{"id":140631,"date":"2026-01-12T17:56:20","date_gmt":"2026-01-12T17:56:20","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/variacion-del-estilo-estructural-en-el-hercinico-del-pirineo-infraestructura-z-transicion-supraestructura\/"},"modified":"2026-01-12T17:56:20","modified_gmt":"2026-01-12T17:56:20","slug":"variacion-del-estilo-estructural-en-el-hercinico-del-pirineo-infraestructura-z-transicion-supraestructura","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/variacion-del-estilo-estructural-en-el-hercinico-del-pirineo-infraestructura-z-transicion-supraestructura\/","title":{"rendered":"Variacion del estilo estructural en el hercinico del pirineo. infraestructura-z. transicion-supraestructura."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Ignasi Capella Sola <\/strong><\/h2>\n<p>El hercinico del pirineo presenta una zonacion estructural definida por la existencia en los niveles profundos del orogeno. Por la disposicion horizontal de las estructuras de caracter dominante, y subvertical para las que configuran los niveles superficiales. Zonaciones similares han estado reconocidas en otros orogenos.  la configuracion de la zonacion antes definida seria el resultado de la superporcion de dos intervalos deformativos asociados a regimenes tectonicos deformativos diferentes. El primero correspondria a una mixta de componente sud. Y se manifestaria en los sectores profundos del orogeno. El segundo responsable de la zonacion definida, seria principalmente una compresion n-s.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Variacion del estilo estructural en el hercinico del pirineo. infraestructura-z. transicion-supraestructura.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Variacion del estilo estructural en el hercinico del pirineo. infraestructura-z. transicion-supraestructura. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Ignasi Capella Sola <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/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>Jordi Carreras Planells<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Manuel Julivert Casagualda <\/li>\n<li>Antonio Estevez  Rubio (vocal)<\/li>\n<li>Philippe Matte (vocal)<\/li>\n<li> Casas Tuset Josep M. (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Ignasi Capella Sola El hercinico del pirineo presenta una zonacion estructural definida por la existencia en los [&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":[27,953,19202],"tags":[19204,116045,255276,87256,21743,185201],"class_list":["post-140631","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-regional","tag-antonio-estevez-rubio","tag-casas-tuset-josep-m","tag-ignasi-capella-sola","tag-jordi-carreras-planells","tag-manuel-julivert-casagualda","tag-philippe-matte"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/140631","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=140631"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/140631\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=140631"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=140631"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=140631"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}