{"id":125352,"date":"2018-03-11T12:24:36","date_gmt":"2018-03-11T12:24:36","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafa%c2%ada-y-sedimentologa%c2%ada-de-las-formaciones-lacustres-del-transito-eoceno-oligoceno-del-ne-de-la-cuenca-del-ebro\/"},"modified":"2018-03-11T12:24:36","modified_gmt":"2018-03-11T12:24:36","slug":"estratigrafa%c2%ada-y-sedimentologa%c2%ada-de-las-formaciones-lacustres-del-transito-eoceno-oligoceno-del-ne-de-la-cuenca-del-ebro","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafa%c2%ada-y-sedimentologa%c2%ada-de-las-formaciones-lacustres-del-transito-eoceno-oligoceno-del-ne-de-la-cuenca-del-ebro\/","title":{"rendered":"Estratigraf\u00eday sedimentolog\u00eda de las formaciones lacustres del tr\u00e1nsito eoceno-oligoceno del ne de la cuenca del ebro"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Alberto Saez Ruiz <\/strong><\/h2>\n<p>El estudio estratigr\u00e1fico y sedimentol\u00f3gico realizado sobre diversas sucesiones estratifr\u00e1ficas del sector ne de la cuenca del ebro han diferenciado dos secuencias sedimentarias aluvio-lacustres:  a) una secuencia priaboniense superior constituida por las formaciones yesos de barbastro, limolitas de tor\u00e1, calizas de castelltallat y parte inferior de areniscas de suria y  b) una secuencia estampiense inferior constituida por la formaci\u00f3n lignitos de calaf y parte alta de la formaci\u00f3n s\u00faria.  los sistemas lacustres de cada secuencia se desarrollaron en el centro de cuenca y, seg\u00fan el an\u00e1lisis de paleocorrientes, se encuentran alimentados por sistemas aluviales de procedencia piren\u00e1ica (formaciones solsona y peraltilla) y catalanide (formaci\u00f3n art\u00e9s).  los hallazgos de yacimientos de micromam\u00edferos y car\u00f3fitas permiten establecer varias biozonas locales. Los an\u00e1lisis de facies, de mineralog\u00eda de arcillas y geoqu\u00edmicos permiten elaborar modelos de sedimentaci\u00f3n en ambientes de playa-lake (formaciones barbastro y tor\u00e1) y de abanico terminal (formaciones s\u00faria). An\u00e1lisis de isolitos y paleocorrientes de la formaci\u00f3n calaf permiten elaborar un modelo de g\u00e9nesis, acumulaci\u00f3n y evoluci\u00f3n de lignito a partir de datos de sondeo.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigraf\u00eday sedimentolog\u00eda de las formaciones lacustres del tr\u00e1nsito eoceno-oligoceno del ne de la cuenca del ebro<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigraf\u00eday sedimentolog\u00eda de las formaciones lacustres del tr\u00e1nsito eoceno-oligoceno del ne de la cuenca del ebro <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Alberto Saez Ruiz <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 30\/04\/1987<\/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: Juan  Antonio Vera Torres <\/li>\n<li>Cai Puigdefabregas Tomas (vocal)<\/li>\n<li>Joaquin Villena Morales (vocal)<\/li>\n<li>Pedro Anadon Monzon (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alberto Saez Ruiz El estudio estratigr\u00e1fico y sedimentol\u00f3gico realizado sobre diversas sucesiones estratifr\u00e1ficas del sector ne de [&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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