{"id":80259,"date":"2018-03-10T00:03:59","date_gmt":"2018-03-10T00:03:59","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-sedimentacion-en-las-rampas-carbonatadas-del-kimmeridgiense-en-las-cuencas-del-este-de-la-placa-iberica\/"},"modified":"2018-03-10T00:03:59","modified_gmt":"2018-03-10T00:03:59","slug":"la-sedimentacion-en-las-rampas-carbonatadas-del-kimmeridgiense-en-las-cuencas-del-este-de-la-placa-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-sedimentacion-en-las-rampas-carbonatadas-del-kimmeridgiense-en-las-cuencas-del-este-de-la-placa-iberica\/","title":{"rendered":"La sedimentacion en las rampas carbonatadas del kimmeridgiense en las cuencas del este de la placa iberica."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Beatriz Badenas Lago <\/strong><\/h2>\n<p>El objetivo del presente trabajo es establecer los factores que determinaron la evoluci\u00f3n sedimentaria de las rampas carbonatadas del kimmeridgiense (jur\u00e1sico superior), desarrolladas en las cuencas del este de la placa ib\u00e9rica. Para ello, se ha realizado el an\u00e1lisis estratigr\u00e1fico y sedimentol\u00f3gico de los materiales kimmeridgienses en cinco sectores, que desde el punto de vista paleogeog\u00e1fico se sit\u00faan en las zonas marginales de dichas cuencas. estos sectores son: sierra de aralar (cuenca vasco-cant\u00e1bria oriental); ricia, sierra menera-sierra palomera y sierra de albarrac\u00edn (cuenca ib\u00e9rica) y altos de chinchilla (zona de enlace entre la cuenca ib\u00e9rica y la cuenca del margen surib\u00e9rico). Dicho an\u00e1lisis ha permitido caracterizar la distribuci\u00f3n de facies y establecer el esquema estratigr\u00e1fico-secuencial de los materiales estudiados en cada sector, as\u00ed como realizar modelos de distribuci\u00f3n paleoambiental para cada una de las etapas evolutivas reconocidas.  en los sectores correspondientes al margen occidental y suroccidental de la cuenca ib\u00e9rica, los materiales depositados durante el kimmeridgiense-tit\u00f3nico basal corresponden a dos secuencias de dep\u00f3sito: secuencia kimmeridgiense-1 (subbiozona galar-kimmeridgiense superior p.P.) Y secuencia kimmeridgiense-2 (kimmeridgiense superior p.P.-Tit\u00f3nico basal). En el sector de sierra de aralar, \u00fanicamente se ha reconocido una secuencia de dep\u00f3sito que se considera equivalente a la secuencia kimmeridgiense-1. En las dos secuencias se han identificado el cortejo transgresivo y el cortejo de alto nivel del mar y, en determinados sectores, el cortejo de regresi\u00f3n forzada.  la comparaci\u00f3n de los datos obtenidos en los cinco sectores estudiados ha permitido establecer la extensi\u00f3n y el car\u00e1cter de los factores que rigieron la evoluci\u00f3n sedimentaria. Adem\u00e1s, a partir de la modelizaci\u00f3n por ordenador de las distribuciones de facies obtenidas en los sectores de ricla<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La sedimentacion en las rampas carbonatadas del kimmeridgiense en las cuencas del este de la placa iberica.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La sedimentacion en las rampas carbonatadas del kimmeridgiense en las cuencas del este de la placa iberica. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Beatriz Badenas Lago <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 29\/06\/1999<\/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>Marcos Aurell Cardona<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Antonio Vera torres <\/li>\n<li>francesc Calvet rovira (vocal)<\/li>\n<li>joaquin Villena morales (vocal)<\/li>\n<li> Garcia ramos Jos\u00e9 Carlos (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Beatriz Badenas Lago El objetivo del presente trabajo es establecer los factores que determinaron la evoluci\u00f3n sedimentaria [&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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