{"id":129555,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/procesado-interpretacion-y-modelado-del-perfil-de-reflexion-profunda-escin-3-3-zonas-asturoccidental-leonesa-y-centro-iberica\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"procesado-interpretacion-y-modelado-del-perfil-de-reflexion-profunda-escin-3-3-zonas-asturoccidental-leonesa-y-centro-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/procesado-interpretacion-y-modelado-del-perfil-de-reflexion-profunda-escin-3-3-zonas-asturoccidental-leonesa-y-centro-iberica\/","title":{"rendered":"Procesado, interpretacion y modelado del perfil de reflexion profunda escin-3.3 (zonas asturoccidental leonesa y centro-iberica)."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Ayarza Arribas M. Puy <\/strong><\/h2>\n<p>El trabajo realizado se ha centrado en el procesado, interpretacion y modelado de los datos tanto de gran angulo como de incidencia vertical pertenecientes a la linea escin-3.3. Tras el modelado de los datos de gran angulo, se ha dividido la corteza en tres partes:  superior, media e inferior con velocidades de 6-6.2, 6.6-6.35 y 6.9 km\/s respectivamente. El moho, situado a 28 km, limita con un manto que exhibe velocidades de 8.3 km\/s.  los datos de incidencia vertical han sidoreprocesados, obteniendose una notable mejora en la relacion se\u00f1al ruido. Se identifican en los primeros segundos del perfil estructuras cuya existencia se conocia o sededucia a partir de datos de superficie.  se argumenta la existencia de una duplicacion de corteza inferior de edad hasta el momento incierta. Existen tambien reflexiones profundas con altos buzamientos que podrian representar la imagen sismica de algun evento de tipo alpino.  el modelo de velocidades deducido a partir de los datos de gran angulo coincide bien con el modelo estructural deducido a partir de los datos de incidencia vertical.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Procesado, interpretacion y modelado del perfil de reflexion profunda escin-3.3 (zonas asturoccidental leonesa y centro-iberica).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Procesado, interpretacion y modelado del perfil de reflexion profunda escin-3.3 (zonas asturoccidental leonesa y centro-iberica). <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Ayarza Arribas M. Puy <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Josep Gallart Muset<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Andres Perez Estaun <\/li>\n<li>Javier Alvarez Pulgar (vocal)<\/li>\n<li>Larry Brown (vocal)<\/li>\n<li> Da\u00f1obeitia Canales Juan  Jos\u00e9 (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Ayarza Arribas M. Puy El trabajo realizado se ha centrado en el procesado, interpretacion y modelado de [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","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":"","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-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-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-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-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-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-gradient":""}},"footnotes":""},"categories":[27,1033,953,3435,9386,20496],"tags":[9050,242944,34386,127809,20499,242945],"class_list":["post-129555","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geofisica","category-geologia","category-geologia-estructural","category-salamanca","category-tectonica","tag-andres-perez-estaun","tag-ayarza-arribas-m-puy","tag-danobeitia-canales-juan-jose","tag-javier-alvarez-pulgar","tag-josep-gallart-muset","tag-larry-brown"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/129555","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=129555"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/129555\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=129555"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=129555"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=129555"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}