{"id":88879,"date":"2018-03-10T00:13:55","date_gmt":"2018-03-10T00:13:55","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-de-poblaciones-de-fallas-en-el-extremo-suroccidental-de-la-pena%c2%adnsul-iberica\/"},"modified":"2018-03-10T00:13:55","modified_gmt":"2018-03-10T00:13:55","slug":"analisis-de-poblaciones-de-fallas-en-el-extremo-suroccidental-de-la-pena%c2%adnsul-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/analisis-de-poblaciones-de-fallas-en-el-extremo-suroccidental-de-la-pena%c2%adnsul-iberica\/","title":{"rendered":"An\u00e1lisis de poblaciones de fallas en el extremo suroccidental de la pen\u00ednsul ib\u00e9rica"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Encarnaci\u00f3n Garc\u00eda Navarro <\/strong><\/h2>\n<p>En \u00e9sta tesis se realiza un estudio de la deformaci\u00f3n fr\u00e1gil desarrollada en el extremo suroccidental del pen\u00ednsula iberica en rocas con edades comprendidas entre el wesfaliense medio-superior hasta el tr\u00edas superior-jur\u00e1sico inferior. se describen los sistemas de fallas y se aplican diversas t\u00e9cnicas, basadas en el an\u00e1lisis de poblaciones de fallas, para el c\u00e1lculo de los tensores de esfuerzo y deformaci\u00f3n relacionados con los \u00faltimos episodios de deformaci\u00f3n varisca en el suroeste del macizo ib\u00e9rico.  a partir de \u00e9stos resultados se plantean mapas de trayectoria de esfuerzo regional, concluyendose que en el extremo oriental de la zona surpotuguesa se produce una rotaci\u00f3n antihoraria de la direcci\u00f3n de esfuerzo regional desde la posici\u00f3n noreste-suroeste a otras noroeste-sueste. Estas trayectorias sufren perturbaciones en los extremos de una falla de orden mayor (la falla de el castillo de las guardas), de duci\u00e9ndose que \u00e9sta estructura tuvo una componente de desplazamiento sinistral, que evoluciona a otra de tipo dextral.Por otra parte se presentan datos de geoqu\u00edmica de una importante red de diques de diabasas que se desarrollan simult\u00e1neamente con los procesos de deformaci\u00f3n fr\u00e1gil.  durante el autuniense tiene lugar la formaci\u00f3n de la cuenca del viar y con posterioridad un episodio compresivo que modela su l\u00edmite oriental.Para \u00e9ste episodio se deduce una direcci\u00f3n ne-so para el esfuerzo m\u00e1simo horizontal.  para las rocas m\u00e1s modernas estudiadas (tr\u00edas superior-jur\u00e1sico inferior) se obtienen dos direcciones de extensi\u00f3n relacionadas con el rifting atl\u00e1ntico: la mas antigua es nne-sso y la mas reciente no-se.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>An\u00e1lisis de poblaciones de fallas en el extremo suroccidental de la pen\u00ednsul ib\u00e9rica<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 An\u00e1lisis de poblaciones de fallas en el extremo suroccidental de la pen\u00ednsul ib\u00e9rica <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Encarnaci\u00f3n Garc\u00eda Navarro <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Huelva<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 15\/02\/2001<\/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>Carlos Fern\u00e1ndez Rodr\u00edguez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: ramon Capote del villar <\/li>\n<li>Jos\u00e9 Manuel Gonz\u00e1lez casado (vocal)<\/li>\n<li>Miguel Orozco fern\u00e1ndez (vocal)<\/li>\n<li>Antonio Casas s\u00e1inz (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Encarnaci\u00f3n Garc\u00eda Navarro En \u00e9sta tesis se realiza un estudio de la deformaci\u00f3n fr\u00e1gil desarrollada en el [&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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