{"id":89874,"date":"2018-03-10T00:15:09","date_gmt":"2018-03-10T00:15:09","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-geodinamica-poliorogenica-de-los-dominios-septentrionales-de-la-zona-de-ossa-morena\/"},"modified":"2018-03-10T00:15:09","modified_gmt":"2018-03-10T00:15:09","slug":"evolucion-geodinamica-poliorogenica-de-los-dominios-septentrionales-de-la-zona-de-ossa-morena","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-geodinamica-poliorogenica-de-los-dominios-septentrionales-de-la-zona-de-ossa-morena\/","title":{"rendered":"Evolucion geodinamica poliorogenica de los dominios septentrionales de la zona de ossa-morena"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Alberto Bandres Martinez <\/strong><\/h2>\n<p>El dominio de obejo-valsequillo-puebla de la reina (dovpr) se situa dentro de la banda de cizalla de badajoz-cordoba en su sector m\u00e1s septentrional. en este dominio afloran litolog\u00edas precambricas comparables con las series de los dominios meridionales de la zom, si bien su organizaci\u00f3n litoestratigrafica y su naturaleza son diferentes.  se han realizado una serie de cartografias detalladas, enfocadas desde el punto de vista estructural de los principales afloramientos de rocas preordovicicas asi como del sector de fuente obejuna, dentro del corredor blastomilonitico de badajoz-cordoba(cbbc). El objetivo de este trabajo ha sido el estudio de las unidades precambricos desde el punto de vista litoestratigrafico,petrologico, geoquimico y estructural. De igual forma se ha establecido la estructura general de los sectores estudiados, los cuales han sido deformados durante la orogenia cadomiense y varisca, en un marco geodinamico poliorogenico.  los principales afloramientos de rocas precambricas, fundamentalmente constituidos por dioritoides y rocas intermedias-acidas subordinadas se han denominado macizos. Con este termino se hace referencia al hecho de que estas rocas estan individualizadas tectonicamente y definen estructuras tectonicas bien diferenciadas en cartografia. Los principales cuerpos de rocas precambricas que afloran en el dovpr y que han sido estudiados en el presente trabajo son (de este a oeste): el hoyo-el entredicho, valsequillo, macizo de valle de la serena, estructura de palomas-puebla de la reina, vulcanitas de oliva de merida y macizo de merida. De forma complementaria se han recnocido otras secciones y cuerpos en donde afloran rocas precambricas (granitoide de el escribano y serie negra de villar del rey-la roca de la sierra).  por tanto en concordancia con otras interpretaciones propuestas, la evolucion de este sector podemos subdividirla en las siguientes etapas:  1.- Subducci\u00f3n cadomiense y formacion del arco<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion geodinamica poliorogenica de los dominios septentrionales de la zona de ossa-morena<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion geodinamica poliorogenica de los dominios septentrionales de la zona de ossa-morena <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Alberto Bandres Martinez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Pa\u00eds vasco\/euskal herriko unibertsitatea<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 24\/04\/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>Luis Equiluz Alarcon<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  ignacio Gil ibarguchi <\/li>\n<li>Jos\u00e9 Brandao silva (vocal)<\/li>\n<li> Gonzalo corral Juan  Carlos (vocal)<\/li>\n<li>Antonio Castro dorado (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alberto Bandres Martinez El dominio de obejo-valsequillo-puebla de la reina (dovpr) se situa dentro de la banda [&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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