{"id":155058,"date":"2026-01-12T17:16:41","date_gmt":"2026-01-12T17:16:41","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-trias-de-facies-germanica-del-sector-central-de-la-cordillera-betica\/"},"modified":"2026-01-12T17:16:41","modified_gmt":"2026-01-12T17:16:41","slug":"el-trias-de-facies-germanica-del-sector-central-de-la-cordillera-betica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-trias-de-facies-germanica-del-sector-central-de-la-cordillera-betica\/","title":{"rendered":"El trias de facies germanica del sector central de la cordillera betica."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Perez Lopez Alberto Diego <\/strong><\/h2>\n<p>Se realiza un estudio de la estratigrafia del trias de facies germanica del sector central de la zona subbetica (trias sudiberico), habiendose procedido a la reconstruccion de la columna estratigrafica original de la sucesion triasica, muy perturbada por la tectonica alpina en este sector. Se ha procedido a la datacion mediante bivalvos, polen, restos de macroflora y foraminiferos de diferentes niveles de la serie, a la diferenciacion de unidades litoestratigraficas en el muschelkalk y el keuper, al analisis de las facies y a la proposicion de un modelo de evolucion sedimentaria en terminos de estratigrafia secuencial. Asimismo se ha reconocido la estructura de los materiales triasicos, que se caracteriza por un marcado caracter caotico, debido sobre todo a la tectonica de despegue de la cobertera postriasica subbetica y a la actuacion de procesos de resedimentacion por gravedad. Finalmente se ha propuesto un modelo de reconstruccion paleogeografica del trias sudiberico.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El trias de facies germanica del sector central de la cordillera betica.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El trias de facies germanica del sector central de la cordillera betica. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Perez Lopez Alberto Diego <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1991<\/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:  Sanz De Galdeano Equiza  Carlos <\/li>\n<li>Francesc Calvet Rovira (vocal)<\/li>\n<li>Federico Orti Cabo (vocal)<\/li>\n<li>Ana Marquez Aliaga (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Perez Lopez Alberto Diego Se realiza un estudio de la estratigrafia del trias de facies germanica del [&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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