{"id":76505,"date":"2005-01-10T00:00:00","date_gmt":"2005-01-10T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-petrologico-del-complejo-plutonico-de-valencia-del-ventoso-badajoz\/"},"modified":"2005-01-10T00:00:00","modified_gmt":"2005-01-10T00:00:00","slug":"estudio-petrologico-del-complejo-plutonico-de-valencia-del-ventoso-badajoz","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/geologia-estructural\/estudio-petrologico-del-complejo-plutonico-de-valencia-del-ventoso-badajoz\/","title":{"rendered":"Estudio petrol\u00f3gico del complejo plut\u00f3nico de Valencia del ventoso (badajoz)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Fernando Sarrionandia Eguidazu <\/strong><\/h2>\n<p>El complejo plut\u00f3nico de Valencia del ventoso est\u00e1 emplazado en el n\u00facleo del antiforma de monesterio, zona de ossa morea. Este macizo est\u00e1 integrado por los stocks de medina de las torres (smt), Valencia del ventoso (svv) y pozuelo (sp), por el plut\u00f3n de Valencia del ventoso (pvv) y dos cortejos filonianos diferentes, uno procedente de los l\u00edquidos m\u00e1s evolucionados de los cuerpos plut\u00f3nicos y otro con mayor desarrollo que atraviesa el cpvv, extendi\u00e9ndose por el encajante. En el pvv, que intruye a los stocks, se diferencia en la parte central una unidad b\u00e1sica (ub), que est\u00e1 rodeada e intruida por una unidad \u00e1cida (uca).     los stocks integran facies b\u00e1sicas e intermedias que muestran estructuras masivas y acumulativas. Son rocas caf\u00e9micas calcoalcalinas magnesianas con neta tendencia monzon\u00edtica y contenidos medios a altos en k. La ub integra gabros y cuarzodioritas moderadamente alcalinos, caf\u00e9micos monzon\u00edticos ricos en k, que definen asociaciones magnesianas a ligeramente ferr\u00edferas. La ua est\u00e1 constituida por rocas intermedias a \u00e1cidas, caf\u00e9micas monozn\u00edticas ferr\u00edferas y con contenidos altos en k. Las aplitas s.L.Tambi\u00e9n se integran n la serie definida pro los stocks y la ua, aunque en ellas prevalece el car\u00e1cter peraluminoso.     el conjunto de manifestaciones filonianas no restringidas espacialmente al cpvv incluye una gran variedad de litolog\u00edas moderadamente alcalinas, que forman un asociaci\u00f3n caf\u00e9mica monzon\u00edtica ferr\u00edfera, con contenidos en k moderados a shoshniticos.     el cpvv proviene de la fusi\u00f3n de una lherzolita con espinela modificada por fluidos y fundidos derivados de la corteza oce\u00e1nica y de los sedimentos subducidos. Una fuerte alterantiva es la mezcla de una lherzolita con espinela + anfibolitas + sedimentos (e.G. 8:1:1). El origen de esta fuente esta \u00edntimamente relacionada con la subducci\u00f3n devono-carbon\u00edfera. Variaciones en las condiciones de fusi\u00f3n dan lugar a dos tipos de magmas parentales; un<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio petrol\u00f3gico del complejo plut\u00f3nico de Valencia del ventoso (badajoz)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio petrol\u00f3gico del complejo plut\u00f3nico de Valencia del ventoso (badajoz) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Fernando Sarrionandia Eguidazu <\/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 01\/10\/2005<\/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>Manuel Carracedo S\u00e1nchez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  ignacio Gil ibarguchi <\/li>\n<li>Andr\u00e9s Cuesta fern\u00e1ndez (vocal)<\/li>\n<li>Carlos Villaseca gonzalez (vocal)<\/li>\n<li> Garc\u00eda lob\u00f3n Jos\u00e9 Luis (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Fernando Sarrionandia Eguidazu El complejo plut\u00f3nico de Valencia del ventoso est\u00e1 emplazado en el n\u00facleo del antiforma [&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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