{"id":55096,"date":"2018-03-09T22:42:47","date_gmt":"2018-03-09T22:42:47","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-geomorfologico-y-estimacion-de-la-susceptibilidad-a-flujos-de-derrubios-y-desprendimientos-de-rocas-en-el-valle-de-benasque\/"},"modified":"2018-03-09T22:42:47","modified_gmt":"2018-03-09T22:42:47","slug":"estudio-geomorfologico-y-estimacion-de-la-susceptibilidad-a-flujos-de-derrubios-y-desprendimientos-de-rocas-en-el-valle-de-benasque","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/geomorfologia\/estudio-geomorfologico-y-estimacion-de-la-susceptibilidad-a-flujos-de-derrubios-y-desprendimientos-de-rocas-en-el-valle-de-benasque\/","title":{"rendered":"Estudio geomorfol\u00f3gico y estimaci\u00f3n de la susceptibilidad a flujos de derrubios y desprendimientos de rocas en el valle de benasque."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Enrique Acosta Arias <\/strong><\/h2>\n<p>La zona de estudio se encuentra en el extremo ne de la provincia de huesca, en la llamada zona axial del pirineo y tiene un \u00e1rea de 297 km2. En esta tesis se ha realizado un estudio geomorfol\u00f3gico de esta zona de monta\u00f1a a escala 1:25.000, dedicando una especial atenci\u00f3n a los sackungen y a dos tipos de movimientos r\u00e1pidos de ladera: flujos de derrubios (debris flows) y desprendimientos de rocas (rock-falls). el doctorando ha participado con una beca del instituto geol\u00f3gico y minero de espa\u00f1a (igme) en el proyecto damocles (evg1-1999-00027p) financiado por el v programa marco de la ue, con investigadores de las universidades de newcastle (uk), mil\u00e1n-bicocca (italia) y p\u00e1dova (italia), y del cnr-irpi de perugia (italia), del cnr-csite de bologna (italia), del ipe-csic de zaragoza y del propio igme.  mediante la aplicaci\u00f3n de algunos modelos que se han desarrollado en el proyecto damocles se ha estimado la propensi\u00f3n de la zona de estudio a verse afectada por flujos de derrubios y desprendimientos de rocas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio geomorfol\u00f3gico y estimaci\u00f3n de la susceptibilidad a flujos de derrubios y desprendimientos de rocas en el valle de benasque.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio geomorfol\u00f3gico y estimaci\u00f3n de la susceptibilidad a flujos de derrubios y desprendimientos de rocas en el valle de benasque. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Enrique Acosta Arias <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 20\/10\/2006<\/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>Aragu\u00e9s R\u00edos<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Garc\u00eda ruiz Jos\u00e9 Mar\u00eda <\/li>\n<li>jeronimo Lopez Martinez (vocal)<\/li>\n<li>\u00e1ngel Mart\u00edn serrano (vocal)<\/li>\n<li>joan Manuel Vilaplana fernandez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Enrique Acosta Arias La zona de estudio se encuentra en el extremo ne de la provincia 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 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