{"id":691,"date":"2016-09-29T16:05:37","date_gmt":"2016-09-29T21:05:37","guid":{"rendered":"https:\/\/www.jsg.utexas.edu\/science-yall\/?p=691"},"modified":"2016-10-04T09:51:36","modified_gmt":"2016-10-04T14:51:36","slug":"damn-it-feels-good-to-be-a-longhorn","status":"publish","type":"post","link":"https:\/\/www.jsg.utexas.edu\/science-yall\/damn-it-feels-good-to-be-a-longhorn\/","title":{"rendered":"It feels good to be a Longhorn"},"content":{"rendered":"<p>Summer at the Jackson School is a pretty unique time for graduate students. It is my first summer here as a Master\u2019s student and I\u2019ve started to notice the relative emptiness of the building after a busy school year. Most grad students make the most of the extra time that they have by doing field work, starting an internship, or sticking around Austin and doing research. Alongside an awesome field experience in California, sitting behind a computer comprised the bulk of my research. As disenchanting as that sounds, I\u2019ve been having a fun time.<\/p>\n<figure id=\"attachment_720\" aria-describedby=\"caption-attachment-720\" style=\"width: 575px\" class=\"wp-caption aligncenter\"><a href=\"https:\/\/www.jsg.utexas.edu\/science-yall\/files\/IMG_3168.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\" wp-image-720\" src=\"https:\/\/www.jsg.utexas.edu\/science-yall\/files\/IMG_3168-1024x508.jpg\" alt=\"Looking west from the summit of Empire Mountain in Sequoia National Park. The skarn I sampled is beneath my feet but this view is unbeatable.\" width=\"575\" height=\"292\" \/><\/a><figcaption id=\"caption-attachment-720\" class=\"wp-caption-text\">Looking west from the summit of Empire Mountain in Sequoia National Park. The skarn I sampled is beneath my feet but this view is unbeatable.<\/figcaption><\/figure>\n<p>A lot of what I do as a computational geoscientist is make pretty looking plots, making it seem as if I\u2019m doing stuff that\u2019s way more impressive than it actually is. For me, these plots deal with understanding how water flows and stable isotopes are transported in the shallow crust in response to a magmatic intrusion. The objective of my research is to determine the mechanisms, be it physical or chemical, that most control fluid flow and stable isotope transport during the formation of a particular type of rocks called skarns. The Sierra Nevada of California has some pretty spectacular exposures of skarns (see picture below) so I was lucky enough to go out there this summer to collect some rocks for analysis. Using facilities on campus, I\u2019m now measuring their stable isotope signatures in order to determine the fluid sources that were involved in the formation of these rocks. I find it so cool that I can use two totally different techniques \u2013 numerical modeling and analytical geochemistry \u2013 to address the same problems. I\u2019ve learned a lot in the process but it is great knowing that I\u2019m only scratching the surface.<\/p>\n<p>But honestly, I\u2019ve spent most of my time this summer trying to figure out how to efficiently get the coffee from the 2<sup>nd<\/sup> floor copy room of EPS to my 5<sup>th<\/sup> floor office in JGB without spilling it. As much as I love going to Pangea Cafe in JGB, I find myself more often than not making the trip to the 2<sup>nd<\/sup> floor of EPS for the free stuff. Fortunately, I recently moved offices to 3<sup>rd<\/sup> floor of EPS so now I only have one flight of stairs to battle on trips for my lifeblood. This may seem unimportant but I know there\u2019s at least one of you out there who can relate with me on this struggle.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Summer at the Jackson School is a pretty unique time for graduate students. It is my first summer here as a Master\u2019s student and I\u2019ve started to notice the relative emptiness of the building after a busy school year. Most grad students make the most of the extra time that&#8230;<\/p>\n","protected":false},"author":89,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":"","_links_to":"","_links_to_target":""},"categories":[7],"tags":[],"class_list":["post-691","post","type-post","status-publish","format-standard","hentry","category-summer-2016"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/posts\/691","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/users\/89"}],"replies":[{"embeddable":true,"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/comments?post=691"}],"version-history":[{"count":20,"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/posts\/691\/revisions"}],"predecessor-version":[{"id":1034,"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/posts\/691\/revisions\/1034"}],"wp:attachment":[{"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/media?parent=691"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/categories?post=691"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.jsg.utexas.edu\/science-yall\/wp-json\/wp\/v2\/tags?post=691"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}