{"id":51386,"date":"2021-09-09T02:11:19","date_gmt":"2021-09-09T02:11:19","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-geologia-del-area-esquistosa-de-galicia-central-cordillera-herciniana-nw-de-espana\/"},"modified":"2021-09-09T02:11:19","modified_gmt":"2021-09-09T02:11:19","slug":"la-geologia-del-area-esquistosa-de-galicia-central-cordillera-herciniana-nw-de-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-geologia-del-area-esquistosa-de-galicia-central-cordillera-herciniana-nw-de-espana\/","title":{"rendered":"La geolog\u00eda del area esquistosa de galicia central (cordillera herciniana, nw de espa\u00f1a)."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Marquinez Garcia Jorge  Luis <\/strong><\/h2>\n<p>En el area esquistosa de galicia central aflora una potente secuencia metasedimentaria  en la que se intercalan rocas acidas y basicas ortoderivadas  cuya edad se atribuye al silurico-devonico. Todas estas rocas han sido afectadas por una intensa deformacion  en la cual puedesn diferenciarse tres etapas principales  que va acompa\u00f1ada por metamorfismo y granitizacion  procesos que alcanzan su maxima intensidad en la interfase f2-f3.  durante la fase 2 se emplaza sobre esta zona una unidad con rocas catazonales (complejo de ordenes) representando la tercera fase de deformacion una etapa de replegamiento general que configura los rasgos principales de la estructura mayor de esta zona.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La geolog\u00eda del area esquistosa de galicia central (cordillera herciniana, nw de espa\u00f1a).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La geolog\u00eda del area esquistosa de galicia central (cordillera herciniana, nw de espa\u00f1a). <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Marquinez Garcia Jorge  Luis <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1983<\/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>Enrique Mart\u00ednez Garc\u00eda<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Enrique Mart\u00ednez Garc\u00eda <\/li>\n<li> Portugal Ferreira Martin R. V. (vocal)<\/li>\n<li>Victor Garcia Due\u00f1as (vocal)<\/li>\n<li>Luis Guillermo Corretg\u00e9 Casta\u00f1\u00f3n (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Marquinez Garcia Jorge Luis En el area esquistosa de galicia central aflora una potente secuencia metasedimentaria en [&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":[27,953,3435,8846,3436],"tags":[9532,5133,62273,115244,3438],"class_list":["post-51386","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-estructural","category-oviedo","category-petrologia-ignea-y-metamorfica","tag-enrique-Martinez-garcia","tag-luis-guillermo-corretge-castanon","tag-marquinez-garcia-jorge-luis","tag-portugal-ferreira-martin-r-v","tag-victor-garcia-duenas"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/51386","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=51386"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/51386\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=51386"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=51386"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=51386"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}