,3.362807e-7,0.0000026382302,0.00006817596,0.000003576528,0.00003156433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999279,0.000011414127,0.000005355982,0.000023856875,0.000009994867,0.000021465345],"domain_scores_gemma":[0.9998989,0.000043775,0.000016472946,0.000012488886,0.000015262878,0.000013135833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016547501,0.0003863079,0.00020434883,0.000660915,0.00045009353,0.0006502359,0.00050186843,0.00033254563,0.000752623],"category_scores_gemma":[0.0004880211,0.0003327216,0.00037733346,0.00045739464,0.00043712393,0.0002468706,0.0004109639,0.00022313494,0.00018933628],"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":[0.00065464363,0.00011130369,0.7063878,0.00020296864,0.00017055476,0.0008217804,0.0012815981,0.12701426,0.15166028,0.0014504001,0.00016835662,0.010076047],"study_design_scores_gemma":[0.0000571372,0.0001331981,0.84149736,0.000015945565,0.000086260115,0.00017582082,0.00063686614,0.13823749,0.018368855,0.0003005415,0.00045433073,0.00003622259],"about_ca_topic_score_codex":0.06156515,"about_ca_topic_score_gemma":0.06571663,"teacher_disagreement_score":0.06156515,"about_ca_system_score_codex":0.0009779698,"about_ca_system_score_gemma":0.00067313924,"threshold_uncertainty_score":0.122413635},"labels":[],"label_agreement":null},{"id":"W2069558153","doi":"10.1046/j.0263-4929.2001.00326.x","title":"Neoproterozoic high‐pressure/low‐temperature metamorphic rocks in the Avalon terrane, southern New Brunswick, Canada","year":2001,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Technical University of Nova Scotia; Acadia University; Dalhousie University","funders":"","keywords":"Terrane; Geology; Metamorphic rock; Schist; Metamorphism; Geochemistry; Sedimentary rock; Volcanic rock; Detritus; Pillow lava; Petrology; Volcano; Paleontology; Tectonics","score_opus":0.009239658294922315,"score_gpt":0.1769667597401275,"score_spread":0.16772710144520517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069558153","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873346,0.0009944061,0.00012336692,0.00021023556,0.00000942694,0.000039350267,0.0023030308,0.00003148841,0.008954057],"genre_scores_gemma":[0.9919499,0.00056848454,0.0003858334,0.00007542592,0.0000028990855,0.000015453541,0.0013324867,0.000011149956,0.0056583313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998311,0.0000058048577,0.00000851767,0.000037160993,0.00006117156,0.000056278684],"domain_scores_gemma":[0.9996153,0.000018191986,0.000045714416,0.000009441821,0.00024043614,0.00007082589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015334599,0.000251804,0.00014712631,0.0020602823,0.0020834366,0.0011005301,0.0005730838,0.00019328484,0.0031793523],"category_scores_gemma":[0.00028727253,0.0002640875,0.00014836932,0.0020331396,0.00072701357,0.00030091256,0.00061490724,0.00029573598,0.00031274252],"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":[0.00013156401,0.000034475594,0.9433167,0.0001607285,0.000076765944,0.0009894272,0.0030202398,0.00061735016,0.016682705,0.0008599703,0.0025981127,0.03151208],"study_design_scores_gemma":[0.0000065572976,0.0000075089147,0.9941263,0.000036755842,0.0000063666644,0.00009595145,0.0014194426,0.00016473848,0.00035647315,0.000037608468,0.0037362413,0.000006122043],"about_ca_topic_score_codex":0.98751163,"about_ca_topic_score_gemma":0.99802244,"teacher_disagreement_score":0.01770378,"about_ca_system_score_codex":0.01770378,"about_ca_system_score_gemma":0.010920993,"threshold_uncertainty_score":0.12845051},"labels":[],"label_agreement":null},{"id":"W2074032067","doi":"10.1111/jmg.12083","title":"Anatectic record and contrasting <i>P–T</i> paths of aluminous gneisses from the central Grenville Province","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Anatexis; Sillimanite; Kyanite; Gneiss; Geochemistry; Felsic; Metamorphic rock; Biotite; Grossular; Granulite; Metamorphism; Andalusite; Partial melting; Petrology; Quartz; Mafic; Crust; Facies; Geomorphology; Paleontology","score_opus":0.008719356803497582,"score_gpt":0.1692555493990057,"score_spread":0.1605361925955081,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074032067","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973749,0.00015959176,0.00010689059,0.000022976048,0.0000021733326,0.0000070501915,0.00045386216,0.000024257826,0.0018484211],"genre_scores_gemma":[0.9987551,0.000043679247,0.00021316872,0.000011655928,0.0000016912394,0.000004712269,0.0005664157,0.000010042845,0.0003934799],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997552,0.000020999896,0.000018916146,0.00010747441,0.00005367034,0.000043730535],"domain_scores_gemma":[0.99976414,0.000027785538,0.00005870934,0.00001918143,0.000099573226,0.00003059238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023463798,0.00025516184,0.0002484278,0.0020524345,0.00051963737,0.0007886182,0.0008046244,0.00037179174,0.0011524019],"category_scores_gemma":[0.0003418203,0.00018074333,0.00020210804,0.0009715141,0.0006741115,0.00023722193,0.00052450935,0.0001869183,0.00041636566],"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":[0.0003162561,0.000054130178,0.78725916,0.00012841978,0.00022063564,0.00070917635,0.002301757,0.0006854344,0.18560688,0.00027136604,0.00031251527,0.022134313],"study_design_scores_gemma":[0.0000042966235,0.000018779238,0.9975648,0.000008316245,0.000007885822,0.00016735164,0.00036258923,0.00013507942,0.0009748599,0.000016394151,0.000734439,0.0000052671007],"about_ca_topic_score_codex":0.26154655,"about_ca_topic_score_gemma":0.38998464,"teacher_disagreement_score":0.26154655,"about_ca_system_score_codex":0.0012739282,"about_ca_system_score_gemma":0.00044243142,"threshold_uncertainty_score":0.5200484},"labels":[],"label_agreement":null},{"id":"W2074400419","doi":"10.1111/j.1525-1314.2006.00633.x","title":"Dating metamorphic reactions and fluid flow: application to exhumation of high‐<i>P</i> granulites in a crustal‐scale shear zone, western Canadian Shield","year":2006,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":172,"is_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":"Granulite; Monazite; Geology; Geochemistry; Metamorphism; Felsic; Shear zone; Metamorphic facies; Mafic; Metamorphic rock; Population; Facies; Migmatite; Petrology; Zircon; Gneiss; Geomorphology; Tectonics; Paleontology; Structural basin","score_opus":0.008354181432704999,"score_gpt":0.19233273690687966,"score_spread":0.18397855547417466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074400419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652135,0.00016578026,0.0009608553,0.000022772156,0.0000025325933,0.000036163474,0.0006037201,0.00006838853,0.0016185967],"genre_scores_gemma":[0.99568236,0.00018498197,0.0029713304,0.000013457139,0.0000014523705,0.000010650753,0.00029528758,0.000016168708,0.000824299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982184,0.000003831169,0.0000059382805,0.00004685998,0.00008419872,0.00003736524],"domain_scores_gemma":[0.99982965,0.000009973244,0.000020468764,0.000006105907,0.00010525354,0.000028460698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018110148,0.00032193091,0.00014331848,0.0017258889,0.0014762431,0.000634493,0.00044831535,0.00023641156,0.000683307],"category_scores_gemma":[0.00032936645,0.00022263468,0.00015004343,0.0011989361,0.0005546663,0.0001459551,0.00028765103,0.00020245078,0.00012216864],"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":[0.00019874031,0.000043244894,0.5263625,0.00009888778,0.00005779383,0.0003139328,0.0017420524,0.0022471698,0.43425742,0.00019418169,0.0002851697,0.034198914],"study_design_scores_gemma":[0.0000046824407,0.000024322446,0.9690007,0.000008202069,0.000016698776,0.00010690687,0.00038295137,0.002631832,0.026587997,0.00001926719,0.0012070251,0.000009372525],"about_ca_topic_score_codex":0.87923765,"about_ca_topic_score_gemma":0.95309603,"teacher_disagreement_score":0.12076235,"about_ca_system_score_codex":0.004581267,"about_ca_system_score_gemma":0.0028281948,"threshold_uncertainty_score":0.24294704},"labels":[],"label_agreement":null},{"id":"W2076612985","doi":"10.1111/j.1525-1314.2007.00729.x","title":"Permian to Cretaceous polymetamorphic evolution of the Stewart River region, Yukon‐Tanana terrane, Yukon, Canada:<i>P–T</i>evolution linked with<i>in situ</i>SHRIMP monazite geochronology","year":2007,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Plutonism; Geology; Terrane; Metamorphism; Monazite; Geochemistry; Geochronology; Zircon; Back-arc basin; Pluton; Subduction; Paleontology; Tectonics","score_opus":0.007963945944734128,"score_gpt":0.1766748552920998,"score_spread":0.16871090934736568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076612985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819297,0.00011057314,0.000044397217,0.000028116277,0.0000014407694,0.0000045567485,0.00034308952,0.000010349676,0.0012645547],"genre_scores_gemma":[0.9988919,0.00007479869,0.000090616624,0.000008185527,5.7926144e-7,0.0000031578577,0.0003647214,0.0000053414196,0.0005607134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999163,0.0000038640433,0.0000052117125,0.00002658119,0.000019485566,0.00002856111],"domain_scores_gemma":[0.99976355,0.000012198546,0.000031589487,0.000009067489,0.000145789,0.000037886457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120002056,0.000228586,0.00015945986,0.0011817646,0.001001003,0.0006503233,0.0003866282,0.00022593039,0.0016522604],"category_scores_gemma":[0.00019590599,0.00017474899,0.00017088972,0.001283152,0.00049321464,0.00019328135,0.00040720514,0.00017571995,0.0001679593],"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":[0.000112101305,0.0000228342,0.9393745,0.00008242075,0.00011645558,0.0005378331,0.002436654,0.0008235845,0.04025086,0.00051731116,0.0005934679,0.015131916],"study_design_scores_gemma":[0.0000027117023,0.0000066303955,0.99814034,0.000005208691,0.000008314673,0.000055947512,0.00058907096,0.00016258185,0.00027976185,0.0000116106885,0.00073488784,0.0000029481491],"about_ca_topic_score_codex":0.8425556,"about_ca_topic_score_gemma":0.943004,"teacher_disagreement_score":0.15744442,"about_ca_system_score_codex":0.004404675,"about_ca_system_score_gemma":0.0040880484,"threshold_uncertainty_score":0.31674325},"labels":[],"label_agreement":null},{"id":"W2077479198","doi":"10.1046/j.1525-1314.2003.00420.x","title":"High‐pressure granulites: formation, recovery of peak conditions and implications for tectonics","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":572,"is_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":"Granulite; Kyanite; Geology; Geochemistry; Felsic; Plagioclase; Eclogite; Petrology; Crust; Continental crust; Metamorphic rock; Mafic; Quartz; Facies; Subduction; Tectonics; Geomorphology; Seismology","score_opus":0.020532549201120853,"score_gpt":0.21022340300719355,"score_spread":0.1896908538060727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077479198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941856,0.0008718215,0.00047840422,0.00007150763,0.0000053977737,0.000016924676,0.0003463449,0.0000547713,0.003969249],"genre_scores_gemma":[0.9991128,0.00012352676,0.00014141707,0.0000061088826,0.0000065247377,0.0000020698972,0.0001329862,0.0000073140045,0.00046728074],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998462,0.000014405384,0.000012116097,0.00005299154,0.00003380615,0.00004030096],"domain_scores_gemma":[0.99968636,0.000037186423,0.00013960137,0.00003351705,0.000050163744,0.000053227992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024317324,0.00019722941,0.0001746677,0.000946625,0.00030857304,0.0010832524,0.00051413383,0.0004619571,0.0027836056],"category_scores_gemma":[0.00042881892,0.00018968758,0.00012425201,0.00082831073,0.00089209864,0.0006711073,0.00048169584,0.00023159852,0.0004227661],"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":[0.0014591044,0.00018203243,0.55406696,0.00048708735,0.00012373854,0.0019507795,0.0009862997,0.0027498845,0.38675717,0.003194889,0.0005038458,0.04753827],"study_design_scores_gemma":[0.000012209269,0.000076899676,0.9906213,0.000006925335,0.000008486061,0.00053538167,0.00013506989,0.0008475943,0.0064367703,0.00029045643,0.0010230513,0.0000058649357],"about_ca_topic_score_codex":0.0037257134,"about_ca_topic_score_gemma":0.0022434199,"teacher_disagreement_score":0.0037257134,"about_ca_system_score_codex":0.000746647,"about_ca_system_score_gemma":0.00017283307,"threshold_uncertainty_score":0.009312034},"labels":[],"label_agreement":null},{"id":"W2077969584","doi":"10.1111/j.1525-1314.2007.00728.x","title":"Using estimated thermodynamic properties to model accessory phases: the case of tourmaline","year":2007,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"McGill University","funders":"University of Bristol","keywords":"Tourmaline; Mineral; Mineralogy; Hydrothermal circulation; Polyhedron; Geology; Phase (matter); Thermodynamics; Materials science; Geochemistry; Chemistry; Physics; Mathematics","score_opus":0.1006775503725876,"score_gpt":0.29519777058033625,"score_spread":0.19452022020774865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077969584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9429686,0.00017420844,0.053518936,0.000034063964,0.000004588328,0.00002894464,0.0005393361,0.00016096595,0.0025704203],"genre_scores_gemma":[0.99175686,0.000056017314,0.007623765,0.000002948859,8.8041577e-7,0.000013645325,0.00016875434,0.000025509044,0.00035160524],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993193,0.000016161674,0.0000045098723,0.000018603872,0.000020780597,0.000007983497],"domain_scores_gemma":[0.9998411,0.000065806846,0.000026091711,0.000022955539,0.000037283942,0.000006653847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016937265,0.00034065061,0.00017646865,0.00059279666,0.00018260133,0.0004192183,0.00041063986,0.00031763202,0.0006739612],"category_scores_gemma":[0.00066537503,0.00014898501,0.00030197072,0.0003326081,0.0002342917,0.00035332827,0.00026015964,0.0001808454,0.00016859906],"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":[0.00022565416,0.000031179035,0.047176182,0.00019408429,0.00006766468,0.000430486,0.00014274279,0.82182825,0.103836566,0.0038008578,0.00020851733,0.022057757],"study_design_scores_gemma":[0.000007418373,0.000039948332,0.009682735,0.000008109681,0.000012881411,0.00008745169,0.00004272453,0.95567507,0.03244901,0.0007929675,0.0011861391,0.00001552198],"about_ca_topic_score_codex":0.010272121,"about_ca_topic_score_gemma":0.009104444,"teacher_disagreement_score":0.010272121,"about_ca_system_score_codex":0.00041182022,"about_ca_system_score_gemma":0.00027860224,"threshold_uncertainty_score":0.020424664},"labels":[],"label_agreement":null},{"id":"W2081129468","doi":"10.1111/j.1525-1314.2008.00788.x","title":"Phase equilibria modelling of kyanite‐bearing anatectic paragneisses from the central Grenville Province","year":2008,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":155,"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; University of Melbourne","keywords":"Kyanite; Grossular; Geology; Solidus; Metamorphic rock; Anatexis; Partial melting; Geochemistry; Muscovite; Mineral; Biotite; Mineralogy; Quartz; Crust; Materials science","score_opus":0.04780677266622697,"score_gpt":0.21403842465592024,"score_spread":0.16623165198969328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081129468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975231,0.000024699704,0.00066742103,0.000010122354,0.0000010395621,0.000016847556,0.00042416685,0.00005743253,0.0012751136],"genre_scores_gemma":[0.99783677,0.000015132611,0.001020945,0.000004250168,5.015012e-7,0.00001243575,0.00057213235,0.00002044531,0.0005174497],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999349,0.000006102946,0.0000038011758,0.00002476386,0.000016327034,0.000014105394],"domain_scores_gemma":[0.99993026,0.000013862961,0.000010805136,0.0000065080185,0.000032287233,0.0000062108593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012097301,0.0002928427,0.00020463624,0.00097277237,0.00037121517,0.00054472365,0.0007787091,0.00047562076,0.0016259003],"category_scores_gemma":[0.00028115427,0.0002389348,0.0002978156,0.00046748444,0.0001996975,0.00019400845,0.00023562126,0.00014987841,0.0003894516],"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":[0.0008504857,0.00017931646,0.22747311,0.00020183368,0.00013230216,0.0006914663,0.00062087324,0.5460334,0.19443579,0.0010010697,0.000504216,0.027876155],"study_design_scores_gemma":[0.00012644121,0.00017629097,0.17526895,0.000017558887,0.00003672424,0.00014113868,0.00045409516,0.79530865,0.025532965,0.00033111795,0.00257938,0.000026660642],"about_ca_topic_score_codex":0.15626231,"about_ca_topic_score_gemma":0.19105822,"teacher_disagreement_score":0.15626231,"about_ca_system_score_codex":0.0013647388,"about_ca_system_score_gemma":0.0005687282,"threshold_uncertainty_score":0.31070554},"labels":[],"label_agreement":null},{"id":"W2083549999","doi":"10.1111/j.1525-1314.2008.00801.x","title":"Constraints on the early metamorphic evolution of Broken Hill, Australia, from <i>in situ</i> U‐Pb dating and REE geochemistry of monazite","year":2008,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 New Brunswick","funders":"National Science Foundation","keywords":"Monazite; Geology; Granulite; Geochemistry; Metamorphism; Gneiss; Metamorphic rock; Metamorphic facies; Geochronology; Zircon; Facies; Paleontology","score_opus":0.030268820496935054,"score_gpt":0.20654325638572574,"score_spread":0.1762744358887907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083549999","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99645066,0.00017779258,0.00023397758,0.000024061543,0.0000019098711,0.000006168281,0.00008791154,0.000007960712,0.0030095938],"genre_scores_gemma":[0.9988752,0.000074776326,0.00021065491,0.000009594793,8.9381336e-7,0.0000023146197,0.00007364575,0.000003695755,0.0007491613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994314,0.0000052460105,0.00000419626,0.000016530345,0.000018514625,0.000012376572],"domain_scores_gemma":[0.999876,0.000009928646,0.000030200934,0.000008573758,0.000055990473,0.000019255885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012928297,0.00015841507,0.00009624933,0.0006075586,0.0004501233,0.00049790094,0.0002446199,0.00020280878,0.001031886],"category_scores_gemma":[0.0002958389,0.0002036249,0.00009259165,0.00028634668,0.000373018,0.0001967178,0.00038816768,0.0001979523,0.00025332635],"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":[0.00026551113,0.000038217193,0.55098677,0.00020102081,0.00006743783,0.0010221782,0.0037812914,0.0008347462,0.41274676,0.00091526157,0.00032579026,0.028815018],"study_design_scores_gemma":[0.0000024371548,0.000030455183,0.9921267,0.000014782719,0.000008679379,0.00016918634,0.0004425139,0.0005336146,0.0051931734,0.000040470266,0.0014345294,0.000003380319],"about_ca_topic_score_codex":0.07365688,"about_ca_topic_score_gemma":0.20178579,"teacher_disagreement_score":0.07365688,"about_ca_system_score_codex":0.00080121926,"about_ca_system_score_gemma":0.00045531438,"threshold_uncertainty_score":0.1464563},"labels":[],"label_agreement":null},{"id":"W2092838869","doi":"10.1111/j.1525-1314.2008.00790.x","title":"Partial melting of metagreywacke: a calculated mineral equilibria study","year":2008,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":138,"is_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; Solidus; Anatexis; Biotite; Partial melting; Plagioclase; Geochemistry; Protolith; Sillimanite; Muscovite; Alkali feldspar; Feldspar; Pelite; Grossular; Mineralogy; Metamorphism; Quartz; Metamorphic rock; Chemistry; Crust","score_opus":0.03394614292898983,"score_gpt":0.22864018062750732,"score_spread":0.1946940376985175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092838869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99699306,0.00008651886,0.0013147611,0.0000042798233,8.707677e-7,0.000007633766,0.00027891152,0.000027290132,0.0012867143],"genre_scores_gemma":[0.9990409,0.000042780284,0.00039605427,0.0000011784347,4.0994172e-7,0.00000482571,0.00016473878,0.000010569704,0.00033864638],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999492,0.0000044505523,0.0000027472058,0.000019069988,0.000012910809,0.0000116552255],"domain_scores_gemma":[0.9999281,0.000022198072,0.000012002127,0.000007640068,0.000024157973,0.000005804525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000102292724,0.00022338888,0.00023573493,0.0005818182,0.00020224067,0.00028721066,0.00044066424,0.00025843922,0.0025726843],"category_scores_gemma":[0.00032916025,0.00016101157,0.00025296866,0.00033433342,0.00012874082,0.00027221144,0.00023992306,0.00014644525,0.00039271958],"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":[0.0011008214,0.00021108678,0.19340405,0.0005786865,0.00025435776,0.001032121,0.000390513,0.24595408,0.5148175,0.0047700135,0.0004772748,0.037009574],"study_design_scores_gemma":[0.00008488647,0.00038671738,0.14153789,0.000025318104,0.00006557348,0.00031425242,0.00027110448,0.5968491,0.2556007,0.0012119687,0.0036256518,0.000026833162],"about_ca_topic_score_codex":0.007950309,"about_ca_topic_score_gemma":0.007255115,"teacher_disagreement_score":0.007950309,"about_ca_system_score_codex":0.00055089244,"about_ca_system_score_gemma":0.00020140916,"threshold_uncertainty_score":0.015808046},"labels":[],"label_agreement":null},{"id":"W2094265794","doi":"10.1046/j.1525-1314.2003.00446.x","title":"Prograde, peak, and retrograde <i>P–T</i> paths from aluminium in orthopyroxene: High‐temperature contact metamorphism in the aureole of the Makhavinekh Lake Pluton, Nain Plutonic Suite, Labrador","year":2003,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Geology Foundation, University of Texas at Austin; University of Texas at Austin; National Science Foundation","keywords":"Geology; Pluton; Metamorphism; Cordierite; Intrusion; Geochemistry; Zoning; Gneiss; Metamorphic rock; Petrology; Mineralogy; Tectonics; Materials science","score_opus":0.006925564277211082,"score_gpt":0.182415193507484,"score_spread":0.17548962923027292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094265794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999571,0.000024344996,0.000021917278,0.0000034861773,2.361856e-7,0.0000014524416,0.000093630835,0.00000496363,0.00027892584],"genre_scores_gemma":[0.9996985,0.000013260653,0.000038061546,0.0000014878182,4.950097e-7,0.0000012484363,0.00008148826,0.0000023862722,0.00016313193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993515,0.0000032697078,0.0000047113617,0.000023284232,0.000013853314,0.00001969383],"domain_scores_gemma":[0.9999312,0.0000071653844,0.000028917617,0.000004422311,0.000015264332,0.00001291979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000056685032,0.00016344881,0.0001344327,0.0010026246,0.00043308374,0.00042740157,0.00031611245,0.00029248698,0.0008928227],"category_scores_gemma":[0.00012476598,0.00025664622,0.00013471926,0.0007145828,0.00045351047,0.00018901486,0.0002576689,0.00016571487,0.00020099209],"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":[0.00048100547,0.000040841696,0.6997185,0.0000646126,0.00005867859,0.0014441502,0.0017126792,0.00070979615,0.2876983,0.0001259237,0.00011679452,0.007828695],"study_design_scores_gemma":[0.0000021471303,0.00002451638,0.9973979,0.0000019471656,0.0000055692585,0.00015742544,0.00023563472,0.00019887237,0.0018479022,0.000006656179,0.00011955094,0.0000018304564],"about_ca_topic_score_codex":0.033862196,"about_ca_topic_score_gemma":0.06294466,"teacher_disagreement_score":0.9661378,"about_ca_system_score_codex":0.0005910768,"about_ca_system_score_gemma":0.00018286165,"threshold_uncertainty_score":0.06733018},"labels":[],"label_agreement":null},{"id":"W2100410593","doi":"10.1046/j.1525-1314.2003.00475.x","title":"Reactive flow of mixed CO<sub>2</sub>–H<sub>2</sub>O fluid and progress of calc‐silicate reactions in contact metamorphic aureoles: insights from two‐dimensional numerical modelling","year":2003,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"","keywords":"Metamorphic rock; Geology; Silicate; Fluid dynamics; Geochemistry; Diopside; Protolith; Mineralogy; Petrology; Thermodynamics; Chemistry","score_opus":0.017792132088528506,"score_gpt":0.2135106818666423,"score_spread":0.1957185497781138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100410593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972379,0.000021688593,0.0019201969,0.000025223595,0.0000027824053,0.000008253757,0.00010074736,0.000057976187,0.0006252257],"genre_scores_gemma":[0.9982211,0.000026440433,0.0013482461,0.000005649522,0.0000017329901,0.000010935707,0.000082685285,0.000009529337,0.0002935261],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999341,0.000010503314,0.000004400989,0.000021822189,0.000013940013,0.000015252966],"domain_scores_gemma":[0.9998435,0.000057230514,0.00004479805,0.000012343961,0.000018599778,0.000023519948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111028494,0.00038962765,0.00028562386,0.00040907544,0.00031887417,0.0006353671,0.00045606194,0.0011312654,0.0006829935],"category_scores_gemma":[0.00041294078,0.00033326796,0.00042891255,0.00029195013,0.0006000784,0.00041930683,0.00026835795,0.000306901,0.00007877761],"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":[0.00017993902,0.0001832341,0.021010572,0.000041121864,0.000033138786,0.00023493059,0.00015075329,0.840071,0.13481082,0.000950551,0.00011667368,0.0022173368],"study_design_scores_gemma":[0.000016331944,0.000027695334,0.0048400643,0.000002042608,0.000004161531,0.000012505953,0.00002124018,0.9899788,0.0049337796,0.00006735492,0.000086106935,0.000010022821],"about_ca_topic_score_codex":0.018202785,"about_ca_topic_score_gemma":0.008457471,"teacher_disagreement_score":0.018202785,"about_ca_system_score_codex":0.001159898,"about_ca_system_score_gemma":0.0005040786,"threshold_uncertainty_score":0.03619367},"labels":[],"label_agreement":null},{"id":"W2101151367","doi":"10.1111/j.1525-1314.2008.00776.x","title":"Geochronology of high‐pressure mafic granulite dykes in SW Sweden: tracking the <i>P–T–t</i> path of metamorphism using Hf isotopes in zircon and baddeleyite","year":2008,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Sveriges Geologiska Undersökning; Swedish Foundation for International Cooperation in Research and Higher Education; National Science Foundation","keywords":"Zircon; Baddeleyite; Metamorphism; Geology; Geochemistry; Granulite; Metamorphic rock; Geochronology; Mafic; Petrology; Facies; Geomorphology","score_opus":0.02360224252797485,"score_gpt":0.20879856479444142,"score_spread":0.18519632226646657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101151367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99954706,0.0000300918,0.00007990246,0.000002385856,0.0000011173285,0.0000020466655,0.00006861051,0.000006541047,0.00026229557],"genre_scores_gemma":[0.9993862,0.000035380304,0.00024198442,0.0000021170683,8.8435115e-7,0.0000032904447,0.00013042994,0.000004471677,0.00019526409],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998994,0.000009721526,0.000009199295,0.000033632143,0.000025136276,0.000022872046],"domain_scores_gemma":[0.99990785,0.000013244634,0.000023245144,0.000010041385,0.000027635402,0.000018013456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018093594,0.00029467492,0.00023142545,0.0015182622,0.0004404232,0.0007371584,0.00022176882,0.00033697032,0.0003833121],"category_scores_gemma":[0.00019805084,0.00024077873,0.00030720312,0.00066653296,0.000369096,0.00013168124,0.00039274787,0.00013315996,0.00019717844],"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":[0.00029227897,0.000047858517,0.89530015,0.000054125143,0.00009394644,0.00083084696,0.0016771539,0.0013873298,0.09076189,0.000124094,0.00008214339,0.00934809],"study_design_scores_gemma":[0.000003992665,0.000037879865,0.994753,0.000005571769,0.000015124062,0.0001786361,0.00048099732,0.0007351504,0.0033993593,0.000010207982,0.00037665694,0.0000034339776],"about_ca_topic_score_codex":0.032615304,"about_ca_topic_score_gemma":0.06997175,"teacher_disagreement_score":0.032615304,"about_ca_system_score_codex":0.00058490236,"about_ca_system_score_gemma":0.0003354836,"threshold_uncertainty_score":0.06485093},"labels":[],"label_agreement":null},{"id":"W2102198333","doi":"10.1046/j.0263-4929.2000.00312.x","title":"Melt segregation in the continental crust: distribution and movement of melt in anatectic rocks","year":2001,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":372,"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 Chicoutimi","funders":"Natural Sciences and Engineering Research Council of Canada; University of Minnesota","keywords":"Geology; Migmatite; Partial melting; Metamorphic rock; Outcrop; Geochemistry; Granulite; Crust; Gneiss; Petrology; Mineralogy; Geomorphology","score_opus":0.01099625583664922,"score_gpt":0.20203330667852082,"score_spread":0.1910370508418716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102198333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985934,0.0002923519,0.00011589541,0.000007534625,4.990092e-7,0.0000030948295,0.0003067356,0.000012683054,0.00066777656],"genre_scores_gemma":[0.9992532,0.00009782403,0.0001431731,0.000002778738,0.0000011375133,0.0000016669494,0.0003358743,0.000007789039,0.00015639109],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998816,0.000009167498,0.000015089042,0.000046879275,0.00002333647,0.000023755856],"domain_scores_gemma":[0.99984396,0.000015042756,0.000055321296,0.000010986347,0.00005455038,0.000020058988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012726698,0.00022174533,0.0003492957,0.0036223393,0.0005656465,0.00078015967,0.00026010335,0.00030967468,0.0012125566],"category_scores_gemma":[0.00034873205,0.00020107068,0.00026280124,0.0021753698,0.00039097527,0.0003479734,0.0005758269,0.00015765273,0.0003541889],"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":[0.00042969603,0.000030973657,0.8148435,0.00012225646,0.00019478482,0.00022213158,0.0011989038,0.0012524601,0.16463141,0.00014410801,0.00006130509,0.016868584],"study_design_scores_gemma":[0.000002054039,0.000015987987,0.9967236,0.000005027793,0.000013283651,0.000066671855,0.00017353581,0.00063758245,0.0020434689,0.00002389751,0.00029117762,0.0000037066789],"about_ca_topic_score_codex":0.023341589,"about_ca_topic_score_gemma":0.02100949,"teacher_disagreement_score":0.023341589,"about_ca_system_score_codex":0.0007219862,"about_ca_system_score_gemma":0.00018881925,"threshold_uncertainty_score":0.046411455},"labels":[],"label_agreement":null},{"id":"W2102377064","doi":"10.1111/j.1525-1314.2007.00702.x","title":"Accessory phase petrogenesis in relation to major phase assemblages in pelites from the Nelson contact aureole, southern British Columbia","year":2007,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Allanite; Monazite; Geology; Staurolite; Andalusite; Geochemistry; Sillimanite; Batholith; Kyanite; Metamorphic rock; Mineralogy; Biotite; Paleontology; Zircon; Tectonics","score_opus":0.017618662943151547,"score_gpt":0.24979336748323802,"score_spread":0.23217470454008649,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102377064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99677247,0.00010616355,0.00005110887,0.00001555627,0.0000010238226,0.0000099491035,0.00048868445,0.000010660625,0.0025443109],"genre_scores_gemma":[0.99785584,0.00009214242,0.00009036703,0.000009357886,6.0309816e-7,0.0000061764845,0.00032271806,0.0000072845933,0.0016154543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981314,0.00000903288,0.000010344698,0.000041509462,0.000055207383,0.00007073331],"domain_scores_gemma":[0.9994306,0.000028382241,0.000054485143,0.000016547196,0.0003587847,0.000111286834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119242264,0.0002863333,0.0002470107,0.0036189435,0.002371929,0.0013820068,0.00050751586,0.00025910808,0.0030197448],"category_scores_gemma":[0.00044493587,0.00034989027,0.00012128938,0.0031166524,0.0006870597,0.00023591594,0.0006912437,0.00024239504,0.00044331182],"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":[0.00025447842,0.000033261014,0.95019495,0.0000656316,0.00004275493,0.0007710533,0.0032516173,0.00017621253,0.027379146,0.00017032292,0.00045464342,0.017205985],"study_design_scores_gemma":[0.0000018433452,0.000005765947,0.99742883,0.000007184308,0.0000052879777,0.0000878418,0.0011369628,0.000089787114,0.00043739198,0.000007691395,0.000788383,0.0000030567949],"about_ca_topic_score_codex":0.9447747,"about_ca_topic_score_gemma":0.9881493,"teacher_disagreement_score":0.055225313,"about_ca_system_score_codex":0.00730857,"about_ca_system_score_gemma":0.0025716666,"threshold_uncertainty_score":0.11110103},"labels":[],"label_agreement":null},{"id":"W2106418812","doi":"10.1111/j.1525-1314.2011.00958.x","title":"Constraining cooling histories: rutile and titanite chronology and diffusion modelling in NW Bhutan","year":2011,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Titanite; Geology; Granulite; Mafic; Closure temperature; Geochemistry; Massif; Metamorphic facies; Eclogite; Rutile; Thermochronology; Mineral; Facies; Zircon; Geomorphology; Paleontology; Materials science; Tectonics","score_opus":0.03599778415056351,"score_gpt":0.18741587578709243,"score_spread":0.15141809163652892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106418812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988294,0.000046452576,0.0005924983,0.000023033157,0.0000017654871,0.0000052514742,0.00016142985,0.00002420694,0.00031583413],"genre_scores_gemma":[0.99937385,0.000024068693,0.00032272577,0.0000038517433,0.0000013372343,0.000003851512,0.00016160567,0.00000883646,0.000099991135],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999231,0.0000122354495,0.0000051834736,0.000031097195,0.000007344515,0.000021060669],"domain_scores_gemma":[0.99968183,0.00013411272,0.000056529432,0.000032752818,0.00004741245,0.00004735023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034188724,0.00036031567,0.00032341704,0.0009335721,0.0004745174,0.00068768335,0.00089469575,0.00054073497,0.0011488069],"category_scores_gemma":[0.0008171055,0.0005012999,0.00048029653,0.00077564747,0.0004676852,0.00049403333,0.00045954587,0.00029696472,0.00019839803],"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":[0.00040212515,0.00008428133,0.40363556,0.00015544092,0.00017791992,0.0006718382,0.00092496676,0.5510942,0.031180596,0.0011005895,0.00020742313,0.010365049],"study_design_scores_gemma":[0.000059773665,0.000033774213,0.120775186,0.000015864232,0.00003796428,0.00009152712,0.00020374304,0.8756015,0.0023633977,0.0002896234,0.0004970213,0.00003064874],"about_ca_topic_score_codex":0.1650108,"about_ca_topic_score_gemma":0.13372873,"teacher_disagreement_score":0.1650108,"about_ca_system_score_codex":0.0019396814,"about_ca_system_score_gemma":0.0007162293,"threshold_uncertainty_score":0.32810068},"labels":[],"label_agreement":null},{"id":"W2107670992","doi":"10.1111/j.1525-1314.2010.00908.x","title":"Coeval thrusting and extension during lower crustal ductile flow – implications for exhumation of high‐grade metamorphic rocks","year":2010,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":122,"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":"Dalhousie University; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Geology; Foreland basin; Crust; Tectonics; Lithosphere; Metamorphic core complex; Petrology; Geophysics; Geomorphology; Seismology","score_opus":0.018591057294972003,"score_gpt":0.2248294157203586,"score_spread":0.2062383584253866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107670992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99732995,0.000051342984,0.0010555035,0.00006197021,0.0000031169095,0.0000030603683,0.00007947904,0.000036764668,0.0013789006],"genre_scores_gemma":[0.9997123,0.000017628272,0.00009584055,0.0000022499098,9.0987317e-7,0.0000012080272,0.000021433309,0.0000050368753,0.00014336612],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999399,0.000015779107,0.0000049749133,0.000014189101,0.000009109404,0.000016002954],"domain_scores_gemma":[0.99978393,0.000052238025,0.000061575854,0.000034700395,0.000023375303,0.000044149623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017291037,0.00032595874,0.00028992112,0.00037161369,0.00031164332,0.0010910778,0.00049446156,0.0006336144,0.0021119888],"category_scores_gemma":[0.00077848946,0.0002730112,0.00047850385,0.00033358458,0.00070620165,0.00045510347,0.00057704304,0.0003319223,0.00013308215],"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":[0.00027533737,0.00011950822,0.07982414,0.000047706082,0.00008511295,0.00031136558,0.00009694339,0.89000666,0.02205968,0.0033055267,0.00013272977,0.0037353162],"study_design_scores_gemma":[0.000044548477,0.000070885304,0.049192414,0.0000092954415,0.0000242529,0.00006749064,0.000081023914,0.94634026,0.0027614774,0.0012015643,0.00018822445,0.000018598712],"about_ca_topic_score_codex":0.010502453,"about_ca_topic_score_gemma":0.0044234907,"teacher_disagreement_score":0.010502453,"about_ca_system_score_codex":0.0006684914,"about_ca_system_score_gemma":0.0003048716,"threshold_uncertainty_score":0.020882666},"labels":[],"label_agreement":null},{"id":"W2108250056","doi":"10.1111/jmg.12042","title":"A window into the Early to mid‐Cretaceous infrastructure of the Yukon‐Tanana terrane recorded in multi‐stage garnet of west‐central Yukon, <scp>C</scp>anada","year":2013,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"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; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Kyanite; Monazite; Geochemistry; Metamorphism; Metamorphic rock; Staurolite; Schist; Terrane; Stage (stratigraphy); Grossular; Paleontology; Zircon; Tectonics","score_opus":0.012073972450572873,"score_gpt":0.19705442214198626,"score_spread":0.1849804496914134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108250056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99815744,0.00013494548,0.000051804214,0.000017460086,0.0000016409923,0.0000027640046,0.00024735654,0.000006511522,0.0013800809],"genre_scores_gemma":[0.99939847,0.000045486733,0.00004568663,0.0000059723907,7.955953e-7,0.0000023360956,0.0001842371,0.0000034402624,0.00031351176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999478,0.000003460678,0.0000035090934,0.000016768496,0.000007901365,0.000020649455],"domain_scores_gemma":[0.9998628,0.000013508383,0.000027339831,0.000008101741,0.00006249764,0.000025805393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008509953,0.00018000552,0.00013307632,0.0010264497,0.0007518536,0.0005528993,0.00022460881,0.00025683572,0.0015896979],"category_scores_gemma":[0.00017184431,0.00014806418,0.00012635163,0.0010110995,0.0004626047,0.000244758,0.00040350156,0.00016649443,0.00017309083],"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":[0.00018780753,0.000019795107,0.8958879,0.000115712806,0.000070369075,0.00095712126,0.0066503463,0.0004718766,0.080209985,0.00066636654,0.0005190264,0.0142437145],"study_design_scores_gemma":[8.255669e-7,0.0000049824152,0.99848384,0.000004383572,0.0000038103335,0.000058796315,0.00067102374,0.000063830405,0.00020270854,0.000010602193,0.00049282896,0.0000023270477],"about_ca_topic_score_codex":0.3122194,"about_ca_topic_score_gemma":0.6428851,"teacher_disagreement_score":0.6877806,"about_ca_system_score_codex":0.0011984593,"about_ca_system_score_gemma":0.00094329566,"threshold_uncertainty_score":0.6208042},"labels":[],"label_agreement":null},{"id":"W2110327848","doi":"10.1111/jmg.12032","title":"An automated method for the calculation of <i>P–T</i> paths from garnet zoning, with application to metapelitic schist from the Kootenay Arc, British Columbia, Canada","year":2013,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Yukon University; University of Calgary","funders":"","keywords":"Schist; Geology; Staurolite; Zoning; Pelite; Fractional crystallization (geology); Geochemistry; Metamorphic facies; Diachronous; Mineralogy; Metamorphic rock; Facies; Law; Seismology; Tectonics; Geomorphology","score_opus":0.006173517365086481,"score_gpt":0.2017305256336789,"score_spread":0.19555700826859243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110327848","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0425361,0.000102957776,0.91110617,0.00010855495,0.00003541804,0.00029163147,0.0012208805,0.040241215,0.0043570045],"genre_scores_gemma":[0.15548457,0.00009438752,0.8371289,0.00005216781,0.000015372467,0.00023030471,0.0012388312,0.0018598399,0.0038956844],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996482,0.00002791913,0.000022038887,0.00008525689,0.00018042068,0.00003615558],"domain_scores_gemma":[0.99914324,0.00019447408,0.00005634417,0.000057641188,0.0005061578,0.000042053118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004798229,0.0011270081,0.0004832669,0.0017618672,0.0012031479,0.0011322082,0.001496327,0.00046777798,0.00946493],"category_scores_gemma":[0.0017717353,0.0005750336,0.00057659444,0.00095008704,0.00045183834,0.00044248434,0.00067474204,0.0005303783,0.0017793763],"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":[0.00023299163,0.0001466057,0.012880693,0.00026907196,0.00015963284,0.00037370625,0.00053229724,0.07750107,0.06414736,0.0031994723,0.011681529,0.8288756],"study_design_scores_gemma":[0.00008560688,0.0000420062,0.010124957,0.000026444412,0.00003101753,0.00016057445,0.00015205116,0.9472169,0.026644807,0.0014511135,0.013988914,0.00007567781],"about_ca_topic_score_codex":0.32440987,"about_ca_topic_score_gemma":0.35297257,"teacher_disagreement_score":0.67559016,"about_ca_system_score_codex":0.0024457416,"about_ca_system_score_gemma":0.004781701,"threshold_uncertainty_score":0.6450432},"labels":[],"label_agreement":null},{"id":"W2114293825","doi":"10.1111/jmg.12050","title":"Quantifying Barrovian metamorphism in the Danba Structural Culmination of eastern Tibet","year":2013,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Geological Survey of Canada","funders":"Natural Environment Research Council; Natural Resources Canada","keywords":"Geology; Metamorphism; Staurolite; Monazite; Metamorphic rock; Geochronology; Sillimanite; Geochemistry; Kyanite; Andalusite; Paleontology; Zircon; Biotite","score_opus":0.030929876544289196,"score_gpt":0.2333073743112384,"score_spread":0.20237749776694922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114293825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988348,0.00008838658,0.00013879352,0.0000038080866,0.0000011203723,0.0000067221313,0.00013316277,0.0000060465063,0.00078722753],"genre_scores_gemma":[0.99920005,0.000035693203,0.00020216717,0.0000037198738,0.0000012588966,0.000004898517,0.00022845097,0.0000028935149,0.00032092712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999087,0.000010842777,0.000007923233,0.00003148582,0.000023762323,0.000017360895],"domain_scores_gemma":[0.99989367,0.000010880069,0.00003083261,0.000006487109,0.0000377702,0.000020246798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023461405,0.00027988976,0.0001480169,0.0025886637,0.00051004783,0.0007926887,0.00025030796,0.0003155166,0.0011857824],"category_scores_gemma":[0.00031166084,0.00013575696,0.0001436389,0.0014916344,0.0003558409,0.0002482592,0.00042460643,0.00014110048,0.00019593103],"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":[0.00021079888,0.0000367008,0.93896645,0.000050089948,0.00006959954,0.00040692615,0.0008525371,0.0016641719,0.042244047,0.00021399355,0.00006825564,0.015216499],"study_design_scores_gemma":[0.000003027794,0.00002194982,0.99843127,0.0000062529543,0.000006389626,0.00004512228,0.0001967814,0.00057002774,0.00042708372,0.000017657136,0.0002726082,0.0000019820773],"about_ca_topic_score_codex":0.04225915,"about_ca_topic_score_gemma":0.11940329,"teacher_disagreement_score":0.04225915,"about_ca_system_score_codex":0.0007764702,"about_ca_system_score_gemma":0.00025080293,"threshold_uncertainty_score":0.08402634},"labels":[],"label_agreement":null},{"id":"W2116832790","doi":"10.1111/j.1525-1314.2005.00608.x","title":"A structural metamorphic study of the Broken Hill Block, NSW, Australia","year":2005,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Discovery Centre","funders":"University of Melbourne","keywords":"Geology; Metamorphism; Granulite; Terrane; Rift; Geochemistry; Facies; Clockwise; Metamorphic rock; Shear zone; Petrology; Proterozoic; Tectonics; Geomorphology; Paleontology; Geometry; Structural basin; Rotation (mathematics)","score_opus":0.03171981266610363,"score_gpt":0.23352704853810366,"score_spread":0.20180723587200003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116832790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997175,0.0000900023,0.0001201928,0.000016800706,0.0000013730545,0.000022009954,0.00021734691,0.0000037709751,0.002353457],"genre_scores_gemma":[0.99638486,0.0000910053,0.00040132538,0.000013359057,0.000001339983,0.000010199426,0.00021586164,0.0000045179295,0.0028775805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987555,0.000007319218,0.000006000608,0.000036309222,0.000051476778,0.000023322244],"domain_scores_gemma":[0.9998191,0.0000066034127,0.00004729404,0.000010945976,0.00008146039,0.000034651286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009686873,0.00019422242,0.0001501502,0.0010162068,0.0010369082,0.00042125853,0.00042816435,0.00021655747,0.0019310116],"category_scores_gemma":[0.00028767818,0.0003747465,0.00015651005,0.0009184732,0.00053850404,0.0001851177,0.00053233176,0.00020639315,0.00041506166],"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":[0.00024657435,0.000111891444,0.82604843,0.00033006843,0.00013720528,0.0039024986,0.013399715,0.0009904514,0.10999306,0.0007273736,0.00062685733,0.043485787],"study_design_scores_gemma":[0.0000017386021,0.00003350449,0.99757415,0.0000092362225,0.0000063361867,0.00025869792,0.0006413707,0.00020696389,0.0003840364,0.000014546535,0.00086792686,0.000001661348],"about_ca_topic_score_codex":0.43625265,"about_ca_topic_score_gemma":0.71505356,"teacher_disagreement_score":0.43625265,"about_ca_system_score_codex":0.001795527,"about_ca_system_score_gemma":0.0011312977,"threshold_uncertainty_score":0.86742675},"labels":[],"label_agreement":null},{"id":"W2117079504","doi":"10.1111/j.1525-1314.2009.00816.x","title":"Interplay between equilibrium and kinetics in prograde metamorphism of pelites: an example from the Nelson aureole, British Columbia","year":2009,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Laurentian University; University of Calgary","funders":"","keywords":"Staurolite; Metamorphism; Pelite; Chlorite; Mineral; Geology; Muscovite; Thermodynamics; Geochemistry; Gibbs free energy; Mineralogy; Chemistry; Kyanite; Quartz; Paleontology","score_opus":0.025088837668624596,"score_gpt":0.23045257544929432,"score_spread":0.20536373778066971,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117079504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98941284,0.00028014503,0.00028978934,0.00009361123,0.0000021866852,0.000017807772,0.00026185554,0.000029075338,0.009612749],"genre_scores_gemma":[0.99743736,0.00013072895,0.00024261093,0.000011036826,6.434425e-7,0.0000033587598,0.00009080729,0.0000086316995,0.002074883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982125,0.000011910861,0.000009697823,0.00004410868,0.00006920896,0.00004385036],"domain_scores_gemma":[0.99965715,0.000047561585,0.000029997202,0.000013669104,0.00020464812,0.000046995192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001836362,0.0002722862,0.0003346242,0.0014342217,0.0020171595,0.0015169336,0.0005042641,0.0003916443,0.002585284],"category_scores_gemma":[0.0005905846,0.0002942746,0.0001475917,0.0013411243,0.00086546957,0.0003132961,0.00047717037,0.0003394537,0.00028275483],"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":[0.0010070589,0.00014467612,0.65119416,0.00043631523,0.00019966616,0.006593026,0.00455522,0.022409681,0.25532478,0.0073891855,0.0012690676,0.049477212],"study_design_scores_gemma":[0.000029209365,0.00006204824,0.95841086,0.00002779678,0.000060532504,0.0005616317,0.0028233172,0.013801306,0.011723566,0.0010334116,0.011400691,0.000065689994],"about_ca_topic_score_codex":0.89017767,"about_ca_topic_score_gemma":0.93561053,"teacher_disagreement_score":0.10982233,"about_ca_system_score_codex":0.011740766,"about_ca_system_score_gemma":0.0036760787,"threshold_uncertainty_score":0.22093815},"labels":[],"label_agreement":null},{"id":"W2117846431","doi":"10.1046/j.0263-4929.2001.356.356.x","title":"Thermodynamic modelling of the reaction muscovite+cordierite→Al<sub>2</sub>SiO<sub>5</sub>+biotite+quartz+ H<sub>2</sub>O: constraints from natural assemblages and implications for the metapelitic petrogenetic grid","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":86,"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; National Science Foundation","keywords":"Geology; Andalusite; Muscovite; Cordierite; Biotite; Metamorphism; Metamorphic rock; Sillimanite; Geochemistry; Staurolite; Quartz; Mineralogy; Schist; Materials science","score_opus":0.021976098565919366,"score_gpt":0.20212947886362612,"score_spread":0.18015338029770675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117846431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879028,0.00008242515,0.006193461,0.0000880694,0.000008088854,0.00003091108,0.00062144676,0.00010984209,0.0049627987],"genre_scores_gemma":[0.99823713,0.000028791696,0.001056391,0.000007777173,0.000002112127,0.000016097289,0.00016313503,0.000025398891,0.00046316796],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991083,0.000023881692,0.0000064200244,0.000020924155,0.000018659432,0.000019236017],"domain_scores_gemma":[0.9996388,0.00022585865,0.00003335093,0.000024378058,0.00004359516,0.000033941455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004016227,0.00039242092,0.00046819908,0.00045605653,0.0004903626,0.0009918781,0.00071263814,0.0007754756,0.0033496036],"category_scores_gemma":[0.0011139435,0.0003648338,0.00064512395,0.00040608927,0.0005728981,0.00053394673,0.0003189523,0.00032141418,0.00036247066],"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":[0.000067977,0.000031478306,0.006102857,0.00003982617,0.000018540115,0.00007654895,0.00004038939,0.98613805,0.005022602,0.0012755361,0.00008549325,0.0011006767],"study_design_scores_gemma":[0.00000872008,0.00001227309,0.0011272016,0.0000015290481,0.000003285942,0.0000068159384,0.0000105175,0.99746954,0.0010031426,0.00025828087,0.000093946146,0.000004738557],"about_ca_topic_score_codex":0.024677366,"about_ca_topic_score_gemma":0.01704157,"teacher_disagreement_score":0.024677366,"about_ca_system_score_codex":0.0012151407,"about_ca_system_score_gemma":0.00086939096,"threshold_uncertainty_score":0.049067438},"labels":[],"label_agreement":null},{"id":"W2119192153","doi":"10.1111/j.1525-1314.2012.01005.x","title":"Multiple partial melting events in the Sulu UHP terrane: zircon U–Pb dating of granitic leucosomes within amphibolite and gneiss","year":2012,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":101,"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":"Zircon; Geology; Geochemistry; Partial melting; Anatexis; Felsic; Metamorphic rock; Gneiss; Terrane; Igneous rock; Protolith; Monazite; Metamorphism; Metamorphic facies; Petrology; Mafic; Mantle (geology); Geomorphology","score_opus":0.02770469346091623,"score_gpt":0.22410836120877264,"score_spread":0.19640366774785642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119192153","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993625,0.000025107138,0.00008176651,0.0000057174216,6.231999e-7,0.0000025888626,0.000062212275,0.0000067949245,0.00045256445],"genre_scores_gemma":[0.9996295,0.000015859494,0.00010562691,0.0000022217732,8.193512e-7,0.0000019246484,0.000100326804,0.00000257713,0.00014105975],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999585,0.0000035156563,0.0000034854738,0.000013494352,0.000011557422,0.000009506222],"domain_scores_gemma":[0.99995947,0.0000032195853,0.00000840635,0.000005017929,0.00001532642,0.000008431738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011205381,0.00019265045,0.00015974932,0.0006986464,0.0005229932,0.0003433887,0.00020619766,0.00020808299,0.0003860185],"category_scores_gemma":[0.00011112509,0.00018984028,0.00017075242,0.00037231226,0.00027070698,0.00015722713,0.00031169385,0.00011189248,0.000103223916],"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":[0.00034758766,0.000033863278,0.7835973,0.000072694056,0.000112017966,0.0017303844,0.0014606513,0.00090179016,0.1930212,0.00022071504,0.00019493271,0.018306848],"study_design_scores_gemma":[0.000005882442,0.00005220143,0.9887518,0.0000046872715,0.000017570355,0.00031858665,0.00035546767,0.0009915003,0.008732359,0.000024279208,0.0007417873,0.0000038448934],"about_ca_topic_score_codex":0.018204222,"about_ca_topic_score_gemma":0.033814665,"teacher_disagreement_score":0.018204222,"about_ca_system_score_codex":0.00034482163,"about_ca_system_score_gemma":0.00019472158,"threshold_uncertainty_score":0.03619653},"labels":[],"label_agreement":null},{"id":"W2120865672","doi":"10.1111/j.1525-1314.2011.00950.x","title":"Petrological consequences of variations in metamorphic reaction affinity","year":2011,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":139,"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; University of Calgary","funders":"","keywords":"Metastability; Thermodynamics; Reaction rate; Gibbs free energy; Chemistry; Metamorphic rock; Context (archaeology); Geology; Physics; Catalysis","score_opus":0.05272874414586014,"score_gpt":0.2170061587248637,"score_spread":0.16427741457900358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120865672","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883189,0.00013019457,0.004549745,0.00006786296,0.0000069670295,0.000011680292,0.00029189876,0.0002706745,0.0063519157],"genre_scores_gemma":[0.99926263,0.000023345454,0.00038148338,0.0000043681216,9.969655e-7,0.000001962446,0.000055111614,0.000030249346,0.0002398995],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99959964,0.00003652652,0.00003187735,0.00012666102,0.00012925491,0.00007596186],"domain_scores_gemma":[0.99884254,0.00039953657,0.00025438945,0.00017091315,0.00023721588,0.0000955173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039803452,0.00028226594,0.00024862093,0.0016687782,0.00042491438,0.0012063064,0.0004611555,0.0005294931,0.002778682],"category_scores_gemma":[0.0028401266,0.00047983666,0.00022504611,0.0012377889,0.00094117376,0.0008387758,0.0008666141,0.00056650385,0.00031230185],"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":[0.001982941,0.00009085299,0.2152454,0.00026304205,0.00016914528,0.00296331,0.0012209777,0.2032287,0.5240882,0.015291959,0.0006420708,0.034813482],"study_design_scores_gemma":[0.0000795668,0.0002053383,0.61356896,0.000022879645,0.00010746637,0.0021932423,0.0009271326,0.15136018,0.21485297,0.010759815,0.005804695,0.00011764965],"about_ca_topic_score_codex":0.004048166,"about_ca_topic_score_gemma":0.0024628816,"teacher_disagreement_score":0.004048166,"about_ca_system_score_codex":0.00086695934,"about_ca_system_score_gemma":0.00023913536,"threshold_uncertainty_score":0.009295583},"labels":[],"label_agreement":null},{"id":"W2147609241","doi":"10.1111/j.1525-1314.2007.00737.x","title":"Formation of eclogite, and reaction during exhumation to mid‐crustal levels, Snowbird tectonic zone, western Canadian Shield","year":2007,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"National Science Foundation","keywords":"Kyanite; Eclogite; Geology; Geochemistry; Plagioclase; Granulite; Metamorphism; Metamorphic rock; Metamorphic facies; Petrology; Sillimanite; Quartz; Tectonics; Seismology; Facies; Geomorphology; Paleontology","score_opus":0.02007841239475969,"score_gpt":0.21236508805897458,"score_spread":0.1922866756642149,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147609241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971199,0.00019806014,0.000047801965,0.000022674933,0.0000014083905,0.00000792632,0.0008932367,0.000006947471,0.0017020414],"genre_scores_gemma":[0.9975297,0.00013128895,0.00009684167,0.000013944648,7.898358e-7,0.0000036494548,0.0008011305,0.000003364688,0.0014193851],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998574,0.000005214627,0.000005347781,0.000035739922,0.000041019543,0.000055182194],"domain_scores_gemma":[0.9997025,0.0000086110185,0.00003664235,0.0000064060405,0.00017328943,0.000072555034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013123499,0.00024355888,0.00012051673,0.0014990004,0.0015256897,0.0007227871,0.00043355688,0.00016327108,0.001477252],"category_scores_gemma":[0.00026542964,0.00018110803,0.00012661611,0.0011775817,0.00059775,0.0002088608,0.00046837315,0.00018588905,0.0001788536],"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":[0.00012243228,0.000013564425,0.9778121,0.00003638506,0.00003552241,0.00026015792,0.0017326421,0.00025667765,0.010609863,0.00012048817,0.00036515485,0.008634918],"study_design_scores_gemma":[7.381383e-7,0.0000036024885,0.99892324,0.0000032807568,0.0000023114178,0.000017866694,0.00035491394,0.000047502876,0.00017298716,0.0000037805926,0.00046853643,0.0000013049937],"about_ca_topic_score_codex":0.9750049,"about_ca_topic_score_gemma":0.99338055,"teacher_disagreement_score":0.024995089,"about_ca_system_score_codex":0.011111299,"about_ca_system_score_gemma":0.0056816973,"threshold_uncertainty_score":0.08061856},"labels":[],"label_agreement":null},{"id":"W2149647785","doi":"10.1111/j.1525-1314.2006.00686.x","title":"Ultrahigh‐pressure metamorphism and exhumation of garnet‐bearing ultramafic rocks from the Lanterman Range (northern Victoria Land, Antarctica)","year":2007,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Carleton University","funders":"","keywords":"Geology; Ultramafic rock; Amphibole; Geochemistry; Metamorphism; Gondwana; Metamorphic rock; Gneiss; Eclogite; Mafic; Petrology; Paleontology; Tectonics; Subduction; Quartz","score_opus":0.010882522771988229,"score_gpt":0.19829037377256534,"score_spread":0.1874078510005771,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149647785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998672,0.00013651019,0.00001489704,0.000008963958,8.60867e-7,0.000005185537,0.00034508517,0.0000031913485,0.00081338384],"genre_scores_gemma":[0.998348,0.00012163461,0.00006642101,0.0000106617035,0.0000017328567,0.000005469584,0.00058615534,0.000003222045,0.0008566818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998946,0.0000074307154,0.000008378331,0.00002201073,0.000026903683,0.000040672232],"domain_scores_gemma":[0.9998165,0.0000102279,0.00005629016,0.000012921857,0.000056357836,0.00004773076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013020031,0.00028961583,0.00014422108,0.0018845863,0.00084126,0.0005023683,0.0003479198,0.00021617128,0.0016916799],"category_scores_gemma":[0.00020000356,0.00016242651,0.0002380689,0.0014023848,0.00032262315,0.00022105695,0.00049824157,0.00014590556,0.00046577462],"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":[0.00021765953,0.000026866792,0.95155734,0.00009241614,0.00007378112,0.000852165,0.0025761146,0.00022067301,0.03037744,0.000056235916,0.0001994033,0.013749961],"study_design_scores_gemma":[9.4463314e-7,0.000010527502,0.99902475,0.0000041410585,0.0000038251296,0.00007954723,0.00029570606,0.000029455221,0.00018722513,0.0000022461145,0.00036055065,0.0000011959072],"about_ca_topic_score_codex":0.15355104,"about_ca_topic_score_gemma":0.29419705,"teacher_disagreement_score":0.15355104,"about_ca_system_score_codex":0.0012472384,"about_ca_system_score_gemma":0.00048550812,"threshold_uncertainty_score":0.30531454},"labels":[],"label_agreement":null},{"id":"W2153315663","doi":"10.1046/j.0263-4929.2001.00357.x","title":"Interaction of metamorphism, deformation and exhumation in large convergent orogens","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":221,"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; Canadian Institute for Advanced Research","keywords":"Geology; Metamorphism; Crust; Lithosphere; Subduction; Petrology; Continental crust; Metamorphic rock; Geophysics; Tectonics; Geomorphology; Seismology","score_opus":0.0231323833167158,"score_gpt":0.2095803260248471,"score_spread":0.1864479427081313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153315663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979638,0.00002402213,0.0008390423,0.000040845487,0.0000021428687,0.000005285836,0.000054324406,0.00002177782,0.0010488363],"genre_scores_gemma":[0.99956185,0.00002302074,0.00019121147,0.0000050840263,0.0000015676153,0.0000049614546,0.000029617797,0.000009512299,0.00017322788],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998834,0.00003276417,0.000009113226,0.00003496346,0.000014944399,0.000024854526],"domain_scores_gemma":[0.9997558,0.00008452253,0.000057818223,0.00003346546,0.000024089191,0.000044360673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000287441,0.0005418099,0.00048260883,0.0004770485,0.00047348748,0.0011862721,0.0008285148,0.0008401709,0.0015689722],"category_scores_gemma":[0.0011444613,0.00046002318,0.0006805323,0.0003677946,0.0010553704,0.0006050516,0.0010137671,0.00038425304,0.0001242667],"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":[0.00019397044,0.00009319069,0.05942285,0.00004363671,0.00016210176,0.0003948282,0.00015966549,0.92492396,0.010390261,0.0023367465,0.00008501317,0.0017937906],"study_design_scores_gemma":[0.000077525765,0.00009422841,0.03159127,0.000008093816,0.000051352996,0.0000913347,0.00014319159,0.9649307,0.0013572675,0.0013963078,0.00023382127,0.000024848532],"about_ca_topic_score_codex":0.017096307,"about_ca_topic_score_gemma":0.009091285,"teacher_disagreement_score":0.017096307,"about_ca_system_score_codex":0.0014878275,"about_ca_system_score_gemma":0.0005113424,"threshold_uncertainty_score":0.0339936},"labels":[],"label_agreement":null},{"id":"W2154648132","doi":"10.1046/j.1525-1314.2003.00415.x","title":"Petrogenetic significance of orthopyroxene‐free garnet + clinopyroxene + plagioclase ± quartz‐bearing metabasites with respect to the amphibolite and granulite facies","year":2002,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":189,"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":"Granulite; Plagioclase; Geology; Geochemistry; Hornblende; Metamorphic facies; Facies; Petrology; Mineral; Quartz; Geomorphology; Chemistry; Biotite","score_opus":0.020550933474847117,"score_gpt":0.19790651840140303,"score_spread":0.1773555849265559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154648132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99641776,0.00015212112,0.00023573072,0.0000065878176,9.704519e-7,0.000010529552,0.00017518019,0.000016798102,0.0029843817],"genre_scores_gemma":[0.9992816,0.00004889272,0.00011385431,0.0000020094456,9.0574457e-7,0.0000027199444,0.00009667059,0.0000064153846,0.00044694293],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989176,0.000013561815,0.000009720174,0.000047369747,0.000015468164,0.000022031856],"domain_scores_gemma":[0.9998394,0.00003340786,0.000047807665,0.000020107736,0.000028688495,0.000030511059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014279589,0.000174153,0.00010598063,0.0007267195,0.00022141176,0.00043638784,0.00014730726,0.00015547333,0.0022170371],"category_scores_gemma":[0.0002567434,0.00014716251,0.00010507549,0.00031923098,0.0004226483,0.0001496154,0.00032098792,0.00010708702,0.0003402024],"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":[0.0008206134,0.000025412484,0.26593468,0.00015928567,0.00006814249,0.00062353496,0.0006440331,0.0008823027,0.70605665,0.0006767811,0.000053369895,0.024055226],"study_design_scores_gemma":[0.0000071630975,0.00007226522,0.98532975,0.0000049194314,0.000012007423,0.00031025015,0.0001245628,0.00030987937,0.012970826,0.00006200596,0.0007927946,0.0000036757692],"about_ca_topic_score_codex":0.0059286407,"about_ca_topic_score_gemma":0.010211459,"teacher_disagreement_score":0.0059286407,"about_ca_system_score_codex":0.0003400041,"about_ca_system_score_gemma":0.0001705035,"threshold_uncertainty_score":0.011788249},"labels":[],"label_agreement":null},{"id":"W2159680326","doi":"10.1111/jmg.12122","title":"Using calculated chemical potential relationships to account for replacement of kyanite by symplectite in high pressure granulites","year":2014,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Australian Research Council","keywords":"Kyanite; Plagioclase; Granulite; Anorthite; Geology; Geochemistry; Mineral; Mineralogy; Metamorphic rock; Chemistry; Quartz; Geomorphology","score_opus":0.02258801382593533,"score_gpt":0.22711402869850247,"score_spread":0.20452601487256714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159680326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96527106,0.00010753658,0.027499504,0.00005775263,0.000014715401,0.000033482214,0.00046250975,0.00027255827,0.0062808413],"genre_scores_gemma":[0.99609226,0.000028410233,0.0029673863,0.000009215653,0.0000010389226,0.000014541045,0.00017126686,0.000046766814,0.00066908135],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99987805,0.000015619404,0.000010591734,0.000037427395,0.00003918424,0.00001911834],"domain_scores_gemma":[0.9998683,0.000037095564,0.000023335713,0.000018261991,0.000044729917,0.000008248463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013414651,0.00033273813,0.00016956478,0.00046349675,0.00030763424,0.00048129997,0.00089931226,0.0003212509,0.0025858262],"category_scores_gemma":[0.0006667042,0.00022545653,0.00027790986,0.00036141672,0.00022741169,0.000487975,0.00025289078,0.00023040938,0.00031124457],"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":[0.00014018208,0.00010563853,0.079374194,0.0001776433,0.00015547108,0.00049519225,0.00014335923,0.7470691,0.14190663,0.011266719,0.00051193166,0.018653946],"study_design_scores_gemma":[0.00004780294,0.000048786736,0.020969942,0.000007778263,0.000025073941,0.00014610146,0.00006614507,0.9406448,0.03411717,0.0019312144,0.0019735033,0.00002167024],"about_ca_topic_score_codex":0.02094609,"about_ca_topic_score_gemma":0.031759467,"teacher_disagreement_score":0.02094609,"about_ca_system_score_codex":0.0013344969,"about_ca_system_score_gemma":0.0005812525,"threshold_uncertainty_score":0.04164833},"labels":[],"label_agreement":null},{"id":"W2166692781","doi":"10.1111/j.1525-1314.2011.00946.x","title":"Implications of garnet resorption for the Lu-Hf garnet geochronometer: an example from the contact aureole of the Makhavinekh Lake Pluton, Labrador","year":2011,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":96,"is_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; Metamorphism; Geochemistry; Pluton; Granulite; Geochronology; Cordierite; Metamorphic rock; Fluorite; Mineralogy; Isochron dating; Isochron; Geomorphology; Facies; Tectonics; Paleontology; Materials science","score_opus":0.064748546002113,"score_gpt":0.22126573796873103,"score_spread":0.15651719196661804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166692781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99648005,0.00019098567,0.00021926039,0.00020019861,0.000004823399,0.000008957172,0.0001966161,0.000053299736,0.0026458234],"genre_scores_gemma":[0.99876475,0.000076852586,0.00032551782,0.00002125939,0.0000053576305,0.000004206131,0.000101247075,0.00002020027,0.0006806538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997764,0.000027343518,0.000012990257,0.00005143708,0.000068706795,0.00006320073],"domain_scores_gemma":[0.9998534,0.000022855837,0.000040070157,0.000013838859,0.000050392424,0.000019445506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033596245,0.0004977507,0.00046110497,0.0010097716,0.0015178632,0.0009406225,0.000820154,0.0006554058,0.0015739617],"category_scores_gemma":[0.0004760555,0.00025360862,0.00025421917,0.0014240525,0.0010322965,0.0004491945,0.00075221295,0.0004120645,0.00026543066],"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":[0.00092984294,0.000057997746,0.8728859,0.00019697759,0.0000887338,0.0074116327,0.011647659,0.002347818,0.060672015,0.00082479976,0.00094489846,0.041991692],"study_design_scores_gemma":[0.000026320988,0.00010934798,0.9840771,0.000029406145,0.00004895808,0.0006060135,0.003590994,0.0020344988,0.004141027,0.00013021418,0.0051874374,0.000018764249],"about_ca_topic_score_codex":0.1769147,"about_ca_topic_score_gemma":0.31387514,"teacher_disagreement_score":0.1769147,"about_ca_system_score_codex":0.0024322753,"about_ca_system_score_gemma":0.0008600591,"threshold_uncertainty_score":0.35176986},"labels":[],"label_agreement":null},{"id":"W2179283172","doi":"10.1111/jmg.12172","title":"A statistical analysis of the distribution of cordierite and biotite in hornfels from the Bugaboo contact aureole: implications for the kinetics of porphyroblast crystallization","year":2015,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Calgary; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Hornfels; Biotite; Cordierite; Geology; Isograd; Nucleation; Crystallization; Mineralogy; Crystal (programming language); Metamorphic rock; Migmatite; Crystallography; Materials science; Geochemistry; Thermodynamics; Chemistry; Quartz; Physics; Composite material; Metamorphic facies; Geomorphology","score_opus":0.025850504045730343,"score_gpt":0.23632617760621283,"score_spread":0.2104756735604825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2179283172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948406,0.000020225732,0.00018863668,0.0000026015607,3.2753704e-7,0.000002218738,0.00011405052,0.000006978889,0.00018084684],"genre_scores_gemma":[0.99946934,0.000010729382,0.00021053008,0.0000014132744,4.79922e-7,0.000002513348,0.00019132985,0.0000047780463,0.0001088439],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998684,0.000008969529,0.000010307965,0.00005408895,0.000035501267,0.000022715305],"domain_scores_gemma":[0.99962246,0.00009484038,0.000107049455,0.000028107394,0.00009579486,0.000051772844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017333758,0.00013963554,0.00019076242,0.0015872795,0.0003807496,0.00061141956,0.000196143,0.00020580304,0.0007025141],"category_scores_gemma":[0.00058548525,0.00013557261,0.00020741227,0.0007142948,0.0005426694,0.0001623223,0.00031107725,0.00011464779,0.00013347295],"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":[0.00021004888,0.000013011278,0.84892285,0.0000358488,0.00005544608,0.00025064556,0.00040668604,0.0007764226,0.14138445,0.000094150346,0.000041135238,0.007809366],"study_design_scores_gemma":[0.0000012149878,0.000014576608,0.99702966,8.4496065e-7,0.000005187813,0.00007308851,0.00012219553,0.00073990267,0.001916018,0.000010682878,0.00008405034,0.0000026294517],"about_ca_topic_score_codex":0.020949366,"about_ca_topic_score_gemma":0.03369766,"teacher_disagreement_score":0.020949366,"about_ca_system_score_codex":0.00049094815,"about_ca_system_score_gemma":0.0002111609,"threshold_uncertainty_score":0.041654825},"labels":[],"label_agreement":null},{"id":"W2223597483","doi":"10.1111/jmg.12180","title":"Crustal reworking in a shear zone: transformation of metagranite to migmatite","year":2016,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Université du Québec à Chicoutimi","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies; Fundação de Amparo à Pesquisa do Estado de São Paulo","keywords":"Migmatite; Geology; Protolith; Residuum; Partial melting; Geochemistry; Plagioclase; Shear zone; Feldspar; Anatexis; Petrology; Crust; Metamorphic rock; Gneiss; Tectonics; Seismology","score_opus":0.01501416236711783,"score_gpt":0.207684369225601,"score_spread":0.19267020685848316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2223597483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951315,0.000039094783,0.00006289444,0.0000037970078,4.6290606e-7,0.000002588801,0.000034826575,0.0000064097276,0.0003368049],"genre_scores_gemma":[0.9996722,0.00001855029,0.0001345316,0.0000021656308,4.3489226e-7,7.3865505e-7,0.000045221255,0.0000020239563,0.00012416535],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999915,0.000004110087,0.0000056007575,0.00003732452,0.000022401899,0.000015596313],"domain_scores_gemma":[0.99994016,0.0000046630107,0.000027246886,0.000008170932,0.0000105132885,0.000009213219],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001361334,0.00019341407,0.00016257899,0.0006826626,0.00027931077,0.00045248703,0.00020371852,0.00021892252,0.00054937345],"category_scores_gemma":[0.00016283388,0.00016437218,0.00017691999,0.00032325462,0.0002700504,0.00017160345,0.00023077258,0.00013415252,0.0001150439],"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":[0.0002667699,0.000032087282,0.37739837,0.000056402976,0.00005978195,0.00058227347,0.0007952658,0.0009015152,0.609671,0.00016817826,0.00004959327,0.010018717],"study_design_scores_gemma":[0.0000056952686,0.00007715798,0.9755592,0.0000050705903,0.00001563725,0.0002923412,0.00030880503,0.0007949139,0.02199888,0.00003958189,0.0008986491,0.000004090007],"about_ca_topic_score_codex":0.0093160095,"about_ca_topic_score_gemma":0.01868474,"teacher_disagreement_score":0.0093160095,"about_ca_system_score_codex":0.0006591584,"about_ca_system_score_gemma":0.00016358259,"threshold_uncertainty_score":0.018523574},"labels":[],"label_agreement":null},{"id":"W2237942576","doi":"10.1111/jmg.12182","title":"Coupled garnet Lu–Hf and monazite U–Pb geochronology constrain early convergent margin dynamics in the Ross orogen, Antarctica","year":2016,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"University of British Columbia","funders":"Pomona College; Deutsche Forschungsgemeinschaft; Antarctica New Zealand; University of Otago; National Science Foundation","keywords":"Monazite; Geology; Geochronology; Geochemistry; Metamorphic rock; Gondwana; Metamorphism; Batholith; Zircon; Paleontology; Tectonics","score_opus":0.01129118699457009,"score_gpt":0.19689623332655606,"score_spread":0.18560504633198596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2237942576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969928,0.00030173972,0.00026914026,0.000021545198,0.0000038835374,0.0000045502634,0.00063557643,0.00003541652,0.0017353907],"genre_scores_gemma":[0.99844825,0.00014691541,0.00036566844,0.000014309304,0.0000035134744,0.000003828804,0.0005249005,0.000022820366,0.0004698082],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994683,0.000007987257,0.0000031319441,0.000014959635,0.000011916946,0.000015207276],"domain_scores_gemma":[0.9999151,0.0000095605965,0.000022980394,0.000012201791,0.000026251266,0.000013864707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020613217,0.00044890319,0.00020040863,0.0013249682,0.00037153417,0.00071280194,0.0002231413,0.0003112588,0.0018906342],"category_scores_gemma":[0.00022627121,0.00016636017,0.00023954886,0.0011605263,0.0002677022,0.00025837962,0.00053226505,0.00011880157,0.0007058615],"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":[0.00048093763,0.000022653918,0.9043354,0.00008676279,0.00024716934,0.00028977386,0.00074547133,0.0040990957,0.058774877,0.0002890626,0.0007628655,0.029865982],"study_design_scores_gemma":[0.0000074272266,0.000025002597,0.99351716,0.0000124915805,0.000053976204,0.00008095442,0.0003229431,0.0022877906,0.0017644113,0.00005634422,0.001864492,0.0000069785515],"about_ca_topic_score_codex":0.04313826,"about_ca_topic_score_gemma":0.0853315,"teacher_disagreement_score":0.04313826,"about_ca_system_score_codex":0.00050357624,"about_ca_system_score_gemma":0.00037997926,"threshold_uncertainty_score":0.08577436},"labels":[],"label_agreement":null},{"id":"W2337355374","doi":"10.1111/jmg.12196","title":"Using monazite and zircon petrochronology to constrain the <i>P</i>–<i>T</i>–<i>t</i> evolution of the middle crust in the Bhutan Himalaya","year":2016,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Dalhousie University","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Natural Environment Research Council; Sight Research UK","keywords":"Monazite; Zircon; Geology; Metamorphic rock; Geochemistry; Partial melting; Allanite; Granulite; Plagioclase; Felsic; Metamorphic facies; Metamorphism; Anatexis; Trace element; Mineralogy; Facies; Mafic; Crust; Quartz; Geomorphology; Paleontology","score_opus":0.03183935438443912,"score_gpt":0.20821640511829206,"score_spread":0.17637705073385296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2337355374","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980641,0.00010152798,0.00092911103,0.0000074824957,0.0000013328049,0.0000070309243,0.00018866049,0.000023389368,0.0006773518],"genre_scores_gemma":[0.99914956,0.00003485198,0.00055765576,0.0000027308959,0.0000010987969,0.0000022979216,0.000120755,0.0000033232761,0.00012765781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998913,0.000012221882,0.000007700822,0.0000446578,0.000022772352,0.000021278964],"domain_scores_gemma":[0.9999056,0.000013388349,0.00002898231,0.000013680511,0.000025302697,0.000013044129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002265862,0.00029877372,0.00016272042,0.0012888935,0.0003501277,0.00064337614,0.0003410329,0.0002517423,0.0006023972],"category_scores_gemma":[0.0002250401,0.00021113393,0.00022431326,0.000996404,0.00023091938,0.00020384093,0.00034355637,0.0001283809,0.00020880345],"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":[0.00036039864,0.00004880485,0.7016595,0.0001121381,0.00018821482,0.00058190664,0.000616182,0.0075687454,0.2544038,0.00029649655,0.0000865725,0.034077223],"study_design_scores_gemma":[0.000011131106,0.000065825734,0.9723741,0.0000072586517,0.000048234106,0.00019638821,0.00020304276,0.012967119,0.01355471,0.00006893428,0.00049166236,0.00001152337],"about_ca_topic_score_codex":0.03159554,"about_ca_topic_score_gemma":0.06813375,"teacher_disagreement_score":0.03159554,"about_ca_system_score_codex":0.0005155786,"about_ca_system_score_gemma":0.00025117194,"threshold_uncertainty_score":0.062823236},"labels":[],"label_agreement":null},{"id":"W2404321806","doi":"10.1111/jmg.12200","title":"A review of thermal history and timescales of tectonometamorphic processes in Sikkim Himalaya (<scp>NE</scp>India) and implications for rates of metamorphic processes","year":2016,"lang":"en","type":"review","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Carleton University","funders":"","keywords":"Metamorphic rock; Sillimanite; Metamorphism; Geology; Gneiss; Muscovite; Geochemistry; Main Central Thrust; Pelite; Zircon; Kyanite; Recrystallization (geology); Shear zone; Petrology; Biotite; Paleontology; Quartz; Tectonics","score_opus":0.048838183620182274,"score_gpt":0.2749192636127076,"score_spread":0.2260810799925253,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2404321806","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004466993,0.9941199,0.0001737682,0.00021348085,0.00013936221,0.000004492167,0.00013973578,0.000014179308,0.0007281172],"genre_scores_gemma":[0.009233104,0.98949033,0.0002968421,0.00011146344,0.00023772426,0.000006001231,0.00012793895,0.000003930194,0.00049264025],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99988174,0.000012084136,0.000029627672,0.00004421066,0.000019900603,0.000012375813],"domain_scores_gemma":[0.9996362,0.00012738949,0.000110048815,0.000012223552,0.000088195775,0.000026021215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003889526,0.0007277088,0.00076599815,0.0048008296,0.00028373237,0.0010595567,0.0007357513,0.0003544399,0.00203577],"category_scores_gemma":[0.0005844199,0.00036797524,0.00037688427,0.006235994,0.00041986362,0.0011978232,0.00036566862,0.00040730956,0.00043640658],"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":[0.00019082439,0.00007511416,0.014758774,0.04657475,0.00053840026,0.0008981012,0.001145049,0.0015217048,0.007404049,0.002446163,0.014182618,0.9102644],"study_design_scores_gemma":[0.000014085641,0.00035190373,0.17591274,0.013072091,0.0009075236,0.0042539276,0.0012250248,0.00049542583,0.0023711575,0.0018029518,0.7994915,0.0001016845],"about_ca_topic_score_codex":0.004721783,"about_ca_topic_score_gemma":0.0077245072,"teacher_disagreement_score":0.0048008296,"about_ca_system_score_codex":0.0009120913,"about_ca_system_score_gemma":0.0009434044,"threshold_uncertainty_score":0.009388626},"labels":[],"label_agreement":null},{"id":"W2598525654","doi":"10.1111/jmg.12250","title":"The <i>P–T–t</i> evolution of the exhumed Himalayan metamorphic core in the Likhu Khola region, East Central Nepal","year":2017,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Université Laval; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Geology; Metamorphic core complex; Metamorphic rock; Classification of discontinuities; Monazite; Main Central Thrust; Crust; Geochemistry; Discontinuity (linguistics); Metamorphism; Paleontology; Zircon; Tectonics; Extensional definition","score_opus":0.028178726340274927,"score_gpt":0.21166266525900646,"score_spread":0.18348393891873152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2598525654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99807906,0.00007742373,0.00010003182,0.000022682527,0.0000013154214,0.000005028225,0.00016930423,0.000010407373,0.0015347115],"genre_scores_gemma":[0.9995584,0.000031191717,0.00007990336,0.0000074097497,0.0000013201405,0.0000034790821,0.00009487121,0.000002760379,0.0002207299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993455,0.000007426428,0.000005254277,0.000019409548,0.000014570028,0.000018865523],"domain_scores_gemma":[0.99987626,0.000022553268,0.000030435285,0.000010790394,0.000042304968,0.000017712277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010752813,0.00011038738,0.00013809268,0.0011225353,0.0005304443,0.0006909921,0.0003291279,0.00028053523,0.0012917466],"category_scores_gemma":[0.00031192126,0.00015602504,0.000119810655,0.0010246075,0.0004334668,0.00023841416,0.00043108134,0.00016378923,0.00024747438],"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":[0.00032730305,0.00006922594,0.86914474,0.00023495835,0.00021610993,0.0044201924,0.005506971,0.003439857,0.08118864,0.0007148045,0.000556865,0.034180332],"study_design_scores_gemma":[0.0000038939033,0.000023023083,0.9961243,0.000010933018,0.000012630669,0.00030531033,0.0008280801,0.0006949483,0.0012207421,0.00003737026,0.0007338028,0.000004970499],"about_ca_topic_score_codex":0.03856049,"about_ca_topic_score_gemma":0.047084842,"teacher_disagreement_score":0.03856049,"about_ca_system_score_codex":0.0005574665,"about_ca_system_score_gemma":0.0003439434,"threshold_uncertainty_score":0.07667208},"labels":[],"label_agreement":null},{"id":"W2606282616","doi":"10.1111/jmg.12252","title":"Petrogenetic relations among titanium‐rich minerals in an anatectic high‐<i>P</i> mafic granulite","year":2017,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"City University of New York","keywords":"Titanite; Geology; Ilmenite; Geochemistry; Granulite; Mafic; Plagioclase; Hornblende; Rutile; Augite; Mineralogy; Quartz; Metamorphic rock; Biotite; Facies; Geomorphology","score_opus":0.017096060147478217,"score_gpt":0.2232599741216862,"score_spread":0.20616391397420797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2606282616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983809,0.000041839285,0.00013958591,0.000007781765,3.960025e-7,0.000004988624,0.00006449228,0.000013555651,0.0013463977],"genre_scores_gemma":[0.9993242,0.00001701866,0.00017651814,0.0000042260376,4.2797964e-7,0.0000016000661,0.000079658996,0.0000049591304,0.00039149506],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999213,0.000003322407,0.000003882613,0.00002626197,0.000024440593,0.000020754513],"domain_scores_gemma":[0.99993837,0.000007222282,0.000018964229,0.000005838985,0.000017665836,0.000012020853],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000054462667,0.00011455261,0.000087342356,0.0005849983,0.00037228793,0.0005019148,0.00022683023,0.00017407995,0.00056644605],"category_scores_gemma":[0.0001302059,0.00013628861,0.00008790376,0.00030792766,0.00047197248,0.00009799834,0.00021620076,0.000104546176,0.00012576251],"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":[0.00024973447,0.000020992551,0.22687434,0.00004842261,0.000027847183,0.001634303,0.00065481535,0.0007208418,0.7625936,0.00041440479,0.00010284841,0.0066578784],"study_design_scores_gemma":[0.000007897609,0.00006537818,0.96352905,0.0000051719453,0.000012392827,0.0007251644,0.00039914544,0.00083511655,0.032214593,0.000076762895,0.0021248246,0.0000045406514],"about_ca_topic_score_codex":0.05302209,"about_ca_topic_score_gemma":0.08584934,"teacher_disagreement_score":0.05302209,"about_ca_system_score_codex":0.0010864462,"about_ca_system_score_gemma":0.00033750723,"threshold_uncertainty_score":0.10542691},"labels":[],"label_agreement":null},{"id":"W2761822877","doi":"10.1111/jmg.12286","title":"The reaction history of kyanite in high‐<i>P</i> aluminous granulites","year":2017,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Kyanite; Geology; Staurolite; Metamorphic rock; Geochemistry; Granulite; Pseudomorph; Sillimanite; Mineralogy; Biotite; Facies; Paleontology; Quartz","score_opus":0.018191894028876276,"score_gpt":0.19713166576270777,"score_spread":0.1789397717338315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2761822877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993043,0.000031714917,0.000096737065,0.000004418308,4.4969497e-7,0.0000028866364,0.000038724338,0.000008624267,0.00051207026],"genre_scores_gemma":[0.9996357,0.000012758462,0.00009042295,0.0000030046904,4.5239787e-7,0.0000020456157,0.000058142527,0.000004963109,0.00019250387],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998473,0.000014533273,0.00001061904,0.00005551004,0.00003578653,0.000036276284],"domain_scores_gemma":[0.9998647,0.000023035404,0.000042817148,0.000011630437,0.000031323725,0.000026477908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012302179,0.000144476,0.00014550403,0.00051224715,0.00025716674,0.000708151,0.00027733415,0.00031004837,0.00072298246],"category_scores_gemma":[0.0002488711,0.00019380488,0.00010651812,0.00019996581,0.00050219597,0.00019043892,0.0002372683,0.00017804961,0.00017263887],"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":[0.00021450104,0.000014377268,0.04632582,0.000026200745,0.000014758271,0.0003404399,0.00024421304,0.0003364586,0.9504722,0.00010099993,0.000020857724,0.0018892211],"study_design_scores_gemma":[0.00001985415,0.0002777797,0.76500976,0.000006894449,0.0000245665,0.0011343672,0.00044501372,0.0022508376,0.22890688,0.000103655046,0.0018043158,0.000016027065],"about_ca_topic_score_codex":0.004705797,"about_ca_topic_score_gemma":0.0048126956,"teacher_disagreement_score":0.004705797,"about_ca_system_score_codex":0.00040311113,"about_ca_system_score_gemma":0.0001583453,"threshold_uncertainty_score":0.009356797},"labels":[],"label_agreement":null},{"id":"W2775993433","doi":"10.1111/jmg.12302","title":"Kinetic control of staurolite–Al<sub>2</sub>SiO<sub>5</sub> mineral assemblages: Implications for Barrovian and Buchan metamorphism","year":2017,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Andalusite; Staurolite; Kyanite; Sillimanite; Geology; Mineral; Geochemistry; Metamorphic rock; Paleontology; Chemistry; Quartz; Biotite","score_opus":0.01829521399636164,"score_gpt":0.22953278137542618,"score_spread":0.21123756737906454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2775993433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99136364,0.00037740025,0.0017433112,0.000102989194,0.000007672262,0.000016302156,0.00013679574,0.00005928368,0.006192628],"genre_scores_gemma":[0.998485,0.00007965703,0.00028942004,0.000009760318,0.0000012510446,0.0000056583553,0.00005186141,0.000010975663,0.0010663478],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99988663,0.000012596662,0.000010230686,0.000033668006,0.000036362017,0.000020485808],"domain_scores_gemma":[0.99986005,0.00003067803,0.00003479616,0.000016871702,0.000028980932,0.00002856051],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023652066,0.000178053,0.00016310396,0.0004556639,0.0003227899,0.001054918,0.00042300677,0.00019807274,0.0025469458],"category_scores_gemma":[0.00043205987,0.00023611735,0.00013223034,0.00021534615,0.0005823883,0.00067574554,0.00045378334,0.00024821778,0.00037285962],"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":[0.0005254553,0.00004181649,0.021827111,0.00010458704,0.00002610306,0.00015021903,0.00016280902,0.0023917267,0.95946664,0.0075795557,0.00014750852,0.0075765755],"study_design_scores_gemma":[0.00010956331,0.00028004227,0.23173884,0.00003039847,0.000033013694,0.0005823802,0.0008938316,0.051633056,0.6972005,0.0076430286,0.009799417,0.00005600634],"about_ca_topic_score_codex":0.004791266,"about_ca_topic_score_gemma":0.01004468,"teacher_disagreement_score":0.004791266,"about_ca_system_score_codex":0.0009860107,"about_ca_system_score_gemma":0.00032208688,"threshold_uncertainty_score":0.00952673},"labels":[],"label_agreement":null},{"id":"W2790655828","doi":"10.1111/jmg.12307","title":"Th/U ratios in metamorphic zircon","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":431,"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":"Zircon; Monazite; Metamorphic rock; Metamorphism; Geology; Geochemistry; Migmatite; Gneiss","score_opus":0.018390652406120284,"score_gpt":0.21388762246085638,"score_spread":0.1954969700547361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790655828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99512684,0.00010894404,0.0027231064,0.0000134044285,0.0000020155896,0.000009383643,0.0007320581,0.000071862654,0.0012124125],"genre_scores_gemma":[0.9987081,0.00005664261,0.0006146861,0.000003046719,5.21535e-7,0.000005520933,0.0003236968,0.0000108603,0.00027690636],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99984527,0.00001404045,0.000014112256,0.00007049993,0.00003475453,0.000021255066],"domain_scores_gemma":[0.99991024,0.000024452771,0.00002667585,0.000013174698,0.000019982072,0.00000545082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023826894,0.00029764388,0.00030467458,0.0006031067,0.0002141216,0.00077418785,0.00044405033,0.00043879013,0.00076632487],"category_scores_gemma":[0.00050455856,0.00029672642,0.0005003559,0.00038901172,0.00030167436,0.00033048054,0.00030259264,0.00020297398,0.0001776982],"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":[0.00064641004,0.00011008443,0.2014174,0.00027933702,0.00021334909,0.0005449052,0.00029152434,0.49036148,0.28542668,0.004689441,0.00034802614,0.01567138],"study_design_scores_gemma":[0.00007263858,0.00028447385,0.13072212,0.000028589544,0.00010947052,0.00024269127,0.000182252,0.7355605,0.12809162,0.0017919808,0.0028591237,0.00005460999],"about_ca_topic_score_codex":0.019926166,"about_ca_topic_score_gemma":0.007960801,"teacher_disagreement_score":0.019926166,"about_ca_system_score_codex":0.0009863263,"about_ca_system_score_gemma":0.0002783564,"threshold_uncertainty_score":0.03962034},"labels":[],"label_agreement":null},{"id":"W2795197313","doi":"10.1111/jmg.12313","title":"Record of plate boundary metamorphism during Gondwana breakup from Lu–Hf garnet geochronology of the Alpine Schist, New Zealand","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 British Columbia","funders":"University of California, Santa Barbara; Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Gondwana; Geology; Metamorphism; Schist; Geochronology; Diachronous; Geochemistry; Subduction; Paleontology; Metamorphic rock; Rift; Petrology; Tectonics","score_opus":0.010881876094117096,"score_gpt":0.1919879565300747,"score_spread":0.1811060804359576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795197313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986084,0.00006434833,0.00012442064,0.000006705025,9.435976e-7,0.0000042350457,0.00029610365,0.000012362504,0.00088242587],"genre_scores_gemma":[0.99926144,0.000047042402,0.00020011725,0.000002205896,0.0000010862177,0.0000044022036,0.0003075274,0.0000040608793,0.00017207889],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993026,0.000004754308,0.0000066836706,0.00002046239,0.000022642676,0.00001514628],"domain_scores_gemma":[0.99971515,0.000020526233,0.00010519293,0.000025651258,0.000096158146,0.000037272137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002345872,0.0002378801,0.00017505218,0.0016321043,0.00043218856,0.0004909961,0.00019954923,0.00016851595,0.0009426999],"category_scores_gemma":[0.0005004866,0.00017870817,0.00019005255,0.0009228135,0.0004013467,0.00028251903,0.0004727465,0.00015971079,0.00017873528],"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":[0.0001905227,0.000015374731,0.94276214,0.000040456296,0.000051291794,0.00021891354,0.0013695271,0.0005213093,0.042249333,0.000120847704,0.00012752332,0.0123327635],"study_design_scores_gemma":[0.0000017783848,0.000010385834,0.99914527,0.0000028626926,0.0000057850984,0.000026165993,0.00006696553,0.00014306005,0.00032471953,0.000005845303,0.00026582016,0.0000013518599],"about_ca_topic_score_codex":0.123519175,"about_ca_topic_score_gemma":0.2335974,"teacher_disagreement_score":0.123519175,"about_ca_system_score_codex":0.0009985646,"about_ca_system_score_gemma":0.00027925274,"threshold_uncertainty_score":0.24560046},"labels":[],"label_agreement":null},{"id":"W2802441917","doi":"10.1111/jmg.12422","title":"The early exhumation history of the Western Tianshan<scp>UHP</scp>metamorphic belt, China: New constraints from titanite U–Pb geochronology and thermobarometry","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Natural Science Foundation of China","keywords":"Titanite; Zircon; Geology; Geochemistry; Epidote; Geochronology; Metamorphic rock; Eclogite; Allanite; Trace element; Petrography; Phengite; Subduction; Quartz; Paleontology; Tectonics","score_opus":0.014107878512480056,"score_gpt":0.18520472156081,"score_spread":0.17109684304832995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802441917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889684,0.00021587446,0.00013227148,0.000014111002,0.0000011593448,0.0000045140414,0.00010589825,0.0000064932187,0.0006228288],"genre_scores_gemma":[0.9995795,0.00007021806,0.000072299124,0.000005298455,0.0000022414838,0.0000024808837,0.00014626345,0.0000022058914,0.00011948642],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998821,0.000009949199,0.000013903455,0.00003701617,0.000035603432,0.000021314268],"domain_scores_gemma":[0.99977463,0.00002522874,0.000068506146,0.000026778567,0.00007563755,0.000029214652],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003064738,0.00029521427,0.00021999281,0.0015785138,0.00035977023,0.00043197523,0.00026989955,0.00022806569,0.0006804088],"category_scores_gemma":[0.0003046101,0.00018940562,0.00018873536,0.0013966291,0.00044565045,0.00031741557,0.00037785558,0.00013200095,0.00010341386],"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":[0.0001640958,0.000018867931,0.89000916,0.00013875736,0.000111952184,0.00053704594,0.0013246363,0.00066700915,0.08336297,0.00028988245,0.0001354429,0.02324017],"study_design_scores_gemma":[0.0000022303336,0.000013770998,0.99824846,0.0000031962318,0.000010357194,0.00005296658,0.00008479556,0.00035521478,0.0009627009,0.00001439853,0.00024962623,0.0000021469928],"about_ca_topic_score_codex":0.039115258,"about_ca_topic_score_gemma":0.043202776,"teacher_disagreement_score":0.039115258,"about_ca_system_score_codex":0.0005817209,"about_ca_system_score_gemma":0.0004623688,"threshold_uncertainty_score":0.07777512},"labels":[],"label_agreement":null},{"id":"W2804629464","doi":"10.1111/jmg.12425","title":"Two successive phases of ultrahigh temperature metamorphism in Rogaland, S. Norway: Evidence from Y‐in‐monazite thermometry","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"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; Providence Health Care","keywords":"Metamorphism; Monazite; Geology; Geochemistry; Granulite; Metamorphic rock; Charnockite; Gneiss; Partial melting; Anatexis; Petrology; Zircon; Facies; Mantle (geology); Geomorphology","score_opus":0.017048700555015797,"score_gpt":0.24378018778387237,"score_spread":0.22673148722885655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804629464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987224,0.00018362289,0.00011460894,0.000009961885,0.0000038785647,0.000004930653,0.000102964805,0.000008391764,0.0008492774],"genre_scores_gemma":[0.9993488,0.000048797112,0.00015174047,0.000007856191,0.0000015706972,0.0000034812333,0.00010385161,0.000004326379,0.00032962958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974173,0.000021309632,0.000024824945,0.000105190804,0.00004643,0.000060459075],"domain_scores_gemma":[0.9997383,0.00003169681,0.0001202132,0.00001761898,0.000060579612,0.000031575015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029962833,0.00024931095,0.00025555966,0.0011228572,0.00052200985,0.00068843644,0.00031585037,0.00038486108,0.00059711933],"category_scores_gemma":[0.000428887,0.00033901967,0.00020001156,0.00051746186,0.0011687012,0.00027547314,0.00045446813,0.0001847488,0.00017695576],"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":[0.00053349754,0.00005235868,0.8256864,0.00013949072,0.00008454168,0.002026234,0.0037089058,0.0009791282,0.14989455,0.00042644647,0.00017401537,0.016294414],"study_design_scores_gemma":[0.00000842493,0.00007415052,0.9959906,0.000012626324,0.000011177558,0.0003026318,0.00047387092,0.00025828308,0.001856346,0.000027180398,0.0009792439,0.0000055131923],"about_ca_topic_score_codex":0.0735662,"about_ca_topic_score_gemma":0.14432679,"teacher_disagreement_score":0.0735662,"about_ca_system_score_codex":0.0009635414,"about_ca_system_score_gemma":0.000725845,"threshold_uncertainty_score":0.146276},"labels":[],"label_agreement":null},{"id":"W2891343200","doi":"10.1111/jmg.12449","title":"Contrasting degrees of recrystallization of carbonaceous material in the Nelson aureole, British Columbia and Ballachulish aureole, Scotland, with implications for thermometry based on Raman spectroscopy of carbonaceous material","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Metamorphism; Sillimanite; Andalusite; Metamorphic rock; Geology; Recrystallization (geology); Cordierite; Geochemistry; Feldspar; Igneous rock; Raman spectroscopy; Mineralogy; Materials science; Quartz; Petrology; Biotite; Metallurgy; Ceramic; Paleontology","score_opus":0.01019848621675536,"score_gpt":0.20249637498680712,"score_spread":0.19229788877005174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891343200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99871755,0.00006392528,0.000030567,0.000009338808,6.588206e-7,0.0000050016174,0.00017532248,0.000006207564,0.000991373],"genre_scores_gemma":[0.99879754,0.00004764239,0.000087275235,0.000008177045,6.4039995e-7,0.000004522883,0.0002327335,0.000006461534,0.0008149677],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999708,0.000010045967,0.000011544326,0.00006639077,0.0001098159,0.00009421599],"domain_scores_gemma":[0.99930024,0.00004253871,0.00012095891,0.00001805044,0.00035045278,0.00016773633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016090414,0.0003357143,0.00030194974,0.0025576719,0.0015522853,0.0009917766,0.0006031802,0.0003450242,0.0015692284],"category_scores_gemma":[0.0005611085,0.00029377,0.0001231624,0.0016775476,0.0010848106,0.0002412643,0.000597034,0.00024492026,0.0003162056],"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":[0.0007583282,0.00004767754,0.71412796,0.00008260881,0.00007109984,0.0011349448,0.004389503,0.00020638449,0.2675175,0.00020000667,0.0003068979,0.011157157],"study_design_scores_gemma":[0.000002243965,0.00001170204,0.9977309,0.000002718447,0.0000033919005,0.000063041356,0.00058913714,0.000048263442,0.0012584515,0.0000034046468,0.00028368487,0.0000031139666],"about_ca_topic_score_codex":0.7653858,"about_ca_topic_score_gemma":0.91654575,"teacher_disagreement_score":0.2346142,"about_ca_system_score_codex":0.003475508,"about_ca_system_score_gemma":0.0013495801,"threshold_uncertainty_score":0.47199172},"labels":[],"label_agreement":null},{"id":"W2891499259","doi":"10.1111/jmg.12454","title":"A comparison of observed and thermodynamically predicted phase equilibria and mineral compositions in mafic granulites","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; University of Oxford","keywords":"Amphibole; Granulite; Geology; Metamorphic rock; Mafic; Metamorphism; Mineral; Metamorphic facies; Geochemistry; Tremolite; Crust; Eclogite; Mineralogy; Facies; Tectonics; Geomorphology; Chemistry; Materials science; Subduction","score_opus":0.035737469043507324,"score_gpt":0.27588733924567677,"score_spread":0.24014987020216944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891499259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99720603,0.000021516065,0.0022106178,0.0000049056484,8.349219e-7,0.000006149876,0.000104591214,0.000038569062,0.00040676177],"genre_scores_gemma":[0.99924076,0.000009174536,0.00059668405,7.77142e-7,2.3910636e-7,0.000004141934,0.00008584837,0.0000054295,0.000056961675],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998729,0.000022318816,0.000011147627,0.000042280422,0.000036846108,0.000014390279],"domain_scores_gemma":[0.9998449,0.00006499502,0.000025850155,0.000021683994,0.00003439724,0.000008063664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028160552,0.00030528023,0.00017510344,0.00041210084,0.00023461695,0.00040889357,0.00046845264,0.00027425247,0.00068449875],"category_scores_gemma":[0.0007228391,0.00018954872,0.00030126708,0.00019422612,0.00022539549,0.00023727553,0.00017311196,0.00011999417,0.00015161133],"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":[0.00069069525,0.00011093175,0.30881566,0.0001499616,0.00015390343,0.00026637028,0.00028740955,0.3215069,0.34853607,0.0011628609,0.00013479192,0.018184524],"study_design_scores_gemma":[0.00006984779,0.00022357646,0.1577113,0.000010087635,0.000047161782,0.00020259371,0.00014849423,0.6872007,0.15287864,0.0006402806,0.0008424323,0.000024809795],"about_ca_topic_score_codex":0.007156505,"about_ca_topic_score_gemma":0.0063002105,"teacher_disagreement_score":0.007156505,"about_ca_system_score_codex":0.000642417,"about_ca_system_score_gemma":0.0002688453,"threshold_uncertainty_score":0.014229655},"labels":[],"label_agreement":null},{"id":"W2896929921","doi":"10.1111/jmg.12460","title":"Low‐<i>P</i>and high‐<i>T</i>metamorphism of basalts: Insights from the Sudbury impact melt sheet aureole and thermodynamic modelling","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Ilmenite; Anatexis; Metamorphism; Geochemistry; Plagioclase; Basalt; Anorthosite; Pyroxene; Mineral; Partial melting; Hornblende; Metamorphic rock; Olivine; Mineralogy; Petrology; Quartz; Biotite; Materials science","score_opus":0.011221071670744057,"score_gpt":0.19759036355661733,"score_spread":0.18636929188587326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896929921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930951,0.00017763072,0.0017206162,0.000092002476,0.000003084283,0.00001638709,0.0006197853,0.00009490322,0.004180458],"genre_scores_gemma":[0.9986211,0.00007868125,0.000617976,0.000007276476,0.000002228627,0.0000064295004,0.0002632343,0.000025947093,0.00037710354],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999201,0.000013049817,0.0000049166874,0.00002139724,0.000019126057,0.000021449052],"domain_scores_gemma":[0.99991155,0.000029311146,0.000015294354,0.000010683474,0.000016451238,0.000016733811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021162914,0.00045263895,0.00038122464,0.0007732872,0.00058057404,0.0014811018,0.00074431504,0.0006259854,0.0021431819],"category_scores_gemma":[0.00045477174,0.0003262264,0.00070452987,0.00061667414,0.0005411524,0.0005786791,0.00038899205,0.0003467577,0.00036195441],"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":[0.00027931645,0.00022138504,0.22551489,0.00021126724,0.00027000665,0.0011508928,0.00046806113,0.6488419,0.09321893,0.0052655824,0.00093639456,0.023621364],"study_design_scores_gemma":[0.000025056599,0.000038833747,0.109718606,0.000025290357,0.00003529273,0.0001362233,0.00018394153,0.88412315,0.0037970827,0.000894329,0.0009819781,0.00004026691],"about_ca_topic_score_codex":0.119597584,"about_ca_topic_score_gemma":0.09788104,"teacher_disagreement_score":0.119597584,"about_ca_system_score_codex":0.0020900278,"about_ca_system_score_gemma":0.0006558376,"threshold_uncertainty_score":0.23780292},"labels":[],"label_agreement":null},{"id":"W2898178828","doi":"10.1111/jmg.12459","title":"Tectonometamorphic evolution of the tip of the Himalayan metamorphic core in the Jajarkot klippe, west Nepal","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Queen's University; Geological Survey of Canada","funders":"Division of Earth Sciences; Natural Sciences and Engineering Research Council of Canada; Ontario Council on Graduate Studies, Council of Ontario Universities; Geological Society of America; National Science Foundation","keywords":"Geology; Metamorphism; Foreland basin; Greenschist; Metamorphic rock; Geochemistry; Metamorphic facies; Orogeny; Geochronology; Petrology; Seismology; Paleontology; Tectonics; Facies","score_opus":0.020000041828917334,"score_gpt":0.20534883918441454,"score_spread":0.1853487973554972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898178828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99779415,0.00011028574,0.00006851985,0.000022387665,0.0000011054782,0.000007275125,0.00020215784,0.000013153551,0.001780982],"genre_scores_gemma":[0.9993857,0.00004216437,0.000075572156,0.00000727066,0.0000011067548,0.0000037841396,0.00014670905,0.0000026678404,0.0003350232],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992144,0.000006343336,0.00000601826,0.000025223544,0.000017571529,0.000023556286],"domain_scores_gemma":[0.9999105,0.000012711778,0.000023595172,0.000007948094,0.000029065375,0.000016175405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008562628,0.00016425842,0.00017749752,0.0015577578,0.0006046831,0.00080609974,0.00028809812,0.00023510556,0.0011093429],"category_scores_gemma":[0.00024237168,0.00025448884,0.00014534652,0.0011087898,0.0004053351,0.0002218752,0.0005057332,0.00016837896,0.00029550825],"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":[0.00017863422,0.00007362192,0.89314955,0.00018550041,0.00018785553,0.003761797,0.0058477777,0.0030976678,0.060967945,0.0006581009,0.0005781901,0.031313445],"study_design_scores_gemma":[0.0000028100517,0.000011512172,0.99801934,0.000008153876,0.000012831885,0.000279217,0.0003742679,0.00046020444,0.00039211885,0.000016861435,0.00041876142,0.000003875764],"about_ca_topic_score_codex":0.058641516,"about_ca_topic_score_gemma":0.116374046,"teacher_disagreement_score":0.058641516,"about_ca_system_score_codex":0.0006108371,"about_ca_system_score_gemma":0.0003862173,"threshold_uncertainty_score":0.116600394},"labels":[],"label_agreement":null},{"id":"W2905342914","doi":"","title":"Low-pressure and high-temperature metamorphism of basalts: insights from the Sudbury impact melt sheet aureole and thermodynamic modelling","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","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":"Metamorphism; Geology; Basalt; Geochemistry; Petrology","score_opus":0.009369480694314973,"score_gpt":0.2124415980071309,"score_spread":0.2030721173128159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905342914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99334633,0.00018105823,0.0012670128,0.00022847342,0.000006559305,0.000015972368,0.00036366103,0.000066594774,0.004524324],"genre_scores_gemma":[0.9991196,0.00009812759,0.000226715,0.0000111591435,0.0000049928867,0.0000052878113,0.00013962152,0.000024734562,0.00036973835],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998579,0.00002234152,0.000013325157,0.000031895866,0.00003269707,0.000041847674],"domain_scores_gemma":[0.9997596,0.00009968518,0.000031039555,0.000028337754,0.00004614456,0.000035288303],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031604376,0.00048083023,0.0007159973,0.0009172042,0.0010367369,0.0021223186,0.0012652472,0.0013271827,0.0034386774],"category_scores_gemma":[0.0013656417,0.0007071205,0.0007050477,0.001021168,0.0013083023,0.0013319668,0.0007808614,0.0007187065,0.00035531397],"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":[0.0003377865,0.00031239135,0.07814824,0.00012835409,0.00012873608,0.0009073726,0.00038799483,0.8757315,0.030427635,0.004964227,0.0004961495,0.008029571],"study_design_scores_gemma":[0.00008034133,0.000038860235,0.057904113,0.000014595467,0.000032226562,0.00010641863,0.00017324326,0.9374742,0.0022300475,0.0014670407,0.00043852057,0.000040338407],"about_ca_topic_score_codex":0.15589227,"about_ca_topic_score_gemma":0.10729688,"teacher_disagreement_score":0.15589227,"about_ca_system_score_codex":0.0026215208,"about_ca_system_score_gemma":0.0017061253,"threshold_uncertainty_score":0.30996972},"labels":[],"label_agreement":null},{"id":"W2907162222","doi":"10.1111/jmg.12468","title":"A paired metamorphic belt in a subduction‐to‐collision orogen: An example from the South Qilian–North Qaidam orogenic belt,<scp>NW</scp>China","year":2018,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Waterloo","funders":"China Geological Survey; China Scholarship Council; National Natural Science Foundation of China","keywords":"Geology; Metamorphism; Zircon; Subduction; Geochemistry; Metamorphic rock; Granulite; Gneiss; Protolith; Foreland basin; Paleontology; Tectonics; Facies","score_opus":0.03496175734135801,"score_gpt":0.21260380270808593,"score_spread":0.17764204536672792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2907162222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99920976,0.000046960766,0.00009925452,0.00001069544,5.9994125e-7,0.00000598812,0.000086738015,0.000004751834,0.0005352815],"genre_scores_gemma":[0.9995505,0.000031324187,0.0001314289,0.0000036071576,9.669853e-7,0.0000020224481,0.00011430931,0.000001953979,0.00016389208],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999094,0.0000050467647,0.0000083701325,0.00003584938,0.000019489522,0.000021766946],"domain_scores_gemma":[0.99992704,0.00000621392,0.000028871918,0.00000809058,0.000017084869,0.000012724214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014271993,0.00020984127,0.00019645371,0.0016067536,0.0005517924,0.00043661025,0.00025861597,0.00024082833,0.00091281504],"category_scores_gemma":[0.00013686215,0.00018732548,0.000266859,0.0018215082,0.0005079391,0.00016163517,0.00039974798,0.000108360546,0.00009919377],"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":[0.00010113685,0.000021640555,0.95370513,0.00006873525,0.00006498334,0.0011431637,0.0011538218,0.00096642,0.031068116,0.00029666105,0.00009314542,0.011317095],"study_design_scores_gemma":[0.0000042281977,0.000017244787,0.997844,0.000003086258,0.000015667782,0.00017792679,0.00022370803,0.000915071,0.00048939715,0.000030533218,0.00027672615,0.0000025016432],"about_ca_topic_score_codex":0.06621276,"about_ca_topic_score_gemma":0.087787256,"teacher_disagreement_score":0.06621276,"about_ca_system_score_codex":0.000735908,"about_ca_system_score_gemma":0.0005016238,"threshold_uncertainty_score":0.13165474},"labels":[],"label_agreement":null},{"id":"W2909539936","doi":"10.1111/jmg.12469","title":"Divergent behaviour of Th and U during anatexis: Implications for the thermal evolution of orogenic crust","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Anatexis; Granulite; Geology; Crust; Continental crust; Terrane; Geochemistry; Partial melting; Mantle (geology); Migmatite; Craton; Crustal recycling; Hadean; Metamorphism; Petrology; Metamorphic rock; Geomorphology; Tectonics; Paleontology; Facies","score_opus":0.013630741372748166,"score_gpt":0.20897069272079552,"score_spread":0.19533995134804735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909539936","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986382,0.000057192552,0.00029341332,0.000031288433,0.0000011364035,0.0000044535805,0.00007276743,0.000011179027,0.00089023466],"genre_scores_gemma":[0.9996284,0.000028186854,0.00016326786,0.0000048349348,6.4467827e-7,0.0000026657385,0.000049339713,0.0000062448407,0.00011640043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999,0.000014702039,0.000007382708,0.000040086434,0.000014641621,0.000023204673],"domain_scores_gemma":[0.9998567,0.000036178713,0.000038864357,0.000017614784,0.000034351488,0.000016258544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023248591,0.00024242737,0.00033912456,0.0008058855,0.00062341295,0.0009631073,0.00049267284,0.00050550664,0.001142677],"category_scores_gemma":[0.0006038342,0.00029878938,0.00029371455,0.0007381661,0.0006552931,0.00040689993,0.0006429792,0.00028617666,0.00018101378],"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":[0.0005990478,0.000053613378,0.79522216,0.000100535166,0.00018803214,0.000511294,0.0012680071,0.013752697,0.17679757,0.0010061084,0.00008075539,0.010420122],"study_design_scores_gemma":[0.000021562208,0.0000690508,0.9709471,0.000015774496,0.000039667026,0.000111638656,0.0007970557,0.019566366,0.007392382,0.0004023968,0.0006214264,0.00001565868],"about_ca_topic_score_codex":0.055931784,"about_ca_topic_score_gemma":0.035365243,"teacher_disagreement_score":0.055931784,"about_ca_system_score_codex":0.0012216037,"about_ca_system_score_gemma":0.00036382535,"threshold_uncertainty_score":0.11121243},"labels":[],"label_agreement":null},{"id":"W2911359702","doi":"10.1111/jmg.12475","title":"Microstructure and compositional changes across biotite‐rich reaction selvedges around mafic schollen in a semipelitic diatexite migmatite","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Université du Québec à Chicoutimi","funders":"Natural Sciences and Engineering Research Council of Canada; China Scholarship Council","keywords":"Mafic; Biotite; Geology; Migmatite; Plagioclase; Geochemistry; Mineral; Cordierite; Granulite; Petrography; Mineralogy; Metamorphic rock; Quartz; Gneiss; Chemistry; Facies; Geomorphology","score_opus":0.009639048209275695,"score_gpt":0.21373383801714108,"score_spread":0.20409478980786538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2911359702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994686,0.000025256159,0.00003253258,0.0000028077952,3.5505755e-7,0.000003135065,0.00008155292,0.0000048093398,0.00038093462],"genre_scores_gemma":[0.9992712,0.000014908225,0.000052371513,0.0000036895378,3.1263244e-7,0.0000021452506,0.00012675315,0.0000035508108,0.0005249908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990916,0.0000033051904,0.0000036791591,0.000030208446,0.00002571157,0.000027871954],"domain_scores_gemma":[0.9999045,0.0000063837547,0.000018921515,0.000004049562,0.00003657196,0.000029508672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008899127,0.00025350827,0.00022813138,0.0012874074,0.000710052,0.0007706944,0.00040582634,0.00029622726,0.0014329596],"category_scores_gemma":[0.00015226965,0.0002749811,0.00014343906,0.00055167463,0.00073348894,0.00015639236,0.00039671396,0.00014462981,0.00021781423],"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":[0.00049276615,0.000035319816,0.6846574,0.00006912759,0.00009633784,0.0010028682,0.002117901,0.0008113125,0.30345124,0.00016399845,0.00012481771,0.006977037],"study_design_scores_gemma":[0.0000027649708,0.00001824291,0.997428,0.0000025018146,0.00000467863,0.00007582056,0.00040589875,0.00020959259,0.0015065565,0.0000056736058,0.00033768688,0.0000025876018],"about_ca_topic_score_codex":0.24929081,"about_ca_topic_score_gemma":0.4493412,"teacher_disagreement_score":0.24929081,"about_ca_system_score_codex":0.002697519,"about_ca_system_score_gemma":0.0004980889,"threshold_uncertainty_score":0.49567956},"labels":[],"label_agreement":null},{"id":"W2915685285","doi":"10.1111/jmg.12479","title":"Mesozoic to Cenozoic tectono‐metamorphic history of the South Pamir–Hindu Kush (Chitral, <scp>NW</scp> Pakistan): Insights from phase equilibria modelling, and garnet–monazite petrochronology","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Monazite; Gondwana; Orogeny; Geochronology; Cenozoic; Metamorphic rock; Mesozoic; Zircon; Paleontology; Geochemistry; Metamorphic core complex; Plateau (mathematics); Solidus; Tectonics; Structural basin; Extensional definition","score_opus":0.016796521690533826,"score_gpt":0.20281593355231534,"score_spread":0.1860194118617815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2915685285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977939,0.00011044822,0.00053399213,0.000026978418,0.0000015019123,0.0000060787147,0.00020014569,0.00001756926,0.0013093705],"genre_scores_gemma":[0.9993537,0.00006596988,0.0003052317,0.000002611661,8.1067145e-7,0.0000014495191,0.000088957866,0.000002876353,0.00017834187],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999584,0.000005862235,0.0000026355942,0.0000147661885,0.000008082318,0.000010225304],"domain_scores_gemma":[0.99995136,0.00000821485,0.0000146693765,0.000005437436,0.000012863422,0.000007500864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011547021,0.00024189541,0.0001117091,0.00096561277,0.00039799712,0.00062567304,0.00018945962,0.00019476653,0.0019470026],"category_scores_gemma":[0.00016032171,0.00016162716,0.00018222182,0.0010265162,0.00032729335,0.00026138563,0.00030029437,0.00015027983,0.00025683522],"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":[0.0003059822,0.00005598146,0.86285114,0.00017904742,0.00013005061,0.0010957363,0.0012484747,0.024399206,0.059086412,0.0016531086,0.0002813139,0.048713464],"study_design_scores_gemma":[0.0000119681745,0.000052834726,0.97740084,0.000014168266,0.000026629396,0.00021424162,0.0006126873,0.017706847,0.0026077915,0.00023279252,0.0011095101,0.000009800499],"about_ca_topic_score_codex":0.061527975,"about_ca_topic_score_gemma":0.09047282,"teacher_disagreement_score":0.061527975,"about_ca_system_score_codex":0.0006427091,"about_ca_system_score_gemma":0.00052037364,"threshold_uncertainty_score":0.122339666},"labels":[],"label_agreement":null},{"id":"W2940453056","doi":"10.1111/jmg.12485","title":"Slow cooling versus episodic fluid injections: Deciphering the Caledonian orogeny in Vestvågøy, Lofoten islands, Norway","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Manitoba; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada; Queen's University; Sigma Xia; Geological Society of America","keywords":"Geology; Allochthon; Thermochronology; Biotite; Metamorphic rock; Orogeny; Zircon; Muscovite; Titanite; Geochemistry; Terrane; Geochronology; Amphibole; Closure temperature; Metamorphic facies; Shear zone; Petrology; Geomorphology; Paleontology; Facies; Tectonics; Quartz","score_opus":0.014455353068293585,"score_gpt":0.20869167023450427,"score_spread":0.19423631716621068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2940453056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977787,0.0003939458,0.00021476184,0.000020069701,0.000006522722,0.000008536286,0.00022570987,0.000007859138,0.001343869],"genre_scores_gemma":[0.9992483,0.00011035192,0.00023148597,0.000007713461,0.0000021968483,0.0000046998803,0.00017046988,0.0000058731757,0.00021897387],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976975,0.000026225058,0.0000217865,0.00008661754,0.000024836583,0.00007076371],"domain_scores_gemma":[0.9997515,0.00007258191,0.00008283804,0.000016837692,0.00004823392,0.000028025072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003632168,0.00028276048,0.0003488581,0.0013675491,0.00044681705,0.0008101677,0.0005511708,0.00042751202,0.0012663878],"category_scores_gemma":[0.001047914,0.00023717737,0.00028188433,0.0009103167,0.0010076094,0.00045028853,0.00086642464,0.0002010216,0.00022240935],"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":[0.0004942187,0.000050328592,0.9065795,0.00033873503,0.00016034606,0.0038871183,0.010718137,0.006127741,0.029281307,0.00072034687,0.00039064873,0.041251533],"study_design_scores_gemma":[0.000011280094,0.00004321917,0.9939382,0.00006100346,0.000023590675,0.00017234348,0.002129101,0.0014391141,0.00047245945,0.000073949326,0.0016262819,0.000009507945],"about_ca_topic_score_codex":0.2236227,"about_ca_topic_score_gemma":0.35659164,"teacher_disagreement_score":0.2236227,"about_ca_system_score_codex":0.0014114731,"about_ca_system_score_gemma":0.0008996877,"threshold_uncertainty_score":0.44464213},"labels":[],"label_agreement":null},{"id":"W2945188929","doi":"10.1111/jmg.12501","title":"Petrochronology of oxidized granulites from southern Peru","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Granulite; Metamorphism; Geology; Geochemistry; Metamorphic rock; Quartz; Massif; Mineral; Facies; Geomorphology; Structural basin; Chemistry; Paleontology","score_opus":0.007574700670305022,"score_gpt":0.1744812942586876,"score_spread":0.16690659358838258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2945188929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987947,0.00009562948,0.00008567031,0.000008830353,3.731062e-7,0.00000706006,0.00013481687,0.0000105187355,0.00086242525],"genre_scores_gemma":[0.99922335,0.000083695806,0.00016726324,0.000004924793,0.0000014184186,0.0000057649518,0.00029593697,0.0000054052166,0.00021218046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990046,0.000010566063,0.000007406223,0.000029233046,0.000029705974,0.000022641396],"domain_scores_gemma":[0.99988794,0.00001608315,0.000041677624,0.000014759966,0.000030028086,0.0000094689085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013021583,0.00027990073,0.00017439511,0.0018794646,0.00052301213,0.000613895,0.00029145952,0.00035490532,0.001552167],"category_scores_gemma":[0.00032390832,0.00023604736,0.0002159313,0.001295317,0.00040225088,0.00015702489,0.00071340904,0.00011172806,0.00023465251],"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":[0.00043138713,0.00003473817,0.78097117,0.0002614642,0.00015138983,0.0029955385,0.0044719246,0.0013958322,0.18819837,0.00022324688,0.00014119875,0.020723673],"study_design_scores_gemma":[0.000005807288,0.000039580835,0.9955882,0.0000068975874,0.000021306329,0.00056401023,0.0004547787,0.00031768976,0.0018130849,0.000020149086,0.0011653953,0.000003127537],"about_ca_topic_score_codex":0.014330146,"about_ca_topic_score_gemma":0.020962846,"teacher_disagreement_score":0.014330146,"about_ca_system_score_codex":0.00044895476,"about_ca_system_score_gemma":0.00015080966,"threshold_uncertainty_score":0.028493464},"labels":[],"label_agreement":null},{"id":"W2969103136","doi":"10.1111/jmg.12507","title":"The significance of Mn‐rich ilmenite and the determination of <i>P–T</i> paths from zoned garnet in metasedimentary rocks from the western Cape Breton Highlands, Nova Scotia","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Carleton University; University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Ilmenite; Geology; Metamorphism; Geochemistry; Petrography; Metamorphic rock; Mineral; Mineralogy","score_opus":0.008492024335327586,"score_gpt":0.18979680310777783,"score_spread":0.18130477877245024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969103136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988199,0.000059571077,0.00006968504,0.000007229356,9.11969e-7,0.000005812952,0.00020806612,0.000008192278,0.0008204776],"genre_scores_gemma":[0.99958926,0.000024211427,0.000072402494,0.0000036569863,4.2024047e-7,0.00000221996,0.00012214234,0.0000034836983,0.00018206882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998691,0.0000065550457,0.000009633483,0.000043861495,0.000035540623,0.000035291763],"domain_scores_gemma":[0.99971455,0.00003123681,0.000067150424,0.00001698235,0.000112503534,0.000057561498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015236899,0.00024896653,0.00012343859,0.0016753632,0.00075726485,0.00072426646,0.00039560045,0.00021629107,0.000872671],"category_scores_gemma":[0.0004911485,0.00022089768,0.00013901008,0.0010194941,0.0006460084,0.0001603266,0.00028617636,0.00015041,0.00022321535],"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":[0.0001682384,0.0000128204465,0.9044583,0.000044320965,0.000041546446,0.00050944835,0.0007245308,0.000680647,0.08949016,0.000096176744,0.00007824074,0.0036955508],"study_design_scores_gemma":[0.0000017451949,0.000009374926,0.9971686,0.0000046488713,0.000005351318,0.000060661547,0.00024296944,0.00032909337,0.0019693875,0.0000071144723,0.00019931931,0.0000017652599],"about_ca_topic_score_codex":0.67719793,"about_ca_topic_score_gemma":0.8312003,"teacher_disagreement_score":0.32280207,"about_ca_system_score_codex":0.0029968568,"about_ca_system_score_gemma":0.0012326591,"threshold_uncertainty_score":0.6494062},"labels":[],"label_agreement":null},{"id":"W2974707062","doi":"10.1111/jmg.12510","title":"Diachronic metamorphic and structural evolution of the Connecticut Valley–Gaspé trough, Northern Appalachians","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Polytechnique Montréal; Université du Québec à Montréal","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Metamorphic rock; Trough (economics); Orogeny; Transect; Devonian; Thermochronology; Muscovite; Geochronology; Geochemistry; Seismology; Paleontology; Zircon; Geomorphology; Structural basin; Oceanography","score_opus":0.0066586603095630074,"score_gpt":0.1781444608615193,"score_spread":0.1714858005519563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2974707062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966149,0.00020932488,0.000051708274,0.00002722694,0.0000019274387,0.0000092284145,0.00030568446,0.000010187334,0.002769779],"genre_scores_gemma":[0.99875593,0.0000970536,0.00010525298,0.000013170425,0.0000010396305,0.0000070841734,0.00024062657,0.000003285091,0.0007765043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989533,0.000009117908,0.000003590593,0.000040274084,0.00002528138,0.000026464457],"domain_scores_gemma":[0.9998454,0.000014382338,0.00003243215,0.000008806449,0.00007209463,0.00002682471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015333721,0.00023730313,0.0001265385,0.002449142,0.0012961495,0.0009203689,0.00039986,0.00039772046,0.0021974558],"category_scores_gemma":[0.00027861077,0.00020399684,0.000097687356,0.002789486,0.00075313175,0.00020964027,0.00045509523,0.00022664972,0.00018708789],"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":[0.00021337398,0.000058831713,0.94275177,0.000058875496,0.00008135277,0.0013444341,0.0023594112,0.0020505618,0.028294245,0.00044029922,0.00085053424,0.021496346],"study_design_scores_gemma":[0.0000027169167,0.000007681155,0.9980769,0.00001024729,0.00000466416,0.0000784363,0.00049673807,0.00024289526,0.0002841093,0.000015366259,0.0007769009,0.0000032578353],"about_ca_topic_score_codex":0.6473092,"about_ca_topic_score_gemma":0.8488423,"teacher_disagreement_score":0.35269082,"about_ca_system_score_codex":0.00295772,"about_ca_system_score_gemma":0.0011416157,"threshold_uncertainty_score":0.7095357},"labels":[],"label_agreement":null},{"id":"W2979234727","doi":"10.1111/jmg.12511","title":"Muscovite dehydration melting: Reaction mechanisms, microstructures, and implications for anatexis","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Geological Survey of Canada","funders":"Geological Society of London","keywords":"Sillimanite; Muscovite; Geology; Feldspar; Plagioclase; Geochemistry; Cordierite; Alkali feldspar; Anatexis; Quartz; Mineralogy; Biotite; Migmatite; Partial melting; Metamorphic rock; Gneiss; Materials science; Metallurgy; Ceramic; Crust","score_opus":0.012110472558530835,"score_gpt":0.2161737585747393,"score_spread":0.20406328601620846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979234727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971818,0.00048535733,0.0007354548,0.000018175117,0.000001520223,0.000010554341,0.00016618051,0.000021474605,0.0013795671],"genre_scores_gemma":[0.99907243,0.00008357159,0.0002735635,0.000004016987,0.0000015636473,0.0000035471328,0.00008365053,0.0000046910563,0.000472924],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999672,0.0000028346867,0.0000025341774,0.000011186947,0.000007399354,0.000008828512],"domain_scores_gemma":[0.9999373,0.000007797963,0.00002176583,0.0000056632953,0.000017648053,0.000009756484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010122439,0.00014520023,0.00010150199,0.0005017993,0.00027475314,0.00041036826,0.00016908284,0.00015470332,0.0011490001],"category_scores_gemma":[0.000101366866,0.00014336262,0.00010555029,0.0003102746,0.0003218941,0.00027221272,0.000119215656,0.00010264039,0.000168413],"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":[0.00016365567,0.000013542937,0.04873655,0.00004208143,0.000013111651,0.00012545616,0.00019062545,0.00037785474,0.9461157,0.00031864597,0.000019164376,0.00388368],"study_design_scores_gemma":[0.000007498309,0.000081971026,0.7747685,0.0000064479073,0.000012501742,0.00034645273,0.00031480778,0.0017009797,0.22127238,0.0002284183,0.001254305,0.000005674792],"about_ca_topic_score_codex":0.0065258592,"about_ca_topic_score_gemma":0.0058494834,"teacher_disagreement_score":0.0065258592,"about_ca_system_score_codex":0.0004324107,"about_ca_system_score_gemma":0.00012479942,"threshold_uncertainty_score":0.012975752},"labels":[],"label_agreement":null},{"id":"W2982316832","doi":"10.1111/jmg.12513","title":"Mineral assemblages and phase equilibria of metabasites from the prehnite–pumpellyite to amphibolite facies, with the Flin Flon Greenstone Belt (Manitoba) as a type example","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Greenschist; Metamorphism; Geology; Metamorphic facies; Actinolite; Geochemistry; Metamorphic rock; Hornblende; Petrology; Epidote; Facies; Chlorite; Biotite; Geomorphology; Paleontology","score_opus":0.0195402674371956,"score_gpt":0.2238410048098318,"score_spread":0.2043007373726362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982316832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99847335,0.000105432926,0.00006775803,0.000007489034,5.721207e-7,0.0000099698445,0.00049957185,0.0000060552575,0.00082986103],"genre_scores_gemma":[0.99805176,0.00011691461,0.00021861344,0.000014464915,6.0875345e-7,0.0000090373005,0.00068748556,0.0000042317893,0.0008968653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999467,0.0000047698727,0.0000037934055,0.000016613723,0.000010232861,0.000017876084],"domain_scores_gemma":[0.99987733,0.0000076190895,0.000024463723,0.0000047681865,0.000053945652,0.000031810032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011889291,0.00029132282,0.000106699365,0.001942243,0.0005932197,0.00038849306,0.00027399452,0.00014353279,0.0014621553],"category_scores_gemma":[0.00013422086,0.00021843442,0.00012213498,0.0012436232,0.00037266666,0.00017897267,0.00029713294,0.00012907799,0.00030613507],"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":[0.00014549488,0.000030326788,0.9368038,0.000034764893,0.000057734615,0.0001536039,0.0008186328,0.000248661,0.05437543,0.000169232,0.00016360254,0.0069987327],"study_design_scores_gemma":[0.0000025085221,0.000018818835,0.998365,0.0000032498806,0.000007877041,0.00002534291,0.00044341056,0.00012746162,0.0007506744,0.000013886823,0.00024003259,0.0000016954049],"about_ca_topic_score_codex":0.5058988,"about_ca_topic_score_gemma":0.83575016,"teacher_disagreement_score":0.49410123,"about_ca_system_score_codex":0.0018739448,"about_ca_system_score_gemma":0.0010860659,"threshold_uncertainty_score":0.9940222},"labels":[],"label_agreement":null},{"id":"W2997719875","doi":"10.1111/jmg.12521","title":"Complete metamorphic cycle and long‐lived anatexis in the <i>c.</i> 2.1 Ga Mistinibi Complex, Canada","year":2019,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of British Columbia; Centre de Géomatique du Québec; University of Toronto; Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada; Ministère de l'Énergie et des Ressources Naturelles","keywords":"Monazite; Geology; Zircon; Metamorphic rock; Metamorphism; Anatexis; Geochemistry; Archean; Geochronology; Orogeny; Metamorphic facies; Precambrian; Facies; Partial melting; Tectonics; Paleontology; Crust; Structural basin","score_opus":0.023205279114899276,"score_gpt":0.2005164774458261,"score_spread":0.17731119833092682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997719875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9863116,0.000604871,0.00026940927,0.00008417539,0.0000073857186,0.000045377612,0.0038352709,0.000043494012,0.008798418],"genre_scores_gemma":[0.995369,0.0001651372,0.00035162998,0.000024251767,0.0000016854831,0.0000102807,0.0012951179,0.00001674629,0.0027661608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996132,0.000007192376,0.000014036562,0.000116512056,0.000105385225,0.00014374124],"domain_scores_gemma":[0.99954057,0.000011271563,0.00007055337,0.000021119575,0.00029105972,0.00006541045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014742643,0.0003053731,0.00030259928,0.0024955692,0.0028169388,0.0010811199,0.0008555757,0.00032173976,0.0018453397],"category_scores_gemma":[0.0003985283,0.00023667203,0.00023770348,0.0029014715,0.00090155797,0.00023415324,0.00054436736,0.0002977415,0.00034487655],"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":[0.00035727353,0.00005210153,0.89405495,0.00015095586,0.00012819988,0.0011354637,0.003354215,0.0012270665,0.048778918,0.0021645061,0.0026262975,0.04597011],"study_design_scores_gemma":[0.0000033733727,0.000014813667,0.99231875,0.000012477713,0.000014425976,0.00015669907,0.00074901956,0.0003864927,0.0010315686,0.000038806495,0.005265133,0.000008491989],"about_ca_topic_score_codex":0.98519784,"about_ca_topic_score_gemma":0.9954137,"teacher_disagreement_score":0.019842928,"about_ca_system_score_codex":0.019842928,"about_ca_system_score_gemma":0.012807908,"threshold_uncertainty_score":0.1439712},"labels":[],"label_agreement":null},{"id":"W3016399428","doi":"10.1111/jmg.12532","title":"Multiple <i>P–T–d–t</i> paths reveal the evolution of the final Nuna assembly in northeast Australia","year":2020,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Pacific Institute for the Mathematical Sciences; University of British Columbia","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Geochemistry; Metamorphic facies; Metamorphic rock; Orogeny; Granulite; Monazite; Craton; Facies; Greenschist; Mafic; Geochronology; Petrology; Zircon; Geomorphology; Paleontology; Tectonics","score_opus":0.036568050744349385,"score_gpt":0.21481081008351732,"score_spread":0.17824275933916794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016399428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99660504,0.00008512909,0.00020162118,0.000026405736,0.00000213456,0.000008942257,0.00012860596,0.00001610652,0.0029258872],"genre_scores_gemma":[0.9985135,0.00003798693,0.00026150982,0.000009574221,0.0000010166362,0.000005034762,0.0000992338,0.000009584324,0.0010624684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999025,0.0000069954203,0.0000043949567,0.000037522594,0.000020391792,0.000028193346],"domain_scores_gemma":[0.9998042,0.00001356201,0.00004329905,0.000013462322,0.000083158004,0.000042327825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020571396,0.00013719023,0.00015895025,0.0011302927,0.0009135311,0.0007534677,0.0002538803,0.0002336882,0.0019011806],"category_scores_gemma":[0.00040002452,0.00026952822,0.0002193749,0.0005643629,0.00074133417,0.00025985646,0.0009987088,0.00026423406,0.00034454116],"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":[0.00028027734,0.000050189847,0.8206974,0.000107650456,0.0001169585,0.0011748285,0.007857125,0.0016942766,0.13534647,0.0017236809,0.00057867216,0.030372418],"study_design_scores_gemma":[0.0000012446897,0.000014551335,0.9968285,0.0000088489405,0.0000070652654,0.0000883461,0.00045378052,0.0005800859,0.00066604477,0.000052670723,0.0012950709,0.0000038308954],"about_ca_topic_score_codex":0.14661601,"about_ca_topic_score_gemma":0.26599658,"teacher_disagreement_score":0.14661601,"about_ca_system_score_codex":0.0013956199,"about_ca_system_score_gemma":0.0005849358,"threshold_uncertainty_score":0.29152524},"labels":[],"label_agreement":null},{"id":"W3024701419","doi":"10.1111/jmg.12539","title":"Simultaneous operation of opposing reaction mechanisms: The influence of matrix heterogeneity on post‐kinematic garnet crystallization in an inverted metamorphic sequence","year":2020,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Carleton University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Metamorphic rock; Geology; Electron backscatter diffraction; Overprinting; Nucleation; Crystallization; Crystallography; Grain size; Microstructure; Mineralogy; Geochemistry; Chemistry","score_opus":0.03227311207548394,"score_gpt":0.25045604161319257,"score_spread":0.21818292953770863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024701419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995189,0.00006721204,0.00008643425,0.0000044614717,4.104681e-7,0.000002450962,0.000028172239,0.000004709805,0.00028729462],"genre_scores_gemma":[0.9997632,0.000029398332,0.00006949629,0.0000025872223,6.98154e-7,0.0000018696512,0.000036680165,0.0000026430985,0.000093382274],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998129,0.000023056671,0.000015403706,0.000066608554,0.000038395057,0.000043678167],"domain_scores_gemma":[0.99971265,0.0000809094,0.00007946138,0.000020287353,0.00005923055,0.00004739235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020011322,0.00021887975,0.00027498428,0.00064414955,0.0003285824,0.0009129899,0.00025420147,0.0002506932,0.0005529491],"category_scores_gemma":[0.0004099657,0.00027309972,0.00014611578,0.00032724437,0.0007939451,0.0003210736,0.000425258,0.00016490027,0.000116161],"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":[0.00039328873,0.000015676209,0.09424511,0.000059727165,0.000037237693,0.00026925368,0.00031159417,0.0007345569,0.9008486,0.00020696597,0.000010386115,0.0028675562],"study_design_scores_gemma":[0.000011873659,0.00019281998,0.91879463,0.0000067480214,0.000050079816,0.00036158846,0.00040063838,0.0022776844,0.07723271,0.00014070047,0.00051478297,0.000015758555],"about_ca_topic_score_codex":0.0054956716,"about_ca_topic_score_gemma":0.00915218,"teacher_disagreement_score":0.0054956716,"about_ca_system_score_codex":0.00045502497,"about_ca_system_score_gemma":0.00036272267,"threshold_uncertainty_score":0.010927379},"labels":[],"label_agreement":null},{"id":"W3034574229","doi":"10.1111/jmg.12552","title":"Quantitative elemental mapping of granulite‐facies monazite: Textural insights and implications for petrochronology","year":2020,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"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","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Monazite; Granulite; Geology; Metamorphism; Geochemistry; Metamorphic rock; Trace element; Mineralogy; Facies; Zircon; Paleontology","score_opus":0.043252865150059785,"score_gpt":0.24390962861872625,"score_spread":0.20065676346866645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034574229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962287,0.00012617839,0.0018769534,0.000017038941,0.0000011708174,0.0000117366435,0.00046920683,0.000052468222,0.0012164606],"genre_scores_gemma":[0.998106,0.000053891494,0.0013044334,0.000005780966,9.859602e-7,0.0000034882091,0.00015751363,0.0000101066835,0.00035773416],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992716,0.000005657667,0.0000033784245,0.000021432968,0.000028928092,0.000013482379],"domain_scores_gemma":[0.9998859,0.000019752128,0.000018249257,0.000010292311,0.000053651565,0.000012163154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016166538,0.0002312843,0.00013481165,0.0011750517,0.00034643686,0.0005667361,0.00020811295,0.00018502628,0.0007814208],"category_scores_gemma":[0.00026867053,0.00011559614,0.00014151778,0.00064197753,0.00037269844,0.00011428453,0.00023313072,0.0000955802,0.00013173863],"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":[0.0004922431,0.000029920542,0.37195668,0.00012892896,0.00009521088,0.00031371118,0.0010701607,0.004221411,0.5920005,0.00035201886,0.00012480145,0.029214464],"study_design_scores_gemma":[0.0000038690428,0.000026802516,0.97631353,0.000005264583,0.000020433592,0.0001609816,0.000455388,0.0047107716,0.01726878,0.000078777055,0.0009493373,0.000006003605],"about_ca_topic_score_codex":0.13293217,"about_ca_topic_score_gemma":0.26255065,"teacher_disagreement_score":0.13293217,"about_ca_system_score_codex":0.0008783345,"about_ca_system_score_gemma":0.00037557355,"threshold_uncertainty_score":0.26431686},"labels":[],"label_agreement":null},{"id":"W3044763357","doi":"10.1111/jmg.12556","title":"The distinct metamorphic stages and structural styles of the 1.94–1.86 Ga Snowbird Orogen, Northwest Territories, Canada","year":2020,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"University of British Columbia; Geological Survey of Canada; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Craton; Terrane; Metamorphism; Monazite; Geochemistry; Titanite; Archean; Shear zone; Tectonics; Laurentia; Metamorphic rock; Zircon; Fold (higher-order function); Paleontology","score_opus":0.010359878413803357,"score_gpt":0.17599736991438503,"score_spread":0.16563749150058166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3044763357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9719945,0.0008370194,0.00028977628,0.00013137469,0.000010747751,0.000044400673,0.0109522985,0.000057813657,0.015681928],"genre_scores_gemma":[0.98052144,0.00071586354,0.0006397971,0.000053915068,0.0000031852799,0.000016235255,0.0045824726,0.000026034404,0.013441131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987364,0.0000036942945,0.0000036068893,0.00003062428,0.000028948236,0.00005952829],"domain_scores_gemma":[0.99977833,0.0000067483898,0.00003087245,0.0000070159435,0.00012104136,0.00005593483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009749073,0.00025468788,0.00015913876,0.0017274291,0.0015553833,0.0007154339,0.000355989,0.00015733106,0.004132492],"category_scores_gemma":[0.0001801903,0.00017419037,0.00014723002,0.0016887673,0.00049012824,0.0001589804,0.0003405298,0.00021653104,0.000450166],"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":[0.00026739758,0.000045136556,0.91100836,0.00014349334,0.00010132237,0.00068072195,0.0034299642,0.0009319799,0.015684348,0.00116283,0.005855472,0.06068903],"study_design_scores_gemma":[0.0000025384797,0.00000539868,0.99494725,0.000014859947,0.0000044745616,0.00005220879,0.000713567,0.00013665904,0.0002804947,0.000018087738,0.0038209173,0.0000036409442],"about_ca_topic_score_codex":0.9865182,"about_ca_topic_score_gemma":0.9975459,"teacher_disagreement_score":0.013481796,"about_ca_system_score_codex":0.00915349,"about_ca_system_score_gemma":0.007864345,"threshold_uncertainty_score":0.06641352},"labels":[],"label_agreement":null},{"id":"W3080903969","doi":"10.1111/jmg.12562","title":"Major and trace element mapping of garnet: Unravelling the conditions, timing and rates of metamorphism of the Snowcap assemblage, west‐central Yukon","year":2020,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Metamorphic rock; Geochronology; Trace element; Geochemistry; Mineralogy","score_opus":0.034164418648269294,"score_gpt":0.22743484484469584,"score_spread":0.19327042619642654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080903969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995009,0.0000097591665,0.00014674176,0.0000041958606,2.1885934e-7,0.0000016499484,0.00014969295,0.000020010764,0.00016682805],"genre_scores_gemma":[0.9994325,0.000011052915,0.00022215072,0.0000018348935,2.0250647e-7,0.0000018932622,0.00023669323,0.0000064195056,0.000087266446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999651,0.0000041605676,0.0000019738898,0.000013132844,0.0000059023846,0.000009617104],"domain_scores_gemma":[0.99994767,0.000009294966,0.000009889307,0.000007226428,0.000016501563,0.0000094517545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000082760336,0.00024423187,0.00018536621,0.00041763135,0.00030667314,0.00030924863,0.0002908541,0.00024096544,0.00059789617],"category_scores_gemma":[0.00013413884,0.00018354501,0.000363562,0.00044224778,0.00018423567,0.0001919524,0.00020240601,0.000082235536,0.0000936302],"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":[0.00043273577,0.0000681576,0.7674824,0.000096986376,0.0001644116,0.00044268928,0.00075371587,0.1182669,0.10016024,0.00045520955,0.00024393723,0.011432634],"study_design_scores_gemma":[0.00003664646,0.000105655956,0.75110245,0.000009566175,0.00006360567,0.00012694273,0.0004883597,0.23909387,0.007545014,0.00020064552,0.001212383,0.000014950157],"about_ca_topic_score_codex":0.23082802,"about_ca_topic_score_gemma":0.28622895,"teacher_disagreement_score":0.76917195,"about_ca_system_score_codex":0.0012743354,"about_ca_system_score_gemma":0.00075800734,"threshold_uncertainty_score":0.45896888},"labels":[],"label_agreement":null},{"id":"W3093924455","doi":"10.1111/jmg.12576","title":"Metamorphic evolution of the Great Slave Lake shear zone","year":2020,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Government of Northwest Territories; Simon Fraser University","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Mylonite; Shear zone; Greenschist; Overprinting; Granulite; Metamorphic rock; Geochemistry; Metamorphic facies; Mafic; Craton; Petrology; Diachronous; Geomorphology; Facies; Seismology; Tectonics; Structural basin","score_opus":0.0188665330339587,"score_gpt":0.1863558753301372,"score_spread":0.1674893422961785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093924455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941754,0.000032403812,0.000037166745,0.0000064462247,4.4869844e-7,0.0000022993095,0.00007292923,0.000005703381,0.00042510935],"genre_scores_gemma":[0.9994993,0.000018227609,0.000054637974,0.0000051023985,5.766981e-7,0.0000022558777,0.00013013442,0.0000024312103,0.00028727914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.0000032817088,0.0000043522373,0.000017596967,0.00001730739,0.0000130868],"domain_scores_gemma":[0.9999409,0.000004353426,0.000024382332,0.000004401535,0.000015041818,0.000010960452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000099999044,0.00017848391,0.00015444524,0.0010347738,0.00036385914,0.00052554975,0.00014168427,0.00019184829,0.001877925],"category_scores_gemma":[0.0001993682,0.00018740854,0.00013428077,0.0007291478,0.00047370256,0.00015250884,0.0006387027,0.00010310842,0.00022279691],"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":[0.00023986383,0.00002621413,0.78586364,0.00010285096,0.0000796838,0.00052810716,0.0019273406,0.0015671933,0.19742468,0.0004666487,0.00022177366,0.011552068],"study_design_scores_gemma":[0.000006332604,0.00002523301,0.9968142,0.0000062531476,0.0000068657087,0.00006768777,0.00021014368,0.0006309589,0.0016744196,0.000030281892,0.0005245269,0.0000031595741],"about_ca_topic_score_codex":0.018670501,"about_ca_topic_score_gemma":0.038032833,"teacher_disagreement_score":0.018670501,"about_ca_system_score_codex":0.00054947234,"about_ca_system_score_gemma":0.00028869588,"threshold_uncertainty_score":0.03712362},"labels":[],"label_agreement":null},{"id":"W3107034389","doi":"10.1111/jmg.12583","title":"Delineation of multiple metamorphic events in the Himalayan Kathmandu Complex, central Nepal","year":2020,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of California, Santa Barbara","keywords":"Titanite; Allanite; Geology; Metamorphic rock; Geothermobarometry; Metamorphism; Geochemistry; Trace element; Monazite; Quartz; Isograd; Mineralogy; Zircon; Metamorphic facies; Paleontology","score_opus":0.04588999606107844,"score_gpt":0.22082081028478964,"score_spread":0.1749308142237112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3107034389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982681,0.00015254524,0.00009428005,0.000020418853,7.2942464e-7,0.000014517697,0.00005687362,0.0000048563593,0.0013877036],"genre_scores_gemma":[0.99920684,0.00008379641,0.00025920413,0.000011285189,0.0000013807208,0.00001222834,0.000109619206,0.0000021390736,0.00031349887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998306,0.000025291583,0.000016375292,0.00005190184,0.000033910303,0.000041924144],"domain_scores_gemma":[0.9998331,0.0000330734,0.000050136478,0.000013640723,0.00004599996,0.000023947567],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021946194,0.000214092,0.00019401696,0.002199482,0.0009896623,0.00082415855,0.0004086348,0.00031100374,0.0011359233],"category_scores_gemma":[0.00048172547,0.0002405339,0.00016641982,0.0014030808,0.0006075181,0.00039575322,0.00093965506,0.00015734861,0.00017352875],"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":[0.00014388157,0.00006782407,0.8831169,0.00022494813,0.00011576633,0.0035061822,0.014226125,0.0006696907,0.049461875,0.0012301796,0.00032546083,0.046911106],"study_design_scores_gemma":[0.000002964657,0.000025639956,0.99596184,0.000015891617,0.000017244134,0.00066826143,0.0013802967,0.0005338342,0.0006932484,0.00005188708,0.00064330554,0.0000055863934],"about_ca_topic_score_codex":0.04306851,"about_ca_topic_score_gemma":0.09199647,"teacher_disagreement_score":0.04306851,"about_ca_system_score_codex":0.0008535705,"about_ca_system_score_gemma":0.00065889896,"threshold_uncertainty_score":0.0856356},"labels":[],"label_agreement":null},{"id":"W3133581279","doi":"10.1111/jmg.12599","title":"Lu–Hf garnet dating and the timing of collisions: Palaeoproterozoic accretionary tectonics revealed in the Southeastern Churchill Province, Trans‐Hudson Orogen, Canada","year":2021,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Centre de Géomatique du Québec; University of Toronto; University of British Columbia; Université Laval","funders":"British Columbia Knowledge Development Fund; Ministère de l'Énergie et des Ressources Naturelles; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Granulite; Metamorphism; Geochemistry; Craton; Anatexis; Zircon; Geochronology; Archean; Tectonics; Continental collision; Metamorphic facies; Orogeny; Terrane; Continental crust; Crust; Laurentia; Petrology; Facies; Paleontology; Subduction; Paleozoic; Partial melting","score_opus":0.01442643138104498,"score_gpt":0.19503039552202672,"score_spread":0.18060396414098173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3133581279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99545044,0.00025976254,0.00019297747,0.000033716828,0.000003942436,0.000010104954,0.0011594837,0.00001870927,0.002870917],"genre_scores_gemma":[0.99761415,0.00011603489,0.00034529972,0.000012577013,0.0000013033034,0.0000047795174,0.00054537365,0.000009860304,0.0013506085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997904,0.000010494376,0.00001054345,0.00005213872,0.00006839631,0.000068121655],"domain_scores_gemma":[0.9995468,0.00002234955,0.000071637405,0.00001917309,0.00028479428,0.00005518857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025552654,0.0002798108,0.00021373385,0.00204148,0.0013278611,0.00083806243,0.0007320606,0.00021996618,0.0015952779],"category_scores_gemma":[0.00054104486,0.00018057246,0.00015343915,0.0024209034,0.00054759096,0.00020113184,0.00042702322,0.00022189127,0.00017779531],"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":[0.00014347711,0.000014697016,0.95920175,0.00004362242,0.00005403619,0.0002198639,0.0016405396,0.000913945,0.018209392,0.00041192982,0.0007474784,0.01839923],"study_design_scores_gemma":[0.0000021241774,0.0000068561176,0.99703974,0.000007726425,0.000007878266,0.00003144654,0.0004411551,0.000361296,0.00089377456,0.000009426659,0.0011950533,0.0000033869464],"about_ca_topic_score_codex":0.9807654,"about_ca_topic_score_gemma":0.9941116,"teacher_disagreement_score":0.019234598,"about_ca_system_score_codex":0.008758858,"about_ca_system_score_gemma":0.006005448,"threshold_uncertainty_score":0.063550234},"labels":[],"label_agreement":null},{"id":"W3160337191","doi":"10.1111/jmg.12609","title":"Late Variscan (315 Ma) subduction or deceptive zircon REE patterns and U–Pb dates from migmatite‐hosted eclogites? (Montagne Noire, France)","year":2021,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Memorial University of Newfoundland","funders":"Institut national des sciences de l'Univers; Česká geologická služba","keywords":"Eclogite; Zircon; Geology; Migmatite; Protolith; Geochemistry; Metamorphism; Subduction; Metamorphic rock; Granulite; Massif; Metamorphic facies; Petrology; Facies; Tectonics; Seismology; Geomorphology; Gneiss","score_opus":0.014377722029929343,"score_gpt":0.20266086839073907,"score_spread":0.18828314636080973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3160337191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969426,0.00025269628,0.000087487206,0.00002012528,0.000003275451,0.0000024356573,0.0004896658,0.000021142045,0.0021805803],"genre_scores_gemma":[0.9984425,0.000045713412,0.00006607758,0.0000076989545,0.000003820888,0.000001191716,0.00058847957,0.0000054393163,0.00083920377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999157,0.0000070049664,0.0000039628326,0.0000337898,0.000011567546,0.000027962045],"domain_scores_gemma":[0.9999342,0.000007070036,0.000019276538,0.0000064897235,0.000017717375,0.00001519498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015126534,0.00023004564,0.00014240225,0.0012896151,0.00043380682,0.0007045779,0.00021911172,0.0004214393,0.0020834804],"category_scores_gemma":[0.00015033499,0.00009287923,0.00017401406,0.000721372,0.00032090684,0.00015744993,0.0003260016,0.0001383183,0.0004850393],"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":[0.0006826768,0.0000350604,0.9127803,0.000044124597,0.000083533574,0.0009126935,0.0013665572,0.0003365479,0.06468201,0.00024983464,0.00047678367,0.018349819],"study_design_scores_gemma":[0.0000019044984,0.00001817846,0.9982311,0.0000032978287,0.0000039979377,0.00008553121,0.00008497551,0.00005815897,0.00059262186,0.000005551153,0.00091350084,0.0000011124043],"about_ca_topic_score_codex":0.05773832,"about_ca_topic_score_gemma":0.10568243,"teacher_disagreement_score":0.05773832,"about_ca_system_score_codex":0.00081498496,"about_ca_system_score_gemma":0.00018648928,"threshold_uncertainty_score":0.11480445},"labels":[],"label_agreement":null},{"id":"W3172950298","doi":"10.1111/jmg.12622","title":"Phase equilibria and microstructural constraints on the high‐<i>T</i> building of the Kohistan island arc: The Jijal garnet granulites, northern Pakistan","year":2021,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Calgary","funders":"","keywords":"Geology; Mafic; Geochemistry; Recrystallization (geology); Granulite; Island arc; Crust; Petrology; Paleontology; Subduction; Tectonics; Facies; Structural basin","score_opus":0.012015109471832878,"score_gpt":0.2232710504421334,"score_spread":0.21125594097030054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3172950298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99854857,0.000034412093,0.00006190043,0.000008921974,6.3273177e-7,0.0000040889086,0.00012109995,0.000003950077,0.0012164037],"genre_scores_gemma":[0.9997317,0.000014693818,0.000052826435,0.0000021513706,9.860594e-7,0.0000023127413,0.00007051035,0.000002469736,0.00012239309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999232,0.0000051881234,0.000006025932,0.000026274847,0.000014052436,0.000025185826],"domain_scores_gemma":[0.9998629,0.00002695162,0.000053339943,0.000008392523,0.000028252545,0.000020101097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090177404,0.00013974117,0.00015055707,0.0013102955,0.0008938067,0.0010711863,0.00022659851,0.00021833011,0.0024922227],"category_scores_gemma":[0.00024746094,0.00020191197,0.00011073191,0.00078822154,0.0009666419,0.00019720814,0.0003691312,0.00018175122,0.0003311902],"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":[0.00075965706,0.00008484727,0.68826526,0.00018151106,0.00007953321,0.0015610512,0.003240599,0.0029305296,0.2812284,0.0017739253,0.00025435316,0.019640358],"study_design_scores_gemma":[0.000012653949,0.000049484934,0.9932243,0.000005992564,0.000014393371,0.00021934457,0.0010239069,0.00053596246,0.0038797543,0.00014323762,0.0008847324,0.0000062163235],"about_ca_topic_score_codex":0.027336948,"about_ca_topic_score_gemma":0.036118776,"teacher_disagreement_score":0.027336948,"about_ca_system_score_codex":0.00084524986,"about_ca_system_score_gemma":0.0003987158,"threshold_uncertainty_score":0.05435568},"labels":[],"label_agreement":null},{"id":"W3174948366","doi":"10.1111/jmg.12624","title":"Bulk inclusion micro‐zircon U–Pb geochronology: A new tool to date low‐grade metamorphism","year":2021,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Fredericton; University of New Brunswick; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Universität Wien","keywords":"Zircon; Metamorphism; Geology; Geochronology; Geochemistry; Metamorphic rock; Greenschist; Metamorphic facies; Schist; Petrology; Facies; Geomorphology","score_opus":0.015572515114826444,"score_gpt":0.21751470899502845,"score_spread":0.20194219388020201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3174948366","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8661274,0.0010558354,0.12653324,0.000040871262,0.000018799248,0.000040850922,0.00085270364,0.0011806664,0.004149744],"genre_scores_gemma":[0.94559,0.00026628826,0.052496735,0.000010500603,0.0000072609487,0.000020160167,0.00032139124,0.00009656423,0.0011911283],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99987304,0.000008889199,0.0000053942363,0.000048190355,0.000051952775,0.000012527724],"domain_scores_gemma":[0.99989915,0.000016289343,0.000025741147,0.000017986144,0.000033613982,0.000007173243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019801458,0.0003521679,0.00034970974,0.00095431064,0.00019881048,0.0005278297,0.00031623183,0.00022931794,0.0009007539],"category_scores_gemma":[0.00020365462,0.00023911029,0.00017564005,0.00038620073,0.00022059816,0.0002733185,0.0004017385,0.0002347559,0.00033533096],"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":[0.00007424169,0.00000819312,0.0102796955,0.00006341713,0.00002149934,0.000063908905,0.00007344871,0.0007714721,0.96363664,0.00028895077,0.00008475449,0.024633758],"study_design_scores_gemma":[0.000020907546,0.00029135792,0.13080378,0.000030493235,0.000070637034,0.0009834184,0.00013658537,0.034798335,0.8245779,0.00051080587,0.007741026,0.000034699948],"about_ca_topic_score_codex":0.0028381112,"about_ca_topic_score_gemma":0.006246244,"teacher_disagreement_score":0.0028381112,"about_ca_system_score_codex":0.00023304939,"about_ca_system_score_gemma":0.00027403815,"threshold_uncertainty_score":0.0056432486},"labels":[],"label_agreement":null},{"id":"W3176313697","doi":"10.1111/jmg.12623","title":"Pressure–temperature–time evolution of subducted crust revealed by complex garnet zoning (Theodul Glacier Unit, Switzerland)","year":2021,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 British Columbia","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Geology; Metamorphic rock; Schist; Mafic; Geochemistry; Lawsonite; Lithology; Subduction; Glaucophane; Petrology; Tectonics; Seismology; Eclogite","score_opus":0.011749489250783621,"score_gpt":0.1976118753718317,"score_spread":0.18586238612104808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3176313697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995578,0.00004864106,0.00005008101,0.000003648629,4.6344928e-7,0.0000010704609,0.00007654926,0.000010882494,0.00025086326],"genre_scores_gemma":[0.9998068,0.000014681447,0.00003522034,0.000001023978,4.891874e-7,7.029407e-7,0.000074475036,0.0000027243887,0.00006394046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996674,0.000003624097,0.0000017508984,0.000011622752,0.000006436722,0.000009790075],"domain_scores_gemma":[0.9999447,0.000008945404,0.000019224583,0.0000057002267,0.000011089164,0.000010366998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009480056,0.00032513068,0.00012816893,0.0012129621,0.00018844118,0.0004103338,0.00012022987,0.00022138642,0.0011186923],"category_scores_gemma":[0.000116778276,0.00013749984,0.00013636168,0.00050723605,0.0003568228,0.00015667849,0.00020086257,0.000089274814,0.00013005166],"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":[0.0004811273,0.000031378106,0.6117286,0.00007010078,0.00011359072,0.0010817697,0.0005560725,0.0058584185,0.36824298,0.00028158168,0.00017299484,0.011381464],"study_design_scores_gemma":[0.0000019053319,0.000020593861,0.9956743,0.0000015546032,0.0000065175923,0.00005954577,0.00003749178,0.0013126953,0.0027305966,0.00001431177,0.00013754985,0.0000028846882],"about_ca_topic_score_codex":0.015201015,"about_ca_topic_score_gemma":0.01840934,"teacher_disagreement_score":0.015201015,"about_ca_system_score_codex":0.00045775555,"about_ca_system_score_gemma":0.000116663876,"threshold_uncertainty_score":0.030225039},"labels":[],"label_agreement":null},{"id":"W3209342003","doi":"10.1111/jmg.12640","title":"The tempo and conditions of metamorphism during magmatism, southern Coast Mountains batholith, British Columbia, Canada","year":2021,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Geological Survey of Canada","funders":"National Science Foundation of Sri Lanka","keywords":"Metamorphism; Geology; Magmatism; Batholith; Geochemistry; Metamorphic rock; Pluton; Partial melting; Metamorphic facies; Solidus; Petrology; Facies; Geomorphology; Crust; Paleontology; Tectonics; Structural basin","score_opus":0.005369160832198272,"score_gpt":0.16617723462403847,"score_spread":0.1608080737918402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3209342003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795322,0.0018728547,0.00016500393,0.00035346314,0.000012650622,0.000037916718,0.0065412675,0.00005700823,0.011427588],"genre_scores_gemma":[0.98764277,0.00094305567,0.00030084435,0.000053778473,0.0000027542205,0.000015734879,0.0016701577,0.000018014494,0.009352935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997224,0.000014101792,0.00001793063,0.00006252899,0.00007787173,0.00010520673],"domain_scores_gemma":[0.9989126,0.00004557028,0.00010318575,0.000023964409,0.00071972125,0.00019498754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020461965,0.00028238195,0.00020483321,0.0028592136,0.0034677975,0.0013585052,0.0007743568,0.0002707785,0.005804466],"category_scores_gemma":[0.0007706816,0.00031684627,0.00018407429,0.0041456353,0.0008264226,0.00038999383,0.00059697684,0.00039558555,0.00057669805],"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":[0.00014598307,0.000034963836,0.9385748,0.00021743157,0.0000775013,0.00048071676,0.003914028,0.0004945679,0.0048219184,0.0004763653,0.0055461843,0.04521552],"study_design_scores_gemma":[0.0000027245603,0.0000046470077,0.9942264,0.0000423413,0.000010151779,0.000050693736,0.0019491093,0.00013252474,0.0002854528,0.000021921047,0.0032662144,0.0000079620695],"about_ca_topic_score_codex":0.99745005,"about_ca_topic_score_gemma":0.9994868,"teacher_disagreement_score":0.024561627,"about_ca_system_score_codex":0.024561627,"about_ca_system_score_gemma":0.019534918,"threshold_uncertainty_score":0.17820793},"labels":[],"label_agreement":null},{"id":"W4200411586","doi":"10.1111/jmg.12648","title":"Testing the equilibrium model: An example from the Caledonian Kalak Nappe Complex (Finnmark, Arctic Norway)","year":2021,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"University of British Columbia; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Metamorphism; Metamorphic rock; Geology; Nappe; Solidus; Geothermobarometry; Orogeny; Alpine orogeny; Isograd; Geochemistry; Mineralogy; Geomorphology; Metamorphic facies; Chemistry; Paleontology; Tectonics","score_opus":0.09546939682737567,"score_gpt":0.23183235071722355,"score_spread":0.13636295388984787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200411586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980982,0.000032308242,0.0004048599,0.000022912443,0.0000018584892,0.000012498584,0.00022060932,0.000014665138,0.0011920603],"genre_scores_gemma":[0.99834824,0.000025213007,0.00087863265,0.000007166893,0.0000010371834,0.000009655556,0.00032064438,0.000012210855,0.0003970961],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9997422,0.00007780232,0.0000143309235,0.00007190825,0.000041837364,0.000051965646],"domain_scores_gemma":[0.99917775,0.00046462464,0.000043183903,0.000055164834,0.00021906995,0.000040109848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062541704,0.0004377231,0.00037398256,0.0007229005,0.00090154255,0.0007957443,0.0012005743,0.0007124864,0.0017861233],"category_scores_gemma":[0.0013926082,0.00023020933,0.00052318146,0.0006492306,0.0008419742,0.0005174113,0.00058673124,0.00023764117,0.0001869365],"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":[0.0005185152,0.00025898044,0.19047832,0.00016634718,0.00013302533,0.0021975227,0.0014799394,0.78753906,0.004852835,0.0039342246,0.00074335624,0.0076978407],"study_design_scores_gemma":[0.00021110321,0.00034658168,0.11669969,0.000044268378,0.000084077474,0.0002508058,0.0033644366,0.8691599,0.0043566357,0.001973415,0.0034439967,0.0000650213],"about_ca_topic_score_codex":0.40654466,"about_ca_topic_score_gemma":0.38423878,"teacher_disagreement_score":0.40654466,"about_ca_system_score_codex":0.0035340604,"about_ca_system_score_gemma":0.0010697392,"threshold_uncertainty_score":0.8083566},"labels":[],"label_agreement":null},{"id":"W4229447147","doi":"10.1111/jmg.12667","title":"Garnet, zircon, and monazite age and REE signatures in (ultra)high‐temperature and high‐pressure rocks: Examples from the Caledonides and the Pamir","year":2022,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 British Columbia","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Vetenskapsrådet; Bundesministerium für Bildung und Forschung; Canada Foundation for Innovation","keywords":"Monazite; Zircon; Geology; Geochemistry; Felsic; Migmatite; Granulite; Rare-earth element; Metamorphism; Recrystallization (geology); Xenolith; Gneiss; Metamictization; Metamorphic rock; Mineralogy; Petrology; Rare earth; Mafic; Mantle (geology); Paleontology","score_opus":0.007846148200733632,"score_gpt":0.17178200411697614,"score_spread":0.16393585591624252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229447147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982875,0.00016858289,0.000054417796,0.0000060135853,8.277662e-7,0.000003477337,0.00011588433,0.000006533421,0.0013567556],"genre_scores_gemma":[0.9991757,0.000096290576,0.00017324685,0.00000526907,0.0000014440885,0.0000015680771,0.00020262589,0.0000037133395,0.0003401187],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998217,0.000014243183,0.000012812221,0.000055117427,0.000038313243,0.000057960224],"domain_scores_gemma":[0.9998568,0.000020598878,0.00005185526,0.000018687218,0.00003171218,0.000020258492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002186234,0.00030527034,0.0002401517,0.0026388604,0.00049553526,0.0004960376,0.00035956263,0.00027656814,0.0008479701],"category_scores_gemma":[0.0002663443,0.00017315736,0.00021616017,0.0017470231,0.0004888724,0.00016861898,0.0006324943,0.00017202251,0.00020699228],"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":[0.0006120389,0.000051746752,0.8144271,0.0001576172,0.00014074089,0.002545008,0.0041248747,0.00049526145,0.14668763,0.0004304825,0.00016420244,0.030163301],"study_design_scores_gemma":[0.0000024004514,0.000037250913,0.9970118,0.0000035887779,0.000009999219,0.0004486687,0.0002735142,0.00007577338,0.0016577409,0.0000117434265,0.00046509717,0.0000024572123],"about_ca_topic_score_codex":0.020824077,"about_ca_topic_score_gemma":0.057492938,"teacher_disagreement_score":0.020824077,"about_ca_system_score_codex":0.0004224696,"about_ca_system_score_gemma":0.00021317354,"threshold_uncertainty_score":0.041405737},"labels":[],"label_agreement":null},{"id":"W4281255549","doi":"10.1111/jmg.12678","title":"Garnet crystallization mechanisms and localized polymetamorphism in the southwestern Meguma Terrane, Nova Scotia, Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"American Association of Petroleum Geologists; Geological Society of America","keywords":"Terrane; Geology; Metamorphic rock; Metamorphism; Orogeny; Geochemistry; Metamorphic facies; Recrystallization (geology); Alpine orogeny; Mineralogy; Petrology; Geomorphology; Facies; Tectonics; Seismology","score_opus":0.013077957996154839,"score_gpt":0.18379910852851924,"score_spread":0.17072115053236442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281255549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99688655,0.0002467821,0.000058887523,0.00003782484,0.0000018915936,0.000013238167,0.00086371246,0.000008526751,0.0018825738],"genre_scores_gemma":[0.9985644,0.00015017153,0.00011263386,0.000016080437,8.0826015e-7,0.0000065344793,0.00039869538,0.0000039710876,0.00074666564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986506,0.0000042037827,0.0000072283265,0.000034917273,0.000031258085,0.000057251404],"domain_scores_gemma":[0.99967134,0.000020652922,0.00004852514,0.000013089867,0.00018862922,0.000057801484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012500893,0.00032040852,0.0002113817,0.0017563023,0.001712851,0.0006950615,0.00045275132,0.00019810694,0.001300802],"category_scores_gemma":[0.00030893568,0.00021387593,0.00023472411,0.0015935648,0.0007054812,0.0001519142,0.00039345573,0.00017660465,0.00018100084],"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":[0.00032682737,0.000034066477,0.9306444,0.00012776007,0.00012345576,0.0014329582,0.0015465141,0.0019844135,0.050158393,0.00035999235,0.00064051576,0.012620668],"study_design_scores_gemma":[0.0000049853993,0.000008221298,0.99766135,0.000013814142,0.000009526574,0.00009016384,0.0005297917,0.00031190072,0.0007210896,0.000015161757,0.0006280354,0.000005913819],"about_ca_topic_score_codex":0.9777509,"about_ca_topic_score_gemma":0.99336433,"teacher_disagreement_score":0.022249103,"about_ca_system_score_codex":0.008454152,"about_ca_system_score_gemma":0.006469795,"threshold_uncertainty_score":0.061339498},"labels":[],"label_agreement":null},{"id":"W4294203117","doi":"10.1111/jmg.12690","title":"Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet","year":2022,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Carleton University; University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Staurolite; Geology; Leucogranite; Schist; Muscovite; Geochemistry; Grossular; Sillimanite; Biotite; Metamorphic rock; Plagioclase; Kyanite; Mineralogy; Quartz; Paleontology; Gneiss","score_opus":0.01708929999311622,"score_gpt":0.2029997706673794,"score_spread":0.18591047067426317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294203117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99937063,0.000025852607,0.000024185227,0.000006696552,0.0000012736572,0.0000018066652,0.00007268155,0.0000045909305,0.00049230276],"genre_scores_gemma":[0.9996637,0.000011681829,0.000022264107,0.000004701565,0.0000019292977,0.0000022802315,0.00010247987,0.000001877457,0.00018907263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994695,0.0000074062496,0.0000028741572,0.000015681095,0.000012802576,0.000014362224],"domain_scores_gemma":[0.999928,0.000007530814,0.000020032494,0.0000038782687,0.00002460878,0.000016007954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013558929,0.00020092867,0.00018993551,0.0008093571,0.00044885892,0.0004492919,0.0002551436,0.00029938022,0.0015414489],"category_scores_gemma":[0.00017942787,0.00012592356,0.00011280716,0.0005384589,0.00035501446,0.00015204244,0.0003181745,0.00015480012,0.00020834088],"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":[0.0010350012,0.0000957989,0.6493569,0.00011360539,0.00008766781,0.0017324002,0.0021557137,0.0015488706,0.33322138,0.0001880333,0.00026513572,0.010199574],"study_design_scores_gemma":[0.000004972418,0.0000453515,0.9972409,0.0000033698977,0.0000063747325,0.000071916904,0.00033365033,0.0004010088,0.0016724906,0.000013937194,0.00020235196,0.0000036394808],"about_ca_topic_score_codex":0.015320015,"about_ca_topic_score_gemma":0.02323674,"teacher_disagreement_score":0.015320015,"about_ca_system_score_codex":0.0006134441,"about_ca_system_score_gemma":0.00015471365,"threshold_uncertainty_score":0.030461669},"labels":[],"label_agreement":null},{"id":"W4307982922","doi":"10.1111/jmg.12698","title":"Trapped K‐feldspar phenocrysts as a signature of melt migration pathways within active high‐strain zones","year":2022,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 British Columbia","funders":"Australian Research Council","keywords":"Phenocryst; Geology; Shear zone; Feldspar; Quartz; Biotite; Mineralogy; Geochemistry; Crust; Plagioclase; Petrology; Seismology","score_opus":0.013571789057725391,"score_gpt":0.19115797749851623,"score_spread":0.17758618844079085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307982922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99961436,0.000029978215,0.000067134344,0.0000031990885,3.5141025e-7,0.0000014628249,0.000051472856,0.0000054059246,0.00022669103],"genre_scores_gemma":[0.9996363,0.000015281425,0.00008915596,0.0000018753492,4.8316514e-7,0.0000010591955,0.00006318946,0.0000021542528,0.00019055414],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000018138882,0.000002592619,0.000014027521,0.000010401725,0.000014462149],"domain_scores_gemma":[0.9998888,0.00000903994,0.00004502701,0.000009916716,0.000024579904,0.000022662387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006259895,0.00012675094,0.00011103177,0.0007719303,0.00022905659,0.00036087702,0.00018243687,0.00016678902,0.0009028436],"category_scores_gemma":[0.000103424805,0.00012554097,0.000088860004,0.0003339473,0.0003925908,0.00015346418,0.0002561544,0.00013618715,0.0001336227],"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":[0.0003142995,0.00003840702,0.3005978,0.00005031574,0.000044807515,0.00054623396,0.0009478247,0.0003143674,0.69185483,0.0001964845,0.00007376761,0.0050208014],"study_design_scores_gemma":[0.0000037997238,0.000045656932,0.98042744,0.0000033454348,0.000007926928,0.0002660263,0.00029833935,0.0004674155,0.018169241,0.000026822798,0.000280412,0.0000034408995],"about_ca_topic_score_codex":0.009126361,"about_ca_topic_score_gemma":0.013019253,"teacher_disagreement_score":0.009126361,"about_ca_system_score_codex":0.00024334861,"about_ca_system_score_gemma":0.00014090406,"threshold_uncertainty_score":0.018146515},"labels":[],"label_agreement":null},{"id":"W4308020751","doi":"10.1111/jmg.12697","title":"Geothermometric constraints on the thermal architecture, metamorphism, and exhumation of the Northern Range, Trinidad","year":2022,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Tectonic Studies in Latin America","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 Toronto","funders":"University of Toronto; Ministero dell’Istruzione, dell’Università e della Ricerca; Natural Sciences and Engineering Research Council of Canada; European Commission; Università degli Studi di Torino; Universities Space Research Association","keywords":"Metamorphism; Geology; Metamorphic rock; Greenschist; Tectonics; Fault (geology); Shear zone; Seismology; Shear (geology); Metamorphic facies; Transpression; Facies; Paleontology; Structural basin","score_opus":0.018817728166293554,"score_gpt":0.1987451249549993,"score_spread":0.17992739678870573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308020751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970192,0.000045582732,0.00025261618,0.000017436583,7.9256813e-7,0.000004788119,0.00033188326,0.000017834205,0.0023097685],"genre_scores_gemma":[0.998865,0.00003018326,0.00033700853,0.0000074927934,6.929162e-7,0.000010723283,0.00033409332,0.000007438335,0.0004073913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998958,0.000011343096,0.000004714228,0.0000411649,0.000021783366,0.000025067504],"domain_scores_gemma":[0.9997677,0.000035928766,0.000068662965,0.000020937889,0.00008852053,0.000018213545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019956427,0.00024981063,0.00012514989,0.0008377946,0.00041601635,0.00041038272,0.00033022984,0.00016286991,0.0018854244],"category_scores_gemma":[0.00042185106,0.00025577124,0.00012021682,0.00088254665,0.00038933876,0.00021963651,0.00043945466,0.00018837795,0.00020394669],"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":[0.00013119906,0.00003965533,0.91648775,0.00008590109,0.000032648342,0.0002297767,0.0018256255,0.0034025286,0.055840846,0.00028488843,0.0006652216,0.02097385],"study_design_scores_gemma":[0.0000020679515,0.0000102956465,0.9969074,0.000010114938,0.0000048165625,0.00003489309,0.00054068275,0.0012137544,0.0007122109,0.000028547736,0.00053104456,0.0000040527893],"about_ca_topic_score_codex":0.20086206,"about_ca_topic_score_gemma":0.46319675,"teacher_disagreement_score":0.20086206,"about_ca_system_score_codex":0.0013093794,"about_ca_system_score_gemma":0.00044847955,"threshold_uncertainty_score":0.3993858},"labels":[],"label_agreement":null},{"id":"W4315490120","doi":"10.1111/jmg.12709","title":"Pattern and source of unusually high‐temperature metamorphism in an Eocene forearc recorded by the Pacific Rim Terrane, British Columbia, Canada","year":2023,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Society of Economic Geologists Foundation","keywords":"Terrane; Geology; Metamorphism; Forearc; Metamorphic rock; Geochemistry; Shear zone; Accretionary wedge; Paleontology; Petrology; Tectonics; Subduction","score_opus":0.008593400611561107,"score_gpt":0.17521466853199585,"score_spread":0.16662126792043475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315490120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935894,0.00045088414,0.00004849706,0.00010517378,0.000004579825,0.000012840568,0.0018742351,0.000017820359,0.0038965195],"genre_scores_gemma":[0.99724305,0.00029109884,0.00010141167,0.000029342884,0.000002171444,0.0000069301036,0.0010678365,0.000006806792,0.0012514831],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978405,0.00001090731,0.00001288752,0.00004273815,0.000072181276,0.00007718116],"domain_scores_gemma":[0.999132,0.000031444444,0.00011529827,0.000024588344,0.00052314,0.0001736177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001662582,0.00024176238,0.00020990049,0.0023600818,0.0020376027,0.00092832337,0.0006245048,0.00032782706,0.002225711],"category_scores_gemma":[0.00054880657,0.0002392008,0.00013495005,0.003819092,0.0005464585,0.00021158175,0.0005547212,0.00037096755,0.00029351132],"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":[0.00006234743,0.00002345951,0.98301214,0.000043249824,0.00004088653,0.00037315922,0.0017435167,0.00008810973,0.0048431642,0.00013087897,0.0014597179,0.008179409],"study_design_scores_gemma":[6.592301e-7,0.000002361334,0.99844474,0.000010186562,0.0000030481444,0.00004315148,0.0007693588,0.000038848095,0.00006157418,0.0000035428359,0.00062018546,0.000002373954],"about_ca_topic_score_codex":0.98335403,"about_ca_topic_score_gemma":0.99622947,"teacher_disagreement_score":0.016645968,"about_ca_system_score_codex":0.008284187,"about_ca_system_score_gemma":0.0057699354,"threshold_uncertainty_score":0.060106218},"labels":[],"label_agreement":null},{"id":"W4321605221","doi":"10.1111/jmg.12715","title":"Prograde zircon growth in migmatites","year":2023,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Migmatite; Anatexis; Geochemistry; Geology; Solidus; Metamictization; Partial melting; Metamorphism; Metamorphic rock; Crust; Materials science; Gneiss; Metallurgy","score_opus":0.018552508947417765,"score_gpt":0.21132725464610486,"score_spread":0.19277474569868708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321605221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99831057,0.000050646217,0.0005656617,0.0000104551955,0.0000012900468,0.0000042140127,0.00010310812,0.000049030677,0.00090495293],"genre_scores_gemma":[0.9994266,0.000018165152,0.0003165215,0.000002165807,7.742562e-7,0.0000021960673,0.00008197085,0.000006665324,0.00014496525],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99990046,0.000007937606,0.00000893904,0.000040636103,0.000024403424,0.000017608232],"domain_scores_gemma":[0.99991643,0.000016209953,0.00002917163,0.00001177664,0.000018155171,0.000008301697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016675069,0.00023555901,0.00018613666,0.00078338385,0.00031728155,0.0008278863,0.0003307655,0.00038555014,0.00065923],"category_scores_gemma":[0.00041794855,0.00018785079,0.00025701502,0.0002862102,0.0003100584,0.00019036904,0.00042154256,0.00020175685,0.00017819858],"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":[0.0004414748,0.000059458307,0.4023411,0.00016345821,0.00008559555,0.0006561803,0.0004996209,0.041065518,0.53369,0.002666422,0.00015013163,0.018181173],"study_design_scores_gemma":[0.00005250573,0.00030806698,0.7801354,0.000019526662,0.000080225465,0.0005611261,0.0004343272,0.10205671,0.1098414,0.0013359148,0.0051481687,0.000026670139],"about_ca_topic_score_codex":0.008153422,"about_ca_topic_score_gemma":0.0074655428,"teacher_disagreement_score":0.008153422,"about_ca_system_score_codex":0.0010853853,"about_ca_system_score_gemma":0.00020108696,"threshold_uncertainty_score":0.016211927},"labels":[],"label_agreement":null},{"id":"W4323844363","doi":"10.1111/jmg.12719","title":"The temporal evolution of subduction initiation in the Samail ophiolite: High‐precision U–Pb zircon petrochronology of the metamorphic sole","year":2023,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Yukon University","funders":"Office of Inspector General","keywords":"Zircon; Metamorphism; Geology; Geochemistry; Ophiolite; Metamorphic rock; Geochronology; Granulite; Subduction; Petrology; Facies; Tectonics; Geomorphology; Paleontology","score_opus":0.016319422580264635,"score_gpt":0.20983515762452282,"score_spread":0.19351573504425817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323844363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994893,0.000045327568,0.000064225256,0.0000035263943,5.0395596e-7,0.0000023513892,0.000080106816,0.000004898529,0.00030979607],"genre_scores_gemma":[0.999579,0.000029261855,0.000099723555,0.000002151333,0.0000010143635,0.0000023112902,0.000110189234,0.0000021994163,0.00017408509],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999174,0.000005671192,0.0000070435226,0.000028696726,0.000021622787,0.000019580855],"domain_scores_gemma":[0.9998511,0.0000129519385,0.000056516794,0.000008936825,0.000048958576,0.000021487822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017199905,0.0002447048,0.00018079522,0.0011259195,0.00028522382,0.00047252933,0.00020847243,0.00021833282,0.00060950156],"category_scores_gemma":[0.0002515048,0.00018558797,0.00014264742,0.0005238301,0.0002887281,0.00017930559,0.00037773873,0.0001309496,0.00013960173],"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":[0.00025732306,0.000015832671,0.6904483,0.000050626873,0.0000520514,0.00039253378,0.00059565523,0.0004449671,0.30063435,0.00008483396,0.00004602746,0.0069774967],"study_design_scores_gemma":[0.0000023970017,0.000026181062,0.9941293,0.0000024529274,0.0000063031043,0.000097307195,0.0000970539,0.00031789657,0.005038059,0.0000069401494,0.00027401836,0.0000021192052],"about_ca_topic_score_codex":0.017407298,"about_ca_topic_score_gemma":0.029095756,"teacher_disagreement_score":0.017407298,"about_ca_system_score_codex":0.00047090452,"about_ca_system_score_gemma":0.00023662511,"threshold_uncertainty_score":0.03461194},"labels":[],"label_agreement":null},{"id":"W4366122322","doi":"10.1111/jmg.12722","title":"Archean ultrahigh temperature event in the northwestern Superior Province, Canada: Metamorphic evolution and tectonic implications of the Pikwitonei Granulite Domain","year":2023,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Manitoba Hydro; Geological Survey of Canada; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Granulite; Geology; Metamorphism; Metamorphic rock; Geochemistry; Archean; Petrology; Geomorphology; Facies","score_opus":0.008330361976149373,"score_gpt":0.1898446517164941,"score_spread":0.18151428974034473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366122322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980009,0.000095104195,0.000050618146,0.00002176696,0.000001049772,0.000006442406,0.00041329704,0.0000077103605,0.0014031315],"genre_scores_gemma":[0.9988445,0.00007002692,0.00011495706,0.000007204,6.3889036e-7,0.0000021787425,0.0003162141,0.000002626652,0.00064161944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998665,0.0000029844143,0.00000486561,0.000029362029,0.00005390675,0.000042437656],"domain_scores_gemma":[0.9998084,0.0000058084474,0.000028657332,0.000006530246,0.00011079518,0.000039859304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009774392,0.0001506296,0.00016898871,0.0010996866,0.0014103766,0.00069637067,0.00030188754,0.00018968992,0.0012806649],"category_scores_gemma":[0.0001946386,0.00014184255,0.00017288911,0.0014210924,0.0006038397,0.00014890038,0.0004834226,0.0001775715,0.0001384801],"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":[0.00011570574,0.000025034771,0.96385807,0.000049112135,0.00003802591,0.0006752459,0.0012277416,0.00057843386,0.022123534,0.00027244337,0.00029777526,0.010738859],"study_design_scores_gemma":[0.000002111047,0.0000068437266,0.9982816,0.0000051381116,0.0000042972024,0.000066628236,0.00050250883,0.00023660426,0.00030414795,0.00001322651,0.00057430414,0.0000025033994],"about_ca_topic_score_codex":0.9564027,"about_ca_topic_score_gemma":0.98284423,"teacher_disagreement_score":0.04359728,"about_ca_system_score_codex":0.0065748277,"about_ca_system_score_gemma":0.005769665,"threshold_uncertainty_score":0.087708},"labels":[],"label_agreement":null},{"id":"W4385265670","doi":"10.1111/jmg.12739","title":"<sup>40</sup>Ar/<sup>39</sup>Ar dates controlled by white mica deformation and strain localization: Insights from comparing in situ laser ablation and single‐grain fusion techniques","year":2023,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Manitoba; University of Winnipeg; University of Ottawa","funders":"","keywords":"Geology; Metamorphism; Nappe; Deformation (meteorology); Devonian; Metamorphic rock; Mica; Shear zone; Shear (geology); Geochemistry; Mineralogy; Petrology; Paleontology; Tectonics","score_opus":0.013519613943719255,"score_gpt":0.19803883561592417,"score_spread":0.18451922167220491,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385265670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99349546,0.00025926874,0.0011389652,0.000018527147,0.0000094527295,0.000012346508,0.00081708166,0.00006635953,0.0041825166],"genre_scores_gemma":[0.9977591,0.000075924974,0.0009804314,0.0000072314365,0.000006422695,0.000008819322,0.0004914791,0.000041644533,0.0006289847],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995919,0.00002972123,0.000024730636,0.00013491651,0.00016176414,0.000056902245],"domain_scores_gemma":[0.99953496,0.00010054144,0.0001415963,0.00005453232,0.00015066208,0.000017819219],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004605396,0.00034580645,0.00026432984,0.00083372195,0.00027250824,0.00078574836,0.000423317,0.0005103078,0.0015511342],"category_scores_gemma":[0.0005249918,0.0002423206,0.00028145843,0.00065267005,0.00041933116,0.000292704,0.00024033012,0.00027799117,0.0005608682],"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":[0.00060010166,0.00002005823,0.04218197,0.00008301989,0.00007190524,0.00024100393,0.00036103232,0.0005803062,0.949402,0.00015771139,0.00014884028,0.0061522643],"study_design_scores_gemma":[0.000017891896,0.00018811812,0.7377345,0.000012518318,0.00008897722,0.00050079747,0.0004213771,0.0017851709,0.25590214,0.000072005525,0.0032512364,0.000025216415],"about_ca_topic_score_codex":0.005592849,"about_ca_topic_score_gemma":0.013466571,"teacher_disagreement_score":0.005592849,"about_ca_system_score_codex":0.00037356318,"about_ca_system_score_gemma":0.00015652482,"threshold_uncertainty_score":0.011120617},"labels":[],"label_agreement":null},{"id":"W4386802130","doi":"10.1111/jmg.12745","title":"Polymetamorphism during the Grenvillian Orogeny in SE Ontario: Results from trace element mapping, in situ geochronology, and diffusion geospeedometry","year":2023,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Ministry of Energy, Northern Development and Mines; St. Francis Xavier University; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Biotite; Geology; Geochemistry; Apatite; Orogeny; Geochronology; Population; Mineralogy; Quartz; Paleontology; Tectonics","score_opus":0.017981190614866346,"score_gpt":0.20462396244710296,"score_spread":0.1866427718322366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386802130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978027,0.000078878635,0.00007350994,0.000020874484,7.2806176e-7,0.000010789254,0.00035307492,0.0000049926343,0.0016545851],"genre_scores_gemma":[0.99825686,0.00007029966,0.0001475626,0.00001182358,7.284411e-7,0.0000056973604,0.00035855474,0.000005574188,0.0011429215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997992,0.000011468672,0.000007700671,0.000054611384,0.00005304689,0.00007392451],"domain_scores_gemma":[0.9997962,0.000013518037,0.000051290164,0.000009997344,0.00010286908,0.000026210448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012211368,0.00021875373,0.00020347936,0.0009703674,0.0010828514,0.000624617,0.0004319192,0.00026094564,0.00083556946],"category_scores_gemma":[0.00038776544,0.00017631339,0.00013135956,0.0012747032,0.0006579828,0.00015611389,0.00037971273,0.0001495746,0.00019585407],"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":[0.00023199529,0.000029249013,0.9370099,0.000059884882,0.000045530356,0.00066831533,0.005794561,0.00027188362,0.044077616,0.0001816917,0.0002805056,0.01134888],"study_design_scores_gemma":[0.0000024342983,0.000011584519,0.99755585,0.0000058757555,0.000007150443,0.000036971953,0.0008722852,0.000098918776,0.0004974285,0.000007718616,0.0009008757,0.0000028054162],"about_ca_topic_score_codex":0.95236015,"about_ca_topic_score_gemma":0.98879695,"teacher_disagreement_score":0.047639847,"about_ca_system_score_codex":0.006911489,"about_ca_system_score_gemma":0.0036042882,"threshold_uncertainty_score":0.09584075},"labels":[],"label_agreement":null},{"id":"W4389612063","doi":"10.1111/jmg.12751","title":"Redistribution of heat‐producing elements during melting of Archean crust","year":2023,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"McGill University; Geological Survey of Canada; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Anatexis; Archean; Geology; Geochemistry; Granulite; Continental crust; Partial melting; Mafic; Allanite; Craton; Epidote; Metamorphic facies; Petrology; Crust; Zircon; Tectonics; Facies; Monazite; Geomorphology","score_opus":0.02288202074157785,"score_gpt":0.2274889331695543,"score_spread":0.20460691242797643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389612063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966876,0.00007638887,0.0006283607,0.000035896282,0.0000027607714,0.0000064317815,0.00031059884,0.000044081702,0.0022079034],"genre_scores_gemma":[0.99904007,0.0000443257,0.00028242127,0.000007614612,0.0000012694143,0.000006326971,0.0001587213,0.000017430784,0.00044178186],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998982,0.000013690824,0.00000744265,0.00003657466,0.00001604898,0.000028010583],"domain_scores_gemma":[0.99988115,0.00002652414,0.000025073401,0.00002294965,0.00002335966,0.000021020154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021971443,0.00061008916,0.00036251664,0.00075536134,0.00052777916,0.0011509751,0.0008876646,0.00073020475,0.002430307],"category_scores_gemma":[0.000565914,0.00043314774,0.0008197719,0.00062164693,0.0007434623,0.00057296583,0.0008315722,0.00039270194,0.00025859106],"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":[0.00032048524,0.00006863689,0.095854826,0.00007400787,0.00017022985,0.00027369583,0.00020497502,0.86465245,0.031988736,0.0017809229,0.00013777327,0.0044733724],"study_design_scores_gemma":[0.000120947756,0.00021280399,0.13098383,0.000037631627,0.00009223649,0.00013800447,0.00037629975,0.8540552,0.01076891,0.0015543578,0.0015961747,0.00006355697],"about_ca_topic_score_codex":0.0447002,"about_ca_topic_score_gemma":0.018529812,"teacher_disagreement_score":0.0447002,"about_ca_system_score_codex":0.0021421777,"about_ca_system_score_gemma":0.0006124883,"threshold_uncertainty_score":0.08888006},"labels":[],"label_agreement":null},{"id":"W4391110383","doi":"10.1111/jmg.12755","title":"Eclogite with biotite porphyroblasts—Which conditions are responsible for their formation? An example from the northern Fleur‐de‐Lys Supergroup, Newfoundland, Canada","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"","funders":"Universität Stuttgart; Ruhr-Universität Bochum; University of Waterloo; Deutsche Forschungsgemeinschaft","keywords":"Geology; Eclogite; Phengite; Omphacite; Biotite; Geochemistry; Lawsonite; Geothermobarometry; Coesite; Blueschist; Metamorphic facies; Amphibole; Petrology; Subduction; Metamorphism; Facies; Paleontology; Quartz","score_opus":0.023213466487971905,"score_gpt":0.20478058123450066,"score_spread":0.18156711474652876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391110383","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940268,0.00030549252,0.00017452748,0.00006908705,0.0000023024932,0.000017058124,0.0002877941,0.000013543672,0.005103494],"genre_scores_gemma":[0.99662364,0.0001481465,0.0003117805,0.000030587333,0.0000013309827,0.0000041162953,0.00022736874,0.0000074667955,0.0026455612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997632,0.000007357907,0.000007232106,0.00005966522,0.0000473246,0.00011520235],"domain_scores_gemma":[0.99973744,0.000015886653,0.000052825733,0.000012230354,0.00012606253,0.00005548743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010176793,0.00024833047,0.00020761191,0.001259786,0.0018081409,0.00095618406,0.00039953407,0.0002876848,0.0017947492],"category_scores_gemma":[0.00020572965,0.00021559885,0.00015308944,0.0010230737,0.0007726748,0.00021906513,0.00053977204,0.0002564459,0.00024700174],"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":[0.00029468187,0.00004233686,0.8736152,0.00008895407,0.000053811746,0.003690407,0.003399425,0.00029713818,0.10349531,0.0005575463,0.00060129235,0.0138637535],"study_design_scores_gemma":[0.0000052470987,0.000023723278,0.98882467,0.000013590432,0.00001907281,0.00078369817,0.0021776508,0.00021767493,0.0032025925,0.00003002343,0.0046935575,0.000008612577],"about_ca_topic_score_codex":0.8759007,"about_ca_topic_score_gemma":0.95256937,"teacher_disagreement_score":0.124099314,"about_ca_system_score_codex":0.006917046,"about_ca_system_score_gemma":0.0026921558,"threshold_uncertainty_score":0.24966025},"labels":[],"label_agreement":null},{"id":"W4391217925","doi":"10.1111/jmg.12759","title":"Paleoarchean metamorphism in the Acasta Gneiss Complex: Constraints from phase equilibrium modelling and in situ garnet Lu–Hf geochronology","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Australian Research Council; Curtin University of Technology","keywords":"Metamorphism; Geochronology; Geology; Metamorphic rock; Gneiss; Geochemistry; Geothermobarometry; Orogeny; Archean; Petrology; Paleontology; Tectonics","score_opus":0.05390858754167688,"score_gpt":0.2620050390712484,"score_spread":0.2080964515295715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391217925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964714,0.000042590447,0.002031707,0.000022621925,0.0000015949568,0.0000064626256,0.00016222366,0.00008160168,0.001179916],"genre_scores_gemma":[0.9983884,0.00002444393,0.0012710763,0.0000044506032,9.641246e-7,0.0000042349047,0.0001540254,0.000027599775,0.00012482377],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99984956,0.000028673523,0.000011361799,0.00005351267,0.000033393928,0.000023590314],"domain_scores_gemma":[0.99981123,0.00006546174,0.0000355305,0.00002662208,0.000045539775,0.000015698506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000382689,0.0006410613,0.00047045024,0.0008805781,0.00047710357,0.0011130187,0.0007360637,0.00063134904,0.001063211],"category_scores_gemma":[0.00086339883,0.00040432785,0.00050037046,0.0006619586,0.0005969748,0.00032693785,0.00034971605,0.00027833067,0.00021611874],"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":[0.00034601733,0.00017950553,0.38067564,0.00015845461,0.00041021057,0.0005156156,0.00079890894,0.5195099,0.07920639,0.0021088552,0.00028992046,0.015800565],"study_design_scores_gemma":[0.000052712534,0.00006924625,0.19360803,0.000019504496,0.00008066345,0.00011094008,0.00023488366,0.7982383,0.0060018986,0.00050271204,0.0010469926,0.000034049615],"about_ca_topic_score_codex":0.2000363,"about_ca_topic_score_gemma":0.27850124,"teacher_disagreement_score":0.2000363,"about_ca_system_score_codex":0.00228654,"about_ca_system_score_gemma":0.0013286322,"threshold_uncertainty_score":0.39774388},"labels":[],"label_agreement":null},{"id":"W4391224402","doi":"10.1111/jmg.12758","title":"Influence of high‐strain deformation on major element mobility in garnet: Nanoscale evidence from atom probe tomography","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Advanced Materials Characterization Techniques","field":"Engineering","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 Winnipeg; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Leibniz-Gemeinschaft; Deutsche Forschungsgemeinschaft","keywords":"Atom probe; Deformation (meteorology); Strain (injury); Nanoscopic scale; Geology; Tomography; Materials science; Composite material; Nanotechnology; Medicine; Microstructure; Radiology; Oceanography; Anatomy","score_opus":0.009824461504015067,"score_gpt":0.2369946065750928,"score_spread":0.22717014507107774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391224402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983511,0.000054659744,0.0009912129,0.000019817093,0.0000013783208,0.0000035691883,0.00008375995,0.000022861952,0.00047162737],"genre_scores_gemma":[0.9992482,0.000039002505,0.000487071,0.000007664777,0.0000011518616,0.0000028561888,0.00005450436,0.0000049083446,0.00015458246],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999329,0.0000054373663,0.0000025331092,0.00002029972,0.000024939762,0.000013925486],"domain_scores_gemma":[0.999861,0.000035922112,0.00004170815,0.00001337031,0.00003445633,0.000013543212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010630989,0.00015528547,0.00014875109,0.00041351098,0.00020578067,0.00034336955,0.0002947418,0.00029579012,0.0009834269],"category_scores_gemma":[0.0002839548,0.00017884574,0.00010482649,0.00021732175,0.0006518752,0.00033256656,0.00034236477,0.00018775213,0.00012588681],"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":[0.000094477546,0.000015887626,0.013563351,0.00003072788,0.000009018339,0.00020874363,0.00012581801,0.0007811476,0.9832661,0.00015554775,0.00003716705,0.0017120218],"study_design_scores_gemma":[0.000017311815,0.00021099504,0.43753234,0.000018555926,0.00003698573,0.00082553003,0.0006278071,0.033197194,0.52568436,0.00035172334,0.0014660723,0.000031214866],"about_ca_topic_score_codex":0.0036070582,"about_ca_topic_score_gemma":0.003384412,"teacher_disagreement_score":0.0036070582,"about_ca_system_score_codex":0.0003105575,"about_ca_system_score_gemma":0.00011857306,"threshold_uncertainty_score":0.0071721673},"labels":[],"label_agreement":null},{"id":"W4391440941","doi":"10.1111/jmg.12761","title":"Formation of multistage garnet grains by fragmentation and overgrowth constrained by microchemical and microstructural mapping","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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; Natural Resources Canada","funders":"Natural Resources Canada; Stockholms Universitet; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Metamorphic rock; Metamorphism; Electron backscatter diffraction; Nucleation; Geochemistry; Mineralogy; Fragmentation (computing); Microstructure; Materials science; Composite material; Chemistry","score_opus":0.007089354508166037,"score_gpt":0.19454475947809954,"score_spread":0.18745540496993351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391440941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99796665,0.000050967054,0.001494906,0.0000065027193,7.6209625e-7,0.0000041927133,0.000051919134,0.00003790965,0.00038627206],"genre_scores_gemma":[0.9987696,0.000022009921,0.0010064939,0.0000020377204,8.747277e-7,0.000002464389,0.000058156893,0.0000076022625,0.00013070759],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999269,0.0000031189343,0.0000026842313,0.000029182065,0.00002025346,0.000017770244],"domain_scores_gemma":[0.9999044,0.0000178381,0.000034824065,0.00001175888,0.000021199457,0.000009918139],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008228181,0.00015214078,0.00012825536,0.0004559261,0.00017731753,0.00034552717,0.00019945679,0.0001730593,0.00084210414],"category_scores_gemma":[0.00017030576,0.00018971796,0.00015475186,0.00023995485,0.00029301865,0.00020314787,0.00019312385,0.00010885798,0.00010564092],"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":[0.00011427628,0.000015445697,0.056161333,0.000039872324,0.000023704657,0.00036035868,0.00020030382,0.004276218,0.931313,0.00027369935,0.00005938863,0.007162325],"study_design_scores_gemma":[0.00001036859,0.00010038475,0.6579478,0.000009669917,0.000038079957,0.0008879939,0.00032445093,0.09457439,0.24398436,0.00038468637,0.0017154672,0.000022329934],"about_ca_topic_score_codex":0.0032452478,"about_ca_topic_score_gemma":0.0056653293,"teacher_disagreement_score":0.0032452478,"about_ca_system_score_codex":0.00032471248,"about_ca_system_score_gemma":0.00012181049,"threshold_uncertainty_score":0.0064526796},"labels":[],"label_agreement":null},{"id":"W4392726361","doi":"10.1111/jmg.12766","title":"Mechanisms and durations of metamorphic garnet crystallization in the lower nappes of the Caledonian Kalak Nappe Complex, Arctic Norway","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Nappe; Metamorphic rock; Geology; Geochemistry; Orogeny; Mineralogy; Geomorphology; Tectonics; Seismology; Structural basin","score_opus":0.01649140189974939,"score_gpt":0.207838922362068,"score_spread":0.19134752046231862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392726361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985154,0.00036455615,0.00011276138,0.0000077393515,0.0000014226003,0.0000033477168,0.00026256466,0.00000973727,0.0007223559],"genre_scores_gemma":[0.99930334,0.00009764736,0.00006118483,0.0000025479264,6.140326e-7,0.0000038304242,0.0002287347,0.0000038114758,0.00029832512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998641,0.0000073057167,0.000009116919,0.00006325445,0.000019334911,0.00003693042],"domain_scores_gemma":[0.9998398,0.000027120497,0.000061655686,0.000006928497,0.000039573755,0.000024918827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023731627,0.00028607514,0.00022676188,0.0017368781,0.000500634,0.0008037431,0.0003723325,0.0002710732,0.0015399049],"category_scores_gemma":[0.00036918657,0.0002353453,0.00019333554,0.0004970872,0.00066532206,0.00026082102,0.0005524218,0.0001318579,0.00020728812],"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":[0.00082736014,0.000030393212,0.7824484,0.00026453024,0.00012050706,0.00093079224,0.003182837,0.0026450038,0.19325964,0.0007193003,0.00016932002,0.015401974],"study_design_scores_gemma":[0.0000022541544,0.000016456705,0.9972549,0.000009479852,0.000010389422,0.000057943562,0.00043862135,0.0004144855,0.0013184694,0.00003532149,0.00043631258,0.000005269865],"about_ca_topic_score_codex":0.13269962,"about_ca_topic_score_gemma":0.21748187,"teacher_disagreement_score":0.13269962,"about_ca_system_score_codex":0.0017498069,"about_ca_system_score_gemma":0.00049024995,"threshold_uncertainty_score":0.26385444},"labels":[],"label_agreement":null},{"id":"W4395484623","doi":"10.1111/jmg.12769","title":"Retentiveness of rare earth elements in garnet with implications for garnet Lu‐Hf chronology","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Université Laval; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Vetenskapsrådet; Deutsche Forschungsgemeinschaft; European Commission","keywords":"Geology; Metamorphic rock; Mineralogy; Geochemistry; Chronology; Diffusion; Thermodynamics","score_opus":0.021257455967616586,"score_gpt":0.2351498721130515,"score_spread":0.21389241614543492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395484623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99685466,0.000563543,0.0009341377,0.000021470794,0.000009959967,0.000004890115,0.00033917752,0.000047643265,0.0012244452],"genre_scores_gemma":[0.9989359,0.00011841112,0.00044207313,0.000008687396,0.0000030587082,0.000003136985,0.00015151109,0.000019902474,0.00031725984],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998753,0.000015262634,0.000014198267,0.00004920682,0.00002070684,0.000025292811],"domain_scores_gemma":[0.9997341,0.000055094413,0.000075222015,0.00003000469,0.00008944003,0.000016185202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029575516,0.00024401446,0.00026030108,0.0015450786,0.00026756953,0.0006672347,0.00018954709,0.00022717199,0.0011595676],"category_scores_gemma":[0.0004357857,0.00012377286,0.00014141217,0.00066057494,0.00037577088,0.0003650791,0.00026803015,0.00011519132,0.00016811473],"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":[0.00054198893,0.000015192556,0.31769595,0.00014935515,0.00008030572,0.0002729824,0.00059294107,0.0009013078,0.6587538,0.0005053586,0.000086242755,0.02040448],"study_design_scores_gemma":[0.0000041352478,0.00006976302,0.937096,0.000016912736,0.00004007292,0.00024544756,0.00029019482,0.0012417278,0.058687374,0.0001713662,0.0021259987,0.000010956381],"about_ca_topic_score_codex":0.0048750634,"about_ca_topic_score_gemma":0.010501358,"teacher_disagreement_score":0.0048750634,"about_ca_system_score_codex":0.00037953738,"about_ca_system_score_gemma":0.00012849407,"threshold_uncertainty_score":0.009693384},"labels":[],"label_agreement":null},{"id":"W4400594395","doi":"10.1111/jmg.12790","title":"Isochemical metamorphism origin of the newly discovered Baqing jadeitoid, eastern‐central Tibet, China","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 British Columbia","funders":"Fundamental Research Funds for the Central Universities; China Scholarship Council; China Postdoctoral Science Foundation; Postdoctoral Innovation Project of Shandong Province; National Natural Science Foundation of China; College of Science and Engineering, Central Michigan University","keywords":"Geology; Omphacite; Phengite; Eclogite; Geochemistry; Metamorphic rock; Metamorphism; Subduction; Protolith; Almandine; Petrology; Paleontology; Tectonics","score_opus":0.013417246119363319,"score_gpt":0.21051390175671264,"score_spread":0.19709665563734932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400594395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99802494,0.00029048845,0.00020321255,0.000026219115,0.0000055391192,0.0000113177175,0.0001961012,0.00001003334,0.0012321923],"genre_scores_gemma":[0.99854386,0.00012057263,0.0002736958,0.00001421112,0.0000039217193,0.000004337893,0.00032504168,0.0000035458513,0.000710735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998914,0.0000061627097,0.000013484198,0.00003516686,0.00003227317,0.000021483871],"domain_scores_gemma":[0.99981695,0.000010192266,0.000047175017,0.000009455063,0.000078385936,0.00003781062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024053482,0.00040346655,0.00025902584,0.0030012624,0.00082109164,0.00044939856,0.00030596467,0.00022737459,0.0009768598],"category_scores_gemma":[0.0002167839,0.00023884165,0.00018120494,0.0021179253,0.00053420535,0.00025083713,0.00039254423,0.00018539713,0.00010011822],"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":[0.00012965735,0.000032194617,0.8913108,0.00024054371,0.000112904556,0.0014003335,0.001620146,0.0004514895,0.083518356,0.00035731037,0.0002135168,0.020612774],"study_design_scores_gemma":[0.0000051651364,0.00002205981,0.9971023,0.0000076090455,0.000018194321,0.0003340914,0.00036207392,0.00028214406,0.00089060667,0.000031548483,0.00093920523,0.0000049786827],"about_ca_topic_score_codex":0.04014155,"about_ca_topic_score_gemma":0.09385208,"teacher_disagreement_score":0.04014155,"about_ca_system_score_codex":0.0007437418,"about_ca_system_score_gemma":0.00050519453,"threshold_uncertainty_score":0.079815805},"labels":[],"label_agreement":null},{"id":"W4405694812","doi":"10.1111/jmg.12804","title":"Cold Deep Over Hot Shallow Crust: A Peculiar Metamorphic Architecture in the Neoarchean Metasedimentary Pontiac Subprovince, Superior Craton (Canada)","year":2024,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Laurentian University; Geological Survey of Canada; Natural Resources Canada; Université Laval","funders":"Canada First Research Excellence Fund","keywords":"Geology; Craton; Crust; Geochemistry; Metamorphic rock; Petrology; Earth science; Paleontology; Tectonics","score_opus":0.00820857843732285,"score_gpt":0.1927771346130458,"score_spread":0.18456855617572296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405694812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973241,0.00025540864,0.00010817459,0.00002384091,0.0000013795053,0.000009360556,0.00044320093,0.000008626704,0.0018257448],"genre_scores_gemma":[0.9985292,0.00014633652,0.00012281156,0.00000787712,6.927996e-7,0.0000023029252,0.00024919043,0.0000043157374,0.0009372783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998877,0.0000025682502,0.0000036891922,0.000029682204,0.000032045184,0.000044308596],"domain_scores_gemma":[0.9998629,0.0000067536994,0.000022528011,0.0000063180787,0.0000746892,0.000026728649],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008887992,0.0002013404,0.00019921806,0.0023101773,0.0011464887,0.00084728794,0.00030683342,0.00019220937,0.0019508721],"category_scores_gemma":[0.00023699221,0.00020483203,0.00012688081,0.002691672,0.0010488204,0.00018136224,0.0005084516,0.0001691946,0.00022050983],"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":[0.00019256426,0.000021589416,0.92803115,0.00011794253,0.00007763919,0.0015294342,0.0051127356,0.00046802248,0.034545384,0.00061959156,0.00042562064,0.028858313],"study_design_scores_gemma":[9.187946e-7,0.000005863818,0.99767154,0.000007500124,0.000006487914,0.00019685006,0.001013609,0.000115354494,0.00027679547,0.00002572741,0.00067647087,0.000002799701],"about_ca_topic_score_codex":0.8884272,"about_ca_topic_score_gemma":0.9638801,"teacher_disagreement_score":0.1115728,"about_ca_system_score_codex":0.004624289,"about_ca_system_score_gemma":0.003701871,"threshold_uncertainty_score":0.22445971},"labels":[],"label_agreement":null},{"id":"W4407577646","doi":"10.1111/jmg.12808","title":"Polyphase Metamorphism of the Northern Rae Craton (Baffin Island, Arctic Canada) and Trace Element Behaviour in Monazite: Insights From Phase Equilibria Modelling and Geochronology","year":2025,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Université du Québec à Montréal; Government of Newfoundland and Labrador; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Monazite; Geochronology; Geology; Metamorphism; Polyphase system; Trace element; Arctic; Geochemistry; Craton; Kyanite; Oceanography; Paleontology; Zircon; Tectonics","score_opus":0.009447875192226967,"score_gpt":0.20195849839983487,"score_spread":0.1925106232076079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407577646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99720085,0.00014002001,0.0002779931,0.00003866041,0.0000013361579,0.000006519659,0.0004244872,0.00003085191,0.0018794194],"genre_scores_gemma":[0.9988398,0.00006240447,0.0002412058,0.000004316952,3.956476e-7,0.0000024378546,0.00024368067,0.000006645287,0.0005991646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999931,0.0000043093746,0.000002795587,0.000023085227,0.00001994321,0.000018994135],"domain_scores_gemma":[0.99988806,0.000010601824,0.000014148963,0.0000062418294,0.00006388647,0.00001700872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014070937,0.0002258072,0.00016977475,0.001121074,0.0008035911,0.00083314814,0.0003759787,0.0002935021,0.0016350681],"category_scores_gemma":[0.0003481579,0.00026642223,0.00018248663,0.0007513264,0.00043441448,0.00025942473,0.00023134692,0.00017386365,0.00016953793],"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":[0.00028952138,0.000059848808,0.9067023,0.000090138776,0.00013287718,0.0002862859,0.0011068349,0.026689667,0.035622314,0.0010872463,0.000759391,0.027173523],"study_design_scores_gemma":[0.000013472645,0.000015015295,0.97509116,0.000012974791,0.00002217403,0.000056411875,0.0004918157,0.020611014,0.0019368436,0.000096486016,0.0016401901,0.000012517926],"about_ca_topic_score_codex":0.94828147,"about_ca_topic_score_gemma":0.97383547,"teacher_disagreement_score":0.051718533,"about_ca_system_score_codex":0.005939954,"about_ca_system_score_gemma":0.0032401786,"threshold_uncertainty_score":0.104046166},"labels":[],"label_agreement":null},{"id":"W4408677617","doi":"10.1111/jmg.12814","title":"Phase Equilibria Analysis for Metacarbonate With Applications to Zoned Calc‐Silicate Aureoles","year":2025,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Silicate; Geology; Geochemistry; Phase (matter); Petrology; Mineralogy; Chemistry","score_opus":0.02084674023988959,"score_gpt":0.2716500399698179,"score_spread":0.2508032997299283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408677617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96876615,0.00006985463,0.029149447,0.000012907828,0.0000035695216,0.000043342094,0.00075342524,0.00040756632,0.0007937424],"genre_scores_gemma":[0.9648354,0.000040862502,0.034179054,0.0000029737812,0.0000025042536,0.000031026928,0.0006453811,0.000040782532,0.00022196195],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999573,0.000006306118,0.0000028518173,0.000014281297,0.000011751642,0.0000074719646],"domain_scores_gemma":[0.99988174,0.00003755475,0.000021283347,0.000015680012,0.000031582647,0.0000121318935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011568071,0.00027863518,0.00023155702,0.0011302705,0.00019337646,0.0002789055,0.0003171781,0.00020571121,0.0009961027],"category_scores_gemma":[0.0003281907,0.00012708569,0.00030049344,0.0006416863,0.00014497059,0.00014661795,0.00028752026,0.00014012933,0.00011234042],"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":[0.00044466884,0.00022356676,0.09453675,0.00025919435,0.000097903205,0.00046154932,0.00028814853,0.4331047,0.4116954,0.0045258612,0.00046357565,0.053898763],"study_design_scores_gemma":[0.00002123609,0.000046452944,0.021569643,0.0000040651566,0.000010297886,0.000041193824,0.00008278329,0.9337744,0.042310968,0.0008135763,0.0013123577,0.000013069047],"about_ca_topic_score_codex":0.010823803,"about_ca_topic_score_gemma":0.008173362,"teacher_disagreement_score":0.010823803,"about_ca_system_score_codex":0.0003501227,"about_ca_system_score_gemma":0.00032160146,"threshold_uncertainty_score":0.021521628},"labels":[],"label_agreement":null},{"id":"W4409407463","doi":"10.1111/jmg.12817","title":"Exhumation Mechanisms of High‐Pressure Rocks With High‐Temperature Overprinting: Insights From Eclogites of the Baie Verte Peninsula, Newfoundland","year":2025,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"Memorial University of Newfoundland; Government of Newfoundland and Labrador; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Overprinting; Eclogite; Geology; Peninsula; Geochemistry; High pressure; Kola peninsula; Metamorphic rock; Seismology; Subduction; Tectonics; Archaeology; Geography","score_opus":0.005275335096043809,"score_gpt":0.17164881159663198,"score_spread":0.16637347650058817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409407463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986659,0.00016403556,0.00019431872,0.00002499044,8.067805e-7,0.0000027968658,0.00019087564,0.000014302708,0.00074191607],"genre_scores_gemma":[0.99944395,0.00007711437,0.00013560957,0.000009478833,7.6009593e-7,0.0000013981304,0.00010391163,0.0000038227954,0.000224021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992275,0.000003995797,0.000004378571,0.000026835049,0.000015077163,0.000026936636],"domain_scores_gemma":[0.999877,0.000013022476,0.00004485444,0.000010376722,0.000036283935,0.000018514744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014138223,0.00025148827,0.00019335249,0.0011022981,0.0006405126,0.000745922,0.00027127692,0.00022078017,0.0010891425],"category_scores_gemma":[0.00023444029,0.0002205624,0.00014556968,0.0007872769,0.00070392183,0.00037234332,0.0005372111,0.00021909186,0.00011778615],"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":[0.00008331796,0.000018708883,0.9373027,0.00006619402,0.00006899606,0.0005985561,0.0011417213,0.0014558105,0.04922397,0.00016462727,0.00014909217,0.0097262515],"study_design_scores_gemma":[9.894945e-7,0.000005142233,0.9984137,0.0000042907354,0.0000068702816,0.00008246512,0.00028860834,0.0004753018,0.00047358425,0.000015230616,0.00023103402,0.0000027760486],"about_ca_topic_score_codex":0.33591565,"about_ca_topic_score_gemma":0.59288764,"teacher_disagreement_score":0.6640843,"about_ca_system_score_codex":0.0016476985,"about_ca_system_score_gemma":0.00081483007,"threshold_uncertainty_score":0.6679208},"labels":[],"label_agreement":null},{"id":"W4409955890","doi":"10.1111/jmg.12820","title":"The Distribution of Major and Trace Elements Across a Garnet Population From the Kalak Nappe Complex (Finnmark, Scandinavian Caledonides): Evidence for Size‐Dependent Growth and Compositional Equilibration in the Garnet Zone","year":2025,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Nappe; Geochemistry; Petrology; Paleontology; Tectonics","score_opus":0.027614102893569335,"score_gpt":0.2753002040295411,"score_spread":0.24768610113597175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409955890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994702,0.000075145814,0.000034460543,0.0000031658722,4.9998357e-7,0.0000026869486,0.00018376073,0.0000014177032,0.0002286237],"genre_scores_gemma":[0.9992569,0.000061288796,0.00008373471,0.000004274677,8.21575e-7,0.0000045168363,0.0003842263,0.0000018681698,0.00020242562],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997707,0.000013255491,0.000019052151,0.00009656676,0.00004654715,0.00005386623],"domain_scores_gemma":[0.99981886,0.000031753316,0.000053551816,0.0000108534405,0.00005679561,0.00002824656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019500381,0.00034251672,0.00034925007,0.0029800436,0.0005779793,0.0007285095,0.0005372938,0.0003303114,0.0010218876],"category_scores_gemma":[0.00022820948,0.00023423473,0.00025007277,0.0009901404,0.0009960486,0.0002789805,0.00063391577,0.00011780456,0.00024086829],"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":[0.00019546814,0.000025240284,0.9479098,0.00007754585,0.00009332171,0.00075009384,0.0028670754,0.00027091955,0.042281732,0.00008874994,0.000057895664,0.0053823045],"study_design_scores_gemma":[0.000001067286,0.000021242173,0.9985662,0.0000049562386,0.00001013836,0.00014940527,0.0007169965,0.00007607144,0.00029985438,0.000006487727,0.00014474256,0.0000029177295],"about_ca_topic_score_codex":0.100483894,"about_ca_topic_score_gemma":0.17923461,"teacher_disagreement_score":0.100483894,"about_ca_system_score_codex":0.0010362165,"about_ca_system_score_gemma":0.00050154416,"threshold_uncertainty_score":0.19979805},"labels":[],"label_agreement":null},{"id":"W4412779116","doi":"10.1111/jmg.70004","title":"Calibration, Validation and Evaluation of Machine Learning Thermobarometers in Metamorphic Petrology: An Application to Biotite and Outlook for Future Strategy","year":2025,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 British Columbia","funders":"European Research Council","keywords":"Biotite; Geology; Metamorphic rock; Geochemistry; Calibration; Petrology; Paleontology; Statistics","score_opus":0.018343979336549424,"score_gpt":0.25653122207408996,"score_spread":0.23818724273754055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412779116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6109947,0.006750715,0.3624497,0.0027442733,0.0005773394,0.0006147287,0.0018490115,0.005328704,0.008690853],"genre_scores_gemma":[0.82848936,0.0011046965,0.16436581,0.00022823783,0.00007750996,0.00031970482,0.0024225388,0.00032986893,0.0026622487],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99559,0.0017854454,0.00022901392,0.00077570265,0.0014655297,0.00015437123],"domain_scores_gemma":[0.9898679,0.0025292195,0.0006576971,0.0012718515,0.0053640855,0.00030916603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.01650789,0.0013752136,0.00095077883,0.001245918,0.00072085555,0.0020050434,0.002688654,0.0018746002,0.001004159],"category_scores_gemma":[0.016541211,0.00036990474,0.00078208605,0.0013516614,0.0010025908,0.0014001769,0.0014012727,0.0013172526,0.0007313455],"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":[0.00080850115,0.0015396766,0.08423256,0.0008378971,0.00047234513,0.00022050884,0.00036748475,0.52262837,0.06540096,0.004474704,0.0082135,0.31080353],"study_design_scores_gemma":[0.000055775978,0.00056343776,0.017398413,0.00024642254,0.00007604509,0.00008436479,0.00021772277,0.92263436,0.04827139,0.0019961225,0.008383784,0.00007214927],"about_ca_topic_score_codex":0.018142307,"about_ca_topic_score_gemma":0.015342216,"teacher_disagreement_score":0.018142307,"about_ca_system_score_codex":0.0018465713,"about_ca_system_score_gemma":0.0019055823,"threshold_uncertainty_score":0.0873031},"labels":[],"label_agreement":null},{"id":"W4413024340","doi":"10.1111/jmg.70005","title":"Thermodynamic and Kinetic Controls on the Growth of Metapelitic Garnet in the Danba Dome (SW China): Insights From Microstructure, Element Mapping and Thermodynamic Modelling","year":2025,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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":"Fundamental Research Funds for the Central Universities; China Scholarship Council; National Natural Science Foundation of China","keywords":"Geology; China; Rare-earth element; Microstructure; Geochemistry; Dome (geology); Seismology; Mineralogy; Paleontology; Archaeology; Metallurgy; Rare earth; Materials science; Geography","score_opus":0.00920172969947175,"score_gpt":0.18574355347385274,"score_spread":0.176541823774381,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413024340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993186,0.00003144906,0.00017688249,0.000009739611,4.5225784e-7,0.000003221962,0.00007131856,0.0000068462773,0.00038160844],"genre_scores_gemma":[0.9997564,0.00002003905,0.000085498024,0.0000011139214,3.2385537e-7,0.0000023829057,0.000045216224,0.0000030237045,0.00008591463],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999443,0.000007981176,0.0000044711633,0.000019508427,0.000011992504,0.000011667782],"domain_scores_gemma":[0.9999547,0.000014063363,0.00000789471,0.0000051075476,0.000011304659,0.0000069741163],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020357715,0.00031597476,0.00024243847,0.00091432704,0.00033424734,0.0005429806,0.0003589833,0.0002897354,0.00069587276],"category_scores_gemma":[0.00022402301,0.00033521844,0.0002849569,0.00040640024,0.00044969725,0.00035976732,0.00026322025,0.0000913087,0.00010666051],"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":[0.0005736953,0.00011289579,0.48510155,0.00019370555,0.00015692394,0.00062007713,0.00048008832,0.1358616,0.36363623,0.0018461351,0.0001437991,0.01127331],"study_design_scores_gemma":[0.000041206185,0.00006840763,0.6597416,0.000009084349,0.000035627872,0.00010594868,0.00036463584,0.31190884,0.026563244,0.0006060011,0.00051957107,0.000035944613],"about_ca_topic_score_codex":0.040850714,"about_ca_topic_score_gemma":0.05749616,"teacher_disagreement_score":0.040850714,"about_ca_system_score_codex":0.0011069066,"about_ca_system_score_gemma":0.00041234132,"threshold_uncertainty_score":0.08122587},"labels":[],"label_agreement":null},{"id":"W4417494721","doi":"10.1111/jmg.70030","title":"Location, Location, Location: Monazite Behaviour During UHT Metamorphism and Melt Crystallization","year":2025,"lang":"en","type":"article","venue":"Journal of Metamorphic Geology","topic":"Geological and Geochemical Analysis","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 Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Monazite; Zircon; Metamorphism; Metamorphic rock; Crystallization; Mineral; Granulite","score_opus":0.008334476671147673,"score_gpt":0.20314502594097794,"score_spread":0.19481054926983027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417494721","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883145,0.00007640271,0.0002234801,0.000012299778,7.695012e-7,0.0000025072302,0.00020500278,0.0000265128,0.0006215583],"genre_scores_gemma":[0.99957997,0.000019710846,0.00013312392,0.0000028624718,7.9444396e-7,0.0000016097335,0.00010516206,0.000008178192,0.00014845835],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999068,0.00001059416,0.0000056830427,0.000036131834,0.000014266881,0.00002647612],"domain_scores_gemma":[0.9998672,0.000020213003,0.000049701917,0.00001298096,0.000036074696,0.000013817738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001469582,0.00014746959,0.00024350503,0.0009214073,0.0004173528,0.0006104838,0.00025789108,0.00035776958,0.001857135],"category_scores_gemma":[0.00039529696,0.00018056421,0.00020533829,0.0005898342,0.00032222387,0.0002991585,0.00039005335,0.00013251751,0.0003526801],"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":[0.00034815518,0.000012533006,0.7935456,0.00008044784,0.000079991885,0.00023226465,0.00082444085,0.0006491747,0.19590162,0.00013585812,0.00010082205,0.008089086],"study_design_scores_gemma":[0.0000036607244,0.00002153541,0.990221,0.0000047309813,0.000015755013,0.0001340111,0.00023556632,0.0008653146,0.007883794,0.000022984503,0.00058700296,0.0000044830194],"about_ca_topic_score_codex":0.020060463,"about_ca_topic_score_gemma":0.031442516,"teacher_disagreement_score":0.020060463,"about_ca_system_score_codex":0.0005080141,"about_ca_system_score_gemma":0.00014981712,"threshold_uncertainty_score":0.03988737},"labels":[],"label_agreement":null}]}