{"meta":{"query_hash":"2977ec0f3b98","filters":{"venue":"Journal of Structural Geology"},"cohort_total":97,"direct_labels_cover":0,"predictions_cover":97,"exported":97,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/2977ec0f3b98","api":"https://metacan.xera.ac/api/v1/cohort?venue=Journal+of+Structural+Geology"},"results":[{"id":"W1477399939","doi":"10.1016/j.jsg.2015.08.012","title":"Geological constraints on the dynamic emplacement of cone-sheets – The Ardnamurchan cone-sheet swarm, NW Scotland","year":2015,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Chicoutimi","funders":"Vetenskapsrådet","keywords":"Geology; Sill; Volcano; Classification of discontinuities; Stress field; Seismology; Outcrop; Geometry; Petrology; Geomorphology; Physics","score_opus":0.027227035617317145,"score_gpt":0.24122325797259922,"score_spread":0.21399622235528207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1477399939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971198,0.000045304147,0.000067592904,0.000066650726,0.0000035224489,0.0000039541046,0.00013198443,0.000003356573,0.0025578556],"genre_scores_gemma":[0.9996537,0.000030080002,0.000046417856,0.000008749214,0.0000029224507,0.000002028162,0.000117079726,0.00000273,0.00013624322],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99960345,0.00005112534,0.000038457438,0.000052406514,0.00009950862,0.00015501394],"domain_scores_gemma":[0.9984085,0.00029732753,0.0005199141,0.00011770184,0.0004242533,0.00023228061],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006232867,0.0002150392,0.00041472353,0.0015750036,0.0017868596,0.0021692107,0.0007002118,0.00038403296,0.003310018],"category_scores_gemma":[0.0040328573,0.00029096808,0.0002477494,0.0018489265,0.0018574648,0.000733983,0.0018069536,0.00039840638,0.0003119543],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046727635,0.00007025197,0.9616622,0.00007271054,0.00006596616,0.0012634645,0.0067311227,0.0031643186,0.009140111,0.002319237,0.0006687147,0.014374614],"study_design_scores_gemma":[0.000010644269,0.00003543984,0.9949319,0.000012945299,0.000010424304,0.00008874231,0.002331826,0.00062960136,0.000096280826,0.0001393294,0.001704669,0.000008317545],"about_ca_topic_score_codex":0.191318,"about_ca_topic_score_gemma":0.38908207,"teacher_disagreement_score":0.191318,"about_ca_system_score_codex":0.0020385028,"about_ca_system_score_gemma":0.0018066148,"threshold_uncertainty_score":0.38040882},"labels":[],"label_agreement":null},{"id":"W1968895964","doi":"10.1016/j.jsg.2004.06.015","title":"Extensional fault arrays in strike-slip and transtension","year":2004,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Transtension; Geology; Strike-slip tectonics; Seismology; Echelon formation; Extensional definition; Shear (geology); Structural basin; Slip (aerodynamics); Fault (geology); Transpression; Petrology; Tectonics; Sinistral and dextral; Geomorphology","score_opus":0.011833827666957565,"score_gpt":0.2048392707366126,"score_spread":0.19300544306965503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968895964","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841034,0.000056900117,0.00030117505,0.000026471009,0.000002081814,9.799323e-7,0.000046410285,0.0000030795984,0.0011526325],"genre_scores_gemma":[0.9993894,0.000024643961,0.00007767598,0.0000028281252,0.000005263496,9.923981e-7,0.000027866128,0.0000021588514,0.00046916836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997565,0.000095758,0.000022137378,0.000050342387,0.00003427047,0.000040945954],"domain_scores_gemma":[0.9912174,0.0067355535,0.00077779754,0.00017629354,0.00062207045,0.00047097227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075781415,0.00017892165,0.00025427542,0.0009230289,0.00032197847,0.000998205,0.0002598084,0.0003304966,0.0046310984],"category_scores_gemma":[0.006889612,0.00025333164,0.00017595298,0.001236654,0.00080064265,0.0015192522,0.0005835618,0.0004398903,0.0003855474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012449715,0.00017578734,0.94851255,0.000030617462,0.0000705578,0.00037399438,0.0012284634,0.01346374,0.0059459927,0.009505226,0.00033809495,0.019110011],"study_design_scores_gemma":[0.00003352655,0.00014310343,0.9609317,0.000016898626,0.000052627995,0.00038629197,0.0013399505,0.02936894,0.00055932766,0.006728451,0.00042102538,0.000018188095],"about_ca_topic_score_codex":0.0034260626,"about_ca_topic_score_gemma":0.00957553,"teacher_disagreement_score":0.0046310984,"about_ca_system_score_codex":0.00031532595,"about_ca_system_score_gemma":0.000254353,"threshold_uncertainty_score":0.0154925585},"labels":[],"label_agreement":null},{"id":"W1975976361","doi":"10.1016/j.jsg.2012.10.008","title":"From intra-oceanic subduction to arc accretion and arc-continent collision: Insights from the structural evolution of the Río San Juan metamorphic complex, northern Hispaniola","year":2012,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Ministerio de Ciencia e Innovación","keywords":"Blueschist; Geology; Metamorphism; Greenschist; Geochemistry; Eclogite; Subduction; Metamorphic facies; Tectonite; Ophiolite; Shear zone; Petrology; Paleontology; Tectonics; Facies; Structural basin","score_opus":0.013078916723811871,"score_gpt":0.20216020810720076,"score_spread":0.1890812913833889,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975976361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99654204,0.00039974737,0.00004630303,0.00015908162,0.00000281868,0.0000029258638,0.000059747905,0.0000030585686,0.0027842124],"genre_scores_gemma":[0.9990546,0.0004101693,0.000048057736,0.000019749017,0.00000466596,0.0000024721198,0.000096244294,0.0000048335974,0.00035916705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999101,0.000011832685,0.0000052949176,0.000027515649,0.000014631412,0.00003061185],"domain_scores_gemma":[0.9997571,0.00006830232,0.000067528854,0.000015273132,0.00004705021,0.000044693305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022266759,0.00018775498,0.00021977015,0.0009467703,0.0009905961,0.0015747284,0.0004833466,0.00052909454,0.003517562],"category_scores_gemma":[0.0012015622,0.00022929607,0.00023849326,0.00152146,0.0012044413,0.00073511177,0.0011490318,0.00045584983,0.00019363107],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004569514,0.000081254126,0.94533545,0.00011578426,0.00014896711,0.0013741219,0.01248489,0.0022078643,0.0062365867,0.0032096186,0.00043354486,0.027914986],"study_design_scores_gemma":[0.0000070697865,0.00002040183,0.993266,0.00002023839,0.00002436434,0.000115049115,0.0041382383,0.0005702848,0.00013616284,0.00046412816,0.0012328933,0.000005370809],"about_ca_topic_score_codex":0.101367645,"about_ca_topic_score_gemma":0.17964377,"teacher_disagreement_score":0.101367645,"about_ca_system_score_codex":0.001331592,"about_ca_system_score_gemma":0.001313261,"threshold_uncertainty_score":0.20155525},"labels":[],"label_agreement":null},{"id":"W1977299116","doi":"10.1016/j.jsg.2006.04.005","title":"Kinematic analysis of radial structures around Irnini Mons, Venus","year":2006,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University; National Aeronautics and Space Administration","keywords":"Geology; Radial stress; Ridge; Compression (physics); Hydroforming; Compressive strength; Stress (linguistics); Extensional definition; Seismology; Geometry; Petrology; Materials science; Tectonics; Deformation (meteorology); Paleontology; Composite material","score_opus":0.007720727242977817,"score_gpt":0.23177596324080024,"score_spread":0.22405523599782243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977299116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919934,0.00014096701,0.0010571376,0.000049007573,0.000011432345,0.000013765601,0.00088539935,0.00009357047,0.0057552145],"genre_scores_gemma":[0.9977361,0.000043893742,0.0007495833,0.0000061367828,0.000006447653,0.0000044596045,0.00076832133,0.000018351931,0.0006667205],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998982,0.000010908138,0.000004270809,0.00003401365,0.000023995492,0.000028569253],"domain_scores_gemma":[0.9997079,0.000028849767,0.00006664774,0.0000290754,0.00009948771,0.000068083566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022263064,0.00030233746,0.00024756853,0.0016373628,0.0005071858,0.00062275113,0.0005318401,0.0002115541,0.001682511],"category_scores_gemma":[0.0008361612,0.00025809498,0.00027343997,0.0013573627,0.00023110067,0.00020192872,0.00049470697,0.0002420066,0.0004312854],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009922365,0.00015501241,0.83820873,0.00009103233,0.00019806885,0.00081582216,0.0011654379,0.058470383,0.041403193,0.0025729476,0.0021857992,0.05374141],"study_design_scores_gemma":[0.000016745338,0.000069833164,0.95954716,0.000019624842,0.000037980346,0.00011388188,0.00036571926,0.03578022,0.0013672038,0.00021479523,0.0024455185,0.00002134592],"about_ca_topic_score_codex":0.06542203,"about_ca_topic_score_gemma":0.10572415,"teacher_disagreement_score":0.06542203,"about_ca_system_score_codex":0.00084514875,"about_ca_system_score_gemma":0.00078781944,"threshold_uncertainty_score":0.13008249},"labels":[],"label_agreement":null},{"id":"W1983486944","doi":"10.1016/j.jsg.2014.07.021","title":"Texture and elastic anisotropy of a mylonitic anorthosite from the Morin Shear Zone (Quebec, Canada)","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministerio de Ciencia e Innovación; Ministerio de Educación, Cultura y Deporte; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Mylonite; Seismic anisotropy; Plagioclase; Granulite; Lineation; Anisotropy; Shear zone; Anorthosite; Gneiss; Mineralogy; Simple shear; Tectonite; Shear (geology); Geophysics; Geochemistry; Petrology; Seismology; Metamorphic rock; Facies; Geomorphology; Mantle (geology); Physics; Optics; Tectonics","score_opus":0.0039159334483658955,"score_gpt":0.16397609225101303,"score_spread":0.16006015880264715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983486944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99607277,0.00017295938,0.00010431248,0.00004464034,0.00000366134,0.000008777606,0.0009522292,0.000009801918,0.0026308233],"genre_scores_gemma":[0.9974572,0.00009139467,0.00013972781,0.000028564406,0.0000019598122,0.0000042651795,0.0005118582,0.0000106302505,0.0017544047],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997923,0.0000061261217,0.000009956298,0.000058985424,0.00006648007,0.000066119035],"domain_scores_gemma":[0.99960893,0.000025785828,0.00003780838,0.000009937133,0.00026021263,0.000057297686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002083514,0.00035724504,0.00032845305,0.0024204543,0.0027024301,0.0011186028,0.00078086363,0.0004914039,0.0028581766],"category_scores_gemma":[0.00038791518,0.00024890245,0.00016909186,0.002545443,0.0009436907,0.00023410725,0.0003592664,0.00028111195,0.0005822678],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013425945,0.00015539081,0.75449437,0.00017639835,0.00017256204,0.0017052756,0.004027407,0.0017197587,0.19651091,0.00049540383,0.0020406977,0.03715928],"study_design_scores_gemma":[0.000009676733,0.000013716183,0.99552935,0.000011278483,0.000018403605,0.00013032256,0.0009255172,0.0005410175,0.0013802276,0.00001470875,0.0014157151,0.00001000061],"about_ca_topic_score_codex":0.97417736,"about_ca_topic_score_gemma":0.9863985,"teacher_disagreement_score":0.02582264,"about_ca_system_score_codex":0.007002867,"about_ca_system_score_gemma":0.004039497,"threshold_uncertainty_score":0.05194938},"labels":[],"label_agreement":null},{"id":"W1990777534","doi":"10.1016/j.jsg.2009.09.006","title":"Structural geology, petrofabrics and magnetic fabrics (AMS, AARM, AIRM)","year":2009,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":281,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"","keywords":"Lineation; Geology; Ellipsoid; Outcrop; Tectonics; Mineralogy; Sedimentary depositional environment; Anisotropy; Geometry; Geochemistry; Seismology; Geodesy; Paleontology; Mathematics","score_opus":0.006884111495717278,"score_gpt":0.22994970989216193,"score_spread":0.22306559839644466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990777534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.744576,0.0709363,0.0036975855,0.0035247933,0.002018536,0.00007007315,0.01689952,0.0004503185,0.15782693],"genre_scores_gemma":[0.89931816,0.01437926,0.0071298815,0.00013010352,0.0006469549,0.000038898248,0.005977635,0.000102055754,0.07227695],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99957603,0.00006816047,0.000047104942,0.000066030894,0.00019569215,0.000047059097],"domain_scores_gemma":[0.99968314,0.000043799755,0.000068166344,0.000032111362,0.00012881888,0.000043943386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00093548564,0.00044011849,0.0003238333,0.003104826,0.00057471934,0.0008083809,0.00035125538,0.00029881133,0.017825348],"category_scores_gemma":[0.0016236542,0.00020632488,0.00027353253,0.004275686,0.00051033235,0.00041218605,0.000658683,0.00040622018,0.0051730606],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00068627886,0.00014006223,0.12534992,0.0005845819,0.000117288044,0.00037446813,0.0006412694,0.0014797506,0.024262227,0.008711114,0.023220876,0.81443214],"study_design_scores_gemma":[0.000019447487,0.00023130071,0.84986585,0.00011471212,0.00007339013,0.0016949578,0.00047548936,0.0005572944,0.0059754136,0.0029447,0.13802114,0.000026269974],"about_ca_topic_score_codex":0.015422915,"about_ca_topic_score_gemma":0.023918046,"teacher_disagreement_score":0.017825348,"about_ca_system_score_codex":0.0006004099,"about_ca_system_score_gemma":0.0006486115,"threshold_uncertainty_score":0.059631705},"labels":[],"label_agreement":null},{"id":"W1990932653","doi":"10.1016/j.jsg.2010.05.006","title":"Tectonic implications for a Cordilleran orogenic base in the Frenchman Cap dome, southeastern Canadian Cordillera","year":2010,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Universidade Estadual da Paraíba","keywords":"Geology; Gneiss; Shear zone; Basement; Tectonics; Socle; Dome (geology); Geomorphology; Seismology; Geochemistry; Paleontology; Metamorphic rock; Inversion (geology)","score_opus":0.012482259556655604,"score_gpt":0.22108742742550144,"score_spread":0.20860516786884584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990932653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9788303,0.0010144436,0.0001381109,0.001358476,0.000022932329,0.000024104833,0.0005797557,0.000022645627,0.018009108],"genre_scores_gemma":[0.9964045,0.0003316973,0.00024935362,0.00008891656,0.000007847655,0.0000053771746,0.0002409401,0.0000054269094,0.0026659493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980766,0.000014553711,0.000008482492,0.000042190622,0.00004414865,0.00008304297],"domain_scores_gemma":[0.999556,0.000032563297,0.000060472754,0.000013641157,0.0002572707,0.00007996499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028845543,0.00030423654,0.00029024025,0.0017942043,0.004075335,0.0019709799,0.00074687443,0.00056380185,0.00838592],"category_scores_gemma":[0.001147653,0.00016122188,0.00021437531,0.0028319587,0.0013889604,0.00036147045,0.00096600753,0.00045215053,0.00031597295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052168354,0.00009459734,0.8771708,0.00016959649,0.00011399664,0.0022177289,0.008619242,0.0038463466,0.00794311,0.012044867,0.0052198335,0.08203814],"study_design_scores_gemma":[0.000026435773,0.000023236273,0.98014414,0.00008759374,0.000044657892,0.00019753528,0.0050843284,0.0018628525,0.00031162635,0.0005224392,0.011676866,0.000018206854],"about_ca_topic_score_codex":0.9871013,"about_ca_topic_score_gemma":0.99570435,"teacher_disagreement_score":0.019852992,"about_ca_system_score_codex":0.019852992,"about_ca_system_score_gemma":0.01552912,"threshold_uncertainty_score":0.14404422},"labels":[],"label_agreement":null},{"id":"W1991516640","doi":"10.1016/j.jsg.2014.12.002","title":"Contrasts in sillimanite deformation in felsic tectonites from anhydrous granulite- and hydrous amphibolite-facies shear zones, western Canadian Shield","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Sillimanite; Geology; Granulite; Tectonite; Shear zone; Geochemistry; Lineation; Dislocation creep; Metamorphic facies; Shear (geology); Deformation mechanism; Felsic; Mineralogy; Petrology; Seismology; Creep; Geomorphology; Composite material; Materials science; Quartz; Facies; Biotite; Mafic; Microstructure","score_opus":0.005415819987153707,"score_gpt":0.17761191142331798,"score_spread":0.17219609143616427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991516640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99838066,0.00007437569,0.000024127834,0.000013974017,9.540787e-7,0.000003419533,0.00035055325,0.000004647222,0.0011473516],"genre_scores_gemma":[0.99926597,0.000040662173,0.000029105928,0.0000074277646,8.003081e-7,0.0000015552968,0.000303784,0.0000027439125,0.00034779252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997819,0.000008067325,0.000013059891,0.00005504453,0.000065593485,0.000076335],"domain_scores_gemma":[0.9995073,0.00003524738,0.000063763684,0.000015874866,0.0002705498,0.00010728342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021383433,0.00034438586,0.0002574275,0.0032541149,0.0020123052,0.0010911525,0.0006639017,0.00036235838,0.002172207],"category_scores_gemma":[0.0004974996,0.00035355994,0.00020762558,0.0023177268,0.0011412427,0.0003126462,0.00058605365,0.00025545075,0.00028887897],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032442872,0.000037437203,0.9630745,0.000046473175,0.00008122507,0.00013351468,0.0024020737,0.0004098243,0.026290787,0.00024613095,0.0002471558,0.0067064874],"study_design_scores_gemma":[0.0000013727487,0.000003150072,0.99936503,0.0000019479758,0.0000039023566,0.000014694761,0.0002751341,0.00006020229,0.0001705955,0.000005352304,0.000096931246,0.0000016827514],"about_ca_topic_score_codex":0.91638565,"about_ca_topic_score_gemma":0.96912515,"teacher_disagreement_score":0.08361435,"about_ca_system_score_codex":0.0053117666,"about_ca_system_score_gemma":0.003973202,"threshold_uncertainty_score":0.16821349},"labels":[],"label_agreement":null},{"id":"W1993598587","doi":"10.1016/j.jsg.2011.01.004","title":"Magnetic fabrics in L–S tectonites: How many specimens?","year":2011,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Homogeneous; Schist; Geology; Tectonite; Anisotropy; Mineralogy; Block (permutation group theory); Remanence; Geometry; Petrology; Magnetization; Paleontology; Magnetic field; Optics; Mathematics; Metamorphic rock; Physics; Combinatorics; Tectonics","score_opus":0.01369113163559305,"score_gpt":0.21559866833620225,"score_spread":0.2019075367006092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993598587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975291,0.00039795812,0.00056121335,0.000054147262,0.0000123409245,0.000016810358,0.00028154647,0.000016592836,0.0011302734],"genre_scores_gemma":[0.9978029,0.00017358329,0.0010863969,0.000043080378,0.000014930167,0.000020540143,0.0002727067,0.00001548216,0.00057037733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994785,0.000092536655,0.00010896164,0.00014481098,0.00010235433,0.000072786235],"domain_scores_gemma":[0.99896705,0.00014224421,0.00023202498,0.00024099828,0.00028571094,0.00013208968],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091078907,0.00025136693,0.00042963546,0.001365255,0.0012096508,0.00090842095,0.0004443897,0.00046243583,0.0008812836],"category_scores_gemma":[0.0013020241,0.00034454576,0.0002476469,0.0010332956,0.0011115961,0.00065889995,0.0006857645,0.00031710646,0.00037064092],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035049857,0.000086556916,0.78400636,0.000110902,0.00031295087,0.0005537958,0.0037627134,0.00032739734,0.15551111,0.00027496376,0.00046034704,0.0542423],"study_design_scores_gemma":[0.000008050226,0.00007564663,0.9831055,0.000022089796,0.00014505569,0.0010208059,0.0031715287,0.00026343582,0.009082908,0.00016015887,0.00292205,0.000022759941],"about_ca_topic_score_codex":0.0073936437,"about_ca_topic_score_gemma":0.037742402,"teacher_disagreement_score":0.0073936437,"about_ca_system_score_codex":0.00044674252,"about_ca_system_score_gemma":0.00020316198,"threshold_uncertainty_score":0.014701247},"labels":[],"label_agreement":null},{"id":"W1994185250","doi":"10.1016/j.jsg.2009.12.007","title":"Emplacement and deformation of the Fomopéa pluton: Implication for the Pan-African history of Western Cameroon","year":2010,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Lineation; Pluton; Geology; Sinistral and dextral; Shear zone; Shear (geology); Seismology; Geochemistry; Biotite; Greenschist; Petrology; Fault (geology); Metamorphic rock; Paleontology; Tectonics","score_opus":0.01013538749794203,"score_gpt":0.20536301868766552,"score_spread":0.19522763118972347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994185250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959622,0.0011087193,0.00015246801,0.00045421688,0.000020872474,0.000008427518,0.00012950026,0.000003541456,0.0021600458],"genre_scores_gemma":[0.9986401,0.000709757,0.00015713838,0.00003210792,0.0000115226185,0.0000038635085,0.000047742844,0.0000024675876,0.00039527196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992156,0.000019114652,0.000006130234,0.000013775542,0.0000054574098,0.000033931665],"domain_scores_gemma":[0.99981505,0.00003576524,0.00007417362,0.00001499211,0.000039643033,0.000020409228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004347426,0.00029899855,0.00015393682,0.0011919593,0.0009823196,0.0010918191,0.00027974093,0.00040110995,0.0041116746],"category_scores_gemma":[0.00070692314,0.00017410652,0.0001273358,0.002414308,0.0012586687,0.00097405957,0.000647551,0.00033198902,0.00017080893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00154319,0.000106639294,0.84822184,0.000528112,0.00012096222,0.0079905335,0.014411114,0.0038555146,0.0273842,0.012487805,0.0010323187,0.08231773],"study_design_scores_gemma":[0.000014001768,0.00004198286,0.9871486,0.00007787085,0.000022794382,0.00045083085,0.0046939678,0.00075977255,0.0007028202,0.00040050797,0.0056764605,0.000010428249],"about_ca_topic_score_codex":0.05466965,"about_ca_topic_score_gemma":0.07604073,"teacher_disagreement_score":0.05466965,"about_ca_system_score_codex":0.0015492331,"about_ca_system_score_gemma":0.000923602,"threshold_uncertainty_score":0.1087029},"labels":[],"label_agreement":null},{"id":"W1995779944","doi":"10.1016/j.jsg.2015.02.002","title":"A critical review of rock slope failure mechanisms: The importance of structural geology","year":2015,"lang":"en","type":"review","venue":"Journal of Structural Geology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":432,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Classification of discontinuities; Engineering geology; Structural geology; Slope stability; Geotechnical engineering; Natural (archaeology); Geomorphology; Seismology; Paleontology; Tectonics","score_opus":0.020464483576869107,"score_gpt":0.3054016090752742,"score_spread":0.2849371254984051,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995779944","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000052545667,0.99890447,0.000067556764,0.00043230245,0.000322481,0.0000030480246,0.000021318707,0.0000023542077,0.00019392632],"genre_scores_gemma":[0.00036932883,0.99874413,0.00011865491,0.0003202189,0.00030074813,0.000003622152,0.000021312682,8.3418496e-7,0.00012106789],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995394,0.00008147644,0.00009799951,0.00008649441,0.00015903523,0.00003567568],"domain_scores_gemma":[0.99717796,0.0016074659,0.00035737868,0.00004958176,0.0006955895,0.000112019516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015729916,0.0011017827,0.0018969064,0.0039532213,0.00033674086,0.0015326521,0.001634475,0.0017678662,0.0042041778],"category_scores_gemma":[0.0043550213,0.0003829419,0.00091855845,0.0044288235,0.0007462526,0.002197641,0.00092602696,0.0017703798,0.0011274065],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084040366,0.00006250444,0.0004003049,0.070397235,0.0002735148,0.000162221,0.00013731091,0.000492371,0.0009987273,0.0042104986,0.09002456,0.83275676],"study_design_scores_gemma":[0.00002342174,0.00011630246,0.0016624341,0.027207768,0.0005079078,0.00060246594,0.00015354413,0.00013817094,0.0002363683,0.002980563,0.9663263,0.000044820932],"about_ca_topic_score_codex":0.0022924412,"about_ca_topic_score_gemma":0.0049909693,"teacher_disagreement_score":0.0042041778,"about_ca_system_score_codex":0.00087022106,"about_ca_system_score_gemma":0.0033369516,"threshold_uncertainty_score":0.014064372},"labels":[],"label_agreement":null},{"id":"W2003141545","doi":"10.1016/j.jsg.2014.06.004","title":"The use of microtomography in structural geology: A new methodology to analyse fault faces","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Ontario Innovation Trust","keywords":"Geology; Microscale chemistry; Fault (geology); Digital elevation model; Brittleness; Kinematics; Surface finish; Characterization (materials science); Mineralogy; Geometry; Seismology; Remote sensing; Materials science","score_opus":0.0482633790175086,"score_gpt":0.285846158831992,"score_spread":0.2375827798144834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003141545","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.042898573,0.0004350551,0.95371825,0.000110806184,0.000043368993,0.000056798974,0.00027771606,0.00047249784,0.001986927],"genre_scores_gemma":[0.20256653,0.00080593134,0.79453266,0.000051700026,0.00006271115,0.00008554001,0.00013697766,0.00016390109,0.001594121],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99981374,0.000031920656,0.000014443514,0.000048902853,0.000071976516,0.000019101695],"domain_scores_gemma":[0.99900097,0.00042389843,0.00012692389,0.00015977862,0.00024135057,0.00004700781],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047465065,0.0005572997,0.0003853001,0.0030580333,0.00037997254,0.0011187968,0.00062259537,0.00060624094,0.0025763016],"category_scores_gemma":[0.0015796385,0.0005549603,0.00036237962,0.0019913977,0.000996991,0.0015052088,0.00070988387,0.00074146205,0.00054667],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015598621,0.00009471325,0.021795928,0.00040484138,0.00010528748,0.00027877383,0.00083686685,0.022131618,0.37144765,0.019614264,0.0016665208,0.56146747],"study_design_scores_gemma":[0.00006170888,0.0003710589,0.0742704,0.0001175185,0.00026899253,0.0031665172,0.0012455039,0.6599174,0.1975728,0.032952826,0.02979478,0.0002605306],"about_ca_topic_score_codex":0.0018453917,"about_ca_topic_score_gemma":0.004649693,"teacher_disagreement_score":0.0030580333,"about_ca_system_score_codex":0.0002244703,"about_ca_system_score_gemma":0.00050906773,"threshold_uncertainty_score":0.008618534},"labels":[],"label_agreement":null},{"id":"W2006903173","doi":"10.1016/s0191-8141(00)00168-1","title":"The role of conjugate crenulation cleavage in the development of ‘millipede’ microstructures","year":2001,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Millipede; Geology; Crenulation; Archean; Sinistral and dextral; Syncline; Geochemistry; Paleontology; Structural basin; Tectonics; Shear zone","score_opus":0.007772402860607289,"score_gpt":0.2076981885534214,"score_spread":0.1999257856928141,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006903173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99133015,0.00032407886,0.003114905,0.000040273204,0.000009930648,0.000007053673,0.000036871297,0.00002418609,0.0051126815],"genre_scores_gemma":[0.99715424,0.000098654105,0.0014145012,0.000012615027,0.0000027942629,0.0000046972464,0.00004425017,0.000013450658,0.0012547004],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99990606,0.000009644292,0.000005768912,0.000033819073,0.000021328566,0.000023360932],"domain_scores_gemma":[0.99957174,0.0001091201,0.00009849816,0.000081299164,0.000085230364,0.000054143904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020882097,0.00015981421,0.00018166425,0.00033101375,0.0004885845,0.0012508663,0.00039500504,0.0005584829,0.0027006534],"category_scores_gemma":[0.0008814612,0.00040271683,0.000110404435,0.00023057772,0.00077864714,0.000844413,0.00048495768,0.0005657724,0.00042038283],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036262177,0.000024162116,0.02860764,0.00010306373,0.000024441058,0.0013589923,0.00055343914,0.0029623606,0.9123753,0.024504224,0.00028736974,0.028836465],"study_design_scores_gemma":[0.000047907215,0.00040199916,0.44289407,0.000043291293,0.000042834625,0.0032666242,0.00093748455,0.012167726,0.51636016,0.0076162284,0.016143527,0.000078188816],"about_ca_topic_score_codex":0.0016408017,"about_ca_topic_score_gemma":0.0022825697,"teacher_disagreement_score":0.0027006534,"about_ca_system_score_codex":0.00037512643,"about_ca_system_score_gemma":0.00035368095,"threshold_uncertainty_score":0.009034574},"labels":[],"label_agreement":null},{"id":"W2015717093","doi":"10.1016/j.jsg.2004.06.012","title":"Reference frame, angular momentum, and porphyroblast rotation","year":2004,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Experimental and Theoretical Physics Studies","field":"Physics and Astronomy","cited_by":37,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada; American Chemical Society Petroleum Research Fund; National Science Foundation","keywords":"Geology; Kinematics; Rotation (mathematics); Matrix (chemical analysis); Inclusion (mineral); Geometry; Mineralogy; Mathematics; Classical mechanics; Physics; Materials science","score_opus":0.005213905175460018,"score_gpt":0.24056249504673,"score_spread":0.23534858987126997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015717093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91710275,0.0028019226,0.018864652,0.0010450403,0.00018532979,0.000014385888,0.00035224177,0.00013458364,0.059499152],"genre_scores_gemma":[0.99357045,0.0004278045,0.0016259181,0.000025149746,0.000023413611,0.000004320093,0.00011060213,0.000020622436,0.0041916845],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99992585,0.000016717098,0.000004200656,0.00001995009,0.000014725221,0.000018552715],"domain_scores_gemma":[0.99977094,0.000050752144,0.00006497261,0.000042626747,0.000046956367,0.000023828396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023694952,0.00017617743,0.00018847533,0.00048767088,0.0006038849,0.0011975197,0.00025698144,0.00040190454,0.0045835963],"category_scores_gemma":[0.0012333409,0.00014164441,0.00013080584,0.0006379821,0.0006803387,0.00088582514,0.00050970836,0.00039650963,0.00055814174],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00232905,0.00014143084,0.045824897,0.00016695008,0.0000486431,0.0009696317,0.0026380774,0.010484189,0.10525832,0.7105347,0.004259296,0.117344745],"study_design_scores_gemma":[0.00036482504,0.0013385174,0.3915734,0.00015783739,0.00015154442,0.0026375868,0.0059113097,0.045285955,0.057269245,0.4221957,0.072824575,0.0002895139],"about_ca_topic_score_codex":0.0038640539,"about_ca_topic_score_gemma":0.0031692237,"teacher_disagreement_score":0.0045835963,"about_ca_system_score_codex":0.00048238074,"about_ca_system_score_gemma":0.00032392654,"threshold_uncertainty_score":0.0153336525},"labels":[],"label_agreement":null},{"id":"W2016454065","doi":"10.1016/s0191-8141(01)00159-6","title":"Chemical changes and the development of quartz preferred orientation in zones of crenulation cleavage, Anglesey","year":2002,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Crenulation; Cleavage (geology); Quartz; Muscovite; Geology; Mineralogy; Pressure solution; Crystallography; Chemistry; Tectonics; Seismology","score_opus":0.026153573947962604,"score_gpt":0.2309238000007822,"score_spread":0.20477022605281958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016454065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995956,0.000057420053,0.00001774563,0.0000035308176,5.96786e-7,0.0000010855629,0.000042572796,4.4352544e-7,0.00028107135],"genre_scores_gemma":[0.9996107,0.000043805143,0.000026742713,0.0000031554594,6.5317164e-7,0.0000011399275,0.000058428443,6.604067e-7,0.00025479886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994254,0.000006740827,0.000004654634,0.000018279188,0.000009327045,0.000018536186],"domain_scores_gemma":[0.99975914,0.00003848163,0.00008482974,0.0000067357023,0.00005996743,0.000050873998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012869945,0.000099770536,0.00010986462,0.0008341216,0.0003935975,0.00068817864,0.00016367556,0.00021993325,0.001331173],"category_scores_gemma":[0.000416353,0.00018803736,0.00007838928,0.0005637847,0.00049590995,0.00023646386,0.00025878567,0.00016476557,0.00011910522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015130001,0.000046510442,0.9058423,0.00003498266,0.000041646188,0.00035293313,0.001067123,0.00023989692,0.08453718,0.0002775985,0.000049485796,0.0059973546],"study_design_scores_gemma":[0.0000024330109,0.000022901919,0.998604,9.252669e-7,0.000002634008,0.000046873745,0.000236897,0.000041361756,0.00093847816,0.000014245982,0.00008837037,9.4122703e-7],"about_ca_topic_score_codex":0.03344118,"about_ca_topic_score_gemma":0.058471188,"teacher_disagreement_score":0.03344118,"about_ca_system_score_codex":0.000518777,"about_ca_system_score_gemma":0.00028275888,"threshold_uncertainty_score":0.066493094},"labels":[],"label_agreement":null},{"id":"W2017709924","doi":"10.1016/j.jsg.2014.05.026","title":"Kinematics and timing of shear zone deformation in the western Coast Belt: evidence for mid-Cretaceous orogen-parallel extension","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Geological Survey of Canada; University of Waterloo","funders":"Natural Resources Canada; U.S. Geological Survey","keywords":"Sinistral and dextral; Geology; Shear zone; Transpression; Shear (geology); Cretaceous; Seismology; Paleontology; Tectonics; Geomorphology","score_opus":0.03680122057770153,"score_gpt":0.2625704177925848,"score_spread":0.22576919721488325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017709924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99917835,0.00006240914,0.000044144348,0.000016893322,0.0000015222561,0.0000016647562,0.00008906932,0.0000033971844,0.0006025801],"genre_scores_gemma":[0.999529,0.000057650795,0.00007240166,0.0000069558464,0.0000017720204,0.0000015879153,0.00012816663,0.0000022179047,0.00020035495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992526,0.000008515394,0.000008554749,0.000024885068,0.00001133264,0.000021483473],"domain_scores_gemma":[0.9996321,0.00004347314,0.00015891717,0.000026623557,0.000091969465,0.000046802237],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020496604,0.00015297635,0.0001413457,0.001064125,0.0002595905,0.00047685058,0.00020957272,0.00020238708,0.0021228206],"category_scores_gemma":[0.0007051455,0.00020392277,0.00012089563,0.0010378482,0.00040890524,0.00031724735,0.0003243301,0.000101845886,0.00026114524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021775477,0.000028183633,0.980682,0.000019667561,0.000028642098,0.00014022441,0.0011273234,0.00021924467,0.009352651,0.00015217805,0.00009691345,0.007935104],"study_design_scores_gemma":[0.0000016879284,0.0000053707313,0.99964046,0.0000023723335,0.0000025630038,0.000018697185,0.00014210504,0.00007112068,0.000047637142,0.000011730298,0.000055583627,8.104309e-7],"about_ca_topic_score_codex":0.07620322,"about_ca_topic_score_gemma":0.13803546,"teacher_disagreement_score":0.07620322,"about_ca_system_score_codex":0.00038459993,"about_ca_system_score_gemma":0.0004917451,"threshold_uncertainty_score":0.15151936},"labels":[],"label_agreement":null},{"id":"W2019875617","doi":"10.1016/j.jsg.2009.10.009","title":"Active fault and shear processes and their implications for mineral deposit formation and discovery","year":2009,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Kalgoorlie Consolidated Gold Mines; Barrick Gold Corporation","keywords":"Geology; Shearing (physics); Shear (geology); Shear zone; Scaling; Shear stress; Echelon formation; Seismology; Creep; Slip (aerodynamics); Petrology; Fault (geology); Geotechnical engineering; Tectonics; Mechanics; Geometry; Engineering","score_opus":0.012706894684277303,"score_gpt":0.23458210458424114,"score_spread":0.22187520989996384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019875617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99214,0.0006124244,0.001911611,0.00041925634,0.000011714945,0.0000062174654,0.000103115366,0.00000957964,0.0047860923],"genre_scores_gemma":[0.99906605,0.00023992597,0.00024608127,0.00000668614,0.000009029427,0.0000011824823,0.000019004565,0.0000017504394,0.00041026162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990594,0.000020747484,0.000009576807,0.000023981082,0.0000209774,0.000018852159],"domain_scores_gemma":[0.9989355,0.0005366962,0.00020262896,0.00008619215,0.00015790937,0.00008099235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006368895,0.00010927388,0.00012542779,0.0011337202,0.0005342405,0.0016089564,0.000329025,0.00046077123,0.0026459377],"category_scores_gemma":[0.0033241478,0.00018718996,0.00012394907,0.0009378086,0.0014007717,0.001749294,0.0004295343,0.00026967246,0.00021261045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008494121,0.00014473188,0.7451973,0.00013197721,0.000086653454,0.0011256139,0.0024705774,0.01050099,0.03198743,0.11297573,0.00074148574,0.093788095],"study_design_scores_gemma":[0.000067718465,0.00015186172,0.8699903,0.000024471005,0.000053819298,0.00059676904,0.0029472369,0.01988185,0.0050179814,0.096739985,0.004494224,0.00003386293],"about_ca_topic_score_codex":0.0035276248,"about_ca_topic_score_gemma":0.006673662,"teacher_disagreement_score":0.0035276248,"about_ca_system_score_codex":0.0007851121,"about_ca_system_score_gemma":0.00030557724,"threshold_uncertainty_score":0.008851528},"labels":[],"label_agreement":null},{"id":"W2020052583","doi":"10.1016/j.jsg.2011.02.006","title":"Structural development of a high-pressure collisional accretionary wedge: The Samaná complex, Northern Hispaniola","year":2011,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Ministerio de Ciencia e Innovación; European Commission","keywords":"Geology; Nappe; Blueschist; Metamorphism; Accretionary wedge; Seismology; Greenschist; Ophiolite; Shear zone; Subduction; Geochronology; Geochemistry; Petrology; Geomorphology; Eclogite; Tectonics","score_opus":0.03565816837214796,"score_gpt":0.2262824890017634,"score_spread":0.19062432062961543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020052583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984383,0.000023652305,0.000031697466,0.000021800955,0.0000014085739,0.0000029643236,0.000013704736,0.0000016390575,0.0014647802],"genre_scores_gemma":[0.9996973,0.000017196566,0.000047558868,0.000003614086,9.454783e-7,0.0000015444265,0.000019998937,8.092459e-7,0.00021108278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993634,0.000009182736,0.000003734755,0.00001551199,0.000011530259,0.000023656481],"domain_scores_gemma":[0.9999223,0.000010428384,0.000019230149,0.0000056465997,0.000017475884,0.000024884761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010352762,0.00017508355,0.00014495067,0.00074958004,0.0015218968,0.000751864,0.0004163925,0.00032684216,0.0024566865],"category_scores_gemma":[0.00041292133,0.00019999058,0.00008445981,0.000925742,0.00081029895,0.00031572484,0.00086577516,0.00022919597,0.00024989783],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009449529,0.00028939365,0.84987193,0.00014900486,0.0000784339,0.011569963,0.02763175,0.0016701741,0.0554917,0.004750266,0.000539949,0.047012504],"study_design_scores_gemma":[0.00001898531,0.00015107157,0.9875717,0.000013474315,0.000012538787,0.001149608,0.00789049,0.00082962436,0.000689987,0.00020277376,0.0014628142,0.000006891004],"about_ca_topic_score_codex":0.03158354,"about_ca_topic_score_gemma":0.07642271,"teacher_disagreement_score":0.03158354,"about_ca_system_score_codex":0.00070383056,"about_ca_system_score_gemma":0.00074342196,"threshold_uncertainty_score":0.062799394},"labels":[],"label_agreement":null},{"id":"W2032034753","doi":"10.1016/s0191-8141(01)00127-4","title":"The influence of backstop dip and convergence velocity in the growth of viscous doubly-vergent orogenic wedges: insights from thermomechanical laboratory experiments","year":2002,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Wedge (geometry); Subduction; Deformation (meteorology); Geometry; Terrane; Convergence (economics); Mantle (geology); Seismology; Tectonics; Geophysics","score_opus":0.011786588834099545,"score_gpt":0.2069324904510445,"score_spread":0.19514590161694495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032034753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992798,0.00002853879,0.0002541113,0.000010380101,0.0000018654139,0.0000020194934,0.000054535143,0.000010237404,0.00035847368],"genre_scores_gemma":[0.99980086,0.000014585722,0.00008905523,0.0000028116874,5.691083e-7,0.0000012854515,0.000019612358,0.0000056022873,0.00006549603],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998982,0.000017563447,0.000011268598,0.000024958454,0.000019065777,0.000028824428],"domain_scores_gemma":[0.9992556,0.0003661612,0.00011331063,0.000068749774,0.00007471084,0.00012154554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028882638,0.00023509144,0.00031573506,0.00035619267,0.00033814154,0.0008793641,0.00031009183,0.00041598183,0.0017388669],"category_scores_gemma":[0.0018121989,0.00038512258,0.000113832735,0.00020834921,0.0006932109,0.0004605442,0.00035779615,0.0003977233,0.00021510954],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019638694,0.0002715021,0.046875726,0.000079924685,0.000031619646,0.0005910074,0.0002459767,0.021103213,0.91829294,0.0011343745,0.00017801095,0.009231841],"study_design_scores_gemma":[0.0003112044,0.00094678876,0.3668504,0.000027614957,0.0000680385,0.00046552604,0.0009005814,0.14720908,0.48134166,0.0010175566,0.0007509392,0.00011055973],"about_ca_topic_score_codex":0.003962658,"about_ca_topic_score_gemma":0.004191829,"teacher_disagreement_score":0.003962658,"about_ca_system_score_codex":0.00043132098,"about_ca_system_score_gemma":0.00039134893,"threshold_uncertainty_score":0.007879198},"labels":[],"label_agreement":null},{"id":"W2033178207","doi":"10.1016/j.jsg.2011.11.016","title":"Paradoxical pseudotachylyte – Fault melt outside the seismogenic zone","year":2011,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Slip (aerodynamics); Seismology; Crystal plasticity; Nucleation; Climb; Tectonics; Fault (geology); Creep; Brittleness; Instability; Intraplate earthquake; Petrology; Plasticity; Mechanics; Composite material; Materials science","score_opus":0.02681194547300365,"score_gpt":0.22337591276942814,"score_spread":0.1965639672964245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033178207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940836,0.000101611644,0.0003398016,0.00041434483,0.000022396449,0.000002989578,0.00006253607,0.000024192836,0.00494858],"genre_scores_gemma":[0.9997009,0.000021241076,0.00003147024,0.000018261771,0.000010682284,5.908215e-7,0.000029645176,0.000003852589,0.00018330198],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997929,0.000025781868,0.00001990005,0.000040128034,0.000050123323,0.00007120096],"domain_scores_gemma":[0.9989987,0.00026014211,0.00028329383,0.00021446226,0.00013359282,0.00010978174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003322905,0.0000975922,0.00037221148,0.00059283455,0.0010456877,0.001403967,0.00042195828,0.0007329932,0.0047606663],"category_scores_gemma":[0.0033090226,0.00015178736,0.00017787653,0.00065093127,0.0015807247,0.0012140283,0.0014325734,0.00071200414,0.00033052024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0073728207,0.00037257173,0.53449714,0.0005158882,0.00041119131,0.009582302,0.010222491,0.012239891,0.23804906,0.123716034,0.00395373,0.059066843],"study_design_scores_gemma":[0.00027959477,0.00034909527,0.88925374,0.000051983698,0.00014502241,0.0035757686,0.006396044,0.008450333,0.018165603,0.059237175,0.014043325,0.000052365835],"about_ca_topic_score_codex":0.0032870562,"about_ca_topic_score_gemma":0.0051157307,"teacher_disagreement_score":0.0047606663,"about_ca_system_score_codex":0.00075133005,"about_ca_system_score_gemma":0.00049840874,"threshold_uncertainty_score":0.015925944},"labels":[],"label_agreement":null},{"id":"W2038860882","doi":"10.1016/j.jsg.2007.11.002","title":"The analogue shear zone: From rheology to associated geometry","year":2007,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Rheology; Geology; Shear (geology); Finite strain theory; Shear zone; Strain hardening exponent; Geotechnical engineering; Mechanics; Finite element method; Materials science; Petrology; Composite material; Physics","score_opus":0.006974036008845784,"score_gpt":0.2236713222184617,"score_spread":0.21669728620961592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038860882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85807735,0.0031654697,0.092874415,0.00071348774,0.00017718192,0.000054423195,0.000486023,0.00026821037,0.04418349],"genre_scores_gemma":[0.99454534,0.0007691735,0.0032707318,0.000017298598,0.00007577048,0.000005294585,0.00005580542,0.000034898636,0.0012256328],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.999866,0.000037065845,0.0000083546975,0.00004352596,0.000029831112,0.000015238798],"domain_scores_gemma":[0.9994123,0.00018634085,0.00012957377,0.00014614487,0.000059748807,0.00006574638],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023593823,0.0002921534,0.00036131026,0.0015574256,0.00027337088,0.0020535365,0.00056367076,0.00048205323,0.004744335],"category_scores_gemma":[0.0027981955,0.0002465627,0.00016703793,0.0011058447,0.0019637323,0.0025618905,0.000985403,0.00057510345,0.0005217427],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006457835,0.00015211717,0.034405854,0.00024906482,0.000056120633,0.0010715838,0.001048369,0.046055987,0.029377572,0.73593456,0.0020984393,0.14890455],"study_design_scores_gemma":[0.00010079833,0.00038156795,0.06542783,0.000098925855,0.00006825444,0.0019873618,0.0009840274,0.26584053,0.0077975495,0.6339884,0.023201864,0.00012285601],"about_ca_topic_score_codex":0.0005205076,"about_ca_topic_score_gemma":0.00023657636,"teacher_disagreement_score":0.004744335,"about_ca_system_score_codex":0.00024175455,"about_ca_system_score_gemma":0.00012143148,"threshold_uncertainty_score":0.015871346},"labels":[],"label_agreement":null},{"id":"W2039091930","doi":"10.1016/j.jsg.2014.10.009","title":"Physical analog (centrifuge) model investigation of contrasting structural styles in the Salt Range and Potwar Plateau, northern Pakistan","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foreland basin; Fault (geology); Basement; Thrust fault; Anticline; Paleontology; Fold (higher-order function); Neogene; Monocline; Petrology; Seismology; Geomorphology; Tectonics","score_opus":0.01227234592487432,"score_gpt":0.2322137487915991,"score_spread":0.21994140286672476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039091930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923206,0.000020988948,0.002718516,0.00005421224,0.000005950431,0.000022743257,0.00060355896,0.00011402285,0.0041394127],"genre_scores_gemma":[0.9985676,0.000018158627,0.0009235604,0.000009085372,0.0000018615741,0.000013062352,0.00019391841,0.0000069569073,0.00026567304],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999162,0.000012817478,0.000006647179,0.000032131844,0.000014401104,0.000017704995],"domain_scores_gemma":[0.9998148,0.00007143581,0.000032231765,0.000025562087,0.000037150363,0.000018827444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009731862,0.0003310346,0.00024518988,0.00042149774,0.0003895004,0.00068740355,0.000733482,0.0006522854,0.0026974112],"category_scores_gemma":[0.00047693713,0.00026522245,0.00039160292,0.00063768483,0.00046665894,0.00033578076,0.0003926574,0.00025005537,0.00015227865],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056682813,0.00008814769,0.024486596,0.000025421588,0.000024358616,0.00028279662,0.00011853878,0.96672094,0.003158307,0.00078484893,0.00023862583,0.0040146955],"study_design_scores_gemma":[0.000039888942,0.000051211922,0.015268963,0.000003423144,0.000014324129,0.000060466304,0.00013240486,0.983127,0.00053969614,0.00034233762,0.00040582556,0.000014383483],"about_ca_topic_score_codex":0.058597527,"about_ca_topic_score_gemma":0.03590623,"teacher_disagreement_score":0.058597527,"about_ca_system_score_codex":0.00080988166,"about_ca_system_score_gemma":0.0006316722,"threshold_uncertainty_score":0.116512895},"labels":[],"label_agreement":null},{"id":"W2043470373","doi":"10.1016/j.jsg.2004.02.012","title":"Comparisons between analogue and numerical models of thrust wedge development","year":2004,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":137,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Dalhousie University; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Thrust; Geology; Wedge (geometry); Finite element method; Mechanics; Plasticity; Geometry; Physics; Structural engineering; Mathematics; Engineering","score_opus":0.03589483541010983,"score_gpt":0.24428593814634256,"score_spread":0.20839110273623274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043470373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95785034,0.0003575678,0.025651919,0.00030824446,0.00008007985,0.000039473507,0.0005273527,0.00030294657,0.014882109],"genre_scores_gemma":[0.9969748,0.00010328902,0.0021370829,0.000013676938,0.000013638045,0.000013713847,0.000096844866,0.000026329872,0.00062060234],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996803,0.00013268918,0.00003010672,0.0000692107,0.000054350727,0.000033350374],"domain_scores_gemma":[0.9938737,0.005013906,0.00023695265,0.0003399284,0.0004306445,0.00010490261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000906212,0.00028755012,0.00046602526,0.00092928304,0.00030545986,0.0011621359,0.0013851923,0.0012975433,0.00504845],"category_scores_gemma":[0.008287161,0.00042678398,0.00048353415,0.0012281325,0.0007809604,0.001029854,0.00046711403,0.0006815802,0.00027043506],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008696265,0.00006292603,0.0033354494,0.000027825035,0.00001578522,0.000025390033,0.00003093834,0.9905049,0.0002013923,0.0021103006,0.0001493904,0.0034486856],"study_design_scores_gemma":[0.00003076649,0.000021058417,0.0011348118,0.000003724785,0.0000069592857,0.0000089369405,0.000011682118,0.9978521,0.00011625266,0.000689321,0.000118339056,0.0000061284422],"about_ca_topic_score_codex":0.016569844,"about_ca_topic_score_gemma":0.007084119,"teacher_disagreement_score":0.016569844,"about_ca_system_score_codex":0.0014941158,"about_ca_system_score_gemma":0.0005730557,"threshold_uncertainty_score":0.032946825},"labels":[],"label_agreement":null},{"id":"W2047158799","doi":"10.1016/j.jsg.2013.01.009","title":"Ring schlieren: Description and interpretation of field relations in the Halifax Pluton, South Mountain Batholith, Nova Scotia","year":2013,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Batholith; Geometry; Schlieren; Physics; Paleontology; Tectonics; Optics","score_opus":0.013971604951137744,"score_gpt":0.2209720508835171,"score_spread":0.20700044593237935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047158799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90752846,0.00069630897,0.027213799,0.00019424944,0.000031086878,0.00026479491,0.016967345,0.0018261182,0.045277797],"genre_scores_gemma":[0.9770299,0.00019289,0.012098518,0.00001411494,0.000005301909,0.00004951761,0.0034238424,0.00010085613,0.007085012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999892,0.000012846193,0.000013539473,0.000030013322,0.000022209637,0.000029386141],"domain_scores_gemma":[0.999579,0.00010896429,0.0000568682,0.000056484227,0.00016540605,0.00003328323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022584015,0.00017108898,0.00011752753,0.002090563,0.0005637957,0.0011019822,0.000510837,0.00013737468,0.0048127593],"category_scores_gemma":[0.0010512457,0.00013532709,0.00012469283,0.0018394075,0.00050660456,0.00043172183,0.0003963337,0.00012562636,0.00062455836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066918076,0.00006396,0.67794806,0.00041442996,0.00008455096,0.0019034846,0.0072948365,0.02772043,0.02211059,0.017636646,0.013644584,0.2305092],"study_design_scores_gemma":[0.000039133323,0.00003825671,0.92248863,0.000112043876,0.000052386255,0.00033775935,0.0027235209,0.033409227,0.0048636976,0.001964406,0.033937033,0.000033947006],"about_ca_topic_score_codex":0.6141425,"about_ca_topic_score_gemma":0.7208571,"teacher_disagreement_score":0.38585752,"about_ca_system_score_codex":0.0024623862,"about_ca_system_score_gemma":0.002184546,"threshold_uncertainty_score":0.77625984},"labels":[],"label_agreement":null},{"id":"W2053265034","doi":"10.1016/s0191-8141(01)00019-0","title":"Magnetic fabrics and petrofabrics: their orientation distributions and anisotropies","year":2001,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":86,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Orientation (vector space); Principal axis theorem; Ellipsoid; Anisotropy; Symmetry (geometry); Geometry; Tensor (intrinsic definition); Orthorhombic crystal system; Principal component analysis; Sample (material); Geology; Outlier; Distribution (mathematics); Magnetic susceptibility; Mineralogy; Mathematics; Statistics; Mathematical analysis; Physics; Condensed matter physics; Optics; Geodesy; Diffraction","score_opus":0.006107839508748015,"score_gpt":0.22304162357816254,"score_spread":0.21693378406941452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053265034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955153,0.0003553173,0.0017125257,0.000041430278,0.0000053035606,0.0000037150385,0.00017300391,0.000025125593,0.0021682868],"genre_scores_gemma":[0.99919575,0.00014207122,0.00034490184,0.0000030973874,0.000007220643,0.0000019571642,0.000071487506,0.000011851078,0.00022152209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.000028612154,0.0000064531414,0.000022916633,0.000020292906,0.000019404128],"domain_scores_gemma":[0.99945897,0.00016974084,0.00015463616,0.00005609429,0.000105863306,0.000054629727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023439381,0.0003351766,0.00021350125,0.0019151205,0.00031106567,0.00066045753,0.00016401976,0.00018549015,0.0032807526],"category_scores_gemma":[0.0014669277,0.00026992528,0.00014690665,0.0018928915,0.0005209357,0.00046083733,0.0003233005,0.0002510448,0.0004610988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002145729,0.000079091194,0.64544123,0.00020074517,0.00017102201,0.00026577146,0.001008506,0.0034552456,0.22251906,0.0046593733,0.00042252374,0.11963177],"study_design_scores_gemma":[0.000026463833,0.000071972245,0.9817208,0.000010166119,0.00005986687,0.00061392074,0.00058970146,0.0045352564,0.009013823,0.0021430135,0.0011890739,0.000026015934],"about_ca_topic_score_codex":0.0026975614,"about_ca_topic_score_gemma":0.003027799,"teacher_disagreement_score":0.0032807526,"about_ca_system_score_codex":0.00018870387,"about_ca_system_score_gemma":0.00013341238,"threshold_uncertainty_score":0.010975242},"labels":[],"label_agreement":null},{"id":"W2060686426","doi":"10.1016/j.jsg.2010.10.011","title":"An Alpine-style Ordovician collision complex in the Sierra de Pie de Palo, Argentina: Record of subduction of Cuyania beneath the Famatina arc","year":2010,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Consejo Nacional de Investigaciones Científicas y Técnicas","keywords":"Geology; Laurentia; PALO; Paleontology; Ordovician; Nappe; Group (periodic table); Basement; Thrust fault; Décollement; Subduction; Geomorphology; Fault (geology); Tectonics; Archaeology","score_opus":0.013993730116556054,"score_gpt":0.23893988627420953,"score_spread":0.22494615615765348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060686426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99795204,0.00026542903,0.000053531967,0.000032654978,0.0000025206764,0.0000066473453,0.00024597457,0.0000041783937,0.0014370267],"genre_scores_gemma":[0.9993187,0.00012293305,0.00007996584,0.0000065612044,0.0000041048397,0.0000053656195,0.0002629263,0.000002136795,0.0001974515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998555,0.000018469782,0.000014729706,0.000046766327,0.000021088366,0.000043397056],"domain_scores_gemma":[0.99959964,0.00005016829,0.00015830787,0.000032723958,0.000089273504,0.00006989092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002549634,0.00020400873,0.0002945693,0.0010776628,0.0010991718,0.00080628373,0.00043396518,0.00037979512,0.0015603229],"category_scores_gemma":[0.0008733656,0.00019607905,0.00011637675,0.0018000132,0.0008803647,0.00036889318,0.0007914071,0.00025382996,0.0001409273],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002070381,0.000028560102,0.9842629,0.000047971054,0.000046970046,0.00037148892,0.0028868276,0.0003052314,0.002960281,0.00033972625,0.00031765178,0.008225255],"study_design_scores_gemma":[0.000003737107,0.000008819875,0.99835086,0.000009213605,0.000005983806,0.00013759473,0.00051315123,0.00014427726,0.00005157003,0.000021764981,0.00075121486,0.0000018108767],"about_ca_topic_score_codex":0.16072951,"about_ca_topic_score_gemma":0.27919862,"teacher_disagreement_score":0.16072951,"about_ca_system_score_codex":0.001207624,"about_ca_system_score_gemma":0.0007655436,"threshold_uncertainty_score":0.31958795},"labels":[],"label_agreement":null},{"id":"W2060693584","doi":"10.1016/j.jsg.2014.12.006","title":"The mechanical and microstructural behaviour of calcite-dolomite composites: An experimental investigation","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":41,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Research Council Canada; Campus France; National Science Council","keywords":"Dolomite; Calcite; Geology; Shear (geology); Mineralogy; Grain Boundary Sliding; Deformation mechanism; Lime; Deformation (meteorology); Composite material; Materials science; Microstructure; Grain boundary","score_opus":0.011008117829357558,"score_gpt":0.23820795536556386,"score_spread":0.2271998375362063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060693584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998548,0.00006672379,0.00046665414,0.0000060207726,0.0000041599133,0.000012428045,0.000080315185,0.000011456374,0.0008042395],"genre_scores_gemma":[0.99881375,0.000043291853,0.0003794264,0.000004930686,0.000002477558,0.000010862267,0.000053307558,0.0000066492794,0.0006853438],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996749,0.000026413065,0.000016771788,0.00007294294,0.00014381923,0.0000651068],"domain_scores_gemma":[0.99929655,0.00021147518,0.00011632306,0.000105216386,0.0002122545,0.000058220827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039492635,0.0003252584,0.00019571405,0.00037350834,0.00068946235,0.00019914476,0.0002714795,0.0004156653,0.003106466],"category_scores_gemma":[0.0005842989,0.0003168381,0.00015056483,0.0002831441,0.0007738353,0.00035890544,0.00030424382,0.00040057613,0.00026229734],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002172193,0.000115361654,0.0010006382,0.000026754902,0.0000027751546,0.000038668153,0.000106776984,0.00023060705,0.9971456,0.00006708194,0.00002141836,0.0010272771],"study_design_scores_gemma":[0.000025997319,0.001002058,0.029441139,0.0000059909416,0.000017997343,0.0001756486,0.00028442687,0.0017335911,0.96632504,0.00006071527,0.0009116593,0.000015671161],"about_ca_topic_score_codex":0.0022725933,"about_ca_topic_score_gemma":0.005085764,"teacher_disagreement_score":0.003106466,"about_ca_system_score_codex":0.00025895768,"about_ca_system_score_gemma":0.00034428475,"threshold_uncertainty_score":0.010392189},"labels":[],"label_agreement":null},{"id":"W2060847583","doi":"10.1016/j.jsg.2014.05.020","title":"Structural geology meets micromechanics: A self-consistent model for the multiscale deformation and fabric development in Earth's ductile lithosphere","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Natural Science Foundation of China; Canada Foundation for Innovation","keywords":"Geology; Micromechanics; Lithosphere; Shearing (physics); Shear zone; Shear (geology); Geometry; Slip (aerodynamics); Strain partitioning; Geophysics; Mechanics; Geotechnical engineering; Tectonics; Petrology; Seismology; Materials science; Physics","score_opus":0.010057434012016392,"score_gpt":0.20368143857977664,"score_spread":0.19362400456776024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060847583","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3731869,0.00090575527,0.6010533,0.0032695562,0.00033406765,0.00015586744,0.00078607904,0.0007056925,0.019602815],"genre_scores_gemma":[0.96775335,0.00049003906,0.024935411,0.0002735405,0.00013933438,0.00016785537,0.00018117187,0.00019346508,0.0058657806],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989927,0.000030856347,0.0000070582823,0.000022575372,0.000024957792,0.000015342286],"domain_scores_gemma":[0.9997545,0.00008658442,0.000046103636,0.000030299874,0.000040058436,0.000042444317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003495367,0.00048593292,0.000712572,0.00050098513,0.0006843445,0.001226792,0.0014442331,0.002120853,0.0017556439],"category_scores_gemma":[0.0013110209,0.000715777,0.00072233024,0.00059845054,0.0012327249,0.00113439,0.0011507695,0.0008339595,0.00029822133],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014037683,0.00003378418,0.0007237615,0.000011251608,0.000016277832,0.000058550067,0.000037387123,0.9834221,0.0009623125,0.0123786,0.00038261266,0.0019594755],"study_design_scores_gemma":[0.0000060058424,0.0000039471847,0.00013656337,0.0000010839841,0.00000275508,0.0000043972004,0.000003990416,0.9981115,0.00003600476,0.0015549029,0.00013576254,0.0000030223937],"about_ca_topic_score_codex":0.017096547,"about_ca_topic_score_gemma":0.012164337,"teacher_disagreement_score":0.017096547,"about_ca_system_score_codex":0.00068784395,"about_ca_system_score_gemma":0.0016648466,"threshold_uncertainty_score":0.03399408},"labels":[],"label_agreement":null},{"id":"W2064721453","doi":"10.1016/j.jsg.2005.04.009","title":"Reply to the comments by Domingo Aerden on “Reference frame, angular momentum, and porphyroblast rotation”","year":2005,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; Western University","funders":"","keywords":"Geology; Angular momentum; Mathematical physics; Geometry; Physics; Mathematics; Classical mechanics","score_opus":0.007701115805843223,"score_gpt":0.22289358431846715,"score_spread":0.2151924685126239,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064721453","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00024697956,0.0022307253,0.00020383889,0.964593,0.031980023,0.000005198853,0.00006217149,0.000026321906,0.0006517727],"genre_scores_gemma":[0.0027568578,0.0013421399,0.00021483723,0.9635195,0.028495332,0.000020636953,0.000036624606,0.000043867287,0.0035701203],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99637127,0.000848258,0.00046801538,0.00074366893,0.0010694165,0.00049939373],"domain_scores_gemma":[0.98486334,0.008200015,0.0012025313,0.0004954052,0.0041676746,0.0010710421],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005818522,0.0012179769,0.0015887037,0.001122963,0.005170796,0.0047575813,0.0037470632,0.03927271,0.0064356937],"category_scores_gemma":[0.040274974,0.0011562973,0.0012769282,0.0014311853,0.0056238403,0.0050273687,0.004235262,0.044512566,0.0055507673],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003097045,0.0000066249886,0.00021600239,0.000051294453,0.000014911415,0.00018453617,0.00049638044,0.00005361788,0.00014095813,0.0021561228,0.99443924,0.0022093977],"study_design_scores_gemma":[0.00003063353,0.00001931981,0.0015240037,0.00030197354,0.000032052634,0.00032895603,0.0017844617,0.00019028131,0.0004781879,0.0043668584,0.9908659,0.00007749127],"about_ca_topic_score_codex":0.017476676,"about_ca_topic_score_gemma":0.018534135,"teacher_disagreement_score":0.03927271,"about_ca_system_score_codex":0.004060008,"about_ca_system_score_gemma":0.003894595,"threshold_uncertainty_score":0.034749925},"labels":[],"label_agreement":null},{"id":"W2066042994","doi":"10.1016/j.jsg.2010.11.014","title":"Deciphering cryptic P–T-d–t histories in the western Thor-Odin dome, Monashee Mountains, Canadian Cordillera: A key to unravelling pre-Cordilleran tectonic signatures","year":2010,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Proterozoic; Paleontology; Metamorphic rock; Rodinia; Basement; Dome (geology); Lithosphere; Tectonics; Metamorphic core complex; Craton; Geochemistry; Extensional definition; Archaeology","score_opus":0.007553248238743909,"score_gpt":0.2128557193749195,"score_spread":0.2053024711361756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066042994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933681,0.0006514181,0.00049641856,0.00018066427,0.0000093601575,0.000015081546,0.0005660668,0.000018540008,0.00469441],"genre_scores_gemma":[0.9987399,0.00012974285,0.00032513184,0.000024452584,0.0000035332935,0.0000030506221,0.00021276172,0.000008049777,0.00055338896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985445,0.000009998919,0.000009976459,0.000048390524,0.000028519169,0.000048627844],"domain_scores_gemma":[0.9995814,0.000034415927,0.00007187206,0.000023295002,0.00022607432,0.00006298306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028409183,0.00018361957,0.00021694084,0.0016353553,0.0020083198,0.0011699063,0.00056810625,0.000379773,0.0026798295],"category_scores_gemma":[0.0010864255,0.00014011971,0.00014973828,0.0032110983,0.0010877537,0.00040975062,0.00078919297,0.00035973956,0.00022542365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048320662,0.0000522838,0.85566837,0.00016776033,0.00013025948,0.0007267328,0.0064574108,0.0021525235,0.048263364,0.0033655786,0.00138017,0.08115227],"study_design_scores_gemma":[0.000008191421,0.000011301982,0.99254084,0.0000208553,0.0000210728,0.00011136385,0.0012599913,0.0012764015,0.0006975864,0.0002457663,0.0037947106,0.000011818187],"about_ca_topic_score_codex":0.88806707,"about_ca_topic_score_gemma":0.9575794,"teacher_disagreement_score":0.11193293,"about_ca_system_score_codex":0.004217446,"about_ca_system_score_gemma":0.00509658,"threshold_uncertainty_score":0.2251842},"labels":[],"label_agreement":null},{"id":"W2066589641","doi":"10.1016/s0191-8141(00)00167-x","title":"A new spin on ‘non-rotating’ porphyroblasts: implications of cleavage refraction and reference frames","year":2001,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Coaxial; Cleavage (geology); Geology; Rotation (mathematics); Fold (higher-order function); Geometry; Geodesy; Mathematics; Paleontology; Computer science","score_opus":0.01576953530041892,"score_gpt":0.24867799523830753,"score_spread":0.2329084599378886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066589641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8848077,0.00053063896,0.038522623,0.0012359761,0.0007390923,0.000028304969,0.00032705537,0.00025835028,0.073550224],"genre_scores_gemma":[0.98745894,0.00017070693,0.0073627965,0.00006268929,0.00007036398,0.000008567796,0.000103032595,0.000067642315,0.0046952777],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999762,0.00002654036,0.000016642893,0.000061556195,0.00006492118,0.00006830865],"domain_scores_gemma":[0.99871695,0.0002103351,0.00019170798,0.000457066,0.00029328847,0.00013072089],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036871387,0.00026728777,0.00034493455,0.0007837804,0.002004389,0.002279466,0.0006489055,0.00073349033,0.008731886],"category_scores_gemma":[0.002475346,0.00034410149,0.00021693236,0.00095289375,0.0022350578,0.001811309,0.0011431512,0.0015354163,0.0006979959],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001635571,0.00010884772,0.0220523,0.00023007127,0.000028654385,0.0026055418,0.0048351865,0.0037577848,0.4067863,0.39554617,0.004642615,0.15777099],"study_design_scores_gemma":[0.00036780085,0.0015740657,0.14660397,0.0003340909,0.0002722492,0.005716009,0.013973152,0.028434996,0.4730119,0.1908299,0.13848285,0.0003990398],"about_ca_topic_score_codex":0.0022113055,"about_ca_topic_score_gemma":0.003917876,"teacher_disagreement_score":0.008731886,"about_ca_system_score_codex":0.00063846936,"about_ca_system_score_gemma":0.0004804939,"threshold_uncertainty_score":0.029211044},"labels":[],"label_agreement":null},{"id":"W2067112992","doi":"10.1016/s0191-8141(01)00119-5","title":"Role of transverse faulting in along-strike termination of Limestone Mountain Culmination, Rocky Mountain thrust-and-fold belt, Alberta, Canada","year":2002,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Shell Canada","keywords":"Geology; Foreland basin; Thrust fault; Fault (geology); Imbrication; Paleozoic; Seismology; Thrust; Fold and thrust belt; Basement; Fold (higher-order function); Mesozoic; Extensional fault; Petrology; Paleontology; Extensional definition; Tectonics","score_opus":0.005131898399634831,"score_gpt":0.18256907313754625,"score_spread":0.17743717473791143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067112992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99577075,0.00022794829,0.0001055457,0.0001690161,0.0000045749,0.000007728795,0.00034388257,0.000007439943,0.0033629895],"genre_scores_gemma":[0.9980882,0.00013438647,0.00010112428,0.0000150167125,0.00000200754,0.0000019978852,0.00023477593,0.0000033673134,0.0014191483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996904,0.00003978162,0.000018656723,0.000031340343,0.00007443534,0.00014527827],"domain_scores_gemma":[0.9973803,0.00032863533,0.0004024603,0.00006642666,0.001367305,0.00045480786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005175309,0.00019933569,0.00025850107,0.0016816998,0.0018924619,0.0020924748,0.0007409376,0.00039055268,0.002836279],"category_scores_gemma":[0.0029559755,0.00018907578,0.00016516683,0.0025273112,0.00097400206,0.00040524933,0.00064152584,0.0003266945,0.00021395528],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019134358,0.00002265429,0.984869,0.000019873534,0.000023119974,0.00019712927,0.0010904473,0.0019946448,0.0010992708,0.0008521464,0.00064153015,0.008998786],"study_design_scores_gemma":[0.00000682714,0.000011054614,0.9958677,0.000021087371,0.000014598036,0.000036939142,0.0019054188,0.0012579663,0.000121749465,0.00010595062,0.00064613996,0.0000044907797],"about_ca_topic_score_codex":0.9801792,"about_ca_topic_score_gemma":0.9932417,"teacher_disagreement_score":0.01982081,"about_ca_system_score_codex":0.010266291,"about_ca_system_score_gemma":0.01602508,"threshold_uncertainty_score":0.07448751},"labels":[],"label_agreement":null},{"id":"W2069785261","doi":"10.1016/j.jsg.2011.11.012","title":"Geometric consequences of ductile fabric development from brittle shear faults in mafic melt sheets: Evidence from the Sudbury Igneous Complex, Canada","year":2011,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Mafic; Geology; Igneous rock; Shear zone; Brittleness; Shear (geology); Geochemistry; Petrology; Brittle fracture; Seismology; Geotechnical engineering; Fracture (geology); Composite material; Tectonics; Materials science","score_opus":0.039224462189191255,"score_gpt":0.2099176968949156,"score_spread":0.17069323470572434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069785261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987061,0.000035115292,0.000026554664,0.00001554963,4.789148e-7,0.0000034852574,0.00023699921,0.0000028491509,0.00097281765],"genre_scores_gemma":[0.9993617,0.00005430181,0.0000620623,0.0000043564937,6.693245e-7,0.0000017224409,0.00020637678,0.0000034933805,0.0003053217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997614,0.000014603977,0.000010901508,0.00003413488,0.000105608415,0.00007339865],"domain_scores_gemma":[0.99897575,0.00010128634,0.00019896144,0.000045227862,0.0005709696,0.000107777414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023648054,0.00023651234,0.00025891673,0.0023106558,0.002400551,0.0013831597,0.0007835557,0.00032657743,0.0019473565],"category_scores_gemma":[0.0013703749,0.00029991212,0.00020346227,0.0031235104,0.0016078608,0.0002607815,0.000618862,0.00028852225,0.0001939023],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024615688,0.000040274244,0.966271,0.00003306626,0.000068919675,0.00055456546,0.002936897,0.0011875024,0.016185757,0.00042947804,0.0002974896,0.011748866],"study_design_scores_gemma":[0.0000028346358,0.0000042609936,0.9988475,0.000003474387,0.0000066204857,0.00004025003,0.00051421137,0.00014806785,0.00023921988,0.000022020058,0.00016857036,0.0000030797219],"about_ca_topic_score_codex":0.95224434,"about_ca_topic_score_gemma":0.98636055,"teacher_disagreement_score":0.04775566,"about_ca_system_score_codex":0.0062171044,"about_ca_system_score_gemma":0.0049257516,"threshold_uncertainty_score":0.09607375},"labels":[],"label_agreement":null},{"id":"W2072129065","doi":"10.1016/j.jsg.2010.11.013","title":"Interfacial friction-induced pressure and implications for the formation and preservation of intergranular coesite in metamorphic rocks","year":2010,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Guangzhou Institute of Geochemistry, Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada","keywords":"Coesite; Metamorphic rock; Geology; Intergranular corrosion; Geochemistry; Petrology; Subduction; Paleontology; Tectonics; Eclogite; Composite material; Microstructure; Materials science","score_opus":0.013949096850546622,"score_gpt":0.22812613216125843,"score_spread":0.2141770353107118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072129065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99929297,0.000121895675,0.00015698624,0.00002564341,0.0000020412006,0.0000017043326,0.000033280245,0.0000051526895,0.0003603377],"genre_scores_gemma":[0.9999161,0.000024811048,0.000017379643,0.0000014661831,7.7767464e-7,3.5595443e-7,0.000011547103,7.840065e-7,0.000026673742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999218,0.000006103116,0.000010114069,0.00001825254,0.00001895972,0.000024783736],"domain_scores_gemma":[0.9998815,0.000024514971,0.000033723554,0.000010653892,0.000026927331,0.000022597997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014187137,0.00016203268,0.00023366882,0.0007168323,0.000570726,0.0012198485,0.0004915925,0.00041542784,0.001447034],"category_scores_gemma":[0.0009369538,0.00020802229,0.00011688445,0.00064969726,0.0010588237,0.0006167749,0.00081091066,0.00026021645,0.00010947423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012577486,0.00021475952,0.60325146,0.00030158096,0.00014199634,0.0026180686,0.001160633,0.014322571,0.34838653,0.005960286,0.00041553564,0.021968894],"study_design_scores_gemma":[0.000048334034,0.00013715522,0.952181,0.000013022161,0.000038327733,0.000595193,0.001186141,0.020473383,0.023265384,0.0014212619,0.0006181661,0.000022595881],"about_ca_topic_score_codex":0.009084912,"about_ca_topic_score_gemma":0.008156461,"teacher_disagreement_score":0.009084912,"about_ca_system_score_codex":0.00070296484,"about_ca_system_score_gemma":0.00033150893,"threshold_uncertainty_score":0.018064082},"labels":[],"label_agreement":null},{"id":"W2073795575","doi":"10.1016/s0191-8141(01)00040-2","title":"Discussion of “Is there a close spatial relationship between faults and plutons?” by S.R. Paterson and K.L. Schmidt","year":2001,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Pluton; Geology; Seismology; Geometry; Geochemistry; Mathematics; Tectonics","score_opus":0.016610646839952926,"score_gpt":0.25100690939073045,"score_spread":0.23439626255077753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073795575","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0023161394,0.013965124,0.01417651,0.93687,0.021859687,0.000017778842,0.00019003637,0.00005719956,0.010547584],"genre_scores_gemma":[0.13714756,0.051048294,0.024881378,0.648917,0.09124039,0.00015857027,0.0005496973,0.00026161977,0.045795497],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976713,0.00091917615,0.0001394597,0.00050127483,0.0006268031,0.00014194188],"domain_scores_gemma":[0.99046236,0.006320637,0.0005743203,0.00033280332,0.0019566047,0.00035327132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0069019394,0.00078433775,0.0013364849,0.0020741927,0.0046574506,0.005629064,0.003782842,0.009579868,0.009084801],"category_scores_gemma":[0.02214986,0.0006392268,0.0013743248,0.0047623115,0.0076523307,0.010265197,0.0034811904,0.011111095,0.0026005285],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000081957456,0.000022841434,0.0018589055,0.00041080386,0.00007010601,0.00075129466,0.0030120895,0.0016007578,0.00069165754,0.29888785,0.6479062,0.04470554],"study_design_scores_gemma":[0.000018934526,0.000027285956,0.0014179527,0.00049148715,0.000027955757,0.00063159136,0.003944054,0.0013747497,0.000490458,0.24823135,0.74330044,0.000043759755],"about_ca_topic_score_codex":0.008939395,"about_ca_topic_score_gemma":0.011427272,"teacher_disagreement_score":0.009579868,"about_ca_system_score_codex":0.0019266246,"about_ca_system_score_gemma":0.0022857157,"threshold_uncertainty_score":0.036501348},"labels":[],"label_agreement":null},{"id":"W2075104819","doi":"10.1016/j.jsg.2007.10.003","title":"Deformation, exhumation, and topography of experimental doubly-vergent orogenic wedges subjected to asymmetric erosion","year":2007,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Wedge (geometry); Erosion; Shear (geology); Kinematics; Geometry; Particle image velocimetry; Simple shear; Geotechnical engineering; Geomorphology; Mechanics; Physics; Petrology; Classical mechanics","score_opus":0.011499679775896436,"score_gpt":0.23915544989231802,"score_spread":0.22765577011642157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075104819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99990547,0.000002355601,0.000021856493,7.290946e-7,5.08744e-7,0.0000011690043,0.000017140621,6.385274e-7,0.000050149672],"genre_scores_gemma":[0.99977607,0.0000076413035,0.000044420456,0.0000028052486,4.6699864e-7,0.0000027659507,0.00005141676,0.0000017088275,0.00011277655],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998913,0.000015397864,0.000011312408,0.000022689563,0.000021656439,0.000037611957],"domain_scores_gemma":[0.99974424,0.00006175478,0.00005204878,0.0000625449,0.000027934037,0.00005152409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016143631,0.00019935108,0.0003893061,0.00024603267,0.00028398354,0.0002732234,0.00040605094,0.0003127121,0.0017337286],"category_scores_gemma":[0.0005025867,0.00021559946,0.0002465211,0.00031315006,0.0007272609,0.0002453627,0.0003889411,0.00035864994,0.00018092801],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.011507342,0.0018237679,0.045795597,0.00006530073,0.00007285407,0.00091936154,0.00081848825,0.003334835,0.9297834,0.00030530582,0.00009478349,0.0054790312],"study_design_scores_gemma":[0.0005531613,0.010208975,0.6494743,0.000016741391,0.0001573096,0.0012155649,0.0021236634,0.014881692,0.32032913,0.00030489126,0.0006876409,0.000046834914],"about_ca_topic_score_codex":0.002988957,"about_ca_topic_score_gemma":0.0025054098,"teacher_disagreement_score":0.002988957,"about_ca_system_score_codex":0.00020194257,"about_ca_system_score_gemma":0.0001847171,"threshold_uncertainty_score":0.0059431195},"labels":[],"label_agreement":null},{"id":"W2077067150","doi":"10.1016/j.jsg.2010.11.012","title":"Minas Fault Zone: Late Paleozoic history of an intra-continental orogenic transform fault in the Canadian Appalachians","year":2010,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta; Laurentian University; Bedford Institute of Oceanography; Saint Mary's University; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Transtension; Laurentia; Transpression; Terrane; Paleontology; Gondwana; Sinistral and dextral; Paleozoic; Devonian; Orogeny; Shear zone; Rift; Carboniferous; Transform fault; Laurasia; Continental margin; Late Devonian extinction; Fault (geology); Structural basin; Tectonics","score_opus":0.006582544483931542,"score_gpt":0.1907764152216596,"score_spread":0.18419387073772808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077067150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99458045,0.0007168005,0.000040727595,0.00014322351,0.0000037699044,0.00000932628,0.00031560162,0.0000032036992,0.004186928],"genre_scores_gemma":[0.9984255,0.00038878238,0.00008827557,0.00001593477,0.0000021864214,0.0000034821123,0.0001669546,0.0000025727447,0.000906482],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976844,0.000012488317,0.000012127119,0.00004838364,0.000052061056,0.00010642335],"domain_scores_gemma":[0.9994561,0.00002968728,0.00009899696,0.00001556843,0.00032124517,0.000078409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027765453,0.00024408476,0.00022490518,0.0022358107,0.0026976587,0.0014811152,0.0006082272,0.00036019238,0.0025388303],"category_scores_gemma":[0.0009603803,0.00021985504,0.00016158615,0.0033099772,0.00132034,0.0004883196,0.00096279895,0.00039186393,0.00014499795],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033985358,0.0000465139,0.9249707,0.00014657261,0.00009472108,0.0006960015,0.016067998,0.0008543079,0.005950958,0.0030780951,0.0010078719,0.046746437],"study_design_scores_gemma":[0.0000030075269,0.0000066179323,0.99488175,0.000022950046,0.0000104281535,0.00008837965,0.0021977157,0.0001248436,0.00010537809,0.000045124805,0.002507761,0.0000059234517],"about_ca_topic_score_codex":0.9823605,"about_ca_topic_score_gemma":0.9952923,"teacher_disagreement_score":0.017639518,"about_ca_system_score_codex":0.011934743,"about_ca_system_score_gemma":0.012322699,"threshold_uncertainty_score":0.08659303},"labels":[],"label_agreement":null},{"id":"W2077697757","doi":"10.1016/j.jsg.2014.10.010","title":"Displacement transfer from fault-bend to fault-propagation fold geometry: An example from the Himalayan thrust front","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Queen's University; Alberta Energy","funders":"Natural Sciences and Engineering Research Council of Canada; Oregon State University; National Science Foundation","keywords":"Geology; Fold (higher-order function); Fault (geology); Thrust; Geometry; Thrust fault; Seismology; Kinematics","score_opus":0.022678659540142584,"score_gpt":0.23023562136712863,"score_spread":0.20755696182698605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077697757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99540365,0.000058828133,0.0006010982,0.000061533414,0.0000049484165,0.000010248108,0.0001198599,0.00002292937,0.003716803],"genre_scores_gemma":[0.999456,0.000046883233,0.00020499092,0.0000072465677,0.0000022531246,0.0000011938386,0.000041444604,0.0000019563654,0.00023807342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995935,0.0000067896967,0.0000026508803,0.000010040639,0.000008290595,0.000012893149],"domain_scores_gemma":[0.99994135,0.000014685719,0.000011072884,0.000012550154,0.000011001623,0.0000093534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058384612,0.0001629283,0.00014044635,0.00041823176,0.0006399159,0.0005408213,0.0002329561,0.00038574924,0.0020465439],"category_scores_gemma":[0.00025304055,0.000097976364,0.00020354027,0.00060666347,0.00061006617,0.00017942769,0.0003258826,0.00022652638,0.0002576195],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001169994,0.00027943734,0.63416624,0.0004090923,0.00017602275,0.027461335,0.010852803,0.055058025,0.16122656,0.015564442,0.002086061,0.09155008],"study_design_scores_gemma":[0.00006823272,0.0002357908,0.92818373,0.000040444633,0.00005902527,0.0031917223,0.0041363263,0.048375033,0.008401053,0.0029562667,0.004290733,0.00006168488],"about_ca_topic_score_codex":0.02297046,"about_ca_topic_score_gemma":0.018188436,"teacher_disagreement_score":0.02297046,"about_ca_system_score_codex":0.0006347688,"about_ca_system_score_gemma":0.00023814812,"threshold_uncertainty_score":0.04567355},"labels":[],"label_agreement":null},{"id":"W2084465018","doi":"10.1016/s0191-8141(00)00174-7","title":"40Ar/39Ar age pattern associated with differential uplift along the Eastern Highlands shear zone, Cape Breton Island, Canadian Appalachians","year":2001,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Cape; Shear (geology); Geomorphology; Seismology; Sinistral and dextral; Shear zone; Paleontology; Oceanography; Archaeology; Tectonics; Geography","score_opus":0.007107678707675775,"score_gpt":0.17674009973293955,"score_spread":0.16963242102526377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084465018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984951,0.000077899516,0.000014107749,0.000055684803,0.000002376935,0.000003597495,0.0004059217,0.0000016759176,0.0009435397],"genre_scores_gemma":[0.99895585,0.00007783036,0.000037171016,0.000016106022,0.0000019273486,0.0000030873023,0.0003010377,0.0000016201157,0.0006054412],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99981266,0.0000120974255,0.000011085225,0.000040691244,0.000038382525,0.00008510867],"domain_scores_gemma":[0.9991824,0.00004734359,0.00016291076,0.00002363887,0.00043165928,0.00015204762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002019807,0.00018311916,0.00019709911,0.0015362822,0.001352474,0.00067275856,0.00044144285,0.00025145637,0.0017137432],"category_scores_gemma":[0.0005784991,0.00019413614,0.00014383202,0.0022820593,0.00081482466,0.00020036928,0.00050857954,0.00025949278,0.00012555259],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014353199,0.00001687884,0.9899615,0.000015074599,0.00003334837,0.00027509234,0.002010841,0.00013005153,0.0028606579,0.00015572422,0.0004904561,0.003906869],"study_design_scores_gemma":[9.789538e-7,0.0000022764877,0.99920434,0.0000022663326,0.0000034487714,0.000020860214,0.00055239897,0.000029107961,0.000025653733,0.000006802043,0.00015006984,0.0000017544808],"about_ca_topic_score_codex":0.9640372,"about_ca_topic_score_gemma":0.98529446,"teacher_disagreement_score":0.03596282,"about_ca_system_score_codex":0.0038433727,"about_ca_system_score_gemma":0.0047492282,"threshold_uncertainty_score":0.07234919},"labels":[],"label_agreement":null},{"id":"W2089475404","doi":"10.1016/j.jsg.2013.01.012","title":"3D form line construction by structural field interpolation (SFI) of geologic strike and dip observations","year":2013,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Interpolation (computer graphics); Geometry; Vector field; Weighting; Mathematics; Computer science; Computer graphics (images); Physics","score_opus":0.017104268670268426,"score_gpt":0.21928173436648696,"score_spread":0.20217746569621853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089475404","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018049732,0.000039918294,0.97267944,0.00006310167,0.0000547768,0.00011197861,0.000940596,0.0064023626,0.0016580939],"genre_scores_gemma":[0.15812369,0.00010183952,0.83603,0.000031114443,0.000019326326,0.00013376726,0.0029602726,0.000712215,0.0018876896],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994686,0.000052884203,0.000030201732,0.00015810246,0.00023044701,0.00005988138],"domain_scores_gemma":[0.9993249,0.00008078743,0.000056754718,0.00017192152,0.00033421302,0.00003155124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063082186,0.0010894991,0.000631331,0.0028706847,0.0006018632,0.0011885874,0.0009546962,0.0006726473,0.008204919],"category_scores_gemma":[0.0018401616,0.00075587194,0.0011467417,0.0022147875,0.00043609797,0.0008396259,0.0012067759,0.0009779838,0.0039020404],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002818503,0.00017932164,0.0071509336,0.00018354978,0.00005017125,0.00014350053,0.00033468576,0.06288298,0.03153227,0.0056223683,0.0117726615,0.8798657],"study_design_scores_gemma":[0.00003635382,0.0001111535,0.0046357266,0.00002700054,0.00003595658,0.00020920658,0.00013340889,0.9435646,0.030539392,0.004501861,0.016144618,0.000060690298],"about_ca_topic_score_codex":0.0077090077,"about_ca_topic_score_gemma":0.010927732,"teacher_disagreement_score":0.008204919,"about_ca_system_score_codex":0.00046560814,"about_ca_system_score_gemma":0.0016170563,"threshold_uncertainty_score":0.027448177},"labels":[],"label_agreement":null},{"id":"W2093764520","doi":"10.1016/j.jsg.2008.07.009","title":"Late Proterozoic reconstructions of North-West Scotland and Central Canada: Magnetic fabrics, paleomagnetism and tectonics","year":2008,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Proterozoic; Paleomagnetism; Tectonics; Paleontology; Seismology; Paleozoic","score_opus":0.006219078894955203,"score_gpt":0.15496185783749705,"score_spread":0.14874277894254184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093764520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99382657,0.0005759579,0.00023782907,0.00015029589,0.0000072286443,0.0000072241855,0.0018018968,0.000032614837,0.0033604123],"genre_scores_gemma":[0.9964915,0.00032290473,0.0003234552,0.00002325353,0.0000029369926,0.0000039957195,0.00079434755,0.000016957541,0.0020206477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983335,0.000010265187,0.000011649232,0.000026017713,0.000040479088,0.00007809748],"domain_scores_gemma":[0.9993863,0.00004087017,0.0000643351,0.000018495972,0.00038300632,0.00010691757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002726104,0.00038316756,0.0002943063,0.003831204,0.002175053,0.0023678693,0.00066998135,0.000344464,0.004980204],"category_scores_gemma":[0.0012815094,0.00034628267,0.00026198593,0.0058621615,0.0006711538,0.00043645568,0.00082894164,0.00035182142,0.00053405185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082446967,0.00007953161,0.84923214,0.0002711314,0.00037765768,0.0010649881,0.00971057,0.011369573,0.0142289335,0.006066398,0.004868156,0.10190646],"study_design_scores_gemma":[0.000017728406,0.000008223344,0.98712105,0.000049667466,0.000040460975,0.000113664806,0.0022370685,0.0018164817,0.00045524366,0.00020338876,0.0079161655,0.000020821108],"about_ca_topic_score_codex":0.98448795,"about_ca_topic_score_gemma":0.9928797,"teacher_disagreement_score":0.015512049,"about_ca_system_score_codex":0.013909553,"about_ca_system_score_gemma":0.011891938,"threshold_uncertainty_score":0.10092139},"labels":[],"label_agreement":null},{"id":"W2095827207","doi":"10.1016/j.jsg.2012.02.016","title":"On stress and strain in a continuous-discontinuous shear zone undergoing simple shear and volume loss","year":2012,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":37,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Otago; Ryerson University","keywords":"Simple shear; Shear (geology); Shear stress; Geology; Shear zone; Critical resolved shear stress; Matrix (chemical analysis); Pure shear; Brittleness; Rheology; Shear rate; Volume fraction; Geotechnical engineering; Composite material; Materials science; Petrology; Tectonics; Seismology","score_opus":0.0079553672336125,"score_gpt":0.22200588078583364,"score_spread":0.21405051355222113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095827207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935359,0.00020625585,0.0038243094,0.00015988562,0.000027759614,0.0000124407525,0.00006920727,0.00003080549,0.0021333988],"genre_scores_gemma":[0.9990871,0.000054497334,0.0003434091,0.0000094438365,0.00001200936,0.0000034973036,0.000022254493,0.0000058166474,0.0004620266],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998287,0.000039909257,0.000012606988,0.000038424892,0.000038172,0.000042160256],"domain_scores_gemma":[0.99890697,0.0006646901,0.00014093965,0.000060035516,0.0001030018,0.00012429745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000628024,0.0004755847,0.0007522639,0.000955467,0.00056980277,0.0012900474,0.0012882628,0.0010559502,0.002128826],"category_scores_gemma":[0.0021644754,0.0003970575,0.0004358223,0.00059185526,0.0032591808,0.0009246864,0.0007842156,0.0006065256,0.00013920481],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005274028,0.00097289897,0.029854063,0.00024590906,0.00013124995,0.003535157,0.0005997418,0.85465145,0.06353916,0.02487714,0.00069756137,0.015621624],"study_design_scores_gemma":[0.00011760738,0.00029482783,0.016990636,0.0000116475285,0.00004028848,0.00017992804,0.00025803308,0.9743824,0.0031928415,0.0042984746,0.00017053759,0.000062840685],"about_ca_topic_score_codex":0.0045995843,"about_ca_topic_score_gemma":0.0025228073,"teacher_disagreement_score":0.0045995843,"about_ca_system_score_codex":0.0005952575,"about_ca_system_score_gemma":0.000412473,"threshold_uncertainty_score":0.0091456175},"labels":[],"label_agreement":null},{"id":"W2097199879","doi":"10.1016/j.jsg.2006.03.022","title":"Networking of shear zones at the brittle-to-viscous transition (Cap de Creus, NE Spain)","year":2006,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":127,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mylonite; Geology; Shearing (physics); Shear zone; Shear (geology); Petrology; Overprinting; Seismology; Geotechnical engineering; Metamorphic rock; Tectonics","score_opus":0.00911002815024685,"score_gpt":0.2105497210716902,"score_spread":0.20143969292144334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097199879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98810834,0.00018705205,0.0004250163,0.00015823448,0.000009696179,0.000013642063,0.00022871129,0.000022982977,0.010846363],"genre_scores_gemma":[0.9977053,0.000047690195,0.00028082705,0.0000105755535,0.0000027707422,0.0000055014366,0.00016694305,0.0000040432956,0.0017763684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987507,0.000014138002,0.0000047940102,0.000028612574,0.000015530786,0.00006187534],"domain_scores_gemma":[0.99954,0.000066266955,0.000088064,0.000024367979,0.00013896439,0.00014237846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024206175,0.00009765476,0.00012136967,0.0010838158,0.00070794043,0.0016108135,0.00040636328,0.0003708705,0.004402637],"category_scores_gemma":[0.0013621936,0.000091310525,0.00007584984,0.00081594964,0.00047028836,0.00049602176,0.0010845445,0.00016321457,0.00033221542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026573725,0.00028729622,0.7525824,0.00015923142,0.000092193695,0.0021908798,0.008722567,0.019584177,0.012224157,0.059113603,0.010190827,0.13219538],"study_design_scores_gemma":[0.0000886966,0.00014085215,0.93062717,0.000120136916,0.00005029346,0.00026399124,0.008596708,0.013050302,0.002041397,0.007212806,0.037781417,0.000026260106],"about_ca_topic_score_codex":0.03477597,"about_ca_topic_score_gemma":0.052619763,"teacher_disagreement_score":0.03477597,"about_ca_system_score_codex":0.0015316906,"about_ca_system_score_gemma":0.0009178625,"threshold_uncertainty_score":0.06914711},"labels":[],"label_agreement":null},{"id":"W2104069596","doi":"10.1016/s0191-8141(99)00151-0","title":"The control of the smectite–illite transition on passive-roof duplex formation: Canadian Rockies Foothills, Alberta","year":2000,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Clay minerals and soil interactions","field":"Materials Science","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Foothills; Geology; Illite; Geomorphology; Geochemistry; Mining engineering; Clay minerals; Geography; Cartography","score_opus":0.005863516326309651,"score_gpt":0.21727627598045227,"score_spread":0.2114127596541426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104069596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99561405,0.000067618654,0.000121450146,0.000083232284,0.000002577743,0.000007827547,0.000119800425,0.000011323426,0.003972023],"genre_scores_gemma":[0.9984003,0.00003442336,0.00008081173,0.000010702359,5.879246e-7,0.0000019337292,0.000041907108,0.0000049258915,0.0014244409],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99963903,0.000016140539,0.000010136097,0.00007247221,0.000107751,0.00015450406],"domain_scores_gemma":[0.9996056,0.000029472068,0.000036891837,0.000010753536,0.00023792224,0.00007935042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020772597,0.00020068437,0.0003791631,0.0011928958,0.004469863,0.0018619638,0.0010071655,0.00051531504,0.002466564],"category_scores_gemma":[0.0005507877,0.0002917631,0.00015013215,0.001027219,0.0022019478,0.00038755074,0.0009375727,0.00039367616,0.00022470564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012770937,0.00019120623,0.80130464,0.00016018518,0.00010716812,0.0008212489,0.010946253,0.010055318,0.12907627,0.007018391,0.0020330702,0.037009083],"study_design_scores_gemma":[0.000022326687,0.000039511622,0.9821149,0.000016884855,0.000022916736,0.00007614604,0.0063866577,0.0026115351,0.0036398598,0.00031718324,0.004729172,0.000022802371],"about_ca_topic_score_codex":0.9745059,"about_ca_topic_score_gemma":0.9933861,"teacher_disagreement_score":0.025494099,"about_ca_system_score_codex":0.02046523,"about_ca_system_score_gemma":0.013095467,"threshold_uncertainty_score":0.14848638},"labels":[],"label_agreement":null},{"id":"W2109328734","doi":"10.1016/j.jsg.2010.06.015","title":"Recognizing soft-sediment structures in deformed rocks of orogens","year":2010,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Lithification; Sedimentary rock; Overprinting; Tectonics; Deformation (meteorology); Sediment; Slumping; Geomorphology; Geochemistry; Paleontology","score_opus":0.012430635195422438,"score_gpt":0.23042249799935963,"score_spread":0.21799186280393718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109328734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940057,0.00010782472,0.0046928497,0.000033772114,0.000008276054,0.000013401617,0.00019220002,0.000065142296,0.0008807497],"genre_scores_gemma":[0.9966234,0.000096771764,0.0025851685,0.000008683996,0.000006963263,0.000002308708,0.00029432058,0.000016025962,0.00036630552],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998673,0.00000844821,0.00001501639,0.00003471309,0.00003182804,0.000042672185],"domain_scores_gemma":[0.9995511,0.0000765086,0.00012328746,0.00004458118,0.00012833838,0.000076135286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017170444,0.0003355164,0.00036971123,0.002137896,0.00033608018,0.0012222468,0.0005378989,0.0005837771,0.001352112],"category_scores_gemma":[0.0008669495,0.00034125225,0.00027763098,0.001282662,0.00042164745,0.00073912344,0.0008333395,0.00029656212,0.00052709016],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013061963,0.00015435768,0.63813597,0.0002181412,0.00017432832,0.0023533762,0.00096358673,0.02719748,0.14991342,0.0010008328,0.00081601966,0.17776628],"study_design_scores_gemma":[0.000036948237,0.000106530984,0.78936434,0.000037086764,0.00016313679,0.0009504825,0.0028858574,0.17653848,0.026449766,0.0016983519,0.0017374934,0.000031630487],"about_ca_topic_score_codex":0.010433432,"about_ca_topic_score_gemma":0.025540594,"teacher_disagreement_score":0.010433432,"about_ca_system_score_codex":0.00026693888,"about_ca_system_score_gemma":0.00045369507,"threshold_uncertainty_score":0.020745397},"labels":[],"label_agreement":null},{"id":"W2125415083","doi":"10.1016/j.jsg.2009.06.007","title":"Structure of the accretionary prism, and the evolution of the Paleogene northern Caribbean subduction zone in the region of Camagüey, Cuba","year":2009,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Tectonic Studies in Latin America","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Ministerio de Economía y Competitividad","keywords":"Geology; Nappe; Ophiolite; Forearc; Accretionary wedge; Ultramafic rock; Subduction; Mafic; Sedimentary rock; Metamorphism; Fold (higher-order function); Geochemistry; Volcanic arc; Paleontology; Seismology; Tectonics","score_opus":0.005359587367894448,"score_gpt":0.18821489448613177,"score_spread":0.18285530711823733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125415083","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945034,0.0009453625,0.00004778327,0.00018107785,0.000004541768,0.0000057568873,0.00029987638,0.000004689082,0.0040075476],"genre_scores_gemma":[0.9991019,0.00028922514,0.00008319688,0.000011190885,0.0000027172491,0.00000483675,0.00016643717,0.0000027768444,0.0003377478],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999049,0.000013479944,0.0000074358736,0.00002099611,0.000013317321,0.00003990233],"domain_scores_gemma":[0.99971646,0.00003449442,0.00009728833,0.000014777955,0.00009356475,0.000043470547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024164416,0.00014933363,0.00019423444,0.0019514238,0.0010381809,0.0017424047,0.0005142603,0.00030824138,0.0017746912],"category_scores_gemma":[0.0010965348,0.00018767838,0.00013922605,0.0029388908,0.0008070616,0.00035058663,0.0010778578,0.00022494892,0.00011984208],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003931302,0.000067907735,0.9537982,0.00016713754,0.00010279022,0.0006164743,0.0056843567,0.0023754584,0.0060651437,0.0036996503,0.000589227,0.02644057],"study_design_scores_gemma":[0.000005832459,0.0000047212247,0.9957963,0.000034568457,0.0000123602995,0.00006420703,0.0018368049,0.0005188219,0.0000959026,0.00009710195,0.0015291307,0.000004361092],"about_ca_topic_score_codex":0.5855248,"about_ca_topic_score_gemma":0.7190492,"teacher_disagreement_score":0.5855248,"about_ca_system_score_codex":0.0039651166,"about_ca_system_score_gemma":0.0027173841,"threshold_uncertainty_score":0.83383226},"labels":[],"label_agreement":null},{"id":"W2133351858","doi":"10.1016/j.jsg.2006.12.006","title":"Importance of differentiating ductile slickenside striations from stretching lineations and variation of shear direction across a high-strain zone","year":2007,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; Western University; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lineation; Geology; Striation; Shear zone; Shear (geology); Simple shear; Perpendicular; Seismology; Geometry; Petrology; Tectonics","score_opus":0.00858220416703783,"score_gpt":0.2378474200250564,"score_spread":0.22926521585801857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133351858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99825877,0.000093572155,0.000605329,0.000020666996,0.00000805681,0.0000035898822,0.00007126833,0.000010672286,0.0009280046],"genre_scores_gemma":[0.99927944,0.00005292071,0.00042820483,0.000008243119,0.000009339564,0.000001320399,0.00005087932,0.0000066052826,0.00016305747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997845,0.000055323177,0.00003383338,0.000050359118,0.000037989823,0.00003799131],"domain_scores_gemma":[0.99732447,0.0010823618,0.00041465551,0.00014620594,0.0006970554,0.0003351926],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068761193,0.0003402462,0.0003098291,0.0011072155,0.00038349463,0.0012239196,0.00033423686,0.000501267,0.0018553884],"category_scores_gemma":[0.0030004208,0.0002447713,0.0001248256,0.00063719007,0.00046704008,0.00077194726,0.00032422715,0.00034204897,0.00036828793],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012535903,0.000079175225,0.9180128,0.00006821505,0.000058848807,0.00041598117,0.0003080732,0.0010145424,0.050708815,0.0001255707,0.000119653116,0.027834874],"study_design_scores_gemma":[0.0000088151955,0.00007589262,0.9933236,0.000008827133,0.000030612144,0.0005514079,0.00048292303,0.001975032,0.0032373413,0.000102609105,0.00019042303,0.000012593224],"about_ca_topic_score_codex":0.002531853,"about_ca_topic_score_gemma":0.007841048,"teacher_disagreement_score":0.002531853,"about_ca_system_score_codex":0.00011933475,"about_ca_system_score_gemma":0.00021672252,"threshold_uncertainty_score":0.0062069297},"labels":[],"label_agreement":null},{"id":"W2143509649","doi":"10.1016/j.jsg.2009.10.002","title":"Magnitude of weakening during crustal-scale shear zone development","year":2009,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Shear zone; Shear (geology); Mylonite; Simple shear; Petrology; Mineralogy; Geotechnical engineering; Seismology; Geometry; Tectonics","score_opus":0.00715958161337515,"score_gpt":0.20989558358275992,"score_spread":0.20273600196938477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143509649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899024,0.00009566481,0.00017047931,0.000015267675,0.0000022116412,0.000004149138,0.0001481177,0.0000057348325,0.0005679949],"genre_scores_gemma":[0.99955696,0.000047457055,0.00006708306,0.0000043560976,0.0000042135594,0.0000023852222,0.00010931201,0.0000023243338,0.00020605304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999378,0.000007391589,0.0000063449643,0.000016040816,0.000014076582,0.000018405044],"domain_scores_gemma":[0.9993736,0.00021708247,0.00013206092,0.000031884734,0.00013064727,0.00011466071],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027658872,0.00014217784,0.00018991162,0.00056814926,0.00017528769,0.0005004458,0.00013498247,0.00032984786,0.0017643613],"category_scores_gemma":[0.0018770333,0.0002427616,0.00013953265,0.000333652,0.00024841525,0.00031425874,0.00029901764,0.0003027811,0.00025807184],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036425826,0.000112034926,0.7013964,0.0001431782,0.000101883445,0.000505458,0.0009854219,0.0024844268,0.2580303,0.0005350086,0.00036384712,0.03169941],"study_design_scores_gemma":[0.0000045221163,0.00006574707,0.9971712,0.0000034361328,0.000008285113,0.000059116443,0.00007706363,0.00042990473,0.002042537,0.00003093791,0.000104299914,0.0000031014997],"about_ca_topic_score_codex":0.0036462294,"about_ca_topic_score_gemma":0.0042920397,"teacher_disagreement_score":0.0036462294,"about_ca_system_score_codex":0.00021134382,"about_ca_system_score_gemma":0.00020488614,"threshold_uncertainty_score":0.007250011},"labels":[],"label_agreement":null},{"id":"W2163109322","doi":"10.1016/s0191-8141(01)00081-5","title":"Determination of fabric and strain ellipsoids from measured sectional ellipses — theory","year":2002,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Optical measurement and interference techniques","field":"Computer Science","cited_by":86,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Ellipse; Ellipsoid; Allowance (engineering); Mathematics; Geometry; Geology; Mathematical analysis; Statistics; Geodesy; Engineering","score_opus":0.034443657815684994,"score_gpt":0.25124903820714745,"score_spread":0.21680538039146247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163109322","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021779016,0.00029453082,0.9761973,0.00006821306,0.000015247343,0.000017614391,0.000027122132,0.00007336327,0.0015275667],"genre_scores_gemma":[0.69723123,0.0009506273,0.29998422,0.00004446637,0.00007818633,0.0000803407,0.000107897235,0.00007585707,0.0014471778],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99955434,0.00015325991,0.00001668426,0.00008319258,0.00016521216,0.000027260461],"domain_scores_gemma":[0.99790084,0.0012803496,0.00021512946,0.00026223593,0.0002788143,0.00006267673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011096669,0.0005196275,0.0005036775,0.0009574317,0.00036006258,0.00069449045,0.0010342776,0.00061219477,0.0007176713],"category_scores_gemma":[0.0055086995,0.00060174445,0.0004373809,0.00045257312,0.0011839415,0.0013330843,0.0009252143,0.0006901099,0.0002698347],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012311306,0.0000965014,0.0060833194,0.00029503432,0.00005422228,0.00014427483,0.0003073582,0.6061592,0.023749257,0.13908814,0.0012550252,0.22264461],"study_design_scores_gemma":[0.0000034495008,0.000017696791,0.0010513338,0.000015454107,0.0000050444937,0.00007728041,0.000015606183,0.9849557,0.0018967536,0.0113664,0.0005794277,0.000015721174],"about_ca_topic_score_codex":0.0010757903,"about_ca_topic_score_gemma":0.00096817105,"teacher_disagreement_score":0.0011096669,"about_ca_system_score_codex":0.00041100523,"about_ca_system_score_gemma":0.0004075661,"threshold_uncertainty_score":0.0058684945},"labels":[],"label_agreement":null},{"id":"W2164380198","doi":"10.1016/j.jsg.2009.08.004","title":"Strain analysis and rheology contrasts in polymictic conglomerates: An example from the Seine metaconglomerates, Superior Province, Canada","year":2009,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Rheology; Strain (injury); Conglomerate; Paleontology; Thermodynamics; Biology; Physics","score_opus":0.011655482113482237,"score_gpt":0.2094180938307298,"score_spread":0.19776261171724754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164380198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961815,0.00014081631,0.000087041655,0.00005420489,0.0000013975618,0.0000072878042,0.0006400965,0.000006510107,0.0028812408],"genre_scores_gemma":[0.9987581,0.00008022414,0.00013211167,0.0000117901645,8.331384e-7,0.000001926045,0.0002626886,0.0000050774775,0.00074728427],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998066,0.000015372938,0.000010282862,0.000037152076,0.000056992896,0.00007366403],"domain_scores_gemma":[0.99955827,0.000037039386,0.000043151063,0.000018114551,0.00028344846,0.000059928057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016362299,0.00028018694,0.00034929405,0.0020362893,0.0027761871,0.0012593636,0.00060983363,0.00031395178,0.0016698843],"category_scores_gemma":[0.0008134317,0.00018490264,0.0001947004,0.0045372793,0.0010850539,0.00025890363,0.00054364535,0.00034906837,0.0002652164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030653656,0.000054135206,0.9432448,0.00006577741,0.00014943788,0.0014626198,0.010956553,0.00152927,0.009743822,0.0010820213,0.001261412,0.030143756],"study_design_scores_gemma":[0.0000036425504,0.0000076762935,0.9951042,0.000008245819,0.000019561936,0.00012338435,0.0029071525,0.0004504616,0.0003171685,0.000038715792,0.0010109453,0.0000088977895],"about_ca_topic_score_codex":0.9875537,"about_ca_topic_score_gemma":0.99602205,"teacher_disagreement_score":0.012446284,"about_ca_system_score_codex":0.008544113,"about_ca_system_score_gemma":0.005463564,"threshold_uncertainty_score":0.061992228},"labels":[],"label_agreement":null},{"id":"W2256100421","doi":"10.1016/j.jsg.2016.02.003","title":"Structural and statistical characterization of joints and multi-scale faults in an alternating sandstone and shale turbidite sequence at the Santa Susana Field Laboratory: Implications for their effects on groundwater flow and contaminant transport","year":2016,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"University of Guelph; Boeing","keywords":"Geology; Lithology; Groundwater flow; Outcrop; Hydraulic conductivity; Petrology; Oil shale; Fault (geology); Geomorphology; Bedding; Sedimentary depositional environment; Bed; Groundwater; Geotechnical engineering; Aquifer; Seismology; Paleontology; Soil science","score_opus":0.016080802335230505,"score_gpt":0.2641835837286163,"score_spread":0.24810278139338576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2256100421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995129,0.000015890193,0.00012303353,0.0000044298636,2.617652e-7,0.000002195346,0.00013771522,0.0000043775613,0.00019916678],"genre_scores_gemma":[0.9994068,0.000012085667,0.00017127182,0.0000015191565,5.7985636e-7,0.0000020431823,0.0002676176,8.441336e-7,0.00013723793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998801,0.000010578773,0.0000084959065,0.000039560782,0.00004102857,0.00002031228],"domain_scores_gemma":[0.9995752,0.00007257714,0.00013510301,0.00003900589,0.00012623839,0.000051942498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015031164,0.00010683876,0.00010959268,0.0010613505,0.0002886513,0.0002696133,0.00018967039,0.00015385568,0.00034425996],"category_scores_gemma":[0.00057919614,0.00009152742,0.000084890096,0.00075416017,0.00032225458,0.00012237187,0.00021886887,0.00009721964,0.00006854414],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003279368,0.000022127313,0.9886596,0.000009800357,0.000014221462,0.00008098846,0.00021848228,0.0008314267,0.004494316,0.00006871665,0.00007058706,0.0054969573],"study_design_scores_gemma":[0.0000015194377,0.000012465467,0.99755484,0.0000013856848,0.000003598792,0.000033403634,0.00018576212,0.0016997247,0.00036600436,0.000022038086,0.00011722241,0.000002056148],"about_ca_topic_score_codex":0.076937504,"about_ca_topic_score_gemma":0.21711367,"teacher_disagreement_score":0.076937504,"about_ca_system_score_codex":0.00055534154,"about_ca_system_score_gemma":0.0005532483,"threshold_uncertainty_score":0.15297931},"labels":[],"label_agreement":null},{"id":"W2301896537","doi":"10.1016/j.jsg.2016.03.005","title":"Benchmarking analogue models of brittle thrust wedges","year":2016,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":81,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; Canada Research Chairs; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Fundação de Amparo à Pesquisa do Estado de Minas Gerais; Vetenskapsrådet; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Thrust; Cohesion (chemistry); Brittleness; Geology; Hourglass; Geotechnical engineering; Structural engineering; Geometry; Engineering; Materials science; Mathematics; Mechanical engineering; Physics; Composite material","score_opus":0.009020403130663766,"score_gpt":0.20969374027280283,"score_spread":0.20067333714213906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2301896537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86012244,0.00066372147,0.08856228,0.00066678895,0.00030761946,0.00019962524,0.0027924322,0.0014868123,0.045198247],"genre_scores_gemma":[0.9897266,0.00011266461,0.0077305795,0.000046362333,0.00002075163,0.000044267184,0.0006588926,0.00012871268,0.0015310423],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99940455,0.00020541639,0.000052079744,0.00009570238,0.00015140475,0.0000908818],"domain_scores_gemma":[0.99531907,0.0031358849,0.0001957356,0.0006008079,0.0005476954,0.00020077673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010000836,0.0006798678,0.001125013,0.0011969011,0.00046880936,0.0015613515,0.002650343,0.002931722,0.00996563],"category_scores_gemma":[0.007485741,0.0005168991,0.00086181494,0.00134116,0.0010917978,0.0011625383,0.001178301,0.0011744222,0.00072096067],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035096622,0.000045559045,0.00042548619,0.000026363052,0.000008814765,0.000031265725,0.000012932053,0.99599373,0.00016050324,0.0015910317,0.00016837592,0.0015008372],"study_design_scores_gemma":[0.0000129203245,0.000016628119,0.00008921361,0.0000036715935,0.0000021376181,0.000005409007,0.000007396628,0.9990356,0.000105535066,0.0006017518,0.000116707655,0.0000030328383],"about_ca_topic_score_codex":0.012500443,"about_ca_topic_score_gemma":0.008482961,"teacher_disagreement_score":0.012500443,"about_ca_system_score_codex":0.0013361203,"about_ca_system_score_gemma":0.0009364184,"threshold_uncertainty_score":0.033338368},"labels":[],"label_agreement":null},{"id":"W2314121611","doi":"10.1016/j.jsg.2016.04.003","title":"The spin zone: Transient mid-crust permeability caused by coseismic brecciation","year":2016,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Breccia; Mylonite; Lineation; Shear zone; Petrology; Overprinting; Seismology; Slip (aerodynamics); Crust; Shear (geology); Tectonics; Metamorphic rock; Geochemistry","score_opus":0.009558010637003718,"score_gpt":0.22076919702220993,"score_spread":0.21121118638520622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314121611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987709,0.000058842616,0.00019334476,0.000030354126,0.0000039184306,0.0000052962696,0.00004923823,0.000024799585,0.00086328154],"genre_scores_gemma":[0.99989974,0.000010632396,0.000011865876,0.0000036327917,0.0000014389863,6.232971e-7,0.000012057956,0.0000017949321,0.00005812051],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999672,0.000003738826,0.0000017392794,0.000005738186,0.0000052513024,0.000016268903],"domain_scores_gemma":[0.99988806,0.000023405268,0.00002900359,0.000016193595,0.000013669967,0.00002970351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000071828064,0.00015422243,0.00021198599,0.00022027196,0.0002613876,0.00035001757,0.00017147276,0.00032554008,0.0022502397],"category_scores_gemma":[0.00048444537,0.00013326705,0.00012139085,0.0001776909,0.00036063645,0.00029608977,0.00037580635,0.00027646322,0.0001419619],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009787976,0.00038535698,0.18097605,0.00017213944,0.00014192033,0.013682772,0.0011564641,0.006263348,0.75685155,0.001531919,0.001299194,0.027751308],"study_design_scores_gemma":[0.00012565801,0.0006385026,0.95715564,0.000013579986,0.00007191689,0.0018173747,0.0006796232,0.008587032,0.029672213,0.00046273318,0.0007544365,0.00002130523],"about_ca_topic_score_codex":0.0032051068,"about_ca_topic_score_gemma":0.0022812658,"teacher_disagreement_score":0.0032051068,"about_ca_system_score_codex":0.00020887652,"about_ca_system_score_gemma":0.00010980052,"threshold_uncertainty_score":0.007527828},"labels":[],"label_agreement":null},{"id":"W2567699116","doi":"10.1016/j.jsg.2016.12.010","title":"Significance of first-order faults in folding mechanically isotropic layers: Evidence from the Sudbury Basin, Canada","year":2016,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fold (higher-order function); Slip (aerodynamics); Geometry; Anisotropy; Petrology; Isotropy; Crust; Brittleness; Fault (geology); Structural basin; Kinematics; Echelon formation; Seismology; Geophysics; Geomorphology; Composite material; Materials science","score_opus":0.017528589591104135,"score_gpt":0.21934685665837103,"score_spread":0.2018182670672669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2567699116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99365,0.00036413295,0.000101142025,0.00013555652,0.0000045330435,0.000016786593,0.0007238417,0.0000053690896,0.0049985107],"genre_scores_gemma":[0.9983494,0.0002502388,0.000177863,0.0000309561,0.0000020224777,0.0000057273946,0.00034050198,0.0000042809647,0.0008389524],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993765,0.000047203594,0.00003376308,0.00010735995,0.00016993772,0.00026532798],"domain_scores_gemma":[0.9969188,0.00031234967,0.00048469214,0.000117738695,0.0018383212,0.00032808504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045109214,0.00034545123,0.00048643758,0.0029870167,0.0048731114,0.002920963,0.0012160821,0.00047276515,0.0032938279],"category_scores_gemma":[0.0031172733,0.00036125068,0.0002459316,0.005586499,0.0021394335,0.00054255896,0.0011664401,0.00050902646,0.00024951712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016042581,0.00004198033,0.97086024,0.000079020436,0.000082154234,0.00034652953,0.0047495537,0.00051441335,0.0031456705,0.0009157318,0.00074995746,0.018354312],"study_design_scores_gemma":[0.0000065481495,0.0000050963204,0.9963911,0.000031397383,0.000016000911,0.00004512182,0.0023524358,0.00017265714,0.00015523049,0.00006294211,0.00075341616,0.000007999582],"about_ca_topic_score_codex":0.9941444,"about_ca_topic_score_gemma":0.99852705,"teacher_disagreement_score":0.015615142,"about_ca_system_score_codex":0.015615142,"about_ca_system_score_gemma":0.017607499,"threshold_uncertainty_score":0.11329633},"labels":[],"label_agreement":null},{"id":"W2595496352","doi":"10.1016/j.jsg.2017.03.006","title":"A trishear model for the deformation of the Sudbury Igneous Complex, Canada","year":2017,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Vale Canada Limited","keywords":"Geology; Igneous rock; Metamorphic rock; Foliation (geology); Shear zone; Sedimentary rock; Geometry; Fault (geology); Deformation (meteorology); Petrology; Shear (geology); Fold (higher-order function); Kinematics; Mineralogy; Seismology; Geochemistry; Tectonics","score_opus":0.02369785055874407,"score_gpt":0.21891369590067564,"score_spread":0.19521584534193157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2595496352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82017374,0.002312881,0.066384345,0.0027084204,0.00023408978,0.00019957655,0.016814757,0.0018460094,0.089326285],"genre_scores_gemma":[0.9762999,0.00061679975,0.0060056974,0.00008720426,0.000021353067,0.00005666978,0.0020118044,0.00020852748,0.014692051],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998784,0.000013562111,0.0000062414183,0.00002740241,0.00003154648,0.000042779982],"domain_scores_gemma":[0.9997266,0.00007150516,0.000020263156,0.0000199344,0.000119328404,0.000042432042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000288252,0.00053381216,0.0007576893,0.00083770603,0.0014801346,0.0016722302,0.0022632903,0.0016666141,0.00744377],"category_scores_gemma":[0.0013064625,0.0005405436,0.0005806612,0.001392095,0.0010250586,0.0006240541,0.00055175927,0.0008455669,0.0005873784],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027823678,0.0000102524755,0.0012978278,0.000012870944,0.000011366956,0.000041173313,0.000031907093,0.9906002,0.00017321392,0.0054295883,0.0008612542,0.0015025791],"study_design_scores_gemma":[0.00001789491,0.0000033797369,0.00073935825,0.0000070248907,0.000005897914,0.000006114079,0.000023020137,0.9970393,0.000044787415,0.0009529496,0.0011514481,0.000008819854],"about_ca_topic_score_codex":0.9557136,"about_ca_topic_score_gemma":0.9164272,"teacher_disagreement_score":0.04428637,"about_ca_system_score_codex":0.009817518,"about_ca_system_score_gemma":0.011509836,"threshold_uncertainty_score":0.08909428},"labels":[],"label_agreement":null},{"id":"W2613319876","doi":"10.1016/j.jsg.2017.05.004","title":"Permo-Triassic structural evolution of the Shiwandashan and Youjiang structural belts, South China","year":2017,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Subduction; Permian; Paleontology; Sinistral and dextral; Foreland basin; Lithosphere; Pluton; Orogeny; Pacific Plate; Plate tectonics; Collision zone; Transpression; Early Triassic; Seismology; Tectonics; Structural basin","score_opus":0.008720413558543978,"score_gpt":0.20813370028107753,"score_spread":0.19941328672253356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2613319876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99929464,0.00007280749,0.000031683412,0.000016159262,8.4722996e-7,0.0000020490388,0.00008142248,0.000002594099,0.00049779704],"genre_scores_gemma":[0.9994647,0.000053982305,0.00002570764,0.000005073188,0.000001043579,0.000002484107,0.00014728928,0.0000014222483,0.0002983446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999124,0.0000069746393,0.000009933099,0.000024580062,0.000018334556,0.000027831033],"domain_scores_gemma":[0.99982256,0.000015196283,0.00004756891,0.000013275788,0.000052320764,0.00004911768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022973068,0.0002751419,0.00020189772,0.0017119511,0.0007296132,0.00045982064,0.00035436946,0.00020279913,0.0013954],"category_scores_gemma":[0.0003036385,0.00028029273,0.00021055536,0.0019806102,0.0005726495,0.00030063497,0.00056739437,0.000135558,0.0001512117],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001948739,0.000038671216,0.950276,0.000073996685,0.000106010324,0.00036688038,0.005187318,0.0009806686,0.023336407,0.0011637378,0.0002058673,0.018069709],"study_design_scores_gemma":[0.0000020711507,0.000008862368,0.9992193,0.0000019375466,0.0000058604724,0.00002509667,0.000260205,0.00014312935,0.00009661111,0.000025807876,0.00020936254,0.0000016900258],"about_ca_topic_score_codex":0.10805167,"about_ca_topic_score_gemma":0.20991978,"teacher_disagreement_score":0.10805167,"about_ca_system_score_codex":0.0011882733,"about_ca_system_score_gemma":0.0016912951,"threshold_uncertainty_score":0.21484548},"labels":[],"label_agreement":null},{"id":"W2626110694","doi":"10.1016/j.jsg.2017.06.005","title":"The effects of dolomitization on petrophysical properties and fracture distribution within rift-related carbonates (Hammam Faraun Fault Block, Suez Rift, Egypt)","year":2017,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":30,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Saudi Aramco; Innovation and Technology Commission; Nebraska Academy of Sciences; Total; Statoil; BG Group","keywords":"Dolomitization; Geology; Dolostone; Petrography; Carbonate rock; Geochemistry; Facies; Dolomite; Carbonate; Rift; Petrophysics; Fault block; Carbonate platform; Petrology; Fault (geology); Mineralogy; Sedimentary rock; Geomorphology; Paleontology; Geotechnical engineering; Structural basin","score_opus":0.00525775519130565,"score_gpt":0.2046082011746371,"score_spread":0.19935044598333146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2626110694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997843,0.0000070442647,0.000014379566,0.0000032550688,2.3957614e-7,6.178246e-7,0.00004776711,8.79627e-7,0.00014156787],"genre_scores_gemma":[0.9998099,0.0000077450995,0.000011822195,0.0000013433806,3.2617604e-7,4.759621e-7,0.00006382387,8.7362355e-7,0.00010360784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989057,0.000009918749,0.000008244691,0.000031424082,0.00002123765,0.00003861054],"domain_scores_gemma":[0.99958843,0.00011920477,0.000098420176,0.000027483777,0.00010905472,0.000057488905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016481822,0.00015273644,0.00016649632,0.00059079233,0.00037142631,0.00056946074,0.00025993426,0.00026404092,0.0012890495],"category_scores_gemma":[0.00079667754,0.00016820949,0.00018350195,0.0006089392,0.00052927184,0.00034743058,0.0003345649,0.00016508024,0.0001864523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003478835,0.000059534643,0.9704525,0.0000173886,0.000052529915,0.0003938153,0.00037556494,0.0038469753,0.018985724,0.000101889105,0.00007584953,0.0052903607],"study_design_scores_gemma":[0.000002169576,0.000017852837,0.99760497,0.0000014978791,0.0000066298726,0.00003291697,0.00026808167,0.0013549987,0.00064069545,0.0000132553905,0.000054566623,0.0000023927778],"about_ca_topic_score_codex":0.04042713,"about_ca_topic_score_gemma":0.08951462,"teacher_disagreement_score":0.04042713,"about_ca_system_score_codex":0.0008003409,"about_ca_system_score_gemma":0.00052352913,"threshold_uncertainty_score":0.0803836},"labels":[],"label_agreement":null},{"id":"W2763328161","doi":"10.1016/j.jsg.2017.10.004","title":"Crustal shortening and thickening in Neoarchean granite-greenstone belts: A case study from the link between the ∼2.7 Ga Elu and Hope Bay belts, northeast Slave craton, Canada","year":2017,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Metamorphism; Craton; Geochemistry; Archean; Metamorphic rock; Thickening; Greenstone belt; Plutonism; Thrust fault; Tectonics; Batholith; Petrology; Orogeny; Seismology; Pluton","score_opus":0.015948367604007193,"score_gpt":0.22650606681878988,"score_spread":0.21055769921478268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763328161","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992569,0.00008942198,0.000015179895,0.000016577598,3.8626715e-7,0.000003944561,0.00016581306,0.0000010865392,0.0004507127],"genre_scores_gemma":[0.9993443,0.0001099204,0.000055903827,0.000007448351,5.437134e-7,0.0000014906906,0.00019586332,0.0000013389941,0.00028320376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998596,0.000011491579,0.0000079649435,0.00002143853,0.00003208697,0.00006746175],"domain_scores_gemma":[0.9996749,0.000050590465,0.00006898417,0.00001815449,0.00011355348,0.00007378763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026925906,0.0002490976,0.000216964,0.0020160608,0.0013250079,0.00094741414,0.0007149101,0.00030426992,0.00097551494],"category_scores_gemma":[0.00078613363,0.0001839185,0.00028089946,0.004121331,0.0012423404,0.0002833585,0.0009611135,0.00021935086,0.00010749113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000944023,0.000024596664,0.98360693,0.00002936766,0.00004202589,0.0011370308,0.006229797,0.00030381302,0.0012882367,0.00024627612,0.0001696665,0.006827877],"study_design_scores_gemma":[0.0000016966629,0.000006208822,0.99569196,0.000010169923,0.000009816979,0.00012783533,0.0036534178,0.00010477458,0.000079805584,0.000022694172,0.0002890258,0.0000025937795],"about_ca_topic_score_codex":0.9515143,"about_ca_topic_score_gemma":0.9835886,"teacher_disagreement_score":0.048485696,"about_ca_system_score_codex":0.0063151903,"about_ca_system_score_gemma":0.00420651,"threshold_uncertainty_score":0.097542405},"labels":[],"label_agreement":null},{"id":"W2789914888","doi":"10.1016/j.jsg.2018.01.009","title":"The structure of composite volcanoes unravelled by analogue modelling: A review","year":2018,"lang":"en","type":"review","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Chicoutimi","funders":"","keywords":"Volcano; Geology; Caldera; Seismology; Magma; Geodetic datum; Petrology; Geodesy","score_opus":0.02280750821166843,"score_gpt":0.2557176224734293,"score_spread":0.23291011426176084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789914888","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012772041,0.9923499,0.0047023483,0.0002583962,0.00016299315,0.000009253736,0.00019790207,0.00005134768,0.0009907223],"genre_scores_gemma":[0.008965387,0.9863913,0.0038442798,0.00008680192,0.0002195231,0.000010636029,0.00023776686,0.000022954398,0.0002214416],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999605,0.000053987565,0.000054641303,0.00013749115,0.00012290987,0.00002598544],"domain_scores_gemma":[0.9979665,0.0013209544,0.00027622114,0.00010779922,0.00027729987,0.000051209783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013723616,0.0016914835,0.0028474568,0.003927048,0.00029153316,0.0021746124,0.003231586,0.0018611338,0.0030981398],"category_scores_gemma":[0.0056315335,0.0007868257,0.0012558026,0.005349258,0.001210842,0.0030772942,0.0012365469,0.0010892255,0.00080917706],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006702291,0.000055941873,0.0028884837,0.029005185,0.0004387929,0.00027156214,0.00029146147,0.019160153,0.0014761544,0.015009164,0.008913661,0.9224225],"study_design_scores_gemma":[0.000051945557,0.00017900132,0.00795162,0.022972573,0.0022624638,0.0026619395,0.00077597395,0.024367858,0.0030263506,0.06647291,0.8689246,0.00035275528],"about_ca_topic_score_codex":0.0047810744,"about_ca_topic_score_gemma":0.005776803,"teacher_disagreement_score":0.0047810744,"about_ca_system_score_codex":0.0007069097,"about_ca_system_score_gemma":0.0022039225,"threshold_uncertainty_score":0.010364294},"labels":[],"label_agreement":null},{"id":"W2891168872","doi":"10.1016/j.jsg.2018.09.012","title":"Structural evolution of a gold-bearing transtensional zone within the Archean Porcupine-Destor deformation zone, southern Abitibi greenstone belt, eastern Ontario, Canada","year":2018,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Greenstone belt; Archean; Geology; Geochemistry; Bearing (navigation); Geography","score_opus":0.011620015786561012,"score_gpt":0.20158172320762818,"score_spread":0.18996170742106716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891168872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971143,0.00011806439,0.00006824557,0.000036122965,0.0000014963872,0.000009626825,0.00032624096,0.0000076285664,0.0023182856],"genre_scores_gemma":[0.99854076,0.00007350063,0.00008353835,0.000006602137,5.5722245e-7,0.0000033837032,0.00014883347,0.0000024201202,0.0011403386],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985385,0.0000071343384,0.000007323374,0.00003269793,0.000044865596,0.000054190907],"domain_scores_gemma":[0.9996718,0.000021976464,0.000053250267,0.000011523077,0.00017129045,0.00007022978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001363445,0.00020507531,0.0002184867,0.0015057278,0.0016732719,0.0011594611,0.0006533101,0.0003132032,0.0019382697],"category_scores_gemma":[0.00060557475,0.00020877816,0.00016722055,0.0027809264,0.00095785677,0.00026117289,0.0007377927,0.00019490716,0.00024223884],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022152513,0.00004696009,0.9519596,0.00009103346,0.00007062558,0.0007572583,0.009812908,0.0018623874,0.0107878335,0.00093493983,0.00078679435,0.022668106],"study_design_scores_gemma":[0.000002549933,0.000006371511,0.99698216,0.000008797331,0.0000059174517,0.00003873773,0.0017891036,0.0002699247,0.00009654845,0.000020684252,0.00077564805,0.0000034363857],"about_ca_topic_score_codex":0.97520185,"about_ca_topic_score_gemma":0.99249023,"teacher_disagreement_score":0.024798155,"about_ca_system_score_codex":0.008814195,"about_ca_system_score_gemma":0.0087384675,"threshold_uncertainty_score":0.06395179},"labels":[],"label_agreement":null},{"id":"W2900901851","doi":"10.1016/j.jsg.2018.11.001","title":"Numerical investigation of slip and fracture instability mechanism of coal- rock parting-coal structure (CRCS)","year":2018,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":28,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Instability; Coal; Slip (aerodynamics); Geology; Dissipation; Acoustic emission; Fracture (geology); Geotechnical engineering; Mechanics; Materials science; Engineering; Composite material; Physics","score_opus":0.010503108301912136,"score_gpt":0.225146231673368,"score_spread":0.21464312337145586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900901851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902559,0.00010118081,0.004244893,0.000090545276,0.00002347136,0.000015184584,0.00010143742,0.00006168995,0.0051058293],"genre_scores_gemma":[0.9985031,0.000021505686,0.000805481,0.000006198104,0.0000036130646,0.000004202415,0.00003341339,0.000004982749,0.00061751535],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998995,0.000014781577,0.000006628824,0.000017921668,0.00003091998,0.000030216366],"domain_scores_gemma":[0.9995376,0.0001923136,0.000064986074,0.000038314414,0.00009788239,0.00006902522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020777629,0.0002762195,0.0004722828,0.00091218035,0.0008553764,0.00049332064,0.000775101,0.0012139671,0.0028277242],"category_scores_gemma":[0.0011232155,0.00033527918,0.0005665748,0.0006035437,0.0007488664,0.00046218903,0.00043394786,0.00035079793,0.0001442043],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017060658,0.00018098472,0.021693598,0.00008653155,0.000044667944,0.00071690493,0.00013203763,0.9558616,0.00953578,0.0042781644,0.00059396285,0.006705194],"study_design_scores_gemma":[0.0000094560955,0.000027203403,0.0027601533,0.0000027284557,0.000006684956,0.000041018524,0.000045462857,0.9963527,0.0004428041,0.00023022247,0.00007616428,0.0000053376875],"about_ca_topic_score_codex":0.016197529,"about_ca_topic_score_gemma":0.0121370405,"teacher_disagreement_score":0.016197529,"about_ca_system_score_codex":0.00058002566,"about_ca_system_score_gemma":0.00058632094,"threshold_uncertainty_score":0.032206476},"labels":[],"label_agreement":null},{"id":"W2906170149","doi":"10.1016/j.jsg.2018.12.007","title":"Interpreting regional 3D fault networks from integrated geological and geophysical data sets: An example from the Guichon Creek batholith, British Columbia","year":2018,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Laurentian University; Geological Survey of Canada; McMaster University; University of Alberta; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Batholith; Geology; Magnetic anomaly; Fault (geology); Geophysics; Magnetic susceptibility; Seismology; Lineament; Anomaly (physics); Magnetic field; Tectonics","score_opus":0.03987509729200993,"score_gpt":0.26347278301286453,"score_spread":0.2235976857208546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906170149","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97911775,0.00056286156,0.0042143906,0.0006936957,0.000018498338,0.00005274267,0.008460923,0.0004639007,0.006415251],"genre_scores_gemma":[0.98103136,0.00040495352,0.011331583,0.000044700108,0.0000063624284,0.00001783489,0.005051932,0.00010853289,0.00200283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970394,0.000039204107,0.000031017316,0.00007640035,0.00009284626,0.000056581976],"domain_scores_gemma":[0.9988084,0.00028630023,0.000078166064,0.00009442675,0.00066798093,0.00006481202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004543131,0.0004986435,0.00033406226,0.0026708916,0.0011757084,0.0029025464,0.00073327543,0.0007270087,0.0025068996],"category_scores_gemma":[0.003215521,0.0003718132,0.00030895954,0.0071562906,0.0005965377,0.00048822002,0.001152492,0.0005614209,0.0005104814],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036113107,0.00020766808,0.6193339,0.0005247225,0.00063286285,0.0045106765,0.0072453567,0.10902585,0.017774135,0.0028530082,0.013119962,0.22441077],"study_design_scores_gemma":[0.00009862681,0.00003640131,0.77443665,0.00029142166,0.0004369147,0.0005154421,0.016402736,0.18028466,0.0031152281,0.0031047498,0.021137973,0.00013908996],"about_ca_topic_score_codex":0.9455769,"about_ca_topic_score_gemma":0.9827833,"teacher_disagreement_score":0.054423094,"about_ca_system_score_codex":0.0043154377,"about_ca_system_score_gemma":0.0049119503,"threshold_uncertainty_score":0.109487176},"labels":[],"label_agreement":null},{"id":"W2909672800","doi":"10.1016/j.jsg.2018.12.011","title":"‘Strain probe’: Best-fitting a homogeneous strain to the motions of scattered points","year":2019,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Geodetic datum; Geology; Strain (injury); Geodesy; Cartesian coordinate system; Geometry; Deformation (meteorology); Reference frame; Finite strain theory; Homogeneous; Mathematical analysis; Mathematics; Frame (networking); Finite element method; Physics; Combinatorics; Computer science","score_opus":0.01564803777806045,"score_gpt":0.23144314315770115,"score_spread":0.2157951053796407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909672800","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.23160306,0.0003888264,0.74807054,0.0003337762,0.00020439007,0.00015377627,0.0019355519,0.015376125,0.0019339465],"genre_scores_gemma":[0.4928203,0.00013975678,0.4981244,0.00016250179,0.000044471384,0.00017338103,0.00459257,0.002033999,0.0019086454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993049,0.00017131219,0.00005314424,0.00023187425,0.0001493804,0.000089459114],"domain_scores_gemma":[0.9987857,0.0005975575,0.000100349054,0.00018974162,0.0002782746,0.00004842605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023146106,0.002133441,0.0010997342,0.0018563557,0.00052512216,0.0010314971,0.0021907527,0.003298286,0.005124643],"category_scores_gemma":[0.008529825,0.0010257361,0.0014338461,0.0018988965,0.00059565343,0.0014040826,0.00091495056,0.0014835995,0.0019736146],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001187244,0.000715867,0.009021268,0.00029067346,0.00031219405,0.0003052202,0.00034280567,0.5358282,0.030694462,0.001645181,0.011635566,0.4080213],"study_design_scores_gemma":[0.000049114355,0.00010764137,0.002790309,0.000014143827,0.000026715747,0.0000799129,0.000057297853,0.9886126,0.0063380017,0.0005353039,0.0013554276,0.00003343595],"about_ca_topic_score_codex":0.010649807,"about_ca_topic_score_gemma":0.014504473,"teacher_disagreement_score":0.010649807,"about_ca_system_score_codex":0.00047792785,"about_ca_system_score_gemma":0.0011137181,"threshold_uncertainty_score":0.021175623},"labels":[],"label_agreement":null},{"id":"W2910207761","doi":"10.1016/j.jsg.2018.12.012","title":"Hot on the trail: Coseismic heating on a localized structure along the Muddy Mountain fault, Nevada","year":2019,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Slip (aerodynamics); Geology; Slipping; Seismology; Episodic tremor and slip; Thermal; Earthquake rupture; Thrust fault; Subduction; Fault (geology); Tectonics; Geometry; Meteorology","score_opus":0.012781479824464268,"score_gpt":0.22452218059202098,"score_spread":0.21174070076755672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910207761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992379,0.000013577383,0.000016902193,0.000028164372,0.0000018175434,0.0000016103587,0.00007006934,0.0000018887894,0.00062816817],"genre_scores_gemma":[0.9994456,0.000015813417,0.000030867006,0.0000090590665,0.0000024403853,0.0000020715704,0.00010253091,0.0000010958069,0.00039058938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996555,0.0000045419474,0.000001507126,0.000009207031,0.0000065678305,0.000012641125],"domain_scores_gemma":[0.99988115,0.000016873715,0.000026432326,0.000008698262,0.000030947675,0.000035813857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007191977,0.00008463314,0.00013833861,0.00038892034,0.00092691684,0.00036169004,0.00030087354,0.00030320225,0.0012738724],"category_scores_gemma":[0.00023939155,0.000093466326,0.000073167364,0.00039804247,0.00035261305,0.00019887096,0.0005026605,0.00019184517,0.00010426622],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022630983,0.00014019864,0.9770602,0.000022185355,0.000037571644,0.00094837596,0.002501028,0.0009877641,0.009497137,0.00023705848,0.00082374254,0.007518405],"study_design_scores_gemma":[0.0000055315677,0.000021210673,0.9965132,0.00000446397,0.000006141514,0.000067649846,0.002276473,0.00039236722,0.00014541108,0.000034034,0.00053113385,0.0000024982783],"about_ca_topic_score_codex":0.13544545,"about_ca_topic_score_gemma":0.45714828,"teacher_disagreement_score":0.13544545,"about_ca_system_score_codex":0.00056282955,"about_ca_system_score_gemma":0.0006561161,"threshold_uncertainty_score":0.2693141},"labels":[],"label_agreement":null},{"id":"W2962832146","doi":"10.1016/j.jsg.2019.103867","title":"Evolution of gold-bearing splays of crustal-scale fault zones of the south-central Archean Abitibi subprovince: Constraints from the Kirana deformation zone, Kirkland Lake, Ontario, Canada","year":2019,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Barcelona Macula Foundation; Society of Economic Geologists Canada Foundation; Colorado School of Mines","keywords":"Geology; Archean; Geochemistry; Greenstone belt; Fault (geology); Deformation (meteorology); Geomorphology; Paleontology","score_opus":0.0054889626251976836,"score_gpt":0.17552180971132653,"score_spread":0.17003284708612884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2962832146","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972024,0.00013660693,0.000052415475,0.00003831625,0.0000011787747,0.0000051334287,0.00053882675,0.0000059523036,0.0020191132],"genre_scores_gemma":[0.99888724,0.00006737069,0.00007105754,0.0000062582203,5.023413e-7,0.0000021941703,0.0002812053,0.0000035355476,0.0006807519],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998103,0.000012137068,0.0000116326655,0.00003665353,0.000056955832,0.00007235257],"domain_scores_gemma":[0.9994655,0.00004241077,0.00010132604,0.000018007137,0.00028041875,0.00009230365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020793048,0.0002463707,0.00028262302,0.002283658,0.0014245271,0.0015203882,0.00068568275,0.00037077395,0.0028084833],"category_scores_gemma":[0.0008886251,0.00032392345,0.00022868169,0.0037420664,0.0009227431,0.00032923964,0.00079683244,0.00027631118,0.00046146862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016597843,0.00002631608,0.975031,0.00005124946,0.0000718467,0.00019279502,0.0039736666,0.0010779633,0.006499167,0.00045520937,0.00049213675,0.011962694],"study_design_scores_gemma":[0.0000022738939,0.0000037397476,0.9985667,0.000005571421,0.000004651981,0.000018652965,0.000818999,0.00018975612,0.000050068105,0.000016842487,0.00031975313,0.0000030850167],"about_ca_topic_score_codex":0.94667155,"about_ca_topic_score_gemma":0.9860088,"teacher_disagreement_score":0.053328454,"about_ca_system_score_codex":0.00733657,"about_ca_system_score_gemma":0.0055757384,"threshold_uncertainty_score":0.10728496},"labels":[],"label_agreement":null},{"id":"W2963398344","doi":"10.1016/j.jsg.2019.103869","title":"Pan-African structural evolution of Paleoproterozoic basement gneiss and Cu-Co mineralized shear zones in the Domes Region of the Lufilian Belt, Mwombezhi Dome, Zambia","year":2019,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Barrick Gold Corporation","keywords":"Geology; Dome (geology); Shear zone; Gneiss; Basement; Geochemistry; Shear (geology); Metallogeny; Geomorphology; Seismology; Mining engineering; Petrology; Tectonics; Metamorphic rock; Pyrite; Archaeology","score_opus":0.007216135380747248,"score_gpt":0.20599858634433504,"score_spread":0.1987824509635878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963398344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990375,0.00023866649,0.00002518272,0.000023416735,7.36372e-7,0.0000035532112,0.0001497543,0.0000017629557,0.0005194682],"genre_scores_gemma":[0.9995136,0.00013521287,0.00007329408,0.0000035770236,5.46594e-7,0.000002770475,0.00008160149,0.0000012097146,0.00018815842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.0000065128943,0.0000051343372,0.000013501492,0.00000622012,0.000030479665],"domain_scores_gemma":[0.9999238,0.000008622253,0.000031271848,0.0000044298595,0.000020829299,0.000010987612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015236362,0.00025207252,0.00018066201,0.001988554,0.00056909095,0.0006273178,0.00022433014,0.0002020383,0.0016042358],"category_scores_gemma":[0.00031093849,0.00028524504,0.000139424,0.0020667405,0.00045768268,0.0002886912,0.00053300656,0.00018484324,0.00017763009],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060322054,0.00005235308,0.91808784,0.00023486103,0.00012527342,0.0009921921,0.010390432,0.00080528174,0.0400089,0.0022048587,0.0002899151,0.02620484],"study_design_scores_gemma":[0.000002441559,0.000008075096,0.9985122,0.000012090472,0.000009489659,0.000053181142,0.00074483274,0.00009196995,0.00016723746,0.000018093091,0.00037906994,0.000001280266],"about_ca_topic_score_codex":0.1522962,"about_ca_topic_score_gemma":0.35265,"teacher_disagreement_score":0.1522962,"about_ca_system_score_codex":0.0012786338,"about_ca_system_score_gemma":0.0005991908,"threshold_uncertainty_score":0.30281943},"labels":[],"label_agreement":null},{"id":"W3009287924","doi":"10.1016/j.jsg.2020.104032","title":"Subvertical, linear and progressive deformation related to gold mineralization at the Galat Sufar South deposit, Nubian Shield, NE Sudan","year":2020,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada); Barrick Gold (Canada)","funders":"Association Nationale de la Recherche et de la Technologie","keywords":"Geology; Shear zone; Lineation; Overprinting; Shearing (physics); Mineralization (soil science); Geochemistry; Shield; Gold ore; Tectonics; Craton; Shear (geology); Seismology; Petrology; Geotechnical engineering","score_opus":0.00976453795590674,"score_gpt":0.20403381051460762,"score_spread":0.19426927255870088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009287924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999607,0.000021918904,0.000009697492,0.0000060308726,6.1035837e-7,0.0000011566781,0.00006150904,8.0449985e-7,0.0002912724],"genre_scores_gemma":[0.99966,0.000023161456,0.000029158142,0.0000037496557,9.066278e-7,0.0000016842533,0.00008488162,5.1812475e-7,0.0001959282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.000018335946,0.00000972624,0.000017807708,0.000014196905,0.000032789703],"domain_scores_gemma":[0.9998605,0.00002450408,0.000041370302,0.0000103291595,0.000032590866,0.00003077997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021929249,0.00021301972,0.00019301468,0.0014974525,0.00092374417,0.00066344975,0.0002869895,0.0003044365,0.0009263588],"category_scores_gemma":[0.00035554267,0.00017212538,0.00016474091,0.0012663233,0.0007035818,0.00018198602,0.0005599012,0.00015323593,0.00015087597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001606702,0.00004703579,0.98432356,0.000025508953,0.000046140118,0.0006352176,0.0016952356,0.0007681715,0.007024221,0.00020720354,0.00011218,0.004954911],"study_design_scores_gemma":[0.0000012907133,0.000007896894,0.9991208,0.0000029300213,0.0000030445938,0.000036377543,0.00053100457,0.00012009175,0.000063013686,0.000011245146,0.000101105696,0.0000013022254],"about_ca_topic_score_codex":0.10740142,"about_ca_topic_score_gemma":0.23941348,"teacher_disagreement_score":0.10740142,"about_ca_system_score_codex":0.0010521149,"about_ca_system_score_gemma":0.00079509284,"threshold_uncertainty_score":0.2135526},"labels":[],"label_agreement":null},{"id":"W3037066864","doi":"10.1016/j.jsg.2020.104096","title":"Tourmaline microboudinage: An indicator of its host rheology","year":2020,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Mylonite; Tourmaline; Lineation; Differential stress; Mineralogy; Quartz; Metamorphic rock; Rheology; Foliation (geology); Brittleness; Shear zone; Petrology; Deformation (meteorology); Seismology; Geochemistry; Tectonics; Composite material; Materials science","score_opus":0.01591869512116961,"score_gpt":0.21986678817802954,"score_spread":0.20394809305685993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3037066864","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99591845,0.000118098025,0.000076814,0.00004608451,0.0000054757957,0.000005127298,0.0009921902,0.000017472767,0.002820341],"genre_scores_gemma":[0.99857676,0.00006791243,0.00012065102,0.000007482827,0.0000049678947,0.0000045040474,0.0005041609,0.000005831317,0.00070769276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999417,0.00000781673,0.000003685551,0.000012309294,0.000017326818,0.000017221942],"domain_scores_gemma":[0.99965537,0.00005183354,0.00011825154,0.000016729733,0.00008309806,0.00007481603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000073312425,0.00018562745,0.00013194745,0.001157681,0.0005069374,0.00072785997,0.00017185938,0.00034273343,0.0034991645],"category_scores_gemma":[0.00059419783,0.000079452075,0.00010447024,0.0012379421,0.0003234371,0.0003994554,0.0005559651,0.00026628384,0.0004904708],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032665883,0.000020394313,0.9589929,0.00010820131,0.00007229033,0.00048747438,0.0019555057,0.00051775586,0.027064174,0.00031806531,0.0007504738,0.0093861725],"study_design_scores_gemma":[0.0000032843166,0.000041807998,0.9946077,0.000010541905,0.000011395246,0.00018556569,0.0011065875,0.0006514136,0.00080854265,0.00002165909,0.0025452336,0.0000062424833],"about_ca_topic_score_codex":0.03935987,"about_ca_topic_score_gemma":0.056542054,"teacher_disagreement_score":0.03935987,"about_ca_system_score_codex":0.0006006308,"about_ca_system_score_gemma":0.00033191088,"threshold_uncertainty_score":0.078261554},"labels":[],"label_agreement":null},{"id":"W3047181794","doi":"10.1016/j.jsg.2020.104134","title":"Intracrystalline vorticity record of flow kinematics during shear zone reactivation","year":2020,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Resources Canada; Canada Foundation for Innovation","keywords":"Geology; Shear zone; Vorticity; Shear (geology); Kinematics; Transpression; Simple shear; Finite strain theory; Monoclinic crystal system; Geometry; Electron backscatter diffraction; Seismology; Diffraction; Petrology; Crystal structure; Crystallography; Mechanics; Vortex; Tectonics; Physics; Optics; Chemistry","score_opus":0.013661576826968962,"score_gpt":0.1990233240703845,"score_spread":0.18536174724341553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047181794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99759775,0.000047463192,0.00027481868,0.000011123333,0.0000043047353,0.0000033641732,0.00065502204,0.000030492922,0.0013756609],"genre_scores_gemma":[0.9990846,0.000024863628,0.00019283713,0.0000036372944,0.000006019586,0.0000030776516,0.00038666753,0.00000896248,0.0002893233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995875,0.0000024178314,0.0000028056675,0.00001163295,0.000009932754,0.000014417726],"domain_scores_gemma":[0.99971753,0.000060537463,0.000056122928,0.00003160105,0.00008115407,0.000053011107],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000086312524,0.00010927055,0.00022279054,0.00072579656,0.0003531323,0.0005405933,0.00019833712,0.00018846148,0.0022784348],"category_scores_gemma":[0.00034614932,0.00017404625,0.0001133451,0.00070016645,0.00026143895,0.0002768037,0.0003150498,0.00034128514,0.00047105734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013023491,0.0002586569,0.59933734,0.00006289086,0.00007196801,0.0004474077,0.00088496384,0.0016728797,0.36247507,0.0005563525,0.00084397226,0.032086056],"study_design_scores_gemma":[0.000009300145,0.000050263407,0.9941789,0.000004786894,0.00001149334,0.000059932263,0.00007885336,0.0012394941,0.0039859833,0.000024550525,0.00035251418,0.000004091469],"about_ca_topic_score_codex":0.008942209,"about_ca_topic_score_gemma":0.0160635,"teacher_disagreement_score":0.008942209,"about_ca_system_score_codex":0.00020771746,"about_ca_system_score_gemma":0.00026203762,"threshold_uncertainty_score":0.017780364},"labels":[],"label_agreement":null},{"id":"W3085407118","doi":"10.1016/j.jsg.2020.104176","title":"Deformation history of the Qianlishan Complex, Khondalite Belt, North China: Structures, ages and tectonic implications","year":2020,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Geology; Craton; Granulite; Metamorphism; Lineation; Terrane; Geochemistry; Zircon; Petrology; Shear zone; Tectonics; Seismology; Paleontology; Facies; Structural basin","score_opus":0.018391449293844165,"score_gpt":0.1954431873747417,"score_spread":0.17705173808089752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3085407118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990232,0.00009088672,0.0000490421,0.00002366826,7.094525e-7,0.0000033222793,0.00010905263,0.0000035536418,0.0006965175],"genre_scores_gemma":[0.9992908,0.000050092083,0.00004960434,0.0000044267467,9.3030576e-7,0.0000027938986,0.0001471804,0.000001263782,0.0004527664],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999058,0.00001093913,0.000011242792,0.000032199976,0.000020859616,0.000018953524],"domain_scores_gemma":[0.99985397,0.000018073502,0.000039607996,0.000013586013,0.000044120265,0.000030721203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022352888,0.0002486994,0.00020895501,0.0017467105,0.00072946266,0.00046158256,0.0004139748,0.00023434062,0.0013952524],"category_scores_gemma":[0.00029812497,0.00024749467,0.00015697787,0.0022743952,0.0006051548,0.000376521,0.0005272045,0.000111658635,0.00018268371],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015771342,0.000044179993,0.9525959,0.0000910448,0.00009297668,0.00031399808,0.004566498,0.0013899917,0.0147359455,0.000929613,0.00024857896,0.02483351],"study_design_scores_gemma":[0.000002310086,0.000010296372,0.99893254,0.0000018975503,0.0000059619024,0.00003484883,0.00020387801,0.00034157862,0.000086352,0.000033883203,0.0003437921,0.0000026110336],"about_ca_topic_score_codex":0.08667065,"about_ca_topic_score_gemma":0.15345697,"teacher_disagreement_score":0.08667065,"about_ca_system_score_codex":0.0010842192,"about_ca_system_score_gemma":0.0012912952,"threshold_uncertainty_score":0.17233229},"labels":[],"label_agreement":null},{"id":"W313264713","doi":"10.1016/j.jsg.2015.05.002","title":"Quantifying the three-dimensional shapes of spheroidal objects in rocks imaged by tomography","year":2015,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of Toronto","funders":"","keywords":"Ellipsoid; Tomography; Geology; Population; Chondrule; Geometry; Chondrite; Mathematics; Physics; Geodesy; Optics; Meteorite","score_opus":0.02389127517557748,"score_gpt":0.25093647139772957,"score_spread":0.22704519622215208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W313264713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9434659,0.00019443844,0.054040812,0.00011243172,0.0000065586937,0.000030621784,0.00047816802,0.000243344,0.0014278047],"genre_scores_gemma":[0.9845333,0.00013797329,0.014899475,0.000013376636,0.0000046802884,0.0000064394485,0.00021440434,0.000035620447,0.0001546774],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983644,0.000022507356,0.000015472768,0.000038782113,0.00006194616,0.0000247567],"domain_scores_gemma":[0.9990576,0.00034593424,0.0002540788,0.00010645179,0.00016393738,0.00007204496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036235285,0.0003573661,0.00021836361,0.0013397385,0.00024899808,0.0014886396,0.00036623413,0.0005791752,0.0007069945],"category_scores_gemma":[0.0026017148,0.0004764625,0.00021361609,0.0010700878,0.0006978043,0.0013968406,0.0008059857,0.00041631944,0.00023082738],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004988098,0.00014881765,0.2424205,0.0003360672,0.00017786917,0.0006989502,0.0013354623,0.21600692,0.44748884,0.0067076315,0.0008144978,0.0833656],"study_design_scores_gemma":[0.000029980629,0.0000890457,0.2617463,0.000049093986,0.000116423034,0.0013167533,0.0012891028,0.6438297,0.0844346,0.005019511,0.0019283866,0.00015110782],"about_ca_topic_score_codex":0.0035184764,"about_ca_topic_score_gemma":0.00526602,"teacher_disagreement_score":0.0035184764,"about_ca_system_score_codex":0.00035247693,"about_ca_system_score_gemma":0.0005806072,"threshold_uncertainty_score":0.006995976},"labels":[],"label_agreement":null},{"id":"W3132986415","doi":"10.1016/j.jsg.2021.104306","title":"The role of structural reactivation for gold mineralization in northeastern Hunan Province, South China","year":2021,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":43,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"National Key Research and Development Program of China Stem Cell and Translational Research; National Natural Science Foundation of China","keywords":"Mineralization (soil science); Geology; Overprinting; Geochemistry; Paleozoic; Gold ore; Tectonics; Cretaceous; Paleontology; Metamorphic rock","score_opus":0.006230997307464333,"score_gpt":0.21510403947302487,"score_spread":0.20887304216556055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3132986415","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988926,0.0001570987,0.000095596,0.00012918988,0.0000031142995,0.0000048477978,0.00008973675,0.000005732303,0.0006221301],"genre_scores_gemma":[0.9995321,0.000065144384,0.00006537672,0.000011600473,0.0000021872816,0.000001935914,0.0000590492,0.0000011704404,0.0002615934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974746,0.000028653785,0.00002986062,0.000067763016,0.000048703907,0.000077483804],"domain_scores_gemma":[0.99960023,0.00006109045,0.00012395624,0.00002646288,0.00012318578,0.00006509312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005186437,0.00031139713,0.00032008855,0.002362917,0.0013547158,0.00090773904,0.0009709525,0.00042577175,0.0011136486],"category_scores_gemma":[0.000701026,0.00031202802,0.0003975298,0.0026041623,0.001071026,0.00067222817,0.0009439128,0.00023824941,0.00006244167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000080375175,0.000040040057,0.9818704,0.00006965438,0.00009360533,0.0003857468,0.0013385009,0.00093479856,0.00360546,0.0007201384,0.00018688574,0.0106743965],"study_design_scores_gemma":[0.00000513049,0.000011243874,0.9968959,0.0000090265075,0.000028604172,0.000036895697,0.0011566812,0.0011581315,0.00017021832,0.00016680776,0.0003553587,0.0000060847924],"about_ca_topic_score_codex":0.26032624,"about_ca_topic_score_gemma":0.45037267,"teacher_disagreement_score":0.26032624,"about_ca_system_score_codex":0.0024941224,"about_ca_system_score_gemma":0.0051663704,"threshold_uncertainty_score":0.51762193},"labels":[],"label_agreement":null},{"id":"W3133582676","doi":"10.1016/j.jsg.2021.104459","title":"A refined approach for quantitative kinematic vorticity number estimation using microstructures","year":2021,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Vorticity; Kinematics; Geology; Microscale chemistry; Shear (geology); Geometry; Shear zone; Geodesy; Mechanics; Seismology; Mathematics; Tectonics; Vortex; Classical mechanics; Physics; Petrology","score_opus":0.031218364070300243,"score_gpt":0.28325264539347256,"score_spread":0.2520342813231723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3133582676","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0050358167,0.00004178497,0.99448556,0.0000130793405,0.000007732421,0.000013520183,0.000060238563,0.00017719473,0.00016511437],"genre_scores_gemma":[0.19314256,0.00020501259,0.80467844,0.000030289986,0.0000451338,0.00008266788,0.0004363062,0.00010904899,0.0012705176],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99964297,0.00007811866,0.000027196633,0.000091245,0.00013362455,0.000026915952],"domain_scores_gemma":[0.99913883,0.00023728263,0.000101299294,0.00018390016,0.0003030969,0.00003561961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006882774,0.0007200039,0.00088911154,0.0020046933,0.00031011988,0.001127755,0.0010776407,0.0007180328,0.0014214951],"category_scores_gemma":[0.0027540552,0.0006038138,0.0006099124,0.001028393,0.0004546049,0.0013381591,0.0011710385,0.000790801,0.0006502886],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016546107,0.00012947677,0.0066089476,0.00019703894,0.00014781016,0.00015661985,0.00016741708,0.2870523,0.09542143,0.032712545,0.00170072,0.57554024],"study_design_scores_gemma":[0.0000041709723,0.000024697292,0.00097049586,0.0000072098396,0.000009348573,0.000027570455,0.000008014069,0.99120903,0.0024942844,0.0045661028,0.0006666082,0.000012477627],"about_ca_topic_score_codex":0.003929227,"about_ca_topic_score_gemma":0.0048650526,"teacher_disagreement_score":0.003929227,"about_ca_system_score_codex":0.0003173045,"about_ca_system_score_gemma":0.000727602,"threshold_uncertainty_score":0.007812738},"labels":[],"label_agreement":null},{"id":"W3150742605","doi":"10.1016/j.jsg.2021.104328","title":"Selective clast survival in an experimentally-produced pseudotachylyte","year":2021,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; H2020 European Research Council; Università degli Studi di Padova","keywords":"Plagioclase; Geology; Quartz; Slip (aerodynamics); Sillimanite; Mineralogy; Ilmenite; Mineral; Geochemistry; Petrology; Biotite; Materials science","score_opus":0.020170664320137466,"score_gpt":0.2628213091545839,"score_spread":0.24265064483444643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3150742605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994961,0.000018686018,0.00012985135,0.000011185664,0.0000037595637,0.000005390896,0.000044105862,0.000006174012,0.00028468482],"genre_scores_gemma":[0.9988111,0.0000155405,0.0001714509,0.0000124853805,0.0000018023796,0.000011956601,0.000090687616,0.0000119919905,0.00087283785],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997893,0.000035551886,0.000018708566,0.000063494364,0.000046198285,0.000046681293],"domain_scores_gemma":[0.99928904,0.0002829395,0.00010717737,0.00007500089,0.000080855985,0.0001649259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016342511,0.00027144872,0.0003040429,0.0003281191,0.0005465069,0.0003576862,0.0008773525,0.0007252445,0.0024421876],"category_scores_gemma":[0.0009242474,0.00033685903,0.00020055122,0.00014794071,0.0008098269,0.0001914459,0.00065002893,0.0007600033,0.00029123787],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006023428,0.00007860285,0.002156933,0.000018456582,0.000008744393,0.00019973544,0.00012512626,0.00023860445,0.9952674,0.00016497208,0.000023768138,0.0011152668],"study_design_scores_gemma":[0.0003975128,0.007447948,0.18063422,0.000041649153,0.00014160853,0.0029911073,0.001243465,0.016856058,0.78700763,0.00062502216,0.0025180723,0.000095789714],"about_ca_topic_score_codex":0.004974078,"about_ca_topic_score_gemma":0.008039156,"teacher_disagreement_score":0.004974078,"about_ca_system_score_codex":0.00061701774,"about_ca_system_score_gemma":0.00049747614,"threshold_uncertainty_score":0.009890258},"labels":[],"label_agreement":null},{"id":"W4245135237","doi":"10.1016/j.jsg.2007.07.007","title":"Photograph of the Month","year":2007,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Medical Case Reports and Studies","field":"Medicine","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Paleontology","score_opus":0.011684674321628022,"score_gpt":0.2853535203346501,"score_spread":0.2736688460130221,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245135237","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0028632323,0.0034013726,0.00047568593,0.027998306,0.08781844,0.00013289899,0.0027318443,0.0006263887,0.8739519],"genre_scores_gemma":[0.0068279444,0.0010028721,0.00030775648,0.0025019804,0.004153039,0.000014693151,0.00048642515,0.00018914382,0.98451614],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998141,0.000022352391,0.0000069354787,0.000033456337,0.00008478151,0.000038427268],"domain_scores_gemma":[0.9994211,0.00006354269,0.000025114501,0.00008161782,0.00024214548,0.00016648875],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025163672,0.00066787563,0.00048250603,0.0016214611,0.002750651,0.0021692985,0.0006979636,0.0017522991,0.44435343],"category_scores_gemma":[0.0014882145,0.0003081788,0.0006917389,0.001049667,0.00043611464,0.001165863,0.001183711,0.003544583,0.14664641],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046322868,0.000010225455,0.00010162241,0.000026442855,0.000002115893,0.00041054212,0.00002692428,0.000016039472,0.00013434477,0.00062546914,0.98784167,0.0107583385],"study_design_scores_gemma":[0.000005215086,0.0000080076325,0.0006499015,0.00002468007,0.0000021919477,0.00030217422,0.00011118913,0.000025210273,0.00006473234,0.00017456227,0.9986284,0.000003821826],"about_ca_topic_score_codex":0.009820902,"about_ca_topic_score_gemma":0.029734315,"teacher_disagreement_score":0.44435343,"about_ca_system_score_codex":0.00068429427,"about_ca_system_score_gemma":0.0006433434,"threshold_uncertainty_score":0.79256237},"labels":[],"label_agreement":null},{"id":"W4284969768","doi":"10.1016/j.jsg.2022.104673","title":"Strain-rate- and capillary-number-dependent deformation of weak viscous particles","year":2022,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Granular flow and fluidized beds","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Eidgenössische Technische Hochschule Zürich","keywords":"Capillary number; Deformation (meteorology); Simple shear; Capillary action; Particle (ecology); Surface tension; Materials science; Shear (geology); Mechanics; Viscosity; Particle size; Strain rate; Plane stress; Composite material; Geology; Thermodynamics; Physics; Finite element method","score_opus":0.006458033537350371,"score_gpt":0.20751680021143581,"score_spread":0.20105876667408545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4284969768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996375,0.00010320296,0.0022259625,0.000090738096,0.000019850204,0.0000070369874,0.000052947657,0.0000182425,0.0011070103],"genre_scores_gemma":[0.99946386,0.000026914724,0.000121888035,0.000006746319,0.0000045406646,0.0000013321612,0.000025546171,0.0000053083922,0.00034391854],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998753,0.000012683383,0.000008733021,0.00002911254,0.000033577584,0.00004058737],"domain_scores_gemma":[0.999238,0.00024427864,0.00013626528,0.00006286675,0.00014311947,0.00017548814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002701127,0.00023717806,0.00028967686,0.000671195,0.00037920757,0.0008128076,0.0004942276,0.00044250058,0.0012733181],"category_scores_gemma":[0.0013772518,0.00023613265,0.00025108934,0.00033687605,0.001304357,0.0007115555,0.00037183144,0.00056700915,0.00015776808],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001978542,0.000795942,0.034822747,0.00021763639,0.00012292716,0.0013437574,0.0007170671,0.1966194,0.7130694,0.023118984,0.0013158944,0.025877746],"study_design_scores_gemma":[0.000046000223,0.00016713672,0.052258987,0.000008061561,0.000021704673,0.00015989202,0.00013660971,0.8355216,0.10896489,0.0023543523,0.00027724204,0.00008358864],"about_ca_topic_score_codex":0.0025630775,"about_ca_topic_score_gemma":0.0017449503,"teacher_disagreement_score":0.0025630775,"about_ca_system_score_codex":0.000501745,"about_ca_system_score_gemma":0.000447818,"threshold_uncertainty_score":0.0050962567},"labels":[],"label_agreement":null},{"id":"W4292242318","doi":"10.1016/j.jsg.2022.104704","title":"Influence of décollement-cover thickness variations in fold-and-thrust belts: Insights from centrifuge analog modeling","year":2022,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Ministerio de Economía y Competitividad","keywords":"Geology; Décollement; Anticline; Sedimentary rock; Fold (higher-order function); Wedge (geometry); Structural basin; Geomorphology; Geometry; Petrology; Paleontology","score_opus":0.011487201866094202,"score_gpt":0.21721539656626476,"score_spread":0.20572819470017056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292242318","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99283147,0.000042642132,0.0037569571,0.00009987457,0.000006167413,0.000011678307,0.00010299031,0.000053752243,0.0030944538],"genre_scores_gemma":[0.99935824,0.000021470103,0.00027624494,0.000007409107,0.0000021197263,0.0000031232128,0.000021323143,0.000007272776,0.00030269544],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998983,0.000035434507,0.0000068710488,0.000021566319,0.000011958925,0.000025833495],"domain_scores_gemma":[0.9996965,0.00012426989,0.00007188096,0.00003347107,0.000026717194,0.000047190886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021785434,0.00040469307,0.00029493743,0.0005210407,0.0002873383,0.0008694888,0.0006136219,0.0007813825,0.0015947677],"category_scores_gemma":[0.0014227146,0.00028286618,0.00049457257,0.00031736353,0.00068209326,0.00051309547,0.0005224529,0.00028367856,0.00010866476],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004779305,0.000045208442,0.011202181,0.000012471724,0.000015952884,0.00015171836,0.000044137487,0.98278266,0.002697237,0.0013507815,0.00006573989,0.0015841072],"study_design_scores_gemma":[0.000009496255,0.000014866681,0.003980289,0.0000020774778,0.0000059008817,0.000016171645,0.000018251763,0.9954465,0.00020026657,0.00023110323,0.00006862938,0.000006485723],"about_ca_topic_score_codex":0.028193336,"about_ca_topic_score_gemma":0.013004329,"teacher_disagreement_score":0.028193336,"about_ca_system_score_codex":0.0010189625,"about_ca_system_score_gemma":0.0004197891,"threshold_uncertainty_score":0.056058466},"labels":[],"label_agreement":null},{"id":"W4313547616","doi":"10.1016/j.jsg.2022.104781","title":"West Spitsbergen fold and thrust belt: A digital educational data package for teaching structural geology","year":2023,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Geology; Foreland basin; Structural geology; Fold (higher-order function); Historical geology; Geologic map; Geospatial analysis; Archipelago; Structural basin; Earth science; Paleontology; Seismology; Remote sensing; Oceanography","score_opus":0.03201743846496107,"score_gpt":0.2815042303407133,"score_spread":0.24948679187575223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313547616","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.047432702,0.00027053873,0.13177626,0.0009281473,0.0001534609,0.0006497413,0.7158613,0.045637913,0.05728995],"genre_scores_gemma":[0.1220303,0.00061535137,0.17433412,0.00017481922,0.0000698524,0.0011942614,0.6679593,0.009452287,0.024169654],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996307,0.00005467341,0.00006927164,0.000075942284,0.00013426006,0.000035153902],"domain_scores_gemma":[0.9980773,0.00076297176,0.000169343,0.00042321783,0.0003984241,0.00016871207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009847897,0.000496275,0.0003524588,0.0043411553,0.0004118267,0.0012008814,0.0009854335,0.00041595567,0.031414878],"category_scores_gemma":[0.0040133856,0.00036298987,0.00034146605,0.005016985,0.00032589005,0.0016358474,0.0016618099,0.0006593328,0.010906154],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003987739,0.0004841482,0.02494067,0.0010429102,0.000069195536,0.00040107412,0.002699731,0.011766605,0.008549106,0.024712902,0.39098927,0.5339456],"study_design_scores_gemma":[0.000103338025,0.000057240046,0.03830309,0.00017759498,0.000040181483,0.00019513066,0.0005999169,0.0078902645,0.007904164,0.0066927867,0.937974,0.000062345855],"about_ca_topic_score_codex":0.02081803,"about_ca_topic_score_gemma":0.03075366,"teacher_disagreement_score":0.031414878,"about_ca_system_score_codex":0.0008085716,"about_ca_system_score_gemma":0.001717733,"threshold_uncertainty_score":0.10509318},"labels":[],"label_agreement":null},{"id":"W4323306183","doi":"10.1016/j.jsg.2023.104834","title":"Oblique lateral extrusion during dextral transpression along the Beardmore-Geraldton belt, Canada","year":2023,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Laurentian University","funders":"Natural Resources Canada","keywords":"Transpression; Geology; Sinistral and dextral; Lineation; Shear zone; Shear (geology); Seismology; Shearing (physics); Fold (higher-order function); Petrology; Paleontology; Geomorphology; Geochemistry; Tectonics; Geotechnical engineering","score_opus":0.007079228931379778,"score_gpt":0.19072949510251144,"score_spread":0.18365026617113167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323306183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99732363,0.00007819657,0.000037884427,0.000036391986,0.0000026759667,0.000006002419,0.00029153776,0.0000036931087,0.0022198735],"genre_scores_gemma":[0.9982705,0.00006147063,0.000058277255,0.000011309754,0.0000013647847,0.0000030039998,0.00022444979,0.000004391074,0.0013652267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997669,0.000011036891,0.000008614209,0.00004273664,0.0000652407,0.000105611616],"domain_scores_gemma":[0.99954885,0.000044703094,0.00008454977,0.000011844055,0.00022896091,0.00008095827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020906939,0.00024779877,0.00033087243,0.0011678905,0.0023616415,0.0014445914,0.0006058317,0.00052182376,0.0032350835],"category_scores_gemma":[0.00087021734,0.0002471518,0.00020050917,0.0018449252,0.00097399415,0.00033611286,0.0009266762,0.00035195766,0.0003441807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046516137,0.000061977466,0.96399826,0.000054397784,0.000061581944,0.00057651766,0.00680456,0.00087583513,0.0092333695,0.00058902573,0.0009519543,0.016327275],"study_design_scores_gemma":[0.0000018087597,0.000004495749,0.9977822,0.000009482269,0.0000033123158,0.000021069156,0.0015033134,0.00013697134,0.000092549606,0.000010709789,0.00043054408,0.0000035642604],"about_ca_topic_score_codex":0.966393,"about_ca_topic_score_gemma":0.9904998,"teacher_disagreement_score":0.033607006,"about_ca_system_score_codex":0.008627791,"about_ca_system_score_gemma":0.008767668,"threshold_uncertainty_score":0.06760979},"labels":[],"label_agreement":null},{"id":"W4366779099","doi":"10.1016/j.jsg.2023.104864","title":"3-D hydromechanical simulation of intersecting faults: Influences on fluid circulation and formation of oriented-orebodies","year":2023,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"iNano Medical (Canada)","funders":"Agence Nationale de la Recherche; Université de Lorraine","keywords":"Geology; Structural basin; Fluid dynamics; Unconformity; Petrology; Fault (geology); Fault block; Permeability (electromagnetism); Geotechnical engineering; Differential stress; Petroleum reservoir; Oil field; Geomorphology; Petroleum engineering; Seismology; Mechanics","score_opus":0.02144830516605369,"score_gpt":0.2627763381222311,"score_spread":0.2413280329561774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366779099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942762,0.000032356715,0.0023800624,0.00014805941,0.000037864927,0.000016778393,0.00054353854,0.00016545519,0.002399703],"genre_scores_gemma":[0.99903226,0.000016711367,0.00054546515,0.000016729737,0.0000053554018,0.0000071986233,0.00012855821,0.00001445232,0.00023313655],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989676,0.000023555074,0.000009310897,0.000024066823,0.000014733657,0.00003156984],"domain_scores_gemma":[0.9993469,0.00032583522,0.00006618583,0.00004278057,0.00007568628,0.00014257159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021483365,0.00043632588,0.0004702496,0.00062820385,0.0005427786,0.000850485,0.00064727984,0.0017455469,0.0034800114],"category_scores_gemma":[0.0012880849,0.00049578375,0.00069463707,0.00060511153,0.00086206634,0.00047583051,0.00047026374,0.0006088591,0.00024048392],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001020675,0.00011416735,0.009529029,0.000015872492,0.000027651591,0.0001337333,0.000048462527,0.98696077,0.0015805049,0.0002556531,0.00017569005,0.0010564887],"study_design_scores_gemma":[0.000026401112,0.000020820029,0.004017895,0.0000022212287,0.000007427823,0.000007219755,0.00003477009,0.99549013,0.00025536993,0.00006190405,0.000068683985,0.000007122942],"about_ca_topic_score_codex":0.043989126,"about_ca_topic_score_gemma":0.02737693,"teacher_disagreement_score":0.043989126,"about_ca_system_score_codex":0.0007794752,"about_ca_system_score_gemma":0.0009791832,"threshold_uncertainty_score":0.08746618},"labels":[],"label_agreement":null},{"id":"W4385439858","doi":"10.1016/j.jsg.2023.104920","title":"Fracture spacings of fiber inclusions in a ductile geological matrix and development of microboudins: 3D numerical modeling","year":2023,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Composite Material Mechanics","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Ultimate tensile strength; Composite material; Saturation (graph theory); Materials science; Fracture (geology); Fiber; Brittleness; Volume fraction; Fracture mechanics; Geology; Mathematics","score_opus":0.01200602245088016,"score_gpt":0.24614750117829529,"score_spread":0.23414147872741511,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385439858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9602254,0.00011491229,0.03510894,0.000071204115,0.0000119677525,0.000030052888,0.00021078158,0.0002039107,0.0040227445],"genre_scores_gemma":[0.9938147,0.00004911085,0.0054048896,0.000005047493,0.0000016039176,0.000010309205,0.000035706627,0.000020402906,0.00065818976],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989426,0.00001725384,0.000008484715,0.000031164138,0.000028231752,0.000020593483],"domain_scores_gemma":[0.999421,0.00027225743,0.000117426796,0.00005486196,0.0000960157,0.00003842168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031122082,0.00028327073,0.000250956,0.0006380684,0.0004756795,0.0008383568,0.0007746761,0.0013460033,0.0014798329],"category_scores_gemma":[0.0012182873,0.00053648604,0.00030485878,0.00049513415,0.0007654772,0.0005029081,0.00038281505,0.0003261577,0.00018154822],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048416514,0.00009166048,0.009571333,0.00003069703,0.0000073610636,0.00022036322,0.00021278717,0.97293335,0.009363962,0.0025708668,0.000104315004,0.0048448895],"study_design_scores_gemma":[0.0000035014828,0.000010344764,0.0016475415,0.0000038841727,0.0000032785401,0.00003107343,0.00003521719,0.99636227,0.0016008011,0.00018335045,0.00011088933,0.000007907798],"about_ca_topic_score_codex":0.009876978,"about_ca_topic_score_gemma":0.0125546055,"teacher_disagreement_score":0.009876978,"about_ca_system_score_codex":0.0007396156,"about_ca_system_score_gemma":0.0008793737,"threshold_uncertainty_score":0.019638956},"labels":[],"label_agreement":null},{"id":"W4392859871","doi":"10.1016/j.jsg.2024.105103","title":"Transpression or polyphase deformation along craton margins: Insights from the Archean–Proterozoic boundary near Sudbury, Canada","year":2024,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Laurentian University","funders":"Society of Economic Geologists Canada Foundation","keywords":"Geology; Archean; Proterozoic; Transpression; Craton; Polyphase system; Geochemistry; Deformation (meteorology); Shear zone; Petrology; Seismology; Tectonics","score_opus":0.009656775503395401,"score_gpt":0.20594589337321306,"score_spread":0.19628911786981768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392859871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931549,0.00037974745,0.00009517133,0.000103295584,0.0000037032125,0.000007718916,0.0007087056,0.0000067247934,0.0055401516],"genre_scores_gemma":[0.99862635,0.00019673054,0.00008977377,0.0000135554155,0.0000016331556,0.0000022415302,0.0002445602,0.00000681099,0.00081848376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998574,0.0000052645096,0.000006434883,0.000025773528,0.000035057208,0.00007008804],"domain_scores_gemma":[0.99965036,0.000028638708,0.000039698163,0.000011826814,0.00021333333,0.000056213543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015554391,0.00020228465,0.00030972046,0.002234184,0.002666758,0.0019367444,0.00055387086,0.0003958149,0.003700415],"category_scores_gemma":[0.0007095798,0.000216368,0.00019758966,0.0040427404,0.0010389789,0.0004819133,0.00077005284,0.00039610537,0.00032201043],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003477541,0.000066813685,0.92967993,0.00012804253,0.00008779647,0.0007057999,0.0062541026,0.0031536801,0.015675597,0.0023220815,0.0014357867,0.04014266],"study_design_scores_gemma":[0.0000024936505,0.0000032672338,0.9967326,0.000020408843,0.0000060044363,0.000028017235,0.0014667829,0.0004999643,0.00017964553,0.00006121634,0.0009946923,0.000005031273],"about_ca_topic_score_codex":0.9734212,"about_ca_topic_score_gemma":0.99186736,"teacher_disagreement_score":0.026578784,"about_ca_system_score_codex":0.009522346,"about_ca_system_score_gemma":0.008587028,"threshold_uncertainty_score":0.06908977},"labels":[],"label_agreement":null},{"id":"W4401560684","doi":"10.1016/j.jsg.2024.105233","title":"Refold structures of the Archaean Nyanzaga gold Project, Sukumaland Greenstone Belt, Tanzania: Precursors to the gold-bearing fault system","year":2024,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Vale (Canada)","funders":"Association Nationale de la Recherche et de la Technologie","keywords":"Greenstone belt; Archean; Geology; Bearing (navigation); Tanzania; Geochemistry; Normal fault; Fault (geology); Seismology; Geography","score_opus":0.013468965666988368,"score_gpt":0.24605276677362772,"score_spread":0.23258380110663934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401560684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970854,0.000056141267,0.00018167669,0.000035830733,0.0000020340399,0.000012839649,0.0006185796,0.000013848022,0.0019936124],"genre_scores_gemma":[0.9974281,0.000032949603,0.0006513345,0.000009795815,9.611912e-7,0.000010537244,0.0007773023,0.000009809809,0.0010791033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999928,0.00000912271,0.0000051768397,0.000015595238,0.000016212305,0.00002589005],"domain_scores_gemma":[0.99977344,0.000027629158,0.000052791325,0.000036479465,0.00008356159,0.000026067266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013491852,0.00017670066,0.00010133903,0.0011768877,0.00088250585,0.0004796089,0.00045081208,0.00035862855,0.0040246947],"category_scores_gemma":[0.0007188746,0.0001681633,0.00009151337,0.0014540359,0.0005009627,0.0003080783,0.00069859007,0.0002056463,0.0007054899],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067008275,0.00018707525,0.8511953,0.00022276983,0.00005149124,0.0042983587,0.023409605,0.003985794,0.029292397,0.0036940274,0.002913523,0.08007956],"study_design_scores_gemma":[0.000014844751,0.000056070592,0.98870265,0.000039277787,0.000015629586,0.0003377126,0.0040896772,0.0011170079,0.00088571326,0.00027416408,0.004458555,0.000008816184],"about_ca_topic_score_codex":0.07452211,"about_ca_topic_score_gemma":0.25559658,"teacher_disagreement_score":0.07452211,"about_ca_system_score_codex":0.00069489266,"about_ca_system_score_gemma":0.00076961773,"threshold_uncertainty_score":0.14817667},"labels":[],"label_agreement":null},{"id":"W4401683543","doi":"10.1016/j.jsg.2024.105238","title":"Slip and stress in block-in-matrix shear zones: 2. numerical modelling of a serpentine-filled dilational jog","year":2024,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Advanced ceramic materials synthesis","field":"Materials Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"GNS Science","keywords":"Geology; Slip (aerodynamics); Shear (geology); Shear stress; Matrix (chemical analysis); Shear zone; Block (permutation group theory); Geometry; Seismology; Geotechnical engineering; Mechanics; Petrology; Composite material; Materials science; Mathematics; Tectonics; Physics; Thermodynamics","score_opus":0.01294072906002638,"score_gpt":0.2681405925775062,"score_spread":0.25519986351747986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401683543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.984884,0.00014450631,0.0053523495,0.0003272309,0.00002424173,0.000061112594,0.00064947683,0.00011429081,0.008442789],"genre_scores_gemma":[0.9951373,0.00009843476,0.003061684,0.000055405995,0.0000097346465,0.000052611806,0.00020549774,0.000026993173,0.0013524097],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998839,0.000021550955,0.000008351055,0.000033032873,0.000024831887,0.000028374327],"domain_scores_gemma":[0.99963987,0.00014270195,0.00007764929,0.000031855656,0.000044488206,0.00006347639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022954894,0.00055602076,0.00054980605,0.0005933713,0.0005769803,0.0015672059,0.0011442188,0.0026805012,0.0017669483],"category_scores_gemma":[0.0011745666,0.00043070732,0.00072510313,0.00051185983,0.0015689356,0.0006327236,0.00095337594,0.00066473807,0.00028291013],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004697683,0.00004601649,0.005212214,0.000026165451,0.000014274479,0.00021852975,0.00011197529,0.99020314,0.002371962,0.00092690426,0.00011561706,0.0007062503],"study_design_scores_gemma":[0.000022281374,0.000016880165,0.0015540293,0.000006123697,0.000005078002,0.00003125688,0.00004858153,0.9976254,0.00022237124,0.00027062692,0.00018816904,0.000009269276],"about_ca_topic_score_codex":0.04106344,"about_ca_topic_score_gemma":0.014335285,"teacher_disagreement_score":0.04106344,"about_ca_system_score_codex":0.0013361183,"about_ca_system_score_gemma":0.0008382237,"threshold_uncertainty_score":0.08164883},"labels":[],"label_agreement":null},{"id":"W4402928548","doi":"10.1016/j.jsg.2024.105269","title":"Control of crustal deformation on orogenic Au mineralization in Himalaya: A case study from Buzhu","year":2024,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Fundamental Research Funds for the Central Universities; China University of Geosciences, Beijing; National Natural Science Foundation of China","keywords":"Geology; Mineralization (soil science); Deformation (meteorology); Geochemistry; Seismology","score_opus":0.009753292399557226,"score_gpt":0.22456586803244136,"score_spread":0.21481257563288414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402928548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990932,0.000033967925,0.00002138558,0.000018970295,4.2071267e-7,0.000002568621,0.000036400445,0.0000014414804,0.00079169567],"genre_scores_gemma":[0.9997433,0.000038855833,0.00003215933,0.000002724899,8.181225e-7,9.0583296e-7,0.000020418258,5.615215e-7,0.00016026314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988556,0.000026137554,0.0000062063837,0.000016401073,0.000019504267,0.000046117155],"domain_scores_gemma":[0.9998567,0.000052303243,0.000031401752,0.000011982744,0.000022968205,0.000024586478],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001613806,0.00022369965,0.00022707129,0.0010869458,0.0011844639,0.0007739688,0.00042376315,0.0004572135,0.0014979322],"category_scores_gemma":[0.00033919766,0.00014913028,0.00025979974,0.0015844264,0.0009390429,0.00027590423,0.0005692855,0.0001833316,0.00011632417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057302054,0.00025320178,0.9262034,0.00016380523,0.00022280037,0.018298617,0.0103516,0.007887679,0.015119609,0.002125673,0.00035943824,0.018441169],"study_design_scores_gemma":[0.000013403017,0.00008846211,0.98184216,0.000019876006,0.0000724241,0.0007309252,0.010356235,0.0043297275,0.001365449,0.0002524578,0.0009157824,0.000013208518],"about_ca_topic_score_codex":0.11542672,"about_ca_topic_score_gemma":0.16181006,"teacher_disagreement_score":0.11542672,"about_ca_system_score_codex":0.0015273948,"about_ca_system_score_gemma":0.00066907046,"threshold_uncertainty_score":0.22950971},"labels":[],"label_agreement":null},{"id":"W4408165774","doi":"10.1016/j.jsg.2025.105373","title":"Structural evolution of the southern Swayze greenstone belt, Superior Craton: Implications for the Neoarchean crustal dynamics","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Laurentian University; Geological Survey of Canada; University of Waterloo","funders":"National Key Research and Development Program of China; Natural Sciences and Engineering Research Council of Canada; China National Funds for Distinguished Young Scientists; Chinese Academy of Sciences; University Grants Committee; Key Technologies Research and Development Program; National Natural Science Foundation of China","keywords":"Greenstone belt; Geology; Craton; Geochemistry; Archean; Earth science; Petrology; Seismology; Tectonics","score_opus":0.009792556298817489,"score_gpt":0.22598558448285602,"score_spread":0.21619302818403854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408165774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994342,0.00006740218,0.000015556541,0.000017308843,4.7829724e-7,0.0000017838121,0.000052496925,0.0000020480375,0.0004087644],"genre_scores_gemma":[0.99958855,0.000075768214,0.0000601174,0.000006072285,7.737498e-7,0.0000012287163,0.000084566505,0.0000011379407,0.0001818079],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.0000049255336,0.000004783032,0.00001574317,0.000016814227,0.000017687968],"domain_scores_gemma":[0.99990857,0.0000066205694,0.000029291776,0.000007692941,0.000025265783,0.000022493014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014612066,0.00023057441,0.00020261742,0.0017192635,0.00048170757,0.00057284656,0.00019578107,0.00023718212,0.0010805298],"category_scores_gemma":[0.00030984476,0.00016305591,0.0001697118,0.001861743,0.001073062,0.0002278412,0.00058995927,0.00012229546,0.00013481062],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007205366,0.000017575776,0.96919346,0.000037098147,0.00003416833,0.0003148147,0.0016320283,0.0009754584,0.016130548,0.0003735089,0.00007394274,0.011145329],"study_design_scores_gemma":[8.5926416e-7,0.0000046397895,0.99947983,0.0000027616184,0.0000016142023,0.000021830547,0.00020057373,0.000116389456,0.000047509177,0.000018220286,0.000104846105,9.952252e-7],"about_ca_topic_score_codex":0.19570804,"about_ca_topic_score_gemma":0.37489277,"teacher_disagreement_score":0.19570804,"about_ca_system_score_codex":0.0016492074,"about_ca_system_score_gemma":0.0010846272,"threshold_uncertainty_score":0.3891378},"labels":[],"label_agreement":null},{"id":"W4408674863","doi":"10.1016/j.jsg.2025.105414","title":"Reactivation potential of inherited structures on southwestern Grand Banks, Newfoundland, Canada","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; Canadian Nuclear Safety Commission; McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Paleontology","score_opus":0.008383960132169816,"score_gpt":0.2321761365699931,"score_spread":0.2237921764378233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408674863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99582857,0.0001317268,0.00010205156,0.00006314881,0.000001812913,0.0000067707924,0.0010356572,0.000013960579,0.0028163504],"genre_scores_gemma":[0.9981218,0.00015002597,0.00014802351,0.000013143548,6.941772e-7,0.000002608427,0.0005724918,0.0000022604836,0.0009890294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987435,0.000005409791,0.0000071893714,0.00002636387,0.000030592804,0.00005604476],"domain_scores_gemma":[0.9993888,0.00006219385,0.00015225897,0.000032499654,0.0002834561,0.000080845326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013042834,0.00017991816,0.0001282759,0.00090516487,0.000901202,0.0008974851,0.00039843522,0.0001687335,0.0017249624],"category_scores_gemma":[0.0007369238,0.00014114448,0.00011932906,0.001266117,0.0006681848,0.00022675174,0.000492291,0.0001921051,0.00017427011],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089292356,0.000020497891,0.95697755,0.00004347618,0.000052366366,0.00083291606,0.0010536911,0.006258621,0.0032633953,0.00041812187,0.0020249311,0.028965151],"study_design_scores_gemma":[0.0000037949826,0.000013117894,0.9940393,0.000023245293,0.000017428792,0.000103800725,0.0011793317,0.0029150876,0.00044988215,0.000035082743,0.0012097225,0.000010215622],"about_ca_topic_score_codex":0.97756976,"about_ca_topic_score_gemma":0.99501294,"teacher_disagreement_score":0.022430241,"about_ca_system_score_codex":0.009389729,"about_ca_system_score_gemma":0.006185405,"threshold_uncertainty_score":0.06812757},"labels":[],"label_agreement":null},{"id":"W4409211654","doi":"10.1016/j.jsg.2025.105419","title":"Corrigendum to “Structural evolution of the southern Swayze greenstone belt, Superior Craton: Implications for the Neoarchean crustal dynamics” [J. Struct. Geol. (2025) 105373]","year":2025,"lang":"en","type":"erratum","venue":"Journal of Structural Geology","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Laurentian University; Geological Survey of Canada; University of Waterloo","funders":"","keywords":"struct; Geology; Craton; Greenstone belt; Geochemistry; Earth science; Paleontology; Archean; Tectonics","score_opus":0.0210353476836643,"score_gpt":0.24465238447735616,"score_spread":0.22361703679369185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409211654","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00016238635,0.0013217992,0.0003230772,0.061980497,0.9181264,0.000056435445,0.0033841883,0.0004910658,0.014154084],"genre_scores_gemma":[0.004998154,0.0049954616,0.0015208767,0.07203644,0.145511,0.00022296961,0.0071827983,0.0008771276,0.7626551],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980312,0.00018655919,0.00031742506,0.00036294785,0.00089357485,0.00020826954],"domain_scores_gemma":[0.9860388,0.0011858293,0.00042520018,0.0005985189,0.01109054,0.00066119747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016463905,0.0016911774,0.0016724716,0.003549017,0.0039779693,0.0027002888,0.0028801798,0.0045175552,0.18962754],"category_scores_gemma":[0.015629373,0.0010571616,0.001458436,0.0025620123,0.001369904,0.0018645801,0.00269819,0.0047104666,0.09684949],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006798517,0.000002359616,0.000032912012,0.000027974074,0.0000017895085,0.00002865448,0.000004568925,0.000012840448,0.000014398159,0.00010331922,0.9982912,0.0014731634],"study_design_scores_gemma":[0.000023877757,0.0000150734795,0.0020909463,0.00015630583,0.000014176262,0.00008105081,0.00007066857,0.00011674656,0.00013959335,0.00046566076,0.99679774,0.000028158845],"about_ca_topic_score_codex":0.13733904,"about_ca_topic_score_gemma":0.22278355,"teacher_disagreement_score":0.18962754,"about_ca_system_score_codex":0.004292726,"about_ca_system_score_gemma":0.004879463,"threshold_uncertainty_score":0.63436735},"labels":[],"label_agreement":null},{"id":"W4409359331","doi":"10.1016/j.jsg.2025.105428","title":"Cooling induced fracturing in impact melt dikes derived from drone photogrammetry and Python simulation: Example from the Lesutoskraal Granophyre Dike in South Africa","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Department of Agriculture, Western Cape Government; Hans Merensky Foundation; National Aeronautics and Space Administration; Ministry of Economy, Trade and Industry; USDA Rural Development","keywords":"Dike; Geology; Python (programming language); Drone; Photogrammetry; Seismology; Geomorphology; Mining engineering; Geochemistry; Remote sensing","score_opus":0.013555726725528457,"score_gpt":0.25405565835948574,"score_spread":0.24049993163395728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409359331","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960133,0.00006014463,0.0014585111,0.00004728371,0.000011113771,0.000024349947,0.0008962806,0.00016727934,0.0013217907],"genre_scores_gemma":[0.9967541,0.000050523435,0.002054339,0.0000071949316,0.0000025926097,0.000013544073,0.0007273162,0.000028717956,0.00036175098],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991083,0.000010106918,0.0000068223917,0.000023078952,0.000021548209,0.000027643655],"domain_scores_gemma":[0.999838,0.00007346829,0.000013394468,0.00002025861,0.000032743596,0.000022117425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014990414,0.0006171956,0.00051989296,0.0010915301,0.0005104233,0.0006829798,0.0006053365,0.0014067589,0.0023407147],"category_scores_gemma":[0.00043561973,0.0003327765,0.00085755583,0.0010021639,0.0004973583,0.0002949172,0.00033281298,0.00047285258,0.00026523613],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022427342,0.00021832707,0.046202917,0.00016952456,0.000093796945,0.0014936618,0.00035525585,0.93007225,0.010276018,0.0003794095,0.00051712524,0.009997453],"study_design_scores_gemma":[0.00007431947,0.00006809052,0.047246855,0.00003070813,0.00003244069,0.00016777276,0.00057660893,0.94791275,0.0026333516,0.00018924264,0.0010274095,0.000040482544],"about_ca_topic_score_codex":0.072030045,"about_ca_topic_score_gemma":0.089544535,"teacher_disagreement_score":0.072030045,"about_ca_system_score_codex":0.00069067837,"about_ca_system_score_gemma":0.0005536363,"threshold_uncertainty_score":0.14322156},"labels":[],"label_agreement":null},{"id":"W4410552378","doi":"10.1016/j.jsg.2025.105463","title":"Quantitative characterization of fracture networks in the Permian organic-rich shales of the Whitehill formation in the Karoo Basin, South Africa and implication for hydrocarbon exploration, CO2 sequestration, and other fractured geofluid systems","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Permian; Geochemistry; Structural basin; Organic matter; Hydrocarbon; Petrology; Paleontology","score_opus":0.012949443063946506,"score_gpt":0.2362489432620816,"score_spread":0.2232995001981351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410552378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995758,0.000019371078,0.00017942651,0.0000016142897,1.5177947e-7,0.0000035641694,0.00014000897,0.0000033220886,0.00007673929],"genre_scores_gemma":[0.99926347,0.000026028687,0.0004372124,0.0000011040802,5.703255e-7,0.0000061570013,0.00017847666,0.0000011451715,0.00008575074],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999168,0.000007007272,0.0000069568,0.00003167494,0.000018202176,0.000019346258],"domain_scores_gemma":[0.9998276,0.00003777707,0.00006745702,0.000010583657,0.00003260204,0.000023917994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011789052,0.0001689734,0.00013551148,0.0019608785,0.00023622994,0.00029356196,0.00021614242,0.00025684576,0.00048747152],"category_scores_gemma":[0.00029355864,0.00016185279,0.00014292735,0.00070266577,0.00032396975,0.0002092397,0.00023569516,0.00008605865,0.00006448303],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001351004,0.00006819966,0.8688467,0.00007950009,0.000049270544,0.00037368288,0.00092069554,0.006412986,0.10835523,0.00014905044,0.000048297847,0.014561443],"study_design_scores_gemma":[0.0000022661798,0.000032256576,0.992671,0.0000052511477,0.000008064552,0.00013444868,0.00036293408,0.004787478,0.0018649608,0.000028342938,0.00009883294,0.000004209135],"about_ca_topic_score_codex":0.010529743,"about_ca_topic_score_gemma":0.031088056,"teacher_disagreement_score":0.010529743,"about_ca_system_score_codex":0.00030828634,"about_ca_system_score_gemma":0.00019422425,"threshold_uncertainty_score":0.020936906},"labels":[],"label_agreement":null},{"id":"W4411049348","doi":"10.1016/j.jsg.2025.105484","title":"Partitioning of strain rates and stresses between a thin shear zone and its walls under transpression or transtension","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"High-Velocity Impact and Material Behavior","field":"Materials Science","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Transpression; Transtension; Geology; Shear (geology); Strain partitioning; Shear zone; Strain (injury); Seismology; Petrology; Fault (geology); Anatomy; Sinistral and dextral; Biology; Tectonics","score_opus":0.028770036287286364,"score_gpt":0.3193023789843972,"score_spread":0.2905323426971108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411049348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986846,0.000024282754,0.00063896354,0.000003568076,0.0000011894817,0.0000024775425,0.000016461541,0.0000052524456,0.0006232323],"genre_scores_gemma":[0.99951684,0.000015663678,0.00015325972,0.0000013870086,7.8524886e-7,0.0000025049485,0.000021348485,0.0000040405753,0.00028420842],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99990106,0.000010905268,0.000005243229,0.000022668977,0.000021523576,0.000038573333],"domain_scores_gemma":[0.99967,0.00010498813,0.000059175632,0.00002372131,0.00005131021,0.0000907277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016933534,0.00026239414,0.0002982026,0.0009044657,0.00043861702,0.0009427076,0.00028640428,0.0002525645,0.0022822407],"category_scores_gemma":[0.0005528951,0.0003317467,0.00015289352,0.00028747888,0.0007950599,0.00045437226,0.0004147275,0.00030884056,0.00029129506],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002065605,0.00027375936,0.050133564,0.000056255696,0.000043862987,0.00028934667,0.00046479792,0.014214151,0.9147956,0.0031643456,0.00007068626,0.0144281555],"study_design_scores_gemma":[0.00008960779,0.0010997151,0.5582749,0.00003620392,0.000080313635,0.00033420895,0.0020838191,0.08935183,0.34506327,0.0030316021,0.000476784,0.00007776488],"about_ca_topic_score_codex":0.0011111922,"about_ca_topic_score_gemma":0.0013668558,"teacher_disagreement_score":0.0022822407,"about_ca_system_score_codex":0.00023374725,"about_ca_system_score_gemma":0.00029931054,"threshold_uncertainty_score":0.0076348186},"labels":[],"label_agreement":null},{"id":"W4412529891","doi":"10.1016/j.jsg.2025.105515","title":"Mineral heterogeneity dominates the tensile failure mode of Eastern Himalayan Gneiss","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China; Center for Health Design","keywords":"Gneiss; Geology; Mineral; Geochemistry; Ultimate tensile strength; Mode (computer interface); Seismology; Mining engineering; Metamorphic rock; Composite material; Metallurgy; Materials science","score_opus":0.0064335657245628095,"score_gpt":0.23483147215289987,"score_spread":0.22839790642833707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412529891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923086,0.000018760078,0.000092935,0.000009438334,4.494304e-7,0.0000015816058,0.00004499283,0.000005496172,0.00059548835],"genre_scores_gemma":[0.99981946,0.000009719146,0.000017562234,0.000001286005,8.2000804e-7,4.984982e-7,0.000024000925,0.0000012759534,0.00012538893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999157,0.000008965557,0.000007166586,0.000023257324,0.000017663635,0.000027279213],"domain_scores_gemma":[0.9997961,0.00006178826,0.000048129372,0.000018617318,0.00005132118,0.000023959476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001581526,0.00027771623,0.00027215254,0.0016612659,0.0006280509,0.0007373829,0.00040636945,0.00033684119,0.0025603508],"category_scores_gemma":[0.0005464202,0.00030518768,0.00019134644,0.00096596987,0.00067334424,0.00033438188,0.00030050403,0.00012487156,0.00028940383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029640982,0.000048205136,0.9237685,0.00007370973,0.0001208001,0.0014071345,0.00089949614,0.018050235,0.04492202,0.00097398885,0.00021099842,0.009228456],"study_design_scores_gemma":[0.000005523452,0.000024896066,0.9878962,0.00000350302,0.000019245454,0.00017053627,0.00046572185,0.010310186,0.0007804069,0.0002027346,0.00011321823,0.000007788194],"about_ca_topic_score_codex":0.03966812,"about_ca_topic_score_gemma":0.06429449,"teacher_disagreement_score":0.03966812,"about_ca_system_score_codex":0.0006100351,"about_ca_system_score_gemma":0.00035485186,"threshold_uncertainty_score":0.07887441},"labels":[],"label_agreement":null},{"id":"W4413903684","doi":"10.1016/j.jsg.2025.105542","title":"Going with the flow — Changes of vorticity control gold enrichment in Archean shear zones (Shebandowan Greenstone Belt, Superior Province, Canada)","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia; Mitacs","keywords":"Greenstone belt; Archean; Geology; Shear zone; Shear (geology); Vorticity; Geochemistry; Flow (mathematics); Petrology; Seismology; Geometry; Vortex; Geography; Tectonics","score_opus":0.0043663820188447776,"score_gpt":0.1805933797927412,"score_spread":0.17622699777389642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413903684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987657,0.000041677125,0.000063424275,0.000013915746,8.31861e-7,0.000002742492,0.000114328875,0.000006644731,0.0009907153],"genre_scores_gemma":[0.99909675,0.000042514683,0.00011482665,0.0000057048296,4.910576e-7,0.0000019324375,0.000101142614,0.0000046478413,0.0006321009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989593,0.000003695744,0.0000034501647,0.000027379614,0.000024144389,0.00004536032],"domain_scores_gemma":[0.9998765,0.000007799408,0.00002596574,0.000004870933,0.000052944648,0.000031957876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000813962,0.00017634887,0.0001551567,0.00094507687,0.0008471693,0.00085185573,0.00027933076,0.00015476705,0.0010593508],"category_scores_gemma":[0.00034350526,0.00019731102,0.00012292166,0.0008420865,0.0009820566,0.00018171586,0.00043717583,0.00013948424,0.00014280011],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016444623,0.000025791196,0.90770483,0.000033916727,0.000045494326,0.00022293137,0.0035757245,0.0012538246,0.06954453,0.0006368536,0.0005005601,0.016291128],"study_design_scores_gemma":[0.0000018315421,0.0000038340877,0.99807334,0.0000031588318,0.000004374117,0.000010720957,0.00063517125,0.00038778043,0.0005122882,0.000029700259,0.00033416107,0.000003640977],"about_ca_topic_score_codex":0.9384223,"about_ca_topic_score_gemma":0.97243494,"teacher_disagreement_score":0.061577678,"about_ca_system_score_codex":0.0060366513,"about_ca_system_score_gemma":0.003762517,"threshold_uncertainty_score":0.123880565},"labels":[],"label_agreement":null},{"id":"W4416549217","doi":"10.1016/j.jsg.2025.105591","title":"Dehydroxylation and amorphization of wet serpentinite gouges during experimental seismic slip and implications for coseismic fluid drainage","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Academia Sinica; National Science and Technology Council","keywords":"Fault gouge; Slip (aerodynamics); Compaction; Shear (geology); Anisotropy; Drainage; Olivine; Shear stress","score_opus":0.008871857995980961,"score_gpt":0.2441344049249405,"score_spread":0.23526254692895954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416549217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996075,0.000024326762,0.000033017317,0.000002951272,9.4874144e-7,0.000002274704,0.000063295294,0.0000028863642,0.000262911],"genre_scores_gemma":[0.9996245,0.000019639048,0.000036325626,0.0000026589794,8.029135e-7,0.000001940374,0.00009337555,0.000003829909,0.00021691283],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993706,0.000008434823,0.000004277227,0.0000148339595,0.000012615932,0.000022767877],"domain_scores_gemma":[0.99987197,0.00002582934,0.000038368627,0.000017453569,0.000024306177,0.000022058646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011291404,0.00018076782,0.00012847409,0.00031642726,0.00036247013,0.0003469409,0.00017219894,0.0001755051,0.0017991833],"category_scores_gemma":[0.00029674624,0.00012440613,0.00010228015,0.00022914723,0.00058191025,0.00031037428,0.00018101808,0.00023454626,0.000118676675],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014084182,0.00007800205,0.01377013,0.000047163598,0.00001991798,0.0003215154,0.0004971196,0.00037055634,0.981128,0.00018798519,0.000050597704,0.002120638],"study_design_scores_gemma":[0.000046738005,0.00068417017,0.24062233,0.000009741134,0.000032336884,0.00033717055,0.0013679025,0.0018296358,0.75330937,0.00014660701,0.0015981455,0.000015947822],"about_ca_topic_score_codex":0.0029869513,"about_ca_topic_score_gemma":0.004064735,"teacher_disagreement_score":0.0029869513,"about_ca_system_score_codex":0.00023225526,"about_ca_system_score_gemma":0.00019981846,"threshold_uncertainty_score":0.0060189366},"labels":[],"label_agreement":null},{"id":"W648083478","doi":"10.1016/j.jsg.2015.06.006","title":"Do faults preserve a record of seismic slip: A second opinion","year":2015,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":301,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Slip (aerodynamics); Seismology; Geologic record; Episodic tremor and slip; Earthquake rupture; Fault (geology); Subduction; Tectonics; Paleontology","score_opus":0.034001315074369674,"score_gpt":0.25989897449649163,"score_spread":0.22589765942212195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W648083478","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027364092,0.030384991,0.00753283,0.9069749,0.010355133,0.000026629226,0.00087368727,0.000044294917,0.016443385],"genre_scores_gemma":[0.4884599,0.054852378,0.0053912103,0.37268505,0.06989389,0.000062517334,0.0012325818,0.00009135705,0.0073311045],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99713683,0.00042807675,0.00021556008,0.0014057691,0.00054380554,0.00026996172],"domain_scores_gemma":[0.9484032,0.023906449,0.0061953324,0.003043451,0.015766144,0.0026854854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009852372,0.0007255289,0.0016777671,0.0014647738,0.0016304975,0.0035412381,0.0039401613,0.010572035,0.009704094],"category_scores_gemma":[0.033265077,0.0003655651,0.00083891896,0.0013435328,0.010613609,0.0088296775,0.0021221864,0.0065755155,0.003937984],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013321429,0.00031351583,0.06260736,0.0043066205,0.0016008997,0.0014466842,0.009288635,0.0012001076,0.0083009405,0.11324021,0.33458096,0.46178195],"study_design_scores_gemma":[0.0003567852,0.0005342574,0.093859226,0.0041172802,0.00089465815,0.0013316371,0.027765423,0.002634293,0.0030079347,0.3937478,0.4714282,0.00032252076],"about_ca_topic_score_codex":0.0062990854,"about_ca_topic_score_gemma":0.007117256,"teacher_disagreement_score":0.010572035,"about_ca_system_score_codex":0.0015023063,"about_ca_system_score_gemma":0.0026283409,"threshold_uncertainty_score":0.05210489},"labels":[],"label_agreement":null},{"id":"W7117373349","doi":"10.1016/j.jsg.2025.105611","title":"Investigating the generation of transport-parallel gradients in ductile strain and kinematic vorticity in the footwalls of metamorphic core complexes: Insights from the Northern Snake Range, Nevada, USA","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus","funders":"National Science Foundation","keywords":"Metamorphic core complex; Metamorphic rock; Detachment fault; Vorticity; Kinematics; Strain partitioning; Fault (geology)","score_opus":0.03942637870081185,"score_gpt":0.23431250971883633,"score_spread":0.1948861310180245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7117373349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99911994,0.00005717852,0.00008985935,0.000013780865,5.503253e-7,0.0000025407014,0.000069440444,0.000002302076,0.0006444834],"genre_scores_gemma":[0.99928206,0.000068319234,0.00025124435,0.000012334348,7.5286584e-7,0.0000026424839,0.0001548096,0.0000027220683,0.00022511627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.000005576277,0.0000023388272,0.000013582316,0.0000128607535,0.000008076248],"domain_scores_gemma":[0.99990475,0.000009818874,0.00002115011,0.0000040890377,0.0000405426,0.000019681253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012360809,0.00010003509,0.00012438088,0.0006323671,0.00035688,0.00039110312,0.00019073005,0.00015376342,0.00047673713],"category_scores_gemma":[0.00022191771,0.000094821626,0.0000949225,0.0004458289,0.00022850274,0.00017784786,0.00029535417,0.0001194912,0.00006560031],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055113564,0.000050182385,0.9598312,0.000021644413,0.000029478708,0.0002119718,0.0009690299,0.0008905268,0.027230695,0.00012837075,0.00013768047,0.010444135],"study_design_scores_gemma":[0.0000016571191,0.0000090331005,0.997724,0.0000041851154,0.0000047636386,0.000039528444,0.0007083056,0.0008125288,0.0003895839,0.00003392241,0.00027037968,0.0000021285543],"about_ca_topic_score_codex":0.11841728,"about_ca_topic_score_gemma":0.30562446,"teacher_disagreement_score":0.11841728,"about_ca_system_score_codex":0.00053616933,"about_ca_system_score_gemma":0.00040777095,"threshold_uncertainty_score":0.23545599},"labels":[],"label_agreement":null},{"id":"W7117541369","doi":"10.1016/j.jsg.2025.105613","title":"Ultracataclastic vein evolution within a granodiorite along the Naxos-Paros Detachment System","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Ontario; University of Ottawa; Geological Society of America","keywords":"Cataclastic rock; Orthoclase; Albite; Vein; Mylonite; Shear zone; Electron microprobe; Quartz; Echelon formation","score_opus":0.00529017738329345,"score_gpt":0.19982422818260281,"score_spread":0.19453405079930935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7117541369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99922717,0.000027651773,0.000024853543,0.000004982018,8.848633e-7,0.0000018606502,0.00003680911,0.0000031211478,0.00067266834],"genre_scores_gemma":[0.99963605,0.00001675598,0.000060262675,0.0000024122269,8.3162723e-7,0.0000014041187,0.00006508819,0.0000017254195,0.00021541044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999168,0.000006528793,0.000006218231,0.000036239697,0.000018302073,0.0000158872],"domain_scores_gemma":[0.99990106,0.000009573591,0.000035941302,0.000008596759,0.0000218938,0.000022871996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000897038,0.00014296852,0.00014991229,0.00081044604,0.00039859666,0.00059841835,0.00020414552,0.0002826691,0.000998745],"category_scores_gemma":[0.00026801787,0.00019170217,0.0001207857,0.00046497144,0.00050055626,0.00015500173,0.00051354733,0.00015839559,0.00022109048],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002550549,0.00003438339,0.9154306,0.00004323296,0.000035400586,0.0008551291,0.0014352683,0.00069205405,0.06899304,0.00030773948,0.00010836185,0.0118097095],"study_design_scores_gemma":[0.0000049896153,0.00003669568,0.99793375,0.0000060644643,0.0000050049516,0.00030616662,0.00034424782,0.0004020238,0.0005358332,0.000025808298,0.0003971105,0.000002372619],"about_ca_topic_score_codex":0.008653397,"about_ca_topic_score_gemma":0.022840733,"teacher_disagreement_score":0.008653397,"about_ca_system_score_codex":0.000388354,"about_ca_system_score_gemma":0.00022948177,"threshold_uncertainty_score":0.017206073},"labels":[],"label_agreement":null}]}