{"id":1754,"date":"2017-10-19T20:19:52","date_gmt":"2017-10-20T01:19:52","guid":{"rendered":"https:\/\/www.csr.utexas.edu\/?p=1754"},"modified":"2020-08-31T17:23:29","modified_gmt":"2020-08-31T22:23:29","slug":"10-23-17-geodetic-constraints-on-subduction-zone-slip-in-alaska-as-a-function-of-space-and-time","status":"publish","type":"post","link":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/10-23-17-geodetic-constraints-on-subduction-zone-slip-in-alaska-as-a-function-of-space-and-time\/","title":{"rendered":"10-23-17 | Geodetic Constraints on Subduction Zone Slip in Alaska as a Function of Space and Time"},"content":{"rendered":"<h5><span style=\"color: #000080;\">Speaker<\/span><\/h5>\n<p><strong>Dr. Jeff Freymueller<\/strong><br \/>\n<em>Geophysics Geophysical Institute, University of Alaska, Fairbanks<\/em><\/p>\n<h5><span style=\"color: #000080;\">Time and Place<\/span><\/h5>\n<p><strong>October 23, 2017\u00a0\u2013 Monday\u00a0\u2013 2:00 PM<\/strong><br \/>\nWPR Building, Conference Room 2.806<br \/>\n3925 W. Braker Lane, Suite 200, Austin, Texas 78759<\/p>\n<p>Thrust earthquakes at subduction zones are the largest on Earth, and can have devastating consequences. We now recognize that the slip behavior of these important faults can be highly variable in both space and time. Precise space geodetic measurements are one of the best tools available to study and characterize these history of slip. The surface displacements due to slip are mixed together in geodetic time series with other signals: time-varying surface loading and volcanic deformation, and other components that are largely steady in time such as long-term deformation of the overriding plate, glacial isostatic adjustment, etc. Thus the study of subduction zone slip generally requires using a broad range of geodetic tools to isolate the desired signals.<\/p>\n<p>Coffee &amp; cookies will be served<br \/>\nFor further information, please contact 471-5573<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Speaker Dr. Jeff Freymueller Geophysics Geophysical Institute, University of Alaska, Fairbanks Time and Place October 23, 2017\u00a0\u2013 Monday\u00a0\u2013 2:00 PM WPR Building, Conference Room 2.806 3925 W. Braker Lane, Suite [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":[],"categories":[19],"tags":[],"_links":{"self":[{"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/posts\/1754"}],"collection":[{"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/comments?post=1754"}],"version-history":[{"count":2,"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/posts\/1754\/revisions"}],"predecessor-version":[{"id":1756,"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/posts\/1754\/revisions\/1756"}],"wp:attachment":[{"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/media?parent=1754"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/categories?post=1754"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/utw10640.utweb.utexas.edu\/wordpress\/wp-json\/wp\/v2\/tags?post=1754"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}