{"id":133824,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-del-borde-meridional-de-la-zona-centroiberica-y-su-relacion-con-el-contacto-entre-las-zonas-centroiberica-y-de-ossa-morena\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"estructura-del-borde-meridional-de-la-zona-centroiberica-y-su-relacion-con-el-contacto-entre-las-zonas-centroiberica-y-de-ossa-morena","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-del-borde-meridional-de-la-zona-centroiberica-y-su-relacion-con-el-contacto-entre-las-zonas-centroiberica-y-de-ossa-morena\/","title":{"rendered":"Estructura del borde meridional de la zona centroiberica y su relacion con el contacto entre las zonas centroiberica y de ossa-morena."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Martinez Poyatos David Jes\u00fas <\/strong><\/h2>\n<p>Se establecen por primera vez y de forma coherente la estructura, cinematica y edad de las deformaciones geologicas reconocidas en el borde meridional de la zona centroiberica. La evolucion preordovicica consiste en las discordancias cadomiense, intraalcudiense y sardica, y se estudia geoquimicamente el magmatismo finiprecambrico.  las deformaciones variscas se integran en un modelo de evolucion del limite entre las zonas centroiberica y de ossa-morena, que incluye tres etapas. Una precarbonifera de engrosamiento cortical produce grandes pliegues tumbados vergentes al ne con un cizallamiento simple ductil asociado. Durante el carbonifero inferior se produce una extension hacia el n, con componente lateral izquierda; en este contexto se explican la sedimentacion sinogenica de facies \u00abculm\u00bb y el magamtismo existente.  durante el carbonifero medio tiene lugar la inversion de las estructuras previas, produciendose un cabalgamiento hacia el ne de la unidad de pliegues tumbados y, posteriormente, un reapretamiento de toda la region mediante pliegues levantados.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructura del borde meridional de la zona centroiberica y su relacion con el contacto entre las zonas centroiberica y de ossa-morena.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructura del borde meridional de la zona centroiberica y su relacion con el contacto entre las zonas centroiberica y de ossa-morena. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Martinez Poyatos David Jes\u00fas <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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> Simancas Cabrera Jos\u00e9 Fernando<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Alberto Marcos Vallaure <\/li>\n<li> Martinez Catalan Jos\u00e9 Ramon (vocal)<\/li>\n<li>Andr\u00e9s Perez Estaun (vocal)<\/li>\n<li> Diez Balda Mar\u00eda  Antonia (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Martinez Poyatos David Jes\u00fas Se establecen por primera vez y de forma coherente la estructura, cinematica y [&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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