{"id":35081,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/morfologia-y-sedimentacion-de-la-plataforma-continental-interna-del-area-central-de-asturias\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"morfologia-y-sedimentacion-de-la-plataforma-continental-interna-del-area-central-de-asturias","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/morfologia-y-sedimentacion-de-la-plataforma-continental-interna-del-area-central-de-asturias\/","title":{"rendered":"Morfolog\u00eda y sedimentacion de la plataforma continental interna del area central de asturias."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Fernandez Valdes Lloret Jos\u00e9 Manuel <\/strong><\/h2>\n<p>Se ha estudiado la plataforma continental interna del \u00e1rea central de asturias, desde la punta del cervig\u00f3n (gij\u00f3n), hasta la desembocadura de la r\u00eda de avil\u00e9s y, desde la l\u00ednea de costa, hasta la isobata de -50 m, tanto desde el punto de vista morfol\u00f3gico, como sedimentol\u00f3gico.  se trata de una plataforma desnutrida; es decir, fundamentalmente rocosa con una sedimentaci\u00f3n poco potente.  los sedimentos presentan car\u00e1cter silicicl\u00e1stico en la franja costera que enlazan con las playas activas y, un mosaico complejo de facies relictas constitu\u00eddas por gravillas y arenas gruesas biocl\u00e1sticas en muchos casos removilizadas.  los sedimentos m\u00e1s antiguos corresponden a las facies relictas, restos de la regresi\u00f3n wurmiense que, son removilizados durante el \u00faltimo ascenso eust\u00e1tico, las cuales culminan con las facies solicicl\u00e1sticas costeras durante el episodio de alto nivel del mar en curso.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Morfolog\u00eda y sedimentacion de la plataforma continental interna del area central de asturias.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Morfolog\u00eda y sedimentacion de la plataforma continental interna del area central de asturias. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Fernandez Valdes Lloret Jos\u00e9 Manuel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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> Flor Rodriguez German Santos<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Antonio Agueda Villar <\/li>\n<li>Jos\u00e9 Bastida Tirado (vocal)<\/li>\n<li>Federico Vilas Martin (vocal)<\/li>\n<li>Ricard Mar\u00ed Sagarra (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Fernandez Valdes Lloret Jos\u00e9 Manuel Se ha estudiado la plataforma continental interna del \u00e1rea central de asturias, [&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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