{"id":"W2127153226","doi":"10.1016/j.tecto.2009.06.010","title":"Deep-mantle contributions to the surface dynamics of the North American continent","year":2009,"lang":"en","type":"article","venue":"Tectonophysics","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":false,"ca_institutions":"Université du Québec à Montréal","funders":"Lawrence Livermore National Laboratory; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canadian Institute for Advanced Research; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Mantle (geology); Mantle convection; Lithosphere; Post-glacial rebound; Ocean surface topography; Hotspot (geology); Geophysics; Plate tectonics; Upwelling; Buoyancy; North American Plate; Convection; Isostasy; Seismology; Tectonics; Geodesy; Geomorphology; Glacial period; Oceanography; Meteorology; Mechanics","routes":{"ca_aff":true,"ca_fund":true,"ca_venue":false,"about_ca":false,"invisible_to_affiliation_only":false},"retraction":null,"screen":null,"direct_labels":[],"prediction":{"model_version":"metacan-v3-hybrid-931329e0061c","candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001654899,0.0003438413,0.0001914123,0.000931069,0.0007198313,0.0009470189,0.0002377173,0.00025861,0.002404233],"category_scores_gemma":[0.0007392171,0.0002519615,0.0002171871,0.001003428,0.0004293613,0.0006534667,0.001000157,0.0003417398,0.0001818245],"about_ca_system_candidate":false,"about_ca_system_consensus":false,"about_ca_system_score_codex":0.0009995183,"about_ca_system_score_gemma":0.0006256144,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_topic_score_codex":0.06440514,"about_ca_topic_score_gemma":0.1031935,"domain_scores_codex":[0.9999684,0.000005628966,0.000001948798,0.000008309066,0.00000600168,0.000009774333],"domain_scores_gemma":[0.9998518,0.00004701932,0.00001890715,0.00001293992,0.00004395709,0.0000252113],"domain_codex":null,"domain_gemma":null,"domain_candidate":null,"domain_consensus":null,"study_design_codex":"observational","study_design_gemma":"observational","study_design_scores_codex":[0.0003938659,0.00006160409,0.8402202,0.0002371719,0.0003047724,0.001003828,0.003876857,0.0207798,0.04152255,0.006636937,0.001940132,0.08302226],"study_design_scores_gemma":[0.000009015393,0.000007669812,0.9863911,0.00001873597,0.00006561443,0.0000727713,0.0006637904,0.005493441,0.0006807467,0.001058341,0.005529069,0.000009794873],"study_design_candidate":"observational","study_design_consensus":"observational","genre_codex":"empirical","genre_gemma":"empirical","genre_scores_codex":[0.9953869,0.0008481169,0.0001353146,0.0003434495,0.00001453042,0.000001285609,0.0002283651,0.00001257948,0.003029509],"genre_scores_gemma":[0.9979919,0.0007815981,0.0001155368,0.00003198253,0.00002045549,0.000002344626,0.0002084441,0.00001154019,0.0008362013],"genre_candidate":"empirical","genre_consensus":"empirical","teacher_disagreement_score":0.06440514,"threshold_uncertainty_score":0.1280605,"prediction_status":"machine_predicted_unvalidated"},"machine_scores":{"provisional":true,"baseline":true,"maturity_gate_passed":false,"score_opus":0.004077384801354111,"score_gpt":0.2047669881284422,"score_spread":0.2006896033270881,"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."}}