{"id":21715,"date":"2018-03-09T09:11:36","date_gmt":"2018-03-09T09:11:36","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-sedimentologica-y-geomorfologica-de-las-vegas-bajas-del-guadiana-entre-merida-y-badajoz-espana\/"},"modified":"2018-03-09T09:11:36","modified_gmt":"2018-03-09T09:11:36","slug":"evolucion-sedimentologica-y-geomorfologica-de-las-vegas-bajas-del-guadiana-entre-merida-y-badajoz-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-sedimentologica-y-geomorfologica-de-las-vegas-bajas-del-guadiana-entre-merida-y-badajoz-espana\/","title":{"rendered":"Evoluci\u00f3n sedimentol\u00f3gica y geomorfol\u00f3gica de las vegas bajas del guadiana entre m\u00e9rida y badajoz (espa\u00f1a)"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Moya Palomares M. Eugenia <\/strong><\/h2>\n<p>Se estudia la sedimentaci\u00f3n y el relieve del valle del r\u00edo guadiana en la cuenca de las vegas bajas (entre m\u00e9rida y badajoz).  se describe e interpreta el registro sedimentario, definiendo cuatro unidades sedimentarias limitadas por discontinuidades (uld 1-4). El an\u00e1lisis de la unidad uld1 lleva a considerarla como formada por los sedimentos de abanicos distales. La reconstrucci\u00f3n de la unidad se\u00f1ala la existencia de aportes desde el oeste de nuestra zona de trabajo asociados a los movimientos de un conjunto de accidentes tect\u00f3nicos principales (falla de plasencia y asociadas).  el an\u00e1lisis de la secuencia de la unidad uld2 lleva a interpretarla como dep\u00f3sito, de abanicos aluviales ocasionalmente perpendiculares a la cuenca para pasar posteriormente a la consolidaci\u00f3n de un sistema fluvial braided arenoso de direcci\u00f3n e-w. La unidad se interrumpe a techo dando lugar a la formaci\u00f3n de zonas pantanosas identificadas con los dep\u00f3sitos culminantes de sld2.  el an\u00e1lisis de la unidad uld3 indica una activaci\u00f3n fluvial en la cuenca, y los dep\u00f3sitos que constituyen dicha unidad son interpretados como pertenecientes a una red fluvial braided de carga mixta, que barr\u00eda la cuenca con un sentido similar a sld2, pero claramente diferente si nos alejamos de la zona hacia el oeste.  la unidad uld4 est\u00e1 formada por las facies proximales de abanicos aluviales dentro de un clima \u00e1rido y posiblemente correlativos a los dep\u00f3sitos de ra\u00f1a que se extienden tanto al norte como al sur del \u00e1rea de trabajo.  del an\u00e1lisis del relieve se obtienen pruebas de las relaciones entre fases de arrasamiento y sedimentaci\u00f3n y se estudia en detalle la morfolog\u00eda reciente de la llanura aluvial y cauces, con especial atenci\u00f3n a los procesos de avenida rel\u00e1mpago de la cuenca del arroyo rivillas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evoluci\u00f3n sedimentol\u00f3gica y geomorfol\u00f3gica de las vegas bajas del guadiana entre m\u00e9rida y badajoz (espa\u00f1a)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evoluci\u00f3n sedimentol\u00f3gica y geomorfol\u00f3gica de las vegas bajas del guadiana entre m\u00e9rida y badajoz (espa\u00f1a) <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Moya Palomares M. Eugenia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 21\/02\/2003<\/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>Juan  De Dios Centeno  Carrillo<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Pedraza gilsanz Javierde <\/li>\n<li>Manuel f. Segura redondo (vocal)<\/li>\n<li>eduardo Acaso deltell (vocal)<\/li>\n<li>Ana Ramos pereira (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Moya Palomares M. Eugenia Se estudia la sedimentaci\u00f3n y el relieve del valle del r\u00edo guadiana en [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[1],"tags":[65342,65341,65340,17726,65339,38972],"class_list":["post-21715","post","type-post","status-publish","format-standard","hentry","category-sin-categoria","tag-ana-ramos-pereira","tag-eduardo-acaso-deltell","tag-juan-de-dios-centeno-carrillo","tag-manuel-f-segura-redondo","tag-moya-palomares-m-eugenia","tag-pedraza-gilsanz-javierde"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/21715","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=21715"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/21715\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=21715"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=21715"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=21715"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}