{"id":129682,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-geometria-y-cinematica-del-emplazamiento-de-los-granitoides-del-area-de-la-alberca-bejar-sistema-central-espanol-zona-centro-iberica\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"estructura-geometria-y-cinematica-del-emplazamiento-de-los-granitoides-del-area-de-la-alberca-bejar-sistema-central-espanol-zona-centro-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-geometria-y-cinematica-del-emplazamiento-de-los-granitoides-del-area-de-la-alberca-bejar-sistema-central-espanol-zona-centro-iberica\/","title":{"rendered":"Estructura, geometria y cinematica del emplazamiento de los granitoides del area de la alberca-bejar (sistema central espa\u00f1ol, zona centro iberica)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Mar\u00eda no Yenes Ortega <\/strong><\/h2>\n<p>Se ha realizado un estudio detallado de los granitoides y de su encajante proximo, en el area granitica de la alberca-bejar, localizada en el extremo noroccidental del sistema central espa\u00f1ol. Se han estudiado los siguientes aspectos:  en los granitoides se realizo un estudio estructural utilizando tecnicas geofisicas (anisotropia magnetica y gravimetria). Ademas se realizo un analisis de las estructuras a nivel de afloramiento y microscopico.  en el encajante metamorfico se han determinado los efectos termales y deformativos provocados por la intrusion de los granitoides.  tambien se ha obtenido una datacion absoluta de las rocas igneas, mediante el metodo k-ar en biotitas. Confirmando una edad de emplazamiento posterior a la segunda fase de deformacion regional, es decir, en el permico inferior.  los resultados obtenidos han permitido establecer la relacion temporal de los granitoides con las fases de deformacion regional y construir cortes geologicos detallados, a partir de los datos estructurales y de la geometria de las rocas igneas.  finalmente se propone un modelo de ascension y emplazamiento de los plutones estudiados que puede ser aplicado a otros plutones tardicinematicos del sistema central espa\u00f1ol.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructura, geometria y cinematica del emplazamiento de los granitoides del area de la alberca-bejar (sistema central espa\u00f1ol, zona centro iberica)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructura, geometria y cinematica del emplazamiento de los granitoides del area de la alberca-bejar (sistema central espa\u00f1ol, zona centro iberica) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Mar\u00eda no Yenes Ortega <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Fernando Alvarez Lobato<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Tubia Martinez Jos\u00e9 Mar\u00eda <\/li>\n<li>Louis Vigneresse Jean (vocal)<\/li>\n<li>Luc Bouchez Jean (vocal)<\/li>\n<li>Jes\u00fas Aller Manrique (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mar\u00eda no Yenes Ortega Se ha realizado un estudio detallado de los granitoides y de su encajante [&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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