{"id":50660,"date":"2021-06-07T22:15:04","date_gmt":"2021-06-07T22:15:04","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-y-sedimentologia-de-las-formaciones-lacustres-del-transito-oligoceno-mioceno-del-se-de-la-cuenca-del-ebro\/"},"modified":"2021-06-07T22:15:04","modified_gmt":"2021-06-07T22:15:04","slug":"estratigrafia-y-sedimentologia-de-las-formaciones-lacustres-del-transito-oligoceno-mioceno-del-se-de-la-cuenca-del-ebro","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-y-sedimentologia-de-las-formaciones-lacustres-del-transito-oligoceno-mioceno-del-se-de-la-cuenca-del-ebro\/","title":{"rendered":"Estratigrafia y sedimentolog\u00eda de las formaciones lacustres del transito oligoceno-mioceno del se de la cuenca del ebro."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Luis Cabrera P\u00e9rez <\/strong><\/h2>\n<p>A partir del estudio estratigrafico y sedimentologico realizado sobre diversas sucesiones estratigraficas de origen lacustre y aluvial en el sector se de la cuenca del ebro  se ha diferenciado dos sitemas deposicionales aluviales (scala dei de procedencia catalanide matarranya-guadalope  de procedencia iberica) que se relacionan entre si y con un tercer sistema (de los monegros) desarrollado esencialmente en el ambito central de la cuenca y caracterizado por un acentuado desarrollo de unidades lacustres. Los hallazgos de yacimientos de micromamiferos fosiles han permitido establecer tres grandes biozonas locales  atribuibles en su conjunto al oligoceno superior y el aquitaniense.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia y sedimentolog\u00eda de las formaciones lacustres del transito oligoceno-mioceno del se de la cuenca del ebro.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia y sedimentolog\u00eda de las formaciones lacustres del transito oligoceno-mioceno del se de la cuenca del ebro. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Luis Cabrera P\u00e9rez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1983<\/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>Joaquin Villena Morales (vocal)<\/li>\n<li> Fernandez De Villalta Comella Jos\u00e9 (vocal)<\/li>\n<li>Antonio Obrador Tuduri (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Luis Cabrera P\u00e9rez A partir del estudio estratigrafico y sedimentologico realizado sobre diversas sucesiones estratigraficas de origen [&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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