{"id":51263,"date":"2021-08-20T06:08:30","date_gmt":"2021-08-20T06:08:30","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-metamorfica-del-sector-centro-septentrional-de-la-sierra-de-guadarrama\/"},"modified":"2021-08-20T06:08:30","modified_gmt":"2021-08-20T06:08:30","slug":"evolucion-metamorfica-del-sector-centro-septentrional-de-la-sierra-de-guadarrama","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-metamorfica-del-sector-centro-septentrional-de-la-sierra-de-guadarrama\/","title":{"rendered":"Evolucion metamorfica del sector centro-septentrional de la sierra de guadarrama."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Carlos Villaseca Gonzalez <\/strong><\/h2>\n<p>Con caracter de penetratividad en los niveles de la serie femica heterogenea  compuesta por tramos metapeliticos metacarbonatados y cuerpos metabasiticos circunscriptos se emplazan en tiempos preordovicicos una serie de ortogneises cuarzofeldespaticos  desde terminos granodioriticos (gneises subplagioclasicos) a leucograniticos (leucogneises). La orografia hercinica que los afecta  se inicia con una etapa metamorfica de bajo gradiente geotermico  de presion intermedia. El comportamiento ductil de volumenes importantes de roca facilito la elevacion de la zona axial de la cadena evolucionado a un metamorfismo de alto gradiente geotermico. La disipacion del flujo termico provoca un metamorfismo retrogado final  que sustituye parcialmente las paragenesis anteriores. La generacion de magmas anatecticos en niveles mesocorticales adyacentes  y su emplazamiento desde momentos finiparoxismales  provoca una serie de estructuras migmatiticas o macizos inhomogeneos  que representan la culminacion local del metamorfismo en niveles hidratados.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion metamorfica del sector centro-septentrional de la sierra de guadarrama.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion metamorfica del sector centro-septentrional de la sierra de guadarrama. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Carlos Villaseca Gonzalez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1983<\/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> Fuster Casas Jos\u00e9 M.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Manuel Alia Medina <\/li>\n<li> Fuster Casas Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li>Carlos Garcia Figuerola (vocal)<\/li>\n<li>Ramon Capote Del Villar (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Carlos Villaseca Gonzalez Con caracter de penetratividad en los niveles de la serie femica heterogenea compuesta por [&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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