{"id":177,"date":"2013-02-12T17:36:59","date_gmt":"2013-02-12T17:36:59","guid":{"rendered":"http:\/\/www.geol.umd.edu\/facilities\/seismology\/?page_id=177"},"modified":"2023-02-21T10:56:05","modified_gmt":"2023-02-21T15:56:05","slug":"data","status":"publish","type":"page","link":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/","title":{"rendered":"Data"},"content":{"rendered":"<div style=\"width:100%; float:left; box-sizing:border-box;\">\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/a-tectonic-regionalization-of-the-world\/\" style=\"text-decoration:none; color:#FFFFFF;\">A tectonic regionalization of the world<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2013\/02\/Data4Re-150x150.png\" alt=\"\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/a-tectonic-regionalization-of-the-world\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of A tectonic regionalization of the world\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/clustering-of-lower-mantle-structure-perm-anomaly\/\" style=\"text-decoration:none; color:#FFFFFF;\">Clustering of Lower Mantle Structure &#8211; Perm Anomaly<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2013\/06\/LM_clustering-150x150.jpg\" alt=\"\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/clustering-of-lower-mantle-structure-perm-anomaly\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of Clustering of Lower Mantle Structure &#8211; Perm Anomaly\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/depth-and-strength-of-the-lithosphere-asthenosphere-transition-across-the-southwestern-united-states\/\" style=\"text-decoration:none; color:#FFFFFF;\">Depth and strength of the lithosphere-asthenosphere transition across the Southwestern United States<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2015\/07\/SWLAB-150x150.png\" alt=\"\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/depth-and-strength-of-the-lithosphere-asthenosphere-transition-across-the-southwestern-united-states\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of Depth and strength of the lithosphere-asthenosphere transition across the Southwestern United States\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/lateral-variations-in-the-velocity-of-shear-waves\/\" style=\"text-decoration:none; color:#FFFFFF;\">Lateral variations in the velocity of shear waves<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2013\/02\/Data3Re-150x150.png\" alt=\"\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/lateral-variations-in-the-velocity-of-shear-waves\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of Lateral variations in the velocity of shear waves\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/lithospheric-thickness-across-southern-california\/\" style=\"text-decoration:none; color:#FFFFFF;\">Lithospheric thickness across Southern California<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2013\/02\/Data1Re-150x150.png\" alt=\"Lithospheric thickness across Southern California\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/lithospheric-thickness-across-southern-california\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of Lithospheric thickness across Southern California\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/morphology-of-lower-mantle-structures\/\" style=\"text-decoration:none; color:#FFFFFF;\">Morphology of Lower Mantle Structures<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2016\/10\/LLSVPsimage-150x150.png\" alt=\"\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/morphology-of-lower-mantle-structures\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of Morphology of Lower Mantle Structures\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/north-america-vp-tomographic-model\/\" style=\"text-decoration:none; color:#FFFFFF;\">North America Vp Tomographic Model<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2017\/10\/Map_at_700km-150x150.png\" alt=\"\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/north-america-vp-tomographic-model\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of North America Vp Tomographic Model\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n\r\n<div style=\"width:32%; float:left; background-color:#E02E31; padding:10px 10px 20px 10px; margin:15px 5px; box-sizing:border-box;\">\r\n\t<p style=\"width:100%; border-bottom:1px solid #FFE573; font-weight:bold; font-size:1.3em; text-decoration:none; color:#FFFFFF;\"><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/the-velocity-structure-beneath-continents\/\" style=\"text-decoration:none; color:#FFFFFF;\">The velocity structure beneath continents<\/a><\/p>\r\n\t<p><img decoding=\"async\" src=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-content\/uploads\/2013\/02\/Data2Re-150x150.png\" alt=\"\" width=100% ><\/p>\r\n\t<p><a href=\"https:\/\/www.geol.umd.edu\/facilities\/seismology\/data\/the-velocity-structure-beneath-continents\/\" style=\"color:#FFFFFF\" aria-label=\"Read more of The velocity structure beneath continents\">[&#8230;Read More&#8230;]<\/a><\/p>\r\n<\/div>\r\n<\/div>","protected":false},"excerpt":{"rendered":"","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"open","ping_status":"open","template":"","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"class_list":["post-177","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/pages\/177","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/comments?post=177"}],"version-history":[{"count":3,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/pages\/177\/revisions"}],"predecessor-version":[{"id":1037,"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/pages\/177\/revisions\/1037"}],"wp:attachment":[{"href":"https:\/\/www.geol.umd.edu\/facilities\/seismology\/wp-json\/wp\/v2\/media?parent=177"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}