{"id":142570,"date":"1993-01-01T00:00:00","date_gmt":"1993-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/plutonismo-sin-orogenico-en-un-area-hercinica-el-complejo-anatectico-de-toledo\/"},"modified":"1993-01-01T00:00:00","modified_gmt":"1993-01-01T00:00:00","slug":"plutonismo-sin-orogenico-en-un-area-hercinica-el-complejo-anatectico-de-toledo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/plutonismo-sin-orogenico-en-un-area-hercinica-el-complejo-anatectico-de-toledo\/","title":{"rendered":"Plutonismo sin-orogenico en un area hercinica: el complejo anatectico de toledo."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Barbero Gonzalez Luis Carlos <\/strong><\/h2>\n<p>El complejo anatectico de toledo esta constituido por orcas metamorficas de alto grado, fundamentalmente granulitas metapeliticas y por granitoides sin-orogenicos catazonales. Las condiciones del climax metamorfico, esencialmente sincronico con la tercera fase de deformacion del area, que se deducen el estudio del equilibrio mineral y de los calculos termodinamicos realizados tanto en las granulitas como en los gabros y granitoides precoces, quedan establecidas en 800 c, 4-5 kb, ah 0 1 y logf0 -18, es decir, condiciones granuliticas fundamentalmente anhidras y reductoras.  estos altos valores de temperatura no se pueden explicar solamente como consecuencia del apilamiento de material, sino que es necesario un aporte de calor derivado de la intrusion en momentos sin-tectonicos, de un relativamente importante magmatismo basico.  el plutonismo mas precoz esta constituido por tres grupos de rocas basicas dos de ellos de afinidad calcoalcalina y un tercero de tendencia shoshonitica. Tan solo a uno de estos grupos se le puede asignar una ascendencia mantelica directa. Este magmatismo basico esta especial y temporalmente asociado a granitoides intermedios-acidos, de los que estan, sin embargo, geneticamente desconectados.  el plutonismo peraluminico, consecuencia del generalizado proceso de anatexia del sector, esta constituido por diversas variedades petrograficas, las mas importantes de las cuales son tipos muy ricos en restitas y leucogranitos con granate y\/o cordierita de composicion semejante a la de los fundidos minimos, derivados de fusion de protolitos peliticos. Estos granitoides evolucionan mediante un mecanismo de desmezcla restita-fundido a partir de un polo restitico, constituido por las granulitas migmatiticas del area, y un polo acido formado por los mencionados leucogranitos de anatexia. La escasez de este tipo de materiales en sectores orogenicos, y en el hercinico en particular, nos lleva a la conclusion de que el<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Plutonismo sin-orogenico en un area hercinica: el complejo anatectico de toledo.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Plutonismo sin-orogenico en un area hercinica: el complejo anatectico de toledo. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Barbero Gonzalez Luis Carlos <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1993<\/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 Villaseca Gonzalez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Mercedes Mu\u00f1oz Garcia <\/li>\n<li>Felix Bellido Mulas (vocal)<\/li>\n<li>Jos\u00e9 Angel Garcia  Lopez (vocal)<\/li>\n<li>Jos\u00e9 Mar\u00eda Ugidos Meana (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Barbero Gonzalez Luis Carlos El complejo anatectico de toledo esta constituido por orcas metamorficas de alto grado, [&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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