{"id":128875,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-cuenca-del-xallas-y-su-entorno-evolucion-cenozoica-del-relieve-en-el-oeste-de-la-provincia-de-la-coruna\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"la-cuenca-del-xallas-y-su-entorno-evolucion-cenozoica-del-relieve-en-el-oeste-de-la-provincia-de-la-coruna","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-cuenca-del-xallas-y-su-entorno-evolucion-cenozoica-del-relieve-en-el-oeste-de-la-provincia-de-la-coruna\/","title":{"rendered":"La cuenca del xallas y su entorno: evolucion cenozoica del relieve en el oeste de la provincia de la coru\u00f1a."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Pages Valcarlos Jos\u00e9 Luis <\/strong><\/h2>\n<p>Tras un analisis de la litolog\u00eda del area y su fracturacion, se estudian los elementos morfologicos mas destacados del relieve: superficies de aplanamiento y rd fluvial. Se definen cinco grupos de niveles de aplanamiento comprendidos entre los 700 y los 50 metros analizando su significado geomorfologico y sus asociaciones en unidades morfologicas.  se analiza la red fluvial prestando especial atencion a los encajamientos, procesos de captura, divisorias en retroceso y sedimentos asociados.  se conjugan los rasgos de niveles de aplanamiento y la red fluvial para reconstruir las distintas etapas evolutivas del relieve y las redes fluviales, a lo largo del cenozoico.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La cuenca del xallas y su entorno: evolucion cenozoica del relieve en el oeste de la provincia de la coru\u00f1a.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La cuenca del xallas y su entorno: evolucion cenozoica del relieve en el oeste de la provincia de la coru\u00f1a. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Pages Valcarlos Jos\u00e9 Luis <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/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>Angela Alonso Millan<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Ram\u00f3n Mas Mayoral <\/li>\n<li>David Serrat Congost (vocal)<\/li>\n<li> Pedraza Gilsanz JavierDe (vocal)<\/li>\n<li>Rafael Rodriguez Martinez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pages Valcarlos Jos\u00e9 Luis Tras un analisis de la litolog\u00eda del area y su fracturacion, se estudian [&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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