{"id":296,"date":"2023-10-05T14:50:38","date_gmt":"2023-10-05T21:50:38","guid":{"rendered":"https:\/\/dornsife.usc.edu\/okaya\/?page_id=296"},"modified":"2024-02-08T14:37:57","modified_gmt":"2024-02-08T22:37:57","slug":"thermalmodeling","status":"publish","type":"page","link":"https:\/\/dornsife.usc.edu\/okaya\/research\/thermalmodeling\/","title":{"rendered":"Thermal Modeling and Plutons"},"content":{"rendered":"\n\n  \n    \n\n\n\n\n\n\n<div\n  class=\"cc--component-container cc--rich-text \"\n\n  \n  \n  \n  \n  \n  \n  >\n  <div class=\"c--component c--rich-text\"\n    \n      >\n\n    \n      \n<div class=\"f--field f--wysiwyg\">\n\n    \n  <h3 style=\"text-align: center;\">Thermal Modeling and Plutons<\/h3>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-full wp-image-297\" src=\"https:\/\/dornsife.usc.edu\/okaya\/wp-content\/uploads\/sites\/365\/2023\/10\/Screen-Shot-2023-10-05-at-2.49.39-PM.png\" alt=\"\" width=\"1134\" height=\"406\" srcset=\"https:\/\/dornsife.usc.edu\/okaya\/wp-content\/uploads\/sites\/365\/2023\/10\/Screen-Shot-2023-10-05-at-2.49.39-PM.png 1134w, https:\/\/dornsife.usc.edu\/okaya\/wp-content\/uploads\/sites\/365\/2023\/10\/Screen-Shot-2023-10-05-at-2.49.39-PM-300x107.png 300w, https:\/\/dornsife.usc.edu\/okaya\/wp-content\/uploads\/sites\/365\/2023\/10\/Screen-Shot-2023-10-05-at-2.49.39-PM-1024x367.png 1024w, https:\/\/dornsife.usc.edu\/okaya\/wp-content\/uploads\/sites\/365\/2023\/10\/Screen-Shot-2023-10-05-at-2.49.39-PM-768x275.png 768w\" sizes=\"(max-width: 1134px) 100vw, 1134px\" \/><\/p>\n<ul>\n<li>Ratschbacher, B.C., C.B. Keller, B. Schoene, S.R. Paterson, J.L. Anderson, D. Okaya, K. Putirka, and R. Lippoldt, 2018, A new workflow to assess emplacement duration and melt residence time of compositionally diverse magmas emplaced in a sub-volcanic reservoir, J. Petrology., p. 1-23, doi:10\/1093\/petrology\/egy079. <\/li>\n<li>Paterson, S.R., D. Okaya, V. Memeti, R. Economos, and R. Miller, 2011, Magma addition and flux calculations of incrementally constructed magma chambers in continental margin arcs: combined field, geochronologic, and thermal modeling studies, Geosphere, 7, 1439-1468.<\/li>\n<li>Memeti, V., S. Paterson, J. Matzel, R. Mundil., and D. Okaya, 2010, Magmatic lobes as &#8220;snapshots&#8221; of magma chamber growth and evolution in large, composite batholiths: An example from the Tuolumne intrusion, Sierra Nevada, California, Bull. Geol. Soc. Amer., 122, 1912-1931, doi:10.1130\/B30004.1.<\/li>\n<li>Albertz, M., S.R. Paterson, and D. Okaya, 2005, Fast strain rates during pluton emplacement: magmatically folded leucocratic dikes in aureoles of the Mount Stuart Batholith, Washington, and the Tuolumne Intrusive Suite, California, Bull. Geol. Soc. Amer, 117, 450-465.<\/li>\n<li>Yoshinobu, A., D. Okaya, and S. Paterson, 1998, Modeling the thermal evolution of fault-controlled magma emplacement models: implications for the solidification of plutons, J. Structural Geology, 20, 1205-1208.<\/li>\n<\/ul>\n\n\n\n<\/div>\n\n\n  <\/div><\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":332,"featured_media":0,"parent":164,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-content-detail.php","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-296","page","type-page","status-publish","hentry"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.1.1 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Thermal Modeling and Plutons - David Okaya<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/dornsife.usc.edu\/okaya\/research\/thermalmodeling\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Thermal Modeling and Plutons - 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