{"id":28,"date":"2024-07-15T18:13:47","date_gmt":"2024-07-15T18:13:47","guid":{"rendered":"https:\/\/mupages.marshall.edu\/sites\/brinkroby\/?page_id=28"},"modified":"2024-08-06T19:31:17","modified_gmt":"2024-08-06T19:31:17","slug":"research","status":"publish","type":"page","link":"https:\/\/mupages.marshall.edu\/brinkroby\/research\/","title":{"rendered":"Research"},"content":{"rendered":"\n<div class=\"wp-block-genesis-blocks-gb-columns gb-layout-service-3 gb-layout-columns-1 gb-1-col-equal gb-columns-center alignfull\" style=\"padding-bottom:4%;padding-left:5%\"><div class=\"gb-layout-column-wrap gb-block-layout-column-gap-4 gb-is-responsive-column\" style=\"max-width:1200px\">\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column gb-is-vertically-aligned-center\"><div class=\"gb-block-layout-column-inner\">\n<h2 class=\"wp-block-heading\">The relationship between fluids and mountain-belt formation within the Sevier Fold-Thrust Belt, Wyoming<\/h2>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"263\" src=\"http:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/sevier-1-1024x263.jpg\" alt=\"\" class=\"wp-image-33\" srcset=\"https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/sevier-1-1024x263.jpg 1024w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/sevier-1-300x77.jpg 300w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/sevier-1-768x197.jpg 768w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/sevier-1.jpg 1440w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<p>Fluid migrations affect both orogenic evolution and the rheological, mechanical, and geochemical properties of rocks. I use O, C, H isotopes, fluid inclusion thermochronology, field mapping, and structural analysis to study (1) what drives fluid migration through and out of fold-thrust belts, (2) the origin of fluids, and (3) migration paths. The aim is to develop a robust model of the relationship between fluid migration and mountain-belt formation. Future research directions include determining the timing of major deformation events using U-Pb LA-ISPMS dating of calcite veins related to fluid migrations.<\/p>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-columns gb-layout-service-3 gb-layout-columns-2 gb-2-col-wideleft gb-has-custom-background-color gb-columns-center alignfull\" style=\"padding-top:4%;padding-right:5%;padding-bottom:4%;padding-left:5%;background-color:#f6f5f1\"><div class=\"gb-layout-column-wrap gb-block-layout-column-gap-4 gb-is-responsive-column\" style=\"max-width:1200px\">\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column\"><div class=\"gb-block-layout-column-inner\">\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"466\" src=\"https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_8197-1024x466.jpg\" alt=\"\" class=\"wp-image-32\" srcset=\"https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_8197-1024x466.jpg 1024w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_8197-300x136.jpg 300w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_8197-768x349.jpg 768w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_8197.jpg 1080w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column gb-is-vertically-aligned-center\"><div class=\"gb-block-layout-column-inner\">\n<h2 class=\"wp-block-heading\">Analog modeling of structural evolution<\/h2>\n\n\n\n<p>Current work, using sandbox or claybox models, focuses on the energy balance and deformation mechanisms of duplex formation in fold-thrust belts, characterizing the structural and geo-mechanical conditions under which duplexes form. Students who have worked on this project: Gage Williams \u201924.<\/p>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-columns gb-layout-service-3 gb-layout-columns-2 gb-2-col-wideleft gb-columns-center alignfull\" style=\"padding-top:4%;padding-right:5%;padding-bottom:4%;padding-left:5%\"><div class=\"gb-layout-column-wrap gb-block-layout-column-gap-4 gb-is-responsive-column\" style=\"max-width:1200px\">\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column gb-is-vertically-aligned-center\"><div class=\"gb-block-layout-column-inner\">\n<h2 class=\"wp-block-heading\">Determining structural controls on subsurface coal fires<\/h2>\n\n\n\n<p>The Centralia Mine subsurface coal fire acts as a case study to build an understanding of the propagation of subsurface coal fires; we use this understanding to develop new coal-fire mitigation techniques. Thousands of coal fires are currently burning around the world, producing not less than 3% of the world\u2019s estimated annual carbon dioxide emissions, in addition to being environmentally and socially devastating locally.<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column gb-is-vertically-aligned-center\"><div class=\"gb-block-layout-column-inner\">\n<figure class=\"wp-block-video\"><video height=\"600\" style=\"aspect-ratio: 500 \/ 600;\" width=\"500\" autoplay controls loop src=\"https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/centralia3.mp4\"><\/video><\/figure>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-columns gb-layout-service-3 gb-layout-columns-2 gb-2-col-wideleft gb-has-custom-background-color gb-columns-center alignfull\" style=\"padding-top:4%;padding-right:5%;padding-bottom:4%;padding-left:5%;background-color:#f6f5f1\"><div class=\"gb-layout-column-wrap gb-block-layout-column-gap-4 gb-is-responsive-column\" style=\"max-width:1200px\">\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column\"><div class=\"gb-block-layout-column-inner\">\n<p><\/p>\n\n\n\n<figure class=\"wp-block-image size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"768\" height=\"1024\" src=\"https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/08\/IMG_93742-768x1024.jpg\" alt=\"\" class=\"wp-image-102\" style=\"width:334px;height:auto\" srcset=\"https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/08\/IMG_93742-768x1024.jpg 768w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/08\/IMG_93742-225x300.jpg 225w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/08\/IMG_93742.jpg 1000w\" sizes=\"auto, (max-width: 768px) 100vw, 768px\" \/><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column gb-is-vertically-aligned-center\"><div class=\"gb-block-layout-column-inner\">\n<h2 class=\"wp-block-heading\">Thermal history of the Lackawanna Synclinorium<\/h2>\n\n\n\n<p>We are using mapping, fluid inclusion analysis, raman spectroscopy, SEM, and Cathodoluminescence to determine the thermal and burial history of the Lackawanna Synclinorium, with the goal of answering a long standing question of valley and ridge geology&#8211; how anthracite coals were produce during the Late Paleozoic Alleghanian orogeny. Kaylee Baker &#8217;26.<\/p>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-columns gb-layout-service-3 gb-layout-columns-2 gb-2-col-wideleft gb-columns-center alignfull\" style=\"padding-top:4%;padding-right:5%;padding-bottom:4%;padding-left:5%\"><div class=\"gb-layout-column-wrap gb-block-layout-column-gap-4 gb-is-responsive-column\" style=\"max-width:1200px\">\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column gb-is-vertically-aligned-center\"><div class=\"gb-block-layout-column-inner\">\n<h2 class=\"wp-block-heading\">Field mapping within the West Virginia Valley and Ridge<\/h2>\n\n\n\n<p>I work with undergraduate or master\u2019s degree students to map portions of the state of West Virginia.<\/p>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-genesis-blocks-gb-column gb-block-layout-column gb-is-vertically-aligned-center\"><div class=\"gb-block-layout-column-inner\">\n<figure class=\"wp-block-image size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"720\" height=\"765\" src=\"http:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_1903.jpg\" alt=\"\" class=\"wp-image-47\" srcset=\"https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_1903.jpg 720w, https:\/\/mupages.marshall.edu\/brinkroby\/wp-content\/uploads\/sites\/253\/2024\/07\/IMG_1903-282x300.jpg 282w\" sizes=\"auto, (max-width: 720px) 100vw, 720px\" \/><\/figure>\n<\/div><\/div>\n<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":247,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-28","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/pages\/28","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/users\/247"}],"replies":[{"embeddable":true,"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/comments?post=28"}],"version-history":[{"count":8,"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/pages\/28\/revisions"}],"predecessor-version":[{"id":105,"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/pages\/28\/revisions\/105"}],"wp:attachment":[{"href":"https:\/\/mupages.marshall.edu\/brinkroby\/wp-json\/wp\/v2\/media?parent=28"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}