{"id":45604,"date":"2019-06-17T13:11:25","date_gmt":"2019-06-17T13:11:25","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/depositos-arenosos-de-las-playas-del-litoral-de-la-region-de-cabo-penas-asturias-sedimentologia-y-dinamica\/"},"modified":"2019-06-17T13:11:25","modified_gmt":"2019-06-17T13:11:25","slug":"depositos-arenosos-de-las-playas-del-litoral-de-la-region-de-cabo-penas-asturias-sedimentologia-y-dinamica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/depositos-arenosos-de-las-playas-del-litoral-de-la-region-de-cabo-penas-asturias-sedimentologia-y-dinamica\/","title":{"rendered":"Depositos arenosos de las playas del litoral de la region de cabo pe\u00f1as (asturias): sedimentolog\u00eda y dinamica"},"content":{"rendered":"<h2>Tesis doctoral de <strong> German Flor Rodriguez <\/strong><\/h2>\n<p>A partir de toda una serie de variables: morfolog\u00eda costera y playera  granulometrias de arenas  estudio del componente biogenico  variedad biologica  analisis de las fracciones ligeras y pesadas  textura de la superficie de los granos y forma  distribucion e identificacion de los procesos de bioturbacion  reparticion de la salinidad en el borde costero  entre las mas importantes  se puede establecer la interrelacion geografica del cabo (anomalia en un sector costero subrectilineo) &#8211; corriente costera tipos de sedimentos y movimiento de las masas de arena.  se diferencia un sector occidental directamente afectado por la corriente costera  con procesos de ascenso (upwelling) en verdicio  un area norosriental de sombra y un sector suroriental  nuevamente expuesto  con ascensos importantes frente a carranques.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Depositos arenosos de las playas del litoral de la region de cabo pe\u00f1as (asturias): sedimentolog\u00eda y dinamica<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Depositos arenosos de las playas del litoral de la region de cabo pe\u00f1as (asturias): sedimentolog\u00eda y dinamica <\/li>\n<li><strong>Autor:<\/strong>\u00a0 German Flor Rodriguez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1979<\/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> Sanchez De La Torre Luis M.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Sanchez De La Torre Luis Mar\u00eda <\/li>\n<li>Inmaculada Corrales Zarauza (vocal)<\/li>\n<li>Juan  Antonio Vera Torres (vocal)<\/li>\n<li>Antonio Cendrero Uceda (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de German Flor Rodriguez A partir de toda una serie de variables: morfolog\u00eda costera y playera granulometrias 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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