{"meta":{"page":1,"per_page":50,"max_per_page":100,"total":1924,"total_is_capped":false,"direct_labels_cover":0,"predictions_cover":1924,"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"},"query_hash":"b1d7f479404f","filters":{"venue":"Abstracts with programs - Geological Society of America"}},"results":[{"id":"W2772143789","doi":"10.1130/abs/2017am-305180","title":"EXOGEOCONSERVATION: PROTECTING GEOLOGICAL HERITAGE ON CELESTIAL BODIES","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":31,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"Memorial University of Newfoundland","funders":"Department of Fisheries and Land Resources; Mitacs; European Commission","keywords":"Context (archaeology); Stewardship (theology); Astrobiology; Natural (archaeology); Planet; Cultural heritage; Earth science; Geography; Environmental resource management; Geology; Archaeology; Environmental science; Political science; Politics; Astronomy; Law","retraction":null,"screen_n_in":null,"score":{"opus":0.04065330232772049,"gpt":0.2615413718338017,"spread":0.2208880695060812,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002539337,0.0002066583,0.000297273,0.000007357861,0.0008983706,0.0001360131,0.0003658317,0.00009013244,0.0001257789],"category_scores_gemma":[0.00003787258,0.0001360739,0.0001360723,0.00006391738,0.00105908,0.0003838459,0.00008070303,0.0003859425,0.00007428575],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000881915,"about_ca_system_score_gemma":0.00004165444,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008716043,"about_ca_topic_score_gemma":0.00001247483,"domain_scores_codex":[0.9986072,0.00004071477,0.0002808772,0.0003763548,0.0002894606,0.0004054426],"domain_scores_gemma":[0.9988327,0.0001034302,0.000535171,0.0003363334,0.00009031707,0.0001020455],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001561712,0.0007359186,0.8688486,0.00002793425,0.0001190178,0.00001216344,0.000977047,0.001591628,0.0003053102,0.0002948908,0.0005993561,0.126332],"study_design_scores_gemma":[0.0009357197,0.003593884,0.9707485,0.0001047599,0.0000417383,0.000005947123,0.004026433,0.002504646,0.001142409,0.002857092,0.01345518,0.0005836901],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9917185,0.00001123526,0.001071049,0.002584604,0.00004363196,0.0004800089,0.000007185209,0.00007195047,0.00401186],"genre_scores_gemma":[0.9828392,0.000004399976,0.0163757,0.0002694204,0.0001846599,0.00008367212,0.0001300254,0.000006153282,0.0001068192],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1257483,"threshold_uncertainty_score":0.6909631,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2537115509","doi":"10.1130/abs/2016am-282405","title":"EXCEPTIONALLY PRESERVED FOSSIL ASSEMBLAGES THROUGH GEOLOGIC TIME AND SPACE","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; W. M. Keck Foundation; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Space (punctuation); Paleontology; Geologic time scale; Deep time; Earth science; Astrobiology; Computer science; Sedimentary rock","retraction":null,"screen_n_in":null,"score":{"opus":0.02583497649085924,"gpt":0.2330030211007102,"spread":0.2071680446098509,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003291168,0.0002709948,0.0004808271,0.00001605918,0.0001999228,0.0000484213,0.0002787708,0.0002286814,0.002103619],"category_scores_gemma":[0.0001241869,0.0001273386,0.0002146627,0.0002724657,0.001340857,0.0002624661,0.00005484551,0.0002005235,0.0001992263],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004038875,"about_ca_system_score_gemma":0.00003132396,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002272637,"about_ca_topic_score_gemma":0.00009534316,"domain_scores_codex":[0.9979445,0.0001054033,0.0003742207,0.0005798118,0.0004203572,0.0005757324],"domain_scores_gemma":[0.9986529,0.0004518821,0.0003165521,0.0002360407,0.0001511036,0.0001915185],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001562671,0.0003173634,0.7235032,0.0000395973,0.0002840398,0.00001949715,0.0002098796,0.009627117,0.0004369135,0.0000193401,0.001260964,0.2641258],"study_design_scores_gemma":[0.000597613,0.002220023,0.9764395,0.0000647526,0.00007966193,0.00001936716,0.0002226676,0.006547548,0.00006775371,0.003367926,0.009974968,0.0003982277],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9840397,0.000724976,0.003063672,0.0089579,0.0000182043,0.0002382819,0.00001826283,0.0001614757,0.002777486],"genre_scores_gemma":[0.956962,0.0005539214,0.04101131,0.0004189695,0.00006317611,0.000006165461,0.00005322901,0.000003987099,0.0009272041],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2637276,"threshold_uncertainty_score":0.9988086,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2536183229","doi":"10.1130/abs/2016am-278498","title":"THE LONG-TERM ENVIRONMENTAL IMPACTS OF THE MOUNT POLLEY MINE TAILINGS SPILL, BRITISH COLUMBIA, CANADA","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":10,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Tailings; Mount; Environmental science; Mining engineering; Environmental impact assessment; Geology; Archaeology; Engineering; Geography; Ecology; Materials science; Metallurgy","retraction":null,"screen_n_in":null,"score":{"opus":0.006782749042026511,"gpt":0.1901390745451153,"spread":0.1833563255030888,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002777151,0.0001753994,0.0003033777,0.000002607206,0.0003776429,0.0001060429,0.001215936,0.0001181676,0.00007740035],"category_scores_gemma":[0.0001241517,0.000101031,0.000202169,0.0002242224,0.00185431,0.0001021252,0.0004669087,0.0002186847,0.000001774874],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000109451,"about_ca_system_score_gemma":0.0002239946,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.3986111,"about_ca_topic_score_gemma":0.127659,"domain_scores_codex":[0.9979149,0.00005497823,0.0004426434,0.0004154389,0.000562229,0.0006098031],"domain_scores_gemma":[0.9982364,0.0003393064,0.0006005188,0.0005846829,0.00008643708,0.0001527107],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0000219648,0.000423569,0.8080738,0.00006866329,0.0001908783,0.00003485573,0.0002244963,0.00006239661,0.003426927,0.00001988271,0.004479581,0.182973],"study_design_scores_gemma":[0.0005237751,0.0005638371,0.9774334,0.000133964,0.00001845709,0.00009481897,0.0002532874,0.00006887777,0.001312335,0.0002512136,0.01909816,0.0002478033],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9893578,0.0002149908,0.0003781382,0.009221331,0.00006422464,0.0003841297,0.000009731123,0.00003803086,0.0003315742],"genre_scores_gemma":[0.9949535,0.0001372791,0.00343235,0.0005094893,0.00002951726,0.00002634891,0.000004161858,0.000004081125,0.0009033325],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2709521,"threshold_uncertainty_score":0.8882589,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2774609511","doi":"10.1130/abs/2017am-304142","title":"UNRAVELING THE BOUNDARY BETWEEN THE YUKON-TANANA TERRANE AND PARAUTOCHTHONOUS NORTH AMERICA IN EASTERN ALASKA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Earthquake and Disaster Impact Studies","field":"Social Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Terrane; Boundary (topology); Geology; Archaeology; Geography; Mathematics; Paleontology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.04879962054880062,"gpt":0.3081718990605998,"spread":0.2593722785117992,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0006224933,0.0002413002,0.0004566127,0.00001239899,0.002485481,0.0003308817,0.0007181352,0.0001166388,0.0000212381],"category_scores_gemma":[0.000203845,0.0001206606,0.0001539557,0.0002136385,0.008167717,0.0002405689,0.0002414298,0.0004553901,0.00001206178],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002503089,"about_ca_system_score_gemma":0.0001191599,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01630716,"about_ca_topic_score_gemma":0.002538819,"domain_scores_codex":[0.9978506,0.0001675801,0.0003863031,0.0003549105,0.0005242031,0.0007164196],"domain_scores_gemma":[0.9982014,0.0004937476,0.0006058213,0.0004519753,0.00009073289,0.0001563097],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002659734,0.0000975411,0.6588882,0.00001294243,0.0001002055,0.000006008348,0.03384006,0.00003803679,5.952778e-7,0.000005832814,0.0001191888,0.3068648],"study_design_scores_gemma":[0.0003145907,0.00048064,0.9351986,0.00004484207,0.00005208257,0.000001886635,0.03340692,0.00003815665,0.000001398613,0.0002755256,0.02999274,0.0001926268],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9756499,0.0005134041,0.0001299504,0.0175053,0.00003750506,0.0006719361,0.000005788488,0.00005141389,0.005434811],"genre_scores_gemma":[0.996657,0.0006237081,0.001325164,0.001029099,0.000159129,0.00004659806,0.000006995214,0.00001072706,0.0001416157],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3066722,"threshold_uncertainty_score":0.9988132,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2730050620","doi":"10.1130/abs/2016rm-276278","title":"A PRECISE U-PB ZIRCON AGE FROM VOLCANIC ASH IN THE PENNSYLVANIAN COPACABANA FORMATION, BOLIVIA","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological and Tectonic Studies in Latin America","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Zircon; Pennsylvanian; Geology; Volcano; Volcanic ash; Geochemistry; Archaeology; Paleontology; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.01965440511150448,"gpt":0.2217135560156943,"spread":0.2020591509041898,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000401988,0.0002825054,0.0004765922,0.00001858601,0.000205801,0.00004099647,0.0006285171,0.0001555235,0.003190874],"category_scores_gemma":[0.000152743,0.0001186639,0.0001962607,0.0004762249,0.001787681,0.0002098781,0.00005954455,0.0003341682,0.0001546804],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001213455,"about_ca_system_score_gemma":0.00003263202,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.005171522,"about_ca_topic_score_gemma":0.0009266958,"domain_scores_codex":[0.9976667,0.0001690737,0.0005309823,0.0004507102,0.0005080024,0.0006745126],"domain_scores_gemma":[0.9979201,0.001129492,0.0004118516,0.0003375177,0.00007234298,0.0001286871],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0001380148,0.0003178701,0.1777565,0.00002243078,0.0001006142,0.00004817828,0.002135179,0.0001713542,0.0001446546,0.0000140306,0.002732693,0.8164185],"study_design_scores_gemma":[0.0007713306,0.001770877,0.9651885,0.00007635341,0.00003463367,0.00001774929,0.002296213,0.0001641471,0.00006986129,0.001782453,0.02751953,0.0003083741],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9569218,0.0007406244,0.002614504,0.006104057,0.0001025266,0.00109428,0.00006210501,0.000158874,0.03220129],"genre_scores_gemma":[0.9779657,0.0003993062,0.02024599,0.001160203,0.00006680627,0.00002483934,0.00006589458,0.000004175222,0.00006712246],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8161101,"threshold_uncertainty_score":0.9977204,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4248581767","doi":"10.1130/abs/2020am-358950","title":"THE LATE GREAT UNCONFORMITY OF THE CENTRAL CANADIAN SHIELD","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Unconformity; Geology; Shield; Paleontology; Sedimentary rock","retraction":null,"screen_n_in":null,"score":{"opus":0.02446553237733682,"gpt":0.227383015201109,"spread":0.2029174828237722,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002373452,0.000130989,0.0002383311,0.000005697973,0.0004169396,0.00001814084,0.0005502505,0.0001730165,0.0005144658],"category_scores_gemma":[0.00009082613,0.00005777408,0.0001635062,0.0003290516,0.002706871,0.00005711291,0.00003133346,0.0004943176,0.00003405584],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001704458,"about_ca_system_score_gemma":0.0002162806,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0779478,"about_ca_topic_score_gemma":0.07965397,"domain_scores_codex":[0.9985413,0.0001025182,0.0002590441,0.0001790072,0.0002500515,0.0006680634],"domain_scores_gemma":[0.9989058,0.0003471456,0.0001867133,0.0001891556,0.00006802061,0.000303187],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004730407,0.00001281882,0.9800624,0.00001700928,0.00006190781,0.000004342255,0.0005517003,0.0006353691,8.189222e-7,0.00001218274,0.000309614,0.01828457],"study_design_scores_gemma":[0.0001632466,0.0005755047,0.9858527,0.000007977011,0.0000172433,0.00001068609,0.0008587871,0.0007418161,0.00003469275,0.0001311179,0.01152173,0.00008447781],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9708844,0.0002238525,0.00000746399,0.02213611,0.00004875695,0.0003342252,0.00001388737,0.00001997112,0.006331335],"genre_scores_gemma":[0.9974038,0.0001197035,0.000540157,0.001785719,0.00002276097,0.000002470113,0.00002378696,0.000001735182,0.00009989364],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02651938,"threshold_uncertainty_score":0.9973578,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4255011188","doi":"10.1130/abs/2020am-352772","title":"A CHRONOSTRATIGRAPHIC FRAMEWORK FOR THE RISE OF THE EDIACARAN MACROBIOTA: NEW CONSTRAINTS FROM MISTAKEN POINT ECOLOGICAL RESERVE, NEWFOUNDLAND","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Point (geometry); Paleontology; Ecology; Geography; Biology; Mathematics","retraction":null,"screen_n_in":null,"score":{"opus":0.02186864476908068,"gpt":0.2447010645289671,"spread":0.2228324197598864,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003245281,0.0002751429,0.0005562252,0.000005236103,0.0002621822,0.00003558239,0.001012511,0.0003191244,0.002204484],"category_scores_gemma":[0.0004010314,0.0001361451,0.0005548176,0.0005603327,0.005972044,0.00008558118,0.0002989178,0.0005992936,0.00002210036],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00005246314,"about_ca_system_score_gemma":0.00007493184,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.003212213,"about_ca_topic_score_gemma":0.0006056242,"domain_scores_codex":[0.9977585,0.0001383806,0.0006036442,0.0005634071,0.0003977504,0.0005382975],"domain_scores_gemma":[0.997337,0.00125933,0.0006902425,0.0004656364,0.00004212798,0.0002056557],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004552779,0.001066726,0.9228344,0.0000448359,0.000901532,0.000008362285,0.002865967,0.006750243,0.001520573,0.0002054539,0.01230022,0.05104644],"study_design_scores_gemma":[0.00115477,0.002360472,0.9631131,0.00003604477,0.0003127447,0.000005505015,0.00185102,0.001638644,0.000442414,0.00448546,0.02426042,0.0003394115],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9572252,0.0002254474,0.008831756,0.03084813,0.00007664559,0.001865993,0.00003944272,0.00005845863,0.0008289422],"genre_scores_gemma":[0.9233686,0.00008045072,0.073814,0.002499506,0.0001078996,0.00007330598,0.00001365372,0.00001225235,0.00003031142],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06498224,"threshold_uncertainty_score":0.9987077,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3097339529","doi":"10.1130/abs/2020am-353274","title":"THE 2020 CANADA DATAPACK FOR TIMESCALE CREATOR: A NEW TOOL FOR MESOZOIC–CENOZOIC STRATIGRAPHY OF THE CANADIAN NORTH","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Cenozoic; Stratigraphy; Mesozoic; Paleontology; Geology; Structural basin; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.02366383141756269,"gpt":0.2022440677024486,"spread":0.1785802362848859,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001377558,0.0001784415,0.0002988199,0.000003026057,0.0006695937,0.0000442497,0.0004437187,0.00008403792,0.0000920785],"category_scores_gemma":[0.0001358991,0.00008233322,0.0002081514,0.0003364837,0.0006198086,0.00007110569,0.00002208632,0.0001678309,0.000002068186],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001027091,"about_ca_system_score_gemma":0.0006215866,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8835851,"about_ca_topic_score_gemma":0.9803687,"domain_scores_codex":[0.9985092,0.00003073271,0.0003528874,0.0002902121,0.0003045216,0.0005125004],"domain_scores_gemma":[0.998717,0.0003851606,0.000297977,0.0001790473,0.0001333733,0.000287463],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003514732,0.0000640276,0.6489179,0.000102274,0.0003669712,0.000001752161,0.0006894296,0.007947762,0.000003893198,0.00006285391,0.1472595,0.1942321],"study_design_scores_gemma":[0.000419198,0.001824181,0.6619537,0.000009954255,0.00006184267,0.000001142299,0.001163071,0.002639029,0.00002211416,0.0003594249,0.3313541,0.0001922321],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8722969,0.001758215,0.001173261,0.1153151,0.0002471393,0.005932294,0.001176827,0.00007881696,0.002021492],"genre_scores_gemma":[0.9889009,0.00009685517,0.008161347,0.002396489,0.0001071565,0.00002517138,0.0002525731,0.00000346174,0.00005601746],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1940399,"threshold_uncertainty_score":0.5150041,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2965074546","doi":"10.1130/abs/2019am-332955","title":"MERCURY AS A PROXY FOR VOLCANIC EMISSIONS IN THE GEOLOGIC RECORD","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":5,"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":"Mercury (programming language); Volcano; Proxy (statistics); Geology; Earth science; Environmental science; Geochemistry; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.02560673369876045,"gpt":0.2419773570730448,"spread":0.2163706233742843,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004913335,0.0002035789,0.0003672403,0.00001269413,0.0001971513,0.00003303909,0.0003615121,0.000167288,0.0009016175],"category_scores_gemma":[0.0001027155,0.00009535038,0.0001906772,0.0004048272,0.0004733579,0.0001198395,0.0000283002,0.0003105446,0.0001404088],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000005604601,"about_ca_system_score_gemma":0.0000386994,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004269872,"about_ca_topic_score_gemma":0.0004092371,"domain_scores_codex":[0.998286,0.00008188793,0.0003751151,0.0004022745,0.0002975736,0.0005571573],"domain_scores_gemma":[0.9988456,0.0005254366,0.0002664151,0.0001917828,0.0000832431,0.00008748812],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002283857,0.0003006792,0.792681,0.00005446128,0.00005392495,0.000005116767,0.0009300563,0.003148341,0.00001258647,0.00003996737,0.001080039,0.2014655],"study_design_scores_gemma":[0.0006760437,0.007336445,0.8760217,0.00003985849,0.00003049285,0.00001349297,0.007824489,0.004861075,0.000008597499,0.004040245,0.0988484,0.0002991677],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9856676,0.0003100464,0.0001959443,0.007919518,0.00006613191,0.001683428,0.000007005169,0.00005690132,0.004093377],"genre_scores_gemma":[0.9866071,0.0002809736,0.01082258,0.001899568,0.00004486781,0.00006925117,0.0001181697,0.000002995346,0.0001545022],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2011663,"threshold_uncertainty_score":0.9872079,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4389362865","doi":"10.1130/abs/2023am-392360","title":"IN SITU EVIDENCE OF AN ACTIVE CARBON CYCLE ON ANCIENT MARS","year":2023,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":4,"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":"Mars Exploration Program; Astrobiology; In situ; Carbon fibers; Environmental science; Geology; Computer science; Meteorology; Geography; Biology","retraction":null,"screen_n_in":null,"score":{"opus":0.02142722295659772,"gpt":0.2654420460692435,"spread":0.2440148231126458,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002205196,0.0001434917,0.0002666993,0.00002191579,0.00004472382,0.000009645759,0.0002332561,0.0000493915,0.00006242454],"category_scores_gemma":[0.000007902783,0.0001013384,0.0000879655,0.0005758844,0.0005108432,0.0001713551,0.00004620217,0.0002310548,0.0000128189],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001186134,"about_ca_system_score_gemma":0.00004896282,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002208439,"about_ca_topic_score_gemma":0.00001290659,"domain_scores_codex":[0.9986901,0.0000441591,0.000242095,0.0003243703,0.0003155872,0.0003837052],"domain_scores_gemma":[0.9992387,0.0001791787,0.0002390099,0.000192359,0.00004580628,0.0001049884],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.00061391,0.002247033,0.3992471,0.00008320726,0.00014104,0.0000323935,0.005020536,0.06896483,0.01265553,0.00008286043,0.0002735522,0.510638],"study_design_scores_gemma":[0.0003446129,0.00323739,0.9824768,0.0001277294,0.00001410132,8.716413e-7,0.003988679,0.004789902,0.004153473,0.0002474048,0.000400673,0.0002183541],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.997519,0.0000118061,0.00004168105,0.0002977406,0.00002362822,0.0002582555,0.000007275131,0.00002868153,0.001811984],"genre_scores_gemma":[0.9960548,0.000006923334,0.003699807,0.0001122087,0.00003106745,0.00001866572,0.00003810504,0.000004758085,0.00003364699],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5832297,"threshold_uncertainty_score":0.4132459,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2533599072","doi":"10.1130/abs/2016am-284684","title":"PETROGENESIS, AGE, AND CORRELATION OF THE KAZAN DIKE SWARM, NUNAVUT, CANADA: IMPLICATIONS FOR AN ABORTED RIFT ORIGIN FOR THE SNOWBIRD TECTONIC ZONE","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Petrogenesis; Geology; Dike; Tectonics; Rift; Rift zone; Swarm behaviour; Seismology; Paleontology; Artificial intelligence; Computer science","retraction":null,"screen_n_in":null,"score":{"opus":0.03017892722546315,"gpt":0.2395566137709718,"spread":0.2093776865455087,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002225335,0.0001438812,0.0002368311,0.000005175793,0.000461726,0.00001647397,0.0002240579,0.00008398453,0.00003048794],"category_scores_gemma":[0.00007735856,0.00005565136,0.0001084114,0.0002081565,0.0007891591,0.00008503674,0.00001957962,0.00008060357,5.320806e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009601771,"about_ca_system_score_gemma":0.00009508822,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.09997665,"about_ca_topic_score_gemma":0.1981367,"domain_scores_codex":[0.9989154,0.00003549869,0.0002990359,0.0002628758,0.0001688643,0.0003183446],"domain_scores_gemma":[0.9985006,0.0007178811,0.0003441176,0.0001933016,0.0001643339,0.00007977377],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001555082,0.0001270046,0.6358567,0.00003337123,0.0001504208,2.013148e-7,0.0001899947,0.00360763,0.0001011077,0.000144999,0.0009711555,0.3586618],"study_design_scores_gemma":[0.0004002662,0.001132969,0.9755594,0.00001301135,0.00006786267,0.000002299182,0.0005337393,0.001270586,0.0000422319,0.000569504,0.02029709,0.0001110754],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9746208,0.0005432095,0.01287988,0.01013495,0.00006948954,0.001481025,0.0001552097,0.0000346468,0.00008084365],"genre_scores_gemma":[0.9940516,0.0002761611,0.005100067,0.0003283676,0.00003995538,0.00008170649,0.00008178121,0.000003562132,0.00003683015],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3585508,"threshold_uncertainty_score":0.9060167,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2729515850","doi":"10.1130/abs/2017rm-293147","title":"REVISED INTERPRETATIONS OF DETRITAL ZIRCON POPULATIONS IN THE MESOPROTEROZOIC BELT AND PURCELL SUPERGROUPS OF MONTANA, IDAHO AND BRITISH COLUMBIA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Mineralogy and Gemology Studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Zircon; Geology; Geochemistry; Earth science; Archaeology; Geography","retraction":null,"screen_n_in":null,"score":{"opus":0.02572531024824005,"gpt":0.2442180455203947,"spread":0.2184927352721547,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002590342,0.00008084348,0.0003013405,0.000008959846,0.0002774671,0.00004849905,0.0001773965,0.00009271373,0.0000725226],"category_scores_gemma":[0.00009909632,0.00006466601,0.00005781228,0.00008318586,0.002273415,0.0001272094,0.00002885827,0.000163036,3.293897e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001048499,"about_ca_system_score_gemma":0.00001051709,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0925462,"about_ca_topic_score_gemma":0.07526392,"domain_scores_codex":[0.9991654,0.00006171196,0.0002939464,0.0001883188,0.0001185634,0.0001720428],"domain_scores_gemma":[0.9992851,0.0001702033,0.0002996453,0.0001529328,0.000054284,0.00003782177],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00001588636,0.00007446855,0.9593412,0.00004190102,0.00003981759,0.00000546658,0.0008246226,0.00003503668,0.0000153336,0.000003939429,0.000147827,0.03945446],"study_design_scores_gemma":[0.0003144889,0.0007780837,0.9963453,0.00005263022,0.0000336023,0.00002351065,0.001404499,0.0001774527,0.000003792789,0.0006769813,0.0001170563,0.00007255883],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9972064,0.0009259048,0.00005497841,0.0007230655,0.00001342481,0.0003567792,0.00003262677,0.000006127691,0.000680648],"genre_scores_gemma":[0.9906978,0.0002586572,0.008833358,0.0001185611,0.000007889083,0.000007301319,0.00004368775,0.00000141729,0.00003132358],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0393819,"threshold_uncertainty_score":0.9416101,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4246776713","doi":"10.1130/abs/2021am-365936","title":"A PERSISTENTLY LOW LEVEL OF ATMOSPHERIC OXYGEN IN EARTH’S MIDDLE AGE","year":2021,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"Army Research Office; Carnegie Institution of Washington; U.S. Department of Defense; National Science Foundation","keywords":"Earth (classical element); Atmospheric oxygen; Oxygen; Astrobiology; Environmental science; Geology; Physics; Astronomy","retraction":null,"screen_n_in":null,"score":{"opus":0.06073735734065164,"gpt":0.2591975559037928,"spread":0.1984601985631411,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001512451,0.0001658782,0.0003831228,0.000002768419,0.00006687934,0.00001185502,0.0001508753,0.00009561492,0.0009756213],"category_scores_gemma":[0.00004875274,0.0001209985,0.0001945102,0.0005326914,0.001221558,0.0001052561,0.0001519953,0.0001735189,0.00003911891],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003400251,"about_ca_system_score_gemma":0.00002813451,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001139814,"about_ca_topic_score_gemma":0.0001239653,"domain_scores_codex":[0.998535,0.00004742354,0.0003681702,0.0003059371,0.0003724663,0.0003710249],"domain_scores_gemma":[0.9993354,0.00007634168,0.0002512982,0.0001895044,0.00003766504,0.0001097809],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001578719,0.003781512,0.6974825,0.0002784964,0.0003953595,0.0001581169,0.01593523,0.006355814,0.01689253,0.00001755492,0.002369499,0.2561755],"study_design_scores_gemma":[0.0006470329,0.0006678995,0.9800777,0.00007716881,0.00002932561,0.00001254663,0.008378272,0.000184303,0.001946029,0.00009329381,0.007651492,0.000234875],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9932749,0.0001625837,0.0002125536,0.00051049,0.0000172581,0.0002287824,0.000005562485,0.00002283316,0.005564987],"genre_scores_gemma":[0.9410938,0.0001277658,0.05750545,0.000444211,0.000008952898,0.00002204018,0.00001702767,0.000007585023,0.000773161],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2825952,"threshold_uncertainty_score":0.9999376,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3096691064","doi":"10.1130/abs/2020am-358317","title":"DISTINGUISHING BETWEEN TERRESTRIAL AND EXTRATERRESTRIAL ORGANIC COMPOUNDS IN THE CM2 AGUAS ZARCAS CARBONACEOUS CHONDRITE: IMPLICATIONS FOR INTRINSIC ORGANIC MATTER","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological and Geophysical Studies Worldwide","field":"Earth and Planetary Sciences","cited_by":4,"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":"Astrobiology; Chondrite; Carbonaceous chondrite; Organic matter; Extraterrestrial life; Meteorite; Environmental chemistry; Geology; Chemistry; Physics; Organic chemistry","retraction":null,"screen_n_in":null,"score":{"opus":0.03330744206725805,"gpt":0.2398961755463674,"spread":0.2065887334791094,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002129816,0.0002639958,0.0005202052,0.00001037505,0.0002996676,0.0001042628,0.0004185772,0.0001317291,0.00012795],"category_scores_gemma":[0.0002034144,0.0001455871,0.0001458166,0.0005385506,0.0008936778,0.00008672079,0.0000689755,0.0004608319,0.00002245796],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006145758,"about_ca_system_score_gemma":0.00003403667,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002062994,"about_ca_topic_score_gemma":0.0003470206,"domain_scores_codex":[0.998121,0.0001026945,0.0004838625,0.0005036671,0.0002270985,0.000561661],"domain_scores_gemma":[0.9980898,0.00125817,0.0002744715,0.0001587272,0.00003627931,0.0001825662],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001739848,0.0001246074,0.9231999,0.0000369662,0.00007403113,0.000005834389,0.0009646813,0.0000704347,0.00004932874,0.00000517286,0.000829268,0.07446582],"study_design_scores_gemma":[0.0009000061,0.001620145,0.9863503,0.0000168363,0.00006150299,0.000007456079,0.000686162,0.0001649365,0.000006620641,0.001016769,0.008936846,0.00023243],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9709784,0.0001835887,0.0001972384,0.02712139,0.00005184676,0.0009251958,0.00003045914,0.00005607515,0.0004558052],"genre_scores_gemma":[0.9934782,0.00003587516,0.003828415,0.002029929,0.0003889158,0.00002441941,0.0001962534,0.000005907437,0.00001208304],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07423339,"threshold_uncertainty_score":0.5936868,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2538213421","doi":"10.1130/abs/2016am-281038","title":"NEW CA-TIMS U-PB GEOCHRONOLOGY FROM THE BELLY RIVER GROUP (UPPER CRETACEOUS) AT DINOSAUR PROVINCIAL PARK, ALBERTA, CANADA, AND IMPLICATIONS FOR DINOSAUR BIOSTRATIGRAPHY OF THE WESTERN INTERIOR BASIN","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":4,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geochronology; Cretaceous; Geology; Biostratigraphy; Archaeology; Group (periodic table); Paleontology; Drainage basin; Geography; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01065987656723406,"gpt":0.2110616686331827,"spread":0.2004017920659486,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001498932,0.0002848971,0.0004100447,0.000008191066,0.0003137068,0.00003586422,0.001084649,0.0001997912,0.00003638261],"category_scores_gemma":[0.000127998,0.0001312956,0.0002387116,0.0002201776,0.001654122,0.0001331384,0.0005214535,0.0001965655,0.000001429074],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00004492289,"about_ca_system_score_gemma":0.0002827563,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.2782615,"about_ca_topic_score_gemma":0.1518523,"domain_scores_codex":[0.9980919,0.00007549956,0.0004594179,0.0006190904,0.0002275794,0.0005264747],"domain_scores_gemma":[0.9973257,0.001118437,0.0005900229,0.0006594016,0.0001572453,0.000149214],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009595031,0.0002162172,0.8300942,0.00006225947,0.0003314882,0.00000198066,0.001695841,0.0000172679,0.005652697,0.0003742515,0.01123219,0.1502256],"study_design_scores_gemma":[0.0006572202,0.0006964456,0.9052537,0.00007632245,0.00005508198,0.00002159951,0.0001287521,0.00007620739,0.001694753,0.001706428,0.08936964,0.0002638389],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.8839211,0.0001423102,0.02214724,0.09225997,0.00008283408,0.001073873,0.00007254585,0.00004398741,0.0002561545],"genre_scores_gemma":[0.9657365,0.00003501524,0.0321187,0.001383348,0.00006556378,0.0001056061,0.00001931652,0.000005412664,0.0005305574],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1499618,"threshold_uncertainty_score":0.8636242,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2982321140","doi":"10.1130/abs/2016am-283146","title":"THE END OF MIDCONTINENT RIFT MAGMATISM AND THE PALEOGEOGRAPHY OF LAURENTIA","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Magmatism; Laurentia; Palaeogeography; Rift; Geology; Metamorphic petrology; Paleontology; Petrology; Ordovician; Tectonics; Volcanism","retraction":null,"screen_n_in":null,"score":{"opus":0.0109957990013015,"gpt":0.220099399812768,"spread":0.2091036008114665,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0008148026,0.0001349852,0.0003658872,0.0000146139,0.0001948633,0.000009933504,0.0003374921,0.0001316891,0.0003400372],"category_scores_gemma":[0.00008057064,0.00004664775,0.0001786192,0.0002056423,0.01225052,0.00005420423,0.00003791273,0.0002033058,0.000007159397],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":2.442042e-7,"about_ca_system_score_gemma":0.00002695742,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008487297,"about_ca_topic_score_gemma":0.0006157609,"domain_scores_codex":[0.9985254,0.0002082025,0.0003899618,0.0002081058,0.0002853088,0.0003829907],"domain_scores_gemma":[0.9972693,0.001894687,0.0004179406,0.0002301074,0.0001136518,0.00007432434],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002431999,0.00004836485,0.8936747,0.00003043468,0.0001429908,0.000001357375,0.0001997317,0.00001039188,0.00001013785,0.0001101974,0.00008350551,0.1054449],"study_design_scores_gemma":[0.0009527523,0.0007827741,0.993203,0.00003635319,0.0000420318,0.00001752723,0.0004836026,0.00005434823,0.00009502322,0.001506196,0.002749671,0.0000766952],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9883651,0.002936358,0.00006929071,0.006585672,0.00003229813,0.00038249,0.00001337448,0.00001451987,0.0016009],"genre_scores_gemma":[0.9955212,0.001551622,0.002749178,0.00009326708,0.00001114521,0.000007578456,0.00001174627,0.000001700303,0.00005251984],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1053682,"threshold_uncertainty_score":0.9904376,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2775626627","doi":"10.1130/abs/2017am-305763","title":"DURATION OF GARNET GROWTH AND P-T-T PATHS FROM SM-ND DATING AND ISOCHEMICAL PHASE DIAGRAMS: COAST MOUNTAINS BATHOLITH, BRITISH COLUMBIA, CANADA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Water Quality and Resources Studies","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Batholith; Duration (music); Geology; Phase (matter); Seismology; Physics; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.02146855967930719,"gpt":0.2295506748165233,"spread":0.2080821151372161,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0001603627,0.0001386651,0.0003588296,0.00000184332,0.0004975758,0.0001510222,0.0001937579,0.0001073985,0.0000725005],"category_scores_gemma":[0.0001148953,0.0001316183,0.00005075527,0.00004761678,0.003118279,0.0001585055,0.000328676,0.0001940487,4.15225e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003131572,"about_ca_system_score_gemma":0.00002057028,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.9408648,"about_ca_topic_score_gemma":0.4696153,"domain_scores_codex":[0.9985737,0.00004399579,0.0003599804,0.0003837068,0.0003306091,0.0003080488],"domain_scores_gemma":[0.9990027,0.0001301165,0.0005171198,0.0001850684,0.0000253085,0.0001396974],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00002989869,0.000422758,0.9341914,0.00006915823,0.00008976371,0.00001881953,0.001941276,0.00001168671,0.001540491,8.26982e-7,0.00110802,0.0605759],"study_design_scores_gemma":[0.001018022,0.0006190155,0.9914624,0.00007589847,0.00005327903,0.00001578777,0.003924003,0.0002145607,0.0005942329,0.0002106957,0.001557468,0.0002546229],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9986881,0.0001192658,0.00005422748,0.0004356137,0.000012576,0.0002526783,0.000069947,0.00001703029,0.0003505341],"genre_scores_gemma":[0.9932121,0.0002122297,0.006223537,0.0001981274,0.00002650184,0.00001886497,0.00005579777,0.000007188815,0.00004562484],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4712495,"threshold_uncertainty_score":0.9995947,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2948512827","doi":"10.1130/abs/2019cd-329812","title":"UPDATE OF THE MODERATE BAJA BRITISH COLUMBIA (AKA MOJAVE BC) HYPOTHESIS FOR 1600 KM OF NORTHWARD TRANSLATION FROM ~90 – 40 MA","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Paleopathology and ancient diseases","field":"Arts and Humanities","cited_by":3,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"AKA; Geology; Translation (biology); Computer science; Chemistry; Library science","retraction":null,"screen_n_in":null,"score":{"opus":0.02940796979111563,"gpt":0.2127441461486045,"spread":0.1833361763574889,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001324533,0.0001451202,0.0004685446,0.00000714609,0.0001953462,0.00006057196,0.0002431357,0.0001185265,0.0007968734],"category_scores_gemma":[0.00002282457,0.0001199977,0.0004168821,0.00006625179,0.001593187,0.0001329553,0.00003056249,0.0001422703,0.000006948124],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000007025864,"about_ca_system_score_gemma":0.00004982152,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006526249,"about_ca_topic_score_gemma":0.002624058,"domain_scores_codex":[0.9986613,0.00005591558,0.0004353387,0.0003057488,0.0002430132,0.0002987295],"domain_scores_gemma":[0.9987658,0.0002319414,0.0005197858,0.0002190362,0.0002056478,0.00005783849],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00183176,0.005606101,0.5768948,0.001142083,0.001545751,0.00001254135,0.02176114,0.002284304,0.001416741,0.0004706218,0.006432885,0.3806012],"study_design_scores_gemma":[0.00259648,0.002157879,0.9374344,0.0003878045,0.0004641303,0.000004505295,0.0061722,0.001319856,0.0007676017,0.008056973,0.04001261,0.000625568],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.996656,0.0002471463,0.00009117977,0.0003034645,0.00006813661,0.0007733755,0.000482359,0.00003980594,0.001338523],"genre_scores_gemma":[0.993067,0.00007530103,0.005756333,0.0003630311,0.00005015199,0.00005889515,0.0001117499,0.00001282721,0.0005046734],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3799756,"threshold_uncertainty_score":0.9865781,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2964879941","doi":"10.1130/abs/2019am-331913","title":"THE CLIMATE LITERACY AND ENERGY AWARENESS NETWORK (CLEAN)","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Hybrid Renewable Energy Systems","field":"Energy","cited_by":3,"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":"Clean energy; Literacy; Computer science; Energy (signal processing); Environmental science; Psychology; Environmental protection; Pedagogy; Physics","retraction":null,"screen_n_in":null,"score":{"opus":0.01125187822533154,"gpt":0.2376807992015145,"spread":0.2264289209761829,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004606688,0.0003696102,0.0006032015,0.0000121743,0.0004082649,0.0001497961,0.0004272719,0.0002169195,0.0000729728],"category_scores_gemma":[0.00002172662,0.0002065948,0.000229502,0.0004380762,0.0009669685,0.0001918918,0.0002332422,0.0002818212,0.00003143767],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003503608,"about_ca_system_score_gemma":0.00005921745,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.008447433,"about_ca_topic_score_gemma":0.0002169569,"domain_scores_codex":[0.9971266,0.0001642682,0.0006348211,0.0005868363,0.0004464329,0.001041057],"domain_scores_gemma":[0.9979683,0.0005515449,0.0005781197,0.0005436615,0.0001494441,0.0002089135],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0002744052,0.000327529,0.07795679,0.0001500807,0.0005124005,0.00002122419,0.0005217873,0.1172926,0.0001179828,0.00509787,0.001168764,0.7965586],"study_design_scores_gemma":[0.001047705,0.001515282,0.03815151,0.0002205251,0.00006279144,0.00006974197,0.001313989,0.008531464,0.0002857241,0.0008748937,0.9472526,0.0006737492],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9806861,0.001718963,0.0005920581,0.001118499,0.0003533092,0.0003514295,0.000003857533,0.000353254,0.01482251],"genre_scores_gemma":[0.9899055,0.001161866,0.006463935,0.0006169715,0.0002405867,0.00009303127,0.00004806282,0.00004434818,0.001425668],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9460838,"threshold_uncertainty_score":0.9981554,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4403857796","doi":"10.1130/abs/2024am-404092","title":"A NEW WORKING MODEL FOR CO-EVOLUTION OF PLANT AND ANIMAL SPECIES ON THE BAJA CALIFORNIA PENINSULA FROM GENOMIC AND GEOLOGIC DATA","year":2024,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Species Distribution and Climate Change","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Department of Environment and Conservation","funders":"","keywords":"Peninsula; Evolutionary biology; Geology; Earth science; Biology; Ecology","retraction":null,"screen_n_in":null,"score":{"opus":0.07155962311618719,"gpt":0.2614971250431039,"spread":0.1899375019269167,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001984426,0.0001529449,0.0002151544,0.000006172274,0.0001269221,0.00004668513,0.0002427679,0.00009509926,0.001083824],"category_scores_gemma":[0.00002528268,0.00008714637,0.00005988266,0.0001145799,0.001071815,0.0000684347,0.0002496883,0.0001560584,0.00001607043],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00008428739,"about_ca_system_score_gemma":0.00001949652,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0009949127,"about_ca_topic_score_gemma":0.00005162003,"domain_scores_codex":[0.9988899,0.00001923581,0.000217652,0.0004081171,0.0002067423,0.0002583558],"domain_scores_gemma":[0.999321,0.0002394185,0.0001371052,0.0002101164,0.000007921867,0.00008439839],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.003350331,0.002024218,0.6063794,0.0004861623,0.001144276,0.000036883,0.009236965,0.00504819,0.05076155,0.009094111,0.1436867,0.1687513],"study_design_scores_gemma":[0.000747157,0.001637498,0.7056208,0.0001093258,0.0001419153,0.00001650232,0.006717456,0.1989531,0.0002085561,0.001718729,0.08371843,0.0004105027],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9908817,0.0005252896,0.004344935,0.002131094,0.00001401386,0.000483928,0.0007708965,0.00004919127,0.0007989692],"genre_scores_gemma":[0.9917906,0.0002955438,0.007213025,0.0002024713,0.00002582893,0.00001980532,0.0003865161,0.000007235603,0.00005895395],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1939049,"threshold_uncertainty_score":0.9998293,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3016721852","doi":"10.1130/abs/2020se-344176","title":"THE MOUNT EPHRAIM BLOCK, COBEQUID HIGHLANDS, NOVA SCOTIA, CANADA: A SIGNIFICANT CA. 750-735 MA MAGMATIC ARC EVENT IN AVALONIA","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Archaeology and ancient environmental studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Mount; Nova scotia; Nova (rocket); Geology; Block (permutation group theory); Event (particle physics); Arc (geometry); Back-arc basin; Seismology; Computer science; Physics; Subduction; Astrophysics; Tectonics; Aeronautics; Oceanography; Operating system; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.01446734383628138,"gpt":0.2008824064337139,"spread":0.1864150625974325,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002683136,0.0002574,0.0004049475,0.000007335962,0.0003024945,0.00001647047,0.0003698404,0.00009159276,0.000454555],"category_scores_gemma":[0.00004436322,0.0001433666,0.0001126044,0.0002771553,0.001747705,0.00006151731,0.00008892721,0.0004149577,0.00007053161],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000334044,"about_ca_system_score_gemma":0.0001357889,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.3957143,"about_ca_topic_score_gemma":0.2854996,"domain_scores_codex":[0.9978291,0.00008902467,0.0004723671,0.0004127551,0.0004930928,0.0007036647],"domain_scores_gemma":[0.9990144,0.0003011365,0.0002795577,0.0001550437,0.00002452899,0.0002253811],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001801427,0.0001476631,0.9601623,0.00005661292,0.0001314212,0.00007718749,0.001122904,0.009295368,0.00002804795,0.000009316183,0.002217905,0.02657108],"study_design_scores_gemma":[0.0004161146,0.001222719,0.9738876,0.00003125654,0.0000263914,0.00001108701,0.003012682,0.002381118,0.00003441767,0.00008404539,0.01864962,0.0002429244],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9799407,0.0008675152,0.0000650974,0.01792012,0.000058528,0.0005453057,0.00003091693,0.00003006197,0.0005418094],"genre_scores_gemma":[0.9952764,0.0002523333,0.002406256,0.001885403,0.00004080881,0.00000801828,0.00006565722,0.000004600599,0.00006054332],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1102148,"threshold_uncertainty_score":0.7275382,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3166212613","doi":"10.1130/abs/2020am-355847","title":"AN OVERVIEW OF CHALCOPHILE ELEMENT CONTENTS OF PYRRHOTITE, PENTLANDITE, CHALCOPYRITE AND PYRITE FROM MAGMATIC NI-CU- PGE DEPOSITS","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Université du Québec","funders":"","keywords":"Pentlandite; Pyrrhotite; Chalcopyrite; Pyrite; Geology; Geochemistry; Mineralogy; Copper; Metallurgy; Materials science","retraction":null,"screen_n_in":null,"score":{"opus":0.04724901100718439,"gpt":0.2656151932257614,"spread":0.218366182218577,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002059641,0.000290572,0.0007449765,0.00001591679,0.0000807743,0.00003658037,0.0007194427,0.0001576997,0.00006620743],"category_scores_gemma":[0.00007607934,0.0002160044,0.0001758376,0.0004129141,0.0006831042,0.0002588517,0.000326921,0.0002460724,0.000003288931],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000970277,"about_ca_system_score_gemma":0.00002968721,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008673039,"about_ca_topic_score_gemma":0.000009199077,"domain_scores_codex":[0.9977027,0.00007714605,0.0007203295,0.0006106436,0.0004729242,0.0004163251],"domain_scores_gemma":[0.9979603,0.0001624906,0.0008665605,0.0004397472,0.0003017499,0.0002691317],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0005880461,0.007148387,0.5671224,0.006450016,0.001900383,0.0001364109,0.02289676,0.002673073,0.03226357,0.001142078,0.00190495,0.355774],"study_design_scores_gemma":[0.005230749,0.01514117,0.8834949,0.001428477,0.0002913195,0.00005017623,0.003584525,0.06374857,0.0131203,0.003855032,0.00851856,0.001536252],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9852839,0.001576665,0.007013147,0.004631378,0.00004105817,0.0007049503,0.00002333356,0.0001256158,0.000599944],"genre_scores_gemma":[0.9288791,0.0003583966,0.06993461,0.0006904803,0.00003670814,0.00002567221,0.00005793146,0.000005449967,0.0000116582],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3542377,"threshold_uncertainty_score":0.8808405,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3017334309","doi":"10.1130/abs/2020nc-348072","title":"THE MIDCONTINENT RIFT AND ITS MINERAL SYSTEMS: OVERVIEW AND TEMPORAL CONSTRAINTS OF NI-CU-PGE MINERALIZED INTRUSIONS","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geoscience and Mining Technology","field":"Engineering","cited_by":3,"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; Rift; Geochemistry; Mineral; Petrology; Seismology; Tectonics; Materials science; Metallurgy","retraction":null,"screen_n_in":null,"score":{"opus":0.02689952996250001,"gpt":0.2393142607169882,"spread":0.2124147307544882,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001719306,0.0001929359,0.0004307404,0.00001191537,0.00009836119,0.00002690196,0.00019659,0.000147172,0.00001017896],"category_scores_gemma":[0.00007872688,0.0001153414,0.00006963895,0.0002476853,0.001609614,0.00006613749,0.0001135535,0.0002405393,0.000001523374],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006047612,"about_ca_system_score_gemma":0.00002071647,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0003901507,"about_ca_topic_score_gemma":0.00001433114,"domain_scores_codex":[0.9988002,0.0000276004,0.0004012446,0.0002443486,0.0001777046,0.0003488881],"domain_scores_gemma":[0.999351,0.0001148845,0.0001896532,0.0001312158,0.00007613142,0.0001371547],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0004080389,0.001116915,0.3041681,0.004517049,0.001839984,0.000103356,0.01224879,0.003747444,0.0388542,0.004898792,0.01705564,0.6110417],"study_design_scores_gemma":[0.01194203,0.01671558,0.4570667,0.002001691,0.0008227415,0.0005902866,0.04200938,0.2106649,0.001848781,0.0007758845,0.2518818,0.003680289],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9924965,0.003602908,0.0001776329,0.002885237,0.00004299293,0.0004337899,0.000009292456,0.0001633344,0.0001883053],"genre_scores_gemma":[0.990348,0.001325893,0.008046787,0.0001826288,0.00002055713,0.00003649818,0.000008326034,0.00001000141,0.00002126881],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.6073614,"threshold_uncertainty_score":0.5930688,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2771374424","doi":"10.1130/abs/2017am-300236","title":"EVOLUTION OF JURA-CRETACEOUS BASINS IN SOUTHWEST YUKON, WITH IMPLICATIONS FOR MESOZOIC ACCRETIONARY PROCESSES IN THE WESTERN NORTH AMERICAN CORDILLERA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Geology; Cretaceous; Mesozoic; Paleontology; Earth science; Structural basin","retraction":null,"screen_n_in":null,"score":{"opus":0.02630691164758571,"gpt":0.2555812964092539,"spread":0.2292743847616682,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000203354,0.0001892355,0.0004053788,0.00002767894,0.0003262754,0.00004145451,0.0004549164,0.00005503861,0.00001388115],"category_scores_gemma":[0.00009729063,0.0001030185,0.00008401027,0.0004451013,0.001943127,0.0001736543,0.00002200263,0.000211111,0.000002628184],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000008318871,"about_ca_system_score_gemma":0.0001477606,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.007862747,"about_ca_topic_score_gemma":0.0442631,"domain_scores_codex":[0.9986366,0.00004252158,0.0003523705,0.000330406,0.0002466834,0.000391394],"domain_scores_gemma":[0.9983258,0.0004388278,0.000660088,0.0003371242,0.0001840585,0.00005405083],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001357125,0.000210589,0.9410541,0.00006350064,0.00004554168,0.00000210778,0.0008852124,0.001027334,8.617383e-7,0.000002787546,0.00002147972,0.05655077],"study_design_scores_gemma":[0.0004687185,0.002136321,0.9937765,0.00005170319,0.00003306487,0.00001103435,0.002222513,0.0001221387,0.000003455707,0.0000611046,0.0009600716,0.0001533797],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9949327,0.0003575798,0.0001761463,0.002918878,0.000008826281,0.0008489913,0.00008860765,0.00002441495,0.0006438728],"genre_scores_gemma":[0.9940679,0.0002535512,0.005283758,0.000184986,0.00002587803,0.00007007639,0.00009919608,0.000004568669,0.00001009595],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05639739,"threshold_uncertainty_score":0.998744,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3094709442","doi":"10.1130/abs/2020am-355223","title":"BIVERGENT SUBDUCTION DURING THE GRENVILLIAN OROGENY? GEOCHEMICAL AND ISOTOPIC EVIDENCE FROM THE CENTRAL GRENVILLE PROVINCE IN QUEBEC","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Orogeny; Subduction; Geology; Geochemistry; Earth science; Seismology; Tectonics","retraction":null,"screen_n_in":null,"score":{"opus":0.01867191203416802,"gpt":0.2114414241646044,"spread":0.1927695121304364,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001743156,0.0002192982,0.0002663632,0.00000461883,0.0002134681,0.00008540216,0.000806567,0.0001279617,0.00004748138],"category_scores_gemma":[0.0001841549,0.0001157804,0.0001171189,0.0003740998,0.0009740376,0.0001907016,0.0004478389,0.000460731,0.000005788313],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000391525,"about_ca_system_score_gemma":0.00007405077,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.01047681,"about_ca_topic_score_gemma":0.0004474501,"domain_scores_codex":[0.9981376,0.000093127,0.0003479177,0.0006033115,0.0003192717,0.0004987515],"domain_scores_gemma":[0.9988315,0.000322467,0.0002671714,0.0003656243,0.00006276018,0.000150533],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.000190285,0.0004903413,0.8887214,0.0002519424,0.0001846925,0.00007339245,0.0151107,0.003218221,0.01006371,0.0001627064,0.001179648,0.08035295],"study_design_scores_gemma":[0.0005613246,0.0005083852,0.9650812,0.0001715688,0.00002663008,0.00002464468,0.002490264,0.007724881,0.003979844,0.0004022692,0.01864023,0.0003887662],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9343738,0.0005238805,0.001449319,0.06303547,0.00002732081,0.0004672831,0.000001740148,0.00006995455,0.00005127145],"genre_scores_gemma":[0.9872218,0.0001869178,0.0115188,0.0008772804,0.00009085813,0.00004050573,0.000006801659,0.000003040822,0.00005397788],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.07996419,"threshold_uncertainty_score":0.9961125,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2513426613","doi":"10.1130/abs/2016am-283470","title":"LOCALIZED AND AREALLY EXTENSIVE ALTERATIONS IN MARATHON VALLEY, ENDEAVOUR CRATER RIM, MARS","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Guelph","funders":"","keywords":"Impact crater; Mars Exploration Program; Geology; Astrobiology; Earth science","retraction":null,"screen_n_in":null,"score":{"opus":0.0178647297875193,"gpt":0.2371229835817802,"spread":0.2192582537942609,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001364172,0.0001529268,0.0002388827,0.00001641295,0.00008375685,0.00003670777,0.0001012045,0.00005814759,0.0001087675],"category_scores_gemma":[0.000006218638,0.00008544615,0.00006492768,0.0001536675,0.0004762302,0.0003027911,0.00003580908,0.0001192008,0.00003274138],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000009991991,"about_ca_system_score_gemma":0.00004042069,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.000552348,"about_ca_topic_score_gemma":0.00001864276,"domain_scores_codex":[0.9989019,0.00004174339,0.000264492,0.0003068034,0.0001696256,0.0003154052],"domain_scores_gemma":[0.9994335,0.00009271022,0.0001701861,0.0001281282,0.00007871285,0.00009677342],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003347158,0.001072245,0.6027774,0.00002897608,0.0001846962,0.00002458866,0.002337741,0.001531028,0.004710557,0.0005239699,0.002716205,0.3837578],"study_design_scores_gemma":[0.003753875,0.003192784,0.9512934,0.0002482807,0.00007427396,0.0000168771,0.005916817,0.002929793,0.001325154,0.01094891,0.01932834,0.0009714774],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9852915,0.00002739869,0.01039444,0.002891386,0.00002051413,0.0003391595,0.00001361287,0.00002887577,0.0009931212],"genre_scores_gemma":[0.9843423,0.0000375092,0.01496111,0.0003245921,0.00003961286,0.00003963918,0.0001129105,0.000005175757,0.0001371816],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3827864,"threshold_uncertainty_score":0.3484393,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3097848281","doi":"10.1130/abs/2020am-354955","title":"LIMNO-CHEMICAL MYSTERY RESOLVED FOR CRAWFORD LAKE, ONTARIO, CANADA; GSSP CANDIDATE FOR THE ANTHROPOCENE EPOCH","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Isotope Analysis in Ecology","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Brock University","funders":"","keywords":"Anthropocene; Epoch (astronomy); Global Boundary Stratotype Section and Point; Geology; Paleontology; Astronomy; Physics; Galaxy; Stage (stratigraphy)","retraction":null,"screen_n_in":null,"score":{"opus":0.0188515656104165,"gpt":0.2341459298562905,"spread":0.2152943642458741,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002469653,0.000266974,0.000508549,0.000004104748,0.0003071257,0.00002872806,0.0005614579,0.0001698301,0.001040493],"category_scores_gemma":[0.0001308943,0.0001626005,0.0002887834,0.0002576913,0.001608423,0.00008582186,0.0002166796,0.0003141699,0.000009016811],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0002180877,"about_ca_system_score_gemma":0.0001938265,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.3780191,"about_ca_topic_score_gemma":0.6291564,"domain_scores_codex":[0.9977786,0.00003214198,0.0004971845,0.0005807527,0.0003838601,0.0007274584],"domain_scores_gemma":[0.9984896,0.0005451555,0.0003896499,0.0003014105,0.00005817217,0.0002160281],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.002032382,0.001526364,0.5819653,0.0002274,0.001739785,0.00004025098,0.003583246,0.01624679,0.002252058,0.00002923699,0.2536361,0.1367211],"study_design_scores_gemma":[0.002223619,0.004040162,0.144078,0.00002438332,0.0004701139,0.00001738818,0.001638033,0.007564768,0.002829117,0.0003339297,0.8359467,0.0008337102],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9512998,0.00006957229,0.01613029,0.02787837,0.0001325926,0.003002457,0.00005905402,0.00009760683,0.001330291],"genre_scores_gemma":[0.9450129,0.00002377027,0.04744608,0.006734504,0.00007386361,0.0003741287,0.0001057423,0.00002107117,0.0002079161],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5823106,"threshold_uncertainty_score":0.9998727,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2770316474","doi":"10.1130/abs/2017ne-290335","title":"LATE GLACIAL ONTARIO LOBE ICE ON THE NIAGARA PENINSULA: HOW FAR DID IT GO?","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Plant and Fungal Species Descriptions","field":"Biochemistry, Genetics and Molecular Biology","cited_by":3,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Glacial period; Peninsula; Geology; Ice sheet; Physical geography; Oceanography; Paleontology; Geography; Archaeology","retraction":null,"screen_n_in":null,"score":{"opus":0.02774535665940616,"gpt":0.2390914792189782,"spread":0.211346122559572,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001671733,0.0002498364,0.0002669254,0.000005611049,0.0006235613,0.0001443899,0.0006109659,0.0002457316,0.0001121313],"category_scores_gemma":[0.00007719322,0.0001464557,0.0002697592,0.00004903932,0.001241676,0.00001412879,0.0001977002,0.000389884,0.00003518502],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002920225,"about_ca_system_score_gemma":0.00007214901,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00193455,"about_ca_topic_score_gemma":0.001790286,"domain_scores_codex":[0.9986404,0.00003515128,0.0001986286,0.0004141351,0.0002656827,0.0004459562],"domain_scores_gemma":[0.9987913,0.00003560837,0.0003814278,0.0005690863,0.0001056749,0.0001168866],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.003855319,0.005818223,0.3544571,0.0001489268,0.003391984,0.0001821019,0.004502234,0.0008220087,0.2540106,0.0009497905,0.2484454,0.1234164],"study_design_scores_gemma":[0.0005608156,0.00226953,0.2099838,0.00002767799,0.00005754162,0.00001633774,0.0003412355,0.00003736551,0.003651916,0.00006049988,0.782652,0.0003413048],"study_design_candidate":"not_applicable","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9761763,0.0000779601,0.0002039249,0.00938523,0.0000851592,0.0004111474,0.00002143509,0.00002755627,0.01361134],"genre_scores_gemma":[0.9901497,0.0002034262,0.002817731,0.001781335,0.0001872341,0.00004319394,0.0001284463,0.0000132544,0.004675636],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5342066,"threshold_uncertainty_score":0.5972292,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3095100757","doi":"10.1130/abs/2020am-359454","title":"APPLYING MACHINE LEARNING METHODS TO PREDICT GEOLOGY USING SOIL SAMPLE GEOCHEMISTRY","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Mineral Processing and Grinding","field":"Engineering","cited_by":3,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Sample (material); Geochemistry; Chemistry","retraction":null,"screen_n_in":null,"score":{"opus":0.03466357371897337,"gpt":0.285885824362606,"spread":0.2512222506436326,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0002677569,0.000318203,0.000535092,0.00001802983,0.0001800898,0.00004174482,0.0002598289,0.0002213008,0.0001058698],"category_scores_gemma":[0.0002082287,0.0002569599,0.0001619955,0.0004970014,0.000290909,0.0000898139,0.0001321895,0.0007678316,0.000007113325],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003728776,"about_ca_system_score_gemma":0.00002889819,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005105214,"about_ca_topic_score_gemma":0.000001961789,"domain_scores_codex":[0.9982035,0.00004942534,0.0004385232,0.0004294273,0.0002413304,0.0006378347],"domain_scores_gemma":[0.9990302,0.0002357793,0.0001747408,0.0001487359,0.00007537329,0.0003351519],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.00005109598,0.0000795366,0.01503079,0.0004988658,0.0002010412,0.000009077846,0.001208841,0.7572712,0.03149704,0.000001742746,0.0002447854,0.1939059],"study_design_scores_gemma":[0.000685042,0.00111816,0.001765206,0.0001502653,0.0001061874,0.00004118651,0.001375447,0.9239587,0.009932297,0.0000933417,0.05994796,0.0008262769],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.7129254,0.000530479,0.2837186,0.0005944063,0.00004347489,0.0004538312,0.000006681038,0.0009290264,0.0007980661],"genre_scores_gemma":[0.5881296,0.00002591702,0.4112235,0.000397759,0.00009284462,0.00005434934,0.00003576986,0.00002687817,0.00001342464],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1930797,"threshold_uncertainty_score":0.9999883,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2774373866","doi":"10.1130/abs/2017am-308060","title":"GEOCHEMICAL, ISOTOPIC, AND MINERALOGICAL CHARACTERIZATION OF THE FROBISHER SUITE MAFIC-ULTRAMAFIC SILLS, SOUTHERN BAFFIN ISLAND, CANADA, WITH IMPLICATIONS FOR METALLOGENIC POTENTIAL","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Mafic; Geology; Geochemistry; Ultramafic rock; Sill; Petrology","retraction":null,"screen_n_in":null,"score":{"opus":0.01046854831688472,"gpt":0.1911753864335365,"spread":0.1807068381166518,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001228651,0.000231186,0.0004448387,0.00000815288,0.0004036663,0.00006378478,0.0004887437,0.0001530106,0.0004382544],"category_scores_gemma":[0.00006480439,0.0001104481,0.000212635,0.0001302224,0.001377831,0.00008755267,0.00005548957,0.000204904,0.000001603995],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000004817296,"about_ca_system_score_gemma":0.00007531753,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1342348,"about_ca_topic_score_gemma":0.07819089,"domain_scores_codex":[0.9985054,0.00003641534,0.0003724134,0.0004237696,0.0002575163,0.0004044894],"domain_scores_gemma":[0.9985663,0.0001280358,0.0006092847,0.000371152,0.0001790386,0.0001462028],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001729362,0.0002163236,0.9616815,0.00005670088,0.0002837095,0.000001705788,0.00009801616,0.0004709336,0.01178164,0.000009661704,0.0001460787,0.02508084],"study_design_scores_gemma":[0.0004568055,0.0004171611,0.9955959,0.00001579769,0.0001628242,0.00001181116,0.0001634791,0.0006124161,0.0005598406,0.0004602685,0.001339029,0.0002046452],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9931385,0.00006722387,0.0003411506,0.005481372,0.00001908189,0.0005149054,0.0002758344,0.00001739483,0.0001445431],"genre_scores_gemma":[0.9942997,0.0000346862,0.0045498,0.0004668574,0.00004445147,0.00001847265,0.0004364146,0.000004122462,0.0001454705],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.05604395,"threshold_uncertainty_score":0.9386297,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2775386294","doi":"10.1130/abs/2017am-295190","title":"IDENTIFICATION OF THE EOCENE THERMAL MAXIMUM 2 (ETM-2) IN A TERRESTRIAL SECTION OF THE HIGH ARCTIC BASED ON NEW U-PB ZIRCON AGES AND CARBON ISOTOPE RECORDS (STENKUL FIORD, ELLESMERE ISLAND, CANADA)","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Fjord; Arctic; Zircon; Geology; The arctic; Oceanography; Section (typography); Isotopes of carbon; Isotope; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.01645054946727159,"gpt":0.2045086527059903,"spread":0.1880581032387187,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002847869,0.0001438118,0.0002731857,0.000008318389,0.0002638054,0.00002800809,0.0002977539,0.0001149182,0.00004608335],"category_scores_gemma":[0.0001495251,0.00006945535,0.00009004599,0.0001419611,0.0006699314,0.00006716524,0.00003861761,0.0002411409,2.870881e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001352005,"about_ca_system_score_gemma":0.0001135303,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.6677707,"about_ca_topic_score_gemma":0.3434764,"domain_scores_codex":[0.9986448,0.00009860431,0.0003650454,0.0002430035,0.0004213795,0.0002271802],"domain_scores_gemma":[0.9987307,0.000123721,0.0007546557,0.0002888212,0.00005235671,0.00004980325],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003379905,0.000120241,0.9085695,0.00003672007,0.00003987139,0.000001313845,0.0002060226,0.009664746,0.0003200014,0.000001004285,0.0001257931,0.08057679],"study_design_scores_gemma":[0.0006111918,0.0007307492,0.9945477,0.00006614128,0.00002577319,9.710161e-7,0.0003451313,0.002530107,0.0005567478,0.0001410527,0.000350842,0.00009364916],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9938864,0.00004977124,0.00003371893,0.005104134,0.0001980988,0.0004689461,0.00001139692,0.000006244454,0.0002413438],"genre_scores_gemma":[0.9992744,0.00006342284,0.0003642509,0.0001836065,0.0000633366,0.000005737689,0.00001580383,0.000002379958,0.00002700995],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3242943,"threshold_uncertainty_score":0.6685035,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3211009424","doi":"10.1130/abs/2020am-352710","title":"COMPLETE METAMORPHIC CYCLE AND LONG LIVED ANATEXIS IN THE C. 2.1 GA MISTINIBI COMPLEX, CANADA","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Université Laval","funders":"","keywords":"Anatexis; Metamorphic rock; Geology; Computer science; Seismology; Paleontology","retraction":null,"screen_n_in":null,"score":{"opus":0.03989332544779151,"gpt":0.2339182195656905,"spread":0.194024894117899,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000131398,0.0001795859,0.0003675303,0.00001011137,0.00007599793,0.00003298416,0.0002245099,0.00006511983,0.00007557004],"category_scores_gemma":[0.00002271667,0.0001102017,0.00009201015,0.0004748479,0.0003603465,0.00005197535,0.00003401625,0.0003103766,0.00000325487],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00002062648,"about_ca_system_score_gemma":0.00003272203,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.0506146,"about_ca_topic_score_gemma":0.01926986,"domain_scores_codex":[0.9987901,0.00006309792,0.0003213118,0.0002219726,0.0003047133,0.0002987397],"domain_scores_gemma":[0.9994576,0.0001207464,0.0000948415,0.0001386426,0.00004231398,0.0001458811],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","study_design_scores_codex":[0.000169665,0.0007843065,0.06707034,0.0009867138,0.002023008,0.0003220726,0.02077527,0.824173,0.003043047,0.00004970558,0.01138905,0.06921382],"study_design_scores_gemma":[0.001430703,0.0007717969,0.2638436,0.00005481635,0.0001853595,0.00001810223,0.0118474,0.6797142,0.0001326471,0.00008422692,0.0411253,0.000791799],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9868942,0.0003244744,0.001966193,0.009143642,0.00001171794,0.0003705782,0.000008214511,0.0001167848,0.001164209],"genre_scores_gemma":[0.9941244,0.0001134516,0.00363137,0.002002616,0.00002349043,0.00002246933,0.00006619997,0.00001136777,0.000004677883],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1967733,"threshold_uncertainty_score":0.9986259,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4244857092","doi":"10.1130/abs/2017am-306997","title":"A COMPARATIVE STUDY OF GLACIOVOLCANIC PALAGONITIZATION OF THOLEIITIC AND ALKALINE SIDEROMELANE AT HELGAFELL, ICELAND AND WELLS GRAY-CLEARWATER VOLCANIC FIELD, BC CANADA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Gray (unit); Volcano; Geology; Field (mathematics); Geochemistry; Mathematics; Medicine","retraction":null,"screen_n_in":null,"score":{"opus":0.01666527582130655,"gpt":0.2382056802297059,"spread":0.2215404044083993,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009281194,0.0001674066,0.0005165996,0.00001797099,0.0001305454,0.00002273657,0.0001249055,0.00008152728,0.00004847085],"category_scores_gemma":[0.00001333281,0.0001163586,0.00005163057,0.00009751309,0.000379252,0.00008660688,0.00006042342,0.0001421488,7.417699e-7],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0000198873,"about_ca_system_score_gemma":0.0000248862,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1014409,"about_ca_topic_score_gemma":0.07929571,"domain_scores_codex":[0.9989661,0.00003785426,0.0003618551,0.0001953342,0.0002445628,0.0001943066],"domain_scores_gemma":[0.9992097,0.00008518546,0.0002871928,0.0002236862,0.00009614242,0.00009807049],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0008533115,0.003584936,0.7543258,0.002381626,0.006828616,0.0001257801,0.05038622,0.1309754,0.0286669,0.0000157691,0.001584186,0.02027143],"study_design_scores_gemma":[0.004918418,0.008522188,0.8597693,0.0002241555,0.0007574024,0.00002415422,0.0387927,0.07442571,0.008634889,0.000102732,0.002845801,0.0009825373],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9988799,0.0001313957,0.0001744304,0.0001951554,0.00001319575,0.0003120921,0.000005706772,0.00002119842,0.0002668918],"genre_scores_gemma":[0.9991595,0.0002276544,0.0004663527,0.00003606167,0.00001084396,0.00001404436,0.0000267929,0.000009015142,0.00004969405],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1054435,"threshold_uncertainty_score":0.9375048,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2775016911","doi":"10.1130/abs/2017am-298728","title":"A REVERSE ENERGY CASCADE FOR CRUSTAL MAGMA TRANSPORT","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of British Columbia","funders":"","keywords":"Cascade; Geology; Magma; Petrology; Energy (signal processing); Magma chamber; Geochemistry; Volcano; Physics; Chemistry","retraction":null,"screen_n_in":null,"score":{"opus":0.01961017870628281,"gpt":0.225742032443107,"spread":0.2061318537368242,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001924356,0.0002547235,0.0005125728,0.00001222095,0.0004772845,0.00004855431,0.0005505639,0.0002100427,0.002015189],"category_scores_gemma":[0.00006650864,0.0001499825,0.0005056107,0.0001265411,0.001627717,0.0001739022,0.00002710886,0.0002176222,0.00002105834],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003348261,"about_ca_system_score_gemma":0.00003389213,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.02110331,"about_ca_topic_score_gemma":0.001154338,"domain_scores_codex":[0.9981466,0.00002150176,0.0003833814,0.0004986495,0.0003297857,0.0006200694],"domain_scores_gemma":[0.9986215,0.0001525447,0.0004608146,0.0003615537,0.000130346,0.0002731967],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004663722,0.0004591216,0.6336512,0.00008973425,0.000358541,0.00004548419,0.0001587556,0.001690002,0.0001268844,0.00008316885,0.001339681,0.361531],"study_design_scores_gemma":[0.0008638604,0.002065977,0.9151278,0.00003072631,0.0001775387,0.00001981474,0.0004649819,0.002971385,0.0004964331,0.006486876,0.07081839,0.00047629],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.984197,0.000190685,0.002555464,0.004983662,0.000048881,0.0003704311,0.00007961159,0.00009999565,0.007474322],"genre_scores_gemma":[0.9640665,0.0001013149,0.03408895,0.0009872578,0.00008574133,0.00001608254,0.0002526223,0.000003804677,0.0003977384],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.3610547,"threshold_uncertainty_score":0.9988971,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W3097883074","doi":"10.1130/abs/2020am-354282","title":"FLUORINE PARTITIONING BETWEEN QUADRILATERAL CLINOPYROXENES AND MELT","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Inorganic Fluorides and Related Compounds","field":"Chemistry","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false},"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Norges Forskningsråd","keywords":"Quadrilateral; Computer science; Materials science; Engineering; Finite element method; Structural engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.02265326728805005,"gpt":0.2403462122283259,"spread":0.2176929449402759,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007914298,0.0002411569,0.0004445164,0.00000557647,0.0001711528,0.00004826931,0.0001819587,0.00025287,0.00032954],"category_scores_gemma":[0.00002210979,0.0001674032,0.0001534426,0.0001898567,0.0006859138,0.00009609054,0.0001209906,0.0005089188,0.00001534361],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001560782,"about_ca_system_score_gemma":0.0000288223,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0002072025,"about_ca_topic_score_gemma":6.685518e-7,"domain_scores_codex":[0.9984498,0.00001439528,0.0004448358,0.0004073123,0.0002560074,0.0004276436],"domain_scores_gemma":[0.9991287,0.0001050228,0.0002813816,0.0001527795,0.00008452321,0.0002476057],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0004742977,0.0008703755,0.6687742,0.001209084,0.002053057,0.0001072485,0.006228794,0.00102232,0.0376097,0.0001857871,0.002046451,0.2794187],"study_design_scores_gemma":[0.01333914,0.01578916,0.2852538,0.001305891,0.002054968,0.0002939597,0.01548818,0.01323538,0.2333817,0.002787031,0.411195,0.005875822],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9941463,0.0002632929,0.0001850131,0.003442455,0.0000173737,0.0001041502,0.000005404792,0.0002125008,0.001623434],"genre_scores_gemma":[0.984566,0.000171294,0.01433424,0.0004833289,0.0002500037,0.00001380303,0.00007470374,0.00001996045,0.00008668771],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4091485,"threshold_uncertainty_score":0.6826503,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2948456801","doi":"10.1130/abs/2019sc-326944","title":"MODELING AND UNDERSTANDING GROUNDWATER CONTAMINATION CAUSED BY CYANOTOXINS FROM HARMFUL ALGAL BLOOMS IN LAKE ERIE","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Environmental science; Algal bloom; Contamination; Groundwater contamination; Groundwater; Water resource management; Ecology; Geology; Aquifer; Biology; Geotechnical engineering; Phytoplankton; Nutrient","retraction":null,"screen_n_in":null,"score":{"opus":0.02793239807609467,"gpt":0.2179624525046944,"spread":0.1900300544285997,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000161555,0.0001886302,0.0003162973,0.000005777053,0.00008991533,0.00004851135,0.0001272149,0.0001835964,0.0003846604],"category_scores_gemma":[0.00000512102,0.00007633276,0.00009083341,0.0001974462,0.0002476125,0.0001666461,0.00003242041,0.0002217594,0.000006921916],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00003022406,"about_ca_system_score_gemma":0.000006467444,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.001835712,"about_ca_topic_score_gemma":0.002024464,"domain_scores_codex":[0.9986042,0.0000357205,0.0003201148,0.0003991995,0.0002959731,0.0003447453],"domain_scores_gemma":[0.9995628,0.0001216223,0.0001215626,0.00005109548,0.00003903651,0.0001038778],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002995287,0.001639789,0.9032379,0.00004953041,0.0001407252,0.00001367232,0.002177357,0.0009659815,0.04398071,0.00005541759,0.0001789459,0.04726048],"study_design_scores_gemma":[0.00348296,0.004919822,0.9295559,0.0002695196,0.00008342297,0.000004801212,0.02237632,0.02613953,0.001906815,0.0007939401,0.009387686,0.001079312],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9978136,0.00006469426,0.0003193642,0.001095568,0.00002790243,0.000427223,0.0000265715,0.00006711104,0.0001578938],"genre_scores_gemma":[0.9981102,0.00009558187,0.0007014088,0.000543848,0.00002189338,0.00002194473,0.0004574481,0.000002024475,0.00004563409],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.04618117,"threshold_uncertainty_score":0.4211761,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2983480299","doi":"10.1130/abs/2019am-339107","title":"CONODONT BIOSTRATIGRAPHY OF THE MIDDLE ORDOVICIAN (DARRIWILIAN) SUCCESSION AT WEST BAY CENTRE PICCADILLY HEAD QUARRY, PORT AU PORT PENINSULA, NEWFOUNDLAND","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Marine and environmental studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Conodont; Ordovician; Biostratigraphy; Peninsula; Geology; Port (circuit theory); Ecological succession; Bay; Paleontology; Harbour; Head (geology); Oceanography; Archaeology; Geography; Biology; Ecology","retraction":null,"screen_n_in":null,"score":{"opus":0.01585632781221404,"gpt":0.2054956131024007,"spread":0.1896392852901866,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002090453,0.0002778664,0.0004888484,0.00001360035,0.0002843311,0.00002131798,0.000342597,0.0001454716,0.002209884],"category_scores_gemma":[0.00001087891,0.0001479703,0.0002911278,0.0002715238,0.001247185,0.0001323628,0.0000880981,0.0002416965,0.00007218844],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001912011,"about_ca_system_score_gemma":0.0000570308,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.05701571,"about_ca_topic_score_gemma":0.02992445,"domain_scores_codex":[0.9979823,0.00005636329,0.0005082265,0.000418902,0.0005066161,0.0005276523],"domain_scores_gemma":[0.9988272,0.0001086303,0.0005465928,0.0003073355,0.00003869731,0.0001715594],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00009177469,0.0002024249,0.9809935,0.000059463,0.00009511061,0.000004062627,0.0005086569,0.0004139485,0.0000325495,0.000001993618,0.0001637969,0.0174327],"study_design_scores_gemma":[0.000478391,0.001093899,0.9761369,0.00006266305,0.00003662484,0.00001083621,0.001969349,0.0001665773,0.00003836985,0.00002478301,0.01976529,0.0002162818],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9834929,0.0002471395,0.000003695877,0.001614128,0.00009507476,0.0005573429,0.00003024127,0.00003025074,0.01392921],"genre_scores_gemma":[0.9971557,0.0001486656,0.001372966,0.0005300117,0.0000375086,0.000002712009,0.0001456107,0.000005473657,0.0006013889],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.02709125,"threshold_uncertainty_score":0.9987022,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2902715524","doi":"10.1130/abs/2018am-317521","title":"INVESTIGATING THE SUBSURFACE HETEROGENEITY OF A NATURALLY FRACTURED RESERVOIR IN RELATION TO CO<sub>2</sub> GEOLOGICAL STORAGE AT THE KEVIN DOME SITE, MONTANA","year":2018,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Schlumberger (Canada)","funders":"","keywords":"Dome (geology); Geology; Relation (database); Petrology; Geomorphology; Earth science","retraction":null,"screen_n_in":null,"score":{"opus":0.0201244053328997,"gpt":0.2674964923342204,"spread":0.2473720870013207,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0007897773,0.0002541405,0.0003323319,0.00001566063,0.0004150091,0.00003275379,0.0004402537,0.0002389672,0.0004247884],"category_scores_gemma":[0.0003315521,0.0001301793,0.000169581,0.000697681,0.003093773,0.0001895459,0.0003235381,0.0006467624,0.0001068133],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001656903,"about_ca_system_score_gemma":0.00002880177,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.002179279,"about_ca_topic_score_gemma":0.00363067,"domain_scores_codex":[0.9976014,0.0002579304,0.0006017355,0.0004949619,0.0005680952,0.0004758374],"domain_scores_gemma":[0.9982732,0.0005014231,0.0005682571,0.0004283591,0.00008921413,0.0001395825],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0004703751,0.0009104033,0.7420108,0.00003033855,0.0001271392,0.00001699989,0.00965097,0.09957096,0.1282375,0.00003728478,0.005261613,0.01367564],"study_design_scores_gemma":[0.0002915499,0.001353996,0.9806842,0.00003405996,0.00001914425,0.00001900793,0.0006766969,0.001873975,0.009379188,0.0002263193,0.005230994,0.0002108838],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9902337,0.00004815769,0.0002167546,0.00733647,0.00003645646,0.0008910208,0.000006361416,0.00005550526,0.001175588],"genre_scores_gemma":[0.9914556,0.00002412152,0.006149426,0.002147869,0.0000323721,0.00006795742,0.00003491625,0.000009100714,0.00007868938],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2386734,"threshold_uncertainty_score":0.9996192,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2773320807","doi":"10.1130/abs/2017am-302947","title":"CYCLOSTRATIGRAPHY OF THE UPPER ORDOVICIAN VAURÉAL FORMATION, ANTICOSTI ISLAND, EASTERN CANADA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Cyclostratigraphy; Ordovician; Geology; Paleontology; Sedimentary rock","retraction":null,"screen_n_in":null,"score":{"opus":0.01812454037881857,"gpt":0.2330905010460652,"spread":0.2149659606672467,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002052991,0.0001562033,0.0003070923,0.00001139448,0.0006084931,0.00003242727,0.0006794794,0.0001494663,0.00032173],"category_scores_gemma":[0.0000668291,0.00008344567,0.0001437083,0.000133952,0.002163189,0.0001645615,0.00004226678,0.0003606485,0.00001159345],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000001313397,"about_ca_system_score_gemma":0.0001996596,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.2401598,"about_ca_topic_score_gemma":0.5020418,"domain_scores_codex":[0.9985584,0.00007741328,0.0003244979,0.000214889,0.000372845,0.0004519365],"domain_scores_gemma":[0.9986621,0.0001560065,0.0005209332,0.0004165412,0.0001353465,0.0001091405],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00004597775,0.00005112534,0.9913203,0.00003943791,0.00006358874,0.000005415402,0.0001506721,0.0001950086,0.000001977444,0.000007013448,0.0002998177,0.007819655],"study_design_scores_gemma":[0.000277845,0.0003869841,0.9948978,0.00002982575,0.00002240408,0.00002737842,0.0004933083,0.0006586673,0.00005675662,0.0001815421,0.002854958,0.000112467],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9889715,0.0001265738,0.00003583757,0.00361704,0.00007250164,0.0003061466,0.00002590396,0.00001168974,0.006832784],"genre_scores_gemma":[0.9975227,0.0000516181,0.001877699,0.0004008446,0.00002152866,0.000003056469,0.00004537977,0.000001971688,0.0000751728],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.261882,"threshold_uncertainty_score":0.7970358,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2795876842","doi":"10.1130/abs/2018ne-311018","title":"RISE OF THE GREEN ALGAE: ALGAL PALYNOMORPHS RECORD THE HISTORY OF WALDEN POND","year":2018,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"American Environmental and Regional History","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"Brock University","funders":"","keywords":"Algae; Green algae; Ecology; Geology; Environmental science; Oceanography; Biology","retraction":null,"screen_n_in":null,"score":{"opus":0.01437974675823655,"gpt":0.2025054726858214,"spread":0.1881257259275848,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000225365,0.0002070799,0.0003444804,0.000006410184,0.0001334925,0.000001611486,0.0006701776,0.000111428,0.001531741],"category_scores_gemma":[0.00001400983,0.00009913174,0.0003087066,0.0002292214,0.03301585,0.00007328788,0.000350017,0.0002678011,0.00005090768],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0002341192,"about_ca_system_score_gemma":0.00004497065,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.007663332,"about_ca_topic_score_gemma":0.00006169089,"domain_scores_codex":[0.9982157,0.00009726928,0.0004197415,0.0003339654,0.0006058821,0.0003274114],"domain_scores_gemma":[0.9984997,0.0001076648,0.0008268208,0.0004455204,0.00002328773,0.00009701468],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"not_applicable","study_design_scores_codex":[0.0006847725,0.003501892,0.3866232,0.0001159514,0.0005142163,0.00001070158,0.01903065,0.0008279691,0.01285311,0.00002855363,0.1482945,0.4275145],"study_design_scores_gemma":[0.0003568344,0.002032614,0.463418,0.00003618666,0.00008118385,0.00001640144,0.002283987,0.0001922195,0.0003599797,0.0001040436,0.5308759,0.0002426231],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9824419,0.0003461041,0.0001294306,0.002265831,0.0001500066,0.0005768033,0.00000723976,0.00002864899,0.01405405],"genre_scores_gemma":[0.9867203,0.00008513442,0.007404004,0.0008704493,0.00004690082,0.00002518566,0.000004235468,0.00001440442,0.004829435],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4272719,"threshold_uncertainty_score":0.999381,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2775285302","doi":"10.1130/abs/2017am-302390","title":"EARLY MIOCENE VEGETATION ACROSS EASTERN AFRICA AS RECONSTRUCTED FROM PHYTOLITH DATA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"African Botany and Ecology Studies","field":"Agricultural and Biological Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Calgary","funders":"","keywords":"Phytolith; Vegetation (pathology); Geology; Paleontology; Late Miocene; Geography; Physical geography; Remote sensing; Ecology","retraction":null,"screen_n_in":null,"score":{"opus":0.05318856407570471,"gpt":0.2714022647846647,"spread":0.21821370070896,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002324667,0.0002806059,0.0005194939,0.000002445,0.001074079,0.0001538755,0.001192067,0.000241018,0.0001342002],"category_scores_gemma":[0.0001517116,0.0001098518,0.0001488563,0.0001476874,0.002326842,0.0004250637,0.0006188033,0.0002874179,0.00006807417],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001724395,"about_ca_system_score_gemma":0.0000167355,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.004777899,"about_ca_topic_score_gemma":0.0004871191,"domain_scores_codex":[0.9978393,0.00005895565,0.000401127,0.0007287537,0.0003053835,0.0006664245],"domain_scores_gemma":[0.9981051,0.000295248,0.0008590204,0.0004132437,0.000160144,0.0001672382],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001609425,0.0004103387,0.5522109,0.00001087367,0.0003011176,0.00001553773,0.001096654,0.000005339728,0.001093744,0.000004270896,0.0002658729,0.4444244],"study_design_scores_gemma":[0.0003390931,0.001286046,0.9840648,0.00004236232,0.00004940724,0.000006000735,0.00331747,0.000109617,0.00008468412,0.0005077097,0.009914421,0.0002783633],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9950488,0.0002394018,0.00001238423,0.002290271,0.00007236164,0.0003371864,0.00009926292,0.0001104656,0.001789906],"genre_scores_gemma":[0.9924982,0.000107791,0.006599989,0.0002374015,0.0001716215,0.00003328675,0.0001866043,0.000002382416,0.0001626811],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.444146,"threshold_uncertainty_score":0.8573347,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2317081482","doi":"10.1130/abs/2016ne-271964","title":"ORGANIC-WALLED MICROFOSSILS FROM THE EDIACARAN-CAMBRIAN GLOBAL BOUNDARY STRATOTYPE SECTION, CHAPEL ISLAND, RANDOM, AND BRIGUS FORMATIONS,  SOUTHEASTERN NEWFOUNDLAND, CANADA","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Stratotype; Section (typography); Geology; Paleontology; Boundary (topology); Chapel; Archaeology; Geography; History","retraction":null,"screen_n_in":null,"score":{"opus":0.008718116836304331,"gpt":0.1939050721244821,"spread":0.1851869552881778,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002190014,0.0002306059,0.0003314109,0.000006515652,0.0004909695,0.0001242865,0.0002672368,0.0001419015,0.001113245],"category_scores_gemma":[0.00005584173,0.0001012077,0.00008847742,0.0002683005,0.0007586399,0.0002822011,0.00002599181,0.0001878733,0.00003033881],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001249136,"about_ca_system_score_gemma":0.0002931655,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.4447762,"about_ca_topic_score_gemma":0.5753021,"domain_scores_codex":[0.9984163,0.00007772744,0.0004214877,0.0002908179,0.0003516762,0.0004420113],"domain_scores_gemma":[0.9987578,0.0004221896,0.0003123996,0.0001796369,0.0001473572,0.0001805502],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002386881,0.00004091715,0.8778795,0.00001856035,0.0001092973,0.000002673738,0.0003003388,0.00004860969,0.00001046665,0.000005694664,0.0006578522,0.1206874],"study_design_scores_gemma":[0.00147937,0.0004824861,0.9555668,0.00003864423,0.00004849917,0.00004032346,0.001698068,0.0001820229,0.000006026405,0.0006511366,0.03957811,0.000228566],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9905664,0.001127704,0.001924232,0.004490961,0.0001280904,0.0004291478,0.0002902121,0.00005143035,0.0009918748],"genre_scores_gemma":[0.9966062,0.0003413993,0.001771747,0.0009023478,0.0001338988,0.000006826082,0.0001700484,0.000002950557,0.00006456536],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1305259,"threshold_uncertainty_score":0.9997998,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4225563118","doi":"10.1130/abs/2022ne-374511","title":"CONTRASTS IN CRUSTAL CHARACTER BETWEEN MEGUMA AND AVALONIA BASED ON WIDE-ANGLE SEISMIC REFLECTION/REFRACTION PROFILES ALONG THE SCOTIAN MARGIN AND ACROSS NOVA SCOTIA, CANADA","year":2022,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"Acadia University","funders":"","keywords":"Nova scotia; Margin (machine learning); Geology; Seismology; Reflection (computer programming); Refraction; Nova (rocket); Character (mathematics); Optics; Geometry; Physics; Computer science; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.02068740829639273,"gpt":0.2530719072074347,"spread":0.232384498911042,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007831089,0.0002018421,0.0003612758,0.00002650785,0.0005641446,0.00003827286,0.0001834131,0.0001306081,0.0004036407],"category_scores_gemma":[0.00005466077,0.0001284351,0.00005007961,0.000329954,0.001110161,0.0001056202,0.0000463184,0.000928684,0.000005847944],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001301453,"about_ca_system_score_gemma":0.000191288,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.4305387,"about_ca_topic_score_gemma":0.4233124,"domain_scores_codex":[0.9979356,0.0003345257,0.0003049488,0.0004249822,0.0003893125,0.0006106379],"domain_scores_gemma":[0.9985625,0.0008876958,0.0002241295,0.0001524025,0.00004481749,0.0001284469],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0002720955,0.00005885904,0.982984,0.00003175846,0.00004474677,0.00003160168,0.0003068257,0.002687929,0.000002592841,3.376658e-7,0.0001760172,0.01340326],"study_design_scores_gemma":[0.0006419917,0.001623125,0.9915162,0.00001808137,0.00001449683,0.00005468427,0.0016342,0.00294655,0.00002698044,0.00001807116,0.001349737,0.0001558601],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9914656,0.0001454368,0.00001441235,0.007418185,0.00006853205,0.0006056498,0.00004916856,0.00002244406,0.00021055],"genre_scores_gemma":[0.9979602,0.000014293,0.000408142,0.001308152,0.00002599147,0.00001696955,0.0002114687,0.000004531224,0.00005025654],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0132474,"threshold_uncertainty_score":0.5872106,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2532720753","doi":"10.1130/abs/2016am-285506","title":"PORTABLE X-RAY FLUORESCENCE TRACE METAL MEASUREMENT IN ORGANIC RICH SOILS: PXRF RESPONSE AS A FUNCTION OF ORGANIC MATTER FRACTION","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Soil water; TRACE (psycholinguistics); Fraction (chemistry); Organic matter; Trace metal; Fluorescence; Environmental chemistry; Metal; Analytical Chemistry (journal); Materials science; Chemistry; Environmental science; Soil science; Physics; Chromatography; Metallurgy; Optics","retraction":null,"screen_n_in":null,"score":{"opus":0.01880355668716101,"gpt":0.2235658068341378,"spread":0.2047622501469768,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001502524,0.0002888387,0.0004997516,0.00004146184,0.0001021829,0.00003295809,0.0005805769,0.0002406271,0.0007985242],"category_scores_gemma":[0.0004139643,0.0001800937,0.0001649872,0.0008837841,0.0005074978,0.0004396411,0.0001758368,0.0003298496,0.0000810786],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0001125544,"about_ca_system_score_gemma":0.0001807684,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0001412048,"about_ca_topic_score_gemma":0.00001124966,"domain_scores_codex":[0.99708,0.0001985157,0.000670832,0.0006868425,0.0007735525,0.0005902972],"domain_scores_gemma":[0.9978046,0.0003143879,0.0007201722,0.0005498728,0.000478319,0.0001326636],"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":[0.002175141,0.004396892,0.1093357,0.0003520905,0.0005240418,0.00006834595,0.001958028,0.0007757949,0.7036225,0.00008507708,0.001840611,0.1748658],"study_design_scores_gemma":[0.002714046,0.006580805,0.9215997,0.0005014539,0.0001239496,0.00009293263,0.001963873,0.0007125221,0.04046961,0.002829128,0.02138495,0.001027042],"study_design_candidate":"observational","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9228466,0.0001505336,0.06462055,0.01066987,0.00007311419,0.000569026,0.000001082316,0.0001614935,0.0009077739],"genre_scores_gemma":[0.9732163,0.00003382662,0.02603197,0.0002717303,0.00002215825,0.00004981598,0.000002549305,0.000007085744,0.0003645974],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.812264,"threshold_uncertainty_score":0.8743281,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2771819684","doi":"10.1130/abs/2017am-304912","title":"STUDENT PERSPECTIVES ON WIRELESS COMMUNICATION TECHNOLOGIES TO FACILITATE INCLUSION IN FIELD ACTIVITIES","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Mobile Learning in Education","field":"Computer Science","cited_by":2,"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":"Wireless; Field (mathematics); Inclusion (mineral); Computer science; Telecommunications; Psychology; Mathematics","retraction":null,"screen_n_in":null,"score":{"opus":0.02937631188406938,"gpt":0.3047432869106693,"spread":0.2753669750266,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003997598,0.000168919,0.0002639573,0.00004351744,0.0006011318,0.0001602985,0.001998541,0.0001413707,0.000005307458],"category_scores_gemma":[0.0001908505,0.0001255634,0.00006535263,0.0002025805,0.0006527001,0.0003487068,0.002398608,0.000474491,0.000009989176],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00009800337,"about_ca_system_score_gemma":0.00004035846,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0008896762,"about_ca_topic_score_gemma":0.0000335147,"domain_scores_codex":[0.9985204,0.00007944825,0.0002454661,0.000444936,0.0004041212,0.0003056687],"domain_scores_gemma":[0.9979582,0.0003473402,0.0003941472,0.001153504,0.00009803143,0.00004870507],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.00004853722,0.001231866,0.02761339,0.00002510702,0.00003365909,0.000002903235,0.06223191,0.001553419,0.0002074715,0.0008207597,0.0001843134,0.9060467],"study_design_scores_gemma":[0.001090445,0.01057568,0.8342657,0.0006192856,0.00001557546,0.000007466007,0.1313396,0.003381777,0.004536558,0.005664022,0.007576413,0.0009274893],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9650524,0.00007807503,0.008186014,0.02404969,0.00003577469,0.0005883044,4.708968e-7,0.0002503086,0.001758925],"genre_scores_gemma":[0.924786,0.000156687,0.07455011,0.0002537919,0.000007881221,0.0001700709,0.000002088348,0.000005137526,0.00006827513],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.9051192,"threshold_uncertainty_score":0.5120327,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2807965184","doi":"10.1130/abs/2018am-324347","title":"U-PB AND HF ISOTOPIC ANALYSIS OF DETRITAL ZIRCONS FROM PALEOZOIC AND CRETACEOUS STRATA OF SOUTHERN VANCOUVER ISLAND, BRITISH COLUMBIA","year":2018,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"National Science Foundation","keywords":"Paleozoic; Geology; Cretaceous; Paleontology; Zircon; Oceanography; Seismology; Geochemistry","retraction":null,"screen_n_in":null,"score":{"opus":0.01323891431471212,"gpt":0.198664642094762,"spread":0.1854257277800499,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001286303,0.0001209093,0.0005323877,0.00001278406,0.0001467455,0.00005052941,0.0001147366,0.0001332061,0.001201396],"category_scores_gemma":[0.0000385778,0.0001015393,0.0001240995,0.0004064569,0.001972198,0.0000812058,0.00003686717,0.0001216819,0.000003212433],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00000153349,"about_ca_system_score_gemma":0.00001369881,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.1245949,"about_ca_topic_score_gemma":0.3048587,"domain_scores_codex":[0.9987631,0.00004055333,0.0003708612,0.0003289623,0.0002346855,0.0002618791],"domain_scores_gemma":[0.999099,0.000197013,0.0003468998,0.0001235689,0.0001311802,0.000102359],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003347221,0.00008790046,0.9025648,0.00001886234,0.0004629311,0.000003359683,0.0005341842,0.0001007103,0.0000204806,1.396844e-7,0.0002599004,0.09591321],"study_design_scores_gemma":[0.0003614949,0.002266086,0.9898557,0.0000210196,0.0003223543,0.000002187769,0.004551209,0.001138546,0.00001218163,0.0002714873,0.001051462,0.0001462591],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9979008,0.0007603266,0.0003336684,0.00006962847,0.00002249726,0.000208183,0.0002467646,0.00001763744,0.0004404823],"genre_scores_gemma":[0.9895668,0.0003952098,0.009742326,0.00008705974,0.00003009739,0.000002502353,0.0001252371,0.0000020248,0.00004874184],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.1802638,"threshold_uncertainty_score":0.9997116,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2771917210","doi":"10.1130/abs/2017am-300972","title":"ASTRONOMICAL TUNING OF THE EARLY TRIASSIC INDUAN STAGE IN THE DISTAL MONTNEY FORMATION, NE BRITISH COLUMBIA, CANADA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Stage (stratigraphy); Geology; Paleontology; Computer science; Remote sensing","retraction":null,"screen_n_in":null,"score":{"opus":0.02179682581269316,"gpt":0.2271840230775182,"spread":0.2053871972648251,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005430207,0.00009855685,0.0002906385,0.000005204155,0.0005935399,0.0001284109,0.0008210278,0.0001355869,0.0002344194],"category_scores_gemma":[0.0001217361,0.00006790061,0.0001006228,0.000121707,0.002225899,0.0001817217,0.00005405459,0.0005741828,0.000002471884],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003980251,"about_ca_system_score_gemma":0.0002220877,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_topic_score_codex":0.8856778,"about_ca_topic_score_gemma":0.951403,"domain_scores_codex":[0.9984741,0.0001862327,0.0003538237,0.0002006849,0.0003328059,0.0004523347],"domain_scores_gemma":[0.9987575,0.0003062603,0.0004673666,0.0003285036,0.00006179258,0.00007856535],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.00003239856,0.00005768964,0.9870772,0.00001683057,0.00002574457,0.000009942108,0.0002980914,0.0002958636,6.500202e-7,0.000001497048,0.0002441269,0.01194002],"study_design_scores_gemma":[0.0004436564,0.000371575,0.995978,0.00002574832,0.00001027355,0.00001817739,0.001601984,0.0005191551,0.000002911187,0.00005657297,0.0008871311,0.00008484277],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9965199,0.00005918869,0.00001353416,0.001668649,0.0000389915,0.0004093754,0.00003115428,0.000007053134,0.00125215],"genre_scores_gemma":[0.9988422,0.0000127697,0.0007745223,0.000163036,0.00001663055,0.000008622614,0.00004664496,0.000001822534,0.0001337511],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.0657253,"threshold_uncertainty_score":0.8201419,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W4389353408","doi":"10.1130/abs/2023am-391318","title":"ENVIRONMENTAL RISKS AND OPPORTUNITIES OF ORPHANED OIL AND GAS WELLS IN THE UNITED STATES","year":2023,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Oil, Gas, and Environmental Issues","field":"Energy","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"McGill University","funders":"","keywords":"Fossil fuel; Environmental science; Petroleum engineering; Waste management; Geology; Engineering","retraction":null,"screen_n_in":null,"score":{"opus":0.04723541021743993,"gpt":0.2524679006971592,"spread":0.2052324904797193,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002432669,0.0001842585,0.0002974096,0.00002822895,0.00007957371,0.00001920462,0.0001331317,0.000105257,0.00008667591],"category_scores_gemma":[0.00000767354,0.0001128362,0.00005951617,0.0001777228,0.002211659,0.00007530882,0.00009785789,0.0001779477,0.000007536005],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001169682,"about_ca_system_score_gemma":0.00000469616,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.006871704,"about_ca_topic_score_gemma":0.00002252334,"domain_scores_codex":[0.9988149,0.00008427542,0.0002914783,0.0002346943,0.0002552106,0.0003194275],"domain_scores_gemma":[0.9993562,0.0002235175,0.0001883781,0.0001477398,0.000006205434,0.00007793395],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"design_other","study_design_gemma":"observational","study_design_scores_codex":[0.0002350753,0.001247722,0.09309818,0.0002393618,0.0002732153,0.00009253649,0.02025385,0.00521548,0.0009795885,0.0000992401,0.0005716312,0.8776941],"study_design_scores_gemma":[0.001812476,0.003490763,0.7032,0.0001151669,0.0001193555,0.00003782484,0.1439003,0.001676989,0.001041531,0.001409342,0.1426222,0.0005739504],"study_design_candidate":"design_other","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9968761,0.0003512804,0.000001723451,0.001874322,0.000008023495,0.00009083229,0.00001139727,0.00004294575,0.0007433683],"genre_scores_gemma":[0.9786118,0.01923964,0.001066764,0.0006332346,0.00001314433,0.00002861067,0.0001948052,0.0000128654,0.0001991819],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.8771202,"threshold_uncertainty_score":0.9997416,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2766952440","doi":"10.1130/abs/2017am-305666","title":"THE AMORPHOUS COMPOSITION OF THREE MUDSTONE SAMPLES FROM GALE CRATER: IMPLICATIONS FOR WEATHERING AND DIAGENETIC PROCESSES ON MARS","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"routes":{"ca_aff":true,"ca_fund":false,"ca_venue":false,"about_ca":false},"ca_institutions":"University of Guelph; University of New Brunswick","funders":"","keywords":"Diagenesis; Impact crater; Weathering; Mars Exploration Program; Geology; Astrobiology; Geochemistry; Composition (language); Art","retraction":null,"screen_n_in":null,"score":{"opus":0.03697683486128975,"gpt":0.2600825460298559,"spread":0.2231057111685661,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006951641,0.00009200954,0.0001449882,0.000003574663,0.000499058,0.00007203208,0.0001849587,0.00002743033,0.0000051313],"category_scores_gemma":[0.000007327382,0.00005466414,0.0000454621,0.0000380985,0.0006739287,0.0001187047,0.00002823103,0.000059305,0.000001672361],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000003253215,"about_ca_system_score_gemma":0.00001984985,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0009367949,"about_ca_topic_score_gemma":0.00003831888,"domain_scores_codex":[0.9994195,0.000007470255,0.0001556887,0.0001756635,0.00008254699,0.0001590915],"domain_scores_gemma":[0.9992149,0.0001783328,0.0003287261,0.0001734329,0.0000653246,0.00003923487],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0001211647,0.0003945062,0.764722,0.000044002,0.0001308312,1.674274e-7,0.0005932616,0.001474678,0.005075714,0.000145424,0.0001616847,0.2271366],"study_design_scores_gemma":[0.0002460701,0.000655019,0.9916757,0.0000325683,0.00003252443,3.262255e-7,0.0004623212,0.0003737163,0.001433369,0.004316146,0.0006729939,0.0000991921],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9904467,0.00006307385,0.007572293,0.001365788,0.000009249,0.0003774037,0.0000630224,0.00001223247,0.00009025281],"genre_scores_gemma":[0.985197,0.00005154254,0.01439309,0.00003414734,0.0000364406,0.00009093258,0.0001876796,0.000004130125,0.000005051551],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.2270374,"threshold_uncertainty_score":0.3838402,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null},{"id":"W2534124462","doi":"10.1130/abs/2016am-282298","title":"CHARACTERIZATION OF ARSENIC-HOSTING SOLID PHASES IN TAILINGS AND TAILINGS DUST FROM GIANT MINE, YELLOWKNIFE, NT","year":2016,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":2,"is_retracted":false,"has_abstract":false,"routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true},"ca_institutions":"","funders":"","keywords":"Tailings; Arsenic; Geology; Characterization (materials science); Mining engineering; Environmental science; Astrobiology; Metallurgy; Materials science","retraction":null,"screen_n_in":null,"score":{"opus":0.0161001007247444,"gpt":0.2307868373480879,"spread":0.2146867366233434,"validation_status":"score_only:v0-immature-baseline"},"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003017001,0.0002445107,0.0004912146,0.00002586639,0.00007355388,0.00003427216,0.0004195148,0.0001955028,0.00003766105],"category_scores_gemma":[0.0002421144,0.0001538659,0.0001139972,0.0003719854,0.0008884381,0.000296606,0.0001985959,0.0002024521,0.0000025688],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.00001749651,"about_ca_system_score_gemma":0.00005144493,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.0005784417,"about_ca_topic_score_gemma":0.000007586063,"domain_scores_codex":[0.9980143,0.00003684852,0.000624435,0.0005904174,0.000279388,0.0004546684],"domain_scores_gemma":[0.9982459,0.0003984044,0.0007191488,0.0003140231,0.0002015729,0.000120929],"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":[0.0001000662,0.0009354671,0.05990036,0.0001354982,0.0001052978,0.00003782874,0.002314446,0.0001496927,0.7208676,0.00007258268,0.00006833822,0.2153129],"study_design_scores_gemma":[0.007139552,0.006148189,0.5296766,0.002893887,0.0001362662,0.0001185828,0.004310421,0.02858667,0.3872339,0.004061294,0.02724196,0.002452754],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9807739,0.00005392706,0.01418034,0.004187318,0.00002666806,0.0002852686,0.00000552408,0.00009019931,0.0003968446],"genre_scores_gemma":[0.9286633,0.00007252913,0.07081583,0.0002201455,0.00003424034,0.00002277672,0.00002286041,0.000004345173,0.0001440245],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.4697762,"threshold_uncertainty_score":0.6274471,"prediction_status":"machine_predicted_unvalidated"},"labels":[],"label_agreement":null}]}