{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":132,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":132,"direct_label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline (scores rank; they never assert a category)","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12","author_layer_release":"2026-06-26"},"query_hash":"bc7ed1038c10","filters":{"venue":"Mineralogy and Petrology"}},"results":[{"id":"W1982739504","doi":"10.1007/s00710-009-0074-1","title":"Large igneous provinces (LIPs) and carbonatites","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":324,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University; University of Ottawa","funders":"","keywords":"Carbonatite; Geochemistry; Geology; Craton; Large igneous province; Mantle plume; Magmatism; Flood basalt; Baddeleyite; Igneous rock; Mafic; Basalt; Ultramafic rock; Mantle (geology); Lithosphere; Zircon; Paleontology; Tectonics; Volcanism","authors":[{"name":"Richard E. Ernst","is_ca":true},{"name":"Keith Bell","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.004449755108096297,"gpt":0.1782269487506196,"spread":0.1737771936425233,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001069202,0.000098397,0.000192326,0.00004709627,0.00009960402,0.0000127536,0.00006423019,0.0000971979,0.002021021],"category_scores_gemma":[0.00002628643,0.00006538482,0.00002560338,0.00007041408,0.0001393865,0.00003868641,0.000009427601,0.000109215,0.00002579444],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":4.570164e-7,"about_ca_system_score_gemma":0.000005401098,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007376472,"about_ca_topic_score_gemma":0.007106963,"domain_scores_codex":[0.999285,0.00005732998,0.0001108935,0.0002349565,0.00004836674,0.0002634393],"domain_scores_gemma":[0.9996798,0.0001259555,0.0000275051,0.00005961414,0.00001393096,0.00009319205],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005165526,0.0000239862,0.9814426,0.000004546602,0.0000215522,0.00005058286,0.0000848335,0.00003037324,0.0004968924,0.002598144,0.0001984002,0.01499648],"study_design_scores_gemma":[0.0002657932,0.0005293842,0.9469901,0.000001119147,0.00003218953,0.0001100385,0.00002639009,0.00305699,0.0000241026,0.0437447,0.005098521,0.0001206949],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.98067,0.003402516,0.00001120891,0.004265136,0.00003455048,0.00003099584,0.0000172596,0.0000219647,0.0115464],"genre_scores_gemma":[0.9965647,0.0001567286,0.0001734746,0.002565517,0.00007485316,4.391221e-7,0.00005474224,5.44153e-7,0.0004089387],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04114656,"threshold_uncertainty_score":0.9988913,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2042857616","doi":"10.1007/s00710-009-0059-0","title":"Source of parental melts to carbonatites–critical isotopic constraints","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":271,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University","funders":"","keywords":"Carbonatite; Mantle (geology); Geology; Radiogenic nuclide; Lithosphere; Geochemistry; Metasomatism; Mantle plume; Igneous rock; Earth science; Subduction; Partial melting; Mantle wedge; Paleontology; Tectonics","authors":[{"name":"Keith Bell","is_ca":true},{"name":"Antonio Simonetti","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.007706397609144521,"gpt":0.2125310986130136,"spread":0.204824701003869,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007987092,0.00008675393,0.0002322129,0.00005875027,0.00004179274,0.000004300156,0.00008682172,0.00008920117,0.004935449],"category_scores_gemma":[0.00007956631,0.00006369578,0.00004379101,0.00009883507,0.0003205465,0.00002065207,0.000009355467,0.00009780846,0.00004054166],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":6.927318e-7,"about_ca_system_score_gemma":0.000006345485,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0007248021,"about_ca_topic_score_gemma":0.001318171,"domain_scores_codex":[0.9992795,0.00005903524,0.0001642789,0.000199139,0.00006438949,0.0002336381],"domain_scores_gemma":[0.9995423,0.0002045865,0.00002097794,0.00007041626,0.00002431454,0.0001373834],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005273196,0.00002977002,0.9723932,0.000004225218,0.00001663884,0.00001298983,0.00006242321,0.00013542,0.001943128,0.00193677,0.0001416149,0.02327106],"study_design_scores_gemma":[0.0001973753,0.0006420804,0.9844339,0.000002152081,0.00002728967,0.00005403166,0.00002293146,0.0008174285,0.0001621181,0.01248499,0.001061571,0.00009414366],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9861124,0.0003453355,0.00009865528,0.005206093,0.00005270852,0.00003102322,0.00001754301,0.0000112258,0.008125034],"genre_scores_gemma":[0.9968987,0.000009440772,0.0004177039,0.002456512,0.00005289621,4.041379e-7,0.00003574914,5.067005e-7,0.0001281597],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02317692,"threshold_uncertainty_score":0.9959742,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2043570922","doi":"10.1007/s00710-006-0125-9","title":"Gold scavenged by bismuth melts: An example from Alpine shear-remobilizates in the Highiş Massif, Romania","year":2006,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Science North","funders":"","keywords":"Geology; Massif; Geochemistry; Greenschist; Hornfels; Shear zone; Vein; Igneous rock; Mineralogy; Quartz; Metamorphism; Biotite; Paleontology","authors":[{"name":"Cristiana L. Ciobanu","is_ca":false},{"name":"Nigel J. Cook","is_ca":false},{"name":"Floarea Damian","is_ca":true},{"name":"Gheorghe Damian","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01230939390875284,"gpt":0.1837802459123337,"spread":0.1714708520035808,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002505917,0.0001722442,0.0003212832,0.00006141049,0.00009438518,0.00002717834,0.0002509742,0.0001787682,0.005238205],"category_scores_gemma":[0.000009641814,0.000100728,0.00004549906,0.0002047264,0.0002510156,0.00008013786,0.00001671689,0.0002210341,0.00005722544],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001573804,"about_ca_system_score_gemma":0.000005878132,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.2021366,"about_ca_topic_score_gemma":0.1664399,"domain_scores_codex":[0.9985294,0.0003077498,0.0002537902,0.0004257541,0.0001019263,0.0003814152],"domain_scores_gemma":[0.9993333,0.0003325134,0.00005102185,0.0001936636,0.0000155406,0.0000740055],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001335085,0.0001296854,0.9868844,0.000003887993,0.00003253397,0.00006323557,0.0001634995,0.0003550561,0.004702977,0.0007487216,0.005665076,0.00111747],"study_design_scores_gemma":[0.0006932366,0.0003684215,0.9540317,0.000001151434,0.00007509653,0.0000261419,0.0001047897,0.003564112,0.00009260339,0.02930747,0.01154103,0.0001942162],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9910306,0.001926289,0.00001642235,0.003453438,0.00005172437,0.00006725864,0.0001009911,0.00002386204,0.003329425],"genre_scores_gemma":[0.9955347,0.00004702464,0.0001811335,0.001839823,0.0001108201,0.000003695278,0.001814607,0.000002134006,0.0004661122],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03569671,"threshold_uncertainty_score":0.9956712,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2018244263","doi":"10.1007/s00710-009-0054-5","title":"Geochronology of carbonatites from the Canadian and Baltic Shields, and the Canadian Cordillera: clues to mantle evolution","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Carleton University","funders":"","keywords":"Magmatism; Carbonatite; Geology; Geochemistry; Mantle plume; Mafic; Craton; Baddeleyite; Archean; Flood basalt; Mantle (geology); Geochronology; Baltic Shield; Paleontology; Earth science; Zircon; Lithosphere; Precambrian; Tectonics; Volcanism","authors":[{"name":"Alexei S. Rukhlov","is_ca":true},{"name":"Keith Bell","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005526777346479093,"gpt":0.1713475660819866,"spread":0.1658207887355075,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001738593,0.0000934022,0.000223502,0.00007466999,0.0003170105,0.00001691407,0.0001108916,0.0001430531,0.0009442963],"category_scores_gemma":[0.00008143601,0.00004919185,0.000022257,0.0001002778,0.0005878426,0.00002097615,0.00001113904,0.0001576968,0.000008805091],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005356387,"about_ca_system_score_gemma":0.000064343,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9819415,"about_ca_topic_score_gemma":0.9994097,"domain_scores_codex":[0.9992067,0.000139486,0.000129361,0.0001980344,0.00004687305,0.000279544],"domain_scores_gemma":[0.999257,0.0003845017,0.00002939038,0.00009922228,0.00002728953,0.0002026363],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006948013,0.00000334761,0.9900125,0.000001660344,0.00004772405,0.000009587227,0.0002811197,0.00008487709,0.00005965593,0.004711149,0.0004657526,0.004253148],"study_design_scores_gemma":[0.0002720507,0.0001589042,0.9629458,0.000001552435,0.00004933563,0.00002160379,0.00004603129,0.002317787,0.000003378409,0.03219677,0.001923162,0.00006359877],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9258435,0.003894289,0.000002105473,0.06626857,0.00004519729,0.00007129044,0.00006394051,0.000003476121,0.003807591],"genre_scores_gemma":[0.9933715,0.0001011323,0.00006232064,0.006275016,0.00006124781,0.000001139952,0.00005912234,6.775177e-7,0.00006782161],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06752799,"threshold_uncertainty_score":0.999969,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2052377311","doi":"10.1007/s007100070002","title":"Columbite-tantalite mineral chemistry from rare-element granitic pegmatites: Separation Lakeh area, N.W. Ontario, Canada","year":2000,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Ministry of Energy, Northern Development and Mines; Geological Survey of Canada","funders":"","keywords":"Pegmatite; Columbite; Geochemistry; Geology; Mineralogy; Materials science; Metallurgy","authors":[{"name":"A. G. Tindle","is_ca":false},{"name":"F. W. Breaks","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005970788370335972,"gpt":0.1707920406396311,"spread":0.1648212522692951,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00006991652,0.000175832,0.000308842,0.00001802623,0.0001458872,0.00002514393,0.0001258292,0.0001279379,0.2046482],"category_scores_gemma":[0.00001078111,0.0001467065,0.00005430612,0.00009175447,0.0001334973,0.00005881339,0.00000939491,0.0001937217,0.00006450839],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000130192,"about_ca_system_score_gemma":0.00009190282,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9773363,"about_ca_topic_score_gemma":0.9989145,"domain_scores_codex":[0.9988006,0.00006934578,0.0002742412,0.000361452,0.0001324374,0.000361958],"domain_scores_gemma":[0.9994753,0.0001469759,0.0000525877,0.0001351648,0.0000266751,0.0001632878],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009890798,0.00002330444,0.992262,0.000006754349,0.00007664921,0.00008904537,0.0001032493,0.0006934979,0.0009579227,0.000009974709,0.003783753,0.001894951],"study_design_scores_gemma":[0.0005671838,0.0001137646,0.9441397,0.00000439353,0.0000931316,0.00005412666,0.0000303045,0.003691975,0.00007201204,0.002644957,0.04833888,0.0002496065],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9780268,0.0004901074,0.000004406112,0.001053392,0.00007198724,0.00005347335,0.0002638748,0.00001673125,0.02001924],"genre_scores_gemma":[0.9873896,0.0000346592,0.00009987393,0.002054648,0.0001130061,0.000003559649,0.002659226,0.000001776842,0.007643642],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2045837,"threshold_uncertainty_score":0.7960789,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1967183046","doi":"10.1007/s00710-009-0067-0","title":"Trace element geochemistry of scheelite and rutile from metaturbidite-hosted quartz vein gold deposits, Meguma Terrane, Nova Scotia, Canada: genetic implications","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Laurentian University; Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Scheelite; Terrane; Geology; Hydrothermal circulation; Rare-earth element; Geochemistry; Rutile; Trace element; Nova scotia; Niobium; Tantalum; Mineral; Quartz; Chondrite; Mineralogy; Plagioclase; Tungsten; Meteorite; Rare earth; Materials science; Metallurgy; Tectonics","authors":[{"name":"J. Dostál","is_ca":true},{"name":"Daniel J. Kontak","is_ca":true},{"name":"Avik Chatterjee","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008153256327119355,"gpt":0.1901933074187557,"spread":0.1820400510916363,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007252486,0.0001601905,0.0003441141,0.00004191149,0.00005902959,0.00001057492,0.0001372485,0.0001387943,0.00188693],"category_scores_gemma":[0.00002395718,0.0001264267,0.000045116,0.0001479443,0.0001503824,0.00003271912,0.00001390432,0.0001626495,0.000006214297],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003117424,"about_ca_system_score_gemma":0.00004308511,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.451367,"about_ca_topic_score_gemma":0.8316493,"domain_scores_codex":[0.9988754,0.00007009121,0.0003067715,0.0003573297,0.00009140138,0.0002989989],"domain_scores_gemma":[0.9993626,0.0001713104,0.00009497926,0.0001719231,0.00004380097,0.0001554105],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008212344,0.00005778857,0.9358549,0.00001793524,0.0001271353,0.00002571139,0.00005739784,0.0001904863,0.04311793,0.0001019804,0.001633908,0.01873275],"study_design_scores_gemma":[0.0003211534,0.0001822861,0.9935588,0.000003762786,0.0001255774,0.00003766771,0.00001975358,0.0007635017,0.001691007,0.002067128,0.001090802,0.0001385698],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9846301,0.008733552,0.00003214318,0.005205812,0.00004106343,0.00005760346,0.0002267669,0.00001010963,0.001062867],"genre_scores_gemma":[0.997215,0.0001005028,0.001020852,0.0009984891,0.00005684954,8.725188e-7,0.0004809968,0.000001383499,0.0001250909],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3802823,"threshold_uncertainty_score":0.9990255,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W640908151","doi":"10.1007/s00710-015-0392-4","title":"Calcite and dolomite in intrusive carbonatites. II. Trace-element variations","year":2015,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Manitoba Hydro; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Carbonatite; Calcite; Geology; Dolomite; Monazite; Rare-earth element; Lithophile; Geochemistry; Fluorapatite; Trace element; Mineralogy; Fractionation; Mineral; Carbonate; Chemistry; Apatite; Partial melting; Rare earth; Zircon; Crust; Mantle (geology)","authors":[{"name":"Anton R. Chakhmouradian","is_ca":true},{"name":"Ekaterina P. Reguir","is_ca":true},{"name":"Christopher Couëslan","is_ca":true},{"name":"Panseok Yang","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01536284421887939,"gpt":0.2084451823386196,"spread":0.1930823381197402,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002076028,0.00009280922,0.0001986554,0.00009332971,0.00006261373,0.000008226647,0.00005621283,0.0001031282,0.0012218],"category_scores_gemma":[0.00005919775,0.00006784731,0.00001879083,0.0001366041,0.0001520867,0.00004797983,0.00002679067,0.0001384553,0.00001609476],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000223779,"about_ca_system_score_gemma":0.00001459533,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005999474,"about_ca_topic_score_gemma":0.03747506,"domain_scores_codex":[0.9992406,0.00009669022,0.0001604213,0.0002234178,0.0000564808,0.0002224172],"domain_scores_gemma":[0.9996065,0.0001413368,0.00003359102,0.00006035361,0.00002517299,0.0001329825],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000495921,0.00002057059,0.9930968,0.00000240636,0.00002598598,0.00002306778,0.0003419626,0.0004933627,0.00008997439,0.001663736,0.0001911683,0.00400142],"study_design_scores_gemma":[0.0007166414,0.000328775,0.950688,0.000001328792,0.00003044561,0.00003901919,0.00005442707,0.01278115,0.000008798919,0.03010446,0.005130434,0.0001165177],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9877889,0.001434729,0.00003156035,0.005584885,0.00005588185,0.00004477273,0.00002300703,0.000009394973,0.005026883],"genre_scores_gemma":[0.9981326,0.00006817503,0.0004055105,0.0009624548,0.00005765335,0.000002421499,0.00008212667,8.053475e-7,0.0002882519],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04240876,"threshold_uncertainty_score":0.9996912,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2054057267","doi":"10.1007/s00710-004-0050-8","title":"Formation of Ni?Cu?Platinum Group Element sulfide mineralization in the Sudbury Impact Melt Sheet","year":2004,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Vale (Canada); Laurentian University","funders":"","keywords":"Norite; Platinum group; Felsic; Mafic; Geochemistry; Geology; Pyrrhotite; Mineralization (soil science); Chalcopyrite; Sulfide; Igneous rock; Mineralogy; Chemistry; Platinum; Copper; Pyrite; Gabbro; Catalysis","authors":[{"name":"Reid R. Keays","is_ca":true},{"name":"P. C. Lightfoot","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009795210128347857,"gpt":0.2146952618919519,"spread":0.2049000517636041,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003246286,0.0001016044,0.0002022901,0.00009215831,0.00005165675,0.000008189048,0.0001136553,0.00009326599,0.00119184],"category_scores_gemma":[0.00002642493,0.00005686373,0.00005284117,0.0002207481,0.0001111931,0.00009951365,0.00000939754,0.0001089916,0.00001252654],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003207318,"about_ca_system_score_gemma":0.000007688216,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.019504,"about_ca_topic_score_gemma":0.0840403,"domain_scores_codex":[0.9991307,0.0001319646,0.0002710867,0.0001473591,0.00009414249,0.0002247287],"domain_scores_gemma":[0.9996531,0.0001163352,0.00008026969,0.00009096103,0.00002142044,0.00003791508],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001041348,0.00004960708,0.9820413,0.00001259388,0.00002003786,0.00001083104,0.0003980795,0.0116791,0.002353595,0.001507414,0.0001798688,0.00164346],"study_design_scores_gemma":[0.000617574,0.0004650181,0.9751324,0.000003054794,0.0000281665,0.00004575879,0.00009114843,0.003668173,0.00009381977,0.01963439,0.0001375193,0.00008297856],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9960447,0.0004482144,0.0002864316,0.001768558,0.00003651666,0.00007053044,0.00002276354,0.000006136407,0.001316176],"genre_scores_gemma":[0.998441,0.00006079454,0.0001726319,0.000722332,0.00004128544,0.000002191945,0.0005368875,8.271251e-7,0.00002200684],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0645363,"threshold_uncertainty_score":0.9997212,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2004657255","doi":"10.1007/s00710-006-0177-x","title":"New evidence from a calcite-dolomite carbonatite dyke for the magmatic origin of the massive Bayan Obo ore-bearing dolomite marble, Inner Mongolia, China","year":2007,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Vale (Canada)","funders":"","keywords":"Dolomite; Carbonatite; Geology; Geochemistry; Calcite; Isotopes of oxygen; Proterozoic; Xenolith; Carbonate; Mineralogy; Mantle (geology); Paleontology; Chemistry","authors":[{"name":"M. J. Le Bas","is_ca":false},{"name":"Rex N. Taylor","is_ca":false},{"name":"Baruch Spiro","is_ca":false},{"name":"James A. Milton","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01659314107425063,"gpt":0.2270062826383892,"spread":0.2104131415641386,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005309964,0.0001962247,0.0003900233,0.00006996678,0.0001967294,0.0000191906,0.0004156507,0.0001978064,0.001535229],"category_scores_gemma":[0.0002661791,0.00009709904,0.0001470143,0.0002971929,0.0003745071,0.00007524285,0.00006682092,0.0003208046,0.0000157449],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004018644,"about_ca_system_score_gemma":0.00003191908,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.04788483,"about_ca_topic_score_gemma":0.06724507,"domain_scores_codex":[0.9985351,0.0001533441,0.0003692916,0.0003553315,0.0001438647,0.000443053],"domain_scores_gemma":[0.9968956,0.00248361,0.0001740259,0.0002778973,0.00004658456,0.0001223051],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002883197,0.00001011074,0.9890982,0.00001654363,0.0001279189,0.000008572854,0.0002637392,0.001457571,0.002390372,0.0003914716,0.0004341083,0.005513062],"study_design_scores_gemma":[0.0004376367,0.0001423254,0.9743289,0.00001601693,0.0001798496,0.00001510369,0.00004192303,0.01081833,0.0003274336,0.01207774,0.001479689,0.0001351056],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9893963,0.003390033,0.001356077,0.004666419,0.0002854906,0.000192277,0.00005936808,0.00001293683,0.0006411027],"genre_scores_gemma":[0.9961053,0.000119832,0.0013359,0.0009658187,0.0002304632,0.000004143408,0.00004104189,0.000003238253,0.001194308],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01936023,"threshold_uncertainty_score":0.9993775,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1196665483","doi":"10.1007/s00710-015-0390-6","title":"Calcite and dolomite in intrusive carbonatites. I. Textural variations","year":2015,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba","funders":"","keywords":"Carbonatite; Dolomite; Calcite; Geology; Igneous rock; Geochemistry; Mineral; Recrystallization (geology); Sill; Mineralogy; Petrology; Chemistry; Mantle (geology)","authors":[{"name":"Anton R. Chakhmouradian","is_ca":true},{"name":"Ekaterina P. Reguir","is_ca":true},{"name":"Anatoly N. Zaitsev","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0149415547198699,"gpt":0.2028436008823916,"spread":0.1879020461625217,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001507711,0.00008512777,0.0001844459,0.00008659505,0.00003762247,0.00001014083,0.00005270206,0.0001045673,0.0008270232],"category_scores_gemma":[0.00007696109,0.00006003311,0.00001686989,0.0001375062,0.0001847407,0.00005366124,0.00001916382,0.0001411123,0.00002607116],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001582698,"about_ca_system_score_gemma":0.00001232601,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.007904829,"about_ca_topic_score_gemma":0.03520305,"domain_scores_codex":[0.9993225,0.0000964625,0.0001309621,0.000201487,0.00004570682,0.0002029235],"domain_scores_gemma":[0.9995899,0.0001788773,0.0000276133,0.00005366595,0.00002425062,0.0001257601],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003829677,0.000007410147,0.9946935,0.000001654701,0.00001550867,0.00002310373,0.000160871,0.0002291921,0.00007277614,0.001169143,0.00008266078,0.003505886],"study_design_scores_gemma":[0.0004581115,0.0001339866,0.9604668,9.172988e-7,0.00001787322,0.00005618378,0.0000336233,0.011308,0.000003752227,0.02632155,0.00111096,0.00008827612],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9895914,0.0009524812,0.00002566915,0.003703028,0.00005516341,0.00003201403,0.00001636852,0.000009507961,0.005614385],"genre_scores_gemma":[0.9980917,0.00004184113,0.0003093187,0.001174618,0.00006007712,0.000001298376,0.0000846373,7.006863e-7,0.0002357863],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03422672,"threshold_uncertainty_score":0.9987016,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2010250255","doi":"10.1007/s00710-012-0197-7","title":"A Raman spectroscopic study on the structural disorder of monazite–(Ce)","year":2012,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Nuclear materials and radiation effects","field":"Materials Science","cited_by":88,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Monazite; Raman spectroscopy; Annealing (glass); Full width at half maximum; Analytical Chemistry (journal); Chemical composition; Materials science; Solid solution; Chemistry; Crystallography; Physics; Metallurgy; Optics","authors":[{"name":"Katja Ruschel","is_ca":false},{"name":"Lutz Nasdala","is_ca":false},{"name":"Andreas Kronz","is_ca":false},{"name":"John M. Hanchar","is_ca":true},{"name":"Daniel M. Többens","is_ca":false},{"name":"Radek Škoda","is_ca":false},{"name":"Friedrich Finger","is_ca":false},{"name":"Andreas Möller","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01040370360225239,"gpt":0.2528144813385561,"spread":0.2424107777363037,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000307086,0.0000924781,0.000184683,0.00003738815,0.0001043128,0.00001096022,0.00009053326,0.00005522844,0.001368587],"category_scores_gemma":[0.00002130781,0.00005297285,0.0000197536,0.00003826474,0.0001353808,0.00005018624,0.00003963494,0.0000652669,0.00006729476],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004814299,"about_ca_system_score_gemma":0.000005307656,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00008549693,"about_ca_topic_score_gemma":0.00002458816,"domain_scores_codex":[0.999157,0.0002880069,0.0001413337,0.000125055,0.00006409654,0.0002245295],"domain_scores_gemma":[0.999577,0.0001524826,0.00006901964,0.000153236,0.00001166077,0.00003655142],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0001291678,0.0001327772,0.1965621,0.00001125065,0.00002188746,0.000002128795,0.00167869,0.00001543424,0.7820576,0.01896851,0.000338182,0.00008221043],"study_design_scores_gemma":[0.0005397335,0.0007233679,0.9934039,0.000001726155,0.00002310098,0.00001188277,0.000150503,0.00003233123,0.003959719,0.0004223899,0.0006574836,0.00007382248],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9978964,0.0001564731,0.000005237432,0.0006071388,0.0006343835,0.0001580184,0.000005951826,0.0000140133,0.0005223813],"genre_scores_gemma":[0.999307,0.000003602155,0.00002689665,0.0003397749,0.0001925989,0.00001022818,0.000002184463,0.000007135775,0.0001105674],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7968418,"threshold_uncertainty_score":0.9995443,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1972494698","doi":"10.1007/s007100200001","title":"Stability range and decomposition of potassic richterite and phlogopite end members at 5-15 GPa","year":2002,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"","keywords":"Phlogopite; Forsterite; Pyrope; Mineralogy; Analytical Chemistry (journal); Olivine; Amphibole; Geology; Silicate; Chemistry; Geochemistry; Mantle (geology)","authors":[{"name":"Reidar G. Trønnes","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01304979732487131,"gpt":0.1909746806835647,"spread":0.1779248833586934,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001338941,0.0001074978,0.000270584,0.00004767649,0.00009107765,0.000006431765,0.00004333532,0.0001100768,0.01222681],"category_scores_gemma":[0.00001623843,0.00007801636,0.00003201444,0.00007300136,0.0004860679,0.00005075559,0.00002718104,0.00009061991,0.00000922067],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001217346,"about_ca_system_score_gemma":0.000001206738,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001191007,"about_ca_topic_score_gemma":0.007816852,"domain_scores_codex":[0.9991872,0.0001232059,0.0001728217,0.0002641146,0.00005362776,0.0001990658],"domain_scores_gemma":[0.999514,0.0002309399,0.00005361221,0.00007788293,0.00001740284,0.0001060943],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008663025,0.00001901843,0.991268,0.0000198569,0.00003037624,0.00001032527,0.0001118329,0.00001008416,0.002779182,0.00005160553,0.00007867099,0.005534354],"study_design_scores_gemma":[0.0004710852,0.0003118235,0.9911836,0.000001656129,0.00006424823,0.0001056111,0.00001272632,0.004517054,0.0001370455,0.002171623,0.0009225286,0.0001010044],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9914086,0.003823652,0.000005484142,0.001610299,0.00003545568,0.00003978804,0.00006348867,0.000008724403,0.003004536],"genre_scores_gemma":[0.9987016,0.00045174,0.0001649842,0.0004469522,0.00002716008,8.972868e-7,0.00006965424,9.120178e-7,0.0001361068],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01221758,"threshold_uncertainty_score":0.9886761,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2094197788","doi":"10.1007/s00710-002-0220-5","title":"A rare earth element-rich carbonatite dyke at Bayan Obo, Inner Mongolia, North China","year":2003,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of New Brunswick","funders":"","keywords":"Carbonatite; Geology; Geochemistry; Rare-earth element; Partial melting; Fractional crystallization (geology); Trace element; Mantle (geology); Mineralogy; Rare earth","authors":[{"name":"Xue-Ming Yang","is_ca":true},{"name":"Xiaoyong Yang","is_ca":true},{"name":"Yong‐Fei Zheng","is_ca":false},{"name":"M. J. Le Bas","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006177892248238265,"gpt":0.173884725584819,"spread":0.1677068333365807,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001469801,0.0002053416,0.0003436911,0.0000975368,0.0002126262,0.00001391768,0.0001347146,0.0001539429,0.01820473],"category_scores_gemma":[0.00004891158,0.0001451878,0.00007597145,0.0002604063,0.0002174786,0.00005601511,0.00002940337,0.0002201345,0.0002297077],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002357114,"about_ca_system_score_gemma":0.00001386075,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002774418,"about_ca_topic_score_gemma":0.09250787,"domain_scores_codex":[0.9984903,0.0002030665,0.0002456901,0.0004278411,0.0001183147,0.0005147767],"domain_scores_gemma":[0.9994245,0.0001155762,0.00006680033,0.0001686289,0.00003048122,0.000194053],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004451626,0.00002204665,0.9974751,0.000006404101,0.00005175609,0.00004730969,0.00006811557,0.0004180184,0.0002152463,0.0004166043,0.0004164813,0.0008183555],"study_design_scores_gemma":[0.0004681774,0.0002421425,0.9727262,9.473851e-7,0.00005331093,0.0000833441,0.00001160468,0.001021543,0.00008958102,0.002505107,0.02259799,0.0002000173],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9751264,0.001280497,0.00000975622,0.0009434195,0.0001189818,0.00006379039,0.00005431231,0.00002686979,0.02237591],"genre_scores_gemma":[0.9936523,0.0001149253,0.0002378927,0.001376148,0.0000754494,0.00000348188,0.0003618486,0.000002649608,0.004175257],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.08973345,"threshold_uncertainty_score":0.9826928,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2094744546","doi":"10.1007/s007100200002","title":"Origin of spongy textures in clinopyroxene and spinel from mantle xenoliths, Hessian Depression, Germany","year":2002,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University","funders":"","keywords":"Spinel; Xenolith; Geology; Mantle (geology); Basalt; Geochemistry; Partial melting; Silicate; Mineralogy; Chemistry; Paleontology","authors":[{"name":"Robert L. Carpenter","is_ca":true},{"name":"A. D. Edgar","is_ca":true},{"name":"Yves Thibault","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0130410782126126,"gpt":0.2012635143263874,"spread":0.1882224361137748,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008920376,0.0001167834,0.0003202725,0.00009042802,0.00004336535,0.000005733579,0.00009393592,0.0001597082,0.008226587],"category_scores_gemma":[0.00002151074,0.00007936158,0.00003232038,0.0001063813,0.0002402679,0.00004347912,0.0000214882,0.0001600147,0.00003337575],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":6.677648e-7,"about_ca_system_score_gemma":0.00000269587,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.007904476,"about_ca_topic_score_gemma":0.01123486,"domain_scores_codex":[0.9990936,0.00009734776,0.000234177,0.000284016,0.00005330542,0.0002375395],"domain_scores_gemma":[0.9995649,0.0001707592,0.00005895193,0.000103904,0.00001175,0.00008972585],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000535288,0.00002758595,0.991153,0.000006628614,0.00001875449,0.00004563196,0.00006272514,0.00005570685,0.00140385,0.0001045069,0.0001591766,0.006908885],"study_design_scores_gemma":[0.0004293651,0.00009711838,0.9850668,0.000004591411,0.00002423821,0.00002784331,0.00001395202,0.004904475,0.0001444603,0.00773159,0.001457562,0.0000980369],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9886985,0.006770995,0.000008693796,0.00103067,0.00004844107,0.00003050535,0.0000409223,0.000008280784,0.003362956],"genre_scores_gemma":[0.9983236,0.0004808898,0.0002524914,0.0005188987,0.00006878419,8.962631e-7,0.00005915656,0.000001268429,0.0002940431],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.009625036,"threshold_uncertainty_score":0.998702,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2090266802","doi":"10.1007/s00710-012-0256-0","title":"Optical microscope-cathodoluminescence (OM–CL) imaging as a powerful tool to reveal internal textures of minerals","year":2012,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Cathodoluminescence; Luminescence; Mineralogy; Mineral; Microscope; Optical microscope; Geology; Microscopy; Trace element; Hyperspectral imaging; Materials science; Geochemistry; Optics; Remote sensing; Scanning electron microscope; Optoelectronics; Metallurgy","authors":[{"name":"Jens Götze","is_ca":false},{"name":"Hans‐Peter Schertl","is_ca":false},{"name":"Rolf D. Neuser","is_ca":false},{"name":"U. Kempe","is_ca":false},{"name":"John M. Hanchar","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009426608930421328,"gpt":0.2353361491307132,"spread":0.2259095402002918,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003694452,0.0001794389,0.0004007503,0.000104844,0.00005874816,0.00001452982,0.0002095551,0.000112958,0.004633423],"category_scores_gemma":[0.0002071964,0.0001281587,0.0000880776,0.0001638387,0.0003179766,0.0001002959,0.00006073262,0.000193945,0.0002708886],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001948415,"about_ca_system_score_gemma":0.00001218509,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001769665,"about_ca_topic_score_gemma":0.001247087,"domain_scores_codex":[0.998581,0.0001229757,0.0003261548,0.0003064633,0.000108813,0.0005545741],"domain_scores_gemma":[0.9991894,0.000283222,0.00007097948,0.0001495028,0.00004937155,0.0002574896],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000197753,0.00004628411,0.9127157,0.00001211609,0.00002892896,0.00001899604,0.0001197632,0.0000234466,0.08043629,0.0003882827,0.001595734,0.004416656],"study_design_scores_gemma":[0.0003874077,0.0004164441,0.9813438,0.0000116889,0.00008134745,0.0004601253,0.00004559263,0.0002331044,0.004976951,0.001737095,0.01002369,0.0002827552],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9868899,0.001453164,0.0001468729,0.002990136,0.0001976917,0.00006566369,0.00003288914,0.00001451759,0.008209164],"genre_scores_gemma":[0.9916779,0.0000243625,0.003401001,0.0031668,0.0002276918,0.00000151151,0.00005332398,0.000002436959,0.001444925],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07545934,"threshold_uncertainty_score":0.9962765,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1970344174","doi":"10.1007/s00710-011-0188-0","title":"Low-Ca contents and kink-banded textures are not unique to mantle olivine: evidence from the Duke Island Complex, Alaska","year":2011,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"University of British Columbia","keywords":"Olivine; Peridotite; Mantle (geology); Geology; Geochemistry; Xenolith; Volcano","authors":[{"name":"Chusi Li","is_ca":false},{"name":"Joyashish Thakurta","is_ca":false},{"name":"Edward M. Ripley","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.04175478051256799,"gpt":0.2140118333711938,"spread":0.1722570528586258,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001503754,0.0001645202,0.0003151031,0.00003935055,0.0001629719,0.00002025066,0.0002175827,0.0001395205,0.00706895],"category_scores_gemma":[0.0001076787,0.00009177886,0.0000464815,0.00009591665,0.0003342498,0.00005446519,0.00005449592,0.0001937872,0.0001160157],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":9.855561e-7,"about_ca_system_score_gemma":0.000005704365,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01529018,"about_ca_topic_score_gemma":0.0885349,"domain_scores_codex":[0.9988688,0.0001929928,0.0001861665,0.0003643439,0.00008147424,0.0003062114],"domain_scores_gemma":[0.9989555,0.0006225964,0.00006360968,0.0001663736,0.00003767412,0.0001542581],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002687747,0.00001778824,0.994628,0.000004378175,0.0000515796,0.00003308891,0.000251265,0.00001399877,0.001630321,0.00005409737,0.00208794,0.0009587983],"study_design_scores_gemma":[0.0002604328,0.0002369731,0.994589,0.00001224213,0.00005237283,0.00002945763,0.00005099135,0.0004213239,0.0002056784,0.00271984,0.001290336,0.0001313498],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9917161,0.000852873,0.00006012719,0.00588594,0.00007682971,0.00008612239,0.0001427131,0.00001471198,0.001164603],"genre_scores_gemma":[0.9910834,0.0001864718,0.0001732198,0.0079173,0.00009705628,0.00000309858,0.00008869666,0.000001789392,0.0004490115],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07324471,"threshold_uncertainty_score":0.9938387,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2833552847","doi":"10.1007/s00710-018-0607-6","title":"Origin of complex zoning in olivine from diverse, diamondiferous kimberlites and tectonic settings: Ekati (Canada), Alto Paranaiba (Brazil) and Kaalvallei (South Africa)","year":2018,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"Australian Research Council; University of Cape Town; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Kimberlite; Olivine; Geology; Geochemistry; Craton; Mantle (geology); Melt inclusions; Petrogenesis; Metasomatism; Partial melting; Chromite; Tectonics; Paleontology","authors":[{"name":"Emilie Lim","is_ca":false},{"name":"Andrea Giuliani","is_ca":false},{"name":"David Phillips","is_ca":false},{"name":"Karsten Goemann","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01432758123853402,"gpt":0.2029905390445894,"spread":0.1886629578060554,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001665168,0.0001588276,0.000422299,0.00008746787,0.0001085614,0.00001127394,0.0001003855,0.0001144842,0.001995717],"category_scores_gemma":[0.00006648978,0.00011891,0.00002436365,0.0001731627,0.000614401,0.00004480798,0.00004774894,0.0001543843,0.000005100538],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002399152,"about_ca_system_score_gemma":0.00002298795,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.2460589,"about_ca_topic_score_gemma":0.747816,"domain_scores_codex":[0.9988151,0.0001485613,0.0002496236,0.000366385,0.000092492,0.0003278906],"domain_scores_gemma":[0.9991999,0.0004570205,0.00008759804,0.00009890235,0.00002968092,0.0001269235],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006247058,0.00001100183,0.9966809,0.00001112102,0.00004767372,0.00001893373,0.0004329803,0.00003184056,0.0006389549,0.00007926121,0.0001842374,0.001800614],"study_design_scores_gemma":[0.0005291019,0.0002963337,0.9904671,0.000006851708,0.00005111624,0.00001356489,0.0001721937,0.003543706,0.00002722777,0.002914155,0.00183647,0.0001422031],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9949586,0.002053181,0.00001095125,0.00111891,0.00004041547,0.00004816681,0.0001177255,0.00000924193,0.001642754],"genre_scores_gemma":[0.9986413,0.00006832995,0.0004547547,0.0005676424,0.00006916455,0.000001024393,0.0001111107,0.000001848532,0.00008480196],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.501757,"threshold_uncertainty_score":0.9989166,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1978911963","doi":"10.1007/s00710-012-0207-9","title":"Potential geodynamic relationships between the development of peripheral orogens along the northern margin of Gondwana and the amalgamation of West Gondwana","year":2012,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"St. Francis Xavier University","funders":"Centre of Excellence for Core to Crust Fluid Systems, Australian Research Council; National Science Foundation","keywords":"Gondwana; Terrane; Geology; Paleontology; Supercontinent; Craton; Subduction; Rodinia; Lithosphere; Earth science; Tectonics","authors":[{"name":"J. Brendan Murphy","is_ca":true},{"name":"Sergei Pisarevsky","is_ca":false},{"name":"R. Damian Nance","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01206123171526003,"gpt":0.1897895756203929,"spread":0.1777283439051329,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000804742,0.00009002499,0.000249146,0.00003194122,0.0002070438,0.000003921967,0.0001421784,0.00008887027,0.0005436665],"category_scores_gemma":[0.00005278607,0.00003854643,0.00005885464,0.0001230845,0.0008338798,0.00004041535,0.00003052947,0.0001653259,0.000004146581],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001213366,"about_ca_system_score_gemma":0.00001730223,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002214573,"about_ca_topic_score_gemma":0.02312685,"domain_scores_codex":[0.9989095,0.0003682763,0.0003449636,0.0001031624,0.00009150641,0.00018254],"domain_scores_gemma":[0.9990681,0.00056081,0.0001752654,0.0001145552,0.0000428565,0.00003841694],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00006911262,0.00001000745,0.9942815,0.000009877667,0.0001017886,1.370686e-7,0.00103387,0.0003609783,0.0001900196,0.0003653058,0.00000471881,0.003572627],"study_design_scores_gemma":[0.0002964801,0.00004174129,0.9958794,0.000001729285,0.000133286,0.00001055791,0.0003045189,0.001696627,0.00003755682,0.001434469,0.0001176393,0.00004599871],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9956039,0.001606804,0.0002167233,0.002014262,0.00003497454,0.00007896068,0.00002392099,0.000002722583,0.0004177942],"genre_scores_gemma":[0.9995041,0.00002934581,0.0002235677,0.00005212097,0.00004708007,0.000001820273,0.0000879955,0.000001161724,0.00005273263],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02091228,"threshold_uncertainty_score":0.9946985,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2806183566","doi":"10.1007/s00710-018-0589-4","title":"Potential for offsetting diamond mine carbon emissions through mineral carbonation of processed kimberlite: an assessment of De Beers mine sites in South Africa and Canada","year":2018,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":69,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"University of British Columbia; Trent University; University of Alberta","funders":"","keywords":"Brucite; Carbonation; Kimberlite; Tailings; Carbonate minerals; Geochemistry; Mineral; Weathering; Olivine; Carbonate; Geology; Carbon dioxide; Carbon sequestration; Environmental science; Mineralogy; Dolomite; Chemistry; Mantle (geology); Magnesium","authors":[{"name":"Evelyn M. Mervine","is_ca":false},{"name":"Sasha Wilson","is_ca":true},{"name":"Ian Power","is_ca":true},{"name":"Gregory M. Dipple","is_ca":true},{"name":"Connor Turvey","is_ca":true},{"name":"Jessica Hamilton","is_ca":false},{"name":"Sterling Vanderzee","is_ca":true},{"name":"Mati Raudsepp","is_ca":true},{"name":"Colette Southam","is_ca":false},{"name":"Juerg Matter","is_ca":false},{"name":"P. B. Kelemen","is_ca":false},{"name":"Johann Stiefenhofer","is_ca":false},{"name":"Zandile Miya","is_ca":false},{"name":"Gordon Southam","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0112351505255278,"gpt":0.2765008007192191,"spread":0.2652656501936913,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001470547,0.00008865915,0.0001690275,0.00004461124,0.00005521381,0.000003857248,0.0000515754,0.00008551966,0.0001000503],"category_scores_gemma":[0.00005559712,0.00008076955,0.00001479114,0.00007836067,0.0002469278,0.00007515414,0.00003067667,0.00007350463,4.891057e-8],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00004116221,"about_ca_system_score_gemma":0.00007413053,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1096844,"about_ca_topic_score_gemma":0.5825613,"domain_scores_codex":[0.9992468,0.00007162539,0.000232015,0.0001988645,0.00006987431,0.0001808445],"domain_scores_gemma":[0.999641,0.00008812884,0.0001170034,0.00007343889,0.00003320624,0.00004723128],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001243252,0.0001091995,0.6896423,0.00002921415,0.00001803308,0.00000502097,0.003302189,0.001125717,0.3048838,0.0003482431,0.0002303154,0.0001815627],"study_design_scores_gemma":[0.001207293,0.001014906,0.9335632,0.00001033845,0.00005622492,0.00002710138,0.0008017221,0.06000672,0.001770875,0.0006633543,0.0007076963,0.0001705082],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9964999,0.00003128461,0.0001636249,0.0008365553,0.00005896811,0.0001224409,0.00002285247,0.000004166118,0.002260184],"genre_scores_gemma":[0.9967539,0.000002579476,0.002694326,0.0001216567,0.00004540756,0.0000208588,0.00006036587,0.000003951926,0.0002969522],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.472877,"threshold_uncertainty_score":0.8962443,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2042795351","doi":"10.1007/s00710-015-0368-4","title":"A primary natrocarbonatitic association in the Deep Earth","year":2015,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Stornoway Diamond (Canada)","funders":"","keywords":"Geology; Mantle (geology); Geochemistry; Silicate; Chromite; Melt inclusions; Carbonate; Diamond; Stishovite; Forsterite; Ultramafic rock; Mineralogy; Mafic; Partial melting; Chemistry; Materials science; Quartz; Metallurgy","authors":[{"name":"Felix V. Kaminsky","is_ca":true},{"name":"I. D. Ryabchikov","is_ca":false},{"name":"Richard Wirth","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0107973431408797,"gpt":0.1829412378158741,"spread":0.1721438946749944,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000450366,0.00006158418,0.0001361713,0.00004500983,0.00002960439,0.000008908457,0.00009212948,0.00009101879,0.0004080337],"category_scores_gemma":[0.00009015758,0.00003564128,0.00002307122,0.000138836,0.00005900894,0.00002770074,0.000007658945,0.0001589833,0.00004142216],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002458754,"about_ca_system_score_gemma":0.00001225719,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002474958,"about_ca_topic_score_gemma":0.03023752,"domain_scores_codex":[0.9992491,0.0002102103,0.0001086066,0.0001324949,0.00009910551,0.0002004728],"domain_scores_gemma":[0.9995372,0.0003059882,0.00003222017,0.00005596123,0.00001957254,0.0000490608],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002128896,0.00001083227,0.9981845,0.000001495979,0.00001029877,0.00001726203,0.0001216029,0.0001599196,0.00001940493,0.000280232,0.00009605647,0.001077113],"study_design_scores_gemma":[0.0002922697,0.0001370204,0.9702522,3.763922e-7,0.00001759529,0.00002655753,0.00004550991,0.003432926,0.000001612189,0.02346993,0.002271155,0.00005288606],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9494939,0.0009260535,0.000004732809,0.005583835,0.00005724954,0.00002860632,0.000002422377,0.000007142385,0.0438961],"genre_scores_gemma":[0.9955961,0.00002458837,0.00008137976,0.003889973,0.00007052349,0.000001472239,0.0000580696,4.644472e-7,0.000277403],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04610227,"threshold_uncertainty_score":0.9874581,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1999592091","doi":"10.1007/s00710-006-0124-x","title":"Carbonate alteration associated with talc-chlorite mineralization in the eastern Pyrenees, with emphasis on the St. Barthelemy Massif","year":2006,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université Laval","funders":"","keywords":"Calcite; Geology; Geochemistry; Chlorite; Massif; Hydrothermal circulation; Mineralogy; Mineralization (soil science); Talc; Radiogenic nuclide; Quartz; Mantle (geology); Paleontology","authors":[{"name":"Philippe Boulvais","is_ca":false},{"name":"P. de Parseval","is_ca":false},{"name":"Alan D’hulst","is_ca":true},{"name":"P. Paris","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.008321641242339223,"gpt":0.1670607878041852,"spread":0.158739146561846,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002606509,0.0001449866,0.00017915,0.00006278532,0.0001389454,0.00003437625,0.0001186752,0.00008808252,0.0005623127],"category_scores_gemma":[0.00001834238,0.00006021343,0.0000264841,0.0002768309,0.0001935671,0.00005118479,0.000005514949,0.0001634178,0.00001029221],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002263841,"about_ca_system_score_gemma":0.000008510634,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.007562725,"about_ca_topic_score_gemma":0.1682576,"domain_scores_codex":[0.9989101,0.0002926717,0.0001601047,0.000241221,0.0001377549,0.0002581471],"domain_scores_gemma":[0.9994177,0.0003420511,0.00007061742,0.0001114467,0.0000301698,0.00002803419],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001518792,0.00003722867,0.9894677,0.000001693678,0.00002956224,0.00003117853,0.00007023053,0.008385675,0.0000620108,0.001227872,0.0001479554,0.0003869706],"study_design_scores_gemma":[0.0005533835,0.0005846891,0.9686385,0.000006454419,0.00004798441,0.00002702623,0.00004339344,0.02588872,0.00001388702,0.00292465,0.001149972,0.0001213439],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9868351,0.0001802755,0.00003614748,0.0077792,0.00002312573,0.0000936243,0.00002842111,0.00001252025,0.00501157],"genre_scores_gemma":[0.9968003,0.00001262655,0.0000193574,0.002030868,0.00007415871,0.000007540263,0.0006107423,0.000002016144,0.0004423959],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1606949,"threshold_uncertainty_score":0.999046,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2039923357","doi":"10.1007/s00710-009-0047-4","title":"Crystallisation conditions (T, P, fO2) from mineral chemistry of Cu- and Au-mineralised alkaline intrusions in the Red River–Jinshajiang alkaline igneous belt, western Yunnan Province, China","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"National Key Research and Development Program of China; Natural Sciences and Engineering Research Council of Canada; Chinese Academy of Sciences","keywords":"Geology; Plagioclase; Geochemistry; Igneous rock; Amphibole; Quartz monzonite; Biotite; Mineral; Intrusion; Fractional crystallization (geology); Pluton; Basalt; Chemistry; Quartz","authors":[{"name":"Bi Xianwu","is_ca":false},{"name":"Ruizhong Hu","is_ca":false},{"name":"J. J. Hanley","is_ca":true},{"name":"James E. Mungall","is_ca":true},{"name":"Shang Linbo","is_ca":false},{"name":"Kaixing Wu","is_ca":false},{"name":"Suang Yan","is_ca":false},{"name":"Hongli Li","is_ca":false},{"name":"Xiaoyan Hu","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.007488572196949418,"gpt":0.2026324819051167,"spread":0.1951439097081673,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001877737,0.0001865373,0.000375994,0.00007787053,0.0001343774,0.00001444841,0.0001784753,0.0001862142,0.00145678],"category_scores_gemma":[0.0000616772,0.0001234423,0.00006165792,0.0001912525,0.0004067708,0.00008265531,0.00002229316,0.0002340617,0.000004653381],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003274224,"about_ca_system_score_gemma":0.00002372628,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0199065,"about_ca_topic_score_gemma":0.07223262,"domain_scores_codex":[0.9987099,0.0001753343,0.0003608167,0.0003428287,0.0001102608,0.000300817],"domain_scores_gemma":[0.9993275,0.0002452854,0.0001275584,0.0001716317,0.00002987969,0.00009817388],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002336215,0.0001515467,0.9181338,0.00001691714,0.00005028418,0.0001002353,0.0006604121,0.0006725251,0.07783717,0.0001694345,0.0004414867,0.001532595],"study_design_scores_gemma":[0.0008639612,0.0002994608,0.9799778,0.000009265563,0.00007827149,0.00007859836,0.00005047639,0.004774687,0.0000862661,0.012948,0.0006773233,0.000155859],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9908922,0.0002964049,0.0000263802,0.006680632,0.00003156643,0.0001103275,0.0002795324,0.00001446818,0.001668535],"genre_scores_gemma":[0.9954661,0.00009263363,0.0002263134,0.001166506,0.0001632194,0.000002961677,0.00256924,0.000001860671,0.0003111961],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0777509,"threshold_uncertainty_score":0.999456,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1982002946","doi":"10.1007/s00710-005-0088-2","title":"A preliminary geological and geochemical study of the Xiangquan thallium deposit, eastern China: the world’s first thallium-only mine","year":2005,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Thallium and Germanium Studies","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université du Québec; Université du Québec à Montréal","funders":"Chinese Academy of Geological Sciences; HORIZON EUROPE Excellent Science; Natural Science Foundation of Anhui Province; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Geochemistry; Thallium; Pyrite; Ordovician; Anticline; Hydrothermal circulation; Cretaceous; Ore genesis; Fluid inclusions; Tectonics; Paleontology; Chemistry","authors":[{"name":"Taofa Zhou","is_ca":false},{"name":"Yu Fan","is_ca":false},{"name":"Feng Yuan","is_ca":false},{"name":"M. A. Wu","is_ca":false},{"name":"M. J. Hou","is_ca":false},{"name":"Gabriel Voicu","is_ca":true},{"name":"Qiaoqing Hu","is_ca":false},{"name":"Q. M. Zhang","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.007740270283804459,"gpt":0.2127429743902946,"spread":0.2050027041064901,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000194599,0.0002159944,0.0003042833,0.00002747542,0.000321244,0.000009686813,0.0003237666,0.0001137656,0.0002257412],"category_scores_gemma":[0.00001598279,0.0001153266,0.00005356607,0.0001161922,0.000959889,0.00005994827,0.0008171003,0.0002785847,0.00001783111],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001566978,"about_ca_system_score_gemma":0.000003856117,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001155748,"about_ca_topic_score_gemma":0.03744057,"domain_scores_codex":[0.9986601,0.0001944016,0.0002619172,0.0003934157,0.000143173,0.000346921],"domain_scores_gemma":[0.9993061,0.0002185662,0.00009914384,0.0003064194,0.000006451193,0.00006331078],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001985039,0.0003829458,0.9938929,0.000008665552,0.00005629112,0.00001656798,0.002402617,0.000169288,0.0007991557,0.000177591,0.001474287,0.0004212075],"study_design_scores_gemma":[0.0007539738,0.0007266535,0.9942194,0.000003828518,0.00009458005,0.0002875011,0.0001839283,0.0003675867,0.00006452833,0.0001136415,0.003056386,0.0001279984],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9825934,0.0008999569,0.00000532687,0.01189111,0.00009332327,0.0002664062,0.000004311567,0.00001644955,0.004229678],"genre_scores_gemma":[0.9965569,0.00005938397,0.00005047764,0.0005964348,0.0001291439,0.00003532917,0.000002241936,0.000008689578,0.002561345],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03628482,"threshold_uncertainty_score":0.9801236,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2129833445","doi":"10.1007/s007100070018","title":"Garnet and diopside-bearing diamondites (framesites)","year":2000,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Memorial University of Newfoundland","funders":"Memorial University of Newfoundland; Österreichischen Akademie der Wissenschaften","keywords":"Geology; Eclogite; Pyrope; Mantle (geology); Peridotite; Geochemistry; Diopside; Olivine; Trace element; Silicate; Omphacite; Kimberlite; Mineralogy; Pyroxene; Grossular; Metasomatism; Almandine; Metamorphic rock; Chemistry; Subduction","authors":[{"name":"G. Kurat","is_ca":false},{"name":"G. Dobosi","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005255021378427259,"gpt":0.1708021666863194,"spread":0.1655471453078922,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001007254,0.0001110331,0.0002121892,0.0000446993,0.0001060571,0.00001861788,0.00007090566,0.0001145209,0.03064138],"category_scores_gemma":[0.0000174603,0.00007849314,0.00003075913,0.00008546485,0.000254338,0.00005706139,0.00001251172,0.0001495633,0.0001891512],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":4.026321e-7,"about_ca_system_score_gemma":0.000003065012,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002257076,"about_ca_topic_score_gemma":0.003279406,"domain_scores_codex":[0.9992079,0.00006686917,0.0001291016,0.0002732793,0.00004654635,0.0002762702],"domain_scores_gemma":[0.9995666,0.0002009829,0.00002006151,0.00008113244,0.000008279444,0.0001229063],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003941396,0.000007633636,0.9720128,0.0000032592,0.00002331,0.0000251242,0.00003359227,0.000142044,0.0002528685,0.0001388258,0.0002035017,0.02711761],"study_design_scores_gemma":[0.0002004218,0.0001552509,0.9771669,0.000001190237,0.00003315138,0.0000987005,0.000007525612,0.00209713,0.00003239052,0.01205415,0.008038555,0.0001146509],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9804447,0.00226905,0.000006181752,0.001523292,0.00002713544,0.00002441438,0.00001370864,0.0000231787,0.01566835],"genre_scores_gemma":[0.9959977,0.000407881,0.000204826,0.001393946,0.00008743461,8.484158e-7,0.00009459769,0.00000113683,0.001811653],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03045222,"threshold_uncertainty_score":0.9702448,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2060014891","doi":"10.1007/s00710-009-0055-4","title":"Iron isotope compositions of carbonatites record melt generation, crystallization, and late-stage volatile-transport processes","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University","funders":"","keywords":"Carbonatite; Igneous rock; Geochemistry; Metasomatism; Silicate; Geology; Mantle (geology); Carbonate; Large igneous province; Isotope fractionation; Silicate minerals; Mineralogy; Fractional crystallization (geology); Fractionation; Chemistry; Magmatism","authors":[{"name":"Clark M. Johnson","is_ca":false},{"name":"Keith Bell","is_ca":true},{"name":"Brian L. Beard","is_ca":false},{"name":"Aaron I. Shultis","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01008684713456572,"gpt":0.1959601959032318,"spread":0.1858733487686661,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00007038047,0.0001009239,0.0002188643,0.00006454322,0.00009989558,0.000006996955,0.00005598057,0.00009632724,0.001757804],"category_scores_gemma":[0.00002068887,0.00007641729,0.00002264942,0.0001565528,0.0001598348,0.00007120255,0.000003946334,0.00007455122,0.000002598392],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":6.374703e-7,"about_ca_system_score_gemma":0.00001485423,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00123179,"about_ca_topic_score_gemma":0.0130899,"domain_scores_codex":[0.9993215,0.00004640765,0.000216088,0.0002112938,0.00005711007,0.0001475592],"domain_scores_gemma":[0.9996423,0.00008421481,0.00006472095,0.00006378372,0.00007859188,0.00006634719],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004012949,0.00002977141,0.984654,0.00002633262,0.00001944771,0.000006096446,0.00009759307,0.002642728,0.01085563,0.0004063011,0.0000584816,0.001163482],"study_design_scores_gemma":[0.0002605717,0.0004450293,0.9782503,0.000003388577,0.00006247759,0.000009701063,0.00001054844,0.01392727,0.0003665342,0.005138653,0.001395895,0.000129674],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9948153,0.001063005,0.0002932504,0.00173617,0.00002577766,0.00005277864,0.00005917489,0.00001457848,0.001939901],"genre_scores_gemma":[0.997216,0.0003372736,0.0007430476,0.0006639392,0.00005001234,9.834069e-7,0.0005835732,9.729735e-7,0.0004041582],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01185811,"threshold_uncertainty_score":0.9991547,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1969957338","doi":"10.1007/s007100200000","title":"Melting experiments on SiO 2 -rich lamproites to 6.4 GPa and their bearing on the sources of lamproite magmas","year":2002,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Western University; Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; Lakehead University","keywords":"Phlogopite; Liquidus; Geology; Partial melting; Solidus; Leucite; Kimberlite; Olivine; Geochemistry; Silicate; Peridotite; Mantle (geology); Mineralogy; Phase (matter); Materials science; Chemistry","authors":[{"name":"Roger H. Mitchell","is_ca":true},{"name":"A. D. Edgar","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02157913648913467,"gpt":0.1926849791938824,"spread":0.1711058427047478,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001333069,0.0001244911,0.000215151,0.00006495494,0.00012259,0.0000124413,0.0001109845,0.00007366539,0.003011876],"category_scores_gemma":[0.00006636374,0.00006418161,0.00003372382,0.0001154779,0.0001281226,0.00002014822,0.00002774077,0.0001398992,0.00004575791],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":6.923649e-7,"about_ca_system_score_gemma":0.000001715328,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0006725998,"about_ca_topic_score_gemma":0.0005503925,"domain_scores_codex":[0.999226,0.00008214877,0.000145014,0.0002499329,0.00006430357,0.0002326462],"domain_scores_gemma":[0.9992375,0.0005042175,0.00004535487,0.0001068521,0.00001286202,0.00009316434],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000126515,0.00004886784,0.9670583,0.000007082355,0.00006797965,0.000007693476,0.001171323,0.0005991237,0.008658022,0.0008313405,0.0004818822,0.02094187],"study_design_scores_gemma":[0.000741232,0.002620687,0.9621049,0.00001997594,0.00004606771,0.00004321583,0.000388506,0.007957469,0.01099302,0.008741539,0.005971093,0.0003722497],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9892607,0.0006775875,0.000006158769,0.004384206,0.00003195187,0.00005653712,0.000008162343,0.00001049917,0.005564171],"genre_scores_gemma":[0.9968803,0.00003849887,0.0001048835,0.002145467,0.0000670076,0.000001688426,0.000008953705,0.000001509224,0.000751669],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02056962,"threshold_uncertainty_score":0.9978995,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2920856122","doi":"10.1007/s00710-019-00654-2","title":"The origin of the carbonate-hosted Huize Zn–Pb–Ag deposit, Yunnan province, SW China: constraints from the trace element and sulfur isotopic compositions of pyrite","year":2019,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":38,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Ministère de l’Emploi et de la Solidarité Sociale (Québec); Université du Québec à Montréal","funders":"CAS-SAFEA International Partnership Program for Creative Research Teams; National Natural Science Foundation of China","keywords":"Pyrite; Sphalerite; Galena; Geology; Geochemistry; δ34S; Mineralogy; Volcanogenic massive sulfide ore deposit; Mineralization (soil science); Sulfide minerals; Sulfur; Sulfide; Hydrothermal circulation; Fluid inclusions; Chemistry","authors":[{"name":"Ruizhong Hu","is_ca":false},{"name":"Xiaowen Huang","is_ca":false},{"name":"Jianfeng Gao","is_ca":false},{"name":"Christian Sasseville","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005966151203676457,"gpt":0.1996418832899489,"spread":0.1936757320862724,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002676749,0.0001254696,0.0002242456,0.00001746698,0.0002178864,0.00001892602,0.0005202949,0.0001015799,0.00002145499],"category_scores_gemma":[0.00002954174,0.00006653323,0.00004768471,0.00009886776,0.0006404664,0.00004077106,0.0002365932,0.0002219476,0.00000107621],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006232416,"about_ca_system_score_gemma":0.00004947654,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0006178988,"about_ca_topic_score_gemma":0.0007422719,"domain_scores_codex":[0.9989236,0.0002375172,0.0002636314,0.0002620622,0.00008760575,0.0002255649],"domain_scores_gemma":[0.9988601,0.000447972,0.0001665045,0.0004298838,0.00006448293,0.00003110968],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001253471,0.0001566797,0.7032539,0.00008914402,0.0003032676,0.00001721203,0.003017214,0.0003216388,0.1732159,0.1149942,0.0009392245,0.003566286],"study_design_scores_gemma":[0.001544112,0.0003296244,0.9660658,0.00003895757,0.00006450619,0.000134031,0.000171432,0.005889868,0.007581407,0.006785929,0.01120492,0.0001893762],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9831895,0.0007311029,0.0005389269,0.01202144,0.0002680999,0.0002428978,0.0000213597,0.00001214241,0.002974523],"genre_scores_gemma":[0.9986189,0.00004224614,0.0002819136,0.000314171,0.0000340211,0.00001151199,0.000006109341,0.000001784643,0.0006893405],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2628119,"threshold_uncertainty_score":0.2713146,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2805662133","doi":"10.1007/s00710-018-0577-8","title":"The birth, growth and ageing of the Kaapvaal subcratonic mantle","year":2018,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Alberta","funders":"Deutsche Forschungsgemeinschaft","keywords":"Mantle (geology); Geology; Geochemistry; Ageing; Medicine","authors":[{"name":"Gerhard P. Brey","is_ca":false},{"name":"Qin Shu","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.005312086436175122,"gpt":0.1735889515197946,"spread":0.1682768650836194,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000135463,0.00006539451,0.0001208389,0.00001699371,0.0002800247,0.000008988058,0.0001304263,0.0000639458,0.000794191],"category_scores_gemma":[0.00004311509,0.00002859855,0.00003383174,0.00009928253,0.0009850485,0.00002009955,0.00003432675,0.0001008833,0.0000145036],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":2.467222e-7,"about_ca_system_score_gemma":0.000005449616,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001411386,"about_ca_topic_score_gemma":0.01139005,"domain_scores_codex":[0.999417,0.00009525616,0.0001175777,0.0001380093,0.00004678418,0.0001853492],"domain_scores_gemma":[0.9995692,0.0002353156,0.00004409172,0.00009194024,0.00002034863,0.00003908279],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004400774,0.000004209486,0.9929277,0.00000444626,0.00002625517,0.000004942675,0.00004669531,0.000003382974,0.001344804,0.002597594,0.0001232565,0.002872658],"study_design_scores_gemma":[0.0001317598,0.0001791186,0.9674075,0.000001075163,0.00002350936,0.00004215819,0.00001988212,0.000780328,0.0003476593,0.02805589,0.00296397,0.00004714453],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9886545,0.001162862,0.000005778523,0.003781777,0.00009634558,0.00002316812,0.000007788013,0.000005046374,0.006262741],"genre_scores_gemma":[0.9988309,0.0001369862,0.00002639928,0.0006247158,0.00007859249,3.332178e-7,0.000004176728,6.757037e-7,0.0002972418],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02552024,"threshold_uncertainty_score":0.8695834,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1086714793","doi":"10.1007/s00710-015-0402-6","title":"Mineralogy of the P-12 K-Ti-richterite diopside olivine lamproite from Wajrakarur, Andhra Pradesh, India: implications for subduction-related magmatism in eastern India","year":2015,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; Lakehead University","keywords":"Phlogopite; Olivine; Geology; Pyroxene; Geochemistry; Diopside; Phenocryst; Mineralogy; Pseudomorph; Volcanic rock; Quartz; Mantle (geology)","authors":[{"name":"Gurmeet Kaur","is_ca":false},{"name":"Roger H. Mitchell","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01777325209386312,"gpt":0.2140933970508689,"spread":0.1963201449570058,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000215919,0.0001742546,0.0004257588,0.0001276943,0.00007592582,0.00001154217,0.0002347217,0.0002579624,0.0005234861],"category_scores_gemma":[0.0001157653,0.0001141675,0.00008744246,0.0002883347,0.0003579423,0.00008861512,0.00004414506,0.0002329668,0.0000190098],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004262562,"about_ca_system_score_gemma":0.00003231719,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.007303388,"about_ca_topic_score_gemma":0.03109769,"domain_scores_codex":[0.9985715,0.0001989388,0.0004424672,0.0003603489,0.00007697174,0.0003498427],"domain_scores_gemma":[0.9990748,0.00033063,0.0001816783,0.0002241207,0.00006099321,0.0001278047],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008835288,0.00004587324,0.9947195,0.000008525416,0.00006074298,0.000003338417,0.0002135726,0.0002308047,0.001610875,0.0004910711,0.0003427985,0.002184513],"study_design_scores_gemma":[0.0009798659,0.0002438817,0.9563319,0.000005121858,0.00007126027,0.00004725943,0.00004019705,0.001183884,0.00003575857,0.04002061,0.000913121,0.0001271032],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9902768,0.001258043,0.00004731865,0.006795237,0.0002294119,0.0001908368,0.0002458124,0.00001453578,0.0009420193],"genre_scores_gemma":[0.9977403,0.00005346259,0.0004424906,0.0005786218,0.0001037591,0.00001718748,0.0005616746,0.000003430857,0.0004990511],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.03952954,"threshold_uncertainty_score":0.999307,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1987671524","doi":"10.1007/s00710-005-0095-3","title":"The Spačice eclogite: constraints on the P–T–t history of the Gföhl granulite terrane, Moldanubian Zone, Bohemian Massif","year":2005,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"","keywords":"Eclogite; Granulite; Geology; Metamorphism; Omphacite; Geochemistry; Terrane; Metamorphic rock; Petrology; Massif; Geomorphology; Subduction; Seismology; Tectonics; Facies","authors":[{"name":"L. Gordon Medaris","is_ca":false},{"name":"E. D. Ghent","is_ca":true},{"name":"H. F. Wang","is_ca":false},{"name":"John Fournelle","is_ca":false},{"name":"Emil Jelínek","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01158249980955542,"gpt":0.1709203301282805,"spread":0.1593378303187251,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003998504,0.0001521096,0.0002252544,0.00003008334,0.0002697726,0.00000978331,0.0004077312,0.0001396458,0.005559425],"category_scores_gemma":[0.00008879677,0.00006115196,0.0001253323,0.0001116039,0.00210024,0.00002882923,0.00003191369,0.0003655334,0.00007112726],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000675376,"about_ca_system_score_gemma":0.00003042496,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001140322,"about_ca_topic_score_gemma":0.01460312,"domain_scores_codex":[0.9987033,0.0003066362,0.0002565091,0.0002487511,0.0001335799,0.0003512512],"domain_scores_gemma":[0.9985847,0.000900024,0.0001149082,0.000297757,0.000027051,0.00007548468],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0005471453,0.0001185205,0.823141,0.0000186921,0.0002653797,0.000027993,0.0007458495,0.001198169,0.003255678,0.01141377,0.04094572,0.1183221],"study_design_scores_gemma":[0.0004499684,0.0002614172,0.6958866,0.000005936985,0.00008686533,0.00008255783,0.0001043326,0.002358208,0.0001255119,0.00581719,0.2946415,0.0001799705],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8966187,0.002329391,0.000009095927,0.04739656,0.0003413633,0.00009716358,0.00004505477,0.00001214997,0.0531505],"genre_scores_gemma":[0.9869768,0.0001344233,0.00003951293,0.006689496,0.0001248049,0.000002928667,0.00002241021,0.000001637121,0.006008008],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2536958,"threshold_uncertainty_score":0.9953496,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2242666027","doi":"10.1007/s00710-015-0413-3","title":"Tululite, Ca14(Fe3+,Al)(Al,Zn,Fe3+,Si,P,Mn,Mg)15O36: a new Ca zincate-aluminate from combustion metamorphic marbles, central Jordan","year":2015,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Carleton University; University of Ottawa","funders":"Siberian Branch, Russian Academy of Sciences; Russian Foundation for Basic Research","keywords":"Brownmillerite; Protolith; Geology; Metamorphic rock; Mineralogy; Calcite; Mineral; Aluminate; Geochemistry; Chemistry; Cement; Metallurgy; Perovskite (structure); Crystallography; Materials science","authors":[{"name":"Hani Khoury","is_ca":false},{"name":"É. V. Sokol","is_ca":false},{"name":"Svetlana N. Kokh","is_ca":false},{"name":"Yurii V. Seryotkin","is_ca":false},{"name":"E. N. Nigmatulina","is_ca":false},{"name":"S. V. Goryaĭnov","is_ca":false},{"name":"Е. В. Белогуб","is_ca":false},{"name":"Ian D. Clark","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01830524888018559,"gpt":0.2025106672903,"spread":0.1842054184101145,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003594315,0.0003674582,0.000700113,0.0001485515,0.0001785853,0.00004866068,0.0003305905,0.0003252937,0.009155368],"category_scores_gemma":[0.0001202788,0.0002770394,0.0001602871,0.0003452308,0.0004514979,0.0001713011,0.00006556141,0.0004739157,0.0005418718],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009180478,"about_ca_system_score_gemma":0.00008302731,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.06412764,"about_ca_topic_score_gemma":0.05368312,"domain_scores_codex":[0.997295,0.0003875158,0.0004591891,0.0007365639,0.0002388111,0.0008829044],"domain_scores_gemma":[0.9984181,0.0002929555,0.0001519711,0.0002895007,0.00008265362,0.0007648183],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0007151488,0.0001165755,0.926513,0.00001359358,0.0003271494,0.0002961759,0.0002911063,0.001033916,0.001553753,0.0005933598,0.06051999,0.008026235],"study_design_scores_gemma":[0.00288206,0.001028264,0.6761332,0.00001159899,0.0005139177,0.0002318965,0.0001734532,0.01634297,0.0001935675,0.0497523,0.2519415,0.0007952459],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9748698,0.004500093,0.0001092772,0.01569758,0.0004931269,0.0001089698,0.0002638247,0.00006078574,0.003896482],"genre_scores_gemma":[0.9866893,0.0002982846,0.0009637903,0.006705902,0.0003058765,0.000003347535,0.002767485,0.000006093193,0.00225992],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2503798,"threshold_uncertainty_score":0.9999682,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2620928737","doi":"10.1007/s00710-017-0517-z","title":"Hydrothermal titanite from the Chengchao iron skarn deposit: temporal constraints on iron mineralization, and its potential as a reference material for titanite U–Pb dating","year":2017,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of New Brunswick","funders":"National Key Research and Development Program of China; China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Titanite; Zircon; Geology; Skarn; Geochronology; Geochemistry; Diorite; Metasomatism; Quartz; Mineralization (soil science); Hydrothermal circulation; Mineralogy; Fluid inclusions; Mantle (geology)","authors":[{"name":"Hao Hu","is_ca":false},{"name":"Jianwei Li","is_ca":false},{"name":"Christopher R.M. McFarlane","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0160248190208879,"gpt":0.2207759564064103,"spread":0.2047511373855224,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001530553,0.0001608395,0.0002302136,0.00002537968,0.0005545842,0.00009085648,0.0002048383,0.0001644671,0.004760001],"category_scores_gemma":[0.00008821474,0.0001017814,0.00003640688,0.00002258383,0.000349038,0.00009494512,0.00003800291,0.0001301295,0.00004374919],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001441386,"about_ca_system_score_gemma":0.000009014019,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005578151,"about_ca_topic_score_gemma":0.009488552,"domain_scores_codex":[0.9990044,0.0001047308,0.0001914611,0.0003476915,0.00007730693,0.0002743997],"domain_scores_gemma":[0.9994141,0.0001755231,0.0001291955,0.0001628104,0.00003336567,0.00008501557],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.001356479,0.00006125926,0.9148749,0.00004185285,0.000145674,0.0000755029,0.0002423783,0.0004242068,0.06761277,0.004464453,0.0005163578,0.01018417],"study_design_scores_gemma":[0.00119957,0.0007428137,0.9769971,0.00001323472,0.0001510478,0.00007859441,0.00004272374,0.01250937,0.0005569056,0.006077533,0.001343972,0.0002871505],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.993293,0.0002196992,0.00006410627,0.001815047,0.0001556614,0.0001227292,0.000367487,0.0000140584,0.003948218],"genre_scores_gemma":[0.9971152,0.00004263735,0.0002512793,0.00109849,0.0003009333,0.000004670381,0.0008450539,0.000003114582,0.0003386019],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06705587,"threshold_uncertainty_score":0.9961498,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2033358212","doi":"10.1007/s00710-006-0171-3","title":"Supergene leaching and formation of platinum in alluvium: evidence from Serro, Minas Gerais, Brazil","year":2006,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Iron oxide chemistry and applications","field":"Energy","cited_by":32,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université Laval","funders":"","keywords":"Alluvium; Geology; Platinum; Supergene (geology); Geochemistry; Fineness; Weathering; Leaching (pedology); Palladium; Mineralogy; Chemistry; Metallurgy; Geomorphology; Materials science; Soil science","authors":[{"name":"Alexandre Raphael Cabral","is_ca":true},{"name":"Georges Beaudoin","is_ca":true},{"name":"Marc Choquette","is_ca":true},{"name":"Bernd Lehmann","is_ca":false},{"name":"J. C. Polônia","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01217456615209099,"gpt":0.2411486142599603,"spread":0.2289740481078693,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001104181,0.00009728741,0.0001834484,0.00004998663,0.00005171995,0.000005329815,0.00006253013,0.0001499573,0.0001098448],"category_scores_gemma":[0.00002051235,0.00009777,0.00001823281,0.00005889899,0.0001032322,0.000125463,0.00003220023,0.0001221221,0.000003847129],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009803908,"about_ca_system_score_gemma":0.000008148918,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005401641,"about_ca_topic_score_gemma":0.007362433,"domain_scores_codex":[0.9993042,0.00005967484,0.0002564593,0.0001856147,0.00003813259,0.000155971],"domain_scores_gemma":[0.999549,0.0002244114,0.00006589563,0.0001202981,0.00001566015,0.00002478923],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.00007210457,0.00003906081,0.05487207,0.00003385872,0.000007863537,0.000006019552,0.0004367863,0.0006690359,0.9355555,0.006849339,0.0005467873,0.0009115398],"study_design_scores_gemma":[0.002320235,0.0001709585,0.7884134,0.00007013986,0.00007405442,0.0001569476,0.0001805525,0.006960615,0.1724154,0.01417171,0.01459872,0.0004672393],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.994697,0.001284184,0.000330641,0.00106007,0.00002925999,0.00003898497,0.00001229512,0.00001343817,0.002534133],"genre_scores_gemma":[0.9985437,0.00009141398,0.0005046941,0.0001265308,0.00009252143,0.00001734249,0.000123015,0.000006141029,0.0004946516],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7631401,"threshold_uncertainty_score":0.8165701,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2143943156","doi":"10.1007/s00710-010-0131-9","title":"Trace-element study and uranium-lead dating of perovskite from the Afrikanda plutonic complex, Kola Peninsula (Russia) using LA-ICP-MS","year":2010,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Geochronology; Geochemistry; Trace element; Perovskite (structure); Pegmatite; Uranium; Partial melting; Mantle (geology); Isotopic signature; Pluton; Strontium; Radiogenic nuclide; Mineralogy; Isotope; Chemistry; Materials science; Tectonics; Crystallography","authors":[{"name":"Ekaterina P. Reguir","is_ca":true},{"name":"Alfredo Camacho","is_ca":true},{"name":"Panseok Yang","is_ca":true},{"name":"Anton R. Chakhmouradian","is_ca":true},{"name":"Vadim S. Kamenetsky","is_ca":false},{"name":"Norman M. Halden","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02198872794288332,"gpt":0.234563432726079,"spread":0.2125747047831957,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004130633,0.0001576965,0.0003604067,0.00003980437,0.0002251062,0.00002629233,0.0001809594,0.0001224955,0.004056547],"category_scores_gemma":[0.0000498142,0.00009326526,0.00005255756,0.0001083955,0.00046781,0.00005358208,0.00005264728,0.0003606736,0.000006540966],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":7.906852e-7,"about_ca_system_score_gemma":0.00001368352,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01375636,"about_ca_topic_score_gemma":0.02779857,"domain_scores_codex":[0.9987257,0.0002690696,0.0002868741,0.0003352294,0.000110662,0.0002725279],"domain_scores_gemma":[0.9988582,0.0007536676,0.0001097852,0.0001710048,0.00002652725,0.00008088463],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008166695,0.00005388035,0.9812453,0.000004205818,0.00009003844,0.00001284358,0.0005002632,0.000115533,0.01437665,0.0001016076,0.00003873773,0.003379275],"study_design_scores_gemma":[0.000710648,0.0002975418,0.9720467,0.00000202298,0.0001472301,0.00004208034,0.0003384098,0.02349627,0.00004715426,0.001328721,0.001422582,0.0001206545],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9966906,0.0006148388,0.00002838226,0.001001071,0.00008210049,0.0001011319,0.00008853297,0.00001059143,0.001382764],"genre_scores_gemma":[0.9986502,0.00002946776,0.0007918238,0.0002630397,0.0001083397,0.000001386103,0.00009772841,0.000002127444,0.00005590017],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02338074,"threshold_uncertainty_score":0.9968539,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2068937457","doi":"10.1007/s00710-003-0007-3","title":"Comparison between magmatic activity and gold mineralization at Conical Seamount and Lihir Island, Papua New Guinea","year":2003,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seamount; Geochemistry; Stockwork; Phenocryst; Pyrite; Mineralization (soil science); Sericite; Basalt; Igneous rock; Volcanic rock; Hydrothermal circulation; Volcano; Chalcopyrite; Paleontology; Chemistry","authors":[{"name":"D. M�ller","is_ca":false},{"name":"Leander Franz","is_ca":false},{"name":"Sven Petersen","is_ca":false},{"name":"Peter Herzig","is_ca":false},{"name":"Mark D. Hannington","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01882546149167604,"gpt":0.2366076218220944,"spread":0.2177821603304184,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001512872,0.0001668792,0.0004636828,0.00005148459,0.0001133757,0.00002267719,0.00005590815,0.0001958074,0.002206142],"category_scores_gemma":[0.00007741785,0.0001198781,0.00003347866,0.0001022367,0.0002679032,0.00006336704,0.00002768669,0.0001633604,0.00003003542],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002384603,"about_ca_system_score_gemma":0.00001099518,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00306537,"about_ca_topic_score_gemma":0.02974869,"domain_scores_codex":[0.9988513,0.0002139938,0.000215339,0.0003474858,0.0000756714,0.0002962174],"domain_scores_gemma":[0.9991943,0.0003989987,0.00007141222,0.00009536184,0.00001767569,0.000222278],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005323122,0.00001317566,0.9950488,0.00001516816,0.00004116348,0.000005834325,0.00004658605,0.00006403135,0.0005784676,0.0003625577,0.001001093,0.00276987],"study_design_scores_gemma":[0.0006809875,0.00031428,0.9824986,0.000002418106,0.0001130405,0.0000695443,0.000009865123,0.004012322,0.0000833177,0.004817982,0.007229848,0.0001677454],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9931136,0.001789338,0.0001613133,0.002088327,0.00004554117,0.00006410686,0.00002699041,0.00001529823,0.002695423],"genre_scores_gemma":[0.997223,0.0001675469,0.0002964386,0.0005433605,0.0000760852,9.483978e-7,0.0001305707,0.00000192566,0.001560102],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02668332,"threshold_uncertainty_score":0.998706,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2062964109","doi":"10.1007/s00710-012-0196-8","title":"Mineralogical, stable isotope, and fluid inclusion studies of spatially related porphyry Cu and epithermal Au-Te mineralization, Fakos Peninsula, Limnos Island, Greece","year":2012,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"","funders":"University of Windsor","keywords":"Sphalerite; Geology; Geochemistry; Fluid inclusions; Molybdenite; Pyrite; Argillic alteration; Galena; Hypogene; Chalcopyrite; Mineralization (soil science); Bornite; Mineralogy; Quartz; Chemistry; Copper","authors":[{"name":"Andrew P. Fornadel","is_ca":false},{"name":"Panagiotis Voudouris","is_ca":false},{"name":"Paul G. Spry","is_ca":false},{"name":"Vasilios Melfos","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01532764829392868,"gpt":0.2204299624065909,"spread":0.2051023141126622,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004349081,0.0002365787,0.0005792067,0.0001194483,0.0003290369,0.00001016137,0.0001045059,0.000236537,0.001523268],"category_scores_gemma":[0.0001369688,0.0001582494,0.00005062245,0.0002064179,0.0006820994,0.000177364,0.0001971378,0.0001697014,0.00001200759],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002615059,"about_ca_system_score_gemma":0.00001503335,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006733886,"about_ca_topic_score_gemma":0.0135302,"domain_scores_codex":[0.998369,0.0002519751,0.0004339707,0.0003541224,0.0001276589,0.000463227],"domain_scores_gemma":[0.9990679,0.0003622284,0.000152758,0.0001257142,0.00009508102,0.000196296],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001745904,0.00006304009,0.9853696,0.00004480411,0.0001287763,0.00001328387,0.0009070986,0.0001894279,0.009722793,0.0005781478,0.0002959927,0.002512505],"study_design_scores_gemma":[0.00101533,0.0007030854,0.9848723,0.00001192129,0.0001806255,0.0001572149,0.0001012041,0.004969033,0.0002086966,0.005337949,0.002157672,0.0002849603],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.982154,0.01480917,0.00002368295,0.001696997,0.0001142614,0.0001113899,0.00005732363,0.00001766959,0.001015564],"genre_scores_gemma":[0.9964879,0.001408233,0.0002587181,0.0007880487,0.000118294,0.000003137269,0.0002200735,0.000003535946,0.0007120507],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01433396,"threshold_uncertainty_score":0.9998804,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2101840425","doi":"10.1007/s00710-008-0017-2","title":"Metasomatic origin of garnet orthopyroxenites in the subcontinental lithospheric mantle underlying Pali Aike volcanic field, southern South America","year":2008,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Ottawa","funders":"","keywords":"Metasomatism; Geochemistry; Geology; Peridotite; Xenolith; Phlogopite; Mantle (geology); Olivine; Basalt; Craton; Partial melting; Tectonics; Paleontology","authors":[{"name":"Jian Wang","is_ca":true},{"name":"Kéiko Hattori","is_ca":true},{"name":"Charles R. Stern","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02481902378250617,"gpt":0.2152826863580022,"spread":0.190463662575496,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001455074,0.0001312474,0.0003314492,0.00005271149,0.00009177393,0.000006034778,0.0001769848,0.00009092425,0.004165028],"category_scores_gemma":[0.00004388298,0.00007624112,0.00008363437,0.0002644505,0.0002808727,0.00003129798,0.00001518362,0.000188051,0.00006368779],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":8.143512e-7,"about_ca_system_score_gemma":0.000009711831,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.008973801,"about_ca_topic_score_gemma":0.01177013,"domain_scores_codex":[0.998922,0.0002180868,0.0002611234,0.0002203414,0.00009583019,0.0002826116],"domain_scores_gemma":[0.999243,0.0004726506,0.0000923391,0.0001282696,0.00001501499,0.00004876322],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004415399,0.00002514928,0.997411,0.000009223867,0.00003497302,0.00004820499,0.000966889,0.0001413458,0.0001955988,0.0000542139,0.00007859316,0.0009906465],"study_design_scores_gemma":[0.0004184974,0.0004062257,0.9908827,0.000003297313,0.00007139275,0.0001337177,0.0009796297,0.003385362,0.00002211607,0.002632436,0.0009178626,0.0001467601],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9956057,0.001355113,0.00006718274,0.001210174,0.00003759201,0.00005478834,0.00002104449,0.000009934008,0.001638435],"genre_scores_gemma":[0.9978289,0.00009400382,0.0002845997,0.001399033,0.0000301962,0.000002466673,0.00006996778,0.000001587028,0.0002892509],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.006528306,"threshold_uncertainty_score":0.9976255,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2890712606","doi":"10.1007/s00710-018-0629-0","title":"Punctuated, long-lived emplacement history of the Renard 2 kimberlite, Canada, revealed by new high precision U-Pb groundmass perovskite dating","year":2018,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":true},"ca_institutions":"Stornoway Diamond (Canada); University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Johns Hopkins University","keywords":"Kimberlite; Diatreme; Geology; Geochemistry; Xenolith; Geochronology; Mantle (geology)","authors":[{"name":"Ilona M. Ranger","is_ca":true},{"name":"Larry M. Heaman","is_ca":true},{"name":"D. Graham Pearson","is_ca":true},{"name":"Colleen Muntener","is_ca":true},{"name":"V Zhuk","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.009321030883848488,"gpt":0.1738610583935143,"spread":0.1645400275096658,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002246489,0.0001580269,0.0003257379,0.00003413416,0.0001161448,0.000005924626,0.0002404656,0.0001278913,0.01132879],"category_scores_gemma":[0.00008911704,0.00009296116,0.00005604863,0.0001222004,0.0003729918,0.00004363331,0.0000502413,0.0001788863,0.00001768775],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002104604,"about_ca_system_score_gemma":0.0001457895,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.661681,"about_ca_topic_score_gemma":0.8354388,"domain_scores_codex":[0.9986354,0.0002204249,0.000313611,0.0003370799,0.0001719064,0.0003216271],"domain_scores_gemma":[0.9991534,0.0002755747,0.0001524114,0.0002170272,0.00006587466,0.0001357651],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002502377,0.00002215525,0.8644573,0.0000128314,0.00008789785,0.000008747979,0.0001499343,0.00008663377,0.003612214,0.00007318849,0.1267223,0.004516549],"study_design_scores_gemma":[0.0007270579,0.0005612394,0.9235155,0.00001049379,0.0001143682,0.00003698583,0.00003138286,0.001263176,0.0001647733,0.001917388,0.07144722,0.0002104101],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.990239,0.001548795,0.0001419892,0.002519848,0.0004734946,0.00007472064,0.00003914909,0.000009139943,0.004953904],"genre_scores_gemma":[0.9818891,0.00003943169,0.0002587309,0.001703419,0.0001481458,0.000001051469,0.0001971909,0.000001992042,0.01576091],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1737579,"threshold_uncertainty_score":0.989575,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1978875039","doi":"10.1007/s00710-010-0140-8","title":"Mineralogy, composition and PGM of chromitites from Pefki, Pindos ophiolite complex (NW Greece): evidence for progressively elevated fAs conditions in the upper mantle sequence","year":2010,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Hudbay Minerals (Canada)","funders":"State Scholarships Foundation; McGill University; Northwestern University","keywords":"Ophiolite; Chromite; Geology; Geochemistry; Chromitite; Mantle (geology); Partial melting; Olivine; Mineralogy; Paleontology","authors":[{"name":"Argirios Kapsiotis","is_ca":false},{"name":"Tassos Grammatikopoulos","is_ca":true},{"name":"Basilios Tsikouras","is_ca":false},{"name":"Konstantin Hatzipanagiotou","is_ca":false},{"name":"Federica Zaccarini","is_ca":false},{"name":"Giorgio Garuti","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.04475528018907661,"gpt":0.2843814464405975,"spread":0.2396261662515209,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002138677,0.0001388912,0.0003062752,0.00007988697,0.0001321112,0.00001737974,0.0001775241,0.0001559916,0.001414943],"category_scores_gemma":[0.00008438476,0.00008843657,0.00005303859,0.0001349397,0.0008253186,0.00009775623,0.00001952511,0.0002325479,0.000007730249],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001048808,"about_ca_system_score_gemma":0.00001376575,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004287192,"about_ca_topic_score_gemma":0.01159868,"domain_scores_codex":[0.9989259,0.000166464,0.0002604525,0.0003095497,0.00007205897,0.000265525],"domain_scores_gemma":[0.9984484,0.001195777,0.0001026944,0.0001268893,0.00006177937,0.00006440203],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001328607,0.00003497579,0.8083713,0.00001697785,0.00002997233,0.00001308584,0.00009604913,0.0000283523,0.1898679,0.0008212981,0.0002005161,0.0003866588],"study_design_scores_gemma":[0.0005403341,0.000283545,0.9779648,0.00001195365,0.000062092,0.00007980142,0.00003011173,0.00661371,0.0004177004,0.01358783,0.0002949778,0.000113196],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9928185,0.0006352941,0.00001860419,0.005566621,0.00005367133,0.0001975936,0.0005492994,0.00000951172,0.0001508908],"genre_scores_gemma":[0.9964738,0.00007576933,0.0008825787,0.001146735,0.00008326401,0.00001721116,0.001297281,0.00000161644,0.00002170128],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1894502,"threshold_uncertainty_score":0.9994979,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2078586481","doi":"10.1007/s00710-007-0220-6","title":"Another look at nagyágite from the type locality, S $\\check{\\rm{a}}$ c $\\check{\\rm{a}}$ rîmb, Romania: Replacement, chemical variation and petrogenetic implications","year":2007,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Crystal Structures and Properties","field":"Materials Science","cited_by":23,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Science North","funders":"Australian Research Council","keywords":"Telluride; Crystallography; Chemical composition; Chemistry; Mineralogy; Analytical Chemistry (journal); Materials science; Metallurgy","authors":[{"name":"Cristiana L. Ciobanu","is_ca":false},{"name":"Nigel J. Cook","is_ca":false},{"name":"Allan Pring","is_ca":false},{"name":"Gheorghe Damian","is_ca":true},{"name":"N. Căpraru","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01434804793124703,"gpt":0.2379401046268606,"spread":0.2235920566956136,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004810684,0.0002041257,0.0002632139,0.00003936787,0.0003045225,0.00005603406,0.000201547,0.0002420879,0.001004686],"category_scores_gemma":[0.00005153545,0.000145368,0.00003890418,0.00009670342,0.0004466109,0.00006505392,0.0002537308,0.0001654406,0.00004646335],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00004396116,"about_ca_system_score_gemma":0.0000265982,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001194005,"about_ca_topic_score_gemma":0.001667479,"domain_scores_codex":[0.9984893,0.0001423548,0.000339723,0.0005136207,0.0001127069,0.0004022514],"domain_scores_gemma":[0.9990639,0.0002787587,0.0001278185,0.0003810959,0.00006168416,0.00008672426],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.000596053,0.00002901766,0.05708787,0.00001236282,0.00004587319,0.00000496545,0.000716489,0.000007539799,0.9375274,0.00153703,0.001786487,0.000648945],"study_design_scores_gemma":[0.001646814,0.0005378373,0.9039378,0.00001131226,0.0001914028,0.0004074377,0.0001208866,0.000180245,0.02924276,0.007561407,0.05567624,0.0004858691],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9929876,0.002264251,0.0007214136,0.002553969,0.0002860259,0.0001716274,0.00005676402,0.00004443372,0.0009139501],"genre_scores_gemma":[0.9962226,0.0001018456,0.0005115372,0.002076255,0.000298247,0.00001462763,0.00006708446,0.00001969023,0.0006881084],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9082846,"threshold_uncertainty_score":0.9999085,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2048501150","doi":"10.1007/s00710-003-0016-2","title":"Mineralogy and geochemistry of silicate dyke rocks associated with carbonatites from the Khibina complex (Kola, Russia) ? isotope constraints on genesis and small-scale mantle sources","year":2004,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba; Carleton University","funders":"","keywords":"Carbonatite; Geology; Geochemistry; Mantle (geology); Silicate; Mantle plume; Igneous differentiation; Olivine; Magma; Silicic; Igneous rock; Petrology; Volcano; Lithosphere; Tectonics; Chemistry","authors":[{"name":"Sven Sindern","is_ca":false},{"name":"Anatoly N. Zaitsev","is_ca":false},{"name":"Keith Bell","is_ca":true},{"name":"A. R. Chakmouradian","is_ca":true},{"name":"U. Kramm","is_ca":false},{"name":"Jacques Moutte","is_ca":false},{"name":"Alexei S. Rukhlov","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01242300679462019,"gpt":0.1768954896873275,"spread":0.1644724828927073,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000131383,0.0001960909,0.0004138899,0.0000383299,0.0001507181,0.000015716,0.0001313861,0.0001865772,0.001093709],"category_scores_gemma":[0.00004151466,0.0001154538,0.00003851605,0.0001047676,0.001219679,0.00002284582,0.00003399831,0.0001867467,0.000004350964],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002016418,"about_ca_system_score_gemma":0.000015708,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01096334,"about_ca_topic_score_gemma":0.02507942,"domain_scores_codex":[0.9988953,0.0001116414,0.0002171299,0.0003922124,0.00008641778,0.0002972747],"domain_scores_gemma":[0.9989925,0.0006157379,0.0001147774,0.00013139,0.00003509513,0.000110484],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001385304,0.00004487672,0.9868513,0.000008779795,0.0001669095,0.00001987448,0.0001624889,0.0003712652,0.009938497,0.00006394536,0.00003643363,0.002197052],"study_design_scores_gemma":[0.0009113614,0.0004003166,0.9927087,0.0000105967,0.0001435083,0.00005403818,0.00009947831,0.0007922076,0.000763872,0.003839417,0.0001166746,0.0001597961],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9926749,0.001512888,0.00001295263,0.003504615,0.00001673026,0.00006822778,0.0002219682,0.00001462772,0.001973081],"genre_scores_gemma":[0.9981157,0.0001284843,0.0001698316,0.001072028,0.00004388492,0.000002619139,0.0003465679,0.000002790573,0.000118147],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01411608,"threshold_uncertainty_score":0.9998194,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2067375572","doi":"10.1007/s007100200029","title":"Accessory mineralogy of orangeite from Swartruggens, South Africa","year":2002,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Lakehead University","funders":"Lakehead University; Purdue University","keywords":"Geology; Calcite; Leucite; Geochemistry; Mineral; Mineralogy; Carbonatite; Paragenesis; Sanidine; Apatite; Quartz; Silicate; Plagioclase; Metamorphic rock; Chemistry; Paleontology","authors":[{"name":"A. L. Hammond","is_ca":true},{"name":"Roger H. Mitchell","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.02280626394069095,"gpt":0.178728790164524,"spread":0.1559225262238331,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009411408,0.0001636927,0.0004301513,0.0001016681,0.00007272183,0.000008042831,0.0001839663,0.0001965363,0.046631],"category_scores_gemma":[0.00003585805,0.000117778,0.00009202106,0.0001832009,0.0003596684,0.00005682881,0.00002817244,0.0001765614,0.000212504],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":7.638175e-7,"about_ca_system_score_gemma":0.000003694027,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002298024,"about_ca_topic_score_gemma":0.003179425,"domain_scores_codex":[0.9987599,0.0001464828,0.0002853641,0.000356137,0.00009290029,0.0003592232],"domain_scores_gemma":[0.9992702,0.0002897802,0.00009933791,0.0001707047,0.00003558407,0.0001344092],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00008860751,0.00004488249,0.9891703,0.000008886787,0.0001131548,0.00004507646,0.0004796888,0.0001986901,0.001945641,0.0001879419,0.003411701,0.004305456],"study_design_scores_gemma":[0.001028944,0.0005417605,0.9466485,0.000004023774,0.0002018612,0.00003558321,0.00007537538,0.009808323,0.0001647991,0.0167629,0.0243703,0.0003576631],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9713967,0.005323152,0.0000307345,0.001404501,0.0001137888,0.00003722773,0.000166919,0.00002297878,0.02150395],"genre_scores_gemma":[0.9971524,0.000158564,0.0003835726,0.0007010328,0.0001349627,0.000001367462,0.000161068,0.000002101441,0.001304966],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0464185,"threshold_uncertainty_score":0.9542405,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2811017101","doi":"10.1007/s00710-018-0601-z","title":"The origin of Type II diamonds as inferred from Cullinan mineral inclusions","year":2018,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geochemistry; Paragenesis; Mafic; Coesite; Enstatite; Pyrope; Craton; Omphacite; Kyanite; Eclogite; Mantle (geology); Metamorphism; Metamorphic rock; Meteorite; Chondrite; Subduction; Paleontology","authors":[{"name":"N. M. Korolev","is_ca":true},{"name":"Maya Kopylova","is_ca":true},{"name":"John Gurney","is_ca":false},{"name":"Andy Moore","is_ca":false},{"name":"Jim Davidson","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01248737523526457,"gpt":0.2292977598245797,"spread":0.2168103845893151,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001326899,0.0001021241,0.0002120592,0.0000371623,0.0003837715,0.000007085223,0.0001782973,0.0001234417,0.008086774],"category_scores_gemma":[0.00009584099,0.00005578073,0.0000476828,0.0001785751,0.0007261619,0.00002998511,0.00006879234,0.0001285946,0.0001293131],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":7.739499e-7,"about_ca_system_score_gemma":0.0000185367,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.01218489,"about_ca_topic_score_gemma":0.03049731,"domain_scores_codex":[0.9991884,0.00009899495,0.0001932535,0.0002021612,0.00007277179,0.0002443681],"domain_scores_gemma":[0.9992894,0.0003553311,0.00005917737,0.0001442792,0.00006531643,0.00008647264],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002323672,0.00002537742,0.9881902,0.000001314287,0.00006900886,0.00000821382,0.0001699154,0.00003001029,0.003224735,0.001584591,0.001736728,0.004727483],"study_design_scores_gemma":[0.0003408112,0.001272874,0.8699186,0.00000181558,0.0000656235,0.00001602024,0.00003130429,0.003165911,0.0001661826,0.07357848,0.05131475,0.0001276705],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9844885,0.0008788021,0.000006845503,0.003579856,0.0002262552,0.0000291122,0.0000295912,0.00001089577,0.01075018],"genre_scores_gemma":[0.9973279,0.0001235452,0.0001403289,0.0007713611,0.0002383326,6.707347e-7,0.0001458841,0.000001087019,0.001250895],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1182717,"threshold_uncertainty_score":0.9943931,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1964114398","doi":"10.1007/s00710-002-0194-3","title":"Hydromagmatic amphibole in komatiitic, tholeiitic and ferropicritic units, Abitibi greenstone belt, Ontario and Qu�bec: evidence for Archaean wet basic and ultrabasic melts","year":2003,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":20,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"National Science Foundation","keywords":"Amphibole; Geology; Geochemistry; Ultramafic rock; Greenstone belt; Petrography; Olivine; Peridotite; Mafic; Ilmenite; Chromite; Gabbro; Archean; Eclogite; Igneous rock; Mineralogy; Basalt; Subduction","authors":[{"name":"W. E. E. Stone","is_ca":false},{"name":"Étienne Deloule","is_ca":false},{"name":"M.S. Stone","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.03780908195411117,"gpt":0.2516738326352662,"spread":0.213864750681155,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005143413,0.000249306,0.0004347829,0.0001491361,0.0002010498,0.00004881715,0.0001628185,0.0001740043,0.0000185448],"category_scores_gemma":[0.0003455073,0.0002401638,0.00001945478,0.0001732809,0.0005413382,0.0002399159,0.00009736833,0.0002585066,9.978082e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002256349,"about_ca_system_score_gemma":0.00008870107,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004959929,"about_ca_topic_score_gemma":0.08411387,"domain_scores_codex":[0.9982339,0.0002493955,0.0003201666,0.0006172662,0.00007652288,0.0005028108],"domain_scores_gemma":[0.9984931,0.0009361868,0.00007194388,0.0002713837,0.00007504448,0.0001523722],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001505502,0.0002129554,0.749416,0.001513378,0.0001270698,0.0004978586,0.01509959,0.00005612341,0.01785372,0.1997521,0.0004642291,0.01485648],"study_design_scores_gemma":[0.003342135,0.001470563,0.8733658,0.0002468047,0.00009297321,0.004197361,0.0003148864,0.005502571,0.000214906,0.1088628,0.001694163,0.0006950875],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9898458,0.002541486,0.002077973,0.004274399,0.0001055594,0.0002391647,0.00000422714,0.00003053741,0.0008809142],"genre_scores_gemma":[0.994837,0.0002131902,0.003305071,0.0008073633,0.00002343731,0.0000473849,0.00001111337,0.000005070247,0.0007503664],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1239498,"threshold_uncertainty_score":0.9793594,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2010662695","doi":"10.1007/s00710-013-0305-3","title":"Mineral inclusions in fibrous diamonds: constraints on cratonic mantle refertilization and diamond formation","year":2013,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Kimberlite; Craton; Mantle (geology); Geochemistry; Olivine; Geology; Diamond; Metasomatism; Fayalite; Chemistry; Paleontology","authors":[{"name":"Christine E. Miller","is_ca":true},{"name":"Maya Kopylova","is_ca":true},{"name":"Evan M. Smith","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.00897688335883542,"gpt":0.19171097954038,"spread":0.1827340961815446,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00008794613,0.0001048835,0.0001810027,0.0001112882,0.00009261914,0.00001598705,0.00005268277,0.0001268945,0.004907943],"category_scores_gemma":[0.00003825369,0.00007408338,0.00002057025,0.0001179362,0.0002240709,0.000128286,0.00002160395,0.000132676,0.00009676683],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002011601,"about_ca_system_score_gemma":0.000005035185,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001965751,"about_ca_topic_score_gemma":0.01163598,"domain_scores_codex":[0.9992254,0.00009535399,0.0001860201,0.0002081207,0.00005343687,0.0002317],"domain_scores_gemma":[0.9996176,0.0001703862,0.00003902828,0.00006793491,0.00001876985,0.00008627031],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00005594724,0.00003256035,0.9741348,0.00001207546,0.00001150365,0.00001428563,0.000157548,0.0003541749,0.002230946,0.0005297622,0.000395038,0.02207133],"study_design_scores_gemma":[0.0003681134,0.0002428519,0.9730545,0.000004094316,0.00001048198,0.00003288956,0.00004028283,0.01518178,0.00005036236,0.01068369,0.0002326993,0.00009823907],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9915942,0.0003653145,0.00002420905,0.002267869,0.00003577155,0.00008072596,0.00001445775,0.0000124266,0.005605005],"genre_scores_gemma":[0.998278,0.0001208878,0.000107348,0.001096119,0.00002576747,0.000004689044,0.0002058481,0.000001116573,0.0001602518],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02197309,"threshold_uncertainty_score":0.9960017,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1984198666","doi":"10.1007/s00710-009-0101-2","title":"Sulphur isotopes in carbonatites and associated silicate rocks from the Superior Province, Canada","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Carleton University; University of Ottawa; Kirkland and District Hospital","funders":"","keywords":"Carbonatite; Geology; Geochemistry; Isotope; Silicate; Pyrite; Pyrrhotite; Mantle (geology); Mineralogy; Chemistry","authors":[{"name":"Sean Farrell","is_ca":true},{"name":"Keith Bell","is_ca":true},{"name":"Ian D. Clark","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.004676618938436677,"gpt":0.1604955881329582,"spread":0.1558189691945215,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001012942,0.0001017761,0.0002161161,0.00002266741,0.00006946216,0.00001270156,0.0001051329,0.00009148215,0.0006037462],"category_scores_gemma":[0.00007315901,0.00005908203,0.00001813795,0.0001016108,0.0001173774,0.0000298104,0.00001172571,0.0001677087,0.000003024116],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000002586173,"about_ca_system_score_gemma":0.00003921429,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8384709,"about_ca_topic_score_gemma":0.9912442,"domain_scores_codex":[0.9992124,0.0001118717,0.0001448802,0.0002286412,0.00006031456,0.0002418629],"domain_scores_gemma":[0.9994254,0.0004011819,0.00003110169,0.00007013312,0.00001359129,0.00005860077],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002664503,0.000008564585,0.9960994,6.128002e-7,0.00001510591,0.00002430638,0.00003343256,0.00007830963,0.000279017,0.00003664998,0.0003701743,0.003027814],"study_design_scores_gemma":[0.0002265537,0.0001023058,0.9908341,0.000001359245,0.00001810635,0.000006304101,0.00002168556,0.002103132,0.00001842779,0.00480937,0.001777215,0.00008146239],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9820958,0.002138569,5.997259e-7,0.01409635,0.00002847466,0.00004698883,0.00006839269,0.000007630399,0.001517175],"genre_scores_gemma":[0.994854,0.00008895531,0.0000149193,0.004582163,0.00003790476,8.84164e-7,0.0001452924,6.246765e-7,0.000275224],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1527732,"threshold_uncertainty_score":0.6610598,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2017158343","doi":"10.1007/s00710-009-0089-7","title":"Auriacusite, Fe3+Cu2+AsO4O, the first M 3+ member of the olivenite group, from the Black Pine mine, Montana, USA","year":2009,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Crystal Structures and Properties","field":"Materials Science","cited_by":18,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Canadian Museum of Nature; University of British Columbia","funders":"","keywords":"Pleochroism; Orthorhombic crystal system; Mohs scale of mineral hardness; Crystallography; Tetrahedrite; Quartz; Chemistry; Malachite; Mineralogy; Triclinic crystal system; Pyrite; Materials science; Crystal structure; Metallurgy; Sphalerite; Copper","authors":[{"name":"Stuart J. Mills","is_ca":true},{"name":"Anthony R. Kampf","is_ca":false},{"name":"Glenn Poirier","is_ca":true},{"name":"Mati Raudsepp","is_ca":true},{"name":"I. M. Steele","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01047248388415222,"gpt":0.2068594623029048,"spread":0.1963869784187525,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002489777,0.0001818671,0.0002766734,0.00001873872,0.0003632591,0.00003679584,0.0004993217,0.0001365214,0.00123984],"category_scores_gemma":[0.00003564375,0.00007483047,0.00008750489,0.0001068864,0.0007619853,0.00006081946,0.0001507203,0.0001980217,0.00001866436],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009247903,"about_ca_system_score_gemma":0.00001427613,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004069048,"about_ca_topic_score_gemma":0.01899008,"domain_scores_codex":[0.9988129,0.0002299773,0.00026772,0.0002626616,0.0001277396,0.0002990286],"domain_scores_gemma":[0.9990581,0.0002890969,0.0001353271,0.0004424462,0.00003897069,0.00003605436],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.001628551,0.0001545411,0.1154297,0.00003961245,0.0001716981,0.00003520248,0.007032817,0.001122411,0.7959681,0.01730585,0.05880116,0.002310386],"study_design_scores_gemma":[0.000757548,0.0003615675,0.8702261,0.00001335389,0.0001058978,0.00008574342,0.0001032423,0.0002631771,0.001900783,0.005007189,0.1209941,0.0001812155],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.979457,0.001697725,0.00001534144,0.01625595,0.0004149998,0.0001585411,0.00007348182,0.00001139425,0.001915597],"genre_scores_gemma":[0.9935693,0.000101258,0.0000522535,0.004979436,0.0003552305,0.000007136206,0.000009670565,0.000007465777,0.0009182717],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.7940673,"threshold_uncertainty_score":0.9996732,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W1964103019","doi":"10.1007/s007100070025","title":"Compositional variations in ferrotapiolite + tantalite pairs from the beryl-columbite pegmatite at Moravanynad Váhom, Slovakia","year":2000,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Slovenská Akadémia Vied","keywords":"Pegmatite; Columbite; Geology; Geochemistry; Mineralogy; Crystallography; Chemistry; Phase (matter)","authors":[{"name":"M. NOVAK","is_ca":true},{"name":"Pavel Uher","is_ca":true},{"name":"P. Černý","is_ca":true},{"name":"Pavol Siman","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.006924928234632163,"gpt":0.1785234077317512,"spread":0.1715984794971191,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001749777,0.0001423993,0.0002612826,0.00004140284,0.0002411461,0.00002320351,0.000161308,0.0001383792,0.05895442],"category_scores_gemma":[0.00001574635,0.00009665729,0.00007064564,0.0002024657,0.0002867757,0.00006880036,0.00002182429,0.0002137048,0.0004651975],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004789191,"about_ca_system_score_gemma":0.00001036118,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.02273965,"about_ca_topic_score_gemma":0.1184869,"domain_scores_codex":[0.9987178,0.000251255,0.0002710616,0.0003264783,0.0001052476,0.0003280938],"domain_scores_gemma":[0.9991327,0.0005585801,0.00004748163,0.0001474986,0.00001905506,0.00009471742],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001096985,0.00002789776,0.9951409,0.000001879944,0.00004800109,0.00002811275,0.0001561324,0.0009200569,0.0004752988,0.0005376114,0.0005000266,0.002054373],"study_design_scores_gemma":[0.0003841684,0.00007107326,0.9653634,0.00000309279,0.00003908899,0.00004425984,0.00001100136,0.008047733,0.000004833863,0.01987677,0.006032559,0.0001220103],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9823454,0.001022214,0.00001178723,0.006339135,0.00006038485,0.00007352536,0.0003529856,0.00001854375,0.009776046],"genre_scores_gemma":[0.992896,0.0001327383,0.000257219,0.003881662,0.0001195547,0.000004959669,0.001434403,0.000001770387,0.001271653],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.09574724,"threshold_uncertainty_score":0.983768,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2011989692","doi":"10.1007/s00710-007-0193-5","title":"Mobility of palladium chloride complexes in mafic rocks: insights from a flow-through experiment at 25 °C using air-saturated, acidic, and Cl-rich solutions","year":2007,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":17,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Université du Québec à Montréal","funders":"National Science Foundation","keywords":"Chloride; Redox; Basalt; Quartz; Chemistry; Mafic; Geology; Elution; Oxidizing agent; Inorganic chemistry; Geochemistry; Chromatography; Organic chemistry","authors":[{"name":"Scott A. Wood","is_ca":false},{"name":"Charles Normand","is_ca":true}],"retraction":null,"screen_n_in":null,"score":{"opus":0.0261611298146814,"gpt":0.2508035963666114,"spread":0.22464246655193,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002306106,0.0001778339,0.0003555895,0.00008388046,0.0001762448,0.000009218628,0.0002086853,0.0002275322,0.0000333908],"category_scores_gemma":[0.0000350963,0.0001630001,0.00003167259,0.000191188,0.0003782678,0.0001263,0.0003773586,0.0001897741,0.000001777279],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00004262623,"about_ca_system_score_gemma":0.0000302911,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0011181,"about_ca_topic_score_gemma":0.001903178,"domain_scores_codex":[0.998542,0.0001126091,0.0003725406,0.0004977448,0.00007782567,0.0003972931],"domain_scores_gemma":[0.9992083,0.000247672,0.0001097594,0.000303689,0.00005931515,0.0000712839],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","study_design_scores_codex":[0.0005420551,0.0004662113,0.1016985,0.0000965517,0.0001450869,0.0002729742,0.01035596,0.006452968,0.8634531,0.01573309,0.0002999291,0.0004836424],"study_design_scores_gemma":[0.007623713,0.001113435,0.3933062,0.0001055252,0.000108775,0.001077234,0.001486997,0.1831847,0.3389134,0.05556031,0.01596772,0.001552023],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9707063,0.002017342,0.0252884,0.0009047306,0.0001969204,0.0000952423,0.000007345854,0.00002671774,0.0007569808],"genre_scores_gemma":[0.9943993,0.00004507119,0.005089935,0.0002718127,0.0000588051,0.000007785728,0.00002491898,0.000002301,0.0001000518],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5245396,"threshold_uncertainty_score":0.664695,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2801585377","doi":"10.1007/s00710-018-0568-9","title":"Provenance history of detrital diamond deposits, West Coast of Namaqualand, South Africa","year":2018,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"ARC Resources (Canada)","funders":"","keywords":"Kimberlite; Geology; Provenance; Craton; Geochemistry; Cretaceous; Placer deposit; Diamond; Paleontology; Mantle (geology); Placer mining","authors":[{"name":"David Phillips","is_ca":false},{"name":"Jeffrey W. Harris","is_ca":false},{"name":"Michiel C. J. de Wit","is_ca":true},{"name":"Erin Matchan","is_ca":false}],"retraction":null,"screen_n_in":null,"score":{"opus":0.01097416354225412,"gpt":0.1722804178430675,"spread":0.1613062543008134,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001092488,0.0001027825,0.0003170068,0.00006819785,0.0000299924,0.000001481712,0.0001136134,0.0001149674,0.002073765],"category_scores_gemma":[0.00004696488,0.00006794639,0.00005884519,0.0001056904,0.0007410182,0.00003196934,0.00001909742,0.00009336418,0.00003075723],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001855832,"about_ca_system_score_gemma":0.0000224018,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001325214,"about_ca_topic_score_gemma":0.01029941,"domain_scores_codex":[0.9992149,0.00006955686,0.0002271754,0.00020261,0.000071333,0.0002143599],"domain_scores_gemma":[0.9995038,0.0001473578,0.0001179709,0.0001018011,0.00005731928,0.00007176049],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001455536,0.00003201847,0.9926828,0.00001844671,0.00003734154,0.000007143635,0.0005646584,0.000009999785,0.004545297,0.0001594225,0.0004237526,0.00137361],"study_design_scores_gemma":[0.0005177186,0.001398317,0.9887506,0.000005348123,0.0000807753,0.00003014866,0.00006860821,0.0004975414,0.000869462,0.001953163,0.005683073,0.0001451978],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9885401,0.003301733,0.00003828646,0.000139511,0.0001252724,0.00003346906,0.00004534561,0.000006974292,0.007769297],"genre_scores_gemma":[0.9986507,0.000026134,0.0003178141,0.0001160314,0.00007682012,7.371014e-7,0.00004004472,0.000001131892,0.0007705468],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.01011063,"threshold_uncertainty_score":0.9988385,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}