{"id":128996,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/arquitectura-deposicional-de-las-facies-utrillas-en-la-zona-central-de-la-cordillera-iberica\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"arquitectura-deposicional-de-las-facies-utrillas-en-la-zona-central-de-la-cordillera-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/arquitectura-deposicional-de-las-facies-utrillas-en-la-zona-central-de-la-cordillera-iberica\/","title":{"rendered":"Arquitectura deposicional de las facies utrillas en la zona central de la cordillera iberica."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Gonzalo Ruiz Cebrian <\/strong><\/h2>\n<p>En la presente tesis doctoral, se ha realizado un estudio de la fm. Arenas de utrillas en un amplio sector de la cordillera iberica. Se ha procedido a la subdivision en varios sectores, en los cuales se han levantado gran cantidad de columnas estratigraficas y sedimentologicas de detalle, y se han aplicado los metodos estratigrafico-secuenciales.  se ha comprobado que hay tres ciclos basicos de deposito de las arenas de utrillas un ciclo basal, de edad incierta, un ciclo albiense, en facies fluviales y limitado geograficamente a un sistema de cubetas, y el ciclo superior, de edad cenomaniense que se extendio por todo el surco iberico, y esta formado por facies fluvio-costeras para acabar en facies de plataforma.  se han establecido secuencias en los mismos, pudiendose comprobar que las arenas cenomanienses, estan ligadas a oscilaciones eustaticas, y las del albiense, a movimientos tecnicos con muy poca influencia del eustatismo. Esta ciclicidad, ha podido ser identificada en todas las zonas, pudiendose constatar par las arenas ligadas al ciclo cenomaniense, la existencia de ciclos de orden menor, tambien de caracter eustatico.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Arquitectura deposicional de las facies utrillas en la zona central de la cordillera iberica.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Arquitectura deposicional de las facies utrillas en la zona central de la cordillera iberica. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Gonzalo Ruiz Cebrian <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/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>Alvaro Garcia Quintana<\/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>Federico Vilas Martin (vocal)<\/li>\n<li>Alfredo Arche Miralles (vocal)<\/li>\n<li> Garcia-hidalgo Pallares Jos\u00e9 Francisco (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gonzalo Ruiz Cebrian En la presente tesis doctoral, se ha realizado un estudio de la fm. Arenas [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,986,245,953,3857],"tags":[6864,38974,16144,234556,242362,22058],"class_list":["post-128996","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-complutense-de-madrid","category-estratigrafia","category-geologia","category-sedimentologia","tag-alfredo-arche-miralles","tag-alvaro-garcia-quintana","tag-federico-vilas-martin","tag-garcia-hidalgo-pallares-jose-francisco","tag-gonzalo-ruiz-cebrian","tag-jose-ramon-mas-mayoral"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/128996","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=128996"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/128996\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=128996"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=128996"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=128996"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}