{"id":26985,"date":"2018-03-09T09:19:03","date_gmt":"2018-03-09T09:19:03","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/recristalizacion-y-deformacion-de-litologa%c2%adas-supracorticales-sometidas-a-metamorfismo-de-alta-presion-complejo-de-malpica-tuy-no-del-macizo-iberico\/"},"modified":"2018-03-09T09:19:03","modified_gmt":"2018-03-09T09:19:03","slug":"recristalizacion-y-deformacion-de-litologa%c2%adas-supracorticales-sometidas-a-metamorfismo-de-alta-presion-complejo-de-malpica-tuy-no-del-macizo-iberico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/pais-vasco-euskal-herriko-unibertsitatea\/recristalizacion-y-deformacion-de-litologa%c2%adas-supracorticales-sometidas-a-metamorfismo-de-alta-presion-complejo-de-malpica-tuy-no-del-macizo-iberico\/","title":{"rendered":"Recristalizaci\u00f3n y deformaci\u00f3n de litolog\u00edas supracorticales sometidas a metamorfismo de alta presi\u00f3n (complejo de malpica-tuy, no del macizo ib\u00e9rico)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Javier Rodr\u00edguez Aller <\/strong><\/h2>\n<p>El complejo al\u00f3ctono de malpica-tuy representa un fragmento de corteza superior del supercontinente gondwana, que fue transportado hasta profundidades mant\u00e9licas (c.90 km) durante la orogenia varisca (380-385 ma). Este proceso de subducci\u00f3n produjo una recristalizaci\u00f3n incompleta de las litolog\u00edas corticoles, caracterizada por microestructuras coron\u00edticas y pseudom\u00f3rficas que evidencian una ausencia de deformaci\u00f3n y una escasez de fluidos durante la subducci\u00f3n continental.  la exhumaci\u00f3n de este bloque cortical metaestable en condiciones mant\u00e9licas conllev\u00f3 la deformaci\u00f3n progresiva de los materiales y su reequilibraci\u00f3n durante varias etapas: d1 en condiciones eclog\u00edticas (365-370 ma), d2 en facies de las anfibolitas con epidota (340-345 ma), y d3 en facies de los esquistos verdes (330 ma). Los criterios cinem\u00e1ticos indican que la exhumaci\u00f3n se produjo de n a s (en coordenadas actuales).  el final de la exhumaci\u00f3n marca el comienzo del magmatismo varisco regional en dos etapas, una sintect\u00f3nica (310-325 ma) y otra postect\u00f3nica (285-295 ma).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Recristalizaci\u00f3n y deformaci\u00f3n de litolog\u00edas supracorticales sometidas a metamorfismo de alta presi\u00f3n (complejo de malpica-tuy, no del macizo ib\u00e9rico)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Recristalizaci\u00f3n y deformaci\u00f3n de litolog\u00edas supracorticales sometidas a metamorfismo de alta presi\u00f3n (complejo de malpica-tuy, no del macizo ib\u00e9rico) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Javier Rodr\u00edguez Aller <\/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 21\/11\/2003<\/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>Juan  Ignacio Gil Ibarguchi<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Peinado moreno Mar\u00eda mercedes <\/li>\n<li>roberto Compagnoni (vocal)<\/li>\n<li>ricardo Arenas mart\u00edn (vocal)<\/li>\n<li> Tub\u00eda mart\u00ednez Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Javier Rodr\u00edguez Aller El complejo al\u00f3ctono de malpica-tuy representa un fragmento de corteza superior del supercontinente gondwana, [&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":[12909],"tags":[77735,9064,77736,21744,35796,25322],"class_list":["post-26985","post","type-post","status-publish","format-standard","hentry","category-pais-vasco-euskal-herriko-unibertsitatea","tag-javier-rodriguez-aller","tag-juan-ignacio-gil-ibarguchi","tag-peinado-moreno-maria-mercedes","tag-ricardo-arenas-martin","tag-roberto-compagnoni","tag-tubia-Martinez-jose-maria"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/26985","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=26985"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/26985\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=26985"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=26985"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=26985"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}