{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":153,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":153,"direct_label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline (scores rank; they never assert a category)","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12","author_layer_release":"2026-06-26"},"query_hash":"6cf76ddf344a","filters":{"venue":"Geofluids"}},"results":[{"id":"W2092952629","doi":"10.1111/j.1468-8123.2009.00244.x","title":"Measurements of gas permeability and diffusivity of tight reservoir rocks: different approaches and their applications","year":2009,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":730,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Thermal diffusivity; Permeability (electromagnetism); Porosity; Tight gas; Geology; Adsorption; Mineralogy; Petroleum engineering; Porous medium; Soil science; Thermodynamics; Geotechnical engineering; Chemistry; Hydraulic fracturing","authors":[{"name":"Xinrui Cui","is_ca":true},{"name":"A. M. M. Bustin","is_ca":true},{"name":"R.M. Bustin","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03529322470865451,"gpt":0.2218627983941505,"spread":0.186569573685496,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009170618,0.0006059544,0.0003728543,0.001585072,0.0003051568,0.0006533362,0.0006192626,0.0008155937,0.0004216002],"category_scores_gemma":[0.001641932,0.000462269,0.0002849827,0.0008830943,0.0005772182,0.001523754,0.0008917298,0.000774386,0.00012958],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007142707,"about_ca_system_score_gemma":0.0002344948,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001346432,"about_ca_topic_score_gemma":0.001752824,"domain_scores_codex":[0.9993786,0.0001258984,0.00004240546,0.000178264,0.0002193929,0.00005536509],"domain_scores_gemma":[0.9992338,0.0003012591,0.0001798789,0.00007833805,0.0001554993,0.00005120459],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0002449136,0.0000650945,0.01411766,0.0005055455,0.0000693607,0.0001373964,0.0002908421,0.006852938,0.9379672,0.001936395,0.0001605469,0.03765216],"study_design_scores_gemma":[0.00001114016,0.0002233564,0.01389119,0.00006018646,0.00005578194,0.0004037094,0.0002152472,0.05120051,0.9300073,0.00104706,0.002788901,0.00009575907],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"methods","genre_scores_codex":[0.7749592,0.01174749,0.2074374,0.0002283602,0.00006474803,0.000124954,0.0005644147,0.0006054385,0.004267878],"genre_scores_gemma":[0.944914,0.002642932,0.05134455,0.00002782201,0.00001500257,0.00008318041,0.00008782578,0.00003926962,0.0008454637],"genre_candidate":"methods","genre_consensus":null,"teacher_disagreement_score":0.001585072,"threshold_uncertainty_score":0.005182445,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1825012390","doi":"10.1111/j.1468-8123.2005.00125.x","title":"Gas breakthrough pressure for hydrocarbon reservoir seal rocks: implications for the security of long‐term CO<sub>2</sub> storage in the Weyburn field","year":2005,"lang":"en","type":"article","venue":"Geofluids","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":195,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Saskatchewan Research Council (Canada); University of Regina","funders":"","keywords":"Caprock; Brine; Petroleum engineering; Evaporite; Geology; Permeability (electromagnetism); Seal (emblem); Enhanced oil recovery; High pressure; Geochemistry; Chemistry; Sedimentary rock; Archaeology","authors":[{"name":"S. Li","is_ca":true},{"name":"Mingzhe Dong","is_ca":true},{"name":"Zhong Li","is_ca":true},{"name":"Shijun Huang","is_ca":true},{"name":"Hairuo Qing","is_ca":true},{"name":"Erik Nickel","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01734432136174161,"gpt":0.2894710791591094,"spread":0.2721267577973677,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001611813,0.0001804885,0.0001986295,0.0002341193,0.0006777511,0.0004901166,0.0003122682,0.0003069718,0.001184508],"category_scores_gemma":[0.0003110408,0.0001673158,0.00009605614,0.0001765525,0.0004814415,0.0003699697,0.0002739255,0.0004212053,0.0001642772],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0008511782,"about_ca_system_score_gemma":0.0006760473,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02842055,"about_ca_topic_score_gemma":0.02806301,"domain_scores_codex":[0.9999007,0.000006789538,0.000004304472,0.00002448404,0.00002964626,0.00003409519],"domain_scores_gemma":[0.9997949,0.00004297759,0.0000514578,0.00001171632,0.00007109613,0.00002778197],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0004807799,0.00004840258,0.03277724,0.0000477432,0.00001169789,0.0002169365,0.0002175967,0.0006710319,0.9613566,0.0001007072,0.00008908883,0.003982275],"study_design_scores_gemma":[0.00002197939,0.0004916934,0.1477668,0.000007320676,0.0000155941,0.0001129205,0.0005903096,0.003821711,0.8463525,0.00005525259,0.0007465024,0.00001739625],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9993298,0.00004487113,0.0001973658,0.00002046224,0.000001198908,0.000004469182,0.00009101516,0.0000141021,0.0002967769],"genre_scores_gemma":[0.9994623,0.00002750676,0.0002225361,0.000006589396,9.440155e-7,0.000005138668,0.00006405903,0.000003840801,0.0002070485],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02842055,"threshold_uncertainty_score":0.05651021,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2753054181","doi":"10.1155/2017/6126505","title":"Worldwide Status of CCUS Technologies and Their Development and Challenges in China","year":2017,"lang":"en","type":"article","venue":"Geofluids","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":145,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Institut National de la Recherche Scientifique","funders":"National Natural Science Foundation of China; China Clean Development Mechanism Fund; Australian Government","keywords":"China; Industrialisation; Scale (ratio); Environmental science; Engineering; Fossil fuel; Business; Political science; Waste management; Geography","authors":[{"name":"H. J. Liu","is_ca":true},{"name":"Patrick Were","is_ca":false},{"name":"Qi Li","is_ca":false},{"name":"Yang Gou","is_ca":false},{"name":"Zhengmeng Hou","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03624130307325615,"gpt":0.2563840181141265,"spread":0.2201427150408703,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002789819,0.0008217151,0.000413687,0.002872636,0.0007254242,0.001985208,0.0007859883,0.0007083853,0.002694383],"category_scores_gemma":[0.00154548,0.0002230618,0.0004788881,0.005689016,0.001076636,0.002107978,0.0013302,0.0004049263,0.0003133839],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.003195024,"about_ca_system_score_gemma":0.009252129,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01215549,"about_ca_topic_score_gemma":0.006611546,"domain_scores_codex":[0.9988713,0.0001244686,0.0001819993,0.0001424757,0.000440397,0.0002395139],"domain_scores_gemma":[0.9979346,0.0002744837,0.0004986527,0.000125067,0.0008255705,0.0003415307],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0002822977,0.0001394006,0.04653899,0.003067589,0.0001060343,0.0009072092,0.0009126135,0.006464608,0.02248977,0.03403575,0.008215622,0.8768402],"study_design_scores_gemma":[0.00006248549,0.001570691,0.2734839,0.001224384,0.0002897028,0.002274627,0.004029795,0.01091207,0.04953635,0.012369,0.6440043,0.0002427352],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"review","genre_scores_codex":[0.6172535,0.2851678,0.01111656,0.01017023,0.0004231486,0.0002763869,0.001219979,0.0003915601,0.07398067],"genre_scores_gemma":[0.8427027,0.1374612,0.00786927,0.0006497369,0.0001578725,0.000100446,0.00116889,0.00003651856,0.009853352],"genre_candidate":"review","genre_consensus":null,"teacher_disagreement_score":0.01215549,"threshold_uncertainty_score":0.0241695,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2107075729","doi":"10.1046/j.1468-8123.2002.00041.x","title":"Equations of state for basin geofluids: algorithm review and intercomparison for brines","year":2002,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":143,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Sedimentary basin; Structural basin; Viscosity; Buoyancy; Geology; Salinity; Sedimentary rock; Flow (mathematics); Mineralogy; Petrology; Soil science; Geomorphology; Geochemistry; Mechanics; Thermodynamics; Oceanography","authors":[{"name":"Jennifer J. Adams","is_ca":false},{"name":"Stefan Bachu","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0273150377971118,"gpt":0.2527909978826558,"spread":0.225475960085544,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004649804,0.001208242,0.001771069,0.002065099,0.0005665988,0.001613918,0.003259421,0.001554245,0.01010165],"category_scores_gemma":[0.01438662,0.001199097,0.001543841,0.002624284,0.0006266029,0.001960412,0.001961756,0.002353244,0.003978633],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001500296,"about_ca_system_score_gemma":0.002702564,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01436212,"about_ca_topic_score_gemma":0.009858863,"domain_scores_codex":[0.9986275,0.0004701452,0.0001735274,0.0001710831,0.0004996114,0.00005810068],"domain_scores_gemma":[0.9941445,0.003271536,0.000234027,0.0003565096,0.001930964,0.00006238134],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.00008450471,0.0001072404,0.002126667,0.001422922,0.0002793218,0.00007840642,0.000206766,0.2876683,0.0009190317,0.037646,0.0202616,0.6491994],"study_design_scores_gemma":[0.00005734173,0.00004192887,0.0009000922,0.0005122915,0.0000779461,0.00007913733,0.00005619726,0.9257574,0.001623206,0.01413579,0.05670493,0.00005375934],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"methods","genre_gemma":"review","genre_scores_codex":[0.002719985,0.009980883,0.9795331,0.0006182894,0.0002449607,0.0002184774,0.0004613624,0.002275376,0.003947542],"genre_scores_gemma":[0.06810331,0.02182107,0.8957621,0.000384512,0.0004007576,0.001326284,0.002503205,0.001804046,0.007894742],"genre_candidate":"review","genre_consensus":null,"teacher_disagreement_score":0.01436212,"threshold_uncertainty_score":0.03379339,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2158304587","doi":"10.1111/j.1468-8123.2010.00289.x","title":"Fluid flows and metal deposition near basement /cover unconformity: lessons and analogies from Pb–Zn–F–Ba systems for the understanding of Proterozoic U deposits","year":2010,"lang":"en","type":"article","venue":"Geofluids","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Unconformity; Geochemistry; Graben; Rift; Fluid inclusions; Proterozoic; Tectonics; Basement; Petrology; Sedimentary rock; Paleontology; Quartz","authors":[{"name":"Marie‐Christine Boiron","is_ca":false},{"name":"‪Michel Cathelineau","is_ca":false},{"name":"Antonin Richard","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02873279294839744,"gpt":0.2178015306717881,"spread":0.1890687377233906,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001539399,0.0002797441,0.00028027,0.001324915,0.0004417057,0.0008924094,0.0003139907,0.0005387014,0.001050757],"category_scores_gemma":[0.0005046488,0.0002436349,0.000294471,0.0007442417,0.001409607,0.00100119,0.0006806692,0.0003614198,0.0001078628],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0009506942,"about_ca_system_score_gemma":0.0003593235,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02272492,"about_ca_topic_score_gemma":0.01061917,"domain_scores_codex":[0.9999446,0.00001024947,0.000005413763,0.00001605672,0.000008809237,0.0000149458],"domain_scores_gemma":[0.9998887,0.0000330284,0.00003399355,0.00001029183,0.00001903725,0.0000149518],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0006063175,0.000305939,0.6622936,0.0004850175,0.0001730256,0.00397219,0.008078704,0.05620772,0.1459827,0.02482682,0.0006286066,0.0964394],"study_design_scores_gemma":[0.00003714582,0.0001659012,0.8820397,0.00007987638,0.00004673852,0.0008187988,0.0041804,0.0855086,0.00764321,0.01370123,0.005710694,0.00006768561],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9947683,0.0007880299,0.001803904,0.0001777953,0.000007923268,0.00001522111,0.00005688313,0.00002514851,0.002356731],"genre_scores_gemma":[0.9984682,0.0005158712,0.000741638,0.00001323499,0.00001027581,0.000003454105,0.00003110394,0.000005469825,0.0002108297],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02272492,"threshold_uncertainty_score":0.04518533,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2132230202","doi":"10.1046/j.1468-8123.2001.11004.x","title":"Interpretation of observed fluid potential patterns in a deep sedimentary basin under tectonic compression: Hungarian Great Plain, Pannonian Basin","year":2001,"lang":"en","type":"article","venue":"Geofluids","topic":"Geological Formations and Processes Exploration","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Neogene; Sedimentary rock; Structural basin; Geomorphology; Petrology; Hydrostatic pressure; Tectonics; Clastic rock; Sedimentary basin; Flysch; Basement; Horst; Geochemistry; Paleontology","authors":[{"name":"J. Tóth","is_ca":true},{"name":"István Almási","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01997188009057461,"gpt":0.2175395886601852,"spread":0.1975677085696106,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001060815,0.0001793959,0.0001734222,0.001092539,0.0002875561,0.0006034568,0.0002083758,0.0002217293,0.0008154199],"category_scores_gemma":[0.0002921993,0.0001507683,0.0001265946,0.001394882,0.0005773454,0.0003400029,0.000424322,0.0000821541,0.00006353837],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007734837,"about_ca_system_score_gemma":0.000386842,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.04696015,"about_ca_topic_score_gemma":0.05812321,"domain_scores_codex":[0.9999499,0.000006129975,0.000005185927,0.00001521513,0.000008196112,0.00001520954],"domain_scores_gemma":[0.9999121,0.00001802793,0.00002045139,0.000007518136,0.0000266927,0.00001506006],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001559215,0.00003260416,0.957296,0.00007415455,0.00007666324,0.0008002553,0.0008317832,0.004612164,0.0171746,0.0002447458,0.0001978158,0.01850329],"study_design_scores_gemma":[0.000004813104,0.000007832312,0.9972885,0.000004318061,0.000006915907,0.00003165344,0.0002470165,0.002002809,0.0002057351,0.00003904551,0.0001578808,0.000003569754],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9991884,0.00003464654,0.00009401098,0.00001390034,8.964312e-7,0.000003438221,0.0001612303,0.000009729282,0.00049376],"genre_scores_gemma":[0.9996829,0.00002640904,0.00009591746,0.000004147526,7.140997e-7,0.000002984572,0.0001274736,0.00000139967,0.00005805174],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04696015,"threshold_uncertainty_score":0.0933736,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2139406724","doi":"10.1111/gfl.12147","title":"Klinkenberg gas slippage measurements as a means for shale pore structure characterization","year":2015,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":100,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slippage; Tortuosity; Permeability (electromagnetism); Geology; Porosity; Oil shale; Anisotropy; Pore water pressure; Mineralogy; Materials science; Geotechnical engineering; Composite material; Chemistry; Optics","authors":[{"name":"Eric Aiden Letham","is_ca":true},{"name":"R.M. Bustin","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03677529876011934,"gpt":0.2441816702756899,"spread":0.2074063715155705,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003892612,0.0001821843,0.0001517395,0.0008650194,0.0002238821,0.0003377826,0.0001645117,0.000148575,0.001391134],"category_scores_gemma":[0.0006539144,0.0001073602,0.0000716116,0.00051453,0.0002458812,0.0004326577,0.000231083,0.0002046983,0.0002342202],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001798187,"about_ca_system_score_gemma":0.000268304,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001221855,"about_ca_topic_score_gemma":0.003085937,"domain_scores_codex":[0.9998063,0.00002460464,0.00001518894,0.00002995968,0.00009906112,0.00002488465],"domain_scores_gemma":[0.9995145,0.000176575,0.0001075442,0.00003411128,0.0001370199,0.00003023937],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0001464969,0.00003840847,0.02728022,0.00009398457,0.00001508637,0.0001423637,0.0002019304,0.002741827,0.9467955,0.0005231199,0.0002169531,0.02180408],"study_design_scores_gemma":[0.000007413435,0.0001954603,0.0750838,0.00001820616,0.00001066807,0.0001843565,0.0002084521,0.02065158,0.9012014,0.0003236088,0.002100317,0.00001476748],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.981478,0.0004192845,0.01576685,0.0000309746,0.00001110688,0.00002068373,0.0004773017,0.0001249585,0.001670938],"genre_scores_gemma":[0.9892693,0.0002853746,0.009345308,0.00001158595,0.000002702396,0.0000307983,0.0002355784,0.00001465249,0.0008045915],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.001391134,"threshold_uncertainty_score":0.004653811,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2935796506","doi":"10.1155/2019/3089292","title":"A General Review on Longwall Mining-Induced Fractures in Near-Face Regions","year":2019,"lang":"en","type":"review","venue":"Geofluids","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":73,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Fundamental Research Funds for the Central Universities; Priority Academic Program Development of Jiangsu Higher Education Institutions","keywords":"Longwall mining; Mining engineering; Overburden; Coal mining; Rock mass classification; Geology; Coal; Hard coal; Ground pressure; Geotechnical engineering; Engineering","authors":[{"name":"Qingsheng Bai","is_ca":true},{"name":"Shihao Tu","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.06528517212905381,"gpt":0.3226440583882088,"spread":0.2573588862591549,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004268023,0.001069598,0.001274626,0.003585058,0.0004333156,0.00131387,0.001048826,0.001311287,0.007285035],"category_scores_gemma":[0.0007013034,0.00047502,0.001312213,0.003240191,0.000364255,0.001935095,0.0006375129,0.00087785,0.002556704],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0005479324,"about_ca_system_score_gemma":0.001547852,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002737978,"about_ca_topic_score_gemma":0.00304891,"domain_scores_codex":[0.9997415,0.00003333909,0.0000511502,0.0000688812,0.00007402655,0.0000311905],"domain_scores_gemma":[0.999613,0.0001477724,0.00008525397,0.00001083596,0.0001140079,0.00002914832],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0001889129,0.0001288314,0.001663089,0.08636964,0.0002822462,0.001224632,0.0003413871,0.00255147,0.01019541,0.00803932,0.07056459,0.8184505],"study_design_scores_gemma":[0.000007691428,0.000143545,0.002277895,0.005573957,0.0002352616,0.001789302,0.0001392137,0.0002321597,0.001297736,0.001277405,0.9869887,0.00003724299],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"review","genre_gemma":"review","genre_scores_codex":[0.0006951775,0.9945911,0.0008849598,0.0002783224,0.0005442878,0.00001648882,0.0001625724,0.00002901931,0.00279817],"genre_scores_gemma":[0.002259975,0.9948391,0.0006360397,0.0002117299,0.0004025453,0.00001434897,0.0002367146,0.000006989463,0.001392598],"genre_candidate":"review","genre_consensus":"review","teacher_disagreement_score":0.007285035,"threshold_uncertainty_score":0.02437085,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2077069342","doi":"10.1111/j.1468-8123.2005.00119.x","title":"Hydrothermal activity associated with the Ries impact event, Germany","year":2005,"lang":"en","type":"article","venue":"Geofluids","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":71,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Canadian Space Agency","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Impact crater; Hydrothermal circulation; Geochemistry; Sedimentary rock; Crater lake; Clastic rock; Impact structure; Mineralogy; Volcano; Paleontology","authors":[{"name":"G. R. Osinski","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008735345670509098,"gpt":0.23393470221001,"spread":0.2251993565395009,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004995872,0.0002112979,0.000139801,0.001137073,0.0002321326,0.0003582043,0.00010032,0.0001312227,0.0009943746],"category_scores_gemma":[0.00009352188,0.0001045737,0.00007725124,0.0006900356,0.000204231,0.0001135583,0.000350904,0.00008959753,0.000144024],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007200667,"about_ca_system_score_gemma":0.0003275618,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02424177,"about_ca_topic_score_gemma":0.06197221,"domain_scores_codex":[0.9999313,0.000002938263,0.000003964502,0.00001632983,0.0000200181,0.0000254215],"domain_scores_gemma":[0.9999467,0.000002926808,0.00002251081,0.000002249869,0.000009693713,0.00001592672],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004813214,0.00005339596,0.8812462,0.000129676,0.000119236,0.001665174,0.001043499,0.001472452,0.08985545,0.0003547126,0.0006746285,0.02290432],"study_design_scores_gemma":[0.000002537688,0.00002912532,0.9965862,0.000002286553,0.000008563227,0.000126536,0.0001727987,0.0001290116,0.002161414,0.00001065099,0.0007681293,0.00000256973],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.997954,0.0000833343,0.00004443021,0.000007287144,0.000001873533,0.000006585376,0.0004898467,0.00001119667,0.001401427],"genre_scores_gemma":[0.9989004,0.0000925132,0.00006239575,0.000003444722,0.000001942997,0.000002105184,0.0004837853,0.000001574714,0.0004517759],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02424177,"threshold_uncertainty_score":0.04820132,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2104894654","doi":"10.1111/j.1468-8123.2004.00084.x","title":"Factors controlling free thermal convection in faults in sedimentary basins: implications for the formation of zinc–lead mineral deposits","year":2004,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":69,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Groundwater recharge; Sedimentary rock; Geothermal gradient; Geochemistry; Sedimentary basin; Hydrothermal circulation; Hydrogeology; Mineral resource classification; Fault (geology); Structural basin; Lead (geology); Anhydrite; Convection; Petrology; Fluid dynamics; Aquifer; Geophysics; Geomorphology; Groundwater; Geotechnical engineering; Seismology; Paleontology","authors":[{"name":"Jianwen Yang","is_ca":true},{"name":"Ross R. Large","is_ca":false},{"name":"Stuart W. Bull","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01885711610508457,"gpt":0.23544983947488,"spread":0.2165927233697954,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000197744,0.0003361253,0.0003173774,0.0003440083,0.0004449888,0.001009724,0.0003581497,0.0005133802,0.0007353731],"category_scores_gemma":[0.001092181,0.0002945089,0.0004317342,0.0002246424,0.0008519386,0.0006700867,0.0005678231,0.0002430627,0.00004403997],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001192048,"about_ca_system_score_gemma":0.0005811761,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02390352,"about_ca_topic_score_gemma":0.01039893,"domain_scores_codex":[0.9999198,0.00002596043,0.000007054908,0.00001798261,0.00000918832,0.00002009484],"domain_scores_gemma":[0.9997575,0.0001070477,0.00005218953,0.00001699149,0.00002591782,0.00004038545],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","study_design_scores_codex":[0.0001901313,0.0001467291,0.1038636,0.00004187138,0.00004618071,0.0002508194,0.0001543092,0.8768794,0.01443973,0.001281855,0.00009859996,0.002606784],"study_design_scores_gemma":[0.00005008218,0.00006650719,0.03527677,0.000003565392,0.00001665917,0.0000248043,0.0001119036,0.9627705,0.001137187,0.0004594974,0.00006954853,0.0000129188],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9986119,0.00002721412,0.0009543921,0.00003211785,0.000002123495,0.000008399324,0.00002752079,0.000009388395,0.0003269445],"genre_scores_gemma":[0.9997742,0.00001226148,0.0001332093,0.000002180866,9.778453e-7,0.000002067451,0.00001029902,0.000001492168,0.00006335694],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02390352,"threshold_uncertainty_score":0.04752874,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2121842257","doi":"10.1111/j.1468-8123.2007.00178.x","title":"Fluids, basin analysis, and mineral deposits","year":2007,"lang":"en","type":"article","venue":"Geofluids","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Diagenesis; Structural basin; Sedimentary basin; Geochemistry; Sedimentary basin analysis; Lithology; Sedimentary rock; Precambrian; Dolomitization; Facies; Geomorphology; Petrology; Paleontology","authors":[{"name":"Kurt Kyser","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.007303273532256536,"gpt":0.1951292845704403,"spread":0.1878260110381838,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003675654,0.0002055947,0.0001724188,0.004839784,0.000301685,0.001094007,0.0002031864,0.0001186801,0.00351137],"category_scores_gemma":[0.001223545,0.0001024617,0.0002907327,0.002757256,0.0004132472,0.0006602578,0.00077627,0.0002164693,0.0002029211],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0008260483,"about_ca_system_score_gemma":0.0007587724,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01242812,"about_ca_topic_score_gemma":0.02102106,"domain_scores_codex":[0.9998165,0.00005789198,0.00001741966,0.00002755622,0.00005523458,0.00002545699],"domain_scores_gemma":[0.9995533,0.0001947913,0.00008612036,0.00002025873,0.0001040592,0.00004147394],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003672942,0.0001042447,0.6563041,0.0002965118,0.0003379744,0.0005466064,0.001431244,0.03302138,0.007609903,0.03488072,0.002408345,0.2626917],"study_design_scores_gemma":[0.00002604095,0.0002044431,0.7266088,0.0001114661,0.0002029247,0.0004970349,0.004901539,0.1783319,0.007118606,0.03846231,0.04348648,0.00004843041],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9643155,0.0007923022,0.01903064,0.000214087,0.00001450419,0.00008629076,0.001485674,0.0003544249,0.01370657],"genre_scores_gemma":[0.9839048,0.0001099505,0.01304926,0.00001217669,0.000007093002,0.00003203349,0.0005063062,0.00003162049,0.002346781],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01242812,"threshold_uncertainty_score":0.02471155,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2756292070","doi":"10.1155/2017/4251209","title":"Flow and Transport in Tight and Shale Formations: A Review","year":2017,"lang":"en","type":"review","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":56,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Regina","funders":"King Abdullah University of Science and Technology","keywords":"Scale (ratio); Flow (mathematics); Nonlinear system; Porous medium; Darcy's law; Slippage; Tight gas; Oil shale; Geology; Transport phenomena; Macroscopic scale; Computer science; Mechanics; Petroleum engineering; Statistical physics; Physics; Porosity; Geotechnical engineering; Materials science; Hydraulic fracturing","authors":[{"name":"Amgad Salama","is_ca":true},{"name":"Kundan Kumar","is_ca":false},{"name":"Shuyu Sun","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.05025749146694465,"gpt":0.3067939164471479,"spread":0.2565364249802033,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004296364,0.001189615,0.001569426,0.00210926,0.0004882584,0.001408654,0.0009774985,0.001420939,0.003056556],"category_scores_gemma":[0.0006435096,0.0004698058,0.0009128685,0.002932314,0.000655235,0.002413014,0.0007652197,0.001054645,0.001295732],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0005402538,"about_ca_system_score_gemma":0.001377535,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002278973,"about_ca_topic_score_gemma":0.001600855,"domain_scores_codex":[0.9997852,0.00002838322,0.0000365241,0.00005930291,0.00006851085,0.00002209492],"domain_scores_gemma":[0.9995523,0.0002483261,0.00007116251,0.00001499438,0.00008761857,0.00002568556],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.00009934128,0.0001874909,0.001247921,0.04883207,0.0001872157,0.0005141406,0.000298513,0.005308955,0.007406559,0.01852054,0.03474129,0.8826561],"study_design_scores_gemma":[0.00000757754,0.000191831,0.001753093,0.005113917,0.0002523647,0.001748097,0.0002197965,0.001843352,0.00275478,0.006495587,0.9795341,0.00008549939],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"review","genre_gemma":"review","genre_scores_codex":[0.0004960434,0.9970505,0.0008788636,0.0002453695,0.0002313757,0.000004032504,0.00002874116,0.00001767538,0.001047404],"genre_scores_gemma":[0.002164953,0.9963199,0.0004907987,0.000104943,0.0003370098,0.000005818221,0.0000508861,0.000004458795,0.0005212457],"genre_candidate":"review","genre_consensus":"review","teacher_disagreement_score":0.003056556,"threshold_uncertainty_score":0.01022518,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2128929598","doi":"10.1111/j.1468-8123.2011.00349.x","title":"The stress regime of the Western Canadian Sedimentary Basin","year":2011,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":55,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Geothermal gradient; Structural basin; Sedimentary rock; Sedimentary basin; Stress (linguistics); Drilling; Hydraulic fracturing; Geomorphology; Petrology; Geotechnical engineering; Geochemistry; Geophysics","authors":[{"name":"J. S. Bell","is_ca":false},{"name":"Stephen E. Grasby","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008614484930297933,"gpt":0.1774194942749636,"spread":0.1688050093446656,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000141998,0.0002595249,0.0002426498,0.002872842,0.002360739,0.0009559836,0.0005008462,0.0001668813,0.001451846],"category_scores_gemma":[0.0005416539,0.0001854413,0.0001386696,0.0041202,0.0008203044,0.0002077478,0.0004525854,0.0001368255,0.0001089231],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.01309893,"about_ca_system_score_gemma":0.0126316,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9900057,"about_ca_topic_score_gemma":0.9969801,"domain_scores_codex":[0.9997646,0.000005038927,0.00001087994,0.0000375965,0.0001088125,0.00007313868],"domain_scores_gemma":[0.999422,0.00001710137,0.0000568404,0.00001122619,0.0004360913,0.00005690565],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0001870706,0.0000370146,0.9096077,0.000231951,0.0001310802,0.0004102721,0.002489628,0.005247818,0.018851,0.001287928,0.002945094,0.05857349],"study_design_scores_gemma":[0.000003186768,0.000009369775,0.9936389,0.00002360545,0.00001506766,0.00003899095,0.000934514,0.0008055074,0.0009200648,0.00007235607,0.003523426,0.00001494825],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9906157,0.0003812782,0.0001929589,0.00008963798,0.000005551608,0.00001257838,0.001630792,0.00002833196,0.007043181],"genre_scores_gemma":[0.9983308,0.0001866305,0.0001952012,0.00001676095,0.000001550623,0.000004722861,0.0005150591,0.000003349355,0.0007459754],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01309893,"threshold_uncertainty_score":0.09503984,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2162228948","doi":"10.1111/gfl.12107","title":"Normal stress‐induced permeability hysteresis of a fracture in a granite cylinder","year":2014,"lang":"en","type":"article","venue":"Geofluids","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":54,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"McGill University","funders":"Canadian Nuclear Safety Commission; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Permeability (electromagnetism); Materials science; Geotechnical engineering; Fracture (geology); Stress (linguistics); Geology; Composite material; Chemistry","authors":[{"name":"A. P. S. Selvadurai","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.00968205724664209,"gpt":0.2054480129860516,"spread":0.1957659557394095,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002216709,0.0001582381,0.0003211061,0.0002485557,0.0003064119,0.000307016,0.000359337,0.0003548424,0.0007354554],"category_scores_gemma":[0.0005470685,0.0001682534,0.0001847953,0.0002061172,0.0006194309,0.0001976096,0.0002957943,0.0003242386,0.00009673581],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0003246691,"about_ca_system_score_gemma":0.0002582122,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002238893,"about_ca_topic_score_gemma":0.002288189,"domain_scores_codex":[0.9998239,0.0000123998,0.000008630216,0.00002452899,0.00008333565,0.00004733934],"domain_scores_gemma":[0.9996686,0.0001022879,0.00007369504,0.00003004906,0.00007900188,0.00004637501],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0004671027,0.00004964964,0.002077027,0.00004879373,0.000009320408,0.0005212001,0.0001147183,0.003305709,0.9907838,0.0001186383,0.00004937982,0.002454574],"study_design_scores_gemma":[0.00004163521,0.001525328,0.04461299,0.00001389605,0.00001907301,0.0007135012,0.000380489,0.0248375,0.9264508,0.0002396099,0.001121003,0.0000441304],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9992985,0.0000617905,0.000401045,0.000009936253,0.000003475412,0.000003673288,0.0000240297,0.00001633461,0.000181291],"genre_scores_gemma":[0.9996837,0.00002568822,0.0001448827,0.000002989999,7.714523e-7,0.000002155317,0.00001961481,0.000002201111,0.0001180533],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.002238893,"threshold_uncertainty_score":0.004451692,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2070171665","doi":"10.1111/gfl.12115","title":"How well can we predict permeability in sedimentary basins? Deriving and evaluating porosity–permeability equations for noncemented sand and clay mixtures","year":2014,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":53,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"McGill University","funders":"","keywords":"Permeability (electromagnetism); Porosity; Silt; Geology; Geotechnical engineering; Sedimentary rock; Mineralogy; Grain size; Soil science; Geomorphology; Geochemistry; Chemistry","authors":[{"name":"Elco Luijendijk","is_ca":false},{"name":"Tom Gleeson","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01841020632849829,"gpt":0.2519785484218695,"spread":0.2335683420933712,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001235686,0.000411171,0.0003799182,0.0007045147,0.0002016647,0.0007916341,0.000590108,0.000551733,0.0002159325],"category_scores_gemma":[0.007839761,0.0003778833,0.0003815772,0.0004238278,0.0006406625,0.001143004,0.0004136981,0.0003739781,0.00008680041],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001344492,"about_ca_system_score_gemma":0.0008654469,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.03499408,"about_ca_topic_score_gemma":0.02176303,"domain_scores_codex":[0.9996307,0.0001251689,0.00003603,0.00008507947,0.00008728216,0.0000358716],"domain_scores_gemma":[0.997061,0.001849298,0.0005507241,0.0001794766,0.0002795734,0.00008004368],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00003737883,0.00002553725,0.05341053,0.00002271257,0.00004713479,0.00005517494,0.00005595858,0.9339591,0.004299706,0.0005949555,0.0000554155,0.007436313],"study_design_scores_gemma":[0.000002995225,0.000006584235,0.007635294,0.000002793564,0.000003913655,0.000009681883,0.00001112314,0.9899548,0.001954198,0.0003603568,0.00005243078,0.000005780754],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.947942,0.00008239491,0.05119488,0.00006501094,0.000003596796,0.00001560026,0.0001369976,0.0001634213,0.0003960608],"genre_scores_gemma":[0.9921165,0.00002616728,0.007690357,0.000004161356,0.000001472838,0.000009774483,0.00005949834,0.00001558219,0.00007653113],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03499408,"threshold_uncertainty_score":0.06958073,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2098780849","doi":"10.1111/j.1468-8123.2007.00201.x","title":"The role of thermochemical sulfate reduction in the origin of Mississippi Valley‐type deposits. I. Experimental results","year":2007,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":53,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto; University of British Columbia","funders":"Eidgenössische Technische Hochschule Zürich","keywords":"Sulfate; Sulfide; Mineralogy; Range (aeronautics); Kinetics; Geology; Chemistry; Environmental science; Materials science; Physics","authors":[{"name":"J. Thom","is_ca":true},{"name":"G. M. Anderson","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0117783262799005,"gpt":0.2485328828707197,"spread":0.2367545565908192,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003613301,0.0002993397,0.0003436519,0.000303851,0.0009656068,0.0003416426,0.000426422,0.0003612806,0.0009429816],"category_scores_gemma":[0.000407229,0.0002544675,0.0002103202,0.0002609096,0.0003576384,0.0002414019,0.0002624709,0.0003628669,0.0002345268],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000764492,"about_ca_system_score_gemma":0.0005050055,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.03100413,"about_ca_topic_score_gemma":0.0339709,"domain_scores_codex":[0.9997554,0.00003902096,0.00001542181,0.00007153042,0.00007171477,0.0000468545],"domain_scores_gemma":[0.9998069,0.00005971878,0.00003001907,0.00002270133,0.00006102284,0.00001957535],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0004852125,0.00009731607,0.01066234,0.0001288839,0.00001815324,0.0001047226,0.0001829922,0.001900589,0.9822707,0.0001639668,0.00004328918,0.003941807],"study_design_scores_gemma":[0.00001671027,0.0003740168,0.02227018,0.000007953937,0.00001519341,0.00007049066,0.0001176066,0.003821409,0.9723271,0.00005849742,0.000905207,0.00001571042],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9981603,0.0001778074,0.0006314636,0.00002034281,0.000001126318,0.00002514157,0.0002868015,0.00001360837,0.00068346],"genre_scores_gemma":[0.9970436,0.0002266774,0.001762368,0.0000116478,0.00000162809,0.00002794881,0.0002916722,0.000005972074,0.0006283768],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03100413,"threshold_uncertainty_score":0.06164736,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2520282094","doi":"10.1111/gfl.12188","title":"The biases and trends in fault zone hydrogeology conceptual models: global compilation and categorical data analysis","year":2016,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Victoria; McGill University","funders":"Japan Atomic Energy Agency; Fonds de recherche du Québec – Nature et technologies; U.S. Geological Survey","keywords":"Electrical conduit; Geology; Lithology; Hydrogeology; Outcrop; Petrology; Fault (geology); Borehole; Sedimentary rock; Permeability (electromagnetism); Categorical variable; Seismology; Geochemistry; Geotechnical engineering","authors":[{"name":"Jacek Scibek","is_ca":true},{"name":"Tom Gleeson","is_ca":true},{"name":"Jeffrey M. McKenzie","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.07192914647151451,"gpt":0.2738672665460626,"spread":0.2019381200745481,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.06294417,0.0008218224,0.001176772,0.02136891,0.0002551631,0.004253349,0.001967015,0.0006004219,0.00162646],"category_scores_gemma":[0.1798152,0.0004914686,0.002846702,0.03099426,0.001571952,0.00398706,0.002071811,0.00100794,0.0004099141],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.002237673,"about_ca_system_score_gemma":0.002074913,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00731665,"about_ca_topic_score_gemma":0.007121861,"domain_scores_codex":[0.9650431,0.01914949,0.005217122,0.004489913,0.00573594,0.0003644928],"domain_scores_gemma":[0.6157086,0.2924773,0.03021792,0.0190848,0.04188152,0.0006298415],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003762669,0.00005734225,0.5630099,0.0251803,0.009294847,0.0001629661,0.004115047,0.02171704,0.0009369521,0.01741297,0.01125936,0.346477],"study_design_scores_gemma":[0.0001046482,0.0005643185,0.7370132,0.0419062,0.007546441,0.0006773317,0.009185092,0.05322084,0.004095302,0.0295229,0.1157436,0.0004201797],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.4400978,0.3571284,0.1289279,0.006811616,0.0007595085,0.000327046,0.04956985,0.00131219,0.01506577],"genre_scores_gemma":[0.8887813,0.05650806,0.03770683,0.0007959164,0.0002842445,0.0003742354,0.0146857,0.0003795474,0.0004840819],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06294417,"threshold_uncertainty_score":0.3328845,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2157640033","doi":"10.1111/j.1468-8123.2011.00360.x","title":"Models of ice‐sheet hydrogeologic interactions: a review","year":2012,"lang":"en","type":"review","venue":"Geofluids","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Ice sheet; Glacial period; Ice-sheet model; Groundwater recharge; Hydrogeology; Greenland ice sheet; Ice stream; Cryosphere; Geomorphology; Aquifer; Groundwater; Climatology; Sea ice; Geotechnical engineering","authors":[{"name":"Mark Person","is_ca":false},{"name":"Victor Bense","is_ca":false},{"name":"Denis Cohen","is_ca":false},{"name":"Amlan Banerjee","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.1298268267287514,"gpt":0.3104961348546333,"spread":0.1806693081258819,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007190292,0.001463688,0.001234032,0.002151591,0.0002422224,0.001566516,0.001528695,0.0008763958,0.002594126],"category_scores_gemma":[0.00146313,0.0006625263,0.00100598,0.003303931,0.0005246371,0.001844731,0.0008461137,0.0007157527,0.001317574],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007530327,"about_ca_system_score_gemma":0.001245686,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005032469,"about_ca_topic_score_gemma":0.002937963,"domain_scores_codex":[0.9998568,0.00002978413,0.00001920543,0.00003701718,0.00004388175,0.00001332312],"domain_scores_gemma":[0.9994037,0.0003600978,0.00005878205,0.00003935053,0.00011192,0.00002619776],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0000998562,0.00008922271,0.004491509,0.0146333,0.0005973366,0.0003062727,0.0001836992,0.1279123,0.001416299,0.02396329,0.03405549,0.7922514],"study_design_scores_gemma":[0.00003141461,0.0001107727,0.004467025,0.008962528,0.0005264108,0.0005110889,0.0001647214,0.04718701,0.001072241,0.0355371,0.901326,0.0001037255],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"review","genre_gemma":"review","genre_scores_codex":[0.002601222,0.9824003,0.008550961,0.0006991117,0.0002963467,0.00001541225,0.0004912455,0.000187097,0.004758326],"genre_scores_gemma":[0.01359937,0.9815031,0.003093515,0.0001504894,0.0003496309,0.00002401948,0.0005566122,0.0000396137,0.0006835834],"genre_candidate":"review","genre_consensus":"review","teacher_disagreement_score":0.005032469,"threshold_uncertainty_score":0.01000637,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2139139371","doi":"10.1111/gfl.12097","title":"Development of connected permeability in massive crystalline rocks through hydraulic fracture propagation and shearing accompanying fluid injection","year":2014,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Centre for Excellence in Mining Innovation; University of Alberta; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Permeability (electromagnetism); Geology; Hydraulic fracturing; Fluid dynamics; Shearing (physics); Geotechnical engineering; Anisotropy; Injection well; Overburden pressure; Petrology; Materials science; Mechanics; Petroleum engineering","authors":[{"name":"Giona Preisig","is_ca":true},{"name":"Erik Eberhardt","is_ca":true},{"name":"Valentin Gischig","is_ca":true},{"name":"Vincent Roche","is_ca":true},{"name":"Mirko van der Baan","is_ca":true},{"name":"Benoît Valley","is_ca":false},{"name":"Peter Kaiser","is_ca":true},{"name":"Damien Jade Duff","is_ca":true},{"name":"Robert Lowther","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01215255295539809,"gpt":0.2254360591670999,"spread":0.2132835062117018,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001414874,0.0002094974,0.0002515242,0.0003201313,0.0002239724,0.0005091895,0.0004036068,0.0005606205,0.001014369],"category_scores_gemma":[0.0004529573,0.0002088106,0.0003057031,0.0001746527,0.0006988118,0.0002958485,0.0003387733,0.0003245457,0.00007513248],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0004364261,"about_ca_system_score_gemma":0.0004036666,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003480666,"about_ca_topic_score_gemma":0.002308398,"domain_scores_codex":[0.9999207,0.000008911437,0.000006352461,0.00001694219,0.00002638756,0.00002076487],"domain_scores_gemma":[0.9998044,0.00006935501,0.00006327354,0.00001844186,0.00002146058,0.00002299227],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0002549727,0.0002408248,0.01516341,0.00008981764,0.00003690742,0.000503169,0.0001461495,0.762562,0.2138941,0.001912677,0.00009460542,0.005101242],"study_design_scores_gemma":[0.00001949571,0.0001230935,0.007186667,0.000006268247,0.00001186262,0.00006992184,0.00005516475,0.9643512,0.02752379,0.0005099148,0.0001272502,0.00001521747],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9908562,0.00003050705,0.007861846,0.00003008293,0.00000525442,0.0000185044,0.00006622731,0.0000579037,0.001073543],"genre_scores_gemma":[0.9989705,0.00001713345,0.0007751036,0.000003597927,8.296466e-7,0.000007531435,0.00001820708,0.00000307064,0.0002039577],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.003480666,"threshold_uncertainty_score":0.006920815,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2156645571","doi":"10.1111/gfl.12098","title":"Is the permeability of crystalline rock in the shallow crust related to depth, lithology or tectonic setting?","year":2014,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Geology; Lithology; Crust; Tectonics; Permeability (electromagnetism); Overburden; Petrology; Geomorphology; Geochemistry; Seismology; Geotechnical engineering","authors":[{"name":"Mark Ranjram","is_ca":true},{"name":"Tom Gleeson","is_ca":true},{"name":"Elco Luijendijk","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01227218156387928,"gpt":0.2508351279314643,"spread":0.2385629463675851,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003231612,0.0002205395,0.000413717,0.001275593,0.0001998438,0.0006310356,0.0002833647,0.0002723805,0.00159601],"category_scores_gemma":[0.001144576,0.0002103814,0.0002302624,0.001429185,0.0007135253,0.0008408524,0.0005870512,0.0002098277,0.0002485676],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000253103,"about_ca_system_score_gemma":0.0001167122,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004117269,"about_ca_topic_score_gemma":0.00447859,"domain_scores_codex":[0.9998411,0.00002077382,0.00002360992,0.00005465926,0.00002613524,0.00003379895],"domain_scores_gemma":[0.9988248,0.0002798301,0.0005854261,0.00009604998,0.000132279,0.00008163138],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001566921,0.00001274718,0.9334463,0.0001512446,0.0001487557,0.0001351069,0.0002423485,0.000811105,0.05809043,0.0001246535,0.00005027891,0.006630209],"study_design_scores_gemma":[0.00000131517,0.00001717323,0.9974528,0.000005157282,0.00001775519,0.00004746404,0.0001263986,0.0003692902,0.001779638,0.00008868727,0.00009003588,0.00000431213],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9985175,0.0002822283,0.0003199323,0.00001569764,0.000001196561,0.000002026533,0.0002821298,0.000008815855,0.0005704807],"genre_scores_gemma":[0.9997435,0.00005175497,0.00004891122,0.000004520247,0.000001276763,8.086359e-7,0.00009788669,0.000002079069,0.00004926015],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.004117269,"threshold_uncertainty_score":0.008186638,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2551400655","doi":"10.1111/gfl.12180","title":"The effects of basement faults on thermal convection and implications for the formation of unconformity‐related uranium deposits in the Athabasca Basin, Canada","year":2016,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Regina","funders":"Cameco","keywords":"Geology; Unconformity; Convection; Convection cell; Fault (geology); Geothermal gradient; Petrology; Basement; Fluid dynamics; Structural basin; Plume; Upwelling; Geophysics; Uranium ore; Thermal; Shear (geology); Geochemistry; Geomorphology; Seismology; Natural convection; Uranium; Mechanics; Combined forced and natural convection; Meteorology","authors":[{"name":"Zhong Li","is_ca":true},{"name":"Guoxiang Chi","is_ca":true},{"name":"Kathryn M. Bethune","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006683669626555591,"gpt":0.1943836317959739,"spread":0.1876999621694183,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001777509,0.0004802217,0.0002823413,0.0005983733,0.001160304,0.001296595,0.000742332,0.0007497512,0.00192139],"category_scores_gemma":[0.0007176686,0.0002317072,0.0005847252,0.000635191,0.0009011037,0.000383085,0.0005923895,0.0003721013,0.0001060098],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.007479225,"about_ca_system_score_gemma":0.00403668,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.7555337,"about_ca_topic_score_gemma":0.639019,"domain_scores_codex":[0.9998627,0.00002166346,0.00000749821,0.00002313774,0.00002575339,0.00005929392],"domain_scores_gemma":[0.9997646,0.00006367319,0.00003229393,0.00001491793,0.00006598265,0.00005843298],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0001592219,0.00008915857,0.100252,0.00006042963,0.00007170845,0.0003992092,0.0002211328,0.8825038,0.009710411,0.001167854,0.0003248843,0.0050401],"study_design_scores_gemma":[0.00009912714,0.00008072472,0.08157495,0.00002274987,0.00004547599,0.00007437589,0.0007312011,0.9140143,0.00213202,0.0005161588,0.0006609941,0.00004799458],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9977914,0.00007401221,0.0003180202,0.00007465574,0.000004231032,0.00000643089,0.0001606438,0.00002628552,0.001544262],"genre_scores_gemma":[0.9995385,0.0000402697,0.0001509523,0.00000646703,6.769441e-7,0.000002131933,0.00004824076,0.000004207367,0.0002085415],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2444663,"threshold_uncertainty_score":0.491812,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2130154173","doi":"10.1111/j.1468-8123.2008.00237.x","title":"What do aqueous geothermometers really tell us?","year":2009,"lang":"en","type":"article","venue":"Geofluids","topic":"Geothermal Energy Systems and Applications","field":"Energy","cited_by":44,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada; St. Francis Xavier University","funders":"","keywords":"Geology","authors":[{"name":"Grant Ferguson","is_ca":true},{"name":"Stephen E. Grasby","is_ca":true},{"name":"Sarah Hindle","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009478589536024186,"gpt":0.2278990310315567,"spread":0.2184204414955325,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006583884,0.001017716,0.001730806,0.001698087,0.0007042613,0.005673673,0.0009997092,0.004125263,0.004482327],"category_scores_gemma":[0.02579485,0.0008876701,0.0007695356,0.001671702,0.005311003,0.01231484,0.001353018,0.003738411,0.003184154],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001085144,"about_ca_system_score_gemma":0.0008975929,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002480325,"about_ca_topic_score_gemma":0.001708383,"domain_scores_codex":[0.9973117,0.001236881,0.0002126571,0.0003807362,0.0006810335,0.0001770082],"domain_scores_gemma":[0.9876865,0.006808984,0.001809393,0.0008611517,0.002318159,0.0005157596],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","study_design_scores_codex":[0.001555212,0.0005172969,0.1388628,0.005519302,0.001214569,0.0006022977,0.001533111,0.006162143,0.03483609,0.06364956,0.07141861,0.674129],"study_design_scores_gemma":[0.0002202869,0.001511416,0.05647643,0.004995932,0.0008790108,0.00312951,0.009622539,0.01225942,0.05191575,0.4414773,0.4167217,0.0007906032],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"genre_codex":"review","genre_gemma":"review","genre_scores_codex":[0.1435917,0.5431253,0.07615964,0.1869108,0.01339093,0.0001276134,0.003557251,0.000943887,0.03219286],"genre_scores_gemma":[0.7349752,0.1747325,0.02859157,0.03999242,0.008558869,0.0002006176,0.00114538,0.000425391,0.01137827],"genre_candidate":"review","genre_consensus":"review","teacher_disagreement_score":0.006583884,"threshold_uncertainty_score":0.0348193,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1711073548","doi":"10.1111/gfl.12003","title":"Fracture mineralization and fluid flow evolution: an example from Ordovician–Devonian carbonates, southwestern Ontario, Canada","year":2012,"lang":"en","type":"article","venue":"Geofluids","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Waterloo; University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Dolomite; Geology; Fluid inclusions; Ordovician; Geochemistry; Devonian; Diagenesis; Dolomitization; Meteoric water; Calcite; Petrography; Anhydrite; Evaporite; Hydrothermal circulation; Sedimentary rock; Paleontology; Structural basin; Gypsum","authors":[{"name":"Omid H. Ardakani","is_ca":true},{"name":"Ihsan S. Al-Aasm","is_ca":true},{"name":"Mario Coniglio","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01388932046625781,"gpt":0.1895283431767472,"spread":0.1756390227104894,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001968309,0.0002850411,0.0002413186,0.002665951,0.002927307,0.001111757,0.0006226561,0.0002813935,0.001399408],"category_scores_gemma":[0.0005656672,0.000235848,0.0002037601,0.004870358,0.0007592132,0.0001869859,0.0004474227,0.000224699,0.0001773032],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.02049657,"about_ca_system_score_gemma":0.01316686,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9949312,"about_ca_topic_score_gemma":0.9989502,"domain_scores_codex":[0.9997289,0.00001074944,0.00001478529,0.00005149421,0.0001088912,0.00008516397],"domain_scores_gemma":[0.9990832,0.00004013268,0.00009397777,0.00002063042,0.0006445488,0.0001174882],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000120138,0.00002944259,0.9645721,0.0001092566,0.00005560575,0.0009490695,0.005920827,0.0003547925,0.006927719,0.0002798827,0.001438204,0.01924288],"study_design_scores_gemma":[0.000002202438,0.000005752275,0.9956589,0.00001104155,0.000008587581,0.00008584645,0.001463699,0.0001505451,0.0002463922,0.00001340825,0.002348755,0.000004796466],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9924744,0.0007554512,0.0001517826,0.0001438479,0.000004714746,0.00003457021,0.002194276,0.00001686079,0.00422414],"genre_scores_gemma":[0.9946737,0.0005529256,0.0005103836,0.00004471641,0.00000293401,0.00001121923,0.001021662,0.000009270027,0.00317307],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02049657,"threshold_uncertainty_score":0.1487137,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1987926773","doi":"10.1046/j.1468-8123.2001.11002.x","title":"FT‐IR measurements of petroleum fluid inclusions: methane, <i>n</i>‐alkanes and carbon dioxide quantitative analysis","year":2001,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":44,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Université Laval","funders":"","keywords":"Methane; Alkane; Fluid inclusions; Chemistry; Carbon dioxide; Analytical Chemistry (journal); Petroleum; Carbon fibers; Mineralogy; Hydrocarbon; Geology; Environmental chemistry; Materials science; Organic chemistry; Quartz","authors":[{"name":"Jacques Pironon","is_ca":false},{"name":"Richard Thiéry","is_ca":false},{"name":"Mοhamed Ayt Ougougdal","is_ca":true},{"name":"Stéphane Teinturier","is_ca":false},{"name":"Georges Beaudoin","is_ca":true},{"name":"F. Walgenwitz","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02542091258169094,"gpt":0.2565937428564665,"spread":0.2311728302747756,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001331769,0.000264929,0.000116151,0.0003689697,0.0002513502,0.0001928331,0.00024541,0.000152427,0.0009016366],"category_scores_gemma":[0.000272508,0.00009991126,0.00007181738,0.0002438663,0.0002191777,0.0001671189,0.0001111673,0.0001491109,0.0002818486],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0004342035,"about_ca_system_score_gemma":0.0002624349,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02005906,"about_ca_topic_score_gemma":0.02751785,"domain_scores_codex":[0.999891,0.000008598468,0.000003470324,0.00002070954,0.00006115049,0.00001503506],"domain_scores_gemma":[0.9999007,0.00001951215,0.00001393915,0.000005004802,0.00004931622,0.00001143768],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0000378467,0.000007019087,0.001118623,0.00001898917,0.000002661174,0.00002078019,0.00002901301,0.0001208638,0.9960437,0.00002749601,0.00003441102,0.002538654],"study_design_scores_gemma":[0.000002716481,0.00004792574,0.014428,0.000003070895,0.000006400021,0.00007647141,0.0000526295,0.002807085,0.9816484,0.00002757385,0.0008933045,0.00000635813],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9772469,0.0002682959,0.01910797,0.00002485771,0.000007491256,0.00002517986,0.0007117137,0.0002825509,0.002325011],"genre_scores_gemma":[0.9846451,0.0001756316,0.01226077,0.00001200096,0.000002399317,0.00002757222,0.0005565558,0.00003157088,0.00228859],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02005906,"threshold_uncertainty_score":0.03988457,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1811157683","doi":"10.1111/j.1468-8123.2010.00295.x","title":"Fluids associated with hydrothermal dolomitization in St. George Group, western Newfoundland, Canada","year":2010,"lang":"en","type":"article","venue":"Geofluids","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Alberta; Memorial University of Newfoundland","funders":"Natural Resources Canada","keywords":"Dolomitization; Geology; Dolomite; Diagenesis; Geochemistry; Petrography; Hydrothermal circulation; Fluid inclusions; Paleozoic; Paleontology; Structural basin","authors":[{"name":"James Conliffe","is_ca":true},{"name":"Karem Azmy","is_ca":true},{"name":"Sarah A. Gleeson","is_ca":true},{"name":"Denis Lavoie","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005084634645659163,"gpt":0.1670344250221531,"spread":0.1619497903764939,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001279405,0.0003108635,0.000165493,0.00201246,0.001926093,0.0009021298,0.0004266399,0.0002459881,0.00211894],"category_scores_gemma":[0.0002787372,0.0001973549,0.000140156,0.001786856,0.0007833723,0.0002726475,0.000554309,0.0002113386,0.0002610738],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.01706817,"about_ca_system_score_gemma":0.01436634,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9871032,"about_ca_topic_score_gemma":0.9960424,"domain_scores_codex":[0.9998178,0.000005012383,0.000008074465,0.0000401746,0.00005412821,0.0000748903],"domain_scores_gemma":[0.9995645,0.00001993022,0.00007949122,0.000007402683,0.0002449938,0.00008369788],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001844061,0.00005006087,0.930206,0.0001767693,0.0000661005,0.001432574,0.002501901,0.0008249183,0.0335526,0.000338518,0.003502938,0.02716312],"study_design_scores_gemma":[0.000005256016,0.00001845934,0.9907962,0.00002950424,0.00001811961,0.0002053758,0.001750807,0.0003622453,0.002205436,0.000021067,0.004575716,0.00001185189],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.992955,0.0005583597,0.0001345286,0.0002013605,0.000009072348,0.00003116813,0.002161081,0.00003786574,0.003911523],"genre_scores_gemma":[0.9944666,0.0004381141,0.0005491407,0.0001095074,0.000005386154,0.00001081056,0.001242557,0.00001020085,0.003167796],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01706817,"threshold_uncertainty_score":0.1238388,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2167619301","doi":"10.1111/gfl.12132","title":"Can argillaceous formations isolate nuclear waste? Insights from isotopic, noble gas, and geochemical profiles","year":2015,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia; University of Ottawa; University of Saskatchewan","funders":"","keywords":"Geology; Groundwater; Radioactive waste; Diffusion; Oil shale; Geochemistry; Earth science; Geotechnical engineering; Chemistry; Paleontology","authors":[{"name":"M. Jim Hendry","is_ca":true},{"name":"D. Kip Solomon","is_ca":false},{"name":"Mark Person","is_ca":false},{"name":"Leonard I. Wassenaar","is_ca":false},{"name":"W. Payton Gardner","is_ca":false},{"name":"Ian D. Clark","is_ca":true},{"name":"K. Ulrich Mayer","is_ca":true},{"name":"Takanori Kunimaru","is_ca":false},{"name":"Kotaro Nakata","is_ca":false},{"name":"Takuma Hasegawa","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01006498308239255,"gpt":0.1914256770178165,"spread":0.181360693935424,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002933952,0.0003029278,0.0003440295,0.001012589,0.0006664383,0.001118827,0.0002597453,0.0005152951,0.0005996939],"category_scores_gemma":[0.0005496801,0.0001796908,0.0001066713,0.0006248566,0.0009653065,0.0008018241,0.0005915947,0.0003106099,0.0001388747],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000546922,"about_ca_system_score_gemma":0.0004649123,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01095937,"about_ca_topic_score_gemma":0.01648682,"domain_scores_codex":[0.9998598,0.00001868617,0.000009252707,0.00003435569,0.00003403697,0.00004377246],"domain_scores_gemma":[0.9998773,0.00002463348,0.00004537211,0.000008371764,0.00002490394,0.00001936802],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0005233328,0.0001179931,0.2510531,0.0002155138,0.00005550662,0.000975402,0.001629001,0.003832253,0.7135299,0.003465591,0.0001659912,0.02443624],"study_design_scores_gemma":[0.0000555433,0.0003947238,0.7042102,0.00006016722,0.00006382925,0.001369795,0.006046478,0.01262214,0.2581322,0.002692834,0.01428111,0.00007089337],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9982071,0.0001336883,0.0006640275,0.00004230682,0.000003061132,0.000004762923,0.00004503641,0.000009852399,0.0008901233],"genre_scores_gemma":[0.9990398,0.00007990183,0.0006302685,0.00001284322,0.000001877441,0.000001835933,0.00003846964,0.000004132497,0.0001908306],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01095937,"threshold_uncertainty_score":0.02179116,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2130893527","doi":"10.1111/j.1468-8123.2010.00280.x","title":"Downward hydrocarbon migration predicted from numerical modeling of fluid overpressure in the Paleozoic Anticosti Basin, eastern Canada","year":2010,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":38,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Institut National de la Recherche Scientifique; Geological Survey of Canada; University of Regina","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Shell Canada","keywords":"Overpressure; Geology; Ordovician; Paleozoic; Structural basin; Source rock; Basin modelling; Dolomitization; Buoyancy; Petrology; Geochemistry; Geomorphology; Paleontology","authors":[{"name":"Guoxiang Chi","is_ca":true},{"name":"Denis Lavoie","is_ca":true},{"name":"R. Bertrand","is_ca":true},{"name":"M.-K. Lee","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006767600115363329,"gpt":0.190047962451985,"spread":0.1832803623366216,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001279048,0.000528915,0.0002647137,0.000644702,0.0013877,0.001206857,0.0009267022,0.0009674177,0.001527123],"category_scores_gemma":[0.0006447342,0.0004102263,0.00048666,0.0006508975,0.0009107323,0.0002619709,0.0004213812,0.0004802404,0.000129846],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.01107941,"about_ca_system_score_gemma":0.008671271,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9339396,"about_ca_topic_score_gemma":0.8439469,"domain_scores_codex":[0.9999266,0.000005461764,0.000003324098,0.00001618225,0.00001778758,0.00003064471],"domain_scores_gemma":[0.9998333,0.00003559134,0.000019436,0.000008228604,0.00006122387,0.0000420686],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00006576939,0.0000388008,0.03446386,0.00001644829,0.00002415159,0.0001540179,0.0001065911,0.9603072,0.001943155,0.0006689819,0.0001985357,0.002012458],"study_design_scores_gemma":[0.00002805295,0.00001751679,0.01541324,0.00000663028,0.00001357728,0.00001419037,0.0001104753,0.9834351,0.0004969321,0.0001094854,0.0003392092,0.00001566928],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9958172,0.00004296517,0.0006855886,0.00007086658,0.000005011284,0.00001168606,0.0003160794,0.00005358082,0.002996964],"genre_scores_gemma":[0.9988231,0.00003999166,0.0004101611,0.000008201934,9.567361e-7,0.000007827057,0.0001164299,0.000007117854,0.0005861237],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06606042,"threshold_uncertainty_score":0.1328989,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2037494018","doi":"10.1111/j.1468-8123.2006.00123.x","title":"Chlorine stable isotope ratios as tracer for pore‐water advection rates in a submarine gas‐hydrate field: implication for hydrate concentration","year":2006,"lang":"en","type":"article","venue":"Geofluids","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Waterloo; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Advection; Clathrate hydrate; Pore water pressure; Seawater; Hydrate; Mineralogy; Chemistry; Oceanography","authors":[{"name":"Reinhard Hesse","is_ca":true},{"name":"P.K. Egeberg","is_ca":false},{"name":"Shaun K. Frape","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006895140307860343,"gpt":0.233662889502424,"spread":0.2267677491945637,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000333248,0.0002464036,0.0001918894,0.0006336989,0.0001848212,0.0004870224,0.0004023241,0.0004157751,0.0002930385],"category_scores_gemma":[0.0005083074,0.0002599134,0.0001760646,0.0002981736,0.0003038968,0.0003174125,0.0001718197,0.0002359407,0.00009922707],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0006529039,"about_ca_system_score_gemma":0.0002115061,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01949884,"about_ca_topic_score_gemma":0.009095423,"domain_scores_codex":[0.9999001,0.00001593157,0.000005304301,0.00003710502,0.00002838309,0.00001311886],"domain_scores_gemma":[0.9996887,0.0001369055,0.00005964212,0.00001812397,0.00006620202,0.00003043985],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0006185989,0.0000522769,0.3264938,0.00004713947,0.00004992799,0.0001711405,0.0001678276,0.002443202,0.6619289,0.0001884518,0.00008155571,0.00775716],"study_design_scores_gemma":[0.00004241507,0.0002581227,0.6396252,0.00001003865,0.00004894135,0.0001166638,0.0002046468,0.05026932,0.3086067,0.0001700257,0.0006146292,0.0000334071],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9985284,0.00007095205,0.0008865299,0.00001794601,0.00000172869,0.000004710125,0.000150861,0.00003857659,0.0003002945],"genre_scores_gemma":[0.9991781,0.0000272884,0.0005814801,0.000008029029,7.243679e-7,0.000004639557,0.00008933106,0.000005727608,0.0001045904],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01949884,"threshold_uncertainty_score":0.03877068,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2160978328","doi":"10.1111/gfl.12148","title":"Reactive transport and thermo‐hydro‐mechanical coupling in deep sedimentary basins affected by glaciation cycles: model development, verification, and illustrative example","year":2015,"lang":"en","type":"article","venue":"Geofluids","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of New Brunswick; University of British Columbia","funders":"Consejo Nacional de Investigaciones Científicas y Técnicas","keywords":"Geology; Sedimentary rock; Structural basin; Deglaciation; Sedimentary basin; Glacial period; Hydraulic conductivity; Evaporite; Groundwater flow; Groundwater; Geochemistry; Geomorphology; Petrology; Geotechnical engineering; Soil science; Aquifer","authors":[{"name":"Sergio A. Bea","is_ca":false},{"name":"K. Ulrich Mayer","is_ca":true},{"name":"Kerry T. B. MacQuarrie","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02705191518840022,"gpt":0.2465663801788441,"spread":0.2195144649904438,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004559035,0.000774833,0.0008105754,0.0006901027,0.0008786864,0.0009591756,0.001257044,0.002198836,0.003388125],"category_scores_gemma":[0.001437147,0.0003975087,0.000988071,0.0006721267,0.00124106,0.0004514343,0.001168331,0.001038041,0.0001793921],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001414342,"about_ca_system_score_gemma":0.001470882,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.08368883,"about_ca_topic_score_gemma":0.03342371,"domain_scores_codex":[0.9998537,0.00004557443,0.000009521123,0.0000224561,0.0000240656,0.00004461526],"domain_scores_gemma":[0.999183,0.00046107,0.00008971517,0.00005044564,0.0001486982,0.00006714583],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00002242438,0.00003178387,0.001256836,0.00001287934,0.000006563753,0.00006594374,0.00001357707,0.9973909,0.0002673716,0.0004875828,0.00008031428,0.0003637484],"study_design_scores_gemma":[0.000023028,0.00001517527,0.0003098178,0.000002307563,0.000003740664,0.000003820387,0.00001582415,0.9992545,0.000135615,0.0001588108,0.00007376195,0.00000349839],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9707034,0.0001381749,0.01514902,0.0003795259,0.00003991127,0.0001130453,0.00117876,0.0004052029,0.01189302],"genre_scores_gemma":[0.9932913,0.00006428587,0.004603763,0.00005440139,0.000008868325,0.00009897168,0.0002847832,0.00003978565,0.001553836],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08368883,"threshold_uncertainty_score":0.1664034,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2102729179","doi":"10.1046/j.1468-8123.2001.00014.x","title":"Computing geochemical mass transfer and water/rock ratios in submarine hydrothermal systems: implications for estimating the vigour of convection","year":2001,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":33,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Hydrothermal circulation; Seawater; Geology; Fluid dynamics; Submarine; Convection; Flow (mathematics); Quartz; Mass transfer; Flow velocity; Basalt; Hydrogeology; Mechanics; Geotechnical engineering; Oceanography; Geochemistry; Seismology","authors":[{"name":"Peter Alt‐Epping","is_ca":true},{"name":"Leslie Smith","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01240429216572107,"gpt":0.228536013406174,"spread":0.2161317212404529,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005809133,0.0005697569,0.0005206413,0.001078241,0.0003300419,0.0008705648,0.0006360542,0.0005692855,0.0004730611],"category_scores_gemma":[0.002870027,0.0003591264,0.0004828304,0.0004996765,0.0002890531,0.0008797512,0.0004124555,0.0003039304,0.0001637007],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007777761,"about_ca_system_score_gemma":0.0006368379,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01558632,"about_ca_topic_score_gemma":0.01217362,"domain_scores_codex":[0.9998711,0.00003704684,0.000008509389,0.00003801334,0.00003284933,0.0000124833],"domain_scores_gemma":[0.9992699,0.0004628541,0.00006717063,0.00004580836,0.00009817033,0.00005605652],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.000236822,0.0001246438,0.07633276,0.00008708778,0.000136575,0.0001096773,0.0001291074,0.803249,0.03022845,0.001037666,0.0002857414,0.08804246],"study_design_scores_gemma":[0.000006215477,0.00001953726,0.004073936,0.000002517745,0.00000529438,0.000007840549,0.00001809726,0.9921159,0.003257528,0.0004057057,0.00008027053,0.000007058483],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.7654251,0.0002101382,0.231294,0.0001139654,0.00001449472,0.00006018304,0.0002554087,0.001630577,0.0009961289],"genre_scores_gemma":[0.9076205,0.00006512466,0.09183154,0.000009370919,0.00000933612,0.00003182397,0.0001096214,0.00005926558,0.0002634092],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01558632,"threshold_uncertainty_score":0.0309912,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2768301781","doi":"10.1155/2017/7508484","title":"Geology and Metallogenesis of the Sediment-Hosted Cu-Ag Deposit of Tizert (Igherm Inlier, Anti-Atlas Copperbelt, Morocco)","year":2017,"lang":"en","type":"article","venue":"Geofluids","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"Université du Québec à Montréal","keywords":"Geology; Bornite; Chalcocite; Geochemistry; Mineralization (soil science); Pyrite; Chalcopyrite; Galena; Covellite; Arenite; Sedimentary rock; Sphalerite; Mineralogy; Clastic rock; Copper","authors":[{"name":"Abdellah Oummouch","is_ca":false},{"name":"Abderrahim Essaifi","is_ca":false},{"name":"Rachid Zayane","is_ca":false},{"name":"Othmane Maddi","is_ca":false},{"name":"Mohamed Zouhair","is_ca":false},{"name":"Lhou Maacha","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01244427448946844,"gpt":0.2071533361547908,"spread":0.1947090616653224,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001197851,0.0002587099,0.0001674855,0.001965728,0.0006460567,0.000522965,0.0002411187,0.0002632637,0.001271385],"category_scores_gemma":[0.0002213495,0.0001634505,0.0001390464,0.001092874,0.0004538759,0.000135228,0.0003377255,0.0001059497,0.0003126904],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00202603,"about_ca_system_score_gemma":0.0004128766,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.1259801,"about_ca_topic_score_gemma":0.1735781,"domain_scores_codex":[0.9999006,0.00001056431,0.000005527883,0.0000237008,0.00001706704,0.00004266331],"domain_scores_gemma":[0.9999198,0.000006537423,0.00003282362,0.000004387319,0.00002072782,0.0000157897],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000386605,0.00006613792,0.9236506,0.0000915382,0.00007847798,0.005150679,0.002977995,0.0009633028,0.03546636,0.0003977387,0.0006272245,0.03014335],"study_design_scores_gemma":[0.000003271465,0.00001753252,0.9986405,0.00000408342,0.000003873737,0.0002353016,0.000220409,0.0001057445,0.0002452106,0.00001078727,0.0005115391,0.000001799744],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.999234,0.0001085839,0.00001439214,0.00001576498,0.000001571288,0.000002149963,0.0001267448,0.000002825919,0.0004939707],"genre_scores_gemma":[0.9993172,0.00006698522,0.00005338419,0.000006798297,0.000003693721,0.000002199297,0.0001229897,0.00000157309,0.000425221],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1259801,"threshold_uncertainty_score":0.2504937,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2921680684","doi":"10.1155/2019/7401304","title":"High Diversity in Iron Cycling Microbial Communities in Acidic, Iron-Rich Water of the Pyhäsalmi Mine, Finland","year":2019,"lang":"en","type":"article","venue":"Geofluids","topic":"Metal Extraction and Bioleaching","field":"Engineering","cited_by":32,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"First Quantum Minerals; Academy of Finland","keywords":"Archaea; Acid mine drainage; 16S ribosomal RNA; Biology; Iron bacteria; Ferrous; Nitrospira; Microbial population biology; Microorganism; Phylum; Euryarchaeota; Bioleaching; Bacteria; Environmental chemistry; Microbiology; Chemistry","authors":[{"name":"Malin Bomberg","is_ca":false},{"name":"Jarno Mäkinen","is_ca":false},{"name":"Marja Salo","is_ca":false},{"name":"Päivi Kinnunen","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01163665471595209,"gpt":0.1945641494370293,"spread":0.1829274947210772,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002703392,0.0003725851,0.0006274511,0.001226147,0.001051588,0.0008537685,0.0002825328,0.0006268215,0.0003977646],"category_scores_gemma":[0.0003691774,0.0003978892,0.0003388463,0.0009036142,0.000635803,0.0005287767,0.0009180496,0.0001716873,0.0001403623],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0003204645,"about_ca_system_score_gemma":0.0005351324,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006606286,"about_ca_topic_score_gemma":0.006989603,"domain_scores_codex":[0.9997334,0.00002042563,0.00002965606,0.000107348,0.00006065707,0.00004848536],"domain_scores_gemma":[0.9998755,0.00002960563,0.0000315701,0.000004752071,0.00003075059,0.00002773737],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0006667347,0.000106054,0.5812235,0.0003949971,0.0001406708,0.001725695,0.007768836,0.00058625,0.3901995,0.0001163257,0.0001114181,0.01696001],"study_design_scores_gemma":[0.00001739284,0.0001419965,0.9903121,0.00002461834,0.00002970887,0.000552933,0.002449432,0.0003992954,0.005241626,0.00006910643,0.0007396443,0.00002224566],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9994459,0.0001344115,0.00007761926,0.00001053884,0.000001336946,0.000007112233,0.0001071322,0.000002126838,0.0002138808],"genre_scores_gemma":[0.9988495,0.0001484523,0.0004220453,0.00002120876,0.000005903395,0.00002576056,0.0002561779,0.000001990917,0.0002688768],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.006606286,"threshold_uncertainty_score":0.01313567,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1983846167","doi":"10.1111/gfl.12009","title":"Synchrotron XRF and <scp>XANES</scp> investigation of uranium speciation and element distribution in fluid inclusions from unconformity‐related uranium deposits","year":2012,"lang":"en","type":"article","venue":"Geofluids","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":32,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Fluid inclusions; Uranium; XANES; Geology; Unconformity; Chemistry; Uranium ore; Quartz; Mineralogy; Analytical Chemistry (journal); Inclusion (mineral); Mineral redox buffer; Synchrotron; Geochemistry; Spectroscopy; Environmental chemistry; Materials science; Metallurgy; Sedimentary rock; Mantle (geology)","authors":[{"name":"Antonin Richard","is_ca":false},{"name":"Jean Cauzid","is_ca":false},{"name":"‪Michel Cathelineau","is_ca":false},{"name":"Marie‐Christine Boiron","is_ca":false},{"name":"Julien Mercadier","is_ca":false},{"name":"Michel Cuney","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.00817281749705797,"gpt":0.2007403445505588,"spread":0.1925675270535009,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001672329,0.0002236031,0.0001671189,0.0008428383,0.0005230535,0.0003572365,0.0002795231,0.0002138031,0.001187847],"category_scores_gemma":[0.000154335,0.0001488781,0.000127299,0.0005936185,0.0003792247,0.0001471185,0.0001966816,0.0001233616,0.0001624209],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0003909807,"about_ca_system_score_gemma":0.0002353435,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0247377,"about_ca_topic_score_gemma":0.03702838,"domain_scores_codex":[0.9998549,0.00001142564,0.000007220041,0.00003886855,0.00006435103,0.00002310164],"domain_scores_gemma":[0.9999129,0.00001351553,0.00001699155,0.00000772021,0.00004035603,0.00000847723],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0001096552,0.00001108118,0.009378145,0.00004175512,0.00001360451,0.0002054412,0.0003289827,0.0002786816,0.9868224,0.00006604355,0.00006701236,0.00267718],"study_design_scores_gemma":[0.00001668255,0.0001220813,0.4529419,0.00001488728,0.00002657685,0.0006709383,0.001076719,0.004545059,0.5363186,0.00008567485,0.004159779,0.00002105303],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9977763,0.00008389491,0.0009773354,0.00001362521,0.000001441691,0.000008287026,0.000363314,0.00002925017,0.0007466445],"genre_scores_gemma":[0.9960542,0.00006696501,0.002243409,0.00001091859,0.000001865282,0.000008793931,0.0005111538,0.00001534362,0.001087446],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0247377,"threshold_uncertainty_score":0.04918748,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2745499881","doi":"10.1155/2017/6740892","title":"The Early Cambrian Mianyang-Changning Intracratonic Sag and Its Control on Petroleum Accumulation in the Sichuan Basin, China","year":2017,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":32,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"National Key Research and Development Program of China","keywords":"Geology; Sichuan basin; Paleontology; Structural basin; Period (music); Source rock; Geochemistry","authors":[{"name":"Shugen Liu","is_ca":false},{"name":"Bin Deng","is_ca":false},{"name":"Luba Jansa","is_ca":true},{"name":"Yong Zhong","is_ca":false},{"name":"Wei Sun","is_ca":false},{"name":"Jinmin Song","is_ca":false},{"name":"Guozhi Wang","is_ca":false},{"name":"Juan Wu","is_ca":false},{"name":"Zhiwu Li","is_ca":false},{"name":"Yanhong Tian","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01561971972126521,"gpt":0.2479760675792512,"spread":0.232356347857986,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001165126,0.0001695205,0.0001574971,0.0009671818,0.0007047585,0.0004886276,0.0001902191,0.0001680612,0.000613295],"category_scores_gemma":[0.0002015094,0.0001265345,0.0001449465,0.001530932,0.0006372377,0.0002417183,0.0004419837,0.0001125478,0.00003886204],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007451472,"about_ca_system_score_gemma":0.00102616,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.06926163,"about_ca_topic_score_gemma":0.1232139,"domain_scores_codex":[0.9999218,0.000007791776,0.00000609927,0.0000197195,0.00001599177,0.00002865627],"domain_scores_gemma":[0.9998931,0.00001227191,0.00003410735,0.00000718612,0.00002072151,0.00003261064],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004709113,0.00002510377,0.9759846,0.0000340631,0.0000385888,0.001043335,0.00245478,0.000771175,0.008599325,0.0006239852,0.0001126509,0.01026527],"study_design_scores_gemma":[9.523939e-7,0.000007634276,0.9988956,0.000002249856,0.000004916055,0.00004793237,0.0004199119,0.0002080426,0.000148523,0.00003824692,0.0002238317,0.000002012641],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9994822,0.00004965246,0.00002744864,0.00001353327,6.096923e-7,0.000001435973,0.00002119928,0.000001799833,0.0004022019],"genre_scores_gemma":[0.9997227,0.00004811147,0.00002730135,0.000004695184,0.000001444699,0.000001409115,0.00003709716,7.622413e-7,0.0001566273],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06926163,"threshold_uncertainty_score":0.137717,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2018660585","doi":"10.1111/j.1468-8123.2008.00233.x","title":"Stable–unstable flow of geothermal fluids in fractured rock","year":2009,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geothermal gradient; Geology; Thermal diffusivity; Thermal conductivity; Fracture (geology); Mechanics; Thermal conduction; Hydraulic conductivity; Matrix (chemical analysis); Fluid dynamics; Geotechnical engineering; Flow (mathematics); Materials science; Geophysics; Thermodynamics; Soil science; Composite material; Physics","authors":[{"name":"Thomas Graf","is_ca":false},{"name":"René Therrien","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006875948256788974,"gpt":0.2090850603337832,"spread":0.2022091120769942,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002303057,0.0001866804,0.0002738958,0.0004330342,0.0003825894,0.0005519497,0.0003182649,0.0003779705,0.0003978814],"category_scores_gemma":[0.0009065783,0.0001440108,0.0003609118,0.0002331261,0.0008264958,0.0003275318,0.0003394104,0.00020404,0.00004194813],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007247553,"about_ca_system_score_gemma":0.0005269056,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006630941,"about_ca_topic_score_gemma":0.003396364,"domain_scores_codex":[0.9999077,0.00002044139,0.000006451281,0.00001480156,0.00002682564,0.00002371168],"domain_scores_gemma":[0.9997022,0.0001509777,0.00005998152,0.00002077763,0.00003832883,0.00002777031],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0003232417,0.0001339261,0.02518992,0.00008176829,0.00006182303,0.0006520093,0.000380948,0.8148836,0.1452226,0.006781751,0.0001418754,0.00614646],"study_design_scores_gemma":[0.00002654555,0.00007735364,0.005510109,0.000005288744,0.000007148099,0.00005480039,0.00006915333,0.9709737,0.02205888,0.001078677,0.0001219166,0.00001637407],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9964586,0.00003323979,0.003032975,0.00002116021,0.000002163797,0.000006907253,0.00003219668,0.00002073381,0.0003920474],"genre_scores_gemma":[0.9991028,0.0000138778,0.0007909671,0.000002315408,6.368726e-7,0.000005427354,0.00001687852,0.000002394691,0.00006462064],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.006630941,"threshold_uncertainty_score":0.01318467,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2111971301","doi":"10.1111/j.1468-8123.2006.00160.x","title":"Fluid inclusion constraints on the origin of the brines responsible for Pb–Zn mineralization at Pine Point and coarse non‐saddle and saddle dolomite formation in southern Northwest Territories","year":2006,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":30,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Alberta","funders":"University of Alberta","keywords":"Dolomite; Geology; Fluid inclusions; Sphalerite; Paragenesis; Geochemistry; Halite; Devonian; Galena; Mineralogy; Pyrite; Calcite; Mineralization (soil science); Dolomitization; Quartz; Gypsum; Facies; Paleontology; Structural basin; Metamorphic rock","authors":[{"name":"Sarah A. Gleeson","is_ca":true},{"name":"William Turner","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01009068784651871,"gpt":0.2105329118887705,"spread":0.2004422240422518,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001284114,0.0001784885,0.0003346258,0.0009490019,0.0009057153,0.001230707,0.0002874084,0.0002174785,0.00149827],"category_scores_gemma":[0.0004108064,0.0003196455,0.0001440202,0.0004307326,0.0008927662,0.0004185478,0.0008489225,0.0002025378,0.000165686],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001441801,"about_ca_system_score_gemma":0.0009455867,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.1348286,"about_ca_topic_score_gemma":0.1729627,"domain_scores_codex":[0.9998729,0.00000852721,0.000008861908,0.00003362968,0.00003549449,0.00004055248],"domain_scores_gemma":[0.9998665,0.00002695187,0.00003975407,0.000005170926,0.00003596283,0.00002556648],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004589773,0.00008367483,0.6263037,0.00008127571,0.00004527481,0.0008735955,0.002727678,0.001487223,0.3600611,0.0010058,0.00009025206,0.006781463],"study_design_scores_gemma":[0.000009995217,0.00003061259,0.9879757,0.00001095959,0.000009712841,0.00009767614,0.002014624,0.001988586,0.00705886,0.0001070912,0.0006885525,0.00000764866],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9993198,0.00002483379,0.00006693629,0.000006841815,4.879402e-7,0.000002450955,0.0000401201,0.000002438912,0.000536044],"genre_scores_gemma":[0.9996144,0.00002324961,0.00007490713,0.000002312408,6.591325e-7,0.000001996567,0.00006491562,0.000002594506,0.0002150212],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8651714,"threshold_uncertainty_score":0.2680877,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1963889001","doi":"10.1046/j.1468-8123.2002.00029.x","title":"Petroleum infiltration of high‐grade basement, South Norway: Pressure‐Temperature‐time‐composition (<i>P–T–t–X</i>) constraints","year":2002,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":29,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"Natural Environment Research Council; Norges Forskningsråd","keywords":"Fluid inclusions; Quartz; Geology; Mineralogy; Geochemistry; Petroleum; Sedimentary rock; Basement; Inclusion (mineral); Petrology","authors":[{"name":"I. A. Munz","is_ca":false},{"name":"B. W. D. Yardley","is_ca":false},{"name":"Sarah A. Gleeson","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008017649257222944,"gpt":0.187698710627922,"spread":0.1796810613706991,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001695449,0.0001932497,0.0002054617,0.0004764441,0.0003451134,0.0006214627,0.0001876974,0.0001597257,0.0007074084],"category_scores_gemma":[0.0003630221,0.000233336,0.0002198641,0.0005028261,0.0005041035,0.0002691659,0.0003878614,0.0001773979,0.0001286655],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001082314,"about_ca_system_score_gemma":0.0005771929,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.1004803,"about_ca_topic_score_gemma":0.10654,"domain_scores_codex":[0.9998448,0.00001425452,0.00001274509,0.00003910372,0.00004301451,0.00004603645],"domain_scores_gemma":[0.9997582,0.00005029333,0.00009721531,0.00001091573,0.00004786929,0.00003547119],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0005430404,0.00005164128,0.8535534,0.0001380508,0.00005925045,0.001142776,0.0007777522,0.00627869,0.1303778,0.000278534,0.0001315862,0.006667393],"study_design_scores_gemma":[0.000009429809,0.00005987156,0.9932534,0.000009615474,0.00001223506,0.0001572886,0.0002789306,0.002262762,0.003408127,0.00004928988,0.0004913043,0.000007725191],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9991374,0.00006234007,0.0001205583,0.000008058043,0.000001230631,0.000001797458,0.0001255878,0.000004703537,0.0005381928],"genre_scores_gemma":[0.9996686,0.00003647077,0.00008950413,0.000003535611,8.432297e-7,0.000001600679,0.0001169241,0.000002089447,0.00008043538],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1004803,"threshold_uncertainty_score":0.1997908,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1999769042","doi":"10.1046/j.1468-8123.2001.00016.x","title":"Application of boron isotopes to the understanding of fluid–rock interactions in a hydrothermally stimulated oil reservoir in the Alberta Basin, Canada","year":2001,"lang":"en","type":"article","venue":"Geofluids","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Calgary","funders":"Arizona State University; U.S. Department of Energy","keywords":"Geology; Geochemistry; Isotopes of boron; Aquifer; Groundwater; Diagenesis; Isotope; Geochemical modeling; Boron; Fractionation; Mineralogy; Chemistry","authors":[{"name":"Lynda B. Williams","is_ca":false},{"name":"Michael E. Wieser","is_ca":true},{"name":"Jon Fennell","is_ca":false},{"name":"Ian Hutcheon","is_ca":true},{"name":"R. L. Hervig","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01700355662927038,"gpt":0.2249594641621543,"spread":0.2079559075328839,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002024209,0.0002397559,0.000266844,0.001500588,0.002108479,0.0008741023,0.0008513701,0.0004645379,0.0007895304],"category_scores_gemma":[0.0002307495,0.0002766847,0.0002041444,0.001410417,0.0005942686,0.0002957585,0.000387285,0.000273038,0.0001063486],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.01312235,"about_ca_system_score_gemma":0.007090202,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9642522,"about_ca_topic_score_gemma":0.9767213,"domain_scores_codex":[0.9998358,0.000008181518,0.000005697704,0.0000319403,0.00006805424,0.00005025337],"domain_scores_gemma":[0.9998474,0.00002044856,0.00001393888,0.000002876802,0.00008917565,0.00002610557],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001209154,0.0001710468,0.6485728,0.0003578578,0.000158929,0.003024517,0.004244201,0.01518974,0.2828487,0.001193622,0.0007882101,0.04224132],"study_design_scores_gemma":[0.00003331005,0.0001127447,0.9346903,0.00004219581,0.00005922199,0.0003439141,0.006551046,0.02662801,0.0262477,0.000382551,0.004867211,0.00004180759],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9955499,0.000484314,0.0007863176,0.0001140965,0.000004397399,0.00002376851,0.0003991959,0.00003011549,0.002607923],"genre_scores_gemma":[0.9975993,0.0001798515,0.001201105,0.00002346196,0.000001368881,0.000004854596,0.0001286672,0.000004897815,0.00085637],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03574783,"threshold_uncertainty_score":0.09520978,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3003770415","doi":"10.1155/2020/5387183","title":"Generation of Synthetic Density Log Data Using Deep Learning Algorithm at the Golden Field in Alberta, Canada","year":2020,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":28,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Korea Institute of Energy Technology Evaluation and Planning; National Research Foundation of Korea; Ministry of Trade, Industry and Energy; Korea Institute of Geoscience and Mineral Resources; National Research Foundation","keywords":"Field (mathematics); Artificial neural network; Well logging; Geology; Algorithm; Deep learning; Computer science; Point (geometry); Data mining; Preprocessor; Artificial intelligence; Geophysics; Mathematics","authors":[{"name":"Sungil Kim","is_ca":false},{"name":"Kwang Hyun Kim","is_ca":false},{"name":"Baehyun Min","is_ca":false},{"name":"Jung-Tek Lim","is_ca":false},{"name":"Kyungbook Lee","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03566398208406647,"gpt":0.2298924848443752,"spread":0.1942285027603087,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002761456,0.0007596231,0.000306143,0.001075163,0.0005246799,0.0005066431,0.001235548,0.0005508675,0.001674366],"category_scores_gemma":[0.0009197372,0.0003045616,0.0004127535,0.001238482,0.0005782896,0.0004170523,0.0004938857,0.0005178541,0.0004034906],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.002880048,"about_ca_system_score_gemma":0.002981437,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.4558803,"about_ca_topic_score_gemma":0.5269918,"domain_scores_codex":[0.99978,0.00001532054,0.00000803861,0.00003985939,0.0001102873,0.00004662733],"domain_scores_gemma":[0.9996295,0.00005188532,0.00001878395,0.00003173265,0.0002222331,0.0000457819],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.0003253924,0.0003400772,0.04790271,0.0001631504,0.00004732551,0.001265708,0.0001869327,0.8608321,0.006578673,0.001574355,0.01211084,0.06867275],"study_design_scores_gemma":[0.00002887562,0.00002559012,0.01377961,0.00001180162,0.000008145932,0.00003915006,0.0001712152,0.980807,0.002876517,0.0005745567,0.001651468,0.00002613768],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9231554,0.0002324185,0.04935502,0.0005269547,0.0001467945,0.0002140974,0.01457112,0.004101948,0.007696273],"genre_scores_gemma":[0.9585594,0.0001235775,0.025874,0.00004653938,0.00001105346,0.0000730053,0.01241743,0.0001175176,0.002777485],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5441197,"threshold_uncertainty_score":0.9064535,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3102524275","doi":"10.1155/2020/8849444","title":"Research on the Pore Evolution of Sandstone in Cold Regions under Freeze-Thaw Weathering Cycles Based on NMR","year":2020,"lang":"en","type":"article","venue":"Geofluids","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"McGill University","funders":"Fundamental Research Funds for the Central Universities; Central South University; Natural Science Foundation of Hainan Province; National Natural Science Foundation of China","keywords":"Porosity; Weathering; Geology; Mineralogy; Materials science; Geomorphology; Geotechnical engineering","authors":[{"name":"Zheng Pan","is_ca":false},{"name":"Keping Zhou","is_ca":false},{"name":"Rugao Gao","is_ca":true},{"name":"Zhen Jiang","is_ca":false},{"name":"Chun Yang","is_ca":false},{"name":"Feng Gao","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.1409035454721252,"gpt":0.3064628681241308,"spread":0.1655593226520056,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001476184,0.0001505376,0.0001961035,0.0005106141,0.0002497633,0.0002579481,0.0001507223,0.0001830438,0.0003335464],"category_scores_gemma":[0.0001829853,0.0001331884,0.0002039815,0.0003288776,0.0003261316,0.0004519178,0.0001718178,0.0001912605,0.00004157941],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0002033672,"about_ca_system_score_gemma":0.0001340832,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005155151,"about_ca_topic_score_gemma":0.006574703,"domain_scores_codex":[0.999933,0.000004635788,0.000003935325,0.00001975632,0.0000213056,0.00001727099],"domain_scores_gemma":[0.9998766,0.00001695447,0.00003290878,0.000007355318,0.00004540359,0.0000208013],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.00009366153,0.00001945744,0.03391705,0.00008818469,0.00002893769,0.0002174379,0.0003214901,0.0005978007,0.9609202,0.0001209803,0.00004405331,0.003630705],"study_design_scores_gemma":[0.00001189765,0.0001906605,0.6968843,0.00001440891,0.00008441351,0.0003727107,0.000770316,0.007544599,0.2925623,0.0001750719,0.001350395,0.00003890615],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9990971,0.0001207179,0.0004676608,0.000006278619,0.000001942764,0.000003549982,0.00009685639,0.00000750225,0.000198482],"genre_scores_gemma":[0.9991416,0.0001081963,0.0004014185,0.000007438869,0.000001796731,0.000005329325,0.0001157445,0.00000357574,0.0002148586],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.005155151,"threshold_uncertainty_score":0.01025027,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2785709093","doi":"10.1155/2018/5854829","title":"Origins of Chalcocite Defined by Copper Isotope Values","year":2018,"lang":"lv","type":"article","venue":"Geofluids","topic":"Metal Extraction and Bioleaching","field":"Engineering","cited_by":25,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Government of Northwest Territories","funders":"Pennsylvania State University; University of Arizona","keywords":"Geology; Materials science","authors":[{"name":"Ryan Mathur","is_ca":false},{"name":"Hendrik Falck","is_ca":true},{"name":"Е. В. Белогуб","is_ca":false},{"name":"Jack E. Milton","is_ca":true},{"name":"Melissa L. Wilson","is_ca":false},{"name":"Andrew L. Rose","is_ca":false},{"name":"Wayne Powell","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01542100496638681,"gpt":0.2502823761080855,"spread":0.2348613711416987,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001627041,0.000251986,0.0002707364,0.003826719,0.0006390078,0.001818593,0.0003398217,0.0004141953,0.002259618],"category_scores_gemma":[0.0006019705,0.0001976049,0.0001541189,0.003681385,0.0008916754,0.0004360069,0.0005636648,0.0002776389,0.0004387502],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001901789,"about_ca_system_score_gemma":0.0008220244,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02897497,"about_ca_topic_score_gemma":0.0393656,"domain_scores_codex":[0.9997497,0.00001497091,0.00001725576,0.00005905181,0.00009693583,0.00006213153],"domain_scores_gemma":[0.9996653,0.00004682647,0.00006008144,0.00002817067,0.0001697205,0.00002994151],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.001523318,0.00004986224,0.288655,0.0004405995,0.0001346033,0.00371009,0.002750272,0.001833674,0.6234304,0.01206301,0.001164899,0.06424426],"study_design_scores_gemma":[0.00005225103,0.0001677619,0.6181635,0.0001246,0.00009359625,0.001856892,0.004468369,0.002220566,0.3250601,0.005604473,0.04210728,0.00008049526],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9817036,0.00111994,0.001262934,0.00009389929,0.00001336819,0.00001786448,0.0008871497,0.00006485799,0.01483646],"genre_scores_gemma":[0.9940514,0.0007682645,0.001016916,0.00002279777,0.000005945498,0.00001331067,0.0006602853,0.00003479439,0.003426254],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02897497,"threshold_uncertainty_score":0.05761266,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2168236881","doi":"10.1046/j.1468-8123.2002.00039.x","title":"Three‐dimensional geometry, ore distribution and time‐integrated mass transfer through the quartz–tourmaline–gold vein network of the Sigma deposit (Abitibi belt, Canada)","year":2002,"lang":"en","type":"article","venue":"Geofluids","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":24,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Geometry; Shear zone; Vein; Quartz; Tourmaline; Echelon formation; Mineralogy; Petrology; Geochemistry; Fault (geology); Seismology; Tectonics; Paleontology; Mathematics","authors":[{"name":"Paolo Garofalo","is_ca":false},{"name":"Stephan K. Matthäi","is_ca":false},{"name":"Christoph A. Heinrich","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009022735878037771,"gpt":0.1749020760435457,"spread":0.1658793401655079,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007924135,0.0002940286,0.0002183861,0.001177,0.0003441604,0.001004379,0.00045509,0.0003197939,0.001950873],"category_scores_gemma":[0.0003144089,0.0003179962,0.0003420891,0.001309309,0.0005226884,0.0001752957,0.0002668842,0.0002057491,0.0003240516],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00212968,"about_ca_system_score_gemma":0.002398733,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.4747053,"about_ca_topic_score_gemma":0.4580366,"domain_scores_codex":[0.9999235,0.000002948992,0.000002033441,0.00002229552,0.00002773323,0.0000215385],"domain_scores_gemma":[0.999874,0.00001764542,0.00002298442,0.00001313629,0.00005124135,0.0000209248],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","study_design_scores_codex":[0.0006366742,0.0002128686,0.3902594,0.0002120019,0.0002763508,0.00140559,0.001694105,0.430757,0.1066183,0.001783235,0.002294095,0.06385028],"study_design_scores_gemma":[0.00004019847,0.00004624028,0.6281504,0.00002356273,0.00004950649,0.0002844979,0.0005787542,0.3596475,0.008612572,0.0003578961,0.002131873,0.00007698137],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9935532,0.00005303034,0.002788293,0.00003860715,0.000003067792,0.00001602014,0.001972674,0.0002430203,0.001332136],"genre_scores_gemma":[0.9953184,0.00005876097,0.002433755,0.00000510707,0.000001491777,0.000007995092,0.00143364,0.0000287655,0.0007120484],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4747053,"threshold_uncertainty_score":0.9438844,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2152361390","doi":"10.1111/gfl.12133","title":"Constraining groundwater flow in the glacial drift and saginaw aquifers in the Michigan Basin through helium concentrations and isotopic ratios","year":2015,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université du Québec à Montréal","funders":"National Science Foundation","keywords":"Aquifer; Geology; Groundwater recharge; Glacial period; Groundwater; Hydrology (agriculture); Structural basin; Groundwater flow; Dilution; Geomorphology","authors":[{"name":"Tao Wen","is_ca":false},{"name":"M. Clara Castro","is_ca":false},{"name":"Chris M. Hall","is_ca":false},{"name":"Daniele L. Pinti","is_ca":true},{"name":"Kyger C. Lohmann","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02366095417582515,"gpt":0.2242239576681915,"spread":0.2005630034923664,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001001617,0.0002118245,0.00016944,0.0002969871,0.0003198247,0.0004185933,0.0002444357,0.0003361329,0.0005667233],"category_scores_gemma":[0.00025513,0.0002524203,0.0002115035,0.0003413238,0.0002390952,0.0003084933,0.0002690076,0.0001186131,0.00003941626],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.001141663,"about_ca_system_score_gemma":0.0006137287,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.09670147,"about_ca_topic_score_gemma":0.1761883,"domain_scores_codex":[0.9999745,0.000007168757,0.000001246485,0.000006991722,0.000002987351,0.000007164034],"domain_scores_gemma":[0.9999317,0.00003215517,0.00001049228,0.000003319186,0.000008542413,0.00001374744],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002841852,0.00009439396,0.5476751,0.00004088028,0.0001638005,0.0002681726,0.0001883208,0.4022763,0.0346493,0.0008978768,0.000447756,0.01301392],"study_design_scores_gemma":[0.00005758792,0.00009115612,0.200866,0.0000107552,0.00005835572,0.00002959564,0.0002630415,0.7922155,0.005016941,0.000716341,0.0006460594,0.00002851241],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9994684,0.00001004379,0.0002236363,0.00002090521,3.496555e-7,9.278712e-7,0.00006546732,0.00000969845,0.0002006726],"genre_scores_gemma":[0.9995796,0.00001319,0.0002513048,0.000003752727,4.139454e-7,0.000001604938,0.00008340146,0.00000184674,0.00006498317],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.09670147,"threshold_uncertainty_score":0.1922772,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2029324660","doi":"10.1111/gfl.12123","title":"Fluid environment for preservation of pore spaces in a deep dolomite reservoir","year":2014,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":24,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"National Natural Science Foundation of China; University of Calgary","keywords":"Dolomite; Geology; Carbonate; Meteoric water; Geochemistry; Hydrothermal circulation; Paleozoic; Carbonate minerals; Ordovician; Carbonate rock; Fluid inclusions; Mineralogy; Paleontology; Sedimentary rock; Chemistry","authors":[{"name":"Dongya Zhu","is_ca":false},{"name":"Qingqiang Meng","is_ca":false},{"name":"Zhijun Jin","is_ca":false},{"name":"Wenxuan Hu","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01116912248788977,"gpt":0.209359836013956,"spread":0.1981907135260663,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001113955,0.0001778477,0.0002455038,0.001089769,0.0005061928,0.0006756397,0.0002629416,0.0002674777,0.001008825],"category_scores_gemma":[0.0003324204,0.0001530395,0.000137042,0.0006067863,0.0005134957,0.0005011647,0.0005376386,0.0001728065,0.00006573494],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0007994678,"about_ca_system_score_gemma":0.0006698798,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.009549598,"about_ca_topic_score_gemma":0.01007037,"domain_scores_codex":[0.9998665,0.000008137864,0.00001059313,0.00003370382,0.00004007982,0.00004095187],"domain_scores_gemma":[0.9998642,0.00001613638,0.00004282077,0.000007851253,0.00003306144,0.00003597146],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0002563119,0.00004310135,0.1320287,0.00009382838,0.00002618371,0.0008117533,0.0004688369,0.004874549,0.8507521,0.0007817407,0.0001089925,0.009753869],"study_design_scores_gemma":[0.00005614011,0.00035638,0.6743481,0.00002620047,0.00005195827,0.0009881029,0.00179924,0.03319525,0.283535,0.001207365,0.004352776,0.00008343971],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9990866,0.00006234719,0.0004303642,0.00001134133,0.000001467063,0.000003440236,0.00008282465,0.0000434781,0.0002781299],"genre_scores_gemma":[0.9995802,0.0000163044,0.000255532,0.000001772877,5.149142e-7,0.000001967707,0.00005712679,0.000002324995,0.00008425162],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.009549598,"threshold_uncertainty_score":0.01898801,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2106088419","doi":"10.1111/j.1468-8123.2005.00100.x","title":"Barite–pyrite mineralization of the Wiesbaden thermal spring system, Germany: a 500‐kyr record of geochemical evolution","year":2005,"lang":"en","type":"article","venue":"Geofluids","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"McGill University","funders":"Natural Environment Research Council","keywords":"Geology; Pyrite; Massif; Geochemistry; Mineralization (soil science); Hydrothermal circulation; Geothermal gradient; δ34S; Aquifer; Hot spring; Mineralogy; Groundwater; Paleontology; Fluid inclusions; Soil science","authors":[{"name":"Thomas Wagner","is_ca":true},{"name":"Thomas Kirnbauer","is_ca":false},{"name":"Adrian J. Boyce","is_ca":false},{"name":"Anthony E. Fallick","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006101955833184998,"gpt":0.169699100058779,"spread":0.163597144225594,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001954006,0.0002670565,0.0002341939,0.001469523,0.0003007499,0.0006602776,0.0001921731,0.0002344331,0.0009014124],"category_scores_gemma":[0.0001957311,0.0002650137,0.0001273609,0.0009977738,0.0002789653,0.0004227814,0.000471791,0.0001950613,0.000311182],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0008409062,"about_ca_system_score_gemma":0.0002778529,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.03939187,"about_ca_topic_score_gemma":0.05730463,"domain_scores_codex":[0.9998913,0.000006431162,0.000009236865,0.00004822608,0.00001930841,0.00002554847],"domain_scores_gemma":[0.9998879,0.000008552896,0.00004777552,0.00001130676,0.00002223277,0.00002206472],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0005052419,0.00009028462,0.8059981,0.0003183993,0.0003549277,0.0006524075,0.001490793,0.00278859,0.1422064,0.0004944546,0.001194244,0.04390609],"study_design_scores_gemma":[0.000005591481,0.00002261751,0.9965038,0.00001020368,0.00001613639,0.00006966821,0.00006098154,0.0002544445,0.001206275,0.00001754477,0.001827329,0.000005433261],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9971666,0.0005868922,0.0001858432,0.00001881897,0.000002880651,0.000005076015,0.001099455,0.00002515244,0.0009094061],"genre_scores_gemma":[0.9979943,0.0003056478,0.0003157977,0.00001035024,0.000004018998,0.000005252931,0.001042517,0.000006347464,0.0003157139],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03939187,"threshold_uncertainty_score":0.07832515,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2170972939","doi":"10.1111/gfl.12051","title":"Boiling as a mechanism for colour zonations observed at the <scp>B</scp>yrud emerald deposit, <scp>E</scp>idsvoll, <scp>N</scp>orway: fluid inclusion, stable isotope and <scp>A</scp>r–<scp>A</scp>r studies","year":2013,"lang":"en","type":"article","venue":"Geofluids","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University; Simon Fraser University","funders":"","keywords":"Emerald; Pegmatite; Halite; Fluid inclusions; Geology; Quartz; Geochemistry; Mineralogy; Boiling; Inclusion (mineral); Chemistry; Geomorphology; Structural basin","authors":[{"name":"Lara Loughrey","is_ca":true},{"name":"Daniel D. Marshall","is_ca":true},{"name":"Peter M. Ihlen","is_ca":false},{"name":"Peter Tom Jones","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02579363819427104,"gpt":0.2281042143458517,"spread":0.2023105761515807,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001091785,0.0001304552,0.00009800619,0.0009896061,0.0003310342,0.0005539564,0.0002596101,0.0003189624,0.001304043],"category_scores_gemma":[0.0001727854,0.0002217067,0.0001164085,0.0002772194,0.0004594268,0.0002829932,0.0003242667,0.0002303775,0.0002619185],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0005168387,"about_ca_system_score_gemma":0.0001788162,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01058772,"about_ca_topic_score_gemma":0.01219119,"domain_scores_codex":[0.9999334,0.00000482331,0.000005179174,0.00002098226,0.00002048001,0.00001523093],"domain_scores_gemma":[0.9999125,0.00001021133,0.00002459873,0.000007787447,0.00003371868,0.00001118973],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.00016546,0.00001771104,0.06744745,0.00005001605,0.00001810979,0.0003238767,0.0003896341,0.0002830199,0.9261235,0.0003617085,0.0001359611,0.004683526],"study_design_scores_gemma":[0.00001854487,0.00006973084,0.6882901,0.0000139948,0.0000214698,0.0004421256,0.0003836374,0.00231757,0.3045388,0.0001697933,0.003719413,0.00001477232],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9961931,0.00008693748,0.0005991336,0.0000290345,0.000003094016,0.000006836147,0.0001567847,0.00004919731,0.002875991],"genre_scores_gemma":[0.9982072,0.00003263546,0.0004503335,0.00001112052,0.000001283772,0.000003673471,0.00007082021,0.00001308668,0.001209763],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01058772,"threshold_uncertainty_score":0.02105218,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3112286583","doi":"10.1155/2020/8880545","title":"Characterization of the Dynamic Imbibition Displacement Mechanism in Tight Sandstone Reservoirs Using the NMR Technique","year":2020,"lang":"en","type":"article","venue":"Geofluids","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":22,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"China University of Petroleum, Beijing; Natural Science Foundation of Shaanxi Province; National Natural Science Foundation of China","keywords":"Imbibition; Displacement (psychology); Permeability (electromagnetism); Materials science; Geology; Geotechnical engineering; Chemistry","authors":[{"name":"Liangbin Dou","is_ca":false},{"name":"Min Yang","is_ca":true},{"name":"Hui Gao","is_ca":false},{"name":"Dongxing Jiang","is_ca":false},{"name":"Chenglu Liu","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01176336228783833,"gpt":0.2212533130117698,"spread":0.2094899507239315,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001641435,0.0001820445,0.0002002524,0.0004159031,0.0001834367,0.0001526233,0.0001708949,0.0001997651,0.0003508574],"category_scores_gemma":[0.0001884734,0.0001256168,0.00008098794,0.000327643,0.000264801,0.0003998005,0.000224965,0.0001610693,0.0000503452],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001935104,"about_ca_system_score_gemma":0.000299413,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004419773,"about_ca_topic_score_gemma":0.006741639,"domain_scores_codex":[0.9999347,0.000005082974,0.000003704067,0.00001724583,0.00002067185,0.00001865004],"domain_scores_gemma":[0.9999198,0.00001837085,0.00002645953,0.000005776782,0.0000187781,0.00001079042],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.00004242211,0.00001105423,0.008140258,0.00004872902,0.000003042661,0.00009161323,0.0001055558,0.0004439114,0.9858304,0.0001173812,0.000008828656,0.005156814],"study_design_scores_gemma":[0.00001618475,0.0005102705,0.197745,0.00001296796,0.00003079662,0.0002798375,0.0005524954,0.01687458,0.7821143,0.0002822526,0.001542854,0.00003846366],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9956429,0.0001157799,0.00380771,0.00001004771,0.000001676324,0.000008895274,0.00003372084,0.00001780276,0.0003614954],"genre_scores_gemma":[0.9970393,0.00007034535,0.002582728,0.000004521708,0.000001242883,0.000008530043,0.00002341297,0.000002440631,0.0002675819],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.004419773,"threshold_uncertainty_score":0.008788109,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1997195218","doi":"10.1111/gfl.12131","title":"Groundwater age, brine migration, and large‐scale solute transport in the <scp>A</scp>lberta <scp>B</scp>asin, <scp>C</scp>anada","year":2015,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"University of Alberta","funders":"U.S. Department of Energy","keywords":"Geology; Aquifer; Hydrogeology; Groundwater; Dilution; Residence time (fluid dynamics); Structural basin; Sedimentary rock; Hydrology (agriculture); Geochemistry; Brine; Groundwater flow; Geomorphology; Chemistry; Geotechnical engineering","authors":[{"name":"Ipsita Gupta","is_ca":false},{"name":"Alicia M. Wilson","is_ca":false},{"name":"Benjamin J. Rostron","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01406610842184752,"gpt":0.2027584018907006,"spread":0.1886922934688531,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001917053,0.0002778166,0.0001689866,0.0002924137,0.0006217071,0.0008127572,0.0005586341,0.0004620483,0.001058126],"category_scores_gemma":[0.0004007278,0.0002868248,0.0004001117,0.0003045668,0.0004203224,0.0002201225,0.0002755472,0.0003143541,0.00008225208],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00636152,"about_ca_system_score_gemma":0.002848211,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8451083,"about_ca_topic_score_gemma":0.8274511,"domain_scores_codex":[0.999962,0.000007255729,0.000001469935,0.000009094528,0.000007846989,0.00001236768],"domain_scores_gemma":[0.9998904,0.00003841202,0.00001158043,0.000006557712,0.00002447387,0.00002855225],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","study_design_scores_codex":[0.0003308735,0.000193201,0.2208265,0.0000333345,0.0001343765,0.0002262908,0.0001902966,0.7586331,0.01409398,0.001000929,0.0004683618,0.003868772],"study_design_scores_gemma":[0.00009225643,0.0001054249,0.1825617,0.000008044166,0.00005385104,0.00002981798,0.00025589,0.8133509,0.002405369,0.0003981745,0.0007054417,0.0000332487],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9992268,0.00001583946,0.0002279478,0.00002416918,0.000001245081,0.000003803624,0.0001160554,0.00001508015,0.0003690928],"genre_scores_gemma":[0.9990771,0.00002163653,0.0003449146,0.000007644522,5.76527e-7,0.000004020551,0.0001405554,0.000003968658,0.0003995818],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1548917,"threshold_uncertainty_score":0.3116078,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2158537855","doi":"10.1046/j.1468-8123.2003.00056.x","title":"Strontium isotopic characterization of the Palmottu hydrosystem (Finland): water–rock interaction and geochemistry of groundwaters","year":2003,"lang":"en","type":"article","venue":"Geofluids","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Waterloo","funders":"Bureau de Recherches Géologiques et Minières; U.S. Geological Survey; Université de Strasbourg; European Commission","keywords":"Plagioclase; Isotopes of strontium; Strontium; Geology; Weathering; Geochemistry; Lithology; Feldspar; Mineralogy; Biotite; Meteoric water; Groundwater; Chemistry; Quartz","authors":[{"name":"Philippe Négrel","is_ca":false},{"name":"Joël Casanova","is_ca":false},{"name":"R. Blomqvist","is_ca":false},{"name":"Juha Kaija","is_ca":false},{"name":"Shaun K. Frape","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.00557862015841353,"gpt":0.1682771766555558,"spread":0.1626985564971422,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001385494,0.000242697,0.0002790358,0.001258351,0.0007692302,0.0005034311,0.0002541591,0.0003759812,0.0006627442],"category_scores_gemma":[0.0002129846,0.0002364988,0.0001689032,0.001147618,0.0004176132,0.0003247286,0.0004600675,0.0001053026,0.0001477685],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0005038379,"about_ca_system_score_gemma":0.0004362288,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02147032,"about_ca_topic_score_gemma":0.02088615,"domain_scores_codex":[0.9998779,0.00001067141,0.000006275855,0.00004722655,0.00002834014,0.00002942429],"domain_scores_gemma":[0.9999382,0.00001342119,0.0000149185,0.000004007748,0.00001560562,0.00001384883],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0006842351,0.0001165861,0.6192874,0.0002695316,0.0001399171,0.001541271,0.002285495,0.002769467,0.3354788,0.0003147048,0.0002463163,0.03686636],"study_design_scores_gemma":[0.00002615008,0.0001738732,0.9581109,0.00002008083,0.00006489903,0.0004756103,0.001403424,0.004660543,0.03280329,0.0002086019,0.002024829,0.00002786988],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9988592,0.00008906992,0.0002806201,0.000006424284,0.000001060158,0.000006687542,0.0002575292,0.00001073583,0.0004887755],"genre_scores_gemma":[0.9992247,0.00003865535,0.0003705576,0.000003778619,0.000001137489,0.000007019116,0.0001644426,0.000002579317,0.0001870989],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02147032,"threshold_uncertainty_score":0.04269069,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2316373037","doi":"10.1111/gfl.12173","title":"Freezing and melting behaviors of H<sub>2</sub>O‐NaCl‐CaCl<sub>2</sub> solutions in fused silica capillaries and glass‐sandwiched films: implications for fluid inclusion studies","year":2016,"lang":"en","type":"article","venue":"Geofluids","topic":"Calcium Carbonate Crystallization and Inhibition","field":"Materials Science","cited_by":21,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Regina","funders":"Natural Sciences and Engineering Research Council of Canada; Chinese Academy of Sciences","keywords":"Fluid inclusions; Crystallization; Inclusion (mineral); Metastability; Melt inclusions; Nucleation; Mineralogy; Phase (matter); Geology; Analytical Chemistry (journal); Materials science; Chemical engineering; Chemistry; Quartz; Metallurgy; Olivine; Chromatography","authors":[{"name":"Haixia Chu","is_ca":true},{"name":"Guoxiang Chi","is_ca":true},{"name":"I‐M. Chou","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0296362683634721,"gpt":0.274688026149171,"spread":0.2450517577856989,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000227763,0.0002797033,0.000200155,0.0002253353,0.0001811414,0.0003072828,0.0003343414,0.0002810653,0.0004921697],"category_scores_gemma":[0.0003870495,0.0001860096,0.0001419164,0.0001295319,0.0003518957,0.000261739,0.0001631254,0.0003567939,0.0000838643],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000318897,"about_ca_system_score_gemma":0.000206379,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002025634,"about_ca_topic_score_gemma":0.002891702,"domain_scores_codex":[0.9998796,0.00001170048,0.000008147709,0.00003020919,0.00004626251,0.00002408489],"domain_scores_gemma":[0.999773,0.00008174925,0.0000560933,0.00001046296,0.00005447886,0.00002424592],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.00002113503,0.000003508561,0.0002491549,0.00001337493,0.000002293202,0.00001961892,0.00002467565,0.00005572795,0.9992985,0.00001281732,0.000003351569,0.0002959837],"study_design_scores_gemma":[0.000002434321,0.00005001119,0.002684049,0.000002158582,0.000005159033,0.00003344254,0.00004000167,0.0007724386,0.9963175,0.000009740468,0.00007911053,0.00000403127],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9973731,0.0003094334,0.001913299,0.00001766965,0.000005636783,0.00001388971,0.00005968197,0.00002733187,0.0002800052],"genre_scores_gemma":[0.9960433,0.0002803499,0.003217695,0.00001359115,0.000003837311,0.0000149296,0.00005146777,0.00001217457,0.0003626802],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.002025634,"threshold_uncertainty_score":0.004027724,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}