{"id":46491,"date":"2019-11-14T10:07:00","date_gmt":"2019-11-14T10:07:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-del-metamorfismo-alpino-en-el-complejo-nevado-ficabride-de-la-sierra-de-baza-cordilleras-beticas-espana\/"},"modified":"2019-11-14T10:07:00","modified_gmt":"2019-11-14T10:07:00","slug":"evolucion-del-metamorfismo-alpino-en-el-complejo-nevado-ficabride-de-la-sierra-de-baza-cordilleras-beticas-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-del-metamorfismo-alpino-en-el-complejo-nevado-ficabride-de-la-sierra-de-baza-cordilleras-beticas-espana\/","title":{"rendered":"Evolucion del metamorfismo alpino en el complejo nevado- ficabride de la sierra de baza (cordilleras beticas, espa\u00f1a)."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Gomez Pugnaire M. Teresa <\/strong><\/h2>\n<p>En el area de la sierra de baza el metamorfismo alpino ha tenido un caracter polifasico y plurifacial  resultado del cual se han producido cuatro fases de deformacion con desarrollo de pliegues y esquistosidades mas o menos penetrativas  y de blastesis. La serie de facies de la primera fase es de alta presion entanto que la de la segunda y tercera fases es de presion intermedia. La ultima fase supone un retrometamorfismo en relacion con las anteriores. Los mantos de corrimiento detectados en el area se han producido con posterioridad al metamorfismo.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion del metamorfismo alpino en el complejo nevado- ficabride de la sierra de baza (cordilleras beticas, espa\u00f1a).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion del metamorfismo alpino en el complejo nevado- ficabride de la sierra de baza (cordilleras beticas, espa\u00f1a). <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Gomez Pugnaire M. Teresa <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1980<\/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> Fontbote Mussolas Jos\u00e9 M.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Fontbote Mussolas Jos\u00e9 Mar\u00eda <\/li>\n<li>Manuel Rodr\u00edguez Gallego (vocal)<\/li>\n<li>Paolo Sassi Francesco (vocal)<\/li>\n<li>Juan  Antonio Vera Torres (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gomez Pugnaire M. Teresa En el area de la sierra de baza el metamorfismo alpino ha tenido [&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],"tags":[110061,109995,3934,35384,4220,111162],"class_list":["post-46491","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","tag-fontbote-mussolas-jose-m","tag-fontbote-mussolas-jose-maria","tag-gomez-pugnaire-m-teresa","tag-juan-antonio-vera-torres","tag-manuel-rodriguez-gallego","tag-paolo-sassi-francesco"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/46491","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=46491"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/46491\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=46491"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=46491"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=46491"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}