{"id":47954,"date":"2020-07-17T00:55:37","date_gmt":"2020-07-17T00:55:37","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/sedimentologia-y-diagenesis-del-cretacico-superior-de-la-mancha-prov-de-cuenca\/"},"modified":"2020-07-17T00:55:37","modified_gmt":"2020-07-17T00:55:37","slug":"sedimentologia-y-diagenesis-del-cretacico-superior-de-la-mancha-prov-de-cuenca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/sedimentologia-y-diagenesis-del-cretacico-superior-de-la-mancha-prov-de-cuenca\/","title":{"rendered":"Sedimentolog\u00eda y diagenesis del cretacico superior de la mancha (prov. de cuenca)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Carlos Fernandez Calvo <\/strong><\/h2>\n<p>Se ha estudiado el cretacico superior de la mancha integrado fundamentalmente por materiales carbonaticos habiendose analizado tanto las caracteristicas sedimentologicas como las diageneticas sobre impuestas.  petrograficamente se han caracterizado las microfacies significativas de cada unidad diferenciada  como base de las interpretaciones sedimentologicas.  los procesos diageneticos mas importantes que se describen son: dolomitizacion dedolomitizacion silicificacion y brechificacion.  finalmente se han caracterizado una serie de unidades lifoestratigraficas informales de facil reconocimiento sobre el terreno.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Sedimentolog\u00eda y diagenesis del cretacico superior de la mancha (prov. de cuenca).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Sedimentolog\u00eda y diagenesis del cretacico superior de la mancha (prov. de cuenca). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Carlos Fernandez Calvo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1981<\/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> Pe\u00f1a Blasco Jos\u00e9 Andr\u00e9s De La<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Bermudo Melendez Melendez <\/li>\n<li> Fuster Casas  Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li>Juan Rosell Sanuy (vocal)<\/li>\n<li>  (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Carlos Fernandez Calvo Se ha estudiado el cretacico superior de la mancha integrado fundamentalmente por materiales carbonaticos [&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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