{"id":118250,"date":"2022-05-01T06:33:03","date_gmt":"2022-05-01T06:33:03","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/los-granitoides-y-la-estructura-hercinica-en-extremadura-central\/"},"modified":"2022-05-01T06:33:03","modified_gmt":"2022-05-01T06:33:03","slug":"los-granitoides-y-la-estructura-hercinica-en-extremadura-central","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/los-granitoides-y-la-estructura-hercinica-en-extremadura-central\/","title":{"rendered":"Los granitoides y la estructura hercinica en extremadura central."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Antonio Castro Dorado <\/strong><\/h2>\n<p>En la region de extremadura central aparecen intimamente asociados trece plutones de granitoides y multitud de intrusiones menores que en conjunto constituyen el batolito de extremadura central. Todos los granitoides pueden ser agrupados en tres tipos petrograficos fundamentales: grupos a  b y c. El grupo a lo constituyen granodioritas y cuarzodioritas; el grupo b  granitoides de feldespato alcalino y el grupo c  granitoides de feldespato calcoalcalino de tendencia alcalina. Todos los plutones intruyen  con posterioridad a la primera fase de deformacion hercinica  bajo un control estructural regional deducido por la estructura interna de los granitoides y por la superposicion de estructuras en los netasedimentos encajantes. Se trata de una zona de cizalla e-w dextra que actua en profundidad (fase-ii) con un desplazamiento de mas de 64 km.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Los granitoides y la estructura hercinica en extremadura central.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Los granitoides y la estructura hercinica en extremadura central. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Antonio Castro Dorado <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1984<\/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 Garcia Figuerola<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carlos Garcia Figuerola <\/li>\n<li>Antonio Arribas Moreno (vocal)<\/li>\n<li> Fuster Casas  Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li>Luis Guillermo Corretg\u00e9 Casta\u00f1\u00f3n (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Antonio Castro Dorado En la region de extremadura central aparecen intimamente asociados trece plutones de granitoides 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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