{"id":46857,"date":"2020-01-15T10:25:19","date_gmt":"2020-01-15T10:25:19","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracteristicas-de-sedimentacion-costera-actual-en-las-rias-de-vigo-y-bayona-pontevedra\/"},"modified":"2020-01-15T10:25:19","modified_gmt":"2020-01-15T10:25:19","slug":"caracteristicas-de-sedimentacion-costera-actual-en-las-rias-de-vigo-y-bayona-pontevedra","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/caracteristicas-de-sedimentacion-costera-actual-en-las-rias-de-vigo-y-bayona-pontevedra\/","title":{"rendered":"Caracteristicas de sedimentacion costera actual en las rias de vigo y bayona (pontevedra)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Federico Vilas Marin <\/strong><\/h2>\n<p>Se estudia la sedimentacion actual de la ria de vigo y los factores hidrodinamicos que la controlan; se observa una influencia fluvial creciente desde las partes esternas de la ria  como la ensenada de bayona hasta las internas  como la ensenada de san simon  donde el rio oitaven aparta gran cantidad de sedimentos redistribuidos por las corrientes mareales. Los organismos que viven en el sedimento presentan una clara accion vertical. Las secuencias sedimentarias son tipicas de llanura tidal en la parte externa (p. Ej. En la ramallosa)  y mas complicadas en la parte interna  donde hay grandes variaciones de tama\u00f1o de grava tanto en la vertical como en la horizontal. Se presentan varias secuencias-tipo y mapas de distribucion de sedimentos segun estaciones.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracteristicas de sedimentacion costera actual en las rias de vigo y bayona (pontevedra)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracteristicas de sedimentacion costera actual en las rias de vigo y bayona (pontevedra) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Federico Vilas Marin <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1980<\/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>Alfredo Arche Miralles<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carmina Virgili Rodon <\/li>\n<li>Francisco Goitian Osea (vocal)<\/li>\n<li>Bermodo Melendez Melendez (vocal)<\/li>\n<li>Francisco Mingarro Martin (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Federico Vilas Marin Se estudia la sedimentacion actual de la ria de vigo y los factores hidrodinamicos [&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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