{"id":"W1585295534","doi":"10.4454/ofioliti.v30i2.277","title":"EXPERIMENTAL HYDROUS PARTIAL MELTING OF HARZBURGITE AT SHALLOW PRESSURES: IMPLICATIONS ON HYDROUS LATE-STAGE MAGMATIC PROCESSES WITHIN THE MANTLE/CRUST TRANSITION OF THE OCEANIC LITHOSPHERE","year":2005,"lang":"en","type":"article","venue":"Ofioliti","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"ca_institutions":"","funders":"","keywords":"Ophiolite; Geology; Partial melting; Geochemistry; Mantle (geology); Lithosphere; Oceanic crust; Solidus; Mid-ocean ridge; Peridotite; Crust; Mineral redox buffer; Petrology; Subduction; Tectonics","routes":{"ca_aff":false,"ca_fund":false,"ca_venue":false,"about_ca":true,"invisible_to_affiliation_only":true},"retraction":null,"screen":null,"direct_labels":[],"prediction":{"model_version":"codex-gemma-dda1882f352a","candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001628109,0.0001401394,0.0002122525,0.00001513293,0.0002117082,0.000017288,0.0003282887,0.00006073382,0.003101603],"category_scores_gemma":[0.00006385842,0.00007213846,0.000131951,0.0002290524,0.000201515,0.00009038212,0.00002544397,0.0001173127,0.00004683254],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.000006282269,"about_ca_system_score_gemma":0.00002686684,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.00081401,"about_ca_topic_score_gemma":0.001213666,"domain_scores_codex":[0.9988376,0.0000869285,0.0003648932,0.0002281477,0.0002598243,0.0002226176],"domain_scores_gemma":[0.9992189,0.0001883541,0.0002147756,0.0002685911,0.00004532511,0.00006398869],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","study_design_scores_codex":[0.0007940746,0.001433505,0.3269237,0.001166588,0.0005966271,0.00001427708,0.01435219,0.5836535,0.0596328,0.003385631,0.0006250789,0.007422062],"study_design_scores_gemma":[0.001059872,0.0005614774,0.2978552,0.0003232507,0.0003914301,0.00002477969,0.002034999,0.1275105,0.5621181,0.005278646,0.002189904,0.0006518172],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9916757,0.0009761017,0.00001069781,0.001095054,0.0000246963,0.0002094642,0.0001530039,0.00002081123,0.00583442],"genre_scores_gemma":[0.9989085,0.00001652421,0.00009134184,0.0003124801,0.00005485739,0.000006114445,0.0000544715,0.000003235135,0.0005524762],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.5024853,"threshold_uncertainty_score":0.9978097,"prediction_status":"machine_predicted_unvalidated"},"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.01423065569089699,"score_gpt":0.2123524745218198,"score_spread":0.1981218188309228,"validation_status":"score_only:v0-immature-baseline","note":"Baseline scores from an immature model (maturity gate not passed). Scores rank; they never assert a category."}}