{"id":537,"date":"2014-06-16T10:30:13","date_gmt":"2014-06-16T17:30:13","guid":{"rendered":"http:\/\/carolinebeghein.com\/?page_id=537"},"modified":"2018-03-09T20:54:43","modified_gmt":"2018-03-10T03:54:43","slug":"western-us-great-basin","status":"publish","type":"page","link":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/research\/regional-tomography\/western-us-great-basin\/","title":{"rendered":"Rayleigh Wave Tomography in the western US Great Basin"},"content":{"rendered":"<div id=\"id2\" class=\"style_SkipStroke_1 shape-with-text\" style=\"color: #000000;\">\n<div class=\"text-content Normal_External_320_479\">\n<div class=\"Normal\">\n<p class=\"paragraph_style\" style=\"font-weight: bold;\"><span class=\"style\">SUMMARY<\/span><\/p>\n<figure id=\"attachment_540\" aria-describedby=\"caption-attachment-540\" style=\"width: 300px\" class=\"wp-caption alignleft\"><a href=\"http:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810.png\"><img fetchpriority=\"high\" decoding=\"async\" class=\"wp-image-540 size-medium\" src=\"http:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810-300x300.png\" alt=\"Tectonic setting\" width=\"300\" height=\"300\" srcset=\"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810-300x300.png 300w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810-150x150.png 150w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810-1024x1024.png 1024w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810-668x668.png 668w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810-600x600.png 600w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810-800x800.png 800w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/Fig1_tecto_b-e1402939677810.png 1081w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/a><figcaption id=\"caption-attachment-540\" class=\"wp-caption-text\">Tectonic setting<\/figcaption><\/figure>\n<p class=\"paragraph_style_1\">I have been performing surface wave tomography of the Great Basin, Nevada, to constrain upper mantle isotropic and anisotropic structure. This work started during my\u00a0<span class=\"style_1\">postdoc at the\u00a0<\/span><a class=\"class1\" style=\"color: #ff2600;\" title=\"http:\/\/sese.asu.edu\/\" href=\"http:\/\/sese.asu.edu\/\">School of Earth and Space Exploration<\/a>\u00a0<span class=\"style_1\">at\u00a0<\/span><a class=\"class2\" style=\"color: #ff2600;\" title=\"http:\/\/www.asu.edu\/\" href=\"http:\/\/www.asu.edu\/\">Arizona State University<\/a><span class=\"style_1\">, in\u00a0<\/span>Matt Fouch<span class=\"style_1\">&#8216;s group.<br \/>\n<\/span><\/p>\n<p class=\"paragraph_style_1\"><span class=\"style_1\">I performed Rayleigh wave phase velocity dispersion measurements using an inter-station method, in collaboration with\u00a0<\/span>Arthur Snoke<span class=\"style_1\">\u00a0at Virginia Tech. The measurements were then inverted to obtain azimuthally anisotropic phase velocity maps. The results are published in Earth and Planetary Science Letters (see\u00a0<\/span><a class=\"style_1\" style=\"color: #000000;\">Publications<\/a><span class=\"style_1\">).<br \/>\n<\/span><\/p>\n<p class=\"paragraph_style_1\"><span style=\"font-weight: bold;\">Citation:<\/span><\/p>\n<p class=\"paragraph_style_1\"><span class=\"style_14\" style=\"font-weight: bold;\"><a title=\"Preprint\" href=\"http:\/\/www2.epss.ucla.edu\/~cbeghein\/PDFS\/2010_Beghein_etal_EPSL_preprint.pdf\" target=\"_blank\" rel=\"noopener\"><img decoding=\"async\" class=\"alignnone wp-image-531 size-full\" src=\"http:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/lnk.gif\" alt=\"lnk\" width=\"22\" height=\"24\" \/><\/a>\u00a0Beghein, C<\/span><span class=\"style_3\">., Snoke, J.A., and Fouch, M.J., Depth Constraints on Azimuthal Anisotropy in the Great Basin from Rayleigh Wave Phase Velocity Maps,\u00a0<\/span><span class=\"style_15\">Earth Planet. Sci. Lett<\/span><span class=\"style_3\">.,\u00a0<\/span><span class=\"style_10\" lang=\"--multilingual\" xml:lang=\"--multilingual\">289, 467-478,<\/span><span class=\"style_3\">\u00a0<\/span><a class=\"style_11\" style=\"color: #ff2600;\" title=\"http:\/\/dx.doi.org\/10.1016\/j.epsl.2009.11.036\" href=\"http:\/\/dx.doi.org\/10.1016\/j.epsl.2009.11.036\">doi:10.1016\/j.epsl.2009.11.036<\/a><span class=\"style_3\">, 2010<\/span><\/p>\n<p class=\"paragraph_style_1\"><span class=\"style_1\">Follow-up work was then performed at UCLA. I used a forward modeling approach to invert the isotropic and anisotropic parts of the phase velocity maps to obtain three-dimensional models of shear-wave velocity and anisotropy in the region. The method employed enabled us to determined reliable model uncertainties as well. Paper under revision<\/span><\/p>\n<figure id=\"attachment_544\" aria-describedby=\"caption-attachment-544\" style=\"width: 616px\" class=\"wp-caption alignright\"><a href=\"http:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png\"><img decoding=\"async\" class=\"wp-image-544 size-full\" src=\"http:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png\" alt=\"Rayleigh wave phase maps for the Great Basin\" width=\"616\" height=\"897\" srcset=\"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png 616w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-206x300.png 206w, https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-600x874.png 600w\" sizes=\"(max-width: 616px) 100vw, 616px\" \/><\/a><figcaption id=\"caption-attachment-544\" class=\"wp-caption-text\">Rayleigh wave phase maps for the Great Basin<\/figcaption><\/figure>\n<\/div>\n<\/div>\n<\/div>\n<div class=\"tinyText\" style=\"color: #000000;\">\n<div id=\"id3\" class=\"style_SkipStroke_1 shape-with-text\">\n<div class=\"text-content Normal_External_640_395\">\n<div class=\"Normal\">\n<p class=\"paragraph_style_2\">This work was presented at the following meetings and conferences:<\/p>\n<ol>\n<li class=\"full-width\" value=\"1\">\n<p class=\"paragraph_style_3\"><span class=\"Bullet\">1.<\/span><span class=\"style_2\">\u00a0<\/span><span class=\"style_3\" style=\"font-weight: bold;\">Beghein, C<\/span><span class=\"style_2\">.,\u00a0<\/span>Models of Seismic Velocity and Anisotropy For the Great Basin, Nevada<span class=\"style_2\">,\u00a0<\/span>Eos Trans. AGU, Fall Meet. Suppl., Abstract,<span class=\"style_2\">\u00a02010<br \/>\n<\/span><\/p>\n<\/li>\n<li class=\"full-width\" value=\"2\">\n<p class=\"paragraph_style_3\"><span class=\"Bullet\">2.<\/span><span class=\"style_2\">\u00a0<\/span><span class=\"style_4\" style=\"font-weight: bold;\">Beghein, C<\/span>., Snoke, J.A., and Fouch, M.J., Azimuthal Anisotropy Signature in the Great Basin Lithosphere from Rayleigh Wave Phase Velocity Maps,\u00a0<span class=\"style_2\">Eos Trans. AGU, 90(52), Fall Meet. Suppl., Abstract, 2009.<br \/>\n<\/span><\/p>\n<\/li>\n<li class=\"full-width\" value=\"3\">\n<p class=\"paragraph_style_3\"><span class=\"Bullet\">3.<\/span><span class=\"style_2\">\u00a0<\/span><span class=\"style_4\" style=\"font-weight: bold;\">Beghein, C<\/span>., Snoke, J.A., and Fouch, M.J., Past and Present Deformation in the Great Basin revealed by Azimuthally Anisotropic Phase Velocity Maps, Earthscope meeting, Abstract, 2009<span class=\"style_5\"><br \/>\n<\/span><\/p>\n<\/li>\n<li class=\"full-width\" value=\"4\">\n<p class=\"paragraph_style_3\"><span class=\"Bullet\">4.<\/span><span class=\"style_2\">\u00a0<\/span><span class=\"style_4\" style=\"font-weight: bold;\">Beghein, C<\/span><span class=\"style_3\" style=\"font-weight: bold;\">.<\/span><span class=\"style_2\">, Snoke, J.A., Fouch, M.J., and West, J.D., Azimuthal Anisotropy From Surface Waves in the Great Basin, Eos Trans. AGU, 89(53), Fall Meet. Suppl., Abstract, 2008<br \/>\n<\/span><\/p>\n<\/li>\n<li class=\"full-width\" value=\"5\">\n<p class=\"paragraph_style_3\"><span class=\"Bullet\">5.<\/span><span class=\"style_4\" style=\"font-weight: bold;\">Beghein, C<\/span>., Snoke, J.A., and Fouch, M.J., Inferences on Upper mantle Seismic Velocity and Anisotropy in Western North America From Surface Waves Analyses, Eos Trans. AGU, 88(52), Fall Meet. Suppl., Abstract, 2007.<\/p>\n<\/li>\n<li class=\"full-width\" value=\"6\">\n<p class=\"paragraph_style_3\"><span class=\"Bullet\">6.<\/span>\u00a0<span class=\"style_4\" style=\"font-weight: bold;\">Beghein, C<\/span>., Fouch, M.J., and Snoke, J.A., Upper mantle seismic velocity structure in the Great Basin, Earthscope meeting, Abstract, 2007.<\/p>\n<\/li>\n<li class=\"full-width\" value=\"7\">\n<p class=\"paragraph_style_3\"><span class=\"Bullet\">7.<\/span>\u00a0<span class=\"style_4\" style=\"font-weight: bold;\">Beghein, C<\/span>., Fouch, M.J., Snoke, J.A., and Warren, L.M., Improved constraints and resolution assessment of upper mantle seismic velocity structure in the western United States, Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract, 2006.<\/p>\n<\/li>\n<\/ol>\n<\/div>\n<\/div>\n<\/div>\n<div class=\"tinyText\"><\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>SUMMARY I have been performing surface wave tomography of the Great Basin, Nevada, to constrain upper mantle isotropic and anisotropic structure. This work started during my\u00a0postdoc at the\u00a0School of Earth and Space Exploration\u00a0at\u00a0Arizona State University, in\u00a0Matt Fouch&#8216;s group. I performed Rayleigh wave phase velocity dispersion measurements using an inter-station method, in collaboration with\u00a0Arthur Snoke\u00a0at Virginia &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/research\/regional-tomography\/western-us-great-basin\/\" class=\"more-link\">Read more<span class=\"screen-reader-text\"> &#8220;Rayleigh Wave Tomography in the western US Great Basin&#8221;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":544,"parent":66,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"inspiro_hide_title":false,"footnotes":""},"class_list":["post-537","page","type-page","status-publish","has-post-thumbnail","hentry"],"jetpack_sharing_enabled":false,"featured_media_urls":{"thumbnail":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-150x150.png",150,150,true],"medium":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-206x300.png",206,300,true],"medium_large":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png",616,897,false],"large":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png",616,897,false],"1536x1536":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png",616,897,false],"2048x2048":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png",616,897,false],"inspiro-featured-image":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png",616,897,false],"inspiro-loop":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-616x320.png",616,320,true],"inspiro-loop@2x":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-616x640.png",616,640,true],"portfolio_item-thumbnail":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-600x400.png",600,400,true],"portfolio_item-thumbnail@2x":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-616x800.png",616,800,true],"portfolio_item-masonry":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-600x874.png",600,874,true],"portfolio_item-masonry@2x":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png",616,897,false],"portfolio_item-thumbnail_cinema":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-616x335.png",616,335,true],"portfolio_item-thumbnail_portrait":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-600x897.png",600,897,true],"portfolio_item-thumbnail_portrait@2x":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps.png",616,897,false],"portfolio_item-thumbnail_square":["https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-content\/uploads\/2014\/06\/GB_Results_maps-616x800.png",616,800,true]},"_links":{"self":[{"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/pages\/537","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/comments?post=537"}],"version-history":[{"count":3,"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/pages\/537\/revisions"}],"predecessor-version":[{"id":2175,"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/pages\/537\/revisions\/2175"}],"up":[{"embeddable":true,"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/pages\/66"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/media\/544"}],"wp:attachment":[{"href":"https:\/\/faculty.epss.ucla.edu\/~cbeghein\/wp-json\/wp\/v2\/media?parent=537"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}