{"id":10801,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1996\/01\/01\/evolucion-petrologica-y-geoquimica-de-los-esquistos-maficos-del-complejo-nevado-filabride-cordilleras-beticas-espana\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"evolucion-petrologica-y-geoquimica-de-los-esquistos-maficos-del-complejo-nevado-filabride-cordilleras-beticas-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-petrologica-y-geoquimica-de-los-esquistos-maficos-del-complejo-nevado-filabride-cordilleras-beticas-espana\/","title":{"rendered":"Evolucion petrologica y geoquimica de los esquistos maficos del complejo nevado-filabride. cordilleras beticas, espa\u00f1a."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Molina Palma Jos\u00e9 Francisco <\/strong><\/h2>\n<p>La composicion quimica de las rocas maficas del complejo nevado-filabride menos metamorfizadas pone de manifiesto que se han generado a partir de magmas alcalino-transicionales que intruyeron en un margen continental adelgazado.Por otra parte, los datos de elementos traza de las fases minerales de la asociacion eclogitica, obtenidos por ablacion laser, sugieren procesos metasomaticos de elementos de alto potencial ionico, considerados clasicamente como inmoviles.Esta rocas han sufrido una intensa blastesis metamorfica durante la orogenia alpina. Los estudios efectuados utilizando tecnicas algebraicas y programas de calculo termodinamico ponen de manifiesto variaciones regionales en el grado metamorfico que son compatibles con un adelgazamiento cortical tras la colision continental durante la que se desarrollaron las asociaciones metamorficas de mayor presion y relativamente baja temperatura.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion petrologica y geoquimica de los esquistos maficos del complejo nevado-filabride. cordilleras beticas, espa\u00f1a.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion petrologica y geoquimica de los esquistos maficos del complejo nevado-filabride. cordilleras beticas, espa\u00f1a. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Molina Palma Jos\u00e9 Francisco <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/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 Bea Barredo<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Mu\u00f1oz Garcia M. Mercedes <\/li>\n<li>Stefano Poli (vocal)<\/li>\n<li>Juan  Ignacio Gil Ibarguchi (vocal)<\/li>\n<li>Ricardo Arenas Martin (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Molina Palma Jos\u00e9 Francisco La composicion quimica de las rocas maficas del complejo nevado-filabride menos metamorfizadas pone [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,16139,953,3831,3436],"tags":[3935,9064,35760,3936,21744,35761],"class_list":["post-10801","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-distribucion-de-oligoelementos","category-geologia","category-geoquimica","category-petrologia-ignea-y-metamorfica","tag-fernando-bea-barredo","tag-juan-ignacio-gil-ibarguchi","tag-molina-palma-jose-francisco","tag-munoz-garcia-m-mercedes","tag-ricardo-arenas-martin","tag-stefano-poli"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/10801","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=10801"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/10801\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=10801"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=10801"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=10801"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}