{"id":46324,"date":"2019-10-17T02:55:45","date_gmt":"2019-10-17T02:55:45","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-bundstandstein-de-los-catalanides-estratigrafia-y-procesos-sedimentarios\/"},"modified":"2019-10-17T02:55:45","modified_gmt":"2019-10-17T02:55:45","slug":"el-bundstandstein-de-los-catalanides-estratigrafia-y-procesos-sedimentarios","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-bundstandstein-de-los-catalanides-estratigrafia-y-procesos-sedimentarios\/","title":{"rendered":"El bundstandstein de los catalanides: estratigrafia y procesos sedimentarios."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Mar\u00eda no Marzo Carpio <\/strong><\/h2>\n<p>Litoestratigraficamente  los afloramientos de buntsandstein de los catalanides pueden agruparse en tres grandes dominios estratigraficos  cada uno de los cuales se caracteriza por una sucesion litologica particular. En cada dominio  que puede interpretarse como una subcuenca delimitada e influenciada por el juego sinsedimentario de un sistema de fracturas de zocalo tardihercinicas  hemos diferenciado un cierto numero de unidades litologicas con connotacion genetica. La mayor parte de ellas son de origen fluvial  excepto la unidad de transito a las facies carbonatdas del muschelkalk inferior que puede interpretarse como depositos de llanuras fangosas evaporiticas supralitorales. Se establece una hipotesis sobre la evolucion paleogeografica de los catalanides durante el triasico inferior.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El bundstandstein de los catalanides: estratigrafia y procesos sedimentarios.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El bundstandstein de los catalanides: estratigrafia y procesos sedimentarios. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Mar\u00eda no Marzo Carpio <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/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>Oriol Riba Arderiu<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Salvador Reguant Serra <\/li>\n<li>Carmina Virgili Vinaoe (vocal)<\/li>\n<li> Fontbote Mussolas Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li>Oriol Riba Arderiu (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mar\u00eda no Marzo Carpio Litoestratigraficamente los afloramientos de buntsandstein de los catalanides pueden agruparse en tres grandes [&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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