{"id":44066,"date":"2018-08-30T06:20:06","date_gmt":"2018-08-30T06:20:06","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-paleogeno-continental-anterior-a-la-transgresion-biorritziense-eoceno-medio-entre-los-rios-govina-y-ripoll-provincias-de-tarragona-y-barcelona\/"},"modified":"2018-08-30T06:20:06","modified_gmt":"2018-08-30T06:20:06","slug":"el-paleogeno-continental-anterior-a-la-transgresion-biorritziense-eoceno-medio-entre-los-rios-govina-y-ripoll-provincias-de-tarragona-y-barcelona","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-paleogeno-continental-anterior-a-la-transgresion-biorritziense-eoceno-medio-entre-los-rios-govina-y-ripoll-provincias-de-tarragona-y-barcelona\/","title":{"rendered":"El paleogeno continental anterior a la transgresion biorritziense eoceno medio, entre los rios govi\u00f1a y ripoll (provincias de tarragona y barcelona)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pedro Anadon Monzon <\/strong><\/h2>\n<p>La presente tesis se centra en el estudio de la sedimentacion continental que tuvo lugar durante el paleogeno inferior en parte de la zona oriental de la cuenca del ebro. El area esta localizada junto a las cordilleras costeras catalanas y comprende el borde de la cuenca del ebro adosado a la cordillera prelitoral. Es en este borde donde tuvo lugar la sedimentacion de los materiales objeto de este estudio  en relacion con los movimientos tectonicos que promovieron el levantamiento del macizo catalan y la deposicion de potentes series molasicas en las zonas de la cuenca del ebro situadas al borde de la misma y adosadas a la cordillera prelitoral en vias de formacion. Se presenta asimismo una nueva propuesta de datacion para parte de los materiales.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El paleogeno continental anterior a la transgresion biorritziense eoceno medio, entre los rios govi\u00f1a y ripoll (provincias de tarragona y barcelona).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El paleogeno continental anterior a la transgresion biorritziense eoceno medio, entre los rios govi\u00f1a y ripoll (provincias de tarragona y barcelona). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pedro Anadon Monzon <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1978<\/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: Luis Sole Sabaris <\/li>\n<li>Salvador Reguant Serra (vocal)<\/li>\n<li>Oriol Riba Arderiu (vocal)<\/li>\n<li> Fernandez De Villalta Comella  Jos\u00e9 (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pedro Anadon Monzon La presente tesis se centra en el estudio de la sedimentacion continental que tuvo [&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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