{"id":39789,"date":"1999-01-01T00:00:00","date_gmt":"1999-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/las-intrusiones-plutonicas-e-hipoabisales-del-sector-meridional-del-complejo-basal-de-fuerteventura\/"},"modified":"1999-01-01T00:00:00","modified_gmt":"1999-01-01T00:00:00","slug":"las-intrusiones-plutonicas-e-hipoabisales-del-sector-meridional-del-complejo-basal-de-fuerteventura","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/las-intrusiones-plutonicas-e-hipoabisales-del-sector-meridional-del-complejo-basal-de-fuerteventura\/","title":{"rendered":"Las intrusiones plutonicas e hipoabisales del sector meridional del complejo basal de fuerteventura."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Agustina Ahijado Quintillan <\/strong><\/h2>\n<p>En este trabajo se han estudiado las caracter\u00edsticas petrol\u00f3gicas y geoqu\u00edmicas de las intrusiones plut\u00f3nicas e hipoabisales del sector meridional del complejo basal de fuerteventura (canarias). Las rocas de la serie ultram\u00e1fica inicial forman las intrusiones plut\u00f3nicas m\u00e1s antiguas (64 ma). El complejo sien\u00edtico-carbonat\u00edtico intruye en estas rocas a favor de una zona de cizalla d\u00factil-fr\u00e1gil de direcci\u00f3n ne-so de xtro-normal. Los flu\u00eddos derivados de las sienitas-carbonatitas producen una intensa fenitizaci\u00f3n. En el contacto con las meta-carbonatitas se forman microskarn con minerales ricos en sr. Tanto sienitas como carbonatitas est\u00e1n recristalizadas. Un denso complejo filoniano de direcci\u00f3n n45e atraviesa todas las rocas plut\u00f3nicas anteriores. Finalmente intruyen piroxenitas oliv\u00ednicas y gabros (serie plut\u00f3nica 3). El emplazamiento de los complejos sien\u00edtico-carbonat\u00edticos, complejo filoniano y serie plut\u00f3nica 3 tuvo lugar entre el oligoceno superior y el mioceno inferior. la signatura isot\u00f3pica (c, o y s) de las carbonatitas indica que el magma parental de estas rocas ha sufrido una asimilaci\u00f3n de carbonatos de origen sedimentario.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Las intrusiones plutonicas e hipoabisales del sector meridional del complejo basal de fuerteventura.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Las intrusiones plutonicas e hipoabisales del sector meridional del complejo basal de fuerteventura. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Agustina Ahijado Quintillan <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1999<\/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>Hernandez Pacheco Rosso De Luna Alfredo<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: eumenio Ancochea soto <\/li>\n<li>julio Nuez pestana (vocal)<\/li>\n<li>Juan Coello armenta (vocal)<\/li>\n<li>Carlos Fernandez rodriguez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Agustina Ahijado Quintillan En este trabajo se han estudiado las caracter\u00edsticas petrol\u00f3gicas y geoqu\u00edmicas de las intrusiones [&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":[27,953,3831,3436],"tags":[102136,21707,16402,102137,102139,102138],"class_list":["post-39789","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geoquimica","category-petrologia-ignea-y-metamorfica","tag-agustina-ahijado-quintillan","tag-carlos-fernandez-rodriguez","tag-eumenio-ancochea-soto","tag-hernandez-pacheco-rosso-de-luna-alfredo","tag-juan-coello-armenta","tag-julio-nuez-pestana"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/39789","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=39789"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/39789\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=39789"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=39789"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=39789"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}