{"id":79056,"date":"2018-03-09T23:24:50","date_gmt":"2018-03-09T23:24:50","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-sedimentaria-del-calloviense-oxfordiense-en-el-sector-central-de-la-cordilleraiberica-rama-aragonesa\/"},"modified":"2018-03-09T23:24:50","modified_gmt":"2018-03-09T23:24:50","slug":"evolucion-sedimentaria-del-calloviense-oxfordiense-en-el-sector-central-de-la-cordilleraiberica-rama-aragonesa","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/estratigrafia\/evolucion-sedimentaria-del-calloviense-oxfordiense-en-el-sector-central-de-la-cordilleraiberica-rama-aragonesa\/","title":{"rendered":"Evoluci\u00f3n sedimentaria del calloviense-oxfordiense en el sector central de la cordilleraib\u00e9rica (rama aragonesa)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Javier Ramajo Cordero <\/strong><\/h2>\n<p>La presente tesis doctoral aborda el estudio de la sedimentaci\u00f3n durante el jur\u00e1sico medioy superior de la rama aragonesa de la cordillera ib\u00e9rica, centrandose en el estudio de losmateriales del intervalo bathoniense superior-kimmeridgiense inferior. Dentro del cual sehace especial incapie en la discontinuidad del l\u00edmite calloviense-oxfordiense yen losdepositos asociados con ooides ferruginosos asociados a este l\u00edmite, que se encuentranrepresentado en la capa de oolitos ferruginosos de arroyofr\u00edo. Se ha realizado una revisi\u00f3nde los principales afloramientos de los materiales correspondientes a este intervalotemporal, as\u00ed como una revisi\u00f3n de la unidades litoestratigr\u00e1ficas para el intervalocalloviense y oxfordiense en la rama aragonesa de la cordillera ib\u00e9rica proponiendose dosnuevas unidades con caracter de miembro, las denominadas miembro margas de talamantesy miembro. Areniscas y conglomerados del monsaterio de veruela de las fm. Sot de chera yaldealpozo respectivamente. Se han caracterizado un total de 14 facies para el intervaloestudiado, elabor\u00e1ndose una serie de mapas de facies en los que se muestra la evolucion delas mismas a lo largo del intervalo estudiado.Se ha propuesto un modelo de g\u00e9nesis de los ooides ferruginosos que postula su origen enrelacion con la emersi\u00f3n de un alto paleogeografico en el \u00e1rea del maestrazgo a partil delcual se produce aportes de fe y de minerales de la arcilla a las areas cercanas, generadoseen estas los ooides ferruginosos en condiciones marinas submareales someras siendoposteriormente redepositados en areas marinas mas profundas.El modelo de evolucion sedimentaria deducido para este intervalo parte desde condicionessomeras durante el bathoniense superior a condicones marinas m\u00e1s profundas de inundaci\u00f3nde la plataforma durante el calloviense inferior y la base del medio medio que da paso auna somerizaci\u00f3n progresiva y una caida del nivel del mar durante el calloviense superior .Durante este periodo y en relac<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evoluci\u00f3n sedimentaria del calloviense-oxfordiense en el sector central de la cordilleraib\u00e9rica (rama aragonesa)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evoluci\u00f3n sedimentaria del calloviense-oxfordiense en el sector central de la cordilleraib\u00e9rica (rama aragonesa) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Javier Ramajo Cordero <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 13\/03\/2006<\/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: Jos\u00e9 Ram\u00f3n Mas Mayoral <\/li>\n<li>Guillermo Mel\u00e9ndez Hevia (vocal)<\/li>\n<li> Mart\u00ednez Garc\u00eda-ramos Jos\u00e9 Carlos (vocal)<\/li>\n<li>Ram\u00f3n Salas Roig (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Javier Ramajo Cordero La presente tesis doctoral aborda el estudio de la sedimentaci\u00f3n durante el jur\u00e1sico medioy [&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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