{"id":25959,"date":"2018-03-09T09:17:33","date_gmt":"2018-03-09T09:17:33","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/modelos-de-sedimentacion-deltaica-en-las-cuencas-neogenas-de-la-cordillera-betica-sectores-central-y-oriental\/"},"modified":"2018-03-09T09:17:33","modified_gmt":"2018-03-09T09:17:33","slug":"modelos-de-sedimentacion-deltaica-en-las-cuencas-neogenas-de-la-cordillera-betica-sectores-central-y-oriental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/modelos-de-sedimentacion-deltaica-en-las-cuencas-neogenas-de-la-cordillera-betica-sectores-central-y-oriental\/","title":{"rendered":"Modelos de sedimentaci\u00f3n deltaica en las cuencas ne\u00f3genas de la cordillera b\u00e9tica (sectores central y oriental)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Fernando Garc\u00eda Garc\u00eda <\/strong><\/h2>\n<p>En las cuencas ne\u00f3geno-cuaternarias de la cordillera b\u00e9tica se desarrollaron numerosos sistemas deltaicos marinos de grano grueso en diferentes contextos tect\u00f3nicos, eust\u00e1ticos y clim\u00e1ticos, cuyo desarrollo fue especialmente importante en el tortoniense superior y el plioceno inferior.  se estudian ejemplos de sistemas deltaicos de las cuencas de granada, guadix, tabernas, campo de dal\u00edas y corredor del andarax.  los sistemas deltaicos tortonienses del borde oriental de la cuenca de granada, en la cuenca de guadix (bodurria y lopera), y en la cuenca de tabernas (alboloduy), tienen en com\u00fan que las cuencas de drenaje de sus sistemas alimentadores est\u00e1n instaladas sobre los relieves de sierra nevada y sierra de filabres.  el sistema tortoniense de alic\u00fan se alimenta de los relieves subb\u00e9ticos del borde norte de la cuenca de guadix. Los sistemas deltaicos pliocenos de alhama de almer\u00eda y adra tienen instaladas, al menos parcialmente, las cuencas de drenaje de sus sistemas alimentadores sobre los relieves de sierra de g\u00e1dor. La descripci\u00f3n de la organizaci\u00f3n secuencial, patr\u00f3n de apilamiento, arquitectura estratigr\u00e1fica y asociaciones de facies de cada uno de los ejemplos permite establecer modelos deltaicos y discutir los principales factores autoc\u00edclicos que controlan la sedimentaci\u00f3n. Tras la correlaci\u00f3n de los ejemplos tortonienses, por un lado, y los pliocenos, por otro, se establecen los factores aloc\u00edclicos que controlaron la sedimentaci\u00f3n deltaica: tect\u00f3nica regional, eustatismo y clima.  los deltas tortonienses se desarrollan en un ciclo transgresivo-regresivo de 4\u00c2\u00ba orden (el intervalo de tiempo que representa es de pocos cientos de miles de a\u00f1os).  en la etapa transgresiva del ciclo se depositaron los deltas de albloduy y las tres primeras secuencias deltaicas de bodurria.  en la etapa regresiva se han diferenciado dos fases de regresi\u00f3n normal separadas por un evento de ca\u00edda relativa del nivel del m<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Modelos de sedimentaci\u00f3n deltaica en las cuencas ne\u00f3genas de la cordillera b\u00e9tica (sectores central y oriental)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Modelos de sedimentaci\u00f3n deltaica en las cuencas ne\u00f3genas de la cordillera b\u00e9tica (sectores central y oriental) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Fernando Garc\u00eda Garc\u00eda <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 29\/09\/2003<\/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>Juan Fernandez Martinez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Antonio Vera torres <\/li>\n<li>pedro alejandro Ru\u00edz ort\u00edz (vocal)<\/li>\n<li>Mar\u00eda no Marzo carpio (vocal)<\/li>\n<li>Jes\u00fas Soria mingorance (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Fernando Garc\u00eda Garc\u00eda En las cuencas ne\u00f3geno-cuaternarias de la cordillera b\u00e9tica se desarrollaron numerosos sistemas deltaicos marinos [&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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