{"id":10814,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1996\/01\/01\/la-cuenca-subbetica-mesozoica-en-el-sector-oriental-de-las-cordilleras-beticas\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"la-cuenca-subbetica-mesozoica-en-el-sector-oriental-de-las-cordilleras-beticas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-cuenca-subbetica-mesozoica-en-el-sector-oriental-de-las-cordilleras-beticas\/","title":{"rendered":"La cuenca subbetica mesozoica en el sector oriental de las cordilleras beticas."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Nieto Albert Luis Miguel <\/strong><\/h2>\n<p>En esta memoria se estudia la estratigrafia y sedimentolog\u00eda de los materiales del jurasico y del cretacico del sector oriental de la zona subbetica con el fin de proponer un modelo paleogeografico. Para ello se ha utilizado la metodolog\u00eda clasica de la geolog\u00eda (campo, laboratorio y gabinete). Hemos comprobado, a partir del analisis de facies, que el comportamiento sedimentario de cada una de las unidades tectonicas consideradas fue muy variable, lo que se traduce en importantes cambios laterales de facies y en variaciones notables de la amplitud de las lagunas estratigraficas asociadas a las discontinuidades observadas. Como resultado de estos hechos, se han reconocido los siguientes dominios paleogeograficos: prebetico interno, dominio intermedio, subbetico externo, subbetico medio y subbetico interno. Se ha dedicado especial atencion a los tres dominios de la zona subbeticas que estuvieron controlados por los procesos de fracturacion durante gran parte del jurasico y del cretacico, lo que favorecio la individualizacion de las unidades tectonicas. La paleogeografia de este sector se ajusta a un modelo de umbrales y surcos individualizados durante el jurasico y que presentan un comportamiento mas homogeneo durante el cretacico.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La cuenca subbetica mesozoica en el sector oriental de las cordilleras beticas.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La cuenca subbetica mesozoica en el sector oriental de las cordilleras beticas. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Nieto Albert Luis Miguel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Pedro Alejandro Ru\u00edz Ort\u00edz<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Antonio Vera Torres <\/li>\n<li>Antonio Estevez  Rubio (vocal)<\/li>\n<li>Lorenzo Vilas Minondo (vocal)<\/li>\n<li>Roque Aguado Merlo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Nieto Albert Luis Miguel En esta memoria se estudia la estratigrafia y sedimentolog\u00eda de los materiales del [&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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