{"id":143196,"date":"1993-01-01T00:00:00","date_gmt":"1993-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-e-interpretacion-de-ondas-p-y-s-de-perfiles-sismicos-aplicacion-al-noroeste-de-la-peninsula-iberica\/"},"modified":"1993-01-01T00:00:00","modified_gmt":"1993-01-01T00:00:00","slug":"analisis-e-interpretacion-de-ondas-p-y-s-de-perfiles-sismicos-aplicacion-al-noroeste-de-la-peninsula-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/analisis-e-interpretacion-de-ondas-p-y-s-de-perfiles-sismicos-aplicacion-al-noroeste-de-la-peninsula-iberica\/","title":{"rendered":"Analisis e interpretacion de ondas p y s de perfiles sismicos: aplicacion al noroeste de la peninsula iberica."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Julia Tellez Pablo <\/strong><\/h2>\n<p>En este trabajo se analizan las principales propiedades de los datos sismicos obtenidos en un experimento de sismica de refraccion: contenido de frecuencias, naturaleza y parametros de la polarizacion y amplitud de las se\u00f1ales y se proponen y desarrollan tecnicas de filtrado basadas en dichas propiedades. El filtrado de los datos permite una buena separacion e identificacion de los diferentes grupos de ondas y hace posible establecer una correlacion segura de las llegadas. Esta metodolog\u00eda se aplica a la interpretacion de los datos de sismica de refraccion del noroeste de la peninsula iberica. Como resultado se obtienen unos modelos para la distribucion de las velocidades de propagacion de las ondas internas, compresionales y de cizalla, y para la relacion de poisson, de cuya interpretacion conjunta se obtiene, a su vez, una informacion decisiva para el conocimiento de la estructura en el noroeste de la peninsula iberica.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Analisis e interpretacion de ondas p y s de perfiles sismicos: aplicacion al noroeste de la peninsula iberica.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Analisis e interpretacion de ondas p y s de perfiles sismicos: aplicacion al noroeste de la peninsula iberica. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Julia Tellez Pablo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1993<\/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>Diego Cordoba Barba<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Agust\u00edn Ud\u00edas Vallina <\/li>\n<li>Jos\u00e9 Gallart Muset (vocal)<\/li>\n<li>Ram\u00f3n Vegas Mart\u00ednez (vocal)<\/li>\n<li>Julio Mezcua Rodr\u00edguez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Julia Tellez Pablo En este trabajo se analizan las principales propiedades de los datos sismicos obtenidos en [&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 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