{"id":140672,"date":"2026-01-12T17:56:39","date_gmt":"2026-01-12T17:56:39","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-permotrias-de-las-baleares-de-la-cordillera-costero-catalana-y-de-la-vertiente-mediterranea-de-la-cordillera-iberica-facies-y-petrologia-sedimentaria\/"},"modified":"2026-01-12T17:56:39","modified_gmt":"2026-01-12T17:56:39","slug":"el-permotrias-de-las-baleares-de-la-cordillera-costero-catalana-y-de-la-vertiente-mediterranea-de-la-cordillera-iberica-facies-y-petrologia-sedimentaria","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-permotrias-de-las-baleares-de-la-cordillera-costero-catalana-y-de-la-vertiente-mediterranea-de-la-cordillera-iberica-facies-y-petrologia-sedimentaria\/","title":{"rendered":"El permotrias de las baleares, de la cordillera costero-catalana y de la vertiente mediterranea de la cordillera iberica: facies y petrolog\u00eda sedimentaria."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Gomez Gras David Manuel <\/strong><\/h2>\n<p>La serie permotriasica de las baleares y del litoral mediterraneo se ha depositado en semigrabens que aislan altos sin sedimentacion. En esta serie se han distinguido dos secuencias deposicionales (a excepcion de los catalanides en que la serie esta formada unicamente por la superior). Estas secuencias presentan tramos correspondientes al descenso del nivel del mar, con una sedimentacion aluvial, seguidos de un ascenso con sedimentacion, primero fluvial, y luego de transicion coincidiendo con el momento de mar alta. Los materiales aluviales proceden de areas fuentes locales. Los fluviales, con un aporte general nw-se, proceden, en lineas generales, de la erosion de la meseta.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El permotrias de las baleares, de la cordillera costero-catalana y de la vertiente mediterranea de la cordillera iberica: facies y petrolog\u00eda sedimentaria.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El permotrias de las baleares, de la cordillera costero-catalana y de la vertiente mediterranea de la cordillera iberica: facies y petrolog\u00eda sedimentaria. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Gomez Gras David Manuel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/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 Rosell Sanuy<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Gaspare Zuffa Gian <\/li>\n<li>Antonio Obrador Tuduri (vocal)<\/li>\n<li>Francisco J. Mart\u00ednez Fern\u00e1ndez (vocal)<\/li>\n<li> De La Pe\u00f1a Blasco Jos\u00e9 Andr\u00e9s (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gomez Gras David Manuel La serie permotriasica de las baleares y del litoral mediterraneo se ha depositado [&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":[27,953,19202,25320],"tags":[19690,78148,25344,232850,255318,473],"class_list":["post-140672","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-regional","category-petrologia-sedimentaria","tag-antonio-obrador-tuduri","tag-de-la-pena-blasco-jose-andres","tag-francisco-j-Martinez-fernandez","tag-gaspare-zuffa-gian","tag-gomez-gras-david-manuel","tag-juan-rosell-sanuy"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/140672","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=140672"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/140672\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=140672"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=140672"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=140672"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}